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
37738|Accident Subgroup|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the South Nicholson Group.||||||
37738|Accident Subgroup|64443|6|Mentioned|p3-4|Calymmian|Calymmian|Of South Nicholson Group. Overlies Wild Cow Subgroup. Includes the Mittiebah Sandstone, Constance Sandstone and Mullera Formation.||||||
37738|Accident Subgroup|65336|5|Briefly described|Map Legend|Calymmian|Calymmian|Of South Nicholson Group. Includes Mittiebah Sandstone. Unconformably underlies Helen Springs Volcanics of Kalkarindji Volcanic Group.||||||
37738|Accident Subgroup|65337|3|Fully described|p v, pp50-60, p86.|Mesoproterozoic|Mesoproterozoic|400 - 3350 m thick. Sandstone-dominant basal part forms resistant ridges. Parent unit correlated with Roper Group, giving an approximate, interpreted, age. |c.1500-1400 Ma.|Unit in South Nicholson Group.|Includes Constance, Mittiebah and Tidna Sandstones and Mullera Formation.|Overlies Wild Cow Subgroup.|Fine-grained shelf tempestites and shales, and coarse-grained fluvial and shallow-marine siliciclastic rocks.|
37738|Accident Subgroup|67150|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin.||Unit in South Nicholson Group.|May include Mittiebah Sandstone.|||17-OCT-11
37738|Accident Subgroup|67352|5|Briefly described|p12-16|Calymmian|Calymmian|||South Nicholson Group|Mittiebah Sandstone|Overlies Wild Cow Subgroup||
37738|Accident Subgroup|68146|4|Described|p28, p196|||South Nicholson Basin. Fig.150 on p106 (by I. Sweet, in preparation) places the Constance Sandstone in the Wild Cow Subgroup, below an unconformity; above which the Elizabeth Sandstone Member is shown as basal Accident Subgroup but without a parent Formation.||South Nicholson Group.|Constance Sandstone, Tidna Sandstone, Mullera Formation, Elizabeth Sandstone Member. See Comments.|Unconformably overlies Wild Cow Subgroup.||
37738|Accident Subgroup|69434|4|Described|p19:2-3, 5-7|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. 400-3350m thick. The various Formations or Members interdigitate, or grade laterally and vertically into one another, over tens of kms of strike.||South Nicholson Group.|Mullera Formation, Constance and Mittiebah Sandstones; also Tidna Sandstone (in QLD).|Overlies Wild Cow Subgroup in the W and SW, conformably to unconformably. Overlies McNamara and Fickling Groups and Caulfield beds unconformably or disconformably.||12-JUL-16
37738|Accident Subgroup|69591|4|Described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). From ~1000m to ~3500m thick.||South Nicholson Group.|Elizabeth Sandstone, Mullera Formation, Tidna Sandstone.|Overlies Wild Cow Subgroup.||
37738|Accident Subgroup|69673|6|Mentioned|p56|||Minimum thickness of 400m in the NT.|||Includes Constance Sandstone, Mittiebah Sandstone, Mullera Formation|Disconformably overlies the Wild Cow Subgroup||
37738|Accident Subgroup|70968|5|Briefly described|p131 Fig.118, p132|Ectasian|Calymmian|||South Nicholson Group.|Mullera Formation; Mittiebah, Constance Sandstones.|Unconformably overlies Wild Cow Subgroup.||
37738|Accident Subgroup|71369|5|Briefly described|p1, p6, p8, p23, p36|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin.||South Nicholson Group.|Constance, Elizabeth, Tidna Sandstones; Mullera Formation.|Unconformably overlies Constance Sandstone (Wild Cow Subgroup).||
37738|Accident Subgroup|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstoen.|||
37738|Accident Subgroup|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstoen.|||
37738|Accident Subgroup|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstone.|||26-NOV-19
37738|Accident Subgroup|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 South Nicholson Group.|Includes Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Constance Sandstone.|||19-MAR-20
37738|Accident Subgroup|72418|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72421|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72422|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|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.||Unit of South Nicholson Group.|Includes Tidna Sandstone, Mullera Sandstone, Elizabeth Sandstone, Constance Sandstone.|||
37738|Accident Subgroup|72526|4|Described|p8 Fig.1.3, p33-34, p56, p67, p86.|Mesoproterozoic|Mesoproterozoic|Shown as located in the South Nicholson Basin.||South Nicholson Group|Constance Sandstone, Mittiebah Sandstone, Mullera Formation.|Shown as unconformably overlying Benmara Group and Fickling Group.|Includes sandstone and green-grey claystone, siltstone, conglomerate.|
37738|Accident Subgroup|72527|4|Described|p3, p7 Fig.1.4, p41, p193, p195-196.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Rawlings et al., (2008) describe Burangoo Sandstone Member as a constituent of the Accident Subgroup.||South Nicholson Group|Includes Buddycurrawa Volcanics, Burangoo Sandstone Member and Constance Sandstone.|Unconformably overlies Wild Cow Subgroup and unconformably underlies Bukalara Sandstone.||
37738|Accident Subgroup|72912|4|Described|p5 Fig.3, p21, p23-24, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the West, Central and East parts of the South Nicholson Basin. In the Central part of the Basin, this unit forms the entire succession and is 2km thick in total.||South Nicholson Group|Mullera Formation,Train Range Ironstone, Mittiebah Sandstone and Constance Sandstone.|Overlies Wild Cow Subgroup.|Includes ironstone, siltstone, dolomitic siltstone, sandstone.|
37738|Accident Subgroup|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west, central and eastern part of the South Nicholson Basin.||South Nicholson Group|Mittebah Sandstone, Mullera Formation and Constance Sandstone|Overlies Wildcow Subgroup.|Includes sandstone, siltstone, dolomitic siltstone, ironstone,|
37738|Accident Subgroup|72919|6|Mentioned|p5, p47, p70, p77|Mesoproterozoic|Mesoproterozoic|Includes Constance Sandstone in NT but not in QLD.||South Nicholson Group|Tidna Sandstone, Mullera Formation, Elizabeth Sandstone, Mittiebah Sandstone, Constance Sandstone|Underlain by Crow Formation, including Tobacco Member (Wild Cow Subgroup). Unconformably overlain by Bukalara Sandstone.||
37738|Accident Subgroup|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||South Nicholson Group|Mullera Formation; Mittiebah, Constance sandstones; Middle Creek Sandstone, Train Range Ironstone and Bowthorn members.|Underlain by Crow Formation and Wallis Formation. Partly overlain by Tidna Sandstone.||
37738|Accident Subgroup|73144|6|Mentioned|p8, p13|Calymmian|Calymmian|South Nicholson Basin.||South Nicholson Group|Tidna Sandstone, Mullera Formation, Middle Creek Sandstone Member, Train Range Ironstone, Elizabeth Sandstone, Constance Sandstone, Schultz Sandstone Member, Bowthorn Member|Unconformably underlain by Wallis Formation (Wild Cow Subgroup).||
28157|Adla Granulite|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
28157|Adla Granulite|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
28157|Adla Granulite|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
28157|Adla Granulite|43225|5|Briefly described|Map Legend||Paleoproterozoic|of Strangways Metamorphic Complex||||||07-NOV-08
28157|Adla Granulite|43503|5|Briefly described|6,15|||Age: 1820-1790Ma||||||
28157|Adla Granulite|48992|2|Defined|p1|Mesoproterozoic|Mesoproterozoic|Prob.Mid Proterozoic?||||||17-JUL-06
28157|Adla Granulite|69427|5|Briefly described|p12:14-15|||Forms scattered outcrops in the Burt Plain, Ankala Domain, Aileron Province.|||||Migmatitic garnet-biotite-sillimanite gneiss and mafic granulite, along with felsic granulite and rare calc-silicate rock and quartzite.|12-JUL-16
24148|Adnera Member|42504|5|Briefly described|Table 4 P73|||Reserved Haines & Bagas Dec 1987.||||||
24148|Adnera Member|42643|2|Defined|p52|late Adelaidean||of Central Mount Stuart Formation. Age latest Proterozoic (late Adelaidean)||||||
24148|Adnera Member|42644|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Central Mount Stuart Formation. Quartz arenite, feldspathic; flaggy red-brown sandstone and siltstone near top. Geological Province: Georgina Basin.||||||15-NOV-05
24148|Adnera Member|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Central Mount Stuart Formation. Red-brown, purple and white cross-bedded sandstone and quartzite, interbedded with mudstone. Geological Province: Georgina Basin.||||||
24148|Adnera Member|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Quartz arenite: feldspathic, cross-bedded.   Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
24148|Adnera Member|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of Central Mount Stuart Formation. Overlies Tops Member. Sandstone and quartzite. Contains rare trace fossils of Ediacaran type.||||||07-FEB-08
24148|Adnera Member|64068|3|Fully described|p53, p19, 52, p159.|Ediacaran|Ediacaran|Contact with Tops Member is locally sharp and erosional. Numerous, generally isolated Th radiometric anomalies.||Of Central Mount Stuart Formation, Mopunga Group.||Conformably and gradationally overlies Tops Member. Overlain with probable disconformity by Octy Formation.|Red-brown, purple and white, medium feldspathic quartz arenite and orthoquartzite; locally abundant cross-bedding; local topmost unit of sandstone and siltstone.|04-APR-12
24148|Adnera Member|65338|5|Briefly described|pp65-66.|Ediacaran|Ediacaran|72 to 310 m thick. Rare trace fossils.||Unit in Central Mount Stuart Formation.||Overlies Tops Member.|Feldspathic quartz arenite and orthoquartzite, granular sandstone; both cross-bedded; red-brown or white; local uppermost interval of interbedded red-brown sandstone and siltstone.|
24148|Adnera Member|65341|4|Described|p5, p17.|||Deposited under shallow-marine and deltaic conditions. Outcrops more strongly than Tops Member. Contains late Neoproterozoic ichnofossils.||Unit in Central Mount Stuart Formation.||Conformably overlies and grades into Tops Member.|Red-brown, purple and white crossbedded medium sandstone and quartzite, interbedded with mudstone.|
24148|Adnera Member|69443|4|Described|p28:11, 14, 35|||Georgina Basin. Shallow-marine and deltaic deposits.||Central Mount Stuart Formation.||Conformably and gradationally overlies Tops Member (probably diachronously). Is overlain by Octy Formation (probably disconformably).|Cross-bedded, medium-grained feldspathic quartz sandstone and orthoquartzite, with a local upper interval of red-brown sandstone and siltstone.|12-JUL-16
81915|Airport Porphyry|71592|5|Briefly described|Appendix A.|Orosirian|Orosirian|Tennant Creek Region.|1846+/-2.9 Ma crystallisation: U-Pb zircon SHRIMP||||Felsic porphyry.|16-JUN-20
26252|Albarta Metamorphics|39887|6|Mentioned|Fig.5|||||||||
26252|Albarta Metamorphics|39898|5|Briefly described|Map legend|Proterozoic|Proterozoic|Quartzofeldspathic gneiss, biotite and muscovite-biotite schist, massive and compositionally layered amphibolite. Geological Province: Arunta Block.||||||31-MAR-06
26252|Albarta Metamorphics|40906|6|Mentioned|p8|||||||||
26252|Albarta Metamorphics|49036|2|Defined|p2|Mesoproterozoic|Mesoproterozoic|Mid Proterozoic or older. Previously Arunta complex.||||||19-MAY-09
26252|Albarta Metamorphics|50369|6|Mentioned|p11.2|||Intruded by: Atneequa Granitic Complex.||||||
26252|Albarta Metamorphics|60549|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26252|Albarta Metamorphics|64956|5|Briefly described|p3 Tb. 1, p31|Paleoproterozoic|Paleoproterozoic|Max. intrusion age: 1771+/-3Ma; metamorphic age: 567+/-9Ma. Geol.prov: Arunta region. Contains an intrusive fine- to med.gr., weakly porphyritic biotite granite, with unknown relationships with metasediments; plus an intrusive leucogranite also.||||||07-FEB-11
26252|Albarta Metamorphics|65232|6|Mentioned|App. 2|||||||||09-FEB-10
26252|Albarta Metamorphics|65556|3|Fully described|p2 Tb.1, p14-22, p45, p46 Fig.74, p54-57||Orosirian|Aileron Province, Arunta Region. High grade metamorphics. Samples in this report are taken from migmatitic quartzo-feldspathic biotite-garnet metapsammite locally interbedded with minor garnet-cordierite metapelite; migmatitic garnet+/-cordierite metapelite, locally interbedded with quartzo-feldspathic biotite-garnet metapsammite; and gneissic granodiorite. In the eastern Arunta, the unit is bounded to the north by the Illogwa Creek Shear Zone. Exposure is fair to good. Maximum deposition age given by SHRIMP U-Pb (detrital) zircon as 1813+/-5 Ma. Magmatic crystallisation of the granodiorite is 1776 +/- 2.9 Ma. Metamorphic age of 1729+/-3 Ma by SHRIMP U-Pb monazite dating.||||||
26252|Albarta Metamorphics|66767|5|Briefly described|p58|||Aileron Province. S of the Illogwa Shear Zone.|1810-1770 Ma deposition age.||||Mid-amphibolite facies metapelitic, metapsammitic and calcsilicate rocks, and minor quartz magnetite layers.|
26252|Albarta Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block.|1771 +/- 3 Ma (maximum depositional age).|||||
26252|Albarta Metamorphics|68150|5|Briefly described|p.viii, p11 Tb.3.2, p52|||Yambah Event-aged (ca. 1770 Ma) intermediate magmatism is also present in Albarta Metamorphics (Carson et al., 2009). SHRIMP age from Casey Inlier (Carson et al. 2009). Rafts of metasedimentary rock within Atneequa Granite are likely part of Albarta Metamorphics, typically foliated calc-silicate, although appears to be relatively undeformed itself.|1729 +/- 3 Ma, metamorphic monazite|||||30-SEP-15
26252|Albarta Metamorphics|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block. Early Proterozoic? age.|||||Quartzofeldspathic gneiss, biotite and muscovite-biotite schist, massive and compositionally-layered amphibolite; minor calc-silicate rock, hornblende gneiss, magnetite-quartzite, granitic gneiss, porphyroblastic-feldspar gneiss and biotite gneiss.|
26252|Albarta Metamorphics|68697|5|Briefly described|v, p46|||Upper-amphibolite facies metamorphism occurred at 1729 +/- 3 Ma (Carson et al., 2009).|||||Includes high-grade garnet-biotite metapelite.|
26252|Albarta Metamorphics|68998|5|Briefly described|v, p1, p6-12, Appendix Tb.2|||Arunta Region. Complex age results detailed and discussed. In situ monazite was dated at 1769 +/- 7 Ma and 1749 +/- 8 Ma. The former indicates formation during the c.1780-1770 Ma Yambah Event, with the latter representing new monazite growth or resetting by the c.1750 Ma event which appears to have been regionally significant at least in the eastern Arunta region.|1769 +/- 7 Ma (monazite).||||Includes garnet metapelite.|
26252|Albarta Metamorphics|69427|4|Described|p12:30, 33-35, 37, 39, 41, 63|Statherian|Statherian|S of the Illogwa Shear Zone, Aileron Province. Metamorphism (Strangways Event) described in some detail, with metamorphic monazite dated at 1729 +/- 3 Ma (Carson et al., 2009). Is intruded by granites with a spatial association with U mineralisation at the Albarta and Tourmaline Gorge prospects. SHRIMP U-Pb zircon age. Another depositional age of 1771 +/- 9 Ma is from a quartzofeldspathic layer of volcaniclastic origin.|1776 +/- 3 Ma (Carson et al., 2009).|||Is intruded by Atneequa Suite.|Amphibolite-facies metapelitic, metapsammitic and calcsilicate rocks and minor quartz magnetite layers. Dominated in the W by foliated, locally migmatitic felsic and intermediate intrusive rocks, with lesser metagabbro and leucogranite.|12-JUL-16
26252|Albarta Metamorphics|69510|5|Briefly described|p12|||Age from garnet-hosted monazites. Upper-amphibolite-facies metamorphism dated at 1729 +/- 3 Ma (Carson et al., 2009).|1749 +/- 8 Ma (Kositcin et al., 2013).||||Includes metapelite.|
26252|Albarta Metamorphics|69917|5|Briefly described|p126-127||Orosirian|Eastern Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Biotite-garnet metapsammite sampled. Maximum depositional age is interpreted to be the youngest recognised detrital component and is reported as 1813+/-5 Ma.|1813+/-5Ma max dep age||||Migmatitic quartzo-feldspathic biotite-garnet metapsammite locally interbedded with minor amounts of garnet-cordierite metapelite.|
26252|Albarta Metamorphics|69925|6|Mentioned|p21|||Southern Arunta Province, Arunta Inlier.||||Is intruded by Atneequa Granitic Complex.||
26252|Albarta Metamorphics|69937|5|Briefly described|p12|||SE Aileron Province. Possible source of (some) zircons in Areyonga Formation.|1770-1750 Ma.|||||
26252|Albarta 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|||||
26252|Albarta Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1729+/-3 Ma (metamorphism: SHRIMP)||||Granodiorite, metapelite.|
27692|Albinia Formation|23356|5|Briefly described|26 Tab.2|Neoproterozoic|Neoproterozoic|Age: ~750Ma||||||17-JUL-06
27692|Albinia Formation|24111|5|Briefly described|p216|Neoproterozoic|Neoproterozoic|Geological Province: Ngalia Basin.  See also p215 Fig. 11.||||||
27692|Albinia Formation|37462|4|Described|Table 4.IX|||||||||
27692|Albinia Formation|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|White, thin bedded, dolomitic in part, siltstone and shale; pale grey, foetid, stromatolitic dolomite with black chert beds. Geological Province: Ngalia Basin.||||||14-FEB-06
27692|Albinia Formation|37928|6|Mentioned|Fig.4|||||||||
27692|Albinia Formation|40906|6|Mentioned|Fig.9|||||||||
27692|Albinia Formation|41717|6|Mentioned|Fig.19|||||||||
27692|Albinia Formation|42059|5|Briefly described|Fig.2|||See also p133||||||17-JUL-06
27692|Albinia Formation|42504|5|Briefly described|Table 4 P73|||||||||
27692|Albinia Formation|42643|6|Mentioned|Fig.4 P19|||||||||
27692|Albinia Formation|43275|5|Briefly described|Map Legend||Neoproterozoic|||||||
27692|Albinia Formation|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
27692|Albinia Formation|43631|3|Fully described|p23,24||Neoproterozoic|||||||
27692|Albinia Formation|43749|6|Mentioned|Fig.1,p6||Neoproterozoic|||||||
27692|Albinia Formation|44158|4|Described|p26 Table.2|Neoproterozoic|Neoproterozoic|of Ngalia Basin.||||||
27692|Albinia Formation|45155|2|Defined|p21|Adelaidean|Adelaidean|||||||
27692|Albinia Formation|46903|6|Mentioned|Fig.5|||Correlation chart||||||
27692|Albinia Formation|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mudstone, dolomitic mudstone, shale; minor stromatolitic dolostone, black chert. Geological Province: Ngalia Basin.||||||
27692|Albinia Formation|61732|6|Mentioned|p26, p131|||Contains microfossils. Geological Province: Ngalia Basin.||||||07-FEB-11
27692|Albinia Formation|64068|6|Mentioned|p44|||Ngalia Basin. Correlated with upper stromatolitic carbonate of the Yackah beds.||||||
27692|Albinia Formation|65232|5|Briefly described|p70|||Disconformably overlies 'Mount Vaughan Quartzite' [misspelling of Vaughan Springs Quartzite]; and both units underlie Naburula Formation and Rinkabeena Shale. Mudstone, dolomitic mudstone, shale. Geol. Prov: Ngalia Basin.||||||09-FEB-10
27692|Albinia Formation|65329|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Vaughan Springs Quartzite, older than Nabarula Formation. Listed as part of a combined Albinia to Mount Doreen unit of mixed lithology.||||||
27692|Albinia Formation|65330|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Vaughan Springs Quartzite, older than Nabarula Formation. Listed as part of a combined Albinia to Mount Doreen unit of mixed lithology.||||||
27692|Albinia Formation|65338|6|Mentioned|p59.|||||||Probably disconformably overlies Vaughan Springs Quartzite.||
27692|Albinia Formation|67872|5|Briefly described|p13, p15, p35, p39|Neoproterozoic|Neoproterozoic|Ngalia Basin. Part of the M1 mega-sequence of Lindsay (2002).||||Overlies Vaughan Springs Quartzite. Is overlain by Walbiri Dolomite.||
27692|Albinia Formation|68270|5|Briefly described|p683|Tonian|Tonian|Ngalia Basin.||||Unconformably overlain by Nabarula Formation. Overlies Vaughan Springs Quartzite.||03-JUL-19
27692|Albinia Formation|69437|5|Briefly described|p22:4-6, 16|Cryogenian|Cryogenian|Ngalia Basin, Centralian A Superbasin. Supersequence 1. May have petroleum source rock potential.|||||Siltstone, shale and dolostone.|12-JUL-16
27692|Albinia Formation|69439|4|Described|p24:2-4, 6-8, 13-14, 18, 20-21|Cryogenian|Cryogenian|Wells and Moss (1983). Ngalia Basin, Centralian A Superbasin. Supersequence 1. A recessive unit; poorly exposed. Inferred thickness 150-500m. Age not determined. Abundant microfossils resemble present-day intertidal to supratidal cyanobacterial mats, suggesting a depositional environment of a shallow epicontinental sea, on a shallow, low-energy marine shelf with very restricted circulation, for long periods of time. Has some hydrocarbon source rock potential.||||Transitionally or disconformably overlies Vaughan Springs Quartzite. Is overlain unconformably by Mount Doreen Formation. Correlated with Bitter Springs Formation.|Thinly interbedded grey mudstone, dolomitic mudstone and foetid black shale; ovoid dolomite nodules are characteristic. Includes a band of distinctive pale grey to black columnar stromatolitic dolostone with thinly bedded to laminated chert lenses.|12-JUL-16
27692|Albinia Formation|69443|6|Mentioned|p28:5|||Ngalia Basin.||||Correlated with Plenty Group.||12-JUL-16
27692|Albinia Formation|69673|5|Briefly described|p105, p107 fig 85|Neoproterozoic|Neoproterozoic|Up to 500m thick. Deposited in shallow tidal marine environment. Some source rock potential.||||Overlies Vaughan Springs Quartzite, overlain by Naburula Formation|Thinly interbedded mudstone, dolomitic mudstone and shale with ovoid dolomitic nodules.|
27692|Albinia Formation|72516|6|Mentioned|p86|||||||||
27692|Albinia Formation|73086|6|Mentioned|p18|||Ngalia Basin.||||Temporal correlative of Gillen Formation (Bitter Springs Group).||
76102|Alcoota beds|5030|14|Not recorded|158, 166, 167|Pliocene|Miocene|From Card file. Shown as "Alcoota beds". Contains mammalian fossils.||||||19-DEC-11
76102|Alcoota beds|43748|5|Briefly described|p17,16, Fig.7|||Waite Basin. Tertiary lacustrine and fluviatile sedimentary rocks. Up to 180 m thick. Largely known from drill holes. Basal mudstone and siltstone.||||||
76102|Alcoota beds|64068|6|Mentioned|p80|||Of Senior (1972) - BMR Record 1972/47. Part now Miocene-Pliocene Waite Formation.||||||
76102|Alcoota beds|69458|5|Briefly described|p42:11, 14|Neogene|Paleogene|Waite Basin. c.250m thick.|||Waite Formation.||Basal mudstone and siltstone, overlain by coal and lignite intervals beneath lacustrine clays; followed up-section by beds of cream or white, chalcedonic calcarenitic limestone (Waite Formation).|12-JUL-16
76102|Alcoota beds|72515|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Jervois Range Special Map Sheet. Waite Basin.|||Includes the Waite Formation.|Unconformably overlies the Cockroach Group.||
76102|Alcoota beds|72516|6|Mentioned|p11, p98|Neogene|Neogene|Waite Basin. Lacustrine and fluvial sedimentary rocks.|||Includes the Waite Formation.|||
39599|Alcurra Dolerite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolerite dykes. Geological Province: Musgrave Block.||||||
39599|Alcurra Dolerite|61154|2|Defined|p42 App., p13, p15-16, p44|Mesoproterozoic|Mesoproterozoic|Dolerite with ophitic to subophitic texture contains plagioclase. Unconformable over Dean Quartzite. Intrudes Pitjantjatjara Supersuite (Kugera Gr. and Ayers Range Gr). Intruded by Angatja Granite. Age: 1080Ma. Geol.Prov: Musgrave Block.||||||01-SEP-09
39599|Alcurra Dolerite|61524|5|Briefly described|p16|||Mafic dykes associated with the Giles Complex. Geological Province: Musgrave Province.||||||
39599|Alcurra Dolerite|61733|5|Briefly described|p46, p56|||Musgrave Block. Has subduction-related isotopic and geochemical signatures. Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|c.1.08 Ga.||||High-Mg, low-Ti tholeiites.|
39599|Alcurra Dolerite|64722|6|Mentioned|p17|Stenian|Stenian|Of a similar age to granites dated at 1080-1070 Ma.|||||Mafic tholeiitic dykes.|11-APR-12
39599|Alcurra Dolerite|64745|5|Briefly described|p376|Stenian|Stenian|Dykes. Age: ca. 1.08 Ga (Sm-Nd isochron Plag-Opx-Cpx. Zhao and McCulloch, 1993). May represent feeder system to Giles Intrusions. Geol. Prov: Musgrave Province.||||||
39599|Alcurra Dolerite|65135|6|Mentioned|p17|Stenian|Stenian|~1070 Ma. Shows geochemical similarities to Giles Event intrusives and the Warakurna Large Igneous Province.||||||
39599|Alcurra Dolerite|65369|5|Briefly described|p35|||Central Australian intraplate (flood-type) basalt.||||||19-MAR-12
39599|Alcurra Dolerite|65693|4|Described|p4,p7- p8 Fig.5, p9-12 Figs. 8-10.|||See also Alcurra Suite, Alcurra suite. Geochemistry is different from Tollu Group: detailed in text. Ages are Ar/Ar from Schmidt et al. (2006).|1085 +/- 2 to 1068 +/- 2 Ma|Unit in Alcurra Suite.|||Relatively evolved, Fe-rich, incompatible trace element-rich suite of tholeiitic intrusions.|22-APR-20
39599|Alcurra Dolerite|65833|5|Briefly described|p17|Stenian|Stenian|Formed during ~1075 Ma Giles Event. Intrudes Pitjantjatjara Supersuite.||||||
39599|Alcurra Dolerite|65906|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|~1070 Ma.||||||
39599|Alcurra Dolerite|67128|6|Mentioned|p6|||||Warakurna Supersuite.|||Mafic dykes.|
39599|Alcurra Dolerite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1067 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite; also of olivine gabbro, accessory biotite, massive to weakly flow-banded; and fine- to medium-grained plagioclase-phyric gabbro, ophitic texture, plagioclase phenocrysts and glomerophenocrysts to 2 cm.|11-APR-12
39599|Alcurra Dolerite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||c.1068 Ma.|Unit in Warakurna Supersuite.|||Dykes, sills or plugs mainly of dolerite and metadolerite but also of olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|67375|4|Described|p13, p19 Fig.11, pp36-37, p41, pp332-339|Mesoproterozoic|Mesoproterozoic|A suite of rocks including the Alcurra Dolerite dyke swarm, small intrusions emplaced peripheral to the Warakurna Supersuite, and the compositionally equivalent olivine-rich gabbros, olivine norites, ferronorites and ferrodiorites which host the Nebo-Babel nickel-copper-PGE sulfide mineralization.|1068 +/- 7 - 1067 +/- 8 Ma (Kirkland et al. 2009).|Unit in Warakurna Supersuite.||Intrudes the Smoke Hill Volcanics and Giles Suite.|Dykes, sills and plugs mainly of dolerite but also of olivine gabbros, olivine norites, ferronorites and ferrodiorites.|
39599|Alcurra Dolerite|67553|5|Briefly described|p11,20,34,37-41,p65, 89,95|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Makes up the Warakurna Supersuite component within the Walpa Pulka Zone. Intrusive age from GSWA 194354, coeval with emplacement of Smoke Hill Volcanics. Highly evolved iron-rich tholeiitic intrusions intruding at a relatively late stage in the Giles Event at c. 1067 Ma. At least locally, these rocks are directly related to orthomagmatic nickel-copper mineralization (Howard et al., 2009).|1068+\-7 Ma|Unit of Warakurna Supersuite.||||06-AUG-19
39599|Alcurra Dolerite|68995|6|Mentioned|p1, p8, p50-56, p61, p64-65.|Mesoproterozoic|Mesoproterozoic|Referred to on p1 as the informal Alcurra Dolerite dyke swarm. Intruded during the Mesoproterozoic Giles Event. Source and origin of this unit is discussed in great detail.||||||
39599|Alcurra Dolerite|68996|5|Briefly described|p7, 24-25, 28-29, 32,33, 35-46,53,54,66|Mesoproterozoic|Mesoproterozoic|Hosts significant mineralization of the Nebo-Babel Ni-Cu-PGE deposit. Includes Saturn gabbro. Age range from current dating may not recognise prolonged magmatism suggested from field relationships. See also Alcurra Dolerite Suite p9.|1072-1068 Ma magmatic||Includes Saturn gabbro.||Dolerite dykes and sills. Average density of 2.98+/-0.17g/cm^3|
39599|Alcurra Dolerite|69003|5|Briefly described|p50|Mesoproterozoic|Mesoproterozoic|Associated with the Giles Event. Hosts the orthomagmatic Ni-Cu-PGE mineralisation of the Nebo-Babel deposit, described in some detail on p51.|c.1070 Ma.||||Iron-rich tholeiitic mafic dykes and sills.|
39599|Alcurra Dolerite|69009|5|Briefly described|Map Legend|Stenian|Stenian||c. 1068 Ma|Of the Warakurna Supersuite.|||Comprises dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|69091|4|Described|p54 Fig.4.2, p74, p103 Fig.5.6|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province (Wingate et al., 2004). Hogarth Formation is compositionally identical with an identical crystallisation age of 1068 +/- 7 Ma. Appears as Alcurra Dolerite Suite on p132, p134 Fig.6.2, p137-138, p141 Fig.6.8, p144, p204-205.|1068 +/- 7 Ma|Warakurna Supersuite|Saturn gabbro||Mafic intrusions; most are relatively small dykes and sills, however some larger intrusions exist.|
39599|Alcurra Dolerite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194354.1.pdf|Mesoproterozoic|Mesoproterozoic|Geochron analysis (194354) of medium- to coarse-grained, ophitic gabbro dyke. 20 analyses|1067+/-8 Ma SHRIMP-A|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, mesocratic orthopyroxene(-olivine) ferronorite to ferrodiorite|
39599|Alcurra Dolerite|69427|6|Mentioned|p12:46|||Musgrave Province.||||Is correlated with Stuart Pass Dolerite (Aileron Province).||12-JUL-16
39599|Alcurra Dolerite|69428|6|Mentioned|p13:16|||Musgrave Province.||||Correlated with the Stuart Pass Dolerite.||12-JUL-16
39599|Alcurra Dolerite|69436|4|Described|p21:1, 4, 11-14, 20-21|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993). Widespread throughout Musgrave Province. Related to the Giles Event (1085-1040 Ma). Chilled margins on some dykes suggest shallow-level intrusions. Similar geochemistry to Mount Harris Basalt suggests a common source. As potential feeders for the Giles Complex, some larger dykes have potential for Cu-Ni-Co mineralisation. Geochronology by Camacho et al. (1991) and Zhao and McCulloch (1993) respectively.|1054 +/- 14 Ma (Rb-Sr); 1090 +/- 32 Ma (Sm-Nd).|Warakurna Supersuite.||Intrudes Musgravian gneiss and Pitjantjatjara Supersuite. Is intruded by Angatja Suite.|Extensive intrusions of dolerite and subordinate gabbro dykes, typically 1-3m wide, but up to 8m wide and 6km long. Geochemically homogeneous olivine tholeiite, generally ophitic to sub-ophitic. Locally metamorphosed to garnet granulite facies.|12-JUL-16
39599|Alcurra Dolerite|69437|6|Mentioned|p22:11-12|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the Musgrave Province.||||||12-JUL-16
39599|Alcurra Dolerite|69438|6|Mentioned|p23:9|||Intrudes basement rocks of the Aileron Province.||||||12-JUL-16
39599|Alcurra Dolerite|69640|6|Mentioned|p11|Proterozoic|Proterozoic|Musgrave Province.||||Intrudes the Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|69655|6|Mentioned|p58|||||||||
39599|Alcurra Dolerite|69729|5|Briefly described|p68, p74 Fig.8, p80-84, p86|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (1993); Scrimgeour et al. (1999). Warakurna Large Igneous Province. Originally defined from the Kulgera region (NT). Geochemistry and provenance discussed; trace element plot.|c.1078 Ma to 1073 Ma.|||Is cross-cut by Kullal Dyle Suite.||
39599|Alcurra Dolerite|70083|6|Mentioned|p207|||Musgrave Inlier. Associated with the Giles Event.|~1085-1050 Ma.|Giles Complex.||Intrudes Birksgate Complex.||
39599|Alcurra Dolerite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic||||||Dolerite, dark grey, medium- to fine-grained, olivine, hypersthene. Poikilitic texture.|
39599|Alcurra Dolerite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|SHRIMP age from dolerite (19454.1.pdf)|1067 Ma - 1068 Ma (Isotopic) 1067  (SHRIMP)|Warakurna Supersuite|||Dolerite dykes, sills or plugs with olivine gabbro, olivine norite, ferronorite and ferrodiorite. Fine-medium grained plagioclase-phyric dolerite and gabbro. Olivine rich gabbro, fine-grained, mesocratic ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded an interpreted (207Pb*/206Pb* and 238U/206Pb* concordia) magmatic crystallisation age of 1067+\-8 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068-1067 Ma (inferred)|Unit of Warakurna Supersuite.|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite; mesocratic pox-olivine ferronorite to ferrodiorite.|
39599|Alcurra Dolerite|70826|6|Mentioned|p10, p14 tbl 5|Mesoproterozoic|Mesoproterozoic|Musgrave Province. |1068-1067 Ma|Warakurna Supersuite.||||20-MAY-20
39599|Alcurra Dolerite|70831|5|Briefly described|p4-p5|Stenian|Stenian|Musgrave Province.|c. 1085-1040 Ma|Warakurna Supersuite||||
39599|Alcurra Dolerite|71170|5|Briefly described|p6|||||||||
39599|Alcurra Dolerite|71210|5|Briefly described|p5, p10-p12, p15, p20, p43,|Stenian|Stenian|Musgrave Province. C. 1080 Ma age is derived from Edgoose et al., 1993; Scrimgeour et al., 1999 and Howard et al., 2009c. Hosts most of the magmatic sulphide mineralisation of the Musgrave Province, including the Nebo-Babel Ni-Cu-PGE deposit. Previously referred to as the G3 member of the Giles Suite. See also p46, p50, p66-p67, p69, p76, p109, p114, p134, p139.|c. 1080 Ma -1068 Ma||||Dolerite, olivine gabbros, norites, ferronorites and diorites.|
39599|Alcurra Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
39599|Alcurra Dolerite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Of Warakurna Large Igneous Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Warakurna Supersuite Magmatic Event (1084-1040 Ma); Giles Event (1085-1040 Ma). Sample GSWA 194354 (gabbro dyke) yielded a weight mean 207Pb/206Pb age of 1067+\-8 Ma, interpreted as magmatic crystallisation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv.|1068+\-4 Ma; 1067+\-8 Ma|Unit of Warakurna Supersuite.|||Dolerite dykes and plugs; plagioclase-phyric dolerite and gabbro; ferronorite: mesocratic opx-olivine, magnetite-rich; mesocratic opx ferrnonorite to ferrodiorite.|
39599|Alcurra Dolerite|71321|6|Mentioned|p1,11,23, 50,58,64|Stenian|Stenian|Geological province: Musgrave Province. Comprises part of basement to the Musgrave Province i.e. intrudes and cross-cuts Musgravian-aged gneisses and granites. Associated with c. 1080 Ma Giles Event (p11 for references).||||||24-OCT-19
39599|Alcurra Dolerite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Warakurna Large Igneous Province. Interpreted age from correlation with Giles Complex.|~1080 Ma.|Warakurna Supersuite.||Correlated with Giles Supersuite.|Massive olivine dolerite, mainly E-trending dykes.|
39599|Alcurra Dolerite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1067+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro with ophitic texture and interstitial pyroxene.|
39599|Alcurra Dolerite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic||Max age 1068+/-4, min 1067+/-8 Ma.|Warakurna Supersuite|||Dolerite in dykes, sills, or plugs, with olivine gabbro, olivine norite, ferronorite, and ferrodiorite.|
39599|Alcurra Dolerite|72094|6|Mentioned|p2, p3 Fig 2|Mesoproterozoic|Mesoproterozoic|Musgrave Province.||Unit of Warakurna Supersuite.||||
39599|Alcurra Dolerite|72238|5|Briefly described|p34-36,38-42|Stenian|Stenian|Geological province: Musgrave Province. Dimensions: mainly <10m, rarely up to 80m wide. Associated with coeval Giles Complex mafic-ultramafic intrusions (prospective for orthomagmatic Ni-Cu PGE mineralisation (Howard et al. 2009). Forms part of the Warakurna Large Igneous Province (Wingate, Pirajno and Morris 2004). Generally of lower olivine content than Amata Dolerite. Locally crosscut by Amata Dolerite dykes. Commonly shows evidence for contamination by host rocks. Sm-Nd isochron age: 1110+\-56 Ma.|c. 1080 Ma|||||
39599|Alcurra Dolerite|72443|5|Briefly described|p737, 739, p748, p751-752, p757|||Emplaced over much of central and western Australia and represents much of the Warakurna Large Igneous Province.|1078-1073 Ma|Warakurna Supersuite|||Dolerite dykes and sills.|
39599|Alcurra Dolerite|72476|6|Mentioned|p35, 39|||Musgrave Province. Intrusion of these sills and dykes is suggested to have reset the apatite U-Pb clock in the easternmost parts of the Province. Associated with the mafic/ultramafic Warakurna Large Igneous Province. See also reference to Alcurra Dolerites (p25).||||||
39599|Alcurra Dolerite|73232|6|Mentioned|p5|||Musgrave Province. [Emplaced] during the Giles Event. Includes dykes.||Giles Complex||Intrudes Birksgate Complex and Pitjantjatjara Supersuite.||
39599|Alcurra Dolerite|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|||Warakurna Supersuite||||
76120|Algamba Dolostone Member|65338|6|Mentioned|p20.|||||Unit in Pine Hill Formation.||||
76120|Algamba Dolostone Member|69427|5|Briefly described|p12:25, 64|||Formerly the Algamba Dolomite Member of Stewart et al. (1980). Aileron Province. 150m thick. Economically insignificant black manganiferous laterite pods have developed locally over this unit in the Reynolds Range area.||Pine Hill Formation.||Correlated with Woodforde River beds.|Massive pure dolostone and limestone (including algal boundstone) topped by siliceous sericitic shale, and ferruginous siltstone and sandstone.|12-JUL-16
24152|Ali Curung Granite|23733|6|Mentioned|p29|||See also p34 Fig.20.||||||
24152|Ali Curung Granite|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Ali Curung Suite. Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24152|Ali Curung Granite|42643|2|Defined|p49|Mesoproterozoic||Age approx. 1660Ma?  Variation on Ali Curung Complex.||||||17-JUL-06
24152|Ali Curung Granite|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
24152|Ali Curung Granite|50369|5|Briefly described|p1.5, 18.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Ali Curung Suite.||||||07-NOV-08
24152|Ali Curung Granite|69425|5|Briefly described|p10:6 Tb.10.1, 10:26|||Secondary Cu mineralisation occurs at the Comet Bore prospect near the contact with this unit.||||Intrudes Ooradidgee Group.|Two-mica granite; includes a medium-grained and equigranular leucocratic phase.|12-JUL-16
24152|Ali Curung Granite|69427|5|Briefly described|p12:20 Fig.12.19; 12:22|||Haines et al. (1991). Aileron Province. Occurs between the Osborne, Crawford and Watt Ranges, N and NE of Barrow Creek roadhouse. Suggested to be the same age as Barrow Creek Granite Complex.|||||A multi-phase intrusion with six mappable units: porphyritic to equigranular biotite and biotite-muscovite granites, with lesser leucogranite and biotite granodiorite.|12-JUL-16
27281|Alice Springs Granite|9199|5|Briefly described|Map legend|||Muscovite-biotite granite.  Geological Province: Arunta Block.||||||04-NOV-04
27281|Alice Springs Granite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|1752+/-11Ma||||||
27281|Alice Springs Granite|23733|5|Briefly described|p34 Fig.20|||Age: 1752Ma.  Remelting.||||||
27281|Alice Springs Granite|24197|5|Briefly described|p20, p60 Tb.4.1|Paleoproterozoic|Paleoproterozoic|Example of the Maramungee Association. Comprises typical trondhjemite of the association. Emplaced at ~1750Ma. Geological province: Arunta Inlier.||||||07-FEB-11
27281|Alice Springs Granite|38606|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27281|Alice Springs Granite|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27281|Alice Springs Granite|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27281|Alice Springs Granite|39888|6|Mentioned|Fig.8|||||||||
27281|Alice Springs Granite|41664|6|Mentioned|Map legend|Mesoproterozoic||||||||
27281|Alice Springs Granite|41665|4|Described|p10|||||||||
27281|Alice Springs Granite|41816|6|Mentioned|p7|||||||||
27281|Alice Springs Granite|42326|5|Briefly described|Table 2 P11|||||||||
27281|Alice Springs Granite|42504|6|Mentioned|p65|||||||||
27281|Alice Springs Granite|48992|2|Defined|p3|||Prob.Late Proterozoic||||||17-JUL-06
27281|Alice Springs Granite|50246|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Age: 1752+/-11Ma. Intrudes Sadadeen Gneiss.||||||07-FEB-11
27281|Alice Springs Granite|50369|5|Briefly described|p1.4, 13.1, 26.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Alice Springs Suite. Age: 1750-1860 +/- 20Ma (Sm-Nd, SHRIMP).||||||07-NOV-13
27281|Alice Springs Granite|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Muscovite-biotite granite.||||||
27281|Alice Springs Granite|62595|5|Briefly described|p8. |Statherian|Statherian|Intruded during the Inkamulla Igneous Event.|1752 +/- 11 Ma (Zhao and Bennett 1995).|||Intrudes or grades into Sadadeen Gneiss.||
27281|Alice Springs Granite|67181|5|Briefly described|p631|Statherian|Statherian|Age from Zhao and McCulloch (1995) and Zhao and Bennet (1995). Of the Calcalkaline-trondhjemitic Group (geochemical grouping) Arunta Region, North Australian Craton.|1751 +/- 12 Ma|||||
27281|Alice Springs Granite|69427|5|Briefly described|p12:3, 14-15, 30, 36|Statherian|Statherian|Wigley Domain, Aileron Province. SHRIMP U-Pb zircon age.|1752 +/- 11 Ma (Zhao and Bennett, 1995).|||Intrudes (likely) Sadadeen Gneiss.|A homogeneous foliated biotite-muscovite granite, varying from equigranular to porphyritic.|12-JUL-16
27281|Alice Springs Granite|69925|5|Briefly described|p18, 21-22, 25-30, 36, 39-40|||Southern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated.|1752 +/- 11 Ma (U-Pb zircon).|||Is overlain unconformably by Heavitree Quartzite. Is intruded by Stuart Dyke Swarm. Probably intrudes Sadadeen Range gneiss.|Muscovite-biotite trondhjemite.|
27281|Alice Springs Granite|69931|6|Mentioned|p273-274, 276, 278-279, 287, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.|||||Coarse- to medium-grained granites, migmatitic granite, biotite-rich granite.|
27281|Alice Springs Granite|69932|6|Mentioned|p302-303, 306-307|||Southern Province, Arunta Inlier. Sm-Nd data tabulated.|1750 Ma.||||Muscovite-biotite leucocratic granite.|
27281|Alice Springs Granite|71348|6|Mentioned|p201,217|Statherian|Statherian|Geological province: Aileron Province, Arunta Region.|c. 1750 Ma|||||
27281|Alice Springs Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1752+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Trondhjemite.|
27281|Alice Springs Granite|72516|5|Briefly described|p121|||Part of the calc-alkaline-trondhjemitic group of Zhao and McCulloch (1995). Outcrops below the informal CAT-line in the eastern Aileron Province.|ca. 1770-1750 Ma|||||09-JUN-21
28277|Alinjabon Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
28277|Alinjabon Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Hanlon Subgroup. Geological Province: Davenport Province.||||||17-MAR-05
28277|Alinjabon Sandstone|24172|5|Briefly described|p65 Tb.9|||Of the Hanlon Subgroup. Geological Province: Tennant Creek Inlier. Of the Hatches Creek Group.||||||17-JUL-06
28277|Alinjabon Sandstone|39624|5|Briefly described|Table 1|||||||||
28277|Alinjabon Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28277|Alinjabon Sandstone|40578|6|Mentioned|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Quartz arenite and feldspathic arenite; siltstone, shale, friable arenite, rare altered basalt.||||||10-JAN-05
28277|Alinjabon Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28277|Alinjabon Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28277|Alinjabon Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Quartz arenite and subordinate feldspathic arenite; rare pebbly arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
28277|Alinjabon Sandstone|41129|4|Described|Table 1|||Mention p24||||||17-JUL-06
28277|Alinjabon Sandstone|41204|4|Described|Table 1|||||||||
28277|Alinjabon Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup. Lithic/feldspathic arenite, quartz arenite, shale, siltstone; minor mafic lava.||||||16-NOV-05
28277|Alinjabon Sandstone|41308|5|Briefly described|Table 2|||||||||
28277|Alinjabon Sandstone|41310|4|Described|Table 1|||See also p12||||||17-JUL-06
28277|Alinjabon Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
28277|Alinjabon Sandstone|41524|4|Described|Table 1|||||||||
28277|Alinjabon Sandstone|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Quartz arenite, some feldspathic; minor basalt.||||||07-NOV-08
28277|Alinjabon Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
28277|Alinjabon Sandstone|42643|4|Described|p12, Table 1 p6|||||||||
28277|Alinjabon Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Quartz arenite, interbedded with feldspathic/kaolinitic/micaceous arenite, siltstone and shale; minor basaltic lava.||||||07-NOV-08
28277|Alinjabon Sandstone|43802|6|Mentioned|p80|||||||||
28277|Alinjabon Sandstone|45167|3|Fully described|Table 1|||of Hanlon Subgroup||||||
28277|Alinjabon Sandstone|49033|2|Defined|p26|Proterozoic|Proterozoic|||||||
28277|Alinjabon Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Subarkosic and sublithic arenite, quartz arenite; minor mafic lava, greywacke, chert and ironstone.. Overlies Errolola Sandstone; underlies Lennee Creek Formation. In the Tennant Creek region.||||||07-NOV-08
28277|Alinjabon Sandstone|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Geological Province: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
28277|Alinjabon Sandstone|64735|5|Briefly described|p206 Fig 2, p210|||?includes basaltic lavas.||Of Hanlon Subgroup, Hatches Creek Group.||||30-APR-12
28277|Alinjabon Sandstone|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||||
28277|Alinjabon Sandstone|65338|6|Mentioned|p20.|||||Unit in Hanlon Subgroup.||||
28277|Alinjabon Sandstone|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup, Hatches Creek Group.||Overlies Errolola Sandstone. Is overlain by Lennee Creek Formation.|Quartz arenite and feldspathic arenite; friable arenite; siltstone; shale and mafic lava.|19-OCT-11
28277|Alinjabon Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Errolola Sandstone. Is overlain by Lennee Creek Formation.|Subarkosic and sublithic arenite, quartz arenite; minor mafic lava, greywacke, chert and ironstone.|
28277|Alinjabon Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
28277|Alinjabon Sandstone|67352|4|Described|p9, p44 fig 48|Statherian|Statherian|Interbedded ridge-forming and recessive units.||Hanlon Subgroup||Overlies conformably Errolola Sandstone. Is overlain conformably by Lennee Creek Formation.|Quartz arenite; silicified lithic, feldspathic arenite: thinly to medium bedded, fine-to-medium-grained; siltstone, sandstone and shale interbeds; amygdaloidal mafic lava near base.|
28277|Alinjabon Sandstone|68518|4|Described|p6 Tb.1, p13|Proterozoic|Proterozoic|Thickness: approx. 500 m. Shallow-marine and possibly deltaic environments indicated. The minor altered basaltic lavas are the youngest volcanics in Hatches Creek Group.||Hanlon Subgroup||Conformable on Errolola Sandstone; is overlain conformably by Lennee Creek Formation and unconformably by Cambrian strata.|Interbedded ridge-forming quartzose to feldspathic arenite and recessive friable arenite, thinly bedded siltstone, mudstone and shale; minor recessive altered basaltic lava and possibly calcareous beds.|30-MAY-16
28277|Alinjabon Sandstone|69425|4|Described|p10:3, 10, 12, 19-20, 23|Statherian|Statherian|300-840m thick. Shallow-marine shelf deposits with possible deltaic influence. Underwent disharmonic folding by the Davenport Event.||Hanlon Subgroup.||Conformably overlies Errolola Sandstone. Is overlain conformably, and may interfinger with basal, Lennee Creek Formation. Correlated with part of Kuerschner Member (Morphett Creek Formation).|Subarkosic and sublithic sandstone, quartz sandstone, siltstone, shale; minor predominantly mafic lava (basalt to trachyte); minor greywacke, chert and ironstone.|12-JUL-16
28277|Alinjabon Sandstone|69431|6|Mentioned|p16:5, 22|||Davenport Province. Folding during the Davenport Event is discussed.||Hanlon Subgroup.||||12-JUL-16
81826|Alkara Suite|73591|6|Mentioned|p21||||ca 1740-1720 Ma||Jamaica Granite, Canefire Granite||S-type granitic suite.|
41842|Alkipi Metamorphics|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Yaya Metamorphic Complex.   Age: 1660Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
41842|Alkipi Metamorphics|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Yaya Metamorphic Complex. Metapelite, metapsammite, granite, migmatite, amphibolite, metasediment, quartzite. Geological Province: Yaya Domain.||||||07-NOV-08
41842|Alkipi Metamorphics|61660|5|Briefly described|p3 Fig.2, p4, pp9-13  .|Proterozoic|Proterozoic|Metamorphosed ca. 1640 Ma. SHRIMP U-Pb zircon analyses are described in detail.||Unit in Yaya Metamorphic Complex.|||A homogeneous pelite-psammite association.|
41842|Alkipi Metamorphics|65272|6|Mentioned|p318 fig 2.|||40Ar/39Ar data.||||||
41842|Alkipi Metamorphics|67565|2|Defined|p60, p15-17, p30-31, p34, p49-50.|Statherian|Statherian|New name, after Alkipi (Mount Larrie) Outstation. Yaya Domain, Warumpi Province. Previously included within undifferentiated Arunta Complex (Ranford, 1969). Type locality 1 km north of Mount Larrie copper Prospect. Moderately to highly magnetic; moderate U and K, high Th radiometric signature. Another sample gave Kinny (2002) a max. deposition age of 1652 +/- 22 Ma. Metamorphosed at 1639 +/- 20 Ma (Kinny, 2000) during the Liebig Orogeny. Metamorphic effects are detailed. Hosts the Mount Larrie Cu prospect which apparently lacks significant mineralisation.|Max. deposition age 1668 +/- 40 Ma (Kinny 2002).|Unit in Yaya Metamorphic Complex.||Is intruded by Papunya Igneous Complex, Ulambaura Granodiorite and Belt Granite. Faulted against the Russell Charnockite and Glen Helen Metamorphics. Is overlain unconformably by Heavitree Quartzite.|Garnet-biotite-sillimanite metapelite, interlayered with psammite; minor strained granite, amphibolite and felsic migmatite; quartz-rich psammite and quartzite interlayered with lesser pelite.|01-DEC-15
41842|Alkipi Metamorphics|69428|5|Briefly described|p13:7-9, 14, 18-19|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province. Metamorphism discussed. Metamorphic zircon rims have ages of 1641 +/- 14 Ma and 1639 +/- 20 Ma. Hosts the Mount Larrie Cu prospect, SW of Papunya Community; no significant mineralisation found.|c.1650 Ma (maximum deposition age).|Yaya Metamorphic Complex.|||Contains a metapelitic unit with interlayered psammitic rock, with biotite granite, felsic migmatite, gneiss, leucogranite and amphibolite; and a quartzose unit with more quartz-rich psammo-pelite and quartzite.|12-JUL-16
41842|Alkipi Metamorphics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1641+/-14 Ma (metamorphism: U-Pb zircon SHRIMP)||||Garnetiferous metapelite.|
27035|Allamber Springs Granite|23714|4|Described|p18|Paleoproterozoic|Paleoproterozoic|Geological Province: Cullen Batholith.||||||07-NOV-08
27035|Allamber Springs Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
27035|Allamber Springs Granite|24047|5|Briefly described|p28, p30 Fig. 23|||Geological Province: Pine Creek Orogen.||||||
27035|Allamber Springs Granite|24197|5|Briefly described|p24, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of Cullen Supersuite. One of a group of concentrically zoned transitional granite and leucogranite dominated plutons. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
27035|Allamber Springs Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27035|Allamber Springs Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Leucogranite and granite.||||||07-NOV-08
27035|Allamber Springs Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27035|Allamber Springs Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27035|Allamber Springs Granite|41311|4|Described|p18|||||||||
27035|Allamber Springs Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27035|Allamber Springs Granite|43140|3|Fully described|p6||Paleoproterozoic|Of the Cullen Batholith. U-Pb age: 1810 Ma.||||||07-NOV-08
27035|Allamber Springs Granite|43624|6|Mentioned|p13|||Geological Province: Cullen Batholith.||||||
27035|Allamber Springs Granite|43832|3|Fully described|34,39,46-50,63,114-5||Paleoproterozoic|Age 1822+-6 Ma (p39); 1818+-5 Ma (and less accurate ages) (p53).||||||07-NOV-08
27035|Allamber 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: 1826-1818 +/- 32Ma (U-Pb, SHRIMP).||||||02-MAR-18
27035|Allamber Springs 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; equigranular biotite leucogranite.  Age: 1825-1820Ma.||||||13-JAN-05
27035|Allamber Springs Granite|62375|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Hornblende biotite granite/biotite leucogranite. Age: 1825Ma. Of the Cullen Batholith. Geological Province: Pine Creek Orogen.||||||09-FEB-10
27035|Allamber Springs Granite|63866|5|Briefly described|p110-p111|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. |1822 +/- 6 Ma and 1818 +/- 5 Ma (emplacement age)|Cullen Supersuite||||
27035|Allamber Springs Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1818-1822Ma U/Pb SHRIMP. I-type. Pink and green, coarse porphyritic hornblende-biotite granite; equigranular biotite leucogranite. Intrudes Manton Group, Mount Partridge Group and South Alligator Group.||||||07-JAN-09
27035|Allamber Springs Granite|67564|3|Fully described|p7 Table 2, p15 Fig.8, p33 Fig.19, p34.|Paleoproterozoic|Paleoproterozoic|I-type. Pluton within Cullen Batholith, Pine Creek Orogen. 600 km2 in area. Contains large (up to 1.5 km across) rafts of Bludells Dolerite. Rare contact metamorphic K-feldspar-cordierite hornfels facies zones.|1825 - 1820 Ma.|Unit in Cullen Supersuite.||Intrudes McCarthys Granite. Is intruded by Frances Creek and Saunders Leucogranites, and Lewin Springs Syenite.|Pink and green, coarse porphyritic hornblende-biotite granite; pink coarse porphyritic and equigranular leucogranites.|
27035|Allamber Springs Granite|69420|4|Described|p5:14, 17-18, 20-22, 99, 111-112|Paleoproterozoic|Paleoproterozoic|Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Includes irregularly-shaped bodies, up to 5km across, of Bludells Dolerite. Spatially related to Au or base metals mineralisation, eg the Evelyn Pb-Zn-Ag mine. Three other age determinations are given.|1826 +/- 18 Ma conventional U-Pb zircon (TIMS).|Allamber Springs Suite.||Is intruded by Bludells Dolerite.|Coarse-grained equigranular leucogranite with porphyritic granite at margins. I-type.|12-JUL-16
27035|Allamber Springs Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1818 +/- 5 Ma.|Allamber Springs Suite.|||Pink, medium-grained, equigranular biotite-hornblende granite; pink and green, coarsely porphyritic hornblende-biotite granite; pink, coarse-grained, porphyritic biotite granite; equigranular biotite leucogranite.|
27035|Allamber Springs Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|1822+/-6 Ma and 1818+/-5 Ma.||||Granite.|
31739|Allamber Springs Suite|69420|5|Briefly described|p5:17, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.|||Allamber Springs, Bonrook Granites.||Zoned, biotite-dominated granite.|12-JUL-16
31739|Allamber Springs Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Cullen Supersuite.|Includes Allamber Springs Granite.|||01-MAR-18
38051|Allanah Gneiss|24301|2|Defined|p36 Appendix 1|Mesoproterozoic|Paleoproterozoic|Also referred to as Allanah Granitic Gneiss. Includes rocks previously mapped as Mulga Park Suite. Geological Province: Musgrave Block||||||07-NOV-08
38051|Allanah Gneiss|24302|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Biotite-bearing granitic gneiss with secondary muscovite, grey, medium-grained; commonly migmatitic with veins of partial melt cutting early gneissic fabric. Geological Province: Musgrave Block||||||29-SEP-05
38051|Allanah Gneiss|24496|5|Briefly described|p14|||May be protolith for some Pottoyu Suite granitoids. Geological Province: Musgrave Block.||||||17-JUL-06
38051|Allanah Gneiss|61154|5|Briefly described|p43 Appendix|Mesoproterozoic|Mesoproterozoic|Amphibolite facies felsic gneiss of the 1600-1540Ma period - in the Olia Chain (Mulga Park Domain).  Age: 1539+/-28Ma. Geological province: Musgrave Block.  See also p44 Appendix, p26.||||||14-JUL-05
38051|Allanah Gneiss|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
38051|Allanah Gneiss|69436|5|Briefly described|p21:5-6|Mesoproterozoic|Mesoproterozoic|Mulga Park Domain, Musgrave Province. SHRIMP U-Pb zircon protolith age range; metamorphic rims dated at 1176 +/- 40 Ma; another age determination of (Musgrave Orogeny) metamorphism is 1206 Ma (Young et al., 2002).|1591-1539 Ma (Scrimgeour et al., 1999).||||Amphibolite-facies felsic gneiss, quartzofeldspathic and equigranular, containing biotite, quartz, K-feldspar, plagioclase and locally-developed garnet. Migmatitic in the Olia Chain, with an intrusive igneous precursor.|12-JUL-16
38051|Allanah Gneiss|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gneiss|
38051|Allanah Gneiss|71592|5|Briefly described|Appendix A.|||Musgrave Province. Both ages are for crystallisation: U-Pb zircon SHRIMP.|1591+/-30 Ma and 1539+/-23 Ma.||||Migmatite.|
39136|Allia Creek Suite|23733|5|Briefly described|p32 Fig. 19|||||||||
39136|Allia Creek Suite|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Predominantly S-type granites.  Geological Province: Litchfield Province (Pine Creek Orogen).||||||07-NOV-08
39136|Allia Creek Suite|24197|5|Briefly described|p103, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Incl: Allia Ck, Two Sisters, Marra-Kamangee, Jammine Granites, Fish Billabong Adamellite, Mt Litchfield, Soldiers Ck and Turnbull Bay Granites. Felsic fractionated S-type; contains pegmatites and greisens. Geol.prov: Pine Creek Inlier. Age: ~1845Ma.||||||07-FEB-11
39136|Allia Creek Suite|50586|5|Briefly described|p1.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Age: 1845Ma. See also Allia Suite.||||||07-NOV-08
39136|Allia Creek Suite|65232|5|Briefly described|p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Predominantly S-type granites.~1830-1829Ma?||||||09-FEB-10
39136|Allia Creek Suite|65339|6|Mentioned|p4.|||Late- to post-tectonic (Barramundi Orogeny) granitoids.|1852 - 1840 Ma.|||||
39136|Allia Creek Suite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Areas with diferent magnetic responses are indicated.|||Includes Murra-Kamangee Granodiorite, Allia Creek and Soldier's Creek Granites.|||
39136|Allia Creek Suite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Two Sisters, Jammine and Mount Litchfield Granites, Fish Billabong Adamellite and Murra-Kamangee Granodiorite.|||23-NOV-11
39136|Allia Creek Suite|67232|5|Briefly described|p3. |Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. |||Includes Two Sisters, Murra-Kamangee and Mount Litchfield Granites.||Dominantly S-type granitoids.|
39136|Allia Creek Suite|67355|6|Mentioned|p5, 15.||Orosirian|Age may include inherited zircons. Resetting of Rb-Sr system occurred at 1780-1760 Ma due to a regional lowgrade metamorphic event, the Shoobridge Event.|~1850 Ma (U-Pb zircon, conventional)|||||25-JAN-17
39136|Allia Creek Suite|67479|6|Mentioned|p6 Fig.2|||||||||
39136|Allia Creek Suite|67564|4|Described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Correlative of Cullen Supersuite, Edith River Group and David Suite to the east.|||||Predominantly S-type granites.|
39136|Allia Creek Suite|67779|5|Briefly described|p5 Fig.4(b), p6.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite suite.|1863-1853 Ma (Page et al. 1985).|||||14-MAY-18
39136|Allia Creek Suite|69417|6|Mentioned|p2:5|Orosirian|Orosirian|Pine Creek Orogen. Appears to be shown in Fig.2.4 as intruding the Cosmo Supergroup.||||||12-JUL-16
39136|Allia Creek Suite|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
39136|Allia Creek Suite|69420|4|Described|p5:4-5, 17-19, 27-28, 33-34, 38, 66, 100|Paleoproterozoic|Paleoproterozoic|See also 111, 115. Wyborn et al. (1997). Litchfield Domain, Pine Creek Orogen. These granite plutons were emplaced during the c.1855 Ma Litchfield Event. Geochemistry described in some detail.|c.1854-1850 Ma.||Jammine, Two Sisters, Mount Litchfield, Allia Creek, Soldiers Creek Granites; Murra-Kamangee Granodiorite; Fish Billabong Adamellite.||Predominantly S-type granites containing peraluminous minerals (eg andalusite, cordierite and muscovite); high-level intrusions (numerous pegmatites and greisens). Fractionated.|12-JUL-16
39136|Allia Creek Suite|69673|6|Mentioned|p3|||||||||
39136|Allia Creek Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Murra-Kamangee Granodiorite; Fish Billabong Adamellite; Two Sisters, Jammine, Mount Lichfield Granites.|||01-MAR-18
39136|Allia Creek Suite|71621|6|Mentioned|p25|||Pine Creek Orogen.||||||02-FEB-19
75901|Alooarjara Metamorphics|66767|5|Briefly described|p58|||Aileron Province.||||Structurally overlies Bruna Granitic Gneiss.|A granulite-facies unit dominated by garnet-rich metapelitic rock and mafic granulite.|
75901|Alooarjara Metamorphics|69427|5|Briefly described|p12:30, 33-35, 39, 47, 59|||Crops out along the Alooarjara Range and immediately S of the Entia Dome, Aileron Province. Maximum depositional age. Metamorphism at c.1730 Ma (Strangways Event) is described in some detail, with zircon overgrowths dated at c.1735-1713 Ma. Juxtaposed against the Irindina Province by the Basil Shear Zone, during the Alice Springs Orogeny. Contains anomalous Ni-Cu sulfide and Ni-Pt mineralisation.|<1754 +/- 6 Ma (Worden et al., 2008).||||Mainly granulite-facies metapelitic and metapsammitic rocks with abundant interlayered mafic granulite; calc-silicate rock is rare. Includes a mylonitised megacrystic biotite granite with minor garnet and hornblende.|12-JUL-16
75901|Alooarjara Metamorphics|69444|6|Mentioned|p29:3 Fig.29.4|Paleoproterozoic|Paleoproterozoic|||||||12-JUL-16
75901|Alooarjara Metamorphics|69917|5|Briefly described|p160-162, 165-167, 1||Statherian|Eastern Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. 2 samples dated. Age is conservative estimate of the maximum depositional age of the protolith.  1770+/-6 Ma is the age estimate of the maximum crystallization age of the igneous protolith for the granulite sample. |1756-1732 Ma max deposit||||Garnet-bearing metapsammite; Garnet-orthopyroxene-hornblende-bearing quartzo-feldspathic granulite sampled from layers within dominantly metapelitic rocks.|
75901|Alooarjara Metamorphics|69937|5|Briefly described|p12|||SE Aileron Province. Possible source of (some) zircons in Areyonga Formation.|1770-1750 Ma.|||||
75901|Alooarjara Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1822+/-10 Ma (U-Pb zircon LA-ICPMS).||||Metapsammite.|
26291|Aloolya Gneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|of Arunta Block.||||||
26291|Aloolya Gneiss|23271|5|Briefly described|Map legend||Proterozoic|of Arunta Block. Age: Middle Proterozoic.||||||
26291|Aloolya Gneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26291|Aloolya Gneiss|39888|6|Mentioned|Fig.8|||||||||
26291|Aloolya Gneiss|42326|5|Briefly described|Table 2 P11|||||||||
26291|Aloolya Gneiss|48992|2|Defined|p4|Mesoproterozoic|Mesoproterozoic|||||||
26291|Aloolya Gneiss|50369|6|Mentioned|p7.3|||Intruded by Possum Creek Charnockite.||||||
26291|Aloolya Gneiss|64956|5|Briefly described|p3 Tb. 1, p12|Paleoproterozoic|Paleoproterozoic|Cryst. Age: 1818+/-5Ma. Geological province: Arunta region. Sample lithology is K-feldspar megacyrstic biotite granite.||||||07-FEB-11
26291|Aloolya Gneiss|65338|6|Mentioned|p34.|||Southwest Anmatjira Range.||||Intrudes Anmatjira Orthogneiss.||
26291|Aloolya Gneiss|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
26291|Aloolya Gneiss|69427|5|Briefly described|p12:6, 20-21, 26|Statherian|Orosirian|Crops out in the SE Anmatjira Range. SHRIMP U-Pb zircon age.|1807 +/- 6 Ma (Worden et al., 2008).|||Intrudes Anmatjira Orthogneiss, Weldon Metamorphics and Tyson Creek Granulite.|Even-grained, tourmaline- and garnet-bearing gneissic granite.|12-JUL-16
26291|Aloolya Gneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1807+/-5.6 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
26291|Aloolya Gneiss|71858|6|Mentioned|p5|||Aileron Province.||||||
81848|Alroy Formation|73427|5|Briefly described|p3, p5, p12-13, App.A|Orosirian|Orosirian|North Australian Craton, East Tennant. Sampled for monazite U-Pb dating to constrain deformation and metamorphism.|ca 1855-1872 Ma||||Pelitic schist (locally gneissic), and subordinate marble and iron-rich rocks.|
81848|Alroy Formation|73506|5|Briefly described|p2, p4-6, p12, p18|Orosirian|Orosirian|Pb-Pb SHRIMP monazite ages of 1843.6+/-6.1 Ma and 1843.5+/-5.1 Ma are attributed to peak metamorphism and deformation. U-Pb detrital zircon maximum depositional ages of 1864.4+/-4.2 Ma to 1873.6+/-6.3 Ma are from the same sequence that was sampled for monazite dating in drill hole NDIBK01 (Kositcin et al., in prep). In drill hole NDIBK01 amphibolite-facies metamorphism and a S2 shear fabric is interpreted to overprint an earlier, sub-parallel S1 fabric, and is overprinted by a locally well-developed lower temperature crenulation cleavage (S3).|ca. 1870-1860 Ma||||Metasedimentary rocks, includes cordierite schist, paragneiss, banded pelitic schist and paragneiss with amphibolite-facies metamorphism.|
42483|Amata Dolerite|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Dolerite dykes, gabbro. Geological Province: Amadeus Basin.||||||
42483|Amata Dolerite|61154|5|Briefly described|p42 Appendix|Neoproterozoic|Neoproterozoic|Intrudes the Pitjantjatjara Supersuite. Age: 800Ma. Geol. Prov: Musgrave Block.||||||03-AUG-09
42483|Amata Dolerite|61524|5|Briefly described|p18 Fig.2(a)|Neoproterozoic|Neoproterozoic|Age: 820Ma. See also Amata dolerite. Geological Province: Musgrave Province.||||||
42483|Amata Dolerite|63866|5|Briefly described|p208|Tonian|Tonian|Numeric age is a U-Pb Baddeleyite date. Zhao and McCulloch 1993 report Sm-Nd ages for the Amata Dolerite of 790 +/- 40 Ma and 797 +/- 49 Ma.|824 +/- 4 Ma (Glikson et al., 1996)|||||
42483|Amata Dolerite|64722|5|Briefly described|p17|Cryogenian|Cryogenian|Also referred to as Amata Dolerite dyke swarm.| 820 Ma  Sm-Nd and U-Pb baddeleyite.|||||11-APR-12
42483|Amata Dolerite|64745|5|Briefly described|p376, 378|Cryogenian|Cryogenian|Dykes. Commonly display primary igneous textures S of Mann Fault. To N, recrystallised to garnet-granulite facies. Age: ca. 820 Ma (Sm-Nd mineral-whole rock and baddelyite U-Pb. Zhao et.al, 1994; Glikson et.al, 1996). Geol. Prov: Musgrave Province.||||||03-AUG-09
42483|Amata Dolerite|65833|5|Briefly described|p17|Cryogenian|Cryogenian|Medium-grained, intergranular to subophitic dolerite. ~800 Ma: 790 +/- 40 Ma (Sm-Nd: Zhao et al., 1994). Possibly linked with Gairdner Dyke Swarm on basis of age and geochemistry. Cuts Kullal Dyke Suite.||||||
42483|Amata Dolerite|65906|6|Mentioned|p7, p21|Neoproterozoic|Neoproterozoic|Date: ~820 Ma.||||||
42483|Amata Dolerite|67375|5|Briefly described|p55.|Neoproterozoic|Neoproterozoic|East Musgrave Province. Linked to Gairdner Dolerite on basis of similar chemistry and age.|790 +/- 40 Ma (Zhao et al. 1994).||||Dolerite dykes.|
42483|Amata Dolerite|67553|6|Mentioned|p57|Tonian|Tonian|Produced by a c. 800 Ma magmatic event.||||||
42483|Amata Dolerite|68994|5|Briefly described|p18|||Spilites in this unit have geochemical affinities with Johnnys Creek Member (Bitter Springs Formation).|820 Ma.|||||13-JAN-17
42483|Amata Dolerite|69091|5|Briefly described|p78|Neoproterozoic|Neoproterozoic|c. 800 Ma event produced Gairdner Dolerite and Amata Dolerite.||||||
42483|Amata Dolerite|69436|5|Briefly described|p21:3, 14-15, 17-18|||Zhao et al. (1994). Maboko (1998). Has similar age, geochemistry and eNd values to the Gairdner Dolerite. Petermann Orogeny metamorphism produced a peak assemblage of hornblende-plagioclase-quartz with rare garnet. Amphibolite dykes of this unit are strained and boudinaged within the foliation.|820 Ma.|||Intrudes Pottoyu Suite.|Mafic dykes, distinguished by distinctive geochemical and isotopic signature (uniformly smooth LREE-enriched patterns and relatively juvenile eNd values of +2.4 to +4.2). Includes large gabbroic bodies with coarse ophitic to sub-ophitic texture.|12-JUL-16
42483|Amata Dolerite|69437|6|Mentioned|p22:12|||Intrudes the Musgrave Province.||||Correlated with Gairdner dyke swarm.||12-JUL-16
42483|Amata Dolerite|69438|5|Briefly described|p23:10, 12-13|||Mafic dykes, with geochemical affinities with spilites in the Bitter Springs Formation. Used to give an estimated youngest age of the Heavitree and Dean Quartzites underlying that unit. U-Pb baddeleyite age. Another date of c.800 Ma (Zhao et al., 1994) is a Sm-Nd isochron age.|824 +/- 4 Ma (Glikson et al., 1996).|||||12-JUL-16
42483|Amata Dolerite|69729|6|Mentioned|p84-85|Neoproterozoic|Neoproterozoic|East Musgrave Province.|c.827-824 Ma.|||||
42483|Amata Dolerite|69937|5|Briefly described|p5, p8|||Part of a continental flood basalt province. Geochemically correlated with a basalt unit in the Bitter Springs Formation (Amadeus Basin). Geochronology details given.|824 +/- 4 Ma; c.800 Ma.|||||
42483|Amata Dolerite|70839|5|Briefly described|p327,336,339|Tonian|Tonian|Geological province: Musgrave Province. NW-trending mafic dyke suite across northern South Australia into Musgrave region. Equivalent to Gairdner Dolerite.|827+\-6 Ma|||||
42483|Amata Dolerite|71129|5|Briefly described|p106|Tonian|Tonian|Geological Province: Musgrave Province, Gawler Craton. Dated at 824+\-6 Ma (S. S. unpublished data in Glikson et al., 1996).|824+\-6 Ma|||Equivalent to Gairdner Dolerite.||
42483|Amata Dolerite|71170|5|Briefly described|p146, p150|Neoproterozoic|Neoproterozoic|[Appears as the Amata Dolerite suite on p146]. Intrudes much of the central Musgrave Province and are genetically related to co-eval plume-sourced dykes in the south and north Australian cratons. Age is Sm-Nd whole-rock and Baddeleyite.|ca. 820 Ma (Glikson, 1996)|||||
42483|Amata Dolerite|71211|6|Mentioned|p230|Cryogenian|Cryogenian||ca. 820 Ma|||||
42483|Amata Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
42483|Amata Dolerite|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Dolerite and amphibolite dykes, sills and plugs; minor gabbro|
42483|Amata Dolerite|71321|5|Briefly described|p1,11,23, 50,64|Tonian|Tonian|Geological province: Musgrave Province. Intruded post-c. 1085-1040 Ma Giles Event (p11 for references).|c. 825 Ma|||Correlable to Gairdner Dolerite (Gawler Craton).||24-OCT-19
42483|Amata Dolerite|71416|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Inferred age by correlation with Gairdner Dolerite.|~827 Ma.|||Correlative of Gairdner Dolerite.|Massive dolerite; mainly WNW-trending dykes.|17-SEP-19
42483|Amata Dolerite|72238|4|Described|p34-43|Tonian|Tonian|Geological province: Musgrave Province. On the ALCURRA 1:100000 map sheet. Mafic dyke suite intruding into c. 1.7-1.5 Ga Birksgate Complex gneisses and c. 1.15 Ga Pitjantjatjara Supersuite granites. Also locally crosscuts Alcurra Dolerite dykes. Part of the Gairdner LIP, alongside Gairdner Dolerite, Willouran Basic province and other coeval mafic igneous rocks (see p34 for references). ESE-Se-trending dyke swarms, commonly form linear magnetic anomalies due to magnetite content and high magnetic susceptibility. Can be traced along strike for up to 10km in length, thickness ranging from <1m to 100m. Generally has higher olivine content compared to Alcurra Dolerite. Outcrop exposure shows an Amata Dolerite dyke to have enclosed around, and intruded into a felsic gneiss sliver. Sm-Nd isochron age of 766+\-53 Ma, Rb-Sr age of 758+\-21 Ma (Dutch et al. 2013; Werner et al. 2014). Age constraints suggest it was part of the Gairdner-Willouran-Guibei Large Igneous Province, which formed in the early Neoproterozoic due to giant mantle plume activity, prior to Rodinia supercontinent breakup.|c. 800 Ma|||Equivalent to Gairdner Dolerite.||17-SEP-19
42483|Amata Dolerite|72242|6|Mentioned|p27|Tonian|Tonian|Geological province: Musgrave Province. ||||||
42483|Amata Dolerite|72369|5|Briefly described|p43|||Geological province: Musgrave Province. Geochemically correlable with basalts in the Johnnys Creek Formation (Barovich and Foden 2000). Interpreted to be part of a continental LIP (Barovich and Foden 2000). Previous geochronological age studies includes c. 800 Ma (Sm-Nd whole rock + clinopyroxene + plagioclase; Zhao and McCulloch 1993; Zhao et al 1994) and 824+\-4 Ma (U-Pb baddeleyite; unpublished data quoted in Glikson et al 1996).||||||
42483|Amata Dolerite|72375|5|Briefly described|p5,10|Tonian|Tonian|Of Amadeus Basin. Part of a continental flood basalt province and has been dated at c. 800 Ma (Sm-Nd whole rock + cpx + plg; Zhao and McCulloch 1993, Zhao et al 1994), and 824+\-4 Ma (U-Pb baddeleyite; unpublished data quoted in Glikson et al 1996). Similar geochemical characteristics to basalts in the Johnnys Creek Formation.|c. 824 Ma|||||
42483|Amata Dolerite|73086|5|Briefly described|p9, p15, p31, p40, p148, p151, p154|Tonian|Tonian|[Also written as Amata Dolerites]. Musgrave Province. Shares a geochemical affinity with basalt of Johnnys Creek Formation (Bitter Springs Group). Geochron is U-Pb baddeleyite age.|824 +/- 4 Ma|||Correlates to Gairdner dykes.||
42483|Amata Dolerite|73232|6|Mentioned|p6|Tonian|Tonian|Musgrave Province.|c. 825 Ma|||||
75900|Ambulbinya Supersuite|69917|5|Briefly described|p138, 142, 147, 152, 153, 154,156, 158|Statherian|Statherian|Dominates outcrop in the Entia Dome. ca. 1770 Ma. Includes Lionel Suite?or is precursor to Lionel Suite rocks? |ca 1770 Ma ||Includes Huckitta Suite, Inkamulla Granodiorite, Aremra Granodiorite.|Includes rafts of metasedimentary Entia and Valley Metamophics.||28-JUL-15
75900|Ambulbinya Supersuite|72516|5|Briefly described|p121|||Part of the calc-alkaline-trondhjemitic group of Zhao and McCulloch (1995). Incorporates the Entia Gneiss Complex. Outcrops below the informal CAT-line in the eastern Aileron Province.|ca. 1770-1750 Ma|||||09-JUN-21
76091|Amelia Dolostone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1645 Ma.|Unit in Loretta Supersequence.||||
76091|Amelia Dolostone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p18  |||Called Dolomite in Tb.1.||Of the Umbolooga Subgroup.||||
76091|Amelia Dolostone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive. The sideritic 'marble' is after sulfate evaporites.||Unit in Umbolooga Subgroup.||Overlies Mallapunyah Formation. Is overlain by Tatoola Sandstone.|Stratiform, domical, conical and columnar stromatolitic dololutite and silty dololutite with interbeds of dolarenite and shale and rare fine-grained sandstone; ooid, brecciated and conglomeratic intervals common; local sideritic 'marble'|
76091|Amelia Dolostone|67352|4|Described|p14 Tb.2, p58|Statherian|Statherian|McArthur Basin. 180 m thick. Sabkha. Hosts the Kilgour copper deposit.||Umbolooga Subgroup||Conformably overlies Mallapunyah Formation. Conformably overlain by Tatoola Sandstone.|Dolomudstone, silty dolomudstone, dolostone, breccia, conglomerate; minor shale; rare fine-grained sandstone.|
76091|Amelia Dolostone|69430|4|Described|p15:3, 17, 34, 42, 48-49|Statherian|Statherian|Southern McArthur Basin. 50-180m thick. Broad marginal marine sediments, with remobilised evaporites and brine flushing. Stromatolites occur as stratiform, domal, conical and columnar forms. Recessive unit. Hosts base metal prospects (eg Apollo, Coppermine Creek).||Umbolooga Subgroup.||Conformably overlies Mallapunyah Formation. Is overlain conformably by Tatoola Sandstone and unconformably by Bukalara Sandstone.|Stromatolitic dololutite and silty dololutite with interbeds of dolarenite and infrequent shale and rare fine-grained sandstone; ooid, brecciated and conglomeratic intervals common; localised diagenetic sideritic dololutite.|12-JUL-16
76091|Amelia Dolostone|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Umbolooga Subgroup||Overlies Mallapunyah Formation, overlain by Tatoola Sandstone||
76091|Amelia Dolostone|72373|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||||Overlain conformably by Tatoola Sandstone.||
76091|Amelia Dolostone|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 Mallapunyah Formation and underlies Tatoola Sandstone.||
76091|Amelia Dolostone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Underlain by Mallapunyah Formation. Overlain by Tatoola Sandstone.||
76091|Amelia Dolostone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Umbolooga Subgroup||Overlies Mallapunyah Formation and underlies Tatoola Sandstone.||
76091|Amelia Dolostone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Underlain by Mallapunyah Formation. Overlain by Tatoola Sandstone.||
76091|Amelia Dolostone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Mallapunyah Formation. Is overlain by Tatoola Sandstone.||
24156|Amesbury Quartzite|42504|6|Mentioned|p68|||Variation of Amesbury Quartzite Member.||||||
24156|Amesbury Quartzite|42643|1|Redefined|p51|Neoproterozoic||Originally 'Amesbury Quartzite Member' of Central Mount Stuart Formation.||||||12-OCT-10
24156|Amesbury Quartzite|42644|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Orthoquartzite, white; minor granule and pebble conglomerate. Geological Province: Georgina Basin.||||||15-NOV-05
24156|Amesbury Quartzite|60122|5|Briefly described|p9|||Within Supersequence 1 on HAY RIVER and HUCKITTA, not TOBERMORY. Geological Province: Georgina Basin.||||||11-MAY-05
24156|Amesbury Quartzite|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Plenty Group. Orthoquartzite; minor granule and pebble conglomerate.  Geological Province: southern Georgina Basin.||||||
24156|Amesbury Quartzite|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Plenty Group. Geological Province: Georgina/Ngalia Basin. Orthoquartzite, feldspathic quartz arenite, granule-bearing quartzite, basal granule/pebble conglomerate. [age shown may be indexing error]||||||14-JAN-16
24156|Amesbury Quartzite|62984|5|Briefly described|p13|Cryogenian|Cryogenian|Unconformably overlain by Boko Formation.  Geological Province: Georgina Basin. Shallow marine deposits known only in thin relict outliers - ~20m thick.||||||23-JAN-07
24156|Amesbury Quartzite|64068|3|Fully described|p44-45, p47, p51, p19, p223|Cryogenian|Neoproterozoic|20 m thick. Appears devoid of radioelements. Correlated with Yackah beds, Heavitree Quartzite, Vaughan Springs Quartzite.||Of Plenty Group.||Is unconformably overlain by Boko and Central Mount Stuart Formations.|White, rippled and cross-bedded orthoquartzite and quartz arenite; local thin basal conglomerate.|14-JAN-16
24156|Amesbury Quartzite|65237|5|Briefly described|p5|Neooproterozoic|Neoproterozoic|Unconformably overlain by Boko Formation and Oorabra Arkose.||||||07-FEB-11
24156|Amesbury Quartzite|65338|4|Described|p iv, p57, pp59-61.|Neoproterozoic|Neoproterozoic|Georgina Basin. Correlated with Vaughan Springs Quartzite. To 20 m thick outcrop. Originally named (Offe 1978) as member of Central Mount Stuart Formation. Upgraded to formation status by Haines et al. (1991). High energy nearshore to tidal environment.||Unit in Plenty Group.||Is unconformably overlain by Boko and Central Mount Stuart Formations.|Well-sorted and well-rounded, coarse-grained quartz arenite; local quartz overgrowths; local clay component; laminated to thinly bedded, shallow-angled planar cross-beds; ripple marks widespread; possible Planolites trace fossils.|
24156|Amesbury Quartzite|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Plenty Group.|||Orthoquartzite, feldspathic quartz arenite, granule-bearing quartzite, basal granule to pebble conglomerate; laminated, medium-bedded, ripple marked.|
24156|Amesbury Quartzite|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Plenty Group.|||Orthoquartzite, feldspathic quartz arenite, granule-bearing quartzite, basal granule/pebble-conglomerate; laminated, medium-bedded, ripple marked, (bioturbated?).|04-JUL-12
24156|Amesbury Quartzite|68270|5|Briefly described|p680,683|Tonian|Tonian|Southern Georgina Basin.||||Overlain unconformably by Boko Formation.||
24156|Amesbury Quartzite|69437|5|Briefly described|p22:4-6|Cryogenian|Cryogenian|SW Georgina Basin, Centralian A Superbasin. Supersequence 1.||Plenty Group.||||12-JUL-16
24156|Amesbury Quartzite|69443|4|Described|p28:5-8|Cryogenian|Cryogenian|Haines et al. (1991). Southern Georgina Basin. Unfossiliferous. c.20m thick. Forms cuestas and low rounded ridges. Probably fluviatile deposits.||Plenty Group.||Is overlain unconformably by Boko and Central Mount Stuart Formations. Correlated with lower interval of the Yackah beds.|Rippled and cross-bedded orthoquartzite and quartz sandstone, with dessication cracks and clay galls; local thin basal conglomerate; bimodal quartz granule to pebble beds occur near the base of the Formation.|12-JUL-16
24156|Amesbury Quartzite|69673|6|Mentioned|p112, p114 fig 92|||Around 20m thick.||Plenty Group|||Orthoquartzite and quartz sandstone.|
24156|Amesbury Quartzite|73086|6|Mentioned|p9, p145|||Georgina Basin, south-western.||||Correlates to Heavitree Formation.||
25761|Amos Formation|22538|6|Mentioned|P717||Statherian|Age of unit is 1614+/-4 Ma.||||||13-OCT-06
25761|Amos Formation|22664|6|Mentioned|Fig. 2 p34|||Of the Batten Subgroup (McArthur Group). Geolo. Prov:  McArthur Basin.||||||17-JUL-06
25761|Amos Formation|23396|4|Described|p413|Statherian|Statherian|Of McArthur Group. Age: 1614+/-4Ma. U-Pb SHRIMP dating from tuffs in the middle of the formation.||||||14-DEC-17
25761|Amos Formation|23397|5|Briefly described|p475|Statherian|Statherian|Age: 1614+/-4Ma.||||||13-OCT-06
25761|Amos Formation|23398|5|Briefly described|p443|||Of McArthur Group..||||||13-OCT-06
25761|Amos Formation|23406|5|Briefly described|p617|||Overlies Looking Glass Formation. Geological province: McArthur Basin. Part of the Lawn Supersequence.||||||24-JUN-09
25761|Amos Formation|23407|5|Briefly described|p628 Fig.4|Statherian|Statherian|Age: 1614+/-4Ma.||||||13-OCT-06
25761|Amos Formation|23776|5|Briefly described|p705 Fig 2|Statherian|Statherian|Age: 1614+/-4 Ma. Of Batten Subgroup.||||||17-JUL-06
25761|Amos Formation|23902|4|Described|p1568 Fig. 2|||Of the Batten Subgroup. Overlies the Stretton Sandstone. Geological Province: McArthur Basin.||||||13-OCT-06
25761|Amos Formation|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Subgroup.||||||
25761|Amos Formation|24048|5|Briefly described|p65|||Of the McArthur Group.  Age: 1614+/-4Ma.  Geological Province: McArthur Basin.||||||17-JUL-06
25761|Amos Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Batten Subgoup. Geological Province: Southern McArthur Basin.||||||
25761|Amos Formation|30344|6|Mentioned|Fig.4|||||||||
25761|Amos Formation|32658|3|Fully described|Table 2|||See also Fig. 3.||||||13-OCT-06
25761|Amos Formation|32660|5|Briefly described|Table 4|||||||||
25761|Amos Formation|35261|6|Mentioned|Fig.2|||||||||
25761|Amos Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25761|Amos Formation|40259|6|Mentioned|p242|||||||||
25761|Amos Formation|40691|4|Described|p55|||Also described Fig.38||||||
25761|Amos Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25761|Amos Formation|41268|5|Briefly described|Fig.3|||||||||
25761|Amos Formation|41277|6|Mentioned|Fig.2|||||||||
25761|Amos Formation|42385|5|Briefly described|p22|||||||||
25761|Amos Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Batten Subgroup (McArthur Group).||In schematic section, relationship not clear. Shown adjacent to unit of Stretton Sandstone with Yalco Formation; and underlies Balbirini Dolomite.|Upper: dolostone. Lower: siltstone, sandstone, sandy dolarenite and dololutite. Detailed lithology given.|09-NOV-11
25761|Amos Formation|42639|4|Described|p34, Table 5 p20|||||||||
25761|Amos Formation|42812|6|Mentioned|Fig.5|||||||||
25761|Amos Formation|42846|5|Briefly described|Fig.1 p502|||Of McArthur Group. Geological Province: McArthur Basin.||||||09-MAY-05
25761|Amos Formation|42935|6|Mentioned|p529 Fig.2|||Of Batten Subgroup.||||||13-OCT-06
25761|Amos Formation|43036|6|Mentioned|Fig.5|||Of McArthur Group.||||||13-OCT-06
25761|Amos Formation|44287|14|Not recorded|p.10, opp.9|||Of the McArthur Group.||||||17-JUL-06
25761|Amos Formation|44288|14|Not recorded|map legend|||Dolomitic siltstone, dolomite, dolomitic sandstone, sideritic chert. Lower (?) Proterozoic.||||||
25761|Amos Formation|45162|2|Defined|p130-136|Proterozoic|Proterozoic|Type section location given.||||||06-APR-18
25761|Amos Formation|60483|5|Briefly described|p7 Fig. 5, p8|Paleoproterozoic|Paleoproterozoic|Of Batten Subgroup (McArthur Group). Age: 1614+/-4Ma. Geological Province: McArthur Basin.||||||07-NOV-08
25761|Amos Formation|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1615-1610 Ma.|Unit in Lawn Supersequence.||||
25761|Amos Formation|63866|5|Briefly described|p56|Statherian|Statherian||1614 +/- 4 Ma|Lawn Supersequence||||
25761|Amos Formation|64815|5|Briefly described|p3, p4 Fig.2 |Statherian|Statherian||1614 +/- 4 Ma (SHRIMP zircon: Page et al, 2000).|Unit in Batten Subgroup.||||
25761|Amos Formation|64816|6|Mentioned|p2 Fig.1|||||Unit in McArthur Group.||||
25761|Amos Formation|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1614 +/- 4 Ma.|Unit in Batten Subgroup.||||
25761|Amos Formation|65228|5|Briefly described|p38, Table 1, Figs.02, 04, 24, 27.|Statherian|Statherian|Basal unit in Lawn Supersequence. Gamma ray log, lithology and facies detailed. Measured section.|1614 +/- 4 Ma.|Unit in Batten Subgroup.||Overlies Stretton Sandstone.||
25761|Amos Formation|66843|4|Described|p23-27, p35, p37, p38 Fig.10|||Southern McArthur Basin. Composite stratigraphic column; gamma-ray curve. Lithofacies detailed. Interpreted as Proterozoic calcrete developed from a gradual transgression from fluvial-mudflat environment to shallow-water (?marine) carbonate shoreline. Tuff layers with carbonate-filled "cross fractures" are compared with the Urquhart Shale in the Mount Isa Group.|1614 +/- 4 Ma (SHRIMP U-Pb zircon).|Topmost McArthur Group.||Overlies Looking Glass Formation. Is overlain by Balbirini Dolomite.|Includes red sandy grainstones and sandstones, and stylolitic and pisoloidal crystalline carbonate; pink tuff beds.|
25761|Amos Formation|67026|6|Mentioned|p343 Fig.12.|Statherian|Statherian|Referred to in a diagram of northern Australia's apparent polar wander path.|1614 Ma.|||||24-APR-12
25761|Amos Formation|69018|5|Briefly described|p450 Fig.1b|Statherian|Statherian|Of McArthur Basin.||Of McArthur Group.||||
25761|Amos Formation|69430|4|Described|p15:3, 16, 19|Statherian|Statherian|Southern McArthur Basin. Up to 70m thick. The lower part of the Formation represents a classic redbed environment; the middle part may have been deposited under shallow-marine conditions; and the upper 30m probably represents calcrete.|1614 +/- 4 Ma.|Batten Subgroup.||Disconformably overlies Stretton Sandstone or Looking Glass Formation. Is overlain unconformably by Balbirini Dolostone (Nathan Group).|Lower: red siltstone, fine sandstone, sandy dolarenite and dolostone. Upper: massive karstic-weathering dark grey to yellow-grey recrystallised dolostone.|12-JUL-16
25761|Amos Formation|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone|1614 +/- 4 Ma|Batten Subgroup||Conformably overlies Stretton Sandstone, Looking Glass Formation||
25761|Amos Formation|71374|5|Briefly described|p18||||1614 +/- 4 Ma (SHRIMP U-Pb)|McArthur Group||||
25761|Amos Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1614+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained pink tuffaceous rock in dolomite sequence.|
25761|Amos Formation|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Batten Subgroup.||||
25761|Amos Formation|72373|5|Briefly described|p17,22|||Of McArthur Basin. Dated at 1614+\-4 Ma; partially overlaps in age with Baiguridji Formation (Ahmad et al 2013).||upper McArthur Group [Batten Subgroup].||||01-OCT-19
25761|Amos Formation|72523|5|Briefly described|p1, p2, p2 Fig.2, p3, p6.|Statherian|Statherian|Date derived from GA sample ID 9577902 from a tuffaceous layer.|1614 +/- 4 Ma deposition|Top of the Batten Subgroup.||Unconformably underlies Nathan Group and underlies Balbirini Dolostone.|Includes tuffaceous rock.|
25761|Amos Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin. Batten Fault Zone (south).|1614 +/- 4 Ma|Batten Sub-group, McArthur Group||Underlain by Stretton Sandstone. Overlain by and partly equivalent to lower Balbirini Dolostone. Equivalent to Looking Glass Formation.||
25761|Amos Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Batten Subgroup.||Overlies Stretton Sandstone. Is overlain unconformably by Smythe Sandstone (Nathan Group).||
29231|Amos Knob Formation|14019|3|Fully described|p8|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Stromatolitic dolostone, dolarenite, mudstone, siltstone and shale. Conformable on Pear Tree Dolostone; conformably overlain by Mallabah Dolostone. Type section thickness: 50m. Geological Province: Birrindudu Basin.||||||07-NOV-08
29231|Amos Knob Formation|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
29231|Amos Knob Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
29231|Amos Knob Formation|24441|5|Briefly described|p1 Fig. 1|||Of Limbunya Group. Overlies Pear Tree Dolostone; overlain by Mallabah Dolostone. Geological Province: Birrindudu Basin||||||17-JUL-06
29231|Amos Knob Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
29231|Amos Knob Formation|28255|3|Fully described|p18, Tb.11 (opp.p8)|||Of the Limbunya Group. Dolomite interbedded with a softer rock type, probably green fissile siltstone.  Conformably overlain by Mallabah Dolomite; conformable on Pear Tree Dolomite. Age is Adelaidean or Carpentarian. Max. thickness: 50m. See also p118-119||||||
29231|Amos Knob Formation|30003|4|Described|p9|||Of the Limbunya Group. Carpentarian or Adelaidean. Max. thickness: 41m.||||||19-APR-05
29231|Amos Knob Formation|30004|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
29231|Amos Knob Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
29231|Amos Knob Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Dolomite and green siltstone, minor sandstone and shale.  Conformably overlis the Pear Tree Dolomite; conformably overlain by the Mallabah Dolomite.  Carpentarian to Adelaidean (per legend).||||||17-NOV-04
29231|Amos Knob Formation|32660|5|Briefly described|Table 6|||||||||
29231|Amos Knob Formation|33375|6|Mentioned|p9 Tb. 1|||Of the Limbunya Group. Interbedded dolomite and silty dolomite. Conformable on Pear Tree Dolomite.  Age is Carpentarian or Adelaidean.||||||26-APR-05
29231|Amos Knob Formation|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
29231|Amos Knob Formation|33378|5|Briefly described|Map legend|||Of the Limbunya Group. Interbedded dolomite and silty dolomite. Age is Carpentarian or Adelaidean.||||||28-APR-05
29231|Amos Knob Formation|45112|5|Briefly described|Table 7|||||||||
29231|Amos Knob Formation|48943|2|Defined|p20|Proterozoic|Proterozoic|Strat. section p129.||||||17-JUL-06
29231|Amos Knob Formation|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Stromatolitic dolostone, dolarenite, mudstone, dolomitic mudstone.  Geological Province: Birrindudu Basin.||||||07-NOV-08
29231|Amos Knob Formation|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dolostone and green siltstone, shale, minor sandstone. Of Limbunya Group. Overlain by Mallabah Dolostone. Overlies Pear Tree Dolostone. Geological Province: Birrindudu Basin.||||||07-NOV-08
29231|Amos Knob Formation|60685|5|Briefly described|p4 Figure 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
29231|Amos Knob Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Pear Tree Dolostone. Is overlain by Mallabah Dolostone.||
29231|Amos Knob Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Pear Tree Dolostone. Is overlain by Mallabah Dolostone.|Dolostone, locally stromatolitic, silty dolostone.|
29231|Amos Knob Formation|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
29231|Amos Knob Formation|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
29231|Amos Knob Formation|69432|5|Briefly described|p17:2, 7|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 50m thick. ||Limbunya Group.|||Composed mostly of red and green mudstone beds, interbedded with 1-3m-thick, biohermal stromatolitic dolostone intervals and thin dolarenite.|12-JUL-16
29231|Amos Knob Formation|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Pear Tree Dolostone, overlain by Mallabah Dolostone||
29231|Amos Knob Formation|70655|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Birindudu Basin.||Limbunya Group||Overlies Pear Tree Dolostone. Is overlain by Mallabah Dolostone.|Dolostone, locally stromatolitic, silty dolostone.|
29231|Amos Knob Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Limbunya Group.||Overlies Pear Tree Dolostone. Is overlain by Mallabah Dolostone.|Dolostone and green siltstone, shale, minor sandstone.|
29231|Amos Knob Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Mallabah Dolostone. Underlain by Pear Tree Dolostone.||
29231|Amos Knob Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Pear Tree Dolostone. Overlain by Mallabah Dolostone.||
29231|Amos Knob Formation|73280|6|Mentioned|p1, p4-5, App.1A|||Birrindudu Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
68767|Ampiara member|60683|5|Briefly described|p9 Tb. 1|Cambrian|Cambrian|Informal name.  Of the Mount Currie Conglomerate.  Conglomerate dominated by clasts of sandstone; very minor basalt and rhyolite. geological Province: Musgrave Block/Amadeus Basin.||||||
68767|Ampiara member|61386|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Mount Currie Conglomerate. Conglomerate with rounded pebble to boulder-sized clasts of silicified Winnall beds sandstone, with minor tuff fragments in the upper section; epidotised sandstone matrix.  Geological Province: Amadeus Basin.||||||23-DEC-09
35317|Amputjuta Dacite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Granite Suite.  Geological Province: Musgrave Block.  Age: ~1150Ma.||||||09-JUN-04
35317|Amputjuta Dacite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Finely porphyritic hypabyssal dacite.  Geological Province: Musgrave Block.||||||12-JAN-05
35317|Amputjuta Dacite|61154|5|Briefly described|p10, p44 App., p28|Mesoproterozoic|Mesoproterozoic|Of Pottoyu Suite (Pitjanjatjara Supersuite). A hybabyssal intrusive unit containing phenocrysts of plagioclase and qtz in a fine-grained matrix of qtz, feldspar, biotite and chlorite with variably developed biotite foliation. Underlies Dean Quartzite.||||||
35317|Amputjuta Dacite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Pottoyu Granite Suite.  Finely porphyritic hypobyssal biotite dacite, less abundant equigranular leucogranite.  Age: ~1150Ma. Geological Province: Musgrave Block.||||||19-OCT-05
35317|Amputjuta Dacite|65256|2|Defined|piii, p7-8, p7 Tb.1, p30, p37|Stenian|Ectasian|New Name. Pb-Pb evaporation on zircon age. Previous informal name said to have been Manananna Porphyry (Forman 1966)[in fact Forman proposed the name Mannanana (sic) Porphyry in 1963]. Shallow level intrusive. Type locality 4.5 km SW of Amputjuta Outstation.|1153+/-3 Ma.|Of the Pottoyu Granite Suite.||Overlain by Kulail Sandstone, Dean Quartzite; intruded by mafic dykes interpreted to belong to Alcurra dolerite..|Porphyritic hypabyssal dacite with fine-grained phenocrysts of plagioclase; less abundant equigranular leucogranite.|26-MAR-15
35317|Amputjuta Dacite|69091|6|Mentioned|p139 Fig.6.6|||Mis-spelt as Amputjatja Dacite.||||||
35317|Amputjuta Dacite|69436|5|Briefly described|p21:9-10|Mesoproterozoic|Mesoproterozoic|Close et al. (2003). A hypabyssal intrusive unit in the Mannanana Range; geochemically equivalent to the rest of the Pottoyu Suite. Kober Pb-Pb zircon crystallisation age.|1153 +/- 5 Ma (Close et al., 2003).|Pottoyu Suite.||Is overlain by Dean Quartzite.|Contains phenocrysts of plagioclase and quartz in a fine-grained matrix of quartz, feldspar, biotite and chlorite, with a variably developed biotite foliation.|12-JUL-16
35317|Amputjuta Dacite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite|
35317|Amputjuta Dacite|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province.||Unit of Pottoyu Granite Suite.|||Finely porphyritic hypabyssal dacite|
80427|Amungee Member|71779|2|Defined|iii, p1-p4, p7-p9, p11-p16, p23|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Name proposed by TJ Munson and D Revie. Named for the Amungee Mungee Station in central-western TANUMBIRINI. The type section occurs in POG Alexander 1 from ca 446m to ca 280m. Corresponds to the now obsolete middle Velkerri Formation of previous usage. Subdivided into informally named A-C organofacies. The primary target for petroleum exploration in the Velkerri Formation. Distinguished from the Kalala and Wyworrie members by generally lower (poor to good) TOC values, geochemistry, geophysical logs; these features are discussed in some detail. Geomorphic expression is discussed briefly. Age is derived from underlying rare tuffs in the Showell Member of the Mainoru Formation. Thickness in various drillholes and mapsheet names for intersections provided. Deposited in a subtidal, sub-wave base, and generally quiet marine environment with regular current activity consistent with periodic turbidity currents. See also p18-p20, p24, p26-p27.||Velkerri Formation||Conformably overlies the Kalala Member. Overlies the Showell Member of the Mainoru Formation. Conformably overlain by the Wyworrie Member.|Interlaminated to thinly interbedded, grey-green to dark grey claystone, pale grey siltstone and rare, light grey fine-grained sandstone with thick intervals of massive to laminated, grey-green and dark grey to brown-black (carbonaceous) claystone.|24-SEP-18
80427|Amungee Member|72381|5|Briefly described|p776|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. ||Unit of Velkerri Formation.||Overlain by Wyworrie Member. Underlain by Kalala Member.||
80427|Amungee Member|72912|6|Mentioned|p36.|||Located in the McArthur Basin.||Velkerri Formation|||May include hydrocarbon bearing shales (Jackson et al., 1988).|
80427|Amungee Member|73242|5|Briefly described|p39|Ectasian|Ectasian|Geochron from black shales (Kendall et al., 2009).|1361 +/- 21 Ma, 1417 +/- 29 Ma Re-Os|Velkerri Formation, Maiwok Subgroup, Roper Group||Underlain by Kalala Member. Overlain by Wyworrie Member.|Includes mudstone and shale.|
80427|Amungee Member|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin +/- Beetaloo Sub-basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||Velkerri Formation||||
24158|Andagera Formation|22954|6|Mentioned|Fig3p9|Early Cambrian|Early Cambrian|||||||
24158|Andagera Formation|24172|5|Briefly described|p54|Early Cambrian|Neoproterozoic|Geological Province: Georgina Basin. Correlated with Rising Sun Conglomerate.||||||
24158|Andagera Formation|40578|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Conglomerate, sandstone.||||||
24158|Andagera Formation|40580|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
24158|Andagera Formation|40836|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Early to Middle Cambrian||||||17-JUL-06
24158|Andagera Formation|41128|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Conglomerate, massive and medium to thick-bedded, oligomictic, pebble to boulder clasts; quartz sandstone. Geological Province: Georgina Basin.||||||16-NOV-05
24158|Andagera Formation|41129|3|Fully described|p10|Cambrian|Cambrian|||||||
24158|Andagera Formation|41204|4|Described|p13|||Mention p4||||||17-JUL-06
24158|Andagera Formation|41205|5|Briefly described|Map legend|Cambrian|Cambrian|Conglomerate, sandstone. Geological Province: Georgina Basin.||||||16-NOV-05
24158|Andagera Formation|41310|5|Briefly described|p14|||||||||
24158|Andagera Formation|41524|2|Defined|p37|Early Cambrian||Described p3 and p11||||||17-JUL-06
24158|Andagera Formation|41525|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Quartz sandstone, thick-bedded, pebbly, conglomerate interbeds; conglomerate, massive, oligomictic; quartz sandstone towards top.||||||26-OCT-05
24158|Andagera Formation|42643|3|Fully described|p26|Neoproterozoic||||||||
24158|Andagera Formation|42644|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Conglomerate, massive, oligomictic, arenaceous matrix; sandstone, pebbly. Geological Province: Georgina Basin.||||||15-NOV-05
24158|Andagera Formation|42956|4|Described|p33|||see also Fig.4 p31||||||
24158|Andagera Formation|45167|5|Briefly described|p53|||||||||
24158|Andagera Formation|47058|6|Mentioned|Fig.3 P123|||||||||
24158|Andagera Formation|60122|6|Mentioned|p9|||||||||
24158|Andagera Formation|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Conglomerate: massive, oligomictic, arenaceous matrix; pebbly sandstone. Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
24158|Andagera Formation|61567|5|Briefly described|p632|Neoproterozoic|Neoproterozoic|Poorly sorted sandstones and conglomerates with pitted weathering surfaces. Age: ca600Ma. Max. thickness: 50m. See also p633 Tb. 1.||||||
24158|Andagera Formation|63562|6|Mentioned|p345|Early Cambrian|Ediacaran|Georgina Basin. ||||||
24158|Andagera Formation|64068|3|Fully described|p53, p51, p224|Middle Cambrian|Ediacaran|Correlations: Red Heart Dolostone (Stidolph et al 1988) or Central Mount Stuart Formation (Haines et al 1991).||Of Mopunga Group.||Unconformably overlies Hatches Creek Group. Overlain disconformably by Thorntonia Limestone or Gum Ridge Formation.|High-energy fluviatile and possibly shallow-marine pebble to boulder conglomerate, pebbly sandstone; minor red siltstone.|04-APR-12
24158|Andagera Formation|65338|6|Mentioned|p3, p63.|Ediacaran|Ediacaran|Davenport Province.||Unit in Mopunga Group.||||
24158|Andagera Formation|65341|6|Mentioned|p14. |||||Unit in Mopunga Group.||||
24158|Andagera Formation|67148|5|Briefly described|Map legend.|Ediacaran|Ediacaran|||Unit in Mopunga Group.|||Conglomerate: massive and medium- to thickly-bedded, oligomict, pebble to boulder clasts; quartz sandstone; rare pebbles and boulders, thinly to thickly bedded, parallel and crossbedded; siltstone lenses.|
24158|Andagera Formation|67352|4|Described|v, p17-18, p44 fig 48|Ediacaran|Ediacaran|Stidolph et al. (1988). Displays marked lateral lithological variation. Lithologically similar to Central Mount Stuart Formation.||Mopunga Group||Is overlain by Thorntonia Limestone and Gum Ridge Formation.|Flat-lying conglomerate, sandstone and minor red siltstone.|
24158|Andagera Formation|68518|3|Fully described|p11, p14|Middle Cambrian|Early Cambrian|Defined by Stidolph and others (in prep.). Was previously mapped as part of Sandover beds (Smith and Milligan, 1966) in central and eastern parts of region, and as part of Tomahawk beds (Smith and Milligan, 1964) in the west. Forms mesas and hills, thickness ranges from less than 1m to possibly 50m, and considered Early to Middle Cambrian (Stidolph and others, in prep.; Walley and Simons, in prep.). Fluvial and scree deposits.||||Overlain conformably by Sandover beds.|Generally flat-lying conglomerate and sandstone.|
24158|Andagera Formation|69424|5|Briefly described|p9:26-27|Ediacaran|Ediacaran|Georgina Basin.|||||Includes conglomerate.|12-JUL-16
24158|Andagera Formation|69425|6|Mentioned|p10:19|Neoproterozoic|Neoproterozoic|||||Unconformably overlies Hanlon Subgroup (Hatches Creek Group).||12-JUL-16
24158|Andagera Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SW Georgina Basin, Centralian A Superbasin. Supersequence 3.||||Equivalent to Central Mount Stuart Formation.||12-JUL-16
24158|Andagera Formation|69443|4|Described|p28:7, 10, 12|Ediacaran|Ediacaran|Bagas et al. in Stidolph et al. (1988). Southern Georgina Basin. Exposed as ridge tops, or terraces and mesas within extant valleys. Up to 50m thick. Previously thought to be Early to early Middle Cambrian, based on inferred correlation with Red Heart Dolostone.||Mopunga Group.||Overlies Grant Bluff Formation, Elkedra Granite nonconformably and Hatches Creek Group unconformably. Overlain disconformably by Thorntonia Limestone and Gum Ridge Formation (possibly transitionally).|Pebble to boulder conglomerate, pebbly sublithic sandstone and minor siltstone. Coarser beds are poorly sorted and feature normal grading, ripples and cross-beds. Generally unfossiliferous.|12-JUL-16
24158|Andagera Formation|69673|5|Briefly described|p114 fig 92, p116, p135|Ediacaran|Ediacaran |50m thick. Some potential as a reservoir rock.||Mopunga Group||Overlies Elkera Formation, Central Mount Stuart Formation|Pebble to boulder conglomerate, coarse to pebbly sandstone and minor siltstone.|
24158|Andagera Formation|69917|6|Mentioned|p115|||Georgina Basin. Walter et al (1995) assigned this unit to Supersequence 4 of their Centralian Superbasin.||||||
24158|Andagera Formation|73083|6|Mentioned|p20|Neoproterozoic|Neoproterozoic|Deposited in paleo-valleys.||||||
24158|Andagera Formation|73086|6|Mentioned|p133|||Georgina Basin.||||Correlates to Julie Formation.||
33655|Angatja Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: ~1070Ma?||||||17-JUL-06
33655|Angatja Granite|60683|2|Defined|p54 Appendix, p19-20|Mesoproterozoic|Mesoproterozoic|Of Angatja Granite Suite. Synonymous with part of Musgrave-Mann Metamorphics of Thomson (1969) and undivided metamorphosed granites of Forman (1972).  A suite of charnockite, hornblende granite and rapakivi granite. Age: c.1070Ma.  See also p9 Tb.1, p42.||||||23-DEC-09
33655|Angatja Granite|61154|4|Described|p14, p13, p42,42 in Appendix|Mesoproterozoic|Mesoproterozoic|See also Angatja Suite. Includes charnockite, hornblende granite and rapakivi granite; the granite is dominantly porphyritic. Intrudes the Alcurra Dolerite in the eastern Mann Ranges. Age: 1071+/-5Ma (Scrimgeour et al 1999). Geol. Province: Musgrave Block||||||14-JUL-05
33655|Angatja Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic orthopyroxene-clinopyroxene granite (locally with rapakivi textures) and coarsely porphyritic hornblende-biotite granite; both variably mylonitised and recrystallised.  Age: ~1070Ma. Geological Province: Musgrave Block.||||||
33655|Angatja Granite|61524|5|Briefly described|p18 Fig.2(a)|||Geological Province: Musgrave Province.||||||
33655|Angatja Granite|61864|6|Mentioned|p19 fig 5|||Granite intrusion and associated dykes related to the Giles Complex.||||||
33655|Angatja Granite|63866|5|Briefly described|p207|Stenian|Stenian|Fregon Domain, Musgrave Province.|1071 +/- 5 Ma (Scrimgeour et al, 1999)|||||
33655|Angatja Granite|65256|6|Mentioned|p15|Stenian|Stenian|Correlated with Hull Granite Suite; 1071+/-5 Ma.||||||
33655|Angatja Granite|67128|5|Briefly described|p3, p27-28|||Eastern Mann Ranges. Strongly deformed during the Petermann Orogeny.|1071 +/- 5 Ma (Scrimgeour et al., 1999).||||Mesocratic, K-feldspar porphyritic to rapakivi-textured, hornblende-orthopyroxene-biotite-garnet bearing granite.|
33655|Angatja Granite|67536|5|Briefly described|Map Legend|Stenian|Stenian|Musgrave Block.|ca. 1070 Ma||||Massive granite; weakly magnetic.|
33655|Angatja Granite|69436|5|Briefly described|p21:11|Mesoproterozoic|Mesoproterozoic|Scrimgeour et al. (1999). Kober Pb-Pb zircon age of granite.|1071 +/- 5 Ma (Scrimgeour et al., 1999).|Angatja Suite.|||Coarsely porphyritic hornblende granite; contains coarse ellipsoidal pale-blue K-feldspar phenocrysts, elongated in the fabric; mafic minerals constitute 20-25% of the rock.|12-JUL-16
33655|Angatja Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1071+/-5 Ma (crystallisation).||||Granite.|
42420|Angatja Suite|24496|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|See also Angatja Granite Suite. Granitoids.  Geological Province: Musgrave Block.||||||
42420|Angatja Suite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Porphyritic granite, coarsely porphyritic granite. Geological Province: Musgrave Block.||||||14-JAN-05
42420|Angatja Suite|60683|6|Mentioned|p10 Tb. 1|||Informal abbreviation of Angatja Granite Suite?||||||
42420|Angatja Suite|61154|5|Briefly described|p12, p28|Mesoproterozoic|Mesoproterozoic|See also Angatja Granite Suite. Age: 1071+/-5Ma.||||||17-JUL-06
42420|Angatja Suite|69436|4|Described|p21:11-12, 14|Mesoproterozoic|Mesoproterozoic|After Angatja Granite (Scrimgeour et al., 1999). Musgrave Province. Emplaced during the Giles Event (1085-1040 Ma). Believed to be genetically related to the Giles Complex. Kober Pb-Pb zircon age of granite.|1071 +/- 5 Ma (Scrimgeour et al., 1999).|Warakurna Supersuite.|Angatja Granite.|Intrudes Alcurra Dolerite and Musgravian gneiss. Is intruded by Kullal Dyke Suite.|Charnockite, dark, overprinted with mylonitic fabric; coarsely porphyritic hornblende granite, with pale blue K-feldspar phenocrysts elongated in the fabric; and rapakivi granite bodies forming fine-grained dykes with coarse K-feldspar crystals.|12-JUL-16
42420|Angatja Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite, granite|
23336|Angulmeri Quartzite Member|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
69778|Anira Metamorphics|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Granulite facies metasediments; cordierite-rich migmatite, meta-psammite.||||||28-JUL-15
69778|Anira Metamorphics|65341|2|Defined|p2 Fig.2, pp3-4, p20, pp27-28. |Paleoproterozoic|Paleoproterozoic|New name (Haines and Scrimgeour). Previously mapped (Shaw and Warren 1975) as part of Woodgreen Granite Complex. Type locality is a hill 2 km north-northwest of Anira Dam. Several small outcrops of granulite-facies metasedimentary rocks, mostly pelitic with well preserved sedimentary layering. Metamorphosed during Strangways Event. Has affinities with Deep Bore Metamorphics which underwent high-T, low-P (3 - 4 kbar and 750 - 800 degrees C) metamorphism during the Strangways Orogeny at 1730 +/- 7 Ma.|Max. deposition age c. 1785 Ma.|||Intruded by Woodgreen Metamorphic Complex.|Cordierite-sillimanite-spinel migmatitic metapelite; lesser metapsammite.|19-JUN-13
69778|Anira Metamorphics|65556|4|Described|p2 Tb.1, p35-38, p45, p46 Fig.74, p69-70||Orosirian|Aileron Province, Arunta Region. Succession of granulite-facies metamorphic rocks dominated by metapelite; biotite-garnet metapsammite forms thin, generally leucosome-free layers. Has high volumes of melt, locally with tabular feldspars and probably equivalent to the enclosing Woodgreen Granite Complex. Occurs as several small outcrops in the Alcoota 1:250,000 map sheet. SHRIMP U-Pb zircon maximum deposition age of 1785+/-19 Ma. SHRIMP U-Pb zircon rim age of 1723+/-3 Ma dates metamorphism.||||||
69778|Anira Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block.|1785 +/- 19 Ma (maximum depositional age).|||||
69778|Anira Metamorphics|68150|5|Briefly described|p11 Tb.3.2|||SHRIMP age: Casey Inlier, MSWD 1.8, 15 analyses, Carson et al. (2009).|1723 +/- 3 Ma, metamorphism|||||
69778|Anira Metamorphics|69427|5|Briefly described|p12:3, 8, 27, 39, 41|Statherian|Statherian|Haines and Scrimgeour (2007). Aileron Province. Crops out S of Kunoth Knob. SHRIMP U-Pb detrital zircon maximum depositional age. Metamorphic rims are similarly dated at 1724 +/- 3 Ma.|<1785 +/- 19 Ma (Carson et al., 2009).|||Transitions into the surrounding Woodgreen Granite Complex.|Dominantly pelitic low-P granulite-facies metasedimentary rocks with well-preserved sedimentary layering; high volume of leucosome. Localised larger garnet-bearing melt accumulations contain tabular K-feldspar.|12-JUL-16
69778|Anira Metamorphics|69510|6|Mentioned|p12|||The 1735-1690 Ma Strangways Event is recognised in monazite and zircon rims in rocks of this unit.||||||
69778|Anira Metamorphics|69917|5|Briefly described|p104, 106|||Granulite-facies metasedimentary rocks. ||||Intruded by Woodgreen Granite Complex.||
69778|Anira Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphosed at 1723 +/- 3 Ma.|1785+/-19 Ma (MDA: SHRIMP zircon).||||Migmatite.|
39322|Ankala Gneiss|9199|5|Briefly described|Map legend|||Leucocratic biotite gneiss, calc-silicate rock, amphibolite.||||||03-NOV-04
39322|Ankala Gneiss|23983|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
39322|Ankala Gneiss|23984|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
39322|Ankala Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Leucocratic biotite gneiss, calc-silicate rock, amphibolite.||||||
39322|Ankala Gneiss|69427|5|Briefly described|p12:9, 14, 41|||Strangways Range region, Ankala Domain, Aileron Province. Crops out immediately S of Harry Creek Shear Zone, and N of Bald Hill and Winnecke Shear Zones. Has undergone widespread retrogression during the Alice Springs Orogeny. Hosts some deposits of the Winnecke goldfield.||||Is intruded by Gumtree Granite.|Felsic gneiss, calc-silicate rock, metapelitic gneiss, mafic rock and rare marble, ultramafic rock, quartz-hematite rock and cummingtonite-rich rock; local skarns at intrusions.|12-JUL-16
39322|Ankala Gneiss|71839|5|Briefly described|p10-p11|||||||Intruded by the Gumtree Granite.||
35247|Anmatyerre Clay|61828|5|Briefly described|p162, p163 Fig. 4|Middle Pleistocene|Early Pleistocene|Distinctive lacustrine facies - red/brown homogeneous clay. Overlain by Tilmouth beds.||||||
35247|Anmatyerre Clay|65194|6|Mentioned|p56|||Lacustrine clay at Lake Lewis. Up to 80m thick, covering over 3000 km2; commonly infills basement depressions. Over nine vertical metres were deposited over last 780,000 years.||||||
35247|Anmatyerre Clay|69458|5|Briefly described|p42:12-13, 24|Pleistocene|Miocene|English (2001, 2005). Lake Lewis Basin. Up to 80m of freshwater lacustrine clays.||||Is overlain by Tilmouth beds.|Continuous uniform red-brown clay.|12-JUL-16
72424|Anningie Member|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Mica, hornblende-biotite and hornblende schist; biotite gneiss; epidote-amphibolite; quartz diorite gneiss; rare schist, hornfels||||||07-NOV-08
72424|Anningie Member|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Lander Rock Formation. Mica, hornblende-biotite and hornblende schist; biotite gneiss; epidote amphibolite/amphibolite; rare sillimanite +/- microcline-bearing schist; calc-silicate rocks.||||||
72424|Anningie Member|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Lander Rock Formation. Mica, hornblende-biotite and hornblende schist; biotite gneiss; epidote amphibolite/amphibolite; rare sillimanite +/- microcline-bearing schist; calc-silicate rocks.||||||
72424|Anningie Member|65338|3|Fully described|App 1 p83-84, p8 Table 1, pp10-11 |Statherian|Orosirian|New name. Polydeformed with moderately dipping S1 foliation. Thickness estimated to c.1200 m. Correlated with part of both the Bullion Schist and Ooradidgee Group. Geophysical interpretation indicates a lower stratigraphic level than Walabanba Member. Age constrained by stratigraphic position and intrusion||Unit in Lander Rock Formation.||Intruded by 1789 +/-6 Ma Esther Granite, un-named granites and dolerite.|Predominantly schistose, micaceous, fine-grained, quartzo-feldspathic; locally more coarse-grained and gneissic; layer-parallel amphibolite; provenance interpreted to include dominant potassic, felsic volcanic component; no sedimentary structures.|
72424|Anningie Member|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Mica, hornblende-biotite and hornblende schist; biotite gneiss; epidote-amphibolite; quartz diorite gneiss; rare sillimanite-bearing schist; hornfels.|
72424|Anningie Member|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Mica, hornblende-biotite and hornblende schist; biotite gneiss; epidote-amphibolite; quartz diorite gneiss; rare sillimanite-bearing schist; hornfels.|
72424|Anningie Member|69427|5|Briefly described|p12:5-6|||Aileron Province. More or less proximal shallow-water deposits.||Lander Rock Formation.||Correlative of Woolla Gneiss.|Schist.|12-JUL-16
76092|Anthony Lagoon Formation|67144|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|||Unit in Barkly Group.||Unconformably overlies Top Springs Limestone.|Dolo-mudstone/sparstone, dolomitic-siliciclastic silt- and mud-stone, dolomitic sandstone-siltstone interbeds; nodular and bedded evaporite, chert concretions; minor intraclast and oncoid dolostone, microbial dololaminite, dolomitic quartz sandstone.|
76092|Anthony Lagoon Formation|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin. Lateral equivalent to Wonarah Formation.||Unit in Barkly Group.||Overlies Gum Ridge Formation.|Dolomudstone/dolosparstone, dolomitic-siliciclastic siltstone and mudstone, dolomitic sandstone-siltstone interbeds; evaporite, chert concretions; minor intraclast and oncoid dolostone, microbial dololaminite, dolomitic quartz sandstone.|
76092|Anthony Lagoon Formation|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin. Lateral equivalent to Wonarah Formation.||Unit in Barkly Group.||Unconformably overlies Gum Ridge Formation.|Dolomudstone/dolosparstone, dolomitic-siliciclastic siltstone and mudstone, dolomitic sandstone-siltstone interbeds; evaporites, chert concretions; minor intraclast and oncoid dolostone, microbial dololaminite, dolomitic quartz sandstone.|
76092|Anthony Lagoon Formation|67352|2|Defined|v, p23-30, 46, 49, 50, 52, 60, p69 |Middle Cambrian|Middle Cambrian|DEFINED on p69; formerly Anthony Lagoon beds (Plumb and Rhodes 1963). It has a clear Th signature. Correlates with: Inca Formation, Gowers Formation, Beetle Creek Formation, Currant Bush Limestone, Blazan Shale (Undilla Sub-basin), Arthur Creek Formation (Georgina Basin). Essentially unfossiliferous.||Barkly Group||Overlies Gum Ridge Fm (conformably) and Top Springs Limestone. Possibly overlies Mittiebah Sandstone (unconformably). Interfingers with Wonarah Fm. Is overlain (unconformably) by Brunette Limestone.|Maroon dolomitic-siliciclastic siltstone; grey dolostone with dolomudstone interbeds, dolopack/grainstone, ooid dolograinstone, microbial dololaminite and sucrosic dolostone; med-coarse dolomitic quartz sandstone; evaporite and siliceous concretions|07-JAN-15
76092|Anthony Lagoon Formation|69431|5|Briefly described|p16:18-19|||Kruse et al. (2009). Georgina Basin.||||Unconformably overlies Gleeson Formation (Renner Group).||12-JUL-16
76092|Anthony Lagoon Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Georgina Basin, Centralian B Superbasin. Sequence 2. Unfossiliferous. Lithologically very similar to Jinduckin Formation to the NW (Daly Basin).||||Overlies Top Springs Limestone and Gum Ridge Formation. Lateral equivalent of Wonarah, Jinduckin Formations.|Dolomitic/siliciclastic siltstone interbedded with dolostone.|12-JUL-16
76092|Anthony Lagoon Formation|69443|4|Described|p28:16, 21-23, 25, 45|Middle Cambrian|Middle Cambrian|Kruse et al. (2010) after Plumb and Rhodes (1963, 1964). Central Georgina Basin. Virtually unfossiliferous heterolithic carbonate-siliciclastic unit. Crops out poorly: rubble tracts, cobble and boulder fields, locally (sandstone) ridge-forming. Is correlated with several units (listed) in the Narpa Group, and Ranken Limestone and Camooweal Dolostone. 50-244.2m thick. Deposited on a mixed carbonate-siliciclastic tidal flat subject to recurring supratidal exposure. Was unsuccessfully  analysed for economic uranium mineralisation in 2008.||Barkly Group.||Overlies Gum Ridge Formation and ?Top Springs Limestone conformably, and Mittiebah Sandstone unconformably. Is overlain unconformably by Brunette Limestone. Passes laterally into Wonarah Formation.|A distinctive maroon dolomitic-siliciclastic siltstone interbedded with pale grey dolostone; nodular and bedded evaporite and siliceous (chert) concretions common; dolomitic sandstone-siltstone interbeds and beds of quartz sandstone present.|12-JUL-16
76092|Anthony Lagoon Formation|69446|5|Briefly described|p31:4|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Overlies Gum Ridge Formation. Lithologically correlated with Jinduckin Formation (Daly Basin).||12-JUL-16
76092|Anthony Lagoon Formation|69447|6|Mentioned|p32:2|||Georgina Basin.||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
76092|Anthony Lagoon Formation|69458|5|Briefly described|p42:19|Cambrian|Cambrian|Georgina Basin.||||Is overlain unconformably by Brunette Limestone.||14-SEP-18
76092|Anthony Lagoon Formation|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
76092|Anthony Lagoon Formation|69673|5|Briefly described|p58, p117|||244m thick.||Barkly Group||Unconformably overlies Renner Group|Siltstone interbedded dolostone, dolomitic sandstone-siltstone and beds of sandstone.|
76092|Anthony Lagoon Formation|70380|5|Briefly described|p745-746, p759|Series 3|Series 3|Kruse et al. (2010); formerly Anthony Lagoon beds. Georgina Basin.||||Interdigitates with Wonarah Formation. Lithologically correlated with Jinduckin Formation (Daly Basin).||
76092|Anthony Lagoon Formation|70968|5|Briefly described|p95|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Unconformably overlies (onlaps) Gleeson Formation locally.||
76092|Anthony Lagoon Formation|72967|6|Mentioned|p5|||Georgina Basin.||Barkly Group||||
76092|Anthony Lagoon Formation|73083|6|Mentioned|p7, p12, p22, p25, p28, p43, p46-48|Cambrian|Cambrian|Georgina Basin.||Barkly Group|||Limestone and siliciclastics.|
73191|Apertawonga Monzogranite|62580|5|Briefly described|p43|||Of the Frederick Suite. Hornblende biotite monzogranite in a non-magnetic, poorly defined pluton south of Tanami Mine.||||||07-FEB-11
73191|Apertawonga Monzogranite|64675|6|Mentioned|Fig.15(b)|||See also Apertawonga granite.||||||
74208|Aquitaine Formation|61542|5|Briefly described|p277 Fig. 2|Namurian|Namurian|Of the Wadeye Group - offshore equivalent of the onshore Point Spring Sandstone. Geological Province: onshore Bonapart Basin/Petrel-Sub-basin. Lower sandstone grading up into siltstone.||||||07-FEB-11
74208|Aquitaine Formation|67354|6|Mentioned|p73. |||||Offshore unit in Wadeye Sub-Group.||||
74208|Aquitaine Formation|69452|3|Fully described|p36:9, 15, 17|||Gorter et al. (2005). Subsurface. Petrel Sub-basin, Bonaparte Basin. Is 95m thick in the type section in Sandbar-1. Mostly non-marine deposits. Over 200m thick. Offshore and onshore.||Wadeye Group.||Unconformably overlies Arco Formation. Lateral equivalent of Point Spring Sandstone (WA). Is overlain unconformably by Kuriyippi Formation.|Fine- to coarse-grained sandstone with a few siltstone interbeds, grading up into siltstone.|12-JUL-16
74208|Aquitaine Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Wadeye Group.||Overlies Arco Formation. Is overlain by Kuriyippi Formation (Kulshill Group).||
74208|Aquitaine Formation|69673|5|Briefly described|p172|||||Wadeye Group|||Interbedded siltstone/shale and sandstone.|
74208|Aquitaine Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Bashkirian|Bashkirian|See also Regional geology: Fig.8. Hydrocarbon reservoir.||Wadeye Group.||Overlies Arco Formation. Is overlain by Kuriyippi Formation.||12-JUL-16
74208|Aquitaine Formation|73117|6|Mentioned|p15|Bashkirian|Bashkirian|Bonaparte Basin, southern. Palynozonation: S. ybertii.||Wadeye Group||Underlain by Arco Formation. Equivalent to Point spring Sandstone.||
24163|Arabulja Volcanics|23733|5|Briefly described|p20, 22|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup.||||||07-NOV-08
24163|Arabulja Volcanics|23809|5|Briefly described|p27 Fig. 25|||Of the Wauchope Subgroup (Hatches Creek Group).  Geological Province: Davenport Province.||||||
24163|Arabulja Volcanics|24197|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of the Treasure Suite. Geological province: Davenport Province.||||||07-FEB-11
24163|Arabulja Volcanics|39624|5|Briefly described|Table 1|||||||||
24163|Arabulja Volcanics|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24163|Arabulja Volcanics|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24163|Arabulja Volcanics|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24163|Arabulja Volcanics|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Felsic lava, generally porphyritic. Geological Province: Tennant Creek Block.||||||07-NOV-08
24163|Arabulja Volcanics|41129|4|Described|Table 1|||Mention p10.||||||18-AUG-08
24163|Arabulja Volcanics|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Felsic lava.||||||16-NOV-05
24163|Arabulja Volcanics|41308|5|Briefly described|Table 2|||||||||
24163|Arabulja Volcanics|41310|5|Briefly described|Table 1|||See also p12||||||18-JUL-06
24163|Arabulja Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
24163|Arabulja Volcanics|41524|4|Described|Table 1|||||||||
24163|Arabulja Volcanics|41525|5|Briefly described|Map legend|Early Cambrian||Of the Wauchope Subgroup (Hatches Creek Group). Felsic volcanics.||||||26-OCT-05
24163|Arabulja Volcanics|41970|6|Mentioned|p337|||||||||
24163|Arabulja Volcanics|42643|4|Described|p12, Table 1 p7|||||||||
24163|Arabulja Volcanics|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Felsic lava; minor interbedded welded and friable tuff, ashstone, agglomerate, possible ignimbrite, micaceous arenite.||||||07-NOV-08
24163|Arabulja Volcanics|43802|6|Mentioned|Table 1,p80|||||||||
24163|Arabulja Volcanics|45167|3|Fully described|Table 1|||Of Wauchope Subgroup.||||||18-AUG-08
24163|Arabulja Volcanics|49033|2|Defined|p20|Proterozoic|Proterozoic|||||||
24163|Arabulja Volcanics|50588|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Of the Wauchope Subgroup. Age: 1819 +/- 8Ma (SHRIMP).||||||14-MAR-13
24163|Arabulja Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lower Wauchope Subgroup (Hatches Creek Group). Felsic lava, minor tuff and ashstone.  In the Tennant Creek region.||||||07-NOV-08
24163|Arabulja Volcanics|64722|5|Briefly described|p10|Orosirian|Orosirian|Tennant Region, North Australian Craton.|1814 +/-  4 Ma.|Of Hatches Creek Group.||||11-APR-12
24163|Arabulja Volcanics|64730|5|Briefly described|p142, Fig.11|Paleoproterozoic|Paleoproterozoic|Age is of crystallisation.|1814 +/- 3 Ma (Claoue-Long et al 2005).|Of [Wauchope Subgroup] Hatches Creek Group.||||02-MAY-12
24163|Arabulja Volcanics|64735|4|Described|p205 Fig 1, p206 Fig 2, p209, p215,|Orosirian|Orosirian|Is at an equivalent stratigraphic level to the upper part of the Yeeradgi Sandstone; age from SHRIMP RG 207Pb/206Pb on zircons from a partly welded dacitic ignimbrite (this publication).|1814+/-3 Ma crystallisation age.|Of Hatches Creek Group, Wauchope Subgroup.||Underlies Coulters Sandstone, Kudinga Basalt.|Subaerial felsic volcanics.|20-APR-12
24163|Arabulja Volcanics|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup. Localised distribution in vicinity of Murray Downs Dome.||Wauchope Subgroup.||||05-JAN-17
24163|Arabulja Volcanics|65338|5|Briefly described|p20.|Orosirian|Orosirian|Laterally equivalent to Newlands and Strzeleckie Volcanics.|1814 +/- 3 Ma (Claoue-Long et al. 2008b).|Unit in Wauchope Subgroup.||||
24163|Arabulja Volcanics|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup, Hatches Creek Group.||Overlies Yeeradgi Sandstone. Is overlain by Coulters Sandstone.|Felsic lava, generally porphyritic.|19-OCT-11
24163|Arabulja Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Shown as disconformably overlain by Coulters Sandstone. Underlian by and part lateral equivalent to Yeeradgi Sandstone.|Felsic lava; minor tuff and ashstone.|08-DEC-14
24163|Arabulja Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area. Extrusion age.|1811 +/- 5 Ma.|Hatches Creek Group.|||Felsic.|
24163|Arabulja Volcanics|67352|4|Described|p9, p41, p44 fig 48|Orosirian|Orosirian|500 m thick. Recessive.||Wauchope Subgroup||Conformably overlies and interfingers with Yeeradgi Sandstone. Is overlain unconformably by Coulters Sandstone.|Felsic lava: sparse alkali feldspar phenocrysts.|
24163|Arabulja Volcanics|68518|4|Described|p7 Tb.1, p12|Proterozoic|Proterozoic|Thickness: 0-500 m.||Wauchope Subgroup||Conformable on Yeeradgi Sandstone; overlain conformably and possibly disconformably by Coulters Sandstone and unconformably by Cambrian strata.|Variably recessive felsic lava (at least 2 separate flows); minor interlayered tuff, ashstone and possible ignimbrite. Individual lavas unusually extensive (over 20km) relative to thicknesses (max less than 300m) and presumably much less viscous.|30-MAY-16
24163|Arabulja Volcanics|68697|5|Briefly described|vi, p24, p46|Orosirian|Orosirian|Lowest volcanic unit of the Hatches Creek Group, apart from some minor interbedded felsic volcanics in the Yeeradgi Sandstone. This age is identical with that determined in this study for a sample of Treasure Volcanics, 2500m more or less directly stratigraphically above.|1814 +/- 3 Ma (Claoue-Long et al., 2008).|Hatches Creek Group.||Overlies Unimbra Sandstone. Partly overlies, and is partly a lateral equivalent of, Yeeradgi Sandstone.||
24163|Arabulja Volcanics|69424|5|Briefly described|p9:5, 27|Paleoproterozoic|Paleoproterozoic|Volcanic rocks are part of the Treasure Suite.|1814 +/- 3 Ma.|Hatches Creek Group.||||12-JUL-16
24163|Arabulja Volcanics|69425|4|Described|p10:3, 10-12, 15-18, 20, 22|Statherian|Statherian|Part of the Treasure Suite. 0 - 500m thick. Mainly comprises two intervals of ridge-forming lava, each consisting of several flows, separated by a recessive valley of probable ignimbrite. Eruption is attributed to volcanic centre(s) in the Murray Downs Dome. Lateral equivalent of Yeeradgi Sandstone. A previous age was 1819 +/- 8 Ma (OZCHRON database).|1814 +/- 3 Ma (Claoue-Long et al., 2005, 2008).|Wauchope Subgroup, lower.||Conformably overlies (and probably interfingers with) Yeeradgi Sandstone. Is overlain conformably (locally unconformably) by Coulters Sandstone. Correlated with Manga Mauda Member (in part).|Red-brown, small feldspar-porphyritic, felsic lava; minor tuff, ashstone; ignimbrite probably represented in recessive interval in middle of unit.|12-JUL-16
24163|Arabulja Volcanics|69431|6|Mentioned|p16:5|||Davenport Province.||Wauchope Subgroup.||||12-JUL-16
24163|Arabulja Volcanics|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1814+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic volcanic rocks.|
83365|Aralka Formation, Lower|73086|4|Described|p160|||[See Aralka Formation definition card, App 2 and ASUD]. [Also written as lower Aralka Formation on p160 in reference to Lower Aralka Formation]. Different type section to the Upper Aralka Formation. Undivided Aralka Formation siltstones referred to [in the body of the article] as lower, middle or upper Aralka Formation according to position relative to formal members; however, the definition card describes a Lower Aralka Formation and Upper Aralka Formation [not commonly referred to in the body of the article]. Transitional contact with the overlying Ringwood Member. [Appears to have more consistent usage and definition than Upper Aralka Formation].||Aralka Formation|||Laminated, thinly-bedded fine-grained calcareous green siltstone interbedded with fine-grained sandstone.|
83366|Aralka Formation, Upper|73086|5|Briefly described|p160|||[See Aralka Formation definition card, App 2 and ASUD]. [Also written as upper Aralka Formation on p160 in reference to Upper Aralka Formation]. Different type section to the Lower Aralka Formation. Undivided Aralka Formation siltstones referred to [in the body of the article] as lower, middle and upper Aralka Formation according to position relative to formal members; however, the definition card describes a Lower Aralka Formation and Upper Aralka Formation [not commonly referred to in the body of the text]. Overlain by Limbla Member[?]. [Upper Aralka Formation described in the definition card does not appear to be equivalent to the upper Aralka Formation informally discussed in the body of the article; may be equivalent to the middle].||Aralka Formation|||Reddish-brown and green siltstone and thickly-bedded to massive sandstone.|
74209|Arco Formation|61542|4|Described|p277 Fig. 2, p288|Namurian|Namurian|Offshore equiv.of onshore Point Spring Sst. Variously overlies Sunbird and Tanmurra Fms.+ Kingfisher Shale.  Geol.P:onshore Bonapart Basin/Petrel-Sub-basin.Interbedded  pyritic siltstone fine- to coarse-gr.sandstones; occasional fossils.||||||07-FEB-11
74209|Arco Formation|67354|6|Mentioned|p73. |||||Offshore unit in Wadeye Sub-Group.||||
74209|Arco Formation|69452|3|Fully described|p36:9, 15, 17|||Gorter et al. (2005). Subsurface. Petrel Sub-basin, Bonaparte Basin. The type section is in the offshore drillhole Sandbar-1, where it is 105m thick (see Lithology). Shallow marine deposits. Up to 650m thick. Offshore and onshore.||Wadeye Group.||Unconformably overlies Sunbird or Tanmurra Formations. Lateral equivalent of Point Spring Sandstone (WA). Is overlain unconformably by Aquitaine Formation.|Lower 62m-thick interval of interbedded siltstone and fine- to very coarse-grained sandstone; up to 5% recrystallised limestone grains, occcasional fossils and common calcite cement; below fine- to coarse- and rarely very coarse-grained sandstone.|12-JUL-16
74209|Arco Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Wadeye Group.||Overlies Sunbird Formation (Weaber Group). Is overlain by Aquitaine Formation.||
74209|Arco Formation|69673|5|Briefly described|p172|Pennsylvanian|Serpukhovian|Age derived from fossils.||Wadeye Group|||Interbedded siltstone/shale and sandstone.|
74209|Arco Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p3|Bashkirian|Bashkirian|See also Regional geology: Fig.8, p11. Hydrocarbon reservoir.||Wadeye Group.||Is overlain by Aquitaine Formation.||12-JUL-16
74209|Arco Formation|73117|6|Mentioned|p15|Serpukhovian|Serpukhovian|Bonaparte Basin, southern. Palynozonation: S. ybertii.||Wadeye Group||Overlain by Aquitaine Formation. Equivalent to Point spring Sandstone.||
26353|Arltunga beds|39583|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26353|Arltunga beds|39931|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
26353|Arltunga beds|43565|5|Briefly described|Table 1,p425|||Superseded the informal  "Arltunga Member" .||||||18-JUL-06
26353|Arltunga beds|43748|5|Briefly described|p10, Tb 1|||Calcarenitic limestone. Probably equivalent to Waite Formation. Separate unit to 'Arltunga Member'||||||19-DEC-11
26353|Arltunga beds|46730|5|Briefly described|p7|Cenozoic|Cenozoic|Geological Province: Amadeus Basin.||||||19-NOV-08
26353|Arltunga beds|60547|5|Briefly described|Map Legend|Tertiary|Tertiary|Kaolinitic quartzose sandstone, siltstone and mudstone; mottled and kaolinised in part.||||||03-JUN-05
26353|Arltunga beds|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Age: 20.5-11.5Ma. Thickness: 30m. Geological Province: East Amadeus Basin.||||||
26353|Arltunga beds|64068|6|Mentioned|p79|||Of Amadeus Basin. Correlated with Poodyea Formation, Austral Downs Limestone, Brunette Limestone, Waite Formation.||||||
26353|Arltunga beds|69458|5|Briefly described|p42:8|||Paddys Basin.|||||Arenaceous limestone, silicified limestone and pebbly sandstone.|12-JUL-16
26353|Arltunga beds|72516|6|Mentioned|p98|Neogene|Neogene|Amadeus Basin. Interpreted to be an age equivalent of the Waite Formation.||||||09-JUN-21
30271|Arnold Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
30271|Arnold Sandstone|23404|5|Briefly described|p645|||Of Roper Group.||||||
30271|Arnold Sandstone|23937|4|Described|p38, p23 Tb. 2|Calymmian|Calymmian|Of the Collara Subgroup (Roper Group).  Unconformably overlain by Jalboi Formation; disconformably overlies Crawford Formation.  Max. thickness: 123m. Geological Province: McArthur Basin.||||||20-OCT-04
30271|Arnold Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: white, coarse-grained, medium-bedded, lenticular thin quartz granule beds, planar and trough cross-beds, current ripples, pseudo-karstically weathered. Geol. Prov: McArthur Basin.||||||13-OCT-05
30271|Arnold Sandstone|24050|3|Fully described|p47, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Formerly Arnold Sandstone Member (Abner Sandstone).  Medium- to coarse-grained quartz sandstone; strongly cross-bedded.  Overlies the Crawford Formation; underlies the Jalboi Formation unconformably.  Thickness: 0-?20m.||||||18-JUL-06
30271|Arnold Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
30271|Arnold Sandstone|24303|5|Briefly described|p61 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Correlates with the lower part of the Powell Formation. See also p24 Tb.4||||||
30271|Arnold Sandstone|44112|6|Mentioned|Fig11p30|||||||||
30271|Arnold Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Quartz sandstone, grey, medium-grained, medium bedded; minor thin bedded siltstone, mudstone and fine sandstone. Does not outcrop in the Roper River mapsheet area.||||||22-FEB-05
30271|Arnold Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Quartz sandstone: grey, medium grained, medium bedded, trough cross stratified, ripple marks; minor thin bedded siltstone, mudstone and fine grained sandstone.||||||
30271|Arnold Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: white, coarse-grained, medium-bedded, lenticular thin quartz granule beds, planar and trough cross-beds, current rippl es, pseudo-karstically weathered. Geol. Prov: McArthur Basin.||||||
30271|Arnold Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
30271|Arnold Sandstone|69430|4|Described|p15:3, 27, 29-30|Calymmian|Calymmian|Abbott et al. (2001). Previously the Arnold Sandstone Member (of Abner Sandstone in the Roper River region) of Dunn (1963). McArthur Basin. 0-123m thick. Coastal tidal platform sediments.||Collara Subgroup.||Disconformably overlies Crawford Formation. Is overlain unconformably by Jalboi Formation.|A thin unit of white, thickly bedded, mainly medium-grained quartz sandstone which is strongly planar cross-bedded.|12-JUL-16
30271|Arnold Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern and Southern McArthur Basin.||Collara Subgroup||Overlain by Jalboi Formation, Overlies Crawford Formation||
30271|Arnold Sandstone|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Tidal platform sandstone.||Of Collara Subgroup.||Overlies Crawford Formation. Overlain by Jalboi Formation||
30271|Arnold Sandstone|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group||Overlies Crawford Formation; overlain by Jalboi Formation.|Sandstone.|
30271|Arnold Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Arnold. McArthur Basin.||||||
30271|Arnold Sandstone|70968|3|Fully described|p6, p35, p39-40, p42, p44, p46-47, p55 |Calymmian|Calymmian|See also p124, p126-128, p131, p140, p143. Dunn (1963). Named after Arnold River. Originally defined as Arnold Sandstone Member (of Abner Sandstone). Raised to Formation rank by Abbott et al. (2001). No type section; these authors propose a reference area S of Hell's Gate area at 440100mE 8375600mN. Abbott et al. (2001) reported a measured section, considered representative, at UP/13 442600mE 8362100mN. Resistant, scarp-forming unit: forms spectacular parakarstic landforms. Widespread throughout McArthur Basin. Lithology described and illustrated in some detail. Thickness 20-290m. Tide-dominated shoreline to shallow-marine deposits. Detrital zircon diagram.||Collara Subgroup.||Overlies Crawford Formation conformably, locally disconformably. Is overlain by Jalboi Formation conformably or disconformably.|Predominantly medium-grained quartz sandstone, typically white-weathering, and massive or well-bedded. Minor thin beds or partings of micaceous siltstone and/or mudstone.|
30271|Arnold Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 20-292+ m thick. Coastal tidal platform deposits.||Collara Subgroup.||Conformably and/or disconformably overlies Crawford Formation. Is overlain unconformably to disconformably by Jalboi Formation.|White-weathering, cross-bedded, fine to coarse quartz sandstone.|
30271|Arnold Sandstone|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Crawford Formation. Overlain by the Jalboi Formation.||
30271|Arnold Sandstone|71779|5|Briefly described|p2 Fig.1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
30271|Arnold Sandstone|71893|4|Described|iii, p2-p5, p8, p17, p20-p24|Ectasian|Calymmian|McArthur Basin. A maximum depositional age of 1681 +/- 34 Ma and a youngest individual age of 1589 +/- 40 Ma are provided. This unit was originally named in Dunn, 1963a and is a resistant scarp-forming unit. Deposited in a tide-dominated shoreline to shallow marine setting. A maximum age is derived from the underlying Showell Member dated at 1493 +/- 4 Ma and a minimum age of 1361 +/- 21 Ma is derived from Re-Os of the Wyworrie Member of the overlying Velkerri Formation.  Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Collara Subgroup||Disconformably or conformably overlies the Crawford Formation. Disconformably or conformably overlain by the Jalboi Formation. Equivalent in part to the Abner Sandstone.|White-weathering, cross-bedded quartz sandstone and white, light brown-weathering, medium-grained quartz sandstone.|
30271|Arnold Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Collara Subgroup||Overlies Crawford Formation and underlies Jalboi Formation.||
30271|Arnold Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Collara Subgroup, Roper Group||Underlain by Crawford Formation. Overlain by Jalboi Formation. Equivalent to Abner Sandstone.||
30271|Arnold Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Collara Subgroup||Overlies Crawford Formation and underlies Jalboi Formation and is equivalent to Abner Sandstone, in part.||
30271|Arnold Sandstone|72919|6|Mentioned|p1, p95|||||Roper Group||||
30271|Arnold Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Crawford Formation. Overlain by Jalboi Formation.||
30271|Arnold Sandstone|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Crawford Formation. Overlain by Jalboi Formation.|Includes tidal Sandstone.|
37960|Aroota Group|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes Mount Cornish Formation and Yardida Tillite.  Geological Province: southern Georgina Basin.||||||
37960|Aroota Group|64068|3|Fully described|p223 App 1, p45, p7, p35, p viii,|Cryogenian||New name.|||Includes Yardida Tillite and Mount Cornish Formation.|Nonconformably overlies Jinka Granite. Overlies Yackah beds of Plenty Group with inferred disconformity. Is disconformably overlain by Keepera Group.||05-APR-12
37960|Aroota Group|65338|6|Mentioned|p63.|||Southeastern Georgina Basin.|||Includes Yardida Tillite.|||
37960|Aroota Group|66767|5|Briefly described|p58|Cryogenian|Cryogenian|Georgina Basin. Glacigene units are probably correlates of Sturtian glacial deposits in SA.||||Overlies Plenty Group.|Glacigene units.|
37960|Aroota Group|69437|5|Briefly described|p22:7|||Southern Georgina Basin. Supersequence 2. |||Yardida Tillite, Mount Cornish Formation.||Glacial sedimentary rocks.|12-JUL-16
37960|Aroota Group|69443|5|Briefly described|p28:2-3, 7-8, 31|Cryogenian|Cryogenian|Kruse in Dunster et al. (2007). Southern Georgina Basin.|||Yardida Tillite, Mount Cornish Formation.|Disconformably overlies Plenty Group. Is equivalent to Areyonga and Naburula Formations, and lower Inindia beds. Is overlain disconformably by Keepera Group.|A glacigene succession.|12-JUL-16
37960|Aroota Group|69673|6|Mentioned|p111, p114 fig 92, p115|Neoproterozoic|Neoproterozoic||||Includes Yardida Tillite, Mount Cornish Formation|||
37960|Aroota Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Mount Cornish Formation.|Disconformably overlain by the Keepera Group. Disconformably overlies the Plenty Group.||
37960|Aroota Group|72516|6|Mentioned|p13, p21, p85-86, p135, p171, p176|Cryogenian|Cryogenian|Georgina Basin.|||Includes the Mount Cornish Formation.|||
37960|Aroota 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.||||||
75503|Arrarra Gneiss|66683|5|Briefly described|p368 Fig.3, p372 Table 3, p378.|||Hollis et al.(2009a) propose this name for quartzofeldspathic gneisses in Arnhem Land, structurally underlying the Kakadu Group, with crystallisation ages between or close to c.2670-2640 Ma.The contact relationships between the Kukalak and Arrarra Gneiss are not clear, due to poor exposure. A plausible relationship is that the Kukalak Gneiss protolith intruded the Arrarra Gneiss at 2530-2510Ma and the composite granitic package was transposed and interleaved by subsequent tectonism, probably during ca. 1865Ma tectonometamorphism.|Two magmatic episodes: 2671+/-3Ma and 2640+/-5Ma|||May be intruded by Kukalak Gneiss and Nanambu Complex.||10-DEC-12
75503|Arrarra Gneiss|67232|5|Briefly described|p2. |Neoarchean|Neoarchean|Nimbuwah Domain basement, Pine Creek Orogen.|2640 Ma.|||||
75503|Arrarra Gneiss|67479|5|Briefly described|p2 Tb.1, p6 Fig.2, pp35-37, p55, p74|Siderian|Neoarchean|Metamorphic age: c. 2498 +/- 14 Ma (determined from five rims).|2640 +/- 5 Ma (crystallisation age).||||Layered leucocratic gneiss.|24-JAN-17
75503|Arrarra Gneiss|67779|2|Defined|p6 Fig.5, p10 Table 1, p104, p116-117.|Neoarchean|Neoarchean|New name, after the Arrarra U-Au prospect in the Alligator River Uranium Field. Previously mapped (Dunn, 1962) as part of Myra Falls Metamorphics, a name now obsolete (Hollis et al. 2009b). Nimbuwah Domain, Pine Creek Orogen. Reference area c.14 km NE of Oenpelli township. Mapped areas have only a weak gravity low. SHRIMP zircon Pb/Pb age of magmatic crystallisation. Geochemistry and geochronology are detailed.|2640 +/- 3 Ma (Hollis et al. 2009c).|||Is intruded by Kukalak Gneiss.|Biotite granodioritic gneiss with well-developed S2 gneissosity; minor amphibolite.|14-MAY-18
75503|Arrarra Gneiss|68998|5|Briefly described|p34|||Pine Creek Orogen. Age of zircon rims interpreted as metamorphism/recrystallisation.|2498 +/- 14 Ma (Carson et al., 2010).|||||
75503|Arrarra Gneiss|69419|5|Briefly described|p4:1-2, 6-8|Archean|Archean|Hollis et al. (2009). Nimbuwah Domain, Pine Creek Orogen. c.14km N of Oenpelli township. SHRIMP U-Pb zircon magmatic crystallisation age, with metamorphic zircon rim overgrowth/recrystallisation at 2498 +/- 14 Ma. These ages are consistent with previous determinations (Worden et al., 2006). Geochemistry briefly described.|2640 +/- 4 Ma (Hollis et al., 2009).||||Felsic gneiss.|12-JUL-16
75503|Arrarra Gneiss|69420|5|Briefly described|p5:4,6,8,23,38, 66-67, 85, 100, 111, 115|Archean|Archean|Part of the basement to the Nimbuwah Domain of the Pine Creek Orogen; western Arnhem Land.|2640 Ma.|||||12-JUL-16
75503|Arrarra Gneiss|69537|6|Mentioned|p5|Archean|Archean|Pine Creek Orogen. Rocks experienced recrystallisation / metamorphism with zircon rims aged 2498 +/- 14 Ma (Carson et al., 2010) and 2473 +/- 12 Ma (Worden et al., 2006).||||||
75503|Arrarra Gneiss|69917|5|Briefly described|p18-21, 45, 1|Neoarchean|Neoarchean|Pine Creek Orogen, Nimbuwah Domain. U/Pb SHRIMP zircon dating and  U/Pb LA-ICPMS zircon dating attempted on another sample, Hf, O analytical data. Sampled in type area. This unit supersedes in part the old Myra Falls Metamorphics.|2640+/-5 Ma mag. cryst.||||Leucocratic quartzo-feldspathic gneiss.|
75503|Arrarra Gneiss|70853|5|Briefly described|Map legend.|Neoarchean|Neoarchean||2640 Ma.||||Biotite granodioritic gneiss; minor amphibolite.|
75503|Arrarra Gneiss|71256|6|Mentioned|p18|Neoarchean|Neoarchean||~2640 Ma|||||
75503|Arrarra Gneiss|71341|6|Mentioned|p198|||Pine Creek Orogen. ||||||
75503|Arrarra Gneiss|72368|5|Briefly described|iii,p4|Neoarchean|Neoarchean|Geological province: Nimbuwah Domain, Pine Creek Orogen. Indistinguishable from Kukalak Gneiss in whole-rock geochemistry, but has distinct more juvenile Nd-isotopic composition. Preserves evidence of metamorphic zircon growth at c. 2490 Ma in the form of rare zircon rim growth (Hollis et al 2009; Carson et al 2010; Hollis and Glass 2012).||||Intruded by Kukalak Gneiss.||
75503|Arrarra Gneiss|72527|6|Mentioned|p192.|Archean|Archean||c. 2640 Ma|Nanambu Complex||||
75075|Ascalon Formation|67370|2|Defined|pp313-318, pp324-325. |Middle Scythian|Early Scythian|New name. Southern Bonaparte Basin. A prominent, widespread unit. Type section is in Ascalon 1A between 4,072.5 - 4,105 m. Synonymous with the Intra-Mount Goodwin Sub-group sandstone of Gorter et al. (1998). There was a widespread regressive event at the base of this unit, equated with the Induan 1 and 2 sea level events; deposition was delta plain transitional paralic to shallow marine, and forms the lowstand deposits of the upper Mount Goodwin Subgroup succession.  Comprises the A1 gas reservoir at Blacktip gas field. Lies within the Kraeuselisporites saeptatus Oppel Zone of Dolby and Balme (1976), which occurs in the Kockatea Shale in the Perth Basin. Apparently correlated with Indoon Member.||Unit in Mount Goodwin Subgroup.||Unconformably overlies Mairmull Formation. Is overlain conformably by Fishburn Formation.|Thin reservoir-quality and gas-bearing sandstones, very fine- to fine-grained, well-sorted; siltstones; shales-out to the northwest.|
75075|Ascalon Formation|69452|3|Fully described|p36:8, 15, 20-21|Olenekian|Olenekian|Gorter et al. (2009). Equivalent to the "Intra Mount Goodwin Formation sandstone" of Gorter et al. (1998). Petrel Sub-basin, Bonaparte Basin. Up to 50m thick; 32.5m thick in the type section in offshore drillhole Ascalon-1A. Undifferentiated Ascalon Fm/Mairmull Fm forms 20m of shale and siltstone onshore, near Mount Goodwin.||Mount Goodwin Subgroup.||Unconformably overlies Mairmull Formation. Is overlain conformably and transitionally by the Fishburn Formation.|A prominent sandstone and siltstone unit, becoming increasingly shaly to the NW.|12-JUL-16
75075|Ascalon Formation|69454|5|Briefly described|p38:4|Olenekian|Olenekian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
75075|Ascalon Formation|69653|6|Mentioned|p10|Early Triassic|Early Triassic|Petrel Sub-basin.||Mount Goodwin Sub-group.||Overlies Mairmull Formation. Is overlain by Fishburn Formation.||
75075|Ascalon Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Fishburn Formation, overlies Mairmull Formation||
75075|Ascalon Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p2|Olenekian|Olenekian|See also Regional geology: Figs.6-7, p11. Sahul: p2. Vulcan: Fig.2, p2. Hydrocarbon reservoir (gas at Blacktip 1). Source rock in Sahul Syncline and Vulcan Sub-basin.||Mount Goodwin Subgroup.||Overlies Mairmull Formation. Is overlain by Fishburn Formation.||12-JUL-16
24166|Atnarpa Igneous Complex|1490|6|Mentioned|p5|||Arunta Inlier. Affected by the 1670 Ma Aileron Event.|1651 +/- 47 Ma.||||Includes granites.|
24166|Atnarpa Igneous Complex|9199|5|Briefly described|Map legend|||Diorite, tonalite, granite, aplogranite, intermediate to acid hypabyssal rocks.  Geological Province: Arunta Block.||||||04-NOV-04
24166|Atnarpa Igneous Complex|22524|6|Mentioned|p37,p43||Statherian|Dated at 1651 Ma and 1880Ma?||||||18-JUL-06
24166|Atnarpa Igneous Complex|23733|5|Briefly described|p31|Paleoproterozoic|Paleoproterozoic|Age: 1879Ma. See also p34 Fig.20.||||||07-NOV-08
24166|Atnarpa Igneous Complex|24197|6|Mentioned|p14 Fig. 1.3.2a|Proterozoic|Proterozoic|Of the Atnarpa Suite. Geological province: Arunta Block.||||||07-FEB-11
24166|Atnarpa Igneous Complex|24567|6|Mentioned|p162|||Felsic rocks.||||||
24166|Atnarpa Igneous Complex|38829|5|Briefly described|p132|||||||||
24166|Atnarpa Igneous Complex|38885|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24166|Atnarpa Igneous Complex|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24166|Atnarpa Igneous Complex|39887|6|Mentioned|Fig.3|||||||||
24166|Atnarpa Igneous Complex|39888|6|Mentioned|Fig.8|||||||||
24166|Atnarpa Igneous Complex|39931|6|Mentioned|Map legend|Paleozoic|Proterozoic|Proterozoic to Palaeozoic||||||07-NOV-08
24166|Atnarpa Igneous Complex|41509|3|Fully described|p7|||||||||
24166|Atnarpa Igneous Complex|42307|4|Described|p251|||||||||
24166|Atnarpa Igneous Complex|42326|5|Briefly described|Table 2 P11|||||||||
24166|Atnarpa Igneous Complex|42770|5|Briefly described|p13, Fig.14|||Age: 1880 Ma.||||||18-JUL-06
24166|Atnarpa Igneous Complex|42830|5|Briefly described|p169|||||||||
24166|Atnarpa Igneous Complex|43568|6|Mentioned|p507|||Emplaced at 1880 Ma||||||
24166|Atnarpa Igneous Complex|46730|4|Described|p6|Paleoproterozoic|Paleoproterozoic|Intrudes Tommys Gap metamorphics.  Age: 1651+/-47Ma (Rb-Sr). Geological Province: Arunta Block.||||||07-NOV-08
24166|Atnarpa Igneous Complex|48992|2|Defined|p7|Mesoproterozoic|Mesoproterozoic|||||||
24166|Atnarpa Igneous Complex|50246|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Age: ~1770Ma. Retrogressed tonalitic gneiss.||||||07-FEB-11
24166|Atnarpa Igneous Complex|50369|5|Briefly described|p1.3, 2.1, 13.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Atnarpa Suite.  Geological Province: Arunta Inlier. I-type granite.||||||07-NOV-08
24166|Atnarpa Igneous Complex|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Diorite, tonalite, granite, aplogranite, intermediate to acid hypabyssal rocks.||||||
24166|Atnarpa Igneous Complex|61208|6|Mentioned|p213|Paleoproterozoic|Paleoproterozoic|Age: 1879+/-11Ma and 1873+/-11Ma (Zhao and Cooper 1992).||||||07-NOV-08
24166|Atnarpa Igneous Complex|62595|5|Briefly described|pp9-10, p31 Fig.9.|Statherian|Statherian|Part of the Alice Springs Arltungs Nappe Complex, a south-directed thrusting event c.430-300 Ma. With Heavitree Quartzite, hosts the Arltunga goldfield deposit.|c.1770 Ma (Zhao and Bennett 1995).||||Retrogressed tonalitic gneiss.|
24166|Atnarpa Igneous Complex|64736|6|Mentioned|p222|||TIMS age of 1897 +11/-10 Ma and 1873 +11/-10 Ma from Zhao and Cooper (1992) refuted in this paper.||||||30-APR-12
24166|Atnarpa Igneous Complex|65681|6|Mentioned|p744.|||Arunta Block. Has multielement plots identical with that of Broken Hill felsic gneisses, implying an igneous origin for the latter.||||||
24166|Atnarpa Igneous Complex|67181|5|Briefly described|p631, p632|Statherian|Statherian|Zhao and Cooper (1992) suggest the complex formed by melting of subducted oceanic crust. Of the Calcalkaline-trondhjemitic Group (geochemical grouping) Arunta Region, North Australian Craton.|1751 +/- 12 Ma (Zhao and Cooper 1992)|||||
24166|Atnarpa Igneous Complex|67323|5|Briefly described|p30|||Arunta Inlier. Emplacement age.|~1880 Ma.||||I-type diorite, tonalite, granodiorite and granite.|
24166|Atnarpa Igneous Complex|68998|6|Mentioned|p6|||Apparently geochemically similar to an un-named granodiorite gneiss dated at 1757 +/- 4 Ma.||||||
24166|Atnarpa Igneous Complex|69427|5|Briefly described|p12:9, 30, 36, 57-58|Paleoproterozoic|Paleoproterozoic|Shaw et al. (1979). Crops out through Giles Creek Synform, White Range and Ruby Gap Nappes (Strangways Range region), Aileron Province. Subduction-related magmatism. Grouped into 3 suites by Zhao and Cooper (1992); their conventional TIMS U-Pb zircon ages are (1) 1879 +11/-10 Ma, (2) 1873 +11/-10 Ma and (3) 1751 +/- 12 Ma. There is a suggestion of inheritance in the 1880-1870 Ma ages. Hosts gold deposits in the Arltunga goldfield.|1751 Ma?||||Tonalite, diorite, trondhjemite, granodiorite, granite and aplite. Grouped into 3 suites: (1) gabbro-diorite-tonalite-trondhjemite suite; (2) a low-Al tonalite-trondhjemite-granodiorite suite; (3) a younger tonalite suite.|12-JUL-16
24166|Atnarpa Igneous Complex|69438|5|Briefly described|p23:49|||Aileron Province.|||||Retrograded tonalite: well-foliated, lineated micaceous schist.|12-JUL-16
24166|Atnarpa Igneous Complex|69917|6|Mentioned|p139-140|||Includes magmatic rocks ca. 1.88 Ga. Probably not source for Entia Metamophics.||||||
24166|Atnarpa Igneous Complex|69925|6|Mentioned|p17-18, 20, 27, 36, 38-40|||Zhao and Cooper (1992). Comprises two suites dated at 1880-1860 Ma and a 1750 Ma younger suite.|1880-1860 Ma (Zhao and Cooper, 1992).||||Contains high-Na calcalkaline suites typical of modern active continental margins.|
24166|Atnarpa Igneous Complex|69929|6|Mentioned|p233, 237|||Part of Arltunga Nappe Complex.|||||Includes deformed granitic rocks.|
24166|Atnarpa Igneous Complex|69931|5|Briefly described|p269, 293, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|1880-1870 Ma.||Atnarpa Suite.||Quartz diorite, trondhjemite, tonalite.|
24166|Atnarpa Igneous Complex|69932|6|Mentioned|p303, 306-307, 309|||Central Province, Arunta Inlier. Sm-Nd data tabulated. Presented as Atnarpa Meta-igneous Complex on p303. See also references to Atnarpa Complex (p309-310).|2122 Ma and 2111 Ma.||Ruby Gap Tonalite.||Diorite.|
24166|Atnarpa Igneous Complex|72516|5|Briefly described|p121|||Part of the calc-alkaline-trondhjemitic group of Zhao and McCulloch (1995). Outcrops below the informal CAT-line in the eastern Aileron Province.|ca. 1770-1750 Ma|||||09-JUN-21
24166|Atnarpa Igneous Complex|72718|6|Mentioned|p2|Orosirian|Orosirian|Arc magmatism.|1880-1860 Ma|||||
24166|Atnarpa Igneous Complex|73088|6|Mentioned|p2, p4|Palaeoproterozoic|Palaeoproterozoic|Aileron Province||||||
79164|Atneequa Granite|68150|5|Briefly described|p.vi Tb.i, p52-55|||On 100K mapsheet: ILLOGWA 6050. Atneequa Granite locally incorporates rafts of metasedimentary rock (likely part of Albarta Metamorphics), typically foliated calc-silicate, although appears to be relatively undeformed itself. Sample is coarse-grained porphyritic biotite granite collected from Atneequa Granitic Complex. Previously dated  magmatic crystallisation age of 1762  +/-  9 Ma, and a Strangways age of 1715  +/-  19 Ma  interpreted (sample was analysed without CL imaging; Zhao and Bennett, 1995; U-Pb SHRIMP interpreted 207Pb /206Pb). An inherited core of 1931  +/-  6 Ma suggests pre-existing crust present in source region. See also Atneequa Granitic Complex and Atneequa Complex in this paper.|1743 +/- 4 Ma, igneous crystallis'n, SHRIMP Pb/Pb||||K-feldspar megacrystic biotite granodiorite|30-SEP-15
79164|Atneequa Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1743+/-4 Ma (U-Pb zircon SHRIMP)||||Granodiorite.|
41810|Atneequa Suite|50369|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1762Ma.||||||07-NOV-08
41810|Atneequa Suite|69427|5|Briefly described|p12:30 Fig.12.28; 12:37|Statherian|Statherian|Whelan et al. (2011). Formerly the Atneequa Granitic Complex of Zhao and Bennett (1995). Included in a map of 1780-1740 Ma granites in the Aileron Province. SHRIMP U-Pb age.|1743 +/- 4 Ma (Whelan et al., 2011).|||Intrudes Albarta Metamorphics.|A suite of coeval felsic and mafic rocks including porphyritic biotite granite, lesser granodiorite, and more mafic compositions including quartz gabbro and gabbro.|12-JUL-16
41810|Atneequa Suite|69510|5|Briefly described|piii, p5, p8|Paleoproterozoic|Paleoproterozoic||c.1745 Ma.||||Strongly foliated to locally mylonitic.|
41810|Atneequa Suite|69931|6|Mentioned|p269, 273|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Presented as Atneequa granitic complex on p269. REE analyses tabulated.|1762 +/- 9 Ma.||Atneequa Granitic Complex.|||
41810|Atneequa Suite|71858|5|Briefly described|p2|||Aileron Province.||||||
41810|Atneequa Suite|72375|5|Briefly described|p7|Statherian|Statherian|Geological province: Aileron Province. Structurally interleaved and infolded with Heavitree Formation and Bitter Springs Group on the LIMBLA and ILLOGWA Creek mapsheets (Kositcin et al 2011, Whelan et al 2011). Unconformably underlies the unnamed quartzite (sampleno: 2134817).|c. 1745 Ma||||Strongly foliated to mylonitic intrusive rocks.|04-DEC-19
41810|Atneequa Suite|72714|6|Mentioned|p2, p4|||Aileron Province. Granite in APDD002 is interpreted as Atneequa Suite, although not explicitly stated as such in the lithology logs of Lyons (2012). Granite from this drillholr includes a mineralogically and texturally distinct 'upper granite' that has zones of little or no quartz, with significant albite. Regionally, copper-bearing fluorite veins are found on the contact between the Atneequa Suite and overlying Heavitree Formation and Bitter Springs Group.|||||Granite|
25768|Attack Creek Formation|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|1749+/-17Ma||||||
25768|Attack Creek Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup, Churchills Head Group. Undifferentiated, dolostone and limestone, siltstone, quartz arenite, and sublithic arenite.||||||07-NOV-08
25768|Attack Creek Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tomkinson Creek Group.||||||
25768|Attack Creek Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||
25768|Attack Creek Formation|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Dololutite.  Age: <1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
25768|Attack Creek Formation|24172|3|Fully described|p35, p6 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Subgroup. Underlain by Short Range Sandstone. Geological Province: Tennant Creek Inlier. Maximum Thickess: >700m. Mixed siliciclastic and carbonate shallow marine to intertidal succession. See also p65 Tb. 9.||||||01-DEC-15
25768|Attack Creek Formation|24303|3|Fully described|p4 Tb.1|Proterozoic|Proterozoic|Of the Tomkinson Creek Group. Overlain by the Bootu Formation. Overlies the Short Range Sandstone. Part of the Middle Tomkinson Cr. Gp. The former upper section is now part of the overlying Bootu Formation. Age: 1752 +/- 26 Ma (U-Pb).||||||
25768|Attack Creek Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Group.  Limestone, dolomitic; massive and laminated; onkoid, stylolitic and cryptomicrobial boundstone and stromatolitic bioherms; minor siliciclastic mudstone and marly dolostone, fine-gr. sst. and mudst., graded, dessicated, rippled.||||||07-NOV-08
25768|Attack Creek Formation|24442|5|Briefly described|p14|||Of the Tomkinson Creek Group.  Geological Province: Ashburton Province.||||||
25768|Attack Creek Formation|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic or Carpentarian||||||07-NOV-08
25768|Attack Creek Formation|33307|6|Mentioned|Fig.6|||||||||
25768|Attack Creek Formation|35771|2|Defined|p26|early Carpentarian|early Carpentarian|Appendix.||||||
25768|Attack Creek Formation|39213|6|Mentioned|Fig.8|||||||||
25768|Attack Creek Formation|39624|5|Briefly described|Table 2|||||||||
25768|Attack Creek Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Tomkinson Creek Subgroup||||||07-NOV-08
25768|Attack Creek Formation|43224|5|Briefly described|Map legend||Proterozoic|of Tomkinson Creek Subgroup||||||
25768|Attack Creek Formation|50353|5|Briefly described|Map Legend|||Of Tomkinson Creek Group||||||
25768|Attack Creek Formation|60684|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup (Churchills Head Group). Dolostone, siltstone, cherty siltstone, quartz arenite.  Conformably overlies Short Range Sandstone; transitional with Bootu Formation above.||||||07-NOV-08
25768|Attack Creek Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Dolostone, limestone, siltstone, sublithic and quartz arenite.  Underlies the Bootu Formation.  In the Tennant Creek region.||||||07-NOV-08
25768|Attack Creek Formation|64780|4|Described|p60,p61,p63 Fig.4,p65,p70 |Palaeoproterozoic|Palaeoproterozoic|~330m thick. Poorly defined SHRIMP U-Pb maximum depositional age.|1752 +/-26 Ma (Armstrong 1998).|Of the Tomkinson Creek Group.||Underlies the Bootu Formation conformably.|Consists of dolostone, limestone, thinly bedded siltstone and mudstone, chert and some beds of intraformational conglomerate.|
25768|Attack Creek Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
25768|Attack Creek Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.||Overlies Short Range Sandstone. Is overlain by Bootu Formation.|Dolostone, limestone, siltstone, sublithic and quartz arenite.|
25768|Attack Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1752 +/- 26 Ma.|Tomkinson Creek Group.||||
25768|Attack Creek Formation|69425|6|Mentioned|p10:12|||Tomkinson Province.||||Correlated with Vaddingilla Formation.||12-JUL-16
25768|Attack Creek Formation|69431|4|Described|p16:1, 3-6, 11-12, 23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.330-400m thick in the type section in northern TENNANT CREEK map area. Recessive and generally poorly exposed. Lithology described in detail. Shallow-marine and open tidal flats deposits, protected from significant terrigenous input, and with periodic exposure. SHRIMP U-Pb detrital zircon maximum depositional age.|<1752 +/- 26 Ma (Armstrong, 1998).|Tomkinson Creek Group.||Overlies Short Range Sandstone conformably to disconformably. Is overlain by Bootu Formation disconformably to conformably, and by Gleeson Formation unconformably.|Massive to laminated dolostone and limestone(?);  laminated to thinly bedded siltstone and mudstone; chert; thinly bedded quartzose dolostone; microbialite, thin to medium beds of intraformational conglomerate.|12-JUL-16
25768|Attack Creek Formation|69673|6|Mentioned|p58|||||Tomkinson Creek Group||||
25768|Attack Creek Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1749+/-17 Ma (MDA: Pb/Pb zircon).||||Dolostone, siltstone.|
23345|Attutra Metagabbro|23844|3|Fully described|p37|Proterozoic|Proterozoic|Geological Province: Arunta Province. Age: ~2050-545Ma (???). See also Fig.21||||||18-JUL-06
23345|Attutra Metagabbro|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Gabbro; dolerite; rare norite: all altered; magnetite rock. Geological Province: Arunta Block.||||||07-NOV-08
23345|Attutra Metagabbro|40668|5|Briefly described|p273|||||||||
23345|Attutra Metagabbro|40906|4|Described|p14|||||||||
23345|Attutra Metagabbro|41594|5|Briefly described|p74|||||||||
23345|Attutra Metagabbro|49036|2|Defined|p4|Neoproterozoic|Mesoproterozoic|Late or Mid-Proterozoic.||||||
23345|Attutra Metagabbro|50369|6|Mentioned|p9.2|||Intruded by Jervois Granite.||||||18-JUL-06
23345|Attutra Metagabbro|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Altered gabbro, dolerite, rare metanorite, diorite.||||||
23345|Attutra Metagabbro|60668|5|Briefly described|p11, p2 Tb. 1|||Homogeneous, weakly recrystallised mafic sequence of medium- to coarse-grained gabbro, magnetite gabbro, magnetite with lesser leucogabbro, pyroxenite and amphibolite; generally equigranular, massive and unfoliated.||||||
23345|Attutra Metagabbro|64068|5|Briefly described|p33, p46|Statherian|Statherian|East of Jervois. Appears to be a continuation of very extensive mafic rocks under Georgina Basin.|Aged 1786 +/- 4 Ma.|||Intrudes the 1807 Ma Bonya Schist and is intruded by a 1775 Ma tonalite. Overlain by Oorabra Arkose with angular unconformity.||05-APR-12
23345|Attutra Metagabbro|66526|6|Mentioned|p13.|||Aileron Province of the Hart Large Igneous Province. Mafic intrusions contain reported PGE-Au-V mineralisation.||||||
23345|Attutra Metagabbro|67181|5|Briefly described|p631|Statherian|Statherian|Aileron Province, North Australian Craton. 1786 +/- 4 Ma from Claoue-Long and Hoatson (2005) and/or Hoatson et al. (2005)|1786 +/- 4 Ma|||||
23345|Attutra Metagabbro|69418|6|Mentioned|p3:24, 29|||Is listed with the Bonya Schist as hosting the Jervois Fe-Ti vanadiferous magnetite-type deposit (described).||||||12-JUL-16
23345|Attutra Metagabbro|69427|4|Described|p12:3, 20, 24, 64|Statherian|Statherian|Shaw et al. (1984); Hoatson et al. (2005). Aileron Province. A wedge-shaped gabbroic intrusion that crops out 5-10km NW of the Jervois mine. The magnetite layers have anomalous V, Cu, Pt, Pd and Au (described in some detail). Has high potential for PGE mineralisation. Numerous scattered outcrops S of Unca Creek were included in this unit by Freeman (1986); but Hoatson and Stewart (2001) assigned outcrops SW of Unka Bore to Bonya Schist, and smaller outcrops S of Unka Waterhole to an unrelated mafic intrusion. Age from gabbro which is cross-cut by a tonalite dyke dated 1775 +/- 5 Ma (both ages by Claoue-Long and Hoatson, 2005).|1786 +/- 4 Ma (SHRIMP U-Pb zircon).||||Weakly recrystallised uralitised gabbro and magnetite gabbro; lesser leucogabbro, pyroxenite, amphibolites and magnetite. Most are generally equigranular, massive and unfoliated; no obvious cyclicity or compositional layering.|12-JUL-16
23345|Attutra Metagabbro|69925|6|Mentioned|p21|||||||Is possibly intruded by Jervois Granite.||
23345|Attutra Metagabbro|70376|6|Mentioned|p834|Paleoproterozoic|Paleoproterozoic|Eastern Aileron Province. Shows back-arc geochemical characteristics. Also associated with tonalite magmatism at 1775+/-4 Ma.|1786+/-4 Ma|||||
23345|Attutra Metagabbro|70809|5|Briefly described|p8||||1786 +/- 4 Ma (Claoue-Long and Hoatson, 2005)|||Intrudes Bonya Metamorphics|Mafic intrusion.|
23345|Attutra Metagabbro|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1786+/-4 Ma (U-Pb zircon SHRIMP)||||Gabbro chilled margin.|
23345|Attutra Metagabbro|71621|5|Briefly described|p45|||Aileron Province. Outcrops in eastern Jervois Range.| ca 1786 Ma.|||||02-FEB-19
23345|Attutra Metagabbro|71866|5|Briefly described|p1-p2, p14-p15|||Jervois Mineral Field, Aileron Province. Analytical procedure, LAICPMS analyses, results and interpretation discussed in detail.|1786 +/- 4 Ma (Claoue-Long and Hoatson, 2005)|||||
23345|Attutra Metagabbro|72367|5|Briefly described|p5|Statherian|Statherian|Geological province: Aileron Province. Nomenclature after Claoue-Long and Hoatson (2005). Broadly consistent timing with Carmencita Granulite intrusion into sedimentary protoliths of Kanandra Metamorphics and subsequent protolith crystallisation.|c. 1786 Ma (emplacement)|||||
23345|Attutra Metagabbro|72370|5|Briefly described|p15,26|||Geological province: Aileron Province. Age-equivalent to Kings Legend Metadolerite. Intruded by tonalite dykes.|c. 1785 Ma|||||
23345|Attutra Metagabbro|72372|5|Briefly described|p5,23,26|Statherian|Statherian|Geological province: Aileron Province. Intruded into Bonya Metamorphics at c. 1.79-1.77 Ga in the form of stocks, sills and dykes. Has an igneous crystallisation age of 1786+\-4 Ma (U-Pb zircon; Claoue-Long and Hoatson, 2005).|1786+\-4 Ma (U-Pb zircon)|Unit of Baikal Supersuite.||Intrudes Bonya Metamorphics.||
23345|Attutra Metagabbro|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1786 +/- 4 Ma (U-Pb zircon)|Casper Suite|||Metagabbro, metadolerite: fine to coarse grained, aphyric with primary textures locally preserved, rare amygdaloidal textures.|
23345|Attutra Metagabbro|72516|1|Redefined|iii, p8, 13,15-17, p19-22, p188 App 2|Statherian|Statherian|Aileron Province. The type locality occurs west of Jervois Mine in Jervois Range 1:100 map sheet at 635248mE 7496321mN. Outcrops extensively in the Jervois Domain and to a lesser extent in the Bonya Domain. Originally defined by Shaw et al 1985 and named after the Attutra copper deposit. Main outcrop occurs in a wedge shaped area between Jervois Range and the Lucy Creek Shear Zone where it occurs as low rounded hills, sinuous strike ridges and isolated nubbins and tors scattered on plains. Thickness ranges from <1m to 1 km in width. Hosts Iron-titanium-vanadium orthomagmatic deposits. SHRIMP age is interpreted as the age of magmatic crystallisation and is derived from Claoue-Long and Hoatson (2005). Intruded by abundant unnamed granodioritic dykes. Co-magmatic and co-genetic with other constituents of the Casper Suite. Geochemistry, geophysics, metamorphism, economic geology, structure and deformation are discussed. See also  p24-25, p27, p29, p35, p38-42, p48-49, p63, p69, p86, p106-107, p109-111, p123-124, p128, p135-137, p139-140, p142-143, p153, p169-171, p173, p188-189, p192,  p202, p204, p206, p209, p218.|1786 +/- 4.2 Ma (SHRIMP Pb-Pb)|Casper Suite||Unconformably overlain by the Oorabra Arkose and the Elyuah Formation. Intrudes the Bonya Metamorphics. Intruded by the Unca Granite, Jericho Granite and the Tarlton Bore Granite.|Metagabbro, metadolerite: fine to coarse-grained, aphyric with primary igneous textures locally preserved, rare amygdaloidal textures; undeformed to locally foliated.|10-JUN-21
23345|Attutra Metagabbro|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Aileron Province.|||||Includes metagabbro.|
77206|Atula Quartzite|62595|6|Mentioned|p28 Fig.4.|||Relative probability plots of detrital zircon data are shown.||||||
81853|Atula calc-silicate|72516|6|Mentioned|p90|Cambrian|Cambrian|Irindina Province. Age correlative of the Mount Baldwin Formation [hence Cambrian in age].||||||02-JUN-21
39515|Ayers Range Granite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Porphyritic clinopyroxene-hornblende-biotite monzonite and granodiorite.  Geological Province: Musgrave Block.||||||
39515|Ayers Range Granite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Granite monzonite, quartz monzonite. Geological Province: Musgrave Block.||||||
39515|Ayers Range Granite|61154|2|Defined|p43 App., p12-13, p29|Mesoproterozoic|Mesoproterozoic|Formerly Ayers Range adamellite. Of Pitjantjatjara Supersuite. Heterogeous granite, grey to pale grey-green, weakly to strongly porphyritic - detailed lithology in text (p12-13). Intrudes the Alcurra Dolerite.  Age: 1159+/-17Ma (U-Pb: Edgoose et  al 1993)||||||14-JUL-05
39515|Ayers Range Granite|69436|5|Briefly described|p21:9|||Edgoose et al. (2004). Formerly Ayers Range adamellite (Edgoose et al., 1993).|||||Quartz monzonite, heterogeneous, grey and porphyritic, generally with an inequigranular granoblastic texture; porphyritic microgranite; weakly foliated granite, with clinopyroxene rimmed by amphibole a ubiquitous and diagnostic feature.|12-JUL-16
81344|Ayers Rock Arkose|70018|5|Briefly described|p234-235|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 4 in the southern Amadeus Basin.  Equivalent to Mount Currie Conglomerate. Correlable to Arumbera Sandstone in the northern Amadeus Basin.||||Underlain by Winnall Beds in Sthn Amadeus Basin..||08-AUG-19
42062|Babylon Volcaniclastic Sediment|23809|5|Briefly described|p35, p28 Tb. 4|Paleoproterozoic|Paleoproterozoic|Unconformably overlain by the Montejinni Formation.  Age: 1798+/-5Ma.  Geological Province: Wiso Basin.||||||07-NOV-08
81823|Bacardi Granite|73123|4|Described|piii, p1, p5-8, Fig.A1, Tb.A1|Orosirian|Orosirian|Aileron Province. Geochron is an interpreted magmatic crystallisation age. Dated sample: GA sample No = 6619619, NTGS sample ID = HU16EEB1346. Outcrops broadly but sparsely across Dneiper 1:100 000 mapsheet. Magma mingling with the Captain Morgan Metadolerite has been recognised in outcrop indicating the units are cogenetic and coeval. [Article includes outcrop, thin section and zircon descriptions].|1808 +/- 5 Ma SHRIMP U-Pb|Black Label Suite|||Foliated biotite-hornblende granite.|
26360|Badalngarrmirri Formation|22538|6|Mentioned|Fig3 P708|||||||||
26360|Badalngarrmirri Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
26360|Badalngarrmirri Formation|24048|1|Redefined|p98 App. 1|Statherian|Statherian|See also p42.  Proposer: Ian Sweet, after Plumb & Roberts (1992). Of the Parsons Range Group.  Overlain by Marura Siltstone; underlain by Mattamurta Sandstone.  Max. thickness: 2850m.  Geological Province: McArthur Basin.||||||20-JUL-06
26360|Badalngarrmirri Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Includes Fairy Glen Sandstone Member, Gali Member and Mount Fawcett Member. Quartz sandstone laminated with mudstone, siltstone and sandstone; pyritic mudstone and sandstone; dolostone and chert. Geol. Prov: McArthur Basin.||||||11-OCT-05
26360|Badalngarrmirri Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Parsons Range Group. Overlies Mattamurta Sandstone. Overlain by Maruru Siltstone. Geological Province: Northern McArthur Basin.||||||
26360|Badalngarrmirri Formation|32660|5|Briefly described|Table 4|||||||||
26360|Badalngarrmirri Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
26360|Badalngarrmirri Formation|43010|2|Defined|p85||Paleoproterozoic|Of Parsons Range Group. Age:  Statherian.||||||07-NOV-08
26360|Badalngarrmirri Formation|44112|3|Fully described|p49,52|||||||||
26360|Badalngarrmirri Formation|44299|4|Described|p.11||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
26360|Badalngarrmirri Formation|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L.Proterozoic.||||||07-NOV-08
26360|Badalngarrmirri Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Includes Fairy Glen Sandstone Member, Gali Member and Mount Fawcett Member. Quartz sandstone laminated with mudstone, siltston e and sandstone; pyritic mudstone and sandstone; dolostone and chert. Geol. Prov: McArthur Basin.||||||
26360|Badalngarrmirri Formation|64817|6|Mentioned|p353 Fig.4 |||||Unit in Parsons Range Group.||||
26360|Badalngarrmirri Formation|65228|5|Briefly described|p23|||NW McArthur Basin.||Unit in Parsons Range Group.||Overlies Mattamurta Sandstone.||
26360|Badalngarrmirri Formation|69430|4|Described|p15:3, 13-14|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 1900-2800m thick. Storm-dominated shelf deposits, from deep basinal to shoreline. Divided into 13 units of alternating coarse- and fine-grained siliciclastic rocks, three of which are named Members.||Parsons Range Group.|Mount Fawcett, Gali, Fairy Glen Sandstone, Members.|Overlies Mattamurta Sandstone presumably conformably. Is overlain presumably conformably by Marura Siltstone.|Medium to thickly bedded, fine- to coarse-grained quartz sandstone; laminated mudstone, siltstone and fine sandstone; pyritic and ferruginous mudstone and sandstone; minor dolostone and chert.|12-JUL-16
26360|Badalngarrmirri Formation|69673|6|Mentioned|p16 fig 13|||Northern McArthur Basin.||||Overlain by Marura Siltstone, overlies Mattamurta Sandstone.||
79081|Badens Camp quartzite|69383|6|Mentioned|p74|||Arunta Region, Irindina Province (Maidment 2005) PhD.||||||
79081|Badens Camp quartzite|72516|6|Mentioned|p89|Ediacaran|Ediacaran|Irindina Province. Age from correlative unit.||||Correlated with the Grant Bluff Formation.||
26362|Baiguridji Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
26362|Baiguridji Formation|23937|6|Mentioned|p13|||Correlates with parts of the Nagi Formation.  See also p89 Appendix 1.||||||
26362|Baiguridji Formation|24048|3|Fully described|p61|||Of Balma Group.  Overlain by Bath Range Formation; underlain by Yarrawirrie Formation.  Max. thickness: 400m.  Geological Province: McArthur Basin.||||||20-JUL-06
26362|Baiguridji Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Sandstone: commonly dolomitic, fine-grained, thin-bedded, flaggy; mudstone: dolomitic in part; tuffaceous mudstone: thin beds; rock types are interbedded, relative proportions vary across sheet area. Geol. Prov: McArthur Basin.||||||21-OCT-05
26362|Baiguridji Formation|32660|5|Briefly described|Table 4|||||||||
26362|Baiguridji Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
26362|Baiguridji Formation|43010|2|Defined|p120||Paleoproterozoic|Of McArthur Group. Of Statherian age.||||||07-NOV-08
26362|Baiguridji Formation|44112|4|Described|p53-54,56-57|||Full description in Haines et al. (1997).||||||
26362|Baiguridji Formation|44299|4|Described|p.12||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
26362|Baiguridji Formation|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
26362|Baiguridji Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Sandstone: commonly dolomitic, fine-grained, thin-bedded, flaggy; mudstone: dolomitic in part; tuffaceous mudstone: thin beds; rock ty pes are interbedded, relative proportions vary across sheet area. Geol. Prov: McArthur Basin.||||||21-OCT-05
26362|Baiguridji Formation|69430|4|Described|p15:21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. c.400m thick. Subtidal, storm-influenced in part, sediments; shallowing at top. See also misspelt Baiguridgi Fm p15:3.||Balma Group.||Conformably overlies Yarrawirrie Formation. Is overlain conformably by Bath Range Formation. Correlated with Stretton Sandstone.|Fine-grained, flaggy, thinly bedded (more thickly bedded in the W), commonly dolomitic sandstone; grey to black mudstone, dolomitic in part; white, thinly bedded tuffaceous mudstone. Rock types are interbedded.|01-OCT-19
26362|Baiguridji Formation|72373|4|Described|iii,p1,15,17-20,24|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Outcrop restricted to BLUE MUD BAY, relatively minor outcrops along southern edge of ARNHEM BAY-GOVE mapsheets. More recessive unit, forming valleys between more resistant Yarrawirrie and Bath Range formations. Previous age constraints provided by 1621+\-21 Ma and 1599+\-11 Ma tuffaceous rocks in the Yarrawirrie and Bath Range formations respectively (Pietsch et al 1994). Sample 2709633 (BM16TJM020A: Fine-grained quartz sandstone; BLUE MUD BAY) yielded interpreted max depositional age of 1626+\-9 Ma. Similar detrital zircon spectra with Bath Range Formation, suggesting derivation from similar source areas and potentially in part laterally equivalent. Broad age constraints make correaltion with McArthur Group units difficult.|1626+\-9 Ma (max dep age)|Unit of Balma Group.||Overlain by Bath Range Formation. Underlain by Yarrawirrie Formation. Correlated with Stretton Sandstone, Ulunourwi Fm..|Regionally variable succession of mainly fine grained sandstone, mudstone and dolostone.|01-OCT-19
80342|Baikal Supersuite|71621|5|Briefly described|p1, p37-p38|||Aileron Province. Age interpreted as magmatic crystallisation. Petrography and zircon description discussed.|1772 +/- 7 Ma (LA-ICPMS)||||Tourmaline-rich orthogneiss sample dated.|01-FEB-19
80342|Baikal Supersuite|72372|5|Briefly described|p5,22,25,27,34|Statherian|Statherian|Geological province: Aileron Province. Intruded into Bonya Metamorphics at c. 1.79-1.77 Ga. Shallow bimodal magmatism, interpreted to have provided the heat source for long-lived high-thermal gradient metamorphism in Bonya Metamorphics until ca 1.70 Ga (Reno et al 2017, Beyer et al 2018, Weisheit et al in review). Contains tourmaline-altered rock assemblages in localise areas around Bonya Hills.|c. 1.79-1.77 Ga||Includes Attutra Metagabbro and Kings Legend Metadolerite.|Intrudes Bonya Metamorphics.||
80342|Baikal Supersuite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|||Includes the Fosters Suite, Mascotte Orthogneiss and the Casper Suite,||Undivided meta-igneous rock: tourmaline altered orthogneiss, biotite granodiorite, biotite-hornblende orthogneiss, quartzofeldspathic gneiss and biotite-rich felsic gneiss.|
80342|Baikal Supersuite|72516|2|Defined|iii, p10, p15, p21, p24, p29-32, p189-90|Statherian|Statherian|Aileron Province. Newly defined; named for the community of Baikal (also known as Bonya community). This unit is the dominant igneous lithostratigraphic unit in the Aileron Province on the Jervois Special map sheet. Constituent units sporadically outcrop in the western and central area of the Jervois Range 1:100 sheet area and are generally poorly exposed. See type localities of constituent units for this supersuite. Intrusion of this supersuite resulted in sygenetic base metal mineral deposits. SHRIMP age is interpreted as an igneous crystallisation age. Lithology of undivided Baikal Supersuite is provided. Structure, geochemistry and geophysics are discussed. See also p72, p101-106, p108-110, p119-123, p125-126, p139, p142, p145, p153, p155, p169, p172, p175.|1790 - 1770 Ma.||Includes the Mascotte Orthogneiss, Casper Suite and the Fosters Suite.|Intrudes the Bonya Metamorphics. Intruded by the Tarlton Bore Granite, Boundary Igneous Complex and the Samarkand Pegmatite.|Voluminous I-type and bimodal intrusions with protoliths ranging from gabbro to granodiorite to granite.|14-APR-22
80342|Baikal Supersuite|73591|6|Mentioned|piii, p9-11, p16, p18, p29||||ca 1790-1770 Ma||Fosters Suite, Molyhil Suite, Casper Suite|||
76089|Balbirini Dolostone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1605-1585 Ma.|Unit in Lawn and Wide Supersequence.||||
76089|Balbirini Dolostone|64815|5|Briefly described|p3, p5 Fig.3  |||Up to 1500 m thick.|1589 +/- 3 Ma (Rawlings 1999).|Of the Nathan Group.||||
76089|Balbirini Dolostone|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Generally recessive.||Unit in Nathan Group.||Overlies Reward Dolostone or undivided Umbolooga Subgroup. Is overlain by Limmen Sandstone.|(Stromatolitic-) dololutite, dolarenite, dolomitic siltstone and shale, silty dololutite; diagnostic silicified ooid beds; pink tuff; conical, large columnar, stratiform and domical stromatolites.|20-SEP-11
76089|Balbirini Dolostone|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. 1500 m thick. Shallow-water to emergent: playa and marginal-marine.||Nathan Group||Overlies Smythe Sandstone (conformably) or McArthur Group (unconformably).|Dolomudstone, dolostone, ooid dolograinstone, silty dolomudstone, dolomitic siltstone and shale; rare sandstone, mudstone.|
76089|Balbirini Dolostone|69430|3|Fully described|p15:3, 13, 19, 21-25, 42-43|Calymmian|Statherian|Walker Fault Zone, northern McArthur Basin. Type section is in the Abner Range area within the Batten Fault Zone. Originally (Jackson et al., 1987) included rocks which were later subdivided by Abbott et al. (2001) into four named units: Mount Birch Sandstone, Knuckey and Walmudga Formations, and Yalwarra Volcanics. Less than 1500m thick. Shallow-marine to emergent (continental playa or sabkha) sediments. Appears as Balbirini Dolomite on 15:13. See also references to Lower Balbirini Dolostone (15:3, 19). Hosts the Eastern Creek base metal prospect (described). SHRIMP zircon ages, including another at 1609 +/- 3 Ma, (Page et al., 2000; Jackson and Southgate, 2000) which suggest a major break in the Nathan Group at this level. The lower part may belong to the McArthur Group.|1613 +/- 4 Ma to 1589 +/- 3 Ma.|Nathan Group.||Gradationally overlies Smythe Sandstone. Unconformably overlies Amos Formation and (probably) Jalma Formation. Is overlain conformably by Dungaminnie Formation, and unconformably by Roper Group.|Dololutite, dolomitic siltstone and shale, silty dololutite more common in lower part of unit often with evaporite pseudomorphs and local cauliflower chert; various stromatolite types; diagnostic ooid dolostone beds; rare thin sandstone beds.|10-OCT-19
76089|Balbirini Dolostone|69673|6|Mentioned|p16 fig 13, p32, p35, p40|Paleoproterozoic|Paleoproterozoic|Interlayered with Smythe Sandstone. Reservoir rock with zones of secondary porosity. Up to 1500m thick.||Nathan Group||Conformably overlain by Dungaminnie Formation, Unconformably overlain by Roper Group, overlies Smythe Sandstone, Unconformably Overlies Bath Range Formation|Sandy dolostone, dolomudstone, dolomitic shale, minor intraclastic breccia, silicified ooid dolostone, dolomitic siltstone and potassium rich mudstone.|
76089|Balbirini Dolostone|71374|4|Described|iii, p18-p19, p27, p30|Statherian|Statherian|McArthur Basin. SHRIMP ages are obtained from tuffs in the lower part of this unit and are provided in GA 91779038 and GA 95779074.  Sampling site provided along with zircon description and SHRIMP analytical discussion.|1613 +/- 4 Ma and 1609 +/- 3 Ma (SHRIMP U-Pb)|||Overlies the Smythe Sandstone. Unconformably overlies the Jalma Formation.||
76089|Balbirini Dolostone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1613+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuffite.|
76089|Balbirini Dolostone|72373|5|Briefly described|p21-22,25,28|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Regionally widespread unit. Can be informally divided into upper and lower successions. Contains a tuff dated at 1589+\-3 Ma (SHIRMP U-Pb zircon; Page et al., 2000.||Unit of Nathan Group.|Underlain by Bath Range Formation/Balma Group.|Lowermost unit of Nathan Group.||
76089|Balbirini Dolostone|72377|5|Briefly described|p13, 15|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Does not have an absolute age; reported by Page et al (2000) to be between c. 1613 Ma and 1589 Ma.||Unit of Nathan Group.||Underlain unconformably by Jalma Formation.||10-OCT-19
76089|Balbirini Dolostone|72523|4|Described|piii, 1, Tb.1-2, p2 Fig.2, p3, p8 Fig.7.|Calymmian|Statherian|McArthur Basin. Type section in Abner Range, Mallapunyah, southern BAUHINIA DOWNS map sheet. Informally subdivided, in ascending order, into 'evaporitic unit', 'stromatolitic unit', and 'recrystallised unit'. More detailed descriptions provided. U/Pb SHRIMP dating of two sandstone samples in the lower and medial parts of the Balbirini Dolostone. Maximum depositional ages determined from these samples (1625+/-14 Ma, 1607 +/- 14 Ma) are constrained by ages from underlying units. The detrital zircon spectrum  from the lower sample resembles spectrum of underlying Stretton Sandstone. Previous U-Pb SHRIMP zircon dating of tuffaceous rocks near the base of the evaporitic unit give ages (1609+/-3 Ma, 1613+/-4 Ma) indistinguishable from underlying Amos Formation (1614+/-4 Ma), the 'upper' Balbirini Dolostone returned a much younger SHRIMP U-Pb zircon age of 1598+/-3 Ma from drillhole BMR Bauhinia Downs-3 (Page et al, 2000). Redbeds said to be deposited in a continental (sabkha) setting whilst the carbonates were deposited in a saline lacustrine or shallow marine setting. Appendices A1, A2 provide analytical data on provenance and maximum depostional age. See also p11.|near base: 1609 +/- 3 Ma. near top: 1598+/-3 Ma|Nathan Group||Overlies Amos Formation and Smythe Sandstone and underlies the Dungaminnie Formation.|Basal redbed evaporitic unit of interbedded fine-grained sandstone/siltstone, lesser dolostone; a few beds of tuffaceous siltstone. Stromatolitic unit of cyclic dolostones , thin cross-bedded quartz sandstone. Recrystallised dolarenite at top.|29-OCT-20
76089|Balbirini Dolostone|72527|5|Briefly described|p10.|Calymmian|Paleoproterozoic|Pristine euhedral 'magmatic' zircons from a tuffaceous claystone layer within the uppermost part of this unit yielded an age of 1589 +/- 3 Ma (Jackson et al., 1999, 2000), i.e a minimum age for this unit.|min age from tuff: 1589+/-3 Ma|Nathan Group||||
76089|Balbirini Dolostone|73412|5|Briefly described|p2|||Southern McArthur Basin. Geochronology by Page et al. (2000).|1613 +/- 4 Ma; 1609 +/- 3 Ma.|McArthur Group.|||Includes tuffs.|
81656|Balbirini Dolostone, 'lower'|72373|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Informal subdivision of the Balbirini Dolostone. Contains SHRIMP U-Pb ages from interbedded tuffaceous rocks of 1613+\-4 and 1609+\-3 Ma, which are indistinguishable from those in the Amos Formation. This unit may be better reinterpreted as a new formation at the top of the McArthur Group, underlying Balbirini Dolostone sensu stricto (Haines et al 1999, Rawlings 1999).||||Correlable with max depositional age of Knuckey Formation.||02-OCT-19
81657|Balbirini Dolostone, 'upper'|72373|5|Briefly described|p22,33|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Informal subdivision of the Balbirini Dolostone. Contains SHRIMP U-Pb zircon age of 1589+\-3 Ma (Jackson et al 2000). Significantly younger than tuffs in 'lower' Balbirini Dolostone (1613+/-4 Ma, 1609+/-3 Ma).||||||02-OCT-19
72382|Balma Group, Lower|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Koolatong Siltstone, Strawbridge Breccia.||Mudstone, dolomitic siltstone, stromatolitic-evaporitic dolostone, sandstone, chert breccia.|04-MAR-20
72383|Balma Group, Middle|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Vaughton to Zamia Creek Siltstones.||Dolomitic mudstone (+/- carbonaceous), dolostone; minor pink chert beds (tuff?).|04-MAR-20
72384|Balma Group, Upper|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Yarrawirrie to  Bath Range Formations.||Dolomitic siltstone, sandstone, dolarenite, chertified evaporitic-stromatolitic dolostone; minor conglomerate and pink chert beds (tuff?).|04-MAR-20
25774|Banyan Formation|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
25774|Banyan Formation|24122|5|Briefly described|p4 Fig.3|||Of Bullita Group.  Geological Province: Victoria Basin.||||||
25774|Banyan Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Unconformably overlies Nero Siltstone; unconformably overlain by Wondoan Hill Formation. Geological Province: Victoria Basin||||||
25774|Banyan Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
25774|Banyan Formation|32170|6|Mentioned|Map legend|Adelaidean|Carpentarian|Adelaidean or Carpentarian||||||
25774|Banyan Formation|32660|5|Briefly described|Table 6|||||||||
25774|Banyan Formation|32700|4|Described|Table 1|||See also p14||||||20-JUL-06
25774|Banyan Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25774|Banyan Formation|33377|6|Mentioned|p266|||||||||
25774|Banyan Formation|45112|5|Briefly described|Table 9|||||||||
25774|Banyan Formation|48942|2|Defined|p54|Adelaidean|Adelaidean|||||||
25774|Banyan Formation|60685|5|Briefly described|p4 Figure 3|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Geological Province: Victoria Basin.||||||
25774|Banyan Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Unconformably overlies Nero Siltstone. Is unconformably overlain by Wondoan Hill Formation of the Tijunna Group.||
25774|Banyan Formation|69432|4|Described|p17:2, 12|||Sweet et al. (1974). Birrindudu Basin. 200m thick. May be a carbonate equivalent of the Mount Gordon and Weaner Sandstones and Battle Creek Formation.||Bullita Group.||Unconformably overlies Nero Siltstone. Is overlain unconformably by Wondoan Hill and/or Stubb Formations.|Stromatolitic and oolitic limestone and dolostone, with minor siltstone and sandstone. Hemispherical bioherms and biostromes of columnar stromatolites common in the middle of the unit. Contains rare epigenetic galena.|12-JUL-16
25774|Banyan Formation|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Overlies Nero Siltstone, Unconformably overlain by Wondoan Hill Formation||
25774|Banyan Formation|71302|5|Briefly described|p6||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||||
25774|Banyan Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Unconformably[?] underlain by Nero Siltstone. Overlain[?] by Wondoan Hill Formation (Tijunna Group). Equivalent to Battle Creek Formation and Weaner Sandstone.||
38410|Baralandji Formation|23937|5|Briefly described|p84 App. 1|||Of the Renner Group.  Contains the Grayling and Sweetwater Members.  In HELEN SPRINGS area.  See also p83 Appendix 1.||||||13-APR-05
38410|Baralandji Formation|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||
38410|Baralandji Formation|24303|2|Defined|p28, p60 Appendix|Calymmian|Calymmian|Of the Renner Group. Overlain by the Powell Formation; overlies the Gleeson Formation. Max. Thickness: 700m. Previously mapped as undifferentiated Tomkinson Creek beds. Comprises Sweetwater and Grayling Members. See also p23 Tb.3.||||||18-OCT-05
38410|Baralandji Formation|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Includes the Grayling Member and Sweetwater Member and undifferentiated micaceous sandstone, mudstone and conglomerate.||||||18-OCT-05
38410|Baralandji Formation|24442|5|Briefly described|p15|||Of the Renner Group.  Geological Province: Ashburton Province.||||||
38410|Baralandji Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Renner Group.||||
38410|Baralandji Formation|69431|4|Described|p16:15, 18-21|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. 100-700m thick. Regressive/transgressive succession from shallow-marine (base) to supratidal hypersaline mudflat, to intertidal to high energy subtidal, shallow-marine (top) deposits.||Renner Group.|Sweetwater, Grayling Members.|Gradationally overlies Gleeson Formation. Is overlain gradationally by Powell Formation, and unconformably by Muckaty Sandstone Member (Helen Springs Volcanics).|Fine- to medium-grained sandstone, siltstone and mudstone with minor coarse-grained sandstone and conglomerate. Comprises two major coarsening-upward units (Members) and a number of smaller-scale fining-upward cycles at the top of the Formation.|12-JUL-16
38410|Baralandji Formation|69673|6|Mentioned|p58|||||Renner Group||||
38410|Baralandji Formation|70968|3|Fully described|v,p93,p95,p98-105,p124,p126-127,p131|Calymmian|Calymmian|Hussey, Beier, Crispe and Donnellan in Hussey et al. (2001). Named after a mesa known also as Mount Castle. The complicated type section (described) starts at 361000mE 7992700mN (base) and ends at 364500mE 7988000mN in HELEN 100k sheet. Three reference sections from Hussey et al. (2001) are also given. Crops out extensively in Ashburton Ranges. About 100-700m thick. Detrital zircon diagram.||Renner Group.|Sweetwater, Grayling Members.|Transitionally overlies Gleeson Formation. Is overlain conformably and gradationally by Powell Formation, and unconformably by Muckaty Sandstone Member (Helen Springs Volcanics).|A laminated to thickly bedded succession of very fine- to medium-grained sandstone, siltstone and claystone, and minor coarse- to very coarse-grained sandstone and conglomerate. Contains halite pseudomorphs in lower part; glauconitic in upper part.|
38410|Baralandji Formation|71893|4|Described|iii, p2-p3, p6, p8, p52, p56-p60|Ectasian|Statherian|Tomkinson Province. This unit is predominantly recessive. This unit is interpreted to range from Statherian to Ectasian on the basis of dating of the unconformably underlying Namerinni Group and a SHRIMP U-Pb date of 1295 +/- 14 Ma for an unnamed dyke which intrudes this unit.||Renner Group|Includes the Grayling Member and Sweetwater Member.|Conformably overlies the Gleeson Formation.|Very fine- to medium-grained sandstone, siltstone and claystone, and minor coarse- to very coarse-grained sandstone and conglomerate.|
32954|Barkly Group|24303|6|Mentioned|p2|||Invalid name, no longer in use.||||||
32954|Barkly Group|44283|14|Not recorded|p.4|||Ref. to Noakes & Traves, 1947,1954.||||||20-JUL-06
32954|Barkly Group|44285|14|Not recorded|p.4||Cambrian|Ref. to Noakes, 1951, Noakes & Traves, 1954.||||||
32954|Barkly Group|44301|14|Not recorded|p.4||Cambrian|Ref to Noakes 1951, Noakes & Traves 1954.||||||
32954|Barkly Group|44441|14|Not recorded|p.4,9|||Includes rocks now included in Ranken Limestone. Mid.Cam? (E53-16).||||||
32954|Barkly Group|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|||||||
32954|Barkly Group|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|||||||
32954|Barkly Group|64443|1|Redefined|p3, p9-10, p39-40|Middle Cambrian||Originally of Noakes and Traves (1954), including Ogilvie's Georgina Limestone (1931). Note: reinstatement and revised definition of abandoned name. Correlative of Narpa Group in part, lower Goulburn Group, Daly River Group in part, Montejinni Limestone, Hooker Creek Formation, Lothari Hill Sandstone, Point Wakefield beds, Goose Hole Group, Tarrara Formation, Hart Spring Sandstone, Pertaoorrta Group; encompasses all Middle Cambrian sedimentary rocks in the central, western and northern Georgina Basin (except Thorntonia Limestone); previously known as Templeton Series, Georgina Series.|||Includes Top Springs Limestone, Gum Ridge Formation, Anthony Lagoon beds, Wonarah Formation, Ranken Limestone, Camooweal Dolostone.|Unconformably overlies Helen Springs Volcanics or Renner Group or South Nicholson Group; conformably underlies Arrinthrunga Formation.|Limestone, dolostone, siltstone; minor quartz sandstone.|14-MAY-14
32954|Barkly Group|65336|4|Described|Map Legend|Middle Cambrian|Middle Cambrian|Of Georgina Basin. Unconformably overlies Narpa Group; unconformably underlies Brunette Limestone. Includes Camooweal Dolostone, Ranken Limestone, Wonarah Formation.||||||29-SEP-11
32954|Barkly Group|65337|6|Mentioned|p61 Table 6, pp65-68.|Middle Cambrian|Middle Cambrian||||Includes Wonarah Formation, Ranken Limestone and Camooweal Dolostone.|||
32954|Barkly Group|67144|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Top Springs Limestone and Anthony Lagoon Formation.|Unconformably overlies Kiana Group.||13-APR-12
32954|Barkly Group|67148|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge and Wonarah Formations.|||
32954|Barkly Group|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge, Anthony Lagoon and Wonarah Formations.|||
32954|Barkly Group|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin.|||Includes Gum Ridge, Anthony Lagoon and Wonarah Formations.|||
32954|Barkly Group|67323|6|Mentioned|GIS attrib tbl, Solid Geology Map.||||||Includes Camooweal Dolomite|||
32954|Barkly Group|67352|4|Described|v, p5, p19, p44 fig 48|Middle Cambrian|Middle Cambrian|Noakes and Traves (1954); Kruse and Radke (2008). Included the Cambrian rocks with rocks in the Hatches Creek tungsten field in this unit.|||Top Springs Limestone, Gum Ridge Formation, Wonarah Formation, Anthony Lagoon Formation|||
32954|Barkly Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
32954|Barkly Group|69443|4|Described|p28:3, 5, 7, 14, 20-25|Middle Cambrian|Middle Cambrian|Noakes and Traves (1954), modified by Kruse and Radke (2008). Barkly and Undilla Sub-basins, Georgina Basin. Includes all Middle Cambrian sedimentary rocks in the central, western and northern Georgina Basin (except Thorntonia Limestone); correlative rocks in the southern and eastern parts of the Basin constitute the Narpa Group. Widely distributed. Correlative of Narpa and Daly River Groups. Is also correlated with the following: lower Goulburn Group (Arafura Basin); Goose Hole Group (Ord Basin); Pertaoorrta Group (Amadeus Basin) in part; Montejinni Limestone, Hooker Creek Formation, Lothari Hill Sandstone and Point Wakefield beds (Wiso Basin); Tarrara Formation, Hart Spring Sandstone, Skewthorpe Formation and Pretlove Sandstone (Bonaparte Basin).|||Gum Ridge, Anthony Lagoon, Wonarah Formations; Top Springs, Ranken Limestones; Camooweal Dolostone.|Unconformably overlies Thorntonia Limestone (Narpa Group) and Helen Springs Volcanics or Renner and South Nicholson Groups. Is overlain conformably by Arrinthrunga Formation.||12-JUL-16
32954|Barkly Group|69591|5|Briefly described|p29, p88|Cambrian|Cambrian|Kruse et al. (2002). Undilla Sub-basin, Georgina Basin.|||Camnooweal Dolostone; Wonarah, Anthony Lagoon, Gum Ridge Formations; Ranken, Top Springs Limestones.|||
32954|Barkly Group|69673|6|Mentioned|p117||||||Includes Gum Ridge Formation, Top Springs Limestone, Anthony Lagoon Formation, Wonarah Formation, Ranken Limestone, Camooweal Dolostone|||
32954|Barkly Group|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Camooweal Dolomite.|||
32954|Barkly Group|72415|4|Described|mapsheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Camooweal Dolomite.|||
32954|Barkly Group|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|||||||
32954|Barkly Group|72919|6|Mentioned|p77|||Georgina Basin. 467 m intersected in drillhole CRDD001.|||Underlain by Helen Springs Volcanics.|||
32954|Barkly Group|72967|6|Mentioned|p5|||Georgina Basin.|||Wonarah Formation, Anthony Lagoon Formation|||
32954|Barkly Group|73083|6|Mentioned|p28||||||Anthony Lagoon Formation|||
35484|Barramundi Metamorphics|23197|6|Mentioned|Fig.1|||||||||
35484|Barramundi Metamorphics|23968|6|Mentioned|p1365 Fig. 21|||Geological Province: McArthur Basin.||||||
27283|Barrow Creek Granite Complex|23733|5|Briefly described|p32 Fig. 19|||See also p34 Fig. 20.  Age: c.1805Ma.||||||
27283|Barrow Creek Granite Complex|23809|5|Briefly described|p27 Fig. 25|Paleoproterozoic|Paleoproterozoic|Age: 1830+/-6Ma and 1809+/-5Ma.||||||07-NOV-08
27283|Barrow Creek Granite Complex|42643|2|Defined|p50|Mesoproterozoic|Paleoproterozoic|Variation on Barrow Creek Granite?||||||07-NOV-08
27283|Barrow Creek Granite Complex|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27283|Barrow Creek Granite Complex|64735|5|Briefly described|p205 Fig 1, p206|Orosirian|Orosirian|See also misnamings: Barrow Creek Igneous Complex (p215), and Barrow Creek Gts in Fig 2 and Fig 15.|1809+/-5 Ma, 1806+/-6 Ma.||Includes Ooralingie Granite, Beantree Granite.|Intrudes Bullion Schist.||20-APR-12
27283|Barrow Creek Granite Complex|69425|6|Mentioned|p10:3|||||||||12-JUL-16
27283|Barrow Creek Granite Complex|69427|5|Briefly described|p12:6, 20, 22|Orosirian|Orosirian|Haines et al. (1991); formerly Barrow Creek Granite (Smith and Milligan, 1964). Encompasses granite that crops out within 15km of Barrow Creek roadhouse.|1810-1800 Ma.||Ooralingie and Bean Tree Granites.|Intrudes the Bullion Schist.||12-JUL-16
27283|Barrow Creek Granite Complex|71592|5|Briefly described|Appendix A.|||Tennant Creek Region. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|1838+/-4 Ma and 1819+/-6 Ma.||||Granodiorite, orthogneiss.|
27283|Barrow Creek Granite Complex|72378|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. |||Includes Ooralingie Granite, Bean Tree Granite.|||
79871|Bawaka Granite|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1872+/-3 Ma (crystallisation: Pb/Pb zircon).||||Granite.|
79871|Bawaka Granite|71605|5|Briefly described|iii, p9, p28, p30||Orosirian|Arnhem Province. S-type granite, interpreted to have been derived from the sedimentary rocks that were metamorphosed to the Melville Bay Metamorphics. |1872 +/- 3 Ma, SHRIMP U-Pb, Kositicin et al 2015a|||||
79871|Bawaka Granite|71620|4|Described|iv, p6, p13, p16, p18, p21, p23, p28|Orosirian|Orosirian|Arnhem Province. SHRIMP age interpreted as the igneous crystallisation age of this unit. Derived from melting of the Melville Bay Metamorphics. Melt generation may be recorded at 1873 +/- 6 Ma and 1868 +/- 8 Ma (metamorphic ages from the Melville Bay Metamorphics).|1872 +/- 3 Ma (SHRIMP Pb/Pb Kositcin et al, 2015)||||S-type granite.|
79871|Bawaka Granite|72365|5|Briefly described|iii,p1,7,14,20,25-27,31-34,36|Orosirian|Orosirian|Geological province: Arnhem Province. S-type granite formed from partial melts of Melville Bay Metamorphics between c. 1880 Ma and ca. 1859 Ma (see Summary section for references). Sample GV14SKR008 (granite; 694738E 8615972E) records detrital zircon spectrum interpreted to represent multiple pulses of zircon growth semicontinuously between 1887+\-9 and 1861+\-9 Ma. 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. Dated sample and sample location are provided.|||||Grey-orange, medium-grained, feldspar megacrystic, garnet-cordierite-biotite granite.|09-JAN-20
79871|Bawaka Granite|72377|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Geological province: Arnhem Province. Interpreted to be co-magmatic with Drimmie Head Granite, and Orunyah Granite.|c. 1872 Ma|||||
24175|Bean Tree Granite|22524|6|Mentioned|p41|||||||||
24175|Bean Tree Granite|23733|5|Briefly described|p45 App. 2|Paleoproterozoic|Paleoproterozoic|Of Barrow Creek Granite Complex. Age: 1803Ma.||||||07-NOV-08
24175|Bean Tree Granite|23809|5|Briefly described|p42, p41 Tb. 5|Paleoproterozoic|Paleoproterozoic|Two-mica granite.  Age: 1803+/-6Ma.  Intrudes the Bullion Schist.  Geological Province: Arunta Province.||||||07-NOV-08
24175|Bean Tree Granite|24197|5|Briefly described|p18, p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Barrow Creek Suite. Age: 1713Ma. Geological province: Arunta Inlier.||||||07-FEB-11
24175|Bean Tree Granite|42643|2|Defined|p51|Mesoproterozoic|Mesoproterozoic|Of Barrow Granite Complex. Reserved. Defn card avail.||||||24-JUL-06
24175|Bean Tree Granite|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Barrow Creek Granite Complex. Biotite-muscovite granite, leucocratic, fine to medium grained, porphyritic to even grained.||||||07-NOV-08
24175|Bean Tree Granite|50369|5|Briefly described|p1.4, 17.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Barrow Creek Suite.||||||07-NOV-08
24175|Bean Tree Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite granite with porphyritic K-feldspar, and locally abundant enclaves and xenoliths; minor orthogneiss; and, equigranular to porphyritic biotite and biotite-muscovite granite, respectively.  In the Tennant Creek region.||||||07-NOV-08
24175|Bean Tree Granite|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Presented, in Fig.1, as Ooralingie & Bean Tree Gr||||||
24175|Bean Tree Granite|65232|6|Mentioned|p65, App. 2|||Minor vein-type uranium occurrences. Torbenite and carnotite coatings on fracture planes within.||||||09-FEB-10
24175|Bean Tree Granite|65338|6|Mentioned|p39.|Statherian|Orosirian|In BARROW CREEK area.|1803 +/- 6 Ma.|||||
24175|Bean Tree Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Equigranular to porphyritic, biotite and biotite-muscovite granite.|
24175|Bean Tree Granite|69424|5|Briefly described|p9:29|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Textural and compositional differences make it unlikely the nearby Warrego Granite is of similar age.|1803 +/- 6 Ma.|||||12-JUL-16
24175|Bean Tree Granite|69427|4|Described|p12:19, 22, 59, 63|Statherian|Orosirian|Barrow Creek area, Aileron Province. SHRIMP U-Pb zircon age. Probably the parent to the Sn-Ta pegmatites of the Barrow Creek field. Hosts the Barrow Creek U occurrence.|1803 +/- 6 Ma (Smith, 2001).|Barrow Creek Granite Complex.||Intrudes Bullion Schist, Lander Rock Formation and Ooralingie Granite.|Fine- to medium-grained, undeformed to weakly foliated, tourmaline-bearing biotite-muscovite leucogranite.|12-JUL-16
24175|Bean Tree Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1803+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
24175|Bean Tree Granite|72378|5|Briefly described|p22|Orosirian|Orosirian|Geological province: Aileron Province. SHRIMP 207Pb/206Pb zircon crystallisation age of 1806+\-6 Ma (Smith 2001), thereby constraining minimum depositional age of Bullion Schist sedimentary protolith.|1806+\-6 Ma (207Pb/206Pb; magmatic)|Unit of Barrow Creek Granite Complex.||Intrudes into Bullion Schist.||
26378|Beestons Formation|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
26378|Beestons Formation|22810|4|Described|Table2 P5, P11|||Maximum thickness: 200m. Unconformable on Rum Jungle and Waterhouse Complexes.||||||02-DEC-08
26378|Beestons Formation|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Part of the Namoona Group. Fine to medium grained friable quartz sandstone and quartzite; quartz pebble and cobble conglomerate; quartz-mica schist.||||||02-DEC-08
26378|Beestons Formation|23714|4|Described|p9|Proterozoic|Proterozoic|See also page 8 Table 1. Overlain by Celia Dolomite. Max. thickness: 300 m.||||||20-NOV-06
26378|Beestons Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the Namoona Group, in the Rum Jungle Region||||||
26378|Beestons Formation|23733|5|Briefly described|p32 Fig. 19|||Of Namoona Group.||||||
26378|Beestons Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of Namoona Group.  Arkose, sandstone, conglomerate.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
26378|Beestons Formation|30838|6|Mentioned|Fig.1|||||||||
26378|Beestons Formation|32660|5|Briefly described|Table 2|||||||||
26378|Beestons Formation|32819|6|Mentioned|p35|||||||||
26378|Beestons Formation|32873|5|Briefly described|p36|||Lithology. See also Figs. 1 and 15.||||||02-DEC-08
26378|Beestons Formation|32875|5|Briefly described|Fig.1|||||||||
26378|Beestons Formation|33278|5|Briefly described|Fig.2|||||||||
26378|Beestons Formation|35055|5|Briefly described|p222|||||||||
26378|Beestons Formation|35140|6|Mentioned|Fig.2|||||||||
26378|Beestons Formation|35247|6|Mentioned|Fig.2|||||||||
26378|Beestons Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
26378|Beestons Formation|37462|6|Mentioned|Fig.4.8|||||||||
26378|Beestons Formation|38239|6|Mentioned|Fig.2|||||||||
26378|Beestons Formation|38349|6|Mentioned|Table 4|||||||||
26378|Beestons Formation|38351|6|Mentioned|Table 3|||||||||
26378|Beestons Formation|39069|5|Briefly described|Table 1|||||||||
26378|Beestons Formation|39320|6|Mentioned|Fig.2|||||||||
26378|Beestons Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26378|Beestons Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group. Quartz conglomerate and grit, arkose, sandstone, orthoquartzite and quartz sandstone.||||||07-NOV-08
26378|Beestons Formation|40243|6|Mentioned|Fig.2|||||||||
26378|Beestons Formation|40493|5|Briefly described|Table 1|||||||||
26378|Beestons Formation|40495|6|Mentioned|Fig.5|||||||||
26378|Beestons Formation|40808|5|Briefly described|Table 2|||||||||
26378|Beestons Formation|40852|5|Briefly described|p25|||||||||
26378|Beestons Formation|41125|6|Mentioned|Fig.14|||||||||
26378|Beestons Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
26378|Beestons Formation|41305|4|Described|p10|||||||||
26378|Beestons Formation|41397|6|Mentioned|p7|||||||||
26378|Beestons Formation|41663|4|Described|p3|||||||||
26378|Beestons Formation|43187|5|Briefly described|p2|||||||||
26378|Beestons Formation|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|Of Batchelor Group. Max. thickness: 1200m.||||||07-NOV-08
26378|Beestons Formation|43832|6|Mentioned|14|||||||||
26378|Beestons Formation|44314|2|Defined|p.5-7,map|||(D52-4). Darwin Sheet.||||||
26378|Beestons Formation|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26378|Beestons Formation|45022|14|Not recorded|p.26,41,43 Fig7, Tb2||Paleoproterozoic|Of Bachelor Group Pl. 28,30||||||07-NOV-08
26378|Beestons Formation|46658|6|Mentioned|p548|||||||||
26378|Beestons Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group.  Quartz conglomerate and grit, arkose, sandstone; minor banded iron formation, pebble to boulder conglomerate; orthoquartzite and quartz sandstone, in places containing magnetite.||||||07-NOV-08
26378|Beestons Formation|46676|14|Not recorded|p.6||Paleoproterozoic|L.Proterozoic. Unit of Batchelor Group.||||||07-NOV-08
26378|Beestons Formation|46700|6|Mentioned|P12|||||||||
26378|Beestons Formation|47049|5|Briefly described|Table|||Moved from Batchelor Gp to Namoona Gp; facies variant of Masson Fm.||||||02-DEC-08
26378|Beestons Formation|50623|4|Described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Rum Jungle Basement. Fluvial to shallow marine. Of Manton Group.||||||07-NOV-08
26378|Beestons Formation|60575|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Namoona Group.||||||07-NOV-08
26378|Beestons Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Manton Group.  Quartz conglomerate and grit, arkose, quartz sandstone, orthoquartzite; minor banded iron formation, pebble to boulder conglomerate. Overlies Rum Jungle Complex. Overlain by Celia Dolostone.||||||14-NOV-06
26378|Beestons Formation|61389|5|Briefly described|Map Legend|||Of the Manton Group. Quartz conglomerate, grit, arkose, sandstone; minor BIF, pebble-boulder conglomerate.||||||30-SEP-05
26378|Beestons Formation|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Arkose, sandstone, conglomerate. Geological Province: Pine Creek Orogen.||||||09-FEB-10
26378|Beestons Formation|63866|5|Briefly described|p108|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. Numeric date is a maximum depositional age.|2506 +/- 14 Ma (Cross et al., 2005)|||||
26378|Beestons Formation|64662|6|Mentioned|p42 Fig. 17, p44|||Unconformably overlies Rum Jungle Complex.Geological Province: Pine Creek Orogen.Sample dominated by detrital zircon ~2.5Ga old, like Ferdies Member, Dead Bullock Formation, Tanami region. Could indicate widespread Neoarchean crust in northern Australia.||||||07-FEB-11
26378|Beestons Formation|64676|5|Briefly described|v, p1, p18-21|||Basal unit of the Pine Creek Orogen. Has a predominantly Neoarchean provenance.|<2506 +/- 14 (maximum deposition age) U/Pb SHRIMP.|||Unconformably overlies Rum Jungle Complex.|Arkose.|18-JAN-17
26378|Beestons Formation|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Of Manton Group. Max Thickness 300m. Quartz conglomerate, feldspathic quartz sandstone.||||||07-JAN-09
26378|Beestons Formation|64730|5|Briefly described|p124, 125 Fig. 3|Paleoproterozoic|Paleoproterozoic|||Of Manton Group.||Underlies Celia Dolostone.|Immature fluviatile arkose and conglomerates.|02-MAY-12
26378|Beestons Formation|65232|5|Briefly described|p51, p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Of Manton Group. Under Celia Dolostone. Fluvial to shallow-marine clastic sedimentary rocks. Arkose, sandstone conglomerate.||||||09-FEB-10
26378|Beestons Formation|65339|4|Described|p7. |||<200 m thick. The feldspathic/arkosic angular matrix in the conglomerates indicates a nearby granitic source. Correlated with Masson Formation, to the east.||Basal unit in Manton Group.||Unconformably overlies Rum Jungle Complex. Is overlain by Celia Dolostone.|Quartz conglomerate and grit, arkose, sandstone; minor banded ironstone, pebble to boulder conglomerate.|
26378|Beestons Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Manton Group.||Is overlain by Celia Dolostone.|Quartz conglomerate, feldspathic quartz sandstone, minor banded ironstone.|23-NOV-11
26378|Beestons Formation|67355|4|Described|p6-10, p12, p15, p26, p47, p60, p65||Neoarchean|Previously assigned to the Batchelor Group (Walpole et al., 1968), and Namoona Group (Needham and Stuart-Smith, 1984). Maximum depositional age (Lally 2002, Lally and Worden 2004). Hosts a thorium prospect.|2506 +/- 14 Ma (SHRIMP zircon)|Manton Group||Conformably underlies the Celia Dolostone, unconformably overlies the Rum Jungle Complex. Correlated with the Masson Formation, Kakadu Group and Cahill Formation.|Medium to coarse, massive quartz sandstone with minor conglomerate.|25-JAN-17
26378|Beestons Formation|67564|5|Briefly described|p9 Fig.4, p11. |Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen. Correlative of Masson Formation and Kakadu Group.||Unit in Manton Group.|||Arkose, sandstone, conglomerate.|
26378|Beestons Formation|67779|5|Briefly described|p6 Fig.5, p16.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. May correlate with Kudjumarndi Quartzite.||Lower unit in Manton Group.||Is overlain by Celia Dolostone.|Conglomerate, coarse-grained arkosic sandstone, quartz sandstone and minor siltstone.|
26378|Beestons Formation|69419|5|Briefly described|p4:3-4,|Paleoproterozoic|Archean|Includes clasts which contain preserved tightly-refolded folds from previous deformation. Dominant detrital zircon age peak is c.2535 Ma.||||Nonconformably overlies Rum Jungle Complex and Stanley Metamorphics.|Arkose; basal quartz-pebble conglomerate includes mineral grains derived from the basement.|12-JUL-16
26378|Beestons Formation|69420|4|Described|p5:4, 6, 8-10, 16, 75|Paleoproterozoic|Paleoproterozoic|Rum Jungle region, Central Domain, Pine Creek Orogen. Up to 300m thick. Fluvial deposits. Maximum deposition age from detrital zircons. Similar Neoarchean detrital zircon population peaks as Acacia Gap Quartzite Member: indicate a provenance in a Rum Jungle Complex-type Archean terrane.|<2506 +/- 14 Ma.|Manton Group.||Unconformably overlies the Rum Jungle Complex. Is overlain conformably by Celia Dolostone.|Quartz conglomerate, grit, arkose, quartz sandstone and minor siltstone.|12-JUL-16
26378|Beestons Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Manton Group.||Is overlain conformably by Celia Dolostone.|Quartz conglomerate; feldspathic quartz sandstone; minor banded ironstone.|
41843|Belt Granite|67565|2|Defined|p61-62, p21, p6 Table 1, p32.|Statherian|Statherian|New name, after Belt Range. Previously within undifferentiated Arunta Complex (Ranford, 1969). Type locality 6 km SSE of Alkipi Outstation. Yaya Domain, Warumpi Province. Outcrops in subdued topography north of Belt Range. Interpreted to have intruded during 1640-1635 Ma Liebig Orogeny. Was metamorphosed at upper amphibolite facies and strongly deformed by 1590-1560 Chewings Orogeny. Geochemistry is discussed briefly.|1640-1630 Ma.|||Intrudes Alkipi Metamorphics and Yaya Metamorphic Complex. Is intruded by Stuart Pass Dolerite. Is thrust-faulted against Bitter Springs Formation.|Foliated, weakly porphyritic biotite +/- hornblende granite and granodiorite; K-feldspar phenocrysts 0.5-1.0 cm diameter; intruded by leucogranite and aplite dykes; variably-developed biotite foliation; contains minor hornblende-bearing leucosomes.|01-DEC-15
41843|Belt Granite|69428|5|Briefly described|p13:11|||Scrimgeour et al. (2005). Forms subdued topography N of the Belt Range.||||Intrudes Yaya Metamorphic Complex. Is intruded by Stuart Pass Dolerite.|Foliated, weakly porphyritic biotite and biotite-hornblende granite and granodiorite.|12-JUL-16
23374|Benalla Formation|13194|4|Described|p386 Tb. 4-16|Norian|Carnian|Type Section: North Hibernia 1 well (2553-3631m). Up to 1100m thick open-marine shelf deposits.||Sahul Group||Coeval with Challis Formation and Nome Formation.|Carbonate; minor shale and sandstone.|
23374|Benalla Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
23374|Benalla Formation|41532|2|Defined|p304|Middle Triassic||WA Definition. Same unit as Benalla Formation, NT.||||||08-NOV-06
23374|Benalla Formation|41716|5|Briefly described|p334|||||||||
23374|Benalla Formation|42442|2|Defined|p23|Norian|Carnian|NT Definition. Same unit as Benalla Formation, WA .||||||24-JUL-06
23374|Benalla Formation|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||||12-JUL-16
23374|Benalla Formation|70061|6|Mentioned|Regional geology Fig.7|Norian|Norian|||Sahul Group.||||12-JUL-16
42492|Benmara Group|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Includes the Buddycurrawa Volcanics and the Breakfast Sandstone.  Stratgraphic equivalent of Peter Creek Volcanics (Queensland).||||||07-NOV-08
42492|Benmara Group|62659|5|Briefly described|Map Legend|Statherian|Statherian|||||||
42492|Benmara Group|65337|4|Described| p10 Table 3, pp17-18, p86.|Paleoproterozoic|Paleoproterozoic|Tentatively interpreted to be thin (400 m) volcanic expression of McNamara Group. Unusual intermediate volcanics host microdiamond and indicator mineral anomalism along Benmara Fault. Recessive to weakly resistant.|||Includes Breakfast Sandstone and Buddycurrawa Volcanics.|Unconformably overlies Murphy Metamorphics and Connelly Volcanics. Is unconformably overlain by South Nicholson Group.|Mixed succession of sandstone, mudstone, conglomerate, stromatolitic chert, trachyte and volcaniclastic sandstone.|
42492|Benmara Group|69433|5|Briefly described|p18:1-5|Statherian|Statherian|Rawlings et al. (2008); previously Benmara beds (Smith and Roberts, 1963). Northern succession, Lawn Hill Platform.|||Breakfast Sandstone, Buddycurrawa Volcanics.|Unconformably overlies Murphy Metamorphics and Connellys Volcanics. Is overlain unconformably by South Nicholson Group.||12-JUL-16
42492|Benmara Group|69434|5|Briefly described|p19:4-5|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||||Is probably overlain unconformably by Crow Formation (South Nicholson Group).||12-JUL-16
42492|Benmara Group|69673|6|Mentioned|p51||||||Includes Buddycurrawa Volcanics, Breakfast Sandstone|||
42492|Benmara Group|72526|5|Briefly described|p5, p6 Fig.1.2, p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the west of the South Nicholson Basin.|||Includes Buddycurrawa Volcanics and Breakfast Sandstone.|Shown as overlying Peters Creek Volcanics and unconformably underlies South Nicholson Group.|Includes sandstone and volcanic rocks.|
42492|Benmara Group|72527|5|Briefly described|p1, p3,p5, p7,  p78, p86.|Paleoproterozoic|Paleoproterozoic||||Includes Buddycurrawa Volcanics and Breakfast Sandstone.|Overlain by Bowgan Sandstone, Crow Formation probably unconformably.||
42492|Benmara Group|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Western South Nicholson Basin.|||Buddycurrawa Volcanics and Breakfast Sandstone.|Unconformably underlies South Nicholson Group.||
42492|Benmara Group|72919|6|Mentioned|p1, p3, p5, p16, p71, p93, p98|Paleoproterozoic|Paleoproterozoic|Isa Superbasin. Unconformably overlies metamorphic rocks of the Murphy Province. An expanded version of this unit was proposed by Carson et al. (2020) to include strata of [or equivalent to?] the Mittiebah Sandstone, Crow Formation, and Bowgan Sandstone in the hanging wall of the Benmara Fault based on comparison of detrital zircon spectra with that of late Paleoproterozoic successions.|||Breakfast Sandstone, Buddycurrawa Volcanics|Equivalent to McNamara Group.||
42492|Benmara Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.|||Mittiebah* Formation, Crow* Formation, Bowgan Sandstone, Caulfield beds, Buddycurrawa Volcanics, Breakfast Sandstone.|||
75949|Benning Gabbro|67232|2|Defined|p35, iv, p8-9, 17-19, 28-29|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Previously part of Wangi Basics, now abandoned. Type locality is a prominent sill within Chilling Sandstone. Disrupted by SSW-trending faults. Feldspars undergone sausseritisation/sericitisation; minor chlorite alteration. Strong positive magnetic response. Geochemistry is described in detail. Interpreted as part of a post-collisional remnant-arc regime.||||Intrudes Burrell Creek Formation and Chilling Sandstone.|Metamorphosed high-Ti tholeiitic gabbro, mostly occurring as NE-trending linear sills; mostly quartz-hypersthene normative; equigranular assemblages of (rare) quartz, plagioclase, clinopyroxene, hornblende; fibrous actinolite/tremolite common.|18-NOV-11
75949|Benning Gabbro|67779|6|Mentioned|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||||||
75949|Benning Gabbro|69420|5|Briefly described|p5:4, 29|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Part of the obsolete Wangi Basics. Shows geochemical affinities with island-arc magmatism. |||||High-Ti rift tholeiite.|12-JUL-16
24715|Bessie Creek Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
24715|Bessie Creek Sandstone|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24715|Bessie Creek Sandstone|23216|5|Briefly described|Table1p8,33-4|||||||||
24715|Bessie Creek Sandstone|23404|5|Briefly described|p645|||||||||
24715|Bessie Creek Sandstone|23776|5|Briefly described|p709|||Of Roper Group.||||||
24715|Bessie Creek Sandstone|23937|2|Defined|p74 App. 1|Calymmian|Calymmian|Now assigned to the redefined Maiwok Subgroup (Roper Group). Conformably overlain by Velkerri Formation; overlies the Corcoran Formation.  Max. thickness: 56m, 217m in type section on BAUHINIA DOWNS.  Geological Province: McArthur Basin. See also p42.||||||13-APR-05
24715|Bessie Creek Sandstone|24048|4|Described|p71|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
24715|Bessie Creek Sandstone|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: buff to red-brown, fine to coarse-grained, thin to medium-bedded; common thin to medium quartz granule conglomerate beds, planar and trough cross-beds, ripples. Geol. Prov: McArthur Basin.||||||13-OCT-05
24715|Bessie Creek Sandstone|24050|4|Described|p50, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Medium-grained quartz sandstone.  Of the Roper Group.  Overlies Corcoran Formation.  Max. thickness: >10m.||||||24-JUL-06
24715|Bessie Creek Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
24715|Bessie Creek Sandstone|24303|5|Briefly described|p34, p61 Appendix|||Of the Roper Group. Geological Province: McArthur Basin. Correlates with the Jangirulu Formation. See also p24 Tb. 4.||||||
24715|Bessie Creek Sandstone|32660|5|Briefly described|Table 4|||||||||
24715|Bessie Creek Sandstone|37568|6|Mentioned|Fig.6|||||||||
24715|Bessie Creek Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24715|Bessie Creek Sandstone|40691|6|Mentioned|p64|||||||||
24715|Bessie Creek Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24715|Bessie Creek Sandstone|41268|6|Mentioned|p292|||||||||
24715|Bessie Creek Sandstone|41531|6|Mentioned|p167|||||||||
24715|Bessie Creek Sandstone|42385|6|Mentioned|p30|||||||||
24715|Bessie Creek Sandstone|42395|6|Mentioned|Fig.26 P86|||||||||
24715|Bessie Creek Sandstone|42597|5|Briefly described|Map Legend|Adelaidean||||||||
24715|Bessie Creek Sandstone|42639|4|Described|p44, Table 7 p39|||||||||
24715|Bessie Creek Sandstone|42812|3|Fully described|p53, Table 5|||Of Roper Group.||||||24-JUL-06
24715|Bessie Creek Sandstone|42846|5|Briefly described|Fig.1 p502|||Of Roper Group. Geological Province: McArthur Basin.||||||09-MAY-05
24715|Bessie Creek Sandstone|43010|4|Described|Table 30.|||Of Roper Group||||||24-JUL-06
24715|Bessie Creek Sandstone|43036|6|Mentioned|Fig.5|||of Roper Group||||||
24715|Bessie Creek Sandstone|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||24-JUL-06
24715|Bessie Creek Sandstone|43645|5|Briefly described|p562|||||||||
24715|Bessie Creek Sandstone|43652|6|Mentioned|p386|||||||||
24715|Bessie Creek Sandstone|44112|6|Mentioned|Fig11p30|||||||||
24715|Bessie Creek Sandstone|44201|14|Not recorded|p.9|||||||||
24715|Bessie Creek Sandstone|44287|14|Not recorded|p.12,18, opp.11|||(E53-3).||||||
24715|Bessie Creek Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone, Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44299|4|Described|p.13|||SD/53-7,8. U (?) Proterozoic. Table 1.||||||
24715|Bessie Creek Sandstone|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic, pt of Roper Gp.||||||
24715|Bessie Creek Sandstone|44332|14|Not recorded|p.8-9,12,opp.6,map|||(D53-14). Friable.||||||
24715|Bessie Creek Sandstone|44333|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Mt.Marubma Sheet. (D53-6).||||||
24715|Bessie Creek Sandstone|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44434|14|Not recorded|p.8, opp. p.6, map|||(D53-11,12).||||||
24715|Bessie Creek Sandstone|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44459|14|Not recorded|p.8, opp.p.6, map|||(E53-2). Formation of Roper Group.||||||
24715|Bessie Creek Sandstone|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|44471|14|Not recorded|p.9,opp.p.7, map|||(D53-10). See also p.10,14, for more details.||||||
24715|Bessie Creek Sandstone|44472|5|Briefly described|map legend|||Of the Roper Group.  Massive white friable quartz sandstone.  Upper (?) Proterozoic.||||||02-DEC-04
24715|Bessie Creek Sandstone|44530|14|Not recorded|p.12,18,opp, 12|||(D53-15).||||||
24715|Bessie Creek Sandstone|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
24715|Bessie Creek Sandstone|45022|14|Not recorded|p.78,81, TB11, PL28||Adelaidean|Of Roper Group||||||
24715|Bessie Creek Sandstone|45162|6|Mentioned|Fig.4|||||||||
24715|Bessie Creek Sandstone|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
24715|Bessie Creek Sandstone|46861|6|Mentioned|Fig.2A|||||||||
24715|Bessie Creek Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
24715|Bessie Creek Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Maiwok Subgroup, underlain by Corcoran Formation.||||||
24715|Bessie Creek Sandstone|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
24715|Bessie Creek Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Quartz sandstone: fine to medium and locally coarse grained, tough cross-stratifycation, ripple marks.||||||29-SEP-05
24715|Bessie Creek Sandstone|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Quartz arenite: buff to red-brown, fine to coarse-grained, thin to medium-bedded; common thin to medium quartz granule conglomerate be ds, planar and trough cross-beds, ripples. Geol. Prov: McArthur Basin.||||||
24715|Bessie Creek Sandstone|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Morphologically prominent mature quartzite and sandstone deposits. Geological Province: McArthur Basin.||||||26-APR-06
24715|Bessie Creek Sandstone|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
24715|Bessie Creek Sandstone|62759|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Geological Province: Beetaloo Sub-basin. Contains oil reservoirs.||||||05-FEB-08
24715|Bessie Creek Sandstone|64784|4|Described|p2 Fig.2, p3 Fig.3, p4-5, p7, p10 |Proterozoic|Proterozoic|Beetaloo Basin. A significant reservoir in the Basin.||Unit in Roper Group.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.|Generally fine- to very fine-grained with occasional medium grain size, and is light to medium to dark gray in colour. Over 400m thick.|
24715|Bessie Creek Sandstone|64816|5|Briefly described|p1-6, p8-21             |Proterozoic|Proterozoic|A potential reservoir unit for Velkerri Formation oil. Pacific Oil and Gas wells encountered good oil shows at the top of this unit. Chemistry of oil inclusions detailed.||Unit in Roper Group.|||Fine- to medium-grained, well sorted, extremely well-cemented quartz arenite with low visible porosity.|
24715|Bessie Creek Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
24715|Bessie Creek Sandstone|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
24715|Bessie Creek Sandstone|65228|6|Mentioned|Fig.02.|||||Unit in Roper Group.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|65236|5|Briefly described|p2, p3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Overlain by Velkerri Formation. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
24715|Bessie Creek Sandstone|65342|6|Mentioned|p9, p12. |||Daly Basin. Max. thickness at least 61 m.||||||
24715|Bessie Creek Sandstone|69018|4|Described|p449-451, 454, 456, 457, 459-461|Calymmian|Calymmian|Part of marine succession. Estimated maximum burial 2.5 km, corresponding to ~75 degrees C. Contains water/gas/oil inclusions as well as bitumen.||Of Roper Group.||Intruded by 1280-1220 Ma dolerite sill at top, in places. Is overlain by Velkerri Formation.|Fine- to medium-grained, well-sorted and well-cemented quartz arenite|
24715|Bessie Creek Sandstone|69430|4|Described|p15:3, 27, 29-31, 62-63|Calymmian|Calymmian|McArthur Basin. c.20-56m thick; up to 400m in Beetaloo Sub-basin. Coastal tidal platform sediments. Caps mesas and buttes. Forms the spectacular "Ruined City" of joint-bounded, karstically weathered towers up to 50m high. Fair to good conventional hydrocarbon reservoirs occur, and has potential for unconventional reservoirs (basin-centred gas), in structural and diagenetic traps. The overlying Velkerri Formation may have been both source rock and seal.||Maiwok Subgroup.||Disconformably overlies Corcoran Formation. Is overlain conformably by Velkerri Formation.|Fine to medium, locally coarse and granule-rich quartz sandstone; mainly thinly to medium bedded and trough cross-stratified.|12-JUL-16
24715|Bessie Creek Sandstone|69673|5|Briefly described|p20, p32, p36, p40, p44, p46|||Northwestern and Southern McArthur Basin. Conventional reservoir potential. Up to 442m thick.||Maiwok Subgroup||Conformably overlain by Velkerri Formation, Disconformably overlies Corcoran Formation|Sandstone and mudstone with pore filling bitumen in places.|
24715|Bessie Creek Sandstone|70734|5|Briefly described|p14, 16, 17|||McArthur Basin. Tidal platform sandstone.||Of Maiwok Subgroup.||Overlain by Velkerri Formation. Overlies Corcoran Formation.||
24715|Bessie Creek Sandstone|70822|5|Briefly described|p102 fig 1 (A), p104|Mesoproterozoic|Mesoproterozoic|||Roper Group||Overlies Corcoran Formation; overlain by Velkerri Formation.|Sandstone.|
24715|Bessie Creek Sandstone|70897|6|Mentioned|Fig.1.7.6,9|||Appears simply as Bessie in Fig.1.7.6. McArthur Basin.||||||
24715|Bessie Creek Sandstone|70968|2|Defined|v, p39, p42, p47-48, p50-51, p55-59, p61|Ectasian|Ectasian|See also p65, p124, p126-129, p131, p137, p140, p143. Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Included in Maiwok Subgroup by Abbott et al. (2001). Named after Bessie Creek. The type section is NW of Beetle Springs at 605000mE 8143700mN (base) to 604800mE 8143500mN in BAUHINIA DOWNS sheet. Widely distributed in McArthur Basin. Forms spectacular parakarstic landforms, eg the Lost City (Limmen National Park) of joint-bounded towers up to 50m high. Resistant unit. Lithology described and illustrated in some detail. Has potential as conventional and unconventional oil/gas reservoir. Thickness from 25m to 367m; 217m in the type section. Deposition in a high-energy tide-dominated shoreline to shallow shelf setting. Detrital zircon diagram and discussion.||Maiwok Subgroup.||Conformably (locally disconformably) overlies Corcoran Formation. Is overlain conformably by Velkerri Formation. Is intruded by Derim Derim Dolerite sills. Correlated with Jangirulu Formation.|White when fresh, mainly fine- to medium-grained clean quartz sandstone, friable when weathered; mudstone partings and thin, locally abundant intraclast-rich intervals; Liesegang banding common.|
24715|Bessie Creek Sandstone|71059|4|Described|p3, p10|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 10-417m thick. Coastal tidal platform deposits. Estimated shale/tight gas/shale oil and condensate resources detailed.||Maiwok Subgroup.||Conformably to disconformably overlies Corcoran Formation. Is overlain conformably by Velkerri Formation.|Fine to medium, locally coarse and granule-rich quartz sandstone.|
24715|Bessie Creek Sandstone|71488|4|Described|p140-p153|Ectasian|Ectasian|Beetaloo Sub-basin. Ages are interpreted as maximum depositional ages. Deposited in a high-energy tidal shoreline to shallow marine shelf setting.|1386 +/- 13 Ma and 1417 +/- 29 Ma|Maiwok Subgroup||Overlies the Corcoran Formation. Conformably overlain by the Velkerri Formation. Overlain by the Moroak Sandstone.|Highly mature quartz sandstones.|01-MAY-18
24715|Bessie Creek Sandstone|71779|5|Briefly described|iii, p2, p6-p9, p12 fig 9, p24-p25|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin. See also figs on p10, 11.||Of Maiwok Subgroup.||Conformably overlain by the Kalala Member (Velkerri Formation).|Cross-bedded fine sandstone is typical.|24-SEP-18
24715|Bessie Creek Sandstone|71893|4|Described|p2-p5, p8, p28-p31|Calymmian|Calymmian|McArthur Basin. A maximum depositional age of 1575 +/- 19 Ma and a youngest individual age of 1385 +/- 116 Ma are provided. Deposited in a high-energy, tide-dominated shoreline to shallow marine shelf setting. A maximum age is derived from the underlying Showell Member dated at 1493 +/- 4 Ma and a minimum age of 1361 +/- 21 Ma is derived from Re-Os of the Wyworrie Member of the overlying Velkerri Formation. Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Maiwok Subgroup||Conformably (or gradationally) overlies the Corcoran Formation.|Thinly- to medium-bedded, cross-bedded, locally coarse-grained and granule-rich quartz sandstone.|
24715|Bessie Creek Sandstone|72381|4|Described|p771-779|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a high-energy tide dominated shoreline to shallow shelf setting (Pietsch et al. 1991; Abbott et al. 2001; Munson 2016). Deposition is coeval with post-orogenic Mount Isa 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). Maximum depositional age constrained by youngest detrital zircon age of 1386+\-13 Ma (youngest near-concordant detrital zircon; Yang et al., 2018). Combined U-Pb and Hf isotopic analysis indicate a mixed provenance from the north (e.g. Pine Creek Orogen, Halls Creek Orogen) and east or SE (e.g. Mount Isa region and adjacent terranes).|c. 1.4 Ga|Unit of Mailwok Subgroup.||Lowermost unit of Maiwok Subgroup. Overlain by Velkerri Formation. Underlain by Corcoran Formation. Intruded by Derim Derim Dolerite.|Highly mature quartz arenite.|04-OCT-19
24715|Bessie Creek Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Maiwok Subgroup||Overlies Corcoran Formation and underlies Velkerri Formation.||
24715|Bessie Creek Sandstone|72718|6|Mentioned|p7, p10|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Notable seismic reflector (coherent impedance boundaries) used for calibration of well-logs and are continuous over long distances.||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Maiwok Subgroup||Overlies Corcoran Formation and underlies Velkerri Formation.||
24715|Bessie Creek Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Velkerri Formation.||
24715|Bessie Creek Sandstone|73242|5|Briefly described|p39|||||Maiwok Subgroup, Roper Group||Underlain by Corcoran Formation. Overlain by Kalala Member, Velkerri Formation. Intruded by Derim Derim Dolerite.|Includes tidal Sandstone.|
24715|Bessie Creek Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Corcoran Formation. Is overlain by Velkerri Formation.||
30960|Bickerton Rhyolite|22538|6|Mentioned|P713||Orosirian|Age of unit is 1814+/-8 Ma||||||
30960|Bickerton Rhyolite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
30960|Bickerton Rhyolite|22808|2|Defined|30|Orosirian|Orosirian|Of the Bustard Subgroup. Overlying unit: Milyakburra Formation; underlying unit: Abarungkwa Sandstone||||||25-JUL-06
30960|Bickerton Rhyolite|23363|5|Briefly described|344 Fig.3|||||||||
30960|Bickerton Rhyolite|23374|5|Briefly described|p14||Orosirian|Age: U/Pb Zircon 1814+/-8Ma. of McArthur Basin.||||||
30960|Bickerton Rhyolite|24048|3|Fully described|p18|Orosirian|Orosirian|Formerly "Bickerton Volcanics".  Age: 1814+/-8Ma.   Max. Thickness: 250m.  Geological Province: McArthur Basin.||||||
30960|Bickerton Rhyolite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Rhyolite: red, porphyritic (K-feldspar). Geol. Prov: McArthur Basin.||||||13-OCT-05
30960|Bickerton Rhyolite|44112|6|Mentioned|Fig11p30|||||||||
30960|Bickerton Rhyolite|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Age: 1814 +/- 8Ma (SHRIMP). Geological Province: Arnhem Block/McArthur Basin. Of the Bickerton Suite.||||||04-JUN-18
30960|Bickerton Rhyolite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Rhyolite: red, porphyritic (K-feldspar). Geol. Prov: McArthur Basin.||||||
30960|Bickerton Rhyolite|63866|5|Briefly described|p115|Orosirian|Orosirian|Leichhardt/Calvert Superbasin.|1814 +/- 8 Ma (Pietsch et al., 1994)|Bustard Subgroup||||
30960|Bickerton Rhyolite|64817|5|Briefly described|p353 Fig.4, p354, p355 Fig.5 |Orosirian|Orosirian|Caledon Shelf South, McArthur Basin.|1814 +/- 8 Ma (Pietsch et al. 1997).|Of the Bustard Subgroup.|||Felsic volcanics.|04-JUN-18
30960|Bickerton Rhyolite|69430|4|Described|p15:3, 5-6|||NE McArthur Basin. Estimated thickness up to 250m. Large subaerial lava domes and coulees. SHRIMP U-Pb zircon age.|1814 +/- 8 Ma (Pietsch et al., 1997).|Bustard Subgroup.||Conformably overlies and intrudes Abarungkwa Sandstone. Is overlain ?disconformably by Milyakburra Formation. A likely correlative of Edith River Group.|Red, K-feldspar-phyric rhyolite to rhyodacite.|12-JUL-16
30960|Bickerton Rhyolite|69673|5|Briefly described|p16 fig 13|||Northeastern McArthur Basin.|1814 +/- 8 Ma|Bustard Subgroup||Overlain by Milyakburra Formation, Milyema Formation, overlies Abarungkwa Sandstone||04-JUN-18
30960|Bickerton Rhyolite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1814+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
30960|Bickerton Rhyolite|73083|6|Mentioned|p13, p41|||Uniformly white or checkered magnetic appearance.||||||
41376|Big Knob beds|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Quartzose and lithic sandstone, polymict conglomerate.||||||
41376|Big Knob beds|60682|4|Described|p17 Table 4, 20|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Shoal Reach Formation and Spencer Sandstone. Max. Thickness: >20m. Quartzose and lithic sandstone, polymict conglomerate. Outcrops as knolls and ridges. Geological Province: Wolfe Creek Basin.||||||
41376|Big Knob beds|65331|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Shown as part of Duerdin Group, Wolfe Creek Basin, but map symbol does not support this. Quartzose and lithic sandstone, polymict conglomerate,||||||02-FEB-10
41376|Big Knob beds|69442|4|Described|p27:1, 3 Tb.27.1, 27:4-5|||Informal name. Wolfe Basin. Assigned to Duerdin Group by Dunster et al. (2000). Over 20m thick. Deposited possibly in kames and eskers. Crops out as clusters of knolls and short whaleback ridges. Lithologically similar to Bullo River Sandstone and Beasly Knob Member.||Duerdin Group.||Overlies Shoal Reach Formation and Spencer Sandstone (Auvergne Group) probably unconformably. Possibly correlated with Skinner Sandstone.|Poorly sorted, ferruginous quartzic and lithic sandstone, polymictic conglomerate/diamictite.|12-JUL-16
41376|Big Knob beds|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|||Ferruginous sandstone and polymictic conglomerate/diamictite.|
41376|Big Knob beds|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Quartzose and lithic sandstone, polymictic conglomerate.|
25685|Big Sunday Formation|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
25685|Big Sunday Formation|23867|5|Briefly described|Fig. 3|||Of El Sherana Group.  Geological Province: McArthur Basin.||||||
25685|Big Sunday Formation|24197|5|Briefly described|p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Jim Jim Suite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
25685|Big Sunday Formation|24340|5|Briefly described|p147 Fig. 3|||Overlies the Gimbat Ignimbrite Member. Geological Province: Pine Creek Inlier.||||||
25685|Big Sunday Formation|24442|6|Mentioned|p27|||||||||
25685|Big Sunday Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25685|Big Sunday Formation|40248|4|Described|p222|||||||||
25685|Big Sunday Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25685|Big Sunday Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25685|Big Sunday Formation|41125|6|Mentioned|Fig.15|||||||||
25685|Big Sunday Formation|41311|4|Described|p13|||||||||
25685|Big Sunday Formation|41397|4|Described|p15|||||||||
25685|Big Sunday Formation|41407|6|Mentioned|Map legend|Proterozoic||||||||
25685|Big Sunday Formation|42324|5|Briefly described|p5|||||||||
25685|Big Sunday Formation|43140|4|Described|p3||Paleoproterozoic|of El Sherana Group.||||||07-NOV-08
25685|Big Sunday Formation|43187|5|Briefly described|p2|||||||||
25685|Big Sunday Formation|43718|2|Defined|p2,64-90|||||||||
25685|Big Sunday Formation|43832|4|Described|23, Table6 p22||Paleoproterozoic|Age ~1870 Ma.||||||07-NOV-08
25685|Big Sunday Formation|46658|6|Mentioned|p556|||||||||
25685|Big Sunday Formation|47049|5|Briefly described|Table|||Replaces Masson Formation in southern part of South Alligator Valley.||||||
25685|Big Sunday Formation|50586|5|Briefly described|p1.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Jim Jim Suite.||||||07-NOV-08
25685|Big Sunday Formation|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the El Sherana Group (Jim Jim Suite). Interbedded volcanolithic to arkosic sandstone, volcanic sandstone and amygdaloidal, commonly porphyritic basalt in lower section.||||||14-JAN-05
25685|Big Sunday Formation|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of El Sherana Group. Age 1825-1829Ma. Max thick 480m. Interbedded volcanolithic to arkosic sandst, volcanic siltst and amygdaloidal, commonly porphyritic basalt in lower section; rhyolite and rhyolitic ignimbrite in upper section.||||||07-JAN-09
25685|Big Sunday Formation|64730|5|Briefly described|p126|Paleoproterozoic|Paleoproterozoic|Age from underlying Pul Pul Rhyolite (Jagodzinski 1998). See also Big Sunday Sandstone (p125).|Max. deposition age 1829 +/- 5 Ma.|Of El Sherana Group.|||Volcaniclastic sedimentary rocks and mafic and felsic extrusives.|02-MAY-12
25685|Big Sunday Formation|65232|6|Mentioned|p44 Fig. 29, p45, App. 2|||Of El Sherana Group. Greywacke, shales and tuff.||||||09-FEB-10
25685|Big Sunday Formation|67564|3|Fully described|p7 Table 2, p17 Table 3, p22, pp28-29.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. 480 m of lacustrine sediments and subaerial volcanic rocks. Rocks of this unit in the Mount Stow area mapped by Stuart-Smith et al. (1988b) are now included in Mount Bonnie Formation, and in the Turnoff Creek area are now in the Plum Tree Creek Volcanics. Contains rocks previously mapped as Pul Pul Rhyolite Member (BMR 1995) and undivided Edith River Volcanics (Walpole 1963). May have had a common subaerial volcanic source as Pul Pul Rhyolite.||Unit in El Sherana Group.||Disconformably overlies Pul Pul Rhyolite. Is overlain unconformably by Kurrundie Sandstone.|Volcanilithic to arkosic sandstone, volcaniclastic siltstone, amygdaloidal basalt; rhyolite and rhyolitic ignimbrite in upper portion.|
25685|Big Sunday Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Topmost unit in El Sherana Group.||Overlies Pul Pul Rhyolite.||
25685|Big Sunday Formation|69420|4|Described|p5:4, 15, 17, 79|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. South Alligator region. Appears in 5:4 as Big Sunday Sandstone. Up to 480m thick. Lacustrine (sedimentary rocks) and subaerial (volcanic rocks) deposits.||El Sherana Group.||Overlies Pul Pul Rhyolite with a local disconformity. Is overlain unconformably by Kurrundie Sandstone.|A valley fill-type succession of volcanilithic to arkosic sandstone, volcaniclastic siltstone, amygdaloidal basalt; rhyolite and rhyolitic ignimbrite in upper portion.|12-JUL-16
25685|Big Sunday Formation|70293|5|Briefly described|p597-599, p615|Orosirian|Orosirian|Jawoyn Sub-basin.||El Sherana Group||Overlies Pul Pul Rhyolite. Is unconformably overlain by Kurrundie Sandstone (Edith River Group).|Sandstone and amygdaloidal basalt.|
31356|Bigrlyi Member|43275|5|Briefly described|Map Legend||Neoproterozoic|Of Vaughan Springs Quartzite.||||||
31356|Bigrlyi Member|44158|4|Described|p22 Table.2|Neoproterozoic|Neoproterozoic|Of Vaughan Springs Quartzite.||||||25-JUL-06
31356|Bigrlyi Member|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Vaughan Springs Quartzite. Quartz sandstone, minor siltstone. Geological Province: Ngalia Basin.||||||
31356|Bigrlyi Member|65338|5|Briefly described|pp57-58.|||||Unit in Vaughan Springs Quartzite.||Overlies Southwark Granitic Suite. Is overlain by Treuer Member.|Conglomerate; typically granules, pebbles and cobbles of quartzite and vein quartz; local concentrations of corroded magnetite crystals.|
31356|Bigrlyi Member|69439|5|Briefly described|p24:2, 4-5|Cryogenian|Cryogenian|Young et al. (1995). Ngalia Basin, Centralian A Superbasin. Supersequence 1. About 200m thick.||Vaughan Springs Quartzite.||Is overlain conformably by Treuer Member.|Medium- to thickly-bedded quartz sandstone, with minor interbedded mudstone and sandstone; local basal pebble conglomerate with clasts of granitic basement.|12-JUL-16
31356|Bigrlyi Member|69673|6|Mentioned|p105, p107 fig 85|||||Vaughan Springs Quartzite||Overlain by Treuer Member||
70541|Bilba Hills Granite|62378|6|Mentioned|p13|||Macroscopic similarities to the Redhackle Granite.||||||26-NOV-18
42069|Billabong Complex|23809|5|Briefly described|p3 Fig. 1|||See also Billabong complex.||||||10-NOV-04
42069|Billabong Complex|61056|6|Mentioned|p778 Fig. 1a||Archean|Term used in a structural context. Age: 2514+/-3Ma.||||||07-NOV-08
42069|Billabong Complex|62580|5|Briefly described|p8|Archean|Archean|Includes othogneiss. Age: 2514+/-3Ma.||||||07-FEB-11
42069|Billabong Complex|62637|5|Briefly described|Map Legend|Archean|Archean|Upper amphibolite facies biotite gneiss, coarse-grained augen gneiss, strongly foliated.||||||07-NOV-08
42069|Billabong Complex|63261|5|Briefly described|p4 Fig. 1, p9 Fig. 5|Archean|Archean|Structural term in this context? Written also as the informal Billabong complex (p7). Age: 2514+/-3Ma.||||||07-FEB-11
42069|Billabong Complex|63866|6|Mentioned|p92|||Southeast Tanami Region.||||||
42069|Billabong Complex|64573|5|Briefly described|p780, p780 Fig. 1|||Geological Province: Tanami Inlier. Leucocratic graintic gneiss was inferred to have a ca 2530Ma igneous precursor.||||||07-FEB-11
42069|Billabong Complex|64662|5|Briefly described|p30 Fig. 3, p44|Archean|Archean|Shown informally as Billabong complex (p30 Fig. 3). Age: 2514+/-3Ma. Geological Province: Tanami region. Possible source of Archean detrital zircons in Ferdies Member, Dead Bullock Formation.||||||07-FEB-11
42069|Billabong Complex|64722|5|Briefly described|Fig. 2 p3-6, p10|Neoarchean|Neoarchean|Of the Tanami Region.|~2510 Ma.|||||11-APR-12
42069|Billabong Complex|64734|5|Briefly described|p187, p186 Fig.1|Neoarchean||~2510 Ma; basement rocks in the Tanami Region; banded granitic gneisses||||||14-SEP-09
42069|Billabong Complex|65232|6|Mentioned|p2|||Archaean basement inlier. Tanami Region||||||09-FEB-10
42069|Billabong Complex|65358|5|Briefly described|p6|Neoarchean|Neoarchean|Basement in Tanami Region. Includes 2520-2500 Ma amphibolite facies gneiss and metasediments.||||||
42069|Billabong Complex|66129|6|Mentioned|p216 Fig.3|Neoarchean|Neoarchean|Unconformably underlies Dead Bullock Formation. 2514 +/- 3 Ma.||||||
42069|Billabong Complex|66468|5|Briefly described|p16-17, p27|Neoarchean|Neoarchean|2514 +/- 3 Ma (Crispe et al., 2007). Unconformably underlies Dead Bullock Formation.||||||
42069|Billabong Complex|66683|5|Briefly described|p365, p377.|Neoarchean|Neoarchean|Tanami Region. Part of felsic basement to North Australian Craton.|2514 +/- 3 Ma. |||Is overlain by Ferdies Member.||
42069|Billabong Complex|67165|5|Briefly described|Map legend.|Archean|Archean||||||Upper amphibolite facies biotite gneiss, coarse-grained augen gneiss, strongly foliated.|
42069|Billabong Complex|67479|6|Mentioned|p56|||||||||
42069|Billabong Complex|67779|5|Briefly described|p117.|Neoarchean|Neoarchean|Tanami Region. Correlated with Kukalak Gneiss.|2514 +/- 3 Ma (Page et al. 1995).|||||
42069|Billabong Complex|67824|5|Briefly described|p384-386 Figs.1-3, p387|Neoarchean|Neoarchean|Oldest exposed rocks in the Tanami region.|2514 +/- 3 Ma (Page et al., 1995).|||Overlain by the Tanami Group.|High grade metasedimentary rocks and leucogranites.|
42069|Billabong Complex|67826|6|Mentioned|p400, p402 Fig.3|Neoarchean|Neoarchean|Oldest known rocks of the Tanami region. Basement. Age determined using 207Pb/206Pb zircon dating.|2514 +/- 3 Ma||||Gneisses.|
42069|Billabong Complex|68474|6|Mentioned|p572, p574|Neoarchaean|Neoarchaean|Granites-Tanami Orogen. Oldest rocks in the Orogen.|ca. 2514 +/- 3 Ma ||||Leucocratic orthogneiss and schistose metasedimentary and felsic volcanic rocks.|
42069|Billabong Complex|68733|5|Briefly described|p186, p187 Fig.6|Neoarchean|Neoarchean|||||Unconformably overlain by the Tanami Group.||
42069|Billabong Complex|68998|5|Briefly described|vi, p1, p31-34, Appendix Tb.11|||SW of De Bavay Hills. The only known Archaean rocks exposed in the Tanami Region. Crops out as a few small tors and pavements. Another age of 2510 +/- 4 Ma was derived from zircon rims and solitary grains. Metamorphism and/or recrystallisation of the igneous protolith occurred at 2481 +/- 7 Ma and c.1805 Ma. Previous age determinations discussed.|2532 +/- 3 Ma (zircon cores).||||Granite gneiss: banded quartz-feldspar-biotite-tourmaline granite, phenocrystic feldspar-quartz-biotite gneissic granite, thin quartz-feldspar-rich leucocratic bands and associatd mica-rich melanosomes.|
42069|Billabong Complex|69003|5|Briefly described|p2, p17|Neoarchean|Neoarchean|Granites-Tanami Orogen.|c.2514 Ma.|||Is overlain unconformably by Dead Bullock Formation.|High-grade metasedimentary rocks and leucogranites.|
42069|Billabong Complex|69031|6|Mentioned|p3|||North Australian Craton.||||||
42069|Billabong Complex|69253|6|Mentioned|p748 Fig.2|Neoarchean|Neoarchean||2514 +/- 3 Ma.|||||
42069|Billabong Complex|69419|5|Briefly described|p4:7,|Neoarchean|Neoarchean|Page et al. (1995). Tanami Region. Limited exposure, immediately S of De Bavay Hills, but extends undercover c.200 km2. SHRIMP U-Pb zircon age; there are also inherited zircons aged c.2550 and 2530 Ma.|2514 +/- 3 Ma (Page et al., 1995).||||Banded quartz-feldspar-biotite-tourmaline gneissic granite (amphibolite facies); thin quartz-feldspar-rich leucocratic bands and associated mica-rich melanosomes.|12-JUL-16
42069|Billabong Complex|69426|5|Briefly described|p11:3-5, 13|Archean|Archean|See also the reference to the informally-named Billabong complex also on p3. Underwent upper-amphibolite facies metamorphism prior to deposition of the Tanami Group.|||||Granite and gneiss.|12-JUL-16
42069|Billabong Complex|69537|5|Briefly described|iv, p1-7|Archean|Archean|Tanami Region. Outcrop is limited to a few small tors and pavements; mostly covered by unconsolidated sand. Granitic gneiss was sampled for zircons to be dated. Previous age (Page et al., 1995) of 2514 +/- 3 Ma. This study found ages of 2532 +/- 3 Ma and 2510 +/- 4 Ma; possibilites include a combination of inheritance and crystallisation, or crystallisation and metamorphism. Similarity with Pine Creek Orogen ages suggests an extensive Neoarchean basement underlying much of the North Australian Craton.|||||Granite, gneissic granite, quartz-feldspar-rich leucocratic bands and associated mica-rich melanosomes.|
42069|Billabong Complex|69618|6|Mentioned|p91 Fig.2, p100 Fig.10||||2514 +/- 3 Ma.|||||
42069|Billabong Complex|69747|5|Briefly described|p264-265|Neoarchean|Neoarchean|Geological province: Granites-Tanami Orogen. Oldest known rocks in the GTO.|2514+\-3 Ma||||Leucocratic orthogneiss and metasedimentary rocks.|
42069|Billabong Complex|70291|4|Described|p179|Neoarchean|Neoarchean|Geological province: Tanami. Oldest rocks in the Tanami region.|~2514+\-3 Ma||||Meta-arkose; high-grade metasedimentary rocks (amphibolite-grade and higher) rocks and leucogranites|
42069|Billabong Complex|71256|6|Mentioned|p21|||Tanami region. Includes a significant proportion of low delta18 O magmatic and inherited zircon.||||||
42069|Billabong Complex|71348|6|Mentioned|p217|Neoarchean|Neoarchean|Geological province: Tanami Region, North Australian Craton. Neoarchean basement complex coeval with Neoarchean magmatism at the Gawler Craton.|c. 2530-2510 Ma|||||
42069|Billabong Complex|71349|5|Briefly described|p736|Archean|Archean|Tanami Region.|2514 +/- 3 Ma (Page et al., 1995).||||Granitic plutons.|
42069|Billabong Complex|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|2514+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
42069|Billabong Complex|73089|4|Described|p3, p5, p7, p10, p22, p30-31|Neoarchean|Neoarchean|Granites-Tanami Orogen, southeastern. Poorly exposed; forms rare inlier of Neoarchean basement rock. Geochron interpreted to record magmatic crystallization. Hf and O isotopes of zircon indicate isotopically heterogeneous basement.|2513 +/- 3 Ma, 2510 +/- 4 Ma|||Overlain by Tanami Group.|Includes quartzofeldspathic gneiss, granitic orthogneiss.|
42069|Billabong Complex|73158|5|Briefly described|p2, p9|Archean|Archean|Southeast of the Granites-Tanami Orogen.|2514+/-3 Ma U-Pb zircon||||Granitic gneisses.|
42069|Billabong Complex|73159|5|Briefly described|p2, 9|Archaean|Archaean|Southeast of the Granites-Tanami Orogen.|2514 +/- 3 Ma (U-Pb; Page et al., 1995).||||Granitic gneisses.|
42069|Billabong Complex|73184|6|Mentioned|p192|||Tanami region, Includes Neoarchean crystallisation ages (Joly et al., 2013).||||||
42069|Billabong Complex|73345|6|Mentioned|p228|||||||||
29906|Birksgate Complex|23483|5|Briefly described|p4|||||||||
29906|Birksgate Complex|24197|5|Briefly described|p97, p98|||Refers to all metamorphic rocks (granulites and amphibolite-facies gneisses) south of Woodroffe Thrust (Fregon Domain) - excl.Giles Complex and Kulgera Supersuite. Includes Wataru Gneiss. Comprises >90% acid lithologies. Geol. Province: Musgrave Block.||||||07-FEB-11
29906|Birksgate Complex|24496|4|Described|p14|Mesoproterozoic|Mesoproterozoic|Includes massive orthogneiss and well layered gneisses, and migmatites. Volcanosedimentary protoliths with ages: ~1550 and ~1300 Ma. Unconformably overlain by Bentley Supergroup. Geological Province: Musgrave Block.||||||03-AUG-09
29906|Birksgate Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.||||||
29906|Birksgate Complex|24499|5|Briefly described|Map legend|||Of the Bentley Supergroup?||||||
29906|Birksgate Complex|43052|5|Briefly described|p158|||||||||
29906|Birksgate Complex|43053|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Metasediments, gneiss, granulite. Includes Wataru Gneiss. Geological Province: Musgrave Block.||||||07-NOV-08
29906|Birksgate Complex|43258|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43298|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
29906|Birksgate Complex|43561|6|Mentioned|p1439|||||||||
29906|Birksgate Complex|50607|6|Mentioned|p1.1|||Geological Province: Musgrave Block. Intruded by: Kulgera Supersuite, Winburn Suite.||||||
29906|Birksgate Complex|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes granulite, gneiss, migmatite and granite. Geological Province: Musgrave Block.||||||22-FEB-05
29906|Birksgate Complex|60662|5|Briefly described|Map Legend|||Includes layered granulites.||||||22-FEB-05
29906|Birksgate Complex|60953|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1560-1300Ma. Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, peltic-calcic paragneiss and iron formation.||||||
29906|Birksgate Complex|61108|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Granulite to amphibolite facies quartzofeldspathic gneiss, felsic to ultramafic orthogneiss, pelitic-calcic paragneiss and iron formation. Age: ~1560-1300 Ma.||||||
29906|Birksgate Complex|61524|5|Briefly described|p16|Mesoproterozoic|Mesoproterozoic|Leucocratic quartz-feldspar gneiss, felsic granulite gneiss and melanocratic quartz-hypersthene gneiss. Age: ~1600-1300 Ma. Geological Province: Musgrave Province. See also p17 Fig.1, p18 Fig. 2(a)||||||
29906|Birksgate Complex|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Sediments and volcanics.|||||Granulite to amphibolite-facies gneiss: para- and orthogneisses with interlayered mafic gneiss.|
29906|Birksgate Complex|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Paleoproterozoic|Age: 1600-1300Ma. Geological Province: Musgrave Province.||||||
29906|Birksgate Complex|64722|5|Briefly described|Fig. 2 p3-6, p16|Calymmian|Calymmian|Oldest exposed unit in Musgrave Orogen. Contains 1600-1500 Ma zircons. Geochemistry suggests subduction related environment to 1555 Ma.|||||Comprises felsic rocks, subordinate mafic units, rare metapelite, quartzite, calcsilicate rock.|11-APR-12
29906|Birksgate Complex|64745|5|Briefly described|p372, p373 Fig. 3, p374 Tab. 1|||Included within informal Musgravian Gneiss in this paper. Geol. Prov: Fregon Domain, Musgrave Province.||||||
29906|Birksgate Complex|64831|5|Briefly described|p1128 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ca 1590-1550Ma. Comprises felsic, intermediate and mafic gneisses - dominantly felsic orthogneiss with subordinate mafic gneiss, intermediate gneiss and metasedimentary rocks. See also p1131.||||||
29906|Birksgate Complex|65135|6|Mentioned|p5|||Used to describe all rocks deformed during the Musgravian Orogeny by Major and Conor (1993)||||||
29906|Birksgate Complex|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|65385|5|Briefly described|pS132|Calymmian|Calymmian|~1600-1400 Ma. Intruded by Pitjantjatjara Supersuite.||||||08-MAR-12
29906|Birksgate Complex|65833|6|Mentioned|p5.|||Musgrave area. Of Major and Conor (1993), who included all rocks formed prior to, and metamorphosed during, the 1225-1150 Ma Musgravian Orogeny.||||||
29906|Birksgate Complex|65906|5|Briefly described|p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Gneisses deposited between 1600-1540 Ma as sedimentary rocks, with volcanics and volcaniclastics. Felsic; island-arc subduction affinities.||||||
29906|Birksgate Complex|67128|6|Mentioned|p6-7|||Includes all gneisses in the eastern Musgrave Province. Some of these were thought to have granitic protoliths up to 1590 +/- 25 Ma old; these now appear to be due to detrital zircon components.||||||
29906|Birksgate Complex|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Musgrave Block.||||||
29906|Birksgate Complex|67375|5|Briefly described|p6, p17. |||Musgrave Province. Included all rocks metamorphosed during the Musgrave Orogeny, including the Mesoproterozoic granite suites and the basement they intruded.||||||
29906|Birksgate Complex|67536|5|Briefly described|Map Legend|||Musgrave Block. Informally subdivided into four parts, one of which is demagnetised or altered gneiss or granulite adjacent to major structures or Giles Complex intrusives. Non-magnetic, weakly magnetic, moderately magnetic, and variably magnetic in parts.|||Includes Wataru Gneiss.||Sheared, altered or granite-intruded gneiss or granulite adjacent to major shear zones; massive mainly meta-igneous gneiss and granulite, may include charnockite/migmatite alteration of layered granulite; layered metasedimentary gneiss and granulite.|02-APR-14
29906|Birksgate Complex|67921|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Shown only in section.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|68100|6|Mentioned|p4, 6 |||Of Major and Conor (1993). Fregon Domain. Includes gneissic basement rocks. Gneissic rocks called Wirku Metamorphics in west Musgrave Province.||||||19-JAN-17
29906|Birksgate Complex|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Metasedimentary and meta-igneous gneiss.|
29906|Birksgate Complex|69091|6|Mentioned|p60, p103 Fig.5.6|||In South Australian section of Musgrave Province, all rocks metamorphosed during Musgrave Orogeny, including Mesoproterozoic granite suites and basement through which they intruded, were initially grouped into Birksgate Complex (Major and Conor, 1993). However, recent work has shown that much of what was previously regarded as exposed basement in west Musgrave Province actually comprises supracrustal packages (now mainly paragneiss) deposited between c. 1340 Ma and 1270 Ma (Evins et al., 2012) - referred to as Wirku Metamorphics (Howard et al., 2007; Evins et al., 2009; Smithies et al., 2009).||||||
29906|Birksgate Complex|69213|5|Briefly described|p35, p36 Fig. 12, p28-29 fig.6|||Musgrave Province.|||||Gneisses. Stromatic metatexite migmatite defined by layer parallel, mostly in source leucosomes. Leucosomes of two types; medium grained, straight margined and coarse grained less sharp margined leucosomes.|
29906|Birksgate Complex|69436|6|Mentioned|p21:2-3||||1600-1540 Ma.|||||12-JUL-16
29906|Birksgate Complex|69640|4|Described|p11-p14, p16-p17, p24, p31-p32|Proterozoic|Proterozoic|Musgrave Province. Subsequently deformed and metamorphosed to amphibolite to granulite facies during the ca 1220-1120 Musgrave Orogeny. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. An additional magmatic crystallisation age of 1617 +/- 8 Ma was obtained. A maximum depositional age of 1588 +/- 7 Ma was also obtained for a quartzo-feldspathic gneiss. Metamorphic ages inculding 1158 +/- 8 Ma are provided. See also p50, p57, p65, p73-p74, p79, p137, p141, p145, p157.|1605 +/- 6 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Pitjantjatjara Supersuite.|Felsic ortho- and paragneisses including biotite quartzo-feldspathic paragneiss, hornblende-biotite-diopside quartzo-feldspathic gneiss, migmatitic gneiss.|
29906|Birksgate Complex|69729|5|Briefly described|p67, p88|||Major and Conor (1993), for west Musgrave Province basement defined as rock metamorphosed during the Musgrave Orogeny. These were reassigned (Howard et al., 2009) to Wirku Metamorphics on the basis of geochronology (discussed).||||||
29906|Birksgate Complex|70083|5|Briefly described|p206-208, 229|||The name used for the Musgravian Gneiss in the Fregon Subdomain, Eastern Musgrave Inlier, Musgrave-Albany-Fraser Orogen. Is termed the Olia Gneiss in the Mulga Park Subdomain.|||Kalamurta Gneissic Unit.|Is dissected (intruded) by Alcurra Dolerite dykes.|Peraluminous metapelite gneiss, intercalated with more quartzofeldspathic, and granitic gneisses.|12-MAY-23
29906|Birksgate Complex|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement to the Musgrave Province. The five facies are mapped separately.|||||Gneiss, granulite and amphibolite facies S of the Woodroffe Thrust. Pale brown, quartzo-feldspathic granofels; layered, quartzo-feldspathic orthogneiss to leucogneiss; layered to migmatitic, quartzo-feldspathic paragneiss; meta-calcsilicate rock.|
29906|Birksgate Complex|70634|6|Mentioned|189540.1.pdf|||Now named Wirku Metamorphics.||||||
29906|Birksgate Complex|71170|5|Briefly described|p9, p23|||Musgrave Province. Name derived from Major and Conor, 1993.||||||
29906|Birksgate Complex|71321|4|Described|p1-2,4-5,8,14,17-18,21,24|Calymmian|Statherian|Geological province: Musgrave Province. Comprises part of basement, and oldest rocks exposed on the Musgrave Province. Occurs in outcrop as blocks or rafts (several cm to hundreds of meters across) within Pintjantjatjara Supersuite. See p14-17 for detailed descriptions of outcrop. Deformed (early gneissic layering and folding) and metamorphosed to amphibolite to granulite facies during c. 1220-1120 Ma Musgravian Orogeny. Intruded by granitoid bodies of Pintjantjatjara Supersuite. Geochemically similar to c. 1345-1293 Ma Wankanki Supersuite granites in the West Musgrave Province (strong compositional similarities to Phanerozoic granites of the Andean continental arc (Smithies, et al., 2010). Dominantly metaluminous, to slightly peraluminous and predominantly magnesian character; strong affinity to I-type granites. Likely formed in a volcanic arc setting. Has c. 1620-1550 Ma zircons indicating igneous protolith age (Camacho and Fanning, 1995; Edgoose, et al., 1993; Edgoose, et al., 2004; Scrimgeour, et al., 1999); protolith magmatic ages as early as c. 1665 Ma from adjacent AGNES CREEK mapsheet. Emplacement ages in the HANGING KNOLL map include c. 1480 Ma and c. 1440 Ma. Nd and Hf isotopic analysis indicate a relatively juvenile source for both para- and orthogneisses. Considered prospective for Zn-Pb-Ag ore bodies similar to Broken Hill. See also p32-41,55-56,60-63,66-67,74.|c. 1630-1560 Ma||||Felsic and mafic orthogneisses and felsic volcanics, volcaniclastics and paragneisses.|
29906|Birksgate Complex|71322|5|Briefly described|p11-19, p26, p28|||Musgrave Province. Hosts Cu mineralisation at the Kenmore II prospect. Summary log for drillhole DD10WOD007. Leococratic migmatite dated. Metamorphosed at 1180 +/- 5 Ma and 1159 +/- 7 Ma.|1520 +/- 9 Ma (maximum depositional age).||||Intermediate to felsic migmatitic gneisses, paragneisses, orthogneisses and intrusive magmatic rocks, calcsilicate, schist.|13-DEC-21
29906|Birksgate Complex|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|The six facies are mapped separately. Most have protolith ages given. Metamorphosed between c.1170 Ma and 1138 Ma. Solid geology interpretation: demagnetised or altered adjacent to major structures or Giles Complex intrusives; non-magnetic, weakly or variably magnetic.|c.1716 Ma - 1565 Ma.|||Correlative of Kalamurta gneiss.|Quartzo-feldspathic paragneiss, commonly migmatitic; mixed felsic +/- mafic gneiss; amphibolite to granulite facies felsic gneiss, commonly migmatitic; leucocratic diatexite; mafic gneiss, locally migmatitic; undivided gneiss, locally migmatitic.|
29906|Birksgate Complex|71536|6|Mentioned|p73, p78|||Was likely the protolith of the 1143 +/- 9 Ma felsic gneiss in the Pitjantjatjara Supersuite.||||||
29906|Birksgate Complex|71592|5|Briefly described|Appendix A.|||Musgrave Province. Over 20 age determinations are given for crystallisation (within this range), provenance clusters and metamorphism.|1617+/-8 Ma to 1564+/-5 Ma.||||Gneiss, syenogranitic gneiss, granite, monzogranite, pelitic to semipelitic migmatite.|
29906|Birksgate Complex|72238|5|Briefly described|p38|Calymmian|Statherian|Geological province: Musgrave Province. Intruded by Amata Dolerite.|c. 1.7-1.5 Ga|||||
29906|Birksgate Complex|72242|6|Mentioned|p27|Calymmian|Statherian|Geological province: Musgrave Province. Associated with Kararan Orogeny. Coeval with Hiltaba Suite and Toolgana Supersuite, and extensive oceanic crust formation.||||||
29906|Birksgate Complex|72344|6|Mentioned|p28|Calymmian|Statherian|Musgrave Province.|c. 1565-1665 Ma (Jagodzinski et al, 2013)|||Time equivalent to the Toolgana Supersuite.||
29906|Birksgate Complex|72476|5|Briefly described|p24, 27|||Dominant basement unit in eastern Musgrave Province.|~1650-1550 Ma.||||Granulite to upper amphibolite facies, volcanic-dominated supracrustal rocks and felsic intrusives (granites through to tonalites, minor intercalated mafics), with minor sedimentary rocks.|
29906|Birksgate Complex|73100|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73109|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Drexel et al. (1993). Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73111|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Subsurface.|||||Metasediments, gneiss, granulite.|
29906|Birksgate Complex|73232|6|Mentioned|p5|||Musgrave Province. This unit dominates the province.||||Intruded by Pitjantjatjara Supersuite and Giles Complex including Alcurra Dolerite.|Deformed and metamorphosed gneissic rocks.|
29906|Birksgate Complex|73234|6|Mentioned|p19|Calymmian|Statherian|Musgrave Province, eastern.|c. 1700-1550 Ma||||Meta-igneous and metasedimentary rocks.|
76182|Birraduk Amphibolite|67779|2|Defined|p8 Table 1, pp23-24, p60, p69, pp118-119|Paleoproterozoic|Paleoproterozoic|New name, after Birraduk Creek. Formerly part of Zamu Complex and Zamu Dolerite (Ferguson and Needham, 1978). Nimbuwah Domain, Pine Creek Orogen. Exposed c.22 km SE of Oenpelli township and c.13 km SW of Nabarlek Uranium Prospect; also in drillcores. Reference area in creek in northwest Myra Falls Inlier. Has strongly defined E-W foliation. Geochemistry is discussed in some detail.||||Occurs within Cahill Formation and Nourlangie Schist.|Fine- to medium-grained, green hornblende-biotite-plagioclase amphibolite with strong schistosity; garnet-bearing; common accessory opaque oxides; biotite wraps elongate feldspar.|14-SEP-12
76182|Birraduk Amphibolite|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||||||Amphibolite: intrusive, metagabbro, fine- to medium-grained, garnet- and biotite-bearing.|
38833|Birthday Suite|63261|5|Briefly described|p9 Fig. 5, p15-16|Paleoproterozoic|Paleoproterozoic|This is the Winnecke Suite of Dean (2001). Includes the formally named Winnecke Granophyre and volcanic rocks of Mount Winnecke Formation. Intruded into the Tanami region between 1825 and 1810Ma. Geological province: Tanami Region.||||||07-FEB-11
38833|Birthday Suite|64662|5|Briefly described|p30 Fig. 3|Orosirian|Orosirian|Age: 1825-1810Ma. Geological Province: Tanami region.||||||07-FEB-11
38833|Birthday Suite|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1820 Ma.|||||
38833|Birthday Suite|64733|5|Briefly described|p170 Fig.2, p174 Fig.4, p175|Orosirian|Orosirian|Locally restricted and highly magnetic.|1825-1810 Ma.|||||20-APR-12
38833|Birthday Suite|64734|5|Briefly described|p186 Fig.1|Orosirian||ca. 1820 Ma||||||30-OCT-18
38833|Birthday Suite|65358|5|Briefly described|p6-7, p9|Statherian|Orosirian|In Tanami Region. Includes auriferous Winnecke Granophyre. Dominated by metaluminous I-type biotite granodiorite and monzogranite. Intruded between 1825-1790 Ma.||||||
38833|Birthday Suite|66129|6|Mentioned|p213, p214 Fig.1|||||||||
38833|Birthday Suite|67824|6|Mentioned|p385 Fig.2|Orosirian|Orosirian||~1820 Ma|||||
38833|Birthday Suite|67826|6|Mentioned|p401 Fig.2|Orosirian|Orosirian||c.1820 Ma|||||
38833|Birthday Suite|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|Ca. 1820 Ma|||||
38833|Birthday Suite|69003|6|Mentioned|p17 Fig.21|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1825-1810 Ma.|||||
38833|Birthday Suite|69253|6|Mentioned|p747 Fig.1|Orosirian|Orosirian|Petrophysical properties described.|c.1820 Ma.|||||
38833|Birthday Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Tanami Region.||||Intrudes Ware Group.||12-JUL-16
38833|Birthday Suite|69426|5|Briefly described|p11:4 Fig.11.3, 11:10-12|Orosirian|Orosirian|Also includes coeval felsic volcanic rocks of the Ware Group. Has a high magnetic response. Geochemistry briefly described.|1825-1815 Ma.||Winnecke Granophyre.|||12-JUL-16
38833|Birthday Suite|69618|6|Mentioned|p90|Paleoproterozoic|Paleoproterozoic||c.1820 Ma.|||||
38833|Birthday Suite|69673|6|Mentioned|p3|||||||||
38833|Birthday Suite|69747|5|Briefly described|p263-p264|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Associated with late syn- to postcollisional tectonic settings within a ~30 Ma million year long period of magmatic activity broadly spanning ca. 1825-1791 Ma (Smith, 2001).|ca. 1820 Ma||||Granitic rocks.|25-JUN-19
38833|Birthday Suite|70291|4|Described|p178,180-181|Orosirian|Orosirian|Geological province: Tanami. Restricted to northeastern part of Tanami region.|ca. 1820 Ma||Includes Felsic volcanic rocks of Ware Group and Winnecke Granophyre.||Felsic volcanic rocks of the Ware Group and the Winnecke Granophyre; also includes monzogranite and granodiorite; highly magnetic|
38833|Birthday Suite|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Winnecke Granophyre.|||
38833|Birthday Suite|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1790 Ma.|||Intrudes Tanami and Ware Groups.||
38833|Birthday Suite|73089|4|Described|p3, p8, p39, p42|Orosirian|Orosirian|Granites-Tanami Orogen, northeastern. Broadly coeval with other granites of the orogen but distinguished by differences in magnetic character (Ahmad et al., 2013). Bimodal character suggests an extensional setting.|c. 1825-1815 Ma||Winnecke Granophyre, Water Tower Tonalite[?]|Intrudes Mount Winnecke Formation (Ware Group).|Felsic and lesser mafic magmatic rocks; alkali-calcic, highly potassic and silica-rich; forms areas of strong magnetization on aeromagnetic images.|
38833|Birthday Suite|73158|5|Briefly described|p2|Orosirian|Orosirian|Granites-Tanami Orogen.|ca. 1825-1815 Ma||||Granitic intrusions.|
38833|Birthday Suite|73159|5|Briefly described|p2|||Granites-Tanami Orogen.|c.1825-1815 Ma.||||Granites.|
79261|Bitter Springs Group|70762|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Amadeus Basin, Centralian Superbasin.||||Overlies Heavitree Quartzite.|Dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|71001|5|Briefly described|p16-18, 20, 22, 25-26, 28|Tonian|Tonian|Amadeus Basin. Formerly Bitter Springs Formation, the Members of which are now Formations of the Bitter Springs Group. Shallow-marine, lagoonal and supratidal environments. Age determinations vary.|~830-750 Ma.||Gillen, Johnnys Creek, Loves Creek Formations.|Overlies Heavitree Quartzite. Is overlain by Areyonga Formation.|Thick halite and sulfate evaporite accumulations.|
79261|Bitter Springs Group|71080|5|Briefly described|p4, p9, 23, 26, 27, p29 Fig 20, p30, 31|Tonian|Tonian|Amadeus Basin. Supersequence 1.|||Includes Gillen Formation, Loves Creek Formation, Johnnys Creek Formation.|Overlies Heavitree Formation.||
79261|Bitter Springs Group|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. [Also referred to as Bitter Springs Formation]. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv.|900-720 Ma (inferred)||Includes Johnnys Creek Formation.|Underlain by Dean Quartzite. Equivalent to Pinyanna beds.|Phyllitic schist, locally sericitic phyllonite; derived from siltstone and mudstone; dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|71279|5|Briefly described|p355 Fig.2, p364, p366-367|||A structurally-complex, salt-rich sedimentary package.|||Gillen, Loves Creek, Johnnys Creek, Formations.||Salty shale, chert, dolostone and limestone.|
79261|Bitter Springs Group|71344|5|Briefly described|p1092, 1093 Fig 1|Neoproterozoic|Neoproterozoic|Amadeus Basin.|575- 565 Ma|||||
79261|Bitter Springs Group|71810|5|Briefly described|Map legend.|Tonian|Tonian|Amadeus Basin (Phase 1), Centralian Superbasin.|<896 Ma.|||Overlies Heavitree Formation. Is overlain by Carnegie Formation.|Dolomite, stromatolitic dolomite, siltstone, and sandstone; evaporites in subsurface.|
79261|Bitter Springs Group|71841|5|Briefly described|iii,p1-2|Cryogenian|Cryogenian|Of Amadeus Basin. Previously termed Bitter Springs Formation. Status upgraded to Group and formalised by Normington et al (2015), Normington and Donnellan (in review). |||Includes Johnnys Creek, Loves Creek and Gillen formations.|Overlain by Inindia beds or Areyonga Formation. Grades into Pinyanna beds.||
79261|Bitter Springs Group|71842|5|Briefly described|iii,p2-5,9|Cryogenian|Cryogenian|Of Amadeus Basin. Part of revised nomenclature after this study in the Mount Conner area.|||Includes Johnnys Creek Formation, Loves Creek Formation and Gillen Formation.|Underlain by Dean Quartzite or Heavitree Quartzite.||
79261|Bitter Springs Group|71898|5|Briefly described|p9|||Amadeus Basin.|||Includes the Loves Creek Formation.|Unconformably overlain by the Tempe Formation.||
79261|Bitter Springs Group|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Neoproterozoic|Amadeus Basin (Phase 1).  Age from biostratigraphy.|||||Dolomite, stromatolitic dolomite, siltstone, sandstone; evaporitic in subsurface.|
79261|Bitter Springs Group|72094|6|Mentioned|p3 Fig 2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||14-APR-22
79261|Bitter Springs Group|72259|6|Mentioned|p10|||Spilitic volcanic rocks occur at the top of the unit. These post-date the negative d13C anomaly dated at ca. 810-790 Ma.|||||Includes spilitic volcanic rocks.|
79261|Bitter Springs Group|72369|5|Briefly described|p15,43|||Of Amadeus Basin.|||Includes Gillen, Loves Creek and Johnnys Creek formations.|Overlain by Winnall Group.|Dolostone, limestone, siltstone, sandstone, halite, evaporites, and a basaltic unit (green-grey to red, fine-grained, and typically shows chlorite-carbonate alteration).|
79261|Bitter Springs Group|72374|5|Briefly described|p6|||Of Amadeus Basin.||||Overlain by Areyonga Formation.||
79261|Bitter Springs Group|72375|4|Described|p2,7,9-11,13,15,17,23|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Normington et al., 2015 (after Wells et al., 1967). Structurally interleaved with Aileron Province basement rocks; isoclinally infolded with Atneequa Suite and Moonlight Gneiss on LIMBLA and ILLOGWA CREEK mapsheets. Depositional age constrained at c. 820 Ma, based on geochemical affinities with c. 824 Ma Amata Dolerite (Glikson et al., 1996).|||Includes Gillen Formation, Loves Creek Formation, Johnnys Creek Formation.|Overlain disconformably by Wallara Formation.|Predominantly of dolostone, limestone, siltstone, sandstone, halite, evaporite and a rare basaltic unit near the top of the sequence.|
79261|Bitter Springs Group|72489|4|Described|p3, p4 Fig.3, p5-7, p7 Fig.6|Tonian|Tonian|Amadeus Basin, including the Limbla Syncline. Thickness c. 1000m.  See also p8 Fig.7, p9-12. Contains REE record that is evidence of either a non-marine environment or an extremely different ocean chemistry. Age of 13C excursion constrained to 811-785 Ma (through international correlations).|||Includes Gillen Formation,  Loves Creek Formation, Johnnys Creek Formation.|Underlies Areyonga Formation. Overlies the Heavitree Formation.|Includes carbonate and siliciclastic succession.|14-SEP-20
79261|Bitter Springs Group|72516|5|Briefly described|p85-86|Tonian|Tonian|Amadeus Basin. Formerly the Bitter Springs Formation.  Correlated with the Yackah beds. Both units contain a columnar, branching stromatolite Acaciella australica. Min age ~820 Ma from intruding dykes.|Ca 820 Ma min age?|||Overlies the Heavitree Formation.||14-APR-22
79261|Bitter Springs Group|72601|5|Briefly described|p3, p7, p10-12, p14, p17, p25|Tonian|Tonian|Amadeus Basin. Previously called the Bitter Springs Formation. Contains diverse Tonian biotic assemblages [palynomorphs].|||Johnnys Creek Formation, Loves Creek Foramtion, Gillen Formation|Underlain by Heavitree Formation and Dean Quartzite. Unconformably overlain by Wallara Formation.|Carbonate rocks with fine siliciclastic interbeds.|
79261|Bitter Springs Group|72714|6|Mentioned|p2, p4|||Amadeus Basin. Regionally, copper-bearing fluorite veins are found on the contact between the Atneequa Suite and overlying Heavitree Formation and Bitter Springs Group. Listed as Bitter Springs Formation p2.||||||
79261|Bitter Springs Group|73085|5|Briefly described|piii, p1-2, p4, p15-16, p27|Tonian|Tonian|Amadeus Basin. Previously called Heavitree Quartzite.|||Johnnys Creek Formation, Loves Creek Formation, Gillen Formation|Underlain by Dean Quartzite and Heavitree Formation. Unconformably[?] overlain by Wallara Formation.||
79261|Bitter Springs Group|73086|1|Redefined|[See comments].|Tonian|Tonian|[Redefined herein. See also definition card, ASUD]. Re-definition of unit/upgrade from formation to group. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. The base is taken to be the first thick (~1 m) shale interval above the Heavitree Formation. Top of the unit coincides with a sequence boundary with up to 200 m relief and is impacted by salt tectonism which caused thickening [etc]. Metamorphosed up to lower amphibolite facies in the Arltunga and Ormiston nappe complexes. Complex folding and faulting are widespread problems with assigning a recognisably complete type or reference section. ~790 m thick at the Ellery Creek type area but the true thickness is difficult to ascertain due to complex structure resulting from orogenesis and halotectonics. Max thickness: 1651.5 m (Murphy-1 drillhole). Stromatolites are present in all constituent formations. Poorly constrained minimum age of ca 820 Ma. Maximum age is less well constrained; globally synchronous carbon isotopic signatures indicate an age range of 815-787 Ma for the unit. Deposited on a shallow, stable shelf with a minor amount of fine-grained siliciclastic input. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. May correlate to Pinyinna beds, Yackah beds, Lewis Range Sandstone, Young Husband Conglomerate, Coominaree Dolomite and Browne Formation. p: iii, 3, 5-11, 14-18, 29-30, 35, 38-40, 49, 53, 57, ~62-68, 70, 72, 100-105, 113,  130, ~143-154, 157, 160, 167, 171, App 2.|Between ca. 1000 Ma and ca. 820 Ma.||Gillen Formation, Loves Creek Formation, Johnneys Creek Formation|Conformable/transitional [in places] contact with the underlying Heavietree Formation. Overlain by Wallara Formation, Areyonga Beds[Formation?], Olympic Formation. [See comments].|Dolostone, limestone and cherty limestone, with subordinate sandstone, red and green siltstone and black shale. Where metamorphosed, the rocks are slate, phyllite, schist, and calc-silicates.|
79261|Bitter Springs Group|73088|6|Mentioned|piii, p1-2, p4, p12|Tonian|Tonian|Amadeus Basin. Present in drillhole BL002. Previously called Bitter Springs Formation.|||Johnnys Creek Formation, Loves Creek Formation, Gillen Formation|Underlain by Heavitree Formation. Overlain by Wallara Formation.|Includes dolostone and dolomitic siltstone.|
79261|Bitter Springs Group|73180|6|Mentioned|p48 Fig.1, p49-51, p53|Neoproterozoic|Neoproterozoic|Amadeus Basin. Disconformable contact with the overlying Areyonga Formation in the east side of the basin where a step-like scour demarcates the western limit of the Sturt ice-sheet, or where it changed from grounded to floating. A narrow, deep valley-like feature observed in seismic images cuts through the upper Bitter Springs Group before terminating in salt within the Gillen Formation, resembles sub-glacial tunnel valleys. Local scouring of the Base Areyonga Disconformity into the Bitter Springs Group suggests locations where the generally floating Sturt ice-sheet grounded. Unconformably underlies the Olympic Formation and Pioneer Formation.|||Gillen Formation, Loves Creek Formation, Johnnys Creek Formation|Conformably overlies the Heavitree Quartzite, Dean Quartzite. Disconformably underlies the Wallara Formation and Areyonga Formation.||
79261|Bitter Springs Group|73338|6|Mentioned|p5, p8|||Unconformably overlies basement in the Mount Kitty 1 well.|||Gillen Formation|||
79261|Bitter Springs Group|73346|6|Mentioned|p5, p28|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
79261|Bitter Springs Group|73437|6|Mentioned|p151|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
79261|Bitter Springs Group|73445|5|Briefly described|p10, 56, 58|Neoproterozoic|Neoproterozoic|Amadeus Basin. Hosts SEDEX-style base metal mineralisation (Enceladus and Iapetus prospects).||||||
81822|Black Label Suite|73123|6|Mentioned|piii, p5, p7-8, p10|Orosirian|Orosirian|Bimodal suite.|ca 1.81 Ga||Bacardi Granite, Captain Morgan Metadolerite, Dneiper Granite.|Intrudes Deep Bore Metamorphics. Intruded by Molyhil Suite and Marshall Granite.||
81822|Black Label Suite|73591|6|Mentioned|p27-28|Statherian|Orosirian||1810-1800 Ma||Dneiper Granite|||
27109|Blackfellow Creek Sandstone|28255|3|Fully described|p72, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Of Duerdin Gp. Blocky/massive, medium-grained quartz sst; some interstitial clay or limonite. Conformable below Moonlight Valley Tillite; overlies Fargoo Tillite (type area); directly over Skinner Sst on AUVERGNE due to erosional break. Max.thick: >45m.||||||18-MAY-15
27109|Blackfellow Creek Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duredin Group.  Quartz sandstone.||||||02-DEC-04
27109|Blackfellow Creek Sandstone|32701|4|Described|Table 1|||Adelaidean.  See also p14. Duerdin Gp.||||||18-MAY-15
27109|Blackfellow Creek Sandstone|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Medium quartz sandstone; massive and blocky, thick-bedded. Disconformable on Fargoo Tillite and Skinner Sandstone.||||||28-APR-05
27109|Blackfellow Creek Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27109|Blackfellow Creek Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Medium quartz sandstone.||||||27-APR-05
27109|Blackfellow Creek Sandstone|37927|5|Briefly described|p507|||||||||
27109|Blackfellow Creek Sandstone|45112|5|Briefly described|Table 18|||||||||
27109|Blackfellow Creek Sandstone|48938|2|Defined|p67|Adelaidean|Adelaidean|||||||
27109|Blackfellow Creek Sandstone|48943|3|Fully described|p81|||||||||
27109|Blackfellow Creek Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Overlies Fargoo Tillite. Quartz sandstone.||||||22-JUL-04
27109|Blackfellow Creek Sandstone|60682|4|Described|p17 Table 4, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Fargoo Tillite. Max. thickness: >30m. Medium grained sandstone. Fluvial sourced from glacials. Geological Province: Wolfe Creek Basin.||||||
27109|Blackfellow Creek Sandstone|64104|6|Mentioned|p63 Fig.1|||Local unit in Keep River area.||||Is overlain by Moonlight Valley Formation.||
27109|Blackfellow Creek Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Quartz sandstone ||||||
27109|Blackfellow Creek Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Unconformably overlies Fargoo Tillite. Is unconformably overlain by Moonlight Valley Tillite.|Medium quartz sandstone.|
27109|Blackfellow Creek Sandstone|68733|6|Mentioned|p177 Fig.2, p183|Cryogenian|Cryogenian|Victoria Basin.||Of the Duerdin Group.||||
27109|Blackfellow Creek Sandstone|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Fargoo Tillite. Is overlain by Moonlight Valley Tillite.||12-JUL-16
27109|Blackfellow Creek Sandstone|69442|5|Briefly described|p27:1-2, 3 Tb.27.1|||Wolfe Basin. Over 30m thick. Fluvial deposits sourced from glacial sediments. Low-angle basal unconformity.||Duerdin Group.||Unconformably overlies Fargoo Tillite or Skinner Sandstone.|Massive to thinly-bedded, medium-grained quartzic sandstone; abundant sole-marks and ripples.|12-JUL-16
27109|Blackfellow Creek Sandstone|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|Maximum thickness of 32m.||Duerdin Group|||Quartzose sandstone.|
27109|Blackfellow Creek Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Quartz sandstone.|
27109|Blackfellow Creek Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Duerdin Group.||Shown as unconformably overlying Fargoo Tillite and unconformably overlain by Moonlight Valley Tillite.|Medium quartz sandstone.|24-JAN-22
27109|Blackfellow Creek Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
36761|Blackjack kimberlite|23772|5|Briefly described|p764|||North Australian Craton.||||||
36761|Blackjack kimberlite|69430|5|Briefly described|p15:56, 59|||Informal name. A kimberlite dyke discovered by Stockdale Prospecting (Fried, 1990) intruding McArthur Basin rocks.||||Intrudes the Bukalorkmi Sandstone.|Highly weathered and ferruginised kimberlite dyke.|12-JUL-16
79086|Bleechmore Metamorphics|68997|4|Described|vi-vii,p1,28-37|Orosirian|Orosirian|Metamorphosed to granulite facies with local evidence for production of large volumes of anatectic melt. Sample: AC08EEB411 (Grid Reference: MGA94 Zone 53: 426364mE 7470352mN). Zircon age spectra of 1822+\-11 Ma, interpreted as maximum depositional age. Single monazite inclusion hosted by a garnet porphyroblast yielded an age of 1804+\-40 Ma, interpreted to be of detrital origin. Monazite analysed in situ within pelitic migmatite yield an upper intercept age of 1741+\-19 Ma, with zircon rims dated at 1713+\-11 Ma. Metamorphic zircon rim ages at 1584+\-12 Ma probably grew during the early part of Strangways Event have undergone discernible ancient loss of radiogenic Pb, probably during the 1590-1560 Ma Chewings Orogeny. In-situ monazite also yield discordia regression with upper intercept age of 1569+\-25 Ma, interpreted to represent isotopic resetting during Chewnings Orogeny. The same in-situ monazite samples have identical lower-intercept ages (464+\-38 Ma and 474+\-110 Ma, respectively) that are consistent with a single episode of dissolution and reprecipitation affecting both monazite populations during the Larapinta Event.|1822+\-11 Ma (max dep age: U-Pb zircon)||||Metapelitic to metapsammopelitic biotite- and garnet-bearing migmatite is dominant, with sillimanite and cordierite in more aluminous layers. More quartz-rich metapsammite layers are common.|
79086|Bleechmore Metamorphics|69510|6|Mentioned|p12, p17|||The 1735-1690 Ma Strangways Event is recognised in monazite and zircon rims in rocks of this unit, as is the 480-460 Ma Larapinta Event.||||||
79086|Bleechmore Metamorphics|69794|6|Mentioned|iv,p14|||Preserves rare evidence in orthogneissses for metamorphic zircon growth and resetting during Larapinta Event (Bodorkos et al. 2013).||||||06-APR-20
79086|Bleechmore Metamorphics|69917|4|Described|p59-63, 66-68, 96, 98, 141||Paleoproterozoic|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. 1822+/-11 Ma is maximum depositional age for the precursor sedimentary rock. Subsequently affected by Strangways Event and Chewings Orogeny.||||Inferred to be intruded by Langford Granite. Intruded by unnamed gneissic granite ? During Strangways Event?|Mafic granulite; migmatitic metapelite.|
79086|Bleechmore Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Age of metamorphism.|1726+/-6 Ma (U-Pb zircon LA-ICPMS).||||Granulite.|
79086|Bleechmore Metamorphics|71858|6|Mentioned|p69|||Aileron Province.||||||
36765|Bloods Range Formation|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||
36765|Bloods Range Formation|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||28-MAY-04
36765|Bloods Range Formation|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Red shales, polymictic conglomerate, volcaniclastics, tuffaceous horizons and local lensoidal quartz sandstone beds.  Geological Province: Musgrave Block.||||||
36765|Bloods Range Formation|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Schist, schistose quartz conglomerate. Of Tjauwata Group. Geological Province: Musgrave Block.||||||14-JAN-05
36765|Bloods Range Formation|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Clastic red-beds of polymictic conglomerate, fine sst and siltstone, grading upwards to immature sst; tuffaceous layers and local lensoidal quarts sst beds. Transitional over Puntitjata Rhyolite. Geol. Prov: Musgrave Block.||||||18-JUL-05
36765|Bloods Range Formation|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Red shales, polymictic conglomerate, volcaniclastics, tuffaceous horizons and local lensoidal quartz sandstone.||||||19-OCT-05
36765|Bloods Range Formation|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Disconformably overlain by Kulail Sandstone in base of Amadeus Basin. Succession of redbed sediments, volcaniclastic rocks and interlayered fine sandstone, siltstone and clast-supported pebble conglomerate; alluvial/fluvial setting.||||||25-JAN-10
36765|Bloods Range Formation|64580|4|Described|map legend||Mesoproterozoic|Of Tjauwata Group. Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.||||||15-DEC-08
36765|Bloods Range Formation|65233|5|Briefly described|p2|||Overlies Mount Harris Basalt. Geological province: Amadeus Basin. Comprises red beds, volcaniclastic rocks and fine-grained to conglomeratic clastic rocks.||||||07-FEB-11
36765|Bloods Range Formation|65256|1|Redefined|p39-40, p6 Tb.1, p8, 10, 12, 14-15, 37|Neoproterozoic|Stenian|Variation of published name: formerly Bloods Range Beds and Bloods Range beds. Thickness approx 100m (laterally variable). No longer correlated with Dixon Range beds. Appears to be derived from Puntitjata Rhyolite and Mount Harris Basalt.||Uppermost unit of the Tjauwata Group|Includes Wankari volcanics.|Overlies Mount Harris Basalt and Puntitjata Rhyolite; unconformably underlies Kulail Sandstone/Dean Quartzite; intruded by Walu Granite.|Polymictic pebble conglomerate, quartzite-cobble conglomerate, immature sandstone, red and dark purple fine sandstone and siltstone, epiclastic and volcaniclastic rocks, rare tuff.|24-MAR-15
36765|Bloods Range Formation|69091|6|Mentioned|p103 Fig.5.6|||||||||
36765|Bloods Range Formation|69153|5|Briefly described|500k_geologyp08_lut.csv||Mesoproterozoic|||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36765|Bloods Range Formation|69436|5|Briefly described|p21:4, 13-14, 19|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Clastic red bed succession. Deformed in the Wankari Detachment Zone of the Petermann Nappe Complex, with growth of kyanite, phlogopite and muscovite.||Tjauwata Group.||Transitionally overlies Puntitjata Rhyolite and Wankari Volcanics.|Conglomerate, fine sandstone and siltstone, grading upwards into immature sandstone. North of Wankari Detachment Zone, comprises gritty and pebbly quartz-muscovite schist, muscovite quartzite, and kyanite-muscovite-phlogopite-quartz schist.|12-JUL-16
36765|Bloods Range Formation|69438|5|Briefly described|p23:9|Mesoproterozoic|Mesoproterozoic|Alluvial-fluvial deposits.||Tjauwata Group.||Is overlain disconformably by Kulail Sandstone.||12-JUL-16
36765|Bloods Range Formation|70018|4|Described|p233,235-236|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Interbedded siliciclastic sedimentary rocks.||Unit of Tjauwata Group.||Uppermost unit of Tjauwata Group. Underlain by Wankari Volcanics.|Red shale, polymictic conglomerate, volcaniclastics, tuffaceous layers and local lensoidal quart sandstone beds.|
36765|Bloods Range Formation|70634|4|Described|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic|||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.|
36765|Bloods Range Formation|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 basalt, basaltic tuff, conglomerate, and quartzite|
36765|Bloods Range Formation|70839|5|Briefly described|p345|||Mineralogically immature, including arkose and conglomerates; similar clasts assemblage to Mount Currie Conglomerate and Mutitjulu Arkose.||Unit of Tjauwata Group.||||
36765|Bloods Range Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone, schist, shale|
36765|Bloods Range Formation|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma). See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1030-1030 Ma (inferred)|Unit of Tjauwata Group.|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36765|Bloods Range Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Tjauwata Group|||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock.|
75904|Bluebush Metamorphics|68997|4|Described|vii-viii,p1,62-66|Orosirian|Orosirian|Upper amphibolite- to granulite-facies migmatites of predominantly pelitic composition within the Limbla mapsheet (Whelan and Webb in prep). Shows local evidence for production of large volumes of anatectic melt. Maximum sedimentary precursor age of 1827+\-10 Ma (Kositcin et al. 2013). Monazite separated from pelitic diatexite (Sample: IC10GPW300. Grid Reference (MGA94 Zone 53): 544973mE 7374008mN) yielded a single age of 1743+\-7 Ma for high-grade metamorphism (central ILLOGWA CREEK).|1827+\-10 Ma (max dep age: U-Pb zircon)||||Pelitic diatexite.|
75904|Bluebush Metamorphics|69510|5|Briefly described|p8, p11-12|||Metamorphism (upper-amphibolite- to granulite-facies) of sedimentary protolith dated at 1743 +/- 7 Ma (Bodorkos et al., 2013).||||Is overlain unconformably by Heavitree Quartzite.|Granulite-facies metasedimentary rocks; includes pelitic diatexite.|
75904|Bluebush Metamorphics|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1743+/-7 Ma (metamorphism: SHRIMP U-Pb zircon).||||Pelitic migmatite, diatexite.|
75904|Bluebush Metamorphics|72375|5|Briefly described|p9|Paleopreterozoic|Paleopreterozoic|Kositcin et al., 2013b provided a maximum timing of deposition at c. 1827 Ma, and subsequent metamorphism at c. 1757 Ma.|||||Granulite facies metamorphic rocks.|04-DEC-19
24190|Boko Formation|42504|5|Briefly described|Table 4 P73|||Reserved Haines and Bagas Dec 1987.||||||26-JUL-06
24190|Boko Formation|42643|2|Defined|p51|Neoproterozoic||||||||
24190|Boko Formation|42644|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite, massive, red-brown mudstone matrix. Geological Province: Georgina Basin.||||||15-NOV-05
24190|Boko Formation|60122|6|Mentioned|p9|||||||||
24190|Boko Formation|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Glacial diamictite with red-brown mudstone matrix and pebble to boulder sized clasts of quartzite, granite and metamorphics; striated and faceted clasts. Geological Province: Georgina Basin.||||||
24190|Boko Formation|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group. Diamictite: massive, mudstone matrix.  Geological Province: southern Georgina Basin.||||||11-OCT-05
24190|Boko Formation|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Keepera Group. Geological Province: Georgina/Ngalia Basin. Tillite, dolomite/limestone, laminated siltstone.||||||
24190|Boko Formation|62984|5|Briefly described|p13|Cryogenian|Cryogenian|Unconformably overllies Amesbury Quartzite; locally overlain by Oorabra Arkose.  Geological Province: Georgina Basin. Glacial diamictite. Representative of the Marinoan galcial episode.||||||23-JAN-07
24190|Boko Formation|64068|3|Fully described|p47-48, p45, 46, p162, p19, p viii|Cryogenian||||Of Keepera Group.||Unconformably overlies Amesbury Quartzite. Is overlain disconformably by Central Mount Stuart Formation.|Massive diamictite including glacially faceted and striated clasts, with chocolate-brown mudstone matrix.|04-APR-12
24190|Boko Formation|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
24190|Boko Formation|65338|4|Described|p iv, pp60-63.|Neoproterozoic|Neoproterozoic|Georgina Basin. Correlated with 600 Ma Marinoan glacial deposits of the Adelaide Fold Belt. Likely provenance is Lander Rock Formation with granite intrusions and possibly Reynolds Range Group. Non-marine tillite.||||Unconformably overlies Amesbury Quartzite and Utopia Quartzite. Is overlain by Oorabra Arkose and disconformably or unconformably by Central Mount Stuart and Elyuah Formations.|Massive diamictite with a red-brown mudstone matrix rarely preserved in exposures; clasts commonly faceted and striated, including quartzite, granite, volcanic and metamorphic rocks to 2 m; varved siltstone, limestone and ? cap dolostone.|
24190|Boko Formation|65341|4|Described|p2 Fig.2, p5, pp12-14. |Cryogenian|Cryogenian|Formerly part of 'Central Mount Stuart beds' (Shaw and Warren 1975); subsequently recognised as a distinct but un-named unit by Walter (1980). The clast assemblage, and presence of glacial facets and striations, distinguish this unit from Oorabra Arkose conglomerates. Lenticular with thickness to 30 m. Correlates with c.600 Ma Marinoan glaciation.||Unit in Keepera Group.||Unconformably overlies Utopia Quartzite. Is overlain conformably by Oorabra Arkose and unconformably by Elyuah Formation.|Glacial diamictite; red-brown mudstone matrix, striated and faceted clasts (quartzite, granite, metamorphic rocks) up to 2 m size.|
24190|Boko Formation|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.||Unit in Keepera Group.|||Tillite, dolostone/limestone, laminated siltstone.|
24190|Boko Formation|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Keepera Group.|||Tillite, dolostone/limestone, laminated siltstone.|
24190|Boko Formation|68270|4|Described|p680-682,686,688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section occurs 34km W of Barrow Creek; lat. 21'31.1'S, long. 133;33.5'E. Less than 30m thick. Non-marine moraine (glacial till) of the Elatina glaciation. Clasts comprise quartzite, sandstone, conglomerate, granite, various metamorphic rocks and rare volcanic rocks. Correlative to Elatina Formation.||||Overlain disconformably by Mopunga Group, locally overlain by Oorabra Arkose. Underlain unconformably by Amesbury Quartzite or basement.|Massive diamictite, with cobble and boulder clasts up to 2 min diameter in a redbrown mudstone matrix.|03-JUL-19
24190|Boko Formation|69437|5|Briefly described|p22:4-5|Cryogenian|Cryogenian|SW Georgina Basin, Centralian A Superbasin. Supersequence 3.||Keepera Group.||||12-JUL-16
24190|Boko Formation|69438|6|Mentioned|p23:17|||Georgina Basin.||||Correlated with the Olympic Formation (Amadeus Basin).||12-JUL-16
24190|Boko Formation|69443|4|Described|p28:7-9, 35|Cryogenian|Cryogenian|Haines in Haines et al. (1991). Georgina Basin. Poorly exposed as low rounded hills. 20m thick at its type locality, but considerably thicker elsewhere. Unfossiliferous.||Keepera Group.||Unconformably overlies Amesbury Quartzite. Is overlain by Central Mount Stuart Formation disconformably; possibly conformably by Oorabra Arkose or unconformably by Elyuah Formation.|Massive diamictite with a mudstone matrix; interpreted as a glacial tillite; rounded cobbles and boulders, many of which are glacially faceted and striated.|12-JUL-16
24190|Boko Formation|69673|5|Briefly described|p114 fig 92, p115|Cryogenian|Cryogenian|20m thick.||Keepera Group|||Massive diamictite with a mudstone matrix.|
24190|Boko Formation|72516|6|Mentioned|p87|Ediacaran|Ediacaran|Georgina Basin. Age from equivalence with Oorabra Arkose.||||Equivalent to the Oorabra Arkose.||02-JUN-21
24190|Boko Formation|73086|6|Mentioned|p101, p167|||Georgina Basin.||||Correlates to Olympic Formation.||
33182|Bonanza Creek Formation|22538|6|Mentioned|Fig3 P708|||||||||
33182|Bonanza Creek Formation|23374|6|Mentioned|p17||Statherian|May have been included with Shadforth Sandstone in MILINGIMBI. of Katherine River Group, McArthur Basin.||||||
33182|Bonanza Creek Formation|23867|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Max. thickness: ~50m.  Geological Province: McArthur Basin.  See also Table 1.||||||07-NOV-08
33182|Bonanza Creek Formation|24050|2|Defined|p81 App. 1|Statherian|Statherian|See also p10.  Of the Katherine River Group.  Thickness in type section: 85m.  Overlies the Shadforth Sandstone; underlies the McCaw Formation.  Possibly equivalent to Wollogorang Formation in southern McArthur Basin.||||||23-DEC-09
33182|Bonanza Creek Formation|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
33182|Bonanza Creek Formation|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Laminated quartz sandstone; medium to thickly bedded fine sandstone with medium to coarse laminae. Geological Province: McArthur Basin. Overlies: Shadforth Sandstone. Underlies: McCaw Formation.||||||14-JAN-05
33182|Bonanza Creek Formation|61572|5|Briefly described|p668 Fig. 3|||Of the Katherine River Group. Fine-grained sandstone. Max. thickness: 85m. Geological Province: McArthur Basin.  See also p671 Tb. 1||||||
33182|Bonanza Creek Formation|64698|4|Described|lithinterp table|Statherian|Statherian|Actually shown as Bonanza Creek - McCaw Formation. McArthur Basin. Of Katherine River Group. Max thick 50m. Fine to medium laminated qtz sandstone, cross-bedded and massive in places; medium to thickly bedded fine sandstone with medium to coarse laminae.||||||07-JAN-09
33182|Bonanza Creek Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.|Shown within 1745-1730 Ma range.|Of the Katherine River Group.|||Shown as mudstone [this is at odds to all othe descriptions of this unit as fine sandstone]|05-JUN-18
33182|Bonanza Creek Formation|65232|5|Briefly described|p7 Fig. 6|||Of Katherine River Group. Underlies McCaw Formation; overlies Shadforth Sandstone. 85m thick. Shallow-marine sandstone.||||||09-FEB-10
33182|Bonanza Creek Formation|65340|6|Mentioned|p92.|||Northern McArthur Basin. Tentatively correlated with Aquarium Formation on the basis of similar lithofacies.||||||
33182|Bonanza Creek Formation|67564|4|Described|p10 Fig.5, p39 Fig.20, pp47-49.|Paleoproterozoic|Paleoproterozoic|50 m of shallow marine (nearshore to upper shoreface) sediments.|1740 - 1720 Ma.|Unit in Katherine River Group.||Overlies Shadforth Sandstone. Is overlain conformably by McCaw Formation.|Laminated, fine to medium quartz sandstone; medium to thickly bedded fine sandstone.|
33182|Bonanza Creek Formation|69430|4|Described|p15:3, 8-9|||NW McArthur Basin. 85m thick. Marine shoreface deposits.||Katherine River Group.||Conformably and gradationally overlies Shadforth Sandstone. Is overlain presumably conformably by McCaw Formation.|Very fine- to fine-grained sandstone; glauconite common in some beds. Also described as fine- to medium-grained laminated quartz sandstone, cross-bedded and massive in places, medium to thickly bedded fine-grained sandstone, medium to coarse laminae.|12-JUL-16
33182|Bonanza Creek Formation|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by McCaw Formation, overlies Shadforth Sandstone||
35951|Bond Springs Gneiss|9199|5|Briefly described|Map legend|||Felsic gneiss, muscovite-garnet gneiss, amphibolite.||||||03-NOV-04
35951|Bond Springs Gneiss|23361|5|Briefly described|31|||||||||
35951|Bond Springs Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Felsic gneiss, muscovite-garnet gneiss, amphibolite.||||||
35951|Bond Springs Gneiss|61309|6|Mentioned|p31|||||||||
35951|Bond Springs Gneiss|69427|5|Briefly described|p12:14-15|||Wigley Domain, Aileron Province.|||||Leucogneiss, garnet-muscovite gneiss and lesser banded biotite gneiss, amphibolite and muscovite schist. Locally migmatitic.|12-JUL-16
30417|Bone Creek Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
30417|Bone Creek Sandstone|23216|4|Described|p25,31-2|||Former name: Bone Creek Formation||||||
30417|Bone Creek Sandstone|23374|4|Described|p18-19||Statherian|Of Mount Rigg Group. In the Pine Creek Inlier.||||||26-JUL-06
30417|Bone Creek Sandstone|23396|5|Briefly described|p 407 fig.2|||Of Mount Rigg Group||||||26-JUL-06
30417|Bone Creek Sandstone|23867|3|Fully described|p15|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group.  Geological  Province: McArthur Basin.  See also Table 1.||||||07-NOV-08
30417|Bone Creek Sandstone|23937|4|Described|p13, p25 Tb. 2|Calymmian|Statherian|Supersedes Bone Creek Formation.  Of the Mount Rigg Group.  Unconformably overlies the Gundi Sandstone; also overlies West Branch Volcanics.  Max. thickness: 30m.  Geological Province: McArthur Basin.||||||13-APR-05
30417|Bone Creek Sandstone|24050|3|Fully described|p32, p9 Tb. 2|Mesoproterozoic|Paleoproterozoic|Medium- to coarse-grained quartz sandstone; minor lithic, pebbly and glauconitic sandstone, mudstone, breccia, rare dolostone.  Parent: Mount Rigg Group.  Overlies Katherine River Group unconformably; underlies Dook Creek Formation.  Max. thickness: 180m.||||||07-NOV-08
30417|Bone Creek Sandstone|24051|5|Briefly described|Map Legend|Calymmian|Statherian|Of Mount Rigg Group. Geological Province: McArthur Basin.||||||
30417|Bone Creek Sandstone|43149|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of Mount Rigg Group. Age Calymmian or Statherian.||||||07-NOV-08
30417|Bone Creek Sandstone|60573|5|Briefly described|Map legend|Calymmian|Statherian|Of Mount Rigg Group. Medium to thick bedded, cross-bedded, medium- to coarse-grained quartz sandstone. Does not outcrop in the ROPER RIVER mapsheet area.||||||26-JUL-06
30417|Bone Creek Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|White, medium to thickly bedded, cross-bedded medium to coarse quartz sandstone.  Geological Province: McArthur  Basin. Overlies: Gundi Sandstone.||||||14-JAN-05
30417|Bone Creek Sandstone|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Mount Rigg Group. Quartz sandstone: medium to thick bedded, cross bedded, medium to coarse grained.||||||30-SEP-05
30417|Bone Creek Sandstone|61572|5|Briefly described|p667|||Of the Mount Rigg Group. Geological Province: McArthur Basin. See also p671 Tb. 1||||||
30417|Bone Creek Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Mount Rigg Group.||||
30417|Bone Creek Sandstone|67564|3|Fully described|p iv, p6 Table 2, p49, p51.|Calymmian|Statherian|Northern McArthur Basin. 180 m of shallow marine sediments deposited during a major transgressive episode. Forms low, rubbly outcrops. The bottom of this unit marks a major regional unconformity between the Katherine River and Mount Rigg Groups.|1610 - 1590 Ma.|Basal unit in Mount Rigg Group.||Overlies Gundi Sandstone unconformably. Is overlain conformably by Dook Creek Formation.|White, medium- to thickly-bedded, crossbedded, medium to coarse quartz sandstone; locally glauconitic.|
30417|Bone Creek Sandstone|69430|4|Described|p15:3, 24-25, 30|||NW McArthur Basin. 20-30m thick. Probably shallow-marine deposits. Correlated with Smythe Sandstone.||Mount Rigg Group.||Overlies Margaret Hill Conglomerate conformably, or West Branch Volcanics, Gundi Sandstone, McCaw Formation unconformably. Is overlain conformably and gradationally by Dook Creek Formation.|Medium to coarse quartz sandstone; scattered granules and pebbles of quartz, jasper and chert.|12-JUL-16
30417|Bone Creek Sandstone|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Northwestern McArthur Basin.||Mount Rigg Group||Overlain by Dook Creek Formation, Overlies Margaret Hill Conglomerate||
30417|Bone Creek Sandstone|72373|5|Briefly described|p27|Mesoproterozoic|Mesoproterozoic|Of northern McArthur Basin. ||Unit of Mount Rigg Group.||Correlable with Mount Birch Sandstone.||
27638|Bonrook Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
27638|Bonrook Granite|24197|5|Briefly described|p24, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. One of a group of concentrically zoned transitional granite and leucogranite dominated plutons. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
27638|Bonrook Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27638|Bonrook Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Granite, leucogranite.||||||07-NOV-08
27638|Bonrook Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27638|Bonrook Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27638|Bonrook Granite|43140|4|Described|p15||Paleoproterozoic|Of Cullen Batholith. Previously included Cullen Granite by Noakes 1949,Malone 1962.||||||07-JAN-09
27638|Bonrook Granite|43624|6|Mentioned|p15|||||||||
27638|Bonrook Granite|43832|4|Described|Table8p39;46,Tb12p63||Paleoproterozoic|||||||07-NOV-08
27638|Bonrook 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
27638|Bonrook Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. I-type.  Pink-grey medium equigranular biotite granite. Intrudes Burrell Creek Formation.||||||07-JAN-09
27638|Bonrook Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Allamber Springs Suite.|||Coarse-grained porphyritic granite and fine equigranular granite. I-type.|12-JUL-16
27638|Bonrook Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Shoobridge Suite.|||Pink to grey, fine- to medium-grained porphyritic to equigranular biotite granite.|
28387|Bonya Metamorphics|42770|5|Briefly described|p12, p13, Fig.14|||Age: 1790 +/- 15 Ma. See also Table 2.||||||26-JUL-06
28387|Bonya Metamorphics|43568|6|Mentioned|p502|||||||||
28387|Bonya Metamorphics|70303|5|Briefly described|iv, p1, p5-12, p19-22|Paleoproterozoic|Paleoproterozoic|New name, replacing Bonya Schist. Aileron Province, Arunta Region. Crops out extensively in the Bonya Hills. A low-P metasedimentary succession. Provenance of the schist dominated by 1900-1760 Ma sources; underwent metamorphism at 1718 +/- 53 Ma (and c.498 Ma). The para-amphibolite has a MDA of 1855 +/- 10 Ma for the sedimentary precursor, and was metamorphosed at 1765 +/- 11 Ma. The maximum depositional age is a Pb/Pb date.|1788 +/- 6 Ma (maximum depositional age).||||Includes porphyroblastic andalusite-K-feldspar schist, and compositionally-layered calc-silicate para-amphibolite.|04-APR-18
28387|Bonya Metamorphics|70809|5|Briefly described|iv, p1, p6, p8-p9, p12-p13, p16|Statherian|Statherian|SHRIMP age is interpreted as a maximum depositional age of the sedimentary protolith to these rocks. SHRIMP metamorphic ages of 1718 +/- 53 Ma and 498 +/- 24 Ma are also derived from Kositicin et al, 2015. Additional LAICPMS dates includes 1789 +/- 10 Ma, 1757 +/- 9 Ma, 1770 +/- 5 Ma and 1760 +/- 4 Ma. Monazite geochronology and petrographic descriptions of dated samples are discussed.|1788 +/- 6 Ma (SHRIMP, Kositcin et al 2015)|||Intruded by Attutra Metagabbro|Cordierite-andalusite schist, andalusite-K-feldspar-sillimanite schist.|
28387|Bonya 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|||||
28387|Bonya Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both ages are of metamorphism: U-Pb monazite LA-ICPMS.|1789+/-10 Ma and 1757+/-9 Ma.||||Metapelite.|
28387|Bonya Metamorphics|71621|4|Described|iii, p1, p14-p21, p23, 26, 30, 42|Statherian|Orosirian|Aileron Province. ICPMS age is interpreted as the maximum depositional age for this unit. SHRIMP maximum depositional ages include titanite 1765 +/- 11 Ma and 1717 +/- 16 Ma (Kositcin et al, 2015). A Pb-Pb age of 1855 +/- 10 Ma and U-Pb age of 1807 +/- 21 Ma are derived from Kositcin et al, 2014. A summary of SHRIMP U-Pb and LAICPMS isotopic data and interpretation is provided. Petrography and zircon description discussed.|1852 +/- 15 Ma (LAICPMS)|||Intruded by the Cappocks Granodiorite, Xanten Granodiorite and the Unca Granite.  Conformably interlayered with Mascotte Orthogneiss, White Violet Orthogneiss, Kings Legend Metadolerite.|Andalusite schist, cordierite-andalusite schist, calc-silicate rock and metasandstone.|01-FEB-19
28387|Bonya Metamorphics|71750|4|Described|iii-iv,p1,6,10,13,17,20,25-31,34|Statherian|Statherian|Geological province: Aileron Province. Occurs east of the Deep Bore Metamorphics. Reported maximum depositional age of 1788+\-6 Ma (Kositcin et al., 2015), suggesting similar provenance to Deep Bore Metamorphics. Syn-depositional with Casper Suite. Sample: GA 2180614 (NTGS HU14BLR672) (603182E 7489890N) monazite analysis yields age of 1763+\-5 Ma (metamorphic monazite growth). Previous detrital zirvcon analysis by Kositcin et al. (2015) of the same sample yielded a maximum depositional age of 1788+\-6 Ma and provenance dominated by 1900-1760 Ma sources.|1763+\-5 Ma metamorphic monazite growth.|||Conformably interlayered with White Violet Orthogneiss, Casper Suite.||20-SEP-19
28387|Bonya Metamorphics|71866|5|Briefly described|p1-p2, p5, p7,  p9, p12, p15, p17|||Jervois Mineral Field, Aileron Province. Analytical procedure, LAICPMS analyses, results and interpretation discussed in detail. Intruded by an unnamed pegmatite unit dated in this study. SHRIMP age from Kositcin et al, 2015 is interpreted as a maximum depositional age of the sedimentary protolith of this unit.|1788 +/- 6 Ma (Kositcin et al, 2015)||||Quartz-muscovite-sericite schist and calc-silicate rock.|
28387|Bonya Metamorphics|72370|5|Briefly described|iii,p1,3-4,8,10-11,13,15-16,19-24,p26-27|||Geological province: Aileron Province. Metamorphosed to lower amphibolite facies. Kositcin et al. (2015) provided a maximum depositional age of 1788+\-6 Ma. LA-ICP-MS U-Pb zircon dating of sample HU15MVM200 yield a c. 1820 Ma maximum depositional age for the sedimentary protolith. The wide spread of maximum depositional ages may indicate a long-lived sedimetnary basin derived from multiple sources. Reno et al. (2016) provided timing of onset of high-thermal gradient conditions and metamorphism to the Bonya Metamorphics sedimentary protolith at 1789+\-10 Ma (LA-ICP-MS monazite 207Pb/206Pb crystallisation age), and timing of main regional fabric (S2) development at 1757+\-9 Ma (LA-ICP-MS 207Pb/206Pb in-situ monazite). LA-ICP-MS U-Pb dating of pegmatite intrusions yield weighted mean 207Pb/206Pb ages of 1771+\-17 Ma (sample HU14MVM096), 1740+\-11 Ma (sample HU14MVM097) and 1744+\-9 Ma (sample HU14MVM098), which shows timing of tantalite crystallisation, and placing constraints of pegmatite emplacement within the Bonya Metamorphics to just after development of main S2 foliation, and minimum timing constrain on polymetallic base metal mineralisation at the Marshall-Reward deposit.||||Intruded by Casper Suite. Crosscut by Samarkand Pegmatite.||16-DEC-19
28387|Bonya Metamorphics|72372|4|Described|iii,p1-4,6,8,10-11,13-14,16,19,21-22|Statherian|Statherian|Geological province: Aileron Province. Metasedimentary succession of probably continentally-derived metamudstone, metasandstone and metacarbonate rocks.  Deposition of sedimentary protolith at c. 1.79 Ga (Kositcin et al 2015, Reno et al 2017, Beyer et al 2018), interpreted to be contemporaneous with metamorphism, bimodal magmatism and base metal mineralisation. Contains discrete layers of tourmaline; associated with metamorphosed synsedimentary, stratabound Cu-Ag-Pb-Zn mineralisation at the Jervois mineral field. Tourmaline layers associated with layers of Fe, Mn and P-rich rocks, all related to mineralisation, and interpreted as metaexhalites (metamorphosed hydrothermal chemical sediments), forming stratigraphic marker layers. Intruded by Baikal Supersuite igneous rocks at c. 1.79-1.77 Ga. Layered tourmaline interpreted to be stratabound, and possibly stratiform, and therefore part of Bonya Metamorphics succession. Previously tourmaline geochronological attempts yielded a poorly constrained Pb-Pb step leach ages of 1710+\-42 Ma, 1737+\-260 Ma, and a c. 1.72 Ga Edwards Creek Pb model age (see p23). Bonya Metamorphics host rocks yield maximum depositional age of 1687+\-6 Ma (Kositcin et al 2015). See also p34,36.|c. 1.79 Ga|||Intruded by Baikal Supersuite.|Andalusite-muscovite-quartz schist and calc-silicate rocks.|10-OCT-19
28387|Bonya Metamorphics|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1787 +/- 6 Ma (U-Pb zircon)||||Undivided metasedimentary rocks: interlayered schists, calc-silicate rock, impure quartzite and layered quartzite; foliated and folded.|
28387|Bonya Metamorphics|72516|1|Redefined|p7-p8, p10, p13-17, p19-29, 191-194|Statherian|Statherian|Aileron Province. Previously called the 'Bonya metamorphic complex' of Warren 1979, 'Bonya Metamorphic Complex' of Stewart et al (1980) and 'Bonya Schist' of Shaw et al, 1985. Variation is of  "Bonya Metamorphics" of Warren and Thorpe 1994 and Warren et al (1995). Name is derived from the Bonya Creek in central JERVOIS RANGE 1:100k sheet. See definition card for locations of type localities of informal subunits. Oldest exposed Aileron Province rocks in the map sheet area. Outcrops in the Bonya, Jervois and Jinka domains. Outcrop characteristics of various informal constituents is detailed. Deposited in a shallow marine or lacustrine environment. Previously interpreted to be age-equivalent to the Strangways Metamorphic Complex. The maximum depositional age is a SHRIMP Pb-Pb age (this study), numerous additional dates are provided. Additional SHRIMP Pb-Pb maximum depositional ages included are 1855 +/- 8 Ma and 1807 +/- 21 Ma. Subdivided into six informal units based on lithology. Apparent maximum thickness is 1-5km. A reference area occurs around and north of the Reward copper deposit (eg 630109mE 7493890mN; 629678mE 7496078mN; 629261mE 7494552mN; Reno et el 2019). Isotope geochemistry, metamorphism, structure, economic geology and geophysics are discussed. See also piii, p32, p35, p39, p42-43, p48, p51-p52, p54, p56-57, p61, p63, p71-72, p75, p88, p101, p119, p123-124, p126, p135-137, p139-145, p153, p155, p157, p171-175, p188-189, p213-218.|1787 +/- 6 Ma (max dep age)|||Intruded by the Baikal Supersuite, Unca Granite,Samarkand Pegmatite, etc. Xenoliths in Thring Granite. Unconformably overlain by the Grant Bluff Formation.|Porphyroblastic schists. Mica schists. Mica-bearing metasandstones. Garnet schists. Quartz-magnetite-hematite rocks and tourmalinites. Abundance varies in Bonya Hills and Jervois mineral field.|14-APR-22
28387|Bonya Metamorphics|72711|6|Mentioned|p2, p3 Fig.2, p4 Tb.1, p6.|Statherian|Orosirian|Shown as part of the Aileron Province. Maximum mineralisation age of ca 1807 Ma. based on a maximum depositional ages of 1807+/- 17 Ma. and 1807 +/- 21 Ma. (zircon 207Pb/206Pb ages; Claoue-Long and Hoatson 2005, Kositcin et al 2014).|Max. dep. age 1807+/-17  Ma.||||Skarn-altered calc-silicate rocks. Includes porphyroblastic and mica schists and impure quartzite.|
28156|Boothby Orthogneiss|1490|6|Mentioned|p6|||Associated with the ~1140 Ma Ormiston Event (aka Teapot Event).|925 +/- 153Ma (Black et al., 1993).|||||
28156|Boothby Orthogneiss|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block.||||||28-OCT-04
28156|Boothby Orthogneiss|23270|5|Briefly described|Table 1, p4||Proterozoic|Of Arunta Block. Age: Rb-Sr Whole Rock 900+/-150ma.||||||26-JUL-06
28156|Boothby Orthogneiss|23271|5|Briefly described|Map legend||Proterozoic|Of Arunta Block. Age: Middle Proterozoic.||||||26-JUL-06
28156|Boothby Orthogneiss|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
28156|Boothby Orthogneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28156|Boothby Orthogneiss|38829|5|Briefly described|p134|||||||||
28156|Boothby Orthogneiss|39888|6|Mentioned|Fig.8|||See also Fig.10||||||
28156|Boothby Orthogneiss|41051|6|Mentioned|p414|||||||||
28156|Boothby Orthogneiss|41964|6|Mentioned|p186|||||||||
28156|Boothby Orthogneiss|42217|6|Mentioned|p417|||||||||
28156|Boothby Orthogneiss|42326|5|Briefly described|Table 2 P11|||||||||
28156|Boothby Orthogneiss|48992|2|Defined|p10|Mesoproterozoic|Mesoproterozoic|||||||
28156|Boothby Orthogneiss|48997|5|Briefly described|p7|||||||||
28156|Boothby Orthogneiss|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite.||||||07-NOV-08
28156|Boothby Orthogneiss|62595|6|Mentioned|p19.|||Granite gneisses correlated with this unit intrude the Lander Rock beds.||||||
28156|Boothby Orthogneiss|64956|5|Briefly described|p3 Tb. 1, p20|Paleoproterozoic|Paleoproterozoic|Cryst. age: 1806+/-4Ma. Geological province: Arunta region. Sample comprises K-feldspar megacrystic biotite granite with a strong, pervasive WNW-striking foliation.||||||07-FEB-11
28156|Boothby Orthogneiss|65232|5|Briefly described|p76, App. 2|Palaeoproterozoic|Palaeoproterozoic|Along with Lander Rock Beds,  hosts REO-uranium mineralisation: fluor-apatite main ore mineral.|||||Coarse, porphyritic, foliated, granitic augen gneiss.|11-APR-12
28156|Boothby Orthogneiss|65338|5|Briefly described|p12, p16, p48.|Orosirian|Orosirian|Outcrops in the Reynolds Range. An age of 1807 +/- 6 Ma (same reference) is given for an outcrop at the southeastern end of Reynolds Range.|1806 +/- 4 Ma (Worden et al. 2008).|||Intrudes Lander Rock Formation.||
28156|Boothby Orthogneiss|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
28156|Boothby Orthogneiss|65343|5|Briefly described|p3-4|||The country rock that surrounds the Nolans Bore REE-P-Th-U deposit, closely resembles the Boothby Orthogneiss, as mapped in the hills to the northeast by Stewart et al. (1981). The Boothby Orthogneiss intrudes the surrounding amphibolite- to granulite-facies metamorphic rocks (high-grade equivalents of the Lander Rock beds, and the Nolans Dam and Aileron metamorphics). The depositional ages of these rocks are not yet known, but are considered to be about 1800-1820 Ma, and the Boothby Orthogneiss is probably 1770-1800 Ma. All of these units were metamorphosed at 1560-1600 Ma.||||||
28156|Boothby Orthogneiss|67127|6|Mentioned|p98, p101|||Correlated with granites which host the Nolans Bore deposit in mineralised fluorapatite veins.|1806 +/- 4 Ma||||Gneissic granite.|
28156|Boothby Orthogneiss|67430|6|Mentioned|p10||||1806 +/- 4 Ma (Collins and Williams, 1995).|||||
28156|Boothby Orthogneiss|69228|6|Mentioned|p370|||Peaked Hill, Arunta Inlier. Associated with a shear zone that hosted fluid flow. Isotope values and metamorphism described.||||||
28156|Boothby Orthogneiss|69427|5|Briefly described|p12:20 Fig.12.19; 12:21, 26|Orosirian|Orosirian|Aileron Province. SHRIMP U-Pb zircon age. Also appears as Mount Boothby Orthogneiss (12:6, 60). Associated with the Nolans Bore REE-P-U-Th deposit.|1806 +/- 4 Ma (Worden et al., 2008).|||Intrudes Lander Rock Formation.|Foliated to gneissic megacrystic granite; biotite-bearing and characterised by coarse phenocrysts of K-feldspar with locally developed rapakivi textures.|12-JUL-16
28156|Boothby Orthogneiss|69917|5|Briefly described|p58||Paleoproterozoic|~1805 Ma. Has Sm-Nd model age of 2.49 Ga for precursor input. This is similar to Aileron Metamorphics oldest source material.||||||
28156|Boothby Orthogneiss|70376|5|Briefly described|p833 fig 2, p835-836, p838-844, p846-848|Paleoproterozoic|Paleoproterozoic|Contains occasional xenoliths of coarse grained cordierite rich granofels. Foliation at places defined by biotite-quartz which outlines cm to m scale isoclinal folds. An initial age of felsic magmatism is roughly ca 1808 Ma followed by cover sequence at 1792 Ma and 1774 Ma. Samples OG1, 2 & 3 discussed, all megacrystic orthogneiss. U-Pb zircon magmatic crystallisation ages:OG1  1809+/-9 Ma, OG2  1779+/-9 Ma, OG3 1797+/-9 Ma LA-ICPMS.|1806 +/- 4 Ma (SHRIMP) 1779 MA +/- 9 Ma LA-ICPMS||||K-feldspar, plagioclase, quartz and biotite orthogneiss which may contain local garnet and sillimanite. K -feldspar augen are characteristic of this unit which is locally migmatitic with K-feldspar leucosomes forming discordant veins.|27-SEP-16
28156|Boothby Orthogneiss|70554|4|Described|p797-799,801-804,806,813,815,818,820|Orosirian|Orosirian|Geologial province: Aileron province. Underwent high-grade (to granulite-facies) metamorphism during Chewnings Orogeny and emplacement of late-metamorphic pegmatites (Collins and Williams, 1995). SHRIMP U-Pb age of 1806 +\-4 Ma (Collins and Williams, 1995). Intruded by narrow mafic and ~1550 Ma granitic pegmatite dykes.|~1806 Ma||||biotite-rich granite gneiss, strong schistose to gneissic fabric, locally mylonitic.|
28156|Boothby Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1806+/-3.7 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
28156|Boothby Orthogneiss|71858|5|Briefly described|p2, p5, p70|||Aileron Province. Hosts the Nolans prospect.|ca 1805 Ma|||||
28156|Boothby Orthogneiss|73399|6|Mentioned|App.E|||||||||
32406|Bootu Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup, Churchills Head Group. Quartz arenite and sublithic arenite; medium to coarse grained, parallel-, or cross-bedded; thin to medium bedded; rippled. Siltstone. Ridge forming.||||||07-NOV-08
32406|Bootu Formation|23733|5|Briefly described|p32 Fig. 19|||Of Tomkinson Creek Group.||||||
32406|Bootu Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||
32406|Bootu Formation|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: <1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49, p60.||||||07-NOV-08
32406|Bootu Formation|24303|1|Redefined|p11, p56 Appendix|Statherian|Statherian|Of the Tomkinson Creek Group. Overlain by the Carmilly Formation; overlies the Attack Creek Formation. Max. Thickness: 2200m. Formerly undifferentiated Tomkinson Creek beds; later included in upper Attack Creek Fm. in FLYNN.||||||25-JAN-10
32406|Bootu Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic| Of the Tomkinson Creek Group. Sandstone; quartz arenite; thin to massive bedded, medium grained to granular; pebbly sandstone, cross-bedded; mudstone, basal litharenite, dolostone, stromatolitic bioherms and praphitic shale, manganiferous; ridge-forming.||||||07-NOV-08
32406|Bootu Formation|24442|5|Briefly described|p14, p20|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group.  Contains a 6-12m thick manganese horizon at its base.  Geological Province: Ashburton Province.||||||07-NOV-08
32406|Bootu Formation|50353|5|Briefly described|Map Legend|||Of Tomkinson Creek Group||||||
32406|Bootu Formation|60684|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Cr. Subgroup (Churchills Head Gp). Previously mapped as uppermost part of Attack Creek Formation, with which it is transitional. On HELEN SPRINGS continues up into Carmilly Fm. Qtz arenite and sublithic arenite, siltstone.Max.thickness:~200m.||||||07-NOV-08
32406|Bootu Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Quartz arenite, sublithic arenite.  Overlies Attack Creek Formation; underlies the Carmilly Formation.  In the Tennant Creek region.||||||07-NOV-08
32406|Bootu Formation|64780|5|Briefly described|p60,p61,p63 Fig.4,p65-70  |Palaeoproterozoic|Palaeoproterozoic|Of Hussey at al.(2001). Up to 2000m thick locally. Hosts the Bootu Creek manganese mine. Inadvertently called Bootu Creek Formation on p65 during discussion of Bootu and Attack Creek Formations.||Of the Tomkinson Creek Group. ||Overlies the Attack Creek Formation conformably. Conformably (gradationally) underlies the Carmilly Formation.|A thick, relatively homogeneous succession of sandstone, with intervals of granular to pebbly sandstone and conglomerate, and minor amounts of siltstone, mudstone and carbonate rocks.|
32406|Bootu Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Tomkinson Creek Group||||
32406|Bootu Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.||Overlies Attack Creek Formation. Is overlain by Carmilly Formation.|Quartz arenite, sublithic arenite.|
32406|Bootu Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
32406|Bootu Formation|69418|6|Mentioned|p3:26|||Tomkinson Province. Hosts numerous hydrothermal-type Mn deposits (described).||||||12-JUL-16
32406|Bootu Formation|69425|6|Mentioned|p10:12|||Tomkinson Province.||||Part-correlative of Yaddanilla Sandstone.||12-JUL-16
32406|Bootu Formation|69431|4|Described|p16:1, 3-6, 11-13, 22-23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.1800-2200m thick. Lithology described in some detail. Protected shallow-marine (periodically supratidal) depositional environment, overlain successively by intertidal and subtidal open marine and shallow marine with minor fluvial red beds. Hosts the Bootu Creek stratiform manganese deposits, which occur along 24km of strike (described in detail).||Tomkinson Creek Group.||Overlies Attack Creek Formation disconformably to conformably. Is overlain conformably by Carmilly Formation, and unconformably by Gleeson Formation.|Medium- to very coarse-grained sandstone and pebbly sandstone; minor thinly bedded siltstone and mudstone; calcareous siltstone and sandstone; minor carbonaceous shale and manganiferous sandstone, stromatolites and halite pseudomorphs.|12-JUL-16
32406|Bootu Formation|69673|6|Mentioned|p58|||||Tomkinson Creek Group||||
80341|Boundary Igneous Complex|71621|5|Briefly described|iii, p1, p28-p29, p32, p35-p36|Statherian|Statherian|Aileron Province. Petrography and zircon description discussed. Igneous crystallisation SHRIMP age 1746.2+/-4.2 Ma (Kositcin et al. 2011).|1761 +/- 34 Ma (LA-ICPMS)|||Intrudes the Tarlton Granite and Thring Granite.|Biotite granodiorite.|16-JUN-21
80341|Boundary Igneous Complex|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1746 +/- 4 Ma -1753 +/- 7 Ma (U-Pb Zircon)||||Biotite granodiorite, biotite granite, leucogranite: fine to medium-grained, equigranular to porphyritic.|
80341|Boundary Igneous Complex|72516|2|Defined|p10, p13-14, p18, p72-75, p195-196|Statherian|Statherian|Aileron Province. New name, named for the Boundary Hill in western TOBERMORY. Type localities for informal subunits are provided on p195. Outcrops occur in the Bonya, Jinka, Jervois and Tarlton domains and consist of scattered boulders, bouldery rises, hillocks and low rounded occurences commonly in isolation of one another. Outcrops were previously assigned to Jervois Granite in HUCKITTA and to unnamed granite in TARLTON. SHRIMP ages derived from Kositicin et al (2011) and Cross et al (2005); an additional magmatic crystallisation age of 1769 +/- 14 Ma is derived from Beyer et al, 2018. Interpreted to have been deposited in a continental margin environment. Distinguishing features, petrography, metamorphism, geochemistry, geophysics, mineralisation, extent and structure are discussed. Interpreted to also intrude the Jervois Granodiorite. See also  p21, p29, p61, p64, p69, p86, p97, p113-118, p122-123, p125-127, p135, p139-141, p143, p145, p169, p171, p175, p189, p197.|1746 +/- 4 Ma - 1753 +/- 7 Ma (SHRIMP Pb-Pb)|||Unconformably overlain by the Mount Cornish Formation. Intrudes the Baikal Supersuite, Thring Granite and the Tarlton Bore Granite.|Biotite granodiorite, biotite granite, leucogranite: fine to medium-grained, equigranular to porphyritic, biotite variably developed, minor secondary muscovite; fresh to slightly weathered; undeformed to moderately foliated.|15-JUN-21
80341|Boundary Igneous Complex|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.||||||
37730|Bowgan Sandstone|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: >1450Ma.||||||
37730|Bowgan Sandstone|65337|2|Defined|p9 Fig.5, p39 Table 5, p40.|Mesoproterozoic|Mesoproterozoic|New name. Northwest MOUNT DRUMMOND area. Up to 100 m of braided fluvial to shallow marine intertidal deposits. Resembles the upper siliciclastic portion of the Buddycurrawa Volcanics; discrimination often impossible. Also similar to Warramana Sandstone.||Unit in Wild Cow Subgroup.||Probably unconformable on Murphy Metamorphics and Benmara Group. Is overlain by Crow Formation.|Maroon, variably ferruginous, lithic to sublithic, fine- to coarse-grained sandstone; possible rare chertified digitate stromatolites; local basal chert clast conglomerate or breccia. Has a speckled appearance in hand specimens.|
37730|Bowgan Sandstone|69433|6|Mentioned|p18:4|||||||Overlies Buddycurrawa Volcanics probably unconformably.||12-JUL-16
37730|Bowgan Sandstone|69434|4|Described|p19:2, 4-5|Mesoproterozoic|Mesoproterozoic|Benmara-Canyon Range area, NW South Nicholson Basin. Up to 100m thick: average is c.10m; locally absent, esp. in the N. Braided fluvial to shallow-marine intertidal deposits.||Wild Cow Subgroup.||Overlies Murphy Metamorphics and Benmara Group probably unconformably. Is overlain conformably by Crow Formation. Lateral equivalent of Playford Sandstone.|Maroon, variably ferruginous, lithic to sublithic, fine to coarse +/- pebbly sandstone; possible rare chertified digitate stromatolites; local basal chert clast conglomerate or breccia.|12-JUL-16
37730|Bowgan Sandstone|69673|4|Described|p56|||less than 100m thick. Braided fluvial to shallow marine intertidal deposit. ||Wild Cow Subgroup|||Ferruginous, lithic to sublithic, sandstone with occasional laminae of quartz granules and small pebbles.|
37730|Bowgan Sandstone|72526|5|Briefly described|p8 Fig.1.3, p86.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Wild Cow Subgroup||Shown as unconformably overlying Benmara Group and underlies Crow Formation.||
37730|Bowgan Sandstone|72527|3|Fully described|p1, p8, p56, p78-85, p86, p88, p193.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Depositional age based on correlation with Playford Sandstone & assumed to be 'near the older end for the Roper Group (1500 -1400 Ma). Displays remarkably similar age spectra to Caulfield beds, Crow Formation and Bullrush Conglomerate. Type locality shown as 136.93949dE 18.08815dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios.This unit is generally thin ranging from <100m to c. 10m in thickness. See also p196-197.|1652+/-10 Ma max.dep age.|Wild Cow Subgroup||Underlies Crow Formation. Assumed to be lateral equivalent of Playford Sandstone. Probably unconformably overlies Benmara Group.|Ferruginous lithic to sublithic fine to coarse grained sandstone, exhibiting massive to thick, gently west-dipping beds with thin pebbly lags.|
37730|Bowgan Sandstone|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin.||Wildcow Subgroup||Unconformably overlies Benmara Group and underlies Crow Formation and is equivalent to Playfod Sandstone (No Mans Sandstone Member, Top Lily Sandstone Member and Wangalinji Member).||
37730|Bowgan Sandstone|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west of the South Nicholson Basin.||Wildcow Subgroup||Underlies Crow Formation.|Includes sandstone.|
37730|Bowgan Sandstone|72919|5|Briefly described|p5, p71|Mesoproterozoic|Mesoproterozoic|Carson et al. (2020) proposed an expanded version of the Benmara Group that includes strata of [or equivalent to?] this unit in the hanging wall of the Benmara Fault based on comparison of detrital zircon spectra with that of late Paleoproterozoic successions.||Wild Cow Subgroup, South Nicholson Group||Overlain by Crow Formation. Equivalent to Playford Sandstone.||
37730|Bowgan Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||Benmara Group||Partly overlain by Crow* Formation. Partly overlain and equivalent to Caulfield beds.||
37730|Bowgan Sandstone|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|||Benmara Group||||
80377|Bowthorn Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). Marine shelf unit.||Constance Sandstone.||Overlies Shultz Sandstone Member. Is overlain unconformably by Elizabeth Sandstone.||
80377|Bowthorn Member|71369|4|Described|p1, p6-7, p12, p23-24, p28, p32-36,|Mesoproterozoic|Mesoproterozoic|See also p49-50. Originally the Bowthorn Siltstone Member of Slater and Mond (1980), Sweet et al. (1981). It was abandoned as a Member of the Constance Sandstone, and absorbed into the Schultz Sandstone Member, by Rawlings et al. (2008). Resurrected and modified in this study as Bowthorn Member (Sweet, 2017) to apply to the upper part of the Constance Sandstone. The type section is 4-5km south of Bowthorn homestead in an area of very low dips and is estimated to be about 300m thick there South Nicholson Basin. Up to 400m thick. A series of prograding marine sand bodies.||Constance Sandstone.||Overlies Schultz Sandstone Member. Is overlain unconformably by Elizabeth Sandstone.|Coarsening-up sequences of green laminated shale, interbedded siltstone and very fine sandstone, to fine sandstone with scattered glauconite.|20-FEB-18
80377|Bowthorn Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn 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 Constance Sandstone.|||Green, laminated shale, siltstone and very-fine-grained sandstone, and medium to thick-bedded, fine-grained quartzose sandstone passing upwards siltstone and sandstone|
80377|Bowthorn Member|72526|5|Briefly described|p8 Fig.1.3, p33, p34.|Mesoproterozoic|Mesoproterozoic|Shown as located in the central and eastern parts of the South Nicholson Basin.||Constance Sandstone||Overlies and is laterally equivalent to Constance Sandstone and underlies Mullera Formation.||
80377|Bowthorn Member|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin.||Constance Sandstone||Part equivalent to Mittebah Sandstone and underlies Mullera Formation.||
80377|Bowthorn Member|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the central part of the South Nicholson Basin.||Upper part of Constance Sandstone.||Laterally equivalent to Mittebah Sandstone. Underlies Mullera Formation.|Includes dolomitic siltstone.|
80377|Bowthorn Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Underlain by and partly equivalent to Constance Sandstone. Overlain by Mullera Formation.||
80377|Bowthorn Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Unconformably overlain by Elizabeth Sandstone[?].||
79781|Breaden Formation|72369|5|Briefly described|p15|||Of Amadeus Basin. Defined by Donnellan and Normington 2017.||Unit of Winnall Group.||Overlain by Gloaming Formation.||
37732|Breakfast Sandstone|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Benmara Group.  Age: ~1725Ma.||||||07-NOV-08
37732|Breakfast Sandstone|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Benmara Group. White to pink, medium to coarse grained silicified sublithic sandstone; thin basal pebble or cobble conglomerate; rare chertified stromatolitic carbonate.||||||
37732|Breakfast Sandstone|65337|2|Defined|p9 Fig.5, p10 Table 3, p17.|Paleoproterozoic|Paleoproterozoic|New name. Northwest MOUNT DRUMMOND area. Up to 80 m of braided fluvial and/or shallow marine deposits. Mildly to strongly resistant; forms ridges with white banded phototones.||Unit in Benmara Group.||Unconformably overlies Murphy Metamorphics. Is overlain by Buddycurrawa Volcanics.|White to pink, medium- to coarse-grained silicified sublithic sandstone; thin basal pebble or cobble conglomerate; rare chertified stromatolitic carbonate.|
37732|Breakfast Sandstone|69433|4|Described|p18:2, 4-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Up to 80m thick. Braided fluvial and/or shallow-marine deposits, fining upwards.||Basal Benmara Group.||Unconformably overlies Murphy Metamorphics. Is overlain conformably by Buddycurrawa Volcanics. Correlative of Shady Bore Quartzite(?).|Resistant, white to maroon, medium to coarse, silicified sublithic sandstone; thin basal pebble or cobble conglomerate; rare chertified stromatolitic carbonate. Various sedimentary structures listed.|12-JUL-16
37732|Breakfast Sandstone|69673|6|Mentioned|p52 fig 42, p53 |||up to 80m thick.|||||Silicified sublithic sandstone.|
37732|Breakfast Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the west of the South Nicholson Basin.||Benmara Group||Shown as overlying Peters Creek Volcanics and underlies Buddycurrawa Volcanics.||
37732|Breakfast Sandstone|72527|5|Briefly described|p7 Fig.1.4, p86.|Paleoproterozoic|Paleoproterozoic|||Benmara Group||Conformably underlies Buddycurrawa Volcanics.||
37732|Breakfast Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the west part of the South Nicholson Basin||Benmara Group||Underlies Buddycurrawa Volcanics.||
37732|Breakfast Sandstone|72919|4|Described|p1, p4-5, p16-20, p93|Statherian|Statherian|South Nicholson Basin, Lawn Hill Platform. Basal unit of the Benmara Group. Unconformably overlies metamorphic rocks of the Murphy Province. Forms resistant strike ridges in some places and is poorly exposed at others, consisting of subcrop of silicified quartz sandstone. Trough cross beds, ripples, and desiccation cracks are common; interpreted to represent a moderate to high energy fluvial to shallow marine depositional environment. New U-Pb SHRIMP zircon maximum depositional age of 1756 +/- 14 Ma. Minimum age constraint is provided by the overling ca. 1660-1630 Ma Buddycurrawa Volcanics. Previously included in the now defunct Benmara beds. Stratigraphically overlies the Murphy Metamorphics and Connellys Volcanics; contact is assumed to be unconformable.|1756 +/- 14 Ma U-Pb SHRIMP|Benmara Group||Overlies Murphy Metamorphics, Connelly Volcanics. Conformably overlain by Buddycurrawa Volcanics.|White to pink, medium- to coarse-grained, silicified sub-lithic sandstone and rare chertified stromatolitic carbonate.|
37732|Breakfast Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||Benmara Group||Overlain by Buddycurrawa Volcanics.||
37732|Breakfast Sandstone|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|||Benmara Goup [?]||||
78970|Briggs Member|70380|3|Fully described|p743, p748-752, p755-759|Middle Cambrian|Middle Cambrian|New name, after Mount Briggs where it is well-exposed. Up to 160.9m thick; it is 134.1m thick in the type section, which is the interval 109.8-243.9m depth in drillhole NTGS86/1. Daly Basin. Mainly ooid shoals deposits seaward of tidal flats. Lithology and mineralogy described in detail. Graphic logs of drillholes.||Oolloo Dolostone.||Conformably and transitionally overlies Jinduckin Formation. Is overlain disconformably by King Member.|Typically well-bedded; fine to medium, crystalline dolostone, ooid dolograinstone, stromatolitic doloboundstone, microbial dololaminite, quartzic dolostone and dolomitic quartz sandstone. Beds are 10-50cm thick. Ooids, mostly <1mm, common throughout.|
25814|Brown Gannet Limestone|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cretaceous|Cretaceous|Type sction Ashmore Reef 1 well (1940-2167m).100-300m thick. Name replaces Woodbine beds"".||Bathurst Island Group||Overlies Sahul Group (disconformably). Overlies Darwin Formation. Grades into Puffin Formation and Vee Formation.|Limestone and marl.|
25814|Brown Gannet Limestone|41532|2|Defined|p308|Late Cretaceous|Early Cretaceous|Reserved as Gannet Formation.||||||02-AUG-06
25814|Brown Gannet Limestone|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25814|Brown Gannet Limestone|42442|2|Defined|p29|Maastrichtian|Albian|Name replaces "Woodbine Beds".||||||02-AUG-06
25814|Brown Gannet Limestone|43699|6|Mentioned|Fig.6,p10||Late Cretaceous|||||||
25814|Brown Gannet Limestone|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Early Cretaceous|||||||
25814|Brown Gannet Limestone|49637|5|Briefly described|Fig.3|Late Cretaceous|Late Cretaceous|Of the Bathurst Island Group. Geological Province: Ashmore Platform.||||||07-FEB-11
25814|Brown Gannet Limestone|70061|5|Briefly described|Regional geology Figs.6-7. Sahul: Fig.2|Santonian|Coniacian|See also Vulcan: Fig.2.||Bathurst Island Group.||Overlies Woolaston Formation. Is ovelain by Fenelon Formation.||12-JUL-16
25814|Brown Gannet Limestone|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Santonian|Coniacian|See also Northern: Fig.2. Yampi: Fig.2. Browse Basin. Not present in Yampi and Leveque Shelves.||Bathurst Island Group.||Overlies Woolaston Formation. Is overlain by Fenelon Formation.||12-JUL-16
79304|Browns Range Granite|69426|6|Mentioned|p11:12 Tb.11.2|||Vandenberg and Crispe (in prep). Not formally defined. [The name is probably invalid, as Browns Range Metamorphics has priority - unless this is the same unit?].||||||08-OCT-18
30280|Browns Range Metamorphics|22496|6|Mentioned|p9||Neoarchean|||||||07-NOV-08
30280|Browns Range Metamorphics|23621|2|Defined|p51 Appendix|Archean|Archean|See also page 13, page 12 table 1. Previously mapped as undivided Halls Creek Group and Tanami Complex. Age: 2507+/-22 Ma. Overlying unit Gardiner Sandstone (unconformably). Browns Range Dome. Max. thickness: >1000 m.||||||07-NOV-08
30280|Browns Range Metamorphics|23622|5|Briefly described|Map Legend|Paleoproterozoic|Archean|Geological Province: Browns Range Dome.||||||07-NOV-08
30280|Browns Range Metamorphics|23809|6|Mentioned|p2, p3 Fig. 1|||In the Tanami region.||||||
30280|Browns Range Metamorphics|43301|5|Briefly described|Map Legend||Archean|Metamorphosed at 2504+/-4 Ma.||||||07-NOV-08
30280|Browns Range Metamorphics|50315|5|Briefly described|Map Legend|Archean|Archean|Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean: felsic and mafic gneiss, granites and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|50374|5|Briefly described|Map Legend|Archean|Archean|||||||07-NOV-08
30280|Browns Range Metamorphics|50376|5|Briefly described|Map Legend|Archean|Archean|Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean - felsic and mafic gneiss, granite and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|60676|5|Briefly described|Map legend|Archean|Archean|Underlies MacFarlane Peak Group. Undifferentiated schist, gneiss, migmatite; undifferentiated Archaean: felsic and mafic gneiss, granite and migmatite.||||||07-NOV-08
30280|Browns Range Metamorphics|61861|4|Described|p3 Table 1, p5, p23, Map 1|Neoarchean|Neoarchean|New name; applied to 1 - 3 km thick high grade metamorphics confined to a narrow fault-bound slice with high magnetic response on southern margin of Browns Range Dome. Gneiss metamorphosed 1882 +/- 14 Ma.|2505 +/- 4 Ma enclaves in 2510 +/- 22 Ma granite.|||Unconformably overlain by Birrindudu Group|Includes granitic gneiss and muscovite schist intruded by fine-grained granite, thin granite sills, aplite and pegmatite.|03-APR-12
30280|Browns Range Metamorphics|62580|6|Mentioned|p8, p12 Fig. 2|Archean|Archean|||||||07-FEB-11
30280|Browns Range Metamorphics|63261|5|Briefly described|p7, p9, p17|||Of Blake et al (2000) for metamorph'd arkosic sed.rocks exposed near Browns Range granite complex in WA. Include quartzofeldspathic gneiss+muscovite schist intruded by aplite+ pegmatite.See also informal Browns Range metamorphics.Age discussion included||||||10-DEC-12
30280|Browns Range Metamorphics|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies.||||||15-DEC-08
30280|Browns Range Metamorphics|64675|5|Briefly described|Fig.7(a-b), Map 4, p14, Fig.20-22|Archean|Archean||1882 Ma|Of the Coomarie Suite.||Unconformably overlain by the Gardiner Sandstone of the Birrindudu Group. Unconformably overlain by the MacFarlane Peak Group.|Comprises granitic orthogneiss, muscovite paragneiss and schist.|19-MAR-14
30280|Browns Range Metamorphics|65323|5|Briefly described|Map legend|Archean|Archean|Most units not present on map; undifferentiated non-magnetic schist, gneiss, migmatite.||||||13-NOV-15
30280|Browns Range Metamorphics|65324|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65326|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||02-FEB-10
30280|Browns Range Metamorphics|65327|5|Briefly described|Map legend|Archean|Archean|Felsic and mafic gneiss, granite and migmatite informally subdivided based on variations in magnetic and gravity response; 3 (of 4) units are shown on this sheet and have high gravity and non-, variably, or moderate-intensely magnetic response||||||
30280|Browns Range Metamorphics|65328|5|Briefly described|Map legend|Archean|Archean|Felsic and mafic gneiss, granite and migmatite informally subdivided based on variations in magnetic and gravity response; 3 (of 4) units are shown on this sheet and have high gravity and non-, variably, or moderate-intensely magnetic response||||||02-FEB-10
30280|Browns Range Metamorphics|65349|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65350|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65351|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65352|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65353|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65354|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65355|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|65356|6|Mentioned|Map legend|Archean|Archean|Not shown on map||||||
30280|Browns Range Metamorphics|67127|5|Briefly described|p175|Palaeoproterozoic|Archaean|Tanami-region. Intruded by an unnamed granitic core.|||||Meta-arkose, feldspathic metasandstone and schist.|
30280|Browns Range Metamorphics|67168|5|Briefly described|Map legend.|Archean|Archean|Areas with different magnetic and gravity responses are mapped separately.||||Unconformably overlain by MacFarlane Peak Group.|Felsic and mafic gneiss, granite, migmatite.|
30280|Browns Range Metamorphics|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv and 500k_geologyp08_lut.csv. Granites-Tanami Complex. Non-magnetic.|c.2510 Ma (Page et al., 1995).||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|25-NOV-15
30280|Browns Range Metamorphics|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|30-JUL-15
30280|Browns Range Metamorphics|69165|4|Described|500k_geologyp08_lut.csv|Paleoproterozoic|Paleoproterozoic||||||Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|69419|5|Briefly described|p4:7,|Paleoproterozoic|Paleoproterozoic|Forms a crescent-shaped belt along the S edge of Browns Range Inlier (previously the Browns Range Dome). Previous interpretations of an Archean age (2510 +/- 22 Ma; Page et al., 1995) were probably based on inherited zircons.|||||Granite, gneiss and metamorphic rocks.|12-JUL-16
30280|Browns Range Metamorphics|69426|5|Briefly described|p11:3-5, 10-11|||Crops out along the S and W margins of Browns Range Dome. Over 3000m thick. Parts of this unit are possibly lateral equivalents of the Dead Bullock Formation. Maximum detrital zircon depositional age. A SHRIMP U-Pb zircon age of 2510 +/- 22 Ma (Page et al., 1995) for the protolith is probably (Cross and Crispe, 2007) from an inherited sedimentary source, as also with zircons from a leucogranite dated at c.1970 Ma and 1882 Ma.|<2507 +/- 22 Ma (Page et al., 1995).||||Quartzofeldspathic gneiss, muscovite schist, fine-grained granite, aplite, pegmatite, and metamorphosed arkosic sandstone.|12-JUL-16
30280|Browns Range Metamorphics|69432|6|Mentioned|p17:4|||Tanami Region.||||||12-JUL-16
30280|Browns Range Metamorphics|69587|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1874-1838 Ma (inferred)||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies|
30280|Browns Range Metamorphics|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1874-1838 Ma (Isotopic)||||Metamorphosed feldspathic siliciclastic rocks, minor calc-silicate rock; meta-ultramafic rock; amphibolite to granulite facies|
30280|Browns Range Metamorphics|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1874-1838 Ma.||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|70154|5|Briefly described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 100k_interpgeop_lut.csv. |1838-1874 Ma||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies|
30280|Browns Range Metamorphics|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Aileron Province [?].||||||15-MAY-20
30280|Browns Range Metamorphics|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|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, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv and geochron files.|1874+\-10 to 1838+\-6 Ma (isotopic)|||Overlain unconfomably by Gairdiner Sandstone/Birrindudu Group.|Feldspathic psammite and subordinate psephite; amphibolite to granulite facies; quartzofeldspathic granofels with sparse to abundant pebbles and cobbles; minor banded ironstone, siltstone, and foliated conglomeratic calc-silicate rocks|
30280|Browns Range Metamorphics|71349|5|Briefly described|p723-739|Archean|Archean|Tanami Region, North Australian Craton. Abbreviated to BRM throughout the article. Immature to sub-mature, meta-arkosic rocks with minor quantities of granitic lithic fragments. Lithology elaborated; photographs, photomicrographs. Geochemistry, zircon analyses detailed. Age range from detrital zircon maximum depositional age and age of granite intrusions.|3026 +/- 11 Ma - c.2.5 Ga.|||Is overlain unconformably by Dead Bullock Formation and Gardiner Sandstone.|Mainly metasandstones, occasional interbedded medium- to coarse-grained conglomerates, and less common calc-silicate rocks and BIF. Cut by numerous felsic and mafic-ultramafic intrusions.|
30280|Browns Range Metamorphics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen|Max age 1874+/-10 Ma, min age 1838+/-6 Ma.||||Feldspathic psammite and subordinate psephite; amphibolite to granulite facies.|
30280|Browns Range Metamorphics|72071|4|Described|p1297-1299,1301-1304|Archean|Archean|Crops out over an area of ~100 km2. Clastic detritus sourced from erosion of Mesoarchean granitic source. Experienced greenschist metamorphism at ca. 1.83 Ga (Crispe et al., 2007). Intruded by minor ca. 2.5 Ga granitic to pegmatitic intrusions and mafic-ultramafic rocks that were affected by regional metamorphism that predate ca. 1.83 Ga metamorphic activity.|3.1-2.5 Ga|||Overlain unconformably by Birrindudu Group. Intruded by Browns range dome granite.|Immature quartz-feldspar meta-arkosic sandstones, with minor interbedded conglomerates and semipelitic schists.|01-JUL-19
30280|Browns Range Metamorphics|73089|4|Described|p3, p5-7, p29-30|Paleoproterozoic|Mesoarchean|Exposed in the western and southern margins of the Browns Range Dome. Proposed as a Neoarchean basement inlier. Interpretation of zircon dates remains the subject of debate; inferred depositional ages ranging from Mesoarchean-Neoarchean to Paleoproterozoic. Some authors suggest the c. 2500 Ma population is inherited; thus, the unit could be correlative with Dead Bullock Formation. [Authors equate this unit to the Kairos member as part of the Tanamai Group]. Unconformably overlain by sedimentary rocks of the Paleoproterozoic to Mesoproterozoic Birrindudu Basin.|1885-1865 Ma? 3000-2500 Ma?|||Unconformably overlain by Gardiner Sandstone.|Feldspathic metasandstone, metaconglomerate and muscovite schist, with less common calc-silicate rock and banded iron formation.|
30280|Browns Range Metamorphics|73158|6|Mentioned|p2, p9|||Granites-Tanami Orogen, northwest.|||||Granitic gneisses.|
30280|Browns Range Metamorphics|73159|5|Briefly described|p2, 9|Archaean|Archaean|Northwest Granites-Tanami Orogen.|||||Granitic gneisses.|
38038|Brumby Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Fine to medium grained, rarer coarse to granule sandstone; laminated, brecciated and stromatolitic chert; chert-clast breccia and conglomerate with sandstone matrix; siltstone and shale.||||||
38038|Brumby Formation|65337|3|Fully described|p9 Fig.5, p22 Table 4, pp24-26.|Paleoproterozoic|Paleoproterozoic|Southeast MOUNT DRUMMOND area. 350 - 800 m thick intertidal to supratidal including sabkha, deeper shelf in upper part, deposits. Forms low hills and plains adjacent to main ridges of Carrara Range.|1725 +/- 3 ma to 1658 - 1653 Ma.|Unit in McNamara Group.||Overlies Drummond Formation. Is overlain by Shady Bore Quartzite or Bullrush Conglomerate.|Interbedded fine- to medium-grained, rarer coarse to granule sandstone; laminated, brecciated and stromatolitic chert; chert-clast breccia and conglomerate with sandstone matrix; siltstone and shale dominate upper part.|
38038|Brumby Formation|69433|4|Described|p18:2, 6, 9|Statherian|Statherian|Rawlings et al. (2008); formerly part of the (now obsolete) Musselbrook Formation. Southern succession, Lawn Hill Platform. Absent from the Maloney Creek Inlier. 350-800m thick. Carbonate ramp deposits followed by deeper water (shelf) deposits.||McNamara Group.||Conformably overlies Drummond Formation. Is overlain conformably by Shady Bore Quartzite.|Siltstone, shale, sandstone and granule conglomerate, laminated and stromatolitic chert, dolostone, and chert-clast conglomerate and breccia. Finer lithologies become more abundant up-section.|
38038|Brumby Formation|69673|4|Described|p52 fig 42, p53|||Up to 800m thick. Deposited in carbonate ramp environment.||McNamara Group|||Siltstone, shale, sandstone and granule conglomerate, laminated and stromatolitic chert, dolostone and chert-clast conglomerate and breccia.|
38038|Brumby 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. Unit located in the NT side of the McNamara Group.||McNamara Group||Overlies Drummond Formation and underlies Bullrush Conglomerate and Shady Bore Quartzite.||
38038|Brumby Formation|72527|4|Described|p1,p8, p91, p105-111, p112, p193, p194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Shift in provenance from underlying Drummond Formation. Considered to have been deposited in a mainly shallow marine environment with some deeper marine, low energy facies higher in the formation (Rawlings et al., 2008).|1671+/-12 Ma max dep age|McNamara Group||Conformably overlies Drummond Formation and underlies Shady Bore Quartzite. Considered to be laterally equivalent to Paradise Creek Formation.|Includes massively to thickly bedded, very fine-grained, very well-sorted and well-rounded quartz sandstone. Rounded quartz grains are mantled by interstitial quartz cement. Minor opaques are present (<1 percent).|
38038|Brumby 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 Drummond Formation and underlies Shady Bore Quartzite and is partially equivalent to Fish River Formation and Bullrush Conglomerate.||
38038|Brumby Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Underlain by Drummond Formation. Overlain by Shady Bore Quartzite.||
38038|Brumby Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Unconformably overlain(?) by Shady Bore Quartzite.||
38038|Brumby Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
76872|Bruna Granitic Gneiss|64337|5|Briefly described|p374 Fig. 1|Paleoproterozoic|Paleoproterozoic|See also variations Bruna Granite (p375, p392) and Bruna Granite Gneiss (p375, p392).[Formal name Bruna Gneiss].|Age range: c. 1770-1730 Ma granitoids.|||||
76872|Bruna Granitic Gneiss|66767|4|Described|p58, p60|||Harts Range area, Aileron Province. Acted as a major detachment during the Paleozoic (Bruna Detachment Zone). Sm-Nd isochron age from a garnet-hornblende migmatite.|449 +/- 10 Ma (Mawby et al., 1999).|||Structurally, is overlain by Alooarjara Metamorphics and overlies Entia Gneiss Complex.|A flat-lying, sheet-like body of highly-deformed megacrystic granite up to 400m thick; typically mylonitic. Has mid to upper amphibolite facies, high-strain zones up to 100m thick at the upper and lower surfaces.|
76872|Bruna Granitic Gneiss|68316|6|Mentioned|p778, p778 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
76872|Bruna Granitic Gneiss|68697|5|Briefly described|v, p44|Statherian|Statherian|Aileron Province, Arunta Region. Intersected in drillcore in the far SE of ILLOGWA CREEK map area.|c.1750 Ma (Carson et al., 2010).||||A [metamorphosed] K-feldspar-phyric granite.|
76872|Bruna Granitic Gneiss|69383|5|Briefly described|p4 Table 1, p58, pviii|Statherian|Statherian|Arunta region. See also Bruna Gneiss p58-63. LA-ICPMS U-Pb geochronology analyses. 2 samples. Crystallisation age.|1747+/-11 Ma|||||
76872|Bruna Granitic Gneiss|69417|5|Briefly described|p2:5|Statherian|Statherian|Aileron Province.|1760-1740 Ma.|||||12-JUL-16
76872|Bruna Granitic Gneiss|69427|5|Briefly described|p12:3, 30, 36-37, 47|Statherian|Statherian|Aileron Province. A flat-lying, sheet-like body of highly-deformed megacrystic granite, 50-400m thick. Separates the Entia Gneiss Complex from the structurally overlying Harts Range Metamorphic Complex. The high-strain fabrics along this unit's margins developed as the Harts Range Metamorphic Complex moved S over the Entia Gneiss Complex at c.450 Ma (Alice Springs Orogeny). Several ages are given, all between c.1756-1745 Ma.|1747 +/- 2 Ma (Cooper et al., 1988).|||Overlies Entia Gneiss Complex.|Deformed, hornblende-bearing, coarsely porphyritic granodiorite and an equigranular granitic phase. Typically mylonitic, but locally preserves magmatic textures in low-strain domains.|12-JUL-16
76872|Bruna Granitic Gneiss|69444|5|Briefly described|p29:2-3, 7|Paleoproterozoic|Paleoproterozoic|Formerly a unit in Harts Range Group. Later recognised as part of the basement (to the now Harts Range Metamorphic Complex). Also appears as Bruna Granite Gneiss in Fig.29.4. Mid-to upper-amphibolite facies metamorphism during Rodingan Event at 449 +/- 10 Ma.|1747 +/- 3 Ma (Buick et al. 2005, Maidment 2005).|Harts Range Group.||||12-JUL-16
24775|Buchanan Hills beds|36335|6|Mentioned|Map legend|early Tertiary|Late Cretaceous|Late Cretaceous to Early Tertiary||||||
24775|Buchanan Hills beds|45148|2|Defined|p20|Tertiary|Ordovician|Also mentioned p18.||||||02-AUG-06
24775|Buchanan Hills beds|60684|6|Mentioned|p50 Appendix|||Overlie Point Wakefield beds and unconformably overlie parts of Lothari Hill Sandstone.||||||02-AUG-06
24775|Buchanan Hills beds|62637|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fine to coarse grained, poorly sorted subangular sandstone.||||||23-DEC-09
24775|Buchanan Hills beds|65333|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Of Wiso Basin. Unconformably overlies Lake Surprise Sandstone. Poorly sorted, angular to rounded, fine to coarse grained terrestrial sandstone. ||||||
24775|Buchanan Hills beds|65334|5|Briefly described|Map Legend|Paleogene|Cretaceous|Of Wiso Basin. Maximum age not certain. Unconformably overlies Lake Surprise Sandstone. Poorly sorted, angular to rounded, fine to coarse grained terrestrial sandstone. ||||||
24775|Buchanan Hills beds|68734|6|Mentioned|p221 Fig.3|Cretaceous|Cretaceous|||||||
24775|Buchanan Hills beds|69447|6|Mentioned|p32:4-5|Cretaceous|Cretaceous|||||Unconformably overlies Hooker Creek Formation or Lothari Hill Sandstone.||12-JUL-16
37731|Buddycurrawa Volcanics|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Benmara Group.  Age: ~1725Ma.||||||07-NOV-08
37731|Buddycurrawa Volcanics|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Benmara Group. Ferruginous coarse sandstone, massive and brecciated trachyte, poorly sorted immature lithic sandstone and pebble conglomerate, mature sandstone, ferruginous siltstone and fine sandstone.||||||
37731|Buddycurrawa Volcanics|65337|2|Defined|pp88-89.|Paleoproterozoic|Paleoproterozoic|New name. Northwest MOUNT DRUMMOND area. Up to 300 m of braided fluvial, shallow lacustrine and/or marine deposits, lava flows and marginal ephemeral alluvial and debris flows. Has high Al, K and Zr. Strong magnetic and radiometric responses.||Unit in Benmara Group.||Overlies Breakfast Sandstone. Is overlain by Bowgan Sandstone and, locally, Crow Formation.|Ferruginous coarse sandstone, massive and brecciated trachyte, poorly sorted immature lithic sandstone and pebble conglomerate, mature sandstone, ferruginous siltstone and fine sandstone; minor but distinctive stromatolitic chert.|
37731|Buddycurrawa Volcanics|69433|4|Described|p18:2, 4-5|Statherian|Statherian|Northern succession, Lawn Hill Platform. Up to 300m thick. Geochemically distinct from Peters Creek Volcanics. ||Benmara Group.||Conformably overlies Breakfast Sandstone. Is overlain, probably unconformably, by Bowgan Sandstone and Crow Formation. Correlative of Plain Creek Formation(?).|Basal ferruginous coarse sandstone, massive and brecciated (peperitic) trachyte, poorly sorted immature lithic sandstone and pebble conglomerate, mature sandstone, ferruginous siltstone and fine sandstone; minor stromatolitic chert.|11-JUL-16
37731|Buddycurrawa Volcanics|69673|6|Mentioned|p52 fig 42, p53 |||Up to 300m thick.|||||Ferruginous sandstone, coherent trachyte, debris flow sandstone and conglomerate, mature sandstone, ferruginous siltstone/fine sandstone and minor stromatolitic chert.|
37731|Buddycurrawa Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the west of the South Nicholson Basin.||Benmara Group||Overlies Breakfast Sandstone and shown as underlying Bowgan Sandstone.||
37731|Buddycurrawa Volcanics|72527|4|Described|p1, p7, p8, p86-90, 192, 196.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. This unit is poorly exposed and deeply weathered, and exhibits elevated REE abundances (D. Champion pers. comm.). Max thickness of 300m inferred. Type locality shown as 136.9228dE 18.15186dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios. Although sample described as high-K felsic volcanic (trachyte), the varied morphology, poor quality and corroded nature of the zircons in this sample are interpreted to represent inherited grains.|1662 +/- 18 Ma maximum depositional age|Benmara Group||Conformably overlies Breakfast Sandstone. Unconformably underlies [Caufield beds?], Bowgan Sandstone, Crow Formation, Wild Cow Subgroup. Possible correlation with McNamara Group.|Comprises basal ferruginous sandstone unit, overlain by a mixed interval of coherent trachyte, debris flow sandstone and conglomerate, mature sandstone, ferruginous siltstone/fine sandstone and minor, but distinctive, stromatolitic chert.|
37731|Buddycurrawa Volcanics|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the west part of the South Nicholson Basin||Benmara Group||Overlies Breakfast Sandstone and shown as unconformably underlying South Nicholson Group.||
37731|Buddycurrawa Volcanics|72919|6|Mentioned|p1, p5, p16, p93|Statherian|Statherian|An age range of ca. 1660-1630 Ma was reported by Carson et al. (2020). Previously included in the now defunct Benmara beds.|ca. 1660-1630 Ma|Benmara Group||Conformably underlain by Breakfast Sandstone.|Includes poorly-sorted ferruginous sandstone.|
37731|Buddycurrawa Volcanics|73042|6|Mentioned|p4|Statherian|Statherian|South Nicholson Basin region, Isa Superbasin. Geochronology is mixed U-Pb zircon igneous crystallisation age and Rb-Sr glauconite age.|ca 1662-1631 Ma|Benmara Group||Underlain by Breakfast Sandstone.||
23433|Buffallo Fly Hill Granodiorite|39889|6|Mentioned|Fig.2|||||||||
29219|Bullion Schist|22524|6|Mentioned|p41|||||||||
29219|Bullion Schist|23733|5|Briefly described|p28|Paleoproterozoic|Paleoproterozoic|See also p32 Fig. 19, p 34 Fig.20.||||||07-NOV-08
29219|Bullion Schist|23809|5|Briefly described|p44, p27 Fig. 25|Proterozoic|Proterozoic|Psammo-pelitic schist.  Intruded by Bean Tree and Ooralingie Granites, and the Barrow Creek Granitic Complex.  Age: >1819Ma. Geological Province: Arunta Province.  Probably correlates with Ooradidgee and Flynn Groups.  see also p41 Tb. 5.||||||10-NOV-04
29219|Bullion Schist|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: >1805Ma.  Geological Province: Arunta Province.||||||07-NOV-08
29219|Bullion Schist|24172|6|Mentioned|p75 Appendix|||Possible correlative of Warramunga Formation.||||||
29219|Bullion Schist|42643|2|Defined|p48|Paleoproterozoic||Reserved. Definition card.||||||07-NOV-08
29219|Bullion Schist|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Metamorphosed pelite, feldspathic/lithic and quartz arenite, quartz mica schist with andalusite, porphyritic felsic volcanics, amphibolite. Geological Province: Arunta Inlier.||||||07-NOV-08
29219|Bullion Schist|50369|6|Mentioned|p17.2|||||||||
29219|Bullion Schist|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metamorphosed pelite, feldspathic/lithic and quartz arenite, quartz-mica schist with andalusite, porphyritic felsic volcanics and amphibolite. In Tennant Creek region.||||||07-NOV-08
29219|Bullion Schist|64735|4|Described|p205 Fig1, p206 Fig2, p211, p212, p216|Orosirian|Orosirian|Barrow Creek area, Aileron Province. Tentatively correlated with Warramunga Formation by Haines et al (1991), but this correlation now discounted; correlated with Ooradidgee Group, Lander Package, Tanami Group by this publication; unknown structural and stratigraphic relationships;  1834-1844 Ma max deposition age using SHRIMP RG 207Pb/206Pb on detrital zircons from an intercalation of psammite (this publication); max depositional age from youngest detrital zircons: 1824+/-10 Ma; similar lithologies and deformation to Lander Package; intruded by Barrow Creek Igneous Complex granites at 1809+/- 5 Ma and 1806 +/-6 Ma.|Max depositional age 1824+/-10 Ma.|||Intruded by Ooralingie Granite, Beantree Granite; interpreted to underlie Strzeleckie Volcanics.|A metapelitic sedimentary package.|20-APR-12
29219|Bullion Schist|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
29219|Bullion Schist|65338|6|Mentioned|p7.|||Aileron Province. Deformed during the Stafford Event and prior to deformation in the Hatches Creek Group. Correlative of Lander Rock Formation, at least in part, of Tennant Region.||||||
29219|Bullion Schist|66767|6|Mentioned|p57|||Aileron Province.||||||
29219|Bullion Schist|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Metamorphosed pelite, feldspathic/lithic and quartz arenite, quartz-mica schist with andalusite, porphyritic felsic volcanics and amphibolite.|
29219|Bullion Schist|69418|6|Mentioned|p3:21|||Arunta Region. Hosts Sn-Ta mineralisation at the Barrow Creek pegmatite field (described).||||||12-JUL-16
29219|Bullion Schist|69424|5|Briefly described|p9:4, 34|||Aileron Province, Arunta Region. Experienced bimodal magmatism and folding during the c.1800 Ma Stafford Event.||||Correlative of Ooradidgee Group.||12-JUL-16
29219|Bullion Schist|69425|5|Briefly described|p10:4, 6, 8, 10|||Aileron Province, Arunta Region. Arguably more distal equivalents of Ooradidgee Group sedimentary units in the contiguous Davenport Province. Possible equivalent to Rooneys Formation. Detrital zircon spectrum is comparable to that of Warnes Sandstone Member (Kurinelli Sandstone). Folded during the Stafford Event, contemporaneous with the Murchison Event in the Davenport Province.||||Correlative of the Ooradidgee Group.||12-JUL-16
29219|Bullion Schist|69427|5|Briefly described|p12:4, 6, 13, 25, 44, 56, 59, 62|||Haines et al. (1991). Aileron Province. Hosts the Home of Bullion Cu(-Pb-Zn) deposit, and pegmatite- and quartz vein-hosted tin, tantalum and tungsten prospects. A number of W (+/- Sn, Ta) prospects occur in pegmatities and quartz veins cutting this unit in the Barrow Creek region. May transition laterally into Ooradidgee Group. Felsic volcanic rocks 12km NW of Barrow Creek roadhouse, mapped as part of this unit by Haines et al. (1991), are now assigned to the Strzeleckie Volcanics. Metamorphism or fluid flow event at 1587 +/- 55 Ma (SHRIMP U-Pb, Smith, 2001).||||Is intruded by Barrow Creek Granite Complex and Bean Tree Granite.|Thinly bedded metapelitic rock: quartz-muscovite(-biotite)(-andalusite) schist; metasandstone (typically micaceous); minor mafic amphibolite. Quartz-tourmaline rock occurs near granite contacts. Generally upper greenschist facies.|12-JUL-16
29219|Bullion Schist|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1833+/-11 Ma (MDA: SHRIMP)||||Metapelite.|
29219|Bullion Schist|72378|4|Described|iii,p1,22,27-28|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Claoue-Long et al .,2008b reported a SHRIMP U-Pb zircon maximum depositional age of 1833 ¿ 11 Ma. Zircon provenance age spectra is a direct correlative with the Lander Rock Formation. The intrusive Ooralingie and Bean Tree granites (c. 1806 Ma; see p22 this study) provide a minimum depositional age of Bullion Schist sedimentary protolith. LA-ICP-MS insitu muscovite geochronology of NTGS BC15MVM022 (mineralised massive sulfide zone within andalusite-biotite-quartz schist) yielded the following interpretive results: a)andalusite growth between 1813+\-20 Ma (207Pb/206Pb )and 1762+\-14 Ma (207Pb/206Pb); and b) fluid infiltration and sulfide growth or deformation at 1778+\-10 Ma (207Pb/206Pb).||||Overlain conformably by Strzeleckie Volcanics. Correlable with Lander Rock Formation. Intruded by Ooralingie and Bean Tree granites.|Thinly-bedded metamudstone and metasandstone with minor mafic amphibolite.|
29219|Bullion Schist|72711|6|Mentioned|p2.|Orosirian|Orosirian|Includes the 'Home of Bullion' Cu-Zn-Pb-Ag-Au VAMS deposit, East of Barrow Creek.|c. 1830 Ma.||||Includes schist.|
29219|Bullion Schist|73592|5|Briefly described|iii, p2-5, 8-10, Appendix A2|Paleoproterozoic|Paleoproterozoic|Aileron Province. Hosts the Home of Bullion Cu-Pb-Zn-(+/- Ag-Au) VMS deposit. Minimum depositional age given by intrusions dated 1823 +/- 9 Ma (Yang et al. in prep). Minimum mineralisation age is 1813 +/- 10 Ma (monazite growth: Reno et al., 2019). Intracontinental basin deposits. Mineralisation described in detail: photomicrographs. Tabulated whole-rock geochemical analyses of 30 samples in Appendix A2.|1833 +/- 11 Ma (MDA: Claoue-Long et al., 2008).|||Likely correlative of Lander Rock Formation.|Thinly bedded metamudstone (mica schists), minor metasandstone, and mafic amphibolite (basalt to basaltic andesite protoliths). Lower greenschist facies; multiply deformed.|
26436|Bullo River Sandstone|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|32660|5|Briefly described|Table 6|||||||||
26436|Bullo River Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Reddish brown quartz sandstone, and conglomerate.||||||02-DEC-04
26436|Bullo River Sandstone|32701|4|Described|Table 1|||Adelaidean||||||
26436|Bullo River Sandstone|32728|6|Mentioned|p16|||||||||
26436|Bullo River Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|33377|5|Briefly described|Table 2|||||||||
26436|Bullo River Sandstone|36473|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26436|Bullo River Sandstone|37462|4|Described|Table 4.VI|||See also Fig.4.13.||||||
26436|Bullo River Sandstone|45112|5|Briefly described|Table 3|||||||||
26436|Bullo River Sandstone|48938|2|Defined|p54|Proterozoic|Proterozoic|?Adelaidean||||||
26436|Bullo River Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Includes Black Point Sandstone Member. Unconformably overlies Shoal Reach Formation. Unconformably overlain by Bucket Spring Member. Quartz sandstone, conglomerate.||||||23-JUL-04
26436|Bullo River Sandstone|60682|4|Described|p17|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Shoal Reach Formation. Overlain by Bucket Spring Member. Max. Thickness: >320m. Geological Province: Wolfe Creek Basin.||||||
26436|Bullo River Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Includes Black Point Sandstone Member. Quartz sandstone, conglomerate||||||
26436|Bullo River Sandstone|68733|5|Briefly described|p177 Fig.2, p183|Cryogenian|Cryogenian|Victoria Basin.||Basal unit of the Duerdin Group.|Includes Black Point Sandstone Member (basal subunit).|Unconformably overlies Shoal Reach Formation.||05-DEC-17
26436|Bullo River Sandstone|69437|6|Mentioned|p22:4-5|Cryogenian|Cryogenian|||||||12-JUL-16
26436|Bullo River Sandstone|69442|4|Described|p27:1-2, 3 Tb.27.1|||Wolfe Basin. Assigned to Duerdin Group by Dunster et al. (2000). Restricted to  620 km2 of inaccessible country in C and SW AUVERGNE map area. Over 320m thick. Depositional environment not determined; possibly fluvial.||Duerdin Group.|Black Point Sandstone Member.|Overlies Shoal Reach Formation (Auvergne Group) mostly dis/unconformably; gradational at one location.|Red-brown to maroon quartz sandstone, typically cross-bedded, poorly sorted; conglomerate.|12-JUL-16
26436|Bullo River Sandstone|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|300m thick.||Duerdin Group|Includes Black Point Sandstone Member||Quartzose sandstone.|
26436|Bullo River Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|Includes Black Point Sandstone Member||Quartz sandstone, conglomerate.|
26436|Bullo River Sandstone|71080|6|Mentioned|p25|||Of Victoria Basin. Higher stratigraphic level than Jasper Gorge Formation.|||Includes Black Point Sandstone Member.|||
26436|Bullo River Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
26436|Bullo River Sandstone|73083|6|Mentioned|p8|Neoproterozoic|Neoproterozoic||||||Includes red beds.|
38039|Bullrush Conglomerate|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. Polymictic granule, pebble and cobble conglomerate: clasts of quartzite, quartz sandstone, quartz, chert, brown porphyritic rhyolite and claystone in lithic sand-granule matrix.||||||
38039|Bullrush Conglomerate|65337|3|Fully described|p9 Fig.5, p21, pp26-27.|Paleoproterozoic|Paleoproterozoic|East-central MOUNT DRUMMOND area. 50 - 500 m of mainly subaerial alluvial fan to fan delta deposits. Clasts suggest rapid erosion of a lower McNamara Group terrane.The puzzling apparent superposition of several contrasting facies may be due to faulting.||Unit in McNamara Group.||Unconformably overlies Top Rocky Rhyolite and Drummond Formation. Is overlain by Plain Creek Formation.|Polymict granule, pebble and cobble conglomerates, cross-bedded sandstone; stromatolitic chert and chert-clast conglomerate, fine-grained lithic sandstone and siltstone.|
38039|Bullrush Conglomerate|69433|4|Described|p18:2, 6, 9-10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 50-500m thick. Contains a variety of sedimentary structures, reflecting deposition in subaerial alluvial fans building out into marine waters.||McNamara Group.||Unconformably overlies Top Rocky Rhyolite and Drummond Formation. Is overlain conformably by Plain Creek Formation. Correlated with Shady Bore Quartzite.|Polymictic granule, pebble and cobble conglomerate, massive or crudely bedded, largely clast supported in a matrix of lithic sand to granules; alternating with white, silicified, fine- to very coarse-grained cross-bedded sandstone.|12-JUL-16
38039|Bullrush Conglomerate|69673|4|Described|p52 fig 42,p53|||Up to 500m thick. Deposited in subaerial alluvial fans.||McNamara Group|||Polymictic granule, pebble and cobble conglomerate, alternating with cross bedded sandstone with minor carbonate rocks and siltstone.|
38039|Bullrush Conglomerate|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin.||McNamara Group||Overlies Brumby Formation and underlies Shady Bore Quartzite.||
38039|Bullrush Conglomerate|72527|4|Described|p3, p8, p119-131, p193, p194, p197.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Previously included in Maloney Creek Formation, then Musselbrook Formation (both now obsolete). Up to 500 m thick. Uncertain  stratigraphic affinity.Two samples dated from conglomerate. Second sample is specifically rhyolite clasts: age 1723+/-6 Ma which confirms source as Top Rocky Rhyolite. Displays remarkably similar age spectra to Caulfield beds, Bowgan Sandstone, and Crow Formation. Type locality near sample site shown as 137.6299dE 18.43856dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios.|1646+/-5 Ma max dep age.|McNamara Group||Conformably overlain by Plain Creek Formation. Unconformably overlies Top Rocky Rhyolite. Shown as laterally equivalent to Shady Bore Quartzite.|Crudely bedded polymict granule, pebble to cobble conglomerate, with interbedded cross-bedded quartz and lithic sandstone, siltstone. Includes carbonate interbeds with relic stromatolites,  qtz, qtzite, ssst, chert, clayst, rhyolite clasts.|
38039|Bullrush Conglomerate|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 and equivalent to Brumby Formation and underlies and equivalent to Shady Bore Quartzite.Partially laterally equivalent to Walford Dolomite and Fish River Formation.||
38039|Bullrush Conglomerate|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Equivalent to Shady Bore Quartzite and Plain Creek Formation.||
38039|Bullrush Conglomerate|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||McNamara Group||Overlain by Plain Creek Formation.||
23442|Bunghara Metamorphics|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Narwietooma Suite. Age: ~1880Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
23442|Bunghara Metamorphics|24608|6|Mentioned|p986|||||||||
23442|Bunghara Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Narwietooma Metamorphic Complex.||||||07-NOV-08
23442|Bunghara Metamorphics|43503|2|Defined|6,15, 75|||||||||
23442|Bunghara Metamorphics|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.|
23442|Bunghara Metamorphics|49831|5|Briefly described|Fig.1 P15|||Name reserved.||||||
23442|Bunghara Metamorphics|50369|5|Briefly described|p1.3, 3.1, 12.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Narwietooma Suite. Age: 1880 +/- 5Ma (Sm-Nd).||||||07-NOV-08
23442|Bunghara Metamorphics|67565|6|Mentioned|p13.|||The westernmost outcrops previously assigned to this unit, in the Hermannsburg 1:250 000 sheet, are now included in the Yaya Metamorphic Complex.||||||
23442|Bunghara Metamorphics|69427|5|Briefly described|p12:17-18, 29, 32|||Aileron Province. Meta-igneous and subordinate metasedimentary rocks, cropping out immediately N of the Redbank Thrust, S of Mount Hay and Mount Chapple. Peak metamorphism is dated (U-Th-Pb chemical dating: Biermeier et al., 2003) at 1767 +/- 9 Ma (?Yambah Event).||Narwietooma Metamorphic Complex.|||Mafic to intermediate granulite; lesser felsic migmatite; local garnet-sillimanite-biotite metapelite and metapsammite.|12-JUL-16
23442|Bunghara Metamorphics|69428|6|Mentioned|p13:7-8|Paleoproterozoic|Paleoproterozoic|Outcrops 15 km SE of Papunya, previously assigned to this unit in HERMANNSBURG map area (Warren and Shaw, 1995), are now included in the Inyalinga Granulite.||||||12-JUL-16
23442|Bunghara Metamorphics|69932|6|Mentioned|p302-303, 306-307|||Central Province, Arunta Inlier. Sm-Nd data tabulated. Presented as Bunghara Granulite on p307.|1880 Ma.||||Banded felsic granulite with dacitic composition.|
23442|Bunghara Metamorphics|72894|6|Mentioned|p19|||||Narwietooma Metamorphic Complex|||Dominated by mafic to intermediate granulite and lesser felsic migmatite|
24791|Bungle Bungle Dolomite|22440|5|Briefly described|p4,5|Stenian|Stenian|Age 1200- 1000Ma.||||||02-AUG-06
24791|Bungle Bungle Dolomite|22496|6|Mentioned|p10||Neoproterozoic|Mapped as Eliot Range Dolomite in the Ruby Plains sheet area||||||
24791|Bungle Bungle Dolomite|22716|5|Briefly described|table4, p236|Calymmian|Calymmian|May be equivalent to part of the Birrindudu Group.||||||
24791|Bungle Bungle Dolomite|22754|5|Briefly described|p11 Tb. 3|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||
24791|Bungle Bungle Dolomite|22764|4|Described|Table1,p7||Carpentarian|Probably conformable on Mount Parker Sandstone and unconformable beneath Wade Creek Sandstone.||||||01-FEB-10
24791|Bungle Bungle Dolomite|22899|6|Mentioned|86|||||||||
24791|Bungle Bungle Dolomite|23314|5|Briefly described|333|||||||||
24791|Bungle Bungle Dolomite|23621|6|Mentioned|p56 Appendix|||||||||
24791|Bungle Bungle Dolomite|23809|5|Briefly described|p47 Fig. 42|Proterozoic|Proterozoic|Geological Province: Osmond Basin.  Correlates with Limbunya Group, misspelt as Lumbunya in text, (Birrindudu Basin), Namerinni Group (Ashburton Province) and McArthur Group (McArtgur Basin).||||||
24791|Bungle Bungle Dolomite|24173|5|Briefly described|p24|Mesoproterozoic|Mesoproterozoic|Of the Osmond Range sequence. Previously included Eliot Range Dolomite||||||02-AUG-06
24791|Bungle Bungle Dolomite|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolarenite, dololutite, and dolorudite, and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone and mudstone, and stromatolitic chert.   Geological Province: Osmond Basin.||||||
24791|Bungle Bungle Dolomite|28255|6|Mentioned|p11|||Age is probably Adelaidean but may be as old as Carpentarian. East Kimberley area (WA).||||||08-JUN-05
24791|Bungle Bungle Dolomite|29805|6|Mentioned|p9|||||||||
24791|Bungle Bungle Dolomite|29809|6|Mentioned|p418|||||||||
24791|Bungle Bungle Dolomite|29813|4|Described|Table 2|||||||||
24791|Bungle Bungle Dolomite|29818|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24791|Bungle Bungle Dolomite|30895|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian and/or Adelaidean||||||
24791|Bungle Bungle Dolomite|31393|6|Mentioned|Pl.25|||||||||
24791|Bungle Bungle Dolomite|32172|6|Mentioned|p9|||Refers Dow and Gemuts(1969) & Sweet et al.(1971)||||||02-AUG-06
24791|Bungle Bungle Dolomite|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|32660|5|Briefly described|Table 6|||||||||
24791|Bungle Bungle Dolomite|32728|5|Briefly described|p42|||Mention p16.||||||02-AUG-06
24791|Bungle Bungle Dolomite|33374|6|Mentioned|p6|||Correlation||||||
24791|Bungle Bungle Dolomite|35120|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|35950|6|Mentioned|p311|||||||||
24791|Bungle Bungle Dolomite|36048|6|Mentioned|p380|||||||||
24791|Bungle Bungle Dolomite|36532|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24791|Bungle Bungle Dolomite|36551|6|Mentioned|p22|||||||||
24791|Bungle Bungle Dolomite|36885|4|Described|p177|||||||||
24791|Bungle Bungle Dolomite|36898|5|Briefly described|p186|||||||||
24791|Bungle Bungle Dolomite|37371|6|Mentioned|p367|||||||||
24791|Bungle Bungle Dolomite|37462|4|Described|Table 4.V|||||||||
24791|Bungle Bungle Dolomite|38243|6|Mentioned|Fig.2|||||||||
24791|Bungle Bungle Dolomite|38988|6|Mentioned|Fig.4|||||||||
24791|Bungle Bungle Dolomite|43631|6|Mentioned|p24|||||||||
24791|Bungle Bungle Dolomite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
24791|Bungle Bungle Dolomite|44155|4|Described|p251-252|||Type area in Osmond Range area. At least 1000m thick. Contains stromatolites. Probable part correlative of Tawallah and McArthur Groups in McArthur Basin.||||Overlies Mount Parker Sandstone conformably. Is overlain unconformably by Wade Creek Sandstone. Equivalent to Talbot Well Formation.|Banded and brecciated cherts, silicified oolite, bouldery cherty ironstone, dolomite and dolomitic shale; several quartz sandstone beds up to 30m thick.|18-MAY-15
24791|Bungle Bungle Dolomite|44317|4|Described|Table 2||Carpentarian|||||||
24791|Bungle Bungle Dolomite|44318|14|Not recorded|map legend|||Adelaidean or Carpentarian.||||||
24791|Bungle Bungle Dolomite|44324|14|Not recorded|p.10||Neoproterozoic|Tb.2. (Upper Proterozoic).||||||
24791|Bungle Bungle Dolomite|44325|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic. Defn on Tech.File SE/52-6.||||||
24791|Bungle Bungle Dolomite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
24791|Bungle Bungle Dolomite|45047|2|Defined|p76|early Adelaidean|late Carpentarian|Early Adelaidean or Late Carpentarian.||||||
24791|Bungle Bungle Dolomite|45112|6|Mentioned|p17|||||||||
24791|Bungle Bungle Dolomite|45140|2|Defined|p12-14, p39-40, p42, p58-60, p74|||See also Appx.p32. Dow and Gemuts (1969). Mapped as Kearney Beds by Casey and Wells (1964). Named after Bungle Bungle outcamp on Turner station. Unnamed basin NW of Birrindudu Basin. Type section is in Osmond Range, Dixon Range sheet area. Forms low mounds. 300m thick. Silicified stromatolitic dolomite contains microfossils.||||Conformably overlies Mount Parker Sandstone. Is overlain unconformably by Wade Creek Sandstone. Probable equivalent to Talbot Well Formation (Birrindudu Group).|Mainly dolomite, dolomitic shale; banded chert, brecciated chert, silicified oolite, bouldery chert ironstone containing possible stromatolitic structures, minor lithic arenite; local micaceous greywacke, siltstone and shale.|
24791|Bungle Bungle Dolomite|46861|6|Mentioned|p9|||||||||
24791|Bungle Bungle Dolomite|46864|5|Briefly described|p40|||||||||
24791|Bungle Bungle Dolomite|48938|6|Mentioned|p76|||Equiv. Limbunya Group||||||
24791|Bungle Bungle Dolomite|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Mesoproterozoic|Geological Province: Osmond Basin.||||||07-FEB-11
24791|Bungle Bungle Dolomite|61732|6|Mentioned|p26|||||||||07-FEB-11
24791|Bungle Bungle Dolomite|63866|5|Briefly described|p130, p132, p137|||Osmond Basin.||||Unconformably overlies the Kimberley Group.|Dolomite, stromatolitic chert, sandstone and siltstone.|
24791|Bungle Bungle Dolomite|64104|6|Mentioned|p63 Fig.1, p75|Neoproterozoic|Neoproterozoic|Says 'Subsequently named Eliot Range Formation' [?]. Osmond Basin. Part of Osmond Range succession. Likely source of clasts in Fargoo Formation. [This article changes the age of a number of units, including this one, without explanation. Error in Figure 10?]||||||19-MAY-15
24791|Bungle Bungle Dolomite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert.||||||09-DEC-08
24791|Bungle Bungle Dolomite|65074|6|Mentioned|p353|||Osmond Range succession in the Halls Creek Orogen.||||Correlated with Gardiner Sandstone.||
24791|Bungle Bungle Dolomite|68244|6|Mentioned|p668|||Erosion and remobilisation of carbonate leading to abundant carbonate framework clasts and high carbonate content of lower Duerdin Group glaciogenic units (Fargoo and Mountain Valley Fms; Corkeron 2008).||||||
24791|Bungle Bungle Dolomite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Osmond Basin|Depositional age: 867+/-2 Ma SHRIMP||Includes 3 unnamed members||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert; members also include quartz sandstone|30-JUL-15
24791|Bungle Bungle Dolomite|69165|4|Described|100k_interpgeop_lut.csv|Neoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv, GA_geochron.csv.|867 Ma||||Dolarenite, dololutite, dolorudite, chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone and stromatolitic chert. Thin to medium bedded, fine to medium grained quartz sandstone.|
24791|Bungle Bungle Dolomite|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Halls Creek Orogen. Of Osmond Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|2500-1600 Ma (Inferred)||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, quartz sandstone and stromatolitic chert|
24791|Bungle Bungle Dolomite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1797 Ma||||Dolarenite, dololutite, dolorudite, chert breccia; commonly stromatolitic, minor dolomuitic sandstone, siltstone, mudstone and chert. Thin to medium bedded fine to medium grained quartz sandstone.|
24791|Bungle Bungle Dolomite|70812|5|Briefly described|p30, p43|Neoproterozoic|Paleoproterozoic|Highly prospective in places for Pb-Zn.||||||
24791|Bungle Bungle Dolomite|71267|4|Described|GEOL_LUT_CSV files|Neoproterozoic|Paleoproterozoic|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). 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.|1797-541 Ma (inferred)||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, quartz sandstone, siltstone, mudstone, and stromatolitic chert|
24791|Bungle Bungle Dolomite|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic|Osmond Basin.|||||Dolarenite, dololutite, and dolorudite and chert breccia; commonly stromatolitic; minor dolomitic sandstone, siltstone, mudstone, and stromatolitic chert.|
24791|Bungle Bungle Dolomite|73255|6|Mentioned|p534 Fig.2, p546, p548 Fig.12|Tonian|Tonian|Contains Collenia frequens stromatolite fossils.|ca 1128 Ma|Osmond Range Succession||Overlies the Mount Parker Sandstone, underlies the Wade Sandstone.||
42077|Bunkers Granodiorite|23809|5|Briefly described|p12-13|||Of the Inningarra Suite.  Medium to coarse granodiorite, with noticeably deformed feldspars and quartz.  In the region of Bunkers Hill open-cut. See also Bunkers granodiorite p10 and Bunkers Tonalite p6, same sample number.||||||02-APR-15
77877|Burangoo Sandstone|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Paleoproterozoic|South Nicholson Basin. Detrital [?zircon] ages: 1600 +/-21 Ma (Magee et al, in prep).||South Nicholson Group|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles to 1cm; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|67539|5|Briefly described|p14|||North of the Elizabeth Creek fault. Raised to formation rank.||Of the South Nicholson Group.||Overlain by the Wallis Siltstone. Underlain by the Pandanus Siltstone.||
77877|Burangoo Sandstone|68146|4|Described|p2, p6, p20-27, p29, p196-197, p211|||South Nicholson Region. Also given 1591 +/- 10 Ma MDA from rocks mistakenly thought to have been Constance Sandstone. Whole-rock Sm-Nd isotopic data tabulated.|1565 +46/-45 Ma max. deposition age.|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|White to,light grey, thick-bedded, mainly fine- to medium-grained felspathic quartz sandstone; some coarser-grained laminae; cross-bedded.|
77877|Burangoo Sandstone|68575|4|Described|p3, p6-7, p18-26, p125, p128|||South Nicholson Basin. Formerly part of Constance Sandstone. Shows significantly different provenance from that of Hedleys Sandstone.|1602 +/- 30 Ma (maximum depositional age).|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|Thick-bedded, cross-bedded, fine- to very coarse-grained quartz sandstone with scattered granules and laminae of granules.|
77877|Burangoo Sandstone|69591|4|Described|p52-54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Predominantly fluvial. Another MDA given is 1600 +/- 21 Ma.|1566 +/- 46 Ma (MDA: Carson et al., 2011).|Wild Cow Subgroup.||Overlies Pandanus Formation. Is overlain by Wallis Formation.|Thick-bedded, medium- to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles to 1cm; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|71369|3|Fully described|p1, p6, p8-9, p12-19, p47-49|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Previously (Roberts et al., 1963) undifferentiated Constance Sandstone; later (Rawlings et al., 2008) the Burangoo Sandstone Member of Constance Sandstone. Upgraded in this study (Sweet, 2017) to Formation status. 50-320m thick. The type section is near Burangoo Waterhole on the Nicholson River, where it is 320m thick. Mainly fluvial deposits.||Wild Cow Subgroup.||Overlies Pandanus Formation ?unconformably and Lawn Hill Formation locally. Is overlain by Wallis Formation and locally by Schultz Sandstone Member.|Basal white to light-grey, thick- and very thick-bedded, fine- to medium-grained quartz sandstone; coarsening-up to very coarse grained and granule-rich sandstone, before fining-upwards to fine- to medium-grained sandstone.|
77877|Burangoo Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1566 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
77877|Burangoo Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Wallis Formation. Underlain by Pandanus Formation.|Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Wallis Formation. Underlain by Pandanus Formation.|Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|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 Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebbles; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification.|
77877|Burangoo Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|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 Wild Cow Subgroup.|||Thick-bedded, medium to coarse-grained, sublithic to quartzose sandstone, with scattered grains and layers of granules and pebble; strongly trough cross-bedded and also planar cross-beds, planar beds and hummocky cross-stratification|
77877|Burangoo Sandstone|72526|5|Briefly described|p8 Fig.1.3|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||?Wild Cow Subgroup, South Nicholson Group||Overlies Pandanus Formation and underlies Wallis Formation.||
77877|Burangoo Sandstone|72527|5|Briefly described|p41|||Elevated to Formation-level in Qld, within the older Wild Cow Subgroup (Sweet, 2017). See also Burangoo Sandstone Member (as used in NT).||Wild Cow Subgroup||||
77877|Burangoo Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|See also misspelling 'Bunangoo Sandstone' on p33 Fig.12. Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Pandanus Formation and underlies Wallis Formation.||
77877|Burangoo Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in QLD. Distinct from Burangoo Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77877|Burangoo Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Pandanus Formation. Overlain by Wallis Formation.||
77877|Burangoo Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Pandanus Formation. Overlain by Wallis Formation.||
33171|Burash Sandstone|22538|2|Defined|p715, App1 p723||Statherian|Supersedes the upper part of Masterton Formation""||||||23-MAR-18
33171|Burash Sandstone|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: ~1670Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
33171|Burash Sandstone|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
33171|Burash Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Of the Tawallah Group.||||
33171|Burash Sandstone|65228|5|Briefly described|p23, p24,  Fig 10.|Statherian|Statherian|Southern McArthur Basin.|1707 +/- 5 Ma (Page et al. 2000).[ not in this ref|||Conformably overlies Tanumbirini Rhyolite. Correlated with Echo Sandstone.||23-MAR-18
33171|Burash Sandstone|65340|5|Briefly described|p12 Fig.6, p53 Fig.51.|||Lateral equivalent of Echo Sandstone.||Unit in Tawallah Group.||Overlies Nyanantu Formation.|Quartzose sandstone.|
33171|Burash Sandstone|69430|4|Described|p15:3, 10, 13|Statherian|Statherian|Rawlings (1999), for a succession of fine- to medium-grained sandstone in eastern TANUMBIRINI map area. Formerly part of Masterton Sandstone. Southern McArthur Basin. Up to 370m thick. High-energy shallow-water deposits.||Tawallah Group.||Conformably overlies Nyanantu Formation and Tanumbirini Rhyolite. Is overlain unconformably by Roper Group. Possible equivalent to Parsons Range Group.|Quartzic sandstone, with minor coarse or granule intervals near top.|12-JUL-16
33171|Burash Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group||Overlies Nyanantu Formation||
33171|Burash Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Quartzose sandstone.|
33171|Burash Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown to be located in the Beetaloo Sub-basin of the Southern McArthur Basin.||Tawallah Group||Overlies Nyanantu Formation.||
33171|Burash Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by Nyanantu Formation. Equivalent to Echo Sandstone||
33171|Burash Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Beetaloo Sub-basin of the Southern McArthur Basin.||Tawallah Group||Overlies Nyanantu Formation.||
33171|Burash Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Underlain by Nyanantu Formation.||
26441|Burnside Granite|23122|5|Briefly described|p409, Fig.2, 410|||||||||
26441|Burnside Granite|23337|5|Briefly described|906 Fig.9|||||||||
26441|Burnside Granite|23385|6|Mentioned|Table 2|||||||||
26441|Burnside Granite|23714|4|Described|p24|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
26441|Burnside Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
26441|Burnside Granite|24047|6|Mentioned|p37|||On MCKINLAY RIVER sheet.||||||
26441|Burnside Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Burnside Suite (Cullen Supersuite). Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
26441|Burnside Granite|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
26441|Burnside Granite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1800-1760Ma. Geological Province: Pine Creek Inlier. Name written as Burnside only under heading for GRANITE.||||||07-NOV-08
26441|Burnside Granite|30319|6|Mentioned|p270|||||||||
26441|Burnside Granite|32660|5|Briefly described|Table 2|||||||||
26441|Burnside Granite|33278|6|Mentioned|Fig.7|||||||||
26441|Burnside Granite|35061|6|Mentioned|p143|||||||||
26441|Burnside Granite|35140|6|Mentioned|p322|||||||||
26441|Burnside Granite|35465|6|Mentioned|p57|||||||||
26441|Burnside Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26441|Burnside Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26441|Burnside Granite|41465|6|Mentioned|p8|||||||||
26441|Burnside Granite|42012|6|Mentioned|p30|||||||||
26441|Burnside Granite|42756|6|Mentioned|Fig.5 P6|||||||||
26441|Burnside Granite|42927|5|Briefly described|p428|||see also Fig.2 P430||||||
26441|Burnside Granite|43140|3|Fully described|p16||Paleoproterozoic|Of Cullen Batholith.||||||07-NOV-08
26441|Burnside Granite|43624|6|Mentioned|p10|||||||||
26441|Burnside Granite|43832|4|Described|Table8p39;46,55,60||Paleoproterozoic|Age 1800+-5 Ma; less accurate 1750+-56 Ma, 1780-1790 Ma (p53)||||||07-NOV-08
26441|Burnside Granite|45022|14|Not recorded|p.123,128,141-303||Precambrian|On many pages.  Pl.28||||||
26441|Burnside Granite|45087|5|Briefly described|p14|||Chem. analyses.||||||
26441|Burnside Granite|46163|14|Not recorded|p.169,171|||||||||
26441|Burnside Granite|46658|6|Mentioned|p559|||||||||
26441|Burnside Granite|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Fine to medium muscovite-biotite adamellite, porphyritic in places.  Intrudes the Mount Partridge and South Alligator Groups.||||||07-NOV-08
26441|Burnside Granite|46676|14|Not recorded|p.9|||||||||
26441|Burnside Granite|46848|6|Mentioned|p167|||||||||
26441|Burnside Granite|46877|6|Mentioned|Fig.1|||||||||
26441|Burnside Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1800-1750 +/- 56Ma (Shrimp, U-Pb).||||||07-NOV-08
26441|Burnside Granite|62375|5|Briefly described|p11|||Biotite. Geological Province: Pine Creek Orogen.||||||09-FEB-10
26441|Burnside Granite|63866|5|Briefly described|p110, p117|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. |1800 +/- 5 Ma |Cullen Supersuite||||
26441|Burnside Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|I-type. Pink-grey medium equigranular biotite granite. Intrudes South Alligator and Finniss River Groups.||||||07-JAN-09
26441|Burnside Granite|67564|5|Briefly described|p33 Fig.19, p35.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Distinct satellite pluton of Cullen Batholith. Up to 85 km2 in area. High SiO2, low CaO, highly-fractionated and peraluminous.|1810 - 1800 Ma.|||||
26441|Burnside Granite|68186|5|Briefly described|p8, p41|Mesoproterozoic|Mesoproterozoic|Nornalup Zone, Kepa Kurl Booya Province. Intruded in the late stages of the Albany-Fraser Orogeny.|Between 1170 and 1150 Ma.|||||
26441|Burnside Granite|69252|6|Mentioned|p9|||Nornalup Zone, Kepa Kurl Booya Province, Albany-Fraser Orogen.||||||
26441|Burnside Granite|69420|5|Briefly described|p5:17-19, 21-22, 34, 37|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Spatially related to Au (Brocks Creek) or base metals mineralisation. A conventional U-Pb zircon (TIMS) age of 1750 +/- 56 Ma is also given.|1800 +/- 5 Ma (SHRIMP U-Pb zircon).|Burnside Suite.||Intrudes Koolpin Formation.|Fine- to medium-grained granite, porphyritic to equigranular. I-type.|12-JUL-16
26441|Burnside Granite|69577|6|Mentioned|p113, 116, p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Central Pine Creek Orogen. Described as ""compositionally and spatially part of the Cullen Supersuite"" but is significantly younger.",,|1800 +/- 5 Ma (U-Pb; Stuart-Smith et al., 1993).|||||
26441|Burnside Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1800 +/- 5 Ma.|Burnside Suite.|||Pink to grey, fine- to medium-grained, porphyritic to equigranular biotite granite, moderately foliated.|
26441|Burnside Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1800+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
31738|Burnside Suite|24197|5|Briefly described|p24|||Of the Cullen Supersuite. Includes the plutons: Burnside Granite, Douglas and Frances Creek Leucogranites and Wandie Granite. Geological province: Pine Creek Inlier.||||||07-FEB-11
31738|Burnside Suite|50586|6|Mentioned|p4.21|||Of the Cullen Supersuite. Geological Province: Pine Creek Inlier.||||||
31738|Burnside Suite|69420|5|Briefly described|p5:17, 19, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Cullen Supersuite.|Burnside, Douglas, Wandie Granites; Frances Creek Leucogranite.|||12-JUL-16
31738|Burnside Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Cullen Supersuite.|Includes Burnside Granite, Douglas Granite, Frances Creek Leucogranite.|||01-MAR-18
27284|Burt Bluff Gneiss|7837|6|Mentioned|p101||||1603 +/- 7 Ma (Zhao and Bennett, 1995).|||||
27284|Burt Bluff Gneiss|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Biotite-quartz-feldspar augen gneiss.  Geological Province: Arunta Block.||||||03-NOV-04
27284|Burt Bluff Gneiss|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Laminated granitic gneiss, biotite-bearing large feldspar orthogneiss.||||||
27284|Burt Bluff Gneiss|23363|5|Briefly described|352 Tab.3|Calymmian|Statherian|Age: 1603+/-7Ma||||||02-AUG-06
27284|Burt 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
27284|Burt Bluff Gneiss|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27284|Burt Bluff Gneiss|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27284|Burt Bluff Gneiss|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27284|Burt Bluff Gneiss|39887|6|Mentioned|Fig.3|||||||||
27284|Burt Bluff Gneiss|41816|4|Described|p10|||||||||
27284|Burt Bluff Gneiss|41837|6|Mentioned|Map legend|Proterozoic||||||||
27284|Burt Bluff Gneiss|42326|5|Briefly described|Table 2 P11|||||||||
27284|Burt Bluff Gneiss|42504|5|Briefly described|p113|||||||||
27284|Burt Bluff Gneiss|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Iwupataka Metamorphic Complex.||||||07-NOV-08
27284|Burt Bluff Gneiss|43503|2|Defined|8,25,78|||Dated at 1603+/-7Ma||||||
27284|Burt Bluff Gneiss|44114|6|Mentioned|p335, 339||||~1610 Ma (Zhao and Bennett, 1995).|||||
27284|Burt Bluff Gneiss|48992|2|Defined|p12|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
27284|Burt Bluff Gneiss|50369|5|Briefly described|p1.5, 22.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Iwupataka Suite. Age: 1603 +/- 7Ma (Shrimp).||||||07-NOV-08
27284|Burt Bluff Gneiss|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite-quartz-feldspar augen gneiss.||||||
27284|Burt Bluff Gneiss|68994|6|Mentioned|p24||||1603 Ma.|||||
27284|Burt Bluff Gneiss|69428|5|Briefly described|p13:6-7|||Linked with Rungutjirba Gneiss on geochemical and isotopic grounds. SHRIMP U-Pb zircon age.|1603 +/- 7 Ma (Zhao and Bennett, 1995).||||A foliated porphyritic biotite granite.|12-JUL-16
27284|Burt Bluff Gneiss|69925|5|Briefly described|p18, 21, 23, 30-31, 40|||Southern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated. Possible intrusive equivalent of Rungutjirba Gneiss.|1603 +/- 7 Ma (crystallisation).|||Is overlain nonconformably by Heavitree Quartzite. Intrudes Simpsons Gap Metasediments. Is intruded by Stuart Dyke Swarm.|Fairly homogeneous granitic gneiss. Rare metasedimentary xenoliths.|
27284|Burt Bluff Gneiss|69931|6|Mentioned|p269, 273-274, 280-281, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.||Burt-Rungutjirba Suite.|||Foliated porphyritic granite, fine-grained granite.|
27284|Burt Bluff Gneiss|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1603+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic gneiss.|
81761|Burt-Rungutjirba Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block. Intrudes the Iwaupataka Package.|1615 +/- 11 Ma.|||||
81761|Burt-Rungutjirba Suite|69931|5|Briefly described|p269, 278, 281-283|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Area of 340 km2.|1603 +/- 17 Ma; 1615 +/- 11 Ma.||Burt Bluff Gneiss, Rungutjirba Gneiss.|Intrudes, and is interlayered with, the Simpsons Gap Metasediments.|Contains no garnet (cf. Boggy Hole Suite).|
83054|Cackleberry Metacarbonates|73128|5|Briefly described|p5, p8|||Re-interpretation by Reno et al (in prep) of the metacarbonate portion of the 'Cackleberry Metamorphics' of Scrimgeour and Raith (2001). Present as surface outcrop at Molyhil tungsten-molybdenum deposit, Jinka 1:100 000 map sheet. Occurs as a complex vein-breccia in places at Molyhil deposit. [Written as 'Cackleberry Metacarbonates' in footnote on p8].|||||Calc-silicate rocks.|
83054|Cackleberry Metacarbonates|73551|6|Mentioned|p11-12, p14-15|||Previously[?] called Cackleberry Metamorphics.||||||
83054|Cackleberry Metacarbonates|73591|6|Mentioned|p33-34|||[Written as Cackleberry Metacarbonate].||Deep Bore Metamorphics|||Metacarbonates.|
26447|Cadney Metamorphics|39888|6|Mentioned|Table 1|||||||||
26447|Cadney Metamorphics|41510|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
26447|Cadney Metamorphics|44114|5|Briefly described|p321|||Central Arunta Inlier. Shallow-marine sedimentary rocks and felsic extrusives. Age possibly >1820 Ma.|>1780 Ma (Black and Shaw, 1995).||||Calcareous and pelitic rocks, quartzofeldspathic gneiss.|
26447|Cadney Metamorphics|50246|5|Briefly described|p4, p9|Paleoproterozoic|Paleoproterozoic|Age: 1780-1760Ma. Includes marbles and calc-silicates. Hosts gold deposits.See also p21 Fig. 3 - appears informally as Cadney metamorphics.||||||07-FEB-11
26447|Cadney Metamorphics|62595|5|Briefly described|p3, p6, p9, pp16-17, p31 Fig.9.|Paleoproterozoic|Paleoproterozoic|Included in Scrimgeour's (2003) Cadney package. Hosts the Pinnacles Cu district. Age estimate based on geological relationships.|c.1800 Ma.||||Marbles and calc-silicates.|
26447|Cadney Metamorphics|66860|6|Mentioned|p18, p64, p72, p74, p91|||Hosts Johnnies Reward prospect. Copper deposits in the Pinnacles district are controlled by a fault which truncates granulite-facies fabrics in this unit.||Uppermost unit in Strangways Metamorphic Complex.||Overlies Erontonga Metamorphics.|Includes sillimanite-bearing metapelite package, quartzofeldspathic gneiss and felsic granulite, marble and calcsilicate rocks; minor mafic granulite.|
26447|Cadney Metamorphics|69427|4|Described|p12:3, 8-11, 37, 53, 55, 57-58|Paleoproterozoic|Paleoproterozoic|Aileron Province. Constitutes most of the upper part of the Complex. A distinctive unit dominated by calcareous and pelitic metasedimentary rocks. Hosts the Johnnies Reward Cu-Au-Pb(-Zn-Ag) prospect(described in detail), and The Pinnacles copper district, a well as deposits in the Arltunga goldfield. Pb-isotope (galena) minimum model age. LA-ICPMS monazite dating (Wade, unpublished, 2008) indicates metamorphism at 1730-1720 Ma and reworking at 1700-1690 Ma.|>1770 Ma (Hussey et al., 2006).|Uppermost unit in Strangways Metamorphic Complex.||Overlies Erontonga Metamorphics and Yambah Granulite.|Calc-silicate rock, marble and metapelitic rock; quartzofeldspathic metasedimentary gneiss and felsic granulite in lower parts; mafic granulite is common.|12-JUL-16
26447|Cadney Metamorphics|69929|6|Mentioned|p233|||||Strangways Metamorphic Complex.||||
26447|Cadney Metamorphics|71839|5|Briefly described|p12|||Previous dating of zircon rims of this unit recorded a U-Pb metamorphic disturbance age of 1002 +/- 7 Ma.||||||
26447|Cadney Metamorphics|71840|5|Briefly described|piii, p2|||Geological province: Aileron Province. Cut by quartz veins associated with pegmatite intrusions. Hosts base metal mineralisation of the polymetallic Cu-Pb (Zn-Ag-Au) Johnnies Reward prospect. 40Ar/39Ar dating of hornblende from a quartz vein yields an inverse isochron age of 428+\-31 Ma, which (if valid; see discussion) provides minimum age constraint on mineralisation at Johnnies Reward prospect.  Sedimentary protolith dominantly mudstone and carbonate rocks, possibly with bimodal volcanic rocks, all intruded by bimodal igneous rocks.|||||Includes altered metafelsic, metamafic and metapelitic granulite and marble.|19-SEP-19
26447|Cadney Metamorphics|72378|5|Briefly described|iii,p1,6,12|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Hypothesised to have a c. 1.80-1.76 Ga maximum depositional age, based on the underlying c. 1.8 Ga Strangways Metamorphic Complex. Inferred minimum age c. 1.73 Ma based on the apparent age of the overprinting Strangways Event (Huston et al 2006). Associated with the Johnnies Reward Cu-Pb-(Ag-Zn) prospect. LA-ICP-MS insitu muscovite geochronology of NTGS AS16MVM009 (gt-bt-qtz-plg- gneiss) yielded the following interpretative results: a) quartz growth and maximum age of garnet growth at 1716+\-15 Ma (207Pb/206Pb); b) minimum age of garnet growth and maximum age of granet fracture development at 1670+\10 Ma (207Pb/206Pb); c) minimum age of garnet fracture development at 1560+\-10 Ma (207Pb/206Pb); d) possible fluid infiltration events at 1604+\-37 Ma (207Pb/206Pb) and 1499+\-28 Ma (207Pb/206Pb), and e) fluid infiltration event at 997+\8 Ma (206Pb/238U; which may be related to Gumtree Granite felsic magmatism at c. 1000 Ma; see p13).||||Underlain by Strangways Metamorphic Complex.||
24806|Cahill Formation|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Intruded by Zamu Dolerite.||||||07-NOV-08
24806|Cahill Formation|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous, with carbonate and calc-silicate gneiss in lower part.  Conformably overlain by the Nourlangie Schist; conformably overlies the Kakadu Group and part of the Nanambu Complex.||||||07-NOV-08
24806|Cahill Formation|9691|5|Briefly described|Map Legend|||Intruded by Zamu Dolerite. Feldspathic quartzite, schist.||||||
24806|Cahill Formation|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Intruded by Zamu Dolerite. Feldspathic quartzite, schist.||||||02-JUN-05
24806|Cahill Formation|22720|6|Mentioned|p 168|||||||||
24806|Cahill Formation|22810|5|Briefly described|Table2 P4|||Equivalent of Masson Formation, upper member equivalent of Mundogie Sandstone||||||
24806|Cahill Formation|23059|5|Briefly described|639|||||||||
24806|Cahill Formation|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|23374|5|Briefly described|p36||Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|23475|5|Briefly described|p4|Proterozoic|Proterozoic|Age: 2200 Ma.||||||
24806|Cahill Formation|23714|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
24806|Cahill Formation|24047|5|Briefly described|p6 Fig. 5|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|24168|6|Mentioned|p646|||||||||
24806|Cahill Formation|24181|4|Described|p84|Paleoproterozoic|Paleoproterozoic|Quartz schist, mica schist, para-amphibolite, calc-silicate and carbonate. Divided into 7 sequences. Geol. Prov.: Pine Creek Inlier. Overlies Kakadu Group. Overlain by Nourlangie Schist and unconformably by Kombolgie Formation. Hosts Ranger Uranium Mine.||||||22-NOV-11
24806|Cahill Formation|31268|6|Mentioned|p19|||||||||
24806|Cahill Formation|31833|6|Mentioned|p28|||Table 2||||||
24806|Cahill Formation|31834|6|Mentioned|p18|||||||||
24806|Cahill Formation|35140|6|Mentioned|Fig.1|||||||||
24806|Cahill Formation|35165|6|Mentioned|p1421|||||||||
24806|Cahill Formation|35256|6|Mentioned|p18|||||||||
24806|Cahill Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
24806|Cahill Formation|35923|5|Briefly described|p247|||||||||
24806|Cahill Formation|36475|6|Mentioned|p59|||||||||
24806|Cahill Formation|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|36751|6|Mentioned|p472|||||||||
24806|Cahill Formation|36902|6|Mentioned|p13|||||||||
24806|Cahill Formation|37462|6|Mentioned|Fig.4.8|||||||||
24806|Cahill Formation|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous with carbonate and calc-silicate gneiss in lower part.||||||07-NOV-08
24806|Cahill Formation|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|37898|6|Mentioned|p49|||||||||
24806|Cahill Formation|38239|4|Described|p22|||See also Fig.2.||||||
24806|Cahill Formation|38349|4|Described|p10|||||||||
24806|Cahill Formation|38351|4|Described|p5|||||||||
24806|Cahill Formation|38557|6|Mentioned|p286|||||||||
24806|Cahill Formation|38639|6|Mentioned|p26|||||||||
24806|Cahill Formation|38649|6|Mentioned|p404|||||||||
24806|Cahill Formation|38740|5|Briefly described|p304|||||||||
24806|Cahill Formation|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|39048|6|Mentioned|p823|||||||||
24806|Cahill Formation|39069|5|Briefly described|Table 1|||||||||
24806|Cahill Formation|39357|6|Mentioned|p9|||||||||
24806|Cahill Formation|39518|6|Mentioned|p4|||||||||
24806|Cahill Formation|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous, with carbonate and calc-silicate gneiss in lower part.||||||07-NOV-08
24806|Cahill Formation|40104|6|Mentioned|p331|||||||||
24806|Cahill Formation|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous, with carbonate and calc-silicate gneiss in lower part.||||||07-NOV-08
24806|Cahill Formation|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous, with carbonate and calc-silicate gneiss in lower part.||||||07-NOV-08
24806|Cahill Formation|40296|6|Mentioned|p345|||||||||
24806|Cahill Formation|40493|5|Briefly described|Table 1|||||||||
24806|Cahill Formation|40532|6|Mentioned|p257|||||||||
24806|Cahill Formation|40553|6|Mentioned|p4|||||||||
24806|Cahill Formation|40593|6|Mentioned|p106|||||||||
24806|Cahill Formation|40768|5|Briefly described|p392|||||||||
24806|Cahill Formation|40808|6|Mentioned|Fig.3|||||||||
24806|Cahill Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24806|Cahill Formation|41072|6|Mentioned|p65|||||||||
24806|Cahill Formation|41125|6|Mentioned|p18|||See also Fig.6||||||
24806|Cahill Formation|41146|6|Mentioned|p858|||||||||
24806|Cahill Formation|41147|6|Mentioned|Fig.1|||||||||
24806|Cahill Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24806|Cahill Formation|41305|6|Mentioned|Fig.3|||||||||
24806|Cahill Formation|41397|6|Mentioned|p7|||||||||
24806|Cahill Formation|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24806|Cahill Formation|41586|6|Mentioned|Map legend|||||||||
24806|Cahill Formation|41601|4|Described|p42|||||||||
24806|Cahill Formation|41649|6|Mentioned|p66|||||||||
24806|Cahill Formation|41663|4|Described|p33|||||||||
24806|Cahill Formation|42012|6|Mentioned|Fig.3 P3|||||||||
24806|Cahill Formation|42198|6|Mentioned|p265|||||||||
24806|Cahill Formation|42355|5|Briefly described|p69|||||||||
24806|Cahill Formation|42372|5|Briefly described|p16|||||||||
24806|Cahill Formation|42927|6|Mentioned|Fig.1 P429|||||||||
24806|Cahill Formation|43187|5|Briefly described|p2|||||||||
24806|Cahill Formation|43624|6|Mentioned|Table 1,p9|Paleoproterozoic|Archean|||||||07-NOV-08
24806|Cahill Formation|43719|5|Briefly described|fig.13,p15,31|||||||||
24806|Cahill Formation|43726|5|Briefly described|p3|||||||||
24806|Cahill Formation|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|A lower unnamed member: feldspathic quartzite and hematititc quartz-mica schist, commonly garnetiferous; and, upper unnamed member: feldspathic quartzite, feldspar-quartz schist, feldspathic schist, quartzite, garnet-mica schist, mica quartz schist......||||||07-NOV-08
24806|Cahill Formation|46658|6|Mentioned|p550|||||||||
24806|Cahill Formation|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Schist, gneiss, quartzite; carbonaceous with carbonate and calc-silicate gneiss in lower part.  Overlain conformably by Nourlangie Schist; conformably overlies the Kakadu Group.   Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
24806|Cahill Formation|46700|5|Briefly described|p12, Table1 p12||Proterozoic|||||||17-APR-18
24806|Cahill Formation|46824|4|Described|p322|||||||||
24806|Cahill Formation|47049|6|Mentioned|Fig.2|||||||||
24806|Cahill Formation|50586|6|Mentioned|p5.3|||Intruded by Jim Jim Suite.||||||
24806|Cahill Formation|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Schist, gneiss, quartzite; carbonaceous, with carbonate and calc-silicate gneiss in lower part.||||||
24806|Cahill Formation|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Schist, gneiss and quartzite.||||||03-AUG-06
24806|Cahill Formation|60680|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Consists of undivided schist, gneiss and quartzite and Upper and Lower (unnamed) Members.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
24806|Cahill Formation|61206|5|Briefly described|p516, p517 Fig.1, p518, p524-525|||Hosts the major U deposits at Ranger 1, Ranger 3, Jabiluka and Koongarra.||||Overlies the Kakadu Group|Lower part includes calcareous rocks, carbonaceous schists, amphibolites, and biotite-muscovite schists.|
24806|Cahill Formation|62375|5|Briefly described|p8 Table 1|Paleoproterozoic|Paleoproterozoic|Quartz schist, pelitic and partly carbonaceous near base, with magnesite lenses. Thickness: <3500m.Geological Province: Pine Creek Orogen. Uncon. Overlain by: Mamadawerre Sandstone.||||||09-FEB-10
24806|Cahill Formation|63866|5|Briefly described|p111-p112, p117|||Nimbuwah Domain, Pine Creek Orogen. Possibly equivalent to the Manton and Namoona Groups.||||Conformably overlies the Kakadu Group. Unconformably overlain by the Nourlangie Schist. Equivalent to the Wildman Siltstone. Intruded by the Zamu Dolerite.|Carbonate rocks, carbonaceous pelitic and quartzo-feldspathic psammitic metasedimentary rocks.|
24806|Cahill Formation|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~1865-2500Ma. Of Namoona Group. Max thick 2000m. Interbedded, well foliated, med mica+/-feldsp+/qtz schist, feldspathic qtzite, meta-arkose and qtzite; Calc-silicate gneiss, metapsammite, metapelite; includes some "Myra Falls Metamorphics"; Metaqtzite||||||
24806|Cahill Formation|64730|6|Mentioned|p141|Paleoproterozoic|Paleoproterozoic|Correlated with Namoona Group.||||Unconformably overlies Nanambu Complex.||03-MAY-12
24806|Cahill Formation|64956|6|Mentioned|p93|||Conformably overlain by Nourlangie Schist.||||||07-FEB-11
24806|Cahill Formation|65232|5|Briefly described|p23, p6, p5, p40, p37, p38, App. 2|Palaeoproterozoic|Palaeoproterozoic|Over: Kakadu Gp (conform); Nanambu Complex (fault). Under: Nourlangie Schist; Bathurst Island Fm; Mamadawerre Sst (unconform/ reverse-fault). Geol. Prov: Pine Creek Orogen. Hosts U. See informal: Upper and Lower Cahill Formations; Myra Falls Metamorphics.||||||09-FEB-10
24806|Cahill Formation|66683|5|Briefly described|pp368-369, p377.|Paleoproterozoic|Paleoproterozoic|Formerly correlated with Mount Partridge Group; zircon detrital spectra are markedly dissimilar. Suggests different depocentres. Hosts the giant uranium deposits at Jabiluka, Koongarra, Ranger and Nabarlek.||||Is overlain by Nourlangie Schist.|Interlayered quartzofeldspathic mica schist and gneiss, feldspathic quartzite, psammitic and pelitic schist; minor carbonate and carbonaceous schist. Mica schists locally garnet- and/or staurolite-bearing.|11-OCT-11
24806|Cahill Formation|67057|5|Briefly described|p454, p457, p461 Fig.6, pp464-465. |||Nimbuwah Domain. Hosts the Jabiluka, Ranger and Koongarra unconformity-related uranium deposits. Syn-ore illite and chlorite formed between 150 - 250 degrees C. Lithogeochemistry discussed in detail.||||Is intruded by Zamu Dolerite.|Lower part includes a dipping sequence of predominantly chlorite-biotite-muscovite-feldspar schists.|
24806|Cahill Formation|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Pine Creek area.||||||
24806|Cahill Formation|67355|6|Mentioned|p6, p10, p25-26|||Nanambu Shelf. Hosts uranium mineralisation and orebodies.||||||25-JAN-17
24806|Cahill Formation|67479|5|Briefly described|p2 Tb.1, p3 Tb.1, p20, pp24-29, p68-70|Orosirian|Neoarchean|Maximum depositional age of both the upper and lower Cahill Formation.|Upper: 2017 +/- 11 Ma; lower: 2500 +/- 8 Ma|||Intruded by the Nimbuwah Complex.|Muscovite schist and silicified tuff.|24-JAN-17
24806|Cahill Formation|67564|3|Fully described|p8 Table 2, p9 Fig.4, pp11-13, p31. |Paleoproterozoic|Paleoproterozoic|Correlative of Celia Dolostone. 2500 m thick. Lower unit: intertidal to shallow marine; upper unit: fluviatile to shallow marine. The lower unit hosts several large, stratabound uranium deposits in the Alligator Rivers Uranium Field. Numerous intercalated metadolerite sills produce a distinct, intense magnetic signature. Amphibolite rocks have very similar major- and trace-element compositions to the Goodparla Dolerite.|Depositional age of 2100 - 2050 Ma.|Unit in Namoona Group.||Conformably overlies Kakadu Group. Is intruded by Goodparla Dolerite sills. Is overlain unconformably by Nourlangie Schist.|Lower unit: pyritic and graphitic garnet-mica schist, calcareous garnet mica schist; upper unit: mica-feldspar-quartz schist, feldspathic quartzite, meta-arkose, quartzite, mica schist, feldspar quartz schist.|
24806|Cahill Formation|67779|3|Fully described|p5 Fig.4(b), p10 Table 1, pp16-19, p50.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Up to 400 m thick. Near-shore shelf environment. Encloses Caramal, Birraduk and Namarrkon Amphibolites. The lower, carbonate and carbonaceous rocks host the Ranger, Jabiluka and Koongarra uranium deposits. Is pervasively altered by chloritisation, sericitisation and hematisation. Maximum depositional age constrained by dating of metamorphic zircon and monazite to ~1870 Ma.. Previous correlations with Mount Partridge and Namoona Groups have been found to be erroneous, based on recent SHRIMP and LA-ICPMS U-Pb detrital zircon analyses. Structures, petrography and geochronology are described in detail.|1866 +/- 11 Ma (Kositcin et al. in press).|Unit in Cosmo Supergroup?||Overlies Kudjumarndi Quartzite paraconformably. Is faulted against Kukalak Gneiss; intruded by the Nimbuwah Complex; overlain unconformably by Mamadawerre Sandstone, conformably by Nourlangie Schist.|Quartz- and quartzofeldspathic mica schist, quartzite, mica schist, amphibolite: locally garnet- and magnetite-bearing; minor tremolite-dolomite marble, calc-silicate rock, and pyritic, garnetiferous and carbonaceous schist.|02-NOV-12
24806|Cahill Formation|67873|6|Mentioned|p73, p161-162|||Associated with a magnetic intensity worm.||||||
24806|Cahill Formation|68697|5|Briefly described|vi, p2, p35-47|||Nimbuwah Domain, Pine Creek Orogen. Maximum depositional age; very similar detrital zircon spectrum to a sample dated by Hollis et al. (2010). Appears on p46 as 1865 +/- 11 Ma. Three additional samples of this unit were dated by in situ monazite analysis: their metamorphic ages of 1862 +/- 6 Ma, 1855 +/- 6 Ma and 1853 +/- 8 Ma are discussed.|1866 +/- 11 Ma.|||Is unconformably overlain by Kombolgie Subgroup.|Includes muscovite-quartz schist, staurolite-garnet-plagioclase-quartz schist, crenulatedbiotite-muscovite-garnet schist.|
24806|Cahill Formation|69383|4|Described|p8-20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Nimbuwah Domain. LA-ICPMS U-Pb geochronology analyses. Max deposition age, from the upper Cahill Formation.|2361+/-21 Ma|||Unconformably overlain by Kombolgie Sandstone.|Mid amphibolite-facies pelitic schist; biotite-muscovite-bearing laminated psammitic schist; pelitic biotite schist;  sillimanite-bearing psammitic schist; muscovite-biotite psammitic schist; sampled|
24806|Cahill Formation|69417|5|Briefly described|p2:4-5,|Orosirian|Orosirian|Eastern Pine Creek Orogen.|c.1870 Ma.|||Is intruded by Nimbuwah Complex.||12-JUL-16
24806|Cahill Formation|69418|5|Briefly described|p3:6, 17-18|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Hosts gold deposits (described). Also hosts several major unconformity-related U deposits including the Austatom, Caramal, Hades Flat, Jabiluka 1 and 2, Koongarra 1 and 2, Ranger 1 No.1 and 3, and Ranger 68 deposits.||||||12-JUL-16
24806|Cahill Formation|69419|5|Briefly described|p4:2 Fig.4.2, 4:6|Paleoproterozoic|Paleoproterozoic|Part of the metamorphosed basement to the McArthur Basin.|||||Amphibolite-facies psammitic and pelitic rocks.|12-JUL-16
24806|Cahill Formation|69420|4|Described|p5:2, 4, 6-7, 14, 23-26, 37-38,60,65-68|Paleoproterozoic|Paleoproterozoic|See also 71, 73-75, 81-82, 85, 100, 111, 115. Nimbuwah Domain, Pine Creek Orogen. Up to 400m thick. Amphibolite-facies metamorphism. The lower part of this unit hosts U mineralisation at Ranger, Jabiluka, Koongarra and elsewhere in the Alligator River area. Previous correlation with Mount Partridge Group is not valid (different detrital zircon geochronology). Hosts the Jabiluka 1 and 2 and Koongarra U and Au deposits. Hosts several significant U deposits (listed; some described in detail).||?Cosmo Supergroup.||Ovelies and is faulted against Namanbu Complex. Is overlain conformably and gradationally by Nourlangie Schist, and unconformably by Mamadawerre Sandstone. Is intruded by Goodparla Dolerite.|Lower part: quartzite, haematite-quartz-mica schist, pyritic carbonaceous schist, dolostone, magnesite, calc-silicate gneiss. Upper part: quartzite, feldspar-quartz schist, garnet-mica schist, mica-quartz schist, minor conglomerate.|12-JUL-16
24806|Cahill Formation|69554|6|Mentioned|p139|||Pine Creek Orogen. Contains detrital zircons aged c.1920 Ma.||||||
24806|Cahill Formation|69577|5|Briefly described|p112-114, 117|Paleoproterozoic|Paleoproterozoic|North Australian Craton. Metamorphosed, deformed and intruded by granitoids during the 1865-1855 Ma Nimbuwah orogenic event. Hosts unconformity-related U deposits. Scenarios for formation of these deposits are discussed.|||||Metasedimentary sequence of siliciclastic to pelitic schists, carbonate and calc-silicate rocks and amphibolites.|
24806|Cahill Formation|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
24806|Cahill Formation|69917|4|Described|p45-51, 52|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Nimbuwah Domain. U/Pb SHRIMP zircon dating, Hf, O analytical data. 2 samples.|2017+/-11 Ma; 1866+/-11 Ma max dep|||Unconformably overlain by Kombolgie Subgroup|Muscovite-bearing quartzo-feldspathic schist; retrogressed mica schist.|
24806|Cahill Formation|70719|6|Mentioned|p7|||Nimbuwah Domain, Pine Creek Orogen. There are some similarities in age spectra with Grindall Formation, Arnhem Province.||||||
24806|Cahill Formation|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||1870 Ma.||||Quartz- and quartzofeldspathic mica schist, quartzite, mica schist, amphibolite; locally garnet- and magnetite-bearing; minor tremolite-dolomite marble, calc-silicate rock, pyritic, garnetiferous and carbonaceous schist, rare ultramafic.|
24806|Cahill Formation|71256|6|Mentioned|p18 Fig 1|||||||||
24806|Cahill Formation|71349|6|Mentioned|p737|||Pine Creek Orogen. Contains zircons aged c.3.1 Ga (significance explained).||||||
24806|Cahill Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2017+/-11 Ma (MDA: zircon).||||Ash tuff, psammite. Semipelitic biotite schist, muscovite-biotite psammitic schist, sillimanite-bearing psammitic schist, micaceous laminated psammitic schist, garnet-staurolite-biotite schist, crenulated biotite-muscovite-garnet schist.|
24806|Cahill Formation|72706|6|Mentioned|p4|||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 the dip and structure of the lower Cahill Formation, but encountered Myra Falls Metamorphics instead.||||Equivalent to Myra Falls Metamorphics?||
24806|Cahill Formation|72713|6|Mentioned|p2, p4, p17|||Pine Creek Orogen. Drillhole 19U4DD002 is logged as Cahill Formation from around 21.7 m to EOH. Schists, breccias and intrusives. Mineralogy is dominantly quartz with chlorite and white mica. Drilling intersected 0.7 m at 1059 ppm U3O8 (179.5m in 19U4DD002); present in irregular blebs and thin fault fractures. Two amphibole-rich zones logged as pelite (upper zone), and biotite schist, and psammo-pelite (lower zone).||||Overlain by Kombolgie Subgroup?|Various schists, breccias and intrusives.|
24806|Cahill Formation|73083|6|Mentioned|p5, p16, p36|Paleoproterozoic|Paleoproterozoic|||||||
24806|Cahill Formation|73089|6|Mentioned|p31-32|Orosirian|Orosirian|Pine Creek Orogen, Nimbuwah Domain. Neoarchean-dominated signatures. Possibly distal source; Gawler Craton or Dharwar Craton (India) based on Hf and O isotopes.|[c. 1870-1855 Ma]|||||
69472|Calamity gneiss|61154|5|Briefly described|p6-7, p43 App. 2a|||Homogeneous gneissic granite and tonalite - fine to medium to coarse-grained; typically has granoblastic texture with gneissic foliation. Four distinct lithotypes; tonalitic biotite gneiss, granitic gneiss, red granite, clinopyroxene-hornblende gneiss. age in 1600-1540 range.||||||12-SEP-18
40762|Callie Member|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Dead Bullock Formation. Geological Province: Tanami Inlier. Siltstone chert, carbonaceous shale, iron rich siltstone, nodular chert.||||||07-NOV-08
40762|Callie Member|63261|3|Fully described|p5 Fig. 2, p9 Fig. 5|Paleoproterozoic|Paleoproterozoic|Of Dead Bullock Fm (Tanami Gp). Overlies Ferdies Member which grades up into it. Age: 1838+/-6Ma. Geol.prov: Tanami Region.Chert-bearing Fe-rich siltstone+carbonaceous shale; equiv. to "Upper Blake beds" (Lambeck 2004), Davidson beds (Smith et al (1998).||||||07-FEB-11
40762|Callie Member|64662|5|Briefly described|p30 Fig. 3, p34|Paleoproterozoic|Paleoproterozoic|Of Dead Bullock Formation (Tanami Group). Age of tuff layer near top of unit: 1836+/-6Ma. The only directly dateable volcanic rock in the Tanami Group. Geol.Prov: Tanami region||||||07-FEB-11
40762|Callie Member|64730|5|Briefly described|p141, p142 Fig.11|Paleoproterozoic|Paleoproterozoic|Age is of extrusion of felsic tuff.|1838 +/- 6 Ma (Cross & Crispe 2007).|Of [Dead Bullock Formation,] Tanami Group.|||Includes felsic tuff.|03-MAY-12
40762|Callie Member|64733|5|Briefly described|p171, p172 Fig.4|Orosirian|Orosirian|Hosts large gold deposits (mines).|1836 +/- 6 Ma.|Upper part of Dead Bullock Formation.|||Carbonaceous siltstone, chert and banded iron formation.|20-APR-12
40762|Callie Member|64734|4|Described|p187-191|Orosirian||Of Dead Bullock Formation; overlies Ferdies Member; consists of siltst, chert, iron-rich siltst and clayst; main Au-host at Dead Bullock Soak goldfield (in carbonaceous siltst, iron formation); 1838+/-6Ma age constrained by age of rock interpreted as tuff||||||10-MAR-10
40762|Callie Member|64735|5|Briefly described|p217|||Age from tuff. Correlated with Epenarra Volcanics.|1838 +/- 6 Ma.|Of Dead Bullock Formation.||||30-APR-12
40762|Callie Member|66129|6|Mentioned|p216 Fig.3|||In Dead Bullock Formation.||||||
40762|Callie Member|66468|6|Mentioned|p17 Fig.4|Orosirian|Orosirian|Unit in Dead Bullock Formation. Hosts gold occurrence.||||||
40762|Callie Member|67824|4|Described|p383, p386 Fig.3,  p388-p390, p392-396|Orosirian|Orosirian|Sedimentary gold host rock. ~ 600m thick. Deposited during decreased rates of clastic deposition as part of a condensed section below storm wave base. Age from a tuffaceous unit.|1836 +/- 3 Ma.|Of the Dead Bullock Formation.||Underlain by the Ferdies Member. Overlain by the Killi Killi Formation.|Predominantly turbidites: siltstone-claystone.|
40762|Callie Member|67826|5|Briefly described|p402 Fig.3|Orosirian|Orosirian||1836 +/- 6 Ma|Of the Dead Bullock Formation.||Overlies Ferdies Member.||
40762|Callie Member|68474|6|Mentioned|p574|||Granites-Tanami Orogen.||Dead Bullock Formation||||
40762|Callie Member|69003|5|Briefly described|p17 Fig.21|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Hosts Au occurrence.|1836 +/- 6 Ma.|Dead Bullock Formation.||||
40762|Callie Member|69253|6|Mentioned|p748 Fig.2|Orosirian|Orosirian|||Unit in Dead Bullock Formation.||||
40762|Callie Member|69426|4|Described|p11:3-6, 11, 16-17, 26|Orosirian|Orosirian|Crispe et al. (2007). Hosts the Callie gold deposit. The numerous informal, local mining names for the constituent units are set out. SHRIMP U-Pb zircon crystallisation age from intercalated tuff.|1838 +/- 6 Ma (Cross and Crispe, 2007).|Dead Bullock Formation.||Conformably overlies Ferdies Member.|Siltstone, chert (including nodular chert), iron-rich siltstone, banded ironstone, carbonaceous siltstone, black graphitic mudstone, fine quartzic sandstone, minor calc-silicate and rare volcaniclastic rocks.|12-JUL-16
40762|Callie Member|69618|5|Briefly described|p91-97,p100 Tb.1,p102,p104 Fig.15,p110|||Top boundary Redefined. ~750m thick.|1838 +/- 6 Ma.|Unit in Dead Bullock Formation.||Conformably overlies Ferdies Member. Is overlain conformably by Killi Killi Formation.|Well-bedded to laminated siliciclastic and ferruginous shale, fine- to coarse-grained turbiditic sandstone, sparse chert bands and nodules, and dolerite sills.|30-MAR-15
40762|Callie Member|69747|5|Briefly described|p265-267|||Geological province: Granites-Tanami Orogen. Occurs locally in association with Dead Bullock Soak goldfield.||Unit of Dead Bullock Formation.|Includes Madigan Beds, Seldom Seen Beds, Colgate Beds, Schist Hills Iron Beds, Dead Bullock Beds and Orac Beds.|||25-JUN-19
40762|Callie Member|70024|6|Mentioned|p35|||Hosts The Granites goldfield.||Dead Bullock Formation.|Schist Hills Iron Beds.||Graphitic and ferruginous pelitic schists, including steeply-dipping iron-rich metasedimentary rocks. Amphibolite facies.|
40762|Callie Member|70291|4|Described|p179,181,183-186,199,201-202|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Deposited in deepwater, sediment-starved conditions. Hosts most lode-gold deposits in the Tanami region. ||Unit of Dead Bullock Formation.|Includes Schist Hills iron member and "Orac formation".|Underlain gradationally by Ferdie Member.|Formerly carbonaneous siltstone, now graphitic units and banded iron formation.|
40762|Callie Member|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. ||Unit of Dead Bullock Formation.||||
40762|Callie Member|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Dead Bullock Formation.||Is overlain by Killi Killi Formation.|Grey siltstone, chert, silty shale, fine-grained sandstone, laminated siltstone, quartzite, black carbonaceous shale, nodular chert, amphibolite, ironstone interlayered with chert.|
40762|Callie Member|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Dead Bullock Formation.|||Siltstone, chert, carbonaceous shale and siltstone, iron-rich siltstone, banded ironstone, nodular chert, fine-grained sandstone, minor calc-silicate rock.|
40762|Callie Member|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1838+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)|Dead Bullock FZ.|||Tuff.|
40762|Callie Member|73089|4|Described|p5-7, p22-28|Orosirian|Orosirian|Known from Dead Bullock Soak and surrounding region. Hosts many of the Au deposits in the region, including the Callie orebody. >730 m thick. Low-energy marine depositional setting, below wave base with low sedimentation rate. Geochron from a felsic unit assigned to this member that was originally described as a tuff, but later thought to represent in intrusive unit, which changes interpretation of the age from a true depositional age to a minimum age constrain.|1875-1865 Ma|Dead Bullock Formation, Tanami Group|Coora dolerite, Madigan beds, Schist Hills Iron member|Conformably underlain by Ferdies Member.|Well-bedded to laminated siltstone, chert, iron-rich siltstone, banded ironstone, carbonaceous siltstone, sandstone, minor calc-silicate rocks and chert, and rare volcaniclastic rocks.|
40762|Callie Member|73158|5|Briefly described|p3, p10|||Lower Callie Member mentioned p10.||Dead Bullock Formation, upper|Coora Dolerite|Overlies Ferdies Member||
40762|Callie Member|73159|5|Briefly described|p3, 10|||Granites-Tanami Orogen. Deep marine deposits. HFSE geochemical plots.||Dead Bullock Formation.||Overlies Ferdies Member. Is intruded by Coora Dolerite.|Well-bedded to laminated siltstones, often carbonaceous, minor sandstones, and rare volcaniclastic rocks.|
25829|Camfield beds|36335|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25829|Camfield beds|38528|6|Mentioned|p287|||||||||
25829|Camfield beds|45148|2|Defined|p23|late Miocene|middle Miocene|Middle to Late Miocene. Also mentioned p22,Fig.5.||||||03-AUG-06
25829|Camfield beds|47044|6|Mentioned|p191|||||||||
25829|Camfield beds|60672|5|Briefly described|Map Legend|Neogene|Neogene|Conglomeritic limestone, chalcedonic limestone, calcareous sandstone, siltstone, basal conglomerate.||||||
25829|Camfield beds|60703|6|Mentioned|p715|Tertiary|Tertiary|See also Camfield Beds.||||||12-APR-05
25829|Camfield beds|61119|6|Mentioned|p124, p127, pp131-132, p137, p143, p146||Cenozoic|Ephemeral freshwater channel and pool deposits? Includes Lungfish and other fossils. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
25829|Camfield beds|65239|5|Briefly described|p3 Fig. 4|Tertiary|Tertiary|Geological province: Wiso Basin. Nearshore marine deposits.||||||
25829|Camfield beds|67151|5|Briefly described|Map legend.|Neogene|Neogene||||||White, finely crystalline limestone, intraformational conglomerate.|
25829|Camfield beds|69458|5|Briefly described|p42:20-22|Miocene|Oligocene|Plane and Gatehouse (1968). Up to 21m thick. Contains the Bullock Creek Local Fauna assemblage of fossil vertebrates (described).||||Unconformably overlies Antrim Plateau Volcanics and Montejinni Limestone. Probable equivalent of Birdum Creek beds.|Flat-lying, dark grey, thickly bedded limestone, soft buff limestone, poorly bedded cherty limestone, gypsiferous siltstone, opaline limestone, and red and grey calcareous sandy siltstone. Basal coarse carbonate-cemented conglomerate.|14-SEP-18
25829|Camfield beds|70655|5|Briefly described|Map Legend|Neogene|Neogene||||||White, finely crystalline limestone, intraformational conglomerate.|
25829|Camfield beds|70854|5|Briefly described|Map legend.|Neogene|Neogene||||||Conglomeratic limestone, chalcedonic limestone, calcareous sandstone, siltstone, basal conglomerate.|
68909|Camooweal Dolostone|60122|6|Mentioned|p57 Appendix|||Correlated with parts of Arthur Creek Formation. Geological Province: central Georgina Basin||||||
68909|Camooweal Dolostone|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Pale microbial dolostone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Pale microbial dolodstone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Dolostone, dolomitic limestone, planar microbial doloaminite with nodular chert; minor marl; basal intraclast and ooid dolograinstone.||||||
68909|Camooweal Dolostone|64068|5|Briefly described|p62, 63, 128, 225|||Western and central Georgina Basin. Correlated with Arthur Creek Formation, Blazan Shale, Inca Formation, Quita Formation. The Cambrian succession in Lake Nash 1 borehole (central Georgina Basin) (1962) was attributed to this unit. Oils and tar were present in recovered cores.||||||24-MAR-16
68909|Camooweal Dolostone|64443|1|Redefined|p2, p5 Fig.3, p6 Tb.1, p14-22, p40-41 |Mindyallan||Note: revised definition. Formerly Camooweal Dolomite (Opik, 1954, 1956). Of Barkly Group. Extensive unit across central and east Georgina Basin. Laterally interdigitates with Age Creek Formation. Correlative with Anthony Lagoon beds (possibly), Age Creek Formation, V Creek Limestone, Mail Change Limestone, Devoncourt Limestone and/or Roaring Siltstone, upper Arthur Creek Formation. Max 167+m thick. Erosion by Gregory River is producing deep gorges.||||Conformably overlies Ranken Limestone, Wonarah Formation, Currant Bush Limestone; conformably underlies Arrinthrunga Formation; unconformably underlies Brunette Limestone and Austral Downs Limestone.|Dolostone, minor marl and quartz sandstone; basal intraclast, ooid and oncoid dolostone and quartz sandstone. Has spheroidal chert concretions, microbial lamination, stromatolites. Essentially unfossiliferous.|14-MAY-14
68909|Camooweal Dolostone|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Barkly Group, Georgina Basin . Overlies Ranken Limestone, underlies Brunette Limestone. Pale microbial dolostone with siliceous concretions; minor marl.||||||
68909|Camooweal Dolostone|65337|4|Described|p9 Fig.5.|Middle Cambrian|Middle Cambrian|Southwest MOUNT DRUMMOND area. 167 + m thick.||Unit in Barkly Group.||Overlies Ranken Limestone, Currant Bush Limestone, Wonarah Formation. Is overlain by Arrinthrunga Formation.|Pale microbial dololaminite with nodular chert, dolosparstone; minor peloid and ooid dolostone, conglomerate, dolomitic limestone, marl; lower high-energy interval of quartzic, intraclast and ooid dolograinstone and quartz sandstone.|
68909|Camooweal Dolostone|65344|5|Briefly described|p3 Fig. 2, p37-42|Early Cambrian|Early Cambrian|Of the Undilla Sub-basin, Georgina Basin.||||Overlies Wonarah Formation or Ranken Limestone.||
68909|Camooweal Dolostone|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||||Overlies Ranken Limestone.||
68909|Camooweal Dolostone|67352|6|Mentioned|p21|||||||Overlies Wonarah Formation.||
68909|Camooweal Dolostone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2. High-energy barrier and protected back barrier deposits.||||Overlies Ranken Limestone, Wonarah Formation, Currant Bush Limestone.|Carbonate rocks.|12-JUL-16
68909|Camooweal Dolostone|69443|4|Described|p28:16, 20-25, 33|Middle Cambrian|Middle Cambrian|Opik (1954, 1956). Central Georgina Basin. Unfossiliferous. Forms prominent hills to low rubbly outcrops; exposures are commonly significantly silicified. Notionally 240-300m thick, but usually less than 200m. Interdigitates with Age Creek Formation and Ranken Limestone. Also correlated with V-Creek, Mail Change, Devoncourt Limestones; Roaring Siltstone, Arthur Creek Formation and possibly Anthony Lagoon Formation. Age from surrounding units. Displays a prominent isolated fold: the Lake Nash Anticline.||Barkly Group.||Transitionally overlies and is partial lateral equivalent of Currant Bush Limestone. Conformably overlies Wonarah Formation and Ranken Limestone. Is overlain conformably by Arrinthrunga Formation.|Lower high-energy interval of dolostone, dolomitic limestone with nodular chert, minor marl and quartz sandstone; overlain by lower-energy microbial dololaminite with thin bands of intercalated dolomudstone, with local intraformational conglomerates.|12-JUL-16
68909|Camooweal Dolostone|69445|6|Mentioned|p30:17|||||||Overlies Colless Volcanics.||12-JUL-16
68909|Camooweal Dolostone|69446|6|Mentioned|p31:4|||Georgina Basin.||||||12-JUL-16
68909|Camooweal Dolostone|69561|6|Mentioned|p32 fig 1, p34|Boomerangian|Undillan|||||Conformably overlies Ranken Limestone, Wonarah Formation|Intraclast grainstone, oncoid rudstone and quartz sandstone.|
68909|Camooweal Dolostone|69591|4|Described|p88, p96|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin. 100-200m thick in drill cores. Basal, high-energy peritidal to shallow subtidal barrier environment, passing upwards into restricted to epeiric back-barrier. Maximum age is middle Cambrian Ptychagnostus gibbus Zone. Unfossiliferous. Coeval with Age Creek Formation, V-Creek Limestone and Mail Change Limestone.||Barkly Group.||Conformably overlies Ranken Limestone and Wonarah Formation.is overlain ("apparently") by Arrinthrunga Formation. Interdigitates with Age Creek Formation.|Dolostone with minor marl, quartz sandstone and basal intraclast, ooid and oncoid dolostone and quartz sandstone.|
68909|Camooweal Dolostone|69673|5|Briefly described|p116, p117|||300m thick.||Barkly Group|||Dolostone, dolomitic limestone, nodular chert, minor marl.|
68909|Camooweal Dolostone|70380|6|Mentioned|p745, p759|Series 3|Series 3|Undilla Sub-basin, Georgina Basin.||||||
68909|Camooweal Dolostone|72516|6|Mentioned|p92|Cambrian|Cambrian|Western and central Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
68909|Camooweal Dolostone|72919|6|Mentioned|p77|||||||||
68909|Camooweal Dolostone|73083|6|Mentioned|p10, p75|middle Cambrian|middle Cambrian|||||Overlain by Arrinthrunga Formation and Ninmaroo Formation.|Includes dolostone, marl, and quartz sandstone.|
33807|Campbell Springs Dolostone|14019|3|Fully described|p4 Fig. 3, 5 Table 1.|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Supersedes Campbell Springs Dolomite. Stromatolitic dolostone. Conformable on Blue Hole Formation; conformably overlain by Fraynes Formation. Age: 1638 +/- 9Ma. Type section: 160m. Geological Province: Birrindudu Basin.||||||07-NOV-08
33807|Campbell Springs Dolostone|23809|5|Briefly described|p49, p47 Fig. 42|Mesoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Overlies the Bluehole Formation. Age: 1638+/-9Ma.  Geological Province: Birrindudu Basin.  Correlates with Mount Parker Sandstone (Osmond Basin), Shillinglaw Formation (Ashburton Province) and Barney Creek Formation (McArthur Basin)||||||31-OCT-11
33807|Campbell Springs Dolostone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33807|Campbell Springs Dolostone|24297|5|Briefly described|p21|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.  See also p4 Fig. 3.||||||
33807|Campbell Springs Dolostone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Blue Hole Formation; overlain by Fraynes Formation.  Geological Province: Birrindudu Basin.||||||25-JAN-06
33807|Campbell Springs Dolostone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33807|Campbell Springs Dolostone|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Birrindudu Basin. Of Limbunya Group. Dolostone, microbal in part, chert, dolomitic siltstone.||||||07-NOV-08
33807|Campbell Springs Dolostone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Limbunya Group.  Grey stromatolitic dolostone, dolarenite, dolorudite, dolosiltite, dolomitic mudstone and minor orange water-laid tuffite. Conformably overlies Blue Hole Formation; conformably overlain by Fraynes Formation where not eroded/exposed.||||||07-NOV-08
33807|Campbell Springs Dolostone|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dolostone, stomatolitic in part, chert, dolomitic siltstone. Of Limbunya Group. Overlain by Fraynes Formation. Overlies Blue Hole Formation. Geological Province: Birrindudu Basin.||||||07-NOV-08
33807|Campbell Springs Dolostone|60682|4|Described|p7|Statherian|Statherian|Of Limbunya Group. Conformably overlies Blue Hole Formation. Conformably overlain by Fraynes Formation. Thickness: 50m. Age: 1638 +/- 9Ma. Geological Province: Birrindudu Basin.||||||
33807|Campbell Springs Dolostone|60685|5|Briefly described|p4 Figure 3, p2|||Of the Limbunya Group. Overlain by the former Bardia Chert Member, now remapped as Tertiary silcrete/duricrust. Geological Province: Birrindudu Basin.||||||
33807|Campbell Springs Dolostone|64737|5|Briefly described|p243|Statherian|Statherian|U-Pb date on a volcaniclastic unit.|1639 +/- 7 Ma (Smith, 2001).|Of Limbunya Group.||||01-MAY-12
33807|Campbell Springs Dolostone|65331|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Limbunya Group, Birrindudu Basin.  Dolostone, chert, dolomitic siltstone ||||||
33807|Campbell Springs Dolostone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Blue Hole Formation. Is overlain by Fraynes Formation.||
33807|Campbell Springs Dolostone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Blue Hole Formation. Is overlain by Wickham Formation.|Dolostone, stromatolitic in part, chert, dolomitic siltstone.|
33807|Campbell Springs Dolostone|68733|5|Briefly described|p177 Fig.2, p179 Tb.1, p184-186, p192|Statherian|Statherian|Birrindudu Basin. Geochronology based on Sm-Nd whole rock analysis. Sm-Nd isotope data tabulated.|ca. 1640 Ma, tuff (Cutovinos et al. 2002)|Of the Limbunya Group.||||05-DEC-17
33807|Campbell Springs Dolostone|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
33807|Campbell Springs Dolostone|69432|4|Described|p17:2, 7-8, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Typically c.170m thick; locally over 300m. Coxco Needles locally abundant in middle and upper parts. Exploration target for base metals. SHRIMP U-Pb zircon age.|1638 +/- 9 Ma (Cutovinos et al., 2002).|Limbunya Group.||Overlies Blue Hole Formation. Age-equivalent to Teena Dolostone.|Alternating cyclic biohermal and/or biostromal stromatolitic dolostone, dolomitic sandstone, oolitic dolostone, plate breccia, dolorudite and dolomitic siltstone; minor interbeds of dolomitic mudstone and waterlain tuff, and diagenetic siderite.|12-JUL-16
33807|Campbell Springs Dolostone|69673|6|Mentioned|p48 fig 35, p188|Statherian|Statherian||1638 +/- 9 Ma (SHRIMP)|Limbunya Group||Overlies Blue Hole Formation, overlain by Fraynes Formation||
33807|Campbell Springs Dolostone|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].||Limbunya Group|||Stromatolitic dolostone, dolarenite, dolorudite, dolosiltite, dolomitic mudstone and minor water-laid tuffite and chert.|18-JUL-16
33807|Campbell Springs Dolostone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Limbunya Group.||Overlies Blue Hole Formation. Appears to be overlain unconformably by Wickham Formation, although setion F-G is confusing.|Dolostone, stromatolitic in part, chert, dolomitic siltstone.|
33807|Campbell Springs Dolostone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Limbunya Group.||Overlies Blue Hole Formation. Is overlain by Fraynes Formation.|Dolostone, stromatolitic in part, chert, dolomitic siltstone.|
33807|Campbell Springs Dolostone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone, granodiorite|
33807|Campbell Springs Dolostone|71302|5|Briefly described|p6,73|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Contains 1636+\-5 Ma tuffs (Fanning, 1991; Smith, 2001), proposed to have been sourced from reworking of upper Limbunya Group rocks (Smith 2001).||Unit of Limbunya Group.||Overlain by Fraynes Formation. Underlain by Blue Hole Formation.||
33807|Campbell Springs Dolostone|71374|5|Briefly described|p36|Statherian|Statherian||1638 +/- 9 Ma (SHRIMP U-Pb)|||Conformably overlies the Farquharson Sandstone.||
33807|Campbell Springs Dolostone|71592|5|Briefly described|Appendix A.|||Birrindudu Basin.|1639+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Water-laid tuffite, interbedded dolostone.|
33807|Campbell Springs Dolostone|72718|6|Mentioned|p7|Statherian|Statherian|Birrindudu Basin. [Written as CAMPBELL SP. DLST]|1638 +/- 9 Ma|Limbunyah Group||Underlain by Blue Hole Formation. Overlain by Fraynes Formation.||
80604|Canefire Granite|73591|4|Described|piii, p2, p19-21|||Aileron Province. Interpreted to be an anatectic granite formed by the partial melting of the Kanandra Metamorphics, specifically from less aluminous parts resulting in a lack of garnet. Generally has a diffuse intrusive contact with the Jamaica Granite but is crosscut by the unit via aplite dykes. Previous SHRIMP U-Pb zircon age of 1735 +/- 4 Ma reported by Kositcin and Reno (2020). [Also written as Canefire granite on p19].|1735 +/- 4 Ma SHRIMP|Alkara Suite||Crosscut by Jamaica Granite.|Includes biotite granite.|
24210|Canulgerra Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
24210|Canulgerra Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Hanlon Subgroup (Hatches Creek Group).  Geological Province: Davenport Province.||||||11-NOV-04
24210|Canulgerra Sandstone|24172|5|Briefly described|p65 Tb.9|||Of Hanlon Subgroup. Geological Province: Tennant Creek Inlier. Of the Hatches Creek Group.||||||03-AUG-06
24210|Canulgerra Sandstone|39624|5|Briefly described|Table 1|||||||||
24210|Canulgerra Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24210|Canulgerra Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Quartz arenite and rare conglomerate; shale and siltstone.||||||10-JAN-05
24210|Canulgerra Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24210|Canulgerra Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Feldspathic arenite; friable arenite and micaceous siltstone. Geological Province: Tennant Creek Block.||||||07-NOV-08
24210|Canulgerra Sandstone|41129|4|Described|Table 1|||||||||
24210|Canulgerra Sandstone|41204|4|Described|Table 1|||||||||
24210|Canulgerra Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup. Quartz arenite, siltstone, shale; minor lithofeldspathic arenite and conglomerate.||||||16-NOV-05
24210|Canulgerra Sandstone|41308|5|Briefly described|Table 2|||||||||
24210|Canulgerra Sandstone|41310|5|Briefly described|Table 1|||||||||
24210|Canulgerra Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24210|Canulgerra Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24210|Canulgerra Sandstone|42643|5|Briefly described|p12|||Of Hanlon Subgroup.||||||03-AUG-06
24210|Canulgerra Sandstone|43802|6|Mentioned|p80|||||||||
24210|Canulgerra Sandstone|45167|3|Fully described|Table 1|||Of Hanlon Subgroup.||||||03-AUG-06
24210|Canulgerra Sandstone|49033|2|Defined|p28|Proterozoic|Proterozoic|||||||
24210|Canulgerra Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Quartz arenite, siltstone, shale; minor feldspathic/lithic arenite; rare conglomerate. Overlies Lennee Creek Formation; underlies Vadingilla [?and Yaddanilla] Formation. In the Tennant Creek region.||||||19-OCT-11
24210|Canulgerra Sandstone|64735|5|Briefly described|p206 Fig 2, p214,|Orosirian|Orosirian|||Of Hanlon Subgroup, Hatches Creek Group.||Overlies Lennee Creek Formation; underlies Vaddingella Formation.||30-APR-12
24210|Canulgerra Sandstone|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||||
24210|Canulgerra Sandstone|65338|6|Mentioned|p20.|||||Unit in Hanlon Subgroup.||||
24210|Canulgerra Sandstone|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup, Hatches Creek Group.||Overlies Lennee Creek Formation. Is overlain by Vaddingilla Formation.|Feldspathic arenite; friable arenite and micaceous siltstone.|19-OCT-11
24210|Canulgerra Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Lennee Creek Formation. Is overlain by Vaddingilla Formation.|Quartz arenite, siltstone, shale; minor feldspathic/lithic arenite; rare conglomerate.|
24210|Canulgerra Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24210|Canulgerra Sandstone|67352|4|Described|p9, p44 fig 48, p45|Statherian|Statherian|500 m thick. Ridge-forming; friable recessive interbeds.||Hanlon Subgroup||Overlies Lennee Creek Formation (conformably)|Quartz arenite to feldspathic arenite; micaceous siltstone, mudstone.|
24210|Canulgerra Sandstone|69425|5|Briefly described|p10:3, 10, 12, 19-20|Statherian|Statherian|500m thick. Shallow-marine shelf, mainly intertidal.||Hanlon Subgroup.||Conformably overlies Lennee Creek Formation. Is overlain conformably by Vaddingilla Formation. Correlated with Short Range Sandstone.|Quartz sandstone, siltstone and shale; minor feldspathic lithic sandstone; pebbly sandstone locally, and rare polymictic conglomerate. Siltstone flakes common in sandstone.|12-JUL-16
24210|Canulgerra Sandstone|69431|6|Mentioned|p16:5|||Davenport Province.||Hanlon Subgroup.||||12-JUL-16
80337|Cappocks Granodiorite|71621|5|Briefly described|iii, p1, p26-p28, p47, 49|Statherian|Statherian|Aileron Province. Age interpreted as magmatic crystallisation. SHRIMP age derived from Kositcin et al, 2011. Petrography and zircon description discussed.|1772.6 +/-3.4 Ma (SHRIMP U-Pb)|||Intrudes the Bonya Metamorphics, Mascotte and White Violet orthogenisses.|Biotite granodiorite.|01-FEB-19
80337|Cappocks Granodiorite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1773 +/- 3 Ma (U-Pb zircon)|Casper Suite|||Biotite-hornblende granodiorite to diorite, rare monzogranite: medium- to coarse grained, equigranular, moderately foliated to gneissic.|
80337|Cappocks Granodiorite|72516|2|Defined|p29, p32, p35, p49-51, p111-112, p197|Statherian|Statherian|Named after the Cappocks Waterhole, previously defined as unnamed granodiorite unit Pgn in HUCKITTA (Freeman et al 1986) and part of Mascotte Gneiss in second edition HUCKITTA.  Type locality occurs south of the Johansen Range at 612691mE 7495398mN. Occurs as Nubbins, isolated boulders and small pavements between the Johannsen and Jervois ranges in the central Bonya Hills. Thickness is unknown. Deposited in a continental margin environment. SHRIMP age is interpreted as magmatic crystallisation age. Petrography, extent, structure, metamorphism, economic geology, geophysical expression and geochemistry are discussed. Interpreted to be cogenetic and comagmatic with other units of the Casper Suite. See also p14, p16, p19-21, p71, p75, p106, p109, p123-124, p127, p135, p144, p171, p189, p192, 198, 205, 210.|1773 +/-3 Ma (SHRIMP Pb-Pb, Kositcin et al, 2011)|Casper Suite||Intruded by the Samarkand Pegmatite. Intrudes the Bonya Metamorphics, Mascotte Orthogneiss and the White Violet Orthogneiss.|Biotite hornblende granodiorite to diorite, rare monzogranite: medium-coarse grained, equigranular; moderately foliated to gneissic.|16-JUN-21
80337|Cappocks Granodiorite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes granodiorite.|
81824|Captain Morgan Metadolerite|73123|4|Described|piii, p1, p5, p7-10, p13, Fig.A2, Tb.A2|Statherian|Orosirian|Aileron Province, northeastern. Geochron is an interpreted magmatic crystallisation age. New zircon growth at 1723 +/- 7 Ma reflects regional metamorphism. Dated sample: GA sample No = 6619617, NTGS sample ID = HU18BLR2038. Outcrops widely but sparsely across Dneiper 1:100 000 mapsheet. Magma mingling with the Bacardi Granite has been recognised in outcrop indicating the units are cogenetic and coeval. Includes xenoliths and larger rafts of the Deep Bore Metamorphics. Hosted in the Deep Bore Domain. [Article includes outcrop, thin section and zircon descriptions].|1805 +/- 6 Ma SHRIMP U-Pb|Black Label Suite||Intruded by Dinkum Orthogneiss and Double Granite (both of the Molyhil Suite).|Glomerophyric metadolerite. Two textural variants: abundant plagioclase phenocrysts and/or glomerocrysts, and fine-grained and aphyric. Ranges from undeformed to locally gneissic.|
76181|Caramal Amphibolite|67779|2|Defined|p9 Table 1, pp20-23, p60, p67, p118.|Paleoproterozoic|Paleoproterozoic|New name, after Caramal uranium prospect, for a suite of amphibolites exposed in creek beds in the Caramal and Myra Falls Inliers. Previously mapped as part of Zamu Complex and Zamu Dolerite (Ferguson and Needham, 1978). Nimbuwah Domain, Pine Creek Orogen. Reference area is a river-washed platform exposure in Caramal Inlier. Geochemistry is described in detail.||||Occurs within Cahill Formation, Nourlangie Schist, Kukalak Gneiss .|Mainly granoblastic hornblende and plagioclase amphibolite; weakly to strongly foliated, locally garnetiferous; hornblende-bearing leucosomes that are cross-cut and deformed in the foliation.|14-SEP-12
76181|Caramal Amphibolite|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||||||Amphibolite: intrusive, metagabbro to metagabbroic diorite, weakly to strongly foliated, locally garnetiferous.|
23467|Caranbirini Member|22538|6|Mentioned|P717|||||||||
23467|Caranbirini Member|22664|5|Briefly described|39|Paleoproterozoic|Paleoproterozoic|Of Lynott Formation (Batten Subgroup). Geological Province: McArthur Basin.||||||07-NOV-08
23467|Caranbirini Member|22853|4|Described|22|Proterozoic|Proterozoic|Of the Lynott Formation. Max thickness 200 m. Overlain by Hot Spring Member.||||||03-AUG-06
23467|Caranbirini Member|23396|5|Briefly described|p413|||Of Lynott Formation. Geological Province: McArthur Basin.||||||03-AUG-06
23467|Caranbirini Member|23397|5|Briefly described|p473|||Of Lynott Formation.||||||03-AUG-06
23467|Caranbirini Member|23398|5|Briefly described|p443|||Of Lynott Formation.||||||
23467|Caranbirini Member|23776|5|Briefly described|p705 Fig 2.|||Of the Lynott Formation. Of Batten Subgroup.||||||03-AUG-06
23467|Caranbirini Member|23902|4|Described|p1568 Fig.2|||Of the Batten Subgroup. Overlies the Reward Dolomite. Overlain by the Hot Spring Member. Geological Province: McArthur Basin||||||
23467|Caranbirini Member|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Batten Group||||||
23467|Caranbirini Member|24048|6|Mentioned|p57|||Of the Lynott Formation.||||||03-AUG-06
23467|Caranbirini Member|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23467|Caranbirini Member|40691|6|Mentioned|Fig.4|||||||||
23467|Caranbirini Member|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23467|Caranbirini Member|41268|3|Fully described|p295|||||||||
23467|Caranbirini Member|42385|4|Described|p22|||See also Table 4 p16||||||03-AUG-06
23467|Caranbirini Member|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
23467|Caranbirini Member|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Lynott Formation.||In schematic section, overlies Reward Dolomite; underlies Hot Spring Member (Lynott Formation).|Dolomitic sandstone and shale, silty dololutite, dololutite, dolarenite, lenses os slump breccia. Detailed lithology given.|09-NOV-11
23467|Caranbirini Member|42639|4|Described|p31, Table 5 p20|||||||||
23467|Caranbirini Member|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
23467|Caranbirini Member|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Lynott Formation. Thin bedded mudstone and dolomitic mudstone, partly carbonaceous and pyritic.||||||19-OCT-05
23467|Caranbirini Member|42812|4|Described|p40, Table 4|||Of Lynott Formation.||||||03-AUG-06
23467|Caranbirini Member|42846|5|Briefly described|Fig.1 p502|||Of Lynott Formation. Geological Province: McArthur Basin.||||||09-MAY-05
23467|Caranbirini Member|42935|6|Mentioned|p529 Fig.2|||Of Lynott Formation.||||||03-AUG-06
23467|Caranbirini Member|43010|6|Mentioned|p128|||||||||
23467|Caranbirini Member|43036|5|Briefly described|p53|||Of Lynott Formation.||||||03-AUG-06
23467|Caranbirini Member|45162|4|Described|p112|||||||||
23467|Caranbirini Member|60483|5|Briefly described|p7 Fig. 5, p8|||Of Lynott Formation (Batten Subgroup, McArthur Group). Geological Province: McArthur Basin. Carbonaceous unit. ||||||
23467|Caranbirini Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Lynott Formation.||||||03-JUN-09
23467|Caranbirini Member|64815|6|Mentioned|p4 Fig.2, p6, p19  |||Described as a suitable reducing trap rock for Pb mineralisation.||Unit in Lynott Formation.||||
23467|Caranbirini Member|64817|6|Mentioned|p353 Fig.4 |||||Unit in Lynott Formation.||||
23467|Caranbirini Member|65228|6|Mentioned|Figs.02, 22.|||||Basal unit in Lynott Formation.||Overlies Reward Dolomite. Is overlain by Hot Spring Member.||
23467|Caranbirini Member|69430|4|Described|p15:3, 16; 37-38, 57, 61|Statherian|Statherian|Jackson et al. (1987). Southern McArthur Basin. Recessive. 0-400m thick. Submarine grading upward to intertidal sediments deposited in actively subsiding sub-basins. Appears as Caranbirini Formation on 15:37. Potential hydrocarbon source rock.||Lynott Formation.||Overlies Reward Dolostone disconformably or unconformably. Is overlain by Hot Spring Member conformably and gradationally.|Thinly bedded laminated dolomitic siltstone and shale, in part carbonaceous and pyritic; silty dololutite, dololutite; minor fine-grained dolarenite and lenses of slump breccia; uncommon ripples and evaporite mineral casts.|12-JUL-16
23467|Caranbirini Member|69673|4|Described|p16 fig 13, p34, p40, p41, p46, p47|||Batten Fault Zone. Regressive unit that was deposited in subtidal marine conditions, grading upward to an intertidal setting. Potential regional seal and possible source rock.||Lynott Formation|||Thinly bedded, laminated fine grained mudstone, dolomitic mudstone that is locally carbonaceous and or pyritic, dolomudstone, intraclast breccia and tuffaceous mudstone.|
23467|Caranbirini Member|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of  [Lynott Formation?,] Batten Subgroup.||||13-SEP-19
23467|Caranbirini Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone. [May be part of the Lynott Formation but this is not clear in Fig.6]||Lynott Formation, Batten Sub-group, McArthur Group||Overlain by the Lynott Formation[?]. Unconformaby[?] underlain by Reward Dolostone (Umbolooga Sub-group).||
23467|Caranbirini Member|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].||Lynott Formation||||
23467|Caranbirini Member|73412|6|Mentioned|p19|||||Lynott Formation.||||
83559|Carmencita Metadolerite|73551|6|Mentioned|p6|||||||||
38418|Carmilly Formation|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: <1780Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
38418|Carmilly Formation|24303|2|Defined|p13, p55 Appendix|Statherian|Statherian|Of the Tomkinson Creek Group. Unconformably overlain by the Jeromah Formation; overlies the Bootu Formation. Max. thickness: >750m. Formerly undifferentiated Tomkinson Creek beds. See also p3 Fig. 2, p4 Tb.2.||||||18-OCT-05
38418|Carmilly Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Gp. Inc: upper mudst., variably dolomitic with stromatolitic bioherms and fine-gr.sst), middle sst, quartz arenite, mudst. and lower sandstone, micaceous mudst., dolostone, chert facies and undiff. mudst., sst., dolostone and chert.||||||07-NOV-08
38418|Carmilly Formation|24442|5|Briefly described|p14|||Of the Tomkinson Creek Group.  Geological Province: Ashburton Province.||||||
38418|Carmilly Formation|60684|5|Briefly described|p12|||On the HELEN SPRINGS map sheet it continues the Tomkinson Creek Subgroup above Bootu Formation; underlies the Namerinni Group.||||||03-AUG-06
38418|Carmilly Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group.  Mudstone, sandstone, dolostone and chert; stromatolitic bioherms and evaporitic pseudomorphs.  Overlies Bootu Formation.  In the Tennant Creek region.||||||07-NOV-08
38418|Carmilly Formation|64780|5|Briefly described|p63 Fig.4,p66, |Palaeoproterozoic|Palaeoproterozoic|||Of the Tomkinson Creek Group.||Conformably (gradationally) overlies the Bootu Formation.|Sandstone units fine and thin upwards, and are sharply overlain by laminated mudstone and dolostone with thin intervals of thinly bedded sandstone in their lower parts.|
38418|Carmilly Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||||||
38418|Carmilly Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.||Overlies Bootu Formation.|Mudstone, sandstone, dolostone and chert; stromatolitic bioherms and evaporite pseudomorphs.|
38418|Carmilly Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
38418|Carmilly Formation|69431|4|Described|p16:1, 3-6, 12-14, 23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. Over 750m thick. Lithology and lithofacies described. Restricted shallow-marine and peritidal, including intertidal and hypersaline, deposits; possibly lacustrine in lower part.||Topmost Tomkinson Creek Group.||Conformably overlies Bootu Formation. Is overlain unconformably by Jeromah Formation (Namerinni Group).|Laminated to thinly bedded silicified dolostone, siltstone and mudstone; thinly to medium bedded, mostly fine- to medium- grained sandstone; stromatolites, evaporite pseudomorphs, enterolithic and nodular chert.|12-JUL-16
38418|Carmilly Formation|69673|6|Mentioned|p58|||||Tomkinson Creek Group||||
26462|Carolina Sandstone Member|22538|6|Mentioned|Fig3 P709|||||||||
26462|Carolina Sandstone Member|23395|6|Mentioned|p385|||||||||
26462|Carolina Sandstone Member|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26462|Carolina Sandstone Member|31348|6|Mentioned|p344|||||||||
26462|Carolina Sandstone Member|35114|6|Mentioned|Table.1|||||||||
26462|Carolina Sandstone Member|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26462|Carolina Sandstone Member|36012|3|Fully described|Table 2|||||||||
26462|Carolina Sandstone Member|38557|5|Briefly described|p293|||||||||
26462|Carolina Sandstone Member|38584|4|Described|p13|||||||||
26462|Carolina Sandstone Member|40691|6|Mentioned|Fig.4|||||||||
26462|Carolina Sandstone Member|41721|4|Described|p18|||Of the Seigal Volcanics. Thickness: 20m. Flaggy to massive, fine-grained, dark red weathering grey sandstone with some siltstone interbeds.||||||02-AUG-07
26462|Carolina Sandstone Member|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26462|Carolina Sandstone Member|42385|6|Mentioned|Fig.5 P8|||||||||
26462|Carolina Sandstone Member|42812|5|Briefly described|p11|||Of Seigal Volcanics.||||||03-AUG-06
26462|Carolina Sandstone Member|43036|6|Mentioned|Fig.5|||||||||
26462|Carolina Sandstone Member|44305|14|Not recorded|p.11||Neoproterozoic|Defn. on Tech.File E/53-8. opp.p.6. U.Prot||||||
26462|Carolina Sandstone Member|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26462|Carolina Sandstone Member|45162|6|Mentioned|p14|||See also Fig.4||||||
26462|Carolina Sandstone Member|49001|5|Briefly described|p5|||Previously defined as a member of the Peters Creek Volcanics. See also p71||||||03-AUG-06
26462|Carolina Sandstone Member|60483|5|Briefly described|p7 Fig. 5|||Of Seigal Volcanics (Tawallah Group). Geological Province: McArthur Basin.||||||05-OCT-07
26462|Carolina Sandstone Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Seigal Volcanics.||||||03-JUN-09
26462|Carolina Sandstone Member|63112|6|Mentioned|p1192 Tb.1|||<20 m thick. Separates two dolerite sills.||Unit in Seigal Volcanics.|||Fine-grained sandstone.|
26462|Carolina Sandstone Member|64817|6|Mentioned|p353 Fig.4 |||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|65228|6|Mentioned|Fig.02.|||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|65340|6|Mentioned|p12 Fig.6. |||||Unit in Seigal Volcanics.||||
26462|Carolina Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. Camooweal-Murphy Domain, Mount Isa Inlier. Calvert Superbasin. Abbreviated to Carolina Sandstone in both Time-Space Plots.|1863 +/- 6 Ma (maximum depositional age).|Seigal Volcanics.|||Sandstone, siltstone|
26462|Carolina Sandstone Member|69383|4|Described|p48-50|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Up to 20m thick beds. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1863+/-6 Ma|Of Seigal Volcanics||Conformably overlies Westmoreland Conglomerate|Flaggy to massive, fine-grained sandstone, with cross bedding, ripple marks and mud cracks indicating a shallow-marine environment.|
26462|Carolina Sandstone Member|69430|5|Briefly described|p15:3, 10|||Southern McArthur Basin.||Seigal Volcanics.|||A prominent sandstone bed.|12-JUL-16
26462|Carolina Sandstone Member|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Seigal Volcanics||||
26462|Carolina Sandstone Member|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Seigal Volcanics.|||Lithic sandstone and quartz sandstone, fine- to medium-grained, flaggy or massive; minor siltstone beds in the north and conglomerate in the southwest.|
26462|Carolina Sandstone Member|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1863+/-6 Ma (MDA: U-Pb zircon LA-ICPMS).||||Massive cross-bedded sandstone.|
26462|Carolina Sandstone Member|72718|6|Mentioned|p7|||Southern McArthur Basin.||Seigal Volcanics, Tawallah Group||Equivalent to Seigal Volcanics and Sly Creek Sandstone.||
41811|Carrington Suite|7821|5|Briefly described|p45|||Arunta Inlier.|1779 +/- 6 Ma.||||Granites.|
41811|Carrington Suite|50369|5|Briefly described|p1.3, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1780Ma.||||||07-NOV-08
41811|Carrington Suite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite, various unnamed divisions within suite.||||||07-NOV-08
41811|Carrington Suite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Undivided; weakly porphyritic to equigranular biotite granite.||||||
41811|Carrington Suite|64677|6|Mentioned|p31||||c.1770 Ma (Young et al., 1995).|||||
41811|Carrington Suite|65329|6|Mentioned|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Carrington Granite Suite||||||
41811|Carrington Suite|65330|6|Mentioned|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Carrington Granite Suite||||||
41811|Carrington Suite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Informally subdivided in to 7 unnamed granite bodies. Varies from fine-, medium-, to coarse-grained, equigranular to porphyritic granodiorite and granite. Shown as equivalent age to Rapide Granite, older than 1770-1760Ma Yambah Event, younger than Reynolds Range Group, Nicker beds.||||||09-OCT-18
41811|Carrington Suite|68994|4|Described|p4, p6, p8||||c. 1805-1770 Ma magmatic age, Edgoose et al. 2008.||Dwarf Well Granite|Intrudes Lander Rock Formation. Dwarf Well Granite is overlain by Lake Mackay Quartzite.|Granitic rocks.|
41811|Carrington Suite|69003|5|Briefly described|p5, p31|Paleoproterozoic|Paleoproterozoic|West Arunta Orogen. Intrusion coincides with the Yambah Event.|1805-1770 Ma.|||Is overlain by Lake McKay Quartzite. Intrudes Lander Rock Formation.|Metagranitic rocks.|
41811|Carrington Suite|69031|5|Briefly described|p4,p6, p17-22, p24, p26,p43,p47,p59,p67|Statherian|Orosirian|Aileron Province, Arunta Orogen. Gravity, magnetic maps. Uranium-rich: distance to this unit was used as a predictor in modelling for U sources.|1805-1770 Ma.||Dwarf Well Granite.|Intrudes Lander Rock Formation.|Granitic rocks.|
41811|Carrington Suite|69417|5|Briefly described|p2:5|Statherian|Statherian|Aileron Province.|1780-1760 Ma.|||||12-JUL-16
41811|Carrington Suite|69427|5|Briefly described|p12:3, 30, 33|Statherian|Statherian|Young et al. (1995). Aileron Province. Included most foliated biotite-rich granitic rocks in MOUNT DOREEN map area, N and S of the Ngalia Basin. SHRIMP U-Pb zircon age. Other ages range from c.1773 Ma to c.1767 Ma.|1779 +/- 7 Ma (Young et al., 1995).|||Intrudes Reynolds Range Group.|Biotite tonalite to biotite-muscovite granite; most commonly equigranular and medium-grained, although porphyritic varieties also occur. Local andalusite-bearing granite; some merging into migmatite: may be S-type.|12-JUL-16
41811|Carrington Suite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Four un-named subunits are mapped separately. LITHOLOGY (continued): Contains aplite and leucocratic veins and rare clots of radial tourmaline; rare cordierite- and garnet-bearing phase.|||Rapide Granite.||Porphyritic to equigranular biotite granite, commonly biotite-rich, varies from fine- to coarse-grained, leucocratic in places; lesser muscovite granite; biotite-hornblende granite; ubiquitously foliated. See COMMENTS for more.|
41811|Carrington Suite|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.|1779-1767 Ma.||Dwarf Well Granite.|Is overlain by Lake MacKay Quartzite.|Coarse-grained biotite metamonzogranite; granite gneiss interlayered with metagabbro.|
41811|Carrington Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
41811|Carrington Suite|71839|6|Mentioned|p10||||1820-1760 Ma||||Felsic intrusions.|22-MAR-23
41811|Carrington Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|Max age 1779+/-7 Ma, min 1767+/-4 Ma.||Includes Dwarf Well Granite, Rapide Granite.||Weakly porphyritic to equigranular biotite metagranite.|
41811|Carrington Suite|72366|5|Briefly described|p7|Statherian|Statherian|Geological province: Aileron Province. Represents second phase (second of three) of felsic magmatism in the MOUNT DOREEN map sheet, as indicated by a biotite granite with 1779+\-7 Ma magmatic crystallisation age (Young et al., 1995).|c. 178-.176 Ga||||Biotite granite.|08-JAN-20
41811|Carrington Suite|72376|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Outcrops ~7km SW of Wilfram Hill tungsten-copper deposit (Young et al., 1996). A biotite granite of the suite near the Mount Hardy deposit has a U-Pb zircon magmatic crystallisation age of 1779+\-7 Ma (Young et al., 1995).|||||Biotite granodiorite, biotite tonalite, and muscovite-biotite granite.|
38416|Carruthers Formation|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Of the Namerinni Group.  Age: 1640Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49, p60.||||||07-NOV-08
38416|Carruthers Formation|24303|2|Defined|p17, p58 Appendix|Statherian|Statherian|Of the Namerinni Group. Overlain by the Shillinglaw Formation; overlies the Jeromah Formation. Max. Thickness: 1100m. Previously mapped as undifferntiated Tomkinson Creek beds.||||||25-JAN-10
38416|Carruthers Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Namerinni Group. Inc: upper (sandstone and mudstone; stromatolitic bioherms, halite and gypsum pseduomorphs), middle (sst; lithic arenite, mudst)and lower (mudst. and fine-gr.sst)) facies as well as undifferentiated sst, mudst, chert and dolostone.||||||07-NOV-08
38416|Carruthers Formation|24442|5|Briefly described|p14|||Of the Namerinni Group.  Geological Province: Ashburton Province.||||||
38416|Carruthers Formation|50353|5|Briefly described|Map Legend|||Of Namerinni Group||||||
38416|Carruthers Formation|64780|6|Mentioned|p63 Fig.4, p65 |Palaeoproterozoic|Palaeoproterozoic|||Of the Namerinni Group||Is overlain by Shillinglaw Formation.|Dominantly a carbonate-mudstone succession.|
38416|Carruthers Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Namerinni Group.||||
38416|Carruthers Formation|69431|4|Described|p16:14-17, 23|Statherian|Statherian|Tomkinson Province. c.800-1100m thick. Three un-named lithofacies are described in detail. Protected shallow-marine, intertidal, and supratidal deposits in a sabkha environment.||Namerinni Group.||Conformably and transitionally overlies Jeromah Formation. Is overlain conformably by Shillinglaw Formation, and unconformably by Gleeson Formation.|Thinly to medium bedded sandstone, siltstone, quartzose dolostone, dolostone; stromatolitic bioherms, microbialite, evaporite pseudomorphs, nodular and enterolithic chert (probably after gypsum and anhydrite).|12-JUL-16
38416|Carruthers Formation|69673|6|Mentioned|p58|||||Namerinni Group||||
38416|Carruthers Formation|72373|4|Described|iii,p1,36-38,42|Paleoproterozoic|Paleoproterozoic|Geological province: Tomkinson Province. Thickness: 800-1100m in the HELEN SPRINGS mapsheet. Sample 2711445 (HS17TJM071: Fine-grained chert-bearing quartz sandstone; HELEN SPRINGS) yielded interpreted max depositional age of 1688+\-13 Ma. Conformable contact with overlying Shillinglaw Formation indicate significant time gap in zircon MDAs is related to changes in sediment source/pathways rather than hiatus.|1688+\-13 Ma (max dep age)|Unit of Namerinni Group.||Overlain conformably by Shillinglaw Formation. Underlain conformably by Jeromah Formation.|Laminated to medium-bedded sandstone, mudstone, chert and dolostone, with abundant stromatolites and evaporite pseudomorphs in some intervals.|
80344|Casper Suite|71750|4|Described|p1,30,31,33|Statherian|Statherian|Geological province: Aileron Province.Variably metamorphosed intermediate to mafic igneous rocks with protolith ages between ca 1.79-1.77 Ga (Weisheit et al in prep). Interpreted to be syn-depositional with Bonya Metamorphics. A previously analysed sample of 'strongly deformed metapsammite', previously interpreted as a unit from Bonya Metamorphics by Claoue-Long and Hoatson (2005), has been remapped and reinterpreted by NTGS as orthogneiss (compositionally a peraluminous granodiorite) but now considered to be an igneous intrusive into Bonya metasedimentary succession prior to high-grade metamorphism. Sample  is chemically indistinguishable from White Violet Orthogneiss of the Casper Suite, but age is younger.  Sample: GA 1597793 (635159E 7499421N) zircon analysis yields age of 1778+\-6 Ma (interpreted magmatic crystallisation age) and 435+\-10 Ma (Metamorphism/resetting age).|c. 1.79-1.77 Ga||Includes White Violet Orthogneiss.|Conformably interlayered with Bonya Metamorphics.||18-SEP-19
80344|Casper Suite|72370|5|Briefly described|p1,4,26|||Geological province: Aileron Province. Includes 1775+\-5 Ma tonalite dykes (SHRIMP 207Pb/206Pb zircon; Claoue-Long and Hoatson 2005).||||Inrudes Bonya Metamorphics.||
80344|Casper Suite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.||Baikal Supersuite|Includes the Jervois Granodiorite, Cappocks Granodiorite, Xanten Granodiorite, Kings Legend Metadolerite, Attutra Metagabbro and the White Violet Orthogneiss.|||
80344|Casper Suite|72516|2|Defined|p16, p29, p32, p35-56, p101, p198-199|Statherian|Statherian|New name. Is the most abundantly outcropping component of the Baikal Supersuite. Named for the Casper iron-titanium-vanadium prospect in the Jervois Range Special area. See constituent units for type localities. Outcrops in western and central Jervois Range map sheet, north of the Marshall River and south and southeast of the Johansen and Jervois ranges; outcrops generally as poorly exposed and scattered outcrops or low, blocky or rounded outcrops. Includes one unnamed unit. SHRIMP date is interpreted as a magmatic crystallisation age and derived from Kositicin et al (2018). The suite is defined on the basis of geochemical, chronologic and isotopic constraints indicating the constituent units represent a continuum of melt generation in a single heterogenous source over 15 my. Deposited in a continental margin environment. Broadly similar ICE patterns and degree of LREE-enrichment to the Fosters Suite. Comagmatic and cogenetic with the Fosters Suite. Unconformably overlain by the Oorabra Arkose and the Grant Bluff Formation. Metamorphism, structure, alteration, mineralisation, geophysics and geochemistry are discussed. See also p19, p105-106, p108-110, p119-123, p126-127, p188-189, p197, p201, 203, 204, 205, 210, 211.|c. 1.79-1.77 Ga, 1778 +/- 6 Ma (SHRIMP U-Pb)|Baikal Supersuite|Includes the Jervois Granodiorite, Cappocks Granodiorite, Xanten Granodiorite, Kings Legend Metadolerite, Attutra Metagabbro, White Violet Orthogneiss.|Intrudes the Bonya Metamorphics. Intruded by the Tarlton Bore Granite, Boundary Igneous Complex and the Samarkand Pegmatite.|Varied constituents include: metagabbro, metadolerite, granodiorite with subordinate tonalite, diorite, quartz diorite, monzodiorite and quartz monzodiorite.|16-JUN-21
80344|Casper Suite|73591|6|Mentioned|p11, p16, p18|||||Baikal Supersuite||||
37728|Caulfield beds|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|||||||
37728|Caulfield beds|62659|5|Briefly described|Map Legend|Calymmian|Statherian|Medium to very thick bedded, coarse grained, poorly sorted lithic sandstone and matrix supported granule to pebble conglomerate; minor intercalated carbonate, chert and siltstone.||||||
37728|Caulfield beds|65337|3|Fully described|p9 Fig.5, pp34-36. |Mesoproterozoic|Mesoproterozoic|New name. Incorporates outcrops previously mapped as Fickling beds. North-central MOUNT DRUMMOND area. Sedimentation was coeval with tectonism. Detritus sourced from Murphy Metamorphics, Nicholson Granite and Cliffdale Volcanics.|c.1500 Ma.|||Is unconformably overlain by Constance Sandstone.|Lower part has three facies: coarse, with conglomerates and sandstone; fine, with sandstone and siltstone, locally shale; carbonate, patches of  dolostone. Upper part has a sandstone facies, a chert facies, and a fine facies of siltstone and shale.|
37728|Caulfield beds|69434|5|Briefly described|p19:1, 3-4, 6, 8|Mesoproterozoic|Paleoproterozoic|Rawlings et al. (2008). Previously mapped as part of Fickling Group by Smith and Roberts (1963). Bauhinia Dome, South Nicholson Basin. Unassigned to any Group. Over 600m thick. Debris flows and sandy turbidites in shallow to deep marine shelf setting (fan delta); syntectonic deposition. Main sediment sources were Murphy Metamorphics, Nicholson Granite Complex and Cliffdale Volcanics (and possibly Westmoreland Conglomerate). Possible correlative of Crow Formation, or parts of Fickling and McNamara Groups. May have some potential for base metals.||||Is overlain unconformably by Constance Sandstone (Accident Subgroup).|Flat to gently-dipping, unmetamorphosed and not significantly deformed, coarse-grained, poorly-sorted lithic sandstone and matrix-supported conglomerate; minor intercalated carbonate, chert and siltstone.|12-JUL-16
37728|Caulfield beds|69673|4|Described|p55|||Informal name? Up to 600m thick.|||||Lithic sandstone, chert, siltstone and conglomerate with minor intercalated carbonate rocks and siltstone.|
37728|Caulfield beds|72526|5|Briefly described|p8 Fig.1.3, p33, p40, p46, p86.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||||Unconformably overlain by Constance Sandsotne.||
37728|Caulfield beds|72527|4|Described|p1, p3, p9, p161-168, p193, p196-197.|Mesoproterozoic|Mesoproterozoic|Stratigraphic position unclear. Tentatively correlated with Crow Formation. Base not exposed. Contains coarse-grained mass-flow facies, similar to Crow Formation. Displays remarkably similar age spectra to Bowgan Sandstone, Crow Formation and Bullrush Conglomerate. Restricted to an area previously mapped as Fickling beds (Smith and Roberts, 1963). Misspelt as Caufield beds p7.|1634+/-20 Ma max.dep. age.|South Nicholson Group||Unconformably underlies Constance Sandstone, South Nicholson Group.|Sample site: medium-grained feldspathic micaceous (muscovite-biotite and minor secondary chlorite) sublithic gritty to pebbly sandstone with local thin discontinuous pebble lags. Minor rounded tourmaline grains and glauconite are present.|
37728|Caulfield beds|72912|5|Briefly described|p5 Fig.3|Mesoproterozoic|Mesoproterozoic|Located in the Central part of the South Nicholson Basin. Spelt incorrectly as 'Caulfield Beds' on p22, p33 Fig.12.||||Shown as roughly equivalent age to Wildcow Subgroup, South Nicholson Group.||
37728|Caulfield beds|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Isa Superbasin.||Benmara Group||Underlain by and partly equivalent to Bowgan Sandstone. Overlain by and partly equivalent to Mittiebah* Formation. Equivalent to Crow* Formation?||
42259|Celia Dolostone|24442|6|Mentioned|p44|||Contains magnesite deposits.  ||||||
42259|Celia Dolostone|50623|4|Described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Conformably overlies Beestons Formation. Shallow marine to subtidal stromatolitic dolomite and magnesite with minor shale. Of Manton Group.||||||07-NOV-08
42259|Celia Dolostone|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Stromatolitic magnesite, dolomite, stromatolitic silicified carbonate occurring as chert or paraquartzite, rare calcareous para-amphibolite and metapelite. Of Manton Group. Overlies Beestons Formation. Overlain by Crater Formation.||||||
42259|Celia Dolostone|61389|5|Briefly described|Map Legend|||Of the Manton Group. Stromatolitic magnesite, dolomite, some silicified, rare para-amphibolite and metapelite.||||||04-AUG-06
42259|Celia Dolostone|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Of Manton Group. Max. thickness 300m. Stromatolitic magnesite, dolostone, some silicified, rare para-amphibolite and mudstone.||||||07-JAN-09
42259|Celia Dolostone|64730|5|Briefly described|p124, 125 Fig. 3|Paleoproterozoic|Paleoproterozoic|||Of Manton Group.||Overlies Beestons Formation.|Supra- to inter-tidal carbonates.|03-MAY-12
42259|Celia Dolostone|65232|5|Briefly described|p51, p52 Fig. 34|||Of Manton Group. Over Beestons Formation. Shallow-water stromatolitic carbonates. See also Celia Dolomite.||||||09-FEB-10
42259|Celia Dolostone|65339|4|Described|pp7-8.  |||Formerly Celia Dolomite (Malone 1962a, b). 300 - 600 m thick. A palaeokarst surface exists between this unit and the overlying Crater Formation.||Unit in Manton Group.||Overlies Beestons Formation. Is overlain by Crater Formation.|Stromatolitic magnesite and dolostone, stromatolitic silicified carbonate occurring as chert or paraquartzite; rare calcareous para-amphibolite, metapelite.|
42259|Celia Dolostone|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Manton Group.||Overlies Beestons Formation.|Stromatolitic magnesite, dolostone; some silicified, rare para-amphibolite and mudstone.|23-NOV-11
42259|Celia Dolostone|67355|4|Described|p7, p10-11, p47||Neoarchean|?replaced the Celia Dolomite. ~300 m maximum thickness. Outcrop is poor. It is magnesitised and forms irregular to lenticular bodies that have been explored for magnesite. Talc, tremolite and quartz are also present.||Manton Group||Conformably overlies the Beestons Formation. Unconformably underlies the Crater Formation.|Stromatolitic carbonate rocks - silicified dolostone, dolostone or stromatolitic magnesite. Calcareous sandstone, metapelite and para-amphibolite were intersected in BMR stratigraphic drillholes.|25-JAN-17
42259|Celia Dolostone|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen. Correlative of Namoona Group and Cahill Formation.|||||Dolostone, magnesite.|
42259|Celia Dolostone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Upper unit in Manton Group.||Overlies Beestons Formation.||
42259|Celia Dolostone|69418|6|Mentioned|p3:31-32|||Rum Jungle area, Pine Creek Orogen. Hosts widely distributed stratabound magnesite bodies, eg at the Celia deposit (described).||||||12-JUL-16
42259|Celia Dolostone|69420|4|Described|p5:4, 6, 8-9, 30, 75, 114|Paleoproterozoic|Paleoproterozoic|Previously Celia Dolomite. Rum Jungle region, Central Domain, Pine Creek Orogen. Up to 300m thick. Subtidal, evaporitic deposits. Deformed into map-scale folds. Local economic stratabound magnesite deposits.||Manton Group.||Conformably overlies Beestons Formation.|Stromatolitic dolostone and magnesite. Commonly silicified at the surface.|12-JUL-16
42259|Celia Dolostone|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Manton Group.||Conformably overlies Beestons Formation. Is overlain unconformably by Mount Partridge Group.|Stromatolitic magnesite, dolostone; rare para-amphibolite and mudstone, locally silicified.|
41993|Cement Dam Gneiss|9199|5|Briefly described|Map legend|||Porphyroblastic gneiss.  Geological Province: Arunta Block.||||||04-NOV-04
41993|Cement Dam Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Porphyroblastic gneiss.||||||
41993|Cement Dam Gneiss|69427|6|Mentioned|p12:14, 30-31|||Wigley Domain, Aileron Province. The biotite granite of this unit has strong affinities with Trephina Granitic Gneiss, 10km to the E.||||||12-JUL-16
38832|Century Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Ware Group. Sandstone, siltstone.||||||09-MAR-10
38832|Century Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Ware Group. Geological Province: Tanami Inlier. Quartz arenite, fine grained lithic arenite, siltstone, granule and pebble conglomerate.||||||07-NOV-08
38832|Century Formation|63261|3|Fully described|p9 Fig. 5, p13, p14|Paleoproterozoic|Paleoproterozoic|Of the Ware Group. Previously mapped as Pargee Sandstone (explained in detail, p13). Faulted contact with Wilson Formation in west. Max. dep. Age: 1823+/-4Ma (SHRIMP U-Pb, Cross and Crispe 2006). Thickness: ~1200m. Detailed lith. Included.||||||07-FEB-11
38832|Century Formation|64662|5|Briefly described|p29 Fig. 2, p30 Fig. 3, p37-38|Orosirian|Orosirian|Of the Ware Group. Detrital zircons in lithic arenite from this unit give maximum depositional age: ca.1823+/-4Ma. Geological Province: Tanami region.||||||07-FEB-11
38832|Century Formation|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1815 Ma.|Unit in Ware Group.||||02-APR-12
38832|Century Formation|64733|6|Mentioned|p170 Fig.2|Orosirian|Orosirian|Presented as Wilson and Century Formation|~1815 Ma.|Of Ware Group.||||20-APR-12
38832|Century Formation|64734|6|Mentioned|p186 Fig.1|||Ca. 1815 Ma. Presented as Wilson and Century Formation. Of Ware Group.||||||14-SEP-09
38832|Century Formation|65359|6|Mentioned|p1|||Tanami Region. In Ware Group.||||||
38832|Century Formation|66129|6|Mentioned|p214 Fig.1|Orosirian|Orosirian|1815 Ma. Unit in Ware Group.||||||
38832|Century Formation|67824|6|Mentioned|p385 Fig.2|Orosirian|Orosirian||~ 1815 Ma |Unit in Ware Group.||||
38832|Century Formation|67826|6|Mentioned|p401 Fig.2|Orosirian|Orosirian||~ 1815 Ma|Of the Ware Group.||||
38832|Century Formation|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1815 ma|Ware Group||||
38832|Century Formation|69426|4|Described|p11:3-5, 8, 11, 14|||Rapidly submerging shoreface, or fluvial and lacustrine. c.1200m thick. Includes parts of the exposures that were previously assigned to the Pargee Sandstone in north-central MCFARLANE sheet area. Affected by the Pargee Fault. SHRIMP U-Pb (detrital) zircon maximum depositional age.|<1823 +/- 4 Ma (Cross and Crispe, 2007).|Ware Group.||Is overlain unconformably by Pargee Sandstone. Is faulted against Wilson and Killi Killi Formations.|Quartz sandstone, fine-grained lithic sandstone, siltstone and granule to pebble conglomerate.|12-JUL-16
38832|Century Formation|70291|4|Described|p178,180|Orosirian|Orosirian|Geological province: Tanami. Age inferred from regional relationships.|1825-1815 Ma.|Unit of Ware Group.|||Conglomeratic sandstone, siltstone and fine-grained sandstone|
38832|Century Formation|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. ||Unit of Ware Group||||
38832|Century Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Ware Group.|||Quartz sandstone, fine-grained lithic sandstone, siltstone, granule and pebble conglomerate.|
38832|Century Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, arenite|
38832|Century Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1823+/-4 Ma (MDA: U-Pb zircon SHRIMP)|Ware Group.|||Lithic arenite.|
38832|Century Formation|73089|6|Mentioned|p8|||||Ware Group||||
26298|Chabalowe Formation|12891|5|Briefly described|p733 Fig. 2|Middle Cambrian|Middle Cambrian|Geological province: SW Georgina Basin.||||||07-FEB-11
26298|Chabalowe Formation|12951|5|Briefly described|p148|||SW Georgina Basin. Age presumably Late Cambrian if lateral equivalent to Arrinthrunga Formation.||||Overlies Arthur Creek Formation. Lateral equivalent of Arrinthrunga Formation.|Terrigenous quartz sandstone with minor siltstone and dolostone.|
26298|Chabalowe Formation|22954|6|Mentioned|Fig3p9|Middle Cambrian|Ordian-Early Templetonia|||||||
26298|Chabalowe Formation|23809|5|Briefly described|p33|Middle Cambrian|Middle Cambrian|Unconformably overlies Barrow Creek Granite.||||||
26298|Chabalowe Formation|24442|5|Briefly described|p45|Late Cambrian|Late Cambrian|Includes the Hagen Member.  Equivalent to basal Arrinthrunga Formation.||||||07-MAY-13
26298|Chabalowe Formation|41204|6|Mentioned|p13|||||||||
26298|Chabalowe Formation|41524|2|Defined|p37|Middle Cambrian||Fully described p18.||||||04-AUG-06
26298|Chabalowe Formation|41525|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Includes the Hagen Member.  Quartz sandstone; ferruginised, with chert in outcrop; dolomitic with siltstone and dolostone interbeds at depth.||||||26-OCT-05
26298|Chabalowe Formation|42059|6|Mentioned|Fig.2 P131|||||||||
26298|Chabalowe Formation|42643|3|Fully described|p30|Middle Cambrian||||||||
26298|Chabalowe Formation|42644|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Quartz arenite, dolomitic, thin bedded; interbeds of dolostone and siltstone, stromatolitic. Geological Province: Georgina Basin.||||||15-NOV-05
26298|Chabalowe Formation|42956|5|Briefly described|p31 Fig.4|||||||||
26298|Chabalowe Formation|47058|6|Mentioned|p135|||||||||
26298|Chabalowe Formation|60122|5|Briefly described|p57 Appendix|||Contains the Hagen Member.  Conformably overlies Arthur Creek Formation.  Potential oil reservoir.||||||
26298|Chabalowe Formation|60123|4|Described|p5|Cambrian|Cambrian|Thickness: 342m. Conformably underlies Arrinthrunga Formation; conformably overlies Arthur Creek Formation; disconformably overlies: Hatches Creek Group. Dolomitic quartz sandstone.||||||26-OCT-05
26298|Chabalowe Formation|60675|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Underlies Arrinthrunga Formation; overlies Arthur Creek Formation; contains Hagen Member. Quartz sandstone, dolomitic, with siltstone and dolostone interbeds.||||||
26298|Chabalowe Formation|61388|5|Briefly described|Map Legend|Cambrian|Cambrian|Surface expression restricted to ferruginous chert and sandstone rubble; alteration of a carbonate -bearing sucession at depth. Geological Province: Georgina Basin.||||||05-OCT-05
26298|Chabalowe Formation|61404|5|Briefly described|Map legend|Late Cambrian|Early Cambrian|Of the Narpa Group. Quartz arenite: dolomitic; interbeds of dolostone and siltstone, stromatolitic. Geological Province: southern Georgina Basin.||||||26-OCT-05
26298|Chabalowe Formation|62082|6|Mentioned|p70|Cambrian|Cambrian|Geological Province: Georgina Terrain.||||||07-FEB-11
26298|Chabalowe Formation|62789|5|Briefly described|p129 Fig. 2|Late Cambrian|Late Cambrian|Southern Georgina Basin.|||Includes Hagen Member.|Overlies Middle Cambrian Arthur Creek Formation.||28-MAR-12
26298|Chabalowe Formation|64068|3|Fully described|p65-66, p56, 62, 67, 69, 81, 89, p93-94|Late Cambrian|Late Cambrian|Conformably overlain by and partially lateraly interdigitates with Arrinthrunga Formation.||Of Narpa Group.|Includes Hagen Member at base.|Conformably overlies Arthur Creek Formation. Disconformable over Neutral Junction Formation, unconformable over Hatches Creek Group.|Dolomitic quartz sandstone and siltstone, intraformational breccia; minor dolostone, mudstone; basal arkosic conglomerate. Capped by Cenozoic calcrete.|04-APR-12
26298|Chabalowe Formation|64443|6|Mentioned|p18|Late Cambrian||||||Conformably underlies Arrinthrunga Formation.||14-MAY-14
26298|Chabalowe Formation|64778|6|Mentioned|p13|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin.||||||
26298|Chabalowe Formation|64812|4|Described|p236, p240 Fig.6, p245-6|Late Cambrian|Late Cambrian|Contains basal Hagen Member.Unconformable over Arthur Creek Fm and/or Steamboat Sandstone. Geol. Prov: Georgina Basin. Peritidal sediments formed by aggradation of a complex carbonate/evaporite/siliciclastic succession. Detailed lithology included.||||||07-FEB-11
26298|Chabalowe Formation|64813|5|Briefly described|p254, p255, p256 Fig. 2|Late Cambrian|Late Cambrian|Contains the Hagen Member. Overlain by Arrinthrunga Formation. Geological province: Georgina Basin. Peritidal deposits formed by aggradation of a complex carbonate/evaporite/siliciclastic succession of carbonate rocks and red beds.||||||07-MAY-13
26298|Chabalowe Formation|65237|5|Briefly described|p3 Fig. 4, p9|Late Cambrian|Late Cambrian|Contains the Hagen Member. Overlies Arthur Creek Fm with sharp contact; some interfingering with Arrinthrunga Fm in east. Geological province: Georgina Basin. Comprises red beds overlying the basal Hagen Member. Forms regional seal.||||||07-FEB-11
26298|Chabalowe Formation|65338|6|Mentioned|p66.|||||||Locally overlies Central Mount Stuart Formation.||
26298|Chabalowe Formation|65341|4|Described|p2 Fig.2, p5, p18.|Late Cambrian|Late Cambrian|Poorly preserved. Deposition probably occurred in a restricted marine or marginal marine sabkha environment.||Unit in Narpa Group.||Unconformably overlies Octy and Central Mount Stuart Formations. Is conformably overlain by Arrinthrunga Formation.|Surface: ferruginous chert rubble and sandstone; chert displays relict carbonate textures and stromatolites; subsurface in BARROW CREEK: interbedded dolostone, sandstone, mudstone and evaporite; stromatolites common.|
26298|Chabalowe Formation|65342|5|Briefly described|p7.|||Georgina Basin. Max. thickness at least 279 m.|||||Quartz arenite, dolomitic; interbeds of stromatolitic dolostone and siltstone.|
26298|Chabalowe Formation|65489|6|Mentioned|p127|Middle Cambrian|Middle Cambrian||||Includes Hagen Member.|||
26298|Chabalowe Formation|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.||Narpa Group.||Is overlain by Arrinthrunga Formation.|Quartz sandstone.|
26298|Chabalowe Formation|69206|6|Mentioned|p2|||Georgina Basin.|||Hagen Member.|||
26298|Chabalowe Formation|69437|5|Briefly described|p22:10, 15|Cambrian|Cambrian|Southern Georgina Basin.|||Hagen Member.|Overlies Arthur Creek Formation. Is overlain by Arrinthrunga Formation.||12-JUL-16
26298|Chabalowe Formation|69443|4|Described|p28:7, 14-19, 35, 45-47|Late Cambrian|Middle Cambrian|Morris et al. in Stidolph et al. (1988). Southern Georgina Basin. Poorly exposed as low rises, mainly of ferruginised sandstone. Up to 342m thick. Nearshore, restricted marine to peritidal (including hypersaline sabkha) deposits. Interdigitates with the overlying Arrinthrunga FZ. Red beds in the upper part of the Formation are potential regional seals. Has had hydrocarbon shows in drilled wells.||Narpa Group.|Hagen Member.|Overlies Arthur Creek Formation conformably; Neutral Junction and ?Octy Formations (Shadow Group) disconformably; Hatches Creek Group unconformably. Is overlain conformably by Arrinthrunga Formation.|Evaporitic, medium to coarse, cross-bedded, dolomitic, quartz and siliciclastic sandstones, commonly with intraformational breccias, and minor quartzose, silty and peloid-intraclast dolostone and mudstone. Local basal arkosic conglomerate.|12-JUL-16
26298|Chabalowe Formation|69561|6|Mentioned|p33 fig 2|Idamean|Mindyallan|||||Overlain by Arrinthrunga Formation, overlies Arthur Creek Formation||
26298|Chabalowe Formation|69673|4|Described|p117, p123, p126, p127, p129, p137|Cambrian|Cambrian |342m thick. Also overlain by Tomahawk Formation, Ninmaroo Formation, Swift Formation.||Narpa Group|Includes Hagen Member|Conformably overlain by Arrinthrunga Formation, conformably overlies Arthur Creek Formation, disconformably overlies Neutral Junction Formation|Evaporitic dolomitic quartz sandstone and dolomitic siliciclastic siltstone, commonly with intraformational breccias; minor dolostone and mudstone.|
26298|Chabalowe Formation|70380|6|Mentioned|p745|Series 4|Series 3|Southern Georgina Basin.||||||
26298|Chabalowe Formation|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Narpa Group|Includes Hagen Member|Overlies Arthur Creek Formation. Is overlain by Arrinthrunga Formation.||
26298|Chabalowe Formation|70951|6|Mentioned|p1069, 1074, 1077, 1082|||Geological province: Georgina Basin.||Unit of Narpa Group.|Includes Hagen Member.|||
26298|Chabalowe Formation|72321|5|Briefly described|Fig 2, p6 Fig 3, p7|Guzhangian|Guzhangian|Elkedra Shelf/Dulcie Syncline, Georgina Basin. Australian Stages: Boomerangian to Mindyallan. ||of Narpa Group.|Includes Hagen Member.|Overlies Arthur Creek Formation in MacIntyre 1, Ross 1. May correlate with Steamboat Sandstone.||
26298|Chabalowe Formation|72516|6|Mentioned|p93|Cambrian|Cambrian|Southwestern and southern Georgina Basin.||||Equivalent to the Arrinthrunga Formation.||
26298|Chabalowe Formation|73288|5|Briefly described|p697-698|Middle Cambrian|Middle Cambrian|||Narpa Group.|Hagen Member.|Overlies Arthur Creek Formation.|Peritidal sediments formed by aggradation of carbonate, evaporite and siliciclastic sediments.|
27739|Chandler Formation|12891|5|Briefly described|p733 Fig. 2|Early Cambrian|Early Cambrian|Geological province: Amadeus Basin.||||||07-FEB-11
27739|Chandler Formation|22560|5|Briefly described|p3||Early Cambrian|||||||
27739|Chandler Formation|22561|4|Described|p21|Neoproterozoic|Neoproterozoic|||||||
27739|Chandler Formation|22563|6|Mentioned|p55|||||||||
27739|Chandler Formation|22564|5|Briefly described|p59||Cambrian|||||||
27739|Chandler Formation|22565|6|Mentioned|p71 in Table 1|||Thickness at Areyonga Creek measured from surface expression 300m thick.  Approx. thickness measured from seismic data 330m.||||||
27739|Chandler Formation|22566|4|Described|p83|Cambrian|Cambrian|informally devided into upper and lower Chandler Formation. Of the Pertaoorrta Group.||||||19-APR-06
27739|Chandler Formation|22646|6|Mentioned|p 100|Middle Cambrian|Middle Cambrian|||||||
27739|Chandler Formation|22649|6|Mentioned|Fig 1 on p 138||Cambrian|||||||
27739|Chandler Formation|22650|4|Described|p 159|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||19-APR-06
27739|Chandler Formation|22651|4|Described|p183|Middle Cambrian||Max age ?Early Cambrian p171.  The basal contact of the Chandler Formation is unconformable.||||||
27739|Chandler Formation|22652|5|Briefly described|p 195|||||||||
27739|Chandler Formation|22653|4|Described|p 227-243||Early Cambrian|Chandler Formation lacks age diagnostic fossils (p228).||||||04-AUG-06
27739|Chandler Formation|22654|5|Briefly described|p 245|||||||||
27739|Chandler Formation|22656|6|Mentioned|Fig 5 on p 283|||||||||
27739|Chandler Formation|22762|4|Described|p369|Cambrian|Cambrian|Informally devided into upper and lower Chandler Formation (p375).||||||04-AUG-06
27739|Chandler Formation|22763|6|Mentioned|Table 1 on p386|Cambrian|Cambrian|Of the Pertaoorrta Group.||||||19-APR-06
27739|Chandler Formation|22804|6|Mentioned|p450|||||||||
27739|Chandler Formation|22805|5|Briefly described|p464 & p475||Early Cambrian|Bedded evaporites within the Chandler Formation are considered to be a possible seal for the Arumbera Sandstone in the eastern area of the Amadeus Basin.||||||19-APR-06
27739|Chandler Formation|22807|6|Mentioned|p494||Cambrian|||||||
27739|Chandler Formation|22823|4|Described|p517||Cambrian|||||||
27739|Chandler Formation|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
27739|Chandler Formation|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic|||||||
27739|Chandler Formation|23981|5|Briefly described|p10 Fig. 5, p74|Toyonian|Toyonian|Geological Province: Amadeus Basin (NT).||||||12-JUL-06
27739|Chandler Formation|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
27739|Chandler Formation|30540|6|Mentioned|p61|||Presence of thick salt deposits||||||
27739|Chandler Formation|34186|6|Mentioned|Fig.3|||See also Figs.4,8.||||||
27739|Chandler Formation|40740|3|Fully described|p30|||Mention p5.||||||04-AUG-06
27739|Chandler Formation|41039|6|Mentioned|p8|||||||||
27739|Chandler Formation|41115|6|Mentioned|p1390|||||||||
27739|Chandler Formation|41190|6|Mentioned|Fig.4|||||||||
27739|Chandler Formation|41233|6|Mentioned|p17|||||||||
27739|Chandler Formation|41270|6|Mentioned|p271|||||||||
27739|Chandler Formation|41717|6|Mentioned|p349|||See also p355.||||||04-AUG-06
27739|Chandler Formation|41801|6|Mentioned|p214|||||||||
27739|Chandler Formation|42058|6|Mentioned|p122|||||||||
27739|Chandler Formation|42059|6|Mentioned|p133|||See also Fig.2||||||
27739|Chandler Formation|42060|6|Mentioned|Fig.5 P140|||||||||
27739|Chandler Formation|42082|6|Mentioned|Fig.3 P323|||||||||
27739|Chandler Formation|42886|5|Briefly described|Fig.2 P219|||||||||
27739|Chandler Formation|42940|5|Briefly described|Plate 8|||||||||
27739|Chandler Formation|43105|6|Mentioned|p8|||||||||
27739|Chandler Formation|43225|5|Briefly described|Map Legend||Cambrian|Of the Pertaoorrta Group||||||19-APR-06
27739|Chandler Formation|43503|6|Mentioned|11-50|Ordian|Botoman|||||||
27739|Chandler Formation|43646|6|Mentioned|Fig.3,p554||Middle Cambrian|||||||
27739|Chandler Formation|44133|5|Briefly described|p4 Fig. 7.2, 42|Early Cambrian|Early Cambrian|Geological Province: Western Warburton Basin.||||||
27739|Chandler Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
27739|Chandler Formation|61732|5|Briefly described|p99|Cambrian|Cambrian|Together with other Cambrian units overlies the Arumbera Sandstone.||||||07-FEB-11
27739|Chandler Formation|62376|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
27739|Chandler Formation|62379|5|Briefly described|p7 Fig. 2, p22|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Limestone, dolostone and chert. Geological Province: Amadeus Basin.||||||
27739|Chandler Formation|64068|6|Mentioned|p59, 225|||Amadeus Basin. Correlated with Thorntonia Limestone.||||||
27739|Chandler Formation|64778|6|Mentioned|p13, 27|Cambrian|Cambrian|Amadeus Basin. Potential hydrocarbon source.||||||
27739|Chandler Formation|64809|5|Briefly described|p2, p3 Fig.2 |Middle Cambrian|Middle Cambrian|May seal the underlying Arumbera Sandstone.||Unit in Pertaoorrta Group.|||Shales.|
27739|Chandler Formation|64813|5|Briefly described|p272|Middle Cambrian|Middle Cambrian|Overlain by Giles Creek Dolostone. Geological province: Amadeus Basin, N.T. Dominated by halite and other evaporitic minerals (anhydrite, gypsum), but contains discrete carbonate and siliciclastic units. ||||||
27739|Chandler Formation|65233|5|Briefly described|p3 Fig. 2, p7|Middle Cambrian|Early Cambrian|Of Pertaoorrta Gp. Disconformable on Arumbera Sst and Chandler Fm [???can't overlie itself] . Max. thickness: >1000m. Geol province: Amadeus Basin. Carbonate+evaporite succession potential as petroleum source rock. Detailed lithology, depositional environment information included.||||||07-FEB-11
27739|Chandler Formation|65342|5|Briefly described|p4.|||Amadeus Basin. Max. thickness at least 213 m.||||Overlies Todd River Dolostone (equivalent). Is overlain by Giles Creek Dolostone.|Limestone, dolostone, chert.|
27739|Chandler Formation|65489|5|Briefly described|p125|Cambrian|Cambrian|Amadeus Basin.||Unit in Pertaoorrta Group.||Overlies Todd River Dolomite.||
27739|Chandler Formation|67326|5|Briefly described|p2, p5|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Eninta Formation, Arumbera Sandstone and ?Todd River Dolostone. Is overlain by Tempe Formation (disconformably); also Hugh River Shale and Giles Creek Dolostone (and probably interfingers).||
27739|Chandler Formation|67856|6|Mentioned|p338 fig 4-30, p349|Cambrian|Cambrian|Central Amadeus Basin.||Of Pertaoorta Group.||||
27739|Chandler Formation|68323|6|Mentioned|p4 Fig.2|Middle Cambrian||Amadeus Basin.||Pertaoorrta Group.||||
27739|Chandler Formation|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Amadeus Basin, Centralian B Superbasin. Sequence 1.||||Overlies Namatjira Formation. Underlies Tempe Formation, Hugh River Shale. Equivalent to Negri Subgroup; Tarrara, Gum Ridge, Border Waterhole Formations; Thorntonia, Tindall, Top Springs Limestones.|Evaporites, carbonate mudstone, shale and siltstone.|12-JUL-16
27739|Chandler Formation|69438|4|Described|p23:2-3, 6, 24, 28-30, 42, 59-61|Middle Cambrian|Early Cambrian|Originally the Chandler Limestone (Ranford et al., 1965). Amadeus Basin. Widespread; generally poorly outcropping. Lithologies and thickness are variable. Deposition was probably in a shallow-water, deep dessicated basin. Lateral equivalent of lower Giles Creek Dolostone. Contains some small domical stromatolites but no diagnostic fossils. Associated with halotectonics, especially in the NE of the Basin. Hydrocarbon source rock intervals may be present. Forms a salt seal over Arumbera Sandstone reservoirs.||Pertaoorrta Group.||Disconformably overlies Namatjira, Areyonga and Bitter Springs Formations and Arumbera Sandstone. Is overlain dis/unconformably by Tempe Formation, Hugh River Shale or upper Giles Creek Dolostone .|Halite, foetid carbonate mudstone, shale and siltstone.|12-JUL-16
27739|Chandler Formation|69439|6|Mentioned|p24:10|||Amadeus Basin.||||||12-JUL-16
27739|Chandler Formation|69449|6|Mentioned|p34:2 Fig.34.2; 34:4|Cambrian|Cambrian|Eastern Amadeus Basin. Has equivalent rocks in the western Warburton Basin.||||||12-JUL-16
27739|Chandler Formation|69606|6|Mentioned|p2|||||||||
27739|Chandler Formation|69673|5|Briefly described|p76, p82, p91, p98, p102, p149 fig 120|||Marine evaporitic succession. Variable thicknesses throughout the basin.||||Disconformably overlain by Tempe Formation, Hugh River Shale, Giles Creek Dolostone, Disconformably overlies Arumbera Sandstone, Namatjira Formation, Areyonga Formation, Bitter Springs Formation|Halite, foetid carbonate mudstone, shale and siltstone.|
27739|Chandler Formation|71114|4|Described|p171, p170 fig 1b, p172-4, 176-180|Stage 5|Stage 4|Amadeus Basin eastern succession etc. Deposited between ~511 and 490 Ma. The evaporites (mostly halite) and the foetid carbonate rocks represent deposition under subaqueous to anoxic conditions. 310m thick in Dingo 1 well.||||Overlies Todd River Dolostone. Overlain by Giles Creek Dolostone. In part age equivalent to Tempe Formation.|Characterised by a thick salt unit (restricted to eastern basin) and carbonate rocks (extend to western/central basin),|14-FEB-18
27739|Chandler Formation|71279|5|Briefly described|p355 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
27739|Chandler Formation|72358|6|Mentioned|p118|Series 3|Series 2|Of Amadeus Basin.||||||
27739|Chandler Formation|72516|6|Mentioned|p91|Cambrian|Cambrian|Amadeus Basin. Age equivalent of the Thorntonia Limestone.||||||02-JUN-21
27739|Chandler Formation|73085|6|Mentioned|p1|middle Cambrian|middle Cambrian|||Pertaoorrta Group [and equivalents?]||Partly underlain by Winnall Group and Arumbera Sandstone. Overlain by Hugh River Shale. Overlain by and partly equivalent to Tempe Formation and Giles Creek Dolostone.||
29239|Charles River Gneiss|9199|5|Briefly described|Map legend|||Garnet-bioite-quartz-feldspar gneiss, amphibolite.  Geological Province: Arunta Block.||||||04-NOV-04
29239|Charles River Gneiss|23361|5|Briefly described|32 Fig.17|||||||||
29239|Charles River Gneiss|41664|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
29239|Charles River Gneiss|41816|4|Described|p12|||||||||
29239|Charles River Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Garnet-biotite-quartz-feldspar gneiss, amphibolite.||||||
29239|Charles River Gneiss|61309|6|Mentioned|p32 Fig. 17|||In the Bond Springs region.||||||06-FEB-08
29239|Charles River Gneiss|69427|5|Briefly described|p12:14-15, 31|||Wigley Domain, Aileron Province. Largely fault-bound unit N of Alice Springs.|||||Characterised by a relative abundance of garnet-bearing gneiss of possible metasedimentary origin, with lesser layered biotite gneiss and amphibolite. Locally migmatitic.|12-JUL-16
79087|Chiripee Metamorphics|68997|4|Described|vi-vii,p1,37-43|Orosirian|Orosirian|Granulite-facies, predominantly metasedimentary rocks that outcrop as locally extensive low-lying domes and pavements to the north of the Bleechmore Metamorphics in south-central ALCOOTA. Similar stratigraphic position to Lander Rock Formation. Zircon age spectra of 1834+\-15 Ma and 1824+\-11 Ma for psammitic (Sample: AC09EEB767. Grid Reference: MGA94 Zone 53: 412363mE 7498176mN) and pelitic components (Sample: AC08LCV819. Grid Reference: MGA94 Zone 53: 427345mE 7490721mN), interpreted as maximum depositional ages. Zircon rims from pelitic migmatite yield  1554+\-12 Ma age, representing a marginally younger late Chewnings thermal event.|1834+\-15 Ma (max dep age: U-Pb zircon)||||Migmatitic metasedimentary (pelitic and psammitic) gneisses interlayered with metamafic intrusions.|
79087|Chiripee Metamorphics|69917|5|Briefly described|p75-79, 109|Mesoproterozoic|Paleoproterozoic|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Migmatitic metapelite sampled. 1824+/-11 Ma is interpreted as the maximum depositional age. Metamorphic rims: 1554 Ma, during Chewings Orogeny. Metapsammite sampled gave 1834+/-15 Ma as the maximum depositional age of the precursor sediments.|1824+/-11 Ma max, 1554 Ma min.||||Migmatitic metasedimentary gneisses (metapelitic and metapsammitic) interlayered with metamafic intrusive rocks.|
79087|Chiripee Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Ages of maximum deposition and metamorphism respectively; both U-Pb zircon SHRIMP ages.|1824+/-11 Ma; 1554+/-12 Ma.||||Migmatite, metapsammite.|
79227|Chookla Member|71898|5|Briefly described|p8|||Amadeus Basin. Outcrops on the HENBURY map sheet. Similar provenance spectra to Quandong Conglomerate.||Puna Kura Kura Formation||||19-NOV-18
79227|Chookla Member|72369|4|Described|iii,p3-4,20,23-26|||Of Amadeus Basin. Presently restricted to southwesternmost HENBURY mapsheet; relationship with Puna Kura Kura Formation is not well understood. Exposures have been previously mapped as Winnall beds or Pertaoorrta Group (Ranford 1965). LA-ICP-MS U-Pb detrital zircon dating of sample HB15VJN268 (very coarse-grained quartz arenite) yielded an interpreted maximum depositional age of 620+\-5 Ma (youngest concordant zircon), but does not further constrained the depositional age of the Puna Kura Kura Formation (or Chookla Member) as this age predates the MDAs of the underlying Gloaming and Liddle formations. Paleoproterozoic detrital zircon spectrum was likely recycled from underlying Amadeus basin succession and/or derived from Aileron and Warumpi Provinces. Also contains a dominant Musgrave Province source (c. 1440Ma to c. 1005 Ma age spectrum). ||Unit of Puna Kura Kura Formation.|||Poorly sorted, Pebble to cobble, polymictic orthoconglomerate.|
79227|Chookla Member|73119|5|Briefly described|p12|||||Puna Kura Kura Formation, Winnall Group|||Poorly sorted, clast- to matrix-supported conglomerate with pebble-, cobble- and small boulder-size clasts of quartzite, vein quartz, and minor basement rock.|
79227|Chookla Member|73279|5|Briefly described|p3, p9|Ediacaran|Cambrian|Amadeus Basin. Detrital zircons analysed for Hf isotopic composition [see article].||Puna Kura Kura Formation, Winnall Group|||Conglomeritic; includes sandstone.|
28454|Chuall beds|43631|6|Mentioned|p27|||||||||
28454|Chuall beds|45155|6|Mentioned|p42|||||||||
28454|Chuall beds|65074|4|Described|p351, p355 Tb.4-11, p358-360, p362|Devonian|Devonian|Of NW Birrindudu Basin. 140 m thick. Type area is SE of Sturt Creek Homestead. Non-fossiliferous.||||Probably overlies Redcliff Pound Group (unconformably). Probably equivalent to Pedestal beds.|Friable quartzose sandstone. Pellet-rich horizons and gritty bands.|
42362|Cleia Formation|5952|5|Briefly described|p217|||Of Gorter and Kirk (1995).||||||05-MAY-09
42362|Cleia Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Late Jurassic|Geological Province: Bonaparte Basin.||||||10-DEC-04
42362|Cleia Formation|64689|5|Briefly described|p7 Fig.6 |Late Jurassic|Late Jurassic|||||||
42362|Cleia Formation|64696|6|Mentioned|p127 Fig.2, p131, p138|||||||Interfingers with Lower Vulcan Formation.|Thick shale unit.|
42362|Cleia Formation|69452|5|Briefly described|p36:15, 21-22|Late Jurassic|Middle Jurassic|Bonaparte Basin. Appears as "lower Frigate Sh/Cleia Fm".||?Flamingo Group.||||12-JUL-16
42362|Cleia Formation|69673|6|Mentioned|p173|||||Flamingo Group||||
42362|Cleia Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Overlies Laminaria Formation.||
28456|Cleland Sandstone|22561|5|Briefly described|p25|Neoproterozoic|Neoproterozoic|Ibirriki Sub-basin||||||
28456|Cleland Sandstone|22566|6|Mentioned|Fig 6 on p82|Late Cambrian|Cambrian|Of the Pertaoorrta Group.||||||04-AUG-06
28456|Cleland Sandstone|22650|6|Mentioned|p 159|Cambrian|Cambrian|||||||
28456|Cleland Sandstone|22651|6|Mentioned|p 171|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group.||||||04-AUG-06
28456|Cleland Sandstone|22652|6|Mentioned|p 195|||||||||
28456|Cleland Sandstone|22655|6|Mentioned|p 254|||||||||
28456|Cleland Sandstone|22657|6|Mentioned|p 288|||||||||
28456|Cleland Sandstone|22760|6|Mentioned|p335|||||||||
28456|Cleland Sandstone|22763|6|Mentioned|p400|||||||||
28456|Cleland Sandstone|22804|6|Mentioned|p445||Cambrian|Of the Pertaoorrta Group.||||||04-AUG-06
28456|Cleland Sandstone|22805|6|Mentioned|p464||Early Cambrian|||||||
28456|Cleland Sandstone|22807|6|Mentioned|p500|Middle Cambrian|Early Cambrian|Of the Pertaoorrta Group.||||||04-AUG-06
28456|Cleland Sandstone|22826|6|Mentioned|p572|Cambrian|Cambrian|||||||
28456|Cleland Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Neoproterozoic III|||||||
28456|Cleland Sandstone|33307|6|Mentioned|Fig.6|||||||||
28456|Cleland Sandstone|33738|6|Mentioned|p47|||||||||
28456|Cleland Sandstone|34442|5|Briefly described|Table 1|||Cambrian.||||||04-AUG-06
28456|Cleland Sandstone|35102|6|Mentioned|Fig.2|||||||||
28456|Cleland Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
28456|Cleland Sandstone|40740|3|Fully described|p32|||Mention p5.||||||04-AUG-06
28456|Cleland Sandstone|40810|5|Briefly described|p13|||Mention p3.||||||04-AUG-06
28456|Cleland Sandstone|41039|6|Mentioned|p11|||||||||
28456|Cleland Sandstone|41190|6|Mentioned|Fig.4|||||||||
28456|Cleland Sandstone|41270|6|Mentioned|p272|||See also Table 1||||||
28456|Cleland Sandstone|41621|5|Briefly described|Map legend|Cambrian||||||||
28456|Cleland Sandstone|41717|6|Mentioned|Fig.2|||||||||
28456|Cleland Sandstone|41723|6|Mentioned|Map legend|Neoproterozoic||||||||
28456|Cleland Sandstone|41819|6|Mentioned|Map legend|Cambrian||||||||
28456|Cleland Sandstone|41820|4|Described|p7|||||||||
28456|Cleland Sandstone|42049|5|Briefly described|p216|||||||||
28456|Cleland Sandstone|42082|6|Mentioned|Fig.3 P323|||||||||
28456|Cleland Sandstone|42940|5|Briefly described|Plate 2|Cambrian|Cambrian|Sandstone, pebbly sandstone, siltstone.  Age: 590-500Ma.  Geological Province: Amadeus Basin.||||||06-FEB-08
28456|Cleland Sandstone|43503|6|Mentioned|12-50|Mindyallan|Undillan|||||||
28456|Cleland Sandstone|44395|14|Not recorded|p.8,10,11, Tb.2||Cambrian|Mid-Upper Cambrian.||||||
28456|Cleland Sandstone|44396|5|Briefly described|map legend|||(Cambrian). SF/52-15.||||||
28456|Cleland Sandstone|44402|5|Briefly described|map legend||Cambrian|Part of Pertaoorrta Group.||||||02-DEC-04
28456|Cleland Sandstone|44439|14|Not recorded|p.7|||Possibly eqiv.to Maurice Formation on Rawlinson (G52-1).||||||
28456|Cleland Sandstone|44493|4|Described|p.11, map||Cambrian|Bloods Range sheet. (G53-3). See p.8,12,13, for details.||||||22-DEC-09
28456|Cleland Sandstone|44494|14|Not recorded|map legend||Cambrian|||||||
28456|Cleland Sandstone|44505|14|Not recorded|p.7,8,10, Table 1||Cambrian|Of Pertaoorrta Group.||||||
28456|Cleland Sandstone|44506|14|Not recorded|map legend||Cambrian|||||||
28456|Cleland Sandstone|45041|5|Briefly described|p56|||Mid.- Upper Cambrian. Refers Wells et al. (1965)||||||
28456|Cleland Sandstone|45170|6|Mentioned|p23|||||||||
28456|Cleland Sandstone|48862|2|Defined|p.36|||On many pages. p.8-20,24,27,36,39-43; Pl.3,8-11. Cambrian deltaic sediments.||||||
28456|Cleland Sandstone|48863|2|Defined|p.13|||Tb.1. opp.p.7, p.12,15,24,37, Pl.9,10,13,15. (G52-4). ?Cambrian.||||||
28456|Cleland Sandstone|48864|2|Defined|p.31|||Tb.1. On many pages. p.1,9,10,27,28,30,33,37,44,47,50,Pl.11. Cambrian-?L.Ordovician. (G52-3).||||||
28456|Cleland Sandstone|48865|14|Not recorded|Fig.4.opp.p.10|||(G52-4).||||||
28456|Cleland Sandstone|48963|6|Mentioned|Fig.3|||||||||
28456|Cleland Sandstone|60674|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Pertaoorrta Group.  Fine-grained pebbly, ferruginous sandstone, locally micaceous and feldspathic. Geological Province: Amadeus Basin.||||||12-JAN-05
28456|Cleland Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
28456|Cleland Sandstone|61385|5|Briefly described|Map legend|Cambrian|Cambrian|Sandstone, pebbly sandstone.  Geological Province: Amadeus Basin.||||||
28456|Cleland Sandstone|61387|5|Briefly described|Map legend||Cambrian|Of the Pertaoorta Group. Sandstone, pebbly sandstone.  Geological Province: Amadeus Basin.||||||04-OCT-05
28456|Cleland Sandstone|61518|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Fine grained to pebbly ferruginous sandstone, locally micaceous and feldspathic. Geological Province: Amadeus Basin.||||||10-FEB-06
28456|Cleland Sandstone|61519|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorta Group. Sandstone, pebbly sandstone. Geological Province: Amadeus Basin.||||||
28456|Cleland Sandstone|62359|6|Mentioned|p554|||Geological Province: northern Amadeus Basin. ||||||
28456|Cleland Sandstone|62376|5|Briefly described|p18|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
28456|Cleland Sandstone|62379|5|Briefly described|p7 Fig. 2, p14|Late Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
28456|Cleland Sandstone|62609|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Sandstone, pebble sandstone, some siltstone. Underlies. Larapinta Group. Overlies: Pertaoorrta Group.||||||14-AUG-06
28456|Cleland Sandstone|62620|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Pertaoorrta Group. Sandstone, pebble snadstone, some siltstone.||||||
28456|Cleland Sandstone|64068|6|Mentioned|p65, 67, 69, 70, 225|||Amadeus Basin. In part correlated with Steamboat Sandstone. Correlated with Chabalowe Formation, Arrinthrunga Formation, Georgina Limestone, Mungerebar Limestone, Selwyn Range Limestone.||||||
28456|Cleland Sandstone|64778|6|Mentioned|p13|Cambrian|Cambrian|Amadeus Basin.||||||
28456|Cleland Sandstone|64809|5|Briefly described|p2, p3 Fig.2 |Late Cambrian|Middle Cambrian|Continental deposition.||Unit in Pertaoorrta Group.||||
28456|Cleland Sandstone|65233|5|Briefly described|p3 Fig. 2, p8, p9|Late Cambrian|Middle Cambrian|Of Pertaoorrta Gp.Max.thick:1060m. Amadeus Basin. Interfingers with Tempe Fm and is believed to change facies eastward into this unit + Deception Siltst.and Petermann Sst. Gravelly braided stream deposits comprised largely of med.- to coarse-gr.sandstone.||||||13-SEP-18
28456|Cleland Sandstone|67326|5|Briefly described|p2-5|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Mount Currie Conglomerate and ?Tempe Formation. Is overlain by Goyder Formation and Petermann Sandstone; may be equivalent to the latter.||
28456|Cleland Sandstone|67565|5|Briefly described|p40, pp46-47.|Late Cambrian|Middle Cambrian|Largely fluviatile sands. Lateral equivalent of Hugh River Shale, Goyder Formation and Petermann Sandstone. Thickness between 540-1067 m. Comprises three sedimentary packages.||||Is overlain conformably by the Goyder Formation and the Pacoota Sandstone.|A succession of fine- to coarse-grained and pebbly, ferruginous, partly feldspathic and micaceous sandstone; pebble beds and scattered pebbles occur throughout, mostly towards the base.|
28456|Cleland Sandstone|67856|6|Mentioned|p338 fig 4-30|Cambrian|Cambrian|||Of Pertaoorta Group.||||
28456|Cleland Sandstone|68323|6|Mentioned|p4 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
28456|Cleland Sandstone|69437|5|Briefly described|p22:10|Series 3|Series 3|Amadeus Basin.||||Is overlain by Goyder Formation (upper part).||12-JUL-16
28456|Cleland Sandstone|69438|4|Described|p23:2-3, 20-21, 24, 29-31|Late Cambrian|Middle Cambrian|Wells et al. (1965). Included in the Pertaoorrta Group by Ranford (1969). Amadeus Basin. Forms prominent strike ridges and low rounded hills. Up to c.1100m thick. Unfossiliferous. A lateral equivalent of the Illara Sandstone-Deception Formation-Petermann Sandstone succession. Grades laterally into Hugh River Shale and Goyder Formation.||Pertaoorrta Group.||Overlies Winnall beds unconformably, Tempe Formation disconformably, and Carnegie Formation conformably. Conformably underlies Goyder Formation and Pacoota Sandstone.|A succession of fine- to coarse-grained and pebbly, ferruginous, partly feldspathic and micaceous sandstone. Pebble beds and scattered pebbles occur throughout, but are most common near the base.|12-JUL-16
28456|Cleland Sandstone|69673|6|Mentioned|p64 fig 531, p66, p88, p91|||||||Overlies Tempe Formation, overlain by lower Goyder Formation||
28456|Cleland Sandstone|71114|6|Mentioned|p170 fig 1b|Cambrian|Cambrian|Southwestern Amadeus Basin?||||Shown as lateral equivalent to Tempe Formation + Illara Sandstone + Deception Formation + Petermann Sandstone. Overlain by Goyder Formation.||
28456|Cleland Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandsonte|
28456|Cleland Sandstone|71268|5|Briefly described|1m_geologyp12_lut.csv|||||Unit of Pertaoorrta Group.|||Sandstone, pebble sandstone, some siltstone.|
28456|Cleland Sandstone|71279|5|Briefly described|p355 Fig.2|Late Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
28456|Cleland Sandstone|72358|6|Mentioned|p118|Series 3|Series 3|Of Amadeus Basin.||||||
28456|Cleland Sandstone|72360|5|Briefly described|Map legend|Cambrian|Cambrian|Of Amadeus Basin.||Unit of Pertaoorta Group.|||Sandstone, pebbly sandstone.|09-SEP-19
28456|Cleland Sandstone|72516|6|Mentioned|p92-94|Cambrian|Cambrian|Amadeus Basin.||||Equivalent to the Steamboat Sandstone in part, Arrinthrunga Formation and the Eurowie Sandstone Member in part.||07-JUN-21
28456|Cleland Sandstone|73085|6|Mentioned|p1, p3-4, p11|late Cambrian|middle Cambrian|Makes up a series of ridges to the southwest of drillhole LA05DD01 but is not found in the drillhole; equivalent units are observed instead.||Pertaoorrta Group [and equivalents?]||Partly underlain by Winnall Group. Overlain by lower Goyder Formation. Partly equivalent to Petermann Sandstone, Deception Sandstone, Illara Sandstone, Tempe Formation.||
28456|Cleland Sandstone|73119|4|Described|piii, p1, p14-16, Appendix|late Cambrian|late Cambrian|Amadeus Basin, western. No fossils have been observed in the unit. Geochron is a new detrital zircon maximum depositional age, which is within error of a previous age of 490 +/- 7 Ma (Beyer et al., 2020). Detrital zircon spectra is dominated by Cambrian to Mesoproterozoic zircons, with only a small number of Palaeoproterozoic to Archaean grains. Sources include the Musgrave, Warumpi, Aileron, and Paterson provinces. [See article for provenance discussion].|485 +/- 10 Ma SHRIMP U-Pb|Pertaoorrta Group|||Red to purple, thin- to medium-bedded, medium- to coarse-grained, feldspathic, micaceous sandstone with occasional pebble beds and lenses.|
37963|Cockroach Group|61404|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Includes the Tomahawk and Ninmaroo Formations.  Geological Province: southern Georgina Basin.||||||12-OCT-05
37963|Cockroach Group|62983|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|Carbonate platform deposition. Geological Province: Georgina Basin. Written in informal format as Cockroach group.||||||23-JAN-07
37963|Cockroach Group|64068|2|Defined|p225-226, pp70-75, p7, 38, p ix|Early Ordovician|Late Cambrian|New name. Top of Group is diachronous: Late Cambrian in west to Early Ordovician in east.|||Includes Chatsworth Limestone, Ninmaroo, Tomahawk and Swift Formations.|Overlies various units of Narpa Group. Is overlain by Kelly Creek Formation.||21-MAR-16
37963|Cockroach Group|65341|6|Mentioned|pp18-19.||||||Includes Tomahawk Formation.|||
37963|Cockroach Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.||||||Includes Chatsworth Limestone, Gola beds, Ninmaroo Formation, Swift Formation|||
37963|Cockroach Group|67870|5|Briefly described|p43, p47, p50-53|Ordovician|Late Cambrian|Georgina Basin. Potential hydrocarbon reservoir.|||Tomahawk Formation, Chatsworth Limestone.||Organic-rich (1-2% TOC) limestone, ooid limestone, shaly limestone, organic-rich siltstone; minor sandstone.|
37963|Cockroach Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Ordovician|Cambrian|Georgina Basin. ||||||
37963|Cockroach Group|69377|5|Briefly described|map legend|Early Ordovician|Cambrian||||Ninmaroo Formation, Chatsworth Limestone|||
37963|Cockroach Group|69443|5|Briefly described|p28:3, 5, 7, 16, 25-27|Early Ordovician|Late Cambrian|Kruse in Dunster et al. (2007). Southern Georgina Basin. Widely distributed. The upper extent of this unit is diachronous. Is correlated with Pacoota Sandstone and ?Djagamara Formation.|||Chatsworth Limestone; Tomahawk, Ninmaroo, Swift Formations.|Overlies Narpa Group units conformably or disconformably. Is overlain conformably (locally disconformably) by Kelly Creek Formation (Toko Group).||12-JUL-16
37963|Cockroach Group|69591|5|Briefly described|p29, p91, p93-94|Early Ordovician|Cambrian|The carbonate-dominated Kelly Creek Formation and Coolibah Formation are here added to this Group, transferred from the otherwise clastic-dominated Toko Group.|||Ninmaroo, Swift, Kelly Creek, Coolibah Formations.||Predominantly carbonates.|
37963|Cockroach Group|69673|6|Mentioned|p111, p114 fig 92, p117||||||Includes Tomahawk Formation, Ninmaroo Formation, Swift Formation|||
37963|Cockroach Group|70749|5|Briefly described|p54|||Georgina Basin, Centralian Superbasin.|||Tomahawk, Ninmaroo Formations.|||
37963|Cockroach Group|72321|6|Mentioned|Fig 2||Jiangshanian|Burke River Structural Belt, Georgina Basin. |||Includes Chatsworth Limestone.|||
37963|Cockroach Group|72515|5|Briefly described|Map Legend|Ordovician|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Includes trilobite and rostroconchs fossils.|||Includes the Tomahawk Formation.|Unconformably overlain by the Alcoota beds. disconformably overlies the Narpa Group.||
37963|Cockroach Group|72516|5|Briefly described|p11, p21, p85, p94, p135, p171, p176|Ordovician|Furongian|Georgina Basin.|ca. 500 Ma (Maximum depositional age)||Includes the Tomahawk Formation.|||
37963|Cockroach Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|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.||||||
37963|Cockroach Group|73137|6|Mentioned|p6|Early Ordovician|Cambrian|||||||
37963|Cockroach Group|73553|6|Mentioned|p7|Early Ordovician|Cambrian|||||||
79092|Coggans Gabbro|69917|5|Briefly described|p174-175, 1|Cambrian|Cambrian|Eastern Arunta Region, Irindina Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. Emplacement age.|506.4+/-9.6 Ma|||Intrudes Indiana Igneous Complex. Geochemically similar to Kalkarindji Suite.|Weakly foliated metagabbro.|
79092|Coggans Gabbro|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen.|506+/-9.6 Ma crystallisation: U-Pb zircon LA-ICPMS||||Metagabbro.|
41999|Coles Dam Granite|9199|5|Briefly described|Map legend|||Granite.  Geological Province: Arunta Block.||||||04-NOV-04
41999|Coles Dam Granite|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Granite.||||||
35509|Collara Subgroup|23937|2|Defined|p76 App. 1|Calymmian|Calymmian|Lower part of  Roper Group.  Includes the Arnold Sst. Mbr., Jalboi Mbr. and Hodgson Sst. Mbr, formerly of Abner Sandstone.  Disconformably overlies McArthur and Nathan Groups in southern McArthur Basin, and Mt. Rigg Group in the north west.  See also p26.||||||13-APR-05
35509|Collara Subgroup|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Roper Group.||||||
35509|Collara Subgroup|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1390 +/- 20 Ma (maximum depositional age).|||||
35509|Collara Subgroup|69430|4|Described|p15:3, 26-27, 30|Calymmian|Calymmian|Abbott et al. (2001), for the units from the base of the Roper Group to the top of the Hodgson Sandstone. McArthur Basin.||Roper Group.|Mantungula, Mainoru, Crawford, Jalboi Formations; Phelp, Limmen, Arnold, Hodgson, Abner Sandstones.|Unconformably overlies Nathan and Mount Rigg Groups. Is overlain conformably to disconformably by Maiwok Subgroup.|Mudstone-dominated, mainly marine sediments.|12-JUL-16
35509|Collara Subgroup|69673|6|Mentioned|p16 fig 13|||Northwestern and Southern McArthur Basin.||Roper Group|Includes Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Crawford Formation, Mainoru Formation, Limmen Sandstone, Mantungula Formation||Sandstone.|
35509|Collara Subgroup|70734|5|Briefly described|p14,16|||McArthur Basin. Tidal/platform sandstone dominated? Shown as Collara subgroup p16. ||Of Roper Group.|Includes Mantuntuga Formation, Limmen Sandstone, Mainoru Formation, Crawford Formation, Arnold Sandstone, Jalboi Formation, Hodgson Sandstone.|||
35509|Collara Subgroup|70968|2|Defined|v-vi, p2, p5-50, p94, p123-124, p126-132|Calymmian|Calymmian|See also p135, p138, p140, p144. Sweet and Abbott in Abbott et al. (2001). Named after the Collara Mountains. Forms ridge and valley topography. Crops out over c.145,000 km2; considerably more extensive subsurface. Up to 1000m thick. Shoreline to shallow-marine inner shelf setting. Detrital zircon spectra discussed in some detail: detrital zircon diagram. May correlate with Constance Sandstone.|1492 +/- 4 Ma (Jackson et al., 1999).|Roper Group.|Phelp, Limmen, Abner, Arnold, Hodgson Sandstones; Mantungula, Mainoru, Crawford, Jalboi Formations.|Overlies Urapunga Granite. Is overlain by Maiwok Subgroup, mostly disconformably.|Cross-bedded, fine- to medium-grained, supermature quartz sandstone, with less abundant mudrock, commonly capped by thin intertidal to emergent facies. Contains minor limestone and two units of pedogenic red beds.|
35509|Collara Subgroup|71059|5|Briefly described|p1-3|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Phelp, Limmen, Arnold, Hodgson, Abner Sandstones; Mantungula, Mainoru, Crawford, Jalboi Formations.||Has a high proportion of shoreline-inner shelf sandstone.|
35509|Collara Subgroup|71488|4|Described|p141 fig 1b, p142, p150|||McArthur Basin. Deposited in a range of depositional environments from shoreline to shallow-marine shelf.||Roper Group|Includes the Phelp Sandstone, Mantungula Formation, Limmen Sandstone, Mainoru Formation, Crawford Formation, Arnold Sandstone, Jalboi Formation and Hodgson Sandstone.|Disconformably overlain by the Maiwok Subgroup.|Sandstone and lesser mudrocks.|
35509|Collara Subgroup|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||lower part of Roper Group.|||Quartzose sandstone, lithic-glauconitic-ferruginous sandstone, mudstone, shale (+/- carbonaceous).|04-MAR-20
35509|Collara Subgroup|71779|5|Briefly described| p2 Fig.1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Of Roper Group.|Includes the Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Crawford Formation, Mainoru Formation, Limmen Sandstone, Mantungula Formation, Phelp Sandstone.|||24-SEP-18
35509|Collara Subgroup|71893|5|Briefly described|iii, p3-p5, p8-p9, p20, p24-p25|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Roper Group|Includes the Phelp Sandstone, Limmen Sandstone, Crawford Formation, Arnold Sandstone, Hodgson Sandstone, Jalboi Formation, Mainoru Formation and the Mantungula Formation.|||
35509|Collara Subgroup|72381|4|Described|p773,779|Mesoproterozoic|Mesoproterozoic|Of  McArthur Basin. Shale-rich succession with less abundant sandstone formations, and generally deposited in deeper shelf environments (Jackson et al. 1988; Abbott and Sweet 2000; Abbott et al. 2001; Ahmad and Munson 2013). Interpreted to have received detritus from Mount Isa province as it was exhumed during Laurentian-Australian rifting event.||Unit of Roper Group.||Overlain by Maiwok Subgroup. Intruded by Derim Derim Dolerite.|Shale-rich with less abundant sandstone formations.|04-OCT-19
35509|Collara Subgroup|72526|5|Briefly described|p3, 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. Minimum age based on age of intrusive Derim Derim Dolerite (1313 Ma).||Roper Group|Abner Sandstone, Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Crawford Formation, Mainoru Formation, Limmen Formation, Mantungula Formation|Shown as unconformably overlying Nathan Group. Intruded by Derim Derim Dolerite.||
35509|Collara Subgroup|72527|6|Mentioned|p10.|Mesoproterozoic|Mesoproterozoic|||Roper Group|Includes Mainoru Formation.|||
35509|Collara Subgroup|72718|6|Mentioned|p7, p9|||McArthur Basin. Wilton package.||Roper Group|Hodgson Sandstone, Jalboi Formation, Arnold Sandstone, Abner Sandstone, Crawford Formation, Mainoru Formation, Showell Member, Limmen Sandstone, Mantungula Formation, Phelp Sandstone.|Partly underlain by Walmudga Formation (Nathan Group), Upper Balbirni Dolostone, Dungaminnie Formation, and Karns Dolostone unconformably. Overlain by Maiwok Subgroup|Sandstone-rich|
35509|Collara Subgroup|72912|5|Briefly described|p5 Fig.3, p20.|Mesoproterozoic|Mesoproterozoic|Minimum age from Derim Derim Dolerite, which intrudes both Collara Subgroup (from Mainoru Formation) and Maiwok Subgroup up to the top (Bukalorkmi Sandstone). [probably U-Pb SHRIMP] baddelyite magmatic age: 1324+/-4 Ma.|1324+/-4 Ma|Roper Group|Mantungula Formation,  Limmen Sandstone, Mainoru Formation, Crawford Formation, Arnold Sandstone, Jalboi Formation, Hodgson Sandstone, Abner Sandstone.|Overlies Nathan Group and underlies Malwick (Maiwok) Subgroup.||
35509|Collara Subgroup|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Roper Group|Jalboi, Crawford, Mainoru, Mantungula formations; Abner, Hodgson, Arnold, Limmen sandstones.|Unconformably underlain by Nathan Group. Overlain by Maiwok Subgroup||
35509|Collara Subgroup|73083|6|Mentioned|p45|||||Roper Group||||
35509|Collara Subgroup|73242|5|Briefly described|p39-40|||||Roper Group||Underlain by Mount Rigg Group[?] and Nathan Group[?]. Overlain by Munyi Member, Corcoran Formation, Maiwok Subgroup. Intruded by Derim Derim Dolerite.||
35509|Collara Subgroup|73412|5|Briefly described|p4, 8, 18|||Southern McArthur Basin.||Roper Group.|Limmen, Abner Sandstones; Mantungula, Mainoni, Crawford Formations.|Unconformably overlies Nathan Group. Is overlain by Maiwok Subgroup.||
24221|Coniston Schist|23270|5|Briefly described|Table 1, p5||Proterozoic|||||||
24221|Coniston Schist|23271|5|Briefly described|Map legend||Proterozoic|Of Arunta Block. Age: Middle Proterozoic.||||||07-AUG-06
24221|Coniston Schist|23809|5|Briefly described|p45, p41 Tb. 5|Paleoproterozoic|Paleoproterozoic|Foliated quartz-feldspar.  Age: 1780+/-10Ma.  Intrudes between Lander Rock beds and Mount Thomas Quartzite (Reynolds Range Group).||||||07-NOV-08
24221|Coniston Schist|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24221|Coniston Schist|39888|6|Mentioned|Fig.8|||||||||
24221|Coniston Schist|42217|6|Mentioned|p416|||||||||
24221|Coniston Schist|42401|6|Mentioned|p644|||||||||
24221|Coniston Schist|48992|2|Defined|p18|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24221|Coniston Schist|64722|5|Briefly described|p11|Statherian|Statherian||1780 Ma.|||Intrudes Reynolds Range Group.||11-APR-12
24221|Coniston Schist|64737|5|Briefly described|p242-3||Statherian|In the NW Reynolds Range. 1780 Ma zircon date reported by Smith (2001) may not date the intrusion due to contamination.||||In contact with Mount Thomas Quartzite.|Foliated felsic intrusion; S-type composition. Contains enclaves of metaquartzite country rock.|01-MAY-12
24221|Coniston Schist|64956|6|Mentioned|p26|||||||||07-FEB-11
24221|Coniston Schist|65338|5|Briefly described|p21, p56.|Statherian|Statherian|S-type quartz-feldspar porphyry intruding the unconformity at the base of the Mount Thomas Quartzite.|1780 +/- 10 Ma (Smith 2000, 2001).|||||
24221|Coniston Schist|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
24221|Coniston Schist|67430|6|Mentioned|p10|||This c.1780 Ma age is of the deposition of sediments forming the Schist.|1780 Ma.|||||
24221|Coniston Schist|68998|5|Briefly described|p14||||1780 +/- 10 Ma.|||Intrudes Reynolds Range Group. Correlative of the Nicker Beds.|Quartz-feldspar porphyry.|
24221|Coniston Schist|69226|5|Briefly described|p239, p243, p250|Statherian|Statherian|Reynolds-Anmatjira Ranges region. The granite precursor intruded and contact-metamorphosed the Reynolds Range Group c.1785 Ma.|c.1785 Ma.|||(Granite precursor) intrudes Reynolds Range Group.||
24221|Coniston Schist|69427|5|Briefly described|p12:25-26, 30, 32|Statherian|Statherian|NW Reynolds Range, Aileron Province. SHRIMP U-Pb age. Occurs within the Reynolds Range Group: most likely an intrusive (brief discussion).|1780 +/- 10 Ma (Smith, 2001).|||Intrudes the Reynolds Range Group.|500m-thick, semi-conformable biotite-sericite-quartz schist with quartz and K-feldspar augen.|12-JUL-16
24221|Coniston Schist|70376|6|Mentioned|p833, p833 fig 2, p834, p849|Paleoproterozoic|Paleoproterozoic|Protolith was voluminous S-type granites.|1780 Ma +/- 10 Ma||||Includes protolith from rhyolitic volcanism.|24-JAN-22
24221|Coniston Schist|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1780+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Schistose quartz-feldspar porphyry.|
24221|Coniston Schist|71858|5|Briefly described|p5, p28, p30|Statherian|Statherian|Aileron Province. Outcrops in the Reynolds Ranges.|ca. 1780 Ma||||Meta-igneous schists.|
24221|Coniston Schist|73399|6|Mentioned|p2, App.E|||[Misspelt as Conniston Schist, App.E].||||||
68733|Connellys Volcanics|69423|4|Described|p8:1, 3-4|Orosirian|Orosirian|Murphy Inlier, Murphy Province. Previously included in the Murphy Metamorphics. Comagmatic with Cliffdale Volcanics and Nicholson Granite Complex.|1855-1845 Ma (Page et al., 2000).|||Stratigraphically equivalent to the Cliffdale Volcanics.|Weathered porphyritic rhyolite or rhyodacite, generally with a mottled and highly weathered appearance; K-feldspar- and quartz-phyric.|12-JUL-16
68733|Connellys Volcanics|69433|6|Mentioned|p18:4|||Murphy Province.||||Is overlain unconformably by Benmara Group (Lawn Hill Platform).||12-JUL-16
68733|Connellys Volcanics|72526|5|Briefly described|p6 Fig.1.2.|Paleoproterozoic|Paleoproterozoic|||||||
68733|Connellys Volcanics|72919|6|Mentioned|p5-6, p11, p16|Orosirian|Orosirian|[Written as Connelly Volcanics on p5 and p16; probably misspelt]. Murphy Province, North Australian Craton. An age of 1864 +/- 5 Ma was reported by Kositcin et al. (2013). Broadly coeval with Nicholson Granite Complex and Cliffdale Volcanics.|1864 +/- 5 Ma||||Felsic volcanic rocks.|
78894|Conner Member|71842|2|Defined|p2,5-6,9, p11|Sturtian|Sturtian|Of Amadeus Basin. New unit part of revised nomenclature after this study in the Mount Conner area proposed by V.J. Normingtion. This unit is named for Mount Conner where the unit is exposed on the eastern most portion of the AYERS ROCK 250k map sheet. The type locality occurs on the western side of Mount Conner (MGA94, 52J, 782684mN, 7176885mE).  New constituent of the Areyonga Formation, represented by prominent ridges surrounding Mount Conner in the AYERS ROCK map sheet; a distinctive, unique, and restricted sandstone unit interpreted to be aeolian in origin, deposited during a (?local?) glacial maxima with minimal fluvial activity. Contains well-frosted quartz grains; regularly bedded and contains high angle (30 to 40°) foresets up 10m in thickness which are characteristic. Age is inferred on basis of stratigraphic position. Structure, metamorphism, geophysical expressions, references, age and evidence are provided.||Unit of Areyonga Formation.||Uppermost unit of Areyonga Formation.|Clean quartz sandstone composed of well rounded, medium-grained, well sorted quartz grains. Underlain by a lower sandstone that is massively bedded and well laminated.|08-JAN-20
78894|Conner Member|72601|6|Mentioned|p14|Cryogenian|Cryogenian|||Areyonga Formation|||Ridge-forming eolian sandstone.|
24864|Constance Sandstone|22673|6|Mentioned|66|||||||||
24864|Constance Sandstone|22680|6|Mentioned|84,86,87|||Geol province: Mount Isa Basin. Of the McNamara Group.||||||07-AUG-06
24864|Constance Sandstone|23065|6|Mentioned|4, 17|||||||||
24864|Constance Sandstone|23393|4|Described|p21|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Group.  Referred to as Constance Range Sandstone in Fig. 7, p28.||||||
24864|Constance Sandstone|23405|5|Briefly described|p586, 587|Statherian|Statherian|Of South Nicholson Group. 1591+/-10Ma from tuffaceous conglomeratic unit near base.||||||11-NOV-10
24864|Constance Sandstone|23937|5|Briefly described|p76 App. 1|||Of the South Nicholson Group.  Overlain by Mullera Formation.  See also p83 Appendix 1.||||||
24864|Constance Sandstone|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Flemington Subgroup? (South Nicholson Group).  Contains 5 sandstone/siltstone members.||||||
24864|Constance Sandstone|26310|4|Described|p3, 10, Table 1|Proterozoic|Proterozoic|Conformably underlies the Mullera Formation; underlies: Gold Creek Volcanics.  Overlies Lawn Hill Formation.  Maximum Thickness: 5,500 feet. Sandstone, greywacke.||||||09-AUG-04
24864|Constance Sandstone|30479|6|Mentioned|Fig.17|||Precambrian age.||||||07-AUG-06
24864|Constance Sandstone|32660|5|Briefly described|Table 5|||||||||
24864|Constance Sandstone|33387|6|Mentioned|p349|||||||||
24864|Constance Sandstone|35640|6|Mentioned|Map legend|Adelaidean|Adelaidean|Carpentarian?||||||
24864|Constance Sandstone|36003|6|Mentioned|Fig.8|||||||||
24864|Constance Sandstone|36012|3|Fully described|Table 4|||See also p16.||||||07-AUG-06
24864|Constance Sandstone|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
24864|Constance Sandstone|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean||||||
24864|Constance Sandstone|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24864|Constance Sandstone|38348|6|Mentioned|p24|||||||||
24864|Constance Sandstone|38584|4|Described|p19|||See also p18.||||||17-JUL-06
24864|Constance Sandstone|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the South Nicholson Group.  Fine to medium quartz sandstone, some coarse-grained; conglomerate beds; lenses of pebble to boulder conglomerate. Unconformably overlies Lawn Hill Fm. and its Widdallion Sandstone Member; conformably overlain by Mullera Fm.||||||10-JAN-05
24864|Constance Sandstone|39445|5|Briefly described|p56|||See Table 3||||||
24864|Constance Sandstone|39497|4|Described|p15|||See also p11.||||||07-AUG-06
24864|Constance Sandstone|39685|6|Mentioned|Fig.1|||||||||
24864|Constance Sandstone|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24864|Constance Sandstone|39925|6|Mentioned|p329|||See also Fig.2.||||||
24864|Constance Sandstone|40623|5|Briefly described|p112|||||||||
24864|Constance Sandstone|41721|3|Fully described|p29|||Of South Nicholson Gp. Contains the Pandanus, Wallis and Bowthorn Siltstone Members. Unconformably overlies Fickling Gp; disconformably overlies Doomadgee Fm. Thickness: >1000m. Geol.prov:  South Nicholson Basin. Mainly med.-grained quartz sst/lithic sst||||||02-AUG-07
24864|Constance Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
24864|Constance Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of South Nicholson Group. Of "Mid Proterozoic" age.||||||07-AUG-06
24864|Constance Sandstone|44210|14|Not recorded|Tb.1|||Equivalent to Pilpah Sandstone.||||||
24864|Constance Sandstone|44271|2|Defined|p39-41,55|||See also Lexicon. Overlies Wollogorang Formation. Unconformably overlain by Lawn Hill Formation.||||||
24864|Constance Sandstone|44272|14|Not recorded|Map Legend||Neoproterozoic|||||||
24864|Constance Sandstone|44274|2|Defined|Tb.2,p9,10,15,16,map|||||||||
24864|Constance Sandstone|44275|14|Not recorded|Map Legend|||||||||
24864|Constance Sandstone|44280|2|Defined|p5,6,7,Tb.1,map|||||||||
24864|Constance Sandstone|44281|14|Not recorded|Map Legend||Neoproterozoic|||||||
24864|Constance Sandstone|44290|14|Not recorded|p439|||||||||
24864|Constance Sandstone|44305|14|Not recorded|p.6,8,14-15|||(E53-8). opp.6,18.||||||
24864|Constance Sandstone|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
24864|Constance Sandstone|44482|14|Not recorded|p.5,6,8,opp.p.6, map|||(E53-12). See also p.9,13,16, for more details.||||||
24864|Constance Sandstone|44483|5|Briefly described|map legend|||Upper(?) Proterozoic.||||||
24864|Constance Sandstone|44751|14|Not recorded|p302|||||||||
24864|Constance Sandstone|44920|14|Not recorded|Map Legend, Sheet 2||Adelaidean|||||||
24864|Constance Sandstone|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of South Nicholson Group.||||||
24864|Constance Sandstone|44989|2|Defined|p.116-121||Neoproterozoic|Tb.II. On many pages. Upper Proterozoic. Overlies Lawn Hill Formation unconformably; and o/lies Wollogorang Formation; underlies Mullera Formation.||||||07-AUG-06
24864|Constance Sandstone|45052|2|Defined|p71|Adelaidean|Adelaidean|||||||
24864|Constance Sandstone|45079|6|Mentioned|p9|||Precambrian age. Map legend on p9.||||||07-AUG-06
24864|Constance Sandstone|45166|5|Briefly described|p33|||||||||
24864|Constance Sandstone|45287|14|Not recorded|p.223,226-7,229|||||||||
24864|Constance Sandstone|46804|6|Mentioned|p154|||||||||
24864|Constance Sandstone|49001|6|Mentioned|p12|||||||||
24864|Constance Sandstone|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Accident Subgroup. White, yellow and brown, friable, medium, coarse and very coarse grained to granule sandstone; minor siltstone and shale.||||||
24864|Constance Sandstone|64443|6|Mentioned|p3|Calymmian|Calymmian|Probable lateral relationship with Mittiebah Sandstone.||Of the Accident Subgroup.||||14-MAY-14
24864|Constance Sandstone|65337|2|Defined|p9 Fig.5, p38 Table 5, pp50-51.|Mesoproterozoic|Mesoproterozoic|North-central MOUNT DRUMMOND area. Possible correlative of Mittiebah Sandstone. 75 - 1100 m thick.Two facies dominate most outcrops: coarse sandstones and lower-energy, deeper-water micaceous sandstone and siltstone. Remarkably similar to Roper Group.||Unit in Accident Subgroup.|Includes Pandanus and Wallis Siltstone Members; Hedleys, Burangoo and Schultz Sandstone Members.|Unconformably overlies Caulfield beds. Disconformably overlies Crow Formation. Is overlain by Mullera Formation.|Dominantly thickly-bedded, cross-bedded, medium- to coarse-grained, granule-rich and occasionally pebbly, quartz or sublithic sandstone; interbedded red to grey-green fine-grained sandstone to siltstone; minor shale.|
24864|Constance Sandstone|67323|5|Briefly described|p39, GIS attrib tbl, Solid Geology Map|Mesoproterozoic|Mesoproterozoic|See also Mount Isa Block Time-Space Plot, Eastern Australia Time-Space Plot. South Nicholson Basin.|1589 +/- 10 Ma (maximum depositional age).|South Nicholson Group.|||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|67352|6|Mentioned|p12|Calymmian|Calymmian|Has an uncertain but probably lateral relationship with Mittiebah Sandstone.||Accident Subgroup||||
24864|Constance Sandstone|67539|5|Briefly described|p14, p15, p15 Fig.8|||Reduced in thickness by recognition of regional unconformity within the unit. The rocks below the unconformity are now excluded from Constance Sandstone, so now equivalent to the Schultz Sandstone Member of Rawlings & others (2008), which is thus rendered obsolete. Forms the base of the South Nicholson Group, south of the Elizabeth Creek Fault. Redefined to include the Bowthorn Siltstone Member which was declared obsolete by Rawlings and others (2008).||Of the South Nicholson Group.||Overlain by the Mullera Formation. Unconformably underlain by the Boodjamulla Formation, Wallis Siltstone and McNamara Group.||
24864|Constance Sandstone|68146|4|Described|p2, p6, p28, p34-41, p196-197, p211|||South Nicholson Region. Fig.150 on p106 (by I. Sweet, in preparation) places the Constance Sandstone at the top of the Wild Cow Subgroup, below an unconformity; Bowthorn Siltstone Member is included as a Member. Described as "lateral equivalent" to Schultz Sandstone Member; similar detrital zircon spectra. An earlier MDA of 1591 +/- 10 Ma (Page et al., 2000) comes from rocks now recognised as Burangoo Sandstone. Whole-rock Sm-Nd isotopic data tabulated.|1599 +/- 19 Ma; maximum depositional age.|Accident Subgroup.|Schultz Sandstone Member, Bowthorn Siltstone Member.|Unconformably overlies Wild Cow Subgroup.|Medium-grained, well-sorted quartz sandstone.|
24864|Constance Sandstone|68575|6|Mentioned|p18-19|||Previously included rocks now called the Burangoo Sandstone.||||Unconformably overlies Wild Cow Subgroup.||
24864|Constance Sandstone|69434|4|Described|p19:2-6, 8|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Widespread in QLD and NT. 75-1100m thick. Sandstone Members are distinguishable only by the intervening siltstone Members; where these latter are absent, the Formation is mapped as a single unit. Detrital zircon maximum depositional age.|<1591 +/- 10 Ma (Page et al., 2000).|Basal Accident Subgroup.|Schultz, Burangoo, Hedleys, Sandstone Members; Wallis, Pandanus, Siltstone Members.|Overlies Caulfield beds unconformably, and Crow Formation conformably to disconformably. Is overlain conformably by Mullera Formation.|Medium- to coarse-grained, granule-rich and occasionally pebbly, quartz or sublithic sandstone, interbedded with very fine-grained sandstone and siltstone. Sandstone intervals are typically thickly bedded and cross-bedded.|12-JUL-16
24864|Constance Sandstone|69591|4|Described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Previously included Hedleys Sandstone, Pandanus Formation, Burangoo Sandstone and Wallis Formation as Members. Fluvial to shelf deposits. Age by Page et al. (2000).|1591 +/- 10 Ma (maximum depositional age).|Wild Cow Subgroup.|Shultz Sandstone Member, Bowthorn Member.|Unconformably overlies Wallis Formation. Is overlain by Bowthorn Member or unconformably by Elizabeth Sandstone.|Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|69673|6|Mentioned|p56|||Maximum thickness of 1100m. Deposited in fluvial to shallow marine, tidal environment.||Accident Subgroup|||Quartz or sublithic sandstone, interbedded with sandstone and siltstone.|
24864|Constance Sandstone|70849|5|Briefly described|Map legend.|Calymmian|Calymmian|South Nicholson Basin. Five facies are mapped separately.||South Nicholson Group.||Unconformably overlies Doomadgee Formation (Fickling Group). Is overlain by Mullera Formation.|Sandstones, siltstone, shale, greywacke.|
24864|Constance Sandstone|70897|4|Described|p39-40, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|The basal member thins to the NW, due to onlap onto the Murphy Inlier, implying positive basement relief during deposition of early stages of the South Nicholson Group.|1591 +/- 10 Ma (maximum depositional age).|Basal South Nicholson Group.|Bowthorn, Wallis, Pandanus, Siltstone Members.|Overlies Lawn Hill Formation with an angular unconformity (locally disconformably).|Includes pebbly, coarse-grained, feldspathic sandstone.|
24864|Constance Sandstone|70968|5|Briefly described|p131 Fig.118, p132|Calymmian|Calymmian|May correlate with the Collara Subgroup.||Accident Subgroup.||||
24864|Constance Sandstone|71369|3|Fully described|p1, p4-9, p14-15, p19-20, p22-25, p27|Mesoproterozoic|Mesoproterozoic|See also p32-34, p36-37, p48-50. South Nicholson Basin. Mapped by Carter and Opik (1961); defined by them in Carter et al. (1961). The type section runs "from latitude 18deg 27'25"S, longitude 138deg17'00"E east-southeast about 4 miles to the base of the formation". Their type section coincides with the stratigraphic span of the Schultz Sandstone Member of Rawlings et al. (2008) who abandoned the Bowthorn Siltstone Member. This latter unit is resurrected and redefined as Bowthorn Member (Sweet, 2017). The Constance Sandstone now encompasses both Members. Two reference sections are detailed. Redefined in this study following recognition of an unconformity; the overlying part is now the Elizabeth Sandstone (Sweet, 2017). Note that Fig. 2e on p6 erroneously includes this unit in the Wild Cow Subgroup. Forms an escarpment in the Constance Range. Up to 970-1170m thick.||Accident Subgroup.|Bowthorn, Schultz Sandstone, Pandanus, Burangoo Sandstone, Hedleys Sandstone and Wallis Siltstone Members.|Unconformably overlies Wallis Formation. Is overlain unconformably by Elizabeth Sandstone (Accident Subgroup). Equivalent to the Mittiebah Sandstone.|Interbedded medium-grained sandstone and finer sandstone and mudstone.|20-FEB-18
24864|Constance Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1599+/-19 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24864|Constance Sandstone|72297|5|Briefly described|p749|||South Nicholson Basin. Poor source material; organic material has mostly reached an advanced stage of thermal maturity.|||||Includes shales.|
24864|Constance Sandstone|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 Schultz Sandstone Member.||Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|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 Schultz Sandstone Member.|Overlain by Elizabeth Sandstone or Mullera Formation. Underlain by Wallis Formation.|Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|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 Schultz Sandstone Member.|Overlain by Elizabeth Sandstone or Mullera Formation. Underlain by Wallis Formation.|Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|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 Schultz Sandstone Member.||Very fine- to coarse-grained and granule-rich to peblbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine sandstone intervals.|
24864|Constance Sandstone|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 Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|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 Accident Subgroup.|Includes Bowthorn Member, Schultz Member.||Very fine to coarse-grained and granule-rich to pebbly, lithic to quartzose (mostly sublithic) sandstone, mostly trough cross-bedded; conglomerate; siltstone and shale associated with very fine-grained sandstone intervals|
24864|Constance Sandstone|72526|4|Described|p1-2, p7, p8, p33-55, p56, p85-87|Calymmian|Calymmian|U-Pb SHRIMP maximum depositional ages obtained from 3 samples. Age with smallest error recorded here. Other ages are within error of this one. Shown as located in the central and eastern parts of the South Nicholson Basin. ~75-1100 m thick and extends across the border between the NT and Qid. Possibly lateral correlative with Mittiebah Sandstone. Shown as part of the Accident Subgroup on p8 Fig.1.3. Previously included Wallis Siltstone Member, Burangoo Sandstone Member, Pandanus Siltstone Member and Hedleys Sandstone Member (Rawlings et al., 2008.|1591+/-18 Ma max. dep.age.|Accident Subgroup|Includes Bowthorn Member, Shultz Sandstone Member.|Unconformably overlies Wallis Formation, Wild Cow Subgroup, Caulfield beds, Fickling Group. Conformably overlain by Mullera Formation, NT. Unconformably overlain by Elizabeth Sandstone, Qld.|Includes green-grey claystone, siltstone and cross-bedded, medium to coarse-grained sandstone; fine to very coarse-grained sandstone, dominated by moderately sorted, subangular to subrounded, quartz and feldspar grains.|
24864|Constance Sandstone|72527|6|Mentioned|p7 Fig.1.4, p10, p20|Mesoproterozoic|Mesoproterozoic|Maximum depositional age from detrital zircons in the basal conglomerate. Source assumed to be tuffs in Lawn Hill Formation. Now mapped as No Mans Sandstone Member in the Mitchiebo region.|Max. dep. age: 1591+/-10 Ma.|Accident Subgroup|Hedley Sandstone Member, Pandanus Sandstone Member, Burangoo Sandstone Member, Wallis Sandstone Member, Schultz Sandstone Member.|Unconformably overlies Tobacco Member and Caulfield beds, underlies Mullera Formation and is unconformably laterally equivalent to Mittiebah Sandstone.|Includes sandstone.|
24864|Constance Sandstone|72912|4|Described|p5 Fig.3, p23-24, p27-34, p48.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin. Hydrocarbon sources from this unit remain unexplained. No information on date shown p33.|1590+/-10 Ma|Base of Accident Subgroup.||Partially, unconformably overlies Wallis Fm and is equivalent to Mittiebah Sandstone and underlying Mullera Formation.||
24864|Constance Sandstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p15, p17 Fig.9.|Mesoproterozoic|Mesoproterozoic|Part of the South Nicholson Basin. Mineral composition boxplots reveal dominant quartz, muscovite and microcline components. Shown as being in the central part of the Isa Superbasin. Identified in 5 wells in this study. See also p26.|1590 +/- 10 Ma|Accident Subgroup|Includes Bowthorn Member.|Unconformably overlies Wallis Formation. Underlies Mullera Formation and is laterally equivalent to Mittebah Sandstone.|Includes sandstone, dolomitic siltstone.|
24864|Constance Sandstone|72919|5|Briefly described|p1, p4-5, p47-52, p70, p94-95|Ectasian|Calymmian|South Nicholson Basin. The stratigraphic position and definition has been revised in several studies; included in the Accident Subgroup in NT and the Wild Cow Subgroup in QLD. New U-Pb SHRIMP zircon maximum depositional age (MDA) of 1468 +/- 36 Ma was reported herein from QLD, which represents the youngest MDA yet recorded for this unit. This is consistent with plausible bracketing ages of ca. 1266 Ma xenotime overgrowths and ca. 1483 Ma from a MDA in the underlying Crow Formation. Conversely, four previous MDAs were reported from QLD of 1599 +/- 19 Ma from Carson et al. (2011), and 1591 +/- 18 Ma, 1578 +/- 53 Ma, and 1569 +/- 37 Ma from Anderson et al. (2019). Two samples (unnamed sandstones) were collected and dated from an interval labelled undifferentiated South Nicholson Group in drillcore NTGS02/1; these were inferred to be probably of this unit (Constance Sandstone) or equivalent based on detrital zircon spectra (MDAs of 1605 +/- 18 Ma and 1610 +/- 35 Ma).|1468 +/- 36 Ma U-Pb SHRIMP|Accident Subgroup/Wild Cow Subgroup, South Nicholson Group|Schultz Sandstone Member, Wallis Sandstone Member, Burangoo Sandstone Member, Pandanus Sandstone Member, Hedleys Sandstone Member|Unconformably underlain by Wallis Formation and Crow Formation, including Tobacco Member (Wild Cow Subgroup). Overlain by Mullera Formation. Equivalent to Mittiebah Sandstone.||
24864|Constance Sandstone|72967|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group||||
24864|Constance Sandstone|73042|6|Mentioned|p2, p4, p9|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Accident Subgroup, South Nicholson Group|Bowthorn Member|Partly underlain by Wallis Formation unconformably. Conformably overlain by Mullera Formation.||
24864|Constance Sandstone|73043|6|Mentioned|p7 Fig.2|Mesoproterozoic|Mesoproterozoic|||South Nicholson Group||||
24864|Constance Sandstone|73083|6|Mentioned|p34-35|Mesoproterozoic|Mesoproterozoic|Has five members.||||Equivalent to Mittiebah Sandstone.||
24864|Constance Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Partial aquifer.||Accident Subgroup, South Nicholson Group|Schultz Sandstone Member, Bowthorn Member|Unconformably underlain by Wallis Formation (Wild Cow Subgroup). Unconformably overlain by Elizabeth Sandstone.||
38421|Coodna Member|23733|2|Defined|p43 App.1|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Approximately ~930m thick. See also p11 and p32 Fig. 19..||||||07-NOV-08
38421|Coodna Member|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||
38421|Coodna Member|24303|3|Fully described|p5|Proterozoic|Proterozoic|Of the Hayward Creek Formation. Overlain by the Whittington Range Member; overlies the Meerie Member. Max. Thickness is 1300m in MUCKATY and 420m in BRUNCHILLY.||||||18-OCT-05
38421|Coodna Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Fm. Subdivided into upper (sandst; qtz arenite: thin to medium bedded, graded, well sorted; mudst; silicified) and lower (sandst.; lithic to qtz arenite; lensing, thin to v. thick beds, granular to pebbly, poorly sorted) lithofacies:||||||07-NOV-08
38421|Coodna Member|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Overlain by Whittington Range Member. Overlies the Meerie Member.||||||07-NOV-08
38421|Coodna Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Group). Sublithic/volcanilithic arenite. Overlies the Meerie Member; underlies Whittington Range Member.  In the Tennant Creek region.||||||07-NOV-08
38421|Coodna Member|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Geol. Prov: Tomkinson Creek Province.||Hayward Creek Formation||||
38421|Coodna Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hayward Creek Formation.||Overlies Meerie Member. Is overlain by Whittington Range Member.|Sublithic/volcanilithic arenite.|
38421|Coodna Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
38421|Coodna Member|69425|6|Mentioned|p10:12|||||Hayward Creek Formation.||Correlated in part with Frew River Formation and Coulters Sandstone.||12-JUL-16
38421|Coodna Member|69431|4|Described|p16:4-8|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.1000-1300m thick. Mainly fluviatile deposits. ||Hayward Creek Formation.||Conformably overlies Meerie Member. Is overlain conformably by Whittington Range Member. Is correlated with Coulters Sandstone.|Lithic, sublithic and feldspathic-sublithic sandstone, and pebbly sandstone. Medium- to coarse-grained, and grain size laminated thinly to thickly bedded, planar and very shallow-angle cross-bedded in laterally persistent bed sets.|12-JUL-16
78840|Cooley Dolostone Member|64815|6|Mentioned|p4 Fig.2|||||Unit in Barney Creek Formation.||||
78840|Cooley Dolostone Member|69430|4|Described|p15:3, 19, 40, 42|Statherian|Statherian|Southern McArthur Basin. These authors state that this unit's status as a Member is debatable. Hosts base metal sulfide deposits (briefly described).||Barney Creek Formation.||Interfingers with W-Fold Shale Member and HYC Pyritic Shale Member.|One or more intraformational, locally-derived (from the Emmerugga and Teena Dolostones), fault-related chaotic breccias; clasts range from millimetres to several tens of metres.|12-JUL-16
78840|Cooley Dolostone Member|69673|5|Briefly described|p16 fig 13, p34|||Batten Fault Zone||Barney Creek Formation|||Faulted related dolostone breccias.|
78840|Cooley Dolostone Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south).||Barney Creek Formation?, Umbolooga Sub-group, McArthur Group||Underlain by Coxco Dolostone Member. Overlain by Reward Dolostone. Equivalent to HYC Pyritic Shale Member and W-Fold Shale Member.||
42256|Coomalie Dolostone|24442|6|Mentioned|p44|||Contains magnesite deposits.  Overlain by Whites Formation.||||||
42256|Coomalie Dolostone|50623|4|Described|p259 Fig.2, p260 Fig.3, p161|Paleoproterozoic|Paleoproterozoic|Stromatolitic Carbonate - magnesite, dolomite, dolomitic marble, and minor calcareous para-amphibolite and metalutite. Conformably overlies Crater Formation. Of Mount Partridge Group.||||||07-NOV-08
42256|Coomalie Dolostone|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Stromatolitic magnesite and dolomite, stromatolitic silicified carbonate, para-amphibolite, metapelite. Overlies Crater Formation. Overlain by Whites Formation. Of Mount Partidge Group.||||||04-FEB-05
42256|Coomalie Dolostone|61389|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Stromatolitic magnesite, dolostone, some silicified, para-amphibolite, metapelite.||||||
42256|Coomalie Dolostone|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Of Mount Partridge Group. Max. thickness 600m. Stromatolitic magnesite, dolostone, some silicified, para-amphibolite, metapelite. Conformably overlies Crater Formation.||||||07-JAN-09
42256|Coomalie Dolostone|64730|5|Briefly described|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age from tuffaceous beds in the Wildman Siltstone (near top of Group).|Min. deposition age 2019 +/- 4 Ma.|Of Mount Partridge Group.||||03-MAY-12
42256|Coomalie Dolostone|65232|5|Briefly described|p51-53, p56|||Of Mount Partridge Group. Under Whites Formation (gradational) and Geolsec Formation (fault); over Crater Formation (gradational). Stromatolitic; dolomite-magnesite rock and talcose dolostone. See also Coomalie Dolomite p6. Uranium mineralisation.||||||09-FEB-10
42256|Coomalie Dolostone|65339|4|Described|p6 Table 1, p9.|||Outcrops are heavily silicified or lateritised, or both. Teepee structures and various stromatolite types are typical. Hosts Huandot magnesite deposit. May be stratigraphically equivalent to Koolpinyah Dolostone to the north.||Unit in Mount Partridge Group.||Overlies Crater Formation. Is overlain by Whites Formation.|Stromatolitic magnesite and dolostone, stromatolitic silicified carbonate occurring as chert or paraquartzite; rare calcareous para-amphibolite, metapelite.|
42256|Coomalie Dolostone|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Mount Partridge Group.||Overlies Crater Formation. Is overlain by White's Formation.|Stromatolitic magnesite, dolostone; some silicified, rare para-amphibolite, pelitic schist.|23-NOV-11
42256|Coomalie Dolostone|67355|4|Described|Throughout||Neoarchean|Previously assigned to the Batchelor Group (Walpole et al. (1968)). ~600 m maximum thickness. Depositional environment was an intertidal to supratidal evaporitic sabkha. Associated with numerous mineral prospects, deposits and occurrences.||Mount Partridge Group||Overlies Crater Formation conformably (dolomitic sandstone grading to dolostone), conformably underlies and interfingers with the Whites Formation. Unconformably overlain by the Geolsec Formation.|Stromatolitic carbonate rocks - stromatolitic magnesite and dolostone, with minor interbeds of calcareous metapelite and para-amphibolite. Several outcrops  are extensively brecciated, with angular dolostone/magnesite clasts in a carbonate matrix.|
42256|Coomalie Dolostone|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen.|||||Dolostone, magnesite.|
42256|Coomalie Dolostone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Mount Partridge Group.||Overlies Crater Formation. Is overlain by Whites Formation.||
42256|Coomalie Dolostone|69418|6|Mentioned|p3:7, 17, 31-32|||Pine Creek Orogen. Hosts gold deposits (described), as well as the Kylie unconformity-related U deposit (briefly described). Also hosts the Coomalie (also known as the Winchester) magnesite deposit (described).||||||12-JUL-16
42256|Coomalie Dolostone|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
42256|Coomalie Dolostone|69420|4|Described|p5:4, 6, 8-11, 14, 37, 54, 57, 60, 64|Paleoproterozoic|Paleoproterozoic|See also 75-78, 81, 89-91, 94-97, 110, 114, 116-117. Formerly Coomalie Dolomite. Rum Jungle region, Central Domain, Pine Creek Orogen. Subtidal, evaporitic deposits. Hosts a number of Au-Pt-Pd prospects (eg the Sundance Au deposit), described in some detail. Is associated with a number of U deposits hosted by the overlying Whites Formation. Hosts the Yarram iron ore deposit, and magnesite in several areas.||Mount Partridge Group.||Overlies Crater Formation. Is overlain conformably by Whites Formation and (unconformably) Geolsec Formation. Correlated with Koolpinyah Dolostone.|Stromatolitic dolostone, magnesite and minor shale.|12-JUL-16
42256|Coomalie Dolostone|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Mount Partridge Group.||Conformably overlies Crater Formation. Is overlain conformably by Whites Formation.|Stromatolitic magnesite and dolostone, in places chloritic and tremolitic, commonly silicified or lateritised at surface; para-amphibolite and pelitic schist; shale, commonly graphitic.|
73196|Coora Dolerite|50152|5|Briefly described|p72 Fig. 3|||Of Dead Bullock Formation. Medium-grained, amphibolite and plagioclase dolerite. Semi-conformable with stratigraphy.||||||
73196|Coora Dolerite|62580|6|Mentioned|p60|||Local name for dolerite sills of the Dead Bullock Formation - also known as Dead Bullock Soak dolerite. See also Coora dolerite - both are informal names.||||||07-FEB-11
73196|Coora Dolerite|64675|6|Mentioned|Fig.4, Fig.31c|||Presented as the Coora dolerite in Fig.31(c).||||||
73196|Coora Dolerite|69618|5|Briefly described|p93 Fig.3, p100 Tb.1, p102 Fig.13|||~300m thick.||Unit in Callie Member.||Overlies Orac Beds. Is overlain by Dead Bullock Beds.|Fine- to coarse-grained basalt and amphibole-pyroxene-plagioclase dolerite; minor graphitic siltstone and claystone; semi-conformable with bedding.|
73196|Coora Dolerite|69747|4|Described|p262,265-272,274|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Intrudes Dead Bullock Formation. Undergone greenschist to amphibolite-facies metamorphism due to subduction of Tanami back-arc oceanic slab. Back-arc basaltic rock affinities; petrologically and geochemically similar to mafic rocks in the former Stubbins Formation. Geochemically similar to the Groundrush dolerite.|ca. 1864 Ma||||Medium- to coarse-grained and dark green; subhedral to euhedral plagioclase and metamorphic hornblende relic the crystal form of pyroxene; common, subtle chrolite alternation. Mineral assemblage of plagioclase, hornblende, chlorite, diopside.|25-JUN-19
73196|Coora Dolerite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1882+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Dolerite.|
73196|Coora Dolerite|73158|6|Mentioned|p10|||||Callie Member||||
73196|Coora Dolerite|73159|5|Briefly described|p10|||||||Intrudes Callie Member (Dead Bullock Formation).|Volcanic arc basalts.|
26495|Copia Granite|23733|5|Briefly described|p34 Fig.20|||||||||
26495|Copia Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jervois ?Suite (Jervois presented in Table 4.1 in isolation). Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26495|Copia Granite|33103|4|Described|Table 2|||||||||
26495|Copia Granite|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26495|Copia Granite|39888|6|Mentioned|Fig.7|||||||||
26495|Copia Granite|42326|5|Briefly described|Table 2 P11|||||||||
26495|Copia Granite|43568|6|Mentioned|Fig.4,p506|||||||||
26495|Copia Granite|50369|5|Briefly described|p1.4, 9.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jervois Suite.||||||07-NOV-08
26495|Copia Granite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
26495|Copia Granite|69427|5|Briefly described|p12:29-30|Statherian|Statherian|Shaw and Warren (1975). Similar to the Crooked Hole Granite.|c.1780-1760 Ma.||||Foliated granitic rock.|12-JUL-16
26495|Copia Granite|69917|5|Briefly described|p103-104|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating attempted but lack of concordant data makes any interpretation difficult. Based on similarity to Crooked Hole Granite, is interpreted to have been emplaced during the 1810-1790 Ma Stafford Event.||||Intrudes Delny Metamorphics. Intruded by Mount Ida Granite.|Medium- to coarse-grained gneissic biotite granite.|
26495|Copia Granite|69925|6|Mentioned|p36|||Huckitta-Alcoota area.||||Correlated with Dneiper Granite.||
26495|Copia Granite|69931|6|Mentioned|p269, 274, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated.||Dneiper suite.|||Gneissic granite.|
27379|Corcoran Formation|22538|6|Mentioned|Fig3 P708|||||||||
27379|Corcoran Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27379|Corcoran Formation|22853|4|Described|28|Proterozoic|Proterozoic|Of the Roper Group. Underlying unit: Abner Sandstone.||||||07-AUG-06
27379|Corcoran Formation|23216|5|Briefly described|Table1p8,34|||||||||
27379|Corcoran Formation|23404|5|Briefly described|p640|||Of Roper Group.||||||
27379|Corcoran Formation|23776|5|Briefly described|p705 Fig 2.|||Of Roper Group.||||||
27379|Corcoran Formation|23937|2|Defined|p76-77 App. 1, p41|Calymmian|Calymmian|Of Maiwok Subgp (Roper Gp).  Overlain by Bessie Creek Sst; underlain by Hodgson Sst. Age:1492-1429Ma. Age inferred from overlying and underlying units. Formerly included in lower part of the Roper Group before redefinition of the Maiwok Subgrp to include it and Bessie Creek Sst.||||||14-NOV-17
27379|Corcoran Formation|24048|4|Described|p71|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
27379|Corcoran Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: buff to pink-brown, fine to medium-grained, thin-bedded, hummocky cross-beds; mudstone; ferruginous, in places micaceous, scree only. Geol. Prov: McArthur Basin.||||||13-OCT-05
27379|Corcoran Formation|24050|3|Fully described|p50, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Mudstone, fine-grained quartz sandstone.  Of Roper Group.  Overlies the Munyi Member; underlies Bessie Creek Sandstone.  Thickness: ?150m.||||||07-AUG-06
27379|Corcoran Formation|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
27379|Corcoran Formation|24303|5|Briefly described|p24 Tb.4|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Correlates with Wiernty Formation (Renner Group).||||||
27379|Corcoran Formation|32660|5|Briefly described|Table 4|||||||||
27379|Corcoran Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27379|Corcoran Formation|40691|6|Mentioned|Fig.4|||||||||
27379|Corcoran Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27379|Corcoran Formation|41220|6|Mentioned|Fig.3|||||||||
27379|Corcoran Formation|41268|6|Mentioned|p291|||||||||
27379|Corcoran Formation|42385|4|Described|p28|||See also Table 5 p25. Member of Abner Sandstone.||||||07-AUG-06
27379|Corcoran Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
27379|Corcoran Formation|42395|6|Mentioned|Fig.26 P86|||||||||
27379|Corcoran Formation|42597|5|Briefly described|Map Legend|Adelaidean||||||||
27379|Corcoran Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Lower Roper Group (Roper Group).||In schematic section, underlies Bessie Creek Formation; overlies Hodgson Sandstone Member (Abner Sandstone).|Mudstone, sitlstone and sandstone. Detailed lithology given.|11-NOV-11
27379|Corcoran Formation|42639|4|Described|p43, Table 7 p39|||||||||
27379|Corcoran Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Fine grained sandstone, medium to coarse grained ferruginous sandstone, ferruginous and in places micaceous mudstone.||||||19-OCT-05
27379|Corcoran Formation|42812|3|Fully described|p53, Table 5|||Of Roper Group.||||||07-AUG-06
27379|Corcoran Formation|42846|5|Briefly described|p503, Fig.1 p502|||Of Roper Group. Fine-grained. Geological Province: McArthur Basin.||||||09-MAY-05
27379|Corcoran Formation|43010|4|Described|Table 30.|||Of Roper Group.||||||07-AUG-06
27379|Corcoran Formation|43036|6|Mentioned|Fig.5|||Of Roper Group.||||||07-AUG-06
27379|Corcoran Formation|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||07-AUG-06
27379|Corcoran Formation|43645|5|Briefly described|p562|||||||||
27379|Corcoran Formation|43652|6|Mentioned|Fig.11,p389|||||||||
27379|Corcoran Formation|44112|6|Mentioned|Fig11p30|||||||||
27379|Corcoran Formation|44287|14|Not recorded|p.12, opp.11|||(E53-3).||||||
27379|Corcoran Formation|44288|14|Not recorded|map legend|||Siltstone, quartz sandstone, ferruginous sandstone. Upper (?) Proterozoic.||||||
27379|Corcoran Formation|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
27379|Corcoran Formation|44332|14|Not recorded|p.8,opp.6,map|||(D53-14).||||||
27379|Corcoran Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
27379|Corcoran Formation|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Conformably overlain by Bessie Creek Sandstone; conformably overlies Munyi Member of Abner Sandstone. Mt. Marumba. (D53-6).||||||07-AUG-06
27379|Corcoran Formation|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27379|Corcoran Formation|44434|14|Not recorded|p.8, opp. p.6, map|||Not exposed. (D53-11,12).||||||
27379|Corcoran Formation|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27379|Corcoran Formation|44436|5|Briefly described|opp. p.7|||No o/c in Robinson River sheet area. (E53-4).||||||02-DEC-04
27379|Corcoran Formation|44459|14|Not recorded|p.8, opp.p.6, map|||(E53-2). Formation of Roper Group.||||||
27379|Corcoran Formation|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27379|Corcoran Formation|44471|14|Not recorded|p.10, opp.p.7, map|||(D53-10).||||||
27379|Corcoran Formation|44472|5|Briefly described|map legend|||Of the Roper Group.  Micaceous fine-grained sandstone, shale, minor limestone.  Upper (?) Proterozoic.||||||02-DEC-04
27379|Corcoran Formation|44530|14|Not recorded|p.11, opp.12|||(D53-15).||||||
27379|Corcoran Formation|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27379|Corcoran Formation|45022|14|Not recorded|p.78,81||Adelaidean|Of Roper Group||||||
27379|Corcoran Formation|45162|6|Mentioned|Table 7|||See also Fig.4||||||
27379|Corcoran Formation|46861|6|Mentioned|Fig.2a|||||||||
27379|Corcoran Formation|46968|6|Mentioned|p304|||||||||
27379|Corcoran Formation|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
27379|Corcoran Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Bessie Creek Sandstone, underlain by Abner Sandstone.||||||
27379|Corcoran Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Contains the Munyi Member.  Lower part - red laminated siltstone; upper part - interbedded fine sandstone and laminated siltstone. Overlies Hodgson Fm; underlies Bessie Sandstone.||||||16-SEP-13
27379|Corcoran Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Red laminated siltstone; interbedded fine grained sandstone and laminated siltstone.||||||29-SEP-05
27379|Corcoran Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: buff to pink-brown, fine to medium-grained, thin-bedded, hummocky cross-beds; mudstone; ferruginous, in places micaceous, scree only. Geol. Prov: McArthur Basin.||||||16-SEP-13
27379|Corcoran Formation|61560|6|Mentioned|p489|||||||||
27379|Corcoran Formation|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Shales and greywacke deposits; potassium-rich with intercalations of claystones. Geological Province: McArthur Basin.||||||
27379|Corcoran Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
27379|Corcoran Formation|64784|5|Briefly described|p2 Fig.2, p3 Fig.3 |Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Overlies Abner Sandstone. Is overlain by Bessie Creek Sandstone.||
27379|Corcoran Formation|64815|6|Mentioned|p5 Fig.3 |||||Of the Roper Group.||||
27379|Corcoran Formation|64816|5|Briefly described|p2 Fig.1, p3 Fig.2|Proterozoic|Proterozoic|||Unit in Roper Group.|||Claystone and siltstone, minor sandstone.|
27379|Corcoran Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
27379|Corcoran Formation|65228|5|Briefly described|Fig.02.|||||Unit in Roper Group.|Includes Munyi Member.|Overlies Abner Sandstone. Is overlain by Bessie Creek Sandstone.||
27379|Corcoran Formation|65236|5|Briefly described|p3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Geological province: Beetaloo Sub-basin.||||||04-JUN-09
27379|Corcoran Formation|65342|5|Briefly described|p8, p12.|||McArthur and Daly Basins. Max. thickness at least 105 m.  Seen as having potential as an insulating layer for geothermal energy.||Unit in Roper Group.|Includes Munyi Member.|Overlies Abner Sandstone.|Mudstone; fine sandstone at top.|
27379|Corcoran Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
27379|Corcoran Formation|69430|4|Described|p15:3, 27, 29-30, 62|Calymmian|Calymmian|McArthur Basin. c.180-225m thick. Distal shelf, and storm-dominated shelf, sediments.||Maiwok Subgroup.|Munyi Member.|Overlies Abner Sandstone, and Hodgson Sandstone conformably to disconformably. Is overlain disconformably by Bessie Creek Sandstone.|Lower part: red to brown ferruginous sandstone, siltstone, mudstone, conglomerate and pisolitic ironstone; grades upward into laminated green-grey to black mudstone and siltstone, minor fine sandstone.|12-JUL-16
27379|Corcoran Formation|69673|6|Mentioned|p16 fig 13, p31, p40|||Northwestern and Southern McArthur Basin. Unexplored source rock potential.||Maiwok Subgroup|Includes Munyi Member|Disconformably overlain by Bessie Creek Sandstone, Overlies Hodgson Sandstone||
27379|Corcoran Formation|70734|4|Described|p13-19, 21-25|||McArthur Basin. Storm-dominated shelf (mudstone-dominated). Whole rocks and pyrite geochem. Data reported & discussed.||Of Maiwok Subgroup.||Overlies Hodgson Sandstone. Overlain by Bessie Creek Sandstone and the Velkerri Formation.|Includes ~50% mudstones.|10-JUL-18
27379|Corcoran Formation|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.|Includes Munyi Member.|Overlies Hodgson Sandstone. Is overlain by Bessie Creek Sandstone.|Interbedded mudstone, siltstone and fine sandstone.|
27379|Corcoran Formation|70897|6|Mentioned|Fig.1.7.6,9|||McArthur Basin.||||||29-NOV-17
27379|Corcoran Formation|70968|2|Defined|p23, p39, p48, p50-55, p57, p59, p69|Ectasian|Ectasian|See also p123, p126, p131, p134, p140, p143. Sweet in Abbott et al. (2001) after Dunn (1963). Included in Maiwok Subgroup by Abbott et al. (2001). Named after Corcoran Creek. Predominantly fine-grained and recessive: poor exposures. The type section is a complete 230.9m-thick intersection in Golden Grove-1 in URAPUNGA sheet, from 396.6m (base) to 165.7m; this excludes the Munyi Member (419.9-396.6m) whose type section is in Urapunga-5. Thickness varies from c.20m to 505m. Storm-dominated, subtidal shallow-marine shelf deposits.||Maiwok Subgroup.|Includes basal Munyi Member.|Disconformably overlies Hodgson Sandstone. Is overlain conformably by Bessie Creek Sandstone.|Interlaminated to finely interbedded light grey to light brown, occasionally laminated and micaceous siltstone, green-grey to black, finely parallel laminated mudrock and minor fine-grained, quartz-rich sandstone.|14-NOV-17
27379|Corcoran Formation|71059|4|Described|p3, p14-16, p18, p20, p24, p31|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 180-225m thick. Storm-dominated to distal marine shelf deposits. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, organic petrology reflectivity, data all detailed.||Maiwok Subgroup.|Munyi Member.|Conformably to disconformably overlies Hodgson Sandstone. Is overlain conformably to disconformably by Bessie Creek Sandstone.|Interlaminated to finely interbedded green-grey to black siltstone, mudrock and minor fine sandstone.|
27379|Corcoran Formation|71488|5|Briefly described|p141 fig 1b, p142, p144 fig 2, p148|||Beetaloo Sub-basin. Deposited mainly in a storm-dominated shallow-marine shelf setting, mostly under relatively low-energy subtidal conditions.||Maiwok Subgroup|Includes the Munyi Member.|Overlain by the Bessie Creek Sandstone.|Mudstone and siltstone succession with minor interbedded quartz arenites.|02-MAY-18
27379|Corcoran Formation|71779|5|Briefly described|p2, p6, p10, p12 fig 9, p25|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Maiwok Subgroup|Includes the Munyi Member.|||23-FEB-20
27379|Corcoran Formation|71893|5|Briefly described|p8, p24|||McArthur Basin.||Maiwok Subgroup|Includes the Munyi Member.|Disconformably (locally conformably) overlies the Hodgson Sandstone.||
27379|Corcoran Formation|72381|5|Briefly described|p772|||Of Beetaloo Sub-basin, McArthur Basin.||||Overlain by Bessie Creek Sandstone. Underlain unconformably by Nathan Group.||
27379|Corcoran Formation|72526|5|Briefly described|p8 Fig.1.3, p33.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Maiwok Subgroup||Overlies Hodgson Sandstone and underlies Bessie Creek Sandstone.||
27379|Corcoran Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Maiwok Subgroup, Roper Group||Underlain by Hodgson Sandstone. Overlain by Bessie Creek Sandstone.||
27379|Corcoran Formation|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Base of Maiwok Subgroup||Overlies Hodgson Sandstone and underlies Bessie Creek Sandstone.||
27379|Corcoran Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Hodgson Sandstone. Overlain by Bessie Creek Sandstone.||
27379|Corcoran Formation|73242|5|Briefly described|p39-40|||||Maiwok Subgroup, Roper Group|Munyi Member|Underlain by Hodgson Sandstone, Collara Subgroup. Overlain by Bessie Creek Sandstone. Intruded by Derim Derim Dolerite.|Includes interbedded mudstone and fine sandstone.|
27379|Corcoran Formation|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
27379|Corcoran Formation|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Abner Sandstone. Is overlain by Bessie Creek Sandstone.||
75784|Corkwood Hill Granite|64337|4|Described|pp375-377, pp386-388, p392|Devonian|Devonian|E-W elongate plug-like body c. 70 m long by c. 30 m wide. Emplaced after peak metamorphic conditions. Age by SHRIMP zircon analysis 206Pb/238U.|386.9 +/- 3.5 Ma.|||Intrudes Harts Range Complex.|Weakly-deformed, fine-grained biotite granite.|29-JUL-15
75784|Corkwood Hill Granite|69917|6|Mentioned|p114|Middle Devonian|Middle Devonian|386.9+/-3.5 Ma crystallisation age.||||||29-JUL-15
75784|Corkwood Hill Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|387+/-3.5 Ma (SHRIMP U-Pb zircon).||||Granite.|
72987|Cosmo Supergroup|66683|5|Briefly described|p365.|Paleoproterozoic|Paleoproterozoic||c.1862 Ma.|||Unconformably overlies Woodcutters Supergroup.|Clastic and carbonaceous sedimentary rocks; felsic tuffs; a thick package of turbiditic greywacke and siltstone.|
72987|Cosmo Supergroup|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Areas with different magnetic responses are indicated.|||Includes Finniss River Group and Hermit Creek Metamorphics.|||18-FEB-14
72987|Cosmo Supergroup|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes South Alligator and Finniss River Groups.|||23-NOV-11
72987|Cosmo Supergroup|67232|5|Briefly described|p2. |Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. The underlying unconformity represents at least 160 My.|1860 - 1840 Ma.|||Overlies unconformably Woodcutters Supergroup. Is intruded by Cullen Supersuite.|Carbonate; carbonaceous, siliciclastic and volcaniclastic sedimentary rocks; subordinate mafic and felsic volcanic rocks.|
72987|Cosmo Supergroup|67355|6|Mentioned|p.6|||See also Cosmo Howley Supergroup (p6-7, p10).||||||23-FEB-20
72987|Cosmo Supergroup|67479|6|Mentioned|p6 Fig.2|||||||||
72987|Cosmo Supergroup|67779|5|Briefly described|p5 Fig.4(b), p6 Fig.5, p91, p105.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Detrital zircon analysis suggests a different provenance from the Nimbuwah Domain (Cahill Formation). Deposition was in a likely foreland basin setting. |1863 Ma.||Includes South Alligator and Finniss River Groups, Hermit Creek and Welltree Metamorphics.|||21-MAY-18
72987|Cosmo Supergroup|69383|6|Mentioned|p28||||||Includes Finniss River Group.|||
72987|Cosmo Supergroup|69417|5|Briefly described|p2:4-5,|Orosirian|Orosirian|Pine Creek Orogen. Broadly synchronous with deposition in the Warramunga and Murphy Provinces. Appears in Fig.2.4 to be intruded by Allia Creek Suite and equivalents.|1865-1860 Ma.||||Flysch succession and felsic volcanic rocks.|12-JUL-16
72987|Cosmo Supergroup|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
72987|Cosmo Supergroup|69420|5|Briefly described|p5:1-2, 4-7, 11-13, 15, 26, 38, 66, 85|Paleoproterozoic|Paleoproterozoic|See also 100, 111, 115. Ahmad and McCready (2001). Pine Creek Orogen. Has distinctly different detrital zircon provenance than Woodcutters Supergroup or Nourlangie Schist.|Deposited c.1865-1855 Ma.||South Alligator, Finniss River Groups; Hermit Creek, Welltree Metamorphics.|Unconformably overlies Woodcutters Supergroup.||12-JUL-16
72987|Cosmo Supergroup|69421|6|Mentioned|p6:1|||Pine Creek Orogen.||||||12-JUL-16
72987|Cosmo Supergroup|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
72987|Cosmo Supergroup|70719|6|Mentioned|iv, |||Pine Creek Orogen.||||Correlative of Grindall Formation.||
72987|Cosmo Supergroup|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Finniss River Group, South Alligator Group, Welltree Metamorphics, Hermit Creek Metamorphics.|||01-MAR-18
72987|Cosmo Supergroup|71256|6|Mentioned|p18 Fig 1|||||||||
72987|Cosmo Supergroup|73089|6|Mentioned|p33|Orosirian|Orosirian|Pine Creek Orogen, Central Domain. Dominantly Paleoproterozoic detritus. Dated by intercalated felsic volcanic rocks, which are coeval with granitic rocks of the Nimbuwah Complex. Upper portion may be a lower-metamorphic-grade correlative of the Welltree Metamorphics and Hermit Creek Metamorphics.|1863-1861 Ma[?]||||Turbiditic metasedimentary rocks.|
24881|Cottee Formation|22538|6|Mentioned|Fig3 P708|||||||||
24881|Cottee Formation|22748|4|Described|p235 Fig.1|||||||||
24881|Cottee Formation|23216|5|Briefly described|Table1p9,23|||||||||
24881|Cottee Formation|23363|5|Briefly described|344 Fig.3|||||||||
24881|Cottee Formation|23374|3|Fully described|Tb2p10,16,17||Statherian|Unconformable beneath Shadforth Sandstone. Of Katherine River Group. Geological Province:  McArthur Basin.||||||07-AUG-06
24881|Cottee Formation|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||07-AUG-06
24881|Cottee Formation|23733|5|Briefly described|p32 Fig. 19|||Of Katherine River Group.||||||
24881|Cottee Formation|23867|3|Fully described|p9|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Can be divided into several informal units.  Max. thickness: 350m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
24881|Cottee Formation|23937|5|Briefly described|p7|||Of the Katherine River Group.  On the KATHERINE sheet.  Geological Province: Calvert Superbasin.||||||
24881|Cottee Formation|24050|3|Fully described|p18, p10|||Of Katherine River Group.  Mudstone; sandy, glauconitic and stromatolitic dolostone; quartz sandstone.||||||07-AUG-06
24881|Cottee Formation|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
24881|Cottee Formation|32660|5|Briefly described|Table 4|||||||||
24881|Cottee Formation|37568|5|Briefly described|p78|||||||||
24881|Cottee Formation|39210|6|Mentioned|p50|||||||||
24881|Cottee Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
24881|Cottee Formation|43010|2|Defined|p100||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
24881|Cottee Formation|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
24881|Cottee Formation|44400|2|Defined|p.7,8,11,Tb.1,opp.p6|||Overlain unconformably by Shadforth Sandstone.  Mt Marumba Sheet. (D53-6).||||||07-AUG-06
24881|Cottee Formation|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
24881|Cottee Formation|45022|4|Described|p.54,56,68||Carpentarian|Of Katherine River Group. Fig.15, Tb.3,4.||||||
24881|Cottee Formation|50545|5|Briefly described|p126|||Contains evaporites.||||||17-DEC-07
24881|Cottee Formation|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Hemispherical stromatolite biotherms; interbedded mudstone; fine-grained sandstone and dolostone. Geological Province: McArthur Basin.||||||30-NOV-04
24881|Cottee Formation|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Laminated mudstone and siltstone with synaeresis cracks and erosion structures (tool marks and flutes casts).  Geological Province: McArthur Basin. Overlies: McKay Sandstone. Underlies: Shadforth Sandstone.||||||14-JAN-05
24881|Cottee Formation|61572|5|Briefly described|p668 Fig. 3|||Of the Katherine River Group. Mudstone, dolostone, and sandstone; dolerite sills. Max. thickness: 300m. Geological Province: McArthur Basin.  See also p671 Tb. 1||||||
24881|Cottee Formation|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1740-1760Ma. McArthur Basin. Of Katherine River Group. Max thick 350m. Red-grey and grey laminated mudst and siltst with synaeresis cracks and erosion structures (tool marks and flute casts) in places; cross-bedded, coarse, glauconitic qtz sandst;||||||
24881|Cottee Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Katherine River Group.|||Mudstone, dolostone.|04-JUN-18
24881|Cottee Formation|65232|5|Briefly described|p7 Fig. 6|||Of Katherine River Group. Underlies Shadforth Sandstone; overlies Mackay Sandstone. 300m thick. Shallow-marine mudstone, sandstone, stromatolitic dolostone.||||||09-FEB-10
24881|Cottee Formation|65337|6|Mentioned|p45.|||McArthur Basin. Storm shelf facies closely resembles that of Crow Formation.||||||
24881|Cottee Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.||Upper Katherine River Group.||||
24881|Cottee Formation|67564|4|Described|p10 Fig.5, p39 Fig.20, pp44-47, p86.|Paleoproterozoic|Paleoproterozoic|Recessive and ridge-forming strata. 350 m of storm-dominated shelf through to shoreline sediments. Distinctly anomalous K radiometric signature.||Unit in Katherine River Group.||Disconformably overlies Snowdrop Sandstone Member. Is overlain unconformably by Shadforth Sandstone.|Red beds; reddish-grey mudstone; crossbedded, coarse glauconitic quartz sandstone; fine to medium quartz sandstone with mudstone intraclasts; thinly-bedded lithic sandstone; minor stromatolitic dolostone.|
24881|Cottee Formation|69430|4|Described|p15:3, 8-9|||NW McArthur Basin. A recessive unit with very poor outcrop. Shallow-marine deposits, often above wave base; bioherms grew in at least 6m of water.||Katherine River Group.||Conformably overlies Marlgowa and McKay Sandstones. Is overlain by Shadforth Sandstone probably unconformably (contacts are not observed).|Hemispherical stromatolitic bioherms, interbedded mudstone, dolostone, and fine- to medium-grained sandstone.|12-JUL-16
24881|Cottee Formation|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by Shadforth Sandstone, overlies McKay Sandstone||
24881|Cottee Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Katherine River Group.||||
24230|Coulters Sandstone|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup, Hatches Creek Group. Quartz arenite, lithic/ feldspathic arenite; minor siltstone.||||||07-NOV-08
24230|Coulters Sandstone|23733|5|Briefly described|p4, p33|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup. Correlative of Meerie and Coodna Members of the Hayward Creek Formation. See also p32 Fig.19, p34 Fig. 20.||||||07-NOV-08
24230|Coulters Sandstone|23809|5|Briefly described|p27|||Of the upper part of the Wauchope Subgroup.  Geological Province: Davenport Province.||||||17-MAR-05
24230|Coulters Sandstone|23823|5|Briefly described|p79 Fig. M3|||See also Coulters Sandstone - both names treated as informal in this study.||||||07-FEB-11
24230|Coulters Sandstone|24172|5|Briefly described|p37, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Overlain by Kudinga Basalt; underlain by Frew River Formation. Geological Province: Tennant Creek Inlier. Max. Thickness: 350m. Of the Hatches Creek Group. Lithic-bearing quartz arenite.||||||07-NOV-08
24230|Coulters Sandstone|39624|5|Briefly described|Table 1|||||||||
24230|Coulters Sandstone|39887|6|Mentioned|p453|||||||||
24230|Coulters Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24230|Coulters Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Quartz arenite and minor feldspathic arenite.  Overlies the Yeeradgi Sandstone.||||||10-JAN-05
24230|Coulters Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24230|Coulters Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24230|Coulters Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Quartz arenite; subordinate feldspathic arenite; minor pebbly arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24230|Coulters Sandstone|41129|4|Described|Table 1|||||||||
24230|Coulters Sandstone|41204|4|Described|Table 1|||||||||
24230|Coulters Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Quartz arenite, lithofeldspathic arenite, minor siltstone, altered basalt lava.||||||09-APR-06
24230|Coulters Sandstone|41308|5|Briefly described|Table 2|||||||||
24230|Coulters Sandstone|41310|4|Described|Table 1|||See also p11.||||||07-AUG-06
24230|Coulters Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24230|Coulters Sandstone|41524|4|Described|Table 1|||||||||
24230|Coulters Sandstone|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Quartz arenite, part feldspathic.||||||07-NOV-08
24230|Coulters Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24230|Coulters Sandstone|42217|6|Mentioned|p421|||||||||
24230|Coulters Sandstone|42643|4|Described|p12, Table 1 p6|||||||||
24230|Coulters Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Quartz arenite, subordinate feldspathic/lithic/kaolinitic arenite, siltstone.||||||07-NOV-08
24230|Coulters Sandstone|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup.||||||07-NOV-08
24230|Coulters Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
24230|Coulters Sandstone|45167|3|Fully described|Table 1|||Of Wauchope Subgroup.||||||07-AUG-06
24230|Coulters Sandstone|49033|2|Defined|p21|Proterozoic|Proterozoic|||||||
24230|Coulters Sandstone|60681|5|Briefly described|Map legend|Statherian|Statherian|Of the Hatches Creek Group. Quartz arenite, minor siltstone.  Geological Province: Davenport Province.||||||11-JAN-05
24230|Coulters Sandstone|60684|5|Briefly described|p12, p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Stated to both overlie and underlie Kudinga Basalt? (discrepancy?). Lithic, feldspathic and quartz arenite. Max. thickness: 350m. Geological Province: Davenport province.||||||07-NOV-08
24230|Coulters Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Upper Wauchope Subgroup (Hatches Creek Group).  Quartz arenite, feldspathic/lithic arenite; minor siltstone and altered mafic lava. In the Tennant Creek region.||||||07-NOV-08
24230|Coulters Sandstone|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Lithologically similar to Unimbra Sandstone. Overlies Yeeradgi Sandstone. Max. thickness: 500m. Geological Province: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
24230|Coulters Sandstone|64735|5|Briefly described|p205 Fig 1, p206 Fig 2, p212 Tb1, p213|Orosirian|Orosirian|Maximum depositional age from youngest detrital zircons.|1809 +/- 18 Ma.|Of Wauchope Subgroup, Hatches Creek Group.||Overlies Arabulja Volcanics; underlies Kudinga Basalt.||30-APR-12
24230|Coulters Sandstone|64956|6|Mentioned|p26|||||||||07-FEB-11
24230|Coulters Sandstone|65209|5|Briefly described|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Upper Wauchope Subgroup.||Wauchope Subgroup||Unconformably overlies Yeeradgi Sandstone. Correlates with Illoquara Sandstone.||05-JAN-17
24230|Coulters Sandstone|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of upper Wauchope Subgroup (Hatches Creek Group), Davenport Province. Disconformably overlies Newlands Volcanics; underlies Kudinga Basalt. Quartz arenite; feldspathic/lithic arenite; minor siltstone and altered mafic lava. Cross-section only||||||
24230|Coulters Sandstone|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of upper Wauchope Subgroup (Hatches Creek Group) Davenport Province. Disconformably overlies Newlands Volcanics; underlies Kudinga Basalt.  Non-outcropping. Inferred quartz arenite; feldspathic/lithic arenite; minor siltstone and altered mafic lava.||||||
24230|Coulters Sandstone|65338|5|Briefly described|p8 Table 1, pp19-20.|Paleoproterozoic|Paleoproterozoic|Non-outcropping, interpreted from geophysical data; lithology inferred from geophysical character and/or outcrop in adjacent sheet areas. Correlative with Gwynne Sandstone.||Unit in Wauchope Subgroup, Hatches Creek Group.||Is overlain by Frew River Formation.|Sandstone; minor siltstone and altered mafic lava.|19-OCT-11
24230|Coulters Sandstone|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup.||Unconformably overlies Mia Mia and Newlands Volcanics. Is overlain by the Frew River Formation.|Quartz arenite; subordinate feldspathic arenite; minor pebbly arenite.|
24230|Coulters Sandstone|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Hatches Creek Group.|||No outcrop: inferred quartz arenite, feldspathic/lithic arenite; minor siltstone and altered mafic lava.|
24230|Coulters Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Upper.||Overlies Yeeradgi and Unimbra Sandstones.|Quartz arenite, feldspathic/lithic arenite; minor siltstone and altered mafic lava.|
24230|Coulters Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1809 +/- 18 Ma (maximum depositional age).|Hatches Creek Group.||||
24230|Coulters Sandstone|67352|4|Described|p9 tab 1, p44 fig 48, p45|Orosirian|Orosirian|Region-wide bevelled, ridge-forming unit; minor recessive beds.||Wauchope Subgroup||Overlies unconformably Arabulja Volcanics, Newlands Volcanics and Yeeradgi Sandstone. Overlain conformably by Frew River Formation.|Quartz arenite; feldspathic, lithic and kaolinitic arenite; minor granule to pebble conglomerate: thinly to thickly bedded, medium-grained, well sorted; friable feldspathic arenite near top.|
24230|Coulters Sandstone|68518|4|Described|p7 Tb.1, p12|Proterozoic|Proterozoic|Thickness: 350-1000 m.||Wauchope Subgroup||Conformable on and possibly disconformable on Newlands Volcanics and Arabulja Volcanics; overlain conformably by Frew River Formation and unconformably by Cambrian and Mesozoic? strata.|Ridge forming quartz-arenite, subordinate feldspathic/lithic/kaolinitic arenite and rare pebbly arenite.|30-MAY-16
24230|Coulters Sandstone|69424|6|Mentioned|p9:10 Fig.9.9|||Murchison Syncline, Murchison Ranges.||||||12-JUL-16
24230|Coulters Sandstone|69425|4|Described|p10:3,10-14,16-18,20,23,24 Figs.10.18,19|Statherian|Statherian|Ridge-forming. 140m - over 1000m thick; thickens southward. Province-wide shallow-marine environment including tidal shelf and beach facies. Is correlated with Illoquara Sandstone, and Meerie and Coodna Members of Hayward Creek Formation. Maximum deposition age.|1809 +/- 6 Ma (Claoue-Long et al., 2008).|Wauchope Subgroup, upper.||Conformably overlies Yeeradgi Sandstone (locally unconformably), and Newlands and Arabulja Volcanics. Is overlain conformably by Frew River Formation and (in the NW) Kudinga Basalt.|Quartz sandstone, feldspathic/lithic sandstone; minor siltstone, micaceous sandstone and mafic lava. Detritus from underlying Arabulja Volcanics present locally. Local minor calcareous beds and altered probable basic lavas in ELKEDRA REGION area.|12-JUL-16
24230|Coulters Sandstone|69431|5|Briefly described|p16:5, 8, 22|||Davenport Province. Folding during the Davenport Event is discussed.||Wauchope Subgroup.||Probably correlated with Illoquara Sandstone, and Meerie and Coodna Members (Hayward Creek Formation).||12-JUL-16
24230|Coulters Sandstone|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1809+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24230|Coulters Sandstone|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24230|Coulters Sandstone|72380|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||||||
24230|Coulters Sandstone|73083|6|Mentioned|p9-10, p13-14, p19, p21, p23|||Davenport Province. Non-magnetic. [Misspelt as Coulter Sandstone, p9, p21]. Basal unit of the Upper Wauchope Subgroup. Thickness up to 1050 m (east limb of the Alexandra Syncline).||Wauchope Subgroup, Hatches Creek Group||Underlain by Newlands Volcanics. Overlain by Kudinga Basalt.||
24636|Cox Formation|23374|6|Mentioned|p21|||Of Arafura Basin.||||||07-AUG-06
24636|Cox Formation|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24636|Cox Formation|32660|5|Briefly described|Table 7|||||||||
24636|Cox Formation|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
24636|Cox Formation|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
24636|Cox Formation|42639|6|Mentioned|p46|||||||||
24636|Cox Formation|42739|5|Briefly described|map legend|Early Cambrian|Early Cambrian|Fine grained, usually micaceous sandstone, siltstone and shale; laminated siltstone, and red and green shale.||||||19-OCT-05
24636|Cox Formation|42812|1|Redefined|p79|Early Cambrian||||||||
24636|Cox Formation|43010|6|Mentioned|p183|||||||||
24636|Cox Formation|44112|6|Mentioned|p76|||||||||
24636|Cox Formation|44332|2|Defined|p.9,opp.6,map|||(D53-14). ?L.Cambrian.||||||
24636|Cox Formation|44333|14|Not recorded|map legend|||Lower Cambrian?||||||
24636|Cox Formation|44475|14|Not recorded|p.8||Proterozoic|(C53-15,16). No longer compared with Wessel Group (Proterozoic).||||||
24636|Cox Formation|44530|14|Not recorded|p.6,7,12,opp.12,16|||(D53-15).||||||
24636|Cox Formation|44531|14|Not recorded|map legend||Early Cambrian|Lower Cambrian.||||||
24636|Cox Formation|46792|6|Mentioned|p53|||Correlation||||||
24636|Cox Formation|64816|6|Mentioned|p3 Fig.2 |Cambrian|Cambrian|||||||
24636|Cox Formation|65337|4|Described|p60.|Early Cambrian|Ectasian|Unfossiliferous. Forms low hills and rubbly rises. Ectasian to earliest Cambrian.||Unit in Kiana Group.||Overlies Bukalara Sandstone.||
24636|Cox Formation|67352|6|Mentioned|p16|Ediacaran|Ediacaran|||Kiana Group||Conformably overlies Bukalara Sandstone.||
24636|Cox Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Northern Georgina Basin.||Kiana Group.||||12-JUL-16
24636|Cox Formation|69443|4|Described|p28:7, 12-13|Ediacaran|Ediacaran|Dunn (1963). Central-northern Georgina Basin. Unfossiliferous. Exposed as rubbly outcrops on low plateaux. Up to 50m thick. Relatively deep, storm-influenced subtidal marine deposits.||Kiana Group.||Conformably overlies Bukalara Sandstone.|Very fine- to fine-grained, usually micaceous sandstone, thinly interbedded with micaceous siltstone and shale, overlain by finely laminated siltstone and shale. Finer-grained lithofacies may be low-angle cross-stratified.|12-JUL-16
24636|Cox Formation|69451|6|Mentioned|p35:6|||Central northern Georgina Basin.||||Overlies the Bukalara Sandstone. Is correlated with the Raiwalla Shale (Arafura Basin).||12-JUL-16
24636|Cox Formation|69673|6|Mentioned|p116, p39, p40, p114 fig 92, p136|Neoproterozoic|Neoproterozoic|Up to 50m thick.||Kiana Group||Conformably overlies Bukalara Sandstone|Sandstone interbedded with siltstone and shale, laminated silstone and shale.|
24636|Cox Formation|70968|6|Mentioned|p89, p125, p131|Neoproterozoic|Neoproterozoic|Bauhinia Downs region. The Hayfield mudstone was misidentified as this unit in McManus-1 well.||||||
24636|Cox Formation|71632|5|Briefly described|Map legend.|||Georgina Basin. Mapped with Antrim Plateau Volcanics, Bukalara Sandstone, Nutwood Downs Volcanics and Top Springs Limestone as a single unit.||||||
24636|Cox Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south, partial) and southeastern McArthur Basin (partial).||||Underlain by Bukalara Sandstone||
24636|Cox Formation|73083|6|Mentioned|p27|Neoproterozoic|Neoproterozoic||||||Probably includes quartzite and sandstone.|
24636|Cox Formation|73086|6|Mentioned|p122|||Georgina Basin, northern.||||Correlates to Pertatataka Formation.||
76090|Coxco Dolostone Member|64815|6|Mentioned|p4 Fig.2, p14 Tb.5, p16-17 |||Called Dolomite in Tb.5.||Unit in Teena Dolostone.||||
76090|Coxco Dolostone Member|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Teena Dolostone.|||Grey crystalline dololutite with radiating, needle-like gypsum crystal pseudomorphs normal to bedding; rare conical stromatolites; uncommon thin interbeds of dolomitic shale and siltstone.|
76090|Coxco Dolostone Member|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. 70 m thick.||Teena Dolostone||Is overlain conformably by Barney Creek Formation.|Crystalline dolomudstone: thickly bedded; minor dolomitic shale, siltstone.|
76090|Coxco Dolostone Member|69430|4|Described|p15:3, 16, 18, 39, 61|Statherian|Statherian|Southern McArthur Basin. 15-70m thick. Seafloor cement associated with transgression and upwelling. Characterised by the presence of "Coxco Needles": radiating fans or layers of bottom-nucleated, acicular, near-vertical dolomite crystals typically 6-10cm long that pseudomorph an earlier mineral. Similar structures occur in apparently coeval Saint Vidgeon Formation and from other Paleoproterozoic north Australian basins. Origins and implications are discussed. Has palaeo-hydrocarbon reservoirs: intervals contain extensive bitumen and other hydrocarbons.||Teena Dolostone.||Is overlain conformably and gradationally by Barney Creek Formation.|Grey crystalline dololutite with radiating, needle-like gypsum crystal pseudomorphs normal to bedding; rare conical stromatolites; uncommon thin intervals of dolomitic shale and siltstone.|12-JUL-16
76090|Coxco Dolostone Member|69673|4|Described|p33, p41, p42, p43, p45|||Batten Fault Zone. Gas show, proven conventional reservoir rock. 15-70m thick.||Teena Dolostone||Conformably overlain by Barney Creek Formation|Brecciated Dolostone, medium to thinly bedded dolomudstone and minor flat pebble conglomerate.|
76090|Coxco Dolostone Member|72373|5|Briefly described|p8,11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Contains tuff unit near the top of the unit dated at 1639+\-6 Ma (Page et al 2000).||Unit of Teena Dolostone.||||
76090|Coxco Dolostone Member|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Batten Fault Zone of the Southern McArthur Basin.||[Teena Dolostone,] Batten Subgroup||Overlies Teena Dolostone and underlies Barney Creek Formation.||
76090|Coxco Dolostone Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Teena Dolostone?, Umbolooga Sub-group, McArthur Group||Underlain by Teena Dolostone. Overlain by Barney Creek Formation including W-Fold Shale Member and Cooley Dolostone Member.||
76090|Coxco Dolostone Member|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Probably of Teena Dolostone, Batten Subgroup||Overlies Teena Dolostone and underlies Barney Creek Formation.||
76090|Coxco Dolostone Member|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group||Underlain by Teena Dolostone. Overlain by Barney Creek Formation.||
27960|Crater Formation|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
27960|Crater Formation|22810|4|Described|Table2 P5, P12|||Unconformable on Celia Dolomite, lateral equivalent of Mundogie Sandstone, maximum thickness 600m||||||
27960|Crater Formation|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Part of the Mount Partridge Group. Feldspathic to arkosic sandstone and conglomerate, quartzite, haematite boulder conglomerate, siltstone.||||||07-NOV-08
27960|Crater Formation|23714|4|Described|p9|Proterozoic|Proterozoic|See also page 8 Table 1. Of Mount Partridge Group. Overlying unit Coomalie Dolomite. Geological Province: Rum Jungle Region. Max. thickness: 600 m.||||||
27960|Crater Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the Mount Partridge Group, in the Rum Jungle Region||||||
27960|Crater Formation|23733|5|Briefly described|p32 Fig. 19|||Of Mount Partridge Group.||||||
27960|Crater Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Sandstone, conglomerate.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
27960|Crater Formation|24442|6|Mentioned|p45|||||||||
27960|Crater Formation|29550|6|Mentioned|p43|||||||||
27960|Crater Formation|30558|4|Described|p35|||Lower Proterozoic age||||||
27960|Crater Formation|30838|6|Mentioned|Fig.1|||||||||
27960|Crater Formation|32660|5|Briefly described|Table 2|||||||||
27960|Crater Formation|32819|6|Mentioned|p35|||||||||
27960|Crater Formation|32873|6|Mentioned|Fig.1|||See also Fig.15||||||
27960|Crater Formation|32875|5|Briefly described|Fig.1|||||||||
27960|Crater Formation|33278|5|Briefly described|Fig.2|||||||||
27960|Crater Formation|35055|5|Briefly described|p222|||||||||
27960|Crater Formation|35140|6|Mentioned|Fig.2|||||||||
27960|Crater Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
27960|Crater Formation|37462|6|Mentioned|Fig.4.8|||||||||
27960|Crater Formation|38239|6|Mentioned|Fig.2|||||||||
27960|Crater Formation|38349|6|Mentioned|Table 4|||||||||
27960|Crater Formation|38351|6|Mentioned|Table 3|||||||||
27960|Crater Formation|39069|5|Briefly described|Table 1|||See also Fig.7.||||||
27960|Crater Formation|39320|6|Mentioned|Fig.2|||||||||
27960|Crater Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27960|Crater Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Siltstone and shale; conglomerate, in places showing graded bedding; sandstone, commonly ripple marked; arkose.||||||07-NOV-08
27960|Crater Formation|40243|6|Mentioned|p142|||Mention Fig.2||||||
27960|Crater Formation|40493|6|Mentioned|p22|||||||||
27960|Crater Formation|40495|6|Mentioned|Fig.5|||||||||
27960|Crater Formation|40808|3|Fully described|p3|||||||||
27960|Crater Formation|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27960|Crater Formation|40852|5|Briefly described|p25|||||||||
27960|Crater Formation|41125|6|Mentioned|p26|||||||||
27960|Crater Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27960|Crater Formation|41305|3|Fully described|p11|||||||||
27960|Crater Formation|41663|6|Mentioned|p15|||||||||
27960|Crater Formation|42202|6|Mentioned|Fig.1 P511|||||||||
27960|Crater Formation|43187|5|Briefly described|p2|||||||||
27960|Crater Formation|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|Max. thickness: 900m.||||||07-NOV-08
27960|Crater Formation|44314|2|Defined|p.6-7,14|||(D52-4). Darwin Sheet. Tb.1.||||||
27960|Crater Formation|44315|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
27960|Crater Formation|45022|5|Briefly described|p.27||Paleoproterozoic|Of Bachelor Group. On many pages. Tb.2. Fig.7, Plate 28,30.||||||07-NOV-08
27960|Crater Formation|46163|14|Not recorded|p.168,170|||||||||
27960|Crater Formation|46658|6|Mentioned|p550|||||||||
27960|Crater Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Siltstone and shale, conglomerate in places, sandstone commonly ripple-marked, arkose; poorly sorted pebble to boulder conglomerate commonly containing pebbles to boulders of BIF.  Unconformably overlies Celia Dolomite.||||||07-NOV-08
27960|Crater Formation|46676|14|Not recorded|p.6||Paleoproterozoic|L. Proterozoic; unit of Batchelor Group.||||||07-NOV-08
27960|Crater Formation|47049|6|Mentioned|Fig.2|||||||||
27960|Crater Formation|50623|4|Described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Manton Gorup. Grades up into Coomalie Dolostone. Arkose, conglomerate, coarse sandstone and minor shale. Of Mount Partridge Group.||||||07-NOV-08
27960|Crater Formation|60575|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.||||||07-NOV-08
27960|Crater Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Conglomerate, in places showing graded bedding; conglomerate containing BIF, sandstone commonly ripple marked; arkose, minor siltstone and shale. Overlies Celia Dolostone. Overlain by Coomalie Dolostone. Of Mount Partidge Group.||||||11-JAN-05
27960|Crater Formation|61389|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Quartz-pebble arkose, poorly sorted BIF-quartz pebble-boulder conglomerate, sandstone, siltstone, shale.||||||
27960|Crater Formation|62375|5|Briefly described|p10 Fig. 3, 14|Paleoproterozoic|Paleoproterozoic|Sandstone, conglomerate. Geological Province: Pine Creek Orogen. Underlies: Coomalie Dolomaite.||||||09-FEB-10
27960|Crater Formation|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Of Mount Partridge Group.  Max. thickness 650m. Feldspathic quartz sandstone, quartz-pebble conglomerate, poorly sorted BIF-quartz pebble-boulder conglomerate, siltstone, mudstone.||||||07-JAN-09
27960|Crater Formation|64730|5|Briefly described|p125, 138|Paleoproterozoic|Paleoproterozoic|In western Central Domain. Age from volcanic rocks in the Wildman Siltstone (near top of Group).|Min. deposition age 2019 +/- 4 Ma.|Basal unit of Mount Partridge Group.|||Fluvial immature clastics.|03-MAY-12
27960|Crater Formation|65232|5|Briefly described|p51, p56-57, p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Of Mount Partridge Group. Grades upwards into Coomalie Dolostone; unconformably over Archean basement. Arkose, coarse sandstone, conglomerate, minor shale.||||||09-FEB-10
27960|Crater Formation|65339|4|Described|pp6-9. |||Exposed on western side of Rum Jungle and Waterhouse Domes. Fluviatile to shallow marine deposits. 300 - 600 m thick. Conglomerates are clast-supported; ironstone sourced from Stanley Metamorphics, and sedimentary clasts from underlying Manton Group. Lower part is anomalously high in thorium.||Unit in Mount Partridge Group.||Unconformably overlies Celia Dolostone. Is overlain by Coomalie Dolostone.|Conglomerate, locally with graded bedding; conglomerate containing banded ironstone; sandstone, commonly ripple-marked; arkose; minor siltstone and shale.|
27960|Crater Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Mount Partridge Group.||Is overlain by Coomalie Dolostone.|Feldspathic quartz sandstone, quartz-pebble conglomerate, poorly-sorted banded ironstone, quartz pebble-boulder conglomerate, siltstone, mudstone.|23-NOV-11
27960|Crater Formation|67355|4|Described|p7, p10-11, p16-17, p25-7, p48 Fig.39||Neoarchean|Previously assigned to the Batchelor Group (Walpole et al.,1968). Maximum thickness of 650 m. Deposited in fluviatile to shallow-marine conditions. Mapped and described by French (1970). Hosts the Batchelor gold mine.||Mount Partridge Group||Underlies the Coomalie Dolostone conformably. Overlies the Celia Dolostone unconformably.|Includes: banded ironstone conglomerate; poorly sorted arkosic coarse sandstone gravel; medium to coarse quartz sandstone, with minor quartz pebble conglomerate.|25-JAN-17
27960|Crater Formation|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen. Correlative of Mundogie Sandstone.|||||Sandstone, conglomerate.|
27960|Crater Formation|67779|5|Briefly described|p6 Fig.5, p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Lateral equivalent of Mundogie Sandstone.||Basal unit in Mount Partridge Group.||Is overlain by Coomalie and Koolpinyah Dolostones.||
27960|Crater Formation|69383|5|Briefly described|p21-27||Archean|Of Woodcutters Supergroup. Pine Creek Orogen, Central Domain. LA-ICPMS  U-Pb and Hf geochronology analyses. 2 samples. Max deposition age.|3125+/-6, 2527+/-15 Ma||||Sandstone sampled from drillcore. Medium- to coarse?grained arkosic quartz sandstone with well defined cross-bedding sampled from outcrop.|
27960|Crater Formation|69419|6|Mentioned|p4:3-4|||W. Pine Creek Orogen. Includes clasts which contain preserved tightly-refolded folds from previous deformation.||||||12-JUL-16
27960|Crater Formation|69420|4|Described|p5:4, 6, 8-9, 30, 75-76|Paleoproterozoic|Paleoproterozoic|Rum Jungle region, Central Domain, Pine Creek Orogen. Up to 900m thick. Fluvial deposits. Detrital zircon populations are from sources not currently recognised in the NT. Deformation discussed.||Mount Partridge Group.||Is overlain by Coomalie and Koolpinyah Dolostones. Lateral equivalent of Mundogie Sandstone.|Conglomerate, arkose, sandstone, and minor siltstone and shale.|12-JUL-16
27960|Crater Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Mount Partridge Group.||Unconformably overlies Celia Dolostone (Manton Group). Is overlain conformably by Coomalie Dolostone.|Feldspathic quartz sandstone, quartz-pebble conglomerate, poorly sorted banded ironstone, quartz-pebble-boulder conglomerate, siltstone, mudstone.|
27960|Crater Formation|71302|5|Briefly described|p73|Mesoarchean|Mesoarchean|Geological province: Pine Creek Orogen.||Unit of Mount Partridge Group.||||09-DEC-19
27960|Crater Formation|71349|6|Mentioned|p737|||Pine Creek Orogen. Contains zircons aged c.3.1 Ga (significance explained).||||||
27960|Crater Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2527+/-15 Ma (MDA: U-Pb zircon LA-ICPMS).||||Sandstone, cross-bedded quartz sandstone.|
27960|Crater Formation|73184|6|Mentioned|p192|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Several detrital zircon ages of 3.68-3.12 Ga from the Crater Formation (Hollis et al., 2010).||||||
27754|Crawford Formation|22538|6|Mentioned|Fig3 P708|||||||||
27754|Crawford Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27754|Crawford Formation|22853|3|Fully described|26|Proterozoic|Proterozoic|Of Roper Group. Max thickness 140 m. Underlying unit: Mainoru Formation.||||||08-AUG-06
27754|Crawford Formation|23404|5|Briefly described|p645|||Of Roper Group.||||||
27754|Crawford Formation|23776|5|Briefly described|p705 Fig 2.|||Of Roper Group.||||||08-AUG-06
27754|Crawford Formation|23937|2|Defined|p77 App. 1, p36|Calymmian|Calymmian|Of Collara Subgroup (Roper Group).  Overlain disconformably by Arnold Sandst, and by Jalboi Fm. where the sandstone is missing; conformably overlies the Showell Member (Mainoru Formation).  Age: ~1490Ma.  Max. thickness: >235m.  Geol.Prov: McArthur Basin.||||||08-AUG-06
27754|Crawford Formation|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
27754|Crawford Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: grey-brown to greenish, fine-grained, thin to thick-bedded, commonly micaceous, glauconitic in places, hummocky cross-beds; interbedded mudstone: khaki green to red, micaceous, thin bedded. Geol. Prov: McArthur Basin.||||||13-OCT-05
27754|Crawford Formation|24050|3|Fully described|p46, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Micaceous and glauconitic sandstone; mudstone and siltstone and upper sandstones.  Overlies Mainoru Formation; underlies Arnold Sandstone.  Max. thickness: 320m.||||||08-AUG-06
27754|Crawford Formation|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
27754|Crawford Formation|24303|6|Mentioned|p61 Appendix|||Correlative of the Grayling Member. See also p24 Tb.4||||||
27754|Crawford Formation|32660|5|Briefly described|Table 4|||||||||
27754|Crawford Formation|35114|6|Mentioned|p204|||||||||
27754|Crawford Formation|38042|6|Mentioned|p159|||||||||
27754|Crawford Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27754|Crawford Formation|40691|4|Described|p75|||||||||
27754|Crawford Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27754|Crawford Formation|41220|6|Mentioned|p366|||||||||
27754|Crawford Formation|41268|6|Mentioned|p291|||||||||
27754|Crawford Formation|42385|4|Described|p26|||See also Table 5 p25.||||||08-AUG-06
27754|Crawford Formation|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
27754|Crawford Formation|42597|5|Briefly described|Map legend|Adelaidean||||||||
27754|Crawford Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Lower Roper Group (Roper Group).||In schematic section, underlies Arnold Sandstone Member (Abner Sandstone); overlies Mainoru Formation.|Micaceous sandstone and siltstone with minor mudstone beds, glauconitic sandstone, feldpathic sandstone. Detailed lithology given.|11-NOV-11
27754|Crawford Formation|42639|4|Described|p38, Table 7 p39|||||||||
27754|Crawford Formation|42700|5|Briefly described|map legend|Mesoproterozoic||||||||
27754|Crawford Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Fine to medium grained glauconitic and micaceous sandstone; siltstone and mudstone, commonly ferruginous and in places micaceous.||||||08-AUG-06
27754|Crawford Formation|42812|3|Fully described|p50, Table 5|||Of Roper Group.||||||08-AUG-06
27754|Crawford Formation|42846|5|Briefly described|Fig.1 p502|||Of Roper Group. Geological Province: McArthur Basin.||||||09-MAY-05
27754|Crawford Formation|43010|5|Briefly described|p164|||||||||
27754|Crawford Formation|43036|4|Described|p60|||Of Roper Group.||||||08-AUG-06
27754|Crawford Formation|43645|5|Briefly described|p562|||||||||
27754|Crawford Formation|43652|6|Mentioned|p386|||||||||
27754|Crawford Formation|44112|5|Briefly described|Table12p68,70-71|||Originally mapped by Dunnet (1965) as the upper sandy part of the 'Wigram Formation' and the overlying 'Pobasso Formation' of the 'Malay Road Group'||||||
27754|Crawford Formation|44287|14|Not recorded|p.12, opp.11|||(E53-3).||||||
27754|Crawford Formation|44288|14|Not recorded|Not recorded|||White card ref. not found.||||||
27754|Crawford Formation|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
27754|Crawford Formation|44300|14|Not recorded|map legend|||||||||
27754|Crawford Formation|44332|14|Not recorded|p.8,opp.6,map|||(D53-14).||||||
27754|Crawford Formation|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
27754|Crawford Formation|44400|2|Defined|p.9,Tb.1,opp.p.6,map|||Overlain by Abner Sandstone (D53-6).||||||08-AUG-06
27754|Crawford Formation|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27754|Crawford Formation|44434|14|Not recorded|p.8, opp. p.6, map|||(D53-11,12).||||||
27754|Crawford Formation|44435|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27754|Crawford Formation|44436|5|Briefly described|p.11,, opp. p.7, map|||(E53-4).||||||02-DEC-04
27754|Crawford Formation|44437|5|Briefly described|map legend|Precambrian|Precambrian|Of the Roper Group.  Blocky micaceous glauconitic feldspathic sandstone, micaceous siltstone.  Conformably overlies Mainoru Formation; conformably overlain by Abner Sandstone.  Upper (?) Proterozoic.||||||08-DEC-04
27754|Crawford Formation|44459|14|Not recorded|p.8, opp.p.6, map|||(E53-2).||||||
27754|Crawford Formation|44460|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27754|Crawford Formation|44471|14|Not recorded|p.9,11,15,opp.7, map|||(D53-10). Glauconitic.||||||
27754|Crawford Formation|44472|5|Briefly described|map legend|||Of the Maiwok Sub-Group (Roper Group).  Blocky quartz sandstone, flaggy micaceous quartz sandstone, siltstone.||||||02-DEC-04
27754|Crawford Formation|44473|14|Not recorded|p.10, opp. p.7|||(E53-7). (Roper Group).||||||
27754|Crawford Formation|44474|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27754|Crawford Formation|44530|14|Not recorded|p.11,12, opp.12|||(D53-15).||||||
27754|Crawford Formation|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
27754|Crawford Formation|45022|14|Not recorded|p.80||Adelaidean|Of Roper Group.||||||
27754|Crawford Formation|45162|6|Mentioned|p148|||||||||
27754|Crawford Formation|46861|6|Mentioned|Fig.2a|||||||||
27754|Crawford Formation|48894|6|Mentioned|p24|||See also PP25,26. 1140-1390 +-20my||||||
27754|Crawford Formation|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin||||||
27754|Crawford Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Abner Sandstone, underlain by Mainoru Formation.||||||
27754|Crawford Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Fine-grained, thick bedded sandstone, red-brown, glauconitic; thinly interbedded very fine and siltstone; minor parallel laminated mudstone. Overlies Mainoru Fm; underlies Jalboi Fm.||||||15-FEB-05
27754|Crawford Formation|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlain by the Abner Sandstone. Overlies the Mainoru Formation. Grey fine- to coarse-grained glauconitic sandstone.||||||23-NOV-04
27754|Crawford Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Sandstone: fine grained, thick bedded, swaley cross-stratified, red-brown, glauconitic.||||||
27754|Crawford Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: grey-brown to greenish, fine-grained, thin to thick-bedded, commonly micaceous, glauconitic in places, hummocky cross-beds; interbedded mudstone: khaki green to red, micaceous, thin bedded. Geol. Prov: McArthur Basin.||||||
27754|Crawford Formation|61566|5|Briefly described|p622|Proterozoic|Proterozoic|Of the Roper Group. Geological Province: McArthur Basin.||||||
27754|Crawford Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||
27754|Crawford Formation|64784|5|Briefly described|p2 Fig.2|Proterozoic|Proterozoic|Beetaloo Basin.||Unit in Roper Group.||Overlies Mainoru Formation.||
27754|Crawford Formation|64815|6|Mentioned|p5 Fig.3 |||||Of the Roper Group.||||
27754|Crawford Formation|64816|6|Mentioned|p2 Fig.1 |||||Unit in Roper Group.||||
27754|Crawford Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
27754|Crawford Formation|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||Unit in Roper Group.||||
27754|Crawford Formation|65228|6|Mentioned|Fig.02.|||||Unit in Roper Group.||Overlies Mainoru Formation. Is overlain by Abner Sandstone.||
27754|Crawford Formation|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
27754|Crawford Formation|65337|6|Mentioned|p45.|||McArthur Basin. Has hummocky cross-stratification similar to that seen in the shallow-water sandstone facies of the Crow Formation.||||||
27754|Crawford Formation|65340|5|Briefly described|p62.|Mesoproterozoic|Mesoproterozoic|Forms moderately resistant, benched sandstone and minor mudstone cliffs. Reflects a mainly subtidal, storm-wave-influenced marine shelf environment.||Unit in Roper Group.||Overlies Mainoru Formation. Is overlain by Abner Sandstone.|Brown or grey, pseudokarstically weathering, thickly bedded, lithic fine sandstone containing large-scale hummocky cross-stratification; minor micaceous mudstone and tabular glauconitic sandstone.|
27754|Crawford Formation|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 101 m.||Unit in Roper Group.||Overlies Mainoru Formation.|Sandstone, mudstone, siltstone.|
27754|Crawford Formation|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|Ridge-forming.||Unit in Roper Group.||Overlies Mainoru Formation. Is overlain by Abner Sandstone.|Red-brown, fine-grained, micaceous sandstone and siltstone with minor mudstone beds; glauconitic sandstone, feldspathic sandstone; cross-beds, mudstone intraclasts and clast imprints, mudcracks, convolute beds.|
27754|Crawford Formation|67352|4|Described|p13 Tb.2|Calymmian|Calymmian|McArthur Basin. Over 200 m thick.||Roper Group||Overlies Mainoru Formation (conformably). Overlain conformably by Abner Sandstone.|Upper: equant to massive, fine- to-medium-grained micaceous and feldspathic sandstone and quartz wacke, in part glauconitic. Lower: tabular, fissile, ferruginous and micaceous siltstone and wacke.|
27754|Crawford Formation|68592|5|Briefly described|p673|||Green (1980). Now the middle part of Box Ridge Volcanics.||||Overlay Pine Ridge Volcanics. Was overlain by Barrier Volcanics.|Mostly siltstone.|
27754|Crawford Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
27754|Crawford Formation|69430|4|Described|p15:3, 26-27, 29-30, 34, 62|Calymmian|Calymmian|McArthur Basin. 0-235m thick. Storm-dominated shelf sediments. Appears as Crawford Member on 15:30.||Collara Subgroup.||Conformably and gradationally overlies Showell Member (Mainoru Formation). Is overlain by Abner Sandstone or disconformably by Arnold Sandstone and Jalboi Formation.|Thickly bedded, mostly fine-grained micaceous and glauconitic sandstone; subsidiary thinly interbedded sandstone, siltstone and mudstone; minor trough cross-bedded medium quartz sandstone.|12-JUL-16
27754|Crawford Formation|69673|6|Mentioned|p16 fig 13|||McArthur Basin.||Collara Subgroup||Overlain by Arnold Sandstone, Overlies Mainoru Formation||
27754|Crawford Formation|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Storm-dominated shelf (sandstone-dominated).||Of Collara Subgroup.||Overlies Mainoru Formation. Overlain by Arnold Sandstone.||
27754|Crawford Formation|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Mainoru Formation; overlain by Arnold Sandstone.|Fluvial and marine sandstones.|
27754|Crawford Formation|70897|6|Mentioned|Fig.1.7.6,9|||McArthur Basin.||||||29-NOV-17
27754|Crawford Formation|70968|2|Defined|p6, p18, p33, p35-39, p41-44, p46, p123|Calymmian|Calymmian|See also p126-128, p131, p137, p140, p143. Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Originally mapped (Dunnet, 1965) as upper part of Wigram Formation and overlying Pobassoo Formation of the Malay Road Group: these names now abandoned. Named after Crawford Creek. 235m thick at the type section, on S slope of Mount Faveng, from 452900mE 8395100mN (base) to 452200mE 8395700mN in URAPUNGA sheet. Crops out as low strike ridges separated by recessive intervals. Widespread unit. Lithology described and illustrated in detail. Storm-dominated marine shelf deposits. Attempts at dating are described. Detrital zircon diagram.||Collara Subgroup.||Conformably and gradationally overlies Mainoru Formation. Is intruded by Derim Derim Dolerite. Underlies Jalboi Formation or Arnold Sandstone disconformably (locally conformably).|Distinctively flat to wavy-laminated, thickly-bedded, red-brown fine-grained sandstone, alternating with thinly interbedded sandstone, mudrocks and minor, grey, trough cross-bedded medium-grained sandstone.|
27754|Crawford Formation|71059|4|Described|p3, p14-16|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 0-235m thick. Storm-dominated marine shelf deposits. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, data all detailed.||Collara Subgroup.||Conformably overlies Showell Member (Mainoru Formation). Is overlain unconformably to disconformably by Jalboi Formation, and conformably to disconformably by Arnold Sandstone.|Thickly bedded, red-brown fine sandstone alternating with recessive thinly interbedded fine sandstone, mudrocks and minor medium quartz sandstone.|
27754|Crawford Formation|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Showell Creek Member (Mainoru Formation). Overlain by the Arnold Sandstone.||
27754|Crawford Formation|71494|6|Mentioned|p3-p4, p10, p14-p15|||||||Conformably overlies Showell Member.||03-MAY-18
27754|Crawford Formation|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
27754|Crawford Formation|71893|3|Fully described|iii, p2-p5, p8, p17-p21|Calymmian|Calymmian|McArthur Basin. A type section occurs at Mount Faveng about 23km NNE of Roper Bar in northwestern URAPUNGA. Originally named by Dunn, 1963a and appears in Sweet and Abbott in Abbott et al, 2001. Characterised by laminated and hummocky and swaley cross-stratified beds. Deposited in a storm-dominated marine shelf environment. A youngest individual age of 1711 +/- 16 Ma was obtained and a maximum depositional age of 1713 +/- 14 Ma (U-Pb-Hf) was also derived in this study. The units age is constrained by a date of 1492 +/- 4 Ma from the underlying Showell Member of the Mainoru Formation and a Re-Os date of 1417 +/- 29 Ma and 1361 +/- 21 Ma from the Kalala and Wyworrie members respectively of the Velkerri Formation. Description at type section, zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Collara Subgroup||Conformably overlies the Mainoru Formation. Disconformably overlain by the Arnold Sandstone, Jalboi Formation or the Abner Sandstone.|Thickly bedded, red-brown fine-grained sandstone which alternates with thinly interbedded sandstone and shale in upwards-coarsening and thickening cycles.|
27754|Crawford Formation|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin, Batten Fault Zone and Southeastern McArthur Basin.||Collara Subgroup||Overlies Mainoru Formation and underlies Arnold Sandstone.||
27754|Crawford Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Collara Subgroup, Roper Group||Underlain by Mainoru Formation. Overlain by Arnold Formation and Abner Sandstone.||
27754|Crawford Formation|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 Mainoru Formation and underlies Arnold Sandstone.||
27754|Crawford Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Mainoru Formation. Overlain by Arnold Sandstone and Abner Sandstone.||
27754|Crawford Formation|73242|5|Briefly described|p38-40|||||Collara Subgroup, Roper Group||Underlain by Showell Member, Mainoru Formation. Overlain by Arnold Sandstone. Intruded by Derim Derim Dolerite.|Includes tidal Sandstone.|
27754|Crawford Formation|73412|5|Briefly described|p4, 8, 11|||Southern McArthur Basin.||Collara Subgroup.||Overlies Mainoru Formation. Is overlain by Abner Sandstone.||
26504|Crooked Hole Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jervois ?Suite (Jervois presented in Table 4.1 in isolation). Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26504|Crooked Hole Granite|33103|4|Described|Table 2|||||||||
26504|Crooked Hole Granite|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26504|Crooked Hole Granite|39888|6|Mentioned|Fig.7|||||||||
26504|Crooked Hole Granite|50369|5|Briefly described|p1.4, 9.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jervois Suite.||||||07-NOV-08
26504|Crooked Hole Granite|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Foliated biotite granite and granodiorite, pegmatite. Geological Province: Arunta Region.||||||07-NOV-08
26504|Crooked Hole Granite|65341|4|Described|p2 Fig.2, p4, p7. |Paleoproterozoic|Paleoproterozoic|A distinctly tabular or sill-like body within Delny Metamorphics gneiss. Reportedly similar to Copia Granite; both are syn- or pre-tectonic. Has relatively low radiometric response and is non- to moderately magnetic.|1780 - 1770 Ma.|||Intrudes Delny Metamorphics.|Strongly foliated biotite granite and granodiorite; abundant plagioclase, largely regressed to sericite; accessory titanite and zircon.|19-JUN-13
26504|Crooked Hole Granite|65556|6|Mentioned|p43|||Intrudes Delny Metamorphics.||||||
26504|Crooked Hole Granite|69427|5|Briefly described|p12:12, 29-30|Statherian|Statherian|Jinka Domain, Aileron Province. Shares a common fabric with the Delny MetamorphicS which it intrudes. Is similar to the Copia Granite.|c.1780-1760 Ma.|||Intrudes Delny Metamorphics.|Strongly foliated biotite granodiorite.|12-JUL-16
26504|Crooked Hole Granite|69917|4|Described|p95-96, 103|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating.  1806+/-12 Ma is interpreted to be the intrusive age of the granite. Sample also shows significant inheritance from Delny Metamorphics.||||Intrudes Delny Metamorphics. Compared with Copia Granite|Gneissic granite. Biotite granodiorite with plagioclase largely retrogressed to sericite and accessory titanite and zircon.|
26504|Crooked Hole Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1806+/-12 Ma (Pb/Pb zircon LA-ICPMS).||||Granite.|
26504|Crooked Hole Granite|73551|5|Briefly described|piii, p3-5, p7, p9|Orosirian|Orosirian|Protolith granite yielded an emplacement age of 1806 +/- 12 Ma (Beyer et al., 2013). A biotite 40Ar/39Ar age records cooling below 320-280C at 441 +/- 5 Ma.|ca 1.81 Ga|||Intrudes the Delney Metamorphics.|Includes gneissic biotite granite-granodiorite.|
81443|Crossing Bore schist|70839|6|Mentioned|p344|||Geological province: Irindina Province. Contains detrital zircon age spectra that resemble Amadeus Basin Supersequence 4 (c. 1.25-1.05 Ga).||||||
81443|Crossing Bore schist|72516|6|Mentioned|p90|Cambrian|Cambrian|Irindina Province. Age correlative of the Mount Baldwin Formation.||||||02-JUN-21
37729|Crow Formation|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Wild Cow Subgroup (South Nicholson Group).  Age: ~1450Ma. ||||||
37729|Crow Formation|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Wild Cow Subgroup. Interbedded lithic micaceous siltstone and fine grained sandstone, reddish brown to grey shale, chalky white claystone, fine to medium grained, quartzose to sublithic sandstone.||||||
37729|Crow Formation|64443|6|Mentioned|p3|Calymmian|Calymmian|||Of the Wild Cow Subgroup.||Disconformably underlies the Mittiebah Sandstone.||14-MAY-14
37729|Crow Formation|65337|2|Defined|p8, p38 Table 5, pp43-50.|Mesoproterozoic|Mesoproterozoic|New name. Encompasses half the outcrops mapped (Smith and Roberts 1963) as Mullera Formation; the rest is now Constance Sandstone. Has several facies: deep-shelf, storm shelf, sandy turbidite, shallow-water sandstone, saprolite. Extensively ferruginised.|1450 Ma.|Unit in Wild Cow Subgroup.|Includes Tobacco Member.|Overlies Bowgan and Playford Sandstones. Is overlain by Mittiebah and, disconformably, Constance Sandstones.|Interbedded lithic micaceous siltstone and fine-grained sandstone, red-brown to grey shale, chalky white claystone, fine- to medium-grained, quartzose to sub-lithic sandstone; minor very coarse-grained sandstone and conglomerate.|
37729|Crow Formation|67352|6|Mentioned|p12|Calymmian|Calymmian|||Wild Cow Subgroup||Is overlain by Mittiebah Sandstone, conformably or disconformably.||
37729|Crow Formation|69433|6|Mentioned|p18:4|||||||Overlies Buddycurrawa Volcanics probably unconformably.||12-JUL-16
37729|Crow Formation|69434|4|Described|p19:2, 4-5, 8|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Formerly mapped by Smith and Roberts (1963) as parts of the Mullera Formation, Mittiebah Sandstone and Benmara beds. Up to 2500m thick. Largely recessive: poor outcrops. Shallow- to deep-marine shelf deposits, with development of fan delta in the NW adjacent to tectonic uplift (localised interdigitated turbidite and debris-flow facies). Hosts several "Clinton-type" oolitic iron ore occurrences (described) in NT. May have some potential for base metals.||Wild Cow Subgroup.|Tobacco Member.|Overlies Bowgan, Playford Sandstones conformably, Benmara Group and Murphy Metamorphics unconformably. Underlies Mittiebah Sandstone conformably, Constance Sandstone disconformably or unconformably.|Interbedded lithic micaceous siltstone and fine sandstone, shale, claystone, fine to medium quartzic to sublithic sandstone; minor, poorly sorted medium to very coarse sandstone, pebbly sandstone and matrix-supported conglomerate.|12-JUL-16
37729|Crow Formation|69673|4|Described|p56|||Up to 2500m thick.||Wild Cow Subgroup|||Interbedded siltstone and sandstone, shale, claystone, quartzose to sublithic sandstone and minor local sandstone and matrix supported conglomerate.|
37729|Crow Formation|70968|5|Briefly described|p131 Fig.118, p132|Calymmian|Calymmian|May correlate (at least in part) with Mainoru Formation.||Wild Cow Subgroup.||||
37729|Crow Formation|71369|5|Briefly described|p6, p8|||Rawlings et al. (2008). South Nicholson Basin.||Wild Cow Subgroup.|Tobacco Member.|||
37729|Crow Formation|72526|5|Briefly described|p8 Fig.1.3, p56, p86.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Wild Cow Subgroup|Includes Tobacco Member.|Overlies Bowgan Sandstone and underlies Mittiebah Sandstone conformably to disconformably, and No Mans Sandstone Member.||
37729|Crow Formation|72527|4|Described|p1, p8, p20, p42, p49-77.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Four samples analysed for age data. Stratigraphic position of samples within Crow Formation is unclear. Other ages determined: 1649+/-19 Ma,  1623+/-24 Ma, 1569+/-22 Ma, both maximum depositional ages. Previous assumptions about depositional age based on tentative correlation with Mainoru Formation of Roper Group (includes tuffs dated at c. 1492 Ma. Thickness up to 2500m . Displays remarkably similar age spectra to Caulfield beds, Bowgan Sandstone and Bullrush Conglomerate. Type locality shown as 136.91709dE 18.08152dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios. See also p78, p86, p161, p193, p195-197.|1483+/-12 Ma max. dep. age|Wild Cow Subgroup|Includes Tobacco Member.|Overlies Bowgan Sandstone,Playford Sandstone, Benmara Group. Unconformably underlies Constance Sandstone.|Interbedded siltstone, sandstone, shale and lesser conglomerate. Sample was of feldspathic sandstone.|
37729|Crow Formation|72912|4|Described|p5 Fig.3, p24-25, p31, p33, p45|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin. A subunit of this Formation constrains the age of the South Nicholson Group on Mount Drummond.||Wild Cow Subgroup|Tobacco Member|Overlies Bowgan Sandstone and No Mans Sandstone Member and underlies Mittiebah Sandstone.|Includes siltstone.|15-MAR-21
37729|Crow Formation|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the west of the South Nicholson Basin.||Wildcow Subgroup||Overlies Bowgan Sandstone and underlies Mittebah Sandstone.|Includes siltstone.|
37729|Crow Formation|72919|5|Briefly described|p4-5, p70-71, p85-89, p94, p97-98|Mesoproterozoic|Mesoproterozoic|A maximum depositional age of ca. 1483 Ma was reported by Kositcin and Carson (2019). Carson et al. (2020) proposed an expanded version of the Benmara Group that includes strata of [or equivalent to?] this unit in the hanging wall of the Benmara Fault based on comparison of detrital zircon spectra with that of late Paleoproterozoic successions.||Wild Cow Subgroup, South Nicholson Group|Tobacco Member|Underlain by Bowgan and Playford sandstones, including No Mans Sandstone Member. Conformably overlain by Mittiebah and Constance sandstones, including Hedleys Sandstone Member (Accident Subgroup).||
37729|Crow Formation|73042|6|Mentioned|p4|||The Crow Formation 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 Crow* Formation, which might indicate tentative or uncertain use of this nomenclature. South Nicholson Basin region, Roper Superbasin (and Isa Superbasin for Crow* Formation).|<ca 1483 Ma (see comment and Fig.1.2)|Wildcow Subgroup, South Nicholson Group and Benmara Group (see comments)|Tobacco Member|South Nicholson Group: underlain by Playford Sandstone, overlain by Mittiebah Sandstone. Benmara Group: underlain by Bowgan Sandstone, overlain by Mittiebah* Formation.||
37729|Crow Formation|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|||Benmara Group||||
37729|Crow Formation|73083|6|Mentioned|p35|||||Wild Cow Subgroup, South Nicholson Group|||Includes siliciclastics.|
26505|Crown Point Formation|13516|6|Mentioned|p147, fig 5|Early Permian|Early Permian|From Pedirka Basin||||||
26505|Crown Point Formation|22566|5|Briefly described|p79|Early Permian|Late Carboniferous|Of the Finke Group.||||||08-AUG-06
26505|Crown Point Formation|22804|6|Mentioned|p455||Early Permian|||||||
26505|Crown Point Formation|22824|6|Mentioned|p537||Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22826|4|Described|p576|Early Permian|Early Permian|Geological Province - Pedirka Basin.||||||
26505|Crown Point Formation|22883|6|Mentioned|P29|Early Permian|Late Carboniferous|Overlying unit is Purni Formation.||||||08-AUG-06
26505|Crown Point Formation|23982|6|Mentioned|p96 Appendix 13|||Geological Province: Great Artesian Basin.||||||
26505|Crown Point Formation|24204|5|Briefly described|p262, 263 Fig.4, p266 Fig.7|Early Permian|Late Carboniferous|Geological Province: Pedirka Basin.||||||
26505|Crown Point Formation|29442|6|Mentioned|p103|||||||||
26505|Crown Point Formation|29591|6|Mentioned|p82|||||||||
26505|Crown Point Formation|30340|6|Mentioned|p2519|||Lithology||||||
26505|Crown Point Formation|30341|4|Described|p120|||Permian age. Pedirka Basin.||||||
26505|Crown Point Formation|30514|6|Mentioned|p100|||Permian age||||||
26505|Crown Point Formation|30544|5|Briefly described|p52|||See also Fig.6 p53.||||||08-AUG-06
26505|Crown Point Formation|30825|6|Mentioned|p37|||||||||
26505|Crown Point Formation|31567|6|Mentioned|p274|||Latest Carb.- early Permian. Unconformable on Finke Gp.||||||
26505|Crown Point Formation|32640|6|Mentioned|p241|||||||||
26505|Crown Point Formation|33103|6|Mentioned|p25|||||||||
26505|Crown Point Formation|33523|6|Mentioned|p23|||||||||
26505|Crown Point Formation|33824|6|Mentioned|p7|||||||||
26505|Crown Point Formation|33832|6|Mentioned|p7|||Stratigraphy||||||
26505|Crown Point Formation|33844|4|Described|p36|||||||||
26505|Crown Point Formation|33931|6|Mentioned|p9|||L.Perm.||||||
26505|Crown Point Formation|33971|3|Fully described|p32|||||||||
26505|Crown Point Formation|33976|6|Mentioned|p5|||||||||
26505|Crown Point Formation|34111|6|Mentioned|p16|||Permian||||||
26505|Crown Point Formation|34580|4|Described|Table 1|||Permian||||||
26505|Crown Point Formation|35845|6|Mentioned|Fig.25|||||||||
26505|Crown Point Formation|36473|6|Mentioned|Map legend|Permian|Permian|||||||
26505|Crown Point Formation|36733|6|Mentioned|p14|||||||||
26505|Crown Point Formation|36751|6|Mentioned|p489|||||||||
26505|Crown Point Formation|36899|6|Mentioned|p1089|||||||||
26505|Crown Point Formation|36922|6|Mentioned|p188|||||||||
26505|Crown Point Formation|37776|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|37855|6|Mentioned|p4|||See also Fig.2.||||||
26505|Crown Point Formation|37917|4|Described|p470|||||||||
26505|Crown Point Formation|39265|6|Mentioned|Fig. 3|||||||||
26505|Crown Point Formation|40637|6|Mentioned|Fig.2|||||||||
26505|Crown Point Formation|40910|5|Briefly described|p15|||||||||
26505|Crown Point Formation|40911|6|Mentioned|Map legend|Permian|Carboniferous|||||||
26505|Crown Point Formation|40925|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous to Permian||||||
26505|Crown Point Formation|40926|3|Fully described|p12|||Mention Table 1||||||
26505|Crown Point Formation|41063|6|Mentioned|p46|||||||||
26505|Crown Point Formation|41183|6|Mentioned|Fig.3 p308|||||||||
26505|Crown Point Formation|41270|6|Mentioned|p279|||||||||
26505|Crown Point Formation|41491|6|Mentioned|Fig.8|||||||||
26505|Crown Point Formation|41689|6|Mentioned|Table 1|||||||||
26505|Crown Point Formation|42463|6|Mentioned|Fig.4 P171|||||||||
26505|Crown Point Formation|42504|5|Briefly described|p81|||||||||
26505|Crown Point Formation|42547|4|Described|p82|||||||||
26505|Crown Point Formation|42746|5|Briefly described|p3, Fig.2 p4|||Pedirka Basin||||||
26505|Crown Point Formation|42940|5|Briefly described|Plate 2|Permian|Permian|Sandstone, diamictite, shale, siltstone. Age: 290-250Ma.  Geological province: Amadeus Basin.||||||23-JAN-08
26505|Crown Point Formation|43052|5|Briefly described|Table 2.1|||||||||
26505|Crown Point Formation|44133|5|Briefly described|p42, 65 Fig 8.4, 89|Permian|Carboniferous|Geological Province: Pedirka Basin. ||||||
26505|Crown Point Formation|44323|14|Not recorded|map legend||Permian|SG/53-6.||||||
26505|Crown Point Formation|44335|4|Described|p.11||Permian|Table 2. p.10||||||
26505|Crown Point Formation|44336|14|Not recorded|map legend||Permian|SG/53-3.||||||
26505|Crown Point Formation|44342|14|Not recorded|Not recorded|||||||||
26505|Crown Point Formation|44393|4|Described|p.6,8,Tb.1,Fig.1||Early Permian|L. Permian.||||||
26505|Crown Point Formation|44394|14|Not recorded|map legend||Early Permian|Lower Permian.||||||
26505|Crown Point Formation|45041|4|Described|p112|||Permian||||||
26505|Crown Point Formation|45104|6|Mentioned|p30|||||||||
26505|Crown Point Formation|45168|6|Mentioned|p10|||||||||
26505|Crown Point Formation|46849|6|Mentioned|p199|||||||||
26505|Crown Point Formation|48865|2|Defined|p.36||Permian|Fig.4. On many pages. p.21,28,33,34,37,39,41,48,51. Fig.13, Pl.6,11. (G53-6).||||||
26505|Crown Point Formation|48880|14|Not recorded|p.20||Permian|(map).||||||
26505|Crown Point Formation|48890|4|Described|p.53||Permian|||||||
26505|Crown Point Formation|48963|6|Mentioned|Plate 5|||||||||
26505|Crown Point Formation|62376|5|Briefly described|p84|Late Carboniferous|Late Carboniferous|Geological Province: Pedirka Basin.||||||09-FEB-10
26505|Crown Point Formation|64778|6|Mentioned|p13, 15-21, 23|Carboniferous|Carboniferous|Pedirka Basin. Thermal history summarised. Max. palaeotemperature analysis summary. Potential hydrocarbon source rock.|314-285 Ma.|||||
26505|Crown Point Formation|65238|5|Briefly described|p3, p5 Fig. 6, p7 Fig. 8|Late Carboniferous|Late Carboniferous|Geological province: Pedirka Basin. Periglacial deposits - dominantly a glacial succession, comprising diamictite, glacial-fluvial outwash, ripple laminated sandstone and siltstone, together with shale and varved successions. See also p8.||||||09-APR-13
26505|Crown Point Formation|65309|6|Mentioned|p21.|||Pedirka Basin. Useful as an aquifer.||||||
26505|Crown Point Formation|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 193 m.||||Overlies Idracowra Sandstone. Is overlain by De Souza Sandstone.||
26505|Crown Point Formation|65489|5|Briefly described|p55, p57-58, p60-61, p63-64, p137-139|Permian|Permian|See also p143, p151. Basal unit in the Pedirka Basin. Perhaps over 600m thick. Has reservoir potential.||||Is overlain by Purni Formation. Equivalent to Merrimelia Formation.|Fluvioglacial and glaciolacustrine sediments.|
26505|Crown Point Formation|67856|6|Mentioned|p348|||Of central Amadeus Basin.||||Correlated with Buck Formation and Ligertwood beds.||
26505|Crown Point Formation|69454|5|Briefly described|p38:1-6,7 Fig.38.6; 38:12-13,14 Fig.38.9|Asselian|Asselian|Wells et al. (1966). The only outcropping strata of the Pedirka Basin. Early Permian. 504m thick in Mount Hammersley-1. Crops out as mesas, buttes and low mounds. Glaciofluvial, glaciolacustrine and periglacial deposits. Sandstones have fair to good reservoir potential.||||Is overlain conformably by, and interfingers with, Tirrawarra Sandstone. Also overlain by Purni Formation. Correlated with Merrimelia, Boorthanna and Kuriyippi Formations.|Conglomerate, diamictite, cross-bedded pebbly and coarse sandstone, ripple-laminated fine sandstone and siltstone, thick claystone-dominated intervals with varvite bands.|12-JUL-16
26505|Crown Point Formation|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
26505|Crown Point Formation|69673|4|Described|p149, p150, p151, p160, p161 fig 131|Permian|Permian|Greater than 504m thick.||||Conformably overlain by Purni Formation,|Conglomerate, diamictite, cross bedded pebbly and coarse sandstone, ripple laminated fine sandstone and siltstone.|
26505|Crown Point Formation|69946|4|Described|p5-6, p36, p44-48, p51|Asselian|Late Carboniferous|Pedirka Basin. Defined by Wells et al. (1966) to replace the informal Crown Point Series. Type section is at One Tree Point, near Crown Point, NT. Diamictite clasts are derived from early Paleozoic sediments and Musgrave Province. Up to 347m thick.||||Is overlain disconformably by Purni Formation or Stuart Range Formation equivalent. Correlates with Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine- to coarse-grained sandstone with interbeds of medium to dark grey siltstone and diamictite units containing faceted and striated exotic pebbles and cobbles.|
26505|Crown Point Formation|69948|6|Mentioned|Fig.4.18|||Pedirka Basin.||||Is overlain conformably by Stuart Range Formation and (locally) unconformably by Purni Formation.||
26505|Crown Point Formation|71342|4|Described|Ch4 p25, Ch5 p5-p6|Early Permian|Late Carboniferous|Pedirka Basin. Formally defined by Wells et al (1966) to replace the informal Crown Point Series. A type section outcropping at One Tree Point on the FINKE 1:250000 map area in the NT is mentioned. Lithology discussed in further detail. This unit has a maximum thickness of 347m at Mount Hammersley 1. Sedimentology is briefly described. Deposited in periglacial, interglacial, fluvioglacial or glaciolacustrine environments. See also Ch5 p30, Ch5 p36, Ch5 p44-p48, Ch5 p51, Ch8 p28, Ch9 p9, Ch9 p11, Ch9 p16, Ch9 p18, Ch9 p20-p21, Ch11 p6-p7, Ch11 p18, Ch12 p7.||||Unconformably overlies the Finke Group. Disconformably overlain by the Purni Formation. Equivalent to the Boorthanna and Merrimelia Formations.|Pale grey to buff, very fine to coarse-grained sandstone with interbeds of medium to dark grey siltstone.|
26505|Crown Point Formation|72476|6|Mentioned|p26, p36 Fig.9|Permian|Carboniferous|Perdika Basin. Time-temperature thermal history diagram.||||||
26505|Crown Point Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Pedirka Basin. See DIP034_Petroleumdata.xlsx.||||||
76183|Culaly Amphibolite|67779|2|Defined|p10 Table 1, p14, p51, p60, pp117-118.|Paleoproterozoic|Neoarchean|New name, after Culaly Plain. Nimbuwah Domain, Pine Creek Orogen. Formerly part of Zamu Complex and Zamu Dolerite (in Ferguson and Needham, 1978). Is found only within the Kukalak Gneiss, and adjacent to to Kudjumarndi Quartzite. Reference area is isolated exposure in Tin Camp Creek; locally forms massive platform exposures. Geochemistry is described in detail.|Poorly constrained. May be Archean||||Amphibolite: moderately foliated, locally garnetiferous: garnets have asymmetric tails, are commonly poikilitic with encircling coronas of recrystallised feldspar.|14-SEP-12
76183|Culaly Amphibolite|70853|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Amphibolite: moderately foliated, locally garnetiferous.|
30778|Cullen Supersuite|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Predominantly I-type granites. Geological Province: Pine Creek Orogen.||||||21-SEP-09
30778|Cullen Supersuite|24197|4|Described|p23, p103|Paleoproterozoic|Paleoproterozoic|Type example of Cullen Association. Includes 26 named granites. I-type, granodioritic, consisting of 3 major pluton types: leucogranites, uniform granodiorite to granite suites and concentrically zoned plutons. Geol.prov: Pine Creek Inlier.||||||07-FEB-11
30778|Cullen Supersuite|50425|6|Mentioned|p3.1|||Geological Province: Pine Creek Inlier.||||||
30778|Cullen Supersuite|50586|5|Briefly described|p1.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Age: 1825Ma.||||||07-NOV-08
30778|Cullen Supersuite|50589|6|Mentioned|p2.2|||||||||
30778|Cullen Supersuite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Age range: 1830-1800Ma.||||||
30778|Cullen Supersuite|63866|4|Described|p106, p109-p112, p117, p124|Statherian|Statherian|Litchfield Province, Pine Creek Orogen. SHRIMP, Rb-Sr and ID-TIMS dates are said to be found in Stuart-Smith et al., 1993 but not provided in the text. Also includes the  Burnside, Shoobridge and the Saunders Creek Granites.|ca 1784-1763 Ma (Rb-Sr whole rock)||Includes the Margaret Granite, McMinns Bluff Granite, Mount Bundey Granite, Mount Goyder Syenite, Umbrawarra Granite, Fingerpost Granite and the Allamber Springs Granite.||I-type granitic plutons.|
30778|Cullen Supersuite|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Age ~1800-1860Ma. Includes at least 27 granites & suites.||||||
30778|Cullen Supersuite|64817|6|Mentioned|p350 |||Barramundi igneous event. Extensive and uniform suite of I- and lesser A-type granites and comagmatic volcanics (Etheridge et al 1987, Wyborn 1988).||||||14-JUN-18
30778|Cullen Supersuite|65232|5|Briefly described|p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Predominantly I-type granites.~1830-1829Ma?||||||09-FEB-10
30778|Cullen Supersuite|65359|6|Mentioned|p23, p26-28 Figs.26-28.|||Major element content and trends are similar to those of Mount Winnecke Formation and Winnecke Granophyre.||||||
30778|Cullen Supersuite|65455|6|Mentioned|p6 Fig. 3|Paleoproterozoic|Paleoproterozoic|In the western half of the Pine Creek region, a known U province. Most high-U samples occur in this Supersuite.||||||09-MAY-12
30778|Cullen Supersuite|67232|5|Briefly described|p2. |Paleoproterozoic|Paleoproterozoic|Post-tectonic granitoids.|1830 - 1800 Ma.|||Intrudes Woodcutters and Cosmo Supergroups.||
30778|Cullen Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1835 +/- 6 Ma.|||||
30778|Cullen Supersuite|67355|5|Briefly described|p5, p15||Paleoproterozoic|Resetting of Rb-Sr system occurred at 1780-1760 Ma due to a regional low-grade metamorphic event, the Shoobridge Event.||||||25-JAN-17
30778|Cullen Supersuite|67479|6|Mentioned|p6 Fig.2|||||||||
30778|Cullen Supersuite|67564|4|Described|p iv, p7 Table 2, p9 Fig.4, pp32-36.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Predominantly fractionated (felsic), I-type; coeval with David Suite and Edith River Group to the east, and Allia Creek Suite to the west. 23 named plutons, many coalesced at <3 km depth.|c.1835 - 1800 Ma.||Includes Minglo, McCarthys, Allamber Springs, Driffield, Mount Davis, Wolfram Hill and Wandie Granites; Frances Creek Leucogranite.||Predominantly I-type granitoids: early mesocratic granitoids, transition granites, and late leucogranites.|
30778|Cullen Supersuite|67779|5|Briefly described|p4, p6 Fig.5, p30, p106 Fig.129, p107.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. I-type granites. Their ages suggest that this unit, thePlum Tree Volcanics of the Edith River Group and the Nabarlek Granite formed as part of the same thermal event.|1835-1820 Ma (Worden et al. 2008a).|||||21-MAY-18
30778|Cullen Supersuite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Central Pine Creek Orogen.||||Intrudes Edith River and El Sherana Groups.||12-JUL-16
30778|Cullen Supersuite|69418|6|Mentioned|p3:20|||Pine Creek Orogen. Tin occurs in mineralised quartz veins in the contact aureoles of granites of this Supersuite; eg Mount Wells mine.||||||12-JUL-16
30778|Cullen Supersuite|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
30778|Cullen Supersuite|69420|4|Described|p5:4, 14, 17-23, 33-34, 38, 42, 62-63|Paleoproterozoic|Paleoproterozoic|See also 66, 85, 100, 109, 111, 115. Central Domain, Pine Creek Orogen. Emplacement was synchronous with a major extensional event related to deposition of El Sherana, Edith and lower Katherine River Groups. Subdivided into three groups: leucogranite-dominated plutons; granite-dominated plutons; and concentrically-zoned transitional granites and leucogranite-dominated plutons. Limited geochemistry. Clear evidence of late-stage release of magmatic fluids. Age determinations briefly discussed; see also constituent units. Deformed by the c.1780 Ma Shoobridge Event.|c.1835-1800 Ma.||Saunders, Burnside, Tennysons, Shoebridge, Allamber Springs, Fingerpost, McMinns, Margaret, Mount Bundey Suites; Bludells Dolerite.|Cuts across Bludells Dolerite.|An I-type (granodiorite) group that has undergone significant fractionation; large contact aureoles; spatially associated with gold deposits; predominantly calc-alkaline.|12-JUL-16
30778|Cullen Supersuite|69421|6|Mentioned|p6:6|||Pine Creek Orogen.||||Correlated with Giddy Suite (Arnhem Province).||14-JUN-18
30778|Cullen Supersuite|69577|6|Mentioned|p113-114, 116|Paleoproterozoic|Paleoproterozoic|Central Pine Creek Orogen.|1835-1818 Ma.|||||
30778|Cullen Supersuite|69673|6|Mentioned|p3|||||||||
30778|Cullen Supersuite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Undivided granite, undivided hornfels, and 19 individual units are all mapped separately.|1835-1800 Ma.||Includes Allamber Springs, Burnside, Fingerpost, McMinns Bluff, Saunders, Shoobridge, Tennysons Suites; Margaret, McKinlay, Prices Springs Granites; Bludells Dolerite.|||01-MAR-18
30778|Cullen Supersuite|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin. Mapped with Jim Jim Suite as a single unit.||||||05-MAR-20
29771|Cumming Leucogabbro|43225|5|Briefly described|Map Legend||Mesoproterozoic|Of Arunta Block.||||||08-AUG-06
29771|Cumming Leucogabbro|43503|2|Defined|8,25,79|||||||||
29771|Cumming Leucogabbro|69428|5|Briefly described|p13:05|||Warren and Shaw (1995). South of the Chewings Range. Undated. A 6 x 1 km body.||||Intrudes the Glen Helen Metamorphics.|Weakly deformed tremolite- and actinolite-bearing rocks, containing rare chromite layers and traces of scheelite.|12-JUL-16
31345|Currinya Clay|61385|5|Briefly described|Map legend|Cenozoic|Cenozoic|Clay, silt, micrite; dark-coloured; shelly; pyritic; lacustrine (littoral carbonate).  Geological Province: overlies Amadeus Basin. Age: Tertiary||||||16-DEC-11
31345|Currinya Clay|67453|5|Briefly described|map legend|Cenozoic|Cenozoic|Of Mount Wedge Basin. Younger than Mount Wedge Clay. Age shown as Tertiary. Clay, silt, micrite; dark coloured; shelly; lacustrine (littoral carbonate). Known only from drill holes / water bores||||||16-DEC-11
31345|Currinya Clay|69458|5|Briefly described|p42:13|||Woodgate et al. (2012). Mount Wedge Basin.||||Overlies Mount Wedge Clay.|A coarse-grained, strongly oxidised alluvial unit.|12-JUL-16
26509|Cyclops Member|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Pertatataka Formation.  Platy, even-bedded sandstone.  Geological Province: Amadeus Basin.||||||
26509|Cyclops Member|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
26509|Cyclops Member|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Of Pertatataka Formation.  Age - Ediacarian in text.||||||08-AUG-06
26509|Cyclops Member|22649|4|Described|p 149|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.||||||08-AUG-06
26509|Cyclops Member|22762|6|Mentioned|p362|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.||||||08-AUG-06
26509|Cyclops Member|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of Pertatataka Formation. Correlate of Tent Hill Formation and Brachina Formation.||||||08-AUG-06
26509|Cyclops Member|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
26509|Cyclops Member|32720|6|Mentioned|Table 1|||||||||
26509|Cyclops Member|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
26509|Cyclops Member|34579|6|Mentioned|Table 1|||||||||
26509|Cyclops Member|35102|6|Mentioned|Fig.11|||||||||
26509|Cyclops Member|35798|6|Mentioned|p307|||||||||
26509|Cyclops Member|36898|6|Mentioned|p198|||||||||
26509|Cyclops Member|37462|6|Mentioned|Fig.4.16|||||||||
26509|Cyclops Member|37928|6|Mentioned|Fig.4|||||||||
26509|Cyclops Member|38157|6|Mentioned|Table VI|||See also p281.||||||08-AUG-06
26509|Cyclops Member|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26509|Cyclops Member|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26509|Cyclops Member|39210|6|Mentioned|p37|||||||||
26509|Cyclops Member|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26509|Cyclops Member|39931|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26509|Cyclops Member|40740|6|Mentioned|p11|||||||||
26509|Cyclops Member|40906|6|Mentioned|Fig.9|||||||||
26509|Cyclops Member|41005|6|Mentioned|p424|||||||||
26509|Cyclops Member|41190|6|Mentioned|Fig.4|||||||||
26509|Cyclops Member|41270|6|Mentioned|Table 1|||||||||
26509|Cyclops Member|41429|6|Mentioned|p246|||||||||
26509|Cyclops Member|41717|6|Mentioned|Fig.2|||||||||
26509|Cyclops Member|41801|6|Mentioned|p218|||See also Fig.4||||||
26509|Cyclops Member|42082|6|Mentioned|Fig.3 P323|||||||||
26509|Cyclops Member|42504|5|Briefly described|Table 4 P73|||||||||
26509|Cyclops Member|42643|6|Mentioned|Fig.4 P19|||||||||
26509|Cyclops Member|42886|5|Briefly described|p223|||Of Pertatataka Formation.||||||08-AUG-06
26509|Cyclops Member|42940|5|Briefly described|Plate 9|||||||||
26509|Cyclops Member|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
26509|Cyclops Member|45041|4|Described|p36|||Proterozoic||||||
26509|Cyclops Member|46730|5|Briefly described|p7|||Overlying Unit: Julie Formation. Geological Province: Amadeus Basin||||||
26509|Cyclops Member|46865|6|Mentioned|p44|||||||||
26509|Cyclops Member|46903|6|Mentioned|p54|||Correlative of Grant Bluff Formation||||||
26509|Cyclops Member|48890|2|Defined|p.25||Neoproterozoic|See also Tb1,Tb2, Fig.4, p.26, Fig.15,Pl.10. pt. Pertatataka Fm. U.Proterozoic. Defn. on Tech.File F/53-15.||||||
26509|Cyclops Member|48963|6|Mentioned|Fig.2|||||||||
26509|Cyclops Member|49796|5|Briefly described|Sect C BDF 10 & 12|||Of Pertatataka Formation.||||||08-AUG-06
26509|Cyclops Member|50246|5|Briefly described|p20 Fig. 2|Proterozoic|Proterozoic|Of the Pertatataka Formation. Sandstone, fine-grained, undulose to flat and laminated and fissile.||||||07-FEB-11
26509|Cyclops Member|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Platy, even-bedded sandstone.||||||
26509|Cyclops Member|61732|4|Described|p91 Fig.34, p95-96|Ediacaran|Ediacaran|Sandstone unit of the Pertatakata Formation - laminated quartz siltstone and fine-grained sandstone; platy, rhythmically bedded. . Geological Province: Amadeus Basin.||||||07-FEB-11
26509|Cyclops Member|62595|6|Mentioned|p28 Fig.4.|Late Neoproterozoic|Late Neoproterozoic|Amadeus Basin. Relative probability plots of detrital zircon data are shown.||Unit in Pertatataka Formation.||||
26509|Cyclops Member|63562|4|Described|p344-347, p351, p352 Fig.10.|Ediacaran||Amadeus Basin. Zircons peak at ~2.5 Ga and between 1.9-1.7 Ga; youngest was 807 Ma. Thus Arunta Inlier, not Musgrave Inlier, was probable source for sediment.|~575 Ma.|Pertatataka Formation.||Correlated with Grant Bluff Formation.|Thinly-bedded, fine-grained, shallow marine, quartz sandstone.|06-DEC-17
26509|Cyclops Member|64809|5|Briefly described|p10, p15 Fig.15|Proterozoic|Proterozoic|||Of the Pertatataka Formation|||Platey evenly bedded sandstone.|
26509|Cyclops Member|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
26509|Cyclops Member|69438|5|Briefly described|p23:8, 19-20|Neoproterozoic|Neoproterozoic|Wells et al. (1967). NE Amadeus Basin. In places forms low ridges. Provenance probably from the Arunta Region. Maximum depositional SHRIMP U-Pb detrital zircon age of c.807 Ma.|~575 Ma inferred age (Maidment, 2005).|Pertatataka Formation.|||Fine laminated flaggy sandstone and rhythmically bedded sandstone.|12-JUL-16
26509|Cyclops Member|69673|5|Briefly described|p74|||||Pertatataka Formation|||Fine laminated, flaggy sandstone and rhythmicallly thinly bedded sandstone.|
26509|Cyclops Member|69937|4|Described|v Fig.1, p3 Tb.1, p26, p29-31, p53-54|Neoproterozoic|Neoproterozoic|Wells et al. (1967). Amadeus Basin. Near the top of the Formation. Characterised by large numbers of small groupings of zircon ages. Likely zircon provenance discussed.|650 +/- 13 Ma (maximum depositional age).|Pertatataka Formation.|||Flaggy sandstone and rhythmically thinly-bedded sandstone.|
26509|Cyclops Member|70018|6|Mentioned|p240|||Amadeus Basin. ||||||
26509|Cyclops Member|70416|5|Briefly described|p65 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||Pertatataka Formation.||||
26509|Cyclops Member|71001|6|Mentioned|p18 Fig.2|Ediacaran|Ediacaran|Amadeus Basin. Marine deposits.||Pertatataka Formation.||||
26509|Cyclops Member|71344|6|Mentioned|p1093 Fig 1|||||Of Pertatataka Formation.||||
26509|Cyclops Member|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|650+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Fine- to medium-grained quartz sandstone, rhythmically bedded.|
26509|Cyclops Member|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||Unit of Pertatataka Formation.||||
26509|Cyclops Member|71842|5|Briefly described|p2-3|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).||Unit of Pertatataka Formation.||||
26509|Cyclops Member|72369|5|Briefly described|p11,14|||Of Amadeus Basin. Restricted to the NE part of Amadeus Basin. Kositcin et al (2015) reported interpreted maximum depositional age of 650+\-13 Ma.||Unit of Pertatataka Formation.||Upper unit of Pertatataka Formation.||
26509|Cyclops Member|72375|4|Described|p1-2,27,29|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Best exposed along the basin margin in ALICE SPRINGS 1:250 000 map sheet. Upper of two distinctive sandstone members of the Pertatataka Formation identified in NE Amadeus Basin; occurs near the top of the Pertatataka Formation, overlying thick shales of the central part of Pertatataka Formation. Previously considered to be correlable with Waldo Pedlar Member (Preiss et al., 1978; Field 1991), but Freeman (1991) disagreed on the basis of lithological differences. SHRIMP U-Pb zircon analysis by Kositin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 650+\-13 Ma, significantly younger than the c. 807 Ma max depositional age provided by Maidment et al., 2007, and that of the Pertatataka Formation (c. 575 Ma; inferred age; Maidment 2005). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS AS13CJE027 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p30 for Hf isotopic results and interpretations). Sample location and description is provided.||Unit of Pertatataka Formation.|||Flaggy sandstone and rythmically thinly-bedded, fine- to medium-grained quartz sandstone.|04-DEC-19
26509|Cyclops Member|72516|6|Mentioned|p89|Ediacaran|Ediacaran|Amadeus Basin.||Pertatataka Formation||Equivalent to the Grant Bluff Formation.||02-JUN-21
26509|Cyclops Member|73085|6|Mentioned|p1|Ediacaran|Ediacaran|||Pertatataka Formation||||
26509|Cyclops Member|73086|1|Redefined|[See comments].|Ediacaran|Ediacaran|[Redefined herein. See also definition card, ASUD]. Re-definition of unit. Post-glacial transgressive unit. Characterised by flaggy to fissile, thinly bedded and laminated micaceous sandstone with rhythmic and even bedding. Amadeus Basin. Type section: Ross River Highway. [Poor age constraint]. Inferred depositional age of 575 Ma (Maidment, 2005).  A detrital zircon maximum depositional age of 650 +/- 15 Ma (SHRIMP U-Pb) is older than the inferred true depositional age. No known fossils. Rhythmic bedding and hummocky cross-stratification suggests deposition in an offshore transition zone. p: 5-6, 53, 79, 99, 121-123, 130-131, 143, 169, 171-172, App 2.|ca 570 Ma|Pertatataka Formation||Probably equivalent to ABC Range Quartzite. Partly correlates to upper Inindia beds.|Platy fine-grained micaceous quartz sandstone with very thin, even and rhythmic beds and laminations.|
26509|Cyclops Member|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||Pertatataka Formation||||
26509|Cyclops Member|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Pertatataka Formation||||
42087|Davenport Dacite|23809|5|Briefly described|p32, p28 Tb. 4|Paleoproterozoic|Paleoproterozoic|Age: 1862+/-5Ma (Pb-Pb). Intruded by Hill of Leaders Granite. Previously mapped as part of Warramunga Group on BONNEY WELL 1:250 000 sheet.||||||14-APR-15
42087|Davenport Dacite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1862+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Flow-banded dacite.|
35396|Dead Bullock Formation|23809|5|Briefly described|p3-4|||Siltstone, graphitic shale, iron-rich beds and silicified nodular chert.  Overlain conformably by Killi Killi Formation.  Max. thickness: 4km.||||||
35396|Dead Bullock Formation|50152|5|Briefly described|p71, p72 Fig. 3|||Of Tanami Group. Conformably underlian by Killi Killi Formation. Comprises graphitic siltstones, mudstones, silicatefacies banded iron formations, cherts and dolerite sills.||||||
35396|Dead Bullock Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Siltstone: white, dark grey to black, thin bedded mudstone, siltstone and black carbonaceous shale, includes minor banded iron formation, thin pale calcareous beds and thin bedded chert; chert nodules common.||||||07-NOV-08
35396|Dead Bullock Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group||||||07-NOV-08
35396|Dead Bullock Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Siltstone; siltstone and black carbonaceous shale, includes minor banded iron formation, thin plae calcareous beds and thin bedded chert; chert nodules common.||||||07-NOV-08
35396|Dead Bullock Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Underlies: Killi Killi Formation. Overlies: MacFarlane Peak Group. Siltstone: thin bedded mudstone, siltstone and carbonaceous shale, includes banded iron formation, thin calcareous beds, thin bedded chert; chert nodules, dolerite sills.||||||07-NOV-08
35396|Dead Bullock Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group. Siltstone, numerous dolerite sills.||||||
35396|Dead Bullock Formation|61861|3|Fully described|p10-12, p3, 4, p9, Figs.11-15,  Map 1|Orosirian|Orosirian|New name. Includes former Mount Charles Beds. Hosts significant gold mineralisation. Forms small isolated silicified outcrops. Intruded by numerous granite bodies, dolerite dykes and sills.Correlated with Halls Creek and Pine Creek Orogen units.|1880-1850 Ma on basis of correlations.|Unit in Tanami Group.||Overlies MacFarlane Peak Group (or possibly laterally equivalent). Is overlain by Killi Killi Formation, transitionally in places. May be lateral equivalent to Twigg Formation.|A succession dominated by fine-grained sedimentary rocks: buff, grey or purple siltstone with interbedded black carbonaceous siltstone or shale, calc-silicates, thin bedded chert and banded iron formation; minor thin-bedded quartz rich sandstone.|
35396|Dead Bullock Formation|62377|4|Described|p1, 11-15|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Sandstone, siltstone, schist, iron formation and mafic rocks. Underlies Killi Killi Formation conformably. Unconformably overlain by Pargee Sandstone, Muriel Range Sandstone, Lucas Formation and Pedestal beds. Max age: 1865 +/- 12Ma (youngest detrital zircon grain).||||||10-DEC-12
35396|Dead Bullock Formation|62580|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group.||||||07-FEB-11
35396|Dead Bullock Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami Inlier.||||||07-NOV-08
35396|Dead Bullock Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region-Aileron Province. Grey siltstone, silty shale, fine grained sandstone, laminated siltstone, massive quartzite, black shale, chert, amphibolite.||||||07-NOV-08
35396|Dead Bullock Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region - Aileron Province. Grey siltstone, intercalated chert, interbedded silty shale, fine grained sandstone, laminated siltstone, massive quartzite, black shale.||||||07-NOV-08
35396|Dead Bullock Formation|63261|3|Fully described|p9 Fig. 5, p10-11|Paleoproterozoic|Paleoproterozoic|Of Tanami Gp. Contains lower Ferdies Member + overlying Callie Member.Conformably overlain by Killi Killi Fm. Fining-upward, deep water succession dominated by siltstone, carbonaceous siltstone, Fe-rich siltstone+mafic sills. Geol.prov: Tanami Region.||||||07-FEB-11
35396|Dead Bullock Formation|63866|5|Briefly described|p92|||Tanami Region.|c. 1840 Ma|||Overlain by the Killi Killi Formation.|Tuff.|
35396|Dead Bullock Formation|64662|5|Briefly described|p28, 27|Orosirian|Rhyacian|Basal unit of Tanami Group. Age of deposition (inferred): ~2.11-1.84Ga. Underlies Killi Killi Fm. Comprises lower sst/upper carbonaceous siltst. Detrital zircons derived from Archean basement, not contemporaneous orogenic products.||||||07-FEB-11
35396|Dead Bullock Formation|64675|5|Briefly described|p9, p10, Maps1, 6, p20, Fig.30-32|Paleoproterozoic|Paleoproterozoic|||Of the Tanami Group.||Underlain by the MacFarlane Peak Group. Overlain by the Killi Killi Formation.|Comprises a siltstone unit with minor carbonaceous shale, calc-silicate and banded iron formation.|19-MAR-14
35396|Dead Bullock Formation|64725|5|Briefly described|p62.|||Host rock for most of the gold in the Granites-Tanami Orogen.|c.1847-1840 Ma.|Lower unit in Tanami Group.|||Carbonaceous siltstone and iron-formation; extensively hydrothermally altered.|
35396|Dead Bullock Formation|64733|3|Fully described|p170 Fig.2, p171-172, p172 Fig.4, p182|Orosirian|Orosirian|1km thick.  Suggested back-arc basin or volcanic arc tectonic setting at time of deposition. Age from tuffaceous sandstone (Cross and Crispe, 2007).|SHRIMP U-Pb zircon age of 1838 +/- 6 Ma.|Of Tanami Group.|Lower part of the Formation is called the Ferdies Member. Upper part  - Callie Member.|Overlain by Killi Killi Formation; overlies Stubbins Formation. Intruded by Inspiration Peak Granite.|Upward-fining sequence of sandstone, turbiditic sandstone, carbonaceous siltstone, siltstone, shale, chert and rare volcanics.|20-APR-12
35396|Dead Bullock Formation|64734|4|Described|p187, p191, p199, p201-2, p186 Fig.1|Orosirian||Basal Tanami Group; includes Ferdies Member, Callie Member; fine sst, siltst (some carbonaceous) grade into chert-bearing BIF and clayst; base unseen; deposited ~1838Ma; large gold deposits; conformable boundary with Killi Killi Formation above suggested||||||10-FEB-11
35396|Dead Bullock Formation|64735|6|Mentioned|p217||||||Includes Callie Member.|||30-APR-12
35396|Dead Bullock Formation|64737|5|Briefly described|p233||Orosirian|Age from a volcaniclastic unit.|1838+/-6 Ma (Cross and Crispe, 2007).|||Overlain by Killi Killi Formation.||01-MAY-12
35396|Dead Bullock Formation|64956|6|Mentioned|p11|||||||||07-FEB-11
35396|Dead Bullock Formation|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor BIF, thin calcareous beds and thin bedded chert; chert nodules common; contains many metadolerite sills ||||||
35396|Dead Bullock Formation|65326|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65327|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65328|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||
35396|Dead Bullock Formation|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||02-MAR-10
35396|Dead Bullock Formation|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; underlies Killi Killi Formation. White, dark grey-black, thin bedded mudst, siltst, black carbonaceous shales; minor banded iron formation, thin calcareous beds, thin bedded chert; chert nodules common; contains many metadolerite sills||||||02-MAR-10
35396|Dead Bullock Formation|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; Siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; Siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||02-FEB-10
35396|Dead Bullock Formation|65354|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group; siltstone with numerous moderate-highly magnetic metadolerite sills; moderate-intensely magnetic with a high gravity response; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65355|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Tanami Group||||||
35396|Dead Bullock Formation|65356|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Tanami Group; underlies Killi Killi Formation||||||
35396|Dead Bullock Formation|65358|4|Described|p6|Orosirian|Orosirian|In Tanami Region. Basal unit of Tanami Group. Conformably overlain by Killi Killi Formation. Upward-fining deep water succession dominated by siltstone, carbonaceous siltstone, banded iron formation and mafic sills. Carbonaceous- and iron-rich lithologies are important hosts for gold mineralisation.||||||
35396|Dead Bullock Formation|66129|4|Described|p213, p214 Fig.1, p216 Fig.3|Orosirian|Orosirian|1864-1844 Ma. ~1km thick, upward fining sequence of metasedimentary sandstone, siltstone, shale, chert and rare volcanics. Contains Callie and Ferdies Members. Unit in Tanami Group. Unconformably overlies Billabong Complex.||||||30-MAR-15
35396|Dead Bullock Formation|66468|5|Briefly described|p16-17, p19|Orosirian|Orosirian|~1864-1844 Ma. ~1km thick. Sandstone, iron-rich siltstone, carbonaceous shale, chert, pillow basalt and rare volcanic rocks. Unconformably overlies Billabong Complex. Conformably underlies Killi Killi Formation. Includes Ferdies and Callie Members.||||||
35396|Dead Bullock Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Unit in Tanami Group.||Is overlain by Killi Killi Formation.|Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, boudin chert, amphibolite.|20-OCT-11
35396|Dead Bullock Formation|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Tanami Group.||Overlain by Killi Killi Formation.|Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, boudin chert, amphibolite.|20-OCT-11
35396|Dead Bullock Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent of lower part of Twigg Formation.||Unit in Tanami Group.||Is overlain by Killi Killi Formation.|Siltstone, numerous metadolerite sills.|
35396|Dead Bullock Formation|67824|4|Described|p383-396|Orosirian|Orosirian|Hosts gold, particularly where crustal faults intersect claystone facies.|~ 1840 Ma|Of the Tanami Group.|Includes Ferdies Member, Callie Member.|Is overlain by Killi Killi Formation.|Contains mafic sediment that is iron-rich.|
35396|Dead Bullock Formation|67826|4|Described|p401 Fig.2, p402|Orosirian|Orosirian|207Pb/206Pb zircon age from a tuff. Lower part of the Tanami Group stratigraphy.|~ 1838 +/- 6 Ma|Of the Tanami Group.|Includes Callie Member, Ferdies Member|Is overlain conformably by Killi Killi Formation.|Consists of graphitic and iron-rich sandstones and siltstones.|
35396|Dead Bullock Formation|68474|4|Described|p572, p574|||Granites-Tanami Orogen. See also Dead Bullock Group. 1km thick. Interpreted to be derived from a provenance dominated by a bimodal suite of Archaean mafic and felsic rocks.||Tanami Group|Includes the Callie Member and the Ferdies Member.|Conformably overlain by the Killi Killi Formation.|Sandstone, turbiditic sandstone, carbonaceous siltstone, siltstone, shale, chert and rare volcanic rocks.|
35396|Dead Bullock Formation|68656|6|Mentioned|GEOCHRON|Paleoproterozoic|Paleoproterozoic|||Tanami Group||Is overlain conformably by Killi Killi Formation.||
35396|Dead Bullock Formation|69003|4|Described|p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Deformed by the c.1844-c.1825 Ma Tanami Event and the c.1795 Ma Tanami Orogeny.|1847-1840 Ma.|Tanami Group.||Unconformably overlies the Billabong Complex. Is overlain unconformably by Killi Killi Formation. Lateral equivalent of Stubbins Formation.|Siliciclastic metasedimentary rocks.|
35396|Dead Bullock Formation|69253|4|Described|p746, p747 Fig.1, p748, p753-767|Orosirian|Orosirian|Redefined to include the Stubbins and Mount Charles Formations in WA. ~3 km thick. Predominantly back-arc affinity. Petrophysical properties detailed.|c.1864 Ma (Bagas et al., 2008).|Unit in Tanami Group.||Is intruded by Lewis and Selby Granites. Is overlain conformably by Killi Killi Formation.|Succession of turbiditic sandstone, variably ferruginous and carbonaceous shale, chert, basalt, and associated dolerite sills and rare felsic volcanics.|
35396|Dead Bullock Formation|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Affected by the Tanami (1835 Ma) and Stafford (1805 Ma) Events.||Tanami Group.|||Grey siltstone, silty shale, fine-grained sandstone, laminated siltstone, massive quartzite, fine-grained black shale, chert, nodular chert, amphibolite, minor calc-silicate rock.|
35396|Dead Bullock Formation|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
35396|Dead Bullock Formation|69424|6|Mentioned|p9:4|||Tanami Region.||||Correlative of Ooradidgee Group.||12-JUL-16
35396|Dead Bullock Formation|69426|3|Fully described|p11:1, 3-7, 9, 11, 15-18, 22, 26, 30-31|Orosirian|Orosirian|Defined by Crispe et al. (2007). Incorporates the Mount Charles Beds (Blake et al., 1975), "Blake beds" and "Davidson beds" (Smith et al., 1998), MacFarlane Peak Group and Twigg Formation (Hendrickx et al., 2000). Thickness <1000m. Quiet marine conditions below storm-wave base, with increasingly deep-water deposition towards top. Hosts several major gold deposits, described in detail. The local informal mining names for constituent units are tabulated. Age from Callie Member tuff. An intrusive granite is dated at 1844 +/- 4 Ma (Smith, 2001); may reflect inherited zircons.|1838 +/- 6 Ma (Cross and Crispe, 2007).|Tanami Group.|Ferdies and Callie Members.|Is overlain conformably and transitionally by Killi Killi Formation (locally folded and sheared).|Siltstone and sandstone (Ferdies Member) fining into graphitic siltstone and banded ironstone (Callie Member); chert, schist, greywacke, mafic volcanic rocks, minor intermediate and acid volcanic rocks.|12-JUL-16
35396|Dead Bullock Formation|69587|5|Briefly described|177278.1.pdf|||Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. ||Unit of Tanami Group.||Underlain by Killi Killi Formation.||
35396|Dead Bullock Formation|69618|4|Described|p89-96, p98-99, p100-102, p104 Fig.15|Paleoproterozoic|Paleoproterozoic|Boundary with overlying Killi Killi Formation revised upwards. See also p106, p109-110. Here includes Stubbins and Mount Charles Formations. Subdivided into Ferdies and Callie Members by Crispe and Vandenberg (2004) and Crispe et al. (2007). Also includes an informal basal unit which the authors call Kairos member. >2km thick. Cross and Crispe (2007) give a SHRIMP U-Pb zircon age of 1838 +/- 6 Ma, regarded as stratigraphically uncertain. Minimum age comes from an intrusive monzogranite SHRIMP zircon dated at 1844 +/- 4 Ma (Smith, 2001), and a lithologically similar succession from WA is dated at c.1864 Ma.|c.1864 Ma.|Unit in Tanami Group.|Includes Ferdie and Callie Members.|Is overlain by Killi Killi Formation.|Low-energy succession of chert, BIF, fine-grained pyritic and carbonaceous sedimentary rocks, and basaltic and subvolcanic dolerite sills.|30-MAR-15
35396|Dead Bullock Formation|69747|4|Described|p262-265,267,271,274|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Upper stratigraphic succession represents transition zone to the overlying Killi Killi Formation. Intruded by dolerite sills (e.g. Coora, Groundrush) that have been metamorphosed to upper greenschist to amphibolite facies; deformed to the same degree as the host rock. Maximum depositional age of 1864+\-3 Ma from detrital zircons from turbiditic sandstone from top of the formation.SHRIMP and detrital ages are derived from Bagas et al, 2008.|1864+\-3 Ma (Igneous cryst. SHRIMP)|Unit of Tanami Group.|Includes former Stubbins Formation and former Mount Charles Formation, Madigan Member, Callie Member, Ferdies Member and Kairos Member.|Lower unit of the Tanami Group. Overlain conformably by Killi Killi Formation.|Mudstone, siltstone, carbonaceous siltstone, basalt (locally pillowed), common dolerite sills, and an upper succession of banded and nodular chert, greywacke and rare rhyolite.|25-JUN-19
35396|Dead Bullock Formation|69933|6|Mentioned|p11|||Similar to a weakly magnetic, unnamed unit that produced too few zircons to be dated.||||||
35396|Dead Bullock Formation|70024|6|Mentioned|p35-36|||||Tanami Group.|Callie Member.|Is overlain conformably by Killi Killi Formation.|Pelitic and psammitic schists. Underwent retrogression in the greenschist facies.|
35396|Dead Bullock Formation|70291|4|Described|p178-179,181,183,p198, 201-202|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Restricted to eastern and central Tanami region, barely extends into WA; deposition potentially controlled by Supplejack Fault Zone along eastern depocentre margin. Shown as Dead Bullock Soak Formation on p183. Hosts the majority of the known gold resource in the tanami region.||Unit of Tanami Group.|Includes Callie Boundin Chert, Callie Member and Ferdie Member.|Basal unit of the Tanami Group. Overlain by Killi Killi Formation.|Siltstone and sandstone (Ferdie Member) fining into graphitic siltstone and BIF (Callie Member). Iron-rich sedimentary rocks occur near the stratigraphic top of the formation.|24-JUN-19
35396|Dead Bullock Formation|70478|6|Mentioned|p2 Fig 1, 12|Orosirian|Paleoproterozoic|Geological Province: Tanami. Described as undivided Dead Bullock Formation on p2 Fig 1. Minimum age from Grimwade Suite monzogranite intrusion at 1808+/-3 Ma.||Unit of Tanami Group|Includes Callie Member and Ferdies Member.|Intruded by Grimwade Suite granite.||
35396|Dead Bullock Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|Callie, Fergies Members.|Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|Ferdies, Callie Members.|Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
35396|Dead Bullock Formation|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|c.1864 Ma.|Tanami Group.||Unconformably overlies Browns Range Metamorphics. Is overlain by Killi Killi Formation.||
35396|Dead Bullock Formation|71397|5|Briefly described|p5,22,46|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen.|c. 1880-1840 Ma|Unit of Tanami Group.||||
35396|Dead Bullock Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1865+/-12 Ma (MDA: U-Pb zircon SHRIMP)||||Metasediment.|
35396|Dead Bullock Formation|73089|5|Briefly described|p: 1, 3-7, 10-12, 14, 17, 22-32, 41, 43|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. >1.3 km thick. Interpreted as deposited in a deep water, sediment-starved setting. Lower portion is dominantly Archean detritus. Intruded by a granitic rock with a date of 1844 +/- 4 Ma; marks minimum age constraint. 40Ar/39Ar dating of metamorphic hornblende from dolerite sills (1840 +/- 14 and 1840 +/- 19 Ma) and metamorphic monazite (1839 +/- 9 Ma) constrains an episode of metamorphism. Possibly broadly correlative to Biscay Formation.||Tanami Group|Ferdies Member, Callie Member|Transitionally overlain by Killi Killi Formation. Correlates to Mount Charles Formation and Stubbins Formation. Intruded by Inspiration Peak Monzogranite.||
35396|Dead Bullock Formation|73158|4|Described|p1, p2 Fig.1, p3, p9-11||Orosirian|Defined based on isolated outcrops and drill core. Mafic geochemical signature of volcaniclastic-sedimentary turbidite successions.|1884+/-8 Ma zircon U-Pb MDA|Tanami Group|Ferdies Member, Callie Member|Underlies Killi Killi Formation|Lower greenschist to amphibolite facies metamorphic grade. Includes tholeiitic extrusive basalts.|
35396|Dead Bullock Formation|73159|5|Briefly described|p1, p2 Fig.1, p3, 9-11|||Granites-Tanami Orogen. Defined based on isolated outcrops and drill core within the Dead Bullock Soak and The Granites goldfields. Mafic arc - backarc volcanism.|1884 +/- 8 Ma MDA: Maidment et al., 2020|Tanami Group.|Ferdies, Callie Members.|Is overlain by Killi Killi Formation.|Includes tholeiitic (extrusive) basalts. Lower greenschist- to amphibolite-facies metamorphism.|
79061|Dead camel granite|64956|5|Briefly described|p31-32|Statherian|Statherian|Crystallization age of the granite is interpreted to be 1736 +/- 3 Ma, with evidence for isotopic resetting at ca 550 Ma.||||Intrudes Albarta Metamorphics.||
32407|Deagan Member|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartz arenite and minor pebbly sandstone; planar-, grain size laminated and bedded, tabular; abundant weathered-out shale clasts. Of Short Range Sandstone.||||||07-NOV-08
32407|Deagan Member|23733|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of Short Range Sandstone (Tomkinson Creek Group).||||||07-NOV-08
32407|Deagan Member|24303|2|Defined|p10, p56 Appendix|Statherian|Statherian|Of the Short Range Sandstone. Disconformably to conformably overlain by the Short Range Sandstone middle lithofacies. Disconformably to conformably overlies the Mitty Member. Max. Thickness: 150m. Formerly undifferentiated Tomkinson Creek beds.||||||
32407|Deagan Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Short Range Sst. Sst; sublithic to quartz arenite; lensing, thin to very thick bedded; well sorted, grainsize laminated, crossbedded; lag conglomerate, mudstone; convolute laminated, rippled, current lineated, dessicated, micaceous, halite pseudomorphs||||||07-NOV-08
32407|Deagan Member|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Short Range Sandstone. Quartz arenite and minor pebbly sandstone; grain size laminated, planar bedded, tabular.||||||07-NOV-08
32407|Deagan Member|60684|6|Mentioned|p12|||Basal interval of Short Range Sandstone.  On HELEN SPRINGS map sheet.||||||
32407|Deagan Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Short Range Sandstone(Tomkinson Creek Group). Siltstone; subordinate interbedded sandstone: quartz arenite and minor pebbly arenite; conglomerate. In the Tennant Creek region.||||||07-NOV-08
32407|Deagan Member|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Morphett Creek Formation||||
32407|Deagan Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Short Range Sandstone.|||Quartz arenite and minor pebbly arenite; conglomerate; siltstone; subordinate interbedded sandstone.|
32407|Deagan Member|69425|5|Briefly described|p10:12|||Tomkinson Province.||Short Range Sandstone.||Partly correlated with Canulgerra Sandstone and possibly Lennee Creek Formation.||12-JUL-16
32407|Deagan Member|69431|4|Described|p16:4-6, 9-11, 23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.30-150m thick. Intertidal to shallow-marine deposits. At least in part transitional between Morphett Creek Formation and the rest of Short Range Sandstone. Lithology described in some detail.||Short Range Sandstone.||Overlies Kuerschner Member gradationally (conformably) and Mitty Member conformably to disconformably.|Predominantly thinly to thickly bedded quartz sandstone with minor conglomerate and mudstone in a fining-upward succession. Local basal pebble to boulder conglomerate, up to 8m thick, planar bedded and laterally persistent.|12-JUL-16
23539|Deep Bore Metamorphics|9694|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division Two). Cordierite felsic granulite, mafic granulite, para-amphibolite, calc-silicate rock, sillimanite gneiss.||||||
23539|Deep Bore Metamorphics|23732|4|Described|p10|Paleoproterozoic|Paleoproterozoic|Intruded by Marshall Granite. Max. age: 1805+/-7Ma. See also figures on p2, p5 and p10.  Geological Province: Arunta Province.||||||07-NOV-08
23539|Deep Bore Metamorphics|23733|5|Briefly described|p34 Fig.20|||Age: 1805Ma.||||||
23539|Deep Bore Metamorphics|23809|5|Briefly described|p43, p41 Tb. 5|Paleoproterozoic|Paleoproterozoic|Cordierite-orthopyroxene biotite gneiss.  Age: 1805+/-7Ma.  Geological Province: Arunta Province.||||||07-NOV-08
23539|Deep Bore Metamorphics|23868|4|Described|p741|||Intruded by the Marshall Granite.  Geological Province: Arunta Inlier.||||||21-SEP-09
23539|Deep Bore Metamorphics|39887|6|Mentioned|Fig.5|||||||||
23539|Deep Bore Metamorphics|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23539|Deep Bore Metamorphics|40906|4|Described|p9|||||||||
23539|Deep Bore Metamorphics|49036|2|Defined|p7|Proterozoic|Proterozoic|Early to Mid-Proterozoic. Previously mapped as Arunta Complex.||||||
23539|Deep Bore Metamorphics|50246|6|Mentioned|p4|||Age: 1810-100Ma.||||||07-FEB-11
23539|Deep Bore Metamorphics|50369|6|Mentioned|p16.2|||Intruded by Marshall Granite.||||||
23539|Deep Bore Metamorphics|62595|6|Mentioned|p3. |||Included in Scrimgeour's (2003) Ongeva package.||||||
23539|Deep Bore Metamorphics|64068|5|Briefly described|p31, 32|||Bundled in with Strangways Metamorphic Complex, Bonya Schist and Cackleberry Metamorphics as the Ongeva package; likely equivalent to lower Hatches Creek Group in Davenport Province. Protoliths have volcaniclastic origin aged 1810-1800 Ma.||||||
23539|Deep Bore Metamorphics|64738|6|Mentioned|p247 Fig.1, p250, Table 1, p251, p260.|Paleoproterozoic|Paleoproterozoic|Metamorphic zircon overgrowths have ages c.1750-1700 Ma, average 1730 +/- 6 Ma.||||||
23539|Deep Bore Metamorphics|65341|5|Briefly described|p4, p20.|||Underwent high-T, low-P metamorphism (3 - 4 kbar and 750 - 800 degrees C) during the Strangways Orogeny at 1730 +/- 7 Ma. Has affinities with Anira Metamorphics, also metamorphosed during the Strangways Event.||||||
23539|Deep Bore Metamorphics|65556|6|Mentioned|p35|||Similar metamorphic style to Anira Metamorphics: localised high-temperature, low pressure.||||||
23539|Deep Bore Metamorphics|68150|5|Briefly described|p11 Tb.3.2, p32|||Age: SHRIMP, MSWD 0.8, 12 analyses, Scrimgeour et al. (2001).|1730 +/- 7 Ma, metamorphism|||is intruded by Marshall Granite||
23539|Deep Bore Metamorphics|69227|6|Mentioned|p264-266|Paleoproterozoic|Paleoproterozoic|Shaw et al. (1984). Jinka Province, Arunta Inlier. Syn- to post-depositional granites intruded at 1780-1710 Ma.||||||
23539|Deep Bore Metamorphics|69427|5|Briefly described|p12:8, 12-13, 39|Statherian|Orosirian|Aileron Province. The package comprising Deep Bore, Cackleberry, Delmore Metamorphics and part of Bonya Schist may be equivalent to the lower part of the Strangways Metamorphic Complex. Metamorphism briefly described. SHRIMP U-Pb zircon age of volcaniclastic protolith; metamorphosed at 1730 +/- 7 Ma.|1805 +/- 7 Ma (Scrimgeour et al., 2001).||||Granulite-facies metapelitic gneiss with less abundant aluminous metapsammitic rock, variably migmatitic; calc-silicate rock and mafic granulite.|12-JUL-16
23539|Deep Bore Metamorphics|69794|6|Mentioned|p16|Paleoproterozoic|Paleoproterozoic|Scrimgeous (2001) reported a maximum depositional age of 1805+\-7 Ma.||||||
23539|Deep Bore Metamorphics|69917|6|Mentioned|p87|||Arunta Region, Jinka Domain||||Stratigraphically equivalent to the Strangways Metamorphic Complex.||
23539|Deep Bore Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1730 +/- 7 Ma (U-Pb zircon SHRIMP).|1805+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Cordierite-orthopyroxene-biotite-quartz gneiss.|
23539|Deep Bore Metamorphics|71750|4|Described|iii,p1,13-20|Statherian|Orosirian|Geological province: Aileron Province. Granulite facies; migmatitic metavolcaniclastic rocks north of the Delny Shear Zone within the Deep Bore Domain. Likely to have similar provenance to Perenti and Kanandra metamorphics based on similarities and provenance spectra and max depositional ages (Claou¿-Long and Hoatson 2005; Kositcin et al 2014, 2015); broadly representing the same sedimentary package at different metamorphic grades. Sample: GA 2306968 (NTGS HU15BLR1032A) (546378E 7492614N) zircon analysis yields ages of 1808+\-5 Ma (interpreted magmatic crystallisation age), and 1727+\-18 (metamorphic rim growth during a long lived Paleoproterozoic event) and 548+\-13 Ma (metamorphic/resetting ages). Sample: GA 2307041 (NTGS HU15EEB1004) (557411E 7490053N) zircon analysis yields ages of 1791+\-6 Ma (interpreted maximum depositional age) and 1738+\-5 Ma (zircon rims; metamorphic growth)  with age range 2684-1763 Ma.|1808+\-5 Ma magmatic crystallisation age.||||Migmatitic metavolcaniclastic rocks, and minor metamudstone and metacalc-silicate rock.|20-SEP-19
23539|Deep Bore Metamorphics|71839|4|Described|iii, p1, p21-p22, p24-p26|Statherian|Statherian|Exposed in the pit wall of the Molyhil W-Mo deposit in central JINKA. A metamorphic Pb-Pb age of 1717 +/- 7 Ma is also derived and interpreted as the minimum metamorphism age. Sampling location and description there are described, additionally zircon morphology, U-Pb analyses and results are also provided. Intepreted to be the grey-coloured gneiss in the Molyhil pit.|1769 +/- 25 Ma (Pb-Pb; Max. dep. age)|||Intruded by the Marshall Granite.|Grey-coloured gneiss, calc-silicate rocks, granulite facies, migmatitic metavolcaniclastic rocks and metamudstone.|20-MAR-23
23539|Deep Bore Metamorphics|72367|5|Briefly described|iii,p1,21-23,26,30|Statherian|Statherian|Geological province: Aileron Province. Metamorphosed sedimentary-volcanoclastic sequence intruded by extensive felsic magmas at c. 1790 Ma (eg Beyer et al in prep). Occur within the Deep Bore Domain north of the Delny Shear Zone in the Aileron Province. Sample HU15EEB1004 (orthopyroxene gneiss) records a maximum deposition age of 1819+\-9 Ma and metamorphic zircon growth at 1787+\-11 Ma. Sample HU15BLR1032A (Crd-Bt-Qtz rock) records a zircon crystallisation age of 1822+\-9 Ma and metamorphic zircon growth at 1781+\-9 Ma and 1728+\-13 Ma. The c. 1820 Ma zircon ages may reflect volcaniclastic deposition of the protolith, or volcanic rock component of the sedimentary protolith. The zircon growth ages at c. 1780 and c.1730 Ma likely represents metamorphic zircon growth related to widepstead felsic magmatism at that time.|||||Granulite facies migmatitic metavolcanoclastic rocks, minor metamudstone, and minor metacalc-silicate rock.|
23539|Deep Bore Metamorphics|72372|6|Mentioned|p2|||Geological province: Aileron Province.||||||
23539|Deep Bore Metamorphics|72516|5|Briefly described|p7, p192|||Aileron Province. Maximum depositional ages: 1822 +/- 9 Ma (Reno et al 2018), 1805 +/- 7 Ma Scrimgeour and Raith 2001), 1791 +/- 6 Ma (Kositcin et al 2018a), 1769 +/- 25 Ma (Kositcin et al 2018b). Occurs in the Jinka 1:100K map sheet area.||||Possible age equivalent to Bonya Metamorphics.||27-MAY-21
23539|Deep Bore Metamorphics|72711|6|Mentioned|p6.|Statherian|Statherian|Interpreted as occurring as rafts within the Marshall Granite. Minimum age inferred from nearby Molyhil tungsten-molybdenum skarn deposit date.|mineralisation age c. 1720 Ma.||||Includes metasedimentary rocks.|
23539|Deep Bore Metamorphics|73123|6|Mentioned|piii, p5, p8|Statherian|Orosirian|Records multiple phases of metamorphic zircon growth between 1787 +/- 11 Ma and 1717 +/- 7 Ma, representing a protracted metamorphic history.|ca 1.82-1.79 Ga|||||
23539|Deep Bore Metamorphics|73128|5|Briefly described|p5, p8|Statherian|Orosirian|Present as surface outcrop at Molyhil tungsten-molybdenum deposit, Jinka 1:100 000 map sheet. U-Pb zircon maximum depositional ages of ca 1822 to 1805 Ma. Multiple phases of metamorphic zircon growth between 1787 +/- 11 Ma and 1717 +/- 7 Ma. Can constitute xenoliths within the Yam Gneiss and Marshall Granite.|ca 1822 to 1805 Ma|||Intruded by Yam Gneiss and Marshall Granite.|Includes metagreywacke gneiss sub-units.|
23539|Deep Bore Metamorphics|73551|5|Briefly described|piii, p11-12, p14-15|Statherian|Orosirian|Interpreted as the host rock for the Molyhil W-Mo deposit. Experienced long-lived metamorphism during the Palaeoproterozoic, with supersolidus metamorphism observed until at least ca 1.72 Ga.|ca 1.79 Ga|||Intruded by Yam Gneiss and Marshall Granite.|Includes a metavolcaniclastic component.|
23539|Deep Bore Metamorphics|73591|4|Described|piv, p2, p14, p30, p33-36|||Aileron Province. Occurs north of the Delny Shear Zone in the Aileron Province. Generally deeply weathered. Previous SHRIMP U-Pb zircon ages reported by Kositcin et al. (2018) and others. Pressure-temperature data also reported. Youngest detrital zircon population analysed for Lu-Hf isotopes yielding a wide range of values.|ca 1808 Ma||Cackleberry Metacarbonate, Utopia Quartzite, Ledan Schist|Cross cut by Marshall Granite. Intruded by Narbarloo Granite.|Granulite facies, locally migmatitic metagreywacke gneiss, aluminous metasandstones, metacarbonates, quartzite, schist, and minor metavolcaniclastic rocks.|
25875|Deering Siltstone Member|22566|6|Mentioned|Fig 2 on p77|||Of Parke Siltstone.||||||08-AUG-06
25875|Deering Siltstone Member|22646|6|Mentioned|p 107|||Of Parke Siltstone.  Situated in Dare Plain||||||08-AUG-06
25875|Deering Siltstone Member|22760|5|Briefly described|p339|Middle Devonian|Middle Devonian|Of Parke Siltstone.||||||08-AUG-06
25875|Deering Siltstone Member|22761|6|Mentioned|p350|||Of Parke Siltstone.||||||08-AUG-06
25875|Deering Siltstone Member|22804|6|Mentioned|p454||Devonian|Of Parke Siltstone.||||||08-AUG-06
25875|Deering Siltstone Member|31566|2|Defined|p232|Devonian|Devonian|||||||
25875|Deering Siltstone Member|32640|6|Mentioned|p237|||||||||
25875|Deering Siltstone Member|35102|6|Mentioned|p39|||||||||
25875|Deering Siltstone Member|41018|6|Mentioned|p236|||||||||
25875|Deering Siltstone Member|41385|6|Mentioned|p364|||See also Fig.2||||||
25875|Deering Siltstone Member|43225|5|Briefly described|Map Legend||Devonian|Of Pertnjara Group.||||||08-AUG-06
25875|Deering Siltstone Member|43503|6|Mentioned|42-45|Late Devonian|Middle Devonian|||||||
25875|Deering Siltstone Member|43648|6|Mentioned|Fig.27,p509|||||||||
25875|Deering Siltstone Member|43649|5|Briefly described|p459,462|||||||||
25875|Deering Siltstone Member|47050|6|Mentioned|p244|||||||||
25875|Deering Siltstone Member|67565|5|Briefly described|p42.|Devonian|Devonian|||Basal unit in Parke Siltstone.||Is overlain by Harajica Sandstone Member.|Laminated and massive red-brown siltstone with minor fine sandstone.|
25875|Deering Siltstone Member|69438|3|Fully described|p23:38-39|||Jones (1972). Amadeus Basin. Type section occurs on the N flank of the Mereenie Anticline where it is 100m thick. Elsewhere up to c.240m thick.||Basal Parke Siltstone.||Generally conformably overlies Mereenie Sandstone. Is overlain conformably/gradationally by Harajica Sandstone Member. Probable equivalent of N'Dahla Member.|Alternating laminated and massive red-brown siltstone; local thin limestone or calcareous siltstone beds; sandstone beds are sporadic and fine- to very fine-grained. Various sedimentary structures listed.|12-JUL-16
25875|Deering Siltstone Member|69673|6|Mentioned|p67|||||Parke Siltstone||||
26516|Delmore Metamorphics|22524|6|Mentioned|p42|||||||||
26516|Delmore Metamorphics|23732|6|Mentioned|p27, 28|||Geological Province: Arunta Province.||||||
26516|Delmore Metamorphics|23733|5|Briefly described|p34 Fig.20|||||||||
26516|Delmore Metamorphics|23868|6|Mentioned|p753 Fig. 10, p754|||Geological Province: Arunta Inlier.||||||
26516|Delmore Metamorphics|33103|4|Described|Table 1|||Mention p14.||||||08-AUG-06
26516|Delmore Metamorphics|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
26516|Delmore Metamorphics|39887|6|Mentioned|Fig.5|||||||||
26516|Delmore Metamorphics|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
26516|Delmore Metamorphics|40906|6|Mentioned|p9|||||||||
26516|Delmore Metamorphics|43568|6|Mentioned|Fig.4,p506|||||||||
26516|Delmore Metamorphics|46868|6|Mentioned|Fig.2|||||||||
26516|Delmore Metamorphics|48992|6|Mentioned|p10|||||||||
26516|Delmore Metamorphics|50369|6|Mentioned|p15.2|||Intruded by Mount Ida Granite.||||||
26516|Delmore Metamorphics|61208|5|Briefly described|p208|||Unconformably overlain by Ledan Schist. ||||||
26516|Delmore Metamorphics|65232|6|Mentioned|App. 2|||||||||09-FEB-10
26516|Delmore Metamorphics|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
26516|Delmore Metamorphics|68997|4|Described|vi-vii,p1,17-23,43|Orosirian|Orosirian|Metasedimentary and meta-igneous rocks that outcrop on Delmore Downs Station in eastern ALCOOTA. Metamorphosed to amphibolite facies. Intruded by 1810-1800 Ma granitic rocks associated with the Stafford Event (eg Scrimgeour 2003). Zircon age spectra of 1814+\-9 Ma from metapelite (Sample: AC07LCV293A. Grid Reference: MGA94 Zone 53: 470626mE 7517574mN), interpreted as maximum depositional age. Intruded by 1707.5+\-2.7 Ma orthogneiss (NTGS AC07LCV356B. Grid Reference: MGA94 Zone 53: 468353mE 7510530mN), likely representing coeval magmatism during 1730-1690 Ma Strangways Event metamorphism. Zircon ages from the orthogneiss include 1676+\-6 Ma and 1579+\-12 Ma, representing Strangways and Chewnings Orogenies respectively. |1814+\-9 Ma (max dep age: U-Pb zircon)||||Calc-silicates, epidote-bearing quartzite, garnet-biotite schist and gneiss, altered intermediate to felsic volcanics and cordierite-anthophyllite rocks.|
26516|Delmore Metamorphics|69427|5|Briefly described|p12:8, 12-13|Statherian|Orosirian|Aileron Province. The package comprising Deep Bore, Cackleberry, Delmore Metamorphics and part of Bonya Schist may be equivalent to the lower part of the Strangways Metamorphic Complex. SHRIMP U-Pb zircon maximum deposition age.|<1806 +/- 21 Ma (Beyer et al., 2010).||||Metapelitic schist, calcareous metasedimentary rocks, possible felsic metavolcanic rocks, amphibolite and a lens of antophyllite-chlorite-cordierite rock.|12-JUL-16
26516|Delmore Metamorphics|69917|5|Briefly described|p85-91, 82, 83|Paleoproterozoic|Paleoproterozoic|Central Arunta Region, Aileron Province. 3 samples dated. U/Pb LA-ICPMS zircon dating. Maximum depositional age for the metavolcaniclastic rock sample is poorly constrained at 1806+/-21 Ma. U/Pb SHRIMP zircon dating, Hf analytical data.  Poorly constrained maximum depositional age of 1814+/-9 Ma for cordierite-bearing metapsammite. Igneous crystallisation age of 1707+/-4 Ma for orthogneiss interpreted as a high-level intrusive within metasedimentary rock.|||||Calc-silicate rock, epidote-bearing quartzite, garnet-biotite schist and gneiss, altered intermediate to felsic volcanic rocks and cordierite-anthophyllite rocks. Metavolcaniclastic rock.|
26516|Delmore Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1814+/-8 Ma (U-Pb zircon SHRIMP)||||Metavolcaniclastics, metapsammite.|
79232|Denara Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both ages are of metamorphism: U-Pb monazite LA-ICPMS.|1723+/-4 Ma and 451+/-6 Ma.||||K-feldspar-plagioclase-quartz migmatite, migmatitic orthogneiss, biotite-feldspar-quartz schist.|
79232|Denara Orthogneiss|71621|4|Described|iii, p1, p7-p13, p33-p34, p37, p43-p44|Statherian|Statherian|Aileron Province. An additional SHRIMP U-Pb age of 1779 +/- 5 Ma is provided along with a LA-ICPMS age of 1778 +/- 6 Ma; these ages are all interpreted as the age of magmatic crystallisation. Metamorphism is dated at 1744 +/- 4 Ma and 1749 +/- 4 Ma by SHRIMP U-Pb (Kositcin et al, 2011). A summary of SHRIMP U-Pb and LA-ICPMS isotopic data and interpretation is provided. Petrography and zircon description discussed.|1778.7 +/-3 Ma(SHRIMP U-Pb)||||Strongly foliated, compositionally layered migmatite with melaonsomes of biotite-plagioclase-quartz-garnet and leucocratic layers of plagioclase-quartz with occasional feldspar and biotite.|01-FEB-19
79232|Denara Orthogneiss|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1779 +/- 5 Ma (U-Pb zircon)||||Migmatite: granite to granodiorite gneiss, medium-grained, leucosomes variably deformed; locally biotite-altered.|
79232|Denara Orthogneiss|72516|2|Defined|iii, p10, 11, p15, p21, p64-69, p200|Statherian|Statherian|Aileron Province, Denara Domain. New name derived from the Denara Bore. Type locality is defined as approximately 9km northeast of Denara Bore at 638358mE 7466068mN. Previously mapped as an unnamed unit within Division One of the Strangways Metamorphic Complex by Freeman et al (1986). This unit is poorly exposed and outcrops commonly as scattered pavements and tors surrounded by sand and colluvium; there are three main areas of outcrop: around Denara Bore between the Marshall River and Bonya Creek, a western area northwest of the Jervois Homestead and an eastern area northeast of the Coolabah Bore. Records highest temperatures in the map sheet area. Additional SHRIMP ages are derived from Beyer et al(1778 +/- 6 Ma) and Kositcinn et al, 2011 (1779 +/- 3 Ma). Distinguishing features, genesis, geophysics, petrography, geochemistry, metamorphism and structure are all discussed. Associated with an unnamed granite. Intruded by quartz veins along the Delny Shear Zone. Coeval with the emplacement of the Baikal Supersuite. See also  p18, p72, p79, p84, p96, p98, p112-116, p118-119, p122-123, p125-127, p135-136, p145-148, p151-152, p158, p165-171, p174-175, p186-187, p200-202.|1779 +/- 5 Ma (SHRIMP U-Pb, Kositcin et al, 2015)|||Unconformably overlain by the Waite Formation. Intruded by the Jervois Granodiorite. Structural contact with the Yambla Gneiss.|I-type migmatite: granite to granodiorite gneiss, medium-grained, leucosomes variably deformed, locally biotite altered.|19-APR-22
79232|Denara Orthogneiss|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes orthogneiss.|
35928|Derim Derim Dolerite|23363|5|Briefly described|369|||||||||
35928|Derim Derim Dolerite|23374|5|Briefly described|p6,20,34,35||Ectasian|Age: 1324Ma. Intrudes Roper Group. Reserved as Derim Derim Dolerite Suite. of McArthur Basin.||||||
35928|Derim Derim Dolerite|23867|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Age: 1324+/-4Ma.||||||
35928|Derim Derim Dolerite|23937|2|Defined|p78 App. 1, p47|Ectasian|Ectasian|Referred to as "Basic Intrusives" by Dunn (1963b).  Intrudes Mount Rigg Group; intrudes Roper Group as sills.  Age: 1324+/-4Ma (SHRIMP U/Pb). Geological Province: McArthur Basin.||||||13-APR-05
35928|Derim Derim Dolerite|24047|6|Mentioned|p27|||Also referred to as Derim Derim Dolerite Suite in the McArthur Basin (Fig. 10, p12).  Geological Province: Georgina Basin.||||||
35928|Derim Derim Dolerite|24050|3|Fully described|p50, p8 Tb. 2|||Medium- to coarse-grained dolerite. Intrusive into Mt. Rigg and Roper Groups.  Max. thickness: 100m.||||||08-AUG-06
35928|Derim Derim Dolerite|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
35928|Derim Derim Dolerite|50545|5|Briefly described|p113, 137||Ectasian|Age: 1324 +/-4 Ma.||||||17-DEC-07
35928|Derim Derim Dolerite|60483|5|Briefly described|p9|||Intrudes Roper Group. Age: ~1324+/-4Ma (SHRIMP, J. Claoue-Long, pers.comm). ||||||
35928|Derim Derim Dolerite|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Medium to coarse-grained dolerite, variably altered; composition dominated by plagioclase, clinopyroxene and opaques.||||||
35928|Derim Derim Dolerite|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Dolerite: medium to coarse grained, variably altered; composition dominated by plagioclase, clinopyroxene and Fe-Ti oxides.||||||
35928|Derim Derim Dolerite|61560|5|Briefly described|p489, p496|Mesoproterozoic|Mesoproterozoic|Dolerite sill. Age: ca.1325Ma. ||||||
35928|Derim Derim Dolerite|61572|5|Briefly described|p667 Fig. 2|Mesoproterozoic|Mesoproterozoic|Medium to coarse dolerite. Concordant sills intrude Roper and Mount Rigg Groups.  Age: 1324+/-4Ma. Max. thickness: 100m. Geological Province: McArthur Basin. See also p671 Tb. 1.||||||
35928|Derim Derim Dolerite|63866|5|Briefly described|p113, p115, p116|Ectasian|Ectasian|Roper Superbasin.|1324 +/- 4 Ma (Claoue-Long, J.C., unpub.)|||||
35928|Derim Derim Dolerite|65337|6|Mentioned|p7.||||c.1324 Ma (Claoue-Long 1997).|||||
35928|Derim Derim Dolerite|65340|6|Mentioned|p11.||||1324 Ma (Claoue-Long, pers. comm.1997).|||||
35928|Derim Derim Dolerite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Appears as Derim Derim dolerite. Sills in the McArthur Province produced in the Fraser Event, ME 20 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1310 Ma.|||||
35928|Derim Derim Dolerite|67057|5|Briefly described|p463.|Mesoproterozoic|Mesoproterozoic||1324 +/- 4 Ma (Sweet et al. 1999b).|||||
35928|Derim Derim Dolerite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
35928|Derim Derim Dolerite|67779|5|Briefly described|p8 Table 1, p40, p103.|Paleoproterozoic|Paleoproterozoic|Widespread unit. Correlated with Galiwinku Dolerite.|1324 +/- 4 Ma (Goldberg, 2010).|||Intrudes Roper Group.||
35928|Derim Derim Dolerite|68146|5|Briefly described|p197|||Roper River area.|c.1324 Ma.|||Intrudes Roper Group.||
35928|Derim Derim Dolerite|69429|6|Mentioned|p14:4 Fig.14.6|||||||||12-JUL-16
35928|Derim Derim Dolerite|69430|4|Described|p15:26-27, 30-31, 43-44, 59|Ectasian|Ectasian|Abbott et al. (2001). 60-70m thick. Uniform in composition and mineralogy (plagioclase, clinopyroxene and opaques). Strong magnetic response. Crops out as low-relief, variably altered and weathered boulders. Weathers to produce eluvial and colluvial heavy mineral concentrates rich in ilmenite and titanomagnetite (and very low in Cr, U and Th). Associated with Dook Creek Formation in the Bulman base metal mineral field. SHRIMP U-Pb baddeleyite age; supersedes the previous minimum age of 1280 Ma (McDougall et al., 1965).|1324 +/- 4 Ma (Abbott et al., 2001).|||Intrudes Roper Group.|Fine- to coarse-grained dolerite.|12-JUL-16
35928|Derim Derim Dolerite|69431|5|Briefly described|p16:22|||SHRIMP U-Pb baddeleyite age.|1324 +/- 4 Ma (Abbott et al., 2001).|||Intrudes Roper Group.|Dolerite.|12-JUL-16
35928|Derim Derim Dolerite|69458|5|Briefly described|p42:38|Proterozoic|Proterozoic|Roper River area. Source of a regolith profile containing an economic deposit of highest-grade ilmenite (the Sill 80 project).||||Intrudes Roper Group.||12-JUL-16
35928|Derim Derim Dolerite|69673|6|Mentioned|p19 fig 16|||Date retrieved from Baddeleyite.|1324 +/- 4 Ma (SHRIMP)|||||
35928|Derim Derim Dolerite|70936|5|Briefly described|p77|Ectasian|Ectasian|Of McArthur Basin. Suite of c.1325 Ma dolerite sykes and suills roughly 1500km ENE of Wongawobbin Basin.|c. 1325 Ma|||||
35928|Derim Derim Dolerite|70968|3|Fully described|p6, p19, p33, p46, p51, p55-56, p67, p77|Ectasian|Ectasian|See also p82, p86, p91-94, p115, p123-124, p126, p131, p135. Sweet and Young in Abbott et al. (2001). Named after Derim Derim Creek. Referred to as Basic Intrusives by Dunn (1963). Forms low hills and rounded boulders. The type section is a sill in Derim Derim Creek between 371800mE 8433500mN (lower contact) and370700mE 8430900mN (upper contact) in URAPUNGA sheet. Widely exposed and encountered in numerous wells. Dykes usually <10m wide; sills from 20m to maximum of 173.4m thick. SHRIMP U-Pb baddeleyite age; supersedes a previous K-Ar age of 1280 Ma by McDougall et al. (1965).|1324 +/- 4 Ma (Abbott et al., 2001).|||Intrudes all units in Maiwok Subgroup except Chambers River Formation; Jalboi Formation, and Mainoru Formation at contact with Crawford Formation. Correlated with Galiwinku Dolerite.|Consists mainly of plagioclase, clinopyroxene and opaques (mainly magnetite); minor quartz. Chemically differentiated continental tholeiites.|24-FEB-17
35928|Derim Derim Dolerite|71169|5|Briefly described|p80|Ectasian|Ectasian|McArthur Basin, Pine Creek Orogen and Tomkinson Province.|1324 +/- 4 Ma|||||
35928|Derim Derim Dolerite|71369|5|Briefly described|p4, p49|||Young and Sweet (2001).|1324 +/- 4 Ma.|||||20-FEB-18
35928|Derim Derim Dolerite|71374|6|Mentioned|p23||||||||Dolerite.|
35928|Derim Derim Dolerite|71488|5|Briefly described|p141 fig 1b, p142, p146|Ectasian|Ectasian|U-Pb SHRIMP Baddelyite age reported in Abbott et al., 2001.|1324 +/- 4 Ma|||Intrudes the Maiwok Subgroup.||
35928|Derim Derim Dolerite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1324+/-4 Ma (baddeleyite: u-Pb SHRIMP)||||Dolerite.|
35928|Derim Derim Dolerite|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin. See also Derim Derim Dolerite Suite elsewhere in map key.|||||Dolerite and gabbro sills.|05-MAR-20
35928|Derim Derim Dolerite|71779|5|Briefly described|p5-p7, p25-p27|||McArthur Basin. 108.8m thick in drillhole POG Walton-2 where it intrudes the Kalala Member.  Thickest intersection mentioned is 281.4 m in POG Altree-2.|c. 1313 Ma|||Intrudes the Roper Group, including the Kalala Member of the Velkerri Formation.||24-SEP-18
35928|Derim Derim Dolerite|71893|4|Described|iii, p8, p33, p37, p40, p52, p56, p64|Ectasian|Ectasian|TIMS date is a baddelyite age from Collins et al, 2018. This unit broadly correlates with an unnamed dolerite sill which intrudes the Renner Group and is dated at 1295 +/- 14 Ma.|1312.9 +/- 0.7 Ma (U-Pb TIMS)|||Intrudes the Moroak Sandstone, Bukalorkmi Sandstone (Roper Group) and the Gleeson Formation (Renner Group).||
35928|Derim Derim Dolerite|72381|5|Briefly described|p773|||Of Beetaloo Sub-basin, McArthur Basin. Intrudes all formations of the upper Roper Group and provides a minimum age constraint on Roper Group deposition. Abbott et al. (2001) reported U-Pb SIMS baddeleyite age of 1324+\-4 Ma; Collins et al., 2018 reported U-Pn TIMS baddeleyite age of 1312.9+\-0.7 Ma.||||Intrudes all upper Roper Group units.||04-OCT-19
35928|Derim Derim Dolerite|72526|5|Briefly described|p3, p85.|Ectasian|Ectasian|The age of this intrusive unit provides a minimum age for the Roper Group. A baddeleyite was age obtained from an intrusion into the Maiwok Subgroup (Collins et al. 2018).|1313 Ma baddeleyite|||Intrudes into Collara Subgroup and the Maiwok Subgroup, Roper Group.||
35928|Derim Derim Dolerite|72527|6|Mentioned|p10.|Ectasian|Ectasian|SHRIMP U/Pb baddeleyite age.|1324 +/- 4 Ma-1312.9 +/- 0.7 Ma|||Intrudes Roper Group between Mainoru Formation and Bukalorkmi Sandstone.|Includes dolerite dykes and sills.|
35928|Derim Derim Dolerite|72718|6|Mentioned|p7, p9|Ectasian|Ectasian|Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Extensively intrudes the Wilton package.|1324 +/- 4 Ma|||Underlain by Bukalorkmi Sandstone. Overlain by Chambers River Formation.||
35928|Derim Derim Dolerite|72912|5|Briefly described|p20-21.|Ectasian|Ectasian|Intrudes both Collara Subgroup (from Mainoru Formation) and Maiwok Subgroup up to the top (Bukalorkmi Sandstone). [probably U-Pb SHRIMP] baddelyite magmatic ages.|1324 +/- 0.7 Ma, 1312.9 +/- 0.7 Ma|||Intrudes the Roper Group.||
35928|Derim Derim Dolerite|73083|6|Mentioned|p36|Mesoproterozoic|Mesoproterozoic|||||||
35928|Derim Derim Dolerite|73242|4|Described|p36-40, p42-47|Ectasian|Ectasian|McArthur Basin, including Beetaloo Sub-basin. Constitutes a major component of Mesoproterozoic intraplate mafic magmatism in northern Australia. Intrudes Roper Group (between Mainoru Formation, Collara Subgroup, and Bukalorkmi Sandstone, Maiwok Subgroup) prior to post-Roper basin inversion, indicated by deformed bedding-parallel sills. Previous magmatic crystallisation age of 1324 +/- 4 Ma based on unpublished U-Pb SHRIMP analysis of baddeleyite. Same samples re-analysed yielded an age of 1320.1 +/- 5.3 Ma. Geochron is ID-TIMS baddeleyite age, which is older than a previous age (1312.9 +/- 0.7 Ma ID-TIMS baddeleyite) from dolerite in the Beetaloo Sub-basin. This is inferred to indicate that magmatism associated with this unit spanned at least 10-15 Myr. Similar age as units from the Tomkinson Province, Nimbuwah Domain, eastern Pine Creek Orogen, and Yanliao Large Igneous Province (LIP) in the northern North China Craton [implications for tectonic reconstruction]. Tectonic setting is distinct from Fraser Complex. Type locality is the bed of Derim Derim Creek at Policemans Yard.  Referred to with Galiwinku Dolerite as Derim Derim-Galiwinku igneous province / mafic igneous province / large igneous province.|1327.5 +/- 0.6 Ma ID-TIMS baddeleyite|||Intrudes Roper Group including Jalboi Formation and Crawford Formation.|Medium- to coarse-grained dolerite sills and dykes.|
35928|Derim Derim Dolerite|73412|5|Briefly described|p4, 9, 11-13, 20|||Southern McArthur Basin.|1313 Ma.|Maiwok Subgroup.||Overlies Sherwin Formation. Is overlain by Kyalla Formation.|Dolerite sills.|
30736|Devils Suite|23733|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Includes Devils Marbles, Elkedra and Warrego Granites. Age: ~1710Ma.||||||07-NOV-08
30736|Devils Suite|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1710Ma.  Geological Province: Davenport Province (Tennant Inlier).  See also p8 Fig. 7.||||||07-NOV-08
30736|Devils Suite|24197|4|Described|p28, p65|Paleoproterozoic|Paleoproterozoic|Comprises Devils Marbles, Elkedra and Warrego Granites. An extremely fractionated, oxidised, fluorite-bearing I-(granodiorite) type. Age: ~1710Ma. Geological Province: Tennant Creek/Davenport Province. Eg. of the Sybella Assoc. See also p68 Tb. 6.1.||||||07-FEB-11
30736|Devils Suite|24567|5|Briefly described|p162, p160 Tb. 2|Mesoproterozoic|Mesoproterozoic|Age: 1710Ma. Geological Province: Tennant Creek Inlier.||||||09-MAY-05
30736|Devils Suite|50588|5|Briefly described|p1.4, 4.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Age: 1710Ma.||||||07-NOV-08
30736|Devils Suite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Warrego, Elkedra and Devils Marble Granites. In the Tennant Creek region.||||||07-NOV-08
30736|Devils Suite|63866|5|Briefly described|p90-p91, p107|Statherian|Statherian|Tennant Region, North Australian Craton. Intruded Tennant Region stratigraphy approximately 1710 Ma.|c. 1700-1750 Ma||||Granites and mantle-derived lamprophyre dykes.|
30736|Devils Suite|64735|5|Briefly described|p206, p215, p216 Fig 15,||Statherian|Syn- to post-tectonic.|ca. 1710 Ma.||Includes Devils Marbles Granite, Elkedra Granite, Kaidwalla granite.|||30-APR-12
30736|Devils Suite|64737|6|Mentioned|p232 Fig.2|Statherian|Statherian|| ~1700 Ma.|||||01-MAY-12
30736|Devils Suite|64738|5|Briefly described|pp257-259. |||High crustal level intrusions.|||Includes Devils Marbles and Elkedra Granites.|||
30736|Devils Suite|65209|5|Briefly described|p35 Fig.1, p37, p39|Paleoproterozoic|Paleoproterozoic||~1720 Ma (Blake et al. 1987)||Warrego Granite, Elkedra Granite, Devils Marbles Granite, Gosse River East Syenite|||05-JAN-17
30736|Devils Suite|65338|4|Described|pp6-7, p20, p.35.|Statherian|Statherian|Tennant Region. Granites define discrete, subcircular gravity lows with little or no magnetic character. Contemporaneous with lamprophyre dykes.|c.1720 - 1700 Ma.||Includes Elkedra, Devils Marble and Kaidwalla Granites.||Granites.|
30736|Devils Suite|65455|6|Mentioned|p7|Paleoproterozoic|Paleoproterozoic|Tennant Creek region. Highly fractionated suite.|||Includes Warrego Granite.|||09-MAY-12
30736|Devils Suite|67148|5|Briefly described|Map legend.|Statherian|Statherian|Tennant Region.|1720 - 1707 Ma.|||Intrudes Ooradidgee Group.|Porphyritic and homogranular granite containing muscovite and/or biotite; minor pegmatite; aplite; greisen.|
30736|Devils Suite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Warrego, Elkedra and Devils Marble Granites, and Gosse River East Syenite.|||
30736|Devils Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p34|||Tennant Creek/Davenport area.|Emplaced 1711 +/- 11 Ma.||||Granites and lamprophyre.|
30736|Devils Suite|67352|4|Described|v, p8, p9, p17, p41, p44-45, p50, p56|Statherian|Statherian|Wyborn (1977). A late-tectonic, oxidised, extremely-fractionated I-type (granodiorite). Associated with minor vein tungsten.|c.1720-1700 Ma.||Elkedra, Devils Marbles and Warrego Granites; Gosse River East Syenite.|Intrudes into Hatches Creek Group, Ooradidgee Group, Woodenjerrie beds.|Porphyritic and even-grained muscovite-biotite or biotite granite, fine-to coarse-grained, locally xenolithic; minor pegmatite, aplite, greisen|
30736|Devils Suite|69187|5|Briefly described|p53 Fig.2, p62|Statherian|Statherian|undivided.|ca. 1720-1705 Ma||||granite|
30736|Devils Suite|69417|6|Mentioned|p2:5|Statherian|Statherian|Warramunga Province.||||||12-JUL-16
30736|Devils Suite|69424|3|Fully described|p9:2-4, 11, 14, 28-29, 39, 54-55|Paleoproterozoic|Paleoproterozoic|Wyborn et al. (1998); they included the Warrego, Devils Marbles and Elkedra Granites. Donnellan and Johnstone (2004) added the Gosse River East Syenite to the Suite. No extrusive rocks are associated with the Suite. Warramunga Province.|1711 +/- 2 Ma (Maidment et al., 2006).||Warrego, Elkedra, Devils Marbles Granites; Gosse River East Syenite.|Intrudes Warramunga, Yungkulungu and Wundirgi Formations, and Hill of Leaders Granite.|Fractionated, fluorite-bearing I-type granites showing a spectrum of peraluminous compositions. Granite, lamprophyre.|12-JUL-16
30736|Devils Suite|69425|4|Described|p10:1-3, 20-22, 24-25|||Wyborn et al. (1998). Donnellan and Johnstone (2004) added the "unnamed younger granites" of Blake et al. (1987) in the Davenport Province, including the Kaidwalla Granite. Davenport Province. No extrusive rocks are known to be associated with this Suite. Associated with W-Sn mineralisation in the Wauchope tungsten field (described).|1720-1710 Ma.||Elkedra, Devils Marbles, Warrego, Kaidwalla Granites; Gosse River East Syenite.||Highly fractionated (?late to) post-tectonic granite that is associated with minor tungsten- and tin-bearing vein mineralisation. I-type.|12-JUL-16
30736|Devils Suite|69431|6|Mentioned|p16:2|||Tennant Region.||||||12-JUL-16
30736|Devils Suite|72379|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Fraser et al (2008) suggested a temporal and genetic link between the Devils Suite and regional tungsten mineralisation, based on Ar-Ar muscovite dating of tungsten-bearing quartz veins, reporting 40Ar/39Ar plateau age of c. 1700 Ma (see p9 for details) for muscovite selvedges on the edge of wolframite-bearing quartz veins at the Bonanza, Green Diamond and Copper Show prospects in the Hatches Creek tungsten field.|c. 1710 Ma|||||
30736|Devils Suite|72380|6|Mentioned|p1,9|Paleoproterozoic|Paleoproterozoic|See also Devils Suite Granite.|||Includes Devils Marble[s] Granite.|||03-OCT-19
30736|Devils Suite|73124|6|Mentioned|p2 Fig.1|||||||||
30736|Devils Suite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.|||Warrego Granite.|||
30736|Devils Suite|73184|6|Mentioned|p193|Statherian|Statherian|Tennant Creek region. Possible source of 1.8-1.7 Ga zircons in the Grant Group.|ca 1.71 Ga||||Granites and dykes.|
30736|Devils Suite|73427|6|Mentioned|p3|Unknown|Orosirian|North Australian Craton, Tennant Region.|Younger than ca. 1810 Ma|||||
30736|Devils Suite|73460|6|Mentioned|p2|||Warramunga Province.||||Equivalent to Warrego Granite.||
30736|Devils Suite|73550|6|Mentioned|p5, p25|Statherian|Statherian|Emplacement is broadly coeval with the Davenport Event.|ca 1710 Ma|||||
30736|Devils Suite|73590|6|Mentioned|piii, p1-2, p25|Statherian|Statherian||ca 1710 Ma|||Equivalent to Warrego Granite.||
30418|Diamond Creek Volcanics|22538|6|Mentioned|Fig3 P708|||||||||
30418|Diamond Creek Volcanics|23216|4|Described|Table1p9,19,24|||||||||
30418|Diamond Creek Volcanics|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||09-AUG-06
30418|Diamond Creek Volcanics|23867|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Katherine River Group.  Originally Diamond Creek Member of Diljin Hill Formation.  Geological Province: McArthur Basin.  See also Figs. 3 and 30.||||||07-NOV-08
30418|Diamond Creek Volcanics|23937|5|Briefly described|p7-8, p25 Tb. 2|||Of the Katherine River Group.  Max. thickness: 200m.  On the KATHERINE sheet.||||||
30418|Diamond Creek Volcanics|24050|5|Briefly described|p11|||||||||
30418|Diamond Creek Volcanics|24432|5|Briefly described|p562 Fig.2|||Of Upper Katherine River Group. Felsic. Geological Province: Northern McArthur Basin.||||||
30418|Diamond Creek Volcanics|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Katherine River Group. Statherian age.||||||07-NOV-08
30418|Diamond Creek Volcanics|46678|6|Mentioned|p9|||Diff. to Table 1 entry of Diamond Creek Member. 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.||||||
30418|Diamond Creek Volcanics|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1720-1825Ma.McArthur Basin. Of Katherine River Group.  Max. thickness 230m.Vesicular and amygdaloidal mafic lava, minor tuff, volcaniclastic sandstone.||||||07-JAN-09
30418|Diamond Creek Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Katherine River Group.|||Shown as disconformably underlying Gundi Sandstone Fig 4 but overlying Gundi Sst Fig 5.|05-JUN-18
30418|Diamond Creek Volcanics|65340|6|Mentioned|p35.|||Northern McArthur Basin. Correlated with Gold Creek Volcanics in southern McArthur Basin.||||||
30418|Diamond Creek Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.||Upper Katherine River Group.||||
30418|Diamond Creek Volcanics|67564|6|Mentioned|p46.|||In Needham and Stuart-Smith (1985); formerly Diamond Creek Formation in Roberts and Plumb (1965). Not present in this sheet area.||||||
30418|Diamond Creek Volcanics|69430|4|Described|p15:3, 8-9|||NW McArthur Basin. Up to 230m thick. Subaerial extrusive and fluviatile rocks.||Katherine River Group.||Conformably overlies and interfingers with McCaw Formation. Is overlain unconformably by Gundi Sandstone.|Vesicular and amygdaloidal mafic lavas; minor tuff, volcaniclastic sandstone and coarse-grained lithic sandstone.|12-JUL-16
30418|Diamond Creek Volcanics|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by Gundi Sandstone, overlies McCaw Formation||
30418|Diamond Creek Volcanics|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
34243|Dingo Member|22651|5|Briefly described|p 184||Cambrian|Of Giles Creek Dolomite.  A thin transgressive unit at the base of the Giles Creek Dolomite.||||||09-AUG-06
34243|Dingo Member|62379|5|Briefly described|p18, 21|||Of the Giles Creek Dolostone. Siliclastic. Geological Province: Amadeus Basin.||||||
34243|Dingo Member|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 10 m.||Unit in Giles Creek Dolostone.||||
34243|Dingo Member|69673|6|Mentioned|p88|||||Giles Creek Dolostone||||
79326|Dinki Di granite|69444|5|Briefly described|p29:5|||Maidment (2005). An informal name. An unfortunate publication from a PhD thesis. Further use of this name is strongly discouraged unless it is to be formalised with a definition.|520 +/- 4 Ma (SHRIMP U-Pb zircon).||||A small body of porphyritic garnet-biotite granite. Occurs within a low-strain boudin in migmatitic biotite gneiss and amphibolite of the upper Stanovos Gneiss Member [sic].|12-JUL-16
80615|Dinkum Orthogneiss|71839|6|Mentioned|p21-22, p26|||Interpreted as the protolith to the Marshall Granite.|||||Migmatitic orthogneiss.|21-MAR-23
80615|Dinkum Orthogneiss|72717|6|Mentioned|p5, p10|||Aileron Province. Variably deformed. Variably gneissic to mylonitic. Mylonitic version has a near-identical appearance to Marshall Granite.||||||
80615|Dinkum Orthogneiss|73123|6|Mentioned|p8, p13|Statherian|Statherian||1793 +/- 4 Ma|Molyhil Suite||Intrudes Captain Morgan Metadolerite.||
80615|Dinkum Orthogneiss|73591|4|Described|piii, p2, p11-16, p18, p33|||Aileron Province. Type locality is immediately east of the Mopunga Range, ca 5 km SSE of Deep Bore. Outcrops widely but sporadically in the western Jinka and eastern Dneiper mapsheets. Moderately well-developed gneissic banding at the type area. Partial melting during high-temperature granulite facies metamorphism gave rise to the Marshall Granite. First magmatic crystallisation U-Pb zircon age of 1795 +/- 7 Ma via LA-ICP-MS. Analysed for Lu-Hf isotopes, which indicated a mixed source.|1795 +/- 7 Ma U-Pb LA-ICP-MS|Molyhil Suite||Cross-cut by Marshall Granite.|Biotite-bearing migmatitic orthogneiss.|
24608|Dirty Water Metamorphics|22810|6|Mentioned|P9|||||||||
24608|Dirty Water Metamorphics|39679|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
24608|Dirty Water Metamorphics|40493|4|Described|p6|||||||||
24608|Dirty Water Metamorphics|40808|6|Mentioned|p3|||||||||
24608|Dirty Water Metamorphics|40809|6|Mentioned|Map legend|Paleoproterozoic|Archean|Early Proterozoic to Archaean||||||07-NOV-08
24608|Dirty Water Metamorphics|41304|6|Mentioned|Map legend|Archean||||||||07-NOV-08
24608|Dirty Water Metamorphics|41305|2|Defined|p50|Paleoproterozoic|Archean|||||||07-NOV-08
24608|Dirty Water Metamorphics|41980|6|Mentioned|Fig.5 P587|||||||||
24608|Dirty Water Metamorphics|43187|5|Briefly described|p3|||||||||
24608|Dirty Water Metamorphics|43624|6|Mentioned|Table 1,p9||Archean|||||||07-NOV-08
24608|Dirty Water Metamorphics|63866|5|Briefly described|p108, p117|Archean|Archean|Central Domain, Pine Creek Orogen. ||||Overlies the Woolner Granite.||
24608|Dirty Water Metamorphics|64698|4|Described|lithinterp table|Paleoproterozoic|Neoarchean|Age ~2500Ma. Max thick 1000m. Qtz-feldsp-biotite/mica gneiss, meta-arkose and qtzite; Chlorite-qtz-calcite, graphitic mica-qtz-calcite, magnetite-chlorite-qtz, hbl-biotite and qtz-chlorite schist, banded magnetite calcite pyrite qtzite, dolomitic marble.||||||07-JAN-09
24608|Dirty Water Metamorphics|64730|5|Briefly described|p124-5 Fig. 3|Neoarchean|Neoarchean|May be correlated with Stanley Metamorphics, in which case age is between between 2675-2545 Ma (Pietsch & Stuart-Smith 1987, Lally 2002).||||Unconformably overlies Woolner Granite.||02-MAY-12
24608|Dirty Water Metamorphics|65339|6|Mentioned|p7.|||Possible correlative of Stanley Metamorphics.||||Overlies Woolner Granite.||
24608|Dirty Water Metamorphics|67355|6|Mentioned|p.6|||||||||
24608|Dirty Water Metamorphics|67564|5|Briefly described|p9 Fig.4.|Archean|Archean|Correlative of Stanley Metamorphics.|||||Schist, gneiss, banded ironstone, marble.|
24608|Dirty Water Metamorphics|69419|5|Briefly described|p4:4-5|Neoarchean|Neoarchean|No surface exposure; known from drillhole data (40-120m depth). Age is uncertain; this age range is from stratigraphic relationships and correlation.|Deposited between 2674 Ma and 2520 Ma.|||Unconformably overlies Woolner Granite. Correlated with Stanley Metamorphics. Is unconformably overlain by Mount Partridge Group.|Gneisses, meta-arkose and quartzite, schists, dolomitic marble.|12-JUL-16
24608|Dirty Water Metamorphics|69420|6|Mentioned|p5:4|Archean|Archean|See also Dirtywater Metamorphics (5:6).||||||12-JUL-16
28261|Djagamara Formation|22804|6|Mentioned|p452|||Geological Province - Ngalia Basin.  Probable Ordovician Age.||||||
28261|Djagamara Formation|23858|5|Briefly described|p916|||Overlain by Kerridy Sandstone. Geological Province: Ngalia Basin. Max. thickness: 300 m.||||||09-AUG-06
28261|Djagamara Formation|24064|4|Described|p227|Ordovician|Ordovician|Geological Province: Ngalia Basin. Maximum thicknes: >320m.||||||
28261|Djagamara Formation|30258|6|Mentioned|p98|||Post Lower Cambrian to pre-Carboniferous See also p99-100,Fig.2.||||||09-AUG-06
28261|Djagamara Formation|31454|6|Mentioned|Fig.2|||||||||
28261|Djagamara Formation|33192|6|Mentioned|p20|||||||||
28261|Djagamara Formation|33757|3|Fully described|p9|||Table 2. Minimum age||||||
28261|Djagamara Formation|33760|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
28261|Djagamara Formation|33761|6|Mentioned|p145|||See also p150. Ord.||||||09-AUG-06
28261|Djagamara Formation|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
28261|Djagamara Formation|37537|5|Briefly described|Map legend|Ordovician|Ordovician|Grey and white, medium, thick bedded to laminated, siliceous, clay pellets, glauconitic sandstone; green siltstone. Geological Province: Ngalia Basin.||||||31-MAR-06
28261|Djagamara Formation|37928|6|Mentioned|p519|||||||||
28261|Djagamara Formation|38945|6|Mentioned|Fig.1|||||||||
28261|Djagamara Formation|39565|6|Mentioned|p33|||See also p42.||||||09-AUG-06
28261|Djagamara Formation|40136|5|Briefly described|p23|||||||||
28261|Djagamara Formation|40906|6|Mentioned|Fig.11|||||||||
28261|Djagamara Formation|41717|6|Mentioned|Fig.19|||||||||
28261|Djagamara Formation|42059|5|Briefly described|Fig.2|||See also p133.||||||09-AUG-06
28261|Djagamara Formation|42504|5|Briefly described|p83|||||||||
28261|Djagamara Formation|43275|5|Briefly described|Map Legend||Ordovician|||||||
28261|Djagamara Formation|43631|3|Fully described|p25,26||Ordovician|||||||
28261|Djagamara Formation|43749|6|Mentioned|Fig.1,p6||Ordovician|||||||
28261|Djagamara Formation|44158|4|Described|p33 Table.2|Ordovician|Ordovician|Of Ngalia Basin.||||||09-AUG-06
28261|Djagamara Formation|45155|2|Defined|p33|Ordovician|Ordovician|Prob. Ordovician||||||
28261|Djagamara Formation|61385|5|Briefly described|Map legend|Ordovician|Ordovician|White to grey sandstone with abundant mudstone pellets, minor glauconitic sandstone, minor green to dark grey mudstone; rare trace fossils. Geological Province: Ngalia Basin.||||||20-OCT-05
28261|Djagamara Formation|64068|6|Mentioned|p72, 73, 75, 77, 226|||Ngalia basin. May correlate with Ninmaroo Formation, Tomahawk Formation, Kelly Creek Formation, possibly Coolibah Formation, Nora Formation, Carlo Sandstone, Georgina Basin.||||||
28261|Djagamara Formation|64334|5|Briefly described|p47|||Central Ngalia Basin.||||Likely correlative of the Larapinta Group (Amadeus Basin).|A relatively thin (<300m) sandy succession; restricted or marginal marine. Trace fossils common.|
28261|Djagamara Formation|65232|5|Briefly described|p70|Ordovician|Ordovician|Angular unconformity with overlying Kerridy Sandstone. Quartz sandstone. Geol. Prov: Ngalia Basin.||||||09-FEB-10
28261|Djagamara Formation|65329|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Bloodwood Formation, older than Kerridy Sandstone. White to grey sandstone, abundant mud pellets, minor glauconitic sandstone and green to dark grey mudstone; rare trace fossils ||||||
28261|Djagamara Formation|65330|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Bloodwood Formation, older than Kerridy Sandstone. White to grey sandstone, abundant mud pellets, minor glauconitic sandstone and green to dark grey mudstone; rare trace fossils ||||||
28261|Djagamara Formation|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 141 m.||||Overlies Mount Doreen Formation. Is overlain by Kerridy Sandstone.|Siliceous sandstone interbedded with green shale.|
28261|Djagamara Formation|67565|6|Mentioned|p5 Fig.3.|||Ngalia Basin.||||||
28261|Djagamara Formation|67872|5|Briefly described|p13, p15|Ordovician|Ordovician|Ngalia Basin. Constitutes the M5 mega-sequence of Lindsay (2002). Associated with Delamerian Orogeny.|447 Ma.|||||
28261|Djagamara Formation|69437|6|Mentioned|p22:10|Ordovician|Furongian|Ngalia Basin. Deposited sometime after the Bloodwood Movement. Age range is shown as approximate: post-Bloodwood Formation, and "may be later Ordovician" [than Warendian].||||||12-JUL-16
28261|Djagamara Formation|69438|6|Mentioned|p23:46|Ordovician|Ordovician|Ngalia Basin.||||||12-JUL-16
28261|Djagamara Formation|69439|4|Described|p24:2-4, 6, 8, 10-11, 13-14,17-18,20-21|Ordovician|Ordovician|Ngalia Basin. Discontinuous outcrops for c.120 km. Up to 320m thick, thinning to the S. Possibly correlated with Pacoota Sandstone (by trace fossils); also with Carmichael Sandstone (Amadeus Basin) if this age is correct. Possible hydrocarbon source rock whose potential is unknown. Contains potential reservoirs.|c.447 Ma glauconite (Cooper et al., 1971).|||Unconformably overlies Mount Doreen, Bloodwood Formations; Walbiri Dolostone; Yuendumu Sandstone. Is faulted against Bloodwood Formation. Underlies Kerridy Sandstone unconformably or ?disconformably.|Clean, white to grey well-sorted sandstone, commonly highly silicified and glauconitic, that varies from thinly to thickly bedded; local thick interbeds of green and dark grey siltstone near the middle of the Formation.|12-JUL-16
28261|Djagamara Formation|69443|6|Mentioned|p28:26-27|||Ngalia Basin. Poorly dated.||||Possibly correlated with Cockroach and Toko Groups.||12-JUL-16
28261|Djagamara Formation|69673|5|Briefly described|p107 fig 85, p108, p110|||Up to 320m thick. Some source rock potential.||||Overlies Bloodwood Formation, overlain by Kerridy Sandstone|Thinly to thickly bedded sandstone with minor interbeds of silstone.|
28261|Djagamara Formation|72516|6|Mentioned|p94|Ordovician|Cambrian|Ngalia Basin.||||Possibly equivalent to the Tomahawk Formation.||09-JUN-21
24248|Don Creek Sandstone|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Carrara Range Group.  ||||||07-NOV-08
24248|Don Creek Sandstone|38237|6|Mentioned|Fig.3|||||||||
24248|Don Creek Sandstone|39338|6|Mentioned|Fig.1|||||||||
24248|Don Creek Sandstone|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Carrara Range Group.  Massive, medium to coarse and gritty quartz sandstone; scattered quartz pebbles and thin congomeratic lenses.  Conformably overlain by Mitchiebo Volcanics; unconformably overlies the Murphy Metamorphics.||||||10-JAN-05
24248|Don Creek Sandstone|39497|4|Described|p7|||||||||
24248|Don Creek Sandstone|39925|6|Mentioned|p335|||||||||
24248|Don Creek Sandstone|45166|5|Briefly described|p27|||||||||
24248|Don Creek Sandstone|49018|2|Defined|p4|Carpentarian|Carpentarian|||||||
24248|Don Creek Sandstone|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. White to pale maroon, silicified to friable, medium to coarse grained, locally pebbly lithic to quartzose sandstone.||||||
24248|Don Creek Sandstone|65337|4|Described|p9 Fig.5, p10 Table 3. |Paleoproterozoic|Paleoproterozoic|Southeast MOUNT DRUMMOND area. 400 - 500 m thickness of braided fluvial deposits.||Basal unit in Carrara Range Group.||Unconformably overlies Murphy Metamorphics. Is overlain by Mitchiebo Volcanics.|White to pale maroon, silicified to friable, medium- to coarse-grained, locally pebbly lithic to quartzose sandstone.|
24248|Don Creek Sandstone|69433|4|Described|p18:2, 5-7|Statherian|Statherian|Southern succession, Lawn Hill Platform. 400-500m thick. Probably braided fluvial deposits.||Carrara Range Group.||Unconformably overlies Murphy Metamorphics. Is overlain conformably by Mitchiebo Volcanics. Correlate of Westmoreland Conglomerate, Yiyintyi Sandstone and possibly Wire Creek Sandstone.|Silicified to friable, lithic to quartzic sandstone with pebbles or cobbles and rare conglomerate. Bedding is thick and trough cross-bedded; beds typically coarsen upwards. Cyclicity on a 10-50m scale is evident.|12-JUL-16
24248|Don Creek Sandstone|69673|4|Described|p52 fig 42,|||||Carrara Range Group|||Lithic to quartzose sandstone with pebbles or cobbles and rare conglomerate.|
24248|Don Creek Sandstone|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||Shown as partially overlying Whitworth Quartzite and underlies Mitchiebo Volcanics.||
24248|Don Creek Sandstone|72527|6|Mentioned|p7 Fig.1.4.|Paleoproterozoic|Paleoproterozoic|||Base of Carrara Range Group.||Underlies Michiebo Volcanics.||
24248|Don Creek Sandstone|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||Shown as overlying Whitworth Quartzite  and underlies Mitchiebo Volcanics.||
24248|Don Creek Sandstone|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Overlain by Mitchiebo Volcanics.||
24248|Don Creek Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Calvert Superbasin.||Carrara Range Group||Overlain by Mitchlebo Volcanics.||
40572|Doom Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Dungaminnie Formation.|||
40572|Doom Supersequence|63114|5|Briefly described|p1253 Fig.2, p1260.|||Isa superbasin.|||Includes the Lawn Hill Formation|||
40572|Doom Supersequence|63866|5|Briefly described|p53-p54|Calymmian|Calymmian|Isa Superbasin.|c. 1585 Ma||Includes the Dungaminine Formation|||
40572|Doom Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Calymmian|Calymmian|Lawn Hill Platform. Shallow water environments.|Max. age c.1580 Ma.|||Is overlain ?unconformably by Roper Group.|Feldspathic siliciclastics, coarsening upward.|
40572|Doom Supersequence|65337|6|Mentioned|p34.|||No evidence of this in the MOUNT DRUMMOND area.||||||
40572|Doom Supersequence|66843|5|Briefly described|p38 Fig.10, p39|||Said to be "informally" named. Depositional cycles and lithofacies described.||||||
40572|Doom Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40572|Doom Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Isa Superbasin. Of Nathan Group, NT (p9). Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Camooweal - Murphy Domain, Mount Isa Inlier.|~1590-1575 Ma.|?Fickling Group||Overlies Wide Supersequence.|Brown and green shale, thin bedded siltstone and fine sandstone|
40572|Doom Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes the Lawn Hill Formation.||||||
40572|Doom Supersequence|69591|5|Briefly described|p27, p43, p47|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the upper part of the Lawn Hill Formation.||||Overlies Wide Supersequence. Is equated with upper part of Doomadgee Formation.||
40572|Doom Supersequence|70897|5|Briefly described|p39-40, Fig.1.7.2-4|||Maintains relatively tabular architecture throughout deposition. Age inferred from dating of detrital zircons in Constance Formation, South Nicholson Group.|1591 +/- 10 Ma.|||Overlies Wide Supersequence.||28-NOV-17
40572|Doom Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation.||||||
40572|Doom Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||||Brown and Green shale and flaggy, thin-bedded siltstone and fine-grained sandstone.|
40572|Doom Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Mesoproterozoic|Paleoproterozic|Both Gun and Doom Supersequences are the subject of further investigation for their Oil or Condensate potential.||||Overlies Wide Supersequence.||
40572|Doom Supersequence|73144|4|Described|p: 8-9, 12-13, 19-20, 23, 25, 40, 42-43|Calymmian|Calymmian|Sequence Stratigraphy. Isa Superbasin. Contains five third order sequences [see article for more detail on third order sequences]. Deposited via prograding wedge and fan, mid-shelf turbidites or mid-inner shelf (Krassay et al., 2000). Poorly preserved in [some] areas due to truncation at the base of the South Nicholson Group. Contemporaneous deposition with the Doom Event, at ~1575 Ma associated with north-south compression.|1575-1585 Ma|||Includes a portion of the Lawn Hill Formation.|Feldspathic and lithic sandstone, carbonaceous siltstone, dolostone, shale, carbonaceous/silty shale, black mudstone and black limestone.|
80199|Double Dam Granite|73591|5|Briefly described|piii, p11, p16-19|||Aileron Province. Outcrops sporadically in the eastern Dneiper mapsheet. Geochronology was unsuccessful due to entirely discordant results.||Molyhil Suite|||Includes biotite granite.|
30405|Douglas Granite|23714|4|Described|p25|||See also page 19 Table 4. Previously mapped as Cullen Granite. Geological Province: Cullen Batholith.||||||
30405|Douglas Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
30405|Douglas Granite|43140|3|Fully described|p18||Paleoproterozoic|Of Cullen Batholith. Prev incl in Cullen Granite by Noakes 1949, Malone 1962, Walpole et al 1968.||||||07-NOV-08
30405|Douglas Granite|45022|3|Fully described|p.137||Adelaidean|Cullen Granite.||||||07-JAN-09
30405|Douglas Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Of Cullen Supersuite. Light grey coarse porphyritic biotite leucogranite. Intrudes McMinns Bluff Granite.||||||07-JAN-09
30405|Douglas Granite|69420|5|Briefly described|p5:17-19|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Burnside Suite.|||Fine- to medium-grained porphyritic granite. I-type.|12-JUL-16
30405|Douglas Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Burnside Suite.|||Light grey, fine-to medium-grained, porphyritic, felsic biotite granite.|
27043|Driffield Granite|23216|5|Briefly described|Table1p9,15,17|||||||||
27043|Driffield Granite|23714|4|Described|p25|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
27043|Driffield Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
27043|Driffield Granite|24197|5|Briefly described|p24, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. One of a group of concentrically zoned transitional granite and leucogranite dominated plutons. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
27043|Driffield Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27043|Driffield Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Pink coarse porphyritic biotite leucogranite. Pink coarse equigranular biotite leucogranite.||||||07-NOV-08
27043|Driffield Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27043|Driffield Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27043|Driffield Granite|41125|6|Mentioned|p55|||||||||
27043|Driffield Granite|41311|4|Described|p18|||||||||
27043|Driffield Granite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27043|Driffield Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27043|Driffield Granite|43140|3|Fully described|p18||Paleoproterozoic|Of Cullen Batholith. Previously mapped as part of Cullen Granite by Walpole et al 1968.||||||07-NOV-08
27043|Driffield Granite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
27043|Driffield Granite|43624|6|Mentioned|p14|||Geological Province: Cullen Batholith.||||||
27043|Driffield Granite|43832|3|Fully described|Table8p39;46,50,63||Paleoproterozoic|||||||07-NOV-08
27043|Driffield 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
27043|Driffield Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Pink medium to coarse biotite leucogranite with minor grey coarse porphyritic biotite granite.  Age: 1825-1820Ma.||||||13-JAN-05
27043|Driffield Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1825Ma. I-type. Of Cullen Supersuite. Grey coarse porphyritic biotite granite; Pink medium to coarse biotite leucogranite. Intrudes Burrell Creek Formation.||||||
27043|Driffield Granite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
27043|Driffield Granite|67564|4|Described|p7 Table 2, p33 Fig.19, p35.|Paleoproterozoic|Paleoproterozoic|I-type. Pluton within Cullen Batholith, Pine Creek Orogen. 180 km2 in area.|1825 - 1820 Ma.|Unit in Cullen Supersuite.||Intrudes McCarthys Granite, Fingerpost Granodiorite and Burrell Creek Formation.|A small core of coarse, porphyritic hornblende-biotite granite, and an envelope of pink, medium to coarse, biotite leucogranite.|
27043|Driffield Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Shoobridge Suite.|||Marginal phase of fine- to medium-grained granite. Coarse-grained core with K-feldspar megacrysts. I-type.|12-JUL-16
27043|Driffield Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Shoobridge Suite.|||Coarse-grained, pink, equigranular to porphyritic biotite leucogranite; medium- to coarse-grained, grey or pink-green, porphyritic hornblende-biotite granite.|
38037|Drummond Formation|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the McNamara Group. White to brown, medium to thick bedded, fine to medium sublithic to quartzose sandstone with scattered coarse and granule laminae.||||||
38037|Drummond Formation|65337|3|Fully described|p9 Fig.5, pp21-23.|Paleoproterozoic|Paleoproterozoic|New name. 350 - 600 m thick. Shallow marine, peritidal mud- and carbonate-flats, and fluvial environments. Forms many of the higher ridges and intervening valleys in Carrara Range; low hills in northern outcrops. Equivalent to Gun Supersequence.|c.1660 Ma.|Unit in McNamara Group.||Locally unconformably overlies Surprise Creek Formation. Is overlain by Brumby Formation or unconformably by Bullrush Conglomerate.|Thin polymict conglomerate overlain by thin- to medium-bedded, fine-grained lithic sandstone, laminated siltstone, red beds of brown lithic dolomitic sandstone and chertified dolostone.|
38037|Drummond Formation|69433|4|Described|p18:2, 6, 9|Statherian|Statherian|Rawlings et al. (2008); formerly part of the (now obsolete) Musselbrook Formation. Southern succession, Lawn Hill Platform. 350-600m thick. Also appears as Drummond Sandstone on 18:6. Contains a variety of distinctive sedimentological features (listed).||McNamara Group.||Unconformably overlies Surprise Creek Formation. Is overlain by Brumby Formation conformably, and by Bullrush Conglomerate unconformably.|Localised basal polymictic conglomerate; fine lithic sandstone; laminated siltstone; red beds of brown, lithic dolomitic sandstone and chertified dolostone; pyritic coarse sandstone; sublithic to quartzic sandstone; minor chert, laminated claystone.|12-JUL-16
38037|Drummond Formation|69673|4|Described|p52 fig 42, p53|||Up to 600m thick.||McNamara Group|||Conglomerate, sandstone, dolomitic sandstone, chertified dolostone, minor chert, claystone, siltstone and stromatolitic chert.|
38037|Drummond Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the central part of the South Nicholson Basin.||McNamara Group, NT.||Underlies Brumby Formation.||
38037|Drummond Formation|72527|4|Described|p1, 8, p91-104, p105, 119, 193, 194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Two samples dated. Sandstone, 1715+/-30 Ma;  sandstone 1792+/-13 Ma max. dep ages. Detrital zircon signature similar to underlying Surprise Creek Formation and Gator Sandstone. Overlying Brumby Fomation significantly different provenance. Interbedded sandstone-siltstone layers are typical of this unit. Deposited in a shallow marine-intertidal to fluvial depositional environment. Age given as MDA for GA samples (2785617, 2786178).|1715+/-30 Ma max depositional age|Base of McNamara Group.||Unconformably overlies Surprise Creek Formation and conformably underlies Brumby Formation. Considered to be laterally equivalent to Paradise Creek Formation|Dominated by lithic to quartzose sandstones, minor chert, claystone, siltstone and stromatolitic dolomitic rocks.|
38037|Drummond Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Shown as being located in the Northern Territory part of the McNamara Group. Shown as equivalent to Paradise Creek Formation.||McNamara Group||Underlies Brumby Formation and is partially and laterally equivalent to Fish River Formation.||
38037|Drummond Formation|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||McNamara Group||Unconformably underlain by Surprise Creek Formation. Overlain by Brumby Formation.||
38037|Drummond Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Calvert Superbasin.||Carrara Range Group||Unconformably underlain by Surprise Creek Formation*.||
38037|Drummond Formation|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
42397|Du Faur Suite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic| Age: >1770Ma.  In the Arunta region.||||||07-NOV-08
42397|Du Faur Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||gabbronorite, dolerite|
42397|Du Faur Suite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province.|||||Dolerite and gabbronorite, metamorphosed to mafic amphibolite; pyroxenite, metamorphosed to amphibolite.|09-SEP-19
79101|Dufaur Dolerite|68832|5|Briefly described|p23|||||||Intrudes Lander Rock beds.||
80616|Duke gabbro|71795|6|Mentioned|p36 tbl 1, p37, p40, p43|||Gabbro at Duke (zinc) Prospect, Rudall Province.|831+/-2.2 U/Pb SHRIMP Magmatic crystallisation.||||this sample: Leucocratic phase within gabbroic intrusion.|12-NOV-18
23567|Eagle Hawk Sandstone|13194|6|Mentioned|p395 Tb. 4-16|||Of Ord Basin.||||||
23567|Eagle Hawk Sandstone|14019|3|Fully described|p24|Middle Cambrian|Middle Cambrian|Of the Elder Subgroup. Comprises fine to medium sandstone, minor siltstone and mudstone. Conformably overlies the Panton Formation; conformably under the Overland Sandstone. Max. thickness type section: 210m. Geol. Prov: Ord Basin.||||||10-MAY-05
23567|Eagle Hawk Sandstone|40993|6|Mentioned|Fig.1|||||||||
23567|Eagle Hawk Sandstone|41840|2|Defined|p43||Middle Cambrian|New name. Replaces Hudson Formation of Sweet 1974.||||||
23567|Eagle Hawk Sandstone|41864|3|Fully described|p24|||Unit called Hudson Formation where it crops out in NT.||||||15-DEC-08
23567|Eagle Hawk Sandstone|41865|5|Briefly described|Map legend||Middle Cambrian|||||||
23567|Eagle Hawk Sandstone|41866|5|Briefly described|Map legend|Late Cambrian||||||||
23567|Eagle Hawk Sandstone|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
23567|Eagle Hawk Sandstone|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
23567|Eagle Hawk Sandstone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
23567|Eagle Hawk Sandstone|60419|4|Described|p1, 11|Middle Cambrian|Middle Cambrian|Of Elder Subgroup. Conformably overlies Panton Formation. Overlain by Overland Sandstone. Thickness: 210 m. Intertidal. Contains ichnofossils. Geological Province: Ord Basin.||||||
23567|Eagle Hawk Sandstone|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup (Goose Hole Group). Fine grained, micaceous, feldspathic snadstone; minor siltstone. Geological Province: Ord Basin.||||||05-NOV-04
23567|Eagle Hawk Sandstone|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Of the Elder Subgroup.  Fine to medium micaceous and feldspathic sandstone; minor siltstone and mudstone.   Conformably overlies Panton Formation; conformably overlain by the Overland Sandstone.  Geological Province: Ord Basin.||||||24-NOV-04
23567|Eagle Hawk Sandstone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
23567|Eagle Hawk Sandstone|67860|4|Described|p417,421,422 Figs.4.85-87; p419 Tb.4-18|Late Cambrian|Middle Cambrian|75-210 m thick. Type section details given. Contains trilobite trails.||Elder Subgroup||Conformably overlies Panton Formation. Is overlain conformably by Overland Sandstone. Equivalent to Hart Spring Sandstone (Bonaparte Basin).|Red micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Elder Subgroup|||Red micaceous feldspathic sandstone; minor siltstone|31-JUL-15
23567|Eagle Hawk Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Furongian|See also 500k_geologyp08_lut.csv. ||Elder Subgroup|||Red Micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Ord Basin, Centralian B Superbasin. Sequence 2. Peritidal deposits.||||Overlies Panton Formation. Is overlain by Overland Sandstone.||12-JUL-16
23567|Eagle Hawk Sandstone|69446|6|Mentioned|p31:4|||Ord Basin.||||||12-JUL-16
23567|Eagle Hawk Sandstone|69447|6|Mentioned|p32:2|||Ord Basin.||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
23567|Eagle Hawk Sandstone|69448|3|Fully described|p33:2-4, 6-8|Middle Cambrian|Middle Cambrian|Mory and Beere (1985). Ord Basin. Generally 75-80m thick; maximum of 210m thick in the type section in northeastern DIXON RANGE map area. Intertidal sand- and mudflat deposits. Broadly correlated with Jinduckin Formation-Oolloo Dolostone interval (Daly Basin); Point Wakefield beds (Wiso Basin); Anthony Lagoon Formation/Wonarah Formation/Ranken Limestone/Camooweal Dolostone succession (Georgina Basin).||Elder Subgroup.||Conformably and gradationally overlies Panton Formation. Is overlain conformably and gradationally by Overland Sandstone. Correlated with Hart Spring Sandstone (Bonaparte Basin).|Fine to medium feldspathic to micaceous, red-brown to maroon sandstone; minor siltstone, mudstone; trough cross-beds, ripple marks, parallel lamination, mud pebble and cobble moulds, decimetre-scale channels, dessication cracks, arthropod tracks.|12-JUL-16
23567|Eagle Hawk Sandstone|69634|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|497-485.4 Ma (Biostrat)|Unit of Elder Subgroup.|||Red micaceous feldspathic sandstone; minor siltstone|
23567|Eagle Hawk Sandstone|69673|5|Briefly described|p194|||210m thick.||Elder Subgroup||Overlies Panton Formation, overlain by Overland Sandstone|Feldspathic to micaceous sandstones with minor siltstone and mudstone.|
23567|Eagle Hawk Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-497 Ma|Elder Subgroup|||Red micaceous feldspathic sandstone; minor siltstone.|
23567|Eagle Hawk Sandstone|71267|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|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.|497-485.4 Ma (biostrat)|Unit of Elder Subgroup.|||Fine to medium micaceous and feldspathic sandstone; minor siltstone and mudstone.|
23567|Eagle Hawk Sandstone|71800|4|Described|p25-p27|Late Cambrian|Middle Cambrian|Ord Basin. Deposited on an intertidal sand flat.||Elder Subgroup||Conformably (gradationally) overlies the Panton Formation. Overlain by the Overland Sandstone.|Red micaceous arkose.|
23567|Eagle Hawk Sandstone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Panton Formation, underlies the Overland Sandstone.||
75905|Eaglebeak Amphibolite|69917|5|Briefly described|p130-132, 1|Orosirian|Orosirian|Eastern Arunta Region, Aileron Province. LA-ICPMS zircon dating, Hf analytical data. Maximum crystallisation age of 1865+/-24 Ma is interpreted to be the age of emplacement for this rock, which makes it the oldest known basement rock in the Arunta Region.|1865+/-24Ma max cryst ||||Amphibolite, also described as metagabbro.|
75905|Eaglebeak Amphibolite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1865+/-24 Ma (U-Pb zircon LA-ICPMS).||||Metagabbro.|
75905|Eaglebeak Amphibolite|71621|5|Briefly described|p25-p26|||Age interpreted as the magmatic crystallisation age and derived from Beyer et al, 2013.|1865 +/- 24 Ma|||||
75905|Eaglebeak Amphibolite|73591|6|Mentioned|p27|Orosirian|Orosirian||ca 1857 Ma|||||
33173|Echo Sandstone|22538|2|Defined|App1 p722||Statherian|Supersedes Masterton Formation""||||||13-DEC-17
33173|Echo Sandstone|23395|5|Briefly described|p401|||Geological Province: McArthur Basin.||||||15-AUG-06
33173|Echo Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
33173|Echo Sandstone|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Includes the Pungalina Member. Pink, medium grained, locally pebbly, lithic to quartzose sandstone and minor conglomerate with large trough and planar cross-beds.||||||07-NOV-08
33173|Echo Sandstone|63112|6|Mentioned|p1191-1192, p1194, p1198, p1201, p1205|||Calvert Superbasin. Age approximated from Fig.2. <10 to >100 m thick.|c.1710-1705 Ma.|Unit in Big Supersequence.|Includes Pungalina Member.||Mudstone and fine sandstones overlain by lithic and quartzose sandstones and minor pebbly sandstones.|
33173|Echo Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Of the Tawallah Group.||||
33173|Echo Sandstone|65228|5|Briefly described|p22, p23, Figs.10, 12.|||McArthur Basin. Defined by Rawlings (1999). Part of the Big Supersequence. See also "Echo Sandstone" in fig 02.|||Includes basal Pungalina Member.|Correlated with Warramana and Burash Sandstones.||13-DEC-17
33173|Echo Sandstone|65232|6|Mentioned|App. 2|||||||||09-FEB-10
33173|Echo Sandstone|65340|3|Fully described|p12 Fig.6, pp25-26, pp47-57. |||Restricted to Wearyan Shelf. Partly equivalent to the lithologically similar Warramana Sandstone. Part-correlated with Tanumbirini Rhyolite. Outcrops assigned in this study were formerly assigned to Masterton Sandstone of lower McArthur Group by Jackson et al. (1987) and Ahmad and Wygralak (1989); because Masterton Sandstone is recognised only in Batten Fault Zone, Rawlings (1999) defined the new formation (Echo Sandstone) to encompass strata that overlie Gold Creek Volcanics and underlie Karns Dolomite or McArthur Group. Ephemeral restricted marine, braided fluviatile environments. Mineralogy, microstructure, depositional conditions and fabric are discussed in detail. |1725 - 1710 Ma.|Unit in Tawallah Group.|Includes Pungalina Member.|Disconformably overlies Gold Creek Volcanics. Overlies Hobblechain Rhyolite. Is unconformably overlain by McArthur Group and Bukalara Sandstone, and by Mallapunyah Formation.|Thin basal cobble conglomerate; lower dolomitic-lithic sandstone with local pebbles, overlain by interbedded lithic sandstone and mudstone; upper pink coarse +/- pebbly lithic sandstone with large planar and trough cross-beds.|
33173|Echo Sandstone|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
33173|Echo Sandstone|69430|4|Described|p15:3, 10, 12-13, 31, 46|Paleoproterozoic|Paleoproterozoic|Formerly part of Masterton Sandstone. SE McArthur Basin. 265-365m thick. Ephemeral restricted marine, braided fluviatile deposits. Is stated to be the parent for the Pungalina Member, but their relative positions as described in pages 15:3 and 15:10 indicate a connection with the Warramana Sandstone. Possible equivalent to Parsons Range Group. Hosts manganese and sedimentary phosphate occurrences.||Tawallah Group.||Overlies Pungalina Member conformably and Gold Creek Volcanics disconformably. Is overlain unconformably by McArthur Group. Part-equivalent to Warramana Sandstone.|Dolomitic-lithic sandstone, lithic sandstone and mudstone, pebbly lithic sandstone, lithic to quartzic sandstone and minor conglomerate.|12-JUL-16
33173|Echo Sandstone|69673|6|Mentioned|p16 fig 13|||Coarse clastic sedimentary rock.||Tawallah Group||Overlies Warramana Sandstone, Wollogorang Formation||
33173|Echo Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Tawallah Group.||||
33173|Echo Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the Southeastern McArthur Basin.||Tawallah Group||Overlies Warramana Sandstone and is shown as unconformably underlying Karns Dolostone.||
33173|Echo Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||Tawallah Group||Underlain by Warramana Sandstone. Partly equivalent to Burash Sandstone, Nyanantu Formation and Tanumbirini Rhyolite.||
33173|Echo Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Southeastern McArthur Basin. Age controlled by older Hobblechain Rhyolite (1725+/-2 Ma).||Tawallah Group||Overlies Warramana Sandstone ? and laterally equivalent to Nyanantu Formation.||
33173|Echo Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group|Pungalina Member(?)|Partly underlain by Hobblechain Rhyolite and Gold Creek Volcanics.||
33173|Echo Sandstone|73083|6|Mentioned|p38, p40|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Virtually non-magnetic.||||Underlain by Wollogorang Formation.||
33173|Echo Sandstone|73412|5|Briefly described|p4|||Southern McArthur Basin.||Tawallah Group.||Overlies Warramana Sandstone. Is overlain unconformably by Masterton Sandstone (McArthur Group).||
26302|Edmirringee Volcanics|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.||||||07-NOV-08
26302|Edmirringee Volcanics|24172|5|Briefly described|p66, Tb. 9|||Of Ooradidgee Subgroup (Hatches Creek Group). Conformably overlain by Kurinelli sandstone. Geological Province: Tennant Creek Inlier.  Basaltic lava; felsic lava. Interfingers with Epenarra Volcanics.||||||15-AUG-06
26302|Edmirringee Volcanics|39624|5|Briefly described|Table 1|||||||||
26302|Edmirringee Volcanics|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Amygdaloidal basalt.||||||10-JAN-05
26302|Edmirringee Volcanics|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26302|Edmirringee Volcanics|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26302|Edmirringee Volcanics|41204|4|Described|Table 1|||||||||
26302|Edmirringee Volcanics|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup. Basalt lava, basaltic volcaniclastic rocks; minor felsic volcanics.||||||09-APR-06
26302|Edmirringee Volcanics|41310|4|Described|Table 1|||Mention p6.||||||15-AUG-06
26302|Edmirringee Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
26302|Edmirringee Volcanics|41970|6|Mentioned|Fig.3 P333|||||||||
26302|Edmirringee Volcanics|42643|4|Described|Table 1, p9, p5|||Of Ooradidgee Subgroup.||||||23-FEB-23
26302|Edmirringee Volcanics|42770|5|Briefly described|p13|||see also Table 2, of Hatches Creek Group.||||||
26302|Edmirringee Volcanics|43223|5|Briefly described|Map Legend||Proterozoic|Of Hatches Creek Group.||||||15-AUG-06
26302|Edmirringee Volcanics|43224|5|Briefly described|Map legend||Proterozoic|Of Hatches Creek Group.||||||15-AUG-06
26302|Edmirringee Volcanics|43568|6|Mentioned|p502|||||||||
26302|Edmirringee Volcanics|43802|6|Mentioned|Table 1,p80|||||||||
26302|Edmirringee Volcanics|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||15-AUG-06
26302|Edmirringee Volcanics|49033|2|Defined|p7|Proterozoic|Proterozoic|Parts of Ooradidgee Subgroup (Hatches Creek Group).||||||15-AUG-06
26302|Edmirringee Volcanics|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||
26302|Edmirringee Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group.  Basaltic lava; minor volcaniclastic arenite and felsic lava.  In the Tennant Creek region.||||||07-NOV-08
26302|Edmirringee Volcanics|65209|6|Mentioned|p35 Fig.1, p36, p37|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
26302|Edmirringee Volcanics|65338|5|Briefly described|p19.|||||Unit in Ooradidgee Group.|||Basaltic volcanic rocks.|
26302|Edmirringee Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Felsic lava and pyroclastic rocks including ignimbrite and lapilli tuff; volcaniclastic arenite and conglomerate; minor altered mafic lava.|
26302|Edmirringee Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area. Appears [indistinctly] as Edmiringee Volcanics.||Ooradidgee Group.||||
26302|Edmirringee Volcanics|68518|4|Described|p10 Tb.1, p11|Proterozoic|Proterozoic|Mineral deposit: galena-bearing quartz veins in basalt at Silver Valley prospects in NW; no recorded production. Host small silver-lead deposits at Silver Valley. Thickness: 2000+ m.||Ooradidgee Subgroup||Overlain conformably by Kurinelli Sandstone. Base not seen.|Recessive amygdaloidal to massive basalt lava; minor andesitic and felsic lava, minor tuff; may include some dolerite sills.|30-MAY-16
26302|Edmirringee Volcanics|69187|6|Mentioned|p53 Fig.2|||||||||
26302|Edmirringee Volcanics|69424|4|Described|p9:3-5, 15, 18, 23, 25-26, 28, 54, 56|Paleoproterozoic|Paleoproterozoic|Warramunga and Davenport Provinces. Up to 2500m thick. Erupted from one volcanic centre (Edmirringee Rockhole) in Warramunga Province and three (in the Kurindi Anticline, Skinner Anticline and Murray Downs Dome) in Davenport Province. Predominantly subaerial; possible local pillow lavas. Hosts Au-bearing quartz veins, and several minor Cu (+/- Au) occurrences in the Whistelduck area.|1840-1820 Ma.|Ooradidgee Group.||Conformably overlies and interfingers with Epenarra Volcanics and Kurinelli Sandstone. Is overlain conformably by Kurinelli and Unimbra Sandstones (the latter also disconformably).|Basalt, predominantly massive/vesicular/amygdaloidal, non-porphyritic pahoehoe and minor aa lava; mugearite locally near base of succession; minor felsic lava and tuff (Epenarra Volcanics equivalent) and sandstone (Kurinelli Sandstone equivalent).|12-JUL-16
26302|Edmirringee Volcanics|69425|4|Described|p10:3-8, 13, 22, 25|||Crops out in the Murray Downs Dome and in the Skinner and Kurundi Anticlines. Erupted from three volcanic centres in Davenport Province and a fourth in Warramunga Province. Mainly subaerial; possible pillow lavas locally. 0 - up to 2500m thick. Local mugearite, tuff and volcaniclastic sedimentary rocks (explosive tephra). Metamorphosed to sub-greenschist facies (has prehnite- and pumpellyite-bearing assemblages). Hosts the Silver Valley Pb (Ag,Cu)  prospect in quartz-filled shear zones.||Ooradidgee Group.||Conformably overlies and interfingers with Epenarra Volcanics and Kurinelli Sandstone. Is overlain conformably by Kurinelli and Unimbra Sandstones (the latter also disconformably).|Basalt, hawaiite, potassic trachybasalt and shoshonite, predominantly massive/vesicular/amygdaloidal, non-porphyritic pahoehoe and minor amygdaloidal probable aa lava; minor felsic lava and tuff; local thick rhyolite lava; sandstone.|12-JUL-16
26302|Edmirringee Volcanics|69591|5|Briefly described|p32|||Tennant Creek-Davenport Province (NT).||||(Possibly) correlated with Oroopo Volcanics (Mount Isa Province, Qld).||
26302|Edmirringee Volcanics|73124|6|Mentioned|p2 Fig.1|||||||Equivalent to Epenarra Volcanics and Kurinelli Sandstone.||
26302|Edmirringee Volcanics|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
26302|Edmirringee Volcanics|73460|6|Mentioned|p2|||Warramunga Province.||||Underlain by and equivalent to Epenarra Volcanics and Kurinelli Sandstone.||
26302|Edmirringee Volcanics|73550|6|Mentioned|p5|Orosirian|Orosirian||ca 1850 Ma|Ooradidgee Group|||Mafic volcanics.|
26302|Edmirringee Volcanics|73590|6|Mentioned|p1-2|Orosirian|Orosirian||ca 1850 Ma|Ooradidgee Group||Underlain by and equivalent to Epenarra Volcanics and Kurinelli Sandstone.|Mafic.|
42370|Ehrenberg Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Illili Suite. Foliated equigranular to porphyritic allanite-bearing biotite granite; locally migmatic. In the Arunta region.||||||07-NOV-08
42370|Ehrenberg Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Illili Suite. Foliated equigranular to porphyritic allanite-bearing biotite granite, locally migmatitic. Geological Province: Warumpi Province||||||07-NOV-08
42370|Ehrenberg Granite|67565|4|Described|p6 Table 1, pp18-19, pp60-61.|Paleoproterozoic|Paleoproterozoic|Yaya Domain, Warumpi Province.||Unit in Illili Suite.||Intrudes Russell Charnockite.|Medium-grained felsic biotite granite, weakly porphyritic.|03-DEC-15
42370|Ehrenberg Granite|69428|5|Briefly described|p13:11|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Yaya Domain, Warumpi Province. Occurs in scattered outcrops between the Ehrenberg Range and the Davenport Hills.||Illili Suite.|||Variably porphyritic, felsic biotite granite.|12-JUL-16
42370|Ehrenberg Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.||Unit of Illili Suite.|||Foliated equigranular to porphyritic allanite-bearing biotite granite, locally migmatitic.|09-SEP-19
24261|El Sherana Group|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Includes the Tollis Formation.||||||
24261|El Sherana Group|22429|6|Mentioned|P23|||||||||
24261|El Sherana Group|22479|5|Briefly described|fig1p2, fig4p10|Orosirian|Orosirian|||||||
24261|El Sherana Group|22538|6|Mentioned|P714||Orosirian|||||||
24261|El Sherana Group|22600|6|Mentioned|Map legend|||||||||
24261|El Sherana Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|23119|5|Briefly described|p434||Proterozoic|Age: Early Proterozoic.||||||
24261|El Sherana Group|23216|5|Briefly described|Fig3p5||Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|23363|5|Briefly described|344 Fig.3|||||||||
24261|El Sherana Group|23374|5|Briefly described|Fig3p5||Paleoproterozoic|Of Pine Creek Inlier.||||||07-NOV-08
24261|El Sherana Group|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
24261|El Sherana Group|23714|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
24261|El Sherana Group|23733|5|Briefly described|p32 Fig. 19|||||||||
24261|El Sherana Group|23867|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.  See also Fig. 3.||||||07-NOV-08
24261|El Sherana Group|23937|6|Mentioned|p88 App. 1|||Geological Province: McArthur Basin.||||||
24261|El Sherana Group|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Sandstone, greywacke, rhyolite.  Age: 1828Ma.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5, p12 Fig. 10.||||||07-NOV-08
24261|El Sherana Group|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
24261|El Sherana Group|24197|5|Briefly described|p28, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the El Sherana Suite.The group includes the Gimbat Ignimbrite which is included in the Jim Jim Suite. Age: ~1865Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
24261|El Sherana Group|24442|6|Mentioned|p27|||||||||
24261|El Sherana Group|39357|4|Described|p12|||||||||
24261|El Sherana Group|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, sandstone, greywacke, shale.||||||07-NOV-08
24261|El Sherana Group|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid and minor basic volcanics, sandstone, greywacke, shale.||||||07-NOV-08
24261|El Sherana Group|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Acid to minor basic volcanics, sandstone, greywacke, shale.||||||07-NOV-08
24261|El Sherana Group|40243|6|Mentioned|p139|||||||||
24261|El Sherana Group|40248|3|Fully described|p222|||||||||
24261|El Sherana Group|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|40861|6|Mentioned|p121|||||||||
24261|El Sherana Group|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|41125|6|Mentioned|p26|||See also fig.6.||||||
24261|El Sherana Group|41146|6|Mentioned|p858|||||||||
24261|El Sherana Group|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24261|El Sherana Group|41295|4|Described|p9|||||||||
24261|El Sherana Group|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24261|El Sherana Group|41311|4|Described|p12|||||||||
24261|El Sherana Group|41325|6|Mentioned|p18|||||||||
24261|El Sherana Group|41397|4|Described|p12|||||||||
24261|El Sherana Group|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|41407|6|Mentioned|Map legend|Proterozoic||||||||
24261|El Sherana Group|41465|6|Mentioned|p6|||||||||
24261|El Sherana Group|41466|5|Briefly described|p23|||||||||
24261|El Sherana Group|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24261|El Sherana Group|41594|6|Mentioned|p20|||||||||
24261|El Sherana Group|41645|6|Mentioned|p10|||||||||
24261|El Sherana Group|41961|6|Mentioned|Table 2 P41|||||||||
24261|El Sherana Group|41980|6|Mentioned|p574|||||||||
24261|El Sherana Group|42012|6|Mentioned|Fig.3 P3|||||||||
24261|El Sherana Group|42324|5|Briefly described|p4|||||||||
24261|El Sherana Group|42344|5|Briefly described|p54|||||||||
24261|El Sherana Group|42355|5|Briefly described|p69|||||||||
24261|El Sherana Group|42812|6|Mentioned|p60|||||||||
24261|El Sherana Group|42927|6|Mentioned|p428|||||||||
24261|El Sherana Group|43010|6|Mentioned|p76|||||||||
24261|El Sherana Group|43140|5|Briefly described|p3||Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|43624|6|Mentioned|Table 1, p9||Carpentarian|Age: 1870-1860 Ma. Early to Middle Proterozoic||||||
24261|El Sherana Group|43718|6|Mentioned|p2||Paleoproterozoic|Late Palaeoproterozoic||||||07-NOV-08
24261|El Sherana Group|43720|5|Briefly described|p1,4|Mesoproterozoic|Paleoproterozoic|Late Palaeoproterozoic - Mesoproterozoic||||||07-NOV-08
24261|El Sherana Group|43726|6|Mentioned|p2|||||||||
24261|El Sherana Group|43749|6|Mentioned|p30|||||||||
24261|El Sherana Group|43832|4|Described|21-23,Table6 p22, 97||Paleoproterozoic|Age ~1870 Ma. In Pine Ck Geosyncline. Finniss River Group underlies, Edith River Group overlies.||||||07-NOV-08
24261|El Sherana Group|44112|6|Mentioned|p63|||||||||
24261|El Sherana Group|46658|4|Described|p556|||||||||
24261|El Sherana Group|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Acid and minor acid volcanics, sandstone, greywacke, shale.   Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
24261|El Sherana Group|47049|5|Briefly described|Table|||New name.||||||
24261|El Sherana Group|50586|5|Briefly described|p1.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the El Sherana Suite.||||||07-NOV-08
24261|El Sherana Group|50606|6|Mentioned|p1.1, 4.3|||||||||
24261|El Sherana Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24261|El Sherana Group|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes Big Sunday Sandstone, Pul Pul Rhyolite, Coronation Sandstone and Scinto Breccia.||||||13-NOV-06
24261|El Sherana Group|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
24261|El Sherana Group|61861|6|Mentioned|Fig.2.|||Pine Creek. Correlative with Flynn and Ooradidgee Subgroups in Tennant Creek.||||||18-FEB-13
24261|El Sherana Group|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Rhyolite, greywacke, siltstone, sandstone, basalt. Age: 1835Ma. Geological Province: Pine Creek Orogen.||||||09-FEB-10
24261|El Sherana Group|63261|6|Mentioned|p23|||Geological province: Pine Creek Orogen.||||||07-FEB-11
24261|El Sherana Group|63866|5|Briefly described|p110-p111, p123|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Age derived from the numeric age of the constituent Pul Pul Rhyolite.|||Includes the Pul Pul Rhyolite.|Unconformably overlain by the Edith River Group. Intrudes the Gimbat Ignimbrite Member.||
24261|El Sherana Group|64677|6|Mentioned|v,|||||||Conformably overlies Burrell Creek Formation.||
24261|El Sherana Group|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Includes Big Sunday Formation, Coronation Sandstone, Pul Pul Rhyolite (1829Ma), Scinto Breccia.||||||07-JAN-09
24261|El Sherana Group|64722|5|Briefly described|Fig. 2 p3-6, p10, 22|Orosirian|Orosirian|Pine Creek Orogen. Age given for this and overlying Edith River Group.|1830 - 1825 Ma.|||Unconformably overlain by Edith River Group. Overlies South Alligator and Finniss River Groups.|Volcanic and sedimentary rocks.|11-APR-12
24261|El Sherana Group|64725|6|Mentioned|p61.|||Clastic, pyroclastic and volcanic rocks deposited in a NW-SE rift near the eastern margin of the Marrakai Domain.||||||
24261|El Sherana Group|64730|5|Briefly described|p125 Fig. 3, p126, 141, p142 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age is of Pul Pul Rhyolite (Jagodzinski 1998).|Deposition age 1829 +/- 5 Ma.||Includes Big Sunday Formation, Pul Pul Rhyolite and Coronation Sandstone.|||02-MAY-12
24261|El Sherana Group|65232|5|Briefly described|p45, p6 Fig. 5, p7, p5 Fig. 4|Orosirian|Orosirian|Includes Coronation Sandstone, Pul Pul Rhyolite and Big Sunday Formation. Unconformable under Edith River Group and Mamadawerre Sandstone. Unconformable base. Age: ~1828 Ma and 1830 Ma. Geol. Prov: Pine Creek Orogen. Sandstone, greywacke, rhyolite.||||||09-FEB-10
24261|El Sherana Group|66683|6|Mentioned|p367.|||Deposition in a rift-related half-graben.|1829 Ma.|||||
24261|El Sherana Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.||||||
24261|El Sherana Group|67355|6|Mentioned|p5, p7 Tb.2||Orosirian|Deposited as a result of graben formation centred on the South Alligator River valley. Deposition occurred at 1865 Ma, and folding at 1850 Ma, according to Needham et al. (1988).|1822 Ma (SHRIMP)|||Coeval with Cullen Supersuite and David Suite. Underlies the Edith River Group, overlies the Cosmo Howley Supergroup.||25-JAN-17
24261|El Sherana Group|67479|5|Briefly described|p6 Fig.2, p58|Orosirian|Orosirian||1829-1825 Ma||||Felsic extrusive volcanic rocks.|24-JAN-17
24261|El Sherana Group|67564|3|Fully described|p7 Table 2, p9 Fig.4, pp25-29, p86.|Paleoproterozoic|Paleoproterozoic|Jawoyn Sub-basin. Up to 2650 m of bimodal volcanic and fluviatile volcaniclastic sedimentary rocks. Mildly deformed. Previously included the Tollis Formation, which is now part of the Finniss River Group. Contains some rocks previously mapped as Edith River Volcanics by Walpole (1963) and Stuart-Smith et al. (1984).|1830 - 1820 Ma.||Includes Scinto Breccia, Coronation Sandstone, Pul Pul Rhyolite and Big Sunday Formation.|Unconformably overlies Masson Formation. Is intruded by David Suite.|Sandstone, conglomerate, sedimentary breccia, mafic and felsic (rhyolitic ignimbrite) volcanic rocks.|
24261|El Sherana Group|67779|5|Briefly described|p5 Fig.4(b), p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Shown as one of a series of Granite suites on p4 [?].|||Includes Coronation Sandstone, Pul Pul Rhyolite and Big Sunday Formation.|||18-MAY-18
24261|El Sherana Group|69417|5|Briefly described|p2:4-5|Orosirian|Orosirian|Pine Creek Orogen.|1825-1810 Ma.|||Is intruded by Cullen Supersuite.|Sandstone, felsic volcanic rocks.|12-JUL-16
24261|El Sherana Group|69418|6|Mentioned|p3:19|||Pine Creek Orogen. Said to host all of the South Alligator Valley U deposits.||||||12-JUL-16
24261|El Sherana Group|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
24261|El Sherana Group|69420|4|Described|p5:2, 4-5, 7, 13-17, 21, 23, 27, 33|Paleoproterozoic|Paleoproterozoic|See also 38-39, 51, 54-55, 62, 66, 78-79, 85, 100, 111, 115. Central Domain, Pine Creek Orogen. As in Needham and Stuart-Smith (1984). Deposition in fault-bounded shallow grabens. Over 2.5km thick. Folded by the Maud Creek Event. Associated with the Coronation Hill Au deposit; U-Au-PGE ore occurs at or below the basal unconformity. Minimum age of 1825 +/- 4 Ma from overlying unit; both SHRIMP U-Pb zircon ages.|1829 +/- 5 Ma ( Jagodzinski, 1999).||Coronation Sandstone; Big Sunday Formation; Pul Pul Rhyolite; Scinto Breccia.|Unconformably overlies South Alligator Group. Is disconformably overlain by Plum Tree Creek Volcanics (Edith River Group).|A succession of mainly interbedded felsic and mafic volcanic rocks, sandstone, conglomerate and sedimentary breccia.|12-JUL-16
24261|El Sherana Group|69424|6|Mentioned|p9:4|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||Time-correlative of Ooradidgee Group.||12-JUL-16
24261|El Sherana Group|69426|5|Briefly described|p11:7|||Pine Creek Orogen.||||Correlated with Ware Group (Tanami Region).||12-JUL-16
24261|El Sherana Group|69430|6|Mentioned|p15:4|||Pine Creek Orogen.||||||12-JUL-16
24261|El Sherana Group|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||||||
24261|El Sherana Group|70293|5|Briefly described|p597-601, p613, p615, p619-620|Orosirian|Orosirian|Unmetamorphosed and only mildly folded sedimentary rocks.|1835 - 1825 Ma||Coronation Hill Sandstone, Scinto Breccia, Pul Pul Rhyolite, Big Sunday Formation|Unconformably overlies South Alligator Group, Zamu Dolerite. Unconformably overlain by Kurrundie Sandstone (Edith River Group).||
24261|El Sherana Group|71256|6|Mentioned|p18 Fig 1|||||||||
24261|El Sherana Group|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1831+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyry.|
24261|El Sherana Group|71606|5|Briefly described|p137|Orosirian|Orosirian|West Arnhem Shelf, McArthur Basin. ||||Overlain unconformably by Pine Creek Granites and Edith River Group. Underlain unconformably by Pine Creek Supergroup.||
24261|El Sherana Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Part of the early Basin volcanism and plutonism in the McArthur Basin. Mapped with Edith River Group as a single unit.|||||Felsic volcanics, sandstone, mudstone, conglomerate; minor basalt.|
24261|El Sherana Group|73089|6|Mentioned|p32, p38, p42|Orosirian|Orosirian|Pine Creek Orogen, Central Domain. Bimodal character may suggest an extensional setting for 1829-1822 Ma igneous rocks.|[c.]1840-1815 Ma|||Correlates[?] to Ware Group.|Includes felsic volcanic and lesser basaltic rocks.|
34215|Elang Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p216|Late Jurassic|Middle Jurassic|In figure, Fm = Formation. Geological Province: Bonaparte Basin. Broadly equivalent to the Montara beds. Also on p230.||||||
34215|Elang Formation|13267|5|Briefly described|pp273-279.|Middle Jurassic|Middle Jurassic|Poor hydrocarbon reservoir quality. Oil shows were observed. Very late stage oil input, probably from adjacent generating carbonaceous claystones. Calcite and ankerite cement deposited during Late Cretaceous via faults.||||Overlies Plover Formation.|Quartzose, very fine- to fine-grained, moderately well-sorted sandstones with interbedded siltstone and claystone. Clay content and carbonate cement in sandstones are variable but macroporosity is greatly reduced.|
34215|Elang Formation|13354|6|Mentioned|p381.|Jurassic|Jurassic|Sahul Platform.||15||||28-OCT-14
34215|Elang Formation|22663|6|Mentioned|NT97 -1-4 p3|||||||||
34215|Elang Formation|23376|4|Described|p229 Fig.2;p227-9,235,240,243|Oxfordian|Callovian|In the Bonaparte Basin.||||||15-AUG-06
34215|Elang Formation|24234|5|Briefly described|p286, p287 Fig.3|Callovian|Callovian|Overlies Plover Formation, overlain by Frigate Formation. Geological Province: Bonaparte Basin.||||||
34215|Elang Formation|24390|5|Briefly described|p3 Table 1|Middle Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin||||||
34215|Elang Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin.||||||09-MAR-05
34215|Elang Formation|60386|6|Mentioned|p300, 302|Late Jurassic|Middle Jurassic|Bonaparte Basin. Deltaic-nearshore-shelf, proximal shelf. ||||||
34215|Elang Formation|64689|5|Briefly described|p7 Fig.6 |Late Jurassic|Middle Jurassic|||||||
34215|Elang Formation|64696|6|Mentioned|p125, 127 Fig.2, p128, p131-132  |Late Jurassic|Middle Jurassic|See also p136, p138. Reservoir unit, c.150 m thick. Referred to as Elang/Laminaria Formation in the Joint Petroleum Development Area. Geophysical properties detailed in Fig.10.||||Overlies Plover Formation gradationally.|Sheet-like deposition of sand-prone marine and deltaic facies (sandstones, siltstones and mudstones).|
34215|Elang Formation|68135|6|Mentioned|p61, p62|||Northern Bonaparte Basin. Sedimentary sequences and fossils described.||||||14-SEP-17
34215|Elang Formation|69452|5|Briefly described|p36:8, 15, 21-22|Oxfordian|Callovian|Petrel Sub-basin, Bonaparte Basin. Thickness up to ?50m.||Flamingo Group.||Is overlain by Frigate Shale. Equivalent to Laminaria and Montara Formations.|Retrogradational deltaic sandstone deposited as a result of a widespread marine transgression.|12-JUL-16
34215|Elang Formation|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p17-18, 76|Late Jurassic|Middle Jurassic|Petrel Sub-basin. Suitable for CO2 storage; sealed by Frigate Shale. Delta-plain - shoreface deposits. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p26-27, 30, 37, 39, 41-43, 45-48, 50, 53, 59, 63-64.||Flamingo Group.||Overlies Plover Formation. Is overlain disconformably by Frigate Shale.|Mudstone; siltstone/fine-grained sandstone; medium- to coarse-grained sandstone. Facies described in detail.|
34215|Elang Formation|69673|6|Mentioned|p173|||||Flamingo Group||||
34215|Elang Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Overlies Plover Formation.||
34215|Elang Formation|70061|5|Briefly described|Petrel Sub-basin Fig.2|Late Jurassic|Middle Jurassic|See also Regional geology: Figs.6-7, p6, p7, p10, p12, p14, p18-19. Sahul: Fig.2, p1-2. Bonaparte Basin; commercial petroleum and gas reservoir. Appears also as Elang (Laminaria) Formation. Source rock in Sahul Syncline.||Flamingo Group.||Overlies Plover Formation. Is overlain by Lower Frigate Shale.|Retrogradational deltaic (shoreface/barrier bar) sandstones.|12-JUL-16
26534|Elcho Island Formation|22600|4|Described|Map legend|Neoproterozoic|Neoproterozoic|||||||
26534|Elcho Island Formation|23373|5|Briefly described|p318||Neoproterozoic|Of Wessell Group. Geological Province:  Arafura Basin.||||||15-AUG-06
26534|Elcho Island Formation|23374|3|Fully described|Tb3 p22,23,20,27||Neoproterozoic|Age uncertain, within the range Neoproterozoic - Middle Cambrian; Neoproterozoic likely. Of the Wessel Group. Geological Province: Arafura Basin.||||||15-AUG-06
26534|Elcho Island Formation|24047|5|Briefly described|p11, p40|||Disconformably overlain by Goulburn Group.  Geological Province: Arafura Basin.||||||
26534|Elcho Island Formation|24049|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: fine to coarse-grained, thin to medium bedded, commonly calcaerous or dolomitic, locally glauconitic; minor mudstone interbeds; carbonate horizons; chert breccia. Geol. Prov: McArthur Basin.||||||13-OCT-05
26534|Elcho Island Formation|32660|5|Briefly described|Table 7|||||||||
26534|Elcho Island Formation|37565|6|Mentioned|p10|||||||||
26534|Elcho Island Formation|40105|6|Mentioned|p313|||||||||
26534|Elcho Island Formation|42058|5|Briefly described|p114|||||||||
26534|Elcho Island Formation|42597|5|Briefly described|Map Legend|Adelaidean||||||||
26534|Elcho Island Formation|43010|2|Defined|p181|Middle Cambrian|Early Cambrian|Of Wessel Group. This definition superseded by defn card.||||||15-AUG-06
26534|Elcho Island Formation|44112|1|Redefined|p76-77,108||Neoproterozoic|Redefinition prompted by a younger sequence being exposed ('Jigaimara Formation')||||||
26534|Elcho Island Formation|44338|14|Not recorded|p.6,7,9||Neoproterozoic|Wessel Island Area. U.Prot. (C53-14).||||||
26534|Elcho Island Formation|44475|2|Defined|p.7,8, opp.p.6, map||Neoproterozoic|(C53-15,16) Of the Wessel Group. Upper Proterozoic. See also Tb.1, for more details.||||||15-AUG-06
26534|Elcho Island Formation|44476|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
26534|Elcho Island Formation|46792|5|Briefly described|p51|||Trilobite fauna||||||
26534|Elcho Island Formation|48894|6|Mentioned|p24|||Age: 780my.||||||15-AUG-06
26534|Elcho Island Formation|60571|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Sandstone: fine- to coarse-grained, thin- to medium-bedded, commonly calcareous or dolomitic; minor mudstone interbeds; carbonate horizons: strongly leached or silicified to chert breccia. Geological Province: Arafura Basin.||||||30-NOV-04
26534|Elcho Island Formation|61403|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Sandstone: fine to coarse-grained, thin to medium bedded, commonly calcaerous or dolomitic, locally glauconitic; minor mudstone inter beds; carbonate horizons; chert breccia. Geol. Prov: McArthur Basin.||||||
26534|Elcho Island Formation|62504|5|Briefly described|p1, 2|Neoproterozoic|Neoproterozoic|Age: 770-790Ma? Of the Wessel Group . Overlies: Marchinbar Sandstone. ||||||
26534|Elcho Island Formation|62505|4|Described|p3|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Overlies: Marchinbar Sandstone. Glauconitic sandstones and siltstones. ||||||
26534|Elcho Island Formation|62788|5|Briefly described|p103, p104|Neoproterozoic|Neoproterozoic|Arafura Basin. Radiometric dates of glaucony from low in the Formation produced dates of 770 Ma (K/Ar) to 790 Ma (Rb/Sr).||Uppermost unit of Wessel Group.||Overlies Marchinbar Sandstone, and underlies Jigaimara Formation of the Cambrian Goulburn Group.||28-MAR-12
26534|Elcho Island Formation|63062|5|Briefly described|p11, p38|||Of the Wessel Group. Geological Province: Arafura and Money Shoal Basins. Contains thick, fine-grained sediments of shallow marine origin.||||||07-FEB-11
26534|Elcho Island Formation|69418|6|Mentioned|p3:24|||Arafura Basin. Hosts the Elcho Island surficial Fe deposit (described).||||||12-JUL-16
26534|Elcho Island Formation|69437|6|Mentioned|p22:4-5|Ediacaran|Ediacaran|Arafura Basin. Minimum age not well constrained.||||||05-SEP-18
26534|Elcho Island Formation|69451|3|Fully described|p35:3-4, 6-7, 12-13|?Early Cambrian|Neoproterozoic|Plumb and Roberts (1992), who nominated  a reference section as cliff outcrops on Elcho Island. Redefined by Rawlings et al. (1997) who nominated a type locality in western ARNHEM BAY map area. Arafura Basin (onshore). Shallow-marine, occasionally exposed deposits; periodic evaporitic conditions. 650-700m thick. The sandstone has cross-beds, ripples, current lineations and load casts. Ages by McDougall et al. (1965) are from a single glauconite low in the formation. Hosts the Elcho Island iron ore deposit in a bauxitic lateritic profile containing a lower sandy haematite layer and an upper haematitic sandstone bed. Potential petroleum source rock.|c.770 Ma (K-Ar) and 790 Ma (Rb-Sr).|Wessel Group.||Overlies Marchinbar Sandstone locally disconformably or possibly conformably. Is overlain unconformably or disconformably by Jigaimara Formation.|Fine- to coarse-grained, thinly to medium bedded sandstone, often calcareous or dolomitic and locally glauconitic; minor mudstone interbeds; occasional carbonate intervals, locally strongly leached or silicified to chert breccia.|05-SEP-18
26534|Elcho Island Formation|69673|5|Briefly described|p195, p196|||700m thick.||Wessel Group|||Locally glauconitic sandstone, interbedded with minor mudstone, chert and sedimentary structures are common.|
26534|Elcho Island Formation|73083|6|Mentioned|p28, p33|Neoproterozoic|Neoproterozoic|||||||
26534|Elcho Island Formation|73086|6|Mentioned|p133|||Arafura Basin.||||Correlates to Julie Formation.||
26535|Elder Subgroup|14019|4|Described|p21|||Lower portion of the Goose Hole Group.  Overlies the Negri Subgroup (Goose Hole Group).   Geological Province: Ord Basin.||||||
26535|Elder Subgroup|22547|5|Briefly described|p30|||Of the Goose Hole Group. Overlain by Negri Subgroup.||||||14-NOV-06
26535|Elder Subgroup|40993|6|Mentioned|Fig.1|||||||||
26535|Elder Subgroup|41840|4|Described|p43|||Formerly "Mount Elder sandstone", In part Elder Sandstone||||||
26535|Elder Subgroup|41864|5|Briefly described|p23|||Formerly Elder Sandstone||||||
26535|Elder Subgroup|41865|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|||||||
26535|Elder Subgroup|41866|6|Mentioned|Map legend|Late Cambrian||||||||
26535|Elder Subgroup|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
26535|Elder Subgroup|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
26535|Elder Subgroup|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
26535|Elder Subgroup|60419|4|Described|p1, p3 Fig.2|Late Cambrian|Middle Cambrian|Of Goose Hole Group. Conformably overlies Negri Subgroup. Max. thickness: 370 m. Geological Province: Ord Basin.||||||
26535|Elder Subgroup|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Goose Hole Group. Includes: Eagle Hawk Sandstone, Overland Sandstone. Geological Province: Ord Basin.||||||03-NOV-04
26535|Elder Subgroup|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Of the Goose Hole Group.  Geological Province: Ord Basin.||||||
26535|Elder Subgroup|67860|5|Briefly described|p417, p419 Tb. 4-18, p421 fig 4-86|Late Cambrian|Middle Cambrian|95-370 m thick.||Goose Hole Group|Includes Eagle Hawk and Overland Sandstones.|Conformably overlies Negri Subgroup.|Feldspathic sandstone; minor siltstone.|
26535|Elder Subgroup|69099|5|Briefly described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone|||
26535|Elder Subgroup|69165|6|Mentioned|100k_interpgeop_lut.csv, |Furongian|Furongian|||Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone,|||
26535|Elder Subgroup|69448|4|Described|p33:1-4, 6-8|Middle Cambrian|Middle Cambrian|Ord Basin. Previously Elder Sandstone. Up to 370m thick. Lacks age-diagnostic fossils.||Goose Hole Group.|Eagle Hawk, Overland Sandstones.|Conformably and gradationally overlies Negri Subgroup. Is overlain unconformably by Mahony Group.|A sandstone-dominated succession.|12-JUL-16
26535|Elder Subgroup|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Goose Hole Group.|Includes Eagle Hawk Sandstone, Overland Sandstone.|||
26535|Elder Subgroup|69673|5|Briefly described|p193, p194|||370m thick.|||Includes Eagle Hawk Sandstone, Overland Sandstone||Sandstones.|
26535|Elder Subgroup|70154|6|Mentioned|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-509 Ma|Goose Hole Group|Includes Eagle Hawk Sandstone, Overland Sandstone|||
26535|Elder Subgroup|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.||Goose Hole Group||Overlies the Negri Subgroup. Unconformably overlain by the Mahony Group.|Sandstone.|
26535|Elder Subgroup|71267|5|Briefly described|100k_interpgeop_lut.csv|||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).||Unit of Goose Hole Group.|Includes Eagle Hawk Sandstone, Overland Sandstone.|||
26535|Elder Subgroup|71800|5|Briefly described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin.||Goose Hole Group|Includes the Eagle Hawk Sandstone and the Overland Sandstone.|Overlies the Negri Subgroup.||
25892|Elkedra Granite|22446|6|Mentioned|p29|Statherian|Statherian|||||||
25892|Elkedra Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1720+/-8Ma.||||||15-AUG-06
25892|Elkedra Granite|23733|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of Devils Suite. See also p32 Fig.1, p34 Fig.20.||||||07-NOV-08
25892|Elkedra Granite|23809|6|Mentioned|p27 Fig. 25|||Geological Province: Davenport Province.||||||
25892|Elkedra Granite|24197|5|Briefly described|p28, p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of the Devils Suite. Age: ~1710Ma. Geological Province: Tennant Creek/Davenport Province.||||||07-FEB-11
25892|Elkedra Granite|39887|6|Mentioned|p453|||||||||
25892|Elkedra Granite|39888|6|Mentioned|Fig.8|||||||||
25892|Elkedra Granite|40836|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|Early to Middle Cambrian||||||07-MAR-13
25892|Elkedra Granite|41204|6|Mentioned|p10|||||||||
25892|Elkedra Granite|41308|6|Mentioned|p9|||||||||
25892|Elkedra Granite|41408|6|Mentioned|Map legend|Proterozoic||||||||
25892|Elkedra Granite|41465|6|Mentioned|p10|||||||||
25892|Elkedra Granite|41524|4|Described|p10|||||||||
25892|Elkedra Granite|41525|5|Briefly described|Map legend||Paleoproterozoic|Biotite granite, medium to coarse; minor tonalite.||||||07-NOV-08
25892|Elkedra Granite|41970|6|Mentioned|p334|||||||||
25892|Elkedra Granite|42504|5|Briefly described|Table 3 P60|||||||||
25892|Elkedra Granite|42643|5|Briefly described|p17|||||||||
25892|Elkedra Granite|42754|6|Mentioned|p3|||||||||
25892|Elkedra Granite|43802|6|Mentioned|p78|||||||||
25892|Elkedra Granite|43832|6|Mentioned|Table 17 p90||Paleoproterozoic|||||||07-NOV-08
25892|Elkedra Granite|45167|5|Briefly described|p48, Table 2|||Age of 1430 Ma?||||||15-AUG-06
25892|Elkedra Granite|46919|6|Mentioned|p221|||||||||
25892|Elkedra Granite|49033|2|Defined|p31|Proterozoic|Proterozoic|||||||
25892|Elkedra 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: 1720 +/- 6Ma (SHRIMP).||||||30-MAY-16
25892|Elkedra Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite: muscovite-biotite-bearing.  In the Tennant Creek region.||||||07-NOV-08
25892|Elkedra Granite|64068|6|Mentioned|p33, 53, 196-197|Statherian|Statherian||1720 +/- 6 Ma.|||Overlain by Andagera Formation.||05-APR-12
25892|Elkedra Granite|64724|6|Mentioned|p46|Statherian|Statherian|Intruded 1720 Ma.||||||02-APR-12
25892|Elkedra Granite|64735|6|Mentioned|p206||Statherian|||Of Devils Suite.||||30-APR-12
25892|Elkedra Granite|64738|5|Briefly described|p247 Fig.1, p249, p250 Table 1, p257-8|Statherian|Statherian||Crystallised 1720 +/- 6 Ma.|Unit in Devils Suite.||||
25892|Elkedra Granite|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Devils Suite||||
25892|Elkedra Granite|65338|5|Briefly described|p7, p35.|Statherian|Statherian|Davenport Province. Has inherited xenocrysts aged c.2260, 1820 and 1785 Ma.|1720 +/- 6 Ma.|Unit in Devils Suite.||||
25892|Elkedra Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Devils Suite.|||Leucogranite; muscovite-biotite-bearing.|
25892|Elkedra Granite|67352|6|Mentioned|p8|Statherian|Statherian|||Devils Suite||||
25892|Elkedra Granite|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 1.3, 9 analyses, Page (1996).|1720 +/- 6 Ma, magmatic crystallisation|||||
25892|Elkedra Granite|68518|4|Described|p5, p10 Tb.1, p11, p13-14|Proterozoic|Proterozoic|Mineral deposit: wolframite-bearing quartz veins, Juggler mine in the SE; no recorded production. Type area: in vicinity of Juggler tungsten mine around GR NS490250. Age: Isotopic K-Ar biotite,1430 Ma (Hurley & others, 1961); Rb-Sr whole rock isochron, about 1640 Ma (L.P.Black pers.comm. 1983, reassessment of age of 1695 obtained by Riley and reported by Compston and Arriens, 1968). Postdates folding of Hatches Creek Group.|probably emplaced about 1640 Ma|||Intrudes Rooneys Formation (Ooradidgee Subgroup, Hatches Creek Group); overlain by subhorizontal Cambrian sedimentary rocks.|Granite pluton|30-MAY-16
25892|Elkedra Granite|69424|5|Briefly described|p9:28-29, 34, 54-55|Paleoproterozoic|Paleoproterozoic|Davenport Province. A single concordant zircon giving an age of 1633 +/- 20 Ma was obtained in the analysis (Page, 1995). Hosts the W-Sn mineralisation at the Juggler mine.|1720 +/- 6 Ma (Compston, 1995).|Devils Suite.||||12-JUL-16
25892|Elkedra Granite|69425|4|Described|p10:20-25|||Assigned to the Devils Suite by Wyborn et al. (1998). The granodiorite and leucocratic microgranite, outcropping near the Tosca Mine, were excluded by Blake et al. (1987) but re-included by Stidolph et al. (1988). Blake and Horsfall (1986) excluded the weakly foliated or gneissic biotite granite near the Tosca Mine, but Donnellan and Johnstone (2004) re-included it. Davenport Province. Interpreted as penecontemporaneous with the Davenport Event. The monzogranite is associated with quartz-feldspar pegmatite, wolframite-bearing quartz-tourmaline and greisenous zones; also a contact aureole of hornfels and spotted schist up to 100m wide. Detrital scheelite occurs in the vicinity. A single concordant zircon with an age of 1633 +/- 20 Ma was obtained in the analysis of Page.|1720 +/- 6 Ma (Page, 1995).|Devils Suite.|||Medium- to coarse-grained, homogeneous, equigranular to locally megacrystic leuco-monzogranite; also granodiorite, tonalite?, leucocratic microgranite, and weakly foliated or locally gneissic biotite granite. Up to 10% muscovite.|12-JUL-16
25892|Elkedra Granite|69443|5|Briefly described|p28:12|Paleoproterozoic|Paleoproterozoic|A major source of sediments for the overlying Andagera Formation.||||Is overlain nonconformably by Andagera Formation.||12-JUL-16
25892|Elkedra Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1720+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
25892|Elkedra Granite|72379|5|Briefly described|iii,p9|Paleoproterozoic|Paleoproterozoic|Geological province: Davenport Province. Hosts tungsten mineralisation at the Juggler prospect (page 1996b).|c. 1720 Ma|||||03-OCT-19
25892|Elkedra Granite|73128|6|Mentioned|p13|Statherian|Statherian||1720 +/- 6 Ma|||Intrudes Hatches Creek Group.||
24266|Ella Creek Member|23714|5|Briefly described|p10|Proterozoic|Proterozoic|Of Koolpin Formation.||||||
24266|Ella Creek Member|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Koolpin Formation. Massive to rubbly geothitic ironstone commonly containing paraquartzite breccia; quartz-flake breccia with rare quartzite nodules, ferruginous chert breccia with oolites, siltstone containing chert nodules.||||||07-NOV-08
24266|Ella Creek Member|40808|3|Fully described|p13|||||||||
24266|Ella Creek Member|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24266|Ella Creek Member|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24266|Ella Creek Member|41305|3|Fully described|p16|||||||||
24266|Ella Creek Member|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Possible palaeoregolith breccia. Base of South Alligator Group.||||||07-NOV-08
24266|Ella Creek Member|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Koolpin Formation (South Alligator Group).||||||
24266|Ella Creek Member|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Massive to rubbly goethitic ironstone commonly containg paraquartzite; breccia, quartz flake breccia, ferruginous chert breccia, oolites, siltstone containg chert nodules, pebble and boulder conglomerate. Of Koolpin Formation.||||||
24266|Ella Creek Member|61389|5|Briefly described|Map Legend|||Of the Koolpin Formation. Massive to rubbly geothitic ironstone & quartzite breccia, quartz flake breccia with quartzite nodules, conglomerate.||||||
24266|Ella Creek Member|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1863-2025Ma. Of Koolpin Formation, South Alligator Goup.  Max. thickness 150m. Massive to rubbly goethitic ironstone and quartzite breccia, quartz flake breccia with quartzite nodules, conglomerate. Unconformably overlies Wildman Siltstone.||||||
24266|Ella Creek Member|65232|5|Briefly described|p51|||Of Koolpin Formation. Possible palaeo-regolith breccia.||||||09-FEB-10
24266|Ella Creek Member|65339|5|Briefly described|p6 Table 1, p12. |||Exposed as small strike ridges.||Basal unit in Koolpin Formation.|||Basal interbedded black shale and sandstone; massive to rubbly goethitic ironstone, commonly containing paraquartzite; breccia, quartz flake or ferruginous chert with ooids; siltstone with chert nodules; pebble and boulder conglomerate.|
24266|Ella Creek Member|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Koolpin Formation.|||Massive to rubbly goethitic ironstone and quartzite breccia, quartz flake breccia with quartzite nodules, conglomerate.|23-NOV-11
24266|Ella Creek Member|67355|5|Briefly described|p.12||Orosirian|Basal unit of the Koolpin Formation and is best exposed to the north and east of the Rum Jungle Dome. Crick (1987) interpreted it as a palaeoregolith formed during weathering of the underlying strata, however Pietsch and Stuart-Smith (1988) debate this. ||Koolpin Formation|||Includes: ironstone; various breccias; siltstone with chert nodules; conglomerate; ferruginous siltstone; quartzite interbedded with black shale; siltstone; dolostone; carbonaceous shale.|
24266|Ella Creek Member|69420|5|Briefly described|p5:11|Paleoproterozoic|Paleoproterozoic|Pietsch and Stuart-Smith (1987), Crick (1987).||Koolpin Formation.|||A 10m thick basal unit of ferruginous breccia, quartzite breccia, minor ferruginous siltstone, and rare pebble and boulder conglomerate.|12-JUL-16
29773|Ellery Granitic Complex|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of Madderns Yard Suite. Age: 1680Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
29773|Ellery Granitic Complex|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Iwupataka Metamorphic Complex.||||||07-NOV-08
29773|Ellery Granitic Complex|43503|2|Defined|8,25,78|||||||||
29773|Ellery Granitic Complex|50369|5|Briefly described|p1.5, 19.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Madderns Yard Suite.||||||07-NOV-08
29773|Ellery Granitic Complex|64809|6|Mentioned|p11 Fig.10 |Mesoproterozoic|Palaeoproterozoic|||||||
29773|Ellery Granitic Complex|69428|5|Briefly described|p13:07|||Warren and Shaw (1995). Crops out as a number of separate intrusions N and S of the Chewings Range. The relationship with Chewings Range Quartzite is unclear.||||Intrudes Lovely Hill Schist and Boggy Hole Gneiss.|Includes biotite-rich foliated porphyritic granite, foliated leucogranite and hornblende granite.|12-JUL-16
79767|Elliott sandstone member|70968|4|Described|p74-75, p77, p79|Mesoproterozoic|Mesoproterozoic|Gorter and Grey (2012). Beetaloo Sub-basin. Informal name for a prominent sandstone-rich interval in the lower part of the Kyalla Formation. Up to 70m thick. Fence diagram of wells in Beetaloo Sub-basin.||Kyalla Formation.|||Beds and bedsets, in varying proportions, of thinly to medium bedded, fine- to coarse-grained quartz sandstone, with minor interbedded mudrocks. Beds are massive, laminated and cross-bedded and may have scoured bases.|24-MAR-17
76085|Emmerugga Dolostone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1640-1630 Ma.|Unit in River Supersequence.||||
76085|Emmerugga Dolostone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p14 Tb.5|||Called Dolomite in Tb.1 and 5.||Of the Umbolooga Subgroup.|Includes Mara and Mitchell Yard, Dolostone Members.|||
76085|Emmerugga Dolostone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Lithology condensed from lithology of Member units.||Unit in Umbolooga Subgroup.|Includes Mara Dolostone and Mitchell Yard Dolostone Members.|Overlies Myrtle Shale. Is overlain by Teena Dolostone.|Massive, dark grey, karstic-weathering, crystalline dololutite; Dololutite, stromatolitic dololutite, dolomitic siltstone, dolarenite and dolomitic breccia; stromatolites; common halite casts and quartz nodules after evaporites.|16-SEP-13
76085|Emmerugga Dolostone|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. 620 m thick.||Umbolooga Subgroup|Mitchell Yard, Mara, Dolostone Members.||Massive crystalline dolomudstone.|
76085|Emmerugga Dolostone|69430|4|Described|p15:3, 16-17, 39-40|Statherian|Statherian|Southern McArthur Basin. 620m thick. Peritidal to deep marine sediments. Consists of a series of upward-shallowing cycles that deepen and thicken up-section. Contains minor discordant Pb-Zn-Ag +/-Cu Mississippi Valley-style deposits (Cooley I, II and III deposits), described in detail.||Umbolooga Subgroup.|Mara, Mitchell Yard, Dolostone Members.|Conformably and gradationally overlies Myrtle Shale. Is overlain conformably by Teena Dolostone.|Dololutite, stromatolitic dololutite, dolomitic siltstone, dolarenite and dolomitic breccia.|12-JUL-16
76085|Emmerugga Dolostone|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Umbolooga Subgroup|Includes Mara Dolostone Member, Mitchell Yard Member|Overlies Tooganinie Formation, overlain by Teena Dolostone||
76085|Emmerugga Dolostone|72373|5|Briefly described|p6,9,11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
76085|Emmerugga Dolostone|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the northern part of the Batten Fault Zone.||Batten Subgroup|Mitchell Yard Member and Mara Dolostone Member|Overlies Tooganinie Formation, Myrtle Shale and underlies Teena Dolostone.||
76085|Emmerugga Dolostone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group|Mara Dolostone Member?, Mitchell Yard Member?.|Underlain by Tooganinie Formation. Overlain by Teena Dolostone.||
76085|Emmerugga Dolostone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the north of the Batten Fault Zone.||Batten Subgroup|Probably includes Mara Dolostone Member, Michell Yard Member.|Overlies Tooganinie Formation. Underlies Teena Dolostone and is laterally equivalent to Mitchell Yard and Mara Dolostone members.||16-MAR-21
76085|Emmerugga Dolostone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group|Mitchell Yard Member, Mara Dolostone Member|Underlain by Tooganinie Formation. Overlain by Teena Dolostone.||
76085|Emmerugga Dolostone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Tooganinie Formation and Myrtle Shale. Is overlain by Barney Creek Formation.||
24269|Enbra Granulite|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex.  Mafic granulite.  Geological Province: Arunta Block.||||||03-NOV-04
24269|Enbra Granulite|23844|3|Fully described|p24|Mesoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. Study required to establish whether or not this granulite body is a transposed fragment of the Mount Hay Granulite body. See also Fig.7||||||07-NOV-08
24269|Enbra Granulite|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24269|Enbra Granulite|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24269|Enbra Granulite|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24269|Enbra Granulite|39610|6|Mentioned|p5|||||||||
24269|Enbra Granulite|48992|2|Defined|p19|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24269|Enbra Granulite|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 1). Of the Strangways Metamorphic Complex.  Mafic granulite.||||||
24269|Enbra Granulite|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Strangways Metamorphic Complex. Mafic granulite. Geological Province: Arunta Block.||||||06-JUN-05
24269|Enbra Granulite|60668|5|Briefly described|p9, p2 Tb. 1|||Homogeneous mafic granulite sequence ?overlain by more fractionated felsic rocks. Mafic granulites are dominant with irregular felsic granulite, garnet-biotite-feldspar-quartz paragneiss and migmatitic paragneiss interlayered. ||||||
24269|Enbra Granulite|64738|5|Briefly described|p247 Fig.2, p250 Table 1, p252, 253, 259|Paleoproterozoic|Paleoproterozoic|Mafic intrusion. Metamorphosed 1685 +/- 11 Ma.|Protolith age of 1810.7 +/- 2.6 Ma, 1811+/-3Ma .|||||
24269|Enbra Granulite|65338|5|Briefly described|p40.|Orosirian|Orosirian|ALICE SPRINGS area.|1811 +/- 3 Ma (Claoue-Long and Hoatson 2005).||||Metagabbro.|
24269|Enbra Granulite|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 0.1, 4 analyses, Claoue-Long and Hoatson, 2005.|1685 +/- 11 Ma, metamorphism|||||
24269|Enbra Granulite|69427|5|Briefly described|p12:9, 23-24|Orosirian|Orosirian|Shaw et al. (1979); Hoatson et al. (2005). Forms a group of hills on the Burt Plain, SW of the Strangways Range, Aileron Province. Extends further W under sand plain cover. S and N margins are fault-bound. Structures suggest intrusive mafic magma mingling with the felsic magmatic host: has similarities with the Mount Hay Granulite. SHRIMP U-Pb crystallisation age.|1812 +/- 2 Ma (Claoue-Long and Hoatson, 2005).||||Homogeneous mafic granulite with more evolved plagioclase-rich and anorthositic rocks in the N; lesser irregular felsic granulite, garnet-biotite-feldspar-quartz paragneiss and migmatitic paragneiss bodies.|12-JUL-16
29220|Endurance Sandstone Member|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
29220|Endurance Sandstone Member|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Micaceous greywacke and siltstone, thin bedded; minor feldspathic arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
29220|Endurance Sandstone Member|41129|4|Described|Table 1|||||||||
29220|Endurance Sandstone Member|41308|5|Briefly described|Table 2|||||||||
29220|Endurance Sandstone Member|41408|6|Mentioned|Map legend|Proterozoic||||||||
29220|Endurance Sandstone Member|45167|4|Described|Table 1|||Of Kurinelli Sandstone.||||||15-AUG-06
29220|Endurance Sandstone Member|49033|2|Defined|p10|Proterozoic|Proterozoic|||||||
29220|Endurance Sandstone Member|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in lower part of  Kurinelli Sandstone.|||Micaceous greywacke and siltstone, thin bedded; minor feldspathic arenite.|17-OCT-11
29220|Endurance Sandstone Member|67352|4|Described|p11 Tb.1|Orosirian|Orosirian|500 m thick. Lenses within Kurinelli Sandstone [although paper gives Plhk not Plok.]||Kurinelli Sandstone|||Micaceous greywacke and siltstone: thinly interbedded, fine-grained; minor feldspathic arenite: thinly to medium bedded.|
29220|Endurance Sandstone Member|69424|5|Briefly described|p9:18, 25|Paleoproterozoic|Paleoproterozoic|Warramunga Province. 400-500m thick; conformable lenses within Kurinelli Sandstone.||Kurinelli Sandstone.|||Thinly interbedded fine-grained, graded, micaceous greywacke and siltstone; feldspathic sandstone.|12-JUL-16
29220|Endurance Sandstone Member|69425|5|Briefly described|p10:5, 8|||Blake et al. (1985). Occurs as conformable lenses within Kurinelli Sandstone. Possibly represents tongues of Rooneys Formation. Maximum thickness 500m.||Kurinelli Sandstone.|||Thinly interbedded fine-grained, graded, micaceous greywacke and siltstone; feldspathic sandstone.|12-JUL-16
29220|Endurance Sandstone Member|72379|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||Unit of Kurinelli Sandstone.||||
29220|Endurance Sandstone Member|72380|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||Unit of Kurinelli Sandstone.||||
79088|Entia Metamorphics|69917|5|Briefly described|p136-140, 151, 152,153, 154-156,163-164|Statherian|Statherian|Eastern Arunta Region, Aileron Province. U/Pb SHRIMP, LA-ICPMS zircon dating, Hf analytical data. 7 samples. Maximum depositional age for the sedimentary protolith of 1788+/-3 Ma; metamorphic zircon growth 1717+/-10 Ma. Intermediate ages given from other samples.|||||Metapelite interlayered with quartzo-feldspathic gneiss, layered amphibolite and epidotised gneiss. Samples: Kyanite-garnet-biotite-muscovite schist; Migmatitic garnet-bearing metapelite.|
79088|Entia Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Other more-or-less similar ages given.|1766+/-7 Ma (MDA: U-Pb zircon LA-ICPMS).||||Calc-silicate rock, metapelite.|
79068|Entire Gneiss|69917|4|Described|p178-180, 1|Ordovician|Neoproterozoic|Eastern Arunta Region, Irindina Province.  U/Pb LA-ICPMS zircon dating, Hf analytical data. Two oldest grains may represent primary igneous zircon (timing of magmatism) at 596 and 523 Ma. The mean age of the majority: 453+/-2 Ma represents matamorphic recrystallisation. Up to 50 m thick.||Of Harts Range Metamorphic Complex.||Interlayered with Yambla Gneiss. Cross cuts (intrudes) Riddock Amphibolite.|Meta-anorthositic gneiss. Contains garnet or corundum locally.|29-JUL-15
79068|Entire Gneiss|72516|6|Mentioned|p79|||QUARTZ map sheet area.|ca 523 Ma|||Intrudes the Yambla Gneiss.||
27287|Epenarra Volcanics|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgroup, Hatches Creek Group.||||||07-NOV-08
27287|Epenarra Volcanics|23733|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group.  Age: 1820Ma.  See also p32 Fig.19, p34 Fig.20.||||||07-NOV-08
27287|Epenarra Volcanics|23809|5|Briefly described|p27 Fig. 25, p31|||Of the Ooradidgee Group.  Age: 1837+/-5Ma.  Geological Province: Davenport Province.||||||
27287|Epenarra Volcanics|24172|6|Mentioned|p66 Tb.9|||Conformably overlain by Edmirringee Volcanics.||||||15-AUG-06
27287|Epenarra Volcanics|24197|6|Mentioned|p22|||Parts included in Tennant Creek Supersuite.||||||07-FEB-11
27287|Epenarra Volcanics|39624|5|Briefly described|Table 1|||||||||
27287|Epenarra Volcanics|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27287|Epenarra Volcanics|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Altered felsic lava, tuff, agglomerate; interlayered partly volcaniclastic arenite; minor conglomerate, sitlstone, ashstone, mafic lava.||||||10-JAN-05
27287|Epenarra Volcanics|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27287|Epenarra Volcanics|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Cleaved felsic tuff; porphyritic lava; agglomerate; volcaniclastic arenite and conglomerate; minor mafic lava and tuff. Geological Province: Tennant Creek Block.||||||07-NOV-08
27287|Epenarra Volcanics|41129|4|Described|Table 1|||Mention p19.||||||15-AUG-06
27287|Epenarra Volcanics|41204|4|Described|Table 1|||||||||
27287|Epenarra Volcanics|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup. Felsic volcanics and volcaniclastic sediments.||||||16-NOV-05
27287|Epenarra Volcanics|41308|5|Briefly described|Table 2|||||||||
27287|Epenarra Volcanics|41310|4|Described|Table 1|||Mention p6.||||||15-AUG-06
27287|Epenarra Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
27287|Epenarra Volcanics|41524|5|Briefly described|p9|||||||||
27287|Epenarra Volcanics|41970|6|Mentioned|p334|||||||||
27287|Epenarra Volcanics|42504|5|Briefly described|p61|||||||||
27287|Epenarra Volcanics|43223|5|Briefly described|Map Legend||Proterozoic|of Ooradidgee Subgroup||||||
27287|Epenarra Volcanics|43224|5|Briefly described|Map legend||Proterozoic|Of Hatches Creek Group.||||||14-OCT-08
27287|Epenarra Volcanics|43652|6|Mentioned|p385|||U-Pb age: 1862+/-45 Ma||||||
27287|Epenarra Volcanics|43802|6|Mentioned|p78|||||||||
27287|Epenarra Volcanics|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||15-AUG-06
27287|Epenarra Volcanics|49033|2|Defined|p5|Proterozoic|Proterozoic|||||||
27287|Epenarra Volcanics|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||
27287|Epenarra Volcanics|50588|5|Briefly described|p2.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Geological Province: Tennant Creek/Davenport Province. Age: 1837 +/- 5Ma (Shrimp).||||||07-NOV-08
27287|Epenarra Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Felsic lava and pyroclastic rocks including ignimbrite and lapilli tuff; volcaniclastic arenite and conglom.; minor altered mafic lava / quartz arenite, volcaniclastic arenite, conglomerate; minor volcs. In the Tennant Creek region.||||||07-NOV-08
27287|Epenarra Volcanics|64730|5|Briefly described|p141, p142 Fig.11|Paleoproterozoic|Paleoproterozoic|Age is of crystallisation. Synchronous with felsic tuff of Callie Member of [Dead Bullock Formation,] Tanami Group.| 1840 +/-4 Ma (Claoue-Long et al 2005).|Of Ooradidgee Group.||||02-MAY-12
27287|Epenarra Volcanics|64735|4|Described|p205 Fig 1, p206 Fig 2, p209-210, p217|Orosirian|Orosirian|Age using SHRIMP RG 207Pb/206Pb on zircons from a fine-grained volcaniclastic sample (this publication). Correlates with Callie Member. A previous SHRIMP 1 dataset from 1990 gave a weighted mean age of 1837+/-5 Ma.|1840+/-4 Ma crystallisation age SHRIMP RG.|Of Ooradidgee Group.|||Felsic volcanics.|23-FEB-23
27287|Epenarra Volcanics|65209|5|Briefly described|p35 Fig.1, p36, p37, p38|Paleoproterozoic|Paleoproterozoic|Geol. Prov: in north Davenport Province||Basal unit of Ooradidgee Group.||Correlated with Rising Sun Conglomerate (in part).|Volcanics including a sandstone member.|05-JAN-17
27287|Epenarra Volcanics|65222|6|Mentioned|p126|||1820-1810 Ma (Blake and Page, 1988).||Of Hatches Creek Group||||
27287|Epenarra Volcanics|65338|5|Briefly described|p16.|Orosirian|Orosirian|Contemporaneous with syn- to immediately post-tectonic granite emplacement asssociated with the Tennant Event.|1840 +/- 4 Ma (Claoue-Long 2005).|||||
27287|Epenarra Volcanics|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Ooradidgee Group.||Is overlain by Rooneys Formation.|Cleaved felsic tuff; porphyritic lava; agglomerate; volcaniclastic arenite and conglomerate; minor mafic lava and tuff.|
27287|Epenarra Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Felsic lava and pyroclastic rocks including ignimbrite and lapilli tuff; volcaniclastic arenite and conglomerate; minor altered mafic lava.|
27287|Epenarra Volcanics|67323|5|Briefly described|p30, Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area. Extrusion age.|~1815-1810 Ma.|Ooradidgee Group.|||Felsic.|
27287|Epenarra Volcanics|67352|4|Described|p11 Tb.1, p41, p44 fig 48|Orosirian|Orosirian|Over 3000 m thick. ||Ooradidgee Group||Overlies (unconformably) Woodenjerrie beds.|Felsic tuff, lapilli tuff: laminated to thinly bedded; porphyritic lava and agglomerate: cleaved; minor amygdaloidal mafic lava  and tuff; volcaniclastic arenite, conglomerate: thinly to medium bedded, silicified.|
27287|Epenarra Volcanics|69187|4|Described|p53 Fig.2, p59-61|Orosirian|Orosirian|Warramunga Province.|1840 +/- 4 Ma (Claou¿-Long et al., 2008b)|Ooradidgee Group||unconformably overlies Hill of Leaders Granite; unconformably overlies Warramunga Formation and porphyries and granitic rocks||
27287|Epenarra Volcanics|69424|4|Described|p9:3-6, 10-11, 14-15, 18, 22-26, 28, 54|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Felsic extrusives of this unit are included in the Tennant Creek Supersuite. Subaerial volcanic rocks erupted from two volcanic centres: larger centre to the N (Warramunga Province), the smaller to the S in the Kurindi Anticline (Davenport Province). The <900m thick sedimentary lithofacies, of ridge-forming quartzose and volcaniclastic sandstone and conglomerate, locally dominate the unit and has been mapped as a separate lithofacies. Up to 3200m thick. Probably correlates in part with Bernborough Formation. Hosts Au-bearing quartz veins.|1840 +/- 4 Ma (Claoue-Long et al., 2008).|Ooradidgee Group.||Unconformably overlies Woodenjerrie beds. Overlain conformably by and interfingers with Rooneys Formation, Edmirringee Volcanics and Kurinelli Sandstone; overlain disconformably by Unimbra Sandstone.|Generally recessive porphyritic felsic lava and ignimbrite; volcanic breccia; agglomerate; felsic tuff and lapilli tuff; phyllitic to schistose felsic volcanic rocks; minor amygdaloidal non-porphyritic mafic lava and tuff; sandstone and conglomerate.|12-JUL-16
27287|Epenarra Volcanics|69425|4|Described|p10:3-8, 10, 13-14|||Mainly crops out in the Kurundi Anticline and the flanks of the Murchison Syncline. Thickness to ?1000m (Tb.10.1) but a maximum thickness of 3200m is stated on the same page. Predominantly subaerial volcanics and shallow-water sediments. The quartzitic and volcaniclastic sandstone and conglomerate are ridge-forming and locally dominate the unit. The sandstone lithofacies is lithologically identical with Kurinelli Sandstone. Also stated to be overlain conformably by, and interdigitate with, Unimbra Sandstone, despite a c.26 m.y. hiatus. Also dated at 1837 +/- 5 Ma by Page (1995).|1840 +/- 4 Ma (Claoue-Long et al., 2008).|Ooradidgee Group.||Unconformably overlies Woodenjerrie beds. Overlain by and interfingers with Rooneys Formation, Edmirringee Volcanics and Kurinelli Sandstone. Underlies disconformably/?unconformably Unimbra Sandstone.|Felsic porphyritic lava and eutaxitic-textured ignimbrite; volcanic breccia, agglomerate, felsic tuff, lapilli tuff; phyllitic to schistose felsic volcanic rocks; minor amygdaloidal aphyric mafic lava and tuff; local sandstone and conglomerate.|12-JUL-16
27287|Epenarra Volcanics|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1840+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic volcanic rocks.|
27287|Epenarra Volcanics|73083|6|Mentioned|p21|||Occurs as rafts enclosed in granite in Frew River 1:250K Sheet (NW).||||||
27287|Epenarra Volcanics|73124|6|Mentioned|p2 Fig.1|||||||Equivalent to Edmirringee Volcanics, Kurinelli Sandstone and Rooneys Formation.||
27287|Epenarra Volcanics|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
27287|Epenarra Volcanics|73427|6|Mentioned|p12|||||Ooradidgee Group||||
27287|Epenarra Volcanics|73460|6|Mentioned|p2|||Warramunga Province.||||Overlain by and equivalent to Edmirringee Volcanics and Kurinelli Sandstone. Equivalent to Rooneys Formation.||
27287|Epenarra Volcanics|73550|6|Mentioned|p5|Orosirian|Orosirian||ca 1840 Ma|||||
27287|Epenarra Volcanics|73590|6|Mentioned|p1-2|Orosirian|Orosirian||ca 1840 Ma|Ooradidgee Group||Overlain by and equivalent to Edmirringee Volcanics and Kurinelli Sandstone. Equivalent to Rooneys Formation.||
27150|Ernie Lagoon Member|28255|5|Briefly described|p76|||Of the Ranford Formation (Duerdin Group).||||||
27150|Ernie Lagoon Member|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Ranford Formation (Duerdin Group).  Light brown quartz sandstone; minor grit.||||||02-DEC-04
27150|Ernie Lagoon Member|32701|4|Described|Table 1|||Adelaidean. Duerdin Gp.||||||
27150|Ernie Lagoon Member|45112|5|Briefly described|Table 18|||||||||
27150|Ernie Lagoon Member|48938|2|Defined|p73|Adelaidean|Adelaidean|||||||
27150|Ernie Lagoon Member|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Ranford Formation, Duerdin Group. Overlies Beasley Knob Member. Quartz sandstone, conglomerate.||||||
27150|Ernie Lagoon Member|60682|4|Described|p17 Table 4, 20|Neoproterozoic|Neoproterozoic|Of Ranford Formation. Conformably overlies Beasly Knob Member. Max. thickness: <10m. Medium grained sandstone, conglomerate. Geological Province: Wolfe Creek Basin.||||||
27150|Ernie Lagoon Member|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Ranford Formation, Wolfe Creek Basin. Quartz sandstone, conglomerate ||||||
27150|Ernie Lagoon Member|69442|5|Briefly described|p27:3 Tb.27.1; 27:4|||Wolfe Basin. Less than 10m thick. Fluvio-glacial deposits.||Ranford Formation.||Conformably overlies Beasly Knob Member.|Medium-grained sandstone; subordinate conglomerate as interbeds and lenses.|12-JUL-16
27150|Ernie Lagoon Member|69673|6|Mentioned|p190|||||Ranford Formation||||
27150|Ernie Lagoon Member|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. [previously of Ranford Formation. Ranford Formation not shown in legend]||Duerdin Group|||Quartz sandstone, conglomerate.|18-JUL-16
27150|Ernie Lagoon Member|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
26303|Errolola Sandstone|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hanlon Subgroup (Hatches Creek Group). Quartz arenite, lithic/feldspathic arenite.||||||07-NOV-08
26303|Errolola Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
26303|Errolola Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Hanlon Subgroup.  Geological Province: Davenport Province.||||||
26303|Errolola Sandstone|24172|5|Briefly described|p37, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Underlain by Kudinga Basalt. Geological Province: Tennant Inlier. Commonly downfaulted against the Unimbra Sandstone.||||||07-NOV-08
26303|Errolola Sandstone|39624|5|Briefly described|Table 1|||||||||
26303|Errolola Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26303|Errolola Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Quartz arenite, feldspathic arenite; conglomerate||||||10-JAN-05
26303|Errolola Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26303|Errolola Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26303|Errolola Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Quartz arenite and subordinate feldspathic arenite; rare pebbly arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
26303|Errolola Sandstone|41129|4|Described|Table 1|||Mention p1.||||||16-AUG-06
26303|Errolola Sandstone|41204|4|Described|Table 1|||||||||
26303|Errolola Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup. Quartz arenite, lithic/feldspathic arenite.||||||16-NOV-05
26303|Errolola Sandstone|41308|5|Briefly described|Table 2|||||||||
26303|Errolola Sandstone|41310|4|Described|Table 1|||||||||
26303|Errolola Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
26303|Errolola Sandstone|41524|4|Described|Table 1|||||||||
26303|Errolola Sandstone|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Quartz arenite, some feldspathic; pebbly.||||||07-NOV-08
26303|Errolola Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
26303|Errolola Sandstone|42643|4|Described|p12, Table 1 p6|||||||||
26303|Errolola Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Quartz arenite, feldspathic/lithic/kaolinitic arenite.||||||07-NOV-08
26303|Errolola Sandstone|43224|5|Briefly described|Map legend||Paleoproterozoic|Of Hanlon Subgroup.||||||07-NOV-08
26303|Errolola Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
26303|Errolola Sandstone|45167|3|Fully described|Table 1|||Of Hanlon Subgroup.||||||16-AUG-06
26303|Errolola Sandstone|49033|2|Defined|p25|Proterozoic|Proterozoic|||||||
26303|Errolola Sandstone|60681|5|Briefly described|Map legend|Statherian|Statherian|Of the Hatches Creek Group.  Feldspathic sublithic arenite.  Geological Province: Davenport Province.||||||11-JAN-05
26303|Errolola Sandstone|60684|5|Briefly described|p12, p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Quartz arenite and feldspathic arenite; pebble conglomerate.  Overlies Kudinga Basalt? ; downfaulted against Unimbra Sandstone. geological Province: Davenport province.||||||07-NOV-08
26303|Errolola Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Feldspathic sublithic arenite, quartz arenite; minor conglomerate. Overlies Kudinga Basalt; underlies Alinjabon Sandstone. In the Tennant Creek region.||||||07-NOV-08
26303|Errolola Sandstone|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Geological Province: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
26303|Errolola Sandstone|64735|5|Briefly described|p205 Fig 1, p206 Fig 2, p211, p214||Orosirian|Age from youngest detrital zircons.|Max depositional age 1810+/-32 Ma.|Of Hanlon Subgroup, Hatches Creek Group.||Overlies Kudinga Basalt.||20-APR-12
26303|Errolola Sandstone|65209|5|Briefly described|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||lowermost sandstone interval of Morphett Creek Formation (Tomkinson Creek Group) correlates with Errolola Sandstone (Hatches Creek Group).||
26303|Errolola Sandstone|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of Hanlon Subgroup, Hatches Creek Group, Davenport Province. Overlies Kudinga Basalt of Wauchope Subgroup. Feldspathic sublithic arenite and quartz arenite. Cross-section only||||||
26303|Errolola Sandstone|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of Hanlon Subgroup of Hatches Creek Group. Wauchope Subgroup rocks. Non-outcropping. Inferred feldspathic sublithic arenite and quartz arenite.||||||
26303|Errolola Sandstone|65338|5|Briefly described|p20.|Paleoproterozoic|Paleoproterozoic|Ridge-forming outcrops. See also misspelling Erololla Sandstone p6.||Unit in Hanlon Subgroup, Hatches Creek Group.|||Quartz-rich sandstone.|19-OCT-11
26303|Errolola Sandstone|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup.||Overlies (possibly unconformably) Kudinga Basalt. Is overlain by Alinjabon Sandstone.|Quartz arenite; subordinate feldspathic arenite; rare pebbly arenite.|
26303|Errolola Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Kudinga Basalt. Is overlain by Alinjabon Sandstone.|Feldspathic sublithic arenite, quartz arenite; minor conglomerate.|
26303|Errolola Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1819 +/- 23 Ma (maximum depositional age).|Hatches Creek Group.||||
26303|Errolola Sandstone|67352|4|Described|p9 Tb.1, p44 Fig.48, p45|Statherian|Statherian|Region-wide bevelled, ridge-forming unit.||Hanlon Subgroup||Overlies (conformably) Kudinga Basalt. Is overlain conformably by Alinjabon Sandstone.|Quartz arenite, subordinate feldspathic and lithic arenite: medium bedded, medium grained, well sorted; rare pebble beds.|
26303|Errolola Sandstone|68518|4|Described|p6 Tb.1, p13|Proterozoic|Proterozoic|Thickness: 200-800 m. Probably deposited on intertidal flats and adjoining subtidal environments.||Hanlon Subgroup||Conformable on Kudinga Basalt; overlain conformably by Alinjabon Sandstone and unconformably by Cambrian strata.|Ridge-forming feldspathic/lithic arenite and quartz arenite; subordinate recessive friable arenite in southeast.|30-MAY-16
26303|Errolola Sandstone|69424|6|Mentioned|p9:10 Fig.9.9|||Murchison Syncline, Murchison Ranges.||||||12-JUL-16
26303|Errolola Sandstone|69425|4|Described|p10:3,10,12-14,17-20,23, 24 Fig. 10.19|Statherian|Statherian|Ridge-forming. 100-over 1200m thick. Intertidal and adjacent subtidal deposits. Maximum deposition age.|1816 +/- 9 Ma (Claoue-Long et al., 2008).|Basal Hanlon Subgroup.||Conformably (locally disconformably) overlies Kudinga Basalt. Is overlain conformably by Alinjabon Sandstone. Correlated with part of Kuerschner Member (Morphett Creek Formation).|Generally medium-grained and well-sorted, feldspathic-sublithic sandstone, quartz sandstone; minor conglomerate in upper part of unit in the NW; rare claystone.|12-JUL-16
26303|Errolola Sandstone|69431|6|Mentioned|p16:5, 22|||Davenport Province. Folding during the Davenport Event is discussed.||Hanlon Subgroup.||||12-JUL-16
26303|Errolola Sandstone|73083|6|Mentioned|p10, p19, p23|||||||Underlain by Kudinga Basalt.||
70576|Esther Granite|61246|6|Mentioned|p51|||||||||
70576|Esther Granite|65338|3|Fully described|p17, pp22-27, p81, App 2|Statherian|Statherian|Newly defined. Well-developed sub-magmatic foliations defined by elongate K-feldspar megacrysts and biotite. Geochemistry, local textural varieties including extreme (to 15 cm) K-feldspar megacrysts, and deformational microstructures, are detailed.|1789 +/- 6 Ma (Cross et al. 2005).|||Intrudes Lander Rock Formation. Is unconformably overlain by Boko, Grant Bluff and Central Mount Stuart Formations.|Grey, biotite-granite, K-feldspar megacrystic; tourmaline-bearing; locally greisenous; aplite; pegmatite.|
70576|Esther Granite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
70576|Esther Granite|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-granite with K-feldspar megacrysts and tourmaline; aplite; pegmatite; locally phyllonitic or mylonitic.|
70576|Esther Granite|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-granite, megacrystic K-feldspar-bearing, tourmaline-bearing; also equigranular/seriate porphyritic variants, and combined elongate and equant K-feldspar megacrystic textural variant; aplite, pegmatite; locally phyllonitic or mylonitic.|
70576|Esther Granite|69427|4|Described|p12:20 Fig.12.19; 12:22, 59|Statherian|Statherian|Donnellan (2008). Aileron Province. Crops out sporadically over c.650 km2. Interpreted to have intruded during (Stafford Event) deformation. SHRIMP U-Pb zircon crystallisation age; inherited cores from 2535-1840 Ma. Tin-rich: probable source of the Anningie pegmatite Sn-Ta field (briefly described).|1789 +/- 6 Ma (Worden et al., 2008).|||Probably intrudes Lander Rock Formation.|Porphyritic, grey, biotite granite with coarse phenocrysts of K-feldspar; locally megacrystic (feldspar to 15cm); also granite with equidimensional, porphyritic K-feldspar to 5cm.|12-JUL-16
70576|Esther Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1789+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyritic biotite granite.|
70576|Esther Granite|71858|6|Mentioned|p5|||Aileron Province.||||||
25899|Ethabuka Sandstone|8187|5|Briefly described|Map legend|Ordovician|Ordovician|Overlain by Cravens Peak beds.||||||24-JUN-04
25899|Ethabuka Sandstone|10116|5|Briefly described|Map Legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose sandstone, mudstone.||||||19-AUG-04
25899|Ethabuka Sandstone|12891|5|Briefly described|p733 Fig. 2|Late Ordovician|Late Ordovician|Geological province: SW Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|12951|5|Briefly described|p143 fig 4, p145 fig 6, p149|Middle Ordovician|Early Ordovician|Toko Syncline, Georgina Basin. ||||||
25899|Ethabuka Sandstone|13995|5|Briefly described|p103|Late Ordovician|Late Ordovician|Georgina Basin. At least in part fluvial deposits.||||||
25899|Ethabuka Sandstone|22646|6|Mentioned|Fig 5 on p 105||Late Ordovician|Georgina Basin.||||||
25899|Ethabuka Sandstone|22954|6|Mentioned|Fig3p9|Llanvirnian|Llanvirnian|||||||
25899|Ethabuka Sandstone|23858|5|Briefly described|p916|||Geological Province: Georgina Basin. Max thickness: ~1150 m.||||||
25899|Ethabuka Sandstone|24442|6|Mentioned|p49|||||||||
25899|Ethabuka Sandstone|36234|6|Mentioned|Fig.1|||||||||
25899|Ethabuka Sandstone|36580|2|Defined|p469|Middle Ordovician|Middle Ordovician|||||||
25899|Ethabuka Sandstone|38832|6|Mentioned|p157|||||||||
25899|Ethabuka Sandstone|39445|5|Briefly described|Table 4|||Toko Group. See also p1.||||||18-SEP-06
25899|Ethabuka Sandstone|39921|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
25899|Ethabuka Sandstone|40136|5|Briefly described|p24|||||||||
25899|Ethabuka Sandstone|41524|6|Mentioned|Fig.3|||||||||
25899|Ethabuka Sandstone|43105|5|Briefly described|Fig.4,p9.|||||||||
25899|Ethabuka Sandstone|45155|6|Mentioned|Fig.8|||||||||
25899|Ethabuka Sandstone|46973|5|Briefly described|p52|||||||||
25899|Ethabuka Sandstone|47024|6|Mentioned|Fig.6|||||||||
25899|Ethabuka Sandstone|49027|4|Described|p20|||||||||
25899|Ethabuka Sandstone|60122|3|Fully described|p33-34, p4-5|Middle Ordovician|Middle Ordovician|Formerly Ethabuka beds, or attributed to Cravens Peak beds. Conformable over Mithaka Fm; unconformable below Cravens Peak beds and poodyea Fm; unconformably overlain by Hooray Sandstone in MOUNT WHELAN. Max. thick: 1147m in MT WHELAN. See also p10 Tb. 1.||||||18-SEP-06
25899|Ethabuka Sandstone|60590|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Quartzose and quartzofeldspathic sandstone, minor siltstone and claystone.||||||
25899|Ethabuka Sandstone|61404|5|Briefly described|Map legend|Middle Ordovician|Middle Ordovician|Of the Toko Group. Quartzose and quartzofeldspathic sandstone, minor siltstone and claystone. Geological Province: southern Georgina Basin.||||||12-OCT-05
25899|Ethabuka Sandstone|63450|4|Described|p78 Fig. 5, p82, p84|Llanvirn|Llanvirn|Conformable over Mithaka Formation. Thickness: 1147m in AOD Ethabuka 1; <40m in outcrop. Geological province: Georgina Basin, West Toko Syncline. Contains quartzose sandstone, quartzofeldspathic sandstone, siltstone and mudstone.||||||07-FEB-11
25899|Ethabuka Sandstone|63562|6|Mentioned|p338 fig 3, p350|Late Ordovician|Late Ordovician|Of Georgina Basin. Sediment source was from uplifted areas between the Amadeus and Georgina Basins. Non-marine. Toko Syncline area.||||Correlated with Carmichael Sandstone.||06-DEC-17
25899|Ethabuka Sandstone|64068|3|Fully described|p78|Late Ordovician|Late Ordovician|||Of Toko Group.||Conformably and gradationally overlies Mithaka Formation. Is unconformably overlain by Cravens Peak beds or, where absent, Hooray Sandstone.|Sublabile to quartzose sandstone; minor siltstone and claystone interbeds; rare conglomerate.|04-APR-12
25899|Ethabuka Sandstone|64778|6|Mentioned|p13|Ordovician|Ordovician|Toko Syncline, Southern Georgina Basin.||||||
25899|Ethabuka Sandstone|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|64813|5|Briefly described|p256 Fig. 3|Middle Ordovician|Middle Ordovician|Geological Province: southern Georgina Basin.||||||11-FEB-09
25899|Ethabuka Sandstone|65237|5|Briefly described|p4 Fig. 7, p10|Ordovician|Ordovician|Geological province: southern Georgina Basin.||||||07-FEB-11
25899|Ethabuka Sandstone|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 Mithaka Formation. Is overlain by Longsight Sandstone.|Quartzose to sublabile sandstone, mudstone, siltstone, clay pellet conglomerate.|
25899|Ethabuka Sandstone|67402|5|Briefly described|p25 tbl RRM3|Gisbornian|Darriwillian|Georgina Basin, West Toko Syncline. Maximum thickness of 778m. Deposited in a sub-tidal and high energy shoreline environment. See also  p213 fig GRG3, p215, p216, p217.||||Overlies the Mithaka Formation. Unconformably overlain by the Craven Peak beds.|Quartzose sandstone, quartzo-feldspathic sandtone, siltstone and mudstone.|
25899|Ethabuka Sandstone|69437|5|Briefly described|p22:10|Ordovician|Ordovician|Southern Georgina Basin.||||Overlies Mithaka Formation.||12-JUL-16
25899|Ethabuka Sandstone|69443|3|Fully described|p28:7, 27, 29-30|Late Ordovician|Late Ordovician|Draper (1980) after Mulready (1975). Southern Georgina Basin. Forms prominent ridges and uplands. 1147m thick in the type section in drillhole Ethabuka-1 in MOUNT WHELAN map area, Qld. In NT only c.35m of the lower part is exposed. Sedimentary structures describedl; undescribed fossil fauna listed.||Toko Group.||Conformably and gradationally overlies Mithaka Formation. Is overlain unconformably by Cravens Peak beds or Hooray Sandstone.|(Lower part): sublabile to quartzic sandstone; minor siltstone and claystone interbeds; rare conglomerate.|12-JUL-16
25899|Ethabuka Sandstone|69458|6|Mentioned|p42:20|||Georgina Basin.||||Is overlain unconformably by Poodyea Formation.||14-SEP-18
25899|Ethabuka Sandstone|69591|3|Fully described|p87, p95-97|Ordovician|Ordovician|West Toko Syncline, Georgina Basin. Draper (1980). The type section is in AOD Ethabuka 1 borehole, resting on Mithaka Formation, and comprises 1147m of very fine to medium sandstone with siltstone interbeds and rare pebble layers. Up to 35m thick. (Some?) rocks of this unit, along the Toomba Range SW of Boulia, were originally mapped as Cravens Peak beds. Appears doubly mis-spelt on p87 as Ethubuka Standstone.||Toko Group.||Conformably overlies Mithaka Formation.|Fine- to medium-bedded (minor thicker beds and flaser bedding), fine-grained quartzose to sublabile sandstone overlain by friable fine sandstone with minor phosphate pellet conglomerate; some siltstone, mudstone and (in upper part) claystone beds.|
25899|Ethabuka Sandstone|69599|6|Mentioned|p600|||||||Is overlain unconformably by the Poodyea Formation.||
25899|Ethabuka Sandstone|69673|5|Briefly described|p114 fig 92, p118, p119 fig 94|Ordovician|Ordovician|35m thick.||Toko Group||Overlies Mithaka Formation|Sandstone with minor siltstone and claystone interbeds with rare conglomerate.|
25899|Ethabuka Sandstone|70380|6|Mentioned|p745|Hirnantian|Katian|Southern Georgina Basin.||||||
25899|Ethabuka Sandstone|71800|6|Mentioned|p26 fig 3|Late Ordovician|Late Ordovician|Georgina Basin.||||||
28237|Eurowie Sandstone Member|9694|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Of the Arrinthrunga Formation. Geological Province: Georgina Basin. Fine to medium thin bedded quartz sandstone, siltstone, shale and dolostone.||||||
28237|Eurowie Sandstone Member|12951|5|Briefly described|p143 fig 4, p148|Late Cambrian|Late Cambrian|Georgina Basin. Age assumed from parent Formation.||Of Arrinthrunga Formation.|||Quartzic dolostone and minor quartz sandstone.|
28237|Eurowie Sandstone Member|22954|6|Mentioned|Fig3p9|Idamean|Mindyallan|||||||
28237|Eurowie Sandstone Member|37572|5|Briefly described|p161|||||||||
28237|Eurowie Sandstone Member|40538|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Arrinthrunga Formation. Quartz arenite; rare siltstone; thin-bedded, red-brown: halite pseudomorphs and abundant ripple marks. Geological Province: Georgina Basin.||||||15-NOV-05
28237|Eurowie Sandstone Member|40906|4|Described|p26|||||||||
28237|Eurowie Sandstone Member|41524|6|Mentioned|p21|||See also Plate 9.||||||18-SEP-06
28237|Eurowie Sandstone Member|42504|5|Briefly described|Table 54 P79|||||||||
28237|Eurowie Sandstone Member|44327|2|Defined|Tb.I,p.10,map||Late Cambrian|(F53-11). Upper Cambrian.||||||11-FEB-09
28237|Eurowie Sandstone Member|44328|14|Not recorded|map legend||Late Cambrian|Upper Cambrian.||||||
28237|Eurowie Sandstone Member|45052|3|Fully described|p109|||U.Camb. See also p32.||||||18-SEP-06
28237|Eurowie Sandstone Member|48844|2|Defined|p.39-40|||On many pages. p. 39-40,43-46,68. Pl.8. (F53-11). Member of Arrinthrunga Fm.||||||07-MAY-13
28237|Eurowie Sandstone Member|60122|4|Described|p20|Late Cambrian|Late Cambrian|Of the Arrinthrunga Formation. Quartz sandstone and quartzic dolostone. Transitional within parent formation. Max. thickness: 60m. Geological Province: Georgina Basin. See also p10 Tb. 1, p19.||||||18-SEP-06
28237|Eurowie Sandstone Member|60551|5|Briefly described|Map Legend|Late Cambrian|Cambrian|Of the Arrinthrunga Formation. Geological province: Georgina Basin.  Fine to medium thin bedded quartz sandstone, calcareous siltstone, shale and dolostone; rare quartz granule conglomerate.||||||
28237|Eurowie Sandstone Member|61022|5|Briefly described|p15 Fig. 2|Late Cambrian|Late Cambrian|Of the Arrinthrunga 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.||||||20-APR-05
28237|Eurowie Sandstone Member|61404|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Arrinthrunga Formation (Narpa Group).  Quartz arenite; rare  siltstone; halite pseudomorphs.  Geological Province: southern Georgina Basin.||||||
28237|Eurowie Sandstone Member|62376|5|Briefly described|p53|Late Cambrian|Late Cambrian|Geological Province: Georgina Basin. Of the Arrinthrunga Formation.||||||09-FEB-10
28237|Eurowie Sandstone Member|62789|6|Mentioned|p129 Fig. 2|Late Cambrian|Late Cambrian|Southern Georgina Basin.||Of Arrinthrunga Formation.||||28-MAR-12
28237|Eurowie Sandstone Member|64068|4|Described|p67, p25, p38, p ix|Late Cambrian|Late Cambrian|||Of Arrinthrunga Formation.|||Quartz sandstone and quartzic dolostone with distinctive halite hopper casts; minor shale, siltstone.|05-APR-12
28237|Eurowie Sandstone Member|64778|6|Mentioned|p13|Cambrian|Cambrian|Toko Syncline, Southern Georgina Basin.||||||
28237|Eurowie Sandstone Member|64812|5|Briefly described|p237 Fig. 2|Late Cambrian|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
28237|Eurowie Sandstone Member|64813|5|Briefly described|p256 Fig. 3|Late Cambrian|Late Cambrian|Geological Province: southern Georgina Basin.||||||11-FEB-09
28237|Eurowie Sandstone Member|65237|5|Briefly described|p3 Fig. 4|Late Cambrian|Late Cambrian|Geological province: southern Georgina Basin.||||||07-FEB-11
28237|Eurowie Sandstone Member|65342|6|Mentioned|p7.|||Georgina Basin. Max. thickness at least 45 m.||Unit in Arrinthrunga Formation.||||
28237|Eurowie Sandstone Member|66767|5|Briefly described|p59|Cambrian|Cambrian|Southern Georgina Basin.||Arrinthrunga Formation.|||Quartz sandstone and quartz-rich dolostone with distinctive halite hopper casts.|
28237|Eurowie Sandstone Member|69443|4|Described|p28:19, 31, 35-36, 40|Late Cambrian|Late Cambrian|K.G. Smith (1964). Georgina Basin. 40-60m thick; maximum 107m. Intermittently emergent hypersaline shoreline depositional environment. Associated with the global SPICE (Steptoean Positive Carbon Isotope Excursion) Event. Associated with the Box Hole-Turkey Creek Pb-Zn prospect and abandoned mine.||Arrinthrunga Formation.|||Quartz sandstone and quartzose dolostone with distinctive halite hopper casts; minor shale.|12-JUL-16
28237|Eurowie Sandstone Member|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin.||Arrinthrunga Formation||||
28237|Eurowie Sandstone Member|72321|6|Mentioned|Fig 2|Pabian|Pabian|Elkedra Shelf/Dulcie Syncline, Toko Syncline, Georgina Basin. Australian stage: Idamean.||of Narpa Group.|Of Arrinthrunga Formation.|||
28237|Eurowie Sandstone Member|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Aileron Province. Cotains fossil trilobites.||Arrinthrunga Formation||Underlain by Steamboat Sandstone.|Quartz sandstone, quartzose dolostone with halite hopper clasts and minor shale.|05-JUL-22
28237|Eurowie Sandstone Member|72516|4|Described|p12, p93-p94|Furongian|Furongian|Georgina Basin. Outcrops as rubbly outcrops to prominent hills and recessive lithologies in HUCKITTA, ELKEDRA; occurs in the subsurface of TOBERMORY map sheet. In the Jervois Range Special sheet it outcrops in the northwestern corner of the map. Conformable relationships with undifferentiated Arrinthrunga Formation. 40-60m thick in the map sheet area, 107m thick in HUCKITTA. Deposited in an intermittently emergent hypersaline shoreline environment.||Arrinthrunga Formation.||Equivalent to the Georgina Limestone, Mungerebar Limestone, Selwyn Range Limestone, O'Hara Shale, Cleland Sandstone and the Goyder Formation.|Quartz sandstone, quartz dolostone with halite hopper clasts; minor shale.|
31357|Eva Springs Member|43275|5|Briefly described|Map Legend||Neoproterozoic|Of Vaughan Springs Quartzite.||||||
31357|Eva Springs Member|44158|4|Described|p25 Table.2|Neoproterozoic|Neoproterozoic|Of Vaughan Springs Quartzite.||||||18-SEP-06
31357|Eva Springs Member|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Vaughan Springs Quartzite. Quartz sandstone. Geological Province: Ngalia Basin.||||||
31357|Eva Springs Member|65338|6|Mentioned|pp57-58.|||||Unit in Vaughan Springs Quartzite.||Overlies Treuer Member.||
31357|Eva Springs Member|69439|3|Fully described|p24:2-6|Cryogenian|Cryogenian|Young et al. (1995). Ngalia Basin, Centralian A Superbasin. Supersequence 1. Forms prominent strike ridges in the Treuer Range. Is c.900m thick in the Vaughan Springs Syncline, the type area for the Formation.||Vaughan Springs Quartzite.||Conformably overlies Treuer Member. Is overlain conformably or disconformably by Mount Doreen Formation and Mount Eclipse Sandstone.|Medium- to thickly-bedded quartz sandstone; has abundant cross-beds and some ripple marks.|12-JUL-16
31357|Eva Springs Member|69673|6|Mentioned|p105, p107 fig 85|||||Vaughan Springs Quartzite||Overlain by Albinia Formation, overlies Treuer Member||
31308|Fagan Supersuite|50591|5|Briefly described|p4.1-4.4, p1.3 Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1710-1715Ma. Geological Province: Arnhem Block/McArthur Basin.||||||24-FEB-10
24971|Fagan Volcanics|22538|5|Briefly described|P715|||||||||
24971|Fagan Volcanics|22600|4|Described|Map legend|Statherian|Statherian|||||||
24971|Fagan Volcanics|22665|6|Mentioned|P231|||Age of unit is 1706+/-10 Ma||||||
24971|Fagan Volcanics|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|||||||
24971|Fagan Volcanics|24048|3|Fully described|p27|Statherian|Statherian|Composed of the Maidjunga Member, Sheridan Member and Dhupuwamirri Member.  Age: 1707+/-12Ma, 1706+/-10Ma (SHRIMP U-Pb).  Parent: Donydji Group.  Max. thickness: 1200m.  Geological Province: McArthur Basin||||||18-SEP-06
24971|Fagan Volcanics|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Includes Dhupuwamirri Member, Sheridan Member, and Maidjunga Member. Geol. Prov: McArthur Basin.||||||12-OCT-05
24971|Fagan Volcanics|24050|6|Mentioned|p27|||||||||
24971|Fagan Volcanics|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Rocks of lava domes and flows.||||||07-FEB-11
24971|Fagan Volcanics|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24971|Fagan Volcanics|32660|5|Briefly described|Table 2|||||||||
24971|Fagan Volcanics|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24971|Fagan Volcanics|37565|6|Mentioned|Fig.5|||||||||
24971|Fagan Volcanics|37568|6|Mentioned|Fig.5|||||||||
24971|Fagan Volcanics|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
24971|Fagan Volcanics|42597|5|Briefly described|Map Legend|Carpentarian||||||||
24971|Fagan Volcanics|43010|2|Defined|p70||Paleoproterozoic|of Orosirian age.||||||07-NOV-08
24971|Fagan Volcanics|44112|3|Fully described|p10,22,31,37||Statherian|Belongs to Supersequence 1(D). Max Age: between 1706 (+/-) 10 and 1707 (+/-) 12 Ma||||||
24971|Fagan Volcanics|44299|4|Described|p.9||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
24971|Fagan Volcanics|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L.Proterozoic.||||||07-NOV-08
24971|Fagan Volcanics|45087|5|Briefly described|p111|||Chemical analyses.||||||
24971|Fagan Volcanics|48867|14|Not recorded|p.7|||Resemble Edith Creek Volcanics.||||||
24971|Fagan 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: 1707-1706 +/- 12Ma (Shrimp).||||||07-NOV-08
24971|Fagan Volcanics|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Includes Dhupuwamirri Member, Sheridan Member, and Maidjunga Member. Geol. Prov: McArthur Basin.||||||
24971|Fagan Volcanics|63866|5|Briefly described|p114, p117|||Leichhardt/Calvert Superbasins. |~1706 Ma mean age (Page, OZCHRON)|Donydji Group||Unconformably overlies the Dhunganda Formation. Conformably overlain by the Parsons Range Group.||13-APR-18
24971|Fagan Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Walker Fault Zone, McArthur Basin.||Of the Donydji Group.|Includes the Dhupuwamirri Member, Sheridan Member, Maidjunga Member.||Felsic volcanics, mafic volcanics.|05-JUN-18
24971|Fagan 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.||
24971|Fagan Volcanics|65337|6|Mentioned|p15.|||Northern McArthur Basin. Contains peperite, closely resembling Top Rocky Rhyolite breccia.||||||
24971|Fagan Volcanics|69421|5|Briefly described|p6:5|||Probably stratigraphically equivalent to the younger intrusive units in the Mirarrmina Complex.|c.1705 Ma.|Donydji Group.||||12-JUL-16
24971|Fagan Volcanics|69430|4|Described|p15:3-4, 6-7, 13-14|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 1000-1200m thick. SHRIMP U-Pb zircon ages of the bottom and top Members respectively (Page et al., 2000). Also given is 1710 Ma (Pietsch et al., 1994).|1707 +/- 12 to 1706 +/- 10 Ma.|Donydji Group.|Maidjunga, Sheridan, Dhupuwamirri Members.|Overlies Ritarango Formation conformably to disconformably. Is overlain by Mattamurta Sandstone.|A succession of felsic and mafic igneous rocks, sandstone, mudstone and minor conglomeratic and volcaniclastic rocks.|12-JUL-16
24971|Fagan Volcanics|69673|6|Mentioned|p16 fig 13, p17||||1710 Ma|Donydji Group|Includes Dhupuwamirri Member, Sheridan Member, Maidjunga Member|||
24971|Fagan Volcanics|71374|6|Mentioned|p24|Palaeoproterozoic|Palaeoproterozoic|Correlated with undated Proterozoic rhyolite dykes that underlie the Coast Range Sandstone.|1710-1700 Ma |Donydji Group|||Felsic igneous rocks.|
24971|Fagan Volcanics|71592|5|Briefly described|Appendix A.|||Walker Trough, Arnhem Province.|1707+/-12 Ma (crystallisation: U-Pb zircon SHRIMP)||||Rhyolite.|
24971|Fagan Volcanics|71606|5|Briefly described|p135|||McArthur Basin. Associated with Fagan Phase magmatism of Rawlings 1994.||Unit of Donydji Group.||Hosted in the upper Donydji Group.||
24971|Fagan Volcanics|72377|5|Briefly described|iii,p9,12, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Exposed in the Mitchell Ranges Fault Zone and the northern part of the Walker Fault Zone, NNW of the Coast Range in ARNHEM BAY mapsheet. Likely time-equivalent with Haddon Volcanics.||Unit of Donydji Group.|Includes Maidjunga and Dhupuwamirri members.|||10-OCT-19
34086|Fairy Glen Sandstone Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
34086|Fairy Glen Sandstone Member|24048|2|Defined|p99 App. 1|Paleoproterozoic|Paleoproterozoic|See also p47.  Proposer: Ian Sweet.  Of the Badalngarrmirri Formation.  Max. thickness: 100m.  Geological Province: McArthur Basin.||||||07-NOV-08
34086|Fairy Glen Sandstone Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation of Parsons Range Group. Sandstone: thick-bedded, fine to medium-grained, porous, highly ferruginous (glauconitic), hummocky and swaley cross-stratification; minor trough cross-bedded sandstone. Geol. Prov: McArthur Basin.||||||12-OCT-05
34086|Fairy Glen Sandstone Member|44112|6|Mentioned|p50|||||||||
34086|Fairy Glen Sandstone Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation of Parsons Range Group. Sandstone: thick-bedded, fine to medium-grained, porous, highly ferruginous (glauconitic), hummoc ky and swaley cross-stratification; minor trough cross-bedded sandstone. Geol. Prov: McArthur Basin.||||||
34086|Fairy Glen Sandstone Member|69430|5|Briefly described|p15:13|||Southern Walker Fault Zone, McArthur Basin. 0-100m thick. Offshore transition zone deposits within a storm-dominated shelf.||Badalngarrmirri Formation.|||Fine- to medium-grained, thickly bedded, ferruginous (glauconitic?) sandstone.|12-JUL-16
30419|Fanny Rhyolite Member|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Plum Tree Volcanics (Edith River Group).  Massive or layered white to purple-brown massive rhyolite and welded felsic tuff.||||||
30419|Fanny Rhyolite Member|23216|5|Briefly described|p13-4|||||||||
30419|Fanny Rhyolite Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Plum Tree Creek Volcanics. Orosirian age.||||||07-NOV-08
30419|Fanny Rhyolite Member|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1825Ma from parent unit - Plum Tree Creek Volcanics, Edith River Group.  Max. thickness 500m. Massive or layered rhyolite and welded felsic tuff.||||||07-JAN-09
25905|Fargoo Tillite|14019|5|Briefly described|p16, 19|||Of the Duerdin Group. Unconformably overlies: Angalarri Siltstone. Geological Province: Wolfe Creek Basin. Correlated with Olympic Formation. Possibly equivalent to diamictite of the Duerdin Group.||||||
25905|Fargoo Tillite|23314|6|Mentioned|334|||||||||
25905|Fargoo Tillite|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
25905|Fargoo Tillite|28255|3|Fully described|p71, Tb. 11(opp.p8)|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite and dolomitic conglomerate. Conformably overlies, and intertongues with, Skinner Sandstone; unconformably overlain by Blackfellow Creek Sandstone (AUVERGNE sheet).  Max. thickness: >20m.||||||18-SEP-06
25905|Fargoo Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25905|Fargoo Tillite|31645|6|Mentioned|Table 2|||Correlation||||||
25905|Fargoo Tillite|32660|5|Briefly described|Table 6|||||||||
25905|Fargoo Tillite|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite, dolomite clasts common.||||||02-DEC-04
25905|Fargoo Tillite|32701|4|Described|Table 1|||Adelaidean. Duerdin Gp. See p14.||||||18-SEP-06
25905|Fargoo Tillite|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25905|Fargoo Tillite|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite, dolomite conglomerate lenses. Intertongues with Skinner Sandstone in east; unconformable on Angalarri Siltstone farther west.||||||26-APR-05
25905|Fargoo Tillite|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25905|Fargoo Tillite|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite, dolomite, conglomerate.||||||27-APR-05
25905|Fargoo Tillite|36888|4|Described|p215|||||||||
25905|Fargoo Tillite|36898|6|Mentioned|p181|||||||||
25905|Fargoo Tillite|37462|5|Briefly described|p293|||||||||
25905|Fargoo Tillite|37927|4|Described|p504|||||||||
25905|Fargoo Tillite|38157|6|Mentioned|Table X|||||||||
25905|Fargoo Tillite|39210|5|Briefly described|Fig.18|||||||||
25905|Fargoo Tillite|41405|5|Briefly described|p206|||||||||
25905|Fargoo Tillite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
25905|Fargoo Tillite|44140|5|Briefly described|p300, p301 fig 4-7, p303 Tb. 4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. Correlated with Marinoan glaciation (670 Ma). Up to 200 m thick.||Duerdin Group||Overlain conformably by Frank River Sandstone.|Tillite with large lenses of boulder conglomerate.|07-MAR-18
25905|Fargoo Tillite|44317|4|Described|Table 3||Adelaidean|||||||
25905|Fargoo Tillite|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25905|Fargoo Tillite|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
25905|Fargoo Tillite|45041|6|Mentioned|p45|||Refers Dow & Gemuts (1969)||||||
25905|Fargoo Tillite|45047|2|Defined|p82|Adelaidean|Adelaidean|See also pp83,36,38,40.||||||18-SEP-06
25905|Fargoo Tillite|45112|4|Described|p39|||p39.||||||18-SEP-06
25905|Fargoo Tillite|48927|6|Mentioned|Table 1|||Refers Dow & Gemuts (1969)||||||
25905|Fargoo Tillite|48938|4|Described|p65|||See also pp66-67. Section p98.||||||18-SEP-06
25905|Fargoo Tillite|48943|3|Fully described|p80|||||||||
25905|Fargoo Tillite|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Unconformably overlies Skinner Sandstone. Overlain by Blackfellow Creek Sandstone. Diamictite, abundant dolostone clasts.||||||21-JUL-04
25905|Fargoo Tillite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Matrix-supported, polymictic pebble-boulder conglomerate, and sandstone; clasts in conglomerate are polished and striated locally.||||||
25905|Fargoo Tillite|60682|4|Described|p17 Table 4, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Conformably overlies Skinner Sandstone. Unconformably overlain by Blackfellow Creek Sandstone. Max. thickness: >100m. Geological Province: Wolfe Creek Basin.||||||
25905|Fargoo Tillite|63458|6|Mentioned|p872-889, p891, p893, p896-897, p900. |Cryogenian|Cryogenian|East Kimberley region. Overlies striated pavement.||Unit in Duerdin Group.||Correlated with Olympic Formation. Is overlain by Frank River Sandstone.|Diamictite and conglomerate.|
25905|Fargoo Tillite|63762|5|Briefly described|p19|||See also Fargoo Formation.||||||07-FEB-11
25905|Fargoo Tillite|64104|6|Mentioned|p63|Neoproterozoic|Neoproterozoic|The author proposes this name be replaced by Fargoo Formation "to distinguish stratigraphic terms from genetic interpretation". Whatever; see references to Fargoo Formation throughout the article.||||||
25905|Fargoo Tillite|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Diamictite, abundant dolostone clasts||||||
25905|Fargoo Tillite|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Overlies Skinner Sandstone. Is unconformably overlain by Blackfellow Creek Sandstone.|Diamictite with locally abundant dolostone clasts, dolostone, conglomerate.|
25905|Fargoo Tillite|67484|6|Mentioned|p295 Fig.2|Cryogenian|Cryogenian|More commonly referred to as the Fargoo Formation in the Text.||Of the Duerdin Group.||||
25905|Fargoo Tillite|68244|6|Mentioned|p667|Neoproterozoic|Neoproterozoic|See Fargoo Formation.||||||
25905|Fargoo Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
25905|Fargoo Tillite|68473|6|Mentioned|p531-532|||Adelaide Rift Complex.||Duerdin Group||||
25905|Fargoo Tillite|68733|6|Mentioned|p177 Fig.2, p188, p189 Fig.8|Cryogenian|Cryogenian|Victoria and Wolfe basin.||Of the Duerdin Group.|||Glacigenic sediments.|05-DEC-17
25905|Fargoo Tillite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin||Duerdin Group|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|31-JUL-15
25905|Fargoo Tillite|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|||Duerdin Group|||Massive, matrix supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|
25905|Fargoo Tillite|69418|6|Mentioned|p3:31|||Wolfe Basin. Hosts barite at the Newry deposit (briefly described).||||||12-JUL-16
25905|Fargoo Tillite|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Skinner Sandstone. Is overlain by Blackfellow Creek Sandstone.||12-JUL-16
25905|Fargoo Tillite|69442|5|Briefly described|p27:1-4, 6-7|||Wolfe Basin. Over 100m thick. Glacial deposits. Low-angle unconformity at the top. Hosts a small uneconomic vein of barite in a minor fault at the Newry prospect.||Duerdin Group.||Conformably overlies Skinner Sandstone. Is overlain unconformably by Blackfellow Creek Sandstone. Correlated with Olympic Formation (Amadeus Basin).|Diamictite: characterised by a predominance of dolostone boulders, some of which are stromatolitic; many have a foetid odour when broken.|12-JUL-16
25905|Fargoo Tillite|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.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally|
25905|Fargoo Tillite|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|More than 100m thick.||Duerdin Group|||Tillite with dolostone boulders.|
25905|Fargoo Tillite|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Massive matrix supported polymictic pebble to boulder conglomerate and poorly sorted massive sandstone.|
25905|Fargoo Tillite|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Diamictite, abundant dolostone clasts.|
25905|Fargoo Tillite|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Duerdin Group.||Shown as overlying Skinner Sandstone, and overlain by Blackfellow Creek Sandstone, unconformably.|Diamictite with locally abundant dolostone clasts, dolostone, conglomerate.|
25905|Fargoo Tillite|71267|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv.|720-635 Ma (inferred)|Unit of Duerdin Group.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally|
25905|Fargoo Tillite|73255|6|Mentioned|p534 Fig.2, p548 Fig.12|Cryogenian|Cryogenian|||Duerdin Group||Disconformably overlies the Helicopter Siltstone, underlies the Frank River Sandstone.||
27154|Farquharson Sandstone|14019|5|Briefly described|p9, 28|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Fine sublitharenite and quartz arenite, dolomitic siltstone; minor dolostone and mudstone. Conformable on Kunja Siltstone; conformably overlain by Blue Hole Formation.  Thickness 110m. Geological Province: Birrindudu Basin.||||||07-NOV-08
27154|Farquharson Sandstone|23809|5|Briefly described|p48|||Of the Limbunya Group.  Overlain by the Bluehole Formation.  Geological Province: Victoria-Birrindudu Basins.||||||
27154|Farquharson Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
27154|Farquharson Sandstone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
27154|Farquharson Sandstone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Kunja Siltstone; overlain by Blue Hole Formation. Geological Province: Birrindudu Basin.||||||
27154|Farquharson Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
27154|Farquharson Sandstone|28255|3|Fully described|p20-21, Tb.11 (opp.p8)|||Of the Limbunya Group. Fine-grained, poorly sorted sandstone with interbeds of siltstone in lower part. Conformably overlain by Blue Hole Formation; conformably overlies Kunja Siltstone.  Max. thickness: 110m. See also p123-125 Appendix.||||||17-JUN-05
27154|Farquharson Sandstone|30003|4|Described|p9|||Of the Limbunya Group. Carpentarian or Adelaidean. Max. thickness: 111m.||||||19-APR-05
27154|Farquharson Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
27154|Farquharson Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
27154|Farquharson Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Fine and medium quartz sandstone, minor siltstone.  Conformably overlies the Kunja Siltstone; conformably overlain by the Blue Hole Formation.   Carpentarian or Adelaidean (per legend).||||||17-NOV-04
27154|Farquharson Sandstone|32660|5|Briefly described|Table 6|||||||||
27154|Farquharson Sandstone|33375|6|Mentioned|p9 Tb. 1|||Of the Limbunya Group. Medium quartz sandstone. Max. thickness: 50m. Conformable on Kunja Siltstone. Age is Carpentarian or Adelaidean.||||||28-APR-05
27154|Farquharson Sandstone|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27154|Farquharson Sandstone|33378|5|Briefly described|Map legend|||Of the Limbunya Group. Medium quartz sandstone. Age is Carpentarian or Adelaidean.||||||27-APR-05
27154|Farquharson Sandstone|45112|5|Briefly described|Table 7|||||||||
27154|Farquharson Sandstone|48943|2|Defined|p23|Proterozoic|Proterozoic|Strat. section p132.||||||18-SEP-06
27154|Farquharson Sandstone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Micaceous sublitharenite, siltstone, mudstone.  Conformably overlies the Kunja Siltstone; conformably overlain by Blue Hole Formation. Geol. Prov. Birrindudu Basin.||||||07-NOV-08
27154|Farquharson Sandstone|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Fine to medium quartz sandstone, minor siltstone. Of Limbunya Group. Overlain by Blue Hole Formation. Overlies Kunja Siltstone. Geological Province: Birrindudu Basin.||||||07-NOV-08
27154|Farquharson Sandstone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
27154|Farquharson Sandstone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Kunja Siltstone. Is overlain by Blue Hole Formation.||
27154|Farquharson Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Kunja Siltstone. Is overlain by Blue Hole Formation.|Medium quartz sandstone, micaceous sublithic sandstone.|
27154|Farquharson Sandstone|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||05-DEC-17
27154|Farquharson Sandstone|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
27154|Farquharson Sandstone|69432|4|Described|p17:2, 7|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 115m thick. Moderate- to low-energy, mostly shallow-marine to fluvial and evaporitic deposits.||Limbunya Group.||Conformably overlies Kunja Siltstone.|Blocky and massive sandstone with interbeds of siltstone and mudstone and minor variably stromatolitic dolostone near the top. Ripples, mudcracks and synaeresis cracks are common.|12-JUL-16
27154|Farquharson Sandstone|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Kunja Siltstone, overlain by Blue Hole Formation||
27154|Farquharson Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Limbunya Group.||Overlies Kunja Siltstone. Is overlain by Blue Hole Formation.|Medium quartz sandstone, micaceous sublithic sandstone.|
27154|Farquharson Sandstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Limbunya Group.||Overlies Kunja Siltstone. Is overlain by Blue Hole Formation.|Fine to medium quartz sandstone, minor siltstone.|
27154|Farquharson Sandstone|71267|6|Mentioned|1m_geologyl12_lithology_lut.csv||||||||sandstone|
27154|Farquharson Sandstone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Blue Hole Formation. Underlain by Kunja Siltstone.||
27154|Farquharson Sandstone|71374|4|Described|iii, p1 tbl 1, p36-p38, p63-p64|Statherian|Statherian|Birrindudu Basin. SHRIMP age is interpreted as the maximum depositional age for this formation. The type section of this formation extends from 664930mE 8088212mN to 664514mE 8087951mN. Sampling site provided along with zircon description and SHRIMP analytical discussion.|1654 +/- 12 Ma (SHRIMP U-Pb)|Limbunya Group||Conformably overlies the Kunja Siltstone. Conformably overlain by the Blue Hole Formation and the Campbell Springs Dolostone. Broadly equivalent to the McArthur Group.|Tabular and blocky, thinly to thickly bedded, typically massive, fine-grained sandstone with some interbeds of siltstone in the lower part.|
27154|Farquharson Sandstone|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Kunja Siltstone. Overlain by Blue Hole Formation.||
81658|Favenc package|72373|5|Briefly described|p1-2|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Informal nomenclature of Rawlings et al (1997) and Rawlings (1999). A basin-wide non-genetic depositional pacakge within the McArthur Basin.||||Ovelain by Wilton package. Underlain by Glyde package.||
81658|Favenc package|72523|6|Mentioned|p1.|Mesoproterozoic|Mesoproterozoic|An informal grouping name used in Northern Territory (Rawlings 1999).||||||
81658|Favenc package|72718|5|Briefly described|p5, p7, p8-9, p10-14, p18,20|Calymmian|Calymmian|Nathan Group and correlatives. Pervasive across McArthur Basin. Depositional age ca 1600 to 1580 Ma or younger determined from SHRIMP U-Pb zircon dating and detrital zircon geochronology.||||Unconformably overies Redbank package except in Batten, Walker and Urapunga fault zones, where it overlies rocks of Glyde package.|Stromatolitic to evaporitic dolostone and sandstone-dominated siliciclastic successions deposited in shallow marginal marine to continental sabkha environments|
81658|Favenc package|72912|6|Mentioned|p5, 18.|Calymmian|Statherian|Of Rawlings, 1999.||||Overlies Glyde package and underlies Wilton package.||
24275|Fenton Granite|1430|5|Briefly described|p81, 82, 83|Proterozoic|Proterozoic|110 miles S-SE of Darwin. Small highly contaminated albitite mass on margin. Geochemical analysis given.||||||17-MAY-18
24275|Fenton Granite|23714|4|Described|p26|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
24275|Fenton Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
24275|Fenton 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
24275|Fenton Granite|33278|6|Mentioned|Fig.7|||||||||
24275|Fenton Granite|35140|6|Mentioned|p322|||||||||
24275|Fenton Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24275|Fenton Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24275|Fenton Granite|42012|2|Defined|p42|Paleoproterozoic||See also Table 1 p6.||||||07-NOV-08
24275|Fenton Granite|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24275|Fenton Granite|42070|4|Described|p3|||||||||
24275|Fenton Granite|42756|6|Mentioned|Fig.5 P6|||||||||
24275|Fenton Granite|43140|3|Fully described|p20||Paleoproterozoic|Of the Cullen Batholith.||||||07-NOV-08
24275|Fenton Granite|43624|6|Mentioned|p18,Fig.15,p20|||||||||
24275|Fenton Granite|43832|4|Described|Table8p38;47,Tb12p62||Paleoproterozoic|||||||07-NOV-08
24275|Fenton Granite|45003|14|Not recorded|p23|||See also Lexicon||||||
24275|Fenton Granite|45022|3|Fully described|p.142||Carpentarian|On many pages||||||
24275|Fenton Granite|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Medium foliated biotite granite; medium foliated leucogranite; coarse porphyritic hornblende-biotite granite, sheared in places with minor adamellite and albite.  Intrudes the Mount Partridge and South Alligator Groups.||||||07-NOV-08
24275|Fenton Granite|46676|14|Not recorded|p.9|||||||||
24275|Fenton 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
24275|Fenton Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1835Ma SHRIMP U/Pb.  I-type. Fine biotite granite. Fine biotite granite. Intrudes South Alligator Group and Wildman Siltstone.||||||07-JAN-09
24275|Fenton Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
24275|Fenton Granite|69420|5|Briefly described|p5:17-19, 51, 54|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Hosts Au in a shear zone at Gold Ridge.||Tennysons Suite.|||Medium- to coarse-grained, commonly porphyritic and partly foliated leucogranite and quartz monzonite. I-type.|12-JUL-16
24275|Fenton Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Tennysons Suite.|||Light grey to pink, medium- to coarse-grained, porphyritic biotite-hornblende granite, sheared in places, partly foliated.|
24275|Fenton Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1835+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
72402|Ferdies Member|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Dead Bullock Formation. Geological Province: Tanami Inlier. Feldspathic sandstone, quartzose psammite.||||||07-NOV-08
72402|Ferdies Member|63261|3|Fully described|p5 Fig. 2, p9 Fig. 5|||Of Dead Bullock Formation (Tanami Group). Grades up into Callie Member. Geological province: Tanami Region. Comprises feldspathic sandstone+ fine-grained sandstone locally intebedded with siltstone; equivalent to the "Lower Blake beds" (Lambeck 2004).||||||07-FEB-11
72402|Ferdies Member|64662|5|Briefly described|p30 Fig. 3, p32-33, p43|Paleoproterozoic|Paleoproterozoic|Basal subunit of Dead Bullock Formation (Tanami Group). Depositional age: ~2.11-1.84Ga. Overlain by Callie Member. Contains arkose and feldspathic arenite - both providing samples for depositional age analysis (see Tbs.1, 2). Geol.Province:Tanami region.||||||07-FEB-11
72402|Ferdies Member|64733|5|Briefly described|p171, p172 Fig.4|Orosirian|Orosirian|||Lower part of Dead Bullock Formation.|||Siltstone with lesser fine-grained sandstone and local coarser sedimentary rocks.|20-APR-12
72402|Ferdies Member|64734|4|Described|p185-187, p198, p188 Fig.2|Neoarchean||Basal part Dead Bullock Formation; underlies Callie Member; fine feldspathic sst commonly interbedded with fine sandy siltst lacking carconaceous matter; basal contact not observed; has undergone greenschist metamorphism; max depositional age of 2500Ma||||||10-MAR-10
72402|Ferdies Member|65358|5|Briefly described|p9|||Of Tanami Formation [misspelt name?]. Metasediments. Intruded by a foliated dolerite sill which hosts auriferous quartz veins of the Groundrush deposit.||||||
72402|Ferdies Member|66129|6|Mentioned|p216 Fig.3|||In Dead Bullock Formation.||||||
72402|Ferdies Member|66468|6|Mentioned|p17 Fig.4|Orosirian|Orosirian|Unit in Dead Bullock Formation. Hosts gold occurrence.||||||
72402|Ferdies Member|66683|5|Briefly described|p377.|||Tanami region. Contains almost exclusively late Neoarchean detritus. The authors suggest the Neoarchean crystalline basement must underlie much of the North Australian Craton, and is possibly contiguous.||||Overlies Billabong Complex.|Arkosic metasedimentary rocks.|
72402|Ferdies Member|67824|5|Briefly described|p386 Fig.3, p387||Orosirian||< 1840 Ma|Of the Dead Bullock Formation.||Overlain by the Callie Member.|Fining-upward sandy siltstone.|
72402|Ferdies Member|67826|5|Briefly described|p402 Fig.3|Orosirian|Orosirian|||Of the Dead Bullock Formation.||Overlain by the Callie Member.||
72402|Ferdies Member|68474|6|Mentioned|p574|||Granites-Tanami Orogen.||Dead Bullock Formation||||
72402|Ferdies Member|69003|5|Briefly described|p17 Fig.21|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Hosts Au occurrence.||Dead Bullock Formation.||||
72402|Ferdies Member|69253|6|Mentioned|p748 Fig.2|Orosirian|Orosirian|||Unit in Dead Bullock Formation.||||
72402|Ferdies Member|69426|5|Briefly described|p11:3-5, 11, 16-17, 29|||Crispe et al. (2007). Intruded by  an auriferous, foliated dolerite sill at the Groundrush mine.||Dead Bullock Formation.||Is overlain conformably by Callie Member.|Arkosic conglomerate and sandstone interbedded with siltstone and minor chert.|12-JUL-16
72402|Ferdies Member|69618|5|Briefly described|p91-97, p100 Tb.1, p102, p109|||Redefined. ~450m thick.||Unit in Dead Bullock Formation.||Conformably overlies Kairos member. Is overlain conformably by Callie Member.|Banded, graphitic and non-graphitic siltstone and claystone; commonly planar-bedded with rare cross-lamination, flame structures and rip-up structures.|
72402|Ferdies Member|69747|5|Briefly described|p265-p266|||Geological province: Granites-Tanami Orogen. Occurs locally in association with Dead Bullock Soak goldfield.||Unit of Dead Bullock Formation.|Includes Blart Beds, Upper and Middle Callie Beds, Callie Laminated Beds and Lazlar Beds.|||25-JUN-19
72402|Ferdies Member|70291|5|Briefly described|p183|Orosirian|Orosirian|Geological province: Tanami. See also misspelt Ferdie Member p181, 201.|~1838 Ma|Unit of Dead Bullock Formation.||Overlain gradationally by Callie Member.|Fine-grained sandstone and siltstone with magnetite content up to 50%|07-AUG-19
72402|Ferdies Member|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. ||Unit of Dead Bullock Formation.||||
72402|Ferdies Member|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Not on main map; appears in the Interpreted Geology diagram only.||Dead Bullock Formation.|||Feldspathic sandstone, quartz sandstone, siltstone.|
72402|Ferdies Member|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Dead Bullock Formation.|||Feldspathic sandstone and conglomerate, quartz sandstone, minor siltstone, minor chert.|
72402|Ferdies Member|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|2109+/-20 Ma (MDA: U-Pb zircon SHRIMP)|Dead Bullock FZ.|||Arkosic conglomerate, feldspathic arenite.|
72402|Ferdies Member|73089|4|Described|p5-7, p10, p12-14, p17, p22-28|||Known from Dead Bullock Soak and surrounding region. Hosts the Auron orebody in the Dead Bullock Soak goldfield. 435 m thick. Low-energy marine depositional setting, below wave base. A date for monazite from metasiltstoneis interpreted as the age of peak metamorphism at 1839 +/- 9 Ma. Misspelt as Ferdies Formation p28.||Dead Bullock Formation, Tanami Group|Blake beds|Conformably overlain by Callie Member. Possibly underlain by Kairos member [conformably].|Banded graphitic and non-graphitic siltstone and claystone as well as carbonaceous siltstone, lesser sandstone, [banded?] iron formation and chert.|
72402|Ferdies Member|73158|4|Described|p3, p10|Orosirian|Orosirian|Upper Ferdies Member mentioned p3.|1884+/-8 Ma zircon U-Pb|Dead Bullock Formation, lower||Underlies Callie Member|Turbiditic sandstone|
72402|Ferdies Member|73159|5|Briefly described|p3, 10|||Granites-Tanami Orogen. HFSE geochemical plots.|1884 +/- 8 Ma MDA: Maidment et al., 2020|Dead Bullock Formation.||Is overlain by Callie Member.|Turbiditic sandstone.|
74920|Fiddlers Lake granite|63261|5|Briefly described|p9 Fig. 5|||||||||07-FEB-11
74920|Fiddlers Lake granite|64662|5|Briefly described|p30 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami region.||||||07-FEB-11
23593|Fingerpost Granodiorite|23714|4|Described|p26|||Previously mapped as part of Cullen Granite. Geological Province: Cullen Batholith.||||||
23593|Fingerpost Granodiorite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
23593|Fingerpost Granodiorite|24197|5|Briefly described|p24, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Biotite-dominated granitic pluton. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
23593|Fingerpost Granodiorite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23593|Fingerpost Granodiorite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Grey coarse porphyritic biotite-hornblende granodiorite.||||||07-NOV-08
23593|Fingerpost Granodiorite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23593|Fingerpost Granodiorite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23593|Fingerpost Granodiorite|42756|6|Mentioned|Fig.5 P6|||||||||
23593|Fingerpost Granodiorite|43140|3|Fully described|p22||Paleoproterozoic|Of Cullen Batholith. U-Pb age 1840 Ma. Previously mapped as part of Cullen Granite until after 1968.||||||07-JAN-09
23593|Fingerpost Granodiorite|43832|3|Fully described|41,46,49,53,55,63||Paleoproterozoic|Age 1823+-3 Ma; less precise 1843+-22 Ma (p53)||||||07-NOV-08
23593|Fingerpost Granodiorite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age; 1843-1823 +/- 22Ma (U-Pb, SHRIMP).||||||02-MAR-18
23593|Fingerpost Granodiorite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Cullen Supersuite. Age 1823 Ma SHRIMP U/Pb. I-type. Coarse porphyritic hornblende bioite granodiorite. Intrudes Finniss River Group. Intruded by Foelsche Leucogranite.||||||
23593|Fingerpost Granodiorite|67564|5|Briefly described|p33 Fig.19, p37.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.|1823 +/- 3 Ma.|||||
23593|Fingerpost Granodiorite|69420|5|Briefly described|p5:17-18, 20, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. A SHRIMP U-Pb zircon age of 1823 +/- 3 Ma is also given.|1843 +/- 22 Ma conventional U-Pb zircon (TIMS).|Fingerpost Suite.|||Coarse-grained porphyritic granodiorite grading into porphyritic granite with up to 40% K-feldspar megacrysts. I-type.|12-JUL-16
23593|Fingerpost Granodiorite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1823 +/- 3 Ma.|Fingerpost Suite.|||Light pink, medium- to coarse-grained biotite-hornblende granodiorite, porphyritic to equigranular.|
23593|Fingerpost Granodiorite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1823+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
31737|Fingerpost Suite|64698|5|Briefly described|lithinterp table|||Age ~1800-1840Ma. Of Cullen Supersuite. Includes Minglo Granite, ?Fingerpost Granodiorite.||||||07-JAN-09
31737|Fingerpost Suite|69420|5|Briefly described|p5:17, 20, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.|||Fingerpost Granodiorite; McCarthys, Minglo Granites.||Hornblende-dominated granites.|12-JUL-16
31737|Fingerpost Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Fingerpost Granodiorite, McCarthys Granite, Minglo Granite.|||01-MAR-18
75076|Fishburn Formation|67370|2|Defined|pp313-314, pp316-318,  p332, p334.|Early Triassic|Early Triassic|Defined. Named after Fishburn-1; type section is between 1,904.5 - 2,084 m. Contains the K. saeptatus Oppel Zone (P. samoilovichii Oppel Zone). Nearshore, mostly transgressive,  depositional environment. Widespread unit in Bonaparte Basin. The top of this unit is an erosional surface below the Osprey Formation (eastern Bonaparte Basin) and Sahul Group (western Bonaparte, northern Browse Basins).||Topmost unit in Mount Goodwin Subgroup.||Overlies Ascalon Formation. Is overlain unconformably by Cape Londonderry Formation (in the east) and Sahul Group (in the west).|Grey and green claystones with minor siltstone and sandstone.|
75076|Fishburn Formation|69452|3|Fully described|p36:8, 15, 20-21|Anisian|Olenekian|Gorter et al. (2009). Equivalent to the Upper Mount Goodwin Formation of Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Widespread offfshore, but is truncated by erosion towards the southern margin and is not recognised onshore. 179.5m thick in the type section in drillhole Fishburn-1.||Mount Goodwin Subgroup.||Conformably and transitionally overlies Ascalon Formation.|Claystone with minor siltstone and sandstone.|12-JUL-16
75076|Fishburn Formation|69454|5|Briefly described|p38:4|Olenekian|Olenekian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
75076|Fishburn Formation|69653|6|Mentioned|p10|Early Triassic|Early Triassic|Petrel Sub-basin.||Mount Goodwin Sub-group.||Overlies Ascalon Formation. Is overlain by Lower Cape Londonderry Formation (Troughton Group).||
75076|Fishburn Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Cape Londonderry Formation, overlies Ascalon Formation||
75076|Fishburn Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Olenekian|Olenekian|See also Regional geology: Figs.6-7. Vulcan: Fig.2.||Mount Goodwin Subgroup.||Overlies Ascalon Formation.||12-JUL-16
41994|Flint Spring Gneiss|9199|5|Briefly described|Map legend|||Porphyroblastic gneiss, layered felsic gneiss, amphibolite.  Geological Province: Arunta Block.||||||05-NOV-04
41994|Flint Spring Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Porphyroblastic gneiss, layered felsic gneiss, amphibolite.||||||
41994|Flint Spring Gneiss|61309|5|Briefly described|p32 Fig. 17|||See also Flint Springs Gneiss - place name is Flint Spring (not Flint Springs)!||||||06-FEB-08
41994|Flint Spring Gneiss|69427|5|Briefly described|p12:14-15|||Shaw et al. (1979). NW of Alice Springs, Wigley Domain, Aileron Province. Appears as Flint Springs Gneiss on 12:14.|||||Characterised by abundant foliated to gneissic megacrystic biotite granite, with lesser banded biotite gneiss (locally with garnet), felsic gneiss, biotite schist and amphibolite.|12-JUL-16
41994|Flint Spring Gneiss|69931|6|Mentioned|p274, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated.|||||Porphyritic tonalitic gneiss.|
75722|Florina Formation|69437|6|Mentioned|p22:10|Early Ordovician|Early Ordovician|Daly Basin.||||||12-JUL-16
75722|Florina Formation|69443|6|Mentioned|p28:27|||Daly Basin.||||Correlated with Toko Group.||12-JUL-16
75722|Florina Formation|69446|4|Described|p31:1-4, 6-9|Early Ordovician|Early Ordovician|Kruse et al. (2012). Daly Basin. A recessive unit, up to 167m thick. Comprises three carbonate intervals separated by two fine-grained glauconitic siliciclastic units: peritidal mudflat to subtidal lagoon deposits. Sparse but diverse fossil fauna indicates a Tremadocian to Floian age. Wide variety of sedimentary structures listed and illustrated.||||Overlies Oolloo Dolostone (Daly River Group) unconformably or disconformably.|Grey to yellow-brown to brown, thinly bedded, dolomitised fine sparstone, microsparstone and biosparstone, lesser grey limestone; yellow to brown to maroon glauconitic fine sandstone and shale; carbonate and siliciclastic intervals.|12-JUL-16
75722|Florina Formation|69451|6|Mentioned|p35:8|Floian|Tremadocian|Similar age to the early Floian Mooroongga Formation (Arafura Basin).||||||12-JUL-16
75722|Florina Formation|69673|5|Briefly described|p192|Ordovician|Ordovician|167m thick. Age derived from fossil assemblage.|||||Dolostone, fine grained glauconitic siliciclastic rocks and minor limestone.|
75722|Florina Formation|70380|3|Fully described|p743-751, p753-759|Early Ordovician|Early Ordovician|Tickell (2010), Kruse et al. (2012), for a 167m-thick interval overlying Oolloo Dolostone. Named after Florina pastoral lease where the most extensive outcrops occur. Youngest Formation on the Daly Basin succession. The type section is a 17km-long stretch of the Daly and Katherine Rivers, downstream from 791890 8377657 (base) to 788496 8394490 (top). Up to 167m thick, in the reference section which is the interval 25-192m depth in the air rotary-drilled water bore RN37043. Graphic logs of drillholes. Lithology described in detail. Generally recessive: karst surface features. Age from fossils.||||Unconformably overlies the Oolloo Dolostone (Daly River Group). Possibly equivalent to the Ninmaroo Formation (Georgina Basin) and the Hanson River beds (Wiso Basin).|Three intervals of dolostone with minor limestone, alternating with thicker siliciclastic intervals (glauconitic sandstone). Contains a sparse fossil fauna of trilobites, brachiopods, conodonts, hyoliths, echinoderms and gastropods.|
23596|Foelsche 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
23596|Foelsche Leucogranite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23596|Foelsche Leucogranite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23596|Foelsche Leucogranite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23596|Foelsche Leucogranite|42756|6|Mentioned|Fig.5 P6|||||||||
23596|Foelsche Leucogranite|43624|6|Mentioned|Fig.15,p20|||||||||
23596|Foelsche Leucogranite|43832|4|Described|Table8p38;46,Tb12p60||Paleoproterozoic|||||||07-NOV-08
23596|Foelsche Leucogranite|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
23596|Foelsche Leucogranite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite.  I-type. Fine-medium equigranular leucogranite. Intrudes Fingerpost Granodiorite.||||||07-JAN-09
23596|Foelsche Leucogranite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
23596|Foelsche Leucogranite|69420|5|Briefly described|p5:17-19|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Saunders Suite.|||Fine- to medium-grained leucogranite; granophyric intergrowths of quartz and K-feldspar. I-type.|12-JUL-16
24278|Fog Bay Metamorphics|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite gneiss.||||||07-NOV-08
24278|Fog Bay Metamorphics|9579|5|Briefly described|Map Sheet|Paleoproterozoic|Paleoproterozoic|Early Proterozoic age.||||||
24278|Fog Bay Metamorphics|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|Placed within Litchfield Province, part of the Pine Creek Inlier.||||||18-SEP-06
24278|Fog Bay Metamorphics|22809|6|Mentioned|5|Proterozoic|Proterozoic|||||||
24278|Fog Bay Metamorphics|22810|5|Briefly described|Table2 P4|||||||||
24278|Fog Bay Metamorphics|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Biotite gneiss.||||||07-NOV-08
24278|Fog Bay Metamorphics|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
24278|Fog Bay Metamorphics|41304|6|Mentioned|Map legend|Paleoproterozoic||Defined in Ref. 88/26225 p52.||||||07-NOV-08
24278|Fog Bay Metamorphics|41305|2|Defined|p52|Paleoproterozoic||Reserved as Fog Bay.||||||07-NOV-08
24278|Fog Bay Metamorphics|41645|6|Mentioned|p4|||||||||
24278|Fog Bay Metamorphics|41980|4|Described|p571|||See also Table 2 p569.||||||18-SEP-06
24278|Fog Bay Metamorphics|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Gneiss, schist, amphibolite. Geological Province: Pine Creek Orogen.||||||09-FEB-10
24278|Fog Bay Metamorphics|63866|4|Described|p105, p107|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. Known only from drillcore. Numeric age is a Rb-Sr whole rock isochron age. Intruded by an unnamed granite at 1855 +/- 3 Ma (Worden et al, in review). Regional metamorphism has been dated in this unit at 1853 +/- 3 Ma.|2002 +/- 42 Ma (de Laeter 1983)||||Graphitic siliciclastic and mafic volcanogenic sedimentary rocks.|
24278|Fog Bay Metamorphics|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Undifferentiated pelitic and semi-pelitic gneiss and schist; amphibolite, quartzite. Intruded by Wagait Granite.||||||07-JAN-09
24278|Fog Bay Metamorphics|64722|5|Briefly described|p10|||Of Litchfield Province of Pine Creek Region. Underwent medium to high grade metamorphism at ~1855 Ma. This unit plus Hermit Creek and Welltree Metamorphics are correlated with Finniss River Group.||||||11-APR-12
24278|Fog Bay Metamorphics|64730|6|Mentioned|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of Litchfield Province. Shown as lateral equivalent of Finniss River Group.||||||03-MAY-12
24278|Fog Bay Metamorphics|64731|4|Described|p145, p149, p151, p158, 160-161, 163|Paleoproterozoic|Paleoproterozoic|Of Litchfield Province. Type locality (drill core) cited. Peak or near-peak high-grade metamorphism dated at: 1853 +/- 4 Ma. Age related to earlier volcanism?|Rb-Sr whole-rock age 2002 +/- 42 Ma (Hickey 1985).|||In faulted contact with Welltree Metamorphics.||12-APR-12
24278|Fog Bay Metamorphics|64956|5|Briefly described|p2 Tb. 15, p68, p76-77|Paleoproterozoic|Paleoproterozoic|Metamorphic age: 1853+/-4ma. Geological province: Pine Creek Orogen. Sample is garnet-biotite-sillimanite gneiss.||||||07-FEB-11
24278|Fog Bay Metamorphics|65232|5|Briefly described|p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Gneiss, schist, amphibolite. General lithology given for three units including Hermit Creek, Fog Bay and Welltree Metamorphics.On figure, presented as Hermit Creek and Fog Bay Metamorphics.||||||09-FEB-10
24278|Fog Bay Metamorphics|65556|4|Described|p2 Tb.1, p4, p7-13, p45, p49-50, p52||Orosirian|Litchfield Province, Pine Creek Orogen. Samples in this report are (a) garnet-biotite-sillimanite quartzo-feldspathic gneiss, with a maximum depositional age given by SHRIMP U-Pb (youngest detrital) zircon age of 2028+/-8 Ma; and (b) graphitic biotite-garnet+/-sillimanite schist, with a monazite metamorphic age of 1854+/-3 Ma. Restricted to weathered outcrops on the north coast and on Turtle Island. ||||||
24278|Fog Bay Metamorphics|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Appears to be included in Woodcutters Supergroup.|||||Quartz-feldspar-biotite gneiss; interlayered para-amphibolite, minor carbonate and quartzite (only intercepted in drill core).|23-NOV-11
24278|Fog Bay Metamorphics|67232|5|Briefly described|p3, p4, p5. |Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Mid-amphibolite facies, peaking at 1855 Ma (Carson et al. 2008). Identified only in drillcore from the northwest of the Province.|Max. sedimentation 2020 Ma (Carson et al. 2009).||||Garnet schist and gneiss, possible volcanigenic rocks, minor carbonate and quartzite.|
24278|Fog Bay Metamorphics|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|||||Gneiss, schist, amphibolite.|
24278|Fog Bay Metamorphics|67779|5|Briefly described|p5 Fig.4(b), p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|<2028 +/- 8 Ma (Carson et al. 2008).|Unit in Woodcutters Supergroup.||||
24278|Fog Bay Metamorphics|69420|4|Described|p5:2, 4, 6-7, 26-27|Paleoproterozoic|Paleoproterozoic|NW Litchfield Domain, Pine Creek Orogen. May be of similar provenance/age to the Woodcutters Supergroup. Entirely subsurface. Amphibolite-facies metamorphism dated at 1854 +/- 3 Ma and 1853 +/- 4 Ma (monazite and metamorphic zircon rims respectively). Detrital zircon maximum depositional age.|2028 +/- 8 Ma (Carson et al., 2009).|Woodcutters Supergroup.||Is faulted against Welltree Metamorphics. May correlate with Woodcutters Supergroup.|Quartz-feldspar-biotite gneiss and schist, amphibolite; minor calc-silicate, marble and quartzite. Shows no significant fabric development; commonly preserves primary bedding structures.|12-JUL-16
24278|Fog Bay Metamorphics|69933|5|Briefly described|p1, p8-10|||Dating failed as no zircon was found in this sample. Petrography, geophysical response and SHRIMP analyses and results are provided.|||||Middle to upper amphibolite facies metasedimentary rock.|21-APR-23
24278|Fog Bay Metamorphics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2028+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Garnet-biotite-sillimanite quartzo-feldspathic gneiss; graphitic biotite-garnet(+/- sillimanite) schist.|
29775|Forty Five Augen Gneiss|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age:1754+/-9Ma.||||||18-SEP-06
29775|Forty Five Augen Gneiss|23733|6|Mentioned|p45 App. 2|||Age: 1760 +/- 11Ma.||||||
29775|Forty Five Augen Gneiss|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1760Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
29775|Forty Five Augen Gneiss|43225|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29775|Forty Five Augen Gneiss|43503|2|Defined|6,19,76|||U-Pb Shrimp Age: 1754+/-9Ma.||||||18-SEP-06
29775|Forty Five Augen Gneiss|50369|5|Briefly described|p1.4, 3.1, 12.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Intrudes: Narwietooma Metamorphic Complex. Age: 1754-1760 +/- 12Ma (Sm-Nd, Shrimp).||||||07-NOV-08
33651|Foster Cliff Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mantarurr Granite Suite. Finely porphyritic to equigranular foliated biotite-titanite-epidote-muscovite granite, minor aplite. Age: ~1170Ma.||||||08-FEB-05
33651|Foster Cliff Granite|60683|2|Defined|p59 Appendix, p18-19|Mesoproterozoic|Mesoproterozoic|Of the Mantururr Granite Suite.  Formerly mapped as Olia Gneiss and unnamed metamorphosed granites of Forman (1969a, 1972).  Finely porphyritic to equigranular biotite-sphene-epidote granite, minor aplite. See also p10 Tb. 1, p49.||||||23-DEC-09
33651|Foster Cliff Granite|61154|6|Mentioned|p44 Appendix|||Of the Pitjantjatjara Supersuite.||||||
33651|Foster Cliff Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Mantarurr Granite Suite. Finely porphyritic to equigranulated biotite-titanite-epidote granite; minor aplite. Age: ~1170Ma. Geological Province: Musgrave Block.||||||
80343|Fosters Suite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.||Baikal Supersuite|Includes the Unca Granite, Thring Granite and Jericho Granite.|||
80343|Fosters Suite|72516|2|Defined|p15, p29, p56, p71, p201|Statherian|Statherian|New name, named for the Fosters Bore in the central part of the map sheet area. See definitions for constituent units for type localities. Constituent units sporadically outcrop as generally poorly exposed, scattered outcrops; irregular, sharp-crested and rubbly hills; low bouldery outcrops in lowlands.Interpreted to have been deposited in a continental margin environment. Broadly similar ICE patterns and degree of LREE-enrichment to the Casper Suite. Comagmatic and cogenetic with the Casper Suite and the Mascotte Orthogneiss. Said to be locally unconformably overlain by Oorabra Arkose and Grand [Grant] Bluff Formation of the Georgina Basin. Structure, metamorphism, alteration, mineralisation, geophysical expression, geochemistry are discussed. See also p101-104, p120-123, p126-127, p189.|1780 +/- 4 Ma (LA-ICPMS, Beyer et al 2018)|Baikal Supersuite|Includes the Unca Granite, Thring Granite and the Jericho Granite.|Intrudes the White Violet Orthogneiss and the Mascotte Orthogneiss. Intruded by the Boundary Igneous Complex and Samarkand Pegmatite.|Mica-bearing leucogranites.|19-APR-22
80343|Fosters Suite|73591|6|Mentioned|p9, p11, p16, p18|||||Baikal Supersuite|Jericho Granite|||
23601|Frances Creek Leucogranite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
23601|Frances Creek Leucogranite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23601|Frances Creek Leucogranite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Pink to grey, fine to medium equigranular leucogranite and fine to medium equigranular alkali feldspar granite.||||||07-NOV-08
23601|Frances Creek Leucogranite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Fine even-grained grey leucocratic granite.||||||07-NOV-08
23601|Frances Creek Leucogranite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23601|Frances Creek Leucogranite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23601|Frances Creek Leucogranite|41309|4|Described|p9|||||||||
23601|Frances Creek Leucogranite|41311|4|Described|p20|||||||||
23601|Frances Creek Leucogranite|42756|6|Mentioned|Fig.5 P6|||||||||
23601|Frances Creek Leucogranite|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
23601|Frances Creek Leucogranite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Grey to pale pink, fine to medium equigranular lecuogranite.  Age: 1810-1800Ma.||||||13-JAN-05
23601|Frances Creek Leucogranite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1800-1820Ma. Of Cullen Supersuite.  I-type. Grey to pale pink, fine to medium equigranular leucogranite. Intrudes McCarthys Granite, Allamber Springs Granite, Minglo Granite and Masson Formation.||||||07-JAN-09
23601|Frances Creek Leucogranite|67564|4|Described|p7 Table 2, p15 Fig.8, p33 Fig.19, p35.|Paleoproterozoic|Paleoproterozoic|I-type. Three separate plutons within Cullen Batholith, Pine Creek Orogen. Contains numerous rafts of Bludells Dolerite.|1810 - 1800 Ma.|Unit in Cullen Supersuite.||Intrudes McCarthys, Minglo and Allamber Springs Granites.|Grey to pale pink, fine to medium, equigranular leucogranite and alkali feldspar granite.|
23601|Frances Creek Leucogranite|69420|5|Briefly described|p5:14, 17-19|Paleoproterozoic|Paleoproterozoic|Includes irregularly-shaped bodies, up to 5km across, of Bludells Dolerite. May represent a localised melt formed by intrusion of the dolerite into a granitic intrusion. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Burnside Suite.|||I-type.|12-JUL-16
23601|Frances Creek Leucogranite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Burnside Suite.|||Light grey to pale pink, fine- to medium-grained, porphyritic to equigranular biotite leucogranite.|
42090|Frankenia Monzogranite|23809|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Age: 1805+/-6Ma (Pb-Pb).||||||07-NOV-08
42090|Frankenia Monzogranite|62580|5|Briefly described|p26, p75|Paleoproterozoic|Paleoproterozoic|Of the Coomarie Suite. A complex pluton - dark pink, fine- to medium-grained equigranular muscovite-biotite monzogranite to quartz monzonite. Age of crystallisation: 1805+/-6Ma (U/Pb zircon).||||||07-FEB-11
42090|Frankenia Monzogranite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1805+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
40071|Frederick Suite|23809|5|Briefly described|p3 Fig. 1|||Same unit as Mount Frederick Suite?  Medium to fine grained, weakly porphyritic to equigranular, foliated to massive biotite monzogranite, hornblende-biotite granodiorite; trondjhemite.||||||22-DEC-08
40071|Frederick Suite|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodorite. I-type; medium to coarse, grey, oval plutons. Age: ~1800Ma.||||||07-NOV-08
40071|Frederick Suite|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite.||||||07-NOV-08
40071|Frederick Suite|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite.||||||07-NOV-08
40071|Frederick Suite|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite hornblende granodiorite: I-type, medium to coarse, grey, oval plutons; strong magnetic response.||||||07-NOV-08
40071|Frederick Suite|61246|6|Mentioned|p30|||Includes the "Pipeline granodiorite".||||||
40071|Frederick Suite|61861|5|Briefly described|p4, 25, Fig 2, Fig.38,  Map 1|Orosirian|Orosirian|Granite suite in Tanami Region, close to WA border. Ovoid, smaller diameter than Coomarie Suite, I-type plutons with high magnetic response. Age inferred from intrusive relationships.|1830 - 1810 Ma.|||||03-APR-12
40071|Frederick Suite|62580|4|Described|p39, p11 Tb. 1, p12 Fig. 2, p69|Paleoproterozoic|Paleoproterozoic|Includes MacFarlanes Peak and Walnut Granodiorites, Nora Range Monzogranite. I-type. Granite plutons of med.- to coarse-gr., equigr., granophyric to porphyritic, leucocratic qtz syenite, biotite-hornblende monzogranite + hornblende-biotite granodiorite.||||||07-FEB-11
40071|Frederick Suite|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier. Medium to fine grained, equigranular biotite or hornblende bearing monzogranite to syenogranite.||||||07-NOV-08
40071|Frederick Suite|63261|4|Described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|Includes the magnetic parts of Browns Range and Coomarie granite suites. Interpreted crystallisation age range: 1815+/-4 to 1801+/-4Ma. Geological province: Tanami Region. Typically medium- to fine-gr. equigranular biotite monzogranite to syenogranite.||||||10-DEC-12
40071|Frederick Suite|64662|5|Briefly described|p30 Fig. 3|Statherian|Orosirian|Age: 1825-1790Ma. Geological Province: Tanami region.||||||07-FEB-11
40071|Frederick Suite|64675|6|Mentioned|Map 1|Paleoproterozoic|Paleoproterozoic|||||||
40071|Frederick Suite|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Orosirian|Moderate to high aeromagnetic response. Spelling error on Fig.2 ('Fredrick Suite')|1815-1790 Ma.|||||20-APR-12
40071|Frederick Suite|65323|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response. Shown as equivalent age to Borefield Road Suite and Granites Suite.||||||18-FEB-13
40071|Frederick Suite|65324|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65326|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||02-FEB-10
40071|Frederick Suite|65327|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65328|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65349|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65350|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65351|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65352|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response.  Shown as equivalent in age to Granites Suite and Bore Field Road Suite.||||||12-DEC-12
40071|Frederick Suite|65353|5|Briefly described|Map legend|Statherian|Orosirian|Intrusive biotite hornblende granodiorite; I-type; moderate-highly magnetic, low gravity response. Shown as equivalent in age to Granites Suite and Bore Field Road Suite.||||||12-DEC-12
40071|Frederick Suite|65354|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65355|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65356|6|Mentioned|Map legend|Statherian|Orosirian|Not shown on map||||||
40071|Frederick Suite|65358|5|Briefly described|p6-7|Statherian|Orosirian|In Tanami Region. Dominated by metaluminous I-type biotite granodiorite and monzogranite. Intruded between 1825-1790 Ma.||||||
40071|Frederick Suite|65359|5|Briefly described|p23, p26-28 Figs.26-28.|||Tanami Region. Felsic plutons with high magnetic signature.||||||
40071|Frederick Suite|66129|5|Briefly described|p213, p214 Fig.1, p215 Fig.2|Statherian|Orosirian|1815-1790 Ma. Medium to fine grained, equigranular biotite monzogranite to syenogranite. Accessory minerals of titanite, magnetite, ilmenite, pyrite, apatite and zircon.||||||
40071|Frederick Suite|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|I-type. Low gravity response; variably magnetic.||||Intrudes MacFarlane Peak and Tanami Groups.|Biotite-hornblende granodiorite.|
40071|Frederick Suite|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|1815-1790 Ma|||||
40071|Frederick Suite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex.|c.1815-1790 Ma (Huston et al., in press).|Granites Supersuite|Includes Balwina, Lewis, Slatey Creek Granites.||Granite, diorite, gabbro.|
40071|Frederick Suite|69003|5|Briefly described|p5, p17 Fig.21|||Granites-Tanami Orogen.|1820-1790 Ma.|||||
40071|Frederick Suite|69253|5|Briefly described|p755-756, p761, p763, p765|Statherian|Orosirian|Petrophysical properties detailed. Appears in Fig. 1 as Fredrick Suite.|c.1815-1790 Ma.||Includes Balwina, Lewis and Selby Granites.|||
40071|Frederick Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Tanami Region.||||Intrudes Ware Group.||12-JUL-16
40071|Frederick Suite|69426|5|Briefly described|p11:4 Fig.11.3, 11:10-12|Statherian|Orosirian|Comprises several un-named granite plutons which have a distinctive moderate to highly magnetic response, but a low gravity response. Hosts a porphyry gold style deposit at the Buccaneer prospect. Geochemistry briefly described.|1815-1778 Ma.||||Typically medium- to fine-grained, equigranular, biotite monzogranite to syenogranite.|12-JUL-16
40071|Frederick Suite|69432|6|Mentioned|p17:2|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
40071|Frederick Suite|69673|6|Mentioned|p3|||||||||
40071|Frederick Suite|69747|5|Briefly described|p263-p264|Statherian|Orosirian|Geological province: Tanami Block, North Australian Craton. Associated with late syn- to postcollisional tectonic settings within a ~30 Ma million year long period of magmatic activity broadly spanning ca. 1825-1791 Ma (Smith, 2001).|ca. 1815-1790 Ma|||||25-JUN-19
40071|Frederick Suite|70291|4|Described|p178,180-181|Statherian|Orosirian|Geological province: Tanami. Affected by D4 event (ESE-trending crenulations; angular folding late syn- to post-granite intrusion). Inferred to have a deeper source.|1815-1790 Ma||||Magnetic, peraluminous biotite monzogranite to syenogranite with hornblende in SiO2-poorer samples.|
40071|Frederick Suite|70478|4|Described|p2 Fig 1, p3-5, p39 App 3|Statherian|Orosirian|Geological Province: Tanami. Granites drilled in drillholes TAN99DDH1, TAN99DDH2, TAN99DDH3 assigned to Frederick Suite. See associated drilling summaries and appendices for more detail. SHRIMP U-Pb magmatic zircon ages of 1802+\-4 Ma (DDH1 granite; Cross et al., 2005); 1801+\-4 Ma (DDH2 granite; Smith 2001); 1815+\-4 Ma (DDH3 granodiorite; Smith 2001).||||Intrudes Killi Killi Formation, Mount Charles Formation.|monzogranite, syenogranite|
40071|Frederick Suite|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region. Shown in the Cross Section only.|1815-1778 Ma.||||Medium- to fine-grained, equigranular biotite- or hornblende-bearing monzogranite to syenogranite.|
40071|Frederick Suite|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1815-1778 Ma.||||Biotite +/- hornblende monzogranite to syenogranite: medium- to fine-grained, equigranular.|
40071|Frederick Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||syenogranite, monzogranite|
40071|Frederick Suite|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1790 Ma.|||Intrudes Tanami and Ware Groups.||
40071|Frederick Suite|73089|5|Briefly described|p3, p8, p39|Statherian|Orosirian|Granites-Tanami Orogen, widespread. Broadly coeval with other granites of the orogen but distinguished by differences in magnetic character (Ahmad et al., 2013).|1815-1778 Ma||Lewis Granite ,Balwina Granite||Medium- to fine-grained, equigranular, biotite monzogranite to syenogranite characterized by relatively strong magnetization.|
40071|Frederick Suite|73158|5|Briefly described|p2|Statherian|Orosirian|Granites-Tanami Orogen.|1815-1778 Ma||||Granitic intrusions.|
40071|Frederick Suite|73159|5|Briefly described|p2|||Granites-Tanami Orogen.|1815-1778 Ma.||||Granites.|
29301|Frere Formation (NT)|41663|6|Mentioned|p38|||Formation misspelt as "Fromation".||||||21-SEP-06
24280|Frew River Formation|23733|5|Briefly described|p44 App.1|||Of Wauchope Subgroup.||||||
24280|Frew River Formation|24172|5|Briefly described|p65 Tb.9|||Of the Wauchope Subgroup. Geological Province: Tennant Creek Inlier. Of the Hatches Creek Group.||||||21-SEP-06
24280|Frew River Formation|39624|5|Briefly described|Table 1|||||||||
24280|Frew River Formation|39887|6|Mentioned|p453|||||||||
24280|Frew River Formation|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24280|Frew River Formation|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Friable arenite, siltstone, mudstone.  Overlies Coulters Sandstone.||||||10-JAN-05
24280|Frew River Formation|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24280|Frew River Formation|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24280|Frew River Formation|41128|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Friable arenite and siltstone, commonly calcareous and dolomitic, locally stromatolitic in upper part; minor silicified quartz arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24280|Frew River Formation|41129|4|Described|Table 1|||Mention p26.||||||07-AUG-06
24280|Frew River Formation|41204|4|Described|Table 1|||||||||
24280|Frew River Formation|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Siltstone, arenite, limestone, dolostone; stromatolites.||||||16-NOV-05
24280|Frew River Formation|41308|5|Briefly described|Table 2|||||||||
24280|Frew River Formation|41310|4|Described|Table 1|||See also p12.||||||07-AUG-06
24280|Frew River Formation|41408|6|Mentioned|Map legend|Proterozoic||||||||
24280|Frew River Formation|41524|4|Described|Table 1|||||||||
24280|Frew River Formation|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Siltstone, arenite; commonly calcareous and dolomitic, locally stromatolitic.||||||07-NOV-08
24280|Frew River Formation|41970|6|Mentioned|Fig.3 P333|||||||||
24280|Frew River Formation|42217|6|Mentioned|p421|||||||||
24280|Frew River Formation|42643|4|Described|p12, Table 1 p6|||||||||
24280|Frew River Formation|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Siltstone, arenite, calcarenite, stromatolitic limestone and dolostone.||||||07-NOV-08
24280|Frew River Formation|43802|6|Mentioned|Table 1,p80|||||||||
24280|Frew River Formation|45167|3|Fully described|Table 1|||Of Wauchope Subgroup.||||||19-SEP-06
24280|Frew River Formation|49033|2|Defined|p22|Proterozoic|Proterozoic|||||||
24280|Frew River Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Upper Wauchope Subgroup (Hatches Creek Group).  Siltstone, feldspathic/lithic arenite, mudstone, limestone and dolostone; stromatolites.  In the Tennant Creek region.||||||07-NOV-08
24280|Frew River Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Upper Wauchope Subgroup.||Wauchope Subgroup.||||05-JAN-17
24280|Frew River Formation|65338|5|Briefly described|p12, pp19-20.|Paleoproterozoic|Paleoproterozoic|||Unit in Wauchope Subgroup, Hatches Creek Group.||Overlies Coulters Sandstone.|Intensely silicified, stromatolitic carbonate rocks.|19-OCT-11
24280|Frew River Formation|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup.||Overlies Coulters Sandstone. Is overlain by Kudinga Basalt.|Friable arenite and siltstone; commonly calcareous and dolomitic, locally stromatolitic in upper part; minor silicified quartz arenite.|
24280|Frew River Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Upper.||Overlies Coulters Sandstone. Is overlain by Kudinga Basalt.|Siltstone, feldspathic/lithic arenite, mudstone, limestone and dolostone; stromatolites.|
24280|Frew River Formation|67352|4|Described|p9 Tb.1, p44 fig 48|Orosirian|Orosirian|Very shallow water, intertidal, sabkha.||Wauchope Subgroup||Overlies Coulters Sandstone (conformably); is conformably overlain by Kudinga Basalt.|Kaolinitic arenite: thinly bedded, fine-grained, friable; micaceous siltstone; cherty mudstone; calcareous or dolomitic in upper part; subordinate feldspathic and quartz arenite: fine-to medium grained, silicified.|
24280|Frew River Formation|68518|4|Described|p7 Tb.1, p12|Proterozoic|Proterozoic|Thickness: 150-600 m. Sedimentary features indicate deposition in very shallow water, possibly in a coastal lagoon environment.||Wauchope Subgroup||Conformable on Coulters Sandstone; is overlain by Kudinga Basalt and unconformably by Cambrian and Mesozoic? strata.|Recessive arenite to micaceous siltstone, cherty siltstone, mudstone, calcareous siltstone, calcarenite, limestone and dolomite. In SE: andesitic flow/sill; and carbonates form manganiferous and hematitic 'gossans'.|30-MAY-16
24280|Frew River Formation|69425|4|Described|p10:3, 10-12, 18-19|Statherian|Statherian|The first significant carbonate-bearing unit in the Hatches Creek Group. 0 - 600m thick; c.500m in the type section in the HATCHES CREEK REGION map area. Coastal lagoon deposits; no evidence for sabkha environment.|< ~1810 Ma|Wauchope Subgroup, upper.||Conformably overlies Coulters Sandstone. Is overlain conformably by Kudinga Basalt. Correlated with Coodna Member (in part).|Sandstone, mainly friable feldspathic/lithic sometimes with carbonate matrix; siltstone, with rare halite casts locally; limestone (commonly stromatoliic) and dolostone; possible mafic lava locally.|18-SEP-18
24280|Frew River Formation|69431|5|Briefly described|p16:5, 8|||Davenport Province.||Wauchope Subgroup.||Probable correlative of Whittington Range Member.||12-JUL-16
24280|Frew River Formation|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24280|Frew River Formation|72380|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||||||
27270|Frigate Shale|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Tithonian|Oxfordian|Type section Petrel 1 well (1571-1820m).||Flamingo Group||Overlies Plover Formation (unconformably). Overlain by Sandpiper Sandstone (conformably).|Shale, calcareous shale; minor glauconitic sandstone.|
27270|Frigate Shale|13234|5|Briefly described|p260, p263 Tb.4.|||Important source rock unit.||Of the Flamingo Group||||
27270|Frigate Shale|22663|6|Mentioned|NT97 -1-4 p3|||Of the Flamingo Group.||||||19-SEP-06
27270|Frigate Shale|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
27270|Frigate Shale|24569|5|Briefly described|p248 Fig. 3|Tithonian|Kimmeridgian|Of the Flamingo Group. Age: >140Ma. Geological Province: Petrel Sub-basin.||||||02-MAR-05
27270|Frigate Shale|41459|6|Mentioned|Fig.2|||||||||
27270|Frigate Shale|41532|6|Mentioned|p305|||||||||
27270|Frigate Shale|41731|6|Mentioned|Fig.3|||||||||
27270|Frigate Shale|42442|2|Defined|p25|Tithonian|Oxfordian|Same as Frigate Shale in WA.||||||19-SEP-06
27270|Frigate Shale|43661|6|Mentioned|Fig.3|||||||||
27270|Frigate Shale|43699|6|Mentioned|Fig.6,p10||Late Jurassic|||||||
27270|Frigate Shale|43739|6|Mentioned|Fig.5,p38|Late Cretaceous|Late Jurassic|||||||
27270|Frigate Shale|43829|5|Briefly described|Fig.2,p225|Early Cretaceous|Middle Jurassic|||||||
27270|Frigate Shale|49637|5|Briefly described|p7|Early Cretaceous|Late Jurassic|Of the Flamingo Group. Geological Province: Sahul Platform and Petrel Sub-basin.||||||07-FEB-11
27270|Frigate Shale|60386|6|Mentioned|p302|Oxfordian|Oxfordian|Bonaparte Basin. Distal shelf/basin.||||||
27270|Frigate Shale|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Of the Flamingo Group. Age: ~156-~142Ma. Geological Province: Northern Bonaparte Basin and Petrel Sub-basin.||||||09-NOV-06
27270|Frigate Shale|64695|6|Mentioned|p268 Fig.13|||||||||
27270|Frigate Shale|64696|6|Mentioned|p134|Oxfordian|Oxfordian|See also references to Frigate Formation (p125, p126, p127 Fig.2, p131, p134, p138, p140 ). Vulcan Sub-basin. Appears as Frigate Shale (Lower Vulcan Formation). About 1000 m thick.||||||
27270|Frigate Shale|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes grey shale.|
27270|Frigate Shale|67200|6|Mentioned|app 2 p8||||||||Shale.|
27270|Frigate Shale|68135|5|Briefly described|p51 fig 2a|Early Cretaceous|Middle Jurassic|Bonaparte Basin.||Flamingo Group.||Is overlain by Swan Formation.||14-SEP-17
27270|Frigate Shale|69452|5|Briefly described|p36:8, 15, 21-22|||Petrel Sub-basin, Bonaparte Basin. Thickness up to 250m.||Flamingo Group.||Overlies Elang Formation. Is overlain by Sandpiper Sandstone.|Marine mudstone.|12-JUL-16
27270|Frigate Shale|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p15, 37, 39|Late Jurassic|Late Jurassic|Petrel Sub-basin. The lower part is suitable as a reservoir, and the upper part as a seal, for CO2 storage in Elang and Plover Formations. Middle shoreface - offshore deposits. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p41-43, 45, 47-49, 51, 53, 59, 63, 68, 73-74, 76. See also references to Frigate Formation (p26-27, 50).||Flamingo Group.||Disconformably overlies Elang Formation. Is overlain by Sandpiper Sandstone.|Sandstone-dominated lower part overlain by mudstone-dominated upper part: bioturbated fine-grained sandstone, bioturbated siltstone with shell fragments, mudstone. Facies described in detail.|
27270|Frigate Shale|69673|6|Mentioned|p173|||||Flamingo Group||||
27270|Frigate Shale|70061|5|Briefly described|Regional geology p6, p12, p14|Valanginian|Oxfordian|Gas- and oil-prone source rocks. Claystones also provide an additional top seal. See also Fig 6 which shows Frigate Shale as Oxfordian to Valanginian, and shown in Upper and Lower parts with time break between in the Laminaria/Flamingo High area and Troubadour Terrace/Sahul Platform area, but no time break in Flamingo/Sahul Syncline or Calder and Malita Graben areas.|||||Marine sediments including mudstones.|18-SEP-18
79774|Froud Formation|72369|5|Briefly described|p15,18|||Of Amadeus Basin. Defined by Donnellan and Normington 2017.||Unit of Winnall Group.||Overlain by Liddle Formation. Underlain by Gloaming Formation.||
34083|Gali Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
34083|Gali Member|24048|2|Defined|p100 App. 1|Paleoproterozoic|Paleoproterozoic|See also p47.  Proposer: Ian Sweet. Of the Badalngarrmirri Formation.  Max. thickness: 360m.  Geological Province: McArthur Basin.||||||07-NOV-08
34083|Gali Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation of Parsons Range Group. Siltstone and sandstone: laminated to thin or wavy bedded, hummocky cross-stratified; interbeds of thin to medium-bedded fine-grained clayey sandstone. Geol. Prov: McArthur Basin.||||||12-OCT-05
34083|Gali Member|44112|5|Briefly described|p49-51|||||||||
34083|Gali Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation of Parsons Range Group. Siltstone and sandstone: laminated to thin or wavy bedded, hummocky cross-stratified; interbeds o f thin to medium-bedded fine-grained clayey sandstone. Geol. Prov: McArthur Basin.||||||
34083|Gali Member|69430|5|Briefly described|p15:13|||Southern Walker Fault Zone, McArthur Basin. 0-360m thick. Storm-dominated shelf to upper shoreface deposits.||Badalngarrmirri Formation.|||Laminated and wavy-bedded siltstone; fine-grained, clayey, thinly to medium bedded sandstone.|12-JUL-16
42092|Galifrey granite|23809|6|Mentioned|p11, p12, p13|Paleoproterozoic|Paleoproterozoic|Age: 1814+/-2Ma (Ozchron, AGSO).  Name is in informal format.||||||07-NOV-08
77145|Galiwinku Dolerite|67779|5|Briefly described|p6 Fig.5, p8 Table 1.|Mesoproterozoic|Paleoproterozoic|NE and ENE-trending dykes; rarely exposed, intersected in drillcore. Correlated with Derim Derim Dolerite and Maningkorrirr Phonolite. Age based on correlations. Referred to informally as Galiwinku dyke swarm on p6 and p40.|c.1320 Ma (Carson et al. 1999).|||Intrudes Mammadawerre Sandstone in drillcore||14-MAY-18
77145|Galiwinku Dolerite|70968|6|Mentioned|p91|||Arnhem Land.||||Correlated with Derim Derim Dolerite.||
77145|Galiwinku Dolerite|71169|5|Briefly described|p80|Ectasian|Ectasian|In one or more of: McArthur Basin, Pine Creek Orogen and Tomkinson Province.|1325 +/- 36 Ma|||||
77145|Galiwinku Dolerite|71488|6|Mentioned|p146|||McArthur Basin. SIMS age derived from Whelan et al., 2016. |1325 +/- 36 Ma (SIMS U-Pb, Baddelyite)|||||
77145|Galiwinku Dolerite|73242|6|Mentioned|p36, p46|Ectasian|Ectasian|McArthur Basin. Part of a radiating swarm of dykes that are spatially associated with Maningkorrirr Phonolite and Mudginberri Phonolite in the Nimbuwah Domain. Referred to with Derim Derim Dolerite as Derim Derim-Galiwinku igneous province / mafic igneous province / large igneous province.|1325 +/- 36 Ma|||||
34076|Garrthalala Granite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
34076|Garrthalala Granite|24048|6|Mentioned|p8|||Geological Province: Arnhem Inlier.||||||
34076|Garrthalala Granite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: dark grey, red-brown weathering, fine to medium-grained, porphyritic, fayalite-bearing. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
34076|Garrthalala Granite|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Giddy Suite. Geological Province: Arnhem Block.||||||07-FEB-11
34076|Garrthalala Granite|44112|2|Defined|Table2 p12,23,27,108||Orosirian|Max Age: 1833 (+/-) 3 Ma||||||27-MAR-18
34076|Garrthalala 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: 1833 +/- 3Ma (Shrimp).||||||07-NOV-08
34076|Garrthalala Granite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: dark grey, red-brown weathering, fine to medium-grained, porphyritic, fayalite-bearing. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
34076|Garrthalala Granite|63866|4|Described|p115|Orosirian|Orosirian|Arnhem Inlier, Northern Caledon Shelf.|1833 +/- 3 Ma (Page, OZCHRON)|Giddy Suite|||A-type granites.|
34076|Garrthalala 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. Exposed as smooth boulders, pavements and irregular bare sheets, small knolls and islands. Is coeval with Bukudal and Giddy Granites. Geochemistry briefly described. SHRIMP U-Pb zircon age.|1833 +/- 3 Ma (Rawlings et al., 1997).|Giddy Suite.||Intrudes Bradshaw Complex. Has a sharp (?intrusive) contact with Bukudal Granite.|Granite, medium- to fine-grained, porphyritic, K-feldspar megacrystic, massive, contains fayalite, distinctly reddish-brown weathered surface; fine- to medium-grained white granite xenoliths (thermally metamorphosed Bradshaw Complex). Metaluminous.|12-JUL-16
34076|Garrthalala Granite|70719|6|Mentioned|p13, p15|||||||Correlated with Bukudal, Giddy Granites.||
37734|Gator Sandstone|24442|5|Briefly described|p23 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Carrara Range Group.  ||||||07-NOV-08
37734|Gator Sandstone|62659|5|Briefly described|Map Legend|Statherian|Statherian|Of the Carrara Range Group. Pink to purple, fine to medium garined, variably ferruginous, sublithic to lithic sandstone, local beds of coarse to pebbly sandstone; minor basalt and microdolerite.||||||
37734|Gator Sandstone|65337|3|Fully described|p9 Fig.5, p10 Table 3, pp13-14.|Paleoproterozoic|Paleoproterozoic|New name. Southeast MOUNT DRUMMOND area. Up to 700 m thickness of braided fluvial deposits with sporadic intertidal inundation and mafic lava flows. Formerly the upper part of Mitchiebo Volcanics (Sweet 1984). Correlated with Sly Creek Sandstone.||Unit in Carrara Range Group.||Overlies Mitchiebo Volcanics. Is overlain by Top Rocky Rhyolite.|Pink to purple, fine- to medium-grained, variably ferruginous, sublithic to lithic sandstone with local beds of very coarse and pebbly sandstone; minor basalt and microdolerite.|
37734|Gator Sandstone|69433|4|Described|p18:2, 6-7|Statherian|Statherian|Rawlings et al. (2008) included in this unit rocks mapped (by Sweet et al., 1984) as the "upper sandstone member" of the Mitchiebo Volcanics. Southern succession, Lawn Hill Platform. 100-700m thick. Type section is in MOUNT DRUMMOND map area.||Carrara Range Group.||Conformably overlies Mitchiebo Volcanics. Is overlain unconformably by Top Rocky Rhyolite.|A lower sandstone interval, fine- to medium-grained, medium to very thickly bedded and sublithic; vesicular basalt and laminated lithic sandy mudstone; an upper medium- to very coarse-grained, thickly to very thickly bedded sublithic sandstone.|12-JUL-16
37734|Gator Sandstone|69673|4|Described|p52 fig 42,|||Up to 700m thick.||Carrara Range Group|||Sandstone with local beds of coarse, very coarse and granule sandstones; vesicular basalt and a laminated, lithic sandy mudstone.|
37734|Gator Sandstone|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 Mitchiebo Volcanics and underlies Top Rocky Rhyolite.||
37734|Gator Sandstone|72527|4|Described|p1, p9, p169-172, p193, p194.|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Thickness 100 -700 m. Previously included in Mitchebo Volcanics. Ferruginous quartz sandstone at the sample locality. Asymmetrical ripple marks, bed load casts and other bedforms are common. The depositional environment is interpreted as moderate to high energy braided fluvial to supratidal (Rawlings et al., 2008). Deposition bracketed between Murphy Province basement (>1845 Ma) and overlying Top Rocky Rhyolite (1725 Ma).|1854+/-7 Ma max.dep. age, Pb/Pb SHRIMP.|Carrara Range Group||Overlies Mitchiebo Volcanics and unconformably overlies Wire Creek Sandstone and Murphy Metamorphics. Unconformably underlies Top Rocky Rhyolite and Surprise Creek Formation.|Fine-to coarse-grained quartz to sub-lithic sandstone, with pebble lags.|
37734|Gator Sandstone|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 Mitchlebo Volcanics and underlies Top Rocky Rhyolite.||
37734|Gator Sandstone|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Carrara Range Group||Underlain by Mitchiebo Volcanics. Unconformably overlain by Top Rocky Rhyolite.||
37734|Gator Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin region, Calvert Superbasin.||Carrara Range Group||Underlain by Mitchlebo Volcanics. Overlain by Top Rocky Rhyolite.||
37734|Gator Sandstone|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|||||||
24283|Gaylad Sandstone|22560|5|Briefly described|p2|||Gaylad Sandstone overlies a regional unconformity above Pioneer Sandstone and Olympic Formation||||||
24283|Gaylad Sandstone|22561|6|Mentioned|p17|||In the Ooraminna Sub-basin.||||||19-SEP-06
24283|Gaylad Sandstone|22566|4|Described|p81|Neoproterozoic|Neoproterozoic|Stratigraphic relations described - p81.||||||19-SEP-06
24283|Gaylad Sandstone|22648|4|Described|p 132 - 135|||Informally divided into upper and lower Gaylad Sandstone p 132.||||||19-SEP-06
24283|Gaylad Sandstone|22649|2|Defined|p 138-143|Neoproterozoic|Neoproterozoic|The Gaylad Sandstone is tentatively placed midway between 700 and 600 Ma.||||||
24283|Gaylad Sandstone|22762|6|Mentioned|p362|Neoproterozoic|Neoproterozoic|||||||
24283|Gaylad Sandstone|22804|6|Mentioned|p440|||||||||
24283|Gaylad Sandstone|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Correlate of Nucaleena Formation and Tent Hill Formation and Brachina Formation.||||||
24283|Gaylad Sandstone|23287|6|Mentioned|Fig.4|||Age: Lower Ediacarian. Geological province:  Amadeus Basin.||||||19-SEP-06
24283|Gaylad Sandstone|42886|5|Briefly described|Fig.2 P219|||||||||
24283|Gaylad Sandstone|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Sandstone, conglomerate.  Geological province: Amadeus Basin.||||||23-JAN-08
24283|Gaylad Sandstone|49796|4|Described|p1 & sections|||||||||
24283|Gaylad Sandstone|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Sandstone, feldspathic sandstone, minor granule conglomerate.||||||
24283|Gaylad Sandstone|61732|5|Briefly described|p91, p95|||Lies near the base of the Pertatataka Formation. Geological Province: Amadeus Basin.||||||07-FEB-11
24283|Gaylad Sandstone|62085|6|Mentioned|p24|Ediacaran|Ediacaran|Eastern Amadeus Basin.||||Intertongues with Olympic Formation.||
24283|Gaylad Sandstone|64625|5|Briefly described|p245 fig 2, p252, p254|||Freeman et al. (1991). Amadeus Basin. Previously mapped as Pioneer Sandstone and correlated with the Olympic Formation (Shaw et al., 1983).||||Unconformably overlies Olympic Formation, Pioneer Sandstone, Bitter Springs Formation. Is overlain by Pertatataka Formation.|Clean, medium- to coarse-grained feldspathic sandstone.|
24283|Gaylad Sandstone|64809|6|Mentioned|p10 |||||||||
24283|Gaylad Sandstone|66767|5|Briefly described|p60|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. About 140m thick.||||Unconformably overlies Olympic Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|
24283|Gaylad Sandstone|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|NE Amadeus Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Olympic Formation. Is overlain by Pertatataka Formation.|Sandstone and conglomerate.|12-JUL-16
24283|Gaylad Sandstone|69438|3|Fully described|p23:2-5, 19|Ediacaran|Ediacaran|Freeman et al. (1991). NE Amadeus Basin. The type section is 17km WNW of Ringwood homestead, on the S flank of the Gaylad Syncline, where it is c.140m thick. Contains four unconformity-bound sequences. Had previously been correlated with Pioneer Sandstone and Olympic Formation. Age estimate is based on dating of units correlated with the underlying Olympic Formation (651 +/- 87 Ma Rb-Sr age for Chambers Bluff Tillite). It could be considerably younger (post-580 Ma) depending on the age of the Elatina Glaciation.|~650 Ma.|||Unconformably overlies Pioneer Sandstone and Olympic Formation. Is overlain conformably by Pertatataka Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate (clasts are composed of underlying units) and rare debris-flow diamictite.|12-JUL-16
24283|Gaylad Sandstone|69443|6|Mentioned|p28:10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||||12-JUL-16
24283|Gaylad Sandstone|69673|5|Briefly described|p63, p64 fig 53, p88, p91|||||||Conformably overlain by Pertatataka Formation, overlies Pioneer Sandstone|Sandstone and conglomerate.|
24283|Gaylad Sandstone|69937|4|Described|v Fig.1, vi, p3 Tb.1, p22-25, p49-50|Neoproterozoic|Neoproterozoic|NE Amadeus Basin. Type section defined by Field (1991). Possible equivalent to Pioneer Sandstone and Olympic Formation; inferred age range of 700-600 Ma. Zircon age spectrum is in sharp contrast with units above and below. Likely zircon provenance discussed.|1049 +/- 27 Ma (maximum depositional age).|||Unconformably overlies Olympic Formation, Pioneer Sandstone. Is overlain conformably by Pertatataka Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|
24283|Gaylad Sandstone|70839|5|Briefly described|p329|Ediacaran|Ediacaran|Of Amadeus Basin.||Unit of Pertatataka Formation.||Basal unit of Pertatataka Formation. Underlain by Pioneer Sandstone.||
24283|Gaylad Sandstone|71001|6|Mentioned|p18 Fig.2, p21|Ediacaran|Ediacaran|Amadeus Basin. Fluvial deposits.||||Overlies Olympic Formation. Is overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
24283|Gaylad Sandstone|71279|6|Mentioned|p355 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||||||
24283|Gaylad Sandstone|71344|5|Briefly described|p1093-1094|||Limited to the north-eastern Amadeus Basin.||Of Pertaoorta Package.||Incised into [unconformable on] Olympic Formation diamictites. Is overlain conformably by Pertatataka Formation.|Yellow to orange, coarse grained, cross-bedded, fluvial sandstone with silty sandstone interbeds.|10-NOV-17
24283|Gaylad Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1049+/-27 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
24283|Gaylad Sandstone|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||||Overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|71842|6|Mentioned|p3|Ediacaran|Ediacaran|Of Amadeus Basin.||||||
24283|Gaylad Sandstone|72369|6|Mentioned|p11-p12|||Of Amadeus Basin. Associated with c. 640-580 Ma Elatina Glaciation (Walter et al., 1995).||||||18-DEC-19
24283|Gaylad Sandstone|72375|4|Described|p1-2,25-26|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Nomenclature of Freeman et al., 1991.  The type section was originally defined by Field (1991). Confined to NE Amadeus Basin. Depositional age constrained to c. 700-600 Ma based on regional correlations with underlying Olympic Formation (Freeman et al., 1991). Several alternate stratigraphic interpretations include: a) equivalent to upper part of Olympic Formation-Pioneer Sandstone succession (Kennedy and Christie-Blick 2011), b) may represent a localised, proximal equivalent to Waldo Pedlar Member (Pertatataka Formation; P Haines, per comm 2013). Sample location and description are provided. SHRIMP U-Pb zircon analyses by Kositcin et al., 2015 yielded an interpreted maximum depositional age (youngest zircon grain 238U/206Pb) of 1049+\-27 Ma, significantly older than the c. 700-600 Ma depositional age (Freeman et al., 1991). LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS AS13CJE018 (feldspathic quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p26 for Hf isotopic results and interpretations).|c. 700-600 Ma|||Overlain conformably by Pertatataka Formation. Underlain unconformably by Pioneer Sandstone, Olympic Formation.|Quartz sandstone, lithic sandstone, subarkose, orthoconglomerate and rare debris-flow diamictite.|04-DEC-19
24283|Gaylad Sandstone|73085|6|Mentioned|p1|Ediacaran|Ediacaran|||||Underlain by and partly equivalent to Pioneer Sandstone / Olympic Formation. Unconformably overlain by Pertatataka Formation.||
24283|Gaylad Sandstone|73086|2|Defined|p: 3, 5-6, 99, 101, 117-120, 123, 143|||[Defined herein. No revised definition card]. Previously proposed type section was formalized herein. Post-glacial transgressive sandstone unit. Amadeus Basin. Part of Supersequence III. Characterized by pale yellow to pale brown, or grey feldspathic sandstone. Named for Gaylad Creek. Type section: Gaylad Syncline. Key localities: Halfway Dam; Larrier Bore. Distribution: confined to the Fergusson and Gaylad synclines in the northeast of the basin. Difficult to distinguish from sandstones of both the Pioneer Sandstone and Waldo Pedlar Member of the Pertatataka Formation. Two informal subunits: lower unit consists of coarse-grained feldspathic sandstone, and upper unit of gritty sandstone. Thickness at type section: 139 m. Maximum thickness: 182 m, or possibly 240 m (highly variable bedding thickness). No known fossils. Detrital zircon maximum depositional age of 1049 +/- 27 Ma from the unit is much older than the inferred true depositional age, which is at the end of the Marinoan glaciation, i.e. probably ca 635 Ma. Deposited in fluvial- to marine-influenced environments, possibly including lagoonal or lacustrine and marginal marine deltaic environments. Possibly partly correlative to Olympic Formation, Pioneer Sandstone, Pertatataka Formation, Elyuah Formation, Gnallan-a-gea Arkose, Bukalara Sandstone, Buckingham Bay Sandstone.||||Unconformably underlain by Olympic Formation, Loves Creek and Gillen formations (Bitter Springs Group). Conformably[?] overlain by Pertatataka Formation. [See comments].|Fine- to coarse-grained (and rarely granular) lithic and feldspathic sandstone, orthoconglomerate, and minor debris flow diamictite.|
24283|Gaylad Sandstone|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||||Underlain by Olympic Formation. Unconformably overlain by Pertatataka Formation. Partly equivalent to Pioneer Sandstone.||
24283|Gaylad Sandstone|73180|6|Mentioned|p53|||Amadeus Basin. Possible correlative of the Pioneer Sandstone.||||||
37623|Geolsec Formation|24442|5|Briefly described|p43|||Consists of haematite-quartzite breccia, siltstone and sandstone. Deposited around the Waterhouse Dome. Unconformably overlies the Mount Partridge Group.||||||19-AUG-09
37623|Geolsec Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Haematitic paraquartzite breccia, milky quartz and chert breccia; haematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia.||||||
37623|Geolsec Formation|61389|5|Briefly described|Map Legend|||Haematitic paraquartzite breccia, milky quartz and chert breccia; haematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia.||||||19-SEP-06
37623|Geolsec Formation|62375|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Hematite quartz breccia, sandstone, fine grained apatite, apatite breccia. Geological Province: Pine Creek Orogen.||||||09-FEB-10
37623|Geolsec Formation|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1700-1825Ma. Max. thickness 200m. Hematitic quartzite breccia, milky quartz & chert breccia; hematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia. Unconformably overlies Coomalie Dolostone, Whites Formation.||||||07-JAN-09
37623|Geolsec Formation|65232|5|Briefly described|p51-53, fig. 36, 37, p56- 57|||Over Coomalie Dolostone (fault); under Depot Creek Sandstone. With Depot Creek Sandstone were overthrusted by Mount Partridge Group rocks. Faulted contact with Whites Formation. Sandstone and haematite-quartz breccia. Hydrothermal alteration.||||||09-FEB-10
37623|Geolsec Formation|65339|4|Described|p6 Table 1, pp15-16.|Mesoproterozoic|Mesoproterozoic|Part of this unit was formerly the Buckshee Breccia (Crick 1987). The haematitic quartzite breccia was formerly the basal Depot Creek Sandstone (Malone 1962a, b); later the Hematite Quartzite Breccia (Spratt 1965).||||Unconformably overlies Coomalie Dolostone. Hosts the Geolsec phosphate deposit.|Haematitic quartzite breccia, breccia fragments of shale and recrystallised carbonate; matrix of reddish ferruginous lutite or arenite.|
37623|Geolsec Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Haematitic quartzite breccia, milky quartz and chert breccia; haematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia.|23-NOV-11
37623|Geolsec Formation|67355|5|Briefly described|p7 Fig.5, p14 Fig.8, p17-22, p24, p26||Paleoproterozoic|See also p59-65, p68. Palaeo regolith? Previous mapping (Crick 1987) assigned portions of this unit to the abandoned Buckshee Breccia in the Depot Creek Sandstone. Indicated preserved thickness of 40-200+ m. Hosts the Geolsec phosphate deposit. Stratigraphic age is uncertain. Fault-controlled estuarine depositional environment is most likely.||||Overlies the Coomalie Dolostone (and less commonly the Whites Formation) with a highly irregular and unconformable contact.|Dominantly haematite-quartz breccia, with lesser interbeds of haematitic sandstone, siltstone, mudstone and rare shale breccia. Upper formation is a medium-coarse sandstone with 2-3 mm angular qtz grains, identical in appearance to lower sandstone.|25-JAN-17
37623|Geolsec Formation|69418|5|Briefly described|p3:31, 33|||Rum Jungle area, Pine Creek Orogen. Hosts the Geolsec phosphate deposit (described).|||||Includes fine-grained apatite-rich mudstone and an equivalent brecciated facies.|12-JUL-16
37623|Geolsec Formation|69420|5|Briefly described|p5:7, 14, 54, 75-78, 116-117|Paleoproterozoic|Paleoproterozoic|Rum Jungle region, Central Domain, Pine Creek Orogen. 40-200m thick. Shallow-marine deposits. Considered to be younger than Finniss River Group, as its basal unconformity is not folded. Overlies most of the Rum Jungle U deposits. Hosts eight phosphate rock occurrences; models of ore genesis are discussed.||||Unconformably overlies Coomalie Dolostone and Whites Formation. Is overlain unconformably by the Depot Creek Sandstone.|Haematitic quartzite breccia, haematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia, fault scarp breccia.|12-JUL-16
37623|Geolsec Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||||Nonconformably overlies Lewin Springs Syenite.|Haematitic quartzite breccia, milky quartz and chert breccia; haematitic mudstone, siltstone and sandstone; minor phosphatic siltstone and breccia.|02-MAR-18
24284|Georgina Gap granitic gneiss|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Informal name. Of the Jennings Suite. Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24284|Georgina Gap granitic gneiss|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
24284|Georgina Gap granitic gneiss|39552|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
24284|Georgina Gap granitic gneiss|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24284|Georgina Gap granitic gneiss|39610|6|Mentioned|p6|||||||||
24284|Georgina Gap granitic gneiss|39887|6|Mentioned|Fig.3|||||||||
24284|Georgina Gap granitic gneiss|39888|6|Mentioned|Fig.10|||||||||
24284|Georgina Gap granitic gneiss|48992|3|Fully described|p21|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24284|Georgina Gap granitic gneiss|50369|5|Briefly described|p1.4, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Informal name. Geological Province: Arunta Inlier. Of the Jennings Suite. Age: 1771Ma (U-Pb).||||||07-NOV-08
24284|Georgina Gap granitic gneiss|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Porphyroblastic-feldspar granitic gneiss.||||||19-SEP-06
27961|Gerowie Tuff|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Black chert tuff, pale green tuffaceous greywacke.||||||07-NOV-08
27961|Gerowie Tuff|9691|5|Briefly described|Map Legend|||Of the South Alligator Group. Black cherty tuff, pale green tuffaceous greywacke.||||||
27961|Gerowie Tuff|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Black cherty tuff, pale green tuffaceous greywacke.||||||02-JUN-05
27961|Gerowie Tuff|22479|5|Briefly described|fig1p2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|22810|5|Briefly described|Table2 P4|||Interbedded with Koolpin Formation and Shovel Billabong Andesite||||||
27961|Gerowie Tuff|23122|5|Briefly described|p409, Fig.2, 410|||||||||
27961|Gerowie Tuff|23205|6|Mentioned|p42|||||||||
27961|Gerowie Tuff|23337|5|Briefly described|906|||||||||
27961|Gerowie Tuff|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 7 Table 1, page 13. Of South Alligator Group.||||||
27961|Gerowie Tuff|23715|5|Briefly described|Map legend||Proterozoic|Of the South Alligator Group, in the Rum Jungle and Central Regions.||||||14-APR-08
27961|Gerowie Tuff|23733|5|Briefly described|p32 Fig. 19|||Of South Alligator Group.||||||
27961|Gerowie Tuff|23999|5|Briefly described|p52|||Of the South Alligator Group. Intruded by the Mount Bundey igneous suite. See also Gerowrie Tuff - the two names are used interchangeably throughout the report.||||||07-FEB-11
27961|Gerowie Tuff|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Cherty tuff, greywacke. Age: ~1885Ma. Geological Province: Pine Creek Orogen. See also p30 Fig. 23.||||||07-NOV-08
27961|Gerowie Tuff|24048|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Age: 1885+/-2Ma.||||||07-NOV-08
27961|Gerowie Tuff|24442|5|Briefly described|p27, p44|Paleoproterozoic|Paleoproterozoic|Age: 1885+/-2Ma (SHRIMP zircon).  ||||||07-NOV-08
27961|Gerowie Tuff|35140|6|Mentioned|p321|||||||||
27961|Gerowie Tuff|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|37462|6|Mentioned|Fig.4.8|||||||||
27961|Gerowie Tuff|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Fine to medium pyroclastic, black-green tuffaceous chert, crystal tuff.||||||07-NOV-08
27961|Gerowie Tuff|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|38239|6|Mentioned|Fig.2|||||||||
27961|Gerowie Tuff|38349|6|Mentioned|Table 4|||||||||
27961|Gerowie Tuff|38351|6|Mentioned|Table 3|||||||||
27961|Gerowie Tuff|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|39069|5|Briefly described|Table 1|||||||||
27961|Gerowie Tuff|39357|4|Described|p11|||||||||
27961|Gerowie Tuff|39518|3|Fully described|p7|||||||||
27961|Gerowie Tuff|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Siliceous tuffaceous shale and siltstone; green to grey argillite, grey chert; minor chert nodules and thin beds of banded iron formation.||||||07-NOV-08
27961|Gerowie Tuff|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Brown and grey siltstone, phyllite and argillite, glassy black tuffaceous chert, crystal tuff and victric tuff.||||||07-NOV-08
27961|Gerowie Tuff|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Grey and brown siltstone and phyllite, hornfels, argillite, tuff, chert.||||||07-NOV-08
27961|Gerowie Tuff|40243|6|Mentioned|p139|||Mention Fig.2||||||
27961|Gerowie Tuff|40493|5|Briefly described|Table 1|||||||||
27961|Gerowie Tuff|40495|6|Mentioned|Fig.5|||||||||
27961|Gerowie Tuff|40808|6|Mentioned|p13|||||||||
27961|Gerowie Tuff|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|41125|6|Mentioned|p26|||See also Fig.14||||||
27961|Gerowie Tuff|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27961|Gerowie Tuff|41305|3|Fully described|p16|||||||||
27961|Gerowie Tuff|41309|4|Described|p5|||||||||
27961|Gerowie Tuff|41311|4|Described|p10|||||||||
27961|Gerowie Tuff|41397|6|Mentioned|p8|||||||||
27961|Gerowie Tuff|41466|6|Mentioned|p23|||||||||
27961|Gerowie Tuff|41663|6|Mentioned|p38|||||||||
27961|Gerowie Tuff|41860|6|Mentioned|p442|||||||||
27961|Gerowie Tuff|41873|5|Briefly described|Table 2|||||||||
27961|Gerowie Tuff|41874|5|Briefly described|Fig.8|||||||||
27961|Gerowie Tuff|41877|5|Briefly described|p27|||||||||
27961|Gerowie Tuff|41878|6|Mentioned|Fig.25|||||||||
27961|Gerowie Tuff|42012|3|Fully described|p8|||See also Table 1 p7.||||||19-SEP-06
27961|Gerowie Tuff|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
27961|Gerowie Tuff|42163|6|Mentioned|p61|||||||||
27961|Gerowie Tuff|43140|4|Described|p3||Paleoproterozoic|Of South Alligator Group.||||||07-NOV-08
27961|Gerowie Tuff|43187|5|Briefly described|p2|||||||||
27961|Gerowie Tuff|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|Max. thickness: 400m.||||||07-NOV-08
27961|Gerowie Tuff|43718|6|Mentioned|p10|||1885+/-2 Ma (U-Pb Shimp age)||||||
27961|Gerowie Tuff|43720|6|Mentioned|Appendix,p6|||||||||
27961|Gerowie Tuff|43726|6|Mentioned|p3|||||||||
27961|Gerowie Tuff|43749|6|Mentioned|p30|||Age: 1885 Ma||||||
27961|Gerowie Tuff|43832|3|Fully described|17-18, Table3 p12||Paleoproterozoic|||||||07-NOV-08
27961|Gerowie Tuff|46658|5|Briefly described|p550|||||||||
27961|Gerowie Tuff|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.  Siliceous tuffaceous shale and siltstone; fine-grained silicified tuff, grey chert, minor chert nodules and thin beds of banded iron formation. Conformably overlies Koolpin Fm; conformably overlain by Mount Bonnie Fm.||||||07-NOV-08
27961|Gerowie Tuff|46700|5|Briefly described|P14, Table1 P10||Proterozoic|Age of unit is 1880 Ma.||||||14-APR-08
27961|Gerowie Tuff|47049|6|Mentioned|Fig.2|||||||||
27961|Gerowie Tuff|50586|5|Briefly described|p1.1, 4.5, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite. Intruded by Cullen Supersuite. Age: 1884 +/- 3Ma (U-Pb).||||||07-NOV-08
27961|Gerowie Tuff|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Of South Alligator Group.||||||07-NOV-08
27961|Gerowie Tuff|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Laminated grey, brown and red silicified siltstone; blue-grey and brown argillite; siliceous siltstone and shale, tuff, tuffaceous chert, greywacke and arenite. Overlies: Koolpin Formation. Underlies: Mount Bonnie Formation.||||||02-NOV-04
27961|Gerowie Tuff|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Black cherty tuff, pale green tuffaceous greywacke.||||||
27961|Gerowie Tuff|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the South Alligator Group.||||||
27961|Gerowie Tuff|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Grey and purple silicified shale and siltstone with grey to black chert bands; black glassy vitric tuff, and spotted crystal tuff and minor tuffaceous chert. Overlies Koolpin Formation. Overlain by Mount Bonnie Formation. Of South Alligator Group.||||||11-JAN-05
27961|Gerowie Tuff|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the South Alligator Group.  Age: 1863Ma. Geological Province: Pine Creek Orogen. Siliceous siltstone and phyllite interbedded with pale cherty argillite, black cherty crystal tuff, spotted feldspathic crystal and lithic tuff.||||||14-JAN-05
27961|Gerowie Tuff|61389|5|Briefly described|Map Legend|||Of the South Alligator Group. Siliceous tuffaceous shale and siltstone, green-grey argillite, grey chert, thin BIF beds.||||||
27961|Gerowie Tuff|62375|5|Briefly described|p9, 10 Fig. 3, 19|Paleoproterozoic|Paleoproterozoic|Tuffaceous Sediments. Age: 1885 +/- 2Ma. Of the South Alligator Group. Geological Province: Pine Creek Orogen. Overlies Koolpin Formation. Overlies: Mount Bonnie Formation.||||||09-FEB-10
27961|Gerowie Tuff|62378|5|Briefly described|p5, 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen. Age: 1864 +/-3, 1862 +/- 3Ma. Volcaniclastic hornfels/siltstone. Of the South Alligator Group. Conformably overlies: Koolpin Formation. Conformably underlies: Mount Bonnie Formation.||||||07-NOV-08
27961|Gerowie Tuff|63866|4|Described|p109|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. The numeric age is an ID-TIMS date. SHRIMP analysis has been performed on two samples of this formation and yield ages of 1864 +/- 3 Ma and 1862 +/- 4 Ma (Worden et al, in press).|1884 +/- 3 Ma (Needham et al., 1988)|South Alligator Group||||
27961|Gerowie Tuff|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of South Alligator Group. Age 1863Ma SHRIMP U/Pb.Max thickness 750m. Pale green, brown or grey siliceous siltstone and phyllite interbedded with pale cherty argillite, black cherty crystal tuff, spotted feldspathic crystal tuff and lithic tuff.||||||07-JAN-09
27961|Gerowie Tuff|64730|5|Briefly described|p125, Fig. 3, p126, p127,134-135, 140|Paleoproterozoic|Paleoproterozoic||Depositional ages 1864 +/- 3 Ma, 1862 +/- 4 Ma.|Middle unit of South Alligator Group.||Intruded by Mount Bundey Granite.|Subaerial to sub-aqueous felsic tuffs and volcanigenic sedimentary rocks.|03-MAY-12
27961|Gerowie Tuff|64956|6|Mentioned|p72|||||||||07-FEB-11
27961|Gerowie Tuff|65232|5|Briefly described|p45, p6 Fig. 5, p64, App. 2|Palaeoproterozoic|Palaeoproterozoic|With Shovel Billabong Andesite, is interbedded within upper part of Koolpin Formation. Mount Bonnie Formation conformably overlies these units. Intruded by sills of Zamu Dolerite. Thinly layered cherty tuff, argillite and greywacke; mudstone and phyllite.||||||09-FEB-10
27961|Gerowie Tuff|65339|4|Described|p6 Table 1, p12, p19.|||Forms light-coloured strike ridges and low hills. Thickness c.300 - 400 m. Metamorphosed by Mount Bundey Granite where it is quarried for hard (cherty) rock. Recent age determinations revise the 1885 +/- 2 Ma of Needham et al. (1988). Has high U + Th radiometric response.|1864 and 1862 +/- 3 Ma.|Unit in South Alligator Group.||Overlies Koolpin Formation. Is overlain by Mount Bonnie Formation.|Laminated grey and purple silicified shale and siltstone, with grey to black chert bands; black glassy vitric tuff, spotted crystal tuff; minor tuffaceous chert.|
27961|Gerowie Tuff|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in South Alligator Group.||Overlies Koolpin Formation. Is overlain by Mount Bonnie Formation.|Pale green, brown or grey siliceous siltstone and phyllite interbedded with pale cherty shale, black cherty crystal tuff, spotted feldspathic crystal tuff and lithic tuff; minor felsic ignimbrite, chloritic volcaniclastic shale, and lapilli tuff.|23-NOV-11
27961|Gerowie Tuff|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1885 +/- 3 Ma.|Of South Alligator Group.||||07-APR-20
27961|Gerowie Tuff|67355|5|Briefly described|p4-7, p10, p12-13|Orosirian|Orosirian|1863 Ma is considered the depositional age (SHRIMP); an older age from conventional U-Pb zircon of 1885 +/- 2 Ma has also been found (Needham et al. 1988). Base of the unit defined by the first appearance of tuff. 200-500 m thick. |1864+/-3 Ma and 1862+/-3 Ma(Lally and Worden 2004)|South Alligator Group||Conformably overlies the Koolpin Formation, underlies the Mount Bonnie Formation.|Tuffaceous sedimentary rocks (tuff, chert and pelite). In the map area, laminated light grey silicified siltstone, red and black argillite, thin banded ironstone and tuffaceous chert predominate.|25-JAN-17
27961|Gerowie Tuff|67564|3|Fully described|p7 Table 2, p9 Fig.4, pp21-22.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Contains rocks previously mapped (Walpole 1963) as Gerowie Chert. 750 m of subaerial dacitic volcanic ash, shallow marine sediments and intrusive porphyritic dacite. A conventional U-Pb age from a dacitic tuff gives an age of 1884 +/- 3 Ma.|1863 Ma.|Unit in South Alligator Group.||Conformably overlies Koolpin Formation. Overlies Shovel Billabong Andesite. Is overlain conformably by Mount Bonnie Formation, and unconformably by Pul Pul Rhyolite and Mamadawerre Sandstone.|Siliceous siltstone and phyllite interbedded with pale cherty argillite, black cherty crystal tuff and lithic tuff; minor felsic ignimbrite, chloritic volcaniclastic shale, lapilli tuff; porphyritic dacite.|
27961|Gerowie Tuff|67779|5|Briefly described|p6 Fig.5, p19, p105.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. May represent a volcanic equivalent of Nimbuwah magmatism.|1863 +/- 2 Ma (Worden et al. 2004, 2008b).|Unit in South Alligator Group.||Overlies Koolpin Formation. Is overlain by Mount Bonnie Formation.||
27961|Gerowie Tuff|69418|6|Mentioned|p3:6, 17|||Pine Creek Orogen. Hosts gold deposits (described), as well as the Fleur de Lys vein-type U deposit (briefly described).||||||12-JUL-16
27961|Gerowie Tuff|69420|4|Described|p5:4, 6, 8, 11-12, 14, 32, 36-38, 51-52|Paleoproterozoic|Paleoproterozoic|See also 62, 65, 67, 79, 83, 101, 112. Previously Gerowie Chert. Central Domain, Pine Creek Orogen. Up to 750m thick. Subaerial, shallow marine deposits. Hosts Au deposits in the Brocks Creek goldfield (quartz veins) and elsewhere. Hosts the Fleur de Lys U deposit, and the Rosemary Sn deposit. SHRIMP zircon deposition age; a previous determination of 1885 +/- 2 Ma by Needham et al. (1988) may have had inherited zircons.|1863 +/- 2 Ma (Worden et al., 2008).|South Alligator Group.||Overlies Koolpin Formation. Is overlain by Mount Bonnie Formation. Includes/hosts the Shovel Billabong Andesite.|Green to grey mudstone, siltstone, cherty shale, black cherty crystal tuff and lithic tuff; minor felsic ignimbrite, chloritic volcaniclastic shale, lapilli tuff; porphyritic dacite.|12-JUL-16
27961|Gerowie Tuff|69421|5|Briefly described|p6:3|||SHRIMP U-Pb zircon age.|1863 +/- 3 Ma (Lally and Worden, 2004).|||Is overlain by Burrell Creek Formation.||12-JUL-16
27961|Gerowie Tuff|69917|5|Briefly described|p52|||Pine Creek Orogen, Central Domain||Of South Alligator Group.||||
27961|Gerowie Tuff|70293|5|Briefly described|p597-600, p612|Orosirian|Orosirian|On p600, this age is also attributed to Carville et al. (1990).|1863+/- 2 Ma (Worden et al., 2004, 2008).|South Alligator Group||Overlies Koolpin Formation. Is overlain by Mount Bonney Formation; intruded by Zamu Dolerite.||
27961|Gerowie Tuff|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1862 +/- 3 Ma.|South Alligator Group.||Conformably overlies Koolpin Formation. Is overlain conformably by Mount Bonnie Formation.|Green, brown or grey siliceous siltstone and phyllite interbedded with pale cherty shale; black cherty crystal tuff, spotted feldspathic crystal tuff and lithic tuff; minor felsic ignimbrite, chloritic volcaniclastic shale, lithic and lapilli tuffs.|
27961|Gerowie Tuff|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1864+/-2.9 Ma (MDA: U-Pb zircon SHRIMP)||||Hornfelsed felsic tuff.|
36070|Gibb Member|23404|5|Briefly described|p639 Fig.2|||Of Mainoru Formation.||||||
36070|Gibb Member|23937|2|Defined|p79 App. 1|Calymmian|Calymmian|Reassigned to Mainoru Fm (Collara Subgp, Roper Gp).  Previously mapped as upper part of Limmen Sst.  Conformably overlain by Wadjeli Sst Mmbr; conformably overlies Limmen Sst.  Thickness: 225-250m in type section.  Geological Province: McArthur Basin.||||||01-NOV-04
36070|Gibb Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group). Dark grey and olive-black mudstone, laminated , thin beds of siltstone and fine-grained sandstone.||||||14-FEB-05
36070|Gibb Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Mudstone: dark grey and olive black, laminated, thin interbeds of siltstone and fine grained sandstone.||||||
36070|Gibb Member|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 0-250m thick. Storm-dominated marine sediments.||Basal Mainoru Formation.||Conformably overlies Limmen Sandstone. Is overlain conformably by Wadjeli Sandstone Member.|Dark grey and olive-black mudstone, fine sandstone.|12-JUL-16
36070|Gibb Member|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Storm-dominated shelf (mudstone-dominated)||Base of Mainoru Formation.||Overlies Limmen Sandstone. Overlain by Nullawun Member.||
36070|Gibb Member|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Mainoru Formation||Overlies Limmen Sandstone. Overlain by Nullawan Member.|Interbedded mudstone, siltstone and fine sandstone.|
36070|Gibb Member|70968|3|Fully described|p13,p17-18,p20-23, p131, p140, p143-144|Calymmian|Calymmian|Young and Sweet in Abbott et al. (2001). Originally mapped (Dunn, 1963) as upper part of Limmen Sandstone. Named after Gibb Bluff, Roper Bar area. Type section is from 478100mE 8381000mN (base) to 478000mE 8382000mN in URAPUNGA sheet. A recessive, fine-grained unit: forms poor exposures in low hills or sandstone-capped scarp slopes. Lithology described and illustrated. Thickness estimated to be 225-250m in the type section. Marine storm-dominated shelf setting.||Mainoru Formation.||Conformably overlies Limmen Sandstone. Is overlain by Wadjeli Sandstone Member conformably and gradationally.|Thinly interbedded, dark grey to olive-black laminated mudstone and commonly ripple cross-laminated, silicified, very fine-grained sandstone and siltstone.|24-FEB-17
36070|Gibb Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 0-250m thick. Storm-dominated marine shelf deposits.||Basal Mainoru Formation.||Conformably overlies Limmen Sandstone. Is overlain conformably by Wadjeli Sandstone Member.|Dark grey and olive-black mudrocks; fine sandstone.|
36070|Gibb Member|71488|5|Briefly described|p141 fig 1b|||||Mainoru Formation||Overlies the Limmen Sandstone. Overlain by the Nullawan Member.||
36070|Gibb Member|71494|4|Described|p2, p4, p8-p9, p15, p17-p19, p26|||0-250m thick. Deposited in a storm dominated marine environment. Previously mapped as the upper part of the Limmen Sandstone (Dunn 1963b, 1963c). Core log features presented in this volume.||||Conformably overlies the Limmen Sandstone. Conformably overlain by the Wadjeli Sandstone Member.|Dark-grey and olive-black mudstone and fine sandstone.|
36070|Gibb Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, , Beetaloo Sub-basin, McArthur Basin.||Mainoru Formation||||24-SEP-18
36070|Gibb Member|73242|5|Briefly described|p39|||||Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Limmen Sandstone. Overlain by Wadjeli Sandstone Member.|Includes interbedded mudstone and fine sandstone.|
28284|Gibbie Formation|14019|4|Described|p16|||Of the Wattie Group. Conformably overlies Neave Sandstone; conformably overlain by Seale Sandstone. Siltstone, fine sandstone and rare stromatolitic dolostone. Max Thickness: 31m. Geological Province: Victoria Basin.||||||19-SEP-06
28284|Gibbie Formation|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
28284|Gibbie Formation|24297|3|Fully described|p7|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Seale Sandstone, conformably overlies Neave Sandstone. Maximum thickness: 144m. (in WATERLOO).  See also p5 Tb. 2.||||||19-SEP-06
28284|Gibbie Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Siltstone, sandstone, minor dolostone.||||||19-SEP-06
28284|Gibbie Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Overlies Neave Sandstone; overlain by Seale Sandstone. Geological Province: Victoria Basin.||||||08-AUG-05
28284|Gibbie Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
28284|Gibbie Formation|28255|3|Fully described|p39, Tb. 11 (opp.p8)|Adelaidean|Adelaidean|Of the Wattie Group. Consists of fine-grained interbedded sandstone and siltstone. Conformably overlain by Seale Sandstone; conformably overlies Neave Sandstone. Max. thickness: 75m.  See also p129 Appendix.||||||19-SEP-06
28284|Gibbie Formation|30003|4|Described|p8, p12|||Of the Wattie Group. Blocky to flaggy fine to medium sandstone, small mud pellets in base; minor green and purple siltstone containing muscovite and medium quartz grains. Max. thickness: 34m.||||||19-APR-05
28284|Gibbie Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
28284|Gibbie Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
28284|Gibbie Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Interbedded micaceous siltstone and fine sandstone.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
28284|Gibbie Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Flaggy and fissile siltstone, fine sandstone; minor dolomite.||||||02-DEC-04
28284|Gibbie Formation|32660|5|Briefly described|Table 6|||||||||
28284|Gibbie Formation|33374|6|Mentioned|p7|||Stratigraphy.||||||
28284|Gibbie Formation|33375|5|Briefly described|p7, p8 Tb. 1|||Of the Wattie Group. Overlies the Neave Formation; overlain by Seale Sandstone.||||||26-APR-05
28284|Gibbie Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28284|Gibbie Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group. Interbedded chocolate and greyish green siltstone and fine sandstone.||||||27-APR-05
28284|Gibbie Formation|45112|6|Mentioned|p19|||||||||
28284|Gibbie Formation|48938|6|Mentioned|p22|||Stratigraphy.||||||
28284|Gibbie Formation|48943|2|Defined|p48|Proterozoic|Proterozoic|Strat. section p133.? Adelaidean.||||||19-SEP-06
28284|Gibbie Formation|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Siltstone, sandstone and minor dolostone.  Geological Province: Victoria Basin.||||||24-NOV-04
28284|Gibbie Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone and siltstone. Overlies Neave Sandstone. Overlain by Seale Formation. Of Wattie Group. Geological Province: Victoria Basin.||||||11-JAN-05
28284|Gibbie Formation|60682|5|Briefly described|p7|||Of Wattie Group.||||||
28284|Gibbie Formation|60685|4|Described|p4 Fig. 3, p7|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Thinly bedded micaceous and calcareous siltstone, fine sandstone and rare stromatolitic dolostone. Conformable on Neave Sandstone; conformable below Seale Sandstone. Max. thickness: <70m. Geological Province: Victoria Basin.||||||
28284|Gibbie Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Overlies Neave Sandstone. Is overlain by Seale Sandstone.||
28284|Gibbie Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies Neave Sandstone. Is overlain by Seale Sandstone.|Interbedded siltstone and fine sandstone; rare dolostone.|
28284|Gibbie Formation|68733|5|Briefly described|p177 Fig.2, p182|||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.||Conformably underlain by the Neave Sandstone.||
28284|Gibbie Formation|69432|4|Described|p17:2, 9|||Birrindudu Basin. 25-70m thick. Mostly low-energy shallow-marine deposits, with periods of exposure possibly in a lagoon or embayment.||Wattie Group.||Conformably overlies Neave Sandstone. Is overlain conformably by Seale Sandstone.|Thinly bedded, variably micaceous, ferruginous and calcareous siltstone, fine sandstone and rare stromatolitic dolostone.|12-JUL-16
28284|Gibbie Formation|69673|6|Mentioned|p48 fig 35|||||Wattie Group||Overlies Neave Sandstone, overlain by Seale Sandstone||
28284|Gibbie Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Wattie Group.||Overlies Neave Sandstone. Is overlain by Seale Sandstone.|Interbedded siltstone and fine sandstone; rare dolostone.|24-JAN-22
28284|Gibbie Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Neave Sandstone. Is overlain by Seale Sandstone.|Sandstone and siltstone.|
28284|Gibbie Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Neave Sandstone. Is overlain by Seale Sandstone.|Siltstone, sandstone, minor dolostone.|
28284|Gibbie Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, siltstone|
28284|Gibbie Formation|71302|5|Briefly described|p6,22||Paleoproterozoic|Of Birindudu Basin.||Unit of Wattie Group.||Overlain by Seale Sandstone. Underlain by Neave Sandstone||09-DEC-19
28284|Gibbie Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Wattie Group||Underlain by Neave Sandstone. Overlain by Seale Sandstone.||
27414|Giddy Granite|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
27414|Giddy Granite|24047|5|Briefly described|p82|Paleoproterozoic|Paleoproterozoic|Age: ca.1836Ma.  See also p83 Fig. 71.||||||07-NOV-08
27414|Giddy Granite|24048|3|Fully described|p11|||Geological Province: Arnhem Inlier.||||||
27414|Giddy Granite|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: massive, white to pink, medium to coarse-grained, equigranular, granophyric, fayalite-bearing. Intruded by dykes and sills of microgranite. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
27414|Giddy Granite|32660|5|Briefly described|Table 2|||||||||
27414|Giddy Granite|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27414|Giddy Granite|41406|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
27414|Giddy Granite|41465|5|Briefly described|p8|||||||||
27414|Giddy Granite|42597|5|Briefly described|Map Legend|Paleoproterozoic||||||||07-NOV-08
27414|Giddy Granite|43010|2|Defined|p57||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
27414|Giddy Granite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27414|Giddy Granite|44112|3|Fully described|p1,7,13,22,25-26||Orosirian|||||||
27414|Giddy Granite|45087|5|Briefly described|p15|||Chem. analyses. See also p26.||||||19-SEP-06
27414|Giddy Granite|48894|6|Mentioned|p23|||Age||||||
27414|Giddy 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: 1836 +/- 4Ma (SHRIMP).||||||12-SEP-17
27414|Giddy Granite|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Granite: massive, white to pink, medium to coarse-grained, equigranular, granophyric, fayalite-bearing. Intruded by dykes and sills of microgranite. G eol. Prov: McArthur Basin, Arnhem Inlier.||||||
27414|Giddy Granite|63866|4|Described|p115|Orosirian|Orosirian|Arnhem Inlier, Northern Caledon Shelf.|1836 +/- 4 Ma (Page, OZCHRON)|Giddy Suite|||A-type granites.|
27414|Giddy Granite|69421|4|Described|p6:1-3, 6-7|Orosirian|Orosirian|Arnhem Province. Dunnet (1965), whose Giddy and Caledon Granites were revised by Rawlings et al. (1997), with the latter becoming superseded. Coeval with Bukudal and Garrthalala Granites. Geochemistry briefly described. SHRIMP U-Pb zircon age.|1836 +/- 4 Ma (Rawlings et al., 1997).|Giddy Suite.||?Intrudes Bradshaw Complex. ?Is intruded by Latram Granite.|Granite, pink to grey, medium- to coarse-grained, massive, equigranular to porphyritic, K-feldspar megacrystic (up to 20 cm across), contains fayalite; locally sheared. Calc-alkaline; A-type.|12-JUL-16
27414|Giddy Granite|70719|4|Described|iv, p1, p15-17, p25|Orosirian|Orosirian|Exposed along Giddy River, NE Arnhem Province. Previously dated at 1836 +/- 4 Ma (Page, 1996).|1829 +/- 5 Ma (magmatic crystallisation age)|Giddy Suite.||Is intruded by Latram Granite (inferred). Correlated with Bukudal, Garrthalala and Dhalinybuy Granites.|Coarse-grained, porphyritic to megacrystic, fayalite-biotite granite. A-type. Locally intruded by late-phase microgranite dykes.|06-FEB-18
27414|Giddy Granite|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1836+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
27414|Giddy Granite|71606|5|Briefly described|p135|||McArthur Basin. Based on field relationships, likely to be older, at least pre-dating upper Groote Eylandt Group.||||||
30863|Giddy Suite|24197|5|Briefly described|p29, p54|Paleoproterozoic|Paleoproterozoic|Example of the Sybella Association. Comprises Bukudal, Garrthalala and Dhalinybuy Granites. I-type fayalite-bearing granites. Age: ~1835Ma. Geological Province: Arnhem Block.||||||07-FEB-11
30863|Giddy Suite|50591|5|Briefly described|p1.3, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1835Ma. Geological Province: Arnhem Block/McArthur Basin. Intrudes: Bradshaw Complex. Unconformably underlies: Erringkarri Rhyolite.||||||07-NOV-08
30863|Giddy Suite|63866|5|Briefly described|p115|||Arnhem Inlier, Northern Caledon Shelf.|||Includes the Giddy Granite, Bukudal Granite and the Garrthalala Granite.||A-type granites.|
30863|Giddy Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Arnhem Orogen.||||Intrudes Groote Eylandt Group.||12-JUL-16
30863|Giddy Suite|69421|4|Described|p6:1-3, 5-7|Orosirian|Orosirian|Budd (2002). Dunnet (1965) recognised the Giddy and Caledon Granites. Plumb and Roberts (1992) revised them into four units: Giddy, Garrthalala, Bukudal and Dhalinybuy Granites. These four were included in the Giddy Suite by Budd et al. (2002). Arnhem Province. Essentially undeformed. Little associated mineralisation, but considered to have some potential for Sn, W, Mo and Ta.|c.1835 Ma.||Bukudal, Giddy, Garrthalala and Dhalinybuy Granites.|Correlated with Cullen Supersuite.||12-JUL-16
30863|Giddy Suite|69673|6|Mentioned|p3|||||||||
30863|Giddy Suite|70302|5|Briefly described|iv|||NW Arnhem Province.||||Is overlain unconformably by Yanungbi Volcanics (Spencer Creek Group).|Granites.|
30863|Giddy Suite|70719|5|Briefly described|iv, |Orosirian|Orosirian|Rawlings et al. (1997). Arnhem Province.|||Giddy, Bukudal Granites.||Fayalite-bearing A-type granites.|
30863|Giddy Suite|71605|5|Briefly described|p6||||||||Fayalite-biotite bearing granites.|
30863|Giddy Suite|71620|6|Mentioned|p26|||||||Intrudes the Wonga gneiss.||
30863|Giddy Suite|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||06-MAR-20
67994|Giles Creek Dolostone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Amadeus Basin. Contains fauna of Ordian age.||||||
67994|Giles Creek Dolostone|62376|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
67994|Giles Creek Dolostone|62379|5|Briefly described|p7 Fig. 2, p18|Middle Cambrian|Middle Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
67994|Giles Creek Dolostone|64068|6|Mentioned|p59, 62, 225|||Amadeus Basin. Lower part correlated with Thorntonia Limestone. Upper part correlated with Arthur Creek Formation, Beetle Creek Formation.||||||
67994|Giles Creek Dolostone|64778|6|Mentioned|p13|Cambrian|Cambrian|Amadeus Basin.||||||
67994|Giles Creek Dolostone|64809|5|Briefly described|p2, p3 Fig.2, p15 Fig.15|Middle Cambrian|Middle Cambrian|||Unit in Pertaoorrta Group.|||Dolostone, limestone, siltstone.|
67994|Giles Creek Dolostone|64813|5|Briefly described|p272|Middle Cambrian|Middle Cambrian|Overlies Chandler Formation. Geological province: Amadeus Basin, N.T. Contains aromatic-naphthenic oil.||||||11-FEB-09
67994|Giles Creek Dolostone|65233|3|Fully described|p3 Fig. 2, p8|Middle Cambrian|Middle Cambrian|Of Pertaoorrta Gp. Interfingers with Tempe Fm; disconform.on Chandler Fm. Conform./gradational below Shannon Fm. and interfingers with Jay Creek Limestone in W. Max. thickness: 383m.Geol.prov: Amadeus Basin.Lith+ environmental.depositon details included||||||07-FEB-11
67994|Giles Creek Dolostone|65342|6|Mentioned|p4.|||Amadeus Basin. Max. thickness at least 309 m.|||Includes Dingo Member.|Overlies Chandler Formation. Is overlain by Hugh River Shale.||
67994|Giles Creek Dolostone|67326|5|Briefly described|p2, p5|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Chandler Formation. Is overlain by Shannon Formation.||
67994|Giles Creek Dolostone|68323|6|Mentioned|p4 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
67994|Giles Creek Dolostone|69437|5|Briefly described|p22:10-11|Series 3|Series 2|Amadeus Basin, Centralian B Superbasin. Sequences 1 and 2. Shallow-marine to peritidal deposits.||||Overlies Todd River Dolostone. Underlies Shannon Formation. Equivalent to Tarrara, Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Walbiri Dolostone.|Carbonate and mudstone/siltstone.|12-JUL-16
67994|Giles Creek Dolostone|69438|3|Fully described|p23:2-3, 8, 24-25, 28-31, 43, 59-61|Middle Cambrian|Middle Cambrian|Formerly Giles Creek Dolomite; Wells et al. (1967). Amadeus Basin. Type section is at Ross River, where the clastic component is absent; a (second) reference section is at Ulta Bank Creek on the S limb of the Ooraminna Anticline. Up to 383m thick. Shallow-marine, tidal flat, intracoastal lagoon, shallow open shelf and shoal deposits. Contains stromatolites, brachiopods, molluscs, trilobite fragments and ichnofauna. Lower part is laterally equivalent to Chandler Formation; upper part is laterally equivalent to Tempe Formation and lower Hugh River Shale. Hydrocarbon source rock intervals may be present. May form a seal over Arumbera Sandstone reservoirs. Has low shale gas potential.||Pertaoorrta Group.||Disconformably overlies Chandler Formation and Todd River Dolostone. Is overlain paraconformably by Shannon Formation. Time-equivalent to Gum Ridge Formation, Montejinni and Tindall Limestones.|A succession of mainly carbonate rocks and mudstone/siltstone, often variegated red-brown to green, and minor sandstone. Contains stromatolites, hyoliths, brachiopods, gastropods, trilobites and echinodermal debris.|12-JUL-16
67994|Giles Creek Dolostone|69439|6|Mentioned|p24:10|||Amadeus Basin.||||Lower part correlated with Walbiri Dolostone; upper part with Bloodwood Formation (both of Ngalia Basin).||12-JUL-16
67994|Giles Creek Dolostone|69449|6|Mentioned|p34:2 Fig.34.2; 34:4|Cambrian|Cambrian|Eastern Amadeus Basin.||||||12-JUL-16
67994|Giles Creek Dolostone|69573|6|Mentioned|p656-657, 661|||Amadeus Basin. Features Cambrian Stage 5 fossil sites.||||||
67994|Giles Creek Dolostone|69673|5|Briefly described|p77, p80, p82, p88, p89, p91, p103,|Cambrian|Cambrian |Potential source rock, potential for unconventional petroleum.|||Includes Dingo Member|Overlies Chandler Formation, overlain by Shannon Formation, correlated with Arthur Creek Formation|Mainly carbonates with mudstone/siltstone and minor sandstone.|
67994|Giles Creek Dolostone|70752|4|Described|p125-141|Middle Cambrian|Middle Cambrian|Wells et al. (1967). Amadeus Basin. The type section is in Ross River Gorge, where the unit is 187m thick. Age is Cambrian Series 3, Stage 5. Contains well-preserved trilobites, and brachiopods with closest affinity with faunas in the NSW Koonenberry Belt. Lithostratigraphic column with brachiopod taxa and their ranges. Early Templetonian. Systematic palaeontological descriptions.||Pertaoorrta Group.||Disconformably overlies Todd River Dolostone.|Largely dominated by micritic limestone, dolostone and numerous interbeds of shale; the micritic limestone and shales more common at the base, and the dolostone predominant toward the top.|
67994|Giles Creek Dolostone|71114|5|Briefly described|p171, p170 fig 1b, p172-4, p176-180|Drumian|Stage 5|Amadeus Basin. Cambrian Series 3 Stage 5 age is based on trilobite biostratigraphy. Deposited between ~511 Ma and 490 Ma, on an open shallow marine, subtidal carbonate platform during sea level highstand. 269m thick in Dingo 1 well. Includes up to 16% anhydrite in Dingo 2, and 25% in Alice 1.||||Overlies Chandler Formation. Is overlain by Hugh River Shale.||14-FEB-18
67994|Giles Creek Dolostone|71279|5|Briefly described|p355 Fig.2|Middle Cambrian|Middle Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
67994|Giles Creek Dolostone|72358|6|Mentioned|p118|Series 3|Series 3|Of Amadeus Basin.||||||
67994|Giles Creek Dolostone|72516|6|Mentioned|p91-92|Cambrian|Cambrian|Amadeus Basin. Lower part age equivalent of the Thorntonia Limestone, and the top considered equivalent to the Arthur Creek Formation.||||||02-JUN-21
67994|Giles Creek Dolostone|73085|6|Mentioned|p1|middle Cambrian|middle Cambrian|||Pertaoorrta Group [and equivalents?]||Unconformably[?] underlain by Arumbera Sandstone and Todd River Dolostone. Partly underlain by and equivalent to Chandler Formation. Overlain by Shannon Formation. Equivalent to Hugh River Shale.||
32943|Gillen Formation|48880|14|Not recorded|p.16||Neoproterozoic|Ref. to Banks 1964 (unpubl). Suggested subdivision of Bitter Springs Limestone. U.Prot.||||||
32943|Gillen Formation|71001|5|Briefly described|p16, 18, 20, 22-23, 25-28|Tonian|Tonian|Amadeus Basin. Formerly Gillen Member (of Bitter Springs Formation). Shallow-marine, lagoon (salina) environment. Closely folded due to salt tectonism.||Bitter Springs Group.||Overlies Heavitree Quartzite. Is overlain by Loves Creek Formation.|Grey to yellow, brecciated limestone/dolostone interbedded with gypsum/anhydrite and siltstone.|
32943|Gillen Formation|71080|5|Briefly described|p9, 26, p29, 30, 31|Tonian|Tonian|Amadeus Basin. Supersequence 1. Part of Gillen-Heavitree pertroleum system. Includes intraformational salt seal over shaly source rocks. Also includes possible reservoirs in intraformational sandstone. Compared with unnamed carbonate unit in Murraba Basin.||Base of Bitter Springs Group.||Directly overlies the Heavitree Formation.|Dominantly carbonate and salt.|
32943|Gillen Formation|71279|5|Briefly described|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||Bitter Springs Group.||||
32943|Gillen Formation|71344|4|Described|p1094, 1093, 1096, 1098-1100, 1102-3|Tonian|Tonian|Amadeus Basin. Algal prokaryote fossils indicate periodically stagnant, hypersaline lagoons in an arid depositional setting.|~850-750 Ma||||Grey to yellow, brecciated limestone/dolostone interbedded with gypsum/anhydrite and siltstone. Evaporite sequence of multiple cycles of halite, anhydrite and partly magnesite near middle of unit.|
32943|Gillen Formation|71841|5|Briefly described|p1,8|Cryogenian|Cryogenian|Of Amadeus Basin. Previously termed Gillen Member. Status upgraded to Formation and formalised by Normington et al (2015), Normington and Donnellan (in review). ||Unit of Bitter Springs Group.||Lowermost unit of Bitter Springs Group. Overlain by Loves Creek Formation. Underlain by Dean Quatzite or Heavitree Formation. Grades into Pinyanna beds.||
32943|Gillen Formation|71842|5|Briefly described|p3|Cryogenian|Cryogenian|Of Amadeus Basin.||Unit of Bitter Springs Group.||||
32943|Gillen Formation|72369|5|Briefly described|p43|||Of Amadeus Basin.||Unit of Bitter Springs Group.||Lowermost unit of Bitter Springs Group. Overlain by Loves Creek Formation.||
32943|Gillen Formation|72375|4|Described|p1-2,10-13|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Type area: central LIMBLA 1:100 000 mapsheet. Comprises five lithofacies (units 1-5), as defined by Lindsay (1993); sample NTGS IC13CJE003 is interpreted as representative of unit 2. SHRIMP U-Pb zircon analysis by Kositcin et al., 2015 yielded an interpreted max depositional age (youngest 206Pb/238U) of 896+\-24 Ma (considerably older than inferred c. 820 Ma deposition of Bitter Springs Group). LA-ICP-MS Hf isotopic signatures for the zircon age populations from NTGS IC13CJE003 (micaceous quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p12 for Hf isotopic results and interpretations). Zircon morphology, SHRIMP analyses, Hf analyses and results are discussed.||Unit of Bitter Springs Group.||Lowermost unit of Bitter Springs Group. Underlain paraconformably by Heavitree Formation.|Dolostone, limestone, siltstone, micaceous quartz sandstone, shale, and evaporites.|04-DEC-19
32943|Gillen Formation|72489|5|Briefly described|p6, p7 Fig.6, p7, p9|Tonian|Tonian|Includes dolostone in the lower parts of this formation. Sampled for carbonate 13C.||Bitter Springs Group||Overlain by Loves Creek Formation.|Includes dolostone.|
32943|Gillen Formation|72601|5|Briefly described|p3, p7, p25|Tonian|Tonian|Amadeus Basin. Previously the Gillen Member.||Bitter Springs Group||Underlain by Heavitree Formation and Dean Quartzite. Overlain by Loves Creek Formation.|[Includes] evaporites.|
32943|Gillen Formation|73085|6|Mentioned|p1|Tonian|Tonian|Amadeus Basin. Previously called Gillen Member.||Bitter Springs Group||Underlain by Dean Quartzite and Heavitree Formation. Overlain by Loves Creek Formation. Equivalent to Pinyinna beds.||
32943|Gillen Formation|73086|1|Redefined|[See comments].|Tonian|Tonian|[Redefined herein. See also definition card, ASUD]. Re definition of unit/upgrade from member to Formation based on distinct lithostratigraphic character, great thickness and wide distribution. Characterised by disharmonic folding associated with salt withdrawal. Contains five unnamed informal members [which are lithologically described in great detail; see definition card]. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Type section thickness: ~1508 m. Salt mobility has resulted in considerable local variability in the thickness. Maximum thickness: >2200 m[?]. May correlate specifically with the Pinyinna beds because of the conformable to transitional basal boundary with quartzite units. Possibly correlative with Albinia Formation, Yackah beds (in part), Lewis Range Sandstone, Young Husband Conglomerate equivalent and Coominaree Dolomite equivalent of the Arkaroola Subgroup. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. p: iii, ~5-9, 14-28, 30-35, 38, 49, 62, 100, 114, 118, 122, ~143-153, 158, 167, App 2.|~896-820 Ma|Bitter Springs Formation||Underlain by Heavietree Formation. Conformably overlain by Loves Creek Formation. Unconformably overlain by Areyonga Formation, Pioneer Sandstone, Olympic Formation and Gaylad Sandstone.|Dolostone, stromatolitic dolostone and cherty limestone; minor grey shale and cross-bedded sandstone; rare evaporites, gypsiferous siltstone, micaceous green shale, and granule conglomerate.|
32943|Gillen Formation|73088|5|Briefly described|piii, p1-4, p7-12|Tonian|Tonian|Amadeus Basin. Present in drillhole BL002 (34 - 173.5 m, EOH). Previously called Gillen Member.||Bitter Springs Group||Underlain by Heavitree Formation. Overlain by Loves Creek Formation.|Grey siltstone, black shale, dolostone, calcareous and carbonaceous siltstone with red mottles, red and orange banding, disseminated or beds of sulfides, thin calcite veins, and possible stromatolites. Minor orange-ish, silty, fine-grain sandstone.|
32943|Gillen Formation|73180|6|Mentioned|p48 Fig.1, p49-51, p53|Neoproterozoic|Neoproterozoic|Amadeus Basin. Contains salt deposits, halotectonics induced isolated high points in overlying units including the Areyonga-Aralka sequence.||Bitter Springs Group|Lower Gillen Formation, Middle Gillen Formation, Upper Gillen Formation|Conformably overlies the Heavitree Quartzite, Dean Quartzite. Disconformably underlies the Loves Creek Formation.|Contains salt deposits.|
32943|Gillen Formation|73338|6|Mentioned|p5|||Unconformably overlies basement in the Mount Kitty 1 well.||Bitter Springs Group||||
28045|Gimbat Ignimbrite Member|23363|5|Briefly described|351 Tab.2|Statherian|Orosirian|Age: 1794+/-11Ma.||||||19-SEP-06
28045|Gimbat Ignimbrite Member|24340|5|Briefly described|p147 Fig. 3|||Overlain by the Big Sunday Formation. Overlies the Pul Pul Rhyolite.||||||
28045|Gimbat Ignimbrite Member|43718|2|Defined|p2,43-48|||||||||
28045|Gimbat Ignimbrite Member|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Intruded by an unnamed porphyry.|1828 +/- 4, 1827 +/- 4 Ma (Jagodzinski, unpub)|||Intruded by the El Sherana Group.||
28045|Gimbat Ignimbrite Member|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1867+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Siliciclastic sedimentary rock.|
23618|Glass Hill Sandstone|22537|6|Mentioned|42|||Parent Mahoney Group||||||
23618|Glass Hill Sandstone|23621|5|Briefly described|p36|Devonian|Devonian|Of Mahony Group. Geological Province: Ord Basin.||||||
23618|Glass Hill Sandstone|23622|5|Briefly described|Map Legend|Devonian|Devonian|Of Mahony Group. Geological Province: Ord Basin.||||||
23618|Glass Hill Sandstone|40993|6|Mentioned|Fig.1|||||||||
23618|Glass Hill Sandstone|41598|5|Briefly described|p412|||||||||
23618|Glass Hill Sandstone|41811|6|Mentioned|p210|||Previously Elder Sandstone||||||
23618|Glass Hill Sandstone|41840|4|Described|p44|||||||||
23618|Glass Hill Sandstone|41864|3|Fully described|p56|||||||||
23618|Glass Hill Sandstone|41865|5|Briefly described|Map legend||Frasnian|||||||
23618|Glass Hill Sandstone|41866|5|Briefly described|Map legend|Frasnian||||||||
23618|Glass Hill Sandstone|42030|4|Described|p750|||||||||
23618|Glass Hill Sandstone|42821|5|Briefly described|p7|||||||||
23618|Glass Hill Sandstone|42829|6|Mentioned|p146|||||||||
23618|Glass Hill Sandstone|43299|5|Briefly described|Map Legend||Devonian|||||||
23618|Glass Hill Sandstone|43855|5|Briefly described|Map Legend||Frasnian|||||||
23618|Glass Hill Sandstone|44868|5|Briefly described|Map Legend||Frasnian|||||||
23618|Glass Hill Sandstone|60519|5|Briefly described|Map Legend|Frasnian|Frasnian|Geological Province: Ord Basin. Of the Mahony Group. Medium to fine grained quartz arenite; minor pebbly sandstone, conglomerate and siltstone.||||||05-NOV-04
23618|Glass Hill Sandstone|64580|6|Mentioned|map legend|||Of Mahony Group.||||||15-DEC-08
23618|Glass Hill Sandstone|65417|5|Briefly described|p165.|Frasnian|Frasnian|Hardman Sub-basin. Upward-coarsening fluvial deposits from uplift of the Osmand Range to the north.||||||
23618|Glass Hill Sandstone|67860|4|Described|p418 Tb.4-18, p422-423 Figs.4-88,89|Frasnian|Frasnian|Forms spectacular joint-controlled sandstone towers in Bungle Bungle Range. 200-1,000 m thick. Type section details given. Contains rare unidentified bivalve fossils. Also appears as Glasshill Standstone [!] in Fig.4-88.||Mahony Group||Unconformably overlies Goose Hole Group. Laterally equivalent to Boll Conglomerate and Purralili Sandstone.|Pebbly quartz sandstone; minor siltstone, conglomerate.|
23618|Glass Hill Sandstone|68656|6|Mentioned|GEOL_LUT_CSV/500k_geologyp08_lut|Frasnian|Frasnian|||Mahony Group||||
23618|Glass Hill Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Ord Basin||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|31-JUL-15
23618|Glass Hill Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|
23618|Glass Hill Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny.|382.7-372.2 Ma (Biostrat)|Unit of Mahony Group.|||Pebbly sandstone; minor siltstone and conglomerate|
23618|Glass Hill Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|||||Mahony Group|||Pebbly sandstone; minor siltstone and conglomerate.|
23618|Glass Hill Sandstone|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|382.7-372.2 Ma (biostrat)|Unit of Mahony Group.|||Medium- to fine-grained quartz arenite; minor pebbly sandstone, conglomerate and siltstone|
23618|Glass Hill Sandstone|73255|6|Mentioned|p534 Fig.2|Devonian|Devonian|||Mahony Group||Overlies the Buchanan Sandstone, underlies the Boll Conglomerate.||
38413|Gleeson Formation|23733|6|Mentioned|p31|||Of the Renner Group.||||||
38413|Gleeson Formation|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||
38413|Gleeson Formation|24303|2|Defined|p24, p59 Appendix|Calymmian|Calymmian|Of the Renner Group. Overlain by the Baralandji Formation. Max. Thickness: 650m. Previously mapped as undifferentiated Tomkinson Creek beds. Phelp Sandstone and Rising Sun Conglomerate in northern TENNANT Creek may be correlatives. See also p23 Tb.3||||||
38413|Gleeson Formation|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Conglomerate; lithic to quartz arenite;lensing, thin to very thick bedded, granular to cobble; micaceous sandstone, pebbly sandstone, lag conglomerate; mudstone, convolute laminated, graded, crossbedded, current lineated, megarippled||||||18-OCT-05
38413|Gleeson Formation|24442|5|Briefly described|p15|||Of the Renner Group.  Geological Province: Ashburton Province.||||||
38413|Gleeson Formation|61406|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group. Undifferentiated rocks: quartz arenite, sublithic arenite, siltstone; minor mudstone and conglomerate; rare stromatolitic dolostone. In the Tennant Creek region.||||||12-OCT-05
38413|Gleeson Formation|64780|6|Mentioned|p63 Fig.4|Mesoproterozoic|Mesoproterozoic|||Of the Renner Group||||
38413|Gleeson Formation|65209|5|Briefly described|p38|||||Renner Group||Possible correlation with Rising Sun Conglomerate.|Conglomeratic units.|05-JAN-17
38413|Gleeson Formation|67175|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Tennant Region.||Unit in Renner Group.|||Conglomerate, pebbly sandstone, lithic and quartz arenite, and mudstone.|
38413|Gleeson Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Renner Group.||||
38413|Gleeson Formation|69424|5|Briefly described|p9:27|Mesoproterozoic|Mesoproterozoic|||Basal Renner Group.|||Includes conglomerate.|12-JUL-16
38413|Gleeson Formation|69431|4|Described|p16:6, 15-20, 23|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. c.30-650m thick. Moderate- to high-energy fluviatile and possibly lacustrine (at base of unit) deposits. Is overlain unconformably by Anthony Lagoon Formation and Muckaty Sandstone Member (Helen Springs Volcanics).||Basal Renner Group.||Unconformably overlies Bootu, Attack Creek, Morphett Creek, Carruthers, Shillinglaw, Willieray Formations and Short Range Sandstone. Is overlain conformably (gradationally) by Baralandji Formation.|Mainly lithic, sublithic and quartz sandstone, with coarse pebbly sandstone and conglomerate locally. Local basal micaceous sandstone and shale. Very wide range of sedimentary structures (listed). Comprises coarsening- and thickening-upward cycles.|12-JUL-16
38413|Gleeson Formation|69673|6|Mentioned|p58|||||Renner Group||||
38413|Gleeson Formation|70968|2|Defined|v, p93-99, p101, p124, p126-129, p131|Calymmian|Calymmian|See also p138-140, p143. Hussey, Beier, Crispe and Donnellan in Hussey et al. (2001). Named after Gleeson Creek. Originally mapped as undivided Tomkinson Creek beds (Randal et al., 1966). Mainly forms upstanding, low relief strike ridges. The type section is 354900mE 7980200mN (base) to 356400mE 7981500mN in HELEN 100k sheet. Details of a reference section are also given. Some or all outcrops assigned to Rising Sun Conglomerate in TENNANT CREEK sheet may belong to this unit. Lithology described and illustrated in detail. 30-650m thick. Transgressive, fluvial to shallow-marine sediments. Detrital zircon diagram and discussion. Equivalent to Phelp Sandstone.|c.1755 Ma (maximum depositional age).|Renner Group.||Unconformably overlies Tomkinson Creek and Namerinni Groups. Is overlain conformably and transitionally by Baralandji Formation, and locally onlapped by Anthony Lagoon Formation.|Variably sorted and micaceous, thinly to very thickly cross-bedded sandstone and pebbly sandstone, with some laminated micaceous mudstone and minor conglomerate. A variety of sedimentary structures described.|
38413|Gleeson Formation|71893|4|Described|iii, p2-p3, p8, p52-p55|Ectasian|Statherian|Tomkinson Province. Appears in Hussey et al, 2001. This unit also yielded an isolated younger age of 1686 Ma. Interpreted to have been deposited under a moderate- to high-energy, shallow water conditions in a broadly transgressive depositional environment ranging from mostly fluvial to shallow marine. A maximum depositional age of 1796 +/- 10 Ma was obtained in addition to a youngest individual age of 1686 +/- 48 Ma. A Statherian to Ectasian age is interpreted on the basis of rough dating of the underlying Namerinni Group and SHRIMP dating of an unnamed dyke which intrudes this unit. Sampling location, Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Basal Renner Group||Unconformably overlies the Namerinni and Tomkinson Creek groups. Conformably overlain by the Baralandji Formation.|Variably sorted and micaceous, thinly to very thickly cross-bedded sandstone and pebbly sandstone with some laminated micaceous mudstone and minor conglomerate.|
79224|Gloaming Formation|72369|4|Described|iii,p3-4,15-18,20|||Of Amadeus Basin. Defined by Donnellan and Normington 2017. Outcrops as fissile to flaggy, red-brown, ridge-forming sandstone. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND411 (fine- to medium-grained sandstone) yielded an interpreted maximum depositional age of 640+\-6 Ma (youngest concordant zircon), but predates the inferred 580-530 Ma Winnall Group depositional age. Contains significant proportion of detrital zircons derived from Musgrave Province (between c. 1445 Ma and c. 1000 Ma age spectrum, but c. 1100 Ma zircons could be derived from Warumpi Province as well) and Aleiron and Warumpi provinces (c. 1800 to c. 1490 Ma age spectrum). Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Winnall Group.||Overlain by Froud Formation. Underlain by Breaden Formation.|Alternating thin and medium-bedded, fine- to medium-grained, wellsorted and well-rounded sandstone.|18-DEC-19
79224|Gloaming Formation|72374|5|Briefly described|p14|||Of Amadeus Basin. Provenance spectra dominated by Musgrave Province-sourced zircon with lesser zircon sourced from Aileron and Warumpi provinces.||Unit of Winnall Group.||||
79224|Gloaming Formation|73086|4|Described|p126-129|||Defined from the central Amadeus Basin. Correlation with Waldo Pedlar Member is based on their similar cyclical alternation in sandstone bed thickness, similarly abundant sedimentary structures and inferred similar stratigraphic position.||Winnall Group||Directly correlates to Waldo Pedlar Member (Pertatataka Formation).||
79224|Gloaming Formation|73279|5|Briefly described|p3, p7|Ediacaran|Ediacaran|Amadeus Basin, central and western. Detrital zircons analysed for Hf isotopic composition [see article].||||May be equivalent to Pertatataka Formation.|Includes sandstone.|
81659|Glyde package|72373|5|Briefly described|p1-2|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Informal nomenclature of Rawlings et al (1997) and Rawlings (1999). A basin-wide non-genetic depositional pacakge within the McArthur Basin.||||Overlain by Favenc pacakge. Underlain by Goyder package.||
81659|Glyde package|72718|5|Briefly described|p5, p6-8, p10-14, p18, 20|Statherian|Statherian|Minimum depositional age from tuffs in the upper parts of the succession. Maximum age from underlying Redbank package (Tanumbirini Rhyolite). Along with Favenc package, considered equivalent to Isa Superbasin.|ca 1710 Ma to more than 1610 Ma||||Thick (up to 5 km) cyclic succession of evaporitic and marine carbonate rocks, tuff, mudrocks and sandstone deposited in environments ranging from locally deep-marine to shallow-marine to emergent to fluvial and continental.|
81659|Glyde package|72912|6|Mentioned|p5, 18.|Statherian|Statherian|Of Rawlings, 1999.||||Overlies Goyder package and underlies Favenc package.||
24291|Gnallan-a-gea Arkose|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Pebbly arkose, sandstone, siltstone, shale. Overlies: Wonnadinna Dolomite. Underlies: Grant Bluff Formation.||||||28-OCT-04
24291|Gnallan-a-gea Arkose|22649|6|Mentioned|p 152|||Province - Georgina Basin.||||||
24291|Gnallan-a-gea Arkose|35798|6|Mentioned|Fig.1|||Geological map of Desert Syncline.||||||
24291|Gnallan-a-gea Arkose|35863|6|Mentioned|Table 1|||||||||
24291|Gnallan-a-gea Arkose|37928|6|Mentioned|Fig.4|||||||||
24291|Gnallan-a-gea Arkose|41429|6|Mentioned|p247|||||||||
24291|Gnallan-a-gea Arkose|45155|6|Mentioned|Fig.7|||Georgina Basin||||||
24291|Gnallan-a-gea Arkose|46903|6|Mentioned|Fig.3|||Magnetic polarity sequences||||||
24291|Gnallan-a-gea Arkose|48990|2|Defined|p11|Adelaidean|Adelaidean|||||||
24291|Gnallan-a-gea Arkose|49027|5|Briefly described|p5|||||||||
24291|Gnallan-a-gea Arkose|61732|6|Mentioned|p108 Fig 40|||Probably partly overlain (in places) by the basal pebbly conglomerate of the Elyuah Formation.||||||07-FEB-11
24291|Gnallan-a-gea Arkose|65338|5|Briefly described|p iv, p63.|Ediacaran|Ediacaran|Probable correlative is recognised in the Boko Formation above the cap dolostone, but not mapped separately in MOUNT PEAKE. Locally interdigitates with Elyuah Formation.||Unit in Mopunga Group.||Is overlain by Grant Bluff Formation.||
24291|Gnallan-a-gea Arkose|67323|5|Briefly described|GIS attrib tbl|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Pebbly feldspathic sandstone, siltstone and shale.|
24291|Gnallan-a-gea Arkose|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump and Sun Hill Arkoses, Little Burke and Yardida Tillites, are all mapped under the symbol, -P-Cg.||||||
24291|Gnallan-a-gea Arkose|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |More than 1450m thick.||Mopunga Group||Overlain by Grant Bluff Formation|Arkose, sandstone, siltstone and shale.|
24291|Gnallan-a-gea Arkose|73086|6|Mentioned|p118, 122|||Georgina Basin, south-eastern.||||Possibly correlates to Gaylad Sandstone and Pertatataka Formation.||
69657|Goat Paddock beds|61155|5|Briefly described|p16|Early Eocene|Early Eocene|Age: ~56.5-~53.5Ma. Thickness: 212m. Geological Province: overlies Ord and Wiso Basins.||||||14-SEP-18
69658|Golliger beds|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|Overlain by Brunette Limestone. Age: <22.5Ma. Thickness: 15m. Geological region: Barkly Tableland.||||||
69658|Golliger beds|65337|6|Mentioned|p69.|Cenozoic|Cenozoic|In BAUHINIA DOWNS area. May correlate with Cleanskin beds, Brunette and Austral Downs Limestones.||||||
69658|Golliger beds|69458|5|Briefly described|p42:21|Miocene|Miocene|Northern Barkly Tableland and southern Gulf of Carpentaria regions. Low outcrops. Up to 15m thick. Contains gastropods. Lacustrine deposits. Early to middle Miocene.||||Is overlain by Brunette Limestone.|Massive, white to yellow limestone; grey sandy limestone; contains abundant gastropods.|12-JUL-16
42477|Goodparla Dolerite|24442|6|Mentioned|p27|||||||||
42477|Goodparla Dolerite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Dark grey, medium olivine metadolerite.  Age: 1870Ma?  Geological Province: Pine Creek Orogen.||||||23-DEC-09
42477|Goodparla Dolerite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1860Ma. Max. thickness 300m. Dark grey, medium olivine metadolerite. Intrudes Masson Formation.||||||07-JAN-09
42477|Goodparla Dolerite|64730|6|Mentioned|p126|Paleoproterozoic|Paleoproterozoic|Possibly correlates with Zamu Dolerite.||||May intrude Finniss River Group.||03-MAY-12
42477|Goodparla Dolerite|65232|6|Mentioned|p44 Fig. 29|||See also misspelt Goodparlia Dolerite.||||||09-FEB-10
42477|Goodparla Dolerite|67564|3|Fully described|p iv, p7 Table 2, p10 Fig.5, p12, p31.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. 300 m thick; continental pre-orogenic intrusive olivine tholeiite. Forms distinctive red soil with dense vegetation. Previously mapped by Stuart-Smith et al. (1984) and Stuart-Smith et al. (1988a) as Oenpelli Dolerite and as an unnamed dolerite. Has a weak magnetic signature. Has very similar major- and trace-element compositions to amphibolites within the Cahill Formation.|c.1860 Ma.|||Intrudes Cahill and Masson Formations.|Dark grey, medium-grained olivine metadolerite with an ophitic texture.|
42477|Goodparla Dolerite|69420|5|Briefly described|p5:13-14, 67, 79|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Barramundi Dome area, and between Old Goodparla ruins and Goodparla. Distinguished (from Zamu Dolerite) by its darker colour, absence of quartz grains, and magnetic properties.||||Intrudes Masson and Cahill Formations.|Dark-grey, medium-grained olivine metadolerite with an ophitic texture.|12-JUL-16
23629|Goose Hole Group|14019|4|Described|p21|Middle Cambrian|Middle Cambrian|Contains all the Middle and Late Cambrian sedimentary rocks of the Ord Basin.  Subdivided into the Negri (below) and Elder (above) Subgroups.  Limestone, sandstone.  Max. thickness: 700m.  Geological Province: Ord Basin.  See also p3 Fig. 2.||||||
23629|Goose Hole Group|22547|3|Fully described|p30||Early Cambrian|Geological province: Ord Basin. Age: 525 Ma.||||||14-NOV-06
23629|Goose Hole Group|22814|5|Briefly described|fig2|Middle Cambrian|Middle Cambrian|||||||
23629|Goose Hole Group|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Of Goose Hole Group. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|24503|5|Briefly described|Map legend|Ordovician|Middle Cambrian|Sandstone, limestone, stromatolitic limestone, siltstone and mudstone.  Geological Province: Ord Basin.||||||01-FEB-16
23629|Goose Hole Group|40993|6|Mentioned|Fig.1|||||||||
23629|Goose Hole Group|41598|5|Briefly described|p412|||||||||
23629|Goose Hole Group|41840|3|Fully described|p40|||||||||
23629|Goose Hole Group|41864|4|Described|p15|||||||||
23629|Goose Hole Group|41865|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|||||||
23629|Goose Hole Group|41866|6|Mentioned|Map legend|Late Cambrian||||||||
23629|Goose Hole Group|43299|5|Briefly described|Map Legend||Cambrian|||||||
23629|Goose Hole Group|43853|5|Briefly described|Map Legend||Ordian|||||||
23629|Goose Hole Group|43855|5|Briefly described|Map Legend||Middle Cambrian|||||||
23629|Goose Hole Group|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
23629|Goose Hole Group|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
23629|Goose Hole Group|60419|5|Briefly described|p1|Late Cambrian|Middle Cambrian|Max. thickness: 700 m. Conformably overlies Antrim Plateau Volcanics. Geological Province: Ord Basin.||||||
23629|Goose Hole Group|60519|5|Briefly described|Map Legend|Late Cambrian|Middle Cambrian|Includes: Negri Subgroup, Elder Subgroup. Geological Province: Ord Basin.||||||03-NOV-04
23629|Goose Hole Group|60589|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|Limestone, sandstone.  Unconformably overlies the Antrim Plateau Volcanics.  Geological Province: Ord Basin.||||||
23629|Goose Hole Group|64443|6|Mentioned|p40|||Of Ord Basin. Correlative of Barkly Group, Georgina Basin.||||||
23629|Goose Hole Group|64580|4|Described|map legend|Furongian|Middle Cambrian|Undivided; sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone; includes HEADLEYS and LINNEKAR LIMESTONES, NELSON SHALE, PANTON FORMATION, and EAGLE HAWK and OVERLAND SANDSTONES.||||||09-DEC-08
23629|Goose Hole Group|67151|5|Briefly described|Map legend.|Cambrian|Cambrian|Ord Basin.|||Includes Headleys Limestone.|||
23629|Goose Hole Group|67860|4|Described|p416 Fig.4-84, p417, p419 Tb. 4-18|Cambrian|Cambrian|See also p421 fig 4-86. 180-700m thick shallow marine to fluvial sediments. Appears also as Goosehole Group.|||Includes Negri and Elder Subgroups.|Conformably overlies Antrim Plateau Volcanics.|Siltstone and sandstone; minor limestone.|
23629|Goose Hole Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Stage 5|Ord Basin? Also says grouped as Cambrian-Ordovician sedimentary rocks, Southern Bonaparte Basin.|||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone.|31-JUL-15
23629|Goose Hole Group|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Cambrian|See also 500k_geologyp08_lut.csv.|||Includes Elder Subgroup, Negri Subgroup||Undivided; sandstone, siltstone, minor limestone (in parts stromatolitic) and mudstone.|
23629|Goose Hole Group|69443|6|Mentioned|p28:21|||Ord Basin.||||Correlated with Barkly Group.||12-JUL-16
23629|Goose Hole Group|69448|5|Briefly described|p33:1-8|Late Cambrian|Middle Cambrian|Traves (1955); Mory and Beere (1985, 1988). Contains the entire Ord Basin succession in NT. Total thickness c.700m. Displaced by  the NW-trending Negri Fault.|||Negri, Elder Subgroups.|Is overlain unconformably by Mahony Group.||12-JUL-16
23629|Goose Hole Group|69634|4|Described|GEOL_LUT_CSV files|Furongian|Stage 5|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|509-485.4 Ma (Inferred)||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone|
23629|Goose Hole Group|69673|6|Mentioned|p192|||700m thick.|||Includes Negri Subgroup, Elder Subgroup|||
23629|Goose Hole Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian|See also 500k_interpgeop_lut.csv.|485-509 Ma||Includes Elder Subgroup, Negri Subgroup||Sandstone, siltstone, minor limestone and mudstone.|
23629|Goose Hole Group|70655|5|Briefly described|Map Legend|Cambrian|Cambrian|Ord Basin.|||Includes Headleys Limestone.|||
23629|Goose Hole Group|70826|6|Mentioned|p7 tbl 3|Cambrian|Cambrian|Ord Basin.||||||
23629|Goose Hole Group|70851|6|Mentioned|p17-p18|||||||||
23629|Goose Hole Group|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.|||Includes the Negri and Elder Subgroups.|||
23629|Goose Hole Group|71267|4|Described|GEOL_LUT_CSV files|Furongian|Stage 5|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, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|508-485.4 Ma (inferred)||Includes Elder Subgroup, Negri Subgroup.||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone|
23629|Goose Hole Group|71800|4|Described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin. Approximately 700m thick in the Hardman syncline.|||Includes the Negri Subgroup and the Elder Subgroup.|Conformably overlies the Antrim Plateau Volcanics.||
23629|Goose Hole Group|72034|5|Briefly described|500k_interpgeop16_lut|Furongian|Stage 5|Ord Basin.|||||Sandstone, siltstone, minor limestone (in part stromatolitic) and mudstone.|
23629|Goose Hole Group|73255|6|Mentioned|p533 Fig.1, p534 Fig.2|Cambrian|Cambrian|Contains Redlichia forresti, Gudugawan hardmanae and Xystridura negrina trilobite fossils.|||Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation, Eagle Hawk Sandstone, Overland Sandstone.|Overlies the Antrim Plateau Basalt, disconformably underlies the Mahony Group.|Includes carbonate rocks.|
39138|Gosse River East Syenite|23733|5|Briefly described|p32 Fig. 19|||||||||
39138|Gosse River East Syenite|23809|6|Mentioned|p27 Fig. 25|||Geological Province: Tennant Inlier.||||||16-NOV-04
39138|Gosse River East Syenite|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Devils Suite||||
39138|Gosse River East Syenite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Devils Suite.|||Syenite.|
39138|Gosse River East Syenite|67352|6|Mentioned|p8|||Included in Devils Suite (Wyborn 1997) by Donnellan (2004).||Devils Suite||||
39138|Gosse River East Syenite|69424|5|Briefly described|p9:28-29|Statherian|Statherian|Does not outcrop; intersected in drill core c.45 km E of Tennant Creek township.|1712 +/- 5 Ma (Compston, 1995).|Devils Suite.|||Probably quartz monzonite rather than syenite.|12-JUL-16
39138|Gosse River East Syenite|69425|6|Mentioned|p10:20-21|||Assigned to the Devils Suite by Wyborn et al. (1998). Davenport Province.||Devils Suite.||||12-JUL-16
39138|Gosse River East Syenite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1712+/-5 Ma (crystallisation: Pb/Pb zircon).||||Syenite.|
81660|Goyder package|72373|5|Briefly described|p1-2|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Informal nomenclature of Rawlings et al (1997) and Rawlings (1999). A basin-wide non-genetic depositional pacakge within the McArthur Basin.||||Overlain by Gyde package. Underlain by Redbank package.||
81660|Goyder package|72718|5|Briefly described|p5, p7|Statherian|Statherian|Southern McArthur Basin. Outcrop confined to the Walker, Batten and Urapunga fault zones.||||||
81660|Goyder package|72912|6|Mentioned|p5, 18.|Statherian|Statherian|Of Rawlings, 1999.|c. 1683-1670 Ma|||Overlies Redbank package and underlies Glyde package.||
38411|Grayling Member|23937|6|Mentioned|p78 App. 1|||Of the Baralandji Formation.  On HELEN SPRINGS  sheet.  See also p84 Appendix 1.||||||
38411|Grayling Member|24303|2|Defined|p29, p60 Appendix|Calymmian|Calymmian|Of the Baralanji Formation. Overlain by the Powell Formation; overlies the Sweetwater Member. Max. Thickness: 500m. Previously mapped as undifferentiated Tomkinson Creek beds. Correlative of Crawford Formation, and possibly of Mainoru Formation.||||||18-OCT-05
38411|Grayling Member|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Baralandji Formation.  Sandstone, sublithic to quartz arentie; laminated to thick bedded, fine- to medium-grained; micaceous, glauconitic; mudstone; quasi-planar and hummocky crossbedded; current lineated; ferruginous, recessive intervals....||||||18-OCT-05
38411|Grayling Member|69431|4|Described|p16:19-21|Mesoproterozoic|Mesoproterozoic|Tomkinson Province. 100-150m thick. Intertidal, locally hypersaline (base) to high-energy subtidal, shallow-marine (top) deposits.||Baralandji Formation.||Conformably overlies Sweetwater Member. Is overlain conformably by Powell Formation.|Red and green-grey laminated micaceous siltstone and mudstone, feldspar-bearing sublithic sandstone, quartz sandstone. Glauconite, and iron oxide pseudomorphs after glauconite or pyrite? Cross-stratification, tool marks and current lineation.|12-JUL-16
38411|Grayling Member|70968|2|Defined|v, p93, p95, p98-99, p101-105, p124|Calymmian|Calymmian|See also p126-129, p131, p143. Hussey and Crispe in Hussey et al. (2001). Named after Mount Grayling. The type section goes from 363000mE 7989900mN (base) to 364500mE 7988000mN in HELEN 100k sheet. Readily recognisable by its red-brown to red-purple, or cream to green-grey, well-laminated micaceous sandstone or siltstone. 100-500m thick. Shallow-marine shelf deposits, between fair-weather and storm wave bases. Lithology well described and illustrated. Detrital zircon diagram and discussion.|1650 Ma (maximum depositional age).|Baralandji Formation.||Conformably overlies Sweetwater Member. Is overlain conformably and transitionally by Powell Formation.|Interbedded laminated siltstone and claystone and thinly to thickly bedded, fine- to medium- (rarely coarse-)grained sandstone; characteristic red-brown colour. Contains detrital white mica and glauconite.|
38411|Grayling Member|71893|4|Described|iii, p2-p3, p6, p8, p56-p59|Ectasian|Statherian|Tomkinson Province. A reference section was sampled and occurs on the top of a low strike ridge about 6km northwest of Banka Banka Outstation in eastern MUCKATY. This unit also yielded an isolated younger age of 1490 Ma. Deposited below fair-weather base but above storm wave base. This unit is interpreted to range from Statherian to Ectasian on the basis of dating of the unconformably underlying Namerinni Group and a SHRIMP U-Pb date of 1295 +/- 14 Ma for an unnamed dyke which intrudes this unit. Sampling location, Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|1650 +/- 21 Ma (Max dep. U-Pb-Hf)|Baralandji Formation||Conformably overlies the Sweetwater Member. Conformably overlain by the Powell Formation.|Red-brown to red-purple or cream to green-grey, well laminated micaceous sandstone or siltstone deposited in a shallow-marine shelf environment.|
78825|Green Swamp Granite|64675|6|Mentioned|Fig.14|||||||||
73205|Grimwade Ridge Intrusives|62580|5|Briefly described|p31|||Of Inningarra Suite. Predominantly fine-grained equigranular biotite monzogranite with minor leucocratic micro-monzogranitic dykes. Interfingers with Tanami Group. Forms low-lying isolated hills and hummocks.||||||07-FEB-11
40137|Grimwade Suite|61246|6|Mentioned|p3, p22|||Includes The Granites Granite?||||||21-SEP-06
40137|Grimwade Suite|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Medium- to coarse-grained, sometimes porphyritic, tourmaline-muscovite-bearing biotite granite; medium-grained granodiorite; strongly foliated to foliated. Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
40137|Grimwade Suite|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier. Coarse and fine grained, porphyritic and non porphyritic biotite or hornblende bearing syenogranite to monzogranite.||||||07-NOV-08
40137|Grimwade Suite|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province. Granite, monzogranite, gneiss.||||||07-NOV-08
40137|Grimwade Suite|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Various unnamed granites, granodiorites.||||||07-NOV-08
40137|Grimwade Suite|63261|4|Described|p9 Fig. 5, p16|Paleoproterozoic|Paleoproterozoic|The Coomarie Supersuite of Dean (2001). Includes Slatey Creek, The Granites and Lewis Granites of Blake et al (1979), and parts of Browns Range and Frankenia granite complexes. Interpreted crystal'n ages between: 1821+/-4 and 1791+/-4Ma (Smith 2001).||||||26-NOV-15
40137|Grimwade Suite|64662|5|Briefly described|p30 Fig. 3|Statherian|Orosirian|Age: 1825-1790Ma. Geological Province: Tanami region. Also referred to as Grimwade suite granites - see p44.||||||07-FEB-11
40137|Grimwade Suite|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.|||||
40137|Grimwade Suite|64733|5|Briefly described|p170 Fig.2, p172 Fig.4, p175|Statherian|Orosirian|Low aeromagnetic response.|1820-1790 Ma.|||||20-APR-12
40137|Grimwade Suite|64734|5|Briefly described|p186 Fig.1|Statherian|Orosirian|1820-1790 Ma||||||14-SEP-09
40137|Grimwade Suite|65358|5|Briefly described|p6-7|Statherian|Orosirian|In Tanami Region. Dominated by metaluminous I-type biotite granodiorite and monzogranite. Intruded between 1825-1790 Ma.||||||
40137|Grimwade Suite|65359|5|Briefly described|p23, p26-28 Figs.26-28.|||Tanami Region. Felsic plutons with weak to no magnetic signature.||||||
40137|Grimwade Suite|66129|6|Mentioned|p213, p214 Fig.1|Statherian|Orosirian|1820-1790 Ma.||||||
40137|Grimwade Suite|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Granite, monzogranite; fine-, medium- and coarse-grained, K-feldspar megacrysts, metasedimentary xenoliths.|20-OCT-11
40137|Grimwade Suite|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Parts of this unit are mapped according to their lithologies and the strength of their magnetic responses.|||||Granites, granodiorites and granite gneiss.|
40137|Grimwade Suite|67824|6|Mentioned|p385 Fig.2|Statherian|Orosirian||~1820-1790 Ma|||||
40137|Grimwade Suite|67826|6|Mentioned|p401 Fig.2|Statherian|Orosirian||1820 - 1790 Ma|||||
40137|Grimwade Suite|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma|||||
40137|Grimwade Suite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Granites-Tanami Complex.|c.1820-1790 Ma (Huston et al., in press).||||Granite.|
40137|Grimwade Suite|69003|5|Briefly described|p5, p17 Fig.21|||Granites-Tanami Orogen.|1820-1790 Ma.|||||
40137|Grimwade Suite|69253|5|Briefly described|p747 Fig.1, p755-760, p763, p765 Fig.21|Statherian|Orosirian|Petrophysical properties detailed. See also p766.|c.1825-1790 Ma.|||||
40137|Grimwade Suite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Tanami Region.||||Intrudes Ware Group.||12-JUL-16
40137|Grimwade Suite|69426|4|Described|p11:4 Fig.11.3, 11:10-12, 14, 21, 24, 26|Statherian|Orosirian|Widely distributed. Also includes parts of the Browns Range, Frankenia and Coomarie Domes, and granites in the Apertowonga Range - MacFarlanes Peak and Officer Hill - Muriel Range areas. Weakly to non-magnetic. Geochemistry briefly described. Gold mineralisation at The Granites goldfield is coincident with the margin of a pluton of this Suite. One pluton intruding the Quorn Au deposit in The Granites goldfield is dated at 1815 +/- 4 Ma (Smith, 2001).|1821-1791 Ma.||Slatey Creek, The Granites, Lewis, Coomarie, Browns Range and Frankenia Granites.|Intrudes Mount Charles Formation.|Monzogranite, syenogranite.|12-JUL-16
40137|Grimwade Suite|69427|5|Briefly described|p12:3, 20, 22|Statherian|Orosirian|Vandenberg et al. (in prep.). Aileron Province. Poor, scattered outcrops extending NW into the Tanami Region. Derived from partial melting of late Archean gneiss, with minor assimilation of Paleoproterozoic sedimentary rocks.|c.1805-c.1785 Ma.||||Granites, most commonly porphyritic, with compositions ranging from monzogranite to syenogranite; coarse- to fine-grained, porphyritic to non-porphyritic.|12-JUL-16
40137|Grimwade Suite|69432|6|Mentioned|p17:2|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
40137|Grimwade Suite|69440|5|Briefly described|p25:2|||||||Is overlain unconformably by Munyu Sandstone.|Granites.|12-JUL-16
40137|Grimwade Suite|69618|6|Mentioned|p90|Paleoproterozoic|Paleoproterozoic||c.1825-1790 Ma.|||||
40137|Grimwade Suite|69673|6|Mentioned|p3|||||||||
40137|Grimwade Suite|69747|5|Briefly described|p263-p264|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Associated with late syn- to postcollisional tectonic settings within a ~30 Ma million year long period of magmatic activity broadly spanning ca. 1825-1791 Ma (Smith, 2001). Granitic plutons derived from a crustal source in response to continental thickening after collision between the Granites-Tanami Orogen and the Arunta Orogen around 1795 Ma.|ca. 1825-1790 Ma|||||25-JUN-19
40137|Grimwade Suite|70291|4|Described|p178,180-181,191|Sthatherian|Orosirian|Geological province: Tanami. Occurred after deposition of Mount Charles Formation (post D3 event).|1820-1790 Ma||||Non-magnetic, peraluminous biotite monzogranite to syenogranite with hornblende in SiO2-poorer samples.|
40137|Grimwade Suite|70478|4|Described|p2 Fig 1, 8-9, 11-13, p39 App 3|Orosirian|Orosirian|Geological Province: Tanami. Granites drilled in drillholes TAN99DDH7, TAN99DDH15, TAN99DDH21, TAN99DDH23, TAN99DDH28 assigned to Grimwade Suite. See associated drilling summaries and appendices for more detail. SHRIMP U-Pb magmatic zircon ages of 1805+\-6 Ma (DDH7 monzogranite; Smith 2001); 1812+\-5 Ma (DDH15 monzogranite; Claoue-Long et al., 2001); 1809+\-3 Ma (DDH21 granodiorite; Cross et al., 2005); 1808+\-3 Ma (DDH23 monzogranite; Cross et al., 2005); 1844+\-4 Ma (DDH28 monzogranite; Claoue-Long et al., 2001).||||Intrudes Mount Charles Formation, Dead Bullock Formation.|monzogranite, syenogranite|11-OCT-19
40137|Grimwade Suite|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1821-1791 Ma.||||Coarse- and fine-grained, porphyritic and non-porphyritic biotite- or hornblende-bearing monzogranite, syenogranite.|
40137|Grimwade Suite|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1821-1791 Ma.||||Biotite +/- hornblende syenogranite to monzogranite: coarse- and fine-grained, equigranular to porphyritic.|
40137|Grimwade Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||monzogranite, granite|
40137|Grimwade Suite|71348|6|Mentioned|p201|Orosirian|Orosirian|Geological province: Aileron Province, Arunta Region.||||||
40137|Grimwade Suite|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1790 Ma.|||Intrudes Tanami and Ware Groups.||
40137|Grimwade Suite|73089|5|Briefly described|p3, p8, p39|Statherian|Orosirian|Granites-Tanami Orogen and northwestern Aileron Province. Broadly coeval with other granites of the orogen but distinguished by differences in magnetic character (Ahmad et al., 2013). A date of 1785 +/- 4 Ma for a granite in the Aileron Province might represent a younger component.|1821-1791 Ma||Lewis Granite|||
40137|Grimwade Suite|73158|5|Briefly described|p2|Statherian|Orosirian|Granites-Tanami Orogen.|1821-1791 Ma||||Granitic intrusions.|
40137|Grimwade Suite|73159|5|Briefly described|p2|||Granites-Tanami Orogen.|1821-1791 Ma.||||Granites.|
33979|Groote Eylandt Group|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
33979|Groote Eylandt Group|22538|3|Fully described|p711, Fig4, p713||Statherian|||||||28-MAR-18
33979|Groote Eylandt Group|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
33979|Groote Eylandt Group|22808|1|Redefined|29|Paleoproterozoic|Paleoproterozoic|Geol province McArthur Basin. Underlying unit Grindall Formation||||||07-NOV-08
33979|Groote Eylandt Group|23374|5|Briefly described|Fig3p5,6,34||Paleoproterozoic|Of McArthur Basin.||||||07-NOV-08
33979|Groote Eylandt Group|23937|6|Mentioned|p53|||||||||
33979|Groote Eylandt Group|24048|3|Fully described|p15|Statherian|Orosirian|Formerly "Groote Eylandt beds".  Includes Bustard and Alyangula Subgroups.  Max. Thickness: 1650m.  Geological Province: McArthur Basin||||||
33979|Groote Eylandt Group|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes Alyangula Subgroup and Bustard Subgroup. Geol. Prov: McArthur Basin.||||||13-OCT-05
33979|Groote Eylandt Group|44112|6|Mentioned|p10,43,93||Statherian|Part of Supersequence 1||||||
33979|Groote Eylandt Group|60573|5|Briefly described|Map legend|Orosirian|Orosirian|Includes the Dalumbu Sandstone.  Do not outcrop in the Roper River mapsheet area.||||||14-FEB-05
33979|Groote Eylandt Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
33979|Groote Eylandt Group|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes Alyangula Subgroup and Bustard Subgroup. Geol. Prov: McArthur Basin.||||||
33979|Groote Eylandt Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Orosirian|McArthur Basin unit deposited during the Post-Barramundi Extension (1830-1810 Ma). Upper part deposited during the Leichhardt Extension (1800-1750 Ma)||||||
33979|Groote Eylandt Group|64817|6|Mentioned|p352-355|||Caledon Shelf South, McArthur Basin.|||Includes Alyangula and Bustard Subgroups.|||
33979|Groote Eylandt Group|65340|6|Mentioned|p9.|||Caledon Shelf, McArthur Basin. Undeformed and flat-lying.|1814 +/- 8 Ma (Pietsch et al. 1997).|||||
33979|Groote Eylandt Group|67779|6|Mentioned|p32.|||Eastern Arnhem Land. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Spencer Creek Group, Gadabara Volcanics, Donji Group and Tawallah Group.||||||
33979|Groote Eylandt Group|69417|5|Briefly described|p2:5|Orosirian|Orosirian|McArthur Basin.||||Is intruded by Giddy Suite.||12-JUL-16
33979|Groote Eylandt Group|69430|4|Described|p15:2-6, 14|||Previously the Groote Eylandt beds. Included outcrops since recognised (Haines et al., 1999) as a separate, ungrouped unit: the Coast Range Sandstone. NE McArthur Basin. Flat-lying to gently dipping outcrops. Thickness varies widely, from tens of metres to over 1km.|||Bustard, Alyangula Subgroups.||Sandstone and conglomerate interbedded with felsic and mafic volcanic rocks.|12-JUL-16
33979|Groote Eylandt Group|69673|6|Mentioned|p3 fig 2, p15, p17|Orosirian|Orosirian|Northeastern McArthur Basin.|||Includes Alyangula Subgroup, Bustard Subgroup|Correlated with Tomkinson Creek Group, Hatches Creek Group||
33979|Groote Eylandt Group|70302|5|Briefly described|iv, p5|Statherian|Statherian|McArthur Basin.|||Alyangula Subgroup.|||
33979|Groote Eylandt Group|71374|6|Mentioned|p2, p24|||northern McArthur Basin.|||Includes the Alyangula Subgroup.|Unconformably overlain by the Coast Range Sandstone. Broadly equivalent to the Tawalah Group.||
33979|Groote Eylandt Group|71606|5|Briefly described|p135,137|Statherian|Orosirian|South Caledon Shelf, McArthur Basin. U-Pb zircon age ~1810 Ma. Part of the ~1840-~100 Ma transition Phase of Rawlings 1994.|||Includes Alyangula and Bustard subgroups.|Correlable to lower Tawallah Group.|Rhyolite and associated siliciclastic rocks overlain disconformably by quartzarenite and basalt.|
33979|Groote Eylandt Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Bustard Subgroup, Alyangula Subgroup.|||04-MAR-20
33979|Groote Eylandt 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).||||||
33979|Groote Eylandt Group|72377|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Alyangula Subgroup.|Overlain unconformably by Coast Range Sandstone.||
81232|Groundrush dolerite|69747|4|Described|p262,267-272,274|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Intrudes Dead Bullock Formation. Undergone greenschist to amphibolite-facies metamorphism due to subduction of Tanami back-arc oceanic slab. Back-arc basaltic rock affinities; petrologically and geochemically similar to mafic rocks in the former Stubbins Formation. Geochemically similar to the Coora Dolerite.|ca. 1864 Ma||||Medium-grained; chlorite alteration. Subhedral plagioclase and anhedral hornblende laths. Mineral assemblage of plagioclase, hornblende, chlorite, diopside.|25-JUN-19
33374|Gumarrirnbang Sandstone|23374|2|Defined|Tb2p10,14,15,42,12,8,9,11,16,24,32||Statherian|Gilruth Volcanic Member at the top. No type section possible, but lower and upper boundary stratotypes given. Probably correlates with lower Sly Creek Sandstone of Tawallah Group. of Kombolgie Subgroup, McArthur Basin.||||||
33374|Gumarrirnbang Sandstone|23384|5|Briefly described|Fig 27|||||||||
33374|Gumarrirnbang Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Kombolgie Subgroup (Katherine River Group).||||||
33374|Gumarrirnbang Sandstone|23867|3|Fully described|p5|Paleoproterozoic|Paleoproterozoic|Of Kombolgie Subgroup.  Medium to coarse quartz sandstone, some scattered pebbles.  Max. thickness: 260m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
33374|Gumarrirnbang Sandstone|24050|3|Fully described|p13, p10|||Of the Kombolgie Subgroup.  Fine- very coarse-grained and granular quartz sandstone.; scattered pebbles.||||||21-SEP-06
33374|Gumarrirnbang Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Kombolgie Subgroup, Katherine River Group. Geological Province: McArthur Basin.||||||
33374|Gumarrirnbang Sandstone|50545|5|Briefly described|p114 Fig.1||Paleoproterozoic|Of Kombolgie Subgroup.||||||07-NOV-08
33374|Gumarrirnbang Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Sandstone: white/grey, fine- to very coarse-grained, medium- to thick-bedded, dominantly planar laminated, trough cross-bedded, quartz arenite. Geological Province: McArthur Basin.||||||30-NOV-04
33374|Gumarrirnbang Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Includes Gilruth Volcanic Member.  Medium to very coarse pebbly quartz sandstone.  Geol.Prov: McArthur Basin. Overlies: Nungbalgarri Volcanics. Underlies: Marlgowa Sandstone.||||||14-JAN-05
33374|Gumarrirnbang Sandstone|61560|5|Briefly described|p489|Paleoproterozoic|Paleoproterozoic|Of the Kombolgie Subgroup. Contains the Liverpool impact crater situated on the boundary between the McArthur Basin and overlying Arafura Basin near the northern coast of NT. ||||||07-NOV-08
33374|Gumarrirnbang Sandstone|61561|5|Briefly described|p531|Paleoproterozoic|Paleoproterozoic|Formerly the Komolgie Formation. Bedrock associated with the Liverpool impact crater. medium-bedded, generally medium-grained, quartzose sandstone - abruptly upturned and brecciated at the margin of the impact crater.  Intruded by the Oenpelli Dolerite.||||||07-NOV-08
33374|Gumarrirnbang Sandstone|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1750-1800Ma. McArthur Basin. Of Katherine River Group. Max thick 280m. White, trough cross-bedded, med/very coarse pebbly qtz sandst; thin to med-bedded wave-rippled med/coarse qtz sandst; minor pebble conglom and very coarse lithic sandst at base.||||||07-JAN-09
33374|Gumarrirnbang Sandstone|65232|5|Briefly described|p65, p69, App. 2|||Of Kombolgie Subgroup (Katherine River Group). In contact with Gilruth Volcanics - unit relationship is unclear in paper. See also misspelt Gumarrinbang Sandstone.Thickness 220-280m from p7.||||||09-FEB-10
33374|Gumarrirnbang Sandstone|67057|6|Mentioned|p455.|||||Unit in Kombolgie Subgroup.||Overlies Nungbalgarri Volcanics. Is overlain by Gilruth Volcanics.||
33374|Gumarrirnbang Sandstone|67564|3|Fully described|p2, p9 Fig.4, p17 Table 3, p39, p41.|Proterozoic|Proterozoic|Of Carson et al. (1999). 280 m of mainly braided fluviatile sediments with minor marine intervals near the base. Component of Arnhem Land Plateau.|1820 Ma (maximum depositional age).|Unit in Kombolgie Subgroup.|Includes Gilruth Volcanic Member.|Unconformably overlies Nungbalgarri Volcanics.|Resistant, white, medium to very coarse pebbly quartz sandstone; minor pebble conglomerate and lithic sandstone at base.|
33374|Gumarrirnbang Sandstone|67779|3|Fully described|p6 Fig.5, p8 Table 1, pp36-38.|Paleoproterozoic|Paleoproterozoic|Previously referred to as the upper part of the former Kombolgie Formation, first defined by Carson et al. (1999) as a distinct unit within Kombolgie Subgroup. McArthur Basin. 150 m thick. Distal braided fluvial with minor marine intervals; aeolian environment (dunes) at top of sequence. Correlated with lower units of Sly Creek Sandstone (Tawallah Group), constraining its maximum age of deposition.|1787 +/- 17 Ma (Hollis et al. 2010a).|Unit in Kombolgie Subgroup.|Includes Gilruth Volcanic Member.|Overlies Nungbalgarri Volcanics unconformably. Is overlain by Marlgowa Sandstone.|Pebbly quartz sandstone: white-grey, fine-grained to very coarse-grained, medium- to thickly-bedded, dominantly planar laminated, trough cross-bedded.|14-MAY-18
33374|Gumarrirnbang Sandstone|69420|6|Mentioned|p5:67, 79, 84|Paleoproterozoic|Paleoproterozoic|Mis-spelt as Gumarrinbang at 5:67, 79.||Katherine River Group.||||12-JUL-16
33374|Gumarrirnbang Sandstone|69430|4|Described|p15:3, 7-8, 51-52|||NW McArthur Basin. 125m thick. Fluvial, braided river deposits; source area to the S. Hosts U mineralisation near the contact with Gilruth Volcanics.||Kombolgie Subgroup.|Gilruth, Henwood Creek, Volcanic Members.|Conformably overlies Nungbalgarri Volcanics. Is overlain by Marlgowa Sandstone probably conformably.|Pink-grey to white, fine- to medium-grained, medium to thickly bedded quartz sandstone; dominantly planar-laminated and trough cross-bedded.|12-JUL-16
33374|Gumarrirnbang Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Gilruth Volcanic Member, Henwood Creek Volcanic Member, overlies Nungbalgarri Volcanics||
33374|Gumarrirnbang Sandstone|70853|5|Briefly described|Map legend.|Statherian|Statherian|||Kombolgie Subgroup.|||Quartz sandstone: white-grey, fine- to very coarse-grained, medium- to thickly-bedded, dominantly planar laminated, trough cross-bedded.|
33374|Gumarrirnbang Sandstone|73083|6|Mentioned|p29|||||||Underlain by Birdie Creek Volcanic Member.|Sandstone.|
79168|Gumtree Suite|68150|6|Mentioned|p1|Paleoproterozoic|Paleoproterozoic|Presented in text as the Napperby, Wuluma and Gumtree suites, and age of the Wuluma suite given as 1726+/-4 Ma. Aileron Province.||||||28-AUG-15
79168|Gumtree Suite|69931|6|Mentioned|p269, 282-283|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Presented as Gum Tree Suite on p282.|||Gumtree Granite.|||
40575|Gun Supersequence|62535|5|Briefly described|p663, p672-674|||Isa Superbasin. Closely comparable to age of middle Paragon Group. Deposition followed a 15-20 m.y. hiatus.|c.1670 Ma - c.1650 Ma.|||Unconformably overlies Prize Supersequence.|Thick suite of stromatolitic carbonates (Lawn Hill Platform), and rhythmically laminated siliciclastic rocks (Leichhardt River Fault Trough).|
40575|Gun Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Masterton Sandstone and lower parts of Mallapunyah Formation.|||
40575|Gun Supersequence|63114|5|Briefly described|p1253 Fig.2, p1270,|||Isa superbasin.|||Includes the Esperanza, Paradise Creek, Gunpowder Creek Formations; Torpedo and Warrina Park Quartzites; Native Bee, Moondarra Siltstones; Breakaway, Urquhart Shales.|||
40575|Gun Supersequence|63866|4|Described|p53-p54, p57-p59, p61|Statherian||Isa Superbasin. Also includes the Native Bee Siltstone, Urquhart Shale, Spear Siltstone, Kennedy Siltstone and the Magazine Shale. Correlated with a unit of thick polymictic conglomerate in the Deighton Quartzite.|c. >1660 Ma||Includes the Masterton, Mallapunyah, Gunpowder Creek, Paradise Creek Formations, Moondarra Siltstone, Esperanaza Formation and the Paradise Creek Formation.|Conformably overlain by the Loretta Supersequence.||
40575|Gun Supersequence|65228|5|Briefly described|p16, pp23-26, Figs.11-14.|||First defined by Southgate et al (1999). Named after the Gunpowder Creek Formation which contains the maximum flooding surface. Constitutes basal McNamara Group in southern Lawn Hill Platform. Gamma ray log, lithology and facies detailed.||||||
40575|Gun Supersequence|65337|6|Mentioned|p32.|||This study includes all of the Drummond Formation as equivalents to this Supersequence.||||Overlies Prize Supersequence. Is overlain by Loretta Supersequence.||
40575|Gun Supersequence|65387|6|Mentioned|p1|||Western Fold Belt, Mt Isa Inlier. Possibly correlated with a psammite host of the Dugald River Pb-Zn deposit, aged 1686 +/- 7 Ma (detrital zircons).||||||
40575|Gun Supersequence|65396|6|Mentioned|p197|||Comprises most of the Mount Isa Group and western equivalents.||||||
40575|Gun Supersequence|66844|4|Described|p243-245,254, 265, 267, 270|||Lawn Hill Platform. Regionally extensive, southeast-facing, storm-dominated mixed carbonate/siliciclastic ramp. Separated from the underlying Prize SS by a regionally correlative unconformity in the lower to middle Gunpowder Creek Formation.||Equivalent to parts of lower McNamara Group.|Subdivided into Gun 1 and Gun 2 third-order depositional sequences, p254, 255-263.|Overlain by Loretta Supersequence (p255). Underlain unconformably by Prize Supersequence, and locally by Myally Sub Group||
40575|Gun Supersequence|67323|4|Described|GIS attrib tbl, p15, p39|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Isa Superbasin.|~1665-1655 Ma.|Mount Isa Group. ?McNamara Group||Overlies Prize Supersequence. Is overlain by Loretta Supersequence. Correlated with upper part of Deighton Quartzite.|Green and red siltstone, shale, micaceous siltstone, sandstone, laminated and stromatolitic dolomite, dolomitic siltstone, grey to white stromolitic chert, chert, and tuff|
40575|Gun Supersequence|68021|5|Briefly described|p135 Fig 4, p136|Statherian|Statherian|Equivalent to McNamara Group, Mount Isa Group, Marimo Slate in part, Soldiers Cap Group in part. Transgressive fluviatile to shallow-marine.|~1670- ~1650 Ma|||Unconformably overlies Calvert Superbasin rocks.|Sandstones, siltstones, dolostones.|03-APR-17
40575|Gun Supersequence|68146|5|Briefly described|p3, p199-200|||The base is the c.1690-1670 Ma Gun unconformity.|||Upper part of Torpedo Creek and Warrina Park Quartzites.|Unconformably overlies Prize Supersequence.||
40575|Gun Supersequence|68732|5|Briefly described|p159, p161, p162, p165 Fig.3, p167-171|Statherian|Statherian|Includes Paradise Creek Formation, Urquhart Shale, Breakaway Shale, Moondarra Siltstone, and Warrina Park Quartzite. Maximum depositional age.|ca. 1674; ca. 1688 Ma.||||Includes stromatolitic bioherms and biostromes.|30-NOV-17
40575|Gun Supersequence|69056|6|Mentioned|p55|||||Mount Isa Group.||Possibly correlated with Lady Clayre Formation.||
40575|Gun Supersequence|69591|5|Briefly described|p27, p39, p42-43, p54|||Mount Isa Province. Includes topmost unit of Deighton Quartzite. Marks the onset of deposition (lower McNamara Group) of the Isa Superbasin.||||Unconformably overlies Yeldham Granite. Is overlain by Loretta Supersequence.||
40575|Gun Supersequence|70657|6|Mentioned|p17|||||||||
40575|Gun Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1675 Ma|||Overlain by the Loretta Supersequence.|Siltstone, carbonaceous shale and dolomite.|
40575|Gun Supersequence|72912|5|Briefly described|p33 Fig.12, p34.|Paleoproterozic|Paleoproterozic|Appear to be affected by oil staining and hence warrant further investigation into their oil or condensate potential.|||Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation and Fish River.|Underlies Loretta Supersequence.||
40575|Gun Supersequence|73144|4|Described|p8-11, p19|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains two third order sequences [see article for more detail on third order sequences]. Deposited below storm wavebase depth in a marine environment (Southgate et al., 2000). Transitions from fluvial and coastal facies in the north and west to progressively peritidal, inner to outer ramp carbonate facies and deeper water, fine-grained siliciclastics and carbonates in the south and east (Southgate et al., 1999). Not considered to contain potential shale gas source rocks (Gorton and Troup, 2018).|1655-1690 Ma|||Includes Esperanza Formation, Paradise Creek Formation, Gunpowder Creek Formation, and Torpedo Creek Formation.|Siltstone, sandstone and dolomudstone.|
42371|Gunbarrel Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Illili Suite. Foliated porphyritic biotite granite with rounded K-feldspar phenocrysts; common rapakivi textures, locally migmatic. In the Arunta region.||||||07-NOV-08
42371|Gunbarrel Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Illili Suite. Foliated porphyritic biotite granite with rounded K feldspar phenocrysts. Geological Province: Warumpi Province||||||07-NOV-08
42371|Gunbarrel Granite|67565|6|Mentioned|p60, p62.|Statherian|Statherian|||Unit in Illili Suite.||Intrudes Russell Charnockite.||
42371|Gunbarrel Granite|69428|5|Briefly described|p13:11|Paleoproterozoic|Paleoproterozoic|Yaya Domain, Warumpi Province.||Illili Suite.|||Coarse, rounded K-feldspar phenocrysts with locally well-developed rapakivi textures.|12-JUL-16
42371|Gunbarrel Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.||Unit of Illili Suite.|||Foliated porphyritic biotite granite with rounded K-feldspar phenocrysts; common rapakivi textures, locally migmatitic.|09-SEP-19
27994|Gundi Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
27994|Gundi Sandstone|22748|6|Mentioned|p235 Fig.1|||||||||
27994|Gundi Sandstone|23216|4|Described|Table1p9,Fig5p20,24-5|||Previously: Gundi Creek Greywacke Member (Ruker, 1959); Gundi Greywacke Member (Randal, 1963); Gundi Greywacke (Walpole et al., 1968).||||||
27994|Gundi Sandstone|23374|3|Fully described|Tb2p10,17,18||Statherian|Unconformable on McCaw Formation, unconformable below Mount Rigg Group. of Katherine River Group, McArthur Basin.||||||
27994|Gundi Sandstone|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||21-SEP-06
27994|Gundi Sandstone|23867|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Formerly Gundi Greywacke Member of Diljin Hill Formation.  Max. thickness: >100m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. 3 and 30.||||||07-NOV-08
27994|Gundi Sandstone|23937|4|Described|p8, p25 Tb. 2|Statherian|Statherian|Of the Katherine River Group.  Supersedes Gundi Greywacke of Dunn (1963b,c).  Max. thickness: >100m.  Geological Province: McArthur Basin.||||||
27994|Gundi Sandstone|24050|3|Fully described|p23, p9 Tb. 2|Paleoproterozoic|Paleoproterozoic|Formerly Gundi Greywacke. Of the Katherine River Group. Overlies the McCaw Formation; underlies West Branch Volcanics conformably, and Bone Creek Sandstone unconformably.  Max. thickness: 250m..||||||07-NOV-08
27994|Gundi Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
27994|Gundi Sandstone|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
27994|Gundi Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Sandstone; localised conglomerate; minor mudstone; ferruginous mafic igneous rocks and porphyritic rhyolite. Geological Province: McArthur Basin.||||||30-NOV-04
27994|Gundi Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group.  Very well sorted quartz sandstone and poorly sorted, coarse to very coarse quartz sandstone. Geol.Prov: McArthur Basin. Overlies: McCaw Formation. Underlies: Bone Creek Sandstone.||||||07-JAN-09
27994|Gundi Sandstone|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the Katherine River Group. Quartz sandstone: pink to fawn, locally lithofeldspathic, medium to coarse grained, planar bedding and cross bedding.||||||
27994|Gundi Sandstone|61572|5|Briefly described|p667|||Of Katherine River Group. Red-pink sandstone; minor conglomerate, mudstone, volcanic rocks. Uncon. overlain by Bone Creek Sandstone; overlies McCaw Formation. Max. thick: 250m. Geol. Prov: McArthur Basin.||||||
27994|Gundi Sandstone|63866|5|Briefly described|p112|||Interpreted to have been deposited synchronously with the intrusion of the Jimbu Microgranite.||||||
27994|Gundi Sandstone|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1710-1720Ma. McArthur Basin. Of Katherine River Group. Max thick 100m. Reddish, med-bedded, very well sorted med qtz sandst and white to pink, very thickly bedded, poorly sorted, coarse/very coarse qtz sandst with minor dispersed granules and pebbles||||||
27994|Gundi Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2|||See also p369, p370. Arnhem Shelf, McArthur Basin. Records local pluton emplacement.||Of the Katherine River Group.||Shown as underlying Diamond Creek Volcanics in Fig 5 and overlying Diamond Creek Volcanics disconformably in Fig 4.|Sandstone and conglomerate.|05-JUN-18
27994|Gundi Sandstone|65232|5|Briefly described|p7 Fig. 6|||Of Katherine River Group. Underlies West Branch Volcanics; overlies McCaw Formation. 150-250m thick. Shallow-marine to aeolian sandstone, minor volcanic rocks.||||||09-FEB-10
27994|Gundi Sandstone|67564|3|Fully described|p6 Table 2, p10 Fig.5, pp49-50.|Paleoproterozoic|Paleoproterozoic|Formerly Gundi Greywacke Member of now-defunct Diljin Hill Formation (Walpole 1963) and Gundi Greywacke (in Roberts and Plumb 1965). Over 100 m of fluviatile and shallow marine sediments. Strongly jointed, red-weathering sandstone outcrops.|1730 - 1710 Ma.|Unit in Katherine River Group.||Overlies ?unconformably the McCaw Formation. Is overlain by West Branch Volcanics and disconformably by Bone Creek Sandstone.|Reddish, medium-bedded, very well-sorted quartz sandstone; white to pink, very thickly-bedded, poorly sorted quartz sandstone.|
27994|Gundi Sandstone|69430|4|Described|p15:3, 8-9, 30|||See Abbott et al. (2001). Formerly Gundi Greywacke (Dunn, 1963). NW McArthur Basin. 300m thick. Shallow-marine, aeolian dune, fluvial deposits and probable subaerial volcanic activity. Was intruded by the 1720 Ma Jimbu Microgranite concurrently with deposition.||Katherine River Group.||Unconformably overlies Diamond Creek Volcanics. Is overlain conformably or locally disconformably by West Branch Volcanics.|Medium- to coarse-grained, medium to thickly bedded, pink lithic and feldspathic sandstone with mud matrix, local pebble to boulder conglomerate; minor mudstone; ferruginous maroon to red-brown mafic igneous rocks and porphyritic rhyolite.|12-JUL-16
27994|Gundi Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by West Branch Volcanics, Overlies Diamond Creek Volcanics, McCaw Formation||
25038|Gunpowder Creek Formation|22438|4|Described|p539, Fig.3 p537|||Subdivided in Fig.3 into an upper and lower formation. See also Fig.10a p546||||||
25038|Gunpowder Creek Formation|22585|6|Mentioned|Fig3 P738|||Actually spelt Gunpowder Creek Fm.||||||
25038|Gunpowder Creek Formation|22680|6|Mentioned|83,85,87|||Geol province Mount Isa Basin. Parent McNamara Group||||||
25038|Gunpowder Creek Formation|22747|6|Mentioned|Table1,p7|||With Paradise Creek Formation correlates with Suprise Creek Beds and Ploughed Mountain Beds||||||
25038|Gunpowder Creek Formation|23031|5|Briefly described|53|||Geol province Lawn Hill Subprovince. Parent McNamara Group. Overlying unit Paradise Creek Formation, underlying unit Torpedo Creek Quartzite||||||13-AUG-13
25038|Gunpowder Creek Formation|23073|5|Briefly described|p744 (fig 2)|||||||||
25038|Gunpowder Creek Formation|23198|6|Mentioned|p873-876|||||||||
25038|Gunpowder Creek Formation|23362|5|Briefly described|339|||||||||
25038|Gunpowder Creek Formation|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
25038|Gunpowder Creek Formation|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group. Overlies Torpedo Creek Quartzite.||||||13-AUG-13
25038|Gunpowder Creek Formation|23396|4|Described|p419|Statherian|Statherian|Of McNamara Group. 1694+/-3Ma.||||||13-AUG-13
25038|Gunpowder Creek Formation|23397|5|Briefly described|p469|||||||||
25038|Gunpowder Creek Formation|23398|4|Described|p447|Statherian|Statherian|Of McNamara Group. 1694+/-3Ma.||||||
25038|Gunpowder Creek Formation|23399|5|Briefly described|p493 Fig.3|||Of McNamara Group.||||||27-MAY-08
25038|Gunpowder Creek Formation|23406|5|Briefly described|p603, p607 Fig. 8, p611|||Geological province: Lawn Hill Platform. Also referred to as Gunpowder Formation.||||||16-JUN-09
25038|Gunpowder Creek Formation|23408|4|Described|p513 Fig. 2, p514|||Of McNamara Group.||||||15-JUN-09
25038|Gunpowder Creek Formation|23409|5|Briefly described|p535 Fig.2|||Of McNamara Group.||||||01-OCT-08
25038|Gunpowder Creek Formation|23466|5|Briefly described|p267|Statherian|Statherian|1694+/-7Ma||||||
25038|Gunpowder Creek Formation|23518|4|Described|p12|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Western Fold Belt.||||||
25038|Gunpowder Creek Formation|23767|5|Briefly described|p1955|||See also p1957.||||||
25038|Gunpowder Creek Formation|23958|5|Briefly described|p1134 Fig.2|Mesoproterozoic|Paleoproterozoic|Of McNamara Group.||||||07-NOV-08
25038|Gunpowder Creek Formation|23964|5|Briefly described|p1265|Proterozoic|Proterozoic|Of McNamara Group.  Geological Province: Mount Isa Inlier.  Maximum thicknees: 800m.||||||
25038|Gunpowder Creek Formation|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
25038|Gunpowder Creek Formation|24033|5|Briefly described|p5|||Includes orthoquartzite, conglomerate, micaceous siltstone and ferruginous siltstone.||||||
25038|Gunpowder Creek Formation|24034|6|Mentioned|p38|||Geological Province: Mount Isa Inlier. Fe-rich litology.||||||
25038|Gunpowder Creek Formation|24156|5|Briefly described|p18|Proterozoic|Proterozoic|Has limited stratabound Zn-Pb-Ag mineralisation at Cowie.|||||Iron-rich sediments.|
25038|Gunpowder Creek Formation|24308|5|Briefly described|p992, p987 Fig. 2|Paleoproterozoic|Paleoproterozoic|Parent: McNamara Group||||||07-NOV-08
25038|Gunpowder Creek Formation|24419|5|Briefly described|p17|Paleoproterozoic|Paleoproterozoic|Of the McNamara Group.  Conformably overlies and interfingers with Torpedo Creek Formation.||||||07-NOV-08
25038|Gunpowder Creek Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Age: 1694 Ma.||||||
25038|Gunpowder Creek Formation|29969|5|Briefly described|p392|||||||||
25038|Gunpowder Creek Formation|30535|6|Mentioned|p404|||Refer de Keyser(1958)||||||
25038|Gunpowder Creek Formation|30914|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|31207|6|Mentioned|p1414|||||||||
25038|Gunpowder Creek Formation|31342|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|31704|6|Mentioned|p4|||Favourable horizon for copper||||||
25038|Gunpowder Creek Formation|31821|5|Briefly described|p1024|||||||||
25038|Gunpowder Creek Formation|31877|5|Briefly described|p378|||||||||
25038|Gunpowder Creek Formation|32264|4|Described|p386|||See Table 1||||||
25038|Gunpowder Creek Formation|32287|4|Described|p19|||See also p17.||||||13-APR-18
25038|Gunpowder Creek Formation|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|32660|5|Briefly described|Table 5|||||||||
25038|Gunpowder Creek Formation|32959|6|Mentioned|Fig.21|||||||||
25038|Gunpowder Creek Formation|33899|6|Mentioned|p22|||||||||
25038|Gunpowder Creek Formation|33900|6|Mentioned|p15|||||||||
25038|Gunpowder Creek Formation|34395|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|35001|6|Mentioned|Fig.45|||||||||
25038|Gunpowder Creek Formation|35004|6|Mentioned|p266|||||||||
25038|Gunpowder Creek Formation|35074|6|Mentioned|Fig.2|||||||||
25038|Gunpowder Creek Formation|35115|6|Mentioned|p207|||||||||
25038|Gunpowder Creek Formation|35116|6|Mentioned|p186|||||||||
25038|Gunpowder Creek Formation|35167|6|Mentioned|p151|||||||||
25038|Gunpowder Creek Formation|35932|6|Mentioned|p462|||||||||
25038|Gunpowder Creek Formation|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|36548|6|Mentioned|p517|||||||||
25038|Gunpowder Creek Formation|37217|6|Mentioned|p650|||||||||
25038|Gunpowder Creek Formation|37459|1|Redefined|p428|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||01-OCT-08
25038|Gunpowder Creek Formation|37555|6|Mentioned|p3|||||||||
25038|Gunpowder Creek Formation|37568|5|Briefly described|p84|||||||||
25038|Gunpowder Creek Formation|37569|5|Briefly described|p91|||||||||
25038|Gunpowder Creek Formation|37816|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|38232|6|Mentioned|p89|||||||||
25038|Gunpowder Creek Formation|38233|5|Briefly described|Table 1|||||||||
25038|Gunpowder Creek Formation|38237|4|Described|p127|||||||||
25038|Gunpowder Creek Formation|38276|6|Mentioned|Fig.1|||||||||
25038|Gunpowder Creek Formation|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|38348|4|Described|p8|||||||||
25038|Gunpowder Creek Formation|38350|4|Described|p15|||||||||
25038|Gunpowder Creek Formation|38446|5|Briefly described|p187|||||||||
25038|Gunpowder Creek Formation|38584|6|Mentioned|p22|||||||||
25038|Gunpowder Creek Formation|38608|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25038|Gunpowder Creek Formation|38919|6|Mentioned|p496|||||||||
25038|Gunpowder Creek Formation|39445|5|Briefly described|Table 2|||See also p41.||||||13-APR-18
25038|Gunpowder Creek Formation|39497|6|Mentioned|Fig.4|||||||||
25038|Gunpowder Creek Formation|39556|5|Briefly described|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Overlies Torpedo Creek Quartzite; underlies Paradise Creek Formation.||||||15-JUN-06
25038|Gunpowder Creek Formation|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|39925|6|Mentioned|Fig.9|||||||||
25038|Gunpowder Creek Formation|39943|6|Mentioned|Table 1A|||||||||
25038|Gunpowder Creek Formation|39944|3|Fully described|p233|||||||||
25038|Gunpowder Creek Formation|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25038|Gunpowder Creek Formation|40221|3|Fully described|p14|||||||||
25038|Gunpowder Creek Formation|40394|6|Mentioned|p285|||||||||
25038|Gunpowder Creek Formation|41298|6|Mentioned|Map legend|Carpentarian||||||||
25038|Gunpowder Creek Formation|41307|4|Described|p16|||||||||
25038|Gunpowder Creek Formation|41489|6|Mentioned|p516|||||||||
25038|Gunpowder Creek Formation|42166|6|Mentioned|p108|||||||||
25038|Gunpowder Creek Formation|42367|5|Briefly described|p18|||McNamara Group||||||
25038|Gunpowder Creek Formation|43235|5|Briefly described|p9,Fig.10.|||Of McNamara Group.||||||27-MAY-08
25038|Gunpowder Creek Formation|44115|14|Not recorded|p17|||||||||
25038|Gunpowder Creek Formation|44210|2|Defined|map,Tb.1,p8,9|||||||||
25038|Gunpowder Creek Formation|44213|14|Not recorded|Map Legend||Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|44271|2|Defined|p35,56|||Contains mineral deposits.||||||
25038|Gunpowder Creek Formation|44275|14|Not recorded|Map Legend|||||||||
25038|Gunpowder Creek Formation|44279|14|Not recorded|Tb.1|||||||||
25038|Gunpowder Creek Formation|44290|2|Defined|p438|||Precambrian probably Palaeoproterozoic.||||||
25038|Gunpowder Creek Formation|44521|14|Not recorded|p8,10,21,map|||upper Early Proterozoic||||||
25038|Gunpowder Creek Formation|44552|14|Not recorded|p6,8,9|||||||||
25038|Gunpowder Creek Formation|44989|2|Defined|p.104-7|||On many pages. Tb.III. Penecontemp.with Ploughed Mount. and Surprise Creek Beds. (E54-13,F54-1).||||||25-SEP-06
25038|Gunpowder Creek Formation|45161|5|Briefly described|Table 3|||||||||
25038|Gunpowder Creek Formation|45166|5|Briefly described|p30|||||||||
25038|Gunpowder Creek Formation|45287|14|Not recorded|p.225,226,229||Paleoproterozoic|||||||07-NOV-08
25038|Gunpowder Creek Formation|46801|6|Mentioned|Fig. 14|||Stratigraphy||||||
25038|Gunpowder Creek Formation|47083|3|Fully described|p15||Proterozoic|Equivalent to Moondarra Siltstone and Breakaway Shale. Of McNamara Gp. Overlain by Paradise Crk Fm; underlain by Torpedo Crk Quartzite. Maximum thickness 800 m.||||||25-SEP-06
25038|Gunpowder Creek Formation|49041|6|Mentioned|Table 4|||||||||
25038|Gunpowder Creek Formation|50224|6|Mentioned|p380 Fig. 6|||||||||07-FEB-11
25038|Gunpowder Creek Formation|50550|5|Briefly described|p1139 Fig.2,p1143 Fig.6||Statherian|Age: 1694 Ma. Overlies Torpedo Creek Quartzite at syn-rift unconformity, overlain by Mount Oxide Chert at post-rift unconformity. Geological Province: Western Fold Belt.||||||19-DEC-07
25038|Gunpowder Creek Formation|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group.  Siltstone, sandstone, dolomite.  Overlain by Paradise Creek Formation.||||||
25038|Gunpowder Creek Formation|60359|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metasiltstone. Of the McNamara Group.||||||
25038|Gunpowder Creek Formation|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Paradise Creek Formation.||||||03-JUN-09
25038|Gunpowder Creek Formation|61936|5|Briefly described|p194 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: ~1694Ma. Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||07-NOV-08
25038|Gunpowder Creek Formation|62084|5|Briefly described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Gunpowder Ck Fm.||McNamara Group|||Variably dolomitic organic siltstones and shales.|
25038|Gunpowder Creek Formation|63109|6|Mentioned|p1108 Fig. 3|||Geological Province: Calvert Superbasin. Consists of sandstone and some shales.||||||30-SEP-08
25038|Gunpowder Creek Formation|63111|5|Briefly described|p1162, p1164 Tb. 1|Statherian|Statherian|Of Prize Supersequence. Age: 1690+/-7Ma. Geological Province: Isa Superbasin. Conglomeratic and massive quartzite, sandstone, siltstone, claystone, fine-grained feldspathic sandstone, dolomitic sandstone.||||||07-FEB-11
25038|Gunpowder Creek Formation|63114|5|Briefly described|p1253 Fig.2. |||Isa superbasin.||Of the Gun supersequence||||
25038|Gunpowder Creek Formation|63866|5|Briefly described|p57|||Calvert Superbasin.||Gun Supersequence||Overlies the Bigie Formation.||
25038|Gunpowder Creek Formation|63884|5|Briefly described|p14|||Siliciclastic. In contact with Paradise Creek Formation.||||||
25038|Gunpowder Creek Formation|64748|6|Mentioned|p276 Fig. 9|Paleoproterozoic|Paleoproterozoic|Palaeomag results shown on polar wander path||||||
25038|Gunpowder Creek Formation|65228|5|Briefly described|p16, Figs.04, 10.|Statherian|Statherian|Contains the maximum flooding surface of the Gun Supersequence, informally named after this unit. Lower part studied in detail by Sami et al. (2000). Age is for the lower part of the unit (in the Prize Supersequence).|1694 +/- 3 Ma.|Unit in McNamara Group.||||
25038|Gunpowder Creek Formation|65337|5|Briefly described|p5, p32, p33 Fig.27.|||Calvert Superbasin. |1694 +/- 3 Ma.|Unit in McNamara Group.||Overlies Surprise Creek Formation. Is overlain by Paradise Creek Formation.|Includes tuffs.|
25038|Gunpowder Creek Formation|66844|5|Briefly described|p243-244,253,254, 264, 271,273|||Lawn Hill Platform. Characterised by a regionally correlative unconformity (Gun Supersequence boundary) in the lower to middle GCF representing a depositional hiatus of 28my, separating the Gun and underlying Prize supersequences. Stromatolites are dominantly domal-columnar, indicative of shallow sub-tidal and peritidal environments.||Of lower McNamara Group; Gun and Prize supersequences.|Informally subdivided into lower and upper parts at Gun and Prize sequence boundaries.||Initially siliciclastic. Includes organic-rich shales and phosphatic precipitates near the top.|
25038|Gunpowder Creek Formation|67323|5|Briefly described|GIS attrib tbl, p10-12, p72|Paleoproterozoic|Paleoproterozoic|See also Solid Geology Map. Isa Superbasin. p10 (Century Domain) says Calvert Superbasin and age 1694 +/-3 Ma, p11(Mount Oxide Domain) says age (from adjacent terranes): 1658+/-3 Ma and 1653+/-7 Ma. In Western Fold Belt, contains most of the Ag anomalies. Appears as Upper Gunpowder Formation in the Mount Isa Block Time-Space Plot.||McNamara Group.|||Laminated siltstone, dolomitic and carbonaceous siltstone, fine sandstone, feldspathic and pyritic quartzite, pebbly clayey sandstone.|
25038|Gunpowder Creek Formation|68146|6|Mentioned|p203|||The lower part of this unit contains peperites related to volcanism at c.1694 Ma.||||||
25038|Gunpowder Creek Formation|68542|6|Mentioned|p6|||||Lower McNamara Group||Overlain by Paradise Creek Formation, overlies Torpedo Creek Quartzite||
25038|Gunpowder Creek Formation|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Kamarga Zn-Pb-Ag deposit.||Lower McNamara Group.||Overlies Torpedo Creek Quartzite. Is overlain by Paradise Creek Formation.||
25038|Gunpowder Creek Formation|68732|5|Briefly described|p160-163, p168|||Hosts the Oxide Mine. Undulatory rhythmite facies common. In its lower parts, this formation contains iron-stained and quartz-rich intraclast grainstones, locally with domal and digitate stromatolite bioherms.||||Overlies Torpedo Creek Quartzite. Overlain by the Mount Oxide Chert.|Siliciclastic sediments. Mainly very fine-grained arkosic sandstones.|30-NOV-17
25038|Gunpowder Creek Formation|69591|5|Briefly described|p38 Fig.2.23,p42-44,p49 Fig.2.41,p54,p88|||Is presented on p43 (in Fig.2.31) as Lower and Upper Gunpowder Creek Formations. Part of Gun Supersequence. Shallow-marine deposits. Is lithologically similar to Moondarra Siltstone (Mount Isa Group).||McNamara Group.||Overlies Torpedo Creek Quartzite. Unconformably overlies Myally Subgroup.|Laminated siltstone, dolomitic and carbonaceous siltstone, fine sandstone, feldspathic and pyritic quartzite, pebbly clayey sandstone.|
25038|Gunpowder Creek Formation|70864|5|Briefly described|p75, 74 Fig 2, p79, 81, 82|Mesoproterozoic||||McNamara Group|Overlain by Surprise Creek Formation||Siltstones, shales and sandstones.|
25038|Gunpowder Creek Formation|71592|5|Briefly described|Appendix A.|||Leichhardt River Domain, Mount Isa Orogen.|1689+/-5 Ma (MDA: U-Pb zircon SHRIMP)||||Chert, sandstone, tuff.|
25038|Gunpowder Creek Formation|72912|5|Briefly described|p33 Fig.12.|Paleoproterozic|Paleoproterozic|Shown as part of McNamara Group.||||Underlies Paradise Creek Formation|Includes dolostone.|
25038|Gunpowder 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||Underlies Paradise Creek Formation.|Includes dolostone.|
25038|Gunpowder Creek Formation|72919|4|Described|p56-57, p63|Statherian|Statherian|Mount Isa Province. [Also written as 'Gunpowder Creek Formation']. Lithological description from Southgate et al. (1999). Deposited between ca. 1694 Ma and ca. 1658 Ma. Tuff crystallisation age of ca. 1694 Ma reported by Page et al. (2000). An internal unconformity has been inferred, although Withnall and Hutton (2013) suggested the portion containing glauconitic sandstones and finer units in Morstone 1 may instead correlate to the Mullera Formation.|Between ca. 1694 Ma and ca. 1658 Ma||||Thin-bedded to laminated siltstone and shale, with minor sandstone, dolostone and chert.|
25038|Gunpowder Creek Formation|73144|6|Mentioned|p9|||Isa Superbasin. Part of the Gun Supersequence.||||||
25038|Gunpowder Creek Formation|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1703+/-15 Ma MDA, 1694+/-3 Ma age of volcanic rock||||Clastics.|
27064|Gwynne Sandstone|23733|5|Briefly described|p32 Fig. 19|||||||||
27064|Gwynne Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the lower part of the Wauchope Subgroup.  Geological Province: N.E. Arunta.||||||
27064|Gwynne Sandstone|42643|2|Defined|p48||Paleoproterozoic|Of Wauchope Subgroup (Hatches Creek Group). Defn.card avail.||||||07-NOV-08
27064|Gwynne Sandstone|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Feldspathic/lithic/micaceous arenite, quartz arenite, sometimes pebbly.||||||07-NOV-08
27064|Gwynne Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Lower Wauchope Subgroup (Hatches Creek Gp).  Subarkosic, sublithic and lithic (partly volcaniclastic?) arenite and quartz arenite, commonly pebbly; minor conglomerate, greywacke and pyroclastic rocks.Underlies Strzeleckie Volcs.in Tennant Creek region.||||||07-NOV-08
27064|Gwynne Sandstone|64735|5|Briefly described|p206 Fig 2, p206, p216 Fig15,|Orosirian|Orosirian|Barrow Creek area, Aileron Province. Correlated with Hatches Creek Group, Ongeva Package, Ware Group.|||||Siliciclastic sedimentary rocks.|20-APR-12
27064|Gwynne Sandstone|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup.||Wauchope Subgroup||||05-JAN-17
27064|Gwynne Sandstone|65338|6|Mentioned|p19.|||Stratigraphic equivalent of Unimbra Sandstone. Correlative with Coulters Sandstone.||Unit in Wauchope Subgroup.||||
27064|Gwynne Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.|||Subarkosic, sublithic and lithic (partly volcaniclastic?) arenite and quartz arenite, commonly pebbly; minor conglomerate, greywacke and pyroclastic rocks.|
27064|Gwynne Sandstone|69425|4|Described|p10:6 Tb.10.1, 10:10-11, 13,15-16,23,25|||Osborne and Crawford Ranges. See also reference to [mis-spelled] Gwynnie Sandstone (p10:3). 40-500m thick. Fluvial and shallow-marine.||Wauchope Subgroup, lower.||Overlies Ooradidgee Group conformably/disconformably/unconformably. Is overlain conformably by Strzeleckie Volcanics. Correlative of Unimbra Sandstone.|Feldspathic/lithic/micaceous sandstone, quartz sandstone and pebbly sandstone. No intercalated volcanic rocks.|12-JUL-16
27064|Gwynne Sandstone|69427|5|Briefly described|p12:13|||||Wauchope Subgroup.||Is overlain conformably by Strzeleckie Volcanics. Correlated with Unimbra Sandstone.|Predominantly feldspathic and lithic sandstones with minor quartz sandstone, pebbly sandstone and siltstone interbeds.|12-JUL-16
27064|Gwynne Sandstone|69431|6|Mentioned|p16:5|||Osborne and Crawford Ranges.||Wauchope Subgroup.||||12-JUL-16
27064|Gwynne Sandstone|72711|6|Mentioned|p2.|Orosirian|Orosirian|Davenport Province.|> 1810 Ma.|Of Hatches Creek Group?|||Includes siltstone, sandstone, volcanic and metasedimentary assemblages.|
27791|HYC Pyritic Shale Member|22538|6|Mentioned|Fig3 P709|||Member actually spelt Mbr||||||
27791|HYC Pyritic Shale Member|22662|6|Mentioned|21,24,30|||Geol province McArthur Basin||||||
27791|HYC Pyritic Shale Member|22664|5|Briefly described|Fig. 2 p34|||Barney Creek Formation, Umbolooga Subgroup, McArthur Group.||||||
27791|HYC Pyritic Shale Member|22665|6|Mentioned|P230|||||||||
27791|HYC Pyritic Shale Member|22853|5|Briefly described|21|Proterozoic|Proterozoic|Parent Barney Creek Formation. Age 1690 +29 -25 Ma. Underlain by W-Fold Shale Member||||||27-SEP-06
27791|HYC Pyritic Shale Member|23534|5|Briefly described|p2318|||Mineralisation occurs in this member. Of Barney Creek Formation. Geological Province: McArthur Basin.||||||
27791|HYC Pyritic Shale Member|23776|5|Briefly described|p705 Fig 2.|||Of Barney Creek Formation.||||||
27791|HYC Pyritic Shale Member|23902|4|Described|p1568 Fig.2|||Of the Barney Creek Formation (Umbolooga Subgroup). Overlain by the Reward Dolomite. Overlies the W-Fold Shale Member. Geological Province: McArthur Basin||||||
27791|HYC Pyritic Shale Member|23910|5|Briefly described|p292|||Of Barney Creek Formation.  Geological Province: McArthur Basin.||||||
27791|HYC Pyritic Shale Member|23937|6|Mentioned|p10|||Of the Barney Creek Formation.||||||
27791|HYC Pyritic Shale Member|23961|6|Mentioned|p1200|||Geological Province: Mt Isa Inlier.||||||
27791|HYC Pyritic Shale Member|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Barney Creek Formation.||||||27-SEP-06
27791|HYC Pyritic Shale Member|30272|6|Mentioned|p2|||||||||
27791|HYC Pyritic Shale Member|30344|6|Mentioned|Fig.4|||Part of Umbolgoola Subgroup||||||
27791|HYC Pyritic Shale Member|30363|6|Mentioned|p22|||||||||
27791|HYC Pyritic Shale Member|32339|6|Mentioned|p143|||||||||
27791|HYC Pyritic Shale Member|33550|6|Mentioned|p272|||||||||
27791|HYC Pyritic Shale Member|37217|6|Mentioned|Fig.1|||||||||
27791|HYC Pyritic Shale Member|37371|6|Mentioned|p368|||||||||
27791|HYC Pyritic Shale Member|40109|6|Mentioned|p302|||||||||
27791|HYC Pyritic Shale Member|40691|6|Mentioned|Fig.4|||||||||
27791|HYC Pyritic Shale Member|41268|6|Mentioned|p284|||||||||
27791|HYC Pyritic Shale Member|42385|4|Described|p21|||Member of Barney Creek Formation.||||||
27791|HYC Pyritic Shale Member|42639|5|Briefly described|p28, Fig.8 p30|||Of Barney Creek Formation.||||||27-SEP-06
27791|HYC Pyritic Shale Member|42812|5|Briefly described|p38, Fig.5|||Of Barney Creek Formation.||||||27-SEP-06
27791|HYC Pyritic Shale Member|42935|4|Described|p532|||Of Barney Creek Formation.||||||27-SEP-06
27791|HYC Pyritic Shale Member|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
27791|HYC Pyritic Shale Member|43036|6|Mentioned|p52|||Of Barney Creek Formation.||||||27-SEP-06
27791|HYC Pyritic Shale Member|45162|4|Described|p99-100, p98|||Type section location p98.||||||06-APR-18
27791|HYC Pyritic Shale Member|60483|5|Briefly described|p7 Fig. 5|||Of Barney Creek Fm (Umbolooga Subgroup, McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
27791|HYC Pyritic Shale Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Barney Creek Formation.||||||03-JUN-09
27791|HYC Pyritic Shale Member|62084|5|Briefly described|p939, p941 Fig.9|||Isa Superbasin. McArthur Basin. Hosts McArthur River (formerly HYC) deposit (Zn-Pb-Ag stratiform) as eight stacked stratiform Zn-Pb-Ag ore lenses at base of unit. Shown as HYC pyritic shale and HYC Pyritic Shale in figures and text.||Barney Creek Formation||Is overlain by Reward Dolomite. Overlies W-fold Shale.|Dolomitic, carbonaceous siltstones.|
27791|HYC Pyritic Shale Member|64815|6|Mentioned|p4 Fig.2|||||Unit in Barney Creek Formation.||||
27791|HYC Pyritic Shale Member|64817|6|Mentioned|p353 Fig.4|||||Unit in Barney Creek Formation.||||
27791|HYC Pyritic Shale Member|65228|6|Mentioned|Fig.02.|||||Unit in Barney Creek Formation.||Overlies W-Fold Shale Member.||
27791|HYC Pyritic Shale Member|69430|4|Described|p15:3, 18-19, 31-40|Statherian|Statherian|Southern McArthur Basin. Hosts the world-class McArthur River (formerly HYC) Zn-Pb-Ag deposit, described in great detail. Shortened to HYC Shale Member (twice) on 15:37, and HYC Pyritic Shale on 15:38. SHRIMP zircon ages from tuffaceous sediments by Page and Sweet (1998), Page et al. (2000); comparable to tuffaceous units in the Limbunya Group (Birrindudu Basin).|1640 +/- 4, 1639 +/- 3 and 1638 +/- 7 Ma.|Barney Creek Formation.||Overlies W-Fold Shale Member.|A recessive, thinly bedded, laminated, carbonaceous, dolomitic pyritic siltstone; also thin beds of tuffaceous mudstone.|12-JUL-16
27791|HYC Pyritic Shale Member|69431|6|Mentioned|p16:25|||An equivalent unit was recognised in a succession in the northern Tomkinson Province, hosting low-grade base metal mineralisation.||||||12-JUL-16
27791|HYC Pyritic Shale Member|69673|4|Described|p16 fig 13, p33|||Batten Fault Zone. Hosts the world class McArthur River Zn-Pb-Ag deposit.||Barney Creek Formation||Overlies W-Fold Shale Member|Thinly bedded, laminated, carbonaceous, dolomitic pyritic siltstone with thin beds of tuffaceous mudstone.|
27791|HYC Pyritic Shale Member|71592|5|Briefly described|Appendix A.|||McArthur Basin. Also appears as Hyc Pyritic Shale Member.|1639+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)|Barney Creek FZ.|||Ash tuff.|
27791|HYC Pyritic Shale Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Barney Creek Formation?, Umbolooga Sub-group, McArthur Group||Underlain by W-Fold Shale Member. Overlain by Reward Dolostone. Equivalent to Cooley Dolostone.||
27791|HYC Pyritic Shale Member|73280|6|Mentioned|p1, p4-5, App.1A, App.1C|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report]. [Also written as Pyritic Shale Member in App.1C].||Barney Creek Formation||||
72381|Habgood Group, Upper|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Darwarunga Sandstone to Gwakura Formation.||Sandstone, dolomitic mudstone and sandstone, stromatolitic-evaporitic dolostone; minor conglomerate.|04-MAR-20
80726|Haddon Volcanics|72377|2|Defined|iii,p1,10-12, p19 App 1|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Newly defined unit  in this record (NTGS2019-007). Sample BM16JAW086 (prophyritic rhyolite 588978E 8510538N): LA-ICP-MS zircon dating yielded 1712+\-12 Ma magmatic crystallisation age i.e. time of sub-volcanic magmatism/volcanism and emplacement of Haddon Volcanics. Likely time-equivalent with Fagan Volcanics (c. 1707 Ma for 2 samples of rhyolite dated from the Maidjunga and Dhupuwamirri members). Minimum age constraint provided by timing of deposition of the overying Jalma Formation (1720+\-10 Ma) and Coast Range Sandstone (1670+\-10 Ma) (Kositcin et al., 2017, see also this record).|1712+\-12 Ma (magmatic)|||||10-OCT-19
26306|Hagen Member|12951|5|Briefly described|p143 Fig.4, p149, 151, 154-155, 157|Late Cambrian|Late Cambrian|Georgina Basin. Shown as basal member of Arrinthrunga Formation in Fig 4., but formerly the basal unit of the Chabalowe Formation. Age assumed from parent Formation. Oil shows in several wells.||Of Arrinthrunga Formation.|||Dolostone with subordinate grainstone at base.|
26306|Hagen Member|22954|6|Mentioned|Fig3p9|Ordian-Early Templetonia|Early Cambrian|||||||
26306|Hagen Member|24442|5|Briefly described|p45|Late Cambrian|Late Cambrian|Of the Chabalowe Formation.  Prosepective for petroleum - offering vuggy dolostone reservoir rocks and an evaporite seal. ||||||
26306|Hagen Member|41524|2|Defined|p38|Middle Cambrian||Fully described p19.||||||25-SEP-06
26306|Hagen Member|41525|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Chabalowe Formation. Dolostone with gypsum beds, chert; minor claystone and fine sandstone interbeds.||||||26-OCT-05
26306|Hagen Member|42643|4|Described|p30|||||||||
26306|Hagen Member|47058|6|Mentioned|p135|||Of Chabalowe Formation.||||||25-SEP-06
26306|Hagen Member|60122|5|Briefly described|p57 Appendix|||Of the Chabalowe Formation. Peritidal, grey evaporitic carbonate.||||||26-OCT-05
26306|Hagen Member|60123|4|Described|p5|Cambrian|Cambrian|Of the Chabalowe Formation. Conformably overlies Arthur Creek Formation; disconformably overlies Hatches Creek Group. Max. thickness: 160m.||||||12-OCT-10
26306|Hagen Member|60675|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Chabalowe Formation. Overlies Arthur Creek Formation. Dolostone with gypsum beds, chert; minor claystone and fine sandstone interbeds.||||||12-JAN-05
26306|Hagen Member|61022|5|Briefly described|p14, p15 Fig. 2|Late Cambrian|Late Cambrian|Overlies the 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.||||||20-APR-05
26306|Hagen Member|62376|5|Briefly described|p53|Late Cambrian|Middle Cambrian|Geological Province: Georgina Basin. Of the Chablowe Formation.||||||09-FEB-10
26306|Hagen Member|62759|5|Briefly described|p1|Late Cambrian|Late Cambrian|Of the Arrinthrunga Formation.||||||01-FEB-07
26306|Hagen Member|62789|5|Briefly described|p129 Fig. 2|Late Cambrian|Late Cambrian|Southern Georgina Basin.||Unit in Chabalowe Formation.||Overlies Middle Cambrian Arthur Creek Formation.||28-MAR-12
26306|Hagen Member|64068|3|Fully described|p66-67, p89, p ix.|Late Cambrian|Late Cambrian|Potential hydrocarbon reservoir rock.||Basal part of Chabalowe Formation.||Conformably overlies Arthur Creek Formation. Unconformably overlies Hatches Creek Group. Laterally interdigitates with basal Arrinthrunga Formation|Light grey evaporitic dolostone; minor grey-green to red siltstone, brown quartz sandstone, grey quartzic dolostone, intraformational conglomerate.|04-APR-12
26306|Hagen Member|64778|6|Mentioned|p13|Cambrian|Cambrian|Dulcie Syncline, Southern Georgina Basin.||||||
26306|Hagen Member|64812|4|Described|p236, p241-2 Figs. 8, 9, 10, p246, p249|Late Cambrian|Late Cambrian|Basal unit of Chabalowe Formation. Geological Province: Georgina Basin. Sharply unconformable on Arthur Creek Formation. Detailed lithological description included for basal grainstone/calcarenite/ooid banks, stromatolitic dolostone, evaporites+red beds.||||||07-FEB-11
26306|Hagen Member|64813|5|Briefly described|p254, p255, p256 Fig. 2|Late Cambrian|Late Cambrian|Of the Chabalowe Formation. Geological province: Georgina Basin. Comprises reservoir-quality dolostone with subordinate grainstone at base, overlain by massive anhydrite which acts as a seal. ||||||
26306|Hagen Member|65237|4|Described|p3 Fig. 4, p9|Late Cambrian|Late Cambrian|Basal member of Chabalowe Fm. Geol.prov: southern Georgina Basin. Includes near-shoreline facies at base (well sorted crossbedded grainstone, ooid banks), overlain by stromatolitic dolostone, and succeeded in the west of basin by supratidal evaporites.||||||07-FEB-11
26306|Hagen Member|65489|5|Briefly described|p127|Middle Cambrian|Middle Cambrian|Georgina Basin. An extensive nearshore regressive blanket. Has reservoir potential with adequate sealing capacity.||Basal unit in Chabalowe Formation.|||Dolostone.|
26306|Hagen Member|69206|6|Mentioned|p2|||Georgina Basin.||Chabalowe Formation.||||
26306|Hagen Member|69437|6|Mentioned|p22:15|||May have potential as a petroleum source and reservoir rock.||Chabalowe Formation.||||12-JUL-16
26306|Hagen Member|69443|5|Briefly described|p28:18-19, 45-46|Late Cambrian|Late Cambrian|Georgina Basin. Subsurface only. Up to 160m thick. Characterised by a relative abundance of evaporite, and a greater proportion of dolostone to siliciclastic rocks, than the rest of the Formation. Thin shales are a viable petroleum source rock. Also a potential petroleum reservoir.||Chabalowe Formation.|||Dolostone, including microbial (stromatolitic and thrombolite) and intraclast types, together with dolomudstone; characterised by massive and bedded gypsum and lesser anhydrite.|12-JUL-16
26306|Hagen Member|69673|5|Briefly described|p120, p127,  p134, p136, p137, p138|||160m thick. Potential as a reservoir rock. Evaporites in this unit may form a seal.||Chabalowe Formation|||Evaporite, stromatolitic and thrombolitic dolostone, dolomudstone, subordinate grainstone.|
26306|Hagen Member|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin. Oil show.||Chabalowe Formation|||Dolomite.|
26306|Hagen Member|70951|5|Briefly described|p1074, 1076, 1077, 1082, 1083|||Geological province: Georgina Basin. Dolomite-dominated in both SWIR and TIR wavelengths.||Unit of Chabalowe Formation.||Underlain by Steamboat Sandstone.||
26306|Hagen Member|72321|6|Mentioned|Fig 2|Guzhangian|Guzhangian|Elkedra Shelf/Dulcie Syncline, Georgina Basin.  Australian Stage: Boomerangian.||Of Chabalowe Formation.||||
26306|Hagen Member|73288|5|Briefly described|p698, 700, 702, 705, 710 Table 3|Middle Cambrian|Middle Cambrian|Southern Georgina Basin. Non-economic oil and gas shows have been recorded. Downhole (Hylogger) logs; scratch test results tabulated.||Chabalowe Formation.||||
25689|Hale Formation|38885|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25689|Hale Formation|39552|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25689|Hale Formation|39583|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25689|Hale Formation|39610|6|Mentioned|p7|||||||||
25689|Hale Formation|39931|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
25689|Hale Formation|43565|4|Described|p424-444|||||||||
25689|Hale Formation|43748|5|Briefly described|p9, Tb 1, Fig. 4, 5, 9|Late Eocene|Paleocene|Hale Basin. Previously included the 'Arltunga Member' - a sandstone unit, herein renamed Tug Sandstone Member.|||Includes 'Ambalindum Sandstone Member', Ulgnamba Lignite Member, Claraville Mudstone Member (Delaney Mudstone Member), Tug Sandstone Member|||17-OCT-12
25689|Hale Formation|46730|5|Briefly described|p7|Cenozoic|Cenozoic|Overlies Amadeus Basin units.  Maximum thickness: 75m.||||||06-SEP-10
25689|Hale Formation|48992|2|Defined|p22|Tertiary|Tertiary|Prob. Tertiary||||||
25689|Hale Formation|60525|5|Briefly described|Map Legend|Tertiary|Tertiary|Includes: Ulgnamba Lignite Member. Kaolinitic quartzose sandstone, boulder conglomerate.||||||
25689|Hale Formation|65194|5|Briefly described|p53|||Probably Eocene. Kaolinitic, argillaceous, poorly sorted sand and gravel beds, overlain by carbonaceous shale or lignite lenses, mud- and silt- rich layers, and an upper sandy unit known as the Tug Sandstone (silicified).||||||
25689|Hale Formation|69418|5|Briefly described|p3:35|Cenozoic|Cenozoic|Hale River Basin.|||Ulgnamba Lignite Member.|||12-JUL-16
25689|Hale Formation|69458|5|Briefly described|p42:7-10, 12-13|||Hale Basin. Appears to have been deposited in a progressively flooding and slowly subsiding basinal setting.|||Ambalindum Sandstone, Delaney Mudstone, Ulgnamba Lignite, Tug Sandstone, Members.|Is overlain unconformably by Waite Formation.||12-JUL-16
83369|Halfway Dam formation|73086|4|Described|p123-124|||Informal unit that has been described by several researchers. Restricted distribution. Stratigraphically between Olympic Formation and Waldo Pedlar Member (Pertatataka Formation); thus, apparently equivalent to the lower Pertatataka Formation. Authors recommend that this unit is a local variant of the lower Pertatataka Formation and should not be interpreted as a separate unit. Thickness: ~205 m.||||Disconformably underlain by Olympic Formation.|Grey-green siltstone with distinctive manganiferous olive-green interbeds of carbonate rock.|
27793|Halls Creek Group|505|6|Mentioned|p711|Archean|Archean|Halls Creek Province.|||Includes Olympio Formation.|||
27793|Halls Creek Group|14019|6|Mentioned|p19|||||||||
27793|Halls Creek Group|22440|5|Briefly described|p4|Orosirian|Orosirian|Age 1800- 1840Ma||||||
27793|Halls Creek Group|22496|3|Fully described|p7|Paleoproterozoic|Paleoproterozoic|Redefined to exclude the Ding Dong Downs Volcanics; now comprises Saunders Creek, Biscay and Olympio Formations: on RUBY PLAINS only the latter two represent this group.||||||07-NOV-08
27793|Halls Creek Group|22526|5|Briefly described|P679, P680||Orosirian|||||||
27793|Halls Creek Group|22537|5|Briefly described|34|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|22547|5|Briefly described|P8||Orosirian|||||||
27793|Halls Creek Group|22661|6|Mentioned|p 313|||||||||
27793|Halls Creek Group|22716|6|Mentioned|p234|||||||||
27793|Halls Creek Group|22741|5|Briefly described|P9, Table3 P19||Proterozoic|||||||
27793|Halls Creek Group|22754|5|Briefly described|p3, p6|||Of the Lamboo Complex.  Age 1880-1840 Ma.  See also p16 and p29.||||||
27793|Halls Creek Group|22764|5|Briefly described|Table 1 p7|Paleoproterozoic|Archean|Includes Olympio Formation.||||||01-FEB-10
27793|Halls Creek Group|22777|5|Briefly described|Map|||||||||
27793|Halls Creek Group|23314|5|Briefly described|329||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|23323|5|Briefly described|p454 Fig.2|Proterozoic|Proterozoic|In the North Australian Craton.||||||07-FEB-07
27793|Halls Creek Group|23383|1|Redefined|p12, p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Lamboo Complex. Comprises: Saunders Creek, Biscay and Olympio Formations. Overlain by Moola Bulla Formation. Intruded by Woodward Dolerite.  Age: 1880 to 1847 Ma.  Geol. Prov: Hooper Orogen.  See also p6 Fig. 3.||||||22-DEC-08
27793|Halls Creek Group|23568|5|Briefly described|p2777 Fig 2|Paleoproterozoic|Paleoproterozoic|Age: ~1915-1845 Ma.||||||07-NOV-08
27793|Halls Creek Group|23599|4|Described|p8|Paleoproterozoic|Paleoproterozoic|Age: c.1880-1850 Ma (SHRIMP U-Pb zircon)||||||07-NOV-08
27793|Halls Creek Group|23601|5|Briefly described| Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Olympio Formation.  Age: c.1860Ma.||||||07-NOV-08
27793|Halls Creek Group|23621|4|Described|p15|Orosirian|Orosirian|See also page 11 table 1. Age: 1880-1845 Ma. Geological Province: Halls Creek Orogen.||||||
27793|Halls Creek Group|23622|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|23722|5|Briefly described|p5|Orosirian|Orosirian|Age: c.1880Ma (U-Pb)||||||
27793|Halls Creek Group|23821|5|Briefly described|p245|Proterozoic|Archean|||||||07-NOV-08
27793|Halls Creek Group|23925|5|Briefly described|p234 Fig. 13|Orosirian|Orosirian|Age: 1915-1845 Ma.  Geological Province: Halls Creek Orogen.||||||
27793|Halls Creek Group|24173|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Includes Saunders Creek, Biscay and Olympio Formations. Unconformably overlies Ding Dong Downs Volcanics. Geological Province: Halls Creek Orogen. Age: ~1880-1845Ma.||||||07-NOV-08
27793|Halls Creek Group|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lamboo Complex (central zone).||||||07-NOV-08
27793|Halls Creek Group|24572|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: >1835Ma.  Geological Province: Halls Creek Orogen.||||||07-NOV-08
27793|Halls Creek Group|29447|6|Mentioned|p11|||||||||
27793|Halls Creek Group|29805|6|Mentioned|p7|||||||||
27793|Halls Creek Group|29807|6|Mentioned|p6|||See also P15||||||
27793|Halls Creek Group|29809|6|Mentioned|Table 1|||||||||
27793|Halls Creek Group|29813|4|Described|Table 2|||||||||
27793|Halls Creek Group|29818|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27793|Halls Creek Group|29845|6|Mentioned|p108|||||||||
27793|Halls Creek Group|30097|6|Mentioned|Table 23|||Also Table 25||||||
27793|Halls Creek Group|30525|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|30526|6|Mentioned|p110|||||||||
27793|Halls Creek Group|30533|3|Fully described|p9|||On Table 1. Age 2700 m.y. (uncertain)||||||
27793|Halls Creek Group|30878|6|Mentioned|p51|||Precambrian. Stratigraphic table||||||
27793|Halls Creek Group|30892|3|Fully described|p93|||? Archaean age. See also pp94-100.||||||25-SEP-06
27793|Halls Creek Group|30893|5|Briefly described|p205|||Archaean age. Lithology||||||
27793|Halls Creek Group|30894|5|Briefly described|p250|||Archaean to Lower Proterozoic||||||
27793|Halls Creek Group|30895|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|30896|4|Described|p9|||Archaean age||||||
27793|Halls Creek Group|30897|4|Described|p8|||Stratigraphy||||||
27793|Halls Creek Group|30898|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|31226|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27793|Halls Creek Group|31230|6|Mentioned|p182|||||||||
27793|Halls Creek Group|31361|6|Mentioned|p4|||||||||
27793|Halls Creek Group|31362|6|Mentioned|p7|||Correlated||||||
27793|Halls Creek Group|31393|6|Mentioned|Pl.25|||||||||
27793|Halls Creek Group|32171|6|Mentioned|p5|||Refers Dow & Gemuts (1969)||||||
27793|Halls Creek Group|32643|6|Mentioned|p535|||||||||
27793|Halls Creek Group|32659|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean or Lower Proterozoic||||||07-NOV-08
27793|Halls Creek Group|32660|4|Described|Table 1|||Re stratigraphy||||||
27793|Halls Creek Group|32664|6|Mentioned|Map legend|Proterozoic|Archean|Archaean or Proterozoic. Briefly described in notes||||||07-NOV-08
27793|Halls Creek Group|32699|5|Briefly described|Map legend|Archean|Archean|Slate, green schist, mica schist and andalusite schist.||||||07-NOV-08
27793|Halls Creek Group|32701|5|Briefly described|Table 1|||||||||
27793|Halls Creek Group|32728|4|Described|p19|||||||||
27793|Halls Creek Group|33376|6|Mentioned|Map legend|Proterozoic|Archean|Archaean and/or Proterozoic||||||07-NOV-08
27793|Halls Creek Group|33377|6|Mentioned|Table 1|||Stratigraphy||||||
27793|Halls Creek Group|33443|6|Mentioned|p260|||||||||
27793|Halls Creek Group|34604|6|Mentioned|Fig.4|||||||||
27793|Halls Creek Group|34684|6|Mentioned|p102|||||||||
27793|Halls Creek Group|34723|6|Mentioned|p239|||||||||
27793|Halls Creek Group|35040|6|Mentioned|p375|||||||||
27793|Halls Creek Group|35120|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean - Proterozoic||||||07-NOV-08
27793|Halls Creek Group|35495|6|Mentioned|p340|||||||||
27793|Halls Creek Group|35726|6|Mentioned|p69|||||||||
27793|Halls Creek Group|35950|6|Mentioned|p302|||||||||
27793|Halls Creek Group|36225|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
27793|Halls Creek Group|36257|6|Mentioned|p27|||||||||
27793|Halls Creek Group|36308|6|Mentioned|p211|||||||||
27793|Halls Creek Group|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
27793|Halls Creek Group|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|36551|6|Mentioned|p22|||Also mentioned p25,P41, p115.||||||25-SEP-06
27793|Halls Creek Group|36885|3|Fully described|p165|||||||||
27793|Halls Creek Group|36887|6|Mentioned|p206|||Formerly Halls Creek Metamorphics.||||||25-SEP-06
27793|Halls Creek Group|36898|6|Mentioned|p183|||||||||
27793|Halls Creek Group|36902|6|Mentioned|p11|||||||||
27793|Halls Creek Group|37299|6|Mentioned|Fig.1|||||||||
27793|Halls Creek Group|37462|3|Fully described|p221|||||||||
27793|Halls Creek Group|37577|6|Mentioned|p26|||||||||
27793|Halls Creek Group|38066|6|Mentioned|Fig.9|||P53||||||
27793|Halls Creek Group|38482|6|Mentioned|Table 1|||||||||
27793|Halls Creek Group|39827|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|39887|6|Mentioned|p453|||||||||
27793|Halls Creek Group|39889|6|Mentioned|p495|||||||||
27793|Halls Creek Group|40494|4|Described|p5|||Also mention on p3.||||||25-SEP-06
27793|Halls Creek Group|40765|6|Mentioned|p3|||||||||
27793|Halls Creek Group|40793|6|Mentioned|p165|||||||||
27793|Halls Creek Group|41125|6|Mentioned|p30|||||||||
27793|Halls Creek Group|41158|6|Mentioned|p18|||||||||
27793|Halls Creek Group|41465|5|Briefly described|p4|||||||||
27793|Halls Creek Group|41635|6|Mentioned|p19|||||||||
27793|Halls Creek Group|41883|6|Mentioned|p65|||||||||
27793|Halls Creek Group|41952|6|Mentioned|p188|||||||||
27793|Halls Creek Group|41976|5|Briefly described|p453|||||||||
27793|Halls Creek Group|41977|4|Described|p471|||||||||
27793|Halls Creek Group|41987|6|Mentioned|p70|||||||||
27793|Halls Creek Group|42149|6|Mentioned|p703|||||||||
27793|Halls Creek Group|42326|5|Briefly described|p9|||||||||
27793|Halls Creek Group|42329|6|Mentioned|Fig.2 P6|||||||||
27793|Halls Creek Group|42504|6|Mentioned|p59|||||||||
27793|Halls Creek Group|42730|5|Briefly described|p19|||||||||
27793|Halls Creek Group|42768|5|Briefly described|p6, Fig.6|||||||||
27793|Halls Creek Group|42811|6|Mentioned|p5|||||||||
27793|Halls Creek Group|42814|6|Mentioned|p5|||||||||
27793|Halls Creek Group|43299|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|43303|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27793|Halls Creek Group|43561|6|Mentioned|p1437|||||||||
27793|Halls Creek Group|43595|4|Described|p74,223,349|||Accumulate approx. 2150 Ma cease approx.1920 Ma||||||
27793|Halls Creek Group|43631|6|Mentioned|p7,9|||of East Kimberley||||||
27793|Halls Creek Group|43632|6|Mentioned|p2||Proterozoic|||||||
27793|Halls Creek Group|43666|6|Mentioned|p52,Table 2||Neoproterozoic|||||||
27793|Halls Creek Group|43794|5|Briefly described|p319||Proterozoic|||||||
27793|Halls Creek Group|43819|6|Mentioned|p33|||||||||
27793|Halls Creek Group|43854|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44155|4|Described|p232-255|Paleoproterozoic|Paleoproterozoic|Matheson and Guppy (1949), Dow and Gemuts (1969). All basalts in this unit are tholeiitic, more-iron-rich than Antrim Plateau Volcanics in the same region.|||Ding Dong Downs Volcanics; Saunders Creek, Biscay, Olympio Formations.|Equivalent to Tickalara Metamorphics. Intruded by Woodward Dolerite.|Undivided: phyllitic siltstone and greywacke, schist; some acid volcanics.|
27793|Halls Creek Group|44231|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes: Saunders Creek, Biscay and Olympio Formations. Age: c. 1855Ma and 1880Ma.  In the Lamboo Complex (eastern zone).||||||07-NOV-08
27793|Halls Creek Group|44317|14|Not recorded|p.5||Proterozoic|||||||
27793|Halls Creek Group|44318|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44324|14|Not recorded|p.5|||Fig.2, Tb.1. (Archaean or Proterozoic).||||||
27793|Halls Creek Group|44325|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44363|4|Described|p.8,9|||Archaean or Lower Proterozoic.||||||
27793|Halls Creek Group|44364|14|Not recorded|map legend|||||||||
27793|Halls Creek Group|44366|14|Not recorded|p.8, Table 1|||Includes Olympio Formation. Archaean or Proterozoic.||||||
27793|Halls Creek Group|44367|14|Not recorded|map legend|||(Reprinted 1971).||||||
27793|Halls Creek Group|44397|14|Not recorded|p.9,18, Fig.4,Tb.1|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44398|14|Not recorded|map legend|||Archaean or Proterozoic.||||||
27793|Halls Creek Group|44693|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44694|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|44868|5|Briefly described|Map Legend||Proterozoic|||||||
27793|Halls Creek Group|45047|2|Defined|p61|Archean|Archean|Prob. Archaean||||||07-NOV-08
27793|Halls Creek Group|45048|5|Briefly described|p10|||Lithology of units||||||
27793|Halls Creek Group|45112|5|Briefly described|Table 4|||||||||
27793|Halls Creek Group|45140|2|Defined|p12-15, p17, p25, p42, p58, p60, p73|||See also Appx.p2, p11-12. Dow and Gemuts (1969). Formerly Halls Creek Metamorphics (Traves, 1955). Named after Halls Creek township. Halls Creek Province. Probably several thousand metres thick. Low-grade metamorphism dated at 1961 +/- 27 Ma (Dow and Gemuts, 1969). Probable maximum age is 2200 Ma (Page, 1976).|>1960 Ma.||Ding Dong Downs Volcanics; Saunders Creek, Biscay, Olympio Formations.|Correlated with the Tanami and Arunta Complexes.|Tightly-folded low-grade metasediments and metavolcanics.|
27793|Halls Creek Group|46797|5|Briefly described|p79|||Age||||||
27793|Halls Creek Group|46864|4|Described|p39|||||||||
27793|Halls Creek Group|46899|6|Mentioned|p8|||Thermal conductivity||||||
27793|Halls Creek Group|48927|6|Mentioned|p10|||||||||
27793|Halls Creek Group|48931|3|Fully described|p9|||||||||
27793|Halls Creek Group|48938|4|Described|p8|||Lithology.||||||
27793|Halls Creek Group|48950|6|Mentioned|p8|||||||||
27793|Halls Creek Group|50437|6|Mentioned|p5.1|||Intrudes: Saunders Creek Formation.||||||
27793|Halls Creek Group|60006|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Halls Creek Orogen. Unconformably overlain by Whitewater Volcanics and Bucket Spring Member. Schist, phyllite, volcanics, slate||||||07-NOV-08
27793|Halls Creek Group|60283|6|Mentioned|p25 Fig.2|||Halls Creek Orogen.||||||
27793|Halls Creek Group|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Lambo Complex (Eastern Zone). Includes: Biscay Formation, Olympio Formation.||||||
27793|Halls Creek Group|60682|4|Described|piii|Paleoproterozoic|Paleoproterozoic|Ferruginous phyllite, quartz-mica schist, mylonitised acid volcanics, quartz-sericite schist and slate. Age: >1800Ma. Geological Province: Halls Creek Orogen.||||||07-NOV-08
27793|Halls Creek Group|60724|1|Redefined|p4, p6|||Proposed the group be redefined to exclude all rocks below unconformity at base of Saunders Creek Fm, including Sophie Downs Granite and Ding Dong Downs Volcs (both prev.mapped within the group). Revision to incl: Saunders Creek, Biscay and Olympio Fms.||||||
27793|Halls Creek Group|61861|6|Mentioned|Fig.2.|||Correlative with Tanami Group.|||Includes Saunders Creek, Biscay and Olympio Formations.|||
27793|Halls Creek Group|63866|5|Briefly described|p105, p130, p137|||Litchfield Province, Pine Creek Orogen. |||Includes the Saunders Creek Formation, Biscay Formation and the Olympio Formation.|Overlies the Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.||
27793|Halls Creek Group|64104|6|Mentioned|p63 Fig.1|Paleoproterozoic|Paleoproterozoic||||Includes Olympio Formation.|||
27793|Halls Creek Group|64329|5|Briefly described|p15|||Contains the informally named "Niobium Tuff" which hosts the Brockman deposit.||||||
27793|Halls Creek Group|64572|6|Mentioned|p802 Fig. 4, p803 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1915-1845Ma. Geological Province: North Australian Craton.||||||22-DEC-08
27793|Halls Creek Group|64580|6|Mentioned|map legend|||||||||
27793|Halls Creek Group|64722|5|Briefly described|Fig. 2 p3-6, p9, 24|Orosirian|Orosirian|Of Halls Creek / Leopold orogen. Inferred to have accumulated on the conjugate passive margin to the proto-North Australian Craton to the east.|~1890-1850 Ma.|||Unconformably overlies Ding Dong Downs Volcanics.||11-APR-12
27793|Halls Creek Group|64731|5|Briefly described|p164, 165|Paleoproterozoic|Paleoproterozoic|High-level bimodal volcanism.|1855 Ma.|||||12-APR-12
27793|Halls Creek Group|64956|6|Mentioned|p96, p97|||||||||07-FEB-11
27793|Halls Creek Group|65331|5|Briefly described|Map legend + overview geology map legend|Palaeoproterozoic|Palaeoproterozoic|Of Halls Creek Orogen. Schist, undifferentiated ferruginous phyllite, altered volcanics, slate||||||
27793|Halls Creek Group|66845|5|Briefly described|p536 Fig.2, p537|Paleoproterozoic|Paleoproterozoic|Eastern zone of Lamboo Complex. Rests unconformably on granite and volcanic rock dated at c. 1910 Ma (Tyler et al. 1995; Blake et al. 2000).|c. 1880-1845 Ma|||||
27793|Halls Creek Group|68078|6|Mentioned|p2, p5|Paleoproterozoic|Paleoproterozoic|Deposited on granitic and volcanic basement of Ding Dong Downs Volcanics.|1845-1880 Ma||||Sedimentary and volcanic rocks.|
27793|Halls Creek Group|68244|6|Mentioned|p664,666|||||||Overlain unconformably by Landrigan Formation (Kuniandi Group).||21-JUN-19
27793|Halls Creek Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv. Lamboo Complex. Variably magnetic.|1910-1840 Ma (Tyler, 2000).||Includes Olympio Formation.||Metasedimentary and igneous rock; mafic volcanic rock.|
27793|Halls Creek Group|69003|4|Described|p19, p20 Fig.25|Paleoproterozoic|Paleoproterozoic|E zone, Lamboo Province, Halls Creek Orogen.|c.1880-c.1845 Ma.||Saunders Creek, Biscay, Olympio Formations.|Overlies Ding Dong Downs Volcanics and Sophie Downs Suite.|Sedimentary and volcanic rocks.|
27793|Halls Creek Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Metamorphic age 1861 +/-5 Ma SHRIMP.|||Includes Olympio Formation, Biscay Formation, Saunders Creek Formation, and unnamed unit.||Pelite, psammite, with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock|31-JUL-15
27793|Halls Creek Group|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv, GA_geochron.csv. |1861 Ma||Includes Olympio Formation, Biscay Formation, Saunders Creek Formation||Undivided; pelite, psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock.|
27793|Halls Creek Group|69422|6|Mentioned|p7:1|||Eastern Zone, Halls Creek Orogen.||||||12-JUL-16
27793|Halls Creek Group|69452|6|Mentioned|p36:6|||Halls Creek Orogen.||||Is overlain unconformably by Kellys Knob Sandstone.||12-JUL-16
27793|Halls Creek Group|69585|5|Briefly described|p2, p4|Orosirian|Orosirian||1880-1845 Ma.||Saunders Creek, Biscay, Olympio Formations.|Unconformably overlies Ding Dong Downs Volcanics.|Metasedimentary and volcanic rocks.|
27793|Halls Creek Group|69587|4|Described|GEOL_LUT_CSV files|||Geological Province: Lamboo Province, Halls Creek Orogen. See 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|||Includes Biscay Formation, Olympio Formation.|||
27793|Halls Creek Group|69597|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Eastern Lamboo Province. Deposited on the passive continental margin of the North Australia Craton. |1910-1845 Ma||||Mafic volcanic rocks.|
27793|Halls Creek Group|69634|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv.|1907-1808 Ma (Inferred)||Includes Olympio Formation, Saunders Creek Formation.||Migmatitic pelitic hornfels comprising quartz-K-feldspar-biotite-cordierite-sillimanite; locally retrogressed to quartz-muscovite-biotite-chlorite(-sillimanite)-andalusite schist|
27793|Halls Creek Group|70154|4|Described|100k_interpgeol_lut.csv|Paleoproterozoic|Paleoproterozoic|See also 500k_interpgeop_lut.csv.|1808-1907 Ma||Olympio Formation||Migmatitic pelitic hornfels comprising quartz, k feldspar, biotite, cordierite and sillimanite.  locally retrogressed to quartz-muscovite-biotite-chlorite(-sillimanite)-andalusite schist.|
27793|Halls Creek Group|70206|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic||||||Ferruginous phyllite, schist, altered volcanic rocks and slate.|
27793|Halls Creek Group|70731|5|Briefly described|p269-270,272-273,277-278|Orosirian|Orosirian|Geological province: Lamboo Province, Halls Creek Orogen, Kimberley Craton.|1880-1847 Ma||Includes Olympio and Biscay formations.|||
27793|Halls Creek Group|70812|4|Described|p5, p7, p9, p11-p12, p19, p25, p38|Orosirian|Orosirian|Eastern Zone of the Halls Creek Orogen, Lamboo Province. Hosts signifcant mineral deposits and occurences which are described.|1880-1847 Ma||Includes the Saunders Creek Formation, Biscay Formation and Olympio Formation and the Ding Dong Downs Volcanics.|Unconformably overlies the Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.|Siliciclastic sedimentary and volcanic rocks.|
27793|Halls Creek Group|70826|6|Mentioned|p5 tbl 2, p9|Paleoproterozoic|Paleoproterozoic|Halls Creek Basin.||||||22-APR-20
27793|Halls Creek Group|70851|4|Described|p3-p5, p18-p19, p23-p24, p28-p29|Paleoproterozoic|Paleoproterozoic|Eastern Zone, Lamboo Province.|c. 1880-1847 Ma||Includes the Saunders Creek Formation, Biscay Formation and the Olympio Formation.|Unconformably overlies the Sophie Downs Suite and Ding Dong Downs Volcanics. Intruded by the Woodward Dolerite.|Siliciclastic sedimentary and volcanic rocks.|
27793|Halls Creek Group|71113|5|Briefly described|p97-98, p109|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen.|1880-1840 Ma||Includes Olympio Formation, Biscay Formation and Saunders Creek Formation.|||21-AUG-19
27793|Halls Creek Group|71140|5|Briefly described|p97-98, 101, 109-110|Orosirian|Orosirian|Eastern Zone, Lamboo Province, Halls Creek Orogen.|1880-1840 Ma.||Saunders Creek, Biscay, Olympio Formations.|Is intruded by sills of Woodward Dolerite.|Low- to medium-grade metasedimentary and meta-igneous rocks.|
27793|Halls Creek Group|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (1832-1821 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv, 100k_interpgeol_lut.csv and geochron files.|1880-1845 Ma||Includes Biscay Formation, Brim Rockhole Formation, Olympio Formation, Saunders Creek Formation.|Underlain by Sophie Downs Suite.|Pelite and psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock|
27793|Halls Creek Group|71281|4|Described|p422|||Eastern Zone, Lamboo Province. Greenschist to lower amphibolite facies metasedimentary and metavolcanic rocks. Folded during the 1835-1810 Ma Halls Creek Orogeny.|||Olympio Formation.|Is intruded by the Sally Downs Supersuite.|Basal sandstones with c.1881 Ma mafic volcanic rocks, overlain by metaturbidites containing intercalated active-margin alkaline volcanic rocks.|
27793|Halls Creek Group|71397|4|Described|p1-6,8,14,33,42,48|Orosirian|Orosirian|Geological province: Eastern Zone, Lamboo Province, Halls Creek Orogen. Exposed in a >275 km long, NNE-trending belt of greenschist facies metasedimentary and metavolcanic rocks. Marks new depositional phase in the Eastern Zone after basement development. Mylonites in the Halls Creek Group likely associated with c. 1000-800 Ma Yampi Orogeny (Tyler and Griffin, 1990; Tyler et al., 1995).|||Includes Olympio Formation, Biscay Formation, Brim Rockhole Formation, Saunders Creek Formation.|Underlain unconformably by Sophie Downs Suite. Intruded by Woodward Dolerite.||28-NOV-19
27793|Halls Creek Group|71873|5|Briefly described|p427|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province. Intruded by Woodward Dolerite during Halls Creek Orogeny c. 1832-1808 Ma.|||Includes Olympio, Biscay, Brim Rockhole and Saunders Creek formations.|Underlain unconformably by Sophie Downs Suite.||
27793|Halls Creek Group|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Halls Creek Orogen.|||||Pelite and psammite with basaltic and andesitic to trachytic metavolcanic and metavolcaniclastic rock.|
27793|Halls Creek Group|72437|6|Mentioned|p7, p11, p24|||||||Intruded by the San Sou suite.||
27793|Halls Creek Group|73089|5|Briefly described|p24-28, p31, p37, p43|Orosirian|Orosirian|Lamboo Province, Eastern Zone. Kimberley region. Comparable to the Tanami Group in terms of lithostratigraphy, changes in provenance and thickness.|1885-1835 Ma|||||
24304|Hanlon Subgroup|22446|4|Described|p20, fig1p25,fig3,|Statherian|Statherian|||||||
24304|Hanlon Subgroup|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Errolola Sandstone. Of Hatches Creek Group.||||||07-NOV-08
24304|Hanlon Subgroup|23733|5|Briefly described|p28, p31|||Of Hatches Creek Group. See also p32 Fig.19 and p34 Fig.20.||||||
24304|Hanlon Subgroup|23809|5|Briefly described|p27|||Of the Hatches Creek Group.  Geological Province: Davenport Province.||||||
24304|Hanlon Subgroup|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: ~1780Ma.    Geological Province: Davenport Province (Tennant Inlier).||||||07-NOV-08
24304|Hanlon Subgroup|24172|5|Briefly described|p54, p65 Tb.9|||Of the Hatches Creek Group. Geological Province: Tennant Creek Inlier. Comprises Canulgerra Sandstone, Lenee Creek Formation, Alinjabon amd Errolola Sandstones.||||||20-NOV-06
24304|Hanlon Subgroup|24197|6|Mentioned|p65|||||||||07-FEB-11
24304|Hanlon Subgroup|24303|5|Briefly described|p55 Appendix|||Geological Province: Davenport province. Probable correlative of Tomkinson Creek Group.||||||
24304|Hanlon Subgroup|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24304|Hanlon Subgroup|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hatches Creek Group.||||||10-JAN-05
24304|Hanlon Subgroup|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24304|Hanlon Subgroup|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24304|Hanlon Subgroup|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Geological Province: Tennant Creek Block.||||||07-NOV-08
24304|Hanlon Subgroup|41129|3|Fully described|p5|||||||||
24304|Hanlon Subgroup|41204|4|Described|p11|||||||||
24304|Hanlon Subgroup|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hatches Creek Group.||||||16-NOV-05
24304|Hanlon Subgroup|41308|4|Described|p11|||||||||
24304|Hanlon Subgroup|41310|4|Described|p12|||See also Table 1||||||
24304|Hanlon Subgroup|41408|6|Mentioned|Map legend|Proterozoic||||||||
24304|Hanlon Subgroup|41524|4|Described|p10|||||||||
24304|Hanlon Subgroup|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Comprises Errolola Sandstone, Alinjabon Sandstone and Lennee Creek Formation.||||||07-NOV-08
24304|Hanlon Subgroup|41970|6|Mentioned|p333|||||||||
24304|Hanlon Subgroup|42643|4|Described|p12, Table 1 p6|||||||||
24304|Hanlon Subgroup|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group.||||||07-NOV-08
24304|Hanlon Subgroup|43223|5|Briefly described|Map Legend||Proterozoic|Of Hatches Creek Group.||||||25-SEP-06
24304|Hanlon Subgroup|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.||||||07-NOV-08
24304|Hanlon Subgroup|43802|6|Mentioned|p77-79|||||||||
24304|Hanlon Subgroup|45167|3|Fully described|p20, Table 1|||Of Hatches Creek Group.||||||25-SEP-06
24304|Hanlon Subgroup|49033|2|Defined|p24|Proterozoic|Proterozoic|||||||
24304|Hanlon Subgroup|50353|5|Briefly described|Map Legend|||Of Hatches Creek Group.||||||
24304|Hanlon Subgroup|50588|5|Briefly described|p1.1, 3.1|||Geological Province: Tennant Creek/Davenport Province. Of the Hatches Creek Group.||||||
24304|Hanlon Subgroup|60684|5|Briefly described|p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Includes Errolola Sandstone.||||||07-NOV-08
24304|Hanlon Subgroup|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group.  Includes the Errolola and Alinjabon Sandstones, Lennee Creek Formation, Canulgerra Sandstone, Vadingilla Formation and Yaddanilla sandstone.  In the Tennant Creek region.||||||07-NOV-08
24304|Hanlon Subgroup|61567|5|Briefly described|p631, p632|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group. Composed of 3 buff-coloured sandstone units: Errolola and Alinjabon Sandstones and Lennee Creek Formation; arenites are separated by recessive siltstones and volcanics.  Age: >1660Ma. Max. thickness: ~900m.  See also p633 Tb. 1.||||||07-NOV-08
24304|Hanlon Subgroup|64735|4|Described|p205 Fig 1, p206 Fig 2, p211|Orosirian|Orosirian|Mis-spelt in Fig 1.||Of Hatches Creek Group.|Includes Yaddanilla, Errolola, Canulgerra and Alinjabon Sandstones, Vaddingilla and Lennee Creek Formations.|Overlies Kudinga Basalt of the Wauchope Subgroup.||30-APR-12
24304|Hanlon Subgroup|65209|5|Briefly described|p36, p37|Paleoproterozoic|Paleoproterozoic|Layer cake stratigraphy. Geol. Prov: Davenport Province||Hatches Creek Group|Yaddanilla Sandstone, Vaddingilla Formation, Canulgerra Sandstone, Lennee Creek Formation, Alinjabon Sandstone, Errolola Sandstone.|||
24304|Hanlon Subgroup|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of Hatches Creek Group, Davenport Province. Includes Errolola Sandstone.||||||
24304|Hanlon Subgroup|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of Hatches Creek Group, Davenport Province. Includes Errolola Sandstone.||||||
24304|Hanlon Subgroup|65338|5|Briefly described|p6, p20.|||||Unit in Hatches Creek Group.|Includes Errolola, Alinjabon, Canulgerra and Yaddanilla Sandstones; Lennee Creek and Vaddingilla Formations.||Siltstone; minor calcareous rocks.|
24304|Hanlon Subgroup|65358|5|Briefly described|p14, p16|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group. Transgressive littoral to neritic sandstone and siltstone.||||||
24304|Hanlon Subgroup|66767|5|Briefly described|p57|||Davenport Province. Up to 5.2km thick.||Hatches Creek Group.||Overlies Wauchope Subgroup.||
24304|Hanlon Subgroup|66860|6|Mentioned|p6 Tb.1|||Tennant Region. Deposition was coeval with Pargee Sandstone (Tanami Region).||||||
24304|Hanlon Subgroup|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hatches Creek Group.|Includes Errolola, Alinjabon, Canulgerra and Yaddanilla Sandstones; Lennee Creek and Vaddingilla Formations.|Overlies Wauchope Subgroup.||
24304|Hanlon Subgroup|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Errolola, Alinjabon, Canulgerra and Yaddanilla Sandstones; Lennee Creek and Vaddingilla Formations.|Overlies Wauchope Subgroup.||
24304|Hanlon Subgroup|67352|4|Described|p8, p9, p44 fig 48, p50||Early Statherian|Shallow marine to deltaic.||Hatches Creek Group|Yaddanilla, Canulgerra, Alinjabon, Errolola Sandstones; Vaddingilla, Lennee Creek Formations.|Overlies Wauchope Subgroup.|Entirely marine.|
24304|Hanlon Subgroup|68518|5|Briefly described|p6 Tb.1, p13|Proterozoic|Proterozoic|||Hatches Creek Group|Lennee Creek Formation, Alinjabon Sandstone, Errolola Sandstone|Overlies Wauchope Subgroup.|May be entirely marine.|30-JUN-14
24304|Hanlon Subgroup|69424|6|Mentioned|p9:2|Paleoproterozoic|Paleoproterozoic|Warramunga Province.||||Hatches Creek Group.||12-JUL-16
24304|Hanlon Subgroup|69425|4|Described|p10:1-3, 10-12, 18-20|Statherian|Statherian|Blake et al. (1985) included this unit with their Wauchope and Ooradidgee Subgroups to form the redefined Hatches Creek Group. Davenport Province. Generally c.4000m thick, maximum exposed c.5200m.||Hatches Creek Group.|Yaddanilla, Canulgerra, Alinjabon, Errolola Sandstones; Vaddingilla, Lennee Creek Formations.|Is overlain unconformably by Andagera Formation.|Predominantly a succession of recessive sandstone and siltstone, with intercalated, low-ridge forming sandstone intervals; minor calcareous intervals.|12-JUL-16
24304|Hanlon Subgroup|69431|5|Briefly described|p16:2, 5, 22|||Davenport Province, Tennant Region. Folding during the Davenport Event is discussed.||Hatches Creek Group.|Errolola, Alinjabon, Canulgerra, Yaddanilla Sandstones; Lennee Creek, Vaddingilla Formations.|||12-JUL-16
81145|Harding Gabbro|71255|6|Mentioned|p2|||Overprinted by the Illogwa Shear Zone during the Palaeozoic Alice Springs Orogeny. Quartz 1:100k map sheet area.||||||19-JUN-19
24306|Harry Anorthositic Gabbro|9199|5|Briefly described|Map legend|||Geological Province: Arunta Block.||||||04-NOV-04
24306|Harry Anorthositic Gabbro|23844|3|Fully described|p26|||Geological Province: Arunta Province. Max Thickness: 1000m? Truncates the Johannsen Metagabbro dyke swarm. See also Fig.10||||||
24306|Harry Anorthositic Gabbro|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24306|Harry Anorthositic Gabbro|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24306|Harry Anorthositic Gabbro|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24306|Harry Anorthositic Gabbro|39610|6|Mentioned|p5|||||||||
24306|Harry Anorthositic Gabbro|39887|6|Mentioned|p453|||See Fig.3||||||
24306|Harry Anorthositic Gabbro|48992|2|Defined|p23|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24306|Harry Anorthositic Gabbro|50369|6|Mentioned|p26.5|||||||||
24306|Harry Anorthositic Gabbro|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 1). Of the Strangways Metamorphic Complex. Meta-anorthositic gabbro.||||||02-NOV-04
24306|Harry Anorthositic Gabbro|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Anorthositic Gabbro.||||||
24306|Harry Anorthositic Gabbro|60668|5|Briefly described|p10, p2 Tb. 1|||Eastwest trending elongated bodies of rock. Dominated by medium- to coarse-grained uralitised anorthositic gabbro metamorphosed to granulite facies. See also Figs. 20a and 20b.||||||
24306|Harry Anorthositic Gabbro|67181|5|Briefly described|p631|Statherian|Statherian|Aileron Province, North Australian Craton. Related tonalite age 1787 +/-  Ma from Claoue-Long and Hoatson (2005) and/or Hoatson et al. (2005)|1787 +/- 3 Ma from a related tonalite|||||
24306|Harry Anorthositic Gabbro|69427|4|Described|p12:9-10, 20, 24, 41|Statherian|Statherian|Shaw et al. (1979); Hoatson et al. (2005). Strangways Range region, Aileron Province. A parallel series of elongate bodies in S foothills of Utnalanama Range. Appears as Harry Anorthositic gabbro on 12:9. SHRIMP U-Pb zircon crystallisation age from a tonalite (probably the Phlogopite Mine Tonalite).|1787 +/- 3 Ma Claoue-Long and Hoatson, 2005).|||Intrudes Utnalanama Granulite and Johannsen Metagabbro. Is intruded by Gumtree Granite.|Dominant rock type is a medium- to coarse-grained uralitised anorthositic gabbro, metamorphosed to granulite facies; minor metamorphosed anorthosite, quartz anorthosite, leucogabbro, gabbro, tonalite; rare pyroxenite.|12-JUL-16
24306|Harry Anorthositic Gabbro|71839|5|Briefly described|p10|||Outcrops in ALICE SPRINGS.||Strangways Metamorphic Complex||Intruded by the Gumtree Granite.||
36822|Harts Range Metamorphic Complex|23858|5|Briefly described|p923|||||||||
36822|Harts Range Metamorphic Complex|61660|6|Mentioned|p2.|Proterozoic|Proterozoic|Irindina Province, eastern Arunta Region. ||||||
36822|Harts Range Metamorphic Complex|63562|6|Mentioned|p351|||Includes a small granitic body dated 387 +/- 4 Ma (Buick et al., 2001).||||||
36822|Harts Range Metamorphic Complex|64068|5|Briefly described|p25, 32, 199|Cambrian|Neoproterozoic|SHRIMP U-Pb dating of detrital zircons from southern Georgina Basin units has recently been undertaken, for comparison with metasedimentary units in the HRMC, as there are no available absolute age determinations (at the time of this study). Also Harts Range Complex p35.||||||
36822|Harts Range Metamorphic Complex|64571|6|Mentioned|p837|||||||||
36822|Harts Range Metamorphic Complex|66767|5|Briefly described|p59|Cambrian|Neoproterozoic|Irindina Province, Arunta Region. Crops out extensively in the Harts Range and extends as scattered low outcrops to the E and SE, into the Simpson Desert, and to the N near Mallee Bore. Similar zircon populations to similarly-aged sedimentary rocks in the adjacent Amadeus and Georgina Basins.|||||A thick metasedimentary succession with subordinate Paleozoic igneous units including mafic to ultramafic intrusions, metabasalts, granites and pegmatites.|
36822|Harts Range Metamorphic Complex|67479|6|Mentioned|p46|Ordovician|Cambrian|||||||
36822|Harts Range Metamorphic Complex|68316|5|Briefly described|pp777-782, pp784-786||Series 2|Inherited zircon in a granite intrusive into these rocks have yielded a SHRIMP U-TH-Pb age as young as c. 520 Ma (Buick et al. 2001).|< 520 Ma||Includes the Harts Range Meta-Igneous Complex.|Structurally underlain by the Entia Gneiss Complex.|Includes metasedimentary rocks.|
36822|Harts Range Metamorphic Complex|68697|5|Briefly described|v, p20, p22, p24, p46|Paleozoic|Neoproterozoic|Irindina Province, Arunta Region.|||Includes Brady and Irindina Gneisses.|||07-JAN-20
36822|Harts Range Metamorphic Complex|68997|4|Described|vii-viii,p55|Early Paleozoic|Neoproterozoic|Thickness 5-6km. Deposited in the Centralian Superbasin during the Neoproterozoic to earliest Palaeozoic prior to Ordovician mid-amphibolite to granulite facies metamorphism (Mawby 2000). The unnamed pelitic gneiss sampled from the Bungitina Metamorphics area (IC08JAW910) contained 445+\-7 Ma metamorphic zircon rims, indicating growth during early 450-300 Ma Alice Springs Orogeny (Scrimgeour and Raith 2001), which required thrusting of the Harts Range Metamorphic Complex over Palaeoproterozoic basement along the proximal Bruna Detachment Zone (eg Mawby et al 1999).|||Includes Yambla Gneiss.||Pelitic and semi-pelitic metasedimentary rocks, amphibolites and calc-silicates, with subordinate quartzite, marble and felsic gneiss.|
36822|Harts Range Metamorphic Complex|69031|5|Briefly described|p5|Cambrian|Neoproterozoic|Dominates the Irindina Province. Structurally interleaved with highly deformed granites.|||||Granulite-facies pelite, psammite, metamafic rocks, and calc-silicate rocks.|
36822|Harts Range Metamorphic Complex|69226|6|Mentioned|p238-239|||Eastern Arunta Inlier.||||||
36822|Harts Range Metamorphic Complex|69418|6|Mentioned|p3:31-32|||Irindina Province. Hosts mica deposits in the Harts Range/Plenty River fields. Source of abrasive quality garnets within alluvial sands in watercourses and sand dunes in the Harts Range area.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69427|5|Briefly described|p12:36-37|Cambrian|Neoproterozoic|Irindina Province. Separated from the structurally underlying Entia Gneiss Complex by the Bruna Granitic Gneiss.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69444|5|Briefly described|p29:1-10|Late Cambrian|Neoproterozoic|Formerly Harts Range Group (Joklik, 1955; Shaw et al., 1982). Irindina Province. Underwent upper amphibolite to granulite facies metamorphism during the Ordovician Larapinta Event.|||Irindina and Brady Gneisses.||An intensely deformed but flat-lying supracrustal succession consisting of pelitic and psammopelitic metasedimentary rocks, metabasite and calc-silicate rock, with subordinate marble, quartzite and felsic gneiss. Mid-amphibolite to granulite facies.|12-JUL-16
36822|Harts Range Metamorphic Complex|69458|6|Mentioned|p42:38|||Irindina Province. Garnetiferous metamorphic rocks are the source of abrasive-quality garnet in alluvial sands in the Harts Range area.||||||12-JUL-16
36822|Harts Range Metamorphic Complex|69510|6|Mentioned|p17|||480-460 Ma metamorphic ages for the Larapinta Event were obtained by Maidment (2005) and others.||||||
36822|Harts Range Metamorphic Complex|69917|5|Briefly described|p114, 138, 141,160,175,177-178|Paleozoic|Neoproterozoic|Cut by granite dykes: magmatism during the Alice Springs Orogeny was not continuous, but occurred in a series of discrete high-grade pulses, including at ca 382 and 360 Ma (Storkey 2004). See also p182, 184, 187, 189, 197, 198.|||Includes Brady, Yambla, Last Hope, Entire, Stanovos, Spriggs and ?Leprechaun Gneisses.|In contact with Paleoproterozoic Bruna Gneiss.||29-JUL-15
36822|Harts Range Metamorphic Complex|69932|6|Mentioned|p310-311|||Presented as Harts Range Metamorphic Igneous Complex on p310. May contain up to 80% Nd of an Archean component possibly from a sialic basement. Formed in association with 1780-1750 Ma back-arc opening.|||||Includes anorthositic gneisses.|
36822|Harts Range Metamorphic Complex|69937|6|Mentioned|p25, p28, p31|Paleozoic|Neoproterozoic||||Irindina Gneiss.|||
36822|Harts Range Metamorphic Complex|70825|6|Mentioned|p40, 42|||Arunta Region, North Australian Craton.||||||
36822|Harts Range Metamorphic Complex|71279|6|Mentioned|p353-354|||||||||
36822|Harts Range Metamorphic Complex|72375|5|Briefly described|p25,27|Paleozoic|Neoproterozoic|Geological province: Irindina Province.|||Includes Irindina Gneiss.|||
36822|Harts Range Metamorphic Complex|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Irindina Province.|||Includes the Yambla Gneiss.|||
36822|Harts Range Metamorphic Complex|72516|4|Described|iii, p7, p64, p78-79, p135-136|Cambrian|Neoproterozoic|Irindina Province. Formerly the Harts Range Group. Previously considered to include the Irindina Gneiss and the Brady Gneiss. |||Includes the Irindina Gneiss, Brady Gneiss, Yambla Gneiss, Pinnacle Gneiss, Last Hope Gneiss and the Leprechaun Gneiss.||Supracrustal succession of metamudstone, metagreywacke, metasandstone, metamafic igneous rocks and calc-silicate rocks with subordinate amounts of marble and felsic gneiss.|
36822|Harts Range Metamorphic Complex|72524|5|Briefly described|piii, p8, p13.|Cambrian|Neoproterozoic|Irindina Province. Deposited or emplaced during the Neoproterozoic-Cambrian and metamorphosed during the 480-460 Ma Larapinta Event. Includes migmatitc gneiss with maximum depositional age of 1019+/-23 Ma, and high grade metamorphism at 467+/-9 Ma. Source rock for Ghost gum granite.|||Yambla Gneiss, Stanovos Gneiss, Last Hope Gneiss, unnamed migmatitic gneiss.||Succession of metasedimentary rocks and subordinate igneous units [both piii and p8].|27-OCT-20
36822|Harts Range Metamorphic Complex|73184|6|Mentioned|p197|Ordovician|Ordovician|Peak metamorphism at ca 470 Ma in the Larapinta Event (Hand et al., 1999). [Possibly mentioned on p196 and 197 as Harts Range?] Cross-cut by numerous pegmatites with SHRIMP U-Pb monazite and zircon ages of ca 450-300 Ma.|ca 470 Ma|||||
24307|Harverson Granite|1490|6|Mentioned|p6|||Associated with the 1140 Ma Ormiston Event (aka Teapot Event).|930 +/- 190 Ma (Black et al., 1993).|||||
24307|Harverson Granite|7837|6|Mentioned|p92|||Northern Arunta Inlier. U-Pb zircon geochronology by Collins and Williams (1995). This ~1820 Ma age replaces the 930 +/- 190 Ma Rb-Sr isochron age (?Shaw and Black, 1991) so this unit cannot be part of the 1050-900 Ma ""Ormiston Event"".|~1820 Ma.|||||
24307|Harverson Granite|7838|5|Briefly described|p69-70, 73-74, 76-77, 83, 87|||Emplaced during the first of two tectonic cycles in the northern Arunta Inlier. Zircon analyses tabulated and discussed.|1818 +/- 8 Ma.|||Intrudes Lander Rock beds.|Coarse-grained, weakly deformed, K-feldspar megacrystic granite which forms a subcircular pluton. S-type.|
24307|Harverson Granite|11884|5|Briefly described|Map Legend|Calymmian|Statherian|Carpentarian age.||||Intrudes the Mount Airy Granite.|Muscovite-biotite granite with a very coarse pophyritic texture, massive, aligned feldspar phenocrysts stubby not tabular.|
24307|Harverson Granite|23270|5|Briefly described|Table 1, p4||Proterozoic|Of Arunta Block. Age: Rb-Sr Whole Rock 900+/-250ma.||||||25-SEP-06
24307|Harverson Granite|23271|5|Briefly described|Map legend||Proterozoic|Of Arunta Block. Age: Middle Proterozoic.||||||25-SEP-06
24307|Harverson Granite|23733|5|Briefly described|p34 Fig.20|||Age: 1818Ma.||||||
24307|Harverson Granite|24197|5|Briefly described|p19, p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Harverson Suite. Coarse-grained, grey, granitic augen gneiss. Age: ~1820Ma. Geological province: Arunta Inlier.||||||07-FEB-11
24307|Harverson Granite|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24307|Harverson Granite|38829|5|Briefly described|p134|||See also Table 3||||||
24307|Harverson Granite|39888|6|Mentioned|Fig.10|||||||||
24307|Harverson Granite|41964|6|Mentioned|p184|||||||||
24307|Harverson Granite|42146|6|Mentioned|p652|||||||||
24307|Harverson Granite|42217|5|Briefly described|p412|||||||||
24307|Harverson Granite|42326|5|Briefly described|Table 2 P11|||||||||
24307|Harverson Granite|43568|6|Mentioned|p506|||||||||
24307|Harverson Granite|48992|2|Defined|p23|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24307|Harverson Granite|50369|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Haverson Suite. Age: 1820 +/- 7Ma (Sm-Nd), 1818 +/- 8Ma (SHRIMP).||||||07-NOV-08
24307|Harverson Granite|64956|5|Briefly described|p3 Tb. 1, p21|Paleoproterozoic|Paleoproterozoic|Intrudes lower amphibolite-facies Lander Rock beds. Cryst. age: 1799+/-3Ma (previously determined as 1818+/-8Ma {Collins and Williams 1995}). Geological province: Arunta region. Sample is K-feldspar megacrystic biotite muscovite granite; S-type.||||||07-FEB-11
24307|Harverson Granite|65338|5|Briefly described|p15, p17.|Statherian|Orosirian|S-type. Is discordant with respect to deformation in the surrounding Lander Rock Formation, but is weakly deformed. Has complex zircon systematics; previous (Collins and Williams 1995) age determination was 1818 +/- 8 Ma.|1799 +/- 3 Ma (Worden et al. 2008).|||Intrudes Lander Rock Formation.||
24307|Harverson Granite|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
24307|Harverson Granite|69226|5|Briefly described|p239-243, p254-255|Orosirian|Orosirian|Reynolds-Anmatjira Ranges region.|1818 +/- 8 Ma (Collins and Williams, 1995).|||Intrudes Lander Rock Beds.||
24307|Harverson Granite|69427|4|Described|p12:20-21, 26|Statherian|Orosirian|Reynolds Range, Aileron Province. A sub-circular pluton. Andalusite and cordierite porphyroblasts occur in contact aureoles. SHRIMP dating; this age is more consistent with field relationships than a previous age determination of 1818 +/- 8 Ma by Collins and Williams (1995).|1799 +/- 3 Ma (Worden et al., 2008).|||Intrudes Lander Rock Formation.|Coarse-grained, weakly deformed K-feldspar megacrystic granite; has an andalusite-bearing contact aureole. S-type.|12-JUL-16
24307|Harverson Granite|69932|6|Mentioned|p302-303, 306-307, 309|||Northern Province, Arunta Inlier. Late-tectonic. Sm-Nd data tabulated.|1820 Ma.||||Small, massive, coarse-grained, megacrystic feldspar granite. S-type.|
24307|Harverson Granite|70376|6|Mentioned|p833, fig 2, p833-834|Paleoproterozoic|Paleoproterozoic|Forms a contact metamorphic aureole ranging from greenschist to lower amphibolite facies and is typically defined by growth of andalusite and cordierite. Also dated at 1799+/-3 Ma (Collins & Williams 1995; Worden et al. 2008).|1818 Ma +/- 8 Ma|||||
24307|Harverson Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1818+/-8 Ma (U-Pb zircon: SHRIMP)||||Granite.|
24307|Harverson Granite|71858|6|Mentioned|p5|||Aileron Province.||||||
30858|Harverson Suite|24197|4|Described|p19|Paleoproterozoic|Paleoproterozoic|Comprises Harverson Granite, Anmatjira, Yaningidjara and Mount Airy Orthogneisses. Intrusive suite that is fractionated, felsic, peraluminous. Age: 1820Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
30858|Harverson Suite|50369|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1820Ma.||||||07-NOV-08
30858|Harverson Suite|69932|6|Mentioned|p301|||Northern Province, Arunta Inlier. Source rock may contain significant Archean component.  Presented as Harverson suite.|||||Includes S-type granite.|
27290|Hayes Metamorphic Complex|37462|5|Briefly described|Tab.4.VIII|||||||||
27290|Hayes Metamorphic Complex|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27290|Hayes Metamorphic Complex|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27290|Hayes Metamorphic Complex|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
27290|Hayes Metamorphic Complex|39887|6|Mentioned|Fig.3|||||||||
27290|Hayes Metamorphic Complex|39888|6|Mentioned|Table 1|||||||||
27290|Hayes Metamorphic Complex|48992|2|Defined|p24|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
27290|Hayes Metamorphic Complex|50246|6|Mentioned|p8, p14|Paleoproterozoic|Paleoproterozoic|Includes Sadadeen Gneiss. Unconformably overlain by Iwapataka metamorphic Complex. Contains an assemblage of metasediments and suspected felsic volcanics which date to 1615Ma. Forms the hills within the town of Alice Springs.||||||07-FEB-11
27290|Hayes Metamorphic Complex|50369|6|Mentioned|p14.1|||||||||
27290|Hayes Metamorphic Complex|62595|5|Briefly described|p8. |Paleoproterozoic|Paleoproterozoic|Basement to Amadeus Basin.|||Includes Sadadeen Gneiss.|||
27290|Hayes Metamorphic Complex|69427|5|Briefly described|p12:15-16|||Shaw et al. (1979). Crops out S of the Charles River Fault, in the vicinity of Alice Springs township. No geochronology done, but interpreted to be older than c.1752 Ma.|||Emily Gap Schist, Teppa Hill Metamorphics.||Amphibolite-facies metasedimentary and meta-igneous rocks.|12-JUL-16
79431|Hayfield mudstone|69430|5|Briefly described|p15:26-27, 29, 62|||Informal name: shown in quotation marks. May be as young as Neoproterozoic and hence not part of the McArthur Basin. Has some reservoir potential. May act as a seal for the Jamison sandstone, sourced from the Kyalla Formation.||||Conformably overlies Jamison sandstone. Is overlain ?unconformably by Bukalara Sandstone.||12-JUL-16
79431|Hayfield mudstone|69673|4|Described|p19 fig 16, p33, p39, p40, p46|||Oil and gas shows, potential reservoir rock. Primarily mixed clastic sedimentary rocks. Informal name. Up to 450m thick.||||Overlain by Bukalara Sandstone, overlies Jamison sandstone|Silty mudstone with subordinate interbedded/laminated siltstone to fine sandstone.|
79431|Hayfield mudstone|70968|3|Fully described|v-vi,p75, p81-82, p84-92, p124-126, p128|Ediacaran|Neoproterozoic|See also p131-132, p137. Subsurface Beetaloo Sub-basin. Lanigan et al. (1994)'s informal name (originally Hayfield Mudstone) for a unit in an un-named Group they thought to be much younger than the unconformably underlying Roper Group, rather than forming a conformable upper unit. Supported by new evidence (reported in this study) showing detrital zircons are distinctly younger (late Mesoproterozoic) than the Maiwok Subgroup. Relationship with Chambers River Formation is unclear: discussed. Presumably named after Hayfield Station near Dunmarra. Shoreline to shallow-marine shelf deposits. Fence diagram of wells in Beetaloo Sub-basin. Up to c.450m thick; generally c.400m. Subtidal, shallow-marine shelf deposits. Lithology well-illustrated. Detrital zircon diagram and discussion.|||Hayfield sandstone member.|Conformably overlies Jamison sandstone. Is overlain unconformably by Antrim Plateau Volcanics or Bukalara Sandstone.|Green-grey to red-brown claystone, masssive to fissile, well-indurated, commonly silty, generally organic-poor; subordinate thinly interlaminated grey, commonly micaceous, siltstone and fine-grained sandstone. Prominent near-basal sandstone interval.|24-MAR-17
79431|Hayfield mudstone|71059|5|Briefly described|p14-16, p20|||TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, organic petrology reflectivity, data all detailed.||||||
79431|Hayfield mudstone|71374|4|Described|p21|Neoproterozoic|Neoproterozoic|Beetaloo Sub-basin, McArthur Basin.||||Overlies the Jamison sandstone. Previously considered equivalent to the Chambers River Formation.||07-MAY-18
79431|Hayfield mudstone|71488|5|Briefly described|p140-p143, p147-p151, p153|||Beetaloo Sub-basin. Deposited in a subtidal to shallow-marine shelf setting. Unconformably overlain by Neoproterozoic to Cambrian sedimentary and volcanic rocks of the Georgina Basin and Kalkaridnji Province.||||Overlies the Jamison sandstone.|Mudrock succession with minor sandstone.|
79431|Hayfield mudstone|71893|4|Described|iii, p2-p3, p6, p8, p40, p48-p51||Mesoproterozoic|Beetaloo Sub-basin of the McArthur Basin. Informal name.  Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|||Includes the Hayfield sandstone member.|Unconformably overlies the Roper Group. Conformably overlies the Jamison sandstone.||
79431|Hayfield mudstone|72381|5|Briefly described|p771-773,776-780|Neoproterozoic|Neoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Described by Munson (2016) as mudstone-dominated unit with sandstone interlayers, indicating a subtidal shallow-marine shelf depositional setting. Detrital zircon U-Pb age analysis by Yang et al (2018) indicate maximum depositional age of 959+\-18 Ma. Intersected in Elliott-1 drillhole, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). Interpreted to have been sourced from the south from the Musgrave Province.|959+\-18 Ma (max dep age)|||Underlain by upper Jamison sandstone.||04-OCT-19
79431|Hayfield mudstone|72526|5|Briefly described|p86-87.|Neoproterozoic|Neoproterozoic|Shown as 'Hayfield Mudstone' on diagram on p8 but text contradicts Mesoproterozoic age shown there. Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||||Overlies Roper Group, Jamison sandstone and underlies Bukalara Sandstone.||
79431|Hayfield mudstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||||Underlain by Jamison sandstone. Overlain by Bukalara Sandstone||
79769|Hayfield sandstone member|70968|5|Briefly described|p89, p124, p128-129||||1135 Ma (maximum depositional age).|Hayfield mudstone.|||A prominent, laterally-persistent, interlaminated medium-grained sandstone, fine-grained sandstone, siltstone and minor intercalated claystone. The sandstone is massive, laminated and locally low-angle cross-bedded.|
79769|Hayfield sandstone member|71893|4|Described|iii, p2-p3, p48-p51|Stenian|Neoproterozoic|Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|1092 +/- 15 Ma (Max dep. U-Pb-Hf)|Hayfield mudstone|||Quartz sandstone.|
77874|Hedleys Sandstone|67323|5|Briefly described|p9|Mesoproterozoic|Mesoproterozoic|Variation on Hedleys Sandstone Member. Detrital [?zircon] ages: 1591+/-10 Ma (2000), 1577 +/-29 Ma (Magee et al, in prep).||Implied to be of South Nicholson Group.||||
77874|Hedleys Sandstone|67539|5|Briefly described|p14|||North of the Elizabeth Creek fault. Raised to formation rank.||Of the South Nicholson Group.||Overlain by the Pandanus Siltstone.||
77874|Hedleys Sandstone|68146|5|Briefly described|p21-23, p29, p196-197|||Geochronology by Magee et al. (in press). This value was applied in determining a constraint on the MDA of Burangoo Sandstone in the current study.|1577 +/- 29 Ma; maximum depositional age.|Basal Wild Cow Subgroup.||||
77874|Hedleys Sandstone|68575|4|Described|p3,p6-7,p10-17,p19,p21,p125,p128,p134|||South Nicholson Basin. Shows significantly different provenance from that of Burangoo Sandstone.|1602 +/- 22 Ma (maximum depositional age).|Basal South Nicholson Group.||Unconformably overlies Doomadgee Formation.|Cross-bedded, sublithic to lithic, fine- to very coarse-grained and granule sandstone, interbedded with lenses of pebble to cobble conglomerate.|
77874|Hedleys Sandstone|69591|4|Described|p52-54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Appears as Hedley Sandstone in Fig.2.47. Predominantly fluvial. 1577 Ma age by Magee et al. (in press).|1591 +/- 10 Ma; 1577 +/- 29 Ma (MDA).|Wild Cow Subgroup.||Is overlain by Pandanus Formation.|Cross-bedded, medium- to coarse-grained quartzose sandstone with scattered granule and pebble bands; pebble to cobble conglomerate basal lenses with well-rounded quartz and quartzite and subangular-subrounded stromatolitic and oolitic chert clasts.|
77874|Hedleys Sandstone|71369|3|Fully described|p1, p6, p8-15, p19, p47, p49|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Raised to Formation status in this study (Sweet, 2017); previously Hedleys Sandstone Member (Rawlings et al., 2008) of Constance Sandstone. 35m thick in the type section from 198870E 8025500N to 199120E 8025290N in HEDLEYS CREEK sheet (diagram); slight variation of coordinates from the original by Rawlings et al. (2008). Outcrop pattern indicates left lateral (fault) movement of 700-800m.|c.1500 Ma.|Wild Cow Subgroup.||Unconformably overlies Doomadgee Formation and Widdallion Sandstone Member (Lawn Hill Formation). Is overlain by Pandanus Formation.|Basal conglomerate and very thick-bedded conglomeratic sandstone, gradually fining-up into thick-bedded, medium- to coarse-grained, strongly cross-bedded sandstone.|20-FEB-18
77874|Hedleys Sandstone|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1602+/-22 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
77874|Hedleys Sandstone|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Wild Cow Subgroup.||Overlain by Pandanus Sandstone.|Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Pandanus Sandstone.|Cross-bedded, medium to corase-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|
77874|Hedleys Sandstone|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 Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts.|19-MAR-20
77874|Hedleys Sandstone|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|10-DEC-19
77874|Hedleys Sandstone|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|10-DEC-19
77874|Hedleys Sandstone|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.|||||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|
77874|Hedleys Sandstone|72423|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet Geological Compilation Series.|||||Cross-bedded, medium to coarse-grained quartzose sandstone, scattered granule and pebble bands; pebble to cobble conglomerate lenses at base with well-rounded quartz and quartzite and subangular to subrounded chert and silicified limestone clasts|
77874|Hedleys Sandstone|72526|5|Briefly described|p8 Fig.1.3|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||?Wild Cow Subgroup, South Nicholson Group||Shown as  overlying Lawn Hill Formation and underlies Pandanus Formation.||
77874|Hedleys Sandstone|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin. Shown as overlying MacNamara Group in NT and QLD.||Wildcow Subgroup||Underlies Pandanus Formation.|Includes sandstone.|
77874|Hedleys Sandstone|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson.||Wildcow Subgroup||Underlies Pandanus Formation.|Includes sandstone.|
77874|Hedleys Sandstone|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in QLD. Distinct from Hedleys Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77874|Hedleys Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. Overlain by Pandanus Formation.||Wildcow Subgroup?, South Nicholson Group||Partly underlain by Widdallion Sandstone Member unconformably. Partly underlain(?) by Lawn Hill Formation.||
77874|Hedleys Sandstone|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Overlain by Pandanus Formation.||
25946|Henschke Breccia|32307|4|Described|Table 1|||L.Proterozoic||||||
25946|Henschke Breccia|32310|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25946|Henschke Breccia|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25946|Henschke Breccia|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25946|Henschke Breccia|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25946|Henschke Breccia|41645|4|Described|p10|||||||||
25946|Henschke Breccia|41646|6|Mentioned|Map legend|Paleoproterozoic||Of the Finnis River Group. Massive breccia conglomerate, passing upwards into a well-bedded pebbly arenite, with a phyllie band about 120m thick.||||||07-NOV-08
25946|Henschke Breccia|41980|4|Described|p573|||||||||
25946|Henschke Breccia|43187|5|Briefly described|p2|||||||||
25946|Henschke Breccia|45112|5|Briefly described|Table 4|||||||||
25946|Henschke Breccia|48942|2|Defined|p18|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25946|Henschke Breccia|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1860Ma. Of Finniss River Group. Max. thickness 2000m. Massive breccia conglomerate, passing upwards into well bedded pebbly arenite with a phyllite band 120m thick. Unconformaby overlies Hermit Creek Metamoprhics.||||||07-JAN-09
25946|Henschke Breccia|69420|5|Briefly described|p5:6-7, 13|Paleoproterozoic|Paleoproterozoic|Litchfield Block [now Domain]; as in Needham and Stuart-Smith, 1984. Crops out near the western margins of the Central Domain, Pine Creek Orogen. Regarded as basal Burrell Creek Formation by Pietsch and Edgoose (1988). c.1500m thick. Talus breccia.||Finniss River Group.|||Polymict conglomerate, breccia and sandstone.|12-JUL-16
25946|Henschke Breccia|69435|6|Mentioned|p20:3|||||||Is overlain unconformably by Moyle River Formation.||12-JUL-16
25946|Henschke Breccia|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary rock, conglomerate, breccia|
26611|Henwood Creek Volcanic Member|22536|5|Briefly described|p9|Proterozoic|Proterozoic|Of Katherine River Group.||||||26-SEP-06
26611|Henwood Creek Volcanic Member|22538|6|Mentioned|Fig3 P708|||||||||
26611|Henwood Creek Volcanic Member|22574|5|Briefly described|map|Proterozoic|Proterozoic|Of the Katherine River Group.||||||26-SEP-06
26611|Henwood Creek Volcanic Member|23216|5|Briefly described|Table1p9,20,22|||||||||
26611|Henwood Creek Volcanic Member|23374|6|Mentioned|p41,42,43||Statherian|Equivalent to Gilruth Volcanic Member. of Kombolgie Subgroup. In the McArthur Basin.||||||26-SEP-06
26611|Henwood Creek Volcanic Member|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
26611|Henwood Creek Volcanic Member|23867|5|Briefly described|Fig. 3|||Superseded.  Of the Kombolgie Formation.  Geological Province: McArthur Basin.||||||26-SEP-06
26611|Henwood Creek Volcanic Member|24432|5|Briefly described|p562 Fig.2|||Of Katherine River Group. Geological Province: Northern McArthur Basin.||||||
26611|Henwood Creek Volcanic Member|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26611|Henwood Creek Volcanic Member|40248|6|Mentioned|p226|||||||||
26611|Henwood Creek Volcanic Member|41294|6|Mentioned|Map legend|Mesoproterozoic||||||||
26611|Henwood Creek Volcanic Member|41295|4|Described|p18|||||||||
26611|Henwood Creek Volcanic Member|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
26611|Henwood Creek Volcanic Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Kombolgie Formation. Of Statherian age.||||||07-NOV-08
26611|Henwood Creek Volcanic Member|43832|5|Briefly described|28, Table7 p26||Mesoproterozoic|Now known to be Palaeoproterozoic in age||||||
26611|Henwood Creek Volcanic Member|44201|14|Not recorded|p.8|||||||||
26611|Henwood Creek Volcanic Member|45022|14|Not recorded|p.64||Carpentarian|Of Kombolgie Formation.||||||
26611|Henwood Creek Volcanic Member|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
26611|Henwood Creek Volcanic Member|47049|6|Mentioned|p237|||||||||
26611|Henwood Creek Volcanic Member|48867|14|Not recorded|p.6,18|||Map. Part of Kombolgie Formation, "altered andesite and basalt." Katherine-Darwin area.||||||26-SEP-06
26611|Henwood Creek Volcanic Member|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1750-1800Ma. McArthur Basin. Of Gumarrirnbang Sandstone, Katherine River Group. Max thickness 10m. Massive to vesicular mafic volcanics.||||||07-JAN-09
26611|Henwood Creek Volcanic Member|64817|6|Mentioned|p353 Fig.4, |||||Of the Kombolgie Subgroup.||||
26611|Henwood Creek Volcanic Member|67564|6|Mentioned|p39 Fig.20.|||In Roberts and Plumb (1965). ||Unit in (superseded) Kombolgie Formation.||||
26611|Henwood Creek Volcanic Member|67779|5|Briefly described|p32.|||Equivalent to Gilruth Volcanic Member.||Unit in Kombolgie Subgroup.||||
26611|Henwood Creek Volcanic Member|69430|6|Mentioned|p15:3|||NW McArthur Basin.||Gumarrirnbang Sandstone.||||12-JUL-16
26611|Henwood Creek Volcanic Member|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Marlgowa Sandstone, overlies Gumarrirnbang Sandstone||
27432|Hibernia 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
27432|Hibernia Formation|13194|4|Described|p383 Tb. 4-16, p396 fig 4-60|Cenozoic|Cenozoic|Up to 1300m thick. Thickest in Vulcan Graben and Ashmore Platform.||||Overlain by Cartier Formation (disconformably). Overlies Bathurst Island Group.|Limestone, sandstone; minor shale and marl.|
27432|Hibernia Formation|13224|6|Mentioned|p485 fig 3|Oligocene|Paleocene|||||||
27432|Hibernia Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Eocene|Of the Woodbine Group.||||||26-SEP-06
27432|Hibernia Formation|23377|6|Mentioned|p212 Fig.5||Eocene|Of Vulcan Sub-basin.||||||26-SEP-06
27432|Hibernia Formation|24171|5|Briefly described|p722 Fig. 3|Tertiary|Tertiary|Geological Province : Vulcan Sub-Basin||||||01-MAR-10
27432|Hibernia Formation|24218|5|Briefly described|p850|Eocene|Eocene|Geological Province: Bonaparte Basin.||||||
27432|Hibernia Formation|41437|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|41532|4|Described|p308|||Mention Fig.15.||||||26-SEP-06
27432|Hibernia Formation|41690|6|Mentioned|p6|||||||||
27432|Hibernia Formation|41733|6|Mentioned|Fig.3|||||||||
27432|Hibernia Formation|42034|4|Described|Fig.4 P11|||||||||
27432|Hibernia Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
27432|Hibernia Formation|42057|6|Mentioned|Fig.3 P70|||||||||
27432|Hibernia Formation|42066|5|Briefly described|Fig.3 P199|||||||||01-MAR-10
27432|Hibernia Formation|42081|5|Briefly described|Fig.2 P291|||||||||
27432|Hibernia Formation|42151|6|Mentioned|Fig.3 P57|||||||||
27432|Hibernia Formation|42442|3|Fully described|p30|Eocene|Paleocene|||||||
27432|Hibernia Formation|43699|6|Mentioned|Fig.6,p10|Eocene|Paleocene|||||||
27432|Hibernia Formation|43707|5|Briefly described|Fig.3,p4-5||Tertiary|||||||
27432|Hibernia Formation|43739|6|Mentioned|Fig.5,p38|Oligocene|Paleocene|||||||
27432|Hibernia Formation|49637|5|Briefly described|Fig. 3|Eocene|Paleocene|Includes the Grebe Sandstone Member. Geological Province: Vulcan Sub-basin.||||||07-FEB-11
27432|Hibernia Formation|60634|6|Mentioned|p1168 Fig.3. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|61155|5|Briefly described|p15, p16|Early Oligocene||See also Hibernia Formation. Age: >32.5Ma. Max. thickness: 1200m in Sahul Platform region. Geological Province: Bonaparte Basin / Ashmore and Sahul Platforms, Vulcan and Petrel Sub-basins; and Money Shoal Basin - north. ||||||
27432|Hibernia Formation|61548|6|Mentioned|p480 Fig.3|Eocene|Eocene|Northern Bonaparte Basin.||||||
27432|Hibernia Formation|61550|6|Mentioned|p495 Fig.2. |Eocene|Eocene|||Unit in Woodbine Group.||Overlies Grebe Formation. Is overlain by Prion Formation.||
27432|Hibernia Formation|62837|5|Briefly described|Stratigraphic columns|Eocene|Eocene|Age: ~50-~42Ma. Geological Province: Western Bonaparte Basin and Northern Bonaparte Basin.||||||22-JAN-07
27432|Hibernia Formation|64695|5|Briefly described|p260, p261 Fig.6, p262 Fig.8|Eocene|Eocene|Northern Bonaparte Basin.||||Overlies Grebe Formation. Is overlain by Prion Formation, and unconformably by Oliver Formation.||
27432|Hibernia Formation|64697|5|Briefly described|p84 Fig.2 |Eocene|Eocene|||||||
27432|Hibernia Formation|65680|6|Mentioned|p709 Fig.2.|Priabonian|Lutetian||||Includes Grebe Sandstone Member.|Overlies Johnson Formation. Is unconformably overlain by Cartier Formation and Oliver Sandstone Member.||
27432|Hibernia Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Eocene|Paleocene|Unit in the Woodbine Group. Underlies the Prion Formation, overlies the Grebe Formation. Mount Ashmore Dome. Limestone dominated with claystone at the base.||||||
27432|Hibernia Formation|68223|6|Mentioned|p178 Fig.3, p179 Fig.4|Eocene|Eocene|||||||
27432|Hibernia Formation|69452|5|Briefly described|p36:15, 22|Paleogene|Paleogene|Bonaparte Basin.||Woodbine Group.|Grebe Sandstone Member.|||12-JUL-16
27432|Hibernia Formation|69673|6|Mentioned|p174|||||||||
27432|Hibernia Formation|70061|5|Briefly described|Regional geology Figs.6-7, p12|Eocene|Eocene|See also Sahul: Fig.2. Vulcan: Fig.2.||Woodbine Group.|Grebe Sandstone Member.|Overlies Johnson Formation. Is overlain by Prion Formation.||12-JUL-16
24310|Hill of Leaders Granite|23809|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic|Age: 1848+/-7Ma.  Intrudes the Davenport Dacite.||||||07-NOV-08
24310|Hill of Leaders Granite|24172|6|Mentioned|p38|||On BONNEY WELL sheet area.||||||26-SEP-06
24310|Hill of Leaders Granite|24197|5|Briefly described|p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of the Tennant Creek Supersuite. Age: ~1850Ma. Geological Province: Tennant Creek/Davenport Province.||||||07-FEB-11
24310|Hill of Leaders Granite|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Porphyritic muscovite-biotite and biotite granite; minor even-grained granite; commonly xenolithic.  Intrudes the Warramunga Group.||||||10-JAN-05
24310|Hill of Leaders Granite|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24310|Hill of Leaders Granite|41204|4|Described|p11|||||||||
24310|Hill of Leaders Granite|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Porphyritic muscovite-biotite granite.||||||16-NOV-05
24310|Hill of Leaders Granite|41310|5|Briefly described|p13|||||||||
24310|Hill of Leaders Granite|41408|6|Mentioned|Map legend|Proterozoic||||||||
24310|Hill of Leaders Granite|42770|6|Mentioned|Fig.14|||||||||
24310|Hill of Leaders Granite|43568|6|Mentioned|Fig.4,p506|||||||||
24310|Hill of Leaders Granite|43802|6|Mentioned|p78|||||||||
24310|Hill of Leaders Granite|45167|3|Fully described|Table 2, P45|||Age of 1400 Ma.||||||26-SEP-06
24310|Hill of Leaders Granite|49033|2|Defined|p32|Proterozoic|Proterozoic|||||||
24310|Hill of Leaders 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: 1848 +/- 7Ma (SHRIMP).||||||03-OCT-19
24310|Hill of Leaders Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of theTennant Creek Supersuite. Granite: biotite and biotite-muscovite-bearing; porphyritic; xenolithic. In the Tennant Creek region.||||||14-APR-15
24310|Hill of Leaders Granite|64730|6|Mentioned|p141|Paleoproterozoic|Paleoproterozoic|Undeformed. Age is the minimum age of deformation & metamorphism during Tennant Event (Maidment et al. 2006).|1846 +/- 3 Ma.|||May intrude Warramunga Formation?||03-MAY-12
24310|Hill of Leaders Granite|64738|6|Mentioned|p259|Statherian||Northern Davenport Region/Tennant Region.|Intruded by 1711.3 +/-2.2 Ma lamprophyre dyke|||||23-APR-12
24310|Hill of Leaders Granite|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Tennant Creek Supersuite||||
24310|Hill of Leaders Granite|65222|5|Briefly described|p109||||1400 Ma K/Ar.|||||
24310|Hill of Leaders Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tennant Creek Supersuite.|||Granite; biotite- and biotite-muscovite-bearing; porphyritic; xenolithic.|
24310|Hill of Leaders Granite|69187|4|Described|p51, p53 Fig.2, p58 Fig.11, p59-60|Orosirian|Orosirian|Warramunga Province. Geochron sample location shown in Fig.2. Zircon cores ages tend to cluster at 1860-1850 Ma, but no discrete group to calculate a weighted mean age. Rim analyses have more restricted range and their pooled age is taken as the crystallisation age of this granite.|crystal'n 1845.5+/-2.4 Ma SHRIMP Pb/Pb zircon rims|Tennant Creek Supersuite||intrudes Woodenjerrie beds; is unconformably overlain by Epenarra Volcanics|coarse-grained, biotite-bearing, with K-feldspar phenocrysts up to 5 cm long in a finer-grained quartz-plagioclase-K-feldspar matrix; contains xenoliths of metasedimentary rock|
24310|Hill of Leaders Granite|69418|6|Mentioned|p3:21|||Tennant Region. Hosts the Mosquito Creek field W vein deposit (briefly described).||||||12-JUL-16
24310|Hill of Leaders Granite|69424|4|Described|p9:3, 10-14, 28-29, 55-56|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Extensive outcrops E of Murchison Ranges. Immediately post-tectonic: contains xenoliths of deformed metasedimentary rocks of the host Woodenjerrie beds and/or Junalki Formation. Hosts Au-bearing quartz veins, and tungsten mineralisation in the Mosquito Creek tungsten field.|1846 +/- 3 Ma (Maidment et al., 2006).|Tennant Creek Supersuite.||Intrudes Junalki Formation and Woodenjerrie beds. Is intruded by a Devils Suite un-named granophyre.|Grey, alkali-feldspar megacrystic and minor equigranular two-mica and biotite granite; blue opalescent quartz; minor aplite and greisen; weakly foliated.|12-JUL-16
24310|Hill of Leaders Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1846+/-2.4 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
24310|Hill of Leaders Granite|72379|5|Briefly described|iii,p10-14|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Hosts tungsten mineralisation at the Hill of Leaders deposit, Mosquito Creek tungsten field. Maidment et al (2006) reported SHRIMP U-Pb zircon age of 1846+\-3 Ma, interpreted as a maximum age of tungsten mineralisation. Shows evidence of gresenisation, which may relate to exsolving of late-stage evolved fluids as it crystallised, suggesting tungsten mineralisation occurred syn-emplacement (Donnellan 2013), or tungsten mineralisation may be associated with a poorly or non-exposed younger granite intrusion that exsolved ore-forming fluids that infiltrated pre-existing granite. Sample BW18MVM003 (molybdenite-scheelite-bearing mineralised quartz vein) returned ID-NTIMS molybdenite Re-Os model ages of c. 6713 and 4940 Ma, which are geologically impossible, irreproducible and subsequently discarded. Sample BW18MVM006 (molybdenite-scheelite-bearing mineralised quartz vein) returned ID-NTIMS molybdenite Re-Os model age of 1777+\-9 Ma, which may record timing of tungsten mineralisation associated with a period of felsic magmatism not recognised at the North Curtis prospect in the Mosquito Creek tungsten field.|||||Porphyritic plagioclase, muscovite-biotite granite.|03-OCT-19
24310|Hill of Leaders Granite|72380|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces. Felsic magmatism, possibly associated with tungsten mineralisation at the Mosquito Creek and Wauchope tungsten fields.||||||
24310|Hill of Leaders Granite|73124|6|Mentioned|p2 Fig.1|||||Tennant Creek Supersuite||||
24310|Hill of Leaders Granite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Tennant Creek Supersuite.||||
24310|Hill of Leaders Granite|73460|6|Mentioned|p2|||Warramunga Province.||Tennant Creek Supersuite||||
24310|Hill of Leaders Granite|73550|6|Mentioned|p25|||||||||
24310|Hill of Leaders Granite|73590|6|Mentioned|p2|||||Tennant Creek Supersuite||||
39149|Hinde Dolostone|14019|5|Briefly described|p4 Fig. 3|||Of the Tolmer Group.  ||||||
39149|Hinde Dolostone|24122|5|Briefly described|p4 Fig.3|||Of Tolmer Group.  Geological Province: Birrindudu Basin.||||||
39149|Hinde Dolostone|24441|5|Briefly described|p1 Fig. 1|||Of the Tolmer Group. Overlies Stray Creek Sandstone; unconformably overlain by Stirling Sandstone. Geological Province: Birrindudu Basin.||||||25-JAN-06
39149|Hinde Dolostone|24442|5|Briefly described|p50 Fig. 1|||Of the Tolmer Group.  Geological Province: Birrindudu Basin.||||||
39149|Hinde Dolostone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Tolmer Group.||Overlies Stray Creek Sandstone. Is unconformably overlain by Stirling Sandstone of the Limbunya Group.||
39149|Hinde Dolostone|67167|5|Briefly described|Map legend.|||||Unit in Tolmer Group.|||Dolostone, stromatolitic dolostone, dolomitic quartz sandstone, dolomitic shale.|
39149|Hinde Dolostone|67186|5|Briefly described|Map legend.|||||Unit in Tolmer Group.||Overlies Stray Creek Sandstone.|Dolostone, stromatolitic dolostone, dolomitic quartz sandstone, dolomitic shale.|23-NOV-11
39149|Hinde Dolostone|67269|6|Mentioned|p20-21 Fig.19|||Birrindudu Basin. Contains un-named stromatolites with an axial zone; photograph shown to demonstrate the continuity of such zones through geological time, and to support the biogenic origin of stromatolitic structures in Strelley Pool Formation (East Pilbara Terrane).||Tolmer Group.||||
39149|Hinde Dolostone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||Unit in Tolmer Group.||||
39149|Hinde Dolostone|68280|6|Mentioned|p26 fig 24|||Birrindudu Basin.||Tolmer Group||||
39149|Hinde Dolostone|69432|4|Described|p17:2, 5-6, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Typically over 120m thick. A complete section in stratigraphic drillhole NTGS 82/68 is at least 315m thick, and contains c.85m of weakly Pb-Zn mineralised carbonaceous, glauconitic dolomitic siltstone which crops out poorly. May have potential for Mississippi Valley-style base-metal deposits.||Tolmer Group.||Conformably overlies Stray Creek Sandstone. Is overlain by Waterbag Creek Formation conformably, and by Uniya Formation.|Pink and grey, variably stromatolitic dolostone interbedded with quartzarenite, minor dolomitic siltstone, glauconitic siltstone and shale. Contains columnar, conical and hemispherical stromatolitic bioherms and biostromes.|12-JUL-16
39149|Hinde Dolostone|69442|6|Mentioned|p27:3 Tb.27.1; 5|||||||Is overlain unconformably by Uniya Formation.||12-JUL-16
39149|Hinde Dolostone|69673|6|Mentioned|p48 fig 35|||||Tolmer Group||Unconformably overlain by Stirling Sandstone, overlies Stray Creek Sandstone||
39149|Hinde Dolostone|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Tolmer Group.||Conformably overlies Stray Sandstone. Is overlain conformably by Waterbag Creek Sandstone.|Dolostone and minor limestone, stromatolitic dolostone, dolomitic quartz sandstone and siltstone.|
39149|Hinde Dolostone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Tolmer Group.||||
26614|Hindrance Creek Sandstone|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Edith River Group.  Fine to coarse pink-grey moderately sorted volcanolithic feldspathic quartz sandstone and arkose, rare rounded quartz pebbles; conglomerate, recrystallised to quartzite near Grace Creek Granite contact.||||||01-NOV-04
26614|Hindrance Creek Sandstone|23216|5|Briefly described|Table1p10,13||Paleoproterozoic|||||||07-NOV-08
26614|Hindrance Creek Sandstone|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985).||||||
26614|Hindrance Creek Sandstone|23733|5|Briefly described|p32 Fig. 19|||||||||
26614|Hindrance Creek Sandstone|23867|5|Briefly described|Fig.3|||Of Edith River Group. Formerly Hindrance Creek Member (Edith River Volcanics). Geological Province: McArthur Basin.||||||
26614|Hindrance Creek Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26614|Hindrance Creek Sandstone|40248|4|Described|p225|||||||||
26614|Hindrance Creek Sandstone|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Edith River Group. Of Orosirian age.||||||07-NOV-08
26614|Hindrance Creek Sandstone|43187|5|Briefly described|p2|||||||||
26614|Hindrance Creek Sandstone|46658|6|Mentioned|p557|||||||||
26614|Hindrance Creek Sandstone|47049|5|Briefly described|Table|||Elevation to formations status from member status - placed in Edith River Group.||||||26-SEP-06
26614|Hindrance Creek Sandstone|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1825-1829Ma. Of Edith River Group. Max. thickness 350m. Purple to brown, thickly bedded to massive, coarse to pebbly lithic quartz sandstone with massive interbeds of polymictic pebble to boulder conglomerate; minor planar-laminated siltstone.||||||07-JAN-09
26614|Hindrance Creek Sandstone|64730|5|Briefly described|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age from age of Plum Tree Creek Volcanics, at the top of the Group.|Min. deposition age 1825 +/- 4 Ma (Page 1996).|Of Edith River Group.||||02-MAY-12
26614|Hindrance Creek Sandstone|65232|6|Mentioned|App. 2|||||||||09-FEB-10
26614|Hindrance Creek Sandstone|67564|5|Briefly described|p39 Fig.20.|Paleoproterozoic|Paleoproterozoic|In Needham and Stuart-Smith (1985); formerly Hindrance Creek Member (Roberts and Plumb 1965). Is correlated with Kurrundie Sandstone. Has been contact metamorphosed by the Grace Creek Granite.||Unit in Edith River Group.||||
26614|Hindrance Creek Sandstone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Basal unit in Edith River Group.||||
26614|Hindrance Creek Sandstone|69420|5|Briefly described|p5:4, 15|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Edith River Group.||Unconformably overlies Tollis Formation. Is overlain by Kurrundie Sandstone and (conformably or faulted against) Plum Tree Creek Volcanics.|Medium- to coarse-grained, poorly sorted, pebbly quartz sandstone and arkose.|12-JUL-16
23654|Hot Spring Member|22538|6|Mentioned|Fig3 P709|||||||||
23654|Hot Spring Member|22664|5|Briefly described|Fig. 2 p34|Paleoproterozoic|Paleoproterozoic|Geol province McArthur Basin. Parent Lynott Formation||||||07-NOV-08
23654|Hot Spring Member|22853|4|Described|22|Proterozoic|Proterozoic|Parent Lynott Formation. Max thickness 350 m. Overlying unit Donnegan Member, underlying unit Caranbirini Member||||||
23654|Hot Spring Member|23396|5|Briefly described|p413|Statherian|Statherian|1636+/-4Ma||||||
23654|Hot Spring Member|23776|5|Briefly described|p705 Fig 2.|||Possibly of the Lynott Formation. Of Batten Subgroup.||||||
23654|Hot Spring Member|23902|4|Described|p1568 Fig.2|||Of the Lynott Formation (Batten Subgroup). Overlies the Carabirini Member. Overlain by the Donnegan Member. Geological Province: McArthur Basin||||||
23654|Hot Spring Member|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Lynott Formation||||||
23654|Hot Spring Member|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|Correct spelling, not Hot Springs as reserved.||||||
23654|Hot Spring Member|40691|6|Mentioned|Fig.4|||||||||
23654|Hot Spring Member|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
23654|Hot Spring Member|41268|5|Briefly described|Fig.3|||||||||
23654|Hot Spring Member|42385|4|Described|p22|||See also Table 4 p16.||||||18-SEP-07
23654|Hot Spring Member|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
23654|Hot Spring Member|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Lynott Formation.||In schematic section, underlies Donnegan Member and overlies Caranbirini Member (both of Lynott Formation).|Dolomitic siltstone; silty dololutite with sandstone, chertified stromatolitc dolostone, dolarenite, sandy dolarenite and dolomitic sandstone. Detailed lithology given.|09-NOV-11
23654|Hot Spring Member|42639|4|Described|p32, Table 5 p20|||||||||
23654|Hot Spring Member|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
23654|Hot Spring Member|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Lynott Formation. Thin bedded dolomitic mudstone, dololutite and muddy dololutite with interbeds of fine to coarse grained sandstone.||||||19-OCT-05
23654|Hot Spring Member|42812|4|Described|p41, Table 4|||of Lynott Formation||||||
23654|Hot Spring Member|42935|6|Mentioned|p529 Fig.2|||of Lynott Formation||||||
23654|Hot Spring Member|43010|6|Mentioned|p128|||||||||
23654|Hot Spring Member|43036|5|Briefly described|p54|||of Lynott Formation||||||
23654|Hot Spring Member|45162|4|Described|p113|||||||||
23654|Hot Spring Member|60483|5|Briefly described|p7 Fig. 5|||Of Lynott Formation (Batten Subgroup, McArthur Group). Age: 1636+/-4Ma. Geological Province: McArthur Basin.||||||05-OCT-07
23654|Hot Spring Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Lynott Formation.||||||03-JUN-09
23654|Hot Spring Member|64815|6|Mentioned|p4 Fig.2 |||||Unit in Lynott Formation.||||
23654|Hot Spring Member|64817|6|Mentioned|p353 Fig.4 |||||Unit in Lynott Formation.||||
23654|Hot Spring Member|65228|6|Mentioned|Figs.02, 22.|||Appears (inevitably) as Hot Springs Member, in Fig.22.||Middle unit in Lynott Formation.||Overlies Caranbirini Member. Is overlain by Donnegan Member.||
23654|Hot Spring Member|69430|4|Described|p15:3, 16, 19, 22|Statherian|Statherian|Jackson et al. (1987). Southern McArthur Basin. 50-350m thick. Intertidal to supratidal flats sediments with sporadic brine logging. Sedimentary features include ripples and cross-beds in sandstone, mainly stratiform and domical stromatolites, common dessication cracks, tepee structures and pseudomorphs after sulfate evaporites and halite. Correlated with Conway Formation: many lithological similarities. Appears as Hot Springs Member on 15:22.|1636 +/- 4 Ma.|Lynott Formation.||Conformably and gradationally overlies Caranbirini Member. Is overlain conformably and gradationally by Donnegan Member.|Thinly bedded dolomitic siltstone and silty dololutite with interbeds of fine-grained sandstone, chertified stromatolitic dolostone, dolarenite, sandy dolarenite and dolomitic sandstone; siltstone and dololutite commonly contain chert pods.|12-JUL-16
23654|Hot Spring Member|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone. Potential source rock.||Lynott Formation||Overlain by Donnegan Member||
23654|Hot Spring Member|71374|5|Briefly described|p9|||McArthur Basin. Age is from GA 95779073, Geochron Delivery and derived from an interbedded tuff in this formation.|1636 +/- 4 Ma (SHRIMP U-Pb)|||Overlain by the Yalco Formation.||
23654|Hot Spring Member|72248|5|Briefly described|p147|||Of McArthur Basin.||Unit of Lynott Formation.||||
23654|Hot Spring Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Lynott Formation, Batten Sub-group, McArthur Group||Overlain by Donnegan Member. Underlain by Caranbirini Member.||
23654|Hot Spring Member|73412|5|Briefly described|p12|||Southern McArthur Basin. Has a marked decrease in density (1.91-2.23 g cm-3) and increased kaolinite and Fe-oxides, suggesting a zone of deep weathering.||Lynott Formation.||||
79309|Howard Sand member|69456|5|Briefly described|p40:4, 7, 13|Early Cretaceous|Early Cretaceous|Doyle (2001). Stated to be informally named. Shallow-marine, neritic environment. 2-26m thick. Unconformably overlies Proterozoic rocks of the Pine Creek Orogen. Source of large amounts of coarse and fine washed sand for the construction industry and concrete aggregate.||Of Darwin Formation.|||Deconsolidated, clean to clayey, medium- to coarse-grained quartz sandstone lenses.|12-JUL-16
79082|Huckitta Bore Granite|69383|5|Briefly described|p4 Table 1|Statherian|Statherian|Informal name? Arunta region, Aileron Province.  LA-ICPMS  U-Pb and Hf geochronology analyses. Crystallisation age. IC07JAW133. This sample shown as 'unnamed granite' from the Huckitta Bore boudin p55-58, so name may be informal. Age gven as 1750+/- 4.5 Ma on pviii for Huckitta Bore boudin.|1756+/-3 Ma||||Hypersthene granite.|
28612|Huckitta Granodiorite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Entia Suite. Age: ~1767Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
28612|Huckitta Granodiorite|34488|5|Briefly described|Table 1|||Archaean. p8.||||||27-SEP-06
28612|Huckitta Granodiorite|39888|6|Mentioned|Fig.7|||||||||
28612|Huckitta Granodiorite|39898|5|Briefly described|Map legend|Proterozoic|Proterozoic|Granitic gneiss, foliated granodiorite, amphibolite. Geological Province: Arunta Block.||||||14-FEB-06
28612|Huckitta Granodiorite|40100|5|Briefly described|p256|||||||||
28612|Huckitta Granodiorite|41967|6|Mentioned|p247|||||||||
28612|Huckitta Granodiorite|44964|14|Not recorded|p.42|||||||||
28612|Huckitta Granodiorite|45041|6|Mentioned|Fig.5|||Precambrian||||||
28612|Huckitta Granodiorite|48880|4|Described|p.10,26,27,Pl.12||Precambrian|Intrudes Harts Range Group.||||||
28612|Huckitta Granodiorite|50369|5|Briefly described|p1.4, 10.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Entia Suite.||||||07-NOV-08
28612|Huckitta Granodiorite|61208|5|Briefly described|p212, p207 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Entia Gneiss Complex. Part of calc-alkaline - trondhjemitic gp of granitoids. Well-layered migmatitic plag-qtz-K-feld-bio-hornblende gneiss. Age: ca.1761.9+/- 3.1Ma. Geol. Prov: eastern Arunta Inlier, Entia Dome.||||||07-NOV-08
28612|Huckitta Granodiorite|64337|5|Briefly described|p374 Fig. 1|Paleoproterozoic|Paleoproterozoic||Age range: c. 1770-1730 Ma granitoids.|||||
28612|Huckitta Granodiorite|64574|5|Briefly described|p706, p715, p716, p718, p704 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1762+/-3Ma. Outcrops within Entia Dome.||||||
28612|Huckitta Granodiorite|68150|5|Briefly described|p10, p11 Tb.3.2|||Maidment et al. (2005) dated a crystallisation age of 1762  +/-  3 Ma, but noted that 7 analyses of high U overgrowths yielded ages ranging from ca. 1720 to ca. 1680 Ma, consistent with metamorphism during Late Strangways Event. SHRIMP ages.|crystallis'n 1762+/-3 Ma; metamorph'm 1720-1680 Ma|||||
28612|Huckitta Granodiorite|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block.|||||Granitic gneiss, foliated granodiorite, and amphibolite.|
28612|Huckitta Granodiorite|69427|5|Briefly described|p12:30, 39|Statherian|Statherian|Foden et al. (1988). Crops out in a megaboudin W of Huckitta Bore, Aileron Province. SHRIMP U-Pb zircon age. Maidment et al. (2005) reported two generations of metamorphic rims on zircons: c.1710 Ma (Strangways Event) and an outer Paleozoic rim.|1762 +/- 3 Ma (Maidment et al., 2005).||||A grey, medium-grained granodiorite intruded by thin planar bodies of coarser biotite-hornblende granodiorite and by later fine- to medium-grained aplites.|12-JUL-16
28612|Huckitta Granodiorite|69917|5|Briefly described|p133|||?informal reference to granodiorite of Huckitta Suite? Names used interchangeably p133.  Zhao and McCulloch (1995) reported that the Huckitta Granodiorite was sourced from a subduction-related magma or from remelting of a previous arc-related magma.||||||
28612|Huckitta Granodiorite|69928|6|Mentioned|p216|||Arunta Inlier. One of the Entia Dome area granitic gneisses (Foden et al., 1988).||Entia Gneiss Complex.||||
28612|Huckitta Granodiorite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1762+/-3.1 Ma (U-Pb zircon SHRIMP)||||Granodiorite.|
79090|Huckitta Suite|69917|5|Briefly described|p133-135, 140, 158|Statherian|Statherian|Eastern Arunta Region, Aileron Province. LA-ICPMS zircon dating, Hf analytical data. Weakly foliated biotite granodiorite sampled. The age reported here is within error of the SHRIMP U-Pb age of 1761+/-3 Ma reported by Maidment et al 2005, and the age of the co-magmatic Inkamulla Granodiorite. It appears that Lionel Suite rocks were previously included in Huckitta Suite (see p140).|1764+/-8Ma|Of Ambulbinya Supersuite.||Interpreted to intrude the 'Entia Gneiss Complex'. Geochemically similar to Aremra Granodiorite, Inkamulla Granodiorite.|Biotite granodiorite.|
79090|Huckitta Suite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1764+/-8 Ma (U-Pb zircon LA-ICPMS).||||Granodiorite.|
36768|Hull Granite Suite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1090-1075Ma.  Includes: Rowley Granophyre, Imbumbunna Granite.||||||09-JUN-04
36768|Hull Granite Suite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes the Walu Granite and Rowley Granophyre.  Age: ~1090-1075Ma.||||||09-JUN-04
36768|Hull Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Walu Granite, Rowley Granophyre and Imbumbunna Granite.  Age: ~1090-1075Ma.||||||
36768|Hull Granite Suite|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Age: 1090-1075Ma. Intruded Mount Harris Basalt; extrusive equivalent is the Puntitjata Rhyolite. Fractionated granites and granophyres.||||||25-JAN-07
36768|Hull Granite Suite|65256|2|Defined|piii, p15-16, p40|Stenian|Stenian|New name: Includes Imbumbunna Granite, Rowley Granophyre, Walu Granite. Ages about 1080 Ma. Texturally variable granites ranging from medium-grained equigranular to coarsely K-feldspar porphyritic. A-type. Crosscut by mafic dykes interpreted to belong to Alcurra dolerite. Correlated with 1071+/-5 Ma Angatja Granite. Intrudes Tjauwata Group.||||||
36768|Hull Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
36768|Hull Granite Suite|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Biotite-muscovite granite, weakly foliated; coarsely porphyritic biotite-muscovite-epidote-garnet granite|
36768|Hull Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1075+/-5 Ma (crystallisation: Pb-Pb evaporation).||||Granite.|
77685|Hyland Bay Subgroup|69452|5|Briefly described|p36:8, 15, 19-20|||Hughes (1978); redefined in Gorter (1998). Petrel Sub-basin, Bonaparte Basin. Up to c.2300m thick collectively.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Is overlain unconformably by Mount Goodwin Subgroup.|Mudstone, siltstone, sandstone and carbonate rocks.|12-JUL-16
77685|Hyland Bay Subgroup|69454|5|Briefly described|p38:4|Changhsingian|Sakmarian|Petrel Sub-basin, Bonaparte Basin.||Kinmore Group.|Fossil Head, Torrens, Pearce, Cape Hay, Dombey, Tern Formations.|Overlies Kulshill Group. Is overlain by Mount Goodwin Subgroup.||12-JUL-16
77685|Hyland Bay Subgroup|69673|5|Briefly described|p153 fig 125, p173|||2300m thick.||Kinmore Group|Includes Torrens Formation, Pearce Formation, Cape Hay Formation, Dombey Formation, Tern Formation||Mudstone, siltstone, sandstone and carbonate rocks.|
77685|Hyland Bay Subgroup|70061|4|Described|Petrel Sub-basin; Figs.2 & 3, p2|Changhsingian|Roadian|See also Regional geology: Figs.6-8, p8-11, p13, p15-16, p19. Vulcan: Fig.2, p2. Hydrocarbon source. Pro-delta, shoreface and open marine sediments. Sealed by thick marine shales of Mount Goodwin Subgroup and Flamingo Group. Units in this Subgroup are now considered primary exploration targets in the central Petrel Sub-basin. Potential gas reservoir in Vulcan Sub-basin. Appears as Hyland Bay Formation on p19.||Kinmore Group.|Torrens, Pearce, Cape Hay, Dombey and Tern Formations.|Overlies Fossil Head Formation. Is overlain by Mount Goodwin Subgroup.|Includes gas-prone shales.|12-JUL-16
77685|Hyland Bay Subgroup|71146|5|Briefly described|p6,  p43 fig 33|Guadalupian|Guadalupian|Bonaparte Basin.||||Overlies the Fossil Head Formation. Overlain by the Mount Goodwin Subgroup.|Mixed sandstone, mudstone, carbonate and coal.|
41844|Ikuntji Metamorphics|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Uwupataka Metamorphic Complex. Biotite-muscovite schist, quartz- muscovite schist, quartzite, rare amphibolite, calc-silicate, tremolite schist and forsterite marble. Age: between 1650-1610Ma.  Geological Province: Haasts Bluff Domain.||||||07-NOV-08
41844|Ikuntji Metamorphics|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Iwupataka Metamorphic Complex. Biotite muscovite schist, quartz muscovite schist, quartzite, rare amphibolite and hornblende-grossular calc-silicate, moderatly magnetic.. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
41844|Ikuntji Metamorphics|61660|5|Briefly described|p3 Fig.2, p4. |Proterozoic|Proterozoic|Haasts Bluff Domain. Crops out south of Belt Range.||Unit in Iwupataka Metamorphic Complex.|||A mid-amphibolite succession of biotite-muscovite schist, quartz-rich metasediments and less common calc-silicate and metapelite.|
41844|Ikuntji Metamorphics|67565|2|Defined|p58-59, p12-13, p29, p34, p48.|Statherian|Statherian|New name, after Ikuntji (Haasts Bluff) Community. Haasts Bluff Domain, Warumpi Province. Previously of undifferentiated Arunta Complex (Ranford, 1969). Type locality 2 km SW of Round Hill. Basement rocks. Lower- to mid-amphibolite facies metasedimentary succession, probably feldspathic arkose interlayered with sandstone, siltstone and minor calcareous sediments. Metamorphic effects are detailed. Correlated with Lizard Schist, Ryans Gap Metamorphics and Chewings Range Quartzite. SHRIMP U-Pb maximum deposition age from detrital zircons. Moderately magnetic; high Th, moderate U and K. Hosts the small but locally high-grade base metal prospect at Ulpuruta (formerly Nickel Hill).|1656 +/- 17 Ma (Cross et al. 2004).|Unit in Iwupataka Metamorphic Complex.||Unconformably overlies Glen Helen Metamorphics. Is intruded by Stuart Pass Dolerite. Is overlain unconformably by Heavitree Quartzite.|Variably feldspathic to quartzose biotite-muscovite schist, psammite, quartzite, quartz-muscovite schist; rare amphibolite, tremolite schist, marble, granite; grades up into massive crystalline quartzite.|01-DEC-15
41844|Ikuntji Metamorphics|68832|4|Described|p35-38, 15, 39, 44|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Maximum deposition age of sampled quartzite from upper part of unit is given.|1656+/-17 Ma|Of Iwupataka Metamorphic Complex.||Quartzite may be equivalent to Chewings Range Quartzite. Relationship with nearby Glen Helen Metamorphics unclear.|Dominated by variably feldspathic to quartzose muscovite-biotite schist, with lesser quartz-muscovite schist, quartzite, amphibolite and calc-silicate rock, grading up into massive quartzite.|
41844|Ikuntji Metamorphics|69428|4|Described|p13:6-7, 15, 18|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Eastern Haasts Bluff Domain, Warumpi Province. Crops out between the Belt Range and the Haasts Bluff Community. The quartzite may be a stratigraphic equivalent of the Chewings Range Quartzite. Has broad lithological affinities with upper Ryans Gap Metamorphics. Metamorphism described. Hosts the Haasts Bluff Cu-Au prospect, and the Ulpuruta and Stokes Yard Pb-Zn(-Cu-Au) prospects. SHRIMP U-Pb detrital zircon maximum depositional age.|1656 +/- 17 Ma (Cross et al., 2005).|Iwupataka Metamorphic Complex.||Correlated with Lizard Schist.|Lower- to mid-amphibolite facies metasedimentary succession: mainly variably feldspathic to quartzic muscovite-biotite schist, with lesser calc-silicate rock, grading up into clean quartzite.|12-JUL-16
41844|Ikuntji Metamorphics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1656+/-17 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
23660|Ilappa Metadolerite|40906|4|Described|p14|||||||||
23660|Ilappa Metadolerite|49036|2|Defined|p8|Mesoproterozoic|Paleoproterozoic|Early to Mid-Proterozoic. Previously mapped as Arunta Complex.E - M||||||07-NOV-08
23660|Ilappa Metadolerite|69427|5|Briefly described|p12:46|||Shaw et al. (1984). Jinka Domain, Aileron Province.||||Intrudes Cackleberry Metamorphics.|Consists of two N-trending dykes containing lath-like cummingtonite in a groundmass of actinolitic hornblende, with titaniferous biotite and clinozoisite-muscovite intergrowths.|12-JUL-16
41845|Illili Suite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Porphyritic biotite granites. Geological Province: Warumpi Province.||||||07-NOV-08
41845|Illili Suite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Gunbarrel and Ehrenberg Granites and some undifferentiated rocks.  In the Arunta region.||||||07-NOV-08
41845|Illili Suite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite granite, Highly magnetic. Geological Province: Yaya Domain.||||||07-NOV-08
41845|Illili Suite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province||||||07-NOV-08
41845|Illili Suite|65358|6|Mentioned|p12|||Felsic. Intrudes Yaya Domain, Warumpi Province.||||||
41845|Illili Suite|67565|3|Fully described|p60-61, p18-19, p6 Table 1, p14, p32.|Statherian|Statherian|New name, after Illili Outstation. Yaya Domain, Warumpi Province. Definition intended but neither type nor reference localities for constituent units nominated. Previously included within undifferentiated Arunta Complex and gneissic granite of Ranford (1969). Forms prominent hills. Geochemistry is discussed briefly. Deformed and metamorphosed to granulite facies during the 1640-1635 Ma Liebig and 1590-1560 Ma Chewings Orogenies.|c.1640 Ma.||Includes Gunbarrel, Ehrenberg and Warumpi Granites.|Intrudes Yaya Metamorphic Complex and Waluwiya Suite.|Foliated to gneissic porphyritic biotite granite, less common porphyritic biotite-hornblende granite and equigranular biotite granite; K-feldspar phenocrysts commonly large and rounded with locally preserved rapakivi textures.|01-DEC-15
41845|Illili Suite|68832|5|Briefly described|p7, 10||||||Includes Warumpi Granite.|||
41845|Illili Suite|69417|6|Mentioned|p2:5|Statherian|Statherian|Yaya Domain, Warumpi Province.||||||12-JUL-16
41845|Illili Suite|69428|5|Briefly described|p13:3, 8, 11|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province. Crops out as prominent hills SE of Papunya, and as scattered exposures throughout the Domain.|1640-1630 Ma.||Warumpi, Ehrenberg and Gunbarrel Granites.||Foliated to gneissic, porphyritic biotite granites; high-K calc-alkaline granites with 70-76% SiO2.|12-JUL-16
41845|Illili Suite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.|||Includes Ehrenberg and Gunbarrel granites.||Locally migmatitic biotite granites.|09-SEP-19
25690|Illoquara Sandstone|23733|6|Mentioned|p9|||See also p34 Fig. 20.||||||
25690|Illoquara Sandstone|23809|5|Briefly described|p27 Fig. 25|||Geological Province: Arunta Province.||||||
25690|Illoquara Sandstone|42643|2|Defined|p49||Paleoproterozoic|Of Wauchope Subgroup, Hatches Creek Group. Reserved. Defn card avail.||||||07-NOV-08
25690|Illoquara Sandstone|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Quartz arenite, feldspathic/lithic arenite, siltstone; locally conglomeratic at base.||||||07-NOV-08
25690|Illoquara Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Upper Wauchope Subgroup (Hatches Creek Group).  Quartz arenite, feldspathic/lithic arenite; minor siltstone and altered mafic lava. In the Tennant Creek region.||||||07-NOV-08
25690|Illoquara Sandstone|65209|5|Briefly described|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Upper Wauchope Subgroup.||Wauchope Subgroup||Correlates with Coulters Sandstone.||05-JAN-17
25690|Illoquara Sandstone|65338|6|Mentioned|p13|||Tennant Region.||Unit in Hatches Creek Group.||||
25690|Illoquara Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Upper.||Shown as disconformably overlying Tinfish Sandstone, Srzeleckie Volcanics.|Quartz arenite, feldspathic/lithic arenite; minor siltstone and altered mafic lava.|09-DEC-14
25690|Illoquara Sandstone|69425|4|Described|p10:3, 10-11, 13, 16-18|Statherian|Statherian|Osborne and Crawford Ranges; this is the major ridge-forming unit in these Ranges. Maximum thickness 1300m. Tight to isoclinally folded. Fluvial or high-energy shallow-marine.||Wauchope Subgroup, upper.||Disconformably overlies Strzeleckie Volcanics and Tinfish Sandstone. Correlated with Coulters Sandstone.|Moderately well-sorted, variably fine- to coarse-grained, medium to thickly bedded, quartz sandstone, feldspathic/lithic sandstone, siltstone; locally conglomeratic at base in SE Osborne Range.|12-JUL-16
25690|Illoquara Sandstone|69431|5|Briefly described|p16:5|||Osborne and Crawford Ranges.||Wauchope Subgroup.||Probably correlated with Coulters Sandstone.||12-JUL-16
42369|Ilpili Dolerite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Within the Yaya Domain, Warumpi Province.  In the Arunta region.||||||07-NOV-08
42369|Ilpili Dolerite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province||||||07-NOV-08
42369|Ilpili Dolerite|67565|5|Briefly described|p24, p62.|Statherian|Statherian|May be the dyke which cuts the Larrie Granodiorite near the summit of Mount Larrie. Doubly mis-spelt as Illpilli Dolerite on p62.|1630-1600 Ma.|||Intrudes Russell Charnockite.|Mafic dykes.|
42369|Ilpili Dolerite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.||||||09-SEP-19
35319|Ilyaralona Granite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Granite Suite.  Geological Province: Musgrave Block.  Age: ~1160Ma.||||||09-JUN-04
35319|Ilyaralona Granite|61154|5|Briefly described|p10, p44 App.|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Suite (Pitjantjatjara Supersuite). Coarsely pophryitic biotite-muscovite granite containing abundant phenocrysts of euhedral pink K-feldspar, quartz and plagioclase in a biotite-, muscovite- and epidote-bearing matrix.||||||
35319|Ilyaralona Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Pottoyu Granite Suite.  Coarsely porphyritic muscovite-biotite granite.  Age: ~1160Ma. Geological Province: Musgrave Block.||||||19-OCT-05
35319|Ilyaralona Granite|65256|2|Defined|piii, p7 Tb.1, p8, p30, p37|Stenian|Stenian|New Name: Of the Pottoyu Granite Suite. Pb-Pb evaporation on zircon age 1163 +/- 4 Ma. Coarsely K-feldspar porphyritic muscovite granite with occasional mafic xenoliths. Type locality 3.5 km N of Ilyaralona Range.||||||
35319|Ilyaralona Granite|69436|5|Briefly described|p21:10|||Close et al. (2003). North side of Ilyaralona Range, Musgrave Province. Kober Pb-Pb zircon evaporation age.|1163 +/- 4 Ma (Close et al., 2003).|Pottoyu Suite.|||Coarsely-porphyritic biotite-muscovite granite, with abundant phenocrysts of euhedral pink K-feldspar, quartz and plagioclase in a biotite-, muscovite- and epidote-bearing matrix.|12-JUL-16
35319|Ilyaralona Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1163+/-8 Ma (crystallisation: Pb-Pb evaporation).||||Granite.|
36767|Imbumbunna Granite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hull Granite Suite.||||||
36767|Imbumbunna Granite|61154|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Of the Hull Suite. Occurs as an isolated outcrop overlain by Dean Quartzite. Characterised by randomly oriented K-feldspar laths, 2-3cms long; contains primary biotite, muscovite and garnet, and seconadry epidote. Geological Province: Musgrave Block.||||||
36767|Imbumbunna Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Hull Granite Suite (~1090-1075Ma). Coarsely porphyritic biotite-muscovite-epidote-garnet granite.||||||27-SEP-06
36767|Imbumbunna Granite|65256|2|Defined|p7 Tb.1, p16, p40, p41 |Stenian|Stenian|New name: Of Hull Granite Suite. Coarsely porphyritic biotite-muscovite-epidote-garnet granite, characteristic euhedral K-feldspar laths. Unconformably underlies Dean Quartzite; correlative of/geochemically similar to Walu Granite and Rowley Granophyre.||||||
36767|Imbumbunna Granite|69436|5|Briefly described|p21:11|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Occurs as an isolated outcrop ENE of Bloods Range.||Hull Suite.||Is overlain by Dean Quartzite.|Relatively undeformed granite; characterised by randomly oriented K-feldspar laths 2-3cm long; contains primary biotite, muscovite and garnet, and secondary epidote.|12-JUL-16
79091|Indiana Igneous Complex|69917|5|Briefly described|p174, 186, 188, 1|Cambrian|Cambrian|Replaces Indiana Walls Granite of Maidment (2005).|522+/-4 Ma SHRIMP|||Intruded by Coggans Gabbro. Age compared with Log Cabin Granite.|Granitic gneiss.|
79091|Indiana Igneous Complex|72516|6|Mentioned|p79|||QUARTZ map sheet area.|519 +/- 9 Ma|||Intrudes the Yambla Gneiss.||17-JUN-21
79091|Indiana Igneous Complex|73591|6|Mentioned|p37|Cambrian|Cambrian|Age of 519 +/- 9 Ma reported by Beyer et al (2013).|519 +/- 9 Ma|||Intrudes Yambla Gneiss.||
83370|Ingwallumum Granite|73086|6|Mentioned|p10|||[See also Ingwallumum granite]. Aileron Province basement. [Possibly see Whelan et al., in prep].||||||
26630|Inindia beds|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
26630|Inindia beds|22560|6|Mentioned|p5|||||||||
26630|Inindia beds|22561|6|Mentioned|p10, Fig 3|Neoproterozoic|Neoproterozoic|||||||
26630|Inindia beds|22566|4|Described|p76|Neoproterozoic|Neoproterozoic|Informally divided into upper and lower Inindia beds.  Stratigraphic relationships described - p76.||||||27-SEP-06
26630|Inindia beds|22649|6|Mentioned|p 150|||||||||
26630|Inindia beds|22763|5|Briefly described|p398|Neoproterozoic|Neoproterozoic|||||||
26630|Inindia beds|22805|6|Mentioned|p464|Neoproterozoic|Neoproterozoic|||||||
26630|Inindia beds|22826|4|Described|p569-570|Neoproterozoic|Neoproterozoic|||||||
26630|Inindia beds|24301|4|Described|p16, p29|Neoproterozoic|Neoproterozoic|Also referred to as Inindia Beds throughout text. Defined by Ranford et al (1996). Can be subdivided into three informal units. Overlain by Winnall beds. Underlain by Bitter Springs Formation. Max. thickness: 2130m. Geological Province: Amadeus Basin||||||
26630|Inindia beds|24302|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Planar and trough cross-bedded, medium- to coarse-grained, grey-brown sandstone; dark brown siltstone, chert, jasper. Geological Province: Amadeus Basin||||||29-SEP-05
26630|Inindia beds|41852|6|Mentioned|p209|||||||||
26630|Inindia beds|42699|5|Briefly described|map legend|Neoproterozoic||||||||
26630|Inindia beds|42940|5|Briefly described|Plate 2|Neoproterozoic|Neoproterozoic|Siltstone, shale, sandstone, chert, dolostone, diamictite.  Geological province: Amadeus Basin.||||||23-JAN-08
26630|Inindia beds|43035|4|Described|p18|||||||||
26630|Inindia beds|43503|6|Mentioned|12-50||Proterozoic|||||||
26630|Inindia beds|45170|6|Mentioned|p9|||||||||
26630|Inindia beds|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Overlies: Pinyinna beds.  Underlies: Winnall beds.||||||31-MAY-04
26630|Inindia beds|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin. Underlie: Winnall beds.  Overlie: Pinyinna beds.||||||09-JUN-04
26630|Inindia beds|60678|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Qtz. sst., medium to coarse, may be massive or well-bedded, often ferruginised, sometimes quartzitic; siltstone, red, yellow or pale, often strongly ferruginised; chert - jasper layers, often structureless, sometimes breccias; conglomerate. Amadeus Basin.||||||04-FEB-05
26630|Inindia beds|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Sandstone, siltstone. Geological Province: Amadeus Basin.||||||
26630|Inindia beds|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Quartz sandstone, medium- to coarse-grained, may be massive or well bedded, often ferruginised, sometimes quartzite; siltstone, red, yellow or pale, often strongly ferruginised; chert and asper layers, breccias, conglomerate.  Geol. Prov: Amadeus Basin.||||||20-OCT-05
26630|Inindia beds|61732|6|Mentioned|p96|||Unconformably overlain by Winnall beds.||||||07-FEB-11
26630|Inindia beds|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin.||||||09-FEB-10
26630|Inindia beds|62379|5|Briefly described|p7 Fig. 2, p28|Late Proterozoic|Late Proterozoic|Geological Province: Amadeus Basin. Sst, sltst, chert and jasper. Thickness: 2130m. Disconforambly overlies Bitter Springs Formation and is overlain by Winnall beds. ||||||
26630|Inindia beds|63562|5|Briefly described|p342|||SW Amadeus Basin.||||Probable correlative of Areyonga and Aralka Formations.|Diamictite, sandstone and shale.|
26630|Inindia beds|64778|6|Mentioned|p13, 27|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
26630|Inindia beds|64809|5|Briefly described|p2, p3 Fig.2 |Proterozoic|Proterozoic|Southern Amadeus Basin. Paralic and possibly continental deposition.||||||
26630|Inindia beds|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Geological province: Amadeus Basin.||||||07-FEB-11
26630|Inindia beds|65256|5|Briefly described|piii, p5, p10, p18|Late Neoproterozoic|Neoproterozoic|Of the Amadeus Basin. Disconformably overlies Pinyinna beds; unconformably underlies Winnall beds. Sandstone dominated. Locally overlain by Larapinta Group. [Formerly Inindia Beds (in Forman 1966)].||||||
26630|Inindia beds|67326|5|Briefly described|p2, p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Unconformably overlies Bitter Springs Formation.||
26630|Inindia beds|67553|6|Mentioned|p72|||Amadeus Basin.||||||
26630|Inindia beds|67856|6|Mentioned|p345 fig 4-34, p337, p338 fig 4-30|Neoproterozoic|Neoproterozoic|||||||
26630|Inindia beds|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
26630|Inindia beds|68270|4|Described|p679,682-683,685,688|Cryogenian|Cryogenian|Amadeus Basin. Type section occurs on the Northern shore of Lake Amadeus; lat. 24'38"S, long. 130'52"E. Crops out in the southern Amadeus Basin. Less than 2200m thick. Lower marine depositional environment, followed by fluvial deposits. Diamictite is present in the lower and uppermost parts of the Inindia beds where it is associated with cross-bedded sandstone. Clasts in diamictite consist of mostly intrabasinal lithologies (quartzite, chert, jasper, siltstone, dolomite and several varieties of metamorphic rocks). Possible sequence boundary beneath thick, cross-bedded, sandstone and interbedded diamictite units in the upper Inindia beds (Lindsay 1989); probably indicating representation of both Sturt and Elatina glacial units. Alternatively upper Inindia beds could also have been reworked from Areyonga Formation. Correlable to Elatina Formation.||||Overlain unconformably by Winnall Beds. Underlain unconformably by Bitter Springs Formation or Pinyanna beds.|Lower: quartz sandstone, siltstone, oolitic chert and some stromatolitic dolomite; Upper: sandstone and diamictite.|03-JUL-19
26630|Inindia beds|68323|6|Mentioned|p4 Fig.2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
26630|Inindia beds|69436|5|Briefly described|p21:4, 18, 20|Neoproterozoic|Neoproterozoic|Amadeus Basin. These rocks were thrust southwards on the Bloods Backthrust Zone to accommodate shortening during the Petermann Orogeny.||||||12-JUL-16
26630|Inindia beds|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Cryogenian|SW Amadeus Basin, Centralian A Superbasin. Supersequence 2-3.||||Is overlain by Arumbera Sandstone.|Diamictite, sandstone and siltstone.|12-JUL-16
26630|Inindia beds|69438|3|Fully described|p23:2-4, 10, 16-18, 20-21, 41-42, 44, 59|Ediacaran|Cryogenian|Ranford et al. (1965). Wells et al. (1970) designated reference areas for the unit as an outcrop 20km N of Curtin Springs for the lower part, and the northern ridges around Mount Conner for the upper part (lithologies described). Amadeus Basin. Up to c.2000m thick. Appears as Inindia Beds on 23:4. Contains the distinctive "clast-supported" stromatolites that occur in the Aralka Formation. Recent work suggests extended deposition and correlation with Boord, Pertatataka, Olympic, Pioneer and Julie Formations. Hosts the Camel Prospect manganese occurrence. One of the most likely oil- and/or gas-prone units in the Basin.||||Disconformably overlies Bitter Springs Formation. Is overlain by Winnall beds and Polly Conglomerate unconformably, and Carnegie Formation conformably. Correlated with Areyonga and Aralka Formations.|Generally thick, but variable unit of sandstone with lesser siltstone, chert and jasper, tillite and dolostone.|12-JUL-16
26630|Inindia beds|69443|5|Briefly described|p28:8, 10|||Amadeus Basin. Correlates with part of the Mopunga Group (Georgina Basin).||||Equivalent to the Aroota Group.||12-JUL-16
26630|Inindia beds|69606|6|Mentioned|p3, p10, p14, p19|||western NT Amadeus Basin. ||||||
26630|Inindia beds|69673|5|Briefly described|p63, p73, p74, p75, p84, p88, p90, p91|||Informal? Thickness of up to 2km. Shaly units may be potential source rocks. Sandstones have potential as reservoir rocks.||||Disconformably overlies Bitter Springs Formation, unconformably overlain by Winnall beds, correlated with Areyonga Formation, Aralka Formation, Boord Formation|Diamictite, sandstone and siltstone. Chert and jasper, tillite and dolostone.|
26630|Inindia beds|70416|5|Briefly described|p64-65|Ediacaran|Cryogenian|Amadeus Basin. In the Mount Conner area, this unit included the Aralka Formation; now obsolete: the stratigraphy has been revised (Edgoose et al., 2015).||||Correlated with units from Wallara Formation to Julie Formation (i.e. equivalent to the obsolete Boord Formation).||
26630|Inindia beds|70839|6|Mentioned|p329|Ediacaran|Neoproterozoic|Of the southern Amadeus Basin.||||Overlain by Winnall Beds. Underlain by Bitter Springs Formation. Equivalent to Julie, Pertatataka, Olympic, Aralka, Areyonga and Wallara formations.||
26630|Inindia beds|71080|6|Mentioned|p30 fig 21|Ediacaran|Tonian|Amadeus basin NT. Shown as equivalent to all of Wallara Formation, Areyonga Formation, Aralka Formation, Olympic Formation, Pertatataka Formation, Julie Formation succession.||||||
26630|Inindia beds|71088|6|Mentioned|p8, p15|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||Correlated with the Carnegie Formation.||
26630|Inindia beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
26630|Inindia beds|71268|5|Briefly described|1m_geologyp12_lut.csv||||||||Quartz sandstone, medium to coarse, may be massive or well bedded, often ferruginised, sometimes quartzitic; siltstone, red, yellow or pale, often strongly ferruginised; chert and jasper layers, often structureless, sometimes breccias.|
26630|Inindia beds|71841|5|Briefly described|p1|Ediacaran|Cryogenian|Of Amadeus Basin.||||Overlain by Pertaoorta Group. Underlain by Bitter Springs Group or Wallara Formation. Grades into Inindia beds.||19-SEP-19
26630|Inindia beds|71842|5|Briefly described|p1-3,9|Cryogenian|Cryogenian|Of Amadeus Basin. Widely distributed across the central, southern, and western Amadeus Basin.||||Overlain by Winnall Beds. Underlain by Bitter Springs Formation. Correlable with Aralka Formation, Areyonga Formation, Julie Formation and Wallara Formation.||08-JAN-20
26630|Inindia beds|72369|5|Briefly described|p10, p15|||Of Amadeus Basin.||||Overlain by Winnall Group.||18-DEC-19
26630|Inindia beds|72374|5|Briefly described|p6|||Of Amadeus Basin.||||Correlatable to Areyonga Formation.||11-OCT-19
26630|Inindia beds|72601|6|Mentioned|p5, p7-8, p14|Cryogenian|Cryogenian|Amadeus Basin. Donnellan and Normington (2017) revised this unit to be variously reassigned to the Aralka Formation, Areyonga Formation and Pioneer Sandstone. Includes potential source rocks.||||Variously evquivalent to Aralka Formation, Areyonga Formation and Pioneer Sandstone.||
26630|Inindia beds|73085|6|Mentioned|p1, p2, p4|Ediacaran|Cryogenian|[Also written as 'Inindia beds']. Partly overlain and equivalent to Winnall Group.||||Unconformably[?] underlain by Wallara Formation. Partly overlain by Arumbera Sandstone. Partly equivalent to Julie, Pertatataka, Olympic, Aralka, and Areyonga formations and Pioneer Sandstone.||
26630|Inindia beds|73086|6|Mentioned|[See comments].|||Amadeus Basin. Central-western NT. Part of Supersequence II and III. Fig. 5 shows the unit is: unconformably underlain by Areyonga Formation; overlain by Arumbera Sandstone; overlain by and equivalent to Winnall Group. Partly overlain, underlain and equivalent to Pertatataka Formation. [Also written as 'Inindia beds']. p: 3, 5, 57, 62, 72, 75, 78, 91, 113, 122, 126, 130, 133, 137, 156, 161, 165.||||Lower portion correlates to Wallara Formation, Areyonga Formation and Aralka Formation. Upper portion correlates to Pertatataka Formation and Julie Formation.||
42375|Ininti Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Foliated porphyritic biotite granite. Age: 1688Ma.  Geological province: Arunta region.||||||07-NOV-08
42375|Ininti Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1688Ma. Foliated porphyritic biotite granite; moderate magnetic intensity. Geological Province: Warumpi Province.||||||15-DEC-08
42375|Ininti Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Foliated porphyritic biotite granite and granitic gneiss.||||||15-DEC-08
42375|Ininti Granite|68077|6|Mentioned|p39|||Western Arunta Orogen.||||||07-SEP-17
42375|Ininti Granite|68994|4|Described|p1, p4, p6-9, p11, p15, p23-24, p26-27|Statherian|Statherian|Warumpi Province. Part of suite of intrusive rocks formed c. 1690-1660 Ma (Meixner et al 2004; Scrimgeour et al. 2005). Sample analysed is a fine-grained, leucocratic metasyenite correlated with Ininti Granite. U-Pb zircon magmatic crystallisation age. Hf analyses provided.|1691 +/- 5 Ma (Kirkland et al. 2009).||||Felsic magmatic rocks. Syenogranitic gneiss. High-K calcalkaline granite. Variably deformed.|13-JAN-17
42375|Ininti Granite|69003|5|Briefly described|p5, p31-32|Paleoproterozoic|Paleoproterozoic|Warumpi Province, West Arunta Orogen. Part of the Argilke Event.|1691 +/- 5 Ma.|||Is overlain by Pollock Hills Formation. Is intruded by Mount Webb Granite.|Strongly foliated metasyenogranite; contains metasedimentary xenoliths.|
42375|Ininti Granite|69031|5|Briefly described|p4, p6 Fig.4, p7, p14, p17-22, p24|Statherian|Statherian|Amongst the oldest rocks in the Warumpi Province, Arunta Orogen. Emplaced during the Argilke Igneous Event. Gravity, magnetic maps. This crystallisation age is identical within error with a NT age of 1688 +/- 8 Ma (Worden et al., 2008).|1691 +/- 5 Ma (Kirkland et al., 2009).|||Intrudes Walungurru Volcanics and Pollock Hills Formation.|A strongly foliated metasyenogranite containing sedimentary xenoliths and pegmatite veins parallel to the foliation.|
42375|Ininti Granite|69417|6|Mentioned|p2:5|Statherian|Statherian|Kintore Domain, Warumpi Province.||||||12-JUL-16
42375|Ininti Granite|69428|5|Briefly described|p13:3, 12|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Forms a number of low isolated outcrops and pavements NW of the Winnecke Hills. SHRIMP U-Pb zircon age. A syenogranite across the WA border, regarded as part of this unit, was similarly dated at 1691 +/- 5 Ma (Kirkland et al., 2009).|1688 +/- 3 Ma (Worden et al., 2006).||||A biotite porphyritic granodiorite; K-feldspar phenocrysts to 2cm, locally tabular and simply-twinned; 10% biotite that defines a well-developed foliation.|12-JUL-16
42375|Ininti Granite|69933|5|Briefly described|v, p1, p17-19, p36|Statherian|Statherian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1688 +/- 5 Ma (SHRIMP U-Pb, magmatic age)||||Biotite porphyritic granite with K-feldspar phenocrysts and biotite defining a well developed foliation.|21-APR-23
42375|Ininti Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Warumpi Province.||||||
42375|Ininti Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42375|Ininti Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1688+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Foliated biotite granite.|
42375|Ininti Granite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1691 Ma.||||Foliated, porphyritic granitic gneiss; may include syenogranitic gneiss with metasedimentary xenoliths.|
42375|Ininti Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Foliated, porphyritic granitic gneiss; may include syenogranitic gneiss with metasedimentary xenoliths.|
42375|Ininti Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain. Geochron Sample No: MR01IRS85. Location: 511889E, 7429825N.|1688 Ma||||Foliated porphyritic biotite granite.|09-SEP-19
42375|Ininti Granite|73058|6|Mentioned|p777|||Arunta Orogen, west.||||||
27437|Inkamulla Granodiorite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Entia Suite. Age: ~1767Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
27437|Inkamulla Granodiorite|34488|5|Briefly described|Table 1|||Archaean||||||
27437|Inkamulla Granodiorite|39888|6|Mentioned|Fig.7|||||||||
27437|Inkamulla Granodiorite|39898|5|Briefly described|Map legend|Proterozoic|Proterozoic|Granodiorite gneiss, granodiorite. Geological Province: Arunta Block.||||||14-FEB-06
27437|Inkamulla Granodiorite|40100|5|Briefly described|p256|||||||||
27437|Inkamulla Granodiorite|44964|14|Not recorded|p.41|||||||||
27437|Inkamulla Granodiorite|45003|14|Not recorded|p81|||See also Lexicon||||||
27437|Inkamulla Granodiorite|45041|6|Mentioned|Fig.5|||Precambrian||||||
27437|Inkamulla Granodiorite|48880|4|Described|p.12||Precambrian|On many pages. p.10,13,26,27,Pl.12. Intrudes Harts Range Group. (F53-15).||||||
27437|Inkamulla Granodiorite|50369|5|Briefly described|p1.4, 10.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Entia Suite.||||||07-NOV-08
27437|Inkamulla Granodiorite|61208|5|Briefly described|p213, p207 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Entia Gneiss Complex. Part of calc-alkaline - trondhjemitic gp of granitoids. Homogeneous coarse-grained (less finer grained phase) qtz-microcline-plag-bio gneiss; minor amphibolite. Age: ca.1763-ca.1751Ma. Geol. Prov: eastern Arunta Inlier, Entia Dome||||||07-NOV-08
27437|Inkamulla Granodiorite|64574|5|Briefly described|p706, p714, p715, p716, p718, p704 Fig.|Paleoproterozoic|Paleoproterozoic|Age: 1773+/-4Ma. Outcrops within Entia Dome.||||||
27437|Inkamulla Granodiorite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
27437|Inkamulla Granodiorite|68517|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Arunta Block.|||||Granodiorite gneiss and granodiorite.|
27437|Inkamulla Granodiorite|69427|5|Briefly described|p12:30|Statherian|Statherian|Maidment et al. (2005); the Inkamulla Granite of Foden et al. (1998).|1773 +/- 4 Ma (Maidment et al., 2005).|||||12-JUL-16
27437|Inkamulla Granodiorite|69917|5|Briefly described|p128-130, 133, 134, 156, 158|Statherian|Statherian|Eastern Arunta Region,  Aileron Province. LA-ICPMS zircon dating, Hf analytical data. Age is slightly younger than the SHRIMP U-Pb zircon age of 1772+/-4.3 Ma for the same unit reported by Maidment et al 2005.|1756+/-8Ma max cryst |Of Ambulbinya Supersuite.||Geochemically similar ot Aremra Granodiorite, Huckitta Suite.|Homogeneous, foliated, medium- to coarse grained hornblende-biotite granodiorite.|
27437|Inkamulla Granodiorite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1773+/-4.3 Ma (U-Pb zircon SHRIMP)||||Granodiorite.|
42097|Inspiration Peak Monzogranite|23809|5|Briefly described|p22, p6 Tb. 3|Paleoproterozoic|Paleoproterozoic|Part of the Frederick Suite.  Pluton surrounded by Dead Bullock Formation.  Age: 1844+/-8Ma. AGSO sample ID 99496223.||||||07-NOV-08
42097|Inspiration Peak Monzogranite|62580|5|Briefly described|p43|||Of the Frederick Suite. Small semi-circular pluton surrounded by metamorphosed Dead Bullock Formation. Consist of undeformed coares- to medium-grained biotite monzogranite.||||||07-FEB-11
42097|Inspiration Peak Monzogranite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1844+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
42097|Inspiration Peak Monzogranite|73089|6|Mentioned|p3, p22, p39|Orosirian|Orosirian|Granites-Tanami Orogen. Two ages from the same 9.3 m interval of a drillcore yielded different ages despite the rock being relatively homogenous.|1844 +/- 4 Ma [and 1802 +/- 14 Ma?]|||Intrudes Dead Bullock Formation.|Monzogranite.|
25958|Inverway Metamorphics|14019|4|Described|p1|||Schist, acid volcanics.  Age: probably 1880-1850Ma.||||||
25958|Inverway Metamorphics|24122|5|Briefly described|p4 Fig.3|||||||||
25958|Inverway Metamorphics|24297|5|Briefly described|p4 Fig.3|||Geological Province: Birrindudu Basin.||||||
25958|Inverway Metamorphics|24441|5|Briefly described|p1 Fig. 1|||Unconformably overlain by the Gardiner Sandstone (Birrindudu Group).||||||
25958|Inverway Metamorphics|24442|6|Mentioned|p50 Fig. 1|||||||||
25958|Inverway Metamorphics|28255|4|Described|p8, Tb. 11 (opp. p8)|||Red-brown, low grade schists consisting of fine-grained matrix containing rounded and angular fragments of quartz and flakes of muscovite.  Unconformably overlain by Limbunya Formation. Age is Archaean or Early Proterozoic. On LIMBUNYA map sheet.||||||
25958|Inverway Metamorphics|32172|5|Briefly described|p6|||L.Proterozoic? Table 1||||||
25958|Inverway Metamorphics|32173|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Red and brown muscovite quartz schist.  Unconformably overlain by the Stirling Sandstone.||||||07-NOV-08
25958|Inverway Metamorphics|33376|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean and/or Lower Proterozoic||||||07-NOV-08
25958|Inverway Metamorphics|33377|5|Briefly described|Table 2|||||||||
25958|Inverway Metamorphics|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25958|Inverway Metamorphics|45112|5|Briefly described|p15|||||||||
25958|Inverway Metamorphics|45140|6|Mentioned|p12-13, Appx.p19|||Victoria River region.||||Is overlain unconformably by the Limbunya Group. Possible correlative of Tanami Complex.||
25958|Inverway Metamorphics|46864|5|Briefly described|p39|||||||||
25958|Inverway Metamorphics|48943|2|Defined|p13|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25958|Inverway Metamorphics|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Muscovite quartz schist, acid volcanics.  Unconformably overlain by the Stirling Sandstone of the Limbunya Group.||||||07-NOV-08
25958|Inverway Metamorphics|60682|6|Mentioned|p3 Fig. 2|||||||||03-MAY-05
25958|Inverway Metamorphics|60685|6|Mentioned|p4 Fig. 3|||||||||
25958|Inverway Metamorphics|65342|6|Mentioned|p11 Fig.13. |||||||Is unconformably overlain by Birrindudu Group.||
25958|Inverway Metamorphics|68733|5|Briefly described|p176-187|Orosirian|Orosirian|Greenschist-facies metamorphic basement to Victoria and Birrindudu Basins. Graded bedding and small-scale tabular crossbedding are typically preserved. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1867 +/- 5 Ma.|||Unconformably overlain by the Stirling Sandstone.|Comprises steeply-dipping, well-bedded, cross-bedded to massive arkosic quartz-muscovite schist with minor metasiltstone and felsic volcanics.|05-DEC-17
25958|Inverway Metamorphics|69429|5|Briefly described|p14:1-2|Paleoproterozoic|Paleoproterozoic|Sweet et al. (1974). Birrindudu Basin. Two small inliers are exposed as small, rounded symmetrical hills. Sub-greenschist to greenschist facies metamorphism. Over 429m thick. Metabasalt and metadolerite dykes were included in this unit by Jones (2009). Absolute age not determined; likely correlative of Tanami and Ware Groups, Tanami Region.||||Is overlain unconformably by Birrindudu and Limbunya Groups.|Muscovite quartz schist, schistose silicic volcanic rocks and minor siltstone; concordant quartz veins are common and form massive quartz reefs 2-4m thick; sericitic and graphitic shale; dolomitic siltstone; quartz-graphite breccia.|12-JUL-16
25958|Inverway Metamorphics|69432|6|Mentioned|p17:2, 5-6|||||||Is overlain unconformably by Stirling Sandstone.||12-JUL-16
25958|Inverway Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||felsic schist|
25958|Inverway Metamorphics|71302|4|Described|p1,3,6-14,72-74|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin. Low-grade metamorphic basement to the Birindudu Basin in Victoria River region. Exposed as two small inliers (<3 km2 in total) on LIMBUNYA 1:250 000 map sheet. Thickness is unknown. Metamorphic grade is sub-greenschist to greenschist facies (Sweet et al., 1974a, b; Cutovinos et al., 2002). Maximum depositional age: 1867+\-5 Ma (Carson, 2013; Munson, 2016 and Munson, in prep). Sample GA 1956880 (quartz-muscovite schist) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1867+\-5 Ma, identical to that of Carson (2013). Almost entirely consists of zircons > 1800 Ma in age; older clusters at c. 1900-2400 and 2500-2550 Ma, which indicates an NAC (e.g. pine Creek orogen, or Kimberley, Tanami, Arunta regions) source. Sample location, description, zircon description, SHRIMP analyses and results are discussed.|||||Steeply dipping, cross-bedded to massive arkosic quartz-muscovite schist with minor metasiltstone and felsic volcanics.|09-DEC-19
25958|Inverway Metamorphics|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1867+/-5 Ma (MDA: Pb/Pb zircon).||||Volcanic rock.|
25958|Inverway Metamorphics|72527|6|Mentioned|p184, p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of correlated units across the Northern Territory with the Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a).||||||
25958|Inverway Metamorphics|73083|6|Mentioned|p31|||||||||
42200|Inyalinga Granulite|61660|4|Described|p4, p11, p15 Fig.6, p23 Table 8.|Proterozoic|Proterozoic|Intruded by voluminous high-K calc-alkaline granite, granodiorite and charnockite and less abundant gabbro. High-grade metamorphosed ca. 1638 Ma.|Maximum deposition age of 1661 +/- 10 Ma.|Unit in Yaya Metamorphic Complex.|||Includes calc-silicates, interlayered pelitic and mafic granulite, massive cordierite-rich metapelite and quartzite.|
42200|Inyalinga Granulite|65272|5|Briefly described|p317, p318 fig 2.,  p321-322.|||Timing of Liebig Orogeny linked to metamorphic zircon rims fom this unit aged 1638 +/- 8 Ma and 1636 +/- 6 Ma (SHRIMP U-Pb; Scrimgeour et al., 2005). 40Ar/39Ar data.||||||
42200|Inyalinga Granulite|67565|2|Defined|p59-60, p14-15, p17, p22, p28, p62.|Statherian|Statherian|New name, after Inyalinga Outstation. Yaya Domain, Warumpi Province. Previously included within undifferentiated Arunta Complex (Ranford, 1969). Type locality 6 km south of Kakalyi Bore. Metamorphic effects are detailed. Age is for granulite; the cordierite pelite has a maximum deposition age of 1661 +/- 10 Ma. Has metamorphic zircon rims aged 1638 +/- 8 Ma (Kinny, 2002). May include rocks of significantly different ages.|Max. deposition age of 1760 +/- 8 Ma.|Unit in Yaya Metamorphic Complex.||Is intruded by Warumpi Granite, Larrie Granodiorite and Papunya Igneous Complex.|Interlayered mafic granulite, garnet-biotite-sillimanite pelite, psammite, rare quartzite; quartzite, calc-silicate rock; massive cordierite pelite, garnet-orthopyroxene-sillimanite granulite, quartzite, rare sapphirine granulite; minor granite.|01-DEC-15
42200|Inyalinga Granulite|68832|5|Briefly described|p7, 10, 12, 13, 21 |Statherian||Includes quartzite informally named 'Papunya quartzite'. Minimum age from unnamed charnockite, which is interpreted to have intruded during high-grade metamorphism in the Liebig Orogeny, 1637.1+/-2.4 Ma. Maximum deposition age and younger metamorphic age given.|1760+/-8 Ma, 1636+/-6 Ma|Of Yaya Metamorphic Complex.||Intruded by Warumpi Granite, an unnamed charnockite, Larrie Granodiorite.||
42200|Inyalinga Granulite|69428|4|Described|p13:7-9, 11-12, 14|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province. A heterogeneous unit of largely metasedimentary granulite-facies rocks: lithologies are described in some detail. SHRIMP U-Pb detrital zircon maximum depositional age.  Metamorphism discussed. High-grade metamorphic rims dated at 1638 +/- 8 Ma (Liebig Orogeny).|1661+/-10 Ma (Kinny 2002, Scrimgeour et al 2005).|Yaya Metamorphic Complex.||Is intruded by Warumpi Granite (Illili Suite) and Waluwiya Suite. Intercalated with Larrie Granodiorite.|Interlayered mafic granulite and metapelitic rock; quartzite and calc-silicate rock; massive cordierite-rich pelitic rock interlayered with calc-silicate and quartzite and intruded by gabbro and charnockite; undivided metasediments.|12-JUL-16
42200|Inyalinga Granulite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen. Metamorphosed at 1638 +/- 8 Ma (U-Pb zircon SHRIMP).|1661+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Cordierite-rich metapelite.|
79074|Irindina Metamorphics|69383|5|Briefly described|p74-79||Neoproterozoic|Arunta Region, Irindina Province.  LA-ICPMS U-Pb and Hf geochronology analyses.  Max deposition age.|882+/-11 Ma||||Quartz-rich metapsammitic rock.|
79074|Irindina Metamorphics|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen.|882+/-11 Ma (MDA: U-Pb zircon LA-ICPMS).||||Metapsammite.|
28048|Ironbark Member|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Plum Tree Volcanics (Edith River Group).  Interbedded greywacke, tuff, cherty tuff; flow-banded glassy pink rhyolite and porphyry; porphyritic microgranite.||||||
28048|Ironbark Member|23216|5|Briefly described|Table1p10,13-4|||||||||
28048|Ironbark Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Edith River Group. Of Orosirian age.||||||07-NOV-08
28048|Ironbark Member|50586|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Of the Jim Jim Suite. Geological Province: Pine Creek Inlier. Age: 1857 +/- 61Ma (U-Pb).||||||07-NOV-08
28048|Ironbark Member|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1825Ma from parent unit - Plum Tree Creek Volcanics, Edith River Group.  Max. thickness 800m. Interbedded greywacke, tuff, cherty tuff; flow-banded rhyolite and porphyry, porphyritic microgranite, banded ironstone and phyllite.||||||07-JAN-09
28048|Ironbark Member|69420|5|Briefly described|p5:18|Paleoproterozoic|Paleoproterozoic|No indication of its parent unit, but listed with constituents of the Jim Jim Suite.|1857 +/- 61 Ma: conventional U-Pb zircon (TIMS).|||||12-JUL-16
24318|Iwupataka Metamorphic Complex|22563|6|Mentioned|p47|||||||||
24318|Iwupataka Metamorphic Complex|37462|5|Briefly described|Tab.4.VIII|||||||||
24318|Iwupataka Metamorphic Complex|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|39887|6|Mentioned|Fig.3|||||||||
24318|Iwupataka Metamorphic Complex|39888|6|Mentioned|Table 1|||||||||
24318|Iwupataka Metamorphic Complex|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Arunta Block.||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|43503|1|Redefined|8,23|||||||||
24318|Iwupataka Metamorphic Complex|48992|2|Defined|p28|Mesoproterozoic|Mesoproterozoic|||||||
24318|Iwupataka Metamorphic Complex|50369|5|Briefly described|p19.1, 22.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier Age: 1615-1600Ma.||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes: Lizard Schist and Ikuntji Metamorphics.  Age: 1650-1610Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1650-1610Ma. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
24318|Iwupataka Metamorphic Complex|61660|4|Described|pp3-4.   |Proterozoic|Proterozoic|Sedimentary protoliths were deposited in the Warumpi Province following high-grade metamorphism of the Madderns Yard Metamorphic Complex. A presumed metavolcanic in this unit has a SHRIMP U-Pb zircon age of 1615 +/- 11 Ma (Zhao and Bennett 1995). This unit is intruded by granites aged 1603 Ma. Lower- to mid-amphibolite facies metamorphism occurred during the Chewings Orogeny (1610 - 1600 Ma).|||Includes Ikuntji Metamorphics.||Lower to middle amphibolite facies cover succession and associated granitic rocks.|
24318|Iwupataka Metamorphic Complex|64722|6|Mentioned|Fig. 2 p3-6,p11|Statherian|Statherian|Deposited between 1630-1600 Ma. Arunta Region.||||||
24318|Iwupataka Metamorphic Complex|65232|5|Briefly described|p72|||High-uranium granitic orthogneiss. With Teapot Granite Complex, provided source rocks for Brewer Conglomerate. Geol. Prov: Amadeus Basin.||||||09-FEB-10
24318|Iwupataka Metamorphic Complex|65272|6|Mentioned|p318 fig 2.|||Haasts Bluff Domain.||||||
24318|Iwupataka Metamorphic Complex|65358|4|Described|p12||Statherian|In Warumpi Province. Overlies Madderns Yard Complex. Lower amphibolite facies. SHRIMP U-Pb date of 1620-1615 Ma (Close et al., 2003) is maximum depositional age.||||||
24318|Iwupataka Metamorphic Complex|66860|6|Mentioned|p6 Tb.1|||Arunta Region. Deposition was coeval with upper parts of Namerinni Group (Tennant Region).||Strangways Metamorphic Complex||||
24318|Iwupataka Metamorphic Complex|67565|4|Described|p4, p5 Fig.3, p7 Table 1, pp11-12, p36.|Paleoproterozoic|Paleoproterozoic|Haasts Bluff Domain, Warumpi Province. A cover succession. A presumed metavolcanic body within this unit has a SHRIMP U-Pb zircon age of 1615 +/- 11 Ma (Zhao and Bennett 1995). Granite intrusions have ages of 1603 +/- 7 Ma and 1603 +/- 11 Ma (Collins et al. 1995; Zhao and Bennett 1995). Age considerations are discussed. Hosts the Ulpuruta (formerly Nickel Hill) and Stokes Yard (Zn-Pb), and Haasts Bluff (Cu-Au), Prospects.|1640 - 1610 Ma.||Includes Lizard Schist and Ikuntji Metamorphics, Rungitjurba Gneiss and Chewings Range Quartzite.|Locally overlies the Madderns Yard Metamorphic Complex.|Amphibolite facies metasedimentary rocks, presumed felsic volcanic rocks and granite.|
24318|Iwupataka Metamorphic Complex|68832|5|Briefly described|p26, 35, 36, 39, 44|||Migmatitic pelite and psammite sampled from drillcore in Stokes Yard base metal prospect may belong to this unit. Depositional age of sample is between 1647 +/- 21 Ma and the 1590 Ma Chewings Orogeny.|1640 - 1610 Ma||Includes Ikuntji Metamorphics, Chewings Range Quartzite and probably Lizard Schist, Nguman Metamorphics.|||
24318|Iwupataka Metamorphic Complex|68994|5|Briefly described|p4|||Haasts Bluff Domain. Phase of sedimentation, 1640-1600 Ma, constrained by youngest detrital zircon component in Iwupataka Metamorphic Complex, and age of volcanic Rungutjirba Gneiss.||||||13-JAN-17
24318|Iwupataka Metamorphic Complex|69221|6|Mentioned|p200-201|Mesoproterozoic|Mesoproterozoic|Basement to Amadeus Basin. Intermediate heat-producing metasediments and orthogneisses (values given).||||||
24318|Iwupataka Metamorphic Complex|69417|6|Mentioned|p2:5|Statherian|Statherian|Haasts Bluff Domain, Warumpi Province.||||||12-JUL-16
24318|Iwupataka Metamorphic Complex|69428|5|Briefly described|p13:1-3, 5-7, 15, 19|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995). Haasts Bluff Domain, Warumpi Province. Cover sequence. Now includes the metasedimentary rocks hosting the Stokes Yard base metal prospect, formerly assigned to the Glen Helen Metamorphics. Age not tightly constrained: Rungutjirba Gneiss is 1615 Ma, and some units have maximum deposition ages of 1670-1650 Ma (similar to Yaya Metamorphic Complex). Hosts the Haasts Bluff Cu(+/- Au) prospect: an IOCG style deposit.|1630-1610 Ma.||Simpsons Gap Metasediments, Rungutjirba Gneiss; Nguman, Ryans Gap, Ikuntji  Metamorphics; Lovely Hill, Lizard Schists; Chewings Range Quartzite.|Unconformably overlies Madderns Yard Metamorphic Complex.||12-JUL-16
24318|Iwupataka Metamorphic Complex|73086|6|Mentioned|p9|||Warumpi Province metamorphic basement. Contains the Chewings Quartzite[?].||||||
30270|Jalboi Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
30270|Jalboi Formation|23404|5|Briefly described|p641|||Of Roper Group.||||||
30270|Jalboi Formation|23937|1|Redefined|p80 Appendix 1, p38|Calymmian|Calymmian|Of the Collara Subgp (Roper Gp).  Supersedes the Jalboi Mbr of the Abner Sst - now upgraded.  Overlain by Hodgson Sst; disconformably overlies the Crawford Fm, and Arnold Sst.when present.  Max.thick: 230m.  Geol.Prov: McArthur Basin.||||||23-DEC-09
30270|Jalboi Formation|24048|4|Described|p70|Mesoproterozoic|Paleoproterozoic|Of the Roper Group.  Geological Province: McArthur Basin.||||||07-NOV-08
30270|Jalboi Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Mudstone and fine to medium-grained sandstone: red-brown, ferruignous, finely micaceous, glauconitic in places, flaggy to thin-bedded, hummocky cross-beds. Geol. Prov: McArthur Basin.||||||13-OCT-05
30270|Jalboi Formation|24050|3|Fully described|p48, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Formerly Jalboi Member (Abner Sandstone).  Now of the Roper Group.  Laminated, micaceous and glauconitic sandstone, mudstone and siltstone.  Overlain by Hodgson Sandstone.  Max. thickness: 100m.||||||28-SEP-06
30270|Jalboi Formation|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Roper Group. Geological Province: McArthur Basin.||||||
30270|Jalboi Formation|24303|5|Briefly described|p61 Appendix|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: McArthur Basin. Correlative of middle part of Powell Formation. See also p24 Tb.4||||||
30270|Jalboi Formation|44112|6|Mentioned|Fig11p30|||||||||
30270|Jalboi Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group.  Thin bedded, fine sandstone and red-brown siltstone: sandstone, structureless to trough cross-stratified, medium- and locally coarse-grained in units up to 2m thick; basal red laminated sltst. Overlies Crawford Fm; underlies Hodgson Fm.||||||15-FEB-05
30270|Jalboi Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Thin bedded fine grained sandstone and red-brown siltstone: flute clasts, synaeresis cracks, toroids.||||||28-SEP-06
30270|Jalboi Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Mudstone and fine to medium-grained sandstone: red-brown, ferruignous, finely micaceous, glauconitic in places, flaggy to thin-bedded, hummocky cross-beds. Geol. Prov: McArthur Basin.||||||
30270|Jalboi Formation|69430|4|Described|p15:3, 27, 29-30|Calymmian|Calymmian|Abbott et al. (2001). Previously the Jalboi Member (of Abner Sandstone in the Roper River region) of Dunn (1963). McArthur Basin. 117-230m thick. Storm-dominated shelf sediments.||Collara Subgroup.||Overlies Showell Member (Mainoru Formation) and Crawford Formation disconformably, and Arnold Sandstone unconformably. Is overlain by Hodgson Sandstone gradationally or locally with erosive contact.|Interbedded fine sandstone and siltstone, alternating with medium to thick beds of medium quartz sandstone.|12-JUL-16
30270|Jalboi Formation|69673|6|Mentioned|p16 fig 13|||Northwestern and Southern McArthur Basin.||Collara Subgroup||Overlain by Hodgson Sandstone, Overlies Arnold Sandstone, Mainoru Formation||
30270|Jalboi Formation|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Storm-dominated shelf (sandstone-dominated).||Of Collara Subgroup.||Overlies Arnold Sandstone. Overlain by Hodgson Sandstone.||
30270|Jalboi Formation|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Arnold Sandstone; overlain by Hodgson Sandstone.|Fluvial and marine sandstones.|
30270|Jalboi Formation|70968|2|Defined|p6, p18, p35, p39-40, p42, p44-48, p50|Calymmian|Calymmian|See also p123, p126, p131, p143. Sweet and Abbott in Abbott et al. (2001) after Dunn (1963). Formerly the Jalboi Member (of Abner Sandstone); raised to Formation rank by Abbott et al. (2001). Named after Jalboi River. The type section is 8km NNW of Mount Chapman, at 408300mE 8392300mN in URAPUNGA sheet. Slightly recessive: forms soil-covered or rubbly zones with low sandstone outcrops, or terraces on hill slopes. Extensive outcrops in McArthur Basin. Lithology described in some detail. 152m thick in the type section; maximum 230m. Lower shoreface to shallow-marine, storm-dominated deposits.||Collara Subgroup.||Overlies Mainoru Formation unconformably, or Crawford Formation and Arnold Sandstone dis- (possibly con-)formably. Is overlain gradationally by Hodgson Sandstone. Is intruded by Derim Derim Dolerite.|Interbedded, mostly fine- to medium-grained sandstone, usually white-weathering; siltstone and mudrocks. Local basal sandstone-clast cobble conglomerate of reworked Crawford Formation.|
30270|Jalboi Formation|71059|4|Described|p3, p14-16|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 117-230m thick. Storm-dominated marine shelf deposits. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, data all detailed.||Collara Subgroup.||Unconformably to disconformably overlies Arnold Sandstone, Crawford Formation and Showell Member (Mainoru Formation). Is overlain conformably by Hodgson Sandstone.|Interbedded fine sandstone and siltstone, alternating with medium to thick beds of medium quartz sandstone.|
30270|Jalboi Formation|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Arnold Sandstone. Overlain by the Hodgson Sandstone.||
30270|Jalboi Formation|71494|6|Mentioned|p4|||||||Disconformably overlies the Showell Member.||
30270|Jalboi Formation|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
30270|Jalboi Formation|71893|5|Briefly described|p5, p8, p17, p20, p24|||McArthur Basin.||Collara Subgroup||Disconformably overlies the Crawford Formation and the Arnold Sandstone. Gradationally (in places unconformably) overlain by the Hodgson Sandstone.||
30270|Jalboi 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.||Collara Subgroup||Overlies Arnold Sandstone and underlies Hodgson Sandstone.||
30270|Jalboi Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Collara Subgroup, Roper Group||Underlain by Arnold Sandstone. Overlain by Hodgson Sandstone. Equivalent to Abner Sandstone.||
30270|Jalboi Formation|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Collara Subgroup||Overlies Arnold Sandstone and underlies Hodgson Sandstone and is laterally equivalent, in part, to Abner Sandstone.||
30270|Jalboi Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Underlain by Arnold Sandstone. Overlain by Hodgson Sandstone.||
30270|Jalboi Formation|73083|6|Mentioned|p45|||||||||
30270|Jalboi Formation|73242|5|Briefly described|p38-39, p47|||||Collara Subgroup, Roper Group||Underlain by Arnold Sandstone. Overlain by Hodgson Sandstone. Intruded by Derim Derim Dolerite.|Includes marine shelf sandstone.|
30270|Jalboi Formation|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
22013|Jalma Formation|22538|6|Mentioned|P716|||Part of the Glyde package||||||
22013|Jalma Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
22013|Jalma Formation|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
22013|Jalma Formation|24048|2|Defined|p101 App. 1|Mesoproterozoic|Paleoproterozoic|See also p. 52.  Proposer: P.W. Haines.  Originally included in the now abandoned "Groote Eylandt Beds".  Overlain by Balbirini Dolomite; underlain by Coast Range Sandstone. Max. thickness: 130m.||||||07-NOV-08
22013|Jalma Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Sandstone: brown to purple, medium grained, thin to medium-bedded, ferruginous; fine-grained, thin-bedded sandstone near base; local basal conglomerate; upper very recessive unit of laminated claystone. Geol. Prov: McArthur Basin.||||||13-OCT-05
22013|Jalma Formation|44112|6|Mentioned|p10,65,67,94|||||||||
22013|Jalma Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Sandstone: brown to purple, medium grained, thin to medium-bedded, ferruginous; fine-grained, thin-bedded sandstone near base; local basal conglomerat e; upper very recessive unit of laminated claystone. Geol. Prov: McArthur Basin.||||||
22013|Jalma Formation|63866|5|Briefly described|p116-p117|||Central Caledon Shelf.||||Unconformably overlies the Coast Range Sandstone.||
22013|Jalma Formation|64817|6|Mentioned|p353 Fig.4|||||||||
22013|Jalma Formation|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
22013|Jalma Formation|69430|4|Described|p15:3, 13-14, 21, 23|||NE McArthur Basin. 70-130m thick. Shallow-marine deposits. Includes minor carbonate. May correlate with parts of the Parsons Range Group or the Balma Group.||||Unconformably overlies Coast Range Sandstone and Grindall Formation. Is overlain by Balbirini Dolostone probably unconformably. Correlated with Mount Bonner Sandstone.|Brown to purple, medium-grained, thinly to medium bedded ferruginous sandstone; fine-grained, thinly bedded sandstone near base; local basal conglomerate; upper recessive laminated claystone unit.|12-JUL-16
22013|Jalma Formation|69673|6|Mentioned|p16 fig 13, p18|||||||||
22013|Jalma Formation|71374|5|Briefly described|iii, p1 tbl 1, p24, p27, p33, p57-p58|Statherian|Statherian|McArthur Basin. The type section of Haines et al (1999) occurs from 586500mE 8505100mN to 585800mE 8505500mN. This unit returned a maximum depositional age of 1720 +/- 10 Ma, older than the underlying Coast Range Sandstone. Sampled from near the top of a lower, moderately resistant, ferruginous and sandstone-dominated subunit. Zircon description and SHRIMP analytical discussion are provided. Based on age is interpreted as a probable correlative of the Parsons Range Group.||||Unconformably overlies the Coast Range Sandstone. Locally overlies the Grindall Formation.|Fine-grained quartz sandstone, mudstone and minor carbonate.|
22013|Jalma Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Sandstone, conglomerate, mudstone.|
22013|Jalma Formation|72377|4|Described|iii,p1,6,10-13, 15, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section: Of Haines et al (1999), which extends from 586500mE 8505100mN (base) north-westwards to 585800mE 8505500mN (top). Restricted to the western flank of the Coast Range and several small outcrops to the north of the range. Kositcin et al (2017) reported interpreted maximum depositional age of 1720+\-10 Ma. Sample BM16TJM041 (fine-grained quartz sandstone; 586227E 8505513N): MC-LA-ICP-MS zircon Hf studies yielded dominant detrital zircon age populations between c. 1868 to c. 1838 Ma with Hf isotope values consistent with zircons of the same age from Arnhem Province basement.|1720+\-10 Ma (max dep age)|||Overlain unconformably by Balbirini Dolostone/Nathan Group. Underlain unconformably by Coast Range Sandstone, or locally by Grindall Formation.|Sandstone, mudstone and minor carbonate rocks. Subdivisible into a lower, moderately resistant, ferruginous sandstone unit, and upper, very receessive, fine-grained (sandstone) unit.|10-OCT-19
80198|Jamaica Granite|71750|4|Described|iii,p1,10,20-24|Statherian|Statherian|Geological province: Aileron Province. Similarities in age spectra with Kanandra Metamorphics suggest that the Jamaica Granite is a deformed S-type granite-orthogneiss formed by the partial melting of the Kanandra Metamorphics during a long-lived Palaeoproterozoic metamorphic cycle (eg Reno et al 2017). Garnet-bearing migmatitic orthogneiss sample: GA 2306969 (NTGS HU15BLR777A) (570156E 7483438N) zircon analysis yields age of 1728+\-6 Ma (interpreted magmatic crystallisation age) and 1710+\-4 Ma (metamorphism).|||||S-type granite-orthogneiss|20-SEP-19
80198|Jamaica Granite|72367|5|Briefly described|iii,p1,6,11-12,19-20|Statherian|Statherian|Geological province: Aileron Province. Deformed S-type granite resulting from anatectic melt generated from partial melting  of Kanandra Metamorphics. Kositcin et al (in review) present a spectrum of 207Pb/206Pb zircon ages that record crystallisation of Jamaica Granite at 1728+\-6 Ma, metamorphic zircon growth c. 1710+\-4 Ma, and Pb loss during continued high temperatures at c. 1605 Ma. Sample HU15BLR777A (garnet orthogneiss) records zircon age populations of 1760+\-12 Ma and 1710+\-8 Ma. REE analysis of c. 1760 Ma zircons suggest that the Jamaica Granite may have been extracted from Kananadra Metamorphics after 1760 Ma but before c. 1710 Ma.|1728 +/- 6 Ma (crystallisation, SHRIMP Pb/Pb)||||S-type granitic rock.|07-JAN-20
80198|Jamaica Granite|72524|5|Briefly described|piii, p5, p7.|Statherian|Statherian|Widespread in Kanandra Domain, NE Aileron Province. Formed from the partial melting of Kanandra Metamorphics. Reno et al, 2018 suggests melt extracted from Kanandra Metamorphics after 1760+/-12 Ma based on U-Pb zircn ages. Metamorphic zircon growth reported by both LA-ICP-MS and, more precisely, by SHRIMP at 1710+/-4 Ma.|c. 1728 +/- 6 Ma magmatic crystallisation age|||Diffuse intrusive contact with Canefire granite and intermingles with Kanandra Metamorphics.|Anatectic deformed S-type granite-orthogneiss.|
80198|Jamaica Granite|73551|5|Briefly described|piii, p3, p6-7|Statherian|Statherian|Comprises accumulations of anatectic melt derived by partial melting of the Kanandra Metamorphics. A biotite 40Ar/39Ar age records cooling below 320-280C at 414 +/- 2 Ma. Several previous zircon U-Pb studies yielded a complex spectrum of ages; magmatic crystallisation approximated at ca 1.73 Ga. May have experienced subsequent recrystallisation during metamorphism and deformation until as late as ca 1.55 Ga.|ca 1.73 Ga||||Includes garnet-biotite-K-feldspar gneiss.|
80198|Jamaica Granite|73591|4|Described|piii, p2, p19, p21-26, p37|Statherian|Statherian|Aileron Province. Interpreted to be an anatectic granite formed by the partial melting of the Kanandra Metamorphics (S-type), specifically from aluminous parts resulting in garnet formation. Generally has a diffuse intrusive contact with the Canefire Granite but crosscuts the unit via aplite dykes. New magmatic crystallisation U-Pb zircon age of 1724 +/- 6 Ma via LA-ICP-MS. Several previous ages reported including a magmatic crystallisation SHRIMP U-Pb zircon age of 1728 +/- 6 Ma and metamorphic age of 1710 +/- 4 Ma reported by Kositcin et al (2018). Three samples analysed for Lu-Hf isotopes.|1724 +/- 6 Ma U-Pb LA-ICP-MS|Alkara Suite||Crosscuts Canefire Granite. Intrudes Kanandra Metamorphics.|Includes biotite-garnet granite and garnet-bearing migmatitic orthogneiss.|
32187|Jamberline Sandstone Member|23937|2|Defined|p81 App. 1|Calymmian|Statherian|Of Dook Creek Formation.  Thick quartz sandstone-chert-clast conglomerate.  Previously mapped as undivided Dook Creek Formation.  Max. thickness: 400m in type section.  Geological Province: McArthur Basin.||||||13-APR-05
32187|Jamberline Sandstone Member|24050|4|Described|p35, P9 Tb. 2|Mesoproterozoic|Paleoproterozoic|Sandstone and massive sedimentary breccia with chert, dolostone and sandstone clasts. Of the Dook Creek Formation.  Max. thickness: 20m.||||||07-NOV-08
32187|Jamberline Sandstone Member|24051|5|Briefly described|Map Legend|Calymmian|Statherian|Of Dook Creek Formation (Mount Rigg Group). Geological Province: McArthur Basin.||||||28-SEP-06
32187|Jamberline Sandstone Member|60573|5|Briefly described|Map legend|Calymmian|Statherian|Of Dook Creek Fm.(Mount Rigg Group). Appears as Jamberline Sandstone only in map legend.  Med.to v. thick bedded quartz sst; chert and sandstone clast pebble and cobble conglom; minor dolomitic limestone. Does not outcrop in the Roper River mapsheet area.||||||14-FEB-05
32187|Jamberline Sandstone Member|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Dook Creek Formation. Medium to very thick bedded quartz sandstone; chert and sandstone clast pebble to cobble conglomerate; minor dolomitic siltstone.||||||
32187|Jamberline Sandstone Member|69430|5|Briefly described|p15:24, 30|||NW McArthur Basin. Over 200m thick. Proximal fluvial and shallow-marine deposits.||Dook Creek Formation.|||Medium to coarse and pebbly quartz sandstone, chert-clast conglomeratic sandstone; minor dolomitic siltstone.|12-JUL-16
79432|Jamison sandstone|69430|5|Briefly described|p15:26, 29, 62|||Informal name: shown in quotation marks. May be as young as Neoproterozoic and hence not part of the McArthur Basin. 75-160m thick. Fair to good conventional hydrocarbon reservoirs occur; overlies Kyalla Formation source rocks and is sealed by the Hayfield mudstone.||||Unconformably overlies Kyalla Formation. Is overlain conformably by the Hayfield mudstone.||12-JUL-16
79432|Jamison sandstone|69673|4|Described|p19 fig 16, p33, p38, p40, p46|||Oil and gas shows, potential reservoir rock. Primarily coarse clastic sedimentary rocks. Informal name.||||Overlain by Hayfield mudstone, overlies Bukalorkmi Sandstone|Argillaceous, very fine to coarse, cross bedded quartz sandstone; minor mudstone rich interbeds and conglomerates.|
79432|Jamison sandstone|70968|3|Fully described|v-vi, p75, p77, p81, p86-90, p124-129|Tonian|Mesoproterozoic|See also p131-132, p137. Beetaloo Sub-basin. Lanigan et al. (1994)'s informal name (originally Jamison Sandstone) for a unit in an un-named Group they thought to be much younger than the unconformably underlying Roper Group, rather than forming a conformable upper unit. Name from Jamison-1 well which intersects 97.8 m of the unit. Previously misidentified with Bukalorkmi Sandstone, Moroak Sandstone and Bukalara Sandstone. Supported by new evidence (reported in this study) showing detrital zircons are distinctly younger (late Mesoproterozoic) than the Maiwok Subgroup. Shoreline to shallow-marine shelf deposits. Generally 100m thick; maximum c.162m. High-energy shoreline to shallow-marine deposits. Detrital zircon diagram and discussion. Ages for lower and upper parts of the unit respectively. See p87 Fig 77 for known distribution.|c.1357 Ma; c.1153 Ma (max. depositional ages).|||Unconformably overlies Kyalla Formation and Velkerri Formation. Is overlain conformably by Hayfield mudstone.|Basal conglomerate. Light to medium grey quartz sandstone, very fine- to coarse-grained, massive to planar laminated to trough cross-bedded, containing minor, thin green-grey mudstone-rich interbeds.|23-NOV-17
79432|Jamison sandstone|71059|5|Briefly described|p14-16, p20|||TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, organic petrology reflectivity, data all detailed.||||||
79432|Jamison sandstone|71374|5|Briefly described|p21|Neoproterozoic|Neoproterozoic|Beetaloo Sub-basin, McArthur Basin.||||Overlain by the Hayfield mudstone.||
79432|Jamison sandstone|71488|5|Briefly described|p140 -p153|||Beetaloo Sub-basin. Informal name. Also referred to as the Jamison sandstone, upper and lower on p140, p143-p148, p150. Deposited in a high-energy shoreline to shallow-marine inner shelf setting. 1092 +/- 16 Ma age derived from the informally sub-divided lower Jamison sandstone. Zircon geochronology results are briefly discussed.|959 +/- 18 Ma|||Unconformably overlies the Moroak Sandstone and the Kyalla and Velkerri Formations. Overlain by the Hayfield mudstone. Previously correlated with the Bukalorkmi Formation.|Medium to coarse quartz sandstones.|
79432|Jamison sandstone|71893|4|Described|iii, p2-p3, p6, p8, p40-p48, p52|Neoproterozoic|Mesoproterozoic|Beetaloo Sub-basin of the McArthur Basin. Informal name, subdivided into informal upper and lower units. Postdates 1313 Ma Derim Derim Dolerite. Min. age is constrained on the basis of dating of  truncating units as Neoproterozoic to Cambrian. Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|||Includes the Jamison sandstone, upper and Jamison sandstone, lower.|Unconformably overlies the Kyalla and Velkerri Formations (Roper Group). Conformably overlain by the Hayfield mudstone. Overlain by the Kalkarindji Suite.|Variably fine- to coarse-grained quartz sandstone, with minor thin, green-grey mudstone-rich interbeds and a thin basal conglomerate.|06-NOV-18
79432|Jamison sandstone|72381|5|Briefly described|p772|Neoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. See also upper and lower Jamison Sandstone discussion pp771, 773-781.||||Overlain by Hayfield mudstone. Underlain unconformably by Kyalla Formation.||04-OCT-19
79432|Jamison sandstone|72526|5|Briefly described|p86-87.|Neoproterozoic|Neoproterozoic|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone. Shown as  'Jamison Sandstone' on p8, but text contradicts Mesoproterozoic age shown there.|max dep age 959+/-18 Ma|||Overlies Bukalorkmi Sandstone, Roper Group and underlies Hayfield mudstone.||
79432|Jamison sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||||Underlain by Chambers River Formation. Overlain by Hayfield mudstone.||
80684|Jamison sandstone, lower|71893|4|Described|iii, p2-p3, p6, p41-p44|Stenian|Ectasian|Beetaloo Sub-basin of the McArthur Basin. Informal name. Sampling location - POG Balmain 1, Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided. Possible source areas for detrital zircons include Musgrave Province, Warumpi Province, Aileron Province.|1296 +/- 15 Ma (Max dep. U-Pb-Hf)|Jamison sandstone|||Quartz sandstone.|06-NOV-18
80684|Jamison sandstone, lower|72381|4|Described|p771, 773-781|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a high-energy shoreline to shallow-marine setting (Munson 2016). Detrital zircon U-Pb age analysis by Yang et al (2018) indicate maximum depositional age of 1092+\-16 Ma. Intersected in Elliott-1 and Jamison-1 drillholes, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). Separated from the underlying Roper Group by a period of over 300my of uplift and non-deposition. Interpreted to have been sourced from the south from the Musgrave Province.|1092+\-16 Ma (max dep age)|||Overlain by upper Jamison sandstone. Underlain unconformably by Kyalla Formation.|Fine- to coarse-grained quartz sandstone with thin mudrock interbeds.|04-OCT-19
80685|Jamison sandstone, upper|71893|4|Described|iii, p2-p3, p6, p44-p47|Neoproterozoic|Stenian|Beetaloo Sub-basin of the McArthur Basin. Informal name. Sampling location - POG Balmain-1, Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|1183 +/- 10 Ma (Max dep. U-Pb-Hf)|Jamison sandstone|||Quartz sandstone.|06-NOV-18
80685|Jamison sandstone, upper|72381|4|Described|p771, 773-781|Neoproterozoic|Neoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a high-energy shoreline to shallow-marine setting (Munson 2016). Detrital zircon U-Pb age analysis by Yang et al (2018) indicate maximum depositional age of 959+\-18 Ma. Intersected in Elliott-1 and Jamison-1 drillholes, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). Interpreted to have been sourced from the south from the Musgrave Province.|959+\-18 Ma (max dep age)|||Overlain by Hayfield mudstone. Underlain by lower Jamison sandstone.|Fine- to coarse-grained quartz sandstone with thin mudrock interbeds.|04-OCT-19
24611|Jammine Granite|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Tourmaline-muscovite leucogranite.||||||07-NOV-08
24611|Jammine Granite|22809|4|Described|14|||||||||
24611|Jammine Granite|23714|4|Described|p16|||See also page 14, Table 2. Litchfield Province.||||||
24611|Jammine Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly S-type. In the Cullen Batholith, of the Rum Jungle and Central Region||||||
24611|Jammine Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|May be misspelt? See also Jamine Granite. Of the Allia Creek Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
24611|Jammine Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24611|Jammine Granite|41661|6|Mentioned|p17|||||||||
24611|Jammine Granite|41980|5|Briefly described|Table 3 P575|||||||||
24611|Jammine Granite|50586|5|Briefly described|p1.1, 3.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite.||||||07-NOV-08
24611|Jammine Granite|63866|5|Briefly described|p107|||Litchfield Province, Pine Creek Orogen.||||||
24611|Jammine Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Tourmaline-muscovite leucogranite.||||||07-JAN-09
24611|Jammine Granite|64956|5|Briefly described|p2 Tb. 3, p50|Paleoproterozoic|Paleoproterozoic|Intrudes Burrell Creek Formation. Max. intrusion age: 1858+/-6ma. Geological province: Pine Creek Orogen. Quartz-K-feldspar-muscovite-biotite granite, with accessory tourmaline.||||||07-FEB-11
24611|Jammine Granite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Tourmaline-muscovite leucogranite.|23-NOV-11
24611|Jammine Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p29|||Pine Creek area. Emplacement age.|1858 +/- 5 Ma.|||Intrudes Burrell Creek Formation.||
24611|Jammine Granite|69420|5|Briefly described|p5:18-19, 28|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Potential source of Sn mineralisation. SHRIMP U-Pb zircon age.|1858 +/- 5 Ma: Worden et al. (2008).|Allia Creek Suite.|||Medium-grained tourmaline-muscovite leucogranite: quartz-muscovite and feldspar-tourmaline greisens. Highly fractionated.|12-JUL-16
24611|Jammine Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1858 +/- 6 Ma.|Allia Creek Suite.|||Medium-grained tourmaline-muscovite leucogranite, inequigranular.|
24611|Jammine Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1858+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Equigranular quartz-K-feldspar-muscovite-biotite granite.|
38407|Jangirulu Formation|23937|6|Mentioned|p74 App. 1|||Of the Renner Group.   On HELEN SPRINGS sheet.||||||
38407|Jangirulu Formation|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49||||||
38407|Jangirulu Formation|24303|2|Defined|p33, p61 Appendix|Calymmian|Calymmian|Of the Renner Group. Overlain by the Lake Woods beds; overlies the Wiernty Formation. Max. Thickness: 700m. Previously mapped as undifferentiated Tomkinson Creek beds. Correlative of Bessie Creek Sandstone.||||||18-OCT-05
38407|Jangirulu Formation|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Sandstone, quartz arenite; lensing thin to very thick bedded, medium-grained to pebbly; crossbedded, rippled, graded, convolute laminated; mudstone, laminated, dessicated; silicified, jointed; ridge-forming..||||||18-OCT-05
38407|Jangirulu Formation|24442|5|Briefly described|p15|||Of the Renner Group.  Geological Province: Ashburton Province.||||||
38407|Jangirulu Formation|64780|6|Mentioned|p63 Fig.4|Mesoproterozoic|Mesoproterozoic|||Of the Renner Group||||
38407|Jangirulu Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Renner Group.||||
38407|Jangirulu Formation|69431|4|Described|p16:15, 18-19, 22-23|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. c.400-700m thick (845m in BEETALOO map area including stratiform sills). High-energy shallow-marine subtidal to intertidal, and (near top of unit) supratidal deposits.||Renner Group.||Transitionally overlies Wiernty Formation. Is overlain transitionally by Lake Woods beds.|Mainly homogeneous, well sorted, medium-grained and medium-bedded sandstone; minor granule to pebble conglomerate. Several sedimentary structures listed. Sandstone has a wide range of grain size and bed thickness variations.|12-JUL-16
38407|Jangirulu Formation|69673|6|Mentioned|p58|||||Renner Group||||
38407|Jangirulu Formation|70968|2|Defined|v, p94-95, p108, p110-114, p124|Ectasian|Ectasian|See also p126-129, p131, p140. Hussey, Beier and Crispe in Hussey et al. (2001). Named after an outstation. Originally mapped as undivided Tomkinson Creek beds (Randal et al., 1966). The type section is 4km E of Fergusson Bore, at 357600mE 8023900mN (base) to 356600mE 8024200mN in ELLIOTT 100k sheet. A reference section is also given. Widespread exposures in Ashburton Ranges. Thickness from c.35m to a maximum of 845m in the type section. Shallow intertidal to subtidal open-marine deposits; intertidal to supratidal in uppermost part. Well-illustrated. Detrital zircon diagram.||Renner Group.||Overlies Wiernty Formation transitionally to disconformably. Is overlain conformably and transitionally by Lake Woods beds. Correlated with Bessie Creek Sandstone.|White to cream to grey-purple quartz sandstone, well-sorted, typically medium- to coarse-grained; minor conglomerate and rare mudrock. Halite pseudomorphs and dessication cracks in uppermost interval. Tabular cross-beds common.|
38407|Jangirulu Formation|71893|3|Fully described|iii, p2-p3, p6, p8, p64-p67|Ectasian|Calymmian|Tomkinson Province. A maximum U-Pb depositional age of 1584 +/- 18 Ma was derived in addition to an isolated younger age of 1414 +/- 82 Ma. The formation feautres bidirectional simple to tabular cross-beds and some trough cross-beds. Interpreted to have been deposited in shallow intertidal to subtidal open marine, apart from the uppermost rocks where intertidal to supratidal environments dominated. The type section for this unit occurs about 4km west of the Stuart Highway and about 40km south of Elliott in southern ELLIOT. The maximum age of late Statherian is interpreted on the basis of dating of the underlying Namerinni Group and SHRIMP dating of an unnamed intrusive dolerite dyke dated at 1295 +/- 14 Ma. Description, sampling location, zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.||Renner Group||Conformably overlies the Wiernty Formation and is conformably overlain by the Lake Woods beds (Renner Group).|Well sorted, preodminantly medium-grained and medium bedded sandstone and minor granule to pebble conglomerate.|
38407|Jangirulu Formation|73083|6|Mentioned|p27|Proterozoic|Proterozoic||||||Sandstone and mudstone.|
30496|Jawoyn Group|43187|5|Briefly described|p7|||||||||
27291|Jennings Granitic Gneiss|23844|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jennings Suite. Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
27291|Jennings Granitic Gneiss|38606|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|38885|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|39552|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|39610|6|Mentioned|p6|||||||||
27291|Jennings Granitic Gneiss|39888|6|Mentioned|Fig.8|||||||||
27291|Jennings Granitic Gneiss|39931|6|Mentioned|Map legend|Paleozoic|Proterozoic|Proterozoic to Palaeozoic||||||07-NOV-08
27291|Jennings Granitic Gneiss|42326|5|Briefly described|Table 2 P11|||||||||
27291|Jennings Granitic Gneiss|46730|5|Briefly described|p5, 17|Paleoproterozoic|Paleoproterozoic|Age: 1650Ma (Black et, al). Intrudes the Randall Peak Metamorphics.  Geological Province: Arunta Block.||||||07-NOV-08
27291|Jennings Granitic Gneiss|48992|2|Defined|p29|Mesoproterozoic|Mesoproterozoic|||||||
27291|Jennings Granitic Gneiss|50369|5|Briefly described|p1.4, 8.1, 14.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jennings Suite. Age: 1771Ma (U-Pb).||||||07-NOV-08
27291|Jennings Granitic Gneiss|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Heterogeneous coarse-grained granitic gneiss; porphyroblastic orthogneiss, fine-grained granitic gneiss.||||||
27291|Jennings Granitic Gneiss|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Biotite granitic gneiss, granodiorite gneiss.||||||
27291|Jennings Granitic Gneiss|69427|5|Briefly described|p12:9, 14, 30-31, 45|Paleoproterozoic|Paleoproterozoic|Strangways Range region, Wigley Domain, Aileron Province. Covers most of Mordor Pound.||Jennings Suite.||Intrudes Randall Peak Metamorphics. Is intruded by Mordor Igneous Complex.|A large body of gneissic granite, containing elongate masses of felsic gneiss and minor amphibolite; includes bodies of gneissic biotite granite and biotite-hornblende granite; local garnet; locally strongly migmatitic with contorted layering.|12-JUL-16
27291|Jennings Granitic Gneiss|69925|6|Mentioned|p18, 21, 28, 39-40|||Southern Arunta Province, Arunta Inlier.||||Mostly concordant with but locally intrudes Randall Peak Metamorphics.||
27291|Jennings Granitic Gneiss|69931|6|Mentioned|p269, 273-274, 280, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.||Jennings Suite.|||Fine-grained to porphyritic tonalite.|
30859|Jennings Suite|24197|5|Briefly described|p26, p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Example of the Cullen Association. Includes Jennings Granitic Gneiss, and 10 informally named granitic gneisses, orthogneiss, granulite or metamorphics. Age:1770Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
30859|Jennings Suite|50369|5|Briefly described|p1.4, 8.1, 14.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1770-1771Ma.||||||07-NOV-08
30859|Jennings Suite|67181|5|Briefly described|p631|Statherian|Statherian|Of the Main Group (geochemical grouping) of Arunta Region felsic magmatism.|1771 +/- 9 Ma|||||
30859|Jennings Suite|69427|5|Briefly described|p12:31|||Zhao and McCulloch (1995). As well as these named gneisses, they included the 1771 +/- 9 Ma orthogneisses within the Randall Peak Metamorphics in this Suite.|||Georgina Gap, Jennings, Granitic Gneisses.|||12-JUL-16
30859|Jennings Suite|69931|6|Mentioned|p269|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Also includes an unnamed orthogneiss in the Randall Peak Metamorphics.|1771 +/- 9 Ma.||Jennings Granitic Gneiss, Georgina Gap Granite.|||
80340|Jericho Granite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1780 +/- 4 Ma (U-Pb zircon)||||Muscovite-biotite granite: fine to medium-grained, equigranular, strongly weathered and moderately foliated to locally gneissic.|
80340|Jericho Granite|72516|2|Defined|p13-15, p17, p19-21, p56-60, p202|Statherian|Statherian|Aileron Province. New name, named for the Jericho W-Cu prospect; previously defined as unnamed granite unit Pgf on HUCKITTA (Freeman, 1986); not related to the informal Jericho pegmatite.The type location is defined at 618214mE 7490078mN. Outcrops between the Bonya Hills and Jervois Range in the Bonya Domain. Forms irregular, sharp-crested hills and bouldery outcrops on the surrounding plains; it is moderately to strongly weatherd with pink to orange-pink weathering surfaces. Cogenetic and comagmatic with the Unca and Thring granites. Unconformably overlain or in faulted contact with the Grant Bluff and Elkera formations. Petrography, geochemistry,alteration, mineralisation, metamorphism and structure are discussed. See also p25, 29, 32, p75, p88, p103-104, p125-127, p135, p142, p171, p189, p192, p218.|1780 +/- 4 Ma (LA-ICPMS, Beyer et al 2018)|Fosters Suite||Nonconformably overlain by the Grant Bluff Formation. Intruded by the Samarkand Pegmatite and the Kings Legend Metadolerite. Intrudes the Mascotte Orthogneiss and the Attutra Metagabbro.|Muscovite biotite granite: fine- to medium-grained, equigranular, locally tourmaline bearing; strongly weathered to rottenstone; moderately foliated to locally gneissic.|19-APR-22
80340|Jericho Granite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Aileron Province.|||||Includes granite.|
80340|Jericho Granite|73591|4|Described|piii, p2, p9-11, p13|||Aileron Province. Type locality is ca 3.8 km east of the abandoned Jericho Cu-W mine in western Jervois Range mapsheet. Occurs as a strongly weathered leucocratic muscovite +/-biotite granite at the type area. Outcrops widely between the Bonya Hills and Jervois Range. New magmatic crystallisation U-Pb zircon age of 1782 +/- 7 Ma via LA-ICP-MS. Analysed for Lu-Hf isotopes yielding juvenile signature. Confirmed to be correlative with a granite sample analysed by Kositcin et al. (2011; 1774 +/- 5 Ma) collected from a locality isolated from the type area.|1782 +/- 7 Ma U-Pb LA-ICP-MS|Fosters Suite|||Includes muscovite-biotite granites.|
38417|Jeromah Formation|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Of the Namerinni Group.  Age: 1640Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
38417|Jeromah Formation|24303|2|Defined|p15, p58 Appendix|Statherian|Statherian|Of the Namerinni Group. Overlain by the Carruthers Formation; unconformably overlies the Carmilly Formation. Max. Thickness: 700m. Formerly undifferentiated Tomkinson Creek beds. See also p16 Tb.2||||||18-OCT-05
38417|Jeromah Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Namerinni Gp. Pebbly sandstone; lithic to quartz arenite; lensing, thin to thick bedded; crossbedded; graded bedded; fluid escape structures; rip-up clasts; current lineated, halite pseudomorphs; micaceous mudstone, convolute laminated, conglomerate.||||||07-NOV-08
38417|Jeromah Formation|24442|5|Briefly described|p14|||Of the Namerinni Group.  Geological Province: Ashburton Province.||||||
38417|Jeromah Formation|64780|6|Mentioned|p63 Fig.4 |Palaeoproterozoic|Palaeoproterozoic|||Of the Namerinni Group||||
38417|Jeromah Formation|65209|5|Briefly described|p38|||||Namerinni Group.||Possible correlation with Rising Sun Conglomerate.|Conglomeratic units.|05-JAN-17
38417|Jeromah Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Namerinni Group.||||
38417|Jeromah Formation|69431|4|Described|p16:13-16, 23|Statherian|Statherian|Tomkinson Province. From about 350m thick to 700m in its type section, in Jeromah Creek (BRUNCHILLY map area). Lithology described in some detail. Probable fluvial, overlain by supratidal, intertidal and channelised shallow-marine sediments.||Basal Namerinni Group.||Unconformably overlies Carmilly Formation. Is overlain conformably and transitionally by Carruthers Formation.|Thinly to thickly bedded sandstone, pebbly sandstone, thinly bedded siltstone and mudstone; minor local basal conglomerate, halite pseudomorphs. Bidirectional, shallow-angle tabular and trough cross-beds.|12-JUL-16
38417|Jeromah Formation|69673|6|Mentioned|p58|||||Namerinni Group||||
38417|Jeromah Formation|72373|5|Briefly described|p36|Paleoproterozoic|Paleoproterozoic|Geological province: Tomkinson Province.||||Overlain conformably by Carruthers Formation.||
80336|Jervois Granodiorite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1771 +/- 6 Ma (U-Pb zircon)|Casper Suite|||Granodiorite, minor diorite to monzodiorite: fine to medium grained, equigranular to less commonly porphyritic.|
80336|Jervois Granodiorite|72516|2|Defined|p16-17, p19-21, p51-56, p203 p|Statherian|Statherian|Aileron Province. Named for the Jervois Range. The type location is defined as a prominent hill of boulders and blocks of fresh, grey granodiorite at 626259mE 7485808mN. Formerly the Jervois Granite of Smith, 1963, Smith 1964a, Freeman 1986. Occurs as a number of isolated bouldery hills and nubbins of foliated biotite granodiorite in the Jervois Domain. Descriptions from Freeman (1986) are provided. Possibly intrudes the Bonya Metamorphics. Additional ages included 1766 +/- 7 Ma (SHRIMP U-Pb; Cross et al, 2005) and 1766 +/- 5 Ma (Cross et al, 2005). Petrography, geochemistry, geophysics, alteration, mineralisation, and distinguishing characteristics are discussed. See also p32, p35,  p47, p49, p64, p69-70, p72, p106, p109, p112, p118, p123-124, p135-137, p140, p145-148, p169, p171, p189, p192, p195, p205|1771 +/- 6 Ma (SHRIMP U-Pb, 1995)|Casper Suite||Intruded by the Samarkand Pegmatite.|Granodiorite, minor diorite and monzodiorite: fine- to medium-grained, equigranular to less commonly porphyritic; fresh to moderately weathered, locally silicified, weakly to moderately foliated to locally gneissic.|19-APR-22
80336|Jervois Granodiorite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes granodiorite.|
30860|Jervois Suite|50369|5|Briefly described|p1.4, 9.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1771Ma.||||||07-NOV-08
30860|Jervois Suite|67181|5|Briefly described|p631|Statherian|Statherian|Of the Main Group (geochemical grouping) of Arunta Region felsic magmatism.|1771 +/- 6 Ma|||||
30860|Jervois Suite|69931|6|Mentioned|p269|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|1771 +/- 6 Ma.||Jervois Granite.|||
41817|Jessie Gap Suite|50369|5|Briefly described|p1.4, 14.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1747 -1750Ma.||||||07-NOV-08
41817|Jessie Gap Suite|67181|5|Briefly described|p631|Statherian|Statherian|Of the Main Group (geochemical grouping) of Arunta Region felsic magmatism.|1747 +/- 9 Ma|||||
41817|Jessie Gap Suite|69931|6|Mentioned|p269|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|1747 +/- 9 Ma.||Jessie Gap Gneiss.|||
22033|Jigaimara Formation|12466|6|Mentioned|p171.|Middle Cambrian|Middle Cambrian|Includes an organic-rich, mature and oil-prone claystone associated with Larapintine 1 Petroleum System.||||||
22033|Jigaimara Formation|22600|4|Described|Map legend||Middle Cambrian|||||||
22033|Jigaimara Formation|23373|4|Described|p318||Middle Cambrian|Of Goulburn Group, Arafura Basin.||||||28-SEP-06
22033|Jigaimara Formation|23374|3|Fully described|Tb3p22,6,20,21,23,35||Middle Cambrian|O f the Goulburn Group. In the Arafura Basin.||||||28-SEP-06
22033|Jigaimara Formation|24049|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Goulburn Group. Chert and silicified calcareous siltstone: white to grey, laminated and brecciated, fossiliferous. Geol. Prov: McArthur Basin.||||||13-OCT-05
22033|Jigaimara Formation|44112|3|Fully described|p76-78,109||Middle Cambrian|||||||
22033|Jigaimara Formation|60571|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Goulburn Group. Chert and silicified calcareous siltstone: white to grey, laminated and brecciated, fossiliferous. Geological Province: Arafura Basin.||||||30-NOV-04
22033|Jigaimara Formation|61403|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Goulburn Group. Chert and silicified calcareous siltstone: white to grey, laminated and brecciated, fossiliferous. Geol. Prov: McArthur Basin.||||||
22033|Jigaimara Formation|62504|5|Briefly described|p1, 2|Middle Cambrian|Middle Cambrian|Fossiliferous. Of the Goulburn Group.||||||
22033|Jigaimara Formation|62788|4|Described|p103, p104, 105, 111, 112|Middle Cambrian|Middle Cambrian|Arafura Basin. Type locality on western tip of Banyan Island. Contains early Templetonian trilobites similar to Beetle Creek Formation fauna of western Queensland.||Of Goulburn Group.|||Chert, cherty siltstone (after limestone, calcareous siltstone).|28-MAR-12
22033|Jigaimara Formation|63062|5|Briefly described|p9 Fig. 9, p14, p41|Middle Cambrian|Middle Cambrian|Basal unit of Goulburn Group. Overlain by Naningbura Formation. Geol.Prov: Arafura and Money Shoal Basins. Marine shelf limestone, shale and dolomite. ?May be part of Early Palaeozoic Larapintine petroleum supersystem.||||||07-FEB-11
22033|Jigaimara Formation|64813|5|Briefly described|p272|Middle Cambrian|Middle Cambrian|Geological province: Arafura Basin, N.T. These are mature effective source rocks (oil). ||||||
22033|Jigaimara Formation|69297|5|Briefly described|p283, p285, p288|Middle Cambrian|Early Cambrian|Arafura Basin. Deposited in a shallow marine shelf environment. Approximate age equivalent of the Thorntonia Limestone. ||Goulburn Group||Overlain by the Naningbura Dolomite.|Shallow marine limestone, shale and dolomite.|
22033|Jigaimara Formation|69437|5|Briefly described|p22:10|Series 4|Series 3|Arafura Basin.||||Is overlain by Naningbura Dolomite.||12-JUL-16
22033|Jigaimara Formation|69451|4|Described|p35:3-7, 13|Middle Cambrian|Middle Cambrian|Haines in Rawlings et al. (1997). Arafura Basin (onshore and offshore). 470m thick. Low-energy, shallow-marine, probably subtidal deposits. Middle to late Templetonian. Shown wrongly as part of Wessel Group in Figs.35.4 and 35.5. Potential as petroleum source rock.||Goulburn Group.||Overlies, probably disconformably, Elcho Island Formation (Wessel Group). Is overlain conformably by Naningbura Dolomite.|White to grey interbedded limestone, shale and dolostone, silicified to chert and brecciated; possible microbial laminations; rich fossil fauna of trilobites, bradoriids, hyaliths, lingulate brachiopods and sponge spicules.|12-JUL-16
22033|Jigaimara Formation|69573|6|Mentioned|p656, 659|||Arafura Basin. Features Cambrian Stage 5 fossil sites.||||||
22033|Jigaimara Formation|69673|5|Briefly described|p196|Cambrian|Cambrian |470m thick.||Goulburn Group|||Interbedded fossiliferous limestone, shale, dolostone and chert.|
22033|Jigaimara Formation|70098|4|Described|p5, p7, p19 Fig.5|Furongian|Series 3|Arafura Basin and Goulburn Graben. Oil-source correlation study suggests that the effective source rock in the Arafura Basin is likely to lie within the Jigaimara Formation (Boreham and Ambrose, 2005). Approximate age equivalent of Thorntonia Limestone.||Base of Goulburn Group||Disconformably overlies Wessel Group. Is overlain by Naningbura Dolomite.|Shallow marine limestone, shale and dolomite succession.|
22033|Jigaimara Formation|73083|6|Mentioned|p33|Cambrian|Cambrian|||||||
30779|Jim Jim Suite|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Predominantly I-type granites.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
30779|Jim Jim Suite|24197|4|Described|p28, p103, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Comprises Jim Jim, Malone Creek, Tin Camp, Grace Creek, Eva Valley, Yeuralba and Nabarlek Granites, volcanics of Edith River Group and parts of El Sherana Group. Age: ~1825Ma. Geological Province: Pine Creek Inlier. Eg. of Sybella Association.||||||07-FEB-11
30779|Jim Jim Suite|50545|5|Briefly described|p115||Paleoproterozoic|||||||07-NOV-08
30779|Jim Jim Suite|50586|5|Briefly described|p1.1, 5.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Age: 1825Ma.||||||07-NOV-08
30779|Jim Jim Suite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Includes: Grace Creek, Malone and Jim Jim Granites and the Edith River and El Sherana Groups.||||||15-AUG-06
30779|Jim Jim Suite|63866|5|Briefly described|p110|||Central Domain, Pine Creek Orogen. ||Cullen Supersuite||||
30779|Jim Jim Suite|64677|6|Mentioned|p6|||Eastern Pine Creek Orogen.|||Nabarlek Granite.|||
30779|Jim Jim Suite|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Includes Malone Creek Granite (1823Ma), Jim Jim Granite (1838Ma), Grace Creek Granite.||||||07-JAN-09
30779|Jim Jim Suite|65232|5|Briefly described|p6 Fig. 5|Palaeoproterozoic|Palaeoproterozoic|Predominantly I-type granites.~1830-1829Ma?||||||09-FEB-10
30779|Jim Jim Suite|66683|6|Mentioned|p366 Fig.2, p367.|||Post-tectonic granitoids intruding Central Domain of Pine Creek Orogen.|1835-1820 Ma.|||||11-OCT-11
30779|Jim Jim Suite|67232|6|Mentioned|p3 Fig.2. ||||||||Granites.|
30779|Jim Jim Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1836 +/- 4 Ma.|||||
30779|Jim Jim Suite|67355|6|Mentioned|p5.|||Of Wyborn et al. (1997). Subsequently David Suite.||||||
30779|Jim Jim Suite|67479|6|Mentioned|p6 Fig.2|||||||||
30779|Jim Jim Suite|67779|5|Briefly described|p4, p6 Fig.5, p26, p30, p106 Fig.129.|Paleoproterozoic|Paleoproterozoic|Litchfield Province. I-type granites. Age range shown as 1863-1818 Ma on Fig.5.|1847-1818 Ma (Worden et al. 2008a).||Includes Tin Camp and Nabarlek Granites.|||
30779|Jim Jim Suite|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
30779|Jim Jim Suite|69420|4|Described|p5:2, 4-6, 17-18, 21, 23, 25, 32-34, 38|Paleoproterozoic|Paleoproterozoic|See also 66, 85, 100, 111, 115. Central Domain, Pine Creek Orogen. A name change to the David Suite (to avoid confusion with Jim Jim Granite) "has not been formally recognised". Emplaced during the Cullen Event. Apparently coeval with Cullen Supersuite. Mineralogy and petrology/geochemistry summarised. Contains shallow-level granites grading into volcanic rocks, and sedimentary rocks (included in El Sherana and Edith River Groups).|1863-1818 Ma.||Jim Jim, Malone Creek, Grace Creek, Eva Valley, Yeuralba, Nabarlek, Tin Camp Granites.||Dominated by felsic end-members with significant fractionation. Compared with other Pine Creek Orogen felsic igneous Suites, Jim Jim Suite is predominantly oxidised. I-type granites.|12-JUL-16
30779|Jim Jim Suite|71621|6|Mentioned|p25|||Pine Creek Orogen.||||||02-FEB-19
30779|Jim Jim Suite|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin. Mapped with Cullen Supersuite as a single unit.||||||06-MAR-20
32314|Jimbu Microgranite|22538|6|Mentioned|Fig3 P708||Statherian|Age of unit is 1720+/-7 Ma.||||||28-SEP-06
32314|Jimbu Microgranite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1720+/-7Ma.||||||28-SEP-06
32314|Jimbu Microgranite|23867|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Age: 1720Ma.  Intrudes the Gundi Sandstone.||||||07-NOV-08
32314|Jimbu Microgranite|23937|5|Briefly described|p6 Tb. 1|Paleoproterozoic|Paleoproterozoic| Age: 1720+/-7Ma (Rawlings and Page, 1999).||||||07-NOV-08
32314|Jimbu Microgranite|24050|2|Defined|p82 App. 1|Paleoproterozoic|Paleoproterozoic|Previously called Mann River Porphyry (Patterson 1954); subsequently  Jimbu Granite (Roberts & Plumb, 1965), defined by Plumb & Roberts (1992).  Now revised to "Jimbu Microgranite". Intrudes Katherine River Group.  Age: 1720+/-7Ma (Rawlings & Page, 1999)||||||23-DEC-09
32314|Jimbu Microgranite|24051|5|Briefly described|Map Legend|Statherian|Statherian|Intrudes Katherine River Group. Geological Province: McArthur Basin.||||||05-JUN-18
32314|Jimbu Microgranite|50545|5|Briefly described|p116||Paleoproterozoic|Intrudes Kombolgie Subgroup.||||||07-NOV-08
32314|Jimbu Microgranite|61572|5|Briefly described|p667 Fig. 2|Paleoproterozoic|Paleoproterozoic|Porphyritic microgranite. Intrudes the Katherine River Group. Coeval with West Branch Volcanics. Age: 1720+/-7Ma. Geological Province: McArthur Basin. See also p671 Tb. 1||||||07-NOV-08
32314|Jimbu Microgranite|63866|5|Briefly described|p112|||Interpreted to have been intruded synchronously with the deposition of the Gundi Sandstone.|1720 +/- 7 Ma|||Intrudes the Katherine River Group.||05-JUN-18
32314|Jimbu Microgranite|64698|4|Described|lithinterp table|Statherian|Statherian|Age 1720Ma SHRIMP U/Pb [age name given as Orosirian - probably wrong?]. Pink-green massive porphyritic microgranite, lesser aplite and pegmatite/granophyre veins and dykes. ||||||
32314|Jimbu Microgranite|64817|6|Mentioned|p353 Fig.4, p370  |Statherian|Statherian||1720 +/- 7 Ma.|Of the Katherine River Group.||||
32314|Jimbu Microgranite|65228|5|Briefly described|Fig.10.|Statherian|Statherian|Northern McArthur Basin. Part of the Big Supersequence.|1720 +/- 7 Ma (Page et al. 2000).|||||
32314|Jimbu Microgranite|65340|6|Mentioned|p66, p74.|||Central Arnhem Land. Radial deformation of Katherine River Group around this unit has been attributed to gravity sliding following uplift caused by the intrusion. A similar explanation is offered for deformation of Gold Creek Volcanics and Pungalina Member around the Packsaddle Microgranite.||||||
32314|Jimbu Microgranite|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic||1720 +/- 7 Ma (Rawlings 1999).|||Intrudes Katherine River Group.||
32314|Jimbu Microgranite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1720 +/- 7 Ma.|||Intrudes Upper Katherine River Group.||
32314|Jimbu Microgranite|67564|6|Mentioned|p86.|Paleoproterozoic|Paleoproterozoic||1720 Ma.|||||
32314|Jimbu Microgranite|69430|4|Described|p15:3, 8-9|||NW McArthur Basin. A small (10-50 km2) high-level granitic pluton. Intruded concurrently with deposition of the Gundi Sandstone. An early stage but essentially comagmatic equivalent of West Branch Volcanics. SHRIMP U-Pb zircon age.|1720 +/- 7 Ma.|Katherine River Group.||Intrudes Katherine River Group (up to and including Gundi Sandstone).|Pink-green, massive porphyritic microgranite; lesser aplite and pegmatite/granophyre veins and dykes.|12-JUL-16
32314|Jimbu Microgranite|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by West Branch Volcanics, overlies McCaw Formation||
42100|Jims Find Granite|23809|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Intrudes the Killi Killi Formation (Tanami Group).  Age: 1807+/-9Ma (Pb-Pb, younger zircons) and 2535+/-5Ma (Pb-Pb, inherited zircons).||||||07-NOV-08
42100|Jims Find Granite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1807+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
23669|Jindare Formation|9538|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Pink to purple fine to medium ferruginous poorly sorted sandstone, pebbly friable arkose, laminated chert, commonly brecciated and limonitic, minor siltstone and conglomerate.||||||01-NOV-04
23669|Jindare Formation|23216|4|Described|Table1p7, p37|Cambrian|Early Cambrian|(Needham and Stuart-Smith, 1984). Also been known as Jindare Sandstone.  Sandstone, mudstone and silicified carbonate rocks.  Previously included in Stray Creek Sandstone Member (of Walpole et al 1968). Interfingers with Antrim Plateau Volcanics.||||||05-JUN-06
23669|Jindare Formation|23714|5|Briefly described|p36|Paleozoic|Paleozoic|See also page 7 Table 1. Max. thickness: 200 m.||||||07-NOV-08
23669|Jindare Formation|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
23669|Jindare Formation|23937|5|Briefly described|p54|Cambrian|Cambrian|||||||
23669|Jindare Formation|39679|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
23669|Jindare Formation|40168|6|Mentioned|Map legend|Cambrian|Cambrian|Thinly bedded, fine to medium white quartz sandstone. Mottled fine to medium and pebbly quartz sandstone, purple micaceous siltstone and silty shale.||||||18-OCT-05
23669|Jindare Formation|40957|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
23669|Jindare Formation|42012|4|Described|p14|Cambrian|Cambrian|||||||05-JUN-06
23669|Jindare Formation|42014|5|Briefly described|Map legend|Ordovician|Cambrian|||||||
23669|Jindare Formation|43140|4|Described|p4|Ordovician|Cambrian|||||||
23669|Jindare Formation|43149|5|Briefly described|Map Legend||Cambrian|||||||
23669|Jindare Formation|43187|5|Briefly described|p2|||||||||
23669|Jindare Formation|43832|3|Fully described|30, Table7 p27.||Cambrian|||||||
23669|Jindare Formation|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Of the Daly River Group. Divided into two parts: an upper medium grained, white, well-sorted friable quartz sandstone; and lower feldspathic quartz sandstone, conglomerate, siltstone breccia.||||||07-NOV-08
23669|Jindare Formation|63866|5|Briefly described|p111|Palaeozoic|Palaeozoic|Central Domain, Pine Creek Orogen. ||||||
23669|Jindare Formation|65337|6|Mentioned|p94.|||||Unit in Kalkarindji Volcanic Group.||Overlies and interdigitates with Antrim Plateau Volcanics.||
23669|Jindare Formation|65339|6|Mentioned|p5 Fig.4. ||||||||Sandstone.|
23669|Jindare Formation|69437|5|Briefly described|p22:10|Series 2|Series 2|Daly Basin.||||Is overlain by Tindall Limestone.||12-JUL-16
23669|Jindare Formation|69445|5|Briefly described|p30:3-4|||Needham and Stuart-Smith (1984), Kruse et al. (1994). NE margin of the Daly Basin. Included in the Kalkarindji Volcanic Group of Kruse (in Rawlings et al., 2008). Over 200m thick. Unfossiliferous. Probably deposited in a littoral, shoreface, ?marine environment.|||||Quartzofeldspathic sandstone, often with characteristic low-angle cross-beds; mudstone; silicified carbonate rocks; localised conglomerate. Laterally interdigitates with Antrim Plateau Volcanics.|12-JUL-16
23669|Jindare Formation|69446|5|Briefly described|p31:1-3, 9|Early Cambrian|Early Cambrian|Part of the basement to Daly Basin. Offset by steep normal faults.||||Is overlain unconformably by Tindall Limestone.||12-JUL-16
23669|Jindare Formation|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Tindall Limestone, overlies Antrim Plateau Volcanics||
23669|Jindare Formation|70380|6|Mentioned|p745-746|Early Cambrian|Early Cambrian|||||||
23669|Jindare Formation|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.||Kalkarindji Suite.|||Mottled ferruginous clayey sandstone, fine- to medium-grained and pebbly feldspathic and quartz sandstone, laminated chert, siltstone, conglomerate, silicified carbonate breccia, grainstone; rare evaporite pseudomorphs; commonly limonitic.|
23669|Jindare Formation|71632|5|Briefly described|Map legend.|||Daly Basin. Mapped with Daly River Group and Antrim Plateau Volcanics as a single unit.||||||
24641|Jinduckin Formation|9324|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Daly River Group. Quartz arenite, coarse friable, ripple-marked; minor limestone lenses.||||||
24641|Jinduckin Formation|22809|5|Briefly described|21|||||||||
24641|Jinduckin Formation|22810|4|Described|Table3 P7, P19|Ordovician|Cambrian|Overlies Tindall Limestone||||||
24641|Jinduckin Formation|22813|5|Briefly described|Map|Ordovician|Cambrian|Maroon dolomitic-siliclastic siltstone and dolomitic sandstone-siltstone interbeds.||||||19-OCT-05
24641|Jinduckin Formation|23216|4|Described|p4,Table1p7,38,42-5|Tremadoc|Late Cambrian|Of the Daly River Group.||||||19-JAN-06
24641|Jinduckin Formation|23373|6|Mentioned|p318|||of Daly Basin.||||||
24641|Jinduckin Formation|23714|5|Briefly described|p7 Table 1.|Paleozoic|Paleozoic|See also page 36. Of Daly River Group. Max. thickness: 350 m.||||||07-NOV-08
24641|Jinduckin Formation|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
24641|Jinduckin Formation|24122|3|Fully described|p13, p3 Fig. 2|Early Ordovician|Middle Cambrian|Of Daly River Group. Conformably overlies Tindall Limestone. Maximum thickness: 356m (on PINE CREEK). Sandstone, siltstone, marl, carbonates.  Geological Province: Daly Basin.||||||
24641|Jinduckin Formation|24300|5|Briefly described|Map Legend|Ordovician|Cambrian|Parent: Daly River Group.   Geological Province: Daly Basin||||||
24641|Jinduckin Formation|24303|4|Described|p39, p41|Early Ordovician|Late Cambrian|Geological Province: Daly Basin. Lithological similarities with Middle Cambrian units, Wonarah beds and Burton beds (Georgina Basin) suggest possibility of Middle Cambrian age for this unit?||||||
24641|Jinduckin Formation|24334|5|Briefly described|p48 Tb.1|Arenig|Late Cambrian|Age: 470 - 495 Ma||||||
24641|Jinduckin Formation|29591|6|Mentioned|p107|||||||||
24641|Jinduckin Formation|30659|6|Mentioned|p91|||||||||
24641|Jinduckin Formation|30660|6|Mentioned|Table 1|||Lower Ordovician age||||||
24641|Jinduckin Formation|30661|6|Mentioned|Table 1|||||||||
24641|Jinduckin Formation|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
24641|Jinduckin Formation|31572|6|Mentioned|p22|||L.Ordovician. Correlation chart||||||
24641|Jinduckin Formation|31917|5|Briefly described|p33|||Early Ordovician. See Fig.2,4||||||
24641|Jinduckin Formation|32107|6|Mentioned|p409|||Palaeomagnetic results||||||
24641|Jinduckin Formation|32170|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian - Lower Ordovician||||||
24641|Jinduckin Formation|32171|6|Mentioned|p8|||Middle Cambrian||||||
24641|Jinduckin Formation|32700|4|Described|Table 2|||See also P16. Refers Randal (1962)||||||
24641|Jinduckin Formation|32775|5|Briefly described|Map legend|Early Ordovician|Middle Cambrian|Sandstone, siltstone, marl, carbonate beds.||||||02-DEC-04
24641|Jinduckin Formation|33373|3|Fully described|p12|||Table 3.||||||
24641|Jinduckin Formation|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
24641|Jinduckin Formation|33738|6|Mentioned|p48|||||||||
24641|Jinduckin Formation|34438|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian or Ord.||||||
24641|Jinduckin Formation|34439|4|Described|Table 1|||Camb. or Ord. See also PP9,11,13,14||||||
24641|Jinduckin Formation|35088|6|Mentioned|Fig.8|||||||||
24641|Jinduckin Formation|36138|6|Mentioned|Table 1|||||||||
24641|Jinduckin Formation|36335|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24641|Jinduckin Formation|37818|6|Mentioned|Table 2|||||||||
24641|Jinduckin Formation|39210|5|Briefly described|Fig.18|||||||||
24641|Jinduckin Formation|40128|6|Mentioned|p1|||||||||
24641|Jinduckin Formation|40136|5|Briefly described|p28|||||||||
24641|Jinduckin Formation|40168|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician. Of the Daly River Group. Limestone (stromatolitic in places), calcareous sandstone, sandy limestone, quartz sandstone, siltstone, shale.||||||18-OCT-05
24641|Jinduckin Formation|40957|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24641|Jinduckin Formation|42012|2|Defined|p43|Early Ordovician|Middle Cambrian|See also p21.||||||28-SEP-06
24641|Jinduckin Formation|42014|5|Briefly described|Map legend|Ordovician||||||||
24641|Jinduckin Formation|42070|4|Described|p3|||||||||
24641|Jinduckin Formation|43011|6|Mentioned|Table 2,p12|||||||||
24641|Jinduckin Formation|43140|5|Briefly described|p4|||of Daly River Group.||||||
24641|Jinduckin Formation|43149|5|Briefly described|Map Legend||Cambrian|of Daly River Group||||||
24641|Jinduckin Formation|43832|4|Described|31, Table7 p26|Early Ordovician|Late Cambrian|Contains late Tremadocian - basal Arenig conodont zones||||||
24641|Jinduckin Formation|44113|5|Briefly described|p240|Early Ordovician|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 397m.||||||
24641|Jinduckin Formation|44201|14|Not recorded|p.10|||||||||
24641|Jinduckin Formation|45058|5|Briefly described|p19|||Unit of Daly River Gp.||||||
24641|Jinduckin Formation|45064|3|Fully described|Table 1|||See also p21.||||||28-SEP-06
24641|Jinduckin Formation|45148|6|Mentioned|Fig.4|||Daly River Basin||||||
24641|Jinduckin Formation|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Of the Daly River Group.  Siltstone and silty shale with minor sandstone and chert.||||||07-NOV-08
24641|Jinduckin Formation|46676|14|Not recorded|p.6||Middle Cambrian|M.Cambrian; unit of Daly River Group.||||||
24641|Jinduckin Formation|46679|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
24641|Jinduckin Formation|48942|3|Fully described|p82|||Strat. section p117.||||||28-SEP-06
24641|Jinduckin Formation|64068|5|Briefly described|p8|||Daly Basin. Paleopoles from this (and other) units define a major change in APWP.||||||
24641|Jinduckin Formation|64975|6|Mentioned|p162 Fig.6.|Cambrian|Cambrian|||||||
24641|Jinduckin Formation|65339|5|Briefly described|p5 Fig.4. |||||Unit in Daly River Group.|||Sandstone, shale, dolostone.|
24641|Jinduckin Formation|65342|5|Briefly described|p8.|||Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 205 m.||||Overlies Tindall Limestone.|Sandstone-siltstone interbeds, dolostone; evaporite common in siltstone and some sandstone.|
24641|Jinduckin Formation|65345|5|Briefly described|p4.|||||Unit in Daly River Group.|||Dolomitic siltstone, dolostone and dolomitic quartz sandstone.|
24641|Jinduckin Formation|67186|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Daly River Group||Overlies Tindall Limestone.|Quartz sandstone, coarse, friable, ripple-marked; minor limestone lenses.|23-NOV-11
24641|Jinduckin Formation|69018|6|Mentioned|p450 Fig.1b|||||||||
24641|Jinduckin Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Daly Basin, Centralian B Superbasin. Sequence 2. Lithologically very similar to Anthony Lagoon Formation (Barkly Sub-basin).||||Overlies Tindall Limestone. Is overlain by Oolloo Dolostone.||12-JUL-16
24641|Jinduckin Formation|69443|5|Briefly described|p28:22|Middle Cambrian|Middle Cambrian|Daly Basin. Correlation, based on striking similarity, has this unit regarded as Middle Cambrian.||||Correlated with Anthony Lagoon Formation. Is overlain by Oolloo Dolostone.||12-JUL-16
24641|Jinduckin Formation|69446|4|Described|p31:1-7, 9, 11|Middle Cambrian|Middle Cambrian|Daly Basin. Up to 356.1m thick; is 335.4m thick in the type section in drillhole NTGS 86/1. Low- to moderate-energy peritidal, tidal flat deposits. Features include nodular anhydrite, halite hopper casts and secondary gypsum veins, mudcracks and/or burrows, flat-pebble breccias, intraformational conglomerate, soft-sediment deformation, stromatolites. Unsuccessfully explored for uranium.||Daly River Group.||Conformably, locally disconformably overlies Tindall Limestone. Is overlain conformably/transitionally by Oolloo Dolostone. Lithologically correlated with Anthony Lagoon Formation (Georgina Basin).|Maroon-green dolomitic-siliciclastic siltstone, dolomitic sandstone-siltstone interbeds, ooid dolograinstone, microbial dolostone; dolomitic quartz sandstone in upper part.|12-JUL-16
24641|Jinduckin Formation|69447|6|Mentioned|p32:2|||Daly Basin.||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
24641|Jinduckin Formation|69561|6|Mentioned|p33 fig 2, p33|Floran|Templetonian|In comparison to underlying Tindall Limestone is essentially unfossiliferous.||||Overlain by Oolloo Dolostone, overlies Tindall Limestone||
24641|Jinduckin Formation|69673|4|Described|p191|||356m thick.||Daly River Group||Overlain by Oolloo Dolostone, overlies Tindall Limestone|Siliciclastic siltstone with dolomitic sandstone-siltstone interbeds and local lenses of ooid dolograinstone, microbial dolostone and dolomitic quartz sandstone.|
24641|Jinduckin Formation|70380|3|Fully described|p743-746, p748-750, p752,p755,p757,p759|Drumian|Stage 5|Daly Basin. Unfossiliferous. Mistakenly thought to include Tremadocian to Floian conodonts, trilobites and brachiopods (Opik, 1968; Jones, 1971) and was mapped accordingly (Kruse et al., 1990, 1994). The strata containing those fossils was later recognised as a younger, separate unit, the Florina Formation. Up to 356.1m thick; is 335.4m thick in the type section in drillhole NTGS86/1. Correlated with Point Wakefield beds (Wiso Basin); also with Anthony Lagoon, Wonarah and Arthur Creek Formations (Georgina Basin). The lower contact represents a (carbonate-to-siliciclastic) major sequence boundary. Several sedimentary structures (listed). Peritidal sediments deposited on a prograding mixed carbonate-siliciclastic tidal flat.||Daly River Group.||Overlies Tindall Limestone conformably (possibly locally disconformably)[4 consecutive adverbs!!]. Is overlain transitionally by Oolloo Dolostone.|Mainly maroon-green dolomitic-siliciclastic siltstone with dolomitic sandstone-siltstone interbeds, and local lenses of ooid dolograinstone, microbial dolostone and, in its upper half, dolomitic quartz sandstone.|
24641|Jinduckin Formation|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.|||Sandstone, siltstone, marl, carbonate.|
24641|Jinduckin Formation|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.||Conformably overlies Tindall Limestone. Is overlain conformably by Oolloo Dolostone.|Dolomitic-siliciclastic siltstone with sandstone-siltstone interbeds; quartz sandstone; dolostone; minor cryptalgal dolostone, ooid dolograinstone and dolomitic quartz sandstone; evaporite (mainly anhydrite), common locally; flat-pebble breccia.|
24641|Jinduckin Formation|70968|6|Mentioned|p75|Cambrian|Cambrian|Fence diagram of wells in Beetaloo Sub-basin.||||||
24641|Jinduckin Formation|73083|6|Mentioned|p39|||||||||
26643|Jinka Granite|9694|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Granite, adamellite-granodiorite, porphyritic granite, leucogranite.||||||
26643|Jinka Granite|22524|6|Mentioned|p43|||||||||
26643|Jinka Granite|23733|5|Briefly described|p34 Fig.20|||||||||
26643|Jinka Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jinka Suite. Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26643|Jinka Granite|33102|6|Mentioned|p441|||||||||
26643|Jinka Granite|33103|6|Mentioned|p14|||||||||
26643|Jinka Granite|33699|6|Mentioned|p443|||||||||
26643|Jinka Granite|35005|6|Mentioned|p144|||Age||||||
26643|Jinka Granite|35061|6|Mentioned|p143|||||||||
26643|Jinka Granite|39888|6|Mentioned|Fig.7|||See also Fig.9.||||||28-SEP-06
26643|Jinka Granite|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite granite, locally porphyritic, minor foliated granodiorite, cream coloured. Geological Province: Arunta Block.||||||07-NOV-08
26643|Jinka Granite|40668|5|Briefly described|p272|||||||||
26643|Jinka Granite|40906|4|Described|p12|||||||||
26643|Jinka Granite|41465|6|Mentioned|p13|||||||||
26643|Jinka Granite|42326|5|Briefly described|Table 2 P11|||||||||
26643|Jinka Granite|44327|14|Not recorded|Tb.I,p.7,14,map||Paleoproterozoic|(F53-11). L.Prot.||||||07-NOV-08
26643|Jinka Granite|44328|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26643|Jinka Granite|44964|14|Not recorded|p.32|||||||||
26643|Jinka Granite|46830|6|Mentioned|p27|||||||||
26643|Jinka Granite|46868|6|Mentioned|Fig.2|||||||||
26643|Jinka Granite|46964|5|Briefly described|p266|||Age dates discussed.||||||
26643|Jinka Granite|48844|2|Defined|p.1,12-13, Pl.8|||K/Ar:1440 m.yrs. Rb/Sr:1840 m.yrs. (F53-11).||||||
26643|Jinka Granite|48997|6|Mentioned|Fig.2|||||||||
26643|Jinka Granite|49036|6|Mentioned|p10|||||||||
26643|Jinka Granite|50369|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jinka Suite.||||||07-NOV-08
26643|Jinka Granite|64068|6|Mentioned|p223, p45, 46|||Georgina Basin.||||Is nonconformably overlain by Mount Cornish Formation, Aroota Group. Overlain nonconformably by Oorabra Arkose.||05-APR-12
26643|Jinka Granite|65358|6|Mentioned|p14|||Hosts the Oorabra Reefs: epizonal quartz veins with infill quartz-barite-fluorite up to several kms long.||||||
26643|Jinka Granite|68150|5|Briefly described|p.vi Tb.i, p1-3, p22|||On 100K mapsheet: JINKA 6052. This sample analysed is fine- to medium-grained, commonly porphyritic, with a gneissic fabric defined by alignment of biotite and feldspar phenocrysts. Accessory minerals include magnetite. Classified as belonging to high-heat production (HHP) granites of Zhao and McCulloch (1995), which fall in age range 1730-1710 Ma, and are thought to have been derived from melting of Zhao and McCulloch's 1780-1750 Ma Main Group granites.|1714 +/- 3 Ma, igneous crystallis'n SHRIMP Pb/Pb||||feldspar porphyritic granite|
26643|Jinka Granite|69418|6|Mentioned|p3:30-31|||At North Narbaloo near Oorabra Waterhole, a fracture zone within this unit contains fluorite-bearing veins close to the unconformity with the Oorabra Arkose.||||||12-JUL-16
26643|Jinka Granite|69427|5|Briefly described|p12:3, 40, 64|||Joklik (1955). Crops out poorly across the Jinka Plain, W of Jervois, Aileron Province. Cut by the Oorabra Reefs, extensive quartz veins up to 7m wide and 13km long which form prominent reefs and commonly contain barite, fluorite and galena mineralisation. Included in a group of 1730-1710 Ma granites.|||||Coarse-grained biotite-bearing granite, most commonly equigranular and undeformed to weakly foliated.|12-JUL-16
26643|Jinka Granite|69794|6|Mentioned|iv,p12|Statherian|Statherian|Geological province: Aileron Province. Intrudes into Mascotte Gneiss Complex. Kositcin et al. (2011) provided an age of 1714+\-3 Ma for the granite.|1714+\-3 Ma|||Intrudes into Mascotte Gneiss Complex.||06-APR-20
26643|Jinka Granite|69925|6|Mentioned|p39|||Huckitta Sheet area, Arunta Inlier.||||||
26643|Jinka Granite|69931|6|Mentioned|p269, 275, 283, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated.||Jinka Suite.|||Porphyritic granite.|
26643|Jinka Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1714+/-3 Ma (U-Pb zircon SHRIMP)||||Granite.|
26643|Jinka Granite|72370|5|Briefly described|iii,p1,4,29-32|||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, Marshall Granite) (Hollis et al 2010, Weisheit et al in review, Beyer et al in prep). Has SHRIMP 207Pb/206Pb zircon age of 1714+\-3 Ma, interpreted as the timing of emplacement (Kositcin et al 2011). Crosscut by quartz-bearing fluorite veins that host minor chalcopyrite, pyrite and sepcularite mineralisation (Ivanac and Pietsch 1976). Variably altered, from unaltered pink, bleached to a pale red representing metasomatism by infltrating hydrothermal fluids during vein formation.  LA-ICP-MS U-Pb zircon dating on sample HU15MVM208 yield an interpreted igneous crystallisation age of 1739+\-37 Ma.|||||Pink-cloured granite; variably altered.|
26643|Jinka Granite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.||||Unconformably overlain by the Plenty Group.|Biotite granite, medium-grained, porphyritic and undeformed.|
26643|Jinka Granite|72516|4|Described|p10, p14,  p20-21, p77-79, p113-116|Statherian|Statherian|Aileron Province. SHRIMP age derived from Kositicin et al, 2011. Outcrops extensively in eastern Jinka to the west of JERVOIS RANGE SPECIAL. Petrogrpahy is discussed. See also p118, p122-123, p135, p145, p171, p192.|1714 +/- 3 Ma (SHRIMP Pb-Pb)|||Intrudes the Thring Granite and the Kings Legend Metadolerite.|I-type biotite granite: medium grained, porphyritic; undeformed.|19-APR-22
26643|Jinka Granite|73591|5|Briefly described|piv, p2, p14, p36-37|||Aileron Province. Previous SHRIMP U-Pb zircon age of 1714 +/- 3 Ma reported by Kositcin et al (2011). Analysed for Lu-Hf isotopes yielding a mixed source.|1714 +/- 3 Ma U-Pb SHRIMP|Sainthill Suite|||Includes biotite granite.|
30861|Jinka Suite|24197|5|Briefly described|p29, p58|Paleoproterozoic|Paleoproterozoic|Example of the Sybella Association. Felsic, fractionated, I-type. Age: 1713Ma. Geological Province: Arunta Inlier. See also p60 Tb. 4.1.||||||07-FEB-11
30861|Jinka Suite|50369|5|Briefly described|p1.1, 1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-NOV-08
30861|Jinka Suite|50588|6|Mentioned|p4.2|||Geological Province: Arunta Inlier.||||||
30861|Jinka Suite|65455|6|Mentioned|p6 Fig. 3|||Within the Arunta region, on northern margin of the Ngalia Basin. Has been identified as having potential for Cu, Au, Ta, Mo and W mineralisation.||||||09-MAY-12
30861|Jinka Suite|69931|6|Mentioned|p269, 278, 282, 284|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|||Jinka Granite.|||
24321|Johannsen Metagabbro|23844|3|Fully described|p28|Mesoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. Max Thickness: <250m. Mafic granulite dyke swarm - truncated by Harry Anorthosite Gabbro. See also Fig.10||||||07-NOV-08
24321|Johannsen Metagabbro|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24321|Johannsen Metagabbro|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24321|Johannsen Metagabbro|39610|5|Briefly described|p6|||||||||
24321|Johannsen Metagabbro|39887|6|Mentioned|Fig.3|||||||||
24321|Johannsen Metagabbro|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
24321|Johannsen Metagabbro|42830|6|Mentioned|Fig.3 P155|||||||||
24321|Johannsen Metagabbro|48992|2|Defined|p31|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24321|Johannsen Metagabbro|60668|5|Briefly described|p10, p2 Tb. 1|||Dyke swarm which is dominated by homogeneous coarse-grained mafic granulite, granoblastic gabbro and felsic granulite. See also Fig. 20a. ||||||
24321|Johannsen Metagabbro|64738|5|Briefly described|p250-252|Paleoproterozoic|Paleoproterozoic|Metamorphosed zircon rims averaging 1696 +/- 8 Ma. Cut by a tonalite intrusion with protoliths aged 1787 +/- 4 Ma and similar overgrowths aged 1685 +/- 20 Ma. See also mis-spelling Johansenn Metagabbro (p247 Fig.2, pp251-252, pp259-260)..|Protolith age of 1805 +/- 4 Ma.||||Metamorphosed suite of mafic sills or dykes.|23-APR-12
24321|Johannsen Metagabbro|65338|5|Briefly described|p40.|Orosirian|Orosirian|ALICE SPRINGS area.|1805 +/- 4 Ma (Claoue-Long and Hoatson 2005).|||||
24321|Johannsen Metagabbro|66860|4|Described|p9, p15, p18, p25, p86|||Probably protolith was a mafic sill complex. CL-assisted SHRIMP zircon age is of mafic granulite zircon protolith; metamorphic overgrowth ages are detailed. Cut by a tonalite intrusion dated 1786.6 +/- 3.5 Ma.  A later dyke's date is 1686 +/- 8 Ma. Mis-spelt as Johannsens on p86.|1805.6 +/- 3.2 Ma (Claoue-Long and Hoatson, 2005)|Strangways Metamorphic Complex||Intrudes Utnalanama Granulite and Erontonga Metamorphics.|Thin mafic granulite sheets interlayered with felsic granulite; cut by tonalite and anorthosite bodies; then all cut by a vertical mafic dyke swarm.|
24321|Johannsen Metagabbro|68150|5|Briefly described|p11 Tb.3.2|||Age: SHRIMP, MSWD 0.8, 18 analyses, Claoue-Long and Hoatson, 2005.|1696 +/- 8 Ma, metamorphism|||||
24321|Johannsen Metagabbro|69427|4|Described|p12:9-10, 20, 24, 41|Orosirian|Orosirian|Strangways Range region, Aileron Province. A swarm of at least 10 metamorphosed mafic dykes, radiating out from an apparent confluence point 2km SW of the Johannsens Phlogopite Mine. SHRIMP U-Pb zircon age.|1806 +/- 3 Ma (Claoue-Long and Hoatson, 2005).|||Intrudes Utnalanama Granulite and Erontonga Metamorphics. Is intruded by Harry Anorthositic Gabbro and Gumtree Granite.|Dykes of homogeneous coarse-grained mafic granulite, granoblastic gabbro and felsic granulite.|12-JUL-16
24321|Johannsen Metagabbro|69931|6|Mentioned|p276|||Arunta Inlier. Arc-type signatures. Presented as Johannsen metagabbro.||||Interfingers with Phlogopite Mine Tonalite.||
24321|Johannsen Metagabbro|70376|5|Briefly described|p833,|Paleoproterozoic|Paleoproterozoic||1805 Ma +/- 3 Ma||||Mafic intrusives.|24-JAN-22
24321|Johannsen Metagabbro|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1696 +/- 8 Ma (U-Pb zircon SHRIMP).|1805+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gabbro.|
24321|Johannsen Metagabbro|71839|5|Briefly described|p10|||Outcrops in ALICE SPRINGS.||Strangways Metamorphic Complex||Intruded by the Gumtree Granite.||
79262|Johnnys Creek Formation|71001|5|Briefly described|p16, 18-28|Tonian|Tonian|Amadeus Basin. Formerly Johnnys Creek Member (of Bitter Springs Formation). Supratidal sabkha environment during sea level regression. Carbon isotope correlation graph.||Bitter Springs Group.||Overlies Loves Creek Formation. Is overlain by Wallara Formation, or unconformably by Areyonga Formation.|Cyclically interbedded red evaporitic siltstones and shales with grey to yellow dolostones and grey limestone. Also contains halite pseudomorphs, chert nodules, dessication cracks. A 40m thick layer of heavily weathered spilitic basalt.|
79262|Johnnys Creek Formation|71080|6|Mentioned|p29 Fig 20, p30|Tonian|Tonian|Amadeus Basin. Supersequence 1.||Of Bitter Springs Group.|||Dominantly carbonate-shale, marl.|
79262|Johnnys Creek Formation|71268|4|Described|250k_interpgeop_lut.csv|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma).|850-720 Ma (inferred)|Unit of Bitter Springs Group.|||Basalt; locally altered|
79262|Johnnys Creek Formation|71279|5|Briefly described|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||Bitter Springs Group.||||
79262|Johnnys Creek Formation|71344|4|Described|p1094, 1093, 1095, 1096-1103|Tonian|Tonian|Amadeus Basin. Shows palaeokarsts in upper part, representing intervals of subaerial exposure and erosion. Depositional environment: sabkha, shallow hypersaline lakes and ponds in an arid, partly redbed setting. Contains a horizon of heavily weathered grey green, spilitic basalt.|~850-750 Ma||||Red siltstones interbedded with shales and grey to yellow dolostones.|10-NOV-17
79262|Johnnys Creek Formation|71841|5|Briefly described|iii,p1-3,6-13,15|Cryogenian|Cryogenian|Of Amadeus Basin. Previously termed Johnnys Creek Member. Status upgraded to Formation and formalised by Normington et al (2015), Normington and Donnellan (in review). Original stratigraphy based on McKinnon-Matthews (2009): not insected in CPD001, 002 and 003. Revised stratigraphy in drill core: not intersected in CPD001. CPD002: 118.4-225m EOH. CPD003: 15-152.8m, 172-181.3m (repetitive stratigraphy representing a fault-thrust sequence). See p6-8 (CPD002), p9-11 (CPD003) for lithological descriptions based on revised drill core intervals. ||Unit of Bitter Springs Group.||Uppermost unit of Bitter Springs Group. Underlain by Loves Creek Formation. Grades into Pinyanna beds.||
79262|Johnnys Creek Formation|71842|5|Briefly described|p3|Cryogenian|Cryogenian|Of Amadeus Basin.||Unit of Bitter Springs Group.||||
79262|Johnnys Creek Formation|72369|4|Described|iii,p3-4,43-45|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Contains distinctive microfossils and stromatolites that have been used to identify and map the unit across the basin (Edgoose 2013, Normington et al 2015). Contains basalts of the Bitter Springs Group in a single interval in the upper part of the formation (Normington et al 2015, Normington and Donnellan in review); the basalts are interpreted to be a continental tholeiitic suite (Barovich and Foden 2000). Basalts intersected in drillhole CPDD002 are at least 78m thick, and comprises several flow units within a sequence of red dolomitic siltstone. Kositcin et al (2015) reported an interpreted maximum depositinal age of c. 1030 Ma (detrital zircon SHRIMP U-Pb; dominantly sourced from Aileron or Warumpi provinces) for the Johnnys Creek Formation. LA-ICP-MS U-Pb detrital zircon dating of sample HA14VJN032 (highly-weathered basalt) and as intersected in drillhole CPDD002 (altered basalt) did not return any robust age determinations.||Unit of Bitter Springs Group.||Uppermost unit of Bitter Springs Group. Underlain by Loves Creek Formation. Correlable to lower Buldya Group (Officer Basin), Burra Group (Adelaide Geosyncline).|Red calcareous mudstone, overlain by dolomitic limestone or stromatolitic dolostone with occasional interbedded sandstone; cyclic.|
79262|Johnnys Creek Formation|72375|4|Described|p1-2,5,10,13-14|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Most widespread in the NW Amadeus Basin. Contains distinctive microfossils and stromatolite forms that correlate with lower part of Buldya Group (Officer Basin) and lower part of Burra Group (Adelaide Rift Complex) (Grey et al 2011, Hill et al 2011). Contains a single basaltic unit near the top of the formation with geochemical affinities to the Amata Dolerite. SHRIMP U-Pb zircon analysis by Kositcin et al., 2015 yielded an interpreted (weighted mean 238U/206Pb) max depositional age of 1085+\-11 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS AS13CJE028 (sandy dolostone) suggest they crystallised in magmas derived from a range of crustal sources (see p14 for Hf isotopic results and interpretations).||Unit of Bitter Springs Group.||Uppermost unit of Bitter Springs Group. Overlain disconformably by Wallara Formation. Underlain by Loves Creek Formation.|Red calcareous siltstone, dolomitic limestone or dolostone with siltstone, stromatolitic dolostone with occasional sandstone beds, plus rare basalt dykes.|
79262|Johnnys Creek Formation|72489|5|Briefly described|p4, p6, p7 Fig.6, p7, p9, p10|Tonian|Tonian|Amadeus Basin. The uppermost formation of Bitter Springs Group.||Bitter Springs Group||?overlies Loves Creek Formation.||
79262|Johnnys Creek Formation|72601|5|Briefly described|p3, p7, p10, p25|Tonian|Tonian|Amadeus Basin. Previously the informal Johnnys Creek beds. Contains diverse Tonian biotic assemblages.||Bitter Springs Group||Underlain by Loves Creek Formation. Unconformably overlain by Wallara Formation.|Red mudstone and interbedded carbonate with a local volcanic component.|
79262|Johnnys Creek Formation|73085|4|Described|piii, p1-3, p15-16, p22-23, p25-27|Tonian|Tonian|Amadeus Basin. Previously called 'Johnneys Creek beds'. 431.9 m thick in drillhole BR05DD01. Upper contact with Wallara Formation is transitional. Basal contact with Loves Creek Formation is sharp and probably erosional.||Bitter Springs Group||Underlain by Loves Creek Formation. Unconformably[?] overlain by Wallara Formation. Equivalent to Pinyinna beds.|Red, calcareous mudstone with planar laminated with buff to white oxidation spots; lesser grey to pink carbonate intervals.|
79262|Johnnys Creek Formation|73086|1|Redefined|[See comments].|Tonian|Tonian|[Redefined herein but definition card isn't included in appendix. See ASUD for definition card]. [Re definition of unit]/upgrade from member to Formation based on distinct lithostratigraphic character, great thickness and wide distribution. Added new type section near the Ross River Homestead. Characterised by a distinguishing red calcareous mudstone, the localised presence of basalt, and a distinct assemblage of stromatolites. Previously unit III of the Loves Creek Member [now Loves Creek Formation]. Occurrences of basalt throughout the Bitter Springs Group in both exposures and subsurface are probably all part of the Johnnys Creek Formation. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Type section: Ross River. Key localities: Shannon Bore. Basalt shares a geochemical affinity with the ca 820 Ma Amata Dolerite. In situ U-Pb dating of zircon from basalts yielded highly discordant ages. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. [Also written as Johnny's Creek Formation]. p: iii, ~5-9, 14-15, 29-59, 62, 81, ~100-103, 143, 147-148, ~151-154, 156, 158, 167.|ca 820 Ma|Bitter Springs Formation||Underlain by Loves Creek Fm. Unconformably overlain by Wallara, Areyonga, and Olympic fms. May correlate to Pinyinna and Yackah beds, Buldya and Burra groups, Lewis Range Sandstone, Amata Dolerite.|Red/brown, generally calcareous, mudstone cyclically interlayered with commonly recrystallised stromatolitic and/or chertified carbonate rocks (dominantly limestone), brown-grey siltstone, and occasional sandstone and glauconitic sandstone.|
79262|Johnnys Creek Formation|73088|6|Mentioned|p1|Tonian|Tonian|Amadeus Basin, northeast. Previously called Johnnys Creek beds.||Bitter Springs Group||Underlain by Loves Creek Formation. Overlain by Wallara Formation.||
79262|Johnnys Creek Formation|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Bitter Springs Group||Conformably overlies the Johnnys Creek Formation, disconformably underlies the Wallara Formation.||
22045|Junalki Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup, Churchills Head Group. Lithic arenite and volcanic arenite with interbedded laminated siltstone and mudstone; cross-bedded, thin to thick bedded. Rhyodacitic lava, crystal-lithic tuff and lapilli tuff, and ignimbrite. Volcanic breccia.||||||07-NOV-08
22045|Junalki Formation|23733|5|Briefly described|p5, p8|||Overlain by Unimbra Sandstone (Wauchope Subgroup, Hatches Creek Group).  See also p7 Fig.1 and p32 Fig.19.||||||
22045|Junalki Formation|23809|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup.  Overlain by the Unimbra Sandstone.  Previously interpreted as a correlative of Yungkulungu Formation - now correlated as a time equivalent with Warramunga Group rocks due to lithological similarities.  Age: ~1862Ma.||||||19-OCT-11
22045|Junalki Formation|24047|5|Briefly described|p8 Fig. 7|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Inlier.||||||07-NOV-08
22045|Junalki Formation|24172|2|Defined|p25, p8 Tb.1|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup. Conformaby overlain by Unimbra Sandstone. Geological Province: Tennant Creek Inlier. Max. Thickness: <1600m. Originally mapped as undifferentiated Warramunga Group or Unimbra Sandstone. Conformable contact with Unimbra Sandstone.||||||13-FEB-13
22045|Junalki Formation|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup.||||||07-NOV-08
22045|Junalki Formation|50353|5|Briefly described|Map Legend|||||||||
22045|Junalki Formation|60684|4|Described|p11, p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup (Churchills Head Group). Dominated by interbedded felsic crystal-lithic tuff and tuffaceous sandstone of volcanic origin. Overlain by Unimbra sandstone. Intruded by Mumbilla granodiorite in north. Max. thickness: ~1600m.||||||07-NOV-08
22045|Junalki Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Lithic/volcaniclastic arenite with interbedded laminated siltst. and mudst; rhyodacitic lava, ignimbrite, crystal-lithic tuff and lapilli tuff; chert, jaspillite and argillaceous banded ironstone; minor dacitic to andesitic lava. Tennant Creek region.||||||07-NOV-08
22045|Junalki Formation|61861|6|Mentioned|Fig.2.|||Tennant Creek.|Age ~1862 Ma.|||||03-APR-12
22045|Junalki Formation|64730|5|Briefly described|p141, p142 Fig.11|Paleoproterozoic|Paleoproterozoic|Age from intercalated volcanics. Correlated with Warramunga Formation,  [South] Alligator and Finniss River Groups.|1862 +/- 4 Ma (Compston 1995; Smith 2001).|||Underlies Ooradidgee Group.||02-MAY-12
22045|Junalki Formation|64735|4|Described|p205 Fig 1, p205, 213, 217,|Orosirian||Age from a felsic volcanic unit; equivalent to Warramunga Formation.|Igneous crystallisation age of 1862+/-5 Ma.|Of Warramunga Group.||Unconformably underlies Ooradidgee Group.||20-APR-12
22045|Junalki Formation|65209|5|Briefly described|p35 Fig.1, p36, p37, p39|Paleoproterozoic|Paleoproterozoic|Formerly of Warramunga Group. Now not in any Group. Originally tentatively correlated with Yungkulungu Formation (Donnellan et al. 1995), but subsequently re-interpreted (Johnstone and Donnellan 2001) as a correlative, with Woodenjerrie beds, of the Warramunga Formation. Folded.||||Correlative of Warramunga Formation.|Contains argillaceous banded ironstone.|05-JAN-17
22045|Junalki Formation|65232|6|Mentioned|p65, App. 2|||Of Flynn Subgroup (of Newton 1979). Minor vein-type uranium occurrences in igneous rocks. Quartzite.||||||10-FEB-10
22045|Junalki Formation|65338|5|Briefly described|p6, p17.|Orosirian|Orosirian|Warramunga Province, Tennant Region. Correlated with Warramunga Formation; but this unit's sediments are shallower-water and more proximal.|1862 +/- 5 Ma (Smith 2001).|||Is unconformably overlain by Ooradidgee Group.|Felsic volcanic rocks.|
22045|Junalki Formation|66767|5|Briefly described|p57|||Warramunga Province, and basement to Davenport Province.||||Correlative of Warramunga Formation.||
22045|Junalki Formation|67148|6|Mentioned|Map legend.|Proterozoic|Proterozoic|Shown as ungrouped unit in interpreted geology key.||||||19-OCT-11
22045|Junalki Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Lithic/volcaniclastic arenite with interbedded laminated siltstone and mudstone; rhyodacitic lava, ignimbrite, crystal-lithic tuff and lapilli tuff; chert, jaspilite and argillaceous banded ironstone; minor dacitic to andesitic lava.|
22045|Junalki Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area.|1862 +/- 9 Ma.|||||
22045|Junalki Formation|67329|6|Mentioned|p1|||Considered analogous to the Warramunga Formation.||||||
22045|Junalki Formation|67352|6|Mentioned|p8, p44 Fig.48, p50|Orosirian|Orosirian|Warramunga Province. Part of a volcanosedimentary package including also the Woodenjerrie beds and Warramunga Formation.||||Correlated with Woodenjerrie beds, Warramunga Formation.||23-MAY-14
22045|Junalki Formation|69187|6|Mentioned|p53 Fig.2|||||||||
22045|Junalki Formation|69424|4|Described|p9:1-7, 9-10, 23, 32-33, 54|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Volcanism c.1860 Ma. Folded during the c.1860-1850 Ma Tennant Event. About 1600m thick. Shallow marine, grading upwards to sublittoral/littoral and possibly fluviatile. Has a distinctive, highly-magnetic character due to its volcanic rocks. Felsic extrusives of this unit are included in the Tennant Creek Supersuite. Hosts Au-bearing quartz veins.|1862 +/- 5 Ma; dacitic lava (Smith, 2000).|||Overlain unconformably by Ooradidgee Group,Unimbra Sandstone. Lateral equivalent of Warramunga Formation,Woodenjerrie beds. Intruded by Cabbage Gum, Hill of Leaders Granites, Mumbilla Granodiorite.|Lithic/volcaniclastic sandstone with interbedded siltstone and mudstone; rhyodacitic lava, ignimbrite, crystal-lithic tuff and lapilli tuff; chert; jaspilite; argillaceous banded ironstone; minor dacite and andesite.|12-JUL-16
22045|Junalki Formation|69425|5|Briefly described|p10:2, 10, 13-15, 24|||Tennant Region.|c.1862 Ma.|||Is overlain unconformably by Unimbra Sandstone. Correlative of Woodenjerrie beds.||12-JUL-16
22045|Junalki Formation|69431|6|Mentioned|p16:2|||Tennant Region.||||||12-JUL-16
22045|Junalki Formation|73083|6|Mentioned|p21|||Occurs as rafts enclosed in granite in the Frew River 1:250K Sheet (NW).||||||
22045|Junalki Formation|73124|5|Briefly described|piii, p2 Fig.1, p19|Orosirian|Orosirian|Geochron is from a flow-banded porphyritic dacite that is indistinguishable in age from an unnamed porphyritic dacite (1858.4 +/- 5.0 Ma) from drillhole R27ARD18 at Rover 27 prospect (sample 2018339531).|1862 +/- 5 Ma|||Correlates to Warramunga Formation.||
22045|Junalki Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||||||
22045|Junalki Formation|73427|5|Briefly described|p3, p11-12, App.A|Orosirian|Orosirian|North Australian Craton, Tennant Region/East Tennant. U-Pb zircon crystallisation age of 1862 +/- 5 Ma previously reported from felsic volcanic rocks. Deformation interpreted to have occurred prior to ca 1855 Ma.|1862 +/- 5 Ma|||Intruded by Tennant Creek Supersuite.|Volcaniclastic sedimentary rocks, tuff and lava.|
22045|Junalki Formation|73460|6|Mentioned|p2|||Warramunga Province.||||||
22045|Junalki Formation|73506|6|Mentioned|p4|Orosirian|Orosirian||ca. 1860 Ma|||||
22045|Junalki Formation|73550|6|Mentioned|p4|||Warramunga Province.|Older than 1860 Ma|||Equivalent to Warramunga Formation. Unconformably overlain (angular) by Ooradidgee Group.||
22045|Junalki Formation|73590|6|Mentioned|p1-2|Orosirian|Orosirian|Warramunga Province. Some of the oldest rocks in the province.|older than 1860 Ma|||Equivalent to Warramunga Formation and Woodenjerrie beds. Unconformably (angular) overlain by Ooradidgee Group.||
72697|Kaidwalla Granite|65338|5|Briefly described|p7, p35.|Statherian|Statherian|May be syntectonic with respect to Davenport Event folding in the Hatches Creek Group.|1707 +/- 4 Ma (Maidment et al. 2006).|Unit in Devils Suite.||||
72697|Kaidwalla Granite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1707+/-4.3 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
79035|Kairos member|69618|5|Briefly described|p91 Fig.2, p93 Fig.3, p100 Tb.1|||Informal name. Basal unit in Dead Bullock Formation, recognised from detailed recent DDH logging. >145m thick. Includes equally informal Marvin Beds, and Zelda, Terran and Lintilla beds.||Basal unit in Dead Bullock Formation.||Is overlain conformably by Ferdies Member.|Very fine- to fine-grained lithic, cross-laminated and slump-bedded sandstone interbedded with minor siltstone and shale; characterised by common cross-lamination and slump structures.|
79035|Kairos member|69747|5|Briefly described|p265|||Geological province: Granites-Tanami Orogen. Occurs locally in association with Dead Bullock Soak goldfield.||Unit of Dead Bullock Formation.||||
79035|Kairos member|73089|5|Briefly described|p5-7, p24, p26-27|Orosirian|Orosirian|Informal usage; defined[?] by Bagas et al. (2014). Known from Dead Bullock Soak. >145 m thick. Marine depositional setting; moderate water depths? [Authors equate this unit to the Browns Range Metamorphics as part of the Tanami Group].|1885-1865 Ma|Dead Bullock Formation, Tanami Group||Possibly overlain by Ferdies Member [conformable].|Cross-laminated and slump-structured, very fine- to fine-grained lithic sandstone, minor siltstone and shale.|
37707|Kakalyi Gneiss|61660|4|Described|p3 Fig.2, p4, pp18-21, pp23-24.    |Proterozoic|Proterozoic|Yaya Domain. Intrusive rock with relatively high volume of leucosome and is geochemically identical to non-migmatised granodiorite elsewhere in the Yaya Domain, eg the Waluwiya Suite. Migmatisation ages are ca. 1570 (the Chewings Orogeny) and ca. 1149 Ma (the Teapot Event).|Protolith age of 1644 +/- 5 Ma.||||Upper amphibolite facies migmatite.|
37707|Kakalyi Gneiss|65272|5|Briefly described|p318|||Timing of Chewings Orogeny constrained by SHRIMP U-Pb metamorphic zircon rim ages of 1571 +/- 5 Ma from this unit (Kinny, 2002).||||||
37707|Kakalyi Gneiss|67565|2|Defined| p63, p19-20, p6 Table 1, p30, p62.|Statherian|Statherian|New name, after Kakalyi Bore; type locality is a hill 4 km south of there. Yaya Domain, Warumpi Province. Previously included in undifferentiated Arunta Complex (Ranford, 1969). Geochemically indistinguishable from the rest of the Waluwiya Suite. Intruded during the Liebig Orogeny and underwent two migmatisation events: zircons have metamorphic rims aged 1571 +/- 5 Ma (Chewings Orogeny)(Kinny, 2002) and 1149 +/- 3 Ma (Teapot Event). Metamorphic effects are detailed. Strong geochemical affinity with the other units in Waluwiya Suite.|1644 +/- 5 Ma (SHRIMP U-Pb zircon).|Unit in Waluwiya Suite.||Is faulted against the Yaya Metamorphic Complex.|Distinctive strongly migmatitic hornblende-biotite felsic orthogneiss with hornblende-bearing leucosomes; locally grades into a weakly porphyritic biotite-hornblende granite with relatively limited migmatisation.|01-DEC-15
37707|Kakalyi Gneiss|69428|5|Briefly described|p13:10, 15-16|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province. Zircons have metamorphic rims aged 1571 +/- 5 Ma (Chewings Orogeny) and 1149 +/- 3 Ma (?migmatisation).|1644 +/- 5 Ma (SHRIMP U-Pb zircon).|Waluwiya Suite.|||A distinctive hornblende-biotite migmatitic orthogneiss with a generally high proportion (40%) of leucosome. Locally grades into weakly porphyritic biotite-hornblende granite with relatively limited migmatisation.|12-JUL-16
37707|Kakalyi Gneiss|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen. Metamorphosed at 1571 +/- 5 Ma and at 1149 +/- 3 Ma (U-Pb zircon SHRIMP).|1644+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Hornblende migmatite, felsic migmatite.|
80426|Kalala Member|71779|2|Defined|iii, p1-p4, p7-p9, p24, p10, 11|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Name proposed by TJ Munson and D Revie. Named for Kalala Station in northeastern DALY WATERS. Corresponds to the now obsolete lower Velkerri Formation of previous usage. The type section is assigned to drillhole Pacific Oil and Gas Ltd (POG) Alexander-1 from ca 617m depth to ca 446m. A maximum thickness of 305.4m is attained in drillhole POG Walton-2. Distinguished from the Amungee Member by generally lower (poor to good) TOC values, chemostratigraphy, geochemistry, geophysical logs; these features are discussed in some detail. Deposited in a subtidal, sub-wave base and generally quiet marine environment. This unit is not differentiated from its parent in outcrop due to poor exposure. Age constrained from SHRIMP U-Pb ages in rare tuffs of the Showell Member. Thickness in various drillholes provided. See also p12 fig 9, p14-p15, p16, 19, 20, 23, 25.||Of Velkerri Formation.||Conformably overlies the Bessie Creek Sandstone. Conformably overlain by the Amungee Member.|Laminated grey-green to dark grey, variably carbonaceous claystone with interlaminated pale grey siltstone and minor thin sandstone intervals that are glauconitic and sometimes micaceous; there are increasingly common towards the base.|24-SEP-18
80426|Kalala Member|71893|4|Described|p17, p20, p25, p37|Ectasian|Calymmian|Equivalent to the informal "Lower" Velkerri Formation of Lanigan et al (1994) and lower Velkerri Formation of subsequent usage.|1417 +/- 29 Ma (Re-Os)|Velkerri Formation||Overlies the Crawford Formation.||
80426|Kalala Member|72381|5|Briefly described|p776|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. ||Unit of Velkerri Formation.||Lowermost unit of Velkerri Fomation. Overlain by Amungee Member. Underlain by Bessie Creek Sandstone.||
80426|Kalala Member|73242|5|Briefly described|p39|||||Velkerri Formation, Maiwok Subgroup, Roper Group||Underlain by Bessie Creek Sandstone. Overlain by Amungee Member. Intruded by Derim Derim Dolerite.|Includes interbedded mudstone and fine sandstone.|
80426|Kalala Member|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin +/- Beetaloo Sub-basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||Velkerri Formation||||
69476|Kalamurta gneiss|61154|5|Briefly described|p6, p43 App.|||Informal name. Mafic rocks interlayered with pelitic gneiss.  Detailed lithology presented in text. Gneiss of the 1600-1540Ma period.  In the eastern Mann Ranges. Geological Province: Musgrave Block.||||||
69476|Kalamurta gneiss|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|||||Correlative of Birksgate Complex.||
75724|Kalkarindji Suite|68193|5|Briefly described|p44|||Kalkarindji Province. Heavily explored, geophysically anomalous locations have all proved negative for diamonds.|||||Basalts.|
75724|Kalkarindji Suite|69417|5|Briefly described|p2:6|Early Cambrian|Early Cambrian|Kalkarindji Province.|507 +/- 4 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69420|6|Mentioned|p5:81|Early Cambrian|Early Cambrian|Covered most of the North Australian Craton.||||||12-JUL-16
75724|Kalkarindji Suite|69422|6|Mentioned|p7:2 Fig.7.2|Cambrian|Cambrian|Kalkarindji Province.||||||12-JUL-16
75724|Kalkarindji Suite|69429|5|Briefly described|p14:4 Fig.14.7|Early Cambrian|Early Cambrian|Kalkarindji Province.|||||Includes basalt flows.|12-JUL-16
75724|Kalkarindji Suite|69432|5|Briefly described|p17:2, 4|Early Cambrian|Early Cambrian|Kalkarindji Province.||||Overlies Birrindudu Group.||12-JUL-16
75724|Kalkarindji Suite|69444|6|Mentioned|p29:5-6|||Shares geochemical similarities with the Indiana Suite in the southeastern Harts Range.|c.508 Ma.|||||12-JUL-16
75724|Kalkarindji Suite|69445|2|Defined|p30:1-12, 16-17|||Glass and Munson in Ahmad and Munson (2013). New name, after Kalkarindji township. Formerly Kalkarindji Volcanic Group of Kruse in Rawlings et al. (2008). Includes the igneous component of Kalkarindji Large Igneous Province, formerly the Kalkarinji (later revised by Glass and Phillip 2006) Continental Flood Basalt Province of Glass (2002). The definition excludes the minor intercalated sedimentary components of the former Group; they are included within the constituent Formations. 60-1100m thick; 760m thick at the type locality at Purnululu National Park, from WGS84 52K 426414mE 8078661mN to 428989mE 8079851mN. Four reference sections are detailed as are type sections for constituent Formations. Geochemistry and petrology described. Correlated with Mount Wright Volcanics and Cymbric Vale Formation (both Gnalta Group), Truro Volcanics, possibly Mooracoochie Volcanics.|||Antrim Plateau, Helen Springs, Colless, Table Hill Volcanics; Milliwindi Dolerite; Mount Ramsay dolerite.|Unconformably overlies Mount Forster Sandstone. Is overlain unconformably by Headleys, Montejinni, Tindall, Top Springs, Thorntonia Limestones; Tarrara, Gum Ridge, Wonarah Formations.|Tholeiitic basalt and dolerite with massive, porphyritic, partly vesicular (flow tops), amygdaloidal glomeroporphyritic textures, microdolerite, basaltic flow breccia, peperite, pyroclastic deposits.|12-JUL-16
75724|Kalkarindji Suite|69917|6|Mentioned|p175|||Geochemically similar to Coggans Gabbro.|ca 508 Ma|||||
75724|Kalkarindji Suite|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Kalkarindji Province.|||Includes Antrim Plateau Volcanics, Jindare Formation.|||01-MAR-18
75724|Kalkarindji Suite|70968|5|Briefly described|p6, p51, p100, p131, p137|Early Cambrian|Early Cambrian||||Helen Springs Volcanics.|Unconformably overlies Roper Group.|Basaltic volcanism.|
75724|Kalkarindji Suite|71267|6|Mentioned|1M_geologyp12_lut.csv|||||||||
75724|Kalkarindji Suite|71779|5|Briefly described|p5|Early Cambrian|Early Cambrian|||||Unconformably overlies the Roper Group.||24-SEP-18
75724|Kalkarindji Suite|71893|5|Briefly described|p41, p948|Cambrian|Cambrian|McArthur Basin.|507 +/- 4 Ma (Ar-Ar, Glass and Phillips 2006)|||Overlies the Jamison sandstone.||
75724|Kalkarindji Suite|73083|6|Mentioned|p: 1, 3, 12, 14-15, 17-18, 21, 24-25...|Cambrian|Cambrian|Strongly magnetic. Part of the Kalkarindji Continental Flood Basalt Province. Marked as Ebk on solid geology maps. Widespread in the Georgina Basin sequence. Associated with possible feeder dykes (labelled Ed - Cambrian dolerite) and altered Cambrian basalt is labelled Ebkl. [Written as Kalkarindji Igneous Suite on p30]. More locations p: 28-31, 34-35, 38, 42-45, 48-49, 55.||||Underlain by Kinevans Sandstone.|Basalt and agglomerate.|
79093|Kanandra Metamorphics|68997|4|Described|vi-vii,p1,45-50|Orosirian|Orosirian|High-grade metasedimentary rocks and mafic intrusions that extend ~100 km eastwards from near the eastern margin of ALCOOTA to the central part of HUCKITTA. Metamorphosed to granulite facies with local evidence for production of large volumes of anatectic melt. Sample: pelitic migmatite: AC07EEB094. Grid Reference (MGA94 Zone 53): 495809mE 7482092mN. Zircon age spectra of 1804+\-10 Ma (in southeastern ALCOOTA), interpreted as maximum depositional age. Zircons rims from pelitic migmatite yielded an age of 1775+\-7 Ma, attributed to 1780-1770 Ma Yambah Event metamorphism. Zircon rims with 1731+\-5 Ma age reflects 1735-1690 Ma Strangways metamorphism.|1804+\-10 Ma (max dep age: U-Pb zircon)||||Mafic granulite, pelitic and psammitic migmatites and spatially associated leucogranite.|
79093|Kanandra Metamorphics|69510|6|Mentioned|p12|||The 1735-1690 Ma Strangways Event is recognised in monazite and zircon rims in rocks of this unit.||||||
79093|Kanandra Metamorphics|69917|5|Briefly described|p70-75, 111|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Maximum depositional age for the precursor sedimentary rock: 1804+/-10 Ma. Sample may be from higher in the succession than the sample from Huckitta sheet (1844+/-8 Ma, Bodorkos et al 2013). Metamorphism from Yambah (1780-1770 Ma) and Strangways (1730-1690 Ma) Events also recorded. 1763+/-8 Ma age from mafic granulite sample is interpreted as the magmatic crystallisation age.|1804+/-10 Ma; 1763+/-8 Ma.||||60% mafic granulite, the remainder being pelitic and psammitic migmatites in the Alcoota sheet area; Mafic granulite, migmatitic metapelite sampled.|
79093|Kanandra Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both Pb/Pb zircon LA-ICPMS ages: crystallisation and metamorphism respectively.|1763+/-9 Ma; 1728+/-4.5 Ma.||||Granulite.|
79093|Kanandra Metamorphics|71750|4|Described|iii,p1,6,9-13,17,20-21,24|Statherian|Statherian|Geological province: Aileron Province. Outcrop between Entire Point and Delny Shear Zones north of the Harts Range. Underwent UHP granulite facies metamorphism during a long-lived Palaeoproterozoic metamorphic cycle (eg Reno et al 2017). Likely to have similar provenance to Perenti and Deep Bore metamorphics based on similarities and provenance spectra and max depositional ages (Claoue-Long and Hoatson 2005; Kositcin et al 2014, 2015); broadly representing the same sedimentary package at different metamorphic grades. Previous geochronological analysis include maximum depositional ages of 1844+\-8 Ma (Smith 2001) or 1804+\-10 Ma (Bodorkos et al., 2013), metamorphic ages of 1775+\-7 and 1731+\-5 Ma (Bodorkos et al., 2013), magmatic crystallisation ages of 1734+\-2 Ma (Claou¿-Long et al 2008) and 1726+\-6 Ma (Hollis et al 2010). Migmatite sample: GA2306967 (NTGS HU15BLR979) (515346E 7483243N) zircon analysis yields ages of 1818+\-6 Ma (interpreted maximum depositional age), and 1729+\-4 Ma (metamorphic zircon growth).|1818+/-6 Ma max depositional age.|||Intruded by voluminous mafic magmas of the Carmencita Granulite.|Migmatitic metamudstones, and minor metasandstones and metacalc-silicate rock.|20-SEP-19
79093|Kanandra Metamorphics|72367|4|Described|iii,p1,5-6,9-12,19-20|Statherian|Statherian|Geological province: Aileron Province. Deposited in a high-thermal gradient basin environment; underwent protracted UHT metamorphism to granulite facies (eg Reno et al 2017a,b). Outcrops between Entire Point and Delny shear zones, north of the Harts Range in HUCKITTA and ALCOOTA map sheets. Partial melting of Kanandra Metamorphics formed S-type granitic plutons e.g. Jamaica Granite.  Bodorkos et al (2013) reported Pb/Pb age 1775+\-7 Ma, interpreted as earliest evidence for metamorphic zircon growth. Sample HU15BLR979 (migmatite) preserves a maximum deposition age of 1797+\-11 Ma and records metamorphic zircon growth at 1761+\-12 Ma and 1718+\-7 Ma. Ti-in-zircon temperatures suggest Kanandra Metamorphics may have reached UHT granulite facies conditions around, or shortly before c. 1760 Ma.||||Intruded by, and interlayered with Carmencita Granulite.|Granulite facies migmatitic metamudstones, minor metasandstones, and minor metacalc-silicate rock.|
79093|Kanandra Metamorphics|72370|6|Mentioned|p3|||Geological province: Aileron Province.||||||
79093|Kanandra Metamorphics|72372|6|Mentioned|p2|||Geological province: Aileron Province.||||||
79093|Kanandra Metamorphics|72516|6|Mentioned|p7, p9, p192|||Aileron Province. Occurs in the Dneiper Special 1:100k map sheet area.||||Possible age equivalent to Bonya Metamorphics.||27-MAY-21
79093|Kanandra Metamorphics|72524|5|Briefly described|piii, p5, p7.|Statherian|Statherian|Metamudstone migmatites that experienced (ultra-) high-temperature granulite facies metamorphism during a long-lived Palaeoproterozoic metamorphic cycle. Experienced widespread metamorphism, partial melting, and deformation. Minimum age from Canefire granite: 1735 +/- 4 Ma  crystallisation age. Metamorphic zircon growth at 1729+/-4 Ma, SHRIMP U-Pb (Kositcin et al 2018). Previous LA-ICP-MS U-Pb zircon dating also reported.|1818 +/- 6 Ma max depositional age|||Intruded by Canefire granite and intermingles with Jamaica Granite.|Metamudstone migmatites .|
79093|Kanandra Metamorphics|73551|6|Mentioned|p6|||Partial melting produced anatectic melt that contributed to the Jamaica Granite.||||||
79093|Kanandra Metamorphics|73591|5|Briefly described|p19, p21, p24, p26, p37, p39|Statherian|Orosirian|Interpreted to be the source rock for the Canefire Granite and Jamaica Granite via partial melting. Monazite dating has yielded a range of Palaeoproterozoic ages (Reno et al 2020).|ca 1800 Ma|||Intruded by Jamaica Granite.||
29766|Karinga beds|43035|4|Described|Table 1, p29|||Reserved as Karinga Formation.||||||
29766|Karinga beds|69458|5|Briefly described|p42:25|Pleistocene|Pleistocene|Along Karinga Creek, part of Lake Amadeus discharge zone. Probable age of 43-22 Ka.|||||Pebble to cobble conglomerate and coarse sandstone, and has a predominantly calcareous matrix. Includes clasts of calcrete dated 77-34 Ka.|12-JUL-16
79433|Karns Dolostone|69418|6|Mentioned|p3:26|||McArthur Basin. Hosts the Masterton No2 surficial-type Mn deposit (described).||||||12-JUL-16
79433|Karns Dolostone|69430|4|Described|p15:3-4, 24-25, 31, 44, 55|Mesoproterozoic|Mesoproterozoic|SE McArthur Basin. Up to 700m thick. Shallow-marine to emergent, and terrestrial (mainly fluvial), sediments. Various authors have equated/correlated this unit with the McArthur or Nathan Groups. Hosts several manganese and sedimentary phosphate occurrences (described), and the Thor base metal prospect.||Nathan Group.||Unconformably overlies Tawallah and McArthur Groups. Is overlain unconformably by Roper Group or Bukalara Sandstone.|Quartz arenite and dolarenite with cross-beds and ripples; gypsum and halite casts, cauliflower chert pebble beds and chert clasts common; stromatolitic dolostone with thin interbeds of dolarenite and quartzarenite (ooids and intraclast breccia).|12-JUL-16
79433|Karns Dolostone|71374|6|Mentioned|p6|||||Nathan Group||Unconformably overlies the Masterton Sandstone.||
79433|Karns Dolostone|72373|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of central/southern McArthur Basin. Broadly Equivalent to Favenc package, and Nathan, Mount Rigg and Balma groups (McArthur Basin), Bullita and Wattie groups (Birrindudu Basin) and Namerinni group (Tomkinson Province).||||||01-OCT-19
79433|Karns Dolostone|72526|5|Briefly described|p6 Fig.1.2, p8 Fig.1.3.|Calymmian|Statherian|Shown as located in the Southeastern McArthur Basin.||Nathan Group||Shown as unconformably and partially underlying Limmen Sandstone and unconformably overlying Echo Sandstone.||
79433|Karns Dolostone|72718|6|Mentioned|p7|||Southern McArthur Basin (southeastern).||||Partly overlain by Limmen Sandstone (Collara Subgroup, Roper Group) unconformably.||
79433|Karns Dolostone|72912|5|Briefly described|p5 Fig.3.|Calymmian|Statherian|Located in the Southeastern McArthur Basin.||Nathan Group||Shown as unconformably underlying Limmen Sandstone, and laterally equivalent to Dungaminnie Formation, upper Balbirini Dolostone and Smythe Sandstone.||
79433|Karns Dolostone|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Unconformably overlain partly by Limmen Sandstone.||
79433|Karns Dolostone|73412|6|Mentioned|p8|||Southern McArthur Basin.||Nathan Group.||||
35316|Karukali Quartzite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||
35316|Karukali Quartzite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||28-MAY-04
35316|Karukali Quartzite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. White crystalline quartz sandstone; rounded quartz pebble conglomerate beds; local heavy mineral layers of hematite and magnetite. Geological Province: Musgrave Block.||||||
35316|Karukali Quartzite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Geological Province: Musgrave Block.||||||14-JAN-05
35316|Karukali Quartzite|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Basal unit of Tjauwata Group. Thin succession  of quartzite, quartz-muscovite schist, and quartz pebble to boulder conglomerate overlying the Musgrave basement granite.  Overlain by Tjuninanta Formation. Geological Province: Musgrave Block.||||||
35316|Karukali Quartzite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. White crystalline quartz sandstone, rounded quartz pebble conglomerate beds, local heavy mineral horizons of hematite and magnetite.||||||
35316|Karukali Quartzite|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Basal unit of the Tjauwata Group. Unconformably overlies the Mesoproterozoic granites of the Musgrave Province. Max. thickness: 10m. The quartzite contains heavy mineral assemblages dominated by hematite, quartz muscovite schist and quartz conglomerate.||||||07-FEB-08
35316|Karukali Quartzite|65256|2|Defined|p6 Tb.1, p8-9, p13, p14 Fig 10, p37, p38|Stenian|Stenian|New name. Previously described as the basal rocks of the Mount Harris Basalt. 5-10m thick. Disconformably(?) underlies basal units of Tjauwata Group; correlated with MacDougall Formation (Bentley Supergroup). Intruded by mafic dykes interpreted to belong to Alcurra dolerite. Sediment probably derived from Pottoyu Granite Suite.||Basal unit of Tjauwata Group.||Unconformably overlies Pottoyu Granite Suite, Bloods Range Formation;underlies Mount Harris Basalt; conformably underlies Tjuninanta Formation.|Crystalline quartz sandstone, quartzite and quartz-muscovite schist often rich in hematite and magnetite with minor quartz pebble conglomerate; contains heavy mineral horizons.|19-MAY-14
35316|Karukali Quartzite|68995|6|Mentioned|p6|||||Tjauwata Group||||
35316|Karukali Quartzite|69091|5|Briefly described|p70|||Basal unit of Bentley Supergroup.||Tjauwata Group||Equivalent to MacDougall Formation (of Kunmarnara Group).||26-SEP-14
35316|Karukali Quartzite|69436|5|Briefly described|p21:4, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Shoreline deposits.||Basal Tjauwata Group.||Is overlain by Tjuninanta Formation. Lateral equivalent of the MacDougall Formation.|A thin (5-10m thick) succession of quartzite, quartz-muscovite schist, and quartz pebble and boulder conglomerate. Includes lenses of rounded quartz cobble clasts, quartz gravel layers and heavy mineral (mainly haematite) horizons.|12-JUL-16
35316|Karukali Quartzite|69729|5|Briefly described|p79|||Bentley Basin.||Tjauwata Group.||Equivalent to the MacDougall Formation.||
35316|Karukali Quartzite|70018|4|Described|p233,235-236|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Interbedded siliciclastic sedimentary rocks.||Unit of Tjauwata Group.||Overlain by Tjuninanta Formation.|Quartzite, quartz conglomerate, quartz muscovite schist.|
35316|Karukali Quartzite|71210|6|Mentioned|p8|||||||Equivalent to MacDougall Formation.||
35316|Karukali Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, sandstone|
35316|Karukali Quartzite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Sequence is aboubt 5-10m thick. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 208466 (micaceous quartzite) yielded a concordia age of 1163+\-13 Ma, interpreted as maximum depositional age of the quartzite. Sample GSWA 208494 (quartzite) yielded a a weighted mean 207Pb/206Pb age of 1177+\-18 Ma, interpreted as maximum depositional age of the sandstone protolith. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeol_lut.csv.|1084-1075 Ma (inferred)|Unit of Tjauwata Group.||Basal unit of Tjauwata Group. Underlain by Pitjantjatjara Supersuite. Equivalent to MacDougall Formation.|Quartzite and quartz-muscovite schist; locally rich in hematite and magnetite; minor quartz-pebble conglomerate|
35316|Karukali Quartzite|72094|4|Described|p7, p9, p17||Stenian|Geological province: Petermann Nappe Complex. Maximum depositional age constrained by 1177+/-18 Ma and 1163+/-13Ma ages. Summary table of zircon geochronology on p9 Table 2.||Of Tjauwata Group.||Basal sequence of the Tjauwata Group. Overlain conformably by Mount Harris Basalt. Likely time- and lateral equivalent to the MacDougall Formation.|Includes quartzite (material dated).|
38048|Katiti Granite|24301|2|Defined|p36 Appendix 1|Mesoproterozoic|Mesoproterozoic|Of Kulpitjata Granite Complex. Intrudes Allanah Gneiss and Opparinna Metamorphics.  Geological Province: Musgrave Block||||||
38048|Katiti Granite|24302|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Kultpitjata Granite Complex.  Medium-grained porphyritic bioite-hornblende granite, strongly foliated.  Geological Province: Musgrave Block||||||29-SEP-05
38048|Katiti Granite|61154|6|Mentioned|p44 Appendix|||Of the Pitjantjatjara Supersuite.||||||04-OCT-06
38048|Katiti Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1172+/-4 Ma (crystallisation).||||Granite.|
75947|Keri Metamorphics|67232|2|Defined|p29. |Paleoproterozoic|Paleoproterozoic|Named after Keri homestead; Litchfield Province, Pine Creek Orogen. Previously part of Wangi Basics, now abandoned. Type locality is boulder-strewn hills 12 km north of Keri homestead. No observable radiometric or gravity response; no mineralisation known. Geochemistry is described in detail.|1860 +/- 6 Ma (Carson et al. 2009).|||Possibly intrudes Welltree Metamorphics.|Metamorphosed mafic/ultramafic assemblages: noritic cumulate, metapyroxenite and metaperidotite; and mafic amphibolite (metaferrogabbro) with distinctive large garnet porphyroblasts to 10 mm, commonly amalgamated in linear segregations.|
75947|Keri Metamorphics|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|1860 +/- 6 Ma (Carson et al. 2009).|||||
75947|Keri Metamorphics|69420|5|Briefly described|p5:4, 29, 105|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Part of the obsolete Wangi Basics.|||||Metamorphosed noritic cumulates, metaferrogabbro.|12-JUL-16
75947|Keri Metamorphics|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1860 +/- 6 Ma.||||Metamorphosed intermediate to ultramafic rocks of original diorite, gabbro, pyroxenite and peridotite composition.|
25117|Kerridy Sandstone|9380|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Geological Province: Ngalia Basin. Sandstone.||||||07-NOV-08
25117|Kerridy Sandstone|13995|5|Briefly described|p103|Late Ordovician|Late Ordovician|Ngalia Basin. At least in part fluvial deposits.||||||
25117|Kerridy Sandstone|23270|5|Briefly described|Table 1, p3||Paleozoic|Age uncertain. Of Ngalia Basin.||||||07-NOV-08
25117|Kerridy Sandstone|23271|5|Briefly described|Map legend||Paleozoic|Of Ngalia Basin.||||||07-NOV-08
25117|Kerridy Sandstone|23858|5|Briefly described|p916|Late Devonian|Late Ordovician|Underlain by Djagamara Formation. Geological Province: Ngalia Basin.||||||04-OCT-06
25117|Kerridy Sandstone|24064|4|Described|p227|Ordovician|Ordovician|Geological Province: Ngalia Basin. Maximum thicknes: 700m.||||||
25117|Kerridy Sandstone|24111|5|Briefly described|p218|Devonian|Devonian|Geological Province: Ngalia Basin. See also p215 Fig. 11.||||||
25117|Kerridy Sandstone|30258|6|Mentioned|Fig.2|||Ordovician age||||||
25117|Kerridy Sandstone|30684|4|Described|p10|||Ordovician ? age||||||
25117|Kerridy Sandstone|31454|6|Mentioned|Fig.2|||||||||
25117|Kerridy Sandstone|33192|6|Mentioned|p20|||||||||
25117|Kerridy Sandstone|33738|6|Mentioned|p54|||||||||
25117|Kerridy Sandstone|33757|3|Fully described|p9|||See also Table 2.||||||04-OCT-06
25117|Kerridy Sandstone|33758|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
25117|Kerridy Sandstone|33760|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
25117|Kerridy Sandstone|33761|6|Mentioned|p145|||Ordovician||||||
25117|Kerridy Sandstone|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
25117|Kerridy Sandstone|37537|5|Briefly described|Map legend|Devonian|Ordovician|Red-brown, medium to coarse, silty, arkosic sandstone and subgreywacke; siltstone. Geological Province: Ngalia Basin.||||||14-FEB-06
25117|Kerridy Sandstone|39565|6|Mentioned|p33|||||||||
25117|Kerridy Sandstone|40136|5|Briefly described|p29|||||||||
25117|Kerridy Sandstone|40906|6|Mentioned|Fig.11|||||||||
25117|Kerridy Sandstone|41717|6|Mentioned|Fig.19|||||||||
25117|Kerridy Sandstone|42059|6|Mentioned|Fig.2 P131|||||||||
25117|Kerridy Sandstone|42141|6|Mentioned|Fig.3 P570|||||||||
25117|Kerridy Sandstone|42504|5|Briefly described|Table 54 P79|||||||||
25117|Kerridy Sandstone|43275|5|Briefly described|Map Legend||Devonian|||||||
25117|Kerridy Sandstone|43749|6|Mentioned|Fig.1,p6|Carboniferous|Late Devonian|||||||
25117|Kerridy Sandstone|44158|4|Described|p33 Table.2|Devonian|Devonian|Of Ngalia Basin..||||||04-OCT-06
25117|Kerridy Sandstone|45155|2|Defined|p36|Devonian|Ordovician|Ordovician or Devonian||||||
25117|Kerridy Sandstone|45168|6|Mentioned|p6|||||||||
25117|Kerridy Sandstone|61385|5|Briefly described|Map legend|Devonian|Devonian|Red-brown sandstone, minor mudstone.  Geological Province: Ngalia Basin.||||||
25117|Kerridy Sandstone|64068|6|Mentioned|p78, 226|||Ngalia Basin. Correlated with Ethabuka Sandstone, Georgina Basin.||||||
25117|Kerridy Sandstone|65232|5|Briefly described|p70, p71 Fig. 43|Devonian|Ordovician|Angular unconformity with underlying Djagamara Formation. Arkosic sandstone.||||||09-FEB-10
25117|Kerridy Sandstone|65329|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Djagamara Formation, older than Mount Eclipse Sandstone.  Red-brown sandstone, minor mudstone||||||
25117|Kerridy Sandstone|65330|5|Briefly described|Map legend|Palaeozoic|Palaeozoic|Of Ngalia Basin. Shown as younger than Djagamara Formation, older than Mount Eclipse Sandstone.  Red-brown sandstone, minor mudstone||||||
25117|Kerridy Sandstone|65342|6|Mentioned|p6.|||Ngalia Basin. Max. thickness at least 123 m.||||Overlies Djagamara Formation. Is overlain by Mount Eclipse Sandstone.||
25117|Kerridy Sandstone|67565|6|Mentioned|p5 Fig.3.|||Ngalia Basin.||||||
25117|Kerridy Sandstone|67872|5|Briefly described|p13, p15|Devonian|Devonian|Ngalia Basin. Part of the M6 mega-sequence of Lindsay (2002).||||||
25117|Kerridy Sandstone|69437|5|Briefly described|p22:10, 16||Ordovician|Ngalia Basin. Age range is highly approximate. Deposited sometime after Djagamara Formation, and "may be Silurian or Devonian" [!]. Has potential as a petroleum reservoir.||||||12-JUL-16
25117|Kerridy Sandstone|69438|6|Mentioned|p23:46|Devonian|Devonian|Ngalia Basin.||||||12-JUL-16
25117|Kerridy Sandstone|69439|3|Fully described|p24:2-4, 10-11, 13-14, 16, 18, 20-21|?Devonian|?Ordovician|Ngalia Basin. Forms discontinuous low ridges and scarps, E of the Walbiri Ranges and in the Naburula Hills. It is 703m thick in the type section in the eastern Walbiri Ranges. Fluvial to deltaic deposits. Possibly correlative with Carmichael and Mereenie Sandstones (Amadeus Basin); its lithofacies more closely resembles that of the Devonian Pertnjara Group. Age is poorly constrained: the arkosic sandstone suggests basement provenance, hence uplift following Djagamara Formation marine deposition; and Shaw et al. (1992) dated uplift and erosion bordering the Ngalia Basin at 370-350 Ma (Late Devonian). Contains potential reservoirs.||||Unconformably overlies Djagamara Formation (apparently conformably at the type section). Is overlain unconformably by Mount Eclipse Sandstone.|Dominantly thinly- to medium-bedded, brown-red arkosic and micaceous sandstone, with abundant soft-sediment deformation structures (convolute bedding, load casts, pellet casts, slump folds; also ripple marks, cross-beds); minor interbedded mudstone.|12-JUL-16
25117|Kerridy Sandstone|69443|6|Mentioned|p28:27|||Ngalia Basin.||||Possibly correlated with Toko Group.||12-JUL-16
25117|Kerridy Sandstone|69673|5|Briefly described|p107 fig 85, p108, p110|||703m thick.||||Overlies Djagamara Formation, overlain by Mount Eclipse Sandstone|Arkosic and micaceous sandstone with abundant soft sediment deformation features.|
69563|Kiana Group|65337|2|Defined|p60, p95.|Early Cambrian|Ectasian|New name. Synonymous with Robertson Beds. Groups all putative Neoproterozoic formations on the northern margin of the Georgina Basin. Thickness to 300 m. Correlative with Wessel Group. Age stratigraphically constrained to Ectasian-earliest Cambrian, but correlation with Wessel Group & absence of glacial deposits suggests Ediacaran maximum age.|||Includes Bukalara Sandstone and Cox Formation.||Thinly to thickly bedded, very fine to very coarse quartz sandstone, commonly feldspathic, some micaceous; interbedded micaceous siltstone and shale; minor shale, conglomerate and possible carbonate rocks.|27-NOV-17
69563|Kiana Group|67144|5|Briefly described|Map legend.|Ediacaran|Ediacaran|Georgina Basin.|||Includes Bukalara Sandstone.|Unconformably overlies South Nicholson Group. Is unconformably overlain by Barkly Group.||13-APR-12
69563|Kiana Group|67352|6|Mentioned|v, p16-17|Ediacaran|Ediacaran|Rawlings et al. (2008); for all putative Neoproterozoic formations on the northern margin of the Georgina Basin.|||Bukalara Sandstone, Cox Formation.|||
69563|Kiana Group|69430|6|Mentioned|p15:57|Neoproterozoic|Neoproterozoic||||Bukalara Sandstone.|||12-JUL-16
69563|Kiana Group|69437|5|Briefly described|p22:7|||Northern Georgina Basin. Centralian A Superbasin. Supersequence 3. Fluviatile to shallow-marine deposits.|||Bukalara Sandstone, Cox Formation.|||12-JUL-16
69563|Kiana Group|69443|5|Briefly described|p28:3, 5, 7, 12-13|Ediacaran|Ediacaran|Rawlings et al. (2008). Central-northern Georgina Basin. 300m thick. Post-glacial deposits.|||Cox Formation, Bukalara Sandstone.|||12-JUL-16
69563|Kiana Group|69673|6|Mentioned|p112, p116|Ediacaran|Ediacaran ||||Includes Bukalara Sandstone, Cox Formation|||
69563|Kiana Group|70968|5|Briefly described|p124, p137|Early Cambrian|Ediacaran|Georgina Basin. Probably Ediacaran age. An essentially flat-lying undeformed succession overlying the McArthur Basin. [Age says 'Ectasian (late Neoproterozoic) to earliest Cambrian. - Ediacaran to earliest Cambrian probably intended].|||Bukalara Sandstone.|||27-NOV-17
69563|Kiana Group|72526|5|Briefly described|p2, p4, p76, p86.|Neoproterozoic|Neoproterozoic|Basal Georgina Basin.|||Includes Bukalara Sandstone.|||
69563|Kiana Group|72912|6|Mentioned|p24.|Neoproterozoic|Neoproterozoic|Georgina Basin.|||Includes Bulkalara Sandstone.|||
69563|Kiana Group|72919|6|Mentioned|p96-97|||Smith and Roberts (1963).|||Bukalara Sandstone|||
69563|Kiana Group|73083|6|Mentioned|p12, p27, p29, p43|Neoproterozoic|Neoproterozoic|Beetaloo Sub-basin.|||Bukalara Sandstone||Includes siliciclastic rocks.|
25971|Killaloc Formation|14019|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Dolostone, dolarenite, stromatolitic dolostone, dololutite, siltstone, minor sandstone. Conformably on Fraynes Formation; unconformably overlain by Wickham Formation. Type section: 104m. Geological Province: Birrindudu Basin.||||||07-NOV-08
25971|Killaloc Formation|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
25971|Killaloc Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
25971|Killaloc Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Fraynes Formation; unconformably overlain by Wickham Formation. Geological Province: Birrindudu Basin.||||||
25971|Killaloc Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
25971|Killaloc Formation|28255|3|Fully described|p28, Tb. 11 (opp. p8)|||Of the Limbunya Gp. Has an upper horizon of siltstone overlying interbedded dolomite and silty dolomite. Conformably overlies Fraynes Fm; unconformably overlain by Wickham Fm and by basalt of the Antrim Plateau Volcs. Max. thick: 60m.||||||14-JUN-05
25971|Killaloc Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
25971|Killaloc Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Siltstone, interbedded dolomite and minor sandstone.  Carpentarian or Adelaidean (per map legend).||||||17-NOV-04
25971|Killaloc Formation|32660|5|Briefly described|Table 6|||||||||
25971|Killaloc Formation|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25971|Killaloc Formation|45112|5|Briefly described|Table 7|||||||||
25971|Killaloc Formation|48943|2|Defined|p35|Adelaidean|Carpentarian|Carp. or Adel.||||||
25971|Killaloc Formation|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Limbunya Group. Dolostone, dolarenite, stromatolitic dolostone, dololutite and yellow dolomitic siltstone. Conformably overlies Fraynes Formation; unconformably overlain by Wickham Formation.  Geological Province: Birrindudu Basin.||||||07-NOV-08
25971|Killaloc Formation|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
25971|Killaloc Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Fraynes Formation.||
25971|Killaloc Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin. Shown as 'Undifferentiated Fraynes/Killaloc formations'.||Unit in Limbunya Group.|||Dolomitic siltstone, silicified dolostone.|31-OCT-11
25971|Killaloc Formation|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
25971|Killaloc Formation|69432|4|Described|p17:2, 8-9|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 60m thick. Hypersaline shallow lagoon or evaporative shallow-marine deposits.||Limbunya Group.||Conformably overlies Fraynes Formation.|Dolostone, dolomitic sandstone and variably stromatolitic and dolomitic siltstone, which fine upward into dololutite and dolomitic siltstone; evaporites; cauliflower chert nodules to 30cm are locally abundant.|12-JUL-16
25971|Killaloc Formation|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Fraynes Formation, unconformably overlain by Wickham Formation||
25971|Killaloc Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Shown as 'Undifferentiated Fraynes/Killaloc formations',  with a single combined description.||Limbunya Group||Shown as unconformably overlain by Wickham Formation.|Dolomitic siltstone, silicified dolostone.|
25971|Killaloc Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin. No outcrop in map area: shown in Section only as undifferentiated Limbunya Group.||Limbunya Group.||||
25971|Killaloc Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
25971|Killaloc Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Wickham Formation. Underlain by Fraynes Formation.||
25971|Killaloc Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Fraynes Formation. Unconformably[?] overlain by Wickham Formation (Wattie Group).||
35397|Killi Killi Formation|23809|5|Briefly described|p16, p6 Tb. 3|||Of the Tanami Group.  Unconformably overlain by the Pargee Sandstone; overlies the Dead Bullock Formation.  Age: 1815+/-13Ma (Pb-Pb).  Intruded by Jims Find Granite and Water Tower Tonalite.Max. thickness: 4km.||||||
35397|Killi Killi Formation|50152|5|Briefly described|p71, p72 Fig. 3|||Of Tanami Group. Conformably overlies Dead Bullock Formation. Comprises turbiditic sandstone.||||||
35397|Killi Killi Formation|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group.  Includes Jasperlitic Chert member.  Sandstone: purple, brown, turbiditic, thick to thin bedded micaceous and silty to quartzitic, interbedded with buff to dark grey siltstone packages; minor pebbly sandstone and chert.||||||07-NOV-08
35397|Killi Killi Formation|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Includes Jasperlitic Chert member (informal).||||||07-NOV-08
35397|Killi Killi Formation|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Includes the informal Jasperlitic Chert Member. Jasperlitic chert, thin bedded, rhythmically alternating pale chert and jasper, highly contorted.||||||07-NOV-08
35397|Killi Killi Formation|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Overlies: Dead Bullock Formation. Sandstone: turbiditic, thick to thin bedded micaceous and silty to quartzitic; interbedded with siltstone packages, pebbly sandstone and chert; volcanic lithics.||||||07-NOV-08
35397|Killi Killi Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Tanami Group.  Sandstone, siltstone.||||||
35397|Killi Killi Formation|61246|6|Mentioned|p19|||||||||
35397|Killi Killi Formation|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Interbedded muscovite psammite and pelite, graded beds (not exposed).   Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
35397|Killi Killi Formation|61861|3|Fully described|p12-14, p4, 9-10, 15, Figs.16-21,  Map 1|Orosirian|Orosirian|Most widespread formation in Tanami Group. Typically deeply weathered and outcrops poorly. Forms incomplete Bouma sequences. Thickness to 4 km. Intruded by basalt-dolerite sills and feldspar porphyry dykes. Age based on youngest detrital zircons and age of intruding granite|Between 1843 +/- 68 and 1840 +/- 11 Ma.|Youngest unit in Tanami Group.|Includes informal 'jasper chert member' near or at top.|Overlies Dead Bullock Formation, transitionally in places. Faulted against Twigg Formation: may be lateral equivalent. Unconformably overlain by Birrindudu Group, Pargee and Muriel Range Sandstones.|Thick sequence of turbiditic sandstone: micaceous greywacke, quartzwacke, lithic greywacke, quartz arenite and lithic arenite, interbedded with siltstone and mudstone and occasional thin chert beds.|03-APR-12
35397|Killi Killi Formation|62377|4|Described|p5, 21-29|Paleoproterozoic|Paleoproterozoic|Conformably overlies the Dead Bullock Formation. Turbiditic sediments. Correlated with Lander Rock beds and Olympio Formation. Unconformably overlain by the Pargee Sandstone and the Gardiner Sandstone. Age: 1840 +/- 18, 1828 +/- 32Ma.||||||07-NOV-08
35397|Killi Killi Formation|62580|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Thick sequence of turbiditic sedimentary sandstone and siltstone.||||||07-FEB-11
35397|Killi Killi Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami Inlier. Greywacke, micaceous; quartzwacke, quartzarenite, siltstone, graphitic siltstone, granule conglomerate.||||||07-NOV-08
35397|Killi Killi Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region-Aileron Province. Interbedded low grade muscovite bearing psammite and pelite.||||||07-NOV-08
35397|Killi Killi Formation|62636|6|Mentioned|Map Legend|||Solid Geology legend.||Of Tanami Group.||||15-APR-11
35397|Killi Killi Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Geological Province: Tanami/Arunta Region - Aileron Province. Interbedded muscovite bearing psammite and pelite, graded beds.||||||07-NOV-08
35397|Killi Killi Formation|63261|3|Fully described|p9 Fig. 5, p11-12, p23|Paleoproterozoic|Paleoproterozoic|Of Tanami Gp.Conformable on Dead Bullock Fm. Age:<1840Ma.Thick succession of monotonous turbiditic rocks. Correlated with widespread Lander Rock beds in Arunta region. Geol.prov: Tanami Region.Former Madigan beds of Smith et al (1998), Detailed lithol.||||||07-FEB-11
35397|Killi Killi Formation|63866|5|Briefly described|p92-p93|||Tanami Region.||||Overlies the Dead Bullock Formation.|Sandstones.|
35397|Killi Killi Formation|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Age: c. 1835Ma. Feldspathic wacke, sandstone, siltstone, and mudstone, minor quartzite, banded chert, dolerite, and gabbro sills; metamorphosed.||||||24-JUN-08
35397|Killi Killi Formation|64662|5|Briefly described|p28, 27, p30 Fig. 3, p34-37, p43|Orosirian|Orosirian|Of Tanami Gp. Age: Constrained between conformably underlying 1838+/-6Ma Callie Member and intrusive 1.82Ga Water Tower Tonalite.Turbidite, including greywacke, qtz arenite + qtz wacke - youngest detrital zircons are ~1.86 Ma (See Tbs.1, 2).||||||07-FEB-11
35397|Killi Killi Formation|64675|5|Briefly described|p9, p10, p12, Fig.12, pp16-18, p23|Orosirian|Orosirian|Youngest detrital zircon age. See also Map 1.|1848 +/- 22 Ma (AGSO OZCHRON)|Of the Tanami Group.||Underlain by the Dead Bullock Formation. Overlain by the Twigg Formation. Unconformably overlain by the Pargee Sandstone.|Comprises a thick turbidite sequence of interbedded shale, siltstone, and medium-thick bedded sandstone.|19-MAR-14
35397|Killi Killi Formation|64722|5|Briefly described|p10|Orosirian|Orosirian|Detrital zircon population dominated by 1880 - 1840 Ma ages.||Of Tanami Group.||||11-APR-12
35397|Killi Killi Formation|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. See also reference to Killi Formation on p.62.|c.1840 Ma.|Upper unit in Tanami Group.||||03-APR-12
35397|Killi Killi Formation|64733|4|Described|p171-176, p182, Figs.2, 4, 6, 7|Orosirian|Orosirian|Up to 4km thick. Age from detrital zircon U-Pb SHRIMP (Cross and Crispe, 2007). Thought by Blake et al. (1979) and Tunks (1996) to be lateral equivalent of Mount Charles Formation. In faulted contact with Stubbins Formation in places.|Maximum depositional age 1864+/-4 Ma.|Of Tanami Group.||Overlies Dead Bullock and Stubbins Formations and Callie Member. Unconformably overlain by Ware Group.|Turbiditic sandstone, pelite and rare dolerite sills.|20-APR-12
35397|Killi Killi Formation|64734|4|Described|p186-189, p194-6, p199, p201-2, Fig.2|Orosirian||Sst, thinly bedded siltst; fine sand grading to clayst (some black); upper Tanami Group; laterally extensive; varying thickness; geochemical similarities to Upper Callie Sequence; conformable boundary with Dead Bullock Formation below suggested||||||10-MAR-10
35397|Killi Killi Formation|64735|5|Briefly described|p211, p217,||Orosirian|Correlated with Lander Package.||||Overlain by Ware Group.||30-APR-12
35397|Killi Killi Formation|64737|5|Briefly described|p233, p234 Fig.4, p236 Tab.4, p241||Orosirian|Dominated by ~1840-1880 Ma detrital zircons. Similar provenance and depositional timing to Lander Package and Ooradidgee Group. Age is a maximum depositional age.|1868-1866 Ma.|Of Tanami Group.||Overlies Dead Bullock Formation.||01-MAY-12
35397|Killi Killi Formation|64956|5|Briefly described|p10|||Conformably overlain by the informally named "Sunset Pound sandstone".||||||07-FEB-11
35397|Killi Killi Formation|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65324|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||
35397|Killi Killi Formation|65326|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65327|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65328|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tanami Group. Interbedded muscovite psammite and pelite, graded beds.||||||
35397|Killi Killi Formation|65338|5|Briefly described|p17.|||Tanami Region. Overlies a tuff dated at 1838 +/- 5 Ma (Cross and Crispe 2007). Detrital zircon data is remarkably consistent with that from Lander Rock Formation, with which it is correlated.||||||
35397|Killi Killi Formation|65349|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; overlies Dead Bullock Formation; includes informal Jasperlitic Chert member. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst, minor pebbly sst, chert; volcanic lithics in west ||||||
35397|Killi Killi Formation|65350|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||02-MAR-10
35397|Killi Killi Formation|65351|5|Briefly described|Map legend|Orosirian|Orosirian|Of Tanami Group; includes informal Jasperlitic Chert member; overlies Dead Bullock Formation. Purple, brown, turbiditic, bedded, micaceous, silty-quartzitic sst interbedded with buff-dark grey siltst with minor pebbly sst, chert; volcanic lithics in west||||||
35397|Killi Killi Formation|65352|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65353|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65354|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65355|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member; of the Tanami Group; overlies Dead Bullock Formation||||||
35397|Killi Killi Formation|65356|5|Briefly described|Map legend|Orosirian|Orosirian|Sandstone, siltstone; non to weakly magnetic; includes the informal Jasperlitic Chert member (not shown on this map); of the Tanami Group; overlies Dead Bullock Formation||||||02-FEB-10
35397|Killi Killi Formation|65358|5|Briefly described|p6|||In Tanami Region. Conformably overlies Dead Bullock Formation. Turbiditic succession. Correlated with Lander Rock Formation in the Arunta Region.||||||
35397|Killi Killi Formation|66129|5|Briefly described|p213, p214 Fig.1, p215 Fig.2, p216 Fig.3|Orosirian|Orosirian|1864-1844 Ma. Turbiditic sandstone, siltstone, shale. Conformably overlies Stubbins and Dead Bullock Formations. Contact metamorphosed. Unit in Tanami Group. Contains Bald Hill Member.||||||
35397|Killi Killi Formation|66468|5|Briefly described|p16-17,p19-20, p21 Fig.6, p22-24, p26-27|Orosirian|Orosirian|1864-1844 Ma. Conformably overlies Stubbins Formation (WA) and Dead Bullock Formation (NT). ~5km thick, medium to coarse grain sandstone that grades into finer-grain sandstone, laminated siltstone and shale succeeded by mudstone and rare dolerite sills.||||||
35397|Killi Killi Formation|67127|6|Mentioned|p111, p168|||Associated with uraniferous xentime and xenotime rich in HREE and a U-REE mineralisation between the unconformity of this unit and the overlying Gardiner Sandstone.||||Unconformably underlies the Gardiner Sandstone.||
35397|Killi Killi Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Unit in Tanami Group.||Overlies Dead Bullock Formation.|Interbedded low-grade muscovite-bearing psammite and pelite, graded beds.|20-OCT-11
35397|Killi Killi Formation|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Low to medium gravity response.||Unit in Tanami Group.||Overlies Dead Bullock Formation.|Interbedded muscovite-bearing psammite and pelite, graded beds.|20-OCT-11
35397|Killi Killi Formation|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Lateral equivalent of upper part of Twigg Formation. Includes a jasperlitic chert unit.||Unit in Tanami Group.||Overlies Dead Bullock Formation. Is unconformably overlain by Pargee Sandstone and by Gardiner Sandstone.|Sandstone, siltstone, jasperlitic chert.|
35397|Killi Killi Formation|67352|6|Mentioned|p50|||||||||
35397|Killi Killi Formation|67824|4|Described|p383, p386-p396|Orosirian|Orosirian|Hosts gold. Prospectivity increases where crustal-penetrating structures intersect claystone facies. Maximum age constrained by the underlying Callie Member. Deepwater below wave base setting. Sedimentary units were sourced from NW. Also aged 1864-1844 Ma.|< 1840 Ma|Of the Tanami Group.||Overlies Callie Member (Dead Bullock Formation). Conformably overlies Stubbins Formation. Is overlain by Tanami Group.|Mainly turbidites: fine-grained, micaceous-lithic muddy sandstone interbedded with siltstone and claystone.|
35397|Killi Killi Formation|67826|4|Described|p401 Fig.2, p402, p402 Fig.3, p404 Fig.4|Orosirian|Orosirian||~ 1864-1844 Ma|Of the Tanami Group.||Overlies  Stubbins Formation; layer-parallel fault contact. Conformably overlies Dead Bullock Formation.|Comprises metamorphosed wacke, siltstone, shale.|
35397|Killi Killi Formation|68474|5|Briefly described|p572-574, p585|||Granites-Tanami Orogen. 5km thick.|ca. 1864-1844 Ma|Tanami Group||Conformably overlies the Stubbins Formation, Mount Charles Formation and the Dead Bullock Formation. Unconformably overlain by the Ware Group.|Turbiditic succession.|
35397|Killi Killi Formation|68656|4|Described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|Tanami Basin. See also 100k_maginterpgeop_lut.csv, and GEOCHRON. Granites-Tanami Complex. Moderate gravity, non-magnetic. Contains detrital zircons with a wide range of ages, discussed in the GEOCHRON folder.|1862 +/- 3 Ma (Wingate et al., 2009).|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation. Correlated with Lander Rock Formation. Is intruded by Balwina Granite. Is overlain unconformably by Ware Group.|Feldspathic metawacke, metasandstone, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite, metagabbro|
35397|Killi Killi Formation|68733|6|Mentioned|p184|Paleoproterozoic|Paleoproterozoic|Tanami Region.||||||05-DEC-17
35397|Killi Killi Formation|68994|5|Briefly described|p6|||||Tanami Group||Is equivalent to Lander Rock Formation.||
35397|Killi Killi Formation|69003|5|Briefly described|p16-17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Up to 5km thick. The age of the occurrence in NT is shown as <1840 Ma.|1864-1844 Ma.|Tanami Group.||Unconformably overlies the Stubbins, Mount Charles and Dead Bullock Formations. Is overlain unconformably by the Ware Group.|Turbiditic sandstones, siltstones and shales.|
35397|Killi Killi Formation|69253|4|Described|p746, p747 Fig.1, p748, p755-767|Orosirian|Orosirian|Maximum depositional age of c.1864 Ma (SHRIMP U-Pb zircon; Bagas et al., 2009). ~5 km thick. Petrophysical properties detailed. Hosts gold mineralisation in the Coyote area.|~1864-1844 Ma.|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation. Is intruded by Selby Granite.|Upward-fining succession of turbiditic sandstone that grades upwards into siltstone and mudstone.|
35397|Killi Killi Formation|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.|||Interbedded low-grade muscovite-bearing psammite and pelite; graded beds.|
35397|Killi Killi Formation|69383|6|Mentioned|p70|||Tanami Region. Detrital zircon spectra compared to Utopia Quartzite spectra.||||||
35397|Killi Killi Formation|69417|5|Briefly described|p2:4,|||Tanami Region. Turbiditic succession.|1845-1835 Ma.|||||12-JUL-16
35397|Killi Killi Formation|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
35397|Killi Killi Formation|69424|6|Mentioned|p9:4|Paleoproterozoic|Paleoproterozoic|Tanami Region.||||Correlative of Ooradidgee Group.||12-JUL-16
35397|Killi Killi Formation|69426|4|Described|p11:3-8, 10-11, 14, 26, 30-31, 36|Orosirian|Orosirian|Thickness <4000m. Turbiditic, deep-marine proximal to mid-fan setting. Metamorphosed to greenschist to middle amphibolite facies. Hosts gold mineralisation at the Tregony and Titania prospects, and The Don U-Au occurrence. Is intruded by a tonalite aged 1821 +/- 4 Ma. Is separated from the Century Formation by the Pargee Fault.||Tanami Group.||Transitionally overlies Dead Bullock Formation. Is overlain unconformably by Ware Group, Mount Charles and Killi Killi Formations and Pargee Sandstone. Correlated with Lander Rock Formation.|A thick succession of micaceous greywacke, quartz greywacke, lithic greywacke, quartz sandstone and lithic sandstone, interbedded with siltstone (in part carbonaceous) and mudstone, and occasional thin chert beds.|12-JUL-16
35397|Killi Killi Formation|69427|5|Briefly described|p12:4-6|||Tanami Region. Age of a tuff immediately underlying this Formation.|<1838 +/- 5 Ma (Cross and Crispe, 2007).|||Stratigraphic equivalent of Lander Rock Formation.||12-JUL-16
35397|Killi Killi Formation|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Of Tanami Basin. Events: Alice Springs Orogeny; Tanami Orogeny D1t. Sample GSWA 177278 (metagreywacke) yielded a concordant age of 1844+\-36 Ma, interpreted as maximum depositional age for the greywacke. Sample GSWA 178803 (sandstone) yielded a weighted mean 207Pb*/206Pb* date of 1862+\-3 Ma,  interpreted as maximum depositional age of the sandstone. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|1840-1835 Ma (inferred)|Unit of Tanami Group.||Overlain by Dead Bullock Formation. Intruded by Balwina Granite.|Feldspathic metawacke, metasandstone, metasiltstone, and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite, and metagabbro|
35397|Killi Killi Formation|69618|4|Described|p89-99, p100 Tb.1, p102, p104, p106-110|Paleoproterozoic|Paleoproterozoic|Hosts the Coyote gold deposit. Sandier and more typical of turbidites than shale-rich Dead Bullock (and Stubbins) Formations. Thickness estimated c.4km. Boundary with Dead Bullock Formation revised upwards to move Madigan beds, Stubbins and Mount Charles Formations into the underlying Callie Member of the Dead Bullock Formation.|~1864-1844 Ma.|Unit in Tanami Group.||Conformably overlies Dead Bullock Formation.|Siliciclastic units: typically fine-grained interbedded shale-topped sandstones.|30-MAR-15
35397|Killi Killi Formation|69747|4|Described|p262,264-265|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton. Deposited in an active continental margin from a provenance predominantly containing Meso- to Neoarchaean granitic and minor mafic volcanic rocks near its base.|ca. 1864-1844 Ma|Unit of Tanami Group.||Upper unit of the Tanami Group. Underlain conformably by Dead Bullock Formation.|Fine- to coarse-grained, poorly sorted immature sandstone units that commonly grade upwards into siltstone and mudstone.|
35397|Killi Killi Formation|69917|6|Mentioned|p87|||Tanami Region. One of a number of North Australian Craton sources of zircons older than 1900 Ma. ||||||
35397|Killi Killi Formation|70024|6|Mentioned|p35|||||Tanami Group.||Conformably overlies Dead Bullock Formation.||
35397|Killi Killi Formation|70130|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.|||Contact-metamorphosed feldspathic metawacke, metasandstone, metasiltstone, and metamudstone; biotite zone.|
35397|Killi Killi Formation|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.||Overlies Stubbins Formation. Is overlain by Gardiner Sandstone.|Contact-metamorphosed feldspathic metawacke, metasandstone, metasiltstone and metamudstone; biotite zone.|
35397|Killi Killi Formation|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.||Tanami Group.||Is faulted against Slatey Creek Granite.|Biotite-zone contact metamorphosed feldspathic metawacke, metasandstone, metasiltstone and metamudstone.|
35397|Killi Killi Formation|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. The contact metamorphosed areas of this Formation are mapped separately.||Tanami Group.|||Feldspathic metawacke, metasandstone, metasiltstone and metamudstone; minor quartzite, banded metachert, metabasalt, metadolerite and metagabbro. Locally contact metamorphosed to biotite zone.|
35397|Killi Killi Formation|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1835-1840 Ma||||Feldspathic metawacke, metasandstone, metasiltstone, metamudstone, metadolerite and metagabbro, minor quartzite, banded metachert, and metabasalt|
35397|Killi Killi Formation|70291|4|Described|p178-179,181,183,185-189,191,199,201-202|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Provenance is likely from Kimberly region to the west. Maximum depositional age 1840 Ma. Intruded by foliated dolerite sills.|<1840 Ma|Unit of Tanami Group.||Upper unit of Tanami Group. Underlain by Dead Bullock Formation.|Coarse-grained turbiditic sandstone and silstone.|
35397|Killi Killi Formation|70478|5|Briefly described|p2 Fig 1, 3-4|Statherian|Paleoproterozoic|Geological Province: Tanami. Minimum, post-deformation age from Frederick Suite granodiorite intrusions at 1802+/-4 Ma, 1801+/-4 Ma.||Unit of Tanami Group||Intruded by Frederick Suite granite.||
35397|Killi Killi Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.||Overlies Callie Member (Dead Bullock Formation).|Micaceous greywacke, quartz greywacke, lithic greywacke, quartz sandstone, siltstone, graphitic siltstone, interbedded muscovite-bearing psammite and pelite, graded beds.|
35397|Killi Killi Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Tanami Group.||Overlies Dead Bullock Formation.||
35397|Killi Killi Formation|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Of Tanami Basin. 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.|1864-1830 Ma (inferred)|Unit of Tanami Group.|||Schistose to phyllitic greywacke, siltstone and shale; minor lithic sandstone, granule conglomerate, quartzite, banded chert, basalt and dolerite.|
35397|Killi Killi Formation|71302|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami region. Paleoproterozoic metasedimentary sequence exposed on the North Australian Craton, and possibly one of several sources of zircon provenance to the Inverway Metamorphics.||||||
35397|Killi Killi Formation|71348|6|Mentioned|p209,214-215|||Geological province: Tanami Region, North Australian Craton. See p215 for summary of U-Pb geochronological data.||||||
35397|Killi Killi Formation|71349|5|Briefly described|p724-725, p737|Paleoproterozoic|Paleoproterozoic|Tanami Region. Contains zircons aged c.3.1 Ga (significance explained).|1840 Ma.|Tanami Group.||Overlies Dead Bullock Formation.|Turbidites.|
35397|Killi Killi Formation|71397|4|Described|p1,5,22,46-48|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen. Deposited as part of a basin-floor fan system (Lamback et al., 2012). May have been formed at an active margin, possibly contiguous with Kimberley margin (Hollis et al., 2010; Hollis and Glass, 2012). Timing of deposition is constrained to after c. 1864 Ma (age of underlying Stubbins Formation), and before the 1840-1825 Ma Tanami Orogeny (Vandenberg et al., 2001). Contain detrital zircons with dominant age components at 1870-1860 Ma and at c. 2500 Ma; similar to that of Olympio Formation. Geochemical analysis suggest a similar sedimentary and chemical source to the Killi Killi and Olympio formations, and interpreted to have been derived from from granitic rocks of the Paperbark Supersuite in the Western Zone of the Lamboo Province (Hollis et al., 2014).|1864-1840 Ma|Unit of Tanami Group.|||Monotonous, variably micaceous and lithic, turbiditic metasandstone that are interbedded with metasiltstone.|
35397|Killi Killi Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1840+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Quartz wacke, greywacke, quartz arenite.|
35397|Killi Killi Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Tanami Basin, Granites-Tanami Orogen.||Tanami Group|||Feldspathic metawacke, metasandstone, metasiltstone, metamudstone, metadolerite, and metagabbro; minor quartzite, banded metachert, and metabasalt.|
35397|Killi Killi Formation|72366|5|Briefly described|p2|Orosirian|Orosirian|Geological province: Tanami Province. Age constrained by an overlying tuff with 1838+\-5 Ma magmatic crystallisation age (Cross and Crispe 2007). ||||Correlable to Lander Rock Formation.||
35397|Killi Killi Formation|72527|6|Mentioned|p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of a metasedimentary unit that has a similar detrital zircon spectra to Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a).||||||
35397|Killi Killi Formation|73089|4|Described|p: 3-8, 11, 13-16, 18, 20, 22-33, 41, 43|Orosirian|Orosirian|Granites-Tanami Orogen. Hosts some Au mineralisation. 4 km thick. Compositionally immature. Interpreted to have been deposited as part of an extensive turbidite system proximal to mid-fan. Relatively high proportion of sandy units deposited as channelized or sheet sand lobes. Geochron metasandstone sample numbers = GA2004085001 and GA 2001082009 [see report for geochon details]. Paleoproterozoic-dominated source terrain. Lithologically more homogeneous than the underlying Dead Bullock Formation.|1840-1820 Ma [1865-1840 Ma?].|Tanami Group||Transitionally underlain by Dead Bullock Formation. Unconformably overlain by Pargee Sandstone. Intruded by Lewis Granite. May correlate to Olympio Formation (Halls Creek Group).|Siliciclastic metasedimentary rocks including micaceous greywacke, quartz wacke, lithic greywacke, quartz and lithic arenite, siltstone and mudstone.|
35397|Killi Killi Formation|73158|4|Described|p2 Fig.1, p3, p9, p10 Fig.9|Orosirian|Orosirian|Granites-Tanami Orogen.|1868+/-7 Ma MDA|Tanami Group||Overlies Dead Bullock Formation|Greywacke deposited as turbidites with increasing thickness towards the west.|
35397|Killi Killi Formation|73159|5|Briefly described|p2 Fig.1, p3, 9, p10 Fig.9|Proterozoic|Proterozoic|Granites-Tanami Orogen. Sediments sourced from nearby continental margin. HFSE geochemical plots.|1866 +/- 7 Ma (MDA).|Tanami Group.||Overlies Dead Bullock Formation.|Felsic greywacke turbidites; thickness increases westwards.|
35397|Killi Killi Formation|73445|5|Briefly described|p7||||1864 +/- 6 Ma (MDA: Bagas et al., 2009).|||Is overlain unconformably by the Redcliff Pound Group.||
78971|King Member|70380|3|Fully described|p743, p748-752, p758-759|Middle Cambrian|Middle Cambrian|New name, after a section of the King River where outcrops occur. Up to 160.9 m thick; it is 58.3m thick in the type section which is the interval 51.5-109.8m depth in drillhole NTGS86/1. Daly Basin. Massive to coarsely bedded dolostone; traces only of terrigenous sediment. Deeper seawater deposits. Graphic logs of drillholes. Lithology and mineralogy described in some detail. Has undergone dolomitisation and later karstification.||Oolloo Dolostone.||Disconformably overlies Briggs Member. Is overlain unconformably by Florina Formation.|Mostly massive; dominated by pink crystalline dolostone, coarsening upwards; minor microbial and stromatolitic dolostone and quartzic dolostone in lower parts; sparse thin shale and mudstone intervals. Widespread development of solution cavities.|14-FEB-17
74210|Kingfisher Shale|61542|4|Described|p278, p277 Fig. 2, p284|Visean|Visean|Formerly referred to as Upper Milligans Formation. Overlies Utting Calcarenite with abrupt change in lithofacies; unconformably underlies Tanmurra Fm. Micaceous and carbonaceous claystone with minor siltstone????detailed lithology included.||||||07-FEB-11
74210|Kingfisher Shale|69452|3|Fully described|p36:9, 11-12, 14-17|Visean|Visean|Gorter et al. (2005). Petrel Sub-basin, Bonaparte Basin. The type section is in Kingfisher-1, where it is 140m thick. Moderately deep marine deposits. Up to 200m thick. Offshore and onshore (subsurface).||Weaber Group.||Conformably overlies Utting Calcarenite. Lateral equivalent of Burvill Formation. Is overlain unconformably by Tanmurra Formation.|Slightly micaceous and carbonaceous claystone with minor siltstone and fine to very fine sandstone. A relatively well described fauna and microflora.|12-JUL-16
74210|Kingfisher Shale|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Utting Calcarenite. Is overlain by Tanmurra Formation.||
74210|Kingfisher Shale|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||Overlies Yow Creek Formation, Utting Calcarenite, overlain by Tanmurra Formation, Wadeye Group|Micaceous and carbonaceous claystone with minor siltstone and sandstone.|
74210|Kingfisher Shale|70061|5|Briefly described|Petrel Sub-basin: Fig.3, p2|Visean|Visean|See also Regional geology: Fig.8, p11. Offshore S Petrel Sub-basin. Hydrocarbon source and regional seal, as well as gas reservoir in Bonaparte 2.||Weaber Group.||Overlies Utting Calcarenite. Is overlain by Tanmurra Formation.||
74210|Kingfisher Shale|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Overlain by Tanmurra Formation. Underlain by Utting Calcarenite. Equivalent to Burvill Formation.||
80334|Kings Legend Metadolerite|71621|5|Briefly described|p1, p21, 23, 39, p45-p46|||Aileron Province. Exposed in a creek bed 4km northwest of Bonya Bore in western Jervois Range. Formerly the Kings Legend Amphibolite of Freeman, 1986. Petrography and zircon description discussed.|No meaningful ICP-MS dating possible.|||Conformably interlayered with the Mascotte Orthogneiss, White Violet Orthogneiss and Bonya Metamorphics.|Metadolerite.|02-FEB-19
80334|Kings Legend Metadolerite|72370|5|Briefly described|p15-16|||Geological province: Aileron Province.  Age-equivalent to Attutra Metagabbro.||||Crosscut by Samarkand Pegmatite.||16-DEC-19
80334|Kings Legend Metadolerite|72372|5|Briefly described|p5,14|Statherian|Statherian|Geological province: Aileron Province. Intruded into Bonya Metamorphics at c. 1.79-1.77 Ga. Intruded by pegmatites at the contact with Bonya Metamorphics.||Unit of Baikal Supersuite.||Intrudes Bonya Metamorphics.||
80334|Kings Legend Metadolerite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.||Casper Suite|||Metadolerite: fine to medium-grained, aphyric to porphyritic or glomerophyric with primary igneous textures locally preserved.|
80334|Kings Legend Metadolerite|72516|2|Defined|p14-17, p19-21, p106-111, p204|Statherian|Statherian|The type locality occurs in the Bonya Hills (type area with 2 main localities): 614054mE 7484234mN and 614499mE 7480626mN. Largely restricted to the Bonya Domain with minor outcrops in the Jinka Domain. Formerly the Kings Legend Amphibolite Member of the "Bonya Schist" of Freeman (1986), the unit is named for the Kings Legend copper occurence in the southern Bonya Hills. Based on new mapping this unit has been separated from the Bonya Metamorphics and renamed. Interpreted to be coeval with the Attutra Metagabbro, no absolute age constraints. The main outcrops occur as prominent strike ridges with smaller scale intrusions forming low rubbly outcrop. Deposited in a continental margin environment. Also has conformably contacts with the White Violet Orthogneiss. Geochemistry, geophysics, distinguishing characteristics, alteration, mineralisation, structure and metamorphism are discussed. See also p24-25, p29-30, p32, p35, p37, p42-46, p60-61, p71, p75, p77, p123-124, p135-137, p142-143, p145, p169, p171, p173, p189, p192.||Casper Suite||Intrudes the Jericho Granite, Bonya Metamorphics, Mascotte Orthogneiss, White Violet Orthogneiss. Intruded by the Samarkand Pegmatite and Thring Granite.|Metadolerite; fine to medium-grained, aphyric to porphyritic or glomerophyric with primary igneous textures locally preserved; rare metasomatic assemblages; undeformed to locally foliated.|20-APR-22
80334|Kings Legend Metadolerite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Inlcudes Metadolerite.|
73692|Kiwirrkurra Formation|64580|4|Described|map legend|Neoproterozoic|Paleoproterozoic|Red-weathering lithic sandstone, quartz sandstone and conglomerate.||||||15-DEC-08
73692|Kiwirrkurra Formation|68994|4|Described|p1, p6-11, p17-19, p23, p25, p27|Neoproterozoic|Neoproterozoic|Not clear if it forms basal unit, or is older than, Amadeus Basin. Sample analysed is coarse-grained, pebbly sandstone. Detrital zircon U-Pb ages listed. Conservative max depositional age is 1633+/-6 Ma, however depositional age could be considerably younger (Kirkland et al. 2009). Hf analyses detailed.|>840 Ma.|||Unconformably overlies Pollock Hills Formation. Unconformably overlain by Heavitree Quartzite (contact not exposed).|Lithic sandstone, quartz sandstone, and conglomerate.|13-JAN-17
73692|Kiwirrkurra Formation|69003|6|Mentioned|p5|||West Arunta Orogen and Amadeus Basin.||||||
73692|Kiwirrkurra Formation|69510|6|Mentioned|p10|||Basal (western) Amadeus Basin. Mentioned as having close similarities with the detrital zircon spectrum of an un-named hematite-bearing quartzite aged 1236 +/- 64 Ma.||||||
73692|Kiwirrkurra Formation|69606|5|Briefly described|p4 fig 2|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.|||||Sandstone.|
73692|Kiwirrkurra Formation|70762|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|North Australian Craton.|||||Red-weathering lithic sandstone, quartz sandstone, and conglomerate.|
73692|Kiwirrkurra Formation|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1633+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
73692|Kiwirrkurra Formation|72034|5|Briefly described|500k_interpgeop16_lut|Neoproterozoic|Paleoproterozoic||Max age 1633+/-6 Ma, min ~1000 Ma.||||Red-weathering lithic sandstone, quartz sandstone, and conglomerate.|
41964|Knuckey Formation|23937|2|Defined|p81 App. 1|Calymmian|Statherian|Redefined as part of Nathan Group below Yalwarra Volcanics - formerly lower part of Kookaburra Creek Formation (McArthur Group). Age: 1614+/-4 and 1609+/-3Ma. Max. Thickness: ?150m. Geol. Prov: McArthur Basin. See also p18, p26 Fig. 12.||||||
41964|Knuckey Formation|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Nathan Group. Red-brown siltstone and mudstone; dololutite and dolomitic siltstone.||||||
41964|Knuckey Formation|69430|4|Described|p15:3, 24-25, 30|||Abbott et al. (2001). These rocks constituted the lower part of the former Kookaburra Creek Formation of Dunn (1963); included within Balbirini Dolostone (Jackson et al., 1987). Urapunga Fault Zone, McArthur Basin. 150m? thick. Subtidal to supratidal sediments.||Nathan Group.||Conformably and gradationally overlies Mount Birch Sandstone. Is overlain conformably by Yalwarra Volcanics. Is correlated with lower Balbirini Dolostone and lower Dook Creek Formation.|Dolomicrostone, dolomitic siltstone and sandstone, stromatolitic dolostone, mudstone and chert.|12-JUL-16
41964|Knuckey Formation|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Urapunga Fault Zone||Nathan Group||Overlain by Yalwarra Volcanics, Overlies Mount Birch Sandstone||
41964|Knuckey Formation|72373|4|Described|iii,p1,28,30,33-35|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Type section: 10km SSE of Mount Vizard in southern URAPUNGA. About 150m thick at type section. Sample 2771376 (UR18TJM075: Fine-grained quartz-lithic sandstone) yielded interpreted max depositional age of 1616+\-7 Ma. Detrital zirzona ge spectra indicate a shared provenance with Mount Birch Sandstone, with a divergence in younger zircon age spectra indicating that younger source areas become more influential in Knuckey Formation.|1616+\-7 Ma (max dep age)|Unit of Nathan Group.||Overlain by Yalwarra Volcanics. Underlain by Mount Birch Sandstone.|Recessive, sparsely exposed succession of dolomicrite, dolomitic siltstone and sandstone, stromatolitic dolostone, shale, mudstone and chert.|
41964|Knuckey Formation|72523|6|Mentioned|p12.|Mesoproterozoic|Mesoproterozoic|NTGS UR18TJM075; (Kositcin and Munson 2019: Fig. 42) - used as an example of provenance age spectrum similarity with Smythe Sandstone.||Nathan Group||||
41964|Knuckey Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin.||Nathan Group||Overlies Mount Birch Sandstone and underlies Yalwarra Volcanics.||
41964|Knuckey Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone.||Nathan Group||Underlain by Mount Birch Sandstone. Overlain by Yalwarra Volcanics.||
41964|Knuckey Formation|72912|5|Briefly described|p5 Fig.3.|Calymmian|Statherian|Located in the Urapunga Fault Zone.||Nathan Group||Overlies Mount Birch Sandstone and underlies Yalwarra Volcanics and is partially equivalent to Balbirini Dolostone and Smythe Sandstone.||
41964|Knuckey Formation|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Underlain by Mount Birch Sandstone. Overlain by Yalwarra Volcanics.||
33373|Kombolgie Subgroup|22538|6|Mentioned|P713, P715|||||||||
33373|Kombolgie Subgroup|23374|1|Redefined|Tb2p10,8,9,40,41,35,36,8,12,19,26,27,28||Statherian|Min Age: 1648+/-29Ma (Rb/Sr from the Nungbalgarri Volcanics - note, too young from regional constraints - probably reset??). Older than 1688+/-13Ma, younger than 1870-1850 Ma. Of Katherine River Group.||||||18-FEB-08
33373|Kombolgie Subgroup|23384|4|Described|p26|Statherian|Orosirian|Age: between 1822 Ma and >1720 Ma.||||||09-OCT-06
33373|Kombolgie Subgroup|23396|5|Briefly described|p 407 fig.2|||||||||
33373|Kombolgie Subgroup|23733|5|Briefly described|p32 Fig. 19|||Of Katherine River Group.||||||
33373|Kombolgie Subgroup|23867|3|Fully described|p3|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Replaces Kombolgie Formation.  Geological Province: McArthur Basin.  See also Table 1, Figs. 3 and 30.||||||07-NOV-08
33373|Kombolgie Subgroup|23937|5|Briefly described|p7|||Of the Katherine River Group.  On the KATHERINE sheet.  Geological Province: Calvert Superbasin.||||||
33373|Kombolgie Subgroup|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the Katherine River Group.  Age: 1815-1710Ma.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5 and p12 Fig.10.||||||07-NOV-08
33373|Kombolgie Subgroup|24050|3|Fully described|p12, p10|||Formerly Kombolgie Formation.||||||
33373|Kombolgie Subgroup|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
33373|Kombolgie Subgroup|24168|5|Briefly described|p646|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
33373|Kombolgie Subgroup|50545|4|Described|p113, p115||Paleoproterozoic|Age: 1822-1720 Ma. Base of Katherine River Group.||||||07-NOV-08
33373|Kombolgie Subgroup|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Includes McKay Sandstone, Marlgowa Sandstone, Gilruth Volcanic Member, Gumarrirnbang Sandstone, Nungbalgarri Volcanics, and Mamadawerre Sandstone. Geological Province: McArthur Basin.||||||30-NOV-04
33373|Kombolgie Subgroup|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group.  Geological Province: McArthur Basin.||||||14-JAN-05
33373|Kombolgie Subgroup|61560|5|Briefly described|p489|Paleoproterozoic|Paleoproterozoic|Includes the Gumarrirnbang Sandstone. ||||||07-NOV-08
33373|Kombolgie Subgroup|61572|5|Briefly described|p671 Tb. 1|||Fine to coarse, mostly quartz sandstones, and lesser basalt units. Max. thickness: ~600m. Geological Province: McArthur Basin.||||||
33373|Kombolgie Subgroup|62375|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Unconformably overlies: Plum Tree Creek Volcanics. Geological Province: Pine Creek Orogen.||||||09-FEB-10
33373|Kombolgie Subgroup|63866|5|Briefly described|p112, p117|Orosirian|Orosirian|Ranges in age from ca 1860 -1810 Ma (Page, OZCHRON). Numeric ages are interpreted as the maximum depositional age.|ca 1798 +/- 18 Ma (Polito et al, 2005)|Katherine River Group||||
33373|Kombolgie Subgroup|64817|6|Mentioned|p353 Fig.4 |||Arnhem Shelf, McArthur Basin.||Of the Katherine River Group.|Includes the McKay, Marlgowa, Gumarirnbang and Mamadawerre Sandstones; Oenpelli Dolerite; and Nungbalgarri Volcanics.|||
33373|Kombolgie Subgroup|64956|5|Briefly described|p64|||Unconformably overlies Tin Camp Granite. Geological province: Pine Creek Orogen.||||||07-FEB-11
33373|Kombolgie Subgroup|65232|5|Briefly described|p7 Fig. 6, p6 Fig. 5, p24|Palaeoproterozoic|Palaeoproterozoic|Lower part of Katherine River Group. Includes Mamadewerre Sandstone, Nungbalgarri Volcanics, Gumarrirnbang Sandstone, Gilruth Volcanic Member, and Marlgowa Sandstone. Oenpelli Dolerite intrudes. Fluvial sandstone, conglomerate, basalt. U +/- Au +/- PGE.||||||09-FEB-10
33373|Kombolgie Subgroup|66683|6|Mentioned|p368 Fig.3, p369, p378.|Paleoproterozoic|Paleoproterozoic|The article proposes that this unit overlies a much larger area of near-surface Neoarchean basement than hitherto recognised, with important implications for regional mineral prospectivity.||||Unconformably overlies Nabarlek Granite.||
33373|Kombolgie Subgroup|67057|4|Described|pp454-456, p461 Fig.6.|Paleoproterozoic|Paleoproterozoic|Six sequence stratigraphic packages are detailed.The clastic units were compartmentalised into diagenetic aquifers and aquitards during burial diagenesis, as early as 1798 Ma. Lithogeochemistry discussed in detail.|c.1822 Ma.|Basal unit in Katherine River Group.|Includes, in order, Mamadawerre Sandstone, Nungbalgarri Volcanics, Gumarrirnbang Sandstone, Gilruth Volcanics, Marlgowa Sandstone  and McKay Sandstone.|Unconformably overlies Nimbuwah Domain.|Unmetamorphosed sandstones and conglomerates and mafic volcanic rocks.|15-MAR-12
33373|Kombolgie Subgroup|67355|6|Mentioned|p7 Tb.2, p25-26, p60|||Suggested source of uranium for ARUF deposits.||Katherine River Group||||25-JAN-17
33373|Kombolgie Subgroup|67479|6|Mentioned|p16, p37||||||Includes the Mamadawerre Sandstone.|||
33373|Kombolgie Subgroup|67564|4|Described|p6 Table 2, p9 Fig.4, p39 Fig.20, p86.|Paleoproterozoic|Paleoproterozoic|Formerly Kombolgie Formation and McKay Sandstone.||Unit in Katherine River Group.|Includes Mamadawerre, Gumarrirnbang, Marlgowa and McKay Sandstones and Nungbalgarri Volcanics.|Is intruded by Oenpelli Dolerite.|Quartz sandstone, basalt.|
33373|Kombolgie Subgroup|67779|3|Fully described|p6 Fig.5, p24, p26, pp32-38, p41, p48.|Paleoproterozoic|Paleoproterozoic|Formerly Kombolgie Formation. Reference area is Kombolgie Creek in the South Alligator River area. Forms a high, dissected sandstone plateau in northwest McArthur Basin. Covers large area of Nimbuwah Complex. Constitutes the basal 1800 m of the Katherine River Group. Deposition began after 1818 Ma (overlies Nabarlek Granite of that age) and before 1798 Ma (oldest Ar/Ar age of diagenetic illite). Structures described in detail. Fluids from this unit were important in uranium mineralisation.||Unit in Katherine River Group.|Includes Mamadawerre, Gumarrirnbang, McKay and Marlgowa Sandstones; Nungbalgarri Volcanics; McAddens Creek, Birdie Creek, Henwood Creek Volcanic Members.|Unconformably overlies Nimbuwah Complex.|Conglomerate, quartz arenite; volcanic intervals in the lower part including basalt, tuff and tuffaceous siltstone.|
33373|Kombolgie Subgroup|67873|6|Mentioned|p21||||||Nungbalgarri Volcanics|||20-APR-18
33373|Kombolgie Subgroup|68575|6|Mentioned|p125|||McArthur Basin. Age distribution is remarkably similar to other basal McArthur Basin clastics (eg Westmoreland Conglomerate; Depot Creek Sandstone).||||||
33373|Kombolgie Subgroup|68697|6|Mentioned|vi, p36|||||||Unconformably overlies Cahill Formation.||
33373|Kombolgie Subgroup|68733|6|Mentioned|p186|||Northern McArthur Basin.|||Includes the Mamadawerre Sandstone (basal unit).|||05-DEC-17
33373|Kombolgie Subgroup|69418|6|Mentioned|p3:18-19|||McArthur Basin.||||||12-JUL-16
33373|Kombolgie Subgroup|69419|6|Mentioned|p4:6,|||McArthur Basin.||||||12-JUL-16
33373|Kombolgie Subgroup|69420|5|Briefly described|p5:23, 26, 65, 69, 81-82, 84, 116|Paleoproterozoic|Paleoproterozoic|Sandstones form escarpments. Hosts the ABC vein-type uranium deposit, and phosphate deposits.||Katherine River Group.|Mamadawerre Sandstone.|||12-JUL-16
33373|Kombolgie Subgroup|69430|4|Described|p15:3, 7-8, 11, 51|||NW McArthur Basin. Originally Kombolgie Formation of Walpole (1958), for one of his two Formations in the Katherine River Group. Later raised to Subgroup rank by Carson et al. (1999). Forms the spectacular escarpment country of the Arnhem Land Plateau. Age is constrained by the underlying and intrusive units. Hosts various U, Au and PGE prospects in western Arnhem Land (briefly described).|Between 1820 Ma and 1729 Ma.|Katherine River Group.|Mamadawerre, Gumarrirnbang, Marlgowa, McKay Sandstones; Nungbalgarri Volcanics.|Unconformably overlies Edith River Group. Is intruded by Oenpelli Dolerite. Lower part is probably equivalent to Westmoreland Conglomerate (Tawallah Group).|A succession of essentially fluvial sandstone and extrusive volcanic units.|12-JUL-16
33373|Kombolgie Subgroup|69577|5|Briefly described|p113, 117|Paleoproterozoic|Paleoproterozoic|Lower part of the McArthur Basin. Diagenetic illite dated 1798 +/- 13 Ma gives a minimum age constraint for deposition of the lower parts (at least) of the Subgroup.|<1818 Ma.|||Intruded by Oenpelli Dolerite.|Quartz sandstone, conglomerate, and mafic volcanic and volcaniclastic rocks.|
33373|Kombolgie Subgroup|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||||
33373|Kombolgie Subgroup|69917|5|Briefly described|p48, 201|||||||Correlated with Westmoreland Conglomerate of McArthur Basin. Unconformably underlain by Cahill Formation.||
33373|Kombolgie Subgroup|70293|6|Mentioned|p597-601, p612-615, p618-620|Statherian|Orosirian|McArthur Basin. Appears as Kombolgie subgroup on p597. Forms the scarps in Kakadu National Park and Arnhem Region. Maximum depositional age from peak diagenetic 40Ar/39Ar plateau age.|<1798 +/- 13 Ma (Polito et al., 2005).||Mamadewerre Sandstone, Nungbalgarri Volcanics|Overlies Edith River Group|Sedimentary and volcanic rocks.|
33373|Kombolgie Subgroup|70853|5|Briefly described|Map legend.|Statherian|Statherian|||Katherine River Group.|Mamadawerre, Gumarrirnbang Sandstones; Nungbalgarri Volcanics.|||
33373|Kombolgie Subgroup|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Katherine River Group.|Includes Mamadawerre Sandstone.|Overlies Geolsec Formation. Is overlain unconformably by Uniya Formation.||01-MAR-18
33373|Kombolgie Subgroup|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1832+/-14 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
33373|Kombolgie Subgroup|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Katherine River Group.||||
33373|Kombolgie Subgroup|72713|6|Mentioned|p4|||Pine Creek Orogen. Quartzites in 19U4DD002 were tentatively assigned to this unit [written as Kombolgie Subgroup?].||||Underlain by Cahill Formation.|Quartzite|
33373|Kombolgie Subgroup|73030|6|Mentioned|p2152|||Pine Creek Orogen.||||||
25130|Koolpin Formation|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Chert-banded carbonaceous siltstone and schist.||||||07-NOV-08
25130|Koolpin Formation|9691|5|Briefly described|Map Legend|||Of the South Alligator Group. Chert-banded carbonaceous siltstone and schist, characteristically stongly hematite stained at surface; hematite schist.||||||
25130|Koolpin Formation|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Chert-banded carbonaceous siltstone and schist, characteristically stongly hematite stained at surface; hematite schist.||||||02-JUN-05
25130|Koolpin Formation|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Chert banded carbonaceous siltstone and schist characteristically strongly hematite stained at surface; hematite schist.||||||
25130|Koolpin Formation|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
25130|Koolpin Formation|22810|5|Briefly described|Table2 P4|||Maximum thickness of 1000m||||||
25130|Koolpin Formation|23122|5|Briefly described|p409, Fig.2, 410|||||||||
25130|Koolpin Formation|23337|5|Briefly described|906|||||||||
25130|Koolpin Formation|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 7 table 1, page 12. Of South Alligator Group. Max. thickness 200 m.||||||
25130|Koolpin Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the South Alligator Group, in the Rum Jungle and Central Regions||||||
25130|Koolpin Formation|23733|5|Briefly described|p32 Fig. 19|||Of South Alligator Group.||||||
25130|Koolpin Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.  Siltstone, chert, shale, dolerite, banded iron formation.  Age: ~1885Ma.  Geological Province: Pine Creek Orogen.  See also p30 Fig. 23.||||||07-NOV-08
25130|Koolpin Formation|24197|6|Mentioned|p25|||Carbonate-rich rocks which host Pb and Zn.||||||07-FEB-11
25130|Koolpin Formation|24260|4|Described|p1014 Fig.2|||Overlain by Gerowie Tuff Formation; underlain by Wildman Sandstone. Geological Province: Pine Creek Inlier.||||||07-JAN-09
25130|Koolpin Formation|24442|6|Mentioned|p27|||||||||
25130|Koolpin Formation|29423|6|Mentioned|p304|||||||||
25130|Koolpin Formation|29551|6|Mentioned|p27|||||||||
25130|Koolpin Formation|29552|6|Mentioned|p37|||Map legend||||||
25130|Koolpin Formation|29599|5|Briefly described|p30|||||||||
25130|Koolpin Formation|30142|6|Mentioned|p12|||||||||
25130|Koolpin Formation|30319|6|Mentioned|p270|||||||||
25130|Koolpin Formation|30558|6|Mentioned|p39|||||||||
25130|Koolpin Formation|30559|6|Mentioned|p281|||||||||
25130|Koolpin Formation|30680|6|Mentioned|p309|||||||||
25130|Koolpin Formation|30830|5|Briefly described|p301|||||||||
25130|Koolpin Formation|30831|6|Mentioned|p1|||||||||
25130|Koolpin Formation|30863|6|Mentioned|p50|||||||||
25130|Koolpin Formation|30912|6|Mentioned|p367|||Lower Proterozoic||||||
25130|Koolpin Formation|31268|6|Mentioned|p21|||||||||
25130|Koolpin Formation|31347|6|Mentioned|p135|||||||||
25130|Koolpin Formation|31824|6|Mentioned|p28|||L.Proterozoic. Lithology||||||
25130|Koolpin Formation|31833|6|Mentioned|p27|||||||||
25130|Koolpin Formation|32144|6|Mentioned|p96|||Fossil evidence||||||
25130|Koolpin Formation|32397|5|Briefly described|p397|||||||||
25130|Koolpin Formation|32660|5|Briefly described|Table 2|||||||||
25130|Koolpin Formation|32758|6|Mentioned|p63|||||||||
25130|Koolpin Formation|32932|4|Described|p324|||||||||
25130|Koolpin Formation|33031|6|Mentioned|p16|||||||||
25130|Koolpin Formation|33084|6|Mentioned|p5|||||||||
25130|Koolpin Formation|33186|3|Fully described|p288|||||||||
25130|Koolpin Formation|33225|6|Mentioned|p20|||||||||
25130|Koolpin Formation|34528|6|Mentioned|p18|||Lower Proterozoic. See also PP19,21,23||||||
25130|Koolpin Formation|34925|6|Mentioned|p125|||||||||
25130|Koolpin Formation|35055|6|Mentioned|p222|||||||||
25130|Koolpin Formation|35064|6|Mentioned|p208|||||||||
25130|Koolpin Formation|35140|6|Mentioned|Fig.1|||||||||
25130|Koolpin Formation|35256|6|Mentioned|p18|||||||||
25130|Koolpin Formation|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
25130|Koolpin Formation|36085|6|Mentioned|p502|||||||||
25130|Koolpin Formation|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|37462|6|Mentioned|Fig.4.8|||||||||
25130|Koolpin Formation|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.||||||07-NOV-08
25130|Koolpin Formation|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|38239|6|Mentioned|p9|||See also Fig.2.||||||
25130|Koolpin Formation|38349|6|Mentioned|p14|||||||||
25130|Koolpin Formation|38351|4|Described|p10|||||||||
25130|Koolpin Formation|38557|5|Briefly described|p287|||||||||
25130|Koolpin Formation|38740|6|Mentioned|p304|||||||||
25130|Koolpin Formation|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|39069|5|Briefly described|Table 1|||||||||
25130|Koolpin Formation|39210|6|Mentioned|p84|||||||||
25130|Koolpin Formation|39357|4|Described|p9|||See also p3.||||||09-OCT-06
25130|Koolpin Formation|39518|3|Fully described|p6|||||||||
25130|Koolpin Formation|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Shale and siltstone, commonly carbonaceous and in places containing gypsum casts.||||||07-NOV-08
25130|Koolpin Formation|40103|6|Mentioned|p185|||||||||
25130|Koolpin Formation|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Ferruginous and carbonaceous phyllite with chert bands, lenses and nodules in places; minor massive limonitic ironstone, silicified dolomite, marl.||||||07-NOV-08
25130|Koolpin Formation|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Brown ferruginous siltstone, shale and phyllite commonly carbonaceous and containing chert bands, lenses and nodules, massive ironstone.||||||07-NOV-08
25130|Koolpin Formation|40243|6|Mentioned|p142|||Mention Fig.2||||||
25130|Koolpin Formation|40493|5|Briefly described|Table 1|||||||||
25130|Koolpin Formation|40495|6|Mentioned|Fig.5|||||||||
25130|Koolpin Formation|40808|5|Briefly described|p13|||||||||
25130|Koolpin Formation|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|40861|6|Mentioned|p122|||||||||
25130|Koolpin Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|41125|6|Mentioned|p26|||See also Fig.6||||||
25130|Koolpin Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25130|Koolpin Formation|41305|3|Fully described|p16|||||||||
25130|Koolpin Formation|41309|4|Described|p5|||||||||
25130|Koolpin Formation|41311|4|Described|p10|||||||||
25130|Koolpin Formation|41397|4|Described|p8|||||||||
25130|Koolpin Formation|41407|6|Mentioned|Map legend|Proterozoic||||||||
25130|Koolpin Formation|41594|6|Mentioned|p20|||||||||
25130|Koolpin Formation|41663|6|Mentioned|p38|||||||||
25130|Koolpin Formation|41846|6|Mentioned|p102|||||||||
25130|Koolpin Formation|41873|5|Briefly described|Table 2|||||||||
25130|Koolpin Formation|41874|5|Briefly described|Fig.8|||||||||
25130|Koolpin Formation|41875|4|Described|p18|||Divided into 3 members, Lower, Middle and Upper.||||||09-OCT-06
25130|Koolpin Formation|41876|6|Mentioned|p21|||||||||
25130|Koolpin Formation|41877|6|Mentioned|p31|||||||||
25130|Koolpin Formation|41878|6|Mentioned|p36|||||||||
25130|Koolpin Formation|41980|6|Mentioned|p571|||||||||
25130|Koolpin Formation|42012|3|Fully described|p7|||See also Table p7.||||||09-OCT-06
25130|Koolpin Formation|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
25130|Koolpin Formation|42163|6|Mentioned|p61|||||||||
25130|Koolpin Formation|42344|6|Mentioned|p54|||||||||
25130|Koolpin Formation|42756|6|Mentioned|p7|||||||||
25130|Koolpin Formation|43115|6|Mentioned|p181|||||||||
25130|Koolpin Formation|43140|4|Described|p3||Paleoproterozoic|Of South Alligator Group.||||||07-NOV-08
25130|Koolpin Formation|43187|5|Briefly described|p2|||||||||
25130|Koolpin Formation|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|Max. thickness: 1000m.||||||07-NOV-08
25130|Koolpin Formation|43718|6|Mentioned|p23|||||||||
25130|Koolpin Formation|43720|5|Briefly described|p5|||||||||
25130|Koolpin Formation|43726|5|Briefly described|p3|||||||||
25130|Koolpin Formation|43832|3|Fully described|12,16-17,97||Paleoproterozoic|||||||07-NOV-08
25130|Koolpin Formation|44399|5|Briefly described|map legend||Paleoproterozoic|Of the South Alligator Group.  Carbonaceous pyritic siltstone with chert lenses, bands and nodules; discontinuous algal bioherms dolomite, dolomite breccia, silicified in places.||||||07-NOV-08
25130|Koolpin Formation|45022|4|Described|p.48||Paleoproterozoic|Of South Alligator Group.  On many pages.||||||07-NOV-08
25130|Koolpin Formation|45121|6|Mentioned|p7|||||||||
25130|Koolpin Formation|46163|14|Not recorded|p.168,170-3|||Unit of South Alligator Group. Overlies & interfingers with Gerowie Chert & Fisher Creek Siltstone.||||||
25130|Koolpin Formation|46658|5|Briefly described|p550|||||||||
25130|Koolpin Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.  Shale and siltstone, commonly carbonaceous and pyritic and containing in places gypsum casts; massive to rubbly ironstone commonly containing paraquartzite breccia; minor shale with chert or paraquartzite nodules.||||||07-NOV-08
25130|Koolpin Formation|46678|5|Briefly described|Table 1|Proterozoic|Proterozoic|Of South Alligator Group.  Algal dolomite as discontinuous bioherms in places at base: pyritic carbonaceous siltstone with chert (afetr dolomite) lenses nodules and bands, carbonaceous siltstone.  Estimated thickness: up to 3,000 feet.||||||
25130|Koolpin Formation|46700|5|Briefly described|P14, Table1 P10||Proterozoic|||||||
25130|Koolpin Formation|46824|6|Mentioned|Table 2|||See also P322||||||
25130|Koolpin Formation|46877|6|Mentioned|Fig.1|||||||||
25130|Koolpin Formation|47049|5|Briefly described|Table|||Restricted to areas west Waterfall Ck Fault. See Fig.2.||||||
25130|Koolpin Formation|48981|5|Briefly described|p2|||||||||
25130|Koolpin Formation|49744|5|Briefly described|Fig.3|||||||||
25130|Koolpin Formation|50586|6|Mentioned|p4.5|||Intruded by Cullen Supersuite.||||||
25130|Koolpin Formation|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Of South Alligator Group.||||||07-NOV-08
25130|Koolpin Formation|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Ferruginous siltstone and shale with chert bands, lenses and nodules; silicified dolomite lenses. Breccia common at base. Overlies: Wildman Siltstone. Underlies: Gerowie Tuff.||||||02-NOV-04
25130|Koolpin Formation|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the South Alligator Group. Chert-banded carbonaceous siltstone and schist characteristically strongly hematite stained at surface; hematite schist.||||||
25130|Koolpin Formation|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the South Alligator Group.  Contains the Ella Creek Member.||||||
25130|Koolpin Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Carbonaceous and ferruginous siltstone and shale, with chert bands and nodules. Overlies Wildman Siltstone. Overlain by Gerowie Tuff. Of South Alligator Group.||||||11-JAN-05
25130|Koolpin Formation|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the South Alligator Group.  Geological Province: Pine Creek Orogen. Haematitic metasiltstone and phyllite with  chert bands, lenses and nodules; graphitic phyllite and slate; silicified doloutite with rare stromatolites, chert breccia.||||||14-JAN-05
25130|Koolpin Formation|61389|5|Briefly described|Map Legend|||Of the South Alligator Group. Shale and siltstone, commonly carbonaceous, gypsum casts in places.||||||09-OCT-06
25130|Koolpin Formation|61861|6|Mentioned|p12|||Lithologically similar to Dead Bullock Formation.||Unit in South Alligator Group.||||
25130|Koolpin Formation|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Siltstone, chert, shale, dolerite, banded iron formation. Geological Province: Pine Creek Orogen. Underlies: Gerowie Tuff.||||||09-FEB-10
25130|Koolpin Formation|62378|5|Briefly described|p8|||Geological Province: Pine Creek Orogen. Underlies Gerowie Tuff conformably.||||||
25130|Koolpin Formation|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1863-2025Ma. Of South Alligator Group. Max thick 350m. Haematitic metasiltst and phyllite with chert bands, lenses and nodules; graphitic phyllite and slate; silicified dololutite w rare stromatolites, chert breccia; minor BIF and qtz metagreywacke.||||||07-JAN-09
25130|Koolpin Formation|64730|5|Briefly described|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Age from dates of the overlying Gerowie Tuff.|Min. depositional age 1863 +/- 2 Ma.|Of South Alligator Group.|||Carbonaceous and pyritic shales and cherts.|02-MAY-12
25130|Koolpin Formation|65232|5|Briefly described|p45, 46, 51, p6 Fig. 5, App. 2|Palaeoproterozoic|Palaeoproterozoic|South Alligator Group base. Incl: Ella Creek Member. Overlies Mount Partridge Gp (unconform). Underlies Mount Bonnie Fm (conform) and Coronation Sst (unconform). Faulted against Pul Pul Rhyolite. Primary U minerals.||||||09-FEB-10
25130|Koolpin Formation|65339|4|Described|p6 Table 1, p12. |||Thickness to 200 m. Outcrops as strike ridges and dark, rubbly ferruginous hills. Has high U radiometric response||Unit in South Alligator Group.|Includes Ella Creek Member.|Unconformably overlies Mount Partridge Group. Is overlain by Gerowie Tuff. Is intruded by Zamu Dolerite sills.|Carbonaceous and ferruginous siltstone and shale with chert bands and nodules, ferruginous breccia, minor silicified dolostone.|
25130|Koolpin Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in South Alligator Group.|Includes Ella Creek Member.|Is overlain by Gerowie Tuff.|Ferruginous metasiltstone and phyllite with chert bands, lenses and nodules; graphitic phyllite and slate; silicified dololutite with rare stromatolites, chert breccia; minor banded ironstone and quartz metagreywacke.|23-NOV-11
25130|Koolpin Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.||South Alligator Group.||||
25130|Koolpin Formation|67355|5|Briefly described|p6-7, p10, p12-13||Orosirian|Deposited during a thermal subsidence phase, following cessation of major extension and normal faulting. Divided into three informal units based on lithology. Maximum thickness of ~800 m.||South Alligator Group|Ella Creek Member (basal).|Overlies the Wildman Siltstone unconformably, underlies the Gerowie Tuff.|Ferruginous and carbonaceous shale and siltstone, with minor cherty horizons. Characteristic chert nodule, banded ironstone and tourmalinite beds. Tuffaceous interbeds.|25-JAN-17
25130|Koolpin Formation|67564|3|Fully described|p7 Table 2, p9 Fig.4, pp19-21, p23. |Paleoproterozoic|Paleoproterozoic|350 m of low-energy supratidal (carbonate rocks) to subtidal shallow marine (pelitic) deposits. Hosts uranium. Includes dolomitic lenses near Moline previously mapped by Stuart-Smith et al. (1998a) as Mount Bonnie Formation. Deformation has produced a folded thrust imbricate system. Has developed a ferricrete crust. Au and U mineralisation is related to reverse faults at the contact with Coronaton Sandstone.|c.1865 Ma.|Basal unit in South Alligator Group.||Is conformably overlain by Gerowie Tuff and Shovel Billabong Andesite.|Hematitic metasiltstone and phyllite with chert bands, lenses and nodules; graphitic phyllite and slate; silicified dolomudstone; minor quartz metagreywacke.|
25130|Koolpin Formation|67779|5|Briefly described|p6 Fig.5, p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Hosts uranium mineralisation in the South Alligator Valley.||Basal unit in South Alligator Group.||Is overlain by Gerowie Tuff.||
25130|Koolpin Formation|67824|5|Briefly described|p383|Orosirian|Orosirian|Ages based on detrital zircons and an overlying tuffaceous unit.|~2020-1860 Ma|Of the South Alligator Group.|||Iron-rich siltstones and mudstones.|
25130|Koolpin Formation|69383|5|Briefly described|p10, 28|||Sample AL07JHO242B from area previously assigned to this unit. Currently assigned to Cahill Formation.||||Intruded by Mount Bundy Syenite.||
25130|Koolpin Formation|69418|6|Mentioned|p3:6-7, 11, 17|||Pine Creek Orogen. Hosts a number of gold deposits, as well as the Evelyn Zn-Pb-Cd-Au deposit (described). Also hosts the South Alligator Valley Mineral Field (all workings) unconformity-related U deposits (described).||||||12-JUL-16
25130|Koolpin Formation|69420|4|Described|p5:4, 6, 8, 11-12, 15, 34, 36-39, 49-50|Paleoproterozoic|Paleoproterozoic|See also 52-53, 60, 63-65, 67, 78-82, 85-87, 99, 103, 112, 117. Central and South Alligator regions, Central Domain, Pine Creek Orogen. Up to 350m thick. Low-energy supratidal to subtidal shallow-marine deposits. Regional section from drillholes; lithologies described in some detail. Hosts Au deposits in various goldfields (described in some detail). Hosts small U deposits (described) and Cu deposits, as well as skarn-related Pb-Zn-Ag deposits adjacent to the Allamber Springs Granite. Hosts fluorite veins at the Olive prospect, and minor graphite occurrences in the Golden Dyke Dome area.||South Alligator Group.|Ella Creek Member.|Is overlain by Gerowie Tuff. Is intruded by Shoobridge and Burnside Granites.|Haematitic metasiltstone and phyllite with chert bands, lenses and nodules; graphitic phyllite and slate; silicified dolomudstone; minor quartz metagreywacke; basal ironstone breccia.|12-JUL-16
25130|Koolpin Formation|69426|6|Mentioned|p11:23|||Pine Creek Orogen. Similar lithologies to those in The Granites goldfield; suggested protoliths of basaltic to andesitic origin.||||||12-JUL-16
25130|Koolpin Formation|70293|5|Briefly described|p597, p599-601, p603, p607, p619-620|Orosirian|Orosirian|||Basal South Alligator Group.||Overlain by Gerowie Tuff, intruded by Zamu Dolerite|Dolomite/limestone and minor black (graphitic) shale.|
25130|Koolpin Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||South Alligator Group.||Unconformably overlies Mount Partridge Group. Is overlain conformably by Gerowie Tuff.|Ferruginous metasiltstone and phyllite with chert bands, lenses and nodules; graphitic phyllite and slate; silicified dolomudstone with rare stromatolites; chert breccia; minor banded ironstone and quartz metagreywacke.|
74950|Koolpinyah Dolostone|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Misspelling or variation on Koolpinyah Dolomite. Age ~2026-2500Ma. Of Mount Partridge Group. Dolomitic marble, dolomitic mica schist, mica squartz schist, dolomitic limestone, calcareous quartzite.||||||07-JAN-09
74950|Koolpinyah Dolostone|64730|5|Briefly described|p125 Fig. 3|Orosirian|Orosirian|Age from tuffaceous beds in the Wildman Siltstone near the top of the Group.|Min. deposition age 2019 +/- 4 Ma.|Of Mount Partridge Group.||||03-MAY-12
74950|Koolpinyah Dolostone|65339|4|Described|p6 Table 1, p10, p19.|||Outcrops nowhere; all stratigraphic information comes from drillholes and waterbores. Equivalent to the Coomalie Dolostone, as a shelf around the Woolner Granite. Produces high gravity readings. A major aquifer in the map area.||Unit in Mount Partridge Group.||Overlies Whites Formation. Is overlain by Wildman Siltstone.|Grey silicified dolostone interbedded with chlorite schist; dolomitic marble, dolomitic mica schist, dolomitic limestone, calcareous quartzite.|
74950|Koolpinyah Dolostone|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Mount Partridge Group.||Overlies Crater Formation. Is overlain by Wildman Siltstone.||
74950|Koolpinyah Dolostone|69419|6|Mentioned|p4:4,|||||||Unconformably overlies Woolner Granite.||12-JUL-16
74950|Koolpinyah Dolostone|69420|4|Described|p5:4, 8, 11|Paleoproterozoic|Paleoproterozoic|Pietsch and Stuart-Smith (1987); description mainly of drillhole intersections. Central Domain, Pine Creek Orogen. Shallow-marine to fluvial deposits.||Mount Partridge Group.||Overlies Crater Formation and (unconformably) the Woolner Granite and Dirtywater Metamorphics. Is overlain by Wildman Siltstone. Correlated with Coomalie Dolostone.|Dolomitic marble, dolomitic mica schist, dolomitic limestone, calcareous quartzite, conglomerate at base.|12-JUL-16
74950|Koolpinyah Dolostone|69456|5|Briefly described|p40:6|Proterozoic|Proterozoic|Pine Creek Orogen.||||Is overlain unconformably by Darwin Formation.||12-JUL-16
72419|Koonoonyeri Granite|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite granite, megacrystic K-feldspar bearing, Phyllonite, mylonite. Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
72419|Koonoonyeri Granite|64677|5|Briefly described|v, p1, p22-24, p53-54|||Donnellan (in prep.). Arunta Region, Aileron Province. Complex results discussed: zircons may have crystallised at c.1807 Ma and been variably reset by a later event (c.1793 Ma).|1792.8 +/- 2.7 Ma ( crystallisation age).||||Grey biotite granite with equant K-feldspar megacrysts.|
72419|Koonoonyeri Granite|65338|3|Fully described|App 1 p81-82, p22, pp27-28, App2|Statherian|Statherian|Newly defined. Of Stafford Event age. Contains inherited zircons, some of which, at c.1807 Ma, are only marginally older than the granite crystallisation. Deformation is restricted to phyllonitic zones that reflect shearing during Alice Springs Orogeny. Geochemical analysis of samples MP01ND036, MP01ND037 given.|1793 +/- 3 Ma (Worden et al. 2006).|||Intrudes probable Lander Rock Formation. Is unconformably overlain by Vaughan Springs Quartzite.|Grey, biotite-granite with equant K-feldspar megacrysts; blue quartz; discrete low-magnetic, high-U phase typically deeply weathered; rapakivi textured; locally to regionally gneissic granite; locally mylonitic to phyllonitic.|
72419|Koonoonyeri Granite|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province. A discrete phase with a high radiometric response is mapped separately.|||||Biotite-granite, megacrystic K-feldspar-bearing, phyllonite, mylonite.|
72419|Koonoonyeri Granite|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province. A phase of this unit with high radiometric response is mapped separately.|||||Biotite granite, megacrystic K-feldspar-bearing, phyllonite, mylonite.|
72419|Koonoonyeri Granite|69427|5|Briefly described|p12:20 Fig.12.19; 12:21|Statherian|Statherian|Aileron Province. Crops out peripherally to the Nanga Range. Deformed prior to full crystallisation, hence immediately pre- to syntectonic with respect to the Stafford Event. SHRIMP U-Pb zircon crystallisation age.|1793 +/- 3 Ma (Worden et al., 2008).|||Is overlain by Vaughan Springs Quartzite.|Grey biotite granite with equant K-feldspar megacrysts, characteristically without rapakivi textures. Deformation in discrete zones of phyllonite or mylonitisation.|12-JUL-16
72419|Koonoonyeri Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1793+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
72419|Koonoonyeri Granite|71858|6|Mentioned|p5|||Aileron Province.||||||
24345|Kudinga Basalt|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup, Hatches Creek Group. Amygdaloidal massive basalt with minor interlayered arenite.||||||07-NOV-08
24345|Kudinga Basalt|23733|6|Mentioned|p2|||||||||
24345|Kudinga Basalt|23809|5|Briefly described|p27 Fig. 25|||Of the Wauchope Subgroup (upper part).  Geological Province: Davenport Province.||||||
24345|Kudinga Basalt|24172|5|Briefly described|p37|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Overlain by Errolola Sandstone; underlain by Coulters Sandstone. Max. Thickness: 150m. Seperates the Coulters Sandstone amd Errolola Sandstone.||||||07-NOV-08
24345|Kudinga Basalt|24173|6|Mentioned|p23|||Possible correlative of Kimberley Group.||||||06-APR-05
24345|Kudinga Basalt|39624|5|Briefly described|Table 1|||||||||
24345|Kudinga Basalt|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24345|Kudinga Basalt|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Amygdaloidal to massive basalt; minor interlayered arenite.||||||10-JAN-05
24345|Kudinga Basalt|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24345|Kudinga Basalt|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24345|Kudinga Basalt|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Amygdaloidal to massive basalt lava, epidotic and chloritic; minor interlayered arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24345|Kudinga Basalt|41129|6|Mentioned|p5|||||||||
24345|Kudinga Basalt|41204|4|Described|Table 1|||||||||
24345|Kudinga Basalt|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Basalt lava; feldspathic/lithic/quartz arenite; minor trachyte.||||||16-NOV-05
24345|Kudinga Basalt|41308|5|Briefly described|Table 2|||||||||
24345|Kudinga Basalt|41310|5|Briefly described|p12|||||||||
24345|Kudinga Basalt|41408|6|Mentioned|Map legend|Proterozoic||||||||
24345|Kudinga Basalt|41524|4|Described|Table 1|||||||||
24345|Kudinga Basalt|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Basalt; minor quartz arenite interbeds.||||||07-NOV-08
24345|Kudinga Basalt|41970|6|Mentioned|Fig.3 P333|||||||||
24345|Kudinga Basalt|42643|4|Described|p12, Table 1 p6|||||||||
24345|Kudinga Basalt|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Basaltic lava, minor trachyte and arenite, rare volcaniclastic siltstone.||||||07-NOV-08
24345|Kudinga Basalt|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup.||||||07-NOV-08
24345|Kudinga Basalt|43802|6|Mentioned|Table 1,p80|||||||||
24345|Kudinga Basalt|45167|3|Fully described|Table 1|||Of Wauchope Subgroup.||||||09-OCT-06
24345|Kudinga Basalt|49033|2|Defined|p23|Proterozoic|Proterozoic|||||||
24345|Kudinga Basalt|60681|5|Briefly described|Map legend|Statherian|Statherian| Of the Hatches Creek Group.  Basalt lava.  Geological Province: Davenport Province.||||||11-JAN-05
24345|Kudinga Basalt|60684|5|Briefly described|p12, p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Amygdaloidal basalt with minor interlayered sandstone.  Max. thickness: 150m. Stated in study to both underlie and overlie the Coulters Sandstone unit? (discrepancy?).||||||07-NOV-08
24345|Kudinga Basalt|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Upper Wauchope Subgroup (Hatches Creek Gp). Basaltic lava; feldspathic/lithic arenite and quartz arenite, minor trachyte; rare volcaniclastic arenite and siltstone, and chert. Overlies Coluters Sst and Frew River Fm; underlies the Errolola Sandstone. .||||||07-NOV-08
24345|Kudinga Basalt|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Of weathered, recessive, medium-grained basalt, and quartz and lithic arenite. Max. thickness: 300m. . Geological Province: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
24345|Kudinga Basalt|61861|6|Mentioned|p23|||Tennant Inlier. May correlate with the basalt horizon near the top of Coomarie Sandstone, Tanami Region.||Unit in Wauchope Subgroup.||||
24345|Kudinga Basalt|64735|4|Described|p206 Fig 2, p210, p214,|Orosirian|Orosirian|Lavas that are not known to have crystallised dateable magmatic phases; age from a magmatic baddeleyite in a dolerite sill believed to be an intrusive equivalent to this unit.|1810+/-4.5Ma (or 1811+/-5Ma).|Of Hatches Creek Group, Wauchope Subgroup.||Underlies Errolola Sandstone, Hanlon Subgroup; overlies Coulters Sandstone.||20-APR-12
24345|Kudinga Basalt|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Upper Wauchope Subgroup.||Wauchope Subgroup||||05-JAN-17
24345|Kudinga Basalt|65232|6|Mentioned|App. 2|||||||||09-FEB-10
24345|Kudinga Basalt|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of upper Wauchope Subgroup (Hatches Creek Group) Davenport Province. Overlies Coulters Sandstone, underlies Errolola Sandstone. Basaltic lava; feldspathic/lithic/volcanilithic/tuffaceous arenite, quartz arenite, siltstone. Cross-section only||||||
24345|Kudinga Basalt|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of upper Wauchope Subgroup (Hatches Creek Group), Davenport Province. Overlies Coulters Sandstone, underlies Errolola Sandstone. Non-outcropping. Inferred basaltic lava; feldspathic/lithic/volcanilithic/tuffaceous arenite, quartz arenite, siltstone.||||||
24345|Kudinga Basalt|65338|5|Briefly described|p6, p20.|||Correlated with the Whittington Range Volcanic Member of the Tomkinson Creek Group. Varies between 50 and 770 m thick.||Topmost unit in Wauchope Subgroup.|||Geographically widespread flood basalt succession, locally pillowed.|
24345|Kudinga Basalt|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup, Hatches Creek Group.||Overlies Frew River Formation. Is overlain (possibly unconformably) by Errolola Sandstone.|Amygdaloidal to massive basalt lava, epidotic and chloritic; minor interlayered arenite.|19-OCT-11
24345|Kudinga Basalt|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Hatches Creek Group.|||No outcrop: inferred basaltic lava; feldspathic/lithic/volcanilithic/tuffaceous arenite, quartz arenite, siltstone.|
24345|Kudinga Basalt|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Upper.||Overlies Coulters Sandstone and Frew River Formation. Is overlain by Errolola Sandstone.|Basaltic lava; feldspathic/lithic arenite and quartz arenite, minor trachyte; rare volcaniclastic arenite and siltstone, and chert.|
24345|Kudinga Basalt|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24345|Kudinga Basalt|67352|4|Described|p8, p9 Tb.1, p44 fig 48 |Orosirian|Orosirian|At top of Subgroup. A regionally extensive flood basalt.||Wauchope Subgroup||Overlies Frew River Formation (conformably). Overlain conformably by Errolola Sandstone.|Basalt: amygdaloidal and scoriaceous to massive, epidotic and chloritic alteration; minor interbedded arenite, some feldspathic: fine-to coarse-grained; minor thinly bedded basaltic tuff.|
24345|Kudinga Basalt|68518|3|Fully described|p6 Tb.1, p12-13|Proterozoic|Proterozoic|Thickness: 150-500 m. Type section: north of Elkedra Pound, from GR NS038754 (base) to GR NS042755 (top). Broad extent of formation, and absence of features of subaqueous eruption, indicate basaltic volcanism and clastic sedimentation on a broad fluvial plain or very shallow marine shlef.||At top of Wauchope Subgroup||Conformable on Frew River Formation; is overlain conformably by Errolola Sandstone and unconformably by Cambrian strata.|Recessive basaltic lava, commonly amygdaloidal; minor arenite. Ridge-forming arenite separated by band of recessive basalt, volcaniclastic (basaltic) arenite and micaceous arenite. Basalt is lateritised, but fresh mounds in places; calcrete common.|30-MAY-16
24345|Kudinga Basalt|69424|6|Mentioned|p9:4, 10 Fig.9.9, 28, 34|Paleoproterozoic|Paleoproterozoic|Davenport Province. Regionally widespread (flood) basalt.||||Correlative of Whittington Range Member.||12-JUL-16
24345|Kudinga Basalt|69425|4|Described|p10:1, 3, 10-12, 17-21|||Davenport and Tomkinson Provinces. Topmost unit in Wauchope Subgroup. Widespread flood basalts: a distinctive marker interval. Broad shallow-water shelf. Thickness varies from c.50m to c.770m. Interpreted to be contemporaneous with c.1811 Ma intrusive mafic magmatism of the Mount Hay Event. The sandstones are feldspathic, lithic or quartz; rarely volcaniclastic.|1811 +/- 5 Ma (Claoue-Long et al., 2008).|Wauchope Subgroup, upper.||Conformably overlies Frew River Formation (also part lateral equivalent) and Coulters Sandstone. Is overlain conformably by Errolola Sandstone. Correlated with Whittington Range Member (in part).|Basalt, basaltic andesite, mugearite, shoshonite and potassic trachybasalt lava; rarely porphyritic; commonly anygdaloidal, lateritised, epidotised and/or actinolised. Minor trachyte lava locally. Subordinate sandstones; rare siltstone, chert.|12-JUL-16
24345|Kudinga Basalt|69431|5|Briefly described|p16:5, 8, 14|||Davenport Province.||Wauchope Subgroup.||Probable correlative of Whittington Range Member.||12-JUL-16
24345|Kudinga Basalt|73083|6|Mentioned|p9-10, p13-14, p19, p21-23|||Davenport Province. Strongly magnetic. Topmost unit of the Upper Wauchope Subgroup. Has a moderate dip in most places.||Wauchope Subgroup, Hatches Creek Group||Underlain by Coulter Sandstone and Unimbra Sandstone. Overlain by Errolola Sandstone.||
38420|Kuerschner Member|24303|2|Defined|p7, p55 Appendix|Statherian|Statherian|Of the Morphett Creek Formation. ?Overlain by the Hayward Creek Formation; unconformably overlies the Whittington Range Member. Max. Thickness: ~1600m. Formerly undifferentiated Tomkinson Creek beds.||||||18-OCT-05
38420|Kuerschner Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Morphett Creek Formation.  Sandst; sublithic to quartz arenite; thin to very thick bedded, medium-grained to pebbly; crossbedded, laminated, rippled, dessicated; pebbly sandstone, conglomerate, mudstone; rip-up clasts, halite pseudomorphs.||||||07-NOV-08
38420|Kuerschner Member|69425|5|Briefly described|p10:12|||Tomkinson Province.||Morphett Creek Formation.||Correlated in part with Alinjabon and Errolola Sandstones.||11-JUL-16
38420|Kuerschner Member|69431|4|Described|p16:6, 8-9|||Tomkinson Province. Probably fluviatile deposits. c.1500-1600m thick. Lithology described in some detail. Forms sandstone ridges alternating with recessive intervals.||Morphett Creek Formation.||Overlies Whittington Range Member. Is overlain gradationally by Mitty Member and Deagan Member (Short Range Sandstone).|Basal conglomerate up to 200m thick, overlain by 300m of lithic and sublithic feldspar-bearing sandstone and minor siltstone; the upper 1100m comprises lithic to sublithic sandstone characterised by abundant weathered-out shale clasts.|11-JUL-16
75502|Kukalak Gneiss|66683|5|Briefly described|p368 Fig.3, p372 Table 3, p378.|||Hollis et al.(2009a) propose this name for those layered biotite quartzofeldspathic gneisses in Arnhem Land, structurally underlying the Kakadu Group, with crystallisation ages between or close to c.2530-2510 Ma. The contact relationships between the Kukalak and Arrarra Gneiss are not clear, due to poor exposure. A plausible relationship is that the Kukalak Gneiss protolith intruded the Arrarra Gneiss at 2530-2510Ma and the composite granitic package was transposed and interleaved by subsequent tectonism, probably during ca. 1865Ma tectonometamorphism.|Protolith age 2527 +/- 3 Ma to 2510 +/- 4 Ma.|||||10-DEC-12
75502|Kukalak Gneiss|67057|6|Mentioned|p454, p457. |||Hosts unconformity-related uranium deposits. Part of the basement in the Nimbuwah Domain.||||||
75502|Kukalak Gneiss|67232|5|Briefly described|p2, p3 Fig.2. |Neoarchean|Neoarchean|Nimbuwah Domain basement, Pine Creek Orogen.|2527 - 2510 Ma.|||||
75502|Kukalak Gneiss|67479|5|Briefly described|p2 Tb.1, p6, pp28-35, p55, p56, p71-73|Neoarchean|Neoarchean|Myra Falls Inlier. Previously mapped as the Myra Falls Metamorphics. Weighted mean 207Pb/206Pb age.|2527 +/- 3 Ma (Magmatic emplacement age).|||Overlain by the Kudjumarndi Quartzite.|Layered leucocratic gneiss.|24-JAN-17
75502|Kukalak Gneiss|67779|2|Defined|p6 Fig.5, p10 Table 1, pp12-14, p117.|Neoarchean|Neoarchean|New name, after Kukalak region (Warddeken Indigenous Area), western Arnhem Land.Reference area is river-polished platform along creek beds in Tin Camp Creek. Previously mapped as part of Myra Falls Metamorphics (Dunn, 9162) and Nimbuwah Complex (Needham et al. 1982). Nimbuwah Domain, Pine Creek Orogen. Has a deep gravity low. Ages are from Myra Falls and Caramal Inliers respectively; a drillcore sample yielded a third SHRIMP zircon Pb/Pb age of 2513 +/- 14 Ma (Carson et al. 2010). Structures, geochemistry and geochronology are described in detail. Correlated with Nanambu, Rum Jungle and Billabong Complexes and possibly Black Angel Gneiss.|2527 +/- 3 - 2510 +/- 4 Ma (Hollis et al. 2009c).|||Probably intrudes Arrarra and Njibinjibinj Gneisses.|A highly strained, compositionally layered quartzofeldspathic biotite granodioritic gneiss: minor amphibolite and sillimanite-mica schist lenses; well-developed gneissosity.|14-MAY-18
75502|Kukalak Gneiss|68697|5|Briefly described|vi, p2, p32-35|Neoarchean|Neoarchean|Nimbuwah Domain, Pine Creek Orogen. Of Hollis et al. (2009), for those layered biotite quartzo-feldspathic gneisses structurally underlying the Kakadu Group in Arnhem Land that have a crystallisation age between or close to c.2530-2510 Ma. Previously known as Myra Falls Metamorphics. No reliable age could be determined from the one sample in this study. Previous SHRIMP U-Pb crystallisation age determinations gave ages of 2527 +/- 3 Ma, 2513 +/- 14 Ma and 2510 +/- 4 Ma (all Hollis et al., 2009). Probably related to Nanambu and Rum Jungle Complexes.|2527-2510 Ma.||||Typically a highly-strained, felsic-layered biotite quartzo-feldspathic orthogneiss with subordinate discontinuous amphibolite.|
75502|Kukalak Gneiss|68998|6|Mentioned|p33|Neoarchean|Neoarchean|Pine Creek Orogen.||||||
75502|Kukalak Gneiss|69419|5|Briefly described|p4:1-2, 6-8|Neoarchean|Neoarchean|Hollis et al. (2009). Nimbuwah Domain, Pine Creek Orogen. A collection of c.2500 Ma rock units; SHRIMP U-Pb zircon magmatic crystallisation ages range from 2527 +/- 3 Ma to 2510 +/- 4 Ma. Geochemistry briefly described.|||||Quartzofeldspathic gneisses.|12-JUL-16
75502|Kukalak Gneiss|69420|6|Mentioned|p5:4,6,8,23,38, 66-67, 85, 100, 111, 115|Archean|Archean|Part of the basement to the Nimbuwah Domain of the Pine Creek Orogen; western Arnhem Land.||||||12-JUL-16
75502|Kukalak Gneiss|69537|6|Mentioned|p6|Archean|Archean|Pine Creek Orogen.|c.2527-2510 Ma.|||||
75502|Kukalak Gneiss|69554|6|Mentioned|p139|||Pine Creek Orogen.|2527-2510 Ma (Hollis et al., 2009).|||||
75502|Kukalak Gneiss|69917|4|Described|p24-26, 19,20, 42, 47, 52, 1|Neoarchean|Neoarchean|Pine Creek Orogen, Nimbuwah Domain. U/Pb SHRIMP zircon dating, Hf, O analytical data. |2527+/-3 Ma mag.cryst.|||Underlies Kudjumarndi Quartzite of the Kakadu Group.|Leucocratic quartzo-feldspathic gneiss.|
75502|Kukalak Gneiss|70853|5|Briefly described|Map legend.|Neoarchean|Neoarchean||2527-2510 Ma.||||Biotite granodioritic gneiss; minor amphibolite and sillimanite-mica schist lenses; migmatised; locally hornfelsed adjacent to Oenpelli Dolerite.|
75502|Kukalak Gneiss|71256|6|Mentioned|p18|Neoarchean|Neoarchean||~2527-2510 Ma|||||
75502|Kukalak Gneiss|71349|5|Briefly described|p736-737|Archean|Archean|Pine Creek Orogen.|2527-2510 Ma.|||||
75502|Kukalak Gneiss|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Both age determinations are for crystallisation: U-Pb zircon SHRIMP.|2527+/-3 Ma and 2510+/-4 Ma.||||Layered quartzo-feldspathic (biotite) gneiss.|
75502|Kukalak Gneiss|72368|5|Briefly described|iii,p4|Neoarchean|Neoarchean|Geological province: Nimbuwah Domain, Pine Creek Orogen. Indistinguishable from Arrarra Gneiss in whole-rock geochemistry, but has distinct more evolved Nd-isotopic composition.||||Intrudes into Arrarra Gneiss.||26-SEP-19
75502|Kukalak Gneiss|72527|6|Mentioned|p192.|Neoarchean|Neoarchean|Given as an example of a source of old detrital zircons identified in that contribute to Murphy Metamorphics.||||||
33810|Kulail Sandstone|50286|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|50321|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|60679|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Quartz Sandstone. Geological Province: Amadeus Basin.||||||14-JAN-05
33810|Kulail Sandstone|61154|5|Briefly described|p17|||Basal part of succession that includes Dean Quartzite. Feldspathic and immature sandstone. Grades up into Dean Quartzite in Bloods Range region.  Geological Province: Amadeus Basin.||||||09-OCT-06
33810|Kulail Sandstone|61386|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red/purple crystalline quartzite sandstone, abundant trough cross beds, locally heavy mineral horizons of hematite and magnetite.  Geological Province: Amadeus Basin.||||||
33810|Kulail Sandstone|62989|5|Briefly described|p39, p40|||Basal unit in Amadeus Basin. Overlain by Dean Quartzite. Comprises deltaic sediments of quartz arenite to quartzofeldspathic beds, with moderately sorted quartz gravel to quartz pebble clasts; grading into finely laminated quartz sandstone layers.||||||25-JAN-07
33810|Kulail Sandstone|65256|2|Defined|piii, p6 Tb.1, p16-17, p40|Cryogenian|Tonian|New name: Disconformably overlies Bloods Range Formation (Tjauwata Group); overlies Amputjuta Dacite, Puntitjata Rhyolite; overlies Pottoyu Granite Suite; conformably underlies (grades into or interfingers with) Dean Quartzite. Formerly mapped as part of the Dean Quartzite. 60-300+m thick. Purple-red to orange, medium-grained crystalline quartz sandstone, sometimes gritty quartzofeldspathic sandstone and minor quartzite, with quartz conglomerate and quartz-muscovite layers, possible rare, poorly preserved mafic volcanics. 850 Ma.||||||
33810|Kulail Sandstone|67565|6|Mentioned|p38.|||In Bloods Range 1:250 000 sheet. A stratigraphic equivalent to the basal interval of the Heavitree Quartzite.||||||
33810|Kulail Sandstone|69003|6|Mentioned|p60|Neoproterozoic|Neoproterozoic|W Amadeus Basin.||||||
33810|Kulail Sandstone|69031|6|Mentioned|p4|||Amadeus Basin.||||||
33810|Kulail Sandstone|69436|6|Mentioned|p21:4|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||12-JUL-16
33810|Kulail Sandstone|69438|5|Briefly described|p23:2-4, 8-9, 18|Cryogenian|Cryogenian|Close et al. (2004). Musgrave Province, Amadeus Basin. Transitional, possibly deltaic deposits. Winnowed heavy mineral horizons sometimes occur.||||Disconformably overlies Bloods Range Formation. Is overlain conformably and gradationally by Dean Quartzite.|Purple-red to orange, medium-grained, generally equigranular quartz to quartzofeldspathic sandstone, containing abundant sedimentary structures. Basal lenses and beds with moderately sorted quartz gravel to quartz pebble clasts.|12-JUL-16
33810|Kulail Sandstone|69606|5|Briefly described|p2, p4 fig 2|Cryogenian|Cryogenian|Southern Amadeus Basin. Potential reservoir rocks.||||Overlain by the Dean Quartzite|Sandstone.|
33810|Kulail Sandstone|69673|6|Mentioned|p63|||||||Overlain by Dean Quartzite||
33810|Kulail Sandstone|70018|5|Briefly described|p234-235,239-240|Neoproterozoic|Neoproterozoic|Amadeus Basin. Of Supersequence 1 in the southern Amadeus Basin. Correlable to Heavitree Quartzite in the northern Amadeus Basin. Deposition occurred during post-rift subsidence after initial uplift of Musgrave Block.||||Overlain by Dean Quartzite. Underlain unconformably by Amadeus Basin stratigraphy.||
33810|Kulail Sandstone|70793|4|Described|500k_interpgeop14_lut.csv + geochron|Cryogenian|Neoproterozoic|Of Amadeus Basin (Phase 1), Centralian Superbasin. Occurs on the SW margin of the Amadeus Basin. Events: Alice Springs Orogeny (450-295 Ma); Areyonga Movement; Delamarian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199407 (sandstone) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum depositional age of 1119+\-13 Ma. See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1000-800 Ma (inferred; biostrat).|||Overlain by Dean Quartzite. Equivalent to Heavitree Quartzite.|Quartz sandstone, sandstone, and conglomerate; kyanite schist locally|
33810|Kulail Sandstone|70826|6|Mentioned|p5 tbl 2|||Supersequence 1, Centralian Superbasin.||||||20-APR-20
33810|Kulail Sandstone|70839|5|Briefly described|p328-334,336|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Basal unit of Supersequence 1; Equivalent to Dean Quartzite, and Heavitree Quartzite to the north. Exposed as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits. SHRIMP U-Pb zircon geochronology samples and analysis on p331-334. Detrital zircon age spectrum range between c. 1.82 and 1.09 Ga (Warakurna Supersuite), with dominant age component at 1.22-1.1 Ga (derived from Pitjantjatjara Supersuite; Musgrave orogeny). Older age peak at c. 1.73 Ga.|Max dep age: 1092+\-11 Ma (207Pb/206Pb)|||Overlain by Dean Quartzite. Correlable to Heavitree and Dean Quartzites.||
33810|Kulail Sandstone|71080|6|Mentioned|p23, 30|Tonian|Tonian|Southern Amadeus Basin. WA only? Base of Supersequence 1.||||Correlated with Munyu Sandstone, Murraba Basin.|Dominantly sandstone.|
33810|Kulail Sandstone|71088|6|Mentioned|p4, p6-p8, p10, p17|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Part of Supersequence 1.|c. 1200-1150 Ma|||||
33810|Kulail Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone|
33810|Kulail Sandstone|71268|4|Described|GEOL_LUT_CSV files|Tonian|Tonian|Of Amadeus Basin (Phase 1), Centralian Superbasin. Events: Delamerian Orogeny (520-505 Ma); Petermann Orogeny (580-520 Ma). Sample GSWA 199407 (quartz-rich sandstone) yielded a weighted mean 207Pb/206Pb age of 1119+\-13 Ma, interpreted as maximum depositional age of the sandstone. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|976-827 Ma (inferred)|||Overlain by Dean Quartzite. Correlable with Heavitree Quartzite, Vaughan Springs Quartzite.|Fine- to coarse-grained, purple-red  quartz- and quartzofeldspathic metasandstone containing heavy mineral bands; locally interbedded with quartzite and poorly sorted, polymictic pebble metaconglomerate; abundant sedimentary structures.|
33810|Kulail Sandstone|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
33810|Kulail Sandstone|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|1119+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Fine-grained quartz sandstone.|
33810|Kulail Sandstone|71841|5|Briefly described|p1|Cryogenian|Cryogenian|Of Amadeus Basin.||||Overlain by, and grades into Dean Quartzite. Underlain by basement.||
33810|Kulail Sandstone|71842|6|Mentioned|p3|Cryogenian|Cryogenian|Of Amadeus Basin.||||||
33810|Kulail Sandstone|72034|5|Briefly described|500k_interpgeop16_lut|Tonian|Tonian|Amadeus Basin (Phase 1). Informal grouping of mostly time-equivalent silicilastic units. Grouped with Dean Quartzite, Heavitree Quartzite, and Vaughan Springs Quartzite. Min age  from biostratigraphy.|||||Informal grouping description: Quartz sandstone, sandstone, and conglomerate; kyanite schist locally [probably only in Dean Quartzite].|
33810|Kulail Sandstone|72094|6|Mentioned|p3 Fig 2|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
33810|Kulail Sandstone|72601|6|Mentioned|p3|Tonian|Tonian|Amadeus Basin. Found in the southern part of the basin.||||||
33810|Kulail Sandstone|73085|6|Mentioned|p1|Tonian|Stenian[?]|||||Overlain by Dean Quartzite.||
33810|Kulail Sandstone|73086|6|Mentioned|p7, p9, p145|||Amadeus Basin. Part of Supersequence I[?]; deposited during the early sag phase of basin development. Restricted to exposures in the southwest of the basin.||||Correlates to Heavitree Formation[?].||
33810|Kulail Sandstone|73346|6|Mentioned|p5|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
33810|Kulail Sandstone|73437|6|Mentioned|p151|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
26673|Kulampirri beds|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
26673|Kulampirri beds|43036|5|Briefly described|p63|||||||||
26673|Kulampirri beds|61155|5|Briefly described|p16|Middle Miocene|Early Miocene|?Overlain by Annie Creek Limestone. Age: <22Ma. Geological region: East Arnhem Land. ||||||
26673|Kulampirri beds|69458|5|Briefly described|p42:21|Neogene|Paleogene|Overlies McArthur Basin succession in northeastern NT. Formed by precipitation of carbonates within the soil profile and/or lacustrine inundation. Undated: presumed to be Paleogene-Neogene.|||||Patches of low-lying, massive travertine and calcrete.|12-JUL-16
39516|Kulgera Granite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Porphyritic hornblende-biotite granite and quartz monzonite.  Geological Province: Musgrave Block.||||||
39516|Kulgera Granite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Granite monzonite, quartz monzonite. Geological Province: Musgrave Block.||||||
39516|Kulgera Granite|61154|2|Defined|p43 App., p13|Mesoproterozoic|Mesoproterozoic|Formerly Kulgera adamellite. Of the Pitjantjatjara Supersuite. Characterised by distinctive reddish colour, and consists of porphyritic and equigranular quartz monzonite to monzogranite, with microgranite dykes. Intruded by Alcurra Dolerite. GeolProv: Mus||||||19-JUL-05
39516|Kulgera Granite|63866|5|Briefly described|p207|||Fregon Domain, Musgrave Province.||Pitjantjatjara Supersuite||||
39516|Kulgera Granite|69436|6|Mentioned|p21:9|||Edgoose et al. (2004). Formerly Kulgera adamellite (Edgoose et al., 1993).||||||12-JUL-16
42439|Kulpitjata Suite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Variably deformed porphyritic biotite granite, minor hornblende granite. Geological Province: Musgrave Block.||||||12-JAN-05
42439|Kulpitjata Suite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Porphyritic biotite granite. Geological Province: Musgrave Block.||||||
42439|Kulpitjata Suite|61154|4|Described|p8, p42 App., p11|Mesoproterozoic|Mesoproterozoic|Of Pitjantjatjatra Supersuite. Variably deformed porphyritic biotite granite, lesser hornblende granite; incl: coarse granite and.............with accessory zircon, opaques, apatite. Underlies Dean Quar||||||03-AUG-05
42439|Kulpitjata Suite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province. Ages derived from Young et al, 2002.|1197 +/- 21 Ma to 1150 +/- 19 Ma|Pitjantjatjara Supersuite||||
42439|Kulpitjata Suite|69436|4|Described|p21:4, 6, 10|Mesoproterozoic|Mesoproterozoic|Young et al. (2002). Dominated the SE end of the Olia Chain, Musgrave Province. Has close affinities with the Mantarurr Suite. SHRIMP U-Pb and Kober Pb-Pb zircon dating of seven samples.|1197-1150 Ma (Young et al., 2002).|Pitjantjatjara Supersuite.||Intrudes Opparinna Metamorphics.|Variably deformed, porphyritic biotite granite, with lesser hornblende granite; locally contains flattened, stretched and recrystallised K-feldspar, and mylonite zones.|12-JUL-16
42439|Kulpitjata Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42439|Kulpitjata Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Other ages given c.1197-1191 Ma.|1150+/-19 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
33489|Kulu Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mantarurr Granite Suite. Coarsely porphyritic foliated biotite-titanite-epidote-muscovite granite, minor aplite.   Age: ~1170Ma.||||||
33489|Kulu Granite|60683|2|Defined|p58 Appendix,  p18|Mesoproterozoic|Mesoproterozoic|Of Mantarurr Granite Suite.  Parts formerly Olia Gneiss of Forman (1966a, 1972). Coarsely porphyritic biotite-sphene-epidote-muscovite granite.  Has sharp intrusive contact with Foster Cliff Granite. Age: 1168+/-4Ma and 1165+/-11Ma. See also p10 Tb.1, p49||||||23-DEC-09
33489|Kulu Granite|61154|6|Mentioned|p44 Appendix|||Of the Pitjantjatjara Supersuite.||||||
33489|Kulu Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Mantarurr Granite Suite. Coarsely porphyritic foliated biotite-titanite-epidote-muscovite granite; minor aplite.  Age: ~1170Ma. Geological Province: Musgrave Block.||||||19-OCT-05
26676|Kurala Sandstone|22538|6|Mentioned|Table1 P712||Statherian|Part of the Goyder package||||||
26676|Kurala Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
26676|Kurala Sandstone|24048|6|Mentioned|p55|||||||||
26676|Kurala Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Sandstone: white to pale grey and pale pink, medium-grained, medium to thick-bedded, cross-bedded to flat-bedded and massive, quartz-rich. Geol. Prov: McArthur Basin.||||||12-OCT-05
26676|Kurala Sandstone|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Parsons Range Group. Geological Province: Northern McArthur Basin.||||||
26676|Kurala Sandstone|32660|5|Briefly described|Table 4|||||||||
26676|Kurala Sandstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
26676|Kurala Sandstone|43010|2|Defined|p130||Paleoproterozoic|Of Habgood Group. Of Statherian age.||||||07-NOV-08
26676|Kurala Sandstone|44112|4|Described|p10,49,53,55|||||||||
26676|Kurala Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Parsons Range Group. Sandstone: white to pale grey and pale pink, medium-grained, medium to thick-bedded, cross-bedded to flat-bedded and massive, quartz-rich. Geol. Prov: McArthur Basin.||||||
26676|Kurala Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Parsons Range Group.||||
26676|Kurala Sandstone|69430|4|Described|p15:3, 13-14, 20, 22|Statherian|Statherian|Originally included in the Habgood Group (Dunnet, 1965; Plumb and Roberts, 1992); later assigned to Parsons Range Group by Haines (1994). Walker Fault Zone, northern McArthur Basin. A prominent ridge-forming unit. Over 300m thick. Shallow-marine deposits. Lower contact not exposed.||Parsons Range Group.||Is overlain conformably by Slippery Creek Siltstone (Habgood Group).|Medium-grained and minor fine-grained white quartz arenite and quartzite.|12-JUL-16
26676|Kurala Sandstone|69673|6|Mentioned|p16 fig 13|||||Parsons Range Group||Overlain by Slippery Creek Siltstone||
24347|Kurinelli Sandstone|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgroup (Hatches Creek Group).||||||07-NOV-08
24347|Kurinelli Sandstone|23733|6|Mentioned|p29|||||||||
24347|Kurinelli Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Ooradidgee Group.  Geological Province: Davenport Province.||||||
24347|Kurinelli Sandstone|23823|5|Briefly described|p79 Fig. M3|||See also Kurinelli sandstone - both names treated as informal in this study.||||||07-FEB-11
24347|Kurinelli Sandstone|24089|5|Briefly described|p27 Fig. 15|||Of Hatches Creek Group.||||||
24347|Kurinelli Sandstone|24172|5|Briefly described|p22, p7 Tb.1, p66 Tb.9|||Of the Ooradidgee Subgroup (Hatches Creek Group). Conformably underlain by Edmirringee Volcanics. Geological Province: Tennant Creek Inlier. With Rooneys Formation constitutes a deltaic complex.||||||09-OCT-06
24347|Kurinelli Sandstone|39624|5|Briefly described|Table 1|||||||||
24347|Kurinelli Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24347|Kurinelli Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).   Feldspathic, lithic and quartzose arenite; siltstone, friable arenite, ashstone; rare felsic lava.||||||10-JAN-05
24347|Kurinelli Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24347|Kurinelli Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24347|Kurinelli Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Feldspathic, lithic and quartzose arenite; minor siltstone and friable arenite; rare felsic volcanic lenses. Geological Province: Tennant Creek Block.||||||07-NOV-08
24347|Kurinelli Sandstone|41129|4|Described|Table 1|||||||||
24347|Kurinelli Sandstone|41204|4|Described|Table 1|||||||||
24347|Kurinelli Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup. Lithic/feldspathic arenite, quratz arenite, pebbly arenite, siltstone; minor felsic and mafic volcanics.||||||16-NOV-05
24347|Kurinelli Sandstone|41308|6|Mentioned|p10|||||||||
24347|Kurinelli Sandstone|41310|4|Described|p11|||See also Table 1.||||||09-OCT-06
24347|Kurinelli Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24347|Kurinelli Sandstone|41524|4|Described|Table 1|||||||||
24347|Kurinelli Sandstone|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Feldspathic, lithic and quartz arenites.||||||07-NOV-08
24347|Kurinelli Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24347|Kurinelli Sandstone|42504|6|Mentioned|Fig. 22 P102|||||||||
24347|Kurinelli Sandstone|42643|4|Described|p5, Table 1 p9|||Of Ooradidgee Subgroup.||||||09-OCT-06
24347|Kurinelli Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Feldspathic/lithic arenite; pebbly arenite; minor siltstone, conglomerate, felsic lava and tuff.||||||07-NOV-08
24347|Kurinelli Sandstone|43223|5|Briefly described|Map Legend||Proterozoic|Of Ooradidgee Subgroup.||||||09-OCT-06
24347|Kurinelli Sandstone|43224|5|Briefly described|Map legend||Proterozoic|of Hatches Creek Group||||||
24347|Kurinelli Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
24347|Kurinelli Sandstone|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||09-OCT-06
24347|Kurinelli Sandstone|49033|2|Defined|p9|Proterozoic|Proterozoic|||||||
24347|Kurinelli Sandstone|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||
24347|Kurinelli Sandstone|50588|5|Briefly described|p3.4, 4.4|||Geological Province: Tennant Creek/Davenport Province. Intruded by: Treasure Suite, Devils Suite.||||||
24347|Kurinelli Sandstone|60681|5|Briefly described|Map legend|Statherian|Orosirian|Of the Ooradidgee Group.  Sandstone, siltstone.||||||
24347|Kurinelli Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group.  Subarkosic/sublithic/lithic arenite, quartz arenite, siltstone; minor felsic and mafic lava and tuff, mudstone, shale, slate and schist.   In the Tennant Creek region.||||||07-NOV-08
24347|Kurinelli Sandstone|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgr.(Hatches Creek Gr.) Med.-bedded, recessive, friable, feldspathic arenite, siltstone; felsic and mafic volcs. Overlies Edmirringee Basalt;underlies Taragan Sst.Max. thickness: 400m. Geol.Prov: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
24347|Kurinelli Sandstone|64068|5|Briefly described|p197|Paleoproterozoic|Paleoproterozoic|Tosca (turquoise) mine area.||Of Hatches Creek Group.||Overlies Rooneys Formation. Is intruded by Elkedra Granite.|Orthoquartzite.|05-APR-12
24347|Kurinelli Sandstone|64735|5|Briefly described|p206, p206 Fig 2, p210|Orosirian|Orosirian|Intruded by dolerite sills.||Of Ooradidgee Group.|Includes Warnes Sandstone Member.|||30-APR-12
24347|Kurinelli Sandstone|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
24347|Kurinelli Sandstone|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Ooradidgee Group. Inferred subarkosic/sublithic/lithic arenite, quartz arenite, minor mudstone, shale, slate and schist; minor to dominant felsic and mafic lava and tuff. Cross-section only||||||
24347|Kurinelli Sandstone|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Ooradidgee Group. Non-outcropping. Inferred subarkosic/sublithic/lithic arenite, quartz arenite, minor mudstone, shale, slate and schist; minor to dominant felsic and mafic lava and tuff.||||||
24347|Kurinelli Sandstone|65338|5|Briefly described|p8 Table 1, p19.|Paleoproterozoic|Paleoproterozoic|Non-outcropping, interpreted from geophysical data; lithology inferred from geophysical character and/or outcrop in adjacent sheet areas. May partly fill the time interval between first and second felsic volcanic episodes of this Group.||Unit in Ooradidgee Group.|||Sandstone, felsic and mafic lava and tuff; minor shale, slate and schist.|
24347|Kurinelli Sandstone|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Ooradidgee Group.|Includes Endurance Sandstone and Warnes Sandstone Members.|Overlies Rooneys Formation. Is overlain by Taragan Sandstone.|Feldspathic, lithic and quartzose arenite; minor siltstone and friable arenite; rare felsic volcanic lenses.|
24347|Kurinelli Sandstone|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Ooradidgee Group.|||No outcrop: inferred subarkosic/sublithic/lithic arenite, quartz arenite, minor mudstone, shale, slate and schist; minor to dominant felsic and mafic lava and tuff.|
24347|Kurinelli Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.||Overlies Rooneys Formation.|Subarkosic/sublithic/lithic arenite, quartz arenite, siltstone; minor felsic and mafic lava and tuff, mudstone, shale, slate and schist.|
24347|Kurinelli Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Ooradidgee Group.|Warnes Sandstone Member.|||
24347|Kurinelli Sandstone|67352|4|Described|p10 Tb.1, p41, p44 fig 48, p56|Orosirian|Orosirian|Over 2000 m thick. Auriferous; quartz veins also contain W and Cu minerals.||Ooradidgee Group|Endurance Sandstone Member.|Conformable on/interfingering with Rooneys Formation, Epenarra Volcanics. Intruded by Devils Suite. Is conformably overlain by Taragan Sandstone.|Feldspathic, lithic and quartz arenite: thinly to thickly bedded, fine-to medium grained, well sorted, locally volcaniclastic or tuffaceous, slightly calcareous, possibly evaporitic; minor siltstone; rare non-porphyritic andesitic lava.|
24347|Kurinelli Sandstone|68518|3|Fully described|p9 Tb.1, p11, p13|Proterozoic|Proterozoic|Thickness: 700-2500 m. Intruded by dolerite sills.||Ooradidgee Subgroup|Warnes Sandstone Member|Conformable on Edmirringee Volcanics and Rooneys Formation; overlain conformably by Taragan Sandstone and Treasure Volcanics and conformably/unconformably by Unimbra Sandstone.|Ridge-forming feldspathic/lithic arenite; minor recessive siltstone, micaceous siltstone, and, in NW, felsic lava, tuff, and ashstone.|30-MAY-16
24347|Kurinelli Sandstone|69187|6|Mentioned|p53 Fig.2|||Warramunga Province.||||||
24347|Kurinelli Sandstone|69418|6|Mentioned|p3:23|||In the Hatches Creek field, contains W-Mo mineralised quartz veins in parallel or en echelon arrangement along zones of shearing.||||||12-JUL-16
24347|Kurinelli Sandstone|69424|4|Described|p9:3, 5, 15, 17-18, 23-26, 28, 54-55|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Warramunga Province. Lower part is interpreted to be marine portion of a delta complex; upper parts represent continued delta progradation, with braided-river deposits and interfluvial salinas. c.2600m thick. Age from a dolerite unit. Hosts W and/or Au-bearing quartz veins.|1811 +/- 5 Ma.|Ooradidgee Group.|Warnes and Endurance, Sandstone Members.|Conformably overlies Rooneys Formation, Edmirringee and Epenarra Volcanics. Is overlain conformably by Taragan and Treasure Volcanics, and Unimbra Sandstone (the last also unconformably).|Ridge-forming tuffaceous, lithic and sublithic (volcanilithic), fluviatile sandstone; quartz sandstone, pebbly sandstone and conglomerate; minor felsic and mafic lava and tuff; siltstone; shale.|12-JUL-16
24347|Kurinelli Sandstone|69425|4|Described|p10:3-8, 13, 21, 23|||0 - over 1000m thick (up to 2600m in Warramunga Province). Lower part interpreted as a delta complex; the remainder probably represents progradation: shallow-water braided river deposits with local salinas. Lower part is lithologically similar to Rooneys Formation and may be a more proximal equivalent. Greisenised by Devils Marbles Granite; intruded by Treasure Suite. Underwent disharmonic folding by the Davenport Event.||Ooradidgee Group.|Warnes and Endurance, Sandstone Members.|Conformably overlies Epenarra and Edmirringee Volcanics, Rooneys Formation. Underlies conformably Taragan Sandstone, Treasure Volcanics. Interfingers with all of them. Underlies Unimbra Sandstone.|Ridge-forming feldspathic/lithic (volcaniclastic/tuffaceous?) sandstone; quartz sandstone, pebbly sandstone and conglomerate; minor felsic and mafic lava and tuff; siltstone; shale; claystone with evaporites; minor calcareous beds; schist and slate.|12-JUL-16
24347|Kurinelli Sandstone|69431|6|Mentioned|p16:22|||Folding during the Davenport Event is discussed.||||||12-JUL-16
24347|Kurinelli Sandstone|72379|5|Briefly described|p8-9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. |||Includes Endurance and Warnes sandstone members.|||
24347|Kurinelli Sandstone|72380|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.|||Includes Endurance and Warnes sandstone members.|||
24347|Kurinelli Sandstone|73083|6|Mentioned|p24|||||||||
24347|Kurinelli Sandstone|73124|6|Mentioned|p2 Fig.1|||||||Underlain by Rooneys Formation. Equivalent to Edmirringee Volcanics, Epenarra Volcanics.||
24347|Kurinelli Sandstone|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
24347|Kurinelli Sandstone|73460|6|Mentioned|p2|||Warramunga Province.||||Underlain by Rooneys Formation. Underlain by and equivalent to Epenarra Volcanics. Overlain by and equivalent to Edmirringee Volcanics.||
24347|Kurinelli Sandstone|73590|6|Mentioned|p2|||||Ooradidgee Group||Underlain by Rooneys Formation. Underlain by and equivalent to Epenarra Volcanics. Overlain by Taragan sandstone and Treasure Volcanics. Overlain by and equivalent to Edmirringee Volcanics.||
30268|Kyalla Formation|23937|1|Redefined|p82 App. 1|Calymmian|Calymmian|Upgraded to formation in Maiwok Subgp (Roper Gp);  replaces Kyalla Mbr (McMinn Fm); also replaces the informal "Cat Creek member" (of the now abandoned Cobanbirini Fm). Disconformably overlain by Bukalorkmi Sst; overlies Sherwin Fm.  Max. thick: ~250m.||||||23-DEC-09
30268|Kyalla Formation|24047|5|Briefly described|p28 Fig. 21|||Age: 1429 +/- 31 Ma (Kralik 1982). Geological Province: McArthur Basin.  See also p22.||||||
30268|Kyalla Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Contains the Sherwin Member. Interbedded siltstone, mudstone and very fine quartz sandstone.  Does not outcrop in the Roper River mapsheet area.||||||14-FEB-05
30268|Kyalla Formation|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
30268|Kyalla Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Interbedded siltstone, mudstone and very fine grained quartz sandstone.||||||29-SEP-05
30268|Kyalla Formation|62376|5|Briefly described|p38|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
30268|Kyalla Formation|64784|4|Described|p1-10   |Proterozoic|Proterozoic|Beetaloo Basin. Organic-rich: one of two major source-rock units in the basin.||||Conformably overlies the Moroak Sandstone. Unconformably underlies the Jamison Sandstone.|Contains light gray to very dark gray and brown, massive to fissile siltstone and claystone, with occasional thin sandstone units.|
30268|Kyalla Formation|64975|5|Briefly described|p161.|||Beetaloo Sub-basin. In Jamieson 1 well, includes gross mudstone interval of c. 50 m within which are 40 m of mature hydrocarbon source rock; represents a potential self-sourcing reservoir.||Unit in McMinn Formation.||||
30268|Kyalla Formation|65236|5|Briefly described|p3 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.Overlain by Jamison Sandstone.  Max. thickness: 730m. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
30268|Kyalla Formation|65342|5|Briefly described|p8.|||Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 657 m. Seen as having potential as an insulating layer for geothermal energy.||Unit in Roper Group.||Overlies Moroak Sandstone. Is overlain by Jamieson Sandstone.|Sandstone, siltstone.|
30268|Kyalla Formation|69018|5|Briefly described|p450 Fig.1b, p451|Calymmian|Calymmian|Previously Kyalla Member.|1429 +/- 31 Ma.|Of Roper Group.||||
30268|Kyalla Formation|69206|6|Mentioned|p3|||McArthur Basin. Has potential for unconventional oil and shale gas.||||||
30268|Kyalla Formation|69418|6|Mentioned|p3:36|||McArthur Basin. Excellent hydrocarbon source rocks.||||||12-JUL-16
30268|Kyalla Formation|69430|4|Described|p15:3, 27, 29-30, 53, 61-62|Calymmian|Calymmian|Abbott et al. (2001) who raised the unit to Formation status and defined it. Originally (Dunn, 1963) the Kyalla Member of the McMinn Formation. Southern McArthur Basin. c.250m thick. Storm-dominated shelf sediments. Potential hydrocarbon source rock; oil and gas shows are common. Has some conventional reservoir potential, as well as potential for unconventional reservoirs (oil and basin-centred gas). May be source rock and seal for Moroak Sandstone.||Maiwok Subgroup.||Conformably and gradationally overlies Sherwin Formation. Is overlain probably disconformably by Bukalorkmi Sandstone (sharp and probably erosional contact).|Interbedded siltstone, sandstone and mudstone. The upper part is sandstone-rich.|12-JUL-16
30268|Kyalla Formation|69673|6|Mentioned|p20, p24, p29, p32, p40, p41, p44, p47|||Shale oil and gas potential. Up to 777m Thick.||Maiwok Subgroup||Conformably overlies Sherwin Formation, Moroak Sandstone, Disconformably overlain by Bukalorkmi Sandstone|Interbedded grey to black mudstone, silty mudstone, siltstone and fine sandstone.|
30268|Kyalla Formation|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Sherwin Ironstone; overlain by Bukalorkmi Formation.|Interbedded mudstone, siltstone and fine sandstone.|
30268|Kyalla Formation|70968|2|Defined|p51, p67, p69-70, p74-82, p86-88, p123|Ectasian|Ectasian|See also p126, p131, p133, p140, p143. Sweet, Young and Abbott in Abbott et al. (2001), who raised it to Formation rank after Dunn (1963) had named it the Kyalla Member (of McMinn Formation). Named after Kyalla Waterholes on Morok Creek. Recessive unit: poor exposures. The type section is in DDH POG Shea-1 from 245.42m (base) to 20.0m depth, at 366526mE 8333623mN in HODGSON DOWNS sheet. Details of a partial reference section are given. Notable for its organic-rich beds with potential as petroleum source rocks. Intruded by Derim Derim Dolerite sills. Lithology described and illustrated in detail. Up to 843.4m thick. Storm-dominated marine shelf deposits. Rb-Sr date from illite gives minimum diagenesis age.|>1429 +/- 31 Ma (Kralik, 1982).|Maiwok Subgroup.|Elliott sandstone member (informal).|Overlies Sherwin Formation and Moroak Sandstone conformably and gradationally. Is overlain by Bukalorkmi Sandstone disconformably, locally unconformably. Unconformably underlies Jamison sandstone.|Medium bedded to thinly interbedded and interlaminated siltstone, silty claystone, claystone and less common very fine-grained sandstone. Includes an iron-rich matrix.|
30268|Kyalla Formation|71059|4|Described|iii, p1, p3, p6, p9-12, p14-21, p23-27|Mesoproterozoic|Mesoproterozoic|See also p31-42, p57-60. McArthur Basin. Of exploration interest for unconventional shale oil and gas: has an average TOC of 1.08 wt%. Estimated shale/tight gas/shale oil and condensate resources detailed. 30-844m thick. Storm-dominated marine shelf deposits. TOC and Pyrolysis, elemental kerogen CHONS, X-ray diffraction, pore fluid saturations, organic petrology reflectivity, gas analysis, data all detailed.||Roper Group.||Conformably and gradationally overlies Sherwin Formation or Moroak Sandstone. Is overlain disconformably by Bukalorkmi Sandstone.|Medium-bedded to thinly interbedded and interlaminated siltstone, mudrock and lesser sandstone.|
30268|Kyalla Formation|71488|4|Described|p140, p141 fig 1b, p142, p144-p153|Ectasian|Ectasian|Beetaloo Sub-basin. Ages are interpreted as maximum depositional ages. Deposited in a storm-dominated shallow-marine shelf environment. LA-ICP-MS zircon geochronology results are briefly discussed.|1313 +/- 47 Ma|Maiwok Subgroup||Overlies the Sherwin Ironstone. Overlain by the Bukalorkmi Sandstone. Unconformably overlain by the Jamison sandstone.|Interbedded siltstone, sandstone and mudstone.|02-MAY-18
30268|Kyalla Formation|71779|5|Briefly described|p2, p10, p12 fig 9|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Maiwok Subgroup||||24-SEP-18
30268|Kyalla Formation|71857|5|Briefly described|iii, p1-2, p8-9, p14-25, p31-33, p38-41|Mesoproterozoic|Mesoproterozoic|See also p43-45, p49, App 1,2, 3, 5. McArthur Basin. Self-sourced, continuous petroleum reservoir with documented oil and gas shows in several wells. Details of 10 wells tabulated. Core data analyzed for potential hydrocarbon resources. Structure, isopach maps. Data tabulated and graphed in 4 Appendices, one each for the Gorrie, Beetaloo, OT Downs and Broadmere Sub-basins.||Roper Group.|||Includes black shale horizons.|04-FEB-19
30268|Kyalla Formation|71893|5|Briefly described|p5, p8, p32, p37, p40|||McArthur Basin.||Maiwok Subgroup||Overlies the Moroak Sandstone. Disconformably overlain by the Bukalorkmi Sandstone. Unconformably overlain by the Jamison sandstone.||
30268|Kyalla Formation|72381|4|Described|p771-778|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Interpreted to have been deposited in a storm-dominated shallow marine shelf environment (Powell et al. 1987; Abbott et al. 2001; Munson 2016). Intersected in Elliott-1 and Jamison-1 drillholes, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). Deposited between c. 1350 and c. 1313 Ma, coeval with subduction-related magmatism, orogeny and metamorphism between the West Australian Craton, and combined North and South Australian Cratons (see p779 for references). Sample EN-yk4 returned dominant peaks at c. 1735 Ma and a minor peak at c. 1790 Ma, consistent with sample from Jamison-1, and those reported by Yang et al. (2018). Absence of c. 1590 zircon grains indicate less input from SE sources (e.g. .g. Mount Isa Province, Georgetown Province, Coen Province and NE South Australia Craton). Dominant c. 1735 Ma peak is consistent with crystallisation ages of exposed magmatic rocks in the eastern Arunta region (Hollis et al. 2010), and supported by hafnium isotopic data.||Uppermost unit of Mailwok Subgroup/Roper Group..||Overlain by Jamison sandstone. Underlain by Moroak Sandstone. Intruded by Derim Derim Dolerite.|Interbedded sandstones and mudrocks.|04-OCT-19
30268|Kyalla 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 Sherwin Formation and underlies Bukalorkmi Sandstone.||
30268|Kyalla Formation|72718|6|Mentioned|p1-3, p7-14, p20|||Beetaloo Sub-basin, McArthur Basin. Roper Superbasin, Wilton package. Occurs within the Urapunga Fault Zone, south-western McArthur Basin, and Batten Fault Zone (north). Unit defines the Beetaloo Sub-basin boundary where it is either missing or shallower than 400 m below the surface. It is the most frequently intersected unit in the area. Represents the top of the Roper Group within the Beetaloo Sub-basin. Characterised predominantly as a semi-continuous to discontinuous, low-frequency reflector.||Maiwok Subgroup, Roper Group||Underlain by Sherwin Formation. Overlain by Bukalorkmi Sandstone.||
30268|Kyalla Formation|72912|4|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. Described as a potential hydrocarbon source rock.||Maiwok Subgroup||Overlies Sherwin Formation and underlies Bukalorkmi Sandstone.||
30268|Kyalla Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Sherwin Formation. Overlain by Bukalorkmi Sandstone.||
30268|Kyalla Formation|73083|6|Mentioned|p28|||||Roper Group||Underlain by Sherwin Formation.||
30268|Kyalla Formation|73242|5|Briefly described|p39|||Unit also assigned a detrital zircon young ages of 1313 +/- 47 Ma and 1317 +/- 36 Ma (Yang et al., 2018), although it is unclear whether this is a maximum depositional age.||Maiwok Subgroup, Roper Group||Underlain by Sherwin Ironstone. Overlain by Bukalorkmi Sandstone. Intruded by Derim Derim Dolerite.|Includes interbedded mudstone and fine sandstone.|
30268|Kyalla Formation|73280|6|Mentioned|piii, p1, p4-5, App.1A|||Beetaloo Sub-basin, McArthur Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
30268|Kyalla Formation|73412|5|Briefly described|p4|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Derim Derim Dolerite.||
81929|Lake Surprise Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1803+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Megacrystic biotite granite.|
28264|Lake Surprise Sandstone|12891|5|Briefly described|p731, p733 Fig. 2|Devonian|Devonian|Overlies Hanson River Beds. Geological province: Wiso Basin.||||||07-FEB-11
28264|Lake Surprise Sandstone|23270|5|Briefly described|p10||Late Paleozoic|Lander River 1:250 000 Sheet.||||||07-NOV-08
28264|Lake Surprise Sandstone|23858|5|Briefly described|p917|||Underlain by Hanson River beds. Geological Province: Wiso Basin.||||||09-AUG-06
28264|Lake Surprise Sandstone|31413|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28264|Lake Surprise Sandstone|34810|4|Described|Table 1|||||||||
28264|Lake Surprise Sandstone|35224|4|Described|Table 1|||See also p6.||||||09-AUG-06
28264|Lake Surprise Sandstone|35227|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28264|Lake Surprise Sandstone|35254|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28264|Lake Surprise Sandstone|36335|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
28264|Lake Surprise Sandstone|40578|5|Briefly described|Map legend|Devonian|Devonian|Probably Devonian.||||||10-JAN-05
28264|Lake Surprise Sandstone|40906|6|Mentioned|p30|||||||||
28264|Lake Surprise Sandstone|41204|4|Described|p14|||Mention p4.||||||09-AUG-06
28264|Lake Surprise Sandstone|41205|5|Briefly described|Map legend|Devonian|Devonian|Sandstone. Geological Province: Wiso Basin.||||||16-NOV-05
28264|Lake Surprise Sandstone|42059|5|Briefly described|Fig.2 P131|||See also p134.||||||09-AUG-06
28264|Lake Surprise Sandstone|42504|6|Mentioned|p83|||Wiso Basin||||||20-MAY-06
28264|Lake Surprise Sandstone|42643|6|Mentioned|p32|||Wiso Basin||||||
28264|Lake Surprise Sandstone|43749|6|Mentioned|p38|||||||||
28264|Lake Surprise Sandstone|45148|2|Defined|p18|Ordovician|Ordovician|Previously mapped as Dulcie Sandstone  - current usage favours Lake Surprise Sandstone. Also mentioned p1.||||||09-AUG-06
28264|Lake Surprise Sandstone|45155|6|Mentioned|Fig.8|||||||||
28264|Lake Surprise Sandstone|45167|5|Briefly described|p54|||||||||
28264|Lake Surprise Sandstone|45168|6|Mentioned|p6|||||||||
28264|Lake Surprise Sandstone|46844|6|Mentioned|Fig. 2|||||||||
28264|Lake Surprise Sandstone|60684|6|Mentioned|p50 Appendix|||Unconformably overlies parts of Lothari Hill Sandstone.||||||
28264|Lake Surprise Sandstone|62637|5|Briefly described|Map Legend|Permian|Permian|Geological Province: Wiso Basin. Well sorted, well rounded medium grained sandstone.||||||16-AUG-06
28264|Lake Surprise Sandstone|65239|5|Briefly described|p3 Fig. 4|Devonian|Ordovician|Conformably overlies the Middle Cambrian sequence of Montejinni Limestone/Hooker Creek Formation/Lothari Hill Sandstone. Geological province: Wiso Basin. Shallow to restricted marine deposits, and fluvial deposits.||||||04-JUN-09
28264|Lake Surprise Sandstone|65333|5|Briefly described|Map Legend|Devonian|Devonian|Of Wiso Basin. Age uncertain. Unconformably overlies Hanson River beds; unconformably underlies Buchanan Hills beds. Well rounded and well sorted, medium to coarse grained marine sandstone.||||||
28264|Lake Surprise Sandstone|65334|5|Briefly described|Map Legend|Devonian|Devonian|Of Wiso Basin. Age uncertain. Unconformably overlies Hanson River beds; unconformably underlies Buchanan Hills beds. Well rounded and well sorted, medium to coarse grained marine sandstone.||||||
28264|Lake Surprise Sandstone|65338|6|Mentioned|p5 Fig.3, p67, p71.|Devonian|Devonian|Wiso Basin. Scattered outcrops occur in LANDER RIVER area. May have potential as an aquifer.||||||
28264|Lake Surprise Sandstone|65342|6|Mentioned|p13. |||Wiso Basin (Lander Trough). Up to 250 m thick.||||||
28264|Lake Surprise Sandstone|65345|5|Briefly described|p7 Fig.6. |Carboniferous|Devonian|Wiso Basin. Over 150 m thick. Fluvial deposits.||||||
28264|Lake Surprise Sandstone|67165|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Wiso Basin.|||||Well-sorted, well-rounded, medium-grained sandstone.|
28264|Lake Surprise Sandstone|69447|4|Described|p32:2-3, 5-6, 9|Devonian|Devonian|Kennewell and Huleatt (1980). Caps the Wiso Basin succession. Shallow marine, shoreface, ?fluviatile deposits. Up to 150m thick. Unfossiliferous and undated. Lithologically similar to Dulcie Sandstone (Georgina Basin). Deposits extend across a thrust fault; the intraformational slumping was most likely caused by the Devonian Pertnjara-Brewer events of the Alice Springs Orogeny. May have reservoir potential, but lacks an effective seal.||||Unconformably overlies Hanson River beds and Lothari Hill Sandstone.|White to light brown, well sorted and well rounded, very fine to coarse quartz sandstone; low-angle cross-beds, slumps. Locally has a matrix of silt and clay.|12-JUL-16
28264|Lake Surprise Sandstone|69673|5|Briefly described|p143, p144 fig 116, p145|Devonian|Devonian|Up to 350m thick.||||Overlies Hanson River beds||
28264|Lake Surprise Sandstone|73083|6|Mentioned|p14|Devonian|Devonian|||||||
38405|Lake Woods beds|23937|6|Mentioned|p95 App. 1|||Of the Renner Group.  On HELEN SPRINGS  sheet.||||||
38405|Lake Woods beds|24303|2|Defined|p34, p62 Appendix|Calymmian|Calymmian|Of the Renner Group. Unconformably overlain by Montejinni Limestone; overlies the Jangirulu Formation. Max. Thickness: >200m. Previously mapped as Cambrian Gum Ridge Formation; subsequently reassigned to Montejinni Limetone. See also p23 Tb.3, p24 Tb. 4.||||||09-OCT-06
38405|Lake Woods beds|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Sandstone, laminated to medium bedded; mudstone;  dolostone; stromatolitic bioherms, cauliflower chert, granule conglomerate; graded, evaporite pseudomorphs.||||||17-OCT-05
38405|Lake Woods beds|24442|5|Briefly described|p15|||Top of the Renner Group. Not exposed in HELEN SPRINGS.||||||
38405|Lake Woods beds|69431|4|Described|p16:15, 18-19, 22|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Informal name. Tomkinson Province. Forms scattered, low-relief outcrops. Over 200m preserved thickness. Shallow-marine to supratidal deposits.||Uppermost Renner Group.||Conformably overlies Jangirulu Formation. Is apparently overlain unconformably by Montejinni Formation.|Sandstone, siltstone and shale; chertified dolostone and chertified probable stromatolitic bioherms; minor granular conglomerate. Poorly to well-sorted, fine- to medium-grained sandstone; laminated or thinly bedded. Nodular chert.|12-JUL-16
38405|Lake Woods beds|69673|6|Mentioned|p58|||informal name.||Renner Group||||
38405|Lake Woods beds|70968|3|Fully described|p94-95, p111-112, p114, p126, p131, p140|Ectasian|Ectasian|Informal. Hussey in Hussey et al. (2001). Named after Lake Woods. Originally mapped as Gum Ridge Formation in HELEN SPRINGS (Randal et al., 1966) and BEETALOO (Brown and Randal, 1969). Subsequently reassigned to Montejinni Limestone by Kennewell and Huleatt (1980), then to the Renner Group by Hussey et al. (2001). Tomkinson Province. No type section. The base occurs at 352700mE 8008000mN in HELEN 100k sheet; the top is not known. Probably over 250m thick. Tidally influenced shallow-marine to supratidal deposits.||Topmost Renner Group.||Conformably and transitionally overlies Jangirulu Formation. Is overlain unconformably by Montejinni Limestone.|Recessive lower part comprises fine- to medium-grained, thinly bedded, ripple-marked sandstone, siltstone and shale, beneath a more resistant ferruginous and poorly-moderately sorted quartz sandstone, and sparse sandstone, mudstone and chert.|24-FEB-17
38405|Lake Woods beds|71779|5|Briefly described|p23, p24, p26, p27|||Tomkinson Province.||Renner Group||||24-SEP-18
38405|Lake Woods beds|71893|5|Briefly described|p6, p8, p64|||Tomkinson province.||Renner Group||Conformably overlies the Jangirulu Formation.||
38405|Lake Woods beds|73083|6|Mentioned|p27|Proterozoic|Proterozoic||||||Ferricrete with sandstone, mudstone, dolostone, chert, and conglomerate.|
34216|Laminaria Formation|22663|6|Mentioned|NT97 -1-4 p3|||||||||
34216|Laminaria Formation|24427|5|Briefly described|p49 Fig.2|Late Jurassic|Middle Jurassic|Geological Province: Bonaparte Basin.||||||
34216|Laminaria Formation|61548|6|Mentioned|p480 Fig.3, p483|Callovian|Callovian|Northern Bonaparte Basin.||||||
34216|Laminaria Formation|64689|5|Briefly described|p7 Fig.6 |Late Jurassic|Middle Jurassic|||||||
34216|Laminaria Formation|64696|6|Mentioned|p125, p127 Fig.2, p131, p136|Late Jurassic|Middle Jurassic|Reservoir unit. Referred to as Elang/Laminaria Formation in the Joint Petroleum Development Area.|||||Sandstones.|
34216|Laminaria Formation|68223|6|Mentioned|p178 Fig.3, p186|Callovian|Bathonian|||||||
34216|Laminaria Formation|69452|5|Briefly described|p36:15, 21-22|Late Jurassic|Middle Jurassic|Bonaparte Basin. Appears as Laminaria Fm/Elang Fm.||Flamingo Group.||Equivalent to Elang Formation.||12-JUL-16
34216|Laminaria Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Is overlain by Cleia Formation.||
34216|Laminaria Formation|70061|5|Briefly described|Regional geology p6-7|Late Jurassic|Middle Jurassic|Bonaparte Basin; commercial petroleum reservoir. Appears as Elang (Laminaria) Formation.|||||Retrogradational deltaic sandstones.|12-JUL-16
69780|Lander Rock Formation|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tanami Group. Includes the Yinabalbu Member and three unnamed facies: greenschist, amphibolite and granulite facies.  Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
69780|Lander Rock Formation|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province. Greenschist facies schist, amphibolite facies schist, granulite facies, gneiss.||||||07-NOV-08
69780|Lander Rock Formation|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Greenschist facies metapsammite and metapelite, schist. Amphibolite and Granulite facies schist and gneiss.||||||07-NOV-08
69780|Lander Rock Formation|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.|||Includes Yinabalbu member.||Greenschist, amphibolite and granulite facies; gneiss, schist.|19-DEC-12
69780|Lander Rock Formation|62637|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region - Aileron Province. Greenschist and amphibolite facies schist, psammite and greywacke.||||||23-DEC-09
69780|Lander Rock Formation|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated mica, hornblende biotite and amphibolite, dolerite; schist. Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
69780|Lander Rock Formation|63866|5|Briefly described|p93|||Reynolds Range, Aileron Province.|c. 1790 Ma|||||
69780|Lander Rock Formation|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Interbedded psammite and pelite; quartz-muscovite schist; may include meta-banded iron-formation and Interbedded metabasalt, metarhyolite and metavolcaniclastic rocks, including metavolcanic conglomerate.||||||15-DEC-08
69780|Lander Rock Formation|64677|5|Briefly described|v, p1, p24-26, p55-56|||Arunta Region, Aileron Province. Complex range of ages discussed: an alternative maximum depositional age is 1773 +/- 12 Ma.|1842 +/- 7 Ma (maximum depositional age).||||Metapsammite, quartz-muscovite-biotite schist, migmatite.|
69780|Lander Rock Formation|64735|6|Mentioned|p215, p217|||Similar detrital zircon age spectra to Bullion Schist; correlated with Mount Stafford Beds of Vernon et al (1990).||||||
69780|Lander Rock Formation|64736|4|Described|p220, 221-2, p224-225, p227, Figs.1, 8|Orosirian|Orosirian|Thickness unknown. SHRIMP U-Pb detrital zircon max depositional age.|1868 Ma.|Of Lander Package.||Underlies Reynolds Range Group unconformably.|Dominantly consists of interbedded pelitic and psammitic metasediments, interpreted to represent turbiditic sedimentation. Interlayered igneous rocks.|30-APR-12
69780|Lander Rock Formation|64737|4|Described|p231, 235, 236-42, 244,Tab.1, Figs.5, 6||Orosirian|Formerly known as Lander Rock Beds.  Name used for low grade metamorphic rocks in the Aileron Province. Occupies more than 60% of exposure in the Aileron Province. Thickness unknown. Intruded by Stafford Event plutons. Provenance dominated by ~1880-1840 ages||Of Lander Package.|||Interbedded pelitic and psammitic rocks interpreted to represent dominantly turbiditic sedimentation. Locally interlayered basalt and dolerite.|30-APR-12
69780|Lander Rock Formation|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Ngadarunga Granite.  Greenschist facies; schist, quartzite; Amphibolite facies: biotite-muscovite schist,  quartz granofels; Granulite facies: migmatitic gneiss, quartzite, mafic gneiss||||||
69780|Lander Rock Formation|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Ngadarunga Granite.  Greenschist facies; schist, quartzite; Amphibolite facies: biotite-muscovite schist,  quartz granofels; Granulite facies: migmatitic gneiss, quartzite, mafic gneiss;  ||||||
69780|Lander Rock Formation|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Informally subdivided into four facies with with distinctive magnetic responses. Greenschist-facies interbedded metapsammite and metapelite; amphibolite-facies schists, metapsammite; granulite-facies migmatitic gneiss; retrogressed gneiss ||||||
69780|Lander Rock Formation|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|In some places differentiated into Walabanba and Anningle members, and two unnamed members. Succession of metasedimentary and stratiform mafic (meta-)igneous rocks.||||||
69780|Lander Rock Formation|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|In some places differentiated into Walabanba and Anningle Members, and two unnamed members. Succession of metasedimentary and stratiform mafic (meta-) igneous rocks.||||||
69780|Lander Rock Formation|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Aileron Province. Includes Yinabalbu member. Age: older than Stafford Event (1805 Ma)?. Dominantly quartz-muscovite-biotite pelitic schist and phyllite interlayered with quartz-muscovite psammite; includes a component of high-grade metasediments||||||
69780|Lander Rock Formation|65338|3|Fully described|App1 p82, p6-17|Statherian|Orosirian|Shallow to deep-water marine. Definition only gives maximum depositional age from detrital zircons. Minimum age from intrusion by Harverson Granite at 1799+/-3Ma. Correlated with Ooradidgee Group, at least in part. Greenschist to granulite facies metamorphism from c.1805-1790 Stafford Event with syn-tectonic granite intrusions. Hosts orogenic gold. Monotonously uniform and widespread.|c.1840 - 1799 Ma.||Includes Walabanba, Anningie, Woodalla and Mount Stafford Members.|Intruded by Koonoonyeri granites, Yaningidjara Orthogneiss, Harverson Granite, dolerite and gabbro. Is overlain by Reynolds Range Group.|Metapsammitic and metapelitic rocks: hornfels, slate, phyllite and schist, variably metamorphosed from greenschist to granulite grade; stratiform amphibolites; rare calc-silicate rocks.|
69780|Lander Rock Formation|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||Grouped with Reynolds Range Group in Fig 2.||19-DEC-12
69780|Lander Rock Formation|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region. See also Lander Rock beds.||||||
69780|Lander Rock Formation|65358|5|Briefly described|p6, p10-11, p13, p17-18|Orosirian|Orosirian|In Arunta Region. Unconformably overlain by Reynolds Range Group. Correlated with Killi Killi Formation in Tanami Region. Turbiditic. Deposited at ~1860-1830 Ma; metamorphosed to greenschist to granulite facies.||||||
69780|Lander Rock Formation|65556|5|Briefly described|p29, p37, p44-45||Orosirian|Sedimentary rocks. Widespread in the Arunta Region. Similar age spectra to rocks analysed in this study suggest correlation with the Casey Inlier and Anira Metamorphics. ~1830 Ma maximum depositional age. Intruded by Stafford Event magmatic intrusions at ~1810-1800 Ma.||||||
69780|Lander Rock Formation|66767|6|Mentioned|p57|||Aileron Province.||||||
69780|Lander Rock Formation|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||||Quartz muscovite-biotite schist, fine- to medium-grained, layered; granulite-facies pelitic, migmatitic gneiss; granulite, strongly foliated and folded; metapsammite.|
69780|Lander Rock Formation|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province. Several separately-mapped but un-named units have their lithologies and magnetic responses indicated.|||Includes Anningie, Walabanba, Woodalla and Mount Stafford Members.||Undifferentiated mica, hornblende-biotite and hornblende schist; phyllite; heavy mineral-bearing/micaceous quartzite; amphibolite; dolerite; rare muscovite-sillimanite, and microcline-sillimanite-garnet-bearing schist.|
69780|Lander Rock Formation|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.|||||Dominantly greenschist facies: quartz-muscovite psammite, micaceous greywacke, quartz-muscovite schist; includes amphibolite facies: micas-andalusite schist and psammite; lesser granulite facies: migmatite with psammitic layers.|
69780|Lander Rock Formation|67352|6|Mentioned|p50|||||||||
69780|Lander Rock Formation|67479|6|Mentioned|p56|||Comprises a widespread body of typically low-grade metasedimentary rocks.||||||
69780|Lander Rock Formation|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||Includes Mount Stafford, Woodalla, Anningie and Walabanba Members.||Undifferentiated: mica, hornblende-biotite and hornblende schist; phyllite; heavy mineral-bearing/micaceous quartzite; amphibolite, dolerite; rare muscovite-sillimanite, and microcline-sillimanite-garnet-bearing schist.|
69780|Lander Rock Formation|68656|5|Briefly described|GEOCHRON|Paleoproterozoic|Paleoproterozoic|Arunta Orogen. Widespread unit. Age is maximum depositional age from detrital zircons.|1838 +/- 15 Ma (Kirkland et al., 2009).|||Is correlated with Killi Killi Formation.||
69780|Lander Rock Formation|68697|6|Mentioned|v, p44|||N, W and Central Aileron Province. Typical detrital zircon spectrum is dominated by post-1900 Ma ages.||||||18-APR-18
69780|Lander Rock Formation|68994|4|Described|p4, p6-12, p20, p23-24, p26-27|Orosirian|Orosirian|Widely distributed, though poorly exposed over northern and western Aileron Province. Metasandstone analysed. Conservative max depositional age of 1872+/-5 Ma (Kirkland et al. 2009). Detrital zircon U-Pb ages listed and Hf analyes detailed.|1840-1830 Ma (Scrimgeour 2006).|||Intruded by Carrington Suite granitic rocks. Equivalent to Killi Killi Formation (Tanami Group). Is unconformably overlain by Munyu Sandstone.|Polydeformed, psammitic and pelitic schists (interbedded quartz-muscovite-biotite schist) and minor interbedded banded-iron formation; predominantly greenschist to amphibolite facies; interpreted largely turbiditic origin.|13-JAN-17
69780|Lander Rock Formation|68997|4|Described|vi-vii,p1,26-28|Orosirian|Orosirian|Widely distributed unit that is sporadically exposed across much of the northern and western Aileron Province. Oldest exposed rocks in the Aileron Province. Similar stratigraphic position to Aileron and Chiripee Metamorphics. Oldest zircon spectra includes c. 3438 Ma. Zircon age spectra from psammitic gneiss (Sample: AC08CJE271A. Grid Reference: MGA94 Zone 53: 370504mE 7550491mN) of 1835+\-6 Ma (in northwestern ALCOOTA), interpreted as maximum depositional age. Metamorphic zircon rims dated at 1763+\-6 Ma are interpreted to reflect a marginally younger event than the 1780-1770 Ma Yambah Event.|1835+\-6 Ma (max dep age: U-Pb zircon)||||Interbedded pelitic and psammitic metasedimentary rocks; turbiditic.|
69780|Lander Rock Formation|68998|5|Briefly described|v, p12-13, p31|Paleoproterozoic|Paleoproterozoic|||||Is intruded by Ennugan Mountains Granite.||
69780|Lander Rock Formation|69003|5|Briefly described|p5, p31|Paleoproterozoic|Paleoproterozoic|Aileron Province, West Arunta Orogen.|1840-1835 Ma.|||Is intruded by the Carrington Suite.|Polydeformed metasedimentary rocks.|
69780|Lander Rock Formation|69031|5|Briefly described|p3-4, p6-7, p12, p23, p43, p50, p59, p79|Orosirian|Orosirian|Oldest outcropping rocks in the Aileron Province, Arunta Orogen. Detrital zircon age spectra described. Quartz veins and pegmatite host base metal deposits (eg Clark and Mount Hardy Cu prospects). Has a distinct magnetic response (discussed). Uranium-enriched: distance to this unit was used as a predictor in modelling for U sources.|1840-1835 Ma.|||Is intruded by Carrington Suite.|Polydeformed psammitic and pelitic rocks, and minor interbedded BIF.|
69780|Lander Rock Formation|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. Three facies are mapped separately: greenschist facies, amphibolite facies, and transitional amphibolite-granulite to granulite facies.|||||Quartz-muscovite+biotite schist; quartz-muscovite+biotite+andalusite+garnet+tourmaline schist; pelitic, psammopelitic and lesser psammitic migmatitic gneiss, lesser felsic migmatitic gneiss, minor mafic granulite.|
69780|Lander Rock Formation|69383|6|Mentioned|p70, 72, 74, 80|||Arunta Region. Includes inherited zircon population in the 1880-1800 Ma range, as does Utopia Quartzite.||||||
69780|Lander Rock Formation|69417|5|Briefly described|p2:4,|Orosirian|Orosirian|Aileron Province. Turbiditic succession.|1845-1835 Ma.|||||12-JUL-16
69780|Lander Rock Formation|69418|6|Mentioned|p3:21, 31, 33|||Arunta Region. Hosts the Anningie field pegmatite Sn deposit and the Mount Doreen field (Wolfram Hill) pegmatite W deposit (described). Also hosts the Nolans Bore phosphate-REE-U deposit (described).||||||12-JUL-16
69780|Lander Rock Formation|69424|5|Briefly described|p9:4, 34|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Experienced bimodal magmatism and folding during the c.1800 Ma Stafford Event.||||Correlative of Ooradidgee Group.||12-JUL-16
69780|Lander Rock Formation|69425|6|Mentioned|p10:6||||||||Includes schists.|12-JUL-16
69780|Lander Rock Formation|69426|5|Briefly described|p11:4 Fig.11.3, 11:11|||Occurs extensively over N and W Aileron Province. The two facies associations are mapped separately in Fig.11.3.||||Correlated with Killi Killi Formation.|Amphibolite-facies pelitic and psammitic schist, gneiss; granite. Greenschist- to amphibolite-facies pelitic and psammitic schist, gneiss; granite.|12-JUL-16
69780|Lander Rock Formation|69427|3|Fully described|p12:3-7,13,18-22,24-27,29,32-33,41|||See also 12:57,59-60,62. Donnellan (2008). Formerly Lander Rock beds of Stewart et al. (1980), Stewart (1981), Young et al. (1995). Widely distributed across N and W Aileron Province. Interbedded pelitic and psammitic rocks of predominantly turbiditic origin. Crops out poorly. Type locality at Lander Rock. Neither base nor top is exposed; suggested minimum thickness 1000m. Equivalent of Killi Killi Formation and Ooradidgee Group. Metamorphic grade varies from greenschist to granulite facies, mapped separately. Deformation described in some detail. Mafic intrusions described. Some areas of this unit mapped by Stewart (1981) were included by Dirks (1990) in his version of the Reynolds Range Group. Detrital zircon maximum depositional age; other ages given. Likely that deposition was between 1840-1830 Ma. Metamorphic zircon rims are dated at 1806 +/- 7 Ma (Kinny, 2002) and c.1760 Ma (Claoue-Long and Scrimgeour, unpublished). Hosts a number of lode gold occurrences (briefly described). Associated with the Nolans Bore REE-P-U-Th deposit (detailed).|<1858 +/- 4 Ma (Claoue-Long et al., 2008).||Mount Stafford Member.|Is overlain by Mount Thomas Quartzite. Is intruded by Stafford, Ooralingie, Redhackle, Wabudali and Bean Tree Granites; Boothby Orthogneiss, Napperby Gneiss and Yumurrpa Granophyre.|Monotonous succesion of lineated biotite-muscovite-andalusite schist, micaceous metasandstone and quartzite; cleaved siltstone and slate; migmatitic units; local minor calc-silicate rock, conformable mafic layers (mainly amphibolite).|12-JUL-16
69780|Lander Rock Formation|69440|5|Briefly described|p25:2|||||||Is overlain unconformably by Munyu Sandstone.|Metasediments including intensely weathered, strongly foliated quartz-mica-feldspar schist.|12-JUL-16
69780|Lander Rock Formation|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Four un-named subunits are mapped separately.|||||Granulite-facies sillimanite-garnet-biotite-cordierite migmatite with small mafic granulite inclusions, rare quartzite. Amphibolite-facies quartz-muscovite-biotite(-andalusite) schist, interbedded metapsammite and metapelite, quartz-muscovite schist.|
69780|Lander Rock Formation|69554|6|Mentioned|p139|||Aileron Province, Arunta Region, Northern Australian Craton. Contains detrital zircons aged c.1920 Ma.||||||
69780|Lander Rock Formation|69587|5|Briefly described|177278.1.pdf|||Geological province: Arunta Orogen. Kirkland et al. (2009) reported a maximum depositional age of 1838+\-15 Ma for a metasandstone sample.|c. 1840-1830 Ma|||Correlable with Killi Killi Formation.||
69780|Lander Rock Formation|69794|6|Mentioned|p16|||Comprises c. 1865 Ma zircon provenance peak, with broad clusters between 2000-1900 Ma and 2550-2500 Ma, and sporadic Archean ages.||||||
69780|Lander Rock Formation|69917|4|Described|p55-57, 117, 82, 87, 93||Paleoproterozoic|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Dating indicates maximum depositional age of 1835+/-6 Ma and metamorphic zircon growth during the high-grade 1780-1770 Ma Yambah Event||||Intruded by Woola Downs Granite. Detrital zircon signature similar to Delny Metamorphics.|Psammitic gneiss.|
69780|Lander Rock Formation|70301|5|Briefly described|p7, p11, p16, p19|Paleoproterozoic|Paleoproterozoic|Mentioned as having ages typical of 2394-1974 Ma zircons occurring in Wangala Granite.||||Is intruded by Wangala Granite and Ennugan Mountains Granite.|Metasedimentary rocks.|
69780|Lander Rock Formation|70376|5|Briefly described|p832, p832 fig 1, p847|Paleoproterozoic|Paleoproterozoic|Intruded by magmatic rocks in the 1810 - 1770 Ma period. Shown as Lander Package p849.|1866-1806 Ma|||Unconformably overlain by Reynolds Range Group|Greywacke, siltstone, shale, schist, gneiss, pelites and psammitic metasediments.|
69780|Lander Rock Formation|70554|4|Described|p798,815|Paleoproterozoic|Paleoproterozoic|Geologial province: Aileron province. Comprised of two similar but temporally discrete (1840-1810 and 1805-1780 Ma) turbiditic packages. Underwent high-grade (to granulite-facies) metamorphism during Chewnings Orogeny and emplacement of late-metamorphic pegmatites (Collins and Williams, 1995).|||||Psammitic metasedimentary rocks; schist, phyllite, andalusite hornfels, garnet-cordierite-biotite-quartz granofels, sillimanite-biotite-cordierite-orthoclase granofels and tourmaline-bearing quartzite.|
69780|Lander Rock Formation|70739|6|Mentioned|p540|||Arunta Region. Has correlatives in the Tanami and Tennant Creek Regions.|1860-1830 Ma.|||||
69780|Lander Rock Formation|70762|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton. Two un-named sub-units are mapped separately: metamorphosed BIF interbedded with psammitic and pelitic schist; and felsic volcanic metasandstone and metaconglomerate interbedded with amygdaloidal metabasalt.|<1840 Ma.|||Is overlain by Lake MacKay Quartzite.|Interbedded psammitic and pelitic schist; quartz-muscovite schist; may include metamorphosed BIF and metavolcanic rocks.|
69780|Lander Rock Formation|70826|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|Aileron Province.||||||
69780|Lander Rock Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region. In the Interpreted Geology diagram, this unit is mapped as two facies, each including undivided granite of Grimwade and Frederick Suites: amphibolite facies pelitic and psammitic schist, gneiss; and greenschist to amphibolite facies pelitic and psammitic schist, gneiss.|||||Biotite-muscovite-andalusite +/- garnet pelitic schist and metapsammite.|
69780|Lander Rock Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, gneiss, greywacke, amphibolite, psammite, schist|
69780|Lander Rock Formation|71302|5|Briefly described|p73|Paleoproterozoic|Paleoproterozoic|Geological province: Arunta region. Paleoproterozoic metasedimentary sequence exposed on the North Australian Craton, and possibly one of several sources of zircon provenance to the Inverway Metamorphics.||||||
69780|Lander Rock Formation|71348|5|Briefly described|p198,201,209,211-212,214-218|Orosirian|Orosirian|Geological province: Aileron Province, Arunta Region. Maximum depositional age between c. 1860 Ma and c. 1830 Ma. Also contains c. 2100-1900 Ma zircon, and Neoarchean to earliest Paleoproterozoic detrital zircon component. Underwent HTLP metamorphism, moderate strain and intrusion by felsic and mafic intrusions from c. 1780-1770 Ma Yambah Event. See p215 for summary of U-Pb geochronological data.||||Overlain unconformably by Reynolds Range Group and Lake Mackay Quartzite.||
69780|Lander Rock Formation|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen, North Australian Craton.|<1838 Ma.||||Interbedded psammitic and pelitic schist, quartz-muscovite schist; may include metamorphosed BIF and metavolcanic rocks.|
69780|Lander Rock Formation|71839|5|Briefly described|iii, p7-p8|||Hosts mineralisation at the Silver King Cu-Pb-Zn-Ag prospect in central DOREEN. U-Pb SHRIMP maximum depositional zircon ages range from 1869+/-4 to 1858+/-4 Ma.|||||Muscovite-sericite schist.|21-MAR-23
69780|Lander Rock Formation|71858|4|Described|p5-p6, p44-p45|||Aileron Province.|ca 1860-1830 Ma||Includes the Mount Stafford beds and the Walabanba Member.|Unconformably overlain by the Wickstead Creek beds (Reynolds Range Group). Intruded by the Wangala Granite and the Ennugan Mountains Granite.||
69780|Lander Rock Formation|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.|||||Interbedded psammite and pelite; quartz--muscovite schist; may include metamorphosed banded iron-formation and metavolcanic rocks.|
69780|Lander Rock Formation|72366|4|Described|p1-2,4-5, p7|Orosirian|Orosirian|Geological province: Aileron Province. Hosts the Mount Hardy Cu-Pb-Ag-Zn deposit (MOUNT DOREEN map sheet). Intruded by barren and mineralised pegmatites, and mineralised quartz veins (Kiek 1941, Grainger 1968, Scrimgeour 2013). Maximum depositional age provided from SHRIMP U-Pb dating ranging between c. 1869 to 1858 Ma and peak zircon spectra at c. 1880-1840 Ma (Donnellan 2008, Scrimgeour 2013 and references therein). Sample MD15MVM001 (766491mE 7552939mN; molybdenite) is from molybdenite-bearing quartz vein in pegmatite selvage that intrudes into quartz-muscovite schist of the LRF; yields Re-Os model age of 1799.9+\-7.8 Ma (consistent with Ngadarunga Granite). Sample MD16MVM078 (766405mE 7552941mN, molybdenite) is from a quartz-muscovite pegmatite intruding in LRF; yields Re-Os model age of 1817.4+\-8.7 Ma. These ages are interpreted to represent magmatic crystallisation ages and the timing of pegmatite emplacement. Preserves zones of partial melting around contact zones with Ngadarunga Granite.||||Correlable to Killi Killi Formation. Intruded by Ngadarunga Granite.|Interbedded turbidites: pelitic and psammitic metasedimentary rocks.|08-JAN-20
69780|Lander Rock Formation|72376|5|Briefly described|iii,p1,3,6|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Hosts the Wilfram Hill tungsten-copper deposit, which is intimately associated with muscovite-bearing pegmatite and quartz veins that intrude and cross-cut the Lander Rock Formation. Mineralisation is hosted in two main reefs of pegmatite and quartz veins (Wells 1972, Warren et al 1974, Young et al 1995). Previous studies provide U-Pb SHRIMP maximum depositional zircon ages spanning from 1869+\-4 Ma to 1835+\-6 Ma (Claoue- Long et al 2008, Donnellan 2008, Scrimgeour 2013, Bodorkos et al 2013). 40Ar/39Ar analysis of sample NTGS MD15MVM015 (muscovite in muscovite-bearing pegmatite that intrudes foliated muscovite schist of Lander Rock Formation) yielded an interpreted minimum age of 1550+\-4 Ma for tungsten and copper mineralisation at Wolfram Hill deposit; this age is consistent with that of Yarunganyi Grantie (1567+\-11 Ma; Young et al., 1995).|||||Foliated, metasedimentary, lower amphibolite facies biotite-muscovite-andalusite-quartz schist and minor metasandstone.|
69780|Lander Rock Formation|72378|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Regionally widespread unit, with a maximum depositional age of c 1.86-1.84 Ga (Claoue-Long et al., 2008a; Bodorkos et al., 2013; Scrimgeour 2013) and a likely depositional age of c. 1.84 Ga (Cross and Crispe 2007).||||Correlable with Bullion Schist.||
69780|Lander Rock Formation|72516|6|Mentioned|p7|||Aileron Province.||||||
69780|Lander Rock Formation|72527|6|Mentioned|p184, p192.|Paleoproterozoic|Paleoproterozoic|Given as an example of correlated units across the Northern Territory with the Murphy Metamorphics. Ref Hollis et al., 2010; Carson, 2013; Cross and Crispe, 2007; Bodorkos et al., 2013; Kositcin et al., 2012, 2013, 2014, 2015a).||||||
69780|Lander Rock Formation|72711|6|Mentioned|p4 Tb.1, p5-6, p6 Fig.4.|Orosirian|Orosirian|Maximum depositional ages of 1840-1830 Ma. (detrital zircon 207Pb/206Pb ages; Young et al 1995, Pietsch 2001, Claoue-Long and Edgoose 2008, Donnellan 2008). These are the oldest known rock formations in the Aileron Province.|c. 1840 Ma. to c. 1830 Ma max. dep.ages||||Includes metasedimentary gneiss and schist, metamudstone, lenses of massive breccia.|
69780|Lander Rock Formation|72894|5|Briefly described|piii, p1, p5-8, p10-13, p16, p19, p23|Statherian|Orosirian|Geological Province: Aileron Province; listed geochronology represents conservative maximum depositional ages for the sedimentary protolith from two samples; high-grade metamorphism is dated at 1769 +/- 14 Ma and 1761 +/- 4 Ma from two samples; unnamed samples of mafic granulite, metapsammite, and S-type granite were dated and correlated to the Lander Rock Formation|1832 +/- 10 Ma and 1841 +/- 8 Ma SHRIMP U-Pb||||Granulite-facies metasedimentary rocks; metapelites that locally have garnet-bearing leucosome patches interlayered with cordierite-biotite-garnet-quartz metapsammite; intermingled with coarse-grained S-type granite (formed from in-situ from melting)|
69780|Lander Rock Formation|73083|6|Mentioned|p11|Orosirian|Orosirian|An age of deposition of 1840-1830 Ma was reported by Scrimgeour (2013). Not equivalent to Ledan Schist.|1840-1830 Ma|||Equivalent to Ooradidgee Group.||
69780|Lander Rock Formation|73089|6|Mentioned|p3, p32-33, p41|Paleoproterozoic|Paleoproterozoic|Aileron Province. Dominantly Paleoproterozoic detritus. Has a similar lithology and provenance signature to both the Killi Killi and Olympio formations. Deposited sometime between c. 1872-1835 and 1820-1770 Ma.||||||
69780|Lander Rock Formation|73399|6|Mentioned|p2, App.E|Orosirian|Orosirian|Oldest rocks in the Reynolds-Anmatjira Ranges. Metamorphosed by voluminous granitic magmatism between 1810 and 1790 Ma. [Previously called the Lander Rock Beds].|ca. 1840 to 1806 Ma|||Unconformably overlain by the Reynolds Range Group.|Pelitic and psammitic metasedimentary rocks.|
69780|Lander Rock Formation|73445|5|Briefly described|p7|||West Arunta Orogen. Is intruded by 1773 +/- 6 Ma granitic rocks.|1840-1835 Ma (MDA: Scrimgeour, 2006).|||Is overlain by Lake McKay Quartzite.|Metasedimentary rocks.|
69780|Lander Rock Formation|73592|5|Briefly described|p3, 9-10|Paleoproterozoic|Paleoproterozoic|Aileron Province. Several other maximum depositional age determinations are given. Intruded by c.1820-1770 Ma granites. Deformed at c.1810-1790 Ma.|1855 +/- 4 Ma (MDA: Kositcin et al., 2019).|||Likely correlative of Bullion Schist.|Sedimentary, volcanic and volcaniclastic rocks.|
69780|Lander Rock Formation|74204|5|Briefly described|p2|Orosirian|Orosirian|Tightly folded during the Stafford Event (1810-1800 Ma).|1840-1810 Ma||||Thick package of turbidite-related mudstones and sandstones.|
73328|Larranganni Formation|64277|5|Briefly described|Map ledgend|Mesozoic|Mesozoic|Geological Province: Canning Basin. Sandstone; minor siltstone and conglomerate.||||||
73328|Larranganni Formation|66129|5|Briefly described|p215 Fig.2|||Sandstone, siltstone, minor conglomerate, commonly silicified. Mesozoic?||||||
73328|Larranganni Formation|68474|5|Briefly described|p573|Mesozoic|Mesozoic|Granites-Tanami Orogen.|||||Sandstone, siltstone, shale, minor conglomerate; commonly silicified.|
73328|Larranganni Formation|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Mesozoic|Mesozoic|Canning Basin|||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|69587|5|Briefly described|GEOL_LUT_CSV files|Mesozoic|Mesozoic|Of Canning Basin. Events: Alice Springs Orogeny; Point Moody Extension; Prices Creek Movement; Red Bluffs Extension; Van Emmerick Extension. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv.|252.17-66 Ma (inferred)||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|70141|5|Briefly described|Map legend.|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone and conglomerate.|
73328|Larranganni Formation|70143|5|Briefly described|Map legend|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone and conglomerate.|
73328|Larranganni Formation|70154|5|Briefly described|500k_interpgeop14_lut.csv|Mesozoic|Mesozoic||66-251 Ma||||Sandstone, minor siltstone, and conglomerate|
73328|Larranganni Formation|70826|6|Mentioned|p7 tbl 4|Mesozoic|Mesozoic|Eastern Canning Basin.||||||
73328|Larranganni Formation|70852|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Sandstone, minor siltstone and conglomerate, poorly sorted, quartz-rich.|
73328|Larranganni Formation|71267|4|Described|GEOL_LUT_CSV files|Mesozoic|Mesozoic|Of Canning Basin. Events: Point Moody Extension (300-242 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|252.17-66 Ma (inferred)||||Medium grained and thin to medium bedded fluvial quartz sandstone with minor siltstone and conglomerate|
73328|Larranganni Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesozoic|Mesozoic|Canning Basin.|||||Sandstone, minor siltstone, and conglomerate.|
41846|Larrie Granodiorite|67565|2|Defined|p62-63, p6 Table 1, p18, p19.|Statherian|Statherian|New name, after Mount Larrie. Yaya Domain, Warumpi Province. Previously included in undifferentiated Arunta Complex (Ranford, 1969). Type area in a creek 4 km ENE of Mount Larrie. A large east-trending body forming prominent hills (eg Mount Larrie). Has intrusive contacts (with no clear timing relationship) with the Warumpi Granite. Aged between c.1644 Ma and c.1631 Ma. Has strong geochemical affinity with the other units in Waluwiya Suite. Supports distinctive vegetation: native pines and beantrees.||Unit in Waluwiya Suite.||Intrudes Papunya Igneous Complex and Inyalinga Granulite. Is intercalated with Warumpi Granite.|Medium-grained, weakly porphyritic to equigranular, foliated and leucosome free, hornblende-biotite-garnet granodiorite; abundant xenoliths of mafic rock; local minor weakly strained to undeformed charnockite.|01-DEC-15
41846|Larrie Granodiorite|68832|5|Briefly described|p7, 10, 21|||||||Intruded by Warumpi Granite. Intrudes quartzite of Inyalinga Granulite.||
41846|Larrie Granodiorite|69428|5|Briefly described|p13:9-11|Paleoproterozoic|Paleoproterozoic|Yaya Domain, Warumpi Province. A large E-trending body, forming prominent hills (eg Mount Larrie).||Waluwiya Suite.||Intrudes Papunya Igneous Complex. Intercalated with Inyalinga Granulite and Warumpi Granite.|Medium-grained, weakly porphyritic to equigranular granodiorite with abundant mafic xenoliths.|12-JUL-16
79095|Last Hope Gneiss|69917|5|Briefly described|p177, 1|Neoproterozoic|Neoproterozoic|||Of Harts Range Metamorphic Complex.||Underlies Yambla Gneiss.||
79095|Last Hope Gneiss|72516|5|Briefly described|p79|Cambrian|Neoproterozoic|New units incorporated into the Harts Range Metamorphic Complex by Whelan et al (in prep). Irindina Province.||Harts Range Metamorphic Complex||||20-APR-22
79095|Last Hope Gneiss|72524|5|Briefly described|p8, p9, p13.|||Preserves a detrital zircon spectra with age populations between ca 1.24 and 0.96 Ga and scattered individual date as young as ca 0.63 Ga. Previously upper Stanovos Gneiss of Maidment et al., 2013.||Harts Range Metamorphic Complex||||20-APR-22
81666|Last Hope dolerite|72379|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Informally named unit of Donellan (in review; see this record), interpreted to be correlable to Pedlar Gabbro. Maidment et al (2006) reported SHRIMP U-Pb zircon age of 1811+\-5 Ma, interpreted to record the timing of emplacement.. In Pioneer deposit area.|1811+\-5 Ma (emplacement; SHRIMP U-Pb).|||||03-OCT-19
22174|Latram Granite|22538|6|Mentioned|Fig3 P708||Statherian|Age of unit is 1712+/-10 Ma.||||||13-OCT-06
22174|Latram Granite|22600|4|Described|Map legend|Statherian|Statherian|||||||
22174|Latram Granite|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1712+/-10Ma.||||||13-OCT-06
22174|Latram Granite|24047|5|Briefly described|p83 Fig. 71|Paleoproterozoic|Paleoproterozoic|Age: ca.1712Ma.||||||07-NOV-08
22174|Latram Granite|24048|5|Briefly described|p14 Fig. 5|||Geological Province: McArthur Basin.||||||
22174|Latram Granite|24049|5|Briefly described|Map Legend|Statherian|Statherian|Granite: massive, red, fine to medium-grained, equigranular, fayalite-bearing; subvolcanic. Geol. Prov: McArthur Basin.||||||12-OCT-05
22174|Latram Granite|24197|5|Briefly described|p29, p54|Paleoproterozoic|Paleoproterozoic|One of 3 small granites associated with the Fagan Suite, the others being Jimbu and Packsaddle Granites.||||||07-FEB-11
22174|Latram Granite|44112|2|Defined|p1,10,13,44-45,109||Statherian|Max Age: 1712 (+/-) 10 Ma.||||||13-OCT-06
22174|Latram Granite|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 +/- 10Ma (SHRIMP).||||||06-JUN-18
22174|Latram Granite|61403|5|Briefly described|Map Legend|Statherian|Statherian|Granite: massive, red, fine to medium-grained, equigranular, fayalite-bearing; subvolcanic. Geol. Prov: McArthur Basin.||||||
22174|Latram Granite|63866|5|Briefly described|p115|||Caledon Shelf/Arnhem Inlier.|1712 +/- 10 Ma (Page, OZCHRON)|||Conformably overlain by the Yanungbi Volcanics. Intrudes the Spencer Creek Group.||
22174|Latram Granite|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian|[?Odd for a granite to be part of a Group.]|1712 +/- 10 Ma.|Shown as of the Spencer Creek Group Fig 4.||Shown as coeval with Yanungbi Volcanics Fig 4.||06-JUN-18
22174|Latram Granite|69421|5|Briefly described|p6:3 Tb.6.1||||1712 +/- 10 Ma.|||?Intrudes Giddy Granite.||12-JUL-16
22174|Latram Granite|69430|5|Briefly described|p15:3-4|||NE McArthur Basin. Subvolcanic plutons.|1712 +/- 10 Ma.|Spencer Creek Group.||||12-JUL-16
22174|Latram Granite|69673|6|Mentioned|p16 fig 13, p17|Statherian|Statherian|Comagmatic subvolcanic plutons. Northeastern McArthur Basin.|1712 +/- 10 Ma|Spencer Creek Group||Overlain by Gove Sandstone||
22174|Latram Granite|70302|5|Briefly described|iv, p7, p9|Statherian|Statherian|Rawlings et al. (1997). Coeval and possibly comagmatic with Yanungbi Volcanics.|1712+/-10 Ma (Page, 1996; Rawlings et al., 1997).||||Subvolcanic granite.|
22174|Latram Granite|70719|5|Briefly described|p15|Statherian|Statherian|Arnhem Province.|1712 +/- 10 Ma (Page, 1996).|||Intrudes Giddy Granite (inferred).||
22174|Latram Granite|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1712+/-10 Ma (crystallisation: Pb/Pb zircon).||||Syenite.|
22174|Latram Granite|71606|5|Briefly described|p135|Statherian|Statherian|McArthur Basin. Associated with 1710-1700 Ma Fagan Phase magmatism of Rawlings 1994.||Unit of Donydji Group.||Hosted in the upper Donydji Group.||
22174|Latram Granite|72377|5|Briefly described|p12, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Page (1996c) reported SHRIMP U-Pb zircon age of 1712+\-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). Sub-volcanic unit, co-magmatic with Yanungbi Volcanics.|1712+\-11 Ma (magmatic)|Unit of Spencer Creek Group.||||10-OCT-19
24355|Laughlen metamorphics|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24355|Laughlen metamorphics|39552|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24355|Laughlen metamorphics|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
24355|Laughlen metamorphics|39610|6|Mentioned|p6|||||||||
24355|Laughlen metamorphics|39887|6|Mentioned|Fig.1|||||||||
24355|Laughlen metamorphics|48992|3|Fully described|p32|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24355|Laughlen metamorphics|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (Division 3). Muscovite-biotite schist, quartzite.||||||02-NOV-04
40579|Lawn Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Amos Formation, Smythe Sandstone and lower parts of Balbirini Dolostone.|||
40579|Lawn Supersequence|63866|5|Briefly described|p53|||Isa Superbasin.|||Includes the Amos Formation and the Balbirini Dolomite, lower.|||
40579|Lawn Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Statherian|Statherian|Lawn Hill Platform and southern McArthur River Region. SHRIMP zircon ages from tuffs. Base is at the base of the Amos Formation, not above it (as in previous studies).|1616 +/- 5 Ma and 1611 +/- 4 Ma.|||Is overlain by Wide Supersequence.|Tuffaceous sandstones and carbonaceous shales.|
40579|Lawn Supersequence|66843|5|Briefly described|p36-39|||Said to be "informally" named, after the Lawn Hill Formation, because unit Pmh4 in the middle part of the Formation contains the MFS of this basin phase. Depositional cycles and lithofacies detailed.|~1615 - 1595 Ma.|||||
40579|Lawn Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40579|Lawn Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Camooweal - Murphy Domain, Mount Isa Inlier. Also recognised within the Nathan Group, NT. ||||Overlies Term Supersequence. Is overlain by Wide Supersequence.|Grey to black carbonaceous shale and siltstone, greenish grey tuff and tuffaceous siltstone, micaceous lithic sandstone and conglomeratic sandstone.|
40579|Lawn Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation.||||||
40579|Lawn Supersequence|69056|6|Mentioned|p56|||||||||
40579|Lawn Supersequence|69591|5|Briefly described|p27, p43, p47, p54|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the lower part of Lawn Hill Formation.||||Is equated with lower part of Doomadgee Formation.||
40579|Lawn Supersequence|70897|5|Briefly described|p39, Fig.1.7.1-3,7|Mesoproterozoic|Mesoproterozoic|Maintains relatively tabular architecture throughout deposition.||||Overlies Term Supersequence. Is overlain by Wide Supersequence.||
40579|Lawn Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic| Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation.|||||Grey to black carbonaceous shale and siltstone, greenish grey tuff and tuffaceous siltstone, micaceous lithic sandstone and conglomeratic sandstone.|
40579|Lawn Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||||
40579|Lawn Supersequence|72912|5|Briefly described|p33, p35 Fig.13, p45-46.|Paleoproterozic|Paleoproterozic|||||Overlies Term Supersequence and underlies Wide Supersequence.||
40579|Lawn Supersequence|73144|4|Described|p4-5, p8-9, p12, p20, p25, p40, p45, p49|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains four third order sequences [see article for more detail on third order sequences]. Deposited in inner-mid-outer shelf and possible submarine fan (Krassay et al., 2000). Drilling at Egilabria-4 has confirmed the presence of multiple thick and organic-rich shale gas intervals (Lawn Shale Gas Play). Potential source rock but maturity ranges are over 1.2% EqVR and 2% EqVR at Desert Creek 1 and Egilabria 1 wells respectively. Followed a significant erosional event. Third-order sequence Lawn 4 is considered one of [two] principal source rocks for the Isa Superbasin.|1600-1615 Ma|||Includes a portion of the Lawn Hill Formation.|Sandstone, siltstone, carbonaceous silty shale, silty shale and shale.|
25162|Leila Sandstone|22453|6|Mentioned|p 12|||||||||
25162|Leila Sandstone|22538|6|Mentioned|Fig3 P709|||||||||
25162|Leila Sandstone|22664|6|Mentioned|35|Paleoproterozoic|Paleoproterozoic|Of the Umbolooga Subgroup. Geological Province: McArthur Basin.||||||07-NOV-08
25162|Leila Sandstone|22670|6|Mentioned|55|||Geol.  province:  McArthur Basin.||||||13-OCT-06
25162|Leila Sandstone|22853|3|Fully described|19|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness 10 m. Overlain by Myrtle Shale; underlain by Tooganinie Formation.||||||03-JUN-09
25162|Leila Sandstone|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
25162|Leila Sandstone|23397|5|Briefly described|p473|||||||||
25162|Leila Sandstone|23398|6|Mentioned|p443|||||||||
25162|Leila Sandstone|23776|5|Briefly described|p705 Fig 2|||Of Umbolooga Subgroup.||||||
25162|Leila Sandstone|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Myrtle Shale. Overlies the Tooganinie Formation. Geological Province: McArthur Basin||||||
25162|Leila Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Umbolooga Subgroup.  Geological Province: McArthur Basin.||||||
25162|Leila Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Umbolooga Subgroup.||||||13-OCT-06
25162|Leila Sandstone|30272|6|Mentioned|p5|||On stratigraphic table||||||
25162|Leila Sandstone|35162|6|Mentioned|Table 1|||||||||
25162|Leila Sandstone|36796|6|Mentioned|Table 5|||||||||
25162|Leila Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25162|Leila Sandstone|40691|6|Mentioned|Fig.4|||||||||
25162|Leila Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25162|Leila Sandstone|41268|5|Briefly described|Fig.3|||||||||
25162|Leila Sandstone|42385|4|Described|p19|||See also Table 4 p17.||||||13-OCT-06
25162|Leila Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
25162|Leila Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Myrtle Shale; overlies Tooganinie Formation.|Dolomitic sandstone, sandy dolostone. Detailed lithology given.|09-NOV-11
25162|Leila Sandstone|42639|4|Described|p25, Table 5 p21|||||||||
25162|Leila Sandstone|42812|6|Mentioned|p36|||Of Tooganinie Formation?||||||13-OCT-06
25162|Leila Sandstone|42935|6|Mentioned|p529 Fig.2|||Of Umbolooga Subgroup.||||||13-OCT-06
25162|Leila Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of "Mid Proterozoic age.||||||13-OCT-06
25162|Leila Sandstone|43036|5|Briefly described|p48|||||||||
25162|Leila Sandstone|45162|2|Defined|p81|Proterozoic|Proterozoic|||||||
25162|Leila Sandstone|60483|5|Briefly described|p7 Fig. 5|||Of Umbolooga Subgroup (McArthur Group). Geological Province: McArthur Basin.||||||05-OCT-07
25162|Leila Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Myrtle Shale, underlian by Tooganinie Formation.||||||
25162|Leila Sandstone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1640 Ma.|Unit in River Supersequence.||||
25162|Leila Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p14 Tb.5|||||Of the Umbolooga Subgroup.||||
25162|Leila Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Umbolooga Subgroup.||Shown as partial lateral equivalent to Tooganinie Formation.||14-JUN-18
25162|Leila Sandstone|65228|5|Briefly described|p26, 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). Outcrops poorly. Gamma ray log, lithology and facies detailed. Measured section.||Unit in Umbolooga Subgroup.||Overlies Tooganinnie Formation. Is overlain by Myrtle Shale.||
25162|Leila Sandstone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive and ridge-forming.||Unit in Umbolooga Subgroup.||Overlies Tooganinie Formation. Is overlain by Myrtle Shale.|Dark grey-weathering dolomitic sandstone; fine- to coarse-grained, poorly-sorted, thinly to medium bedded, commonly cross-bedded and rippled; thin interbeds of sandy dolostone.|
25162|Leila Sandstone|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 30m thick.||Umbolooga Subgroup||Overlies (conformably) Tooganinie Formation. Overlain (conformably) by Myrtle Shale.|Dolomitic and quartz sandstone: fine- to coarse-grained, thinly to medium bedded; minor quartzic dolostone, dolomitic shale, breccia.|
25162|Leila Sandstone|69430|4|Described|p15:3, 17|Statherian|Statherian|Jackson et al. (1987); previously Leila Sandstone Member of Tooganinie Formation (Plumb and Brown, 1973). Southern McArthur Basin. <10-30m thick. Shallow-marine sediments.||Umbolooga Subgroup.||Conformably and gradationally overlies Tooganinie Formation. Is overlain conformably and gradationally by Myrtle Shale.|Dark grey-weathering, fine- to coarse-grained, poorly sorted, thinly to medium bedded dolomitic sandstone, commonly cross-bedded and rippled; thin interbeds of sandy dolostone.|12-JUL-16
25162|Leila Sandstone|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Tooganinie Formation||Overlain by Myrtle Shale||
25162|Leila Sandstone|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
25162|Leila Sandstone|72373|4|Described|iii,p1,10-14|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. Previous age constranits 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 2709631 (BD16TJM090: Fine-grained dolomitic quartz sandstone; BAUHINIA DOWNS) yielded interpreted max depositional age of 1756+\-32 Ma. Similar detrital zircon spectra with Tooganinie Fomation, suggesting derivation from similar source areas and potentially in part laterally equivalent.|1756+\-32 Ma (max dep age)|Unit of Umbolooga Subgroup.||Overlain conformably by Myrtle Shale. Underlain conformably by Tooganinie Formation.|Relatively thin succession of mostly crossbedded quartz and dolomitic sandstone, with lesser thin interbeds of dolomitic shale, dolarenite, dolomudstone, stromatolitic dolostone and intraclast breccia.|25-SEP-19
25162|Leila Sandstone|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 Tatoola Sandstone and underlies Myrtle Shale.||
25162|Leila Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south).||Umbolooga Sub-group, McArthur Group||Underlain by and equivalent to Tooganinie Formation. Overlain by Myrtle Shale.||
25162|Leila Sandstone|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 Tatoola Sandstone and underlies Myrtle Shale and is partly equivalent to Tooganinie Formation.||
25162|Leila Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Underlain by Tatoola Sandstone. Overlain by Myrtle Shale. May be equivalent to Tooganinie Formation.||
25162|Leila Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Tooganinie Formation. Is overlain by Myrtle Shale.||
42373|Leisler Metamorphics|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Yaya Metamorphic Complex.  Cordierite-sillimanite-biotite pelitic migmatite; minor metapsammite, foliated quartz diorite and cordierite-biotite S-type granite; granitic to sublinear texture. In the Arunta region.||||||07-NOV-08
42373|Leisler Metamorphics|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Yaya Metamorphic Complex. Cordierite-sillimanite-biotite pelitic migmatite; minor metapsammite, foliated quartz diorite and cordierite-biotite S type granite. Geological Province: Warumpi Province.||||||07-NOV-08
42373|Leisler Metamorphics|62378|5|Briefly described|p5, 31|||Geological Province: Arunta Region. Cordierite migmatite.||||||
42373|Leisler Metamorphics|64677|5|Briefly described|v, p1, p31-33, p60-61|||Arunta Region, Warumpi Province. Isolated outcrops; age unclear. Interpreted to have been metamorphosed during the c.1640 Ma Liebig Orogeny. Complex zircon population(s) discussed.|1704 +/- 3 Ma (protolith maximum deposition age).|Yaya Metamorphic Complex.|||Includes migmatitic metapelite interlayered with lesser (non-migmatitic) metapsammite.|
42373|Leisler Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||psammite, migmatite|
42373|Leisler Metamorphics|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.|||||Cordierite-sillimanite-biotite pelitic migmatite; minor metapsammite, foliated quartz diorite and cordierite-biotite S-type granite.|09-SEP-19
24357|Lennee Creek Formation|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
24357|Lennee Creek Formation|23809|5|Briefly described|p27, Fig. 25|||Of the Hanlon Subgroup.  Geological Province: Davenport Province.||||||
24357|Lennee Creek Formation|23823|5|Briefly described|p75|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group (upper). Interbedded feldspathic sandstone, siltstone and shale. Max. thickness:~1800m.  Geological Province: Davenport Geosyncline.||||||07-FEB-11
24357|Lennee Creek Formation|24172|5|Briefly described|p65 Tb.9|||Of the Hanlon Subgroup (Hatches Creek Group).||||||13-OCT-06
24357|Lennee Creek Formation|39624|5|Briefly described|Table 1|||||||||
24357|Lennee Creek Formation|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24357|Lennee Creek Formation|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Siltstone, shale, feldspathic arenite and subordinate calcareous beds; minor arenite.||||||10-JAN-05
24357|Lennee Creek Formation|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24357|Lennee Creek Formation|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24357|Lennee Creek Formation|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Arenite; siltstone and shale; minor quartz arenite and calcareous beds. Geological Province: Tennant Creek Block.||||||07-NOV-08
24357|Lennee Creek Formation|41129|4|Described|Table 1|||||||||
24357|Lennee Creek Formation|41204|4|Described|Table 1|||||||||
24357|Lennee Creek Formation|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hanlon Subgroup. Shale, siltstone, minor lithic/feldspathic arenite.||||||09-APR-06
24357|Lennee Creek Formation|41308|5|Briefly described|Table 2|||||||||
24357|Lennee Creek Formation|41310|4|Described|Table 1|||See also p12.||||||13-OCT-06
24357|Lennee Creek Formation|41408|6|Mentioned|Map legend|Proterozoic||||||||
24357|Lennee Creek Formation|41524|4|Described|Table 1|||||||||
24357|Lennee Creek Formation|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group).  Shale; siltstone; lithic or feldspathic arenite.||||||07-NOV-08
24357|Lennee Creek Formation|41970|6|Mentioned|Fig.3 P333|||||||||
24357|Lennee Creek Formation|42643|5|Briefly described|p12|||Of Hanlon Subgroup.||||||13-OCT-06
24357|Lennee Creek Formation|43802|6|Mentioned|p80|||||||||
24357|Lennee Creek Formation|45167|3|Fully described|Table 1|||Of Hanlon Subgroup.||||||13-OCT-06
24357|Lennee Creek Formation|49033|2|Defined|p27|Proterozoic|Proterozoic|||||||
24357|Lennee Creek Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Shale, siltstone, lithic/feldspathic arenite, minor mudstone and quartz arenite. Overlies Alinjabon Sandstone; underlies Canulgerra Sandstone. In the Tennant Creek region.||||||07-NOV-08
24357|Lennee Creek Formation|61567|5|Briefly described|p632|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgr(Hatches Creek Gr.) Contains some red shale in uppermost parts. Geological Province: Tennant Creek Inlier.  See also p633 Tb. 1.||||||07-NOV-08
24357|Lennee Creek Formation|64735|4|Described|p205 Fig 1, p206 Fig 2, p212 Tb1, p214-5|Orosirian|Orosirian|Age from youngest detrital zircons from a basal silicified quartz sandstone sample.|Max depositional age 1826+/-36 Ma.|Of Hanlon Subgroup, Hatches Creek Group.||Overlain by a continuation of clastic sedimentation in the Canulgerra Sandstone, Vaddingella Formation and Yaddanilla Sandstone.||20-APR-12
24357|Lennee Creek Formation|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||||
24357|Lennee Creek Formation|65338|6|Mentioned|p20.|||||Unit in Hanlon Subgroup.||||
24357|Lennee Creek Formation|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup, Hatches Creek Group.||Overlies Alinjabon Sandstone. Is overlain by Canulgerra Sandstone.|Arenite; siltstone and shale; minor quartz arenite and calcareous beds.|19-OCT-11
24357|Lennee Creek Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Alinjabon Sandstone. Is overlain by Canulgerra Sandstone.|Shale, siltstone, lithic/feldspathic arenite; minor mudstone and quartz arenite.|
24357|Lennee Creek Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24357|Lennee Creek Formation|67352|4|Described|p9 fig 1, p44 fig 45|Statherian|Statherian|1500 m thick. Recessive. High magnetic in part.||Hanlon Subgroup||Overlies (conformably) Alinjabon Sandstone. Overlain (conformably) by Canulgerra Sandstone.|Feldspathic, lithic, kaolinitic and sericitic arenite; siltstone, shale; minor quartz arenite; local calcareous beds; all thinly bedded.|
24357|Lennee Creek Formation|68518|3|Fully described|p6 Tb.1, p13|Proterozoic|Proterozoic|Max. thickness: 1500 m. Deposited in deeper water than most other Hatches Creek Group sediments. Type section: south of Elkedra Pound, extending from GR NS070532 (base) to GR NS070548.||Hanlon Subgroup||Conformable on Alinjabon Sandstone; is overlain unconformably by Cambrian strata.|Recessive medium to fine-grained feldspathic/lithic/kaolinitic arenite, micaceous and non-micaceous siltstone, shale; minor low-ridge-forming quartz arenite, recessive calcareous? beds. Medium bedded to laminated. Magnesite and calcrete concretions.|30-MAY-16
24357|Lennee Creek Formation|69425|4|Described|p10:3, 10, 12, 19-20, 23|Statherian|Statherian|700-1500m thick. Subtidal deposits. Underwent disharmonic folding by the Davenport Event. Possibly correlated with part of Deagan Member (Short Range Sandstone). Maximum deposition age.|1854 +/- 6 Ma (Claoue-Long et al., 2008).|Hanlon Subgroup.||Conformably overlies (and probably partly interfingers with) Alinjabon Sandstone. Is overlain conformably by Canulgerra Sandstone. Correlated with Mitty Member (Morphett Creek Formation).|Shale, siltstone, lithic/feldspathic sandstone; minor quartz sandstone, mudstone and claystone. Fine-grained rock types are variably micaceous; calcareous beds and chert concretions locally. Probably gypsiferous locally.|12-JUL-16
24357|Lennee Creek Formation|69431|6|Mentioned|p16:5, 22|||Davenport Province. Folding during the Davenport Event is discussed.||Hanlon Subgroup.||||12-JUL-16
79065|Leprechaun Gneiss|69917|5|Briefly described|p193-196, 175, 1|Ordovician|Neoproterozoic|Eastern Arunta Region, Irindina Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. U-Pb isotopic data indicate a maximum depositional age of 544+/-11 Ma for the sedimentary protolith of the Leprechaun Gneiss. Maximum age of metamorphic zircon: 488+/-9 Ma.||||Interlayered with Yambla Gneiss. May represent first-cycle sediments shed from the Riddock Amphibolite|Strongly layered quartz-hornblende gneiss.|
79065|Leprechaun Gneiss|70839|6|Mentioned|p344|||Geological province: Irindina Province. Contains detrital zircon age spectra that resemble Amadeus Basin Supersequence 4 (c. 1.22-1.01 Ga).||||||20-APR-22
79065|Leprechaun Gneiss|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen.|488+/-9 Ma (metamorphism: U-Pb zircon LA-ICPMS).||||Gneiss.|
79065|Leprechaun Gneiss|72516|6|Mentioned|p79|Cambrian|Neoproterozoic|New units incorporated into the Harts Range Metamorphic Complex by Whelan et al (in prep). Irindina Province.||Harts Range Metamorphic Complex||||20-APR-22
23724|Lewin Springs Syenite|23714|4|Described|p36|Proterozoic|Proterozoic|||||||
23724|Lewin Springs Syenite|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions||||||
23724|Lewin Springs Syenite|24181|5|Briefly described|p87 Fig.2|Paleoproterozoic|Paleoproterozoic|Intrusive. Geological Province: Pine Creek Inlier.||||||07-NOV-08
23724|Lewin Springs Syenite|24340|6|Mentioned|p147 Fig. 3|||Geological Province: Pine Creek Inlier.||||||
23724|Lewin Springs Syenite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Edith River Group. Porphyritic microgranite, rhyolite, porphyritic quartz microsyenite and quartz micromonzonite.||||||07-NOV-08
23724|Lewin Springs Syenite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23724|Lewin Springs Syenite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23724|Lewin Springs Syenite|41311|4|Described|p21|||||||||
23724|Lewin Springs Syenite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23724|Lewin Springs Syenite|42756|5|Briefly described|p7|||||||||
23724|Lewin Springs Syenite|43140|6|Mentioned|p22 & 37.|||||||||
23724|Lewin Springs Syenite|43187|5|Briefly described|p2|||||||||
23724|Lewin Springs Syenite|43624|6|Mentioned|Fig.15,p20|||||||||
23724|Lewin Springs Syenite|43832|4|Described|66, Table13 p67|||Age post-Palaeoproterozoic.  Occurs as dykes.||||||
23724|Lewin Springs Syenite|50586|6|Mentioned|p6.4|||||||||
23724|Lewin Springs Syenite|67564|4|Described|p6 Table 2, p34, pp37-38.|Paleoproterozoic|Paleoproterozoic|Numerous dykes up to 100 m wide and 2000 m in length, trending NW.|c.1825 Ma.|||Intrudes McCarthys and Allamber Springs Granites, Fingerpost Granodiorite and Plum Tree Creek Volcanics.|Porphyritic quartz syenite, quartz microsyenite, syenite and microgranitoid; porphyritic, with embayed quartz, rounded feldspar phenocrysts to 10 mm, and minor aggregates of secondary chlorite and carbonate.|
23724|Lewin Springs Syenite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||||Is overlain nonconformably by Geolsec Formation.|Porphyritic quartz syenite, quartz microsyenite, syenite, microgranite, microleucogranite, quartz micromonzonite, microleucomonzonite.|
79225|Liddle Formation|72369|4|Described|iii,p3-4,15,18-20|||Of Amadeus Basin. Defined by Donnellan and Normington 2017. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND415 (coarse-grained to granular quartz arenite) yielded an interpreted maximum depositional age of 886+\-11 Ma (youngest concordant zircon), but pre-dates the c. 580-530 Ma Petermann Orogeny that may have resulted in Winnall Group deposition. Contains detrital zircons derived from Aleiron and Warumpi provinces (c. 1770 to c. 1490 Ma age spectrum), and Musgrave Province (c. 1435 Ma to c. 1060 Ma age spectrum). Significant proportion of total Liddle Formation zircon age spectra is > 1800 Ma, and is interpreted to have been sourced from metasedimentary rocks in the Aileron Province (1860-1830 Ma) or elsewhere in east Gondwana. Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Winnall Group.||Overlain unconformably by Puna Kura Kura Formation. Underlain by Froud Formation.|Fine-grained, very thinly to thinly bedded and laminated sandstone.|18-DEC-19
79225|Liddle Formation|73119|5|Briefly described|piii, p1, p5-11, p13, Appendix|late Ediacaran|late Ediacaran|Amadeus Basin, western. Exposed in generally northwest-striking ridges. Contains informal sub-members. New SHRIMP U-Pb detrital zircon maximum depositional ages include 1158 +/- 4 Ma (which is significantly older than expected), 662 +/- 9 Ma, and 669 +/- 7 Ma. The latter two ages are close to the previous age of 696 +/- 13 Ma (Beyer et al., 2020). Dominant detrital zircon age components are Mesoproterozoic, with a major peak between ca 1170 - 1120 Ma and other minor peaks. These ages suggest the Musgrave Province was a major source of detritus, with minor contributions from the older Aileron and Warumpi provinces or similar. Provenance of ca 1000-662 Ma zircons is not clear as there are no obvious Australian sources. [See article for provenance discussion].|662 +/- 9 Ma, 669 +/- 7 Ma SHRIMP U-Pb|Winnall Group||Overlain by Puna Kura Kura Formation.|Includes thick-bedded medium-grained sandstone, well-sorted medium-grained sandstone, and festoon cross-stratified sandstone.|
29411|Ligertwood beds|42940|5|Briefly described|Plate 2|Carboniferous|Carboniferous|Breccia, conglomerate, conglomeratic sandstone, sandstone.  Age: 360-290Ma. Geological province: Amadeus Basin.||||||23-JAN-08
29411|Ligertwood beds|61387|5|Briefly described|Map legend|Permian|Carboniferous|Breccia, sandstone, conglomerate, conglomeratic sandstone.||||||
29411|Ligertwood beds|61519|5|Briefly described|Map Legend|Permian|Carboniferous|Breccia, sandstone, conglomerate, conglomeratic sandstone.||||||
29411|Ligertwood beds|64778|6|Mentioned|p13|||Amadeus Basin.||||||
29411|Ligertwood beds|67856|4|Described|p347 tab 4-9, p337, p346, 348|Permian|Permian|Of Wells et al., 1964, 1970. Type section: Ligertwood Cliffs. About 25m thick. Correlated with Paterson Formation. Fluvio-glacial sequence. No age determination. Age assumed from correlation.||||Correlated with Crown Point Formation, Paterson Formation and in part with Grant Group.|Bedded dolomite/limestone conglomerate with secondary matrix of travertine followed by conglomerate and sandstone.|
29411|Ligertwood beds|69438|3|Fully described|p23:4, 42|Permian|Carboniferous|Wells et al. (1965); named after Ligertwood Cliffs, far NW Amadeus Basin, which form the type area. Exposed over a strike length of c.115km. Not folded; deposition post-dated the 450-300 Ma Alice Springs Orogeny.||||Corrlated (tentatively) with the Buck Formation in WA.|A lower interval of interbedded sandstone, calcareous sandstone and calcareous pebble and cobble conglomerate; disconformably overlain by an upper unit of interbedded silicified sandstone, conglomeratic sandstone, and pebble conglomerate.|12-JUL-16
29411|Ligertwood beds|70839|6|Mentioned|p330|Late Paleozoic|Late Paleozoic|||||||
29411|Ligertwood beds|71088|5|Briefly described|p12, p17, p33|Paleozoic|Paleozoic|Amadeus Basin. Units previously mapped as this formation have been reassigned to the new Mu Formation. The type area was on Mount Rennie in the NT.||||||
29411|Ligertwood beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sedimentary breccia, conglomerate, sandstone|
29411|Ligertwood beds|72360|5|Briefly described|Map legend|Permian|Carboniferous|Of Canning Basin.|||||Breccia, sandstone, conglomerate, conglomeratic sandstone.|09-SEP-19
75948|Lilyarba Mafics|67232|2|Defined|iv, pp8-9, pp21-23, p29, pp34-35.|Paleoproterozoic|Paleoproterozoic|Named after Lilyarba Waterhole. Litchfield Province, Pine Creek Orogen. Previously part of Wangi Basics, now abandoned. Type locality is a large exposure in FERGUSSON RIVER and WINGATE MOUNTAINS, 60 km south of Daly River township. Fine-grained, altered low-grade metamorphic rocks with distinctive strong alkaline geochemical signatures and low Si, high Al; c.30 My younger than other former Wangi Basics constituents. Crops out as boulder-strewn hummocky rises. Geochemistry is described in detail. Has lamprophyric/shoshonitic affinities indicative of post-collisional tectonics.|1829 +/- 4 Ma (Worden et al. 2008a).|||Intrudes Burrell Creek Formation. Is intruded by Soldiers Creek Granite.|Possible altered lamprophyre; mineralogy dominated by sericitised plagioclase and hornblende, and minor biotite and opaque minerals.|
75948|Lilyarba Mafics|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.|1829 +/- 4 Ma (Worden et al. 2008b).|||||
75948|Lilyarba Mafics|69420|5|Briefly described|p5:4, 29|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. E of the Giants Reef Fault. Part of the obsolete Wangi Basics. Shows geochemical affinities with island-arc magmatism. SHRIMP zircon extrusion age; attributed also to Worden et al. (2008).|1829 +/- 4 Ma (Jagodzinski, 1998).||||Probably of shoshonitic/lamprophyric affinity.|12-JUL-16
26689|Limbla Member|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Pertatataka Formation.  Cross-laminated sandstone, sandy calcarenite.  Geological Province: Amadeus Basin.||||||
26689|Limbla Member|22506|6|Mentioned|p130 Fig.4|Cryogenian|Cryogenian|||||||
26689|Limbla Member|22566|6|Mentioned|p81|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||30-OCT-06
26689|Limbla Member|22649|6|Mentioned|p 153|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||30-OCT-06
26689|Limbla Member|22762|6|Mentioned|p374|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||30-OCT-06
26689|Limbla Member|22826|5|Briefly described|p569|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.||||||30-OCT-06
26689|Limbla Member|23250|5|Briefly described|p1124 Fig.2||Cryogenian|Of Aralka Formation. Correlate of Angepena Formation equivalent and Etina Formation.||||||30-OCT-06
26689|Limbla Member|30258|6|Mentioned|Fig.2|||Proterozoic age. Member of Pertatataka Formation.||||||
26689|Limbla Member|32720|6|Mentioned|Table 1|||Pertatataka Fm.||||||
26689|Limbla Member|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
26689|Limbla Member|34111|5|Briefly described|Table 1|||Precambrian. See also Table 4||||||
26689|Limbla Member|34488|5|Briefly described|Table 1|||Proterozoic||||||
26689|Limbla Member|34579|4|Described|Table 1|||||||||
26689|Limbla Member|35102|6|Mentioned|p19|||||||||
26689|Limbla Member|35805|6|Mentioned|Fig.3|||||||||
26689|Limbla Member|37928|6|Mentioned|p517|||||||||
26689|Limbla Member|38157|6|Mentioned|p272|||See also Table VI.||||||
26689|Limbla Member|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26689|Limbla Member|39210|6|Mentioned|p37|||||||||
26689|Limbla Member|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26689|Limbla Member|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Aralka Formation. Fine cross laminated sandstone, some with festoon cross bedding. Geological Province: Amadeus Basin.||||||14-FEB-06
26689|Limbla Member|40740|5|Briefly described|p12|||||||||
26689|Limbla Member|40906|6|Mentioned|Fig.9|||||||||
26689|Limbla Member|41190|6|Mentioned|Fig.4|||||||||
26689|Limbla Member|41270|6|Mentioned|Table 1|||||||||
26689|Limbla Member|41717|6|Mentioned|Fig.2|||||||||
26689|Limbla Member|42082|6|Mentioned|Fig.3 P323|||||||||
26689|Limbla Member|42504|5|Briefly described|Table 4 P73|||||||||
26689|Limbla Member|42886|5|Briefly described|Fig.2 P219|||||||||
26689|Limbla Member|42940|5|Briefly described|Plate 9|||||||||
26689|Limbla Member|44335|4|Described|p.7||Proterozoic|Table 1. p.8.||||||
26689|Limbla Member|44336|14|Not recorded|map legend||Proterozoic|SG/53-3, mb of Pertatataka Formation.||||||
26689|Limbla Member|44433|14|Not recorded|map legend||Proterozoic|||||||
26689|Limbla Member|45041|4|Described|p37|||Proterozoic||||||
26689|Limbla Member|46865|6|Mentioned|p44|||||||||
26689|Limbla Member|48890|2|Defined|p.27||Neoproterozoic|See also Tables, Figs & Plates. pt. Pertatataka Fm. U.Proterzoic.||||||
26689|Limbla Member|48963|6|Mentioned|Fig.2|||||||||
26689|Limbla Member|49796|5|Briefly described|Sect C BDF 60|||Of Aralka Formation.||||||30-OCT-06
26689|Limbla Member|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Pertatataka Formation. Geological Province: Amadeus Basin. Cross-laminated sandstone, sandy calcarenite.||||||
26689|Limbla Member|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Aralka Formation.  Fine cross-laminated sandstone.||||||
26689|Limbla Member|61732|5|Briefly described|p94|||Formerly part of the Pertatataka Formationnow redefined within the Aralka Formation.||||||07-FEB-11
26689|Limbla Member|62595|6|Mentioned|p28 Fig.4.|Middle Neoproterozoic|Middle Neoproterozoic|Amadeus Basin. Relative probability plots of detrital zircon data are shown.||||||
26689|Limbla Member|63562|4|Described|p342-343, p351, p352 fig 10|||Of Amadeus Basin. A distinctive unit within the parent Formation's tillites. Tidal deposition. Zircons of mixed ages (2.5-1.08 Ga) derived probably from Arunta (ice flows) and Musgrave (progradation) Inliers.||Aralka Formation|||Fine-grained feldspathic sandstone with small-scale planar cross beds and herringbone crossbeds.|
26689|Limbla Member|69438|5|Briefly described|p23:16|Cryogenian|Cryogenian|Amadeus Basin. Dating of detrital zircons indicates likely Musgrave Province provenance.||Aralka Formation.|||A dominantly clastic unit characterised by pebbly and sandy limestone, and festoon-bedded sandstone.|12-JUL-16
26689|Limbla Member|69606|6|Mentioned|p12|||Eastern Amadeus Basin.||||||
26689|Limbla Member|69673|5|Briefly described|p74|||||Aralka Formation|||Pebbly and sandy limestone, festoon bedded sandstone.|
26689|Limbla Member|69937|5|Briefly described|v Fig.1, vi, p3 Tb.1, p14-16|Neoproterozoic|Neoproterozoic|Amadeus Basin. See also p43-p44. The Cryogenian depositional age is inferred from the underlying Areyonga Formation. The youngest detrital zircons (shown as maximum depositional age) are likely from the Musgrave Province.|1018 +/- 23  Ma (maximum depositional age).|Aralka Formation.|||Dominantly clastic unit characterised by pebbly and sandy limestone and festoon-bedded sandstone.|29-AUG-18
26689|Limbla Member|70018|6|Mentioned|p240|||Amadeus Basin. ||||||
26689|Limbla Member|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.||||||
26689|Limbla Member|70416|5|Briefly described|p64|Cryogenian|Cryogenian|Locally recognized.||Aralka Formation.|||Sandstone and pebbly calcarenite.|
26689|Limbla Member|71001|6|Mentioned|p18 Fig.2|Cryogenian|Cryogenian|Amadeus Basin. Marine deposits.||Aralka Formation.||||
26689|Limbla Member|71344|6|Mentioned|p1093 Fig 1|Cryogenian|Cryogenian|||Of Aralka Formation.||||
26689|Limbla Member|71801|6|Mentioned|p230|Cryogenian|Cryogenian|Amadeus Basin.||Aralka Formation||Overlies the Ringwood Member. Overlain by the Olympic Formation.||
26689|Limbla Member|71841|5|Briefly described|p1-2|Cryogenian|Cryogenian|Of Amadeus Basin.||Unit of Aralka Formation.||||
26689|Limbla Member|71842|5|Briefly described|p2-3|Cryogenian|Cryogenian|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).||Unit of Aralka Formation.||Unit within upper part of Aralka Formation.||
26689|Limbla Member|72369|4|Described|iii,p3-4,7,9-11|||Of Amadeus Basin. Kositcin et al (2015) reported interpreted maximum depositional age of 1018+\-23 Ma, which is vastly older than 600 Ma sedimentation age of Preiss (1978) and Re-Os ages of 658+\-5 Ma (Kendall and Creaser 2004) and 657.2+\-5.4 Ma (Kendall et al 2006). LA-ICP-MS U-Pb detrital zircon dating of sample RD15VJN206 (fine- to medium-grained quartz arenite) yielded an interpreted maximum depositional age of 931+\-7 Ma (youngest concordant zircon) but does not further constrain the timing of deposition of the unit. Contains significant proportion of detrital zircons derived from Musgrave Province (c. 1450 to c. 1100 Ma spectrum), and Aleiron and Warumpi provinces (c. 1810 to c. 1625 Ma age spectrum). Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Aralka Formation.||Overlies the Ringwood Member.|Pebbly and sandy limestone, and festoon-bedded sandstone in the upper part.|18-DEC-19
26689|Limbla Member|72375|4|Described|p1-2,19-20|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. SHIRMP U-Pb zircon analysis by Kositcin et al., 2015 yielded an interpreted max depositional age (weighted mean 238U/206Pb) of 1018+\-23 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS AS13CJE011 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p19-20 for Hf isotopic results and interpretations).||Unit of Aralka Formation.||Underlain by Ringwood Member.|Pebbly and sandy limestone and festoon-bedded sandstone.|
26689|Limbla Member|72489|5|Briefly described|p3, p5 Fig.4, p6-7, p7 Fig.6, p10, 12|Cryogenian|Cryogenian|Amadeus Basin. Characterised by festoon crossbedding.||Aralka Formation||Overlies Ringwood Member.||
26689|Limbla Member|72601|5|Briefly described|p3-4, p7|Cryogenian|Cryogenian|Amadeus Basin. Defined by Wells et al. (1967).||Aralka Formation||Underlain and overlain by undifferentiated Aralka Formation siltstone.|Characterized by festoon cross-laminated sandstone in its upper portion and sandy calcarenite in the lower portion.|
26689|Limbla Member|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. Re definition of unit. Characterised by festoon cross-laminated and cross-bedded sandstone. Amadeus Basin. Type section: Hi Jinx Syncline. Key localities: Halfway Dam. Previously part of the Pertatataka Formation. No known fossils. Detrital zircon maximum depositional age of 1018 +/- 23 Ma interpreted to be much older than true depositional age. Substantially greater siliciclastic component than Ringwood Member. Similar 'tramline' topographic expression to that seen more generally in the Ringwood Member. [Also written as Limbla member and Limbla Formation]. p: 5-6, 61, 66, 71-74, 79, 81, 86, ~90-100, 122, 126, 143, 160, 163-166, App 2.|658 +/- 5 Ma, 657.2 +/- 5.4 Ma Re-Os|Aralka Formation||Bounded by parent unit (Aralka Formation). Partly overlain disconformably by Olympic Formation. Correlates to Rinkabeena Shale, Etina Formation, part of Yankaninna Formation, and lower Inindia beds.|Carbonate-cemented siliciclastic sandstone and [minor] intraformational clast-bearing granule and small-pebble conglomerate, carbonate cemented sandstone shale and minor limestone.|
26689|Limbla Member|73088|6|Mentioned|p1|Cryogenian|Cryogenian|Amadeus Basin, northeast.||Aralka Formation||||
26689|Limbla Member|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Aralka Formation||Conformably overlies the Ringwood Member, disconformably underlies the Olympic Formation and Pioneer Sandstone.||
26689|Limbla Member|73279|5|Briefly described|p3, p5|Cryogenian|Cryogenian|Amadeus Basin. From the uppermost part of the Aralka Formation. Detrital zircons analysed for Hf isotopic composition [see article].||Aralka Formation|||Includes sandstone.|
79064|Lionel Suite|69917|4|Described|p140-146, 149-151, 156-157|||?Previously included in Huckitta Suite? Of Ambulbinya Supersuite?, Eastern Arunta Region, Aileron Province. Dating attempted on 6 samples, some previously included in 'Entia Gneiss Complex'. U/Pb LA-ICPMS zircon dating, Hf analytical data. Ages difficult to interpret.  Tentatively interpret mafic igneous precursor emplaced at ca 1770 Ma and recrystallization, metamorphic zircon growth occurred during Strangways Event, ca 1704 Ma. Includes biotite granite (p141) previously considered to intrude Harts Range Metamorphic Complex. |1756+/-7Ma, 1771+/-10Ma cryst, 1723+/-20Ma meta|||Intrudes Harts Range Metamorphic Complex? Lenses of Entia Metamorphics present nearby.|1. Metagabbro. Amphibolite-facies metamorphism + hydrothermal alteration (chalcedony infilling cracks). 2. Foliated biotite granite. 3. Mafic amphibolite. 4. Hornblende-biotite granodiorite. 5. granitic gneiss.|
79064|Lionel Suite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1771+/-10 Ma (U-Pb zircon LA-ICPMS).||||Gneiss, metagabbro, granite, amphibolite, granodiorite.|
22206|Littlers Pegmatite|43225|5|Briefly described|Map Legend||Mesoproterozoic|Of Arunta Block.||||||30-OCT-06
22206|Littlers Pegmatite|43503|2|Defined|9,26,80|||||||||
31284|Liverpool Breccia|23374|2|Defined|p24,25,43,44|Cretaceous|Paleoproterozoic|Age uncertain, in the range Palaeoproterozoic to Cretaceous. Impact breccia of the Liverpool Crater.||||||07-NOV-08
31284|Liverpool Breccia|61560|5|Briefly described|p490|Cretaceous|Paleoproterozoic|Two distinct breccia units. Authigenic breccia, and allogenic breccia. Age is uncertain in Palaeoproterozoic rocks of Gumarrirnbang Sandstone but post-impact sediments are interpreted as Creatceous age.||||||07-NOV-08
41847|Lizard Schist|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Uwupataka Metamorphic Complex. Biotite-muscovite quartz schist, metapsammite, rare quartzite; variable tourmalinisation.  Age: between 1650-1610Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
41847|Lizard Schist|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Iwupataka Metamorphic Complex. Biotite-muscovite-quartz schist, metapsammite, rare quartzite, moderatly magnetic. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
41847|Lizard Schist|67565|2|Defined|p59, p7 Table 1, p13, p30, p34.|Statherian|Statherian|New name, after Lizard Bore. Haasts Bluff Domain, Warumpi Province. Type locality is a hill 8 km SSW of Mount Liebig Community. Previously of undifferentiated Arunta Complex (Ranford, 1969). Maximum deposition age from SHRIMP U-Pb detrital zircons. Correlated with Ikuntji Metamorphics. Metamorphosed to lower to middle amphibolite facies during the 1590-1560 Ma Chewings Orogeny.|1657 +/- 28 Ma (Cross et al. 2004).|Unit in Iwupataka Metamorphic Complex.||Is faulted against Peculiar Complex. Is overlain by Heavitree Quartzite.|Biotite-muscovite-quartz schist interlayered with quartz-muscovite metapsammite and narrow quartzite layers; varying degrees of tourmalinisation; rare quartzite and garnet-bearing schist.|01-DEC-15
41847|Lizard Schist|68832|4|Described|p39-44,6 |||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Grey crystalline quartzite layer sampled. Maximum deposition age|1657+/-28 Ma|?Iwupataka Metamorphic Complex.||Adjacent to (possibly intruded by) Talipata Granite. Unconformably overlain by Heavitree Quartzite. Strong lithological similarities with the Ikuntji Metamorphics.|Muscovite-biotite schist and metapsammite.|
41847|Lizard Schist|69428|5|Briefly described|p13:6-7|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Haasts Bluff Domain, Warumpi Province. Crops out SW of Mount Liebig. SHRIMP U-Pb detrital zircon maximum depositional age.|1657 +/- 28 Ma (Cross et al., 2005).|Iwupataka Metamorphic Complex.||Is overlain by Heavitree Quartzite. Correlated with Ikuntji Metamorphics.|Dominated by biotite-muscovite-quartz schist interlayered with muscovite-bearing quartz-rich psammitic rock layers.|12-JUL-16
41847|Lizard Schist|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1657+/-28 Ma (MDA: U-Pb zircon SHRIMP)||||Schist.|
77878|Lloyd Gabbronorite|69917|4|Described|p169-173, 1|Early Devonian|Early Devonian|Eastern Arunta Region, Irindina Province.  2 samples. U/Pb SHRIMP zircon 411+/-5.7 Ma emplacement, baddeleyite 391+/-31 Ma date, Hf analytical data.  U/Pb LA-ICPMS zircon dating was inconclusive. Youngest known mafic magmatism in Arunta Region.||||Intrudes Yambla Gneiss.|Olivine gabbronorite.|29-JUL-15
77878|Lloyd Gabbronorite|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen.|411+/-5.7 Ma crystallisation: U-Pb zircon LA-ICPMS||||Gabbronorite.|
75895|Log Cabin Granite|69917|4|Described|p187-190, 180|Cambrian|Cambrian|Of Harts Range Metamorphic Complex?, Eastern Arunta Region, Irindina Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. 2 samples. Age represents crystallisation. Second sample appears to contain only inherited zircons.|524+/-3 Ma.|||Age compared with Indiana Igneous Complex. Intrudes Yambla Gniess.|Garnet-biotite granite; Biotite gneiss. S-type granite.|
75895|Log Cabin Granite|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen.|||||Gneiss.|
40580|Loretta Supersequence|62535|5|Briefly described|p672|Statherian|Statherian|Isa Superbasin.|c.1645 Ma.|||||
40580|Loretta Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Tooganinie Formation, Tatoola Sandstone, Amelia Dolostone and upper parts of Mallapunyah Formation.|||
40580|Loretta Supersequence|63866|5|Briefly described|p53-p54, p56-p57, p59|||Isa Superbasin.|||Includes the Tatoolla Sandstone and Lady Loretta Formation.|Equivalent to the Walford Dolomite, Kennedy Siltstone and Magazine Shale. Conformably overlies the Gun Supersequence.||
40580|Loretta Supersequence|65228|4|Described|pp26-29, Figs.11-21.|Statherian|Statherian|At Mount Isa, interpreted as comprising Kennedy Siltstone, Magazine Shale, Leila Sandstone, Myrtle Shale, Emmerugga Dolomite. A karst surface marks the top of this unit. Gamma ray log, lithology and facies detailed.|c.1650 Ma.|||Equates with Walford Dolomite and Lady Loretta Formation.|Mixed succession of carbonates and siliciclastics. Basal conglomerate, interbedded sandstone and siltstone with evaporites, oolitic and stromatolitic carbonates with thin green shales.|
40580|Loretta Supersequence|65337|6|Mentioned|p33 Fig.27.|||||||Overlies Gun Supersequence. Is overlain by River Supersequence.||
40580|Loretta Supersequence|66844|5|Briefly described|p244-246,269|Mesoproterozoic|Paleoproterozoic|Lawn Hill and Gunpowder region. See also reference to Loretta 1.1, p255 fig 7.||Of McNamara Group.|Includes Lady Loretta Formation.|Underlain unconformably by Gun Supersequence.|non-marine and marine siliciclastics.|
40580|Loretta Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.|~1650-1645 Ma.|||Overlies Gun Supersequence. Is overlain by River Supersequence.|Thin-bedded, intraclastic and stromatolitic dolomite, interbeds of dolomitic siltstone and fine-grained sandstone|
40580|Loretta Supersequence|68732|5|Briefly described|p159, p162, p165 Fig.3|||Contains domal, columnar and digitate stromatolites which combine to form bioherms and biostromes. Includes Lady Loretta and Magazine/Kennedy Siltstones.||||||01-DEC-17
40580|Loretta Supersequence|69591|5|Briefly described|p27, p42-43, p46, p54, p108|||Mount Isa Province, Isa Superbasin. Shallow-water carbonate platform deposits. Includes the Lady Loretta Formation.||||Unconformably overlies Gun Supersequence. Is overlain by River Supersequence.||
40580|Loretta Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill.|ca. 1650 Ma|||Overlies the Gun Supersequence.|Siltstone, carbonaceous shale and dolomite.|
40580|Loretta Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Paleoproterozic|Paleoproterozic|Kerogens within this unit contain the potential to generate gas and condensate over a large area.||||||
40580|Loretta Supersequence|73144|4|Described|p8-9, p11, p19-20|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains two third order sequences [see article for more detail on third order sequences]. Deposited in shallow marine ram setting with subtidal tempestite cycles (Southgate et al., 2000). Thick carbonate succession. Basal breccia unit sourced from underlying Gun Supersequence. Contains dates of ca 1655 Ma [near the base?] and 1647 +/- 4 Ma [near the top?]. Potential hydrocarbon reservoirs; no potential unconventional hydrocarbon source rocks identified within this supersequence (Gorton and Troup, 2018).|1645-1655 Ma|||Includes Lady Loretta Formation.|Dolomudstone. Includes basal breccia unit.|
22219|Lovely Hill Schist|7837|6|Mentioned|p94|||||||||
22219|Lovely Hill Schist|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Iwupataka Metamorphic Complex.||||||07-NOV-08
22219|Lovely Hill Schist|43503|2|Defined|8,23,78|||||||||
22219|Lovely Hill Schist|64809|6|Mentioned|p11 Fig.10 |Mesoproterozoic|Palaeoproterozoic|||||||
22219|Lovely Hill Schist|69428|5|Briefly described|p13:6-7|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995). Eastern Haasts Bluff Domain, Warumpi Province. Crops out N of the Chewings Range.||Iwupataka Metamorphic Complex.||Intruded by Ellery Granitic Complex.|A succession of metapelitic rocks (locally garnet and sillimanite-bearing), fine-grained quartzofeldspathic rocks and minor quartzite, metaconglomerate and calc-silicate rock. Metamorphosed to upper amphibolite facies.|12-JUL-16
79260|Loves Creek Formation|71001|5|Briefly described|p16, 18-24, 26-28|Tonian|Tonian|Amadeus Basin. Formerly Loves Creek Member (of Bitter Springs Formation). Basin-wide deposition during a 20 m.y. transgressive phase. Hosts a pre-Sturtian glaciation (811-788 Ma), negative carbon isotope excursion. Carbon isotope correlation graph. Forms topographic highs.||Bitter Springs Group.||Overlies Gillen Formation. Is overlain by Johnnys Creek Formation.|Laterally continuous interval of stromatolitic, cyclic dolostone (2-12m thicknesses). Domal, columnar, tabulate and stratiform forms.|
79260|Loves Creek Formation|71080|5|Briefly described|p23, p29 Fig 20, p30|Tonian|Tonian|Amadeus Basin. Supersequence 1. Inferred to be older than c. 827 Ma, by biostratigraphic correlation with SA unit overlain by 827 Ma volcanics.||Of Bitter Springs Group.|||Dominantly carbonate.|
79260|Loves Creek Formation|71279|5|Briefly described|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||Bitter Springs Group.||||
79260|Loves Creek Formation|71344|4|Described|p1094, 1093, 1096-1103|Tonian|Tonian|Amadeus Basin. The Acaciella australica stromatolite assemblage is regarded as a robust stratigraphic marker and transitions from domal, through columnar, to stratiform stromatolites. An open shallow marine depositional environment, shallowing upward, is likely.|~850-750 Ma||||Grey to yellow, dolomitic limestone containing stromatolites and chert nodules.|
79260|Loves Creek Formation|71841|5|Briefly described|p1,8|Cryogenian|Cryogenian|Of Amadeus Basin. Previously termed Loves Creek Member. Status upgraded to Formation and formalised by Normington et al (2015), Normington and Donnellan (in review). ||Unit of Bitter Springs Group.||Overlain by Johnnys Creek Formation. Underlain by Gillen Formation. Grades into Pinyanna beds.||
79260|Loves Creek Formation|71842|5|Briefly described|iii,p2-3,5,9|Cryogenian|Cryogenian|Of Amadeus Basin. Deposited in a series of upward-shallowing cycles (Southgate 1991). Part of revised nomenclature after this study in the Mount Conner area. Low rises on the peripheries of the Mount Conner area are recognised as belonging to this formation.||Unit of Bitter Springs Group.||||08-JAN-20
79260|Loves Creek Formation|71898|5|Briefly described|p9|||Amadeus Basin.||Bitter Springs Group||Unconformably overlain by the Tempe Formation.||
79260|Loves Creek Formation|72369|5|Briefly described|p43,45|||Of Amadeus Basin.||Unit of Bitter Springs Group.||Overlain by Johnnys Creek Formation. Underlain by Gillen Formation.||
79260|Loves Creek Formation|72375|4|Described|p10,13|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||Unit of Bitter Springs Group.||Overlain by Johnnys Creek Formation. Underlain by Gillen Formation.||
79260|Loves Creek Formation|72489|5|Briefly described|p3, p6, p7 Fig.6, p9|Tonian|Tonian|Formation greater than 190m thick in places. Significant 13C excursion preserved.||Bitter Springs Group||Overlies Gillen Formation. ?overlain by Johnnys Creek Formation.|Includes carbonate and siliciclastic succession.|
79260|Loves Creek Formation|72601|5|Briefly described|p3, p7, p10-11, p14, p25|Tonian|Tonian|Amadeus Basin. Previously the Loves Creek Member. Contains diverse Tonian biotic assemblages.||Bitter Springs Group||Underlain by Gillen Formation. Overlain by Johnnys Creek Formation.|[Includes] stromatolitic carbonate.|
79260|Loves Creek Formation|73085|4|Described|piii, p1-3, p5, p15-16, p23, p25-27|Tonian|Tonian|Amadeus Basin. Previously called Loves Creek Member. Contains diagnostic stromatolite taxa (Acaciella australica Assemblage). 156.1 m thick in drillhole BR05DD01. Carbonate minerals are comprised almost exclusively of dolomite and calcite, with minor ankerite.||Bitter Springs Group||Overlain by Johnnys Creek Formation. Underlain by Gillen Formation. Equivalent to Pinyinna beds.|Grey to buff dolostone with intervals of dark grey to brown dolostone; variably stromatolitic.|
79260|Loves Creek Formation|73086|1|Redefined|[See comments].|Tonian|Tonian|[Redefined herein. See also definition card, ASUD]. Re definition of unit/upgrade from member to Formation based on distinct lithostratigraphic character, great thickness and wide distribution. Characterised by a diverse stromatolite assemblage (Acaciella australica Assemblage). Authors suggest two member subdivisions but do not propose names. Amadeus Basin. Part of Supersequence I; deposited during the early sag phase of basin development. Geochron constraint based on globally recognized negative delta13C isotopic excursion. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. p: iii, 5-7, 14-15, 18, 25, ~27-39, ~49-55, 62, 66, 103, 105, 118, 143, 147, 151-155, 158, App 2.|815-787 Ma|Bitter Springs Formation||Underlain by Gillen Formation. Overlain by Johnnys Creek Formation. Unconformably overlain by Gaylad Sandstone.|Stromatolitic dolostone with interbeds of chert, non-stromatolitic dolostone and minor limestone.|
79260|Loves Creek Formation|73088|6|Mentioned|p1|Tonian|Tonian|Amadeus Basin, northeast. Previously called Loves Creek Member.||Bitter Springs Group||Underlain by Gillen Formation. Overlain by Johnnys Creek Formation.||
79260|Loves Creek Formation|73180|6|Mentioned|p48 Fig.1, p51 Fig.6|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Bitter Springs Group||Disconformably overlies the Gillen Formation, conformably underlies the Jonnys Creek Formation.||
79066|Lucy Gabbro|69917|5|Briefly described|p108-109, 1|Statherian|Statherian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating is poorly constrained. Mafic intrusion took place during the 1780-1770 Ma Yambah Event.|||||Two pyroxene mafic granulite characterised by a fine-grained granoblastic assemblage of plagioclase, orthopyroxene, hornblende, clinopyroxene and quartz.|
79066|Lucy Gabbro|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1776+/-10 Ma (U-Pb zircon LA-ICPMS).||||Metagabbro.|
42372|Lyell Brown Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Coarse-grained, weakly foliated porphyritic biotite granite with coarse tabular to rounded grey K-feldspar phenocrysts.  In the Arunta region.||||||07-NOV-08
42372|Lyell Brown Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Coarse grained, weakly foliated porphyritic biotite granite with coarse tabular to rounded grey K feldspar phenocrysts. Geological Province: Warumpi Province||||||07-NOV-08
42372|Lyell Brown Granite|69428|5|Briefly described|p13:11|||Close et al. (in prep). Crops out W of the Ehrenberg Range.|||||A coarse-grained porphyritic biotite granite characterised by grey, tabular to ellipsoidal K-feldspar phenocrysts to 5cm, in a coarse-grained matrix. Commonly undeformed, but with locally developed biotite foliation.|12-JUL-16
42372|Lyell Brown Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42372|Lyell Brown Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.|||||Coarse grained, weakly foliated porphyritic biotite granite with coarse tabular to rounded grey K-feldspar phenocrysts.|09-SEP-19
42108|MacFarlane Granodiorite|23809|5|Briefly described|p11|Paleoproterozoic|Paleoproterozoic|See also MacFarlane granodiorite.  Probably misspelt also - and should be MacFarlanes?  May be informal reference to a granodiorite within the MacFarlanes Peak Group.  Of the Inningarra Suite.||||||07-NOV-08
42108|MacFarlane Granodiorite|62580|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Of the Coomarie Suite. Intrudes the McFarlane Peak Group southwest of the Tanami Mine. Foliated, pink to grey, fine- to medium-grained, hornblende-biotite granodiorite. Age for crystallisation: 1809+/-8Ma (U/Pb zircon).||||||05-JUN-20
29769|Madderns Yard Metamorphic Complex|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the  Arunta Block.||||||07-NOV-08
29769|Madderns Yard Metamorphic Complex|43503|2|Defined|7, 21, 77|||||||||
29769|Madderns Yard Metamorphic Complex|50369|5|Briefly described|p19.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1650-1680Ma.||||||07-NOV-08
29769|Madderns Yard Metamorphic Complex|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes: Udor Granite, Talipata Granite, Peculiar Complex and the Glen Helen Metamorphics.  Age: 1690-1660Ma.  Geological Province: Warumpi Province||||||07-NOV-08
29769|Madderns Yard Metamorphic Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1660-1690Ma. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
29769|Madderns Yard Metamorphic Complex|61660|4|Described|p1, p3, p4, p23.  |Proterozoic|Proterozoic|Metamorphosed at 1640 - 1635 Ma (the newly-coined "Liebig Orogeny", this article), 1571 and 1149 Ma; also reworked during the Chewings Orogeny (1610 - 1600 Ma).|1688 +/- 14 Ma.||Includes Glen Helen Metamorphics.|Intruded by the Teapot Granite Complex.|Upper amphibolite facies felsic gneisses and minor metasedimentary rocks.|03-DEC-15
29769|Madderns Yard Metamorphic Complex|67565|5|Briefly described|p4, p5 Fig.3, p8 Table 1.|Paleoproterozoic|Paleoproterozoic|Glen Helen Subdomain, Haasts Bluff Domain, Warumpi Province.|||Includes Glen Helen Metamorphics.|Is locally overlain by the Iwupataka Metamorphic Complex.||
29769|Madderns Yard Metamorphic Complex|69221|6|Mentioned|p200-201|Mesoproterozoic|Mesoproterozoic|Basement to Amadeus Basin. Intermediate heat-producing metasediments and orthogneisses (values given).||||||
29769|Madderns Yard Metamorphic Complex|69417|5|Briefly described|p2:5|Statherian|Statherian|Haasts Bluff Domain, Warumpi Province.||||Is intruded by Talipata and Udor Granites.||12-JUL-16
29769|Madderns Yard Metamorphic Complex|69428|5|Briefly described|p13:1-3|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995). Eastern Haasts Bluff Domain, Warumpi Province.|||Glen Helen Metamorphics, Boggy Hole Gneiss.|Is overlain unconformably by Iwupataka Metamorphic Complex.|Upper amphibolite-facies felsic gneiss and lesser metasedimentary rocks.|12-JUL-16
33044|Madderns Yard Suite|24197|5|Briefly described|p22, p26, p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Example of the Kalkadoon Association. Age: 1660Ma. Geological province: Arunta Inlier. Example of the Cullen Association. Age: 1680Ma.||||||07-FEB-11
33044|Madderns Yard Suite|50369|5|Briefly described|p1.5, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1680Ma.||||||07-NOV-08
23749|Mahony Group|14019|6|Mentioned|p21|||Conglomerate.  Geological Province: Ord Basin.||||||
23749|Mahony Group|22537|6|Mentioned|34|Devonian|Devonian|||||||
23749|Mahony Group|22814|5|Briefly described|fig2|Late Devonian|Late Devonian|||||||
23749|Mahony Group|23621|5|Briefly described|p36|Devonian|Devonian|See also page 9 table 1. Underlying unit Headleys Limestone. Geological Province: Ord Basin.||||||
23749|Mahony Group|23622|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Ord Basin.||||||
23749|Mahony Group|23858|5|Briefly described|p919|Late Devonian|Late Devonian|Geological Province: Ord Basin. Max. thickness: >1000 m.||||||
23749|Mahony Group|24503|5|Briefly described|Map legend|Devonian|Devonian|Quartz sandstone, pebbly sandstone and pebble to boulder conglomerate.  Geological Province: Ord Basin.||||||
23749|Mahony Group|40993|6|Mentioned|Fig.1|||||||||
23749|Mahony Group|41840|3|Fully described|p44|||||||||
23749|Mahony Group|41864|4|Described|p55|||||||||
23749|Mahony Group|41865|6|Mentioned|Map legend||Frasnian|||||||
23749|Mahony Group|41866|6|Mentioned|Map legend|Frasnian||||||||
23749|Mahony Group|42030|4|Described|p750|||||||||
23749|Mahony Group|43299|5|Briefly described|Map Legend||Devonian|||||||
23749|Mahony Group|43301|5|Briefly described|Map Legend||Paleozoic|age Devonian?||||||07-NOV-08
23749|Mahony Group|43855|5|Briefly described|Map Legend||Frasnian|||||||
23749|Mahony Group|44868|5|Briefly described|Map Legend||Frasnian|||||||
23749|Mahony Group|60419|5|Briefly described|p1|Late Devonian|Late Devonian|Sandstone and minor conglomerate. Geological Province: Ord Basin.||||||
23749|Mahony Group|60519|5|Briefly described|Map Legend|Frasnian|Frasnian|Geological Province: Ord Basin. Includes: Glass Hill Sandstone.||||||
23749|Mahony Group|64580|4|Described|map legend||Frasnian|Sandstone (in places pebbly), pebble to boulder conglomerate; includes PURRALILI and GLASS HILL SANDSTONES, and BOLL CONGLOMERATE.||||||09-DEC-08
23749|Mahony Group|67860|4|Described|p416,417 Figs.4-84,85; p418 Tb. 4-18|Frasnian|Frasnian|See also p421-422. 200-1000 m thick.|||Includes Glass Hill and Purralili Sandstones, and Boll Conglomerate.|Overlies Goose Hole Group unconformably. Correlated with Cockatoo Group (Bonaparte Basin).|Quartz sandstone and conglomerate.|
23749|Mahony Group|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Frasnian|Frasnian|Ord Basin. See also 500k_geologyp08_lut.|||Includes Purralili, Glass Hill Sandstones and Boll Conglomerate.||Undivided; sandstone (pebbly in places), pebble to boulder conglomerate|
23749|Mahony Group|69099|4|Described|GEOL_LUT_CSV files + geochron files|Frasnian|Frasnian|Ord Basin|||Includes Glass Hill Sandstone, Boll Conglomerate||Sandstone (pebbly in places), and pebble to boulder conglomerate.|03-AUG-15
23749|Mahony Group|69165|4|Described|100k_interpgeop_lut.csv|Frasnian|Frasnian|See also 500k_geologyp08_lut.csv. |||Includes Glass Hill Sandstone, Boll Conglomerate, Purralili Sandstone||Undivided sandstone (in places pebbly), pebble to boulder conglomerate.|
23749|Mahony Group|69448|5|Briefly described|p33:1-3, 6-8|Late Devonian|Late Devonian|Forms the top of the Ord Basin succession in WA. Up to 1000m thick. Alluvial fan, fluviatile, aeolian, minor intertidal deposits. Probable Frasnian age. Displaced by  the NW-trending Negri Fault.||||Unconformably overlies Elder Subgroup (Goose Hole Group).|Quartz sandstone, pebbly sandstone, conglomerate; minor siltstone.|12-JUL-16
23749|Mahony Group|69587|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological province: Halls Creek Orogen, North Australian Craton. Of Ord Basin; Hardman Fold belt Events: Alice Springs Orogeny. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|||||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|69634|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|382.7-372.2 Ma (Inferred)||Includes Boll Conglomerate, Glass Hill Sandstone, Purralili Sandstone.||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|70141|5|Briefly described|Map legend.|Frasnian|Frasnian|Ord Basin.|||||Sandstone, pebbly in places, and pebble to boulder conglomerate.|
23749|Mahony Group|70154|5|Briefly described|100k_interpgeop_lut.csv|Frasnian|Frasnian|See also 500k_interpgeop_lut.csv.|372-383 Ma||Includes Boll Conglomerate, Glass Hill Sandstone||Sandstone and pebble to boulder conglomerate.|
23749|Mahony Group|70826|6|Mentioned|p7 tbl 3|Devonian|Devonian|Ord Basin.||||||
23749|Mahony Group|70851|6|Mentioned|p18|||||||||
23749|Mahony Group|71146|5|Briefly described|p6|Frasnian|Givetian|Ord Basin.|||Includes the Boll Conglomerate.|Unconformably overlies the Elder Subgroup.|Sandstone.|
23749|Mahony Group|71267|4|Described|GEOL_LUT_CSV files|Frasnian|Frasnian|Geological Province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|382.7-372.2 Ma (inferred)||Includes Boll Conglomerate, Galss Hill Sandstone, Purralili Sandstone.||Sandstone (pebbly in places), and pebble to boulder conglomerate|
23749|Mahony Group|71800|5|Briefly described|p25, |Devonian|Devonian|Ord Basin.||||Unconformably overlies the Overland Sandstone.||
23749|Mahony Group|72034|5|Briefly described|500k_interpgeop16_lut|Frasnian|Frasnian|Ord Basin. |||||Sandstone (pebbly in places), and pebble to boulder conglomerate.|
23749|Mahony Group|73255|6|Mentioned|p533 Fig.1, p534 Fig.2|Devonian|Devonian||||Buchanan Sandstone, Glass Hill Sandstone, Boll Conglomerate.|Disconformably overlies the Goose Hole Group, Overland Sandstone.||
22242|Maidjunga Member|22538|6|Mentioned|Fig3 p708||Statherian|Age of unit is 1707+/-12 Ma.||||||23-MAR-18
22242|Maidjunga Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
22242|Maidjunga Member|23363|5|Briefly described|344 Fig.3|Statherian|Statherian|Age: ~1706Ma.||||||31-OCT-06
22242|Maidjunga Member|24048|3|Fully described|p28|Statherian|Statherian|Of the Fagan Volcanics.  Age: 1707+/-12Ma (SHRIMP U-Pb).  Geological Province: McArthur Basin.||||||31-OCT-06
22242|Maidjunga Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics, Donydji Group. Rhyolite: brown and pink, coarsely porphyritic with phenocrysts of K-feldspar, quartz and albite; minor volcaniclastic sandstone and mudstone; locally foliated and sheared. Geol. Prov: McArthur Basin.||||||13-OCT-05
22242|Maidjunga Member|44112|3|Fully described|p29,38-39,109-110||Statherian|Max Age: 1707 (+/-) 12 Ma.||||||31-OCT-06
22242|Maidjunga Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics, Donydji Group. Rhyolite: brown and pink, coarsely porphyritic with phenocrysts of K-feldspar, quartz and albite; minor volcaniclastic sandstone and mudstone; locally foliated and sheared. Geol. Prov: McArthur Basin.||||||07-OCT-19
22242|Maidjunga Member|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1707 +/- 12 Ma.|Of the Fagan Volcanics.||||
22242|Maidjunga Member|69430|4|Described|p15:3, 6-7|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 150-250m thick; locally removed. Shallow-water, low energy sediments; extrusive and high-level intrusive igneous rocks. SHRIMP U-Pb zircon age.|1707 +/- 12 Ma (Page et al., 2000).|Fagan Volcanics.||Conformably (or mildly disconformably) overlies Ritarango Formation. Is overlain conformably by Sheridan Member.|Rhyolite; minor volcaniclastic sandstone and mudstone; locally foliated and sheared.|12-JUL-16
22242|Maidjunga Member|69673|6|Mentioned|p16 fig 13|||||Fagan Volcanics||Overlain by Sheridan Member, overlies Ritarango Formation||
22242|Maidjunga 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 1707+\-12 Ma, interpreted to record timing of volcanism in the Donydji Group.|1707+\-12 Ma (Pb/Pb; volcanism)|Unit of Fagan Volcanics.|||Rhyolite.|10-OCT-19
75074|Mairmull Formation|67370|2|Defined|p313 Fig.2, p314, pp316-318, pp332-333.|Early Triassic|Early Triassic|New name (this study). Named after Mairmull Creek southeast of Wadeye, NT. Type section is in Fishburn-1 between 2,121 - 2,320 m. Deposited in shallow water conditions: contains Lingula, conchastracans and spinose acritarchs. Occurs throughout Bonaparte Basin and in eastern Browse Basin.||Unit in Mount Goodwin Subgroup.||Unconformably overlies Penguin Formation or Hyland Bay Sub-group. Is overlain unconformably by Ascalon Formation.|Predominantly greenish, sometimes reddish, claystone and siltstone; rare coarser sediments: thin sandstone beds in the uppermost interval.|
75074|Mairmull Formation|69452|3|Fully described|p36:8, 15, 20-21|Olenekian|Induan|Gorter et al. (2009). Equivalent to the Lower Mount Goodwin Formation of Gorter (1998) and Gorter et al. (1998). Petrel Sub-basin, Bonaparte Basin. 199m thick in the type section in drillhole Fishburn-1. Undifferentiated Ascalon Fm/Mairmull Fm forms 20m of shale and siltstone onshore, near Mount Goodwin. Has distinctive low-angle cross-lamination; contains lingulid brachiopods, estheriid conchostracens, indeterminate plants and vertebrate remains.||Mount Goodwin Subgroup.||Overlies Penguin Formation conformably or Hyland Bay Subgroup unconformably. Is overlain unconformably by Ascalon Formation.|Claystone and siltstone with rare thin sandstone interbeds, which are more common towards the top.|12-JUL-16
75074|Mairmull Formation|69454|5|Briefly described|p38:4|Olenekian|Changhsingian|Petrel Sub-basin, Bonaparte Basin.||Mount Goodwin Subgroup.||||12-JUL-16
75074|Mairmull Formation|69653|6|Mentioned|p10|Early Triassic|Early Triassic|Petrel Sub-basin.||Mount Goodwin Sub-group.||Overlies Penguin Formation. Is overlain by Ascalon Formation.||
75074|Mairmull Formation|69673|6|Mentioned|p153 fig 125|||||Mount Goodwin Subgroup||Overlain by Ascalon Formation, overlies Penguin Formation||
75074|Mairmull Formation|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3|Induan|Induan|See also Regional geology: Figs.6-8. Vulcan: Fig.2.||Mount Goodwin Subgroup.||Overlies Penguin Formation. Is overlain by Ascalon Formation.||12-JUL-16
75074|Mairmull Formation|73304|6|Mentioned|p77|||Bonaparte Basin.||||||
25195|Maiwok Subgroup|22538|6|Mentioned|Fig3 P709|||||||||
25195|Maiwok Subgroup|22600|6|Mentioned|Map legend|||||||||
25195|Maiwok Subgroup|22808|6|Mentioned|7 fig 4|||||||||
25195|Maiwok Subgroup|23216|6|Mentioned|Table1p7,34|||||||||
25195|Maiwok Subgroup|23374|5|Briefly described|Fig3p5||Mesoproterozoic|In the McArthur Basin.||||||31-OCT-06
25195|Maiwok Subgroup|23937|2|Defined|p84 App. 1|Calymmian|Calymmian|Of the Roper Group. Unit redefined to include the Corcoran Fm and Bessie Creek Sst, based on lithological evidence.  Max. thick: 600m (excluding Chambers River Fm).   Conformably overlies the Collara Subgroup.  Geol.Prov: McArthur Basin. See also p40.||||||12-APR-18
25195|Maiwok Subgroup|24048|6|Mentioned|p71|||||||||
25195|Maiwok Subgroup|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|In regional setting map legend.||||||
25195|Maiwok Subgroup|37568|6|Mentioned|Fig.5|||||||||
25195|Maiwok Subgroup|40691|6|Mentioned|Fig.4|||||||||
25195|Maiwok Subgroup|41268|5|Briefly described|Fig.4|||Mention p290.||||||31-OCT-06
25195|Maiwok Subgroup|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
25195|Maiwok Subgroup|41531|5|Briefly described|p167|||||||||
25195|Maiwok Subgroup|42395|6|Mentioned|Fig.26 P86|||||||||
25195|Maiwok Subgroup|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Roper Group.|Includes: Kyalla and Moroak Sandstone Members (McMinn Formation) and Velkerri Formation.|Overlies Lower Roper Group.||24-OCT-11
25195|Maiwok Subgroup|42639|4|Described|p44, Table 7 p39|||||||||
25195|Maiwok Subgroup|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25195|Maiwok Subgroup|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Quartz sandstone, micaceous sandstone and mudstone, black shale, calcareous mudstone, pisolitic and oolitic ironstone.||||||19-OCT-05
25195|Maiwok Subgroup|42812|4|Described|p54, Table 5|||Of Roper Group.||||||31-OCT-06
25195|Maiwok Subgroup|42846|6|Mentioned|Fig.1 p502|||Of Roper Group||||||31-OCT-06
25195|Maiwok Subgroup|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Roper Group. Of "Mid Proterozoic" age.||||||31-OCT-06
25195|Maiwok Subgroup|43036|5|Briefly described|Fig.3|||||||||
25195|Maiwok Subgroup|43149|5|Briefly described|Map Legend||Mesoproterozoic|Of Roper Group. Of Calymmian age.||||||31-OCT-06
25195|Maiwok Subgroup|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
25195|Maiwok Subgroup|44287|14|Not recorded|p.12|||(E53-3).||||||
25195|Maiwok Subgroup|44332|14|Not recorded|p.8-13,opp.6,map|||(D53-14).||||||
25195|Maiwok Subgroup|44333|14|Not recorded|map legend|||Upper(?) Proterozoic.||||||
25195|Maiwok Subgroup|44471|14|Not recorded|p.10,13,opp.p.7, map|||(D53-10).||||||
25195|Maiwok Subgroup|44530|14|Not recorded|p.12, opp.12|||(D53-15).||||||
25195|Maiwok Subgroup|45022|4|Described|p.80||Adelaidean|On many pages.||||||31-OCT-06
25195|Maiwok Subgroup|46861|6|Mentioned|Fig.2|||||||||
25195|Maiwok Subgroup|60483|5|Briefly described|p7 Fig. 5|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
25195|Maiwok Subgroup|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Includes McMinn and Velkerri Formations.||||||03-JUN-09
25195|Maiwok Subgroup|60573|5|Briefly described|Regional Setting legend|Mesoproterozoic|Mesoproterozoic|Of the Roper River Group.||||||15-FEB-05
25195|Maiwok Subgroup|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Roper Group.||||||
25195|Maiwok Subgroup|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|In regional setting map legend.||||||14-OCT-05
25195|Maiwok Subgroup|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.|Includes the McMinn and Velkerri Formations.|||
25195|Maiwok Subgroup|65228|6|Mentioned|Fig.02.|||||Unit in Roper Group.|Includes Velkerri and McMinn Formations.|||
25195|Maiwok Subgroup|67323|6|Mentioned|Eastern Australia Time-Space Plot|||McArthur region.||||||
25195|Maiwok Subgroup|69430|4|Described|p15:3, 26-27, 29-30|Calymmian|Calymmian|Dunn (1963), Randal (1963): for Roper Group strata, above the Bessie Creek Sandstone, characterised by finer grainsize and presence of oolitic ironstone. Redefined by Abbott et al. (2002) to include the entire Corcoran Formation - Chambers River Formation succession. McArthur Basin.||Roper Group.|Corcoran, Velkerri, McMinn, Sherwin, Kyalla, Chambers River Formations; Bessie Creek, Moroak, Bukalorkmi Sandstones.|||12-JUL-16
25195|Maiwok Subgroup|69673|6|Mentioned|p16 fig 13|||Northwestern and Southern McArthur Basin.||Roper Group|Includes Corcoran Formation, Bessie Creek Sandstone, Velkerri Formation, McMinn Formation, Moroak Sandstone, Sherwin Formation, Kyalla Formation, Bukalorkmi Sandstone||Sandstone and mudstone.|
25195|Maiwok Subgroup|70734|5|Briefly described|p14, 16|Mesoproterozoic||McArthur Basin. Mudstone-dominated? Shown as Maiwok subgroup p16.||Of Roper Group.|Includes Corcoran Formation, Bessie Creek Sandstone, Velkerri Foramtion, McMinn Formation, Chambers River Formation.|||
25195|Maiwok Subgroup|70968|3|Fully described|v-vi, p2, p5-6, p50-86, p94, p123-124|Ectasian|Ectasian|See also p127-132, p134-135, p137-138, p140, p144. Sweet and Abbott in Abbott et al. (2001), after Dunn (1963) who included rocks from basal Velkerri Formation to top of the Roper Group. Abbott et al. (2001) included the Corcoran Formation and Bessie Creek Sandstone. Pietsch et al. (1991) included rocks previously mapped as Cobanbirini Formation in BAUHINIA DOWNS sheet. Named after Maiwok Creek. Generally forms subdued ridge and valley topography. Up to c.1840m thick. Deposition in shallow-marine mud-dominated shelf setting via wave-induced density flows or turbidity currents, as well as from suspension. Detrital zircon spectra discussed. May correlate with the Mullera Formation.||Roper Group.|Corcoran, Velkerri, Sherwin, Kyalla, Chambers River Formations; Bessie Creek, Moroak, Bukalorkmi Sandstones.|Overlies Collara Subgroup disconformably, locally conformably. Is overlain unconformably by Kalkarindji Suite. Is intruded by Derim Derim Dolerite sills.|Commonly interlaminated and interbedded claystone, siltstone and minor fine-grained sandstone. Minor but diagnostic oolitic ironstone.|
25195|Maiwok Subgroup|71059|5|Briefly described|p1-3|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Corcoran, Velkerri, Sherwin, Kyalla, Chambers River Formations; Bessie Creek, Moroak, Bukalorkmi Sandstones.||Mudrock-dominated.|
25195|Maiwok Subgroup|71488|4|Described|p140-142, p148-p150, p152-p153|||Beetaloo Sub-basin. Referred to as the lower Maiwok Subgroup on p150.||Roper Group|Includes the Corcoran Formation, Bessie Creek Sandstone, Velkerri Formation, Moroak Sandstone, Sherwin Ironstone, Kyalla Formation, Bukalorkmi Sandstone, Chambers River Formation.|Intruded by the Derim Derim Dolerite. Disconformably overlies the Collara Subgroup.|Dominated by mudrock sequences with less voluminous sandstones deposited in a range of environments.|02-MAY-18
25195|Maiwok Subgroup|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Upperpart of Roper Group.|||Mudstone, shale (+/- carbonaceous), lithic-glauconitic sandstone, ooidal ironstone, quartzose sandstone.|04-MAR-20
25195|Maiwok Subgroup|71779|5|Briefly described|p1-p2, p5, p6, p24, 25|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Has been redefined in Abbott et al, 2001 to include the underlying Corcoran Formation and Bessie Creek Sandstone.||Roper Group|Includes the Velkerri Formation, Bukalorkmi Sandstone, Chambers River Formation, Kyalla Formation, Sherwin Formation, Moroak Sandstone, Bessie Creek Sandstone, Corcoran Formation.|||24-SEP-18
25195|Maiwok Subgroup|71893|4|Described|iii, p3-p5, p8-p9|Mesoproterozoic|Mesoproterozoic|McArthur Basin. See also p20, p24-p25, p28, p37.||Roper Group|Includes the Bessie Creek Sandstone, Moroak Sandstone, Bukalorkmi Sandstone, Kyalla Formation, Velkerri Formation, Corcoran Formation, Sherwin Formation and the Chambers River Formation.|||
25195|Maiwok Subgroup|72381|4|Described|p773,776-780|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Dominated by sandstones (some glauconitic) with less voluminous mudrocks, deposited in a range of depositional environments from shoreline to shallow marine shelf (Jackson et al. 1988; Abbott and Sweet 2000; Abbott et al. 2001; Ahmad and Munson 2013). Faults and fault-related basement highs of the present-day Beetaloo Sub-basin acted as bathymetric barriers during early Maiwok Subgroup sedimentation (Yang et al., 2018). 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 (e.g. Mount Isa) to southern sources (e.g. Arunta region), supported by hafnium isotopic data. Interpreted to have received detritus from Mount Isa province as it was exhumed during Laurentian-Australian rifting event. ||Unit of Roper Group.|Includes Kyalla Formation, Moroak Sandstone, Velkerri Formation and Bessie Creek Sandstone.|Uppermost unit of Roper Group. Underlain by Collara Subgroup. Intruded by Derim Derim Dolerite.|Sandstones (some glauconitic) with less voluminous mudrocks.|
25195|Maiwok Subgroup|72526|5|Briefly described|p3, p85, p8 Fig.1.3.|Ectasian|Mesoproterozoic|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone. Spelling incorrect in diagram p8 showing 'Malwick Subgroup'. Minimum age based on age of intrusive Derim Derim Dolerite (1313 Ma)||Roper Group|Bukalorkmi Sandstone, Kyalla Formation, Sherwin Formation, Moroak Sandstone, Velkerri Formation, Bessie Creek Sandstone, Corcoran Formation.|Overlies Collara Subgroup. Intruded by Derim Derim Dolerite.||
25195|Maiwok Subgroup|72527|6|Mentioned|p10.|Ectasian|Ectasian|TIMS U-Pb baddeleyite age has helped constrain the age of this group.|1312.9+/-0.7 Ma TIMS U-Pb baddeleyite||Includes Bukalorkmi Sandstone.|||
25195|Maiwok Subgroup|72718|6|Mentioned|p7, p9|||McArthur Basin. Wilton package.||Roper Group|Bukalorkmi Sandstone, Kyalla Formation, Sherwin Formation, Moroak Sandstone, Velkerri Formation, Bessie Creek Sandstone, Corcoran Formation.|Underlain by Collara Subgroup. Overlain by Derim Derim Dolerite.|Generally finer-grained|
25195|Maiwok Subgroup|72912|5|Briefly described|p20|Mesoproterozoic|Mesoproterozoic|Mispelt as 'Malwick Subgroup' in diagram p5 Fig.3. Minimum age from Derim Derim Dolerite, which intrudes both Collara Subgroup (from Mainoru Formation) and Maiwok Subgroup up to the top (Bukalorkmi Sandstone). [probably U-Pb SHRIMP] baddelyite magmatic age: 1312.9 +/- 0.7 Ma reported  (Collins et al., 2018).|1312.9 +/- 0.7 Ma min,age.|Roper Group|Bukalorkmi Sandstone, Kyalla Formation, Sherwin Formation, Moroak Sandstone, Velkerri Formation, Bessie Creek Sandstone, Corcoran Formation.|Overlies Collara Subgroup.||
25195|Maiwok Subgroup|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Roper Group|Kyalla, Sherwin, Velkerri, Corcoran formations; Bukalorkmi, Moroak, Bessie Creek sandstones.|Underlain by Collara Subgroup. Overlain by Jamison Sandstone.||
25195|Maiwok Subgroup|73083|6|Mentioned|p11-12|||Mapped as underlying a large area of Cenozoic superficial rocks in the Bauhinia Downs 1:250K Sheet area but this is equally likely be Lower Roper Group.||||||
25195|Maiwok Subgroup|73242|5|Briefly described|p39-40|||||Roper Group|Chambers River Formation, Bukalorkmi Sandstone, Kyalla Formation, Sherwin Ironstone, Moroak Sandstone, Velkerri Formation, Bessie Creek Sandstone, Corcoran Formation, and units therein|Underlain by Hodgson Sandstone, Collara Subgroup. Intruded by Derim Derim Dolerite.||
25195|Maiwok Subgroup|73412|5|Briefly described|p4, 8, 18|||Southern McArthur Basin.||Roper Group.|Corcoran, Velkerri, Sherwin, Kyalla Formations; Bessie Creek, Moroak Sandstones; Derim Derim Dolerite.|Overlies Collara Subgroup.||
23751|Malita Formation|13194|4|Described|p386 Tb. 4-16, p396 fig 4-60|Jurassic|Late Triassic|Type Section: Petrel 1 well (2229-2471m). 120-392m thick continental to marginal marine deposits.||Troughton Group||Overlies Cape Londonderry Formation or Sahul Group (both conformably). Overlain by Plover Formation (disconformably).|Red sandstone and shale; minor limestone.|
23751|Malita Formation|13224|6|Mentioned|p485 fig 3|Pliensbachian|Norian|||||||
23751|Malita Formation|13234|6|Mentioned|p250 Fig.2,p263 Tb.4, |Early Jurassic|Late Triassic|Potential reservoir.||||Overlies Cape Londonderry Formation, offshore.|Redbed fluvial sands.|
23751|Malita Formation|13354|6|Mentioned|p376 Fig.7, p379.|Late Triassic|Late Triassic|Bonaparte Basin, Petrel Sub-basin. Overlies Challis Formation.||62||||28-OCT-14
23751|Malita Formation|22663|5|Briefly described|NT97 -1-4 Fig.3||Triassic|||||||01-MAR-10
23751|Malita Formation|23377|6|Mentioned|p212 Fig.5||Late Triassic|In the Vulcan Sub-basin.||||||31-OCT-06
23751|Malita Formation|24569|5|Briefly described|p248 Fig. 3|Sinemurian|Norian|Of the Troughton Group. Geological Province: Petrel Sub-basin.||||||17-MAR-05
23751|Malita Formation|40077|6|Mentioned|Table 1|||||||||
23751|Malita Formation|41436|6|Mentioned|p44|||||||||
23751|Malita Formation|41459|6|Mentioned|Fig.2|||||||||
23751|Malita Formation|41532|3|Fully described|p304|||||||||
23751|Malita Formation|41690|5|Briefly described|p5|||||||||
23751|Malita Formation|41731|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|41733|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|41759|6|Mentioned|p270|||||||||
23751|Malita Formation|42034|4|Described|Fig.4 P11|||||||||
23751|Malita Formation|42056|5|Briefly described|p98|||||||||
23751|Malita Formation|42057|6|Mentioned|Fig.3 P70|||||||||
23751|Malita Formation|42081|5|Briefly described|Fig.2 P291|||||||||
23751|Malita Formation|42151|6|Mentioned|Fig.3 P57|||||||||
23751|Malita Formation|42442|2|Defined|p24|Pliensbachian|Carnian|||||||
23751|Malita Formation|43661|6|Mentioned|Fig.3|||||||||
23751|Malita Formation|43699|6|Mentioned|Fig.6,p10|Middle Jurassic|Early Jurassic|||||||
23751|Malita Formation|43705|6|Mentioned|p20|Early Jurassic|Middle Triassic|||||||
23751|Malita Formation|43739|6|Mentioned|Fig.5,p38|Early Jurassic|Triassic|||||||
23751|Malita Formation|43826|6|Mentioned|Fig.2,p163|Early Jurassic|Late Triassic|||||||01-MAR-10
23751|Malita Formation|49637|5|Briefly described|p7|Early Jurassic|Eary Jurassic|Of the Troughton Group. Fluviodeltaic siliciclastics. Geological Province: Londonderry High/Sahul Platform. See also Figs. 3 and 6.||||||29-APR-13
23751|Malita Formation|60386|6|Mentioned|p300|Early Jurassic|Late Triassic|Bonaparte Basin. Deltaic-nearshore-shelf. ||||||
23751|Malita Formation|61548|6|Mentioned|p480 Fig.3|Late Triassic|Late Triassic|Northern Bonaparte Basin.||||||
23751|Malita Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Of the Troughton Group.  Age: ~222-~198Ma. Geological Province:  Petrel Sub-basin (offshore).||||||01-MAR-10
23751|Malita Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Ashmore Platform (east) and Petrel Sub-basin. Non-marine sediments with local red beds.||||Overlies Nome Formation.||
23751|Malita Formation|66124|5|Briefly described|p171 Fig.2|Rhaetian|Rhaetian|Ashmore Platform (East); also present in Petrel Sub-basin. Non-marine. Overlies Nome Formation.||||||
23751|Malita Formation|67370|6|Mentioned|p323 Fig.14.|Late Triassic|Late Triassic|Southeastern Bonaparte Basin. Type section in Petrel-1 between 2,229 - 2471 m.||Unit in Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.||
23751|Malita Formation|68135|5|Briefly described|p51 fig 2a|Middle Jurassic|Early Jurassic|Bonaparte Basin.||Troughton Group.||Is overlain by Plover Formation.||14-SEP-17
23751|Malita Formation|68223|6|Mentioned|p178 Fig.3|Norian|Norian|||||||
23751|Malita Formation|69452|5|Briefly described|p36:8, 15, 21|Late Triassic|Late Triassic|Petrel Sub-basin, Bonaparte Basin. Up to 300m thick. Generally non-marine, possibly arid environment.||Troughton Group.|||Red beds.|12-JUL-16
23751|Malita Formation|69454|5|Briefly described|p38:4|Rhaetian|Norian|Petrel Sub-basin, Bonaparte Basin.||Troughton Group.||||12-JUL-16
23751|Malita Formation|69456|6|Mentioned|p40:3|||Bonaparte Basin.||Troughton Group.||||12-JUL-16
23751|Malita Formation|69653|6|Mentioned|p6, 8, 10, p13 Fig.2.4, p25-27, 30|Triassic|Triassic|Petrel Sub-basin. Schematic (gamma ray) well sections. Composite well diagram. See also p41-43, 48, 50.||Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.||
23751|Malita Formation|69673|5|Briefly described|p153 fig 125, p173|||||Troughton Group||Overlies Cape Londonderry Formation|Sandstone, siltstone and shale.|
23751|Malita Formation|69689|6|Mentioned|p16|Jurassic|Jurassic|Bonaparte Basin.||||Overlies Mount Goodwin Sub-group.||
23751|Malita Formation|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Norian|Norian|See also Regional geology: Figs.6-7, p5. Vulcan: Fig.2.||Troughton Group.||Overlies Cape Londonderry Formation. Is overlain by Plover Formation.|Fluvial sediments.|12-JUL-16
33806|Mallabah Dolostone|14019|3|Fully described|p8, 28|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Supersedes the Mallabah Dolomite. Dololutite, dolarenite, shale, dolostone. Conformable on Amos Knob Formation; conformably overlain by Kunja Siltstone. Type section: 100m. Geological Province: Birrindudu Basin.||||||07-NOV-08
33806|Mallabah Dolostone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33806|Mallabah Dolostone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33806|Mallabah Dolostone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Amos Knob Formation;  overlain by Kunja Siltstone. Geological Province: Birrindudu Basin.||||||08-AUG-05
33806|Mallabah Dolostone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33806|Mallabah Dolostone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Stromatolitic dolostone, dolomitic mudstone, minor carbonaceous mudstone.  Conformably overlies the Pear Tree Dolostone; conformably overlain by Kunja Siltstone.  Geological Province: Birrindudu Basin.||||||07-NOV-08
33806|Mallabah Dolostone|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dolostone and ferruginous dolostone, intraformational conglomerate. Of Limbunya Group. Overlain by Kunja Siltstone. Overlies Amos Knob Formation. Geological Province: Birrindudu Basin.||||||07-NOV-08
33806|Mallabah Dolostone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
33806|Mallabah Dolostone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Amos Knob Formation. Is overlain by Kunja Siltstone.||
33806|Mallabah Dolostone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Amos Knob Formation. Is overlain by Kunja Siltstone.|Stromatolitic dolostone, dolomitic mudstone, minor carbonaceous mudstone, intraformal conglomerate (section only).|
33806|Mallabah Dolostone|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
33806|Mallabah Dolostone|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
33806|Mallabah Dolostone|69432|5|Briefly described|p17:2, 7, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. Thickness varies widely up to c.100m. Exploration target for base metals.||Limbunya Group.|||In outcrop, generally comprises ferruginous, laminated, planar stromatolitic dolostone grading into dolomitic mudstone. Black carbonaceous shale occurs in drillhole intersections. Silicified Conophyton and biostromal stromatolites locally abundant.|12-JUL-16
33806|Mallabah Dolostone|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Amos Knob Formation, overlain by Kunja Siltstone||
33806|Mallabah Dolostone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Section only.||Limbunya Group||Overlies Amos Knob Formation. Is overlain by Kunja Siltstone.|Stromatolitic dolostone, dolomitic mudstone, minor carbonaceous mudstone, intraformal conglomerate.|
33806|Mallabah Dolostone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Limbunya Group.||Overlies Amos Knob Formation. Is overlain by Kunja Siltstone.|Dolostone and ferruginous dolostone, intraformational conglomerate.|
33806|Mallabah Dolostone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
33806|Mallabah Dolostone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Kunja Siltstone. Underlain by Amos Knob Formation.||
33806|Mallabah Dolostone|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Amos Knob Formation. Overlain by Kunja Siltstone.||
33806|Mallabah Dolostone|73280|6|Mentioned|p1, p4-5, App.1A|||Birrindudu Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
34024|Mamadawerre Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
34024|Mamadawerre Sandstone|23374|2|Defined|Tb2p10,9,10,11,12,13,14,15,41,36||Statherian|No type section possible in study area, but lower and upper boundary stratotypes given. Of Kombolgie Subgroup, Katherine River Group, McArthur Basin.||||||31-OCT-06
34024|Mamadawerre Sandstone|23384|6|Mentioned|Fig 27|||||||||
34024|Mamadawerre Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Kombolgie Subgroup (Katherine River Group).||||||
34024|Mamadawerre Sandstone|23867|3|Fully described|p3, Tb. 1, Figs.3, 30|Paleoproterozoic|Paleoproterozoic|Of Kombolgie Subgroup.  Previously identified as "lower Kombolgie Formation" (Needham 1984), raised to formation status by Carson et al (1999). Overlain by Nungbalgarri Volcanics.  Max. thickness: 1100m.  Geological Province: McArthur Basin.||||||07-NOV-08
34024|Mamadawerre Sandstone|24050|3|Fully described|p12, p10|||Of the Kombolgie Subgroup.  Medium- to thick-bedded, medium- to coarse-grained sandstone; scattered granule and pebble layers.  Overlain by Nungbalgarri Volcanics.||||||31-OCT-06
34024|Mamadawerre Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Kombolgie Subgroup, Katherine River Group. Geological Province: McArthur Basin.||||||
34024|Mamadawerre Sandstone|50545|5|Briefly described|p114 Fig.1||Paleoproterozoic|Of Kombolgie Subgroup.||||||07-NOV-08
34024|Mamadawerre Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Sandstone: white/grey, fine- to coarse-grained, medium- to thick-bedded, planar cross-bedded, trough cross-bedded and minor planar cross-bedded, quartz arenite. Geological Province: McArthur Basin.||||||30-NOV-04
34024|Mamadawerre Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of Kombolgie Subgroup (Katherine River Gp).  White, thickly bedded, poorly sorted, medium to coarse quartz sandstone with pebble/granule bands. Geol.Prov: McArthur Basin. Overlies: Plum Tree Creek Volcanics. Underlies: Nungbalgarri Volcanics.||||||14-JAN-05
34024|Mamadawerre Sandstone|61206|6|Mentioned|p516, p518, p520 |||||Unit in Kombolgie subgroup.||Is overlain by Nungbalgarri Volcanics. Intruded by Oenpelli Dolerite.|Hematitic fluviatile sandstone and conglomerate; well-cemented, poorly-sorted, quartz sandstone.|
34024|Mamadawerre Sandstone|62375|5|Briefly described|p20|Mesoproterozoic|Paleoproterozoic|Of the Kombolgie Subgroup. Sandstone sucession, with intermediate to basic volcanic rocks. Geological Province: Pine Creek Orogen. Thickness: 2000m. Unconformably Overlies: Edith River Group, Cahill Formation.||||||09-FEB-10
34024|Mamadawerre Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.||Of the Kombolgie Subgroup.|||Sandstone and conglomerate.|04-JUN-18
34024|Mamadawerre Sandstone|65232|5|Briefly described|p44-46, p25 Tab. 4, p37, p42|||Of Kombolgie Subgroup. Under Nungbalgarri Volcanics; unconform. over Cahill Formation and El Sherana Group; unconform. contact with Nimbuwah Complex. Basal conglomerate (hosts secondary U mineralisation), quartz sandstone. See also Mamadewerre Sandstone.||||||09-FEB-10
34024|Mamadawerre Sandstone|67057|6|Mentioned|p455 Fig.2.|||Also mis-spelt on the same page as Mamadawere Sandstone.||Basal unit in Kombolgie Subgroup.||Is overlain by Nungbalgarri Volcanics.||15-MAR-12
34024|Mamadawerre Sandstone|67479|6|Mentioned|p16|||||Of the Kombolgie Subgroup.||||
34024|Mamadawerre Sandstone|67564|3|Fully described|p2, p6 Table 2, p10 Fig.5, p18, pp39-41.|Proterozoic|Proterozoic|Outcrops extensively in Arnhem Land Plateau. 1000 m of braided fluviatile deposits; minor shallow marine in upper portion.|1820 - 1800 Ma.|Unit in Kombolgie Subgroup.||Unconformably overlies Nourlangie Schist and Edith River Group. Is intruded by Oenpelli Dolerite. Is overlain conformably by Nungbalgarri Volcanics.|White, thickly bedded, poorly sorted, medium to coarse quartz sandstone; minor siltstone; polymict pebble to boulder conglomerate at base.|
34024|Mamadawerre Sandstone|67779|3|Fully described|p6 Fig.5, p8 Table 1, pp33-34.|Paleoproterozoic|Paleoproterozoic|Formerly Mamadawerre Sandstone Member. McArthur Basin. 150-250 m thick. Distal braided fluvial with minor shallow marine in upper portion; aeolian environment at top of sequence. Ages based on age of Nabarlek Granite and oldest diagenetic illite. Is intruded by Oenpelli Dolerite, commonly at the basal unconformity; also is faulted against Gumarrirnbang Sandstone.|<1818 Ma; >1793 +/- 13 Ma.|Basal unit in Kombolgie Subgroup.||Unconformably overlies Nimbuwah Complex, Tin Camp and Nabarlek Granites, Kudjumarndi Quartzite, Cahill Formation, Nourlangie Schist. Is overlain conformably by Nungbalgarri Volcanics.|Quartz sandstone: white-grey, fine- to coarse-grained, medium- to thickly-bedded, trough and planar cross-bedded; minor siltstone; conglomerate lenses and basal pebble or boulder conglomerate.|14-MAY-18
34024|Mamadawerre Sandstone|68733|6|Mentioned|p186|||Northern McArthur Basin.||Basal unit of the Kombolgie Subgroup.||||
34024|Mamadawerre Sandstone|69420|5|Briefly described|p5:24-25, 67-69, 71-75, 78-80, 84|Paleoproterozoic|Paleoproterozoic|Associated with the Ranger 3 uranium deposit (described in detail) and others.||Kombolgie Subgroup.||Unconformably overlies Nourlangie Schist and Cahill Formation.|Sandstone and conglomerate.|12-JUL-16
34024|Mamadawerre Sandstone|69430|4|Described|p15:3, 7-8, 51-52|||NW McArthur Basin. Sediment source area to the W or SW. Over 176m thick. Distal braided fluvial deposits; aeolian environment at top.||Kombolgie Subgroup.||Unconformably overlies Edith River Group and Nimbuwah Complex. Nonconformably overlies Tin Camp Granite. Is overlain conformably by Nungbalgarri Volcanics.|White to grey, fine- to coarse-grained, medium to thickly bedded sandstone. Trough cross-bedding dominates the lower part of the unit; also planar cross-bedded and minor planar laminated.|12-JUL-16
34024|Mamadawerre Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by Nungbalgarri Volcanics||
34024|Mamadawerre Sandstone|70293|5|Briefly described|p597-599, p612-614||Orosirian|||Kombolgie Subgroup||Unconformably overlies Plum Tree Creek Volcanics, overlain by Nungbalgarri Volcanics.|Sandstone.|24-FEB-17
34024|Mamadawerre Sandstone|70853|5|Briefly described|Map legend.|Statherian|Statherian|||Kombolgie Subgroup.|||Quartz sandstone: white-grey, fine- to coarse-grained, medium- to thickly-bedded, trough and planar cross-bedded; minor siltstone; conglomerate lenses and basal conglomerate.|
34024|Mamadawerre Sandstone|70866|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||Kombolgie Subgroup.||Overlies Geolsec Formation. Is overlain unconformably by Uniya Formation.|Ripple-marked and cross-bedded, very coarse to pebbly quartz sandstone, purple clayey coarse-grained to pebbly sandstone, quartz pebble conglomerate, boulder conglomerate, purple quartz sandstone; lithic greywacke and calcareous siltstone at base.|
34024|Mamadawerre Sandstone|73083|6|Mentioned|p16|||||||||
27964|Manbulloo Limestone Member|23216|6|Mentioned|p38,42|||(Randal, 1963).||||||
27964|Manbulloo Limestone Member|32170|6|Mentioned|Map legend|Early Ordovician|Late Cambrian|Mid.Camb.-L.Ord.||||||
27964|Manbulloo Limestone Member|32700|6|Mentioned|Table 2|||Mention p16. Refers Randal (1962).||||||31-OCT-06
27964|Manbulloo Limestone Member|40136|5|Briefly described|p31|||||||||
27964|Manbulloo Limestone Member|42012|6|Mentioned|p14|||||||||
27964|Manbulloo Limestone Member|44201|14|Not recorded|p.10||Middle Cambrian|Middle Cambrian.||||||31-OCT-06
27964|Manbulloo Limestone Member|45022|5|Briefly described|p.104. Tb.13, Pl.28.|Ordovician|Cambrian|Of Jinduckin Formation.||||||
27964|Manbulloo Limestone Member|45058|6|Mentioned|p19|||Member of Jinduckin Formation.||||||31-OCT-06
27964|Manbulloo Limestone Member|45064|4|Described|Table 1|||||||||
27964|Manbulloo Limestone Member|46679|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
27964|Manbulloo Limestone Member|48942|6|Mentioned|p82|||Correlation.||||||
38423|Manga Mauda Member|23733|2|Defined|p43 App.1|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Approximately ~1000m thick. See also p10 and p4 Tb. 1.||||||07-NOV-08
38423|Manga Mauda Member|23809|5|Briefly described|p27 Fig.25|||Of the Tomkinson Creek Group. Geological Province: Tennant Inlier.||||||
38423|Manga Mauda Member|24303|3|Fully described|p5|Proterozoic|Proterozoic|Of the Hayward Creek Formation. Overlain by the Meerie Member. Max. Thickness: >600m.||||||
38423|Manga Mauda Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hayward Creek Formation. Sandstone; lithic to quartz arenite; lensing or planar, thin to thick bedded; granular to pebbly; laminated; trough or tabular crossbedded, rippled, dessicated; mudstone; silicified.||||||07-NOV-08
38423|Manga Mauda Member|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Overlain by Meerie Member||||||07-NOV-08
38423|Manga Mauda Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Group). Lithic/sublithic/volcanilithic arenite, pebbly arenite; shale and siltstone particularly at the top. Overlies Blanche Creek Member.  In the Tennant Creek region.||||||07-NOV-08
38423|Manga Mauda Member|65209|5|Briefly described|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|Interpreted to be predominantly fluviatile. Geol. Prov: Tomkinson Creek Province.||Hayward Creek Member||Correlates with Unimbra Sandstone.||05-JAN-17
38423|Manga Mauda Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hayward Creek Formation.|||Lithic/sublithic/volcanilithic arenite, pebbly arenite; shale and siltstone particularly at top.|
38423|Manga Mauda Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
38423|Manga Mauda Member|69424|5|Briefly described|p9:5, 26-27|Paleoproterozoic|Paleoproterozoic|Fluviatile sediments.||Hayward Creek Formation.||Is overlain by Meerie Member.||12-JUL-16
38423|Manga Mauda Member|69425|6|Mentioned|p10:12-13|||||Hayward Creek Formation.||Correlated in part with Arabulja and Newlands Volcanics, and Yeeradgi Sandstone.||12-JUL-16
38423|Manga Mauda Member|69431|4|Described|p16:4-5, 7-8|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.600-1000m thick. Predominantly fluviatile deposits, with locally well-developed channels. Lithology at the type section described in some detail.||Hayward Creek Formation.||Variably overlies Brumbreu Formation. Is overlain conformably by Meerie Member. Is correlated with the Unimbra Sandstone, and is a possible lateral equivalent of Yeeradgi Sandstone.|Lithic and sublithic, locally pebble-bearing sandstone and siltstone in a number of fining-upwards cycles; locally includes probable felsic volcanic rocks and tuffs; also immature wacke. Contains weathered mafic dykes and sills.|12-JUL-16
38423|Manga Mauda Member|72379|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
27827|Maningkorrirr Phonolite|9534|5|Briefly described|Map legend|Adelaidean|Adelaidean|Part of a phonolite dyke swarm.||||||
27827|Maningkorrirr Phonolite|9691|5|Briefly described|Map Legend|||Phonolite dyke swarm.||||||02-JUN-05
27827|Maningkorrirr Phonolite|9701|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarm.||||||02-JUN-05
27827|Maningkorrirr Phonolite|9733|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarm.||||||
27827|Maningkorrirr Phonolite|23374|5|Briefly described|p20||Ectasian|Of the Nimbuwah Complex.||||||31-OCT-06
27827|Maningkorrirr Phonolite|33186|6|Mentioned|p293|||||||||
27827|Maningkorrirr Phonolite|36535|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27827|Maningkorrirr Phonolite|36635|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27827|Maningkorrirr Phonolite|37815|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27827|Maningkorrirr Phonolite|39620|5|Briefly described|p9|||||||||
27827|Maningkorrirr Phonolite|43715|6|Mentioned|p28|||||||||
27827|Maningkorrirr 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.||||||06-JUN-07
27827|Maningkorrirr Phonolite|50586|6|Mentioned|p2.1|||Intrudes: Nimbuwah Complex.||||||
27827|Maningkorrirr Phonolite|60550|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Phonolite dyke swarms.||||||
27827|Maningkorrirr Phonolite|63866|6|Mentioned|p117|||||||||
27827|Maningkorrirr Phonolite|67779|5|Briefly described|p8 Table 1.|Mesoproterozoic|Mesoproterozoic|Correlated with Galiwinku Dolerite.|c.1320 Ma.|||||10-SEP-12
27827|Maningkorrirr 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|||||
33647|Mantapayika Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Umutju Granite Suite.  Hornblende and clinopyroxene-bearing granites, typically porphyritic with blue-grey K-feldspars; variably deformed and recrystallised to garnet-bearing assemblages.  Age: ~1180-1120Ma.  Geological Province: Musgrave Block.||||||08-FEB-05
33647|Mantapayika Granite|60683|2|Defined|p55-56 Appendix, p14-16|Mesoproterozoic|Mesoproterozoic|Of the Umutju Granite Suite. Formerly comprised part of Olia Gneiss (Forman 1966a, 1972).  Porphyritic granites and hornblende-garnet gneisses.  Age: 1120+/-9Ma, 1147+/-3Ma (Pb-Pb evap.technique) See also p10 Tb.1.||||||
33647|Mantapayika Granite|61154|5|Briefly described|p12, p44 App.|Mesoproterozoic|Mesoproterozoic|Of the Umutju Suite (Pitjantjatjara Supersuite). Comprises tecturally variable granite and migmatite - primarily clinopyroxene-bearing porphyritic granite and scattered, pale, equigranular to weakly porphyritic hornblende granite. Age:1120+/-9, 1147+/-3Ma||||||
33647|Mantapayika Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Umutju Granite Suite.  Hornblende and clinopyroxene-bearing granites, typically porphyritic with blue-grey feldspars;  variably deformed and recrystallised to garnet-bearing assemblages. . Geological Province: Musgrave Block.||||||19-OCT-05
33647|Mantapayika Granite|69436|5|Briefly described|p21:8|||Fregon Domain, Musgrave Province. Widely scattered outcrops to the N of the Mann Ranges. Contains migmatitic shear zones dating to the Petermann Orogeny. Kober Pb-Pb zircon ages by Scrimgeour et al. (1999).|1147 +/- 3 Ma and 1120 +/- 9 Ma.|Umutju Suite.|||Texturally variable granite and migmatite. Includes clinopyroxene-bearing porphyritic granite and scattered pale, equigranular to weakly porphyritic hornblende granite.|12-JUL-16
33647|Mantapayika Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Metamorphosed at 561 +/- 11 Ma (U-Pb zircon SHRIMP.|1139+/-22 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneiss.|
33647|Mantapayika Granite|73437|6|Mentioned|p152|||K-Ar hornblende metamorphism/cooling age of 565+/-9 Ma from Scrimgeour et al., (1999).|||||Includes migmatic gneiss.|
33648|Mantarurr Granite Suite|24301|6|Mentioned|p37 Appendix 1|||See also Mantarurr Suite p10.||||||
33648|Mantarurr Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Wala Walu, Utanta, Kulu and Foster Cliff Granites.  Age: ~1170Ma.||||||
33648|Mantarurr Granite Suite|60683|2|Defined|p57 Appendix, p18|Mesoproterozoic|Mesoproterozoic|Formerly part of Olia Gneiss and unnamed metamorphosed granites of Forman (1966a, 1972). Comprises Utanta, Wala Wuru, Kulu and Foster Cliff Granites, and unnamed leucogranite. Age: 1186+/-14Ma (SHRIMP zirc), 1165+/-11Ma (sphene).  See also p10 Tb.1, p43.||||||20-APR-05
33648|Mantarurr Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Wala Wuru, Kulu, Utanta and Foster Cliff Granites.  Age: ~1170Ma. Geological Province: Musgrave Block.||||||
33648|Mantarurr Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
25203|Manton Group|24442|6|Mentioned|p43|||Of the Pine Creek Orogen.  Intruded by the Zamu Dolerite.||||||
25203|Manton Group|38884|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25203|Manton Group|39069|5|Briefly described|Table 1|||See also Fig.4.||||||
25203|Manton Group|39320|6|Mentioned|Fig.1|||||||||
25203|Manton Group|40492|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25203|Manton Group|40493|5|Briefly described|Table 1|||Also mention on p21.||||||31-OCT-06
25203|Manton Group|42202|6|Mentioned|Fig.1 P511|||||||||
25203|Manton Group|50623|4|Described|p259 Fig.2, p260 Fig.3|Paleoproterozoic|Paleoproterozoic|Unconformably overlies Rum Jungle Basement. Unconformably overlain by Mount Partridge Group.||||||07-NOV-08
25203|Manton Group|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Overlies Rum Jungle Complex. Overlain by Mount Partidge Group.||||||
25203|Manton Group|61389|5|Briefly described|Map Legend|||||||||
25203|Manton Group|63866|5|Briefly described|p108, p112|||Central Domain, Pine Creek Orogen. ||||Equivalent to the Namoona Group.||
25203|Manton Group|64698|5|Briefly described|lithinterp table|Orosirian|Paleoproterozoic|Includes Beestons Formation, Celia Dolostone.||||||07-JAN-09
25203|Manton Group|64730|5|Briefly described|p124, 125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age is of maximum deposition (SHRIMP zircon).|2506 +/- 14 Ma (Cross et al. 2005).||Includes Celia Dolostone and Beestons Formation.|Unconformably underlies Mount Partridge Group.||02-MAY-12
25203|Manton Group|64956|5|Briefly described|p72|||Unconformably overlain by Mount Partridge Group.||||||07-FEB-11
25203|Manton Group|65232|5|Briefly described|p51, p7|Palaeoproterozoic|Palaeoproterozoic|Includes Beestons Formation and Celia Dolostone. Unconformable under Mount Partridge Group. Unconformable over Rum Jungle Complex.||||||09-FEB-10
25203|Manton Group|65339|5|Briefly described|p5 Fig.4, p7. |||Western equivalent of Namoona Group. Contains oldest Paleoproterozoic sedimentary rocks in Pine Creek Orogen.|||Includes basal Beestons Formation and Celia Dolostone.|Unconformably overlies Rum Jungle Complex.|Sandstone, dolostone, magnesite.|
25203|Manton Group|66683|6|Mentioned|p368.|Paleoproterozoic|Paleoproterozoic|Correlative of Kudjumarndi Quartzite and Mount Basedow Gneiss.||Unit in Woodcutters Supergroup.||||
25203|Manton Group|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Woodcutters Supergroup.|Includes Beestons Formation and Celia Dolostone.|||23-NOV-11
25203|Manton Group|67355|6|Mentioned|p6-7, p10, p47 Fig. 38||Neoarchean|||Woodcutters Supergroup|Celia Dolostone, Beestons Formation.|Correlative to Namoona Group.|Sedimentary rocks.|25-JAN-17
25203|Manton Group|67564|6|Mentioned|p11.|Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen.|||Includes Beestons Formation.|||
25203|Manton Group|67779|5|Briefly described|p6 Fig.5, p16.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|<2506 +/- 14 Ma (Cross et al. 2005).|Lower unit in Woodcutters Supergroup.|Includes Beestons Formation and Celia Dolostone.|Unconformably overlies the Rum Jungle Complex.||
25203|Manton Group|69419|6|Mentioned|p4:3-4|||W. Pine Creek Orogen.||||||12-JUL-16
25203|Manton Group|69420|5|Briefly described|p5:2, 4, 6, 8-10, 15-16, 24, 116|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Mainly fluvial to shallow-marine deposits. Sediment derived from Archean basement highs. Similar (detrital zircon) provenance with Kakadu and Mount Partridge Groups.||Woodcutters Supergroup.|Beestons Formation, Celia Dolostone.|Unconformably overlies Rum Jungle Complex. Is overlain unconformably by Mount Partridge Group.||12-JUL-16
25203|Manton Group|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. The undivided unit (under cover) and its constituents are mapped separately.||Woodcutters Supergroup.|Includes Celia Dolostone, Beestons Formation.|Unconformably overlies Rum Jungle Complex. Is overlain unconformably by Mount Partridge Group.||01-MAR-18
23762|Mantungula Formation|22538|6|Mentioned|Fig3 P708|||||||||
23762|Mantungula Formation|22600|4|Described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
23762|Mantungula Formation|22853|4|Described|26|Proterozoic|Proterozoic|Of the Roper Group.||||||31-OCT-06
23762|Mantungula Formation|23404|5|Briefly described|p639 Fig.2|||Of Roper Group.||||||
23762|Mantungula Formation|23776|5|Briefly described|p705 Fig 2.|||Of Roper Group||||||
23762|Mantungula Formation|23937|2|Defined|p85 App. 1, p28, p26 Fig. 12|Calymmian|Calymmian|Of Collara Subgp (Roper Gp).  Previously inc. in Limmen Sst; known as Wilberforce beds in Arnhem Land (Dunnet, 1965). Overlain by Limmen Sst (erosive contact); conformably overlies Phelp Sst. Age: ~1500Ma.  Max. thick: 170m.  Geol.Prov: McArthur Basin.||||||31-OCT-06
23762|Mantungula Formation|24049|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: fine-grained, thin to very thin-bedded, micaceous, wave rippled interbedded with mudstone: grey-green to black. Geol. Prov: McArthur Basin.||||||13-OCT-05
23762|Mantungula Formation|24050|6|Mentioned|p42|||||||||
23762|Mantungula Formation|24303|5|Briefly described|p60 Appendix|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Geological Province: McAthur Basin. Correlative of lower part of Sweetwater Member (Baralandji Formation). See also p24 Tb.4||||||
23762|Mantungula Formation|40691|6|Mentioned|Fig.7|||||||||
23762|Mantungula Formation|41268|5|Briefly described|Fig.4|||Mention p290.||||||31-OCT-06
23762|Mantungula Formation|41531|6|Mentioned|p167|||||||||
23762|Mantungula Formation|42385|5|Briefly described|p26|||See also Table 5 p25.||||||31-OCT-06
23762|Mantungula Formation|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Lower Roper Group (Roper Group).||Not shown in schematic sections.|Basal conglomerate/breccia, brecciated mudstone and siltstone, glauconitic sandstone. Micaceous mudstone and siltstone. Detailed lithology given.|09-NOV-11
23762|Mantungula Formation|42639|4|Described|p37, Table 7 p39|||||||||
23762|Mantungula Formation|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
23762|Mantungula Formation|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Lower Roper Group. Red-brown micaceous and rarely glauconitic mudstone and fine grained sandstone.||||||19-OCT-05
23762|Mantungula Formation|42812|3|Fully described|p45, Table 5|||Of the Roper Group.||||||19-DEC-06
23762|Mantungula Formation|43036|4|Described|p57|||Of Roper Group.||||||31-OCT-06
23762|Mantungula Formation|44112|3|Fully described|Table12p68,69|||||||||
23762|Mantungula Formation|60483|5|Briefly described|p7 Fig. 5, p32|||Of the Roper Group. Geological Province: McArthur Basin.||||||05-OCT-07
23762|Mantungula Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Roper Group. Overlain by Limmen Sandstone.||||||03-JUN-09
23762|Mantungula Formation|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Grey, green and red, laminated mudstone; fine-grained sandstone and dolostone; minor siltstone. Overlies Phelp Sandstone; underlies Limmen Sandstone.||||||22-FEB-05
23762|Mantungula Formation|60574|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group. Overlain by the Limmen Sandstone. Consists of micaceous siltstone.||||||
23762|Mantungula Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Mudstone: green, gray and red, laminated; fine-grained sandstone and dolostone; minor siltstone.||||||
23762|Mantungula Formation|61403|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of Roper Group. Sandstone: fine-grained, thin to very thin-bedded, micaceous, wave rippled interbedded with mudstone: grey-green to black. Geol. Prov: McArthur Basin.||||||
23762|Mantungula Formation|62376|6|Mentioned|p38|||Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
23762|Mantungula Formation|64815|6|Mentioned|p5 Fig.3, p17  |||||Of the Roper Group.||||
23762|Mantungula Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Roper Group.||||
23762|Mantungula Formation|65228|6|Mentioned|Fig.02.|||||Unit in Roper Group.||Is overlain by Limmen Sandstone.||
23762|Mantungula Formation|65236|6|Mentioned|p3 Fig. 3|||Geological province: Beetaloo Sub-basin.||||||04-JUN-09
23762|Mantungula Formation|65340|5|Briefly described|p61.|Mesoproterozoic|Mesoproterozoic|Poorly exposed, recessive unit.||Unit in Roper Group.||Unconformably overlies Karns Dolomite. Is overlain by Limmen Sandstone.|Tabular red/brown ferruginous, micaceous, dolomitic siltstone and fine sandstone with parallel laminations and ripples.|
23762|Mantungula Formation|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 85 m.||Unit in Roper Group.||Overlies Nathan Group. Is overlain by Limmen Sandstone.|Mudstone, fine sandstone, dolostone.|
23762|Mantungula Formation|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
23762|Mantungula Formation|69430|4|Described|p15:3, 26-27, 30|Calymmian|Calymmian|NE McArthur Basin. <100-150m thick. Storm-dominated marine shelf sediments.||Basal Collara Subgroup.||Conformably overlies Phelp Sandstone. Is overlain ?disconformably by Limmen Sandstone (erosive contact).|A recessive unit of mudstone and siltstone, with a local basal conglomerate.|12-JUL-16
23762|Mantungula Formation|69673|6|Mentioned|p16 fig 13|||Northeastern and Southern McArthur Basin.||Collara Subgroup||Unconformably overlies Walmudga Formation, Dungaminnine Formation, , Overlain by Limmen Sandstone||
23762|Mantungula Formation|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Storm-dominated shelf (mudstone-dominated), pedogenic mudstone.||Of Collara Subgroup.||Overlies Phelp Sandstone. Overlain by Limmen Sandstone.||
23762|Mantungula Formation|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlies Phelp Sandstone; overlain by Limmen Sandstone.|Interbedded mudstone, siltstone and fine sandstone.|
23762|Mantungula Formation|70897|5|Briefly described|p43, Fig.1.7.6,9|Mesoproterozoic|Mesoproterozoic|||Basal Roper Group.||Is overlain conformably by Limmen Sandstone.|A thin siltstone-mudstone unit.|
23762|Mantungula Formation|70968|3|Fully described|p6-8,p10-14,p126,p131,p138-140,p143-144|Calymmian|Calymmian|Sweet in Abbott et al. (2001) after Sweet and Jackson (1986). Previously included in Limmen Sandstone by Paine (1963), Dunn (1963), Plumb and Paine (1964); called the Wilberforce beds by Dunnet (1965). Named after Mantungula Creek. Represents basal Roper Group locally. Poor, weathered exposures: type section is thus a complete section (102m thick) of the Formation (273.15m to 170.6m depth) in DDH BHP McA-6 at 558100mE 8228900mN. An incomplete reference section is described. The red beds at the top resemble those in overlying Nullawun Member.||Roper Group.||Overlies Phelp Sandstone conformably or Nathan Group unconformably. Is overlain by Limmen Sandstone, probably conformably.|The type section: a 48m succession of thinly interlaminated glauconitic sandstone and micaceous siltstone and shale, under 39m of mudstone/siltstone breccia interbedded with mudstone and limestone beds; then laminated shale, siltstone, red beds.|
23762|Mantungula Formation|71059|5|Briefly described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. <100 - 174m thick. Storm-dominated marine shelf deposits; possibly continental floodplain at top.||Collara Subgroup.||Conformably overlies Phelp Sandstone. Is overlain conformably by Limmen Sandstone.|Mudrocks; fine sandstone.|
23762|Mantungula Formation|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlies the Phelp Sandstone. Overlain by the Limmen Sandstone.||
23762|Mantungula Formation|71494|6|Mentioned|p4, p8, p17, p22-p23|||||||Contact with overlying Limmen Sandstone is erosive.||03-MAY-18
23762|Mantungula Formation|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Collara Subgroup||||24-SEP-18
23762|Mantungula Formation|71893|5|Briefly described|p5, p8|||McArthur Basin.||Collara Subgroup||Conformably overlies the Phelp Sandstone.||
23762|Mantungula Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone. Minimum age from Mainoru Formation, higher in Collara Subgroup.||Collara Subgroup||Underlies Limmen Sandstone. Unconformably overlies Nathan Group.||
23762|Mantungula Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Collara Subgroup, Roper Group||Partly underlain by Phelp Sandstone. Overlain by Limmen Sandstone.||
23762|Mantungula Formation|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Collara Subgroup||Unconformably overlies Dungaminnie Formation, Balbirini Dolostone, Walmudga Formation. Overlain by Limmen Sandstone.||
23762|Mantungula Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Collara Subgroup, Roper Group||Unconformably underlain by Walmudga Formation. Partly overlain by Limmen Sandstone.||
23762|Mantungula Formation|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Phelp Sandstone. Overlain by Limmen Sandstone.|Includes interbedded mudstone and fine sandstone with mudstone and shale.|
23762|Mantungula Formation|73412|5|Briefly described|p4, 8, 11|||Southern McArthur Basin.||Collara Subgroup.||Unconformably overlies upper Balbirini Dolostone (Nathan Group). Is overlain by Mainoru Formation.||
27478|Mapata Gneiss|33103|4|Described|Table 1|||Mention p3.||||||31-OCT-06
27478|Mapata Gneiss|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
27478|Mapata Gneiss|39887|6|Mentioned|Fig.5|||||||||
27478|Mapata Gneiss|40906|6|Mentioned|p8|||||||||
27478|Mapata Gneiss|50369|6|Mentioned|p15.2|||Intruded by Mount Swan Granite.||||||31-OCT-06
27478|Mapata Gneiss|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartzofeldspathic gneiss, biotite schist, minor amphibolite. Geological Province: Arunta Region.||||||07-NOV-08
27478|Mapata Gneiss|65341|5|Briefly described|p3, p4, p20.|||Metamorphosed to middle to upper amphibolite facies.||Unit in Strangways Metamorphic Complex.||In sheared contact with Delny Metamorphics.|Quartzofeldspathic gneiss, biotite schist; minor amphibolite.|
27478|Mapata Gneiss|69383|5|Briefly described|p65, 80-81|||Arunta region, Aileron Province. LA-ICPMS U-Pb and Hf geochronology analyses on sample GA 2003082021 gave detrital zircon data but no primary crystallisation age. ||||A lower grade equivalent of the Kanandra Granulite.|Interbedded quartz-biotite pelitic schist and metapsammitic rock intruded by numerous equigranular quartz-feldspar-biotite gneissic granite bodies, inferred to be in situ partial melts of the host metasedimentary rocks.|
27478|Mapata Gneiss|69427|5|Briefly described|p12:12-13|||Occurs N of the Delny Shear Zone, Aileron Province. Suggested to be a lower-grade equivalent of the Kanandra Granulite, with less mafic rock.||Strangways Metamorphic Complex.|||Mainly biotite-quartz-feldspar migmatite with ptygmatically folded leucosomes; minor biotite schist, muscovite schist and amphibolite.|12-JUL-16
76086|Mara Dolostone Member|64815|6|Mentioned|p4 Fig.2, p14 Tb.5 |||Called Dolomite in Tb.5.||Unit in Emmerugga Dolostone.||||
76086|Mara Dolostone Member|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming.||Unit in Emmerugga Dolostone.||Is overlain by Mitchell Yard Dolostone Member.|Dololutite, stromatolitic dololutite, dolomitic siltstone, dolarenite and dolomitic breccia; columnar, domical and conical stromatolites, commonly forming bioherm series; common halite casts and quartz nodules after evaporites.|
76086|Mara Dolostone Member|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. Over 220 m thick. Shallow lagoon and saline lacustrine.||Emmerugga Dolostone||Overlies Myrtle Shale conformably. Underlies Mitchell Yard Dolostone Member.|Dolomudstone, dolostone, dolomitic breccia, sandstone, siltstone.|
76086|Mara Dolostone Member|69430|4|Described|p15:3, 16-17, 34-35, 39-42, 48, 57|Statherian|Statherian|Southern McArthur Basin. Ridge-forming. Shallow-marine, peritidal and flanking carbonate sabkha deposits. Is shown as Mara Dolostone on 15:34-35. Hosts various base metal (Cu-Pb-Zn) deposits (described).||Emmerugga Dolostone.||Conformably and gradationally overlies Myrtle Shale. Is overlain conformably by Mitchell Yard Dolostone Member or Teena Dolostone.|Dololutite, stromatolitic dololutite, dolomitic sandstone, dolarenite and dolomitic breccia; columnar, domal and conical stromatolites, often forming bioherm series; common halite casts and quartz nodules after evaporites.|12-JUL-16
76086|Mara Dolostone Member|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Emmerugga Dolostone||||
76086|Mara Dolostone Member|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the southern part of the Batten Fault Zone.||Emmerugga Dolostone||Overlies Myrtle Shale and underlies Mitchell Yard Member.||
76086|Mara Dolostone Member|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone (south).||Emmerugga Dolostone?, Umbolooga Sub-group, McArthur Group||Underlain by Myrtle Shale. Overlaing by Mitchell Yard Member.||
76086|Mara Dolostone Member|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the South part of the Batten Fault Zone of the Southern McArthur Basin.||Emmerugga Dolostone, Batten Subgroup||Overlies Myrtle Shale, and underlies Mitchell Yard Member.||
76086|Mara Dolostone Member|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Emmerugga Dolostone, Batten Subgroup, McArthur Group||Underlain by Myrtle Shale. Overlain by Mitchell Yard Member.||
26721|Maranboy Porphyry|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Pinkish green-grey medium-grained feldspar-quartz porphyry, strongly porphyritic hornblende granite.||||||
26721|Maranboy Porphyry|23216|5|Briefly described|Table1p10,15,49|||||||||
26721|Maranboy Porphyry|23733|5|Briefly described|p32 Fig. 19|||||||||
26721|Maranboy Porphyry|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26721|Maranboy Porphyry|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
26721|Maranboy Porphyry|43187|5|Briefly described|p2|||||||||
26721|Maranboy Porphyry|69420|5|Briefly described|p5:105|||Pine Creek Orogen. Associated with the Tollis Formation-hosted Sn deposit in the Maranboy tinfield.||||Intrudes Tollis Formation.||12-JUL-16
26014|Margery Formation|14019|3|Fully described|p7|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Dolostone, doite, dololutite, siltstone, sandstone, claystone. Disconformable on Stirling Sandstone; conformably overlain by Pear Tree Dolostone. Max. thickness: 125m. Geological Province: Birrindudu Basin.||||||07-NOV-08
26014|Margery Formation|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
26014|Margery Formation|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
26014|Margery Formation|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Stirling Sandstone;  overlain by Pear Tree Dolostone. Geological Province: Birrindudu Basin.||||||08-AUG-05
26014|Margery Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
26014|Margery Formation|28255|3|Fully described|p14, Tb. 11 (opp. p8)|||Of Limbunya Gp. Comprises upper chert horizon, central claystone horizon and lower chert horizon. Unconformable on Stirling Sst; conformable below chert of  Antrim Plateau Volcs; probably conformable below Pear Tree Fm.Max.thick: >120m. See also p117 App.||||||
26014|Margery Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
26014|Margery Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Limbunya Group.  Siltstone and claystone, minor dolomite, chert at top and base.  Conformably overlies the Stirling Sandstone; conformably overlain by the Pear Tree Dolomite.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
26014|Margery Formation|32660|5|Briefly described|Table 6|||||||||
26014|Margery Formation|33375|6|Mentioned|p9 Tb. 1|||Of the Limbunya Group. Chert and claystone. Age is Carpentarian or Adelaidean.||||||26-APR-05
26014|Margery Formation|33376|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26014|Margery Formation|33378|5|Briefly described|Map legend|||Of the Limbunya Group.  Age is Carpentarian or Adelaidean.||||||28-APR-05
26014|Margery Formation|45112|5|Briefly described|Table 7|||||||||
26014|Margery Formation|48943|2|Defined|p18|Proterozoic|Proterozoic|Strat. section p129.||||||02-NOV-06
26014|Margery Formation|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Stromatolitic dolostone, claystone, dolarenite, dololutite, stromatolitic chert, dolomitic sandstone and siltstone.  Conformably overlies Stirling Sandstone; conformably overlain by Pear Tree Formation.  Geol. Prov. Birindudu Basin||||||07-NOV-08
26014|Margery Formation|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
26014|Margery Formation|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Stirling Sandstone. Is overlain by Pear Tree Dolostone.||
26014|Margery Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Stirling Sandstone. Is overlain by Pear Tree Dolostone.|Stromatolitic dolostone, claystone, dolarenite, dololutite, stromatolitic chert, dolomitic sandstone and siltstone (section only).|
26014|Margery Formation|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
26014|Margery Formation|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
26014|Margery Formation|69432|5|Briefly described|p17:2, 6-7|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 125m thick. Shallow-marine to intertidal deposits with localised evaporitic conditions and emergence.||Limbunya Group.|||Basal red oxidised claystone overlain by fine-grained sandstone, biohermal stromatolitic dolostone and chert, and dolomitic sandstone and mudstone. Cauliflower chert, scour-and-fill, flake breccia, mudcracks and dewatering structures are common.|12-JUL-16
26014|Margery Formation|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Stirling Sandstone, overlain by Pear Tree Dolostone||
26014|Margery Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin. Section only.||Limbunya Group||Overlies Stirling Sandstone. Is overlain by Pear Tree Dolostone.|Stromatolitic dolostone, claystone, dolarenite, dololutite, stromatolitic chert, dolomitic sandstone and siltstone.|
26014|Margery Formation|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin.||Limbunya Group.|||Stromatolitic dolostone, claystone, dolarenite, dololutite, stromatolitic chert, dolomitic sandstone and siltstone, sublithic quartz sandstone, quartz sandstone, mudstone, nodular chert.|
26014|Margery Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolostone|
26014|Margery Formation|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Pear Tree Dolostone. Underlain by Stirling Sandstone.||
26014|Margery Formation|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Stirling Sandstone. Overlain by Pear Tree Dolostone.||
26014|Margery Formation|73083|6|Mentioned|p31|||||||||
26014|Margery Formation|73280|6|Mentioned|p1, p4-5, App.1A|||Birrindudu Basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||||||
33183|Marlgowa Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
33183|Marlgowa Sandstone|23374|2|Defined|Tb2p10,16,43,12,9,14,15,17,18,27,32||Statherian|No type section possible, but lower and upper boundary stratotypes given. Upper portion laterally equivalent to at least part of McKay Sandstone. of Kombolgie Subgroup, Katherine River Group, McArthur Basin.||||||
33183|Marlgowa Sandstone|23384|5|Briefly described|Fig 27|||||||||
33183|Marlgowa Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Kombolgie Subgroup (Katherine River Group).||||||
33183|Marlgowa Sandstone|23867|3|Fully described|p6|Paleoproterozoic|Paleoproterozoic|Of Kombolgie Subgroup.  Overlies Gumarrirnbang Sandstone.  Max. thickness: 420m.  Geological Province: McArthur Basin.  See also Table 1 and Figs.3 and 30.||||||07-NOV-08
33183|Marlgowa Sandstone|24050|3|Fully described|p15, p10|||Of the Kombolgie Subgroup.  Fine- to very coarse-grained and pebbly quartz sandstone.||||||02-NOV-06
33183|Marlgowa Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Kombolgie Subgroup, Katherine River Group. Geological Province: McArthur Basin.||||||
33183|Marlgowa Sandstone|50545|5|Briefly described|p114 Fig.1||Paleoproterozoic|Of Kombolgie Subgroup.||||||07-NOV-08
33183|Marlgowa Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Sandstone: white/grey, fine-grained to granular, thick- to very thick-bedded, dominantly trough cross-bedded, planar cross-bedded, quartz arenite. Geological Province: McArthur Basin.||||||30-NOV-04
33183|Marlgowa Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Kombolgie Subgroup (Katherine River Group). Well-sorted medium quartz sandstone with minor pebbly beds.  Geol.Prov: McArthur Basin. Overlies: Gurmarrimbang Sandstone. Underlies: McKay Sandstone.||||||14-JAN-05
33183|Marlgowa Sandstone|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1740-1780Ma. McArthur Basin. Of Katherine River Group. Max thick 410m. Med to thick bedded, trough cross-bedded, well sorted qtz sandst with minor pebbly beds; laminated and wave-rippled, interbedded with low-angle cross-bedded, qtz sandst.||||||07-JAN-09
33183|Marlgowa Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Kombolgie Subgroup.||||
33183|Marlgowa Sandstone|65232|5|Briefly described|p7 Fig. 6, App. 2|||Of Kombolgie Subgroup (Katherine River Group). Overlies Gilruth Volcanic Member; underlies Mackay Sandstone [McKay Sandstone].Thickness 360-410m.||||||09-FEB-10
33183|Marlgowa Sandstone|67057|6|Mentioned|p455.|||||Unit in Kombolgie Subgroup.||Overlies Gilruth Volcanics. Is overlain by McKay Sandstone.||
33183|Marlgowa Sandstone|67564|4|Described|p2, p6 Table 2, p10 Fig.5, p39, p43.|Proterozoic|Proterozoic|McArthur Basin. Forms spectacularly eroded joint-bounded masses of white quartz sandstone. Up to 410 m of shallow marine (upper portion) and braided fluviatile (lower portion) sediments; includes a thin interval of probably aeolian sandstone.||Unit in Kombolgie Subgroup.||Overlies Gumarrirnbang Sandstone. Is overlain by McKay Sandstone.|Well-sorted, thickly bedded, trough crossbedded, medium-grained quartz sandstone with minor pebbly beds; under alternating laminated and wave-rippled quartz sandstone with crossbedding; dolerite sills.|
33183|Marlgowa Sandstone|67779|5|Briefly described|p6 Fig.5, p8 Table 1, p38.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Up to 400 m thick. Lower part is distal braided fluvial environment; upper part is shallow tidal marine.||Topmost unit in Kombolgie Subgroup in the Howship/Oenpelli area?.||Overlies Gilruth Volcanic Member disconformably and Gumarrirnbang Sandstone.|Quartz sandstone: white-grey, fine-grained to granular, thickly bedded to very thickly bedded, dominantly trough cross-bedded, planar cross-bedded; minor siltstone and pebble conglomerate.|14-MAY-18
33183|Marlgowa Sandstone|69420|5|Briefly described|p5:67|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Katherine River Group.||||12-JUL-16
33183|Marlgowa Sandstone|69430|4|Described|p15:3, 7-8|||NW McArthur Basin. 360m thick. Braided fluvial and shallow tidal marine deposits.||Kombolgie Subgroup.||Overlies Gumarrirnbang Sandstone probably conformably. Is overlain conformably by McKay Sandstone and Cottee Formation. Is intruded by Oenpelli Dolerite.|White-grey, medium-grained to granular, thickly to very thickly bedded quartz sandstone, with some coarse-grained to pebbly bands and interbeds of ferruginous sandstone.|12-JUL-16
33183|Marlgowa Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Kombolgie Subgroup||Overlain by McKay Sandstone, overlies Gilruth Volcanic Member, Henwood Creek Volcanic Member||
76874|Marligur Formation|67564|6|Mentioned|p52.|Cretaceous|Cretaceous|Money Shoal Basin.||||||
76874|Marligur Formation|69456|5|Briefly described|p40:2; 40:3 Fig.40.4; 40:4, 6-8|Cretaceous|Cretaceous|Mory (1988); formerly the Marligur Member of Hughes and Senior (1974). Money Shoal Basin. Up to 62m thick. Exposures are generally poor, deeply weathered and only a few metres thick. In many areas, is capped by surficial ferricrete above a mottled zone.||Bathurst Island Group.||Lateral equivalent of (and interfingers with) Darwin Formation.|Medium- to coarse-grained, poorly consolidated quartz sandstone, clayey sandstone and sandy claystone; thin basal quartzic conglomerate.|12-JUL-16
76874|Marligur Formation|69673|6|Mentioned|p204|Cretaceous|Cretaceous|20-63m thick.||Bathurst Island Group||Equivalent to Darwin Formation|Quartz sandstone, clayey sandstone and sandy claystone.|
76874|Marligur Formation|73083|6|Mentioned|p17|Cretaceous|Cretaceous|Money Shoal Basin.||||||
80345|Mascotte Orthogneiss|71621|5|Briefly described|iii, p1, p21-p23, p26, 38, 39, 45, 47|Statherian|Statherian|Aileron Province. SHRIMP age is interpreted as the age of magmatic crystallisation. Petrography and zircon description discussed.|1788.5 +/- 3.1 Ma (SHRIMP U-Pb)|||Intruded by the Thring Granite, Cappocks Granodiorite. Conformably interlayered with White Violet Orthogniess, Kings Legend Metadolerite, Bonya Metamorphics.|Orthogneiss.|01-FEB-19
80345|Mascotte Orthogneiss|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1789 +/- 3 Ma (U-Pb zircon)||||Biotite granitic gneiss: fine to medium-grained, equigranular, fresh to moderately weathered, massive to foliated to gneissic with discontinuous banding.|
80345|Mascotte Orthogneiss|72516|2|Defined|p14-17, p21, p24, p29, p32-35, p205|Statherian|Statherian|Type locality occurs in Bonya Hills at 609429mE 7487049mN. Originally named for Mount Mascotte in eastern Jinka. Bonya Domain and isolated outcrops in the Jinka Domain. Generally poorly exposed, occuring as low, blocky outcrops or jointed pavements. Weathering is described. Previously the Mascotte Gneiss Complex of Shaw et al (1985) the name became obsolete as the constituent lithologies have been separated based on dominant lithology and redefined as the Mascotte Orthogneiss, White Violet Orthogneiss and Thring Granite.  Interlayered with the White Violet Orthogneiss and Kings Legend Metadolerite. Geochemistry is detailed. Interpreted to be comagmatic and cogenetic with the Casper Suite and the Foster Suite. Broadly similar ICE patterns and degree of LREE-enrichment to the Fosters Suite.Regional aspects, extent, geomorphology, structure, metamorphism, alteration, mineralisation, geophysics and geochemistry are discussed. See also  p42, p56, p60-61, p71, p75, p97, p101-104, 120-122, p126-127, p135, p142-143, p145, p149, p169, p171, p189, p192.|1789+/- 3 Ma (SHRIMP U-Pb; Kositcin et al, 2011)|Baikal Supersuite||Intruded by the Cappocks Granodiorite, Samarkand Pegmatite, Thring Granite and Jericho Granite. Intrudes the Bonya Metamorphics.|Biotite granitic gneiss: fine- to medium-grained, equigranular, locally occurring allanite, rare hornblende; fresh to moderately weathered; massive to foliated to gneiss with discontinuous mm-cm scale banding.|21-APR-22
80345|Mascotte Orthogneiss|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes orthogneiss.|
80345|Mascotte Orthogneiss|73123|6|Mentioned|p13|||||Molyhil Suite||||
80345|Mascotte Orthogneiss|73591|6|Mentioned|p11, p16, p18|||||Molyhil Suite||||
25730|Masterton Sandstone|14019|5|Briefly described|p6|||Of the McArthur Group.  Contains evaporites and is overlain by an evaporitic carbonate unit.  Geological Province: McArthur Basin.  Correlated with the Stirling Sandstone (Birrindudu Group) in the Birrindudu Basin.||||||
25730|Masterton Sandstone|22538|5|Briefly described|p709, App1 p722, 723|||Sandstone unit at the base of the McArthur Group retains this name. Older sandstone exposed widely on Wearyan Shelf is herein renamed Echo Sandstone and sst in NE Tanumbirini sheet area is now Burash Sandstone..||||||05-APR-18
25730|Masterton Sandstone|22664|5|Briefly described|Fig. 2 p34|||Of the Umbolooga Subgroup (McArthur Group).||||||02-NOV-06
25730|Masterton Sandstone|22670|6|Mentioned|52,53|||Geol province McArthur Basin||||||
25730|Masterton Sandstone|22853|3|Fully described|14|Proterozoic|Proterozoic|Of the Umbolooga Subgroup. Max thickness: 600 m. Overlain by Mallapunyah Formation; underlain by Tawallah Group.||||||18-SEP-07
25730|Masterton Sandstone|23065|5|Briefly described|16|||Geol province McArthur Basin.||||||02-NOV-06
25730|Masterton Sandstone|23387|6|Mentioned|p18 fig.19|||Of Umbolooga Subgroup.||||||
25730|Masterton Sandstone|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||02-NOV-06
25730|Masterton Sandstone|23397|5|Briefly described|p463|||Of McArthur Group.||||||02-NOV-06
25730|Masterton Sandstone|23398|5|Briefly described|p440|||Of McArthur Group.||||||02-NOV-06
25730|Masterton Sandstone|23776|5|Briefly described|p705 Fig 2|||Of Umbolooga Subgroup.||||||
25730|Masterton Sandstone|23902|4|Described|p1568 Fig.2|||Of the Umbolooga Subgroup. Overlain by the Mallapunyah Formation. Geological Province: McArthur Basin||||||
25730|Masterton Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
25730|Masterton Sandstone|23963|4|Described|p1238, 1239 Fig.2|||Geological Province: McArthur Basin. Basal unit of the McArthur Group. Disconformably overlies the Wollogorang Formation. Overlain by the Mallapunyah Formation.||||||10-MAR-05
25730|Masterton Sandstone|24048|5|Briefly described|p38|||Geological Province: McArthur Basin.||||||
25730|Masterton Sandstone|26310|6|Mentioned|p8|||||||||
25730|Masterton Sandstone|32519|6|Mentioned|p343|||Re age||||||
25730|Masterton Sandstone|32904|6|Mentioned|p91|||Refs. Orridge & Mason 1975||||||
25730|Masterton Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25730|Masterton Sandstone|40259|6|Mentioned|Table 1|||||||||
25730|Masterton Sandstone|40691|5|Briefly described|p13|||Mention p84.||||||02-NOV-06
25730|Masterton Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
25730|Masterton Sandstone|41268|5|Briefly described|Fig.3|||||||||
25730|Masterton Sandstone|41277|6|Mentioned|Fig.2|||||||||
25730|Masterton Sandstone|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
25730|Masterton Sandstone|41721|3|Fully described|p26|||Of McArthur Group. Overlies Gold Creek Volcanics, Hobblechain Rhyolite and Wollogorong Formation, where the latter two are not developed. Max. thickness: 650m+. Geol.prov: McArthur Basin.Sandstone, minor conglomerate - lower marine and upper fluvial unit.||||||01-AUG-07
25730|Masterton Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
25730|Masterton Sandstone|42385|4|Described|p14, p8 Fig. 5|||Basal unit of Umbolooga Subgp (McArthur Gp). Max. thick: 650m. Unconformable on several Tawallah Group units; unconformable below Mallapunyah Fm. Quartzarenite, fine- to med.gr., moderately sorted; very fine-gr. sandstone and siltsto See also Table 4 p17.||||||18-SEP-07
25730|Masterton Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
25730|Masterton Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Umbolooga Subgroup (McArthur Group).||In schematic section, underlies Mallapunyah Formation; overlies undifferentiated Tawallah Group units.|Quartzarenite, sandstone and siltstone, basal sandstone conglomerate common. Detailed lithology given.|09-NOV-11
25730|Masterton Sandstone|42639|4|Described|p19, Table 5 p21|||||||||
25730|Masterton Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
25730|Masterton Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Umbolooga Subgroup. Quartzarenite, white to pink, fine to medium grained, well sorted; minor intervals of sandstone and mudstone.||||||19-OCT-05
25730|Masterton Sandstone|42812|3|Fully described|p29, Table 4|||Of the Umbolooga Subgroup.||||||02-NOV-06
25730|Masterton Sandstone|42873|5|Briefly described|Fig.1, P110|||||||||
25730|Masterton Sandstone|42935|6|Mentioned|p529 Fig.2|||of Umbolooga Subgroup||||||
25730|Masterton Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|of "Mid Proterozoic" age.||||||
25730|Masterton Sandstone|43036|3|Fully described|p39|||Of the Umbolooga Subgroup (McArthur group).||||||18-SEP-07
25730|Masterton Sandstone|44112|6|Mentioned|p55,58|||||||||
25730|Masterton Sandstone|44459|14|Not recorded|p.6|||(E53-2). Includes Tanumbirini Volcanic Member.||||||
25730|Masterton Sandstone|45162|1|Redefined|p45|Proterozoic|Proterozoic|To replace "Masterton Formation".||||||02-NOV-06
25730|Masterton Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Umbolooga Subgroup. Overlian by Mallapunyah Formation.||||||03-JUN-09
25730|Masterton Sandstone|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Masterton Sst.||||||
25730|Masterton Sandstone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1670-1655 Ma.|Unit in Gun Supersequence.||||
25730|Masterton Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p14, p18  |||Mainly siliciclastic. Presented in Fig.2 as part of Tawallah Group, but in Fig.3 as part of McArthur Group.[Currently (2014) in Umbolooga Subgroup of McArthur Group].||||||
25730|Masterton Sandstone|64817|6|Mentioned|p353 Fig.4 |||||Of the Umbolooga Subgroup.||||
25730|Masterton Sandstone|65228|4|Described|p7, pp23-25, Table 1, Figs.02, 11-12|||McArthur Basin. Type section at Archies Creek, McArthur River Region, includes an erosion surface representing probably 25 My of missing rock record. Defined by Jackson et al. (1987) as the base of McArthur Group. Formally revised by Rawlings (1999) into two components: lower part is now Echo Sandstone and part of the Big Supersequence of Calvert Superbasin; upper part stays as Masterton Sandstone, the base of the Gun Supersequence in the Isa Superbasin. Gamma ray log, lithology and facies detailed. Measured section.||Unit in Umbolooga Subgroup.||Is overlain conformably by Mallapunyah Formation.|Prominently outcropping reddish-brown sandstone.|
25730|Masterton Sandstone|65340|5|Briefly described|p47, p79.|||Formerly (Jackson et al. 1987; Ahmad and Wygralak 1989) included outcrops on Wearyan Shelf; since this unit is recognised only in Batten Fault Zone, those outcrops were assigned to a new formation (Echo Sandstone) by Rawlings (1999).||Unit in McArthur Group.||Unconformably overlies Warramana Sandstone and other Tawallah Group units.||
25730|Masterton Sandstone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming. The very fine-grained sandstone and siltstone form recessive units.||Unit in Umbolooga Subgroup.||Is overlain by Mallapunyah Formation.|Pink, brown and buff, fine- to medium-grained, moderately sorted quartz arenite; extensively rippled; minor recessive very fine sandstone to siltstone; ferruginous mottled sandstone with evaporite casts in upper part; basal conglomerate common.|
25730|Masterton Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Maximum depositional age of 1755 +/- 15 Ma.|~1660-1650 Ma.|Umbolooga Subgroup.||||
25730|Masterton Sandstone|67352|4|Described|p14 Tb.2|Statherian|Statherian|McArthur Basin. 650m thick.||Umbolooga Subgroup||Conformably overlain by Mallapunyah Formation.  Overlies (all unconformably) Gold Creek Volcanics, Wollogorang Formation, Wununmantyala Sandstone, Hobblechain Rhyolite.|Fine- to medium-grained quartz arenite, lithic arenite and lithic wacke: thinly to thickly bedded; minor very fine-grained sandstone and siltstone; basal sandstone conglomerate.|
25730|Masterton Sandstone|69383|5|Briefly described|p53-56||Paleoproterozoic|McArthur Basin. LA-ICPMS U-Pb geochronology analyses. Max deposition age.|1755+/-15 Ma|||Unconformably overlain by ?|Fine- to medium-grained, well sorted pale pink quartz sandstone with ripple-marked bedding and thin intervals (1-10 mm) of heavy minerals.|
25730|Masterton Sandstone|69430|4|Described|p15:3, 10, 12-13, 17, 22, 34-35, 55|Statherian|Statherian|Jackson et al. (1987), Ahmad and Wygralak, (1989); redefined by Rawlings (1999). Formerly recognised in SE McArthur Basin, where it has been replaced by the Echo Sandstone. Is now recognised only in the Batten Fault Zone. Ridge-forming unit. 40-650m thick. Alluvial fan and braided river basal deposits, the remainder very shallow-marine and intertidal to supratidal sediments. Hosts phosphate deposits (briefly described).||Umbolooga Subgroup.||Overlies Warramana Sandstone (Tawallah Group) unconformably, and Nyanantu Formation probably disconformably. Is overlain by Karns Dolostone, and by Mallapunyah Formation conformably and gradationally.|Basal conglomerate. Pink, brown and buff, fine- to medium-grained, moderately sorted quartzarenite; minor recessive very fine-grained sandstone and siltstone units; distinctly ferruginous mottled sandstone with halite and gypsum casts.|12-JUL-16
25730|Masterton Sandstone|69673|6|Mentioned|p16 fig 13|||Batten Fault Zone||Umbolooga Subgroup||Overlain by Mallapunyah Formation||
25730|Masterton Sandstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||McArthur Group.||Overlies Hobblechain Rhyolite (Tawallah Group). Is overlain unconformably by Karns Dolomite.|Medium- to coarse-grained sandstone, pebbly in upper part; minor beds of clast-supported conglomerate; micaceous siltstone.|
25730|Masterton Sandstone|71374|4|Described|iii, p1 tbl 1, p6-p8, p14, p20, p23, |Statherian|Statherian|McArthur Basin. Type section occurs in Archies Creek about 900m west of its junction with the Kilgour River in northeastern KILGOUR. SHRIMP age is interpreted as the maximum depositional age for this formation. Sedimentary structures include cross-laminations, cross beds, pebble bands, ripples and dessication features. A maximum age is inferred between 1690 and 1670 Ma by its unit relationships. Sampling site provided along with zircon description and SHRIMP analytical discussion.  Conformably (transitional) overlain by the Mallapunyah Formation. Unconformably overlain by the Karns Dolostone. See also p26, p28, p32, p34, p43-p44.|1755 +/- 6 Ma (SHRIMP U-Pb)|McArthur Group||Unconformably overlies the Gold Creek Volcanics, Wollogorang Formation and Wununmantyala Sandstone.|Thinly to medium-bedded, fine- to coarse-grained, quartz and lithic sandstone. A thin, pebbly sandstone is found at the base of the formation.|
25730|Masterton Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1755+/-15 Ma (MDA: U-Pb zircon LA-ICPMS).||||Ripple-martked sandstone.|
25730|Masterton Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower McArthur Group.||||
25730|Masterton Sandstone|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|McArthur Basin.|ca. 1700 Ma||||Sandstone and greywacke.|
25730|Masterton Sandstone|72248|6|Mentioned|p147|||Of McArthur Basin.||Unit of Umbolooga Subgroup.||||
25730|Masterton Sandstone|72373|6|Mentioned|iii,p11|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||||||
25730|Masterton Sandstone|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||Underlies Mallapunyah Formation. Unconformably overlies Tawallah Group.||
25730|Masterton Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Overlain by Mallapunyah Formation.||
25730|Masterton Sandstone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Umbolooga Subgroup||Unconformably overlies Tawallah Group and underlies Mallapunyah Formation.||
25730|Masterton Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Umbolooga Subgroup, McArthur Group||Ovelain by Mallapunyah Formation.||
25730|Masterton Sandstone|73412|5|Briefly described|p4, 8, 12|||Southern McArthur Basin.||Umbolooga Subgroup.||Unconformably overlies Nyanantu Formation (Tawallah Group). Is overlain by Mallapunyah Formation.||
24374|Maud Dolerite|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Medium-grained grey-green dolerite, metadolerite.||||||
24374|Maud Dolerite|23119|5|Briefly described|p438|||||||||
24374|Maud Dolerite|23216|5|Briefly described|Table1p10,12,15|||||||||
24374|Maud Dolerite|23733|5|Briefly described|p32 Fig. 19|||||||||
24374|Maud Dolerite|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24374|Maud Dolerite|41295|4|Described|p14|||||||||
24374|Maud Dolerite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24374|Maud Dolerite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
24374|Maud Dolerite|67564|6|Mentioned|p86.|||||||Is intruded by David Suite.||
24374|Maud Dolerite|69420|5|Briefly described|p5:13-14|Paleoproterozoic|Paleoproterozoic|Exposed in a small area ~15km E of Katherine. Has been contact metamorphosed by Yeuralba Granite. May be of similar age to Zamu Dolerite.||||Intrudes Tollis Formation. Is overlain unconformably by Plum Tree Creek Volcanics.|Massive, medium- to coarse-grained to gabbroic, dark-grey quartz dolerite.|12-JUL-16
42116|Maverick Monzogranite|23809|5|Briefly described|p16|Paleoproterozoic|Paleoproterozoic|Equigranular, homogeneous, undeformed hornblende-biotite monzogranite to granodiorite.||||||07-NOV-08
42116|Maverick Monzogranite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1801+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
25218|McAddens Creek Volcanic Member|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Kombolgie Formation.  Dark grey-purple massive andesite, vesicular in places, minor banded tuff.||||||
25218|McAddens Creek Volcanic Member|22536|5|Briefly described|p9|Proterozoic|Proterozoic|Of the Katherine River Group.||||||06-NOV-06
25218|McAddens Creek Volcanic Member|22574|5|Briefly described|map|Proterozoic|Proterozoic|Of the Katherine River Group.||||||06-NOV-06
25218|McAddens Creek Volcanic Member|23216|5|Briefly described|Table1p9,20,22|||||||||
25218|McAddens Creek Volcanic Member|23374|6|Mentioned|p40||Statherian|Equivalent to Nungbalgarri Volcanics. Of Kombolgie Subgroup, McArthur Basin.||||||06-NOV-06
25218|McAddens Creek Volcanic Member|23384|6|Mentioned|Fig 27|||Of Needham and Stuart-Smith (1985). Still applies to units in the Mount Evelyn and Katherine 1:250 000 sheet areas.||||||
25218|McAddens Creek Volcanic Member|23867|5|Briefly described|p5|||Recommended by Sweet (2001) that this name be replaced by Nungbalgarri Volcanics.||||||
25218|McAddens Creek Volcanic Member|24050|6|Mentioned|p13|||||||||
25218|McAddens Creek Volcanic Member|30559|6|Mentioned|p284|||||||||
25218|McAddens Creek Volcanic Member|32660|6|Mentioned|p250|||||||||
25218|McAddens Creek Volcanic Member|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
25218|McAddens Creek Volcanic Member|40248|6|Mentioned|p226|||||||||
25218|McAddens Creek Volcanic Member|41125|6|Mentioned|p55|||||||||
25218|McAddens Creek Volcanic Member|41294|6|Mentioned|Map legend|Mesoproterozoic||||||||
25218|McAddens Creek Volcanic Member|41295|4|Described|p17|||||||||
25218|McAddens Creek Volcanic Member|41586|6|Mentioned|Map legend|Mesoproterozoic||||||||
25218|McAddens Creek Volcanic Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Kombolgie Formation. Of Statherian age.||||||07-NOV-08
25218|McAddens Creek Volcanic Member|43832|5|Briefly described|28, Table7 p26.||Mesoproterozoic|Now known to be Palaeoproterozoic in age.||||||06-NOV-06
25218|McAddens Creek Volcanic Member|44201|14|Not recorded|p.8||Neoproterozoic|U.Proterozoic.||||||
25218|McAddens Creek Volcanic Member|45022|4|Described|p.56,64,183.||Carpentarian|Of Kombolgie Formation. Fig.15, Tb.3, Pl.28.||||||
25218|McAddens Creek Volcanic Member|46679|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
25218|McAddens Creek Volcanic Member|48867|14|Not recorded|p.6,17-18|||map. Unit of Kombolgie Formation.||||||
25218|McAddens Creek Volcanic Member|62375|5|Briefly described|p20|Mesoproterozoic|Paleoproterozoic|Of the Mamadawerre Sandstone. Geological Province: Pine Creek Orogen. Thickness: 150m.||||||09-FEB-10
25218|McAddens Creek Volcanic Member|63866|5|Briefly described|p112, p117|||Contains a significant inherited zircon component.|1830 +/- 30 Ma|||Equivalent to the Nungbalgarri Volcanics.|Rhyolitic rocks.|
25218|McAddens Creek Volcanic Member|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1780-1810Ma. McArthur Basin. Of Mamadewerre Sandstone, Katherine River Group. Dark grey, massive top vesicular mafic volcanic rocks, minor hematitic siltstone, banded tuff.||||||07-JAN-09
25218|McAddens Creek Volcanic Member|65232|5|Briefly described|p65|||Lies between Mamadawerre Sandstone and Gumarrirnbang Sandstone of the lower Katherine River Group in vicinity of ABC uranium prospect. Mafic volcanic rocks. Secondary uranium mineralisation hosted by a siliceous tuffaceous horizon.||||||12-APR-12
25218|McAddens Creek Volcanic Member|67564|6|Mentioned|p39 Fig.20.|||In Roberts and Plumb (1965). Edith Falls Basin. Equivalent to rocks attributed to Nungbalgarri Volcanics by Sweet et al. (1999) and these authors recommend the name be abandoned.||Unit in (superseded) Kombolgie Formation.||||
25218|McAddens Creek Volcanic Member|67779|5|Briefly described|p32.|||Equivalent to Nungbalgarri Volcanics.||Unit in Kombolgie Subgroup.||||
25218|McAddens Creek Volcanic Member|69418|6|Mentioned|p3:17|||Pine Creek Orogen. Hosts the ABC vein-type U deposit (described).||||||12-JUL-16
25218|McAddens Creek Volcanic Member|69420|5|Briefly described|p5:84|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Parent unit not stated. Lies between Mamadawerre and Gumarrirnbang Sandstones.||Katherine River Group.||||12-JUL-16
40831|McArthur Group, Lower|23963|5|Briefly described|p1237, 1242|||Geological Province: McArthur Basin. Overlies the Tawallah Group.||||||
40831|McArthur Group, Lower|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
40831|McArthur Group, Lower|60483|5|Briefly described|p6 Fig. 4, p52 Tb. 4|||Informal - see McArthur Group. Geological Province: McArthur Basin.||||||05-OCT-07
40831|McArthur Group, Lower|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Masterton Sandstone to Emmerugga Dolomite.||Evaporitic-stromatolitic dolostone, dolomitic siltstone and sandstone, quartzose sandstone; minor basal conglomerate.|04-MAR-20
72389|McArthur Group, Middle|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes from Teena to Reward Dolomites.||Carbonaceous-pyritic shale and dolomitic siltstone, dolostone; minor pink chert beds (tuff?).|04-MAR-20
23776|McCarthys Granite|23216|5|Briefly described|Table1p9,15,18|||||||||
23776|McCarthys Granite|23714|4|Described|p27|||See also page 19 Table 4. Previously mapped as part of Cullen Granite. Geological Province: Cullen Batholith.||||||
23776|McCarthys Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
23776|McCarthys 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
23776|McCarthys Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23776|McCarthys Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Granite and leucogranite.||||||07-NOV-08
23776|McCarthys Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23776|McCarthys Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23776|McCarthys Granite|41311|4|Described|p17|||||||||
23776|McCarthys Granite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23776|McCarthys Granite|42756|6|Mentioned|Fig.5 P6|||||||||
23776|McCarthys Granite|43140|3|Fully described|p27||Paleoproterozoic|Part of the Cullen Batholith. Mapped as part of Cullen Granite by Walpole et al (1968) and earlier workers.||||||07-NOV-08
23776|McCarthys Granite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
23776|McCarthys Granite|43624|6|Mentioned|p14|||Geological Province: Cullen Batholith.||||||
23776|McCarthys Granite|43832|3|Fully described|Table8p40;49;Tb12p64||Paleoproterozoic|||||||07-NOV-08
23776|McCarthys 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
23776|McCarthys Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1840Ma. Of Cullen Supersuite. I-type.  Pink and green, coarse porphyritic hornblende-biotite granite; Pink to grey, fine to medium equigranular leucogranite; Light grey coarse porphyritic biotite leucogranite.||||||07-JAN-09
23776|McCarthys Granite|67564|3|Fully described|p7 Table 2, p33 Fig.19, p34, p55.|Paleoproterozoic|Paleoproterozoic|I-type. Pluton within Cullen Batholith, Pine Creek Orogen. 350 km2 in area. Rare contact metamorphic K-feldspar-cordierite hornfels facies zones.|c.1830 Ma.|Unit in Cullen Supersuite.||Is intruded by Lewin Springs Syenite.|Pink and green, coarse porphyritic hornblende-biotite granite with K-feldspar megacrysts to 5 cm length; minor fine equigranular leucogranite, coarse porphyritic biotite leucogranite.|
23776|McCarthys Granite|69420|5|Briefly described|p5:14, 17-18, 20, 22, 117|Paleoproterozoic|Paleoproterozoic|Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. Includes irregularly-shaped bodies, up to 5km across, of Bludells Dolerite. Hosts barite veins SE of Pine Creek.||Fingerpost Suite.|||Coarse-grained porphyritic to equigranular granite gradational to leucogranite. I-type.|12-JUL-16
23776|McCarthys Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Fingerpost Suite.|||Coarse-grained, pink-green, porphyritic hornblende-biotite granite; coarse-grained, grey porphyritic biotite granite; coarse-grained, pink, partly porphyritic biotite leucogranite.|
26021|McDermott Formation|22538|6|Mentioned|Fig3 P709|||||||||
26021|McDermott Formation|22670|6|Mentioned|55|||Geol. province: McArthur Basin.||||||06-NOV-06
26021|McDermott Formation|23065|5|Briefly described|16|Proterozoic|Proterozoic|Of Tawallah Group.||||||29-FEB-08
26021|McDermott Formation|23395|5|Briefly described|p388|||||||||
26021|McDermott Formation|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||06-NOV-06
26021|McDermott Formation|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26021|McDermott Formation|23867|5|Briefly described|p16|||Formerly the "Aquarium Formation" (in part?).  Of Tawallah Group.  Correlates with Cottee Formation (Katherine River Group).  Geological Province: McArthur Basin.  See also Fig. 30.||||||29-FEB-08
26021|McDermott Formation|24050|5|Briefly described|p19|||Of the Tawallah Group.||||||06-NOV-06
26021|McDermott Formation|31421|6|Mentioned|p507|||||||||
26021|McDermott Formation|32660|5|Briefly described|Table 4|||||||||
26021|McDermott Formation|33665|6|Mentioned|p365|||See also p368.||||||06-NOV-06
26021|McDermott Formation|35114|6|Mentioned|p203|||||||||
26021|McDermott Formation|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|36012|3|Fully described|Table 2|||||||||
26021|McDermott Formation|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26021|McDermott Formation|37568|5|Briefly described|p78|||||||||
26021|McDermott Formation|38582|6|Mentioned|Fig.3|||||||||
26021|McDermott Formation|38584|4|Described|p14|||||||||
26021|McDermott Formation|39445|5|Briefly described|Table 2|||See also p36.||||||06-NOV-06
26021|McDermott Formation|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|40489|6|Mentioned|p89|||||||||
26021|McDermott Formation|40691|5|Briefly described|p9|||||||||
26021|McDermott Formation|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|41721|3|Fully described|p18|||Of the Tawallah Group. Conformably overlies Seigal Volcanics. Thickness: 200m. Geological province: McArthur Basin. Dolomite, siltstone and sandstone.||||||01-AUG-07
26021|McDermott Formation|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26021|McDermott Formation|42385|6|Mentioned|Fig.5 P8|||||||||
26021|McDermott Formation|42812|5|Briefly described|p14|||see also Fig.5||||||
26021|McDermott Formation|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of Tawallah Group. Of "Mid Proterozoic" age.||||||06-NOV-06
26021|McDermott Formation|43036|6|Mentioned|Fig.5|||||||||
26021|McDermott Formation|44287|14|Not recorded|p.8|||(E53-3).||||||
26021|McDermott Formation|44305|14|Not recorded|p.11-12||Neoproterozoic|(E53-8). opp.6,18. U.Prot.||||||
26021|McDermott Formation|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26021|McDermott Formation|44473|14|Not recorded|p.8, opp. p.7|||(E53-7). L?Prot.||||||
26021|McDermott Formation|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26021|McDermott Formation|45162|2|Defined|p14|Proterozoic|Proterozoic|||||||
26021|McDermott Formation|45166|5|Briefly described|p28|||||||||
26021|McDermott Formation|46804|6|Mentioned|p154|||||||||
26021|McDermott Formation|49001|6|Mentioned|p5|||||||||
26021|McDermott Formation|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
26021|McDermott Formation|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Sly Creek Sandstone, underlain by Seigal Volcanics.||||||
26021|McDermott Formation|63112|5|Briefly described|p1191 Fig.2, p1192, p1205|||Leichhardt Superbasin. Age approximated from Fig.2. 120-500 m thick.|c.1755-1757 Ma.||||Interbedded dolostone, chert, halite-cast-bearing mudstone, glauconitic sandstone, stromatolitic dolostone, and shales.|
26021|McDermott Formation|63866|5|Briefly described|p54, p56|||||||Equivalent to the Quilalar Supersequence.||
26021|McDermott Formation|64817|6|Mentioned|p353 Fig.4,p355 Fig.5,p367 Tb.2,p369  |||||Of the Tawallah Group.|||Carbonate-mudstone +/- sandstone.|
26021|McDermott Formation|65228|5|Briefly described|p21, Figs.02, 06, 07.|||McArthur Basin. Carbonate unit; map symbol Ptd.||Unit in Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Wununmantyala Sandstone. Is equivalent to Sly Creek Sandstone.||
26021|McDermott Formation|65340|4|Described|p12 Fig.6, pp92-93. |||Revised in this study to include areas mapped as Aquarium Formation by Pietsch et al. (1991a) and Haines et al. (1993) in the Batten Fault Zone. Also now includes sedimentary intervals in BAUHINIA DOWNS and MOUNT YOUNG maps that had been assigned to the Settlement Creek Dolerite.||Unit in Tawallah Group.||Overlies Sly Creek Sandstone. Is disconformably overlain by Wununmantyala Sandstone.|Sandstone, dolostone and mudstone.|
26021|McDermott Formation|67144|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Sly Creek Sandstone.|Fine- to medium-grained quartz, glauconitic and dolomitic sandstone; dolostone, siltstone and chert interbeds.|
26021|McDermott Formation|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map, p32|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin.|~1750-1740 Ma.|Tawallah Group|||Stromatolitic and oolitic dolomite, sandstone, shale and siltstone.|
26021|McDermott Formation|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. Over 400m thick.||Tawallah Group||Overlies (conformably) Seigal Volcanics. Is conformably overlain by Sly Creek Sandstone.|Fine- to medium-grained quartz, glauconitic and dolomitic sandstone, dolostone, siltstone and chert interbeds.|
26021|McDermott Formation|69430|4|Described|p15:3, 10-12|||Jackson et al. (1987). Includes outcrops previously part of the Aquarium Formation in the Batten Fault Zone and SW McArthur Basin. 200m thick. Shallow-water marginal marine deposits: subtidal to supratidal carbonate bank shoreline facies. Is said to be overlain by Sly Creek Sandstone: this contradicts the relationships shown in Fig.15.4, and is inconsistent with Sly Creek Sandstone being correlated with upper Seigal Volcanics which conformably underlies McDermott Formation.||Tawallah Group.||Conformably overlies Seigal Volcanics. Is overlain conformably by Wununmantyala Sandstone.|Alternating bands of shallow-marine dolostone and siltstone, with sandstone at the base.|12-JUL-16
26021|McDermott Formation|69591|5|Briefly described|p39, p56|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|Dolomite, sandstone, siltstone.|
26021|McDermott Formation|69673|4|Described|p16 fig 13, p24, p32, p33, p40|||Mixed carbonates and clastic sedimentary rock. Deposited in shallow marine, subtidal to supratidal settings. Possible source rock.||Tawallah Group||Disconformably overlain by Wununmantyala Sandstone, Conformably overlies Rosie Creek Sandstone Member|Dolostone, chert, mudstone and sandstone.|
26021|McDermott Formation|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Sly Creek Sandstone.|Dolomite, laminated, stromatolitic, sandy, oolitic and interclast-rich; dolarenite; quartz sandstone with interbedded shale; glauconitic sandstone; shale and siltstone.|
26021|McDermott Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Tawallah Group.||||
26021|McDermott 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||Overlies Rosie Creek Sandstone Member and underlies Wununmantyala Sandstone.||
26021|McDermott Formation|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group|Rosie Creek Sandsotne Member?|Underlain by Rosie Creek Sandstone Member. Overlain by Wununmantyala Sandstone.||
26021|McDermott Formation|72912|4|Described|p5 Fig.3, p17, 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 and TOC is discussed.||Tawallah Group||Overlies Rosie Creek Sandstone Member and underlies Wununmantyala Sandstone.||15-MAR-21
26021|McDermott Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.||Tawallah Group||Underlain by Rosie Creek Sandstone Member. Overlain by Wununmantyala Sandstone.||
26021|McDermott Formation|73412|5|Briefly described|p4, 8-9|||Southern McArthur Basin. Non-magnetic.||Tawallah Group.||Overlies Rosie Creek Sandstone. Is overlain unconformably by Wununmantyala Sandstone.||
26731|McKinlay Granite|23714|4|Described|p27|||See also page 19 Table 4. Geological Province: Cullen Batholith.||||||
26731|McKinlay Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
26731|McKinlay Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
26731|McKinlay Granite|33278|6|Mentioned|Fig.7|||||||||
26731|McKinlay Granite|35061|6|Mentioned|p143|||||||||
26731|McKinlay Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26731|McKinlay Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Pink-green coarse porphyritic granite.||||||07-NOV-08
26731|McKinlay Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26731|McKinlay Granite|42756|6|Mentioned|Fig.5 P6|||||||||
26731|McKinlay Granite|42927|5|Briefly described|p428|||see also Fig.2 p430.||||||06-NOV-06
26731|McKinlay Granite|43140|3|Fully described|p29||Paleoproterozoic|Part of Cullen Batholith.||||||07-NOV-08
26731|McKinlay Granite|43624|6|Mentioned|p14|||||||||
26731|McKinlay Granite|43832|4|Described|41,46,49,53,55,65||Paleoproterozoic|||||||07-NOV-08
26731|McKinlay Granite|45003|14|Not recorded|p52|||||||||
26731|McKinlay Granite|45022|3|Fully described|p.139.||Carpentarian|On many pages.  Pl.28.||||||
26731|McKinlay Granite|46676|14|Not recorded|map legend.||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26731|McKinlay 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
26731|McKinlay Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Light grey medium/coarse granite.||||||07-JAN-09
26731|McKinlay Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
26731|McKinlay Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Margaret Suite.|||Medium- to coarse-grained mostly equigranular granodiorite. I-type.|12-JUL-16
26731|McKinlay Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||||Light grey, medium- to coarse-grained, predominantly equigranular biotite-hornblende granite.|
23781|McMinns Bluff Granite|23714|5|Briefly described|p19 T.4|||||||||
23781|McMinns Bluff Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
23781|McMinns Bluff Granite|24197|5|Briefly described|p24, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Hornblende-dominated granitic pluton. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
23781|McMinns Bluff Granite|24260|5|Briefly described|p1013 Fig.1|Orosirian|Orosirian|Age: 1835 +/- 6Ma. Geological Province: Pine Creek Inlier||||||
23781|McMinns Bluff Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23781|McMinns Bluff Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Pink-green coarse porphyritic hornblende-biotite granite.||||||07-NOV-08
23781|McMinns Bluff Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23781|McMinns Bluff Granite|41311|6|Mentioned|p17|||||||||
23781|McMinns Bluff Granite|42012|4|Described|p13|||||||||
23781|McMinns Bluff Granite|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
23781|McMinns Bluff Granite|42756|6|Mentioned|Fig.5 P6|||||||||
23781|McMinns Bluff Granite|42927|5|Briefly described|p428|||see also Fig.2 p430.||||||06-NOV-06
23781|McMinns Bluff Granite|43140|3|Fully described|p31||Paleoproterozoic|Of Cullen Batholith. U-Pb age 1820 Ma.||||||07-NOV-08
23781|McMinns Bluff Granite|43624|6|Mentioned|p13|||Geological Province: Cullen Batholith.||||||
23781|McMinns Bluff Granite|43832|3|Fully described|41,46,48-55,64-65||Paleoproterozoic|Age 1835+-6 Ma.||||||07-NOV-08
23781|McMinns Bluff Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1835-1818 +/- 6Ma (Shrimp, U-Pb).||||||07-NOV-08
23781|McMinns Bluff Granite|62375|6|Mentioned|p12|||Geological Province: Pine Creek Orogen.||||||09-FEB-10
23781|McMinns Bluff Granite|63866|5|Briefly described|p110-p111|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Numeric ages are derived from Page, OZCHRON.|1835 +/- 6 Ma (SHRIMP)|Cullen Supersuite||||
23781|McMinns Bluff Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Grey coarse porphyritic biotite-hornblende granite, fine-coarse biotite granite.||||||07-JAN-09
23781|McMinns Bluff Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
23781|McMinns Bluff Granite|69420|5|Briefly described|p5:18, 20, 22, 34, 61, 93|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. A SHRIMP U-Pb zircon age of 1835 +/- 6 Ma is also given.|1818 +/- 3 Ma conventional U-Pb zircon (TIMS).|McMinns Suite.||?Intrudes Burrell Creek Formation.|Coarse- to fine-grained porphyritic granite. Forms two chemically and petrographically distinct bodies separated by younger sedimentary rocks. I-type.|12-JUL-16
23781|McMinns Bluff Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1818 +/- 3 Ma.|McMinns Bluff Suite.|||Pink and grey, coarse-grained, predominantly porphyritic biotite-hornblende granite; fine- to coarse-grained biotite granite.|
31735|McMinns Bluff Suite|69420|5|Briefly described|p5:17, 22|Paleoproterozoic|Paleoproterozoic|[This is the current name]. There is also a McMinns Suite on p5:20. Both claim the McMinns Bluff Granite as the sole constituent. It could be a case of simple omission of the word Bluff, but confusion is compounded by their both having entries in the Index.|||McMinns Bluff Granite.||Biotite-dominated granite.|12-JUL-16
31735|McMinns Bluff Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes McMinns Bluff Granite.|||01-MAR-18
67841|McNamara Group, Lower|24432|6|Mentioned|p565 Fig.4|||||||||
67841|McNamara Group, Lower|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mount Isa Inlier.|~1690-1650 Ma.||Torpedo Creek, Gunpowder Creek, Paradise Creek, Esperanza, Lady Loretta Formations.|||
67841|McNamara Group, Lower|68542|5|Briefly described|p6, p8||||||Includes Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation|Overlies Surprise Creek beds, overlain by Upper McNamara Group|Marine carbonates and clastic sedimentary rocks.|22-OCT-19
67841|McNamara Group, Lower|68576|4|Described|Q_2: p6, p8|Proterozoic|Proterozoic|Lawn Hill Platform, Mount Isa Inlier. Hosts the exceptionally high-grade, sediment-hosted Lady Loretta Pb-Zn deposit, and the Lady Annie (Cu) Project (both described in detail).|||Torpedo Creek Quartzite, Gunpowder Creek Formation, Paradise Creek Formation, Esperanza Formation, Lady Loretta Formation.|Overlies Surprise Creek Beds. Is overlain by Upper McNamara Group.|Basal coarse clastics fining upwards into a thick sequence of dolomitic siltstones and sandstones. Occasional local non-dolomitic quartz-clastic sediments. Chert horizons common.|
67841|McNamara Group, Lower|73083|6|Mentioned|p54|||||||||
40828|McNamara Group, Upper|23957|6|Mentioned|p1124|||Informal - refers to McNamara Group.||||||16-DEC-04
40828|McNamara Group, Upper|24432|6|Mentioned|p565 Fig.4|||||||||
40828|McNamara Group, Upper|50550|5|Briefly described|p1146 Fig.9, p1152 Fig.13|||Geological Province: Western Fold Belt.||||||19-DEC-07
40828|McNamara Group, Upper|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also Eastern Australia Time-Space Plot. Mount Isa Inlier.|~1650-1590 Ma.||Shady Bore Quartzite, Riversleigh Siltstone, Termite Range and Lawn Hill Formations.|||
40828|McNamara Group, Upper|68542|6|Mentioned|p6||||||Includes Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation.|Overlies Lower McNamara Group, overlain by South Nicholson Group.||
40828|McNamara Group, Upper|68576|4|Described|Q_2: p6|Proterozoic|Proterozoic|Lawn Hill Platform, Mount Isa Inlier.|||Shady Bore Quartzite, Riversleigh Siltstone, Termite Range Formation, Lawn Hill Formation.|Overlies Lower McNamara Group. Is overlain unconformably by South Nicholson Group.|Non-dolomitic clastic facies associated with deeper water conditions, sometimes as turbidites.|
40828|McNamara Group, Upper|73083|6|Mentioned|p54, p69|||||||||
38422|Meerie Member|23733|2|Defined|p43 Appendix 1|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Approximately ~870m thick. See also p11, p3 Tb. 1 and p32 Fig. 19.||||||07-NOV-08
38422|Meerie Member|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||30-MAR-05
38422|Meerie Member|24303|3|Fully described|p5|Proterozoic|Proterozoic|Of the Hayward Creek Formation. Overlain by the Coodna Mamber; overlies the Manga Mauda Member. Geological Province: Ashburton province. Max. Thickness: 1000m. Max. Age: 1784 +/- 9 Ma (Compston, 1995)||||||18-OCT-05
38422|Meerie Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hayward Creek Formation. Sandstone; sublithic to quartz arenite; planar, thin to medium bedded, medium- to coarse-grained; laminated, well sorted, tabular crossbedded, rippled, dessicated; pebbly sandstone.||||||07-NOV-08
38422|Meerie Member|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Overlain by Coodna Member; overlies the Manga Mauda Member.||||||07-NOV-08
38422|Meerie Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Group). Sublithic/lithic/volcanilithic arenite, feldspathic sublitharenite, pebbly arenite; acid to intermediate volcanic rocks particularly at top.  Underlies Coodna Member. In the Tennant Creek region.||||||07-NOV-08
38422|Meerie Member|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Geol. Prov: Tomkinson Creek Province.||Hayward Creek Member||||
38422|Meerie Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hayward Creek Formation.||Is overlain by Coodna Member. Shown as disconformably underlain by Manga Mauda Member.|Sublithic/lithic/volcanilithic arenite, feldspathic sublitharenite, pebbly arenite; acid to intermediate volcanic rocks particularly at top.|09-DEC-14
38422|Meerie Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
38422|Meerie Member|69424|5|Briefly described|p9:5|Paleoproterozoic|Paleoproterozoic|Shallow marine sediments.||Hayward Creek Formation.||Overlies Manga Mauda Member.||12-JUL-16
38422|Meerie Member|69425|6|Mentioned|p10:12|||||Hayward Creek Formation.||Correlated in part with Coulters Sandstone.||12-JUL-16
38422|Meerie Member|69431|4|Described|p16:4-5, 7-8|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.700-1100m thick. Predominantly intertidal to shallow-marine deposits. Local basal conglomerate. The coarse-grained sandstone is characteristically bidirectionally cross-bedded, well-sorted and well-rounded. Sediment was likely sourced at least partly from Warramunga Formation.||Hayward Creek Formation.||Conformably (and generally gradationally) overlies Manga Mauda Member. Is overlain conformably by Coodna Member. Is correlated with Coulters Sandstone.|Sublithic, locally granule- and pebble-bearing sandstone; fine-grained sandstone and siltstone at top of unit are thin and planar-bedded and probably include volcaniclastic rocks. Abundant ripple marks and dessication features. Typically thin-bedded.|12-JUL-16
26025|Meeway Volcanics|22810|5|Briefly described|Table2 p4|||Maximum thickness: 75m.||||||09-APR-21
26025|Meeway Volcanics|24197|5|Briefly described|p105|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
26025|Meeway Volcanics|32307|4|Described|Table 1|||L.Proterozoic||||||
26025|Meeway Volcanics|32310|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26025|Meeway Volcanics|32660|5|Briefly described|Table 2|||||||||
26025|Meeway Volcanics|33376|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26025|Meeway Volcanics|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26025|Meeway Volcanics|40808|5|Briefly described|Table 2|||||||||
26025|Meeway Volcanics|43187|5|Briefly described|p2|||||||||
26025|Meeway Volcanics|45112|5|Briefly described|Table 21|||||||||
26025|Meeway Volcanics|48942|2|Defined|p16|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26025|Meeway Volcanics|50586|5|Briefly described|p1.1, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite.||||||07-NOV-08
26025|Meeway Volcanics|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Of Finniss River Group. Age assumed from age of parent unit. Max. thickness 1000m. Porphyritic acid lavas and tuffs. Within or at base of Burrell Creek Formation in Fitzmaurice area.||||||
26025|Meeway Volcanics|64730|6|Mentioned|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Correlated with Mulluk Mulluk Volcanic Member, and Warrs Volcanic Member of Burrell Creek Formation and Berinka Volcanics.||Of Finniss River Group.||||03-MAY-12
26025|Meeway Volcanics|64956|5|Briefly described|p2 Tb. 10|Paleoproterozoic|Paleoproterozoic|Geological province: Pine Creek Orogen.||||||07-FEB-11
26025|Meeway Volcanics|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Finniss River Group.|||Porphyritic rhyolite, tuff, sandy tuff.|
26025|Meeway Volcanics|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Appears to be shown as unit in Burrell Creek Formation.||||18-MAY-18
26025|Meeway Volcanics|69420|5|Briefly described|p5:4, 6, 13|Paleoproterozoic|Paleoproterozoic|Crops out near the western margins of the Central Domain, Pine Creek Orogen. Comagmatic with Mulluk Mulluk and Berinka Volcanics, and Warrs Volcanic Member.||Finniss River Group.||Is interbedded with basal Burrell Creek Formation.|Porphyritic felsic lava and tuff.|12-JUL-16
26025|Meeway Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite|
26025|Meeway Volcanics|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. [appears to have wrong description in App].|||||Granodiorite.|09-APR-21
30958|Melville Bay Metamorphics|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
30958|Melville Bay Metamorphics|24048|5|Briefly described|p10|||Part of the Bradshaw Complex.  Geological Province: Arnhem Inlier.||||||06-NOV-06
30958|Melville Bay Metamorphics|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bradshaw Complex. Gneiss: granulite facies, cordierite-garnet and orthopyroxene-quartz bands; mafic gneiss: two pyroxene; intruded by pods and veins of medium-grained garnetiferous leucogranite. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
30958|Melville Bay Metamorphics|44112|2|Defined|Table2p12,13,17,110|Orosirian|Orosirian|Max Age: ~1850-60 Ma||||||
30958|Melville Bay Metamorphics|50591|6|Mentioned|p2.2|||Geological Province: Arnhem Block/McArthur Basin. Intruded by Bradshaw Suite.||||||
30958|Melville Bay Metamorphics|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bradshaw Complex. Gneiss: granulite facies, cordierite-garnet and orthopyroxene-quartz bands; mafic gneiss: two pyroxene; intruded by pods and vein s of medium-grained garnetiferous leucogranite. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
30958|Melville Bay Metamorphics|69421|5|Briefly described|p6:2-4|||NE Arnhem Province. Source of Drimmie Head Granite which also intrudes this unit. P/T estimates are 700-750 oC and 4-5 kbar.||Bradshaw Complex.||Is intruded by Drimmie Head Granite.|Banded granulite, alternate dark pelitic layers and white felsic layers, medium- to coarse-grained with localised veins and pods of coarse-grained, garnetiferous leucogranite.|12-JUL-16
30958|Melville Bay Metamorphics|69455|6|Mentioned|p39:7 Fig.39.8|Paleoproterozoic|Paleoproterozoic|Part of the basement in the Gove area (Arnhem Province). Misprinted as Melville Bay Metamophics.||||||12-JUL-16
30958|Melville Bay Metamorphics|70719|5|Briefly described|iv, p5, p7-8|||Northern Gove Peninsula, Arnhem Province. Interpreted as metamorphosed equivalent of Grindall Formation. Heterogeneous melting of this unit provided the magma for the Drimmie Head Granite.||||Is intruded by Drimmie Head Granite.||
30958|Melville Bay Metamorphics|71374|5|Briefly described|p14, p32, p35|||Arnhem Province.||||||
30958|Melville Bay Metamorphics|71605|4|Described|iii-iv, p1, p6, p9-p15, p17||Orosirian|Arnhem Province. Preserves evidence for high thermal gradient, granulite-facies metamorphism. SHRIMP ages are interpeted as the maximum depositional ages. SHRIMP ages interpreted to represent zircon growth during high grade metamorphism are 1860 +/- 5 and 1857 +/- 4 Ma. Interpreted as the source of S-type granites in the Arnhem Province. Sample location, LA-ICPMS ages and SHRIMP analyses are discussed. See also p24-p25, p27-p28, p35. |1884 +/- 20 Ma, 1895 +/- 8 Ma (SHRIMP U-Pb)|Bradshaw Complex|||Interlayered garnet-biotite-plagioclase-quartz-cordierite migmatite, quartzite,metasiltstone and interlayered greywacke and sandstone.|
30958|Melville Bay Metamorphics|71620|4|Described|iv, p3, p5-p7, p10-p13|Orosirian|Orosirian|Arnhem Province. SHRIMP age is interpreted as the maximum depositional age of the protolith of this unit. Metamorphosed during a protracted high temperature granulite facies cycle (Reno et al, 2015). Melts derived from this unit formed plutons of S-type granites including the Wonga gneiss, Bawaka Granite and the Drimmie Head Granite. Metamorphic ages (1876 +/- 22 Ma, LAICPMS) are provided along with discussions on LAICPMS analyses, results, monazite characteristics, petrography and sampling location. See also p16, p18, p21-p23, p26-p28.|1895 +/- 8 Ma (SHRIMP, Kositcin et al, 2017)|||Unconformably overlain by the Grindall Formation.|Metapelitic migmatite, cordierite biotite-sillimanite migmatite, cordierite biotite migmatite, garnet-cordierite quartzite.|
30958|Melville Bay Metamorphics|72365|4|Described|iii,p1,6-7,10-14,19-20,22,25-27,29,31-34|Orosirian|Orosirian|Geological province: Arnhem Province. Deposited in a high thermal gradient between c. 1900-1880 Ma (Whelan et al 2017, Kositcin et al in press, Reno et al 2017) and underwent HT metamorphism to granulite facies (eg Reno et al 2015, 2017). Subsequently underwent partial melting, and accummulated to form a series of S-type granites in the Arnhem Province. Previous zircon dating results from Kisitcin et al. (in press) include 1895+\-8 Ma and 1884+\-20 Ma (max dep ages); 1860+\-5 Ma and 1857+\-4 Ma (metamorphic age, zircon growth). Previous zircon dating results from Reno et al. (2017; in press) include  1898+\-8 Ma (protolith max dep age), 1866+\-6 Ma (metamorphic zircon growth), and ages ranging from c. 1880 to 1850 Ma (metamorphic monazite growth). Sample GV14BLR010B (metamudstone migmatite; 683601E 8652567N) records maximum timing for deposition of the sedimentary protolith at 1898+\-8 Ma, metamorphic zircon growth in equilibrium with garnet at 1866+\-6 Ma. Sample GV14SKR061B (quartzite; 685267E 8649456N) records a maximum timing for deposition of the sedimentary protolith at 1901+\-10 Ma, and metamorphic synchronous zircon growth in equilibrium with garnet growth at 1876+\-14 Ma. Dated sample and sample location are provided.|c. 1900-1880 Ma|||Intruded by Drimmie Head Granite.|Metasedimentary gneisses comprised predominantly of garnet-cordierite-biotite schistose gneiss.|09-JAN-20
30958|Melville Bay Metamorphics|72373|5|Briefly described|p20|||Geological province: Arnhem Province.||||||
30958|Melville Bay Metamorphics|72377|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Geological province: Arnhem Province.||||Intruded by sub-volcanic dykes of the Gadabara Volcanics.||
30958|Melville Bay Metamorphics|73089|6|Mentioned|p31-32|Orosirian|Orosirian|Arnhem Province.|1900-1880 Ma|||||
36790|Merlin kimberlite|23772|5|Briefly described|p764||Devonian|In the McArthur Basin. Age: 370 Ma.||||||06-NOV-06
36790|Merlin kimberlite|69430|4|Described|p15:56, 58|Carboniferous|Devonian|Informal name. More often referred to collectively as the Merlin pipes; 12 kimberlite pipes and 2 sandstone breccia pipes. Diamondiferous. Described in detail. Rb-Sr phlogopite age, although the paragraph in which this date appears calls this Carboniferous.|367 +/- 4 Ma (Atkinson et al., 1990).|||Intrudes Bukalara Sandstone.|Kimberlite, consisting of serpentine, iron oxides, silica, calcite/Mg calcite, phlogopite, spinel and chlorite; fresh olivine is rarely present.|12-JUL-16
26313|Mia Mia Volcanics|23733|5|Briefly described|p32 Fig. 19|||||||||
26313|Mia Mia Volcanics|23809|5|Briefly described|p27 Fig. 25|||Of the Ooradidgee Group.  Geological Province: Davenport Province.||||||
26313|Mia Mia Volcanics|23823|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Gp. Recessive, commonly cleaved, felsic lavas and pyroclastics, and, near the top, minor interlayered ridge-forming sandstone. Max. thickness: >200m. Geological Prov: Davenport Geosyncline.||||||07-FEB-11
26313|Mia Mia Volcanics|24172|5|Briefly described|p67 Tb.9|||Of the Ooradidgee Subgroup. Overlain by Unimbra Sandstone. Geological Province: Tennant Creek Inlier. Of Hatches Creek Group. Felsic tuff and lave with subordinate sandstone.||||||06-NOV-06
26313|Mia Mia Volcanics|39624|5|Briefly described|Table 1|||||||||
26313|Mia Mia Volcanics|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26313|Mia Mia Volcanics|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26313|Mia Mia Volcanics|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Cleaved massive felsic tuff and lava, commonly porphyritc; minor bedded tuff; feldspathic and volcaniclastic arenite and conglomerate. Geological Province: Tennant Creek Block.||||||07-NOV-08
26313|Mia Mia Volcanics|41129|4|Described|Table 1|||Mention p19 and p24.||||||06-NOV-06
26313|Mia Mia Volcanics|41308|5|Briefly described|Table 2|||||||||
26313|Mia Mia Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
26313|Mia Mia Volcanics|41524|5|Briefly described|Table 1|||||||||
26313|Mia Mia Volcanics|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group). Felsic volcanics.||||||07-NOV-08
26313|Mia Mia Volcanics|41970|6|Mentioned|Fig.3 P333|||||||||
26313|Mia Mia Volcanics|43802|6|Mentioned|Table 1,p80|||||||||
26313|Mia Mia Volcanics|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||06-NOV-06
26313|Mia Mia Volcanics|49033|2|Defined|p14|Proterozoic|Proterozoic|||||||
26313|Mia Mia Volcanics|50588|5|Briefly described|p3.1|||Geological Province: Tennant Creek/Davenport Province. Of the Ooradidgee Subgroup.||||||
26313|Mia Mia Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Felsic tuff and lava; minor feldspathic/lithic arenite and quartz arenite; rare volcaniclastic arenite. In the Tennant Creek region.||||||07-NOV-08
26313|Mia Mia Volcanics|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
26313|Mia Mia Volcanics|65338|6|Mentioned|p19.|||Undated but correlate with Treasure Volcanics.||||||
26313|Mia Mia Volcanics|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Ooradidgee Group.||Overlies Taragan Sandstone.|Cleaved massive felsic tuff and lava, commonly porphyritic; minor bedded tuff; feldspathic and volcaniclastic arenite and conglomerate.|
26313|Mia Mia Volcanics|67175|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||||||
26313|Mia Mia Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Ooradidgee Group.||||
26313|Mia Mia Volcanics|67352|4|Described|p10, p41, p44 fig 48, p45|Orosirian|Orosirian|Over 2000 m thick. Subaqueous extrusives.||Ooradidgee Group||Lateral equivalent of Treasure Volcanics.|Felsic tuff: massive, ignimbritic, laminated to thinly bedded; rhyolitic lava: vesicular, amygdaloidal and porphyritic; minor feldspathic, volcaniclastic and quartz arenite: medium bedded, medium-to coarse-grained; rare volcaniclastic conglomerate.|
26313|Mia Mia Volcanics|68518|4|Described|p8-9 Tb.1, p12|Proterozoic|Proterozoic|Thickness: 1000+ m.||Ooradidgee Subgroup||Overlain conformably or disconformably by Unimbra Sandstone; base not seen.|Variably recessive, iron-stained to bleached, massive to poorly bedded felsic tuff and lava; commonly cleaved.|30-MAY-16
26313|Mia Mia Volcanics|68697|5|Briefly described|p24|||Localised. Topmost volcanic unit in the Ooradidgee Group.||Ooradidgee Group.||Correlated with Treasure Volcanics.||
26313|Mia Mia Volcanics|69424|5|Briefly described|p9:5, 23, 25, 55|Paleoproterozoic|Paleoproterozoic|Davenport Province.||Ooradidgee Group.||Correlated with Treasure Volcanics. Is intruded by Treasure Suite.|Predominantly a succession of pyroclastic and volcaniclastic rocks, with minor felsic lava.|12-JUL-16
26313|Mia Mia Volcanics|69425|4|Described|p10:3-5, 9-10, 13|||Confined to the Mia Mia Dome. Probable subaqueous, predominantly fragmental, deposition from major volcanic centre. Over 2000m thick; base not exposed.||Ooradidgee Group.||Is overlain by Unimbra Sandstone conformably/disconformably. Correlated with Treasure Volcanics.|Felsic tuff and (commonly phenocryst-bearing) lava; massive ignimbrite?; subordinate feldspathic/lithic and quartz sandstone; rare volcaniclastic sandstone.|12-JUL-16
38101|Michell Nob Granite|24301|4|Described|p13, p6 Tb. 1|Mesoproterozoic|Mesoproterozoic|Overlain by Nulchara Charnockite.  Geological Province: Musgrave Block||||||
38101|Michell Nob Granite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Granite. Geological Province: Musgrave Block.||||||
38101|Michell Nob Granite|61154|5|Briefly described|p14, p28|Mesoproterozoic|Mesoproterozoic|Felsic intrusion in N.T. near Mulga Park Station. Coarse-grained, porphyritic and contains phenocrysts of K-feldspar as well as plagioclase, quartz, biotite, garnet and amphibole.  Age: 1068+/-6Ma (SHRIMP U-Pb zircon: Camacho 1997). See also p13, p44 App.||||||
38101|Michell Nob Granite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province.|1068 +/- 6 Ma (Camacho, 1997, SHRIMP U-Pb)|||||
38101|Michell Nob Granite|67128|4|Described|p3, p12, p27-28, p30|||Mulga Park area, Musgrave Ranges. Also appears as Michael Nob Granite on p12 and p30. Strongly deformed during the Petermann Orogeny.|1068 +/- 13 Ma (Camacho, 1997).|||Is crosscut by Nulchara Charnockite.|Mesocratic, K-feldspar porphyritic to rapakivi-textured, hornblende-orthopyroxene-biotite-garnet bearing granite. Mylonitic: up to 3cm subrounded microcline and perthite phenocrysts wrapped by granoblastic fabric.|
38101|Michell Nob Granite|69436|5|Briefly described|p21:11-12|Mesoproterozoic|Mesoproterozoic|Young et al. (2002). Occurs in a small area, on the SA border, near Mulga Park station. Musgrave Province. Emplaced during the Giles Event (1085-1040 Ma). SHRIMP U-Pb zircon age.|1068 +/- 6 Ma (Camacho, 1997).|Warakurna Supersuite.|||Coarse-grained K-feldspar-porphyritic granite, with plagioclase, quartz, biotite, garnet and amphibole. Has a strong, anastomosing mylonitic fabric. Biotite and hornblende define a mineral elongation parallel to the stretching lineation.|12-JUL-16
38101|Michell Nob Granite|70018|5|Briefly described|p235|||Amadeus Basin. Comagmatic with Nulchara Charnockite based on presence of Nulchara Charnockite xenoliths in the MNG and vice versa. Average 207Pb/206Pb age (Jaffey et al., 1971) is 1074.3+\-0.9 Ma.||||Overlain by Nulchara Charnockite.|Porphyritic with large (up to 3 cm) sub-rounded, simply twinned crystals of K-feldspar wrapped by a finer-grained mylonitic fabric.|
38101|Michell Nob Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1068+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
25235|Middle Creek Sandstone Member|23393|6|Mentioned|p21|Mesoproterozoic|Mesoproterozoic|Of Mullera Formation.||||||
25235|Middle Creek Sandstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Mullera Formation.  ||||||
25235|Middle Creek Sandstone Member|26310|2|Defined|p4, 10, 15|Proterozoic|Proterozoic|Of the Mullera Formation. Quartzitic sandstone, siltstone, shale. Maximum Thickness: 480 feet. Type section in text.||||||
25235|Middle Creek Sandstone Member|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Mullera Formation (South Nicholson Group).  Grey and light brown, massive to flaggy, fine to medium sandstone,with some interbedded sitlstone and shale.||||||10-JAN-05
25235|Middle Creek Sandstone Member|39497|4|Described|p15|||See also p5.||||||06-NOV-06
25235|Middle Creek Sandstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
25235|Middle Creek Sandstone Member|44482|14|Not recorded|p.9|||(E53-12).||||||
25235|Middle Creek Sandstone Member|44483|5|Briefly described|map legend|||Defn. on Tech.File E/533-12. Upper (?) Proterozoic.||||||
25235|Middle Creek Sandstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Mullera Formation.||||||
25235|Middle Creek Sandstone Member|45166|5|Briefly described|p33|||||||||
25235|Middle Creek Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Mullera Formation.||||||
25235|Middle Creek Sandstone Member|65337|4|Described|p9 Fig.5, p38 Table 5, pp59-60.|Mesoproterozoic|Mesoproterozoic|Southeast MOUNT DRUMMOND area. Formerly the Mistake Creek Sandstone Member. Thickness to 70 m of shallow-marine intertidal and shoreface, above fair-weather wave-base, deposits.||Unit in Mullera Formation.|||White, silicified, fine-grained, sublithic glauconitic sandstone with distinctive decimetre-scale amalgamated trough cross-beds defined by hematite (altered glauconite) dustings on foresets.|
25235|Middle Creek Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin||South Nicholson Group|||Sandstone; siltstone, shale|
25235|Middle Creek Sandstone Member|67539|6|Mentioned|p15, p15 Fig.8|||||Of the Mullera Formation.||||
25235|Middle Creek Sandstone Member|68146|6|Mentioned|p196|||||Mullera Formation||||
25235|Middle Creek Sandstone Member|69434|5|Briefly described|p19:2, 7|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. Shallow-marine intertidal and shoreface deposits, above fair-weather wave base.||Mullera Formation.|||White, silicified, fine +/- medium, sublithic glauconitic sandstone with distinctive decimetre-scale amalgamated trough cross-beds defined by haematite dustings on foresets.|12-JUL-16
25235|Middle Creek Sandstone Member|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT).||Mullera Formation.||||
25235|Middle Creek Sandstone Member|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Middle Creek, within Mullera [Formation]. South Nicholson Basin.||||||29-NOV-17
25235|Middle Creek Sandstone Member|71369|5|Briefly described|p5-6, p37, p42-44, p48|Mesoproterozoic|Mesoproterozoic|Carter and Zimmerman (1960). South Nicholson Basin. Up to 150m thick. Progradational deposits.||Mullera Formation.|||A series of quartz-rich, dark-speckled resistant sandstone units, each 5-10m thick, separated by laminated and thin-bedded mudstone.|
25235|Middle Creek Sandstone 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.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone 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.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone 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.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone 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.|||Cross-bedded , fine-to medium-grained, quartz-rich sandstone and mudstone.|
25235|Middle Creek Sandstone 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.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Mullera Formation.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone 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.|||Cross-bedded, fine to medium-grained, quartz-rich sandstone and mudstone|
25235|Middle Creek Sandstone Member|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as located in the central and eastern parts of the South Nicholson Basin.||Probably Mullera Formation.||||
25235|Middle Creek Sandstone Member|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|||mid- Mullera Formation, Accident Subgroup||||
25235|Middle Creek Sandstone Member|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in East and Central parts of the South Nicholson Basin.||Mullera Formation||||
25235|Middle Creek Sandstone Member|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the central part of the South Nicholson Basin.||Mullera Formation,  Accident Subgroup||Shown as within upper Mullera Formation.|Includes sandstone.|
25235|Middle Creek Sandstone Member|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|||Mullera Formation, Accident Subgroup, South Nicholson Group||||
25235|Middle Creek Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin. (Relationship between Mullera Formation and Middle Creek Sandstone Member is not clear in Fig.1.2.)||Mullera Formation, Accident Subgroup, South Nicholson Group||Underlain(?) by Train Range Ironstone. Overlain(?) by Tidna Sandstone.||
25235|Middle Creek Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Aquitard with potential shale gas/oil play.||Mullera Formation, Accident Subgroup, South Nicholson Group||||
39039|Milliwindi Dolerite|24122|5|Briefly described|p12|Cambrian|Cambrian|Age: 513+/-12Ma (SHRIMP).||||||
39039|Milliwindi Dolerite|24297|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Dolerite dyke.  Age: 513+/-12Ma (SHRIMP zircon,  Hanley and Wingate, 2000).||||||
39039|Milliwindi Dolerite|24303|6|Mentioned|p62 Appendix|||Age: 513 +/- 12 Ma. Correlates with Antrim Plateau Volcanics.||||||
39039|Milliwindi Dolerite|60685|6|Mentioned|p18|Early Cambrian|Early Cambrian|Dolerite dyke in west Kimberley region. Age: 513 +/- 12Ma (SHRIMP Zircon, Hanley and Wingate, 2000).||||||24-NOV-09
39039|Milliwindi Dolerite|64589|5|Briefly described|dated_samples file||Cambrian|U-Pb zircon crystallization age 513 +/-12 Ma. Kimberley.||||||12-NOV-08
39039|Milliwindi Dolerite|66526|6|Mentioned|p7, p17, p27.|||In Hanley and Wingate, (2000). Referred to on p17 and p27 as Milliwindi dolerite dyke. Kimberley Province; coeval and geochemically comagmatic with the Kalkarindji Large Igneous Province lavas.||||||
39039|Milliwindi Dolerite|69445|5|Briefly described|p30:1, 6, 10, 16-17|Cambrian|Cambrian|Hanley and Wingate (2000). A 250km long feeder dyke for the Antrim Plateau Volcanics (Kalkarindji Suite). SHRIMP U-Pb zircon age.|513 +/- 12 Ma (Hanley and Wingate, 2000).|Kalkarindji Suite.||||12-JUL-16
39039|Milliwindi Dolerite|69634|4|Described|GEOL_LUT_CSV files|Series 2|Series 2|Of Kalkarindji Large Igneous Province. Events: Alice Springs Orogeny. See 250k_interpgeol_lut.csv, 250k_geologyl_lut.csv.|510 Ma Isisotopic)|Unit of Kalkarindji Supersuite.|||Dolerite dyke|
39039|Milliwindi Dolerite|69660|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.||||Dolerite dyke.|
39039|Milliwindi Dolerite|70126|5|Briefly described|Map legend|Cambrian|Cambrian|Kalkarindji Large Igneous Province.|c.510 Ma.||||Dolerite dykes.|
39039|Milliwindi Dolerite|70154|6|Mentioned|100k_geologyp_lut.csv|Cambrian||See also 100k_geologyl_lut.csv, 100k_interpgeol_lut.csv.|510 +/-1Ma|Kalkarindji Supersuite |||Dolerite dyke.|22-SEP-17
39039|Milliwindi Dolerite|70826|6|Mentioned|p14 tbl 5|Cambrian|Cambrian|West Kimberley.|512 Ma|||||
39039|Milliwindi Dolerite|71267|4|Described|GEOL_LUT_CSV files|Series 2|Series 2|Of the Kalkarindji LIP. Events: Alice Springs Orogeny (450-295 Ma). See 100k_interpgeop_lut.csv, 100k_geologyp_lut.csv, 250k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 1m_interpgeol_lut.csv, 500k_interpgeol_lut.csv, 2_5m_interpdykel15_lut.csv, 100k_geologyl_lut.csv.|510+\-1 Ma (isotopic)|Unit of Kalkarindji Supersuite.|||Dolerite dyke|
22337|Milyakburra Formation|22538|6|Mentioned|Fig3 P708|||||||||
22337|Milyakburra Formation|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
22337|Milyakburra Formation|22808|2|Defined|30|Orosirian|Orosirian|Of the Bustard Subgroup. Overlies Bickerton Rhyolite, Abarungkwa Sandstone||||||06-NOV-06
22337|Milyakburra Formation|24048|3|Fully described|p18|Statherian|Orosirian|Of the Bustard Group.  Max. thickness: 40m.  Geological Province: McArthur Basin.||||||06-NOV-06
22337|Milyakburra Formation|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Cobble and boulder conglomerate: matrix to clast-supported, coarse sand to granule matrix; locally interbedded with granule conglomerate and medium to coarse-grained lithic sandstone. Geol. Prov: McArthur Basin.||||||13-OCT-05
22337|Milyakburra Formation|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
22337|Milyakburra Formation|44112|6|Mentioned|Fig11p30|||||||||
22337|Milyakburra Formation|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Cobble and boulder conglomerate: matrix to clast-supported, coarse sand to granule matrix; locally interbed ded with granule conglomerate and medium to coarse-grained lithic sandstone. Geol. Prov: McArthur Basin.||||||
22337|Milyakburra Formation|64817|5|Briefly described|p353 Fig.4, p355 Fig.5 ||Orosirian|Caledon Shelf South, McArthur Basin.|1814 - 1790 Ma|Of the Bustard Subgroup.|||Sandstone and conglomerate.|04-JUN-18
22337|Milyakburra Formation|69430|4|Described|p15:3, 5-6|||NE McArthur Basin. Up to 40m thick (incomplete section). High-energy fluvial and alluvial fan deposits.||Bustard Subgroup.||Overlies Abarungkwa Sandstone unconformably and Bickerton Rhyolite ?disconformably. Correlated with Milyema Formation.|Massive to cross-bedded, matrix- to clast-supported, polymictic cobble and boulder conglomerate with coarse sand to granule matrix; locally interbedded with granule conglomerate and medium- to very coarse-grained lithic sandstone.|12-JUL-16
22337|Milyakburra Formation|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Bustard Subgroup||Overlain by Woodnah Sandstone, overlies Bickerton Rhyolite||
34025|Milyema Formation|22538|6|Mentioned|Fig3 P708|||||||||
34025|Milyema Formation|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
34025|Milyema Formation|22808|2|Defined|30|Orosirian|Orosirian|Of the Bustard Subgroup. Underlies Alyinga Sandstone.||||||06-NOV-06
34025|Milyema Formation|24047|5|Briefly described|p49|Paleoproterozoic|Paleoproterozoic|Pebbly lithic sandstone and quartz arenite.  See also p50 Fig. 41.||||||07-NOV-08
34025|Milyema Formation|24048|5|Briefly described|p21|||||||||
34025|Milyema Formation|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Basal granule to boulder conglomerate: polymict, interbedded coarse-grained pebbly lithic sandstone, cross-bedded; sandstone: predominantly medium-grained, minor granule lenses. Geol. Prov: McArthur Basin.||||||13-OCT-05
34025|Milyema Formation|44112|6|Mentioned|Fig11p30|||||||||
34025|Milyema Formation|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Bustard Subgroup, Groote Eylandt Group. Basal granule to boulder conglomerate: polymict, interbedded coarse-grained pebbly lithic sandstone, cross- bedded; sandstone: predominantly medium-grained, minor granule lenses. Geol. Prov: McArthur Basin.||||||
34025|Milyema Formation|64817|5|Briefly described|p353 Fig.4, p355 Fig.5|||Caledon Shelf South, McArthur Basin.|1814 - 1790 Ma.|Of the Bustard Subgroup.|||Sandstone and conglomerate.|04-JUN-18
34025|Milyema Formation|69430|4|Described|p15:3, 5|||NE McArthur Basin. 50m thick. High-energy, braided fluviatile deposits: shallow-marine in the upper part.||Bustard Subgroup.||Is overlain apparently disconformably by Alyinga Sandstone. Correlated with Milyakburra Formation.|Basal granule to boulder conglomerate; cross-bedded, coarse-grained pebbly lithic sandstone.|12-JUL-16
34025|Milyema Formation|69455|6|Mentioned|p39:10|Paleoproterozoic|Paleoproterozoic|Groote Eylandt.||||||12-JUL-16
34025|Milyema Formation|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Bustard Subgroup||Overlain by Anyinga Sandstone, overlies Bickerton Rhyolite||
25243|Mirarrmina Complex|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
25243|Mirarrmina Complex|22538|6|Mentioned|P714||Orosirian|||||||
25243|Mirarrmina Complex|22600|4|Described|Map legend|Orosirian|Orosirian|||||||
25243|Mirarrmina Complex|23374|5|Briefly described|Fig3p5||Paleoproterozoic|||||||07-NOV-08
25243|Mirarrmina Complex|24048|3|Fully described|p11|Paleoproterozoic|Paleoproterozoic|Previously informally known as "McClaren Complex".  Geological Province: Arnhem Inlier.||||||07-NOV-08
25243|Mirarrmina Complex|24049|5|Briefly described|Map Legend|Orosirian|Orosirian|Gneiss; foliated garnetiferous granite; metasedimentary rocks; younger undivided sedimentary and igneous rocks with complex structural or intrusive relationships. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||13-OCT-05
25243|Mirarrmina Complex|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25243|Mirarrmina Complex|32660|5|Briefly described|Table 1|||||||||
25243|Mirarrmina Complex|35950|6|Mentioned|p301|||||||||
25243|Mirarrmina Complex|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
25243|Mirarrmina Complex|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25243|Mirarrmina Complex|42597|5|Briefly described|Map Legend|Paleoproterozoic|Archean|||||||07-NOV-08
25243|Mirarrmina Complex|43010|2|Defined|p41||Paleoproterozoic|Of Orosirian or Statherian ages.||||||07-NOV-08
25243|Mirarrmina Complex|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25243|Mirarrmina Complex|44112|3|Fully described|p20-22,72||Paleoproterozoic|Unconformably overlaid by the ?Dhunganda Formation.||||||07-NOV-08
25243|Mirarrmina Complex|44299|4|Described|p.8|Paleoproterozoic|Archean|SD/53-7,8. L.Proterozoic/Archaean, Table 1.||||||07-NOV-08
25243|Mirarrmina Complex|44300|14|Not recorded|map legend|Paleoproterozoic|Archean|SD/53-7,8. L.Proterozoic - Archaean.||||||07-NOV-08
25243|Mirarrmina Complex|45087|6|Mentioned|p215|||Chemical analyses||||||
25243|Mirarrmina Complex|46658|6|Mentioned|p546|||||||||
25243|Mirarrmina Complex|50591|5|Briefly described|p1.3, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Bradshaw Suite.  Geological Province: Arnhem Block/McArthur Basin. Age: 1875 +/- 6Ma (U-Pb).||||||07-NOV-08
25243|Mirarrmina Complex|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25243|Mirarrmina Complex|61403|5|Briefly described|Map Legend|Orosirian|Orosirian|Gneiss; foliated garnetiferous granite; metasedimentary rocks; younger undivided sedimentary and igneous rocks with complex structural or intrusive re lationships. Geol. Prov: McArthur Basin, Arnhem Inlier.||||||
25243|Mirarrmina Complex|63866|5|Briefly described|p114, p124|||Caledon Shelf/Arnhem Inlier.||||Unconformably overlain by the Donydji Group.||
25243|Mirarrmina Complex|69421|5|Briefly described|p6:1, 3-6|||Arnhem Province. Poorly exposed. A composite unit including basement, parts of Donydji and probably Parsons Range Groups, and dolerite dykes. Comprises high-grade metamorphic and anatectic rocks intruded by felsic and mafic dykes. All components except the dykes have been overprinted by "Post-Nathan Shortening" event deformation. Basement metamorphic age of 1870 +/- 8 Ma, and felsic intrusives are dated at 1705 +/- 10 Ma.||||Is (probably) overlain unconformably by Dhunganda Formation.|An 'older' group of metasedimentary gneiss, migmatite, granite, minor cataclasite, commonly foliated, garnetiferous; intruded by a 'younger' group of porphyritic microgranite, rhyolite, dolerite, minor hybrid rock.|12-JUL-16
25243|Mirarrmina Complex|69430|6|Mentioned|p15:6|||||||Is overlain unconformably by Donydji Group.||12-JUL-16
25243|Mirarrmina Complex|71606|5|Briefly described|p137|Orosirian|Orosirian|Central Walker Trough, McArthur Basin. Associated with 1885-1870 Ma Barramundi Orogeny.||||Overlain unconformably by Donydji Group.||
25243|Mirarrmina Complex|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
25243|Mirarrmina Complex|72377|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Arnhem Province.||||Overlain unconformably by Dhunganda Formation.||
76087|Mitchell Yard Dolostone Member|64815|6|Mentioned|p4 Fig.2, p14 Tb.5 |||Called Dolomite in Tb.5.||Unit in Emmerugga Dolostone.||||
76087|Mitchell Yard Dolostone Member|67144|5|Briefly described|Map legend.|Statherian|Statherian|Generally recessive.||Unit in Emmerugga Dolostone.||Overlies Mara Dolostone Member.|Massive, dark grey, karstic-weathering, crystalline dololutite; lacks obvious internal sedimentary structure.|
76087|Mitchell Yard Dolostone Member|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. Over 90 m thick.||Emmerugga Dolostone||Conformably overlies Mara Dolostone Member.|Massive crystalline dolomudstone.|
76087|Mitchell Yard Dolostone Member|69430|4|Described|p15:3, 16-17, 22, 34-35, 38, 42|||Southern McArthur Basin. Possibly deep marine deposits. Shortened to Mitchell Yard Member in Fig.15.4 [probably for lack of space] and 15:38, and to Mitchell Yard Dolostone in Figs.15.31-32. An inferred hiatus before burial has been suggested. Hosts the Buffalo Lagoon Pb prospect.||Emmerugga Dolostone.||Conformably overlie Mara Dolostone Members. Is overlain conformably by Teena Dolostone.|Massive, dark grey, karstic-weathering, crystalline dololutite; lacks obvious internal sedimentary structures.|12-JUL-16
82948|Mittiebah Formation|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|See also Mittiebah Sandstone, of the Accident Subgroup, South Nicholson Group. [Probably the same unit, but may be significant uncertainty around age?]||Benmara Group||Partly underlain by Crow* Formation, partly underlain and equivalent to Caulfield beds.||
38419|Mitty Member|24303|2|Defined|p7 p55 Appendix|Statherian|Statherian|Of the Morphett Creek Formation. Overlain by the Deagan Member and unconformably overlain by the Gleeson Formation; overlies the Kuerschner Member. Max. Thickness: 2200m. Formerly undifferentiated Tomkinson Creek beds.||||||18-OCT-05
38419|Mitty Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Morphett Creek Fm. Mudstone; sst, dolomitic mudst. and sst, dolost, pebble conglom., tuffaceous siltstone; stromatolitic bioherms, oolid grainstone, lensing beds, cauliflower and enterolithic chert, halite, gypsum and anhydrite pseudomorphs; recessive.||||||07-NOV-08
38419|Mitty Member|69425|5|Briefly described|p10:12|||Tomkinson Province.||Short Range Sandstone.||Correlated with Lennee Creek Formation.||12-JUL-16
38419|Mitty Member|69431|4|Described|p16:6, 8-9, 13|||Tomkinson Province. c.1500-2200m thick. Recessive; typically poorly exposed. Lithology described in some detail. Intertidal, shallow-marine, sabkha and probable fluviatile deposits.||Morphett Creek Formation.||Conformably overlies Kuerschner Member. Is overlain by Deagan Member conformably to disconformably, and by Gleeson Formation unconformably.|Chert, stromatolitic dolostone, sandstone and mudstone; overlain by lithic and sublithic sandstone, interbedded with mudstone and rare conglomerate and carbonate rocks. Pseudomorphs after evaporites common. Some chert may be silicified tuff.|12-JUL-16
73523|Mollie Granite Complex|65341|2|Defined|p2 Fig.2, p4, p10, p28. |Paleoproterozoic|Paleoproterozoic|New name (Haines and Scrimgeour). Scattered outcrops of low hills of weathered granite, and low domes, pavements and tors of fresh granite. Tentatively related to Strangways Orogeny granitoids. Aeromagnetic interpretation suggests outcrops comprise a single body; however field outcrops show a wide lithological range. Small pegmatite bodies are abundant; those in the south are typically rich in tourmaline.|||Includes Esther, Anmatjira, Queenie Flat and Crooked Hole Granites.|Probably intrudes Utopia Quartzite.|Dark biotite-rich granodiorite with abundant dark enclaves, intruded by younger leucocratic microgranite and leucocratic K-feldspar-porphyritic granite; locally foliated; later phases are intimately interlayered and appear to be comagmatic.|
73523|Mollie Granite Complex|69427|5|Briefly described|p12:40 Fig.12.34; 12:41|||Haines and Scrimgeour (2007). Scattered outcrops of granitoid rocks in a belt trending NW from the Utopia tantalite prospect.|||||An early phase of dark, biotite-rich granodiorite with abundant dark enclaves is intruded by leucocratic, interlayered and ?co-magmatic microgranite and porphyritic granite with a distinctive flow foliation of tabular K-feldspar phenocrysts.|12-JUL-16
81819|Molyhil Suite|73123|5|Briefly described|piii, p8, p13-14|Statherian|Statherian||ca 1.79 Ga||Narbarloo Granite, Dinkum Orthogneiss, Double Granite, Mascotte Orthogneiss|Intrudes Black Label Suite.|Felsic intrusives.|14-APR-22
81819|Molyhil Suite|73591|5|Briefly described|piii, p11, p16, p18, p30||||ca 1790 Ma|Baikal Supersuite|Dinkum Orthogneiss, Double Dam Granite, Narbarloo Granite, Mascotte Orthogneiss||Felsic granitic suite.|
79602|Moonlight Gneiss|69510|6|Mentioned|p5|Statherian|Statherian|Aileron Province, Arunta Region.|c.1770 Ma.||||Strongly foliated to locally mylonitic.|16-JAN-17
25260|Moonlight Valley Tillite|14019|5|Briefly described|p19|Neoproterozoic|Neoproterozoic|Possibly equivalent to diamictite of Duerdin Group. Age: 793 +/- 30Ma (Rb-Sr) and 610Ma. Geological Province: Wolfe Creek Basin. Correlated with Elatina Formation.||||||
25260|Moonlight Valley Tillite|22496|3|Fully described|p11||Neoproterozoic|Of the Duerdin Group. Unconformably overlies both the Illjarra Sandstone and the Eliot Range Dolomite. Geological Province: Wolfe Basin.||||||14-APR-08
25260|Moonlight Valley Tillite|22547|4|Described|p28||Neoproterozoic III|Of the Duerdin Group.  In the  Wolfe Creek Basin. Max. thickness: 280 m. Overlain by Ranford Formation.||||||07-NOV-06
25260|Moonlight Valley Tillite|22901|6|Mentioned|76 fig 2|||||||||
25260|Moonlight Valley Tillite|23314|5|Briefly described|332|||||||||
25260|Moonlight Valley Tillite|23621|4|Described|p33|||See also page 9 Table 1 - Moonlight Vally Tillite (misspelt). Of Duerdin Group. Underlain by Eliot Range Dolomite. Geological Province: Wolfe Basin.||||||09-AUG-06
25260|Moonlight Valley Tillite|23622|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Geological Province: Wolfe Basin.||||||
25260|Moonlight Valley Tillite|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|Of Duerdin Group.||||||
25260|Moonlight Valley Tillite|24173|4|Described|p25, p11 Tb.2|Neoproterozoic III|Neoproterozoic III|Of the Duerdin Group. Conformably overlain by Ranford Formation;  unconformable on Eliot Range Dolomite and Illjara Sandstone. Geological Province: Wolfe Basin. Max Thickness: 200m. Correlates with Landrigan Tillite (Kuniandi Group) to the west.||||||06-APR-05
25260|Moonlight Valley Tillite|28255|3|Fully described|p73, Tb.11 (opp. p8)|Adelaidean|Adelaidean|Of the Duerdin Group. Unconformably overlies rocks of the Auvergne Group (AUVERGNE sheet); conformably overlain by Ranford Formation and unconformably overlain in several areas by Kinevans Sandstone and Antrim Plateau Volcanics. Max. thickness: >50m.||||||09-AUG-06
25260|Moonlight Valley Tillite|30533|6|Mentioned|p21|||Correlated with Mount House Group||||||
25260|Moonlight Valley Tillite|30895|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|32660|5|Briefly described|Table 5|||||||||
25260|Moonlight Valley Tillite|32664|6|Mentioned|Map legend|Adelaidean|Adelaidean|Mention in notes||||||
25260|Moonlight Valley Tillite|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite overlain by dolomite.  sandstone, granitic clasts predominate.||||||02-DEC-04
25260|Moonlight Valley Tillite|32701|4|Described|Table 1|||Adelaidean. Of the Duerdin Group.||||||07-NOV-06
25260|Moonlight Valley Tillite|32720|6|Mentioned|p7|||Age: 739 + or - 30 my.||||||09-AUG-06
25260|Moonlight Valley Tillite|32728|6|Mentioned|Table 7|||See also Fig.16||||||
25260|Moonlight Valley Tillite|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Tillite; cobbles and boulders of quartzite, granite, dolomite, etc; laminated dolomite at top. Conformable on Blackfellow Creek Sandstone; unconformable on Angalarri Siltstone and Saddle Creek Formation.||||||27-APR-05
25260|Moonlight Valley Tillite|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group.  Tillite, laminated dolomite at top.||||||27-APR-05
25260|Moonlight Valley Tillite|34230|6|Mentioned|Plate 8|Proterozoic|Proterozoic|||||||28-OCT-04
25260|Moonlight Valley Tillite|35255|6|Mentioned|p15|||||||||
25260|Moonlight Valley Tillite|36048|6|Mentioned|p377|||||||||
25260|Moonlight Valley Tillite|36551|6|Mentioned|Table 12|||||||||
25260|Moonlight Valley Tillite|36888|4|Described|p215|||||||||
25260|Moonlight Valley Tillite|36898|6|Mentioned|p181|||||||||
25260|Moonlight Valley Tillite|37238|6|Mentioned|p355|||||||||
25260|Moonlight Valley Tillite|37462|5|Briefly described|p293|||||||||
25260|Moonlight Valley Tillite|37927|4|Described|p504|||||||||
25260|Moonlight Valley Tillite|38157|6|Mentioned|Table X|||||||||
25260|Moonlight Valley Tillite|38350|6|Mentioned|p22|||||||||
25260|Moonlight Valley Tillite|38988|6|Mentioned|Fig.4|||||||||
25260|Moonlight Valley Tillite|39210|5|Briefly described|p49|||Age||||||
25260|Moonlight Valley Tillite|39827|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25260|Moonlight Valley Tillite|40494|4|Described|p11|||||||||
25260|Moonlight Valley Tillite|41405|5|Briefly described|p206|||||||||
25260|Moonlight Valley Tillite|41429|6|Mentioned|p247|||||||||
25260|Moonlight Valley Tillite|42811|5|Briefly described|p30|||||||||
25260|Moonlight Valley Tillite|42829|5|Briefly described|p147|||||||||
25260|Moonlight Valley Tillite|43299|5|Briefly described|Map Legend||Neoproterozoic|Of Duerdin Group.||||||09-AUG-06
25260|Moonlight Valley Tillite|43303|5|Briefly described|Map Legend||Neoproterozoic|Of Duerdin Group.||||||09-AUG-06
25260|Moonlight Valley Tillite|43853|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|43855|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|44140|5|Briefly described|p300, p301 fig 4-7, p302 Tb.4-2|Neoproterozoic|Neoproterozoic|Of East Kimberley area. Up to 140 m thick. Correlated with Marinoan glaciation (670 Ma).||Duerdin Group||Overlies Frank River Sandstone unconformably. Is overlain by Jarrad Sandstone Member (Ranford Formation).|Tillite, lenses of dolomitic quartz sandstone and conglomerate; capped by pink and cream dolomite.|07-MAR-18
25260|Moonlight Valley Tillite|44230|5|Briefly described|Map Legend||Proterozoic|||||||
25260|Moonlight Valley Tillite|44317|4|Described|Table 3, p.7||Adelaidean|||||||
25260|Moonlight Valley Tillite|44318|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25260|Moonlight Valley Tillite|44324|14|Not recorded|p.10||Adelaidean|Tb.2 (Adelaidean) of Duerdin Group.||||||
25260|Moonlight Valley Tillite|44325|14|Not recorded|map legend||Adelaidean|Adelaidean.||||||
25260|Moonlight Valley Tillite|44363|5|Briefly described|p.6,14,17,21|||(Adelaidean) Duerdin Group.||||||
25260|Moonlight Valley Tillite|44364|14|Not recorded|map legend|||||||||
25260|Moonlight Valley Tillite|44868|5|Briefly described|Map Legend||Phanerozoic|||||||
25260|Moonlight Valley Tillite|45041|6|Mentioned|p45|||Refers Dow - Gemuts (1969). Corr. Areyonga Formation||||||
25260|Moonlight Valley Tillite|45047|2|Defined|p87|Adelaidean|Adelaidean|Described pp36, 40.||||||07-NOV-06
25260|Moonlight Valley Tillite|45112|6|Mentioned|p36|||||||||
25260|Moonlight Valley Tillite|45140|6|Mentioned|p59|||||||Lateral equivalent of Redbank Yard Formation.||
25260|Moonlight Valley Tillite|48927|6|Mentioned|Table 1|||Refers Dow and Gemuts (1969)||||||09-AUG-06
25260|Moonlight Valley Tillite|48931|6|Mentioned|p59|||Correlation. Refers Dow and Gemuts(1969)||||||09-AUG-06
25260|Moonlight Valley Tillite|48938|2|Defined|p68|Adelaidean|Adelaidean|||||||
25260|Moonlight Valley Tillite|48943|3|Fully described|p82|||||||||
25260|Moonlight Valley Tillite|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Unconformably overlies Spencer Sandstone and Shoal Reach Formation. Diamictite, dolostone.||||||07-NOV-06
25260|Moonlight Valley Tillite|60519|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Duerdin Group. Geological Province: Wolfe Creek Basin. Age: c. 610Ma. Massive, matrix-supported, polymictic pebble to boulder conglomerate, poorly sorted massive sandstone, larger clasts polished and striated.||||||
25260|Moonlight Valley Tillite|60682|4|Described|p17 Table 4, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Auvergne Group. Conformably overlain by Jarrad Sandstone Member and Beasly Knob Member. Age: 739 +/- 30Ma. Max. thickness: >130m. Geological Province: Wolfe Creek Basin. Diamictite, dolostone.||||||03-MAY-05
25260|Moonlight Valley Tillite|63458|5|Briefly described|p871-874, p877 Tb.1.  |Cryogenian|Cryogenian|East Kimberley region. Dolostone facies deposited by turbidity currents. Isotopic and elemental composition of carbonate unit given. The 'cap dolomicrite' facies is dealt with in detail. See also p883-884, p886-889, p891-p901.||Unit in Duerdin Group.||Overlies Frank River Sandstone. Correlated with Elatina Formation, Landrigan and Walsh Tillites. Is overlain by Ranford Formation.|Uppermost unit is ca. 9 m thick, thinly bedded, cream-pink dolomicrite, which overlies pebble-bearing mudstone and siltstone.|
25260|Moonlight Valley Tillite|63762|5|Briefly described|p19|||See also Moonlight Valley Formation.||||||07-FEB-11
25260|Moonlight Valley Tillite|64104|6|Mentioned|p63|Neoproterozoic|Neoproterozoic|The author proposes this name be replaced by Moonlight Valley Formation "to distinguish stratigraphic terms from genetic interpretation".||||||
25260|Moonlight Valley Tillite|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Diamictite, dolostone ||||||
25260|Moonlight Valley Tillite|65337|5|Briefly described|p94.|Neoproterozoic|Neoproterozoic|One of youngest known units underlying Antrim Plateau Volcanics. Correlated with Marinoan glacial event (late Cryogenian - early Ediacaran) in Adelaide Rift.||||||
25260|Moonlight Valley Tillite|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Unconformably overlies Blackfellow Creek Sandstone. Is overlain by Ranford Formation.|Diamictite; laminated dolostone at top.|
25260|Moonlight Valley Tillite|67484|6|Mentioned|p295 Fig.2|Cryogenian|Cryogenian|More commonly referred to as the Moonlight Valley Formation in the text; see also p294-296.||Of the Duerdin Group.||Overlies Frank River Sandstone. Is overlain by Ranford Formation.||
25260|Moonlight Valley Tillite|68244|6|Mentioned|p671|||East Kimberly area, Kimberley region. [Potentially referring specifically to glaciogenic tillitic units within the Moonlight Valley Formation? Or alternate nomenclature to Moonlight Valley Formation].||||||
25260|Moonlight Valley Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
25260|Moonlight Valley Tillite|68473|6|Mentioned|p531-532|||||Duerdin Group||||
25260|Moonlight Valley Tillite|68733|5|Briefly described|p177 Fig.2, p188, p189 Fig.8|Cryogenian|Cryogenian|Victoria and Wolfe Basin.||Of the Duerdin Group.|||Glacigenic sediments.|05-DEC-17
25260|Moonlight Valley Tillite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Ediacaran||Wolfe Creek Basin.||Duerdin Group|Includes unnamed finely laminated mudstone and siltstone member||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally; includes finely laminated mudstone and siltstone member.|30-AUG-18
25260|Moonlight Valley Tillite|69165|4|Described|100k_interpgeop_lut.csv|Ediacaran|Ediacaran|See also 100k_xsecgeop_lut.csv. ||Duerdin Group|||Massive, matrix supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally. Finely laminated mudstone and siltstone.|
25260|Moonlight Valley Tillite|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Overlies Blackfellow Creek Sandstone. Is overlain by Ranford Formation.||12-JUL-16
25260|Moonlight Valley Tillite|69441|6|Mentioned|p26:1|||Wolfe Basin.||||Correlated with Olympic and Elatina Formations.||12-JUL-16
25260|Moonlight Valley Tillite|69442|5|Briefly described|p27:1-6|||Wolfe Basin. Over 280m thick. Glacial deposits; recognisable by abundant erratics on the residual weathering surface. Represents a continental ice sheet deposit; forms a local striated pavement. Correlated with Uniya Formation, and Elatina Formation (Adelaide Fold Belt).|?635 Ma.|Duerdin Group.||Unconformably overlies Auvergne Group. Is overlain conformably by Beasly Knob Member and (presumably) Jarrad Sandstone Member. Partial lateral equivalent of Bucket Spring Member (Ranford Formation).|Diamictite, dolostone "cap". Erratics are flattened, subrounded, striated, gouged and chatter-marked cobbles and boulders. The most common dropstones are orthoquartzite, sandstone, meta-siltstone, schist, volcanic rocks, granite and dolostone.|12-JUL-16
25260|Moonlight Valley Tillite|69445|5|Briefly described|p30:4, 10, 17|Neoproterozoic|Neoproterozoic|Woolfe Basin. Minor displacement occurs along the Blackfella Creek Fault.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
25260|Moonlight Valley Tillite|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.|||Massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally; finely laminated mudstone and siltstone|
25260|Moonlight Valley Tillite|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|||Tillite with flattened, subrounded, striated and gouged cobbles and boulders.|
25260|Moonlight Valley Tillite|70154|4|Described|100k_interpgeop_lut.csv|Ediacaran|Cryogenian||541-850 Ma|Duerdin Group|||Massive matrix supported polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; finely laminated mudstone and siltstone.|
25260|Moonlight Valley Tillite|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Diamictite, dolostone.|
25260|Moonlight Valley Tillite|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Duerdin Group.||Shown as unconformably overlying Blackfellow Creek Sandstone. Is shown as overlain by Ranford Formation, Antrim Plateau Volcanics.|Diamictite; laminated dolostone at top.|21-JAN-22
25260|Moonlight Valley Tillite|71267|4|Described|GEOL_LUT_CSV files|Cryogenian|Cryogenian|Geological province: Halls Creek Orogen. Of Wolfe Basin, Centralian Superbasin. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|720-635 Ma (inferred)|Unit of Duerdin Group.|||Finely laminated mudstone and siltstone; massive, matrix-supported, polymictic pebble to boulder conglomerate and poorly sorted massive sandstone; larger clasts in conglomerate are polished and striated locally.|
25260|Moonlight Valley Tillite|73083|6|Mentioned|p48||||||||Includes siltstone.|
25260|Moonlight Valley Tillite|73255|4|Described|p532-535, p537, p539, p541-546, p548-550|Ediacaran|Cryogenian|Correlated with the Elatina Glaciation (Corkeron, 2008). 'Cap carbonate' sandstones comprise the top 8-10m of the unit. Base of the Ediacaran is at the base of the 'cap carbonate', 635 Ma. Trough cross-bedded dolomitic sandstone facies deposited in fluvial paleochannels. Evidence of paleosols includes dessication cracks, mineral weathering trends of dolomite, Rivularites repertus microbial trace fossils. Dolomite likely sourced from glacial erosion of the Bungle Bungle Dolomite. Soil type of  paleosols in the upper parts of the unit interpreted as calcic xerosols. Mean annual precipitation estimated to be 265-325 mm based on paleosols, mean annual range of precipitation of 37-48 mm, cool to frigid temperatures. Contains Palaeopascichnus and Yangtziramulus fossils in upper parts. Common early burial alterations include gleisation. Specific locations in text include p534 Fig.2, p539 Fig.6, p542 Fig.10.|635 Ma|Duerdin Group||Overlies the Frank River Sanddstone, conformably underlies the Ranford Formation and Jarrad Member.|Upper 'cap carbonate' contains abundant dolomitic sandstone. Includes trough cross-bedded, medium to coarse dolomitic sandstone, fine-grained sandstone and siltstone laminae between dolomitic sandstone beds, some sandstones contain dolomitic nodules.|
25731|Mordor Igneous Complex|22524|5|Briefly described|p37||Stenian|||||||23-JUL-12
25731|Mordor Igneous Complex|23844|6|Mentioned|p10, p54 Tb.1|||Geological Province: Arunta Province. Name used interchangeably with Mordor Complex. See also Fig.25||||||
25731|Mordor Igneous Complex|24047|5|Briefly described|p10|Mesoproterozoic|Mesoproterozoic|Age: 1200Ma.  Geological Province: Arunta province.||||||
25731|Mordor Igneous Complex|24540|5|Briefly described|p5, p11|||Age: 1150Ma (Rb-Sr and Sm-Nd methods); and, 1132+/-4Ma (SHRIMP U-Pb zircon). Geological Province: Arunta region. Not related to Mud Tank Carbonatite Complex as has been previously suggested.||||||07-FEB-11
25731|Mordor Igneous Complex|36526|6|Mentioned|p154|||||||||
25731|Mordor Igneous Complex|37462|5|Briefly described|Tab.4.VIII|||See also p280.||||||07-NOV-06
25731|Mordor Igneous Complex|38606|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25731|Mordor Igneous Complex|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25731|Mordor Igneous Complex|39552|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25731|Mordor Igneous Complex|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
25731|Mordor Igneous Complex|39610|4|Described|p14|||See also p6.||||||07-NOV-06
25731|Mordor Igneous Complex|39888|6|Mentioned|p464|||||||||
25731|Mordor Igneous Complex|41125|6|Mentioned|p10|||||||||
25731|Mordor Igneous Complex|41509|6|Mentioned|p4|||||||||
25731|Mordor Igneous Complex|42481|6|Mentioned|Fig.1 P183|||||||||
25731|Mordor Igneous Complex|43595|6|Mentioned|p448|||Age: 1185 Ma||||||
25731|Mordor Igneous Complex|43715|6|Mentioned|p28|||||||||
25731|Mordor Igneous Complex|43749|6|Mentioned|p31|||Age: 1200 Ma||||||
25731|Mordor Igneous Complex|43806|6|Mentioned|p365|||Age: 1100-1200 Ma.||||||07-NOV-06
25731|Mordor Igneous Complex|44114|5|Briefly described|p316, 335, 340-341|||Southern Arunta Inlier. Intruded during the Teapot magmatic event. Early Rb-Sr isochron ages are 1128 +/- 20 Ma and 1118 +/- 17 Ma (Langworthy and Black, 1978).|~1150 Ma.||||Alkaline.|
25731|Mordor Igneous Complex|46830|6|Mentioned|p23|||||||||
25731|Mordor Igneous Complex|46868|6|Mentioned|p79|||||||||
25731|Mordor Igneous Complex|48992|1|Redefined|p33|Neoproterozoic|Neoproterozoic|||||||
25731|Mordor Igneous Complex|50246|5|Briefly described|p5, p10|Mesoproterozoic|Mesoproterozoic|Ages:1150-1130Ma, 1132+/-5Ma and 1135+/-5Ma. Plug-like alkaline body within the Mordor Pound. Includes Palaeoproterozoic schist, gneiss, amphibolite forming the floor of the Pound. The walls are capped by Heavitree Quartzite. See also p19 Fig.1, p21 Fig.3||||||07-FEB-11
25731|Mordor Igneous Complex|50369|6|Mentioned|p26.2|||||||||
25731|Mordor Igneous Complex|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Phlogopite, peridotite, shonkinite, monzonite, syenite, pegmatite, diorite, ultramafic rock.||||||
25731|Mordor Igneous Complex|60668|5|Briefly described|p2 Tb. 1, p16|||See also Mordor Complex - names are used interchangeably. Alkaline ultramafic plugs. See also Fig.21a and 21b.||||||
25731|Mordor Igneous Complex|61154|5|Briefly described|p34|||Alkaline rocks. Emplaced at 1132+/-5Ma in the Strangways Range area near southern margin of the Aileron Province.||||||08-MAR-13
25731|Mordor Igneous Complex|62595|4|Described|p4, p7, p10, p32 Figs.10 & 11.|Stenian|Stenian|Eastern Arunta region. The main manifestation of the 1150-1130 Ma Teapot Event. Hosts the Mithril orthomagmatic PGE-Au-Cu-Ni prospects associated with ultramafic rocks.|1132 +/- 5 Ma )Claoue-Long and Hoatson 2005).|||Is overlain by thrust-faulted Heavitree Quartzite.|A plug-like alkaline igneous suite, including syenite, monzonite, phlogopite-plagioclase-clinopyroxene pyroxenite, layered ultramafics.|
25731|Mordor Igneous Complex|64500|6|Mentioned|p643 fig 1, p645 fig 2.|Mesoproterozoic|Mesoproterozoic|There is a typo (Igneos) in fig.2. See also references to Mordor Alkaline Igneous Complex (p641-645, p660) and to Mordor Complex (p642, p643). Petrology and geochemistry described in detail.|||||Includes syenite, porphyritic pyroxene syenite, pyroxene syenite (phlogopite-pyroxenite), and mafic-ultramafic rocks: dunite and peridotite.|
25731|Mordor Igneous Complex|64738|6|Mentioned|p248.|||Emplaced to the south of the Strangways Metamorphic Complex by the Teapot Event (~1130 Ma). Alkaline.|c.1130 Ma.|||||
25731|Mordor Igneous Complex|66860|6|Mentioned|p6 Tb.1, p2 fig 2|||Of Arunta Region.|1132 Ma.|||||
25731|Mordor Igneous Complex|67127|6|Mentioned|p87, p98, p100, p107, p109|||Arunta region, NT. Located in a zone that also contains the Nolans Bore REE 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. Previously explored for REE, PGEs, Ni, Cu, Cr, diamonds and vermiculite-phlogopite.|||||Alkaline ultramafic rocks.|
25731|Mordor Igneous Complex|69427|5|Briefly described|p12:45 Fig.12.38|||Generally abbreviated in this work to Mordor Complex: see references (12:2, 9, 40 Fig.12.34; 12:45-46, 51).|||||Syenite and minor granitic gneiss; monzonite; pyroxenite and shonkinite; phlogopite pyroxenite, phlogopite olivine pyroxenite, lherzolite and wehrlite.|12-JUL-16
25731|Mordor Igneous Complex|69925|6|Mentioned|p21|||||||Intrudes Randall Peak Metamorphics.||
25731|Mordor Igneous Complex|69937|5|Briefly described|p31|||Aileron Province, NW of Alice Springs. Possible source of some zircons in the Cyclops Member of the Pertatataka Formation.|~1130 Ma.|||||
25731|Mordor Igneous Complex|73551|6|Mentioned|p1, p23|Stenian|Stenian|Aileron Province, southern.|ca 1.13 Ga|||||
30269|Moroak Sandstone|23937|2|Defined|p86 App. 1|Calymmian|Calymmian|Supersedes Moroak Sst Mbr (McMinn Fm) - upgraded to formation status in Maiwok Subgp (Roper Gp). Upper beds assigned to Sherwin Fm. Also replaces "Broadmere Sst mbr". Overlain by Sherwin Fm; disconformably overlies Velkerri Fm.  Geol.Prov: McArthur Basin.||||||
30269|Moroak Sandstone|24047|5|Briefly described|p23|||Geological Province: McArthur Basin.||||||
30269|Moroak Sandstone|61250|5|Briefly described|p43|Mesoproterozoic|Mesoproterozoic|Contains rich petroleum systems. Geological Province: Beetaloo Sub-basin.||||||27-MAY-06
30269|Moroak Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Quartz sandstone: thin to medium bedded, fine grained, trough cross bedded, ripple marks; interbedded siltstone and mudstone.||||||
30269|Moroak Sandstone|62759|5|Briefly described|p1|Mesoproterozoic|Mesoproterozoic|Geological Province: Beetaloo Sub-basin. Contains oil reservoirs.||||||05-FEB-08
30269|Moroak Sandstone|64784|4|Described|p2-10     |Proterozoic|Proterozoic|Beetaloo Basin. An economically significant reservoir target; between the two major source units.||Unit in Roper Group.||Conformably? underlies the Kyalla Formation and unconformably? overlies the Velkerri Formation.|Consists of predominantly fine to coarse quartz sandstone. Occasionally it contains some anhydrite cement and commonly has authigenic silica cement. Overall cleaning-upward and coarsening upward trend.|
30269|Moroak Sandstone|65236|5|Briefly described|p2, p3 Fig. 3, p4 Fig. 4|Mesoproterozoic|Mesoproterozoic|Overlies Velkerri Formation. Geological province: Beetaloo Sub-basin.||||||04-JUN-09
30269|Moroak Sandstone|65342|6|Mentioned|p8.|||Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 407 m.||Unit in Roper Group.||Is overlain by Kyalla Formation.||
30269|Moroak Sandstone|69018|5|Briefly described|p450 Fig.1b|Calymmian|Calymmian|||Of Roper Group.||||
30269|Moroak Sandstone|69430|4|Described|p15:3, 27-30, 53, 62|Calymmian|Calymmian|Abbott et al. (2001) who raised the unit to Formation status and defined it. Originally (Dunn, 1963) the Moroak Sandstone Member of the McMinn Formation. An overlying succession of interbedded sandstone, siltstone and mudstone, originally part of the unit, was reassigned to the overlying Sherwin Formation by Abbott et al. (2001). Southern McArthur Basin. 2.5-420m thick. Coastal tidal platform sediments. Fair to good conventional hydrocarbon reservoirs occur, and has potential for unconventional reservoirs (basin-centred gas). Occurs between two significant source rocks (Velkerri and Kyalla Formations; may be sealed by Kyalla Formation.||Maiwok Subgroup.||Disconformably overlies Velkerri Formation. Is overlain conformably and gradationally by Sherwin Formation.|Upward-coarsening, thinly to medium bedded, medium to fine quartz sandstone; coarse-grained and quartz-granule intervals up to 1m thick near the base.|12-JUL-16
30269|Moroak Sandstone|69673|6|Mentioned|p20, p32, p33, p37, p38, p40, p44, p46|||Southern McArthur Basin. Conventional reservoir potential. Up to 485m thick.||Maiwok Subgroup||Disconformably overlies Velkerri Formation, Overlain by Sherwin Formation, Conformably overlain by Kyalla Formation||
30269|Moroak Sandstone|70734|6|Mentioned|p14|||McArthur Basin. See also Moroak Sandstone Member p16, p17||||Overlies Velkerri Formation.||
30269|Moroak Sandstone|70822|5|Briefly described|p102 fig 1 (A), p104|Mesoproterozoic|Mesoproterozoic|||Roper Group||Overlies Velkerri Formation; overlain by Sherwin Ironstone.|Cross-bedded sandstone.|
30269|Moroak Sandstone|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Moroak. McArthur Basin.||||||
30269|Moroak Sandstone|70968|3|Fully described|p51, p65-69, p74-75, p126-127, p131|Ectasian|Ectasian|See also p133, p140, p143. Sweet in Abbott et al. (2001) after Dunn (1963). Named after Moroak Station, presumably after Morok [sic] Creek. Previously the Moroak Sandstone Member of McMinn Formation (Dunn, 1963); raised to Formation status, along with the other Members, by Abbott et al. (2001) and the name McMinn was abandoned. The type section, on the northern slopes of Mount McMinn, is at 432800mE 8375100mN in URAPUNGA sheet; a new section is required as this location is no longer accessible. Resistant unit: forms low cuestas, benches and pavements. Variable thickness from 2.5m up to 482.9m. High-energy, tide-dominated shoreline to shallow shelf deposits. Detrital zircon diagram.||Maiwok Subgroup.||Conformably overlies Velkerri Formation. Is overlain conformably and gradationally by Sherwin Formation or Kyalla Formation. Is intruded by Derim Derim Dolerite sills.|Flaggy to blocky, medium- to fine-grained quartz sandstone with minor quartz granule-rich coarse-grained sandstone, conglomerate and siltstone interbeds. Well-developed siliceous cement. Minor sedimentary ironstone near the top locally.|16-NOV-17
30269|Moroak Sandstone|71059|4|Described|p3, p10, p20|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 2.5-420m thick. Coastal tidal platform deposits. Estimated shale/tight gas/shale oil and condensate resources detailed. Organic petrology reflectivity data tabulated.||Maiwok Subgroup.||Overlies Velkerri Formation conformably / locally disconformably. Is overlain conformably and gradationally by Kyalla Formation.|Fine and medium to coarse and minor granule-rich quartz sandstone; minor conglomerate and siltstone.|
30269|Moroak Sandstone|71488|4|Described|p140-p153|Ectasian|Ectasian|Beetaloo Sub-basin. Ages are interpreted as maximum depositional ages. The youngest age is from the underlying Velkerri Formation. Deposited in a high-energy tide-dominated shoreline to shallow shelf setting. Zircon geochronology results are briefly discussed. Referred to as the Moroak Formation on p153.|1308 +/- 41 Ma|Maiwok Subgroup||Conformably overlies the Velkerri Formation and overlies the Bessie Creek Sandstone. Overlain by the Sherwin Ironstone. Unconformably overlain by the Jamison sandstone.|Fine to medium quartz sandstones.|02-MAY-18
30269|Moroak Sandstone|71779|5|Briefly described|p2, p6, p12 fig 9, p16-p17, p23, 26|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin. See also Figs on  p10, 11, p19.||Maiwok Subgroup||Overlies the Wyworrie Member of Velkerri Formation.|Medium-grained sandstone.|23-FEB-20
30269|Moroak Sandstone|71893|4|Described|p2-p5, p8, p32-p35|Calymmian|Calymmian|McArthur Basin. A maximum depositional age of 1570 +/- 15 Ma and a youngest individual age of 1406 +/- 78 Ma were obtained. Age is constrained by Re-Os dates of 1417 +/- 29 Ma and 1361 +/- 21 Ma from the underlying Kalala and Wyworrie Members of the Velkerri Formation and a minimum age is derived from U-Pb TIMS baddeleyite age of 1312.9 +/- 0.7 Ma for the intruding Derim Derim Dolerite. Deposited in a high energy, tide dominated shoreline to shallow marine shelf setting. Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.  Intruded by the Derim Derim Dolerite.||Maiwok Subgroup||Conformably (to locally disconformably) overlies the Velkerri Formation. Conformably overlain by the Sherwin Formation. Overlain by the Kyalla Formation.|Thinly- to medium-bedded, predominantly medium- to fine-grained quartz sandstone with coarse grained and granule-rich intervals.|
30269|Moroak Sandstone|72381|4|Described|p771-775,777-778|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Deposited in a similar environment as Bessie Creek Sandstone (high-energy tide dominated shoreline to shallow shelf setting). Intersected in Elliott-1 and Jamison-1 drillholes, and U-Pb zircon dating and Hf isotopic analysis was undertaken (this study). Deposited between c. 1350 and c. 1313 Ma, coeval with subduction-related magmatism, orogeny and metamorphism between the West Australian Craton, and combined North and South Australian Cratons (see p779 for references). Sample EN-Mo8 returned dominant age peak at c. 1700 Ma and minor peak at c. 1560 Ma. Characterised by different detrital zircon age spectra and Hf isotopic results from the Bessie Creek Sandstone; Moroak Sandstone show Hf isotopic signature similar to those from Mount Isa Province or Gawler Craton. Hafnium isotopic data reported by Munson et al (2018) from the Urupunga Fault Zone to the north indicate that the Walton High, or the Mallapunyah Fault may have acted as a bathymetric high during deposition between the Urupunga Fault Zone and the Beetaloo Sub-basin.||Unit of Mailwok Subgroup.||Overlain by Kyalla Formation. Underlain by Velkerri Formation. Intruded by Derim Derim Dolerite.|Fine to medium-grained quartz sandstones.|
30269|Moroak Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Ectasian|Calymmian|Shown as located in the Urapunga Fault Zone, Beetaloo Sub-basin and northern part of the Batten Fault Zone.||Maiwok Subgroup||Overlies Velkerri Formation and underlies Sherwin Formation.||
30269|Moroak Sandstone|72718|6|Mentioned|p7, p10|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north). Notable seismic reflector (coherent impedance boundaries) used for calibration of well-logs and are continuous over long distances; however, gradational change in acoustic impedance is noted at a regional scale.||Maiwok Subgroup, Roper Group||Underlain by Velkerri Formation. Overlain by Sherwin Formation.||
30269|Moroak Sandstone|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Maiwok Subgroup||Overlies Velkerri Formation and underlies Sherwin Formation.||
30269|Moroak Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Velkerri Formation. Overlain by Sherwin Formation.||
30269|Moroak Sandstone|73242|5|Briefly described|p39|||||Maiwok Subgroup, Roper Group||Underlain by Wyworrie Member, Velkerri Formation. Overlain by Sherwin Ironstone.|Includes tidal Sandstone.|
30269|Moroak Sandstone|73412|5|Briefly described|p4|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Velkerri Formation. Is overlain by Sherwin Formation.||
24389|Mount Airy Orthogneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|In the Arunta Block.||||||07-NOV-06
24389|Mount Airy Orthogneiss|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||07-NOV-06
24389|Mount Airy Orthogneiss|23316|6|Mentioned|p357|||Contains a greenschist-facies shear zone.  In Sandy Creek area. Mount is Mt in text.||||||07-FEB-07
24389|Mount Airy Orthogneiss|24197|5|Briefly described|p19, p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Harverson Suite. Coarse-grained, grey, granitic augen gneiss. Age: ~1820Ma. Geological province: Arunta Inlier.||||||07-FEB-11
24389|Mount Airy Orthogneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24389|Mount Airy Orthogneiss|39888|6|Mentioned|Fig.8|||||||||
24389|Mount Airy Orthogneiss|42146|6|Mentioned|p652|||||||||
24389|Mount Airy Orthogneiss|42217|6|Mentioned|p417|||||||||
24389|Mount Airy Orthogneiss|42326|5|Briefly described|Table 2 P11|||||||||
24389|Mount Airy Orthogneiss|48992|2|Defined|p34|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24389|Mount Airy Orthogneiss|50369|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Haverson Suite.||||||07-NOV-08
24389|Mount Airy Orthogneiss|64956|5|Briefly described|p3 Tb. 1, p23|Paleoproterozoic|Paleoproterozoic|Cryst. age: 1799+/-3Ma. Geological province: Arunta region. Sample is biotite granite containing K-feldspar megacrysts and muscovite.||||||07-FEB-11
24389|Mount Airy Orthogneiss|65338|6|Mentioned|p15, p21.|Statherian|Orosirian|Age said to be in the 1820-1770 Ma range.||||Intrudes Lander Rock Formation.|Widely-distributed, rapakivi textured gneissic granite.|
24389|Mount Airy Orthogneiss|69226|6|Mentioned|p239|||Reynolds-Anmatjira Ranges region.||||||
24389|Mount Airy Orthogneiss|69228|6|Mentioned|p370|||Sandy Creek, Arunta Inlier. Associated with a shear zone that hosted fluid flow. Isotope values and metamorphism described.||||||
24389|Mount Airy Orthogneiss|69427|5|Briefly described|p12:20 Fig.12.19; 12:21, 26|Statherian|Orosirian|Aileron Province. SHRIMP U-Pb zircon age.|1799 +/- 3 Ma (Worden et al., 2008).||||Foliated to gneissic megacrystic granite; biotite-bearing and characterised by coarse phenocrysts of K-feldspar with locally developed rapakivi textures.|12-JUL-16
24389|Mount Airy Orthogneiss|70376|6|Mentioned|p833 fig 2|Paleoproterozoic|Paleoproterozoic|||||||
24389|Mount Airy Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1799+/-2.6 Ma crystallisation: U-Pb zircon SHRIMP||||Granite.|
24389|Mount Airy Orthogneiss|71858|6|Mentioned|p5|||Aileron Province.||||||
24389|Mount Airy Orthogneiss|73399|6|Mentioned|p2, App.E|||||||||
79394|Mount Bleechmore Carbonatite|69427|6|Mentioned|p12:40 Fig.12.34|||Also called the Bleechmore dykes. A swarm of carbonatite dykes, in the same area but distinct from the Mud Tank Carbonatite. Considered to be a vermiculite resource in a 500x50 to 100 m. area. Age, unit relationships not discussed, but broad geographic association with Mud Tank Carbonatite which is Neoproterozoic.||||||08-FEB-23
26755|Mount Bleechmore Granulite|23844|6|Mentioned|p41|||On ALCOOTA Sheet||||||
26755|Mount Bleechmore Granulite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Jervois ?Suite (Jervois presented in Table 4.1 in isolation). Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26755|Mount Bleechmore Granulite|33103|4|Described|Table 1|||Mention p3.||||||07-NOV-06
26755|Mount Bleechmore Granulite|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
26755|Mount Bleechmore Granulite|38829|6|Mentioned|p132|||||||||
26755|Mount Bleechmore Granulite|39887|6|Mentioned|Fig.5|||||||||
26755|Mount Bleechmore Granulite|39888|6|Mentioned|Appendix|||||||||
26755|Mount Bleechmore Granulite|48992|6|Mentioned|p50|||||||||
26755|Mount Bleechmore Granulite|50369|5|Briefly described|p1.4, 9.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jervois Suite.||||||07-NOV-08
26755|Mount Bleechmore Granulite|61208|5|Briefly described|p210-211, p207 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: ca.1.8Ga. Geological Province: eastern Arunta Inlier. Mount is Mt in text.||||||07-NOV-08
26755|Mount Bleechmore Granulite|62595|6|Mentioned|p3. |||Included in Scrimgeour's (2003) Ongeva package.||||||
26755|Mount Bleechmore Granulite|64574|5|Briefly described|p704 Fig. 1, p706, p716, p717|Paleoproterozoic|Paleoproterozoic|Mount is Mt in text. Age: 1800Ma for deposition.||||||
26755|Mount Bleechmore Granulite|69427|4|Described|p12:13, 28, 34, 38-39, 44|||Shaw et al. (1979). Crops out at Mount Bleechmore on Alcoota station, Aileron Province. May be related to Delny Metamorphics. SHRIMP U-Pb detrital zircon maximum deposition age; zircon rims record metamorphism at c.1780 and 1730 Ma (Strangways Event) and resetting at 1713 +/- 7 Ma (Beyer et al., 2010); also overgrowths with LA-ICPMS U-Pb age of 1554 +/- 16 Ma.|<1810-1800 Ma (Maidment et al., 2005).|||Is overlain unconformably by Mendip Metamorphics.|Dominantly pelitic to psammopelitic biotite- and garnet-bearing migmatite, with sillimanite and cordierite in more aluminous layers. More quartz-rich metapsammite layers are common. Mafic granulite is common in the E.|12-JUL-16
27066|Mount Bonnie Formation|22810|5|Briefly described|Table2 P4|||Interbedded with and overlies Gerowie Tuff. Maximum thickness: 500m.||||||07-NOV-06
27066|Mount Bonnie Formation|23122|5|Briefly described|p409, Fig.2, 410|||||||||
27066|Mount Bonnie Formation|23205|6|Mentioned|p42|||In the Pine Creek Inlier.||||||07-NOV-06
27066|Mount Bonnie Formation|23337|5|Briefly described|907|||||||||
27066|Mount Bonnie Formation|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 7 Table 1, page 13. Of South Alligator Group. Max. thickness: 700 m.||||||
27066|Mount Bonnie Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the South Alligator Group, in the Rum Jungle and Central Regions||||||
27066|Mount Bonnie Formation|23733|5|Briefly described|p32 Fig. 19, p5|||Of South Alligator Group.  Geological Province: Pine Creek Orogen.  See also p30.||||||
27066|Mount Bonnie Formation|23999|6|Mentioned|p44|||Mentioned only in connection with "rooster red" washed and screened pebbles for landscaping purposes.||||||12-APR-12
27066|Mount Bonnie Formation|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.  Age: 1885Ma.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
27066|Mount Bonnie Formation|24197|5|Briefly described|p25, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier. Contains Au deposits.||||||07-FEB-11
27066|Mount Bonnie Formation|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
27066|Mount Bonnie Formation|24442|5|Briefly described|p27, p44|Paleoproterozoic|Paleoproterozoic|Age: 1885+/-2Ma (SHRIMP zircon).  Mount is Mt in text.||||||07-NOV-08
27066|Mount Bonnie Formation|38349|6|Mentioned|Table 4|||||||||
27066|Mount Bonnie Formation|38351|6|Mentioned|Table 3|||||||||
27066|Mount Bonnie Formation|39357|6|Mentioned|p3|||See also p2.||||||07-NOV-06
27066|Mount Bonnie Formation|39518|3|Fully described|p7|||||||||
27066|Mount Bonnie Formation|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27066|Mount Bonnie Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27066|Mount Bonnie Formation|39801|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Reddish-brown siltstone and shale with minor interbeds of tuffaceous siliceous siltstone, banded iron formation, greywacke and rare siltstone beds containing chert nodules.||||||12-APR-12
27066|Mount Bonnie Formation|40168|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Shale, mudstone, phyllite, siltstone, medium feldspathic greywacke, minor tuffaceous chert, glassy black crystal tuff, victric tuff, lithic crystal tuff, carbonaceous shale and rare bif.||||||12-APR-12
27066|Mount Bonnie Formation|40223|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group. Siltstone and slate with minor laminated black chert bands, lenses and nodules, massive medium to coarse feldspathic greywacke; minor banded iron formation, argillite, crystal tuff and tuffaceous chert.||||||12-APR-12
27066|Mount Bonnie Formation|40243|6|Mentioned|Fig.2|||||||||
27066|Mount Bonnie Formation|40495|6|Mentioned|Fig.5|||||||||
27066|Mount Bonnie Formation|40808|5|Briefly described|Table 2|||||||||
27066|Mount Bonnie Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27066|Mount Bonnie Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27066|Mount Bonnie Formation|41125|6|Mentioned|Fig.14|||||||||
27066|Mount Bonnie Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27066|Mount Bonnie Formation|41305|3|Fully described|p17|||||||||
27066|Mount Bonnie Formation|41309|4|Described|p6|||||||||
27066|Mount Bonnie Formation|41311|4|Described|p10|||||||||
27066|Mount Bonnie Formation|41397|4|Described|p3|||||||||
27066|Mount Bonnie Formation|41466|6|Mentioned|p23|||||||||
27066|Mount Bonnie Formation|41860|5|Briefly described|p443|||Also known as Kapalga Formation.||||||07-NOV-06
27066|Mount Bonnie Formation|41873|5|Briefly described|Table 2|||||||||
27066|Mount Bonnie Formation|41874|5|Briefly described|p11|||||||||
27066|Mount Bonnie Formation|41877|5|Briefly described|p27|||||||||
27066|Mount Bonnie Formation|41878|6|Mentioned|p38|||Informally divided into Upper and Lower parts.||||||
27066|Mount Bonnie Formation|42012|3|Fully described|p9|||See also Table 1 p7.||||||07-NOV-06
27066|Mount Bonnie Formation|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
27066|Mount Bonnie Formation|42163|5|Briefly described|p61|||||||||
27066|Mount Bonnie Formation|42756|6|Mentioned|p7|||||||||
27066|Mount Bonnie Formation|43140|4|Described|p3||Paleoproterozoic|Of the South Alligator Group.||||||07-NOV-08
27066|Mount Bonnie Formation|43187|5|Briefly described|p2|||||||||
27066|Mount Bonnie Formation|43624|6|Mentioned|Table 1,p9||Paleoproterozoic|Mount is Mt. in text.  Max. thickness: 400m.||||||07-NOV-08
27066|Mount Bonnie Formation|43718|6|Mentioned|p10|||Age: 1885+/-2 Ma (U-Pb Shimp).||||||07-NOV-06
27066|Mount Bonnie Formation|43832|3|Fully described|18-19,Table3 p12, 97||Paleoproterozoic|Age 1885+-2 Ma. Gerowie Tuff underlies, Burrell Creek Formation overlies.||||||07-NOV-08
27066|Mount Bonnie Formation|46658|5|Briefly described|p550|||||||||
27066|Mount Bonnie Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.  Reddish-brown siltstone and shale; minor silicified tuffaceous shale, feldspathic greywacke; rare chert nodules and thin beds of banded iron formation. Conformably overlain by Burrell Creek Formation.||||||07-NOV-08
27066|Mount Bonnie Formation|46700|6|Mentioned|P21|||||||||
27066|Mount Bonnie Formation|47049|5|Briefly described|Table|||Replaces Kapalga Formation west of Waterfall Creek Fault.||||||
27066|Mount Bonnie Formation|50586|5|Briefly described|p1.1, 4.5, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite. Intruded by Cullen Supersuite.||||||07-NOV-08
27066|Mount Bonnie Formation|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Of South Alligator Group.||||||07-NOV-08
27066|Mount Bonnie Formation|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of South Alligator Group. Laminated reddish brown shale and siltstone with minor laminated black chert bands, lenses and nodules, minor pyritic banded iron formation, argillite, crystal tuff, tuffaceous chert, greywacke, dolomite. Overlies Gerowie Tuff||||||07-NOV-06
27066|Mount Bonnie Formation|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the South Alligator Group.||||||
27066|Mount Bonnie Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Multi-coloured laminated siliceous, argillaceous and tuffaceous siltstone; banded iron formation and massive feldspathic greywacke, chert bands and nodules. Overlies Gerowie Tuff; overlain by Burrell Creek Formation. Of South Alligator Group.||||||07-NOV-06
27066|Mount Bonnie Formation|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the South Alligator Group.  Geological Province: Pine Creek Orogen. Interbedded carbonaceous sericitic and commonly pyritic or choritic slate, phyllite, mudstone and siltstone.||||||14-JAN-05
27066|Mount Bonnie Formation|60684|6|Mentioned|p19|||Geological Province: Pine Creek Geosyncline.||||||28-APR-05
27066|Mount Bonnie Formation|61389|5|Briefly described|Map Legend|||Of the South Alligator Group. Red-brown siltstone & shale, minor tuffaceous siliceous siltstone, BIF, greywacke.||||||
27066|Mount Bonnie Formation|62375|5|Briefly described|p9, 10 Fig. 3, 23|Paleoproterozoic|Paleoproterozoic|Tuffaceous Sediments. Age: 1885 +/- 2Ma. Of the South Alligator Group. Conformably underlies Burrell Creek Formation; overlies Gerowie Tuff.||||||09-FEB-10
27066|Mount Bonnie Formation|62378|5|Briefly described|p8|||Geological Province: Pine Creek Orogen. Overlies Gerowie Tuff conformably.||||||
27066|Mount Bonnie Formation|63866|5|Briefly described|p109|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. The numeric age is an ID-TIMS date.|1877 +/- 11 Ma (Needham et al., 1988)|South Alligator Group||||
27066|Mount Bonnie Formation|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1863Ma. Of South Alligator Group. Max thick.1200m. Interbeds carbonaceous sericitic and pyritic/chloritic slate, phyllite, mudst and siltst; fine/coarse feldspath metagreywacke; ferrug. phyllite (metasiltst) with chert bands, lenses and nodules.||||||07-JAN-09
27066|Mount Bonnie Formation|64730|5|Briefly described|p125 Fig. 3, p126, p139|Paleoproterozoic|Paleoproterozoic|Max depositional age from dates of the underlying Gerowie Tuff. Minimum depositional age from overlying Berinka Volcanics.|Between 1863 +/- 2 Ma and 1861 +/- 4 Ma.|Of South Alligator Group.||Conformably underlies the Finniss River Group.||02-MAY-12
27066|Mount Bonnie Formation|65232|5|Briefly described|p45, p6 Fig. 5, p50, App. 2|Palaeoproterozoic|Palaeoproterozoic|Of South Alligator Group. Replaces Kapalga Formation in area of Sleisbeck uranium occurrence. Over Koolpin Formation (conform). Under Burrell Creek Formation (grades up). Age: 1885 Ma. Chert-banded ferruginous siltstone and shale with greywacke; phyllite.||||||09-FEB-10
27066|Mount Bonnie Formation|65339|4|Described|p6 Table 1, pp12-13, pp23-24.|||Occurs as a series of distinctly coloured red-brown strike ridges and low hills. Average thickness c. 500 m. Hosts gold in iron-rich beds and quartz stockwork veins; mined at Rustlers Roost Mine which also supplies decorative 'Rooster Red' stone for Darwin gardens.||Unit in South Alligator Group.||Overlies Gerowie Tuff. Is overlain by Burrell Creek Formation. Is intruded by Zamu Dolerite, Mount Bundey Granite and Mount Goyder Syenite.|Red, brown and purple laminated siliceous, argillaceous and tuffaceous siltstone; common chert beds and nodules; ironstone and massive feldspathic greywacke.|
27066|Mount Bonnie Formation|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in South Alligator Group.||Overlies Gerowie Tuff.|Interbedded carbonaceous sericitic, commonly pyritic or chloritic slate, phyllite, mudstone and siltstone; fine to coarse feldspathic metagreywacke; ferruginous phyllite with chert bands lenses and nodules; crystal and vitric tuffs; siliceous shale.|23-NOV-11
27066|Mount Bonnie Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1885 +/- 2 Ma.|South Alligator Group.||||
27066|Mount Bonnie Formation|67355|5|Briefly described|p4, p7, p12-13||Paleoproterozoic|Includes the former Fisher Creek Siltstone. Older age from SHRIMP, younger from conventional U-Pb zircon. The maximum thickness of the unit is approximately 500 m.|2025 +8/-5 Ma, 1885 +/- 2 Ma |South Alligator Group||Underlies the Burrell Creek Formation, conformably overlies the Gerowie Tuff.|Tuffaceous sedimentary rocks, increasingly arenaceous. Consists, in the Rum Jungle Mineral Field, predominantly of red-brown shale and siltstone with minor fine to medium sandstone and chert beds.|25-JAN-17
27066|Mount Bonnie Formation|67564|3|Fully described|p7 Table 2, p9 Fig.4, pp22-23.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Contains rocks previously mapped by Walpole (1963) as Burrell Creek Formation and the now defunct Golden Dyke Formation, Gerowie Chert and Fisher Creek Siltstone; also rocks mappped by Stuart-Smith et al. (1984) as Fisher Creek Siltstone, and (1988b) as Big Sunday Formation and the now defunct Kapalga Formation. Dolomitic lenses around Moline, previously mapped within this unit by Stuart-Smith et al. (1998a), are now mapped as Koolpin Formation. 1200 m of shallow marine inner shelf to deeper mid-shelf (turbidite) deposits. Greywacke beds commonly host sulfide-bearing quartz vein-hosted Au systems. Hosts Cu deposits, eg Coronet Hill.|1863 Ma.|Unit in South Alligator Group.||Conformably overlies Gerowie Tuff. Is intruded by Zamu and Oenpelli Dolerites and Cullen Batholith. Is overlain conformably by Burrell Creek Formation.|Interbedded carbonaceous slate, phyllite, mudstone and siltstone; feldspathic metagreywacke; hematitic phyllite with chert bands, lenses and nodules; minor crystal and vitric tuff; siliceous argillite; rare banded ironstone, dolomudstone.|
27066|Mount Bonnie Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Topmost unit in South Alligator Group.||Overlies Gerowie Tuff. Is overlain by Burrell Creek Formation.||
27066|Mount Bonnie Formation|69418|6|Mentioned|p3:6-7, 11, 21, 31|||Pine Creek Orogen. Hosts numerous gold deposits, as well as the Mount Bonnie and Iron Blow Zn-Pb-Cu-Au deposits (described) and the Hayes Creek Sn vein deposit (briefly described). May host the Quantum REE deposit (described).||||||12-JUL-16
27066|Mount Bonnie Formation|69420|4|Described|p5:4, 6, 8, 11-13, 35, 36-37, 39-40|Paleoproterozoic|Paleoproterozoic|See also 43-44, 48-49, 51, 56, 60, 65, 67, 79-80, 84, 86-87, 101, 108. Central Domain, Pine Creek Orogen. Formerly Kapalga Formation. 1000-5000m thick. Shallow-marine inner shelf to deeper mid-shelf (turbidite) deposits. Hosts Au deposits in various goldfields (described in some detail), and the Sleisbeck U deposit, among others. Also hosts Zn-Cu-Au-Pb and Sn deposits.||South Alligator Group.||Overlies Gerowie Tuff. Is overlain conformably by Burrell Creek Formation (Finniss River Group). Is intruded by Shoobridge Granite.|A succession of interbedded siltstone, shale, greywacke, crystal and vitric tuff, rare banded ironstone, mudstone.|12-JUL-16
27066|Mount Bonnie Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. This unit also includes minor banded ironstone, dolomudstone lenses and biotite-quartz schist.||South Alligator Group.||Conformably overlies Gerowie Tuff.|Interbedded carbonaceous, sericitic and commonly pyritic or chloritic slate, phyllite, mustone and siltstone; feldspathic metagreywacke; ferruginous phyllite with chert bands, lenses and nodules; crystal and vitric tuffs; siliceous shale.|
27066|Mount Bonnie Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1877+/-11.0 Ma (MDA: U-Pb TIMS).||||Crystal-rich tuff.|
79363|Mount Bundey Suite|69420|5|Briefly described|p5:17, 20|Paleoproterozoic|Paleoproterozoic|Of Stuart-Smith el al. (1993 and Wyborn et al (1997). [Unclear if NTGS uses these Suites or not.] Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. See also Mount Bundey igneous suite on p5:22.|||Mount Bundey Granite, Mount Goyder Syenite.|||12-JUL-16
24395|Mount Davenport Diamictite Member|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mount Doreen Formation. Polymictic diamictite; subrounded, faceted and striated erratics; green matrix, poorly sorted siltstone. Geological Province: Ngalia Basin.||||||14-FEB-06
24395|Mount Davenport Diamictite Member|38945|4|Described|p131|||||||||
24395|Mount Davenport Diamictite Member|43631|6|Mentioned|p25|||||||||
24395|Mount Davenport Diamictite Member|44158|4|Described|p29 Table.2|Neoproterozoic|Neoproterozoic|Of Mount Doreen Formation.||||||09-NOV-06
24395|Mount Davenport Diamictite Member|45155|2|Defined|p29|Adelaidean|Adelaidean|||||||
24395|Mount Davenport Diamictite Member|68270|4|Described|p680,682-683,686,688|Cryogenian|Cryogenian|Ngalia Basin. Type section occurs in Eastern Naburula Hills, lat. 22'17'S, long. 131'19'E. Crops out in the northern part of the basin. Less than 77m thick. Fluvioglacial deposit. Related to Elatina glaciation. Correlable to Elatina Formation.||Unit of Mount Doreen Formation.||Overlain by Wanapi Dolomite Member. Underlain by Rinkabeena Shale or Vaughan Springs Quartzite.|Diamictite (pebble, cobble, and rare boulder-sized (up to 4 min diameter) erratics, which are sub-rounded, striated and faceted), thin lenses of poorly sorted pebbly dolomitic sandstone and angular feldspathic sandstone and minor dolomite.|03-JUL-19
24395|Mount Davenport Diamictite Member|69439|4|Described|p24:2, 8|Ediacaran|Ediacaran|Ngalia Basin, Centralian A Superbasin. Supersequence 3. 77m thick in the Patmungala Syncline. Most clasts were sourced from the Aileron Province. Represents the latest Cryogenian Elatina glaciation.||Mount Doreen Formation.||Is overlain conformably by Wanapi Dolostone Member. Correlated with Olympic and Pioneer Formations.|Green to red-brown and maroon diamictite, with pebble-, cobble- and rare boulder-sized, commonly striated, erratics of widely varying lithologies; local beds of pebbly quartz sandstone, mainly in the lower parts.|12-JUL-16
24395|Mount Davenport Diamictite Member|69673|5|Briefly described|p106, p107 fig 85|||77m thick.||||Overlain by Wanapi Dolostone Member,|Diamictite containing pebble cobble and rare boulder sized commonly striated erratics.|
27660|Mount Deane Volcanic Member|39069|6|Mentioned|Fig.7|||||||||
27660|Mount Deane Volcanic Member|39518|6|Mentioned|p5|||||||||
27660|Mount Deane Volcanic Member|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wildman Siltstone. Altered basic volcanics, in places vesicular or brecciated.||||||07-NOV-08
27660|Mount Deane Volcanic Member|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27660|Mount Deane Volcanic Member|41305|4|Described|p15|||||||||
27660|Mount Deane Volcanic Member|43187|5|Briefly described|p2|||||||||
27660|Mount Deane Volcanic Member|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wildman Siltstone (Mount Partridge Group).  Altered basic volcanics, in places vesicular or brecciated.||||||07-NOV-08
27660|Mount Deane Volcanic Member|47049|6|Mentioned|p236|||||||||
27660|Mount Deane Volcanic Member|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wildman Siltstone (Mount Partridge Group).||||||
27660|Mount Deane Volcanic Member|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Altered basic volcanics, in places vesicular or brecciated. Of Wildman Siltstone.||||||
27660|Mount Deane Volcanic Member|61389|5|Briefly described|Map Legend|||Of the Wildman Siltstone.  Altered basic volcanics, in places vesicular or brecciated.||||||30-SEP-05
27660|Mount Deane Volcanic Member|64698|4|Described|lithinterp table|Orosirian|Orosirian|Of Wildman Siltstone which has age 2026Ma SHRIMP U/Pb, so Member must be similar age. Max. thickness 150m. Altered mafic volcanics, in places vesicular or brecciated. Lies within -Wildman Siltstone, above Acacia Gap Quartzite Member.||||||07-JAN-09
27660|Mount Deane Volcanic Member|65232|5|Briefly described|p51|||Of Wildman Siltstone. Thin basaltic volcanic rocks.||||||09-FEB-10
27660|Mount Deane Volcanic Member|65339|5|Briefly described|p6 Table 1, pp10-12. |||Correlated with Yarrawonga Volcanic Member to the north. Thickness to 200 m. Weathered rubbly outcrops contain silica-lined amygdales, commonly distorted or stretched.||Unit in Wildman Siltstone.|||Altered mafic volcanic rocks, locally vesicular or brecciated.|
27660|Mount Deane Volcanic Member|67355|5|Briefly described|.p7 Tb.2, p10-12||Paleoproterozoic|The Member is stratigraphically above the Acacia Gap Quartzite Member to the east of the Rum Jungle Dome and thins along strike to the southeast, where outcrops become narrow and discontinuous.||Wildman Siltstone ||Stratigraphically above the Acacia Gap Quartzite Member.|Weathered mafic volcanic unit - poorly exposed, forming rubbly outcrops of red-brown weathered material. Vesicular units with flow-top breccias 1-1.5 m thick are interbedded with quartzite and siltstone. Minor felsic to intermediate volcanic rocks.|25-JAN-17
27660|Mount Deane Volcanic Member|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Wildman Siltstone.|||Altered mafic volcanic rocks, in places vesicular or brecciated.|
23816|Mount Dobbie Granite|8217|5|Briefly described|Map Legend|Carpentarian|Carpentarian|Coarse-grained leucocratic muscovite granite. Age: 1662 +/- 25Ma (K/Ar). Underlies: Yackah beds.||||||28-OCT-04
23816|Mount Dobbie Granite|24442|5|Briefly described|p49|||Malachite has been recognised in the granite.  Geological Province: Arunta Province.||||||
23816|Mount Dobbie Granite|39888|6|Mentioned|Fig.7|||||||||
23816|Mount Dobbie Granite|39921|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23816|Mount Dobbie Granite|46959|6|Mentioned|p206|||||||||
23816|Mount Dobbie Granite|48990|6|Mentioned|p15|||||||||
23816|Mount Dobbie Granite|48992|2|Defined|p34|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
23816|Mount Dobbie Granite|48997|5|Briefly described|p7|||See also Fig.2.||||||
23816|Mount Dobbie Granite|49027|6|Mentioned|p2|||Mention p23.||||||09-NOV-06
23816|Mount Dobbie Granite|60122|6|Mentioned|p6, p47|||Contains minor malachite. Probably Palaeoproterozoic in age. On HAY RIVER sheet. Geological Province: Arunta Province.||||||09-NOV-06
23816|Mount Dobbie Granite|64068|6|Mentioned|p152, p44, p223|||Prominent quartz veins associated with this unit were sampled for mineralisation; minor malachite and galena were observed.||||Nonconformably overlain by Yackah beds.||05-APR-12
23816|Mount Dobbie Granite|69427|5|Briefly described|p12:30 Fig.12.28; 12:36|||Shergold (1985). Included in a map of 1780-1740 Ma granites in the Aileron Province. Poor outcrops E of Mount Barrington. Emplaced at 12-15km depth.|||||A homogeneous, coarse-grained muscovite granite.|12-JUL-16
77201|Mount Doom Ultramafics|62595|5|Briefly described|p33 Fig.12.|||Hosts the Mithril Prospect. See also excursion site 1.8 on Fig 10, p32|||||Pyroxenite and peridotite.|15-OCT-12
41952|Mount Dunkin Schist|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Sillimanite schist and gneiss.||||||
41952|Mount Dunkin Schist|65338|6|Mentioned|p17.|||Partial lateral correlative of Lander Rock Formation.||||||
41952|Mount Dunkin Schist|69427|5|Briefly described|p12:25, 32|||SE Reynolds Range, Aileron Province. Included by Dirks (1990) in his version of the Reynolds Range Group.||||Is intruded by Napperby Gneiss.||12-JUL-16
41952|Mount Dunkin Schist|73399|6|Mentioned|App.E||||||||Schist.|
37867|Mount Fawcett Member|24048|2|Defined|p107 App. 1|Paleoproterozoic|Paleoproterozoic|See also p44.  Proposer: Ian Sweet. Of the Badalngarrmirri Formation. Underlain by Mattamurta Sandstone.  Max. thickness: 240m.  Geological Province: McArthur Basin.||||||07-NOV-08
37867|Mount Fawcett Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation (Parsons Range Group). Siltstone: laminated to thin-bedded; sandstone: glauconitic, thick-bedded, cross-bedded coarse to very coarse-grained, silicified stromatolitic dolostone at base. Geol. Prov: McArthur Basin.||||||09-NOV-06
37867|Mount Fawcett Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Badalngarrmirri Formation (Parsons Range Group). Siltstone: laminated to thin-bedded; sandstone: glauconitic, thick-bedded, cross-bedded coarse to very coarse-grained, silicified stromatolitic dolostone at base. Geol. Prov: McArthur Basin.||||||09-NOV-06
37867|Mount Fawcett Member|69430|4|Described|p15:13|||Southern Walker Fault Zone, McArthur Basin. 0-240m thick. Shelf to marginal marine sediments.||Badalngarrmirri Formation.||Conformably (locally disconformably) overlies Mattamurta Sandstone.|Olive-green and grey, laminated to thinly bedded siltstone; thickly bedded, glauconitic, coarse-grained sandstone; stromatolitic dolostone at base.|12-JUL-16
41953|Mount Freeling Schist|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Muscovite-biotite schist, quartzite, cordierite granulite, quartz-rich metasediment, andalusite schist.||||||09-NOV-06
41953|Mount Freeling Schist|23316|6|Mentioned|p356 Fig. 1(b)|||mentioned only as Mount Freeling Schist Zone represented on map.||||||
41953|Mount Freeling Schist|65338|6|Mentioned|p17.|||Partial lateral correlative of Lander Rock Formation.||||||
41953|Mount Freeling Schist|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
41953|Mount Freeling Schist|69427|5|Briefly described|p12:25, 32|||SE Reynolds Range, Aileron Province. Included by Dirks (1990) in his version of the Reynolds Range Group.||||Is intruded by Napperby Gneiss.||12-JUL-16
41953|Mount Freeling Schist|70376|6|Mentioned|p833 fig 2|Paleoproterozoic|Paleoproterozoic|Misspelt as Mount Freeeling Schist.||||||
41953|Mount Freeling Schist|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Five U-Pb SHRIMP metamorphism age determinations are given within this range. The unit is confusingly presented as Reynolds Range Group/Pine Hill FZ(Mt Freeling Schist).|1586+/-3 Ma to 1562+/-4 Ma.||||Leucosome in granulite.|
41953|Mount Freeling Schist|73399|6|Mentioned|App.E||||||||Schist.|
75073|Mount Goodwin Subgroup|69452|4|Described|p36:8, 15, 19-21|||Helby (1974); redefined in Gorter et al. (2009). Petrel Sub-basin, Bonaparte Basin. Extensive in the subsurface; represented onshore by a thin 20m-thick succession near Port Keats. Up to 670m thick.||Kinmore Group.|Ascalon, Mairmull, Penguin, Fishburn Formations.|Unconformably overlies Hyland Bay Subgroup. Is overlain unconformably by Sahul Group.|Shale, claystone, siltstone and minor sandstone.|12-JUL-16
75073|Mount Goodwin Subgroup|69454|5|Briefly described|p38:4|Olenekian|Changhsingian|Petrel Sub-basin, Bonaparte Basin.||Kinmore Group.|Penguin, Mairmull, Ascalon, Fishburn Formations.|Overlies Hyland Bay Subgroup. Is overlain by Troughton Group.||12-JUL-16
75073|Mount Goodwin Subgroup|69673|5|Briefly described|p153 fig 125, p173|||570-670m thick.||Kinmore Group|Includes Penguin Formation, Mairmull Formation, Ascalon Formation, Fishburn Formation|Unconformably overlain by Troughton Group|Siltstone and shale.|
75073|Mount Goodwin Subgroup|70061|5|Briefly described|Petrel Sub-basin Figs.2 & 3, p2-3|Middle Triassic|Early Triassic|See also Regional geology: Figs.6-8, p10-12. Vulcan: Fig.2. Marine shales form a regional seal for Permian reservoirs, eg the Hyland Bay Subgroup. Appears as Mount Goodwin Formation on p12.||Kinmore Group.|Penguin, Mairmull, Ascalon and Fishburn Formations.|Overlies Hyland Bay Subgroup. Is overlain by Cape Londonderry Formation.|Includes transgressive, thick marine shales.|12-JUL-16
75073|Mount Goodwin Subgroup|71146|5|Briefly described|p6|Lopingian|Lopingian|Bonaparte Basin.||||Overlies the Hyland Bay Subgroup. Overlain by the Osprey Formation.|Mudstone.|
27965|Mount Goyder Syenite|22619|6|Mentioned|p174,5|Statherian|Orosirian|Part of the Mt Bundy Pluton. Mount spelled Mt in text.||||||14-APR-08
27965|Mount Goyder Syenite|23999|6|Mentioned|p47 Tb. 17|||Pink-brown in colour, coarse-grained and well-jointed; major mineral is orthoclase. Lamprophyre dykes present. Mount is Mt in text of Table. See also p54.||||||07-FEB-11
27965|Mount Goyder Syenite|24047|5|Briefly described|p21, p39|||Of the Mount Bundey igneous suite.||||||
27965|Mount Goyder Syenite|32660|5|Briefly described|Table 2|||||||||
27965|Mount Goyder Syenite|32958|6|Mentioned|p953|||||||||
27965|Mount Goyder Syenite|35465|6|Mentioned|p56|||||||||
27965|Mount Goyder Syenite|39069|6|Mentioned|p24|||||||||
27965|Mount Goyder Syenite|39518|3|Fully described|p9|||||||||
27965|Mount Goyder Syenite|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27965|Mount Goyder Syenite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27965|Mount Goyder Syenite|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27965|Mount Goyder Syenite|41305|4|Described|p19|||||||||
27965|Mount Goyder Syenite|43624|6|Mentioned|Fig.15,p20|||||||||
27965|Mount Goyder Syenite|44314|2|Defined|p.9,10,14,map|||(D52-4). On DARWIN Sheet.||||||09-NOV-06
27965|Mount Goyder Syenite|45022|3|Fully described|p.143,144||Carpentarian|Pet. Desc.on Tech.File D/52.4. On many pages.||||||
27965|Mount Goyder Syenite|50586|6|Mentioned|p6.4|||||||||
27965|Mount Goyder Syenite|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Coarse pink syenite.||||||05-NOV-04
27965|Mount Goyder Syenite|62375|6|Mentioned|p26|||Intrudes the Mount Partridge and South Alligator Groups. Medium to coarse, slightly porphyritic massive rock. Low quartz content (<10%), higher hornblende content (>10%), and commonly in the presence of clinopyroxene.||||||09-FEB-10
27965|Mount Goyder Syenite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. |1829 +/- 31 Ma (SHRIMP Monazite)|Cullen Supersuite||||
27965|Mount Goyder Syenite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite.  I-type. Pink syenite.||||||07-JAN-09
27965|Mount Goyder Syenite|64769|6|Mentioned|p29|Mesoproterozoic|Mesoproterozoic|NT.||||||06-MAY-09
27965|Mount Goyder Syenite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
27965|Mount Goyder Syenite|65339|5|Briefly described|pp12-13, p15.|||Does not outcrop in map area.||||Intrudes South Alligator Group.|Brown-purple, medium- to coarse-grained porphyritic syenite.|
27965|Mount Goyder Syenite|69418|6|Mentioned|p3:25|||Includes a roof pendant of Wildman Siltstone in which is the Mount Bundey Fe deposit: tabular lenses of magnetite.||||||12-JUL-16
27965|Mount Goyder Syenite|69420|5|Briefly described|p5:14, 17-18, 20, 22, 118|Paleoproterozoic|Paleoproterozoic|Granite-dominated plutons; mineralogy and petrology/geochemistry summarised. Is intruded by lamprophyre dykes at Toms Gully mine workings. Thought to be a hybrid pluton, formed by interaction between Mount Bundey Granite and (shoshonitic) lamprophyre dyke magmas. is quarried for dimension stone (called Darwin Brown) at Mount Bundey.||Mount Bundey Suite.||Is intruded by Mount Bundey Granite.|Cumulate-textured coarse-grained syenite. I-type.|12-JUL-16
41995|Mount Laughlen Quartzite|9199|5|Briefly described|Map legend|||Quartzite, muscovite schist.  Geological Province: Arunta Block.||||||04-NOV-04
41995|Mount Laughlen Quartzite|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Quartzite, muscovite schist.||||||
27843|Mount Litchfield Granite|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Non-foliated to moderatly foliated granite; adamellite: associated tourmaline bearing pegmatites.||||||07-NOV-08
27843|Mount Litchfield Granite|9579|5|Briefly described|Map Sheet|Orosirian|Orosirian||ca. 1850-1840 Ma (Page, BMR)|||Synorogenic with the Murra-Kamangee Granodiorite, Wagait Granite.||
27843|Mount Litchfield Granite|22809|4|Described|14|||||||||
27843|Mount Litchfield Granite|22810|4|Described|Table3 P8, P16||Proterozoic|Unconformably overlain by Tindall Limestone. Age of unit is 1850 to 1840 Ma.||||||09-NOV-06
27843|Mount Litchfield Granite|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Adamellite, granodiorite.||||||07-NOV-08
27843|Mount Litchfield Granite|23714|4|Described|p16|||See also page 14, Table 2. Litchfield Province.||||||
27843|Mount Litchfield Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly S-type. In the Cullen Batholith, of the Rum Jungle and Central Region||||||
27843|Mount Litchfield Granite|23822|6|Mentioned|p299|||Geological Province: Litchfield Province.  Superseded by the Litchfield Granite. Mount is Mt. in text.||||||09-NOV-06
27843|Mount Litchfield Granite|24197|5|Briefly described|p18|Paleoproterozoic|Paleoproterozoic|Of the Allia Suite. Geological province: Litchfield Block/Pine Creek Inlier.||||||07-FEB-11
27843|Mount Litchfield Granite|41980|5|Briefly described|Table 3 P575|||||||||
27843|Mount Litchfield Granite|42070|6|Mentioned|p3|||||||||
27843|Mount Litchfield Granite|45022|3|Fully described|p.132,133.||Archean|Pet. Desc.on Tech-File D/52-7.||||||07-NOV-08
27843|Mount Litchfield Granite|45112|6|Mentioned|p50|||||||||
27843|Mount Litchfield Granite|48942|6|Mentioned|p24|||Refers Hossfeld (1937).||||||
27843|Mount Litchfield Granite|50586|5|Briefly described|p1.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite. Age: 1768 +/- 16Ma (Rb-Sr).||||||07-NOV-08
27843|Mount Litchfield Granite|63866|5|Briefly described|p107|||||||||
27843|Mount Litchfield Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Non-foliated to moderately foliated granite, adamellite, associated tourmaline-bearing pegmatites.||||||07-JAN-09
27843|Mount Litchfield Granite|64731|5|Briefly described|p148 Fig.3, p150|Proterozoic|Proterozoic|S-type. May be co-magmatic with Two Sisters Granite.||||||12-APR-12
27843|Mount Litchfield Granite|64956|6|Mentioned|p50|||Has contact with Fish Billabong Adamellite.||||||07-FEB-11
27843|Mount Litchfield Granite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Unfoliated to moderately foliated quartz monzonite and granodiorite; associated tourmaline-bearing pegmatites.|23-NOV-11
27843|Mount Litchfield Granite|67232|6|Mentioned|p4 Fig.3.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.||||
27843|Mount Litchfield Granite|69420|5|Briefly described|p5:18-19, 28|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised.|1768 +/- 16 Ma (Rb-Sr).|Allia Creek Suite.|||Quartz monzonite to granodiorite: fine to medium foliated to non-foliated granite.|12-JUL-16
27843|Mount Litchfield Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Allia Creek Suite.|||Fine- to coarse-grained biotite monzonite, poikilitic texture and minor myrmekite; some aplite.|
27843|Mount Litchfield Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
79324|Mount Peake Gabbro|71349|5|Briefly described|p734|||Arunta Inlier. Mentioned in the context of studies of radiogenic Pb loss.||||||
79324|Mount Peake Gabbro|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1053+/-24 Ma (U-Pb zircon LA-ICPMS).||||Olivine gabbro.|
79324|Mount Peake Gabbro|72709|6|Mentioned|p2, p4|||Aileron Province. Beyer et al. (2016). Magnetite gabbro in the SDDD001 drill hole is [tentatively] assigned to Mount Peake Gabbro, which is underlain by units of siltstone and quartzite.|||||Magnetite gabbro|
27050|Mount Porter Granite|23714|6|Mentioned|p19|||Now part of Allamber Springs Granite.||||||
27050|Mount Porter Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. Age: ~1825Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
27050|Mount Porter Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27050|Mount Porter Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Pink-green coarse porphyritic hornblende-biotite granite.||||||07-NOV-08
27050|Mount Porter Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27050|Mount Porter Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27050|Mount Porter Granite|43832|4|Described|Table8p40;49;Tb12p65||Paleoproterozoic|||||||07-NOV-08
27050|Mount Porter 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
27050|Mount Porter Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite.  I-type. Coarse porphyritic biotite and biotite-hornblende granite.||||||07-JAN-09
27050|Mount Porter Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
27050|Mount Porter Granite|69420|5|Briefly described|p5:17-18, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Margaret Suite.|||Coarse-grained porphyritic granite. I-type.|12-JUL-16
36064|Mount Reid Rhyolite|23398|5|Briefly described|p433|||Previously Mount Reid Volcanics.||||||01-OCT-19
36064|Mount Reid Rhyolite|23937|1|Redefined|p88 App. 1|Orosirian|Orosirian|Originally called Mount Reid beds.  Volcanic component formerly named "Mt. Reid Formation" (Rawlings, 1999).  Overlain by Limmen Sst; unconformably  by Knuckey Fm. Intruded by Urapunga Granite.  Age: 1847+/-16Ma (Page et al, 2000).  Geol.Prov: McArthur B.||||||23-DEC-09
36064|Mount Reid Rhyolite|61390|5|Briefly described|Map Legend|Orosirian|Orosirian|Fine grained rhyolitic volcanic rocks.||||||
36064|Mount Reid Rhyolite|63866|5|Briefly described|p114|Orosirian|Orosirian|Walker/Urapunga Fault Zones. Associated with the intrusion of the Urapunga Granite.|1847 +/- 16 Ma (Page et al., 2000)|||||
36064|Mount Reid Rhyolite|69429|5|Briefly described|p14:3-4|Paleoproterozoic|Paleoproterozoic|Urapunga Inlier. Coeval with Urapunga Granite. SHRIMP U-Pb zircon age.|1847 +/- 6 Ma (Page et al., 2000).||||Fine rhyolite containing sparse phenocrysts (up to 2mm) of rounded and embayed quartz and feldspar in a recrystallised siliceous matrix.|12-JUL-16
36064|Mount Reid Rhyolite|69430|6|Mentioned|p15:24-25, 30, 51|||||||Is overlain unconformably by Mount Birch Sandstone (Nathan Group) and Katherine River Group.||12-JUL-16
36064|Mount Reid Rhyolite|71592|5|Briefly described|Appendix A.|||Urapunga Inlier.|1847+/-16 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyry.|
36064|Mount Reid Rhyolite|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Part of the early Basin volcanism and plutonism in the McArthur Basin.|||||Rhyolitic volcanics.|
36064|Mount Reid Rhyolite|72373|5|Briefly described|p27|||||||Locally overlain unconformably by Mount Birch Sandstone.||
36064|Mount Reid Rhyolite|72919|6|Mentioned|p7|Orosirian|Orosirian|Urapunga Inlier. An age of 1847 +/- 16 Ma was reported by Page et al. (2000).|1847 +/- 16 Ma|||||
27067|Mount Shepherd Rhyolite Member|23216|5|Briefly described|Table1p10,13-4|||||||||
27067|Mount Shepherd Rhyolite Member|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27067|Mount Shepherd Rhyolite Member|41295|6|Mentioned|p13|||||||||
27067|Mount Shepherd Rhyolite Member|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27067|Mount Shepherd Rhyolite Member|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Edith River Group. Of Orosirian age.||||||07-NOV-08
80497|Mount Solitaire Sandstone|63866|6|Mentioned|p99|||Shown as Mt Solitaire Ssts in time space plot with a max deposition age within the 1850-1800 Ma range (~1820 Ma).||||||29-MAR-18
72421|Mount Stafford Member|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Quartz-mica schist and phyllite, spotted and layered predominatly metapelitic and subordinate to minor metapsammitic hornfels, migmatite, amphibolite.||||||07-NOV-08
72421|Mount Stafford Member|65338|3|Fully described|App 1 p84, p12-13, p39, p51-54|Orosirian|Orosirian|Name variation. Deep-water, turbiditic; possibly locally shallow-marine. Constitutes much of Yundurbulu and Bilba Hills and an area encompassing Mount Stafford. A localised, high-metamorphic-grade equivalent of Woodalla Member. P-T conditions detailed.|Max. 1866 +/- 3 Ma (Claoue-Long et al. 2008a).|Unit in Lander Rock Formation.||Conformable, and laterally transitional contact with Woodalla Member. Intruded by 1795 +/-3Ma Anmatjira Orthogneiss, granite and dolerite.|Greenschist- to granulite-facies metasedimentary rocks: spotted and layered predominantly metapelitic and subordinate metapsammitic hornfels, orthoamphibolite, migmatite; protoliths were a succession of sandstone, siltstone and mudstone.|
72421|Mount Stafford Member|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Quartz-mica schist and phyllite, spotted and layered, predominantly metapelitic; metapsammitic hornfels; migmatite; amphibolite.|
72421|Mount Stafford Member|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Quartz-mica schist and phyllite, spotted and layered metapelitic and subordinate to minor metapsammitic hornfels (andalusite/spinel/orthopyroxene+garnet-cordierite-K-feldspar); migmatite; amphibolite.|
72421|Mount Stafford Member|69427|5|Briefly described|p12:5, 19|||Donnellan (2008). Formerly Mount Stafford beds of Stewart et al. (1980). A localised, unusually low-P, high-T metamorphosed unit with a temperature gradient of 800-400oC (granulite to greenschist facies) over 10km. Metamorphosed at 1805-1795 Ma (the Stafford Event). High-grade equivalent of the Woodalla Member.||Lander Rock Formation.|||Metapelitic rocks.|12-JUL-16
72421|Mount Stafford Member|73399|6|Mentioned|App.E|||[Previously Mount Stafford Beds].|||||May include metapelitic and metapsammitic hornfels.|
40026|Mount Stafford dolerite|23844|3|Fully described|p35|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province. Max Thickness: <200m. Occurs within the Mount Stafford beds. Intruded by the Anmatjira Orthogneiss. See also Fig.19||||||07-NOV-08
40026|Mount Stafford dolerite|60668|5|Briefly described|p12, p2 Tb. 1|||Folded dykes and sills - stacked sequence of hypabyssal sills and asscoaied dykes, tightly folded.  Dolerite, doleritic gabbro, gabbro and gabbronorite; fine-grained, massive and weakly recrystallised. Max. thickness: 200m. ||||||
28815|Mount Thomas Quartzite|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block.||||||
28815|Mount Thomas Quartzite|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Reynolds Range Group (Geological Province: Arunta Block). Quartzite.||||||
28815|Mount Thomas Quartzite|23270|5|Briefly described|Table 1, p6||Proterozoic|In the Arunta Block (Division 3 - Reynolds Range Group).||||||09-NOV-06
28815|Mount Thomas Quartzite|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block(Division Three). Age: Early or Middle Proterozoic.||||||09-NOV-06
28815|Mount Thomas Quartzite|23809|5|Briefly described|p45|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Age: 1820-1780Ma. Geological Province: Arunta Province.||||||20-OCT-11
28815|Mount Thomas Quartzite|24047|5|Briefly described|p7 Fig. 6, p10|Paleoproterozoic|Paleoproterozoic|Lower part of the Reynolds Range Group. Mount is Mt in text of figure. Geological Province: Arunta Province. See also p36.||||||20-OCT-11
28815|Mount Thomas Quartzite|32480|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|35221|4|Described|Table.1|||||||||
28815|Mount Thomas Quartzite|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|39855|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|39887|6|Mentioned|Fig.5|||||||||
28815|Mount Thomas Quartzite|42217|5|Briefly described|p414|||||||||
28815|Mount Thomas Quartzite|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|43631|3|Fully described|p10,11||Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|43749|6|Mentioned|Fig.1,p6||Paleoproterozoic|||||||07-NOV-08
28815|Mount Thomas Quartzite|44158|4|Described|p9, Table.1|Paleoproterozoic|Paleoproterozoic|Basal formation of the Reynolds Range Group. Age: 1820 - 1780 Ma. Conformably underlies Pine Hill Formation.||||||05-MAY-10
28815|Mount Thomas Quartzite|48992|2|Defined|p37|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||18-JUN-13
28815|Mount Thomas Quartzite|50369|6|Mentioned|p5.1|||Intruded by Warimbi Granite.||||||09-NOV-06
28815|Mount Thomas Quartzite|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex. Quartzite, conglomerate locally at base.||||||07-NOV-08
28815|Mount Thomas Quartzite|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group.  Medium-grained quartz sandstone; silica-cemented, well-sorted, local conglomerate at base. Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
28815|Mount Thomas Quartzite|62378|5|Briefly described|p5, 17, 23|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Age: 1834 +/- 48Ma. Quartz sandstone. Of the Reynolds Range Group. Overlies Lander Rock beds.||||||07-NOV-08
28815|Mount Thomas Quartzite|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Geological Province: Tanami/Arunta Region-Aileron Province. Well sorted fine to medium grained quartz sandstone, thick bedded, heavy mineral laminations.||||||07-NOV-08
28815|Mount Thomas Quartzite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Geological Province: Arunta Region - Aileron Province. White fine to medium grained, well bedded quartzite.||||||07-NOV-08
28815|Mount Thomas Quartzite|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.||Of Reynolds Range Group.|||Medium grained quartz sandstone; silica cemented, well sorted, local conglomerate near base.|15-APR-11
28815|Mount Thomas Quartzite|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Geological Province: Arunta Region - Aileron Province. Orthoquartzite and tourmaline bearing orthoquartzite, fine to medium grained.||||||07-NOV-08
28815|Mount Thomas Quartzite|63866|5|Briefly described|p93|||Aileron Province.|c. 1800 Ma|||||
28815|Mount Thomas Quartzite|64677|5|Briefly described|v, p1, p26-29, p57-58|||Arunta Region, Aileron Province. Crops out as isolated ridges. An overlying calc-silicate rock is intruded by a granite aged 1773 +/- 2 Ma, so this unit may have been deposited around 1780-1775 Ma. This c.1800 Ma is a conservative age; the youngest individual zircons are aged 1628 +/- 26 Ma and c.1746 Ma.|1799.7 +/- 5.6 Ma (maximum depositional age).||||Strongly foliated crystalline metasedimentary quartzite.|
28815|Mount Thomas Quartzite|64737|4|Described|p232-3, 238-9, 241-3, Figs.2, 3, 6, Tb.2||Orosirian|Sedimentary structures indicate intertidal high energy sedimentation. Continuum of detrital ages from <1800 to >2500 Ma. Detrital zircons indicate recycling from underlying sediments. Dated by SHRIMP U-Pb. Maximum age from youngest detritus. Youngest defined group 1798+/-10 Ma.|1785 +/- 16 Ma.|Basal unit of Reynolds Range Group/Reynolds Package.|||Mature orthoquartzite.|30-APR-12
28815|Mount Thomas Quartzite|64956|6|Mentioned|p26|||||||||07-FEB-11
28815|Mount Thomas Quartzite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group.Quartzite; local basal conglomerate; high linear magnetic response||||||
28815|Mount Thomas Quartzite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group. Quartzite; local basal conglomerate; high linear magnetic response||||||
28815|Mount Thomas Quartzite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group. White to grey fine- to medium-grained, well bedded quartzite||||||
28815|Mount Thomas Quartzite|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Reynolds Range Group, Aileron Province; underlies Pine Hill Formation. Consists of medium-grained, silica cemented, well sorted quartz sandstone, local conglomerate near base.||||||
28815|Mount Thomas Quartzite|65338|4|Described|p7, pp20-21.|Statherian|Statherian|Outcrop of these rocks is confined to southwestern MOUNT PEAKE area. Intruded by granite aged 1773 +/- 2 Ma (Worden et al. 2006).|Max deposition age 1779 +/- 14 Ma.|Unit in Reynolds Range Group.||Sheared, faulted contact with Redhackle Granite. Overlies Lander Rock Formation.|Thinly-bedded and flaggy fine-grained quartzite; variably planar to low-angle cross-bedded; biotite- and tourmaline-bearing quartzofeldspathic quartzite.|19-DEC-12
28815|Mount Thomas Quartzite|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Reynolds Range Group.|||Well-sorted fine- to medium-grained quartz sandstone, thickly bedded, heavy mineral laminations, 10 m planar crossbeds, silica cemented.|20-OCT-11
28815|Mount Thomas Quartzite|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Reynolds Range Group.||Is overlain by Pine Hill Formation.|Orthoquartzite and tourmaline-bearing orthoquartzite, fine- to medium-grained.|
28815|Mount Thomas Quartzite|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Reynolds Range Group.||Is overlain by Pine Hill Formation.|Orthoquartzite and tourmaline-bearing orthoquartzite, fine- to medium-grained.|
28815|Mount Thomas Quartzite|68998|5|Briefly described|p13|||Several maximum depositional ages given.||Reynolds Range Group.||||
28815|Mount Thomas Quartzite|69226|6|Mentioned|p240|||Reynolds-Anmatjira Ranges region.||Reynolds Range Group.||||
28815|Mount Thomas Quartzite|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Reynolds Range Group.|||Well-sorted, fine- to medium-grained quartz sandstone, thick-bedded, heavy mineral laminations, 10m thick planar crossbeds, silica cemented.|
28815|Mount Thomas Quartzite|69427|4|Described|p12:25, 32, 64|||Aileron Province. Type section is in central Reynolds Range. Ridge-forming unit. Deposited in a high-energy intertidal environment affected by wave action on a clastic inner shelf. 150-400m thick in Wabudali Range. Contains small massive lenses of haematite, up to 15m thick and discontinuous for over 10km along strike. Contains a 1785 Ma population of detrital zircons at the base; other ages given. Is intruded by granite dated at 1773 +/- 2 Ma.||Basal Reynolds Range Group.||Overlies Lander Rock Formation. Is overlain by, and interfingers with, Pine Hill Formation. Is intruded by Warimbi Schist. Is faulted against Redhackle Granite.|Medium- to thickly-bedded recrystallised quartz sandstone; local basal conglomerate.|12-JUL-16
28815|Mount Thomas Quartzite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Reynolds Range Group.|||White to grey, fine- to medium-grained, well-bedded quartzite.|
28815|Mount Thomas Quartzite|70301|6|Mentioned|p22|Paleoproterozoic|Paleoproterozoic||c.1785 Ma.|Basal Reynolds Range Group.||||
28815|Mount Thomas Quartzite|70376|5|Briefly described|p847|Paleoproterozoic|Paleoproterozoic|Maximum depositional age from detrital zircons? Youngest grain dated at 1785 +/- 8 Ma.|1798 Ma +/- 10 Ma|Base of Reynolds Range Group.||||
28815|Mount Thomas Quartzite|71350|5|Briefly described|p7|Statherian|Orosirian|Aileron Province. Ages provided are SHRIMP maximum depositional ages from Claoue-Long et al, 2008. An older, poorly constrained maximum depositional age of 1834 +/- 38 Ma is provided from Worden et al, 2004, SHRIMP. A [?]minimum depositional age of 1780 +/- 10 Ma is provided from Collins and Williams, 1995.|1799 +/-8 Ma and 1798 +/- 12 Ma |Basal Reynolds Range Group||Intruded by the Wabudali Granite and the Napperby Gneiss.||
28815|Mount Thomas Quartzite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1798+/-10 Ma (MDA: U-Pb zircon SHRIMP)||||Cross-bedded sandstone, strongly foliated quartzite.|
28815|Mount Thomas Quartzite|71858|6|Mentioned|p6, p30|||Aileron Province.|ca 1779 Ma|Reynolds Range Group||||
23837|Mount Tietkens Granite Complex|24442|6|Mentioned|p49|Paleoproterozoic|Paleoproterozoic|Ages (exposed and drillholes): 1753+/7 and 1846+/-6, 1763+/-4, 1749+/-8Ma.  On TOBERMORY sheet.||||||07-NOV-08
23837|Mount Tietkens Granite Complex|48992|2|Defined|p38|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
23837|Mount Tietkens Granite Complex|60122|5|Briefly described|p4-5 Figs.3 and 4, p6,  p15|Paleoproterozoic|Paleoproterozoic|Of Warren and Stewart et al (1980). Also named Tietkens Granite Complex (Simpson et al 1985) but remains as Mount Tietkens Granite Complex in this study. Nonconformably overlain by Thorntonia Limestone.  Geological Province: Arunta Province.||||||07-NOV-08
23837|Mount Tietkens Granite Complex|60590|5|Briefly described|Map legend|Statherian|Statherian|Biotite-muscovite granite; leucogranite, biotite granite, quartz diorite; coarse leucogranite; biotite granodiorite, granite; muscovite-biotite leucogranite, porphyritic leucogranite, tourmaline leucogranite, pegmatite.||||||26-NOV-04
23837|Mount Tietkens Granite Complex|64068|5|Briefly described|p153|||Mentioned as the last lithology intersected in MIM's Boat Hill prospect BHD9 drillhole. Results of this drilling program seriously downgraded prospectivity for Pt group elements.|||||Includes muscovite-biotite granite, pegmatite and minor metamorphic rock.|05-APR-12
23837|Mount Tietkens Granite Complex|70303|5|Briefly described|iv, p1, p15-17, p25-26|Paleoproterozoic|Paleoproterozoic|Cross et al. (2005) reported an igneous crystallisation age of 1846 +/- 6 Ma.|1852 +/- 5 Ma (magmatic crystallisation age).|||Is overlain nonconformably by the Thorntonia Limestone.|Includes feldspar-quartz-muscovite granite.|
23837|Mount Tietkens Granite Complex|71350|5|Briefly described|iii, p9, p12|||Aileron Province. The unnamed granite dated in this study was previously included in this group.|ca 1760 Ma-1740 Ma (Kruse et al, 2002)||||Leucogranites and pegmatites.|
23837|Mount Tietkens Granite Complex|71621|5|Briefly described|p25|||Originally included an unnamed orthogneiss that is dated in this study. It should be noted that Kruse et al (2002) who assigned this orthogneiss to the complex conceded that the complex is poorly defined and contains a number of granitoids that may or may not be related.||||||
31336|Mount Webb Suite|24197|4|Described|p33, p58|Paleoproterozoic|Paleoproterozoic|Comprises Mt Webb Granite, Pollock Hills Fm and Kintore Volcs. Fractionated granite, with extensive alteration effects incl: sodic-calcic, sericitic and hematite-K-feldspar in granite. Ages:1615Ma, ~1640Ma.Geol.P: west Arunta Block. Eg.of Hiltaba Assoc.||||||07-FEB-11
31336|Mount Webb Suite|50369|5|Briefly described|p1.2, 1.5, 21.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: ~1615Ma.||||||07-NOV-08
31336|Mount Webb Suite|64726|6|Mentioned|p83 Fig.2.|||||||||
31336|Mount Webb Suite|67323|5|Briefly described|p90|||Georgina Basin. Heat production for geothermal energy briefly discussed.|||||Granite.|
30827|Mount Wedge Clay|61385|5|Briefly described|Map legend|Cenozoic|Cenozoic|Clay, silt, micrite; dark-coloured; shelly; pyritic; lacustrine (littoral carbonate).  Geological Province: overlies Amadeus Basin.||||||16-DEC-11
30827|Mount Wedge Clay|65194|5|Briefly described|p53-54, p56-57|Eocene|Eocene|Lacustrine clay unit overlying crystalline bedrock. Tentatively correlated with the Eyre Formation in SA. Pyrite-bearing grey-green lacustrine clays. Up to 100m thick.||||||08-APR-16
30827|Mount Wedge Clay|67453|5|Briefly described|map legend|Cenozoic|Cenozoic|Of Mount Wedge Basin, Tarawera Basin. Age shown as Tertiary. Older than Currinya Clay. Clay, silt, micrite; dark coloured, shelly; pyritic: lacustrine (littoral carbonate). Known only from drill holes / water bores||||||16-DEC-11
30827|Mount Wedge Clay|69458|5|Briefly described|p42:13|Eocene|Eocene|Mount Wedge Basin. A thick (c.350m), laterally extensive lacustrine unit.||||Is overlain by the Currinya Clay.|Grey-green clay and sandy clay.|12-JUL-16
29774|Mount Zeil Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1760Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
29774|Mount Zeil Granite|43225|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29774|Mount Zeil Granite|43503|2|Defined|6,19,76|||||||||
29774|Mount Zeil Granite|50369|5|Briefly described|p1.4, 3.1, 12.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Mount Zeil Suite. Intrudes Narwietooma Metamorphic Complex. Age: 1760 +/- 9Ma (Sm-Nd).||||||07-NOV-08
29774|Mount Zeil Granite|69427|5|Briefly described|p12:30 Fig.12.28; 12:32|Statherian|Statherian|Warren and Shaw (1995). Crops out immediately N of the Redbank Thrust; forms Mount Zeil (highest point in the NT). Included in a map of 1780-1740 Ma granites in the Aileron Province. Sm-Nd isochron age.|1760 +/- 9 Ma (quoted in Budd, 1997).||||Homogeneous to migmatitic medium-grained granodiorite and granite, and lesser augen gneiss; metamorphosed at granulite-facies conditions.|12-JUL-16
31337|Mount Zeil Suite|50369|5|Briefly described|p1.4, 12.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1760Ma.||||||07-NOV-08
22460|Muckaty Sandstone Member|24303|2|Defined|p34, p62 Appendix|Early Cambrian|Early Cambrian|Of the Helen Springs Volcanics. Geological Province: Georgina Basin. Max. Thickness: >16m. Possibly extends into Wiso Basin? Possible correlative is Jindare Formation.||||||
22460|Muckaty Sandstone Member|65337|6|Mentioned|p94.|||||Unit in Helen Springs Volcanics.||||
22460|Muckaty Sandstone Member|69424|5|Briefly described|p9:27|Early Cambrian|Early Cambrian|||Helen Springs Volcanics.|||Includes conglomerate.|12-JUL-16
22460|Muckaty Sandstone Member|69431|5|Briefly described|p16:18-19|||Age is given as Early(?) Cambrian.||Helen Springs Volcanics.||Unconformably overlies Renner Group (Gleeson, Baralandji, Powell, Wiernty Formations).||12-JUL-16
22460|Muckaty Sandstone Member|69445|5|Briefly described|p30:5, 17|Early Cambrian|Early Cambrian|East of the Tennant Region.||Basal Helen Springs Volcanics.|||A sedimentary unit containing peperite.|12-JUL-16
22460|Muckaty Sandstone Member|69673|6|Mentioned|p58|||||Helen Springs Volcanics||Unconformably overlies Renner Group||
22460|Muckaty Sandstone Member|70968|5|Briefly described|p93, p100, p105, p108|Early Cambrian|Early Cambrian|||Helen Springs Volcanics.||Unconformably overlies Baralandji, Powell, Wiernty Formations (Renner Group).||
39323|Mulga Creek Granitic Gneiss|23983|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
39323|Mulga Creek Granitic Gneiss|23984|5|Briefly described|p3 Fig.2|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
39323|Mulga Creek Granitic Gneiss|61309|6|Mentioned|p31, p32 Fig. 17|||||||||
39323|Mulga Creek Granitic Gneiss|69427|5|Briefly described|p12:9, 14, 30-31|||Strangways Range region, Wigley Domain, Aileron Province.||||Is Intruded by Georgina Gap Granitic Gneiss.|Foliated muscovite-biotite leucocratic granite.|12-JUL-16
33652|Mulyati Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Granite Suite.  Fine- to medium-grained equigranular K-feldspar-rich foliated biotite granite.  Age: ~1190-1140Ma.||||||08-FEB-05
33652|Mulyati Granite|60683|2|Defined|p57 Appendix, p17-18|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Granite Suite.  Formerly part of the Olia Gneiss of Forman (1966a, 1972).  Fine- to medium-grained K-feldspar rich equigranular biotite granite. See also p11 Tb. 1||||||
33652|Mulyati Granite|61154|5|Briefly described|p10, p44 App.|Mesoproterozoic|Mesoproterozoic|Of the Pottoyu Suite (Pitjantjatjara Supersuite). Equigranular, medium- to fine-grained leucogranite; quartz, K-feldspar and plagioclase.||||||
33652|Mulyati Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Pottoyu Granite Suite.  Fine- to medium-grained equigranular K-feldspar rich foliated biotite granite.  Geological Province: Musgrave Block.||||||19-OCT-05
33652|Mulyati Granite|69091|6|Mentioned|p139 Fig.6.6|||||||||
33652|Mulyati Granite|69436|5|Briefly described|p21:9|||Scrimgeour et al. (1999). On the southern (hangingwall) side of the Wankari Detachment Zone.||Pottoyu Suite.|||A large area of equigranular, medium- to fine-grained leucogranite; locally highly strained and contains partial melts.|12-JUL-16
22471|Mumbilla Granodiorite|22645|6|Mentioned|Table3 P213||Orosirian|Age of unit is 1850+/-6 Ma.||||||13-NOV-06
22471|Mumbilla Granodiorite|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granodiorite; ranges from tonalite to granite: biotite-bearing, coarse to very coarse grained and massive; strongly foliated to sheared in part; abundant metasediment xenoliths; localised alteration (silicification, albitisation, tourmalinisation).||||||07-NOV-08
22471|Mumbilla Granodiorite|23733|5|Briefly described|p7 Fig.1|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma.||||||07-NOV-08
22471|Mumbilla Granodiorite|23809|5|Briefly described|p27 Fig. 25|||Of the Tennant Creek Supersuite. Geological Province: Tennant Inlier.||||||12-AUG-08
22471|Mumbilla Granodiorite|24172|4|Described|p38|Paleoproterozoic|Paleoproterozoic|Informally referred to as "North Seismic adamellite", "Gosse River North adamellite", "South Gosse adamellite" and in part "Gosse River East granite" by Mendum and Tonkin (1976) & Black (1977). Age: 1850+/-6Ma. Intrudes the Yungkulungu Formation.||||||07-NOV-08
22471|Mumbilla Granodiorite|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
22471|Mumbilla Granodiorite|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
22471|Mumbilla Granodiorite|43751|6|Mentioned|Fig.2,p610|||||||||
22471|Mumbilla Granodiorite|43850|4|Described|p263|||Previously North Seismic Adamellite (Black 1977).||||||12-AUG-08
22471|Mumbilla Granodiorite|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: 1850 +/- 6Ma (SHRIMP).||||||17-APR-15
22471|Mumbilla Granodiorite|60684|2|Defined|p52 Appendix, p23|Paleoproterozoic|Paleoproterozoic|Predominantly a biotite-bearing, light grey granodiorite, ranging from tonalite to granite in modal composition; coarse-grained seriate porphyritic to equigranular texture cream-coloured alkali feldspar megacrysts, more. Age: 1850+/-6Ma. Intrudes Flynn Subgroup.||||||14-APR-15
22471|Mumbilla Granodiorite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Tennant Creek Supersuite. Biotite granodiorite (ranges from tonalite to granite);  megacrystic; seriate porhyritic to equigranular; locally abundant porphyritic enclaves with rapakivi texture and blue ovoid quartz; xenoliths. In Tennant Creek region.||||||07-NOV-08
22471|Mumbilla Granodiorite|64559|6|Mentioned|p973|||Age: 1850+/-6Ma (U-Pb).||||||23-DEC-08
22471|Mumbilla Granodiorite|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Tennant Creek Supersuite||||
22471|Mumbilla Granodiorite|65222|5|Briefly described|p109, p110 Fig.2, p114, p116, 117, 125|Orosirian|Orosirian|Shown as intruding Warramunga Formation rocks in Fig 9 p125. Previous 1510 Ma K/Ar age. Zircon Sample locality.|1850 +/- 6 Ma U/Pb SHRIMP.||||Moderately foliated granodiorite. I-type.|24-JAN-22
22471|Mumbilla Granodiorite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tennant Creek Supersuite.|||Granodiorite (ranges from tonalite to granite); biotite-bearing, megacrystic, seriate porphyritic to equigranular; abundant metasediment xenoliths; strongly foliated to sheared in part; locally abundant porphyritic enclaves with rapakivi texture.|
22471|Mumbilla Granodiorite|69187|5|Briefly described|p52, p53 Fig.2|||Warramunga Province.||Tennant Creek Supersuite||intrudes Warramunga Formation||
22471|Mumbilla Granodiorite|69424|5|Briefly described|p9:3, 10-14, 17, 22, 28|Paleoproterozoic|Paleoproterozoic|Warramunga Province. U-Pb zircon age. Is intruded by an un-named quartz-diorite plug aged 1841 +/- 6 Ma.|1850 +/- 6 Ma (Compston, 1995).|Tennant Creek Supersuite.||Intrudes Yungkulungu and Junalki Formation. Is intruded by Treasure Suite.|Megacrystic seriate porphyritic to coarse-grained equigranular biotite-bearing to biotite granodiorite with large (to 10cm) zoned alkali-feldspar phenocrysts, and blue opalescent quartz; minor granite and tonalite. Abundant and varied enclaves.|12-JUL-16
22471|Mumbilla Granodiorite|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1850+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
22471|Mumbilla Granodiorite|73124|6|Mentioned|p2 Fig.1|||||Tennant Creek Supersuite||||
22471|Mumbilla Granodiorite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Tennant Creek Supersuite.||||
22471|Mumbilla Granodiorite|73460|6|Mentioned|p2|||Warramunga Province.||Tennant Creek Supersuite||||
22471|Mumbilla Granodiorite|73590|6|Mentioned|p2|||||Tennant Creek Supersuite||||
27851|Mundogie Sandstone|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Intruded by Zamu Dolerite.||||||07-NOV-08
27851|Mundogie Sandstone|9691|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Interbedded medium quartz sandstone, arkosic sandstone, siltstone, metasiltstone, phyllite, coarse quartzite and feldspathic quartzite, with minor conglomerate beds.||||||
27851|Mundogie Sandstone|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Interbedded medium quartz sandstone, arkosic sandstone, siltstone, metasiltstone, phyllite, coarse quartzite and feldspathic quartzite, with minor conglomerate beds.||||||02-JUN-05
27851|Mundogie Sandstone|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
27851|Mundogie Sandstone|22810|5|Briefly described|Table2 P5|||Unconformable on Masson Formation, maximum thickness 2400m.||||||13-NOV-06
27851|Mundogie Sandstone|23714|4|Described|p12|Proterozoic|Proterozoic|See also page 8 Table 1. Of Mount Partridge Group. Max. thickness: 500 m.||||||
27851|Mundogie Sandstone|23715|5|Briefly described|Map legend||Proterozoic|Of the Mount Partridge Group, in the Central Region.||||||07-JAN-09
27851|Mundogie Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Mount Partridge Group.||||||
27851|Mundogie Sandstone|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Pebbly sandstone.  Geological Province: Pine Creek Orogen.  See also p30 Fig. 23.||||||07-NOV-08
27851|Mundogie Sandstone|24181|4|Described|p102|Paleoproterozoic|Paleoproterozoic|Conglomerate, arkose, sandstone and siltstone. Of Mount Partridge Group. Conformably overlain by Wildman Siltstone. Geological Province: Pine Creek Inlier.||||||07-NOV-08
27851|Mundogie Sandstone|24260|6|Mentioned|p1013 Fig.1|||Geological Province: Pine Creek Inlier||||||
27851|Mundogie Sandstone|30831|6|Mentioned|p9|||||||||
27851|Mundogie Sandstone|35140|6|Mentioned|Fig.2|||||||||
27851|Mundogie Sandstone|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
27851|Mundogie Sandstone|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|37462|6|Mentioned|Fig.4.8|||||||||
27851|Mundogie Sandstone|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Coarse to medium sandstone and quartzite, commonly pebbly feldspathic quartz and chert pebble conglomerate; siltstone and phyllite' cross-bedding, graded bedding and scour structures in places.||||||07-NOV-08
27851|Mundogie Sandstone|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|38239|6|Mentioned|Fig.2|||||||||
27851|Mundogie Sandstone|38349|4|Described|p13|||||||||
27851|Mundogie Sandstone|38351|6|Mentioned|Table 3|||||||||
27851|Mundogie Sandstone|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|39069|5|Briefly described|Table 1|||||||||
27851|Mundogie Sandstone|39357|4|Described|p7|||||||||
27851|Mundogie Sandstone|39518|3|Fully described|p3|||||||||
27851|Mundogie Sandstone|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Coarse, pebbly feldspathic quartzite arkose and micaceous quartzite; minor chert and quartz pebble conglomerate.||||||07-NOV-08
27851|Mundogie Sandstone|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Coarse to pebbly feldspathic quartz sandstone, quartzite and arkose; minor pebble conglomerate.||||||07-NOV-08
27851|Mundogie Sandstone|40243|6|Mentioned|Fig.2|||||||||
27851|Mundogie Sandstone|40493|5|Briefly described|Table 1|||Also mention on p12.||||||13-NOV-06
27851|Mundogie Sandstone|40808|6|Mentioned|Table 2|||||||||
27851|Mundogie Sandstone|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|40861|6|Mentioned|p122|||||||||
27851|Mundogie Sandstone|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|41125|6|Mentioned|p26|||Mention Fig.15||||||
27851|Mundogie Sandstone|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27851|Mundogie Sandstone|41305|3|Fully described|p14|||||||||
27851|Mundogie Sandstone|41309|4|Described|p3|||||||||
27851|Mundogie Sandstone|41311|4|Described|p9|||||||||
27851|Mundogie Sandstone|41397|4|Described|p7|||||||||
27851|Mundogie Sandstone|41407|6|Mentioned|Map legend|Proterozoic||||||||
27851|Mundogie Sandstone|41594|6|Mentioned|Fig.15|||See also Fig.8||||||
27851|Mundogie Sandstone|42372|5|Briefly described|p17|||||||||
27851|Mundogie Sandstone|43140|5|Briefly described|p2||Paleoproterozoic|Of Mount Partridge Group.||||||07-NOV-08
27851|Mundogie Sandstone|43187|5|Briefly described|p2|||||||||
27851|Mundogie Sandstone|43624|5|Briefly described|Table 1,p9,10||Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|43718|6|Mentioned|p28|||||||||
27851|Mundogie Sandstone|43832|3|Fully described|13-15, 97||Paleoproterozoic|||||||07-NOV-08
27851|Mundogie Sandstone|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of  Mount Partridge Group. Overlain by Wildman Siltstone. Interbedded medium quartz sandstone, arkosic and feldspathic sandstone, siltstone, metasiltstone, phyllite, schist, coarse quartzite and feldspathic quartzite, pebbly in places, and conglomerate.||||||22-SEP-14
27851|Mundogie Sandstone|46658|6|Mentioned|p550|||||||||
27851|Mundogie Sandstone|46700|5|Briefly described|P14, Table1 P10||Proterozoic|||||||
27851|Mundogie Sandstone|47049|6|Mentioned|Fig.2|||||||||
27851|Mundogie Sandstone|49744|5|Briefly described|Fig.3|||||||||
27851|Mundogie Sandstone|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Fine to coarse quartz sandstone, quartzite and arkose; minor pebble conglomerate; graded bedding, cross-bedding and scour structures in places. Underlies Wildman Siltstone.||||||13-NOV-06
27851|Mundogie Sandstone|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Feldspathic sandstone, quartzite, arkose, coarse quartz conglomerate, minor phyllite and minor schist with rare amphibolite.||||||10-JUN-05
27851|Mundogie Sandstone|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Mount Partridge Group. Geological Province: Pine Creek Orogen. Thick bedded, medium to coarse, poorly sorted, feldspathic quartz meta-arenite.||||||14-JAN-05
27851|Mundogie Sandstone|61206|6|Mentioned|p517 Fig.1|Early Proterozoic|Early Proterozoic|||||||
27851|Mundogie Sandstone|62375|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Pebble Sandstone. Geological Province: Pine Creek Orogen.||||||09-FEB-10
27851|Mundogie Sandstone|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Of Mount Partridge Group. Max Thickness 1400m. Thickly bedded, medium to very coarse, poorly sorted, feldspathic quartz meta-arenite; graded bedding, lenticular cross-bedding and bedding scours are preserved in places.||||||07-JAN-09
27851|Mundogie Sandstone|64730|5|Briefly described|p125 Fig. 3, p126, 130, 138|Paleoproterozoic|Paleoproterozoic|In eastern Central Domain. Underlying Stag Creek Volcanics provide maximum age: 2021+/-10 Ma.||Basal unit of Mount Partridge Group.||Unconformably overlies Stag Creek Volcanics.|Conglomerate and coarse sandstone, fluvial fan deposits.|22-SEP-14
27851|Mundogie Sandstone|64956|4|Described|p2 Tb. 23, p70, p90-91|Paleoproterozoic|Paleoproterozoic|Of Mount Partridge Group. Unconformably overlies Stag Creek Volcanics and Namoona Group. Max. depositional age: 2284+/-18Ma. Geological province: Pine Creek Orogen. Sample is a coarse muscovite-bearing quartzite from a conglomeratic bed.||||||07-FEB-11
27851|Mundogie Sandstone|65232|5|Briefly described|p45, p6 Fig. 5, App. 2|Palaeoproterozoic|Palaeoproterozoic|Of Mount Partridge Group. With Wildman Siltstone, unconformably overlies Namoona Group. Pebbly sandstone and conglomerate.||||||09-FEB-10
27851|Mundogie Sandstone|65339|5|Briefly described|p10.|||Correlative with Crater Formation.||||Is overlain by Wildman Siltstone.|Fine to coarse sandstone.|
27851|Mundogie Sandstone|67355|6|Mentioned|p7 Tb.2, p10||Paleoproterozoic|||Mount Partridge Group|||Shallow-marine arenite.|25-JAN-17
27851|Mundogie Sandstone|67564|3|Fully described|p8 Table 2, p9 Fig.4, pp11-12, pp14-15.|Paleoproterozoic|Paleoproterozoic|Formerly mapped as Coirwong Greywacke Member, Mundogie Sandstone Member and Mount Partridge Formation by Walpole (1963). Correlative of Crater Formation, Rum Jungle Region. Type locality around the northern nose of the Barramundie Dome. Up to 3500 m of mainly braided fluviatile, some shallow marine in upper portion, deposits. Forms prominent strike ridges, ranges and hills; commonly with talus deposits.|<2050 Ma.|Basal unit in Mount Partridge Group.||Unconformably overlies Stag Creek Volcanics and Masson Formation. Is conformably overlain by Wildman Siltstone.|Thickly bedded, medium to very coarse, feldspathic quartz meta-arenite; minor laminated metasiltstone and polymictic pebble conglomerate.|
27851|Mundogie Sandstone|67779|5|Briefly described|p6 Fig.5, p19.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Lateral equivalent of Crater Formation.||Basal unit in Mount Partridge Group.||Is overlain by Wildman Siltstone.||
27851|Mundogie Sandstone|69383|5|Briefly described|p26-29||Neoarchean|Of Woodcutters Supergroup. Pine Creek Orogen, Central Domain. LA-ICPMS  U-Pb geochronology analyses. Max deposition age given. Source different to Burrell Creek Formation source.|2518+/-5 Ma||||Massive white to grey, medium- to coarse-grained, well sorted quartz sandstone sampled.|
27851|Mundogie Sandstone|69418|6|Mentioned|p3:11|||Pine Creek Orogen. Hosts the Mary River Gossan sediment-hosted Zn-Cu deposit (described).||||||12-JUL-16
27851|Mundogie Sandstone|69420|4|Described|p5:4, 6, 9-11, 67, 79, 86, 93, 101, 112|Paleoproterozoic|Paleoproterozoic|Central and South Alligator regions, Central Domain, Pine Creek Orogen. c.1400m thick. Mainly braided fluviatile deposits; shallow-marine in upper portion. Hosts the Mary River Gossan (Zn-Cu-Pb) deposit, and the Margaret Sn deposit. Detrital zircon maximum deposition age.|<2284 +/- 18 Ma.|Mount Partridge Group.||Is overlain conformably by Wildman Siltstone. Lateral equivalent of Crater Formation.|Arkose, subarkose, feldspathic arenite, quartzite, conglomerate, phyllite and siltstone.|12-JUL-16
27851|Mundogie Sandstone|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Mount Partridge Group.||Is overlain conformably by Wildman Siltstone.|Thickly-bedded, medium- to very coarse-grained, poorly sorted, feldspathic quartz metasandstone; graded bedding, lenticular cross-beds and bedding scours are locally preseved.|
27851|Mundogie Sandstone|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1994+/-102 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
27851|Mundogie Sandstone|73083|6|Mentioned|p5-6|||A ridge of what was previously attributed to this unit in the Alligator River 1:250K Sheet (SW) was reassigned to the Wildman Siltstone. Produces a strong positive anomaly, probably caused by its magnetite-bearing pelite component.||||Underlain by Masson Formation. Conformably overlain by Wildman Siltstone.|Sandstone, siltstone, phyllite, schist, quartzite (pebbly in places), conglomerate, and pelite (locally magnetic).|
29251|Munmarlary Quartzite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group.  Feldspathic quartzite, quartzite.||||||07-NOV-08
29251|Munmarlary Quartzite|9691|5|Briefly described|Map Legend|||Of the Kakadu Group. Feldspathic quartzite, quartzite.||||||
29251|Munmarlary Quartzite|9701|5|Briefly described|Map Legend|Proterozoic|Archean|Of the Kakadu Group. Feldspathic quartzite, quartzite.||||||07-NOV-08
29251|Munmarlary Quartzite|22810|5|Briefly described|Table2 P5|||Maximum thickness: 200m.  Equivalent of Kudjumarandi Quartzite.||||||13-NOV-06
29251|Munmarlary Quartzite|35140|6|Mentioned|Fig.2|||||||||
29251|Munmarlary Quartzite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29251|Munmarlary Quartzite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29251|Munmarlary Quartzite|37462|6|Mentioned|Fig.4.8|||||||||
29251|Munmarlary Quartzite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29251|Munmarlary Quartzite|38239|6|Mentioned|Fig.2|||||||||
29251|Munmarlary Quartzite|38349|6|Mentioned|p10|||||||||
29251|Munmarlary Quartzite|38351|4|Described|p5|||||||||
29251|Munmarlary Quartzite|38884|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
29251|Munmarlary Quartzite|39069|5|Briefly described|Table 1|||||||||
29251|Munmarlary Quartzite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29251|Munmarlary Quartzite|40493|5|Briefly described|Table 1|||||||||
29251|Munmarlary Quartzite|40808|5|Briefly described|Table 2|||||||||
29251|Munmarlary Quartzite|41146|5|Briefly described|Fig.2|||||||||
29251|Munmarlary Quartzite|43187|5|Briefly described|p2|||||||||
29251|Munmarlary Quartzite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group. Feldspathic quartzite, quartzite.||||||07-NOV-08
29251|Munmarlary Quartzite|46700|5|Briefly described|P7, Table1 P12||Proterozoic|||||||
29251|Munmarlary Quartzite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Kakadu Group. Feldspathic quartzite, quartzite.||||||
29251|Munmarlary Quartzite|60680|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kakadu Group.  Feldspathic quartzite and quartzite.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
29251|Munmarlary Quartzite|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2025-2500Ma. Of Kakadu Group. Feldspathic quartzite, quartzite. Unconformably overlies and tectonically reworked into Nanambu Complex.||||||07-JAN-09
29251|Munmarlary Quartzite|64956|6|Mentioned|p87|||Lateral equivalent of Kudjumarndi Quartzite. Geological province: Pine Creek Orogen.||||||07-FEB-11
29251|Munmarlary Quartzite|66683|6|Mentioned|p368.|Paleoproterozoic|Paleoproterozoic|||Unit in Kakadu Group.||||
29251|Munmarlary Quartzite|67564|6|Mentioned|p11.|Paleoproterozoic|Paleoproterozoic|||Unit in Kakadu Group.||||
29251|Munmarlary Quartzite|67779|5|Briefly described|p6 Fig.5, p16.|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Correlated with Kudjumarndi Quartzite.||Unit in Kakadu Group.||Overlies Mount Basedow Gneiss.||
29251|Munmarlary Quartzite|69420|5|Briefly described|p5:4, 6-7, 24, 6|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Over 200m thick. Fluvial to shallow-marine deposits. Appears as Munmalary Quartzite on 5:2.||Kakadu Group.|||Gneissic orthoquartzite; minor schist.|12-JUL-16
29251|Munmarlary Quartzite|69917|6|Mentioned|p3 Table 1, p5 Tb. 2 |||See [misspelt] Munmalary Quartzite p41.|2530+/-17 Ma Max. dep. age U/Pb ICP-MS|||||18-SEP-18
29251|Munmarlary Quartzite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2530+/-17 Ma (MDA: U-Pb zircon LA-ICPMS).||||Quartzite (monomineralic granoblastic sutured quartz).|
26785|Munyi Member|22853|5|Briefly described|28|Proterozoic|Proterozoic|Of the Abner Sandstone.||||||13-NOV-06
26785|Munyi Member|23404|5|Briefly described|p641|||Of Corcoran Formation.||||||
26785|Munyi Member|23937|2|Defined|p88 App. 1|Calymmian|Calymmian|Previously of the Abner Sandstone, now reassigned to the Corcoran Formation (Maiwok Subgroup, Roper Group) into which it grades upwards.  Overlies Hodgson Sandstone.  Age: >1429+/-31Ma. Age inferred from Rb/Sr dating of Kyalla Formation. Max. thickness: 23m.  Geological Province: McArthur Basin.||||||14-NOV-17
26785|Munyi Member|24047|5|Briefly described|p27|Mesoproterozoic|Mesoproterozoic|Of the Abner Sandstone (Roper Group).  Geological Province: McArthur Basin.  See also p12 Fig. 10.||||||
26785|Munyi Member|24048|5|Briefly described|p71|Mesoproterozoic|Paleoproterozoic|Of the Corcoran Formation.  Geological Province: McArthur Basin.||||||07-NOV-08
26785|Munyi Member|24050|4|Described|p50, p8 Tb. 2|Mesoproterozoic|Mesoproterozoic|Previously included in the Abner Sandstone.  Ferruginous pebbly sandstone, mudstone and medium-grained sandstone.Of the Corcoran Formation.  Max. thickness: 15m.||||||13-NOV-06
26785|Munyi Member|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Corcoran Formation, Roper Group. Geological Province: McArthur Basin.||||||
26785|Munyi Member|40691|6|Mentioned|Fig.4|||||||||
26785|Munyi Member|41268|6|Mentioned|p291|||||||||
26785|Munyi Member|42385|5|Briefly described|p28|||Member of Abner Sandstone recognised  north and west of McArthur River Region.||||||13-NOV-06
26785|Munyi Member|42395|6|Mentioned|Fig.26 P86|||||||||
26785|Munyi Member|42639|5|Briefly described|p43|||Of Abner Sandstone.||||||13-NOV-06
26785|Munyi Member|42739|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Of the Corcoran Formation. Fine to coarse grained sandstone and mudstone; basal and near basal thin granule conglomerate beds.||||||19-OCT-05
26785|Munyi Member|42812|3|Fully described|p53, Table 5|||Of Corcoran Formation.||||||13-NOV-06
26785|Munyi Member|43010|4|Described|Table 30.|||Of Abner Sandstone?||||||13-NOV-06
26785|Munyi Member|43036|6|Mentioned|Fig.5|||Of Roper Group.||||||13-NOV-06
26785|Munyi Member|44299|4|Described|p.13|||SD/53-7,8. U(?) Proterozoic. Table 1.||||||
26785|Munyi Member|44300|14|Not recorded|map legend||Neoproterozoic|SD/53-7,8. U.Proterozoic, pt of Roper Gp.||||||
26785|Munyi Member|44332|14|Not recorded|p.8,opp.6,map|||(D53-14).||||||
26785|Munyi Member|44333|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
26785|Munyi Member|44400|2|Defined|Tb.1,opp.p.6,map|||U.?Proterozoic. (D53-6).||||||
26785|Munyi Member|44401|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
26785|Munyi Member|44471|14|Not recorded|p.10, opp.p.7, map|||(D53-10). Ferruginous member of Abner Sandstone (Roper Group).||||||
26785|Munyi Member|44472|5|Briefly described|map legend|||Of the Abner Sandstone (Roper Group).  Ferruginous sandstone, siltstone, shale.   Upper (?) Proterozoic.||||||02-DEC-04
26785|Munyi Member|44530|14|Not recorded|p.11,16, opp.12|||(D53-15).||||||
26785|Munyi Member|44531|14|Not recorded|map legend|||Upper (?) Proterozoic.||||||
26785|Munyi Member|45162|6|Mentioned|p163|||||||||
26785|Munyi Member|46861|6|Mentioned|Fig.2A|||||||||
26785|Munyi Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Corcoran Formation (Roper Group).  Ferruginous siltstone and fine sandstone; thin bedded , dessication cracks, iron-ozide pisolites; corss-bedded medium-grained sandstone; basal erosion surface veneered by quartz-pebble conglomerate.||||||
26785|Munyi Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Corcoran Formation. Ferruginous siltstone and fine-grained sandstone; thin bedded, dessication cracks, iron oxide psiolites; cross bedded medium grained sandstone.||||||13-NOV-06
26785|Munyi Member|65228|6|Mentioned|Fig.02.|||||Unit in Corcoran Formation.||||
26785|Munyi Member|65342|6|Mentioned|p8.|||McArthur Basin. Max. thickness at least 23 m.||Unit in Corcoran Formation.||||
26785|Munyi Member|69430|4|Described|p15:27, 29-30|Calymmian|Calymmian|Dunn (1963) divided the Abner Sandstone in the Roper River region into four Members, this unit being the topmost. Later reassigned to the base of the overlying Corcoran Formation by Haines et al. (1993). The lower three were raised to Formation status by Abbott et al. (2001). McArthur Basin. 13-23m thick. Shallow-marine to fluvial sediments.||Corcoran Formation.||Overlies Hodgson Sandstone conformably to disconformably.|Red to brown ferruginous sandstone, siltstone, mudstone, conglomerate and pisolitic ironstone.|12-JUL-16
26785|Munyi Member|69673|6|Mentioned|p36|||||Corcoran Formation||Disconformably overlies Hodgson Sandstone||
26785|Munyi Member|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Of Corcoran Formation? Or underlying Hodgson Sandstone? Paralic to fluvial sandstone, siltstone, mudstone.||||Overlies Hodgson Sandstone. Overlain by (rest of?)Corcoran Formation.||
26785|Munyi Member|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Corcoran Formation||Overlies Hodgson Sandstone.|Fluvial sandstone.|
26785|Munyi Member|70897|6|Mentioned|Fig.1.7.6|||Appears simply as Munyi. McArthur Basin.||||||
26785|Munyi Member|70968|2|Defined|p23, p39, p48, p51-56, p69, p126, p131|Ectasian|Ectasian|See also p140, p143-144. Of Dunn (1963), who identified this as one of his four Members of his Abner Sandstone. Subsequently reassigned to the Corcoran Formation by Haines et al. (1993). Defined by Abbott and Sweet in Abbott et al. (2001). Named after Munyi Bluff. The type section is the interval 34.8m (base) - 10.7m depth in drillhole Urapunga-5, at 437712mE 8373601mN in URAPUNGA sheet. Has a distinctive dark tone on aerial photographs. Lithology well described and illustrated. Varied environments of deposition from fluvial to very shallow-marine.||Basal Corcoran Formation.||Disconformably overlies Hodgson Sandstone. Is intruded by Derim Derim Dolerite sills.|Dark red- to brown-weathering, locally ferruginous, thinly to medium bedded, commonly cross-bedded sandstone; interbedded siltstone, mudstone, minor conglomerate and minor ironstone. Includes distinctive pisolitic red beds.|
26785|Munyi Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 12-23m thick. Shallow-marine to fluvial deposits.||Basal Corcoran Formation.||Conformably to disconformably overlies Hodgson Sandstone.|Red to brown ferruginous sandstone, siltstone, mudstone, conglomerate and pisolitic ironstone.|
26785|Munyi Member|71488|5|Briefly described|p141 fig 1b, p148|||||Corcoran Formation||Unconformably overlies the Hodgson Sandstone.||
26785|Munyi Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga, Beetaloo Sub-basin and Bauhinia Downs Regions, McArthur Basin.||Corcoran Formation||||24-SEP-18
26785|Munyi Member|71893|5|Briefly described|p24|||McArthur Basin.||Corcoran Formation||Disconformably (in places conformably) overlies the Hodgson Sandstone.||
26785|Munyi Member|73242|5|Briefly described|p39|||||Corcoran Formation, Maiwok Subgroup, Roper Group||Underlain by Hodgson Sandstone, Collara Subgroup. Intruded by Derim Derim Dolerite.|Includes fluvial sandstone.|
26787|Murra-Kamangee Granodiorite|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Muscovite-biotite tonalite, moderatly to strongly foliated, garnetiferous, contains numerous xenoliths.||||||07-NOV-08
26787|Murra-Kamangee Granodiorite|9579|5|Briefly described|Map Sheet|Orosirian|Orosirian||ca. 1850-1840 Ma (Page, BMR)|||Synorogenic with the Mount Litchfield Granite, Wagait Granite.||
26787|Murra-Kamangee Granodiorite|22809|3|Fully described|12|||Age: 1840 Ma.||||||13-NOV-06
26787|Murra-Kamangee Granodiorite|23714|4|Described|p17|||See also page 14, Table 2. Litchfield Province.||||||
26787|Murra-Kamangee Granodiorite|23715|5|Briefly described|Map legend||Proterozoic|||||||02-MAR-18
26787|Murra-Kamangee Granodiorite|24197|5|Briefly described|p18|Paleoproterozoic|Paleoproterozoic|Of the Allia Suite. Geological province: Litchfield Block/Pine Creek Inlier. See also Marra-Kamangee Granite of Pine Creek Inlier - one is misspelt?||||||07-FEB-11
26787|Murra-Kamangee Granodiorite|41645|3|Fully described|p14|||||||||
26787|Murra-Kamangee Granodiorite|41646|6|Mentioned|Map legend|Paleoproterozoic||Tonalite; biotite granodiorite, sometimes garnetiferous, weakly to moderatly foliated, numerous xenoliths; porphyritic biotite adamellite; porphyritic biotite microdiorite. (1852 +/- 33Ma).||||||07-NOV-08
26787|Murra-Kamangee Granodiorite|41660|5|Briefly described|Map legend|Paleoproterozoic||Biotite granodiorite; tonalite; often garnetiferous, may be weakly- to moderately-foliated, contains numerous xenoliths. Age: 1852 +/1 33 Ma U/Pb.||||||07-NOV-08
26787|Murra-Kamangee Granodiorite|41661|3|Fully described|p16|||||||||
26787|Murra-Kamangee Granodiorite|41980|5|Briefly described|Table 3 P575|||||||||
26787|Murra-Kamangee Granodiorite|63866|5|Briefly described|p105, p107|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. |1852  +/- 33 Ma (Page et al., 1985)|||||
26787|Murra-Kamangee Granodiorite|64956|5|Briefly described|p2 Tb. 4, p50, p53, p56|Paleoproterozoic|Paleoproterozoic|Has contact with Fish Billabong Formation. Max. deposition age: 1862+/-3Ma, cryst age1853 +/-4 Ma . Geological province: Pine Creek Orogen. One sample is medium-grained biotite gneiss/granodiorite(?); another is described as quartz-plagioclase-biotite granodiorite.||||||02-MAR-18
26787|Murra-Kamangee Granodiorite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Biotite-granodiorite, tonalite, porphyritic biotite-quartz monzonite, porphyritic biotite microdiorite; commonly garnetiferous, may be weakly to moderately foliated, contains numerous xenoliths.|
26787|Murra-Kamangee Granodiorite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Actually spelt Murra-Kamangee Graniodionte||Unit in Allia Creek Suite.|||Biotite-granodiorite, tonalite, porphyritic biotite-quartz monzonite, porphyritic biotite microdiorite; commonly garnetiferous, may be weakly to moderately foliated, contains numerous xenoliths.|23-NOV-11
26787|Murra-Kamangee Granodiorite|67232|5|Briefly described|p5.|Paleoproterozoic|Paleoproterozoic|Southern Litchfield Province, Pine Creek Orogen. Contains mafic igneous xenoliths, presumed to be Wangi Basics. |1854 +/- 4 Ma (Worden et al. 2008a).|||Intrudes the former Wangi Basics.||
26787|Murra-Kamangee Granodiorite|69420|5|Briefly described|p5:18-19, 28-29|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Garnet is almost always present as euhedra to 2cm diameter. Two other age determinations are given.|1862 +/- 2 Ma (SHRIMP U-Pb zircon).|Allia Creek Suite.|||Medium-grained, moderately to strongly foliated, garnet-bearing granodiorite to tonalite, quartz monzonite.|12-JUL-16
26787|Murra-Kamangee Granodiorite|69435|5|Briefly described|p20:3|Paleoproterozoic|Paleoproterozoic|Part of the basement to the Fitzmaurice Basin.|1852 +/- 33 Ma.|||Is overlain unconformably by Moyle River Formation.||12-JUL-16
26787|Murra-Kamangee Granodiorite|69673|6|Mentioned|p60 fig 48||||1852 +/- 33 Ma|||||
26787|Murra-Kamangee Granodiorite|69933|6|Mentioned|p1, p5|||In contact with the Hermit Creek Metamorphics [although the nature of the contact is not provided].||||||
26787|Murra-Kamangee Granodiorite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1853 +/- 4 Ma.|Allia Creek Suite.|||Biotite granodiorite, tonalite, porphyritic biotite-quartz monzonite, porphyritic biotite microdiorite; commonly garnetiferous, may be weakly to moderately foliated, numerous xenoliths.|
26787|Murra-Kamangee Granodiorite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite|
26787|Murra-Kamangee Granodiorite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1862+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Medium-grained biotite gneiss; medium-grained quartz-plagioclase-biotite granodiorite.|
24412|Murrenja Dolerite|9324|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Dolerite.||||||
24412|Murrenja Dolerite|9579|5|Briefly described|Map Sheet|Mesoproterozoic|Mesoproterozoic|Middle Proterozoic age.||||||
24412|Murrenja Dolerite|22813|5|Briefly described|Map|Mesoproterozoic|Mesoproterozoic|Dolerite.||||||19-OCT-05
24412|Murrenja Dolerite|40764|6|Mentioned|Map legend|Neoproterozoic|Mesoproterozoic|Middle to Late Proterozoic||||||
24412|Murrenja Dolerite|40765|3|Fully described|p11|||||||||
24412|Murrenja Dolerite|40809|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24412|Murrenja Dolerite|41645|4|Described|p17|||||||||
24412|Murrenja Dolerite|41646|6|Mentioned|Map legend|Mesoproterozoic||Altered gabbro; dolerite.||||||17-OCT-05
24412|Murrenja Dolerite|41660|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Dolerite.||||||07-OCT-05
24412|Murrenja Dolerite|41661|6|Mentioned|Fig.5|||||||||
24412|Murrenja Dolerite|41980|5|Briefly described|Table 3 P575|||||||||
24412|Murrenja Dolerite|43187|5|Briefly described|p2|||||||||
24412|Murrenja Dolerite|63866|5|Briefly described|p106, p108, p117, p124|Mesoproterozoic|Mesoproterozoic|Litchfield Province, Pine Creek Orogen.||||Intrudes the Moyle River Formation.|Bi-modal magmatic rocks.|
24412|Murrenja Dolerite|64698|4|Described|lithinterp table|Statherian|Orosirian|Age ~1750-1820Ma. Altered gabbro and dolerite. Intrudes Fitzmaurice Group and older rocks.||||||07-JAN-09
24412|Murrenja Dolerite|67167|5|Briefly described|Map legend.||||||||Dolerite, minor gabbro.|
24412|Murrenja Dolerite|67186|5|Briefly described|Map legend.||||||||Dolerite, minor gabbro|23-NOV-11
24412|Murrenja Dolerite|67232|6|Mentioned|p7.|||Litchfield Province, Pine Creek Orogen.||||||
24412|Murrenja Dolerite|67779|6|Mentioned|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||||||
24412|Murrenja Dolerite|69435|5|Briefly described|p20:3|Mesoproterozoic|Mesoproterozoic||1537 Ma, 1393 Ma (K/Ar).|||Intrudes Moyle River Formation.||12-JUL-16
24412|Murrenja Dolerite|69673|6|Mentioned|p60 fig 48||||1537 - 1393 Ma|||||
24412|Murrenja Dolerite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolerite|
31843|Mutitjulu Arkose|24301|2|Defined|p37 Appendix 1|Cambrian|Neoproterozoic|Replaces informal names "Uluru arkose" and Uluru Arkose. Also previously included as part of the Mount Currie Conglomerate (Forman, 1965). Maximum thickness: ~2400m. Geological Province: Amadeus Basin||||||
31843|Mutitjulu Arkose|24302|5|Briefly described|Map Legend|Cambrian|Cambrian|Coarse to very coarse-grained arkosic sandstone and arkose, trough cross-bedded; granule to pebble conglomerate, fine- to medium-grained arkosic sandstone. Geological Province: Amadeus Basin||||||29-SEP-05
31843|Mutitjulu Arkose|24497|5|Briefly described|Map legend|Early Paleocene|Neoproterozoic|Geological Province: Amadeus Basin.||||||
31843|Mutitjulu Arkose|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
31843|Mutitjulu Arkose|68100|6|Mentioned|p27|||Amadeus Basin. Detrital zircon ages mentioned.||||||
31843|Mutitjulu Arkose|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Idirriki Sub-basin, SW Amadeus Basin.||||Is overlain by Maurice Formation.||12-JUL-16
31843|Mutitjulu Arkose|69438|4|Described|p23:3-4, 22-23, 26-27|Early Cambrian|Ediacaran|Young et al. (2002); previously the Uluru arkose. Amadeus Basin. Forms the inselberg at Uluru. Dips steeply to the SW and is over 2400m thick. Possibly a lateral variant of Mount Currie Conglomerate; might be equivalent to Arumbera Sandstone.||Pertaoorrta Group.||Is correlated with the Mount Currie Conglomerate.|Well sorted, planar bedded or ripple laminated, very fine to medium sandstone; trough cross-bedded sandstone to granule conglomerate (most common facies); planar-bedded and cross-bedded granule to pebble conglomerate; massive conglomerate.|12-JUL-16
31843|Mutitjulu Arkose|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
31843|Mutitjulu Arkose|69673|6|Mentioned|p65|||||||||
31843|Mutitjulu Arkose|70839|4|Described|p324,329-330,341-345|Cambrian|Cambrian|Of the southern Amadeus Basin. Part of Supersequence 4. Estimated thickness: at least 2.5km. 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). Metamorphosed to greenschist-facies (Edgoose et al., 2004) indicating significant burial. Alternative possibility from this study suggests this unit dates from late in the development of c. 1.0 Ga Ngaanyatjarra Rift.||||Underlain by Winnall beds. Equivalent to Mount Currie Conglomerate.|Finer-grained conglomerate. Clasts include fresh igneous and metamorphic rocks including granite, basalt, and other lithologies.|
31843|Mutitjulu Arkose|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).||||Equivalent (assumed) to the Mount Currie Conglomerate.||
30315|Nagi Formation|22538|6|Mentioned|Fig3 P709|||||||||
30315|Nagi Formation|23398|5|Briefly described|p444|Statherian|Statherian|Age: 1634+/-4Ma.||||||20-NOV-06
30315|Nagi Formation|23937|2|Defined|p89 App. 1, p12|Statherian|Statherian|Previously mapped as upper part of Vizard Fm (Dunn,1963a). Now part of the upgraded Vizard Gp. Unconformably overlain by Mt Birch Sst; disconformably overlies Saint Vidgeon Fm. Age: 1634Ma (Page et al, 2000). Max. thick: 220m. Geol.Prov: McArthur Basin.||||||18-APR-05
30315|Nagi Formation|60483|5|Briefly described|p7 Fig. 5|||Of the Vizard Group. Geological Province: McArthur Basin.||||||05-OCT-07
30315|Nagi Formation|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the Vizard Group. Feldspathic sandstone, dolomitic sandstone and dolarenite.||||||20-NOV-06
30315|Nagi Formation|63866|5|Briefly described|p114|Statherian|Statherian|Isa Superbasin.|1634 +/- 4 Ma (Page et al, 2000)|Vizard Group||Overlain by the Saint Vidgeon Group.||
30315|Nagi Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Vizard Group.||||
30315|Nagi Formation|65228|4|Described|Table 1.|Statherian|Statherian|At Mt. Birch, near Roper Bar. Measured section. Possibly equivalent to Lynott Formation and Stretton Sandstone.|1634 +/- 4 Ma (SHRIMP).|Unit in Vizard Group.||Overlies Saint Vidgeon Formation.|Dominantly sandstones.|
30315|Nagi Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1634 +/- 4 Ma.|||||
30315|Nagi Formation|69430|4|Described|p15:3, 22-23, 30|Statherian|Statherian|Formerly mapped as part of the Vizard Formation (Dunn, 1963). Southern McArthur Basin. 220m thick. Fluvial to shallow-marine sediments. SHRIMP U-Pb zircon age from a tuff bed. |1634 +/- 4 Ma (Page et al., 2000).|Vizard Group.||Disconformably overlies Saint Vidgeon Formation. Is overlain unconformably by Mount Birch Sandstone (Nathan Group). Correlates with Lynott Formation (upper McArthur Group).|A succession of fine-grained arkose and shale, dolomitic sandstone and siltstone, K-metasomatised sedimentary rocks and tuff, and chert.|12-JUL-16
30315|Nagi Formation|69673|6|Mentioned|p16 fig 13|Statherian|Statherian|Urapunga Fault Zone|1634 +/- 4 Ma|Vizard Group||Overlies Saint Vidgeon Formation||
30315|Nagi Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1634+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Tuffite.|
30315|Nagi Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Vizard Group.|||Dolomitic and feldspathic sandstone, dolomitic siltstone, dolarenite.|04-MAR-20
30315|Nagi Formation|72373|4|Described|iii,p1,24-27,33|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Reference section: 1 km S of Mount Birch in central URAPUNGA. Exposures confined to southeastern URAPUNGA, mostly south of the Roper River. From URAPUNGA map sheet. Uppermost surface is interpreted as a paleoregolith surface below basal conglomerates of the Mount Birch Sandstone. Previous age constraints provided by 1634+\-4 Ma tuff about 30m above the base of the formation, and 1640+\-4 Ma tuff from the underlying Saint Vidgeon Formation (Page et al., 2000). Sample 2711446 (UR17TJM049: Fine-grained chert-bearing quartz sandstone) yielded interpreted max depositional age of 1631+\-16 Ma. Shows similar detrital zircon age spectra to Stretton Sandstone and Yalco Formation, supporting previous interpretations that these formations are broadly equivalent, and potentially sources from the same or similar terranes.|1631+\-16 Ma (max dep age)|Uppermost unit of Vizard Group.||Unconformably overlain by Mount Birch Sandstone. Underlain unconformably by Saint Vidgeon Formation.|Fine arkose and shale, dolomitic sandstone and siltstone, potassic tuff and chert .|01-OCT-19
30315|Nagi Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age.|1634 +/-4 Ma|Vizard Group||Overlies Saint Vidgeon Formation and shown as unconformably underlying Mount Birch Sandstone.||
30315|Nagi Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin. Urapunga Fault Zone.|1634 +/- 4 Ma|Vizard Group||Underlain by Saint Vidgeon Formation. Unconformably overlain[?] by Mount Birch Sandstone (Nathan Group).||
30315|Nagi Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Urapunga Fault Zone. U-Pb zircon sedimentary depositional age (Ma).|1634 +/- 4 Ma|Vizard Group||Overlies Saint Vidgeon Formation and unconformably underlies Nathan Group.||
30315|Nagi Formation|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1634 +/- 4 Ma (see Fig.1.2)|Vizard Group||Unconformably overlain(?) by Mount Birch Sandstone. Underlain by Saint Vidgeon Formation.||
76184|Namarrkon Amphibolite|67779|2|Defined|p8 Table 1, p24 Fig.24, pp68-69, p117.|Paleoproterozoic|Paleoproterozoic|New name, after Namarrkon waterhole. Nimbuwah Domain, Pine Creek Orogen. Formerly part of Zamu Complex and Zamu Dolerite (Ferguson and Needham, 1978). Exposed c.15 km ENE, and as an isolated outcrop c.30 km SE, of Oenpelli township; also intersected in drillcore c.2 km SE of the Nabarlek Uranium Prospect. Geochemistry is discussed in some detail.||||Occurs within Cahill Formation and Nourlangie Schist.|Fine- to medium-grained, hornblende-feldspar (+/- biotite) amphibolite; locally garnetiferous; moderate schistosity.|
76184|Namarrkon Amphibolite|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||||||Amphibolite: intrusive, metagabbro to metagabbroic diorite, fine- to medium-grained, locally contains biotite.|
24417|Namatjira Formation|22561|6|Mentioned|p18|Neoproterozoic|Neoproterozoic|||||||
24417|Namatjira Formation|22646|5|Briefly described|p 101|||||||||
24417|Namatjira Formation|22650|6|Mentioned|p 159|||Age uncertain but Kennard and Lindsay correlate this unit with the Todd River Dolomite p 159.||||||
24417|Namatjira Formation|22651|4|Described|p 182|||Interfingers with the Arumbera sandstone.  Abundant vertical and horizontal burrows within the Namatjira Formation suggests Cambrian age p182.||||||
24417|Namatjira Formation|22652|6|Mentioned|p 223|||||||||
24417|Namatjira Formation|22653|5|Briefly described|p 228|Early Cambrian|Neoproterozoic|||||||
24417|Namatjira Formation|22654|6|Mentioned|Fig 1 on p 246|||||||||
24417|Namatjira Formation|22804|6|Mentioned|Fig 2 on p432|Early Cambrian||Parent - Pertaoorrta Group.  Max. Age - ?Neoproterozoic or Early Cambrian.||||||
24417|Namatjira Formation|22826|6|Mentioned|Fig 2 on p565|Cambrian|Cambrian|||||||
24417|Namatjira Formation|23361|5|Briefly described|16 Fig.4|Neoproterozoic III|Neoproterozoic|||||||
24417|Namatjira Formation|40740|3|Fully described|p20|||||||||
24417|Namatjira Formation|41233|2|Defined|p17|Early Cambrian||||||||
24417|Namatjira Formation|41270|6|Mentioned|p274|||||||||
24417|Namatjira Formation|41801|5|Briefly described|p217|||||||||
24417|Namatjira Formation|42940|5|Briefly described|Plate 8|||||||||
24417|Namatjira Formation|43503|6|Mentioned|12-50|Botoman|Atdabanian|||||||
24417|Namatjira Formation|44133|6|Mentioned|p42  |||||||||
24417|Namatjira Formation|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
24417|Namatjira Formation|62376|5|Briefly described|p18|Late Proterozoic|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
24417|Namatjira Formation|62379|5|Briefly described|p7 Fig. 2|Late Proterozoic|Late Proterozoic|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||
24417|Namatjira Formation|64068|6|Mentioned|p224|||Amadeus Basin. Correlated with Shadow Group, Georgina Basin.||||||
24417|Namatjira Formation|65233|5|Briefly described|p3 Fig. 2|Neoproterozoic|Neoproterozoic|Of the Pertaoorrta Group. Geological province: Amadeus Basin.||||||07-FEB-11
24417|Namatjira Formation|67856|6|Mentioned|p338 fig 4-30|Early Cambrian|Early Cambrian|||Of Pertaoorta Group.||||
24417|Namatjira Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Amadeus Basin.||||Overlies Arumbera Sandstone. Is overlain by Chandler Formation.||12-JUL-16
24417|Namatjira Formation|69438|3|Fully described|p23:2-3, 24, 27-28|Early Cambrian|Early Cambrian|Bradshaw in Kennard and Nicoll (1986); Bradshaw (1988). Restricted to a 10km strike section in eastern Gardiner Range Anticline, Carmichael Sub-basin, Amadeus Basin. 50-100m thick. Suggested correlations include with parts of Arumbera Sandstone or Todd River Dolostone. Contains dispersed, non-economic copper mineralisation in Namatjiras prospect (Areyonga Copper Deposit).||Pertaoorrta Group.||Overlies or partially interfingers with Arumbera Sandstone. Is overlain disconformably by Chandler Formation.|A basal clastic unit rapidly transitions upwards to a mixed carbonate and clastic unit, which is topped by a carbonate unit, mostly comprising smaller depositional cycles. Contains horizontal trails and steeply inclined burrows.|12-JUL-16
24417|Namatjira Formation|69443|6|Mentioned|p28:14|||Amadeus Basin.||||Correlated with (part of) the Shadow Group.||12-JUL-16
24417|Namatjira Formation|69673|6|Mentioned|p64 fig 53|||||||Overlies Arumbera Sandstone, disconformably overlain by Chandler Formation||
24417|Namatjira Formation|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
24417|Namatjira Formation|71841|5|Briefly described|p1|Early Cambrian|Early Cambrian|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by Arumbera Sandstone.||
24417|Namatjira Formation|71842|5|Briefly described|p3|Early Cambrian|Early Cambrian|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by Arumbera Sandstone.||
24417|Namatjira Formation|73085|6|Mentioned|p1|early Cambrian|early Cambrian|||||Partly underlain by, equivalent to and overlain by Arumbera Sandstone. Possible equivalent to Winnall Group.||
38414|Namerinni Group|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Shillinglaw Formation and Carruthers Creek Formation.||||||07-NOV-08
38414|Namerinni Group|23733|6|Mentioned|p28 Tb.5, 29|||See also p32 Fig. 19.  Of the Tennant Inlier.||||||
38414|Namerinni Group|23809|5|Briefly described|p47, p27 Fig. 25|Proterozoic|Proterozoic|Correlates with the McArthur Group (McArthur Basin), Lumbunya (mispelt Limbunya) Group (Birrindudu Basin), and the Bungle Bungle Dolomite (Victoria Basin).  Geological Province: Ashburton Province.||||||
38414|Namerinni Group|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Age: 1640Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
38414|Namerinni Group|24303|2|Defined|p15, p57 Appendix|Statherian|Statherian|Unconformably overlain by the Renner Group; unconformably overlies the Tomkinson Creek Group. Max. Thickness: 2800m. Formerly included in Tomkinson Creek beds. Comprises Jeromah, Carruthers, Shillinglaw and Willeray Formations. Probable age: 1660-1610 Ma.||||||25-JAN-10
38414|Namerinni Group|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Willieray, Shillinglaw (with upper and lower facies), Carruthers (with upper, middle and lower facies) and Jeromah Formations.||||||07-NOV-08
38414|Namerinni Group|50353|5|Briefly described|Map Legend|||||||||
38414|Namerinni Group|60684|6|Mentioned|p12|||Unconformably overlies Bootu Formation. On HELEN SPRINGS map sheet.||||||
38414|Namerinni Group|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated rocks: quartz arenite, sublithic/lithic arenite, dolostone, mudstone; minor conglomerate.  In the Tennant Creek region.||||||07-NOV-08
38414|Namerinni Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|Northern Tennant Creek Province unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
38414|Namerinni Group|64780|5|Briefly described|p62 Fig.3, p63 Fig.4 |Palaeoproterozoic|Palaeoproterozoic||||Includes the Willieray, Shillinglaw, Carruthers, and Jeromah Formations.|Unconformably overlies the Tomkinson Creek Group.||
38414|Namerinni Group|65209|5|Briefly described|p35 Fig.1, p38|Paleoproterozoic|Paleoproterozoic|Geol. Prov: northern Tomkinson Creek Province.|||Jeromah Formation|Overlies Tomkinson Creek Group with angular unconformity; correlates with McArthur Group and McNamara Group.||05-JAN-17
38414|Namerinni Group|66860|6|Mentioned|p6 Tb.1|||Tennant Region. Deposition was coeval with Yaya and Iwupataka Metamorphic Complexes (Arunta Region).|1660-1640 Ma.|||||
38414|Namerinni Group|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Quartz arenite, sublithic/lithic arenite, dolostone, mudstone; minor conglomerate. Evaporite pseudomorphs locally abundant; stromatolites.|
38414|Namerinni Group|67323|4|Described|Eastern Australia Time-Space Plot, p35|Paleoproterozoic|Paleoproterozoic|Tennant Creek/Davenport area.|~1660-1650 Ma.||Includes Willieray, Shillinglaw, Carruthers Creek, Jeromah Formations.|Overlies Tomkinson Creek Group. Is overlain by Renner Group.|Quartz arenite, sublithic/lithic arenite, dolostone, mudstone, minor conglomerate.|
38414|Namerinni Group|69417|5|Briefly described|p2:5-6|Statherian|Statherian|Tomkinson Basin.|c.1650-1630 Ma.|||||12-JUL-16
38414|Namerinni Group|69424|6|Mentioned|p9:2|||||||||12-JUL-16
38414|Namerinni Group|69425|6|Mentioned|p10:2|||Tennant Region.||||||12-JUL-16
38414|Namerinni Group|69429|6|Mentioned|p14:4 Fig.14.7|Mesoproterozoic|Mesoproterozoic|Tomkinson Province.||||||12-JUL-16
38414|Namerinni Group|69431|4|Described|p16:1-4, 12-18, 20, 22-24|Statherian|Statherian|Tomkinson Province. Up to c.2800m thick. Shows cyclicity on a number of scales.|c.1660-1610 Ma (SHRIMP U-Pb zircon).||Jeromah, Caruthers, Shillinglaw and Willieray Formations.|Unconformably overlies Tomkinson Creek Group. Is overlain unconformably by the Renner Group. Correlated with Umbolooga Subgroup (McArthur Group).|Unmetamorphosed succession of sandstone, siltstone and carbonate rocks.|12-JUL-16
38414|Namerinni Group|69673|6|Mentioned|p3 fig 2, p18, p57, p58|Statherian|Statherian|Maximum thickness of 2800m, age not well constrained and is currently based on its correlation with the McArthur Group.||||Unconformably overlies the Tomkinson Creek Group, unconformably overlain by the Renner Group, Correlated with McArthur Group, Limbunya Group|Sandstone, siltstone and carbonate rocks.|
38414|Namerinni Group|70968|5|Briefly described|p92, p95, p98, p102, p123, p138-139|||Tomkinson Province.|1660-1610 Ma (Ward, 1983; Donnellan, 2013).|||Is overlain unconformably by Gleeson Formation (Renner Group).||
38414|Namerinni Group|71374|6|Mentioned|p2|||Tomkinson Province.||||||
38414|Namerinni Group|71893|4|Described|p52, p56, p60, p64|Statherian|Statherian|Tennant Region.|ca. 1660-1610 Ma (Ward 1983, Donnellan 2013c)|||Unconformably overlain by the Gleeson Formation (Renner Group).||
38414|Namerinni Group|72373|5|Briefly described|iii,p1-2,36,39|Paleoproterozoic|Paleoproterozoic|Geological province: Tomkinson Province.|||Includes Willieray, Shillinglaw and Carruthers formations.|||
38414|Namerinni Group|72718|6|Mentioned|p9|||Tomkinson Province. Favenc package. Tennant Region.||||||
27856|Nanambu Complex|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|The Mount Basedow Gneiss (Kakadu Group) is transitional into this complex.||||||07-NOV-08
27856|Nanambu Complex|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite, migmatite, gneiss, granite schist.  Conformably overlain by the Kakadu Group.  Age: ~2500Ma.||||||07-NOV-08
27856|Nanambu Complex|9691|5|Briefly described|Map Legend|||Gneiss, quartzite.||||||01-JUN-05
27856|Nanambu Complex|9701|5|Briefly described|Map Legend|Proterozoic|Archean|Gneiss, quartzite.||||||07-NOV-08
27856|Nanambu Complex|9733|5|Briefly described|Map Legend|Archean|Archean|Granite, gneiss, schist.||||||07-NOV-08
27856|Nanambu Complex|22446|6|Mentioned|p19||Archean|||||||07-NOV-08
27856|Nanambu Complex|22479|5|Briefly described|fig1 p2|Archean|Archean|2500Ma old. Placed in Alligator Rivers Region.||||||12-JUL-16
27856|Nanambu Complex|22600|6|Mentioned|Map legend|||||||||
27856|Nanambu Complex|23374|5|Briefly described|Fig3 p5,8,28||Archean|In the Pine Creek Inlier.||||||12-JUL-16
27856|Nanambu Complex|24047|5|Briefly described|p5 Fig.4, p40|Archean|Archean|Granite, gneiss, schist.  Age: 2500Ma.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
27856|Nanambu Complex|24049|5|Briefly described|Map Legend|Archean|Archean|In regional setting map legend.||||||07-NOV-08
27856|Nanambu Complex|24442|6|Mentioned|p44|||In Jabiru.||||||
27856|Nanambu Complex|29551|6|Mentioned|p27|||||||||
27856|Nanambu Complex|30142|6|Mentioned|p13|||||||||
27856|Nanambu Complex|30559|6|Mentioned|p282|||||||||
27856|Nanambu Complex|30680|6|Mentioned|p309|||||||||
27856|Nanambu Complex|30832|5|Briefly described|p318|||||||||
27856|Nanambu Complex|30863|6|Mentioned|p50|||||||||
27856|Nanambu Complex|31268|6|Mentioned|p20|||||||||
27856|Nanambu Complex|31347|6|Mentioned|p133|||||||||
27856|Nanambu Complex|31833|6|Mentioned|Table 2|||||||||
27856|Nanambu Complex|32397|5|Briefly described|p397|||||||||
27856|Nanambu Complex|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27856|Nanambu Complex|32660|5|Briefly described|Table 2|||||||||
27856|Nanambu Complex|32932|4|Described|p324|||||||||
27856|Nanambu Complex|32959|6|Mentioned|p3|||||||||
27856|Nanambu Complex|33084|6|Mentioned|p11|||||||||
27856|Nanambu Complex|33186|4|Described|p289|||||||||
27856|Nanambu Complex|34834|6|Mentioned|p210|||||||||
27856|Nanambu Complex|35140|6|Mentioned|Fig.1|||||||||
27856|Nanambu Complex|35165|6|Mentioned|p1421|||||||||
27856|Nanambu Complex|35465|6|Mentioned|Fig.2|||Summary of positions of magnetic units in the Lower Proterozoic||||||
27856|Nanambu Complex|35495|6|Mentioned|p350|||||||||
27856|Nanambu Complex|35551|6|Mentioned|p11|||||||||
27856|Nanambu Complex|35950|5|Briefly described|p299|||See also Fig.1||||||
27856|Nanambu Complex|36085|6|Mentioned|p502|||||||||
27856|Nanambu Complex|36473|6|Mentioned|Map legend|Proterozoic|Archean|Archaean to Proterozoic||||||07-NOV-08
27856|Nanambu Complex|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27856|Nanambu Complex|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27856|Nanambu Complex|37462|4|Described|p220|||Also described Table 4.II.||||||20-NOV-06
27856|Nanambu Complex|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite, migmatite, gneiss, granite, schist.||||||07-NOV-08
27856|Nanambu Complex|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27856|Nanambu Complex|38239|6|Mentioned|Fig.2|||||||||
27856|Nanambu Complex|38349|4|Described|p3|||||||||
27856|Nanambu Complex|38351|4|Described|p4|||||||||
27856|Nanambu Complex|38639|6|Mentioned|Fig.1|||||||||
27856|Nanambu Complex|38884|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27856|Nanambu Complex|39048|6|Mentioned|p824|||||||||
27856|Nanambu Complex|39069|6|Mentioned|Table 1|||||||||
27856|Nanambu Complex|39118|6|Mentioned|p140|||||||||
27856|Nanambu Complex|39357|6|Mentioned|p3|||||||||
27856|Nanambu Complex|39563|6|Mentioned|Map legend|Paleoproterozoic|Archean|Early Proterozoic to Archaean||||||07-NOV-08
27856|Nanambu Complex|39566|6|Mentioned|p49|||||||||
27856|Nanambu Complex|39620|6|Mentioned|p9|||||||||
27856|Nanambu Complex|39679|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
27856|Nanambu Complex|39801|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic. Leucogranite, migmatite, gneiss, granite schist.||||||07-NOV-08
27856|Nanambu Complex|40104|6|Mentioned|p334|||||||||
27856|Nanambu Complex|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite, migmatite, gneiss, granite schist.||||||07-NOV-08
27856|Nanambu Complex|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite, migmatite, gneiss, granite, schist.||||||07-NOV-08
27856|Nanambu Complex|40243|6|Mentioned|p150|||||||||
27856|Nanambu Complex|40296|6|Mentioned|p345|||||||||
27856|Nanambu Complex|40493|6|Mentioned|p21|||||||||
27856|Nanambu Complex|40768|5|Briefly described|p392|||Mention Fig.2||||||
27856|Nanambu Complex|40808|6|Mentioned|Table 2|||||||||
27856|Nanambu Complex|40811|6|Mentioned|p317|||||||||
27856|Nanambu Complex|40823|6|Mentioned|Map legend|Paleoproterozoic|Archean|Archaean to Early Proterozoic||||||07-NOV-08
27856|Nanambu Complex|41072|6|Mentioned|p65|||||||||
27856|Nanambu Complex|41125|6|Mentioned|p15|||See also Fig.6||||||
27856|Nanambu Complex|41146|5|Briefly described|p857|||||||||
27856|Nanambu Complex|41147|5|Briefly described|p1152|||||||||
27856|Nanambu Complex|41304|6|Mentioned|Map legend|Archean||||||||07-NOV-08
27856|Nanambu Complex|41311|6|Mentioned|p5|||||||||
27856|Nanambu Complex|41397|6|Mentioned|p6|||||||||
27856|Nanambu Complex|41406|6|Mentioned|Map legend|Archean||||||||07-NOV-08
27856|Nanambu Complex|41407|6|Mentioned|Map legend|Paleoproterozoic|Archean|||||||07-NOV-08
27856|Nanambu Complex|41465|5|Briefly described|p4|||||||||
27856|Nanambu Complex|41586|6|Mentioned|Map legend|||||||||
27856|Nanambu Complex|41601|5|Briefly described|p42|||||||||
27856|Nanambu Complex|41649|6|Mentioned|p66|||||||||
27856|Nanambu Complex|41663|6|Mentioned|p30|||See also Fig.2||||||
27856|Nanambu Complex|42372|5|Briefly described|p18|Archean||||||||07-NOV-08
27856|Nanambu Complex|43187|5|Briefly described|p2|||||||||
27856|Nanambu Complex|43292|5|Briefly described|Map Legend||Archean|||||||07-NOV-08
27856|Nanambu Complex|43561|6|Mentioned|p1434|||||||||
27856|Nanambu Complex|43595|5|Briefly described|p229||Paleoproterozoic|||||||07-NOV-08
27856|Nanambu Complex|43624|6|Mentioned|p8|||||||||
27856|Nanambu Complex|43832|6|Mentioned|11|||Age 2470 Ma||||||
27856|Nanambu Complex|45121|6|Mentioned|Table 3|||||||||
27856|Nanambu Complex|46639|5|Briefly described|Map legend|Paleoproterozoic|Archean|Age: 2500-1800Ma.||||||07-NOV-08
27856|Nanambu Complex|46658|6|Mentioned|Fig.4 P546|||||||||
27856|Nanambu Complex|46675|5|Briefly described|Map legend|Paleoproterozoic|Archean|Leucogranite, migmatite, gneiss, granite schist. Conformably overlain by the Kakadu Group. Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
27856|Nanambu Complex|46700|5|Briefly described|p7, Table1 p12|Proterozoic|Archean|||||||12-JUL-16
27856|Nanambu Complex|46824|6|Mentioned|p321|||||||||
27856|Nanambu Complex|46991|6|Mentioned|p245|||||||||
27856|Nanambu Complex|47047|6|Mentioned|p219|||||||||
27856|Nanambu Complex|47049|6|Mentioned|Fig.2|||||||||
27856|Nanambu Complex|49176|14|Not recorded|?|||||||||
27856|Nanambu Complex|60526|5|Briefly described|Map Legend|Proterozoic|Archean|Leucogranite, migmatite, gneiss, granite, schist.||||||07-NOV-08
27856|Nanambu Complex|60550|5|Briefly described|Map Legend|Archean|Archean|Granite, gneiss, schist.||||||07-NOV-08
27856|Nanambu Complex|60680|5|Briefly described|Map legend|Paleoproterozoic|Archean|Pale pink, coarse mica-feldspar-quartz leucogneiss.  Age: 2504Ma.||||||07-NOV-08
27856|Nanambu Complex|61056|6|Mentioned|p785|||||||||
27856|Nanambu Complex|61206|5|Briefly described|p516, p517 Fig.1|Archean|Archean|||||Overlain by the Kakadu Group.|Granitic gneisses.|
27856|Nanambu Complex|61403|5|Briefly described|Map Legend|Archean|Archean|In regional setting map legend.||||||07-NOV-08
27856|Nanambu Complex|62375|5|Briefly described|p8 Table 1, 10 Fig. 3|Archean|Archean|Granite, augen gneiss, leucogneiss, minor quartzite and schist. Age: >2470Ma. Geological Province: Pine Creek Orogen.||||||09-FEB-10
27856|Nanambu Complex|63866|5|Briefly described|p111, p117|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Crops out in the Jim Jim Fault Zone.|2470 +/- 47 Ma (Page et al, 1980)|||Intruded by the Zamu Dolerite.||
27856|Nanambu Complex|64567|5|Briefly described|p1098||Neoarchean|Pine Creek block. Includes granite with SHRIMP U/Pb zircon age of about 2.50Ga.||||||07-NOV-08
27856|Nanambu Complex|64698|4|Described|lithinterp table|Paleoproterozoic|Neoarchean|Age 2500Ma. I-type. Musc-biotite, and leucocratic muscovite, gneiss and granite; augen gneiss, minor biotite musc schist, migmatised and sheared Kakadu Group metaseds at margins; Amphibolite, meta-gabbro and meta-dolerite, interp from mag and drilling.||||||22-JUN-09
27856|Nanambu Complex|64725|5|Briefly described|p74.|Neoarchean|Neoarchean|Uranium ore occurs in dipping graphitic units.|||||Chlorite-biotite-muscovite schist, uraniferous; granitic gneiss.|
27856|Nanambu Complex|64730|5|Briefly described|p124-5 Fig. 3, p141|Paleoproterozoic|Paleoproterozoic|Age is of granite crystallisation.|2470 Ma ID-TIMS zircon (Page et al. 1980).|||||03-MAY-12
27856|Nanambu Complex|64731|6|Mentioned|p147 Fig.2|Neoarchean|Neoarchean|Nimbuwah Domain, Pine Creek Orogen.||||||12-APR-12
27856|Nanambu Complex|64956|5|Briefly described|p2 Tb. 17, p77|Paleoproterozoic|Paleoproterozoic|Overlain by Katherine River Group. Geological province: Pine Creek Orogen. Sample is biotite granite-gneiss collected from "Granite Hill".||||||07-FEB-11
27856|Nanambu Complex|65232|5|Briefly described|p23, p6 Fig. 5, p2, p24, p40, App. 2|Palaeoproterozoic|Archaean|Under Bathurst Island Formation. Presumed under Kakadu Group (unconform); under Cahill Formation (fault). Granite, gneiss, schist. Anomalous high avg U. Age: 2500 Ma on figure. See Nanambu granite p23 (of Page et al 1980).||||||09-FEB-10
27856|Nanambu Complex|65339|6|Mentioned|p4.|Neoarchean|Neoarchean|Northwestern Pine Creek Orogen. Forms part of the granitic basement.|2500 - 2400 Ma.|||||
27856|Nanambu Complex|66683|5|Briefly described|pp365-369, pp372-374, pp377-378.|Neoarchean|Neoarchean|Pine Creek Orogen. Part of felsic crystalline basement to North Australian Craton, exposed near Jabiru. Responsible for metamorphic zircon rims at c.2500 Ma in older crust (Arrarra Gneiss).|2520 +/- 3 Ma.|||Intrudes the Arrarra Gneiss.|Granite and granitic gneiss; minor amphibolite and mica schist.|11-OCT-11
27856|Nanambu Complex|67057|5|Briefly described|p454. |Archean|Archean|Nimbuwah Domain, eastern Pine Creek Orogen.|2520 +/- 3 Ma (Hollis et al. 2009a).|||||
27856|Nanambu Complex|67232|5|Briefly described|p2. |Neoarchean|Neoarchean|Nimbuwah Domain basement, Pine Creek Orogen. Previously dated at 2470 +/- 47 Ma by Page et al. (1980).|2520 Ma (Hollis et al. 2009b).|||||
27856|Nanambu Complex|67355|6|Mentioned|p4, p6 Fig.4||Paleoproterozoic|Date from granite gneiss zircon. |2500 Ma (conventional U-Pb zircon)|||||25-JAN-17
27856|Nanambu Complex|67479|6|Mentioned|p6|Archean|Archean|||||||
27856|Nanambu Complex|67564|4|Described|p iv, p8 Table 2, pp8-11. |Paleoproterozoic|Neoarchean|Contains the oldest rocks in the map area. Subdivided into Archean granite, gneissic Archean granite, and Paleoproterozoic pegmatoid leucogneiss, schist and migmatite. Surrounded by Paleoproterozoic metasedimentary rocks of the Pine Creek Orogen. Near Mount Basedow, a leucogneiss grades into meta-arkose of the Mount Basedow Gneiss, suggesting some leucogneiss units are metamorphic products of sedimentary rocks.|2470 Ma.|||Is overlain unconformably by Kakadu Group.|Pale pink, coarse-grained mica-feldspar-quartz leucogneiss; foliated granite.|
27856|Nanambu Complex|67779|5|Briefly described|p6 Fig.5, p7, p16, p41, p66, p117.|Archean|Archean|Nimbuwah Domain, Pine Creek Orogen. Characterised by distinct gravity lows. Source of sediment for Mount Basedow Gneiss. Correlated with Kukalak Gneiss.|2520 +/- 3 Ma (Carson et al. 2010).|||Is intruded by Mudginberri Phonolite.||
27856|Nanambu Complex|67873|6|Mentioned|p43, p57|||Also appears as Nanambu complex (p57).||||||
27856|Nanambu Complex|68697|5|Briefly described|vi, p2, p34-36, p46|Neoarchean|Neoarchean|Nimbuwah Domain, Pine Creek Orogen. This is a more precise age than the 2470 +47/-40 Ma of Page et al. (1980). Magmatic crystallisation age, which is consistent with emplacement of Kukalak Gneiss; they may form part of the same regional felsic magmatic event, along with the Rum Jungle Complex.|2520 +/- 3 Ma.||||Includes quartzo-feldspathic layered biotite orthogneiss.|
27856|Nanambu Complex|68998|5|Briefly described|p33|Neoarchean|Neoarchean|Pine Creek Orogen.||||||
27856|Nanambu Complex|69003|6|Mentioned|p2|||||||||
27856|Nanambu Complex|69419|5|Briefly described|p4:1-2, 5-8|Archean|Archean|Needham (1984, 1988). Nimbuwah Domain, Pine Creek Orogen. Occurs as three elongated to oval-shaped domes: Magela, Jim Jim and Mummarlary masses. Magmatic crystallisation age from a porphyritic granitic gneiss. Other age determinations are discussed in the context of subsequent metamorphism at c.1865 Ma. Geochemistry briefly described. U-rich granite and gneiss are the likely ultimate source for the uranium orebodies of the Orogen.|2520 +/- 3 Ma (Hollis et al., 2009).||||Massive, foliated, white to light grey, medium- to coarse-grained granite; strongly foliated granite and augen orthogneiss.|12-JUL-16
27856|Nanambu Complex|69420|5|Briefly described|p5:4, 6, 8, 16, 23, 38, 64-69, 71,75,85|Neoarchean|Neoarchean|See also 100, 111, 115. Part of the basement to the Nimbuwah Domain of the Pine Creek Orogen, W of Jabiru. SHRIMP zircon emplacement age.|2520 +/- 3 Ma (Hollis et al., 2009).|||Is overlain by, and faulted against, Cahill Formation.||12-JUL-16
27856|Nanambu Complex|69537|6|Mentioned|p6|Archean|Archean|Pine Creek Orogen.|c.2520 Ma.|||||
27856|Nanambu Complex|69554|6|Mentioned|p139|||Pine Creek Orogen.|c.2520 Ma (Hollis et al.,2009).|||||
27856|Nanambu Complex|69577|6|Mentioned|p112|Paleoproterozoic|Paleoproterozoic|||||||
27856|Nanambu Complex|69917|5|Briefly described|p26-29, 42|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Nimbuwah Domain. U/Pb LA-ICPMS zircon dating, Hf, O analytical data. Sample from BMR Kapalga 19, 23.5-24.1 m. Age interpreted as minimum magmatic crystallisation. Other sample ambiguous.|2467+/-13 Ma||||K-feldspar phenocrystic hornblende granite; quartzo-feldspathic gneiss.|
27856|Nanambu Complex|71256|6|Mentioned|p18|Neoarchean|Neoarchean||~2520 Ma|||||
27856|Nanambu Complex|71349|5|Briefly described|p736-737|Archean|Archean|Pine Creek Orogen.|2520 Ma.|||||
27856|Nanambu Complex|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Age determination by U-Pb zircon LA-ICPMS.|2467+/-13 Ma (crystallisation).||||K-feldspar phenocrystic hornblende granite; quartzo-feldspathic layered biotite orthogneiss with feldspar augen; biotite granitic gneiss; gneiss (metamorphosed Zamu Dolerite?).|
27856|Nanambu Complex|71632|5|Briefly described|Map legend.|Archean|Archean|Basement to McArthur Basin.||||||05-MAR-20
27856|Nanambu Complex|72527|6|Mentioned|p192.|Archean|Archean||2670-2640 Ma||Includes Arrarra and Njibinibinj Gneiss|||
27856|Nanambu Complex|73083|6|Mentioned|p6, p16|Archean|Archean|Archean, but reworked in the Paleoproterozoic.||||Overlain by Masson Formation.||
72291|Naningbura Dolomite|62505|4|Described|p3, 4|Early Ordovician|Late Cambrian|Of the Goulburn Group. Overlies: Jigaimara Formation. Underlies: Milingimbie Formation. Thickness: 1128m.||||||29-SEP-16
72291|Naningbura Dolomite|69297|5|Briefly described|p283, p285|Lower Ordovician|Middle Cambrian|Arafura Basin. Deposited in a shallow marine shelf environment. ||Goulburn Group||Overlies the Jigaimara Formation. Overlain by the Milingimbi Formation.|Dolomite.|
72291|Naningbura Dolomite|69437|5|Briefly described|p22:10|Early Ordovician|Furongian|Arafura Basin.||||Overlies Jigaimara Formation. Is overlain by Milingimbi Formation.||12-JUL-16
72291|Naningbura Dolomite|69451|3|Fully described|p35:3-4, 6-8; 35:13 Fig.35.9|Ordovician|Cambrian|Originally named the Naningbura Formation (Nicoll et al., 1966), but not defined and only briefly described. Subsequently renamed Naningbura Dolomite by Nicoll (2006), who established a type section in Arafura-1 and gave a more detailed description. Arafura Basin (offshore). Shallow-marine deposits. 1128m thick in the type section. Furongian to early Tremadocian age from conodonts for the top of the unit; the base may be Middle Cambrian.||Goulburn Group.||Conformably overlies Jigaimara Formation. Is overlain conformably by Milingimbi Formation.|A thick dolostone succession with silty dolostone intervals; conodont fauna near top.|12-JUL-16
72291|Naningbura Dolomite|69673|6|Mentioned|p197|||||||||
72291|Naningbura Dolomite|70098|5|Briefly described|p19 Fig.5|Furongian|Furongian|See also Naningbura Formation in this paper.||Goulburn Group||Overlies Jigaimara Formation. Is overlain by Milingimbi Formation.||
41156|Nanny Goat Volcanics|23809|6|Mentioned|p7, p3 Fig. 1|||Abbreviation of Nanny Goat Creek Volcanics?  Or superseded by that name?  Referred to as Crusade Dacite in text, an informal name relating to the Crusade prospect of Otter Exploration, where the sample was taken.  Age: 1816+/-7Ma, 1821+/-5Ma.||||||22-NOV-04
41156|Nanny Goat Volcanics|50315|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Winnecke Group.  Age: <1830Ma.||||||07-NOV-08
41156|Nanny Goat Volcanics|50374|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mount Winnecke Group||||||07-NOV-08
41156|Nanny Goat Volcanics|50376|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Mount Winnecke Group. Sandstone, basalt, rhyolite lava, ignimbrite.  Age: <1830 Ma.||||||07-NOV-08
41156|Nanny Goat Volcanics|60676|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Mount Winnecke Group.||||||07-NOV-08
41156|Nanny Goat Volcanics|61861|3|Fully described|p20-22, 23,24, 4,14,19, Figs.31-35,Map 1|Paleoproterozoic|Paleoproterozoic|Includes the volcanic component of Nanny Goat Creek beds and Nongra beds. A period of wider extension acompanied by felsic volcanism. Predominantly subaerial. Arenites resemble those in Birrindudu and Mount Winnecke Groups. Hosts gold deposits.|1816 +/- 7 Ma (Smith, 2000a).|||Is probably overlain by Gardiner Sandstone. Is unconformably overlain by Supplejack Downs Sandstone, Birrindudu Group.|Extrusive volcanic rocks: quartz-feldspar ignimbrite, feldspar ignimbrite, flow-banded autoclastic rhyolite lava, massive purple basalt; minor siliciclastic sediments: volcanogenic sandstone interbedded with lithic quartz arenite, and quartz arenite|
41156|Nanny Goat Volcanics|62580|4|Described|p47, p51, p66|Paleoproterozoic|Paleoproterozoic|Of Winnecke Suite. Here with Mount Winnecke Gp due to petrographic, chemical and temporal similarities.Several distinct volc.components, incl: fine-gr., foliated, amygdaloidal basalt and basaltic andesite and sub-ophitic textured dolerite.Age: 1816+/- 7Ma||||||07-FEB-11
41156|Nanny Goat Volcanics|63261|3|Fully described|p9 Fig. 5, p12-13|Paleoproterozoic|Paleoproterozoic|Of Ware Group. Incorporate former Nanny Goat Creek beds of Blake et al (1975). Age:1816+/-7,1821+/-5Ma (SHRIMP U-Pb, Smith 2001).Overlie Mt Winnecke Fm.Volcanic rocks include quartz-rich ignimbrite, feldspar-rich ignimbrite, rhyolite, basalt+sandstone.||||||07-FEB-11
41156|Nanny Goat Volcanics|64662|5|Briefly described|p29 Fig. 2, p30 Fig. 3|Orosirian|Orosirian|Of the Ware Group. Age:1825-1815Ma. Geological Province: Tanami region. See also Nanny Goat Volcanic Complex.||||||07-FEB-11
41156|Nanny Goat Volcanics|64675|5|Briefly described|p13, p24, Fig.37, Map 1|Paleoproterozoic|Paleoproterozoic|Extrusive felsic volcanics. Misspelt as Nanny goat Volcanics in Fig.2. See also informal Nanny Goat volcanics.||||||19-MAR-14
41156|Nanny Goat Volcanics|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1820 Ma.|Unit in Ware Group.||||
41156|Nanny Goat Volcanics|64730|5|Briefly described|p142, Fig.11|Paleoproterozoic|Paleoproterozoic|Tanami region.|Extrusion ages: 1816 +/- 7 Ma, 1821+/- 5 Ma.|?Of Ware Group.||||03-MAY-12
41156|Nanny Goat Volcanics|64733|6|Mentioned|p170 Fig.2|Orosirian|Orosirian||~1820 Ma.|Of Ware Group.||Overlies Mount Winnecke Formation and overlain by Wilson and Century Formations.||20-APR-12
41156|Nanny Goat Volcanics|65323|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Mount Winnecke Group; includes 5 unnamed units; sandstone, basalt, rhyolite lava, rhyolitic ignimbrites; units range from non- to moderate-highly magnetic;||||||02-FEB-10
41156|Nanny Goat Volcanics|65324|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65326|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||02-FEB-10
41156|Nanny Goat Volcanics|65327|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65328|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65349|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65350|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65351|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65352|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; includes 5 unnamed units; of the Mount Winnecke Group||||||
41156|Nanny Goat Volcanics|65353|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; includes 5 unnamed units; of the Mount Winnecke Group||||||
41156|Nanny Goat Volcanics|65354|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; of the Mount Winnecke Group; includes 5 unnamed units||||||
41156|Nanny Goat Volcanics|65355|6|Mentioned|Map legend|Orosirian|Orosirian|Not shown on map; includes 5 unnamed units; of the Mount Winnecke Group||||||
41156|Nanny Goat Volcanics|65356|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Mount Winnecke Group; includes 5 unnamed units: sandstone; basalt; rhyolite lava; rhyolitic feldspar-quartz ignimbrite and rhyolitic quartz-feldspar ignimbrite. Units range from non- to moderate-highly magnetic||||||
41156|Nanny Goat Volcanics|65359|6|Mentioned|p1|Orosirian|Orosirian|Tanami Region. In Ware Group. U/Pb SHRIMP zircon ages : 1816 +/- 7 Ma (Smith, 2001); 1821 +/- 5 Ma (Claoue-Long et al, 2001).||||||
41156|Nanny Goat Volcanics|66129|6|Mentioned|p214 Fig.1|Orosirian|Orosirian|1820 Ma. Unit in Ware Group.||||||
41156|Nanny Goat Volcanics|67168|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Mount Winnecke Group.||Intrudes and unconformably overlies Killi Killi Formation (Tanami Group). Is unconformably overlain by  Birrindudu Group, Antrim Plateau Volcanics.|Rhyolitic quartz and feldspar ignimbrite, rhyolite lava, basalt.|13-JAN-12
41156|Nanny Goat Volcanics|67824|6|Mentioned|p385 Fig.2|Orosirian|Orosirian|Appears as Nanny Goat Volcanic.|~ 1820 Ma|Unit in Ware Group.||||
41156|Nanny Goat Volcanics|67826|6|Mentioned|p402|Orosirian|Orosirian|Appears as Nanny Goat Volcanic in p401 Fig.2. Ages from 207Pb/206Pb zircon.|1816 +/- 7 and 1821 +/- 5 Ma (Smith 2001)|Of the Ware Group.||||
41156|Nanny Goat Volcanics|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1820 Ma|Ware Group||||
41156|Nanny Goat Volcanics|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
41156|Nanny Goat Volcanics|69426|4|Described|p11:3-5, 7-8, 11, 30|Orosirian|Orosirian|Hendrickx et al. (2000). Formerly the Nanny Goat Creek Beds (Blake et al., 1975) which included a sandstone now assigned to the Wilson Formation. Predominantly subaerial. Hosts gold mineralisation in the Crusade and Tregony prospects. Ages are of ignimbrite (Claoue-Long et al., 2001) and dacite (Smith, 2001) respectively.|1821 +/- 5 Ma and 1816 +/- 7 Ma.|Ware Group.||Unconformably overlies the Tanami Group. Is overlain unconformably by the Birrindudu Group.|Consists generally of five mappable units: quartz-rich feldspar ignimbrite, feldspar-rich ignimbrite, rhyolitic lava, basalt, and volcaniclastic sandstone.|12-JUL-16
41156|Nanny Goat Volcanics|70291|4|Described|p178,180|Orosirian|Orosirian|Geological province: Tanami. Misspelt/shown as Nanny Goat Volcanic on p178. Age inferred from associated volcanic units.|ca. 1820 Ma|Unit of Ware Group.|||Volcanogenic sandstone interbedded mainly with felsic volcanic rocks|
41156|Nanny Goat Volcanics|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. ||Unit of Ware Group||||
41156|Nanny Goat Volcanics|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1800+/-13 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic volcanics.|
41156|Nanny Goat Volcanics|73089|6|Mentioned|p8|||||Ware Group||||
27091|Napperby Gneiss|7821|6|Mentioned|p46|||Exhibits high-grade foliation associated with the Strangways Orogeny.||||||
27091|Napperby Gneiss|7837|6|Mentioned|p100|||Reynolds Range. Contains thin zircon overgrowths dated at 1600 Ma.||||||
27091|Napperby Gneiss|7838|5|Briefly described|p69-70, 72, 75-76, 81-82, 84-85, 87|||Northern Arunta Inlier. The granitic protolith was emplaced during the first stage of the second tectonic cycle affecting this region. A large, composite sheet-like body. A leucogranite in the unit, dated 1775 +/- 12 Ma, which cuts previous folds, gives an age range for this second cycle of only 10 m.y. Zircon analyses tabulated and discussed.|1780 +/- 10 Ma (protolith age).|||Intruded (and contains xenoliths of) Reynolds Range Group.|Well-foliated migmatitic quartzo-feldspathic gneiss, grading in places to augen gneiss. Contains deformed and pegmatitic dykes. In part, consists of pods, dykes and veinlets of an equigranular leucocratic granite.|
27091|Napperby Gneiss|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Granitic gneiss.||||||20-NOV-06
27091|Napperby Gneiss|22733|6|Mentioned|p308||Proterozoic|||||||
27091|Napperby Gneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|In the Arunta Block. Age: 1800 - 1500 Ma.||||||20-NOV-06
27091|Napperby Gneiss|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||20-NOV-06
27091|Napperby Gneiss|23361|6|Mentioned|13 Fig.2|||||||||
27091|Napperby Gneiss|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1780+/-10Ma.||||||20-NOV-06
27091|Napperby Gneiss|23733|5|Briefly described|p34 Fig.20|||Age: 1780Ma.||||||
27091|Napperby Gneiss|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
27091|Napperby Gneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27091|Napperby Gneiss|39888|6|Mentioned|Fig.8|||||||||
27091|Napperby Gneiss|42146|5|Briefly described|p652|||||||||
27091|Napperby Gneiss|42217|6|Mentioned|p417|||||||||
27091|Napperby Gneiss|42326|5|Briefly described|Table 2 P11|||||||||
27091|Napperby Gneiss|42401|6|Mentioned|p644|||||||||
27091|Napperby Gneiss|43749|6|Mentioned|p21|||||||||
27091|Napperby Gneiss|44114|5|Briefly described|p325, 340|||Reynolds Range, Arunta Inlier. Underwent partial melting at ~1650 Ma.|1760 Ma (protolith intrusion).|||||
27091|Napperby Gneiss|48992|1|Redefined|p40|Mesoproterozoic|Mesoproterozoic|||||||
27091|Napperby Gneiss|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite. Age: 1775 +/- 12Ma (Shrimp).||||||07-NOV-08
27091|Napperby Gneiss|61309|6|Mentioned|p13 Fig. 2|||||||||
27091|Napperby Gneiss|62595|5|Briefly described|p19.|Statherian|Statherian|Granite gneisses correlated with this unit intrude the Lander Rock beds.|1778 +/- 8 Ma (SHRIMP:Collins and Williams 1995).|||||
27091|Napperby Gneiss|64722|5|Briefly described|Fig. 2 p3-6, p11|Statherian|Statherian||1780 Ma.|||Intrudes Reynolds Range Group.||11-APR-12
27091|Napperby Gneiss|65338|5|Briefly described|p21.|Statherian|Statherian||1780 +/- 10 Ma (Smith 2000, 2001).|||Intrudes Reynolds Range Group.||
27091|Napperby Gneiss|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
27091|Napperby Gneiss|65343|5|Briefly described|p3 Fig.4, p4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
27091|Napperby Gneiss|67127|6|Mentioned|p98|||Correlated with granites which host the Nolans Bore deposit in mineralised fluorapatite veins.|1778 +/- 8 Ma|||||
27091|Napperby Gneiss|67430|6|Mentioned|p10||||1778 +/- 8 Ma (SHRIMP: Worden et al., 2008).|||||
27091|Napperby Gneiss|68998|5|Briefly described|p14|||Arunta Region. Younger overprinting events are dated at 1659 +/- 6 Ma and 1587 +/- 6 Ma (Collins and Williams, 1995).|1780 +/- 10 Ma; 1775 +/- 12 Ma.|||Is intruded by the  Ngalurbindi Orthogneiss.|Has considerable heterogeneity.|
27091|Napperby Gneiss|69226|5|Briefly described|p239, p240 Tb.1, p243, p247, p255-256|Statherian|Statherian|Reynolds-Anmatjira Ranges region. Associated with the c.1780-1770 Ma Strangways Orogeny. Had a granitic precursor. Crustal heat production discussed. Also dated at 1773 +/- 19 Ma (Hand et al., 1995).|1788 +/- 8 Ma (Collins and Williams, 1995).|||Intrudes Reynolds Range Group.|Voluminous sheet-like granites; metamorphosed.|
27091|Napperby Gneiss|69228|5|Briefly described|p359 Fig.1, p361, p364-365, p369-370|Paleoproterozoic|Paleoproterozoic|See also p372 Fig.11, p373, p375. Reynolds Range, Arunta Inlier. Role as source of fluids during metamorphism discussed in detail.|1.78 Ga.|||Intrudes and is overlain by Reynolds Range Group.|Metagranite.|
27091|Napperby Gneiss|69427|4|Described|p12:3, 25-26, 30, 32, 44, 60, 63|Statherian|Statherian|Crops out along the entire length of the Yalyirimbi Range and SE Reynolds Range, Aileron Province. SHRIMP U-Pb age (others mentioned). Metamorphic zircon rims aged 1587 +/- 6 Ma reflect the Chewings Orogeny. Associated with the Nolans Bore REE-P-U-Th deposit. Potential source for surficial or sandstone-hosted U deposits.|1780 +/- 10 Ma (Collins and Williams, 1995).|||Intrudes Lander Rock, Pine Hill Formations, Aileron Metamorphics, Wickstead Creek beds, Mount Dunkin and Mount Freeling Schists.|Gneissic granite: medium-grained, strongly foliated to gneissic grey biotite(-muscovite) granitic gneiss; locally (to the E) changes into a grey, discontinuously layered migmatitic gneiss with extensive evidence for partial melting. S-type.|12-JUL-16
27091|Napperby Gneiss|70376|5|Briefly described|p833,p833 fig 2, p834|Paleoproterozoic|Paleoproterozoic|Protolith was voluminous S-type granites.|1778 Ma +/- 8 Ma|||Intrudes Reynolds Range Group.||
27091|Napperby Gneiss|71348|6|Mentioned|p201|Statherian|Statherian|Geological province: Aileron Province, Arunta Region.||||||
27091|Napperby Gneiss|71350|5|Briefly described|p7|Statherian|Statherian|Aileron Province.|1780 +/- 10 Ma (SHRIMP Collins and Williams 1995)|||Intrudes the Mount Thomas Quartzite.||
27091|Napperby Gneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both ages are for crystallisation (U-Pb zircon SHRIMP). Metamorphosed at 1659 [sic] +/- 6 Ma (also U-Pb zircon SHRIMP).|1778+/-8 Ma and 1587+/-6 Ma.||||Well-foliated, migmatitic quartzo-feldspathic orthogneiss.|
27091|Napperby Gneiss|71858|5|Briefly described|p2|||Aileron Province.||||||
27091|Napperby Gneiss|72380|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Represents evidence for felsic and mafic magmatism c. 1690-1660 Ma (eg Scrimgeour 2013) in the Aileron Province, based on SHRIMP U-Pb zircon dating that returned younger zircon populations at 1656+\-6 Ma (Collins and Williams 1995), which may be related to a major magmatic/metamorphic episode in the southern Aileron and Warumpi provinces and possibly associated hydrothermal activity (eg Black and Shaw 1992, Collins and Williams 1995).|c. 1780 Ma|||||
27091|Napperby Gneiss|73399|6|Mentioned|p2, p8, p12, App.E|||[Metamorphic?] age of 1659 +/- 6 Ma reported by Collins and Williams (1995). May have undergone a single, long-lived (190 Myr) metamorphic event.|||||Granulite facies gneiss formed from an S-type granite protolith.|
27091|Napperby Gneiss|74204|5|Briefly described|p2|Statherian|Statherian|Emplaced during the Yambah Event.|1790-1770 Ma||||Large granite body.|
30862|Napperby Suite|24047|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Also referred to as Napperby HHP Suite (see Fig. 6, p7).  Age: 1770Ma.  Geological Province: Arunta province.||||||07-NOV-08
30862|Napperby Suite|24197|5|Briefly described|p26, p57|Paleoproterozoic|Paleoproterozoic|Example of the Cullen Association. Includes the Napperby Gneiss, Possum Creek Charnockite, Boothby and Ngalurbindi Orthogneisses, Wangala Granite, Uldirra Porphyry and the Yakalibadgi Microgranite. Age: 1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
30862|Napperby Suite|50369|5|Briefly described|p1.1, 1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Age: 1770-1780Ma. Geological Province: Arunta Inlier. I-Type felsic granites.||||||07-NOV-08
30862|Napperby Suite|65455|6|Mentioned|p6 Fig. 3|||Within the Arunta region, on northern margin of the Ngalia Basin. Has been identified as having potential for Cu, Au, Ta, Mo and W mineralisation.||||||09-MAY-12
30862|Napperby Suite|67323|5|Briefly described|p90|||Georgina Basin. Heat production for geothermal energy briefly discussed.|||||Granite.|
30862|Napperby Suite|68150|6|Mentioned|p1|||Presented in text as the Napperby, Wuluma and Gumtree suites. Aileron Province.||||||
30862|Napperby Suite|71858|4|Described|p30|||Aileron Province. Name derived from Budd et al, 2001.|ca. 1780 Ma||Includes the Ngalurbindi Orthogneiss.|||
81882|Narbarloo Granite|73123|4|Described|piii, p1, p12-14, Fig.A4, Tb.A4|Statherian|Statherian|Aileron Province, northeastern. Geochron is an interpreted magmatic crystallisation age. New age matches previous (1791 +/- 3 Ma) for an outcrop previously mapped as Marshall Granite but reinterpreted as Narbarloo Granite. Zircon rims record interpreted metamorphism at 1728 +/- 8 Ma. Dated sample: GA sample No = 6619618, NTGS sample ID = HU15EEB1015A. Outcrops widely in the eastern Mopunga Range in the western Jinka 1:100 000 mapsheet.  Intimately associated with the Marshall Granite[?]. Hosted in the Deep Bore Domain. [Article includes outcrop, thin section and zircon descriptions].|1792 +/- 3 Ma SHRIMP U-Pb|Molyhil Suite||Intruded by dykes of the Marshall Granite.|Foliated to locally gneissic hornblende +/- biotite granite.|
81882|Narbarloo Granite|73591|4|Described|piv, p2, p11, p14, p16, p18, p29-31|||Aileron Province. Previous SHRIMP U-Pb zircon age of 1791 +/- 3 Ma was reported by Kositcin et al. (2011). Analysed for Lu-Hf isotopes yielding a juvenile signature. 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.|1791 +/- 3 Ma U-Pb SHRIMP|Molyhil Suite||Intrudes Deep Bore Metamorphics. Intruded by Marshall Granite.|Includes hornblende granite.|
25329|Narbib Granulite|39887|6|Mentioned|Fig.3|||||||||
25329|Narbib Granulite|69427|5|Briefly described|p12:9, 14-15|||Strangways Range region, Ankala Domain, Aileron Province. Separated from the Sliding Rock Metamorphics to the NE by the intrusive Oolbra Orthogneiss. Distinguished from Adla Granulite by a lack of pelitic units.||||Is intruded by Oolbra Orthogneiss.|Interlayered mafic and felsic granulite. Strongly deformed and variably retrogressed to amphibolite-facies assemblages.|12-JUL-16
37962|Narpa Group|61404|5|Briefly described|Map legend|Late Cambrian|Early Cambrian|Includes: Thorntonia Limestone, Steamboat Sandstone, Chabalowe Formation and Arrinthrunga Formation. Geological Province: southern Georgina Basin.||||||11-OCT-05
37962|Narpa Group|62658|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|||||||
37962|Narpa Group|62983|5|Briefly described|p11|Middle Cambrian|Middle Cambrian|Carbonate platform deposition. Geological Province: Georgina Basin. Written in informal format as Narpa group.||||||23-JAN-07
37962|Narpa Group|64068|2|Defined|p225 App 1, p4, p57-70, p82, p7, p ix|Late Cambrian|Middle Cambrian|New name. Includes Thorntonia, Devoncourt, Georgina, Mungerebar, Selwyn Range, Pomegranate, Currant Bush, V-Creek and Mail Change Limestones; Border Waterhole, Arthur Creek, Beetle Creek, Inca, Quita, Chabalowe, Arrinthrunga, Gowers and Age Creek Formations; O'Hara and Blazan Shales; Roaring Siltstone and Steamboat and Split Rock Sandstones.||||||18-MAR-16
37962|Narpa Group|64443|5|Briefly described|p7-9, p17-p40|||Of Georgina Basin.|||Includes Arrinthrunga Formation, Arthur Creek Formation and Thorntonia Limestone.|Correlative of Barkly Group in part.||14-MAY-14
37962|Narpa Group|65336|4|Described|Map Legend|Middle Cambrian|Middle Cambrian|Of Georgina Basin. Includes Thorntonia Limestone. Unconformably overlies Kalkarindji Volcanic Group; unconformably underlies Barkly Group.||||||
37962|Narpa Group|65337|5|Briefly described|pp63-68.|||Includes all Middle to medial Upper Cambrian units in eastern and southern Georgina Basin.|||Includes Border Waterhole Formation and Currant Bush Limestone.|||
37962|Narpa Group|65341|6|Mentioned|p5, p18.||||||Includes Chabalowe Formation.|||
37962|Narpa Group|66767|5|Briefly described|p59|Middle Cambrian|Middle Cambrian|Southern Georgina Basin.|||Thorntonia Limestone; Arthur Creek, Chabalowe, Arrinthrunga Formations.|Is overlain by Tomahawk Formation.|Marine bioclastic carbonate rocks, black shale and dolostone, quartz sandstone overlain by a thick succession of peritidal, evaporitic and stromatolitic limestone and dolostone, with minor quartz sandstone, siltstone and shale.|
37962|Narpa Group|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|||CONSTITUENTS (continued): Currant Bush, Devoncourt, Georgina,  Mail Change, Mungerebar, Pomegranate, Selwyn Range, Thorntonia, V-Creek Limestones; Split Rock, Steamboat Sandstones.|||Includes Age Creek, Beetle Creek, Border Waterhole, Inca, Kajabbi, Mount Hendry, Quita Formations; Blazan, O'Hara Shales; Roaring Siltstone. See COMMENTS  for limestone and sandstone constituents.|||
37962|Narpa Group|67870|5|Briefly described|p43|Late Cambrian|Early Cambrian|Georgina Basin.|||Thorntonia Limestone; Arthur Creek, Arrinthrunga Formations.|||
37962|Narpa Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
37962|Narpa Group|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
37962|Narpa Group|69377|5|Briefly described|map legend|Cambrian|Cambrian||||O'Hara Shale, Pomegranate Limestone, Roaring Siltstone, Thorntonia Limestone|||
37962|Narpa Group|69443|5|Briefly described|p28:3, 5, 7, 14, 16-21, 27, 32|Middle Cambrian|Middle Cambrian|Includes all Middle and early Late Cambrian rocks in the southern and eastern Georgina Basin; correlative rocks in the central and northern parts of the Basin constitute the Barkly Group. QLD constituents include Beetle Creek, Inca, Quita, Kajabbi, Gowers, Age Creek Formations; Blazan, O'Hara Shales; Devoncourt, Georgina, Mungerebar, Selwyn Range, Pomegranate, V-Creek, Mail Change Limestones; Roaring Siltstone; Split Rock Sandstone. Is correlated with Gum Ridge Formation, Anthony Lagoon Formation, Wonarah Formation, Ranken Limestone and Camooweal Dolostone (central and western Georgina Basin), and Top Springs Limestone (northern Georgina Basin). Contains a diverse fauna, particularly of trilobites.|||In NT: Chabalowe, Arrinthrunga, Arthur Creek, Border Waterhole Formations; Thorntonia, Currant Bush Limestones; Steamboat Sandstone. See Comments for QLD constituents.|Overlies Shadow Group. Gradationally overlies Colless Volcanics. Is overlain by Cockroach Group. Lateral equivalent of Wonarah Formation, Ranken Limestone and Camooweal Dolostone.||12-JUL-16
37962|Narpa Group|69591|5|Briefly described|p29, p88-90, p92, p94|Cambrian|Cambrian|Kruse and Mohammed (2005). S and E Georgina Basin. Mainly platform carbonates.|||Thorntonia, Currant Bush, V-Creek, Mail Change, Georgina, Pomegranate, Selwyn Range Limestones; Border Waterhole, Beetle Creek, Inca, Gowers, Age Creek Formations; Split Rock Sandstone; O'Hara Shale.||Peritidal dolostones, platform limestones with interbedded black shales and dark foetid limestones with interbedded black shales.|
37962|Narpa Group|69673|6|Mentioned|p111, p114 fig 92, p116||||||Includes Chabalowe Formation, Arrinthrunga Formation|||
37962|Narpa Group|70723|5|Briefly described|p22, p24-25, p30-31|Cambrian|Cambrian|Georgina Basin. Kerogen type and biomarker compositions discussed in detail.|508-504 Ma||Thorntonia, Currant Bush, Mungerebar, Georgina Limestones; Inca, Beetle Creek, Age Creek, Arthur Creek, Quita, Chabalowe, Arrinthrunga Formations; Blazan Shale; Steamboat Sandstone.|||
37962|Narpa Group|70951|6|Mentioned|p1069|Middle Cambrian|Middle Cambrian|Geological province: Georgina Basin. Includes key middle Cambrian petroleum source rocks.|||Includes Thorntonia Limestone and Arthur Creek Formation, Chabalowe Formation.|||
37962|Narpa Group|72321|5|Briefly described|Fig 2, p3|Furongian|Series 2|Elkedra Shelf/Dulcie Syncline, Toko Syncline, Burke River Structural Belt, Undilla Sub-basin, Georgina Basin. |||See Fig 2.|||
37962|Narpa Group|72414|4|Described|map sheet|Middle Cambrian|Middle Cambrian|Of Geogina Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Thorntonia Limestone, Border Waterhole Formation.|||
37962|Narpa Group|72415|4|Described|mapsheet|Early Ordovician|Cambrian|Of Geogina Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Thorntonia Limestone, Border Waterhole Formation.|||
37962|Narpa Group|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Arrinthrunga Formation, Steamboat Sandstone, Arthur Creek Formation and the Thorntonia Limestone.|Disconformably overlain by the Cockroach Group. Disconformably overlies the Shadow Group.||
37962|Narpa Group|72516|5|Briefly described|p11-12, p21, p85, p91-94, 135, 171, 176|Furongian|Furongian|Georgina Basin.|ca 825 Ma (max dep age)||Includes the Arrinthrunga Formation, Steamboat Sandstone, Arthur Creek Formation and Thorntonia Limestone.|||21-APR-22
37962|Narpa Group|72526|5|Briefly described|p6 Fig.1.2.|Cambrian|Cambrian|||||||
37962|Narpa Group|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.|||Includes O'Hara Shale, Devoncourt Limestone, Selwyn Limestone, Roaring Siltstone, Thorntonia Limestone, Shadow Group.|Overlies Shadow Group.|Siltstone; minor chert and sandstone; lateritic rubble capping. Impure limestone, calcilutite, bituminous limestone and marl and and subordinate chert with silicified shale.|
37962|Narpa Group|72684|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin. Overlies the Mitakoodi Domain. Shown as younger than the Isan Orogeny (1590-1500 Ma).|||Includes O'Hara Shale, Selwyn Range Limestone, Devoncourt Limestone, Roaring Siltstone, Thortonia Limestone.|Shown as unconformably overlying Shadow Group.|Thick-bedded, dolomitic limestone and dolomite with layers and nodules of chert and chert breccia. Siltstone and sandstone and Impure limestone, calcilutite, bituminous limestone and marl. Lateritic rubble capping.|
37962|Narpa Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|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.||||||
37962|Narpa Group|73083|6|Mentioned|p75||||||||Includes siliciclastics.|
37962|Narpa Group|73137|6|Mentioned|p6|Cambrian|Cambrian|||||||
37962|Narpa Group|73288|5|Briefly described|p697||||||Arthur Creek, Chabalowe Formations; Thorntonia Limestone.|||
37962|Narpa Group|73418|5|Briefly described|p4 Fig.3|Furongian|Cambrian Series 2|Georgina Basin, Burke River Structural Belt and Undilla Sub-basin. Also includes Gowers Formation, Currant Bush Limestone, V-Creek Limestone, Mail Change Limestone, Split Rock Sandstone, Age Creek Formation.|||Hay River Formation, Ardmore Chert, Thorntonia Limestone, Beetle Creek Formation, Inca Formation, Roaring Siltstone, Devoncourt Limestone, Selwyn Range Limestone, Pomegranate Limestone||Includes limestone, shale, siltstone, sandstone, dolomite and phosphorite/shale units.|
37962|Narpa Group|73553|6|Mentioned|p7|Cambrian|Cambrian|||||||
29528|Narwietooma Metamorphic Complex|23733|5|Briefly described|p34 Fig.20|||Age: >1880Ma.||||||
29528|Narwietooma Metamorphic Complex|23844|6|Mentioned|p30|||||||||
29528|Narwietooma Metamorphic Complex|43225|5|Briefly described|Map Legend||Paleoproterozoic|In the Arunta Block.||||||07-NOV-08
29528|Narwietooma Metamorphic Complex|43749|6|Mentioned|p45|||||||||
29528|Narwietooma Metamorphic Complex|44158|6|Mentioned|p40|||||||||
29528|Narwietooma Metamorphic Complex|50369|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Intruded by: Mount Zeil Granite, Forty Five Augen Gneiss.||||||07-NOV-08
29528|Narwietooma Metamorphic Complex|60668|6|Mentioned|p7|||||||||
29528|Narwietooma Metamorphic Complex|67565|6|Mentioned|p5 Fig.3.|||Aileron Province.||||||
29528|Narwietooma Metamorphic Complex|69427|5|Briefly described|p12:6, 8, 14, 17-18, 23, 29, 40, 44|||Warren and Shaw (1995). 50-150 km WNW of Alice Springs. The age of the metasedimentary precursors is poorly understood: no geochronology has been done. There is evidence of moderate- to high-grade metamorphism at 1780-1760 Ma (?Yambah Event); but Claoue-Long and Hoatson (2005) have dated metamorphic zircon rims at c.1725 Ma and c.1700 Ma (Strangways Event). This unit included a map unit (PLnx: unnamed Metamorphic rocks) in the northeastern HERMANNSBURG map area which has now been reassigned to the Lander Rock Formation.|||Mount Hay Granulite; Bunghara, Mount Chapple Metamorphics.|||12-JUL-16
29528|Narwietooma Metamorphic Complex|72894|6|Mentioned|piii, p19|||Of Warren and Shaw (1995). Unnamed sample of metapsammite (HE03IRS006) dated herein was originally assigned to this unit, but is now considered consistent with a Lander Rock Formation protolith.|||Mount Hay Granulite, Mount Chapple Metamorphics, Bunghara Metamorphics|||
26072|Nathan Group|14019|6|Mentioned|p14|||Possibly correlates with sedimentary units in the Victoria Basin.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|22453|6|Mentioned|p 12|||McArthur Basin||||||
26072|Nathan Group|22479|5|Briefly described|fig4, pg10|Calymmian|Calymmian|||||||
26072|Nathan Group|22538|4|Described|p710, Fig4, p718|Calymmian||Part of the Favenc package.||||||26-MAR-18
26072|Nathan Group|22600|4|Described|Map legend|Calymmian|Calymmian|||||||
26072|Nathan Group|22644|5|Briefly described|3,5|||Geol. province: McArthur Basin.||||||20-JUL-06
26072|Nathan Group|22662|5|Briefly described|22,23 fig 2|Proterozoic|Proterozoic|Geo.l province: McArthur Basin||||||20-JUL-06
26072|Nathan Group|22664|6|Mentioned|34|Paleoproterozoic|Paleoproterozoic|Geol province McArthur Basin||||||07-NOV-08
26072|Nathan Group|22716|6|Mentioned|p236|||May be equivalent to the Birrindudu Group of the Birrindudu Basin.||||||
26072|Nathan Group|22808|6|Mentioned|7 fig 4|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|22853|5|Briefly described|23|Proterozoic|Proterozoic|Overlying unit: Roper Group, underlying unit: McArthur Group.||||||20-JUL-06
26072|Nathan Group|23216|6|Mentioned|p30||Statherian|Age: < 1640 Ma.||||||
26072|Nathan Group|23362|6|Mentioned|339 Fig.2|||||||||
26072|Nathan Group|23374|5|Briefly described|Fig3p5,34,35,6,18,29||Mesoproterozoic|Correlative of Mount Rigg Group. In the McArthur Basin.||||||20-NOV-06
26072|Nathan Group|23387|6|Mentioned|p18 fig.19|||||||||
26072|Nathan Group|23393|5|Briefly described|p17 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23395|6|Mentioned|p383|||||||||
26072|Nathan Group|23396|5|Briefly described|p 407 fig.2|||||||||
26072|Nathan Group|23398|5|Briefly described|p443|||||||||
26072|Nathan Group|23405|5|Briefly described|p594|||||||||
26072|Nathan Group|23407|5|Briefly described|p626|||||||||
26072|Nathan Group|23409|5|Briefly described|p536|||In the Isa Superbasin.||||||20-NOV-06
26072|Nathan Group|23733|5|Briefly described|p32 Fig. 19|||Geological Province: MacArthur Basin.||||||
26072|Nathan Group|23776|5|Briefly described|p706|Calymmian|Statherian|Age 1615-1575 Ma.||||||20-JUL-06
26072|Nathan Group|23809|5|Briefly described|protero|Proterozoic|Proterozoic|Geological Province: McArthur Basin.  Correlates with Bullita and Wattie Groups, and Lower Wade Creek Formation of the Victoria Basin.||||||22-NOV-04
26072|Nathan Group|23867|5|Briefly described|p14|Mesoproterozoic|Paleoproterozoic|Geological  Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|23902|6|Mentioned|p1568 Fig.1|||Geological Province: McArthur Basin||||||
26072|Nathan Group|23910|4|Described|p290|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|23937|4|Described|p17, p24 Tb. 2|Calymmian|Statherian|Overlain by Phelp Sandstone; unconformably overlies the Vizard Group.  Age: 1614-1589Ma.  Type section in BAUHINIA DOWNS.  Geological Province: McArthur Basin.||||||18-APR-05
26072|Nathan Group|23963|6|Mentioned|p1238|||Geological Province: McArthur Basin.||||||10-MAR-05
26072|Nathan Group|24047|5|Briefly described|p12 Fig. 10, p11|Mesoproterozoic|Mesoproterozoic|Age: 1600-1570?Ma.  Overlies the McArthur Group.  Geological Province: McArthur Basin.||||||
26072|Nathan Group|24048|4|Described|p64|Calymmian|Calymmian|Geological Province: McArthur Basin.||||||
26072|Nathan Group|24049|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||13-OCT-05
26072|Nathan Group|24050|5|Briefly described|p7|Mesoproterozoic|Paleoproterozoic|Age: 1589+/-Ma, 1613+/-4Ma.||||||07-NOV-08
26072|Nathan Group|24122|6|Mentioned|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|24297|5|Briefly described|p1|Proterozoic|Proterozoic|Possibly correlated with Wattie and Bullita Groups. Grological Province: McArthur Basin.||||||
26072|Nathan Group|24419|5|Briefly described|p13 Fig. 5|Paleoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-NOV-08
26072|Nathan Group|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|40105|6|Mentioned|p310|||||||||
26072|Nathan Group|40109|5|Briefly described|p302|||||||||
26072|Nathan Group|40259|6|Mentioned|Table 1|||||||||
26072|Nathan Group|40691|3|Fully described|p11|||||||||
26072|Nathan Group|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26072|Nathan Group|41019|5|Briefly described|p243|||||||||
26072|Nathan Group|41268|4|Described|p284|||||||||
26072|Nathan Group|41277|5|Briefly described|p80|||||||||
26072|Nathan Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|41721|5|Briefly described|p26, p27|||Includes the Balbirini Dolomite. Geological Province: McArthur Basin.||||||01-AUG-07
26072|Nathan Group|42385|4|Described|p23|||See also Table 4 p16.||||||20-NOV-06
26072|Nathan Group|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
26072|Nathan Group|42395|6|Mentioned|Fig.26 P86|||||||||
26072|Nathan Group|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.|||Includes: Dungaminnie Formation, Balbirini Dolomite and Smythe Sandstone.|Shown in legend as adjacent to Karns Dolomite. Underlies Lower Roper Group (Roper Group) units; overlies Batten Subgroup (McArthur Group) units.||07-NOV-11
26072|Nathan Group|42639|4|Described|p35, Table 6|||||||||
26072|Nathan Group|42700|5|Briefly described|map legend|Mesozoic|Early Cretaceous|||||||
26072|Nathan Group|42739|5|Briefly described|map legend|Calymmian|Calymmian|Cyclic dolostone, dolarenite, sandstone, mudstone, evaporite casts, basic to intermediate volcanics, feldspathic sandstone, tuffite.||||||19-OCT-05
26072|Nathan Group|42812|3|Fully described|p42, Table 4|||||||||
26072|Nathan Group|42846|5|Briefly described|p503, Fig.1 p502|||Geological Province: McArthur Basin.||||||09-MAY-05
26072|Nathan Group|42935|6|Mentioned|p527|||||||||
26072|Nathan Group|43010|6|Mentioned|Table 14.|||||||||
26072|Nathan Group|43036|5|Briefly described|p55|||||||||
26072|Nathan Group|43292|5|Briefly described|Map Legend||Mesoproterozoic|||||||
26072|Nathan Group|43486|5|Briefly described|21|||||||||
26072|Nathan Group|43595|4|Described|p438||Mesoproterozoic|||||||
26072|Nathan Group|43788|6|Mentioned|p13||Proterozoic|||||||
26072|Nathan Group|44112|4|Described|p63,65|||Part of Supersequence 4||||||
26072|Nathan Group|45162|2|Defined|p136|Proterozoic|Proterozoic|Mention p45.||||||20-NOV-06
26072|Nathan Group|50225|5|Briefly described|p406 Fig. 10, p407|Mesoproterozoic|Paleoproterozoic|Geological Province: McArthur Basin.||||||07-FEB-11
26072|Nathan Group|60483|4|Described|p7 Fig. 5, p9, p32|||Incl: Kookaburra Ck and Dungaminnie Fm, Mt Birch and Smythe Ssts, and Balbirini Dolomite. Unconform.over McArthur Gp.and under Roper Gp. Thickness: 700m. Geol.Prov: McArthur Basin. Correlates with Karns Dolomite.||||||05-OCT-07
26072|Nathan Group|60558|5|Briefly described|p7, p8 Fig. 6|Proterozoic|Proterozoic|Includes four units. Dominated by shallow water to locally emergent, often evaporitic carbonates with minor associated fine-grained shallow water clastics.||||||
26072|Nathan Group|60573|5|Briefly described|Map legend|Calymmian|Statherian|Includes Walmudga, Yalwarra, Kookaburra Creek Formations and Mount Birch Sandstone.  Overlain by Phelp Sandstone. Does not outcrop in the ROPER RIVER mapsheet area.||||||20-JUL-06
26072|Nathan Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|60682|6|Mentioned|p6|||Geological Province: Macarthur Basin.||||||
26072|Nathan Group|60685|5|Briefly described|p1|||Geological Province: McArthur Basin.||||||
26072|Nathan Group|61390|5|Briefly described|Map Legend|Calymmian|Statherian|||||||
26072|Nathan Group|61403|5|Briefly described|Map Legend|Calymmian|Calymmian|Includes Balbirini Dolomite. Geol. Prov: McArthur Basin.||||||
26072|Nathan Group|63112|6|Mentioned|p1190|||Southern McArthur Basin.||||||
26072|Nathan Group|63866|5|Briefly described|p113-p114, p116-p117, p123|||Walker Fault Zone, northern and central Caledon Shelf and Urapunga Fault Zone.|<1710 Ma (unit relationships)|||Unconformably overlain by the Roper Group. Unconformably overlies the West Branch Volcanics, Mount Bonner Sandstone and the Jalma Formation. Equivalent to the Mount Rigg Group.||
26072|Nathan Group|64724|5|Briefly described|p45 Fig.5, p46, 47|Calymmian|Statherian|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
26072|Nathan Group|64784|6|Mentioned|p3 Fig.3 |||||||||
26072|Nathan Group|64815|5|Briefly described|p3, p11, p13, p15 Fig.9 |Calymmian|Statherian|See also p16-18 Figs.10-12, p17, p19. Rawlings (1999) assigned the lower part of the Nathan Group to the McArthur Group.|1613 +/- 4 Ma and 1609 +/- 3 Ma.||Includes Balbirini Dolostone, Smythe Sandstone and Dungaminnie Formation.|Generally unconformably overlies the McArthur Group.|Dolostone; basal polymict conglomerate and pebbly lithic (chert) sandstone; beds of fine sandstone and siltstone.|
26072|Nathan Group|64816|6|Mentioned|p2 Fig.1, p4  |||||||||
26072|Nathan Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Balbirini Dolomite, Kookaburra Creek Formation, Mount Birch Sandstone, Dungaminnie Formation, Smythe Sandstone.|||
26072|Nathan Group|64975|6|Mentioned|p162 Fig.6.|Mesoproterozoic|Mesoproterozoic|||||||
26072|Nathan Group|65228|4|Described|p7, p9, pp38-39, Fig.02.|Statherian|Statherian|McArthur Basin. Mixed carbonates and clastics. 1,200 m thick. Contains discontinuities.|1614-1610 Ma.||Includes Smythe Sandstone, Balbirini Dolomite and Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.||
26072|Nathan Group|65232|6|Mentioned|p5 Fig. 4|||Presented as Nathan and Mount Rigg groups on figure. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
26072|Nathan Group|65236|6|Mentioned|p4 Fig. 4|||Geological province: Beetaloo Sub-basin.||||||
26072|Nathan Group|65337|6|Mentioned|p7.||||c.1590 (Jackson et al. 2000b).|||||
26072|Nathan Group|65340|5|Briefly described|p57, p59, p10-11.|||Batten Trough. Possible partial correlation with Karns Dolomite, although characteristic pink tuffite beds of this unit have not been observed in the Karns Dolomite.|1589 +/- 3 Ma (Jackson et al. 2000b) medial Group.|||||26-MAR-18
26072|Nathan Group|65342|5|Briefly described|p8.|||McArthur Basin. Max. thickness at least 437 m.||||Is overlain by Mantungula Formation.|Dolostone, chert, dolomitic sandstone, siltstone.|
26072|Nathan Group|66843|4|Described|p23-26, p34, p37-39|||Southern McArthur Basin. Composite stratigraphic column; gamma-ray curve. Lithofacies described in great detail, organised in 9 cycles. Evolution of the Group is revised in this study.|||Includes Balbirini Dolomite, Dungaminnie Formation.|Unconformably overlies McArthur Group. Is overlain unconformably by Roper Group.|A succession of stromatolitic carbonates with minor sandstone and shale.|12-SEP-19
26072|Nathan Group|67144|5|Briefly described|Map legend.|Calymmian|Calymmian|McArthur Basin.|||Includes Balbirini Dolostone.|Overlies McArthur Group. Is overlain by Roper Group.||13-APR-12
26072|Nathan Group|67269|6|Mentioned|p20-21 Fig.19|||McArthur Basin.|||Dungaminnie Formation.|||
26072|Nathan Group|67323|5|Briefly described|Eastern Australia Time-Space Plot; p9|||NT (Jackson & Southgate 2000). Supersequences extend on to Lawn Hill Platform.|||Includes Yalwarra Volcanics and unconformity-bounded Lawn, Wide and Doom Supersequences.|||
26072|Nathan Group|67352|4|Described|v, p11,  p13 Tb.2, p51|Calymmian|Statherian|McArthur Basin. 1.6 km thick. Deposition terminated by Isan Orogeny.|1615-1575 Ma||Balbirini Dolostone, Smythe Sandstone.|Overlies McArthur Group paraconformably. Overlain by Roper Group (unconformably).|Dominated by stromatolitic and evaporitic dolostone; basal conglomerate and pebbly lithic sandstone.|
26072|Nathan Group|67564|5|Briefly described|p51.|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin. Correlative of Mount Rigg Group in Pine Creek Orogen.|1613 - 1590 Ma.|||||
26072|Nathan Group|68280|6|Mentioned|p26 fig 24|||McArthur Basin.|||Includes Dungaminnie Formation|||
26072|Nathan Group|69018|5|Briefly described|p450 Fig.1a, b|Calymmian|Statherian|Of McArthur Basin.|||Includes Balbirini Dolomite, Dungaminnie Formation.|||
26072|Nathan Group|69417|6|Mentioned|p2:5|Calymmian|Statherian|McArthur Basin.||||||12-JUL-16
26072|Nathan Group|69429|5|Briefly described|p14:3 Fig.14.4, 14:4|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Hosts quartz hematite (ironstone) lenses (the Murphys Fe prospect).|||Mount Birch Sandstone.|||12-JUL-16
26072|Nathan Group|69430|4|Described|p15:2-4, 9, 16, 19, 21-25, 27, 29-30, 61|||Jackson et al. (1987), for units overlying a regional unconformity within the upper part of the revised (Plumb and Brown, 1973) McArthur Group, but underlying the Roper Group. McArthur Basin. Fair to good conventional hydrocarbon reservoirs occur.|||Balbirini, Karns Dolostones; Mount Birch, Smythe Sandstones; Knuckey, Walmudga, Dungaminnie Formations; Yalwarra Volcanics.|Unconformably overlies Amos Formation (Batten Subgroup, McArthur Group), Bath Range Formation (Balma Group), Vizard and Tawallah Groups. Is overlain unconformably by Roper Group.|Includes a relatively thin and lenticular basal siliciclastic and often conglomeratic unit, overlain by thicker carbonate and siliciclastic rocks.|12-JUL-16
26072|Nathan Group|69591|6|Mentioned|p47|||Northern Territory. Includes the Term, Lawn, Wide and Doom Supersequences.||||||
26072|Nathan Group|69673|4|Described|vii, p3 fig 2, p15, p32, p41|Paleoproterozoic|Paleoproterozoic|Fair to good conventional reservoir properties.|||Includes Balbarini Dolostone, Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Smythe Sandstone, Dungaminnie Formation, Karns Dolostone|Unconformably overlies McArthur Group|Basal fluvial chert-clast sandstone overlain by stromatolitic and ooidal dolostone; minor siliciclastic sandstone.|
26072|Nathan Group|70822|5|Briefly described|p102 fig 1 (A), p103|Mesoproterozoic|Mesoproterozoic||1589 +/- 3 Ma.|||Overlies McArthur Group. Overlain unconformably by Phelp Sandstone (Roper Group).||
26072|Nathan Group|70897|5|Briefly described|p42-45|||Correlated with upper part of South Nicholson Group. Uppermost units deposited c.1590 Ma.|||Dungaminnie Formation, Balbirini Dolomite.|Is overlain unconformably by Roper Group.|Tightly folded and faulted carbonate-rich succession.|
26072|Nathan Group|70968|5|Briefly described|p2 Fig.3,p6-8,p10,p13,p123,p132,p138-139|Calymmian|Statherian|On detrital zircon and lithological grounds, doubt is cast on the general acceptance of equivalence of this unit with Bullita and Wattie Groups. SHRIMP U-Pb zircon age of a tuff in the upper part of the Group.|1589 +/- 3 Ma (Page et al., 2000).||Walmudga Formation.|Is overlain unconformably by Phelp or Limmen Sandstones (Roper Group).||
26072|Nathan Group|71059|5|Briefly described|p1-3, p7|Mesoproterozoic|Mesoproterozoic|McArthur Basin.||||Is overlain unconformably by Phelp Sandstone (Roper Group). Equivalent to Wattie and Bullita Groups (Birrindudu Basin).||
26072|Nathan Group|71374|5|Briefly described|iii, p1 tbl 1, p2, p6, p18, p30, p33|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.|||Includes the Smythe Sandstone, Balbirini Dolostone and Karns Dolostone.|Overlies the McArthur Group, Habgood Group and Balma Group. Equivalent to the Bullita and Wattie Groups.||
26072|Nathan Group|71488|6|Mentioned|p141 fig 1b|Mesoproterozoic|Mesoproterozoic|||||Unconformably overlain by the Roper Group.||
26072|Nathan Group|71606|5|Briefly described|p135,137-138|Calymmian|Calymmian|Walker Trough, Caledon Shelf, Bauhinia Shelf and Batten Trough; 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. Correlable to Mount Rigg Group and Karn Dolomite.||||Overlain unconformably by Roper Group. Underlain unconformably by Balma Group, Vizard Formation, Spencer Creek Group, Tawallah group and McArthur Group.||
26072|Nathan Group|71632|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|McArthur Basin.|||Includes Yalwarra Volcanics.||Cyclic coarse-grained evaporitic-stromatolitic-ooidal dolostone, sandstone, siltstone; minor conglomerate; synsedimentary basaltic sills, sandstone, mudstone (Yalwarra Volcanics).|05-MAR-20
26072|Nathan Group|71779|5|Briefly described|p5|Mesoproterozoic|Palaeoproterozoic|McArthur Basin.||||Disconformably or unconformably overlain by the Roper Group.||
26072|Nathan Group|71893|4|Described|p9, p13|Calymmian|Calymmian|McArthur Basin. SHRIMP age is derived from a tuff in this unit.|1589 +/-3 (SHRIMP, Page et al, 2000)||Includes the Walmudga Formation.|Unconformably overlain by the Phelp Sandstone and the Limmen Sandstone (Collara Subgroup) .||
26072|Nathan Group|72248|5|Briefly described|p146,148|||Of McArthur Basin.|||||Dolostone with lesser sandstone and fine-grained clastics.|
26072|Nathan Group|72373|5|Briefly described|iii,p1-2,37-28,33,36,39|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Smythe Sandstone, Balbirini Dolostone, Knuckey Formation and Mount Birch Sandstone.|Underlain by Balma Group.||
26072|Nathan Group|72377|5|Briefly described|p13|Mesoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Balbirini Dolostone.|||10-OCT-19
26072|Nathan Group|72381|5|Briefly described|p772|||Of [or under?] Beetaloo Sub-basin, McArthur Basin.||||Overlain unconformably by Cororan Formation.||03-OCT-19
26072|Nathan Group|72523|5|Briefly described|piii, p1, p1 Fig.1, p2 Fig.2, p8, p12.|Early Mesoproterozoic|Early Mesoproterozoic|Described as part of the Favenc package (Rawlings 1999).|||Includes Smythe Sandstone, Balbirini Dolostone, Dungaminnie Formation and Knuckey Formation.|Unconformably overlies Amos Formation, McArthur and Tawallah groups. Unconformably overlain by Roper Group.||
26072|Nathan Group|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin. Part of the Favenc package (Lithostratigraphic package).|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Balbirini Dolostone, Smythe Sandstone, Dungaminnie Formationh and Karns Dolostone.|Shown as overlying Vizard Group, McArthur Group and shown as unconformably underlying Roper Group.||
26072|Nathan Group|72527|6|Mentioned|p10.|Paleoproterozoic|Paleoproterozoic|Dating of this group has assisted in constraining maximum depositional ages for the South Nicholson Group.|||Includes Balbirini Dolostone.||Includes tuffs.|
26072|Nathan Group|72718|6|Mentioned|piii, p5-9|Mesoproterozoic|Mesoproterozoic|Beetaloo Sub-basin, McArthur Basin. Isa Superbasin, Favenc package. A tuff in the upper portion of the group yielded a SHRIMP U-Pb zircon age of 1589 +/- 3 Ma.|||Wakmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone.|Unconformably underlain[?] by Nagi Formation (Vizard Group). Unconformably overlain by Phelp Sandstone and[?] Mantungula Formation (both of Collara Subgroup, Roper Group).||
26072|Nathan Group|72912|5|Briefly described|p5 Fig.3, p18.|Calymmian|Statherian|This group extends across all of the  Southern McArthur Basin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Balbirini Dolostone, Smythe Sandstone and Karns Dolostone.|Unconformably underlies Roper Group and unconformably overlies Vizard and McArthur Groups.||
26072|Nathan Group|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.|||Walmudga Formation, Yalwarra Volcanics, Knuckey Formation, Mount Birch Sandstone, Dungaminnie Formation, Upper Balbirini Dolostone, Smythe Sandstone, Karns Dolostone.|Unconformably underlain(?) by Vizard Group and McArthur Group. Unconfrmably overlain by Roper Group.||
26072|Nathan Group|73242|6|Mentioned|p39|||||||Overlain by[?] Phelp Sandstone, Collara Subgroup, Roper Group.||
26072|Nathan Group|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].||||||
26072|Nathan Group|73412|4|Described|p2, 4, 6, 8, 10-11, 13, 15-19|||Southern McArthur Basin. Dry bulk density tabulated.|c.1610-1580 Ma.||Smythe Sandstone, upper Balbirini Dolostone, Dungaminnie Formation, Karns Dolostone.|Unconformably overlies McArthur and (locally) Tawallah Groups. Is overlain unconformably by Roper Group.|Siliciclastic and carbonate rocks with minor intercalated mafic volcanics.|
27520|Negri Subgroup|14019|4|Described|p21|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group.  Includes Headleys Limestone, Nelson Shale, Linnekar Limestone and Panton Formation.  Underlies the Elder Subgroup (Goose Hole Group).  Max. thickness: 530m.  Geological Province: Ord Basin.||||||25-JUL-06
27520|Negri Subgroup|22547|5|Briefly described|p30|||Of the Goose Hole Group. Overlain by Elder Subgroup.||||||14-NOV-06
27520|Negri Subgroup|23621|5|Briefly described|p36|Late Cambrian|Middle Cambrian|See also page 9 Table 1. Of Goose Hole Group. Geological Province: Ord Basin.||||||
27520|Negri Subgroup|40993|6|Mentioned|Fig.1|||||||||
27520|Negri Subgroup|41840|4|Described|p41|||Formerly Negri Group, "Negri Series"||||||
27520|Negri Subgroup|41864|4|Described|p18|||Formerly Negri Group, "Negri series"||||||
27520|Negri Subgroup|41865|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
27520|Negri Subgroup|41866|5|Briefly described|Map legend|Middle Cambrian||||||||
27520|Negri Subgroup|43299|5|Briefly described|Map Legend||Cambrian|of Goose Hole Group.||||||
27520|Negri Subgroup|43819|6|Mentioned|p31||Early Cambrian|||||||
27520|Negri Subgroup|43853|5|Briefly described|Map Legend||Ordian|||||||
27520|Negri Subgroup|43855|5|Briefly described|Map Legend||Ordian|||||||
27520|Negri Subgroup|44230|5|Briefly described|Map Legend||Middle Cambrian|||||||
27520|Negri Subgroup|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
27520|Negri Subgroup|60419|4|Described|p1, p3 Fig.2|Middle Cambrian|Middle Cambrian|Of Goose Hole Group. Conformably overlain by Elder Subgroup. Peritidal, with marine incursions. Max. thickness: 530 m. Geological Province: Ord Basin.||||||
27520|Negri Subgroup|60519|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group. Includes: Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation. Geological Province: Ord Basin.||||||03-NOV-04
27520|Negri Subgroup|60589|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Of the Goose Hole Group.  Geological Province: Ord Basin.||||||
27520|Negri Subgroup|67860|5|Briefly described|p417, p419 Tb. 4-18, p421 fig 4-86|Middle Cambrian|Middle Cambrian|160-530 m thick.||Goose Hole Group|Includes Headleys and Linnekar Limestones; Nelson Shale; Panton Formation.|Conformably overlies Antrim Plateau Volcanics. Is overlain conformably by Elder Subgroup. Equivalent to Tarrara Formation (Bonaparte Basin).|Mainly siltstone and mudstone; minor limestone, sandstone and gypsum.|
27520|Negri Subgroup|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Ord Basin||Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone||Siltstone, shale, limestone.|03-AUG-15
27520|Negri Subgroup|69165|5|Briefly described|100k_interpgeop_lut.csv|Cambrian|Cambrian|See also 100k_xsecgeop_lut.csv. ||Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone||Undivided, siltstone, shale and limestone.|
27520|Negri Subgroup|69437|5|Briefly described|p22:11|Cambrian|Cambrian|Ord Basin, Centralian B Superbasin. Sequence 1. Dominantly peritidal and lesser shallow-marine deposits.|||Headleys, Linnekar Limestones; Nelson Shale; Panton Formation.|Equivalent to Tarrara, Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Walbiri, Giles Creek Dolostones.|Fine-grained siliciclastic rocks and limestone.|12-JUL-16
27520|Negri Subgroup|69448|4|Described|p33:1-6, 8|Late Cambrian|Middle Cambrian|Ord Basin. Up to 530m thick. Fossils allow correlation with Tindall Limestone (Daly Basin), Montejinni Limestone and Hooker Creek Formation (Wiso Basin), Top Springs Limestone/Gum Ridge Formation/Thorntonia Limestone/Border Waterhole Formation (Georgina Basin).||Goose Hole Group.|Headleys, Linnekar Limestones; Nelson Shale; Panton Formation.|Disconformably overlies Antrim Plateau Volcanics. Is overlain conformably and gradationally by Elder Subgroup. Is broadly correlated with Tarrara Formation (Bonaparte Basin).|Dominantly maroon gypsiferous siltstone and mudstone, punctuated by three brief marine carbonate incursions.|12-JUL-16
27520|Negri Subgroup|69634|5|Briefly described|100k_interpgeop_lut.csv|||||Unit of Goose Hole Group.|Includes Headleys Limestone, Linnekar Limestone, Nelson Shale, Panton Formation.|||
27520|Negri Subgroup|69673|6|Mentioned|p192, p193|Cambrian|Cambrian |||Goose Hole Group|Includes Headleys Limestone, Nelson Shale, Linnekar Limestone, Panton Formation||Gypsiferous silstone and mudstone.|
27520|Negri Subgroup|70154|6|Mentioned|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-509 Ma|Goose Hole Group|Includes Panton Formation, Linnekar Limestone, Nelson Shale, Headleys Limestone|||
27520|Negri Subgroup|71146|5|Briefly described|p6|Cambrian|Cambrian|Ord Basin.||Goose Hole Group||Overlies the Antrim Plateau Volcanics. Overlain by the Elder Subgroup.|Mudstone and carbonate.|
27520|Negri Subgroup|71267|4|Described|GEOL_LUT_CSV files|||Geological province: Halls Creek Orogen. Of Ord Basin. See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.||Unit of Goose Hole Group.|Includes Headleys Limestone, Linnekar Limestone, Nelson Shale, Panton Formation.||Micritic and stromatolitic limestone and chert; siltstone, calcareous mudstone; minor feldspathic sandstone|
27520|Negri Subgroup|71800|4|Described|p25-p26|Middle Cambrian|Middle Cambrian|Ord Basin. Deposited in intertidal to shallow subtidal environments.||Goose Hole Group|Includes the Headleys Limestone, Nelson Shale, Linnekar Limestone and the Panton Formation.|Overlain by the Elder Subgroup.||
80965|Neoproterozoic-Cambrian sedimentary rocks, Amadeus Basin 80965|72034|5|Briefly described|500k_interpgeop16_lut|Cambrian|Neoproterozoic|Amadeus Basin (Phase 1). Informal, group rank.|||||Sandstone, minor siltstone and conglomerate.|
26075|Nero Siltstone|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
26075|Nero Siltstone|24122|5|Briefly described|p4 Fig.3|||Of Bullita Group.  Geological Province: Victoria Basin.||||||
26075|Nero Siltstone|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Overlies Skull Creek Formation;  unconformably overlain by Banyan Formation and Mount Gordon Sandstone. Geological Province: Victoria Basin.||||||08-AUG-05
26075|Nero Siltstone|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
26075|Nero Siltstone|28255|4|Described|p56, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of Bullita Gp. Olive-green, fissile, laminated sltst and shale; thin bedded, fine-grained sltst occur near top. Conformably overlain by Mount Gordon Sst; also overlain by Wondoan Hill Fm; underlying beds believed to be Skull Creek Fm. Max.thick: 80m.||||||20-NOV-06
26075|Nero Siltstone|30003|4|Described|p7, p12|||Of the Bullita Group. Overlies the Skull Creek Formation; conformably overlain by Mount Gordon Sandstone.  Carpentarian or Adelaidean Max. thickness: >70m.||||||19-APR-05
26075|Nero Siltstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
26075|Nero Siltstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26075|Nero Siltstone|45112|5|Briefly described|Table 10|||||||||
26075|Nero Siltstone|48943|2|Defined|p67|Proterozoic|Proterozoic|Strat. section p137. ?Adelaidean||||||20-NOV-06
26075|Nero Siltstone|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Siltstone and shale, minor quartz siltstone and quartz sandstone. Of Bullita Group. Geological Province: Victoria Basin.||||||
26075|Nero Siltstone|60685|5|Briefly described|p4 Fig. 3|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Geological Province: Victoria Basin.||||||
26075|Nero Siltstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Overlies Skull Creek Formation. Is unconformably overlain by Banyan Formation.||
26075|Nero Siltstone|69432|4|Described|p17:2, 11-12|||Sweet et al. (1974). Birrindudu Basin. 80m thick. Probably a partial lithostratigraphic correlative of part of Bynoe Formation.||Bullita Group.||Is overlain by Mount Gordon Sandstone.|A succession of siltstone and shale, and minor quartz sandstone.|12-JUL-16
26075|Nero Siltstone|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Overlies Skull Creek Formation, unconformably overlain by Banyan Formation, Mount Gordon Sandstone||
26075|Nero Siltstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Skull Creek Formation. Is overlain by Mount Gordon Sandstone.|Siltstone and shale, minor quartz siltstone and quartz sandstone.|
26075|Nero Siltstone|70968|5|Briefly described|p115|||||Bullita Group.||Is overlain unconformably by Wondoan Hill Formation.||
26075|Nero Siltstone|71302|5|Briefly described|p6||Paleoproterozoic|Of Birindudu Basin.||Unit of Bullita Group.||Equivalent to Bynoe Formation. Underlain by Skull Creek Formation.||
26075|Nero Siltstone|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Skull Creek Formation. Overlain by Banyan Formation and Weaner Sandstone unconformably[?]. Equivalent to Bynoe Formation.||
24426|Neutral Junction Formation|42504|5|Briefly described|Table 4 p73|||Name reserved July 88, Haines and Bagas.||||||18-FEB-16
24426|Neutral Junction Formation|42643|2|Defined|p53|Early Cambrian||||||||
24426|Neutral Junction Formation|42644|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Silty sandstone and siltstone, micaceous, glauconitic, grey and green, weathers red-brown; minor silty glauconitic limestone. Geological Province: Georgina Basin.||||||15-NOV-05
24426|Neutral Junction Formation|60122|5|Briefly described|p14|Early Cambrian|Early Cambrian|In ALCOOTA  and BARROW CREEK.  Geological Province: Georgina Basin.||||||20-NOV-06
24426|Neutral Junction Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group. Silty sandstone and siltstone: micaceous, glauconitic; minor silty glauconitic limestone; abundant ichnofossils. Geological Province: southern Georgina Basin.||||||20-NOV-06
24426|Neutral Junction Formation|62984|5|Briefly described|p14|Early Cambrian|Early Cambrian|Sharply overlies Octy Fm, the boundary being interpreted as a marine flooding surface over a minor hiatus. Fine calcareous sandstone and mudstone. Contains abundant and diverse early Cambrian trace fossils in lower section. Geol. Prov: Georgina Basin.||||||23-JAN-07
24426|Neutral Junction Formation|64068|3|Fully described|p56, p19, 54, 55|Early Cambrian|Early Cambrian|Glauconite and micaceous components apparently contribute to high levels of radioelements. Mapped as Grant Bluff Formation by Smith and Milligan (1964). Correlations: Upper Mount Baldwin Formation, possibly Sylvester Sandstone, Arumbera Sandstone 4 Yuendumu Sandstone 2.||Of Shadow Group.||Overlies Octy Formation probably disconformably. Disconformably overlain by Chabalowe Formation.|Red-brown silty and micaceous sandstone and siltstone, sandstone commonly calcareous and glauconitic; minor grey silty and glauconitic limestone.|04-APR-12
24426|Neutral Junction Formation|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
24426|Neutral Junction Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Overlies Octy Formation. Is overlain by Red Heart Dolostone.||12-JUL-16
24426|Neutral Junction Formation|69443|4|Described|p28:7, 14-15, 18|Early Cambrian|Early Cambrian|Haines in Haines et al. (1991). Southern Georgina Basin. A recessive unit, poorly exposed. 39m thick. Low-energy, sub-tidal marine deposits.||Shadow Group.||Overlies Octy Formation (probably disconformably). Is overlain disconformably by Chabalowe Formation. Is correlated with upper Mount Baldwin Formation and possibly Sylvester Sandstone.|Silty and micaceous sandstone and siltstone, with minor thin intervals of silty and glauconitic limestone. Sandstone is commonly calcareous and glauconitic, and is ripple cross-stratified.|12-JUL-16
24426|Neutral Junction Formation|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Red Heart Dolostone, overlies Octy Formation||
24426|Neutral Junction Formation|69673|5|Briefly described|p114 fig 92, p116, p127|||39m thick.||Shadow Group||Overlies Octy Formation, disconformably overlain by Chabalowe Formation, correlated with Mount Baldwin Formation|Sandstone and siltstone with minor intervals of limestone.|
24426|Neutral Junction Formation|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation, along with the Octy Formation and the Adam Shale..||02-JUN-21
24427|Newhaven Shale Member|37537|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mount Doreen Formation. Red shale. Geological Province: Ngalia Basin.||||||20-NOV-06
24427|Newhaven Shale Member|41429|6|Mentioned|p247|||||||||
24427|Newhaven Shale Member|43631|6|Mentioned|p25|||||||||
24427|Newhaven Shale Member|44158|4|Described|p31 Table.2|Neoproterozoic|Neoproterozoic|Of the Mount Doreen Formation.||||||20-NOV-06
24427|Newhaven Shale Member|45155|2|Defined|p30|Adelaidean|Adelaidean|||||||
24427|Newhaven Shale Member|68270|4|Described|p680,683|Ediacaran|Ediacaran|Ngalia Basin.||Unit of Mount Doreen Formation.||Underlain by Wanapi Dolomite Member.||
24427|Newhaven Shale Member|69439|4|Described|p24:2, 8|Ediacaran|Ediacaran|Ngalia Basin, Centralian A Superbasin. Supersequence 3. About 20m thick. Probably represents deepening water conditions at the end of the glacial cycle.||Mount Doreen Formation.||Conformably overlies, and locally interfingers with, Wanapi Dolostone Member. Is overlain unconformably by Djagamara Formation.|Thinly-bedded, red to purple-red shale; a few thin bands of dolomudstone occur near the base, and bands of poorly bedded, friable iron-stained sandstone, a few metres thick, are present near the top.|12-JUL-16
24427|Newhaven Shale Member|69673|5|Briefly described|p106, p107 fig 85|||20m thick.||||Overlies Wanapi Dolostone Member|Thinkly bedded shale.|
24428|Newlands Volcanics|23733|6|Mentioned|p20|Paleoproterozoic|Paleoproterozoic|See also p32 Fig. 19.  Of Wauchope Subgroup.||||||07-NOV-08
24428|Newlands Volcanics|23809|5|Briefly described|p27 Fig. 25|||Of the lower part of the Wauchope Group.  Geological Province: Davenport Province.||||||22-NOV-04
24428|Newlands Volcanics|24197|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of the Treasure Suite. Geological province: Davenport Province.||||||07-FEB-11
24428|Newlands Volcanics|39624|5|Briefly described|Table 1|||||||||
24428|Newlands Volcanics|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24428|Newlands Volcanics|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24428|Newlands Volcanics|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Porphyritic dacitic ignimbrite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24428|Newlands Volcanics|41129|4|Described|Table 1|||Mention p21.||||||20-NOV-06
24428|Newlands Volcanics|41308|5|Briefly described|Table 2|||||||||
24428|Newlands Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
24428|Newlands Volcanics|41524|4|Described|Table 1|||||||||
24428|Newlands Volcanics|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Porphyritic dacitic ignimbrite, lava, tuff; minor arenite.||||||07-NOV-08
24428|Newlands Volcanics|41970|6|Mentioned|p337|||||||||
24428|Newlands Volcanics|42643|4|Described|p12, Table 1 p7|||||||||
24428|Newlands Volcanics|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Dacitic-rhyolitic ignimbrite and lava, porphyritic; bedded tuff; minor volcaniclastic or tuffaceous arenite, siltstone, shale, ashstone, agglomerate, flow margin breccia, quartzite.||||||07-NOV-08
24428|Newlands Volcanics|43802|6|Mentioned|Table 1,p80|||||||||
24428|Newlands Volcanics|45167|3|Fully described|Table 1|||Of the Wauchope Subgroup.||||||20-NOV-06
24428|Newlands Volcanics|49033|2|Defined|p18|Proterozoic|Proterozoic|||||||
24428|Newlands Volcanics|50588|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province.  Age: 1818 +/- 10Ma (SHRIMP)||||||21-NOV-13
24428|Newlands Volcanics|60681|5|Briefly described|Map legend|Statherian|Statherian|Of the Hatches Creek Group.  Geological Province: Davenport Province.||||||11-JAN-05
24428|Newlands Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Lower Wauchope Subgroup (Hatches Creek Gp). Dacitic and rhyolitic ignimbrite, lava and tuff; minor feldspathic/lithic/volcaniclastic/tuffaceous arenite and siltstone.  Overlies Unimbra Sst and interfingers with Yeeradgi Sst. In Tennant Creek region.||||||07-NOV-08
24428|Newlands Volcanics|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup. Treasure Volcanics and Newlands Volcanics are thicker in central and wastern Davenport Province, and absent in Murchison Range area to the northwest.||Wauchope Subgroup.||||05-JAN-17
24428|Newlands Volcanics|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of lower Wauchope Subgroup (Hatches Creek Group), Davenport Province. Overlies Unimbra Sandstone; disconformably underlies Coulters Sandstone. Dacitic to rhyolitic ignimbrite, lava, tuff; minor arenite, siltstone.||||||
24428|Newlands Volcanics|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of lower Wauchope Subgroup (Hatches Creek Group),  Davenport Province. Overlies Unimbra Sandstone; disconformable under Coulters Sandstone. Inferred dacitic to rhyolitic ignimbrite, lava and tuff; minor arenite, and siltstone.||||||
24428|Newlands Volcanics|65338|5|Briefly described|p8 Table 1, pp19-20.|Paleoproterozoic|Paleoproterozoic|Non-outcropping, interpreted from geophysical data; lithology inferred from geophysical character and/or outcrop in adjacent sheet areas. Laterally equivalent to Arabulja and Strzeleckie Volcanics.||Unit in Wauchope Subgroup.|||Felsic ignimbrite, lava and tuff; minor sandstone and siltstone.|
24428|Newlands Volcanics|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup, Hatches Creek Group..||Overlies Yeeradgi Sandstone. Is overlain by Coulters Sandstone.|Porphyritic dacitic ignimbrite.|19-OCT-11
24428|Newlands Volcanics|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Hatches Creek Group.||Overlies Unimbra Sandstone.|Non-outcropping: inferred dacitic to rhyolitic ignimbrite, lava and tuff; minor feldspathic/lithic/volcanilithic/tuffaceous arenite and siltstone.|
24428|Newlands Volcanics|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Hatches Creek Group.|||No outcrop: inferred dacitic to rhyolitic ignimbrite, lava and tuff; minor feldspathic/ lithic/volcanilithic/ tuffaceous arenite, and siltstone.|
24428|Newlands Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Shown as lateral equivalent to Yeeradgi Sandstone.|Dacitic and rhyolitic ignimbrite, lava and tuff; minor feldspathic/lithic, volcaniclastic/tuffaceous arenite and siltstone.|08-DEC-14
24428|Newlands Volcanics|67352|4|Described|p10, p41, p44 fig 48|Orosirian|Orosirian|500m thick pyroclastic deposits of subaerial volcanism.||Wauchope Subgroup||Overlies (conformably) or interfingers with Yeeradgi Sandstone. Is overlain unconformably by Coulters Sandstone.|Porphyritic dacitic lava: abundant tabular sodic plagioclase phenocrysts; minor bedded tuff, ashstone, agglomerate, siltstone, shale and arenite.|
24428|Newlands Volcanics|68518|3|Fully described|p7-8 Tb.1, p12|Proterozoic|Proterozoic|Thickness: 0-2000+ m. Type section: in eastern part of Elkedra Pound; it extends from GR NS 110645 to GR NS115592. Dacitic to rhyolitic composition.||Wauchope Subgroup||Conformable on Yeeradgi Sandstone and also on Unimbra Sandstone (in SE); overlain conformably or disconformably by Coulters Sandstone and unconformably by Cambrian strata.|Generally recessive porphyritic felsic ignimbrite and lava, bedded tuff; minor feldspathic/volcaniclastic/tuffaceous arenite, siltstone, shale, mudstone, ashstone, agglomerate, flow-margin breccia, and quartzite (possible fumarolic sinter).|30-MAY-16
24428|Newlands Volcanics|69424|6|Mentioned|p9:5|Paleoproterozoic|Paleoproterozoic|Volcanic rocks are part of the Treasure Suite.||Hatches Creek Group.||||12-JUL-16
24428|Newlands Volcanics|69425|4|Described|p10:3, 10-13, 15-16, 22, 25|Statherian|Statherian|Part of the Treasure Suite. 0 - over 2000m thick. Appears as Newland Volcanics in p10:3. Intercalated sedimentary rocks interpreted as fluviatile to shallow-marine. Eruption is attributed to volcanic centre(s) in the Elkedra Dome. Localised amphibolite-facies mineral assemblages. Hosts the Trew Prospect; a tantalite-bearing quartz vein in shale. SHRIMP U-Pb igneous crystallisation age.|1818 +/- 10 Ma (OZCHRON database).|Wauchope Subgroup, lower.||Conformably overlies Unimbra, Yeeradgi Sandstones (probably interfingers with the latter). Is overlain conformably and disconformably by Coulters Sandstone. Correlated with part of Manga Mauda Member.|Dark grey, feldspar-porphyritic dacitic and rhyolitic ignimbrite and lava; minor feldspathic/lithic (volcaniclastic/tuffaceous) sandstone, quartz sandstone, siltstone, shale, mudstone, ashstone, tuff and agglomerate.|12-JUL-16
24428|Newlands Volcanics|69427|6|Mentioned|p12:13|||Davenport Province.||||Correlated with Strzeleckie Volcanics.||12-JUL-16
24428|Newlands Volcanics|69431|6|Mentioned|p16:5|||Davenport Province.||Wauchope Subgroup.||||12-JUL-16
24428|Newlands Volcanics|71592|5|Briefly described|Appendix A.|||Davenport Province, Tennant Creek Region.|1818+/-10 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyry.|
24428|Newlands Volcanics|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24428|Newlands Volcanics|72380|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||||||
24428|Newlands Volcanics|73083|6|Mentioned|p10, p19|||||||Overlain by Coulters Sandstone.||
31355|Ngadarunga Granite|7821|5|Briefly described|p45-47, 49-51, 64-65|||Mount Doreen area, Arunta Inlier. Considered transitional granulite-facies Lander Rock beds. Zircon analyses tabulated. Contains abundant inherited zircons. Provides a minimum age for the Yuendumu Tectonic Event and the Lander Rock beds.|1880 +/- 5 Ma (U-Pb zircon).|||Intrudes Lander Rock beds.|Strongly peraluminous, felsic, quartz-rich, S-type cordierite metasedimentary gneiss. Undeformed. Contains xenoliths of migmatitic gneiss (Lander Rock beds).|
31355|Ngadarunga Granite|7838|6|Mentioned|p83||||1880 +/- 5 Ma.|||S-type granite.||
31355|Ngadarunga Granite|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: ~1880Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
31355|Ngadarunga Granite|43275|5|Briefly described|Map Legend||Paleoproterozoic|Misspelt as Ngadurunga when reserved.||||||07-NOV-08
31355|Ngadarunga Granite|43697|6|Mentioned|p27|||Age: 1880 +/-5 Ma.||||||08-AUG-05
31355|Ngadarunga Granite|43749|6|Mentioned|Fig.1,p6,12||Paleoproterozoic|Age: approx 1880 Ma.||||||07-NOV-08
31355|Ngadarunga Granite|44158|4|Described|p13 Table.1|Paleoproterozoic|Paleoproterozoic|Age: 1880+/-5 Ma, U-Pb zircon date. In the Arunta Inlier. Intrudes Lander Rock beds.||||||05-MAY-10
31355|Ngadarunga Granite|50369|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Ngadarunga Suite.||||||07-NOV-08
31355|Ngadarunga Granite|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex. Xenolithic quartz-rich cordierite-garnet-biotite granite.||||||07-NOV-08
31355|Ngadarunga Granite|63866|5|Briefly described|p93|Statherian|Orosirian|Aileron Province.|1806 +/- 6 Ma||||Undeformed granite including enclaves of sedimentary rocks/|
31355|Ngadarunga Granite|64735|5|Briefly described|p216||||~1810-1800 Ma.|||Intrudes Lander Package.||30-APR-12
31355|Ngadarunga Granite|64736|3|Fully described|p220-226, p228, Figs. 1, 3-7, 9-10|Orosirian|Orosirian|In Arunta Region. Outcrops as 8x1.5km body 20km west of Yuendumu Community. Derived from partial melting of Lander Rock Formation. Gradational contact with surrounding metasediments. Age on adjacent sediments said to record the thermal event responsible for the granite.|1803 +/- 6 Ma SHRIMP U-Pb zircon age.||||Strongly peraluminous S-type; medium-grained, quartz-rich, feldspar-poor. Undeformed.|30-APR-12
31355|Ngadarunga Granite|64737|5|Briefly described|p231|Statherian|Orosirian||1803+/-6 Ma (Claoue-Long and Edgoose, 2008)|||Intrudes Lander Package.||01-MAY-12
31355|Ngadarunga Granite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Patmungala beds, younger than Lander Rock Formation. Xenolithic quartz-rich cordierite-sillimanite-garnet-biotite granite; moderate sublinear magnetic response||||||
31355|Ngadarunga Granite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Reynolds Range Group, Patmungala beds, younger than Lander Rock Formation. Xenolithic quartz-rich cordierite-sillimanite-garnet-biotite granite; moderate sublinear magnetic response||||||
31355|Ngadarunga Granite|65338|5|Briefly described|p16.|Statherian|Orosirian|S-type. Derived from melted Lander Rock Formation contemporaneous with metamorphism during the Stafford Event.|1803 +/- 5 Ma (Claoue-Long 2003).|||||
31355|Ngadarunga Granite|69427|4|Described|p12:5, 20-22, 33|Statherian|Orosirian|Young et al. (1995). Small body, 9km NNW of Mount Denison homestead, 20km W of Yuendumu [? Can't be both, unless there are two exposures]. Formed by accumulation of partial melt from low-P metamorphism of granulite-facies migmatites of Lander Rock Formation. Has affinities with some granites of the Carrington Suite. SHRIMP U-Pb zircon age of metamorphic rims in enclosing metasedimentary rock, interpreted to be the timing of partial melting that formed the Granite. A previous age determination of 1880 +/- 5 Ma (Young et al., 1995) reflects inherited zircons rather than age of intrusion.|1803 +/- 6 Ma (Claoue-Long and Edgoose, 2008).|||Intrudes Lander Rock Formation.|Strongly peraluminous, medium-grained, quartz-rich garnet- and cordierite-bearing granite. Contains numerous xenoliths of granulite-facies pelitic gneiss of Lander Rock Formation. S-type.|12-JUL-16
31355|Ngadarunga Granite|69917|5|Briefly described|p65|||northwest Arunta Region. S-type cordierite-bearing granite.||||||
31355|Ngadarunga Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1880+/-5 Ma (U-Pb zircon SHRIMP)||||Granite.|
31355|Ngadarunga Granite|72366|4|Described|iii, p7|Orosirian|Orosirian|Geological province: Aileron Province. Represents oldest phase (first of three) of felsic magmatism in the MOUNT DOREEN map sheet. Age reference: Claoue-Long and Edgoose 2008. Age is consistent with Re-Os age obtained from molybdenite dating from veins (Sample MD15MVM001) intruding into Lander Rock Formation. Previous SHRIMP U-Pb dating yielded an interpreted magmatic crystallisation age of 1880+\-5 Ma (Young et al., 1995); this result was superseded by an interpreted emplacement age of 1803+\-6 Ma (Claoue-Long and Edgoose 2008) based on reinterpretation of field relationships between the granites and metasandstones of Lander Rock Formation (e.g. evidence of contact effect between granites and metasandstones), and new detrital zircon analyses from metasandstones.|1803+\-6 Ma|||Intrudes into Lander Rock Formation.|Strongly peraluminous, garnet-bearing S-type granite.|08-JAN-20
24429|Ngalurbindi Orthogneiss|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Coarse porphyritic granitic augen gneiss, granite, metamorphically retrogressed rock, granodiorite.||||||
24429|Ngalurbindi Orthogneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|In the Arunta Block. Intrudes Napperby Gneiss.||||||20-NOV-06
24429|Ngalurbindi Orthogneiss|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||20-NOV-06
24429|Ngalurbindi Orthogneiss|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24429|Ngalurbindi Orthogneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24429|Ngalurbindi Orthogneiss|39888|6|Mentioned|Fig.8|||||||||
24429|Ngalurbindi Orthogneiss|42326|5|Briefly described|Table 2 P11|||||||||
24429|Ngalurbindi Orthogneiss|48992|2|Defined|p40|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||30-APR-10
24429|Ngalurbindi Orthogneiss|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite.||||||07-NOV-08
24429|Ngalurbindi Orthogneiss|68998|5|Briefly described|v, p1, p14-18, Appendix Tb.4|||Arunta Region. Complex dating results are discussed. Evidence of zircon resetting at 1753 +/- 3 Ma. Outcrops on the Denison mapsheet.|1775 +/- 3 Ma (igneous protolith).|||Intrudes Napperby Gneiss. Is intruded by Wangala Granite.|Coarse-grained granitic augen gneiss. Has considerable heterogeneity.|30-JUN-20
24429|Ngalurbindi Orthogneiss|69427|5|Briefly described|p12:20 Fig.12.19; 12:21, 26, 30|||Aileron Province.|||||Foliated to gneissic megacrystic granite; biotite-bearing and characterised by coarse phenocrysts of K-feldspar with locally developed rapakivi textures.|12-JUL-16
24429|Ngalurbindi Orthogneiss|70301|5|Briefly described|v, p1, p24-25|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Overgrowths on zircon cores are dated at 1753 +/- 3 Ma.|1775 +/- 3 Ma (SHRIMP U-Pb zircon).|||Enclaves occur within the Wangala Granite.|Biotite-bearing, megacrystic granitic gneiss characterised by abundant rounded K-feldspar megacrysts, typically 1-2 cm in diameter in a groundmass of medium- to coarse-grained quartz, plagioclase and biotite.|
24429|Ngalurbindi Orthogneiss|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|1775+/-3 Ma (U-Pb zircon SHRIMP)||||Gneiss.|
24429|Ngalurbindi Orthogneiss|71858|4|Described|p5-p6, p9, p24-p27, p30|Statherian|Statherian|Aileron Province. Previously granite Types 3, 5 and 6 of Stewart et al, 1980b. This unit forms an east-west trending belt in the Wangala Hills. Named for Ngalurbindi Hills and first defined by Stewart et al (1979) with detailed descriptions discussed in Stewart et al (1980a, b). The best exposures are in the vicinity at 207107mE 7536036mN. Petrographic descriptions, geochemistry analyses and results are discussed. SHRIMP age interpreted as the magmatic crystallisation age for the protolith to this gneiss. See also p32, p34, p36-p40, p63-p64.|1775 +/- 3 Ma (SHRIMP U-Pb)|Napperby Suite||Intruded by the Wangala Granite. Faulted against the Uldirra Porphyry.|Medium- to coarse-grained porphyritic biotite-bearing granite with rounded K-feldspar megacrysts, locally-developed porphyroblastic gneiss and rare allanite-bearing microgranite.|
22544|Ngilipitji Conglomerate Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
22544|Ngilipitji Conglomerate Member|24048|2|Defined|p101 App. 1|Statherian|Statherian|See also p60.  Proposer: P.W. Haines.  Age: 1621+/-21Ma.  Of the Yarrawirrie Formation.  Max. thickness: 200m.||||||20-NOV-06
22544|Ngilipitji Conglomerate Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Yarrawirrie Formation (Balma Group). Conglomerate: polymict with dominant sandstone clasts, pebble to cobble-size, friable lithic sandstone matrix. Geol. Prov: McArthur Basin.||||||20-NOV-06
22544|Ngilipitji Conglomerate Member|44112|4|Described|p55-56|||||||||
22544|Ngilipitji Conglomerate Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Yarrawirrie Formation, Balma Group. Conglomerate: polymict with dominant sandstone clasts, pebble to cobble-size, friable lithic sandstone matrix. Geol. Prov: McArthur Basin.||||||
22544|Ngilipitji Conglomerate Member|69430|4|Described|p15:21-22|Statherian|Statherian|Southern Walker Fault Zone, McArthur Basin. 0-100m thick. High-energy transgressive marginal ?marine/fluviatile sediments.||Yarrawirrie Formation.||Overlies Zamia Creek Siltstone probably conformably, and locally Conway Formation unconformably.|Polymict conglomerate with pebble- to cobble-sized, dominantly sandstone, clasts and a friable lithic sandstone matrix.|12-JUL-16
42368|Nguman Metamorphics|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Interlayered quartzofeldspathic muscovite schist and biotite muscovite schist; and, interlayered quartzite and quartz muscovite schist.  Of the Haasts Bluff Domain, Warumpi Province. In the Arunta region.||||||07-NOV-08
42368|Nguman Metamorphics|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Schist. Geological Province: Warumpi Province.||||||07-NOV-08
42368|Nguman Metamorphics|67565|5|Briefly described|p36.|||In the Mount Rennie 1:250 000 sheet. Equivalent to the Iwupataka Metamorphic Complex. Age from detrital zircons.|Max. deposition c.1630 Ma.||||Includes quartzite.|
42368|Nguman Metamorphics|68832|4|Described|p42-48|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Crystalline quartzite sampled. Maximum deposition age and younger metamorphic age.|1630+/-15 Ma, ~1590 Ma|Likely be part of Iwupataka Metamorphic Complex.||Strong similarities with the Lizard Schist and Ikuntji Metamorphics|Variably quartzose to feldspathic biotite-muscovite schist and metapsammite, with minor quartzite, mafic amphibolite and tremolite schist.|
42368|Nguman Metamorphics|69428|5|Briefly described|p13:7, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Western Haasts Bluff Domain, Warumpi Province. A succession of lower-amphibolite facies metasedimentary rocks and minor mafic rocks. Maximum depositional age. Metamorphic zircon rim age of c.1600 Ma.|1630 +/- 15 Ma (Cross et al., 2005).|Iwupataka Metamorphic Complex.||Is overlain by Heavitree Quartzite.|Biotite-muscovite schist, muscovite-quartz schist, and minor mafic amphibolite and quartzite; small outcrops of tremolite-chlorite schist.|12-JUL-16
42368|Nguman Metamorphics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, schist|
42368|Nguman Metamorphics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1630+/-15 Ma (MDA: U-Pb zircon SHRIMP)||||Psammite.|
42368|Nguman Metamorphics|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Haasts Bluff Domain.|||||Interlayered quartzofeldspathic muscovite schist and biotite muscovite schist locally intruded by muscovite bearing pegmatite dykes; tremolite chlorite schist with local massive chlorite; interlayered quartzite and quartz muscovite schist.|09-SEP-19
22550|Nicker beds|7821|5|Briefly described|p45-48, 55, 58-59, 63-66|||Mount Doreen area, Arunta Inlier. Volcanism predates Strangways Orogeny; tightly folded during the Wabudali Tectonic Phase. Zircon analyses tabulated.|1772 +/- 5 Ma.|||Is faulted against Lander Rock beds.|Arenaceous sediments (sandstone, siltstone), local felsic volcanics and volcaniclastic rocks.|
22550|Nicker beds|23733|5|Briefly described|p34 Fig.20|||Age: 1722Ma.||||||
22550|Nicker beds|23809|5|Briefly described|p45|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Province.||||||07-NOV-08
22550|Nicker beds|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
22550|Nicker beds|43631|3|Fully described|p8,9||Paleoproterozoic|||||||07-NOV-08
22550|Nicker beds|43697|6|Mentioned|p27|||Age: 1772+/-5.||||||20-NOV-06
22550|Nicker beds|43749|6|Mentioned|Fig.1,p6||Paleoproterozoic|Age: approx 1770 Ma.||||||07-NOV-08
22550|Nicker beds|44114|6|Mentioned|p342||||1780 Ma.|||||
22550|Nicker beds|44158|4|Described|p12, Table.1|Paleoproterozoic|Paleoproterozoic|Age: 1772+/-6 Ma, U-Pb zircon date. Intruded by Southwark Granite Suite.||||||05-MAY-10
22550|Nicker beds|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex.  Quartzite, muscovite quartzite, quartz-muscovite-schist, metasiltstone, schistose felsic volcanic and volcaniclastic rocks.||||||07-NOV-08
22550|Nicker beds|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Muscovite quartzite, feldspathic quartz sandstone, meta siltstone, quartz muscovite schist. quartz muscovite bioitite schist.||||||07-NOV-08
22550|Nicker beds|62636|6|Mentioned|Map Legend|||Possible equivalent to low-grade metasediments/metavolcanics in Mount Theo sheet area. Solid Geology legend.||||||
22550|Nicker beds|64677|6|Mentioned|p31||||c.1770 Ma (Young et al., 1995).|||||
22550|Nicker beds|64956|5|Briefly described|p3 Tb. 1, p27|Paleoproterozoic|Paleoproterozoic|Max. intrusion age: 1805+/-16Ma. Geol.prov: Arunta region. A succession of upper greenschist to lower amphibolite facies quartzite, metapelite (phyllite and andalusite schist), feldspathic quartzite, muscovite-quartz schist and rhyolite.||||||07-FEB-11
22550|Nicker beds|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Carrington Suite, younger than Lander Rock formation, similar age to Reynolds Range Group. Quartzite, quartz-muscovite schist, metasiltstone, schistose felsic volcanic and volcaniclastic rocks; low flat magnetic response||||||
22550|Nicker beds|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Carrington Suite, younger than Lander Rock formation, similar age to Reynolds Range Group. Quartzite, quartz-muscovite schist, metasiltstone, schistose felsic volcanic and volcaniclastic rocks; low flat magnetic response||||||
22550|Nicker beds|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Shown as equivalent age to Reynolds Range Group, older than Carrington Suite granites, younger than Lander Rock Formation. Muscovite quartzite, sandstone, meta-siltstone, schists and weakly schistose fine-grained felsic volcanics with feldspar laths, minor amphibolite||||||27-SEP-11
22550|Nicker beds|67565|6|Mentioned|p5 Fig.3.|||Aileron Province.||||||
22550|Nicker beds|69427|5|Briefly described|p12:3, 8, 13, 33|Statherian|statherian|Aileron Province. SHRIMP U-Pb zircon age of rhyolite. Detrital zircons give a maximum depositional age of 1809 +/- 11 Ma (Worden et al., 2008).|1772 +/- 5 Ma (Young et al., 1995).||||A succession of quartzite, phyllite, andalusite schist, feldspathic quartzite, muscovite-quartz schist, and rhyolite (flow or high-level sill).|12-JUL-16
22550|Nicker beds|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||||Muscovite quartzite, feldspathic quartz sandstone, meta siltstone, quartz-muscovite(-biotite +/- andalusite) schist; lesser weakly schistose fine-grained felsic volcanic rocks with feldspar laths, minor amphibolite.|
22550|Nicker beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||schist, quartzite|
41446|Nilyanjurrung Syenite|50586|6|Mentioned|p6.4|||||||||
41446|Nilyanjurrung Syenite|63866|5|Briefly described|p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Numeric age likely contains inherited analyses.|1859 +/- 17 Ma (Page, OZCHRON)|David Suite||||
25343|Nimbuwah Complex|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite granite, granodiorite.||||||07-NOV-08
25343|Nimbuwah Complex|9691|5|Briefly described|Map Legend|||Foliated heterogeneous to homogeneous granitoid rocks.||||||
25343|Nimbuwah Complex|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Foliated heterogeneous to homogeneous granitoid rocks.||||||02-JUN-05
25343|Nimbuwah Complex|9733|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Diatextite, metadextite, Lit-par-lit gneiss, banded gneiss, garnet biotite schist; minor hornblende, quartzite. Muscovite biotite schist and banded gneiss.||||||20-NOV-06
25343|Nimbuwah Complex|22479|5|Briefly described|fig1p2,fig4p10|Orosirian|Orosirian|||||||
25343|Nimbuwah Complex|22600|6|Mentioned|Map legend|||||||||
25343|Nimbuwah Complex|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|23374|4|Described|p5,7,9,11,19,20,26-31,35,36,44,14||Orosirian|Deformation age 1870-1850Ma. In the Pine Creek Inlier.||||||20-NOV-06
25343|Nimbuwah Complex|23714|5|Briefly described|p37|Orosirian|Orosirian|Age: 1886+/-5 Ma (U-Pb zircon).||||||
25343|Nimbuwah Complex|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Foliated granite, granodiorite, metasediments.  Age: 1870Ma.  Geological Province: Pine Creek Orogen.  See also p90.||||||07-NOV-08
25343|Nimbuwah Complex|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
25343|Nimbuwah Complex|24197|5|Briefly described|p22, p103|Paleoproterozoic|Paleoproterozoic|Of the Nimbuwah Suite. Emplaced at ~1860Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
25343|Nimbuwah Complex|29423|6|Mentioned|p304|||||||||
25343|Nimbuwah Complex|30142|6|Mentioned|p13|||||||||
25343|Nimbuwah Complex|30559|6|Mentioned|p282|||||||||
25343|Nimbuwah Complex|30863|6|Mentioned|p50|||||||||
25343|Nimbuwah Complex|31347|6|Mentioned|p135|||||||||
25343|Nimbuwah Complex|31410|6|Mentioned|Fig.1|||Overlain by Marligur Member||||||
25343|Nimbuwah Complex|31833|6|Mentioned|Table 2|||||||||
25343|Nimbuwah Complex|31834|6|Mentioned|Table 2|||||||||
25343|Nimbuwah Complex|32397|5|Briefly described|p397|||||||||
25343|Nimbuwah Complex|32659|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|32660|5|Briefly described|Table 2|||||||||
25343|Nimbuwah Complex|32959|6|Mentioned|p3|||||||||
25343|Nimbuwah Complex|33084|6|Mentioned|p5|||||||||
25343|Nimbuwah Complex|33085|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|33093|6|Mentioned|Fig.1|||||||||
25343|Nimbuwah Complex|33186|4|Described|p289|||||||||
25343|Nimbuwah Complex|35140|6|Mentioned|p313|||||||||
25343|Nimbuwah Complex|35165|6|Mentioned|p1427|||||||||
25343|Nimbuwah Complex|35465|6|Mentioned|p54|||Stratigraphy||||||
25343|Nimbuwah Complex|35495|6|Mentioned|p344|||Also P349||||||
25343|Nimbuwah Complex|35950|6|Mentioned|p302|||||||||
25343|Nimbuwah Complex|36085|6|Mentioned|p502|||||||||
25343|Nimbuwah Complex|36473|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|37462|4|Described|Table 4.II|||||||||
25343|Nimbuwah Complex|37579|5|Briefly described|Regional setting map legend|Paleoproterozoic|Paleoproterozoic|Migmatite, granite, granodiorite.||||||07-NOV-08
25343|Nimbuwah Complex|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|38239|6|Mentioned|Fig.2|||||||||
25343|Nimbuwah Complex|38351|6|Mentioned|p10|||See also P17||||||
25343|Nimbuwah Complex|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|38900|6|Mentioned|p66|||||||||
25343|Nimbuwah Complex|39048|6|Mentioned|p824|||||||||
25343|Nimbuwah Complex|39069|6|Mentioned|Fig.4|||||||||
25343|Nimbuwah Complex|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|39571|6|Mentioned|p130|||||||||
25343|Nimbuwah Complex|39620|6|Mentioned|p9|||||||||
25343|Nimbuwah Complex|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite, granite, granodiorite.||||||07-NOV-08
25343|Nimbuwah Complex|40104|6|Mentioned|p334|||||||||
25343|Nimbuwah Complex|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite, granite, granodiorite.||||||07-NOV-08
25343|Nimbuwah Complex|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Migmatite, granite, granodiorite.||||||07-NOV-08
25343|Nimbuwah Complex|40243|6|Mentioned|Fig.1|||||||||
25343|Nimbuwah Complex|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|41125|6|Mentioned|p15|||||||||
25343|Nimbuwah Complex|41146|6|Mentioned|p858|||||||||
25343|Nimbuwah Complex|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25343|Nimbuwah Complex|41305|5|Briefly described|Fig.4|||||||||
25343|Nimbuwah Complex|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25343|Nimbuwah Complex|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
25343|Nimbuwah Complex|41465|5|Briefly described|p8|||||||||
25343|Nimbuwah Complex|41586|6|Mentioned|Map legend|||||||||
25343|Nimbuwah Complex|41601|6|Mentioned|p42|||||||||
25343|Nimbuwah Complex|41649|6|Mentioned|p66|||||||||
25343|Nimbuwah Complex|42597|5|Briefly described|Map Legend|Paleoproterozoic|Archean|||||||07-NOV-08
25343|Nimbuwah Complex|43010|2|Defined|p56||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
25343|Nimbuwah Complex|43187|5|Briefly described|p2|||||||||
25343|Nimbuwah Complex|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
25343|Nimbuwah Complex|43624|6|Mentioned|p8|||||||||
25343|Nimbuwah Complex|43832|6|Mentioned|11|||Age 1870 Ma||||||
25343|Nimbuwah Complex|44112|6|Mentioned|p13|||||||||
25343|Nimbuwah Complex|44338|14|Not recorded|p.6-8,opp.6|||Gneissic granites. (C53-14).||||||
25343|Nimbuwah Complex|44339|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
25343|Nimbuwah Complex|45022|3|Fully described|p.129||Precambrian|To be refined and formalized by R S Needham. On many pages.||||||20-NOV-06
25343|Nimbuwah Complex|45121|6|Mentioned|Fig.2|||||||||
25343|Nimbuwah Complex|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: ~1870Ma. Heterogeneous granitic and granodioritic migmatite: massive to foliated fine- to coarse-grained biotite granite, dumortierite-tourmaline granite: weakly foliated to massive coarse or porphyroblastic granitoid tonalite, garnetiferous in places||||||25-FEB-16
25343|Nimbuwah Complex|46658|5|Briefly described|p555|||||||||
25343|Nimbuwah Complex|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Migmatite, granite, granodiorite. Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
25343|Nimbuwah Complex|46700|5|Briefly described|P28, Table1 P10||Orosirian|Age of unit is 1870 Ma.||||||20-NOV-06
25343|Nimbuwah Complex|46824|6|Mentioned|Table 1|||See also P321||||||
25343|Nimbuwah Complex|47047|6|Mentioned|p222|||||||||
25343|Nimbuwah Complex|47049|5|Briefly described|Table|||Transitional and lit-par-lit gneiss zones moved to Myra Falls Metamorphics.||||||20-NOV-06
25343|Nimbuwah Complex|50586|5|Briefly described|p1.1, 2.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Nimbuwah Suite. Age: 1866 +/- 8Ma (U-Pb).||||||07-NOV-08
25343|Nimbuwah Complex|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Migmatite, granite, granodiorite.||||||
25343|Nimbuwah Complex|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Diatextite; granitoid migmatitic rocks, metatextite; granitic and granodioritic. Lit-par-lit gneiss, banded gneiss, garnet biotite schist, muscovite-biotite schist.||||||20-NOV-06
25343|Nimbuwah Complex|60571|5|Briefly described|Map legend|Orosirian|Orosirian|Medium- to coarse-grained, massive to foliated, equigranular to porphyroblastic granite. Geological Province: McArthur Basin.||||||20-NOV-06
25343|Nimbuwah Complex|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|West Arnhem Land.|||||Granitic and tonalitic migmatitic gneisses.|
25343|Nimbuwah Complex|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
25343|Nimbuwah Complex|62375|5|Briefly described|p8 Table 1, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Granitoid migmatite, granite, gneiss, schist. Age: 1865Ma. Geological Province: Pine Creek Orogen.||||||09-FEB-10
25343|Nimbuwah Complex|63866|5|Briefly described|p112, p124|Orosirian|Orosirian|Nimbuwah Domain, Pine Creek Orogen. Numeric ages are SHRIMP U-Pb zircon dates. Ages derived from Worden et al, review.|1860 +/- 5 Ma and 1864 +/- 4 Ma ||||Granitic rocks.|
25343|Nimbuwah Complex|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1860Ma. I-type. Porphyroblastic granite and granodiorite, gneissic granite; Coarse or porphyroblastic granitoid tonalite, garnetiferous in places; Granulite facies metaseds, amphibolite gneiss; Stromatic migmatite, migmatite, biotite gneiss.||||||17-JUN-09
25343|Nimbuwah Complex|64730|6|Mentioned|p126|Paleoproterozoic|Paleoproterozoic|Age of granites in the complex: 1886-1866 Ma (Page et al. 1980).||||||03-MAY-12
25343|Nimbuwah Complex|64956|5|Briefly described|p2 Tb. 5, p59|Paleoproterozoic|Paleoproterozoic|Intruded by Tin Camp Granite. Cryst. Ages: 1864+/-4Ma, 1860+/-5Ma. Geological province: Pine Creek Orogen. A complex of granitoid migmatite and tonalite interlayered with ortho-amphibolite of the Zamu Dolerite.||||||07-FEB-11
25343|Nimbuwah Complex|65232|5|Briefly described|p23, p6 Fig. 5, p42|Palaeoproterozoic|Palaeoproterozoic|Foliated granite, granodiorite, metasediments. Age: various analyses between 1850 and 1870 Ma. Uranium occurrences in gneiss adjacent to unconformable contact with Mamadawerre Sandstone.||||||09-FEB-10
25343|Nimbuwah Complex|66683|5|Briefly described|pp367-369, p376, p378.|||Voluminous syn-orogenic plutons intrude Neoarchean basement and overlying Paleoproterozoic strata in Pine Creek Orogen; thought to be responsible for amphibolite facies metamorphism.|c.1867-1862 Ma.||||Porphyritic granites and granodiorites; gneissic and migmatitic components common.|
25343|Nimbuwah Complex|67057|6|Mentioned|p454, p457. |||Part of the basement in the Nimbuwah Domain.|||||Syn-orogenic granodiorite.|
25343|Nimbuwah Complex|67232|5|Briefly described|p2. |||Thought to be the heat source for mid-amphibolite facies metamorphism of Neoarchean basement in Nimbuwah Domain, Pine Creek Orogen.|1867 - 1862 Ma.||||Granitic, granodioritic and subordinate tonalitic gneiss.|
25343|Nimbuwah Complex|67323|5|Briefly described|p29|||Pine Creek area. Emplacement age.|~1885-1865 Ma.|||||
25343|Nimbuwah Complex|67355|6|Mentioned|p1 Fig.1, p6 Fig.4.||Paleoproterozoic||1880 - 1860 Ma|||||25-JAN-17
25343|Nimbuwah Complex|67479|5|Briefly described|p2 Tb.1, p6 Fig.2, p18-21, p56, p65 Tb.6|Orosirian|Orosirian|Magmatic emplacement age. Coeval with the deposition of felsic ash-fall tuff deposits within the South Alligator Group.|1866 +/- 3 Ma|||Intrudes the Cahill Formation and Nourlangie Schist.|K-feldspar phyric granodiorite.|24-JAN-17
25343|Nimbuwah Complex|67564|5|Briefly described|p9 Fig.4, p86.|Paleoproterozoic|Paleoproterozoic|Syntectonic granitoids.|1850 Ma?|||Is intruded by David Suite.|Foliated granite, granodiorite, migmatite.|
25343|Nimbuwah Complex|67779|3|Fully described|pp2-4, p6 Fig.5, p8, pp24-28, p32.|Paleoproterozoic|Paleoproterozoic|Formerly Nimbuwah Granite (Dunn, 1962); subsequently changed to Nimbuwah Complex (Needham et al. 1973, 1974, 1975) to reflect heterogeneity and to include metasedimentary rocks; later Needham (1982c) excluded metasedimentary rocks. Arnhem Land; Nimbuwah Domain. End of sedimentation was rapidly followed by burial, I-type granitic magmatism, compressional tectonism, and mid- to high-pressure amphibolite facies metamorphism (1865-1855 Ma). A large number of coalesced plutons of varied bulk compositions emplaced over an extended period (>10 m.y.): the two oldest are 1886 Ma and 1884 Ma; the youngest is 1857 Ma. Correlated with Gunbatgari Complex, and has strong geochemical and isotopic similarities with Kalkadoon Supersuite. Geochemistry and geochronology are detailed.|1863 +/- 2 Ma (Page et al. 1980).|||Intrudes Cahill Formation, Nourlangie Schist, Arrarra and Kukalak Gneisses. Is intruded by Oenpelli Dolerite. Is overlain unconformably by Kombolgie Subgroup.|Granitic, granodioritic, dioritic and rare tonalitic plutons and gneissic equivalents: medium- to coarse-grained, massive to foliated, equigranular to porphyroblastic; minor gabbroic components.|
25343|Nimbuwah Complex|68697|5|Briefly described|vi, p2, p27-32, p39, p41, p44, p46-47|Orosirian|Orosirian|Beatrice Inlier, Nimbuwah Domain, Pine Creek Orogen. This age is from a granodioritic gneiss and is similar to two other samples from the Beatrice Inlier: 1862 +/- 3 Ma and 1857 +/- 4 Ma. The heat source of amphibolite-facies metamorphism in the Nimbuwah Domain [see references to Cahill Formation: vi, p2, p35-46] is commonly attributed to emplacement of these plutons.|1861 +/- 4 Ma.||||Includes granodioritic gneiss, metadiorite and garnet-bearing plagioclase cumulate.|
25343|Nimbuwah Complex|69383|5|Briefly described|pvii|||Arnhem Land. |ca 1867-1862 Ma||||Granodioritic.|15-JUL-15
25343|Nimbuwah Complex|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Nimbuwah Region, Pine Creek Orogen.||||Intrudes Cahill Formation.||12-JUL-16
25343|Nimbuwah Complex|69419|5|Briefly described|p4:2 Fig.4.2, 4:7|Paleoproterozoic|Paleoproterozoic|Glass et al. (2009). Part of the basement to the McArthur Basin.|||||Granites and felsic gneiss.|12-JUL-16
25343|Nimbuwah Complex|69420|4|Described|p5:2, 4-6, 17-19, 23, 25, 32-34, 38, 67|Paleoproterozoic|Paleoproterozoic|See also 85, 100, 111, 115. Formerly the Nimbuwah Suite of Wyborn et al. (1997). Nimbuwah Domain, Pine Creek Orogen. These syn-orogenic plutons were emplaced (as a series of E-W elongate lobes) during the Nimbuwah Event (formerly part of the now-abandoned Barramundi Orogeny) at c.1865 Ma. Coincident with felsic volcanism of Gerowie Tuff, Berinka Volcanics and Warrs Volcanic Member. Migmatisation has occurred immediately adjacent to these plutons. Geochemistry/petrology described in some detail. Four age determinations.|1866 +/- 8 Ma - 1860 +/- 4 Ma.|?Cosmo Supergroup.|Nimbuwah Suite.||Migmatitic, foliated, porphyritic coarse granodiorite; tonalite; quartz monzonite. Restite-dominated suite with little or no fractionation.  A-type (also described as I-type). [?]|12-JUL-16
25343|Nimbuwah Complex|69430|6|Mentioned|p15:8-9|||||||Is overlain unconformably by Mamadawerre Sandstone (Kombolgie Subgroup). Is intruded by Oenpelli Dolerite.||12-JUL-16
25343|Nimbuwah Complex|69673|6|Mentioned|p3|||||||||
25343|Nimbuwah Complex|69917|5|Briefly described|p29-39, 52, 54|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Nimbuwah Domain. U/Pb LA-ICPMS zircon dating and U/Pb SHRIMP zircon dating, Hf, O analytical data. Dating attempted on 7 samples. Some dates stated to have low priority. Other dates: 1867+/-5 Ma U/Pb LA-ICPMS magmatic crystallisation age of sample.|1884+/-5 Ma Mag.cryst.; 1866+/-3 Ma SHRIMP||||Coarse-grained garnet-bearing biotite granodioritic gneiss; Hornblende granodioritic gneiss; Hornblende granite; K-feldspar phyric granodiorite; Biotite granite; Biotite granitic gneiss.|
25343|Nimbuwah Complex|69933|5|Briefly described|v, p4|||Western Arnhem Land. A sample appears to have had an Archaean precursor dated at 2634 +/- 4 Ma (SHRIMP, this volume).|||||High-grade metasedimentary gneiss mantling a core of granite.|
25343|Nimbuwah Complex|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||1867-1860 Ma.||||Granite and granodiorite and gneissic equivalents: medium- to coarse-grained, massive to foliated, equigranular to porphyroblastic; minor dioritic to gabbroic components.|
25343|Nimbuwah Complex|71374|6|Mentioned|p14||||||||Granitoids.|
25343|Nimbuwah Complex|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Metamorphosed at 1886 +/- 5 Ma.|||||Hypersthene granite; coarse-grained garnet-biotite granodioritic gneiss; coarse-grained biotite granodiorite, weakly deformed; medium-grained biotite or hornblende granodiorite gneiss; coarse-grained feldspar-porphyritic hornblende gneiss.|
25343|Nimbuwah Complex|71606|5|Briefly described|p137|Orosirian|Orosirian|East Arnhem Shelf, McArthur Basin. Associated with 1885-1870 Ma Barramundi Orogeny.||||Overlain unconformably by Mount Rigg Group.||
25343|Nimbuwah Complex|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||05-MAR-20
25343|Nimbuwah Complex|73083|6|Mentioned|p28|||Pine Creek Orogen.|||||Includes granite.|
25343|Nimbuwah Complex|73089|5|Briefly described|p33, p36-38|Orosirian|Orosirian|Nimbuwah Domain. Coeval with intercalated felsic volcanic rocks of the Cosmo Supergroup. Includes a c. 1866 Ma granitic rock [see text for geochemical signature]. Magnesian, calc-alkaline geochemical affinities [for granitic rocks]. Possible continental arc setting? Or inherited signature from basement rocks?|1867-1857 Ma|||||
75717|Njibinjibinj Gneiss|67479|5|Briefly described|p2 Tb.1, pp37-39, p55, p56, p75 Tb.14|Neoarchean|Neoarchean|Myra Falls Inlier. Metamorphic age: 2508 +/- 8 Ma (determined from one rim).|2671 +/- 3 Ma (crystallisation age).|||Overlain by the Kudjumarndi Quartzite.|Layered leucocratic quartzo-feldspathic gneiss.|24-JAN-17
75717|Njibinjibinj Gneiss|67779|2|Defined|pp7-8, p10 Table 1, p11, p104, p116.|Neoarchean|Neoarchean|New name, after Njibinjibinj sacred site, c.37 km east of Oenpelli. Nimbuwah Domain, Pine Creek Orogen. Previously part of Myra Falls Metamorphics (Dunn, 1962). SHRIMP zircon Pb/Pb age of crystallisation, within the error margin of the subcropping Woolner Granite; metamorphosed at 2508 +/- 8 Ma: structures and geochemistry described in detail. Has deep gravity lows.|2671 +/- 3 Ma (Hollis et al. 2009c).|||Is intruded by Kukalak Gneiss.|Quartzofeldspathic biotite granodioritic gneiss; strong hematitic and chloritic alteration with secondary remobilisation of silica; moderate gneissic compositional layering with local isoclinal folds.|14-MAY-18
75717|Njibinjibinj Gneiss|68697|5|Briefly described|p46|Neoarchean|Neoarchean|Nimbuwah Domain. Similarity in age with the Woolner Granite (2674 +/- 3 Ma) and other rocks is consistent with a coherent Neoarchean crustal block across a large part of the Pine Creek Orogen.|2671 +/- 4 Ma (Carson et al., 2010).|||||
75717|Njibinjibinj Gneiss|69419|5|Briefly described|p4:2 Fig.4.2, 4:6|Neoarchean|Neoarchean|Hollis and Glass (2012). NE Myra Falls Inlier. SHRIMP U-Pb zircon magmatic crystallisation age; the oldest known exposed basement in NT.|2671 +/- 3 Ma (Hollis et al., 2009).||||Quartzofeldspathic gneiss.|12-JUL-16
75717|Njibinjibinj Gneiss|69420|6|Mentioned|p5:6, 8, 23|Archean|Archean|Part of the basement to the Nimbuwah Domain of the Pine Creek Orogen; western Arnhem Land.||||||12-JUL-16
75717|Njibinjibinj Gneiss|69917|4|Described|p16-18, 19, 20, 1|Neoarchean|Neoarchean|Pine Creek Orogen, Nimbuwah Domain. U/Pb SHRIMP zircon dating, Hf, O analytical data. |2671+/-3 Ma mag. cryst.|||Underlies Kudjumarndi Quartzite|Leucocratic quartzo-feldspathic gneiss.|
75717|Njibinjibinj Gneiss|70853|5|Briefly described|Map legend.|Neoarchean|Neoarchean||2671 Ma.||||Biotite granodioritic gneiss.|
75717|Njibinjibinj Gneiss|71256|6|Mentioned|p18|Neoarchean|Neoarchean||~2670 Ma|||||
75717|Njibinjibinj Gneiss|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen. Metamorphosed at 2508 +/- 8 Ma (U-Pb zircon SHRIMP).|2671+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Layered quartzo-feldspathic biotite gneiss.|
68735|No Mans Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Playford Sandstone. Medium to thick bedded, medium to coarse grained sandstone with granule to pebble lags; sublithic to quartz rich; strongly trough cross-bedded.||||||22-AUG-06
68735|No Mans Sandstone Member|65337|2|Defined|p9 Fig.5, p39 Table 5, pp40-42.|Mesoproterozoic|Mesoproterozoic|New name. Southwest MOUNT DRUMMOND area. 130 - 200 m of fluvial or intertidal marine deposits. The trough cross-bedded sandstone facies is very similar to the tidal platform sandstone facies in the Roper Group.|Estimate of c. 1493 Ma.|Unit in Playford Sandstone.||Overlies Top Lily Sandstone Member. Is overlain by Crow Formation.|Medium- to coarse-grained sandstone with granule to pebble lags; sublithic to quartz rich; strongly trough cross-bedded.|
68735|No Mans Sandstone Member|69434|4|Described|p19:2, 4-5|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. Type section: MITCHIEBO 53K 724230mE 7935820mN, 3km ESE of Mitchiebo Waterhole. 130-200m thick. Fluvial or intertidal marine deposits.||Playford Sandstone.||Conformably overlies Top Lily Sandstone Member. Is overlain conformably by Crow Formation.|Medium to coarse sandstone with granule to pebble lags; sublithic to quartz-rich; strongly trough cross-bedded.|12-JUL-16
68735|No Mans Sandstone Member|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Playford Sandstone||Overlies Top Lily Sandstone Member and underlies Crow Formation.||
68735|No Mans Sandstone Member|72527|3|Fully described|p8, p20-26, p27, p193, p195.|Mesoproterozoic|Mesoproterozoic|Recognised only in the Mitchiebo Region. Previously mapped as Constance Sandstone (Smith and Roberts, 1963). Thickness 130 m in type section. Up to 200 m thick further east.  Sampled at Type locality shown as 137.12523dE 18.655dS. SHRIMP date derived using 207Pb/206Pb isotopic ratios.|1615 +/- 15 Ma  maximum depositional age|Top of Playford Sandstone.||Overlies Top Lily Sandstone Member and underlies Crow Formation with sharp but conformable contacts. Shown as laterally equivalent with Bowgan Sandstone.|Mainly coarse-grained sandstone with granule to pebble lags and some finer grained intervals. Sample is white, slightly feldspathic, quartz sandstone.|
68735|No Mans Sandstone Member|72912|5|Briefly described|p5 Fig.3, p25.|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin.||Playford Sandstone||||
68735|No Mans Sandstone Member|72919|6|Mentioned|p5, p24|Mesoproterozoic|Mesoproterozoic|Basal contact is sharp and locally erosional, but essentially conformable.||Playford Sandstone, Wild Cow Subgroup, South Nicholson Group||Conformably underlain by Top Lily Sandstone Member. Overlain by Crow Formation.||
68735|No Mans Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Playford Sandstone, Wildcow Subgroup, South Nicholson Group||Underlain by Top Lily Sandstone Member. Overlain by Crow Formation.||
41951|Nolans Dam Metamorphics|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Cordierite gneiss, Quartzofeldspathic gneiss, Garnet-biotite gneiss, Sillimanite gneiss, Metamorphically retrogressed rock, Muscovite schist.||||||
41951|Nolans Dam Metamorphics|65338|6|Mentioned|p17.|||Partial lateral correlative of Lander Rock Formation.||||||
41951|Nolans Dam Metamorphics|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
41951|Nolans Dam Metamorphics|69427|5|Briefly described|p12:4, 6, 26|||Aileron Province. Locally sheared and retrogressed, particularly in the NW.|||||Pelitic and felsic gneiss; pelite units have an assemblage containing cordierite, garnet and sillimanite, with retrograde andalusite.|12-JUL-16
41951|Nolans Dam Metamorphics|70376|6|Mentioned|p833 fig 2|Paleoproterozoic|Paleoproterozoic|||||||
25346|Nome Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 15|Late Triassic|Late Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
25346|Nome Formation|7142|6|Mentioned|p350 Fig.4.|Early Jurassic|Late Triassic|Browse Basin.||||Overlies Challis Formation. Is overlain by Plover Formation.||
25346|Nome Formation|13194|4|Described|p386 Tb. 4-16|Norian|Carnian|Type Section: Jabiru 1A well (1887-2184m). Up to 500m thick deltaic deposits.||Sahul Group||Overlies Challis Formation. Coeval with Benalla Formation.|Interbedded sandstone, siltstone and shale; minor coal.|
25346|Nome Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
25346|Nome Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Early Jurassic|Late Triassic|Bonaparte Basin. Unit of Sahul Group. Overlies Challis Formation and underlies Plover Formation.||96||||28-OCT-14
25346|Nome Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Triassic|Of the Sahul Group.||||||01-MAR-10
25346|Nome Formation|23378|6|Mentioned|p180 Fig.2||Late Triassic|Of the Sahul Group.  In the Vulcan Sub-basin.||||||21-NOV-06
25346|Nome Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
25346|Nome Formation|24207|5|Briefly described|p209 Fig. 5|Late Triassic|Late Triassic|||||||01-MAR-10
25346|Nome Formation|24427|5|Briefly described|p49 Fig.2||Triassic|Geological Province: Bonaparte Basin.||||||
25346|Nome Formation|41532|2|Defined|p302|Late Triassic||||||||
25346|Nome Formation|42053|5|Briefly described|Fig.2 P29|||||||||01-MAR-10
25346|Nome Formation|42066|6|Mentioned|Fig.3 P199|||||||||
25346|Nome Formation|42442|2|Defined|p22|Norian|Carnian|Variation of Nome Formation, WA.||||||
25346|Nome Formation|43826|6|Mentioned|Fig.2,p163||Late Triassic|||||||01-MAR-10
25346|Nome Formation|60634|6|Mentioned|p1168 Fig.3. |Early Jurassic|Late Triassic|||Unit in Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation.||
25346|Nome Formation|61548|6|Mentioned|p480 Fig.3|Late Triassic|Late Triassic|Northern Bonaparte Basin.||||||
25346|Nome Formation|61550|6|Mentioned|p495 Fig.2. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Challis Formation.||
25346|Nome Formation|62837|5|Briefly described|Stratigraphic columns|Early Jurassic|Late Triassic|Of the Sahul Group.  Age: ~213-~203Ma. Geological Province:  Vulcan Sub-basin (Western Bonaparte Basin).||||||01-MAR-10
25346|Nome Formation|63358|5|Briefly described|p4 Fig. 1.3, p152++|Hettangian|Norian|||||||01-MAR-10
25346|Nome Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Late Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine, with local red beds, sediments.||||Overlies Challis Formation. Is overlain by Malita Formation.||
25346|Nome Formation|64689|5|Briefly described|p7 Fig.6|Late Triassic|Late Triassic|Rhaetian.||||Overlies Challis Formation. Is overlain unconformably by Plover Formation.||20-SEP-14
25346|Nome Formation|64693|6|Mentioned|p375|Triassic|Triassic|||||Unconformably overlies Challis Formation.||
25346|Nome Formation|64696|6|Mentioned|p127 Fig.2 |Rhaetian|Rhaetian|||||Is overlain unconformably by Plover Formation.||
25346|Nome Formation|64697|5|Briefly described|p84 Fig.2 |Late Triassic|Late Triassic|||||||
25346|Nome Formation|66124|5|Briefly described|p171 Fig.2|Norian|Rhaetian|Ashmore Platform (East). Marine; contains conodonts. Underlies Malita Formation and overlies Challis Formation.||||||
25346|Nome Formation|66187|5|Briefly described|p413 Fig.2, p414 Tb.1|Rhaetian|Norain|Sahul Group. Underlies the Plover Formation, overlies the Challis Formation. Mount Ashmore Dome. Mixed shallow marine to deltaic sandstone and claystone with minor shallow-marine limestone.||||||
25346|Nome Formation|67195|5|Briefly described|Appendix 2|||Browse Basin.|||||Includes dark grey siltstone; highly fractured (healed? Doubtful drilling induced?)|23-DEC-22
25346|Nome Formation|67200|6|Mentioned|app 2 p7||||||||Siltstone.|
25346|Nome Formation|68223|6|Mentioned|p178 Fig.3|Norian|Norian|||||||
25346|Nome Formation|69297|6|Mentioned|p305|Rhaetian|Norian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Sahul Group||Overlies the Challis Formation. Overlain by the Ashmore Volcanics and the Plover Formation.|Sandstone and mudstone.|
25346|Nome Formation|69452|5|Briefly described|p36:15|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||||12-JUL-16
25346|Nome Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||Overlies Mount Goodwin Sub-group. Is overlain by Plover Formation.||
25346|Nome Formation|70061|5|Briefly described|Regional geology; Figs.6-7, p12|Rhaetian|Norian|See also Vulcan: Fig.2, p1-2. Hydrocarbon reservoir. Shallow marine sediments.||Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation.||12-JUL-16
25346|Nome Formation|70064|5|Briefly described|Regional Fig.6;p6,p8-9. Central: Fig.2|Rhaetian|Norian|See also Northern: Fig.2; p1-2. Yampi: Fig.2. Browse Basin. Potential reservoirs in horsts and tilted fault-blocks. Hosts gas (280m gas column) in the Crux structure within the Heywood Graben.||Sahul Group.||Overlies Challis Formation. Is overlain by Plover Formation or Ashmore Volcanics.|Relatively high-energy fluvial environment; includes quartz-rich, medium- to very coarse-grained sandstone with interbedded siltstone, mudstone and minor coal.|12-JUL-16
30717|Nongra beds|22446|6|Mentioned|p19||Archean|||||||07-NOV-08
30717|Nongra beds|61861|6|Mentioned|p3 Table 1, p5, 6.|Paleoproterozoic|Paleoproterozoic|Of Blake et al (1979). Reassigned in this study to Browns Range Metamorphics and MacFarlane Peak Group.||Unit in Tanami Complex.||||03-APR-12
30717|Nongra beds|64956|6|Mentioned|p6|||Yielded volcanic rock sample informally named "Nongra volcanics". Interpreted to be part of the Ware Group. In the Tanami region.||||||07-FEB-11
30717|Nongra beds|65359|4|Described|p1-38.|||Of Blake et al. (1975). Tanami region. Volcanic rocks in this unit are now in the Ware Group; sedimentary rocks are in the Tanami Group. Amygdaloidal quartz-phyric rhyolite, probable lava flow. Interbedded fine and medium vitriclastic sandstone, waterlain in a moderate to low energy environment. Fiamme overlies lava, typical of seafloor diagenesis. SHRIMP U-Pb zircon age of 1818 +/- 5 Ma (Worden et al. in prep).||||||
73219|Nora Range Monzogranite|62580|5|Briefly described|p46|||Of the Frederick Suite. Highly magnetic intrusive - previously mapped as part of Lewis Granite. Pervasively weathered, foliated (magmatic) , coarse- to medium-grained, equigranular, biotite monzogranite. Unconformably overlain by Gardiner Sandstone.||||||07-FEB-11
23881|Nourlangie Schist|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz-mica schist, quartz schist, mica schist, commonly garnetiferous.  Intruded by Oenpelli Dolerite and Zamu Dolerite.||||||07-NOV-08
23881|Nourlangie Schist|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz schist.  Conformably overlies the Cahill Formation.||||||07-NOV-08
23881|Nourlangie Schist|9691|5|Briefly described|Map Legend|||Quartz-mica schist, quartz schist, mica schist, commonly garnetiferous; staurolite, kyanite and magnetite in places.||||||
23881|Nourlangie Schist|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz-mica schist, quartz schist, mica schist, commonly garnetiferous; staurolite, kyanite and magnetite in places.||||||02-JUN-05
23881|Nourlangie Schist|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
23881|Nourlangie Schist|22810|5|Briefly described|Table2 P4|||Equivalent of the Wildman Siltstone, South Alligator Group and Burrell Creek Formation||||||
23881|Nourlangie Schist|23216|6|Mentioned|Fig3p5||Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|23714|5|Briefly described|p6 Fig 4|Proterozoic|Proterozoic|||||||
23881|Nourlangie Schist|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Quartz-mica schist.  Geological Province: Pine Creek Orogen.  See also p6 Fig. 5.||||||07-NOV-08
23881|Nourlangie Schist|24181|5|Briefly described|p84|Paleoproterozoic|Paleoproterozoic|Overlies Cahill Formation. Geological Province: Pine Creek Inlier.||||||07-NOV-08
23881|Nourlangie Schist|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|37462|6|Mentioned|Fig.4.8|||||||||
23881|Nourlangie Schist|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz schist.||||||07-NOV-08
23881|Nourlangie Schist|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|38239|6|Mentioned|Fig.2|||||||||
23881|Nourlangie Schist|38349|4|Described|p13|||||||||
23881|Nourlangie Schist|38351|4|Described|p9|||||||||
23881|Nourlangie Schist|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|39069|5|Briefly described|Table 1|||||||||
23881|Nourlangie Schist|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz schist.||||||07-NOV-08
23881|Nourlangie Schist|40104|6|Mentioned|p337|||||||||
23881|Nourlangie Schist|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz schist.||||||07-NOV-08
23881|Nourlangie Schist|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz schist.||||||07-NOV-08
23881|Nourlangie Schist|40493|5|Briefly described|Table 1|||||||||
23881|Nourlangie Schist|40768|5|Briefly described|p392|||||||||
23881|Nourlangie Schist|40808|6|Mentioned|Fig.3|||||||||
23881|Nourlangie Schist|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23881|Nourlangie Schist|41125|6|Mentioned|Fig.6|||||||||
23881|Nourlangie Schist|41146|5|Briefly described|Fig.2|||||||||
23881|Nourlangie Schist|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23881|Nourlangie Schist|41305|6|Mentioned|Fig.3|||||||||
23881|Nourlangie Schist|41407|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
23881|Nourlangie Schist|41586|6|Mentioned|Map legend|||||||||
23881|Nourlangie Schist|42012|6|Mentioned|Fig.3 P3|||||||||
23881|Nourlangie Schist|42372|4|Described|p17|||||||||
23881|Nourlangie Schist|42927|6|Mentioned|Fig.1 P429|||||||||
23881|Nourlangie Schist|43187|5|Briefly described|p2|||||||||
23881|Nourlangie Schist|43624|6|Mentioned|Table 1,p9|Paleoproterozoic|Archean|||||||07-NOV-08
23881|Nourlangie Schist|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz mica schist, quartz schist, mica schist, commonly garnetiferous; staurolite, kyanite and magnetite in places.||||||07-NOV-08
23881|Nourlangie Schist|46658|6|Mentioned|p556|||||||||
23881|Nourlangie Schist|46675|5|Briefly described|Map legend for regional setting...|Paleoproterozoic|Paleoproterozoic|Quartz schist.  Geological Province: Pine Creek Geosyncline.||||||07-NOV-08
23881|Nourlangie Schist|46700|5|Briefly described|P21, Table1 P10||Proterozoic|||||||
23881|Nourlangie Schist|47049|5|Briefly described|Table|||Stratigraphic range extended.||||||
23881|Nourlangie Schist|50586|6|Mentioned|p5.3|||||||||21-NOV-06
23881|Nourlangie Schist|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz schist.||||||
23881|Nourlangie Schist|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Quartz mica schist, quartz schist, mica schist, commonly garnetiferous; staurolite, kyanite and magnetite in places.||||||
23881|Nourlangie Schist|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Pale brown to grey, crenulated, quartz-mica schist, mica schist and qrtz schist commonly feldspathic and garnetiferous, with staurolite and magnetite in places; interbedded metasiltstone, phyllite, slate and metagreywacke.  Geol.Prov: Pine Creek Orogen.||||||13-JAN-05
23881|Nourlangie Schist|61206|5|Briefly described|p516, p517 Fig.1|Early Proterozoic|Early Proterozoic|||||Overlies the Kakadu Group||
23881|Nourlangie Schist|62375|5|Briefly described|p8 Table 1, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Layered schist, gneiss. Geological Province: Pine Creek Orogen.||||||09-FEB-10
23881|Nourlangie Schist|63866|5|Briefly described|p112, p117|||Nimbuwah Domain, Pine Creek Orogen.||||Intruded by the Zamu Dolerite.||
23881|Nourlangie Schist|64677|5|Briefly described|v, p1, p4-5, p38-39|||Pine Creek Orogen. A conservative age: the youngest zircon was dated at 2008 +/- 16 Ma.|2024 +/- 7 Ma (maximum depositional age).||||Quartz-mica schist.|
23881|Nourlangie Schist|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-2050Ma. Max thick. 3000m. Crenulated qtz-mica schist, mica schist and qtz schist, graphite, feldspar and garnet common, staurolite and magnetite in places; interbedded; Lit-par-lit gneiss, banded gneiss, garnet-biotite schist, amphibolite.||||||07-JAN-09
23881|Nourlangie Schist|64730|6|Mentioned|p125 Fig. 3, p126|Paleoproterozoic|Paleoproterozoic|Tentatively correlated with Wildman Siltstone, Mount Partridge Group (Needham 1988).||||||03-MAY-12
23881|Nourlangie Schist|64956|4|Described|p2 Tb. 24, p92-93|Paleoproterozoic|Paleoproterozoic|Overlies Cahill Fm; transitional into Myra Falls Metamorphics; unconform. below Katherine River Gp. Intruded by Jim Jim Granite+Oenpelli Dolerite. Max.dep.age:1655+/-10Ma. In Pine Creek Orogen.Sample: garnet-biotite-sillimanite-staurolite-quartz schist||||||07-FEB-11
23881|Nourlangie Schist|65232|5|Briefly described|p23, p6 Fig. 5, p5 Fig. 4, App. 2|Palaeoproterozoic|Palaeoproterozoic|Overlies Cahill Formation. With Cahill Formation, is probable equivalent of Myra Falls Metamorphics. Quartz-mica schist and metaquartzite. Geol. Prov: Pine Creek Orogen.||||||09-FEB-10
23881|Nourlangie Schist|65339|6|Mentioned|p5 Fig.4. ||||||||Gneiss, schist, para-amphibolite.|
23881|Nourlangie Schist|66683|5|Briefly described|p368 Fig.3.|Paleoproterozoic|Paleoproterozoic|||||Overlies Cahill Formation.|Psammitic to pelitic schist; locally garnet- and/or staurolite-bearing.|
23881|Nourlangie Schist|67057|5|Briefly described|p454, p457. |||Nimbuwah Domain. Hosts unconformity-related uranium deposits, eg Nabarlek.||||Is intruded by Zamu Dolerite.|Comprises a muscovite-quartz-biotite schist interlayered with amphibolite, a footwall amphibolite that contains most of the ore at Nabarlek, and a unit of alternating psammitic schists, pelitic schists and thin quartzite and amphibolite layers.|
23881|Nourlangie Schist|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Pine Creek area.||||||
23881|Nourlangie Schist|67355|6|Mentioned|p.6.|||Kakadu Shelf.||?Cosmo Howley Supergroup||||
23881|Nourlangie Schist|67479|6|Mentioned|p6 Fig.2, p18, p56|||||||Intruded by the Nimbuwah Complex (based on drill core evidence).||
23881|Nourlangie Schist|67564|3|Fully described|p8 Table 2, pp9-13, pp18-19, p86.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Contains rocks previously mapped by Walpole (1963) as the now defunct Fisher Creek Siltstone and undifferentiated South Alligator Group. Poorly exposed. >3000m of shallow marine deposits; correlated with Wildman Siltstone. Maximum depositional age from detrital zircon is 2024 +/- 7 Ma.|2000 - 1860 Ma.|Unit in Mount Partridge Group [? or equivalnet to?].||Unconformably overlies Cahill Formation. Is intruded by David Suite and Zamu and Oenpelli Dolerites. Is overlain unconformably by the Katherine River Group.|Crenulated quartz-mica schist, mica schist and quartz schist, commonly feldspathic and garnetiferous; interbedded graphitic, sericitic or chloritic metasiltstone, phyllite, slate and feldspathic metagreywacke.|14-MAY-18
23881|Nourlangie Schist|67779|3|Fully described|p5 Fig.4(b), p6 Fig.5, p10, pp20-21, 94.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Contains rocks previously mapped (Dunn, 1962) as the Fisher Creek Siltstone, undifferentiated South Alligator Group, Mount Partridge Formation and Myra Falls Metamorphics. The previously mapped contact between Cahill Formation and Myra Falls Metamorphics in the Myra Falls Inlier (Needham et al. 1982) is now mapped as a contact between Cahill Formation and this unit. Type locality is at the base of the northern scarp of Mount Brockman. Structures, petrography and geochronology are described in detail. Max depostional age better constrained from underlying Cahill Fm. an dindrusive Nimbuwah Complex. Oldest metamorphic zircon age from underlying Cahill Fm is 1871 +/-4 Ma. See also pp92, 94.|Max Deposition 1868 +/- 58 Ma (U-Pb zircon).|Unit in Cosmo Supergroup?||Overlies Cahill Formation conformably. Encloses Namarrkon and Birraduk Amphibolites. Is intruded by Nimbuwah Complex and Oenpelli Dolerite. Is overlain unconformably by Mamadawerre Sandstone.|Fine to coarse, commonly layered, crenulated quartz-mica schist: commonly garnetiferous; locally staurolite-, kyanite-, and magnetite-bearing.|14-MAY-18
23881|Nourlangie Schist|69383|5|Briefly described|p18-22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen, Nimbuwah Domain. LA-ICPMS U-Pb geochronology analyses. Max deposition age.|2059 +/-12 Ma|||Higher metamorphic grade but ?may be correlated with Cahill Formation to the west|Laminated fine-grained chlorite-muscovite schist sampled.|
23881|Nourlangie Schist|69417|6|Mentioned|p2:4,|||Eastern Pine Creek Orogen.|c.1870 Ma.|||||12-JUL-16
23881|Nourlangie Schist|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
23881|Nourlangie Schist|69420|4|Described|p5:2,4-7, 23-25,38,66-68,85,100,111,115|Paleoproterozoic|Paleoproterozoic|Nimbuwah Domain, Pine Creek Orogen. Type locality is at the northern scarp of Mount Brockman. Has distinctly different detrital zircon provenance than Cosmo Supergroup. Up to 3000m thick. Marine deposits. Amphibolite-facies metamorphism. Previous correlation with Mount Partridge Group is not valid (different detrital zircon geochronology). Mis-spelt as Nouralangie Schist on 5:68. Probably is the unit that hosts the Nabarlek U deposit.||?Cosmo Supergroup.||Conformably and gradationally overlies Cahill Formation. Is overlain unconformably by Mamadawerre Sandstone.|A succession of crenulated quartz-mica schist, locally garnet- and/or staurolite-bearing; minor quartzite.|12-JUL-16
23881|Nourlangie Schist|69554|6|Mentioned|p139|||Pine Creek Orogen. Contains detrital zircons aged c.1920 Ma.||||||
23881|Nourlangie Schist|70719|6|Mentioned|p7|||Nimbuwah Domain, Pine Creek Orogen. There are some similarities in age spectra with Grindall Formation, Arnhem Province.||||||
23881|Nourlangie Schist|70853|5|Briefly described|Map legend.|Orosirian|Orosirian||1870 Ma.||||Quartz-mica schist: commonly garnetiferous; locally staurolite-, kyanite-, and magnetite-bearing.|
23881|Nourlangie Schist|71256|6|Mentioned|p18 Fig 1|||||||||
23881|Nourlangie Schist|71349|6|Mentioned|p737|||Pine Creek Orogen. Contains zircons aged c.3.1 Ga (significance explained).||||||
23881|Nourlangie Schist|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2059+/-12 Ma (MDA: U-Pb zircon LA-ICPMS).||||Chlorite-muscovite schist.|
23881|Nourlangie Schist|72706|6|Mentioned|p4|||Said to be equivalent to altered metapelitic rocks encountered at Narbalek (i.e. near this drillhole 19NBDD002).||||||
23881|Nourlangie Schist|73083|6|Mentioned|p5, p36|||||||||
23881|Nourlangie Schist|73089|6|Mentioned|p31-32|Orosirian|Orosirian|Pine Creek Orogen, Nimbuwah Domain. Neoarchean-dominated signatures. Possibly distal source; Gawler Craton or Dharwar Craton (India) based on Hf and O isotopes.|[c. 1870-1855 Ma]|||||
38102|Nulchara Charnockite|24301|4|Described|p8, p6 Tb. 1|Mesoproterozoic|Mesoproterozoic|Overlies Michell Nob Granite. Geological Province: Musgrave Block||||||21-NOV-06
38102|Nulchara Charnockite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Charnockite. Geological Province: Musgrave Block.||||||
38102|Nulchara Charnockite|61154|5|Briefly described|p14, p28|Mesoproterozoic|Mesoproterozoic|Felsic intrusion in NT - intrusive contact with underlying Michell Nob Granite. Rock is dark green, medium- to coarse-grained and porphyritic; igneous minerals include phenocrysts of K-feldspar with locally developed rapakivi textures....See also p13, p44||||||19-JUL-05
38102|Nulchara Charnockite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province.|1044 +/- 5 Ma (Camacho, 1997)|||||
38102|Nulchara Charnockite|67128|5|Briefly described|p13, p30|||Mulga Park area, Musgrave Ranges.|1044 +/- 10 Ma.|||Crosscuts Michell Nob Granite.|Heterogeneous, medium- to coarse-grained, blue-green to dark green charnockite with rapakivi feldspar phenocrysts up to 5cm and mafic clots of clinopyroxene, orthopyroxene and hornblende.|
38102|Nulchara Charnockite|69436|5|Briefly described|p21:11|Mesoproterozoic|Mesoproterozoic|Young et al. (2002). Musgrave Province. Emplaced during the Giles Event (1085-1040 Ma). SHRIMP U-Pb zircon age.|1044 +/- 5 Ma (Camacho, 1997).|Warakurna Supersuite.|||Dark grey-green, medium- to coarse-grained and porphyritic charnockite; phenocrysts of K-feldspar with locally-developed rapakivi texture, in a granoblastic groundmass. Secondary biotite replaces hornblende and Fe-oxides.|12-JUL-16
38102|Nulchara Charnockite|70018|5|Briefly described|p235|||Amadeus Basin. Shallow-dipping granitic sheet that overlies the Michell Nob granite. Comagmatic with Michell Nob Granite based on presence of Nulchara Charnockite xenoliths in the MNG and vice versa. Average 207Pb/206Pb age (Jaffey et al., 1971) is 1074.1+\-1.3 Ma.||||Underlain by Michell Nob Granite.||
38102|Nulchara Charnockite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1044+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Charnockite.|
36069|Nullawun Member|23404|5|Briefly described|p639 Fig.2|||Of Mainoru Formation.||||||
36069|Nullawun Member|23937|2|Defined|p89-90 App. 1|Calymmian|Calymmian|Of the Mainoru Fm (Collara Subgroup, Roper Gp).  Conformably overlain by Mountain Valley Lst Mbr; conformably overlies Wadjeli Sst Mbr and Limmen Sst.  Age: >1492+/-4Ma (Jackson et al, 1999). Max. thickness: 71.5m.  Geological Province: McArthur Basin.||||||02-NOV-04
36069|Nullawun Member|24051|5|Briefly described|Map Legend|Calymmian|Calymmian|Of Mainoru Formation (Roper Group). Geological Province: McArthur Basin.||||||23-DEC-09
36069|Nullawun Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group). Red-brown mudstone, variably structureless to brecciated, with palaeoweathering features. Does not outcrop in the Roper River mapsheet area||||||07-NOV-17
36069|Nullawun Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Mudstone: red-brown, variably structureless to brecciated, palaeoweathering features.||||||
36069|Nullawun Member|69430|4|Described|p15:26-27|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 71.5m thick. Non-marine mudstone, probably fluvial floodplain deposits; brecciated during paleosol formation. Appears as Nullawan Member on 15:30.||Mainoru Formation.||Overlies Wadjeli Sandstone Member conformably and Limmen Sandfstone apparently disconformably. Is overlain conformably by Mountain Valley Limestone Member.|Massive red-brown mudstone and mudstone breccia.|12-JUL-16
36069|Nullawun Member|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Pedogenic mudstone.||Of Mainoru Formation.||Overlies Gibb Member. Overlain by Mountain Valley Limestone Member.||
36069|Nullawun Member|70968|2|Defined|p13, p17-18, p20-21, p23-27, p131, p140|Calymmian|Calymmian|See also p143-144. Sweet in Abbott et al. (2001). Named after Nullawun Lagoon. The type section is a complete intersection in Urapunga-6 drillhole, 204.4m (base) to 132.9m, taken from 1km SE of Roper Bar Store, at 450000mE 8370400mN in URAPUNGA sheet. Very recessive unit: poorly exposed. Red beds resemble those in the underlying Mantungula Formation. 42-72m thick. Aggradational floodplain environment.||Mainoru Formation.||Overlies Wadjeli Sandstone Member conformably and Limmen Sandstone disconformably. Is overlain conformably and gradationally by Mountain Valley Limestone Member.|Red-brown and red-grey siltstone and in-situ shale-intraclast breccia; minor grey-green laminated claystone and thin beds of very fine to medium sandstone. Discontinuous intraclastic limestone near the top. Contains distinctive massive red beds.|
36069|Nullawun Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 42-72m thick. Continental fluvial floodplain deposits; brecciated during palaeosol formation.||Mainoru Formation.||Conformably overlies Wadjeli Sandstone Member, and (locally) disconformably overlies Limmen Sandstone. Is overlain conformably by Mountain Valley Limestone Member.|Massive red-brown siltstone, in situ shale-intraclast breccia, minor claystone and sandstone.|
36069|Nullawun Member|71494|4|Described|p2-p4, p6-p9, p12-p13, p15, p17-p19, p26|||Up to 71.5 metres thick. The most distinctive member of the Mainoru Formation. Deposited as non-marine mudstone; probably fluvial floodplain deposits; brecciated during palaeosol formation. Core log features presented in this volume.||Mainoru Formation||Disconformably overlies the Limmen Sandstone. Conformably overlain by the Mountain Valley Limestone Member.|Massive reddish-brown mudstone and mudstone breccia.|
36069|Nullawun Member|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Mainoru Formation||||24-SEP-18
36069|Nullawun Member|73242|5|Briefly described|p39|||||Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Wadjeli Sandstone Member. Overlain by Mountain Valley Limestone Member.|Includes mudstone and shale.|
42398|Nyirripi beds|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Aileron Province.||||||07-NOV-08
42398|Nyirripi beds|68832|4|Described|p51-55|||Aileron Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Maximum deposition age and younger metamorphic age.|1790+/-12 Ma, 1644+/-9 Ma|||Likely metamorphosed by Andrew Young Igneous Complex. May be similar age to Reynolds Range Group.|Pelitic and psammitic granulite facies metasedimentary rocks. Quartz-K-feldspar-cordierite-biotite-sillimanite-rutile granofels sampled.|
42398|Nyirripi beds|68994|5|Briefly described|p5|||Underwent low-pressure, high-temperature metamorphism by intrusion of Andrew Young Igneous Complex at 1640+/-6 Ma.||||Intruded by Andrew Young Igneous Complex.||13-JAN-17
42398|Nyirripi beds|69427|5|Briefly described|p12:8, 25|||Aileron Province. These rocks had originally been assumed to be metamorphosed Lander Rock Formation.|<1790 +/- 12 Ma (Cross et al., 2005).||||Granulite-facies metamorphosed shale and sandstone: mainly cordierite-rich hornfels with variable amounts of cordierite and/or garnet-bearing leucosomes; localised garnet- and cordierite-bearing granite; minor corundum-bearing granite; rare tonalite.|12-JUL-16
42398|Nyirripi beds|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||migmatite|
24436|Octy Formation|42504|5|Briefly described|Table 4 P73|||Reserved, Haines and Bagas Dec 1987.||||||21-NOV-06
24436|Octy Formation|42643|2|Defined|p52|Early Cambrian||||||||
24436|Octy Formation|42644|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Quartz arenite, feldspathic, white and brown; minor siltstone and conglomerate; trace fossils. Geological Province: Georgina Basin.||||||15-NOV-05
24436|Octy Formation|60122|5|Briefly described|p14|Early Cambrian|Early Cambrian|In ALCOOTA  and BARROW CREEK. Geological Province: Goergina Basin.||||||
24436|Octy Formation|61388|5|Briefly described|Map Legend|Cambrian|Cambrian|Brown and white cross-bedded sandstone, minor mudstone; trace fossils common. Geological Province: Georgina Basin.||||||05-OCT-05
24436|Octy Formation|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Of the Shadow Group. Quartz arenite: feldspathic; minor siltstone and conglomerate; Ichnofossils.  Geological Province: southern Georgina Basin.||||||11-OCT-05
24436|Octy Formation|62984|5|Briefly described|p14|Early Cambrian|Early Cambrian|Unconformably overlies Adnera Member of Central Mount Stuart Fm; sharply overlain by Neutral Junction Formation. Dominated by relatively clean sandstone and minor mudstone. Contains typical Early Cambrian trace fossils. Geol.Prov: Georgina Basin.||||||07-FEB-08
24436|Octy Formation|64068|3|Fully described|p55-56, p51, 53, 54, 55, 82|Early Cambrian|Early Cambrian|Previously uppermost beds of Central Mount Stuart Formation. Correlations: Mount Baldwin Formation, possibly Sylvester Sandstone, Arumbera Sandstone 3-4, Yuendumu Sandstone 2.||Of Shadow Group.||Overlies Adnera Member probably disconformably. Overlain disconformably by Neutral Junction Formation, or rocks tentatively assigned to Chabalowe Formation.|White and brown, locally glauconitic, medium feldspathic quartzarenite; minor interbedded siltstone, mudstone, purple silty sandstone; local basal conglomerate.|04-APR-12
24436|Octy Formation|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
24436|Octy Formation|65338|5|Briefly described|p65.|Early Cambrian|Early Cambrian|Removed from Central Mount Stuart Formation (Haines et al. 1991) after recognition of a disconformity. Contains ichnofauna.||||Overlies Adnera and Tops Members.|Clastic sedimentary rocks.|
24436|Octy Formation|65341|4|Described|p2 Fig.2, p5, p16. |Early Cambrian|Early Cambrian|Part-equivalent to Mount Baldwin Formation. Correlated also with upper parts of Arumbera Sandstone (Amadeus Basin) and Yuendumu Sandstone (Ngalia Basin). Definitive ichnofossils common, including Treptichnus ('Phycodes') pedum.||Unit in Shadow Group.||Unconformably overlies Central Mount Stuart Formation. Is unconformably overlain by Chabalowe Formation.|Brown and white, crossbedded medium sandstone and quartzite; basal mudstone; locally glauconitic.|
24436|Octy Formation|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Is overlain by Neutral Junction Formation.||12-JUL-16
24436|Octy Formation|69443|4|Described|p28:7, 14-15|Early Cambrian|Early Cambrian|Haines in Haines et al. (1991). Southern Georgina Basin. A  resistant range-capping unit. Up to 150m thick. Open marine to tidal deposits with occasional exposure.||Shadow Group.||Overlies Adnera Member ?disconformably. Is similarly overlain by Neutral Junction Formation, or by ?Chabalowe Formation. Is correlated with lower Mount Baldwin Formation and ?Sylvester Sandstone.|Locally glauconitic, predominantly medium-grained, cross-bedded and planar laminated feldspathic quartz sandstone, interbedded with minor siltstone, mudstone and silty sandstone; local thin basal conglomerate.|12-JUL-16
24436|Octy Formation|69561|6|Mentioned|p33 fig 2|Cambrian|Cambrian|||||Overlain by Neutral Junction Formation||
24436|Octy Formation|69673|5|Briefly described|p114 fig 92, p116|||Up to 150m thick.||Shadow Group||Overlain by Neutral Junction Formation, correlated with Mount Baldwin Formation|Sandstone interbedded with minor sitlstone, mudstone and silty sandstone,|
24436|Octy Formation|72516|6|Mentioned|p90|Cambrian|Cambrian|Georgina Basin.||||Equivalent to the Mount Baldwin Formation, along with the Neutral Junction Foramiton  and Adam Shale..||02-JUN-21
28161|Old Hamilton Downs Gneiss|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wigley Complex.  Biotite-quartz-feldspar granitic gneiss.  Geological Province: Arunta Block.||||||03-NOV-04
28161|Old Hamilton Downs Gneiss|9814|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Biotite-bearing granitic gneiss; muscovite present in east.||||||
28161|Old Hamilton Downs Gneiss|38606|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28161|Old Hamilton Downs Gneiss|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
28161|Old Hamilton Downs Gneiss|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28161|Old Hamilton Downs Gneiss|39888|6|Mentioned|Fig.8|||||||||
28161|Old Hamilton Downs Gneiss|41816|4|Described|p13|||||||||
28161|Old Hamilton Downs Gneiss|41837|6|Mentioned|Map legend|||||||||
28161|Old Hamilton Downs Gneiss|48992|2|Defined|p42|Neoproterozoic|Neoproterozoic|||||||
28161|Old Hamilton Downs Gneiss|50369|6|Mentioned|p26.3|||||||||
28161|Old Hamilton Downs Gneiss|60547|5|Briefly described|Masp Legend|Proterozoic|Proterozoic|Of the Wigley Complex. Geological Province: Arunta Block. Biotite-quartz-feldspar granitic gneiss.||||||
28161|Old Hamilton Downs Gneiss|69427|5|Briefly described|p12:14, 30-31|||Shaw et al. (1979). Wigley Domain, Aileron Province. Crops out over a wide area N of the Charles River Gneiss, W of Simpsons Gap.|||||Homogeneous, medium-grained, foliated leucocratic biotite- and/or muscovite-bearing granite.|12-JUL-16
28161|Old Hamilton Downs Gneiss|73086|6|Mentioned|p9|||Aileron Province. MacDonnell Ranges.||||Faulted contact with the Heavitree Formation.||
76768|Ongeva Package|63866|5|Briefly described|p93|||Aileron Province.|||||Marine sedimentary rocks and bimodal magmatics.|
76768|Ongeva Package|64722|5|Briefly described|Fig. 2 p3-6, p10-11|Orosirian|Orosirian|Informal name. Accumulated between 1810 and 1800 Ma. Together with Lander Package it is broadly correlative with the Tanami and Ware Groups in the Tanami Region.||||||11-APR-12
76768|Ongeva Package|64735|4|Described|p216 Fig15, p216,|Orosirian|Orosirian|Aileron Province. Coeval with Hatches Creek Group, Strzeleckie Volcanics, Tinfish Sandstone, Gwynne Sandstone, Ware Group.|||||Comprises mafic and felsic protoliths of Strangways Metamorphic Complex and clastic metasediments; carbonates and volcanic-hosted massive sulphide deposits.|20-APR-12
76768|Ongeva Package|64737|5|Briefly described|p231-3, p232 Fig.2, p241-2, p244|Orosirian|Orosirian|In east Aileron Province. Narrow age range coeval with the ~1810-1800 Ma Stafford Event. Coeval with Ware and Hatches Creek Groups. Protolith of Strangways Metamorphic Complex, Kanandra Granulite and Bonya Schist||||Overlies Lander Package.|Variably metamorphosed sedimentary and volcanic units, dominantly pelites and psammites, but also mafic and felsic gneisses.|30-APR-12
76768|Ongeva Package|65556|6|Mentioned|p19|||Metasediments.||||||
76768|Ongeva Package|69431|6|Mentioned|p16:1|||Arunta Region. Possible correlative of Hatches Creek Group and, by inference, Tomkinson Creek Group.||||||12-JUL-16
76768|Ongeva Package|70825|6|Mentioned|p40-41|||Arunta Region, North Australian Craton. Is presented as Ongeva package on p40.|c.1.8 Ga.|Strangways Metamorphic Complex.|||Mainly pelites and psammitic rocks of volcaniclastic origin; felsic and mafic gneisses.|
79098|Oodnarta Diorite|69917|5|Briefly described|p167-168, 1|Statherian|Statherian|Eastern Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. Maximum crystallisation age of 1725+/-4 Ma, making it the youngest mafic rock in the Aileron Province in the Quartz sheet area.|1725+/-4 Ma|||Intrudes Bruna Gneiss|Quartz gabbro to diorite. Quartz diorite sampled.|
79098|Oodnarta Diorite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1725+/-7 Ma (U-Pb zircon LA-ICPMS).||||Diorite.|
24443|Oolloo Dolostone|23216|4|Described|p3,Table1p7,38,45-6||Tremadoc|Of the Daly River Group.||||||19-JAN-06
24443|Oolloo Dolostone|23714|5|Briefly described|p7 Table 1.|Paleozoic|Paleozoic|See also page 36. Of Daly River Group. Max. thickness: 190 m.||||||07-NOV-08
24443|Oolloo Dolostone|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
24443|Oolloo Dolostone|42012|2|Defined|p43|Early Ordovician||Supersedes Oolloo Limestone (defn never published).||||||
24443|Oolloo Dolostone|42014|5|Briefly described|Map legend|Ordovician||||||||
24443|Oolloo Dolostone|42070|4|Described|p3|||||||||
24443|Oolloo Dolostone|43140|5|Briefly described|p4|||Of the Daly River Group.||||||21-NOV-06
24443|Oolloo Dolostone|43149|5|Briefly described|Map Legend||Ordovician|Of the Daly River Group.||||||21-NOV-06
24443|Oolloo Dolostone|65339|6|Mentioned|p5 Fig.4. |||||Unit in Daly River Group.|||Sandstone, shale, dolostone.|
24443|Oolloo Dolostone|65345|5|Briefly described|p4.|||||Unit in Daly River Group.|||Ooid and stromatolitic dolostone; minor dolomitic sandstone.|
24443|Oolloo Dolostone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Daly Basin, Centralian B Superbasin. Sequence 2.||||Overlies Jinduckin Formation.||12-JUL-16
24443|Oolloo Dolostone|69443|5|Briefly described|p28:22|Middle Cambrian|Middle Cambrian|Daly Basin.||||Overlies Jinduckin Formation.||12-JUL-16
24443|Oolloo Dolostone|69446|3|Fully described|p31:2-4, 6-7, 9, 11|Middle Cambrian|Middle Cambrian|Kruse et al. (1990); formerly the Oolloo Limestone of Randal (1962), Malone (1962). Central Daly Basin. Up to 249.9m thick; is 192.4m thick in the type section in drillhole NTGS 86/1. High-energy ooid shoals; rare lagoonal, marine deposits. Fossils are rare and generally indeterminate. Potential for modified roll front-style U deposits has been speculated.||Daly River Group.||Conformably and transitionally overlies Jinduckin Formation. Is overlain disconformably/unconformably by Florina Formation.|Lower: thinly bedded fine to medium dolostone, ooid dolograinstone, stromatolitic doloboundstone, cryptomicrobial dololaminite, quartzose dolostone and dolomitic sandstone. Upper: massive/thickly bedded dolostone, minor claystone and sandy mudstone.|12-JUL-16
24443|Oolloo Dolostone|69561|6|Mentioned|p33 fig 2, p33|Boomerangian|Undillan|In comparison to underlying Tindall Limestone is essentially unfossiliferous.||||Overlies Jinduckin Formation||
24443|Oolloo Dolostone|69673|4|Described|p191|||225m thick.||Daly River Group||Overlies Jinduckin Formation|Dolostone, ooid dolograinstone, stromatolitic doloboundstone, dololaminite, quartzic dolostone and dolomitic sandstone with sparse silty laminae, breccias, silty and shaly dolostone beds.|
24443|Oolloo Dolostone|70380|3|Fully described|p743-746, p748-753, p755, p759|Middle Cambrian|Middle Cambrian|Daly Basin. Unfossiliferous. Thought to contain Tremadocian to Floian fossils and was mapped accordingly (Kruse et al., 1990, 1994). The strata containing those fossils was later recognised as a younger, separate unit, the Florina Formation. Previously Oolloo Limestone (Malone, 1962; Randal, 1962). Forms extensive pavements and ridges; includes karst features such as dolines, karren and kamenitza. Up to 250.0m thick; is 192.4m thick in the type section in drillhole NTGS86/1. Graphic logs of drillholes.||Daly River Group.|Briggs, King Members.|Transitionally overlies Jinduckin Formation. Is overlain unconformably by Florina Formation. Correlated with Camooweal Dolostone (Georgina Basin).|A lower well-bedded and an upper massive subdivision is evident in outcrops and down-hole gamma logs.|
24443|Oolloo Dolostone|70866|5|Briefly described|Map legend.|Ordovician|Ordovician|Daly Basin.||Daly River Group.||Conformably overlies Jinduckin Formation.|Pink-grey dolostone, ooid dolograinstone, stromatolitic doloboundstone and cryptalgal dololaminite; minor dolomitic sandstone toward base.|
39122|Ooradidgee Group|23733|5|Briefly described|p2, 8, 27|Paleoproterozoic|Paleoproterozoic|Supersedes Ooradidgee Subgroup.||||||07-NOV-08
39122|Ooradidgee Group|23809|5|Briefly described|p44, p27 Fig. 25|||Geological Province: Davenport Province.  Probably correlates with Bullion Schist.||||||
39122|Ooradidgee Group|50353|5|Briefly described|Map Legend|||||||||
39122|Ooradidgee Group|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Includes: Epenarra Volcanics and the Kurinelli Sandstone.  Age: 1860-1810Ma.||||||21-NOV-06
39122|Ooradidgee Group|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Monument, Bernborough, Yungkulungu and Wundurgi Formations, and Warrego Volcanics. In the Tennant Creek region.||||||07-NOV-08
39122|Ooradidgee Group|63261|5|Briefly described|p23|||Lower section is a time-equivalent of the Killi Killi Formation (Tanami region) and Lander Rock beds (Arunta region).||||||07-FEB-11
39122|Ooradidgee Group|63866|5|Briefly described|p90, p93|||Southern Tennant Region, North Australian Craton. Intruded by dolerites and granites dated at 1810 Ma.|c. 1840 Ma|||Unconformably overlies the Warramunga Group. Unconformably overlain by the Hatches Creek Group.|Bimodal volcanics and sedimentary rocks.|
39122|Ooradidgee Group|64068|5|Briefly described|p31, 33|Statherian|Orosirian|Part of the metasedimentary basement of the Davenport province; deposited 1860-1760 Ma.||||||
39122|Ooradidgee Group|64722|5|Briefly described|Fig. 2 p3-6, p10, 11|Orosirian|Orosirian|Tennant region of the North Australian Craton. Ages from constituents: Epenara Volcanics and Treasure Volcanics.|1840 +/- 4 Ma to 1814 +3 / -6 Ma.||Includes Epenara Volcanics and Treasure Volcanics.||Subaerial to shallow marine sedimentary and bimodal volcanic rocks.|11-APR-12
39122|Ooradidgee Group|64730|5|Briefly described|p141-142|Orosirian|Orosirian|Age constrained by crystallisation ages of volcanics within the sequence (Claoue-Long et al. 2005).|Deposited 1840-1815 Ma.||Includes Epenarra Volcanics near base and Treasure Volcanics near top.|Overlies Warramunga Formation.||03-MAY-12
39122|Ooradidgee Group|64735|3|Fully described|p206 Fig2, p212,  p215, p216 Fig15|Orosirian|Orosirian|Davenport Province. Correlated with Lander Package, Bullion Schist, Tanami Group; sedimentary rocks from the lower part of this group host gold mineralisation.|<1840Ma.||Includes Epenarra Volcanics, Edmirringee Volcanics, Treasure Volcanics,  Kurinelli Sandstone, Rooneys Formation, Taragan Sandstone.|Unconformably overlies Warramunga Formation, Junalki Formation; underlies Hatches Creek Group.|Siliciclastic shallow-marine to sub-aerial sedimentary rocks and bimodal volcanics.|18-APR-18
39122|Ooradidgee Group|64736|6|Mentioned|p221 Fig.3|Orosirian|Orosirian|In Tennant Region. Lateral equivalent of Lander Package in the Arunta Region||||Overlies Warramunga Formation. Overlain by Hatches Creek Group.||30-APR-12
39122|Ooradidgee Group|64737|5|Briefly described|p232, p232 Fig.2, p241, p244|||Of Tennant Region. Similar provenance and depositional timing to Killi Killi Formation and Lander Package.||||Unconformably overlies Warramunga Group.||01-MAY-12
39122|Ooradidgee Group|65209|5|Briefly described|p36, p37, p38, p39|Paleoproterozoic|Paleoproterozoic|Flynn and Ooradidgee Subgroups combined in Ooradidgee Group (Donnellan et al 2001). Volcano-sedimentary succession characterised in outcrop by lateral variations, interdigitation and partial correlation between consituent formations around localised volcanic centres. Likely Warramunga Formation/Ooradidgee Group provenance of Blanche Creek Member clasts. Geol. Prov: Davenport Province.|||Epenarra (basal unit), Treasure, Mia Mia, Warrego, Epenarra, Edmirringee Volcanics; Rooneys, Yungkulungu, Bernborough, Wundirgi Formations; Taragan, Kurrinelli Sandstones.|Overlain by redefined Hatches Creek Group (Hanlon over Wauchope Subgroups)|Volcano-sedimentary succession.|05-JAN-17
39122|Ooradidgee Group|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Sedimentary and mafic to felsic volcanic succession including Treasure Volcanics and Kurinelli Sandstone. Undifferentiated in places where it consists of schistose metasediments, and stratiform mafic meta-igneous rocks. Cross-section only||||||
39122|Ooradidgee Group|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Sedimentary and mafic to felsic volcanic succession including Treasure Volcanics and Kurinelli Sandstone. Undifferentiated in places where it consists of schistose metasediments, and stratiform mafic meta-igneous rocks. Cross-section only.||||||
39122|Ooradidgee Group|65338|3|Fully described|p8 Table 1, p6, p19. |Paleoproterozoic|Paleoproterozoic|Warramunga Province, Tennant Region. Non-outcropping, interpreted from geophysical data; lithology inferred from geophysical character and/or outcrop in adjacent sheet areas. Correlated with Lander Rock Formation, at least in part.|c.1840 - 1815 Ma (Claoue-Long et el. 2008b).||Includes Yungkulungu Formation, Epenarra, Edmirringee and Treasure Volcanics.|Unconformably overlies Junalki Formation, Warramunga Formation and Woodenjerrie beds. Is overlain by Hatches Creek Group.|Bimodal volcanic rocks and fluviatile and shallow-marine sedimentary rocks, metamorphosed to schist, stratiform mafic meta-igneous rocks.|
39122|Ooradidgee Group|65342|6|Mentioned|p13. |Paleoproterozoic|Paleoproterozoic||||Includes Rooneys Formation.|||
39122|Ooradidgee Group|66767|5|Briefly described|p57|||Davenport Province, Tennant Region.|1850-1815 Ma.|||Is overlain by Hatches Creek Group, locally conformably to unconformably. Correlated with Bullion Schist and Lander Rock Formation.|A folded succession of predominantly subaerial felsic and mafic volcanic and fluviatile sedimentary rocks which partly interfinger.|
39122|Ooradidgee Group|66860|6|Mentioned|p6 Tb.1|||Tennant Region. Deposition was coeval with upper parts of both Lander Rock beds (Arunta Region) and Tanami Group (Tanami Region).|||||Bimodal volcanism and shallow-water sediments.|
39122|Ooradidgee Group|67148|5|Briefly described|Map legend.|Orosirian|Orosirian||||Includes Epenarra, Mia Mia and Treasure Volcanics; Kurinelli and Taragan Sandstones, Rooneys Formation.|Is overlain by Hatches Creek Group. Is intruded by Devils Suite granites.||17-OCT-11
39122|Ooradidgee Group|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province. Not shown on legend because it does not outcrop in map area.|||Includes Kurinelli Sandstone and Treasure Volcanics.|||
39122|Ooradidgee Group|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Wundirgi, Monument, Bernborough, Yungkulungu and Rooneys Formations; Warrego, Epenarra and Edmirringee Volcanics; Kurinelli and Taragan Sandstones.||Felsic ignimbrite, tuff, lapilli tuff and lava; chert; sublithic and lithic arenite and wacke; shale and mudstone; pebble beds and conglomerate.|
39122|Ooradidgee Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|~1845-1815 Ma.||Brumbreu, Wundirgi, Bernborough, Rooneys Formations; Taragon, Kurinelli Sandstones; Mia Mia, Epenarra, Edmirringee Volcanics.|Is overlain by Hatches Creek and Tomkinson Creek Groups. Is intruded by Channingum Granite.||
39122|Ooradidgee Group|67329|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic||||||Felsic extrusives and sandstones.|17-JAN-17
39122|Ooradidgee Group|67352|4|Described|v, p8, p10-11 Tb.1, p41, p43-45, p50.|Orosirian|Orosirian|Raised from Subgroup to Group status by Donnellan et al. (2001). Davenport Province.|||Mia Mia Volcanics, Treasure Volcanics, Taragan Sandstone, Kurinelli Sandstone, Rooneys Formation, Epenarra Volcanics, Yungkulungu Formation|Is overlain by Hatches Creek Group.|A volcanosedimentary package with pronounced lateral lithofacies variations.|
39122|Ooradidgee Group|68697|5|Briefly described|p24, p46|||Davenport Province.|||Treasure Volcanics, Mia Mia Volcanics.|Is overlain conformably and transitionally by Hatches Creek Group.||
39122|Ooradidgee Group|69187|4|Described|p51-55 (incl. Fig.2 and 3), p59-61|||Felsic volcanic rocks yielded SHRIMP zircon U-Pb ages of 1840 +/- 4 Ma and 1814 +3/?6 Ma (Claou¿-Long et al. 2008b).|||Includes Epenarra  and Warrego Volcanics and Bernborough, Brumbreu, Monument, Wundirgi and Yungkulungu Formations|unconformably overlies Warramunga Formation; is unconformably overlain by Tomkinson Creek Group and Hatches Creek Group|consists of subaerial to shallow marine siliciclastic sedimentary rocks with intercalated felsic volcanic units|14-APR-15
39122|Ooradidgee Group|69417|5|Briefly described|p2:4-5|Orosirian|Orosirian|Tennant Region, Warramunga Province.|1845-1810 Ma.||||Shallower marine sandstone and felsic volcanic rocks.|12-JUL-16
39122|Ooradidgee Group|69424|3|Fully described|p9:1-6, 10, 14-28, 30-32, 34, 53-54|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Warramunga Province. Originally defined (Blake et al., 1985) as a Subgroup of Hatches Creek Group in the Davenport Province. Reasons for upgrade are explained. Four spatially-discrete successions have been mapped, and are described in detail. Up to c.3000m thick. Folding during the Davenport Event is described. Ended c.1810 Ma.|||Brumbreu, Wundirgi, Bernborough, Monument, Yungkulungu, Rooneys Formations; Warrego, Epenarra, Treasure, Edmirringee Volcanics;  Taragan, Kurinelli Sandstones.|Is overlain unconformably by Wauchope and Hanlon Subgroups (Hatches Creek Group) and by Tomkinson Creek Group. Time-correlative of Edith River and El Sherana Groups.|Volcanic rocks in this area are exclusively felsic (rhyolitic to dacitic).|12-JUL-16
39122|Ooradidgee Group|69425|3|Fully described|p10:1-10, 13, 15, 20, 22-23, 25|Orosirian|Orosirian|Blake et al. (1985) included their Ooradidgee Subgroup with their Wauchope and Hanlon Subgroups to form the redefined Hatches Creek Group. Subsequently Donnellan et al. (2001) combined the Ooradidgee and Flynn Subgroups to form their own (Ooradidgee) Group. Warramunga and Davenport Provinces. Metamorphosed mostly to greenschist facies. Associated with the Cu-Ni deposit at Prospect D, and the secondary Cu mineralisation in quartz veins at the Comet Bore prospect. Stated to be Statherian on p10:1, but all geochronologic ages are Orosirian.|||Epenarra, Edmirringee, Treasure, Mia Mia Volcanics; Rooneys Formation; Kurinelli, Taragan Sandstones.|Is overlain by Gwynne Sandstone conformably/disconformably/unconformably. Is intruded by Ali Curung and Elkedra Granites. Correlated with Bullion Schist and Lander Rock Formation (Aileron Province).|Siltstone, quartz-mica schist, meta-lithic sandstone and metamorphosed pyroclastic rocks, feldspathic/lithic sandstone and amphibolite (probably partially intrusive).|12-JUL-16
39122|Ooradidgee Group|69426|6|Mentioned|p11:7|||Davenport Province (Tennant Region).||||||12-JUL-16
39122|Ooradidgee Group|69427|5|Briefly described|p12:3-4, 6, 59|||Warramunga and Davenport Provinces, Tennant Region. Direct stratigraphic correlatives occur in 1860-1830 Ma sedimentary protoliths of metasedimentary rocks in the Aileron Province. May transition laterally into Bullion Schist. Hosts the Prospect D Ni(-Cu-Au-Ag) deposit (described in some detail), 30km NE of Barrow Creek.||||Time-equivalent of Lander Rock Formation.||12-JUL-16
39122|Ooradidgee Group|69431|5|Briefly described|p16:1-4, 6-8, 13-14, 22|Orosirian|Orosirian|Warramunga Province. Rocks which were previously assigned to the Flynn Subgroup (Donnellan et al., 1995) were assigned to this unit by Donnellan et al. (2001). Does not crop out in the Tomkinson Province. Is intruded in the Kurinelli area by a dolerite sill aged 1811 +/- 5 Ma (Maidment et al., 2006; Claoue-Long et al., 2008).|c.1850-1810 Ma (SHRIMP U-Pb zircon).||Brumbreu, Wundirgi Formations.|Is overlain unconformably by Tomkinson Creek Group.||12-JUL-16
39122|Ooradidgee Group|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
39122|Ooradidgee Group|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1872+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyry.|
39122|Ooradidgee Group|72379|5|Briefly described|p4,p10|Paleoproterozoic|Paleoproterozoic|Geological province:Warramunga Province.|||Includes Wundirgi Formation.|||
39122|Ooradidgee Group|72380|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.|||Includes Treasure Volcanics and Taragan Sandstone.|||
39122|Ooradidgee Group|72707|6|Mentioned|p2, p4|||Warramunga Province. RVDD0002 drill hole contains volcaniclastic sandstones of variable grainsize tentitatively assigned to the Ooradidgee Group. This felsic to intermediate volcaniclastic and volcanic rock sequence (rhyodacite/dacite origin) was variably chlorite-, feldspar- and/or hematite-altered.||||||
39122|Ooradidgee Group|73083|6|Mentioned|p11, p14|||Warramunga Province. Previously called Ooradidgee Subgroup. Not equivalent to Ledan Schist.||||Equivalent to Lander Rock Formation.||
39122|Ooradidgee Group|73089|6|Mentioned|p32, p38|Orosirian|Orosirian|Tennant Region.|[c.]1840-1815 Ma|||||
39122|Ooradidgee Group|73124|6|Mentioned|p2 Fig.1||||||Brumbreu Formation, Wundirgi Formation, Warrego Volcanics, Bernborough Formation, Monument Formation|||
39122|Ooradidgee Group|73125|5|Briefly described|p1-2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province. Comprises the major part of the mineralised basement in the Rover field.|||Monument, Wundirgi, Brumbreu, Yungkulungu, Rooneys Formations; Warrego, Epenarra, Edmirringee, Treasure Volcanics; Kurinelli, Taragan Sandstones.|||
39122|Ooradidgee Group|73427|5|Briefly described|p3-4, p12-13, App.A|Orosirian|Orosirian|North Australian Craton, Tennant Region/East Tennant. Reflect a shallow marine to subaerial setting.|1855-1810 Ma||Yungkulungu Formation, Monument Formation, Epenarra Volcanics, Bernborough Formation||Bimodal volcanic rocks and sedimentary rocks that are mostly unmetamorphosed.|
39122|Ooradidgee Group|73460|6|Mentioned|p2|||Warramunga Province.|||Brumbreu Formation, Wundirgi Formation, Warrego Volcanics, Bernborough Formation, Monument Formation|||
39122|Ooradidgee Group|73550|5|Briefly described|p1, p4-7, p11, p19-20|||Hosts copper-gold-bismuth mineralisation in the Rover field. Varies upward from deep-water to sublittoral/littoral and finally fluviatile facies. Comprise basement rocks across large areas of the Rover field and Bluebush area.|||Monument Formation, Yungkulungu Formation, Edmirringee Volcanics|Unconformably underlain (angular) by Warramunga Formation, Junalki Formation and Woodenjerrie beds.|Dominantly volcanic (and volcaniclastic) rocks intercalated with sedimentary sequences.|
39122|Ooradidgee Group|73590|5|Briefly described|p1-2|||Donnellan (2013) recognised three volcanic episodes in the Ooradidgee Group. Folded during the Davenport Event. Hosts mineralisation.|||Brumbreu, Wundirgi, Bernborough, Monument, Yungkulungu, and Rooneys formations; Epenarra, Edmirringee, and Treasure volcanics; and Taragan and Kurinelli sandstones|Unconformably (angular) underlain by Warramunga Formation, Junalki Formation, and Woodenjerrie beds.|Dominantly volcanic and volcaniclastic rocks intercalated with sedimentary sequences that vary upward from deep-water to sublittoral/littoral and finally fluviatile facies.|
27297|Ooralingie Granite|22524|6|Mentioned|p41|||||||||
27297|Ooralingie Granite|23733|5|Briefly described|p27, 28|Paleoproterozoic|Paleoproterozoic|Of Barrow Creek Granite Complex.||||||07-NOV-08
27297|Ooralingie Granite|23809|5|Briefly described|p43, p41 Tb. 5|Paleoproterozoic|Paleoproterozoic|Foliated megacrystic biotite-rich granite.  Age: 1809+/-5Ma.  Intrudes Bullion Schist.  Geological Province: Arunta Province.||||||07-NOV-08
27297|Ooralingie Granite|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Ali Curung Suite. Age: 1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
27297|Ooralingie Granite|42643|2|Defined|p50|Mesoproterozoic|Paleoproterozoic|Of the Barrow Creek Granite Complex. Reserved. Defn card avail.||||||07-NOV-08
27297|Ooralingie Granite|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Barrow Creek Granite Complex. Biotite granite-adamellite, medium to coarse grained, porphyritic, foliated, xenolith rich.||||||07-NOV-08
27297|Ooralingie Granite|50369|5|Briefly described|p1.5, 17.1, 18.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Ali Curung Suite.||||||07-NOV-08
27297|Ooralingie Granite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Biotite granite with porphyritic K-feldspar, and locally abundant enclaves and xenoliths; minor orthogneiss; and, equigranular to porphyritic biotite and biotite-muscovite granite, respectively.  In the Tennant Creek region.||||||07-NOV-08
27297|Ooralingie Granite|64735|5|Briefly described|p206||||1809 +/-5 Ma.|Of Barrow Creek Granite Complex.||Intrudes Bullion Schist.||20-APR-12
27297|Ooralingie Granite|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Presented, in Fig.1, as Ooralingie & Bean Tree Gr||||||
27297|Ooralingie Granite|65338|6|Mentioned|p39.|Orosirian|Orosirian|In BARROW CREEK area.|1809 +/- 5 Ma.|||||
27297|Ooralingie Granite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||||Biotite granite with porphyritic K-feldspar, locally abundant enclaves and xenoliths, minor orthogneiss.|
27297|Ooralingie Granite|69424|5|Briefly described|p9:29|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Textural and compositional differences make it unlikely the nearby Warrego Granite is of similar age.|1809 +/- 5 Ma.|||||12-JUL-16
27297|Ooralingie Granite|69427|4|Described|p12:19, 22|Orosirian|Orosirian|Barrow Creek area, Aileron Province. SHRIMP U-Pb zircon age.|1805 +/- 5 Ma (Smith, 2001).|Barrow Creek Granite Complex.||Intrudes Lander Rock Formation. Is intruded by Bean Tree Granite.|Medium- to very coarse-grained, foliated porphyritic biotite granite and quartz monzonite; contains abundant xenoliths.|12-JUL-16
27297|Ooralingie Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1809+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
27297|Ooralingie Granite|72378|5|Briefly described|p22|Orosirian|Orosirian|Geological province: Aileron Province. SHRIMP 207Pb/206Pb zircon crystallisation age of 1809+\-5 Ma (Smith 2001), thereby constraining minimum depositional age of Bullion Schist sedimentary protolith.|1809+\-5 Ma (207Pb/206Pb; magmatic)|Unit of Barrow Creek Granite Complex.||Intrudes into Bullion Schist.||
38050|Opparinna Metamorphics|24301|2|Defined|p38 Appendix 1|Neoproterozoic|Paleoproterozoic|Intruded by dykes of Kulpitjata Granite Complex.  Maximum thickness: 85m.  Geological Province: Musgrave Block||||||07-NOV-08
38050|Opparinna Metamorphics|24302|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Quartzite, amphibolite, muscovite-biotite-garnet schist, viridine (Mn-rich andalusite) schist. Geological Province: Musgrave Block||||||29-SEP-05
38050|Opparinna Metamorphics|24496|5|Briefly described|p14|||Geological Province: Musgrave Block.||||||
38050|Opparinna Metamorphics|61154|5|Briefly described|p8, p9 Fig. 6|||Metasedimentary rocks. Intruded by 1150Ma Kulpitjata Suite granite and pegmatite dykes. Age:<1150Ma; in the Kelly Hills has a single zircon population with age of 1603+/-36Ma. See also p26.||||||19-JUL-05
38050|Opparinna Metamorphics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|1603 +/- 36 Ma (maximum depositional age).|||||
38050|Opparinna Metamorphics|69417|5|Briefly described|p2:5|Statherian|Statherian|Musgrave Province.||||Is intruded by Musgravian gneiss.||12-JUL-16
38050|Opparinna Metamorphics|69436|5|Briefly described|p21:6|||Young et al. (2002). SW Kelly Hills, N of the Musgrave Ranges, Musgrave Province. SHRIMP U-Pb detrital zircon maximum deposition age.|>1603 +/- 36 Ma (Young et al, 2002).|||Is intruded by Kulpitjata Suite.|Basal Mn-rich quartz-muscovite schist (up to 30m) with viridine porphyroblasts; overlain by 15m of quartzite and c.50m of meta-igneous amphibolite, which is partly interlayered with the quartzite.|12-JUL-16
38050|Opparinna Metamorphics|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1603+/-36 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
73222|Orion Granodiorite|62580|5|Briefly described|p47|||Part of the composite Lewis Granite (Frederick Suite). Fine- to medium-grained, equigranular biotite granodiorite.||||||07-FEB-11
29772|Ormiston Pound Granite|7837|5|Briefly described|p91-98, 100-103|||Southern Arunta Inlier. Intruded during late-stage Chewings Orogeny, not at 1050 Ma as previously inferred. Zircon analyses tabulated.|1603 +/- 10 Ma.||||A small, irregular pluton of equigranular, leucocratic, strongly to weakly recrystallized and foliated granite. Has numerous N-trending satellite dykes. Rare xenoliths of country-rock gneiss dated at least 1678 +/- 14 Ma.|
29772|Ormiston Pound Granite|23363|5|Briefly described|352 Tab.3|Calymmian|Statherian|Age: 1603+/-10Ma.||||||21-NOV-06
29772|Ormiston Pound Granite|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
29772|Ormiston Pound Granite|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the Iwupataka Metamorphic Complex.||||||07-NOV-08
29772|Ormiston Pound Granite|43503|2|Defined|8,25,78|||Age: 1000-1100Ma (??).||||||21-NOV-06
29772|Ormiston Pound Granite|44114|5|Briefly described|p334-335, 341|||Age of zircons in a gneissic xenolith. Another population was dated 1678 +/- 14 Ma.|1600 Ma (Collins et al. 1995).||||Variably deformed.|
29772|Ormiston Pound Granite|50369|5|Briefly described|p1.5, 22.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Iwupataka Suite. Age: 1603 +/- 10Ma.||||||07-NOV-08
29772|Ormiston Pound Granite|61660|5|Briefly described|p3. |Proterozoic|Proterozoic|Interpreted syn-tectonic. Contains a gneissic xenolith aged 1678 +/- 14 Ma (Collins et al. 1995), identical in age with migmatitic orthogneiss from the Glen Helen Metamorphics. Metamorphic zircon rims have an age of 1575 +/- 20 Ma, similar to rims in the Kakalyi Gneiss.||||||
29772|Ormiston Pound Granite|64809|5|Briefly described|p11 Fig.10 |Mesoproterozoic|Palaeoproterozoic|||||||
29772|Ormiston Pound Granite|69417|5|Briefly described|p2:5|Statherian|Statherian|Haasts Bluff Domain, Warumpi Province.|1610-1600 Ma.|||||12-JUL-16
29772|Ormiston Pound Granite|69428|5|Briefly described|p13:7, 15|||Warren and Shaw (1995). SHRIMP U-Pb zircon age. Abbreviated to Ormiston Granite (twice) on p13:15. Contains a xenolith with zircon metamorphic rims aged 1575 +/- 20 Ma.|1603 +/- 10 Ma (Collins et al., 1995).|||Intrudes Glen Helen Metamorphics.|Foliated granite, leucogranite and pegmatite.|12-JUL-16
81664|Orunyah Granite|72377|5|Briefly described|p10|Paleoproterozoic|Paleoproterozoic|Interpreted to be co-magmatic with c. 1872 Ma Bawaka Granite and c. 1862 Ma Drimmie Head Granite, based on similar chemistry and mineralogy.||||Overlain by Haddon Volcanics.||04-OCT-19
69486|Outounya gneiss|61154|6|Mentioned|p43 Appendix|Mesoproterozoic|Mesoproterozoic|Gneiss of the 1600-1540Ma period. Geological Province: Musgrave Block.||||||21-NOV-06
69486|Outounya gneiss|65309|6|Mentioned|p7, p16.|||Airborne magnetic data suggest this unit extends, with structural continuity, from Kulgera map area into Umbeara map rea.|1550 Ma.|||||16-JAN-15
28141|Overland Sandstone|14019|3|Fully described|p24-25|Late Cambrian|Late Cambrian|Of the Elder Subgroup. Lithic arkose and sandstone. Conformably overlies Eagle Hawk Sandstone, unconformably underlies the Mahony Group. Type section: 230m. Geological Province: Ord Basin.||||||
28141|Overland Sandstone|40993|6|Mentioned|Fig.1|||||||||
28141|Overland Sandstone|41840|3|Fully described|p43|||Formerly included in the Elder Sandstone.||||||15-DEC-08
28141|Overland Sandstone|41864|4|Described|p26|||||||||
28141|Overland Sandstone|41865|5|Briefly described|Map legend|Late Cambrian|Middle Cambrian|||||||
28141|Overland Sandstone|41866|5|Briefly described|Map legend|Late Cambrian||||||||
28141|Overland Sandstone|43855|5|Briefly described|Map Legend|Boomerangian|Templetonian|||||||
28141|Overland Sandstone|44868|5|Briefly described|Map Legend|Boomerangian|Ordian|||||||
28141|Overland Sandstone|60419|4|Described|p1, 11|Late Cambrian|Late Cambrian|Of Elder Subgroup. Overlies Eagle Hawk Sandstone. Fluvial. Geological Province: Ord Basin.||||||
28141|Overland Sandstone|60519|5|Briefly described|Map Legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup (Goose Hole Group).  White, fine to medium grained lithic arkose. Geological Province: Ord Basin.||||||03-NOV-04
28141|Overland Sandstone|60589|5|Briefly described|Map legend|Late Cambrian|Late Cambrian|Of the Elder Subgroup.  White, fine to medium lithic arkose and sandstone.  Conformably overlies Eagle Hawk Sandstone.  Geological Province: Ord Basin.||||||
28141|Overland Sandstone|64580|6|Mentioned|map legend|||Of Goose Hole Group.||||||15-DEC-08
28141|Overland Sandstone|67860|4|Described|p417 fig4-85, p419 Tb.4-18, p421 fig4-86|Late Cambrian|Late Cambrian|0-230 m thick. Type section details given. Unfossiliferous.||Elder Subgroup||Conformably overlies Eagle Hawk Sandstone.|White lithic feldspathic sandstone; rare shale.|
28141|Overland Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Furongian|Furongian|Ord Basin||Elder Subgroup|||White lithic feldspathic sandstone; rare shale.|04-AUG-15
28141|Overland Sandstone|69165|5|Briefly described|100k_interpgeop_lut.csv|Furongian|Furongian|See also 500k_geologyp08_lut.csv. ||Elder Subgroup|||White lithic feldspathic sandstone, rare shale.|
28141|Overland Sandstone|69437|5|Briefly described|p22:10-11|Series 4|Series 4|Ord Basin, Centralian B Superbasin. Sequence 2. Fluviatile deposits.||||Overlies Eagle Hawk Sandstone.||12-JUL-16
28141|Overland Sandstone|69446|6|Mentioned|p31:4|||Ord Basin.||||||12-JUL-16
28141|Overland Sandstone|69448|3|Fully described|p33:2-4, 6-7|Cambrian|Middle Cambrian|Mory and Beere (1985). Ord Basin. 230m thick at the type section, a steep-sided plateau straddling the WA-NT border in the northwestern LIMBUNYA map area. In WA, the unit thins to the SW and pinches out. Braided fluviatile deposits. Unfossiliferous; most likely late Middle or early Late Cambrian.||Elder Subgroup.||Conformably and gradationally overlies Eagle Hawk Sandstone. Is overlain unconformably by Mahony Group. Correlated with Skewthorpe Formation (Bonaparte Basin).|White to pale grey or fawn, fine to medium lithic arkose and sandstone; trough and planar cross-beds, current ripple marks, parallel lamination.|12-JUL-16
28141|Overland Sandstone|69634|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|497-485.4 Ma (Biostrat)|Unit of Elder Subgroup.|||White lithic feldspathic sandstone; rare shale|
28141|Overland Sandstone|69673|5|Briefly described|p194|||230m thick.||Elder Subgroup||Overlies Eagle Hawk Sandstone|Lithic arkose and sandstone.|
28141|Overland Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv|Ordovician|Cambrian||485-497 Ma|Elder Subgroup|||White lithic feldspathic sandstone; rare shale.|
28141|Overland Sandstone|71267|4|Described|GEOL_LUT_CSV files|Furongian|Furongian|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.|497-485.4 Ma (biostrat)|Unit of Elder Subgroup.|||White lithic feldspathic sandstone; rare shale|
28141|Overland Sandstone|71800|5|Briefly described|p25-p26|Late Cambrian|Middle Cambrian|Ord Basin. Deposited in a fluvial environment.||Elder Subgroup||Overlies the Eagle Hawk Sandstone. Unconformably overlain by the Mahony Group.|White, clayey arkose.|
28141|Overland Sandstone|73255|6|Mentioned|p534 Fig.2|Cambrian|Cambrian|||Goose Hole Group||Overlies the Eagle Hawk Sandstone, disconformably underlies the Buchanan Sandstone.||
77885|Pandanus Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Purplish brown and grey thin-bedded and laminated micaceous siltstone, shale and fine sandstone.|
77885|Pandanus Formation|68146|5|Briefly described|p21|||||Wild Cow Subgroup.||Is overlain by Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77885|Pandanus Formation|68575|5|Briefly described|p19|||South Nicholson Basin.||Wild Cow Subgroup.||Is overlain by Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77885|Pandanus Formation|69591|5|Briefly described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Storm-dominated shelf deposits.||Wild Cow Subgroup.||Overlies Hedley Sandstone. Is overlain by Burangoo Sandstone.|Purplish-brown and grey, thin-bedded and laminated micaceous siltstone, shale and fine sandstone.|
77885|Pandanus Formation|71369|4|Described|p1, p6, p8-9, p11-15, p22, p35, p47, p49|Mesoproterozoic|Mesoproterozoic|See also p19. South Nicholson Basin. Previously the Pandanus Siltstone Member (Smith and Roberts, 1962; Roberts et al., 1963) of Constance Sandstone. Raised to Formation status in this study (Sweet, 2017). Rarely exposed; covered by debris on scree slopes. Up to 130m thick. Shallow- to moderate-depth shelf deposits. Outcrop pattern indicates left lateral (fault) movement of 700-800m.|c.1500 Ma.|Wild Cow Subgroup.||Overlies Hedleys Sandstone. Is overlain by Burangoo Sandstone ?unconformably.|Greyish-green to greyish red shale coarsening-up to siltstone and interbedded fine-grained sandstone.|20-FEB-18
77885|Pandanus 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 Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|26-NOV-19
77885|Pandanus 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 Wild Cow Subgroup.||Overlain by Burangoo Sandstone. Underlain by Hedleys Sandstone.|Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Burangoo Sandstone. Underlain by Hedleys Sandstone.|Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus 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 Wild Cow Subgroup.|||Greyish green o greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone.|
77885|Pandanus Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus 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.||Unit of Wild Cow Subgroup.|||Greyish green to greyish red, thin-bedded and laminated, micaceous siltstone, shale and fine-grained sandstone|
77885|Pandanus Formation|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as located in the eastern part of the South Nicholson Basin.||South Nicholson Group||Overlies Hedleys Sandstone and underlies Burangoo Sandstone.||
77885|Pandanus Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Hedleys Sandstone and underlies Burangoo Sandstone.|Includes siltstone.|
77885|Pandanus Formation|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Hedleys Sandstone and underlies Bunangoo Sandstone.|Includes siltstone.|
77885|Pandanus Formation|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Used in Qld. Distinct from Pandanus Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77885|Pandanus Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Hedleys Sandstone. Overlain by Burangoo Sandstone.||
77885|Pandanus Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Hedleys Sandstone. Overlain by Burangoo Sandstone.||
28201|Pandanus Siltstone Member|23065|6|Mentioned|17|||Geological province: South Nicholson Basin. Of the South Nicholson Group.||||||22-NOV-06
28201|Pandanus Siltstone Member|23393|5|Briefly described|p21|Mesoproterozoic|Mesoproterozoic|Of Constance Sandstone.||||||
28201|Pandanus Siltstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Constance Sandstone.||||||
28201|Pandanus Siltstone Member|35640|6|Mentioned|Map legend|Adelaidean|Carpentarian|Prob. Adelaidean - Carpentarian.||||||22-NOV-06
28201|Pandanus Siltstone Member|36012|3|Fully described|Table 4|||||||||
28201|Pandanus Siltstone Member|36439|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||22-NOV-06
28201|Pandanus Siltstone Member|36442|6|Mentioned|Map legend|Adelaidean|Carpentarian|Carpentarian or Adelaidean.||||||22-NOV-06
28201|Pandanus Siltstone Member|38584|4|Described|p19|||||||||
28201|Pandanus Siltstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
28201|Pandanus Siltstone Member|41721|4|Described|p29|||Of Constance Sandstone. Thickness: 130m. Fissile/ flaggy, green, purplish-brown and grey coarse siltstone with shaly partings and thin interbeds of very fine to fine-grained sandstone and wacke; middle section often contains a prominent bed of blocky sst.||||||02-AUG-07
28201|Pandanus Siltstone Member|44305|14|Not recorded|p.14-15||Neoproterozoic|Defn. on Tech.File (E/53-8). opp.6. U.Prot.||||||
28201|Pandanus Siltstone Member|44306|14|Not recorded|map legend|||(?) Upper Proterozoic.||||||
28201|Pandanus Siltstone Member|44482|14|Not recorded|p.9,opp. p.6, map|||(E53-12). (Of Constance Sandstone).||||||
28201|Pandanus Siltstone Member|44483|5|Briefly described|map legend|||Upper (?) Proterozoic.||||||
28201|Pandanus Siltstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Constance Sandstone.||||||
28201|Pandanus Siltstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Constance Sandstone. Flaggy brown micaceous lithic fine grained sandstone; minor siltstone and shale.||||||
28201|Pandanus Siltstone Member|65337|3|Fully described|p9 Fig.5, p38 Table 5, p51.|Mesoproterozoic|Mesoproterozoic|Deeper marine: lower shoreface and shelf environment. Shows parting lineations, hummocky cross-stratification, small trough cross-beds, parallel lamination, slumping and convolute bedding.||Unit in Constance Sandstone.||Overlies Hedleys Sandstone Member. Is overlain by Burangoo Sandstone Member.|Flaggy, brown, micaceous, lithic fine-grained sandstone; minor siltstone and shale.|
28201|Pandanus Siltstone Member|67539|6|Mentioned|p15 Fig.8|||Replaced by Pandanus Siltstone||||||
28201|Pandanus Siltstone Member|69434|4|Described|p19:2, 6|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. 20-50m thick. Deeper-marine deposits: lower shoreface and storm-dominated shelf.||Constance Sandstone.||Conformably overlies Hedleys Sandstone Member. Is overlain conformably by Burangoo Sandstone Member.|Flaggy, micaceous, lithic fine sandstone; minor siltstone and shale.|12-JUL-16
28201|Pandanus Siltstone Member|70897|5|Briefly described|p38, Fig.1.7.6|Mesoproterozoic|Mesoproterozoic|Represents regional flooding episodes.||Constance Sandstone.|||Siltstone, shale.|
28201|Pandanus Siltstone Member|71369|5|Briefly described|p5-6, p8, p13, p20|Mesoproterozoic|Mesoproterozoic|Smith and Roberts (1962), Roberts et al. (1963) as a unit in Constance Sandstone. Raised to Formation status in this study (Sweet, 2017). South Nicholson Basin. Misnamed in Fig.2d on p6 as Pandanus Sdst Mbr.||Constance Sandstone||||20-FEB-18
28201|Pandanus Siltstone Member|72526|5|Briefly described|p33,|||Of Rawlings et al. (2008) [Name replaced by Pandanus Formation].||Of Constance Sandstone of Rawlings et al., 2008.||||
28201|Pandanus Siltstone Member|72527|6|Mentioned|p7 Fig.1.4, p41.|Mesoproterozoic|Mesoproterozoic|Shown as (abbreviated) sandstone member on p7 Fig. 1.4.||Constance Sandstone||Overlies Hedley Sandstone Member and underlies Burangoo Sandstone Member.||
28201|Pandanus Siltstone Member|72919|6|Mentioned|p47|Ectasian|Calymmian|Rawlings et al. (2008).||Of Constance Sandstone.||||
22623|Paperbark Granite|22754|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.||||||07-NOV-08
22623|Paperbark Granite|23323|5|Briefly described|p456 Table 1|Orosirian|Orosirian|Age: 1854 +/- 3 Ma.||||||07-FEB-07
22623|Paperbark Granite|24197|5|Briefly described|p89 Tb. 11.1|Paleoproterozoic|Paleoproterozoic|Of the Paperbark Supersuite. Age: 1850Ma. Geological province: Kimberley Province (East).||||||07-FEB-11
22623|Paperbark Granite|24503|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Paperbark supersuite.  Age: 1865-1850Ma.||||||07-NOV-08
22623|Paperbark Granite|43854|5|Briefly described|Map Legend||Proterozoic|Of the Paperbark supersuite.||||||22-NOV-06
22623|Paperbark Granite|44868|5|Briefly described|Map Legend||Proterozoic|||||||
22623|Paperbark Granite|50437|5|Briefly described|p1.5, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Kimberley Region. Of the Paperbark Supersuite. Age: 1854 +/- 3Ma (Shrimp).||||||07-NOV-08
22623|Paperbark Granite|63866|5|Briefly described|p132|||Western Zone, Halls Creek Orogen.|c. 1854 Ma|Paperbark Supersuite||||
22623|Paperbark Granite|66845|4|Described|p537 Fig.3, p539 Tb.1, p540, p543|||Single analysed zircon grain (no. 46.1) distinctly high Th/U ratio with age 2028 Ma; 16 analyses for magmatic crystallis'n age. The Sally Downs supersuite represents a major episode of granite magmatism that is signicantly younger than the Paperbark supersuite.|magmatic crystallis'n age 1854+/-3 Ma SHRIMP U-Pb|Paperbark supersuite|||Porphyritic monzogranite.|04-AUG-15
22623|Paperbark Granite|66846|5|Briefly described|p558 Table 4|Orosirian|Orosirian|Age probably from U-Pb SHRIMP dating of zircon (see p547). |~1854 Ma|Of Paperbark supersuite.||||
22623|Paperbark Granite|69099|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Lamboo Province, Halls Creek Orogen. Data from OZCHRON1. Comment: 'This magmatic age for the granite is based on 16 of the 17 analytical data'.|1854+/-3 Ma U/Pb SHRIMP|Paperbark Supersuite|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock.|04-AUG-15
22623|Paperbark Granite|69165|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|See also GA_geochron.csv. |1854 Ma|Paperbark Supersuite|||Medium-coarse grained monzogranite and syenogranite with rapakivi texture; medium to fine grained biotite-hornblende monzogranite and granodiorite with local inclusions of mafic rock.|
22623|Paperbark Granite|69634|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Halls Creek Orogeny; Halls Creek Orogeny D1/M1; Halls Creek Orogeny D2/M2; Hooper Orogeny; Hooper Orogeny D1/M1 - Western Zone; Hooper Orogeny D2/M2 - Western Zone.|1854-1854 Ma (Isotopic)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock|
22623|Paperbark Granite|70154|4|Described|100k_interpgeop_lut.csv|Paleoproterozoic|Paleoproterozoic||1854 Ma|Paperbark Supersuite|||Medium to coarse grained monzogranite and syenogranite with rapakivi texture; medium to fine grained biotite-hornblende monzogranite and granodiorite.|
22623|Paperbark Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Lamboo Province, Halls Creek Orogen. Events: Alice Springs Orogeny (450-295 Ma); King Leopold Orogeny (670-510 Ma); Yampi Orogeny (1000-800 Ma); Halls Creek Orogeny D2/M2 (1821-1808 Ma); Halls Creek Orogeny (1832-1808 Ma); Halls Creek Orogeny D1/M1 (183 -1821 Ma); Hooper Orogeny D2/M2 - Western Zone (1864-1850 Ma); Hooper Orogeny (1870-1850 Ma); Hooper Orogeny D1/M1 - Western Zone (1870-1864 Ma). See 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv and geochron files.|1854+\-3 Ma (isotopic)|Unit of Paperbark Supersuite.|||Medium- to coarse-grained monzogranite and syenogranite with rapakivi texture; medium- to fine-grained biotite-hornblende monzogranite and granodiorite; locally abundant inclusions of mafic rock|
22623|Paperbark Granite|72437|5|Briefly described|p81-82, p84-85|||Lamboo Complex. Whole-rock analyses are provided.||Paperbark Supersuite|||Foliated biotite-monzogranite, coarse-grained biotite monzogranite and fine-grained biotite monzogranite.|
41848|Papunya Igneous Complex|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Age: 1635Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
41848|Papunya Igneous Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Gabbro, gabbronorite, mafic granulite, mafic amphibolite, extremely magnetic. Geological Province: Yaya Domain.||||||25-OCT-15
41848|Papunya Igneous Complex|65358|5|Briefly described|p12|Statherian|Statherian|The dominant mafic suite intruding Yaya Domain, Warumpi Province. Dated at 1635 Ma (Scrimgeour et al., 2005).||||||
41848|Papunya Igneous Complex|67565|2|Defined|p64, p15, p23-24, p33, p34, p50, p62.|Statherian|Statherian|New name, after the Papunya Community. Previously included in undifferentiated gneiss, schist and other rocks (Ranford, 1969). Includes the informal 'Papunya gabbro', 'South Papunya gabbro', 'Papunya ultramafic' and 'West Papunya gabbro' of Hoatson and Stewart (2001) and Hoatson and Claoue-Long (2002). Yaya Domain, Warumpi Province. Type locality is 1 km north of Beantree Creek. Multiple bodies of various sizes, the largest up to 4 km in length. Ages calculated by Hoatson and Claoue-Long, 2002; other samples gave ages of 1639 +/- 2 Ma and 1635 +/- 5 Ma. Intruded at a similar time to Andrew Young Igneous Complex, but is geochemically distinct. Geochemistry is discussed briefly.|1637 +/- 2 Ma (SHRIMP U-Pb zircon).|||Intrudes Alkipi Metamorphics. Is intruded by Larrie Granodiorite.|Gabbro, gabbronorite, mafic granulite, mafic amphibolite, plagioclase pyroxenite, quartz-bearing gabbro, pyroxenite, minor biotite tonalite and biotite leucogranite.|01-DEC-15
41848|Papunya Igneous Complex|69428|5|Briefly described|p13:10-11, 19|||Scrimgeour et al. (2005). Multiple plutons of variable size up to 4km in length. Geochemistry suggests varying magmatic sources or crustal contamination. Thought to have potential for Ni-Cu-Co sulfides, and lesser potential for PGE mineralisation.||||Intrudes the Yaya Metamorphic Complex. Intruded by Larrie Granodiorite.|Dominantly tholeiitic gabbro: variably recrystallised gabbro, gabbronorite and rare plagioclase pyroxenite, with lesser quartz gabbro, tonalite and leucogranite.|12-JUL-16
41848|Papunya 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.||||||
41848|Papunya Igneous Complex|72711|6|Mentioned|p12.|||||||||
27873|Parsons Range Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
27873|Parsons Range Group|22538|4|Described|Fig4, p710, p714|Statherian|Statherian|Part of the Goyder package.||||||28-MAR-18
27873|Parsons Range Group|22600|4|Described|Map legend|Statherian|Statherian|||||||
27873|Parsons Range Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27873|Parsons Range Group|23374|5|Briefly described|Fig3p5,6,29,34,35||Paleoproterozoic|In the McArthur Basin.||||||07-NOV-08
27873|Parsons Range Group|23937|6|Mentioned|p5 Fig. 5|||||||||02-NOV-04
27873|Parsons Range Group|24047|5|Briefly described|p12 Fig. 10, p11|Paleoproterozoic|Paleoproterozoic|Age: >1670Ma.  Overlain conformably by both Habgood and Balma Groups.  Geological Province: McArthur Basin.||||||07-NOV-08
27873|Parsons Range Group|24048|3|Fully described|p37|Statherian|Statherian|Formerly "Parsons Range Formation".  Max. thickness: 6000m.  Geological Province: McArthur Basin.||||||
27873|Parsons Range Group|24049|5|Briefly described|Map Legend|Statherian|Statherian|Includes Kurala Sandstone, Fleming Sandstone, Marura Siltstone, Mattamurta Sandstone, and Badalngarrmirri Formation (includes Fairy Glen Member, Gali Member, and Mount Fawcett Member). Geol. Prov: McArthur Basin.||||||13-OCT-05
27873|Parsons Range Group|24051|5|Briefly described|Map Legend|Statherian|Statherian|Geological Province: McArthur Basin.||||||
27873|Parsons Range Group|24432|4|Described|p562 Fig.2|Statherian|Statherian|Overlain by Habgood Group. Max. thickness: ~6 km. Age: 1710-1670 Ma. Shallow marine to fluvial deposits. Geological Province: Northern McArthur Basin.||||||
27873|Parsons Range Group|32659|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27873|Parsons Range Group|32660|4|Described|Table 4|||||||||
27873|Parsons Range Group|36473|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27873|Parsons Range Group|37462|4|Described|Table4.IV|||||||||
27873|Parsons Range Group|37565|6|Mentioned|Fig.5|||||||||
27873|Parsons Range Group|37568|6|Mentioned|p77|||||||||
27873|Parsons Range Group|41019|5|Briefly described|p243|||||||||
27873|Parsons Range Group|41406|6|Mentioned|Map legend|Mesoproterozoic||||||||
27873|Parsons Range Group|42597|5|Briefly described|Map Legend|Carpentarian||||||||
27873|Parsons Range Group|42812|6|Mentioned|p10|||||||||
27873|Parsons Range Group|43010|2|Defined|p84-91||Paleoproterozoic|Of Statherian age.||||||28-MAR-18
27873|Parsons Range Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27873|Parsons Range Group|43630|6|Mentioned|p13||Paleoproterozoic|||||||07-NOV-08
27873|Parsons Range Group|44112|3|Fully described|p10-11,20-21,49-50|||Belongs to Supersequence 2. Previously mapped as 'Parsons Range Formation' by Crohn (1956)||||||
27873|Parsons Range Group|44299|4|Described|p.11||Paleoproterozoic|SD/53-7,8. L.Proterozoic. Table 1.||||||07-NOV-08
27873|Parsons Range Group|44300|14|Not recorded|map legend||Paleoproterozoic|SD/53-7,8. L. Proterozoic.||||||07-NOV-08
27873|Parsons Range Group|44434|14|Not recorded|opp.p.6, map|||Equivalent of Groote Eylandt Beds (Tawallah Group). (D53-11,12).||||||22-NOV-06
27873|Parsons Range Group|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27873|Parsons Range Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
27873|Parsons Range Group|61403|5|Briefly described|Map Legend|Statherian|Statherian|Includes Kurala Sandstone, Fleming Sandstone, Marura Siltstone, Mattamurta Sandstone, and Badalngarrmirri Formation (includes Fairy Glen Member, Gali Member, and Mount Fawcett Member). Geol. Prov: McArthur Basin.||||||
27873|Parsons Range Group|63866|5|Briefly described|p54, p114, p116|||Potentially a part of the Prize Supersequence.|ca 1707 Ma (unit relationships)|||Conformably overlies the Donydji Group. Conformably overlain by the Habgood Group and the Balma Group.||
27873|Parsons Range Group|64724|5|Briefly described|p45 Fig.5, p46|Statherian|Statherian|McArthur Basin unit deposited during the Calvert Event (~1730-1690 Ma).||||||02-APR-12
27873|Parsons Range Group|64816|6|Mentioned|p2 Fig.1 |||||||||
27873|Parsons Range Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4, p355 Fig.5 |||Walker Fault Zone, McArthur Basin.|||Includes Kurala, Fleming and Mattamurta Sandstones, Marura Siltstone and Badalngarrmirri Formation.|||
27873|Parsons Range Group|65228|5|Briefly described|p18, p23, Figs.04, 10.|Statherian|Statherian|Northern McArthur Basin. Within Prize Supersequence. The Parsons Range Group has not been directly dated.|||Includes Badalngarrmirri Formation.|Is overlain by Balma Group.||23-FEB-20
27873|Parsons Range Group|65340|6|Mentioned|p10 Fig.5.|||||||||
27873|Parsons Range Group|67323|5|Briefly described|Eastern Australia Time-Space Plot, p34|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Shallow marine to fluvial deposits. Appears as Parson Range Group in the Eastern Australia Time-Space Plot.|~1690-1670 Ma.|||||
27873|Parsons Range Group|69018|6|Mentioned|p450 Fig.1a|||Of McArthur Basin.||||||
27873|Parsons Range Group|69417|6|Mentioned|p2:5|Statherian|Statherian|McArthur Basin.||||||12-JUL-16
27873|Parsons Range Group|69421|6|Mentioned|p6:6|||McArthur Basin.||||||12-JUL-16
27873|Parsons Range Group|69430|4|Described|p15:2-4, 6, 13-14, 20-21, 23|Statherian|Statherian|Plumb and Roberts (1965, 1992), Dunnet (1965). Walker Fault Zone, northern McArthur Basin. 5 to 6km-thick succession. Possible equivalent to Rorruwuy and Coast Range Sandstones, as well as Burash and topmost Echo Sandstones. Age range from surrounding units.|1710-1670 (Rawlings, 1999).||Mattamurta, Fleming, Kurala Sandstones; Marura Siltstone; Badalngarrmirri Formation.|Conformably overlies Donydji Group. Is overlain conformably by Koolatong Siltstone (Habgood Group).||12-JUL-16
27873|Parsons Range Group|69673|4|Described|p3 fig 2, p15, p16 fig 13, p17|Statherian|Statherian|Possibly equivalent to Rorruwuy Sandstone and Coast Range Sandstone. 5-6 km thick. Shallow marine, shoreline and lesser fluvial depositional environments.|||Includes Kurala Sandstone|Overlies Donydji Group, overlain by Habgood Group|Dominantly quartz sandstone and siltstone.|
27873|Parsons Range Group|70968|6|Mentioned|p2 Fig.3|||||||||
27873|Parsons Range Group|71059|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
27873|Parsons Range Group|71374|5|Briefly described|iii, p2, p6, p24, p26-p28, p30, p32|||northern McArthur Basin. Age correlative of the Coast Range Sandstone. ||||||
27873|Parsons Range Group|71606|5|Briefly described|p135,137|Statherian|Orosirian|North Walker Trough, McArthur Basin. Arenitic sequence.||||Overlain by Habgood and Balma Groups and Parsons Range Group.||
27873|Parsons Range Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Quartzose sandstone; minor siltstone and dolostone.|
27873|Parsons Range Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Goyder Package.||||||
27873|Parsons Range Group|72377|5|Briefly described|p6,13, 15|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Rawlings et al (1997) suggested that Mount Bonner Sandstone and Jalma Formation may be attenuated lateral facies variants of the Parsons Range Group, deposited on the higher-relief flanks of the main depositional areas for this group.||||||10-OCT-19
27873|Parsons Range Group|72718|6|Mentioned|p5 Tb.1|||McArthur Basin. Calvert Superbasin of Jackson et al. (1999, 2000). Goyder package.||||Overlies Redbank package (Tawallah Group and correlates).||
33805|Pear Tree Dolostone|14019|3|Fully described|p7-8|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group. Supersedes the Pear Tree Dolomite. Dolarenite, dolorudite, dololutite, dolostone, mudstone. Conformably on Margery Formation; conformably overlain by Amos Knob Formation. Thickness: 92m. Geological Province: Birrindudu Basin.||||||07-NOV-08
33805|Pear Tree Dolostone|24122|5|Briefly described|p4 Fig.3|||Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33805|Pear Tree Dolostone|24297|5|Briefly described|p4 Fig.3|Proterozoic|Proterozoic|Of Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33805|Pear Tree Dolostone|24441|5|Briefly described|p1 Fig. 1|||Of the Limbunya Group. Overlies Margery Formation;  overlain by Amos Knob Formation. Geological Province: Birrindudu Basin.||||||25-JAN-06
33805|Pear Tree Dolostone|24442|5|Briefly described|p50 Fig. 1|||Of the Limbunya Group.  Geological Province: Birrindudu Basin.||||||
33805|Pear Tree Dolostone|60589|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Limbunya Group.  Dolarenite, dolorudite, dololutite, stromatolitic dolostone, dolomitic mudstone, minor carbonaceous mudstone; microbial chert at top.  Conformably overlies the Margery Formation; conformably underlies the Mallabah Dolostone.||||||07-NOV-08
33805|Pear Tree Dolostone|60672|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dolarenite, minor dolostone and sandstone. Of Limbunya Group. Overlain by Amos Knob Formation. Geological Province: Birrindudu Basin.||||||07-NOV-08
33805|Pear Tree Dolostone|60685|5|Briefly described|p4 Fig. 3|||Of the Limbunya Group. Geological Province: Birrindudu Basin.||||||
33805|Pear Tree Dolostone|65342|6|Mentioned|p11 Fig.13. |||Birrindudu Basin.||Unit in Limbunya Group.||Overlies Margery Formation. Is overlain by Amos Knob Formation.||
33805|Pear Tree Dolostone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Limbunya Group.||Overlies Margery Formation. Is overlain by Amos Knob Formation.|Dolostone.|
33805|Pear Tree Dolostone|68733|6|Mentioned|p177 Fig.2|||Birrindudu Basin.||Of the Limbunya Group.||||
33805|Pear Tree Dolostone|69429|6|Mentioned|p14:2 Fig.14.2|Paleoproterozoic|Paleoproterozoic|||Limbunya Group.||||12-JUL-16
33805|Pear Tree Dolostone|69432|5|Briefly described|p17:2, 7, 13|Paleoproterozoic|Paleoproterozoic|Birrindudu Basin. 80m thick. Upper part has anomalous Cu.||Limbunya Group.|||Intraclastic dolostone, dolomitic sandstone, silty dolostone, stromatolitic dolostone and oolitic dolostone in a coarsening-up-section succession. Basal cauliflower chert common. Distinctive stromatolites with a diamond-shaped horizontal section.|12-JUL-16
33805|Pear Tree Dolostone|69673|6|Mentioned|p48 fig 35|||||Limbunya Group||Overlies Margery Formation, overlain by Amos Knob Formation||
33805|Pear Tree Dolostone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Limbunya Group||Overlies Margery Formation. Is overlain by Amos Knob Formation.|Dolostone.|24-JAN-22
33805|Pear Tree Dolostone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Limbunya Group.||Is overlain by Amos Knob Formation.|Dolarenite, minor dolostone and sandstone.|
33805|Pear Tree Dolostone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dolarenite|
33805|Pear Tree Dolostone|71302|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of Birindudu Basin.||Unit of Limbunya Group.||Overlain by Amos Knob Formation. Underlain by Margery Formation.||
33805|Pear Tree Dolostone|72718|6|Mentioned|p7|||Birrindudu Basin.||Limbunyah Group||Underlain by Margery Formation. Overlain by Amos Knob Formation.||
41849|Peculiar Complex|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Part of the Madderns Yard Metamorphic Complex [?].   Age: 1679Ma.  Geological Province: Warumpi Province.||||||03-DEC-15
41849|Peculiar Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1680Ma. Rhyolite, schist, quratzite, sediments, leucogranite, granphyre. Of the Madderns Yard Metamorphic Complex [?]. Geological Province: Haasts Bluff Domain.||||||03-DEC-15
41849|Peculiar Complex|67565|2|Defined|p57, p8-9, p5 Fig.3, p30-31, p46|Statherian|Statherian|New unit. Warumpi Province. Outcrops as rocky hills; named after Mount Peculiar. Type locality is an outcrop of flow-banded rhyolite 10 km WNW of Mount Peculiar; thickness >200 m. Subaerial felsic ignimbrite and widespread granite intrusion constituted the Argilke Igneous Event, limited to the Haasts Bluff Domain. The leucogranite is geochemically similar to the rhyolite; interpreted as a subvolcanic intrusive. Previously included in undifferentiated gneiss, granite and other lithologies by Ranford (1969). Metamorphosed to lower to middle amphibolite facies during 1590-1560 Chewings Orogeny. Weakly magnetic; high K, moderate U and Th. Geochemistry is discussed. Age by Cross et al. (2004).|1680 +/- 4 Ma (SHRIMP U-Pb zircon).|||Is faulted against Lizard Schist and Talipata Granite. Is intruded by Udor Granite and Stuart Pass Dolerite. Is overlain unconformably by Heavitree Quartzite.|Flow-banded rhyolite, muscovite-quartz schist, minor porphyritic rhyolite, quartzite, biotite schist; discontinuous layers in rhyolite of laminated siliceous siltstone, calc-silicate rock, minor lithic arkose; fine-medium equigranular leucogranite.|01-DEC-15
41849|Peculiar Complex|68832|5|Briefly described|p19-20|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Crystallisation age of rhyolite sample. Felsic volcanic interval appears to be >200 m thick.|1680+/-4 Ma||||Dominated by flow-banded rhyolite, variably recrystallised to quartz-muscovite schist. The rhyolite is typically aphyric.|
41849|Peculiar Complex|69428|5|Briefly described|p13:3-5|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Haasts Bluff Domain, Warumpi Province. SHRIMP U-Pb zircon crystallisation age of rhyolite.|1680 +/- 4 Ma (Cross et al., 2005).||||Felsic volcanics (mainly flow-banded rhyolite variably recrystallised to quartz-muscovite schist), related shallow-level leucogranites, and minor banded (intercalated Fe- and Mn-rich sediments and quartz-rich sandstone) metasedimentary rocks.|12-JUL-16
27535|Pedestal beds|23621|4|Described|p36|Devonian|Devonian|See also Page 9 Table 1. Underlain by Gardiner Sandstone. In the Ord Basin. Max. thickness: >10 m.||||||22-NOV-06
27535|Pedestal beds|23622|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Ord Basin.||||||
27535|Pedestal beds|36335|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27535|Pedestal beds|43301|6|Mentioned|Map Legend||Paleozoic|age Devonian?||||||07-NOV-08
27535|Pedestal beds|43631|6|Mentioned|p27|||||||||
27535|Pedestal beds|45155|6|Mentioned|p42|||||||||
27535|Pedestal beds|61861|5|Briefly described|p4|Devonian|Devonian|Flat-lying siliciclastic rocks. Also mis-spelt as Pedestal Beds on same page.||||Overlies Antrim Plateau Volcanics, unconformably overlies Dead Bullock Formation.||03-APR-12
27535|Pedestal beds|62632|5|Briefly described|Map Legend|Paleozoic|Paleozoic|Sandstone, fine grained, planar bedded, laminated; conglomeratic sandstone, laminated, silicified, ferruginous; conglomerate.||||||07-NOV-08
27535|Pedestal beds|64675|6|Mentioned|p10|||See also Pedestal Beds||||||
27535|Pedestal beds|65074|4|Described|p350 fig 4-36, p351, p358-360, p362|Devonian|Devonian|Of North/Centre Birrindudu Basin. Appears as Pedestal Beds on p350. 500 m thick. Type area is in Macfarlanes Peak Range (NT). Non-fossiliferous.||||Possibly equivalent to Pertnjara Group (NT). Overlies (all unconformably) Lucas Formation, Tanami Complex, Redcliff Pound Group, Hidden Basin beds, Antrim Plateau Volcanics.|Quartz sandstone; minor conglomerate, shale, siltstone.|
27535|Pedestal beds|67163|5|Briefly described|Map legend.|Paleozoic|Paleozoic|||||Overlies Lucas beds.|Sandstone, fine-grained, planar-bedded, laminated; conglomeratic sandstone, laminated, silicified, ferruginous; conglomerate, well-rounded cobbles and pebbles, thickly bedded, graded.|19-OCT-11
27535|Pedestal beds|69288|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Also appears as Pedestal Beds.|||||Fine-grained, planar-bedded, laminated sandstone; laminated, silicified, ferruginous conglomeratic sandstone with beds 30cm - 1m thick; thickly-bedded, graded conglomerate with well rounded cobbles and pebbles.|
27535|Pedestal beds|69440|5|Briefly described|p25:2|Devonian|Devonian|Canning Basin.||||Unconformably overlies Erica Sandstone.||12-JUL-16
27535|Pedestal beds|69453|5|Briefly described|p37:1-2|||Lucas Outlier, Canning Basin. Up to 500m thick. Deformation (including E-plunging folds) occurred probably during the Alice Springs Orogeny.||||Unconformably overlies Antrim Plateau Volcanics; inferred to unconformably overlie Lucas Formation. Stratigraphically equivalent to Pertnjara Group.|Medium- to fine-grained, poorly sorted, thin to very thick quartz sandstone with isolated (stringers of) pebbles; interbedded with minor massive, pebble and cobble conglomerate, and shale.|12-JUL-16
27535|Pedestal beds|69673|5|Briefly described|p200|||Up to 500m thick.|||||Thin to very thick sandstone interbedded with minor conglomerate and shale.|
27535|Pedestal beds|70852|5|Briefly described|Map legend.|Paleozoic|Paleozoic|Canning Basin.|||||Quartz sandstone; minor conglomerate, siltstone, shale.|
27535|Pedestal beds|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.|||||Fine grained sandstone, planar bedded, laminated; conglomeratic sandstone with beds 30 cm-1 m;laminated, silicified, ferruginous; conglomerate, well rounded cobbles and pebbles, thickly bedded, graded.|
81900|Peko Smelter Porphyry|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1847+/-2.5 Ma crystallisation: U-Pb zircon SHRIMP||||Felsic porphyry.|
80195|Penyeme Orthogneiss|71839|6|Mentioned|p21-22||||ca 1793 Ma (Beyer et al., in prep)||||Orthogneiss.|22-MAR-23
24454|Peppimenarti Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Wagait Suite. Age: ~1850Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
24454|Peppimenarti Granite|41645|2|Defined|p26|Paleoproterozoic||||||||07-NOV-08
24454|Peppimenarti Granite|41646|6|Mentioned|Map legend|Paleoproterozoic||Biotite leucogranite; adamellite; porphyritic, microgranite.||||||07-NOV-08
24454|Peppimenarti Granite|41980|5|Briefly described|Table 3 P575|||||||||
24454|Peppimenarti Granite|50586|5|Briefly described|p1.1, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Wagait Suite.||||||07-NOV-08
24454|Peppimenarti Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Biotite leucogranite, adamellite, porphyritic microgranite.||||||07-JAN-09
24454|Peppimenarti Granite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Wagait Suite.|||Coarse biotite-hornblende granite, fine biotite granite.|
24454|Peppimenarti Granite|69420|5|Briefly described|p5:18, 28-29|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Wagait Suite.|||Dominated by coarse-grained, massive and equigranular monzogranite to granite, with some aplite and pegmatite phases present, suggesting late-stage evolution of a magmatic phase. Saussuritisation and chloritisation of biotite are common.|12-JUL-16
24454|Peppimenarti Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
24455|Perenti Metamorphics|23732|6|Mentioned|p3, p27|||Geological Province: Arunta Province.||||||
24455|Perenti Metamorphics|23868|6|Mentioned|p741|||Geological Province: Arunta Inlier.||||||
24455|Perenti Metamorphics|40538|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24455|Perenti Metamorphics|40906|2|Defined|p56|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24455|Perenti Metamorphics|50369|6|Mentioned|p9.2, 15.2|||Intruded by Dneiper Granite, Mount Swan Granite.||||||
24455|Perenti Metamorphics|69427|5|Briefly described|p12:8, 12, 39|||Shaw et al. (1984). Aileron Province. Metamorphic grade, estimated at up to 4 kbar, decreases to the W.|||||Layered felsic granulite and quartz-sillimanite-biotite-cordierite rock with minor calc-silicate rock and metadolerite.|20-SEP-19
24455|Perenti Metamorphics|69925|6|Mentioned|p21|||||||Is intruded by Mount Swan Granite.||
24455|Perenti Metamorphics|71750|4|Described|iii,p1,6-10,13,20|Statherian|Orosirian|Geological province: Aileron Province. Occur as a series of isolated outcrops surrounded and intruded by Dneiper and Mount Swan granites. Likely to have similar provenance to Kanandra and Deep Bore metamorphics based on similarities and provenance spectra and max depositional ages (Claou¿-Long and Hoatson 2005; Kositcin et al 2014, 2015); broadly representing the same sedimentary package at different metamorphic grades. Sample: GA23066966 (NTGS HU15BLR957) (506852E 7515521N) zircon analysis yields maximum depositional age of 1817+\-17 Ma; |1817+/-7 Ma max depositional age|||Intruded by Dneiper Graniteand Mount Swan Granite.|Layered felsic granulite and quartz- sillimanite-biotite-cordierite rocks with minor calc-sillimanite rock and metadolerite.|20-SEP-19
24455|Perenti Metamorphics|72516|6|Mentioned|p192|||Aileron Province. Minimum depositional age based on igneous crystallisation age of intruding Dneiper Granite (1771 +/- 6 Ma, Zhao and Bennett 1995) and Mount Swan Granite (1713 +/- 7 Ma, Zhao and Bennett 1995)||||Intruded by the Dneiper Granite and the Mount Swan Granite. Possible age equivalent to Bonya Metamorphics.||27-MAY-21
24455|Perenti Metamorphics|73591|5|Briefly described|piv, p2, p31-32|||Aileron Province. Occur as a series of isolated outcrops surrounded by the Mount Swan and Dneiper granites and as xenoliths in the former. Youngest detrital zircon population of Kositcin et al. (2018) were analysed for Lu-Hf isotopes yielding a wide range of values.|||||Layered felsic granulite and quartz-sillimanite-biotite-cordierite rocks with minor calc-silicate rocks and metadolerite.|
22644|Perta Hill Metamorphics|9199|5|Briefly described|Map legend|Precambrian|Precambrian|Of the Hayes Complex.  Epidote-diopside-plagioclase gneiss.  Geological Province: Arunta Block.||||||03-NOV-04
22644|Perta Hill Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Of the Hayes Complex. Geological Province: Arunta Block. Epidote-diopside-plagioclase gneiss.||||||22-NOV-06
39866|Petermann Nappe Complex|24442|5|Briefly described|p29|||Geological Province: Amadeus Basin.||||||
39866|Petermann Nappe Complex|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
39866|Petermann Nappe Complex|61154|5|Briefly described|p2, p22 Fig. 16|||Name refers to a structural subdomain on the northwestern margin of the Musgrave Block.  See also p33.||||||
39866|Petermann Nappe Complex|69003|5|Briefly described|p67|||Northern Petermann Orogen. Comprises discrete upper crustal shear zones with low-grade synorogenic metamorphism (<640 oC; <650 MPa).||||||
39866|Petermann Nappe Complex|69091|5|Briefly described|p79, p88, p145|||Mapped in the Northern Territory.|590 Ma to 560 Ma|||||
39866|Petermann Nappe Complex|69436|4|Described|p21:3, 17-20|||Western Mulga Park Domain. A 200km wide,  internally duplexed basement-cored wedge, consisting of interleaved basement and basal Amadeus Basin sedimentary rocks, that has been thrust northwards during the Petermann Orogeny. Described in detail.||||||12-JUL-16
39866|Petermann Nappe Complex|73437|6|Mentioned|p153, p157, p160, p162|||Contains rocks of the Musgrave region interleaved with the basal sedimentary sequence of the Aamadeus Basin during the Petermann Orogeny. Lower greenschist facies in northern part. Characterised by structures of foreland fold and thrust belts. Zircon (U-Th)/He cooling ages of 546+/-52 Ma and 531+/-72 Ma from northern end. Apatite fission track ages of 388-271 Ma indicate cooling, exhumation during latest stage of the Alice Springs Orogeny.||||||
30513|Phelp Sandstone|23404|5|Briefly described|p645|||||||||
30513|Phelp Sandstone|23937|2|Defined|p90 App. 1, p26|Calymmian|Calymmian|Of the Collara Subgroup (Roper Group).  Conformably overlain by Mantungula Formation; disconformably overlies Nathan Group.  Age: ~1500Ma.  Max. thickness: 80m. Geological Province: McArthur Basin.||||||18-APR-05
30513|Phelp Sandstone|24050|6|Mentioned|p42|||||||||
30513|Phelp Sandstone|24303|5|Briefly described|p28|Mesoproterozoic|Mesoproterozoic|Geological Province: McArthur Basin. Correlative of Gleeson Formation. See also p24 Tb. 4||||||
30513|Phelp Sandstone|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Quartz sandstone, medium to thick bedded, fine- to medium-grained; minor siltstone; chert-clast breccia and conglomerate present in outcrops south of Roper River. Overlies the Nathan Group; underlies Mantungula Formation.||||||15-FEB-05
30513|Phelp Sandstone|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Collara Subgroup. Quartz sandstone: medium to thick bedded, fine to medium grained; minor siltstone; chert-clast breccia and conglomerate.||||||
30513|Phelp Sandstone|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|NW Roper River region, NW McArthur Basin. <40-80m thick. Fluvial and shallow-marine sediments.||Basal Collara Subgroup.||Unconformably overlies Nathan Group. Is overlain conformably by Mantungula Formation.|White quartz sandstone and siltstone; minor conglomerate and breccia.|12-JUL-16
30513|Phelp Sandstone|70734|5|Briefly described|p16 Fig. 2|||McArthur Basin. Tidal platform sandstone.||||Overlain by Mantungula Formation.||
30513|Phelp Sandstone|70822|5|Briefly described|p102 fig 1 (A)|Mesoproterozoic|Mesoproterozoic|||Roper Group.||Overlain by Mantungula Formation; unconformably overlies Nathan Group.|Sandstone.|
30513|Phelp Sandstone|70968|2|Defined|p6-11, p124, p126-129, p131, p138-140|Calymmian|Calymmian|See also p143-144. Sweet in Abbott et al. (2001). Originally mapped by Dunn (1963) as part of Kookaburra Creek Formation (now Nathan Group); also as part of Mantungula Formation. Named after Phelp River. 75m thick at the type section which is the interval from 502600mE 8446000mN (base) to 502400mE 8446000mN in ROPER RIVER sheet. Forms strike ridges and scattered low pavements of sandstone and conglomerate. Mapped as Mantungula Formation locally (described). Represents basal Roper Group locally. Lithology described in detail. Detrital zircon diagram.||Collara Subgroup.||Unconformably or disconformably overlies Nathan Group. Is overlain conformably by Mantungula Formation. Locally underlies Vizard Group (thrust contact). Equivalent to Gleeson Formation.|White quartz sandstone, locally grading laterally into coarse conglomerate and sedimentary breccia; lesser shale and minor conglomerate.|
30513|Phelp Sandstone|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. <45-75m thick. Shallow-marine shelf, possibly some fluvial, deposits.||Collara Subgroup.||Unconformably overlies Nathan Group. Is overlain conformably by Mantungula Formation.|Quartz sandstone, siltstone, conglomerate, breccia.|
30513|Phelp Sandstone|71488|5|Briefly described|p141 fig 1b|||||Collara Subgroup||Overlain by the Mantungula Formation.||
30513|Phelp Sandstone|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Collara Subgroup||||24-SEP-18
30513|Phelp Sandstone|71893|4|Described|iii, p2-p4, p8-p13|Calymmian|Calymmian|McArthur Basin. Deposited in a shallow marine to possibly fluvial environments. Sample locality is described. The maximum age is constrained by a date of 1589+/- 3 Ma from the underlying Nathan Group and a minimum age of 1492 +/- 4 Ma from the Mainoru Formation. Zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided.|1760 +/- 8 Ma (Max dep. U-Pb-Hf)|Collara Subgroup||Unconformably overlies the Walmudga Formation (Nathan Group). Conformably overlain by the Mantungula Formation.|Quartz sandstone and siltstone, minor conglomerate and breccia.|
30513|Phelp Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone (partial) and southwestern McArthur Basin (partial).||Collara Subgroup, Roper Group||Partly underlain by Walmudga Formation (Nathan Group) and upper Balbirini Dolostone unconformably. Overlain by Mantungula Formation.||
30513|Phelp Sandstone|73242|5|Briefly described|p39|||||Collara Subgroup, Roper Group||Underlain by Mount Rigg Group[?] and Nathan Group[?]. Overlain by Mantungula Formation.|Includes tidal Sandstone.|24-JAN-23
77799|Phoenix Orthogneiss|68997|4|Described|vi-vii,p1,8-10|Orosirian|Orosirian|Emplaced during Stafford event, based on 1802+\-6 Ma tonalite precursor (northeastern ALCOOTA): zircon age from sample of tonalitic orthogneiss (Sample: AC09CJE389. Grid Reference: MGA94 Zone 53: 488321mE 7527241mN).|1802+\-6 Ma (U-Pb zircon)||||Tonalitic orthogneiss. Mineral assemblage: quartz, plagioclase, clinopyroxene, hornblende and a distinctive granular pink titanite.|
77799|Phoenix Orthogneiss|69917|5|Briefly described|p91-93, 1|Paleoproterozoic|Paleoproterozoic|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. 1802+/-6 Ma  is interpreted as the magmatic crystallisation age of the igneous precursor to the gneiss.|||||Tonalitic orthogneiss.|
77799|Phoenix Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1802+/-7 Ma (U-Pb zircon SHRIMP)||||Orthogneiss.|
26103|Pine Hill Formation|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Cordierite granulite, Felsic granulite, Garnet-biotite gneiss, Calc-silicate rock, Quartzofeldspathic garnet gneiss.||||||
26103|Pine Hill Formation|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Reynolds Range Group (Geological Province: Arunta Block). Biotite muscovite schist, muscovite schist, quartz rich metasediment.||||||
26103|Pine Hill Formation|11884|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Lower Proterozoic age. Minimum age constrained by the intruding Napperby Granite.|> ca. 1800-1500 Ma|Of the Reynolds Range Group.|Includes Algamba Dolomite Member.|Intruded by the Napperby Granite; overlies (and interleaves with ?) Mount Thomas Quartzite; interleaved with Woodforde River Beds ?|Silimanite-biotite-cordierite-quartz granofels, metaquartzite, calc-silicate rock.|
26103|Pine Hill Formation|23270|5|Briefly described|Table 1, p6||Proterozoic|In the Arunta Block (Division 3). Of the Reynolds Range Group.||||||23-NOV-06
26103|Pine Hill Formation|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block (Division Three). Age: Early or Middle Proterozoic.||||||23-NOV-06
26103|Pine Hill Formation|24047|6|Mentioned|p36|||||||||
26103|Pine Hill Formation|32480|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26103|Pine Hill Formation|35221|4|Described|Table.1|||||||||
26103|Pine Hill Formation|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26103|Pine Hill Formation|38896|6|Mentioned|Table 1|||||||||
26103|Pine Hill Formation|39855|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26103|Pine Hill Formation|39887|6|Mentioned|Fig.5|||||||||
26103|Pine Hill Formation|42217|6|Mentioned|p415|||||||||
26103|Pine Hill Formation|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
26103|Pine Hill Formation|43631|3|Fully described|p11,12|||||||||
26103|Pine Hill Formation|43749|6|Mentioned|Fig.1,p6||Paleoproterozoic|||||||07-NOV-08
26103|Pine Hill Formation|44158|4|Described|p9, Table.1|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Age: 1820 - 1780 Ma. Conformable on Mount Thomas Quartzite.||||||05-MAY-10
26103|Pine Hill Formation|48992|2|Defined|p43|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
26103|Pine Hill Formation|50369|5|Briefly described|p5.1, 7.3|||Intruded by Warimbi granite, Napperby Gneiss.||||||
26103|Pine Hill Formation|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex. Metamorphosed sandstone and siltstone, pelitic schist, minor clacareous rocks and metabasalt.||||||07-NOV-08
26103|Pine Hill Formation|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Quartzite, pelitic and psammitic andalusite schist, minor calc-silicate and basalt.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
26103|Pine Hill Formation|62378|6|Mentioned|p33|||Of the Reynolds Range Group.||||||
26103|Pine Hill Formation|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Of the Reynolds Range Group. Muscovite schist, muscovite biotite schist, muscovite biotite andalusite schist, amphibolite, minor calc-silicate.||||||07-NOV-08
26103|Pine Hill Formation|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.||Of Reynolds Range Group.|||Quartzite, pelitic and psammitic andalusite schist, minor.|15-APR-11
26103|Pine Hill Formation|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Geological Province: Arunta Region - Aileron Province. Biotite-muscovite schist. muscovite/haematite/feldspar-bearing quartz arenite.||||||07-NOV-08
26103|Pine Hill Formation|64737|5|Briefly described|p235 Tab.2, p238, p243||Orosirian|Dating of detrital zircons defines maximum deposition. Equivalent to part of the Reynolds Range Group.|1832+/-20 Ma U-Pb SHRIMP.|||||11-JUL-16
26103|Pine Hill Formation|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group.Sandstone and siltstone, pelitic schist, minor calcareous rocks and metabasealt; low to medium linear magnetic response||||||
26103|Pine Hill Formation|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group. Sandstone and siltstone, pelitic schist, minor calcareous rocks and metabasealt; low to medium linear magnetic response||||||
26103|Pine Hill Formation|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Of Reynolds Range Group. Muscovite, +/-biotite, +/-andalusite schist, amphibolite, minor calc-silicate||||||
26103|Pine Hill Formation|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Reynolds Range Group, Aileron Province; overlies Mount Thomas Quartzite. Consists of quartzite, pelitic and psammitic andalusite schist, minor calc-silicate and basalt.||||||
26103|Pine Hill Formation|65338|4|Described|p7, pp20-21.|||Outcrop of these rocks is confined to southwestern MOUNT PEAKE area. Represents deeper-water, offshore sedimentation by comparison with Mount Thomas Quartzite.||Unit in Reynolds Range Group.|Includes Algamba Dolostone Member.|Conformably overlies Mount Thomas Quartzite or forms a meta-pelitic lens within it.|Biotite-muscovite schist and variably muscovite-, haematite- and feldspar-bearing quartz arenite; minor interlayered mafic rocks: metabasalt lavas.|
26103|Pine Hill Formation|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Reynolds Range Group.||Overlies Mount Thomas Quartzite.|Biotite-muscovite schist, muscovite/haematite/feldspar-bearing quartz arenite.|
26103|Pine Hill Formation|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Reynolds Range Group.||Overlies Mount Thomas Quartzite.|Biotite-muscovite schist, muscovite/haematite/feldspar-bearing quartz arenite.|
26103|Pine Hill Formation|69427|4|Described|p12:25, 32, 41, 64|||SE Reynolds Range, Aileron Province. Age of Group ~1780 Ma.||Reynolds Range Group.|Algamba Dolostone Member.|Overlies, and interfingers with, Mount Thomas Quartzite. Is intruded by Napperby Gneiss and Wabudali Granite.|Metapelitic rocks; lesser meta-sandstone, calc-silicate and basalt (with local flow-banding, amygdaloidal, up to 30m thick). Andalusite porphyroblasts occur in the Wabudali Granite metamorphic aureole.|22-SEP-18
26103|Pine Hill Formation|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Another five age determinations are given within the range of ~1586-1562 Ma, confusingly presented as Reynolds Range Group/Pine Hill FZ(Mt Freeling Schist).|1585+/-3 Ma to 1557+/-2 Ma (metamorphism).|Reynolds Range Group.|||Amphibolite- to granulite-facies metapelite, migmatitic granulite, pelitic gneiss.|
26103|Pine Hill Formation|71858|6|Mentioned|p6|||Aileron Province.||Reynolds Range Group||||
26103|Pine Hill Formation|73399|5|Briefly described|p2-7, p9, App.C|Statherian|Statherian|Metamorphic grade ranges from sub-greenschist to granulite within the Reynolds Ranges. This was investigated using phase equilibria models [see article]. May have undergone a single, long-lived (190 Myr) metamorphic event.|1800-1785 Ma|Reynolds Range Group|||Includes fine-grained muscovite-chlorite-quartz slate, interlayered with psammite with a changing mineral assemblage and leucosomes appearing at higher metamorphic grades.|
81855|Pinnacle Gneiss|72516|6|Mentioned|p79|Cambrian|Neoproterozoic|New units incorporated into the Harts Range Metamorphic Complex by Whelan et al (in prep). Age from Harts Range Metamorphic Complex.||Harts Range Metamorphic Complex||||06-MAY-20
42376|Pinpirnga Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province.|||||Equigranular, medium grained biotite granite|09-SEP-19
81901|Pipeline Granite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1802+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Biotite-hornblende tonalite.|
39078|Pitjantjatjara Supersuite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes: Pottoyu Suite, Amputjuta Dacite, Manturrur and Umutju Suites, Walal Granite, Kulpitjata Suite, Ayers Range Granite, Kulgera Granite and the Umbeara granites.  Age: 1190-1120Ma. Geological Province: Musgrave Block.||||||
39078|Pitjantjatjara Supersuite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Age: 1190-1120 Ma. Predominantly granites with some other similar rocks. Geological Province: Musgrave Block.||||||14-JAN-05
39078|Pitjantjatjara Supersuite|61154|2|Defined|p42 App., p9, p26-27|Mesoproterozoic|Mesoproterozoic|Comprises extensive suites of geochemically related granite bodies: Pottoyu, Umutju, and Kulpitjata Suites, Ayers Range and Kulgera Granites, Mantarurr Suite, Wala Granite(NT); and, Ernabella Adamellite suite, Ngarinya Adamellite(SA).  Age: ~1190-1120Ma.||||||03-AUG-05
39078|Pitjantjatjara Supersuite|61524|5|Briefly described|p16, p17 Fig.1, p18 Fig.2(a)|Mesoproterozoic|Mesoproterozoic|Felsic intrusives - alkali granite to diorite, almost exclusively charnockite in mapping area; undeformed to strongly deformed. Intrudes Birksgate Complex. Previously known as the Kulgara Suite. Age: 1170-1120Ma. Geological Province: Musgrave Province.||||||03-MAY-13
39078|Pitjantjatjara Supersuite|61864|5|Briefly described|p18, p19 fig 5|||Part of the basement of Musgrave Province. Associated with Musgravian Orogeny.|||||Granitic plutons; charnockitic and microgranite compositions.|
39078|Pitjantjatjara Supersuite|63224|5|Briefly described|p9||Mesoproterozoic|Elongated intrusive bodies. Geological Province: Beadell Province.||||||07-FEB-08
39078|Pitjantjatjara Supersuite|63776|6|Mentioned|p1089|Mesoproterozoic|Mesoproterozoic|Age: 1200-1140Ma. Voluminous granites.||||||
39078|Pitjantjatjara Supersuite|63864|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: c. 1155Ma or 1186-1164Ma. Charnockite; orthopyroxene-clinopyroxene metamonzogranite weakly, strongly and massively foliated. See map legend for more information.||||||
39078|Pitjantjatjara Supersuite|63866|5|Briefly described|p202, p206-p207|||Musgrave Province. Previously known as the Kulgera Supersuite.|c. 1190-1120 Ma||Includes the Pottoyu Suite, Umutju Suite, Walal Granite, Kulgera Granite, Umbeara Granite, Mantarurr Suite and the Kulpitjata Suite.||Alkali granite to diorite and extensive biotite granite gneiss.|
39078|Pitjantjatjara Supersuite|64408|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Two dates shown: 1171-1180 Ma, 1194-1215 Ma. Not clear what was dated. Subdivided into 2 named & 11 unnamed units. Geol.  Province - Musgrave Complex.||||||16-SEP-08
39078|Pitjantjatjara Supersuite|64645|5|Briefly described|p16 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: 1200 - 1140Ma. Geological Province: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p17, 27|Stenian|Stenian|Of the Musgrave Orogen. Syn- to post-tectonic. Has within-plate, A-type affinities. Subjected to amphibolite-granulite facies metamorphism.|U-Pb zircon ages of ~1200-1120 Ma.||||Granite to diorite composition.|11-APR-12
39078|Pitjantjatjara Supersuite|64745|5|Briefly described|p375, p370, p373 Fig. 3, p374 Tab.1|||Voluminous emplacement of granitic rocks: adamellite to diorite composition, commonly porphyritic. A-type granites. Age: ca. 1.12 - 1.14Ga (U-Pb SHRIMP). Geol. Prov: Musgrave Province.||||||
39078|Pitjantjatjara Supersuite|64831|5|Briefly described|p1128 Fig. 2, p1129 Fig.3|Mesoproterozoic|Mesoproterozoic|Granitoid plutons ranging from alkali granite to quartz diorite in composition; contains microgranite and charnockite bodies. Magmatism was active from ca 1200Ma to 1150Ma (SHRIMP). See also pages 1130, 1135.||||||10-FEB-09
39078|Pitjantjatjara Supersuite|65135|4|Described|p1, p6 Fig.4, p12-13, p12 Fig.8, p16-18|Stenian|Ectasian|Most abundant in the northeast of west Musgrave Complex, but only forms small plutons and dykes in the southwest. Voluminous A-type granites. Broadly charnockitic. Metamorphosed to granulite facies. Preserves rapakivi textures in low strain zones. Divided into 2 main age groups: 1219-1200 and 1190-1155 Ma. Syn- to post-tectonic. Intruded by Alcurra Dolerite.||||||
39078|Pitjantjatjara Supersuite|65376|6|Mentioned|p9 Fig.1.2. |Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|65385|5|Briefly described|pS131 Tab.2, pS132|Stenian|Stenian|Synorogenic granites. Of Musgrave Province. Intruded Birksgate Complex between 1190-1120 Ma.||||||08-MAR-12
39078|Pitjantjatjara Supersuite|65693|6|Mentioned|p3 Fig.1.|||Includes mafic dykes dated c.1149 Ma.||||||
39078|Pitjantjatjara Supersuite|65833|5|Briefly described|p1, p6 Fig.4, p12 Fig.8, p12-13, p16-18|Stenian|Stenian|Voluminous A-type granites. Rapakivi textured. Primary mineralogy includes orthopyroxene, pyroxene and biotite. Syn- to post-tectonic (Musgravian Orogeny); granulite facies metamorphism. Two major episodes of magmatism and metamorphism: 1219-1200 Ma and 1190-1155 Ma. Dated granites range from 1219 +/- 12 Ma (Bodorkos et al., 2008) to 1164 +/- 10 Ma (GSWA preliminary data). Mafic dykes intrude Musgrave Complex.||||||
39078|Pitjantjatjara Supersuite|65898|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Authors separate this into 2 unnamed Early (1219-1190 Ma), 4 unnamed Late (1190-1155 Ma) units and an ungrouped ?younger unit. Metagranites and gneiss. Also misspelt on Interpreted Bedrock Geology Figure as Pitjantjatjarra Supersuite.||||||
39078|Pitjantjatjara Supersuite|65906|6|Mentioned|p3, p5|Mesoproterozoic|Mesoproterozoic|Large proportion of outcrop in Musgrave Block. Age: 1220-1140 Ma. Produced by magmatism associated with the Musgravian Orogeny. Diorite to monzonite; within-plate, A-type affinities.||||||
39078|Pitjantjatjara Supersuite|65907|5|Briefly described|p5, p10, p13, pp26-27.|||Syn- to post-tectonic granitic intrusions; A type; metamorphosed to granulite facies. Two distinct age groups, defining Early and Late Musgravian Orogeny. |c.1219-1200 Ma, and c.1190-1155 Ma.|||||
39078|Pitjantjatjara Supersuite|66256|4|Described|p4 Fig.3, p6, p8-11, p13, see comments|Stenian|Ectasian|In west Musgrave Province. Edgoose et al. (2004) grouped syn- to post-tectonic granite magmas (of Musgrave Orogeny) into Pitjantjatjara Supersuite. Supersuite can be subdivided into eight suites based on geochemical similarities within groups of similar age and limited geographical extent. All rocks have been recrystallized at granulite facies. Granite geochemistry (whole-rock geochemical, Nd and Hf isotopic analyses) provided. Geochron (SHRIMP) results for crystallisation and metamorphic ages detailed. See also  p15-18, p23 Figs.20&21, p24-32, p34-47, p53-54 App.1, p71 App.4.|||Mirturtu, Ilurpa, Walpa, Waratjarra, Pirntirri, Punuwarra, Tjuni Purlka, Kapi-Parra suites.||3 granite groups: monzodiorite to alkali-feldspar granite; locally schlieric, biotite-orthopyroxene monzogranite to syenogranite; locally derived anatectic melts - highly leucocratic sheets and veins; depleted in REE and HFSE, enriched in LILE.|11-JAN-17
39078|Pitjantjatjara Supersuite|66280|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Divided on map into early (c.1219-1190 Ma, monzodiorite; leucogranite) and late (c.1190-1155 Ma, leucogranite; syenogranite; more) Pitjantjatjara Supersuite as well as several mapped but unnamed units of metagranite and gneiss.||||||
39078|Pitjantjatjara Supersuite|66281|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metamonzogranites, granodiorites, metaleucogranites, metasyenogranites, mylonitic granitic rock.|
39078|Pitjantjatjara Supersuite|66282|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Metagranite and gneiss. Mapped as eleven lithologically-different but un-named units.|||||Weakly to strongly foliated metamorphosd monzogranite, syenogranite, porphyritic leucogranite, granofels, leucosyenogranite.|
39078|Pitjantjatjara Supersuite|66284|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Includes an early and a late phase, separated by Mirturtu Monzogranite; and 13 separately-mapped but un-named units.|c.1219 - 1155 Ma.||Includes Umutju Granite.||Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|66526|5|Briefly described|p35.|Proterozoic|Proterozoic|Granitic rocks. They include a dated gabbro intrusion and associated mafic granulite produced in the Pitjantjatjara Event, ME 22 in the Proterozoic Mafic-Ultramafic Magmatic Event Series.|c.1180 Ma.|||||
39078|Pitjantjatjara Supersuite|67128|5|Briefly described|p5 Fig.3, p6-8, p15|||Walpa Pulka Zone, western Musgrave Province. Voluminous A-type felsic and minor mafic magmatism associated with the c.1220-1150 Ma Musgravian Orogeny.|c.1220-1150 Ma.|||Is overlain unconformably by MacDougall Formation.|Typically K-feldspar porphyritic granite plutons with ultra high-T metamorphic assemblages; local schlieric biotite-orthopyroxene leucogranites.|
39078|Pitjantjatjara Supersuite|67244|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as four separate but un-named sub-units. Informally grouped into an unnamed unit and an older 'Late Pitjantjatjara Supersuite' (1190-1150) grouping of 3 unnamed units.|>1150 Ma.||||Metagranodiorite intercalated with pelitic gneiss and olivine gabbro; mylonitic, seriate to porphyritic metagranitic rock; foliated biotite-hornblende metasyenogranite with locally abundant xenoliths of felsic gneiss.|01-MAY-15
39078|Pitjantjatjara Supersuite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Musgrave Block.|~1190-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|67372|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Mapped as no fewer than 40 separate but un-named (except for the 2 units comprising the Mirturtu Suite) units.|1220 - 1150 Ma.||Includes Mirtutu Suite.||40 mapped units of variably-metamorphosed leucogranite, granodiorite, monzogranite, syenogranite, granite, olivine gabbro, monzodiorite and charnockite; pelitic gneiss; mafic granulite.|02-DEC-13
39078|Pitjantjatjara Supersuite|67375|3|Fully described|p6,Fig.5, p15, pp26-32, p58, pp150-213.|Mesoproterozoic|Mesoproterozoic|Of Edgoose et el. (2004); formerly the Kulgera Suite of Major and Conor (1993). Incorporates all igneous rocks formed during the Musgrave Orogeny, and anatectic melts as young as 1121 +/- 11 Ma resulting from high-grade metamorphism in the late stages of the Musgrave Orogeny. Most granites are metaluminous, K-rich, A-type. Enormous amounts of granitic magma, covering half the entire Musgrave Province. Most have been metamorphosed to granulite-facies, and range from statically recrystallized and unfoliated to strongly foliated and mylonitized. Is intruded by a tubular-shaped mafic-ultramafic chonolith which hosts the world-class Nebo-Babel Ni-Cu-PGE sulfide orebody.|1219 +/- 12 Ma - 1148 +/- 6 Ma.||Includes Tjuni Purlka Suite. Encloses xenoliths and rafts of Wirku Metamorphics. Intrudes Wankanki Supersuite.||Three groups: monzodiorite to alkali-feldspar granite dykes and small plutons; schlieric biotite-orthopyroxene leucogranite veins and sheets; locally derived anatectic melts, typically with granofelsic textures. Rare leucogabbro and norite.|
39078|Pitjantjatjara Supersuite|67536|5|Briefly described|Map Legend|Ectasian|Stenian|Musgrave Block. Informally subdivided into two parts. Possibly occurs in the Beadell Province as elliptical non-magnetic to weakly magnetic intrusive bodies, some with magnetic rims and N-trending magnetic lineations.|ca. 1200 - 1175 Ma ?||||Granitoid plutons and phases of larger plutons, non-magnetic to moderately magnetic; granitoid plutons, massive to internally zoned, including intrusive charnockite, strongly magnetic.|
39078|Pitjantjatjara Supersuite|67553|4|Described|p8-9,11-12,16-17,19-20-34,39,59,61|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province, North Australian Craton. High-K granitic plutons, dominant within the Walpa Pulka Zone, and covers roughly half of the entire Musgrave Province. Calc-alkaline to alkaline calcic 'charnockitic' magmatism at 1220-1150 Ma (Close et al., 2003; and GSWA data). Based on SHRIMP U-Pb geochronology, this can subdivided into two groups,  Early and Late Musgravian granites reflecting magmatism and metamorphism c. 1220 and 1200 Ma and c. 1190 and 1155 Ma respectively. Oldest and youngest Early Musgravian granites dated at 1219+\-12 Ma (GSWA 174737) and 1157+\-9 Ma (GSWA 189254) respectively. Most granites in the Mamutjarra Zone have late Musgravian intrusive ages between 1189+\-11 Ma (GSWA 184147, Kirkland et al., 2009d) and 1148+\-6 Ma (GSWA 189522, Kirkland et al., in prep.).  Granites in the Yjuni Purlka zone include deformed early Mugsgravian granites, similar Mamutjarra Late musgravian granites and schlieric biotite-orthopyroxene leucogranites ranging from 1210+\-10 Ma (GSWA 185339, Kirkland et al., 2009e) to 1165+\-10 Ma (GSWA 183509, Kirkland et al., 2008c). Most rocks metamorphosed to granulite-facies conditions late in Musgrave Orogeny and during Giles Event. Exhumation during Petermann Orogeny exposed deep metamorphic assemblages. Subdivisible into three main lithological components (see p28-30). See also p67,70-71,73-75,78,82,95 for general field trip notes.|1220-1150 Ma||Includes Mamut, Mirtutu, Kapi-Parra, Waratjarra, Pirntirri, Ilurpa, Walpa Punuwarra and Tjuni Purlka suites.||Monzodiorite to alkali-feldspar granite, locally schlieric biotite-orthopyroxene leucogranites (monzogranite to syenogranite) and locally derived anatectic melts forming highly leucocratic sheets and veins, typically with granofelsic textures.|
39078|Pitjantjatjara Supersuite|67581|6|Mentioned|p44 Fig.8|||||||||
39078|Pitjantjatjara Supersuite|68077|5|Briefly described|p3 Fig.1, p4-6, p11-14, p18-19, p30|Mesoproterozoic|Mesoproterozoic|See also p32-38. The Musgrave Orogeny produced these extensive, >1000 oC granites. Forms a sheet up to 5km thick. Isotopic composition (Lu-Hf and Sm-Nd) and evolution tabulated and discussed in detail.|1219-1180 Ma (U-Pb zircon)||||Charnockitic and locally rapakivi-textured granites, ferroan and typically alkali-calcic; pegmatites, metagranite, metagranodiorite, monzodiorite, gabbro and dolerite.|07-SEP-17
39078|Pitjantjatjara Supersuite|68100|5|Briefly described|p2, 3, 4-5, 7-9, 12,14,15,16,24-29,33,34|Mesoproterozoic|Mesoproterozoic|Leucogranites appear as magnetic lows. Metamorphosed to granulite facies ~1080-1030 Ma (Giles Event).|1220-1150 Ma||||K-feldspar porphyritic granites and minor mafic rocks. The granites are primarily anhydrous charnockites. Anatectic, garnetiferous, mylonitic leucogranites; gabbro.|19-JAN-17
39078|Pitjantjatjara Supersuite|68131|5|Briefly described|p2 Fig.1|Mesoproterozoic|Mesoproterozoic||||||Granitic rocks.|
39078|Pitjantjatjara Supersuite|68995|5|Briefly described|p2, p5, p6, p48, p50, p51 Tb. 4, p65|Stenian|Ectasian|Intruded during the Musgrave Orogeny. Interpreted to be mostly derived from a mantle source based on isotopic concentrations and thermal limits of intrusion.|c.1220-1150 Ma|||Unconformably overlain by the Kunmarnara Group.|Orthopyroxene-bearing and locally rapikivi textured granites.|
39078|Pitjantjatjara Supersuite|68996|5|Briefly described|p3, 4, 24-25, 28-30,35-49, 54, 59|Mesoproterozoic|Mesoproterozoic|Musgrave Orogeny granites. Densities range from 2.57-3.25g/cm^3|1220-1155 Ma||||High grade granitic gneisses and charnockites. Chemistry suggests within-plate, A-type magmatism.|
39078|Pitjantjatjara Supersuite|68998|6|Mentioned|p31|||Musgrave Province. Mentioned as a significant source of zircons in the Mount Eclipse Sandstone.||||||
39078|Pitjantjatjara Supersuite|69003|5|Briefly described|p4, p37-39, p42-43, p45, p51|Mesoproterozoic|Mesoproterozoic|W Musgrave Province, Paterson Orogen. Associated with the 1220-1150 Ma Musgrave Orogeny.|1220-1150 Ma.||Tjuni Purlka suite.||Voluminous, anhydrous, orthopyroxene-bearing felsic magmatic rocks; mainly composite plutons ranging from monzodiorite through to alkali-feldspar granite, including significant rapakivi granite. Mafic rocks are extremely rare.|
39078|Pitjantjatjara Supersuite|69009|5|Briefly described|Map Legend|Stenian||Musgrave Province.|> 1078 Ma||||Comprises metagranite and gneiss.|03-APR-14
39078|Pitjantjatjara Supersuite|69091|4|Described|p52 Fig.4.1, p53, see comments|Mesoproterozoic|Mesoproterozoic|Formed during 1220-1150 Ma Musgrave Orogeny. West Musgrave Province. Mount West Orogeny and Musgrave Orogeny, including mixed with Wankanki Supersuite (Fig.4.3). In Wannarn area, Kunmarnara Group are interleaved with felsic basement, including granulite facies metagranites of Pitjantjatjara Supersuite. See also p54-56, p59 Fig.4.6, p64-67, p82-83, p85-88, p103 Fig.5.6, p105-107, p109 Fig.5.10, p113-115, p117 Fig.5.15, p119 Fig.5.16, p121, p131-132, p137-139 Figs.6.4-6.6, p141-142, p151, p183-184, p206.|1220-1150 Ma||Tjuni Purlka, Kapi-Parra, Mamut, Mirturtu, Pirntirri, Ilurpa and Waratjarra suites; Pottoyu Granite Suite.|Is unconformably overlain by Kunmarnara and Tjauwata Groups.|High-K granite plutons; most metamorphosed granulite-facies; granites range from statically recrystallised and unfoliated, to strongly foliated and mylonitised; includes high-grade granitic gneisses and charnockites; suggests A-type magmatism.|
39078|Pitjantjatjara Supersuite|69153|5|Briefly described|GEOL_LUT_CSV files;GEOCHRON/194637.1.pdf|Mesoproterozoic|Mesoproterozoic|Paterson Orogen, Musgrave Province. Some of this unit is divided into subparts: Pitjantjatjara Supersuite 1 and Pitjantjatjara Supersuite 2. Age mentioned in GEOCHRON/194637.1.pdf.|1220-1150 Ma, Smithies et al., 2010||Umutju Granite (in sub-part Pitjantjatjara Supersuite 2)||Metagranodiorite, metasyenogranite, metamonzogranite, granitic schist, granitic granofels/hornfels, mafic granulite, granitic gneiss;  intercalated with, intruded by, and included in other granitic rocks|
39078|Pitjantjatjara Supersuite|69203|5|Briefly described|p59|||Musgrave Province.|c.1190-1120 Ma.||||Voluminous I-type magmatism.|
39078|Pitjantjatjara Supersuite|69213|6|Mentioned|p36, p35|||Musgrave Province.|~1200-1140 Ma||||Anhydrous charnockites.|
39078|Pitjantjatjara Supersuite|69383|6|Mentioned|p74, 77|||Musgrave Province.|1190-1120 Ma|||||
39078|Pitjantjatjara Supersuite|69417|6|Mentioned|p2:10|Mesoproterozoic|Mesoproterozoic|Granitoids, interpreted to have formed by the extensional Musgrave Orogeny.||||||12-JUL-16
39078|Pitjantjatjara Supersuite|69436|4|Described|p21:1-2, 4-10, 15-18, 21|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Voluminous widespread syn- to post-tectonic granitic magmatism, synchronous with the Musgrave Orogeny (1220-1150 Ma). Extensively reworked by the Petermann Orogeny with pervasive biotite foliation. Peak metamorphic assemblages include biotite-epidote-muscovite +/- garnet. Three metamorphic zircon rims have ages between 574 +/- 5 Ma and 568 +/- 12 Ma. Has some potential for iron oxide-Cu-Au deposits.|1220-1120 Ma.||Pottoyu, Umutju, Mantarurr, Kulpitjata Suites; Walal, Ayers Range, Kulgera Granites.||Comprises extensive Suites of geochemically related granite bodies, from diorite to granite, generally subalkaline and predominantly ultrapotassic, although some are high-K calc-alkaline types. Metaluminous I-type.|12-JUL-16
39078|Pitjantjatjara Supersuite|69640|4|Described|p11-p12, p15, p23-p24, p27|Proterozoic|Proterozoic|Musgrave Province. Petrology, petrographic description, SHRIMP methodology, results and analayses for numerous samples are provided. Additional magmatic crystallisation ages of 1147 +/- 11 Ma,1147 +/- 16 Ma, 1143 +/- 9 Ma,  1143 +/- 8 Ma, 1155 +/- 14 Ma and 1152 +/- 9 Ma were obtained by SHRIMP. Also includes medium-grained equigranular granite with pegmatite with a rough ca 1140 Ma magmatic age and a biotite micro-syenogranite dyke dated at 1154 +/- 9 Ma. See also  p32, p50, p82, p88, p94, p100, p107, p115, p122, p130, p137, p141, p145, p148, p152, p157, p164, p174, p190, p207, p214.|1564 +/- 5 Ma (SHRIMP, magmatic crystallisation)|||Intruded by the Alcurra and Kullal dolerites. Intrudes the Birksgate Complex.|Anatectic granites, plutonic A type porphyritic granites and late crosscutting microgranitic and aplitic dykes. Porphyritic biotite monzogranite,  biotite monzogranite dykes, biotite micro-monzogranite,  monzodiorite.|
39078|Pitjantjatjara Supersuite|69655|5|Briefly described|p3, p5-p7, p9, p37|Stenian|Ectasian|See also p39, p44, p57-p58, p66, p77-p78. Musgrave Province. Musgrave Orogeny.|c. 1220-1150 Ma||||Orthopyroxene-bearing and locally rapakivi granites.|
39078|Pitjantjatjara Supersuite|69729|4|Described|p66-70, p74-78, p84-85, p87-88, p90|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (2004). Musgrave Province. Emplaced during the Musgrave Orogeny. Geochemistry detailed. UHT conditions discussed.|1220-1150 Ma.|||Cross-cuts and encloses Wirku Metamorphics and Wankanki Supersuite.|Almost exclusively felsic, high-temperature, anhydrous, A-type, high-K, granulite facies metagranites.|
39078|Pitjantjatjara Supersuite|69917|5|Briefly described|p115|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Granites of  1190-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|69937|5|Briefly described|vi, p7, p9, p12, p19, p22, p27, p31|||Musgrave Province. One of the sediment sources for the Amadeus Basin.|1220-1120 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|70083|6|Mentioned|p204, 206-208, 226, 229, 231-232|||Musgrave Inlier. Associated with widespread amphibolite-granulite facies metamorphism of the Musgrave Orogeny. Magnetic anomalies support a connection with contemporaneous Nornalup Complex granites (Albany-Fraser Orogen) and Teapot [Granite Complex] granites (Warumpi Province).|~1220-1140 Ma.||||Voluminous A-type felsic magmatic rocks: felsic granitoids and microgranitic dykes.|
39078|Pitjantjatjara Supersuite|70084|4|Described|p219-225,228-229|Stenian|Ectasian|Geological province: Musgrave Province, Paterson Orogen. Associated with Musgrave Orogeny, coeval with emplacement of Esperance Supersuite and Gnowangerup Fraser Dyke Suite in the Albany-Fraser Orogen. Voluminous granitic magmatism accompanied by UHT metamorphic conditions (associated with unusually thin crust and extreme geothermal gradients), and one of the largest exposed UHT belts on Earth. Granitic composition described from Smithies et al., 2011. Lies within a single, narrow, Nd and Hf-isotopic evolution band with TDM2 values within a range of 2.2-1.6 Ga, together with the Wankanki, Papulankutja and Warlawurru supersuites, reflecting reworking of juvenile crust between ca. 2.0 and 1.6 Ga (Kirkland et al., 2013a). Mid-crustal accummulation of high Th, U and K-rich granites resulted in slow post-Musgrave Orogeny thermal decline, consistent with prolonged migmatite events (Smithies et al., 2014a).|1220-1150 Ma||||Almost exclusively felsic, anhydrous, A-type granites (ferroan, typically alkali-calcic (high-K) and range in silica content from 56.8 to 78.0 wt%, with very high concentrations of both TiO2 and P2O5 and enrichments in REE, HFSE, Th, and U.|
39078|Pitjantjatjara Supersuite|70134|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|||||Metagranite and gneiss (section only).|
39078|Pitjantjatjara Supersuite|70338|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Part of the basement of the Musgrave Province. Seven facies are mapped separately. Lithologies are described in a little more detail.|||||Undivided: adamellite, alkali granite, diorite. Micromonzogranite to microsyenogranite; microsyenogranite; syenogranite to quartz-monzodiorite; metasyenogranite to metaquartz-monzodiorite; monzogranite to syenogranite: porphyritic or equigranular.|07-JAN-16
39078|Pitjantjatjara Supersuite|70383|6|Mentioned|p51|Stenian|Stenian|Musgrave Province. Mentioned as a possible source of zircons aged c.1178 +/- 15 Ma, extracted from the Sprigg Diamictite Member.||||||
39078|Pitjantjatjara Supersuite|70619|5|Briefly described|map legend|Mesoproterozoic|Mesoproterozoic|Musgrave Province.|1219-1148 Ma||||Metagranite and gneiss.|
39078|Pitjantjatjara Supersuite|70634|4|Described|100k_geologyp_lut,csv|Mesoproterozoic|Mesoproterozoic|Musgrave Province/(Complex?), SHRIMP dates obtained from samples (file 174558.1.pdf,   194802.1.pdf)|1134Ma (SHRIMP) -   1215 Ma (SHRIMP)|Musgrave Complex|Includes Mirturtu Suite, Umutju Granite, Mirturtu Monzongranite Suite|Intruded by Warakurna Supersuite|Hornblende--biotite--pyroxene metasyenogranite and metamonzogranite, leucogabbro, quartz diorite, feldspar porphyritic charnockite.|
39078|Pitjantjatjara Supersuite|70748|6|Mentioned|p15, p50|||Musgrave Province. Similar in age to the Eyre 1 granite.||||||25-SEP-18
39078|Pitjantjatjara Supersuite|70749|5|Briefly described|p50-51|||Emplaced during the Musgrave Orogeny.|||||Widespread and voluminous felsic intrusions.|
39078|Pitjantjatjara Supersuite|70763|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Associated with the Musgrave Orogeny. Three facies are mapped separately.|1219-1148 Ma.||||Three facies mapped separately: metagranite and gneiss; hornblende-biotite metamonzogranite and biotite-hornblende metamonzogranite, both well-foliated to gneissic, garnet-bearing, locally migmatitic.|
39078|Pitjantjatjara Supersuite|70778|6|Mentioned|p21|||Musgrave Province. Emplaced during the Musgrave Orogeny.||||||
39078|Pitjantjatjara Supersuite|70793|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Sample GSWA 174558 (quartz diorite) yielded an interpreted igneous crystallisation age of 1145+\-12 Ma (weighted mean 207Pb*/206Pb*). Sample GSWA 174594 (metaleucograbbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1190+\9 Ma. Sample GSWA 174736 (granofelsic metasyenogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\7 Ma. Sample GSWA 174737 (foliated metamonzogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1219+\12 Ma, and metamorphic zircon rim growth at 1171+\-12 MA. Sample GSWA 174747 (metagabbro) yielded an interpreted (weighted mean 207Pb*/206Pb*) maximum igneous crystallisation age of 1205+\-24 Ma, and metamorphic zircon rim growth at 1214+\-7 Ma. Sample GSWA 180262 (mylonitic synogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1180+\-4 Ma. Sample GSWA 180270 (metamonzogranite dyke) yielded an interpreted (weighted mean 207Pb*/206Pb*) igneous crystallisation age of 1183+\-9 Ma. Sample GSWA 180860 (metamonzogranite) yielded an interpreted (concordia) igneous crystallisation age of 1159+\-13 Ma. Sample GSWA 183459 (charnockite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1178+\-12 Ma. Sample GSWA 183509 (leucogranite) yielded an interpreted (weighted mean 207Pb*/206Pb*) magmatic crystallisation age of 1165+\-10 Ma. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 100k_interpgeol_lut.csv, 500k_interpgeop_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv + geochron files for more geochronological sample analyses.|1219+\-12 Ma; 1148+\-6 Ma||Includes Mirturtu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Intruded by Warakurna Supersuite. Intrudes into Wirku Metamorphics.|Mafic granulite, granitic gneiss, metasyenogranite and metamonzogranite, granulite, metagranite and gneiss, leucocratic syenogranite, metaleucosyenogranite.|
39078|Pitjantjatjara Supersuite|70826|6|Mentioned|p10|Mesoproterozoic|Mesoproterozoic|Musgrave Province. ||||||
39078|Pitjantjatjara Supersuite|70831|5|Briefly described|p1, p3-p4, p6, p9, p13-p15, p20-p21, p23|Stenian|Ectasian|Musgrave Province. Average mineralogy is discussed. Petrography of constituent samples is discussed.|c. 1220-1150 Ma||||Well-foliated to gneissic, garnet-bearing, biotite-hornlende metamonzogranites.|
39078|Pitjantjatjara Supersuite|70839|5|Briefly described|p326-327,332,334,339-341,345|Stenian|Ectasian|Geological province: Musgrave Province. Dominates the Musgrave Province in outcrop. Emplaced between c. 1.22 and 1.15 Ga during Musgrave Orogeny (Smithies et al., 2011).|c. 1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|70968|5|Briefly described|p130|||Mentioned as possible source of detrital zircons in post-Roper Group units in greater McArthur Basin.|1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|71088|5|Briefly described|p2, p4-p5, p7, p10, p25|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during the Musgrave Orogeny; an extensional and intracontinental event characterised by ultra-high temperatures.|1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71143|5|Briefly described|p433,437|||Geological province: Musgrave Province. Similar age and composition to orthopyroxene- and pigeonite-bearing monzogabbro to monzodiorite rocks found from the Moodini Supersuite in the Madura Province (includes juvenile mantle input).||||||
39078|Pitjantjatjara Supersuite|71169|6|Mentioned|p82|Stenian|Ectasian|Musgrave Province. |1220-1120 Ma|||||
39078|Pitjantjatjara Supersuite|71170|5|Briefly described|xi-xii, p5-p6, p9, p42-p43|Mesoproterozoic|Mesoproterozoic|Musgrave Orogen. Emplaced at high temperatures (>900c). See also p45, p65-p67, p109, p145, p147.|1220-1150 Ma (Smithies et al, 2010)||||Charnockitic, A-type granitic rocks.|
39078|Pitjantjatjara Supersuite|71210|6|Mentioned|p4-p5, p7-p8, p21, p23, p51, p53|||Musgrave Province. See also p66-p67, p69, p78-p82, p86, p95-p97, p99, p113. Also appears as Pitjantjatjara Supergroup p8.||||Overlain by the Kunmarnara Group.||
39078|Pitjantjatjara Supersuite|71211|5|Briefly described|p6, p7 fig 1.4, p9, p24 fig 2.1|||Musgrave Province. See also p84 fig 3.1, p104, p106, p107, p136 fig 4.1 , p230. |1220-1150 Ma||||Granites.|
39078|Pitjantjatjara Supersuite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
39078|Pitjantjatjara Supersuite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). Metamorphosed to granulite facies, with garnet-biotite rims around zircons indicating cooling post-peak metamorphism. Sample GSWA 174558 (mesocratic quartz diorite) yielded a weighted mean 207Pb/206Pb date of 1215+\-13 Ma, interpreted as the igneous crystallization age of the quartz diorite. Sample GSWA 174594 (plagioclase leucogabbro) yielded a weighted mean 207Pb/206Pb date of 1190+\-9 Ma, interpreted as the igneous crystallization age of the leucogabbro. Sample GSWA 174736 (granofelsic metasyenogranite) yielded a weighted mean 207Pb/206Pb date of 1180+\-7 Ma, interpreted as the igneous crystallization age of the syenite. Sample GSWA 174737 (foliated monzogranite) hosts the syenite, and is dated at 1219+\-12 Ma, and contains metamorphic zircon growths at 1171+\-12 Ma. These relationships suggest that syenogranite emplacement was broadly synchronous with the high-grade metamorphic event that affected the host monzogranite. Sample GSWA 180262 (mylonitic syenogranite) yielded a weighted mean 207Pb/206Pb age of 1180+\-4 Ma, interpreted as age of igneous crystallization of the precursor syenogranite. Sample GSWA 184146 (monzogranite) yielded a concordia age of 1201+\-6 Ma, interpreted as magmatic crystallsiation age. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 100k_interpgeol_lut.csv, 100k_geologyl_lut.csv, 250k_interpgeol_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1219-1148 Ma (inferred)||Includes Permano Adamellite, Mirtutu Suite, Pottoyu Granite Suite, Umutju Granite Suite.|Overlain by Tjauwata Group.|Granite, monzogranite, monzonite, granodiorite. Includes metagranodiorite, metamonzogranite, gneissic porphyritic leucogranite, medium-grained mafic granulite, granitic gneiss, metasyenogranite.|
39078|Pitjantjatjara Supersuite|71302|5|Briefly described|p75|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Voluminous granitic magmatism at c. 1220-1120 Ma.||||||
39078|Pitjantjatjara Supersuite|71321|4|Described|p1-2,4-5,10,14,17-19,21,24|Stenian|Stenian|Geological province: Musgrave Province. Voluminous, felsic, A-type granitoids synchronous with, and post-dating Birksgate Complex deformation during c. 1155 Ma Musgravian Orogeny. Form several large plutonic bodies distributed over TIEYON and dominate the basement outcrop exposure of the map sheet. Plutons also show magmatic foliation as a result of Musgravian Orogeny. Also contains locally developed, ductile to brittle structures (i.e. mylonites, schistosity, and joints) which may be attributed to Neoproterozoic-Cambrian Petermann Orogeny. Broadly grouped into 3 suites based on lithology, geochemistry and field relationships; anatectic granite suite, plutonic granite suite (intrudes into anatectic suite) and microgranite dyke suite (intrudes into both anatectic and microgranite suites). See p18-22 for detailed lithological and petrographic descriptions and field relationships in outcrop. See p40-49 for detail geochemistry breakdown and analysis. Plutons emplaced between c. 1155-1143 Ma (average c. 1148.1+\-2.4 Ma). Anatectic granite suite may have been produced by melting of Birksgate Complex basement rocks. Nd isotopic analysis indicate the anatectic and porphyritic granitic suites overlap in isotopic signatures with the Birksgate Complex, while the microgranitic suite is the most evolved. Hf isotopic analysis indicate reworking of older Birksgate crust with addition of new juvenile mantle material, while the microgranite suite reflects mixing of evolved Archean source with juvenile Birksgate basement. Contains anomalous hydrothermal related Ag-REE mineralisation. See also p32-36,38,40-50,55-56,60-64,66,74.|c. 1155-1143 Ma|||Intrudes into Birksate Complex.|Adamellite; alkali granite; diorite; often porphyritic, foliated or even massive.|24-OCT-19
39078|Pitjantjatjara Supersuite|71322|5|Briefly described|p11, p26, p33|||Musgrave Province. Age range c.1220-1150 Ma, with ultra-high temperatures persisting to c.1120 Ma. Metamorphosed at 1156 +/- 9 Ma.|1219 +/- 9 Ma (SHRIMP).||||Includes charnockitic granite.|13-DEC-21
39078|Pitjantjatjara Supersuite|71415|6|Mentioned|p16|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province.||||||19-AUG-19
39078|Pitjantjatjara Supersuite|71416|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Solid geology interpretation: monzogranite to syenogranite plutons; early stage moderately to strongly magnetic, massive to weakly foliated, mainly medium-grained, equigranular to sparsely K-feldspar-phyric, commonly leucocratic; late stage strongly magnetic, massive to weakly foliated, medium- to coarse-grained, porphyritic. SHRIMP U-Pb zircon magmatic crystallisation age.|c.1150 Ma (Dutch et al., 2013).||||Porphyritic granite to monzonite, biotite and/or hornblende, rare clinopyroxene, locally inequigranular.|
39078|Pitjantjatjara Supersuite|71536|5|Briefly described|p1, p71, p73, p78|Stenian|Stenian|SHRIMP age derived from this volume and interpreted as the magmatic age of a felsic gneiss from this supersuite.|1143 +/- 9 Ma (U-Pb SHRIMP)||||Peraluminous granite derived from melting of a pre-existing sedimentary rock (probably Birksgate Complex).|
39078|Pitjantjatjara Supersuite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1190+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Metamorphosed leucogabbro, metagabbro, monzogranite, pegmatite, quartz monzodiorite, syenogranite, monzonite, granite, coarse-grained leucogranite, charnockite, granoblastic garnetiferous granite, biotite-hornblende granite.|
39078|Pitjantjatjara Supersuite|71800|5|Briefly described|p29|Mesoproterozoic|Mesoproterozoic|Musgrave Province. The probable source of sediments in the Officer and Amadeus basins on the basis of geochronology.|1.22-1.15 GA|||||
39078|Pitjantjatjara Supersuite|71893|5|Briefly described|p44, p48, p51|||Musgrave Province.|ca. 1220-1120|||||
39078|Pitjantjatjara Supersuite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1219+/-12 Ma, min age 1148+/-6 Ma.||Includes Umutju Granite Suite, Pottoyu Granite Suite, and informal Pitjantjatjara Supersuite 1, Pitjantjatjara Supersuite 2.||Metagranite and gneiss. Mylonitic and blastomylonitic, seriate to porphyritic granitic rock. Mylonitic, medium-grained, porphyritic metamonzogranite; K-feldspar phenocrysts up to 2 cm.|
39078|Pitjantjatjara Supersuite|72094|5|Briefly described|p2, p3, p6, 12, 13, 14, p15-16|Stenian|Ectasian|Musgrave Province. Emplacement associated with Musgrave Orogeny, which metamorphosed Warlawurru, Papulankutja, Wankanki supersuites and Wirku Metamorphics to UHT (Edgoose et al., 2004; Smithies et al., 2010). Summary table of zircon geochronology on p8 Table 1 showing ages ranging from 1171+/-4 Ma to 1157+/-9 Ma.|1219-1148 Ma|||Tectonically interleaved with Kunmarnara Group along with Warlawurru Supersuite.|Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|72238|5|Briefly described|p36, 38|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Includes 1.15 Ga granites. Intruded by Amata Dolerite.|||Includes Wallaby Rock pluton, crosscut by Amata Dolerite.|||17-SEP-19
39078|Pitjantjatjara Supersuite|72242|5|Briefly described|p27|Stenian|Stenian|Geological province: Musgrave Province. Associated with Maralinga Event (including Musgrave Orogeny). Coeval with Moodini Supersuite.||||||
39078|Pitjantjatjara Supersuite|72443|5|Briefly described|p736-737, p747-748, p753, p758|Mesoproterozoic|Mesoproterozoic|Produced by the Musgrave Orogeny. Intrudes the  exposed mid-crust of the entire 1220-1150 Ma period. Interpreted to have been emplaced at temperatures of up to 1000 degrees C and coincided with a 100 Myr period of UHT metamorphism.|1220-1150 Ma||||Ferroan, alkali-calcic granites.|
39078|Pitjantjatjara Supersuite|72476|5|Briefly described|p25|||Eastern Musgrave Province.|1190-1120 Ma.||||Abundant high temperature granites.|
39078|Pitjantjatjara Supersuite|72934|6|Mentioned|p11-12|||Musgrave Province.|||||May include A-type granite intrusions.|
39078|Pitjantjatjara Supersuite|73058|5|Briefly described|p761, p769, p771 Fig.5-6, p773-776|Stenian|Ectasian|Musgrave Province. Ferroan and typically alkali-calcic granites, extreme enrichments in REE and HFSE. Intruded almost continuously throughout the Musgrave Orogeny as voluminous, high-temperature, anhydrous granites in mid-crustal regions, source dominated by new mantle additions. Hf and Nd model ages suggest mantle extraction event at c. 1900 Ma. Inferred additional significant juvenile mantle additions are masked in Hf isotope record by HFSE enriched crustal sources. Misspelt Pitjantatjara Supersuite p775. Location in text includes p772 Fig.8-9, p777 Fig.14.|c.1220-1150 Ma||||Includes orthopyroxene-bearing (charnockitic) and locally rapakivi-textured granites.|
39078|Pitjantjatjara Supersuite|73084|6|Mentioned|p12, p96, p98, p109, p124|Stenian|Ectasia|Musgrave Province. Similar in composition and age to the Moodini Supersuite and Esperance Supersuite. Part of a regionally extensive, high-temperature event named the Maralinga Event by Spaggiari et al. (2016).|1220-1150 Ma|||||
39078|Pitjantjatjara Supersuite|73177|5|Briefly described|p1100, 1114 Fig.16|||Musgrave Province.|c.1220-1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73225|5|Briefly described|p21|||Eastern Musgrave Province.|c.1155-1136 Ma.||||Granites.|
39078|Pitjantjatjara Supersuite|73232|6|Mentioned|p5, p12-14|Stenian|Ectasian|Musgrave Province. [Emplaced] during the Musgravian Orogeny. Deeply weathered, gradational boundary with overlying palaeovalley infill sediments in drillholes DH1a and S22i.|c. 1220-1120 Ma|||Intrudes Birksgate Complex. Intruded by Giles Complex including Alcurra Dolerite.|Includes granitic plutons.|
39078|Pitjantjatjara Supersuite|73234|6|Mentioned|p19|Stenian|Ectasian|Musgrave Province.|1220-1140 Ma||||Includes granites.|
39078|Pitjantjatjara Supersuite|73338|6|Mentioned|piii, p7|Stenian|Ectasian|Widespread throughout the Musgrave Province. Broadly coincident with the Musgrave Orogeny. Ages are of magmatic crystallisation. Dominant interval emplaced from 1180 Ma to 1140 Ma (Close 2013).|Ranges from 1220 Ma to 1120 Ma.|||||
39078|Pitjantjatjara Supersuite|73346|6|Mentioned|p2, p5-6, p24, p26|Stenian|Ectasian|Musgrave Province; dominates the province in outcrop. Produced during the 1219-1149 Ma Musgrave Orogeny.|1219-1149 Ma||||Includes granite.|
39078|Pitjantjatjara Supersuite|73437|5|Briefly described|p151, p153|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Emplaced during Musgrave Orogeny as voluminous mantle-derived granitic magmas.|1220-1150 Ma||||Metagranite and orthogneiss.|
39078|Pitjantjatjara Supersuite|74367|6|Mentioned|p23|||Musgrave Province.||||||
37727|Playford Sandstone|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Wild Cow Subgroup (South Nicholson Group).  Age: >1450Ma.||||||
37727|Playford Sandstone|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Wild Cow Subgroup. Very fine to medium and occasionally coarse grained sublithic to lithic sandstone; ferruginous sandstone; quartzose sandstone, shale, siltstone ans minor conglomerate, ironstone and carbonates.||||||22-AUG-06
37727|Playford Sandstone|65337|2|Defined|p9 Fig.5, pp37-42, pp96-97.|Mesoproterozoic|Mesoproterozoic|New name. East-central MOUNT DRUMMOND area. 390 - 1400 m thick; outcrops strongly as alternating strike ridges and narrow valleys. Lateral equivalent of Bowgan Sandstone.||Unit in Wild Cow Subgroup.|Includes Wangalinji, Top Lily Sandstone and No Mans Sandstone Members.|Disconformably or unconformably overlies Widdallion Sandstone Member. Is overlain by Crow Formation or Constance Sandstone.|Very coarse-grained basal quartz sandstone, overlain by interbedded laminated shale with thinly-bedded siltstone and lithic sandstone; coarse sandstone interbeds; thick and cross-bedded, lithic sandstone; minor ironstone and stromatolitic carbonates|
37727|Playford Sandstone|69434|4|Described|p19:2, 4-5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Composite thickness 390m to over 1400m. Forms alternating strike ridges and narrow valleys.||Wild Cow Subgroup.|No Mans, Top Lily, Sandstone Members; Wangalinji Member.|Is overlain conformably by Crow Formation. Lateral equivalent of Bowgan Sandstone.|Sublithic and quartzic sandstone, siltstone, granule sandstone and minor carbonate rocks.|12-JUL-16
37727|Playford Sandstone|69673|4|Described|p56|||Up to 1400m thick. Deposited in a range of increasingly shallow settings from a relatively deep basinal to shallow marine shelf and minor peritidal environments.||Wild Cow Subgroup|||Sublithic and quartzose sandstone, siltstone, granule sandstone and minor carbonate rocks.|
37727|Playford Sandstone|70968|6|Mentioned|p131 Fig.118|Calymmian|Calymmian|||Wild Cow Subgroup.||||
37727|Playford Sandstone|71369|5|Briefly described|p6, p8|||Rawlings et al. (2008). South Nicholson Basin.||Wild Cow Subgroup.|No Mans Member, Top Lily Sandstone Member, Wangalinji Sandstone Member.|||
37727|Playford Sandstone|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Wild Cow Subgroup|Includes  Wangalinji Member, Top Lily Sandstone Mmeber, No Mans Sandstone Member.|Shows as unconformably and partially overlying Fickling Group and Benmara Group and partially underlies Crow Formation.||
37727|Playford Sandstone|72527|3|Fully described|p1, p12, p20, p27, p34, p78, p140.|Mesoproterozoic|Mesoproterozoic|See also p193,  p195, p7 Fig.1.4.|c. 1820-1800 Ma|Wild Cow Subgroup|Wangalinji Member, Top Lily and No Mans Sandstone Members.|Unconformably overlies McNamara Group, underlies Crow Formation and is assumed to be equivalent to Bowgan Sandstone||
37727|Playford Sandstone|72912|4|Described|p5 Fig.3, p24-25, p31 Fig.11.|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin.||Wild Cow Subgroup|No Mans Sandstone Member, Top Lily Sandstone Member and Wangalinji Member.|Shown as overlying Fickling Group, underlies Crow Formation and is equivalent to Bowgan Sandstone.||
37727|Playford Sandstone|72919|6|Mentioned|p5, p24-25|Mesoproterozoic|Mesoproterozoic|||Wild Cow Subgroup, South Nicholson Group|No Mans Sandstone Member, Top Lily Sandstone Member, Wangalinji Member|Unconformably underlain by Widdallion Sandstone Member (McNamara Group). Overlain by Crow Formation. Equivalent to Bowgan Sandstone.||
37727|Playford Sandstone|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup, South Nicholson Group|No Mans Sandstone Member, Top Lily Sandstone Member, Wangalinji Member|Partly underlain by Doomadgee Formation. Overlain by Crow Formation.||
37959|Plenty Group|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Includes Amesbury Quartzite and Yackah beds.  Geological Province: southern Georgina Basin.||||||11-OCT-05
37959|Plenty Group|62642|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Georgina/Ngalia Basin.||||||
37959|Plenty Group|62983|6|Mentioned|p11|||Geological Province: Georgina Basin.||||||
37959|Plenty Group|64068|3|Fully described|p223 App 1, p164, 44, 35, 7|Cryogenian|Neoproterozoic|New name. Thickness to 350 m.|||Includes Yackah beds and Amesbury Quartzite.||Mainly fluviatile siliciclastic rocks; also stromatolitic carbonate and a hypersaline succession. Poorly sorted labile sediments indicate minimal transport.|14-JAN-16
37959|Plenty Group|65338|6|Mentioned|p59.||||||Includes Yackah beds and Amesbury Quartzite.|||
37959|Plenty Group|66767|5|Briefly described|p58|Cryogenian|Cryogenian|Georgina Basin. Up to 350m thick.||||Is overlain by Aroota Group.|Dominantly fluviatile siliciclastic rocks, with intertidal to shallow-marine stromatolitic carbonate and partially emergent, hypersaline, lacustrine to anoxic deep-marine successions.|
37959|Plenty Group|67164|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Georgina/Ngalia Basins.|||Includes Amesbury Quartzite and may include Vaughan Springs Quartzite.|||05-OCT-11
37959|Plenty Group|67892|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic||||Includes Amesbury Quartzite.|||
37959|Plenty Group|69437|5|Briefly described|p22:6|Cryogenian|Cryogenian|Southern Georgina Basin. Supersequence 1. |||Yackah beds, Amesbury Quartzite.|||12-JUL-16
37959|Plenty Group|69443|5|Briefly described|p28:2-3, 5-8, 30-31|Neoproterozoic|Neoproterozoic|Kruse in Dunster et al. (2007). Southern Georgina Basin.|||Yackah beds, Amesbury Quartzite.|Is overlain disconformably by Aroota Group. Correlated with Heavitree Quartzite and Bitter Springs Formation, and Vaughan Springs Quartzite and Albinia Formation.||12-JUL-16
37959|Plenty Group|69673|6|Mentioned|p111, p114 fig 92|Cryogenian|Cryogenian||||Includes Yackah beds, Amesbury Quartzite|||26-APR-22
37959|Plenty Group|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Yackah beds|Disconformably overlain by the Aroota Group. Unconformably overlies the Samarkand Pegmatite and the Jinka Granite.||
37959|Plenty Group|72516|5|Briefly described|p14, p21, p85-86, p135, p171, p176|Tonian|Tonian|Georgina Basin.|||Includes the Yackah beds.|||26-APR-22
37959|Plenty 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.||||||
26849|Point Spring Sandstone|7142|6|Mentioned|p350 Fig.4.|Late Carboniferous|Late Carboniferous|Browse Basin.||||Overlies Tanmurra Formation. Is overlain by Kulshill Group?.||20-SEP-14
26849|Point Spring Sandstone|12466|5|Briefly described|p177 Fig.10.|||||||Overlies Tanmurra Formation. Is overlain by Kuriyippi Formation.||03-SEP-14
26849|Point Spring Sandstone|13194|4|Described|p389 Tb. 4-16; p382, 402 figs 4-59,-66|Upper Carboniferous|Visean|Type Section: near Point Spring 15o24'S 128o57'E. 180-380m thick outcrop, but to 880m thick subsurface. Deltaic.||Weaber Group||Overlies Burvill Formation, Tanmurra Formation (both conformably). Part equivalent to Tanmurra Formation.|Sandstone and pebbly sandstone; minor siltstone.|
26849|Point Spring Sandstone|13234|6|Mentioned|p250 Fig.2,p262 Tb.2, |||Potential reservoir.||||Overlies Tanmurra Formation offshore.||
26849|Point Spring Sandstone|13354|6|Mentioned|p375 Fig.6.|Late Carboniferous|Late Carboniferous|Overlies Tanmurra Formation and underlies Kulshill Group of the Kinmore Group.||78||||28-OCT-14
26849|Point Spring Sandstone|22663|5|Briefly described|W97 8 to 10 fig.2||Carboniferous|||||||
26849|Point Spring Sandstone|23377|6|Mentioned|p212 Fig.5||Mississippian|In the Vulcan Sub-basin.||||||23-NOV-06
26849|Point Spring Sandstone|24390|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
26849|Point Spring Sandstone|24569|5|Briefly described|p248 Fig. 3|Westphalian|Namurian|Of the Weaber Group. Geological Province: Petrel Sub-basin.||||||02-MAR-05
26849|Point Spring Sandstone|32648|6|Mentioned|p32|||Namurian||||||
26849|Point Spring Sandstone|32662|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
26849|Point Spring Sandstone|32663|4|Described|Table 2|||L.Carb.||||||
26849|Point Spring Sandstone|32664|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|Briefly described in notes||||||
26849|Point Spring Sandstone|32870|5|Briefly described|p48|||||||||
26849|Point Spring Sandstone|34085|6|Mentioned|Cor.chart|||Visean - Namurian||||||
26849|Point Spring Sandstone|36257|6|Mentioned|Table 2.1|||||||||
26849|Point Spring Sandstone|36551|6|Mentioned|Table 16|||||||||
26849|Point Spring Sandstone|36890|3|Fully described|p381|||||||||
26849|Point Spring Sandstone|36904|6|Mentioned|p9|||||||||
26849|Point Spring Sandstone|40301|6|Mentioned|p7|||||||||
26849|Point Spring Sandstone|40993|6|Mentioned|Fig.1|||||||||
26849|Point Spring Sandstone|41532|6|Mentioned|p292|||||||||
26849|Point Spring Sandstone|41598|5|Briefly described|p413|||Mention p412.||||||23-NOV-06
26849|Point Spring Sandstone|41839|1|Redefined|p32|||||||||
26849|Point Spring Sandstone|41864|3|Fully described|p131|Westphalian|Visean|Unit probably diachronous.||||||
26849|Point Spring Sandstone|41865|5|Briefly described|Map legend|Westphalian|late Visean|||||||
26849|Point Spring Sandstone|41867|5|Briefly described|Map legend|Westphalian|late Visean|||||||
26849|Point Spring Sandstone|42055|4|Described|Fig.1 P52|||||||||
26849|Point Spring Sandstone|42056|6|Mentioned|p96|||||||||
26849|Point Spring Sandstone|42442|3|Fully described|p13|Namurian|Visean late|||||||
26849|Point Spring Sandstone|42547|4|Described|p103|||||||||
26849|Point Spring Sandstone|42994|6|Mentioned|p48|||||||||
26849|Point Spring Sandstone|44159|6|Mentioned|Table p.38||Early Carboniferous|||||||
26849|Point Spring Sandstone|44994|6|Mentioned|Fig.6|||See also p14. Correlation.||||||23-NOV-06
26849|Point Spring Sandstone|45038|2|Defined|p.107||Carboniferous|See also Plates and Figures. Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45039|6|Mentioned|p7|||See also pp26,27. Laower Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45050|6|Mentioned|p9|||See also pp12,17,19 etc.||||||23-NOV-06
26849|Point Spring Sandstone|45063|6|Mentioned|p8|||See also pp21, 27 & Fig. 3. L.-U. Carboniferous.||||||23-NOV-06
26849|Point Spring Sandstone|45097|6|Mentioned|p19|||Refers Thomas (1971). Correlation chart||||||
26849|Point Spring Sandstone|45169|4|Described|p6|||||||||
26849|Point Spring Sandstone|48635|14|Not recorded|p.20|||See Pl.1-sh1, Pl.2-sh.2, Fig.1. Upper Carboniferous? (D/52-10,11,14,15). p.1,5,9,10,17,22,23.||||||
26849|Point Spring Sandstone|48886|14|Not recorded|Map||Early Carboniferous|Lower Carboniferous.||||||
26849|Point Spring Sandstone|50085|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||
26849|Point Spring Sandstone|60006|5|Briefly described|Map Legend|Namurian|Namurian|Geological Province: Bonaparte Basin. Of the Weaber Group. (not recognised in Auvergne). Sandstone, conglomerate.||||||23-JUL-04
26849|Point Spring Sandstone|60364|5|Briefly described|p189|||Conformably overlies Burvill Formation. Geological Province: Bonaparte Basin.||||||11-MAY-05
26849|Point Spring Sandstone|60386|5|Briefly described|p291|Carboniferous|Carboniferous|Petrel Sub-basin.||||Unconformably overlain by Kuriyippi Formation||
26849|Point Spring Sandstone|60682|4|Described|p22 Table 5, 26|Carboniferous|Carboniferous|Of Weaber Group. Conformably overlies Burvill Formation. Previously mapped as Border Creek Formation. Max. thickness: >240m. Sandstone, conglomerate. Geological Province: Bonaparte Basin.||||||23-NOV-06
26849|Point Spring Sandstone|61023|5|Briefly described|p2 Fig. 2|Carboniferous|Carboniferous|Geological Province: Bonaparte Basin.||||||11-APR-08
26849|Point Spring Sandstone|61542|3|Fully described|p276, p277 Fig. 2, p286|Namurian|Namurian|Formerly part of Weaber Gp now revised as Wadeye Gp - as the onshore equivalent of Arco and Aquitaine Formations. Geological Province: Bonapart Basin/Petrel-Sub-basin. Sandstone and pebbly sandstone, siltstone, shale. More on interpretation included.||||||07-FEB-11
26849|Point Spring Sandstone|62837|5|Briefly described|Stratigraphic columns|Namurian|Namurian|Of the Weaber Group.  Age: ~322-~314Ma. Geological Province:  Petrel Sub-basin (offshore).||||||
26849|Point Spring Sandstone|64580|6|Mentioned|map legend|||Of Weaber Group.||||||15-DEC-08
26849|Point Spring Sandstone|64694|5|Briefly described|p234 Fig.2, p235 Fig.3, p238 Tb.1|Serpukhovian|Serpukhovian|See also p241, p245 Fig.9. Onshore Bonaparte Basin. Appears as Point Spring Formation on p242.||Unit in Weaber Group.||Overlies Burvill and Tanmurra Formations. Is overlain by Kuriyippi Formation.||
26849|Point Spring Sandstone|65331|5|Briefly described|Map legend|Bashkirian|Serpukhovian|Of Bonaparte Basin. Of Weaber Group. Age shown as Namurian. Sandstone, conglomerate.||||||19-JUL-16
26849|Point Spring Sandstone|65382|6|Mentioned|p717 App. 2|Pennsylvanian|Pennsylvanian|Bonaparte Basin. 309 Ma at top. At the boundary of the S. ybertii and D. birkheadensis palynozones.||||||
26849|Point Spring Sandstone|67195|5|Briefly described|Appendix 2|||Bonaparte Basin.|||||Includes salmon pink medium-grained sandstone.|
26849|Point Spring Sandstone|67200|5|Briefly described|app 2 p8||||||||Medium grained sandstone.|
26849|Point Spring Sandstone|69099|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||04-AUG-15
26849|Point Spring Sandstone|69165|6|Mentioned|500k_geologyp08_lut.csv|Pennsylvanian|Mississippian|||Weaber Group||||
26849|Point Spring Sandstone|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
26849|Point Spring Sandstone|69452|5|Briefly described|p36:9, 12, 14, 17|Pennsylvanian|Mississippian|Formerly topmost unit in Weaber Group; since assigned to Wadeye Group by Gorter et al. (2005).||Wadeye Group.||Unconformably overlies Tanmurra Formation. Lateral equivalent of Arco and Aquitaine Formations (Wadeye Group).||23-SEP-18
26849|Point Spring Sandstone|69634|5|Briefly described|500k_geologyp08_lut.csv|Carboniferous|Carboniferous|||Unit of Weaber Group.||||
26849|Point Spring Sandstone|69673|6|Mentioned|p176 fig 146, p181|Carboniferous|Carboniferous|||||Overlies Tanmurra Formation, overlain by Kuriyippi Formation||
26849|Point Spring Sandstone|70206|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Bonaparte Basin. Not recognised in map area.||Weaber Group|Includes Border Creek Member.||Sandstone, conglomerate.|
26849|Point Spring Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv.||Unit of Wadeye Group.|||Quartz sandstone, minor conglomerate|
23916|Pollard Formation|5952|5|Briefly described|p214 Fig. 4, p215 Fig. 5, p221 Fig. 15|Late Triassic|Middle Triassic|Of Sahul Group. In figure, Fm = Formation. Geological Province: Bonaparte Basin.||||||01-MAR-10
23916|Pollard Formation|7142|6|Mentioned|p350 Fig.4.|Late Triassic|Middle Triassic|Browse Basin.||||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|13194|6|Mentioned|p386 Tb. 4-16|Carnian|Anisian|Type Section: Sahul Shoals 1 well (2355-3249m). Up to 832m thick open-marine shelf deposits.||Sahul Group||Overlies Osprey Formation (conformably). Overlain by Challis Formation (conformably).|Sandstone with interbedded shale; minor limestone.|
23916|Pollard Formation|13222|6|Mentioned|p229 Fig.2.|||||Unit in Sahul Group.||||
23916|Pollard Formation|13354|6|Mentioned|p375 Fig.6, p376 Fig.7.|Late Triassic|Middle Triassic|Bonaparte Basin. Unit of Sahul Group. Overlies Osprey Formation and underlies Challis Formation.||96||||28-OCT-14
23916|Pollard Formation|22663|5|Briefly described|AC97 1-4 Fig.4||Late Triassic|Of the Sahul Group.||||||01-MAR-10
23916|Pollard Formation|23377|6|Mentioned|p211|||In the Vulcan Sub-basin.||||||23-NOV-06
23916|Pollard Formation|23378|6|Mentioned|p180 Fig.2||Late Triassic|Of the Sahul Group. In the Vulcan Sub-basin.||||||23-NOV-06
23916|Pollard Formation|24171|5|Briefly described|p722 Fig. 3|Triassic|Triassic|Geological Province : Vulcan Sub-Basin.||||||01-MAR-10
23916|Pollard Formation|24207|5|Briefly described|p209 Fig. 5|Late Triassic|Middle Triassic|||||||
23916|Pollard Formation|41532|2|Defined|p301|Middle Triassic||||||||
23916|Pollard Formation|42053|4|Described|p37|||See also Fig.2 p29.||||||01-MAR-10
23916|Pollard Formation|42066|5|Briefly described|Fig.3 P199|||||||||
23916|Pollard Formation|42442|2|Defined|p22|Carnian|Anisian|Age: Middle to early Late Triassic (Anisian to Carnian)||||||23-NOV-06
23916|Pollard Formation|43826|6|Mentioned|Fig.2,p163||Middle Triassic|||||||01-MAR-10
23916|Pollard Formation|60634|6|Mentioned|p1168 Fig.3. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|61548|6|Mentioned|p480 Fig.3|Ladinian|Ladinian|Northern Bonaparte Basin.||||||
23916|Pollard Formation|61550|6|Mentioned|p495 Fig.2. |Late Triassic|Late Triassic|||Unit in Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|62837|5|Briefly described|Stratigraphic columns|Middle Triassic|Early Triassic|Of the Sahul Group.  Age: >240->230Ma. Geological Province:  Ashmore Platform, Vulcan Sub-basin, Londonderry High (all in Western Bonaparte Basin) and Sahul Platform (Northern Bonaparte Basin).||||||01-MAR-10
23916|Pollard Formation|63358|5|Briefly described|p4 Fig. 1.3|Carnian|Anisian|||||||01-MAR-10
23916|Pollard Formation|63929|6|Mentioned|p131 Fig.2.|Late Triassic|Middle Triassic|Ashmore Platform (east), Sahul Platform. Includes marine and non-marine sediments. Has a carbonate member at its base correlated with near the top of Locker Shale; represents a major marine highstand event across the North West Shelf.||||Overlies Osprey Formation. Is overlain by Challis Formation.||
23916|Pollard Formation|64689|6|Mentioned|p13 Fig.13|||||||Is overlain by Challis Formation, appears to overlie Mount Goodwin Limestone||
23916|Pollard Formation|66124|5|Briefly described|p171 Fig.2|Carnian|Anisian|Ashmore Platform (East). Marine. Underlies Challis Formation and overlies Osprey Formation.||||||17-AUG-18
23916|Pollard Formation|66187|5|Briefly described|p413 Fig.2|Late Triassic||Sahul Group. Underlies the Challis Formation, overlies the Osprey Formation. Mount Ashmore Dome.||||||
23916|Pollard Formation|67370|6|Mentioned|p313 Fig.2. |Triassic|Triassic|||||Overlies Osprey Formation.||
23916|Pollard Formation|68223|6|Mentioned|p178 Fig.3|Ladian|Ladian|||||||
23916|Pollard Formation|69297|6|Mentioned|p305|Carnian|Ladinian|Caswell, Barcoo and Seringapatam Sub-basins of the Browse Basin. ||Sahul Group||Overlies the Osprey Formation. Overlain by the Challis Formation.|Sandstone and siltstone.|
23916|Pollard Formation|69452|5|Briefly described|p36:15, 21|Triassic|Triassic|Bonaparte Basin.||Sahul Group.||Equivalent to upper part of Cape Londonderry Formation.||12-JUL-16
23916|Pollard Formation|69689|6|Mentioned|p16|Triassic|Triassic|Browse, Bonaparte Basins.||||||
23916|Pollard Formation|70061|5|Briefly described|Regional geology Fig.6-7.Vulcan Fig.2,p2|Norian|Anisian|||Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||12-JUL-16
23916|Pollard Formation|70064|5|Briefly described|Regional Fig. 6. Central: Fig.2|Norian|Ladinian|See also Northern: Fig.2. Yampi: Fig.2. Caswell-Barcoo Sub-basins, Browse Basin.||Sahul Group.||Overlies Osprey Formation. Is overlain by Challis Formation.||12-JUL-16
27881|Polly Conglomerate|22650|6|Mentioned|p 166|Devonian|Devonian|Of the Finke Group..||||||23-NOV-06
27881|Polly Conglomerate|22760|6|Mentioned|p340|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|22826|6|Mentioned|p576|Devonian|Devonian|||||||
27881|Polly Conglomerate|23858|5|Briefly described|p916|||Of Finke Group. Overlain by Langra Conglomerate. Geological Province: Amadeus Basin.||||||23-NOV-06
27881|Polly Conglomerate|30544|6|Mentioned|p51|||On map legend||||||
27881|Polly Conglomerate|31566|6|Mentioned|p244|||Devonian||||||
27881|Polly Conglomerate|31567|3|Fully described|p276|||||||||
27881|Polly Conglomerate|33832|6|Mentioned|p8|||Stratigraphy||||||
27881|Polly Conglomerate|33844|6|Mentioned|Table 1|||||||||
27881|Polly Conglomerate|33971|3|Fully described|p28|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|34580|4|Described|Table 1|||Devonian - Carboniferous||||||
27881|Polly Conglomerate|35102|6|Mentioned|Fig.17|||||||||
27881|Polly Conglomerate|43035|6|Mentioned|p23|||Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|44133|5|Briefly described|p44|Carboniferous?|Late Devonian|Of the Finke Group. Conformably overlies Mereenie Sandstone. Geological Province: Pedirka Basin.||||||
27881|Polly Conglomerate|44323|14|Not recorded|map legend|Carboniferous|Devonian|SG53-6. Dev-Carb. Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|44342|4|Described|p.7, Table 2|Carboniferous|Devonian|SG/53-5. Dev-Carbon.||||||
27881|Polly Conglomerate|44343|14|Not recorded|map legend|Carboniferous|Devonian|Devonian-Carbon.||||||
27881|Polly Conglomerate|44393|4|Described|p.3,7,8,Tb.1,Fig.1|Carboniferous|Devonian|Correlated with Pertnjara Group. Dev-Carb.||||||
27881|Polly Conglomerate|45041|4|Described|p104|||Devonian. Of the Finke Group.||||||23-NOV-06
27881|Polly Conglomerate|48865|2|Defined|p.3,4,Fig.29|Carboniferous|Devonian|Overlain by Langra Formation.||||||23-NOV-06
27881|Polly Conglomerate|48890|4|Described|p.51|Carboniferous|Devonian|See also Tb.2,Tb.3,Fig.4. Of the Finke Group.  Devonian to Carboniferous. Defn on Tech.File G/53-6.||||||23-NOV-06
27881|Polly Conglomerate|50372|5|Briefly described|Map Legend|Devonian|Devonian|Of Finke Group. Geological Province: Amadeus Basin. Well rounded pebble to cobble, rarely boulder conglomerate in a clayey sand matrix. Clasts predominantly composed of granite, gneiss and quartzite.||||||
27881|Polly Conglomerate|65233|5|Briefly described|p13|Devonian|Devonian|Of the Finke Group. Overlain by Horsebend Shale.||||||07-FEB-11
27881|Polly Conglomerate|65309|4|Described|p6 Table 1, pp13-14, p19.|Devonian|Devonian|Sits directly on basement rock from which it is derived, and occurrence is restricted to immediately north of exposed basement. Maximum outcrop thickness is 65m. Type area at Horseshoe Bend, where clasts include material from Winnall beds. |Deposition age c.380 Ma.|Unit in Finke Group.|||Well-rounded pebble to cobble, rarely boulder conglomerate; white medium to coarse clayey sand matrix; clasts predominantly composed of granite, gneiss and quartzite.|
27881|Polly Conglomerate|65342|6|Mentioned|p10.|||Pedirka Basin. Max. thickness at least 393 m.||||Overlies Mereenie Sandstone. Is overlain by Langra Sandstone.||
27881|Polly Conglomerate|65489|6|Mentioned|p63|||Amadeus Basin. Contains potential reservoir beds.||||||
27881|Polly Conglomerate|69438|3|Fully described|p23:2-3, 20, 40-41|Late Devonian|Late Devonian|Wells et al. (1966). Amadeus Basin. Type locality is on the N flank of the Black Hill Range where it is 40m thick; up to 393m thick elsewhere, and locally absent from the Group's succession. Alluvial fan or proximal braided stream deposit.||Finke Group.||Unconformably overlies Winnall and Inindia beds and Stairway Sandstone. Is overlain conformably and gradationally by Langra Formation.|Polymictic, clast- to matrix-supported conglomerate, with interbeds of medium- to coarse-grained sandstone and rare brown or green siltstone.|12-JUL-16
27881|Polly Conglomerate|69449|5|Briefly described|p34:5|Devonian|Devonian|||Finke Group.||Overlies Mereenie Sandstone. Is overlain by Langra Formation.||12-JUL-16
27881|Polly Conglomerate|69673|6|Mentioned|p64 fig 53, p149|||||Finke Group||Overlain by Langra Formation||
27881|Polly Conglomerate|71279|5|Briefly described|p355 Fig.2|Late Devonian|Late Devonian|Amadeus Basin.||Finke Group.||||
27881|Polly Conglomerate|72476|5|Briefly described|p36|Silurian|Silurian|Amadeus Basin. Time-temperature thermal history diagram.|||||Coarse conglomerate.|
27881|Polly Conglomerate|73085|6|Mentioned|p1|late Devonian|late Devonian|||Finke Group||Overlain by Langra Formation. Equivalent to Parke Siltstone (Pertnjara Group).||
27881|Polly Conglomerate|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
26321|Possum Creek Charnockite|7837|5|Briefly described|p100|||Anmatjira Range.|1588 +/- 5 Ma.||||Includes small pegmatitic pods.|
26321|Possum Creek Charnockite|7838|5|Briefly described|p69-70, 74-75, 78-79, 83-87|||Northern Arunta Inlier. Peak granulite facies metamorphism during the second stage of the second tectonic cycle affecting this region is (zircon) dated at 1774 +/- 6 Ma. Zircon analyses tabulated and discussed. A population of 1588 +/- 5 Ma zircons is attributed to regional hydrothermal activity.|1774 +/- 6 Ma.||||Syntectonic intrusion. Occurs as thin composite sheets; total thickness 300m.|
26321|Possum Creek Charnockite|11884|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Lower Proterozoic age. Minimum age constrained by the intruding Anmatijira Granite.|> 1642 +/- 100 Ma|||Intruded by the Anmatjira Granite and Aloolya Granite. Intrudes Weldon Granulite and Tyson Creek Granulite.|Hornblende (brown)-hypersthene-quartz-andesine-sanidine granite, medium even foliated with sparse rapikivi feldspar augen.|
26321|Possum Creek Charnockite|23270|5|Briefly described|Table 1, p6||Proterozoic|In the Arunta Block (Division 1).||||||23-NOV-06
26321|Possum Creek Charnockite|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block(Division One). Age: Early or Middle Proterozoic.||||||23-NOV-06
26321|Possum Creek Charnockite|23363|5|Briefly described|351 Tab.2|Statherian|Statherian|Age: 1774+/-6Ma.||||||23-NOV-06
26321|Possum Creek Charnockite|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26321|Possum Creek Charnockite|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26321|Possum Creek Charnockite|39887|6|Mentioned|Fig.5|||||||||
26321|Possum Creek Charnockite|43749|6|Mentioned|p21|||U-Pb Age: 1774+/-6 Ma.||||||23-NOV-06
26321|Possum Creek Charnockite|48992|2|Defined|p44|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26321|Possum Creek Charnockite|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite. Age: 1774 +/- 6Ma (Shrimp).||||||07-NOV-08
26321|Possum Creek Charnockite|65338|5|Briefly described|p32, p56.|Statherian|Statherian|Anmatjira Range. Crosscuts granulite-grade foliation in Tyson Creek Metamorphics; this may correspond to the Yambah, as distinct from the Stafford, Event.|1774 +/- 6 Ma (Collins and Williams 1995).|||||
26321|Possum Creek Charnockite|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
26321|Possum Creek Charnockite|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
26321|Possum Creek Charnockite|69226|5|Briefly described|p239, p240 Tb.1, p242-245, p247, p255|Statherian|Statherian|Reynolds-Anmatjira Ranges region. Associated with the c.1780-1770 Ma Strangways Orogeny.|1774 +/- 6 Ma (Collins and Williams, 1995).|||Intrudes Mount Stafford Beds.||
26321|Possum Creek Charnockite|69427|4|Described|p12:6, 26, 28, 30, 32|Statherian|Statherian|Stewart (1980). SE Anmatjira Range, Aileron Province. Syntectonic or intruded between two high-grade metamorphic events. Intrusion of this unit caused granulite-facies metamorphism of Weldon Metamorphics and Tyson Creek Granulite. SHRIMP U-Pb age.|1774 +/- 6 Ma (Collins and Williams, 1995).|||Crosscuts Tyson Creek Granulite.|Forms a series of sheets of pyroxene-bearing granite that truncate granulite-facies fabrics in adjacent country rocks and contain angular xenoliths of granulite-facies rocks. Has undergone high-grade metamorphism.|12-JUL-16
26321|Possum Creek Charnockite|69925|6|Mentioned|p39|||Northern Arunta Province, Arunta Inlier.||||||
26321|Possum Creek Charnockite|69931|6|Mentioned|p274|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Sm-Nd isotopic analyses tabulated. Presented as Possum Charnockite on p274.|||||Charnockite.|
26321|Possum Creek Charnockite|70376|6|Mentioned|p833 fig 2, p834|Paleoproterozoic|Paleoproterozoic|Voluminous mafic magmatic protolith.|1774 Ma +/- 6 Ma|||||
26321|Possum Creek Charnockite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Both U-Pb zircon SHRIMP crystallisation ages.|1774+/-6 Ma and 1588+/-5 Ma.||||Charnockite.|
26321|Possum Creek Charnockite|73399|6|Mentioned|App.E|||[Misspelt as Possum Creek Charnokite].|||||Charnockite.|
33649|Pottoyu Granite Suite|24301|6|Mentioned|p37 Appendix 1|||||||||
33649|Pottoyu Granite Suite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block.  Age: ~1190 - 1140Ma.||||||31-MAY-04
33649|Pottoyu Granite Suite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Musgrave Block. Age: ~1190-1140Ma. Includes Amputjuta Dacite and Ilyaralana Granite.||||||06-MAY-13
33649|Pottoyu Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mulyati Granite and undivided Pottoyu Granite Suite rocks. Age: ~1190-1140Ma.||||||06-MAY-13
33649|Pottoyu Granite Suite|60683|1|Redefined|p56-57 Appendix, p16-17|Mesoproterozoic|Mesoproterozoic|Formerly the Pottoyu Granite Complex of Forman (1966a, 1972) and parts previously mapped as Olia Gneiss. Coarsely porphyritic biotite granite, typically with rapakivi texture. Age: 1192+/- and 1144+/-12Ma (SHRIMP U-Pb zircon). See also p11 Tb. 1, p42-43.||||||23-DEC-09
33649|Pottoyu Granite Suite|61154|6|Mentioned|p44 Appendix|Mesoproterozoic|Mesoproterozoic|Possibly an informal name? - see also Pottoyu Suite. Of the Pitjantjatjara Supersuite.||||||23-NOV-06
33649|Pottoyu Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mulyati and Ilyaralona Granites, and Ampitjuta Dacite. Age: ~1190-1140Ma. Geological Province: Musgrave Block.||||||06-MAY-13
33649|Pottoyu Granite Suite|63866|5|Briefly described|p202, p206|||Musgrave Province. See also Pottoyu Suite [unclear which name takes precedence].||Pitjantjatjara Supersuite||||
33649|Pottoyu Granite Suite|65256|4|Described|piii, p5-9, p7, p38, p31|Stenian|Mesoproterozoic|Includes Amputjuta Dacite, Ilyaralona Granite. Coarsely porphyritic biotite granite, typically with rapakivi texture; less abundant equigranular granite and aplite. Unconformably underlies Karukali Quartzite or Dean Quarzite or Kulail Sandstone. SHRIMP U-Pb ages of 1192+/-13 Ma and 1144+/-12 Ma; Rb-Sr whole rock ages of 1150 and 1190 Ma. Intruded by mafic dykes interpreted to belong to Alcurra dolerite. Suggested source of sediment for Karukali Quartzite. Given as Pottoyu Suite and Pottoyu Granite on piii.||||||
33649|Pottoyu Granite Suite|69091|5|Briefly described|p85, p137-139 Figs.6.4-6.6|||Name shortened to Pottoyu Suite in legend on p137-139 Figs.6.4-6.6.||Pitjantjatjara Supersuite|||Amphibolite facies metagranites.|
33649|Pottoyu Granite Suite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1192+\-13 Ma; 1148+\-12 Ma|Unit of Pitjantjatjara Supersuite.|||Fine- to coarse-grained, foliated, biotite metagranite|
33649|Pottoyu Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
33649|Pottoyu Granite Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1192+\-13 Ma; 1148+\-12 Ma|Unit of Pitjantjatjara Suite.|Includes Amputjuta Dacite.||Fine- to coarse-grained, foliated, biotite metagranite|
33649|Pottoyu Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Both crystallisation ages: U-Pb zircon SHRIMP.|1192+/-13 Ma and 1144+/-12 Ma.||||Granite.|
33649|Pottoyu Granite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1192+/-13 Ma, Min 1148+/-12 Ma.|Pitjantjatjara Supersuite|||Fine- to coarse-grained, foliated, biotite metagranite.|
42438|Pottoyu Suite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite. Coarsely porphyritic foliated biotite granite, typically with rapakivi texture, locally migmatititc with coarse hornblende; less abundant equigranular leucogranite. Geological Province: Musgrave Block.||||||11-JAN-05
42438|Pottoyu Suite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Mainly coarsely porphyritic foliated granite and fine- to medium-grained foliated biotite granite, and dacite. Geological Province: Musgrave Block.||||||14-JAN-05
42438|Pottoyu Suite|60683|5|Briefly described|p11 Tb. 1, p41|||Informal abbreviation of Pottoyu Granite Suite?  See also p17.||||||
42438|Pottoyu Suite|61154|4|Described|p9, p42 Appendix|Mesoproterozoic|Mesoproterozoic|See also Pottoyu Granite Suite. Of the Pitjantjatjara Supersuite. Comprises Mulyati Granite, Amputjuta Dacite and Ilyaralona Granite. Dominated by foliated, coarsely porphyritic biotite granite.  Age: 1192+/-13Ma and 1144+/-12Ma. Geol.Prov: Musgrave Block||||||
42438|Pottoyu Suite|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Granite. Geological Province: Musgrave Province.||||||
42438|Pottoyu Suite|61864|6|Mentioned|p18 fig 4||||||||Granites.|
42438|Pottoyu Suite|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province. See also Pottoyu Granite Suite [unclear which name takes precedence]. Ages derived from Scrimgeour et al., 1999.|1192 +/- 13 Ma to 1144 +/- 12 Ma|Pitjantjatjara Supersuite||||
42438|Pottoyu Suite|67375|5|Briefly described|p179.|Mesoproterozoic|Mesoproterozoic|Of Edgoose et el., 2004. Forms part of the later stage of the Pitjantjatjara Supersuite.||Unit in Pitjantjatjara Supersuite.|Includes Pottoyu Granite.|||
42438|Pottoyu Suite|69091|6|Mentioned|p137-139 Figs.6.4-6.6|||See references to Pottoyu Granite Suite (p85, p137-139 Figs.6.4-6.6).||||||
42438|Pottoyu Suite|69436|3|Fully described|p21:4, 9-10, 14, 19, 21|Mesoproterozoic|Mesoproterozoic|Forman (1972), Scrimgeour et al. (1999). Musgrave Province. Is the main basement lithology throughout the Pottoyu Hills and Petermann Ranges. In the Pottoyu Hills, metamorphic grade increases to the S to upper amphibolite facies, with leucosomes and melt-bearing shear zones. Is thrust over the Tjauwata Group, Dean Quartzite and Pinyinna beds in the Petermann Nappe Complex. Hosts malachite-bearing quartz veins assayed up to 2% Cu. Is enriched in U, but has not been explored. SHRIMP U-Pb crystallisation ages by Scrimgeour et al. (1999).|1192 +/- 13 Ma and 1144 +/- 12 Ma.|Pitjantjatjara Supersuite.|Mulyati, Ilyaralona Granites, Amputjuta Dacite.|Intruded by Kullal Dyke Suite and Amata Dolerite.|Dominated by foliated, coarsely porphyritic biotite granite. Numerous weakly porphyritic (rounded K-feldspar to 8cm, commonly with rapakivi texture), equigranular and aplitic phases also occur.|12-JUL-16
42438|Pottoyu Suite|73437|6|Mentioned|p152|||Apatite fission track cooling ages 271+/-15 Ma, 327+/-28 Ma from Tingate, (1990). Rb-Sr biotite cooling ages of 570+/-50 Ma and 600+/-50 Ma from Scrimgeour et al., (1999).|||||Includes granite.|
38409|Powell Formation|23937|6|Mentioned|p80 App. 1|||Of the Renner Group.  On HELEN SPRINGS  sheet.||||||
38409|Powell Formation|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||
38409|Powell Formation|24303|3|Fully described|p30, p61 Appendix|Calymmian|Calymmian|Of the Renner Group. Overlain by the Wiernty Formation; overlies the Grayling Member. Previously mapped as undifferentiated Tomkinson Creek beds. Equivalent of Arnold Sandstone, Jalboi Formation and Hodgson Sandstone. See also p23 Tb.3.||||||18-OCT-05
38409|Powell Formation|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Sandstone; quartz arenite; lensing, medium to very thick bedded, medium-grained to granular; quartz-rich; micaceous mudstone, rip-up clasts and breccia; laminated, crossbedded, ripples, graded, dessicated, halite pseudomorphs.||||||18-OCT-05
38409|Powell Formation|24442|5|Briefly described|p15|||Of the Renner Group.  Geological Province: Ashburton Province.||||||
38409|Powell Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Renner Group.||||
38409|Powell Formation|69431|4|Described|p16:15, 18-19, 21-22|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. c.300-820m thick. Open-marine shelf to supratidal deposits. Lithology described in some detail.||Renner Group.||Transitionally overlies Grayling Member (Baralandji Formation). Is overlain transitionally by Wiernty Formation, and unconformably by Muckaty Sandstone Member (Helen Springs Volcanics).|Mainly  moderately- to well-sorted, fine- to coarse-grained quartz sandstone with angular sedimentary clasts. Minor granular to pebbly quartz-clast conglomerate, siltstone and mudstone. Numerous sedimentary structures (listed).|12-JUL-16
38409|Powell Formation|69673|6|Mentioned|p58|||||Renner Group||||
38409|Powell Formation|70968|2|Defined|p94-95, p99, p104-108, p126, p131, p140|Calymmian|Calymmian|Hussey, Beier, Crispe and Donnellan in Hussey et al. (2001). Originally mapped as undivided Tomkinson Creek beds (Randal et al., 1966). Tomkinson Province. Named after Powell Creek. The type section is from 354200mE 7983400mN (base) to 353300mE 7984500mN in HELEN 100k sheet. Extensive exposures throughout the Province; forms an extensive, almost continuous, upstanding strike ridge N of Morphett Creek. Lithology described in detail as three lithofacies; well illustrated. 300-850m thick; c.750m in the type section. Marginal, shallow-marine to supratidal deposits.||Renner Group.||Conformably and transitionally overlies Baralandji Formation. Is overlain conformably and transitionally by Wiernty Formation, and unconformably by Muckaty Sandstone Member (Helen Springs Volcanics).|Fine- to very coarse-grained quartz sandstone, lesser sublithic sandstone, typically cream to white, variably silicified; minor granular to pebbly quartz-clast conglomerate, and rare cream to green-grey siltstone and mudstone.|
38409|Powell Formation|71893|3|Fully described|iii, p2-p3, p6, p8, p56-p58, p60-p63|Ectasian|Statherian|Tomkinson Province. The type section was sampled and is located about 17km SSW of Powell Creek Outstation in western HELEN. Deposited in marginal shallow marine to supratidal conditions. Description, sampling location, zircon description, LAICPMS U-Pb and Hf analysis, results and interpretation are provided. This unit is interpreted to range from Statherian to Ectasian on the basis of dating of the unconformably underlying Namerinni Group and a SHRIMP U-Pb date of 1295 +/- 14 Ma for an unnamed dyke which intrudes this unit. Mesoproterozoic age for this unit is confined by overlying early Cambrian sedimentary rocks, a dolerite intrusion in younger Renner Group strata that correlates with the Derim Derim Dolerite.||Renner Group||Conformably overlies the Grayling Member (Baralandji Formation). Conformably overlain by the Wiernty Formation.|Quartz sandstone, granular to small pebble quartz conglomerate and minor shale.|
74921|Prickle Hill"" sandstone|64662|6|Mentioned|p42 Fig. 17, p45|||Of northern Arunta region. Similar detrital zircon age distributions to Killi Killi Formation, Tanami region. May both have been part of a much larger depositional system.||||||07-FEB-11
40571|Prize Supersequence|62535|5|Briefly described|p663, p672-674|||Calvert Superbasin. Time-equivalent to the ~1695-1685 Ma Broken Hill Group. Thickness varies up to 1500m. Deposition was followed by a 15-20 m.y. hiatus.|c.1695? Ma - c.1690 Ma.|||Unconformably overlies Big Supersequence. Is overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|63112|6|Mentioned|p1191 Fig.2|||Calvert Superbasin.||||||
40571|Prize Supersequence|63866|5|Briefly described|p53-p54, p56, p58, p61-p62|||Calvert Superbasin. Magmatism in the Leichhardt River Fault trough initiated at 1690 and is expressed as peprites within stratigraphic units of this supersequence.|||Includes the Wunummantyala Sandstone, Aquarium Fomration, Wollogorang Formation, Packsaddle Granite, Hobblechain Rhyolite, Tanumbirini Rhyolite and Nyanantu Formation.|Equivalent to the Fish River Formation.||
40571|Prize Supersequence|65228|5|Briefly described|p21, p25, Fig.10.|||Calvert Superbasin. Gamma ray log, lithology and facies detailed.||||||
40571|Prize Supersequence|65337|6|Mentioned|p32.|||This study includes a younger  (<1700 Ma) component of Surprise Creek Formation in this Supersequence.||||Is overlain by Gun Supersequence.||
40571|Prize Supersequence|66844|4|Described|p243-245,254, 264, 265|||Lawn Hill Platform. Lower suite of fault-bounded, storm dominated siliclastic ramps.  Separated from the overlying Gun SS by a regionally correlative unconformity in the lower to middle Gunpowder Creek Formation. Shown as Prize Sequence on p264.||Equivalent to parts of lower McNamara Group.|Divided into Prize 1 and Prize 2 (p254) depositional sequences.|Overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot|||See also p13, p15, p39. Leichhardt River Domain, Mount Isa Inlier. Unconformity at base.|~1705-1680 Ma.|||Overlies Big Supersequence. Is overlain by Gun Supersequence. Equated with the Knapdale Quartzite.||
40571|Prize Supersequence|67539|6|Mentioned|p3|||||||||
40571|Prize Supersequence|68021|5|Briefly described|p135 Fig 4, p136, 137 Fig 5|Statherian|Statherian|Calvert Superbasin. Environment changing from near-shore to deltaic or shallow marine. |~1790 - ~1785 Ma|||Equivalent to Surprise Creek Formation.|Several cycles of upward-fining mainly siliciclastic sedimentation, followed by increasing amounts of thinly laminated carbonaceous shale or rhythmite.|
40571|Prize Supersequence|68146|5|Briefly described|p194, p199-200|||Magmatism started with Sybella-aged peperites at c.1690 Ma and lasted until emplacement of the Queen Elizabeth pluton at c.1655 Ma.|||Lower part of Torpedo Creek and Warrina Park Quartzites.|Is overlain unconformably by Gun Supersequence.||
40571|Prize Supersequence|68575|6|Mentioned|p40|||||||||
40571|Prize Supersequence|68732|5|Briefly described|p159, p161, p162, p166-169, p171|||Includes lower Gunpowder Creek Formation, Surprise Creek Formation, Warrina Park Quartzite, Deighton Quartzite (units 1-4), Knapdale Quartzite, Roxmere  Quartzite, Doherty Formation. Contains pink cherty beds with a detrital zircon age of ca 1690 Ma.|||||Comprises a full suite of shelfal siliclastic facies.|
40571|Prize Supersequence|69056|6|Mentioned|p54|||Calvert Superbasin.||||Equivalent to Knapdale Quartzite.||
40571|Prize Supersequence|69591|5|Briefly described|p27, p37-40, p54|||Mount Isa Province. Includes the Surprise Creek Formation, Stanbroke Sandstone and Knapdale Quartzite.||||Correlated with middle unit of Deighton Quartzite.||
40571|Prize Supersequence|70657|6|Mentioned|p17|||||||||
40571|Prize Supersequence|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Lawn Hill. Intruded by the Sybella Batholith.|ca. 1700 Ma|||Overlies the Fiery Creek Volcanics.|Sandstone and greywacke.|
40571|Prize Supersequence|73144|4|Described|p9-10, p29|Statherian|Statherian|Sequence Stratigraphy. Calvert Superbasin. Deposited in a coastal plain, nearshore environment with some below storm wavebase deposits (Southgate et al., 2000). Consists of a basal sandstone that dirties upwards to deeper water siltstone and black shales.|1690-1705 Ma|||Includes Surprise Creek Formation and Warrina Park Quarzite, Torpedo Creek Quartzite, and the lower Gunpowder Creek Formation.|Sandstone, conglomerate and siltstone.|
73224|Ptilotus Granodiorite|62580|5|Briefly described|p35|Paleoproterozoic|Paleoproterozoic|Of The Granites Suite. Foliated coarse-grained, weakly porphyritic biotite granodiorite; strongly zoned foliation. Intrudes Dead Bullock Formation. Age: 1805+/-5Ma (U/Pb zircon).||||||07-FEB-11
33654|Puka Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Umutju Granite Suite.  Porphyritic hornblende and clinopyroxene granites, variably deformed and recrystallised to garnet-bearing assemblages.  Age: ~1180-1120Ma.  Geological Province: Musgrave Block.||||||
33654|Puka Granite|60683|2|Defined|p56 Appendix, p16, p10 Tb.1|Mesoproterozoic|Mesoproterozoic|Of the Umutju Granite Suite.  Synonymous with Musgrave-Mann Metamorphics of Thomson (1969) and undivided metamorphosed granites of Forman (1972). Hornblende- and clinopyroxene-bearing granites, varaibly porphyritic. Intrusive age: 1145+/-6Ma (Pb-Pb).||||||27-NOV-06
33654|Puka Granite|61154|5|Briefly described|p12|Mesoproterozoic|Mesoproterozoic|Of the Umutju Suite (Pitjantjatjara Supersuite). Comprises foliated clinopyroxene and hornblende granite. Age: 1172+/-6Ma (Kober Pb-Pb zircon). Geological Province: Musgrave Block.  See also p44 Appendix.||||||
33654|Puka Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Umutju Granite Suite.  Porphyritic hornblende and clinopyroxene granites, variably deformed and recrystallised to garnet-bearing assemblages;  rare migmatite.  Geological Province: Musgrave Block.||||||19-OCT-05
33654|Puka Granite|69436|5|Briefly described|p21:8|||Fregon Domain, Mann Ranges, Musgrave Province. Kober Pb-Pb zircon age.|1172 +/- 6 Ma (Scrimgeour et al., 1999).|Umutju Suite.|||Foliated clinopyroxene and hornblende granite; medium-grained to coarse to megacrystic (rounded plagioclase phenocrysts to 9cm); local equigranular phases; mafic minerals occur in coarse aggregates to 1cm. Includes an isolated unfoliated charnockite.|12-JUL-16
33654|Puka Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1145+/-6 Ma (crystallisation).||||Granite.|
79226|Puna Kura Kura Formation|71898|5|Briefly described|p8|||Amadeus Basin. Outcrops on the HENBURY map sheet. Similar provenance spectra to Quandong Conglomerate.||Winnall Group|Includes the Chookla Member.|||19-NOV-18
79226|Puna Kura Kura Formation|72369|4|Described|iii,p3-4,15,18,20-26|||Of Amadeus Basin. Defined by Donnellan and Normington 2017. Typically layered, and locally massive, and red-brown (Fe-rich, oxidised) in outcrop. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND453 (fine-grained sandstone) yielded an interpreted maximum depositional age of 959+\-7 Ma (youngest concordant zircon), but does not further constrained the depositional age of the Puna Kura Kura Formation as this age predates the MDAs of the underlying Gloaming and Liddle formations. Paleoproterozoic detrital zircon spectrum was likely recycled from underlying Amadeus basin succession and/or derived from Aileron and Warumpi Provinces. Also contains a dominant Musgrave Province source (c. 1440Ma to c. 1005 Ma age spectrum). Sample locality, zircon description, SHRIMP results and analyses are discussed.||Unit of Winnall Group.|Includes Chookla Member.|Uppermost unit of the Winnall Group. Underlain unconformably by Liddle Formation. Potentially correlable to Arumbera and Eninta sandstones.|Fe-rich (oxidised) orange-brown sandstone; medium-grained, well sorted and well-rounded quartz grains, with a component of feldspar grains.|18-DEC-19
79226|Puna Kura Kura Formation|73119|5|Briefly described|piii, p1, p5, p7, p9, p12-14, Appendix|Cambrian|late Ediacaran|Amadeus Basin, western. Geochron is a new detrital zircon maximum depositional age, which is younger than the previous age of 690 +/- 10 Ma (Beyer et al., 2020) and much younger than that of Normington et al. (2018) (ca 959 Ma). Has a diverse detrital zircon provenance signature, which suggests a significant amount of recycling from metasedimentary sources. Sources include the Musgrave, Warumpi, and Aileron provinces and reworking of the underlying Amadeus Basin succession. [See article for provenance discussion].|657 +/- 23 Ma SHRIMP U-Pb|Winnall Group|Chookla Member|Underlain by Liddle Formation.|Well-sorted feldspathic sandstone.|
79226|Puna Kura Kura Formation|73279|5|Briefly described|p3, p8-9|Ediacaran|Cambrian|Amadeus Basin, central and western. Forms the uppermost part of the Winnall Group. Detrital zircons analysed for Hf isotopic composition [see article].||Winnall Group|Chookla Member||Includes sandstone.|
33811|Puntitjata Rhyolite|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: ~1075Ma.||||||03-AUG-09
33811|Puntitjata Rhyolite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1075Ma. Of the Tjauwata Group.||||||28-MAY-04
33811|Puntitjata Rhyolite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite. Geological Province: Musgrave Block.||||||03-AUG-09
33811|Puntitjata Rhyolite|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Rhyolite. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
33811|Puntitjata Rhyolite|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite; tuff and epiclastic sediments. Overlies Mount Harris Basalt; transitionally overlain by Bloods Range Formation. Age: 1075+/-2Ma. Geological Province: Musgrave Block. See also p5Tb. 1, p44 Appendix.||||||03-AUG-09
33811|Puntitjata Rhyolite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.  Porphyritic rhyolite.||||||19-OCT-05
33811|Puntitjata Rhyolite|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: 1075+/-2.5Ma. extrusive equivalent of the intrusive Hull Granite Suite. Correlated with Smoke Hill Volcanics of the Tollu Group in WA.||||||25-JAN-07
33811|Puntitjata Rhyolite|63866|4|Described|p203|Stenian|Stenian|Mulga Park Domain, Musgrave Province. Numeric age is a Pb-Pb Kober zircon age.|1075 +/- 3 Ma (Close et al., 2003)|Tjauwata Group||Overlies the Mount Harris Basalt.||
33811|Puntitjata Rhyolite|64745|5|Briefly described|p376|Stenian|Stenian|Paper implies of Tollu Group. Age: ca. 1.075Ga.||||||
33811|Puntitjata Rhyolite|65135|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. Dated at 1075 +/- 3 Ma.||||||
33811|Puntitjata Rhyolite|65256|2|Defined|p6 Tb.1, p11-12, p14 Fig 10, p37, p39|Stenian|Stenian|New name: within the upper stratigraphy of the Tjauwata Group. Finely porphyritic rhyolite, tuff, minor volcaniclastics. A-type. Overlies or is laterally equivalent to Mount Harris Basalt; underlies Bloods Range Formation gradationally, or Kulail Sandstone/Dean Quartzite. Pb-Pb evaporation on zircon age 1075+/-2.5 Ma; coeval and correlated with Smoke Hill Felsic Volcanics (Tollu Group).||||||
33811|Puntitjata Rhyolite|65833|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. 1075 +/- 3 Ma: a c.30 m.y. gap between this unit and the Wankari Volcanics, also of Tjauwata Group. Possible age equivalent of Skirmish Hill Volcanics.||||||
33811|Puntitjata Rhyolite|65906|5|Briefly described|p19, p22|Mesoproterozoic|Mesoproterozoic|Unit in Tjauwata Group and is a correlative of the Smoke Hill Volcanics. Age 1075 +/- 3 Ma (Edgoose et al., 2004).||||||
33811|Puntitjata Rhyolite|67128|5|Briefly described|p3, p12, p18, p27, p30|||Western Bloods Range. Age equivalent of Skirmish Hill Volcanics.|1075 +/- 2 Ma (Close et al., 2003).|Tjauwata Group.||Extrusive equivalent of Rowley Granophyre.||
33811|Puntitjata Rhyolite|67375|5|Briefly described|p217.|Mesoproterozoic|Mesoproterozoic|May post-datre many Giles Suite intrusions, negating a tentative correlation with the Kunmarnara Group.|c.1075 Ma.|Unit in Tjauwata Group.||||
33811|Puntitjata Rhyolite|69436|4|Described|p21:4, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Has been broadly correlated with Smoke Hill Volcanics based on their implied stratigraphic positions and geochronological ages. Also appears as Puntijata Rhyolite in 21:14. Kober Pb-Pb zircon age.|1075 +/- 3 Ma (Close et al., 2003).|Tjauwata Group.||Overlies, or is laterally equivalent to, Mount Harris Basalt. Is overlain transitionally by Bloods Range Formation. Correlated with Wankari and Smoke Hill Volcanics.|A succession of rhyolite flows, tuff and epiclastic sedimentary rocks. A-type.|12-JUL-16
33811|Puntitjata Rhyolite|70018|4|Described|p233,235-239|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Rhyolite. 1075+\-2.5 Ma age from Close et al., 2003; 1073+\-13 Ma from this study.|c. 1074 Ma|Unit of Tjauwata Group.||Overlain by Wankari Volcanics. Underlain by, or laterally equivalent to Mount Harris Basalt.|Porphyritic rhyolite.|
33811|Puntitjata Rhyolite|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Smoke Hill Volcanics was established by Close et al., 2003a.||Tjauwata Group||Equivalent to the Smoke Hill Volcanics.||
33811|Puntitjata Rhyolite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||rhyolite|
33811|Puntitjata Rhyolite|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin.||Unit of Tjauwata Group.|||Porphyritic rhyolite|
41850|Putardi Quartzite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzite, quartz-muscovite schist, rarekyanite-staurolite-quartz schist.  Geological Province: Warumpi Province.||||||07-NOV-08
41850|Putardi Quartzite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Quartzite, quartz-muscovite schist, biotite-muscovite and muscovite-kyanite-quartz phyllite and schist. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
41850|Putardi Quartzite|65272|6|Mentioned|p318 fig 2.|||Haasts Bluff Domain.||||||
41850|Putardi Quartzite|67565|2|Defined|p58, p11-12, p24, p29, p30, pp34-35.|Statherian|Statherian|New name. Haasts Bluff Domain, Warumpi Province. Named after Mount Putardi. Previously included within unnamed quartzite of the Arunta Complex (Ranford, 1969). Basement quartzite. Forms prominent ridges over discontinuous strike length of 100 km. Type locality is adjacent to Mount Liebig-Browns Bore track. Structurally repeated and interleaved with granite. Metamorphic effects are detailed. Non-magnetic with low radiometric response. Age determinations and inherited zircons are discussed.|<1663 +/- 4 Ma.|||Overlies Udor Granite. Is intruded by Stuart Pass Dolerite. Is overlain unconformably by Heavitree Quartzite.|Crystalline quartzite, quartz-muscovite +/- kyanite +/- staurolite schist; biotite-muscovite phyllite and schist, quartz-muscovite-kyanite schist, interleaved with the quartzite unit.|01-DEC-15
41850|Putardi Quartzite|68832|4|Described|p32-35|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Maximum deposition age is ambiguous.|1752+/-11 Ma|||Interpreted to overlie Udor Granite. Truncated by undeformed dykes of Stuart Pass Dolerite.|Dominated by crystalline metasedimentary quartzite, often containing kyanite and/or muscovite, interlayered with quartz-muscovite and muscovite-biotite phyllite and schist.|
41850|Putardi Quartzite|69428|5|Briefly described|p13:3, 5, 15|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Haasts Bluff Domain, Warumpi Province. Occurs as prominent strike ridges (including Mounts Udor, Putardi and Peculiar) along a discontinuous strike length of c.100 km. Most commonly occurs within the Udor Deformed Zone (described in some detail), structurally repeated and interleaved with granite. Age uncertain: either overlies or is intruded by the 1663 Ma Udor Granite. Detrital zircons give maximum depositional ages of either 1752 +/- 11 Ma or 1580 +/- 40 Ma.|||||Mainly crystalline quartzite, often containing kyanite and/or muscovite, interlayered with quartz-muscovite and muscovite-biotite phyllite and schist.|12-JUL-16
41850|Putardi Quartzite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1752+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
79099|Queenie Flat Granite Complex|68997|4|Described|vi-vii,p1,11-16|Statherian|Statherian|Felsic meta-igneous rocks that crop out over approximately 100 km2 in the southeastern part of ALCOOTA, north of the Harts Range. Emplaced during Stafford event at 1795+\-5 Ma (northeastern ALCOOTA), based on a 1795+\-5 Ma porphyritic orthogneiss (NTGS AC09CJE382. Grid Reference: MGA94 Zone 53: 477617mE 7476133mN) and a 1795+\-5 Ma migmatitic orthogneiss (NTGS AC07LCV412. Grid Reference: MGA94 Zone 53: 474058mE 7469267mN). These samples crop out close to Neoproterozoic rocks of the Irindina Province that were affected by Ordovician high-grade metamorphism during the Larapinta Event (Buick et al 2001). Zircon rims within porphyritic phase yielded a 1774+\-5 Ma age, attributed to 1780-1770 Ma Yambah Event metamorphism. Zircon rims with 1719+\-25 and 1711+\-21 Ma age reflects 1735-1690 Ma Strangways metamorphism. Evidence of Ordovician Larapinta Event recorded from metamorphic zircon rims in migmatitic orthogneiss (NTGS AC07LCV412) with a 486+\-9 Ma age.|1795+\-5 Ma (emplacement: U-Pb zircon)||||Foliated porphyritic biotite granite to leucocratic migmatite with a very strongly developed gneissosity.|
79099|Queenie Flat Granite Complex|69510|6|Mentioned|p17|||The 480-460 Ma Larapinta Event is recognised in orthogneisses in this unit.||||||
79099|Queenie Flat Granite Complex|69794|6|Mentioned|iv,p14|||Preserves rare evidence in orthogneissses for metamorphic zircon growth and resetting during Larapinta Event (Bodorkos et al. 2013).||||||06-APR-20
79099|Queenie Flat Granite Complex|69917|5|Briefly described|p99-100|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb SHRIMP zircon dating, Hf analytical data. Foliated biotite granite sampled. Igneous crystallisation age of 1795+/-5 Ma. Metamorphic zircon ages also recorded.|||||A diversity of I-type granites and granitic gneisses.|
79099|Queenie Flat Granite Complex|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphosed at 1711 +/- 21 Ma and at 486 +/- 9 Ma.|1795+/-5 Ma crystallisation (SHRIMP U-Pb zircon).||||Orthogneiss, granite.|
68884|Quorn dyke tonalite|61056|5|Briefly described|p779 Tb. 1, p782 Fig. 4|Paleoproterozoic|Paleoproterozoic|Informal name. Samples examined: foliated metatonalite (folded and boudinaged, heavily jointed and variably fractured); and foliated andalusite tonalite (boudinaged, heavily jointed and varaibly weathered). Age: 1870+/-3Ma.||||||07-NOV-08
77472|Radiolarite Member|13224|5|Briefly described|p489|Valanginian|Valanginian|New name. This zone containing this unit was not studied because its [non] calcareous nature made it unsuitable for GOI analysis.||Bathurst Island Group.||||26-NOV-18
28948|Ragged Range Conglomerate|13194|4|Described|p394 Tb. 4-16, p402 fig 4-66|Frasnian|Frasnian|Type Section: Conglomerate Hill 16o24'S 128o21E. 290-600m thick alluvial fan deposits. [Stratigraphic details contradictory].||||Overlies Kununurra Formation (conformably) at Matheson Ridge. Overlain by Cyril Sandstone (conformably).|Red conglomerate, pebbly sandstone and sandstone.|
28948|Ragged Range Conglomerate|23821|4|Described|p245|Devonian|Devonian|Geological Province: Ord Basin.||||||
28948|Ragged Range Conglomerate|32870|6|Mentioned|Fig.6|||Refers Kaulback & Veevers (1969).||||||27-NOV-06
28948|Ragged Range Conglomerate|40993|6|Mentioned|p4|||||||||
28948|Ragged Range Conglomerate|41158|6|Mentioned|p40|||See also p41.||||||27-NOV-06
28948|Ragged Range Conglomerate|41864|1|Redefined|p49|||||||||
28948|Ragged Range Conglomerate|41865|5|Briefly described|Map legend|Frasnian||||||||
28948|Ragged Range Conglomerate|42030|5|Briefly described|p749|||||||||
28948|Ragged Range Conglomerate|42191|6|Mentioned|Fig.8 P442|||||||||
28948|Ragged Range Conglomerate|44230|5|Briefly described|Map Legend||Frasnian|||||||
28948|Ragged Range Conglomerate|45038|14|Not recorded|p.26 Fig 71|||Abbreviation of Ragged Range Conglomerate Member?||||||27-NOV-06
28948|Ragged Range Conglomerate|45039|6|Mentioned|p16|||Upper Devonian||||||
28948|Ragged Range Conglomerate|45047|6|Mentioned|p105|||||||||
28948|Ragged Range Conglomerate|45058|6|Mentioned|Fig. 3|||L.Cambrian||||||
28948|Ragged Range Conglomerate|60006|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Geological Province: Bonaparte Basin. Of Cockatoo Group. Sandstone, polymict conglomerate.||||||
28948|Ragged Range Conglomerate|60682|4|Described|p22 Table 5, 23|Frasnian|Frasnian|Of Cockatoo Group. Previously Ragged Range Conglomerate Member. Unconformably overlies Whitewater Volcanics and Antrim Plateau Volcanics. Overlain by Kellys Knob Sandstone. Thickness: >300m. Geological Province: Bonaparte Basin. Sandstone and conglomerate||||||12-DEC-06
28948|Ragged Range Conglomerate|64580|6|Mentioned|map legend|||Of Cockatoo Group.||||||15-DEC-08
28948|Ragged Range Conglomerate|65331|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of Cockatoo Group, Bonaparte Basin. Sandstone, polymict conglomerate||||||
28948|Ragged Range Conglomerate|69165|6|Mentioned|500k_geologyp08_lut.csv|Frasnian|Frasnian|||Cockatoo Group||||
28948|Ragged Range Conglomerate|69452|4|Described|p36:6, 9-10|Frasnian|Frasnian|Veevers and Roberts (1968). Equivalent to Ragged Range Conglomerate Member (Plumb, 1968). Petrel Sub-basin, Bonaparte Basin. Onshore. Up to c.300m thick. Alluvial fan to shallow tidal environments of deposition, proximal to uplifted Proterozoic rocks. Contains pelecypods and gastropods.||Cockatoo Group.||Unconformably overlies Antrim Plateau Volcanics and Whitewater Volcanics. It is conformably overlain by, and interfingers with, Kellys Knob Sandstone.|Flat-lying beds of polymictic conglomerate and red-brown sandstone with occasional cross-beds; conglomerate clasts are up to cobble-boulder size and set in a sandy matrix.|11-JUL-16
28948|Ragged Range Conglomerate|69634|5|Briefly described|500k_geologyp08_lut.csv|||||Unit of Cockatoo Group.||||
28948|Ragged Range Conglomerate|69673|5|Briefly described|p169, p169 fig 140|Frasnian|Frasnian|Up to 300m thick.||Cockatoo Group||Overlain by Kellys Knob Sandstone|Polymictic conglomerate and sandstone.|
28948|Ragged Range Conglomerate|70206|5|Briefly described|Map Legend|Devonian|Devonian|Bonaparte Basin.||Unassigned Cockatoo Group|||Sandstone, polymictic conglomerate.|
28948|Ragged Range Conglomerate|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||sandstone, conglomerate|
27545|Raiwalla Shale|9534|5|Briefly described|Map legend||Cambrian|Of the Wessel Group.  Fissile interlaminated grey-green and purple shale, fine quartz grewacke, siltstone.||||||07-JUL-04
27545|Raiwalla Shale|9691|5|Briefly described|Map Legend|||Of the Wessel Group. Fissile interlaminated grey-green and purple shale, fine quartz greywacke, siltstone.||||||
27545|Raiwalla Shale|9701|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Fissile interlaminated grey-green and purple shale, fine quartz greywacke, siltstone.||||||02-JUN-05
27545|Raiwalla Shale|9733|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Fissile interlaminated grey-green and purple shale, fine quartz greywacke, siltstone.||||||
27545|Raiwalla Shale|22600|4|Described|Map legend|Neoproterozoic|Neoproterozoic|||||||
27545|Raiwalla Shale|23374|3|Fully described|Tb3p22,20,21,27,36|Neoproterozoic|Neoproterozoic|Of the Wessel Group. In the Arafura Basin.||||||27-NOV-06
27545|Raiwalla Shale|24047|6|Mentioned|p84|Neoproterozoic|Neoproterozoic|See also p86 Fig. 74.||||||
27545|Raiwalla Shale|24049|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Mudstone: grey and green when fresh, red when weathered, micaceous, interbedded with fine to medium-grained flaggy sandstone; sandstone rubble dominates in most weathered outcrops. Geol. Prov: Arafura Basin.||||||13-OCT-05
27545|Raiwalla Shale|32660|5|Briefly described|Table 7|||||||||
27545|Raiwalla Shale|36535|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
27545|Raiwalla Shale|36635|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
27545|Raiwalla Shale|42058|5|Briefly described|p113|||See also p122.||||||27-NOV-06
27545|Raiwalla Shale|42597|5|Briefly described|Map Legend|Adelaidean||||||||
27545|Raiwalla Shale|43010|2|Defined|p178|Middle Cambrian|Early Cambrian|Of the Wessel Group.||||||27-NOV-06
27545|Raiwalla Shale|44112|3|Fully described|Table13p74,75-76|Neoproterozoic|Neoproterozoic|||||||12-MAY-06
27545|Raiwalla Shale|44338|14|Not recorded|p.7,opp.6|||Middle formatio of Wessel Group.||||||27-NOV-06
27545|Raiwalla Shale|44339|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic, part of Wessel Group.||||||
27545|Raiwalla Shale|44475|2|Defined|p.8,opp.p.6,map,Tb.1|||(C53-15,16).||||||
27545|Raiwalla Shale|44476|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
27545|Raiwalla Shale|46639|5|Briefly described|Map legend|Cambrian|Cambrian|Of the Wessel Group. Overlain by Marchinbar Sandstone, underlain by Buckingham Bay Sandstone. Fissile laminated grey-green and purple shale, fine quartz greywacke, siltstone (non-outcropping).||||||14-AUG-07
27545|Raiwalla Shale|46792|6|Mentioned|p53|||Correlation||||||
27545|Raiwalla Shale|60550|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Wessel Group. Fissile interlaminated grey-green and purple shale, fine quartz greywacke, siltstone.||||||10-JUN-05
27545|Raiwalla Shale|60571|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Mudstone: grey-green when fresh, maroon when weathered, micaceous; sandstone: fine- to medium-grained, thin bedded. Geological Province: Arafura Basin.||||||30-NOV-04
27545|Raiwalla Shale|61403|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of Wessel Group. Mudstone: grey and green when fresh, red when weathered, micaceous, interbedded with fine to medium-grained flaggy sandstone; sandsto ne rubble dominates in most weathered outcrops. Geol. Prov: Arafura Basin.||||||
27545|Raiwalla Shale|61561|5|Briefly described|p533||Cambrian|Overlies Buckingham Bay Sandstone.||||||20-APR-06
27545|Raiwalla Shale|62504|5|Briefly described|p1, 2|Neoproterozoic|Neoproterozoic|Siliceous chert and cherty siltstone. Overlies Buckingham Bay Sandstone. Of the Wessel Group,||||||
27545|Raiwalla Shale|62505|4|Described|p3|Neoproterozoic|Neoproterozoic|Of the Wessel Group. Underlies: Marchinbar Sandstone. Overlies: Buckingham Bay Sandstone.||||||
27545|Raiwalla Shale|62788|5|Briefly described|p103, 104|Neoproterozoic|Neoproterozoic|Arafura Basin. Contains fossils of Chuaria, a widespread Neoproterozoic alga.||Of the Wessel Group.||Overlies Buckingham Bay Sandstone and underlies Marchinbar Sandstone.||28-MAR-12
27545|Raiwalla Shale|63062|5|Briefly described|p11, p38|||Of the Wessel Group. Geological Province: Arafura and Money Shoal Basins. Contains thick, fine-grained sediments of shallow marine origin.||||||07-FEB-11
27545|Raiwalla Shale|65337|6|Mentioned|p95.|Ediacaran|Ediacaran|||Unit in Wessel Group.||||
27545|Raiwalla Shale|69437|6|Mentioned|p22:4-5|Ediacaran|Ediacaran|Arafura Basin.||||||12-JUL-16
27545|Raiwalla Shale|69443|5|Briefly described|p28:12|Neoproterozoic|Neoproterozoic|Onshore Arafura Basin. Contains the carbonaceous macrofossil Chuaria.||Wessel Group.||Is correlated with Cox Formation.||12-JUL-16
27545|Raiwalla Shale|69451|3|Fully described|p35:3-6; 35:12 Fig.35.8; 35:13|Neoproterozoic|Neoproterozoic|Plumb and Roberts (1992), who nominated a reference area around the Woolen River in ARNHEM BAY map area. Arafura Basin (onshore). Contains the carbonaceous fossil Chuaria, but no metazoan or trace fossils. Subtidal marine shelf deposits, gradual upward shallowing with increasing storm influence. 1000m thick. Potential petroleum source rock.||Wessel Group.||Conformably overlies Buckingham Bay Formation. Is overlain conformably (gradationally) by Marchinbar Sandstone. Correlated with Cox Formation (Georgina Basin).|Grey and green micaceous mudstone, red-brown when weathered, very recessive and poorly exposed; interbedded with fine- to medium-grained tabular sandstone.|12-JUL-16
27545|Raiwalla Shale|69673|5|Briefly described|p195|||up to 1000m thick.||Wessel Group|||Mudstone and sandstone interbeds.|
27545|Raiwalla Shale|73083|6|Mentioned|p33|||||||||
27545|Raiwalla Shale|73086|6|Mentioned|p122|||Arafura Basin.||||Correlates to Pertatataka Formation.||
38003|Randall Peak Metamorphics|9199|5|Briefly described|Map legend|||Leucocratic biotite gneiss, amphibolite, muscovite-biotite schist.  Geological Province: Arunta Block.||||||04-NOV-04
38003|Randall Peak Metamorphics|46730|4|Described|p5|||Intruded by Jennings Granitic Gneiss. Geological Province: Arunta Block.||||||
38003|Randall Peak Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Leucocratic biotite gneiss, amphibolite. Muscovite-biotite schist.||||||
38003|Randall Peak Metamorphics|64738|6|Mentioned|p249, p250 Table 1.|Paleoproterozoic|Paleoproterozoic||1684 +/- 36 Ma.|||||
38003|Randall Peak Metamorphics|68150|5|Briefly described|p11 Tb.3.2|||Unattributed, unknown if crystallisation or metamorphism age.|1684 +/- 36 Ma, 1 analysis, Zhao and Bennett 1995|||||
38003|Randall Peak Metamorphics|69427|4|Described|p12:9, 14-15, 31, 46|Statherian|Statherian|Strangways Range region, Wigley Domain, Aileron Province. The 1771 +/- 9 Ma orthogneisses in this unit are included in the Jennings Suite. SHRIMP U-Pb zircon age of intrusion of a strongly foliated tonalite.|1771 +/- 9 Ma (Zhao and Bennett, 1995).|||Is intruded by Trephina Granitic Gneiss and Whistleduck Dyke Swarm.|Characterised by felsic gneiss, amphibolite and migmatitic biotite gneiss; minor biotite-muscovite gneiss, tonalitic biotite-hornblende gneiss, sillimanite-bearing gneiss and megacrystic orthogneiss.|12-JUL-16
38003|Randall Peak Metamorphics|69925|5|Briefly described|p21-23, 25, 28-29, 36, 40|||Southern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated. Age from a tonalitic gneiss.|1771 +/- 9 Ma (U-Pb).|||Is intruded by Mordor Igneous Complex. Concordant but locally intruded by Jennings, Trephina and Georgina Gap Granitic Gneisses.|Quartzofeldspathic gneiss with minor amphibolite and biotite gneiss interlayers. Amphibolite facies metamorphism.|
38003|Randall Peak Metamorphics|69931|6|Mentioned|p269, 273, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses tabulated.|||||Includes orthogneiss, coarse-grained foliated tonalite.|
38003|Randall Peak Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1771+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Foliated tonalitic orthogneiss.|
27886|Ranken Limestone|36473|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
27886|Ranken Limestone|37572|4|Described|p157|||||||||
27886|Ranken Limestone|40852|6|Mentioned|p37|||See also Fig.3.7||||||
27886|Ranken Limestone|41129|6|Mentioned|Fig.8|||||||||
27886|Ranken Limestone|41524|6|Mentioned|Fig.3|||||||||
27886|Ranken Limestone|44233|14|Not recorded|p.60,61||Middle Cambrian|||||||
27886|Ranken Limestone|44285|2|Defined|p.8||Middle Cambrian|M.Cam. (F53-4).||||||
27886|Ranken Limestone|44355|14|Not recorded|map legend||Middle Cambrian|Fossiliferous oolitic and crystalline limestone, some chert nodules. Middle Cambrian.||||||
27886|Ranken Limestone|44441|14|Not recorded|opp.p.6, Tb.1, map||Middle Cambrian|Includes rocks previously included in Alroy Downs Beds & Barkly Group. Middle Cambrian. (E53-16). See also p.9-11, for more details.||||||
27886|Ranken Limestone|44442|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
27886|Ranken Limestone|45052|3|Fully described|p80|||M.Camb.||||||
27886|Ranken Limestone|45102|6|Mentioned|p65|||||||||
27886|Ranken Limestone|60122|6|Mentioned|p57 Appendix|||Geological Province: central Georgina Basin.  Possibly correlated with parts of Arthur Creek Formation.||||||
27886|Ranken Limestone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Georgina Basin.  Contains fauna of Ordian age.||||||
27886|Ranken Limestone|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Bioclast, bioclast-ooid and bioclast-intraclast rudstone, commonly silicified; minor bioclast wacke/floatstone, calcimudstone and calcimudstone-siliclastic mudstone interbeds.||||||21-AUG-06
27886|Ranken Limestone|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Bioclast, bioclast-ooid and bioclast-intraclast rudstone, commonly silicified; minor bioclast wacke/floatstone, calcimudstone and calcimudstone-siliciclastic mudstone interbeds.||||||14-MAY-14
27886|Ranken Limestone|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Limestone, shale and siltstone, commonly chertified or ferruginised; minor phosphorite; basal quartz sandstone.||||||
27886|Ranken Limestone|64068|5|Briefly described|p62, 63, 225|||Western and central Georgina Basin. Correlated with Arthur Creek Formation, Beetle Creek Formation, Blazan Shale, Inca Formation.||||||
27886|Ranken Limestone|64443|1|Redefined|p2, p5 Fig.3, p6 Tb.1, p13-14, p40-41|Early Boomerangian||Of Opik (1956). Note: revised definition; formerly known as Ranken limestone.  Correlative of Anthony Lagoon beds, lower Camooweal Dolostone, Age Creek Formation, Currant Bush Limestone, V Creek Limestone, Mail Change Limestone, Devoncourt Limestone and/or Roaring Siltstone, medial Arthur Creek Formation. Max 74+ m thick.||Of Barkly Group.||Conformably overlies Wonarah Formation; conformably underlies Camooweal Dolostone; unconformably underlies Brunette Limestone; passes laterally into adjacent Camooweal Dolostone.|Bioclast, bioclast-ooid and bioclast-intraclast rudstone, bioclast wacke/floatstone; minor calcimudstone. Red-brown silicification, abundant fossils characteristic.|14-MAY-14
27886|Ranken Limestone|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Barkly Group, Georgina Basin. Probably overlies Wonarah Formation, underlies Camooweal Dolostone. Bioclast, bioclast-ooid and bioclast-intraclast rudstone; minor bioclast wacke/floatstone, calcimudstone, calcimudstone-siliciclastic mudstone interbeds. ||||||
27886|Ranken Limestone|65337|3|Fully described|p9 Fig.5, p66.|Middle Cambrian|Middle Cambrian|Southwest MOUNT DRUMMOND area. 36 - 146 m thick. Now recognised asa bioclastic lithofacies within the basal high-energy interval of the Camooweal Dolostone.||Unit in Barkly Group.||Overlies Wonarah Formation. Is overlain by Camooweal Dolostone.|Pervasively chertified fossiliferous bioclast and bioclast-ooid rudstone.|
27886|Ranken Limestone|65344|5|Briefly described|p3 Fig. 2, p34-37, 47|||See thin section descriptions for detail.||||Overlies Wonarah Formation.||03-MAY-12
27886|Ranken Limestone|65345|5|Briefly described|p6 Fig.5. |Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin.||||Overlies Wonarah Formation. Is overlain by Camooweal Dolostone.||
27886|Ranken Limestone|67352|6|Mentioned|p21|||||||Overlies Wonarah Formation.||
27886|Ranken Limestone|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Western Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2.||||Overlies Wonarah Formation. Is overlain by Camooweal Dolostone.|Bioclastic limestone.|12-JUL-16
27886|Ranken Limestone|69443|4|Described|p28:16, 21-24, 43|Middle Cambrian|Middle Cambrian|Opik (1956). Central Georgina Basin. Forms scattered bouldery outcrops. At least 74m thick.||Barkly Group.||Conformably overlies Wonarah Formation. Is overlain conformably by, and passes laterally into, the Camooweal Dolostone. Lateral equivalent of several units in the Narpa Group.|Dominantly bioclast, bioclast-ooid and bioclast-intraclast rudstone (bioclasts of hyoliths, trilobites and echinoderm plates, brachiopods and molluscs); lesser interdigitating bioclast wacke/floatstone with similar bioclasts in calcimudstone matrix.|12-JUL-16
27886|Ranken Limestone|69446|6|Mentioned|p31:4|||Georgina Basin.||||||12-JUL-16
27886|Ranken Limestone|69561|4|Described|p31, p32 fig 1, p33 fig 2, p34, p37, p49|Boomerangian|Undillan|Limestone reef fossils(microbialites, trilobites, brachiopods, hyoliths, molluscs and sponges)||||Conformably overlies Wonarah Formation, conformably overlain by Camooweal Dolostone|Bioclast ooid and bioclast-intraclast rudstone of hyoliths, trilobites, echinoderm plates, bioclast wacke, limestone and floatstone.|
27886|Ranken Limestone|69573|6|Mentioned|p659, 665|||Georgina Basin. Carbonate reef environment. Contains Drumian Stage [Cambrian] fossil sites.||||||
27886|Ranken Limestone|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
27886|Ranken Limestone|69673|5|Briefly described|p116, p117|||74m thick.||Barkly Group|||Fossiliferous, bioclast and bioclast-ooid rudstone; minor conglomerate and calcimudstone.|
27886|Ranken Limestone|70380|6|Mentioned|p745, p759|Series 3|Series 3|Undilla Sub-basin, Georgina Basin.||||||
27886|Ranken Limestone|70835|6|Mentioned|p352|Cambrian|Cambrian|Georgina Basin, NT. Series 2, Stage 4. Mentioned in connection with a univalve mollusc fossil which resembles a new South Australian species described in this article.||||||
27886|Ranken Limestone|72516|6|Mentioned|p92|Cambrian|Cambrian|Western and central Georgina Basin.||||Equivalent to the Arthur Creek Formation.||03-JUN-21
35679|Rapakivi granite|44158|5|Briefly described|Table.1|Mesoproterozoic|Mesoproterozoic|Age: Probably between 1670-1570Ma. Of the Southwark Granitic Suite.||||||05-MAY-10
72411|Rapide Granite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Garnet bearing biotite granite, mostly porphyritic with tabular feldspars, sometimes defining a weak foliation.||||||07-NOV-08
72411|Rapide Granite|64580|4|Described|map legend|Paleoproterozoic|Paleoproterozoic|Of Carrington Suite. Garnet-bearing biotite granite, mostly porphyritic with tabular feldspars, weak to strong foliation; may include banded gneiss.||||||15-DEC-08
72411|Rapide Granite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Shown as equivalent age to Carrington Suite, younger than 1805 Ma Stafford Event. Garnet-bearing biotite granite, mostly porphyritic with tabular feldspars, locally defining a weak foliation||||||
72411|Rapide Granite|69427|5|Briefly described|p12:3, 30-31, 33|Statherian|Statherian|Edgoose et al. (in prep.). Poor, extensive outcrops E of Lake Mackay, Aileron Province. May have been generated by granulite-facies partial melting of a metasedimentary succession. SHRIMP U-Pb zircon tentative magmatic age, isotopically disturbed at 1590 Ma.|1760 Ma (Kinny, 2002).||||Leucocratic, typically undeformed garnet-bearing granite and syenogranite, locally with coarse tabular K-feldspar; peraluminous, locally contains minor amounts of orthopyroxene or spinel +/- corundum.|12-JUL-16
72411|Rapide Granite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Carrington Suite.|||Garnet-bearing biotite granite, mostly porphyritic with tabular K-feldspar, sometimes defining a weak foliation.|
72411|Rapide Granite|69794|5|Briefly described|iv, p1, p6-9|Statherian|Statherian|Geological province: Aileron Province. Of Arunta region. Weakly porphyritic. Sample NTGS LM01CJE006 (biotite granite) yielded a magmatic crystallisation age of 1615+\-6 Ma, which matched felsic intrusives exposed in the Warumpi Province, and the Ennugans Mountains Granite (NTGS NB11EEB319A; Kositcin et al 2013). Metamorphic zircon rims dated at c. 1578 Ma indicate age of metamorphism, consistent with c. 1590-1560 Ma Chewnings Event. Previously dated at c. 1760 Ma by Kinny (2002).||||||06-APR-20
72411|Rapide Granite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|Intruded during intracratonic reactivation of the Capricorn Orogen.||||||
72411|Rapide Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
72411|Rapide Granite|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphosed at 1578 +7.1/-2.5 Ma.|1615+/-6 Ma (U-Pb zircon SHRIMP)||||Granite.|
72411|Rapide Granite|71858|5|Briefly described|p2, p55|Statherian|Statherian|Aileron Province. Outcrops on the LAKE MACKAY map sheet.|1615 +/- 6 Ma (Kositcin et al, 2014)|||||
72411|Rapide Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Orogen.||Carrington Suite|||Garnet-bearing biotite metagranite, mostly porphyritic with tabular feldspars; weak to strong foliation; may include banded gneiss.|
74104|Red Cliff Granite|24197|5|Briefly described|p68 Tb. 6.1|Paleoproterozoic|Paleoproterozoic|Of Tennant Creek Supersuite. Age: ~1850Ma. Geological province: Tennant Creek Davenport Province.||||||07-FEB-11
78826|Red Eye Granite|64675|6|Mentioned|Fig.14|||Shown as Red Eye granite in figure caption. ?Informal company name?||||||19-MAR-14
42197|Red Heart Dolostone|12951|5|Briefly described|p143, fig 4, p154 fig 16, p155|Early Cambrian|Early Cambrian|Georgina Basin.||||Disconformably overlain by Thorntonia Limestone.|Archaeocyath-bearing dolostone.|
42197|Red Heart Dolostone|24442|5|Briefly described|p49|Early Cambrian|Early Cambrian|Unit bears calcimicrobial-archaeocyathan patch reefs.  On TOBERMORY sheet.||||||
42197|Red Heart Dolostone|60122|4|Described|p14-15|Early Cambrian|Early Cambrian|Formerly Red Heart Dolomite on HAY RIVER and Errara Fm on HUCKITTA.  Not exposed at TOBERMORY. Disconformable on Adam Shale and Mt Baldwin Fm; also nonconformable on Mt Tietkins Granite Complex. Overlain by Thorntonia Lst or Arthur Cr Fm. Max. thick: 19m.||||||23-MAY-05
42197|Red Heart Dolostone|60123|5|Briefly described|p5|||Disconformably underlies: Thorntonia Limestone.||||||28-APR-05
42197|Red Heart Dolostone|60590|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Dolostone, minor quartzic dolostone, mudstone and conglomerate; basal dolomitic quartzofeldspathic sandstone.  Overlain by the Thorntonia Limestone.||||||23-DEC-09
42197|Red Heart Dolostone|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.||||||20-APR-05
42197|Red Heart Dolostone|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Dolostone, minor quartzic dolostone, mudstone and conglomerate; basal dolomitic quartzofeldspathic sandstone. Geological Province: southern Georgina Basin.||||||
42197|Red Heart Dolostone|62376|5|Briefly described|p53|Middle Cambrian|Early Cambrian|Geological Province: Georgina Basin.||||||09-FEB-10
42197|Red Heart Dolostone|62789|5|Briefly described|p128, p129 Fig. 2|Early Cambrian|Early Cambrian|Contains archaeocyaths and small shelly fossils. 21.2 m thick at Pacific Oil & Gas Baldwin No. 1 exploration well.||||Overlies Mount Baldwin Formation and underlies early Middle Cambrian Thorntonia Limestone.||28-MAR-12
42197|Red Heart Dolostone|62983|5|Briefly described|p11|Early Cambrian|Early Cambrian|Carbonate platform deposition. Geological Province: Georgina Basin.||||||23-JAN-07
42197|Red Heart Dolostone|64068|3|Fully described|p56-57, p44, 51, 53, 54, 55,58,61,83,4|Early Cambrian|Early Cambrian|Potential hydrocarbon reservoir rock. Has archaeocyaths and small skeletal fossils. Now includes Errarra Formation rocks of Freeman (1986), Ambrose at al (2001).||Of Shadow Group.||Probably disconformable on Adam Shale, unconformable on Grant Bluff Formation. Disconformable beneath Thorntonia Limestone.|Dolostone with basal arkose or sandstone and siltstone, below dolostone and sandstone.|05-APR-12
42197|Red Heart Dolostone|64676|6|Mentioned|p31|Early Cambrian|Early Cambrian|Georgina Basin.||||||
42197|Red Heart Dolostone|64778|6|Mentioned|p13|Cambrian|Cambrian|Southern Georgina Basin.||||||
42197|Red Heart Dolostone|64812|5|Briefly described|p237 Fig. 2, p251|Early Cambrian|Early Cambrian|Geological Province: southern Georgina Basin. Comprises poorly sorted dolomitic, calcitic and phosphatic allochems including stromatolites deposited in a muddy matrix.||||||07-FEB-11
42197|Red Heart Dolostone|64813|5|Briefly described|p256 Fig. 3|Early Cambrian|Early Cambrian|Overlies Mount Baldwin Formation and Adam Shale. Geological Province: southern Georgina Basin. Carbonates with varying amounts of sandstone and red shale at the base.||||||11-FEB-09
42197|Red Heart Dolostone|65237|5|Briefly described|p3 Fig. 4|Early Cambrian|Early Cambrian|Interfingers with Errarra Formation. Max. thickness: 92m. Geological province: southern Georgina Basin. Archaeocyathid-bearing red dolostone with variable clastic content.||||||07-FEB-11
42197|Red Heart Dolostone|65342|6|Mentioned|p7.|||Georgina Basin. Max. thickness at least 92 m.||||||
42197|Red Heart Dolostone|66767|5|Briefly described|p59|Early Cambrian|Early Cambrian|Southern Georgina Basin.|||||Carbonates.|
42197|Red Heart Dolostone|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Southern Georgina Basin.||||Overlies Neutral Junction, Mount Baldwin Formations and Adam Shale.||12-JUL-16
42197|Red Heart Dolostone|69443|3|Fully described|p28:7, 11-12, 14-17, 31, 38, 40, 46-47|Early Cambrian|Early Cambrian|Walter in Walter et al. (1979). Southern Georgina Basin. The first carbonate package in the Georgina Basin succession. 9m in the type section in cored drillhole BMR Hay River-11B. Up to 126m elsewhere. Contains mid-Early Cambrian small skeletal fossils and reef-building archaeocyaths of late Atdabanian stage, as well as the ichnofossil ?Diplocraterion sp. Marginal marine, then shallow-marine, deposits. Is correlated with Todd River Dolostone. Associated with minor Pb-Zn mineralisation in the Marqua-Boat Hill area. Potential petroleum reservoir, particularly structurally. Has had hydrocarbon shows in drilled wells.||Shadow Group.||Locally disconformably overlies Elkera Formation and Adam Shale, and overlies Mount Baldwin or Grant Bluff Formations unconformably. Is overlain disconformably by Arthur Creek Formation.|Stylolitic, mottled, brecciated and vuggy dolostone above basal arkose or sandstone, with thin mudstone interbeds. Local basal sandstone and quartzose siltstone below dolomitic sandstone and quartzose dolostone; also conglomerate and marly mudstone.|12-JUL-16
42197|Red Heart Dolostone|69561|6|Mentioned|p33 fig 2, p34|Cambrian|Cambrian|||||Overlies Adam Shale, Mount Baldwin Formation, Neutral Junction Formation||
42197|Red Heart Dolostone|69673|5|Briefly described|p114, p116, p129, p130, p131, p138|||126m thick. Potential conventional reservoir and hydrocarbon seal.||Shadow Group||Disconformably overlain by Arthur Creek Formation, unconformably overlies Mount Baldwin Formation|Stylolitic, mottled, brecciated, vuggy dolostone and arkose or sandstone with mudstone interbeds.|
42197|Red Heart Dolostone|70723|5|Briefly described|p24 Fig. 2|Cambrian|Cambrian|Georgina Basin. Oil show. Diagram implies it is basal Narpa Group.|||||Dolomite.|
42197|Red Heart Dolostone|70833|5|Briefly described|p204|Cambrian|Cambrian|Of Georgina Basin. Broadly coeval with Todd River Dolostone (Amadeus Basin); equivalent to Errarra Formation and correlable to M. etheridgei zone in Arrowie Basin.. Type section: BMR Hay River 1lB core? Intersected 9.8m section.||||||
42197|Red Heart Dolostone|70951|6|Mentioned|p1077, 1082|||Dolomite-dominated.||||||
42197|Red Heart Dolostone|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Includes fossil Archaeocyaths, brachiopods, ichnofossils, small skeletal fossils, tubes, hyoliths, chancelloriids, sponge spicules, stromatolites.||Shadow Group||Unconformably overlies the Mount Baldwin Formation.|Basal arkose, sandstone, quartzitic siltstone; dolomitic sandstone; quartzitic dolostone; granule conglomerate.|
42197|Red Heart Dolostone|72516|3|Fully described|p12-13, p79, p90-92|Cambrian Series 2|Cambrian Series 2|Georgina Basin. Defined by Ambrose et al (2001) and replaces the Errarra Formation (informal name) and the Red Heart Dolomite. Occurs in northern HAY RIVER (with the type section located in cored drillhole BMR Hay River 11B) in the subsurface, in southern TOBERMORY, in southwestern ELKEDRA and in HUCKITTA. In the present map sheet is exposed northwest of Jervois Range and northwest and northeast of the Lucy Creek Fault Zone. Contains fossil archaeocyaths, brachiopods, ichnofossils, small skeletal fossils, tubes, hyoliths, chancelloriids, sponge spicules and stromatolites.  Fossil assemblage indicates a Series 2 and Stage 3 depositional age during the Cambrian. 20-80m thick in the mapped area, 5-126m thick elsewhere. Deposited in low to high energy marginal marine environment or a shallow marine environment for the upper part. Misspelt as Read Heart Dolostone p13.||Shadow Group||Disconformably overlain by the Thorntonia Limestone, Unconformably overlies the Grant Bluff Formation and the Mount Baldwin Formation.|Basal arkose, sandstone; quartzitic siltstone; dolomitic sandstone, quartzitic dolostone, granule conglomerate.|04-JUL-22
81661|Redbank package|72373|5|Briefly described|p1-2|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Informal nomenclature of Rawlings et al (1997) and Rawlings (1999). A basin-wide non-genetic depositional package within the McArthur Basin.||||Overlain by Goyder package.||02-OCT-19
81661|Redbank package|72718|5|Briefly described|p5, p6-7, p12, p14|Statherian|Statherian|Southern McArthur Basin. Inferred to be present in the Beetaloo Sub-basin, underlying the Glyde package. Maximum depositional age of Redbank package is constrained by a SHRIMP U-Pb zircon age of 1851+/-7 Ma for the underlying Palaeoproterozoic Scrutton Volcanics. Minimum age a little younger than 1713+/-3 Ma from Tanumbirini Rhyolite, near top of package. Depositional age range between ca 1790 and ca 1700 is suggested.|younger than 1851+/-7 Ma to ca 1713 +/-6 Ma.||||Dominated by shallow-marine to fluvial sandstone, with lesser shale, conglomerate, dolostone and bimodal volcanic rocks.|
81661|Redbank package|72912|6|Mentioned|p5, 18.|Statherian|Statherian|Of Rawlings, 1999.||||Underlies Goyder package.||
70535|Redhackle Granite|62378|5|Briefly described|p5, 17|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region. Age: 1772 +/- 3Ma. Metamorphic rims with age: 1579 +/- 7Ma. Granite. Formerly Giles Range granite.||||||07-NOV-08
70535|Redhackle Granite|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Biotite-granite/gneiss.||||||07-NOV-08
70535|Redhackle Granite|65338|3|Fully described|App1 p82, p20, p22, pp28-32, App 2|Statherian|Statherian|Newly defined. Coeval with Strangways Event. New zircon growth at 1579 +/- 7 Ma (Chewings Orogeny age) recognised. Gneissic foliation; dynamic and static recrystallisation structures. Mineralogy and microstructure are detailed.|1772 +/- 3 Ma (Worden et al. 2004).|||Intrudes Lander Rock Formation. Sheared, faulted contact with Mount Thomas Quartzite.|Grey, biotite-granite/gneiss; equigranular/seriate porphyritic and K-feldspar megacrystic phases; dark blue, opalescent quartz; local rapakivi texture; tourmaline-bearing; aplite, pegmatite.|
70535|Redhackle Granite|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-granite/gneiss, megacrystic K-feldspar-bearing with rare rapakivi texture; tourmaline-bearing; locally intensely crenulated; minor garnet-bearing gneiss and porphyry.|
70535|Redhackle Granite|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite granite/gneiss, megacrystic K-feldspar-bearing with rare mantled (rapakivi) feldspars; tourmaline-bearing; locally intensely crenulated; equigranular/seriate porphyritic and 'orbicular'; sheared and muscovitised textural variants.|
70535|Redhackle Granite|69427|4|Described|p12:30 Fig.12.28; 12:32, 44|Statherian|Statherian|Donnellan (2008). Sparse outcrops in the vicinity of Giles Range, W of Mount Stafford. Included in a map of 1780-1740 Ma granites in the Aileron Province. Syntectonic with Yambah Event; affected by Chewings Orogeny. SHRIMP U-Pb zircon age. Two metamorphic zircon rims similarly dated at 1579 +/- 7 Ma (Chewings Orogeny).|1772 +/- 3 Ma (Worden et al., 2004).|||Intrudes Lander Rock Formation. Is faulted against Mount Thomas Quartzite.|Grey, K-feldspar porphyritic biotite granite typically with a gneissic fabric; late pegmatite and aplite occur, with biotitisation and tourmalinisation in the granite at the margins of pegmatite dykes.|12-JUL-16
70535|Redhackle Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1579 +/- 7 Ma (U-Pb zircon SHRIMP).|1772+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Gneissic biotite granite.|
70535|Redhackle Granite|71858|6|Mentioned|p5, p29, p69|||Aileron Province.|ca. 1772 Ma|||||
38406|Renner Group|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
38406|Renner Group|23733|6|Mentioned|p28 Tb.5|||In the Tennant Inlier.||||||28-NOV-06
38406|Renner Group|23809|6|Mentioned|p27 Fig. 25|||||||||30-MAR-05
38406|Renner Group|23937|6|Mentioned|p23|||Correlated with the Roper Group.  Geological Province: Tennant creek Inlier.||||||
38406|Renner Group|24047|5|Briefly described|p7 Fig. 6, p9|Mesoproterozoic|Mesoproterozoic|Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||
38406|Renner Group|24303|2|Defined|p23, p59 Appendix|Calymmian|Calymmian|Formerly undifferentiated Tomkinson Creek beds.  The oldest units in the Renner Group are inferred to be slightly older than 1492 +/- 4 Ma by correlation with Roper Group stratigraphy of the McArthur Basin (cf Mainoru Formation, Jackson et al 1999) whereas the youngest unit in the Renner Group is inferred to be older than 1429 +/- 31 Ma (cf Kyalla Member, Kralik 1982). Unconformably overlies the Namerinni and Tomkinson Creek Groups. Unconformably overlain by Muckaty Sandstone Member.||||||10-SEP-14
38406|Renner Group|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Gleeson, Baralanji, Powell, Wiernty and Jangirulu Formations and the Lake Woods beds.||||||17-OCT-05
38406|Renner Group|24442|5|Briefly described|p14|Proterozoic|Proterozoic|Divided into Gleeson, Baralandji, Powell, Wiernty and Jangirulu Formations and the uppermost Lake Woods beds.  Unconformably overlies the Namerinni and Tomkinson Creek Groups.  Max. thickess: 3500m.  Geological Province: Ashburton Province.||||||
38406|Renner Group|50353|5|Briefly described|Map Legend|||||||||
38406|Renner Group|61406|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Undifferentiated rocks: quartz arenite, sublithic arenite, siltstone; minor mudstone and conglomerate; rare stromatolitic dolostone. In the Tennant Creek region.||||||12-OCT-05
38406|Renner Group|64443|6|Mentioned|p3, p4, p40|Mesoproterozoic||Correlative of South Nicholson Group; may unconformably underlie Barkly Group. Exposed in Tomkinson Creek (formerly Ashburton) Province.||||||
38406|Renner Group|64724|6|Mentioned|p45 Fig.5|Calymmian|Calymmian|Northern Tennant Creek Province||||||
38406|Renner Group|64780|5|Briefly described|p62 Fig.3, p63 Fig.4 |Mesoproterozoic|Mesoproterozoic||||Includes the Jangirulu and Gleeson Formations.|||
38406|Renner Group|65209|6|Mentioned|p38||||||Gleeson Formation|||
38406|Renner Group|65337|6|Mentioned|p86.|||Correlative with Accident Subgroup.||||||
38406|Renner Group|65344|4|Described|p3, 6,13,15-16, Figs. 2, 5, p7 Tbls 1, 2|Mesoproterozoic|Mesoproterozoic|Tennant Creek region. Underlies the Barkly Sub-basin, Georgina Basin. Correlated with the Roper Group of the McArthur Basin. See well logs and thin section description for detail.||||Underlies the Helen Springs Volcanics.|Quartz sandstone with mudstone wisps to interbeds.|03-MAY-12
38406|Renner Group|66860|6|Mentioned|p6 Tb.1|||||||||
38406|Renner Group|67175|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Tennant Region.|||Includes Gleeson Formation.||Quartz arenite, sublithic arenite, siltstone; minor mudstone and conglomerate; rare stromatolitic dolostone. Locally abundant halite pseudomorphs.|
38406|Renner Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||See also p36 Fig.4.10. Tennant Creek/Davenport area. Shown grouped with upper McNamara Group, in a tectonic time-slice diagram for the interval 1620-1570 Ma, as infill for a 1620-1590 Ma basin.|~1600-1590 Ma.||Baralandji, Jangirulu, Powell, Gleeson Formations.|Overlies Namerinni Group.||
38406|Renner Group|67352|5|Briefly described|p8, p11, p16, p17, p19, p45, p49, p51|||Hussey et al. (2001). Tomkinson Province version of South Nicholson Group. Floors much of central Georgina Basin.||||Tomkinson Province version of South Nicholson Group.||
38406|Renner Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|Tomkinson Basin.|||||Predominantly shallow marine sandstones.|12-JUL-16
38406|Renner Group|69424|6|Mentioned|p9:2, 27|Mesoproterozoic|Mesoproterozoic||||Gleeson Formation.|||12-JUL-16
38406|Renner Group|69425|6|Mentioned|p10:2|||Tennant Region.||||||12-JUL-16
38406|Renner Group|69429|6|Mentioned|p14:4 Fig.14.7|Mesoproterozoic|Mesoproterozoic|Tomkinson Province.||||||12-JUL-16
38406|Renner Group|69430|5|Briefly described|p15:26|Mesoproterozoic|Mesoproterozoic|Tomkinson Province.||||Correlated with Roper Group (McArthur Basin).||12-JUL-16
38406|Renner Group|69431|4|Described|p16:1-4, 14-15, 17-23|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. Over 3500m thick succession of fluviatile and shallow-marine sedimentary rocks. Is intruded by dolerite sills which are correlated with the c.1324 Ma Derim Derim Dolerite. Faulting and folding briefly discussed.|c.1500-1430 Ma.||Gleeson, Baralandji, Powell, Wiernty, Jangirulu Formations; Lake Woods beds.|Unconformably overlies Tomkinson Creek and Namerinni Groups. Is overlain unconformably by Muckaty Sandstone Member (Helen Springs Volcanics) and Anthony Lagoon Formation. Correlated with Roper Group.|Unmetamorphosed.|12-JUL-16
38406|Renner Group|69443|5|Briefly described|p28:21-22|Mesoproterozoic|Mesoproterozoic|Tomkinson Province.||||Is overlain dis/unconformably by Wonarah Formation (Barkly Group). Correlated with South Nicholson Group.||12-JUL-16
38406|Renner Group|69591|6|Mentioned|p109 Fig.2.106|||Appears in a diagram of the geodynamic setting of ~1620-1570 Ma eastern Australia.||||||
38406|Renner Group|69673|6|Mentioned|p3 fig 2, p57, p58|Mesoproterozoic|Mesoproterozoic|3500m thick. Also correlated with Roper Group, South Nicholson Group, Tijunna Group.||||Unconformably overlies the Namerinni Group, Tomkinson Creek Group, Unconformably overlain by Muckaty Sandstone Member, Anthony Lagoon Formation.||
38406|Renner Group|70968|3|Fully described|v-vi, p2-3, p92-115, p120, p123-124|Ectasian|Calymmian|See also p126-131, p137-140, p143. Hussey, Beier, Crispe and Donnellan in Hussey et al. (2001). Tomkinson Province. Named after Renner Springs. Originally named Ashburton Sandstone (Noakes and Traves, 1954); later as the upper part of Tomkinson Creek beds (Randal et al., 1966). Part of the Wilton package. Over 3500m thick. Depositional environments include shallow-marine shelf and shoreline, and intertidal, supratidal and fluvial facies. Detrital zircon spectra discussed. Several Formations are intruded by unnamed dolerite sills dated at 1295 +/- 14 Ma (Melville, 2010).|||Gleeson, Baralandji, Powell, Wiernty, Jangirulu Formations; Lake Woods beds.|Unconformably overlies the Namerinni and Tomkinson Creek Groups. Is overlain unconformably by Muckaty Sandstone Member (Helen Springs Volcanics). Correlated with Roper and Tijunna Groups.|Sandstone- and subordinate mudrock-rich units.|24-FEB-17
38406|Renner Group|71059|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Tomkinson Province.||||Equivalent to the Roper Group.||
38406|Renner Group|71374|5|Briefly described|p2|||Tomkinson Province.||||Broadly equivalent to the Roper Group and Tijunna Group.||
38406|Renner Group|71488|6|Mentioned|p142|||Tomkinson Province.||||||
38406|Renner Group|71779|5|Briefly described|p5, p23-p24, p26-p27|||Tomkinson Province. Probably equivalent to the Velkerri Formation.|||Includes the Lake Woods beds.|||
38406|Renner Group|71893|4|Described|iii, p1-p3, p6, p8, p52-p54|Ectasian|Statherian|Tomkinson Province. This group is interpreted to range from Statherian to Ectasian on the basis of dating of the unconformably underlying Namerinni Group and a SHRIMP U-Pb date of 1295 +/- 14 Ma for an unnamed dyke which intrudes this group. See also p56, p58, p62-p64, p66.|||Includes the Gleeson Formation, Baralandji Formation, Powell Formation, Jangirulu Formation, Wiernty Formation and Lake Wood beds.|Unconformably overlies the Namerinni and Tomkinson Creek groups.||
38406|Renner Group|72373|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of Tomkinson Province. Broadly equivalent to Wilton package, Roper Group (McArthur Basin) and Tijunna Group (Birrindudu Basin).||||||
38406|Renner Group|72381|5|Briefly described|p773|||Geological province: Tomkinson Province.||||Correlatable with Wilton Package, Roper Group (McArthur Basin) and Birrindudu Group (Birrindudu Basin).||04-OCT-19
38406|Renner Group|73242|6|Mentioned|p46|||Tomkinson Province. Intruded by a 1295 +/- 14 Ma gabbro.||||||
42230|Repulse Aplite|23809|4|Described|p4|||Possibly an informal name referring to an aplite dyke cutting the Tanami Group in the Tanami Gold Mine.  Age: stated to be <2528+/-5Ma but as this aplite intrudes Proterozoic stratigraphy it is concluded it cannot be Archaean.  Thickness of dyke: 3-4m.||||||06-DEC-04
76088|Reward Dolostone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1   |||See also p14 Tb.5, p17. Called Dolomite in Tb.1 and 5.||Of the Umbolooga Subgroup.||||
76088|Reward Dolostone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming and recessive.||Unit in Umbolooga Subgroup.||Overlies Barney Creek Formation.|Dololutite, stromatolitic dololutite, silty dololutite and dolarenite with lesser sandy dolarenite, dolorudite and sandstone; laminated, thinly to massive bedded, cross-bedded, brecciated and slumped; oncoids, ooids and silica spheroids.|
76088|Reward Dolostone|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. 350 m thick.||Umbolooga Subgroup||Overlies Barney Creek Formation (comformably to discomformably).|Dolomudstone, silty dolomudstone, dolostone, quartzic dolostone, dolomitic quartz sandstone: laminated to thinly to massive bedded; breccia.|
76088|Reward Dolostone|69418|6|Mentioned|p3:11|||McArthur Basin. Hosts Pb-Zn deposits (described).||||||12-JUL-16
76088|Reward Dolostone|69430|4|Described|p15:3, 14, 16, 19, 34-35, 39-42, 48, 57|Statherian|Statherian|Southern McArthur Basin. Ridge-forming and recessive. 30-350m thick. Shallow-marine upward-shallowing cycles, local high-energy to peritidal deposits. Sedimentary features include pseudomorphs after sulfate evaporites and pyrite (pyritohedra), onkoids, ooids and small silica spheroids. There is a paleoregolith developed on the surface of this unit. Hosts various base metal (Pb-Zn-Ag +/-Cu) deposits (described).||Umbolooga Subgroup.||Conformably (locally disconformably) overlies Barney Creek Formation. Is overlain disconformably or unconformably by Caranbirini Member (Lynott Formation), but may be locally transitional.|Dololutite, stromatolitic dololutite, silty dololutite and dolarenite with lesser sandy dolarenite, dolorudite and sandstone; laminated, thinly to massive bedded, cross-bedded, brecciated and slumped.|12-JUL-16
76088|Reward Dolostone|69673|6|Mentioned|p18, p34, p40, p41, p42, p44|||Batten Fault Zone. Reservoir rock.||Umbolooga Subgroup||Overlies Barney Creek Formation, unconformably overlain by Lynott Formation||
76088|Reward Dolostone|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 Barney Creek Formation and unconformably underlies Lynott Formation and Hot Springs Member.||
76088|Reward Dolostone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group||Underlain by Barney Creek Formation including HYC Pyritic Shale Member and Cooley Dolostone Member. Overlain by Caranbirini Member and Lynott Formation (Batten Sub-group).||
76088|Reward Dolostone|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Batten Fault Zone of the Southern McArthur Basin.||Batten Subgroup||Overlies Barney Creek Formation and unconformably underlies Lynott Formation and Hot Springs Member.||
76088|Reward Dolostone|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin.||Batten Subgroup, McArthur Group||Underlain by Barney Creek Formation. Unconformably overlain by Lynott Formation.||
76088|Reward Dolostone|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].||||||
76088|Reward Dolostone|73412|5|Briefly described|p4, 8, 19|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Barney Creek Formation. Is overlain unconformably by Lynott Formation (Batten Subgroup).||
25441|Reynolds River Granite|22810|5|Briefly described|P17|||||||||
25441|Reynolds River Granite|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Granite, adamellite.||||||07-NOV-08
25441|Reynolds River Granite|23714|4|Described|p17|||See also page 14, Table 2. Litchfield Province.||||||
25441|Reynolds River Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly S-type. In the Cullen Batholith, of the Rum Jungle and Central Region.||||||28-NOV-06
25441|Reynolds River Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Wagait Suite. Age: ~1850Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
25441|Reynolds River Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
25441|Reynolds River Granite|41980|5|Briefly described|Table 3 P575|||||||||
25441|Reynolds River Granite|45022|6|Mentioned|p.145. Pl.28.||Carpentarian|||||||
25441|Reynolds River Granite|46676|14|Not recorded|p.9|||||||||
25441|Reynolds River Granite|50586|5|Briefly described|p1.1, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Wagait Suite.||||||07-NOV-08
25441|Reynolds River Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma.  I-type. Granite, adamellite. Intrudes Burrell Creek Formation.||||||07-JAN-09
25441|Reynolds River Granite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Wagait Suite.|||Biotite leucogranite, quartz monzonite, porphyritic microgranite.|23-NOV-11
25441|Reynolds River Granite|69420|5|Briefly described|p5:18, 28-29|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Crops out as low pavements and small bouldery hills.||Wagait Suite.|||A small stock of light grey to pink, medium- to coarse-grained biotite granite to monzogranite. Locally, distinctively layered.|12-JUL-16
25441|Reynolds River Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Wagait Suite.|||Biotite leucogranite, quartz monzonite, porphyritic microgranite.|
29328|Ritarango Formation|22538|5|Briefly described|P715||Statherian|||||||
29328|Ritarango Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
29328|Ritarango Formation|24048|3|Fully described|p26|Statherian|Paleoproterozoic|Includes the upper half of the former "Ritarango beds".  Of the Donydji Group.  Max. thickness: 1500m.  Geological Province: McArthur Basin||||||07-NOV-08
29328|Ritarango Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Sandstone: maroon to white, fine to very coarse-grained, locally pebbly or conglomerate, lithic, cross-bedded; minor volcaniclastic sandstone, minor mudstone; locally foliated and sheared. Geol. Prov: McArthur Basin.||||||13-OCT-05
29328|Ritarango Formation|24050|6|Mentioned|p27|||||||||
29328|Ritarango Formation|44112|3|Fully described|p10,17, 30, 31, 34-35,110-111|Statherian|Orosirian|Belongs to Supersequence 1(D). Max Age: ~1870 Ma; Min Age: ~1710 Ma. Basal age constraint from Mirarrmina Complex. Min age from SHRIMP date in overlying Maidjunga Member (Page, pers. comm. 1992).||||||22-SEP-18
29328|Ritarango Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Donydji Group. Sandstone: maroon to white, fine to very coarse-grained, locally pebbly or conglomerate, lithic, cross-bedded; minor volcaniclastic sandstone, minor mudstone; locally foliated and sheared. Geol. Prov: McArthur Basin.||||||
29328|Ritarango Formation|63866|5|Briefly described|p114|||Leichhardt/Calvert Superbasins. |1707 +/- 12 Ma (Page, OZCHRON)|Donydji Group||Unconformably overlies the Dhunganda Formation.||
29328|Ritarango Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Walker Fault Zone, McArthur Basin.||Of the Donydji Group. ||||
29328|Ritarango Formation|69430|4|Described|p15:3-4, 6-7|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 500-1500m thick. Mostly shallow-water high-energy fluvial, and lesser low-energy deltaic, deposits.||Donydji Group.||Overlies Dhunganda Formation possibly unconformably. Is overlain by Fagan Volcanics conformably to disconformably.|Coarse-grained (partly conglomeratic) fluvial lithic sandstone; minor volcaniclastic sandstone; minor mudstone; locally foliated and sheared. Intruded by many rhyolite and basalt dykes and sills.|12-JUL-16
29328|Ritarango Formation|69673|4|Described|p16 fig 13, p17|Statherian||2km thick.|min age 1710 Ma|Donydji Group||Overlain by Maidjunga Member,|Sandstone, shale and bimodal volcanics.|22-SEP-18
29328|Ritarango Formation|72377|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||||Underlain unconformably by Dhunganda Formation.||
40577|River Supersequence|62535|5|Briefly described|p672, p674|Statherian|Statherian|Isa Superbasin.|c.1640 - c.1630 Ma.|||||
40577|River Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Lynott and Barney Creek Formations, Teena and Emmerugga Dolostones, Leila Sandstone,  Myrtle Shale.|||
40577|River Supersequence|63866|5|Briefly described|p53-p54, p57|||Isa Superbasin.|||Includes the Teena Dolomite, Lynott Formation and the Riversleigh Formation.|||
40577|River Supersequence|65228|5|Briefly described|p16, p29, pp31-35, Figs.11, 19-22.|Statherian|Statherian|Best preserved in southern Lawn Hill Platform. Informally named after the Riversleigh Siltstone, which contains the maximum flooding surface. Comprises upper Umbolooga Subgroup and lower Batten Subgroup. Includes Teena Dolomite to top of Yalco Formation. Gamma ray log, lithology and facies detailed.|c.1640 Ma.|||Is overlain by Term Supersequence.||
40577|River Supersequence|65337|6|Mentioned|p33 Fig.27.|||Its beginning is marked by the Bullrush Conglomerate lying unconformably on Drummond Formation.||||Overlies Loretta Supersequence. Is overlain by Term Supersequence.||
40577|River Supersequence|66843|6|Mentioned|p38 Fig.10|||Said to be "informally" named.||||||
40577|River Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40577|River Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier.|~1645-1635 Ma.|McNamara Group.||Overlies Loretta Supersequence. Is overlain by Term Supersequence.||
40577|River Supersequence|68732|6|Mentioned|p159, p165 Fig.5|||Includes Riversleigh Formation and Shady Bore Formation.||||||
40577|River Supersequence|69591|5|Briefly described|p27, p43, p46-47, p54, p108|||Mount Isa Province. Includes Shady Bore Quartzite and Riversleigh Siltstone. Formed in a N-S series of depocentres.||||Overlies Loretta Supersequence. Is overlain by Term Supersequence.|Deeper-water clastic turbidites, with syn-sedimentary pyrite and Zn/Pb mineralisation.|
40577|River Supersequence|70897|5|Briefly described|p39, Fig.1.7.1,3,7|||Shows rapid thickness and lithofacies variations across regional fault systems.||||Is overlain by Term Supersequence.||
40577|River Supersequence|72912|5|Briefly described|p13, p33 Fig.12, p35 Fig.13.|Statherian|Statherian|Of Lawn Hill Hill Platform, Isa Superbasin. Shown to contain the highest Hydrogen Index (mg/g TOC) of all the units analysed for the South Nicholson, Fickling and McNamara Groups, at c. 265mg/g TOC indicated likihood of being oil prone (uniquely) as well as gas prone. Data from Jarrett et al. (2019).|c. 1640-1630 Ma|||Overlies Loretta Supersequence and underlies Term Supersequence.||
40577|River Supersequence|73144|4|Described|p4-5, p8-9, p11-12, p20, p25, p45, p49|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains four third order sequences labelled 5-8 representing those found on the southern flanks of the Murphy Inlier. All eight are reported on the central Lawn Hill Platform [see article for more detail on third order sequences]. Deposited in shallow-midouter shelfal environments, deep marine with some submarine fans and turbidites (Southgate et al., 2000). Drilling at Egilabria-4 has confirmed the presence of multiple thick and organic-rich shale gas intervals (Riversleigh Shale Gas Play). Potential source rock but modelled as overmature with 2% EqVR at Desert Creek 1 and Egilabria 1 wells. SHRIMP ages indicate it was probably deposited between 1645 and 1630 Ma (Krassay et al., 2000).  Contemporaneous deposition with the River Event, at ~1640 Ma associated with north-south extension.|1630-1645 Ma|||Includes Riversleigh Siltstone and Shady Bore Quartzite.|Siltstone, silty shale, lithic sandstone and sandstone.|
24472|Riversleigh Siltstone|22438|6|Mentioned|p549, Fig.12|||||||||
24472|Riversleigh Siltstone|22665|6|Mentioned|P231|||||||||
24472|Riversleigh Siltstone|22680|6|Mentioned|83,85,87|||Geological province: Mount Isa Basin. Of the McNamara Group.||||||28-NOV-06
24472|Riversleigh Siltstone|23031|6|Mentioned|40|||Geological  province: Lawn Hill Subprovince. Of the McNamara Group. Overlain by Termite Range Formation.||||||28-NOV-06
24472|Riversleigh Siltstone|23072|5|Briefly described|p754|||||||||
24472|Riversleigh Siltstone|23362|6|Mentioned|339 Fig.2|||||||||
24472|Riversleigh Siltstone|23387|6|Mentioned|p18 fig.19|||Of McNamara Group.||||||
24472|Riversleigh Siltstone|23393|4|Described|p19, p20|Paleoproterozoic|Paleoproterozoic|Of McNamara Group.  Overlain by Termite Range Formation.||||||07-NOV-08
24472|Riversleigh Siltstone|23396|5|Briefly described|p407 Fig.2|Statherian|Statherian|Of the McNamara Group. Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23397|5|Briefly described|p472|Statherian|Statherian|Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23398|4|Described|p450|Statherian|Statherian|Of McNamara Group. Age: 1647+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23405|5|Briefly described|p565|||Of McNamara Group.||||||
24472|Riversleigh Siltstone|23406|5|Briefly described|p614|Statherian|Statherian|Of McNamara Group. Age: 1644+/-8Ma.||||||16-JUN-09
24472|Riversleigh Siltstone|23408|5|Briefly described|p513 Fig.2|||Of the McNamara Group.||||||28-NOV-06
24472|Riversleigh Siltstone|23409|4|Described|p541|Statherian|Statherian|Age: 1644+/-8Ma.||||||28-NOV-06
24472|Riversleigh Siltstone|23466|5|Briefly described|p272 Fig.6|Statherian|Statherian|||||||
24472|Riversleigh Siltstone|23958|3|Fully described|p1135|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Maximum thickness: 2900m.||||||07-NOV-08
24472|Riversleigh Siltstone|23964|5|Briefly described|p1268|Proterozoic|Proterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.  Maximum thicknees: 3200m. See also p1269 Table 1.||||||01-OCT-08
24472|Riversleigh Siltstone|23965|5|Briefly described|p1297|Mesoproterozoic|Paleoproterozoic|Of McNamara Group. Geological Province: Mount Isa Inlier.||||||07-NOV-08
24472|Riversleigh Siltstone|24309|5|Briefly described|p1013|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24472|Riversleigh Siltstone|24432|4|Described|p562 Fig.2|Statherian|Statherian|Of McNamara Group. Overlies Shady Bore Quartzite. Overlain by Termite Range Formation. Age: 1644-1636 Ma. Geological Province: Lawn Hill Platform.||||||
24472|Riversleigh Siltstone|36227|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|37459|2|Defined|p431|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian||||||
24472|Riversleigh Siltstone|38237|4|Described|p129|||||||||
24472|Riversleigh Siltstone|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|38310|6|Mentioned|p237|||||||||
24472|Riversleigh Siltstone|38348|4|Described|p15|||||||||
24472|Riversleigh Siltstone|38584|6|Mentioned|p22|||||||||
24472|Riversleigh Siltstone|39445|5|Briefly described|Table 2|||||||||
24472|Riversleigh Siltstone|39497|6|Mentioned|p13|||See also Fig.4||||||
24472|Riversleigh Siltstone|39562|5|Briefly described|Map legend|Carpentarian|Carpentarian|Top unit in McNamara Group. Laminated fine siltstone and shale with thin interbeds of coarse siltstone and fine sandstone.||||||15-JUN-06
24472|Riversleigh Siltstone|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|39925|6|Mentioned|Fig.9|||||||||
24472|Riversleigh Siltstone|40004|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
24472|Riversleigh Siltstone|40221|4|Described|p19|||||||||
24472|Riversleigh Siltstone|41298|6|Mentioned|Map legend|Carpentarian||||||||
24472|Riversleigh Siltstone|43486|5|Briefly described|21||Paleoproterozoic|Of the Upper McNamara Group.||||||07-NOV-08
24472|Riversleigh Siltstone|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of McNamara Group.||||||
24472|Riversleigh Siltstone|45166|5|Briefly described|p30|||See also p71.||||||28-NOV-06
24472|Riversleigh Siltstone|47083|5|Briefly described|p18||Proterozoic|Of McNamara Group. Underlain by Shady Bore Quartzite.||||||28-NOV-06
24472|Riversleigh Siltstone|50550|5|Briefly described|p1139 Fig.2||Statherian|Age: c.1644 Ma. Conformably overlies Shady Bore Siltstone, confromably overlain by Termite Range Formation. Geological Province: Western Fold Belt.||||||01-OCT-08
24472|Riversleigh Siltstone|50600|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the McNamara Group. Siltstone, carbonaceous siltstone and shale, massive to blocky, silicified very fine sandstone; dolomite, dolomitic siltstone, medium sandstone. Overlies Shady Bore Formation.||||||01-OCT-08
24472|Riversleigh Siltstone|60558|5|Briefly described|p5 Fig. 4|||Of McNamara Group. Overlain by Termite Range Formation, underlain by Shady Bore Quartzite.||||||
24472|Riversleigh Siltstone|61736|5|Briefly described|p674|||Of the McNamara Group. Age: 1644+/-8Ma.||||||
24472|Riversleigh Siltstone|61936|5|Briefly described|p194 Fig. 6|||Geological Province: Lawn Hill Platform, Western Fold Belt, Mount Isa Inlier. ||||||
24472|Riversleigh Siltstone|62084|4|Described|p936 Fig.5|||Isa Superbasin. Lawn Hill. Shown as Riversleigh Slst.|1647+/-8 Ma U-Pb SHRIMP (after Page et al. 2000)|McNamara Group|||Variably dolomitic organic siltstones and shales.|
24472|Riversleigh Siltstone|62535|5|Briefly described|p672, p674|Statherian|Statherian|Lawn Hill Platform. Hosts the Grevillea Pb-Zn-Ag prospect. Lithology not specified on p672.|1644 +/- 8 Ma.|McNamara Group.||||
24472|Riversleigh Siltstone|63109|6|Mentioned|p1108 Fig. 3|||Overlain by Termite Range Formation and Mount Les Siltstone. Geological Province: Isa Superbasin. Consists of siltstone.||||||30-SEP-08
24472|Riversleigh 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
24472|Riversleigh Siltstone|63113|6|Mentioned|p1214 Fig.2, p1219 Fig.8, p1225 Fig.13. |||Part of River supersequence. Shown as L.Riv.Sltst, M.Riv.Sltst, U.Riv.Sltst with their different lithologies, in Fig.2.|c.1644 Ma.|Of the McNamara Group||Overlies Shady Bore Quartzite or Lady Loretta Formation. Is overlain by Lawn Hill Formation or ?unconformably by Termite Range Formation.||
24472|Riversleigh Siltstone|63114|5|Briefly described|p1253 Fig.2, p1256, p1268. |||Isa superbasin. Appears only as Riversleigh in Fig.2. Hosts the Flat Tyre Zn-Pb prospect. Dolomite was added to this unit during mineralization.||Of the River supersequence.||||
24472|Riversleigh Siltstone|63115|6|Mentioned|p1279 Fig.4.|||Isa superbasin.||||||
24472|Riversleigh Siltstone|63116|6|Mentioned|p1297 Fig.2,p1299 Tb.1,p1300, |||Isa superbasin. Material properties detailed.||||||
24472|Riversleigh Siltstone|64575|6|Mentioned|p665|||||||||
24472|Riversleigh Siltstone|65228|5|Briefly described|p16, p33, Fig.04.|Statherian|Statherian|Mid-shelf to deep marine, commonly turbiditic clastic facies. Contains the maximum flooding surface of the River Supersequence, informally named after this unit.|1644 +/- 8 Ma (SHRIMP).|||||
24472|Riversleigh Siltstone|65337|5|Briefly described|p33 Fig.27.|||Correlative with Plain Creek Formation.|1647 +/- 8 to 1630 +/- 5 Ma (Page et al. 2000).|||Overlies Shady Bore Quartzite. Is overlain by Termite Range Formation.||
24472|Riversleigh 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; p9, p11. Mount Isa Inlier, Isa Superbasin. Camooweal - Murphy and Century Domains, Mount Isa Inlier. |1644 +/- 8 Ma.|McNamara Group.|||Laminated fine siltstone and shale with thin interbeds of coarse siltstone and fine sandstone.|
24472|Riversleigh Siltstone|68542|6|Mentioned|p6|||||Upper McNamara Group||Overlies Shady Bore Quartzite, disconformably overlain by Termite Range Formation||
24472|Riversleigh Siltstone|68576|5|Briefly described|Q_2: p6|||Lawn Hill Platform, Mount Isa Inlier. Hosts the Grevillea Zn-Pb-Ag deposit.||Upper McNamara Group.||Overlies Shady Bore Quartzite. Is overlain by Termite Range Formation.||
24472|Riversleigh Siltstone|69591|4|Described|p43 Fig.2.31, p46-47, p54|||Camooweal-Murphy and Century Domains, Isa Superbasin. Part of River Supersequence. Up to 3300m thick. The sandstone and quartzite beds are lowstand deposits: fluvial channels, shoreface deposits and deeper-marine turbidites and sand-rich submarine fans. See also reference to Riversleigh Formation (p108).|1644 +/- 7 Ma (MDA: Page et al., 2000).|McNamara Group.||Equivalent to Mount Les Siltstone.|Mainly laminated fine siltstone and shale, with several sandstone and locally quartzite interbeds.|
24472|Riversleigh Siltstone|69673|6|Mentioned|p54|||High enough TOC to be considered valid source rock.||||Correlated with Plain Creek Formation||
24472|Riversleigh Siltstone|70897|6|Mentioned|Fig.1.7.7|||Isa Superbasin.||||||
24472|Riversleigh Siltstone|71592|5|Briefly described|Appendix A.|||Mount Isa Orogen.|1647+/-8 Ma.||||Shale.|
24472|Riversleigh Siltstone|71863|6|Mentioned|p2|Proterozoic|Proterozoic|Isa Superbasin.||||||
24472|Riversleigh Siltstone|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.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of McNamara Group.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|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.|||Laminated siltstone and shale with thin interbeds of very fine to fine-grained sandstone|
24472|Riversleigh Siltstone|72526|5|Briefly described|p8 Fig.1.3, p10.|Statherian|Statherian|Shown as located in the Lawn Hill Platform of the Mount Isa Province and the east part of the South Nicholson Basin. Age given as U-Pb zircon sedimentary depositional age.|1647 +/- 8 Ma, 1644 +/- 8 Ma|McNamara Group||Conformably overlies Shady Bore Quartzite and underlies Termite Range Formation.||
24472|Riversleigh Siltstone|72527|6|Mentioned|p132.|Statherian|Statherian|Tuff ages considered 'reasonably firm' age constraints. Variation on Riversleigh Formation.|1647+/-8 Ma. 1644+/-8 Ma|McNamara Group||Correlative with Plain Creek Formation, Termite Range Formation.|Includes tuffaceous horizons.|
24472|Riversleigh Siltstone|72912|4|Described|p5 Fig.3, p14, p32, 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 Isa Superbasin, Mount Isa Province, and the East part of the South Nicholson Basin. Also shown as Riversleigh Formation p32, 45. See also p45-46, p49.||McNamara Group||Overlies Shady Bore Quartzite and underlies Termite Range Formation.|Includes organic rich siltstone and shales.|
24472|Riversleigh Siltstone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p22, 23, 26|Paleoproterozoic|Paleoproterozoic|Shown as being in the eastern and Lawn Hill Platform part of the Isa Superbasin. Identified in 3 wells in this study.  Mineral composition shows majority quartz, microcline, muscovite and dolomite.|1644 +/- 5 Ma|McNamara Group||Overlies Shady Bore Quartzite and underlies Termite Range Formation.|Includes organic rich siltstone.|
24472|Riversleigh Siltstone|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.||McNamara Group||||
24472|Riversleigh Siltstone|73042|5|Briefly described|p1, p4, p6, p11-13|Statherian|Statherian|South Nicholson Basin region and Mount Isa Province, Isa Superbasin. Re-Os age overlaps with existing zircon depositional age constraints including zircon U-Pb geochronology of tuff and tuffaceous intervals (ca 1647-1644 Ma, Page et al., 2000); the unit is an important source rock in the Isa Superbasin.|1608 +/- 40 Ma Re-Os|McNamara Group||Conformably underlain by the Shady Bore Quartzite. Unconformably overlain by the Termite Range Formation.|Siltstone, shale, sandstone, dolomitic and carbonaceous siltstone.|23-JUN-22
24472|Riversleigh Siltstone|73098|6|Mentioned|p4, p7, p25|||Lawn Hill Platform. Organic petrolography performed on four samples from the Amoco DDH 83-1 well. [See report for bitumen/maceral description].|||||Includes weakly laminated dark brown to dark grey shale.|
24472|Riversleigh Siltstone|73144|6|Mentioned|p8-9|Statherian|Statherian|Isa Superbasin. River Supersequence. Aquifer. Potential shale gas/oil play. Includes oil show and gas show.||McNamara Group||Unconformably underlain by Lady Loretta Formation. Overlain by Termite Range Formation.||
24472|Riversleigh Siltstone|73525|5|Briefly described|p4-5 Fig.2|Statherian|Statherian|Mount Oxide-(Ardmore-May Downs) Domain.|1647+/-8 Ma crystallisation of volcanic rock||||Carbonates, siliciclastics.|
24476|Rooneys Formation|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgroup. Of the Hatches Creek Group.||||||07-NOV-08
24476|Rooneys Formation|23733|5|Briefly described|p15|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Intruded by Elkedra Granite.  Age: >1710Ma.||||||30-SEP-11
24476|Rooneys Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Ooradidgee Group.  Geological Province: Davenport Province.||||||29-NOV-04
24476|Rooneys Formation|24172|5|Briefly described|p66 Tb.9|||Of the Ooradidgee Subgroup. Geological Province: Tennant Creek Inlier. Of Hatches Creek Group. Greywacke, siltstone, feldspathic and/or lithic arenite. With the Kurninelli Sandstone constitutes a deltaic complex.||||||28-NOV-06
24476|Rooneys Formation|39624|5|Briefly described|Table 1|||||||||
24476|Rooneys Formation|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24476|Rooneys Formation|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24476|Rooneys Formation|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Feldspathic and lithic arenite with micaceous siltstone, laminated to thin bedded; minor feldspathic arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24476|Rooneys Formation|41129|4|Described|Table 1|||||||||
24476|Rooneys Formation|41308|5|Briefly described|Table 2|||||||||
24476|Rooneys Formation|41408|6|Mentioned|Map legend|Proterozoic||||||||
24476|Rooneys Formation|41524|4|Described|Table 1|||||||||
24476|Rooneys Formation|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Siltstone, thin-bedded; ferruginous; minor arenite; felsic volcanics.||||||07-NOV-08
24476|Rooneys Formation|41970|6|Mentioned|Fig.3 P333|||||||||
24476|Rooneys Formation|43223|5|Briefly described|Map Legend||Proterozoic|Of the Ooradidgee Subgroup.||||||28-NOV-06
24476|Rooneys Formation|43224|5|Briefly described|Map legend||Proterozoic|Of the Ooradidgee Subgroup.||||||28-NOV-06
24476|Rooneys Formation|43802|6|Mentioned|Table 1,p80|||||||||
24476|Rooneys Formation|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||28-NOV-06
24476|Rooneys Formation|49033|2|Defined|p8|Proterozoic|Proterozoic|||||||
24476|Rooneys Formation|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||28-NOV-06
24476|Rooneys Formation|50588|5|Briefly described|p4.4|||Intruded by: Devils Suite. See also Rooney Formation.||||||27-JUL-04
24476|Rooneys Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Greywacke, siltstone, subarkosic/sublithic/lithic arenite; minor felsic porphyry; locally schistose.  In the Tennant Creek region.||||||07-NOV-08
24476|Rooneys Formation|64068|5|Briefly described|pp194-197|Paleoproterozoic|Paleoproterozoic|Age said to be Mesoproterozoic p194, but elsewhere shown as Paleoproterozoic.Tosca (turquoise) mine area.  Mapped as 'Other Palaeoproterozoic' on the 1:500 000 southern Georgina Basin mapsheet.||Of Hatches Creek Group.||Is overlain by Kurinelli Sandstone. Is intruded by Elkedra Granite.|Ferruginous shale.|05-APR-12
24476|Rooneys Formation|64735|5|Briefly described|p206 Fig 2, p210|Orosirian|Orosirian|Intruded by dolerite sills dated at 1810 +/- 4.5 Ma, thus giving minimum deposition age.||Of Ooradidgee Group||||30-APR-12
24476|Rooneys Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
24476|Rooneys Formation|65338|6|Mentioned|p19.|||In LANDER RIVER area; more distal, thus likely to be dominated by clastic sedimentary rocks than volcanics.||||||
24476|Rooneys Formation|65342|6|Mentioned|p13. |Paleoproterozoic|Paleoproterozoic|Fine-grained sedimentary rocks.||Unit in Ooradidgee Group.||||
24476|Rooneys Formation|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Ooradidgee Group.||Overlies Epenarra Volcanics. Is overlain by Kurinelli Sandstone.|Feldspathic and lithic arenite with micaceous siltstone, laminated to thin-bedded; minor feldspathic arenite.|
24476|Rooneys Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.||Overlies (probably unconformably) Woodenjerrie Beds. Is overlain by Kurinelli Sandstone.|Greywacke, siltstone, subarkosic/sublithic/lithic arenite; minor felsic porphyry; locally schistose.|
24476|Rooneys Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Ooradidgee Group.||||
24476|Rooneys Formation|67352|4|Described|p11 Tb.1, p41, p54, p55|Orosirian|Orosirian|Over 1200 m thick. Generally recessive with low ridges, hills. Hosts gold in quartz veins in dolerite/gabbro and sandstone.||Ooradidgee Group||Conformably overlies/interfingers with Epenarra Volcanics. Intruded by Devils Suite. Overlain by Kurinelli Sandstone.|Feldspathic and lithic arenite: fine-grained; micaceous siltstone: laminated to thinly bedded|
24476|Rooneys Formation|68518|4|Described|p10 Tb.1, p11, p13|Proterozoic|Proterozoic|Mineral deposit: small copper prospect; no recorded production. Thickness: 1000+ m. Possibly deltaic origin.||Ooradidgee Subgroup||Overlain conformably by Kurinelli Sandstone and unconformably by Cambrian strata; intruded by Elkedra Granite and unnamed granodiorite. Base not seen.|Greywacke and siltstone; minor bands of feldspathic and sericitic arenite and felsic porphyry (possibly intrusive). Increasingly schistose eastwards. Metamorphosed to spotted micaceous schist and quartzitic hornfels within 100 m of Elkedra Granite.|30-MAY-16
24476|Rooneys Formation|69187|6|Mentioned|p53 Fig.2|||Warramunga Province.||||||
24476|Rooneys Formation|69424|4|Described|p9:3, 5, 15, 18, 23-26, 28,54|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Over 1200m thick. Deltaic, including delta-front, wave-affected deposits, and high-energy shoreface, including storm deposits. Age range from surrounding, interfingering units. Hosts Au-bearing quartz veins.|Between 1840 +/- 4 Ma and 1837 +/- 7 Ma.|Ooradidgee Group.||Conformably overlies and interfingers with Epenarra Volcanics. Is overlain conformably by, and interfingers with, Kurinelli Sandstone.|Thinly bedded to laminated, fine-grained feldspathic/lithic sandstone and siltstone; generally recessive, with minor ridge-forming arkose.|12-JUL-16
24476|Rooneys Formation|69425|4|Described|p10:3-8, 20, 23-25|||Small outcrop area in extreme SE of Davenport Province. 0 - c.1200m thick. Deltaic sedimentation including delta-front, wave-affected deposition and high-energy shoreface sedimentation including storm deposits. Elkedra Granite cross-cuts folding in this unit, thus providing a lower (c.1710 Ma) constraint on the Davenport Event. Associated with minor malachite in vein quartz.||Ooradidgee Group.||Conformably overlies and interfingers with Epenarra Volcanics. Is overlain conformably by and interfingers with Kurinelli Sandstone. Possibly equivalent to Bullion Schist. Intruded by Elkedra Granite.|Greywacke, thinly bedded to laminated, fine-grained feldspathic/lithic sandstone and siltstone; generally recessive with minor ridge-forming arkose. Variably micaceous and locally schistose.|12-JUL-16
24476|Rooneys Formation|73083|6|Mentioned|p21|||||||||
24476|Rooneys Formation|73124|6|Mentioned|p2 Fig.1|||||||Overlain by Kurinelli Sandstone. Equivalent to Epenarra Volcanics.||
24476|Rooneys Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
24476|Rooneys Formation|73460|6|Mentioned|p2|||Warramunga Province.||||Overlain by Kurinelli Sandstone. Equivalent to Epenarra Volcanics.||
24476|Rooneys Formation|73590|6|Mentioned|p2|||||Ooradidgee Group||Overlain by Kurinelli Sandstone. Equivalent to Epenarra Volcanics.||
22777|Rorruwuy Sandstone|22538|6|Mentioned|P715|||Part of the Goyder package.||||||28-NOV-06
22777|Rorruwuy Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
22777|Rorruwuy Sandstone|24048|3|Fully described|p37|||||||||
22777|Rorruwuy Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: white to pink, fine to medium-grained, quartzose, low-angle cross-bedded to flat-bedded, common ripples and mudclasts. Geol. Prov: McArthur Basin.||||||13-OCT-05
22777|Rorruwuy Sandstone|44112|2|Defined|p1,10,44,48,98,111|Statherian|Statherian|Max Age: ~1710 Ma.||||||28-NOV-06
22777|Rorruwuy Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: white to pink, fine to medium-grained, quartzose, low-angle cross-bedded to flat-bedded, common ripples and mudclas ts. Geol. Prov: McArthur Basin.||||||
22777|Rorruwuy Sandstone|63866|5|Briefly described|p114, p116|||Northern Caledon Shelf.||||Unconformably overlies the Cato Volcanics. Unconformably overlain by the Durabudboi beds.||
22777|Rorruwuy Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf North, McArthur Basin. Mis-spelt Rorruwoy in Fig.5.||Of the Spencer Creek Group.||||
22777|Rorruwuy Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot; p34|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Shallow marine to fluvial deposits.|~1690-1670 Ma.|||||
22777|Rorruwuy Sandstone|69430|5|Briefly described|p15:3, 13-14|||Rawlings et al. (1997); previously mapped as part of the Mount Bonner Sandstone. NE McArthur Basin. Shallow-water, possibly fan-delta or intertidal, deposits. Possible equivalent to Parsons Range Group.||Spencer Creek Group.|||White to pink, mature, silicified, fine- to medium-grained quartzic sandstone.|12-JUL-16
22777|Rorruwuy Sandstone|69673|6|Mentioned|p16 fig 13, p17|||Possibly equivalent to Parsons Range Group.||||||
22777|Rorruwuy Sandstone|71374|6|Mentioned|p24|||||Spencer Creek Group||||
22777|Rorruwuy Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Quartzose sandstone.|
22777|Rorruwuy Sandstone|72377|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Spencer Creek Group.||Similar stratigraphic position to Coast Range Sandstone.||
79075|Rover Field volcaniclastic|69187|5|Briefly described|p56-57, p60 Tb.1|Orosirian|Orosirian|Name clearly informal. Shown as Rover Field Volcaniclastic only in Fig.9. Area is SW of Tennant Creek. Indistinguishable ages of cores and rims suggest that both formed in the same magmatic event, and resultant age provides a crystallisation age for these grains. Lack of abrasion of zircon grains, dominant single age component and compositional and textural immaturity of the sample suggests that true depositional age might be close to maximum depositional age.|Max dep age: 1842.3+/-4.5 Ma Pb/Pb SHRIMP, zircon||||quartzofeldspathic rock - weakly metamorphosed volcaniclastic rocks|
36771|Rowley Granophyre|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Hull Granite Suite.  Age: ~1075Ma.||||||
36771|Rowley Granophyre|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1075Ma.  Of the Hull Granite Suite.||||||28-MAY-04
36771|Rowley Granophyre|61154|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Of Hull Suite. Porphyritic rock with plagioclase, K-feldspar and quartz phenocrysts in a groundmass of medium-coarse-grained quartz and feldspar; mafic minerals include biotite, chlorite and opaques.  Age: 1075+/-2Ma (Kober Pb-Pb). Geol.Prov: Musgrave Blo||||||
36771|Rowley Granophyre|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Hull Granite Suite (~1090-1075Ma). Finely porphyritic biotite-chlorite granophyre.||||||
36771|Rowley Granophyre|63866|5|Briefly described|p206|Stenian|Stenian|Musgrave Province.|1075 +/- 2 Ma (Close et al, 2003, Pb-Pb Kober)|Hull Suite||||
36771|Rowley Granophyre|65256|2|Defined|p7 Tb.1, p10,  p15-16, p30, p37, p41|Stenian|Stenian|New name. Zircon Pb-Pb evaporation age. Crosscut by mafic dykes interpreted to belong to Alcurra dolerite. Correlative of/geochemically similar to Walu Granite and Imbumbunna Granite.|1075+/-2 Ma (Close et al. 2003).|Of Hull Granite Suite.||Intrudes the middle section of the Tjauwata Group (Tjuninanta Formation).|Shallow level granite. Porphyritic biotite-epidote granite with fine-grained phenocrysts of feldspar.|19-MAY-14
36771|Rowley Granophyre|67128|5|Briefly described|p3, p12, p27|||Western Bloods Range. Kober Pb evaporation age.|1075 +/- 3 Ma.|||Cut by Alcurra Dolerite. Intrusive equivalent of Puntitjata Rhyolite.|Plagioclase, K-feldspar and quartz phenocrysts in a medium- to coarse-grained quartz and feldspar groundmass.|
36771|Rowley Granophyre|69436|5|Briefly described|p21:11|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Is cut by strongly sheared, poorly preserved mafic dykes, possibly Alcurra Dolerite. Kober Pb-Pb zircon age.|1075 +/- 2 Ma (Close et al., 2003).|Hull Suite.|||Porphyritic granophyre with plagioclase, K-feldspar and quartz phenocrysts in a groundmass of medium- to coarse-grained quartz and feldspar. Mafic minerals include biotite, chlorite and opaques.|12-JUL-16
39143|Ruby Gap Tonalite|23733|5|Briefly described|p34 Fig.20|||||||||
39143|Ruby Gap Tonalite|69932|6|Mentioned|p306|||Sm-Nd data tabulated. Presented as Ruby Gap tonalite.|1870 Ma.|Atnarpa Igneous Complex.||||
24482|Rungutjirba Gneiss|7837|6|Mentioned|p101|||U-Pb zircon geochronology by Zhao and Bennett (1995).|1615 +/- 11 Ma.|||||
24482|Rungutjirba Gneiss|23363|5|Briefly described|352 Tab.3|Statherian|Statherian|Age: 1615+/-11Ma.||||||28-NOV-06
24482|Rungutjirba 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
24482|Rungutjirba Gneiss|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24482|Rungutjirba Gneiss|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24482|Rungutjirba Gneiss|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24482|Rungutjirba Gneiss|39887|6|Mentioned|Fig.3|||||||||
24482|Rungutjirba Gneiss|39888|6|Mentioned|Fig.8|||||||||
24482|Rungutjirba Gneiss|41816|4|Described|p9|||||||||
24482|Rungutjirba Gneiss|41837|6|Mentioned|Map legend|Proterozoic||||||||
24482|Rungutjirba Gneiss|48992|2|Defined|p46|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24482|Rungutjirba Gneiss|50369|5|Briefly described|p1.5, 22.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Iwupataka Suite. Age: 1615 +/- 11Ma (SHRIMP).||||||07-NOV-08
24482|Rungutjirba Gneiss|68994|5|Briefly described|p5, p24|||Haasts Bluff Domain.|1615+/-11 Ma (Zhao and Bennett 1995).|||||13-JAN-17
24482|Rungutjirba Gneiss|69925|5|Briefly described|p18, 21, 23, 25, 30, 32, 40|||Southern Arunta Province, Arunta Inlier. Ion probe U-Pb isotope analyses tabulated.|1615 +/- 11 Ma (crystallisation).|||Is overlain conformably by Chewings Range Quartzite. Possible volcanic equivalent of Burt Bluff Gneiss.|Fairly homogeneous granitic gneiss. Finer-grained than Burt Bluff Gneiss.|
24482|Rungutjirba Gneiss|69931|6|Mentioned|p269, 273-274, 280-281, 296|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. REE analyses, Sm-Nd isotopic analyses, tabulated.||Burt-Rungutjirba Suite.|||Fine-grained or foliated granitic gneisses.|
24482|Rungutjirba Gneiss|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1615+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Felsic gneiss.|
41851|Russell Charnockite|67565|2|Defined|p64, p20-21, p6 Table 1, p17, p60, p62.|Statherian|Statherian|New name. Previously included in undifferentiated Arunta Complex (Ranford, 1969) and undifferentiated gneissic granite (Ranford, 1968). Yaya Domain, Warumpi Province. Type locality is northern edge of Ehrenberg Range. Scattered outcrops. Geochemically indistinguishable from, and correlated with, Talyi-Talyi Charnockite. Correlated also with Larrie Granodiorite. Metamorphosed at upper amphibolite facies.||Unit in Waluwiya Suite.||Intrudes Yaya Metamorphic Complex. Is intruded by Ehrenberg Granite and Ilpili Dolerite. Is faulted against the Alkipi Metamorphics.|Distinctive rock type; orthopyroxene- and clinopyroxene-bearing granite, commonly undeformed, with rounded quartz and zoned plagioclase phenocrysts; contains abundant mafic xenoliths; locally foliated with hornblende and leucosomes.|01-DEC-15
41851|Russell Charnockite|69428|5|Briefly described|p13:10-11|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Yaya Domain, Warumpi Province. Forms prominent hills at Mount Russell and in the Ehrenberg Range, and scattered small outcrops between the latter and Davenport Hills.||Waluwiya Suite.|||Distinctive rock, commonly undeformed, with abundant rounded plagioclase and pyroxene phenocrysts in a fine-grained granoblastic hornblende-bearing groundmass; abundant mafic xenoliths.|12-JUL-16
41851|Russell Charnockite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite|
41851|Russell Charnockite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.|||||Charnockite.|09-SEP-19
22797|Ryans Gap Metamorphics|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
22797|Ryans Gap Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of the Iwupataka Metamorphic Complex.||||||07-NOV-08
22797|Ryans Gap Metamorphics|43503|2|Defined|8,23,78|||||||||
22797|Ryans Gap Metamorphics|50369|5|Briefly described|p1.5, 22.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Iwupataka Suite.||||||07-NOV-08
22797|Ryans Gap Metamorphics|64809|6|Mentioned|p11 Fig.10 |Mesoproterozoic|Palaeoproterozoic|||||||
22797|Ryans Gap Metamorphics|67565|6|Mentioned|p7 Table 1, p13. |Paleoproterozoic|Paleoproterozoic|Correlated with Ikuntji Metamorphics by lithological affinities.||||||
22797|Ryans Gap Metamorphics|69428|5|Briefly described|p13:06|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995). Eastern Haasts Bluff Domain, Warumpi Province. Crops out extensively between Standley Chasm and Ormiston Gorge. May be a lateral equivalent of Ikuntji Metamorphics /Simpsons Gap Metasediments.||Iwupataka Metamorphic Complex.|||Layered and laminated quartzofeldspathic biotite-rich schist, overlain by muscovite-bearing quartzofeldspathic gneiss and schist interbedded with thin beds of quartz-rich sediments and, towards the top, layers of quartzite.|12-JUL-16
34027|Saint Vidgeon Formation|22538|6|Mentioned|Fig3 P709|||Saint actually spelt St||||||
34027|Saint Vidgeon Formation|23398|5|Briefly described|p444|Statherian|Statherian|Age: 1640+/-4Ma.||||||29-NOV-06
34027|Saint Vidgeon Formation|23937|2|Defined|p92 App. 1, p9|Statherian|Statherian|Formerly mapped as part of the Vizard Formation (Dunn, 1963a), which is now superseded by the Vizard Group.  Disconformably overlain by the Nagi Formation.  Age: 1640+/-4Ma (Page et al, 2000).  Max. thickness: 110m.  Geological Province: McArthur Basin.||||||29-NOV-06
34027|Saint Vidgeon Formation|60483|5|Briefly described|p7 Fig. 5|||Of the Vizard Group. Age: 1634+/-4Ma. Geological Province: McArthur Basin. Saint is St in text.||||||05-OCT-07
34027|Saint Vidgeon Formation|61390|5|Briefly described|Map Legend|Statherian|Statherian|Of the Vizard Group. Dolostone, tuffaceous and dolomitic siltstones.||||||30-SEP-05
34027|Saint Vidgeon Formation|64817|6|Mentioned|p353 Fig.4|||||Of the Vizard Group.||||
34027|Saint Vidgeon Formation|65228|5|Briefly described|p35, Table 1|Statherian|Statherian|St Vidgeon in text. Of Abbott et al, in press (as of 2000). Possibly equivalent (similar facies and evaporite pseudomorphs) to Teena Dolomite and Barney Creek Formation. Measured section.|1640 +/- 4 Ma (SHRIMP).|Unit in Vizard Group.||Is overlain by Nagi Formation.|Carbonate and siltstone.|
34027|Saint Vidgeon Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1640 +/- 4 Ma.|||||
34027|Saint Vidgeon Formation|69430|4|Described|p15:3, 18, 22-23, 30|Statherian|Statherian|Southern McArthur Basin. 110m thick. Upward-fining and -deepening succession, from shallow-marine into locally anoxic shale facies. Contains stromatolites and "Coxco Needles" which are a distinctive feature of the apparently coeval Coxco Dolostone Member. A unit of silicified conical stromatolites commonly caps the Formation. SHRIMP U-Pb zircon age from a tuff bed.|1640 +/- 4 Ma; 1634 +/- 4 Ma.|Vizard Group.||Base not seen. Is overlain disconformably by Nagi Formation. Time-equivalent of Barney Creek Formation.|A succession of dolostone, dolomitic and tuffaceous siltstone, K-metasomatised sedimentary rocks, tuff and chert. At the top are silty dololutite and fine dolomitic sandstone, pyritic black shale, and rare interbeds of dolomitic sandstone.|12-JUL-16
34027|Saint Vidgeon Formation|69673|6|Mentioned|p16 fig 13, p31|Statherian|Statherian|Urapunga Fault Zone|1634 +/- 4 Ma, 1640 +/- 4 Ma|Vizard Group||Overlain by Nagi Formation, Correlated with Barney Creek Formation|Dolostone, dolomitic and tuffaceous siltstone, potassium metasomatised sedimentary rock and chert.|
34027|Saint Vidgeon Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1640+/-4 Ma (MDA: U-Pb zircon SHRIMP)||||Tuffite.|
34027|Saint Vidgeon Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Vizard Group.|||Carbonaceous-pyritic shale and dolomitic siltstone, dolostone; minor pink chert beds (tuff?).|04-MAR-20
34027|Saint Vidgeon Formation|72373|5|Briefly described|p24-25|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Includes 1640+\-4 Ma tuffaceous unit (SHRIMP U-Pb zircon age; Page e al., 2000).||||Overlain unconformably by Nagi Formation.||02-OCT-19
34027|Saint Vidgeon Formation|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin. Age given as U-Pb zircon sedimentary depositional age.|1640 +/-4 Ma|Vizard Group||Underlies Nagi Formation.||
34027|Saint Vidgeon Formation|72718|6|Mentioned|p7|Statherian|Statherian|Southern McArthur Basin. Urapunga Fault Zone.|1634 +/- 4 Ma, 1640 +/- 4 Ma|Vizard Group||Overlain by Nagi Formation.||
34027|Saint Vidgeon Formation|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Urapunga Fault Zone. U-Pb zircon sedimentary depositional age (Ma).|1640 +/- 4 Ma|Vizard Group||Underlies Nagi Formation.||
34027|Saint Vidgeon Formation|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1640 +/- 4 Ma (see Fig.1.2)|Vizard Group||Overlain by Nagi Formation.||
81827|Sainthill Suite|73591|6|Mentioned|p14, p36||||ca 1730-1710 Ma||Marshall Granite, Jinka Granite|||
81146|Salthole Gneiss|71255|4|Described|p1-2, p5|Paleoproterozoic|Paleoproterozoic|Aileron province, Arunta Region. Juxtaposed against thrust slices of basal Neoproterozoic stratigraphy of the Aadeus Basin via the Illogwa Shear Zone. SHRIMP U-Pb dating yields 1769.3+\-2.8 Ma (Kositcin et al., 2011), and is likely to represent partial recrystallisation and/or new zircon growth during contact etaorphis with Arera Granodiorite. Hf isotopic results gives two-stage odel ages ranging fro 1.84-2.2 Ga, indicating that the agatic protolith was likely derived from mixing between recycled, or evolved Paleoproterozoic component and juvenile Paleoproterozoic crust.|1793.8 +/- 2.9 Ma crystallisation age.|||Intruded by Aremra Granodiorite.|Mylonitic biotite-quartz-feldspar schistose gneiss sampled.|19-JUN-19
81146|Salthole Gneiss|73551|5|Briefly described|piii, p3, p18|Statherian|Orosirian|Granitic protolith was emplaced at 1794 +/- 3 Ma (Kositcin et al., 2011). A muscovite 40Ar/39Ar age records cooling below ca 430-390C at 327 +/- 2 Ma.|ca 1.79 Ga||||Includes quartz-biotite-muscovite schist/mylonite.|
26131|Samarkand Pegmatite|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Tourmaline pegmatite; rare aplite: locally layered, white. Geological Province: Arunta Block.||||||07-NOV-08
26131|Samarkand Pegmatite|40906|4|Described|p16|||||||||
26131|Samarkand Pegmatite|49036|2|Defined|p11|Paleoproterozoic|Paleoproterozoic|Previously included in the Arunta Complex.||||||07-NOV-08
26131|Samarkand Pegmatite|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Pegmatite. Geological Province: Arunta Block.||||||17-NOV-04
26131|Samarkand Pegmatite|71621|6|Mentioned|p1|||Sample HU14BLR532, elsewhere (p47) described as 'unnamed pegmatiite' contained no zircon.|||||Pegmatite.|02-FEB-19
26131|Samarkand Pegmatite|72370|5|Briefly described|p1,4,15-16|||Geological province: Aileron Province. Previous dating of Samarkand Pegmatite at the Samarkand and Jericho tungsten prospects include Rb-Sr whole rock ages of 1680+\-60 Ma and 1680+\-30 Ma, and Rb-Sr muscovite ages of c. 1708 Ma and 1695 Ma respectively (Dobos 1978).||||Crosscuts White Violet Orthogneiss, Bonya Metamorphics and Kings Legend Metadolerite.||
26131|Samarkand Pegmatite|72372|5|Briefly described|p6,17,24,28,30, 35, 36|Statherian|Statherian|Geological province: Aileron Province. S-type flelsic magmatism in the NE Aileron Province, post-dating D2 and D3 deformation in the Bonya Hills area and associated with epigenetic mineralisation. Has poorly constrained 207Pb/206Pb apatite crystallisation age of ca 1.70 Ga from the Samarkand W-Cu prospect, providing approximate minimum age for epigenetic tungsten mineralisation in the study area (McGloin and Weisheit in review).|||||Tourmaline-bearing pegmatite.|10-OCT-19
26131|Samarkand Pegmatite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.||||Unconformably overlain by the Plenty Group.|Pegmatite, pegmatitic granite and leucogranite, fine- to coarse-grained to megacrystic.|
26131|Samarkand Pegmatite|72516|3|Fully described|p10, p14-18, p21, p24-25, p29, p75-76|Statherian|Statherian|Aileron Province. Named for the Samarkand tungsten deposit and was first defined by Shaw et al (1985). Mineralogically and compositionally similar to an undivided pegmatite in the Bonya and Jervois domains. Occurs primarily in the Bonya Domain but is also identified in the Jervois and Jinka domains. Intrusion characteristics, petrography, geophysics and economic geology are discussed.Outcrop is generally highly weathered with a jointed and dissected appearance. Structure, geochemistry, geophysics and metamorphism are discussed. See also  p32, p35, p42, p49, p56, p60, p71, p75-77, p113-116, p118, p122-123, p125-126, p135-137, p139, p143-145, p171, p173, p189.|1635 +/- 87 Ma (minimum cryst. Age)|||Intrudes the Bonya Metamorphics and Mascotte Orthogneiss, White Violet Orthogneiss, Kings Legend Metadolerite, Jericho Granite and Cappocks Granodiorite.|Pegmatite, pegmatitic granite and leucogranite: fine to coarse-grained to megacrystic, muscovite-tourmaline-bearing, rare beryl and garnet.|04-JUL-22
26131|Samarkand Pegmatite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|From the interpretive geology map of the Jervois Range Special (modified from Weisheit et al 2019). Shown as part of the Aileron Province.|||||Includes pegmatite.|
74206|Sandbar Sandstone|61542|5|Briefly described|p277 Fig. 2, p285|Visean|Visean|Newly added to the Weaber Group -  forms part of revision by authors. Overlain by Sunbird Fm.which may(?) truncate it, or it pinches out. Geological Province: onshore Bonapart Basin/offshore Petrel-Sub-basin. tyep section in offshore Sandbar-1.||||Overlain by Sunbrid Formation. Overlies Tanmurra Fm.||26-NOV-18
74206|Sandbar Sandstone|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Tanmurra Formation. Is overlain unconformably by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||
74206|Sandbar Sandstone|69673|6|Mentioned|p168 fi, p 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74206|Sandbar Sandstone|70061|5|Briefly described|Petrel Sub-basin Fig.3|Visean|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Tanmurra Formation. Is overlain by Sunbird Formation.||12-JUL-16
74206|Sandbar Sandstone|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sunbird Formation.||
23956|Sandpiper Sandstone|13194|4|Described|p385 Tb. 4-16, p396 fig 4-60|Berriasian|Tithonian|Type section Petrel 1 well (1329-1571m).||Flamingo Group||Overlies Frigate Shale (conformably).|Fine to coarse grained glauconitic sandstone.|
23956|Sandpiper Sandstone|13234|6|Mentioned|p260, p263 Tb.4.|||Reservoir quality sandstones.||Unit in Flamingo Group.||||
23956|Sandpiper Sandstone|22663|6|Mentioned|NT97 -1-4 Fig.4|||||||||
23956|Sandpiper Sandstone|23376|4|Described|p244||Berriasian|In the Bonaparte Basin.||||||29-NOV-06
23956|Sandpiper Sandstone|24047|5|Briefly described|p13|Jurassic|Jurassic|Geological Province: Money Shoal Basin.||||||
23956|Sandpiper Sandstone|24427|5|Briefly described|p49 Fig.2|Berriasian|Tithonian|Geological Province: Bonaparte Basin.||||||
23956|Sandpiper Sandstone|24569|5|Briefly described|p248 Fig. 3|Berriasian|Berriasian|Of the Flamingo Group.  Age:~140Ma.  Geological Province: Petrel Sub-basin.||||||02-MAR-05
23956|Sandpiper Sandstone|41459|6|Mentioned|Fig.2|||||||||
23956|Sandpiper Sandstone|41532|3|Fully described|p305|||||||||
23956|Sandpiper Sandstone|41731|6|Mentioned|Fig.3|||||||||
23956|Sandpiper Sandstone|42442|2|Defined|p26|Berriasian|Tithonian|Variation of Sandpiper Sandstone, WA. Age latest Jurassic to earliest Cretaceous||||||
23956|Sandpiper Sandstone|43661|6|Mentioned|Fig.3|||||||||
23956|Sandpiper Sandstone|43699|6|Mentioned|Fig.6,p10||Early Cretaceous|||||||
23956|Sandpiper Sandstone|49637|5|Briefly described|Fig. 3|Neocomian|Neocomian|Of the Flamingo Group. Geological Province: Petrel Sub-basin.||||||07-FEB-11
23956|Sandpiper Sandstone|60386|6|Mentioned|p302|Early Cretaceous|Late Jurassic|Bonaparte Basin. ||||||
23956|Sandpiper Sandstone|62837|5|Briefly described|Stratigraphic columns|Late Jurassic|Late Jurassic|Of the Flamingo Group. Age: ~142-~136Ma. Geological Province:  Petrel Sub-basin.||||||01-MAR-10
23956|Sandpiper Sandstone|64689|5|Briefly described|p7 Fig.6 |Early Cretaceous|Late Jurassic|Tithonian to Berriasian.||||||
23956|Sandpiper Sandstone|64696|6|Mentioned|p127 Fig.2 |Berriasian|Tithonian|||||||
23956|Sandpiper Sandstone|69452|5|Briefly described|p36:8, 15, 21-22|Early Cretaceous|Late Jurassic|Petrel Sub-basin, Bonaparte Basin. 30-270m thick.||Flamingo Group.||Overlies Frigate Shale.|Fluvial to deltaic sandstone-dominated unit.|12-JUL-16
23956|Sandpiper Sandstone|69653|5|Briefly described|p1, 6, 8, 10, p13 Fig.2.4, p15, 17-18|Cretaceous|Cretaceous|Petrel Sub-basin. Suitable for CO2 storage; sealed by Bathurst Island Group. Shallowing marine environment; fluvial to shoreface sediments. Schematic (gamma ray) well sections. Composite well diagram. Photomicrographs. See also p26-27, 30, 36-39, 41-43, 47-48, 50-53, 59-60, 63, 70, 73-76.||Flamingo Group.||Overlies Frigate Shale. Is overlain by Echuca Shoals Formation.|Mudstone; fine-grained sandstone interbedded with shale; massive fine-grained sandstone; fine- to coarse-grained sandstone. Facies described in detail.|
23956|Sandpiper Sandstone|69673|6|Mentioned|p173|||||Flamingo Group||||
23956|Sandpiper Sandstone|69689|6|Mentioned|p16|Cretaceous|Cretaceous|Bonaparte Basin.||||||
23956|Sandpiper Sandstone|70061|5|Briefly described|Petrel Sub-basin; Fig.2|Valanginian|Berriasian|See also Regional geology: Figs.6-7, p12, p19. Sahul: Fig.2, p2. Vulcan: Fig.2. Marine shelf and possibly slope and basin-floor fan complexes. A secondary reservoir in the N Bonaparte Basin. Hosts gas in anticlinal, fault block and stratigraphic traps (Saratoga 1).||Flamingo Group.||Overlies Upper Frigate Shale. Is overlain by Echuca Shoals Formation.|Quartzose clastics.|12-JUL-16
42367|Sandy Blight Quartzite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Interlayered and strongly foliated quartzite and quartz-muscovite schists. Of the Kintore Domain, Warumpi Province.  In the Arunta region.||||||07-NOV-08
42367|Sandy Blight Quartzite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Interlayered and strongly foliated quartzite and quartz muscovite schist. Geological Province: Warumpi Province||||||07-NOV-08
42367|Sandy Blight Quartzite|65358|6|Mentioned|p24|||1100 +/- 5 Ma age for muscovite from quartz vein (Wygralak and Mernagh, 2004).||||||
42367|Sandy Blight Quartzite|68994|5|Briefly described|p4|||Kintore Domain in Warumpi Province.|||||Quartzite and phyllite.|
42367|Sandy Blight Quartzite|69428|5|Briefly described|p13:2-3, 12, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Forms a series of isolated hills and ridges extending for 45km W from near Sandy Blight Junction. Greenschist facies metamorphism. Timing of deposition is uncertain. SHRIMP U-Pb detrital zircon maximum deposition age.|1680 +/- 3 Ma (Worden et al., 2006).||||Crystalline metasedimentary quartzite containing a variably defined muscovite foliation, with less abundant quartz-muscovite phyllite that contains a bedding-parallel cleavage and 5-20cm-thick quartzite interbeds.|12-JUL-16
42367|Sandy Blight Quartzite|69933|5|Briefly described|v, p1, p18-21, p37|Statherian|Statherian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1681 +/- 8 Ma (Max dep age, SHRIMP U-Pb)||||Crystalline metasedimentary quartzite containing a variably defined muscovite foliation.|21-APR-23
42367|Sandy Blight Quartzite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||pelite, greenstone, schist, quartzite|
42367|Sandy Blight Quartzite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1681+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
42367|Sandy Blight Quartzite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain.|||||Foliated quartzite and quartz-muscovite schist.|09-SEP-19
27056|Saunders Granite|23714|4|Described|p31|||See also page 20 Table 4. First mapped as part of Cullen Granite. Geological Province: Cullen Batholith.||||||
27056|Saunders Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
27056|Saunders Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27056|Saunders Granite|41311|6|Mentioned|p20|||||||||
27056|Saunders Granite|43140|3|Fully described|p41||Paleoproterozoic|Of Cullen Batholith. Part of Cullen Granite by Noakes(1949). Include the Blundells Monzonite?||||||07-NOV-08
27056|Saunders Granite|43624|6|Mentioned|p15|||May be 'Leucogranite'.||||||29-NOV-06
27056|Saunders Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Of Cullen Supersuite. I-type. Medium equigranular biotite leucogranite. Intrudes Allamber Springs Granite.||||||07-JAN-09
27056|Saunders Granite|69420|5|Briefly described|p5:17-19|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Saunders Suite.|||Fine- to medium-grained, equigranular leucogranite. I-type.|12-JUL-16
27056|Saunders Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Saunders Suite.|||Pink to light grey, fine- to medium-grained, predominantly equigranular mafic to felsic hornblende-biotite granite.|
31734|Saunders Suite|24197|5|Briefly described|p24|||Of the Cullen Supersuite. Consists of 2 plutons: Saunders and Foelsche Leucogranites. Geological province: Pine Creek Inlier.||||||07-FEB-11
31734|Saunders Suite|50586|6|Mentioned|p4.21|||Of the Cullen Supersuite. Geological Province: Pine Creek Inlier.||||||
31734|Saunders Suite|69420|5|Briefly described|p5:17, 19, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Cullen Supersuite.|Saunders, Mount Davis Granites; Foelsche Leucogranite.|||12-JUL-16
31734|Saunders Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Saunders Granite.|||01-MAR-18
37737|Schultz Sandstone Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Constance Sandstone.||||||
37737|Schultz Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Constance Sandstone. White to brown, friable, medium, coarse and very coarse grained to granule sandstone; platy, thinly laminated very fine grained sandstone and minor siltstone and shale.||||||
37737|Schultz Sandstone Member|65337|3|Fully described|p9 Fig.5, p38 Table 5.|Mesoproterozoic|Mesoproterozoic|New name. Northeast MOUNT DRUMMOND area. Includes siltstone lenses formerly (Sweet 1981) named Bowthorn Siltstone Member. Basal beds outcrop as spectacular, bare rocky platforms cut by deeply eroded joints; giant displaced blocks are common.||Unit in Constance Sandstone.||Disconformably overlies Wallis Siltstone Member. Is overlain by Mullera Formation.|Yellow to white, subfriable medium- to coarse-grained, well-sorted quartz sandstone; some granule layers; becomes medium-grained up-section. Very pure quartz sandstone with siliceous cement continues to top of Formation. Cross-bedded throughout.|
37737|Schultz Sandstone Member|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Basal yellow to white, subfriable, medium- to coarse-grained well-sorted quartz sandstone; passes up into medium-grained, very pure quartz sandstone with siliceous cement.|
37737|Schultz Sandstone Member|67539|6|Mentioned|p14, p15 Fig.8|||Rawlings and others (2008). Equivalent to the new, reduced Constance Sandstone and therefore rendered obsolete.||||||
37737|Schultz Sandstone Member|68146|4|Described|p2, p6, p27-33, p35, p196-197, p211|||South Nicholson Region. A distinctive, tor-like outcropping unit. Described as "laterally equivalent" to Constance Sandstone, and is also presented on that page as Constance Sandstone-Schultz Sandstone[sic]; similar detrital zircon spectra. Whole-rock Sm-Nd isotopic data tabulated.|1577 +/- 21 Ma; maximum depositional age.|Basal Constance Sandstone.||Unconformably overlies Wild Cow Subgroup.|Fine- to medium-grained, well-sorted, quartz sandstone.|
37737|Schultz Sandstone Member|69434|4|Described|p19:2, 6|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. 120-over 600m thick. Shallow-marine deposits: upper shoreface to intertidal; may include braided fluvial.||Constance Sandstone.||Disconformably overlies Wallis Siltstone Member. Is overlain conformably by Mullera Formation.|White to brown, friable, medium, coarse and very coarse to granule sandstone; 220m-thick intercalated unit of platy, thinly laminated, very fine sandstone.|12-JUL-16
37737|Schultz Sandstone Member|69591|5|Briefly described|p52-53|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). High-energy fluvial deposits.||Constance Sandstone.||Unconformably overlies Wallis Formation. Is overlain unconformably by Elizabeth Sandstone.|Resistant sandstone with a basal layer of coarse cobble-to-boulder conglomerate.|
37737|Schultz Sandstone Member|71369|3|Fully described|p5-7, p12, p19-20, p23-31, p33, p36, p50|Mesoproterozoic|Mesoproterozoic|See also p1. Rawlings et al. (2008). Their description, having abandoned the Bowthorn Siltstone Member, coincided with the entire span of the Constance Sandstone of Carter et al. (1961). Redefinition in this study has this Member applied only to the lower part of the Constance Sandstone. South Nicholson Basin. Up to 700-1000m thick; c.200m in the type section, whose base is 14km SE of Bowthorn homestead. Proximal fluvial deposits. Forms distinctive slabby outcrops. Facies discussed in detail.||Constance Sandstone.||Unconformably overlies Wallis Formation (Wild Cow Subgroup) and Termite Range Formation (McNamara Group). Is overlain by Bowthorn Member (and locally by Elizabeth Sandstone unconformably).|Thick-bedded, pink-brown to red, mainly granule-rich but also pebbly to cobbly sandstone lacking fine-grained interbeds. Basal conglomerate lenses, and distinctive sandstone with no partings or interbeds thus forming very large blocks in outcrop.|20-FEB-18
37737|Schultz Sandstone Member|71592|5|Briefly described|Appendix A.|||South Nicholson Basin.|1577+/-21 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
37737|Schultz Sandstone 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 Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone 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 Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone 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 Constance Sandstone.|||Fine- to coarse-grained, well sorted, thick-bedded, cross-bedded sandstone and sublithic sandstone; minor hematitic siltstone and very fine- to fine-grained sandstone.|
37737|Schultz Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone 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 Constance Sandstone.|||Fine to coarse-grained, well-sorted, thick-beddded, cross-bedded quartzose and sublithic sandstone; minor hematitic siltstone and very fine to fine-grained sandstone|
37737|Schultz Sandstone Member|72526|5|Briefly described|p33-34.|Mesoproterozoic|Mesoproterozoic|Of Rawlings et al., 2008 and Sweet, 2017. Along with Bowthorn Member this unit is interpreted as part of the Constance Sandstone in Queensland. [Current status of this unit is unclear. Not shown in p8 figure.]||Of Constance Sandstone of Rawlings et al., 2008 and Sweet, 2017.||Probably underlies Bowthorn Member.||
37737|Schultz Sandstone Member|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|||Constance Sandstone||Overlies Wallis Sandstone Member and underlies Mullera Formation.||
37737|Schultz Sandstone Member|72919|6|Mentioned|p5, p47-48, p94-95|Ectasian|Calymmian|Included in Constance Sandstone in both NT and QLD, but the Accident Subgroup in NT (Rawlings et al., 2008) and the Wild Cow Subgroup in QLD (Sweet, 2017). Previous maximum depositional age in QLD of 1577 +/- 21 Ma from Carson et al. (2011).|1577 +/- 21 Ma (QLD)|Constance Sandstone||Overlain by Mullera Formation. Underlain by Wallis Sandstone Member.||
37737|Schultz Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard. Known oil show.||Constance Sandstone, Accident Subgroup, South Nicholson Group||Unconformably underlain by Wallis Formation (Wild Cow Subgroup).||
28991|Seale Sandstone|14019|4|Described|p16|||Of the Wattie Group. Consists predominantly of medium quartz sandstone.  Conformably but sharply overlies the Gibbie Formation.  Max. thickness: 111m in WAVE HILL.  Geological Province: Victoria Basin.  See also p4 Fig. 3.||||||
28991|Seale Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
28991|Seale Sandstone|24297|3|Fully described|p7|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Timber Creek Formation (Bullita Group), conformably overlies Gibbie Formation. Maximum thickness: 111m. (in WATERLOO).  See also p5 Tb. 2.||||||
28991|Seale Sandstone|24441|5|Briefly described|p1 Fig. 1, p7-8|Mesoproterozoic|Mesoproterozoic|Of Wattie Gp. Fine to medium dolomitic sandstone, (qtz arenite composition) and subordinate laminated dolomitic mudstone. Overlies Gibbie Fm;  conformably overlain by Timber Creek Fm. Thickness: >37m. Geol.Prov: Victoria Basin.||||||25-JAN-06
28991|Seale Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
28991|Seale Sandstone|28255|6|Mentioned|p41|Adelaidean|Adelaidean|May have superseded Seale Formation?||||||15-JUN-05
28991|Seale Sandstone|30003|4|Described|p8, p12|||Of the Wattie Group.  White and fawn blocky thin-bedded feldspathic sandstone with gery and white thickly cross-bedded units up to 1m thick; mud flakes common. Carpentarian or Adelaidean||||||19-APR-05
28991|Seale Sandstone|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
28991|Seale Sandstone|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
28991|Seale Sandstone|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Massive to blocky sandstone.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
28991|Seale Sandstone|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive and blocky medium quartz sandstone.||||||07-NOV-16
28991|Seale Sandstone|32660|5|Briefly described|Table 6|||||||||
28991|Seale Sandstone|33374|6|Mentioned|p7|||Strat.||||||
28991|Seale Sandstone|33375|5|Briefly described|p7, p8 Tb. 1|||Of the Wattie Group. Overlies the Gibbie Formation.||||||26-APR-05
28991|Seale Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
28991|Seale Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group. Massive fine and medium quartz sandstone.||||||28-APR-05
28991|Seale Sandstone|45112|5|Briefly described|Table 9|||||||||
28991|Seale Sandstone|48938|6|Mentioned|p21|||||||||
28991|Seale Sandstone|48943|2|Defined|p49|Adelaidean|Adelaidean|||||||
28991|Seale Sandstone|60682|5|Briefly described|p7|||Of Wattie Group. Thickness: 5m.||||||
28991|Seale Sandstone|60685|4|Described|p4 Fig. 3, p7|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Dolomitic sandstone; subordinate laminated dolomitic mudstone. Conformable on Gibbie Formation; conformable below Timber Creek Formation. Max. Thickness: 111m. Geological Province: Victoria Basin.||||||
28991|Seale Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Overlies Gibbie Formation. Is overlain by Timber Creek Formation of the Bullita Group.||
28991|Seale Sandstone|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Overlies Gibbie Formation. Is unconformably overlain by Timber Creek Formation.|Massive fine and medium quartz sandstone.|
28991|Seale Sandstone|68733|6|Mentioned|p177 Fig.2, p179 Tb.1, p185 Tb.4, p192|||Previously included in the Victoria Basin by Cutovinos et al. (2002). Now included in the Birrindudu Basin due to a recent subdivision by the NGTS (Dunster and Ahmad 2013). Sm-Nd isotope data tabulated.||Of the Wattie Group.||||06-DEC-17
28991|Seale Sandstone|69432|5|Briefly described|p17:2, 9, 14-15|||Birrindudu Basin. 5-111m thick. High-energy, shallow-marine transgressive deposits. Known to contain live oil.||Wattie Group.||Conformably overlies Gibbie Formation.|Predominantly medium quartz sandstone.|12-JUL-16
28991|Seale Sandstone|69673|6|Mentioned|p48 fig 35, p50|||Contains live oil||Wattie Group||Overlies Gibble Formation, overlain by Timber Creek Formation|Quartz sandstone.|
28991|Seale Sandstone|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Shown as top of Wattie Group.||Overlies Mount Sanford Formation, possibly unconformably. Overlies Gibbie Formation. Is unconformably overlain by Timber Creek Formation.|Massive fine and medium quartz sandstone.|24-JAN-22
28991|Seale Sandstone|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Gibbie Formation. Is overlain unconformably by Timber Creek Formation (Bullita Group).|Fine to medium feldspathic and quartz sandstone.|
28991|Seale Sandstone|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Overlies Gibbie Formation. Is overlain by Timber Creek Formation (Bullita Group).|Quartz sandstone, feldspathic sandstone.|
28991|Seale Sandstone|71267|4|Described|GEOL_LUT_CSV files|||See 1m_geologyp12_lithology_lut.csv, 1m_geologyl12_lithology_lut.csv.|||||sandstone|
28991|Seale Sandstone|71302|4|Described|p1,6-7,22-27,72,74||Paleoproterozoic|Of Birindudu Basin. Deposited under high-energy, shallow marine transgressive conditions. Reaches 111m thick in the WAVE HILL 1:250 000 sheet. Sample GA 1956889 (quartz sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositioanal age of 1605+\-12 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.||Unit of Wattie Group.||Overlain gradationally by Timber Creek Formation/Bullita Group. Underlain conformably by Gibbie Formation.|Medium-grained quartz sandstone, locally reddish and ferruginous.|
28991|Seale Sandstone|72718|6|Mentioned|p7|||Birrindudu Basin.||Wattie Group||Underlain by Gibbie Formation. Overlain by Timber Creek Formation (Bullita Group).||
38902|Settlement Creek Dolerite|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
38902|Settlement Creek Dolerite|60574|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Tawallah Group. Overlies the Aquarium Formation. Overlain by the Wollogorang Formation. Black to orange equigranular dolerite; local hornfels enclaves.||||||07-NOV-08
38902|Settlement Creek Dolerite|65340|1|Redefined|p12 Fig.6, pp16-22, pp92-93. |||Formerly Settlement Creek Volcanics (Jackson et al. 1987); name change reflects interpretation as an intrusion. Type area is the Mallapunyah Dome. Unusual and diagnostic wrinkles are locally recognised on upper surface; interpreted as pahoehoe-like. Margins strongly brecciated locally. Mudstones above and below are hornfelsed; these contact zones are relatively resistant; otherwise generally recessive with dark red/brown aerial phototones. Forms local apophyses, sometimes spectacular, into overlying Wollogorang Formation; and laccoliths at the Robinson and Mallapunyah domes. Correlated with parts of Peters Creek and Gold Creek Volcanics and McCaw Formation; interpreted correlative feeders include the stratigraphically lower Oenpelli Dolerite. Most sedimentary intervals formerly assigned to this unit in BAUHINIA DOWNS and MOUNT YOUNG maps have been re-mapped as McDermott Formation. Produces a high-frequency magnetic response beneath Mesozoic and Cenozoic cover.|c.1730 - 1725 Ma.|Unit in Tawallah Group.||Overlies Wununmantyala Sandstone and, nonconformably, the Aquarium Formation. Is overlain nonconformably by Wollogorang Formation.|Extensive sills; cores are medium to coarse grained, aphyric to locally porphyritic, ophitic and subophitic textures, comprising plagioclase, pyroxene and opaque oxides; incipiently altered; jointing common; hornfelsed contacts and rafts.|
38902|Settlement Creek Dolerite|67323|6|Mentioned|Eastern Australia Time-Space Plot|||||||||
38902|Settlement Creek Dolerite|69430|4|Described|p15:3, 10-12, 44, 46|||Southern McArthur Basin. 20-200m thick. High-level sill or laccolith intruded into evaporitic mudstone. Hosts Cu-bearing breccia pipes (described in some detail).||Tawallah Group.||Intrusive contacts separating Wununmantyala Sandstone and Aquarium Formation below from Wollogorang Formation above.|Dolerite and lesser basalt; brecciated or ropy upper surface; local hornfelsed mudstone enclaves.|12-JUL-16
38902|Settlement Creek Dolerite|69673|6|Mentioned|p16 fig 13, p17 fig 14|||||Tawallah Group||Overlain by Wollogorang Formation, overlies Wununmantyala Sandstone, Wuraliwuntya Member, Aquarium Formation|Dolerite.|
38902|Settlement Creek Dolerite|71592|5|Briefly described|Appendix A.|||McArthur Basin.|||||Andesite.|
38902|Settlement Creek Dolerite|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Partly underlain by Aquarium Formation and Wununmantyala Sandstone including Wuraliwuntya Member. Overlain by Wollogorang Formation.||
38902|Settlement Creek Dolerite|73083|6|Mentioned|p15, p47, p78|Paleoproterozoic|Paleoproterozoic|||||||
38902|Settlement Creek Dolerite|73412|5|Briefly described|p4, 8-9, 12, 14-15, 20|||Southern McArthur Basin. See also references to Settlement Creek Volcanics (p2, 9).|c.1730 Ma.|Tawallah Group.||Overlies Wununmantyala Sandstone and Aquarium Formation. Is overlain by Wollogorang Formation. Intrusive equivalent to the eruptive Gold Creek Volcanics.|High-level sills.|
25472|Shadforth Sandstone|22538|6|Mentioned|Fig3 P708|||||||||
25472|Shadforth Sandstone|22748|6|Mentioned|p235 Fig.1|||||||||
25472|Shadforth Sandstone|23216|5|Briefly described|Table1p9,23-4|||||||||
25472|Shadforth Sandstone|23374|3|Fully described|Tb2p10,17||Statherian|Unconformable on Cottee Formation. Of Katherine River Group. In the McArthur Basin.||||||30-NOV-06
25472|Shadforth Sandstone|23396|5|Briefly described|p 407 fig.2|||Of Katherine River Group.||||||30-NOV-06
25472|Shadforth Sandstone|23867|3|Fully described|p12|Paleoproterozoic|Paleoproterozoic|Of Katherine River Group.  Max. thickness: ~50m.  Geological Province: McArthur Basin.  See also Table 1 and Figs. and 30.||||||07-NOV-08
25472|Shadforth Sandstone|23937|5|Briefly described|p7|||Of the Katherine River Group.  Geological Province: Calvert Superbasin.||||||
25472|Shadforth Sandstone|24048|5|Briefly described|p36|||Of the Katherine River Group.||||||30-NOV-06
25472|Shadforth Sandstone|24050|2|Defined|p80 App. 1|Statherian|Statherian|Of the Katherine River  Group.  Thickness in type section: 40m.  Upper part of unit, previously mapped into this unit (Roberts  Plumb, 1965), now included in the overlying Bonanza Creek Formation.  May correlate with Wununmantyala Sandstone (Tawallah Gp).||||||23-DEC-09
25472|Shadforth Sandstone|24051|5|Briefly described|Map Legend|Statherian|Statherian|Of Katherine River Group. Geological Province: McArthur Basin.||||||
25472|Shadforth Sandstone|32660|5|Briefly described|Table 4|||||||||
25472|Shadforth Sandstone|42597|5|Briefly described|Map Legend|Carpentarian||||||||
25472|Shadforth Sandstone|43010|2|Defined|p102||Paleoproterozoic|Of the Katherine River Group. Of Statherian age.||||||07-NOV-08
25472|Shadforth Sandstone|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Katherine River Group. Of Statherian age.||||||07-NOV-08
25472|Shadforth Sandstone|44112|6|Mentioned|p43,49|||||||||
25472|Shadforth Sandstone|44400|2|Defined|p.7,8,11,Tb.1|||Overlain by McCaw Formation, MOUNT MARUMBA Sheet. (D53-6),opp.p.6, map.||||||30-NOV-06
25472|Shadforth Sandstone|44401|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
25472|Shadforth Sandstone|45022|4|Described|p.56, 68.|||Of Katherine River Group.||||||30-NOV-06
25472|Shadforth Sandstone|60571|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Sandstone: white to cream/orange, medium- to coarse-grained, medium- to thick-bedded, trough and tabular cross-bedded quartz arenites. Geological Province: McArthur Basin.||||||30-NOV-04
25472|Shadforth Sandstone|60680|5|Briefly described|Map legend|Statherian|Statherian|Of the Katherine River Group. Medium to very coarse, poorly sorted quartz sandstone with scattered granules or pebbles. Geological Province: McArthur Basin. Overlies: Cottee Formation. Underlies: Bonanza Creek Formation.||||||14-JAN-05
25472|Shadforth Sandstone|64698|4|Described|lithinterp table|Statherian|Statherian|Age ~1730-1740Ma. McArthur Basin. Of Katherine River Group. Max thickness 50m. White, pink or grey, trough cross-bedded, medium to very coarse, poorly sorted quartz sandstone with scattered granules or pebbles.||||||07-JAN-09
25472|Shadforth Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Arnhem Shelf, McArthur Basin.|1745 - 1730 Ma inferred.|Of the Katherine River Group.|||Sandstone and conglomerate.|05-JUN-18
25472|Shadforth Sandstone|65232|5|Briefly described|p7 Fig. 6|||Of Katherine River Group. Underlies Bonanza Creek Formation; 40 m thick. overlies Cottee Formation. Fluvial Sandstone.||||||09-FEB-10
25472|Shadforth Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.||Upper Katherine River Group.||||
25472|Shadforth Sandstone|67564|4|Described|p6 Table 2, p10 Fig.5, p39 Fig.20, p47.|Paleoproterozoic|Paleoproterozoic|Resistant quartz sandstone. 50 m of shallow marine sediments, fluviatile at base.|1740 - 1720 Ma.|Unit in Katherine River Group.||Unconformably overlies Cottee Formation. Is overlain conformably by Bonanza Creek Formation.|Crossbedded, poorly sorted pebbly quartz sandstone; well-sorted quartz sandstone with mudstone intraclast cavities; minor glauconite.|
25472|Shadforth Sandstone|69430|4|Described|p15:3, 8-9|||NW McArthur Basin. 40m thick. Fluvial, to probably shallow-marine at top, deposits.||Katherine River Group.||Overlies Cottee Formation probably unconformably. Is overlain conformably and gradationally by Bonanza Creek Formation.|Medium- to coarse-grained (also described as fine- to medium-grained), medium to thickly bedded, grey-white to cream-orange quartz arenite with coarse-grained to granular bands; trough and tabular cross-bedded.|12-JUL-16
25472|Shadforth Sandstone|69673|6|Mentioned|p16 fig 13|||Northwestern McArthur Basin.||Katherine River Group||Overlain by McCaw Formation, Bonanza Creek Formation, overlies Cottee Formation||
25472|Shadforth Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Katherine River Group.||||
37961|Shadow Group|61404|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Includes Octy, Neutral Junction, Mount Baldwin Formations and the Adam Shale.  Geological Province: southern Georgina Basin.||||||
37961|Shadow Group|62983|5|Briefly described|p11|Early Cambrian|Early Cambrian|Referred to informally as the lower Shadow Group. Siliciclastic sedimentation. Thickness: ~360m. Geological Province: Georgina Basin.||||||07-FEB-08
37961|Shadow Group|64068|3|Fully described|p224 App 1, pp54-57, p7, 36, p ix|Middle Cambrian|Neoproterozoic|New name. Includes all Lower Cambrian rocks in southern Georgina Basin. Complex relationships detailed.|||Includes Octy, Neutral Junction, Mount Baldwin and Riversdale Formations, Sylvester Sandstone, Mount Birnie beds, Adam Shale and Red Heart Dolostone.|||09-FEB-16
37961|Shadow Group|65341|6|Mentioned|p5, pp17-18.||||||Includes Octy Formation.|||
37961|Shadow Group|67323|6|Mentioned|GIS attrib tbl, Solid Geology Map.||||||Includes Mount Birnie beds, Riversdale Formation, Sylvester Sandstone|||
37961|Shadow Group|68553|6|Mentioned|Map legend; schematic diagram.|Cambrian|Cambrian|Georgina Basin. ||||||
37961|Shadow Group|69377|5|Briefly described|map legend|Cambrian|Cambrian||||Mount Birnie beds|||
37961|Shadow Group|69437|6|Mentioned|p22:9|Early Cambrian|Early Cambrian|Georgina Basin, Centralian B Superbasin.||||||12-JUL-16
37961|Shadow Group|69443|5|Briefly described|p28:3, 5, 7, 13-16, 31|Cambrian|Cambrian|Kruse in Dunster et al. (2007). Includes all early Cambrian strata of the southern Georgina Basin. Represents a renewal of sedimentation following the Huckitta Movement. Is correlated with the upper Arumbera Sandstone, Winnall beds, Quandong Conglomerate, Eninta Sandstone, Mount Currie Conglomerate, Mutitjulu Arkose, Namatjira Formation and Todd River Dolostone (Amadeus Basin), and with upper Yuendumu Sandstone (Ngalia Basin).|||Neutral Junction, Octy, Mount Baldwin, Riversdale Formations; Adam Shale; Red Heart Dolostone; Sylvester Sandstone; Mount Birnie beds.|Unconformably or disconformably overlies Mopunga and Keepera Groups. Is overlain unconformably by Thorntonia Limestone, Beetle Creek or Chabalowe Formations. Correlative of Barkly Group.||12-JUL-16
37961|Shadow Group|69591|5|Briefly described|p29, p90-91, p94|Cambrian|Neoproterozoic|Oban Sub-basin, Georgina Basin.|||Riversdale Formation, Mount Birnie beds, Yardida Tillite, Black Stump Arkose, Gnallan-a-Gea Arkose.|||
37961|Shadow Group|69673|6|Mentioned|p111, p114 fig 92, p116|Cambrian|Cambrian ||||Includes Adam Shale, Mount Baldwin Formation, Octy Formation, Neutral Junction Formation, Red Heart Dolostone|||
37961|Shadow Group|72515|5|Briefly described|Map Legend|Cambrian|Cambrian|Jervois Range Special Map Sheet. Georgina Basin.|||Includes the Red Heart Dolostone and the Mount Baldwin Formation.|Disconformably overlain by the Narpa Group. Unconformably overlies the Mopunga Group.||
37961|Shadow Group|72516|6|Mentioned|p12, p21, p85, p90, p135, p171, p176|Cambrian|Cambrian|Georgina Basin.|||Includes the Red Heart Dolostone, Mount Baldwin Formation|||02-JUN-21
37961|Shadow Group|72683|5|Briefly described|Map legend|Cambrian|Cambrian|Georgina Basin.|||Includes Mount Birnie beds.|Underlies Narpa Group.||
37961|Shadow Group|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).|||Includes Mount Birnie beds|Shown as unconformably underlying Narpa Group.|Includes massive ferruginous sandstone, cross-bedded sandstone, conglomerate, red and green shale, mudstone and dolomite; basal tillite.|
37961|Shadow Group|72711|6|Mentioned|p3 Fig.2.|Cambrian|Cambrian|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.||||||
37961|Shadow Group|73137|6|Mentioned|p6|Cambrian|Cambrian|||||||
37961|Shadow Group|73553|6|Mentioned|p7|Cambrian|Cambrian|||||||
41151|Shaw Granite|50286|5|Briefly described|Map Legend|||||||||22-DEC-09
29329|Sheridan Member|22538|6|Mentioned|Fig3 P708|||||||||
29329|Sheridan Member|22600|4|Described|Map legend|Statherian|Statherian|||||||
29329|Sheridan Member|24048|3|Fully described|p30|Statherian|Statherian|Replaces "Sheridan Formation".  Of the Fagan Volcanics.  Max. thickness: 250m.  Geological Province: McArthur Basin.||||||30-NOV-06
29329|Sheridan Member|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics (Donydji Group). Sandstone: cross-bedded, medium to coarse-grained, lithic; interbedded with mudstone: ferruginous, micaceous; local volcaniclastic breccia, conglomerate and sandstone; locally sheared. Geol. Prov: McArthur Basin.||||||30-NOV-06
29329|Sheridan Member|44112|1|Redefined|p31,40-41,111-112|Statherian|Statherian|Previously known as 'Sheridan Formation' [Plum and Roberts (1965)]. Max Age: ~1710 Ma||||||
29329|Sheridan Member|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Fagan Volcanics (Donydji Group). Sandstone: cross-bedded, medium to coarse-grained, lithic; interbedded with mudstone: ferruginous, micaceous; local volcaniclastic breccia, conglomerate and sandstone; locally sheared. Geol. Prov: McArthur Basin.||||||30-NOV-06
29329|Sheridan Member|64817|6|Mentioned|p353 Fig.4 |||||Of the Fagan Volcanics.||||
29329|Sheridan Member|69430|4|Described|p15:3, 7|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. 250-400m thick. Shallow-water, low- to moderate-energy (lacustrine or fan-delta) deposits.||Fagan Volcanics.||Conformably overlies Maidjunga Member. Is overlain conformably by Dhupuwamirri Member.|Sandstone, interbedded with mudstone; local volcaniclastic breccia, conglomerate and sandstone.|12-JUL-16
29329|Sheridan Member|69673|6|Mentioned|p16 fig 13|||||Fagan Volcanics||Overlain by Dhupuwamirri Member, overlies Maidjunga Member||
40033|Sherwin Formation|23937|1|Redefined|p92 App. 1|Calymmian|Calymmian|Supersedes the Sherwin Ironstone Member (McMinn Fm).  Now upgraded to formation status in the Maiwok Subgroup (Roper Grp).  Conformably overlain by Kyalla Fm; conformably overlies the Moroak Sst.  Max.thick:~100m.  Geol.Prov: McArthur Basin.||||||23-DEC-09
40033|Sherwin Formation|24047|4|Described|p12 Fig. 10, p11|Mesoproterozoic|Mesoproterozoic|Of the Roper Group.  Contains massive oolitic and pisolitic ironstone within interbedded medium to very coarse ferruginous ripple-marked sandstone, sandy mudstone and shale.  Geol. Prov: McArthur Basin.  See also p22-23, Figs. 18 (p24) and 19 (p25).||||||
40033|Sherwin Formation|24442|5|Briefly described|p20|||Contains oolitic limestone beds.  Geological Province: McArthur Basin.||||||
40033|Sherwin Formation|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Maiwok Subgroup. Interbedded fine grained sandstone, siltstone and mudstone; pisolitic ironstone.||||||
40033|Sherwin Formation|67827|6|Mentioned|p422-423|Mesoproterozoic|Mesoproterozoic|Roper River area. Contains 'Clinton' type ironstone deposits.|||||Ironstone.|
40033|Sherwin Formation|69418|6|Mentioned|p3:24-25|||McArthur Basin. Hosts the Roper Bar and Roper River Projects oolitic Fe deposits (described).||||||12-JUL-16
40033|Sherwin Formation|69430|4|Described|p15:3, 27, 29-31, 52-55|Calymmian|Calymmian|Abbott et al. (2001) who raised the unit to Formation status and defined it. Originally (Dunn, 1963) the Sherwin Ironstone Member of the McMinn Formation. Southern McArthur Basin. Up to 100m thick. Fluvial to marginal marine sediments. The upper boundary is defined as the last occurrence of oolitic ironstone. Contains significant low-grade stratiform ironstone deposits, described in detail (including Hodgson Downs, Mountain Creek and Roper Bar project areas).||Maiwok Subgroup.||Conformably and gradationally overlies Moroak Sandstone. Is overlain conformably and gradationally by Kyalla Formation.|Dominated by interbedded sandstone, siltstone and mudstone, but characterised by local oolitic/pisolitic ironstone lenses.|12-JUL-16
40033|Sherwin Formation|69673|6|Mentioned|p16 fig 13|||Southern McArthur Basin.||Maiwok Subgroup||Overlain by Kyalla Formation, Conformably overlies Moroak Sandstone||
40033|Sherwin Formation|70968|3|Fully described|p23, p51, p53, p65-66, p68-74, p77-78|Ectasian|Ectasian|See also p81, p123, p126, p130-131, p133, p140, p143-144. Abbott and Young in Abbott et al. (2001) after Dunn (1963). Formerly the Sherwin Ironstone Member of McMinn Formation (Dunn, 1963); raised to Formation rank by Abbott et al. (2001) who redefined it and the underlying Moroak Sandstone. Named after Sherwin Creek. Two type areas nominated by Abbott et al. (2001) are no longer accessible; a new type section/area is required. Poor exposure except for ironstone units on dip slopes and caps on mesas. Has a distinctive dark tone on aerial photographs. Lithology described and illustrated in great detail. Mined for iron ore in 2013-2014. Up to 100m thick. Subaerial/fluvial to shallow-marine deposits.||||Conformably overlies Moroak Sandstone. Is overlain conformably by, and interfingers with, Kyalla Formation.|A succession of fine- to medium-grained, tabular to blocky, sandstone with siltstone and claystone. Includes distinctive sandy, oolitic and pisolitic ironstone, ferruginous sandstone and hematitic shale "red beds".|24-FEB-17
40033|Sherwin Formation|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 10-100m thick. Proximal shallow-marine shelf to subaerial/fluvial deposits.||Maiwok Subgroup.||Conformably and gradationally overlies Moroak Sandstone. Is overlain conformably and gradationally by Kyalla Formation.|Interbedded sandstone, siltstone and mudrock; interbeds/lenses of pisolitic ironstone and redbeds.|
40033|Sherwin Formation|71488|5|Briefly described|p141 fig 1b, p142|||Betaloo Sub-basin.  Referred to as the Sherwin Ironstone on p141 fig 1b.||Maiwok Subgroup||Overlies the Moroak Sandstone. Overlain by the Kyalla Formation.||
40033|Sherwin Formation|71779|5|Briefly described|p2 Fig. 1|||Urapunga Region, McArthur Basin.||Maiwok Subgroup||||24-SEP-18
40033|Sherwin Formation|71893|5|Briefly described|p8, p32|||McArthur Basin.||Maiwok Subgroup||Conformably overlies the Moroak Sandstone.||
40033|Sherwin 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 Moroak Sandstone and underlies Kyalla Formation.||
40033|Sherwin Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone, southwestern McArthur Basin, and Batten Fault Zone (north).||Maiwok Subgroup, Roper Group||Underlain by Moroak Sandstone. Overlain by Kyalla Formation.||
40033|Sherwin Formation|72912|5|Briefly described|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the Urapunga Fault Zone, Beetaloo Sub-basin and the northern part of the Batten Fault Zone in the Southern McArthur Basin.||Maiwok Subgroup||Overlies Moroak Sandstone and underlies Kyalla Formation.||
40033|Sherwin Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|Southern McArthur Basin, Roper Superbasin.||Maiwok Subgroup, Roper Group||Underlain by Moroak Sandstone. Overlain by Kyalla Formation.||
40033|Sherwin Formation|73083|6|Mentioned|p28|||||||Overlain by Kyalla Formation.|Includes ironstone composed of ooids of hematite, goethite, and greenalite.|
40033|Sherwin Formation|73412|5|Briefly described|p4|||Southern McArthur Basin.||Maiwok Subgroup.||Overlies Moroak Sandstone. Is overlain by Derim Derim Dolerite.||
22837|Shillinglaw Formation|14019|5|Briefly described|p4|Statherian|Statherian|Of the Namerinni Group.  Age: 1639+/-28Ma (Hussey et al, 2001).  Geological Province: Ashburton Province, Tennant Inlier.||||||
22837|Shillinglaw Formation|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Namerinni Group.||||||07-NOV-08
22837|Shillinglaw Formation|23733|5|Briefly described|p34 Fig.20|||Age: 1639Ma.||||||
22837|Shillinglaw Formation|23809|5|Briefly described|p47 Fig. 42|Paleoproterozoic|Paleoproterozoic|Age: 1639+/-27Ma.  Geological Province: Ashburton Province.  Correlates with Barney Creek Formation (McArthur Basin), Campbell Springs Dolostone (Birrindudu Basin) and Mount Parker Sandstone (Osmond Basin, WA).||||||07-NOV-08
22837|Shillinglaw Formation|24047|5|Briefly described|p7 Fig. 6, p9|Paleoproterozoic|Paleoproterozoic|Of the Namerinni Group.  Age: 1640Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49, p59.||||||07-NOV-08
22837|Shillinglaw Formation|24303|2|Defined|p20, p58 Appendix|Statherian|Statherian|Of the Namerinni Group. Overlain by the Willieray Formation; overlies the Carruthers Formation. Max. Thickness: 650m. Previously mapped as undifferentiated Tomkinson Creek beds. Probable age: 1660-1610 Ma - see p57 Appendix.||||||18-OCT-05
22837|Shillinglaw Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Namerinni Group. Includes an upper dolostone lithofacies (thick-bedded, laminated or massive);  and lower mudstone lithofacies (dolomitic-siliciclastic, lamintaed, thin-bedded; sandstone and dolostone) and undifferentiated rocks.||||||07-NOV-08
22837|Shillinglaw Formation|24442|5|Briefly described|p14, p20|Paleoproterozoic|Paleoproterozoic|Of the Namerinni Group.  Age: 1639+/-27Ma.  Geological Province: Ashburton Province.||||||07-NOV-08
22837|Shillinglaw Formation|50353|5|Briefly described|Map Legend|||Of Namerinni Group.||||||26-JUL-07
22837|Shillinglaw Formation|64780|6|Mentioned|p63 Fig.4, p65 |Palaeoproterozoic|Palaeoproterozoic|Hosts manganese ore at Renner Springs.||Of the Namerinni Group||Overlies Carruthers Formation.|Interbedded sandstone, dolotutite and dolomitic siltstone.|
22837|Shillinglaw Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Namerinni Group.||||
22837|Shillinglaw Formation|69431|4|Described|p16:12, 14-17, 23-25|Statherian|Statherian|Tomkinson Province. c.500-650m thick. Two lithofacies described in detail. Lower (mixed siliciclastic/carbonate) lithofacies represents marginal-marine to continental sabkha sediments, overlain by probable shallow-water to subtidal upper (predominantly calcareous) lithofacies. Probable minor fluvial and aeolian components. Hosts the Renner Springs manganese and base metals occurrences. SHRIMP U-Pb single crystal zircon age from a probable tuff (now green chert).|1639 +/- 27 Ma (Nunn, 1997).|Namerinni Group.||Conformably and transitionally overlies Carruthers Formation. Is overlain conformably and transitionally by Willieray Formation, and unconformably by Gleeson Formation.|Dolomitic mudstone, dolostone, sandstone and siltstone; interbedded sandstone and siltstone; quartzose dolostone; minor rudstone and bafflestone; microbialite, stromatolitic bioherms, angular solution breccia; conglomerate; chertified probable tuff.|12-JUL-16
22837|Shillinglaw Formation|69673|6|Mentioned|p58|||||Namerinni Group||||
22837|Shillinglaw Formation|72373|4|Described|iii,p1,36,38-42|Mesoproterozoic|Mesoproterozoic|Geological province: Tomkinson Province. Type section: 12.5km W of Renner Springs in central HELEN. Thickness: 550-700m thick mixed siliciclastic-carbonate succession. From HELEN SPRINGS map sheet. Previous age constraints include SHRIMP U-Pb zircon date of 1639+\-27 Ma from an altered, illitic tuffaceous unit (BHP Minerals drillhole H2DD; Nunn, 1997). Sample 2711444 (HS17TJM067: Medium-grained chert-bearing quartz sandstone) yielded interpreted max depositional age of 1595+\-10 Ma. Conformable contact with underlying Carruthers Formation indicate significant time gap in zircon MDAs is related to changes in sediment source/pathways rather than hiatus.|1595+\-10 Ma (max dep age)|Unit of Namerinni Group.||Overlain conformably by Willieray Formation. Underlain conformably by Carruthers Formation.|Lower lithofacies: Interbedded sandstone, mudstone and dolostone and evaporite pseudomorphs. Upper lithofacies: calcareous and quartzic dolostone that becomes progressively coarser and more siliciclastic up-section.|01-OCT-19
24493|Shoobridge Granite|23714|4|Described|p32|||See also page 20 Table 4. Geological Province: Cullen Batholith.||||||
24493|Shoobridge Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
24493|Shoobridge Granite|24197|5|Briefly described|p24, p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. One of a group of concentrically zoned transitional granite and leucogranite dominated plutons. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
24493|Shoobridge Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24493|Shoobridge Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24493|Shoobridge Granite|41465|6|Mentioned|p8|||||||||
24493|Shoobridge Granite|42012|2|Defined|p42|Paleoproterozoic||See also Table 1 p6.||||||07-NOV-08
24493|Shoobridge Granite|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24493|Shoobridge Granite|42756|6|Mentioned|Fig.5 p6|||||||||02-MAR-18
24493|Shoobridge Granite|43140|4|Described|p47||Paleoproterozoic|Part of Cullen Batholith.||||||07-NOV-08
24493|Shoobridge Granite|43832|4|Described|40,46,50,55,62||Paleoproterozoic|Age: 1775+-16 Ma.||||||07-NOV-08
24493|Shoobridge Granite|45022|3|Fully described|p.143||Carpentarian|On many pages.||||||30-NOV-06
24493|Shoobridge Granite|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Mainly porphyritic hornblende-biotite adamellite with core of leucocratic adamellite and fringe of hornblende-biotite granodiorite.  Intrudes the Mount Partridge, South Alligator and Finniss River Groups.||||||07-NOV-08
24493|Shoobridge Granite|46676|14|Not recorded|map legend.||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
24493|Shoobridge Granite|50542|6|Mentioned|p95|Mesoproterozoic|Mesoproterozoic|Informal name. Geological Province: Yilgarn Craton. Intrudes the Ravensthorpe quartz diorite and a basaltic greenstone unit. Hosted by the Annabelle Volcanics.||||||07-FEB-11
24493|Shoobridge Granite|50586|5|Briefly described|p1.1, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Cullen Supersuite. Age: 1775 +/- 16Ma (U-Pb).||||||07-NOV-08
24493|Shoobridge Granite|63866|5|Briefly described|p110-p111, p117|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. |1775 +/- 16 Ma (ID-TIMS)|Cullen Supersuite||||
24493|Shoobridge Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Fine/medium biotite granite, fine porphyritic biotite granodiorite, fine/medium hornblende biotite tonalite.||||||07-JAN-09
24493|Shoobridge Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
24493|Shoobridge Granite|69420|5|Briefly described|p5:17-18, 20, 34, 108-109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Parent granite to the pegmatites which host the Mount Shoobridge tin field deposits.||Shoobridge Suite.||Intrudes Koolpin, Burrell Creek and Mount Bonnie Formations.|Medium-grained, concentrically-zoned from granodiorite through quartz monzonite to leucocratic quartz monzonite. I-type.|12-JUL-16
24493|Shoobridge Granite|69577|6|Mentioned|p117 Fig.6|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1775 Ma.|||||
24493|Shoobridge Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Shoobridge Suite.|||Dark grey to pink, mainly porphyritic hornblende-biotite granite; core of leucocratic granite and fringe of hornblende-biotite granodiorite.|
24493|Shoobridge Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1775+/-16.0 Ma (crystallisation: U-Pb).||||Granite.|
31733|Shoobridge Suite|69420|5|Briefly described|p5:17, 20|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Also appears mis-spelt as Shoebridge Suite in 5:20.|||Shoobridge, Tabletop, Mount Davis, Driffield Granites.||Zoned, hornblende-dominated granites.|12-JUL-16
31733|Shoobridge Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Bonrook, Driffield, Shoobridge, Tabletop Granites.|||01-MAR-18
26139|Short Range Sandstone|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Includes Deagan Member. Of Tomkinson Creek Subgroup, Churchills Head Group. Undifferentiated, quartz arenite; sublithic and lithic arenite; feldspathic sublitharenite; siltstone.||||||07-NOV-08
26139|Short Range Sandstone|23733|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group. Includes Deagan Member. Parts previously mapped as Hayward Creek Formation. Conformably overlain by Attack Creek Formation and conformably overlies Morphett Creek Formation.||||||07-NOV-08
26139|Short Range Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Tomkinson Creek Group.  Geological Province: Arunta Inlier.||||||
26139|Short Range Sandstone|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
26139|Short Range Sandstone|24172|3|Fully described|p30, p6 Tb.1, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Subgroup. Overlain by Attack Creek Formation (conformably); underllain by Morphett Creek Formation (conformably). Geological Province: Tennant Creek Inlier. Max. thickness: ~2025m in type section.||||||07-NOV-08
26139|Short Range Sandstone|24303|3|Fully described|p9, p4 Tb.2|Proterozoic|Proterozoic|Of the Tomkinson Creek Formation. Overlain by the Attack Creek Formation. Max. Thickness: 850m. Part of the Middle Tomkinson Creek Group. See also p3 Fig.2. Contains the Deagan Member.||||||
26139|Short Range Sandstone|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Includes the Deagan Member and undifferentiated quartz arenite, lensing, thin- to very thick-bedded, fine-grained to pebbly; rippled, cross-bedded.||||||07-NOV-08
26139|Short Range Sandstone|24442|5|Briefly described|p14|||Of the Tomkinson Creek Group.  Geological Province: Ashburton Province.||||||
26139|Short Range Sandstone|32174|6|Mentioned|Map legend|Carpentarian|Paleoproterozoic|Early Proterozoic or Carpentarian||||||07-NOV-08
26139|Short Range Sandstone|33307|6|Mentioned|Fig.8|||||||||
26139|Short Range Sandstone|35771|2|Defined|p25|early Carpentarian|early Carpentarian|Appendix.||||||
26139|Short Range Sandstone|39213|6|Mentioned|Fig.8|||||||||
26139|Short Range Sandstone|39624|5|Briefly described|Table 2|||||||||
26139|Short Range Sandstone|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Tomkinson Creek Subgroup.||||||07-NOV-08
26139|Short Range Sandstone|43224|5|Briefly described|Map legend||Proterozoic|Of Tomkinson Creek Subgroup.||||||30-NOV-06
26139|Short Range Sandstone|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group.||||||07-NOV-08
26139|Short Range Sandstone|60684|5|Briefly described|p5 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Subgroup (Churchills Head Group). Quartz arenite and lithic arenite, feldspathic sublitharenite, siltstone.  Conformably underlies Attack Creek Formation; conformably overlies Morphett Creek Formation.||||||07-NOV-08
26139|Short Range Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Tomkinson Creek Group. Contains the Deagan Member. Quartz arenite, sublithic and lithic arenite, feldspathic sublitharenite, and siltstone.  Overlies Morphett Creek Formation. In the Tennant Creek region.||||||07-NOV-08
26139|Short Range Sandstone|64780|5|Briefly described|p63 Fig.4 |Palaeoproterozoic|Palaeoproterozoic|||Of the Tomkinson Creek Group|Includes Deegan Member.|||
26139|Short Range Sandstone|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Tomkinson Creek Group||||
26139|Short Range Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Tomkinson Creek Group.|Includes Deagan Member.|Overlies Morphett Creek Formation.|Quartz arenite, lithic and sublithic arenite, feldspathic sublitharenite, and siltstone.|
26139|Short Range Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Tomkinson Creek Group.||||
26139|Short Range Sandstone|69424|6|Mentioned|p9:39 Fig.9.24|Paleoproterozoic|Paleoproterozoic|Tennant Creek area.||Tomkinson Creek Group.||||12-JUL-16
26139|Short Range Sandstone|69425|5|Briefly described|p10:12|||Tomkinson Province.|||Deagan, Mitty Members.|Correlated with Canulgerra Sandstone.||12-JUL-16
26139|Short Range Sandstone|69431|4|Described|p16:1, 3-6, 9-11, 23|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. 650-1025m thick. Lithology described and illustrated in detail. Shallow-marine, predominantly littoral to subtidal deposits; minor fluvial or deltaic deposits.||Tomkinson Creek Group.|Deagan Member.|Overlies Morphett Creek Formation conformably to disconformably. Is overlain by Attack Creek Formation conformably and transitionally, and unconformably by Gleeson Formation.|Thinly to very thickly bedded, fine- to coarse-grained sandstone; minor thinly bedded micaceous fine-grained sandstone and siltstone, and lesser laminated mudstone; some pebbly sandstone and conglomerate lags; rare halite pseudomorphs.|12-JUL-16
26139|Short Range Sandstone|69673|6|Mentioned|p58|||||Tomkinson Creek Group||||
23967|Shovel Billabong Andesite|22810|6|Mentioned|Table2 P4|||Maximum thickness: 300m.||||||30-NOV-06
23967|Shovel Billabong Andesite|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the South Alligator Group.||||||07-NOV-08
23967|Shovel Billabong Andesite|39069|5|Briefly described|Table 1|||||||||
23967|Shovel Billabong Andesite|39357|4|Described|p11|||||||||
23967|Shovel Billabong Andesite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
23967|Shovel Billabong Andesite|40243|6|Mentioned|p139|||Mention Fig.2||||||
23967|Shovel Billabong Andesite|40493|5|Briefly described|Table 1|||||||||
23967|Shovel Billabong Andesite|40808|5|Briefly described|Table 2|||||||||
23967|Shovel Billabong Andesite|41125|6|Mentioned|p26|||Mention Fig.15||||||
23967|Shovel Billabong Andesite|41309|6|Mentioned|p7|||||||||
23967|Shovel Billabong Andesite|41397|4|Described|p10|||||||||
23967|Shovel Billabong Andesite|41407|6|Mentioned|Map legend|Proterozoic||||||||
23967|Shovel Billabong Andesite|43187|5|Briefly described|p2|||||||||
23967|Shovel Billabong Andesite|43726|5|Briefly described|p3|||||||||
23967|Shovel Billabong Andesite|46658|6|Mentioned|Fig.5 P548|||||||||
23967|Shovel Billabong Andesite|47049|6|Mentioned|Fig.2|||||||||
23967|Shovel Billabong Andesite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the South Alligator Group.  Geological Province: Pine Creek Orogen. Massive pitchstone, variolitic andesite and porphyritic microdiorite.||||||14-JAN-05
23967|Shovel Billabong Andesite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1863Ma.Of South Alligator Group. Max thickness 300m. Dull grey-green, massive pitchstone, variolitic andesite and porphyritic microdiorite.||||||07-JAN-09
23967|Shovel Billabong Andesite|65232|5|Briefly described|p45|||With Gerowie Tuff, is interbedded within upper part of Koolpin Formation. Mount Bonnie Formation conformably overlies these units.||||||09-FEB-10
23967|Shovel Billabong Andesite|67564|4|Described|p7 Table 2, p21, p61.|Paleoproterozoic|Paleoproterozoic|300 m thick; submarine. Has a gravity high and a distinct, moderate to high, linear magnetic signature. Very similar geochemistry to Zamu Dolerite.|c.1865 Ma.|Unit in South Alligator Group.|||Green-grey, massive pitchstone; variolitic andesite; microdiorite.|
23967|Shovel Billabong Andesite|69420|5|Briefly described|p5:8, 13-14, 51|Paleoproterozoic|Paleoproterozoic|South Alligator region, Pine Creek Orogen. Up to 300m thick. Submarine depositional environment.||South Alligator Group.||A concordant body within the Gerowie Tuff.|Green-grey, massive pitchstone; variolitic andesite, microdiorite. Contains mainly sodic plagioclase and minor augite phenocrysts in a holocrystalline groundmass of the same composition.|12-JUL-16
23967|Shovel Billabong Andesite|70293|5|Briefly described|p597, p599-600|Paleoproterozoic|Paleoproterozoic|||South Alligator Group||Intruded by Zamu Dolerite sills.||
41979|Showell Member|23937|2|Defined|p93 App. 1, p35|Calymmian|Calymmian|Of Mainoru Fm (Collara Subgp, Roper Gp).  Conformably overlain by Crawford Fm, disconformably by Jalboi Fm; conformably overlies Wooden Duck Mbr.  Age: 1492+/-4, 1493+/-4Ma (SHRIMP, Jackson et al, 1999). Max. thick: >155m.||||||03-NOV-04
41979|Showell Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group).  Laminated calcareous and non-calcareous mudstone; medium bedded laminated limestone with minor thin interbeds of glauconitic siltstone and sandstone.||||||14-FEB-05
41979|Showell Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Laminated calcareous and non-calcareous mudstone; medium bedded laminated limestone with minor thin interbeds of glauconitic siltstone and sandstone.||||||23-DEC-09
41979|Showell Member|69430|4|Described|p15:26-27, 30|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 40m to over 155m thick. Distal to storm-dominated shelf sediments.||Topmost Mainoru Formation.||Conformably overlies Wooden Duck Member. Is overlain conformably by Crawford Formation, or disconformably by Jalboi Formation.|Laminated calcareous mudstone; scattered glauconite, sulfides, and carbonate nodules; laminated limestone near base.|12-JUL-16
41979|Showell Member|70968|2|Defined|p17-18,20,30, 33-35, 123,131,140,143|Calymmian|Calymmian|Sweet in Abbott et al. (2001). Named after Showell Creek. Appeared as Showell Creek Member in MOUNT MARUMBA sheet (Sweet et al., 1999). The type section is from 442300mE 8464000mN (base) to 443900mE 8463200mN in MOUNT MARUMBA sheet. Recessive: forms low rises and pavements littered with mudrock rubble. Very similar mineralogy and texture to Wooden Duck Member: difficult to tell apart. Lithology described and illustrated. Thickens eastward, from 155m to possibly 700m. Marine storm-dominated shelf deposits. SHRIMP U-Pb zircon ages from tuffs.|1492 +/- 4; 1493 +/- 4 Ma.|Mainoru Formation.||Conformably overlies Wooden Duck Member. Is overlain by Crawford Formation gradationally, or locally by Jalboi Formation disconformably. Is intruded by Derim Derim Dolerite.|Dominantly green-grey to black mudrocks, commonly laminated and calcareous claystone and siltstone; thinly interlaminated, very fine-grained micaceous and glauconitic sandstone, and minor limestone towards the base. Secondary chert near top.|10-NOV-17
41979|Showell Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 64 - 346+ m thick. Storm-dominated marine shelf deposits.||Topmost Mainoru Formation.||Conformably overlies Wooden Duck Member. Is overlain conformably by Crawford Formation, and unconformably to disconformably by Jalboi Formation.|Green-grey to green-black and black mudrocks, thinly interbedded and interlaminated very fine sandstone, minor limestone near base.|
41979|Showell Member|71494|4|Described|p2-p4, p6-p8, p11-p13, p17, p26|||Thickness ranges from 40 to 155 metres plus. Deposited in distal to storm-dominated shelf environments. The uppermost mudstone is generally non-calcareous, strongly laminated and forms excellent flagstones. Core log features presented in this volume.||Mainoru Formation||Conformably overlies the Wooden Duck Member. Conformably overlain by the Crawford Formation or disconformably by Jalboi Formation.|Laminated calcareous mudstone, scattered glauconite, sulphides and carbonate nodules, laminated limestone near the base.|
41979|Showell Member|71779|5|Briefly described|p2, p23, 24, 26|Calymmian|Calymmian|Urapunga Region, McArthur Basin. SHRIMP ages are from rare tuffs in this member.|1492 +/- 4 Ma and 1493 +/- 4 Ma (SHRIMP U-Pb)|Mainoru Formation||Overlain by the Amungee Member of the Velkerri Formation.|Rare tuffs.|24-SEP-18
41979|Showell Member|71893|5|Briefly described|p9, p13, p20, p25, p32|||McArthur Basin. SHRIMP ages are derived from Jackson et al, 1999.|1492 +/- 4 Ma and 1493 +/- 4 Ma (SHRIMP)|Mainoru Formation||Overlies the Limmen Sandstone.||
41979|Showell Member|72718|6|Mentioned|p9|Calymmian|Calymmian|Ages from rare tuffs in the member.|1492 +/- 4 Ma, 1493 +/- 4 Ma SHRIMP U-Pb|Mainoru Formation, Collara Subgroup, Roper Group||||
41979|Showell Member|73242|5|Briefly described|p39|||||Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Wooden Duck Member. Overlain by Crawford Formation. Intruded by Derim Derim Dolerite.|Includes interbedded mudstone and fine sandstone.|
24495|Simpsons Gap Metasediments|38606|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24495|Simpsons Gap Metasediments|38885|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24495|Simpsons Gap Metasediments|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24495|Simpsons Gap Metasediments|41816|4|Described|p7|||||||||
24495|Simpsons Gap Metasediments|41837|6|Mentioned|Map legend|Proterozoic||||||||
24495|Simpsons Gap Metasediments|43225|5|Briefly described|Map Legend||Paleoproterozoic|Of Iwupataka Metamorphic Complex.||||||07-NOV-08
24495|Simpsons Gap Metasediments|43503|5|Briefly described|8,23|||||||||
24495|Simpsons Gap Metasediments|44114|5|Briefly described|p317, 321|||Southern Arunta Inlier. Felsic volcanic and volcaniclastic rocks. Appears first (p317) as Simpsons Gap metasediments.|1650-1610 Ma (Zhao and Bennett, 1995).||||Platform-style sediments: quartzite-shale-carbonate successions. Felsic and pelitic gneisses and schists.|
24495|Simpsons Gap Metasediments|48992|2|Defined|p47|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24495|Simpsons Gap Metasediments|50369|6|Mentioned|p22.2|||||||||
24495|Simpsons Gap Metasediments|69428|5|Briefly described|p13:06|Paleoproterozoic|Paleoproterozoic|Eastern Haasts Bluff Domain, Warumpi Province. The dominant unit east of Standley Chasm. Also appears as Simpsons Gap Metamorphics on 13:6.||Iwupataka Metamorphic Complex.||Unconformably overlies the Sadadeen Gneiss. Is overlain ?conformably by Rungutjirba Gneiss.|Basal conglomerate and grit conglomerate grading upwards into a succession of biotite-muscovite-andalusite +/- sillimanite schist (locally with garnet and/or staurolite), quartzite, quartz-muscovite phyllite, meta-arkose and minor amphibolite.|12-JUL-16
24495|Simpsons Gap Metasediments|69925|6|Mentioned|p21|||Southern Arunta Province, Arunta Inlier.||||Is intruded by Burt Bluff Gneiss.||
24495|Simpsons Gap Metasediments|69931|6|Mentioned|p281|||Arunta Inlier. Presented as Simpsons Metasediment.||||Is intruded by, and interlayered with, the Burt-Rungutjirba Suite.||
24495|Simpsons Gap Metasediments|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphism age. |1149+/-12 Ma (monazite U-Pb LA-ICPMS).||||Metapelite.|
26141|Skinner Sandstone|28255|3|Fully described|p69, Tb. 11 (opp. p8)|Adelaidean|Adelaidean|Of Duerdin Gp. Massive x-bedded grey, medium to coarse gr.and conglomeratic sst. Overlies Angalarri Sltst on WATERLOO, not clear elsewhere. Truncates both Ang.Sltst.and Saddle Cr Fm on AUVERGNE. Unconformable on Auvergne Gp acc. to Pontifex et al (1968)||||||15-JUN-05
26141|Skinner Sandstone|32699|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin group.  Grey and brown dolomitic sandstone conglomeratic sandstone, conglomerate.||||||02-DEC-04
26141|Skinner Sandstone|32701|4|Described|Table 1|||Adelaidean. See p14. Of the Duerdin Group.||||||30-NOV-06
26141|Skinner Sandstone|33375|6|Mentioned|p11 Tb. 1, p13|Adelaidean|Adelaidean|Of the Duerdin Group. Medium and coarse quartz sandstone, dolomitic sandstone, conglomerate; minor tillite; strongly cross-bedded. Highly lenticular.||||||28-APR-05
26141|Skinner Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26141|Skinner Sandstone|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Duerdin Group. Medium and coarse quartz sandstone, dolomitic sandstone, conglomerate; minor tillite.||||||28-APR-05
26141|Skinner Sandstone|37927|5|Briefly described|p507|||||||||
26141|Skinner Sandstone|45112|4|Described|p36|||||||||
26141|Skinner Sandstone|48938|2|Defined|p60|Adelaidean|Adelaidean|||||||
26141|Skinner Sandstone|48943|3|Fully described|p79|||||||||
26141|Skinner Sandstone|60006|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Geological Province: Wolfe Creek Basin. Of Duerdin Group. Unconformably overlies Angalarri Siltstone. Unconformably overlain by Fargoo Tillite. Basal diamictite, dolomitic sandstone, conglomerate.||||||21-JUL-04
26141|Skinner Sandstone|60682|4|Described|p17, 18|Neoproterozoic|Neoproterozoic|Of Duerdin Group. Unconformably overlies Auvergne Group. Conformably overlain by Fargoo Tillite. Max. thickness: >60m. Basal diamictite, dolomitic sandstone, conglomerate. Geological Province: Wolfe Creek Basin.||||||
26141|Skinner Sandstone|63458|6|Mentioned|p886 Fig.11. |Neoproterozoic|Neoproterozoic|||Unit in Duerdin Group.||||
26141|Skinner Sandstone|64104|6|Mentioned|p63 Fig.1|||Local unit in Keep River area.||||Is overlain by Fargoo Formation.||
26141|Skinner Sandstone|65331|5|Briefly described|Map legend|Neoproterozoic |Neoproterozoic |Of Duerdin Group, Wolfe Creek Basin. Basal diamictite, dolomitic sandstone, conglomerate ||||||
26141|Skinner Sandstone|67151|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Wolfe Basin.||Unit in Duerdin Group.||Is overlain by Fargoo Tillite.|Basal diamictite, medium and coarse quartz sandstone, dolomitic sandstone, conglomerate.|
26141|Skinner Sandstone|69437|5|Briefly described|p22:4-5, 7|Cryogenian|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3.||Duerdin Group.||Is overlain by Fargoo Tillite.||12-JUL-16
26141|Skinner Sandstone|69442|5|Briefly described|p27:1-2, 3 Tb.27.1, 5|||Wolfe Basin. Highly variable thickness: 0-60m in AUVERGNE map area; thicker in paleovalleys elsewhere. The basal diamictite may be a lateral equivalent of Moonlight Valley or Fargoo Tillites.||Duerdin Group.||Unconformably overlies Auvergne Group. Is overlain conformably by Fargoo Tillite. Possible correlative of Big Knob beds.|Basal diamictite of boulders, cobbles and pebbles in green shale; medium-grained, cross-bedded dolomitic sandstone, with lenses of conglomerate.|12-JUL-16
26141|Skinner Sandstone|69673|5|Briefly described|p190|Neoproterozoic|Neoproterozoic|||Duerdin Group|||Diamictite and dolomitic sandstone with lenses of conglomerate.|
26141|Skinner Sandstone|70206|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin. ||Duerdin Group|||Basal diamictite, dolomitic sandstone, conglomerate.|
26141|Skinner Sandstone|70655|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Wolfe Basin||Shown as base of Duerdin Group.||Shown as overlain by Fargoo Tillite.|Basal diamictite, medium and coarse quartz sandstone, dolomitic sandstone, conglomerate.|
26141|Skinner Sandstone|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||diamictite, sandstone|
26900|Slatey Creek Granite|22446|6|Mentioned|p19|Statherian|Statherian|||||||
26900|Slatey Creek Granite|24197|5|Briefly described|p26, p84 Tb. 10.1|Paleoproterozoic|Paleoproterozoic|Part of the Granites Supersuite. Age: 1810Ma. Geological province: Granites-Tanami Block.||||||07-FEB-11
26900|Slatey Creek Granite|29813|4|Described|Table 2|||||||||
26900|Slatey Creek Granite|29818|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26900|Slatey Creek Granite|36532|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26900|Slatey Creek Granite|39888|6|Mentioned|Fig.7|||||||||
26900|Slatey Creek Granite|41465|6|Mentioned|p13|||||||||
26900|Slatey Creek Granite|42504|5|Briefly described|Table 3 P60|||||||||
26900|Slatey Creek Granite|45140|2|Defined|p12-13, p15-16, p22-25, p32-35, p37-38|Paleoproterozoic|Paleoproterozoic|See also p47, p74, Appx.p10. Blake et al. (1977). The Granites-Tanami Block. Scattered outcrops SW of Gardner Range; most to the S of Slatey Creek after which the unit is named. Previously mapped as part of Lewis Granite by Casey and Wells (1964). The type area is a 60m high scarp face, 16km NNW of Tent Hill, at 19deg 22'S, 128deg 41'30"E. Chemically similar to Winnecke Granophyre; geochemistry detailed.|1770 +/- 62 Ma (Rb-Sr: Page et al., 1976).|||Intrudes the Killi Killi Beds (Tanami Complex). Is overlain by Gardiner Sandstone and caps of Lewis Range Sandstone.|Porphyritic and non-porphyritic, mainly medium- to fine-grained muscovite, biotite-muscovite, and biotite adamellite; minor biotite granodiorite, pegmatite and aplite veins.|
26900|Slatey Creek Granite|46788|4|Described|p10|||Entered as in NT, but probably wrong [CEBJan97].||||||
26900|Slatey Creek Granite|46864|6|Mentioned|p37|||Re age dates||||||
26900|Slatey Creek 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: 1733 +/- 55Ma (Rb-Sr).||||||07-NOV-08
26900|Slatey Creek Granite|62580|5|Briefly described|p47|||Of the Frederick Suite. Possibly misspelt and should be MacFarlane Peak Monzogranite in the singular???||||||07-FEB-11
26900|Slatey Creek Granite|63261|6|Mentioned|p16|||Included in the Grimwade Suite.||||||07-FEB-11
26900|Slatey Creek Granite|64277|5|Briefly described|Map ledgend|Paleoproterozoic|Paleoproterozoic|Age: 1795Ma. Muscovite and biotite monzogranite; locally porphyritic; minor biotite granodiorite.||||||24-NOV-15
26900|Slatey Creek Granite|64580|4|Described|map legend||Paleoproterozoic|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.||||||09-DEC-08
26900|Slatey Creek Granite|64733|5|Briefly described|p170 Fig.2, p175, p176 Fig.7|Statherian|Statherian||~1795 Ma.|||Intrudes lower part of Stubbins Formation.||20-APR-12
26900|Slatey Creek Granite|66129|5|Briefly described|p213, p214, p214 Fig.1, p215 Fig.2, p217|||6000 sq. km, continuous ellipsoidal shapes. In Frederick Suite. Fine to medium grained seriate monzogranite to granodiorite, overprinted by scarce pegmatite and aplite dykes.||||||
26900|Slatey Creek Granite|66468|6|Mentioned|p16-18 Figs.2,3,5; p20, p22, p25-27|Paleoproterozoic|Paleoproterozoic|Moderately magnetic.||||||
26900|Slatey Creek Granite|67826|5|Briefly described|p401 Fig.2, p408|Statherian|Orosirian|A large pluton several tens of kilometers in diameter with a narrow (<1 km) contact hornfels zone.|~ 1793 +/- 8 Ma (Bagas et al. 2010)|||||
26900|Slatey Creek Granite|68474|6|Mentioned|p572-573|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.||||||
26900|Slatey Creek Granite|68656|5|Briefly described|GEOL_LUT_CSV/100k_interpgeop_lut|Paleoproterozoic|Paleoproterozoic|See also 100k_maginterpgeop_lut.csv, and 500k_geologyp08_lut.csv. Granites-Tanami Complex. Non- to highly magnetic. 1796 +/- 5 Ma (SHRIMP, GA).|c.1815-1790 Ma (Huston et al., in press).|Frederick Suite|||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|27-NOV-15
26900|Slatey Creek Granite|69099|5|Briefly described|500k_geologyp08_lut.csv||Paleoproterozoic||||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|04-AUG-15
26900|Slatey Creek Granite|69253|6|Mentioned|p753, p757, p758|||Trans-Tanami Fault Corridor, Granites-Tanami Orogen.||||||
26900|Slatey Creek Granite|69426|6|Mentioned|p11:10|||Blake et al. (1979).||||||12-JUL-16
26900|Slatey Creek Granite|69587|4|Described|GEOL_LUT_CSV files + geochron files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen, North Australian Craton. Events: Alice Springs Orogeny; Tanami Orogeny D1t. See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 500k_geologyp08_lut.csv.|1820-1790 Ma (inferred)|||Overlain unconformably by Lewis Range Sandstone.|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite|
26900|Slatey Creek Granite|70141|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70142|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.|||Is faulted against Killi Killi Formation. Is overlain by Lewis Range Sandstone.|Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70143|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1820-1790 Ma.||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|70154|4|Described|500k_interpgeop14_lut.csv|Paleoproterozoic|Paleoproterozoic||1790-1820 Ma||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite|
26900|Slatey Creek Granite|71080|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. ||||Unconformably underlies Lewis Range Sandstone.||
26900|Slatey Creek Granite|71267|4|Described|GEOL_LUT_CSV files|Paleoproterozoic|Paleoproterozoic|Geological province: Granites-Tanami Orogen. Alice Springs Orogeny (450-295 Ma); Stafford Event (1810-1790 Ma). See 1m_geologyp12_lithology_lut.csv, 1M_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv.|1795 Ma (inferred)|Unit of The Granites Supersuite.|||Porphyritic and non-porphyritic, mainly medium to fine grained, muscovite, biotite-muscovite, and biotite monzogranite; minor biotite granodiorite. Some pegmatite and aplite veins.|
26900|Slatey Creek Granite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen. Age inferred.|||||Muscovite and biotite monzogranite, locally porphyritic; minor biotite granodiorite.|
26900|Slatey Creek Granite|73089|6|Mentioned|p3, p8, p38|Statherian|Statherian|Geochron is an upper intercept date from Bagas et al. (2010). May be associated with the 1810-1790 Ma Stafford Event.|1793 +/- 8 Ma||||Monzogranites to granodiorites.|
26142|Sly Creek Sandstone|22538|6|Mentioned|P714||Statherian|||||||
26142|Sly Creek Sandstone|22670|6|Mentioned|52|||Geological Province: McArthur Basin.||||||14-APR-08
26142|Sly Creek Sandstone|22853|3|Fully described|6|Proterozoic|Proterozoic|Geological Province: McArthur Basin. Of the Tawallah Group. Max thickness: 770 m. Underlain by Seigal Volcanics.||||||14-APR-08
26142|Sly Creek Sandstone|23065|5|Briefly described|16|||Geological Province: McArthur Basin. Of the Tawallah Group. Overlain by Aquarium Formation; underlain by McDermott Formation.||||||14-APR-08
26142|Sly Creek Sandstone|23197|6|Mentioned|p850|||Referred to as Yiyinti-Sly Creek Sandstone.||||||
26142|Sly Creek Sandstone|23363|5|Briefly described|344 Fig.3|||||||||
26142|Sly Creek Sandstone|23374|6|Mentioned|p42||Statherian|Equivalent to Gumarrirnbang Sandstone. Of the Tawallah Group; in the McArthur Basin.||||||04-DEC-06
26142|Sly Creek Sandstone|23395|5|Briefly described|p388 Fig.4|||||||||
26142|Sly Creek Sandstone|23396|5|Briefly described|p407 Fig.2|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
26142|Sly Creek Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
26142|Sly Creek Sandstone|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with upper part of Kombolgie Subgroup (Katherine River Group).  Geological Province: McArthur Basin.||||||
26142|Sly Creek Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
26142|Sly Creek Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group.||||||14-APR-08
26142|Sly Creek Sandstone|24050|5|Briefly described|p16|||Of the Tawallah Group.  Geological Province: McArthur Basin.||||||04-DEC-06
26142|Sly Creek Sandstone|31421|6|Mentioned|p507|||||||||
26142|Sly Creek Sandstone|32660|5|Briefly described|Table 4|||||||||
26142|Sly Creek Sandstone|33665|6|Mentioned|p366|||See also p368.||||||04-DEC-06
26142|Sly Creek Sandstone|35114|6|Mentioned|p203|||||||||
26142|Sly Creek Sandstone|35640|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|36012|3|Fully described|Table 2|||||||||
26142|Sly Creek Sandstone|36439|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|36442|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
26142|Sly Creek Sandstone|37568|5|Briefly described|p78|||||||||
26142|Sly Creek Sandstone|38582|6|Mentioned|Fig.3|||||||||
26142|Sly Creek Sandstone|38584|4|Described|p14|||||||||
26142|Sly Creek Sandstone|39445|5|Briefly described|Table 2|||See also p36.||||||04-DEC-06
26142|Sly Creek Sandstone|39791|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26142|Sly Creek Sandstone|40489|6|Mentioned|p89|||||||||
26142|Sly Creek Sandstone|40691|5|Briefly described|p9|||||||||
26142|Sly Creek Sandstone|41013|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
26142|Sly Creek Sandstone|41721|3|Fully described|p20|||Of the Tawallah Group. Thickness: 320m. Conformably overlies McDermott Formation, grading into glaucontic sandstone of the Aquarium Formation above. Geological province: McArthur Basin. Sandstone, fine- to medium-grained, laminated, well sorted...........||||||01-AUG-07
26142|Sly Creek Sandstone|41722|6|Mentioned|Map legend|Mesoproterozoic||||||||
26142|Sly Creek Sandstone|42385|3|Fully described|p6-7, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Tawallah Group. Includes Rosie Creek Sandstone Mbr. Conformable over Seigal Volcanics. Max. thick: 770m. Sandstone, very fine- to very coarse-grained, conglomeratic sandstone feldspathic in places; arkosic ferruginous or galuconitic.||||||18-SEP-07
26142|Sly Creek Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
26142|Sly Creek Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.|Includes: Rosie Creek Sandstone Member at top.|In schematic section, underlies Aquarium Formation; overlies Seigal Volcanics.|Quartzarenite, pebble beds common in upper part; minor siltstone and shale. Detailed lithology given.|09-NOV-11
26142|Sly Creek Sandstone|42639|3|Fully described|p10 Table 4 p11|||||||||
26142|Sly Creek Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
26142|Sly Creek Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Quartzarenite, white to pale pink, mainly fine to medium grained and thin to very thick bedded with rare quartz pebble beds.||||||19-OCT-05
26142|Sly Creek Sandstone|42812|3|Fully described|p11, Table 3|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterzoic" age.||||||04-DEC-06
26142|Sly Creek Sandstone|43036|3|Fully described|p15|||Of Tawallah Group.||||||04-DEC-06
26142|Sly Creek Sandstone|44287|14|Not recorded|p.8, opp.7|||(E53-3).||||||
26142|Sly Creek Sandstone|44288|14|Not recorded|map legend||Paleoproterozoic|Quartz sandstone, pebbly bands, minor siltstone. Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44305|14|Not recorded|p.6,12|||(E53-8). opp.p.6,18.||||||
26142|Sly Creek Sandstone|44306|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44473|14|Not recorded|p.8, opp. p.7|||(E53-7).||||||
26142|Sly Creek Sandstone|44474|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|44530|14|Not recorded|p.4,8, opp.8|||(D53-15).||||||
26142|Sly Creek Sandstone|44531|14|Not recorded|map legend||Paleoproterozoic|Lower Proterozoic.||||||07-NOV-08
26142|Sly Creek Sandstone|45162|2|Defined|p19|Proterozoic|Proterozoic|Revised herein. Rosie Creek Sandstone incorporated into Sly Creek Sandstone.||||||21-FEB-18
26142|Sly Creek Sandstone|45166|5|Briefly described|p28|||||||||
26142|Sly Creek Sandstone|46804|6|Mentioned|p154|||||||||
26142|Sly Creek Sandstone|49001|6|Mentioned|p5|||||||||
26142|Sly Creek Sandstone|60483|5|Briefly described|p7 Fig. 5, p27|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
26142|Sly Creek Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Includes Rosie Creek Sandstone Member. Overlain by Aquarium Formation, underlain by Seigal Volcanics.||||||
26142|Sly Creek Sandstone|62082|5|Briefly described|p115|Proterozoic|Proterozoic|Geological Province: Carpentaria Terrain.||||||07-FEB-11
26142|Sly Creek Sandstone|62084|6|Mentioned|p936 Fig.5|||Leichhardt Superbasin. Shown as Sly Ck Sst.||||||
26142|Sly Creek Sandstone|63112|5|Briefly described|p1190-1192, Tb.1, p1194, p1206|||Leichhardt Superbasin. Age approximated from Fig.2. 200-770 m thick.|c.1755-1760 Ma.||||Pebblestone conglomerates and coarse-grained pebbly sandstones overlain by a semi- to supermature quartzarenite, which is in turn overlain by coarser grained pebbly sandstones.|
26142|Sly Creek Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
26142|Sly Creek Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p370 |||A SW-thickening siliciclastic apron west of a basaltic volcanic zone in the Murphy Tectonic Ridge.||Of the Tawallah Group.|Includes Rosie Creek Sandstone Member.|||
26142|Sly Creek Sandstone|65228|5|Briefly described|p21, Figs.02, 05, 06, 07.|||McArthur Basin.||Unit in Tawallah Group.||Equivalent to McDermott Formation.||
26142|Sly Creek Sandstone|65337|6|Mentioned|p14. |||Southern McArthur Basin. Correlated with Gator Sandstone. Contains a local basalt interval.||||||
26142|Sly Creek Sandstone|65340|4|Described|p12 Fig.6. |||Revised in this study. Defined by Roberts et al. (1963) and Ahmad and Wygralak (1989); this study removes the unit underlying the Aquarium Formation throughout the Wearyan Shelf, and incorporates it into the Wununmantyala Sandstone [??].||Unit in Tawallah Group.|Includes Rosie Creek Sandstone Member.|Overlies Seigal Volcanics. Is overlain by McDermott Formation.||21-FEB-18
26142|Sly Creek Sandstone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Ridge-forming.||Unit in Tawallah Group.||Overlies McDermott Formation. Is overlain by Settlement Creek Volcanics.|Fine- to medium-grained quartz arenite; pebble beds common in upper part; planar to trough cross-beds, channel-lag deposits, ripples, minor graded bedding, rare dessication cracks; minor thinly-bedded siltstone and shale, commonly micaceous.|
26142|Sly Creek Sandstone|67323|4|Described|GIS attrib tbl, Solid Geology Map, p31|Paleoproterozoic|Paleoproterozoic|See also Eastern Australia Time-Space Plot. McArthur Basin, Leichhardt Superbasin.|1787 +/- 17 Ma (maximum depositional age).|Tawallah Group.||Overlies Seigal Volcanics.|White, pink or grey massive medium-grained quartzose sandstone, pebbly sandstone, conglomerate.|
26142|Sly Creek Sandstone|67352|4|Described|p15 Tb.2|Statherian|Statherian|McArthur Basin. 900 m thick. Forms prominent ridges.||Tawallah Group||Cconformably overlies McDermott Formation or Seigal Volcanics. Overlain conformably by Settlement Creek Volcanics.|Very fine- to very coarse-(mainly medium)-grained quartz arenite: glauconitic, feldspathic, arkosic; minor pebbly sandstone, conglomerate, micaceous siltstone, shale, chert breccia, dolarenite.|
26142|Sly Creek Sandstone|67564|5|Briefly described|p86.|||Southern McArthur Basin.||Unit in Tawallah Group.|Includes Rosie Creek Member.|||
26142|Sly Creek Sandstone|67779|5|Briefly described|p36.|||Lower parts are correlated with Gumarrirnbang Sandstone.|1787 +/- 17 Ma (Hollis et al. 2010a).|Unit in Tawallah Group.||||
26142|Sly Creek Sandstone|69383|5|Briefly described|p52-54||Paleoproterozoic|McArthur Basin. LA-ICPMS U-Pb geochronology analyses.  Max deposition age.|1787+/-17 Ma||||An orange, medium-grained sandstone with prominent wave ripple-marks was sampled from top of unit.|
26142|Sly Creek Sandstone|69430|4|Described|p15:3, 10-12|||The previous definition was replaced by Wununmantyala Sandstone (as defined by Pietsch et al., 1991); the name is now used for the succession overlying the Seigal Volcanics in the Batten Fault Zone and SW McArthur Basin. 320m thick (also said to be up to 900m thick with Rosie Creek Sandstone Member). Nearshore shallow-marine deposits. Is stated to conformably overlie McDermott Formation, but this contradicts the relationships shown in Fig.15.4, and is inconsistent with Sly Creek Sandstone being correlated with upper Seigal Volcanics which conformably underlies McDermott Formation.||Tawallah Group.|Rosie Creek Sandstone Member.|Overlies Seigal Volcanics. Is overlain conformably and gradationally by Aquarium Formation. Correlated with upper Seigal Volcanics.|White, pink or grey massive medium-grained quartz sandstone, pebbly sandstone, conglomerate.|12-JUL-16
26142|Sly Creek Sandstone|69591|5|Briefly described|p39, p58|||Camooweal-Murphy Domain, Mount Isa Province. Part of the McArthur Basin succession. Alluvial braidplain deposits.||Tawallah Group.||Lateral equivalent of Peters Creek Volcanics.|White, pink or grey massive medium-grained quartzose sandstone, pebbly sandstone, conglomerate.|
26142|Sly Creek Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group|Includes Rosie Creek Sandstone Member|Overlies Seigal Volcanics||
26142|Sly Creek Sandstone|70849|5|Briefly described|Map legend.|Statherian|Statherian|McArthur Basin.||Tawallah Group.||Overlies McDermott Formation. Is overlain by Aquarium Formation.|Lithic and quartz sandstone, fine- to medium-grained, flaggy, locally feldspathic; minor conglomerate.|
26142|Sly Creek Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1787+/-17 Ma (MDA: U-Pb zircon LA-ICPMS).||||Ripple-martked sandstone.|
26142|Sly Creek 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||Partially overlies and is laterally equivalent to Seigal Volcanics and underlies Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group||Underlain by and partly equivalent to Seigal Volcanics. Overlain by Rosie Creek Sandstone Member. Equivalent[?] to Carolina Sandstone Member.||
26142|Sly Creek Sandstone|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. Shown as Sly Creek Formation p19.||Tawallah Group||Partially overlies Seigal Volcanics and underlies Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Leichhardt Superbasin.||Tawallah Group||Underlain by and partly correlated to Seigal Volcanics. Overlain by Rosie Creek Sandstone Member.||
26142|Sly Creek Sandstone|73412|5|Briefly described|p4, 8-9, 14|||Southern McArthur Basin. Non-magnetic.||Tawallah Group.||Overlies Seigal Volcanics. Is overlain by Rosie Creek Sandstone.||
33827|Snowdrop Sandstone Member|23867|2|Defined|p22 Appendix|Statherian|Statherian|Of McKay Sandstone.  Overlain disconformably by Cottee Formation.  Age: 1822-1720Ma.  From stratigraphically lower Plum Tree Creek Volcanics and younger Jimbu Microgranite. Max. thickness: 50m.  Geological Province: McArthur Basin.  See also p9, Table 1 and Fig. 3||||||22-SEP-18
33827|Snowdrop Sandstone Member|60680|5|Briefly described|Map legend|Statherian|Statherian|Of McKay Sandstone (Kombolgie Subgroup, Katherine River Gp). White medium bedded and trough cross-bedded, medium qrtz sandstone with scattered mudstone intraclasts; thinly to medium bedded, wave-rippled sandstone. Geol.Prov: McArthur Basin.||||||
33827|Snowdrop Sandstone Member|67564|2|Defined|p6 Table 2, p43, p46, p86.|Statherian|Statherian|New name. Named after Snowdrop Creek, a tributary of Katherine River. Thickness c.30-50 m. Type section is on a tributary of Snowdrop Creek. Forms narrow strike ridges; its upper surface forms a distinctive white dip slope marker bed. Shallow marine, probably shoreline, deposits. Age constrained by ages of stratigraphically lower Plum Tree Creek Volcanics and younger Jimbu Microgranite.|Between 1822 Ma and 1720 Ma.|Unit in McKay Sandstone.||Conformably overlies lower part of McKay Sandstone. Is overlain disconformably by Cottee Formation.|Basal 8 m of thickly-bedded, trough cross-bedded medium sandstone; overlain by 30-40 m of medium-bedded, internally horizontally laminated, strongly wave-rippled, white, medium-grained quartz sandstone; glauconitic; scattered mudstone intraclasts.|
40018|Southwark Suite|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Age: 1570Ma.  Geological Province: Arunta Province.||||||
40018|Southwark Suite|24197|5|Briefly described|p26, p58|Mesoproterozoic|Mesoproterozoic|Example of the Cullen Association. Fractionated, with broad compositional range - pegmatite, aplite, microgranite and greisen phases. Ages: 1570Ma and 1567Ma. Geological Province: Arunta Inlier. Same unit as Southwark Granite Suite?||||||07-FEB-11
40018|Southwark Suite|50369|5|Briefly described|p1.2, 1.5, 24.1, Table 1.1|Mesoproterozoic|Mesoproterozoic|Geological Province: Arunta Inlier. Age: 1567-1570Ma.||||||
40018|Southwark Suite|61246|6|Mentioned|p62|||Includes granite in the Arunta region (Aileron Province).||||||
40018|Southwark Suite|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Wabudali Granite [does it really?]. Age: <1760Ma.  Geological Province: Arunta region - Aileron Province.||||||27-OCT-10
40018|Southwark Suite|62633|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Arunta Region - Aileron Province.||||||16-AUG-06
40018|Southwark Suite|62636|6|Mentioned|Map Legend|||Solid Geology legend.||||||15-APR-11
40018|Southwark Suite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Southwark Granite Suite. Geol Prov: Arunta Region - Aileron Province.||||||28-SEP-11
40018|Southwark Suite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Abbreviation of Southwark Granite Suite. Geol Prov: Arunta Region - Aileron Province||||||28-SEP-11
40018|Southwark Suite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Includes Yunkanjini Granite.  [Although shown as Paleoproterozoic, also shown as younger than 1590-1570 Ma Chewings Event ie Mesoproterozoic. Map key is missing 'Mesoproterozoic']||||||27-SEP-11
40018|Southwark Suite|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Aileron Province. Includes Yarunganyi granite. Age < 1700 Ma (younger than 1730-1700 Strangways Event)?||||||
40018|Southwark Suite|65455|6|Mentioned|p6 Fig. 3|||Within the Arunta region, on northern margin of the Ngalia Basin. Has been identified as having potential for Cu, Au, Ta, Mo and W mineralisation.||||||09-MAY-12
40018|Southwark Suite|67323|5|Briefly described|p90|||Georgina Basin. Heat production for geothermal energy briefly discussed.|||||Granite.|
40018|Southwark Suite|69383|6|Mentioned|p77|||Arunta region, Aileron Province. Magmatic expression of Chewings Orogeny (1590-1560 Ma).|||||Granites.|
40018|Southwark Suite|69417|6|Mentioned|p2:5|Calymmian|Calymmian|Aileron Province.||||||12-JUL-16
40018|Southwark Suite|69427|4|Described|p12:3, 40 Fig.12.34; 12:44-45, 63|Mesoproterozoic|Mesoproterozoic|Formerly the Southwark Granitic Suite (Young et al., 1995). Crops out immediately N of the Ngalia Basin, Aileron Province. Interpreted to be the source of tungsten mineralisation at Wolfram Hill. Hosts a significant U occurrence at Anomaly B, 10km N of Rankins Reward, and is a potential source for surficial or sandstone-hosted U deposits.|c.1570-1530 Ma.||Wakurlpa, Yarunganyi, Ethel Creek, Yunkanjini Granites.||Undeformed, biotite and biotite-muscovite granite, commonly containing K-feldspar megacrysts (typically >1cm, locally up to 10cm long); local rapakivi granite. High SiO2, K, Th and U; high heat-producing granite with I-type affinities.|12-JUL-16
40018|Southwark Suite|69439|5|Briefly described|p24:6|Mesoproterozoic|Mesoproterozoic|Part of basement to Ngalia Basin.||||Is overlain unconformably, and with thrust contact, by Vaughan Springs Quartzite.||12-JUL-16
40018|Southwark Suite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||Yunkanjini Granite.||Undivided granite.|
40018|Southwark Suite|69917|6|Mentioned|p117|||Granites in the western Aileron Province.||||||
40018|Southwark Suite|69937|6|Mentioned|p31|||NW of Alice Springs. Possible source of some zircons in the Cyclops Member of the Pertatataka Formation.|1570-1530 Ma.|||||
40018|Southwark Suite|70554|5|Briefly described|p799,813-814,818|Mesoproterozoic|Mesoproterozoic|Geologial province: Aileron province. Suite of I-type granites with ages of ~1567 Ma (Young et al. 1995) and ~1533 Ma (Cross et al. 2005). Extensively outcrops across the Aileron province. Distribution may reflect thermal anomalies and/or the underlying architecture of the Aileron province during Chewnings extension (c.f. Korsch et al., 2011).|1570-1530 Ma||||Fractionated, moderately reduced to moderately oxidised, I-type biotite granite with moderate to high enrichment in Th, Ce, U and Y.|
40018|Southwark Suite|70839|5|Briefly described|p327|Calymmian|Calymmian|Geological province: Aileron Province. Associated with Chewnings Orogeny.|1.57-1.53 Ma|||||
40018|Southwark Suite|71088|6|Mentioned|p6|||Aileron Province. Partly coeval with the Chewings Orogeny.||||||
40018|Southwark Suite|71169|5|Briefly described|p71|Calymmian|Calymmian|North Australian Craton.|c. 1550 Ma||||Felsic to intermediate volcanics.|
40018|Southwark Suite|71348|6|Mentioned|p201|Calymmian|Calymmian|Geological province: Aileron Province, Arunta Region.||||||
40018|Southwark Suite|71858|5|Briefly described|p2, p69|Calymmian|Calymmian|Aileron Province. Referred to as the Southwark Granite Suite on p69.|ca 1570-1530 Ma|||||
40018|Southwark Suite|72366|5|Briefly described|p7|Orosirian|Orosirian|Geological province: Aileron Province. Represents youngest phase (last of three) of felsic magmatism in the MOUNT DOREEN map sheet. Age reference: Young et al., 1995.|c. 1.57-1.53 Ga||Includes Yarunganyi Granite.|||
40018|Southwark Suite|72376|5|Briefly described|iii,p1,4,9|||Geological province: Aileron Province.|||Includes Yarunganyi Granite.||Granite, leucogranite, pegmatite, aplite.|
22869|Speares Metamorphics|24608|5|Briefly described|p983|||Geological Province: Arunta Block.||||||04-DEC-06
22869|Speares Metamorphics|43225|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
22869|Speares Metamorphics|43503|2|Defined|7, 21, 77|||||||||
22869|Speares Metamorphics|67565|6|Mentioned|p4, pp13-14.|Statherian|Statherian|Of Warren and Shaw (1995). The eastern extent of the Yaya Domain.||Unit in the Yaya Metamorphic Complex.||||
22869|Speares Metamorphics|69428|5|Briefly described|p13:7-9, 16|Paleoproterozoic|Paleoproterozoic|Warren and Shaw (1995), Biermeier et al. (2003). Yaya Domain, Warumpi Province. Outcrops 15 km SE of Papunya, previously assigned to this unit in HERMANNSBURG map area (Warren and Shaw, 1995), are now included in Inyalinga Granulite. Likely to be a combination of Inyalinga Granulite and Alkipi Metamorphics to the east. Electron microprobe monazite and xenotime metamorphic ages of 1139 +/- 25 Ma and 1173 +/- 42 Ma respectively.||Yaya Metamorphic Complex.|||Includes augen gneiss (probably Warumpi Granite), felsic gneiss, mafic granulite and amphibolite, metapelitic rock, quartzic metasedimentary rocks, quartzite and calc-silicate rocks.|12-JUL-16
29406|Spencer Creek Group|22479|5|Briefly described|fig4, pg10|Statherian|Statherian|||||||
29406|Spencer Creek Group|22538|4|Described|Fig4 p710, p715|Statherian||||||||28-MAR-18
29406|Spencer Creek Group|22600|4|Described|Map legend|Statherian|Statherian|||||||
29406|Spencer Creek Group|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
29406|Spencer Creek Group|23374|5|Briefly described|Fig3 p5,6||Paleoproterozoic|In the McArthur Basin.||||||28-MAR-18
29406|Spencer Creek Group|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: 1740-1700Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
29406|Spencer Creek Group|24048|3|Fully described|p23|||||||||
29406|Spencer Creek Group|24049|5|Briefly described|Map Legend|Statherian|Statherian|Includes Rorruwuy Sandstone, Cato Volcanics, Yuduyudu Formation, Gove Sandstone, and Yanungbi Volcanics. Geol. Prov: McArthur Basin.||||||12-OCT-05
29406|Spencer Creek Group|24050|6|Mentioned|p30|||||||||
29406|Spencer Creek Group|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
29406|Spencer Creek Group|44112|1|Redefined|p1,44-45,112||Statherian|Max Age: ~1712 (+/-) 10 Ma. Part of Supersequence 1; igneous units belong to Supersequence 1(D)||||||
29406|Spencer Creek Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin. Creek is Ck is map legend.||||||
29406|Spencer Creek Group|61403|5|Briefly described|Map Legend|Statherian|Statherian|Includes Rorruwuy Sandstone, Cato Volcanics, Yuduyudu Formation, Gove Sandstone, and Yanungbi Volcanics. Geol. Prov: McArthur Basin.||||||
29406|Spencer Creek Group|63866|5|Briefly described|p112, p115, p123|||Northern Caledon Shelf.||||Intruded by the Latram Granite and the Yanungbi Volcanics. Equivalent to the Katherine River Group, Donydji Group and the Tawallah Group.||
29406|Spencer Creek Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4, p355 Fig.5 |||Caledon Shelf North, McArthur Basin.|||Includes the Rorruwuy Sandstone, Cato Volcanics, Yuduyudu Formation, Gove Sandstone, Yanungbi Volcanics, Latram Granite.|||
29406|Spencer Creek Group|65340|6|Mentioned|p7, p9.|||Caledon Shelf, McArthur Basin. Contemporaneous with Tawallah, Katherine River and Donydji Groups.||||||
29406|Spencer Creek Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1711 +/- 11 Ma.|||||
29406|Spencer Creek Group|67779|6|Mentioned|p32.|||Northeastern Arnhem Land. Included by Rawlings (1999) in his Redbank Package, with Katherine River Group, Donji Group, Gadabara Volcanics, Groote Eylandt Group and Tawallah Group.||||||
29406|Spencer Creek Group|69421|5|Briefly described|p6:3|||McArthur Basin.|||Yanungbi Volcanics, Gove Sandstone.|Overlies Bradshaw Complex, and Dhalinybuy Granite unconformably.||12-JUL-16
29406|Spencer Creek Group|69430|5|Briefly described|p15:2-4, 23|Statherian|Statherian|NE McArthur Basin.|>1710 Ma.||Latram Granite; Yanungbi, Cato Volcanics; Gove, Rorruwuy Sandstones.|Is overlain unconformably by Mount Bonner Sandstone.||12-JUL-16
29406|Spencer Creek Group|69673|6|Mentioned|p16 fig 13, p17|Statherian|Statherian|Northeastern McArthur Basin.|1710 Ma||Includes Cato Volcanics, Yuduyudu Formation, Gove Sandstone, Yanungbi Volcanics, Latram Granite|||
29406|Spencer Creek Group|70302|5|Briefly described|iv, p7, p9|Statherian|Statherian|NE McArthur Basin. The 1712 +/- 5 Ma age derived from the Yanungbi Volcanics is interpreted as the minimum age for this group.|||Yanungbi Volcanics.|Unconformably overlies Giddy Suite.||06-FEB-18
29406|Spencer Creek Group|70968|6|Mentioned|p2 Fig.3|||||||||
29406|Spencer Creek Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
29406|Spencer Creek Group|71374|5|Briefly described|p2, p24, p32|||northern McArthur Basin.|||Includes the Rorruwuy Sandstone.|Broadly equivalent to the Tawalah Group.||
29406|Spencer Creek Group|71606|5|Briefly described|p135,137-138|Statherian|Statherian|North Caledon Shelf, McArthur Basin. ||||Overlain unconformably by Nathan Group. Underlain by Arnhem Granites.||
29406|Spencer Creek Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||||Quartzose and lithic sandstone, mudstone; shallow rhyolitic intrusions and volcanics; high-level microgranite plutons.|
29406|Spencer Creek Group|72373|5|Briefly described|p2|Paleoproterozoic|Paleoproterozoic|Of northern McArthur Basin. Broadly equivalent to Goyder Package and Redbank package.||||||
29406|Spencer Creek Group|72377|5|Briefly described|p6,12,15, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Includes Latram Granite, Cato and Yanungbi volcanics, and Rorruwuy Sandstone.|||10-OCT-19
77798|Spinifex Gabbro|69917|4|Described|p101-103, 1|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating. 1796+/-7 Ma is interpreted to be the magmatic crystallisation age of the igneous precursor to the mafic granulite.||||Intrudes metasedimentary rocks correlated with the Bleechmore Metamorphics.|Mafic granulite thought to have meta-quartz gabbro precursor.|
77798|Spinifex Gabbro|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1796+/-7 Ma (U-Pb zircon LA-ICPMS).||||Gabbro.|
79067|Spriggs Gneiss|69917|5|Briefly described|p196-197, 1, p183, 184|Cambrian|Neoproterozoic|Eastern Arunta Region, Irindina Province. Previously included in 'upper Irindina Gneiss'. U/Pb LA-ICPMS zircon dating, Hf analytical data. However, given its stratigraphic location within the Harts Range Metamorphic Complex, the sedimentary protolith of this rock is likely to have been deposited some time during the late Neoproterozoic. The text is contradictory, saying (p196) it is structurally overlain by, but on p197 it is above, the Stanovos Gneiss. U/Pb zircon ICP-MS dating also show metamorphism at 497+/-10 Ma - Larapinta Event.|1701+/-9 Ma max depos|Of Harts Range Metamorphic Complex||Structurally overlain by Stanovos Gneiss (?) and intruded by Riddock Amphibolite. Conformably overlian by Brady Gneiss.|Sillimanite-garnet metapelite, locally migmatitic and with intense foliation.|17-SEP-18
79067|Spriggs Gneiss|71592|5|Briefly described|Appendix A.|||Irindina Province, Arunta Orogen. Metamorphosed at 497 +/- 10 Ma (U-Pb zircon LA-ICPMS).|1701+/-9 Ma (MDA: zircon LA-ICPMS).||||Metapelite.|
42234|Stafford Granite|23809|5|Briefly described|p46|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma.  Geological Province: Arunta Province.||||||07-NOV-08
42234|Stafford Granite|69427|5|Briefly described|p12:19, 21|Statherian|Statherian|Aileron Province. Previously (Stewart, 1981) included in Anmatjira Orthogneiss. Other, similar ages are given, preferred to an earlier determination of 1818 +/- 15 Ma (Collins and Williams, 1995).|1795 +/- 4 Ma (Worden et al., 2008).|||Intrudes Lander Rock Formation.||12-JUL-16
42234|Stafford Granite|69925|6|Mentioned|p39|||Arunta Inlier. Reynolds Range area. Associated with an 1820 Ma intrusive episode with low-P, high-T metamorphism (up to granulite facies), and E-W compressive deformation,.||||||
81268|Stafford Suite|70554|6|Mentioned|p799|Paleoproterozoic|Paleoproterozoic|Geologial province: Aileron province? See also Stafford Event p798.|1815-1795 Ma|||||07-AUG-19
26147|Stairway Sandstone|9814|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Fossiliferous sandstone, silty sandstone.||||||
26147|Stairway Sandstone|12891|5|Briefly described|p733|Middle Ordovician|Middle Ordovocian|Geological province: Amadeus Basin. Similar to the fossiliferous sandstones of Hansons River Beds.||||||07-FEB-11
26147|Stairway Sandstone|13995|5|Briefly described|p69, p73, p75, p79, p90, p101, p103|Middle Ordovician|Middle Ordovician|Amadeus Basin. Brachiopod, rostroconch, pelecypod species. Nautiloids mentioned; contemporary fauna occur in the Coolibah Formation (Georgina Basin). At Mount Watt, this unit has the type locality for Arandaspis prionotolepis and Porophoraspis crenulata, the first record of Ordovician vertebrates (armoured agnathans) in the Southern Hemisphere.||Larapinta Group.||Conformably overlies Horn Valley Siltstone. Is overlain conformably by Stokes Siltstone.|The middle unit of this formation contains phosphorite layers and red beds.|
26147|Stairway Sandstone|22560|4|Described|p5|Late Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22561|6|Mentioned|p23|Neoproterozoic|Neoproterozoic|also see Stairway Formation p9||||||
26147|Stairway Sandstone|22565|5|Briefly described|p71 & Table 1||Ordovician|Thickness at Areyonga Creek measured from surface expression - 250m thick.  Approx. thickness measured from seismic data - 310m.||||||
26147|Stairway Sandstone|22566|5|Briefly described|p85|Ordovician|Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22646|5|Briefly described|p105|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22650|4|Described|p 160|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22651|6|Mentioned|Fig 10 btw p182-183|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22655|5|Briefly described|p 273|||informally divided into upper and lower Stairway Sandstone p253.||||||04-DEC-06
26147|Stairway Sandstone|22656|4|Described|p 278|Early Ordovician|Early Ordovician|||||||
26147|Stairway Sandstone|22758|6|Mentioned|Fig 2 on p305|||Max Age - late Arenig||||||
26147|Stairway Sandstone|22759|6|Mentioned|p318|||Informally divided into upper and lower Stairway Sandstone.||||||04-DEC-06
26147|Stairway Sandstone|22763|6|Mentioned|p400||Early Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22804|6|Mentioned|p452|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|22805|4|Described|p470-471||Ordovician|Shown to be a secondary reservoir p468.  Informally divided into upper and lower Stairway Sandstone p471.||||||04-DEC-06
26147|Stairway Sandstone|22806|4|Described|p485|Ordovician|Ordovician|Informally divided into upper and lower Stairway Sandstone p480.||||||04-DEC-06
26147|Stairway Sandstone|22807|4|Described|p499-503|Ordovician|Ordovician|Parent - Larapinta Group.  The Stairway Sandstone has been divided into upper, middle and lower subunits see p499.||||||04-DEC-06
26147|Stairway Sandstone|22823|6|Mentioned|p512|||||||||
26147|Stairway Sandstone|22824|4|Described|p526 and p530-531|Ordovician|Cambrian|Of the Larapinta Group.  Age range of Llavirnian to Llandelian, corresponding to an absolute age of 478-458 Ma.  see p526.||||||04-DEC-06
26147|Stairway Sandstone|22825|6|Mentioned|p544|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|22826|4|Described|p574|Ordovician|Ordovician|Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|23361|5|Briefly described|16 Fig.4|Cambrian|Cambrian|||||||
26147|Stairway Sandstone|23818|6|Mentioned|p111|||Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24063|5|Briefly described|p220|Ordovician|Cambrian|Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24064|5|Briefly described|p229 Fig.7|Ordovician|Ordovician|Of Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|24301|4|Described|p20|Ordovician|Ordovician|Of Larapinta Group. Originally defined as Stairway Greywacke (Prichard and Quinlan, 1962).  See also Stairway sandstone on p7 Tb.2. Max. thickness: 600m.  Overlies Inindia beds, underlies Stokes Siltstone.  Geological Province: Amadeus Basin.||||||31-MAR-09
26147|Stairway Sandstone|29721|6|Mentioned|Table 44|||||||||
26147|Stairway Sandstone|29972|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|30238|4|Described|p68|||Cambrian - Ordovician age||||||
26147|Stairway Sandstone|30258|6|Mentioned|Fig.2|||Ordovician age. Part of Larapinta Group.||||||
26147|Stairway Sandstone|30540|6|Mentioned|p61|||Reservoir rock of secondary importance||||||
26147|Stairway Sandstone|30544|6|Mentioned|p49|||||||||
26147|Stairway Sandstone|30615|6|Mentioned|p177|||Reservoir rock of secondary importance||||||
26147|Stairway Sandstone|30659|6|Mentioned|p89|||Palaeomagnetism. Middle Ordovician age||||||
26147|Stairway Sandstone|30660|6|Mentioned|Table 1|||Middle Ordovician age||||||
26147|Stairway Sandstone|30661|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|30662|6|Mentioned|p188|||Palaeomagnetic dates||||||
26147|Stairway Sandstone|30983|5|Briefly described|p75|||||||||
26147|Stairway Sandstone|31566|6|Mentioned|p231|||See also Fig. 2||||||
26147|Stairway Sandstone|31567|6|Mentioned|p276|||Overlain unconformably by Polly Conglomerate.||||||04-DEC-06
26147|Stairway Sandstone|31707|4|Described|p53|||Lithology||||||
26147|Stairway Sandstone|32208|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|32209|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
26147|Stairway Sandstone|32854|6|Mentioned|p351|||Stratigraphy p352.||||||04-DEC-06
26147|Stairway Sandstone|33307|6|Mentioned|Fig.6|||||||||
26147|Stairway Sandstone|33625|6|Mentioned|Table 2|||||||||
26147|Stairway Sandstone|33738|6|Mentioned|p52|||||||||
26147|Stairway Sandstone|33761|6|Mentioned|p146|||Ordovician. Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|33832|6|Mentioned|p8|||Stratigraphy||||||
26147|Stairway Sandstone|33971|4|Described|p28|||Of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|34111|5|Briefly described|Table 2|||Cambrian - Ordovician. See also pp4,15,17-19.||||||04-DEC-06
26147|Stairway Sandstone|34280|6|Mentioned|p10|||||||||
26147|Stairway Sandstone|34442|5|Briefly described|Table 1|||Cambrian - Ordovician||||||
26147|Stairway Sandstone|34580|4|Described|Table 1|||Ordovician||||||
26147|Stairway Sandstone|34612|6|Mentioned|p111|||Correlation. Ordovician. Amadeus Basin.||||||
26147|Stairway Sandstone|34722|6|Mentioned|p288|||||||||
26147|Stairway Sandstone|35088|6|Mentioned|Fig.8|||||||||
26147|Stairway Sandstone|35102|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|36096|6|Mentioned|p219|||||||||
26147|Stairway Sandstone|36331|6|Mentioned|p53|||||||||
26147|Stairway Sandstone|36818|6|Mentioned|p203|||||||||
26147|Stairway Sandstone|36821|6|Mentioned|p398|||||||||
26147|Stairway Sandstone|37818|6|Mentioned|Table 2|||||||||
26147|Stairway Sandstone|39213|6|Mentioned|Fig.6|||Amadeus Basin Succession||||||
26147|Stairway Sandstone|40136|5|Briefly described|p39|||See also p18 and p23.||||||04-DEC-06
26147|Stairway Sandstone|40137|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|40740|3|Fully described|p54|||Mention p6.||||||04-DEC-06
26147|Stairway Sandstone|40810|4|Described|p10|||||||||
26147|Stairway Sandstone|40852|6|Mentioned|p34|||||||||
26147|Stairway Sandstone|40910|6|Mentioned|p13|||||||||
26147|Stairway Sandstone|40911|6|Mentioned|Map legend|Ordovician|Ordovician|Prob. Ordovician||||||
26147|Stairway Sandstone|40926|6|Mentioned|p11|||||||||
26147|Stairway Sandstone|41039|4|Described|p6|||Mention p13.||||||04-DEC-06
26147|Stairway Sandstone|41115|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|41190|5|Briefly described|p267|||||||||
26147|Stairway Sandstone|41203|5|Briefly described|p13|||||||||
26147|Stairway Sandstone|41224|6|Mentioned|p428|||||||||
26147|Stairway Sandstone|41270|6|Mentioned|Table 1|||||||||
26147|Stairway Sandstone|41385|6|Mentioned|Fig.2|||||||||
26147|Stairway Sandstone|41621|5|Briefly described|Map legend|Early Ordovician||||||||
26147|Stairway Sandstone|41708|6|Mentioned|p206|||||||||
26147|Stairway Sandstone|41711|6|Mentioned|p259|||||||||
26147|Stairway Sandstone|41717|6|Mentioned|p355|||||||||
26147|Stairway Sandstone|41723|6|Mentioned|Map legend|Ordovician||||||||
26147|Stairway Sandstone|41819|6|Mentioned|Map legend|Early Ordovician||||||||
26147|Stairway Sandstone|41820|3|Fully described|p11|||||||||
26147|Stairway Sandstone|42037|5|Briefly described|Table 3 P79|||||||||
26147|Stairway Sandstone|42049|6|Mentioned|p220|||||||||
26147|Stairway Sandstone|42059|6|Mentioned|p132|||See also Fig.2||||||
26147|Stairway Sandstone|42060|6|Mentioned|Fig.5 P140|||||||||
26147|Stairway Sandstone|42082|4|Described|p323|||See also Fig.3||||||
26147|Stairway Sandstone|42354|6|Mentioned|Fig.3 P5, P6|||||||||
26147|Stairway Sandstone|42504|5|Briefly described|p77|||||||||
26147|Stairway Sandstone|42699|5|Briefly described|map legend|Ordovician||||||||
26147|Stairway Sandstone|42940|5|Briefly described|Plate 8|||||||||
26147|Stairway Sandstone|43035|5|Briefly described|p21|||Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|43105|5|Briefly described|p8|||||||||
26147|Stairway Sandstone|43225|5|Briefly described|Map Legend||Ordovician|Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|43230|6|Mentioned|p9||Ordovician|Reservoir target.||||||
26147|Stairway Sandstone|43503|6|Mentioned|p11-50|Darriwilian|Yapeenian|||||||11-JUL-16
26147|Stairway Sandstone|43646|6|Mentioned|Fig.3,p554||Darriwilian|||||||
26147|Stairway Sandstone|43647|6|Mentioned|p531|||||||||
26147|Stairway Sandstone|43648|6|Mentioned|Fig.1,p488|||||||||
26147|Stairway Sandstone|43649|6|Mentioned|p453||Ordovician|||||||
26147|Stairway Sandstone|43803|6|Mentioned|Fig.5,p71|||||||||
26147|Stairway Sandstone|44133|5|Briefly described|p40, 43, 4 Fig. 7.2|Late Ordovician|Middle Ordovician|Geological Province: Western Warburton Basin. Of the Larapinta Group.||||||
26147|Stairway Sandstone|44323|14|Not recorded|map legend||Ordovician|SG/53-6. Ordovician.||||||
26147|Stairway Sandstone|44342|4|Described|p.6, Table 2||Ordovician|SG/53-5. U-M Ordovician.||||||
26147|Stairway Sandstone|44343|14|Not recorded|map legend||Late Ordovician|U.Ordovician.||||||
26147|Stairway Sandstone|44395|14|Not recorded|p.8,9,10,13, Tb.2||Ordovician|||||||
26147|Stairway Sandstone|44396|5|Briefly described|map legend|||(Camb-Ord). Of Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|44402|5|Briefly described|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||02-DEC-04
26147|Stairway Sandstone|44433|14|Not recorded|map legend|||Cambrian to Ordovician.||||||
26147|Stairway Sandstone|44484|14|Not recorded|p.4,8,11,12,13, Tb.1|||(Camb-Ord).||||||
26147|Stairway Sandstone|44485|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||
26147|Stairway Sandstone|44495|4|Described|p.6, map||Ordovician|AYERS ROCK sheet (G52-8). See p.8,10,11, for details. Middle-Upper Ordovician.||||||04-DEC-06
26147|Stairway Sandstone|44496|5|Briefly described|map legend||Ordovician|White fine sandstone and kaolititic sandstone, minor siltstone.||||||02-DEC-04
26147|Stairway Sandstone|44497|4|Described|p.11, Table 2|Ordovician|Cambrian|SF/53-13. Cambrian-Ord.||||||
26147|Stairway Sandstone|44498|14|Not recorded|map legend|Ordovician|Cambrian|Part of Larapinta Group. Camb-Ord.||||||22-DEC-09
26147|Stairway Sandstone|44505|14|Not recorded|p.5,8,10, Table 1|Ordovician|Cambrian|Of Larapinta Group. Camb-Ord.||||||
26147|Stairway Sandstone|44506|14|Not recorded|map legend|Ordovician|Cambrian|Cambrian to Ordovician.||||||
26147|Stairway Sandstone|45036|2|Defined|p3|Middle Ordovician|Middle Ordovician|See also p4-61||||||04-DEC-06
26147|Stairway Sandstone|45041|4|Described|p71|||See also pp72-78. Middle Ord.||||||04-DEC-06
26147|Stairway Sandstone|45115|6|Mentioned|p7|||||||||
26147|Stairway Sandstone|45118|6|Mentioned|p1,3|||||||||
26147|Stairway Sandstone|45148|6|Mentioned|Fig.4|||See also p18.||||||04-DEC-06
26147|Stairway Sandstone|45155|6|Mentioned|Fig.8|||||||||
26147|Stairway Sandstone|45170|6|Mentioned|p8|||||||||
26147|Stairway Sandstone|46740|14|Not recorded|p.187|||Phosphate.||||||
26147|Stairway Sandstone|46841|6|Mentioned|p106|||||||||
26147|Stairway Sandstone|46928|6|Mentioned|p323|||See also Table 1.||||||
26147|Stairway Sandstone|47050|6|Mentioned|p240|||||||||
26147|Stairway Sandstone|47052|6|Mentioned|p261|||||||||
26147|Stairway Sandstone|48639|4|Described|p.13||Ordovician|See also page, 77,11,13,16. Mising in section in Alice No.1. (G55-2).||||||
26147|Stairway Sandstone|48862|14|Not recorded|p.15||Early Ordovician|On many pages. p.8,15,18,24-28,40,43; opp.8,9; Pl.4,9-11. L.-M.Ord. Supersedes 'Stairway Greywacke'. (F52-15).||||||04-DEC-06
26147|Stairway Sandstone|48863|2|Defined|p.27||Ordovician|Tb.1. opp.p.7,9,10,16,19,20,24,28,29,40-42,Pl.4,5,6,11,13,15,16. Middle Ordovician. (G52-4,G53-1).||||||
26147|Stairway Sandstone|48864|14|Not recorded|p.32, Pl.13|||Now called Stairway Greywacke (?). (G52-8).||||||04-DEC-06
26147|Stairway Sandstone|48865|2|Defined|p.5,10,Fig.23||Ordovician|Many figures. Fig.4,22,15,45,46,49,50,Pl.1,2,7,9,10. Unit of Larapinta Gp. (G52-8,G53-5,6).||||||
26147|Stairway Sandstone|48890|4|Described|p.46||Ordovician|See also Tables, Figs and Plates. of the Larapinta Group.||||||04-DEC-06
26147|Stairway Sandstone|48963|6|Mentioned|p2|||||||||
26147|Stairway Sandstone|50089|5|Briefly described|p430 Fig. 5|Ordovician|Ordovician|Geological Province: Amadeus Basin.||||||04-MAY-05
26147|Stairway Sandstone|50098|5|Briefly described|p1, p3 Fig. 2|||Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|60674|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Thinly bedded, fine to medium clean sandstone; minor minor interbedded sandy limestone, coarse sandstone, medium silty sandstone, phophorite. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61309|5|Briefly described|p16 Fig. 4|||Geological Province: Amadeus Basin.||||||06-FEB-08
26147|Stairway Sandstone|61385|5|Briefly described|Map legend|Ordovician|Ordovician|Sandstone, siltstone, limestone; fossiliferous. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61387|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone, siltstone, limestone; marine fossils. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61518|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Thin bedded fine to medium grained clean sandstone; minor interbedded sandy limestone, coarse sandstone, medium grained silty sandstone, phosporite. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|61519|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Larapinta Group. Sandstone, siltstone, limestone; marine fossils. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|62359|6|Mentioned|p547 Fig. 7|||Geological Province: Amadeus Basin. See also the misspelt(?) Stairways Sandstone. ||||||
26147|Stairway Sandstone|62376|5|Briefly described|p18|Early Ordovician|Early Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
26147|Stairway Sandstone|62379|5|Briefly described|p7 Fig. 2|Ordovician|Ordovician|Of the Larapinta Group. Geological Province: Amadeus Basin.||||||
26147|Stairway Sandstone|62595|6|Mentioned|p28 Fig.4.|Early Ordovician|Early Ordovician|Amadeus Basin. Relative probability plots of detrital zircon data are shown.||||||
26147|Stairway Sandstone|62794|5|Briefly described|p288, 289, 290, p291-292, 299, 336, 337|Early Ordovician|Early Ordovician|Unit in Larapinta Group. Unconformably overlies Horn Valley Siltstone and underlies Stokes Siltstone. Two cliff-forming, resistant sandstone units separated by fine clastics, phosphorites and carbonates. Base of the unit is fossiliferous.||||||
26147|Stairway Sandstone|62795|6|Mentioned|p347, p348|Ordovician|Middle Ordovician|In Amadeus Basin. Basal fauna including Prosopiscus tatei and conodonts are dated as early Darriwilian Stage. This correlates with the middle part of Rowena Formation, Mutawintji Group, western NSW.||||||
26147|Stairway Sandstone|62982|5|Briefly described|p7|Llanvirnian|Llanvirnian|Of the Larapinta Group. Shallow-marine deposits. Overlies Horn Valley Siltstone; overlain by Stokes Siltstone. Geological Province: Amadeus Basin.||||||16-JAN-07
26147|Stairway Sandstone|63562|4|Described|p338 fig 3, p352 fig 10, p353, p347-9|Early Ordovician|Early Ordovician|Of Amadeus Basin. Mixed aged zircons, similar to Pacoota Sandstone and Tomahawk Formation: a third were 0.65-0.5 Ga.||Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.|Well-sorted, fine-grained quartz sandstone with cross beds and ripple marks; abundant body fossils.|
26147|Stairway Sandstone|64068|6|Mentioned|p77, 226|||Of Amadeus Basin. Correlated with Nora Formation, Georgina Basin.||||||
26147|Stairway Sandstone|64334|5|Briefly described|p39-41, 43, 45, 47|Ordovician|Ordovician|Amadeus Basin. Appears as Stairway Siltstone on p39. Reservoir rock.||Larapinta Group.||Unconformably overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.|Shallow-marine sandstone.|
26147|Stairway Sandstone|64778|6|Mentioned|p13, 17, 20-21, 27-28|Ordovician|Ordovician|Amadeus and Pedirka Basins.||||Overlies Horn Valley Siltstone.||
26147|Stairway Sandstone|64809|5|Briefly described|p2, p3 Fig.2, p6 Fig.4, p11 Fig.10|Middle Ordovician|Middle Ordovician|See also p13 Fig.13. Deposition on an open shelf in well-oxygenated waters.||Of the Larapinta Group||||
26147|Stairway Sandstone|65233|3|Fully described|p3 Fig. 2, p10|Early Ordovician|Early Ordovician|Of lower Larapinta Group. Conformable on/gradational with Stairway Sst; gradational below Stokes Siltstone. Max. thickness: 550m decreasing east, west and south. Geological province: Amadeus Basin. Tripartite lithology - details included.||||||07-FEB-11
26147|Stairway Sandstone|65309|6|Mentioned|p14.|Ordovician|Ordovician|Angular clasts occur in Langra Formation.||||||
26147|Stairway Sandstone|65342|6|Mentioned|p3.|||Amadeus Basin. Max. thickness at least 109 m.||||Overlies Horn Valley Siltstone (equivalent). Is overlain by Mereenie Sandstone.||
26147|Stairway Sandstone|65489|5|Briefly described|p125|Ordovician|Ordovician|Amadeus Basin. Hosts the Mereenie Mount Wikter 1 (and others) oil and gas shows.||Unit in Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||
26147|Stairway Sandstone|66623|6|Mentioned|p446.|Ordovician|Ordovician|Amadeus Basin. Contains Darriwilian age Prosopiscus tatei, and Arandaspis sp. impression, both of which occur in upper Rowena Formation, Koonenberry Belt.||||||
26147|Stairway Sandstone|67326|5|Briefly described|p2-4|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||
26147|Stairway Sandstone|67565|5|Briefly described|p41, p50, p51.|Middle Ordovician|Middle Ordovician|Amadeus Basin. Forms prominent ridges. Up to 460 m thick. Contains fossils of the agnathan Porophoraspis, as well as trilobites, nautiloids, pelecypods, fish and ichnofauna. One of the reservoirs in the Mereenie oil/gas field; an abundance of oil-stained core in the Mount Winter-2A well. Contains pelletal phosphate occurrences, but they are too thin and low grade to be economic.|||||Thinly-bedded, fine- to medium-grained clean sandstone with minor interbedded sandy limestone, grey siltstone, coarse sandstone and purple-brown, medium silty sandstone; local phosphorite and phosphatic sandstone.|
26147|Stairway Sandstone|67856|6|Mentioned|p338 fig 4-30|Late Ordovician|Early Ordovician|||Of Larapinta Group.||||
26147|Stairway Sandstone|68297|5|Briefly described|p177|Llanvirn|Arenig|Amadeus Basin. Includes first complete Ordovician vertebrates from Australasia||||||
26147|Stairway Sandstone|68316|6|Mentioned|p778 Fig.1|||||||||
26147|Stairway Sandstone|68323|6|Mentioned|p4 Fig.2|Early Ordovician|Early Ordovician|Amadeus Basin.||Larapinta Group.||||
26147|Stairway 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
26147|Stairway Sandstone|69437|5|Briefly described|p22:10, 15|Ordovician|Ordovician|Amadeus Basin. Has considerable unconventional petroleum potential: tight gas.||||Overlies Horn Valley Siltstone. Is overlain by Stokes Siltstone.||12-JUL-16
26147|Stairway Sandstone|69438|4|Described|p23:2-3, 7, 10, 20, 34-36, 53-57, 59-61|Middle Ordovician|Middle Ordovician|Pritchard and Quinlan (1965). Amadeus Basin. Thickens northwards up to 544m. The bottom unit has basal pyritic ooids and a thin quartz pebble layer at top. Contains abundant fossils (listed). Deposited in a broad E-W oriented epicontinental seaway. Darriwilian to early Gisbornian age. Hosts malachite at the Boggy Hole Cu occurrence, and pelletal phosphate rock at several locations (briefly described). One of the main hydrocarbon reservoirs for the Basin; sealed by thick shales of Stokes Siltstone.||Larapinta Group.||Unconformably/disconformably overlies Horn Valley Siltstone, Winnall beds and Bitter Springs Formation. Is overlain conformably and gradationally by Stokes Siltstone.|Prominent massively bedded quartzic sandstone; overlain by thinly bedded sandstone with local residual phosphatic gravels, thin limestone, black shale and siltstone; quartzic sandstone with interbeds of mudstone, siltstone and phosphorites at top.|12-JUL-16
26147|Stairway Sandstone|69443|6|Mentioned|p28:27|||Amadeus Basin.||||Correlated with Toko Group.||12-JUL-16
26147|Stairway Sandstone|69447|6|Mentioned|p32:5|||Amadeus Basin. Contains fossils with affinities to Hanson River beds (Wiso Basin).||||||12-JUL-16
26147|Stairway Sandstone|69449|6|Mentioned|p34:2 Fig.34.2; 34:4|Ordovician|Ordovician|Eastern Amadeus Basin.||||Probable correlative of Innamincka Formation.||12-JUL-16
26147|Stairway Sandstone|69673|4|Described|p66, p79, p87, p89, p92, p96, p103, |Ordovician|Cambrian |Maximum thickness of 544m. Main reservoir in surprise oil field.||Larapinta Group||disconformably overlies Horn Valley Siltstone, conformably overlain by Stokes Siltstone, Unconformably overlies Pertaoorrta Group|Massively bedded quartzic sandstone and thinly bedded sandstone with minor black shale, siltstone and thin limestone layers.|
26147|Stairway Sandstone|71146|5|Briefly described|p6,  p43 fig 33|Middle Ordovician|Middle Ordovician|Amadeus Basin.||Larapinta Group||Unconformably overlies the Horn Valley Siltstone. Overlain by the Stokes Siltstone.|Sandstone.|
26147|Stairway Sandstone|71171|6|Mentioned|p2, p20|||Amadeus Basin. Coeval with the Goldwyer Formation. ||||||
26147|Stairway Sandstone|71279|5|Briefly described|p355 Fig.2, p365, p370, p374|Early Ordovician|Early Ordovician|Amadeus Basin. Has a K-radiometric high.||Larapinta Group.||||
26147|Stairway Sandstone|71342|6|Mentioned|Ch9 p16, Ch9 p20|||||||Unconformably overlies the Todd River Dolomite. Unconformably overlain by the Mereenie Sandstone.||
26147|Stairway Sandstone|71800|5|Briefly described|p26-p27|Middle Ordovician|Middle Ordovician|Amadeus Basin.||||Uncoformably overlies the Horn Valley Siltstone. Overlain by the Stokes Siltstone.|Quartz sandstone.|
26147|Stairway Sandstone|71898|5|Briefly described|p20|||Amadeus Basin.||||Unconformably overlies the Horn Valley Siltstone.||
26147|Stairway Sandstone|72360|5|Briefly described|Map legend|Ordovician|Ordovician|Of Amadeus Basin.||Unit of Larapinta Group.|||Sandstone, siltstone, limestone; marine fossils.|09-SEP-19
26147|Stairway Sandstone|72369|4|Described|iii,p3-4,29-31|||Of Amadeus Basin. Age constraint by fossils to Darriwilian (467-458 Ma) to early Gisbornian (460-456 Ma; Edgoose 2013 and references therein). Maidment (2005) provided a c. 465 Ma maximum depositional age, based on detrital zircon SHIRMP U-Pn analysis. LA-ICP-MS U-Pb detrital zircon dating of sample HB15ND556 (very fine- to fine-grained sandstone) yielded an interpreted maximum depositional age of 514+\-6 Ma (youngest concordant zircon), but does not further constrain the age of the formation as it is greater than the MDA provided by Maidment (2005). Contains zircons derived from the Musgrave Province (c. 1425-1045 Ma age spectrum). Neoproterozoic to Cambrian age zircon populations (c. 665-506 Ma or the c. 975-565 Ma) are inferred to have been derived from distal or buried sources.||Unit of Larapinta Group.||Overlain conformably by Stokes Siltstone. Underlain disconformably by Horn Valley Siltstone, or unconformably by Pertaoorrta Group.|Variably fossiliferous, commonly quartzic sandstone, with minor siltstone, limestone and phosphatic intervals.|
26147|Stairway Sandstone|73085|4|Described|piii, p1, p3-7, p11|early Ordovician|early Ordovician|Amadeus Basin. 21 m thick in drillhole LA05DD01. Top part of drillhole LA05DD01 are 'red beds' of this unit.||Larapinta Group||Underlain by Horn Valley Siltstone. Overlain by Stokes Siltstone.|Red-brown, fine-grained variably micaceous sandstone and lesser red-brown, finely laminated siltstone.|
26147|Stairway Sandstone|73119|5|Briefly described|piii, p1, p19-21, Appendix|Middle Ordovician (Darriwilian?)|Middle Ordovician (Darriwilian?)|Amadeus Basin, western. Broadly constrained by fossils. Geochron from Edgoose (2013). New SHRIMP U-Pb detrital zircon maximum deposition age of 578 +/- 7 Ma is probably older than the true depositional age; is older than previous age of 514 +/- 6 Ma (Normington et al., 2018). Detrital zircon age components are overwhelmingly dominated by a single Mesoproterozoic population at ca 1180 Ma suggesting that the bulk of detritus was likely derived from the Musgrave Province with negligible input from elsewhere. [See article for provenance discussion].|467-458 Ma|Larapinta Group||Conformably overlain by Stokes Siltstone.|Predominantly sandstone with lesser siltstone and limestone.|
26147|Stairway Sandstone|73279|5|Briefly described|p3, p11-12|Ordovician|Ordovician|Amadeus Basin. Middle part of the Larapinta Group. Detrital zircons analysed for Hf isotopic composition [see article].||Larapinta Group|||Includes sandstone.|
26147|Stairway Sandstone|73346|6|Mentioned|p10, p18-19|Late Ordovician|Early Ordovician|Amadeus Basin. Broadly similar in age to the Cobb Formation. Middle portion contains pelletal phosphorites. Includes the arandaspids Arandaspis prionotolepis, Porophoraspis crenulata, Porophoraspis sp., Arandaspis sp., and Sacabambaspis sp.||||||
37624|Stanley Metamorphics|50623|6|Mentioned|p260|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
37624|Stanley Metamorphics|60677|5|Briefly described|Map Legend|Archean|Archean|Schist, gneiss, banded iron formation and some intrusive granite.||||||07-NOV-08
37624|Stanley Metamorphics|61389|5|Briefly described|Map Legend|||Mostly schists and banded iron formation, some intrusive granite.||||||
37624|Stanley Metamorphics|63866|5|Briefly described|p108, p117|||Central Domain, Pine Creek Orogen. ||||Intercalated with the Rum Jungle and Waterhouse Complexes.||
37624|Stanley Metamorphics|64698|5|Briefly described|lithinterp table|Neoarchean|Neoarchean|Age ~2535-2600Ma. Of Rum Jungle Complex. Mostly schists, some intrusive granite.||||||07-JAN-09
37624|Stanley Metamorphics|64730|6|Mentioned|p124-5 Fig. 3|Neoarchean|Neoarchean|May be correlated with Dirty Water Metamorphics in which case age is between 2675-2545 Ma (Pietsch & Stuart-Smith 1987, Lally 2002).||||||03-MAY-12
37624|Stanley Metamorphics|65232|5|Briefly described|p51|Archean|Archean|Schist and banded ironstone, intruded by various granitic phases of Rum Jungle Complex.||||||09-FEB-10
37624|Stanley Metamorphics|65339|5|Briefly described|pp6-7. |Archean|Archean|Oldest rocks in map area; probably derived from the Woolner Granite to the north. Possible correlative of Dirty Water Metamorphics. Small outcrops, scattered in low-lying topography.|c.2535 - c.2525 Ma.||||Gneiss, metasedimentary schist and banded ironstone; minor granite.|
37624|Stanley Metamorphics|66683|6|Mentioned|p367.|||||Occurs as enclaves in Rum Jungle Complex.|||Metasedimentary mica schist, feldspathic gneiss, and banded iron formation.|
37624|Stanley Metamorphics|67186|5|Briefly described|Map legend.|Neoarchean|Neoarchean||||||Schist, banded ironstone and some intrusive granite.|23-NOV-11
37624|Stanley Metamorphics|67355|5|Briefly described|p6, p8|Neoarchean|Archean|North Australian Craton. Intruded by granite during 2535-2525 Ma. This unit is poorly exposed and little is known about its characteristics. Rhodes (1965) suggested a metamorphic grade of almandine-amphibolite facies.|2675-2535 Ma|||Correlated with the Dirty Water Metamorphics, unconformably overlies the Woolner Granite.|Metasedimentary. Common constituent rock types are biotite gneiss, biotite-muscovite gneiss, biotite granofels, feldspathic gneiss, quartz-muscovite schist and banded ironstone.|25-JAN-17
37624|Stanley Metamorphics|67564|5|Briefly described|p9 Fig.4.|Archean|Archean|Rum Jungle Region, Pine Creek Orogen. Correlative of Dirty Water Metamorphics.|||||Quartz-muscovite schist, biotite-muscovite gneiss, banded ironstone.|
37624|Stanley Metamorphics|67779|6|Mentioned|p6 Fig.5.|Archean|Archean|Central Domain, Pine Creek Orogen.||||||
37624|Stanley Metamorphics|69419|5|Briefly described|p4:4-5,|Archean|Archean|Lally (2002), Ahmad et al. (2006). Oldest known sedimentary rocks within the North Australian Craton.|>2520 Ma.|||Is intruded by Rum Jungle Complex granitic rocks. Is overlain unconformably by Beestons Formation. Correlated with Dirty Water Metamorphics.|Metasedimentary rocks.|12-JUL-16
37624|Stanley Metamorphics|69420|6|Mentioned|p5:4, 6, 8, 75|Archean|Archean|Part of the basement to the Central Domain of the Pine Creek Orogen. ||||||12-JUL-16
37624|Stanley Metamorphics|70866|5|Briefly described|Map legend.|Neoarchean|Neoarchean|Pine Creek Orogen.|||||Schist, gneiss, banded ironstone and some intrusive granite.|
37624|Stanley Metamorphics|71256|5|Briefly described|p18, 20, 21-23|||Deformed and metamorphosed to amphibolite-facies prior to being incorporated into Rum Jungle Complex, and variably retrogressed (Rhodes, 1965; Lally, 2002).|||||Amphibolite-facies metasedimentary rocks; biotite gneiss, biotite-muscovite gneiss, biotite granofels, feldspathic gneiss, quartz-muscovite schist, chlorite schist, actinolite schist, and banded ironstone|
75910|Stanovos Gneiss|62595|4|Described|p4 Table 2, pp12-13, p14, p28 Fig.4.|Early Cambrian|Neoproterozoic|Southeastern Harts Range. Lower unit is possible equivalent of Naringa Gneiss; the upper parts may be approximate correlative of Arumbera Sandstone. Its widespread mafic units and pelitic character suggest deposition in a rift-related sub-basin between Amadeus and Georgina Basins. Mis-spelled as Stanvos Gneiss p.13. Forms line of hills (Indiana Walls) along E side of Stanovos Valley. Relative probability plots of detrital zircon data are shown.|c.545 Ma.|Unit in Harts Range Group.||Structurally underlies Irindina Gneiss and Indiana Walls Granite.|Quartzite, grossular-diopside-wollastonite marble, calc-silicate and minor metapelite; overlain by garnet-poor metapelite with amphibolite, quartzofeldspathic gneiss and quartzite.|28-SEP-12
75910|Stanovos Gneiss|66767|5|Briefly described|p59|Neoproterozoic|Neoproterozoic|Oldest unit in Irindina Province.||||Is overlain by Irindina Gneiss.|Quartzite, marble, calc-silicate rock and biotite-rich and quartzofeldspathic gneiss.|
75910|Stanovos Gneiss|69444|5|Briefly described|p29:5|||Highly inconsistent use; apparently interchangeable with Stanovos Gneiss Member (of Irindina Gneiss): see references (29:1-3, 5). Stanovos Valley, southeastern Harts Range.|||||Includes marble, calc-silicate rocks, quartzite and biotite-rich metapelitic gneiss.|12-JUL-16
75910|Stanovos Gneiss|69917|6|Mentioned|p190-193, 182, 196|||Stanovos Gneiss? - quartzite sampled. Eastern Arunta Region, Irindina Province.  U/Pb LA-ICPMS zircon dating, Hf analytical data. Previously mapped as Irindina Gneiss. May represent a small previously unrecognised sliver of exposed Stanovos Gneiss on the eastern side of the Entia Dome.||Of Harts Range Metamorphic Complex.||Stratigraphically lower  than Yambla Gneiss.||29-JUL-15
75910|Stanovos Gneiss|70094|6|Mentioned|p84, p85 Fig.6|||Is ambiguously presented as a Member of Irindina Gneiss and as a separate Formation. See also references to Stanovos Gneiss Member (p76, 78), Lower Stanovos Gneiss (p80) and Upper Stanovos Gneiss (p76-77, 79-81, 83, 85).||Harts Range Group.||||
75910|Stanovos Gneiss|71592|5|Briefly described|Appendix A.|||Arunta Orogen.|427+/-6 Ma (SHRIMP U-Pb zircon).||||Quartzite.|
75910|Stanovos Gneiss|72524|5|Briefly described|p8-9, p13.|||Has a detrital zircon spectra with age populations between ca 1.90 and 1.35 Ga with a peak at ca 1.58 Ga, age populations between 1.20-1.04 Ga, and zircon rims with an age of 453 +/- 4 Ma (Lower Stanovos Gneiss of Maidment et al 2013).||Harts Range Metamorphic Complex||||27-OCT-20
26914|Strawbridge Breccia|22538|6|Mentioned|Fig3 P708|||||||||
26914|Strawbridge Breccia|22600|4|Described|Map legend|Statherian|Statherian|||||||
26914|Strawbridge Breccia|24048|3|Fully described|p55|Paleoproterozoic|Paleoproterozoic|Of the Balma Group. Overlain by Vaughton Siltstone; underlain by Koolatong Siltstone.  Max. thickness: 100m.  Geological Province: McArthur Basin.||||||07-NOV-08
26914|Strawbridge Breccia|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Chert breccia: relict microbial laminations, stromatolites, intraclastic conglomerates, ooids; locally ferruginous and manganiferous. Geol. Prov: McArthur Basin.||||||13-OCT-05
26914|Strawbridge Breccia|32660|5|Briefly described|Table 4|||||||||
26914|Strawbridge Breccia|42597|5|Briefly described|Map Legend|Carpentarian||||||||
26914|Strawbridge Breccia|43010|2|Defined|p112||Paleoproterozoic|Of the McArthur Group. Of Statherian age.||||||07-NOV-08
26914|Strawbridge Breccia|44112|6|Mentioned|p55|||||||||
26914|Strawbridge Breccia|44299|4|Described|p.12|||SD/53-7,8. Lower(?) Proterozoic. Table 1.||||||
26914|Strawbridge Breccia|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
26914|Strawbridge Breccia|45162|6|Mentioned|p45|||||||||
26914|Strawbridge Breccia|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Chert breccia: relict microbial laminations, stromatolites, intraclastic conglomerates, ooids; locally ferruginous and manganiferous. Geol. Prov: McArthur Basin.||||||
26914|Strawbridge Breccia|64817|6|Mentioned|p353 Fig.4|||||Of the Balma Group.||||
26914|Strawbridge Breccia|67323|4|Described|Eastern Australia Time-Space Plot|||McArthur region.||||||
26914|Strawbridge Breccia|69430|4|Described|p15:3, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. Resistant, ridge-forming unit. Up to 100m thick. Shallow intertidal sediments. Depositional hiatus before burial.||Balma Group.||Overlies Koolatong Siltstone probably conformably (base not seen). Is overlain disconformably by Vaughton Siltstone.|Chert breccia, relict microbial laminations, stromatolites, intraclastic conglomerate, ooids; locally ferruginous and manganiferous.|12-JUL-16
26914|Strawbridge Breccia|69673|6|Mentioned|p16 fig 13|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone||Balma Group||Overlain by Vaughton Siltstone, overlies Koolatong Siltstone||
26914|Strawbridge Breccia|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Lower Balma Group.||||
26914|Strawbridge Breccia|72373|5|Briefly described|p6,9|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.||Unit of Balma Group.||||
25695|Strzeleckie Volcanics|23733|5|Briefly described|p9, p33|Paleoproterozoic|Paleoproterozoic|Age: 1819+/-9Ma.||||||07-NOV-08
25695|Strzeleckie Volcanics|23809|5|Briefly described|p34, p41|Paleoproterozoic|Paleoproterozoic|Welded rhyolite ignimbrite.  Age: 1819+/-9Ma (Pb-Pb).  Possibly overlies Barrow Creek Orthogneiss unconformably, or the volcanics may have intruded the orthogneiss?  Geological Province: Arunta Province.||||||07-NOV-08
25695|Strzeleckie Volcanics|42643|2|Defined|p48||Paleoproterozoic|Of Wauchope Subgroup. Reserved. Defn card avail. NOT variation on Strzelecki Formation, Vic.||||||07-NOV-08
25695|Strzeleckie Volcanics|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Tuff, tuffaceous siltstone and arenite, porphyritic dacite-rhyolite, quartz arenite.||||||07-NOV-08
25695|Strzeleckie Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Lower Wauchope Subgroup (Hatches Creek Gp). Dacitic and rhyolitic ignimbrite, lava and tuff; minor feldspathic/lithic/volcaniclastic/tuffaceous arenite and siltstone.  Overlies Gwynne Sst and interfingers with Tinfish Sst. In Tennant Creek region.||||||07-NOV-08
25695|Strzeleckie Volcanics|64735|4|Described|p206 Fig 2, p206, p207, p216 Fig15,|Orosirian|Orosirian|Discussion of U-Pb age of 1819+/-11 Ma (Smith 2001), and 1805+6/-3 Ma  crystallisation age using SHRIMP RG 207Pb/206Pb on zircons from a partly welded dacitic ignimbrite (this publication); Barrow Creek area, Aileron Province. An extensive volcanic sheet. Proposed to correlate with higher part of Hatches Creek Group than suggested by Haines et al (1991); correlated with Ongeva Package, Ware Group.|1805 +6 / -3 Ma crystallisation age.|||Interpreted to stratigraphically overlie Bullion Schist.|Felsic volcanics.|30-APR-12
25695|Strzeleckie Volcanics|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|In text (p37, p38) misspelt as Strzelecki Volcanics. Encompassed by informal Lower Wauchope Subgroup.||Wauchope Subgroup||||05-JAN-17
25695|Strzeleckie Volcanics|65338|5|Briefly described|p19.|Statherian|Orosirian|Stratigraphic equivalent of Newlands Volcanics.|1805 +6/-3 Ma (Claoue-Long et al. 2008b).|Unit in Wauchope Subgroup.||||
25695|Strzeleckie Volcanics|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Shown as overlying Gwynne Sandstone, and lateral equivalent of Tinfish Sandstone. Shown as disconformably overlain by Illoquara Sandstone.|Dacitic and rhyolitic ignimbrite, lava and tuff; minor feldspathic/lithic, volcaniclastic/tuffaceous arenite and siltstone.|08-DEC-14
25695|Strzeleckie Volcanics|69424|5|Briefly described|p9:5|Paleoproterozoic|Paleoproterozoic|Volcanic rocks are part of the Treasure Suite. Mis-spelt as Strzelecki on p9:5.|1805 +6/-3 Ma.|Hatches Creek Group.||||12-JUL-16
25695|Strzeleckie Volcanics|69425|3|Fully described|p10:3, 10-11, 13, 15-16|Statherian|Statherian|Part of the Treasure Suite. Osborne and Crawford Ranges. Type section is at the NW end of the Osborne Range in BARROW CREEK map area. Thickness from 500m, to 1700m at the type section. Volcanics sourced from a volcanic centre probably in the NW Osborne Range. Lithostratigraphic correlation with Arabulja and Newlands Volcanics may conflict with their various ages; these units may be older than the Strzeleckie Volcanics. An age determination by Smith (2000) gave 1819 +/- 11 Ma but distribution was markedly skewed and the median was 1821 +14/-23 Ma.|1805 +6/-3 Ma (Claoue-Long et al., 2008).|Wauchope Subgroup, lower.||Conformably overlies Gwynne Sandstone. Is overlain conformably by (and partly interfingers with) Tinfish Sandstone, and disconformably by Illoquara Sandstone.|Dacitic to rhyolitic ignimbrite, lava and tuff; minor feldsdpathic/lithic/volcaniclastic/tuffaceous sandstone and siltstone.|12-JUL-16
25695|Strzeleckie Volcanics|69427|4|Described|p12:13|Orosirian|Orosirian|Now includes felsic volcanic rocks, 12km NW of Barrow Creek roadhouse, originally mapped as Bullion Schist by Haines et al. (1991). SHRIMP U-Pb zircon age.|1807 +/- 3 Ma (Claoue-Long et al., 2008).|Wauchope Subgroup.||Conformably overlies Gwynne Sandstone. Is overlain conformably by, and interdigitates with, Tinfish Sandstone. Correlated with Newlands Volcanics.|Porphyritic lava and ignimbrite, tuff, tuffaceous siltstone and sandstone.|12-JUL-16
25695|Strzeleckie Volcanics|69431|6|Mentioned|p16:5|||Osborne and Crawford Ranges.||Wauchope Subgroup.||||12-JUL-16
25695|Strzeleckie Volcanics|72378|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. SHRIMP 207Pb/206Pb zircon crystallisation age of 1805+\-6 Ma (Claoue-Long et al., 2008b).|1805+\-6 Ma (207Pb/206Pb)|||Underlain conformably by Bullion Schist.|Metarhyolitic ignimbrite.|
25695|Strzeleckie Volcanics|73128|6|Mentioned|p13|Orosirian|Orosirian||1819 +/- 9 Ma SHRIMP U-Pb|Hatches Creek Group||||
22910|Stuart Pass Dolerite|22524|6|Mentioned|p38|Stenian|Stenian|||||||
22910|Stuart Pass Dolerite|43225|5|Briefly described|Map Legend||Mesoproterozoic|In the Arunta Block.||||||05-DEC-06
22910|Stuart Pass Dolerite|43503|2|Defined|9,27,80|||Sm-Nd Age: 1080 Ma.||||||03-DEC-15
22910|Stuart Pass Dolerite|44194|6|Mentioned|p5|||Age 1076+/-33 Ma Sm-Nd.||||||05-DEC-06
22910|Stuart Pass Dolerite|50246|5|Briefly described|p8|Mesoproterozoic|Mesoproterozoic|Unconformably overlain by Heavitree Quartzite. Age: 1080Ma.||||||07-FEB-11
22910|Stuart Pass Dolerite|60674|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Age: <1080Ma.  Geological Province: Amadeus Basin.||||||
22910|Stuart Pass Dolerite|61154|5|Briefly described|p42 Appendix|Mesoproterozoic|Mesoproterozoic|Age: 1076+/-33Ma (Sm-Nd: Zhao and McCulloch 1993).  Of the southern Arunta region.  Correlates with Alcurra Dolerite.  See also p34.||||||
22910|Stuart Pass Dolerite|61518|5|Briefly described|Map Legend|Neoproterozoic|Mesoproterozoic|Geological Province: Amadeus Basin.||||||
22910|Stuart Pass Dolerite|62595|5|Briefly described|p8. |Stenian|Stenian||1080 Ma (Zhao and McCulloch 1993).|||Is unconformably overlain by Heavitree Quartzite.||
22910|Stuart Pass Dolerite|62986|6|Mentioned|p18|||North of the Amadeus Basin in central Australia.||||||22-DEC-08
22910|Stuart Pass Dolerite|64572|6|Mentioned|p810 Fig. 10|Neoproterozoic|Neoproterozoic|Age: ca. 1076MA (Sm-Nd).||||||22-DEC-08
22910|Stuart Pass Dolerite|65135|6|Mentioned|p17|Stenian|Stenian|~1070 Ma.||||||
22910|Stuart Pass Dolerite|65256|6|Mentioned|p8, p26|Stenian|Stenian|Intrudes Arunta basement but not basal sediments; age of 1083+/-23 Ma.||||||
22910|Stuart Pass Dolerite|65693|6|Mentioned|p4.||||1076 +/- 33 Ma (Zhao & McCulloch 1993).|||||
22910|Stuart Pass Dolerite|65833|6|Mentioned|p17|Stenian|Stenian|||||||
22910|Stuart Pass Dolerite|65906|6|Mentioned|p7|Mesoproterozoic|Mesoproterozoic|~1070 Ma.||||||
22910|Stuart Pass Dolerite|66256|6|Mentioned|p17 Fig.13|||Arunta Orogen. In Warakurna LIP.||||||
22910|Stuart Pass Dolerite|67375|5|Briefly described|p14 Fig.9, p36. |Mesoproterozoic|Mesoproterozoic|Part of the Warakurna Large Igneous Province.|c.1070 Ma.|||||
22910|Stuart Pass Dolerite|67553|6|Mentioned|p15,37-38|||Of Amadeus Basin, part of the Warakurna Large Igneous Province. Geochemically similar to the Alcurra Dolerite. Intrudes into Pitjantjatjara Supersuite, with mylonitic contacts.||||||
22910|Stuart Pass Dolerite|67565|4|Described|p6 Table 1, p10, pp24-25, pp33-34.|Mesoproterozoic|Mesoproterozoic|Warumpi Province. Produces distinctive ENE-trending linear magnetic anomalies. Has geochemical affinity with dykes dated (Sm-Nd isochron) at 1076 +/- 33 Ma (Zhao and McCulloch 1993a,b), as well as with the Dashwood Gabbro. Geochemistry is discussed briefly.|1080 Ma.|||Intrudes Udor Granite, Peculiar Complex, Putardi Quartzite and Ikuntji Metamorphics. Is overlain by Heavitree Quartzite.|Fine- to medium-grained dolerite, olivine dolerite, dykes; generally undeformed; most commonly has an intergranular to subophitic texture.|
22910|Stuart Pass Dolerite|68832|5|Briefly described|p32|||||||Truncates (intrudes) Putardi Quartzite.||
22910|Stuart Pass Dolerite|69003|5|Briefly described|p48 Fig.57, p50 Fig.59|Mesoproterozoic|Mesoproterozoic|Included as a contributing unit to Australia's Apparent Polar Wander Path through the Proterozoic.|c.1075 Ma.|||||
22910|Stuart Pass Dolerite|69031|5|Briefly described|p8|Stenian|Stenian||1076 +/- 33 Ma (Sm-Nd: Zhao and McCulloch, 1993).||||Dolerite dykes.|
22910|Stuart Pass Dolerite|69427|4|Described|p12:46|Mesoproterozoic|Mesoproterozoic|Warren and Shaw (1995). Formerly the Stuart Dyke Swarm (Zhao and McCulloch, 1993). A dyke swarm in the vicinity of Alice Springs in Aileron Province, but most extensive in Warumpi Province. Sm-Nd mineral isochron age.|1076 +/- 33 Ma (Zhao and McCulloch, 1993).|||Is correlated with Alcurra Dolerite (Musgrave Province).|Dykes mainly oriented N-S, ranging in width 1-50m, and containing cumulus olivine and are dominantly olivine-normative, high-Mg tholeiites with a geochemical signature similar to island-arc basalts in subduction regimes.|12-JUL-16
22910|Stuart Pass Dolerite|69428|4|Described|p13:11, 16|Mesoproterozoic|Mesoproterozoic|Warren and Shaw (1995); formerly the Stuart Dyke Swarm (Zhao and McCulloch, 1993). Extensive swarm of dykes in the eastern Warumpi Province. Individual dykes vary from 1-50m wide; mostly oriented N-S. Have a geochemical signature similar to island-arc basalts from subduction regimes. Sm-Nd mineral isochron age.|1076 +/- 33 Ma (Zhao and McCulloch, 1993).|||Intrudes the Belt Granite. Correlated with Alcurra Dolerite.|Numerous dykes containing cumulus olivine and are dominantly olivine-normative, high-Mg tholeiites.|12-JUL-16
22910|Stuart Pass Dolerite|69437|6|Mentioned|p22:11|||Associated with the c.1070 Ma Warakurna Large Igneous Province. Emplaced within the southern Arunta Region.||||||12-JUL-16
22910|Stuart Pass Dolerite|69438|6|Mentioned|p23:9|||Intrudes basement rocks of the Musgrave Province.||||||12-JUL-16
22910|Stuart Pass Dolerite|73551|6|Mentioned|p1, p23|Stenian|Stenian|Aileron Province, southern.|ca 1.08 Ga|||||
74207|Sunbird Formation|61542|4|Described|p276, p277 Fig. 2, p285-6||Visean|Top unit of Weaber Group - forms part of revision by authors.Unconformably overlies Sandbar Sandstone and Tanmurra Fm. Geol. Province: Bonapart Basin/Petrel-Sub-basin. Detailed lithology included. type section described. 638-725 m in Bonaparte-1, onshore WA. Reference section in Sunbird-1, offshore NT.||||Unconformable on Tanmurra Fm. Nature of contact with underlying Sandbar Sst unknown.||26-NOV-18
74207|Sunbird Formation|67354|5|Briefly described|p73. |||||Unit in Weaber Group.||Is overlain by Wadeye Sub-Group.||
74207|Sunbird Formation|69452|5|Briefly described|p36:12, 14-15, 17|Carboniferous|Carboniferous|||Weaber Group.||Unconformably overlies Sandbar Sandstone and Tanmurra Formation.||12-JUL-16
74207|Sunbird Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||
74207|Sunbird Formation|69673|6|Mentioned|p168 fig 138, p171|Carboniferous|Carboniferous|||Weaber Group||||
74207|Sunbird Formation|70061|5|Briefly described|Petrel Sub-basin Fig.3|Serpukhovian|Visean|See also Regional geology: Fig.8.||Weaber Group.||Overlies Sandbar Sandstone. Is overlain by Arco Formation (Wadeye Group).||12-JUL-16
74207|Sunbird Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Tanmurra Formation. Equivalent to Sandbar Sandstone.||
33808|Supplejack Dolostone Member|24122|3|Fully described|p6, p5 Tb.1|Proterozoic|Proterozoic|Of Skull Creek Formation. Supersedes Supplejack Dolomite Member. Conformable within Skull Creek Formation.  Maximum thickness: 50m.  Geological Province: Victoria Basin.||||||
33808|Supplejack Dolostone Member|24297|3|Fully described|p10|Proterozoic|Proterozoic|Of Skull Creek Formation.  Formerly Supplejack Dolomite Member (Sweet et al, 1974 c).  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||
33808|Supplejack Dolostone Member|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Microbial dolostone and dolarenite.||||||05-DEC-06
33808|Supplejack Dolostone Member|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Skull Creek Formation.   Geological Province: Victoria Basin||||||05-DEC-06
33808|Supplejack Dolostone Member|24441|5|Briefly described|p2 Fig. 2, p7|Mesoproterozoic|Mesoproterozoic|Of Skull Creek Formation (Bullita Group). Conformable thickly bedded dolostone. Max. thickness: 28m. Geological Provicne: Victoria Basin.||||||08-AUG-05
33808|Supplejack Dolostone Member|60006|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin. Of Skull Creek Formation. Microbial dolostone, dolarenite||||||
33808|Supplejack Dolostone Member|60682|4|Described|p8|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Formerly Supplejack Dolomite Member. Dark, poorly bedded, microbial dolostone and dolarenite. Thickness: 1-20m. Geological Province: Victoria Basin.||||||
33808|Supplejack Dolostone Member|60685|4|Described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Retained as a member of Skull Creek Formation. Thickly to massively bedded stromatolitic dolostone containing biotherms. Conformably within Skull Creek Formation. Max. Thickness: 28m. Geological Province: Victoria Basin.||||||
33808|Supplejack Dolostone Member|65331|5|Briefly described|Map legend|Mesoproterozic|Mesoproterozic|Of Skull Creek Formation, Bullita Group, Victoria Basin.  Microbial dolostone, dolarenite||||||
33808|Supplejack Dolostone Member|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Skull Creek Formation.|||Dolostone, stromatolitic, especially at top; dolomitic sandstone.|
33808|Supplejack Dolostone Member|69432|5|Briefly described|p17:10-11, 13|||Birrindudu Basin. Up to 30m thick. Occurs within the top 60m of the parent Formation. The upper and lower contacts are regionally anomalous in base metals, esp. Pb, but drilling has found no significant mineralisation.||Skull Creek Formation.|||Distinctive dark grey recrystallised biohermal and biostromal dolostone, interbedded with dolarenite and dolorudite.|12-JUL-16
33808|Supplejack Dolostone Member|70206|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Birindudu Basin [misspelling of Birrindudu Basin].||Skull Creek Formation|||Microbial dolostone and dolarenite.|18-JUL-16
33808|Supplejack Dolostone Member|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Skull Creek Formation.|||Dolostone, stromatolitic, especially at top; dolomitic sandstone.|
33808|Supplejack Dolostone Member|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Skull Creek Formation.|||Microbial dolostone and dolarenite.|
33808|Supplejack Dolostone Member|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Skull Creek Formation.|||Microbial dolostone and dolarenite.|
27664|Sweets Member|22810|4|Described|Table3 p8, p15||Proterozoic|Member of Welltree Metamorphics||||||18-SEP-18
27664|Sweets Member|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Part of the Welltree Metamorphics. Para-amphibolite, biotite gneiss.||||||07-NOV-08
27664|Sweets Member|23714|5|Briefly described|p9|||Of Welltree Metamorphics.||||||
27664|Sweets Member|23715|5|Briefly described|Map legend||Proterozoic|Of the Welltree Metamorphics. In the Litchfield Province.||||||05-DEC-06
27664|Sweets Member|23733|5|Briefly described|p32 Fig. 19|||||||||
27664|Sweets Member|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27664|Sweets Member|39803|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27664|Sweets Member|40493|5|Briefly described|Table 1|||||||||
27664|Sweets Member|40495|4|Described|p9|||||||||
27664|Sweets Member|40808|3|Fully described|p15|||||||||
27664|Sweets Member|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27664|Sweets Member|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27664|Sweets Member|41305|4|Described|p18|||||||||
27664|Sweets Member|41980|5|Briefly described|Table 2 p569|||||||||18-SEP-18
27664|Sweets Member|43187|5|Briefly described|p2|||||||||
27664|Sweets Member|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~1860-2500Ma. Welltree Metamorphics. Max thick 600m. Marble in places graphitic, para-amphibolite, calc-silicate gneiss, quartz-feldspar-biotite gneiss.||||||07-JAN-09
27664|Sweets Member|64731|5|Briefly described|p150|Paleoproterozoic|Paleoproterozoic|500m thick.||Of Welltree Metamorphics.|||Marble (locally graphitic), calc-silicate and amphibolite.|12-APR-12
27664|Sweets Member|69420|5|Briefly described|p5:27, 117|Paleoproterozoic|Paleoproterozoic|NE Litchfield Domain, Pine Creek Orogen. Poorly exposed. Hosts minor graphite occurrences.||Welltree Metamorphics.|||Marble, calc-silicate rocks, para-amphibolite and quartzofeldspathic gneiss.|12-JUL-16
27664|Sweets Member|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Welltree Metamorphics.|||Marble, in places graphitic, para-amphibolite, calc-silicate gneiss, quartz feldspar-biotite gneiss.|
38412|Sweetwater Member|23937|6|Mentioned|p83 App. 1|||Of the Baralandji Formation (Renner Group).||||||
38412|Sweetwater Member|24303|2|Defined|p28, p60 Appendix|Calymmian|Calymmian|Of the Baralandji Formation. Overlain by the Grayling Member;  overlies the Gleeson Formation. Max. Thickness: 200m. Previously mapped as undifferentiated Tomkinson Creek beds. Correlative of Mantungula Fm. and Limmen Sandstone.||||||18-OCT-05
38412|Sweetwater Member|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Baralandji Formation.  Sandstone; laminated to very thick bedded, medium to coarse grained; micaceous, crossbedded, current lineated, rippled, dessicated, halite pseudomorphs, gutter casts; conglomerate; graded, megarippled.......||||||18-OCT-05
38412|Sweetwater Member|69431|4|Described|p16:19-20|Mesoproterozoic|Mesoproterozoic|Tomkinson Province. Up to 225m thick. Deposited below fair-weather wave base and above storm wave base on a marine shelf. Sedimentary structures, including megaripples and cross-beds, are listed.||Baralandji Formation.||Gradationally overlies Gleeson Formation. Is overlain conformably by Grayling Member.|Variably micaceous fine-grained sandstone and green-grey shale overlain by quartz sandstone and progressively more lithic sandstone in coarsening-upward succession; granule- and pebble-bearing sandstone and conglomerate intervals.|12-JUL-16
38412|Sweetwater Member|70968|2|Defined|p93-95,p98-102,p126,p131,p139-140,p143|Calymmian|Calymmian|Hussey and Crispe in Hussey et al. (2001). Named after Sweetwater Bore. The complicated type section (described) goes from 361000mE 7992700mN (base) to 363000mE 7989900mN in HELEN 100k sheet: 225m thick. A reference section is also given. Lithology is well described and illustrated. 50-300m thick.||Baralandji Formation.||Conformably overlies Gleeson Formation. Is overlain conformably by Grayling Member, and unconformably by Helen Springs Volcanics.|A coarsening- and thickening-upward succession, comprising a lower interval of variably micaceous, fine-grained sandstone and minor interbedded mudrocks, overlain by a succession of quartz to sublithic sandstone.|
38412|Sweetwater Member|71893|4|Described|p6, p8, p56|Ectasian|Statherian|Tomkinson province. This unit is interpreted to range from Statherian to Ectasian on the basis of dating of the unconformably underlying Namerinni Group and a SHRIMP U-Pb date of 1295 +/- 14 Ma for an unnamed dyke which intrudes this unit.||Baralandji Formation||Conformably overlain by the Grayling Member.||
27578|Tabletop Granite|23714|4|Described|p32|||See also page 20 Table 4. Previously mapped as part of Cullen Granite. Geological Province: Cullen Batholith.||||||
27578|Tabletop Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly I-type. In the Cullen Batholith, of the Rum Jungle and Central Regions.||||||
27578|Tabletop Granite|24197|5|Briefly described|p24, p106 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Cullen Supersuite. One of a group of concentrically zoned transitional granite and leucogranite dominated plutons. Age: ~1825Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
27578|Tabletop Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27578|Tabletop Granite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Cullen Batholith. Granite, leucogranite.||||||07-NOV-08
27578|Tabletop Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27578|Tabletop Granite|41874|6|Mentioned|p14|||||||||
27578|Tabletop Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27578|Tabletop Granite|43140|3|Fully described|p49|||Of the Cullen Batholith. Mapped as part of Cullen Granite by Walpole et al (1968). and earlier workers.||||||27-APR-11
27578|Tabletop Granite|43624|6|Mentioned|p13|||Geological Province: Cullen Batholith.||||||
27578|Tabletop Granite|43832|3|Fully described|39,40,46,50,62||Paleoproterozoic|||||||07-NOV-08
27578|Tabletop 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
27578|Tabletop Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Coarse porphyritic hornblende-biotite granite, medium/coarse equigranular biotite granite, fine/medium equigranular leucogranite. Intrudes Burrell Creek Formation.||||||07-JAN-09
27578|Tabletop Granite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
27578|Tabletop Granite|69420|5|Briefly described|p5:17-18, 20-23|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Concentrically zoned transitional granites and leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Pluton has three phases, younging inwards. Spatially related to Au or base metals mineralisation.||Shoobridge Suite.|||Coarse-grained porphyritic granite and leucogranite, fine equigranular granite. I-type.|12-JUL-16
27578|Tabletop Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Shoobridge Suite.|||Pink to rare green, coarse-grained, porphyritic hornblende-biotite granite; medium- to coarse-grained equigranular biotite granite; fine- to medium-grained equigranular leucogranite.|
42239|Talbot South Monzogranite|23809|5|Briefly described|p25, p6 Tb. 3|Paleoproterozoic|Paleoproterozoic|Age: 1812+/-5Ma.||||||07-NOV-08
42239|Talbot South Monzogranite|62580|5|Briefly described|p26|Paleoproterozoic|Paleoproterozoic|Of the Coomarie Suite. Several irregularly shaped plutonic bodies cut by numerous faults. Pink, medium- to coarse-grained equigranular biotite monzogranite that has been pervasively sericitized to depths of 100m.||||||07-FEB-11
42239|Talbot South Monzogranite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1812+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Monzogranite.|
37706|Talipata Granite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Madderns Yard Metamorphic Complex.  Coarse-grained foliated porphyiritc biotite granite with flattened K-feldspar phenocrysts.  Age: 1683Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
37706|Talipata Granite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Coarse grained foliated porphyritic biotite granite with flattened K feldspar phenocrysts, highly magnetic. Of the Madderns Yard Metamorphic Complex. Age: 1683Ma. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
37706|Talipata Granite|67565|2|Defined|p57-58, p9-10, p13, p31, p34.|Statherian|Statherian|New unit. Haasts Bluff Domain, Warumpi Province. Named after Talipata Gorge. Previously included within undifferentiated gneiss, granite and other lithologies in the Arunta Complex (Ranford, 1969). Type locality 10 km west of Berry Pass. High magnetic and U, K and Th radiometric responses. Geochemistry is discussed briefly. Age from Cross et al. (2004).|1683 +/- 2 Ma SHRIMP U-Pb zircon.|||Is faulted against Peculiar Complex. Is unconformably overlain by Heavitree Quartzite.|Foliated coarse-grained porphyritic biotite and biotite-hornblende granite; K-feldspar phenocrysts typically 1-2 cm diameter, flattened and elongated; pervasive greenschist facies retrogression.|01-DEC-15
37706|Talipata Granite|68832|5|Briefly described|p4-7|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Crystallisation age.|1683+/-2 Ma|||Adjacent to Lizard Schist. Possibly intrudes it.|Coarse-grained biotite and biotite-hornblende granite.|
37706|Talipata Granite|69417|5|Briefly described|p2:5|Statherian|Statherian|Haasts Bluff Domain, Warumpi Province.||||Intrudes Madderns Yard Metamorphic Complex.||12-JUL-16
37706|Talipata Granite|69428|5|Briefly described|p13:3-4|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Haasts Bluff Domain, Warumpi Province. Crops out in the valley between Berry Pass and Mount Palmer. SHRIMP U-Pb zircon age.|1683 +/- 2 Ma (Cross et al. 2005).||||Coarse-grained, K-feldspar-porphyritic biotite and biotite-hornblende granite.|12-JUL-16
37706|Talipata Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1683+/-2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
41852|Talyi-Talyi Charnockite|67565|2|Defined|p62-63,p6 Table 1, p20, p28, p34, p50.|Statherian|Statherian|New name, after Talyi-Talyi Hills; type locality is a hill 3 km SSW of there. Yaya Domain, Warumpi Province. Previously included in undifferentiated Arunta Complex (Ranford, 1969). Geochemically indistinguishable from Tjungkuba Granodiorite. Correlated with Russell Charnockite. Age by Cross et al. (2004). Metamorphism occurred within error of the age of crystallisation. Stream sediment anomalies suggest it may have economic potential.|1631 +/- 4 Ma (SHRIMP U-Pb zircon).|Unit in Waluwiya Suite.||Is faulted against Yaya Metamorphic Complex.|Medium-grained, weakly porphyritic, foliated charnockite with blue-grey plagioclase phenocrysts to 8 mm diameter, metamorphic garnet and hornblende.|01-DEC-15
41852|Talyi-Talyi Charnockite|68832|4|Described|p12-14|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Crystallisation age.|1631+/-4 Ma|Of Waluwiya Suite.|||Medium grained and weakly porphyritic charnockite.|
41852|Talyi-Talyi Charnockite|69428|5|Briefly described|p13:10|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province. Crops out in the Talyi-Talyi Hills N of Mount Liebig. Geochemically very similar to Tjungkuba Granodiorite. SHRIMP U-Pb zircon age.|1631 +/- 4 Ma (Cross et al., 2005).|Waluwiya Suite.|||Medium-grained and weakly porphyritic charnockite, with blue-grey plagioclase phenocrysts to 8mm diameter.|12-JUL-16
24513|Taragan Sandstone|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgroup (Hatches Creek Group).||||||07-NOV-08
24513|Taragan Sandstone|23733|5|Briefly described|p9, p33|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group.  See also Taragon Sandstone.||||||07-NOV-08
24513|Taragan Sandstone|39624|5|Briefly described|Table 1|||||||||
24513|Taragan Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24513|Taragan Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Quartz arenite and feldspathic arenite; minor conglomerate, felsic lava.||||||10-JAN-05
24513|Taragan Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24513|Taragan Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24513|Taragan Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Quartz arenite; feldspathic arenite, commonly pebbly; minor conglomerate; siltstone; mudstone; friable arenite; calcareous beds and felsic lava. Geological Province: Tennant Creek Block.||||||07-NOV-08
24513|Taragan Sandstone|41129|4|Described|Table 1|||||||||
24513|Taragan Sandstone|41204|4|Described|Table 1|||Mention p10.||||||11-DEC-06
24513|Taragan Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup. Lithic/feldspathic/pebbly arenite, conglomerate, siltstone.||||||16-NOV-05
24513|Taragan Sandstone|41308|5|Briefly described|Table 2|||||||||
24513|Taragan Sandstone|41310|4|Described|Table 1|||See also p11.||||||11-DEC-06
24513|Taragan Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24513|Taragan Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24513|Taragan Sandstone|42643|4|Described|p11, Table 1 p9|||||||||
24513|Taragan Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Quartzose and feldspathic/lithic arenite, pebbly, grading into conglomerate; minor felsic lava and micaceous siltstone.||||||07-NOV-08
24513|Taragan Sandstone|43223|5|Briefly described|Map Legend||Proterozoic|Of Ooradidgee Subgroup.||||||11-DEC-06
24513|Taragan Sandstone|43224|5|Briefly described|Map legend||Proterozoic|Of Ooradidgee Subgroup.||||||11-DEC-06
24513|Taragan Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
24513|Taragan Sandstone|45167|3|Fully described|Table 1|||Of Ooradidgee Subgroup.||||||11-DEC-06
24513|Taragan Sandstone|49033|2|Defined|p12|Proterozoic|Proterozoic|||||||
24513|Taragan Sandstone|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||
24513|Taragan Sandstone|50588|5|Briefly described|p3.4, 4.4|||Geological Province: Tennant Creek/Davenport Province. Intruded by: Treasure Suite, Devils Suite.||||||
24513|Taragan Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group.  Feldspathic/sublithic arenite, quartz arenite, pebble arenite, conglomerate; minor siltstone, mudstone and altered felsic lava.  In the Tennant Creek region.||||||07-NOV-08
24513|Taragan Sandstone|61567|5|Briefly described|p632, p633 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Subgroup (Hatches Creek Group). Overlies Kurinelli Sandstone. Max. thickness: 100m. Geol.Prov: Tennant Creek Inlier.||||||07-NOV-08
24513|Taragan Sandstone|64735|5|Briefly described|p210|Orosirian|Orosirian|Intruded by dolerite sills.||Of Ooradidgee Group.||||30-APR-12
24513|Taragan Sandstone|65209|6|Mentioned|p35 Fig.1, p37|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||||
24513|Taragan Sandstone|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.||||
24513|Taragan Sandstone|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Ooradidgee Group.||Overlies Kurinelli Sandstone. Is overlain by Mia Mia and Treasure Volcanics.|Quartz arenite; feldspathic arenite, commonly pebbly; minor conglomerate; siltstone; mudstone; friable arenite; calcareous beds and felsic lava.|
24513|Taragan Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Feldspathic/sublithic arenite, quartz arenite, pebbly arenite, conglomerate; minor siltstone, mudstone and altered felsic lava.|
24513|Taragan Sandstone|67352|4|Described|p3, p8, p10 Tb.1, p44 fig 48, p54, p56.|Orosirian|Orosirian|Over 1000 m thick. Forms high, dissected plateaux. Quartz veins contain W and Cu minerals.||Ooradidgee Group||Overlies Kurinelli Sandstone (conformably); is conformably overlain by and partly interfingers with Treasure Volcanics.|Feldspathic and quartz arenite: medium to thickly bedded, medium- to coarse-grained, poorly sorted, commonly pebbly; minor conglomerate, siltstone, mudstone, calcareous beds and felsic lava.|
24513|Taragan Sandstone|68518|5|Briefly described|p9 Tb.1, p11-12|Proterozoic|Proterozoic|||Ooradidgee Subgroup||Conformable on Kurinelli Sandstone; overlain conformably by and in places interfingers with Treasure Volcanics.|Ridge-forming pebbly quartzose and feldspathic/lithic arenite grading into conglomerate; minor recessive felsic lava and micaceous siltstone.|30-MAY-16
24513|Taragan Sandstone|69187|6|Mentioned|p53 Fig.2|||Warramunga Province.||||||
24513|Taragan Sandstone|69418|6|Mentioned|p3:21, 23|||Tennant Region. Hosts the Wauchope field W vein deposit (described).||||||12-JUL-16
24513|Taragan Sandstone|69424|4|Described|p9:3, 5, 15, 17, 23-26, 28, 54-55|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Up to 900m thick. Predominantly fluviatile with three vertical and lateral facies: fan, meandering stream, and marine. Age range from surrounding units. Is intruded by 1811 +/- 5 Ma mafic sills. Hosts W and/or Au-bearing quartz veins.|Between 1837 +/- 7 Ma and 1814 +/- 3 Ma.|Ooradidgee Group.||Conformably overlies/interfingers with Kurinelli Sandstone. Is overlain conformably by, and interfingers with, Treasure Volcanics. Is overlain conformably/disconformably by Unimbra Sandstone.|Ridge-forming polymictic conglomerate (has quartz-haematite clasts probably derived from Warramunga Formation or equivalents); pebbly sandstone; quartz/feldspathic/sublithic sandstone. Recessive, variably micaceous siltstone; minor calcareous beds.|12-JUL-16
24513|Taragan Sandstone|69425|4|Described|p10:3, 5-6, 8-10, 13-14, 21, 23|||Thickness 0-over 1000m. Predominantly fluviatile (braided stream) deposition; three facies recognised vertically and laterally: alluvial fan, meandering stream and marine. Is overlain conformably/disconformably by Unimbra Sandstone. Hornfelsed by Devils Marbles Granite.||Ooradidgee Group.||Interfingers with and overlies Kurinelli Sandstone conformably (locally unconformably). Is overlain by, and interfingers with, Treasure Volcanics; and by Taragan Sandstone conformably/disconformably.|Ridge-forming polymictic conglomerate; pebbly sandstone; quartz/feldspathic/sublithic sandstone; recessive variably micaceous siltstone; sandstone; minor calcareous beds.|12-JUL-16
24513|Taragan Sandstone|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24513|Taragan Sandstone|72380|5|Briefly described|p1, p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces. Intruded by mineralised quartz veins at the Hit or Miss deposit, Hatches Creek tungsten field.||Unit of Ooradidgee Group.||||02-OCT-19
24513|Taragan Sandstone|73083|6|Mentioned|p22|||||||||
24513|Taragan Sandstone|73124|6|Mentioned|p2 Fig.1|||||||Underlain by Kurinelli Sandstone. Equivalent to Treasure Volcanics.||
24513|Taragan Sandstone|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
24513|Taragan Sandstone|73460|6|Mentioned|p2|||Warramunga Province.||||Underlain by Kurinelli Sandstone. Equivalent to Treasure Volcanics.||
24513|Taragan Sandstone|73590|6|Mentioned|p2|||||Ooradidgee Group||Underlain by Kurinelli Sandstone. Equivalent to Treasure Volcanics.||
80346|Tarlton Bore Granite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|||||Leucogranite: medium to coarse-grained, equigranular to weakly porphyritic, extensively altered, weakly to moderately foliated.|
80346|Tarlton Bore Granite|72516|2|Defined|iii, p10, p13-15, p21, p29, p64, 206-207|Statherian|Statherian|Aileron Province. Type location is defined as  634618mE 7482134mN. New name incorporating outcrops of weathered leucogranite that are widespread across the southern Jervois Domain and east of the Lucy Creek Fault Zone in the Tarlton Domain and rocks previously mapped as a leucocratic variant of the Jervois Granodiorite. Outcrops are commonly low rises and less commonly, small prominent hills; subcrop is widespread and occurs on the flats between more substantial outcrops. Named for the Tarlton Bore. Based on airborne magnetics the granite is interpreted to dominate the Tarlton Domain, extending east into TOBERMORY (where it is mapped as part of the mount Tietkins Granite Complex). Petrography, geochemistry, geophysics,alteration, mineralisation, metamorphism and structure are all discussed. See also p69-71, p85, p88, p96, p113-118, p122-123, p125-126, p135-137, p139, p145, p169, p171, p189, p206, p218.|1790-1750 Ma|||Unconformably overlain by the Grant Bluff Formation and the Yackah Beds. Intrudes the Baikal Supersuite and the Attutra Metagabbro. Intruded by the Boundary Igneous Complex.|Leucogranite: medium- to coarse-grained, equigranular to weakly porphyritic, strongly weathered to rottenstone, extensively altered, weakly to moderately foliated.|04-JUL-22
38787|Tawallah Group, Lower|23910|5|Briefly described|p292 Fig. 4|||Informal name - see Tawallah Group.||||||04-MAR-20
38787|Tawallah Group, Lower|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Sandstone. Geological Province: Southern McArthur Basin.||||||
38787|Tawallah Group, Lower|60483|5|Briefly described|p27, p64|||Informal - see Tawallah Group. Discusses low reflectivity.||||||
38787|Tawallah Group, Lower|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||includes Yiyintyi Sandstone to McDermott Formation..||Quartzose sandstone; subordinate conglomerate, ferruginous sandstone, dolostone, mudstone; basaltic volcanics; dolerite sills and dykes.|04-MAR-20
38787|Tawallah Group, Lower|73412|6|Mentioned|p18|||Southern McArthur Basin. Deposition during N-S to NE-SW directed extension.|c.1760-1740 Ma.|||||
40834|Tawallah Group, Upper|23963|6|Mentioned|p1237|||Geological Province: McArthur Basin.||||||03-MAR-05
40834|Tawallah Group, Upper|23968|6|Mentioned|p1362|||Geological Province: McArthur Basin.||||||
40834|Tawallah Group, Upper|24432|6|Mentioned|p559|Statherian||||||||
40834|Tawallah Group, Upper|60483|5|Briefly described|p29, p64|||Informal - see Tawallah Group. Discusses low to moderate reflectivity. Thickness: 1200-1800m. ||||||
40834|Tawallah Group, Upper|69423|6|Mentioned|p8:4 Fig.8.7|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Tawallah Group.||||12-JUL-16
40834|Tawallah Group, Upper|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|||Includes Wununmantyala Sandstone to Echo Sandstone.||Quartzose and lithic sandstone, mudstone, evaporitic-stromatolitic dolostone, shale (carbonaceous); synsedimentary basaltic sills and volcanics; dolerite sills; rhyolitic volcanics; high-level microgranite plutons.|04-MAR-20
40834|Tawallah Group, Upper|73412|6|Mentioned|p18|||Southern McArthur Basin. Deposition during NW-SE directed extension.||||||
29770|Teapot Granite Complex|22524|5|Briefly described|p37,table1p38|Stenian|Stenian|||||||
29770|Teapot Granite Complex|24567|6|Mentioned|p164 Fig. 6b|||||||||
29770|Teapot Granite Complex|24608|5|Briefly described|p986|Mesoproterozoic|Mesoproterozoic|Age: 1137 +/- 9 Ma.||||||
29770|Teapot Granite Complex|43225|5|Briefly described|Map Legend||Mesoproterozoic|Of Arunta Block.||||||11-DEC-06
29770|Teapot Granite Complex|43503|2|Defined|8,26,80|||Dated at 1040Ma.||||||11-DEC-06
29770|Teapot Granite Complex|44114|6|Mentioned|p340, 342|||Western end of the Chewings Zone, southern Arunta Inlier. Appears on p342 as Teapot Complex.|1150-1050 Ma.|||||
29770|Teapot Granite Complex|61660|5|Briefly described|p4. |Proterozoic|Proterozoic||1136 +/- 6 Ma SHRIMP zircon: Black and Shaw 1995.|||Intrudes Madderns Yard Metamorphic Complex.|Comprises intensely migmatitic quartzofeldspathic gneiss, and homogeneous granite formed by anatexis of the gneiss.|
29770|Teapot Granite Complex|64809|6|Mentioned|p11 Fig.10, p13 Fig.13 |Mesoproterozoic|Palaeoproterozoic|||||||
29770|Teapot Granite Complex|65232|5|Briefly described|p72|||High-uranium granitic orthogneiss. With Iwupataka Metamorphic Complex, provided source rocks for Brewer Conglomerate. Geol. Prov: Amadeus Basin.||||||09-FEB-10
29770|Teapot Granite Complex|65455|6|Mentioned|p6 Fig. 3|||In the southern Arunta region. Has moderate U enrichments and is considered to have moderate Cu-Au potential.||||||09-MAY-12
29770|Teapot Granite Complex|69221|5|Briefly described|p200-201|Mesoproterozoic|Mesoproterozoic|Basement to Amadeus Basin. High heat-producing granites (values given).|||||Granites.|
29770|Teapot Granite Complex|69418|6|Mentioned|p3:19|||Warumpi Province. Has potential for low-grade, high-tonnage U deposits.||||||12-JUL-16
29770|Teapot Granite Complex|69428|5|Briefly described|p13:3, 16, 19|Mesoproterozoic|Mesoproterozoic|Haasts Bluff Domain, Warumpi Province. Associated with the Teapot Event (1150-1130 Ma). Strongly enriched in radioactive elements; has a distinct positive radiometric anomaly. Has potential for uranium and REE mineralisation.|1136 +/- 6 Ma (Black and Shaw, 1995).|||Intrudes Glen Helen Metamorphics.|An extensive area of homogeneous leucocratic granite, locally with K-feldspar phenocrysts, and associated intensely migmatitic felsic gneiss.|12-JUL-16
29770|Teapot Granite Complex|69458|6|Mentioned|p42:36|||Warumpi Province. Extensively exposed in the MacDonnell Ranges. Source of REE-bearing alluvium at the Charley Creek deposit.||||||12-JUL-16
29770|Teapot Granite Complex|69932|6|Mentioned|p301-303, 306-307, 309-311|||Southern Province, Arunta Inlier. Characterised by low Sr/very high Y, with high Th-U-K. Sm-Nd data tabulated. Protolith paleosome age 1660 +/- 4 Ma.|1136 +/- 6 Ma (Black and Shaw, 1995).||||Banded migmatitic quartzofeldspathic gneiss of adamellite composition; granular, unfoliated granitoid (forms an apophysis); granite with flow foliation outlined by tabular feldspars.|
29770|Teapot Granite Complex|69937|6|Mentioned|p19, p22|||Warumpi Province. Associated with the 1150-1130 Ma Teapot Event. Possible source of (some) zircons in the Olympic Formation.||||||
29770|Teapot Granite Complex|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1136+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
76084|Teena Dolostone|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin; southern McArthur Basin. Age approximated from Fig.2.|c.1635 Ma.|Unit in River Supersequence.||||
76084|Teena Dolostone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3, p8 Tb.1, p14 Tb.5 |||See also p16-17. Called Dolomite in Tb.1 and 5.||Of the Umbolooga Subgroup.|Includes Coxco Dolostone Member.|||
76084|Teena Dolostone|67144|5|Briefly described|Map legend.|Statherian|Statherian|Recessive.||Unit in Umbolooga Subgroup.|Includes Coxco Dolostone Member.|Overlies Emmerugga Dolostone. Is overlain by Barney Creek Formation.|Thinly bedded to laminated dololutite, silicified in places; dolomitic shale, sandstone; intraclast breccia, conglomerate and dolarenite.|
76084|Teena Dolostone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.|1641 +/- 6 Ma (maximum depositional age).|||||
76084|Teena Dolostone|67352|4|Described|p13 Tb.2|Statherian|Statherian|McArthur Basin. 130 m thick.||Umbolooga Subgroup|Coxco Dolostone Member|Conformably overlies Mitchell Yard Dolostone Member and Mara Dolostone Member. Is overlain conformably by Barney Creek Formation.|Lower: thinly bedded to laminated dolomudstone: locally silicified; dolomitic shale and sandstone; mudstone, breccia, conglomerate, dolostone|
76084|Teena Dolostone|69430|4|Described|p15:3, 16, 18-19, 22, 34-35, 42, 61|Statherian|Statherian|Southern McArthur Basin. Marine sediments, partly below wave base. Hosts the Barneys Pb prospect. Fair to good conventional hydrocarbon reservoirs occur.|1641 +/- 6 Ma.|Umbolooga Subgroup.|Coxco Dolostone Member.|Conformably overlies Emmerugga Dolostone. Is overlain conformably and gradationally by Barney Creek Formation.|Dololutite, crystalline or thinly bedded to laminated and locally silicified; dolomitic shale and sandstone; intraclast breccia and conglomerate; dolarenite.|12-JUL-16
76084|Teena Dolostone|69432|6|Mentioned|p17:7|||McArthur Basin. Contains Coxco Needles: radiating clusters of botttom-nucleated acicular crystal pseudomorphs which are identical to those from the Blue Hole Formation (Limbunya Group), Birrindudu Basin.||||||12-JUL-16
76084|Teena Dolostone|69673|4|Described|p18, p32, p33, p41, p42, p43|||Batten Fault Zone. Potential reservoir rock.|1641 +/- 6 Ma|Umbolooga Subgroup|Includes Coxco Dolostone Member|Conformably overlies Emmerugga Dolostone, conformably overlain by Barney Creek Formation|Thickly to thinly bedded or finely laminated dolomudstone that is in places stromatolitic. Thin beds of dolomitic shale, siltstone and sandy dolostone and some thin beds of potassium rich mudstone.|
76084|Teena Dolostone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1639+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ash tuff.|
76084|Teena Dolostone|72373|5|Briefly described|p8,11,17|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Dated at 1641+\-6 Ma; partially overlaps in age with Baiguridji Formation (Ahmad et al 2013).||Unit of  upper McArthur Group.|Includes Coxco Dolostone Member.|||02-OCT-19
76084|Teena Dolostone|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.|1639 +/-6 Ma|Batten Subgroup|[Coxco Dolostone Member]|Overlies Emmerugga Dolostone and Mitchell Yard Member and underlies Coxco Dolostone Member.||
76084|Teena Dolostone|72718|6|Mentioned|p7|||Southern McArthur Basin. Batten Fault Zone.||Umbolooga Sub-group, McArthur Group|Coxco Dolostone Member?|Underlain by Emmerugga Dolostone including Mitchell Yard Member. Overlain by Coxco Dolostone Member.||
76084|Teena Dolostone|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).|1639 +/- 6 Ma|Batten Subgroup|Probably includes Coxco Dolostone Member.|Overlies Emmerugga Dolostone and Mitchell Yard Member.||
76084|Teena Dolostone|73042|6|Mentioned|p4|Statherian|Statherian|Southern McArthur Basin, Isa Superbasin. Geochronology is a U-Pb zircon sedimentary depositional age (?maximum depositional age).|1639 +/- 6 Ma (see Fig.1.2)|Batten Subgroup, McArthur Group||Underlain by Emmerugga Dolostone. Overlain by Coxco Dolostone Member.||
76084|Teena Dolostone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Umbolooga Subgroup.||Overlies Tooganinie Formation and Myrtle Shale. Is overlain by Barney Creek Formation.||
39127|Tennant Creek Supersuite|23733|5|Briefly described|p13, p15, p28|Paleoproterozoic|Paleoproterozoic|Age: 1850Ma.  See also p32 Fig. 19, p34 Fig. 20.||||||07-NOV-08
39127|Tennant Creek Supersuite|23809|5|Briefly described|p27|Paleoproterozoic|Paleoproterozoic|Includes Tennant Creek, Cabbage Gum, Channingum, and Hill of Leader Granites, Mumbilla Granodiorite and unnamed porphyries, granophyre and granites.Age: ca1850Ma.||||||07-NOV-08
39127|Tennant Creek Supersuite|24047|5|Briefly described|p7 Fig. 6, p37|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Inlier.||||||07-NOV-08
39127|Tennant Creek Supersuite|24197|4|Described|p22, p65-66|Paleoproterozoic|Paleoproterozoic|Comprises Tennant Creek, Cabbage Gum, Hill of Leaders and Channinggum(sp?) Granites, Mumbilla Granodiorite + parts of Berborough and Warramunga Fms, Epenerra and Warrego Volcs. I-(granodiorite) type.Geol.P: Tennant Creek Inlier. Eg.of Kalkadoon Assocn.||||||07-FEB-11
39127|Tennant Creek Supersuite|50588|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Age: 1850Ma.||||||07-NOV-08
39127|Tennant Creek Supersuite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes Tennant Creek, Cabbage Gum, Channingum Granites, Mumbilla granodiorite and Hill of LeadersGranite. In the Tennant Creek region.||||||07-NOV-08
39127|Tennant Creek Supersuite|64722|5|Briefly described|Fig. 2 p3-6, p10|Orosirian|Orosirian|Of Tennant Region of the North Australian Craton.|~1850 Ma.|||Intrudes the Warramunga Formation.||13-MAR-13
39127|Tennant Creek Supersuite|64735|6|Mentioned|p205||Orosirian|Igneous crystallisation age.|ca.1.85 Ga.|||Intrudes Warramunga Formation.||30-APR-12
39127|Tennant Creek Supersuite|65209|5|Briefly described|p35 Fig.1, p37, p39|Paleoproterozoic|Paleoproterozoic|Magmatism that is broadly syn-, to post-tectonic with respect to the Tennant Event was assigned to this unit by Wyborn et al. (1998). In general, granites are apparently localised in the Warramunga Province.|||Tennant Creek Granite, Cabbage Gum Granite, Channingum Granite, Mumbilla Granodiorite, Hill of Leaders Granite.|||05-JAN-17
39127|Tennant Creek Supersuite|65338|5|Briefly described|p6. |Orosirian|Orosirian||c.1850 - 1840 Ma.|||Intrudes Warramunga and Junalki Formations, Woodenjerrie beds and Ooradidgee Group.|Granitic intrusives.|
39127|Tennant Creek Supersuite|67148|5|Briefly described|Map legend.|Proterozoic|Proterozoic||||||Granite: biotite and biotite-muscovite bearing; porphyritic; xenolithic; leucogranite.|
39127|Tennant Creek Supersuite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.|||Includes Tennant Creek, Cabbage Gum, Channingum and Hill of Leaders Granites; Mumbilla Granodiorite; and an un-named porphyry and granite.|||
39127|Tennant Creek Supersuite|67352|6|Mentioned|p44 Fig.48||||||||Granite and leucogranite.|08-JAN-15
39127|Tennant Creek Supersuite|69187|5|Briefly described|p53 Fig.2, p54 Fig.3|||See also Tennant Supersuite on p51-52, p61-62.|||Tennant Creek Granite, Cabbage Gum Granite, Channingum Granite, Mumbilla Granodiorite, Hill of Leaders Granite|||
39127|Tennant Creek Supersuite|69417|5|Briefly described|p2:5|Orosirian|Orosirian|Warramunga Province.||||Intrudes Warramunga Formation.||12-JUL-16
39127|Tennant Creek Supersuite|69424|4|Described|p9:2-4, 6, 10-15, 28-29, 34, 50-51|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Wyborn et al. (1988). Warramunga Province. This unit also includes felsic extrusives of the Bernborough and Junalki Formations, Epenarra Volcanics and Woodenjerrie beds. The article adds "volcanic rocks of the Yungkulungu Formation should also be included..."[?]. Syn- to post-tectonic in relation to the Tennant Event. Magmatism was contemporary with folding in the c.1860-1850 Ma Tennant Event. Had previously been classified as I-type (Wyborn et al., 1998). Petrography and mineralogy described.|c.1850-1840 Ma.||Tennant Creek, Cabbage Gum, Channingum, Hill of Leaders Granites; Mumbilla Granodiorite. See Comments for more.||Granitic rocks (including granite, granodiorite and tonalite), some felsic porphyry and dolerite, and extrusive felsic rocks. A-type.|12-JUL-16
39127|Tennant Creek Supersuite|69425|6|Mentioned|p10:2, 20|||Tennant Region. Unlike Devils Suite, this unit has associated extrusive rocks.||||||12-JUL-16
39127|Tennant Creek Supersuite|69431|6|Mentioned|p16:2|||Tennant Region.||||||12-JUL-16
39127|Tennant Creek Supersuite|69917|6|Mentioned|p131|||Warramunga Province, Tennant Region.|||Includes Tennant Creek Granite|||
39127|Tennant Creek Supersuite|70303|6|Mentioned|iv, p17|Paleoproterozoic|Paleoproterozoic|Tennant Region. Felsic magmatism typically aged ~1850 Ma.||||||
39127|Tennant Creek Supersuite|71621|6|Mentioned|p25|||Warramunga Province, Tennant Region.||||||02-FEB-19
39127|Tennant Creek Supersuite|73124|5|Briefly described|piii, p2 Fig.1, p6, p12|Orosirian|Orosirian|Age of intrusive [and extrusive?] felsic magmatism matches that of four unnamed units (ca 1854-1849 Ma): a quartz-feldspar porphytic rhyloite and an extrusive dacite from drillhole RVDD0002, and two volcaniclastic sandstones (drillholes RVDD0002 and MXCURD002).||||||
39127|Tennant Creek Supersuite|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.|||Tennant Creek, Cabbage Gum, Channingum, Hill of Leaders Granites; Mumbilla Granodiorite; Warrego Volcanics.|||
39127|Tennant Creek Supersuite|73427|5|Briefly described|p1, p3-5, p12-14, App.A|Orosirian|Orosirian|North Australian Craton, Tennant Region/East Tennant. Emplacement post-dated a significant amount of regional deformation. The Yungkulungu Formation and Monument Formation represent extrusive equivalents.|1855-1845 Ma|||Intrudes Warramunga Formation, Woodenjerrie beds, and Junalki Formation.||
39127|Tennant Creek Supersuite|73460|6|Mentioned|p2|||Warramunga Province.|||Tennant Creek Granite, Cabbage Gum Granite, Channingum Granite, Mumbilla Granodiorite, Hill of Leaders Granite|||
39127|Tennant Creek Supersuite|73550|5|Briefly described|p4|Orosirian|Orosirian||ca 1850-1840 Ma||||Comprises mainly granitic intrusions with lesser granodiorite, tonalite, felsic porphyry and dolerite, as well as extrusive felsic volcanic rocks.|
39127|Tennant Creek Supersuite|73590|5|Briefly described|piii, p1-2, p25|Orosirian|Orosirian||ca 1850-1840 Ma||Tennant Creek Granite, Cabbage Gum Granite, Channingum Granite, Mumbilla Granodiorite, Hill of Leaders Granite||Mainly granite with lesser granodiorite, tonalite, felsic porphyry and dolerite, as well as felsic volcanic rocks.|
27058|Tennysons Leucogranite|23120|5|Briefly described|p428|||||||||
27058|Tennysons Leucogranite|23216|5|Briefly described|Table1p10,12,15,17,38|||||||||
27058|Tennysons 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
27058|Tennysons Leucogranite|24340|4|Described|p143, p152|Paleoproterozoic|Paleoproterozoic|Age: ~1825 Ma. Geological Province: Pine Creek Inlier. Classified as Transitional Igneous Suite by Klominsky et al., 1996||||||07-NOV-08
27058|Tennysons Leucogranite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27058|Tennysons Leucogranite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27058|Tennysons Leucogranite|41125|6|Mentioned|p55|||||||||
27058|Tennysons Leucogranite|41311|6|Mentioned|p17|||||||||
27058|Tennysons Leucogranite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27058|Tennysons Leucogranite|42756|6|Mentioned|Fig.5 P6|||||||||
27058|Tennysons Leucogranite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
27058|Tennysons Leucogranite|43832|3|Fully described|Table8 p37; 46,50,61||Paleoproterozoic|||||||07-NOV-08
27058|Tennysons Leucogranite|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
27058|Tennysons Leucogranite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Coarse porphyritic muscovite-biotite leucogranite. Intrudes Finniss River Group.||||||07-JAN-09
27058|Tennysons Leucogranite|65232|6|Mentioned|p65, App. 2|||Greisenised. Uranium occurrences are tabular or lenticular bodies within a shear zone that includes siliceous haematitic breccia.||||||09-FEB-10
27058|Tennysons Leucogranite|67564|6|Mentioned|p33 Fig.19, p59.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
27058|Tennysons Leucogranite|69420|5|Briefly described|p5:17-19, 23, 42, 84|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Associated with several uranium occurrences.||Tennysons Suite.|||Coarse-grained porphyritic leucogranite with interspersed phase of medium to fine leucogranite. I-type.|12-JUL-16
31732|Tennysons Suite|24197|5|Briefly described|p24|||Of Tennysons Suite (Cullen Supersuite). Includes the Tennysons Leucogranite, Wolfram Hill (?), Fenton Granite and Umbrawarra Leucogranite. Geological province: Pine Creek Inlier.||||||07-FEB-11
31732|Tennysons Suite|50586|6|Mentioned|p4.21|||Geological Province: Pine Creek Inlier. Of the Cullen Supersuite.||||||
31732|Tennysons Suite|69420|5|Briefly described|p5:17, 19, 22|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised.||Cullen Supersuite.|Tennysons, Yenberrie, Umbrawarra Leucogranites; Wolfram Hill, Fenton Granites.|||12-JUL-16
31732|Tennysons Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Fenton Granite, Umbrawarra Leucogranite.|||01-MAR-18
40574|Term Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes Stretton Sandstone and Looking Glass Formation.|||
40574|Term Supersequence|63866|5|Briefly described|p53, p56|||Isa Superbasin.|||Includes the Stretton Sandstone.|||
40574|Term Supersequence|65228|5|Briefly described|p32, pp35-37, Figs.22-23, 28.|Statherian|Statherian|Up to 2,500 m thick. Represented by basal Stretton Sandstone and Looking Glass Sandstone (in McArthur River Region), and by Termite Range Formation and lower part of Lawn Hill Formation (in southern Lawn Hill Platform). Gamma ray log, lithology and facies detailed.|c.1630-1620 Ma.|||Overlies River Supersequence.|Turbiditic and hemipelagic sandstones and shales.|
40574|Term Supersequence|66843|6|Mentioned|p38 Fig.10|||Said to be "informally" named.||||||
40574|Term Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40574|Term Supersequence|67323|5|Briefly described|Mount Isa Block Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|Mount Isa Inlier.|~1635-1615 Ma.|McNamara Group.||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation and Termite Range Formation.||||||
40574|Term Supersequence|69056|6|Mentioned|p56|||||||||
40574|Term Supersequence|69591|5|Briefly described|p27, p43, p46-47, p54, p108|||Mount Isa Province. Deeper-water medium- to coarse-grained clastic turbidite packages. Recognised in the Nathan Group (NT). Consists of the Termite Range Formation.||||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|70897|5|Briefly described|p39, Fig.1.7.1-3,7|||Shows rapid thickness and lithofacies variations across regional fault systems.||||Overlies River Supersequence. Is overlain by Lawn Supersequence.||
40574|Term Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Lawn Hill Formation and uppermost Termite Range Formation.|||||White and grey thick-bedded sandstone and lithic sandstone interbedded with siltstone.|
40574|Term Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||||Fissile to flaggy tuff and tuffaceous siltstone, thinly interbedded micaceous siltstone, shale and claystone. Grey to black carbonaceous shale containing light grey silty carbonate concretions and flaggy siltstone interbeds, minor tuff.|
40574|Term Supersequence|72912|5|Briefly described|p33 Fig.12, p34, p35 Fig.13.|Paleoproterozic|Paleoproterozic|This unit requires more Rock-Eval for hydrocarbon potential to be determined.||||Overlies River Supersequence and underlies Lawn Supersequence.||
40574|Term Supersequence|73144|4|Described|p8-9, p11-12, p20, p25|Statherian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains five third order sequences [see article for more detail on third order sequences]. Deposited in mid-outer self, silty turbidites and submarine fans (Krassay et al., 2000). Forms a series of onlapping wedges which gradually thin to the north. An emergent basement high associated with the Murphy Inlier is considered as the source of turbidites. Capped by a significant erosional event.|1615-1630 Ma|||Includes a portion of the Lawn Hill Formation, and Termite Range Formation.|Siltstone, shale, carbonaceous siltstone, sandstone including coarse-grained sandy turbidites.|
80338|Thring Granite|71621|5|Briefly described|p1, p21, 23, 32, 36, p38-p40|||Aileron Province.  [Interpreted intrusive age said to be 1.77 Ga (Beyer et al, in prep), but this is not explained.] Zircons were unsuitable for LA-ICP-MS dating. Petrography and zircon description discussed.|No meaningful ICP-MS dating possible.|||Intruded by the Boundary Igneous Complex. Interpreted to intrude Mascotte and White Violet orthogneisses, Kings Legend Metadolerite.|Fine- to medium-grained, equigranular, quartz-K-feldspar-plagioclase leucogranite.|02-FEB-19
80338|Thring Granite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|||||Leucogranite: medium to coarse-grained, equigranular, strongly weathered to rottenstone and altered (silicified); weakly to moderately foliated.|
80338|Thring Granite|72516|2|Defined|p13, p15, p17, p19-21, p208|Statherian|Statherian|Georgina Basin, Jinka Domain. New name, named for the Thring Creek, a tributary of the Plenty River south of Bonya Hills. The type location is defined as 611792mE 7476200mN. Formerly included as part of the Mascotte Gneiss Complex of Freeman (1986) and Freeman et al (1986). Outcrops as blocky and bouldery hills and nubbins in southwestern Bonya Hills. Deposited in a continental back margin environment. Geochemistry, structure, distinguishing features, structure, metamorphism, alteration, mineralisation and geophysics are discussed. Interpreted to be comagmatic with the Jericho Granite and Unca Granite. See also p29, p32, p35, p44, p56, p60-63, p73, p75, p77, p86, p104, p125-126, p135-137, p145, p153, p171, p189, p192, p195, p208, p218. |Ca. 1760 Ma-1780 Ma|Fosters Suite||Nonconformably overlain by the Oorabra Arkose. Unconformably overlain by the Elkera Formation and the Mount Baldwin Formation.|Leucogranite: medium to coarse-grained, equigranular, minor biotite and chlorite after biotite, secondary muscovite common; strongly weathered to rottenstone and altered (silcified); weakly to moderately foliated.|04-JUL-22
80338|Thring Granite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes granite.|
35323|Tijunna Group|14019|5|Briefly described|p2 Fig. 1|||Geological Province: Victoria Basin.||||||
35323|Tijunna Group|24122|2|Defined|p8, p20 App.2|Proterozoic|Proterozoic|Sandstone, siltstone.  Includes Stubb Formation and Wondoan Hill Formation.Geological Province: Victoria Basin.||||||25-JAN-10
35323|Tijunna Group|24297|3|Fully described|p14|Mesoproterozoic|Mesoproterozoic|Includes Stubb Formation and Wondoan Hill Formation.  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||
35323|Tijunna Group|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
35323|Tijunna Group|24300|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Victoria Basin|||Includes Wondoan Hill Formation, Stubb Formation.|||
35323|Tijunna Group|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Unconformably overlies Bullita Group; unconformably overlain by Auvergne Group. Geological Province: Victoria Basin.||||||
35323|Tijunna Group|24442|5|Briefly described|p50 Fig. 1|||Includes the Stubb and Wondoan Hill Formations.  Geological Province: Victoria Basin.||||||
35323|Tijunna Group|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Sandstone, siltstone. Geological Province: Victoria Basin.||||||
35323|Tijunna Group|60682|6|Mentioned|p3 Fig. 2|||Geological Province: Victoria Basin.||||||
35323|Tijunna Group|60685|5|Briefly described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Comprises the Stubb and Wondoan Hill Formations. Sandstone and siltstone. Age: 1.43-1.35Ga. Geological Province: Victoria Basin. See also Tijunna group.||||||
35323|Tijunna Group|64724|6|Mentioned|p45 Fig.5|Calymmian|Calymmian|Victoria River Basin||||||
35323|Tijunna Group|65342|5|Briefly described|pp10-11.|||Victoria Basin.|||Includes Wondoan Hill Formation and Stubb Formation.|Unconformably overlies Bullita Group. Is unconformably overlain by Auvergne Group.|Sandstone and mudstone.|
35323|Tijunna Group|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.|||Includes Wondoan Hill and Stubb Formations.|Unconformably overlies Bullita Group. Is unconformably overlain by Auvergne Group.||
35323|Tijunna Group|68733|5|Briefly described|p177, p179 Tb.1, p181-186, p191-192|Cryogenian||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). Separated from the overlying Auvergne Group by a major regional unconformity which separates Birrindudu and Victoria Basins.|||Includes Stubb Formation and Wondoan Hill Formation.|Unconformably overlain by the Auvergne Group.||06-DEC-17
35323|Tijunna Group|69417|5|Briefly described|p2:5-6|Calymmian|Calymmian|Southern Birrindudu Basin.|||||Predominantly shallow marine sandstones.|12-JUL-16
35323|Tijunna Group|69432|4|Described|p17:1-3, 12-13|||Beier et al. (2002). Birrindudu Basin. Previously (Cutovinos et al., 2002) asssigned to the Victoria Basin. Inclusion in Birrindudu Basin is supported by detrital zircons with greater affinities with those in underlying strata than with those in Auvergne Group. Wide variation in thickness: zero (absent) to 300m. Is gently folded into broad domes, anticlines and synclines 10-50km across. Possible exploration target for base metals.|||Wondoan Hill, Stubb Formations.|Unconformably overlies Bullita Group. Is overlain unconformably by Auvergne Group.|Sandstone and mudstone assemblages.|12-JUL-16
35323|Tijunna Group|69441|6|Mentioned|p26:1|||Birrindudu Basin. Assigned to the Birrindudu Basin as its detrital zircons have greater affinities with these older rocks than with those of the overlying Auvergne Group (Victoria Basin).||||Is overlain unconformably by Auvergne Group.||12-JUL-16
35323|Tijunna Group|69445|5|Briefly described|p30:4|Proterozoic|Proterozoic|Victoria River region, Birrindudu Basin.||||Is overlain unconformably by Antrim Plateau Volcanics.||12-JUL-16
35323|Tijunna Group|69673|6|Mentioned|p3 fig 2, p47, p48 fig 35|Mesoproterozoic|Mesoproterozoic|Up to 300m thick.|||Includes Wondoan Hill Formation, Stubb Formation|Unconformably overlies Bullita Group, unconformably overlain by Auvergne Group|Sandstone and mudstone assemblages.|
35323|Tijunna Group|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.|||Includes Stubb Formation, Wondoan Hill Formation.|Unconformably overlies Bullita Group. Is unconformably overlain by Auvergne Group.||
35323|Tijunna Group|70850|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wondoan Hill, Stubb Formations.|Unconformably overlies Bullita Group. Is overlain unconformably by Auvergne Group.||
35323|Tijunna Group|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wondoan Hill Formation.|Unconformably overlies Bullita Group. Is overlain unconformably by Auvergne Group.||
35323|Tijunna Group|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Wondoan Hill, Stubb Formations.|Unconformably overlies Bullita Group. Is overlain unconformably by Antrim Plateau Volcanics.|Sandstone, siltstone, shale, mudstone, claystone.|
35323|Tijunna Group|70968|3|Fully described|v-vi, p2-3, p115-120, p123-124, p126-133|Ectasian|Calymmian|See also p137, p139-140. Beier and Dunster in Beier et al. (2002). Named after Tijunna Bore. Top of Birrindudu Basin succession. Part of the Wilton package. Lithologies and depositional environments are similar to those of the relatively thicker Roper Group. Generally poor exposures. Thickness varies considerably, from 0 to 300m. Detrital zircon diagram.|||Wondoan Hill, Stubb Formations.|Unconformably overlies Bullita Group. Is overlain unconformably by Jasper Gorge Sandstone (Auvergne Group). Correlated with Renner and Roper Groups.|Alternating cross-bedded quartz sandstone- and mudrock-dominated units, deposited in marine shelf to shoreface settings.|
35323|Tijunna Group|71059|6|Mentioned|p2|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||||Equivalent to the Roper Group.||
35323|Tijunna Group|71169|5|Briefly described|p71|Calymmian|Calymmian|North Australian Craton.|c. 1550-1400 Ma|||||
35323|Tijunna Group|71302|5|Briefly described|p2,6,72-74|Mesoproterozoic|Paleoproterozoic|Of Birindudu Basin.|||Includes Stubb Formation and Wondoan Hill Formation.|Overlain unconformably by Auvergne Group. Underlain by Bullita Group.||
35323|Tijunna Group|71374|5|Briefly described|p2|||Birrindudu Basin.||||Broadly equivalent to the Roper Group and Renner Group.||
35323|Tijunna Group|71488|6|Mentioned|p142|||Birrindudu Basin.||||||
35323|Tijunna Group|71779|5|Briefly described|p5, p23, p24, 26, 27|||Birrindudu Basin. Probably equivalent to the Velkerri Formation.||||Unconformably overlies the Wattie, Bullita and upper Limbunya groups. Equivalent to the Roper Group.||24-SEP-18
35323|Tijunna Group|71893|5|Briefly described|iii, p1-p3, p7-p8, p68-p69, p71|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.|||Includes the Wondoan Hill Formation and the Stubb Formation.|||
35323|Tijunna Group|72373|5|Briefly described|p2|Mesoproterozoic|Mesoproterozoic|Of Birrindudu Basin. Broadly equivalent to Wilton package, Roper Group (McArthur Basin) and Renner Group (Tomkinson province).||||||
35323|Tijunna Group|72381|5|Briefly described|p773|||Of Birrindudu Basin.||||Correlable with Wilton Package, Roper Group (McArtbur Basin) and Renner Group (Tomkinson Province).||
35323|Tijunna Group|72718|6|Mentioned|p7, p18|||Birrindudu Basin. Equivalent to units of the Wilton package.|||Stubb Formation, Wondoan Hill Formation|||
70607|Tilmouth beds|61828|5|Briefly described|p162, p163 Fig. 4|Late Pleistocene|Late Pleistocene|Distinctive lacustrine facies - olive-grey clay with gypsum laminae.||||||
70607|Tilmouth beds|69458|5|Briefly described|p42:13, 24|Holocene|Pleistocene|Lake Lewis Basin. Represents the onset of fluctuating lake conditions and high levels of salinity in a closed palaeolake system. Tentatively assigned to the last interglacial period at around 130-110 Ka.||||Overlies Anmatyerre Clay.|Olive-grey lacustrine clay with gypsum laminae.|12-JUL-16
36758|Timber Creek kimberlites|14019|6|Mentioned|p14|||Informal reference to part of the Timber Creek Formation.  Age: 179+/-2Ma (Belousova et al, 2001) but is much younger than ages assigned to surrounding rocks.||||||
36758|Timber Creek kimberlites|23772|5|Briefly described|p757-759|Jurassic|Proterozoic|Situated within the Proterozoic Victoria River Basin. Age: 1462+/-53 Ma, 1038+/-66 Ma, and a much younger zircon population of 179+/-2 Ma.Also see p762. Max. thickness: 3500 m.||||||17-FEB-22
36758|Timber Creek kimberlites|24122|6|Mentioned|p1|||Informal name.  Age: 179+/-2Ma.||||||
36758|Timber Creek kimberlites|24297|6|Mentioned|p4|||Informal name.  Age: 179+/-2Ma.  Geological Province: Victoria Basin.||||||
36758|Timber Creek kimberlites|24568|6|Mentioned|p173|Mesoproterozoic|Mesoproterozoic|Informal name.  Age: 1.462Ga.||||||06-APR-05
36758|Timber Creek kimberlites|60685|5|Briefly described|p4|||Informal - see Timber Creek Formation. Age: 179 +/- 2Ma. Intrudes Timber Creek Formation.||||||17-FEB-22
40053|Tin Pot Suite|24047|5|Briefly described|p10|Mesoproterozoic|Mesoproterozoic|Age: 1140Ma.  Geological Province: Arunta province.||||||
24525|Tindall Limestone|9324|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group. Limestone, fine-grained, crystalline, dolomitic, algal and cherty in part with layers of quartz arenite and siltstone.||||||
24525|Tindall Limestone|14019|5|Briefly described|p20|Middle Cambrian|Middle Cambrian|Fossiliferous unit.  Overlies the Antrim Plateau Volcanics.||||||
24525|Tindall Limestone|22809|4|Described|20|||||||||
24525|Tindall Limestone|22810|4|Described|Table3 P7, P19|Ordovician|Cambrian|Maximum thickness 124.3m. Overlies Tolmer Group.||||||11-DEC-06
24525|Tindall Limestone|22813|5|Briefly described|Map|Cambrian|Cambrian|Part of the Daly River Group. Siltstone, limestone, mudstone, packstone, arkosic sandstone and conglomerate.||||||19-OCT-05
24525|Tindall Limestone|23216|4|Described|p3-4,Table1p7,37-42||Middle Cambrian|Of the Daly River Group. Age by Opik (1956).||||||19-JAN-06
24525|Tindall Limestone|23328|5|Briefly described|1030|Middle Cambrian|Early Cambrian|||||||07-SEP-09
24525|Tindall Limestone|23714|5|Briefly described|p7 Table 1.|Paleozoic|Paleozoic|See also page 36. Of Daly River Group. Max. thickness: 180 m.||||||07-NOV-08
24525|Tindall Limestone|23715|5|Briefly described|Map legend||Paleozoic|||||||07-NOV-08
24525|Tindall Limestone|24047|5|Briefly described|p62|Cambrian|Cambrian|Overlain by Petrel Formation.  Geological Province: Dunmarra Basin.||||||
24525|Tindall Limestone|24122|3|Fully described|p13, p3, Fig. 2|Cambrian|Cambrian|Of Daly River Group. Conformably overlain by Jinduckin Formation. Approximately 180m. thick.  Limestone, mudstone.  Geological Province: Daly Basin.||||||
24525|Tindall Limestone|24297|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral equivalent of Montejinni Limestone. Geological Province: Daly Basin.||||||
24525|Tindall Limestone|24300|5|Briefly described|Map Legend|Cambrian|Cambrian|Of the Daly River Group.   Geological Province: Daly Basin.||||||11-DEC-06
24525|Tindall Limestone|24303|5|Briefly described|p38, p39|||Geological Province: Daly Basin. Max. Thickness: 182.8m. Equivalent to Gum Ridge Formation.||||||
24525|Tindall Limestone|28255|6|Mentioned|p94-95, p82|||Correlated with Headleys Limestone.  Geological Province: Day River and Wiso Basins.||||||15-JUN-05
24525|Tindall Limestone|29591|6|Mentioned|p107|||||||||
24525|Tindall Limestone|30003|6|Mentioned|p14|||Geological Province: Daly River Basin.||||||19-APR-05
24525|Tindall Limestone|31572|6|Mentioned|p22|||M.Camb.||||||
24525|Tindall Limestone|31917|6|Mentioned|Table 1|||M.Camb.||||||
24525|Tindall Limestone|32170|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|32171|6|Mentioned|p8|||Mid Cambrian||||||
24525|Tindall Limestone|32700|4|Described|Table 2|||||||||
24525|Tindall Limestone|32775|5|Briefly described|Map legend|Middle Cambrian|Middle Cambrian|Fossiliferous limestone and dolomitic limestone.||||||02-DEC-04
24525|Tindall Limestone|33373|3|Fully described|p10|||On Table 3.||||||
24525|Tindall Limestone|33374|6|Mentioned|p13|||Correlation||||||
24525|Tindall Limestone|33376|6|Mentioned|Map legend|Early Ordovician|Middle Cambrian|Middle Cambrian to Lower Ordovician||||||
24525|Tindall Limestone|34051|5|Briefly described|Table 1|||L.- M.Camb. See also pp6,8,12,13.||||||11-DEC-06
24525|Tindall Limestone|34052|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|34053|6|Mentioned|p8|||L.- M.Cambrian||||||
24525|Tindall Limestone|34438|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
24525|Tindall Limestone|34439|5|Briefly described|Table 1|||M.Camb. See also pp9,11.||||||11-DEC-06
24525|Tindall Limestone|34440|5|Briefly described|Table 1|||M.Camb. See also pp9,10.||||||11-DEC-06
24525|Tindall Limestone|34441|6|Mentioned|p12|||M.Camb. Correlate||||||
24525|Tindall Limestone|35224|6|Mentioned|p5|||||||||
24525|Tindall Limestone|35231|6|Mentioned|p8|||||||||
24525|Tindall Limestone|36335|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|Middle Cambrian(Ordian).||||||
24525|Tindall Limestone|38267|6|Mentioned|p84|||||||||
24525|Tindall Limestone|38902|6|Mentioned|p20|||||||||
24525|Tindall Limestone|39210|5|Briefly described|p48|||See also Fig.18||||||
24525|Tindall Limestone|39523|6|Mentioned|p95|||||||||
24525|Tindall Limestone|40136|6|Mentioned|p22|||See also p28.||||||11-DEC-06
24525|Tindall Limestone|40168|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician. Of the Daly River Group. Massive thinly bedded limestone with chert bands and nodules in places.||||||18-OCT-05
24525|Tindall Limestone|40852|6|Mentioned|p37|||||||||
24525|Tindall Limestone|40957|6|Mentioned|Map legend|Ordovician|Cambrian|Cambrian to Ordovician||||||
24525|Tindall Limestone|41586|6|Mentioned|Map legend|Middle Cambrian|Early Cambrian|||||||
24525|Tindall Limestone|41660|5|Briefly described|Map legend|Cambrian|Cambrian|Of Daly River Group. Grey and beige dolomitic limestone, algal and cherty in part.||||||07-OCT-05
24525|Tindall Limestone|41661|4|Described|p23|||||||||
24525|Tindall Limestone|42012|1|Redefined|p42|Middle Cambrian||See also p15. [Listed as DEF when entered, but is RDEF of Randal (1962) CEBMar95]||||||11-DEC-06
24525|Tindall Limestone|42014|5|Briefly described|Map legend|Cambrian||||||||
24525|Tindall Limestone|42070|4|Described|p3|||||||||
24525|Tindall Limestone|42206|6|Mentioned|p260|||||||||
24525|Tindall Limestone|42267|6|Mentioned|Fig.3 P312|||||||||
24525|Tindall Limestone|42639|6|Mentioned|p46|||In the Daly Basin.||||||11-DEC-06
24525|Tindall Limestone|43140|4|Described|p4|||Of the Daly River Group.||||||11-DEC-06
24525|Tindall Limestone|43149|5|Briefly described|Map Legend|Ordovician|Cambrian|Of the Daly River Group.||||||11-DEC-06
24525|Tindall Limestone|43187|5|Briefly described|p2|||||||||
24525|Tindall Limestone|43652|6|Mentioned|p386||Middle Cambrian|||||||
24525|Tindall Limestone|43832|4|Described|31, Table7 p26|Templetonian|Ordian|Age Middle Cambrian (late Ordian - early Templetonian)||||||
24525|Tindall Limestone|44113|5|Briefly described|p240|Middle Cambrian|Middle Cambrian|Of the Daly River Group. Geological Province: Daly River Basin. Maximum Thickness: 152m.||||||
24525|Tindall Limestone|44161|14|Not recorded|p.47||Middle Cambrian|||||||
24525|Tindall Limestone|44201|14|Not recorded|p.10||Cambrian|L.M.Cambrian.||||||
24525|Tindall Limestone|44332|14|Not recorded|p.10,opp.6,map|||(D53-14).||||||
24525|Tindall Limestone|44333|14|Not recorded|map legend|||Middle Cambrian?||||||
24525|Tindall Limestone|44459|14|Not recorded|p.9,14, opp.p.6, map|||(E53-2).||||||
24525|Tindall Limestone|44460|14|Not recorded|map legend||Middle Cambrian|Middle Cambrian.||||||
24525|Tindall Limestone|45022|3|Fully described|p.102, 103.|Ordovician|Cambrian|On many pages.||||||11-DEC-06
24525|Tindall Limestone|45058|6|Mentioned|p18|||See also p19. Unit of Daly River Group||||||11-DEC-06
24525|Tindall Limestone|45064|3|Fully described|Table 1|||See also p20.||||||11-DEC-06
24525|Tindall Limestone|45148|6|Mentioned|Fig.4|||Daly River Basin. See also p24.||||||11-DEC-06
24525|Tindall Limestone|45168|6|Mentioned|p6|||||||||
24525|Tindall Limestone|46675|5|Briefly described|Map legend|Paleozoic|Paleozoic|Of the Daly River Group.  Fossiliferous limestone with minor chert nodules and bands.||||||07-NOV-08
24525|Tindall Limestone|46676|14|Not recorded|p.6||Middle Cambrian|M.Cambrian; unit of Daly River Group.||||||
24525|Tindall Limestone|46679|14|Not recorded|map legend|||Map legend, of Katherine, 1 mile (D53-9).||||||
24525|Tindall Limestone|46792|6|Mentioned|p53|||Stratigraphy||||||
24525|Tindall Limestone|48942|6|Mentioned|p82|||Correlation||||||
24525|Tindall Limestone|60685|5|Briefly described|p19|Middle Cambrian|Middle Cambrian|Lateral correlative of Montejinni Limestone. Geological Province: Daly River Basin.||||||
24525|Tindall Limestone|60990|6|Mentioned|p85|Middle Cambrian|Middle Cambrian|Daly Basin. Faunal links with Antarctica.||||||
24525|Tindall Limestone|62376|5|Briefly described|p38|Cambrian|Cambrian|Geological Province: Beetaloo Sub-Basin.||||||09-FEB-10
24525|Tindall Limestone|62787|6|Mentioned|p82 Fig. 3|Cambrian|Neoproterozoic|Geological Province: Daly Basin (NT).||||||07-FEB-11
24525|Tindall Limestone|63569|6|Mentioned|p123|Cambrian|Cambrian|Daly Basin. Contains lingulate brachiopods that correlate with Redlichia guizhouensis Zone of China.||||||
24525|Tindall Limestone|64816|5|Briefly described|p3 Fig.2|Cambrian|Cambrian||||||Limestone with intervals of siltstone.|
24525|Tindall Limestone|64975|6|Mentioned|p162 Fig.6.|Cambrian|Cambrian|||||||
24525|Tindall Limestone|65236|5|Briefly described|p3 Fig. 3, p4 Fig. 4|Cambrian|Cambrian|Geological province: Beetaloo Sub-basin.||||||04-JUN-09
24525|Tindall Limestone|65337|5|Briefly described|p94.|Middle Cambrian|Middle Cambrian|Daly Basin. Carbonates.||||Unconformably overlies Kalkarindji Volcanic Group.||
24525|Tindall Limestone|65339|5|Briefly described|p5 Fig.4. |||||Unit in Daly River Group.|||Sandstone, limestone.|
24525|Tindall Limestone|65342|6|Mentioned|p8, p9.|||Daly Basin and Beetaloo Sub-basin, Dunmarra Basin. Max. thickness at least 200 m.||||Overlies Jamieson Sandstone. Is overlain by Jinduckin Formation.||14-FEB-17
24525|Tindall Limestone|65344|6|Mentioned|p8, 13|||Of the Daly Basin.||||||
24525|Tindall Limestone|65345|5|Briefly described|p4.|||Daly Basin. Equivalent to the Gum Ridge Formation of western Georgina Basin, and to the Montejinni Limestone/Hooker Creek Formation/Lothari Hill Sandstone sequence in the Wiso Basin.||Unit in Daly River Group.|||Bioclastic, mottled, oncoid and stromatolitic limestone; minor mudstone and basal conglomerate, arkosic sandstone and siltstone.|
24525|Tindall Limestone|67186|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Daly River Group.||Is overlain by Jinduckin Formation.|Limestone, fine-grained, crystalline, dolomitic, and chert with layers of quartz sandstone and siltstone.|23-NOV-11
24525|Tindall Limestone|67352|6|Mentioned|p19|Middle Cambrian|Middle Cambrian|Daly Basin. Contains a widespread (NT-SA-Antarctica) fossil fauna.||||||
24525|Tindall Limestone|69018|6|Mentioned|p450 Fig.1b|||||||||
24525|Tindall Limestone|69418|6|Mentioned|p3:29|||Daly Basin. A number of barite veins occur, eg Mathison Creek deposit.||||||12-JUL-16
24525|Tindall Limestone|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Daly Basin, Centralian B Superbasin. Sequence 1. Shallow-marine to peritidal deposits. Is correlated with Negri Subgroup; Thorntonia, Top Springs Limestones; Tarrara, Gum Ridge, Chandler and Border Waterhole Formations; Walbiri, Giles Creek Dolostones.||||Overlies Jindare Formation and Antrim Plateau Volcanics. Is overlain by Jinduckin Formation.||12-JUL-16
24525|Tindall Limestone|69438|5|Briefly described|p23:29|Middle Cambrian|Middle Cambrian|Daly 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
24525|Tindall Limestone|69443|6|Mentioned|p28:21|||Daly Basin.||||Correlated with Gum Ridge Formation.||12-JUL-16
24525|Tindall Limestone|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Kruse et al. (1994). Daly Basin.||||Unconformably overlies Antrim Plateau Volcanics (Kalkarindji Suite).||12-JUL-16
24525|Tindall Limestone|69446|3|Fully described|p31:1-6, 9|Middle Cambrian|Middle Cambrian|Oldest unit in the Daly Basin; widespread outcrops around its margins. Exposures include rugged karst terrain and isolated residuals. Open shelf marine, minor peritidal deposits. Up to 204m thick; is 180.7m thick in the type section in drillhole NTGS 86/1. Probably continuous with Montejinni Limestone (Wiso Basin) under cover. Strong species-level similarity with correlative faunas of Linnekar Limestone and Panton Formation (Ord Basin), and Montejinni Limestone and Hooker Creek Formation (Wiso Basin). Broadly age-equivalent to Top Springs Limestone, Gum Ridge Formation, Thorntonia Limestone and Border Waterhole Formation (Georgina Basin). Offset by steep normal faults. Is quarried on Elsey Station for quicklime and ground limestone. Contains stratiform and surficial barite deposits, some vein fluorite and insignificant phosphate, and uneconomic base metal occurrences.||Daly River Group.||Unconformably overlies Antrim Plateau Volcanics, Jindare Formation or Roper Group. Is overlain by Jinduckin Formation conformably or locally disconformably.|Grey mottled, oncoid, ribbon and bioclast limestone; minor intercalated maroon-green siltstone or dark grey mudstone, microbial laminite and stromatolitic boundstone. Rich fauna of trilobites, bradoriids, brachiopods, hyoliths, molluscs and sponges.|12-JUL-16
24525|Tindall Limestone|69447|6|Mentioned|p32:2|||Daly Basin. Has strong species-level correlative faunas with Montejinni Limestone and Hooker Creek Formation (Wiso Basin).||||||12-JUL-16
24525|Tindall Limestone|69448|6|Mentioned|p33:3|||Daly Basin.||||Correlated with Negri Subgroup (Ord Basin).||12-JUL-16
24525|Tindall Limestone|69561|5|Briefly described|p31, p32 fig 1, p33 fig 2, p33, p42|Ordian|Ordian|Limestone reef fossils. Trilobites (Redlichia and Xystridura which are age diagnostic), archaeocopides, brachiopods, hyoliths, molluscs and sponges (metazoans).||||Overlies Jindare Formation, Antrim Plateau Volcanics, overlain by Jinduckin Formation|Fossiliferous limestone.|
24525|Tindall Limestone|69673|4|Described|p191|Cambrian|Cambrian |204m thick.||Daly River Group||Overlain by Jinduckin Formation|Fossiliferous oncoid, ribbon and bioclast limestone with minor intercalated siltstone or mudstone, microbial laminite and stromatolitic boundstone.|
24525|Tindall Limestone|70380|4|Described|p743-746, p759|Middle Cambrian|Middle Cambrian|Daly Basin. Up to 204m thick. Ordian age from diagnostic trilobites Redlichia and Xystridura. Correlated with Top Springs and Thorntonia Limestones, and Gum Ridge and Border Waterhole Formations, of the Georgina Basin; also with Lothari Hill Sandstone, Hooker Creek Formation and Montejinni Limestone of the Wiso Basin. Shallow-marine to peritidal sediments. The upper surface represents a (carbonate-to-siliciclastic) major sequence boundary.||Daly River Group.||Unconformably overlies Antrim Plateau Volcanics or Jindare Formation, or Roper Group in the SE. Is overlain conformably (possibly locally disconformably) by Jinduckin Formation.|Grey mottled, oncoid, ribbon and bioclast limestone, with minor intercalated maroon-green siltstone or dark grey mudstone, microbial laminite and stromatolitic boundstone; richly fossiliferous.|
24525|Tindall Limestone|70752|6|Mentioned|p141|Cambrian|Cambrian|Daly Basin. Brachiopod species discussed. Series 2, Stage 4 (Ordian) age.||||||
24525|Tindall Limestone|70850|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.|||Limestone and dolomitic limestone.|
24525|Tindall Limestone|70866|5|Briefly described|Map legend.|Cambrian|Cambrian|Daly Basin.||Daly River Group.||Is overlain conformably by Jinduckin Formation.|Part-dolomitised limestone with silt laminations, interbedded calcilutite and marl; bioclastic limestone, mudstone and siltstone; minor stromatolitic boundstone and cryptalgal laminite; local bioclastic grainstone, arkosic sandstone and conglomerate.|
24525|Tindall Limestone|70968|6|Mentioned|p75|Cambrian|Cambrian|Fence diagram of wells in Beetaloo Sub-basin.||||||
24525|Tindall Limestone|72718|6|Mentioned|p10, p14|Cambrian|Cambrian|Strongly disrupts seismic signals.|||||Karstic, partially-dolomitised limestone.|
24525|Tindall Limestone|73083|6|Mentioned|p16, p29-30|Cambrian|Cambrian|Daly and Wiso Basins.||||||
24526|Tinfish Sandstone|23733|6|Mentioned|p9|Paleoproterozoic|Paleoproterozoic|See also p32 Fig. 19.||||||07-NOV-08
24526|Tinfish Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Wauchope Subgroup (lower part).  Geological Province: Arunta Province.||||||
24526|Tinfish Sandstone|42643|2|Defined|p49||Paleoproterozoic|Of Wauchope Subgroup (Hatches Creek Group). Reserved. Definition card available.||||||05-JAN-17
24526|Tinfish Sandstone|42644|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Feldspathic/micaceous/lithic arenite, quartz arenite, feldspathic quartz-biotite schist.||||||07-NOV-08
24526|Tinfish Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Lower Wauchope Subgroup (Hatches Creek Gp). Overlies Gwynne Sandstone.  In Tennant Creek region. Lithology not presented.||||||07-NOV-08
24526|Tinfish Sandstone|64735|5|Briefly described|p206 Fig 2, p206, p216 Fig15,|Orosirian|Orosirian|Barrow Creek area, Aileron Province. Correlated with Hatches Creek Group, Ongeva Package, Ware Group.|||||Siliciclastic sedimentary rocks.|30-APR-12
24526|Tinfish Sandstone|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup.||Wauchope Subgroup||||05-JAN-17
24526|Tinfish Sandstone|65338|6|Mentioned|p20.|||Correlative with Yeeradgi Sandstone.||Unit in Wauchope Subgroup.||||
24526|Tinfish Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Shown as overlying Gwynne Sandstone, and lateral equivalent of Strzeleckie Volcanics. Shown as disconformably overlain by Illoquara Sandstone.||08-DEC-14
24526|Tinfish Sandstone|69425|4|Described|p10:3, 10-11, 13, 15|Statherian|Statherian|NW Osborne Range. Similar association of rock types to the Yeeradgi Sandstone. Maximum thickness 400m. Predominantly fluvial deposits with contemporaneous or penecontemporaneous volcanism.||Wauchope Subgroup, lower.||Conformably overlies and partly interfingers with Strzeleckie Volcanics. Is overlain disconformably by Illoquara Sandstone. Correlated with Yeeradgi Sandstone (in part?).|Feldspathic/micaceous sandstone, quartz sandstone, feldspathic quartz-biotite schist.|12-JUL-16
24526|Tinfish Sandstone|69427|5|Briefly described|p12:13|||Probably derived from local reworking of the Strzeleckie Volcanics in a fluviatile environment. Also appears, in the same paragraph, as Tin Fish Sandstone.||Wauchope Subgroup.||Conformably overlies, and interdigitates with, Strzeleckie Volcanics. Correlated with Yeeradji Sandstone.||12-JUL-16
24526|Tinfish Sandstone|69431|6|Mentioned|p16:5|||Osborne and Crawford Ranges.||Wauchope Subgroup.||||12-JUL-16
42374|Tinki Granite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Coarse-grained, unfoliated, equigranular to porphyritic biotite granite.  Age: 1690Ma.  Geological province: Arunta region.||||||07-NOV-08
42374|Tinki Granite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1690Ma. Biotite granite. Geological Province: Warumpi Province||||||07-NOV-08
42374|Tinki Granite|68832|5|Briefly described|p45-49|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Confidently interpreted as crystallisation age.|1691+/-4 Ma||||Undeformed coarse-grained, weakly porphyritic biotite monzogranite.|
42374|Tinki Granite|69417|6|Mentioned|p2:5|Statherian|Statherian|Kintore Domain, Warumpi Province.||||||12-JUL-16
42374|Tinki Granite|69428|5|Briefly described|p13:3, 12, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. SHRIMP U-Pb zircon age.|1691 +/- 4 Ma (Cross et al., 2005).|||Is overlain by Walungurru Volcanics.|Undeformed biotite granite and quartz monzonite, typically coarse-grained, equigranular to porphyritic (K-feldspar phenocrysts to 4cm); mafic xenoliths common; intruded by fine-grained to microcrystalline felsic dykes.|12-JUL-16
42374|Tinki Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
42374|Tinki Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1691+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Biotite monzogranite.|
42374|Tinki Granite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain. Geochron Sample No: MR01IRS44. Location: 558618E, 7424891.|1690 Ma||||Coarse grained, unfoliated equigranular to porphyritic biotite granite.|09-SEP-19
36772|Tjauwata Group|24442|5|Briefly described|p28, p29|||Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Age: 1080-1050 Ma. Volcanics and sediments deposited in a regional zone of transtensile shear. Equivalent to the Bentley Supergroup. Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|24497|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
36772|Tjauwata Group|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes: Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Puntitjata Rhyolite, Bloods Range Formation.||||||09-JUN-04
36772|Tjauwata Group|60660|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Bimodal volcanics and sediments. Equivalent to the Bentley Supergroup.||||||22-FEB-05
36772|Tjauwata Group|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes: Bloods Range Formation, Puntitjara Rhyolite, Mount Harris Basalt, Tjuninanta Formation and Wankari Volcanics.  Geological Province: Musgrave Block.||||||
36772|Tjauwata Group|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Includes metasediments, rhyolite and basalt. Geological Province: Musgrave Block.||||||14-JAN-05
36772|Tjauwata Group|61154|4|Described|p16, p3, p5 Tb. 1.|Mesoproterozoic|Mesoproterozoic|Comprises basal Karukali Qtzite, deformed sediments and bimodal volcanics which include: mafic and felsic volcanics; felsic tuffs; interlayered mafic volcancis; felsic volcanics; volcaniclastic sediments and quartz. Age: 1090-1040Ma. Geol.Prov: Musgrave Bl.||||||05-AUG-14
36772|Tjauwata Group|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Karukali Quartzite, Tjuninanta Formation and Mount Harris Basalt.||||||11-DEC-06
36772|Tjauwata Group|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Part of rift sequence along with Wankari Volcanics and Bloods Range Beds. Geological Province: Musgrave Province.||||||02-JUN-06
36772|Tjauwata Group|61733|5|Briefly described|p46|||Emplaced during the Warakurna igneous event at c.1.08-1.05 Ga.|||||Bimodal volcanics and associated rift sediments.|
36772|Tjauwata Group|61864|6|Mentioned|p18 fig 4|||Part of a rift sequence.||||||
36772|Tjauwata Group|62989|5|Briefly described|p39, p40|Mesoproterozoic|Mesoproterozoic|Age: 1090-1040Ma. Includes Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Bloods Range Formation and Wankari Volcanics. Overlain by Dean Quartzite.  Geological Province: Amadeus Basin. Hosts small Cu prospects.||||||05-AUG-14
36772|Tjauwata Group|63562|6|Mentioned|p341|Stenian|Stenian|Of Amadeus Basin.|c.1090-c.1040 Ma (Close et al., 2005).||Includes Mount Harris Basalt, Bloods Range beds and Dixon Range beds.|Correlated with Tollu Group.|Relatively thin package of sedimentary and bimodal volcanic rocks.|
36772|Tjauwata Group|63866|4|Described|p202-p203, p205-p206, p208, p212|Stenian|Stenian|Mulga Park Domain, Musgrave Province.||Bentley Supergroup|Includes the Tjuninata Formation, Mount Harris Basalt and the Puntitjata Rhyolite.||Sediments and bi-modal volcanics.|
36772|Tjauwata Group|64580|6|Mentioned|map legend|||||||||
36772|Tjauwata Group|64722|6|Mentioned|p17|Stenian|Stenian|Equivalent of Tollu Group therefore Stenian age inferred.||||||
36772|Tjauwata Group|64745|5|Briefly described|p373 Fig. 3|||Geol. Prov: Mulga Park Domain, Musgrave Province. See also name variations: Supercrustal, Supercrustals and supracrustal.||||||
36772|Tjauwata Group|65135|5|Briefly described|p16, p17|Stenian||Sequence of supracrustal rocks with a similar lithological range to Kunmarnara and Tollu Groups. Straddles WA and NT border. Unconformably underlies basal sedimentary rocks of Amadeus Basin. Includes Puntitjata Rhyolite, dated at 1075 +/- 3 Ma.||||||
36772|Tjauwata Group|65233|5|Briefly described|p2|||Thick package of sediments and volcanics unconformably overlies basement Musgrave Province.  Geological province: Amadeus Basin.||||||07-FEB-11
36772|Tjauwata Group|65256|2|Defined|piii, p8, p14 Fig. 10, p37|Tonian|Mesoproterozoic|New Name. Lower section equivalent to Bloods Range beds. >1km thick. Middle section intruded by Rowley Granophyre and Walu Granite. Correlative of Tollu Group; intruded by Hull Granite Suite and Alcurra dolerite.|1075+/-2.5 Ma (Pb-Pb zircon).||Includes Karukali Quartzite, Tjuninanta Formation, Mount Harris Basalt, Puntitjata Rhyolite, Bloods Range Formation.|Unconformably overlies Pottoyu Granite Suite; disconformably underlies Kulail Sandstone and Dean Quartzite;|Voluminous mafic volcanics, minor felsic volcanics, polymictic conglomerate, red beds and quartzite (elaborated in text).|24-MAR-15
36772|Tjauwata Group|65338|6|Mentioned|p59.|||Southwestern Amadeus Basin. Rift succession. |1090 - 1040 Ma.|||||
36772|Tjauwata Group|65385|5|Briefly described|pS132|Stenian|Stenian|In western Musgrave Province. ~1090-1040 Ma.||||||08-MAR-12
36772|Tjauwata Group|65833|5|Briefly described|p16|Stenian||Unconformably overlain by Amadeus Basin sediments. Similar lithological range to Kunmarnara and Tollu Groups. Straddles WA and NT border. Includes Puntitjata Rhyolite and Wankari Volcanics.||||||
36772|Tjauwata Group|65906|5|Briefly described|p6, p19-20|Mesoproterozoic|Mesoproterozoic|A package of deformed sediments and bi-modal volcanics: basal quartzite and conglomerate, basalt overlain by rhyolites and epiclastic sediments. Considered a correlative of the Bentley Supergroup volcanics and associated sediments. Depositional age of Puntitjata Rhyolite member: 1075 +/- 3 Ma (Edgoose et al., 2004). Includes Mount Harris Basalt and Wankari Volcanics.||||||
36772|Tjauwata Group|67128|5|Briefly described|p3, p18, p30|||Western Bloods Range. Basement to Amadeus Basin.|||KaruKali Quartzite, Mount Harris Basalt, Puntitjata Rhyolite, Wankari Volcanics.|||
36772|Tjauwata Group|67375|5|Briefly described|p7 Fig.4, p16 Fig.10, p41, p217, p230.|Mesoproterozoic|Mesoproterozoic|Incorporated and replaces the Bloods Range Beds and the Mount Harris Volcanics. A sequence of supracrustal rocks straddling the WA/NT border; correlated with Tollu Group.|1085 - 1040 Ma (Edgoose et al. 2004).||Includes Puntitjata Rhyolite.||Sequence of volcanic, volcaniclastic and clastic rocks.|
36772|Tjauwata Group|67553|5|Briefly described|p8,17,43,59|Stenian|Stenian|Geological province: Musgrave Province, North Australian Craton. Supracrustal sequence with similar lithological range to the Kunmarnara anf Tollu groups.||||Equivalent to Bentley Supergroup.||
36772|Tjauwata Group|67565|5|Briefly described|p38.|Stenian|Stenian|A rift succession in the southwestern Amadeus Basin.|1090-1040 Ma.|||||
36772|Tjauwata Group|68994|5|Briefly described|p18|||Underlies the southwestern Amadeus Basin.|1090-1040 Ma (Close et al. 2004).|||||13-JAN-17
36772|Tjauwata Group|68995|5|Briefly described|p3 Fig.1, p4 Fig.2, p5, p22|Stenian|Stenian|Bloods Range area. |c. 1075 Ma|Bentley Supergroup|Karukali Quartzite, Mount Harris Basalt||Intrusive and extrusive mafic rocks.|
36772|Tjauwata Group|68996|6|Mentioned|p5, p36, p45, 47, p48, p69|Mesoproterozoic|Mesoproterozoic|Depositional age range indicated.|1090-1040 Ma|||||
36772|Tjauwata Group|69003|6|Mentioned|p37|Mesoproterozoic|Mesoproterozoic|W Musgrave Province.||||||
36772|Tjauwata Group|69091|4|Described|p52 Fig.4.1, p58, p69-70, see comments|||In area to north and east of Warakurna and continuing into Northern Territory (Bloods Range area). See also p84, p88, p105, p106 Fig.5.7a,b, p107 Fig.5.8a, p109 Fig.5.10, p131 Fig.6.1, p136, p137-139 Figs.6.4-6.6.|||Karukali Quartzite, Mount Harris Basalt.|Equivalent to Kunmarnara Group; overlies Pitjantjatjara Supersuite.|Supracrustal rocks, bimodal volcanics.|11-JUL-16
36772|Tjauwata Group|69153|6|Mentioned|500k_geologyp08_lut.csv||||||Bloods Range Formation, Mount Harris Basalt|||
36772|Tjauwata Group|69436|4|Described|p21:1-4, 11-14, 19, 21|Mesoproterozoic|Mesoproterozoic|Close et al. (2003). Crops out between the Petermann Ranges and Bloods Range, northern Musgrave Province. Extrusive equivalent of the Giles Complex. The felsic volcanic rocks form a highly fractionated suite from a common source. Is structurally interleaved with Dean Quartzite in the Wankari Detachment Zone of the Petermann Nappe Complex. Hosts a few occurrences of secondary Cu minerals but with insignificant mineralisation at depth. Is a potential target for red-bed Cu mineralisation. Quartz veins and soil samples show encouraging Au anomalies.|1090-1040 Ma.||Karukali Quartzite; Tjuninanta, Bloods Range Formations; Mount Harris Basalt; Puntitjata Rhyolite; Wankari Volcanics.|Is intruded by Hull Suite. Is broadly correlated with Bentley Supergroup.|A package of deformed quartz-rich and volcanigenic sedimentary rocks, epiclastic rocks, and bimodal volcanic rocks. A-type.|12-JUL-16
36772|Tjauwata Group|69437|5|Briefly described|p22:12|||Musgrave Province. Interpreted as a rift-related succession.|1090-1040 Ma.|||||12-JUL-16
36772|Tjauwata Group|69438|5|Briefly described|p23:2, 8-9|||A rift succession underlying the SW Amadeus Basin.|1080-1050 Ma (Close et al., 2004).||Bloods Range Formation.|||12-JUL-16
36772|Tjauwata Group|69606|5|Briefly described|p4 fig 2, p5|Mesoproterozoic|Mesoproterozoic|Amadeus Basin.|||Dixon Range beds, Wankari Volcanics.||Sandstone.|15-SEP-22
36772|Tjauwata Group|69655|5|Briefly described|p3|Stenian|Stenian||c. 1090-1040 Ma|||||
36772|Tjauwata Group|69729|6|Mentioned|p66 Fig.1, p70, p79|||Bentley Basin: Bloods Range area in NT.||||||
36772|Tjauwata Group|69937|5|Briefly described|vi, p7, p9, p16, p28, ;p34|||Musgrave Province. One of the sediment sources for the Amadeus Basin.|1085-1040 Ma.||||Sedimentary and volcanic rocks.|
36772|Tjauwata Group|70018|4|Described|p233,235-236,239-240|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Extension and deposition occurred after initial uplift of Musgrave Block. Prominent erosional and angular unconformity with the overlying Kulail Sandstone and Dean Quartzite suggest a major basin reorganisation.|||Includes Bloods Range Formation, Wankari Volcanics, Puntitjata Rhyolite, Mount Harris Basalt, Tjuninanta Formation and Karukali Quartzite.||Bimodal volcanic sand coarse-grained siliciclastic rocks including conglomerates.|
36772|Tjauwata Group|70083|6|Mentioned|p206|||Musgrave Inlier.|1085-1020? Ma.||||Volcanic, pyroclastic and sedimentary rocks.|
36772|Tjauwata Group|70634|6|Mentioned|500k_geolgyp08_lut.csv|Mesoproterozoic|Mesoproterozoic||||Includes Bloods Range Formation, Mount Harris Basalt|||
36772|Tjauwata Group|70793|4|Described|GEOL_LUT_CSV files|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). See 500k_interpgeop14_lut.csv, 2_5m_interpgeop15_lut.csv.|1085-1040 Ma (inferred)|Unit of Bentley Supergroup.|Includes Bloods Range Formation, Mount Harris Basalt.||Metamorphosed sandstone and siltstone, and felsic and mafic schist derived from volcanic rock|
36772|Tjauwata Group|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Bentley Basin. ||Bentley Supergroup||||
36772|Tjauwata Group|70831|5|Briefly described|p3|||Bentley Basin.||||||
36772|Tjauwata Group|70839|5|Briefly described|p326-332,345|Mesoproterozoic|Mesoproterozoic|Geological province: Musgrave Province. Of Bentley Basin. Exposed along NW margin of Musgrave region and in inliers in SW Amadeus Basin (Edgoose et al., 2004) and as part of 30-60km wide belt of ranges immediate south of southern limit of Supersequence 4 deposits (this study). Emplaced within Ngaanyatjarra Rift (Evins et al., 2010; Aitken et al., 2012).|||Includes Dixon Range beds and Bloods Range Formation.|Overlain unconformably by Dean Quartzite and Kulail Sandstone, locally by Dixon Range beds.||
36772|Tjauwata Group|71080|6|Mentioned|p30 fig 21|Mesoproterozoic|Mesoproterozoic|Underlies Amadeus Basin in WA.|||||Dominantly sandstone.|
36772|Tjauwata Group|71088|5|Briefly described|p4, p6-p8|||Amadeus Basin. Deposited within the structural Ngaanyatjara Rift.||Bentley Supergroup|Includes the Dixon Range beds.|Equivalent to the Kunmarnara Group.||
36772|Tjauwata Group|71170|5|Briefly described|p5|||||||||
36772|Tjauwata Group|71210|5|Briefly described|p4-p5, p8-p9, p21, p51, p79, p113|||Musgrave Province.|c. 1090 Ma (Edgoose et al., 2004)||Includes the Mount Harris Basalt, Puntitjata Rhyolite and Wankari Volcanics.|||
36772|Tjauwata Group|71211|6|Mentioned|p6 fig 1.3, p7 fig 1.4|||See also p24 fig 2.1, p84 fig 3.1, p136 fig 4.1 , p233. ||Bentley Supergroup|Includes the Smoke Hill Felsic Volcanic and the Wankari Volcanics.|||
36772|Tjauwata Group|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Late-stage component of the Bentley Supergroup. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeol_lut.csv.|1073+\-7 Ma; 1026+\-26 Ma|Unit of Bentley Supergroup.|Includes Bloods Range Formation, Dixon Range Formation, Karukali Quartzite, Mount Harris Basalt, Puntitjata Rhyolite, Tjuninanta Formation, Wankari Volcanics, Warrupura Formation.|Underlain by Pitjantjatjara Supersuite.|Siliciclastic sedimentary and volcanic rocks; locally metamorphosed|
36772|Tjauwata Group|71279|6|Mentioned|p353|||Musgrave Province. Source of c.1.3 to 0.8 Ga zircons in Pertatataka Formation.||||||
36772|Tjauwata Group|71321|6|Mentioned|p5|||Geological province: Musgrave Province.||||||
36772|Tjauwata Group|71344|6|Mentioned|p1093|Stenian|Stenian|Marks initiation of Amadeus Basin?|~1080 Ma||||Bimodal volcanics and sedimentary rocks.|
36772|Tjauwata Group|71810|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Bentley Basin.|c.1044 Ma - c.1039 Ma.|||Is overlain by Heavitree Formation.|Siliciclastic metasedimentary and volcanic rocks; locally metamorphosed (section only).|
36772|Tjauwata Group|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup|Includes Mount Harris Basalt, Bloods Range Formation.||Metamorphosed siliciclastic sedimentary and volcanic rocks.|
36772|Tjauwata Group|72094|5|Briefly described|p3 Fig 2, p7-8, 17, 18|Stenian|Mesoproterozoic|Bentley Basin. Variably deformed rhyolitic subvolcanic rocks. Magmatic crystallisation ages: 1041+/-6 Ma, 1039+/-7 Ma. Summary table of zircon geochronology on p8 Table 1.||Unit of Bentley Supergroup.|Includes Karulaki Quartzite and Mount Harris Basalt.|Strongly folded ridges of Dean Quartzite interleaved with Tjauwata Group rhyolite-dominant rocks. Equivalent to Kunmarnara Group.|Includes variably deformed rhyolitic sub-volcanic rocks.|
36772|Tjauwata Group|72375|5|Briefly described|p5|Stenian|Stenian|Of Amadeus Basin.|c. 1090-1040 Ma|||Overlain by Dean Quartzite.||
36772|Tjauwata Group|72443|6|Mentioned|p737|||Bentley Basin.||||||
36772|Tjauwata Group|73086|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Amadeus Basin, southwest. Preserves a Neoproterozoic succession that represents the initial basin-forming rifting event.||||||
36772|Tjauwata Group|73437|6|Mentioned|p151|Mesoproterozoic|Mesoproterozoic|Bentley Basin.||Bentley Supergroup||||
36773|Tjuninanta Formation|50286|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||31-MAY-04
36773|Tjuninanta Formation|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group.||||||28-MAY-04
36773|Tjuninanta Formation|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Amygdaloidal basalt, quartzite, phyllitic schist, volcaniclastics. Geological Province: Musgrave Block.||||||
36773|Tjuninanta Formation|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Basalt, quartzite schist, volcaniclastics. Of Tjauwata Group. Geological Province: Musgrave Block.||||||
36773|Tjuninanta Formation|61154|5|Briefly described|p16, p18 Fig. 10|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Gp. Comprises interbedded siliciclastic seds., volcaniclastics, phyllitic schist, mafic and felsic volcanics. Secondary Cu minerals occur in sheared basalt and schistose sediments of this unit. Overlies Karukali Q'tzite; under Mt Harris Basalt||||||
36773|Tjuninanta Formation|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Interlensed silicified epidotised amygdaloidal basalt, quartzite, quartz-muscovite schist and dark grey phyllitic schist, and volcaniclastics.||||||
36773|Tjuninanta Formation|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Predominantly quartz-rich sediments, volcaniclastic sediments and bimodal volcanics. Overlain by Mount Harris Basalt.||||||25-JAN-10
36773|Tjuninanta Formation|65233|5|Briefly described|p2|||Of Close et al (2005). Overlain by Mount Harris Basalt. Geological province: Amadeus Basin. Quartz-rich sediments, volcaniclastic sediments and bimodal volcanics.||||||07-FEB-11
36773|Tjuninanta Formation|65256|2|Defined|p6 Tb.1, p9-10, p14-15, p37, p38|Stenian|Stenian|New name. Formerly part of Bloods Range beds and Mount Harris Basalt. May be equivalent to Glyde Formation. Mis-spelt as Tjuntinanta Formation in Table 1, p6.||Of the Tjauwata Group.||Underlies Mount Harris Basalt - gradational contact; conformably overlies Karukali Quartzite; intruded by Rowley Granophyre.|Interlensed succession of silicified epidotised amygdaloidal basalt (pillows); quartzite, quartz muscovite schist, dark grey phyllitic schist, quartz sandstone and rare diagenetic chert; and volcaniclastics/felsic volcanics.|19-MAY-14
36773|Tjuninanta Formation|69436|5|Briefly described|p21:4, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Shallow-water deposits. There is no equivalent succession in the Blackstone Sub-basin.||Tjauwata Group.||Overlies Karukali Quartzite. Is overlain by Mount Harris Basalt.|Interlayered basalt (some pillows and hyaloclastite), epiclastic rocks, felsic volcanic rocks, quartz sandstone, quartzite, phyllite and rare diagenetic chert. Highly strained, with a pervasive schistose fabric.|12-JUL-16
36773|Tjuninanta Formation|70018|4|Described|p233,235-239|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. Detrital zircon age distribution is predominantly Musgravian, with groupings at 1035 ¿ 13 Ma, 1110 ¿ 49 Ma, and1169 ¿ 30 Ma, and significantly, very minor >1600 Ma zircons, which are common in the Arunta region.||Unit of Tjauwata Group.||Overlain by Mount Harris Basalt. Underlain by Karukali Quartzite.|Metamorphosed interbedded sedimentary rocks, volcaniclastic rocks, and mafic and felsic volcanic rocks. Quartz-muscovite schist, muscovite-bearing quartzites. Minor metamorphosed quartz and lithic sandstones, dark-grey shale, and rare black cherts.|
36773|Tjuninanta Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||quartzite, basalt, schist, volcaniclastic rock|
36773|Tjuninanta Formation|71268|4|Described|1m_geologyp12_lut.csv|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin.||Unit of Tjauwata Group.|||Intercalated, silicified, epidotised amygdaloidal basalt; quartzite, quartz-muscovite schist and dark grey phyllitic schist; volcaniclastics.|
37740|Tobacco Member|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the Mittiebah Sandstone?  Age: <1450Ma.||||||11-DEC-06
37740|Tobacco Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Crow Formation. White, silicified, fine to very coarse grained to pebbly, quartzose to lithic sandstone and local pebble to cobble conglomerate; minor glauconitic sandstone, interbedded shale and siltstone.||||||
37740|Tobacco Member|65337|2|Defined|p9 Fig.5, p38 Table 5.|Mesoproterozoic|Mesoproterozoic|Northwest MOUNT DRUMMOND area. Shallow intertidal to storm-influenced marine shelf. 300 - 600 m of stacked sandstone units. Outcrops as banded white to pale red-brown resistant strike ridges.||Unit in Crow Formation.||Overlies Crow Formation. Is overlain disconformably or unconformably by Mittiebah Sandstone.|White, silicified, fine- to very coarse-grained +/- pebbly, quartzose to lithic, often glauconitic sandstone and local pebble-cobble conglomerate; minor interbedded white flaggy shale and siltstone.|
37740|Tobacco Member|69434|4|Described|p19:2, 5|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. 300-600m thick. Shallow intertidal to storm-influenced marine shelf deposits.||Crow Formation.||Is overlain by Mittiebah Sandstone disconformably or unconformably.|White, silicified, fine to very coarse +/- pebbly, quartzic to lithic, often glauconitic sandstone and localised pebble-cobble conglomerate; minor interbedded shale and siltstone.|12-JUL-16
37740|Tobacco Member|71369|5|Briefly described|p6|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin.||Crow Formation.||||
37740|Tobacco Member|72526|5|Briefly described|p8 Fig.1.3, p56|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Crow Formation||Is conformably to disconformably overlain by Mittiebah Sandstone.||
37740|Tobacco Member|72527|6|Mentioned|p7 Fig.1.4.|Mesoproterozoic|Mesoproterozoic|||Top of Crow Formation, Wild Cow Subgroup||Unconformably underlies Mittiebah and Constance Sandstones.||
37740|Tobacco Member|72912|6|Mentioned|p5 Fig.3.|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin.||Crow Formation||||
37740|Tobacco Member|72919|4|Described|p1, p4-5, p70, p85-89, p97-98|Calymmian|Statherian|Forms comparatively resistant strike ridges in the Mittiebah and Canyon Ranges. The type section is defined by Rawlings et al. (2008) in the central Mittiebah Range where it is 300-600 m thick. Low angle trough beds and hummocky cross-stratification (HCS; indicative of storm action) are common. Interpreted as a shallow-water to tidal and storm influenced marine shelf depositional environment. A new U-Pb SHRIMP zircon maximum depositional age of 1591 +/- 7 Ma was reported from the Canyon Range area, which contrasts with the late Paleoproterozoic age at the measured section in the Mittiebah Range area (Kositcin and Carson, 2019).|1591 +/- 7 Ma U-Pb SHRIMP|Crow Formation, Wild Cow Subgroup, South Nicholson Group||Conformably to disconformably overlain by Mittiebah Sandstone and Constance Sandstone (Accident Subgroup).|Diffusely bedded, quartz to lithic, locally ferruginous (+/-micaceous; +/-glauconitic), fine- to medium-grained sandstone with interbedded white tabular shale and siltstone, and local pebble to cobble conglomerate lags.|
37740|Tobacco Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Crow Formation, Wildcow Subgroup, South Nicholson Group||Underlain(?) by No Mans Sandstone Member.||
37740|Tobacco Member|73043|6|Mentioned|p7 Fig.2|Paleoproterozoic|Paleoproterozoic|Not shown what Formation this unit is a member of.||Benmara Group||||
69015|Todd River Dolostone|60122|5|Briefly described|p14|Early Cambrian|Early Cambrian|Contains archaeocyaths, brachiopods, hyoliths, molluscs, fragmentary echinoderms and problematical skeletal fossils which are of Atdabanian age in Siberian terms. Geological Province: Amadeus Basin.||||||23-MAY-05
69015|Todd River Dolostone|62376|5|Briefly described|p18|Middle Cambrian|Early Cambrian|Of the Pertaoorrta Group. Geological Province: Amadeus Basin.||||||09-FEB-10
69015|Todd River Dolostone|62379|5|Briefly described|p24|||||||||
69015|Todd River Dolostone|64068|5|Briefly described|p36, 38, 57, 224|Early Cambrian|Early Cambrian|Amadeus Basin. Faunal similarity with Red Heart Dolostone of Georgina Basin may indicate extensive contiguous deposition during the Cambrian.||||||
69015|Todd River Dolostone|64778|6|Mentioned|p13, 16-17, 20|Cambrian|Cambrian|Amadeus and Pedirka Basins. Max. palaeotemperature analysis summary.||||||
69015|Todd River Dolostone|64797|6|Mentioned|p153 Fig.2|Cambrian|Cambrian|Amadeus Basin. Lithology not shown in diagram.||||||
69015|Todd River Dolostone|64809|5|Briefly described|p2, p3 Fig.2, p15 Fig.15 |Middle Cambrian|Early Cambrian||||||Pink dolostone, sandstone, siltstone|
69015|Todd River Dolostone|65233|5|Briefly described|p3 Fig. 2, p7|Early Cambrian|Early Cambrian|Of the Pertaoorrta Group. Forms cap over Upper Arumbera Sandstone. Geological province: Amadeus Basin. Shallow marine carbonate rocks.||||||07-FEB-11
69015|Todd River Dolostone|65342|6|Mentioned|p4, p10.|||Amadeus and Eromanga Basins. Max. thickness at least 23 m.||||Overlies Arumbera Sandstone. Is overlain by Chandler Formation.||
69015|Todd River Dolostone|67326|5|Briefly described|p2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||Overlies Arumbera Sandstone.||
69015|Todd River Dolostone|68323|6|Mentioned|p4 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
69015|Todd River Dolostone|69437|5|Briefly described|p22:10|Cambrian|Cambrian|Amadeus Basin.||||Overlies Arumbera Sandstone.||12-JUL-16
69015|Todd River Dolostone|69438|4|Described|p23:2-3, 6, 8, 24-25, 27-28, 43, 55|Early Cambrian|Early Cambrian|Formerly Todd River Dolomite; Wells et al. (1967). Eastern Ooraminna Sub-basin, Amadeus Basin. Up to c.155m thick. Six distinct lithofacies are recognised. Atdabanian to Botomian age from archaeocyathids. Contains phosphatic calcareous silty shale at the RR2 prospect.||Pertaoorrta Group.||Overlies and interfingers with Arumbera Sandstone. Probably equivalent to Namatjira Formation. Is overlain disconformably by Giles Creek Dolostone.|A succcession of thickly bedded, archaeocyathan-rich dolostone, and overlying thinly bedded sandstone, siltstone, mudstone and dolostone. Contains archaeocyathids, small shelly fossils, inarticulate brachiopods, molluscs, hyoliths and problematica.|12-JUL-16
69015|Todd River Dolostone|69443|5|Briefly described|p28:14-16|Early Cambrian|Early Cambrian|NE Amadeus Basin. Contains reef-building archaeocyaths of late Atdabanian stage (Stage 3).||||Correlated with Red Heart Dolostone (Shadow Group).||12-JUL-16
69015|Todd River Dolostone|69449|5|Briefly described|p34:2 Fig.34.2; 34:3-5|Cambrian|Cambrian|Eastern Amadeus Basin. Has a dolostone-limestone equivalent in the western Warburton Basin, based on similar faunal assemblage, archaeocyathids and other shallow marine remains.|||||Includes laminated calcareous siltstone, laminated red siltstone and fine sandstone.|12-JUL-16
69015|Todd River Dolostone|69673|6|Mentioned|p64 fig 53, p65, p88, p91, p149,|||Potential reservoir rock.||||Overlies Arumbera Sandstone||
69015|Todd River Dolostone|70752|5|Briefly described|p125-126, p140|Middle Cambrian|Middle Cambrian|Contains Series 2, Stage 3 brachiopods.||Pertaoorrta Group.||Is overlain disconformably by Giles Creek Dolostone.|Fossiliferous pink dolostone with minor sandstone and siltstone.|
69015|Todd River Dolostone|70833|5|Briefly described|p204|Cambrian|Cambrian|Of Amadeus Basin. Broadly coeval with Red Heart Dolostone. Richly fossiliferous (reference to a type section for the TR Dolostone made, but not actually given), containing acritarchs associated with M. etheridgei zone, as well as abundant other faunal assemblages indicating a lower Cambrian age, and correlation to the M. etheridgei zone stratigraphy of Arrowie Basin.|||||Thinly bedded calcareous sandstones interbedded with thin dolostone beds.|
69015|Todd River Dolostone|71102|6|Mentioned|p260|||Of Amadeus Basin.||||||
69015|Todd River Dolostone|71114|4|Described|p171, p170 fig 1b, p172-3, p178-179|Series 2|"Paranetrelytron" halosa upper (7ci) Subzone|Restricted to the north-eastern Amadeus Basin. Age: Cambrian Series 2, Stage 3, based on archaeocyathids and brachiopods and correlation to adjacent basins. Represents the onset of marine transgression.|~521-517 Ma|||Conformably overlies Arumbera Sandstone. Is overlain by Chandler Formation.|A sequence of interbedded sandstones, siltstones and dolostones.|14-FEB-18
69015|Todd River Dolostone|71279|5|Briefly described|p355 Fig.2|Early Cambrian|Early Cambrian|Amadeus Basin.||Pertaoorrta Group.||||
69015|Todd River Dolostone|71841|5|Briefly described|p1|Early Cambrian|Early Cambrian|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by, and grades inro Arumbera Sandstone.||
69015|Todd River Dolostone|71842|5|Briefly described|p3|Early Cambrian|Early Cambrian|Of Amadeus Basin.||Unit of Pertaoorrta Group.||Underlain by Arumbera Sandstone.||
69015|Todd River Dolostone|72358|6|Mentioned|p118|Series 2|Ediacaran|Of Amadeus Basin.||||||
69015|Todd River Dolostone|72516|6|Mentioned|p90|Cambrian|Cambrian|Amadeus Basin. Contains identical archaeocyathan fossil fauna to the Red Heart Dolostone.||||||02-JUN-21
69015|Todd River Dolostone|73085|6|Mentioned|p1|early Cambrian|early Cambrian|||||Underlain by and equivalent to Arumbera Sandstone. Unconformably overlain by Giles Creek Dolostone.||
69015|Todd River Dolostone|73281|6|Mentioned|p1, Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
27070|Tollis Formation|9538|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the El Sherana Group.  Interbedded greywacke, siltstone, pale green argillite; minor cherty tuff, metamudstone, conglomerate, banded iron formation.||||||
27070|Tollis Formation|23119|5|Briefly described|p433|||||||||
27070|Tollis Formation|23120|5|Briefly described|p428|||||||||
27070|Tollis Formation|23216|4|Described|p6,11-2,39,50||Orosirian|Age: SHRIMP U-Pb 1890 (+/-) 18-15 Ma - ?inherited component, thus ~ 1870 Ma.||||||
27070|Tollis Formation|23384|6|Mentioned|Fig 27|||Also shown as El Sherana Group by Needham and Stuart-Smith (1985).||||||
27070|Tollis Formation|23733|5|Briefly described|p32 Fig. 19|||Of Finniss River Group.||||||
27070|Tollis Formation|23867|5|Briefly described|Fig. 3|||Now of the Finniss Group; formerly of the El Sherana Group.  Geological Province: McArthur Basin.||||||
27070|Tollis Formation|24047|6|Mentioned|p108 Appendix 1|||Geological Province: Pine Creek Orogen.||||||
27070|Tollis Formation|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
27070|Tollis Formation|24340|4|Described|p143, p149|Paleoproterozoic|Paleoproterozoic|Age: 1890 +18/ -15 Ma (U-Pb). Conformably overlies the Burrell Creek Formation. Geological Province: Pine Creek Inlier.||||||07-NOV-08
27070|Tollis Formation|24442|6|Mentioned|p27|||||||||
27070|Tollis Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27070|Tollis Formation|40248|4|Described|p224|||||||||
27070|Tollis Formation|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27070|Tollis Formation|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27070|Tollis Formation|41294|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27070|Tollis Formation|41295|4|Described|p10|||||||||
27070|Tollis Formation|41311|4|Described|p13|||||||||
27070|Tollis Formation|41466|5|Briefly described|p23|||||||||
27070|Tollis Formation|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27070|Tollis Formation|41961|6|Mentioned|p51|||||||||
27070|Tollis Formation|43140|4|Described|p3||Paleoproterozoic|Of the El Sherana Group.||||||07-NOV-08
27070|Tollis Formation|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of the Finniss River Group. Of Orosirian age.||||||07-NOV-08
27070|Tollis Formation|43187|5|Briefly described|p2|||||||||
27070|Tollis Formation|43832|3|Fully described|23, Table6 p22||Paleoproterozoic|Age ~1870 Ma||||||07-NOV-08
27070|Tollis Formation|46658|6|Mentioned|p556|||||||||
27070|Tollis Formation|47049|5|Briefly described|Table|||See also p237 and Fig.3.||||||11-DEC-06
27070|Tollis Formation|50586|5|Briefly described|p1.1, 4.5, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite.  Intruded by Cullen Supersuite, Jim Jim Suite. Age: 1885 +/- 2Ma (U-Pb).||||||07-NOV-08
27070|Tollis Formation|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Finniss River Group.  Geological Province: Pine Creek Orogen. Poorly sorted fine to coarse volcaniclastic metagreywacke.||||||14-JAN-05
27070|Tollis Formation|62375|5|Briefly described|p9, 20|Paleoproterozoic|Paleoproterozoic|Greywacke, siltstone, slate, argillite, ignimbrite. Age: 1900-1870Ma. Of the El Sherana Group. Thickness: 2200m. ||||||09-FEB-10
27070|Tollis Formation|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1850-1863Ma. Of Finniss River Group. Max thick 1000m. Poorly sorted fine to coarse volcaniclastic metagreywacke; green, grey and brown colour-laminated slate and mudstone; minor pale green cherty argillite and laminated black crystal tuff.||||||07-JAN-09
27070|Tollis Formation|64730|5|Briefly described|p125 Fig. 3, p126, p138|Paleoproterozoic|Paleoproterozoic|Age from underlying Warrs Volcanic Member conflicts with earlier SHRIMP zircon date (1890 +18/-15 Ma) by Page & Williams (1988) - maybe affected by inherited zircons?|Max. deposition age 1862 +/- 3 Ma.|||Overlies Burrell Creek Formation.||02-MAY-12
27070|Tollis Formation|64956|5|Briefly described|p2 Tb. 13, p70-71|Paleoproterozoic|Paleoproterozoic|Max. intrusion age: 1868+/-5ma. Geological province: Pine Creek Orogen. Sample is quartzo-feldspathic volcaniclastic metasedimentary rock from an outcrop of thick greywacke beds interbedded with thin shale beds.||||||07-FEB-11
27070|Tollis Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Pine Creek area.|1868 +/- 5 Ma (maximum deposition age).|||||
27070|Tollis Formation|67564|3|Fully described|p7 Table 2, p9 Fig.4, p23, pp24-25.|Paleoproterozoic|Paleoproterozoic|Type area is near Edith Falls. 2200 m of proximal mid-submarine fan deposits from a nearby recently uplifted volcanic source. Formerly part of El Sherana Group (Kruse et al. 1994).|c.1860 Ma.|Unit in Finniss River Group.||Conformably overlies Burrell Creek Formation. Is intruded and contact metamorphosed by Wolfram Hill Granite. Is overlain unconformably by Edith River Group.|Poorly sorted, fine to coarse, volcaniclastic metagreywacke; laminated slate and mudstone; minor cherty argillite and laminated black crystal lithic tuff.|
27070|Tollis Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|<1868 +/- 5 Ma (Worden et al. 2008b).|Unit in Finniss River Group.||||
27070|Tollis Formation|69418|6|Mentioned|p3:6, 21|||Pine Creek Orogen. Hosts gold deposits (described). Also hosts the Maranboy field, Mount Todd field and Yeuralba field Sn vein deposits (briefly described).||||||12-JUL-16
27070|Tollis Formation|69420|3|Fully described|p5:4, 7, 12-15, 33, 36-37, 40, 101|Paleoproterozoic|Paleoproterozoic|See also 104-105, 110. Central Domain, Pine Creek Orogen. South Alligator region. Limited areal extent. Previously (Needham and Stuart-Smith, 1985; Stuart-Smith et al., 1993) assigned to the El Sherana Group. c.1000m thick. Proximal mid-submarine fan deposits. Has been contact metamorphosed by Yeuralba Granite. Hosts Au deposits at Gold Creek and in the Mount Todd goldfield (described). Hosts Sn at the Morris, Maranboy and Yeuralba fields. SHRIMP zircon maximum depositional age, described as "conservative": brief discussion.|<1868 +/- 5 Ma (Worden et al., 2008).|Finniss River Group.|Dorothy Volcanic Member.|Conformably overlies Burrell Creek Formation. Is overlain unconformably by Phillips Creek or Hindrance Creek Sandstones. Is intruded by Maud Dolerite sills.|Poorly sorted, fine to coarse, volcaniclastic metagreywacke; laminated slate and mudstone; minor cherty shale and laminated black crystal tuff.|12-JUL-16
27070|Tollis Formation|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1890+/-16 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
39871|Tomahawk Formation|24442|5|Briefly described|p45|Ordovician|Cambrian|Terrigenous quartz-glauconite sandstone.  Interfingers with Ninmaroo Formation.||||||12-OCT-10
39871|Tomahawk Formation|44469|6|Mentioned|p 13|||Accidental variation on Tomahawk Beds in table.||||||
39871|Tomahawk Formation|60122|2|Defined|p20-21, p57 Appendix, p10 Tb. 1|Late Cambrian|Late Cambrian|Quartzose and galuconitic sst, minor beds of dolostone, mudstone and conglom.; upper part dominantly limestone with lesser interbedded sst, and marl at the top. Disconformable on Arrinthrunga Fm; conformable below Kelly Cr Fm; interfingers with Ninmaroo F||||||24-MAY-05
39871|Tomahawk Formation|60123|4|Described|p5|Ordovician|Cambrian|Disconformably overlies: Arrinthrunga Formation. Thickness: 190m. Quartzose and glauconitic sandstone, minor dolostone, limestone, dolomitic quartz sandstone, conglomerate.||||||28-APR-05
39871|Tomahawk Formation|60590|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Quartzose and glauconitic sandstone, minor dolostone, limestone, dolomitic quartz sandstone and conglomerate; interbedded limestone or dolostone and marl at top. Overlies the Arrithrunga Formation; underlies the Kelly Creek Formation.||||||25-NOV-04
39871|Tomahawk Formation|60675|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Quartzose and glauconitic sandstone, minor dolostone, limestone, dolomitic quartz sandstone and conglomerate.||||||
39871|Tomahawk Formation|61022|5|Briefly described|p15 Fig. 2|Middle Ordovician|Late Cambrian|Geological Province: Georgina Basin. Named in abstract for: Carbonate ramp facies and oil plays in Late Cambrian-southern Georgina Basin (abstract) by Ambrose, G.J. and Putnam, P.E.||||||20-APR-05
39871|Tomahawk Formation|61388|6|Mentioned|Map Legend|Cambrian|Cambrian|Geological Province: Georgina Basin.||||||
39871|Tomahawk Formation|61404|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Cockroach Group.  Quartzose and galuconitic sandstone, minor dolostone, limestone, dolomitic quartz sandstone and conglomerate; interbedded limestone or dolostone and marl at the top.  Geological Province: southern Georgina Basin.||||||
39871|Tomahawk Formation|62376|5|Briefly described|p53|Middle Ordovician|Late Cambrian|Geological Province: Georgina Basin||||||12-OCT-10
39871|Tomahawk Formation|62595|6|Mentioned|p28 Fig.4.|||Georgina Basin. Relative probability plots of detrital zircon data are shown.||||||
39871|Tomahawk Formation|62789|6|Mentioned|p129 Fig. 2|Early Ordovician|Cambrian|Southern Georgina Basin.||||Overlies the Upper Cambrian Arrinthrunga Formation.||28-MAR-12
39871|Tomahawk Formation|63562|6|Mentioned|p338,345,347,352,353 Figs. 3,7,9,10,11|Early Ordovician|Early Ordovician|See also p341, p349. Of Kruse et al. (2002); formerly Tomahawk beds of Smith (1964). Of Georgina Basin. Similar zircon age spectrum to Pacoota Sandstone.||||Disconformably overlies Arrinthrunga Formation. Correlated with Pacoota Sandstone. Is overlain by Kelly Creek Formation.|Sandstone, siltstone; lesser dolostone and limestone.|
39871|Tomahawk Formation|64068|3|Fully described|p44, p71-73, 75, p19, 38, p151, p ix-x|Early Ordovician|Late Cambrian|Replaces Tomahawk beds. Formerly (Smith 1964) included rocks now in Kelly Creek Formation. Max thickness ~190 m. Hosts minor galena.||Of Cockroach Group.||Overlies Arrinthrunga Formation disconformably. Laterally interdigitates with Ninmaroo Formation. Conformably overlain by Kelly Creek Formation.|Quartz +/- glauconite sandstone, minor limestone, dolostone, mudstone, conglomerate; upper part limestone and minor interbedded sandstone and marl. Contains surficial manganocrete.|05-APR-12
39871|Tomahawk Formation|64334|6|Mentioned|p45|Early Ordovician|Early Ordovician|Georgina Basin. Detrital zircon ages and provenances discussed.||||||
39871|Tomahawk Formation|64443|6|Mentioned|p18||Late Cambrian|||||Disconformably overlies Arrinthrunga Formation.||14-MAY-14
39871|Tomahawk Formation|64778|6|Mentioned|p13, 33|Ordovician|Ordovician|Dulcie Syncline, Southern Georgina Basin. Appears as Tomahawk beds on p13.||||||
39871|Tomahawk Formation|64812|5|Briefly described|p237 Fig. 2|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin.||||||07-FEB-11
39871|Tomahawk Formation|64813|5|Briefly described|p256 Fig. 3, p257|Middle Ordovician|Late Cambrian|Geological Province: southern Georgina Basin. Lateral equivalent of Ninmaroo Formation.||||||12-OCT-10
39871|Tomahawk Formation|65237|5|Briefly described|p3 Fig. 4|Ordovician|Late Cambrian|See also Tomahawk Beds. Geological province: southern Georgina Basin.||||||07-FEB-11
39871|Tomahawk Formation|65341|5|Briefly described|p2 Fig.2. |Ordovician|Cambrian|Does not outcrop in this map area. Contains good aquifers; 90% of bores drilled into this unit have been successful.||Unit in Cockroach Group.||Disconformably overlies Arrinthrunga Formation.|Medium to coarse, crossbedded sandstone; minor interbeds of mudstone, limestone and dolostone; ichnofossils and shelly fossils are common.|
39871|Tomahawk Formation|65342|5|Briefly described|p6.|||Georgina Basin. |||||Quartzose and glauconitic sandstone; minor dolostone, mudstone, and conglomerate; upper part dominantly limestone with lesser interbedded sandstone, marl at top.|
39871|Tomahawk Formation|66767|5|Briefly described|p59|Late Cambrian|Late Cambrian|Southern Georgina Basin.||||Overlies Narpa Group.|Terrigenous quartz sandstone and lesser siliciclastic mudstone.|
39871|Tomahawk Formation|67870|5|Briefly described|p43|Ordovician|Late Cambrian|Georgina Basin.||Cockroach Group.||||
39871|Tomahawk 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
39871|Tomahawk Formation|69443|3|Fully described|p28:7, 19, 25-27, 31, 38, 40, 44|Early Ordovician|Early Ordovician|Kruse in Dunster et al. (2007), after K.G. Smith (1964). Southern Georgina Basin. Crops out as contiguous tracts of hilly country, or isolated low to moderate hills, or prominent ridges. Siliciclastic deposits from emergent land to the W, deposited on a broad epeiric platform. Up to 190m thick; 149m in the type section in NTGS Elkedra-6. Moderately diverse fossil assemblage. Sediment (sand) derived from exposed Aileron or Davenport Province basement to the (present) W. Hosts the Lucy Creek 2 manganese deposit.||Cockroach Group.||Disconformably overlies Arrinthrunga Formation. Is overlain conformably by Kelly Creek Formation (Toko Group). Interdigitates with Ninmaroo Formation.|Mainly fine to coarse, locally dolomitic, glauconite-bearing quartz sandstone with minor quartz wacke, subarkose and sublithic sandstone, plus thin interbeds of conglomerate, micaceous siltstone and shale. Some dolostone interbeds, recrystallised.|12-JUL-16
39871|Tomahawk Formation|69561|6|Mentioned|p33 fig 2|Datsonian|Payntonian|||||||
39871|Tomahawk Formation|69673|4|Described|p114 fig 92, p117, p118, p135|Ordovician|Cambrian |190m thick. Some reservoir potential.||Cockroach Group||Conformably overlain by Kelly Creek Formation, overlies Chabalowe Formation, Arrinthrunga Formation|Dolomitic, glauconite bearing quartz sandstone with minor quartz wacke, subarkose and sublithic sandstone with interbeds of conglomerate, siltstone and shale.|
39871|Tomahawk 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.||||||
39871|Tomahawk Formation|70380|5|Briefly described|p745, p758-759|Tremadocian|Furongian|Southern Georgina Basin.||||Interdigitates with Ninmaroo Formation.|Consists of glauconitic sandstone with interbedded carbonate.|
39871|Tomahawk Formation|70749|6|Mentioned|p52, p54|||Georgina Basin, Centralian Superbasin.||Cockroach Group.||||
39871|Tomahawk Formation|71800|6|Mentioned|p26-p27|Early Ordovician|Late Cambrian|Georgina Basin.||||Overlain by the Kelly Creek Formation.|Medium sandstone.|
39871|Tomahawk Formation|72515|5|Briefly described|Map Legend|Ordovician|Cambrian|Jervois Range Special Map Sheet. Georgina Basin. Contains fossil trilobites, rostroconchs.||Cockroach Group|||Glauconite arenite, laminated, cross bedded, ripple, current and wrinkle marks; syneresis cracks; minor quartzwacke, subarkose, sublitharenite, limestones, dolostone, minor sandstone, marl.|
39871|Tomahawk Formation|72516|2|Defined|p11, p93-95|Early Ordovician|Furongian|Georgina Basin. Type section occurs in cored drillhole NTGS Elkedra 6 with a lower boundary stratotype also. Widespread unit in the southern Georgina Basin in HUCKITTA, ELKEDRA, BARROW CREEK, ALCOOTA, TOBERMORY and SANDOVER RIVER.In Jervois Range Special it outcrops northeast of the Lucy Creek Fault Zone as a contiguous tract of hills, isolated low to moderate hills and some prominent ridges. Thickness ranges from 150-190m. Hosts trilobite and rostroconch fossils which indicate a Furongian whilst trilobites, costate orthide brachiopods and indeterminate pseudoplanispiral gastropods in the upper part indicate a Lower Ordovician age. Deposited in a littoral to sublittoral, broad marine platform, restricted to open-marine setting. Equivalent to the Ninmaroo Formation, Pacoota Sandstone, and possibly the Djagamara Foramtion and Brady Gneiss. SHRIMP results are briefly discussed for samples from sandstone.|ca. 500 Ma (Maximum depositional age)|Cockroach Group||Disconformably overlies the Arrinthrunga Formation. Conformably overlain by the Kelly Creek Formation.|Glauconite arenite; laminated, cross-bedded; ripple, current, wrinkle marks; syneresis cracks; minor quartzwacke, subarkose, sublitharenite, limestone, dolostone, minor sandstone, marl.|04-JUL-22
39871|Tomahawk Formation|73591|6|Mentioned|p40, p42|||Georgina Basin.||||||
38005|Tommys Gap Metamorphics|9199|5|Briefly described|Map legend|||Interlayered hornblende gneiss, orthoamphibolite, quartzite, felsic gneiss, basic metavolcanics, tuffaceous metasiltstone, calc-silicate rock, marble.  Geological Province: Arunta Block.||||||12-DEC-06
38005|Tommys Gap Metamorphics|46730|4|Described|p5|||See also Tommys Gap metamorphics. Geological Province: Arunta Block.||||||
38005|Tommys Gap Metamorphics|60547|5|Briefly described|Map Legend|Precambrian|Precambrian|Interlayered hornblende gneiss, orthoamphibolite, quartzite, felsic gneiss, basic metavolcanics, tuffaceous metasiltstone, calc-silicate rock, marble.||||||
38005|Tommys Gap Metamorphics|69427|5|Briefly described|p12:9, 16|||Strangways Range region, Aileron Province. Crops out in the Giles Creek Synform.||||Correlated with Cavenagh Metamorphics.|An interlayered succession of hornblende gneiss, meta-igneous amphibolite, quartz-rich metasedimentary rock, metabasalt, quartzite, marble and chlorite schist.|12-JUL-16
68748|Top Lily Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Playford Sandstone. White, pink and darker pink-red, thick to very thick bedded, very fine to fine grained, well sorted lithic sandstone.||||||
68748|Top Lily Sandstone Member|65337|2|Defined|p9 Fig.5, p39 Table 5, pp40-41.|Mesoproterozoic|Mesoproterozoic|New name. Southwest MOUNT DRUMMOND area. 140 - 1100 m of marine shelf to shoreline, possibly tidal channel, minor supratidal including aeolian, deposits. Outcrops poorly as a series of ridges and plateaux, deeply weathered to sandstone rubble.||Unit in Playford Sandstone.||Overlies Wangalinji Member. Is overlain by No Mans Sandstone Member.|White, pink, thickly to very thickly bedded, very fine- to fine-grained, well-sorted lithic sandstone; minor, more thinly bedded, ferruginous very fine-grained sandstone and siltstone, and hematitic siltstone to ironstone.|
68748|Top Lily Sandstone Member|69434|4|Described|p19:3, 4-5|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. Type section: MITCHIEBO 53K 724230mE 7935820mN, 3km ESE of Mitchiebo Waterhole. 140-1100m thick. Marine shelf to shoreline, and possibly tidal channel, deposits; minor supratidal, including aeolian.||Playford Sandstone.||Conformably overlies Wangalinji Member. Is overlain conformably by No Mans Sandstone Member or by Crow Formation.|White, pink, and pink-red, thickly to very thickly bedded, very fine to fine, well-sorted lithic sandstone; minor, thinner bedded, ferruginous very fine sandstone and siltstone, haematitic siltstone to ironstone, and stromatolitic carbonate rocks.|12-JUL-16
68748|Top Lily Sandstone Member|71369|5|Briefly described|p6|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin.||Playford Sandstone.||||
68748|Top Lily Sandstone Member|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Playford Sandstone||Overlies Wangalinji Member and underlies No Mans Sandstone Member.||
68748|Top Lily Sandstone Member|72527|4|Described|p8, p12-16, p27-40, p140-144, 193, 194.|Mesoproterozoic|Mesoproterozoic|Two samples analysed, other max dep ages: 1656+/-12 Ma. This member is up to 1100m think in places (e.g. Ten Mile Anticline). Type locality shown as 137.12567dE 18.65977dS.  SHRIMP date derived using 207Pb/206Pb isotopic ratios.|1546 +/- 26 Ma  maximum depositional age|Playford Sandstone||Gradationally overlies Wangalinji Member and sharply but conformably overlain by No Mans Sandstone Member. Unconformably overlain by Wonarah Formation.|Includes white to reddish fine-grained lithic sandstone, with minor pebble lags and numerous current and shallow water indicators such as current lineations, ripples and large cross-beds.|
68748|Top Lily Sandstone Member|72912|5|Briefly described|p5 Fig.3, p24-25.|Mesoproterozoic|Statherian|Located in the west of South Nicholson Basin. Previous dating suggests this unit is Mesoproterozoic, but more recent dating (sample GA2786167) suggests this new sample may possibly be late Paleoproterozoic and equivalent to McNamara Group.||Playford Sandstone||Overlies  Wangalinji Member and underlies No Mans sandstone Member and is laterally equivalent to Bowgan Sandstone.||
68748|Top Lily Sandstone Member|72919|4|Described|p4-5, p24, p26-28, p98|Calymmian|Statherian|[The names Top Lily Sandstone and Top Lily Sandstone Member appear to be used interchangeably without a clear indication of which is considered currently more correct and/or in what areas, or if there is a distinction]. South Nicholson Basin, Lawn Hill Platform. Unit is 143 m thick in the type section and up to 1100 m thick elsewhere. Top contact is sharp and locally erosional, but essentially conformable. Interpreted to have been deposited in tidal channel or on a shallow-water marine shelf. South of the Mitchiebo Fault, a sample from rocks attributed to this unit [or the nomenclatural variant Top Lily Sandstone?] at a measured section yielded a maximum depositional age of 1546 +/- 26 Ma (Kositcin and Carson, 2019), while samples from north of the Mitchiebo Fault yielded maximum depositional ages of 1641 +/- 14 Ma (herein) and 1656 +/- 12 Ma (Kositcin and Carson, 2019). This age discrepancy was used to infer the latter samples were from a unit deposited in the late Paleoproterozoic, rather than the Mesoproterozoic [unresolved nomenclature; both sets of samples are referred to the Top Lily Sandstone / Top Lily Sandstone Member without distinction between these names and the validity of the younger set of maximum depositional ages was not specified].|1641 +/- 14 Ma U-Pb SHRIMP|Playford Sandstone, Wild Cow Subgroup, South Nicholson Group||Conformably underlain by Wangalinji Member. Conformably overlain by No Mans Sandstone Member.|White to reddish, fine-grained lithic sandstone, with minor pebble lags and numerous current and shallow water indicators, such as current lineations, ripples and large cross-beds.|
68748|Top Lily Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Playford Sandstone, Wildcow Subgroup, South Nicholson Group||Underlain by Wangalinji Member. Overlain by No Mans Sandstone Member.||
26328|Tops Member|42504|5|Briefly described|Table 4 P73|||Reserved Haines, July 1988.||||||
26328|Tops Member|42643|2|Defined|p52|Adelaidean||Of the Central Mount Stuart Formation. Age: Late Proterozoic (late Adelaidean)||||||12-DEC-06
26328|Tops Member|42644|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Central Mount Stuart Formation. Arkose and feldspathic quartz arenite, lithic, thin to thick bedded, interbeds of siltstone; minor conglomerate and dolostone. Geological Province: Georgina Basin.||||||15-NOV-05
26328|Tops Member|61388|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Of the Central Mount Stuart Formation. Red-brown and purple cross-bedded sandstone and arkose, interbedded with mudstone, dolostone and anhydrite. Geological Province: Georgina Basin.||||||05-OCT-05
26328|Tops Member|61404|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Mopunga Group. Arkose, feldspathic quartz arenite: lithic, cross-bedded; siltstone interbeds; minor conglomerate and dolostone.  Age: Ediacaran.  Geological Province: southern Georgina Basin.||||||
26328|Tops Member|62984|5|Briefly described|p14|Neoproterozoic III|Neoproterozoic III|Of lower Central Mount Stuart Formation. Overlain by Adnera Member. Recessive and immature sandstone, arkose, conglomerate, mudstone and minor carbonate. Contains Ediacara-style fauna (Mount Skinner fauna) dominated by medusoids.||||||23-JAN-07
26328|Tops Member|64068|3|Fully described|p51-52, p159, 162|Ediacaran|Ediacaran|Probably equivalent to Elkera Formation as shown in Woodgreen map (Haines et al 2007). Numerous though generally isolated Th radiometric anomalies.||Of Central Mount Stuart Formation, Mopunga Group.||Conformably and gradationally overlies Elkera and Grant Bluff Formations and conformably and gradationally overlain by Adnera Member.|Evaporitic and chertified dolostone and dolomitic sandstone, below red-brown arkose, feldspathic arenite, siltstone, cupriferous mudstone; minor conglomerate.|05-APR-12
26328|Tops Member|65338|5|Briefly described|p65.|Ediacaran|Ediacaran|114 to 580 m thick. Rare trace fossils||Unit in Central Mount Stuart Formation.||Is overlain by Adnera Member.|A lower interval of evaporitic and chertified dolostone, and dolomitic sandstone; overlain by red-brown arkosic and feldspathic arenite and siltstone, with varying proportions of interbedded grey-green mudstone.|
26328|Tops Member|65341|4|Described|p5, pp16-17, pp22-24.|||The lower third is very recessive. Depositional environment ranged from sabkha for the bottom third, to deltaic for the rest. Contains a body fossil assemblage called  the Mount Skinner fauna, and rare ichnofossils. Widespread but uneconomic malachite and azurite mineralisation was tested by several companies.||Unit in Central Mount Stuart Formation.||Overlies, probably conformably, Grant Bluff Formation. Is conformably overlain by, and grades into, Adnera Member.|Red-brown and purple crossbedded lithic and feldspathic sandstone and arkose, interbedded with mudstone; reduced grey-green cupriferous horizons; dolostone and anhydrite in lower third in subsurface.|
26328|Tops Member|69443|5|Briefly described|p28:11, 34-35|||Georgina Basin. Marginal marine sabkha to deltaic deposits, with possible high-energy fluviatile facies. Associated with base metal mineralisation in Mount Skinner area.||Central Mount Stuart Formation.||Is overlain conformably and gradationally (probably diachronously) by Adnera Member.|A lower interval of evaporitic and chertified dolostone and dolomitic sandstone, and an upper interval of arkose, feldspathic sandstone, siltstone, mudstone and minor conglomerate.|12-JUL-16
26328|Tops Member|73592|6|Mentioned|p2|||Aileron Province.||Central Mount Stuart Formation.||||
30738|Treasure Suite|23733|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Age: 1829-1816Ma.  See also p8, 12, 13.||||||07-NOV-08
30738|Treasure Suite|23809|6|Mentioned|p27|Paleoproterozoic|Paleoproterozoic|Intrusive rocks.  Of Wyborn et al (1998).  Age: ca 1820Ma.  Geological Province: Tennant Inlier.||||||07-NOV-08
30738|Treasure Suite|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Inlier.||||||07-NOV-08
30738|Treasure Suite|24197|4|Described|p25, p65|Paleoproterozoic|Paleoproterozoic|Includes Wundirgi Fm, Treasure Volcanics, ?Arabulja and Newlands Volcanics in Davenport Province; Hayward Creek Fm (Tomkinson Creek Subgp) in Tennant Creek Prov. Age:1829-1816Ma. Geol.prov: Tennant Creek Inlier, Davenport Province. Eg.of Cullen Assocn.||||||26-NOV-15
30738|Treasure Suite|24567|5|Briefly described|p160 Tb. 2|Paleoproterozoic|Paleoproterozoic|Age: 1820Ma. Geological Province: Tennant Creek Inlier.||||||07-NOV-08
30738|Treasure Suite|50588|5|Briefly described|p1.4, 2.5, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Age: 1820Ma.||||||07-NOV-08
30738|Treasure Suite|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Comprises an unnamed monzonite, felsic porphyry and dolerite. In the Tennant Creek region.||||||07-NOV-08
30738|Treasure Suite|65209|5|Briefly described|p35 Fig.1, p37, p39|Paleoproterozoic|Paleoproterozoic|Includes 3 unnamed units.|||Treasure Volcanics, Arabulja Volcanics, Newlands Volcanics, and unnamed porphyry, granophyre, and monzo-diorite||Felsic volcanics, porphyry, granophyre, and monzodiorite.|05-JAN-17
30738|Treasure Suite|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes K-feldspar megacrystic biotite granite and minor granitic gneiss. Cross-section only||||||
30738|Treasure Suite|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Includes K-feldspar megacrystic biotite granite and minor granitic gneiss.||||||
30738|Treasure Suite|65338|5|Briefly described|p6. |Orosirian|Orosirian||c.1820 - 1810 Ma.||||Dacitic, rhyolitic and basaltic volcanic rocks, shallow intrusives including granophyres and porphyries, monzodiorite, diorite and gabbro.|
30738|Treasure Suite|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region. Shown as comprising three un-named units; a monzonite, a porphyry and dolerite.|||||Monzonite, quartz-monzonite, diorite, quartz-diorite; felsic porphyry; dolerite.|
30738|Treasure Suite|69187|6|Mentioned|p53 Fig.2, p54 Fig.3, p62|||undivided.|||||granitoids|
30738|Treasure Suite|69417|6|Mentioned|p2:5|Orosirian|Orosirian|||||Intrudes Hatches Creek Group.||12-JUL-16
30738|Treasure Suite|69424|4|Described|p9:2-4, 14-15, 27-29, 34, 39, 55|Paleoproterozoic|Paleoproterozoic|Wyborn et al. (1998). Warramunga Province. The c.1820-1810 Ma age range for the Suite is contradicted by the inclusion of rocks dated at 1841 +/- 6 Ma, 1829 +/- 8 Ma and 1827 +/- 6 Ma.|c.1820-1810 Ma.||Treasure, Newlands, Arabulja, Strzeleckie Volcanics.|Intrudes Ooradidgee and Hatches Creek Groups, Hayward Creek Formation, and probably Tennant Creek Supersuite.|Mainly volcanic rocks (dacite, rhyolite, basalt); also plutons, dykes and sills: shallow intrusives (granophyre and felsic porphyry), and diorite, monzodiorite and dolerite.|12-JUL-16
30738|Treasure Suite|69425|4|Described|p10:1-5, 20-22|||Wyborn et al. (1998). Mainly Warramunga Province; local outcrops in Davenport Province. Unlike Devils Suite, this unit has associated extrusive rocks. Unnamed units of dolerite/gabbro, granophyre and granite are described in varying detail. Mafic sills in the Kurinelli area are dated at 1811 +/- 5 Ma (Claoue-Long et al., 2008) and are interpreted to be comagmatic with the Kudinga Basalt.|c.1820-1810 Ma.||Treasure, Newlands, Arabulja and Strzeleckie Volcanics.|Intrudes Kurinelli and Unimbra Sandstones; Rooneys and Hayward Creek Formations; Mia Mia Volcanics.|Unnamed units include dolerite, gabbro, granophyre, microgranite and microgranodiorite, leucogranite, pegmatite and greisen.|12-JUL-16
30738|Treasure Suite|69431|6|Mentioned|p16:2|||Tennant Region.||||||12-JUL-16
30738|Treasure Suite|72380|6|Mentioned|p1,9|Paleoproterozoic|Paleoproterozoic|See Treasure Volcanics.|c. 1820-1810 Ma.|||||03-OCT-19
30738|Treasure Suite|73124|6|Mentioned|p2 Fig.1|||||||||
30738|Treasure Suite|73125|6|Mentioned|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||||||
30738|Treasure Suite|73460|6|Mentioned|p2|||Warramunga Province.||||||
30738|Treasure Suite|73590|6|Mentioned|p2|||||||||
24535|Treasure Volcanics|23410|5|Briefly described|Regional Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.||||||07-NOV-08
24535|Treasure Volcanics|23733|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group.  Age: 1813Ma.  See also p45 Appendix 2.||||||07-NOV-08
24535|Treasure Volcanics|23809|5|Briefly described|p27 Fig. 25|Proterozoic|Proterozoic|Of the Ooradidgee Group.  Geological Province: Davenport Province.||||||
24535|Treasure Volcanics|24172|5|Briefly described|p66 Tb.9|||Of the Ooradidgee Subgroup (Hatches Creek Group). Geological Province: Tennant Creek Inlier. Conformable and interfingers with Taragon Sandstone; conformable with Kurinelli Sandstone also.||||||12-DEC-06
24535|Treasure Volcanics|24197|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of the Treasure Suite. Geological province: Davenport Province.||||||07-FEB-11
24535|Treasure Volcanics|39624|5|Briefly described|Table 1|||||||||
24535|Treasure Volcanics|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24535|Treasure Volcanics|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24535|Treasure Volcanics|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24535|Treasure Volcanics|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Dacitic to rhyolitic lava, commonly porphyritic; minor quartzose and feldspathic arenite; basaltic lava and bedded tuff. Geological Province: Tennant Creek Block.||||||07-NOV-08
24535|Treasure Volcanics|41129|4|Described|Table 1|||Mention p22.||||||12-DEC-06
24535|Treasure Volcanics|41204|4|Described|Table 1|||||||||
24535|Treasure Volcanics|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Ooradidgee Subgroup. Felsic volcanics; lithic/feldspathic arenite, quartz arenite.||||||16-NOV-05
24535|Treasure Volcanics|41308|5|Briefly described|Table 2|||||||||
24535|Treasure Volcanics|41310|4|Described|Table 1|||See also p11.||||||12-DEC-06
24535|Treasure Volcanics|41408|6|Mentioned|Map legend|Proterozoic||||||||
24535|Treasure Volcanics|41465|5|Briefly described|p10|||||||||
24535|Treasure Volcanics|41524|4|Described|Table 1|||||||||
24535|Treasure Volcanics|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup (Hatches Creek Group).  Dacitic to rhyolitic lava and ignimbrite, commonly porphyritic; minor tuff, agglomerate.||||||12-APR-12
24535|Treasure Volcanics|41970|6|Mentioned|p334|||||||||
24535|Treasure Volcanics|42643|4|Described|p11, Table 1 p9|||||||||
24535|Treasure Volcanics|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Ooradidgee Subgroup. Dacitic-rhyolitic lava, porphyritic and non porphyritic; minor interbedded arenite and tuff.||||||07-NOV-08
24535|Treasure Volcanics|42770|5|Briefly described|p12|||Age: 1813+/- 5 Ma.||||||12-DEC-06
24535|Treasure Volcanics|43223|5|Briefly described|Map Legend||Proterozoic|Of Hatches Creek Group.||||||12-DEC-06
24535|Treasure Volcanics|43224|5|Briefly described|Map legend||Proterozoic|Of Hatches Creek Group.||||||12-DEC-06
24535|Treasure Volcanics|43568|6|Mentioned|p504|||Zircon age: 1813+/- Ma||||||
24535|Treasure Volcanics|43802|6|Mentioned|p78|||||||||
24535|Treasure Volcanics|45167|3|Fully described|Table 1|||Of the Ooradidgee Subgroup.||||||12-DEC-06
24535|Treasure Volcanics|49033|2|Defined|p13|Proterozoic|Proterozoic|||||||
24535|Treasure Volcanics|50353|5|Briefly described|Map Legend|||Of Ooradidgee Group.||||||
24535|Treasure Volcanics|50588|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Of the Treasure Suite. Age: 1819-1816 +/- 11Ma (SHRIMP).||||||17-APR-15
24535|Treasure Volcanics|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Rhyolitic and dacitic lava and pyroclastic rocks including ignimbrite; felsic intrusives; feldspathic/lithic (including volcaniclastic), arenite, quartz arenite; minor basaltic lava. In the Tennant Creek region.||||||07-NOV-08
24535|Treasure Volcanics|64722|5|Briefly described|p10|Orosirian|Orosirian|Tennant Region, North Australian Craton.|1814 +3 / -6 Ma.|Of Ooradidgee Group.||||11-APR-12
24535|Treasure Volcanics|64730|5|Briefly described|p142, Fig.11|Paleoproterozoic|Paleoproterozoic|Age is of crystallisation.|1815 +/- 3 Ma (Claoue-Long et al 2005).|Of Ooradidgee Group.||||02-MAY-12
24535|Treasure Volcanics|64735|5|Briefly described|p205, Fig 1, p206 Fig 2, p209, 210, 215|Orosirian|Orosirian|Top of Ooradidgeee Group on stratigraphic grounds, but age indistinguishable from Arabulja Volcanics in overlying Wauchope Subgroup of Hatches Creek Group. Mistakenly said to be part of Hatches Creek Group on p210. Crystallisation ages using SHRIMP RG 207Pb/206Pb on zircons from a volcaniclastic sample (this publication).|1816 +/- 8 Ma and 1814 +3/-6 Ma.|Ooradidgeee Group.|||Felsic volcanics.|17-APR-15
24535|Treasure Volcanics|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|Treasure Volcanics and Newlands Volcanics are thicker in central and western Davenport Province, and absent in Murchison Range area to the northwest.||Ooradidgee Group||||05-JAN-17
24535|Treasure Volcanics|65222|6|Mentioned|p126|||1820-1810 Ma (Blake and Page, 1988).||Of Hatches Creek Group||||
24535|Treasure Volcanics|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Ooradidgee Group. Inferred rhyolitic to dacitic lava and intrusive rocks, pyroclastic rocks, possible stratiforma mafic igneous rocks; feldspathic/lithic/quartz arenite. Cross-section only||||||
24535|Treasure Volcanics|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Ooradidgee Group. Non-outcropping. Inferred rhyolitic to dacitic lava and intrusive rocks, pyroclastic rocks, possible stratiforma mafic igneous rocks; feldspathic/lithic/quartz arenite.||||||
24535|Treasure Volcanics|65338|4|Described|p8 Table 1, p6, p19. |Paleoproterozoic|Paleoproterozoic|Non-outcropping, interpreted from geophysical data; lithology inferred from geophysical character and/or outcrop in adjacent sheet areas. Distinctive, highly magnetic interval.Younger interval of felsic episodes in Ooradidgee Group.|1814 +3/-6 Ma (Claoue-Long et al. 2008b).|Unit in Ooradidgee Group.|||Felsic lava and pyroclastic rocks, stratiform felsic and mafic intrusive igneous rocks, sandstone.|
24535|Treasure Volcanics|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|Associated with Hatches Creek Tungsten Field.|1814 Ma.|Unit in Ooradidgee Group.||Overlies Taragan Sandstone.|Dacitic to rhyolitic lava, commonly porphyritic; minor quartzose and feldspathic arenite; basaltic lava and bedded tuff.|
24535|Treasure Volcanics|67165|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Unit in Ooradidgee Group.|||No outcrop: inferred rhyolitic to dacitic lava and intrusive rocks, pyroclastic rocks, possible stratiform mafic igneous rocks; feldspathic/lithic/quartz arenite.|
24535|Treasure Volcanics|67175|6|Mentioned|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||||||
24535|Treasure Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area. Extrusion age.|1814 +/- 3 Ma.|Hatches Creek Group.|||Felsic.|
24535|Treasure Volcanics|67352|4|Described|p10, p41, p44 fig 48, p45, p46, p57|Orosirian|Orosirian|Over 1700 m thick. Lava is recessive; arenite is ridge-forming. Hosts tungsten ore in quartz veins.||Ooradidgee Group||Lateral equivalent of Mia Mia Volcanics.  Conformably overlies/interfingers with Taragan Sandstone.|Felsic lava: mainly rhyodacite, porphyritic, spherulitic, vesicular, amygdaloidal; subordinate feldspathic and quartz arenite interbeds: locally pebbly; basaltic lava: vesicular, amygdaloidal, scoriaceous; minor thinly bedded tuff.|
24535|Treasure Volcanics|68518|4|Described|p9 Tb.1, p11|Proterozoic|Proterozoic|Max. thickness: 1800 m.||Ooradidgee Subgroup||Conformable on Kurinelli Sandstone and on and interfingers with Taragan Sandstone. Overlain conformably by and interfingers with Unimbra Sandstone; overlain unconformably by Cambrian strata.|Variably recessive felsic volcanics: porphyritic and subordinate non-porphyritic dacitic to rhyolitic lava flows; minor interlayered arenite, bedded tuff; porphyritic, rhyolitic ignimbrite, agglomerate, cherty to phyllitic ashstone; felsic lava.|30-MAY-16
24535|Treasure Volcanics|68697|5|Briefly described|v-vi, p2, p24-26, p46|Orosirian|Orosirian|Davenport Province. SE flank of the Murray Downs Dome. Topmost volcanic unit in the Ooradidgee Group. This age is identical with that of a sample of Arabulja Volcanics, 2500m more or less directly stratigraphically below, datermined by Claoue-Long et al. (2008).|1814 +/- 3 Ma.|Ooradidgee Group.||Is overlain by and interdigitates with Unimbra Sandstone. Correlated with Mia Mia Volcanics.|A thick succession of felsic volcanics and volcaniclastics, and some layered clastic sedimentary rocks.|
24535|Treasure Volcanics|69187|6|Mentioned|p53 Fig.2|||Warramunga Province.||||||
24535|Treasure Volcanics|69418|5|Briefly described|p3:21, 23|||Tennant Region. Hosts the Hatches Creek field W-Cu vein deposit (briefly described).|||||Porphyritic acid volcanic rocks.|12-JUL-16
24535|Treasure Volcanics|69424|4|Described|p9:3-5, 15-17, 23, 25-27, 55|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Of the Treasure Suite. Up to 3500m thick. Subaerial felsic volcanic rocks erupted from two centres, in the Murray Downs Dome and the Hatches Creek tungsten field. Sandstone records an upward transition from fluviatile to shoreline and shallow subaqueous (marine or lacustrine) sedimentation. Is intruded by 1811 +/- 5 Ma mafic sills. Hosts W-bearing quartz veins in the Hatches Creek tungsten field.|1814 +3/-6 Ma (Claoue-Long et al., 2008).|Treasure Suite.||Conformably overlies Kurinelli and Taragan Sandstones. Is overlain by Unimbra Sandstone both unconformably and conformably (interfingering). Correlated with Mia Mia Volcanics.|Recessive, weakly metamorphosed porphyritic dacite to rhyolite lava, local non-porphyritic felsic lava; minor volcanic breccia; minor quartzic/feldspathic/lithic/volcanilithic sandstone; minor schist. Includes ignimbrites. Minor basalt locally.|12-JUL-16
24535|Treasure Volcanics|69425|4|Described|p10:4-6, 8-10, 13-14, 16|||Subaerial volcanics erupted from two volcanic centres in Warramunga Province. A third centre in Murray Downs Dome (Davenport Province) comprises a succession of ignimbrite and lava overlain by felsic tuff and agglomerate. Sandstones record an upward transition from fluviatile to shoreline and shallow subaqueous (marine or lacustrine) sedimentation. c.1800m thick in Davenport Province; up to ?3500m in Warramunga Province. Ridge-forming quartzic and feldspathic sandstone locally forms discrete mappable lithofacies. Correlated with Mia Mia Volcanics. Identical age from an ignimbrite and a probable lava (Kositcin et al., 2013), 60km apart.|1814 +3/- 6 Ma (Claoue-Long et al., 2005, 2008).|Treasure Suite. ||Conformably overlies Kurinelli and Taragan Sandstones (interfingers with the latter). Is overlain both conformably and unconformably by, and interfingers with, Unimbra Sandstone.|Weakly metamorphosed, porphyritic dacitic to rhyolitic lava and ignimbrite, and non-porphyritic felsic lava locally; tuff; agglomerate; minor quartzic/feldspathic/lithic/volcanilithic sandstone; minor schist; recessive basalt and tephritic lava.|12-JUL-16
24535|Treasure Volcanics|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1814+/-3.6 Ma crystallisation: U-Pb zircon SHRIMP||||Felsic volcanic rocks, extrusive dacite, porphyry.|
24535|Treasure Volcanics|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24535|Treasure Volcanics|72380|5|Briefly described|p1,3,5|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces. [Also referred to as Treasure Suite on p1]. Felsic porphyritic volcanics intruded by mineralised quartz veins at the Hit or Miss deposit, Hatches Creek tungsten field. Claoue-Long et al (2008) and Kositcin et al (2013) reported SHRIMP U-Pb zircon ages of 1814+\-6 and 1814+\-3 Ma respectively, representing timing of magmatic zircon crystallisation and emplacement, and therefore placing a maximum constraint on timing of deposit mineralisation. MC-ICP-MS analysis of molybdenite from two samples of scheelite-molybdenite-bearing quartz vein (see this record for sample details) returned Re-Os model ages of 1677+\-10 Ma and 1602+\-9 Ma, which are younger than mineralisation ages previously reported for the Hatches Creek tungsten field (eg Fraser et al 2008).||Unit of Ooradidgee Group.||||03-OCT-19
24535|Treasure Volcanics|73083|6|Mentioned|p21|||Three uneven arcuate bodies in the Frew River 1:250K Sheet may be the remains of a volcanic centre. Interpreted as cut by granite.||||||
24535|Treasure Volcanics|73124|6|Mentioned|p2 Fig.1|||||||Equivalent to Taragan Sandstone.||
24535|Treasure Volcanics|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
24535|Treasure Volcanics|73460|6|Mentioned|p2|||Warramunga Province.||||Underlain by Kurinelli Sandstone. Equivalent to Taragan Sandstone.||
24535|Treasure Volcanics|73550|6|Mentioned|p5|Orosirian|Orosirian||ca 1814 Ma|||||
24535|Treasure Volcanics|73590|6|Mentioned|p1-2|Orosirian|Orosirian||ca 1814 Ma|Ooradidgee Group||Underlain by Kurinelli Sandstone. Equivalent to Taragan Sandstone.||
24536|Trephina granitic gneiss|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Informal name. Of the Jennings Suite. Age: ~1771Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24536|Trephina granitic gneiss|38885|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24536|Trephina granitic gneiss|39552|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24536|Trephina granitic gneiss|39583|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24536|Trephina granitic gneiss|39610|6|Mentioned|p6|||||||||
24536|Trephina granitic gneiss|39887|6|Mentioned|Fig.3|||||||||
24536|Trephina granitic gneiss|39888|6|Mentioned|Fig.8|||||||||
24536|Trephina granitic gneiss|48992|3|Fully described|p53|Proterozoic|Proterozoic|||||||
24536|Trephina granitic gneiss|50369|5|Briefly described|p1.4, 8.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Jennings Suite.||||||07-NOV-08
24536|Trephina granitic gneiss|60525|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Biotite granitic gneiss.||||||
23055|Tug Sandstone Member|43565|5|Briefly described|Table 1,p425,426-440|||||||||
23055|Tug Sandstone Member|43748|5|Briefly described|p10, Tb 1 Fig.4,7, p16|Late Eocene|Late Eocene|Replaces informal 'Arltunga Member'.||Top of Hale Formation.|||Poorly consolidated, fine-grained, brown silty sandstone|19-DEC-11
23055|Tug Sandstone Member|65194|6|Mentioned|p53|Late Oligocene|Late Eocene|Of Hale Formation. Overlies Ulgnamba Lignite Member. Is overlain unconformably by Waite Formation (equivalent).||||||
23055|Tug Sandstone Member|69458|5|Briefly described|p42:7-8|||Hale Basin. Low-energy fluvial-lacustrine deposits. Silcrete formed after deposition.||Uppermost Hale Formation.||Overlies Ulgnamba Lignite Member. Is overlain unconformably by Waite Formation.|Poorly consolidated, fine-grained, brown silty sandstone, with minor sandy siltstone and claystone interbeds.|12-JUL-16
42248|Twin Bonanza Porphyry|23809|5|Briefly described|p10-11|Paleoproterozoic|Paleoproterozoic|Possibly an informal name referring to porphyritic rocks of the Twin Bonanza prospect.  Probably part of The Granites Suite.  Coarse porphyritic granite.  See also the informal Twin Bonanza porphyry and misspelt Twin Bonazer Posphyry.||||||31-MAR-15
42248|Twin Bonanza Porphyry|62580|5|Briefly described|p36|Paleoproterozoic|Paleoproterozoic|Small inrusive of coarse-grained, equigranular biotite monzogranite with large, euhedral perthitic alkali feldspar megacrysts; some gold mineralisation. Age: 1802+/-8Ma (U/Pb zircon). See also Twin Bonanza porphyry.||||||07-FEB-11
42248|Twin Bonanza Porphyry|69618|5|Briefly described|p106-107|||Smith (2001). Hosts Buccaneer and Cypress gold prospects. Gold occurs in stockwork veins associated with two alteration events (early hydrothermal and later phyllic). Fig 18 suggests this is the same unit as the Buccaneer Porphyry.|c.1795 Ma.|||Intrudes Wilson Formation of Ware Group.|A composite body consisting of porphyritic syenogranite, monzogranite and monzonite.|31-MAR-15
42248|Twin Bonanza Porphyry|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1802+/-8 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyritic granite.|
24544|Two Sisters Granite|22632|5|Briefly described|p520-3,530-2||Proterozoic|Intrudes Finniss River Group.||||||13-OCT-08
24544|Two Sisters Granite|22810|4|Described|Table3 P8, P17||Proterozoic|Unconformably overlain by Tindall Limestone.||||||13-OCT-08
24544|Two Sisters Granite|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Granite, adamellite and granodiorite in places pegmatitic with accessory garnet and tourmaline.||||||07-NOV-08
24544|Two Sisters Granite|23714|4|Described|p17|Proterozoic|Proterozoic|See also page 14, Table 2. Litchfield Province. Also previously named Roberts Creek Granite.||||||21-NOV-08
24544|Two Sisters Granite|23715|5|Briefly described|Map legend||Proterozoic|Predominantly S-type. In the Cullen Batholith, of the Rum Jungle and Central Region||||||
24544|Two Sisters Granite|23822|6|Mentioned|p301|||Geological Province: Litchfield Province.||||||
24544|Two Sisters Granite|24197|5|Briefly described|p18, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Allia Creek Suite. Previously mapped as Turnbull Bay Granite and Roberts Creek Granite. Age: ~1845Ma. Geological province: Litchfield Block/Pine Creek Inlier.||||||07-FEB-11
24544|Two Sisters Granite|24442|5|Briefly described|p40|Paleoproterozoic|Paleoproterozoic|With S-type characteristics.  Intrudes Burrell Creek Formation.  Age: 1850-1800Ma.||||||21-NOV-08
24544|Two Sisters Granite|39069|6|Mentioned|p21|||||||||
24544|Two Sisters Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24544|Two Sisters Granite|39803|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24544|Two Sisters Granite|40495|4|Described|p11|||||||||
24544|Two Sisters Granite|40764|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24544|Two Sisters Granite|40765|3|Fully described|p10|||||||||
24544|Two Sisters Granite|40808|3|Fully described|p16|||||||||
24544|Two Sisters Granite|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24544|Two Sisters Granite|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24544|Two Sisters Granite|41305|2|Defined|p51|Paleoproterozoic||||||||07-NOV-08
24544|Two Sisters Granite|41980|5|Briefly described|Table 3 P575|||||||||
24544|Two Sisters Granite|42070|6|Mentioned|Fig.3 P4|||||||||
24544|Two Sisters Granite|43624|6|Mentioned|Fig.1,p7|||||||||
24544|Two Sisters Granite|50586|5|Briefly described|p1.1, 3.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Allia Suite. Age: 1768 +/- 16Ma (Rb-Sr).||||||07-NOV-08
24544|Two Sisters Granite|62375|6|Mentioned|p11|||Geological Province: Pine Creek Orogen.||||||09-FEB-10
24544|Two Sisters Granite|63866|5|Briefly described|p107|||Litchfield Province, Pine Creek Orogen.||||||
24544|Two Sisters Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Granite, adamellite and granodiorite in places pegmatitic with accessory garnet and tourmaline. Intrudes Burrell Creek Formation, unconformably overlain by Tolmer Group and -Cla (?Tindall Limestone).||||||07-JAN-09
24544|Two Sisters Granite|64731|6|Mentioned|p148 Fig.3, p150|Proterozoic|Proterozoic|S-type. May be co-magmatic suites with Mount Litchfield Granite.||||||12-APR-12
24544|Two Sisters Granite|64956|5|Briefly described|p2 Tb. 8, p50, p65|Paleoproterozoic|Paleoproterozoic|Intrudes Wangi Basics, Welltree Metamorphics + Burrell Creek Fm. Max.intrusion age: 1862+/-6Ma. Geol.prov: Pine Creek Orogen. Sample: two-mica granite in Litchfield province - deeply weathered, pink-grey in colour, medium-grained, foliated to massive.||||||07-FEB-11
24544|Two Sisters Granite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.|||Granite, quartz monzonite and granodiorite, in places pegmatitic with accessory garnet and tourmaline.|23-NOV-11
24544|Two Sisters Granite|67232|6|Mentioned|p4 Fig.3.|Paleoproterozoic|Paleoproterozoic|||Unit in Allia Creek Suite.||||
24544|Two Sisters Granite|69420|5|Briefly described|p5:18-19, 28, 105-106, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Mineralogy and petrology/geochemistry summarised. Associated with late-stage pegmatite Sn deposits. SHRIMP U-Pb zircon age.|1862 +/- 5 Ma: Worden et al. (2008).|Allia Creek Suite.|||Two phases: a fine to medium, equigranular, variably foliated granite; and a coarse garnet-bearing pegmatitic variety consisting of a sodic granodiorite and a quartz-feldspar graphic leucogranite. S-type.|12-JUL-16
24544|Two Sisters Granite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1862 +/- 6 Ma.|Allia Creek Suite.|||Light grey to pink, medium- to coarse-grained, weakly to strongly foliated, granite, quartz monzonite and granodiorite; commonly garnetiferous, in places pegmatitic with accessory garnet and tourmaline.|
24544|Two Sisters Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1862+/-6 Ma (crystallisation: U-Pb zircon SHRIMP)||||Pink-grey medium-grained biotite-muscovite granite, foliated.|
76123|Tyson Creek Metamorphics|65338|5|Briefly described|p56.|Statherian|Statherian|Has a granulite-grade foliation which is cross-cut by Possum Creek Charnockite. In Napperby 1:250 000 sheet area.|1767 +/- 17 Ma (Hand et al. 1995).|||||
24545|Tyson Creek granulite|23270|5|Briefly described|Table 1, p6||Proterozoic|In the Arunta Block (Division 1).||||||12-DEC-06
24545|Tyson Creek granulite|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block (Division One). Age: Early or Middle Proterozoic.||||||12-DEC-06
24545|Tyson Creek granulite|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24545|Tyson Creek granulite|39887|6|Mentioned|Fig.5|||||||||
24545|Tyson Creek granulite|39888|6|Mentioned|Appendix|||Published isotopic ages.||||||
24545|Tyson Creek granulite|48992|3|Fully described|p52|Proterozoic|Proterozoic|||||||
24545|Tyson Creek granulite|50369|6|Mentioned|p4.2, 7.3|||Informal name. Intruded by Possum Creek Charnockite.||||||
41854|Udor Granite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Madderns Yard Metamorphic Complex.   Age: 1663Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
41854|Udor Granite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1663Ma. Foliated biotite and muscovite bearing granite, non-magnetic. Of the Madderns Yard Metamorphic Complex. Geological Province: Haasts Bluff Domain.||||||07-NOV-08
41854|Udor Granite|67565|2|Defined|p58, p10, p7 Table 1, p34, p48.|Statherian|Statherian|New name. Haasts Bluff Domain, Warumpi Province. Named after Mount Udor; type locality 2 km north of there. Previously included in undifferentiated Arunta Complex (Ranford, 1969).  Outcrops poorly over large areas. Distinctive low, flat magnetic signature on aeromagnetic images. Geochemistry is discussed briefly. Age by Cross et al. (2004). Metamorphosed to lower to middle amphibolite facies during the 1590-1560 Ma Chewings Orogeny.|1663 +/- 4 Ma (SHRIMP U-Pb zircon).|||Intrudes Peculiar Complex. Is intruded by Stuart Pass Dolerite in subcrop. Is overlain by Heavitree and Putardi Quartzites.|Foliated, leucocratic, equigranular to weakly porphyritic biotite-muscovite granite; lesser biotite granite and biotite-muscovite-garnet granite.|01-DEC-15
41854|Udor Granite|68832|4|Described|p3-5,32|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Crystallisation age, and younger metamorphic age.|1663+/-4 Ma, 1594+/-12 Ma|||Interpreted to underlie the Putardi Quartzite.|Equigranular to weakly porphyritic, and relatively leucocratic granite. Foliated biotite granite sampled.|
41854|Udor Granite|69417|5|Briefly described|p2:5|Statherian|Statherian|Haasts Bluff Domain, Warumpi Province.||||Intrudes Madderns Yard Metamorphic Complex.||12-JUL-16
41854|Udor Granite|69428|5|Briefly described|p13:3-5, 15|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Haasts Bluff Domain, Warumpi Province. Texturally variable but geochemically and geophysically homogeneous. Has a distinctively low and flat magnetic signature. SHRIMP U-Pb zircon age. Evidence of recrystallisation or Pb loss at 1594 +/- 12 Ma.|1663 +/- 4 Ma (Cross et al., 2005).||||Foliated biotite and biotite-muscovite leucogranite and granite; less common foliated muscovite granite, muscovite leucogranite and coarsely-porphyritic biotite-muscovite granite.|12-JUL-16
41854|Udor Granite|70739|6|Mentioned|p541|||Warumpi Province, Arunta Region. Underwent zircon recrystallisation or Pb loss at 1594 +/- 12 Ma (Chewings Event).||||||
41854|Udor Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1663+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Biotite granite.|
41855|Ulambaura Granodiorite|67565|2|Defined|p61, p21,  p6 Table 1, p32.|Statherian|Statherian|New name, after Ulambaura Outstation. Previously included in undifferentiated Arunta Complex (Ranford, 1969). Yaya Domain, Warumpi Province. A large number of discrete bodies, up to 3 km in length. Type locality c.500 m SE of Alkipi (Mount Larrie) Outstation. Geochemistry is discussed briefly. Interpreted to have intruded during 1640-1635 Ma Liebig Orogeny. Metamorphosed at upper amphibolite facies during the 1590-1560 Chewings Orogeny.||||Intrudes Alkipi Metamorphics and Yaya Metamorphic Complex.|Weakly porphyritic, foliated hornblende-biotite granodiorite and tonalite; minor biotite granodiorite.|01-DEC-15
41855|Ulambaura Granodiorite|69428|5|Briefly described|p13:11|||Scrimgeour et al. (2005). A large number of discrete bodies. Has an arc-like geochemical signature.||||Intrudes Yaya Metamorphic Complex.|Foliated granodiorite; contains coarse igneous hornblende overprinted by secondary hornblende and biotite with minor titanite and epidote that are metamorphic in origin. Low-K calc-alkaline granodiorites and tonalites.|12-JUL-16
24546|Uldirra Porphyry|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Metamorphically retrogressed rock, porphyritic microgranite.||||||
24546|Uldirra Porphyry|23270|5|Briefly described|Table 1, p4||Proterozoic|In the Arunta Block.||||||13-DEC-06
24546|Uldirra Porphyry|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block.  Age: Middle Proterozoic.||||||13-DEC-06
24546|Uldirra Porphyry|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24546|Uldirra Porphyry|48992|2|Defined|p53|Proterozoic|Proterozoic|||||||
24546|Uldirra Porphyry|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite.||||||07-NOV-08
24546|Uldirra Porphyry|69427|5|Briefly described|p12:30 Fig.12.28; 12:32|||Stewart et al. (1980). Crops out in the Ngarlurbindi Hills SE of Mount Denison homestead. Included in a map of 1780-1740 Ma granites in the Aileron Province.|||||Porphyritic microgranite and microgranodiorite, and equigranular muscovite leucogranite.|12-JUL-16
24546|Uldirra Porphyry|71858|4|Described|p6, p17, p24-p25, p37-p40|Statherian|Statherian|Aileron Province. Named for the Uldirra Hill and was defined in Stewart et al (1980a) as a body of porphyritic microgranite, even-grained leucogranite and porphyritic microgranodiorite. The best exposures occur northwest of Natural Dam. This unit was previously interpreted as part of the 1780-1760 Ma magmatic event in the Aileron Province. Age is further constrained by dating of the Ngalurbindi Orthogneiss. Petrographic descriptions from numerous localities are discussed. Geochemistry analysis and discussion are discussed.||||Intruded by the Wangala Granite. Faulted against the Ngalurbindi Orthogneiss.|Pale-grey, porphyritic biotite granite intruded by pegmatite dykes including tourmaline-bearing dykes and quartz-tourmaline veins.|
24547|Ulgnamba Lignite Member|38885|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
24547|Ulgnamba Lignite Member|39552|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
24547|Ulgnamba Lignite Member|39583|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
24547|Ulgnamba Lignite Member|39610|4|Described|p15|||||||||
24547|Ulgnamba Lignite Member|39931|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
24547|Ulgnamba Lignite Member|43565|5|Briefly described|p424-440|Late Eocene|Middle Eocene|||||||
24547|Ulgnamba Lignite Member|43748|5|Briefly described|p10, 11, Fig. 4, Tb 1|Late Eocene|Middle Eocene|4m thick in type section in BMR DDH Alice Springs SH 2. Facies variant of the upper part of the Claraville Mudstone Member. Max age likely to be Late Cretaceous or Paleocene. Min age Late Oligocene or Miocene. Mid to Late Eocene age implied by palynomorph assemblage and palaeomagnetic data.||Of Hale Formation.||Conformably overlies Ambalindum Sandstone Member, or Claraville Mudstone Member.|Lignite and carbonaceous shale.|07-OCT-15
24547|Ulgnamba Lignite Member|46730|5|Briefly described|p7|Middle Eocene|Middle Eocene|Of Hale Formation.  Geological Province: Amadeus Basin.||||||
24547|Ulgnamba Lignite Member|48992|2|Defined|p54|Tertiary|Tertiary|||||||
24547|Ulgnamba Lignite Member|60525|5|Briefly described|Map Legend|Tertiary|Tertiary|Of the Hale Formation. Lignite.||||||
24547|Ulgnamba Lignite Member|61155|5|Briefly described|p16|Middle Eocene|Middle Eocene|Of the Hale Formation. Overlies the Ambalindom Sandstone Member; underlies the Arltunga Member. Geological Province: Hale, Ti-Tree and Waite  Basins.||||||
24547|Ulgnamba Lignite Member|65194|6|Mentioned|p53, p55|Late Eocene|Middle Eocene|Of Truswell and Marchant (1986). Unit in Hale Formation. Carbonaceous shale or lignite lenses, mud- and silt-rich layers. Overlies Claraville Mudstone Member; is overlain by Tug Sandstone Member.||||||
24547|Ulgnamba Lignite Member|69418|5|Briefly described|p3:35|Cenozoic|Cenozoic|Hale River Basin. c.10m thick.||Hale Formation.|||Grey carbonaceous clay and lignite.|12-JUL-16
24547|Ulgnamba Lignite Member|69458|4|Described|p42:7-8, 11, 13, 34, 37|Eocene|Eocene|Hale Basin. 4m thick in the type section in drillhole Alice Springs-SH2 (Stewart et al., 1980). Paludal deposits. Probable middle to late Eocene age from palynomorphs. Shortened to Ulgnamba Lignite on 42:11. Poor quality: has high ash and sulfur content, but does have hydrocarbon (oil shale) potential.||Hale Formation.||Conformably overlies Ambalindum Sandstone Member. Is overlain by Tug Sandstone Member. Lateral equivalent of Delaney Mudstone Member.|Lignite and carbonaceous shale and, locally, oil shale.|12-JUL-16
24547|Ulgnamba Lignite Member|69673|6|Mentioned|p208|Eocene|Eocene|||||||
37622|Ulta Limestone|60703|2|Defined|p704|Late Oligocene|Late Oligocene|A lithoclast carbonate deposited in a structurally controlled palaeochannel at the northern margin of Lake Eyre Basin. Max. thickness (inferred): ~40m. Correlated with parts of the Wipajiri Formation and Carl Creek Limestone.||||||13-DEC-06
37622|Ulta Limestone|66573|6|Mentioned|p873|||Contains Kangaroo Well local fauna, an evolutionary intermediate between the Ngama and Kutjamarpu faunas.||||||
37622|Ulta Limestone|69458|5|Briefly described|p42:8, 19, 22|Oligocene|Oligocene|Of Megirian et al. (2004). Up to 40m thick. Forms low mesas up to 30m relief, or rubbly exposures, along a sinuous outcrop of c.50km. Contains vertebrate fossil assemblages: the Kangaroo Well Local Fauna (briefly described).||||Correlated with Etadunna, Namba Formations.|An alluvial calcilithite composed primarily of caliche fabrics; yellow-orange limestone facies (deposited in paleochannels), with varieties of caliche, chalcedonic limestone and chalcedony.|12-JUL-16
72418|Umbeara Sandstone|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Geological Province: Arunta Region - Aileron Province. Non-outcropping; inferred subarkosic/sublithic/lithic arenite, quartz arenite; minor pyroclastic rocks.||||||07-NOV-08
69491|Umbeara granite|61154|5|Briefly described|p13|||Seven granitic phases. Granite generally forms discrete veins, dykes ansd small bodies scattered within more extensive exposures of Musgravian gneisses;  many textural types, including equigranular to porphyritic, and fine to coarse granite, microgranite.||||||19-JUL-05
69491|Umbeara granite|69436|5|Briefly described|p21:9|||Edgoose et al. (2002). A group of seven intrusive phases forming discrete veins, dykes and small bodies, scattered within Musgravian gneiss. Intruded by numerous veins and dykes of pegmatite, aplite, microdiorite, granophyre, leucogranite and granite breccia.|||||Equigranular to porphyritic, fine- to coarse-grained, leucogranodiorite, quartz monzonite, quartz leucomonzonite, leucogranite, quartz monzodiorite, quartz diorite and granodiorite. Locally foliated.|12-JUL-16
33650|Umutju Granite Suite|24301|6|Mentioned|p37 Appendix 1|||||||||
33650|Umutju Granite Suite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Mantapyika and Puka Granites.  Age: ~1180-1120Ma.  Geological Province: Musgrave Block.||||||
33650|Umutju Granite Suite|60683|2|Defined|p55 Appendix, p14|Mesoproterozoic|Mesoproterozoic|Includes Mantapayika, Puka and Walytjatjata Granites and unnamed charnockite and clinopyroxene granite.  Synonymous with part of Musgrave-Mann Metamorphics, Olia Gneiss and unnamed metamorphosed granites of Forman (1966a, 1972). See also p10 Tb.1, p42-43.||||||
33650|Umutju Granite Suite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Includes the Walytjatjata, Puka and Mantapayika Granites. Age: ~1180-1120Ma. Geological Province: Musgrave Block.||||||19-OCT-05
33650|Umutju Granite Suite|69091|6|Mentioned|p103 Fig.5.6|||||||||
33650|Umutju Granite Suite|70793|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma); Musgrave Orogeny (1220-1150 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop14_lut.csv, 500k_interpgeop_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Supersuite.|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite|
33650|Umutju Granite Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||charnockite, migmatite, granite|
33650|Umutju Granite Suite|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen, Musgrave Province. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). See 100k_geologyp_lut.csv, 100k_interpgeop_lut.csv, 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeop16_lut.csv.|1175+\-10 Ma; 1148+\-6 Ma|Unit of Pitjantjatjara Suite.|||Medium- to coarse-grained hornblende--pyroxene(--garnet) metagranite|
33650|Umutju Granite Suite|71592|5|Briefly described|Appendix A.|||Musgrave Province. Age determination by zircon Pb-Pb evaporation.|1172+/-6 Ma (crystallisation).||||Granite.|
33650|Umutju Granite Suite|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Musgrave Province, Paterson Orogen.|Max age 1175+/-10 Ma, Min 1148+/-6 Ma.|Pitjantjatjara Supersuite|||Medium- to coarse-grained hornblende-pyroxene(-garnet) metagranite.|
26285|Unca Granite|24197|5|Briefly described|p60 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Alarinjela Suite. Age: ?1713Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
26285|Unca Granite|39888|6|Mentioned|Fig.9|||||||||
26285|Unca Granite|40538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Leucogranite, foliated, cream-pink. Geological Province: Arunta Block.||||||07-NOV-08
26285|Unca Granite|40668|5|Briefly described|p273|||||||||
26285|Unca Granite|40906|4|Described|p13|||||||||
26285|Unca Granite|49036|2|Defined|p13|Mesoproterozoic|Mesoproterozoic|Previously undivided metamorphics of the Arunta complex||||||
26285|Unca 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
26285|Unca Granite|60551|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Leucogranite, very weakly foliated.||||||
26285|Unca Granite|69427|5|Briefly described|p12:30|||Shaw et al. (1984). Jervois Range and Bonya Hills area, Aileron Province.|||||Leucogranite.|12-JUL-16
26285|Unca Granite|71621|5|Briefly described|p1, p42-p43|||Aileron Province. Outcrop is strongly weathered; epidote and chlorite are common alteration phases.Petrography and zircon description discussed.||||Intrudes the Bonya Metamorphics.|Fine-grained, equigranular, quartz-K-feldspar-plagioclase-biotite granite with secondary muscovite.|02-FEB-19
26285|Unca Granite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|||||Leucogranite: fine to medium-grained, equigranular, commonly strongly weathered and altered (silicified).|
26285|Unca Granite|72516|2|Defined|p13, p15, p17, p19-21, p29, p209|||Named for Unca Creek and initially defind by Shaw et al 1985 and further described in Freeman 1986.The type location is defined as 632496mE 7498959mN. Rubbly hills of this unit occur 6km north of the Jervois Mineral field in the Jervois domain. Deeply weathered with an orange to pink weathering surface. Deposited in a continental margin environment. Direct dating was not possible due to highly metamict nature of zircons but the unit is interpreted to have been deposited prior to 1.76 Ga. Geochemistry, distinguishing features, extent, structure, metamorphism, alteration, mineralisation and geophysical response are discussed. See also p36-p56, p63-64, p86, p88, p104-105, p125-126, p135, p137, p171, p188-189, p192, p209, p218.||Fosters Suite||Unconformably overlain by the Elyuah Formation and the Oorabra Arkose. Intrudes the Bonya Metamorphics and the Attutra Metagabbro.|Leucogranite: medium to fine-grained, equigranular, minor biotite and chlorite after biotite; commonly strongly weathered and altered; moderately to strongly foliated.|04-JUL-22
26285|Unca Granite|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes granite.|
26188|Undandita Member|9199|5|Briefly described|Map legend|Devonian|Devonian|Of the Brewer Conglomerate (Pertnjara Group). Conglomerate, pebbly sandstone, rare siltstone.||||||05-NOV-04
26188|Undandita Member|9814|5|Briefly described|Map Legend|Devonian|Devonian|Of the Brewer Conglomerate. Conglomerate with sedimentary clasts, sandstone lenses.||||||
26188|Undandita Member|22760|4|Described|p343|||Of the Brewer Conglomerate.  Organic matter, including spores, leaves and woody material, is commonly preserved in beds with an early diagenetic carbonate cement p345.||||||13-DEC-06
26188|Undandita Member|22804|5|Briefly described|p454|Devonian|Devonian|Of the Brewer Conglomerate.  Age - Famennian-Frasnian.||||||13-DEC-06
26188|Undandita Member|22826|4|Described|p575|Devonian|Devonian|Of the Brewer Conglomerate.||||||13-DEC-06
26188|Undandita Member|23858|5|Briefly described|p916|Late Ordovician|Late Ordovician|Of Brewer Conglomerate. Geological Province: Amadeus Basin.||||||
26188|Undandita Member|31566|2|Defined|p243|Devonian|Devonian|See also p244.||||||13-DEC-06
26188|Undandita Member|32209|6|Mentioned|Map legend|Devonian|Devonian|||||||
26188|Undandita Member|32640|6|Mentioned|p236|||||||||
26188|Undandita Member|35102|6|Mentioned|p39|||||||||
26188|Undandita Member|38885|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26188|Undandita Member|39583|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
26188|Undandita Member|41125|6|Mentioned|p40|||||||||
26188|Undandita Member|41270|6|Mentioned|p278|||||||||
26188|Undandita Member|41385|6|Mentioned|Fig.12|||||||||
26188|Undandita Member|41492|6|Mentioned|p158|||||||||
26188|Undandita Member|43225|5|Briefly described|Map Legend||Devonian|Of the Brewer Conglomerate.||||||13-DEC-06
26188|Undandita Member|43503|6|Mentioned|42-45|Late Devonian|Middle Devonian|||||||
26188|Undandita Member|43748|6|Mentioned|p36|||Late Devonian age. Has tilted duricrust capping indicating uplift in western MacDonnell Ranges in the Pliocene or Pleistocene.||Of Brewer Conglomerate.||||07-OCT-15
26188|Undandita Member|47050|6|Mentioned|p250|||||||||
26188|Undandita Member|60547|5|Briefly described|Map Legend|Devonian|Devonian|Of the Brewer Conglomerate. Conglomerate, pebbly sandstone, rare siltstone. Geological Province: Amadeus Basin.||||||03-JUN-05
26188|Undandita Member|65232|5|Briefly described|p10, p72|Late Devonian|Late Devonian|Of Brewer Conglomerate. Hosts sandstone-type uranium; associated with redox boundaries. Fluviatile pebbly sandstone, minor siltstone and conglomerate. Geol. Prov: Amadeus Basin.||||||09-FEB-10
26188|Undandita Member|69438|4|Described|p23:40, 50-52|Famennian|Famennian|Jones (1972) defined this unit as an upper succession of conglomeratic sandstones that can be distinguished from more massive conglomerates below. Variable thickness, up to an estimated 1000m. Hosts sedimentary U deposits at Angela and Pamela, and several other localities to the E; detailed descriptions.||Brewer Conglomerate.||Locally interdigitates with or is transitional over Ljiltera Member (Hermannsburg Sandstone).|Massive, or less commonly trough cross-bedded, coarse- to very coarse-grained conglomeratic and pebbly lithic sandstone, interlayered with conglomerate. Bedding appears uniformly 1-3m thick.|12-JUL-16
26188|Undandita Member|69673|5|Briefly described|p67|||Host to sedimentary Uranium deposits.||Brewer Conglomerate|||Conglomeratic sandstones.|
26188|Undandita Member|71279|5|Briefly described|p370|Late Devonian|Late Devonian|Amadeus Basin. Hosts uranium mineralisation.||Brewer Conglomerate.|||Conglomerate with beds of dark grey shale.|
28281|Unimbra Sandstone|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup, Hatches Creek Group. Quartz arenite and lithic/feldspathic arenite, commonly pebbly.||||||07-NOV-08
28281|Unimbra Sandstone|23733|5|Briefly described|p5|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup.||||||07-NOV-08
28281|Unimbra Sandstone|23809|5|Briefly described|p27|||Of the lower part of the Wauchope Subgroup (Hatches Creek Group).  Overlies the Junalki Formation.  Geological Province: Davenport Province.||||||
28281|Unimbra Sandstone|23823|5|Briefly described|p79 Fig. M3|||See also Unimbra sandstone - both names treated as informal in this study.||||||07-FEB-11
28281|Unimbra Sandstone|24089|5|Briefly described|p27 Fig. 15|||Of Hatches Creek Group.||||||
28281|Unimbra Sandstone|24172|5|Briefly described|p8 Tb.1, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Underlain by Junalki Formation. Geological Province: Tennant Creek Inlier. Of Hatches Creek Group. Conformable contact with Junalki Formation. Parts now included in Junalki Formation.||||||07-NOV-08
28281|Unimbra Sandstone|39624|5|Briefly described|Table 1|||||||||
28281|Unimbra Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28281|Unimbra Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Feldspathic arenite, commonly pebbly; minor quartz arenite, conglomerate, siltstone, partly volcaniclastic arenite.||||||10-JAN-05
28281|Unimbra Sandstone|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
28281|Unimbra Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28281|Unimbra Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Feldspathic arenite; subordinate quartz arenite; minor pebbly arenite and felsic lava. Geological Province: Tennant Creek Block.||||||07-NOV-08
28281|Unimbra Sandstone|41204|4|Described|Table 1|||||||||
28281|Unimbra Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Quartz arenite and lithic/feldspathic arenite, commonly pebbly; minor felsic volcanics.||||||16-NOV-05
28281|Unimbra Sandstone|41308|5|Briefly described|Table 2|||Mention p12.||||||13-DEC-06
28281|Unimbra Sandstone|41310|4|Described|Table 1|||See also p11.||||||13-DEC-06
28281|Unimbra Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
28281|Unimbra Sandstone|41524|4|Described|Table 1|||||||||
28281|Unimbra Sandstone|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Feldspathic arenite; minor felsic volcanics.||||||07-NOV-08
28281|Unimbra Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
28281|Unimbra Sandstone|42504|6|Mentioned|Fig. 22 P102|||||||||
28281|Unimbra Sandstone|42643|4|Described|p11, Table 1 p7|||||||||
28281|Unimbra Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Feldspathic/kaolinitic arenite, pebbly; conglomerate; minor quartz arenite, arkose, lithic arenite, micaceous siltstone; local volcaniclastic arenite.||||||07-NOV-08
28281|Unimbra Sandstone|43224|5|Briefly described|Map legend||Paleoproterozoic|Of the Wauchope Subgroup.||||||07-NOV-08
28281|Unimbra Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
28281|Unimbra Sandstone|45167|3|Fully described|Table 1|||Of the Wauchope Subgroup.||||||13-DEC-06
28281|Unimbra Sandstone|49033|2|Defined|p16|Proterozoic|Proterozoic|||||||
28281|Unimbra Sandstone|50588|5|Briefly described|p3.4, 4.4|||Geological Province: Tennant Creek/Davenport Province. Of the Wauchope Subgroup. Intruded by Treasure Suite, Devils Suite.||||||13-DEC-06
28281|Unimbra Sandstone|60681|5|Briefly described|Map legend|Statherian|Statherian|Of the Hatches Creek Group. Arenite, volcaniclastic arenite.  Geological Province: Davenport Province.||||||11-JAN-05
28281|Unimbra Sandstone|60684|4|Described|p12, p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Quartz arenite and pebble conglomerate, with interbedded adesitic lava flows. Conformably overlies Junalki Formation (Flynn Subgroup). Geological Province: Davenport province.||||||07-NOV-08
28281|Unimbra Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lower Wauchope Subgroup (Hatches Creek Group). Subarkosic, sublithic and lithic (partly volcaniclastic?) arenite and quartz arenite, commonly pebbly; minor conglomerate, greywacke and pyroclastic rocks. In the Tennant Creek region.||||||07-NOV-08
28281|Unimbra Sandstone|61567|5|Briefly described|p632, p633 Tb. 1|Paleoproterozoic|Paleoproterozoic|Basal unit of Wauchope Subgr. (Hatches Creek Gr.) White, ridge-forming quartzo-feldspathic to lithic arenite. Displays shatter cones related to Amelia Creek impact structure. Overlies Ooradidgee Subgr; underlies Yeeradgi Sst. Max. thickness: 400m.||||||07-NOV-08
28281|Unimbra Sandstone|64735|5|Briefly described|p205 Fig 1, p206 Fig 2, p212-213|Orosirian|Orosirian|Maximum depositional age from youngest detrital zircons in a  medium-grained quartzite. Intruded by dolerite sills.|1835 +/- 40 Ma or 1838 +/- 16 Ma.|Of Wauchope Subgroup, Hatches Creek Group.||Overlies Warnes Sandstone Member.|Includes rare hematite shale clasts.|30-APR-12
28281|Unimbra Sandstone|64956|6|Mentioned|p26|||Geological province: Davenport Province.||||||07-FEB-11
28281|Unimbra Sandstone|65209|5|Briefly described|p35 Fig.1, p37, p38|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup. Interpreted to record a marine transgression and subsequent regression. Base of Unimbra Sandstone correlates with base of Manga Mauda Member; variably overlies and locally interfingers with Treasure Volcanics; variably overlies Edmirringie Volcanics, Epenarra Volcanics, Taragan Sandstone, Woodenjerrie beds and Junalki Formation. Is overlain unconformably by Andagerra Formation. Correlated with Rising Sun Conglomerate. Geol. Prov: Davenport Province.||Wauchope Subgroup||||05-JAN-17
28281|Unimbra Sandstone|65333|5|Briefly described|Map Legend|Statherian|Statherian|Basal unit of Wauchope Subgroup, Hatches Creek Group, Davenport Province. Underlies Newlands Volcanics. Subarkosic/sublithic/lithic arenite; quartz arenite.||||||29-SEP-11
28281|Unimbra Sandstone|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of lower Wauchope Subgroup (Hatches Creek Group),  Davenport Province. Underlies Newlands Volcanics. Subarkosic/sublithic/lithic arenite; quartz arenite.||||||
28281|Unimbra Sandstone|65338|5|Briefly described|p8 Table 1, p6, p19. |Paleoproterozoic|Paleoproterozoic|||Basal unit of Hatches Creek Group.|||Quartz-rich sandstone.|
28281|Unimbra Sandstone|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup, Hatches Creek Group.||Is overlain by Yeeradgi Sandstone.|Feldspathic arenite; subordinate quartz arenite; minor pebbly arenite and felsic lava.|17-OCT-11
28281|Unimbra Sandstone|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Hatches Creek Group.||Is overlain by Newlands Volcanics.|Non-outcropping: inferred subarkosic/sublithic/lithic arenite, quartz arenite; minor pyroclastic rocks.|
28281|Unimbra Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Ooradidgee Group. Is overlain by Yeeradgi and Newlands Volcanics. Shown as lateral equivalent to Gwynne Sandstone.|Subarkosic, sublithic and lithic (partly volcaniclastic?) arenite and quartz arenite, commonly pebbly; minor conglomerate, greywacke and pyroclastic rocks.|08-DEC-14
28281|Unimbra Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1838 +/- 16 Ma (maximum depositional age).|Hatches Creek Group.||||
28281|Unimbra Sandstone|67352|4|Described|p10 Tb.1, p44 fig 48, p45|Orosirian|Orosirian|1000 m thick. Shallow marine and fluviatile. Major bevelled ridges.||Wauchope Subgroup||Overlies Mia Mia Volcanics or Treasure Volcanics. Overlain by Yeeradgi Sandstone (conformably).|Feldspathic, quartz arenite: medium bedded, medium-to coarse-grained, moderately well sorted; minor rhyolite and felsic lava lenses; pebble lenses near base.|
28281|Unimbra Sandstone|68518|4|Described|p8 Tb.1, p12, p13|Proterozoic|Proterozoic|Max. thickness: 1500 m. Local variation in thickness may be due to disposition on an uneven volcanic surface. Intruded by quartz dolerite.||Basal formation in Wauchope Subgroup||Conformable, disconformable over, and interfingers with Mia Mia Volcanics, Treasure Volcanics, Kurinelli Sandstone; overlain conformably by Yeeradgi Sandstone and unconformably by Cambrian strata.|Ridge-forming variably feldspathic/lithic arenite, minor quartz arenite, arkose, quartz greywacke.|30-MAY-16
28281|Unimbra Sandstone|68697|5|Briefly described|p24|||||Basal Hatches Creek Group.||Overlies and interdigitates with Treasure Volcanics. Is overlain by Yeeradgi Sandstone and Arabulja Volcanics.||
28281|Unimbra Sandstone|69187|6|Mentioned|p53 Fig.2|||Davenport Province.||||||
28281|Unimbra Sandstone|69424|5|Briefly described|p9:3, 5-6, 8, 10, 17-18, 24, 26-28|Paleoproterozoic|Paleoproterozoic|Davenport Province. Shallow marine and fluvial sediments; rapidly deposited.||Wauchope Subgroup.||Overlies Woodenjerrie beds unconformably. Unconformably and conformably (interfingering) overlies Treasure Volcanics.||12-JUL-16
28281|Unimbra Sandstone|69425|4|Described|p10:1,3,5-16,19-21,23, 24 Figs. 10.18,19|Statherian|Statherian|Marks the boundary between Davenport and Warramunga Provinces. Basal Hatches Creek Group. A marine transgressive/regressive succession: variably fluvial to shallow-marine. Ridge-forming. 100-1500m thick. Age range from surrounding units. Maximum deposition age of 1858 +/- 6 Ma (Claoue-Long et al., 2008). Interfingers with Epenarra and Treasure Volcanics, but also locally overlies Treasure Volcanics and Kurinelli Sandstone unconformably. Is overlain conformably by Yeeradgi Sandstone and Newlands Volcanics. Is intruded by Devils Marbles Granite and Treasure Suite. Correlative of Gwynne Sandstone and (in part) Rising Sun Conglomerate, Blanche Creek Member and Manga Mauda Member.|1817-1811 Ma.|Base of lower Wauchope Subgroup.||Overlies Junalki Formation and Woodenjerrie beds unconformably; Mia Mia, Epenarra, Edmirringee, Treasure Volcanics and Kurinelli and Taragan Sandstones conformably/disconformably.|Medium- to coarse-grained, poorly to moderately well-sorted, medium to thickly bedded, feldspathic/lithic (partly volcanilithic?) and quartz sandstone, commonly pebbly; minor conglomerate, greywacke, siltstone, felsic lava and pyroclastic rocks.|12-JUL-16
28281|Unimbra Sandstone|69427|5|Briefly described|p12:13|||Davenport Province.||||Correlated with Gwynne Sandstone.||12-JUL-16
28281|Unimbra Sandstone|69431|6|Mentioned|p16:5, 14, 22|||Davenport Province. Folding during the Davenport Event is discussed.||Wauchope Subgroup.||||12-JUL-16
28281|Unimbra Sandstone|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1858+/-6 Ma (MDA: U-Pb zircon SHRIMP)||||Sandstone.|
28281|Unimbra Sandstone|73083|6|Mentioned|p19, p21, p23, p44|||Davenport Province||Wauchope Subgroup||Overlain by Kudinga Basalt.||
28281|Unimbra Sandstone|73124|6|Mentioned|p2 Fig.1|||||||||
28281|Unimbra Sandstone|73125|6|Mentioned|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||||||
28281|Unimbra Sandstone|73460|6|Mentioned|p2|||Warramunga Province.||||||
28281|Unimbra Sandstone|73590|6|Mentioned|p2|||||||||
26967|Uniya Formation|9324|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Tillite, glacio-lacustrine arenite with dropstones; glacio-fluvial conglomerate.||||||
26967|Uniya Formation|9579|5|Briefly described|Map Sheet|Neoproterozoic|Neoproterozoic|Late Proterozoic age.||||||
26967|Uniya Formation|22809|3|Fully described|17|Proterozoic|Proterozoic|||||||
26967|Uniya Formation|22813|5|Briefly described|Map|Neoproterozoic|Neoproterozoic|Tillite, sandstone, siltstone.||||||19-OCT-05
26967|Uniya Formation|23714|4|Described|p36|Proterozoic|Proterozoic|See also page 7 table 1. Max. thickness: 30 m.||||||
26967|Uniya Formation|23715|5|Briefly described|Map legend||Proterozoic|In the Litchfield Province.||||||13-DEC-06
26967|Uniya Formation|40765|6|Mentioned|Fig.3|||||||||
26967|Uniya Formation|41645|6|Mentioned|Fig.4|||||||||
26967|Uniya Formation|41646|6|Mentioned|Map legend|Neoproterozoic||Diamictite, sandstone, siltstone.||||||17-OCT-05
26967|Uniya Formation|41660|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Diamictite; glaciolacustrine arenite and siltstone with dropstones; glaciofluvial conglomerate (137m proved in drillhole NTGS 83/1).||||||07-OCT-05
26967|Uniya Formation|41661|5|Briefly described|Table 1|||||||||
26967|Uniya Formation|41980|6|Mentioned|p585|||||||||
26967|Uniya Formation|42014|5|Briefly described|Map legend|Neoproterozoic||||||||
26967|Uniya Formation|43187|5|Briefly described|p2|||||||||
26967|Uniya Formation|63866|5|Briefly described|p108|Neoproterozoic|Neoproterozoic|Litchfield Province, Pine Creek Orogen. Crops out south of Daly River and on the eastern edge of the Wingate Plateau.||||Unconformably overlies the Tolmer Group. Overlies the Auvergne Group.|Glacial sedimentary rocks.|
26967|Uniya Formation|64104|6|Mentioned|p70 fig 7, p72|||[Author has consistently mis-spelt Edgoose as Edgegoose in bibliographic references]||||Correlated with Moonlight Valley Formation.||
26967|Uniya Formation|67167|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Tillite, glacio-lacustrine sandstone with dropstones, glacio-fluvial conglomerate.|
26967|Uniya Formation|67186|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic||||||Tillite, glacio-lacustrine sandstone with dropstones, glacio-fluvial conglomerate.|23-NOV-11
26967|Uniya Formation|68244|6|Mentioned|p659-p660|Neoproterozoic|Neoproterozoic|Geological province: Litchfield Province, Pine Creek Orogen. Small Meoproterozoic outlier glaciogenic deposits.||||||21-JUN-19
26967|Uniya Formation|69432|6|Mentioned|p17:6|||Wolfe Basin.||||Overlies Hinde Dolostone.||12-JUL-16
26967|Uniya Formation|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Cryogenian|Victoria/Wolfe Basins, Centralian A Superbasin. Supersequence 3. Ungrouped. ||||Is overlain by Ranford Formation.|Glacigene sedimentary rocks.|12-JUL-16
26967|Uniya Formation|69442|4|Described|p27:1; 2 Fig.27.2; 3 Tb.27.1; 5-6|||Dundas et al. (1987); Edgoose et al. (1989). Includes and supersedes the former Uniya Tillite, and the Jarong Conglomerate (Pontifex and Mendum, 1972; Sweet et al., 1974). Assigned to the Wolfe Basin by Dunster (this study: 2013), but not explicitly to the Duerdin Group. Typically 60-80m thick; 137m thick in drillhole NTGS 83/1. Glacial, fluvio-glacial and glaciolacustrine deposits. Correlated with Moonlight Valley Tillite.||||Unconformably overlies Soldiers Creek Granite, Stray Creek Sandstone, Hinde Dolostone, Saddle Creek Formation and Angalarri Siltstone. Is overlain by Antrim Plateau Volcanics.|Dominantly a true tillite, variously described as a polymictic conglomerate or diamictite, subordinate interbedded sandstone, varved carbonate/siltstone (possibly a cap carbonate).|12-JUL-16
26967|Uniya Formation|69445|6|Mentioned|p30:3-4|||Includes the former Jarong Conglomerate of Pontifex and Mendum (1972), Sweet et al. (1974).||||||12-JUL-16
26967|Uniya Formation|69673|5|Briefly described|p190|||137m thick.|||||Polymictic conglomerate and diamictite with subordinate interbedded sandstone.|
26967|Uniya Formation|70866|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||||Overlies Tolmer Group and (unconformably) the Mamadawerre Sandstone (Kombolgie Subgroup).|Diamictite, glaciolacustrine sandstone with dropstones, fluvioglacial conglomerate.|05-MAR-18
30318|Urapunga Granite|22479|5|Briefly described|fig4, pg10|Orosirian|Orosirian|||||||
30318|Urapunga Granite|22600|6|Mentioned|Map legend|||||||||
30318|Urapunga Granite|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
30318|Urapunga Granite|23374|5|Briefly described|Fig3p5||Paleoproterozoic|||||||07-NOV-08
30318|Urapunga Granite|23398|5|Briefly described|p433|Orosirian|Orosirian|||||||
30318|Urapunga Granite|23937|2|Defined|p94 App. 1|Orosirian|Orosirian|Previously mapped as part of the now redefined "Mount Reid beds" of Dunn (1963c).  Intrudes Mount Reid Rhyolite.  Age: 1858+/-7Ma (Page et al, 2000).  Nonconformably overlain by Mount Birch Sandstone. Geological Province: McArthur Basin.||||||18-APR-05
30318|Urapunga Granite|24047|6|Mentioned|p40|||Geological Province: McArthur Basin.||||||
30318|Urapunga Granite|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
30318|Urapunga Granite|50591|5|Briefly described|p5.1|Paleoproterozoic|Paleoproterozoic|Age: 1858 +/- 7Ma. Supersedes 'Roper River granite'. Geological Province: Arnhem Block/McArthur Basin.||||||07-NOV-08
30318|Urapunga Granite|60573|5|Briefly described|Map legend|Orosirian|Orosirian|Does not outcrop in the Roper River mapsheet area.  See also in regional Setting map legend.||||||15-FEB-05
30318|Urapunga Granite|61390|5|Briefly described|Map Legend|Orosirian|Orosirian|Biotite Granite: coarse grained.||||||
30318|Urapunga Granite|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
30318|Urapunga Granite|63112|6|Mentioned|p1190|||Part of basement to southern McArthur Basin.||||||
30318|Urapunga Granite|63866|5|Briefly described|p114|Orosirian|Orosirian|Walker/Urapunga Fault Zones. Associated with the extrusion of the Mount Reid Rhyolite.|1858 +/- 7 Ma (Page et al., 2000)|||||
30318|Urapunga Granite|69429|5|Briefly described|p14:3-4|Paleoproterozoic|Paleoproterozoic|Urapunga Inlier. Coeval with Mount Reid Rhyolite. SHRIMP U-Pb zircon age.|1858 +/- 7 Ma (Abbott et al., 2001).||||Non-foliated biotite granite containing K-feldspar megacrysts up to 2cm long.|12-JUL-16
30318|Urapunga Granite|69430|6|Mentioned|p15:24-25, 30|||||||Is overlain unconformably by Mount Birch Sandstone (Nathan Group) and Katherine River Group.||12-JUL-16
30318|Urapunga Granite|70284|6|Mentioned|p1245|||||||||
30318|Urapunga Granite|70968|6|Mentioned|p6, p13||||1850 Ma.|||Is overlain nonconformably by Limmen Sandstone (Roper Group).||
30318|Urapunga Granite|71592|5|Briefly described|Appendix A.|||Urapunga Inlier.|1858+/-7 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30318|Urapunga Granite|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Basement to McArthur Basin.||||||06-MAR-20
30318|Urapunga Granite|71779|5|Briefly described|p5|Orosirian|Orosirian|McArthur Basin.|c. 1850 Ma (Abbott et al, 2001)|||Disconformably or unconformably overlain by the Roper Group.||
30318|Urapunga Granite|72373|5|Briefly described|p27|||||||Locally overlain unconformably by Mount Birch Sandstone.||
30318|Urapunga Granite|72919|6|Mentioned|p7|Orosirian|Orosirian|Urapunga Inlier. An age of 1858 +/- 7 Ma was reported by Page et al. (2000).|1858 +/- 7 Ma|||||
33487|Utanta Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mantarurr Granite Suite. Felsic, coarsely porphyritic foliated biotite granite.   Age: ~1170Ma.||||||
33487|Utanta Granite|60683|2|Defined|p58 Appendix, p18|Mesoproterozoic|Mesoproterozoic|Of the Mantarurr Granite Suite.  Felsic coarsely porphyritic biotite granite.  Has sharp intrusive contact with the Wala Wuru Granite.  See also p10 Tb. 1.||||||13-DEC-06
33487|Utanta Granite|61154|6|Mentioned|p44 Appendix|||Of the Pitjantjatjara Supersuite.||||||
33487|Utanta Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Mantarurr Granite Suite. Felsic coarsely porphyritic foliated biotite granite.  Age: ~1170Ma. Geological Province: Musgrave Block.||||||19-OCT-05
24549|Vaddingilla Formation|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
24549|Vaddingilla Formation|23809|5|Briefly described|p27 Fig.25|||Of the Hanlon Subgroup (Hatches Creek Group).  Geological Province: Davenport Province.||||||30-NOV-04
24549|Vaddingilla Formation|23823|5|Briefly described|p75|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group (upper). Feldspathic and micaceous sandstone and siltstone which may be tuffaceous. Max. thickness: ~700m. Geological Province: Davenport Geosyncline.||||||07-FEB-11
24549|Vaddingilla Formation|39624|5|Briefly described|Table 1|||||||||
24549|Vaddingilla Formation|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24549|Vaddingilla Formation|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Siltstone; shale; feldspathic and micaceous arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24549|Vaddingilla Formation|41129|4|Described|Table 1|||||||||
24549|Vaddingilla Formation|41308|5|Briefly described|Table 2|||||||||
24549|Vaddingilla Formation|41408|6|Mentioned|Map legend|Proterozoic||||||||
24549|Vaddingilla Formation|41970|6|Mentioned|Fig.3 P333|||||||||
24549|Vaddingilla Formation|42643|5|Briefly described|p12|||Of the Hanlon Subgroup.||||||13-DEC-06
24549|Vaddingilla Formation|43802|6|Mentioned|p80|||||||||
24549|Vaddingilla Formation|45167|3|Fully described|Table 1|||Of the Hanlon Subgroup.||||||13-DEC-06
24549|Vaddingilla Formation|49033|2|Defined|p29|Proterozoic|Proterozoic|||||||
24549|Vaddingilla Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Siltstone, shale, fedlspathic/lithic and micaceous arenite. Overlies Canulgerra Sandstone; underlies Yaddanilla Sandstone. In the Tennant Creek region.||||||07-NOV-08
24549|Vaddingilla Formation|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||||
24549|Vaddingilla Formation|65338|6|Mentioned|p20.|||||Unit in Hanlon Subgroup.||||
24549|Vaddingilla Formation|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup, Hatches Creek Group .||Overlies Canulgerra Sandstone. Is overlain by Yaddanilla Sandstone.|Siltstone; shale; feldspathic and micaceous arenite.|19-OCT-11
24549|Vaddingilla Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Canulgerra Sandstone. Is overlain by Yaddanilla Sandstone.|Siltstone, shale, feldspathic/lithic and micaceous arenite.|
24549|Vaddingilla Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24549|Vaddingilla Formation|67352|4|Described|p9, p44 fig 48|Statherian|Statherian|Marine; recessive. 800 m thick.||Hanlon Subgroup||Overlies Canulgerra Sandstone (conformably).  Overlain by Yaddanilla Sandstone (conformably).|Siltstone, shale; friable, fine- to-medium-grained, feldspathic and micaceous arenite.|
24549|Vaddingilla Formation|69425|5|Briefly described|p10:3, 10-12, 19-20|Statherian|Statherian|NE Davenport Province. 800m thick. Probably marine.||Hanlon Subgroup.||Conformably overlies Canulgerra Sandstone. Is overlain conformably by Yaddanilla Sandstone. Correlated with Attack Creek Formation.|Siltstone, shale and variably feldspathic/lithic and micaceous sandstone.|12-JUL-16
24549|Vaddingilla Formation|69431|6|Mentioned|p16:5|||Davenport Province.||Hanlon Subgroup.||||12-JUL-16
75902|Valley Metamorphics|69917|5|Briefly described|p147-148, 152, 153-154, 1|||Eastern Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating, Hf analytical data. Incorporated as rafts of metasediments in the Ambulbinya Supersuite. Dating attempted on 2 samples. Second gives an age of 2514+/-10 Ma for the maximum depositional age.|2512.6+/-7.5 Ma max deposit||||Garnet-muscovite-biotite schist.|
75902|Valley Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|2514+/-10 Ma (MDA: U-Pb zircon LA-ICPMS).||||Metapsammite, schist.|
30314|Vizard Group|22538|4|Described|Fig4, P710, P717|Calymmian|Statherian|Part of the Glyde package.||||||13-DEC-06
30314|Vizard Group|23937|2|Defined|p95 App. 1|Statherian|Statherian|Supersedes Vizard Fm (McArthur Gp).  Constituents are: Saint Vidgeon and Nagi Fms.  Unconformably overlain by Mount Birch Sst.  Age: 1640+/-4Ma (St Vidgeon Fm) and 1634+/-4Ma (Nagi Fm).  Thickness in type section: 330m.  Geol.Prov: McArthur Basin.||||||
30314|Vizard Group|24047|5|Briefly described|p12 Fig. 10|Paleoproterozoic|Paleoproterozoic|Age: ~1640Ma.  Geological Province: McArthur Basin.||||||07-NOV-08
30314|Vizard Group|60483|5|Briefly described|p7 Fig. 5|||Includes Mount Reid, Saint Vidgeon and Nagi Formations. Geological Province: McArthur Basin. Mount is Mt in text, Saint is St. ||||||
30314|Vizard Group|60573|5|Briefly described|Map legend|Statherian|Statherian|Includes the Nagi and Saint Vidgeon Formations.  Does not outcrop in the Roper River mapsheet area.||||||13-DEC-06
30314|Vizard Group|60574|5|Briefly described|Map Legend|||Geological Province: McArthur Basin.||||||
30314|Vizard Group|61390|5|Briefly described|Map Legend|Statherian|Statherian|||||||
30314|Vizard Group|63866|5|Briefly described|p114, p123|||Urapunga Fault Zone. Partially equivalent to the Balma Group and the Habgood Group. |||Includes the Saint Vidgeon Group and the Nagi Formation.|||
30314|Vizard Group|64724|5|Briefly described|p46|Proterozoic|Proterozoic|McArthur Basin unit deposited as part of sedimentation in the Isa Superbasin (1660-1590 Ma)||||||
30314|Vizard Group|64817|6|Mentioned|p352 Fig.3, p353 Fig.4 ||||||Includes Nagi Formation, Saint Vidgeon Formation and Mount Reid Formation.|||
30314|Vizard Group|65228|5|Briefly described|Measured section.||||||Includes Nagi and Saint Vidgeon Formations.|Equivalent to McArthur Group.||
30314|Vizard Group|65340|6|Mentioned|p10 Fig.5.|||||||||
30314|Vizard Group|69429|6|Mentioned|p14:4 Fig.14.6|||||||||12-JUL-16
30314|Vizard Group|69430|4|Described|p15:2-4, 14, 18, 22-23, 25, 30|||Abbott et al. (2001); previously the Vizard Formation (Dunn, 1963) of the McArthur Group. Southern McArthur Basin. c.300m thick. Possible equivalent of upper McArthur Group.|||Saint Vidgeon, Nagi Formations.|Is overlain unconformably by Mount Birch Sandstone (Nathan Group).|Stromatolitic carbonates and fine-grained siliciclastic rocks.|12-JUL-16
30314|Vizard Group|69673|6|Mentioned|p16 fig 13|Statherian|Statherian|Urapunga Fault Zone|||Includes Nagi Formation, Saint Vidgeon Formation|||
30314|Vizard Group|70968|6|Mentioned|p2 Fig.3, p7|||||||Locally thrust over Phelp Sandstone.||
30314|Vizard Group|71059|6|Mentioned|p2|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||||||
30314|Vizard Group|71374|6|Mentioned|p2|||southern McArthur Basin.||||||
30314|Vizard Group|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin. Unnecessarily informally subdivided into Lower and Upper parts.||||||04-MAR-20
30314|Vizard Group|72373|5|Briefly described|iii,p1-2,24|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. From URAPUNGA map sheet. |||Includes Nagi Formation.|||
30314|Vizard Group|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin.|||Includes Nagi Formation and Saint Vidgeon Formation.|Shown as underlying Nathan Group.||
30314|Vizard Group|72718|6|Mentioned|p5 Tb.1, p7|||McArthur Basin. Isa Superbasin of Jackson et al. (1999, 2000). Glyde package. Urapunga Fault Zone.|||Nagi Formation, Saint Vidgeon Formation.|Unconformably overlain[?] by Mount Birch Sandstone (Nathan Group).||
30314|Vizard Group|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the Urapunga Fault Zone. U-Pb zircon sedimentary depositional ages given.|1640 +/- 4 Ma to 1634 +/- 4 Ma||Nagi Formation and Saint Vidgeon Formation.|Unconformably underlies Nathan Group.||
30314|Vizard Group|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.|||Nagi Formation, Saint Vidgeon Formation|Unconformably overlain(?) by Mount Birch Sandstone (Nathan Group).||
23115|Wabudali Granite|24197|5|Briefly described|p61 Tb. 4.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Suite (or Southwark Granite Suite?). Age: 1567Ma, by correlation with Yarunganyi Granite date. Geological Province: Arunta Inlier.||||||07-FEB-11
23115|Wabudali Granite|43275|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23115|Wabudali Granite|43631|3|Fully described|p15-17||Mesoproterozoic|Age: 1750 Ma||||||
23115|Wabudali Granite|43749|6|Mentioned|p22|||||||||
23115|Wabudali Granite|44158|4|Described|p18, Table.1|Mesoproterozoic|Mesoproterozoic|Age: Probably between 1760 - 1570 Ma. In the Arunta Inlier. Intrudes Lander Rock beds, Yumurrpa Granophyre and Reynolds Range Group.||||||05-MAY-10
23115|Wabudali Granite|50369|5|Briefly described|p1.5, 24.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Southwark Suite.||||||07-NOV-08
23115|Wabudali Granite|61385|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Arunta Complex. Biotite-muscovte granite, commonly with abundant tabular feldspar megacrysts.||||||20-OCT-05
23115|Wabudali Granite|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Southwark Suite.  Biotite-muscovite granite with tabular feldspar megacrysts.  Age: <1760Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
23115|Wabudali Granite|62378|5|Briefly described|p5, 23, 33|||Geological Province: Arunta Region. Muscovite Granite. Intrudes the Reynolds Range Group.||||||
23115|Wabudali Granite|62632|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami/Arunta Region-Aileron Province. Biotite-muscovite granite with tabular feldspar megacrysts.||||||07-NOV-08
23115|Wabudali Granite|62633|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Biotite +/- muscovite granite, commonly with abundant fine to medium tabular feldspar phenocrysts.||||||07-NOV-08
23115|Wabudali Granite|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.|||||Biotite-muscovite granite with tabular feldspar megacrysts, commonly showing igneous flow alignment.|15-APR-11
23115|Wabudali Granite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Southwark Granite Suite, younger than Andrew Young Igneous Complex. Biotite-muscovite granite, commonly with abundant tabular feldspar megacrysts; low gravity response, low flat magnetite response||||||
23115|Wabudali Granite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Southwark Granite Suite, younger than Andrew Young Igneous Complex. Biotite-muscovite granite, commonly with abundant tabular feldspar megacrysts; low gravity response, low flat magnetite response||||||
23115|Wabudali Granite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Yunkanjini Granite, younger than 1770-1760Ma Yambah Event. Biotite +/- muscovite granite, abundant feldspar phenocrysts common, lesser fine to med. grained equigranular phase, rare biotite blebs and rafts of retrogressed metasediments||||||
23115|Wabudali Granite|65335|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Aileron Province. Biotite-muscovite granite with tabular feldspar megacrysts. Age: older than Chewings Event (1590-1570 Ma), younger than Strangways Event (1730-1700 Ma). ||||||
23115|Wabudali Granite|67163|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-muscovite granite with tabular feldspar megacrysts; low gravity response.|20-OCT-11
23115|Wabudali Granite|69288|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||||Biotite-muscovite granite with tabular feldspar megacrysts.|
23115|Wabudali Granite|69427|5|Briefly described|p12:40 Fig.12.34; 12:41|||Young et al. (1995). Western part of the Wabudali Range, and in outcrops up to 20km to the W, Aileron Province. Hosts Cu-W mineralisation in quartz veins and greisenised granite at Wilsons Find. Most likely age is 1730-1720 Ma or 1570-1530 Ma.||||Intrudes Lander Rock Formation and Pine Hill Formation (Reynolds Range Group).|Pale, undeformed to weakly foliated, medium- to coarse-grained biotite-muscovite granite with tabular white feldspar phenocrysts "up to 3 m" [!!? Surely cm: see Fig.12.35] long.|12-JUL-16
23115|Wabudali Granite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.|||||Biotite +/- muscovite granite, commonly with abundant fine to medium tabular feldspar phenocrysts, lesser fine- to medium-grained equigranular phase; rare biotite blebs and rafts of retrogressed metasediments.|
23115|Wabudali Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
23115|Wabudali Granite|71350|5|Briefly described|iii, p1, p6-p9, p14|Calymmian|Calymmian|Aileron Province. Sampled on CHILLA (5054) 1:100 000 Sheet area (which is a part of the SF52-05 1:250 000 sheet). Hosts veined tungsten mineralisation interpreted to be genetically related to granite emplacement. Hosts zircons that give inherited ages between ca 2384 and ca 1772 Ma. Grid reference for dated sample, zircon characteristics, SHRIMP analyses and results discussed.|1586 +/- 4 Ma (SHRIMP, magmatic crystallisation)|||Intrudes the Mount Thomas Quartzite.|Coarse megacrystic mica-K-feldspar granite.|
23115|Wabudali Granite|72366|5|Briefly described|p7|Calymmian|Calymmian|Geological province: Aileron Province. Exposed in western MOUNT DOREEN and southeast MOUNT THEO map sheets. Previously interpreted, and widely disparate, magmatic crystallisations ages include either c. 1730-1710 Ma or c. 1570-1530 Ma (Young et al 1995, Scrimgeour 2013). Subsequent SHRIMP U-Pb zircon dating yielded magmatic crystallisation age of 1586+\-4 Ma (Kositcin and McGloin 2017).|1586+\-4 Ma (magmatic)|||||
23115|Wabudali Granite|72376|5|Briefly described|p1|Calymmian|Calymmian|Geological province: Aileron Province. Magmatic zircon crystallisation age of 1586+\-4 Ma (207Pb/206Pb; Kositcin and McGloin 2017), interpreted as representing a maximum and likely true age for tungsten mineralisation at the Singleton Bore prospect (southwesternmost MOUNT THEO mapsheet) based on the field relationships that suggest a genetic relationship to granite emplacement. The new muscovite 40Ar/39Ar age of 1550+\-4 Ma from pegmatites intruding into Lander Rock Formation (NTGS MD15MVM015; this study) is comparable to the 1586+\-4 Ma age of Wabudali Granite; this likely represents a true age for tungsten mineralisation at the Singleton Bore prospect.|1586+\-4 Ma|||||
33982|Wade Creek Formation|24503|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone and mudstone. Geological Province: Victoria River  Basin.||||||19-MAY-15
33982|Wade Creek Formation|63866|5|Briefly described|p129-p130, p137|||Victoria River Basin.||||||
33982|Wade Creek Formation|64580|4|Described|map legend|Mesoproterozoic|Paleoproterozoic|Sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.||||||15-DEC-08
33982|Wade Creek Formation|69099|4|Described|GEOL_LUT_CSV files + geochron files|Mesoproterozoic|Mesoproterozoic|Victoria River Basin|||Includes Mount John Shale Member and two unnamed members.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone; also ferruginous chert breccia member.|04-AUG-15
33982|Wade Creek Formation|69165|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv. |||Includes Mount John Shale Member||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, mudstone and stromatolitic chert.|
33982|Wade Creek Formation|69634|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological province: Halls Creek Orogen. Of Victoria River Basin. Events: Alice Springs Orogeny; Yampi Orogeny D1/M1. See 100k_interpgeop_lut.csv, 500k_geologyp08_lut.csv, 500k_interpgeop_lut.csv.|1600-1000 Ma (Inferred)||Includes Mount John Shale Member.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone, chert breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix|
33982|Wade Creek Formation|70154|4|Described|100k_interpgeop_lut.csv|Mesoproterozoic|Mesoproterozoic|See also 500k_interpgeop_lut.csv.|1000-1600 Ma||||Fine to coarse grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone and thin bedded sandstone. Chert Breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix.|
33982|Wade Creek Formation|70826|6|Mentioned|p5 tbl 2, p10|Mesoproterozoic|Mesoproterozoic|Osmond Basin.||||||
33982|Wade Creek Formation|71267|4|Described|GEOL_LUT_CSV files|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). See 100k_interpgeop_lut.csv, 500k_interpgeop16_lut.csv, 2_5m_interpgeop15_lut.csv, 500k_interpgeop_lut.csv.|1600-1000 Ma (inferred)||Includes Mount John Shale Member.||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone, Chert breccia; angular to rounded chert fragments in a ferruginous chert-sandstone matrix|
33982|Wade Creek Formation|72034|5|Briefly described|500k_interpgeop16_lut|Mesoproterozoic|Mesoproterozoic|Osmond Basin.|||||Fine- to coarse-grained quartz sandstone, lithic quartz sandstone, pebbly sandstone, conglomerate, siltstone, and mudstone.|
74204|Wadeye Group|61542|4|Described|p276, p277 Fig. 2, p286|Westphalian|Namurian|Includes Point Spring Sandstone (formerly part of Weaber Group), Arco and Aquitaine Formations. Overlies Weaber Group; unconformably overlain by Kulshill Group. Geological province: Bonapart Basin/Petrel-Sub-basin.||||||07-FEB-11
74204|Wadeye Group|64630|5|Briefly described|p31 Fig.2, p37|Bashkirian|Serpukhovian|Province: Bonaparte Basin. Underlies the Kulshill Group, unconformably overlies the Weaber Group. Palynology age: S. ybertii.||||||18-JAN-10
74204|Wadeye Group|69452|4|Described|p36:4-5, 9, 11-12, 14-15, 17-18|Carboniferous|Carboniferous|Gorter et al. (2005). Gorter et al. (2008) referred to this succession as the Wadeye Sub-group and recommended it be included in the overlying Kulshill Group; this is not [?yet] the case. Petrel Sub-basin, Bonaparte Basin. Outcrops identified as Border Creek Member in AUVERGNE are no longer assigned to this Group. Late Mississippian to Early Pennsylvanian.|||Arco, Aquitaine Formations; Point Spring Sandstone.|Unconformably overlies Weaber Group. Is overlain unconformably by Kulshill Group.|Siltstone, shale, sandstone.|12-JUL-16
74204|Wadeye Group|69653|6|Mentioned|p10, 14|Carboniferous|Carboniferous|Petrel Sub-basin.|||Arco, Aquitaine Formations.|Overlies Weaber Group. Is overlain by Kulshill Group.||
74204|Wadeye Group|69673|6|Mentioned|p167, p170 fig 142 p171, p172|Carboniferous|Carboniferous||||Includes Arco Formation, Aquitaine Formation|Overlies Kingfisher Shale, overlain by Kuriyippi Formation, unconformably overlain by Kulshill Group||
74204|Wadeye Group|70061|5|Briefly described|Petrel Sub-basin Fig.3|Bashkirian|Serpukhovian|See also Regional geology: Fig.8, p5.|||Arco and Aquitaine Formations.|Overlies Weaber Group. Is overlain by Kulshill Group.||12-JUL-16
74204|Wadeye Group|71146|5|Briefly described|p6|Serpukhovian|Serpukhovian|Bonaparte Basin.||||Unconformably overlies the Weaber Group.|Mixed sandstone, mudstone and coal.|
74204|Wadeye Group|71267|5|Briefly described|1M_geologyp12_lut.csv||||||Includes Border Creek Formation, Point Spring Sandstone.|||
74204|Wadeye Group|73117|6|Mentioned|p11, p15, p31|Bashkirian|Serpukhovian|Bonaparte Basin. Approximately coeval with Reeves Formation. Lies below coarse siliciclastic facies with a 'possible glacial fingerprint'. Contains facies unlikely to yield conodonts. Palynozonation: S. ybertii.|||Aquitaine Formation, Arco Formation.|||
74204|Wadeye Group|73184|6|Mentioned|p200, p201 Fig.12|||Bonaparte Basin, southeast. Possibly glaciogenic.||||||
40035|Wadjeli Sandstone Member|23937|2|Defined|p95 App. 1|Calymmian|Calymmian|Previously mapped at upper boundary of Limmen Sandstone (Dunn, 1963a, 1963c).  Together with Gibb Member now reassigned to lower Mainoru Fm (Abbott and Sweet, 2001).  Age: >1493+/-4Ma.  Max. thick: 15m.  Geological Province: McArthur Basin.  See also p31.||||||03-NOV-04
40035|Wadjeli Sandstone Member|24047|5|Briefly described|p22-23, p26|||Of the Mainoru Formation.  Geological Province: McArthur Basin.  Referred to as Wadjeli Sandstone in Fig. 10, p12 - abbreviated?||||||14-DEC-06
40035|Wadjeli Sandstone Member|60573|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mainoru Formation (Roper Group). Together with other members appears as Wadjeli Sandstone only in map legend. Quartz sandstone, fine-grained, medium bedded, crossd-stratified, ripple marked.||||||
40035|Wadjeli Sandstone Member|61390|5|Briefly described|Map Legend|Ectasian|Calymmian|Of the Mainoru Formation. Quartz sandstone: fine grained, medium bedded, cross-stratified, ripple marked.||||||
40035|Wadjeli Sandstone Member|69430|4|Described|p15:26-27, 30-31, 52|Calymmian|Calymmian|Abbott et al. (2001). McArthur Basin. 15m thick. Storm-dominated shelf to coastal tidal platform sediments. Hosts the Kipper Creek iron prospect.||Mainoru Formation.||Conformably overlies Gibb Member. Is overlain conformably by Nullawun Member.|Medium bedded, medium to fine sandstone; minor oolitic ironstone and ferruginous sandstone.|12-JUL-16
40035|Wadjeli Sandstone Member|70968|2|Defined|p13, p17-18, p20-25, p53, p69, p131|Calymmian|Calymmian|See also p140, p143-144. Young in Abbott et al. (2001). Originally mapped (Dunn, 1963) as upper part of Limmen Sandstone. Named after Wadjeli Lagoon, Roper Bar area. About 15m thick in the type section, 15km NE of Ngukurr, is at 481200mE 8382200mN (base) to 481500mE 8382600mN in URAPUNGA sheet. A resistant unit: caps Gibb Member, and is exposed as a cuesta. The ironstone is 2.6m average thickness, with 29.2 % Fe over 10km strike length. Has a distinctive dark tone on aerial photographs. Tidal platform sandstone facies. Lithology well described and illustrated.||Mainoru Formation.||Conformably and gradationally overlies Gibb Member. Is overlain probably conformably by Nullawun Member.|Medium- to fine- (less commonly coarse-)grained, grey-white quartz sandstone, ferruginous quartz sandstone, distinctive minor interbedded oolitic to pisolitic ironstone, and minor thinly interbedded mudrock.|10-NOV-17
40035|Wadjeli Sandstone Member|71059|4|Described|p3|Mesoproterozoic|Mesoproterozoic|McArthur Basin. 15m thick. Coastal tidal platform, possibly some non-marine, deposits.||Mainoru Formation.||Conformably overlies Gibb Member. Is overlain conformably by Nullawun Member.|Medium to fine quartz sandstone; minor ironstone and mudrock.|
40035|Wadjeli Sandstone Member|71494|4|Described|p4, p8-p9, p15, p17-p19, p26|||15m thick. Previously mapped at upper boundary of Limmen Sandstone (Dunn 1963b, 1963c). Deposited in a storm-dominated shelf to coastal tidal platform. Core log features presented in this volume.||||Conformably overlies the Gibb Member. Conformably overlain by the Nullawun Member.|Medium-bedded, medium to fine sandstone; minor ironstone and ferruginous sandstone.|03-MAY-18
40035|Wadjeli Sandstone Member|71779|5|Briefly described|p2 Fig.1|||Urapunga Region, McArthur Basin.||Mainoru Formation||||24-SEP-18
40035|Wadjeli Sandstone Member|73242|5|Briefly described|p39|||||Mainoru Formation, Collara Subgroup, Roper Group||Underlain by Gibb Member. Overlain by Nullawun Member.|Includes marine shelf sandstone.|
24629|Wagait Granite|9579|5|Briefly described|Map Sheet|Orosirian|Orosirian||ca. 1850-1840 Ma (Page, BMR)|||Synorogenic with the Murra-Kamangee Granodiorite, Mount Litchfield Granite.||
24629|Wagait Granite|23822|6|Mentioned|p303|||Geological Province: Litchfield Province.||||||
24629|Wagait Granite|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Wagait Suite. Age: ~1850Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
24629|Wagait Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24629|Wagait Granite|39803|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24629|Wagait Granite|39889|6|Mentioned|p485|||||||||
24629|Wagait Granite|40495|4|Described|p11|||||||||
24629|Wagait Granite|40764|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24629|Wagait Granite|40765|3|Fully described|p9|||||||||
24629|Wagait Granite|41980|5|Briefly described|Table 3 P575|||||||||
24629|Wagait Granite|50586|5|Briefly described|p1.1, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Wagait Suite.||||||07-NOV-08
24629|Wagait Granite|63866|5|Briefly described|p105|Orosirian|Orosirian|Litchfield Province,  Pine Creek Orogen. Age is consistent with earlier Rb-Sr age of 1852 +/- 33 Ma derived from Page et al., 1985.|1863 +/- 4 Ma (Worden et al., 2006b)|||||
24629|Wagait Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. I-type. Hornblende granodiorite, adamellite, mylonitised adamellite, biotite granite and granodiorite, epidotised granite, rarely porphyritic. Intrudes Fog Bay Metamorphics.||||||
24629|Wagait Granite|64730|5|Briefly described|p141-142|Paleoproterozoic|Paleoproterozoic|One of the few 1863 Ma I-type granites in Litchfield Province.||||||02-MAY-12
24629|Wagait Granite|64731|5|Briefly described|p148 Fig.3, p150|Proterozoic|Proterozoic|I-type.||||||12-APR-12
24629|Wagait Granite|64956|5|Briefly described|p2 Tb. 9, p66|Paleoproterozoic|Paleoproterozoic|Intrudes Welltree Metamorphics; underlies Moyle River Formation. Cryst. Age: 1863+/-4Ma. Geological province: Pine Creek Orogen. Sample is a K-feldspar megacrystic biotite hornblende granite.||||||07-FEB-11
24629|Wagait Granite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Wagait Suite.|||Hornblende-granodiorite, quartz monzonite, mylonitised quartz monzonite, biotite granite and granodiorite, epidotised granite, rarely porphyritic.|23-NOV-11
24629|Wagait Granite|67232|6|Mentioned|p4 Fig.3.|Paleoproterozoic|Paleoproterozoic|||Unit in Wagait Suite.||||
24629|Wagait Granite|69420|5|Briefly described|p5:18, 28-29, 100, 105|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Mineralogy described. SHRIMP U-Pb zircon age.|1863 +/- 3 Ma: Worden et al. (2008).|Wagait Suite.|||Mainly medium-grained granodiorite, monzogranite and granite. Saussuritisation and chloritisation of biotite are common.|12-JUL-16
24629|Wagait Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite, granodiorite|
24629|Wagait Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1863+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||K-feldspar-megacrystic biotite-hornblende granite.|
31691|Wagait Suite|24197|5|Briefly described|p22, p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Example of the Kalkadoon Association. Includes Wagait, Peppimenarti, Reynolds River and Koolendong Granites. Age: ~1850Ma. Geological province: Pine Creek Inlier.||||||07-FEB-11
31691|Wagait Suite|50586|5|Briefly described|p1.1, 6.2, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Age: 1850Ma.||||||07-NOV-08
31691|Wagait Suite|64698|5|Briefly described|lithinterp table|Orosirian|Orosirian|Age ~1820-1860Ma. Includes Koolendong Granite (1860Ma), ?Wagait Granite.||||||07-JAN-09
31691|Wagait Suite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Areas with diferent magnetic responses are indicated.|||Includes Peppimenarti and Koolendong Granites.|||
31691|Wagait Suite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Wagait Granite and Reynolds River Granite.|||23-NOV-11
31691|Wagait Suite|67232|5|Briefly described|p3, p4 Fig.3. |Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen. Syn- to post-tectonic.|||Includes Wagait Granite.|||
31691|Wagait Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot; p29|||Pine Creek area. Emplacement age.|~1860 Ma.|||Intrudes Burrell Creek Formation.|Granitoids.|
31691|Wagait Suite|67355|6|Mentioned|p.5.||Orosirian|Age may include inherited zircons. Resetting of Rb-Sr system occurred at 1780-1760 Ma due to a regional lowgrade metamorphic event, the Shoobridge Event.|~1850 Ma (U-Pb zircon,conventional)|||||
31691|Wagait Suite|67479|6|Mentioned|p6 Fig.2|||||||||
31691|Wagait Suite|67779|5|Briefly described|p5 Fig.4(b).|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Granite suite.|1863-1853 Ma (Page et al. 1985).|||||
31691|Wagait Suite|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
31691|Wagait Suite|69420|3|Fully described|p5:2, 4, 17-18, 27-29, 33-34, 38, 66, 85|Paleoproterozoic|Paleoproterozoic|See also 111, 115. Wyborn et al. (1997). Litchfield Domain, Pine Creek Orogen. Relatively little data is available. Geochemistry described in some detail. Suite is probably an extension of the Paperbark Suite of Halls Creek Orogen.|c.1863-1853 Ma.||Wagait, Koolendong, Peppimenarti, Reynolds River Granites.||Restite-rich, with some late fractionation of felsic phase. Mainly medium-grained granodiorite, monzogranite and granite.|12-JUL-16
31691|Wagait Suite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Reynolds River Granite.|||01-MAR-18
30242|Wakurlpa Granite|24197|5|Briefly described|p61 Tb. 4.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Suite (or Southwark Granite Suite?). Age: 1567Ma by correlation with Yarunganyi Granite date. Geological Province: Arunta Inlier.||||||07-FEB-11
30242|Wakurlpa Granite|43275|5|Briefly described|Map Legend||Mesoproterozoic|||||||
30242|Wakurlpa Granite|44158|4|Described|p19, Table.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Granitic Suite. Intrudes Lander beds. Age: Probably around 1570Ma.||||||05-MAY-10
30242|Wakurlpa Granite|50369|5|Briefly described|p1.5, 24.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Southwark Suite.||||||07-NOV-08
30242|Wakurlpa Granite|61385|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Arunta Complex. Megacrystic muscovite-biotite granite.||||||20-OCT-05
30242|Wakurlpa 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. Megacrystic muscovite-biotite granite; low gravity response; low to moderate, flat, granitic or sub-linear magnetic response [Mesoproterozoic is missing from map key]||||||19-DEC-12
30242|Wakurlpa 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. Megacrystic muscovite-biotite granite; low gravity response; low to moderate, flat, granitic or sub-linear magnetic response [Mesoproterozoic is missing from map key]||||||19-DEC-12
30242|Wakurlpa Granite|69427|5|Briefly described|p12:44|||Immediately N of Ngalia Basin, Aileron Province.||Southwark Suite.||||12-JUL-16
33488|Wala Wuru Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mantarurr Granite Suite.  Foliated megacrystic granite with a fine-grained biotite -rich matrix.  Age: ~1170Ma.||||||08-FEB-05
33488|Wala Wuru Granite|60683|2|Defined|p58 Appendix, p18|Mesoproterozoic|Mesoproterozoic|Of the Matarurr Granite Suite. Formerly comprised part of Olia Gneiss of Forman (1966a, 1972).  Megacrystic granite with fine-grained biotite-rich matrix.  has sharp intrusive contact  with Foster Cliff and Utanta Granites. See also p10 Tb. 1.||||||23-DEC-09
33488|Wala Wuru Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of the Mantarurr Granite Suite. Foliated megacrystic granite with a fine-grained biotite-rich matrix.  Age: ~1170Ma. Geological Province: Musgrave Block.||||||20-OCT-05
72423|Walabanba Member|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Slate, phyllite and mica schist, metapelite, metasiltstone and metasandstone including felsic tuff.||||||07-NOV-08
72423|Walabanba Member|65333|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Lander Rock Formation. Slate, phyllite and mica schist; heavy mineral bearing/micaceous quartzite; epidote amphibolite; retrogressed andalusite-bearing hornfels, minor tourmalinised rock.||||||
72423|Walabanba Member|65334|5|Briefly described|Map Legend|Orosirian|Orosirian|Of Lander Rock Formation. Slate, phyllite and mica schist; heavy mineral bearing/micaceous quartzite; epidote amphibolite; retrogressed andalusite-bearing hornfels, minor tourmalinised rock.||||||
72423|Walabanba Member|65338|3|Fully described|App1 p83, p8 Table 1, pp8-11, p19.|Statherian|Orosirian|New name. Shallow marine. Age may be more tightly constrained by age of parent unit. May represent more compositionally mature material than Anningie Member; deposited as interlayered winnowed quartzitic sandstone and siltstone/mudstone in a more proximal environment. Polydeformed; locally overturned strata.|Between c.1863 Ma and 1789 +/- 6 Ma.|Unit in Lander Rock Formation.||Intruded by 1789 +/-6 Ma Esther Granite, dolerite and gabbro.|Interbedded slate and sandstone, and stratiform mafic meta-igneous rocks; sandstone generally poorly outcropping, hornfelsed and massive; slate has well-developed slaty cleavage; sandstone has localised heavy mineral laminations.|
72423|Walabanba Member|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Slate, phyllite and mica schist, metapelite, metasiltstone and metasandstone including felsic tuff; epidote-amphibolite; diorite; retrogressed andalusite-bearing hornfels; heavy mineral-bearing/micaceous quartzite.|
72423|Walabanba Member|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Slate, phyllite and mica schist, metapelite, metasiltstone and metasandstone including felsic tuff; medium to thick 'bed' sets; heavy mineral-bearing/micaceous quartzite; medium to thick-bedded/massive, cross-bedded; epidote-amphibolite; diorite.|04-JUL-12
72423|Walabanba Member|69427|5|Briefly described|p12:5|||Aileron Province. More or less proximal shallow-water deposits.||Lander Rock Formation.|||Interbedded slate and sandstone.|12-JUL-16
72423|Walabanba Member|71858|5|Briefly described|p44|||Aileron Province. Outcrops in southeastern MOUNT PEAKE map sheet. Described by Donnellan (2008) as more schistose proximal to granite contacts.||Lander Rock Formation|||Succession of interbedded metapelitic and metapsammitic rocks with intervals of feldspathic, micaceous and heavy-mineral bearing quartzite.|
33656|Walal Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic hornblende-biotite granite and granodiorite, with less abundant equigranular leucogranite, variably deformed and recrystallised to garnet-bearing assemblages. Geological Province: Musgrave Block.||||||08-FEB-05
33656|Walal Granite|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Pitjantjatjara Supersuite.  Porphyritic hornblende-biotite granite and granodiorite, with less abundant equigranular leucogranite; variably deformed and recrystallised to garnet-bearing assemblages. Geological Province: Musgrave Block.||||||12-JAN-05
33656|Walal Granite|60679|5|Briefly described|Map Legend|Stenian|Stenian|Of Pitjantjatjara Supersuite. Porphyritic granite and granodiorite. Geological Province: Musgrave Block.||||||
33656|Walal Granite|60683|2|Defined|p55 Appendix, p10 Tb. 1, p13|Mesoproterozoic|Mesoproterozoic|Synonymous with part of the Musgrave-mann Metamorphics (Thomson 1969 and Forman 1972). Porphyritic hornblende-biotite-granodiorite & granite, with abundant equigranular felsic granite. Age: c.1177Ma, but possibl related to c.1070Ma Angatja Granite Suite.||||||14-DEC-06
33656|Walal Granite|61154|4|Described|p12, p26, p44 App.|Mesoproterozoic|Mesoproterozoic|Of Pitjantjatjara Supersuite. Characterised by coarse phenocrysts of purple-brown K-feldspar, recrystallised to form a gneissic banding in highstrain zones. Comp. ranges from granodiorite to granite, including a medium-grained equigranular aplite phase.||||||19-JUL-05
33656|Walal Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic hornblende-biotite granite and granodiorite, with less abundant equigranular leucogranite, variable deformed and recrystallised to garnet-bearing assemblages. Geological Province: Musgrave Block.||||||19-OCT-05
33656|Walal Granite|63866|5|Briefly described|p207|||Fregon Domain, Musgrave Province.||Pitjantjatjara Supersuite||||
33656|Walal Granite|69436|5|Briefly described|p21:6, 8-9|||Scrimgeour et al. (1999). Eastern Mann Ranges. Timing of the Musgrave Orogeny is indicated by metamorphic rims on inherited zircons dated at 1190 +/- 35 Ma. The zircon cores are aged 1590 Ma.|||||Granodiorite to granite, with a medium-grained equigranular aplite phase. Characterised by coarse phenocrysts of purple-brown K-feldspar. Abundant mafic xenoliths, less common felsic gneiss xenoliths, throughout.|12-JUL-16
33656|Walal Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granodiorite, granite|
75550|Walbiri Dolostone|64068|6|Mentioned|p225|||Ngalia Basin. Correlated with Narpa Group.||||||
75550|Walbiri Dolostone|65232|5|Briefly described|p70|Cambrian|Cambrian|Unconformably overlies Yuendumu Sandstone; underlies Bloodwood Formation. Dolostone. Geol. Prov: Ngalia Basin.||||||09-FEB-10
75550|Walbiri Dolostone|69437|5|Briefly described|p22:10-11|Series 2|Series 2|Ngalia Basin, Centralian B Superbasin. Sequence 1.||||Is overlain by Bloodwood Formation. Equivalent to Tarrara, Gum Ridge, Border Waterhole, Chandler Formations; Thorntonia, Tindall, Top Springs Limestones; Giles Creek Dolostone.|Carbonate and siliciclastic rocks.|12-JUL-16
75550|Walbiri Dolostone|69439|3|Fully described|p24:2-4, 9-10, 13-14, 18, 20-21|Cambrian|Cambrian|Ngalia Basin. Forms low rounded hills and strike ridges along the Walbiri Ranges. The type section is on the northern flank of the Ranges. Over 1000m thick (in drillhole). Lithologies listed in some detail. Is correlated with Giles Creek Dolostone and Chandler Formation (Amadeus Basin) and Thorntonia Limestone (Georgina Basin), and with the Montejinni Limestone to Lothari Hill Sandstone interval in the Wiso Basin. Hosts the uneconomic lead-barite prospect at White Point. Possible hydrocarbon source rock whose potential is unknown. Contains potential reservoirs. Has potential for likely seals for Yuendumu Sandstone reservoirs.||||Unconformably overlies Yuendumu Sandstone and Walbiri Dolostone. Is overlain conformably by Bloodwood Formation.|A lower part of shale, mudstone, sandstone and dolostone, overlain by dolostone with minor interbeds of stromatolitic dolostone and sandstone.|12-JUL-16
75550|Walbiri Dolostone|69673|4|Described|p107, p107 fig 85, p110|||Over 1km thick. Deposited in a shallow marine environment. Source rock potential.||||Overlies Yuendumu Sandstone, overlain by Bloodwood Formation|Interbedded fossiliferous shale, dolomitic mudstone, dolomitic, feldspathic and micaceous sandstone, oolitic and glauconitic dolostone and oolitic, fossiliferous, intraclastic dolostone.|
27602|Waldo Pedlar Member|9199|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Pertatataka Formation.  Platy sandstone, siltstone. Geological Province: Amadeus Basin.||||||04-NOV-04
27602|Waldo Pedlar Member|22506|6|Mentioned|p130 Fig.4|Neoproterozoic III|Neoproterozoic III|||||||
27602|Waldo Pedlar Member|22646|6|Mentioned|Fig 4 on p 102|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.  Age - Ediacarian in text.||||||14-DEC-06
27602|Waldo Pedlar Member|22649|4|Described|p 147|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.||||||14-DEC-06
27602|Waldo Pedlar Member|22762|6|Mentioned|p362|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.||||||14-DEC-06
27602|Waldo Pedlar Member|23250|5|Briefly described|p1124 Fig.2||Neoproterozoic III|Of the Gaylad Sandstone. Correlate of Tent Hill Formation and Brachina Formation.||||||14-DEC-06
27602|Waldo Pedlar Member|30258|6|Mentioned|Fig.2|||Proterozoic age. Member of Pertatataka Formation||||||
27602|Waldo Pedlar Member|32720|6|Mentioned|Table 1|||Of thePertatataka Formation.||||||14-DEC-06
27602|Waldo Pedlar Member|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
27602|Waldo Pedlar Member|34488|5|Briefly described|Table 1|||Proterozoic||||||
27602|Waldo Pedlar Member|34579|4|Described|Table 1|||||||||
27602|Waldo Pedlar Member|35102|6|Mentioned|Fig.11|||||||||
27602|Waldo Pedlar Member|35805|6|Mentioned|Fig.3|||||||||
27602|Waldo Pedlar Member|37462|6|Mentioned|Fig.4.16|||||||||
27602|Waldo Pedlar Member|37928|6|Mentioned|Fig.4|||||||||
27602|Waldo Pedlar Member|38157|6|Mentioned|Table VI|||||||||
27602|Waldo Pedlar Member|38885|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27602|Waldo Pedlar Member|39210|6|Mentioned|p37|||||||||
27602|Waldo Pedlar Member|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
27602|Waldo Pedlar Member|39898|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation. Thin-bedded to laminated sandstone. Geological Province: Amadeus Basin.||||||14-FEB-06
27602|Waldo Pedlar Member|40740|6|Mentioned|p11|||||||||
27602|Waldo Pedlar Member|40906|6|Mentioned|Fig.9|||||||||
27602|Waldo Pedlar Member|41190|6|Mentioned|Fig.4|||||||||
27602|Waldo Pedlar Member|41270|6|Mentioned|Table 1|||||||||
27602|Waldo Pedlar Member|41429|6|Mentioned|p246|||||||||
27602|Waldo Pedlar Member|41717|6|Mentioned|Fig.2|||||||||
27602|Waldo Pedlar Member|41801|6|Mentioned|Fig.4|||||||||
27602|Waldo Pedlar Member|42082|6|Mentioned|Fig.3 P323|||||||||
27602|Waldo Pedlar Member|42504|5|Briefly described|Table 4 P73|||||||||
27602|Waldo Pedlar Member|42940|5|Briefly described|Plate 9|||||||||
27602|Waldo Pedlar Member|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
27602|Waldo Pedlar Member|44335|4|Described|p.7||Proterozoic|Table 1. p.8.||||||
27602|Waldo Pedlar Member|44336|14|Not recorded|map legend||Proterozoic|SG/53-3. Member of Pertatataka Formation.||||||14-DEC-06
27602|Waldo Pedlar Member|44433|14|Not recorded|map legend||Proterozoic|||||||
27602|Waldo Pedlar Member|45041|5|Briefly described|p36|||Proterozoic||||||
27602|Waldo Pedlar Member|46865|6|Mentioned|p44|||||||||
27602|Waldo Pedlar Member|46903|6|Mentioned|p54|||Correlative of Gnallan-a-gea Arkose||||||
27602|Waldo Pedlar Member|48890|2|Defined|p.29,30||Neoproterozoic|Tb.1, Fig.4, Upper Proterozoic.||||||
27602|Waldo Pedlar Member|48963|6|Mentioned|Fig.2|||||||||
27602|Waldo Pedlar Member|49796|5|Briefly described|Sect C BDF 50 & 53|||Equivalent to Cyclops Member, Pertatataka Formation?||||||
27602|Waldo Pedlar Member|60547|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Pertatataka Formation. Geological Province: Amadeus Basin. Platy sandstone, siltstone.||||||
27602|Waldo Pedlar Member|60549|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of the Pertatataka Formation.  Thin-bedded to laminated sandstone.||||||
27602|Waldo Pedlar Member|61732|5|Briefly described|p94|||Of the Pertatataka Formation, but not always differentiated as such.  May be a Gaylad Sandstone correlative?  Succession of thin-bedded silicified sandstone with shale interbeds.||||||07-FEB-11
27602|Waldo Pedlar Member|69438|5|Briefly described|p23:19|||Wells et al. (1970). NE Amadeus Basin.||Pertatataka Formation.|||Thinly bedded, fine-grained flaggy sandstone with ripple and current flow markings.|12-JUL-16
27602|Waldo Pedlar Member|69673|5|Briefly described|p74|||||Pertatataka Formation|||Thinly bedded, fine grained flaggy sandstone.|
27602|Waldo Pedlar Member|69937|4|Described|v Fig.1, p3 Tb.1, p23, p26-31, p51-52|Neoproterozoic|Neoproterozoic|Wells et al. (1967). Amadeus Basin. Characterised by large numbers of small groupings of zircon ages. Likely zircon provenance discussed.|678 +/- 11 Ma (maximum depositional age).|Pertatataka Formation.||Unconformably overlies the Olympic Formation.|Thinly-bedded, fine-grained, flaggy sandstone with ripple and current-flow markings.|
27602|Waldo Pedlar Member|70416|5|Briefly described|p65 Fig.2|Ediacaran|Ediacaran|Amadeus Basin.||Pertatataka Formation.||||
27602|Waldo Pedlar Member|71001|6|Mentioned|p18 Fig.2|Ediacaran|Ediacaran|Amadeus Basin. Marine deposits.||Pertatataka Formation.||||
27602|Waldo Pedlar Member|71344|6|Mentioned|p1093 Fig 1|||||Of Pertatataka Formation.||||
27602|Waldo Pedlar Member|71592|5|Briefly described|Appendix A.|||Amadeus Basin.|678+/-11 Ma (MDA: U-Pb zircon SHRIMP)||||Finely laminated fine-grained sandstone.|
27602|Waldo Pedlar Member|71841|5|Briefly described|p1|Ediacaran|Ediacaran|Of Amadeus Basin.||Unit of Pertatataka Formation.||||
27602|Waldo Pedlar Member|71842|5|Briefly described|p2-3|Ediacaran|Ediacaran|Of Amadeus Basin. Nomenclature after Edgoose 2013 (NE Amedeus, NT).||Unit of Pertatataka Formation.||||
27602|Waldo Pedlar Member|72369|5|Briefly described|p11,14|||Of Amadeus Basin. Restricted to the NE part of Amadeus Basin. Kositcin et al (2015) reported interpreted maximum depositional age of 678+\-11 Ma.||Unit of Pertatataka Formation.||Lower unit of Pertatataka Formation.||
27602|Waldo Pedlar Member|72374|5|Briefly described|p14|||Of Amadeus Basin. Provenance spectra dominated by Musgrave Province-sourced zircon with lesser zircon sourced from Aileron and Warumpi provinces.||Unit of Pertatataka Formation.||||11-OCT-19
27602|Waldo Pedlar Member|72375|4|Described|p1-2,27-29|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Lower of two distinctive sandstone members of the Pertatataka Formation identified in NE Amadeus Basin; occurs at the base of the Pertatataka Formatin. Previously considered to be correlable with Cyclops Member (Preiss et al., 1978; Field 1991), but Freeman (1991) disagreed on the basis of lithological differences. SHRIMP U-Pb zircon analysis by Kositin et al., 2015 yielded an interpreted maximum depositional age (weighted mean 238U/206Pb) of 678+\-11 Ma, which is significantly older than the inferred depositional age of Pertatataka Formation. LA-ICP-MS Hf isotopic signatures for the zircon age populations in NTGS HA13CJE003 (quartz sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p27-28 for Hf isotopic results and interpretations).||Unit of Pertatataka Formation.||Underlain unconformably by Olympic Formation.|Thinly-bedded, fine-grained, flaggy sandstone with ripple and current flow markings.|
27602|Waldo Pedlar Member|73085|6|Mentioned|p1|Ediacaran|Ediacaran|||Pertatataka Formation||||
27602|Waldo Pedlar Member|73086|1|Redefined|[See comments].|Ediacaran|Ediacaran|[Redefined herein. See also definition card, ASUD]. Re-definition of unit. Post-glacial transgressive unit. Characterised as exposures of blocky and flaggy to fissile, well laminated, more or less in situ sandstone float that defines weak benches. Amadeus Basin. Type section: SW of Waldo Pedlar Bore (area). Inferred depositional age of 575 Ma (Maidment, 2005). A detrital zircon maximum depositional age of 678 +/- 11 Ma (SHRIMP U-Pb) is older than the inferred true depositional age. Can be difficult to distinguish from non-diamictite lithologies of the Olympic Formation. No known fossils. Contains localised occurrences of a variety of sedimentary structures. Correlation with Gloaming Formation is based on their similar cyclical alternation in sandstone bed thickness, similar abundant sedimentary structure and inferred similar stratigraphic position. Medium to high energy nearshore or intertidal depositional environment. p: 5-6, 79, 99-100, 117, 121-130, 143, ~167-171, App 2.|ca 570 Ma|Pertatataka Formation||Underlain by Olympic Formation in places. Directly correlates to Gloaming Formation (Winnall Group). Partly correlates to upper Inindia beds.|Fine-grained felspathic quartz sandstone and arkose with green micromicaceous siltstone.|
27602|Waldo Pedlar Member|73088|6|Mentioned|p1|Ediacaran|Ediacaran|Amadeus Basin, northeast.||Pertatataka Formation||||
27602|Waldo Pedlar Member|73180|6|Mentioned|p48 Fig.1|Neoproterozoic|Neoproterozoic|Amadeus Basin.||Pertatataka Formation||||
42431|Waldrons Hill Complex|60681|5|Briefly described|Map legend|Statherian|Orosirian|Dolerite/amphibolite.  Age: 1820-1730Ma.||||||
79411|Walford Dolostone|69433|4|Described|p18:2-4|Statherian|Statherian|Northern succession, Lawn Hill Platform. Discontinuous outcrops S of the Murphy Inlier. 250-400m thick. Shallow-marine sub- to supratidal deposits. SHRIMP U-Pb zircon age from a tuffaceous bed within the unit.|1649 +/- 7 Ma (Page et al., 2000).|Fickling Group.||Conformably overlies Fish River Formation. Is overlain conformably by Mount Les Siltstone.|Oolitic, stromatolitic and intraclastic dolostone with minor black shale and dolomitic glauconitic sandstone; commonly silicified at the surface.|12-JUL-16
79411|Walford Dolostone|69673|4|Described|p52 fig 42, p53 |Statherian|Statherian|400m thick, deposited in shallow marine sub-supra tidal environment.|1649 +/- 7 Ma||||Oolitic, stromatolitic and intraclastic dolostone with minor black shale and dolomitic-glauconitic sandstone.|
79411|Walford Dolostone|70849|5|Briefly described|Map legend.|Statherian|Statherian|Lawn Hill Platform.||Fickling Group.||Overlies Fish River Formation. Is overlain by Mount Les Siltstone.|Dolomite, blocky grey oolite, stromatolitic and interclastic; minor dolomitic sandstone and shale, commonly silicified at the top.|
79411|Walford Dolostone|72913|5|Briefly described|p4, p7, p8, p9 Tb.1, p22, p25, p26.|Paleoproterozoic|Paleoproterozoic|Part of the Isa Superbasin.  Identified in 4 wells in this study. Mineral composition shows majority dolomite, quartz, microcline and muscovite. See also Walford Dolomite p7.||Fickling Group||Underlies Mount Les Siltstone.|Includes dolomitic siltstone.|
79411|Walford Dolostone|72967|6|Mentioned|p6|Paleoproterozoic|Paleoproterozoic|Lawn Hill Platform.Termed the Walford Dolostone in the Northern Territory and Walford Dolomite in Queensland.||Fickling Group and McNamara Group||||
24069|Walkandi Formation|13497|5|Briefly described|p64, p104, p112|Triassic|Triassic|Simpson Basin. ||||Equivalent to the Nappamerri Formation and Tinchoo Formation.||
24069|Walkandi Formation|22839|6|Mentioned|P33|||Lateral equivalent of the Tinchoo Formation||||||
24069|Walkandi Formation|22883|5|Briefly described|P29, Fig2||Triassic|Overlain by Peera Peera Formation.||||||14-DEC-06
24069|Walkandi Formation|24204|5|Briefly described|p262, 270, 263 Fig.4|Triassic|Triassic|Probable equivalent to Nappamerri Group (Cooper Basin). Overlain by Peera Peera Formation (unconformable). Geological Province: Simpson Basin.||||||
24069|Walkandi Formation|41063|2|Defined|p40|Middle Triassic|Early Triassic|Previously named "Unnamed redbeds" E - M.||||||14-DEC-06
24069|Walkandi Formation|41176|6|Mentioned|Fig.3|||||||||
24069|Walkandi Formation|41183|6|Mentioned|p308|||See also Fig.3||||||
24069|Walkandi Formation|41536|5|Briefly described|p384|||||||||
24069|Walkandi Formation|42008|4|Described|p266|||||||||
24069|Walkandi Formation|42463|6|Mentioned|Fig.4 P171|||||||||
24069|Walkandi Formation|42746|4|Described|p6, Fig.2 p4|||||||||
24069|Walkandi Formation|43052|5|Briefly described|Table 2.1|||||||||
24069|Walkandi Formation|44133|5|Briefly described|p43, 94|Triassic|Triassic|Conformably underlies: Peera Peera Formation. Thickness: 134m.||||||
24069|Walkandi Formation|62376|5|Briefly described|p84|Middle Triassic|Late Permian|Geological Province: Pedirka Basin.||||||09-FEB-10
24069|Walkandi Formation|64778|6|Mentioned|p13|Triassic|Triassic|Simpson Desert Basin.||||||
24069|Walkandi Formation|65238|5|Briefly described|p7 Fig. 8, p9, p14 Fig. 17|Early Triassic|Early Triassic|Unconformable below Peera Peera Fm. In:Simpson Desert Basin.Shallow/ephemeral/lacustrine deposits of basal red beds, grading up into a slightly carbonaceous shale/siltstone succession in basinal areas. Lithology: interbedded shale/siltstone/minor sst||||||
24069|Walkandi Formation|65489|5|Briefly described|p55, p58, p61-63, p137, p149, p151|Middle Triassic|Early Triassic|Simpson Basin. Restricted in area to the Poolowanna Trough depocentre. Shallow ephemeral lacustrine environment. 130m thick. Tight, potential seal to underlying Permian where present. Possible local reservoir development.||||Is overlain conformably by Peera Peera Formation. Correlated with Tinchoo Formation; probably equivalent to Arrabury Formation.|Interbedded shale, siltstone and minor sandstone redbeds; with low porosity and permeability.|
24069|Walkandi Formation|69454|5|Briefly described|p38:3-4, 6, 7 Fig.38.6; 38:8-9, 13|Anisian|Changhsingian|Moore (1986). Pedirka Basin (subsurface only). 247m thick in Blamore-1. Shallow ephemeral lacustrine deposits (continental red-beds). Forms an important regional seal.||||Unconformably overlies Purni Formation. Underlies Poolowanna Formation unconformably, and by Peera Peera Formation disconformably or unconformably. Correlated with Arrabury Formation (Cooper Basin).|Interbedded shale, siltstone and minor very fine to fine sandstone. All have a distinctive colour ranging from grey-green/maroon to brick red.|12-JUL-16
24069|Walkandi Formation|69457|6|Mentioned|p41:5 Fig.41.4|||||||||12-JUL-16
24069|Walkandi Formation|69673|5|Briefly described|p149, p151, p152, p154 fig 126, p161|Triassic|Triassic|Maximum thickness of 247m.||||Unconformably overlies Purni Formation, unconformably overlain by Poolowanna Formation|Interbedded shale, siltstone and minor very fine grained to fine grained sandstone.|
24069|Walkandi Formation|69946|4|Described|p8, p36, p51-52|Early Triassic|Early Triassic|Poolowanna Trough, Simpson Basin. Of Moore (1986). Type section is the interval 2768 - 2902m in Poolowanna 1. Up to 134m thick.||||Is overlain conformably by Peera Peera Formation. Correlated with Arrabury Formation (Cooper Basin).|Oxidised, pale grey, grey-green, brick-red, brown and maroon shale and siltstone interbedded with minor pale grey-green, very fine- to fine-grained sandstone.|
24069|Walkandi Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Unconformably overlies Purni Formation. Is overlain by Peera Peera Formation.||
24069|Walkandi Formation|71321|6|Mentioned|p15|||Of Simpson Basin.||||Overlain by the Peera Peera Formation.||24-OCT-19
24069|Walkandi Formation|71342|4|Described|Ch4 p25, Ch5 p8-p9|Early Triassic|Early Triassic|Poolowanna Trough, Simpson Basin. Originally identified as unnamed redbeds by Weiltshire (1978) before being defined by Moore (1986). A type section in Poolowanna 1 is mentioned. A maximum thickness of 134m is recorded in Poolowanna 2. Age derived from palynofloras. See also Ch5 p30, Ch5 p36, Ch5 p51-p52, Ch9 p18, Ch12 p3, Ch12 tbl 12.1, Ch12 p12.||||Conformably overlain by the Peera Peera Formation. Equivalent to the Arrabury Formation of the Cooper Basin.|Oxidised, pale grey, grey-green, brick-red, brown or maroon shale and siltstone interbedded with minor pale grey-green, very fine to fine-grained sandstone.|
24069|Walkandi Formation|72476|6|Mentioned|p36 Fig.9|||Simpson Basin. Time-temperature thermal history diagram.||||||
24069|Walkandi Formation|73281|6|Mentioned|p1, Appendix (DIP)|||[Misspelt as Walikandi Formation, p1]. Pedirka Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx. Also written as Walkandi Formation, lower and Walkandi Formation, upper.||||||
23121|Walker River Formation|22600|4|Described|Map legend|Cenomanian|Aptian|||||||
23121|Walker River Formation|23374|5|Briefly described|p25|Cenomanian|Aptian|||||||
23121|Walker River Formation|23425|5|Briefly described|p381.|||||||||
23121|Walker River Formation|23867|5|Briefly described|p2|||||||||
23121|Walker River Formation|23937|5|Briefly described|p55|Cretaceous|Cretaceous|||||||
23121|Walker River Formation|24047|5|Briefly described|p49, p54|Cretaceous|Cretaceous|Of Krassay (1994b).  Max. thickness: 100m.   Same as Walker Creek Formation?  See also p50 Fig. 41.||||||
23121|Walker River Formation|24048|4|Described|p75|Mesozoic|Mesozoic|||||||
23121|Walker River Formation|24049|5|Briefly described|Map Legend|Cenomanian|Aptian|Sandstone: fine to medium and coarse-grained; graded beds, planar and hummocky cross-beds, fossiliferous; ichofacies trace fossils, interbedded laminated clayey siltstone and chert granule and pebble conglomerate. Geol. Prov: McArthur Basin.||||||13-OCT-05
23121|Walker River Formation|24050|4|Described|p54|Cretaceous|Cretaceous|||||||
23121|Walker River Formation|24051|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Geological Province: McArthur Basin.||||||
23121|Walker River Formation|43630|2|Defined|p10-14|Cenomanian|Aptian|Microfossils - palynological dating. Previously part of Mullaman beds (discontinued)||||||14-DEC-06
23121|Walker River Formation|44112|5|Briefly described|p79,81|||||||||
23121|Walker River Formation|61403|5|Briefly described|Map Legend|Cenomanian|Aptian|Sandstone: fine to medium and coarse-grained; graded beds, planar and hummocky cross-beds, fossiliferous; ichofacies trace fossils, interbedded lamina ted clayey siltstone and chert granule and pebble conglomerate. Geol. Prov: McArthur Basin.||||||
23121|Walker River Formation|63866|5|Briefly described|p115|Cretaceous|Mesozoic|Carpentaria Basin. ||||||
23121|Walker River Formation|65337|6|Mentioned|p68.|Cretaceous|Cretaceous|Assigned (Krassay 1994) from parts of the Mullaman beds of Skwarko (1966).||||||
23121|Walker River Formation|65340|6|Mentioned|p64.|Cenomanian|Aptian|Assigned by Krassay (1994); formerly part of the Mullaman beds of Skwarko (1966).||||||
23121|Walker River Formation|67564|6|Mentioned|p5.|Cretaceous|Cretaceous|Carpentaria Basin.||||||
23121|Walker River Formation|69418|6|Mentioned|p3:26|||Carpentaria Basin. Hosts the Groote Eylandt and Rosie Creek South sedimentary-type Mn deposits (described).||||||12-JUL-16
23121|Walker River Formation|69455|5|Briefly described|p39:2, 39:4 Fig.39.3; 39:5-6, 10-11, 13|Cenomanian|Aptian|Krassay (1994); Rawlings et al. (1997). Onshore Western Gulf Sub-basin, Carpentaria Basin. Previously part of the Mullaman Beds. Broadly correlated with Gilbert River Formation. Contains molluscan macrofossils and marine trace fossils. Predominantly a shallow-marine shelf depositional environment above storm wave base. Hosts the Groote Eylandt manganese deposits (described in detail). Also hosts the Rosie Creek South Mn prospect, in claystone and conglomerate at the basal unconformity.||||Unconformably overlies Yiyintyi Sandstone. Is overlain disconformably by Yirrkala Formation.|Moderately to well sorted, typically cross-bedded, fine- to coarse-grained quartzic sandstone, interbedded with laminated clayey siltstone and chert granule and pebble conglomerate.|12-JUL-16
23121|Walker River Formation|69673|5|Briefly described|p201|Cenomanian|Albian||||||Sandstone, often interbedded with claystone and siltstone.|
78876|Wallara Formation|70416|5|Briefly described|p64, p65 Fig.2|Cryogenian|Cryogenian|Amadeus Basin. Previously the informal Finke beds. Now includes part of the former Boord Formation.||||Correlated with lower part of Inindia beds.||
78876|Wallara Formation|70839|5|Briefly described|p329|Neoproterozoic|Neoproterozoic|Of Amadeus Basin.||||Overlain by Areyonga Formation. Underlain by Bitter Springs Formation or Pinyanna beds.||
78876|Wallara Formation|71001|6|Mentioned|p21, 23-24|Tonian|Tonian|Amadeus Basin. Formerly known as the Finke Beds.||||Overlies Johnnys Creek Formation.|Black pyritic shales interbedded with dolostone and minor red siltstone.|
78876|Wallara Formation|71080|5|Briefly described|p27, p29 fig 20, p30, 31|Tonian|Tonian|Amadeus Basin. Upper supersequence 1. Recently recognised (Normington et al. 2015). Previously refered to as 'Finke beds', 'Johnnys Creek beds'. Probable paleo-oil column identified in this unit based on grain fluorescence studies (Marshall et al., 2007).|||||Dominantly carbonate-shale, marl.|
78876|Wallara Formation|71088|6|Mentioned|p8|Neoproterozoic|Neoproterozoic|Amadeus Basin.||||||
78876|Wallara Formation|71279|6|Mentioned|p355 Fig.2|Cryogenian|Cryogenian|Amadeus Basin.||||||
78876|Wallara Formation|71344|5|Briefly described|p1094, 1093, 1095, 1096, 1102-3|Tonian|Tonian|Amadeus Basin. Limited exposure and occurrence.|~750 Ma||||Interbedded dolostone, dolomitic siltstone and shale with occasional pyrite and glauconite.|10-NOV-17
78876|Wallara Formation|71810|5|Briefly described|Map legend.|Tonian|Tonian|Amadeus Basin (Phase 1), Centralian Superbasin.|||||Dolomite, oolitic dolomite, sandstone and siltstone; stromatolitic, commonly silicified to chert and sandy chert at surface.|
78876|Wallara Formation|71841|5|Briefly described|iii,p1-2,9-11,13-14|Cryogenian|Cryogenian|Of Amadeus Basin. Previously informally termed finke beds. Renamed Wallara Formation; formalised by Normington et al (2015), Normington and Donnellan (in review). Revised stratigraphy in drill core: indentified in CPD003 at 181.3-201.1m. See p9-11 (CPD003) for lithological descriptions based on revised drill core intervals.||||||
78876|Wallara Formation|71842|4|Described|iii,p2-5,9|Cryogenian|Cryogenian|Of Amadeus Basin. Part of revised nomenclature after this study in the Mount Conner area. Formerly known as Finke Beds (this name is now superseded; Normington et al 2015; Normington and Donnellan in review). Originally identified in wells in the central part of the basin, has since been recognised in outcrop in the far west of the basin in WA (Haines et al., 2010) and central north/central part of the basin (HENBURY; Donnellan and Normington 2017). Contains diagnostic stromatolite Bacalia burra; recorded in most exposures (Allen et al 2012, Haines and Allen 2014, Normington et al 2015) and in drillholes (Grey et al 2012).||||Overlain by Areyonga Formation. Underlain unconformably by Bitter Springs Group. Probably overlies the Loves Creek Formation. Equivalent to/replaces Finke Beds.|Sandstone, siltstone, chert (surface exposures only) and carbonate lithofacies.|08-JAN-20
78876|Wallara Formation|72375|4|Described|p1-2,13,15-17|Neoproterozoic|Neoproterozoic|Of Amadeus Basin. Formerly known as Finke beds, newly formalised term of Normington et al., 2015. Type section in drillhole: Wallara-1. Recognised in several stratigraphic and petroleum exploration wells in the central and centralnorthern part of the Amadeus Basin (eg drillholes Wallara 1 and Finke 1; Edgoose 2013). Expressed in outcrop as a silicified regolith unit or paleosurface overlying Johnnys Creek Formation. Inferred to be Cryogenian (c. 720-635 Ma) based on first occurrence of the acritarch Cerebrosphaera buickii (Grey et al., 2011). LA-ICP-MS U-Pb isotopic analysis by Normington et al., 2016 yielded an interpreted max depositional age (youngest individual zircon) of 1006+\-13 Ma. LA-ICP-MS Hf isotopic signatures for the zircon age populations of sample NTGS HB14VJN001 (very coarse- to coarse-grained sandstone) suggest they crystallised in magmas derived from a range of crustal sources (see p16 for Hf isotopic results and interpretations).||||Overlain by Areyonga Formation. Underlain disconformably by Johnnys Creek Formation.|In drill core: stromatolitic and micritic dolostone, and fine- to coarse grained sandstone with siltstone and dolomitic siltstone intervals.|
78876|Wallara Formation|72601|5|Briefly described|p3, p7, p9-12, p14, p17, p25|Tonian|Tonian|Amadeus Basin. Shallow marine setting. Contains the biostratigraphic marker stromatolite Baicalia burra (Grey et al., 2012). Previously [included?] the informal Finke beds (name invalid). Palynomorph assemblages have less diversity than underlying units, but contain the distinctive species Cerebrosphaera buickii.||||Unconformably underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation.|Ooid chert and carbonates.|
78876|Wallara Formation|73085|4|Described|piii, p1-3, p5, p15-16, p20, p22, p24-27|Tonian|Tonian|Amadeus Basin. Previously 'Finke beds'. Contains diagnostic stromatolite taxa. Includes the acritarch Cerebrosphaera buickii, which is an important global time marker for the late Tonian both nationally and internationally. 104.7 m thick in drillhole BR05DD01. Capped by a ~2m buff, silicified sedimentary breccia that has a sharp contact with the overlying Areyonga Formation. Basal contact with Johnnys Creek Formation is transitional.||||Unconformably[?] underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably[?] overlain by Areyonga Formation and Inindia beds.|Alternating silicified, buff carbonate rocks and red and silicified, buff to grey siltstone with calcite-filled voids and veins; carbonate intervals are variably stromatolitic.|
78876|Wallara Formation|73086|1|Redefined|[See comments].|Cryogenian|Cryogenian|[Redefined herein. See also definition card, ASUD]. New name; previously known as Finke beds. Amadeus Basin. Part of Supersequence I. Typically exposed as silcrete and ferricrete. Contains the first appearance of the acritarch Cerebrosphaera buickii in the Amadeus Basin. A detrital zircon maximum depositional age of 1023 +/- 34 Ma (U-Pb LA-ICP-MS) is significantly older than the suspected true depositional age. Areyonga Movement resulted in uplift and erosion of parts of the Heavitree - Wallara Formation succession. Upper contact is marked by a 90 cm-thick interval of brecciated dolostone interpreted to be palaeokarst. Unconformably underlain by Heavitree Formation in places. p: iii, 3, 5-7, 39, 53, 56-60, 62, 143, 156, 158, App 2.||||Underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation. Correlates to Inindia beds, Buldya Group, Burra Group, Browne Formation, Hussar Formation.|Predominantly dolostone, quartz sandstone, feldspathic quartz sandstone, and red and green mudstone; with subordinate dark carbonaceous mudstone and shale and arkosic sandstone.|
78876|Wallara Formation|73088|6|Mentioned|p1|Tonian|Tonian|Amadeus Basin, northeast. Previously called Finke beds.||||Underlain by Johnnys Creek Formation (Bitter Springs Group). Unconformably overlain by Areyonga Formation.||
78876|Wallara Formation|73180|5|Briefly described|p48 Fig.1, p49|Neoproterozoic|Neoproterozoic|Amadeus Basin. Locally separates the underlying Bitter Springs Group from the overlying Areyonga Formation, suggested to be bounded by disconformities.||||Disconformably overlies the Bitter Springs Group, disconformably underlies the Areyonga Formation.|Mixed sandstone, siltstone and dolostone sequence.|
78876|Wallara Formation|73346|6|Mentioned|p28|Tonian|Tonian|Amadeus Basin.||||||
77886|Wallis Formation|67323|5|Briefly described|GIS attrib tbl|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin.||South Nicholson Group|||Shale, siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|68146|5|Briefly described|p21|||||Wild Cow Subgroup.||Overlies Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77886|Wallis Formation|68575|5|Briefly described|p19|||South Nicholson Basin.||Wild Cow Subgroup.||Overlies Burangoo Sandstone.|Siltstone, shale, very fine sandstone.|
77886|Wallis Formation|69591|5|Briefly described|p52, p54|Mesoproterozoic|Mesoproterozoic|Camooweal-Murphy Domain, South Nicholson Basin (Qld and NT). Formerly a Member of the Constance Sandstone. Absent from the central part of the Basin due to faulting and uplift. Storm-dominated shelf deposits.||Wild Cow Subgroup.||Overlies Burangoo Sandstone. Is overlain unconformably by Shultz Sandstone Member (Constance Sandstone).|Shale, siltstone, thinly interbedded sandstone.|
77886|Wallis Formation|71369|4|Described|p1, p6-8, p12-14, p18-20, p24,p35,p48-49|Mesoproterozoic|Mesoproterozoic|See also p22. South Nicholson Basin. Previously the Wallis Siltstone Member (Roberts et al., 1963) of Constance Sandstone. Recognition of an overlying regional unconformity sees it raised to Formation status in this study (Sweet, 2017). Usually c.100m, up to 150m, thick. Marine shelf deposits.||Wild Cow Subgroup.||Overlies Burangoo Sandstone. Is overlain unconformably by Schultz Sandstone Member (Constance Sandstone).|Fine-grained sandstone and mudstone; laminated and thin-bedded shale and siltstone, and minor sandstone. Local ironstone beds.|20-FEB-18
77886|Wallis 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 Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis 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 Wild Cow Subgroup.||Overlain by Cosntance Sandstone or Schultz Sandstone Member. Underlain by Burangoo Sandstone.|Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Wild Cow Subgroup.||Overlain by Constance Sandstone or Schultz Sandstone Member. Underlain by Burangoo Sandstone.|Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|26-NOV-19
77886|Wallis 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 Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone.|
77886|Wallis Formation|72418|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72421|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72422|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis 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.||Unit of Wild Cow Subgroup.|||Laminated and thin-bedded shale and siltstone and thinly interbedded sandstone; also can be medium-bedded and coarse-grained|
77886|Wallis Formation|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|||?Wild Cow Subgroup, South Nicholson Group||Overlies Burangoo Sandstone and partially and unconformably underlies Constance Sandstone.||
77886|Wallis Formation|72912|5|Briefly described|p5 Fig.3, p33 Fig.12.|Mesoproterozoic|Mesoproterozoic|Located in the East part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Burangoo Sandstone and unconformably underlies Constance Sandstone.|Includes siltstone.|
77886|Wallis Formation|72913|5|Briefly described|p7 Fig.2.|Mesoproterozoic|Mesoproterozoic|Shown as being in the eastern part of the South Nicholson Basin.||Wildcow Subgroup||Overlies Bunangoo Sandstone and unconformably underlies Constance Sandstone.|Includes siltstone.|
77886|Wallis Formation|72919|6|Mentioned|p5|Mesoproterozoic|Mesoproterozoic|Distinct from Wallis Sandstone Member in NT[?].||Wild Cow Subgroup, South Nicholson Group||||
77886|Wallis Formation|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Wildcow Subgroup?, South Nicholson Group||Underlain by Burangoo Sandstone. Unconformably overlain by Constance Sandstone.||
77886|Wallis Formation|73144|6|Mentioned|p8|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||Wild Cow Subgroup, South Nicholson Group||Underlain by Burangoo Sandstone. Unconformably overlain by Schultz Sandstone Member (Constance Sandstone, Wild Cow Subgroup).||
30312|Walmudga Formation|23937|2|Defined|p96 App. 1|Calymmian|Statherian|Of the Nathan Group.  Unconformably overlain by Phelp Sandstone; conformably overlies Yalwarra Volcanics. Max. thickness: 250m.  Geological Province: McArthur Basin.||||||
30312|Walmudga Formation|60573|5|Briefly described|Map legend|Calymmian|Statherian|Of the Nathan Group.  Purple mudstone and siltstone; dolomitic siltstone; chert, oolitic, banded or stromatolitic; quartz sandstone, variably feldspathic, fine- to medium-grained, halite casts.||||||
30312|Walmudga Formation|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Nathan Group. Purple mudstone and siltstone; dolomitic siltstone.||||||
30312|Walmudga Formation|69430|4|Described|p15:3, 24-25, 30|||Abbott et al. (2001). Corresponds to the former Kookaburra Creek Formation (Dunn, 1963) above the Yalwarra Volcanics. Later included within Balbirini Dolostone (Jackson et al., 1987). Urapunga Fault Zone, McArthur Basin. 250m thick. Peritidal carbonate ramp and subtidal high-energy sand flat sediments. The upper, unconformity surface is marked by a pronounced paleoregolith.||Nathan Group.||Conformably and gradationally overlies Yalwarra Volcanics. Is overlain unconformably by the Roper Group.|Oolitic, banded and stromatolitic chert (silicified carbonate rock), fine- to medium-grained quartz and feldspathic sandstone, dolomitic siltstone, purple-brown mudstone and shale. Local lithic arkose and granule conglomerate.|12-JUL-16
30312|Walmudga Formation|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Urapunga Fault Zone||Nathan Group||Overlies Yalwarra Volcanics||
30312|Walmudga Formation|70968|5|Briefly described|p7-10|||Source of chert (silicified dolostone) in Phelp Sandstone.||Topmost Nathan Group.|||Capped by a 2m-thick ferruginous and manganiferous chert breccia (=regolith).|
30312|Walmudga Formation|71893|5|Briefly described|p9|||McArthur Basin. ||Nathan Group||Unconformably overlain by the Phelp Sandstone (Collara Subgroup).||
30312|Walmudga Formation|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin.||Nathan Group||Overlies Yalwarra Formation and shown as unconformably underlying Mantungula Formation.||
30312|Walmudga Formation|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone.||Nathan Group||Underlain by Yalwarra Volcanics. Unconformably overlain by Phelp Sandstone and[?] Mantungula Formation (both of Collara Subgroup, Roper Group).||
30312|Walmudga Formation|72912|5|Briefly described|p5 Fig.3.|Calymmian|Calymmian|Located in the Urapunga Fault Zone.||Nathan Group||Overlies Yalwarra Volcanics and unconformably underlies Nathan Group.||
30312|Walmudga Formation|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Underlain by Yalwarra Volcanics. Unconformably overlain by Mantungula Formation.||
42255|Walnut Granodiorite|23809|5|Briefly described|p16, p6 Tb. 3, p5 Table 2|Paleoproterozoic|Paleoproterozoic|Of the Inningarra Suite (but shown as of Frederick Suite in Table 2 p5).  Age: 1801+/-5Ma (SHRIMP zircon).  See also p5 Tb. 2. In Grimwade Range.||||||26-NOV-18
42255|Walnut Granodiorite|62580|5|Briefly described|p46|||Of the Frederick Suite. Variably porphyritic, medium-grained, equigranular, hornblende-biotite granodiorite.||||||07-FEB-11
42255|Walnut Granodiorite|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1801+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
33813|Walu Granite|50321|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Age: ~1090Ma.  Of the Hull Granite Suite.  Intrudes the Mount Harris Basalt.||||||09-JUN-04
33813|Walu Granite|61154|5|Briefly described|p14|Mesoproterozoic|Mesoproterozoic|Of Hull Suite. Pale pink, leucocratic and medium- to fine-grained. Contains greenish biotite, and more rarely, hornblende, as well as patches/veins of epidote and quartz; unfoliated or weakly so, with narrow shear zones. Veins intrude Mt Harris Basalt.||||||18-DEC-06
33813|Walu Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Hull Granite Suite (~1090-1075Ma).  Medium-grained biotite-hornblende granite.||||||
33813|Walu Granite|63866|4|Described|p203, p206|Stenian|Stenian|Mulga Park Domain, Musgrave Province. Numeric age is a SHRIMP U-Pb zircon date. |1084 +/- 9 Ma (Close et al., 2003)|Hull Suite||Intrudes the Mount Harris Basalt.||
33813|Walu Granite|65256|2|Defined|p6-7 Tb.1, p15, p37, p41|Stenian|Stenian|New name. One area of outcrop, 8.5 km SW of Mount Harris. SHRIMP U-Pb zircon age. Crosscut by mafic dykes interpreted to belong to Alcurra dolerite.|1084+/-9 Ma (Armstrong 1998).|Of Hull Granite Suite.||Intrudes Mount Harris Basalt. Correlative of/geochemically similar to Rowley Granophyre and Imbumbunna Granite.|Shallow level granite. Medium-grained, equigranular biotite-muscovite granite.|19-MAY-14
33813|Walu Granite|65906|5|Briefly described|p6, p20|Mesoproterozoic|Mesoproterozoic|Intrudes Mount Harris Basalt (Tjauwata Group). Age: 1084 +/- 9 Ma (SHRIMP U-Pb zircon: Close et al., 2003).||||||
33813|Walu Granite|67128|5|Briefly described|p3, p12, p18-19|||Western Bloods Range. Also appears on p12 as Walu leucogranite.|1084 +/- 9 Ma.|||Intrudes Mount Harris Basalt.|Unfoliated, medium- to fine-grained leucogranite; green biotite, rare hornblende; epidote and quartz patches and veins.|
33813|Walu Granite|69436|5|Briefly described|p21:11, 13-14|Mesoproterozoic|Mesoproterozoic|Musgrave Province. SHRIMP U-Pb zircon age.|1084 +/- 9 Ma (Close et al., 2003).|Hull Suite.||Intrudes Mount Harris Basalt.|Pale pink, leucocratic, medium- to fine-grained, unfoliated or weakly foliated granite with rare, narrow shear zones. Contains green biotite and, more rarely, hornblende, as well as patches and veins of epidote and quartz.|12-JUL-16
33813|Walu Granite|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1084+/-9 Ma (metamorphism: U-Pb zircon SHRIMP)||||Granite.|
42366|Walungurru Volcanics|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Felsic to intermediate rocks (including silicified cryptocrystalline, porphyritic andesite and dacite); and, mafic to intermediate rocks (including silicified microcrystalline basalt, metad.  Of the Kintore Domain, Warumpi Province.  In the Arunta region.||||||07-NOV-08
42366|Walungurru Volcanics|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province.||||||07-NOV-08
42366|Walungurru Volcanics|64580|4|Described|map legend|Devonian|Paleoproterozoic|Dacitic and rhyodacitic volcanic rocks.||||||04-DEC-15
42366|Walungurru Volcanics|64677|5|Briefly described|v, p1, p33-35, p52-63|||Arunta Region, Warumpi Province. Felsic extrusive rocks. Complex zircon age spectrum discussed. This is a conservative age: the youngest concordant analysis is 1617 +/- 14 Ma.|1699 +/- 14 Ma (maximum extrusion age).||||Dark, very fine-grained, quartz- and feldspar-phyric dacite; flow banding, flattened possible fiamme or shards.|
42366|Walungurru Volcanics|67565|6|Mentioned|p5 Fig.3.|||Warumpi Province.||||||
42366|Walungurru Volcanics|68994|4|Described|p1, p4, p6-11, p17, p23-27|||Kintore Domain in Warumpi Province. Its role in a speculative model of tectono-magmatic evolution of southern Arunta region discussed. Crystallisation age of an upper greenschist to amphibolite facies metarhyodacite. Hf analyses detailed.|1650 +/- 4 Ma (Hollis et al., 2013).||||Metamorphosed felsic, intermediate and mafic volcanics, including silicified, cryptocrystalline, porphyritic andesite; dacite; basaltic andesite; basalt; and dolerite.|13-JAN-17
42366|Walungurru Volcanics|69003|5|Briefly described|p32|Paleoproterozoic|Paleoproterozoic||c.1650 Ma.|||Overlies the Ininti Granite.|Wide range of felsic, intermediate and mafic compositions; overall calc-alkaline affinity.|
42366|Walungurru Volcanics|69031|5|Briefly described|p4, p6, p7|Statherian|Statherian|Warumpi Province, Arunta Orogen.|1650 +/- 4 Ma (Kirkland et al., 2009).|||Is intruded by Ininti Granite.|A calc-alkaline succession of volcanic and volcaniclastic rocks including metabasalt, metarhyolite and metarhyodacite.|
42366|Walungurru Volcanics|69417|6|Mentioned|p2:5|Statherian|Statherian|Kintore Region, Warumpi Province.||||||12-JUL-16
42366|Walungurru Volcanics|69428|5|Briefly described|p13:2-3, 12-13, 15|Paleoproterozoic|Paleoproterozoic|Close et al. (in prep). Kintore Domain, Warumpi Province. Crops out in the Kintore Range. Estimated at over 2000m thick. Various lithologies are described and three scenarios for magma formation discussed. A genetic relationship with Ilpilli Dolerite was suggested. Not directly dated: this 1650 Ma SHRIMP U-Pb zircon age is from a WA rhyodacite interpreted to belong to the Walungurru Volcanics.|1650 +/- 4 Ma (Kirkland et al., 2009).|||Overlies Tinki Granite. Is overlain unconformably by Heavitree Quartzite.|A succession of undeformed felsic, intermediate and mafic volcanics, with minor intervals of tuffaceous claystone, sandstone and mudstone.|12-JUL-16
42366|Walungurru Volcanics|69933|5|Briefly described|v, p1, p20-22, p39|Orosirian|Orosirian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|ca 1846 Ma (Maximum extrusion)||||Fine- to medium-grained dacitic volcanic rock, locally amygdaloidal, pale green in colour.|
42366|Walungurru Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||dacite, andesite|
42366|Walungurru Volcanics|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen.|1650+/-4 Ma (crystallisation: U-Pb zircon).||||Metarhyodacite.|
42366|Walungurru Volcanics|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|c.1650 Ma.||||Metadacite and metarhyodacite; may include intermediate to mafic metavolcanic rocks.|
42366|Walungurru Volcanics|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Metadacite and metarhyodacite; may include intermediate to mafic metavolcanic rocks.|
42366|Walungurru Volcanics|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Kintore Domain.|||||Felsic: porphyritic andesite, dacite; local epidote-chlorite, carbonate, sericite, quartz alteration. Mafic: basalt, microdolerite, basaltic andesite, andesite, microdiorite, minor dolerite; local epidote-chlorite-sericite-quartz alteration.|09-SEP-19
41856|Waluwiya Suite|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province.||||||07-NOV-08
41856|Waluwiya Suite|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes undifferentiated rocks (high magnetic intensity) and charnockite of variable magnetic intensity.  In the Arunta region.||||||07-NOV-08
41856|Waluwiya Suite|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Charnockite, granodiorite, migmatite, diorite. Geological Province: Yaya Domain.||||||07-NOV-08
41856|Waluwiya Suite|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province||||||07-NOV-08
41856|Waluwiya Suite|61660|5|Briefly described|p18. |Proterozoic|Proterozoic|Crops out throughout the Yaya Domain. Has strong geochemical affinity with Kakalyi Gneiss.|||||Granodiorite and charnockite.|
41856|Waluwiya Suite|64580|4|Described|map legend|Paleoproterozoic|Devonian|||||||
41856|Waluwiya Suite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Andrew Young Igneous Complex, younger than Carrington Suite. Charnockite; high granitic magnetic response||||||
41856|Waluwiya Suite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Andrew Young Igneous Complex, younger than Carrington Suite. Charnockite; high granitic magnetic response||||||
41856|Waluwiya Suite|65358|6|Mentioned|p12|||Felsic. Intrudes Yaya Domain, Warumpi Province.||||||
41856|Waluwiya Suite|67565|2|Defined|p62, p19-21, p6 Table 1, p14, p32, p60.|Statherian|Statherian|New name, after Waluwiya Outstation. Previously within undifferentiated Arunta Complex (Ranford, 1969). Yaya Domain, Warumpi Province. Geochemistry is discussed briefly.|||Includes Russell and Talyi-Talyi Charnockites; Tjungkuba and Larrie Granodiorites, and Kakalyi Gneiss.|Intrudes Yaya Metamorphic Complex and Papunya Igneous Complex. Is intruded by Ehrenberg and Gunbarrel Granites and Ilpili Dolerite.|An extensive suite of variably deformed charnockite with plagioclase phenocrysts, foliated and locally migmatitic hornblende-biotite granodiorite locally containing metamorphic garnet, with lesser granite.|01-DEC-15
41856|Waluwiya Suite|68832|5|Briefly described|p12||||||Includes Talyi-Talyi Charnockite.|||
41856|Waluwiya Suite|69428|5|Briefly described|p8/11/2016 13:03|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Yaya Domain, Warumpi Province.|1640-1630 Ma.||Larrie, Tjungkuba Granodiorites; Kakalyi Gneiss; Talyi-Talyi, Russell Charnockites.||Geochemically homogeneous, extensive Suite of variably deformed charnockite and granodiorite.|12-JUL-16
41856|Waluwiya Suite|70826|6|Mentioned|p10|Paleoproterozoic|Paleoproterozoic|||||||
41856|Waluwiya Suite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||diorite, granodiorite|
41856|Waluwiya Suite|71810|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen, North Australian Craton.|||||Foliated hornblende metagranodiorite to quartz metadiorite; may include two-pyroxene metagranite or migmatitic felsic rocks.|
41856|Waluwiya Suite|72034|5|Briefly described|500k_interpgeop16_lut|Paleoproterozoic|Paleoproterozoic|Warumpi Province, Arunta Orogen.|||||Foliated hornblende metagranodiorite to quartz metadiorite; may include two-pyroxene metagranite or migmatitc felsic rocks.|
41856|Waluwiya Suite|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya domain.|||||Charnockite; variably migmatitic fine grained, equigranular to weakly porphyritic biotite, hornblende granodiorite; pervasively retrogressed charnockite and granodiorite; abundant epidote retrogression and quartz-epidote veining.|09-SEP-19
33653|Walytjatjata Granite|60572|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Porphyritic clinopyroxene granite with rounded blue-grey phenocrysts of K-feldsparlocally megacrystic or coarse-grained equigranular, variably deformed and recrystallised to garnet-bearing assemblages; rare migmatite.  Geological Province: Musgrave Block.||||||08-FEB-05
33653|Walytjatjata Granite|60683|2|Defined|p56 Appendix, p10 Tb. 1|Mesoproterozoic|Mesoproterozoic|Of Umutju Granite Suite. Synonymous with part of Musgrave-mann Metamorphics (Thomson 1969) and undivided metamorphics (Forman 1972). Porphyritic clinopyroxene granite with rounded blue-grey phenocrysts of K-feldspar.  Intrusive age: 1177+/-10, 1175+/-10Ma||||||20-APR-05
33653|Walytjatjata Granite|61154|5|Briefly described|p12, p20|Mesoproterozoic|Mesoproterozoic|Of Umutju Suite (Pitjantjatjara Supersuite).  Comprises coarsely porphyritic clinopyroxene-bearing granite with distinctive blue-grey phenocrysts of K-feldspar. Age: 1175+/-10Ma (Kobert Pb-Pb zircon evaporation). Geol. Prov: Musgrave Block. See also p44 A||||||
33653|Walytjatjata Granite|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Part of Umutju Granite Suite.  Porphyritic clinopyroxene granite with rounded blue-grey phenocrysts of K-feldspar, locally megacrystic or coarse-grained equigranular, variably deformed and recrystallised. Geological Province: Musgrave Block.||||||19-OCT-05
33653|Walytjatjata Granite|69436|5|Briefly described|p21:8, 16|||Fregon Domain, western Mann Ranges, Musgrave Province. Migmatitic shear zones dating to the Petermann Orogeny are described in some detail. Kober Pb-Pb zircon evaporation age. Metamorphic zircon rims are aged 561 +/- 11 Ma and 555 +/- 7 Ma (Scrimgeour et al. 1999; Gregory et al. 2009).|1175 +/- 10 Ma (Scrimgeour et al., 1999).|Umutju Suite.|||Coarsely porphyritic clinopyroxene-bearing granite with distinctive, large (2-3cm), rounded blue-grey phenocrysts of K-feldspar; locally includes equigranular medium-grained phases. Mafic minerals occur as coarse aggregates, elongated in the fabric.|12-JUL-16
79380|Wanapi Dolostone Member|69439|4|Described|p24:2, 8-9|Ediacaran|Ediacaran|Ngalia Basin, Centralian A Superbasin. Supersequence 3. A cap dolostone unit, common to many Elatina glacial deposits in Australia. Thin (3-4m), well-exposed unit; forms prominent benches.||Mount Doreen Formation.||Conformably overlies Mount Davenport Diamictite Member. Is overlain conformably by Newhaven Shale Member.|Pink, finely-laminated dolomudstone, with nodular and bulbous stromatolites, slump breccias and barite pseudomorphs after gypsum and anhydrite.|11-JUL-16
79380|Wanapi Dolostone Member|69673|5|Briefly described|p106, p107 fig 85|||3-4m thick.||||Overlies Mount Davenport Diamictite Member, overlain by Newhaven Shale Member|Finely laminated dolomudstone.|
27657|Wandie 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
27657|Wandie Granite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27657|Wandie Granite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27657|Wandie Granite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27657|Wandie Granite|41311|4|Described|p20|||||||||
27657|Wandie Granite|42756|6|Mentioned|Fig.5 P6|||||||||
27657|Wandie Granite|43624|6|Mentioned|p14|||||||||
27657|Wandie Granite|43832|4|Described|Table8p38;46,Tb12p61||Paleoproterozoic|||||||07-NOV-08
27657|Wandie 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
27657|Wandie Granite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Cullen Supersuite.  Pale pink, medium-grained leucogranite.  Age: 1810-1800Ma.||||||13-JAN-05
27657|Wandie Granite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1800-1820Ma. Of Cullen Supersuite. I-type. Pale pink, medium grained leucogranite. Intrudes Burrell Creek Formation.||||||
27657|Wandie Granite|67564|3|Fully described|p7 Table 2, p33 Fig.19, p36.|Paleoproterozoic|Paleoproterozoic|I-type. A small (3.5 km2) pluton within Cullen Batholith, Pine Creek Orogen. Similar to Saunders Leucogranite. Contains tin-bearing greisen veins; probably the source for tin mineralisation at the Crest of the Wave mine to the NE.|1812 - 1800 Ma.|Unit in Cullen Supersuite.||Intrudes Burrell Creek Formation and McCarthys Granite.|Massive, pale pink, medium-grained equigranular biotite leucogranite.|
27657|Wandie Granite|69420|5|Briefly described|p5:17-19, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Sn is present in greisens associated with this unit.||Burnside Suite.|||Medium-grained equigranular granite. I-type.|12-JUL-16
24556|Wangala Granite|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Porphyritic granite, gneissic granite, metamorphically retrogressed rock, pegmatite, diorite.||||||
24556|Wangala Granite|11884|5|Briefly described|Map Legend|Calymmian|Statherian|Carpentarian age.||||Intrudes the Ngalurbindi Granite.|Biotite granite with a coarse porphyritic texture and aligned tabular feldspars.|
24556|Wangala Granite|23270|5|Briefly described|Table 1, p4||Proterozoic|In the Arunta Block. Age: Rb-Sr Whole Rock 1500+/-100ma.||||||18-DEC-06
24556|Wangala Granite|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||18-DEC-06
24556|Wangala Granite|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24556|Wangala Granite|24540|6|Mentioned|p8|||Example of a rare earth element-bearing granite. Also contains allanite. On the NAPPERBY sheet. Mapped as Yaloolgarrie Granite by Young et al (1995) on MOUNT DOREEN.||||||07-FEB-11
24556|Wangala Granite|38829|6|Mentioned|p132|||||||||
24556|Wangala Granite|39888|6|Mentioned|Fig.8|||See also Fig.9||||||
24556|Wangala Granite|41465|6|Mentioned|p14|||||||||
24556|Wangala Granite|48992|2|Defined|p55|Mesoproterozoic|Mesoproterozoic|Prob. Middle Proterozoic||||||30-APR-10
24556|Wangala Granite|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite.||||||07-NOV-08
24556|Wangala Granite|64329|6|Mentioned|p16|Proterozoic|Proterozoic|Contains a hematitic porphyry.||||||29-JUL-08
24556|Wangala Granite|65232|6|Mentioned|App. 2|||||||||09-FEB-10
24556|Wangala Granite|68998|5|Briefly described|v-vi, p1, p12, p14, p25-28, Appx Tb.9|||Arunta Region. High heat-producing. Zircons have 1565 +/- 31 Ma overgrowths, attributed to the 1590-1560 Chewings Orogeny. Hosts unusual biotite-apatite schist aged 1573.6 +/- 1.5 Ma, likely representing discrete zones of Wangala Granite (or pegmatite) that were hydrothermally altered or greisenised during a later event.|1777 +/- 6 Ma (Beyer et al. in prep).|||Intrudes Reynolds Range Group and Ngalurbindi Orthogneiss.|Dominated by peraluminous coarse-grained porphyritic biotite-muscovite granite; has a rapakivi phase; biotite-apatite schist.|
24556|Wangala Granite|69427|5|Briefly described|p12:30 Fig.12.28; 12:33, 61-63|||Mount Denison homestead area. Included in a map of 1780-1740 Ma granites in the Aileron Province. Includes granite mapped as Yaloolgarrie Granite in eastern MOUNT DOREEN map area. Is enriched in U, Th and REE; has potential for U, REE and IOCG mineralisation (eg Quartz Hill prospect). Hosts the Quartz Hill apatite-REE occurrence in uraniferous apatite-mica schists (?hydrothermally altered pegmatite or granite).|||||Contains multiple phases of variably fractionated, crustally contaminated granodiorite-granite. Includes biotite-muscovite porphyritic granite, equigranular granite, rapakivi granite, microgranite and leucogranite.|12-JUL-16
24556|Wangala Granite|70301|5|Briefly described|v, p1, p6-19, p21, p23|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Emplaced during the 1780-1770 Ma Yambah Event. Zircon rims aged 1571 +/- 28 Ma are associated with the Chewings Event. Other, similar ages given. U-Pb and Lu-Hf isotope results.|1777 +/- 11 Ma.|||Includes enclaves of Ngalurbindi Orthogneiss.|Peraluminous muscovite-biotite granite, biotite-apatite schist, greisen.|
24556|Wangala Granite|71858|4|Described|iii, p2, p4-p19, p21-p25|||Aileron Province. First investigated in 1968 as part of mapping of the first edition Napperby 1;250k sheet (Evans and Glikson 1969, Evans 1972). The unit was first named in Stewart et al, 1980a. and fully defined in Stewart et al, 1980b.Outcrops in DENISON northwestern Napperby and is a lense shaped body with a surface area of around 600km3.  An isotopic resetting event is intepreted by U-rich zircon overgrowths at 1571 +/- 28 Ma. Considered prospective for REE mineralisation. This granite can be identified in radiometrics. Petrographic descriptions, geochemistry analyses and results are discussed. See also p27-p43, p62-p68, p70-p72.|1777 +/- 11 Ma (LA-ICPMS)|||Intrudes the Lander Rock Formation, Ngalurbindi Orthogneiss and the Wickstead Creek beds (Reynolds Range Group). Unconformably overlain by the Mount Stuart Formation. Intrudes the Uldirra Porphyry.|S-type muscovite-biotite monzogranite and coarse-grained, porphyritic biotite-muscovite granite.|
38512|Wangalinji Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Playford Sandstone. White, thick bedded, medium to coarse grained, silicified to friable, locally pebbly, sublithic to quartzose sandstone; laminated shale, siltstone.||||||
38512|Wangalinji Member|65337|3|Fully described|p37-39, p39 Table 5.|Mesoproterozoic|Mesoproterozoic|Also called Wangalinji Sandstone Member, p30. Southwest MOUNT DRUMMOND area. Highly ferruginous and manganiferous crusts suggest some mudstones are pyritic.||Unit in Playford Sandstone.||Unconformably overlies Widdallion Sandstone. Is overlain by Top Lily Sandstone Member.|Basal white, blocky, coarse-grained to granule and pebbly sandstone; overlain by laminated shale with thinly bedded siltstone and fine-grained lithic sandstone interbeds. Occasional gypsum moulds and carbonates.|
38512|Wangalinji Member|69434|4|Described|p19:3, 4|Mesoproterozoic|Mesoproterozoic|Rawlings et al. (2008). South Nicholson Basin. 115-750m thick. Basinal, through storm-dominated shelf, to shoreface or marginal marine depositional environments.||Playford Sandstone.||Overlies Widdallion Sandstone Member disconformably (locally unconformably). Is overlain conformably by Top Lily Sandstone Member.|Basal white, thick-bedded, medium to coarse grained silicified to friable, locally pebbly, sublithic to quartzic sandstone; overlain by laminated shale, thin-bedded siltstone, very fine-grained lithic sandstone and coarser white sandstone interbeds.|12-JUL-16
38512|Wangalinji Member|72526|5|Briefly described|p8 Fig.1.3.|Mesoproterozoic|Mesoproterozoic|Shown as being located in the west of the South Nicholson Basin.||Playford Sandstone||Shown as unconformably overlying Benmara Group and Fickling Group and underlies Top Lily Sandstone Member.||
38512|Wangalinji Member|72527|3|Fully described|p8, p12-19, p27, p140, p193, p195.|Mesoproterozoic|Mesoproterozoic|Feldspathic sandstone sampled at type locality. Type locality shown as 137.12591dE 18.66525dS.  Up to 390 m thick. SHRIMP date derived using 207Pb/206Pb isotopic ratios. Written as Wangalinji Sandstone Member p140.|1600 +/- 20 Ma  maximum depositional age|Base of Playford Sandstone.||Underlies Top Lily Sandstone gradationally and conformably. unconformably overlies the Widdallion Sandstone Member.|Coarse-grained to granule and pebbly cross-bedded sandstone, overlain by interbedded siltstone and fine-grained sandstone, laminated shales and fine-grained lithic sandstone. Also rare cherts and carbonates.|
38512|Wangalinji Member|72912|5|Briefly described|p5 Fig.3, p25.|Mesoproterozoic|Mesoproterozoic|Located in the west of South Nicholson Basin.||Playford Sandstone||Shown as unconformably overlying Benmara and Fickling groups. Underlies Top Lily Sandstone Member and partially and laterally equivalent to Bowgan Sandstone.||
38512|Wangalinji Member|72919|6|Mentioned|p5, p24|Mesoproterozoic|Mesoproterozoic|||Playford Sandstone, Wild Cow Subgroup, South Nicholson Group||Unconformably underlain by Widdallion Sandstone Member (McNamara Group). Conformably overlain by Top Lily Sandstone Member.||
38512|Wangalinji Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Roper Superbasin.||Playford Sandstone, Wildcow Subgroup, South Nicholson Group||Partly underlain by Doomadgee Formation. Overlain by Top Lily Sandstone Member.||
33646|Wankari Volcanics|24496|5|Briefly described|p15|Mesoproterozoic|Mesoproterozoic|Of Tjauwata Group. Geological Province: Musgrave Block.||||||
33646|Wankari Volcanics|60678|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite with rare epidotised and amygdaloidal mafic volcanics. Geological Province: Musgrave Block.||||||11-JAN-05
33646|Wankari Volcanics|60679|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Rhyolite. Geological Province: Musgrave Block. Of Tjauwata Group.||||||14-JAN-05
33646|Wankari Volcanics|61386|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Porphyritic rhyolite with rare epidotised and locally amygdaloidal mafic volcanics. Age: ~1041Ma.||||||03-AUG-09
33646|Wankari Volcanics|61524|5|Briefly described|p17 Fig.1|Mesoproterozoic|Mesoproterozoic|Part of rift sequence along with Tjauewata Group and Bloods Range Beds. Geological Province: Musgrave Province.||||||
33646|Wankari Volcanics|61864|6|Mentioned|p18 fig 4|||Part of a rift sequence.||||||
33646|Wankari Volcanics|62989|5|Briefly described|p39|Mesoproterozoic|Mesoproterozoic|Of the Tjauwata Group. Age: 1041+/-2Ma. Pervasively overprinted by the Petermann Orogeny.||||||25-JAN-07
33646|Wankari Volcanics|64745|5|Briefly described|p376|Stenian|Stenian|Uppermost unit of Tjauwata Supercrustal. Age: ca. 1.04Ga. Correlated with Hogarth Formation (Tollu Group).||||||
33646|Wankari Volcanics|65135|6|Mentioned|p16|Stenian|Stenian|Dated at 1041 +/- 2 Ma.||||||
33646|Wankari Volcanics|65833|5|Briefly described|p16|Stenian|Stenian|Of Tjauwata Group. 1041 +/- 2 Ma: a c.30 m.y. time gap between this unit and the Puntitjata Rhyolite, also of the Tjauwata Group.||||||
33646|Wankari Volcanics|65906|5|Briefly described|p6, p19|Mesoproterozoic|Mesoproterozoic|A series of porphyritic felsic volcanics interlayered with minor mafic volcanic units. Correlative of the Hogarth Formation, Tollu Group. Age: 1041+/-2 Ma. Unit in the Tjauwata Group.||||||
33646|Wankari Volcanics|67128|5|Briefly described|p13, p30-31|||Bloods Range. Coeval with granite magmatism in the central Musgrave Province to the east.|1051 +/- 22 Ma (SHRIMP).|Tjauwata Group.|||Locally amygdaloidal, fine-grained, porphyritic felsic volcanics with minor interlayered mafic units. Includes porphyritic rhyolite with rare epidotized and amygdaloidal mafic volcanics.|
33646|Wankari Volcanics|69436|5|Briefly described|p21:13-14, 19|Mesoproterozoic|Mesoproterozoic|Musgrave Province. Kober Pb-Pb zircon age.|1041 +/- 2 Ma (Scrimgeour et al., 1999).|Tjauwata Group.||Is overlain by Bloods Range Formation. Is correlated with Puntitjata Rhyolite.|A succession of fine-grained, porphyritic, felsic volcanic rocks with minor interlayered mafic units.|12-JUL-16
33646|Wankari Volcanics|69606|6|Mentioned|p5|||Musgrave Province.|1041+/-2 Ma|Tjauwata Group, upper part||||
33646|Wankari Volcanics|70018|5|Briefly described|p233,235|Mesoproterozoic|Mesoproterozoic|Amadeus Basin. SHRIMP U-Pb age of 1051+\-22 Ma; Scrimgeour et al., 1999).|1051+\-22 Ma|Unit of Tjauwata Group.||Overlain conformably by Bloods Range Formation. Underlain by Puntitjata Rhyolite.||
33646|Wankari Volcanics|71210|5|Briefly described|p9|Stenian|Stenian|Correlation with the Hogarth Formation was established by Close et al., 2003a.||Tjauwata Group||Equivalent to the Hogarth Formation.||
33646|Wankari Volcanics|71211|6|Mentioned|p234||||ca. 1040 Ma|||||
33646|Wankari Volcanics|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||basic volcanic rock, rhyolite|
33646|Wankari Volcanics|71268|4|Described|GEOL_LUT_CSV files|Mesoproterozoic|Mesoproterozoic|Geological Province: Paterson Orogen. Of Bentley Basin. Events: Alice Springs Orogeny (450-295 Ma); Petermann Orogeny (580-520 Ma); Paterson Orogeny (635-540 Ma); Giles Event (1085-1040 Ma). Sample GSWA 210702 (schistose, porphyritic rhyolite) yielded a regression intersecting concordia curve at 1044+\-8 Ma, interpreted as magmatic crystallisation age of the rhyolite. Sample GSWA 208439 (metarhyolite) yielded a regression intersecting concordia curve at 1039+\-7 Ma, interpreted as magmatic crystallisation age of the metarhyolite. Sample GSWA 208498 (quartzite) yielded a weighted mean 207Pb/206Pb age of 1105+\-24 Ma, interpreted as maximum depositional age of sandstone protolith. See 250k_interpgeop_lut.csv, 500k_interpgeop_lut.csv, 1m_geologyp12_lut.csv, 500k_interpgeol_lut.csv.|1051-1039 Ma (inferred)|Unit of Tjauwata Group.|||Quartzite; blocky to flaggy, muscovite-bearing; sericite schist, massive to quartz-amygdaloidal basalt, quartz-feldspar-phyric metarhyolite; quartz-feldspar-phyric schist and felsic intrusives.|
33646|Wankari Volcanics|71592|5|Briefly described|Appendix A.|||Musgrave Province.|1051+/-22 Ma (crystallisation: U-Pb zircon SHRIMP)||||Volcanic rock.|
38831|Ware Group|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Includes the Century and Wilson Formations.   Age: 1825-1810Ma.||||||
38831|Ware Group|61246|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Volcanic and siliclastic rocks. Overlies the Tanami Group. Age: 1825-1810Ma.||||||07-NOV-08
38831|Ware Group|62377|4|Described|p5, 19|Paleoproterozoic|Paleoproterozoic|Overlies Tanami Group. Rhyolites, ignimbrites, siliclastic sediments. Age: 1825-1810Ma.||||||07-NOV-08
38831|Ware Group|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Tanami Inlier.||||||07-NOV-08
38831|Ware Group|63261|3|Fully described|p9 Fig. 5, p12-14, p19|Paleoproterozoic|Paleoproterozoic|Comprises Mount Winnecke Fm, Nanny Goat Volcs, Century + Wilson Fms. Age: ~1825-1810Ma.Unconform.on Tanami Gp. Dominated by felsic volcanic rocks+coarse-gr.lithic sandstones+ minor siltstone, basalt. Geol.prov:Tanami Region. Deposition details included.||||||07-FEB-11
38831|Ware Group|63866|5|Briefly described|p92-p93|||Tanami Region.|||||Bimodal volcanic rocks.|
38831|Ware Group|64662|5|Briefly described|p28, p30 Fig. 3, p37, 41, 43|Orosirian|Orosirian|Includes Nanny Goat Volcanics, Mount Winnecke, Wilson and Century Fms. Coarse sandstone, felsic volcanic rocks. Detrital zircons ages from Century and Wilson Fms similar to volcanics ages. Geological Province: Tanami region.||||||07-FEB-11
38831|Ware Group|64722|5|Briefly described|Fig. 2 p3-6, p10|Orosirian|Orosirian||1825-1810 Ma (Cross and Crispe, 2007).|||Unconformably overlies Tanami Group.|Siliciclastic sedimentary and felsic volcanic rocks|11-APR-12
38831|Ware Group|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|||Includes Mount Winnecke, Wilson, Century Formations and Nanny Goat Volcanics.|||
38831|Ware Group|64730|5|Briefly described|p141-142|Orosirian|Orosirian|Tanami region. Age from included felsic volcanic rocks (Smith 2001; Page 1996; Crispe et al. 2007). Broadly correlated with El Sherana and Edith River Groups.|1825-1810 Ma.|||||03-MAY-12
38831|Ware Group|64733|4|Described|p170 Fig.2, p172-3, p172 Fig.4|Orosirian|Orosirian||~1825-1815 Ma.||Contains Wilson and Century Formations, Nanny Goat Volcanics and Mount Winnecke Formation.|Unconformably overlies Tanami Group, and is unconformably overlain by Mount Charles Formation.|Tubiditic sandstone, siltstone and felsic volcanics.|20-APR-12
38831|Ware Group|64734|5|Briefly described|p186 Fig.1, p187|Orosirian||Includes the Wilson and Century Formation, Nanny Goat Volcanic and Mount Winnecke Formation; ~1820 Ma; deposition of this group followed the Tanami Orogenic Event at ~1840-1825 Ma; sandstone, siltstone and felsic volcanic rocks||||||14-SEP-09
38831|Ware Group|64735|4|Described|p216 Fig15, p217|Orosirian|Orosirian|Dated to ca. 1820-1800 Ma (by detrital zircons); correlated with Hatches Creek Group, Strzeleckie Volcanics, Tinfish Sandstone, Gwynne Sandstone.||||Overlies Killi Killi Formation.|Contains volcanics and clastic sediments.|20-APR-12
38831|Ware Group|64737|5|Briefly described|p232-3, Fig.2, Fig.4, p236 Tab.4, p242-4|Orosirian|Orosirian|In Tanami Region. Coeval with Hatches Creek Group and Ongeva Package.|~1825-1810 Ma.|||Overlies Tanami Group.|Sedimentary and bimodal volcanic succession.|01-MAY-12
38831|Ware Group|64956|5|Briefly described|p7|||Contains the Mount Winnecke Formation. Also interpreted to contain the "Nongra volcanics" sample.||||||07-FEB-11
38831|Ware Group|65338|6|Mentioned|p5 Fig.3.|Paleoproterozoic|Paleoproterozoic|||||||
38831|Ware Group|65358|5|Briefly described|p6-7|Orosirian|Orosirian|In Tanami Region. Unconformably overlies Tanami Group. Rhyolite, ignimbrite, siliciclastic sediments and felsic ignimbrite. Deposited between 1825-1810 Ma.||||||
38831|Ware Group|65359|5|Briefly described|p1, p33|Orosirian|Orosirian|Tanami Region. A volcanosedimentary succession of Paleoproterozoic age (1825-1810 Ma). Contains the Mount Winnecke Formation, Nanny Goat Volcanics, Wilson Formation, Century Formation, and volcanic rocks of the former Nongra beds. ||||||
38831|Ware Group|66129|5|Briefly described|p214 Fig.1, p216 Fig.3|||Contains Wilson Formation, Century Formation, Nanny Goat Volcanics and Mount Winnecke Formation. Unconformably underlies Pargee Sandstone; overlies either the Killi Killi Formation or Mount Charles Formation.||||||
38831|Ware Group|66468|6|Mentioned|p16 Fig.2, p17 Figs.3,4|Orosirian|Orosirian|1825-1815 Ma. Overlies Killi Killi Formation (Tanami Group) and Mount Charles Formation.||||||
38831|Ware Group|66860|6|Mentioned|p6 Tb.1|||Tanami Region. Coeval with Ongeva package (middle Strangways Metamorphic Complex) in Arunta Region, and lower parts of both Wauchope Subgroup and Tomkinson Creek Group (Tennant Region).|1825-1790 Ma.||||Bimodal volcanism and shallow-water sediments.|
38831|Ware Group|67323|5|Briefly described|p30|||Granites-Tanami terrane. Age of eruption/deposition.|~1820-1810 Ma.||||Rhyolite, ignimbrite; siliciclastic rocks.|
38831|Ware Group|67824|5|Briefly described|p385-p388, p391 Fig.8, p392, p395|Orosirian|Orosirian|Age from a rhyolite unit (Ozchron database, Geoscience Australia). Also shown as 1825-1815 Ma.|1824 +/- 5 Ma (SHRIMP U-Pb; #87495029).||Includes Wilson, Century and Mount Winnecke Formations; Nanny Goat Volcanics.|Unconformably overlies Tanami Group.|Dominated by felsic volcanic rocks and coarse-grained lithic sandstone with minor siltstone.|
38831|Ware Group|67826|4|Described|p401 Fig.2, p402, p403|Orosirian|Orosirian|Age range determined from constituents. Intruded by extensive granitic magmatism ~ 1820-1790 Ma.|~ 1825-1815 Ma||Includes Wilson Formation, Century Formation, Nanny Goat Volcanics, Mount Winnecke Formation.|Unconformably overlies Tanami Group.|Includes coarse sandstones and felsic volcanic rocks.|
38831|Ware Group|68474|6|Mentioned|p572, p574|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|||Includes the Wilson Formation, Century Formation, Nanny Goat Volcanics and Mount Winnecke Formation|Unconformably overlies the Killi Killi Formation.||
38831|Ware Group|68656|5|Briefly described|GEOCHRON|Paleoproterozoic|Paleoproterozoic||1825-1810 Ma (Crispe et al., 2007).|||Unconformably overlies Tanami Group.|Rhyolite, siliciclastic sedimentary rocks, and felsic ignimbrite.|
38831|Ware Group|68733|5|Briefly described|p186, p187 Fig.6|Orosirian|Orosirian|Tanami region.|ca. 1825 - 1815 Ma|||Unconformably overlain by the Mount Charles Formation. Unconformably underlain by the Tanami Group.||06-DEC-17
38831|Ware Group|69003|5|Briefly described|p5, p17|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|1825-1815 Ma.|||Unconformably overlies Killi Killi Formation.|Siliciclastic sedimentary and volcanic rocks.|
38831|Ware Group|69253|6|Mentioned|p747 Fig.1|Orosirian|Orosirian||1825-1815 Ma.|||||
38831|Ware Group|69417|5|Briefly described|p2:4-5|||Tanami Region.|1825-1810 Ma.||||Sandstone, felsic volcanic rocks.|12-JUL-16
38831|Ware Group|69418|6|Mentioned|p3:7|||Tanami Region. Hosts gold deposits (described).||||||12-JUL-16
38831|Ware Group|69426|4|Described|p11:3-5, 7-8, 10-14, 27, 30|Orosirian|Orosirian|Felsic volcanic rocks, coeval with Winnecke Granophyre, form part of the Birthday Suite. Sedimentation was contemporaneous with volcanic activity. Deformation described. The age range is constrained by SHRIMP U-Pb zircon dating of constituents as well as of detrital zircons.|1830-1815 Ma.||Mount Winnecke, Century, Wilson Formations; Nanny Goat Volcanics.|Unconformably overlies Killi Killi Formation (Tanami Group). Correlated with El Sherana Group, upper Ooradidgee and lower Hatches Creek Groups.|Dominated by felsic volcanic rocks and coarse lithic clastic rocks, but also contains minor siltstone and mafic volcanic rocks.|12-JUL-16
38831|Ware Group|69427|5|Briefly described|p12:14|Orosirian|Orosirian|Tanami Region.|1825-1810 Ma.|||||12-JUL-16
38831|Ware Group|69429|6|Mentioned|p14:2, 4|||Tanami Region. A likely correlative of the Inverway Metamorphics (Birrindudu Basin).||||||12-JUL-16
38831|Ware Group|69432|6|Mentioned|p17:2, 4|||||||Is overlain unconformably by the Birrindudu Group.||12-JUL-16
38831|Ware Group|69587|5|Briefly described|177278.1.pdf|||Geological province: Granites-Tanami Orogen, North Australian Craton. |c. 1825-1810 Ma|||Underlain unconformably by Tanami Group.|Rhyolite, siliciclastic sedimentary rocks, and felsic ignimbrite.|
38831|Ware Group|69618|6|Mentioned|p89-91, p98, p106-107|Paleoproterozoic|Paleoproterozoic||1825-1810 Ma (Cross and Crispe, 2007).||||Includes post-orogenic thick conglomerate and pebble sandstone.|
38831|Ware Group|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
38831|Ware Group|69747|5|Briefly described|p263,265|Orosirian|Orosirian|Geological province: Tanami Block, North Australian Craton.|1825-1815 Ma|||||
38831|Ware Group|70291|4|Described|p178,180-181,201|Paleoproterozoic|Paleoproterozoic|Geological province: Tanami. Deposition occurred after D1 Tanami Event. Coeval with, and intruded by Winnecke Granophyre.|1825-1815 Ma||Includes Wilson and Century formations, Nanny Goat Volcanics and Mount Winnecke Formation.||Sandstone, siltstone, and felsic volcanic rocks|
38831|Ware Group|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. Undivided Ware Group also shown on p2 Fig 1.|||Includes Wilson Formation, Century Formation and Nanny Goat Volcanics.|||11-OCT-19
38831|Ware Group|70848|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Mount Winnecke Formation.|||
38831|Ware Group|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.|||Century, Wilson Formations.|||
38831|Ware Group|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||schist|
38831|Ware Group|71349|5|Briefly described|p724-725|Paleoproterozoic|Paleoproterozoic|Tanami Region.|1825-1815 Ma.|||Unconformably overlies Tanami Group (inferred: contact not exposed). Is intruded by Birthday, Frederick and Grimwade Suites.|Coarse-grained sandstones and felsic volcanic rocks.|
38831|Ware Group|71397|5|Briefly described|p5,46-47|Orosirian|Orosirian|Geological province: Granites-Tanami Orogen.||||Underlain unconformably by Tanami Group.||
38831|Ware Group|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|||Century FZ.|||
38831|Ware Group|73083|6|Mentioned|p14|||Tanami Province.||||||
38831|Ware Group|73089|5|Briefly described|p: 3-4, 6-8, 10, 23, 29-32, 38-39, 41-42|Orosirian|Orosirian|Granites-Tanami Orogen. 5.5 km thick. Subaerial to marine depositional setting. Sedimentary units deposited in a fluvial to lacustrine, or shallow-marine setting. Intruded by granitic rocks. Felsic volcanic rocks of this unit represent coeval magmatism with the Winnecke Granophyre and Water Tower Tonalite (Birthday Suite intrusions). Pre-dates the Stafford Event and are of relatively low metamorphic grade, except near contacts with granitic rocks.|1825-1815 Ma||Mount Winnecke Formation, Nanny Goat Volcanics, Wilson Formation, Century Formation|Unconformably underlain by Tanami Group. Correlates[?] to El Sherana Group and Edith River Group.|Felsic volcanic rocks, coarse-grained lithic sandstone, minor siltstone and basalt.|
38831|Ware Group|73158|5|Briefly described|p2|Orosirian|Orosirian|Granites-Tanami Orogen.|ca. 1824 to 1816 Ma||||Magmatic and sedimentary rocks.|
38831|Ware Group|73159|6|Mentioned|p2|||Granites-Tanami Orogen.|c.1824-1816 Ma.|||||
26331|Warimbi Schist|7838|5|Briefly described|p79|||Stewart (1981). Called Warimbi Granite in this article.|||||Has a well-developed schistosity defined by abundant, finely recrystallised micaceous aggregates.|
26331|Warimbi Schist|22733|6|Mentioned|p306||Proterozoic|||||||
26331|Warimbi Schist|23270|5|Briefly described|Table 1, p5||Proterozoic|||||||
26331|Warimbi Schist|23271|5|Briefly described|Map legend||Proterozoic|Of the Arunta Block. Age: Middle Proterozoic.||||||18-DEC-06
26331|Warimbi Schist|24047|5|Briefly described|p36|||Granitic orthoschist sill.||||||
26331|Warimbi Schist|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
26331|Warimbi Schist|39888|6|Mentioned|Fig.8|||||||||
26331|Warimbi Schist|48992|2|Defined|p56|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
26331|Warimbi Schist|50369|6|Mentioned|p5.1|||Superseded by Warimbi granite?||||||18-DEC-06
26331|Warimbi Schist|64737|5|Briefly described|p242-3|Calymmian|Statherian|Deformed metamorphosed granitoid in contact with the Reynolds Package in the Reynolds Range area. Age uncertain, but may be ~1590 or ~1780 Ma.||||||01-MAY-12
26331|Warimbi Schist|65338|5|Briefly described|p56.|Statherian|Orosirian|Granitic precursor.|1785 +/- 22 Ma (Collins and Williams 1995).|||||
26331|Warimbi Schist|69226|5|Briefly described|p239, p240 Tb.1, p243, p247, p250, p254|Statherian|Orosirian|Reynolds-Anmatjira Ranges region. Associated with the c.1780-1770 Ma Strangways Orogeny. Had a granitic precursor. Appears as Warimbi Granite in Fig.5 on p243 [possibly influenced by mention of the Harverson Granite a few lines above].|1785 +/- 22 Ma (Collins and Williams, 1995).|||(Granite precursor) intrudes Reynolds Range Group.||
26331|Warimbi Schist|69427|4|Described|p12:26, 28, 30, 32, 64|Statherian|Orosirian|Collins and Williams (1995). Central Reynolds Range, Aileron Province. Foliated granite up to 1km thick. SHRIMP U-Pb zircon age.|1785 +/- 22 Ma (Collins and Williams, 1995).|||Intrudes Lander Rock Formation, Mount Thomas Quartzite and Reynolds Range Group.|A series of sills and lopolith-like bodies: typically occurs as quartz augen schist, locally with weakly foliated, fine-grained biotite-bearing quartz monzonite.|12-JUL-16
26331|Warimbi Schist|70376|6|Mentioned|p833, p833 fig 2, p834|Paleoproterozoic|Paleoproterozoic|Protolith was voluminous S-type granites.|1785 Ma +/-  22 Ma|||||
26331|Warimbi Schist|71858|5|Briefly described|p5, p28, p30|Statherian|Statherian|Aileron Province. Outcrops in the Reynolds Ranges.|ca. 1780 Ma||||Meta-igneous schists.|
24562|Warnes Sandstone Member|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24562|Warnes Sandstone Member|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24562|Warnes Sandstone Member|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24562|Warnes Sandstone Member|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Kurinelli Sandstone. Arenite and feldspathic arenite, massive to poorly bedded, poorly sorted. Geological Province: Tennant Creek Block.||||||07-NOV-08
24562|Warnes Sandstone Member|41129|4|Described|Table 1|||||||||
24562|Warnes Sandstone Member|41204|6|Mentioned|p10|||||||||
24562|Warnes Sandstone Member|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Kurinelli Sandstone. Quartz and lithic/feldspathic arenite; massive to poorly bedded.||||||16-NOV-05
24562|Warnes Sandstone Member|41308|5|Briefly described|Table 2|||||||||
24562|Warnes Sandstone Member|41310|5|Briefly described|Table 1|||See also p11.||||||18-DEC-06
24562|Warnes Sandstone Member|41408|6|Mentioned|Map legend|Proterozoic||||||||
24562|Warnes Sandstone Member|42643|4|Described|p5, Table 1 p9|||Of the Kurinelli Sandstone.||||||18-DEC-06
24562|Warnes Sandstone Member|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Kurinelli Sandstone. Quartz arenite, feldspathic arenite, poorly bedded.||||||07-NOV-08
24562|Warnes Sandstone Member|45167|4|Described|Table 1|||Of the Kurinelli Sandstone.||||||18-DEC-06
24562|Warnes Sandstone Member|49033|2|Defined|p11|Proterozoic|Proterozoic|||||||
24562|Warnes Sandstone Member|64735|4|Described|p212|Orosirian|Orosirian|A massive unit near base of Oooradidgee Group. Mean age using SHRIMP RG 207Pb/206Pb on detrital zircons from silicified quartz sandstone (this publication). See also abbreviations Warnes Member (p206 Fig 2, p212); Warnes Sandstone (p205 Fig 1, p212 Tb1, p213).|1837+/-7 Ma.|Of Kurinelli Sandstone.||||20-APR-12
24562|Warnes Sandstone Member|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in upper part of Kurinelli Sandstone.|||Arenite and feldspathic arenite: massive to poorly bedded, poorly sorted.|17-OCT-11
24562|Warnes Sandstone Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area. The Rank (Member) is omitted.|1836 +/- 7 Ma (maximum depositional age).|Kurinelli Sandstone.||||
24562|Warnes Sandstone Member|67352|4|Described|p10 Tb.1|Orosirian|Orosirian|500 m thick. Forms knobbly strike ridges. Quartz veins contain W minerals.||Kurinelli Sandstone||Lenses within Kurinelli Sandstone.|Feldspathic, lithic arenite: massive to poorly bedded, medium-to coarse-grained, poorly sorted.|
24562|Warnes Sandstone Member|68518|4|Described|p10 Tb.1, p11|Proterozoic|Proterozoic|Thickness: 0-500+ m.||Kurinelli Sandstone||Conformable band at or near base of Kurinelli Sandstone in NW; intruded by rhyolitic granophyre.|Knobbly ridge-forming quartz arenite (pooorly-bedded to non-bedded) and feldspathic arenite.|30-MAY-16
24562|Warnes Sandstone Member|69424|5|Briefly described|p9:5, 25, 55|Paleoproterozoic|Paleoproterozoic|500m thick; conformable lenses within Kurinelli Sandstone. Appears as Warnes Creek Member on p9:55, where it is mentioned as hosting W-bearing quartz veins at the Wolfram Hill group of deposits in the Hatches Creek [sic] tungsten field.|1837 +/- 7 Ma maximum deposition age.|Kurinelli Sandstone.|||Variably feldspathic (and lithic?) sandstone and quartz sandstone.|12-JUL-16
24562|Warnes Sandstone Member|69425|4|Described|p10:5, 8|||Blake et al. (1985). Occurs as conformable lenses within Kurinelli Sandstone. Bedding is destroyed by slumping and/or earthquake activity. Maximum thickness 500m. Maximum depositional age; detrital zircon spectrum is comparable to that of the Bullion Schist.|1837 +/- 7 Ma (Claoue-Long et al., 2008).|Kurinelli Sandstone.|||Characteristically massive, variably feldspathic (and lithic?) sandstone and quartz sandstone.|12-JUL-16
24562|Warnes Sandstone Member|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1837+/-11 Ma (MDA: U-Pb zircon SHRIMP)|Ooradidgee Group.|||Sandstone.|
24562|Warnes Sandstone Member|72379|5|Briefly described|p8-9|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. Claoue-Long et al (2008) reported interpreted maximum depositional age of 1837+\-7 Ma (SHRIMP U-Pb zircon).|1837+\-7 Ma (max dep age; SHRIMP U-Pb)|Unit of Kurinelli Sandstone.||||
24562|Warnes Sandstone Member|72380|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||Unit of Kurinelli Sandstone.||||
24563|Warramana Sandstone|22538|6|Mentioned|App1 P722|||||||||
24563|Warramana Sandstone|22853|4|Described|14|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of theTawallah Group.Overlain by Masterton Sandstone and Nyaran beds; underlain by Wollogorang Formation and Gold Creek Volcanics.||||||18-DEC-06
24563|Warramana Sandstone|23395|5|Briefly described|p388|||||||||
24563|Warramana Sandstone|23396|5|Briefly described|p407 Fig.2|||Of the Tawallah Group.||||||18-DEC-06
24563|Warramana Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
24563|Warramana Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
24563|Warramana Sandstone|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with Gundi Sandstone (Katherine River Group).  Geological Province: McArthur Basin.||||||
24563|Warramana Sandstone|24050|6|Mentioned|p27|||||||||
24563|Warramana Sandstone|32658|6|Mentioned|p106|||See also p107. Refers Smith (1964). Name not in use.||||||18-DEC-06
24563|Warramana Sandstone|42385|4|Described|p14, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of Tawallah Group. Disconformably overlain by Nyantu beds, unconformably by Masterton Sst. Max. thickness: 120m. Med.- to coarse-grained, feldspathic and lithic sandstone; conglomeratic in places. Parts now reassigned to Masterton and Tatoola Sandstones.||||||18-SEP-07
24563|Warramana Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||In schematic section, underlies Smythe Sandstone.|Lithic and felspathic sandstone, in places conglomeratic; shale. Detailed lithology given.|09-NOV-11
24563|Warramana Sandstone|42639|4|Described|p16|||||||||
24563|Warramana Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
24563|Warramana Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Lower red hematitic medium-to thick bedded litharenite, seperated from upper white thin to medium bedded sublitharenite and minor litharenite by a thin ferruginous interval.||||||19-OCT-05
24563|Warramana Sandstone|42812|1|Redefined|p80|Proterozoic||Age: 1713 +/- 6Ma. Of the Tawallah Group.||||||18-DEC-06
24563|Warramana Sandstone|42873|5|Briefly described|Fig.1, P110|||||||||
24563|Warramana Sandstone|43036|3|Fully described|p33|||Of the Tawallah Group.||||||18-DEC-06
24563|Warramana Sandstone|44287|14|Not recorded|p.11, opp.9|||Torrential cross-bedding present. (E53-3).||||||
24563|Warramana Sandstone|44288|14|Not recorded|map legend|||Quartz sandstone. Lower (?) Proterozoic.||||||
24563|Warramana Sandstone|44530|14|Not recorded|p.6,9,10, opp.10|||(McArthur Group). (D53-15).||||||
24563|Warramana Sandstone|44531|14|Not recorded|map legend|||Lower (?) Proterozoic.||||||
24563|Warramana Sandstone|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
24563|Warramana Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Overlain by Nyanantu beds and Tanumbirini Rhyolite, underlain by Wollogorang Formation.||||||
24563|Warramana Sandstone|62084|5|Briefly described|p936 Fig.5|||Calvert Superbasin. Shown as Warramana Sst.||||||
24563|Warramana Sandstone|63112|6|Mentioned|p1189, p1191 Fig.2, p1192, p1198-1206 |||See also p1194-1197. Calvert Superbasin. Framework grain dissolution after burial produced secondary porosity, allowing movement of basinal brines similar to those reported from Pb-Zn and U deposits of southern McArthur Basin. Mis-spelt as Waramana on p1197. Age approximated from Fig.2. 120 to >256 m thick.|c.1725 Ma.|Unit in Big Supersequence.|||Proximal fluvial facies: poorly sorted and immature, coarse- to fine-grained; locally conglomeratic.|
24563|Warramana Sandstone|64815|6|Mentioned|p5 Fig.3, p16  |||Often missing in stratigraphic successions.||Of the Tawallah Group.||||
24563|Warramana Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Of the Tawallah Group.|Appears to include Pungalina Member.|||07-JUN-18
24563|Warramana Sandstone|65228|4|Described|pp22-23, Figs.02, 05, 07, 10.|||McArthur Basin. c.200-300 m thick shallow marine clastic unit. Has an interpreted important sequence boundary which matches a discontinuity in the Echo Sandstone.||Unit in Tawallah Group.||Overlies Wollogorang Formation and Gold Creek Volcanics. Is overlain locally by Tanumbirini Rhyolite. Correlated with Echo Sandstone.|Massive to pisolitic ironstone, haematitic mudstone, ferruginous pebbly sandstone, sandstone.|
24563|Warramana Sandstone|65337|6|Mentioned|p15.|||Southern McArthur Basin.||||||
24563|Warramana Sandstone|65340|5|Briefly described|p12 Fig.6, p47, p53 .|||Partly equivalent to the lithologically similar Echo Sandstone. Restricted to Wearyan Shelf.||Unit in Tawallah Group.||Overlies Gold Creek Volcanics. Is unconformably overlain by Nyanantu Formation, Masterton Sandstone and Tanumbirini Rhyolite.||23-MAR-18
24563|Warramana Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region. Is intruded by an unnamed granitoid dated at 1725 +/- 4 Ma.||||||
24563|Warramana Sandstone|69430|4|Described|p15:3, 10, 12|||SW McArthur Basin. Over 250m thick. Mainly shallow-marine high-energy deposits. Lithologically similar and part-equivalent to Echo Sandstone. Is correlated with the Pungalina Member-Hobblechain Rhyolite succession in the SE of the Basin.||Tawallah Group.|Pungalina Member.|Conformably overlies Wollogorang Formation or Gold Creek Volcanics. Is overlain by Tanumbirini Rhyolite conformably, Nyanantu Formation disconformably, and Masterton Sandstone unconformably.|Medium- to coarse-grained, litharenite, ferruginous sandstone, mudstone, pisolitic ironstone and conglomerate, sublitharenite and quartzarenite.|12-JUL-16
24563|Warramana Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group|Includes Pungalina Member|Overlain by Nyanantu Formation, Tanumbirini Rhyolite, Echo Sandstone, overlies Gold Creek Volcanics, Hobblechain Rhyolite, Wollogorang Formation||
24563|Warramana 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||Overlies Wollogorang Formation and partially overlies Gold Creek Volcanics and is partially equivalent to Pungalina Member and underlies Nyanantu Formation.||
24563|Warramana Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin. Partly equivalent to Pungalina Member[?].||Tawallah Group|Pungalina Member?|Partly underlain by Wollogorang Formation, Gold Creek Volcanics, Hobblechain Rhyolite, Packsaddle Microgranite. Partly overlain by Nyanantu Formation, Tanumbirini Rhyolite, Echo Sandstone.||
24563|Warramana 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||Overlies Wollogorang Formation and also equivalent to Gold Creek Volcanics, equivalent to Pungalina Member and equivalent to Hobblechain Rhyolite and underlies Nyanantu Fm and Echo Sandstone.||
24563|Warramana Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group||Partly underlain by Wollogorang Formation and Gold Creek Volcanics. Overlain by Nyanantu Formation and(?) Tanumbinini Rhyolite. May be equivalent to Pungalina Member (Echo Sandstone(?)).||
24563|Warramana Sandstone|73412|5|Briefly described|p4, 8|||Southern McArthur Basin.||Tawallah Group.||Overlies Gold Creek Volcanics and Wollogorang Formation. Is overlain by Tanunbirini Rhyolite, Nyanantu Formation and Echo Sandstone.||
30741|Warramunga Formation|22446|5|Briefly described|p20|Orosirian|Orosirian|Also on page 26||||||
30741|Warramunga Formation|22524|6|Mentioned|p34,p35|Orosirian|Orosirian|||||||
30741|Warramunga Formation|22645|6|Mentioned|P212, Fig9||Orosirian|Age of unit is 1860 Ma||||||
30741|Warramunga Formation|23118|4|Described|p439||Paleoproterozoic|||||||07-NOV-08
30741|Warramunga Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Undifferentiated, lithic arenite including volcanic arenite ('metagreywacke'), siltstone, shale, slate and terrigenous mudstone; 'haematite shale'; minor phyllite; chert including jasper. Also subdivided into siltstone and sandstone lithofacies.||||||07-NOV-08
30741|Warramunga Formation|23733|3|Fully described|p4|Paleoproterozoic|Paleoproterozoic|Previously combined with the now Flynn Group and known as Warramunga Group.  See also p2, p26||||||07-NOV-08
30741|Warramunga Formation|23809|5|Briefly described|p26, p27|Paleoproterozoic|Paleoproterozoic|Age: 1862+/-5Ma.  Time equivalent of Junalki Formation.  Geological Province: Tennant Inlier.||||||07-NOV-08
30741|Warramunga Formation|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Age: 1860Ma.  Intruded by Tennant Creek Suite.  Geological Province: Tennant Inlier.  See also p21 and 33.||||||07-NOV-08
30741|Warramunga Formation|24172|2|Defined|p4, p74 Appendix, p56|Paleoproterozoic|Paleoproterozoic|Overlain by Flynn Subgroup (unconformably). Geological Province: Tennant Creek Inlier. Max. thickness: ~3000m. Age: 1862+/-9Ma. Replaces Warramunga Group of Ivanac (1954).||||||07-NOV-08
30741|Warramunga Formation|24197|6|Mentioned|p22, p65|||Parts included in Tennant Creek Supersuite. Polydeformed succession of lithic, sublithic, arenite, wacke and siltstone, terrigenous mudstone and hematitic shale. Geological province: Tennant Creek/Davenport province.||||||07-FEB-11
30741|Warramunga Formation|24294|5|Briefly described|p1168 Fig.1, p1170|Paleoproterozoic|Paleoproterozoic|Unconformbly overlain by the Churchhills Head Group. Age: ~1860 MA. Geological Province: Tennant Creek Inlier.||||||07-NOV-08
30741|Warramunga Formation|43223|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Formerly part of Warramunga Group.||||||07-NOV-08
30741|Warramunga Formation|43224|5|Briefly described|Map legend||Paleoproterozoic|||||||07-NOV-08
30741|Warramunga Formation|43568|6|Mentioned|p501|||Formerly 'Carraman Formation'||||||
30741|Warramunga Formation|43749|6|Mentioned|p4|||Age: 1860-1870 Ma||||||
30741|Warramunga Formation|43751|4|Described|p609||Paleoproterozoic|Depositional age(max): 1860 Ma||||||07-NOV-08
30741|Warramunga Formation|43850|5|Briefly described|p262,261.1|||Previously lower part of Warramunga Group.||||||14-APR-08
30741|Warramunga Formation|44158|6|Mentioned|p37|||||||||
30741|Warramunga Formation|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Turbiditic crystal-lithic; tuffaceous, volcaniclastic and lithic sandstone ('metagreywache'), siltstone, shale (including 'haematite shale'), slate and mudstone.||||||07-NOV-08
30741|Warramunga Formation|50588|5|Briefly described|p1.1, 2.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Age: 1872 +/- 9Ma (Shrimp). Intruded by Tennant Creek Supersuite.||||||07-NOV-08
30741|Warramunga Formation|60675|6|Mentioned|Map legend|||Mentioned only in relation to correlatives of the group.||||||11-JAN-05
30741|Warramunga Formation|60684|5|Briefly described|p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Supersedes Warramunga Gp based on lith./structural grounds.  Succession of tuffaceous lithic arenite and lithic wacke, and siltstone' terrigenous mudst. and argillaceous, banded-ironst. ("Haematite shale").Max. thick:~3000m.Age:1862+/-9, 1859+/-13Ma.||||||01-MAR-13
30741|Warramunga Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|In the Tennant Creek region.||||||07-NOV-08
30741|Warramunga Formation|61861|6|Mentioned|Fig.2.|||Tennant Creek.||||||
30741|Warramunga Formation|62082|5|Briefly described|p94|||Includes turbidites - graded beds of sandstone and siltstone weathered to ferruginous saprolite. Geological Province: Tennant Creek Terrain.||||||07-FEB-11
30741|Warramunga Formation|64559|5|Briefly described|p973, p975 Fig. 8, p975 Fig. 9|||Underlie Flynn Subgroup. Age: 1860Ma (detrital zircons). Sequence of well-bedded sandstone and shale derived from felsic volcanic protolith and emplaced in a turbiditic depositional environment. See p975 Fig. 9 for more ages.||||||02-JUN-10
30741|Warramunga Formation|64722|5|Briefly described|Fig. 2 p3-6, p10|Orosirian|Orosirian|Oldest exposed rock unit in the Tennant Region of the North Australian Craton.|~1862 Ma.|||||11-APR-12
30741|Warramunga Formation|64725|5|Briefly described|p69.|Paleoproterozoic|Paleoproterozoic|Warramunga Province, Tennant Creek Inlier. Lower greenschist facies clastic sedimentary and volcaniclastic rocks; host to Au, Cu, Bi mineralisation.|c.1870 Ma.|||||
30741|Warramunga Formation|64730|5|Briefly described|p141-142|Paleoproterozoic|Paleoproterozoic|Age from intercalated volcanics. Correlated with Junalki Formation, [South] Alligator and Finniss River Groups.|1862 +/- 9 Ma (Compston 1995; Smith 2001).|||Underlies Ooradidgee Group.||03-MAY-12
30741|Warramunga Formation|64735|4|Described|p205 Fig 1, p206 Fig 2, p215, p216 Fig15|Orosirian|Orosirian|Previously correlated with Bullion Schist; formerly suggested as equivalent to Lander Package; equivalent to Junalki Formation, Woodenjerrie beds; possibly correlates with Stubbins Formation.|ca. 1860Ma.|Of Warramunga Group.||Unconformably underlies Ooradidgee Group; intruded by Tennant Creek Supersuite.||20-APR-12
30741|Warramunga Formation|64736|6|Mentioned|p221 Fig.3, p222|Orosirian|Orosirian|In Tennant Region.||||Underlies Ooradidgee Group and unconformably underlies Hatches Creek Group.||30-APR-12
30741|Warramunga Formation|64737|6|Mentioned|p232 Fig.2, p244||Orosirian|Name possibly used interchangeably with Warramunga Group in this paper.|~1860 Ma.|||||01-MAY-12
30741|Warramunga Formation|64738|6|Mentioned|p258.|Paleoproterozoic|Paleoproterozoic|Intruded by a suite of phlogopite-bearing lamprophyre dykes aged 1711.3 +/- 2.2 Ma which contain inherited zircons aged c.1860-1800 Ma. [See also Warramunga Group.]||||||23-APR-12
30741|Warramunga Formation|65209|5|Briefly described|p35 Fig.1, p36, p37, p38, p39|Paleoproterozoic|Paleoproterozoic|Of Donellan et al. (1991, 1995). Formerly of Warramunga Group. Now not in any Group. Tightly folded sedimentary rocks. Likely Warramunga Formation/Ooradidgee Group provenance of Blanche Creek Member clasts.||||Is unconformably overlain by Yungkulungu Formation. Broadly correlated with Junalki Formation and Woodenjerrie beds.||05-JAN-17
30741|Warramunga Formation|65222|4|Described|p113-115, Tb 1, p109, 110, 111,123-126|Paleoproterozoic|Paleoproterozoic|Oldest known rocks in the Tennant Creek Block. 3 samples dated here by U/Pb SHRIMP. Previous data: 1766 +/- 80 Ma Rb-Sr (Black, 1977) - measuring post-lithification processes; ~ 1935 Ma conventional U-Pb including inheritance (Page, 1993). Deep water environment. Shows Barramundi Orogeny deformation.|1861 +/-7 Ma; 1859 +/-13 Ma; 1862+/-9 Ma.||Eldorado greywacke, Gecko felsic tuff, White Devil greywacke|Unconformably overlain by Churchills Head Group (nth), Hatches Creek Group (sth)|Deformed monotonous volcaniclastic greywackes. Unaltered medium-grained feldspathic to lithic greywacke and an altered felsic tuff sampled for dating.|24-JAN-22
30741|Warramunga Formation|65232|6|Mentioned|App. 2|||||||||09-FEB-10
30741|Warramunga Formation|65338|5|Briefly described|p6. |Orosirian|Orosirian|Warramunga Province, Tennant Region.|c.1860 Ma (Maidment et al. 2006).||||Polydeformed, sub- to lowermost-greenschist-facies, tuffaceous turbiditic succession.|
30741|Warramunga Formation|65345|6|Mentioned|p11 Figs.11 & 12.  |||||||||
30741|Warramunga Formation|66767|5|Briefly described|p57|||Warramunga Province, and basement to Davenport Province. Hosts significant IOCG mineralisation in the Tennant Creek and Rover fields.||||Correlative of Junalki Formation and Woodenjerrie beds.||
30741|Warramunga Formation|66860|6|Mentioned|p6 Tb.1|||Tennant Region. Deposition was coeval with lower parts of Tanami Group (Tanami Region) and Lander Rock beds (Arunta region).||||||
30741|Warramunga Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region. Parts of this unit with different magnetic responses are mapped separately.|||||Volcanilithic and turbiditic sequences: metagreywacke, siltstone, shale, haematite shale, slate, siltstone.|
30741|Warramunga Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p30|||Tennant Creek/Davenport area.|1859 +/- 7 Ma (maximum depositional age).|||||
30741|Warramunga Formation|67329|5|Briefly described|p1|Paleoproterozoic|Paleoproterozoic|Tennant Creek area. Ironstones host high grade Au-Cu-Bi deposits. Considered analogous to the Junalki Formation.||||||
30741|Warramunga Formation|67352|5|Briefly described|p8|Orosirian|Orosirian|Warramunga Province. Part of a volcanosedimentary package including also the Woodenjerrie beds and Junalki Formation.||||Correlated with Junalki Formation and Woodenjerrie beds.|Turbiditic.|08-JAN-15
30741|Warramunga Formation|69187|4|Described|p51-56, p60-62, incl. Fig.2 and 3, Tb.1|Orosirian|Orosirian|Warramunga Province. Relatively deep water turbiditic sedimentary rocks. Mineralisation hosted by structurally controlled ironstone bodies. Max age:1861.4 +/- 3.3 Ma  from White Devil Mine. Min age: intruding granites and felsic porphyries range between 1858 +/- 12 and 1840 +/- 9 Ma. Also interpreted maximum depositional age 207Pb/206Pb ages of 1860.8 +/- 3.7 Ma from Explorer28 diamond hole. Relatively small age range obtained from felsic intrusive rocks in this study suggests that magmatism in Warramunga Formation took place over a very short period of time, with six ages obtained within 2 uncertainty limits of a weighted mean age of 1847.6 +/- 1.9 Ma.|max depositional age ca. 1860 Ma, detrital zircon||[informal] Smelter porphyry, [informal] Airport porphyry, ?possibly [informal] Quarry porphyry, ?possibly [informal] White Devil porphyry|is unconformably overlain by Yungkulungu Formation and Epenarra Volcanics (Ooradidgee Group)|turbiditic sequence of interbedded sandstone, siltstone, mudstone and banded ironstone; contains felsic porphyries|14-APR-15
30741|Warramunga Formation|69417|5|Briefly described|p2:4-5,|Orosirian|Orosirian|Warramunga Province.||||Is intruded by Tennant Creek Supersuite.||12-JUL-16
30741|Warramunga Formation|69418|5|Briefly described|p3:7, 12, 25|||Tennant Region. Hosts several gold-in-ironstone IOCG deposits; also several Cu-Au(-Bi-Co) deposits and the Explorer 108 Zn-Pb-Ag deposit (described).|||||Contains pipe-like to podiform lenses of ironstone.|12-JUL-16
30741|Warramunga Formation|69423|6|Mentioned|p8:1|||Warramunga Province. Possible stratigraphic equivalent of the Murphy Metamorphics (Murphy Province).||||||12-JUL-16
30741|Warramunga Formation|69424|4|Described|p9:1-10, 12, 14-15, 17, 26, 28-34, 39-40|Paleoproterozoic|Paleoproterozoic|See also 43-48, 50-51, 53. Warramunga Province. Turbidite deposits c.3000m thick, derived from the east. Hosts iron-oxide associated copper-gold mineralisation in the Tennant Creek goldfield (eg Nobles Nob mine). Deformation during the c.1850 Ma Tennant Event is described. Has widespread slaty cleavage, and local schistosity in shear zones. Deformation detailed. Geochemistry (REE) briefly described. Other ages indicate maximum deposition of greywackes at 1861 +/- 7 Ma and 1859 +/- 13 Ma. Lateral equivalent of Junalki Formation, Woodenjerrie beds; correlate of Finniss River Group.|1862 +/- 9 Ma; probable tuff (Compston, 1995).|||Is overlain unconformably by Warrego Volcanics and Yungkulungu Formation (and faulted against the latter). Is intruded by Tennant Creek Granite and Devils Suite.|A polydeformed succession of tuffaceous/volcanilithic sandstone/wacke ("metagreywacke") and siltstone; banded argillaceous ironstone ("haematite shale"); shale; slate; minor schist.|12-JUL-16
30741|Warramunga Formation|69425|6|Mentioned|p10:2, 22|||Tennant Region.||||||12-JUL-16
30741|Warramunga Formation|69431|6|Mentioned|p16:2-3, 7|||Tennant Region. A likely source of sediments for the Meerie Member (Hayward Creek Formation).||||||12-JUL-16
30741|Warramunga Formation|69458|6|Mentioned|p42:15; 42:32 Fig.42.35|Paleoproterozoic|Paleoproterozoic|Bedrock to the Cabbage Gum Basin.||||||12-JUL-16
30741|Warramunga Formation|69673|6|Mentioned|p3 fig 2|Orosirian|Orosirian|||||||
30741|Warramunga Formation|69747|5|Briefly described|p272|Orosirian|Orosirian|Geological province: Tennant Creek Inlier. SHRIMP detrital zircons U-Pb data yielded maximum depositional age constraints of ca. 1860 Ma. Minimum age constraint of 1847 Ma provided by felsic intrusive and porphyries. Hosts the Tennant Creek Goldfield.|1860 Ma||||Turbiditic sequence of interbedded greywacke, siltstone, mudstone and banded ironstone.|25-JUN-19
30741|Warramunga Formation|69917|6|Mentioned|p87|||Tennant Region. One of a number of North Australian Craton sources of zircons older than 1900 Ma. ||||||
30741|Warramunga Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1862 /- 9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Greywacke, felsic volcanics; gold ore replacing greywacke.|
30741|Warramunga Formation|72707|6|Mentioned|p2, p4|||Warramunga Province.||||||
30741|Warramunga Formation|73083|6|Mentioned|p44|||||||||
30741|Warramunga Formation|73089|6|Mentioned|p32, p34|||Warramunga Province, Tennant Region. Dominant age components at c. 1861 Ma and minor components at c. 2500 Ma. Minor felsic volcanic rocks in the unit were emplaced at 1862 +/- 9 and 1862 +/- 5 Ma and sedimentation possibly continued until deformation and felsic magmatism of the c. 1850 Ma Tennant Event.|||||Turbiditic metasedimentary rocks.|
30741|Warramunga Formation|73124|5|Briefly described|piii, p2 Fig.1, p19|Orosirian|Orosirian|Geochron is from a felsic tuff that is indistinguishable in age from an unnamed porphyritic dacite (1858.4 +/- 5.0 Ma) from drillhole R27ARD18 at Rover 27 prospect (sample 2018339531). This is the best direct evidence as far of the presence of this unit in the Rover field subsurface (oldest known rock in the field). Hosts significant gold, copper and bismuth mineralisation at Tennant Creek.|1862 +/- 9 Ma|||Overlain by Yungkulungu Formation. Correlates to Junalki Formation.||
30741|Warramunga Formation|73125|5|Briefly described|iii, 1-2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province. A minor part of the mineralised basement in the Rover field.||||||
30741|Warramunga Formation|73128|6|Mentioned|p13|Orosirian|Orosirian||1.86 Ga|||Unconformably overlain by Hatches Creek Group.||
30741|Warramunga Formation|73427|4|Described|p3-5, p11-12, p14, App.A|Orosirian|Orosirian|North Australian Craton, Tennant Region/East Tennant. Reflects a turbiditic setting. Deposition may have continued until ca 1848 Ma, although this interpretation requires re-examination. Regionally metamorphosed to lowermost greenschist-facies conditions. Deformation interpreted to have occurred between ca 1860 and 1855 Ma.|1865-1860 Ma|||Unconformably overlain by Yungkulungu Formation. Intruded by Tennant Creek Supersuite.|Turbiditic wacke, siltstone, and minor felsic volcanic rocks.|
30741|Warramunga Formation|73460|6|Mentioned|p2|||Warramunga Province.||||||
30741|Warramunga Formation|73550|5|Briefly described|p4-5, p19|Orosirian|Orosirian|Warramunga Province. Outcrop is confined to the Tennant Creek goldfield.|ca 1860 Ma|||Equivalent to Junalki Formation and Woodenjerrie beds. Unconformably overlain (angular) by Ooradidgee Group.|Mostly weakly metamorphosed turbiditic greywacke, locally tuffaceous, with lesser siltstone, shale and argillaceous ironstone.|
30741|Warramunga Formation|73590|5|Briefly described|p1-2|Orosirian|Orosirian|Warramunga Province. Some of the oldest rocks in the province. No known exposures of the unit's base. Literature refers to the argillaceous ironstone as 'haematitic ironstone'. Hosts mineralisation.|older than 1860 Ma|||Equivalent to Junalki Formation and Woodenjerrie beds. Unconformably (angular) overlain by Ooradidgee Group.|Weakly metamorphosed, turbiditic greywacke, locally tuffaceous, with lesser siltstone, shale, and argillaceous ironstone.|
24631|Warrs Volcanic Member|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Burrell Creek Formation. Submarine acid volcanics; dacitic lavas; interbedded tuffaceous siltstone and volcaniclastic lithic arenite.||||||07-NOV-08
24631|Warrs Volcanic Member|23714|4|Described|p11|Proterozoic|Proterozoic|See also page 7, Table 1. Of Burrell Creek Formation.||||||
24631|Warrs Volcanic Member|23715|5|Briefly described|Map legend||Proterozoic|Of the Finniss River Group, in the Litchfield Province.||||||18-DEC-06
24631|Warrs Volcanic Member|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24631|Warrs Volcanic Member|43187|5|Briefly described|p2|||||||||
24631|Warrs Volcanic Member|63866|5|Briefly described|p105, p108-p109|Orosirian|Orosirian|Litchfield Province, Pine Creek Orogen. |1862 +/- 3 Ma (Worden et al, in press)|Finniss River Group||||
24631|Warrs Volcanic Member|64730|5|Briefly described|p125 Fig. 3, p126-127, p136-137|Paleoproterozoic|Paleoproterozoic|Age is of extrusion. Correlated with Meeway Volcanics, Berinka Volcanics and with Mulluk Mulluk Volcanic Member of Burrell Creek Formation.|1862 +/- 3 Ma (U/Pb SHRIMP zircon).|Near base of Finniss River Group.|||Includes amygdaloidal green metadacite.|02-MAY-12
24631|Warrs Volcanic Member|64956|6|Mentioned|p72|||||||||07-FEB-11
24631|Warrs Volcanic Member|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Burrell Creek Formation.|||Metamorphosed volcanic rock; biotite-chlorite metadacite; tuffaceous siltstone; volcaniclastic lithic sandstone.|23-NOV-11
24631|Warrs Volcanic Member|67232|5|Briefly described|p4, p8 Fig.6, p29, p30.|Paleoproterozoic|Paleoproterozoic|Felsic volcanism. Hosts a belt of copper anomalies.|1862 +/- 3 Ma (Worden et al. 2006a,b).||||Includes metadacite.|
24631|Warrs Volcanic Member|67355|6|Mentioned|p.4 ||Orosirian||1862 Ma (zircon)|||||
24631|Warrs Volcanic Member|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.|1862 +/- 3 Ma (Worden et al. 2008a).|Unit in Burrell Creek Formation.||||
24631|Warrs Volcanic Member|69418|5|Briefly described|p3:15|||Daly River area, Pine Creek Orogen. Hosts VMS Cu-Zn-Ag deposits in chloritised shear zones.|||Burrell Creek Formation.|||12-JUL-16
24631|Warrs Volcanic Member|69420|5|Briefly described|p5:4, 6-7, 13, 32, 84, 87-88, 97-99|Paleoproterozoic|Paleoproterozoic|Western region, Central Domain, Pine Creek Orogen. Crops out in the Daly River region immediately W of the Giants Reef Fault. c.500m thick. Submarine lava. Comagmatic with Mulluk Mulluk, Meeway and Berinka Volcanics. Hosts volcanigenic Cu mineralisation near the Daly River Settlement: described in detail.|1862 +/- 3 Ma (Worden et al., 2008).|Burrell Creek Formation.|||Felsic volcanic flows (locally amygdaloidal), metadacite, tuffaceous sedimentary rocks, and volcaniclastic lithic sandstone. Near Giants Reef Fault, is typically strongly altered to actinolite-, chlorite- and carbonate-bearing assemblages.|12-JUL-16
24631|Warrs Volcanic Member|69917|5|Briefly described|p52|||||Basal volcanics of Finniss River Group||||
24631|Warrs Volcanic Member|69933|5|Briefly described|v, p1, p7-8, p28|Orosirian|Orosirian|Petrography, zircon characteristics, SHRIMP analyses and results are provided.|1862 +/- 3 Ma (SHRIMP U-Pb)||||Green coloured volcanic rock comprising fine-grained quartz-dominated matrix, comprehensively altered by actinolite, chlorite, carbonate and possibly siderite.|
24631|Warrs Volcanic Member|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|1862 +/- 3 Ma.|Burrell Creek Formation.|||Submarine acid volcanic rocks; metamorphosed biotite-chlorite metadacite; interbedded tuffaceous siltstone and volcaniclastic lithic sandstone.|
24631|Warrs Volcanic Member|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|1862+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Green-coloured dacitic tuff.|
41857|Warumpi Granite|65272|6|Mentioned|p317-318|||Timing of Chewings Orogeny constrained by SHRIMP U-Pb zircon ages of 1590 +/- 4 Ma and 1585 +/- 8 Ma from this unit (Page, 1996).|1640-1635 Ma.|||||
41857|Warumpi Granite|67565|2|Defined|p61, p18, p7 Table 1, p23, p34.|Statherian|Statherian|New name, after Warumpi Outstation. Yaya Domain, Warumpi Province. Previously included in undifferentiated Arunta Complex (Ranford, 1969). Forms prominent hills north of Mount Larrie, and a large hill (Warumpi: the type locality is on the SW side) 3 km ESE of Papunya Community. SHRIMP U-Pb zircon ages by Cross et al. (2004). Has intrusive contacts (with no clear timing relationship) with the Larrie Granodiorite. Has strong geochemical affinity with other Illili Suite granites.|1639 +/- 3 Ma and 1642 +/- 3 Ma.|Unit in Illili Suite.||Intrudes Inyalinga Granulite.|Foliated to gneissic biotite granite with large, rounded K-feldspar phenocrysts up to 3 cm diameter and locally flattened and elongated; local rapakivi texture preserved; has undergone local partial melting.|01-DEC-15
41857|Warumpi Granite|68832|4|Described|p7-12|||Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology.  Two crystallisation ages, two metamrphic ages|1639+/-3, 1642+/-3 Ma, 1591+/-4, 1585+/-8 Ma|Of Illili Suite.||Intrudes Inyalinga Granulite and Larrie Granodiorite|Foliated to gneissic porphyritic biotite granite. Granulite facies fabric in places. Locally migmatitic.|
41857|Warumpi Granite|69428|5|Briefly described|p13:8-9, 11, 14-15|Paleoproterozoic|Paleoproterozoic|Yaya Domain, Warumpi Province. Forms prominent hills N of Mount Larrie, as well as a large hill (Warumpi) 3km E of Papunya Community. SHRIMP U-Pb zircon ages by Cross et al. (2005). Metamorphic zircon rims have ages of 1590 +/- 4 Ma and 1585 +/- 8 Ma.|1642 +/- 3 Ma and 1639 +/- 3 Ma.|Illili Suite.||Intrudes Inyalinga Granulite. Intercalated with Larrie Granodiorite.|Dominated by foliated to gneissic, porphyritic biotite granite; rounded K-feldspar phenocrysts, typically 1-2 cm in diameter, commonly flattened and elongated and locally preserve rapakivi textures; local granulite-facies fabric and partial melting.|12-JUL-16
41857|Warumpi Granite|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen. Metamorphosed at 1591 +/- 4 Ma.|1639+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Porphyritic biotite granite.|
42258|Water Tower Tonalite|23809|5|Briefly described|p13, p6 Tb. 3|Paleoproterozoic|Paleoproterozoic|Of the Inningarra Suite.  Granodiorite.  Intrudes the Killi Killi Formation.  Age: 1840+/-11Ma (conventional zircon dating by Cooper and Ding, 1997), and 1821+/-4Ma (Pb-Pb).||||||07-NOV-08
42258|Water Tower Tonalite|64662|5|Briefly described|p43|Orosirian|Orosirian|Age: 1.82Ga (Crispe et al 2006). Intrudes the Killi Killi Formation.||||||07-FEB-11
42258|Water Tower Tonalite|73089|5|Briefly described|p39|Orosirian|Orosirian|Represent coeval magmatism with the felsic volcanic rocks of the Ware Group.|1821 +/- 4 Ma|Birthday Suite[?]||||
24565|Wauchope Subgroup|22446|4|Described|p20, fig1p25,fig3,|Statherian|Statherian|||||||
24565|Wauchope Subgroup|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group. Includes Kudinga Basalt, Coulters Sandstone, Yeeradgi Sandstone and Unimbra Sandstone.||||||07-NOV-08
24565|Wauchope Subgroup|23733|5|Briefly described|p3, p31|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.||||||07-NOV-08
24565|Wauchope Subgroup|23809|5|Briefly described|p27|||Of the Hatches Creek Group.  Lower part includes Unimbra Sst., Yeeradgi Sst., Arabulja and Newlands Volcanics, Tinfish Sst., Strzeleckie Volcanics and Gwynne Sst; upper part consists of Coulters Sst., Kudinga Basalt and Illoquara Sst.||||||30-NOV-04
24565|Wauchope Subgroup|24047|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.  Overlies the Ooradigee Group.  Geological Province: Tennant Inlier.||||||07-NOV-08
24565|Wauchope Subgroup|24172|5|Briefly described|p1, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Geological Province: Tennant Creek Inlier. Comprising the Frew River Formation and Coulters, Yeeradgi and Unimbra Sandstones.||||||07-NOV-08
24565|Wauchope Subgroup|24197|6|Mentioned|p65|||||||||07-FEB-11
24565|Wauchope Subgroup|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24565|Wauchope Subgroup|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hatches Creek Group.||||||10-JAN-05
24565|Wauchope Subgroup|40580|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24565|Wauchope Subgroup|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24565|Wauchope Subgroup|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Geological Province: Tennant Creek Block.||||||07-NOV-08
24565|Wauchope Subgroup|41129|3|Fully described|p5|||||||||
24565|Wauchope Subgroup|41204|4|Described|p10|||||||||
24565|Wauchope Subgroup|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Hatches Creek Group.||||||16-NOV-05
24565|Wauchope Subgroup|41308|4|Described|p11|||See also Table 2||||||
24565|Wauchope Subgroup|41310|4|Described|p11|||See also Table 1||||||
24565|Wauchope Subgroup|41408|6|Mentioned|Map legend|Proterozoic||||||||
24565|Wauchope Subgroup|41524|4|Described|p9|||||||||
24565|Wauchope Subgroup|41525|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group.  Comprises Unimbra Sandstone, Newlands and Arabulja Volcanics, Coulters Sandstone, Frew River Formation, and Kudinga Basalt.||||||07-NOV-08
24565|Wauchope Subgroup|41970|6|Mentioned|p333|||||||||
24565|Wauchope Subgroup|42643|3|Fully described|p11, Table 1 p6-8|||||||||
24565|Wauchope Subgroup|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Hatches Creek Group.||||||07-NOV-08
24565|Wauchope Subgroup|43223|5|Briefly described|Map Legend||Proterozoic|Of the Hatches Creek Group.||||||19-DEC-06
24565|Wauchope Subgroup|43224|5|Briefly described|Map legend||Paleoproterozoic|Of the Hatches Creek Group.||||||07-NOV-08
24565|Wauchope Subgroup|43802|6|Mentioned|p77-79|||||||||
24565|Wauchope Subgroup|45167|3|Fully described|p18, Table 1|||Of the Hatches Creek Group.||||||19-DEC-06
24565|Wauchope Subgroup|49033|2|Defined|p15|Proterozoic|Proterozoic|||||||
24565|Wauchope Subgroup|50353|5|Briefly described|Map Legend|||Of Hatches Creek Group.||||||
24565|Wauchope Subgroup|50588|5|Briefly described|p1.1, 3.4|||Geological Province: Tennant Creek/Davenport Province. Intruded by Treasure Suite.||||||
24565|Wauchope Subgroup|60684|5|Briefly described|p8 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. Includes Kudinga Basalt, Coulters, Yeeradgi and Unimbra Sandstones.  Geological Province: Davenport province.||||||07-NOV-08
24565|Wauchope Subgroup|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group. See also the informally named Lower and Upper Wauchope Subgroups for further details. In the Tennant Creek region.||||||07-NOV-08
24565|Wauchope Subgroup|61567|5|Briefly described|p631, p632, p633 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Gr. Includes Unimbra, Yeeradgi and Coulters Ssts, and Kudinga Basalt. Massive white x-bedded aeolian and shallow marine arenites with minor recessive foliated basalts, felsic volcanics and volcaniclastics. Age: >1660Ma. Geol.Prov:TCI||||||07-NOV-08
24565|Wauchope Subgroup|61861|6|Mentioned|p23, Fig.2.|||Tennant Inlier. Correlated with Birrindudu Group of Tanami Region.|||Includes Kudinga Basalt.|||
24565|Wauchope Subgroup|63261|6|Mentioned|p23|||Lower section is referred to. Geological province: Tennant region.||||||07-FEB-11
24565|Wauchope Subgroup|64735|5|Briefly described|p205 Fig 1, p206 Fig 2,|Orosirian|Orosirian|Mis-spelt in Fig 1.||Of Hatches Creek Group|Includes Kudinga Basalt; Arabulja Volcanics; Yeeradgi, Coulters and Unimbra Sandstones.|||30-APR-12
24565|Wauchope Subgroup|64817|6|Mentioned|p367|||Davenport Province.||||||
24565|Wauchope Subgroup|65209|5|Briefly described|p36, p37|Paleoproterozoic|Paleoproterozoic|Layer cake stratigraphy. Comprises informal Upper (Kudinga Basalt, Frew River Formation, Coulters Sandstone, Illoquara Sandstone) and Lower (Yeeradgi Sandstone, Arabulja Volcanics, Newlands Volcanics, Strzeleckie Volcanics, Tinfish Sandstone, Unimbra Sandstone, Gwynne Sandstone and Ledan Schist) subdivisions: see informal Lower Wauchope Subgroup and Upper Wauchope Subgroup. Geol. Prov: Davenport Province.||Hatches Creek Group|Informal Upper Wauchope Subgroup (4 units) and Lower Wauchope Subgroup (8 units) subdivisions. See comments.|||05-JAN-17
24565|Wauchope Subgroup|65333|5|Briefly described|Map Legend|Statherian|Statherian|Of Hatches Creek Group, Davenport Province. Includes Kudinga Basalt, Coulters Sandstone, Newlands Volcanics, Unimbra Sandstone.||||||
24565|Wauchope Subgroup|65334|5|Briefly described|Map Legend|Statherian|Statherian|Of Hatches Creek Group, Davenport Province. Underlies Errolola Sandstone of Hanlon Subgroup. Includes Kudinga Basalt, Coulters Sandstone in upper part and  Newlands Volcanics, Unimbra Sandstone in lower part.||||||
24565|Wauchope Subgroup|65338|6|Mentioned|p6, pp20-21.|Paleoproterozoic|Paleoproterozoic|||Unit in Hatches Creek Group.|Includes Unimbra, Yeeradgi, Tinfish, Coulters and Gwynne Sandstones; Newlands, Arabulja and Strzeleckie Volcanics; Frew River Formation and Kudinga Basalt.|||
24565|Wauchope Subgroup|65358|5|Briefly described|p14|Paleoproterozoic|Paleoproterozoic|Of Hatches Creek Group. Similar to Ooradidgee Subgroup but with less volcanic input.||||||
24565|Wauchope Subgroup|66767|5|Briefly described|p57|||Davenport Province. Average thickness 4km.|1815-1810 Ma.|Hatches Creek Group.||Is overlain by Hanlon Subgroup.||
24565|Wauchope Subgroup|66860|6|Mentioned|p6 Tb.1|||||||||
24565|Wauchope Subgroup|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Hatches Creek Group.|Includes Unimbra, Yeeradgi and Coulters Sandstones; Arabulja and Newlands Volcanics; Frew River Formation and Kudinga Basalt.|Is overlain by Hanlon Subgroup.||
24565|Wauchope Subgroup|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hatches Creek Group.|Includes Lower and Upper units.|Is overlain by Hanlon Subgroup.||
24565|Wauchope Subgroup|67352|5|Briefly described|p8, p9, p10 Tb.1, p44 Fig.48, p50, p59|Orosirian|Orosirian|||Hatches Creek Group|Includes Kudinga Basalt; Frew River Formation; Coulters, Yeeradgi, Unimbra Sandstones; Newlands, Arabulja Volcanics.|Is overlain by Hanlon Subgroup.|Fluviatile to nearshore-marine siliciclastic deposits.|
24565|Wauchope Subgroup|68518|4|Described|p6-8 Tb.1, p12-13|Proterozoic|Proterozoic|||Hatches Creek Group|Kudinga Basalt, Frew River Formation, Coulters Sandstone, Arabulja Volcanics, Newlands Volcanics, Yeeradgi Sandstone and Unimbra Sandstone|Overlies Ooradidgee Subgroup; overlain by Hanlon Subgroup.||30-MAY-16
24565|Wauchope Subgroup|69424|6|Mentioned|p9:2, 8, 28|Paleoproterozoic|Paleoproterozoic|||Hatches Creek Group.|Unimbra Sandstone.|||12-JUL-16
24565|Wauchope Subgroup|69425|5|Briefly described|p10:1-3, 10-20|Statherian|Statherian|Blake et al. (1985) included this unit with their Ooradidgee and Hanlon Subgroups to form the redefined Hatches Creek Group. Davenport Province.||Hatches Creek Group.|Wauchope Sgp lower (Yeeradgi, Unimbra, Gwynne, Tinfish Sandstones; Arabulja, Newlands, Strzeleckie Volcanics);Wauchope Sgp upper (Coulters, Illoquara Sandstones; Frew River Formation; Kudinga Basalt).|||12-JUL-16
24565|Wauchope Subgroup|69427|5|Briefly described|p12:8, 13|||Crops out in the Osborne and Crawford Ranges, adjacent to the N margin of the Aileron Province. Total thickness is c.3900m.||Hatches Creek Group.|Gwynne, Tin Fish Sandstones; Strzeleckie Volcanics.|||12-JUL-16
24565|Wauchope Subgroup|69431|5|Briefly described|p16:2, 5, 8, 22|||Tennant Region: Davenport Province, Osborne and Crawford Ranges. Folding during the Davenport Event is discussed.||Hatches Creek Group.|Gwynne, Tinfish, Illoquara, Unimbra, Yeeradgi, Coulters Sandstones; Strzeleckie, Arabulja, Newlands Volcanics; Frew River Formation; Kudinga Basalt.|||12-JUL-16
24565|Wauchope Subgroup|73083|6|Mentioned|p9|||Davenport Province.||Hatches Creek Group|Coulter Sandstone, Kudinga Basalt, Unimbra Sandstone, Yeeradgi Sandstone|||
39130|Wauchope Subgroup, Lower|23733|5|Briefly described|p32 Fig.19|||Informal - see Wauchope Subgroup.||||||
39130|Wauchope Subgroup, Lower|23809|5|Briefly described|p27 Fig. 25|||Informal - see Wauchope Subgroup.  Of the Hatches Creek Group. Includes Unimbra and Yeeradgi Sandstones, Arabulja and Newlands Volcancs, Tinfish Sandstone, Strzeleckie Volcanics, Gwynne Sandstone.Geological Province: Davenport Province.||||||19-DEC-06
39130|Wauchope Subgroup, Lower|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Informal name - see Wauchope Subgroup.  Age: ~1780Ma.    Geological Province: Davenport Province (Tennant Inlier).||||||07-NOV-08
39130|Wauchope Subgroup, Lower|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal - see Wauchope Group. Of the Hatches Creek Group.  Includes the Unimbra and Yeeradgi Sandstone, Arabulja, Newlands and Strzelecki Volcanics, Gwynne and Tinfish Sandstones, and the Ledan Schist. In the Tennant Creek region.||||||07-NOV-08
39130|Wauchope Subgroup, Lower|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|See Wauchope Subgroup, and informal Upper Wauchope Subgroup.||Wauchope Subgroup.|Informal subdivision encompassing Yeeradgi Sandstone, Arabulja Volcanics, Newlands Volcanics, Strzeleckie Volcanics, Tinfish Sandstone, Unimbra Sandstone, Gwynne Sandstone and Ledan Schist.|||05-JAN-17
39130|Wauchope Subgroup, Lower|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup.|Includes Unimbra, Yeeradgi, Gwynne and Tinfish Sandstones; Arabulja, Newlands and Strzeleckie Volcanics.|||
39130|Wauchope Subgroup, Lower|73083|6|Mentioned|p44|||[Written as 'Lower Wauchope Subgroup' probably to indicate specific usage].||||||
39131|Wauchope Subgroup, Upper|23733|5|Briefly described|p34 Fig.20|||Informal - see Wauchope Subgroup.  See also p32 Fig. 19.||||||
39131|Wauchope Subgroup, Upper|23809|5|Briefly described|p27 Fig. 25|||Informal - see Wauchope Subgroup.  Of the Hatches Creek Group.   Includes Coulters Sandstone, Kudinga Basalt and Illoquara Sandstone.||||||30-NOV-04
39131|Wauchope Subgroup, Upper|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Informal name - see Wauchope Subgroup.  Age: ~1780Ma.    Geological Province: Davenport Province (Tennant Inlier).||||||07-NOV-08
39131|Wauchope Subgroup, Upper|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Informal - see Wauchope Group. Of the Hatches Creek Group.  Includes the Coulters Sandstone, Frew River Formation Kudinga Basalt and Illoquara Sandstone.  . In the Tennant Creek region.||||||07-NOV-08
39131|Wauchope Subgroup, Upper|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|See Wauchope Subgroup, and informal Lower Wauchope Subgroup.||Wauchope Subgroup.|Informal subdivision encompassing Kudinga Basalt, Frew River Formation, Coulters Sandstone, Illoquara Sandstone.|||05-JAN-17
39131|Wauchope Subgroup, Upper|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup.|Includes Coulters and Illoquara Sandstones, Frew River Formation and Kudinga Basalt.|||
39131|Wauchope Subgroup, Upper|73083|6|Mentioned|p13-14, p21|||Basal unit is the Coulters Sandstone. Topmost unit is the Kudinga Basalt.||||||
26206|Weaner Sandstone|14019|5|Briefly described|p4 Fig. 3|||Of the Bullita Group.  Geological Province: Victoria Basin.||||||
26206|Weaner Sandstone|24122|5|Briefly described|p4 Fig.3|||Of Bullita Group.  Geological Province: Victoria Basin.||||||
26206|Weaner Sandstone|24297|3|Fully described|p13|Proterozoic|Proterozoic|Of Bullita Group.  Conformably overlain by Battle Creek Formation, unconformably overlies Bynoe Formation. Weaner Sandstone. Maximum thickness: 15m.||||||
26206|Weaner Sandstone|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Parent: Bullita Group. Quartz sandstone, minor granular and pebbly sandstone at base.||||||19-OCT-05
26206|Weaner Sandstone|24441|5|Briefly described|p1 Fig. 1, Appendix 2-1:4|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Sandstone and conglomerate. Unconformably overlies the Bynoe Formation; overlain by Battle Creek Formation. Thickness: 3-15m. Geological Province: Victoria Basin.||||||25-JAN-06
26206|Weaner Sandstone|24442|5|Briefly described|p50 Fig. 1|||Of the Bullita Group. Geological Province: Victoria Basin.||||||
26206|Weaner Sandstone|28255|3|Fully described|p52, Tb. 11 (op.. p8)|Adelaidean|Adelaidean|Of the Bullita Group. Consists of massive, coarse-grained quartz sandstone with grit bands. Conformably overlies Bynoe Formation; unconformably overlain by Wondoan Hill Fm and Antrim Plateau Volcs. Max. thickness: 15m. Restricted to VICTORIA RIVER DOWNS||||||
26206|Weaner Sandstone|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Bullita Group.  Coarse, quartz sandstone, grit, pebbly beds near base.||||||02-DEC-04
26206|Weaner Sandstone|33374|6|Mentioned|p7|||Strat.||||||
26206|Weaner Sandstone|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26206|Weaner Sandstone|45112|5|Briefly described|Table 10|||||||||
26206|Weaner Sandstone|48943|2|Defined|p63|Adelaidean|Adelaidean|||||||
26206|Weaner Sandstone|60685|3|Fully described|p4 Fig. 3, p1|Mesoproterozoic|Mesoproterozoic|Of the Bullita Group. Sandstone and minor polymictic pebble conglomerate. Unconformable on Bynoe Formation, on Skull Creek Formation; conformably underlies Battle Creek Formation. Max. Thickness: 179m. Geological Province: Victoria Basin.||||||
26206|Weaner Sandstone|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Bullita Group.||Is overlain by Battle Creek Formation.||
26206|Weaner Sandstone|68733|4|Described|p177 Fig.2, p179-186||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). Between 3-15m thick. Maximum depositional age of ca. 1600 +/- 24 Ma. Sm-Nd isotope data tabulated.|Maximum depositional age of ca. 1600 +/- 24 Ma.|Bullita Group.||Unconformably underlain by the Bynoe Formation. Conformably overlain by the Battle Creek Formation.|Poorly sorted, cross-bedded, gritty sandstone.|06-DEC-17
26206|Weaner Sandstone|69432|4|Described|p17:2, 10-13|||Birrindudu Basin. 3-15m thick. Uplift was probably active prior to or during deposition of this unit. Detrital zircon maximum depositional age. Is a lithostratigraphic correlative of Mount Gordon Sandstone and is possibly synonymous with it.|<1600 +/- 24 Ma (Carson, 2010).|Bullita Group.||Overlies Bynoe Formation conformably and locally unconformably. Is overlain conformably by Battle Creek Formation.|Thinly to thickly cross-bedded sandstone and minor polymictic pebble conglomerate that contains rare oolitic grainstone (?from Banyan Formation) and clasts of volcanic rock.|12-JUL-16
26206|Weaner Sandstone|69673|6|Mentioned|p48 fig 35|||||Bullita Group||Unconformably overlies Bynoe Formation||
26206|Weaner Sandstone|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Bullita Group.||Overlies Bynoe Formation, ?unconformably. Is overlain by Battle Creek Formation, and unconformably by Jasper Gorge Sandstone.|Quartz sandstone, minor granular and pebbly sandstone at base.|
26206|Weaner Sandstone|70968|5|Briefly described|p115, p124, p132|||SHRIMP U-Pb detrital zircon age: Carson (2013).|1600 +/- 24 Ma (maximum depositional age).|Top of Bullita Group.||Is overlain unconformably by Wondoan Hill Formation.||
26206|Weaner Sandstone|71302|4|Described|p1,6-7,35-42,72||Paleoproterozoic|Of Birindudu Basin. Only exposed in VICTORIA RIVER DOWNS 1:250 000 map sheet; forming a crescent shaped belt of subcrop and small scarps around the northern and western margin of the Fitzgerald Range and adjacent to Gordon Creek. Typically 3-15m thick, deposited under shoaling, shallow marine conditions (Dunster and Ahmad, 2013a). Sample GA 1956891 (immature sandstone) yielded an interpreted (weighted mean 207Pb/206Pb) maximum depositional age of 1557+\-23 Ma. Previous geochronological analysis indicated a maximum depositional age of 1600+\-24 Ma (Sample GA 1957143 of Carson, 2013; Munson, 2016 and Munson, in prep). 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. Appears as the Weaner Formation on p7. Sample description, locality, zircon description, SHRIMP analyses and results are discussed.||Unit of Bullita Group.||Overlain conformably by Battle Creek Formation. Underlain unconformably by Bynoe Formation.|Thinly to thickly cross-bedded sandstone and minor polymictic pebble conglomerate with clasts of volcanic rock.|09-DEC-19
26206|Weaner Sandstone|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1600+/-24 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
26206|Weaner Sandstone|72718|6|Mentioned|p7|||Birrindudu Basin.||Bullita Group||Underlain by Bynoe Formation and Nero Siltstone unconformably[?]. Overlain by Battle Creek Formation. Equivalent to Banyan Formation.||
73949|Weldon Metamorphics|24540|5|Briefly described|p9|||Contains a grossular garnet-monazite pod or lens about 1m in length (Kojan 1980). Host lithologies are granulite facies migmatitic metasediments, predominantly metapelites.||||||07-FEB-11
73949|Weldon Metamorphics|44114|5|Briefly described|p320, 324|||Anmatjira-Reynolds Range region, Arunta Inlier. Granulite-facies metamorphosed equivalents of the Lander assemblage.||||Transitionally overlies Lander Rock beds.||
73949|Weldon Metamorphics|64735|5|Briefly described|p216|Orosirian|Orosirian|Metasedimentary unit.||Of Lander Package.||||30-APR-12
73949|Weldon Metamorphics|64737|5|Briefly described|p231, p236 Tab.3, p240, p240 Fig.8||Orosirian|In Aileron Province. U-Pb SHRIMP dating defines maximum deposition of 1868-1879 Ma (97.5% confidence). Metamorphosed to granulite grade.||Of Lander Package.||||01-MAY-12
73949|Weldon Metamorphics|65338|6|Mentioned|p15, p34.|||Anmatjira Ranges.||||Faulted contact with Lander Rock Formation. Intruded by Anmatjira Orthogneiss.||
73949|Weldon Metamorphics|67323|6|Mentioned|Eastern Australia Time-Space Plot|||Arunta Block.||||||
73949|Weldon Metamorphics|69418|6|Mentioned|p3:32|||Reynolds Range. Commonly contains garnets.||||||12-JUL-16
73949|Weldon Metamorphics|69427|4|Described|p12:4, 6, 21, 26|||SE Anmatjira Range, Aileron Province. Apparently underwent two granulite-facies metamorphic events: c.1774 Ma (Possum Creek Charnockite intrusion), and 1590-1560 Ma Chewings Orogeny. Detrital zircon population is similar to that of Lander Rock Formation; maximum depositional age.|<1871 +/- 8 Ma (Claoue-Long et al., 2008).|||Is intruded by Anmatjira Orthogneiss and Aloolya Gneiss.|Pelitic metasedimentary gneiss, typically comprising garnet-, sillimanite- and cordierite-bearing migmatite; minor metapsammite, quartzite and mafic rock, metamorphosed at granulite-facies conditions. Cordierite-rich pelitic granofels is common.|12-JUL-16
73949|Weldon Metamorphics|70376|6|Mentioned|p833 fig 2|Paleoproterozoic|Paleoproterozoic||1860 Ma - 1818 Ma|||||
73949|Weldon Metamorphics|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Age of metamorphism.|1557+/-10 Ma (Pb/Pb monazite LA-ICPMS).||||Metapelite, metasandstone.|
73949|Weldon Metamorphics|71858|5|Briefly described|p4, p70|||Aileron Province.||||Intruded by the Yaningidjara Orthogneiss.||
73949|Weldon Metamorphics|73399|6|Mentioned|p2, App.E||||||||May include pelite, granofels, and granulite.|
27928|Wessel Group|9534|5|Briefly described|Map legend||Cambrian|Includes Marchinbar and Buckingham Bay Sandstones and Raiwalla Shale.||||||
27928|Wessel Group|9691|5|Briefly described|Map Legend|||||||||
27928|Wessel Group|9701|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||02-JUN-05
27928|Wessel Group|9733|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
27928|Wessel Group|22452|6|Mentioned|p6|Cambrian|Cambrian|||||||
27928|Wessel Group|22600|4|Described|Map legend|Neoproterozoic|Neoproterozoic|||||||
27928|Wessel Group|22808|6|Mentioned|7 fig 4|||||||||
27928|Wessel Group|23373|5|Briefly described|p318||Neoproterozoic|In the Arafura Basin.||||||19-DEC-06
27928|Wessel Group|23374|3|Fully described|Tb3p22,20,21,5,6,35,36,23,26||Neoproterozoic|Age of top of the group is uncertain - possibly Neoproterozoic. In the Arafura basin.||||||19-DEC-06
27928|Wessel Group|24047|5|Briefly described|p11|||Geological Province: Arafura Basin.||||||
27928|Wessel Group|24048|5|Briefly described|p68|Neoproterozoic|Neoproterozoic|Geological Province: Arafura Basin.||||||
27928|Wessel Group|24049|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Elcho Island Formation, Marchinbar Sandstone, Raiwalla Shale and Buckingham Bay Sandstone. Geol. Prov: Arafura Basin.||||||13-OCT-05
27928|Wessel Group|24442|6|Mentioned|p38|||Geological Province: Arafura Basin.||||||
27928|Wessel Group|32659|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
27928|Wessel Group|32660|4|Described|Table 7|||||||||
27928|Wessel Group|33729|6|Mentioned|p80|||Fauna.||||||
27928|Wessel Group|34201|6|Mentioned|p391|||Fauna||||||
27928|Wessel Group|34287|6|Mentioned|p43|||||||||
27928|Wessel Group|36473|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
27928|Wessel Group|36635|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
27928|Wessel Group|37815|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
27928|Wessel Group|38584|6|Mentioned|p21|||||||||
27928|Wessel Group|39679|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27928|Wessel Group|41406|6|Mentioned|Map legend|Ordovician|Cambrian|||||||
27928|Wessel Group|42056|4|Described|p95|||||||||
27928|Wessel Group|42058|4|Described|p113|||||||||
27928|Wessel Group|42186|6|Mentioned|p384|||||||||
27928|Wessel Group|42597|5|Briefly described|Map Legend|Adelaidean||||||||
27928|Wessel Group|43010|2|Defined|p174|Middle Cambrian|Early Cambrian|||||||
27928|Wessel Group|43292|5|Briefly described|Map Legend||Neoproterozoic|||||||
27928|Wessel Group|44112|3|Fully described|p68,Table13p74,74||Neoproterozoic|||||||
27928|Wessel Group|44338|14|Not recorded|p.6,7,opp.6|||Includes Marchinbar Sandstone, Raiwalla Shale and basal Buckingham Bay Sandstone.||||||19-DEC-06
27928|Wessel Group|44339|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
27928|Wessel Group|44475|2|Defined|p.8,10,opp.p.6, map|||(C53-15,16). Also includes Elcho Island Formation. See also Tb.1, for more details.||||||
27928|Wessel Group|44476|14|Not recorded|map legend||Neoproterozoic|Upper Proterozoic.||||||
27928|Wessel Group|46639|5|Briefly described|Map legend|Cambrian|Cambrian|Includes Buckingham Bay Sandstone, Raiwalla Shale and Marchinbar Sandstone.||||||
27928|Wessel Group|46792|5|Briefly described|p53|||Dated||||||
27928|Wessel Group|60550|5|Briefly described|Map Legend|Cambrian|Cambrian|||||||
27928|Wessel Group|60571|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Includes the Elcho Island Formation, Marchinbar Sandstone, Raiwalla Shale, and Buckingham Bay Sandstone.  Geological Province: Arafura Basin.||||||
27928|Wessel Group|61403|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Includes Elcho Island Formation, Marchinbar Sandstone, Raiwalla Shale and Buckingham Bay Sandstone. Geol. Prov: Arafura Basin.||||||
27928|Wessel Group|61561|5|Briefly described|p533|Neoproterozoic III|Neoproterozoic III|Includes Buckingham Bay Sandstone.||||||20-APR-06
27928|Wessel Group|62504|6|Mentioned|p1, 2|Neoproterozoic|Neoproterozoic|Underlies Goulburn Group.||||||19-DEC-06
27928|Wessel Group|62505|4|Described|p2|Neoproterozoic|Neoproterozoic|Siliclastic marine sediments, mostly quartz sandstones and shales. Thickness: 2300m. ||||||
27928|Wessel Group|62510|5|Briefly described|p3|Proterozoic|Proterozoic|Geological Province: Arafura Basin.||||||
27928|Wessel Group|62788|5|Briefly described|p103, p104|Neoproterozoic|Neoproterozoic|Plumb (1963) included all onshore units of southern Arafura Basin, and gave a Cambrian age. Rawlings et al.(1997) reassigned ages and stratigraphy.|||Includes Buckingham Bay Sandstone, Raiwalla Shale, Marchinbar Sandstone and Elcho Island Formation.|||03-DEC-12
27928|Wessel Group|63062|4|Described|p9 Fig. 9, p11, p49|Neoproterozoic|Neoproterozoic|Incl:Buckingham Bay Sst,Raiwalla Shale,Marchinbar Sst,Elcho Island Fm.Disconf.below Goulburn Gp. Geol.Prov:Arafura/Money Shoal Basins.Age:590-550Ma.Onshore thickness: 2300m (inferred). Shallow marine sandstone/mudstone + lesser conglomerate and carbonates||||||07-FEB-11
27928|Wessel Group|63866|5|Briefly described|p115|Cambrian|Neoproterozoic|Arafura Basin.||||||
27928|Wessel Group|64698|4|Described|lithinterp table|Ediacaran|Cryogenian|Age ~545-800Ma (Neoproterozoic III). Arafura Basin. Max thick 2300m. Succession of basal quartz sandstone followed by mudstone, quartz sandstone and calcareous/dolomitic sandstone.||||||07-JAN-09
27928|Wessel Group|65337|5|Briefly described|p95.|Ediacaran|Ediacaran|Arafura Basin. Correlative with Kiana Group. Lacks glacial deposits and underlies fossiliferous Middle Cambrian rocks.|||Includes Buckingham Bay Sandstone and Raiwalla Shale.|||
27928|Wessel Group|69297|5|Briefly described|p282, p285|Neoproterozoic|Neoproterozoic|Arafura Basin. Outcrops onshore and is present throughout the offshore part of the basin. Deposited in a shallow marine environment. ||||Disconformably overlain by the Goulburn Group.|Sandstone and mudstone with lesser conglomerate and carbonate rocks.|
27928|Wessel Group|69421|6|Mentioned|p6:6|||Arafura Basin.||||||12-JUL-16
27928|Wessel Group|69443|6|Mentioned|p28:12|||Onshore Arafura Basin.|||Buckingham Bay Sandstone, Raiwalla Shale.|||12-JUL-16
27928|Wessel Group|69451|4|Described|p35:1-6, 9-11, 13|?Early Cambrian|Neoproterozoic|Arafura Basin. Deposited in half grabens. Thickness c.10,000m offshore and c.2,300m onshore. Wrongly shown as including Jigaimara Formation in Figs.35.4 and 35.5. Age determinations discussed. Hosts lateritic bauxite on Marchinbar and Elcho Islands.|||Buckingham Bay, Marchinbar Sandstones; Raiwalla Shale; Elcho Island Formation.|Is overlain, probably disconformably, by Jigaimara Formation.|A succession of shallow marine, mostly quartz sandstone, mudstone and minor carbonate rocks.|12-JUL-16
27928|Wessel Group|69456|5|Briefly described|p40:2 Fig.40.3|Early Cambrian|Neoproterozoic|Arafura Basin. Younger age limit shown as "?early Cambrian".||||Is overlain by Goulburn Group.||12-JUL-16
27928|Wessel Group|69673|6|Mentioned|p195||||||Includes Buckingham Bay Sandstone, Raiwalla Shale, Marchinbar Sandstone, Elcho Island Formation|Disconformably (or unconformably) overlain by Goulburn Group||
27928|Wessel Group|70098|4|Described|p4-5, p7, p18 Fig.4, p19 Fig.5|Ediacaran|Cryogenian|Outcrops onshore and present throughout basin extent offshore. Age is poorly constrained. Max thickness: 10 000 m.||||Is disconformably overlain by Jigaimara Formation (Goulburn Group).|Onshore: consists mainly of shallow marine sandstones and mudstones, with lesser amounts of conglomerates and carbonates.|
27928|Wessel Group|72377|5|Briefly described|p8|Paleoproterozoic|Paleoproterozoic|Of Arafura Basin.|||Includes Buckingham Bay Sandstone.|||
27928|Wessel Group|73083|6|Mentioned|p49|Neoproterozoic|Neoproterozoic|Arafura Basin.||||Underlain by Roper Group.||
68831|Westwood Formation|60682|4|Described|p25 Fig. 22|Frasnian|Frasnian|Limestone. Interfingers with Kellys Knob Sandstone. Unconformably overlain by Buttons Formation. Of Cockatoo Group. Geological Province: Bonaparte Basin.||||||
68831|Westwood Formation|69452|6|Mentioned|p36:6 Fig.36.5|||||||||12-JUL-16
26998|Whippet Sandstone Member|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Bernborough Formation (Flynn Subgroup, Churchills Head Group). Lithic arenite; siltstone and shale; sandstone, pebble beds and granule conglomerate; thin to thick bedded to massive; heavy mineral-bearing laminae.||||||07-NOV-08
26998|Whippet Sandstone Member|23733|6|Mentioned|p6, p32 Fig. 19|||Of the Bernborough Formation.||||||
26998|Whippet Sandstone Member|23809|5|Briefly described|p27 Fig. 25|Paleoproterozoic|Paleoproterozoic|Of the Bernborough Formation.  Shown as younger than the 'Lower Flynn Group' (Wundirgi Formation) age of: 1854+/-4 or 1864+/-4Ma.  Geological Province: Tennant Inlier.||||||24-FEB-23
26998|Whippet Sandstone Member|24172|3|Fully described|p18, p8 Tb.1, p66 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Bernborough Formation. Conformably underlain by Monument Formation. Geological Province: Tennant Creek Inlier. Max. thickness: ~100m in type area. Supersedes Whippet Sandstone Formation and Whippet Sandstone.||||||07-NOV-08
26998|Whippet Sandstone Member|32174|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
26998|Whippet Sandstone Member|32959|5|Briefly described|p21|||||||||
26998|Whippet Sandstone Member|33307|5|Briefly described|p18|||Mention Fig.8.||||||
26998|Whippet Sandstone Member|35771|4|Described|Table 1|||||||||
26998|Whippet Sandstone Member|39213|5|Briefly described|p18|||See also Fig.8.||||||
26998|Whippet Sandstone Member|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of Bernborough Formation (Flynn Subgroup).||||||07-NOV-08
26998|Whippet Sandstone Member|46992|6|Mentioned|p254|||||||||
26998|Whippet Sandstone Member|48891|4|Described|p.9,10||Paleoproterozoic|Tb.1, L.Proterozoic.||||||07-NOV-08
26998|Whippet Sandstone Member|60684|5|Briefly described|p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Bernborough Formation (Flynn Subgroup). Fine- to coarse-grained, poorly to well sorted sublithic and lithic arenite with minor conglomerate and siltstone.  Max. thickness: ~100m in type area.||||||07-NOV-08
26998|Whippet Sandstone Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Bernborough Formation (Ooradidgee Group). Lithic arenite and siltstone, shale; granule conglomerate. In the Tennant Creek region.||||||07-NOV-08
26998|Whippet Sandstone Member|65209|6|Mentioned|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|||Bernborough Formation||||
26998|Whippet Sandstone Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Bernborough Formation.|||Lithic arenite and siltstone, shale; granule conglomerate.|
26998|Whippet Sandstone Member|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area. The Rank (Member) is omitted.||Bernborough Formation.||||
26998|Whippet Sandstone Member|69424|4|Described|p9:5, 15-16, 20|Paleoproterozoic|Paleoproterozoic|Revised definition by Donnellan et al. (1995). Warramunga Province. c.100m thick in type area. The top of the Member is the base of a thin (2-5m), slightly recessive green chert unit. Sublittoral to littoral and possibly fluviatile: represents a regressive succession. Correlated with part of Yungkulungu and Wundirgi Formations. Age constrained by underlying Monument Formation age of 1853+/-5 Ma and overlying Bernborough Formation age of 1845+/-+/-4 Ma.||Bernborough Formation.||Conformably overlies Monument Formation.|Fine- to coarse-grained, poorly to well sorted sublithic and lithic sandstone; minor conglomerate and siltstone.|24-FEB-23
68351|Whistleduck Dyke Swarm|69427|5|Briefly described|p12:46|||Shaw et al. (1979). Whistleduck Bore area, NE of Alice Springs; Wigley Domain, Aileron Province. No age data; but their amphibolite-facies metamorphism suggests they may be Paleo- or Mesoproterozoic in age.||||Intrudes Randall Peak Metamorphics and Trephina Granitic Gneiss.|A swarm of E-trending dolerite dykes composed of mafic amphibolites.|12-JUL-16
80339|White Violet Orthogneiss|71621|5|Briefly described|iii, p1, p21, p23-p24, p26,38-41, 45|Statherian|Statherian|Aileron Province. SHRIMP age is interpreted as the age of magmatic crystallisation and is derived from Kositcin et al, 2014. Petrography and zircon description discussed.|1793.9 +/- 6 Ma (SHRIMP U-Pb)|||Intruded by the Thring Granite, Cappocks Granodiorite. Conformably interlayered with Mascotte Orthogneiss, Kings Legend Metadolerite, Bonya Metamorphics.|Orthogneiss.|01-FEB-19
80339|White Violet Orthogneiss|71750|4|Described|p31,33|Statherian|Statherian|Geological province: Aileron Province. Exposed in western JERVOIS RANGE map sheet ('unnamed orthogneiss' of Kositcin et al 2014, Weisheit et al in prep). One of the oldest units of the Casper Suite. Interpreted to be syn-depositional with Bonya Metamorphics. U-Pb SHRIMP magmatic crystallisation age of 1794+\-3 Ma (Kositcin et al., 2014).|1794 +/-3 Ma|Unit of Casper Suite.||Conformably interlayered with Bonya Metamorphics.||20-SEP-19
80339|White Violet Orthogneiss|72370|5|Briefly described|p15|||Geological province: Aileron Province. Previously yielded a SHRIMP zircon 207Pb/206Pb igneous crystallisation age of 1794+\-6 Ma (Kositcin et al 2014).||||Crosscut by Samarkand Pegmatite.||16-DEC-19
80339|White Violet Orthogneiss|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1794 +/- 6 Ma (U-Pb zircon)|Casper Suite|||Granodioritic gneiss, rare monzodiorite and quartz monzodiorite: fine to medium-grained, equigranular to sparsely porphyritic, leucocratic with minor biotite; fresh to moderately weathered.|
80339|White Violet Orthogneiss|72516|2|Defined|p16-17, p19-p21, p24, p29, p32|Statherian|Statherian|Bonya Domain. New name, named for the White Violet copper-tungsten mine. The type location occurs in the central Bonya Hills at 607837mE 7486133mN. Previously interpreted as part of the Mascotte Gneiss Complex of Shaw et al (1985) and Freeman et al (1986). Occurs predominantly as prominent hills and ridges of boulders and tors in the Bonya Hills east of the Charlotte Fault Zone and as isolated low, rounded outcrops in the plains between the Johannsen and Jervois Ranges. SHRIMP age is derived from Kositicin et al (2014) and is interpreted as the age of magmatic crystallisation. Layers range in thickness from the 10s of metres to <1km. Generally fresh in outcrop with a thin weathering rind. Geochemistry, metamorphism, structure, regional aspects, alteration, mineralisation, geophysical response and genesis/deposition environment are detailed. Interpreted as comagmatic and cogenetic with other rocks of the Casper Suite. See also p35-39, p42, p49, p61, p105-107, p109, p123-124, p127, p135, p142-143, p145, p153, p169, p171, p189, p192, p210.|1794 +/- 6 Ma (SHRIMP Pb-Pb)|Casper Suite||Intruded by the Kings Legend Metadolerite. Interlayered with the Mascotte Orthogneiss. Intrudes the Bonya Metamorphics. Intruded by the Cappocks Granodiorite, Thring Granite and Samarkand Pegmatite.|Granodioritic gneiss, rare monzodiorite and quartz monzodiorite: fine to medium-grained, equigranular to sparsely porphyritic, leucocratic with minor biotite; fresh to moderately weathered; foliated to gneissic with discontinuous cm scale banding.|
80339|White Violet Orthogneiss|72711|6|Mentioned|p3 Fig.2.|Paleoproterozoic|Paleoproterozoic|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 Aileron Province.|||||Includes orthogneiss.|
24572|Whites Formation|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
24572|Whites Formation|22810|4|Described|Table2 P4, P13|||Previously assigned to the Golden Dyke Formation and the Masson Formation.  Maximum thickness: 500m.||||||19-DEC-06
24572|Whites Formation|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Sericite schist, commonly graphitic and pyritic.||||||07-NOV-08
24572|Whites Formation|23714|5|Briefly described|p9|Proterozoic|Proterozoic|Of Mount Partridge Group. Underlain by Coomalie Dolomite. Geological Province: Rum Jungle Region. Max. thickness: 500 m.||||||19-DEC-06
24572|Whites Formation|23715|5|Briefly described|Map legend||Proterozoic|Of the Mount Partridge Group. In the Rum Jungle Region.||||||19-DEC-06
24572|Whites Formation|23733|5|Briefly described|p32 Fig. 19|||Of Mount Partridge Group.||||||
24572|Whites Formation|24047|5|Briefly described|p5 Fig.4, p21|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Shale, dolomite. Geological Province: Pine Creek Orogen.||||||07-NOV-08
24572|Whites Formation|24442|6|Mentioned|p44|||Overlies the Coomalie Dolostone.  Magnesite deposits at the contact with the Coomalie Dolostone.||||||
24572|Whites Formation|39069|4|Described|p6|||See also Fig.7 and Table 1.||||||19-DEC-06
24572|Whites Formation|39320|6|Mentioned|Fig.2|||||||||
24572|Whites Formation|39518|6|Mentioned|p5|||||||||
24572|Whites Formation|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24572|Whites Formation|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Calcareous and carbonaceous pyritic argillite; dololutite, dolarenite; rare quartzite and calcareous para-amphibolite.||||||07-NOV-08
24572|Whites Formation|40243|6|Mentioned|Fig.2|||||||||
24572|Whites Formation|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24572|Whites Formation|40493|4|Described|p11|||||||||
24572|Whites Formation|40495|6|Mentioned|Fig.5|||||||||
24572|Whites Formation|40808|3|Fully described|p12|||||||||
24572|Whites Formation|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24572|Whites Formation|41125|6|Mentioned|p24|||Mention Fig.6||||||
24572|Whites Formation|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24572|Whites Formation|41305|4|Described|p15|||||||||
24572|Whites Formation|41663|6|Mentioned|Fig.1|||||||||
24572|Whites Formation|41878|6|Mentioned|p38|||||||||
24572|Whites Formation|42202|4|Described|p510|||See also Table 1||||||
24572|Whites Formation|43115|6|Mentioned|p181|||||||||
24572|Whites Formation|43187|5|Briefly described|p2|||||||||
24572|Whites Formation|46658|6|Mentioned|p550|||||||||
24572|Whites Formation|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Calcareous and carbonaceous pyritic argillate dololutite, dolarenite; rare quartzite and calcareous para-amphibolite.  Conformably overlies Coomalie Dolomite; conformably overlain by  Wildman Siltstone.||||||07-NOV-08
24572|Whites Formation|47049|5|Briefly described|Table|||Replaces Masson Formation in Rum Jungle area.||||||
24572|Whites Formation|50623|5|Briefly described|p257, p259 Fig.2, p260 Fig..3, p261|Paleoproterozoic|Paleoproterozoic|Graphitic pelite. Conformably overlain by Wildman Formation. Of Mount Partridge Group.||||||07-NOV-08
24572|Whites Formation|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mount Partridge Group.||||||
24572|Whites Formation|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Calcareous and carbonaceous pyritic argillite, dololutite and dolarenite; rare quartzite. Overlies Coomalie Dolostone. Overlain by Wildman Siltstone. Of Mount Partidge Group.||||||
24572|Whites Formation|61389|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Calcareous and carbonaceouspyritic argillite, dololutite and dolarenite, rare quartzite.||||||19-DEC-06
24572|Whites Formation|62375|5|Briefly described|p10 Fig. 3, 15|Paleoproterozoic|Paleoproterozoic|Shale, dolomite. Overlies Coomalie Dolomite. Geological Province: Pine Creek Orogen.||||||09-FEB-10
24572|Whites Formation|64698|4|Described|lithinterp table|Orosirian|Paleoproterozoic|Age ~2026-2500Ma. Of Mount Partridge Group. Max thick 1000m.Calcareous and carbonaceous pyritic mudstone/siltstone, dolomitic mudstone, rare quartzite; Quartz sandstone interbedded.||||||07-JAN-09
24572|Whites Formation|64730|5|Briefly described|p125 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age referred from ages of tuffaceous beds in the overlying Wildman Siltstone.|Min. deposition age 2019 +/- 4 Ma.|Of Mount Partridge Group.||Underlies Wildman Siltstone.|Carbonaceous sediments.|02-MAY-12
24572|Whites Formation|65232|5|Briefly described|p51-56, p6 Fig. 5, App. 2|Palaeoproterozoic|Palaeoproterozoic|Of Mount Partridge Group. Over Coomalie Dolostone (gradational contact). Faulted contact with Geolsec Formation. Carbonaceous siltstone and mudstone, and interbedded dololutite; slate; shale; dolomite; sandstone. Primary uranium mineralisation.||||||09-FEB-10
24572|Whites Formation|65339|4|Described|p6 Table 1, pp9-10, p19.|||Named by Crick (1984); formerly Golden Dyke Formation (Malone 1962a) and Masson Formation (Needham et al. 1980). Poorly exposed on eastern side of Rum Jungle and Waterhouse Domes. Thickness to 1200 m. Type section is 2 km southeast of Batchelor. Dark blue radiometric image is related to fixing of uranium by carbonaceous matter in original sediment.||Unit in Mount Partridge Group.||Overlies Coomalie Dolostone. Is overlain by Koolpinyah Dolostone and Wildman Siltstone.|Dark graphitic shale, carbonaceous pyritic argillite, dolostone and calcareous para-amphibolite.|
24572|Whites Formation|66683|5|Briefly described|p377.|Paleoproterozoic|Paleoproterozoic|Carbonaceous. Hosts the Rum Jungle uranium deposits as well as the Browns lead-copper-nickel-cobalt-zinc oxide and sulfide deposits.||Unit in Mount Partridge Group.||Overlies Neoarchean basement.||
24572|Whites Formation|67355|4|Described|Throughout|Paleoproterozoic|Neoarchean|Thickness: type area (2 km southeast of Batchelor) of 300 to 500 m, ranging 100 to 1300 m elsewhere. Hosts numerous occurrences of  mineral commodities (including U, Au, Cu-Co-Ni, Zn-Pb-Ag, phosphate, magnesite, iron ore and Th) close to the contact with the Coomalie Dolostone.|considered to be >2026 Ma|Mount Partridge Group||Overlies the Coomalie Dolostone conformably, underlies the Wildman Siltstone and less commonly the Geolsec Formation. Includes a correlate to the Acacia Gap Quartzite Member.|Carbonaceous argillite - consists of fine-grained, commonly pyritic calcareous and/or carbonaceous argillite with minor quartzite, dolomudstone and para-amphibolite.|25-JAN-17
24572|Whites Formation|67564|5|Briefly described|p9 Fig.4.|Paleoproterozoic|Paleoproterozoic|Rum Jungle Region, Pine Creek Orogen.|||||Shale, dolostone.|
24572|Whites Formation|67779|5|Briefly described|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen.||Unit in Mount Partridge Group.||Overlies Coomalie Dolostone. Is overlain by Wildman Siltstone.||
24572|Whites Formation|69418|5|Briefly described|p3:11-12, 15, 17, 24, 29|||Pine Creek Orogen. Hosts several Pb-Zn-Sb +/- Cu-Co-Ni(-U) deposits (described). The Cu deposits are generally sediment-hosted chalcopyrite in carbonaceous shale. Also hosts a number of unconformity-related U deposits: Dysons, Mount Burton, Mount Fitch, Rum Jungle Creek South, and Whites (described). Hosts the Beetsons surficial Fe deposit (briefly described).|||||Includes cupriferous carbonaceous shale.|12-JUL-16
24572|Whites Formation|69419|6|Mentioned|p4:3 Fig.4.3|||W. Pine Creek Orogen.||||||12-JUL-16
24572|Whites Formation|69420|4|Described|p5:4, 6, 8-9, 11-12, 14, 57, 60, 64-65|Paleoproterozoic|Paleoproterozoic|See also 75-78, 81-82, 86, 89-92, 94-97, 110. Rum Jungle region, Central Domain, Pine Creek Orogen. Over 1000m thick. Euxenic marine deposits. Hosts several U deposits (listed, including Rum Jungle), adjacent to the contact with the underlying Coomalie Dolostone. The Sundance Au deposit occurs in a similar stratigraphic context. Hosts a number of Cu, Pb, Co and/or Ni deposits; the Woodcutters and Browns deposits are described in detail. Hosts a number of iron ore deposits.||Mount Partridge Group.||Conformably overlies Coomalie (Koolpinyah) Dolostone. Is overlain by Wildman Siltstone and (unconformably) by Geolsec Formation.|Calcareous and carbonaceous shale, dololutite, dolarenite; rare quartzite.|12-JUL-16
24572|Whites Formation|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.||Mount Partridge Group.||Conformably overlies Coomalie Dolostone. Is overlain conformably by Wildman Siltstone.|Calcareous and carbonaceous pyritic mudstone/siltstone, dolomitic mudstone, rare quartzite.|
30740|Whittington Range Member|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Subgroup (Churchills Head Group). Interbedded leached calcareous shale and arenite; quartz arenite; mudstone; chertified stromatolitic bioherms; deeply weathered volcanic rocks including vesicular lava. Predominantly lateritised.||||||07-NOV-08
30740|Whittington Range Member|23733|3|Fully described|p11, p43 App.1|Paleoproterozoic|Paleoproterozoic|Of Tomkinson Creek Group. Formerly defined as Whittington Range Volcanics by Donnellan et al (1995). Conformably overlain by Morphett Creek Formation and conformably overlies Coodna Member.||||||07-NOV-08
30740|Whittington Range Member|23809|5|Briefly described|p27 Fig. 25|||Of Tomkinson Creek Group.  Geological Province: Tennant Inlier.||||||
30740|Whittington Range Member|24172|5|Briefly described|p25, p7 Tb.1, p65 Tb.9|Paleoproterozoic|Paleoproterozoic|Of the Hayward Creek Formation. Geological Province: Tennant Creek Inlier. Max. thickness: ~300m. Supersedes Whittington Range Volcanics. Intermediate volcanic rocks with thin-bedded sandstone, siltstone and mudstone.||||||07-NOV-08
30740|Whittington Range Member|24303|3|Fully described|p6, p45|Proterozoic|Proterozoic|Of the Hayward Creek Formation. Overlain by the Morphett Creek Formation. Overlies the Coodna Member. Formerly the overlying Whittington Range Volcanics, now included as part of Hayward Creek Formation. Parts previously mapped as Helen Springs Volcanics.||||||
30740|Whittington Range Member|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|At top of Hayward Creek Formation Tomkinson Creek Group). Basalt, aphanitic to medium-grained, amydaloidal to massive, deeply weathered and ferruginised; recessive; sst and micaceous mudst; thin-bedded; rippled, convolute, graded beds, dessicated, rip-up||||||07-NOV-08
30740|Whittington Range Member|24442|5|Briefly described|p14|||Top part of Hayward Creek Formation.  ||||||
30740|Whittington Range Member|43223|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation.||||||07-NOV-08
30740|Whittington Range Member|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation. Overlies the Coodna Member.||||||07-NOV-08
30740|Whittington Range Member|60684|5|Briefly described|p6 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of the Hayward Creek Formation (Tomkinson Creek Subgroup). Andesitic vesicular volcanic rock; interbedded leached white and pink siltstone and fine sandstone; quartz arenite; green mudstone.||||||07-NOV-08
30740|Whittington Range Member|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Hayward Creek Formation (Tomkinson Creek Group). Vesicular andesitic lava; mudstone, siltstone; chertified calcareous siltstone, sandstone; stromatolites. Overlies the Coodna Member.  In the Tennant Creek region.||||||07-NOV-08
30740|Whittington Range Member|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|Geol. Prov: Tomkinson Creek Province.||Hayward Creek Formation||||
30740|Whittington Range Member|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Hayward Creek Formation.||Overlies Coodna Member.|Vesicular andesitic lava; mudstone, siltstone; chertified calcareous siltstone, sandstone; stromatolites.|
30740|Whittington Range Member|69424|5|Briefly described|p9:4, 34|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. Also referred to as Whittington Range Volcanics in 9:4. Regionally widespread (flood) basalt.||Hayward Creek Formation.||Correlative of Kudinga Basalt.|Includes widespread, stratiform mafic rocks.|12-JUL-16
30740|Whittington Range Member|69425|5|Briefly described|p10:1, 10, 12, 18-19|||Davenport and Tomkinson Provinces. Interpreted to be contemporaneous with c.1811 Ma intrusive mafic magmatism of the Mount Hay Event. Appears as Whittington Range Volcanic Member on p10:10.||Hayward Creek Formation.||Correlated with Kudinga Basalt.|Widespread flood basalts.|12-JUL-16
30740|Whittington Range Member|69431|4|Described|p16:4-6, 8, 14|Paleoproterozoic|Paleoproterozoic|Tomkinson Province. c.300-600m thick. Widespread unit. Sedimentary rocks are probably shallow-marine. Correlative of Kudinga Basalt and Frew River Formation.||Hayward Creek Formation.||Conformably (gradationally) overlies Coodna Member. Is overlain disconformably, possibly locally unconformably, by Morphett Creek Formation.|Andesine-bearing, amygdaloidal basalt ("andesite") lava, and minor spherulitic rhyolite; subarkose, quartz sandstone and siltstone. The volcanic rocks are intensively weathered and lateritised.|12-JUL-16
26213|Wickham Formation|14019|3|Fully described|p14-15|||Basal unit of the Wattie Group. Sandstone, minor chert and conglomerate. Unconformably overlies Killaloc Formation; progressively overlies younger formations of Limbunya Group from east to west. Min. thickness: 315m. Geological Province: Victoria Basin.||||||
26213|Wickham Formation|24122|5|Briefly described|p4 Fig.3|||Of Wattie Group.  Geological Province: Victoria Basin.||||||
26213|Wickham Formation|24297|3|Fully described|p5|Proterozoic|Proterozoic|Of Wattie Group. Conformably overlain by Burtawurta Formation, unconformably overlies Limbunya Group. 176m thick at type section.  Geological Province: Victoria Basin.  See also p5 Tb. 2.||||||
26213|Wickham Formation|24298|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group. Quartz sandstone.||||||19-DEC-06
26213|Wickham Formation|24441|5|Briefly described|p1 Fig. 1|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Unconformably overlies the Killaloc Formation; overlain by Burtawurta Formation. Geological Province: Victoria Basin.||||||25-JAN-06
26213|Wickham Formation|24442|5|Briefly described|p50 Fig. 1|||Of the Wattie Group. Geological Province: Victoria Basin.||||||
26213|Wickham Formation|28255|3|Fully described|p33, Tb. 11 (op.. p8)|Adelaidean|Adelaidean|Basal unit of the Wattie Group. Consists of sandstone and conglomerate with subordinate siltstone and chert. Unconformably overlies several units of the Limbunya Group; conformably overlain by Burtawurta Formation. Max. thickness: 155m. See also p122 App.||||||
26213|Wickham Formation|30003|4|Described|p8, p12|||Basal unit of the Wattie Group.  Unconformably overlies the Limbunya Group. Carpentarian or Adelaidean.||||||19-APR-05
26213|Wickham Formation|30004|6|Mentioned|Map legend|Proterozoic|Proterozoic|Carpentarian or Adelaidean||||||
26213|Wickham Formation|32172|4|Described|Table 1|||Carpentarian or Adelaidean||||||
26213|Wickham Formation|32173|5|Briefly described|Map legend|Adelaidean|Carpentarian|Of the Wattie Group.  Feldspathic sandstone, laminated and brecciated chert interbeds.  Carpentarian or Adelaidean (per legend).||||||17-NOV-04
26213|Wickham Formation|32175|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive and blocky fine and medium quartz sandstone.||||||02-DEC-04
26213|Wickham Formation|32660|5|Briefly described|Table 6|||||||||
26213|Wickham Formation|33374|6|Mentioned|p7|||See also p9. Strat. table.||||||19-DEC-06
26213|Wickham Formation|33375|5|Briefly described|p7, p9 Tb. 1|||Of the Wattie Group. Overlain by the Burtawurta Formation.||||||26-APR-05
26213|Wickham Formation|33376|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26213|Wickham Formation|33378|5|Briefly described|Map legend|Adelaidean|Adelaidean|Of the Wattie Group.  Massive quartz sandstone, laminated and brecciated chert interbeds.||||||27-APR-05
26213|Wickham Formation|45112|5|Briefly described|Table 7|||||||||
26213|Wickham Formation|48943|2|Defined|p40|Adelaidean|Adelaidean|Strat. section p133.||||||07-NOV-16
26213|Wickham Formation|60589|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Wattie Group.  Quartz sandstone.  Unconformably overlies the Killaloc Formation of the Limbunya Group.  Geological Province: Victoria Basin.||||||
26213|Wickham Formation|60672|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Quartz Sandstone, micaceous stilstone and chert, basal conglomerate. Of Wattie Group. Unconformably overlies Limbunya Group. Overlain by Burtawurta Formation. Geological Province: Victoria Basin.||||||11-JAN-05
26213|Wickham Formation|60685|4|Described|p4 Fig. 3, p5|Paleoproterozoic|Paleoproterozoic|Of the Wattie Group. Fine to medium grained sandstone. Unconformably overlies Limbunya Group; conformably overlain by Burtawurta Formation. Max. Thickness: 176m in WAVE HILL. Geological Province: Victoria Basin.||||||07-NOV-08
26213|Wickham Formation|65342|6|Mentioned|p11 Fig.13. |||Victoria Basin.||Unit in Wattie Group.||Is overlain by Burtawurta Formation.||
26213|Wickham Formation|67151|5|Briefly described|Map legend.|Proterozoic|Proterozoic|Birindudu Basin.||Unit in Wattie Group.||Unconformably overlies Campbell Springs Dolostone and Fraynes and Killaloc Formations. Is overlain by Burtawurta Formation.|Massive quartz sandstone, laminated and brecciated chert interbeds.|
26213|Wickham Formation|68733|5|Briefly described|p177-184||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. 1639 +/- 16 Ma|Maximum depositional age of ca. 1639 +/- 16 Ma|Basal unit of the Wattie Group.||Unconformably underlain by the Limbunya Group. Conformably overlain by the Burtawurta Formation.|Thick bedded, red-purple ferruginous medium-grained feldspathic sandstone.|06-DEC-17
26213|Wickham Formation|69432|4|Described|p17:2, 9|||Birrindudu Basin. 175m thick. Detrital zircon maximum depositional age.|<1639 +/- 16 Ma (Carson, 2010).|Wattie Group.||Unconformably overlies several Limbunya Group units. Is overlain conformably by Burtawurta Formation or Hughie Sandstone.|Fine to medium, moderately well-sorted immature sandstone, conglomerate and chert, and rare siltstone; basal conglomerate common. Local cauliflower chert, ripple marks and mudcracks.|12-JUL-16
26213|Wickham Formation|69673|6|Mentioned|p48 fig 35|||Age is maximum depositional age.|1639 +/- 16 Ma|Wattie Group||Unconformably overlies Killaloc Formation, overlain by Burtawurta Formation||
26213|Wickham Formation|70655|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Birindudu Basin.||Shown as base of Wattie Group.||Unconformably overlies Campbell Springs Dolostone, Blue Hole Formation, Fraynes and Killaloc Formations. Is overlain by Burtawurta Formation.|Massive quartz sandstone, laminated and brecciated chert interbeds.|
26213|Wickham Formation|70848|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Victoria Basin.||Wattie Group.|||Basal conglomerate, pebbly sandstone, chert, quartzite, quartz sandstone, siltstone, medium-thick bedded.|
26213|Wickham Formation|70854|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Unconformably overlies Fraynes Formation (Limbunya Group). Is overlain by Burtawurta Formation.|Quartz sandstone, micaceous siltstone and chert, basal conglomerate.|21-SEP-17
26213|Wickham Formation|70855|5|Briefly described|Map legend.|Mesoproterozoic|Mesoproterozoic|Birrindudu Basin.||Wattie Group.||Unconformably overlies Limbunya Group. Is overlain by Burtawurta Formation.|Quartz sandstone, micaceous siltstone and chert; local basal conglomerate.|
26213|Wickham Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||siltstone, sandstone|
26213|Wickham Formation|71302|5|Briefly described|p6,72,74||Paleoproterozoic|Of Birindudu Basin. Maximum depositional age: 1639+\-16 Ma (Carson, 2013; Munson, 2016 and Munson, in prep).||Unit of Wattie Group.||Overlain by Burtawurta Formation. Underlain by Killaloc Formation.||
26213|Wickham Formation|71592|5|Briefly described|Appendix A.|||Victoria River Region.|1639+/-16 Ma (MDA: Pb/Pb zircon).||||Sandstone.|
26213|Wickham Formation|72718|6|Mentioned|p7|Statherian[?]|Statherian|Birrindudu Basin.|1639 +/- 16 Ma|Wattie Group||Unconformably[?] underlain by Killaloc Formation (Limbunya Group). Overlain by Burtawurta Formation.||
26213|Wickham Formation|73083|6|Mentioned|p30-31|||||Wattie Group||Unconformably underlain by Limbunya Group.||
24573|Wickstead Creek beds|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Calc-silicate rock, Muscovite-biotite schist.||||||
24573|Wickstead Creek beds|9380|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block (division 2). Calc-silicate rock, quartz-rich metasediment, marble, quartzite, epidote rock, quartzofeldspathic gneiss, sillimanite gneiss, hornfels.||||||
24573|Wickstead Creek beds|23270|5|Briefly described|Table 1, p6||Proterozoic|In the of Arunta Block (Division 2).||||||19-DEC-06
24573|Wickstead Creek beds|23271|5|Briefly described|Map legend|Mesoproterozoic|Paleoproterozoic|In the Arunta Block(Division Two). Age: Early or Middle Proterozoic.||||||07-NOV-08
24573|Wickstead Creek beds|24047|6|Mentioned|p105 Appendix 1|||Geological Province: Arunta province.||||||
24573|Wickstead Creek beds|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24573|Wickstead Creek beds|39887|6|Mentioned|Fig.5|||||||||
24573|Wickstead Creek beds|42217|6|Mentioned|p415|||||||||
24573|Wickstead Creek beds|48992|2|Defined|p58|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24573|Wickstead Creek beds|50369|6|Mentioned|p7.3|||||||||
24573|Wickstead Creek beds|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||19-JUN-13
24573|Wickstead Creek beds|69427|5|Briefly described|p12:25, 32|||Stewart et al. (1980). Eastern Yalyirimbi Range, Aileron Province.||Reynolds Range Group.||Is intruded by Napperby Gneiss.|Includes diopside- or tremolite-bearing calc-silicate rock, epidote quartzite, biotite-rich calc-silicate rock and minor metapelitic rock.|12-JUL-16
24573|Wickstead Creek beds|70301|5|Briefly described|v, p1, p22-24|Paleoproterozoic|Paleoproterozoic|Aileron Province, Arunta Region. Detrital zircons indicate a mixed source region with evolved Palaeoproterozoic and Archean crust.|1773 +/- 4 Ma (maximum depositional age).|||Is intruded by Wangala Granite.|Quartzofeldspathic schist with thick, alternating layers of porphyroblastic schist with coarse-grained quartz porphyroblasts in a fine-grained muscovite-feldspar matrix; there are more quartz-rich layers with fewer porphyroblasts and minor biotite.|
24573|Wickstead Creek beds|71858|4|Described|p5-p7, p28, p30, p32, p65|||Aileron Province.||Reynolds Range Group||Unconformably overlies the Lander Rock Formation. Intruded by the Wangala Granite.|Calc-silicate rocks, serpentine-bearing marble and sericitic quartzite.|
27305|Widdallion Sandstone Member|23393|5|Briefly described|p21|Paleoproterozoic|Paleoproterozoic|Of Lawn Hill Formation.||||||07-NOV-08
27305|Widdallion Sandstone Member|23397|5|Briefly described|p476|||||||||
27305|Widdallion Sandstone Member|23964|5|Briefly described|p1269 Table 1|||Of Lawn Hill Formation. Geological Province: Mount Isa Inlier.||||||
27305|Widdallion Sandstone Member|24309|5|Briefly described|p1014|Proterozoic|Proterozoic|Of the Lawn Hill Formation.||||||19-DEC-06
27305|Widdallion Sandstone Member|37459|2|Defined|p433|Mesoproterozoic|Mesoproterozoic|Age is more specifically Carpentarian.||||||19-DEC-06
27305|Widdallion Sandstone Member|38291|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27305|Widdallion Sandstone Member|38310|6|Mentioned|p237|||||||||
27305|Widdallion Sandstone Member|38348|6|Mentioned|p22|||||||||
27305|Widdallion Sandstone Member|39422|5|Briefly described|Map legend|Carpentarian|Carpentarian|Of the Lawn Hill Formation.  Blocky to massive, thick-bedded, micaceous, cross-bedded medium quartz sandstone.||||||10-JAN-05
27305|Widdallion Sandstone Member|39497|4|Described|p14|||||||||
27305|Widdallion Sandstone Member|39797|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
27305|Widdallion Sandstone Member|39925|4|Described|p332|||||||||
27305|Widdallion Sandstone Member|44922|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of Lawn Hill Formation.||||||
27305|Widdallion Sandstone Member|45166|5|Briefly described|p30|||||||||
27305|Widdallion Sandstone Member|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the Lawn Hill Formation. Greyish red to brown, purple weathering, highly lithic and micaceous fine to coarse sandstone; minor glauconite; siltstone and claystone.||||||
27305|Widdallion Sandstone Member|65337|3|Fully described|p9 Fig.5, pp21-22, pp29-30.|Paleoproterozoic|Paleoproterozoic|50 - 370 m of inner shelf - high energy shoreface environment deposits. Forms low banded strike ridges.||Unit in Lawn Hill Formation.||Overlain disconformably, locally unconformably, by Playford Sandstone.|Greyish red to brown, purple-weathering, highly lithic and micaceous fine to coarse sandstone; minor glauconite; siltstone and claystone.|
27305|Widdallion Sandstone Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Camooweal-Murphy and Century Domains, Mount Isa Inlier. Isa Superbasin. Appears as Widdallion Sanstone[sic] in both Time-Space Plots.|1589 +/- 3 Ma.|Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|69433|4|Described|p18:2, 6, 10|Statherian|Statherian|Southern succession, Lawn Hill Platform. 50-370m thick. A distinctive ridge-forming unit. Repeated progradational deposits in a high-energy shoreface environment.||Lawn Hill Formation.||Is overlain by South Nicholson Group disconformably or locally unconformably.|Lithic and micaceous, fine-, medium-, and less commonly coarse-grained sandstone; beds are medium to very thick, arranged in cycles from 5m to 20m thick which become coarser, better sorted, slightly less lithic, and lighter coloured upwards.|12-JUL-16
27305|Widdallion Sandstone Member|69434|6|Mentioned|p19:3|||Parent unit not named.||||Is overlain by Wangalinji Member disconformably (unconformably SW of Mitchiebo Waterhole).||12-JUL-16
27305|Widdallion Sandstone Member|69591|6|Mentioned|p43 Fig.2.31|||Isa Superbasin.||||||
27305|Widdallion Sandstone Member|69673|6|Mentioned|p52 fig 42, p54|||up to 370m thick.||McNamara Group|||Lithic and micaceous sandstone.|
27305|Widdallion Sandstone Member|71369|5|Briefly described|p9|||Lawn Hill Gorge area.||Lawn Hill Formation.||Is overlain unconformably by Hedleys Sandstone.||
27305|Widdallion Sandstone Member|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72415|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|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.|||Reddish-brown, flaggy to blocky, fine- to medium-grained ferruginous, micaceous, feldspathic sandstone; brown to purple siltstone interbeds.|
27305|Widdallion Sandstone Member|72418|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72421|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72422|4|Described|mapsheet|Mesoproterozoic|Paleoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|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 Lawn Hill Formation.|||Reddish-brown, flaggy to blocky, fine to medium-grained ferruginous micaceous, feldspathic sandstone; brown to purple siltstone interbed|
27305|Widdallion Sandstone Member|72527|3|Fully described|p1, p8, p12, p140-146, p193-195|Paleoproterozoic|Paleoproterozoic|South Nicholson Basin. Unit varies in thickness from 50m to 370m. Sampled material is feldspathic sandstone.|1606+/-7 Ma max dep. age|Lawn Hill Formation?, McNamara Group||Overlies Lawn Hill Formation (presumably conformably) and unconformably underlies Wangalinji Member, Playford Formation.|Characterised by friable brown to purple lithic and micaceous fine to coarse-grained sandstone and minor laminated siltstone and claystone. Bedding is medium to very thick (several metres) with abundant pebble lags and gritty lenses.|
27305|Widdallion Sandstone Member|72919|6|Mentioned|p5|Paleoproterozoic|Paleoproterozoic|||Lawn Hill Formation, McNamara Group||Unconformably overlain by Wangalinji Member (Playford Sandstone, Wild Cow Subgroup, South Nicholson Group).||
27305|Widdallion Sandstone Member|73042|6|Mentioned|p4|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin region, Isa Superbasin.||||Underlain(?) by Lawn Hill Formation. Partly overlain by Hedleys Sandstone unconformably.||
27305|Widdallion Sandstone Member|73043|6|Mentioned|p15 Fig.8|Paleoproterozoic|Paleoproterozoic|Not shown what Formation this unit is a member of.||||||
27305|Widdallion Sandstone Member|73144|6|Mentioned|p8|Calymmian|Calymmian|Isa Superbasin. Shown as included in both the Wide and Doom supersequences. Partial aquifer. Potential tight gas/oil.||Lawn Hill Formation, McNamara Group||||14-OCT-22
40576|Wide Supersequence|63112|6|Mentioned|p1191 Fig.2|||Isa Superbasin.|||Includes upper parts of Balbirini Dolostone.|||
40576|Wide Supersequence|63866|6|Mentioned|p53|||Isa Superbasin.||||||
40576|Wide Supersequence|65228|5|Briefly described|pp37-39, Fig.28.|Calymmian|Statherian|Lawn Hill Platform.|1600-1585 Ma.|||Overlies Lawn Supersequence.|Shale, feldspathic sandstone.|
40576|Wide Supersequence|66843|5|Briefly described|p38-39|||Lawn Hill Platform. Depositional cycles and lithofacies detailed.||||||
40576|Wide Supersequence|66844|6|Mentioned|p244|||Lawn Hill and Gunpowder region.||Of McNamara Group.||||
40576|Wide Supersequence|67323|5|Briefly described|GIS attrib tbl, p9, p36|Paleoproterozoic|Paleoproterozoic|See also Mount Isa Block Time-Space Plot. Deposited on the Lawn Hill Platform during the deposition of the upper McNamara Group (~1620-1595 Ma). Or Nathan Group, NT (p9). Camooweal - Murphy Domain, Mount Isa Inlier.||||Overlies Lawn Supersequence. Is overlain by Doom Supersequence.|Grey to black siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite|
40576|Wide Supersequence|68146|6|Mentioned|p4, p203|||Lawn Hill Platform and southern McArthur Basin.||||||
40576|Wide Supersequence|68732|6|Mentioned|p159, p165 Fig.3|||Includes Lawn Hill Formation.||||||
40576|Wide Supersequence|69591|5|Briefly described|p27, p43, p47, p54|||Mount Isa Province. Recognised in the Nathan Group (NT). Consists of the middle part of Lawn Hill Formation. Generally coarsens upwards.||||Overlies Lawn Supersequence. Is overlain by Doom Supersequence. Is equated with upper part of Doomadgee Formation.||
40576|Wide Supersequence|70897|5|Briefly described|p39,40,  Fig.1.7.2-3,7|Mesoproterozoic|Mesoproterozoic|Shows rapid thickness and lithofacies variations across regional fault systems. Age from underlying Lawn Hill Formation tuff.|Max age 1595 +/- 6 Ma (Page and Sweet, 1998).|||||22-SEP-18
40576|Wide Supersequence|72408|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet. Equivalent to the Widdallion Sandstone Member.|||||Grey to brown, siltstone and shale, tuffaceous siltstone and sandstone, feldspathic, micaceous sandstone and siltstone interbeds, minor dolomite.|
40576|Wide Supersequence|72414|4|Described|map sheet|Mesoproterozoic|Paleoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.||||||
40576|Wide Supersequence|72912|5|Briefly described|p17, p33 Fig.12, p34, p35 Fig.13.|||||||||15-MAR-21
40576|Wide Supersequence|73144|4|Described|p8-9, p12-13, p20, p25|Calymmian|Statherian|Sequence Stratigraphy. Isa Superbasin. Contains three third order sequences [see article for more detail on third order sequences]. Deposited via outer shelf turbidites or silty prograding lowstand wedge (Krassay et al., 2000). Oldest measured age 1595 +/- 6 Ma [no further age detail]. Upward coarsening. Lower portion is characterized by dolomitic limestone and siltstone, while the upper portion comprise arkosic sandstone and siltstone. Contemporaneous deposition with the Wide Event, at ~1595 Ma associated with west to north-west transtension.|1585-1600 Ma|||Includes a portion of the Lawn Hill Formation.|Silty shale, dolostone, dark grey carbonaceous siltstone and sandy siltstone, siltstone and lithic sandstone.|
38408|Wiernty Formation|23937|6|Mentioned|p76 App. 1|||Of the Renner Group.   On HELEN SPRINGS sheet.||||||
38408|Wiernty Formation|24047|5|Briefly described|p7 Fig. 6|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Age: 1500? Ma.  Geological Province: Ashburton Province (Tennant Inlier).||||||
38408|Wiernty Formation|24303|2|Defined|p32, p61 Appendix|Calymmian|Calymmian|Of the Renner Group. Overlain by the Jangirulu Formation; overlies the Powell Formation. Max. Thickness: 500m. Previously mapped as undifferentiated Tomkinson Creek beds. Correlates with Corcoran Formation (Roper Group). See also p23 Tb.3, p24 Tb. 4.||||||18-OCT-05
38408|Wiernty Formation|24304|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Renner Group.  Sandstone; lithic to quartz arenite; lensing, very thin to medium bedded, very fine to medium grained; micaceous; mudstone, granule conglomerate; silicified dolomitic mudstone; rip-up clasts; halite pseudomorphs; cauliflower chert.||||||18-OCT-05
38408|Wiernty Formation|24442|5|Briefly described|p15|||Of the Renner Group.  Geological Province: Ashburton Province.||||||
38408|Wiernty Formation|69431|4|Described|p16:15, 18-19, 21-22|Mesoproterozoic|Mesoproterozoic|Hussey et al. (2001). Tomkinson Province. c.400-500m thick; recessive and poorly exposed. Shallow-marine to supratidal, and possibly fluviatile, deposits. Is intruded by locally exposed dolerite sills.||Renner Group.||Gradationally overlies Powell Formation. Is overlain gradationally by Jangirulu Formation, and unconformably by Muckaty Sandstone Member (Helen Springs Volcanics).|Fine to medium micaceous sandstone; minor coarse to very coarse sandstone and granular conglomerate; siltstone, shale and chertified dolostone. Laminated to medium bedded, with nodular chert and locally abundant (intraformational) shale clasts.|12-JUL-16
38408|Wiernty Formation|69673|6|Mentioned|p58|||||Renner Group||||
38408|Wiernty Formation|70968|2|Defined|p94-95, p105-106, p108-111, p114, p126|Ectasian|Ectasian|See also p131, p140. Hussey, Beier, Crispe and Donnellan in Hussey et al. (2001). Originally mapped as undivided Tomkinson Creek beds (Randal et al., 1966). Tomkinson Province. Named after Wiernty Bore. Recessive unit: poor exposures, mainly throughout Ashburton Ranges. The type section is from 362700mE 8010700mN (base) to 361300mE 8011500mN in ELLIOTT 100k sheet. A reference section is also given. Lithology well described and illustrated. 100-500m thick.||Renner Group.||Conformably and transitionally overlies Powell Formation. Is overlain by Jangirulu Formation transitionally to disconformably, and by Muckaty Sandstone Member (Helen Springs Volcanics) unconformably.|Laminated to thinly bedded, fine- to medium-grained sandstone and mudrock, minor coarse- to very coarse-grained sandstone and granular conglomerate, minor dolomitic mudrock and minor chertified dolostone.|
38408|Wiernty Formation|71893|5|Briefly described|p6, p8, p60-p61, p64|||Tomkinson province.||Renner Group||Conformably overlain by the Jangirulu Formation. Conformably overlies the Powell Formation.||
37739|Wild Cow Subgroup|24442|5|Briefly described|p23 Fig. 2|Mesoproterozoic|Mesoproterozoic|Of the South Nicholson Group.  ||||||
37739|Wild Cow Subgroup|62657|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the South Nicholson Group.||||||
37739|Wild Cow Subgroup|62659|5|Briefly described|Map Legend|Calymmian|Calymmian|Of the South Nicholson Group.||||||
37739|Wild Cow Subgroup|64443|6|Mentioned|p3|Calymmian|Calymmian||||Includes Crow Formation.|Underlies Accident Subgroup.||14-MAY-14
37739|Wild Cow Subgroup|65337|4|Described|p v, pp37-50. |Mesoproterozoic|Mesoproterozoic|Comprises all of South Nicholson Group below a disconformity, locally unconformity, within that Group.||Unit in South Nicholson Group.|Includes Bowgan and Playford Sandstones and Crow Formation.|Is overlain by Accident Subgroup.|Fine-grained shelf tempestites and shales, and coarse-grained fluvial and shallow-marine siliciclastic rocks.|
37739|Wild Cow Subgroup|67352|6|Mentioned|p12|Calymmian|Calymmian|||South Nicholson Group|Crow Formation|Overlain by Accident Subgroup.||
37739|Wild Cow Subgroup|68146|5|Briefly described|p21, p28-29, p35, p196|||||South Nicholson Group.|Hedleys, Burangoo, Constance Sandstones; Pandanus, Wallis Siltstones.|Is overlain unconformably by Accident Subgroup.||
37739|Wild Cow Subgroup|68575|5|Briefly described|p19|||South Nicholson Basin.||South Nicholson Group.|Burangoo Sandstone; Wallis, Pandanus Formations.|Is overlain unconformably by Constance Sandstone.||
37739|Wild Cow Subgroup|69434|4|Described|p19:2-6|Mesoproterozoic|Mesoproterozoic|W and SW South Nicholson Basin. Rocks assigned to this Subgroup by Rawlings et al. (2008) were originally mapped by Smith and Roberts (1963) as younger units of the South Nicholson Group (now the Accident Subgroup).||South Nicholson Group.|Crow Formation; Bowgan, Playford Sandstones.|Unconformably overlies Murphy Metamorphics and McNamara Group (and probably Benmara Group). Is overlain by Accident Subgroup disconformably (locally unconformably).||12-JUL-16
37739|Wild Cow Subgroup|69591|5|Briefly described|p52|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin (Qld and NT). 450m thick in the north, thinning to <200m in the south.||South Nicholson Group.|Hedley, Burangoo, Constance Sandstones; Pandanus, Wallis Formations.|Is overlain by Accident Subgroup.||
37739|Wild Cow Subgroup|69673|4|Described|p56|||||South Nicholson Group|Includes Playford Bowgan Sandstone, Playford Sandstone, Crow Formation|Overlain disconformably by the Accident Subgroup||
37739|Wild Cow Subgroup|70968|5|Briefly described|p131 Fig.118, p132|Calymmian|Calymmian|||South Nicholson Group.|Crow Formation, Playford Sandstone.|Is overlain unconformably by Accident Subgroup.||
37739|Wild Cow Subgroup|71369|5|Briefly described|p1, p5-6, p8, p23-24, p48|||Rawlings et al. (2008), who recognised an unconformity with the overlying Constance Sandstone. Note that Fig. 2e on p6 erroneously includes Constance Sandstone in this Subgroup. South Nicholson Basin. 200-450m thick.||South Nicholson Group.|Hedleys, Burangoo Sandstones; Pandanus, Wallis Formations.|Is overlain unconformably by Elizabeth Sandstone (Accident Subgroup).||
37739|Wild Cow Subgroup|72408|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Basement Geology 1: 100 000 map sheet.|||Includes Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone.|||
37739|Wild Cow Subgroup|72414|4|Described|map sheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of Musselbrook Sheet 6560 Surface Geology 1: 100 000 map sheet.|||Includes Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone.|Overlain by Accident Subgroup.||
37739|Wild Cow Subgroup|72415|4|Described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. Of MUSSELBROOK Sheet 6560 Surface Geology 1: 100 000 compilation.|||Includes Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone.|Overlain by Accident Subgroup.||
37739|Wild Cow Subgroup|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 Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone.|||
37739|Wild Cow Subgroup|72418|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|Of South Nicholson Basin. See BOWTHORN sheet 6561 Basement Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Burangoo Sandstone, Pandanus Formation, Wallis Formation, Hedleys Sandstone.|||10-DEC-19
37739|Wild Cow Subgroup|72421|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 map sheet.||Unit of South Nicholson Group.|Includes Burangoo Sandstone, Pandanus Formation, Wallis Formation, Hedleys Sandstone.|||10-DEC-19
37739|Wild Cow Subgroup|72422|5|Briefly described|mapsheet|Mesoproterozoic|Mesoproterozoic|See BOWTHORN sheet 6561 Surface Geology 1:100 000 Geological Compilation Series.||Unit of South Nicholson Group.|Includes Burangoo Sandstone, Pandanus Formation, Wallis Formation.|||
37739|Wild Cow Subgroup|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.||Unit of South Nicholson Group.|Includes Burangoo Sandstone, Pandanus Formation, Wallis Formation.|||
37739|Wild Cow Subgroup|72526|5|Briefly described|p4, p33, p34, p40, p46, p86|||See also Wildcow Subgroup p8. Included a revised Constance Sandstone in Sweet (2017), but this unit placed in overlying Accident Subgroup by Carr et al. (2019).|||Includes Bowgan Sandstone, Crow Formation|Unconformably overlain by Constance Sandstone.||
37739|Wild Cow Subgroup|72527|4|Described|p3, p41, p49, p63, p71, p195.|Mesoproterozoic|Mesoproterozoic|South Nicholson Basin. Most components of this Subgroup have now been dated, giving a maximum deposotopnal age range for the Subgroup from Wangalinji Member 1600+/-20 Ma at the base to Crow Formation 1483+/-12 Ma near the top of the Subgroup. Misspelt as 'Wildcow Subgroup p12,20, Wild Cow Sub-group p56, 'Wild Cow subgroup' on p193 Fig.9.1.|c. 1600 -1483 Ma max. dep. age range|South Nicholson Group|Playford Sandstone, Tobacco Member, Crow Formation, and Bowgan Sandstone.|Unconformably underlies Accident Subgroup and partially equivalent to Playford Sandstone.||
37739|Wild Cow Subgroup|72912|5|Briefly described|p21, 23, 24.|Mesoproterozoic|Mesoproterozoic|See also Wildcow Subgroup in Figs p5, 33||South Nicholson Group|Includes Crow Formation, Playford Sandstone.|Overlain by Accident Subgroup.||
37739|Wild Cow Subgroup|72919|6|Mentioned|p5, p24, p85|Mesoproterozoic|Mesoproterozoic|Includes Constance Sandstone in QLD but not in NT.||South Nicholson Group|Crow Formation, Bowgan Sandstone, Playford Sandstone, Constance Sandstone, Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone|Unconformably underlain by Widdallion Sandstone Member (McNamara Group). Overlain by Mittiebah Sandstone and Constance Sandstone, including Hedleys Sandstone Member (Accident Subgroup).||
37739|Wild Cow Subgroup|73083|6|Mentioned|p35|||||South Nicholson Group||||
37739|Wild Cow Subgroup|73144|6|Mentioned|p8, p13|Calymmian|Calymmian|South Nicholson Basin. Leaky aquitard.||South Nicholson Group|Wallis Formation, Burangoo Sandstone, Pandanus Formation, Hedleys Sandstone|Unconformably overlain by Schultz Sandstone Member (Constance Sandstone, Accident Subgroup).||
24105|Wildman Siltstone|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Intruded by Zamu Dolerite.||||||07-NOV-08
24105|Wildman Siltstone|9691|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Siltstone, red and cream banded siltstone, feldspathic sandstone, arkose; minor quartzite and quartz greywacke.||||||
24105|Wildman Siltstone|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Siltstone, red and cream banded siltstone, feldspathic sandstone, arkose; minor quartzite and quartz greywacke.||||||02-JUN-05
24105|Wildman Siltstone|22810|4|Described|Table2 P4, P13|||Maximum thickness of 2000m. Overlies Mundogie Sandstone; overlain by Koolpin and Kapalga Formations.||||||19-DEC-06
24105|Wildman Siltstone|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Overlies the Whites Formation. Of the Mount Partridge Group. Colour banded siltstone.||||||07-NOV-08
24105|Wildman Siltstone|23337|5|Briefly described|906|||||||||
24105|Wildman Siltstone|23714|4|Described|p10|Proterozoic|Proterozoic|See also page 8 Table 1, page 12. Max. thickness: 750 m.||||||
24105|Wildman Siltstone|23715|5|Briefly described|Map legend||Proterozoic|Of the Mount Partridge Group, in the Rum Jungle and Central Regions.||||||14-APR-08
24105|Wildman Siltstone|23733|5|Briefly described|p32 Fig. 19|||Of Mount Partridge Group.||||||
24105|Wildman Siltstone|23999|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Consists of folded, cleaved and indusrated, steepldipping laminated siltstone, shale, sandy siltstone and quartz sandstone. Outcrops on flanks of ridges of Acacia Gap Quartzite.||||||07-FEB-11
24105|Wildman Siltstone|24001|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Siltstone and shale, colour-banded and pyritic at depth.||||||
24105|Wildman Siltstone|24047|5|Briefly described|p5 Fig.4, p21|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group.  Siltstone, greywacke.  Geological Province: Pine Creek Orogen.  See also p30 Fig. 23.||||||07-NOV-08
24105|Wildman Siltstone|24181|4|Described|p102|Paleoproterozoic|Paleoproterozoic|Siltstone, black carbonaceous laminated shale and minor sandstone. Conformably overlies Mundogie Sandstone. Of Mount Partridge Group. Geological Province: Pine Creek Inlier.||||||07-NOV-08
24105|Wildman Siltstone|24260|5|Briefly described|p1014 Fig.2|||Overlain by Koolpin Formation. Geological Province: Pine Creek Inlier.||||||19-DEC-06
24105|Wildman Siltstone|24442|6|Mentioned|p30|||On NOONAMAH sheet.||||||
24105|Wildman Siltstone|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|37462|6|Mentioned|Fig.4.8|||||||||
24105|Wildman Siltstone|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Siltstone, carbonaceous and pyritic at depth in places, red and cream laminated siltstone; minor quartzite, arkose and quartz greywacke, phyllite and schist in Mount partridge range.||||||07-NOV-08
24105|Wildman Siltstone|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|38239|6|Mentioned|Fig.2|||||||||
24105|Wildman Siltstone|38349|4|Described|p13|||||||||
24105|Wildman Siltstone|38351|6|Mentioned|Table 5|||||||||
24105|Wildman Siltstone|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|39068|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Siltstone, in places colour banded; silty sandstone (quartz arenite, sublitharenite) with minor colour banding, minor quartzite; metamorphosed to lower greenschist facies.||||||14-FEB-06
24105|Wildman Siltstone|39069|4|Described|p6|||See also Table 1.||||||
24105|Wildman Siltstone|39357|4|Described|p9|||||||||
24105|Wildman Siltstone|39518|3|Fully described|p4|||||||||
24105|Wildman Siltstone|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Shale and argillite, commonly colour-banded.||||||07-NOV-08
24105|Wildman Siltstone|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Siltstone, phyllite, carbonaceous phyllite and minor laminated fine to coarse quartz sandstone, dolarenite and spotted micaceous hornfels.||||||07-NOV-08
24105|Wildman Siltstone|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Siltstone, phyllite, slate, shale, sandstone, quartzite, dolarenite, claystone, ironstone, hornfels.||||||07-NOV-08
24105|Wildman Siltstone|40243|6|Mentioned|Fig.2|||||||||
24105|Wildman Siltstone|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|40493|4|Described|p12|||||||||
24105|Wildman Siltstone|40495|6|Mentioned|Fig.5|||||||||
24105|Wildman Siltstone|40808|3|Fully described|p12|||||||||
24105|Wildman Siltstone|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24105|Wildman Siltstone|41125|6|Mentioned|Fig.14|||||||||
24105|Wildman Siltstone|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24105|Wildman Siltstone|41305|3|Fully described|p15|||||||||
24105|Wildman Siltstone|41309|4|Described|p4|||||||||
24105|Wildman Siltstone|41311|4|Described|p9|||||||||
24105|Wildman Siltstone|41397|6|Mentioned|p7|||||||||
24105|Wildman Siltstone|41663|6|Mentioned|Fig.1|||||||||
24105|Wildman Siltstone|41874|5|Briefly described|Fig.8|||||||||
24105|Wildman Siltstone|42012|6|Mentioned|p11|||||||||
24105|Wildman Siltstone|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
24105|Wildman Siltstone|42202|6|Mentioned|Fig.1 P511|||||||||
24105|Wildman Siltstone|42372|5|Briefly described|p17|||||||||
24105|Wildman Siltstone|43140|4|Described|p2||Paleoproterozoic|Of the Mount Partridge Group.||||||07-NOV-08
24105|Wildman Siltstone|43187|5|Briefly described|p2|||||||||
24105|Wildman Siltstone|43624|5|Briefly described|p8|||Of Mount Partidge Group.||||||
24105|Wildman Siltstone|43832|3|Fully described|13,15,97||Paleoproterozoic|Refers to Stuart-Smith et al. (1985) for subdivision into 2 members.  Minimum age: 1890 Ma.||||||07-NOV-08
24105|Wildman Siltstone|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Underlain by Mundogie Sandstone. Siltstone, red and cream banded siltstone (carbonaceous at depth); minor quartzite and greywacke.||||||07-NOV-08
24105|Wildman Siltstone|46658|6|Mentioned|p550|||||||||
24105|Wildman Siltstone|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Contains the Mount Deane Volcanic Member and the Acacia Gap Quartzite Member. Shale and argillite, commonly colour banded. Conformably overlies Whites Formation.||||||07-NOV-08
24105|Wildman Siltstone|46700|5|Briefly described|P14, Table1 P10||Proterozoic|||||||
24105|Wildman Siltstone|47049|6|Mentioned|Fig.2|||||||||
24105|Wildman Siltstone|50586|6|Mentioned|p4.5, 6.1|||Intruded by Cullen Supersuite. Of the Gerowie Suite. Geological Province: Pine Creek Inlier.||||||
24105|Wildman Siltstone|50623|5|Briefly described|p260 Fig.3, p261|Paleoproterozoic|Paleoproterozoic|Conformably overlies Whites Formation. Of Mount Partridge Group.||||||07-NOV-08
24105|Wildman Siltstone|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Laminated colour banded shale, siltstone and sandstone, dolomite and quartzite. Deeply weathered ferruginous volcanics also occurs in this unit. Overlies Mundogie Sandstone. Underlies Koolpin Formation.||||||19-DEC-06
24105|Wildman Siltstone|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of the Mount Partridge Group. Siltstone, red and cream banded siltstone, minor quartzite and quartz greywacke.||||||
24105|Wildman Siltstone|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Mount Partridge Group. Contains the Mount Dean Volcanic Member and the Acacia Gap Quartzite Member.||||||14-APR-08
24105|Wildman Siltstone|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Shale and argillite, commonly colour banded. Overlies Whites Formation. Overlain by Koolpin Formation. Of Mount Partidge Group.||||||
24105|Wildman Siltstone|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Mount Partridge Group. Age: 2026Ma. Geological Province: Pine Creek Orogen. Banded silty carbonaceous phyllite (metasiltstone), interbedded with sandy ferruginous metasiltstone.||||||14-JAN-05
24105|Wildman Siltstone|61389|5|Briefly described|Map Legend|||Of the Mount Partridge Group. Shale and argillite, commonly colour banded.||||||
24105|Wildman Siltstone|62378|5|Briefly described|p5, 12, 14|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Orogen. Age: 2029 +/- 12Ma, 2025 +8/-5Ma. Volcaniclastic siltstone. Of the Mount Partridge Group. Unconformably overlies: Rum Jungle Complex. Unconformably overlain by the South Alligator Group.||||||07-NOV-08
24105|Wildman Siltstone|63866|4|Described|p109-p110|Orosirian|Orosirian|Central Domain, Pine Creek Orogen. Hornfelsed where it contacts the Mount Bundey Granite.|2019 +/- 4 Ma (crystallisation age)|Mount Partridge Group||Intruded by the Mount Bundey Granite.|Tuffaceous siltstone.|
24105|Wildman Siltstone|64662|6|Mentioned|p44|||Contains the Acacia Gap Quartzite Member. Of Pine Creek Orogen.||||||07-FEB-11
24105|Wildman Siltstone|64676|6|Mentioned|v, p19|||||Mount Partridge Group.|Acacia Gap Quartzite Member.|||
24105|Wildman Siltstone|64677|6|Mentioned|v,|||Pine Creek Orogen.|c.2024 Ma.|||||
24105|Wildman Siltstone|64698|4|Described|lithinterp table|Orosirian||Of Mount Partridge Group. Age 2026Ma SHRIMP U/Pb. Max thick 2000m. Colour-banded silty carbonaceous phyllite (metasiltstone), interbedded with sandy ferruginous metasiltstone,  feldspathic quartz meta-arenite, quartzite, lithofeldpspathic metagreywacke.||||||07-JAN-09
24105|Wildman Siltstone|64730|5|Briefly described|p125, Fig. 3, p126, 127, 128-129,131-134|Paleoproterozoic|Paleoproterozoic|Age is of deposition of tuffaceous siltstone. Tentatively correlated with Nourlangie Schist (Needham 1988).|2019+/-4 Ma SHRIMP U/Pb.|Of Mount Partridge Group.|||Terrigenous sandstones, mudstones, interbedded volcanics and volcanogenic sediments.|02-MAY-12
24105|Wildman Siltstone|64956|4|Described|p2 Tb. 14, p72-73|Paleoproterozoic|Paleoproterozoic|Of the Mount Partridge Group. Cryst. Age: 2019+/-4Ma. Geological province: Pine Creek Orogen. Sample is tuffaceous siltstone.||||||07-FEB-11
24105|Wildman Siltstone|65232|5|Briefly described|p45, 51, p7, p6 Fig. 5, App. 2|Orosirian|Orosirian|Of the upper Mount Partridge Group. Includes Acacia Gap Quartzite Member and Mount Deane Member. With Mundogie Sandstone, unconformably overlies Namoona Group. Siltstone, greywacke. Age: 2025Ma SHRIMP U-Pb zircon dating of tuffaceous beds.||||||09-FEB-10
24105|Wildman Siltstone|65339|4|Described|p6 Table 1, pp10-11, p16, p18.|||Thickness irregular to about 1500 m. Vermiform, platy cemented ferricrete hardpans occur near Townend Road. Stratiform pyrrhotite horizons produce curvilinear zones of high magnetic intensity.|c.2025 Ma (Worden et al. 2004).|Unit in Mount Partridge Group.|Includes Acacia Gap Quartzite Member and Mount Deane and Yarrawonga Volcanic Members.|Overlies Whites Formation, Mundogie Sandstone and Koolpinyah Dolostone.|Grey and purple, finely laminated siltstone and shale, commonly containing sandstone and quartzite beds; commonly pyritic. Vein quartz and quartz boudins commonly occur parallel to bedding.|
24105|Wildman Siltstone|66882|5|Briefly described|p116, p117|Orosirian|Orosirian|Pine Creek Orogen. Possible source rock for c.2000 Ma zircons in Cleve Group.|2000 Ma||||Tuffaceous.|
24105|Wildman Siltstone|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|||Unit in Mount Partridge Group.|Includes Acacia Gap Quartzite Member.|Overlies White's Formation.|Laminated, red-brown and cream banded, silty carbonaceous phyllite, interbedded with sandy ferruginous metasiltstone, thinly-bedded feldspathic quartz metasandstone, quartzite, lithofeldspathic metagreywacke; minor crenulated quartz-sericite schist.|23-NOV-11
24105|Wildman Siltstone|67232|5|Briefly described|p4. |||Central Domain, Pine Creek Orogen.|Max. deposition 2020 Ma (Worden et al. 2008a,b).|Unit in Mount Partridge Group.||||
24105|Wildman Siltstone|67355|4|Described|p4, p7, p10-12, p39-40, p46, p68||Orosirian|Depositional environment considered subtidal marine. Thickness probably reaches a maximum of 1500 m. Includes intermediate to acid volcanic interbeds up to 200 m thick. Age from (Carson et al.2005).|2025 +8/-5 Ma (SHRIMP U-Pb zircon, tuff bed)|Mount Partridge Group|Acacia Gap Quartzite Member, Mount Deane Volcanic Member.|Conformably overlies and interfingers with the Whites Formation, underlies the South Alligator Group (Koolpin Formation).|Carbonaceous argillite - laminated argillite and shale, and has a distinctive colour-banded appearance in outcrop, with red-brown, green-grey, black and pale grey layers. Scattered pyrite cubes are locally present.|25-JAN-17
24105|Wildman Siltstone|67564|3|Fully described|p8 Table 2, p9 Fig.4, p13, p15, pp17-19.|Paleoproterozoic|Paleoproterozoic|Previously mapped as Masson Formation or Mount Partridge Formation by Walpole (1963). 2000 m of shallow marine (prodelta or mid-shelf) deposits; correlated with Nourlangie Schist. Hosts Au-Pt-Pd at Gold Ridge, western PINE CREEK.|2025 +8/-5 Ma (SHRIMP U-Pb: Worden et al. 2004).|Unit in Mount Partridge Group.||Conformably overlies Mundogie Sandstone. Is conformably overlain by Koolpin Formation.|Tightly folded, laminated colour-banded silty carbonaceous phyllite (metasiltstone) interbedded with hematitic metasiltstone, thinly bedded feldspathic quartz meta-arenite, quartzite and lithofeldspathic metagreywacke.|
24105|Wildman Siltstone|67779|5|Briefly described|p6 Fig.5, p20, p104.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Previous interpretation (Needham and Stuart-Smith, 1985) that the Nourlangie Schist is a metamorphosed equivalent of this unit are shown to be erroneous by recent detrital zircon analyses.|2019 +/- 4 Ma (Worden et al. 2008a,b).|Topmost unit in Mount Partridge Group.|Includes Acacia Gap Quartzite Member.|Overlies Mundogie Sandstone, Whites Formation and Koolpinyah Dolostone.||
24105|Wildman Siltstone|69383|5|Briefly described|p72||Orosirian|Includes tuff dated at 2019+/-4 Ma (Worden et al 2004, 2008)||||||
24105|Wildman Siltstone|69418|6|Mentioned|p3:7, 21, 25|||Pine Creek Orogen. Hosts gold deposits (described). Hosts the Billycan, Jessops and Mount Masson Sn vein deposits (briefly described). A roof pendant of this Formation within the Mount Goyder Syenite contains the Mount Bundey skarn-type iron ore deposit: tabular lenses of magnetite.||||||12-JUL-16
24105|Wildman Siltstone|69419|5|Briefly described|p4:5,|Orosirian|Orosirian|SHRIMP U-Pb zircon age from tuffaceous rocks.|2019 +/- 4 Ma (Worden et al., 2008).|Mount Partridge Group.|||Includes tuffaceous rocks.|12-JUL-16
24105|Wildman Siltstone|69420|4|Described|p5:1, 4, 6, 8-10, 12, 37, 45, 54, 60, 67|Paleoproterozoic|Paleoproterozoic|See also 79, 90, 94, 100, 110-112, 117. Central and South Alligator regions, Central Domain, Pine Creek Orogen. Up to 2000m thick. Shallow-marine deposits: prodelta or mid-shelf. Hosts the Toms Gully Au deposit (described in some detail); associated with the Gold Ridge Au deposit and the McCarthys Ag-Pb mine. Also hosts a number of Sn deposits and numerous iron ore deposits (listed). SHRIMP U-Pb zircon (tuff) depositional age.|2019 +/- 4 Ma.|Mount Partridge Group.|Acacia Gap Quartzite Member; Mount Dean, Yarrawonga, Volcanic Members.|Conformably overlies Mundogie Sandstone. Lateral equivalent of, and overlies, Whites Formation and Koolpinyah Dolostone.|A succession of laminated, red-brown and cream, carbonaceous shale, haematitic siltstone, quartz sandstone, quartzite, greywacke.|12-JUL-16
24105|Wildman Siltstone|69456|5|Briefly described|p40:6|Proterozoic|Proterozoic|Pine Creek Orogen.||||Is overlain unconformably by Darwin Formation.||12-JUL-16
24105|Wildman Siltstone|69917|6|Mentioned|p43||||||Includes Acacia Gap Quartzite Member.|||
24105|Wildman Siltstone|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|2019 +/- 4 Ma.|Mount Partridge Group.|Includes Mount Deane Volcanic Member, Acacia Gap Quartzite Member.|Conformably overlies Whites Formation and Mundogie Sandstone. Is overlain unconformably by Koolpin Formation (South Alligator Group).|Laminated red-brown and cream banded, silty carbonaceous phyllite interbedded with sandy ferruginous metasiltstone, thinly-bedded feldspathic quartz metasandstone, quartzite and lithofeldspathic metagreywacke; minor crenulated quartz-sericite schist.|28-FEB-18
24105|Wildman Siltstone|71341|6|Mentioned|p198|||Pine Creek Orogen. ||||||
24105|Wildman Siltstone|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2019+/-4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Green-grey fine-bedded tuffaceous siltstone.|
24105|Wildman Siltstone|73083|6|Mentioned|p5-6|||Rocks that compose a dome structure in the Alligator River 1:250K Sheet (SW) that were previously thought to be of this unit were reassigned to the Masson Formation. A ridge of what was previously attributed to the Mundogie Sandstone in the Alligator River 1:250K Sheet (SW) was reassigned to this unit.|||||Siltstone, minor quartzite, and greywacke.|
38415|Willieray Formation|24047|5|Briefly described|p7 Fig. 6|Paleoproterozoic|Paleoproterozoic|Of the Namerinni Group.  Age: 1640Ma.  Geological Province: Ashburton Province (Tennant Inlier).  See also p57 Fig. 49.||||||07-NOV-08
38415|Willieray Formation|24303|2|Defined|p22, p59 Appendix|Statherian|Statherian|Of the Namerinni Group. Unconformably overlain by the Gleeson Formation; overlies the Shillinglaw Formation. Max. Thickness: >400m. Previously mapped as undifferentiated Tomkinson Creek beds (Randal et al 1966, Randal and  Brown 1969)||||||25-JAN-10
38415|Willieray Formation|24304|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Namerinni Group. Sandstone; thin to medium bedded; rippled; mudstone, rip-up clasts, ripple cross laminated, current lineated, dessicated, halite pseudomorphs; conglomerate, crossbedded, graded; basal dolomitic sandstone; flaggy, strike ridges.||||||07-NOV-08
38415|Willieray Formation|24442|5|Briefly described|p14|||Of the Namerinni Group.Geological Province: Ashburton Province.||||||
38415|Willieray Formation|64780|6|Mentioned|p63 Fig.4, |Palaeoproterozoic|Palaeoproterozoic|||Of the Namerinni Group||||
38415|Willieray Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|~1639 Ma.|Namerinni Group.||||
38415|Willieray Formation|69431|4|Described|p16:14-18, 23|Statherian|Statherian|Tomkinson Province. c.70m to over 400m thick. Transgressive, intertidal to supratidal deposits.||Topmost Namerinni Group.||Conformably and transitionally overlies Shillinglaw Formation. Is overlain unconformably by Gleeson Formation (Renner Group).|Thinly to medium bedded sublithic and quartz sandstone and siltstone; minor pebbly sandstone, conglomerate and mudstone; minor quartzose dolostone and dolostone. Many sedimentary structures (listed).|12-JUL-16
38415|Willieray Formation|69673|6|Mentioned|p58|||||Namerinni Group||||
38415|Willieray Formation|72373|5|Briefly described|p39|Paleoproterozoic|Paleoproterozoic|Geological province: Tomkinson Province.||Unit of Namerinni Group.||Underlain conformably by Shillinglaw Formation.||
38834|Wilson Formation|60681|5|Briefly described|Map legend|Orosirian|Orosirian|Of the Ware Group. Sandstone, siltstone.||||||09-MAR-10
38834|Wilson Formation|62377|5|Briefly described|p19|Paleoproterozoic|Paleoproterozoic|Of the Ware Group. Greywacke and conglomerate. Age: 1800 +/- 31 and 1791 +/- 66Ma.||||||07-NOV-08
38834|Wilson Formation|62628|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of the Ware Group. Geological Province: Tanami Inlier. Greywacke, quartzwacke, granule conglomerate, phyllitic siltstone, schist.||||||07-NOV-08
38834|Wilson Formation|63261|3|Fully described|p13|Paleoproterozoic|Paleoproterozoic|Of Ware Gp. Prev'ly mapped with Nanny Goat Creek beds.Total thickness:1000m.Max.dep.age:1802+/-8Ma (Smith 2001). Assoc'n of greywacke, qtz wacke + siltst.; also, granular conglom.,qtz wacke+minor siltst. locally metamorph'd to phyllite + fine-gr. schist.||||||07-FEB-11
38834|Wilson Formation|64662|5|Briefly described|p29 Fig. 2, p30 Fig. 3, p38-39, 43|Orosirian|Orosirian|Of the Ware Group. Detrital zircons in greywacke give maximum deposition age: ca.1831+/-7Ma. Contains tightly folded, thick-bedded, graded, granular conglomerate and greywacke. Geological Province: Tanami region||||||07-FEB-11
38834|Wilson Formation|64725|5|Briefly described|p63 Fig.7.|Paleoproterozoic|Paleoproterozoic|Granites-Tanami Orogen.|c.1815 Ma.|Unit in Ware Group.||||
38834|Wilson Formation|64733|6|Mentioned|p170 Fig.2|Orosirian|Orosirian|Presented as Wilson and Century Formation.|~1815 Ma.|Of Ware Group.||||20-APR-12
38834|Wilson Formation|64734|6|Mentioned|p186 Fig.1|Orosirian||Ca. 1815 Ma. Presented as Wilson and Century Formation. Of Ware Group.||||||14-SEP-09
38834|Wilson Formation|65359|6|Mentioned|p1|||Tanami region. In Ware Group.||||||
38834|Wilson Formation|66129|6|Mentioned|p214 Fig.1|Orosirian|Orosirian|1815 Ma. Unit in Ware Group.||||||
38834|Wilson Formation|67824|6|Mentioned|p385 Fig.2|Orosirian|Orosirian||~ 1815 Ma |Unit in Ware Group.||||
38834|Wilson Formation|67826|6|Mentioned|p401 Fig.2|Orosirian|Orosirian||~ 1815 Ma|Of the Ware Group.||||
38834|Wilson Formation|68474|6|Mentioned|p572|Palaeoproterozoic|Palaeoproterozoic|Granites-Tanami Orogen.|ca. 1815 ma|Ware Group||||
38834|Wilson Formation|69426|4|Described|p11:3-5, 7-8, 11, 13-14|||Includes parts of the sedimentary units previously assigned to Nanny Goat Creek Beds and Killi Killi Beds by Blake et al. (1975). Deeper marine sediments. c.1000m thick. Commonly weathered to pink or buff colour, capped by ferricrete, and locally metamorphosed to phyllite and fine-grained schist. Is separated from Century Formation by the Pargee Fault. Detrital zircons maximum depositional age.|<1815 +/- 13 Ma (Claoue-Long et al., 2001).|Ware Group.|||Interbedded, laterally continuous graded greywacke, quartz wacke, minor siltstone and granular sandstone containing a high proportion of angular volcanic quartz grains and felsic volcanic lithic grains.|12-JUL-16
38834|Wilson Formation|69618|5|Briefly described|p106-107|Paleoproterozoic|Paleoproterozoic|||Unit in Ware Group.||Is intruded by Twin Bonanza Porphyry.|Includes sandy turbiditic sandstone and shale.|
38834|Wilson Formation|70291|4|Described|p178,180|Orosirian|Orosirian|Geological province: Tanami.|ca. 1815-1802 Ma|Unit of Ware Group.|||Graywacke, quartz wacke and siltstone.|
38834|Wilson Formation|70478|6|Mentioned|p2 Fig 1|||Geological Province: Tanami. ||Unit of Ware Group||||
38834|Wilson Formation|70852|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tanami Region.||Ware Group.|||Lithic greywacke, quartz greywacke, granule sandstone; locally metamorphosed to phyllitic siltstone, fine-grained schist.|
38834|Wilson Formation|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||conglomerate, greywacke|
38834|Wilson Formation|71592|5|Briefly described|Appendix A.|||Tanami Orogen.|1831+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Graded, thick-bedded, granular conglomerate and greywacke.|
38834|Wilson Formation|73089|6|Mentioned|p8|||Possibly a deeper water depositional setting.||Ware Group||||
81655|Wilton package|72373|5|Briefly described|p1-2|Mesoproterozoic|Mesoproterozoic|Of McArthur Basin. Informal nomenclature of Rawlings et al (1997) and Rawlings (1999). A basin-wide non-genetic depositional pacakge within the McArthur Basin.||||Underlain by Favenc package.||
81655|Wilton package|72381|5|Briefly described|p772-773|Mesoproterozoic|Mesoproterozoic|Includes Roper Group, McArthur Basin; Renner Group Tomkinson Province and Tijunna Group, Birrindudu Basin. .Mainly contains shallow-water siliciclastic sedimentary rocks (Abbott and Sweet 2000; Ahmad and Munson 2013; Munson 2016; Munson and Revie 2018); regionally widespread, covering an area >145000km2.||||||04-OCT-19
81655|Wilton package|72718|5|Briefly described|p5, p7, p9, p10-14, p18, 20|Ectasian|Calymmian|Laterally extensive. Roper Group in McArthur Basin. Rocks of the Wilton package have been identified in all 26 wells drilled across the Beetaloo Sub-basin and, based on the current interpretation, reach stratigraphic thicknesses of up to 3700 m in the OT Downs depocentre in the east. Maximum age constrained by 1589+/-3 Ma age of tuff in underlying Nathan Group, and minimum age constrained by ca 1313 Ma age of intrusive Derim Derim Dolerite.|ca 1590 - 1313 Ma|||Intruded by Derim Derim Dolerite.|Alternating successions of sandstone and mudrocks. Lithologies are predominantly marine mudrocks alternating with shoreline sandstone, but minor calcareous mudstone, fluvial sandstone and conglomerate have also been observed.|
81655|Wilton package|72912|6|Mentioned|p5, 18.|Mesoproterozoic|Mesoproterozoic|Of Rawlings, 1999.||||Overlies Favenc package.||
72416|Windajong Granite|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Biotite-muscovite granite, equigranular/seriate porphyritic. Geological Province: Arunta Region - Aileron Province.||||||07-NOV-08
72416|Windajong Granite|65338|3|Fully described|App 1 p83  p iv, p22, pp34-35.|Statherian|Statherian|Newly defined. Coeval with Strangways Event. Discrete, subcircular gravity low with little or no magnetic character. Weakly foliated to massive in outcrop; deformational microstructures. Associated with Devils Suite granites.|1730 +/- 3 Ma (Cross et al. 2005).|||Intrudes Lander Rock Formation.|Biotite-muscovite granite; equigranular/seriate porphyritic; rutilated quartz.|
72416|Windajong Granite|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-muscovite granite, equigranular/seriate porphyritic.|
72416|Windajong Granite|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.|||||Biotite-muscovite granite, equigranular/seriate porphyritic.|
72416|Windajong Granite|69417|6|Mentioned|p2:5|Statherian|Statherian|Aileron Province.||||||12-JUL-16
72416|Windajong Granite|69427|5|Briefly described|p12:3, 40 Fig.12.34; 12:41|Statherian|Statherian|Northern Aileron Province. Interpreted to be associated with the Devils Suite granites (Davenport Province).|1730 +/- 3 Ma (Cross et al., 2005).||||Even-grained to porphyritic, undeformed to weakly foliated biotite-muscovite granite. Coincides with a subcircular, non-magnetic gravity low.|12-JUL-16
72416|Windajong Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1731+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
30320|Windoo Sandstone|23621|2|Defined|p57 Appendix|Late Cambrian|Late Cambrian|Replaces parts of Gardiner beds.  See also page 36, 9 table 1. Type section included. Underlying unit Antrim Plateau Volcanics. Max. thickness 50 m.||||||06-DEC-06
30320|Windoo Sandstone|23622|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Ord Basin.||||||
30320|Windoo Sandstone|43302|5|Briefly described|Map Legend||Paleozoic|||||||07-NOV-08
30320|Windoo Sandstone|69099|4|Described|GEOL_LUT_CSV files + geochron files|Cambrian||Grouped as Cambrian-Ordovician sedimentary rock, Southern Bonaparte Basin|||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert.|04-AUG-15
30320|Windoo Sandstone|69634|4|Described|100k_interpgeop_lut.csv|Ordovician|Series 3|Geological province: Halls Creek Orogen. Of Southern Bonaparte Basin. Events: Alice Springs Orogen; Mount Eclipse Movement; Pertnjara-Brewer Movements.|509-443.4 Ma (Inferred)||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert|
30320|Windoo Sandstone|70154|5|Briefly described|100k_interpgeop_lut.csv||||||||Quartz sandstone; minor mudstone, dolomite and stromatolitic chert.|
30320|Windoo Sandstone|70826|6|Mentioned|p7 tbl 3|Ordovician|Cambrian|Ord Basin.||||||
30320|Windoo Sandstone|71267|4|Described|GEOL_LUT_CSV files|Early Ordovician|Series 2|Geological province: Halls Creek Orogen. Of Ord Basin. Events: Alice Springs Orogeny (450-295 Ma); Pertnjara-Brewer Movements (Alice Springs Orogeny phase 2) (390-360 Ma); Rodingan Movement (Alice Springs Orogeny phase 1) (450-420 Ma); King Leopold Orogeny (670-510 Ma). See 1m_geologyp12_lithology_lut.csv, 100k_interpgeop_lut.csv, 1M_geologyp12_lut.csv.|510-470 Ma (inferred)||||Quartz sandstone, minor mudstone, dolomite, stromatolitic chert|
79223|Winnall Group|70416|5|Briefly described|p65 Fig.2|Early Cambrian|Ediacaran|Edgoose et al. (2015); previously Winnall beds. Amadeus Basin.|||Carnegie Formation, Ellis Sandstone, Maurice Formation.|Overlies Julie Formation. Equivalent to Arumbera Sandstone (Arunta Province).||
79223|Winnall Group|71898|5|Briefly described|iii, p6, p8|Cambrian|Late Neoproterozoic|Amadeus Basin. Rocks previously assigned to the Pertaoorrta Group are now included in this group on the basis of new mapping by NTGS. Similar provenance spectra to Quandong Conglomerate.|||Includes the Puna Kura Kura Formation.|Overlies the Quandong Conglomerate.|Thinly bedded to flaggy, fine grained micaceous sandstone.|19-NOV-18
79223|Winnall Group|72369|4|Described|iii,p15-16,23|Cambrian|Neoproterozoic|Of Amadeus Basin. Formerly known as Winnall Beds (of Ranford et al 1965, redefined by Donnellan and Normington 2017). Occurs in the south-central and western Amadeus Basin. A review of recent NTGS mapping (Normington and Donnellan in prep, Donnellan et al in prep) identified discrete lithostratigraphic units (Breaden, Gloaming, Froud, Liddle and Puna Kura Kura formations; defined by Donnellan and Normington 2017) previously mapped as informal units at Winnall Ridge in LAKE AMADEUS map sheet by Ranford et al (1965). Interpreted to have been deposited during Petermann Orogeny (c. 580-530 Ma), and contains dominant Musgrave Province source (SHRIMP U-Pb detrital zircon dating; Camacho et al 2002).|||Includes Breaden, Gloaming, Froud, Liddle and Puna Kura Kura formations.|Overlain by Pertaoorrta Group. Underlain by Inindia beds, or Aralka Formation or Pertatataka Formation or Bitter Springs Group.|Succession of ridge-forming sandstone and recessive, generally poorly-exposed siltstone.|
79223|Winnall Group|72374|5|Briefly described|p14|||Of Amadeus Basin.|||Includes Gloaming Formation.|||
79223|Winnall Group|73085|6|Mentioned|p1, p4, p27|early Cambrian|Ediacaran|Previously the Winnall beds. Lower portion may correlate with the Pertatataka Formation. Upper portion may correlate with the Arumbera Sandstone.||||Underlain by and partly equivalent to Inindia beds. Partly overlain by Cleland Sandstone, Tempe Formation, Chandler Formation. Possibly partly equivalent to Arumbera Sandstone and Namatjira Formation.||
79223|Winnall Group|73086|6|Mentioned|p3, p5, p126-127, p129|||Amadeus Basin. Central-western NT. Informal upper portion is part of Supersequence IV.|||Gloaming Formation|Underlain by and equivalent to Inindia beds. Equivalent to Arumbera Sandstone.||
79223|Winnall Group|73119|6|Mentioned|piii, p5, p7, p9, p12|||Amadeus Basin, western. Dominant detrital zircon age components are Mesoproterozoic, with a major peak between ca 1170 - 1120 Ma and other minor peaks. These ages suggest the Musgrave Province was a major source of detritus, with minor contributions from the older Aileron and Warumpi provinces or similar. Provenance of ca 1000-662 Ma zircons is not clear as there are no obvious Australian sources.  [See article for provenance discussion].|||Liddle Formation, Puna Kura Kura Formation, Chookla Member|||
79223|Winnall Group|73279|6|Mentioned|p8|||Amadeus Basin.|||Puna Kura Kura Formation, Chookla Member|||
27010|Witch Wai Conglomerate|39210|5|Briefly described|p49|||||||||
27010|Witch Wai Conglomerate|39679|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
27010|Witch Wai Conglomerate|40852|6|Mentioned|Fig.3.7|||||||||
27010|Witch Wai Conglomerate|45022|4|Described|p.97.||Early Cambrian|Age given as Lower Cambrian?||||||
27010|Witch Wai Conglomerate|46676|14|Not recorded|p.6||Early Cambrian|L.Cambrian.||||||
69133|Wonarah Formation|62657|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Chertified limestone and mudstone, dolostone; siliceous concretions; minor intraclast and bioclast wacke, grainstone, siltstone, sandstone.||||||
69133|Wonarah Formation|62658|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of the Barkly Group. Chertified limestone and mudstone, dolostone; siliceous concretions; minor intraclast and bioclast wacke to grainstone, siltstone and sandstone.||||||
69133|Wonarah Formation|62659|5|Briefly described|Map Legend|Cambrian|Cambrian|Siliceous shale, siltstone, chertified limestone; basal quartz sandstone and conglomerate.||||||
69133|Wonarah Formation|64443|1|Redefined|p2, p4, p5 Fig.3, p6 Tb.1, p10-13, p40|Middle Cambrian|Middle Cambrian|Note: revised definition - formalisation of Wonarah beds as Wonarah Formation; of Barkly Group. Previously known as Alroy Downs beds, Wonarah beds, Alexandria beds and Burton beds. Conformably underlies Camooweal Dolostone and Ranken Limestone; unconformably underlies Brunette Limestone. Correlative of Anthony Lagoon beds, Inca Formation, Gowers Formation, Beetle Creek Formation, Currant Bush Limestone, Blazan Shale, Arthur Creek Formation. Dated to latest Ordian-?Floran; max 191+m thick. Forms low, dissected hills which are the most elevated areas of this map area. Characteristics include siliciclastic laminations, chert concretions, phosphorite, evaporites, disseminated pyrite, fossils.||||Disconformably overlies Thorntonia Limestone or unconformably overlies Helen Springs Volcanics, Mittiebah Sandstone, Renner Group or South Nicholson Group. See Comments.|Silty dolostone, calci/dolomudstone and siliciclastic mudstone interbeds, micaceous siltstone; minor wacke- to grainstone, basal carbonaceous marly laminite.|14-MAY-14
69133|Wonarah Formation|65336|5|Briefly described|Map Legend|Middle Cambrian|Middle Cambrian|Of Barkly Group, Georgina Basin. Unconformably overlies Thorntonia Limestone of Narpa Group; underlies Ranken Limestone. Predominantly chertified limestone and mudstone, dolostone; siliceous concretions.||||||
69133|Wonarah Formation|65337|3|Fully described|p9 Fig.5, pp65-66.|Middle Cambrian|Middle Cambrian|Southwest MOUNT DRUMMOND area. 36 - 146 m thick. Includes former Burton, Alexandria and Alroy Downs beds. Outcrops are mostly strongly silicified, with low cliffs of brecciated chert with a silcrete matrix. Moderately fossiliferous.||Unit in Barkly Group.||Unconformably overlies South Nicholson Group and Helen Springs Volcanics. Unconformably overlies Kalkarindji Volcanic Group. Is overlain by Ranken Limestone.|Pervasively chertified fossiliferous limestone, shale and siltstone; minor phosphorite; basal sandstone.|
69133|Wonarah Formation|65344|5|Briefly described|p3, 9, 12, 13, 24-30, 47, Figs. ,Tbls|Middle Cambrian|Middle Cambrian|Of the Barkly Sub-basin, the Alexandria-Wonarah Basement High and the Undilla Sub-Basin. See thin section descriptions for detail.||||Overlies the Gum Ridge Formation, Helen Springs Volcanics or Thorntonia Limestone. Overlain by Camooweal Dolostone or Ranken Limestone.||03-MAY-12
69133|Wonarah Formation|65345|5|Briefly described|p3, p6 Fig.5, pp14 -23.|Middle Cambrian|Middle Cambrian|Undilla Sub-basin, Georgina Basin. Hosts major phosphate deposits. This Record summarises phosphate exploration carried out by exploration companies, mainly focussed on this Formation.||||Unconformably overlies Thorntonia Limestone. Is overlain by Ranken Limestone.||
69133|Wonarah Formation|67148|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|||Unit in Barkly Group.||Unconformably overlies Gum Ridge Formation.|Chertified limestone and mudstone, dolostone (silty dolostone, dolosparstone, mudstone interbeds); siliceous concretions; minor intraclast and bioclast wacke- to grainstone, oncoid rudstone, siltstone and sandstone.|
69133|Wonarah Formation|67149|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin. Lateral equivalent to Anthony Lagoon Formation.||Unit in Barkly Group.||Overlies Gum Ridge Formation.|Chertified limestone and mudstone, dolostones; siliceous concretions; minor intraclast and bioclast wacke- to grainstone, oncoid rudstone, siltstone and sandstone.|
69133|Wonarah Formation|67150|5|Briefly described|Map legend.|Middle Cambrian|Middle Cambrian|Georgina Basin. Lateral equivalent to Anthony Lagoon Formation.||Unit in Barkly Group.|||Chertified limestone and mudstone, dolostones; siliceous concretions; minor intraclast and bioclast wacke- to grainstone, oncoid rudstone, siltstone and sandstone.|
69133|Wonarah Formation|67352|4|Described|Throughout article.|||Of Kruse and Radke (2008); formerly Wonarah beds (Opik, 1956). Subsumes the partial synonyms Burton beds (Smith and Roberts 1963), Alexandria beds (Opik 1956), Alroy Downs beds (David 1932). A widely distributed unit. Forms low hills. It has a moderately diverse fauna, unlike Anthony Lagoon Formation. Contains phosphate deposits. See also Relationships notes: Is overlain (conformably) by Camooweal Dolostone, Ranken Limestone. Is correlated with lower Arthur Creek Formation.||Barkly Group||Interfingers with Anthony Lagoon Formation. Disconformably overlies Thorntonia Limestone, Gum Ridge Formation, Helen Springs Volcanics, Mittiebah Sandstone. See more in Comments.|Light grey, silty dolostone, siliciclastic mudstone, interbeds of calci-dolomudstone and siliciclastic mudstone; ferricrete and silcrete caps.|
69133|Wonarah Formation|69418|6|Mentioned|p3:31|||Georgina Basin. Hosts the Alroy, Buchanan Dam and Wonarah phosphate deposits (briefly described).||||||12-JUL-16
69133|Wonarah Formation|69434|5|Briefly described|p19:4|Middle Cambrian|Middle Cambrian|Georgina Basin.||||Unconformably overlies South Nicholson Group.||12-JUL-16
69133|Wonarah Formation|69437|5|Briefly described|p22:10-11|Series 3|Series 3|Western Undilla Sub-basin, Georgina Basin, Centralian B Superbasin. Sequence 2. Low- to moderate-energy marine deposits.||||Overlies Thorntonia Limestone. Is overlain by Ranken Limestone and Camooweal Dolostone. Lateral equivalent of Anthony Lagoon Formation and Point Wakefield beds.|Silty dolostone, calci/dolomudstone and siliciclastic mudstone.|12-JUL-16
69133|Wonarah Formation|69443|4|Described|p28:16, 21-24, 34, 42-43|Middle Cambrian|Middle Cambrian|Kruse in Kruse and Radke (2008), after Opik (1956). Central Georgina Basin. Crops out as low hills and plateau caps. 118-over 191m thick. Moderately diverse fossil fauna. Subtidal (below wave base) platform marine deposits. Lateral equivalent of Narpa Group. Correlated with, and passes laterally into, Anthony Lagoon and Arthur Creek Formations. Is overlain conformably by Ranken Limestone and Camooweal Dolostone. Has some mesoscale folding. Hosts the Alroy and Buchanan Dam phosphate deposits. May be the host unit (currently regarded as the Gum Ridge Formation) for an ore-grade (>15% P2O5) phosphorite horizon in the Wonarah area.||Barkly Group.||Overlies Gum Ridge Formation conformably (also ?disconformably); Thorntonia Limestone disconformably or Helen Springs Volcanics, Renner Group or South Nicholson Group unconformably.|Mostly silty dolostone with calci/dolomudstone and siliciclastic mudstone interbeds. These lithotypes are intergradational, locally recrystallised to dolosparstone, and exhibit varying degrees of pressure solution boudinage and possible bioturbation.|12-JUL-16
69133|Wonarah Formation|69445|5|Briefly described|p30:5, 17|Middle Cambrian|Middle Cambrian|Central Georgina Basin.||||Unconformably overlies Helen Springs Volcanics (Kalkarindji Suite).||12-JUL-16
69133|Wonarah Formation|69446|6|Mentioned|p31:4|||Georgina Basin.||||||12-JUL-16
69133|Wonarah Formation|69447|5|Briefly described|p32:2, 5|||Georgina Basin. Contains late Templetonian to Floran age trilobites which also occur in the Point Wakefield beds (Wiso Basin).||||Broadly correlated with Point Wakefield beds (Wiso Basin).||12-JUL-16
69133|Wonarah Formation|69561|6|Mentioned|p32 fig 1|Floran|Templetonian|||||Overlies Thorntonia Limestone, Conformably overlain by Ranken Limestone, Camooweal Dolostone||
69133|Wonarah Formation|69573|6|Mentioned|p656|||Features Cambrian Stage 5 fossil sites.||||||
69133|Wonarah Formation|69591|5|Briefly described|p88|Cambrian|Cambrian|Undilla Sub-basin, Georgina Basin.||Barkly Group.||||
69133|Wonarah Formation|69673|5|Briefly described|p116, p117, p129, p135|||Greater than 191m thick.||Barkly Group|||Silty dolostone with calci/dolomudstone and siliciclastic mudstone interbeds.|
69133|Wonarah Formation|70380|5|Briefly described|p745-746, p759|Series 3|Series 3|Kruse and Radke (2008). Includes the former Wonarah and Burton beds. Undilla Sub-basin, Georgina Basin.||||Interdigitates with Anthony Lagoon Formation.||
69133|Wonarah Formation|72527|6|Mentioned|p34-35.|Cambrian|Cambrian|Georgina Basin.||||Unconformably overlies Top Lily Sandstone.|Includes silicified cherty breccia at interface with Top Lily Sandstone.|
69133|Wonarah Formation|72967|6|Mentioned|p5|||Georgina Basin.||Barkly Group||||
69133|Wonarah Formation|73083|6|Mentioned|p7, p15, p22, p35|Cambrian|Cambrian|Georgina Basin.|||||Includes limestone.|
81653|Wonga Gneiss|72365|5|Briefly described|iii,p1,6,13-14,18-20,22,26-27,32,36|Orosirian|Orosirian|Geological province: Arnhem Province. S-type granite formed from partial melts of Melville Bay Metamorphics between c. 1880 Ma and ca. 1859 Ma (see Summary section for references). Kositcin et al (2015) reported SHRUMP U-Pb age of 1872+\-3 Ma (interpreted zircon crystallisation). Reno et al. (this record) provided continuum of zircon ages between 1887+\-9 Ma and 1861+\-9 Ma (LA-ICP-MS 207Pb/206Pb), interpreted as long-lived zircon growth spanning melt generation to granite crystallisation. Sample GV14JAW182A (migmatitic orthogneiss; 684225E 8623749N) records continuous monazite growth during a protracted HT metamorphic event. Zircon growth dated at 1871+\-7 Ma may indicate crystallisation of this igneous protolith, or  metamorphic zircon growth. Dated sample and sample location are provided.|1880+/-5 Ma igneous crystallisation.||||Fine- to medium-grained, porphyritic, garnet-biotite gneiss.|09-JAN-20
79872|Wonga Orthogneiss|71605|4|Described|iii, p1, p6-p9, p24||Orosirian|Arnhem Province. SHRIMP age interpreted as the timing of emplacement of the igneous protolith to the gneiss. This unit is oldest known plutonic unit in the Arnhem Province. Referred to as the Wonga Gneiss on iii. Metamorphism dated between 1877 Ma and 1864 (SHRIMP U-Pb this volume). Sample location and SHRIMP analyses discussed.|1880 +/- 5 Ma (SHRIMP U-Pb)||||Fine- to medium-grained, porphyritic garnet-biotite gneiss.|06-AUG-18
42196|Wonnadinna Dolostone|24442|6|Mentioned|p49|||Geological Province: Georgina Basin.||||||
42196|Wonnadinna Dolostone|60122|4|Described|p4-5, p11 Tb. 1, p12, p41|Neoproterozoic|Neoproterozoic|Of Keepera Gp. Purple-red to yellow-brown and green-grey, locally quartzic dolostone interbedded with dolomitic arkose, sltst. and shale. Conformable on Black Stump Arkose; disconformable below Elyuah Fm and Gnallan-a-Gea Arkose. Max. thick: 460m.||||||24-MAY-05
42196|Wonnadinna Dolostone|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group.  Dolostone, quartzic dolostone.  Overlies the Black Stump Arkose; overlain by Gnallan-a-Gea Arkose.||||||
42196|Wonnadinna Dolostone|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Keepera Group. Dolostone, quartzitic dolostone. Geological Province: southern Georgina Basin.||||||
42196|Wonnadinna Dolostone|64068|3|Fully described|p48, p18, p46, p19, p viii|Ediacaran|Ediacaran|450 m thick. Correlated with Nuccaleena Formation.||Of Keepera Group.||Conformably overlies Black Stump Arkose. Is overlain disconformably by Gnallan-a-Gea Arkose.|Variably-coloured dolostone; interbedded more or less dolomitic arkose, siltstone and shale.|05-APR-12
42196|Wonnadinna Dolostone|65338|6|Mentioned|p60, p63.|||||Unit in Keepera Group.||Is overlain by Mopunga Group.||
42196|Wonnadinna Dolostone|68270|4|Described|p680-681,683,686|Ediacaran|Ediacaran|Southern Georgina Basin. Composite section: drillhole Hay River 8 (lat. 23'8'12"N, long. 137'41'0"E) and nearby outcrop. Less than 460m thick. Intertidal to deep marine deposit. Cap dolomite unit to the Black Stump Arkose related to end of Elatina glaciation. Correlable to Wanapi Dolomite Member, Nuccaleena Formation, lower Boondawari Formation.||||Overlain disconformably by Gnallan-a-Gea Arkose. Underlain by Black Stump Arkose (paraconformity).|Purple-red to yellowbrown and green-grey dolomite that is sandy in parts; locally interbedded with red-brown, purple and green-grey arkose and siltstone, some of which is dolomitic.|03-JUL-19
42196|Wonnadinna Dolostone|69437|5|Briefly described|p22:4-5, 7|Ediacaran|Ediacaran|SE Georgina Basin, Centralian A Superbasin. Supersequence 3.||||Overlies Black Stump Arkose (Keepera Group).||12-JUL-16
42196|Wonnadinna Dolostone|69443|4|Described|p28:7-10, 33; 28:38 Fig.28.36|Ediacaran|Ediacaran|Walter (1980). Georgina Basin. Forms low rises, hills and moderate ridges locally; otherwise regressive. Up to 460m thick. Intertidal, shallow subtidal and deeper marine depositional environments. Exposed by Tarlton Fault.||Keepera Group.||Conformably and gradationally overlies Black Stump Arkose. Is overlain by Gnallan-a-Gea Arkose disconformably or with slight angular unconformity.|Dolostone and quartzose dolostone, interbedded with dolomitic arkose, siltstone and shale. The dolostone bears oncoids, fenestrae and possible columnar stromatolites.|12-JUL-16
42196|Wonnadinna Dolostone|69673|5|Briefly described|p114 fig 92, p115|Ediacaran|Ediacaran |up to 460m thick.||Keepera Group|||Dolostone interbedded with dolomitic arkose, siltstone and shale.|
23244|Woodah Sandstone|22538|6|Mentioned|Fig3 p708|||||||||04-JUN-18
23244|Woodah Sandstone|22600|4|Described|Map legend|Statherian|Statherian|||||||
23244|Woodah Sandstone|22808|2|Defined|31|Statherian|Statherian|Of the Alyangula Subgroup. Overlain by Bartalumba Basalt; underlain by Grindall Formation.||||||20-DEC-06
23244|Woodah Sandstone|24048|3|Fully described|p20|Paleoproterozoic|Paleoproterozoic|Of the Alyangula Subgroup.  Max. thickness: 60m.  Geological Province: McArthur Basin.||||||07-NOV-08
23244|Woodah Sandstone|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup, Groote Eylandt Group. Thin basal pebble-boulder conglomerate, polymict; medium to fine-grained pebbly sandstone and interbedded mudstone; sandstone: medium-grained, flat to cross-bedded. Geol. Prov: McArthur Basin.||||||13-OCT-05
23244|Woodah Sandstone|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
23244|Woodah Sandstone|44112|6|Mentioned|Fig11p30|||||||||
23244|Woodah Sandstone|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Alyangula Subgroup (Groote Eylandt Group). Thin basal pebble-boulder conglomerate, polymict; medium to fine-grained pebbly sandstone and interbedded mudstone; sandstone: medium-grained, flat to cross-bedded. Geol. Prov: McArthur Basin.||||||20-DEC-06
23244|Woodah Sandstone|63866|5|Briefly described|p114-p115|||Leichhardt/Calvert Superbasins. ||||Overlain by the Gadabara Volcanics. Equivalent to the Dhunganda Formation and the Alyinga Sandstone.||
23244|Woodah Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5|||Caledon Shelf South, McArthur Basin.||Of the Alyangula Subgroup.|||Sandstone and conglomerate.|04-JUN-18
23244|Woodah Sandstone|69430|3|Fully described|p15:3, 5-7, 13|||NE McArthur Basin. Maximum thickness 50-60m exposed at type section on Morgan Island (53L 618300mE 8510000mN). Braided fluvial deposits. Appears as Woodnah Sandstone in 15:3. Lateral equivalent of Alyinga Sandstone.||Alyangula Subgroup.||Unconformably overlies Grindall Formation and Bukudal Granite. Is overlain unconformably by Coast Range Sandstone, and disconformably and intruded by Gadabara Volcanics.|Medium- to coarse-grained sandstone, cobble to boulder conglomerate, mudstone.|12-JUL-16
23244|Woodah Sandstone|70302|4|Described|iv, p1, p5-7, p11-12|Statherian|Statherian|McArthur Basin. Mainly sourced from Pine Creek Orogen. SHRIMP U-Pb zircon maximum depositional age of 1815 +/- 13 Ma (Kositcin et al., 2015) is significantly older than true depositional age (inferred from correlation) of c.1730 Ma. Deposited in a braided fluvial environment.|c.1730 Ma.|Basal Alyangula Subgroup.||Unconformably overlies Grindall Formation. Correlated with Tawallah Group.|Poorly-sorted, pebble to boulder basal conglomerate grading into medium- to coarse-grained, moderately well-sorted, orange sandstone.|06-FEB-18
23244|Woodah Sandstone|70719|5|Briefly described|p5|Orosirian|Orosirian|McArthur Basin. Geochronology by Kositcin et al. (2015).|1815 +/- 13 Ma (maximum depositional age).|||Unconformably overlies Grindall Formation.||
23244|Woodah Sandstone|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1815+/-13 Ma (MDA: U-Pb zircon SHRIMP)||||Medium-grained, orange, quartz-rich sandstone with rare feldspar grains.|
23244|Woodah Sandstone|71605|6|Mentioned|p35|||||||Disconformably overlain by the Gadabara Volcanics.||
23244|Woodah Sandstone|72377|5|Briefly described|p9|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Kositcin et al., 2015b reported SHRIMP U-Pb zircon maximum depositional age of 1815+\-13 Ma.|1815+\-13 Ma (max dep age)|||Overlain unconformably, and intruded by Gadabara Volcanics.||
72422|Woodalla Member|62642|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province. Interbedded sandstone/wacke and micaceous siltsotne/slate/phyllite/schist; laminated, graded and cross-bedded.||||||07-NOV-08
72422|Woodalla Member|65338|3|Fully described|App 1 p84, p8 Table 1, p12|Orosirian|Orosirian|New name. Deep-water, turbiditic: represents Bouma sequences. Deformed by Stafford Event and overprinted by Yambah Event. Correlates with Lander Rock Formation in MOUNT DOREEN. Passes laterally into Mount Stafford Member.|1866 +/- 3 Ma (Claoue-Long et al. 2008a).|Unit in Lander Rock Formation.||Intruded by granite.|Feldspathic quartzarenite: granular, massive, laminated or graded, interbedded with cleaved siltstone; local stratiform amphibolite.|
72422|Woodalla Member|67164|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Interbedded sandstone/wacke and micaceous siltstone/slate/phyllite/schist; laminated, graded and cross-bedded.|
72422|Woodalla Member|67892|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Arunta Region; Aileron Province.||Unit in Lander Rock Formation.|||Interbedded sandstone/wacke and micaceous siltstone/slate/phyllite/schist; laminated, graded and cross-bedded.|
72422|Woodalla Member|69427|5|Briefly described|p12:5|||Aileron Province. A turbiditic succession similar in nature to turbiditic Lander Rock Formation in the westen Aileron Province.||Lander Rock Formation.||||12-JUL-16
72988|Woodcutters Supergroup|66683|5|Briefly described|p365, p377.|Paleoproterozoic|Paleoproterozoic|Clastic and carbonate sedimentary rocks thought to have been deposited during a phase of continental rifting of the underlying Neoarchean basement (Needham et al., 1988) at ca. 2020 Ma, constrained by U-Pb zircon dating of interlayered felsic volcanic rocks (Worden et al., 2008b).|c.2020 Ma.||Includes Kakadu, Manton and Mount Partridge Groups.|Is overlain unconformably by Cosmo Supergroup.|Clastic and carbonate sedimentary rocks; interlayered with felsic volcanics.|11-JUL-16
72988|Woodcutters Supergroup|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||Includes Manton and Mount Partridge Groups.|||23-NOV-11
72988|Woodcutters Supergroup|67232|4|Described|p2. |Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. The overlying unconformity represents at least 160 My.|2020 Ma.|||Is intruded by Cullen Supersuite. Is overlain unconformably by Cosmo Supergroup.|Carbonate; carbonaceous, siliciclastic and volcaniclastic sedimentary rocks; subordinate mafic and felsic volcanic rocks.|
72988|Woodcutters Supergroup|67355|5|Briefly described|p6-7, p10|Orosirian|Siderian|Unconformably overlies the Archean complexes. There appears to be a major hiatus between this and the overlying Cosmo Howley Supergroup.|||Kakadu Group, Namoona Group, Mount Partridge Group, Masson Formation, Cahill Formation, Manton Group.|Underlies the Cosmo Howley Supergroup unconformably.|Comprises current-bedded and ripple-marked fluviatile arenite, intertidal stromatolitic carbonate and argillite, including carbonaceous and pyritic shale.|27-JAN-17
72988|Woodcutters Supergroup|67479|6|Mentioned|p6 Fig.2|||||||||
72988|Woodcutters Supergroup|67779|5|Briefly described|p4, p6 Fig.5, p91, p104.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Detrital zircon analysis suggests a different provenance from the Nimbuwah Domain (Cahill Formation). Stratigraphic correlation with Kakadu Group.|||Includes Namoona, Manton and Mount Partridge Groups and Fog Bay Metamorphics.|||
72988|Woodcutters Supergroup|69383|5|Briefly described|pvii|||Includes Crater Formation, Mundogie Sandstone.|ca 2020 Ma (Worden et al 2004, 2008)|||||
72988|Woodcutters Supergroup|69417|5|Briefly described|p2:4-5,|Orosirian|Orosirian|Pine Creek Orogen.|2030-2000 Ma.||||Sandstone, shale, mudstone and carbonate rocks.|12-JUL-16
72988|Woodcutters Supergroup|69419|6|Mentioned|p4:2 Fig.4.2|||||||||12-JUL-16
72988|Woodcutters Supergroup|69420|4|Described|p5:1-2, 4-6, 8-9, 11, 15, 32, 38, 66, 85|Paleoproterozoic|Paleoproterozoic|See also 100, 111, 115. Ahmad and McCready (2001). Pine Creek Orogen. Deposited at or before c.2020 Ma. Typically has smooth REE patterns, consistent with provenance from calc-alkaline andesitic rocks. No detrital zircons younger than c.2000 Ma.|||Manton, Mount Partridge, Namoona and Kakadu Groups; Fog Bay Metamorphics.|Is overlain unconformably by Cosmo Supergroup.||12-JUL-16
72988|Woodcutters Supergroup|69673|6|Mentioned|p3 fig 2|Orosirian|Rhyacian|||||||
72988|Woodcutters Supergroup|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||Includes Mount Partridge, Manton, Namoona  Groups.|||28-FEB-18
72988|Woodcutters Supergroup|71256|5|Briefly described|p18|Paleoproterozoic|Paleoproterozoic||~2020 Ma|||Underlain unconformably by Rum Jungle Complex.|Sedimentary and volcanic rocks.|
72988|Woodcutters Supergroup|73089|6|Mentioned|p31|Orosirian|Orosirian|Pine Creek Orogen, Central Domain. Archean detritus consistent with underlying basement.|c. 2020 Ma|||||
76081|Woodenjerrie beds|64735|5|Briefly described|p205 Fig 1, p205, p217,|Orosirian|Orosirian|Equivalent to Warramunga Formation.||Of Warramunga Group.||||30-APR-12
76081|Woodenjerrie beds|65209|5|Briefly described|p35 Fig.1, p37, p39|Paleoproterozoic|Paleoproterozoic|With Junalki Formation, this unit is broadly correlated with Warramunga Formation. Development of axial planar slaty cleavage.|||||Contains argillaceous banded ironstone.|05-JAN-17
76081|Woodenjerrie beds|65338|5|Briefly described|p6. |||Warramunga Province, Tennant Region. Correlated with Warramunga Formation. Deformed during the c.1850 Ma Tennant Event. Granitic intrusions c.1850 - 1840 Ma.||||Intruded by granitic rocks of Tennant Creek Supersuite.||
76081|Woodenjerrie beds|66767|5|Briefly described|p57|||Warramunga Province, and basement to Davenport Province.||||Correlative of Warramunga Formation.||
76081|Woodenjerrie beds|67148|5|Briefly described|Map legend.|Orosirian|Orosirian||||||Interbedded phyllitic siltstone and fine-grained greywacke; porphyritic felsic lava.|
76081|Woodenjerrie beds|67352|4|Described|v, p8, p11, p41, p44, p50, p57|Orosirian|Orosirian|Warramunga Province. Includes former Warramunga Group rocks mapped by Smith (1964), reassigned by Donnellan (2004). Quartz-haematite veins contain W minerals.|1860-1850 Ma|||Overlain by Epenarra Volcanics (unconformably). Correlated with Warramunga and Junalki Formations.|Interbedded phyllitic siltstone and fine-grained greywacke, lithic arenite: thinly to medium bedded; siltstone, shale; subordinate vesicular and porphyritic felsic volcanic rocks, chert, jaspilite and banded ironstone.|
76081|Woodenjerrie beds|69187|6|Mentioned|p53 Fig.2, p59|||Warramunga Province.||||correlative of Warramunga Formation||
76081|Woodenjerrie beds|69424|4|Described|p9:2-7, 9-10, 15, 32-33, 56|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Informal name, for rocks previously mapped as undifferentiated Warramunga Group immediately to the N of Davenport Province; excludes rocks now assigned to Junalki Formation on the basis of their contrasting magnetic character. Moderately deep-water depositional environment, at least partly turbiditic; presumably subaqueous volcanism. Thickness unknown. Folded during the c.1850 Ma Tennant Event. An "ambiguous" age, from probable porphyritic dacitic lava, by Smith (1999, 2000). Felsic extrusives of this unit are included in the Tennant Creek Supersuite. Hosts W in quartz veins: minor wolframite produced from the Woodenjerrie mine.|1864 +/- 4 Ma or 1854 +/- 4 Ma.|||Is overlain unconformably by Epenarra Volcanics (Ooradidgee Group) and Unimbra Sandstone (Hatches Creek Group). Lateral equivalent of Junalki and Warramunga Formations.|Greywacke and lithic sandstone, siltstone, shale; subordinate but locally dominant felsic volcanic rocks (ie volcanic lithofacies); chert; jaspilite; argillaceous banded ironstone.|12-JUL-16
76081|Woodenjerrie beds|69425|5|Briefly described|p10:2, 10, 13, 15, 24|||Tennant Region.||||Is overlain unconformably by Unimbra Sandstone. Correlative of Junalki Formation.||12-JUL-16
76081|Woodenjerrie beds|69431|6|Mentioned|p16:2|||Tennant Region.||||||12-JUL-16
76081|Woodenjerrie beds|73124|6|Mentioned|p2 Fig.1|||||||||
76081|Woodenjerrie beds|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||||||
76081|Woodenjerrie beds|73427|5|Briefly described|p3, p12, App.A|Orosirian|Orosirian|North Australian Craton, Tennant Region/East Tennant.|1865-1860 Ma|||Intruded by Tennant Creek Supersuite.|Turbiditic wacke, siltstone, and minor felsic volcanic rocks.|
76081|Woodenjerrie beds|73460|6|Mentioned|p2|||Warramunga Province.||||||
76081|Woodenjerrie beds|73550|6|Mentioned|p4|||Warramunga Province.|Older than 1860 Ma|||Equivalent to Warramunga Formation. Unconformably overlain (angular) by Ooradidgee Group.||
76081|Woodenjerrie beds|73590|6|Mentioned|p1-2|Orosirian|Orosirian|Warramunga Province. Some of the oldest rocks in the province.|older than 1860 Ma|||Equivalent to Warramunga Formation and Junalki Formation. Unconformably (angular) overlain by Ooradidgee Group.||
24584|Woodforde River beds|8222|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Geological Province: Arunta Block. Marble, sillimanite schist, calc-silicate rock, quartzite.||||||20-DEC-06
24584|Woodforde River beds|23270|5|Briefly described|Table 1, p6||Proterozoic|In the Arunta Block (Division 3 - Reynolds Range Group). Correlated with Algamba Dolomite Member.||||||20-DEC-06
24584|Woodforde River beds|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block(Division Three). Age: Early or Middle Proterozoic.||||||20-DEC-06
24584|Woodforde River beds|24047|6|Mentioned|p40|||See also Woodforde River Beds.  Geological Province: Arunta province.||||||
24584|Woodforde River beds|37058|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24584|Woodforde River beds|39887|6|Mentioned|Fig.5|||||||||
24584|Woodforde River beds|42217|6|Mentioned|p415|||||||||
24584|Woodforde River beds|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
24584|Woodforde River beds|44158|4|Described|p11, Table.1|Paleoproterozoic|Paleoproterozoic|Of the Reynolds Range Group. Age: 1820 - 1780 Ma. Intruded by rapakivi granite of the Southwark Granitic Suite.||||||05-MAY-10
24584|Woodforde River beds|48992|2|Defined|p59|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24584|Woodforde River beds|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex. Metamorphosed sandstone and siltstone, pelitic schist, minor calcareous rocks and metabasalt.||||||07-NOV-08
24584|Woodforde River beds|65329|5|Briefly described|Map legend|Palaeoproterozoic|Paleoproterozoic|Of Reynolds Range Group. Epidotic calc-silicate and calcareous rocks; moderate linear magnetic response||||Shown as lateral equivalent to Pine Hill Formation||19-DEC-12
24584|Woodforde River beds|65330|5|Briefly described|Map legend|Palaeoproterozoic|Paleoproterozoic|Of Reynolds Range Group. Epidotic calc-silicate and calcareous rocks; moderate linear magnetic response||||Shown as lateral equivalent to Pine Hill Formation||19-DEC-12
24584|Woodforde River beds|69427|5|Briefly described|p12:25|||Aileron Province.||||Correlated with Algamba Dolostone Member.|Ferruginous siltstone, gedrite-cordierite gneiss, diopside-plagioclase-quartz rock, spinel-olivine marble, epidote-bearing calc-silicate and carbonate rocks.|12-JUL-16
28280|Woodgreen Granite Complex|33103|4|Described|Table 2|||Mention p17.  High radioactive anomalies.||||||20-DEC-06
28280|Woodgreen Granite Complex|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
28280|Woodgreen Granite Complex|39888|6|Mentioned|Fig.8|||||||||
28280|Woodgreen Granite Complex|61388|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Granite, gneissic granite, porphyritic granite. Geological Province: Arunta Region.||||||07-NOV-08
28280|Woodgreen Granite Complex|64068|6|Mentioned|p162, 163|||Part of ?Proterozoic basement in Mount Skinner area.||||||
28280|Woodgreen Granite Complex|65341|4|Described|p2 Fig.2, p4, pp7-10. |Paleoproterozoic|Paleoproterozoic|Several un-named sub-units are mapped and described separately. Lack of deformation suggests it may be related to the 1730 - 1700 Ma Strangways Orogeny. S-type. Commonly overlain by silcrete.||||Separated from Delny Metamorphics to the south by the Waite River Shear Zone. Intrudes Anira Metamorphics.|Diverse granites: coarse, porphyritic, commonly garnet-and biotite-bearing; gneissic granite and migmatite; medium biotite granite; medium leucogranite.|
28280|Woodgreen Granite Complex|65556|6|Mentioned|p35|||Encloses Anira Metamorphics.||||||
28280|Woodgreen Granite Complex|69427|5|Briefly described|p12:27, 40-41|||Haines and Scrimgeour (2007). Comprises diverse granites and minor migmatite over a wide area S of Mount Skinner and Kunoth Knob, Aileron Province.||||Surrounds and transitions into Anira Metamorphics.|Coarse-grained biotite-garnet granite with tabular K-feldspar phenocrysts, finer-grained equigranular biotite granite, and biotite-rich, garnet-absent porphyritic granite. Local cordierite-bearing migmatitic rocks. Some peraluminous, S-type phases.|12-JUL-16
28280|Woodgreen Granite Complex|69917|5|Briefly described|p104-107|Statherian|Statherian|Central Arunta Region, Aileron Province.  U/Pb LA-ICPMS zircon dating of 2 samples suggests that the Complex was produced by granulite-facies partial melting of the Anira Metamorphics during the early stages of the 1730-1690 Ma Strangways Event.||||Intrudes Anira Metamorphics. Inferred to intrude Delny Metamorphics (shear zone).|Dominant rock types include coarse-grained biotite-garnet granite with tabular K-feldspar phenocrysts, fine-grained equigranular biotite granite, and biotite-rich garnet-free porphyritic granite; minor migmatite.|
28280|Woodgreen Granite Complex|73551|6|Mentioned|p5|||||||||
77814|Woola Downs Granite|69917|4|Described|p93-95, 1|Statherian|Orosirian|Central Arunta Region, Aileron Province. U/Pb LA-ICPMS zircon dating. Age is interpreted as the magmatic crystallisation age.|1805+/-6 Ma|||Intrudes Lander Rock Formation.|Strongly altered granite with large relict igneous feldspar phenocrysts (>2 mm across, most likely K-feldspar) that are extensively replaced by epidote and zoisite.|29-JUL-15
77814|Woola Downs Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1805+/-6 Ma (U-Pb zircon LA-ICPMS).||||Granite.|
75946|Woolianna Gabbro|67232|2|Defined|iv, p6, p8 Fig.6, pp9-19, pp26-30, p34.|Paleoproterozoic|Paleoproterozoic|Named after Woolianna homestead, Road and school 5 km north of Daly River township. Litchfield Province, Pine Creek Orogen. Previously part of Wangi Basics, now abandoned. Type locality is a large outcrop on MOYLE and WINGATE MOUNTAINS, about 40 km SW of Daly River township. Possible correlative of Tickalara Metamorphics, Halls Creek Orogen. Metamorphosed to amphibolite facies with overprinting greenschist-facies retrogression. Distinctive back-arc geochemical signature; contamination from adjacent Ti-Tree Granophyre produces 'crust-like' signature. Local minor shear-zone-hosted Cu-Pb-Zn-Ag mineralisation. Strong magnetic response. Geochemistry is described in detail. Interpreted to represent part of a now dismembered island arc tholeiite/BABB association; only subvolcanic levels are exposed.|1860 - 1855 Ma (Glass 2010).||||Metamorphosed medium- to coarse-grained, variably altered, equigranular rocks: gabbro, hypersthene gabbro and microgabbro to coarse-grained dolerite; locally metaperidotite, metapyroxenite, metaharzburgite, amphibolite, metadolerite and metabasalt.|
75946|Woolianna Gabbro|67779|6|Mentioned|p6 Fig.5.|Paleoproterozoic|Paleoproterozoic|Litchfield Province, Pine Creek Orogen.||||||
75946|Woolianna Gabbro|69420|5|Briefly described|p5:4, 29|Paleoproterozoic|Paleoproterozoic|Litchfield Domain, Pine Creek Orogen. Part of the obsolete Wangi Basics. Probably representative of back-arc basin oceanic crust.|||||High-alumina gabbro and dolerite, depleted low-Ti gabbro, low-Ti dolerite.|12-JUL-16
75946|Woolianna Gabbro|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||||Metamorphosed diorite, dolerite, gabbro, pyroxenite and peridotite.|
24634|Woolner Granite|22479|5|Briefly described|fig1p2|Archean|Archean|Age: 2700Ma old.||||||07-NOV-08
24634|Woolner Granite|22810|6|Mentioned|P9||Archean|Age of unit is 2675+/-14 Ma.||||||07-NOV-08
24634|Woolner Granite|24047|5|Briefly described|p5 Fig.4, p40|Archean|Archean|Foliated granite.  Age: 2700Ma.  Geological Province: Pine Creek Orogen.||||||07-NOV-08
24634|Woolner Granite|39679|6|Mentioned|Map legend|Archean|Archean|||||||07-NOV-08
24634|Woolner Granite|40492|6|Mentioned|Map legend|Paleoproterozoic|Neoarchean|Early Proterozoic to Late Archaean||||||07-NOV-08
24634|Woolner Granite|40493|4|Described|p5|||||||||
24634|Woolner Granite|40808|6|Mentioned|p3|||See also Fig.4||||||
24634|Woolner Granite|41304|6|Mentioned|Map legend|Archean||||||||07-NOV-08
24634|Woolner Granite|41305|3|Fully described|p3|||||||||
24634|Woolner Granite|41980|6|Mentioned|Fig.5 P587|||||||||
24634|Woolner Granite|43187|5|Briefly described|p3|||||||||
24634|Woolner Granite|43624|6|Mentioned|Table 1,p9||Archean|||||||07-NOV-08
24634|Woolner Granite|46658|6|Mentioned|p547|||||||||
24634|Woolner Granite|50623|6|Mentioned|p259|Archean|Archean|||||||07-NOV-08
24634|Woolner Granite|62375|5|Briefly described|p8, 10 Fig. 3|Archean|Archean|Age: 2675 +/- 15Ma. ||||||09-FEB-10
24634|Woolner Granite|63866|5|Briefly described|p108, p117|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. |2675 +/- 15 Ma (McAndrew et al., 1985)|||Overlain by the Dirty Water Metamorphics.||
24634|Woolner Granite|64698|5|Briefly described|lithinterp table||Neoarchean|Age 2675Ma SHRIMP U/Pb. I-type. Granite. Basement to Palaeoproterozoic succession.||||||07-JAN-09
24634|Woolner Granite|64730|5|Briefly described|p124-5 Fig. 3|Neoarchean|Neoarchean||2675+/-15 Ma SHRIMP zircon (McAndrew et al.1985)|||Unconformably underlies Dirty Water Metamorphics.||02-MAY-12
24634|Woolner Granite|65232|5|Briefly described|p5, p6 Fig. 5|Archaean|Archaean|Age: 2700 Ma. Foliated granite. Erosional upper contact. Variation on Woolner Complex, see also p2||||||09-FEB-10
24634|Woolner Granite|65339|5|Briefly described|p4.|||Northwestern Pine Creek Orogen. Forms a concealed part of the granitic basement.|2675 +/- 15 Ma (McAndrew et al. 1985).|||Is overlain by Dirty Water Metasediments.||
24634|Woolner Granite|66683|5|Briefly described|pp365-367, pp377-378.|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. Felsic crystalline basement concealed under c.50m of Cretaceous cover. Age similarity with Nimbuwah Domain basement suggests a common shallow Neoarchean basement to a large area of Paleoproterozoic rocks in the Orogen.|2675 +/- 28 Ma.||||Foliated and gneissic biotite granite, muscovite-biotite granite, muscovite-biotite-orthoclase granite.|
24634|Woolner Granite|67232|5|Briefly described|p2. |Archean|Archean|Part of the basement to the Central Domain, Pine Creek Orogen.|2674 Ma.|||||
24634|Woolner Granite|67355|6|Mentioned|p4, p6 Fig.4||Neoarchean|Age from Williams and Compston (1983).|2675 +/- 15 Ma (SHRIMP U-Pb zircon) |||Unconformably underlies the Stanley Metamorphics.||27-JAN-17
24634|Woolner Granite|67479|6|Mentioned|p56|||Unexposed.||||||
24634|Woolner Granite|67564|5|Briefly described|p9 Fig.4.|Archean|Archean||2675 Ma.||||Foliated granite.|
24634|Woolner Granite|67779|5|Briefly described|p6 Fig.5, p7, p12, p78.|Archean|Archean|Central Domain, Pine Creek Orogen. Characterised by distinct gravity lows. Crystallisation age by SHRIMP U-Pb zircon. No inherited zircons: crystallised from a single mantle-derived juvenile source.|2674 +/- 3 Ma (Glass et al. 2010).|||||
24634|Woolner Granite|68697|5|Briefly described|vi, p2, p26-28, p46|Neoarchean|Neoarchean|Central Domain, Pine Creek Orogen. Subcropping. This igneous crystallisation age confirms the presence of Neoarchean felsic crystalline basement to the Palaeoproterozoic stratigraphy of the Pine Creek Orogen. An earlier U-Pb intercept age had been derived of 2675 +/- 28 Ma (Williams and Compston , 1983). This age makes it the oldest known rock in the Pine Creek Orogen, the Northern Territory and the North Australian Craton.|2674 +/- 3 Ma (Glass et al., 2010).||||Foliated and gneissic biotite granite, muscovite-biotite granite and muscovite-biotite-orthoclase granite.|
24634|Woolner Granite|69419|5|Briefly described|p4:1-2, 4, 6|Neoarchean|Neoarchean|Pine Creek Orogen. Subsurface: intersected in drill core (40-120m depth) in the Money Shoal Basin. Pronounced gravity lows. SHRIMP U-Pb zircon age; this validates the earlier determination of 2675 +/- 14 Ma (Williams and Compston, 1983), and confirms it as the oldest known rock in the NT.|2674 +/- 3 Ma (Glass et al., 2010).|||Is overlain unconformably by Dirty Water Metamorphics and Koolpinyah Dolostone.|Three granite varieties: foliated and gneissic, red-brown and grey, albitised biotite granite; grey muscovite-biotite granite; pink muscovite-biotite-orthoclase granite. Pegmatite intrusions are more common in the gneissic variety.|12-JUL-16
24634|Woolner Granite|69420|5|Briefly described|p5:4-6, 8-9, 11, 16|Archean|Archean|Part of the basement to the Central Domain of the Pine Creek Orogen. SHRIMP zircon emplacement age.|2674 +/- 3 Ma (Glass et al., 2010).|||Is overlain unconformably by Koolpinyah Dolostone.||12-JUL-16
24634|Woolner Granite|69917|4|Described|p14-15|Neoarchean|Neoarchean|Pine Creek Orogen, Central Domain. U/Pb SHRIMP zircon dating, Hf, O analytical data. Intersected in drill holes at 40-120 m depth in Woolner area. |2674.3+/-3.0 Ma ||||Foliated and gneissic biotite granite, muscovite-biotite granite (dated), and muscovite-biotite-orthoclase granite|
24634|Woolner Granite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|2674+/-3 Ma (crystallisation: U-Pb zircon SHRIMP)||||Altered pink quartz-feldspar-muscovite-biotite foliated granite.|
41833|Wuluma Suite|50369|5|Briefly described|p1.4, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Age: 1728Ma.||||||07-NOV-08
41833|Wuluma Suite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Arunta Block.|1724 +/- 6 Ma.|||||
41833|Wuluma Suite|68150|5|Briefly described|p1|||Presented in text as the Napperby, Wuluma (1726  +/-  4 Ma; Collins and Williams, 1995; Lafrance et al., 1995) and Gumtree suites. See also Wuluma Granite in this paper. Aileron Province.|1726 +/- 4 Ma||Wuluma Granite|||
41833|Wuluma Suite|69931|6|Mentioned|p269, 282-283|Paleoproterozoic|Paleoproterozoic|Arunta Inlier.|1726 +/- 4 Ma (Lafrance et al., 1995).||Wuluma Granitoid.|||
23268|Wundirgi Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Sublithic and lithic arenite, siltstone and shale: medium to thick bedded. Minor thin to medium bedded tuff; chert (silicified tuff?).||||||07-NOV-08
23268|Wundirgi Formation|23733|3|Fully described|p6, p4 Tb.1|Proterozoic|Proterozoic|Conformably overlain by Brumbreu Formation.  Age: 1829+/-8Ma and 1877(1827??)+/-9Ma (Compston, 1995).  Max. thickness: ~3000m.||||||14-NOV-06
23268|Wundirgi Formation|23809|5|Briefly described|p27 Fig. 25|||Of the Flynn Group.  Geological Province: Tennant Inlier.||||||
23268|Wundirgi Formation|24172|2|Defined|p21, p7 Tb.1|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Brumbreu Formation; conformably underlain by Warrego Volcanics. Geological Province: Tennant Creek Inlier. Max. thickness: 600-1500m. Age: 1840+/-8Ma and 1845+/-4Ma (Compston, 1994)||||||07-NOV-08
23268|Wundirgi Formation|24197|5|Briefly described|p25|Paleoproterozoic|Paleoproterozoic|Of the Treasure Suite. Geological province: Davenport Province.||||||07-FEB-11
23268|Wundirgi Formation|43223|5|Briefly described|Map Legend||Paleoproterozoic|Of the Flynn Subgroup.||||||07-NOV-08
23268|Wundirgi Formation|43751|6|Mentioned|Fig.2,p610|||||||||
23268|Wundirgi Formation|50353|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Overlain by the Brumbreu Formation. Sublithic and lithic arenite, siltstone, shale. Medium to thick bedded. Minor thin to medium bedded tuff; chert (silicified tuff?)||||||07-NOV-08
23268|Wundirgi Formation|50588|5|Briefly described|p3.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Tennant Creek/Davenport Province. Of the Treasure Suite. Age: 1829-1827 +/- 9Ma (SHRIMP).||||||14-APR-15
23268|Wundirgi Formation|60684|4|Described|p11, p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Arenites/thinsiltstone/conglom/breccia/felsic volcanics.Conformably overlain by Brumbreu Formation; disconformably/unconformably overlies Warramunga Formation. Max. thickness: ~3000m by analogy with Monument Formation.||||||07-NOV-08
23268|Wundirgi Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Ooradidgee Group. Sublithic/lithic arenite and siltstone, shale; minor tuff chert (silicified tuff).  In the Tennant Creek region.||||||07-NOV-08
23268|Wundirgi Formation|65209|5|Briefly described|p35 Fig.1, p36, p37|Paleoproterozoic|Paleoproterozoic|||Ooradidgee Group||Overlies Warrego Volcanics. Conformable and apparently transitional under Brumbreu Formation.||05-JAN-17
23268|Wundirgi Formation|65222|5|Briefly described|p123-124, 110,111,121,126,128,116 Tb 3|Paleoproterozoic|Paleoproterozoic|Flynn Subgroup, Churchills Head Group. 1920 +/- 60 Ma whole-rock Rb-Sr age may be metamorphic age? Igneous crystallisation suggested to be ~2400 Ma (Black & McCulloch, 1984).Two zircon sample localities; granite, felsic volcanics. SHRIMP ages probably represent min age for Fm. unit subjected to amphibolite-facies metamorphism in a shear zone.|1829 +/- 8 Ma; 1827 +/- 9 U/Pb SHRIMP Max [?]|Of Flynn Subgroup||Mainly amphibolite facies metasediments.|Quartzofeldspathic schist (sheared granite or felsic porphyry); moderately foliated felsic schist.|24-JAN-22
23268|Wundirgi Formation|65338|6|Mentioned|p19.|||Undated, but broadly correlated with volcanic rocks of Yungkulungu and Bernborough Formations.||||||
23268|Wundirgi Formation|65345|6|Mentioned|p11 Fig.12. |||||||||
23268|Wundirgi Formation|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Sublithic/lithic arenite and siltstone, shale; minor tuff, chert (silicified tuff).|
23268|Wundirgi Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.|1837 +/- 5 Ma.|Ooradidgee Group.||||
23268|Wundirgi Formation|69187|6|Mentioned|p53 Fig.2, p54 Fig.3|||Warramunga Province.||Ooradidgee Group||||
23268|Wundirgi Formation|69418|6|Mentioned|p3:31|||Georgina Basin. Hosts the Alexandria phosphate deposit (briefly described).||||||12-JUL-16
23268|Wundirgi Formation|69424|4|Described|p9:3-5, 15-17, 19-20, 22, 26-29, 53-54|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Warramunga Province. Thickness probably 600-1500m; c.3000m by analogy with Monument Formation; base not exposed. Predominantly subaqueous (deep-water marine to littoral), with minor subaerial surge and fall deposits. Associated with two Au-bearing vein quartz deposits: Last Hope and Bull Pup mines. Minimum age from sheared intrusive porphyry or granite. Lateral equivalent to all or part of Warrego Volcanics and Monument, Bernborough and Yungkulungu Formations.|>1829 +/- 8 Ma (Compston, 1995).|Ooradidgee Group.||Conformably overlies Warrego Volcanics. Is overlain conformably and transitionally by Brumbreu Formation. Is intruded by Devils Suite.|Fine- to coarse-grained, and thinly to medium bedded sublithic/lithic sandstone; thinly bedded siltstone; minor conglomerate and breccia; felsic volcanic rocks.|12-JUL-16
23268|Wundirgi Formation|69431|5|Briefly described|p16:14, 22|||Warramunga Province. Folding during the Davenport Event is discussed. Is intruded by dolerite, near the Last Hope Mine (immediately S of Tomkinson Province), aged 1821 +/- 8 Ma (Compston, 1994).||Ooradidgee Group.||||12-JUL-16
23268|Wundirgi Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1827+/-9 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite; quartzofeldspathic schist (sheared granite or felsic porphyry); felsic schist (originally grano felsic volcanic).|
23268|Wundirgi Formation|72379|5|Briefly described|p4-5|Paleoproterozoic|Paleoproterozoic|Geological province:Warramunga Province. Minimum depositional age constrained by monzodiorite intrusion dated at 1821+\-8 Ma (SHRIMP U-Pb; Compston 1995).  Intruded by sills and small plutons of monzonite, quartz monzonite and quartz diorite (Donnellan 2001, Donnellan 2013a). DDH1 drillhole (EXP027, BMR) intersected mineralisation at the Explorer 27 prospect in central eastern SHORT RANGE, Tennant Creek mineral field. Two samples of a chalcopyrite-molybdenite-pyrite-bearing quartz vein returned Re-Os model ages (ID-NTIMS molybdenite) of 1711+\-8 Ma (Sample TC18MVM001) and 1719+\-8 Ma (Sample TC18MVM001). The c. 1719-1711 Ma model ages constrain absolute timing for copper-molybdenum mineralisation at Explorer 27, and represent the first time Cu mineralisation of this age has been reported from the Tennant Creek mineral field.||Unit of Ooradidgee Group.|||Arenite, siltstone, shale and tuff.|
23268|Wundirgi Formation|73124|6|Mentioned|p2 Fig.1|||||Ooradidgee Group||Overlain by Brumbreu Formation. Equivalent to Bernborough Formation and Monument Formation.||
23268|Wundirgi Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province.||Ooradidgee Group.||||
23268|Wundirgi Formation|73460|6|Mentioned|p2|||Warramunga Province.||Ooradidgee Group||Overlain by Brumbreu Formation. Equivalent to Bernborough Formation and Monument Formation.||
23268|Wundirgi Formation|73590|6|Mentioned|p2|||||Ooradidgee Group||Overlain by Brumbreu Formation. Equivalent to Bernborough Formation and Monument Formation.||
27950|Wununmantyala Sandstone|22538|6|Mentioned|P714||Statherian|||||||
27950|Wununmantyala Sandstone|22670|6|Mentioned|52,55|||Geological province: McArthur Basin.||||||20-DEC-06
27950|Wununmantyala Sandstone|22853|3|Fully described|12|Proterozoic|Proterozoic|Geological province: McArthur Basin. Of the Tawallah Group. Max thickness: 520 m. Overlain by Settlement Creek Volcanics; underlain by Aquarium Formation.||||||20-DEC-06
27950|Wununmantyala Sandstone|23395|5|Briefly described|p388|||||||||
27950|Wununmantyala Sandstone|23396|5|Briefly described|p407 Fig.2|||Of the Tawallah Group.||||||20-DEC-06
27950|Wununmantyala Sandstone|23397|6|Mentioned|p480|||||||||
27950|Wununmantyala Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Tawallah Group.  Geological Province: MacArthur Basin.||||||
27950|Wununmantyala Sandstone|23776|5|Briefly described|p705 Fig 2.|||Of Tawallah Group.||||||
27950|Wununmantyala Sandstone|23867|5|Briefly described|Fig. 30|||Of Tawallah Group.  Correlates with Shadforth Sandstone (Katherine River Group).  Geological Province: McArthur Basin.  See also p16.||||||
27950|Wununmantyala Sandstone|23910|5|Briefly described|p292 Fig. 3|||Of Tawallah Group.  Geological Province: McArthur Basin.||||||
27950|Wununmantyala Sandstone|23963|5|Briefly described|p1239 Fig.2|||Geological Province: McArthur Basin. Of the Tawallah Group.||||||
27950|Wununmantyala Sandstone|24048|5|Briefly described|p36|||Of the Tawallah Group.||||||20-DEC-06
27950|Wununmantyala Sandstone|24050|6|Mentioned|p21|||Geological Province: McArthur Basin.||||||
27950|Wununmantyala Sandstone|40691|6|Mentioned|Fig.4|||||||||
27950|Wununmantyala Sandstone|42385|3|Fully described|p12, p8 Fig. 5, p9 Tb. 3|Mesoproterozoic|Mesoproterozoic|Of the Tawallah Group. Conformably overlies Aquarium Fm; conformably overlain by Settlement Creek Volcanics. Thickness: <520m. Red to mauve-grey, locally feldspathic sandstone, mainly med-grained, moderately to well sorted, thin- to med.- bedded.||||||18-SEP-07
27950|Wununmantyala Sandstone|42386|5|Briefly described|Map legend|Mesoproterozoic||||||||
27950|Wununmantyala Sandstone|42638|5|Briefly described|Map legend|Mesoproterozoic||Age: Middle Proterozoic.||Of Tawallah Group.||In schematic section, underlies Masterton Sandstone (Umbolooga Subgroup); overlies Aquarium Formation.|Feldspathic sandstone; shale interbeds. Detailed lithology given.|11-NOV-11
27950|Wununmantyala Sandstone|42639|3|Fully described|p12, Table 4 p11|||||||||
27950|Wununmantyala Sandstone|42700|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
27950|Wununmantyala Sandstone|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Tawallah Group. Quartzarenite and sublitharenite, red-brown to purple, hematitic, mainly medium grained.||||||19-OCT-05
27950|Wununmantyala Sandstone|42812|3|Fully described|p20, Table 3|||Of the Tawallah Group.||||||20-DEC-06
27950|Wununmantyala Sandstone|43010|5|Briefly described|Fig.6||Mesoproterozoic|Of the Tawallah Group. Of "Mid Proterozic" age..||||||20-DEC-06
27950|Wununmantyala Sandstone|43036|3|Fully described|p24|||Of the Tawallah Group.||||||20-DEC-06
27950|Wununmantyala Sandstone|44112|6|Mentioned|p43,49|||||||||
27950|Wununmantyala Sandstone|45162|2|Defined|p30|||||||||
27950|Wununmantyala Sandstone|60483|5|Briefly described|p7 Fig. 5, p29|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
27950|Wununmantyala Sandstone|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Tawallah Group. Includes Wuraliwuntya Member. Overlain by Settlement Creek Volcanics, underlain by Aquarium Formation.||||||
27950|Wununmantyala Sandstone|62084|6|Mentioned|p936 Fig.5|||Calvert Superbasin. Shown as Wununmantyala Sst.||||||
27950|Wununmantyala Sandstone|63112|6|Mentioned|p1191 Fig.2,p1192,p1194-1198,p1200-1205 |||Calvert Superbasin. Age approximated from Fig.2. 200-520 m thick.|c.1730 Ma.|Unit in Big Supersequence.|||Mudstone, stromatolitic dolostone, fine-grained glauconitic sandstone, coarse-grained lithic sandstone, dolomitic-glauconitic-micaceous sandstone, and a thick upper section of fine- to medium-grained commonly silicified quartzose sandstone.|
27950|Wununmantyala Sandstone|63866|5|Briefly described|p54|||||Prize Supersequence||||
27950|Wununmantyala Sandstone|64815|6|Mentioned|p4 Fig.2, p5 Fig.3|||||Of the Tawallah Group.||||
27950|Wununmantyala Sandstone|64817|6|Mentioned|p353 Fig.4, p355 Fig.5, p367 Tb.2|||See also p369, p370, p376. This unit is coeval with the initiation of collision in the Strangways arc at 1745-1730 Ma.||Of the Tawallah Group.|Includes Wuraliwuntya Member.|||
27950|Wununmantyala Sandstone|65228|4|Described|p21, Figs.02, 05, 06, 07, 10.|Statherian|Statherian|Mis-spelt as Wunnunmantyala on p21. The base of this unit is the boundary of the Calvert Superbasin. Fig. 02 implies that this unit's Wuraliwuntya Member is/should become a separate Formation, equivalent to Aquarium Formation.|c.1730 Ma.|Unit in Tawallah Group.|Includes Wuraliwuntya Member.|Overlies McDermott Formation and Rosie Creek Sandstone Member (Sly Creek Sandstone). Is overlain by Aquarium Formation.|Quartz arenite to sub-litharenite.|
27950|Wununmantyala Sandstone|65337|6|Mentioned|p14. |||Southern McArthur Basin. This unit's 'redbeds' resemble part of the upper section of the Gator Sandstone.||||||
27950|Wununmantyala Sandstone|65340|4|Described|p12 Fig.6, p13, 14, 16, 18, 68, 84, 92.|||Revised in this study. A 200 - 300 m thick sheet of sandstone. Mixed braidplain-inner shelf environment. Defined by Jackson et al. (1987) and Pietsch et al. (1991a); rocks  underlying the Aquarium Formation throughout the Wearyan Shelf, have been reassigned from the Sly Creek Sandstone, to Wununmantyala Sst (Jackson et al. 2000a). Only occurs in the subsurface in this map area.||Unit in Tawallah Group.|Includes Wuraliwuntya Member.|Disconformably overlies McDermott Formation. Is overlain by Aquarium Formation and Settlement Creek Dolerite.|Medium-grained quartz sandstone.|23-MAR-18
27950|Wununmantyala Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot; p33|||McArthur Basin.|~1740 Ma.||||Arenite.|
27950|Wununmantyala Sandstone|67352|5|Briefly described|p14 Tb.2|||[It is overlain by Masterton Sandstone which has now been defined (database) as part of it].||||Overlain by Masterton Sandstone (unconformably) or Wollogorang Formation (conformably).||
27950|Wununmantyala Sandstone|69430|4|Described|p15:3, 10-12|||Defined by Pietsch et al. (1991) to replace the previous definition of the Sly Creek Sandstone, which now has a more restricted application. Southern McArthur Basin. Up to 800m thick. Storm-dominated subtidal marine to very shallow-marine deposits, occasionally exposed.||Tawallah Group.|Wuraliwuntya Member.|Conformably overlies McDermott Formation and has a gradational contact with Aquarium Formation. Is overlain by the intrusive Settlement Creek Dolerite.|Red-brown to purple, haematitic, mainly medium-grained laminated quartzarenite and sublitharenite.|12-JUL-16
27950|Wununmantyala Sandstone|69673|6|Mentioned|p16 fig 13, p17 fig 14|||Coarse clastic sedimentary rock.||Tawallah Group|Includes Wuraliwuntya Member|Overlain by Settlement Creek Dolerite, disconformably overlies McDermott Formation||
27950|Wununmantyala Sandstone|71374|6|Mentioned|p6|||McArthur Basin.||Tawallah Group||Unconformably overlain by the Masterton Sandstone.||
27950|Wununmantyala Sandstone|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Tawallah Group.||||
27950|Wununmantyala 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|Probably includes Wuraliwuntya Member.|Overlies McDermott Formation and underlies and is partially laterally equivalent to Wuraliwuntya Member and Aquarium Formation and underlies Settlement Creek Dolorite.||
27950|Wununmantyala Sandstone|72718|6|Mentioned|p7|||Southern McArthur Basin.||Tawallah Group|Wuraliwuntya Member?|Underlain by McDermott Formation. Partly overlain by Settlement Creek Dolerite and Aquarium Formation.||
27950|Wununmantyala 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|Includes Wuraliwuntya Member.|Overlies McDermott Formation and underlies Settlement Creek Dolorite, Aquarium Formation.||
27950|Wununmantyala Sandstone|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Tawallah Group|Wuraliwuntya Member|Underlain by McDermott Formation. Partly overlain by Settlement Creek Dolorite. Partly overlain by and equivalent to Aquarium Formation.||
27950|Wununmantyala Sandstone|73412|5|Briefly described|p2, 4, 8-9, 12, 14|||Southern McArthur Basin. Overlies a regional unconformity. Non-magnetic.||Tawallah Group.||Unconformably overlies McDermott Formation. Is overlain by Aquarium Formation and Settlement Creek Dolerite.||
29229|Wuraliwuntya Member|22538|5|Briefly described|Fig3 P709|||||||||23-MAR-18
29229|Wuraliwuntya Member|22670|6|Mentioned|53|||Geological province: McArthur Basin. Of the Wununmantyala Sandstone.||||||20-DEC-06
29229|Wuraliwuntya Member|23395|5|Briefly described|p388|||Of the Wununmantyala Sandstone.||||||20-DEC-06
29229|Wuraliwuntya Member|23776|5|Briefly described|p705 Fig 2.|||Of the Tawallah Group.||||||20-DEC-06
29229|Wuraliwuntya Member|42385|6|Mentioned|Fig.5 p8|||||||||23-MAR-18
29229|Wuraliwuntya Member|42739|5|Briefly described|map legend|Statherian|Statherian|Of the Wununmantyala Sandstone. Fine-grained and rarely medium grained sandstone and mudstone; mottled brown to fawn, very thin to medium bedded, typically flaggy.||||||19-OCT-05
29229|Wuraliwuntya Member|42812|2|Defined|p81|Proterozoic||Age: between 1851 +/- 7Ma and 1713 +/- 6Ma. Of the Wununmantyala Sandstone.||||||20-DEC-06
29229|Wuraliwuntya Member|43036|3|Fully described|p26|||Of the Wununmantyala Sandstone.||||||19-DEC-13
29229|Wuraliwuntya Member|60483|5|Briefly described|p7 Fig. 5|||Of the Tawallah Group. Geological Province: McArthur Basin.||||||05-OCT-07
29229|Wuraliwuntya Member|60558|5|Briefly described|p8 Fig. 6|Proterozoic|Proterozoic|Of Wununmantyala Sandstone.||||||03-JUN-09
29229|Wuraliwuntya Member|63112|6|Mentioned|p1191 Fig.2, p1192 and Tb.1|||Calvert Superbasin. Mis-spelt as Wurilawantya in Fig.2. Age approximated from Fig.2. Its position in Tb.1 implies it is a Member of Aquarium Formation.|c.1730 Ma.|Unit in Big Supersequence.||||
29229|Wuraliwuntya Member|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||||Unit in Wununmantyala Sandstone.||||
29229|Wuraliwuntya Member|65228|5|Briefly described|Figs.02, 05, 07.|||[Of Wununmantyala Sandstone]. Fig. 02 implies that this unit is/should become a separate Formation, equivalent to Aquarium Formation.||Unit in Wununmantyala Sandstone.||Is overlain by Settlement Creek Volcanics.||
29229|Wuraliwuntya Member|65340|6|Mentioned|p12 Fig.6, p.16, p18, p92.|||Correlated with Aquarium Formation.||Unit in Wununmantyala Sandstone.||||23-MAR-18
29229|Wuraliwuntya Member|69430|6|Mentioned|p15:3|||Southern McArthur Basin.||Wununmantyala Sandstone.||||12-JUL-16
29229|Wuraliwuntya Member|69673|5|Briefly described|p16 fig 13, p17 fig 14|||||Wununmantyala Sandstone||Overlain by Settlement Creek Dolerite, Correlated with Aquarium Formation|Mixed sandstone and shale.|
29229|Wuraliwuntya Member|72526|5|Briefly described|p8 Fig.1.3.|Statherian|Statherian|Shown as located in the northern part of the Batten Fault Zone.||Shown as part of Wununmantyala Sandstone||Overlies and is partially equivalent to Wununmantyala Sandstone and underlies Settlement Creek Dolorite.||
29229|Wuraliwuntya Member|72718|6|Mentioned|p7|||Southern McArthur Basin.||Wununmantyala Sandstone?, Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolerite. Equivalent to Aquarium Formation.||
29229|Wuraliwuntya Member|72912|5|Briefly described|p5 Fig.3.|Statherian|Statherian|Located in the north of the Batten Fault Zone.||Wununmantyala Sandstone, Tawallah Group||Underlies Settlement Creek Dolorite.||
29229|Wuraliwuntya Member|73042|6|Mentioned|p4|Paleoproterozoic|Paleoproterozoic|Southern McArthur Basin, Calvert Superbasin.||Wununmantyala Sandstone, Tawallah Group||Underlain by and equivalent to Wununmantyala Sandstone. Overlain by Settlement Creek Dolorite.||
24126|Wurugoij Dolerite|9534|5|Briefly described|Map legend|Adelaidean|Adelaidean|Ophitic dolerite.||||||
24126|Wurugoij Dolerite|9691|5|Briefly described|Map Legend|||Ophitic dolerite.||||||
24126|Wurugoij Dolerite|9701|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Ophitic dolerite.||||||02-JUN-05
24126|Wurugoij Dolerite|9733|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Ophitic dolerite.||||||
24126|Wurugoij Dolerite|23374|6|Mentioned|p19||Statherian|Now considered to be part of Oenpelli Dolerite. In the McArthur Basin.||||||20-DEC-06
24126|Wurugoij Dolerite|24050|5|Briefly described|p30|Mesoproterozoic||||||||
24126|Wurugoij Dolerite|36535|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24126|Wurugoij Dolerite|36635|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24126|Wurugoij Dolerite|37815|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
24126|Wurugoij Dolerite|39048|6|Mentioned|p825|||||||||
24126|Wurugoij Dolerite|39679|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24126|Wurugoij Dolerite|43187|5|Briefly described|p2|||||||||
24126|Wurugoij Dolerite|43624|6|Mentioned|Fig.32,p38|||Age: 1200 Ma||||||
24126|Wurugoij Dolerite|46639|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Age: ~1200Ma.  Medium quartz and olivine diorite.||||||
24126|Wurugoij Dolerite|60550|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Ophitic dolerite.||||||
80428|Wyworrie Member|71779|2|Defined|iii, p2-p4, p7, p9, p16-20, 26-27, 2319|Mesoproterozoic|Mesoproterozoic|McArthur Basin. Name proposed by TJ Munson and D Revie. Named for the Wyworrie Station in northern central LARRIMAH. The type section is in POG Alexander 1 drillhole from ca 280m depth to ca 62m. Intersected in numerous drillholes, the mapsheets in which this unit is intersected are provided. Corresponds to the now obsolete upper Velkerri Formation of previous usage. Not recognised at the surface due to generally poor outcrop of this unit and its parent the Velkerri Formation. Distinguished from the Amungee Member by generally lower (poor to good) TOC values, geochemistry, geophysical logs; these distinguishing features are discussed in some detail. Thickness in various drillholes provided. Deposited in a subtidal, sub-wave base and generally quiet marine depositional environment. See also p10, 11, p12 fig 9, p13-p20, p23, 25.||Velkerri Formation||Conformably overlies the Amungee Member. Conformably overlain by the Moroak Sandstone.|Alternating, interbedded and interlaminated mudstone and siltstone, and lesser fine-grained sandstone which increases in proportion towards the top.|24-SEP-18
80428|Wyworrie Member|71893|4|Described|p17, p20, p25, p37, p40|Ectasian|Ectasian|Equivalent to the informal "Upper" Velkerri Formation of Lanigan et al (1994) and upper Velkerri Formation of subsequent usage.|1361 +/- 21 Ma (Re-Os)|Velkerri Formation||Overlies the Crawford Formation.||
80428|Wyworrie Member|72381|5|Briefly described|p776|Mesoproterozoic|Mesoproterozoic|Of Beetaloo Sub-basin, McArthur Basin. Characterised by dominant peak at c. 1600 Ma and 2 minor peaks at c. 1820 and c. 1690 Ma (Fanning 2012; Yang et al. 2018) which may suggest an overall provenance from the Eastern Fold Belt (Mount Isa Province; Griffin et al. 2006), or 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 Velkerri Formation.||Uppermost unit of Velkerri Formation. Overlain by Moroak Sandstone. Underlain by Amungee Member.||
80428|Wyworrie Member|73242|5|Briefly described|p39|||||Velkerri Formation, Maiwok Subgroup, Roper Group||Underlain by Amungee Member. Overlain by Moroak Sandstone.|Includes interbedded mudstone and fine sandstone.|
80428|Wyworrie Member|73280|6|Mentioned|p1, p4-5, App.1A|||McArthur Basin +/- Beetaloo Sub-basin. Sampled for XRD mineralogy to investigate brittleness and Kubler indices [see report].||Velkerri Formation||||
80335|Xanten Granodiorite|71621|4|Described|iii, p1, p30-p32|Statherian|Statherian|Aileron Province. ICPMS age is interpreted as the magmatic crystallisation age for this granite. Formerly the Xanten Granite of Freeman, 1986. Potentially isotopically reset at ca 501 +/- 12  Ma. Possesses a juvenilte Hf signature. Referred to as the Xanten Granite on p iii. Said to have an unconformable contact with the Grant Bluff and Elkera formations [although the exact nature of these contacts is not provided]. Petrography and zircon description discussed.|1777 +/- 8 Ma (LAICPMS)|||Intrudes the Bonya Metamorphics.|Fine- to medium-grained leucocratic granodiorite.|01-FEB-19
80335|Xanten Granodiorite|72515|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Jervois Range Special Map Sheet. Aileron Province.|1777 +/- 8 Ma (U-Pb zircon)|Casper Suite|||Granodiorite to tonalite: fine to medium-grained, equigranular, leucocratic with rare biotite and muscovite; strongly weathered and altered, moderately foliated, locally gneissic.|
80335|Xanten Granodiorite|72516|1|Redefined|p16, p19-21, p29, p35, p211|Statherian|Statherian|Defined by Shaw et al (1985) as Xanten Granite and named after the Xanten copper prospect; the type locality was defined as roughly 12km to the northwest of the main occurence (611905mE 7491646mN). It is redefined here as a granodiorite to reflect the dominant lithology. The type location is here defined as 622232mE 748748mN. Petrography, geophysics and geochemsitry are discussed. Weathering is characterised by orange-brown weathering surface. Forms low blocky hills that are largely devoid of vegetation. Unconformity and fault contact with Grant Bluff and Elkera Formations. SHRIMP age is interpreted as the age of magmatic crystallisation. See also p46-48, p95, p106, p109, p111, p123-124, p135-137, p171, p189, p192, p211, p218.|1777 +/- 8 Ma (SHRIMP Pb-Pb, Beyer et al, 2018)|Casper Suite||Intrudes the Bonya Metamorphics. Coeval with the Jervois Granodiorite. Unconformably overlain by the Grant Bluff Formation and the Elkera Formation.|Granodiorite to tonalite: fine to medium-grained, equigranular, leucocratic with rare biotite and muscovite; strongly weathered and altered (silicified); moderately foliated, locally gneissic.|04-JUL-22
24590|Yaddanilla Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of the Hanlon Subgroup (Hatches Creek Group).||||||
24590|Yaddanilla Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Hanlon Subgroup (Hatches Creek Group).  Geological Province: Davenport Province.||||||
24590|Yaddanilla Sandstone|23823|5|Briefly described|p75|Paleoproterozoic|Paleoproterozoic|Of the Hatches Creek Group (upper). Ridge-forming sandstone. Max. thickness:~700m.  Geological Province: Davenport Geosyncline.||||||07-FEB-11
24590|Yaddanilla Sandstone|39624|5|Briefly described|Table 1|||||||||
24590|Yaddanilla Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24590|Yaddanilla Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup. Quartz arenite and feldspathic arenite. Geological Province: Tennant Creek Block.||||||07-NOV-08
24590|Yaddanilla Sandstone|41129|4|Described|Table 1|||||||||
24590|Yaddanilla Sandstone|41308|5|Briefly described|Table 2|||||||||
24590|Yaddanilla Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24590|Yaddanilla Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24590|Yaddanilla Sandstone|42643|5|Briefly described|p12|||Of the Hanlon Subgroup.||||||20-DEC-06
24590|Yaddanilla Sandstone|45167|3|Fully described|Table 1|||Of the Hanlon Subgroup.||||||20-DEC-06
24590|Yaddanilla Sandstone|49033|2|Defined|p30|Proterozoic|Proterozoic|||||||
24590|Yaddanilla Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Hanlon Subgroup (Hatches Creek Group). Quartz arenite, feldspathic/sublithic arenite. Overlies Vaddingilla Formation. In the Tennant Creek region.||||||07-NOV-08
24590|Yaddanilla Sandstone|64735|5|Briefly described|p206 Fig 2, p214,|Orosirian|Orosirian|||Of Hanlon Subgroup, Hatches Creek Group.||Overlies Vaddingilla Sandstone.||30-APR-12
24590|Yaddanilla Sandstone|65209|6|Mentioned|p35 Fig.1|Paleoproterozoic|Paleoproterozoic|||Hanlon Subgroup||||
24590|Yaddanilla Sandstone|65338|6|Mentioned|p20.|||||Unit in Hanlon Subgroup.||||
24590|Yaddanilla Sandstone|67148|5|Briefly described|Map legend.|Statherian|Statherian|||Unit in Hanlon Subgroup, Hatches Creek Group.||Overlies Vaddingilla Formation.|Quartz arenite and feldspathic arenite.|19-OCT-11
24590|Yaddanilla Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Vaddingilla Formation.|Quartz arenite, feldspathic/sublithic arenite.|
24590|Yaddanilla Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24590|Yaddanilla Sandstone|67352|4|Described|p9 Tb.1, p44 Fig.48|Statherian|Statherian|Crops out as ridge-forming, with recessive concealed interbeds. Over 1000 m thick.||Hanlon Subgroup||Overlies Vaddingilla Formation (conformably).|Quartz arenite and feldspathic arenite: fine-to medium-grained, thin to medium bedded.|
24590|Yaddanilla Sandstone|69425|5|Briefly described|p10:3, 10-12, 19-20|Statherian|Statherian|NE Davenport Province. Forms low ridges. ?1000m thick. Shallow-marine shelf deposits.||Topmost unit in Hanlon Subgroup.||Conformably overlies Vaddingilla Formation. Is partly correlative with Bootu Formation.|Quartz sandstone and feldspathic/lithic sandstone; mudstone pellets on some bedding planes.|12-JUL-16
24590|Yaddanilla Sandstone|69431|6|Mentioned|p16:5|||Davenport Province.||Hanlon Subgroup.||||12-JUL-16
24592|Yakalibadgi Microgranite|23270|5|Briefly described|Table 1, p5||Proterozoic|In the Arunta Block.||||||20-DEC-06
24592|Yakalibadgi Microgranite|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||20-DEC-06
24592|Yakalibadgi Microgranite|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Napperby Suite. Age: ~1775Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
24592|Yakalibadgi Microgranite|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
24592|Yakalibadgi Microgranite|39888|6|Mentioned|Fig.8|||||||||
24592|Yakalibadgi Microgranite|42146|6|Mentioned|p652|||||||||
24592|Yakalibadgi Microgranite|42217|5|Briefly described|p412|||||||||
24592|Yakalibadgi Microgranite|48992|2|Defined|p60|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
24592|Yakalibadgi Microgranite|50369|5|Briefly described|p1.3, 7.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Napperby Suite.||||||07-NOV-08
24592|Yakalibadgi Microgranite|69427|5|Briefly described|p12:26, 30, 32|Statherian|Statherian|Stewart et al. (1980). NW Reynolds Range, Aileron Province. Appears to have been emplaced along the contact with the Mount Thomas Quartzite.|1780-1770 Ma.|||Intrudes Lander Rock Formation.|Medium-grained granite and microgranite that grades into micaceous orthoschist.|12-JUL-16
24592|Yakalibadgi Microgranite|71858|6|Mentioned|p5|||Aileron Province. One of a group of 1780- 1770 granites.||||||
31339|Yaloolgarrie Granite|24197|5|Briefly described|p61 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Southwark Suite (or Southwark Granite Suite?). Age: 1567Ma by correlation with Yarunganyi Granite date. Geological Province: Arunta Inlier.||||||07-FEB-11
31339|Yaloolgarrie Granite|24540|6|Mentioned|p8|||This is Wangala Granite mapped by Young et al (1995) as Yaloolgarrie Granite - at MOUNT DOREEN.||||||07-FEB-11
31339|Yaloolgarrie Granite|43275|5|Briefly described|Map Legend||Mesoproterozoic|Misspelling of reserved name Yaloogarrie Granite - correct place name is Yaloogarrie.||||||20-DEC-06
31339|Yaloolgarrie Granite|50369|5|Briefly described|p1.5, 24.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Southwark Suite.||||||07-NOV-08
31339|Yaloolgarrie Granite|65329|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as Wabudali Granite age, older than Southwark Granite Suite, younger than Andrew Young Igneous Complex. Megacrystic muscovite-biotite granite with pegmatite, aplite and quartz-tourmaline segregations, weakly foliated; low gravity response; variable magnetic response||||||27-OCT-10
31339|Yaloolgarrie Granite|65330|5|Briefly described|Map legend|Palaeoproterozoic|Palaeoproterozoic|Shown as older than Southwark Granite Suite, younger than Andrew Young Igneous Complex. Megacrystic muscovite-biotite granite with pegmatite, aplite and quartz-tourmaline segregations, weakly foliated; low gravity response; variable magnetic response||||||
31339|Yaloolgarrie Granite|69427|5|Briefly described|p12:33, 41|||Young et al. (1995). Eastern MOUNT DOREEN map area. This granite is part of the Wangala Granite [and is therefore obsolete?]. Associated with Cu-Pb-Zn-Ag mineralisation in greisen veins at the Silver King prospect. May be similar in age to Wabudali Granite.||||Intrudes Lander Rock Formation.|Weakly foliated porphyritic biotite-muscovite granite with tabular K-feldspar phenocrysts.|12-JUL-16
31339|Yaloolgarrie Granite|72376|5|Briefly described|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Aileron Province. Outcrops ~8km SSW of Wilfram Hill tungsten-copper deposit. Scrimgeour (2013) speculated that the granite is likely to have a c. 1730-1710 Ma crystallisation age. Aplite dyke at the Silver King Cu-Pb-Zn-Ag prospect (central MOUNT DOREEN mapsheet) is inferred to be related to Yaloolgarrie Granite ands its emanating aplite dykes (based on similar mineralogy and structural trends), and is dated at 1763+\-9 Ma (207Pb/206Pb magmatic crystallisation; Kositcin et al., 2018).|||||Megacrystic muscovite-biotite granite.|
34018|Yalwarra Volcanics|22538|6|Mentioned|P718|||||||||
34018|Yalwarra Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
34018|Yalwarra Volcanics|23937|2|Defined|p97 App. 1|Calymmian|Statherian|Supersedes Yalwarra Volcanic Member (Kookaburra Creek Fm) of Dunn (1963c). Of the Nathan Group. Max. thickness: 115m. Conformably overlain by Walmudga Formation; conformably overlies Knuckey Formation.  Geological Province: McArthur Basin.||||||18-APR-05
34018|Yalwarra Volcanics|61390|5|Briefly described|Map Legend|Calymmian|Statherian|Of the Nathan Group. Basalt: commonly amygdaloidal or vesicular, locally containing xenoliths.||||||
34018|Yalwarra Volcanics|63866|6|Mentioned|p117|||||||||
34018|Yalwarra Volcanics|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region.||Nathan Group.||||
34018|Yalwarra Volcanics|69430|4|Described|p15:3, 24-25, 30|||Abbott et al. (2001); formerly included within Balbirini Dolostone (Jackson et al., 1987). Urapunga Fault Zone, McArthur Basin. Localised vulcanism; basaltic activity is not known elsewhere in the Basin. 80-115m thick. Lacustrine or marine shoreline sediments within a lava-dominated terrain.||Nathan Group.||Conformably overlies Knuckey Formation. Is overlain conformably and gradationally by Walmudga Formation.|Basalt, peperite, volcanigenic sandstone with interbedded oolitic chert at the top, and conglomerate; minor siltstone.|12-JUL-16
34018|Yalwarra Volcanics|69673|6|Mentioned|p16 fig 13|Paleoproterozoic|Paleoproterozoic|Urapunga Fault Zone||Nathan Group||Overlain by Walmudga Formation, overlies Knuckey Formation||
34018|Yalwarra Volcanics|71632|5|Briefly described|Map legend.|||McArthur Basin.||Nathan Group.|||Synsedimentary basaltic sills, sandstone, mudstone.|
34018|Yalwarra Volcanics|72373|5|Briefly described|p33|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin.|||Underlain by Knuckey Formation.|||
34018|Yalwarra Volcanics|72526|5|Briefly described|p8 Fig.1.3.|Calymmian|Calymmian|Shown as being located in the Urapunga Fault Zone in the Southern McArthur Basin.||Nathan Group||Overlies Knuckey Formation and underlies Walmudga Formation.||
34018|Yalwarra Volcanics|72718|6|Mentioned|p7|||Southern McArthur Basin. Urapunga Fault Zone.||Nathan Group||Underlain by Knuckey Formation. Overlain by Walmudga Formation.||
34018|Yalwarra Volcanics|72912|5|Briefly described|p5 Fig.3.|Calymmian|Calymmian|Located in the Urapunga Fault Zone.||Nathan Group||Overlies Knuckey Formation and underlies Walmudga Formation and is partially equivalent to Balbirini Dolostone.||
34018|Yalwarra Volcanics|73042|6|Mentioned|p4|Mesoproterozoic|Paleoproterozoic|Southern McArthur Basin, Isa Superbasin.||Nathan Group||Underlain by Knuckey Formation. Overlain by Walmudga Formation.||
82949|Yam Gneiss|73123|4|Described|piii, p1, p10-12, Fig.A3, Tb.A3|Statherian|Orosirian|Aileron Province, northeastern. Geochron is an interpreted magmatic crystallisation age of protolith. Zircon rims record interpreted metamorphism at 1736 +/- 6 Ma. Dated sample: GA sample No = 6619620, NTGS sample ID = HU15BLR872. Jinka 1:100 000 mapsheet. Indeterminate, probably igneous protolith. Hosted in the Deep Bore Domain. [Article includes outcrop, thin section and zircon descriptions].|1797 +/- 7 Ma SHRIMP U-Pb|||Intruded by dykes of the Marshall Granite.|Strongly weathered, biotite-bearing quartzofeldspathic gneiss.|
82949|Yam Gneiss|73128|5|Briefly described|p5, p8|Statherian|Orosirian|Present as surface outcrop at Molyhil tungsten-molybdenum deposit, Jinka 1:100 000 map sheet. Can include xenoliths of the Deep Bore Metamorphics and can constitute xenoliths within the Marshall Granite.|1797 +/- 7 Ma|||Intrudes Deep Bore Metamorphics. Intruded by Marshall Granite.||
82949|Yam Gneiss|73551|5|Briefly described|piii, p11-12, p14-15|Statherian|Orosirian|Interpreted as the host rock for the Molyhil W-Mo deposit. Experienced long-lived metamorphism during the Palaeoproterozoic, with supersolidus metamorphism observed until at least ca 1.72 Ga.|ca 1.80 Ga|||Intrudes the Deep Bore Metamorphics. Intruded by Marshall Granite.||
82949|Yam Gneiss|73591|6|Mentioned|p40|||||||||
79100|Yambla Gneiss|68997|4|Described|vii-viii,p1,54-58|Statherian|Statherian|Thickness: 400m. Metamorphosed to granulite-facies. Part of the Harts Range Metamorphic Complex in northwestern ILLOGWA CREEK. Sample: IC09LJH778. Grid Reference (MGA94 Zone 53): 512900mE 7432142mN. Zircon age spectra from pelitic migmatite dominated by 1825-1700 Ma material with little older source input. Also contains youngers detrital zircon component at 1679+\-15 Ma, representing maximum depositional age of its sedimentary precursor. Metamorphic zircon rims at 461+\-5 Ma represent Ordovician Larapinta Event.|1679+\-15 Ma (max dep age: U-Pb zircon)|Unit of Harts Range Metamorphic Complex.|||Pelitic migmatites.|
79100|Yambla Gneiss|69510|6|Mentioned|p17|||The 480-460 Ma Larapinta Event is recognised in pelitic migmatite in this unit.||||||
79100|Yambla Gneiss|69917|4|Described|p110-113,175-178,180-182,169,170,189,190|Ordovician|Neoproterozoic|Central and Eastern Arunta Regions, Irindina Province.  U/Pb LA-ICPMS zircon dating, Hf analytical data. 3 samples. Previously 'lower Irindina Gneiss'. 1727+/-13 Ma is conservative estimate of maximum 207Pb/206Pb depositional age, but age constraints from underlying units and correlatives indicate deposition after ca 1100 Ma.  Metamorphism during the late phase of the Ordovician Larapinta Event, at 456+/- 6 Ma is also recorded.|post 1100 Ma|Of Harts Range Metamorphic Complex.||Intruded by Lloyd Gabbronorite, Log Cabin Granite. Intruded by and interlayered with Riddock Amphibolite.Interlayered with Leprechaun Gneiss, Entire Gneiss.Overlies Last Hope Gneiss, Stanovos Gneiss.|Transitional granulite-facies metasedimentary rocks with interlayered meta-mafic igneous rocks;  interlayered mafic and felsic orthogneisses and some marble.|
79100|Yambla Gneiss|70809|5|Briefly described|iv, p1, p27-p28|||Irindina Province. Metamorphism dated by monazite growth at 456 +/- 8 Ma via LAICPMS.  Monazite geochronology and petrographic descriptions of dated samples are discussed.|||||Quartz-K-feldspar-plagioclase-biotite-muscovite gneiss.|
79100|Yambla Gneiss|71592|5|Briefly described|Appendix A.|||Arunta Orogen. Metamorphosed at 461 +/- 5 Ma.|1679+/-15 Ma (MDA: SHRIMP U-Pb zircon).||||Migmatite.|
79100|Yambla Gneiss|71621|4|Described|iii, p1, p47-p52||Statherian|Irindina Province. ICPMS age is interpreted as the maximum depositional age of the precursor to the gneiss although the actual age of deposition is likely to be considerably younger. An age of 376 +/-54 Ma is interpreted as isotopic resetting during the Alice Springs Orogeny. Intruded by an unnamed dyke dated at 467 +/- 5 Ma. Petrography and zircon description discussed.|1754 +/- 15 Ma (LAICPMS) MDA for precursor.||||Biotite-bearing, schistose gneiss with mm- to cm-thick gneissic layering.|02-FEB-19
79100|Yambla Gneiss|72515|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Jervois Range Special Map Sheet. Irindina Province.||Harts Range Metamorphic Complex|||Metasedimentary rocks including metsandstone, gneiss, schist and quartzite.|
79100|Yambla Gneiss|72516|3|Fully described|iii, p14, p18, p21, p64, p78-84|Cambrian Series 2|Tonian|Irindina Province, extends into JINKA, DNEIPER, ALCOOTA and is inferred to extend into ALICE SPRINGS map sheet. Formerly referred to as the Irindina Gneiss and an unnamed quartzite of the Harts Range Group. Preserves evidence for a Paleozoic tectonothermal cycle. <1000m thick in Quartz. In a tectonised (sheared?) contact with Palaeoproterozoic Aileron Province rocks. A SHRIMP U-Pb age of 376 +/- 54 Ma is interpreted as the metamorphic age of this rock whilst a SHRIMP age of 1754 +/- 7 Ma is given as a conservative maximum depositional age and an age of 1772 +/- 7 Ma as the magmatic crystallisation. The 964 +/-19 Ma age is interpreted to be a max dep age from detrital zircons in a quartzite unit. Forms a series of 20-30m high ridges and patches of partially covered outcrop; unnamed subunit outcrop characteristics are discussed further.  Metamorphism, deformation, petrography and structure of various lithologies are discussed. Structural contact with the Denara Orthogneiss. See also p101, p125-127, p135-136, p148-149, p152, p155, p170-171, p177, p186-187, p200.|ca 630 Ma max dep age|Harts Range Metamorphic Complex||Intruded by the Riddock Amphibolite Member, Indiana Igneous Complex and the Entire Gneiss.|Undivided metasedimentary rocks: metasandstone, feldspar gneiss, schist and quartzite.|19-APR-22
79100|Yambla Gneiss|72524|5|Briefly described|p8-9, p13.|Cambrian|Cambrian|Has a detrital zircon spectra dominated by a unimodal peak at ca. 1750 Ma and a maximum deposition age of ca. 530 Ma (Irindina Gneiss of Scrimgeour 2013, Buick et al 2005, Maidment 2005, Beyer et al 2013). Beyer et al (2018) records maximum deposition of 1754 +/- 7 Ma and isotopic resetting of 376 +/- 54 Ma in a sample of Yambla Gneiss, and a magmatic crystallisation age of 467 +/- 5 Ma for a leucogranite within the Yambla Gneiss.|c. 530 Ma max depositional age|Harts Range Metamorphic Complex|||Includes a quartzite layer.|
79100|Yambla Gneiss|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 Irindina Province.|||||Includes greywacke gneiss, quartzite.|
79100|Yambla Gneiss|73591|5|Briefly described|p37, p39|Terreneuvian|Tonian|Irindina Province, widely outcropping. Near unimodal detrital zircon U-Pb age spectra in most instances. [Written as 'Jervois quartzite' in reference to usage by Maidment et al., 2013]. Deposition of the sedimentary precursor occurred in the Tonian-Terreneuvian.|Younger than ca 1040 Ma|||Intruded by Indiana Igneous Complex.|Metamudstone and metagreywacke.|
27307|Yaningidjara Orthogneiss|23270|5|Briefly described|Table 1, p5||Proterozoic|In the Arunta Block..||||||20-DEC-06
27307|Yaningidjara Orthogneiss|23271|5|Briefly described|Map legend||Proterozoic|In the Arunta Block. Age: Middle Proterozoic.||||||20-DEC-06
27307|Yaningidjara Orthogneiss|23732|5|Briefly described|p22|Paleoproterozoic|Paleoproterozoic|Age: 1806+/-6Ma.  Geological Province: Arunta Province.||||||07-NOV-08
27307|Yaningidjara Orthogneiss|23868|5|Briefly described|p752|Paleoproterozoic|Paleoproterozoic|Age: 1806+/-6Ma.  Geological Province: Arunta Inlier.||||||07-NOV-08
27307|Yaningidjara Orthogneiss|24197|5|Briefly described|p19, p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Of the Harverson Suite. Coarse-grained, grey, granitic augen gneiss. Age: ~1820Ma. Geological province: Arunta Inlier.||||||07-FEB-11
27307|Yaningidjara Orthogneiss|24540|5|Briefly described|p9|||Age: 1806Ma (Vry et al 1996). Associated with hydrothermal alteration and metasomatism.||||||07-FEB-11
27307|Yaningidjara Orthogneiss|37058|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27307|Yaningidjara Orthogneiss|39888|6|Mentioned|Fig.8|||||||||
27307|Yaningidjara Orthogneiss|42217|6|Mentioned|p417|||||||||
27307|Yaningidjara Orthogneiss|42326|5|Briefly described|Table 2 P11|||||||||
27307|Yaningidjara Orthogneiss|48992|2|Defined|p62|Mesoproterozoic|Mesoproterozoic|Prob.Middle Proterozoic||||||
27307|Yaningidjara Orthogneiss|50369|5|Briefly described|p1.3, 4.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Harverson Suite.||||||07-NOV-08
27307|Yaningidjara Orthogneiss|64956|5|Briefly described|p3 Tb. 1, p24|Paleoproterozoic|Paleoproterozoic|Intrudes sedimentary rocks of Lander Rock Beds. Cryst. age: 1798+/-5Ma. Previous dating for the granite precursor:1806+/6Ma (Vry et al 1996). Geol.prov: Arunta region. Sample is biotite granite with K-feldspar megacrysts; contains sillimanite + garnet||||||07-FEB-11
27307|Yaningidjara Orthogneiss|65338|5|Briefly described|p15, p17.|Statherian|Orosirian|Has complex zircon systematics; previous (Vry et al. 1996) age determination was 1806 +/- 6 Ma.|1798 +/- 4 Ma.|||Intrudes Lander Rock Formation.||
27307|Yaningidjara Orthogneiss|65341|6|Mentioned|p2 Fig.2. |Paleoproterozoic|Paleoproterozoic|||||||
27307|Yaningidjara Orthogneiss|65343|5|Briefly described|p3 Fig.4|Paleoproterozoic|Paleoproterozoic|Arunta Region.||||||
27307|Yaningidjara Orthogneiss|69226|5|Briefly described|p239, p240 Tb.1|Orosirian|Orosirian|Reynolds-Anmatjira Ranges region.|1806 +/- 6 Ma (Vry et al., 1996).|||Intrudes Lander Rock Beds.||
27307|Yaningidjara Orthogneiss|69228|6|Mentioned|p370-371|||Yaningidjara Hills, Arunta Inlier. Associated with a shear zone that hosted fluid flow. Isotope values and metamorphism described.||||||
27307|Yaningidjara Orthogneiss|69427|4|Described|p12:20-21, 26|Statherian|Orosirian|Reynolds Range, Aileron Province. Andalusite and cordierite porphyroblasts occur in contact aureoles. Another age of 1806 +/- 3 Ma is from Vry et al.(1996); both SHRIMP U-Pb zircon.|1798 +/- 3 Ma (Worden et al., 2008).|||Intrudes Lander Rock Formation.|Foliated to gneissic megacrystic granite; biotite-bearing and characterised by coarse phenocrysts of K-feldspar with locally developed rapakivi textures.|12-JUL-16
27307|Yaningidjara Orthogneiss|69931|6|Mentioned|p269|Paleoproterozoic|Paleoproterozoic|Arunta Inlier. Presented as Yaningidjara orthogneiss.||Haverson Suite.||||
27307|Yaningidjara Orthogneiss|70376|6|Mentioned|p833 fig 2, p833|Paleoproterozoic|Paleoproterozoic|Also spelled Yaningigjara Orthogneiss, p833, with age: 1798+/-5 Ma (Vry et al 1996).|1806 Ma +/- 6 Ma|||||
27307|Yaningidjara Orthogneiss|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen. Metamorphosed at 1566 +/- 2 Ma (U-Pb monazite SHRIMP).|1798+/-4.1 Ma crystallisation: U-Pb zircon SHRIMP||||K-feldspar megacrystic biotite granite, granite.|
27307|Yaningidjara Orthogneiss|71858|5|Briefly described|p4, p70|Orosirian|Orosirian|Aileron Province.|ca. 1806 Ma|||Intrudes the Weldon Metamorphics.||
23289|Yanungbi Volcanics|22538|6|Mentioned|Fig3 P708|||||||||
23289|Yanungbi Volcanics|22600|4|Described|Map legend|Statherian|Statherian|||||||
23289|Yanungbi Volcanics|23363|5|Briefly described|344 Fig.3|||||||||
23289|Yanungbi Volcanics|24048|5|Briefly described|p37|Statherian|Statherian|Age: 1710Ma.||||||
23289|Yanungbi Volcanics|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Rhyolite: pink to red, aphyric to slightly porphyritic (K-feldspar), locally granophyric. Geol. Prov: McArthur Basin.||||||12-OCT-05
23289|Yanungbi Volcanics|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Of the Fagan Suite. Rocks of lava domes and flows.||||||07-FEB-11
23289|Yanungbi Volcanics|44112|2|Defined|p25,44-46,112-113||Statherian|Max Age: 1712 (+/-) 10 Ma.||||||20-DEC-06
23289|Yanungbi 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
23289|Yanungbi Volcanics|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Rhyolite: pink to red, aphyric to slightly porphyritic (K-feldspar), locally granophyric. Geol. Prov: McArthur Basin.||||||
23289|Yanungbi Volcanics|63866|5|Briefly described|p115|||Caledon Shelf/Arnhem Inlier.||||Conformably overlies the Latram Granite. Intrudes or is overlain conformably by the Spencer Creek Group.||
23289|Yanungbi Volcanics|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf North, McArthur Basin.||Of the Spencer Creek Group.||Shown as coeval with Latram Granite and  overlain by Gove Sandstone Fig 4. [Probably wrongly] shown as overlying Yuduyudu Formation Fig 5.||06-JUN-18
23289|Yanungbi Volcanics|69421|5|Briefly described|p6:6||||>c.1710 Ma.|Spencer Creek Group.||Intrudes, and overlies Dhalinybuy Granite unconformably or nonconformably.||12-JUL-16
23289|Yanungbi Volcanics|69430|6|Mentioned|p15:3|||NE McArthur Basin.||Spencer Creek Group.||||12-JUL-16
23289|Yanungbi Volcanics|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Spencer Creek Group||Overlain by Gove Sandstone||
23289|Yanungbi Volcanics|70302|4|Described|iv, p1, p7-9, p13|Statherian|Statherian|McArthur Basin. Coeval and possibly comagmatic with Latram Granite. SHRIMP U-Pb zircon magmatic crystallisation age.|1712 +/- 5 Ma (Kositcin et al., 2015).|Spencer Creek Group.||Unconformably overlies Giddy Suite and Dhalinybuy Granite.|Felsic volcanic succession: includes orange-pink, K-feldspar-porphyritic rhyolite.|05-FEB-18
23289|Yanungbi Volcanics|71374|6|Mentioned|p30|||||||Unconformably overlain by the Mount Bonner Sandstone.||
23289|Yanungbi Volcanics|71592|5|Briefly described|Appendix A.|||Arnhem Province.|1712+/-5 Ma (crystallisation: Pb/Pb zircon).||||Rhyolite.|
23289|Yanungbi Volcanics|72377|5|Briefly described|p9,12, 15, 19|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Contact with overlying Mount Bonner Sandstone is interpreted to show deeply incised paleotopography. Exposed in GOVE mapsheet; Kositcin et al., 2015b reported a magmatic crystallisation age of 1712+\-5 Ma (SHIRMP U-Pb zircon dating), which is within uncertainty with the magmatic crystallisation age of the Haddon Volcanics (1712+\-12 Ma; this record). Interpreted to be correlable with Gadabara Volcanics (Rawlings et al., 1997).|1712+\-5 Ma (magmatic)|Unit of Spencer Creek Group.||Overlain unconformably by Mount Bonner Sandstone.||09-OCT-19
29185|Yarawoi Formation|22538|6|Mentioned|Fig3 P708|||||||||
29185|Yarawoi Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
29185|Yarawoi Formation|24048|6|Mentioned|p56|||||||||
29185|Yarawoi Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, grey and green, variably dolomitic; dololutite and silty dololutite; sandstone: fine to medium-grained; chert: (silicified carbonate), stromatolitic. Geol. Prov: McArthur Basin.||||||13-OCT-05
29185|Yarawoi Formation|24432|5|Briefly described|p565 Fig.2|Statherian|Statherian|Of Habgood Group. Overlies Slippery Creek Siltstone. Overlain by Yarrawirrie Formation. Geological Province: Northern McArthur Basin.||||||
29185|Yarawoi Formation|32660|5|Briefly described|Table 4|||||||||
29185|Yarawoi Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
29185|Yarawoi Formation|43010|2|Defined|p133||Paleoproterozoic|Of the Habgood Group. Of Statherian age.||||||07-NOV-08
29185|Yarawoi Formation|44112|4|Described|p54-58|||||||||
29185|Yarawoi Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Habgood Group. Mudstone: red, grey and green, variably dolomitic; dololutite and silty dololutite; sandstone: fine to medium-grained; chert: (silic ified carbonate), stromatolitic. Geol. Prov: McArthur Basin.||||||
29185|Yarawoi Formation|64817|6|Mentioned|p353 Fig.4 |||||Of the Habgood Group.||||
29185|Yarawoi Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot; p35|Paleoproterozoic|Paleoproterozoic|McArthur Basin.|1645-1620 Ma.|||||
29185|Yarawoi Formation|69430|4|Described|p15:3, 20|||Walker Fault Zone, northern McArthur Basin. 650-700m thick. Shallow-water to subtidal deposits. Neither lower nor upper contact is exposed.||Habgood Group.||Overlies Slippery Creek Siltstone. Is overlain by Darwarunga Sandstone.|Red, grey and green mudstone, variably dolomitic; dololutite and silty dololutite; fine- to medium-grained sandstone; stromatolitic chert (silicified carbonate); and dolostone.|12-JUL-16
29185|Yarawoi Formation|69673|6|Mentioned|p16 fig 13|||Walker Fault Zone||Habgood Group||overlain by Darwarunga Sandstone, overlies Slippery Creek Siltstone||
29185|Yarawoi Formation|71374|5|Briefly described|iii, p1 tbl 1, p12-p15, p47-p48|Statherian|Statherian|Northern McArthur Basin. SHRIMP age is interpreted as the maximum depositional age for this formation. Sampling site provided along with zircon description and SHRIMP analytical discussion. 600-700m thick. Informally subdivided intoSparsely exposed. At the reference area this unit is informally subdivided.|1705 +/- 18 Ma (SHRIMP U-Pb)|Habgood Group||Conformably overlies the Slippery Creek Siltstone. Conformably overlain by the Darwarunga Sandstone.|Interlayered dolomitic shale, dolostone and sandstone.|09-MAY-18
29185|Yarawoi Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Middle Habgood Group.|||Mudstone, dolomitic siltstone, sandstone, stromatolitic chert.|04-MAR-20
26242|Yardida Tillite|8187|5|Briefly described|Map legend|Adelaidean|Adelaidean|Diamictite, shale, siltstone, sandstone.  Overlain by Black Stump Arkose.||||||21-JUN-04
26242|Yardida Tillite|8217|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Laminated black shale with dolomite lenses. Underlies: Black Stump Arkose.||||||28-OCT-04
26242|Yardida Tillite|24442|5|Briefly described|p49|Sturtian|Sturtian|Geological Province: Georgina Basin.||||||
26242|Yardida Tillite|35863|6|Mentioned|Table 1|||||||||
26242|Yardida Tillite|36234|6|Mentioned|p164|||||||||
26242|Yardida Tillite|36898|6|Mentioned|p181|||||||||
26242|Yardida Tillite|37462|4|Described|Table 4.IX|||||||||
26242|Yardida Tillite|37928|6|Mentioned|Fig.4|||||||||
26242|Yardida Tillite|37929|4|Described|p525|||||||||
26242|Yardida Tillite|38157|6|Mentioned|Table IX|||||||||
26242|Yardida Tillite|38832|6|Mentioned|p157|||||||||
26242|Yardida Tillite|39445|6|Mentioned|p56|||||||||
26242|Yardida Tillite|39921|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
26242|Yardida Tillite|40906|6|Mentioned|Fig.9|||||||||
26242|Yardida Tillite|41277|5|Briefly described|p83|||||||||
26242|Yardida Tillite|41405|6|Mentioned|p205|||||||||
26242|Yardida Tillite|43595|5|Briefly described|p548,Fig.5-33,549||Adelaidean|||||||
26242|Yardida Tillite|44158|6|Mentioned|p29|||In the Georgina Basin.||||||20-DEC-06
26242|Yardida Tillite|45155|6|Mentioned|Fig.7|||In the Georgina Basin.||||||20-DEC-06
26242|Yardida Tillite|46903|6|Mentioned|p53|||||||||
26242|Yardida Tillite|46959|6|Mentioned|p207|||||||||
26242|Yardida Tillite|48990|2|Defined|p16|Adelaidean|Adelaidean|||||||
26242|Yardida Tillite|49027|6|Mentioned|p2|||||||||
26242|Yardida Tillite|60122|4|Described|p9, p11, p41|Neoproterozoic|Neoproterozoic|Green-grey diamictite siltstone, dolomitic shale, dolostone, minor quartz sandstone, arkose. Disconformable on Yacha beds; disconformably overlain by Black Stump Arkose.  Max. thickness: 2900m. Geological Province: Georgina Basin. In Supersequence 2.||||||24-MAY-05
26242|Yardida Tillite|60590|5|Briefly described|Map legend|Cryogenian|Cryogenian|Diamictite, siltstone, dolomitic shale, dolostone, minor quartz sandstone and arkose.||||||
26242|Yardida Tillite|61404|5|Briefly described|Map legend|Cryogenian|Cryogenian|Of the Aroota Group.  Diamictite, siltstone, dolomitic shale, dolostone, minor quartz sandstone and arkose. Geological Province: southern Georgina Basin.||||||
26242|Yardida Tillite|62082|6|Mentioned|p66|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
26242|Yardida Tillite|63450|5|Briefly described|p78 Fig. 5|Neoproterozoic|Neoproterozoic|Disconformably overlies Yackah beds; disconformably overlain by Black Stump Arkose and Wonnadinna Dolomite. Geological province: Georgina Basin, West Toko Syncline.||||||07-FEB-11
26242|Yardida Tillite|64068|3|Fully described|p45, 46, p19, p151, p223|Cryogenian||Over 650 m thick.||Of Aroota Group.||Disconformably overlies Yackah beds. Is disconformably overlain by Black Stump Arkose.|Green-grey diamictite and laminated siltstone;  minor fine to coarse quartz sandstone and arkose. Local dolomitic capping.|04-APR-12
26242|Yardida Tillite|64778|6|Mentioned|p13|Neoproterozoic|Neoproterozoic|Toko Syncline, Southern Georgina Basin.||||||
26242|Yardida Tillite|65338|6|Mentioned|p63.|||Southeastern Georgina Basin. May correlate with the diamictite at the base of Central Mount Stuart Formation.||Unit in Aroota Group.||||
26242|Yardida Tillite|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Neoproterozoic|Neoproterozoic|Centralian Superbasin.|||||Tillite.|
26242|Yardida Tillite|68270|4|Described|p681-683,686-688|Cryogenian|Cryogenian|Southern Georgina Basin. Type section is a composite section with outcrop in Field River Anticline and area 6km SSE of Aroota Bore, drillholes Hay River 5 (lat. 23'11'9"N, long. 137'54'12"E) 6 (lat 23'10'42N, long. 137'52'48"E) and section at the end of seismic traverse 3. Crops out in the central-southern Georgina Basin. Less than 650m thick. Glacial and periglacial deposit. Related to Sturt glaciation. Correlative to Sturt Tillite. Lateral equivalent to Mount Cornish Formation.||||Overlain disconformably by Black Stump Arkose. Underlain disconformably (inferred) with Yackah beds.|Green-grey diamictite and laminated siltstone with minor fine to very coarse (pebbly) grained quartz sandstone and arkose, locally capped by grey, laminated dolomitic shale and lenticular dolomite.|03-JUL-19
26242|Yardida Tillite|68277|6|Mentioned|p95|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
26242|Yardida Tillite|68553|6|Mentioned|Map legend; schematic diagram.|Early Paleozoic|Neoproterozoic|Georgina Basin. This unit, as well as Black Stump, Gnallan-a-gea and Sun Hill Arkoses and Little Burke Tillite, are all mapped under the symbol, -P-Cg.||||||
26242|Yardida Tillite|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
26242|Yardida Tillite|69439|6|Mentioned|p24:7|||Georgina Basin.||||Correlated with Naburula Formation (Ngalia Basin).||12-JUL-16
26242|Yardida Tillite|69443|4|Described|p28:5, 7-8, 33, 45|Cryogenian|Cryogenian|Walter (1980). Desert Syncline and Field River Anticline, SE Georgina Basin. Unfossiliferous. Generally recessive and poorly exposed. Thickness probably c.650m. Glacial and periglacial deposits with a (postglacial) cap carbonate. Exposed by Toomba Fault. A shale within this Formation contains TOC up to 0.90%.||Aroota Group.||Disconformably overlies Yackah beds. Is overlain disconformably by Black Stump Arkose. Correlated with Mount Cornish Formation.|Diamictite and laminated siltstone, and minor fine to vey coarse (to pebbly) quartz sandstone and arkose; locally capped by laminated dolomitic shale and lenticular dolostone up to 100m thick.|12-JUL-16
26242|Yardida Tillite|69591|5|Briefly described|p94|||Toko Syncline. Thickness is 100m in GSQ Mount Whelan 1, but up to 2900m in the NT. Correlated with Sturtian (lower) tillite in the Flinders Ranges (SA).||||Is overlain disconformably by Black Stump Arkose.|A glacigene deposit of highly variable thickness.|
26242|Yardida Tillite|69673|4|Described|p114 fig 92|Cryogenian|Cryogenian|Approximately 650m thick.||Aroota Group|||Diamictite, laminated siltstone and minor sandstone locally capped by dolomitic shale and dolostone.|
26242|Yardida Tillite|72516|6|Mentioned|p86|Cryogenian|Cryogenian|Georgina Basin.||||Equivalent to the Mount Cornish Formation.||02-JUN-21
26242|Yardida Tillite|73086|6|Mentioned|p62, p158|||Georgina Basin.||||Correlates to Areyonga Formation.||
27030|Yarrawirrie Formation|22538|6|Mentioned|Fig3 P708||Statherian|Age of unit is 1620+/-21 Ma.||||||20-DEC-06
27030|Yarrawirrie Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
27030|Yarrawirrie Formation|23937|5|Briefly described|p13|||Of the Balma Group.  Correlates with part of the Nagi Formation.||||||
27030|Yarrawirrie Formation|24048|3|Fully described|p59|Mesoproterozoic|Paleoproterozoic|Of the Balma Group.  Overlain by Baiguridji Formation; underlain by Zamia Creek Siltstone.  Geological Province: McArthur Basin.||||||07-NOV-08
27030|Yarrawirrie Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Includes Ngilipitji Conglomerate Member. Dololutite and dolarenite; silty dololutite; dolomitic sandstone; mudstone: dolomitic; carbonate rocks leached or silicified (chert). Geol. Prov: McArthur Basin.||||||11-OCT-05
27030|Yarrawirrie Formation|24432|5|Briefly described|p562 Fig.2|Statherian|Statherian|Of Habgood Group. Overlies Yarawoi Formation. Geological Province: Northern McArthur Basin.||||||
27030|Yarrawirrie Formation|32660|5|Briefly described|Table 4|||||||||
27030|Yarrawirrie Formation|42597|5|Briefly described|Map Legend|Carpentarian||||||||
27030|Yarrawirrie Formation|43010|2|Defined|p117||Paleoproterozoic|Of the  McArthur Group. Of Statherian age.||||||07-NOV-08
27030|Yarrawirrie Formation|44112|3|Fully described|p53-56||Statherian|Max Age: 1620 (+/-) 21 Ma||||||
27030|Yarrawirrie Formation|44299|4|Described|p.12|||SD/53-7,8. Lower?Proterozoic. Table 1.||||||
27030|Yarrawirrie Formation|44300|14|Not recorded|map legend|||SD/53-7,8. Lower (?) Proterozoic.||||||
27030|Yarrawirrie Formation|45162|6|Mentioned|p45|||||||||
27030|Yarrawirrie Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Balma Group. Includes Ngilipitji Conglomerate Member. Dololutite and dolarenite; silty dololutite; dolomitic sandstone; mudstone: dolomitic; carbon ate rocks leached or silicified (chert). Geol. Prov: McArthur Basin.||||||
27030|Yarrawirrie Formation|63866|5|Briefly described|p114|Calymmian|Statherian|Isa Superbasin.|1620 +/- 21 Ma (Pietsch et al., 1994)|Balma Group||||
27030|Yarrawirrie Formation|64817|6|Mentioned|p353 Fig.4 |Statherian|Statherian||1620 +/- 21 Ma.|Of the Balma Group.||||
27030|Yarrawirrie Formation|67323|5|Briefly described|Eastern Australia Time-Space Plot|||McArthur region. See also GIS attrib tbl |1620 +/- 21 Ma.|||||
27030|Yarrawirrie Formation|69430|4|Described|p15:3, 14, 21-22|Statherian|Statherian|Walker Fault Zone, northern McArthur Basin. c.600m thick. Very shallow-water (marine?) or lacustrine sediments; periodic exposure and evaporitic conditions. Hiatus before deposition of this unit. Possible correlative of Stretton Sandstone. SHRIMP U-Pb single zircon age from tuffaceous rock.|1621 +/- 21 Ma (Pietsch et al., 1994).|Balma Group.|Ngilipitji Conglomerate Member.|Overlies Vaughton Siltstone and Zamia Creek Siltstone unconformably. Is overlain conformably by Baiguridji Formation.|Stromatolitic, nodular, intraclastic dololutite and dolarenite, commonly microbially laminated; silty dololutite; dolomitic sandstone, commonly dolomitic mudstone. Fluvial to shallow-marine polymictic conglomerate at base.|12-JUL-16
27030|Yarrawirrie Formation|69673|6|Mentioned|p16 fig 13, p17|Mesoproterozoic|Paleoproterozoic|Walker Fault Zone|1620 +/- 21 Ma|Balma Group||Overlain by Baiguridgi Formation, Overlies Zamia Creek Siltstone, Unconformably overlies Vaughton Siltstone||
27030|Yarrawirrie Formation|71374|5|Briefly described|p15|Calymmian|Statherian|SHRIMP maximum depositional age from a tuffaceous rock (Pietsch et al, 1994). |1620 +/- 21 Ma (SHRIMP U-Pb)|Balma Group||Equivalent to the Darwarunga Sandstone.||
27030|Yarrawirrie Formation|71592|5|Briefly described|Appendix A.|||McArthur Basin.|1620+/-21 Ma (MDA: U-Pb zircon SHRIMP)||||Dacite.|
27030|Yarrawirrie Formation|71606|5|Briefly described|p138|Statherian|Statherian|Central Walker Trough, McArthur Basin. Maximum U-Pb zircon age 1620+\-21 Ma from tuffaceous mudstone.||Unit of Balma Group.||||
27030|Yarrawirrie Formation|71632|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|McArthur Basin.||Upper Balma Group.||||
27030|Yarrawirrie Formation|72373|5|Briefly described|p15,17-18|Paleoproterozoic|Paleoproterozoic|Of McArthur Basin. Contains 1621+\-21 Ma tuff unit in the upper part of the formation (Pietsch et al 1994).||||Overlain by Baiguridji Formation.||
24596|Yarrawonga Volcanic Member|24197|5|Briefly described|p105 Tb. 15.1|Paleoproterozoic|Paleoproterozoic|Of the Gerowie Suite - parent unit not given. Age: ~1885Ma. Geological Province: Pine Creek Inlier.||||||07-FEB-11
24596|Yarrawonga Volcanic Member|39069|6|Mentioned|Fig.7|||||||||
24596|Yarrawonga Volcanic Member|40492|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24596|Yarrawonga Volcanic Member|40493|4|Described|p12|||||||||
24596|Yarrawonga Volcanic Member|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24596|Yarrawonga Volcanic Member|41305|4|Described|p16|||||||||
24596|Yarrawonga Volcanic Member|43187|5|Briefly described|p2|||||||||
24596|Yarrawonga Volcanic Member|50586|5|Briefly described|p1.1, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Pine Creek Inlier. Of the Gerowie Suite.||||||07-NOV-08
24596|Yarrawonga Volcanic Member|65339|5|Briefly described|p6 Table 1, p10.|||||Unit in Wildman Siltstone.|||Highly altered mafic volcanic rocks.|
24596|Yarrawonga Volcanic Member|69420|5|Briefly described|p5:8, 10|Paleoproterozoic|Paleoproterozoic|Central region, Central Domain, Pine Creek Orogen. c.40m thick.||Wildman Siltstone.|||Dacite, ignimbrite, rhyolite.|12-JUL-16
23298|Yarunganyi Granite|7821|5|Briefly described|p47, 61-64, 66|||Mount Doreen area, Arunta Inlier. Zircon analyses tabulated. Post-Wabudali Tectonic Phase.|1567 +/- 11 Ma.|||Intrudes the Reynolds Range Group.|K-feldspar-megacrystic (up to 30 cm long) biotite granite. Undeformed. Local pronounced flow foliation.|
23298|Yarunganyi Granite|24197|5|Briefly described|p61 Tb. 4.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Suite. Age: 1567Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
23298|Yarunganyi Granite|43275|5|Briefly described|Map Legend||Mesoproterozoic|||||||
23298|Yarunganyi Granite|43631|6|Mentioned|p18||Mesoproterozoic|Age:1567+/-6 Ma.||||||20-DEC-06
23298|Yarunganyi Granite|43749|6|Mentioned|p5|||Age: 1567 Ma. Previously known as 'Mount Doreen Granite'.||||||20-DEC-06
23298|Yarunganyi Granite|44114|6|Mentioned|p340|||Northern Arunta Inlier. Associated with the Chewings Orogeny.||||||
23298|Yarunganyi Granite|44158|4|Described|p19 Table.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Granitic Suite. Age: 1567+/-11Ma, U-Pb zircon date. Intrudes Lander Rock beds, Patmungala beds and Reynolds Range Group.||||||05-MAY-10
23298|Yarunganyi Granite|50369|5|Briefly described|p1.5, 24.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Southwark Suite. Age: 1567 +/- 11Ma (SHRIMP).||||||07-NOV-08
23298|Yarunganyi Granite|61385|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Of the Arunta Complex. Megacrystic muscovite-biotite granite.||||||20-OCT-05
23298|Yarunganyi Granite|62082|5|Briefly described|p51|||Geological Province: Arunta terrain.||||||07-FEB-11
23298|Yarunganyi 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. Megacrystic muscovite-biotite granite; low gravity response; low to moderate mixed magnetic response [map key is missing Mesoproterozoic]||||||19-DEC-12
23298|Yarunganyi 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. Megacrystic muscovite-biotite granite; low gravity response; low to moderate mixed magnetic response [map key is missing Mesoproterozoic]||||||19-DEC-12
23298|Yarunganyi Granite|69427|5|Briefly described|p12:44-45, 62|Mesoproterozoic|Mesoproterozoic|Immediately N of Ngalia Basin, Aileron Province. Intruded about the end of the Chewings Event. SHRIMP U-Pb zircon age. Associated with wolframite-bearing pegmatites at the Wolfram Hill (Mount Doreen wolfram field) prospect.|1567 +/- 11 Ma (Young et al., 2005).|Southwark Suite.||||12-JUL-16
23298|Yarunganyi Granite|71592|5|Briefly described|Appendix A.|||Aileron Province, Arunta Orogen.|1567+/-11 Ma (crystallisation: U-Pb zircon SHRIMP)||||Undeformed biotite-muscovite K-rich granite.|
23298|Yarunganyi Granite|72366|5|Briefly described|p7|Calymmian|Calymmian|Geological province: Aileron Province. Representative of youngest phase (last of three) of felsic magmatism in the MOUNT DOREEN map sheet. Age reference: Young et al., 1995.|1567+\-11 Ma|Unit of Southwark Suite.||||
23298|Yarunganyi Granite|72376|5|Briefly described|iii,p1,4,9|Calymmian|Calymmian|Geological province: Aileron Province. Outcrops ~3km ENE of Wilfram Hill tungsten-copper deposit. U-Pb zircon magmatic crystallisation age of 1567+\-11 Ma (Young et al 1995). The new muscovite 40Ar/39Ar age of 1550+\-4 Ma from pegmatites intruding into Lander Rock Formation (NTGS MD15MVM015; this study) provides a temporal, and by inference, genetic link between tungsten and copper mineralisation at Wolfram Hill and the Yarunganyi Granite.|1567+\-11 Ma (U-Pb magmatic)|Unit of Southwark Suite.|||Megacrystic muscovite-biotite granite.|
41858|Yaya Metamorphic Complex|60674|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Alkipi Metamorphics and the Inyalinga granulite.  Age: 1660Ma.  Geological Province: Warumpi Province.||||||07-NOV-08
41858|Yaya Metamorphic Complex|61387|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Leisler Metamorphics and undifferentiated rocks. In the Arunta region.||||||07-NOV-08
41858|Yaya Metamorphic Complex|61518|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: 1660Ma.  Geological Province: Yaya Domain.||||||07-NOV-08
41858|Yaya Metamorphic Complex|61519|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Warumpi Province||||||07-NOV-08
41858|Yaya Metamorphic Complex|61660|3|Fully described|p3 Fig.2, pp4-9, pp14-15, pp23-25.|Proterozoic|Proterozoic|Yaya Domain. A newly-recognised succession of granulite facies metasedimentary rocks, deposited between c. 1660 - 1640 Ma, that has undergone a polymetamorphic Proterozoic evolution. Abundant detrital zircons aged 1700 - 1660 Ma with Haasts Bluff Domain provenance. Metamorphosed around 1640- 1635 Ma, i.e. less than 20 million years between deposition and deep crustal metamorphism, followed by rapid exhumation. High-temperature reworking of the terrane followed at 1570 and 1150 Ma. Zircon analyses are detailed.|Max. deposition age 1661 +/- 10 Ma.||Includes Inyalinga Granulite and Alkipi Metamorphics.||High-grade pelitic metasedimentary rocks and felsic gneiss.|
41858|Yaya Metamorphic Complex|64677|6|Mentioned|p31||||c.1660 Ma.||Leisler Metamorphics.|||
41858|Yaya Metamorphic Complex|65358|5|Briefly described|p12|Statherian|Statherian|Metasedimentary succession intruded by voluminous 1640-1635 Ma granites and gabbros. 1660-1640 Ma.||||||
41858|Yaya Metamorphic Complex|65487|6|Mentioned|p61-62|||A fore-arc sedimentary sequence interlayered with mafic rocks; deposited 1660-1650 Ma, metamorphosed (highT, high-P) 1640-1635 Ma during Liebig Orogeny.||||||
41858|Yaya Metamorphic Complex|66860|6|Mentioned|p6 Tb.1|||Arunta Region. Deposition was coeval with lower parts of Namerinni Group (Tennant Region).|1660-1640 Ma.|||||
41858|Yaya Metamorphic Complex|67565|2|Defined|p59, p4, p6 Tbl 1, p13-18, p36.|Statherian|Statherian|New name, after Yaya Creek. Includes all metasedimentary rocks and migmatitic orthogneiss in the Yaya Domain, Warumpi Province. Previously included within undifferentiated Arunta Complex (Ranford, 12969). Reference localities detailed. Metamorphosed to granulite facies during the Liebig Orogeny of 1640-1630 Ma. Age considerations are discussed.|Deposition between 1660-1640 Ma.||Includes Alkipi and Speares Metamorphics and Inyalinga Granulite.|Faulted against Kakalyi Gneiss. Is intruded by Ulambaura Granodiorite, Belt Granite, Illili and Waluwiya Suites, Papunya Igneous Complex and Stuart Pass Dolerite. Is overlain by Heavitree Quartzite|Garnet-biotite-sillimanite metapelite, metapsammite, quartzose metasedimentary rocks, quartzite, strained biotite granite, felsic migmatite, massive cordierite granulite, calc-silicate rock, interlayered granulite and metapelite, mafic amphibolite.|01-DEC-15
41858|Yaya Metamorphic Complex|68832|5|Briefly described|p19-25|||Includes quartzite informally named 'Papunya quartzite'. Warumpi Province, Arunta Region. SHRIMP U-Pb zircon geochronology. Maximum deposition age and younger metamorphic age.|1760+/-8 Ma, 1636+/-6 Ma||Includes Inyalinga Granulite.|||
41858|Yaya Metamorphic Complex|68994|5|Briefly described|p3-4|||Yaya Domain in central Warumpi Province. Deposition of sedimentary precursors to high-grade metasedimentary rocks at 1661-1639 Ma is constrained by max depositional age of youngest detrital zircon  and age of metamorphic zircon growth.|1660-1640 Ma.|||||
41858|Yaya Metamorphic Complex|69417|6|Mentioned|p2:5|Statherian|Statherian|Yaya Domain, Warumpi Province.||||||12-JUL-16
41858|Yaya Metamorphic Complex|69428|5|Briefly described|p13:1-3, 5, 7-9, 11|Paleoproterozoic|Paleoproterozoic|Scrimgeour et al. (2005). Includes all metasedimentary rocks and migmatitic orthogneiss within the Yaya Domain, Warumpi Province. A supracrustal succession. Metamorphosed to granulite facies during the 1640-1635 Liebig Orogeny.|1660-1650 Ma.||Speares, Alkipi, Liesler Metamorphics and Inyalinga Granulite.|Intruded by Papunya Igneous Complex.|Dominantly metapelites with significant calc-silicate rock, quartzite, mafic granulite and felsic orthogneiss; also an undivided, heterogeneous unit of felsic migmatites and strained granites, minor mafic rock and quartzic and pelitic metasediments.|12-JUL-16
41858|Yaya Metamorphic Complex|71592|5|Briefly described|Appendix A.|||Warumpi Province, Arunta Orogen. Metamorphosed at 1636 +/- 6 Ma.|1760-+/-8 Ma (MDA: U-Pb zircon SHRIMP)||||Quartzite.|
41858|Yaya Metamorphic Complex|72360|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Geological province: Warumpi Province. Of Yaya Domain.||||||09-SEP-19
24597|Yeeradgi Sandstone|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup (Hatches Creek Group). Lithic/feldspathic/micaceous arenite; greywacke; siltstone.||||||07-NOV-08
24597|Yeeradgi Sandstone|23733|5|Briefly described|p32 Fig. 19|||Of Wauchope Subgroup.||||||
24597|Yeeradgi Sandstone|23809|5|Briefly described|p27 Fig. 25|||Of the Wauchope Subgroup (lower section).  Geological Province: Davenport Province.||||||
24597|Yeeradgi Sandstone|24172|5|Briefly described|p37, p65 Tb. 9|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Underlain by Unimbra Sandstone. Geological Province: Tennant Creek Inlier. Max. thickness: 300m. Of the Hatches Creek Group. Recessive volcanilithic sandstone unit.||||||07-NOV-08
24597|Yeeradgi Sandstone|39624|5|Briefly described|Table 1|||||||||
24597|Yeeradgi Sandstone|39900|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24597|Yeeradgi Sandstone|40578|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup (Hatches Creek Group).  Arenite, partly volcaniclastic; minor siltstone and shale; rare felsic lava.||||||10-JAN-05
24597|Yeeradgi Sandstone|40836|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
24597|Yeeradgi Sandstone|41128|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Feldspathic arenite; friable arenite; siltstone; mudstone; ashstone; micaceous tuff; shale and rare calcareous beds. Geological Province: Tennant Creek Block.||||||07-NOV-08
24597|Yeeradgi Sandstone|41129|4|Described|Table 1|||Mention p24.||||||20-DEC-06
24597|Yeeradgi Sandstone|41204|4|Described|Table 1|||||||||
24597|Yeeradgi Sandstone|41205|5|Briefly described|Map legend|Proterozoic|Proterozoic|Of the Wauchope Subgroup. Lithic/feldspathic/micaceous arenite, greywacke, siltstone; minor felsic volcanics.||||||16-NOV-05
24597|Yeeradgi Sandstone|41308|5|Briefly described|Table 2|||||||||
24597|Yeeradgi Sandstone|41310|4|Described|Table 1|||See also p11.||||||20-DEC-06
24597|Yeeradgi Sandstone|41408|6|Mentioned|Map legend|Proterozoic||||||||
24597|Yeeradgi Sandstone|41524|5|Briefly described|Table 1|||||||||
24597|Yeeradgi Sandstone|41970|6|Mentioned|Fig.3 P333|||||||||
24597|Yeeradgi Sandstone|42643|4|Described|p12, Table 1 p7|||||||||
24597|Yeeradgi Sandstone|42644|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup. Micaceous arenite, feldspathic/lithic arenite, ashstone, minor micaceous and phyllitic siltstone and shale, tuffaceous arenite, felsic volcanics.||||||07-NOV-08
24597|Yeeradgi Sandstone|43224|5|Briefly described|Map legend||Paleoproterozoic|Of the Wauchope Subgroup.||||||07-NOV-08
24597|Yeeradgi Sandstone|43802|6|Mentioned|Table 1,p80|||||||||
24597|Yeeradgi Sandstone|45167|3|Fully described|Table 1|||Of the Wauchope Subgroup.||||||20-DEC-06
24597|Yeeradgi Sandstone|49033|2|Defined|p17|Proterozoic|Proterozoic|||||||
24597|Yeeradgi Sandstone|60681|5|Briefly described|Map legend|Statherian|Statherian|Of the Hatches Creek Group.  Sandstone, siltstone, shale.  Geological Province: Davenport Province.||||||11-JAN-05
24597|Yeeradgi Sandstone|60684|5|Briefly described|p12, p8 tb.1|Paleoproterozoic|Paleoproterozoic|Of the Wauchope Subgroup (Hatches Creek Group). Lithic, feldspathic and micaceous arenite; greywacke, siltstone.  Max. thickness: ~300m. Conformably overlies Unimbra Sandstone. Geol.Prov: Davenport province.||||||07-NOV-08
24597|Yeeradgi Sandstone|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Lower Wauchope Subgroup (Hatches Creek Group). Subarkosic and sublithic, volcaniclastic/tuffaceous arenite, siltstone and shale; minor felsic volcanic rocks inc. lava, tuff and cherty ashstone.  Overlies Unimbra Sst. In the Tennant Creek region.||||||07-NOV-08
24597|Yeeradgi Sandstone|61567|5|Briefly described|p632, p633 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Wauchope Subgroup. Composed primarily of feldspathic volcanics, volcaniclastics, brown siltstone and shale; strongly foliated. Overlies Unimbra Sandstone; underlies Coulters Sst. max. thickness: 400m.  Geol.Prov:Tennant Creek Inlier.||||||07-NOV-08
24597|Yeeradgi Sandstone|64735|5|Briefly described|p206 Fig 2, p209|Orosirian|Orosirian|At equivalent stratigraphic level to Arabulja Volcanics.||Of Wauchope Subgroup, Hatches Creek Group.||||30-APR-12
24597|Yeeradgi Sandstone|65209|5|Briefly described|p35 Fig.1, p38|Paleoproterozoic|Paleoproterozoic|Encompassed by informal Lower Wauchope Subgroup.||Wauchope Subgroup||Is unconformably overlain by Coulters Sandstone.||05-JAN-17
24597|Yeeradgi Sandstone|65338|6|Mentioned|p20.|||Correlative with Tinfish Sandstone.||Unit in Wauchope Subgroup.||||
24597|Yeeradgi Sandstone|67148|5|Briefly described|Map legend.|Orosirian|Orosirian|||Unit in Wauchope Subgroup, Hatches Creek Group.||Overlies Unimbra Sandstone. Is overlain by Arabulja and Newlands Volcanics.|Feldspathic arenite; friable arenite; siltstone; mudstone; ashstone; micaceous tuff; shale and rare calcareous beds.|19-OCT-11
24597|Yeeradgi Sandstone|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Wauchope Subgroup, Lower.||Overlies Unimbra Sandstone. Is disconformably overlain by Coulters Sandstone. Is shown as lateral equivalent of Newlands Volcanics and part lateral equivalent, part underlying Arabulja Volcanics|Subarkosic and sublithic, volcaniclastic/tuffaceous arenite, siltstone and shale; minor felsic volcanic rocks including lava, tuff and cherty ashstone.|08-DEC-14
24597|Yeeradgi Sandstone|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Tennant Creek/Davenport area.||Hatches Creek Group.||||
24597|Yeeradgi Sandstone|67352|4|Described|p10 tab 1, p44 fig 48|Orosirian|Orosirian|800 m thick. Fluviatile during volcanism. Low strike ridges; in part recessive.||Wauchope Subgroup||Overlies Unimbra Sandstone. Grades laterally into Newlands Volcanics or Arubulja Volcanics. Is overlain unconformably by Coulters Sandstone.|Feldspathic, lithic, kaolinitic and micaceous arenite: friable to silicified, thinly to medium bedded, fine-to medium-grained; siltstone, mudstone, ashstone, shale; rare calcareous and carbonaceous beds; lenticular thinly bedded micaceous tuff.|
24597|Yeeradgi Sandstone|68518|4|Described|p8 Tb.1, 12|Proterozoic|Proterozoic|Max. thickness: 600 m. Has appreciable amounts of probably penecontemporaneous volcanic detritus.||Wauchope Subgroup||Conformable on Unimbra Sandstone; overlain conformably by and may interfinger with basal parts of Newlands Volcanics and Arabulja Volcanics; overlain unconformably by Cambrian strata.|Ridge-forming to recessive micaceous arenite and feldspathic/lithic arenite; minor micaceous and commonly phyllitic siltstone and shale. Some beds may be calcareous. Readily eroded.|30-MAY-16
24597|Yeeradgi Sandstone|68697|5|Briefly described|p24|||||Hatches Creek Group.||Overlies Unimbra Sandstone. Partly underlies, and is partly lateral equivalent of, Arabulja Volcanics.|Includes minor interlayered felsic volcanic rocks.|
24597|Yeeradgi Sandstone|69425|5|Briefly described|p10:3, 11-13, 15, 21, 25|Statherian|Statherian|A recessive unit. 0-800m thick. Fluvial sediments; abrupt change from quartz sandstone of underlying unit probably reflects fresh influx of volcanic detritus. Correlative of Tinfish Sandstone; lateral equivalent of Arabulja  Volcanics. Greisenised by Devils Marbles Granite; produced 250-500 kg of tungsten.||Wauchope Subgroup, lower.||Conformably overlies Unimbra Sandstone. Is overlain conformably by Arabulja and Newlands Volcanics (interfingers), and Coulters Sandstone (locally unconformably). Correlated with Manga Mauda Member.|Subarkosic and sublithic (variably volcaniclastic/tuffaceous) sandstone, siltstone, shale; minor felsic volcanic rocks (including lava, tuff and cherty ashstone) and greywacke.|12-JUL-16
24597|Yeeradgi Sandstone|69431|5|Briefly described|p16:5, 8|||Davenport Province.||Wauchope Subgroup.||Possible distal lateral equivalent of Manga Mauda Member (Hayward Creek Formation).||12-JUL-16
24597|Yeeradgi Sandstone|72379|6|Mentioned|p8|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga Province. ||||||
24597|Yeeradgi Sandstone|72380|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Geological province: Warramunga and Davenport provinces.||||||
24597|Yeeradgi Sandstone|73083|6|Mentioned|p44|||||Wauchope Subgroup||||
30409|Yenberrie Granite|43140|5|Briefly described|Fig.1, p56||Paleoproterozoic|||||||07-NOV-08
30409|Yenberrie Granite|43624|6|Mentioned|p14|||May be 'Leucogranite'.||||||20-DEC-06
30409|Yenberrie Granite|69420|6|Mentioned|p5:110|||Hosts wolframite and minor molybdenite in greisenised quartz-aplite dykes in the Yenberrie mineral field.||||||11-JUL-16
24140|Yenberrie Leucogranite|23120|5|Briefly described|p428|||||||||
24140|Yenberrie Leucogranite|23216|5|Briefly described|Table1p10,15,17|||||||||
24140|Yenberrie 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
24140|Yenberrie Leucogranite|24340|4|Described|p143, p152|Paleoproterozoic|Paleoproterozoic|Age: 1870 - 1860 Ma. Geological Province: Pine Creek Inlier. Classified as Young Igneous Suite by Klominsky et al., 1996.||||||07-NOV-08
24140|Yenberrie Leucogranite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24140|Yenberrie Leucogranite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
24140|Yenberrie Leucogranite|41125|6|Mentioned|p55|||||||||
24140|Yenberrie Leucogranite|41586|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
24140|Yenberrie Leucogranite|42756|6|Mentioned|Fig.5 P6|||||||||
24140|Yenberrie Leucogranite|43149|5|Briefly described|Map Legend||Paleoproterozoic|Of Orosirian age.||||||07-NOV-08
24140|Yenberrie Leucogranite|43624|6|Mentioned|Fig.15,p20|||||||||
24140|Yenberrie Leucogranite|43832|4|Described|Table8 p37; 46,50,61||Paleoproterozoic|Of the Tennysons suite.||||||07-NOV-08
24140|Yenberrie Leucogranite|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
24140|Yenberrie Leucogranite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Age ~1820-1850Ma. Of Cullen Supersuite. I-type. Fine to coarse leucogranite, greisen. Intrudes Burrell Creek Formation.||||||07-JAN-09
24140|Yenberrie Leucogranite|67564|6|Mentioned|p33 Fig.19.|Paleoproterozoic|Paleoproterozoic|Pluton within Cullen Batholith, Pine Creek Orogen.||||||
24140|Yenberrie Leucogranite|69418|6|Mentioned|p3:21|||Pine Creek Orogen (Central Domain). Hosts the Yenberrie W-Mo-Bi greisen deposit (briefly described).||||||12-JUL-16
24140|Yenberrie Leucogranite|69420|5|Briefly described|p5:17-19, 41, 101, 109|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Leucogranite-dominated plutons; mineralogy and petrology/geochemistry summarised. Hosts the Yenberrie W, Mo, Bi, Sn deposit.||Tennysons Suite.|||Fine-grained leucogranite and greisen. I-type.|12-JUL-16
69781|Yinabalbu Member|61405|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Poorly sorted silty and clayey sandstone and subgreywacke, minor coarse quartzite and slate, faulted and invaded by quartz veins. Age: >1835Ma.  Geological Province: Arunta region - Aileron Province.||||||07-NOV-08
23310|Yirrkala Formation|22600|4|Described|Map legend|Cenomanian|Aptian|||||||
23310|Yirrkala Formation|23374|5|Briefly described|p25|Cenomanian|Aptian|||||||
23310|Yirrkala Formation|23425|5|Briefly described|p381.|||||||||
23310|Yirrkala Formation|23937|5|Briefly described|p55|Cretaceous|Cretaceous|||||||
23310|Yirrkala Formation|24047|5|Briefly described|p13, p55|Cretaceous|Early Cretaceous|Formerly part of the Mullaman beds.  Unconformably overlies the Bradshaw Complex.  Geological Province: Carpentaria Basin.||||||21-DEC-06
23310|Yirrkala Formation|24048|4|Described|p75|Mesozoic|Mesozoic|||||||
23310|Yirrkala Formation|24049|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone: white to pale grey, fine to very coarse-grained, massive to thick planar beds, trough cross-beds, rare chert pebbles and plant fossils.||||||
23310|Yirrkala Formation|24050|6|Mentioned|p53|||||||||
23310|Yirrkala Formation|24442|6|Mentioned|p21|Cretaceous|Cretaceous|||||||
23310|Yirrkala Formation|43630|2|Defined|p13-15|Cenomanian|Albian|Palynological dating. Formerly part of Mullaman Beds?||||||
23310|Yirrkala Formation|44112|4|Described|p79,81-82|||||||||
23310|Yirrkala Formation|61403|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Sandstone: white to pale grey, fine to very coarse-grained, massive to thick planar beds, trough cross-beds, rare chert pebbles and plant fossils.||||||
23310|Yirrkala Formation|63866|5|Briefly described|p115|Cretaceous|Mesozoic|Carpentaria Basin. ||||||
23310|Yirrkala Formation|64822|5|Briefly described|pS88|Cretaceous|Cretaceous|Fluvial arkosic sandstone and quartzose sandstones.  Overlain by a large bauxite deposit in the Gove area, Arnhem Land.||||||
23310|Yirrkala Formation|65337|6|Mentioned|p68.|Cretaceous|Cretaceous|Assigned (Krassay 1994) from parts of the Mullaman beds of Skwarko (1966).||||||
23310|Yirrkala Formation|65340|6|Mentioned|p64.|Cenomanian|Aptian|Assigned by Krassay (1994); formerly part of the Mullaman beds of Skwarko (1966).||||||
23310|Yirrkala Formation|69418|6|Mentioned|p3:28|||Carpentaria Basin. Hosts the Dhupuma and Gove residual bauxite deposits (described).||||||12-JUL-16
23310|Yirrkala Formation|69455|5|Briefly described|p39:2, 39:4 Fig.39.3; 39:6-9|Cenomanian|Albian|Krassay (1994); Rawlings et al. (1997). Onshore Western Gulf Sub-basin, Carpentaria Basin. Previously part of the Mullaman Beds. Broadly correlated with Rolling Downs Group (equivalent). Fluvial, high-energy channel deposits and valley fills. Age from lithostratigraphic correlation. Hosts the Gove bauxite deposit (described in detail).||||Disconformably overlies Walker River Formation. Is correlated with the offshore Normanton Formation.|Massive to thickly planar-bedded, friable, kaolinised arkosic sandstone and poorly sorted, fine- to very coarse-grained, matrix-poor quartzic sandstone that are interbedded with minor claystone.|12-JUL-16
23310|Yirrkala Formation|69673|5|Briefly described|p201|Cenomanian|Albian||||||Sandstone, often interbedded with claystone and siltstone.|
27634|Your Dam Metamorphics|24442|6|Mentioned|p49|||On TOBERMORY sheet.||||||
27634|Your Dam Metamorphics|39921|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27634|Your Dam Metamorphics|48997|6|Mentioned|Fig.2|||||||||
27634|Your Dam Metamorphics|49027|6|Mentioned|p1|||||||||
27634|Your Dam Metamorphics|60122|5|Briefly described|p4-5, p6|Paleoproterozoic|Paleoproterozoic|Scattered outcrops of muscovite-feldspar-quartz granofels, schistose gneiss and schist. Geological Province: Arunta Province.||||||07-NOV-08
27634|Your Dam Metamorphics|60590|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Possibly Orosirian in age.||||||07-NOV-08
27634|Your Dam Metamorphics|69427|5|Briefly described|p12:8, 27|||Warren (1981); Kruse et al. (2002). Far eastern Aileron Province. Crops out poorly: scattered low outcrops as inliers in S Georgina Basin.|||||Muscovite-biotite-quartz schist and muscovite-feldspar-quartz granofels.|12-JUL-16
74205|Yow Creek Formation|61542|4|Described|p277 Fig. 2, p284|Visean|Visean|New addition to Weaber Gp. when Milligans Fm. further subdivided into Milligans Fm.and Yow Fm. Max.thick:at type section:1160m. Geol.prov:onshore Bonapart Basin/Petrel-Sub-basin. Shale and sandy siltstone. Further details of lithology and fossils given.||||||07-FEB-11
74205|Yow Creek Formation|69452|3|Fully described|p36:9, 11-12, 14-16|Early Carboniferous|Early Carboniferous|Defined by Gorter et al. (2005); formerly upper part of the Milligans Formation. Petrel Sub-basin, Bonaparte Basin. Subsurface. Type section is a 180m interval in drillhole Bonaparte-1. Prograding delta deposits. Up to 400m thick. Offshore and onshore (subsurface).||Weaber Group.||Unconformably overlies Milligans Formation. Is overlain unconformably by Utting Calcarenite.|Slightly silty and rarely fossiliferous shale, with common ironstone and a basal, weakly fossiliferous sandy siltstone.|12-JUL-16
74205|Yow Creek Formation|69653|6|Mentioned|p10|Carboniferous|Carboniferous|Petrel Sub-basin.||Weaber Group.||Overlies Milligans Formation. Is overlain by Utting Calcarenite.||
74205|Yow Creek Formation|69673|6|Mentioned|p168 fig 138, p170 fig 142, p171|Carboniferous|Carboniferous|400m thick.||Weaber Group||Overlies Milligans Formation, overlain by Kingfisher Shale, Utting Calcarenite|Silty and rarely fossiliferous shale with common ironstone and weakly fossiliferous sandy siltstone.|
74205|Yow Creek Formation|70061|5|Briefly described|Petrel Sub-basin Fig.3|Visean|Visean|See also Regional geology: Fig.8, p11. Offshore S Petrel Sub-basin. Prospective hydrocarbon reservoir.||Weaber Group.||Overlies Milligans Formation. Is overlain by Utting Calcarenite.||12-JUL-16
74205|Yow Creek Formation|73117|6|Mentioned|p15|Visean|Visean|Bonaparte Basin, southern.||Weaber Group||Underlain by Milligans Formation. Overlain by Utting Calcarenite.||
23312|Yuduyudu Formation|22538|6|Mentioned|Fig3 P708|||||||||
23312|Yuduyudu Formation|22600|4|Described|Map legend|Statherian|Statherian|||||||
23312|Yuduyudu Formation|24048|5|Briefly described|p36|||Of the Spencer Creek Group.||||||21-DEC-06
23312|Yuduyudu Formation|24049|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: fine-grained, ferruginous; mudstone. Geol. Prov: McArthur Basin.||||||12-OCT-05
23312|Yuduyudu Formation|44112|3|Fully described|p10,43-4,47,113||Statherian|Part of Supersequence 1(C). Max Age: ~1710 Ma.||||||21-DEC-06
23312|Yuduyudu Formation|61403|5|Briefly described|Map Legend|Statherian|Statherian|Of Spencer Creek Group. Sandstone: fine-grained, ferruginous; mudstone. Geol. Prov: McArthur Basin.||||||
23312|Yuduyudu Formation|64817|6|Mentioned|p353 Fig.4, p355 Fig.5 |||Caledon Shelf North, McArthur Basin.||Of the Spencer Creek Group.||Shown as overlying Gove Sandstone and underlying Cato Volcanics. [Probably wrongly shown as also underlying Yanungbi Volcanics in Fig 5.]|Shown as mudstone in Fig 5.|06-JUN-18
23312|Yuduyudu Formation|65340|6|Mentioned|p92.|||Northern McArthur Basin. Tentatively correlated with Aquarium Formation on the basis of similar lithofacies.||||||
23312|Yuduyudu Formation|69430|6|Mentioned|p15:3|||NE McArthur Basin.||Spencer Creek Group.||||12-JUL-16
23312|Yuduyudu Formation|69673|6|Mentioned|p16 fig 13|||Northeastern McArthur Basin.||Spencer Creek Group||Overlain by Cato Volcanics, overlies Gove Sandstone||
26250|Yuendumu Sandstone|24064|4|Described|p226|Cambrian|Cambrian|Geological Province: Ngalia Basin. Maximum thickness: >700m.||||||19-DEC-12
26250|Yuendumu Sandstone|30258|6|Mentioned|Fig.2|||Proterozoic age||||||
26250|Yuendumu Sandstone|33757|3|Fully described|p9|||See also Table 1. Unconformable between Vaughan Springs Quartzite and Walbiri Dolomite.||||||21-DEC-06
26250|Yuendumu Sandstone|33760|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
26250|Yuendumu Sandstone|33761|6|Mentioned|p145|||Cambrian||||||
26250|Yuendumu Sandstone|36473|6|Mentioned|Map legend|Ordovician|Adelaidean|Adelaidean to Ordovician||||||
26250|Yuendumu Sandstone|37462|4|Described|Table 4.IX|||||||||
26250|Yuendumu Sandstone|37537|6|Mentioned|Map legend|Cambrian|Adelaidean|Red-brown, fine and coarse, thin to medium bedded, fissile, silty, micaceous, slumped and cross-bedded sandstone; minor quartzwacke and arkose. Geological Province: Ngalia Basin.||||||14-FEB-06
26250|Yuendumu Sandstone|39565|6|Mentioned|p33|||||||||
26250|Yuendumu Sandstone|40105|6|Mentioned|p319|||||||||
26250|Yuendumu Sandstone|40810|5|Briefly described|p13|||||||||
26250|Yuendumu Sandstone|40906|6|Mentioned|Fig.9|||||||||
26250|Yuendumu Sandstone|41429|6|Mentioned|p247|||||||||
26250|Yuendumu Sandstone|41801|6|Mentioned|p217|||||||||
26250|Yuendumu Sandstone|42059|5|Briefly described|Fig.2 P131|||||||||
26250|Yuendumu Sandstone|42504|5|Briefly described|p83|||||||||
26250|Yuendumu Sandstone|42643|6|Mentioned|p21|||Ngalia Basin||||||
26250|Yuendumu Sandstone|43275|5|Briefly described|Map Legend||Cambrian|||||||
26250|Yuendumu Sandstone|43595|5|Briefly described|p548,Fig.5-33,549|Cambrian|Adelaidean|||||||
26250|Yuendumu Sandstone|43749|6|Mentioned|Fig.1,p6||Cambrian|||||||
26250|Yuendumu Sandstone|44158|4|Described|p31 Table.2|Cambrian|Neoproterozoic|of Ngalia Basin.||||||
26250|Yuendumu Sandstone|45155|2|Defined|p30|Early Cambrian|late Adelaidean|Late Adelaidean - Earliest Cambrian||||||
26250|Yuendumu Sandstone|46903|5|Briefly described|p48|||||||||
26250|Yuendumu Sandstone|61385|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Red brown to pale brown sandstone, minor arkosic sandstone; trace fossils.   Geological Province: Ngalia Basin.||||||
26250|Yuendumu Sandstone|64068|6|Mentioned|p51, 56, 224|||Ngalia Basin. Correlated in part with Central Mount Stuart Formation, part 2 with Octy Formation, Neutral Junction Formation, southern Georgina Basin.||||||
26250|Yuendumu Sandstone|65232|5|Briefly described|p70|||Unconformably underlies Walbiri Dolostone. Shallow-marine sandstone. Geol. Prov: Ngalia Basin.||||||09-FEB-10
26250|Yuendumu Sandstone|65329|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Mount Doreen Formation, older than Walbiri Dolomite. Red-brown to pale brown sandstone, minor arkosic sandstone; trace fossils||||||28-SEP-11
26250|Yuendumu Sandstone|65330|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Of Ngalia Basin. Shown as younger than Mount Doreen Formation, older than Walbiri Dolomite. Red-brown to pale brown sandstone, minor arkosic sandstone; trace fossils||||||28-APR-10
26250|Yuendumu Sandstone|65341|6|Mentioned|p18.|||Ngalia Basin. Correlated with Octy Formation.||||||
26250|Yuendumu Sandstone|69437|5|Briefly described|p22:4-5, 8, 10, 16|Ediacaran|Ediacaran|Ngalia Basin, Centralian A Superbasin. Supersequence 4. Has potential as a petroleum reservoir.||||Is overlain unconformably by Walbiri Dolostone. Lower part is correlated with lower part of Arumbera Sandstone.||12-JUL-16
26250|Yuendumu Sandstone|69439|3|Fully described|p24:3-4, 9-10, 13, 16, 18, 20-21|Early Cambrian|Neoproterozoic|Wells and Moss (1983). Forms low hills NE of the Walbiri Ranges, along the N margin of the Ngalia Basin. Is over 700m thick in the type section, 4 km S of Yuendumu. There is a slight unconformity in the middle of this unit. The same trace fossils occur in the uppermost Arumbera Sandstone (Amadeus Basin): useful for dating this unit. Contains potential reservoirs, possibly sealed by Walbiri Dolostone or Bloodwood Formation.|||Yuendumu Sandstone, Lower and Upper.|Unconformably overlies Vaughan Springs Quartzite. Is overlain unconformably by Walbiri Dolostone and Djagamara Formation. Correlated with Arumbera Sandstone.|Fine- to medium-grained, medium to thinly bedded, brown silty sandstone that is in part arkosic and micaceous, particularly in the lower parts; with cross-beds, slumped bedding, large clay pellets and marine trace fossils (Planolites ballandus).|12-JUL-16
26250|Yuendumu Sandstone|69443|6|Mentioned|p28:10, 14|||Ngalia Basin. Lower part correlates with part of the Mopunga Group (Georgina Basin). Upper part correlates with part of the Shadow Group.||||||12-JUL-16
26250|Yuendumu Sandstone|69673|5|Briefly described|p106, p107 fig 85, p110|Cambrian|Neoproterozoic|Over 700m thick. Potential reservoir rock.||||Overlies Mount Doreen Formation, overlain by Walbiri Dolostone|Arkosic and micaceous silty sandstones.|
30244|Yulyupunyu Granitic Gneiss|24197|5|Briefly described|p59 Tb. 4.1|Paleoproterozoic|Paleoproterozoic|Age: 1780Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
30244|Yulyupunyu Granitic Gneiss|43275|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
30244|Yulyupunyu Granitic Gneiss|43749|6|Mentioned|p13|||||||||
30244|Yulyupunyu Granitic Gneiss|44158|4|Described|p15 Table.1|Paleoproterozoic|Paleoproterozoic|Age: Older than about 1760 Ma. Intrudes Lander Rock beds.||||||05-MAY-10
30244|Yulyupunyu Granitic Gneiss|50369|5|Briefly described|p1.3, 6.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier.||||||07-NOV-08
30244|Yulyupunyu Granitic Gneiss|61385|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Arunta Complex.  Deformed megacrystic muscovite-biotite granite; augen gneiss, locally migmatitic.||||||07-NOV-08
30244|Yulyupunyu Granitic Gneiss|69427|5|Briefly described|p12:30 Fig.12.28; 12:32-33|||Young et al. (1995). Crops out W of Mount Denison homestead. Included in a map of 1780-1740 Ma granites in the Aileron Province.|||||A strongly-deformed, porphyroblastic biotite-muscovite granite with feldspar augen up to 4cm in length.|12-JUL-16
30244|Yulyupunyu Granitic Gneiss|71858|6|Mentioned|p5|||Aileron Province.||||||
31344|Yumurrpa Granophyre|24197|5|Briefly described|p61 Tb. 4.1|Mesoproterozoic|Mesoproterozoic|Of the Southwark Suite (or Southwark Granite Suite?). Age of Suite (based on age of Yarunganyi Granite): 1567Ma. Geological Province: Arunta Inlier.||||||07-FEB-11
31344|Yumurrpa Granophyre|43631|6|Mentioned|p12-13||Paleoproterozoic|Description of 'Gneissic Granophyre' may refer to this unit p12-13||||||07-NOV-08
31344|Yumurrpa Granophyre|43749|6|Mentioned|Fig.1,p6,12||Paleoproterozoic|||||||07-NOV-08
31344|Yumurrpa Granophyre|44158|4|Described|p13 Table.1|Paleoproterozoic|Paleoproterozoic|Age: Older than about 1760 Ma. Of Arunta Inlier. Intrudes Lander Rock beds.||||||05-MAY-10
31344|Yumurrpa Granophyre|50369|5|Briefly described|p1.5, 24.1, Table 1.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Inlier. Of the Southwark Suite.||||||07-NOV-08
31344|Yumurrpa Granophyre|62636|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Geological Province: Arunta Region - Aileron Province.|||||Dark grey schistose muscovite bearing granitic rock with small augen of feldspar and quartz.|15-APR-11
31344|Yumurrpa Granophyre|69427|5|Briefly described|p12:30 Fig.12.28; 12:33|||Young et al. (1955). North side of Wabudali Range. Included in a map of 1780-1740 Ma granites in the Aileron Province. Intrusion at shallow levels was prior to deposition of the Reynolds Range Group.||||Intrudes Lander Rock Formation.|A dark grey, strongly foliated biotite-muscovite granite.|12-JUL-16
23318|Yungkulungu Formation|23410|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgroup (Churchills Head Group). Undifferentiated, lithic arenite including volcanic arenite; siltstone and shale; felsic lava and minor tuff. Also subdivided into tuffaceous, sedimentary and volcanic lithofacies.||||||07-NOV-08
23318|Yungkulungu Formation|23733|5|Briefly described|p5, p16|||Of Flynn Group.  See also p4 Tb. 1.||||||
23318|Yungkulungu Formation|23809|5|Briefly described|p27, Fig. 25, p29|||Of the Flynn Group.  Age: >1840Ma.  Correlates with the Bernborough Formation.  Geological Province: Tennant Inlier.||||||
23318|Yungkulungu Formation|24172|4|Described|p22, p8 Tb. 1, p67 Tb.9, p78 appendix.|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup. Unconformably overlain by Rising Sun Conglomerate; underlain by Warramunga Formation. Geological Province: Tennant Creek Inlier. Max. thickness: ~5200m.||||||07-NOV-08
23318|Yungkulungu Formation|43224|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of the Flynn Subgroup.||||||07-NOV-08
23318|Yungkulungu Formation|50588|6|Mentioned|p5.1|||Geological Province: Tennant Creek/Davenport Province.||||||
23318|Yungkulungu Formation|60684|4|Described|p11, p7 Tb. 1|Paleoproterozoic|Paleoproterozoic|Of Flynn Subgp (Churchills Head Gp). Lithic arenite and volcanic litharenite; minor granule and pebble beds; interbedded tabular siltstone, felsic ignimbr.........Intruded by Channingum Granite. max. thickness:~1000m in type section. Geol.Prov: Davenport.||||||07-NOV-08
23318|Yungkulungu Formation|61406|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Of Ooradidgee Group. Lithic/sublithic/volcanilithic arenite, siltstone, shale; sandstone, magnetite laminae; welded and non-welded felsic crystal-lithic tuff and lapilli tuff; minor felsic lava and ignimbrite. In the Tennant Creek region.||||||07-NOV-08
23318|Yungkulungu Formation|65209|5|Briefly described|p35 Fig.1, p36|Paleoproterozoic|Paleoproterozoic|Originally tentatively correlated with Junalki Formation (Donnellan et al 1995), but subsequently re-interpreted (Johnstone and Donnellan 2001) to unconformably overlie Warramunga Formation (a Junalki Formation correlative). ||Ooradidgee Group||Unconformably overlies Warramunga Formation.|Thick succession of volcanic rocks, and overlying and intercalated sedimentary rocks.|05-JAN-17
23318|Yungkulungu Formation|65338|5|Briefly described|p6, p17.|Orosirian|Orosirian|Contemporaneous with syn- to immediately post-tectonic granite emplacement asssociated with the Tennant Event. Dacitic ignimbrite in lower part was dated.|1849 +/- 5 Ma (Smith 2000).|Unit in Ooradidgee Group.|||Includes dacitic ignimbrite.|12-DEC-14
23318|Yungkulungu Formation|67148|6|Mentioned|Map legend.|Proterozoic|Proterozoic|||Unit in Ooradidgee Group.||||
23318|Yungkulungu Formation|67352|6|Mentioned|p44 fig 48|||||Ooradidgee Group||||
23318|Yungkulungu Formation|69187|5|Briefly described|p53 Fig.2, p54 Fig.3, p61|Orosirian|Orosirian|Warramunga Province. Shown in figure separately as volcanic lithofacies and sedimentary lithofacies.|crystallis'n 1849 +/- 5 Ma (Smith,2001)|Ooradidgee Group||unconformably overlies Warramunga Formation and porphyries and granitic rocks||
23318|Yungkulungu Formation|69424|4|Described|p9:5-6, 10, 15-17, 21-23, 26, 28-29|Paleoproterozoic|Paleoproterozoic|See also 39 Fig.9.24. Warramunga Province. c.5200m thick. Subaerial and subaqueous volcanic rocks; shallow-marine, sublittoral, littoral and fluviatile sedimentary rocks. Is intruded by Treasure Suite, Channingum and Cabbage Gum Granites and Mumbilla Granodiorite, and has faulted contact with the last.|1849 +/- 5 Ma (Smith, 2000).|Ooradidgee Group.||Unconformably overlies, and is faulted against, Warramunga Formation. Is unconformably overlain by Rising Sun Conglomerate.|Medium to thickly bedded lithic/volcanilithic sandstone; minor granule and pebble beds. Interbedded tabular siltstone, tuff and felsic ignimbrite. Thick, predominantly foliated porphyritic rhyolitic lava.|12-JUL-16
23318|Yungkulungu Formation|69425|6|Mentioned|p10:23|||ENE-trending folds along the Gosse River Road in TENNANT CREEK map area are probably examples of macroscale Davenport Event folding.||||||12-JUL-16
23318|Yungkulungu Formation|71592|5|Briefly described|Appendix A.|||Tennant Creek Region.|1849+/-5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Extrusive porphyritic dacite.|
23318|Yungkulungu Formation|73083|6|Mentioned|p44|||||||||
23318|Yungkulungu Formation|73124|5|Briefly described|piii, p2 Fig.1|Orosirian|Orosirian|Age of extrusive magmatism matches that of four unnamed units (ca 1854-1849 Ma): a quartz-feldspar porphytic rhyloite and an extrusive dacite from drillhole RVDD0002, and two volcaniclastic sandstones (drillholes RVDD0002 and MXCURD002). Sedimentary lithofacies overlies volcanic lithofacies of this unit.||||Underlain by Warramunga Formation.||
23318|Yungkulungu Formation|73125|5|Briefly described|p2|Palaeoproterozoic|Palaeoproterozoic|Warramunga Province. On p2 this unit is shown as comprising a sedimentary lithofacies overlying a volcanic lithofacies.||Ooradidgee Group.||||
23318|Yungkulungu Formation|73427|5|Briefly described|p1, p3-4, p11-13|Orosirian|Orosirian|North Australian Craton, Tennant Region. Extends locally under cover to the east and southwest of Tennant Creek. Part of the lowermost package of the Ooradidgee Group. Represents the extrusive equivalent of the Tennant Creek Supersuite. Reflect a shallow marine to subaerial setting.|1855-1845 Ma|Ooradidgee Group||Unconformably underlain by Warramunga Formation.||
23318|Yungkulungu Formation|73460|6|Mentioned|p2|||Warramunga Province. Includes upper sedimentary lithofacies and lower volcanic lithofacies.||||||
23318|Yungkulungu Formation|73550|6|Mentioned|p4, p7|Orosirian|Orosirian|Most likely comprises the host rock of mineralisation at the Curiosity prospect.|ca 1850 Ma|Ooradidgee Group|||Includes siliciclastics.|
23318|Yungkulungu Formation|73590|6|Mentioned|piii, p1-2, p8, p25|Orosirian|Orosirian|Comprises lower volcanic lithofacies and upper sedimentary lithofacies. Represents bimodal magmatism.|ca 1850-1840 Ma|Ooradidgee Group||||
79294|Yungkulungu Formation - ignimbritic lithofacies|69424|4|Described|p9:17, 22-23|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Subaerial; up to 200m thick. Conformable within the sedimentary lithofacies. Is referred to, on p9:21-23, as  "the tuffaceous subunit".||Yungkulungu Formation.|||Felsic ignimbrite, welded tuff, rhyolitic lava and ashstone. Interbedded reworked volcaniclastic rocks.|24-FEB-23
72692|Yungkulungu Formation - sedimentary lithofacies|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Lithic/sublithic/volcanilithic arenite, siltstone, shale; sandstone, magnetite laminae; welded and non-welded felsic crystal-lithic tuff and lapilli tuff; minor felsic lava and ignimbrite.|
72692|Yungkulungu Formation - sedimentary lithofacies|69424|4|Described|p9:3, 11, 16-17, 22-23|Paleoproterozoic|Paleoproterozoic|Warramunga Province. Dominated by reworked felsic volcanic detritus: c.3600m thick (p9:17; confusingly stated to be c.2000m thick on p9:21). Shallow marine, grading upwards to sublittoral/littoral and possibly fluviatile. Is immediately younger than this 1849 Ma age for the conformably underlying volcanic lithofacies.|<1849 +/- 5 Ma (Smith, 1999).|Yungkulungu Formation.||Conformably overlies Yungkulungu Formation - volcanic lithofacies. Is intruded by Mumbilla Granodiorite and Channingum Granite. Correlated with Bernborough Formation.|Medium to thickly bedded, medium- to coarse-grained, lithic/volcanilithic sandstone with magnetite and other heavy-mineral-bearing laminae; minor granule to pebble beds with rhyolite clasts towards base; quartz sandstone towards top; minor phyllite.|12-JUL-16
72693|Yungkulungu Formation - volcanic lithofacies|67175|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Tennant Region.||Unit in Ooradidgee Group.|||Felsic crystal-lithic tuff and lapilli tuff; rhyolitic and rhyodacitic lava and ignimbrite; volcanilithic arenite with interbedded siltstone.|
72693|Yungkulungu Formation - volcanic lithofacies|69424|4|Described|p9:3-4, 11, 16, 22-24|Paleoproterozoic|Paleoproterozoic|Warramunga Province. c.1600m thick (p9:17; confusingly stated to be c.3000m thick on p9:21). Subaqueous volcanic and volcaniclastic rocks, latter becoming more prevalent up-section and are shallow-marine. Probably correlates with Monument Formation and lower part of Wundirgi Formation.|1849 +/- 5 Ma (Smith, 1999).|Yungkulungu Formation.||Unconformably overlies Warramunga Formation. Is overlain conformably by Yungkulungu Formation - sedimentary lithofacies. Is intruded by Mumbilla Granodiorite, Channingum and Cabbage Gum Granites.|Thickly bedded, foliated, porphyritic rhyolite to rhyodacite lava with shattered quartz and/or feldspar phenocrysts in medium-grained matrix. Medium bedded volcanilithic sandstone and ashstone, and ignimbrite towards top of the unit.|12-JUL-16
72410|Yunkanjini Granite|62633|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Southwark Suite. Geological Province: Arunta Region - Aileron Province. Coarse to megacrystic porphyritic biotite granite, less abundant dark fine grained phase.||||||16-AUG-06
72410|Yunkanjini Granite|65332|5|Briefly described|Map Legend|Palaeoproterozoic|Palaeoproterozoic|Of Southwark Suite. Shown as older than Vaughan Springs Quartzite, younger than Wabudali Granite. Coarse to megacrystic porphyritic biotite granite, less abundant dark fine-grained phase.[Although shown as Paleoproterozoic, also shown as younger than 1590-1570 Ma Chewings Event ie Mesoproterozoic]||||||27-SEP-11
72410|Yunkanjini Granite|69427|5|Briefly described|p12:44-45|Mesoproterozoic|Mesoproterozoic|Edgoose et al. (in prep.). Immediately N of Ngalia Basin, Aileron Province.|1533 +/- 5 Ma (Cross et al., 2005).|Southwark Suite.|||Coarse-grained granite.|12-JUL-16
72410|Yunkanjini Granite|69508|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Arunta Region, Aileron Province.||Southwark Suite.|||Coarse to megacrystic, porphyritic biotite granite; less abundant, dark fine-grained phase.|
72410|Yunkanjini Granite|71267|6|Mentioned|1m_geologyp12_lithology_lut.csv||||||||granite|
38049|Yununba Granite|24301|2|Defined|p39 Appendix 1|Mesoproterozoic|Mesoproterozoic|Of Kulpitjata Granite Complex. Intrudes Allanah Gneiss and Opparinna Metamorphics.  Geological Province: Musgrave Block||||||
38049|Yununba Granite|24302|5|Briefly described|Map Legend|Mesoproterozoic|Mesoproterozoic|Of the Kultpitjata Granite Complex.  Medium- to coarse-grained muscovite-biotite granite, weakly to strongly porphyritic, strongly foliated.  Geological Province: Musgrave Block||||||29-SEP-05
38049|Yununba Granite|61154|6|Mentioned|p44 Appendix|||Of the Pitjantjatjara Supersuite.||||||19-JUL-05
27310|Zamu Dolerite|9324|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates.||||||07-NOV-08
27310|Zamu Dolerite|9534|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metadolerite, amphibolite, dolerite, syenite.  Intrudes Nourlangie Schist, Cahill Formation, Wildman Siltstone, Masson Formation and Mundogie Sandstone.||||||07-NOV-08
27310|Zamu Dolerite|9538|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates; amphibolites in the east.||||||07-NOV-08
27310|Zamu Dolerite|9691|5|Briefly described|Map Legend|||Metadolerite, amphibolite, dolerite, syenite and differentiates. Intrudes: Cahill Formation, Nourlangie Schist, Wildman Siltstone.||||||01-JUN-05
27310|Zamu Dolerite|9701|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Intrudes: Cahill Formation, Nourlangie Schist, Wildman Siltstone. Metadolerite, amphibolite, dolerite, syenite and differentiates||||||10-FEB-10
27310|Zamu Dolerite|22479|5|Briefly described|fig1p2|Orosirian|Orosirian|||||||
27310|Zamu Dolerite|22600|6|Mentioned|Map legend|||||||||
27310|Zamu Dolerite|22808|6|Mentioned|7 fig 4|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|22809|5|Briefly described|3|Proterozoic|Proterozoic|||||||
27310|Zamu Dolerite|22813|5|Briefly described|Map|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates.||||||07-NOV-08
27310|Zamu Dolerite|23122|5|Briefly described|p411|||||||||
27310|Zamu Dolerite|23205|6|Mentioned|p42|||of Pine Creek Inlier.||||||
27310|Zamu Dolerite|23337|5|Briefly described|907|||||||||
27310|Zamu Dolerite|23374|5|Briefly described|Fig3p5||Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|23714|5|Briefly described|p11|Proterozoic|Proterozoic|See also page 7 Table 1, page 13.||||||
27310|Zamu Dolerite|23715|5|Briefly described|Map legend||Proterozoic|In the Rum Jungle and Central Regions.||||||21-DEC-06
27310|Zamu Dolerite|23733|5|Briefly described|p32 Fig. 19|||||||||
27310|Zamu Dolerite|24047|5|Briefly described|p5 Fig.4|Paleoproterozoic|Paleoproterozoic|Quartz dolerite, granophyre.  Maximum thickness: 50m.  Geological Province: Pine Creek Orogen.  See also p28.||||||07-NOV-08
27310|Zamu Dolerite|24049|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
27310|Zamu Dolerite|24181|5|Briefly described|p87 Fig.2|Paleoproterozoic|Paleoproterozoic|Tholeiitic sills. Geological Province: Pine Creek Inlier.||||||07-NOV-08
27310|Zamu Dolerite|24197|6|Mentioned|p132|||High Mg-tholeiite. Geological province: Pine Creek Inlier.||||||07-FEB-11
27310|Zamu Dolerite|24340|6|Mentioned|p147 Fig. 3|||Geological Province: Pine Creek Inlier.||||||
27310|Zamu Dolerite|24442|5|Briefly described|p43|||Intrudes the Manton, Mount Partridge, South Alligator and Finniss River Groups.||||||
27310|Zamu Dolerite|35140|2|Defined|p309|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|35465|6|Mentioned|p54|||Stratigraphy||||||
27310|Zamu Dolerite|36535|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|36635|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|37462|4|Described|Table 4.II|||See also p232.||||||20-JUL-06
27310|Zamu Dolerite|37579|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Quartz dolerite and granophyre; amphibolite in the east.||||||07-NOV-08
27310|Zamu Dolerite|37815|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|38239|4|Described|p20|||See also p9.||||||20-JUL-06
27310|Zamu Dolerite|38349|4|Described|p13|||||||||
27310|Zamu Dolerite|38351|4|Described|p10|||See also p4.||||||20-JUL-06
27310|Zamu Dolerite|38884|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|39069|6|Mentioned|p25|||||||||
27310|Zamu Dolerite|39357|4|Described|p16|||See also p3.||||||20-JUL-06
27310|Zamu Dolerite|39518|5|Briefly described|p9|||||||||
27310|Zamu Dolerite|39563|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|39679|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|39801|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates: amphibolite in east.||||||07-NOV-08
27310|Zamu Dolerite|39889|6|Mentioned|Table 1|||||||||
27310|Zamu Dolerite|40104|6|Mentioned|p336|||||||||
27310|Zamu Dolerite|40168|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates: amphibolite in east.||||||07-NOV-08
27310|Zamu Dolerite|40223|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates, amphibolite in east.||||||07-NOV-08
27310|Zamu Dolerite|40243|6|Mentioned|p139|||||||||
27310|Zamu Dolerite|40493|6|Mentioned|p22|||||||||
27310|Zamu Dolerite|40808|3|Fully described|p16|||||||||
27310|Zamu Dolerite|40809|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|40823|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|40957|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|41125|6|Mentioned|p15|||Mention Fig.14||||||
27310|Zamu Dolerite|41146|5|Briefly described|Fig.2|||||||||
27310|Zamu Dolerite|41304|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27310|Zamu Dolerite|41305|4|Described|p18|||||||||
27310|Zamu Dolerite|41309|4|Described|p8|||||||||
27310|Zamu Dolerite|41311|4|Described|p12|||||||||
27310|Zamu Dolerite|41397|6|Mentioned|p11|||||||||
27310|Zamu Dolerite|41406|6|Mentioned|Map legend|Paleoproterozoic||||||||07-NOV-08
27310|Zamu Dolerite|41407|6|Mentioned|Map legend|Proterozoic||||||||
27310|Zamu Dolerite|41586|6|Mentioned|Map legend|||||||||
27310|Zamu Dolerite|41594|6|Mentioned|p20|||||||||
27310|Zamu Dolerite|41660|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Dolerite and differentiates.||||||07-NOV-08
27310|Zamu Dolerite|41661|6|Mentioned|p27|||See also Fig.5||||||
27310|Zamu Dolerite|41876|6|Mentioned|p22|||||||||
27310|Zamu Dolerite|41877|5|Briefly described|p27|||||||||
27310|Zamu Dolerite|41961|6|Mentioned|Fig.3 P48|||||||||
27310|Zamu Dolerite|42012|3|Fully described|p10|||See also Table 1 p6.||||||21-DEC-06
27310|Zamu Dolerite|42014|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
27310|Zamu Dolerite|42372|5|Briefly described|p18|||||||||
27310|Zamu Dolerite|42812|6|Mentioned|p65|||||||||
27310|Zamu Dolerite|43140|6|Mentioned|p3||Paleoproterozoic|See also p16.||||||07-NOV-08
27310|Zamu Dolerite|43187|5|Briefly described|p2|||||||||
27310|Zamu Dolerite|43292|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|43624|5|Briefly described|p10|||||||||
27310|Zamu Dolerite|43718|5|Briefly described|p2|||||||||
27310|Zamu Dolerite|43720|6|Mentioned|Appendix,p23|||||||||
27310|Zamu Dolerite|43726|6|Mentioned|p3|||||||||
27310|Zamu Dolerite|43832|4|Described|11,35,71,73,97||Paleoproterozoic|Age: 1870-1880 Ma.||||||07-NOV-08
27310|Zamu Dolerite|46639|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metadolerite, amphibolite; dolerite and felsic differentiates in south and west.||||||07-NOV-08
27310|Zamu Dolerite|46658|6|Mentioned|p555|||||||||
27310|Zamu Dolerite|46675|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Intrudes the Mount Partridge, South Alligator and Finniss River Groups. Geological Province: Pine Creek Geosyncline.|||||Dolerite and differentiates: amphibolite in east|10-FEB-10
27310|Zamu Dolerite|46700|5|Briefly described|P7, Table1 P10|Carpentarian|Proterozoic|||||||
27310|Zamu Dolerite|49744|5|Briefly described|Fig.3|||||||||
27310|Zamu Dolerite|50586|6|Mentioned|p2.2, 4.5|||Intruded by: Nimbuwah Suite, Cullen Supersuite, Jim Jim Suite. Geological Province: Pine Creek Inlier.||||||
27310|Zamu Dolerite|50623|5|Briefly described|p261|Paleoproterozoic|Paleoproterozoic|Dolerite and gabbro sills of varying thickness.||||||07-NOV-08
27310|Zamu Dolerite|60526|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Massive quartz dolerite.||||||
27310|Zamu Dolerite|60550|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Metadolerite, amphibolite, dolerite, syenite and differentiates.||||||
27310|Zamu Dolerite|60573|6|Mentioned|Regional Setting legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
27310|Zamu Dolerite|60575|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
27310|Zamu Dolerite|60677|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Mafic intrusives, dolerite.||||||
27310|Zamu Dolerite|60680|5|Briefly described|Map legend|Orosirian|Orosirian|Age: 1870Ma?  Geological Province: Pine Creek Orogen. Grey, medium to coarse quartz dolerite, minor hornblende granophyre; rare biotite-hornblende-augite pegmatite.||||||14-JAN-05
27310|Zamu Dolerite|61206|6|Mentioned|p517 Fig.1|Early Proterozoic|Early Proterozoic|||||||
27310|Zamu Dolerite|61403|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|In regional setting map legend.||||||07-NOV-08
27310|Zamu Dolerite|61861|6|Mentioned|p15, Fig.2.|||Pine Creek Orogen. Correlated with older sills in Tanami Region.||||||
27310|Zamu Dolerite|62375|5|Briefly described|p8 Table 1, 9 table 2, 10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Layered tholeiitic dolerite sills and minor dykes. Age: 1890Ma. Thickness: <2500m. Geological Province: Pine Creek Orogen.||||||09-FEB-10
27310|Zamu Dolerite|62378|5|Briefly described|p10|||Intrudes the Gerowie Tuff.||||||
27310|Zamu Dolerite|62580|6|Mentioned|p71|||In the Pine Creek Orogen.||||||07-FEB-11
27310|Zamu Dolerite|63866|4|Described|p107, p109, p112|Orosirian|Orosirian|Central and Nimbuwah Domains, Pine Creek Orogen. Equivalent to parts of the Wangi Basics. Numeric age is interpreted as the maximum age of intrusion as it contains a significant inherited component.|1870 +/- 6 Ma (SHRIMP, Page, OZCHRON)|||Intrudes the Cahill Formation, Nourlangie Schist and Nanambu Complex. Equivalent (in part) to the Wangi Basics.||
27310|Zamu Dolerite|64698|4|Described|lithinterp table|Orosirian|Orosirian|Max thick 2000m. Intrudes Koolpin Formation, Gerowie Tuff, Mount Bonnie Formation and Burrell Creek Formation. Grey, medium to coarse quartz dolerite, minor hornblende granophyre; rare biotite-hornblende-augite pegmatite.|Age ~1850-1860Ma.|||||10-FEB-10
27310|Zamu Dolerite|64730|5|Briefly described|p125 Fig. 3, p126, 140|Paleoproterozoic|Paleoproterozoic|Intrudes South Alligator Group & Finniss River Group prior to widespread deformation & metamorphism. Interpreted SHRIMP zircon crystallisation age of 1870+/-6 Ma (Page 1996) might include xenocrystic zircons. Volcanics in Finniss River Group are dated at ~1860 Ma||||Intrudes South Alligator Group & Finniss River Group.||03-MAY-12
27310|Zamu Dolerite|64731|5|Briefly described|p150|Paleoproterozoic|Paleoproterozoic|May be protolith of Wangi Basics.||||||12-APR-12
27310|Zamu Dolerite|64956|6|Mentioned|p60|||Interlayered with granitoid migmatite of the Nimbuwah Complex.||||||07-FEB-11
27310|Zamu Dolerite|65232|5|Briefly described|p45, p7, p6 Fig. 5, p51|Palaeoproterozoic|Palaeoproterozoic|Sills intrude metasedimentary succession of Namoona, Mount Partridge, South Alligator and Finniss River Groups. Tholeiitic dolerite and gabbro sills; quartz dolerite, granophyre.||||||09-FEB-10
27310|Zamu Dolerite|65339|5|Briefly described|p5 Fig.4, p6 Table 1, pp12-14. |||Has an essentially continental tholeiitic composition with normative hypersthene.||||Intrudes Rum Jungle Complex, Mount Partridge and South Alligator Groups.|Mafic intrusive rock; dolerite metamorphosed to amphibolite.|
27310|Zamu Dolerite|67057|5|Briefly described|p454. |Paleoproterozoic|Paleoproterozoic||1870 +/- 6 Ma.|||Intrudes Cahill Formation and Nourlangie Schist.||
27310|Zamu Dolerite|67167|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartz dolerite, gabbro and amphibolite.|
27310|Zamu Dolerite|67186|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic||||||Quartz dolerite, gabbro and amphibolite.|23-NOV-11
27310|Zamu Dolerite|67232|5|Briefly described|p6.|Paleoproterozoic|Paleoproterozoic|Central Domain, Pine Creek Orogen. Suggested by Dundas et al. (1987a) to be comagmatic with Wangi Basics.||||||
27310|Zamu Dolerite|67323|5|Briefly described|p29|||Pine Creek area. Emplacement age.|~1870-1860 Ma.|||||
27310|Zamu Dolerite|67355|5|Briefly described|p.5, 36, 39, 60; Fig.4, 20, |Orosirian|Orosirian|Preorogenic; deformed and metamorphosed with the sedimentary rocks it intruded. Possible source of metals for polymetallic deposits. Marks the top of the Whites Formation in some locations, and succeeded by the Wildman Siltstone.|c.1870 Ma intrusion.|||||
27310|Zamu Dolerite|67564|4|Described|p7 Table 2, p10 Fig.5, pp31-32, p86.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen. Sills up to 2000 m thick. Continental, pre-orogenic intrusive rock.|1870 +/- 6 Ma (SHRIMP U-Pb).|||Intrudes Burrell Creek Formation and South Alligator Group rocks. Is intruded by David Suite and Oenpelli Dolerite.|An extensive, quartz-rich tholeiite: grey, medium to coarse quartz dolerite; minor granophyre; rare biotite-hornblende-augite pegmatite.|
27310|Zamu Dolerite|67779|5|Briefly described|p14, p20, pp23-24, p87.|||A chemically and isotopically diverse group of widely scattered basement mafic rocks that have undergone deformation and metamorphism. Amphibolites in Caramal and Myra Falls Inliers, previously included in this unit, have been assigned to the Caramal Amphibolite. Sm-Nd isotope chemistry is discussed.||||||18-SEP-14
27310|Zamu Dolerite|67873|6|Mentioned|p43|||||||||
27310|Zamu Dolerite|69418|6|Mentioned|p3:6|||Pine Creek Orogen. Hosts gold deposits (described).||||||12-JUL-16
27310|Zamu Dolerite|69420|5|Briefly described|p5:4, 11, 13-14, 26, 37, 49-52, 60, 62|Paleoproterozoic|Paleoproterozoic|See also 67, 75, 79, 112. Central Domain, Pine Creek Orogen. Absent from Nimbuwah Domain. Composite thickness of c.1.5 km. Hosts the Bons Rush Au deposit. Maximum age from cross-cutting relationship with Gerowie Tuff. A SHRIMP U-Pb zircon age of 1870 +/- 6 Ma (Page, 1996) probably includes inherited zircons. May be of similar age to Maud Dolerite.|<1863 Ma.|||Intrudes Koolpin Formation (South Alligator Group).|A suite of continental tholeiite dolerite sills. Mainly massive, medium- to coarse-grained, grey quartz dolerite. Fractionated phases include hornblende-bearing granophyre, granophyric quartz dolerite and metadiorite.|12-JUL-16
27310|Zamu Dolerite|70293|5|Briefly described|p597, p599-600, p615, p619|Orosirian|Orosirian||1855 Ma.|||Intrudes South Alligator Group: Koolpin Formation, Shovel Billabong Andesite, Mount Bonney Formation, Gerowie Tuff. Is unconformably overlain by El Sherana Group.||
27310|Zamu Dolerite|70866|5|Briefly described|Map legend.|Paleoproterozoic|Paleoproterozoic|Pine Creek Orogen.|||||Grey, medium- to coarse-grained quartz dolerite, gabbro and amphibolite; commonly chloritised.|
27310|Zamu Dolerite|71374|6|Mentioned|p14|||Pine Creek Orogen.||||||04-MAY-18
27310|Zamu Dolerite|71592|5|Briefly described|Appendix A.|||Pine Creek Orogen.|||||Dolerite.|
27310|Zamu Dolerite|73083|6|Mentioned|p5, p36|||Coincident with a prominent high-intensity magnetic anomaly in the Mount Evelyn 1:250k Sheet area and interpreted to comprise a concealed dolerite sill in the Alligator River 1:250K Sheet based on a a prominent high-intensity magnetic anomaly therein.||||||
33727|black soil 33727|44483|5|Briefly described|map legend|Cenozoic|Cenozoic|Black soil.||||||19-NOV-08
31434|dolerite 31434|33759|6|Mentioned|Map legend|Precambrian|Precambrian|Dolerite.||||||
35743|gneiss 35743|33104|6|Mentioned|Map legend|Precambrian|Precambrian|Gneiss; minor schist.||||||
35746|gneiss 35746|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Schistose biotite gneiss, muscovite-biotite schist,calc-silicate rock,layered amphibolite; some biotite and quartzofeldspathic rock,sillimanite and cordierite gneiss,mafic granulite, marble,porphyroblastic feldspar gneiss,massive amphibolite.||||||07-NOV-08
35747|gneiss 35747|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzofeldspathic gneiss, felsic granulite, mafic granulite; subordinate biotite gneiss,  garnet-biotite gneiss; some migmatite and sillimanite gneiss.||||||07-NOV-08
35748|gneiss 35748|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzofeldspathic gneiss, lenses of mafic granulite; some biotite gneiss, cordierite and garnet-bearing quartzofeldspathic gneiss; rare sapphirine and kornerupine-bearing granofels.||||||07-NOV-08
35749|gneiss 35749|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Quartzofeldspathic gneiss, migmatite, biotite gneiss; some garnet-biotite gneiss, amphibolite, mafic granulite, felsic granulite, sillimanite gneiss, actinolite-quartz calc-silicate rock, muscovite-biotite schist.||||||07-NOV-08
35750|gneiss 35750|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Garnet-bearing quartzofeldspathic gneiss; schistose and banded biotite gneiss, locally garnet-bearing; amphibolite.||||||07-NOV-08
35751|gneiss 35751|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Garnet-biotite gneiss, amphibolite, some hornblende gneiss.||||||07-NOV-08
31351|gneisses 31351|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob. Early Palaeoproterozoic||||||07-NOV-08
30721|granite 30721|29811|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
31347|granite 31347|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
31348|granite 31348|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob.Early Proterozoic||||||07-NOV-08
31349|granite 31349|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
31352|granite 31352|39583|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
31433|granite 31433|33759|6|Mentioned|Map legend|Precambrian|Precambrian|Granite.||||||
31696|granite 31696|41408|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
31350|granitic gneiss 31350|39583|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|Prob. Early Palaeoproterozoic. Hornblende-biotite-microcline granitic gneiss, minor amphibolite.||||||07-NOV-08
31431|orthogneiss 31431|33104|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
31432|pegmatite 31432|33104|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
35744|quartzite 35744|33104|6|Mentioned|Map legend|Proterozoic||Mylonized quartzite.||||||
31439|sandstone 31439|33759|6|Mentioned|Map legend|Adelaidean|Adelaidean|Sandstone.||||||
31435|schist 31435|33759|6|Mentioned|Map legend|Precambrian|Precambrian|Schist.||||||
