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
21173|Badja Granodiorite|22815|4|Described|p80|||||||||
21173|Badja Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Badja Suite.||||||19-AUG-08
21206|Beanbah Granite|23171|6|Mentioned|p12,30|||||||||
21206|Beanbah Granite|23173|4|Described|Map Legend|Ludlovian|Ludlovian|||||||
21206|Beanbah Granite|43153|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
21206|Beanbah Granite|43774|3|Fully described|p16-17||Silurian|||||||
21206|Beanbah Granite|68823|6|Mentioned|p377, p378 Fig.4|Late Silurian|Late Silurian|North of Cobar.||||||
21206|Beanbah Granite|69095|5|Briefly described|Map legend|Early Silurian|Early Silurian||||||Poorly exposed biotite granite/granodiorite; coincident with relative magnetic high.|
21206|Beanbah Granite|69541|6|Mentioned|p645 Fig.1(b)|Late Silurian|Late Silurian|Lachlan Orogen.||||||
21206|Beanbah Granite|70941|4|Described|pviii, p7 fig 3, p9, p63-65, p114, ||Early Silurian?|Named for Beanbah Trigonometric station. Previosuly informal. Has not been subdivided or assigned to a suite due to poor exposure.I type granite. Relatively magnetic. Distribution, structure and geomorphology discussed. No type locality is given. Has formed a local contact metamorphic aureole. Displays a magnetic anomaly. Age is unknown but may be maximum early Silurian. Minor molybdenum and metal sulfides are associated with this unit.Contact metamorphosed surrounding rocks. See also p133, p140 fig 58, p141, p145||||Intrudes the Girilambone Group.|Unfoliated massive biotite granite, partially porphyritic.|
21219|Belimebung Volcanics|22638|4|Described|p28|Early Silurian|Late Ordovician|New name. Does not outcrop. Age questionable||||||
21219|Belimebung Volcanics|22857|5|Briefly described|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|||||||
21219|Belimebung Volcanics|24007|5|Briefly described|p326|Ordovician|Ordovician|||||||
21219|Belimebung Volcanics|24101|6|Mentioned|p110|||Geological Province: Lachlan Fold Belt||||||26-NOV-04
21219|Belimebung Volcanics|24417|6|Mentioned|p18|||Not distinguished on the FORBES 1:250 000 sheet.||||||
21219|Belimebung Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
21219|Belimebung Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
21219|Belimebung Volcanics|50191|6|Mentioned|p5 Fig. 4|Silurian|Ordovician|||||||
21219|Belimebung Volcanics|63278|6|Mentioned|p145 Fig. 1|||Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
21219|Belimebung Volcanics|67322|6|Mentioned|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Age is speculative.||||||
21219|Belimebung Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
21219|Belimebung Volcanics|72084|6|Mentioned|p39, p40 Fig.42|||High magnetic response.||||||
21219|Belimebung Volcanics|72495|6|Mentioned|p218, 225, 236, 241|||Also referred to as the Belimebung Igneous Complex on p225, 240.||||||26-MAR-20
21242|Beugamel Sandstone|22831|4|Described|p 66|||||||||
21242|Beugamel Sandstone|22857|4|Described|p448 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Wallingalair Group. Medium to coarse-grained, thickly bedded, diminantly quartzose arenite. Contains brachiopods. Correlative of Yarra Yarra Creek and Trundle Groups. Max. thickness: 180m. Geological Province: Bogan Gate Terrace.||||||
21242|Beugamel Sandstone|24417|3|Fully described|p92|Early Devonian|Early Devonian|Of Trundle Group.  Parts previously included in Hervey Group, Trundle Group and "Wallingalair Beds".  Overlain by Bird Flat Volcanic Member; underlain by Euchabil Gap Formation.  Max. thickness: 150m.||||||
21242|Beugamel Sandstone|43441|5|Briefly described|30||Early Devonian|||||||08-JAN-10
21242|Beugamel Sandstone|44160|5|Briefly described|Map Legend|Emsian|Pragian|||||||08-JAN-10
21242|Beugamel Sandstone|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.||||||
21242|Beugamel Sandstone|60009|5|Briefly described|Map Legend|Emsian|Pragian|Of the Trundle Group.  Overlies: Kadungle Volcanics, Euchabil Gap Formation.||||||13-JUL-04
21242|Beugamel Sandstone|62569|5|Briefly described|p607|Early Devonian|Early Devonian|Of Wallingalair Group. Originally interpreted as Weddin Sandstone by Conolly (1965). Geological Province: Lachlan Fold Belt.||||||10-AUG-07
21249|Billilingra Dacite Member|49690|4|Described|Tb.4, p9-11, p19, p20, p22|Late Silurian|Late Silurian|Type section nominated along the road east of Rothlyn Homestead from GR 982074(base) to GR 975074 (top).|K/Ar age 407 +/- 3 Ma.||||Crystal-rich, greenish-grey, hornblende-biotite dacitic crystal tuff.|11-NOV-14
21260|Bitter Ground Volcanics|22736|4|Described|p611,14,30||Frasnian|||||||
21260|Bitter Ground Volcanics|22857|4|Described|p500 App.1 Tb.A1.7|Frasnian|Frasnian|Basalt, andesite and dacite flows, dolerite intrusions and intercalated tuff, siltstone and arenite. Max. thickness: ~3km.||||||
21260|Bitter Ground Volcanics|44093|5|Briefly described|p67 Fig 6.6|Devonian|Devonian|In the Southern Hastings Block. Geological Province: New England Fold Belt.||||||28-FEB-05
21260|Bitter Ground Volcanics|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
21278|Bogan Schist|22831|2|Defined|p 17|Bendigonian|Lancefieldian|Tottenham Subgroup||||||
21278|Bogan Schist|22857|5|Briefly described|p414 App. 1 Tb. A1.5|Ordovician||Of the Tottenham Subgroup (Girilambone Group). Feldspathic quartz-muscovite schist.||||||
21278|Bogan Schist|24417|5|Briefly described|p14|Ordovician|Ordovician|Of Girilambone Group.||||||
21278|Bogan Schist|43441|3|Fully described|8|||Age: ?Early Ordovician||||||08-JAN-10
21278|Bogan Schist|44160|5|Briefly described|Map Legend|Bendigonian|Lancefieldian|||||||08-JAN-10
21278|Bogan Schist|67322|5|Briefly described|p20|Darriwilian|Tremadocian|Defined by Sherwin (1996). Age from Tottenham Subgroup. Moderately strongly metamorphosed and unfossiliferous. Occurs in the Condobolin - West Wyalong region.||Of the Tottenham Subgroup||||21-FEB-18
21318|Braymont Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
21321|Bredbo Group|22815|4|Described|p35,37,124 fig10,16|Early Devonian|Late Silurian|||||||
21321|Bredbo Group|22857|5|Briefly described|p464 App.1 Tb.A1.6|Silurian|Silurian|Shallow marine, shelfal deposits. Geological Province:Canberra-Yass Shef and Monaro Forearc Basin. See also p468 App.1 Tb.A1.6.||||||
21321|Bredbo Group|23309|6|Mentioned|p390|||||||||
21321|Bredbo Group|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
21321|Bredbo Group|44093|6|Mentioned|p191 App. 1|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||15-JUL-15
21321|Bredbo Group|61413|5|Briefly described|p81, p82 Fig.103.|Late Silurian|Late Silurian|Very low-grade sedimentary and volcanic rocks. Separated from the Cooma Complex by the Murrumbidgee Fault.||||Unconformably overlies Ryrie Formation.|Sedimentary and volcanic rocks|
21321|Bredbo Group|62070|5|Briefly described|p37, p39, p40,|Late Silurian|Late Silurian|Includes limestone in basal formations.|||Includes Cappanana Formation.|||
21321|Bredbo Group|69635|5|Briefly described|p12, 14, 18, 25, 43, 1||||||Includes Colinton Volcanics, Rothlyn Formation.|||
21321|Bredbo Group|70601|5|Briefly described|p28, p34, p43, p55|Late Silurian|Middle Silurian|Monaro region. Post-Benambran Orogeny. Correlated with offshore samples of Pridoli-Lochkovian fossiliferous limestone, limestone, siltstone, felsic volcanics and lithic sandstone.||||Unconformably overlies Yalmy Group.|Quartzose and lithic sandstones, felsic volcanics and limestones.|
21321|Bredbo Group|71069|6|Mentioned|p24, p100, p134|||||||||
21325|Bribbaree Formation|22638|3|Fully described|p18|Early Devonian|Late Silurian|New name||||||
21325|Bribbaree Formation|22857|5|Briefly described|p418 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Siltstone, mudstone, claystone, siliceous siltstone and sandstone.||||||
21325|Bribbaree Formation|23366|5|Briefly described|p13 fig.8|Ordovician|Ordovician|||||||
21325|Bribbaree Formation|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
21325|Bribbaree Formation|44936|5|Briefly described|Map Legend||Ordovician|||||||
21325|Bribbaree Formation|50191|6|Mentioned|p23|Early Silurian|Late Ordovician|||||||
21325|Bribbaree Formation|60280|5|Briefly described|p2, p3 Fig. 1|||||||||
21325|Bribbaree Formation|67322|6|Mentioned|p20|||Warren et al. (1995). Occurs in the Parkes-Forbes-Junee area.|||Flint Hill Chert Member|Possible equivalent of the Kirribilli Formation.||
21325|Bribbaree Formation|67847|5|Briefly described|p21-p22|||||||Equivalent to the Kirribilli, Cotton and Jingerangle Formations.|Inter-bedded sandstones, siltstones and slate.|
21325|Bribbaree Formation|70684|5|Briefly described|p54 Fig.27|Ordovician|Ordovician|Adaminaby Superterrane.||||||21-FEB-18
21325|Bribbaree Formation|72082|5|Briefly described|p22|Late Ordovician|Late Ordovician|Warren et al. (1995). Has similar age, lithology, metamorphic facies, bedding strike/dip, folding and interpreted turbiditic depositional environment, as the Trigalong, Bronxhome and Illabo Formations. Contains Ordovician conodonts.|||Flint Hill Chert Member.|||
21325|Bribbaree Formation|72495|6|Mentioned|p218|Ordovician|Ordovician|Adaminaby Superterrane.|||||Turbidite.|
21339|Brookong Formation|730|5|Briefly described|p23|Early Devonian|Early Devonian|Of Kopyje Group in SW corner of Bourke sheet area.||||||
21339|Brookong Formation|23171|5|Briefly described|p31|||(Glen 1994).||||||
21339|Brookong Formation|23173|4|Described|Map Legend|Lochkovian|Pridoli|||||||
21339|Brookong Formation|42983|6|Mentioned|Fig.3,p345|||||||||
21339|Brookong Formation|43153|5|Briefly described|Map Legend||Lochkovian|of Kopyje Group||||||
21339|Brookong Formation|43774|2|Defined|p24||Lochkovian|||||||
21339|Brookong Formation|65469|6|Mentioned|p14|||Lachlan Orogen.||||||
21339|Brookong Formation|68823|6|Mentioned|p378 Fig.4|Lochkovian|Ludlow|Kopyje Shelf, Lachlan Orogen.||Unit in Kopyje Group.||||
21339|Brookong Formation|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
21339|Brookong Formation|71360|5|Briefly described|Map legend|||Mapped in the same unit as the Meryula Formation, "Little Mountain Formation", and Drysdale Conglomerate Member extending from the Cobar 1:100 000 map sheet area.||Kopyje Group.||||
21339|Brookong Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Thin-bedded siltstone and fine quartzose to lithic sandstone, basal boulder to granule polymictic conglomerate.|
21339|Brookong Formation|73143|5|Briefly described|p1-4|||Lachlan Orogen. Cobar Superbasin, northern.||Kopyje Group|Elura Limestone Member|Interfingers with Elura Limestone Member, underlies CSA siltstone.|Thinly bedded siltstone, fine-grained quartzose to lithic sandstone and basal conglomerate. Includes fossiliferous sandstone and mudstone.|
21339|Brookong Formation|73174|5|Briefly described|p1036-1043, p1045|Lochkovian|Lochkovian|Kopyje Shelf. Contains age-diagnostic brachiopod.|425 +/- 7.3 Ma U-Pb LA-ICP-MS MDA|Kopyje Group, Cobar Supergroup||Equivalent to Meryula Formation and Baledmund Formation.|Basal conglomerate facies and overlying sandstone-mudstone facies including thick, cross-bedded sandstone.|24-NOV-22
21388|Burilda Granite|22815|4|Described|p88|||||||||
21388|Burilda Granite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
21409|Cabonne Group|22529|6|Mentioned|1|Late Ordovician|Late Ordovician|||||||
21409|Cabonne Group|22679|5|Briefly described|p 12|||||||||
21409|Cabonne Group|22798|6|Mentioned|p851 Fig.2||Ordovician|||||||
21409|Cabonne Group|22857|4|Described|p129, p422 App. 1, Tb. A1.5|Early Silurian|Late Ordovician|See also p424 App. 1 Tb.A1.5.||||||
21409|Cabonne Group|23043|5|Briefly described|Map Legend|Llandovery|Yapeenian|||||||
21409|Cabonne Group|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
21409|Cabonne Group|23170|2|Defined|p31 Fig.3|Bolindian|Darriwilian|Age: early Darriwilian - Late Bolindian (Ordovician). Thickness varies from 800 - 4000m.||||||
21409|Cabonne Group|23202|6|Mentioned|Fig.1||Ordovician|||||||
21409|Cabonne Group|23213|5|Briefly described|p10,13,20|Late Ordovician|Ordovician|Age: Middle to Late Ordovician. May include older Mitchell Formation that has not been recognised outside Bakers Swamp area.||||||
21409|Cabonne Group|23214|4|Described|p51|Llandovery|Darriwilian|Characterised by intermediate to mafic, often potassic (shoshonitic), volcanism and associated volcaniclastic products. Max. thickness 4500m.||||||04-MAR-09
21409|Cabonne Group|23245|6|Mentioned|p129|||||||||
21409|Cabonne Group|23309|6|Mentioned|p390|||||||||
21409|Cabonne Group|23454|5|Briefly described|p33|Ordovician|Ordovician|||||||
21409|Cabonne Group|24233|5|Briefly described|p256|Ordovician|Ordovician|Geological Province: Lachlan Orogen.||||||
21409|Cabonne Group|24417|5|Briefly described|p164|Ordovician|Ordovician|||||||
21409|Cabonne Group|42712|4|Described|5, 12, 19|Late Ordovician|Early Ordovician|||||||
21409|Cabonne Group|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
21409|Cabonne Group|43494|6|Mentioned|p16|Silurian|Ordovician|Includes the Kabadah Formation.||||||16-MAR-06
21409|Cabonne Group|43639|5|Briefly described|Map Legend||Ordovician|||||||
21409|Cabonne Group|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes; Angullong Formation, Forest Reefs Volcanics, Millambri Formation, Malongulli Formation, Weemalla Formation, Mount Pleasent Basalt Member.||||||15-JUL-08
21409|Cabonne Group|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Inculdes; Blayney Volcanics, Cowringa Limestone Member, Forest Reefs Volcanics, Rockley Volcanics, Weemalla Formation, Mount Pleasent Basalt Member, Byng Volcanics.||||||
21409|Cabonne Group|43782|5|Briefly described|Map Legend|Llandovery|Darriwilian|||||||
21409|Cabonne Group|44093|5|Briefly described|p201 App. 1|Early Silurian|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
21409|Cabonne Group|50231|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Includes: Kenyu Formation.||||||
21409|Cabonne Group|50590|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes: Oakdale Formation, Wooloo Limestone Member.||||||
21409|Cabonne Group|63287|4|Described|p316, p316 Fig. 1, p317 Fig. 2, p334-335|Late Ordovician|Late Ordovician|Includes; Malongulli Fm, Malachis Hill Fm, Millambri Fm, Angullong Fm, Cheesemans Creek Fm. Geological Province: Molong Volcanic Belt. Consists of volcanic/volcaniclastic successions.||||||07-FEB-11
21409|Cabonne Group|63290|5|Briefly described|p400 Fig. 5(b)|Ordovician|Ordovician|Geological Province: Molong Volcanic Belt. Consists of volcanics and volcaniclastics.||||||
21409|Cabonne Group|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Includes Kenyu Formation and Rockley Volcanics.||||||
21409|Cabonne Group|64826|5|Briefly described|p1040 Tb. 1|Bolindian|Bolindian|Contains Reedy Creek Limestone, Angullong and Oakdale Formations.||||||
21409|Cabonne Group|66185|5|Briefly described|p397, p399|Late Ordovician|Middle Ordovician|Contains the Kenyu Formation.||||||
21409|Cabonne Group|67322|4|Described|p4 Fig.2, p21-23, p25, p39; Fig.5|Late Ordovician|Middle Ordovician|Macquarie Arc. Defined by Pogson (in Pogson and Watkins 1998), the Cabonne Group has now subsumed both the Barrajin and Kenilworth Groups as a result of reassessment of stratigraphic relationships on the Dubbo 1:250 000 sheet (Meakin and Morgan 1999) and Goulburn 1:250 000 sheet (Thomas et al. in press).|||Coomber Formation, Tucklan Formation, Burranah Formation, Bowan Park Limestone Subgroup, Cargo Volcanics, Byng Volcanics.|Now a correlate of Northparkes Group.||21-FEB-18
21409|Cabonne Group|67847|5|Briefly described|p32|||Previously included the Kabadah Formation.||||||
21409|Cabonne Group|68003|5|Briefly described|p23, p24 Fig.3-e, p147. |Bolindian|Darriwilian|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Oakdale, Kabadah and Tucklan Formations.||Basalt, basaltic andesite, latite lava and intrusions; chert; volcaniclastic siltstone, sandstone; limestone, calcareous breccia.|
21409|Cabonne Group|68004|6|Mentioned|pp115-116, p125.|Late Ordovician|Late Ordovician|Mineral potential and level of certainty are discussed.||||||
21409|Cabonne Group|68310|6|Mentioned|p237|||Cowra-Canowindra region.||||||
21409|Cabonne Group|68592|2|Defined|p74 Tb.5, p127,p280, p370-400,p426,p1170|Late Ordovician|Middle Ordovician|Defined by Pogson and Watkins (1998) after Glen and Watkins (1994); revised by Meakin and Morgan (1999) and redefined here (Pogson and Thomas, 2012). Now considered to include all intermediate to mafic volcanic/volcaniclastic and carbonate sequences of the Molong-Wellington and Rockley-Gulgong volcanic belts of Middle to Late Ordovician age. Also includes Cheesemans Creek, Tucklan, Burranah, Coomber, Triangle Formations; Sourges Shale; Gunnars Dam beds; Mozart Chert; Reedy Creek, Cargo Creek, Canomodine, Regans Creek, Limestones; Gidyen Volcanics; Cliefden Caves Limestone, Bowan Park Limestone, Subgroups. Exposed in two extensively faulted meridional belts. Goulburn structural zone: deformation and metamorphism described.|||Kenyu, Oakdale, Malachis Hill, Millambri, Angullong, Malongulli, Coombing, Weemalla Formations; Rockley, Fairbridge, Forest Reefs, Milthorpe, Byng, Blayney, Walli, Cargo Volcanics; see Comments.|||
21409|Cabonne Group|70036|5|Briefly described|Map legend|Ordovician|Ordovician|Lachlan Fold Belt. Included in a mapped unit of strongly deformed basaltic metasedimentary rocks, basalt, conglomerate, sandstone and mudstone.||||||
21409|Cabonne Group|70192|5|Briefly described|Map Legend|Bolindian|Darriwilian|On Boorowa and Taralga 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Rockley Volcanics, Kenyu Formation.|||
21409|Cabonne Group|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 intrusions and volcanic units.|||Formation: Oakdale, Malachis Hill, Millambri, Angullong, Cheesemans Creek. Volcanics: Sofala, Rockley, Blayney, Forest Reefs, Byng, Millthorpe. Subgroup: Bowan Park Limestone, Cliefden Caves Limestone|||
21409|Cabonne Group|70543|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes Rockley Volcanics|||
21409|Cabonne Group|70545|5|Briefly described|Map Legend|Ordovician|Ordovician||||Includes the Kenyu Formation.|||
21409|Cabonne Group|71069|6|Mentioned|p52|||Macquarie Arc. Author makes clear that the proposed interbedding with the Adaminaby Group has not been demonstrated conclusively.||||||
21409|Cabonne Group|71656|5|Briefly described|p12 Fig.2, p16|Bolindian|Darriwilian|Only shown in correlation chart (Fig.2).|||Includes Kenyu Formation.|Shown as largely equivalent to Bendoc Group.||
21409|Cabonne Group|72263|5|Briefly described|p515-517|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen.|||Includes Fairbridge Volcanics.|Underlain unconformably by Hensleigh Formation.||
21429|Candelo Tonalite|22815|4|Described|p72|||||||||
21429|Candelo Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Candelo Suite.||||||
21487|Chellington Quartz Syenite|22638|4|Described|p78||Late Devonian|New name.||||||
21487|Chellington Quartz Syenite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
21510|Cobargo Granodiorite|22815|4|Described|p68|Early Devonian|Late Silurian|||||||
21510|Cobargo Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Cobargo Suite.||||||
21515|Coco Range Sandstone|22518|4|Described|Table 1, p 4, 7|Middle Devonian|Early Devonian|Mulga Downs Group, Darling Basin||||||
21515|Coco Range Sandstone|22730|2|Defined|p557-9, 566,68|Eifelian|Emsian|upgrading of Coco Range beds of Ward et al 1969.  Contains 5 units including The Valley Tank and Copi Dam Arenites.||||||
21515|Coco Range Sandstone|22768|5|Briefly described|p165,185|Eifelian|Emsian|||||||
21515|Coco Range Sandstone|22857|4|Described|p165, p183, p210, p486 App.1 Tb.A1.7|Middle Devonian|Early Devonian|Fine arenite with fish fossils. Max. thickness: >1320m. Geological Province: Ravendale Basin.||||||
21515|Coco Range Sandstone|22859|5|Briefly described|p210||Emsian|||||||
21515|Coco Range Sandstone|23336|4|Described|p15, p17 Fig. 12|Givetian|Pragian|Of the Mulga Downs Group. Supersedes Coco Range Beds. Classified by Neef et al (1995) into Lower Fine Arenite, The Valley Tank Member Arenite , Central Fine Arenite,  Copi Tank Member and Upper Fine Arenite.||||||21-MAR-06
21515|Coco Range Sandstone|23380|5|Briefly described|p109|Middle Devonian|Early Devonian|Equivalent to Snake Cave Sandstone and lower Mulga Downs Group. Age: Emsian - Eifelian. of Wonaminta Block.||||||
21515|Coco Range Sandstone|24241|5|Briefly described|p15 Fig.2|Devonian|Devonian|Geological Province: Darling Basin.||||||
21515|Coco Range Sandstone|44093|5|Briefly described|p140 App. 1|Early Carboniferous|Early Devonian|Underlies Nundooka Sandstone. Geological Province: Kanmantoo Fold Belt.||||||
21515|Coco Range Sandstone|60648|4|Described|p43-44|Eifelian|Emsian|Of Mulga Downs Gp. Subdivided into the Upper Fine Arenite, Copi Dam Arenite Member, Central Fine Arenite, The Valley Tank Pebbly Arenite Member & Lower Fine Arenite.Contains very rare body & trace fossils. Max. thickness: 1320m. Geol.Prov: Darling Basin.||||||28-APR-05
21515|Coco Range Sandstone|65759|6|Mentioned|p114 Fig.2|||Darling Basin. Includes Copi Dam Arenite Member. Fluvial. (Is this the same as Coco Range Beds?)||||||
21515|Coco Range Sandstone|66589|6|Mentioned|p179|Eifelian|Emsian|Case studies cited; not visited in the field by the authors of this study.||||||
21515|Coco Range Sandstone|67562|6|Mentioned|p103 Fig.9||||||Includes Copi Dam Arenite Member and The Valley Tank Arenite Member.|||23-JAN-17
21522|Combaning Formation|22638|3|Fully described|p60|Early Devonian|Late Silurian|New name. Probably equivalent to the Derriwong/ Trundle Groups.||||||
21522|Combaning Formation|22685|5|Briefly described|p728,Fig1p729,732|Early Devonian|Late Silurian|Siltstone, sandstone, felsic volcanics and minor conglomerate.||||||17-JAN-06
21522|Combaning Formation|22857|5|Briefly described|p450 App.1, Tb.A1.6|Early Devonian|Late Silurian|Siltstone, arenite, shale, conglomerate, minor felsic volcanics. Contains trilobites, brachiopods, lamellibranchs, corals.||||||
21522|Combaning Formation|23309|6|Mentioned|p390|||||||||
21522|Combaning Formation|24101|6|Mentioned|p108|Devonian|Silurian|Geological Province: Lachlan Fold Belt||||||
21522|Combaning Formation|24417|5|Briefly described|p65|||Cootamundra 1:250 000 map sheet.||||||
21522|Combaning Formation|44192|5|Briefly described|Map Legend|Lochkovian|Ludlovian|||||||
21522|Combaning Formation|44936|5|Briefly described|Map Legend|Devonian|Silurian|Derriwong Group.||||||
21522|Combaning Formation|50191|6|Mentioned|p6, 11|||Of the Derriwong Group.||||||
21522|Combaning Formation|65890|6|Mentioned|p159|Early Devonian|Late Silurian|Sedimentary rocks. Intruded by Middledale Gabbroic Diorite.||||||13-APR-11
21522|Combaning Formation|69801|6|Mentioned|p3, p45, p138|Early Devonian|Late Silurian|Eastern Lachlan Orogen. Hosts trilobite and brachiopod assemblages.||||Intruded by the Gundibindyal Granite.|Locally fossiliferous sedimentary rocks.|
21522|Combaning Formation|72082|5|Briefly described|p4, p7, p25, p33|Early Devonian|Late Silurian|||||Possibly overlies unconformably the Temora Volcanics. Is faulted against the Trigalong Formation.|Metasedimentary rocks.|08-JAN-20
21522|Combaning Formation|72084|5|Briefly described|p2, p15, p41-43|Devonian|Silurian|Occupies an elongate NNW-SSE trending basin of low magnetic response. Forms hills.|||||Metasedimentary rocks including lithic sandstone and conglomerate.|
21532|Connemarra Formation|22831|3|Fully described|p 61|Pragian|Lochkovian|||||||
21532|Connemarra Formation|22857|4|Described|p446 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Trundle Group. Siltstone, mudstone and marl; limestone lenses. Contains brachiopods, conodonts. Max. thickness: 1350m. Geological Province: Bogan Gate Terrace.||||||
21532|Connemarra Formation|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
21532|Connemarra Formation|43441|5|Briefly described|29||Early Devonian|||||||08-JAN-10
21532|Connemarra Formation|44160|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||08-JAN-10
21532|Connemarra Formation|50077|6|Mentioned|p19|Devonian|Devonian|||||||
21532|Connemarra Formation|61894|6|Mentioned|p179 Fig.3|||||||||
21532|Connemarra Formation|62569|5|Briefly described|p606|Early Devonian|Early Devonian|Middle unit of Trundle Group. Geological Province: Lachlan Fold Belt. Contains a late Lochkovian-early Pragian brachiopod-conodont fauna.||||||10-AUG-07
21532|Connemarra Formation|66498|6|Mentioned|p42-43, 45|||||||||
21546|Coolumbooka Granodiorite|22815|4|Described|p83||Early Devonian|Rb/Sr Age: 396Ma.||||||
21546|Coolumbooka Granodiorite|23329|5|Briefly described|1042|Early Devonian|Early Devonian|||||||
21546|Coolumbooka Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Coolumbooka Suite.||||||
21553|Coonardoo Sandstone|22831|2|Defined|p64-65|Devonian|Devonian|Of the Wallingalair Group.||||||01-NOV-13
21553|Coonardoo Sandstone|22857|4|Described|p448 App.1, Tb.A1.6|Pragian|Pragian|Of Wallingalair Group. Medium to coarse arenite, pebbly to conglomeratic arenite; contains brachiopods, conodonts, fish plates. Max. thickness: 300m. Geological Province: Bogan Gate Terrace.||||||21-MAY-08
21553|Coonardoo Sandstone|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
21553|Coonardoo Sandstone|24417|3|Fully described|p89|Early Devonian|Early Devonian|Of Trundle Group.  Previously assigned to Troffs Formation.  Overlain by Euchabil Gap Formation; underlain by Yarrabandai Formation.  Max. thickness: 100m.||||||
21553|Coonardoo Sandstone|43441|5|Briefly described|30||Early Devonian|||||||08-JAN-10
21553|Coonardoo Sandstone|44160|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||08-JAN-10
21553|Coonardoo Sandstone|60009|5|Briefly described|Map Legend|Pragian|Lochkovian|Of the Trundle Group. Underlies: Kadungle Volcanics, Euchabil Gap Formation.||||||13-JUL-04
21553|Coonardoo Sandstone|62569|5|Briefly described|p606 Fig. 1D, p612|Late Devonian|Givetian|Basal unit of Wallingalair Group. Geological Province: Lachlan Fold Belt. Contains the Boor Hill fossil fish locality. New age: Givetian or younger||||||21-AUG-12
21568|Cowangara Formation|22736|2|Defined|p617|Tournaisian|Famennian|southern Hastings Block unit||||||
21568|Cowangara Formation|22857|4|Described|p500 App.1 Tb.A1.7|Tournaisian|Famennian|Interdigitates with Rollans Road Formation. Cleaved turbiditic siltstone, arenite, lithic arenite, rare conglomerate lenses; bioturbation. Max. thickness: >2km.||||||
21568|Cowangara Formation|43755|6|Mentioned|Fig.1,p548|Carboniferous|Devonian|||||||
21568|Cowangara Formation|44093|5|Briefly described|p232 App. 1|Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||26-MAY-08
21568|Cowangara Formation|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
21568|Cowangara Formation|71628|6|Mentioned|p17:74|||||||Is intruded by Hannam Vale Granodiorite.||
21594|Currumburrama Volcanics|22638|4|Described|p27|Early Silurian|Late Ordovician|New name. Does not outcrop. Age questionable||||||
21594|Currumburrama Volcanics|22857|6|Mentioned|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|||||||
21594|Currumburrama Volcanics|24417|5|Briefly described|p33|||Of Bacchin et al (1999).||||||
21594|Currumburrama Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
21594|Currumburrama Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
21594|Currumburrama Volcanics|50191|6|Mentioned|p5 Fig. 4|Silurian|Ordovician|||||||
21594|Currumburrama Volcanics|67322|6|Mentioned|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Southernmost part of the Junee-Narromine Volcanic Belt. Age is speculative. Only recognised subsurface from borehole intersections.||||||21-FEB-18
21669|Dirnaseer Gabbro|22638|4|Described|p79|Early Devonian|Late Silurian|Previously "Dirnaseer basic intrusion"||||||
21669|Dirnaseer Gabbro|22685|5|Briefly described|Fig1p729|Late Devonian|Late Devonian|Gabbro.||||||17-JAN-06
21669|Dirnaseer Gabbro|44192|5|Briefly described|Map Legend||Famennian|||||||
21669|Dirnaseer Gabbro|44936|5|Briefly described|Map Legend||Late Devonian|||||||
21693|Dramoore Granodiorite|22815|4|Described|p62|||||||||
21693|Dramoore Granodiorite|43233|5|Briefly described|Map Legend||Silurian|Possible Silurian age. Of Cooma Suite.||||||
21740|Ellenborough Volcanics|22616|6|Mentioned|Fig.1 p670|Devonian|Devonian|||||||
21740|Ellenborough Volcanics|22736|2|Defined|p615,627,9|Famennian|Frasnian|southern Hastings Block unit||||||
21740|Ellenborough Volcanics|22857|4|Described|p502 App.1 Tb.A1.7|Frasnian|Frasnian|Basaltic and andesitic massive flows and rare pillow lava and breccia; intercalations of of thinly bedded to laminated mudstone, siltstone, sandstone and ashfall tuff. Pass laterally into Birdwood Formation. Max. thickness: 2000m.||||||17-FEB-06
21740|Ellenborough Volcanics|44093|5|Briefly described|p 67 Fig 6.6|Devonian|Devonian|Geological Province: Southern Hastings Block.||||||
21740|Ellenborough Volcanics|70939|6|Mentioned|p826, p828|Devonian|Devonian|Southern Hastings Block.||||||
21773|Farmborough Claystone Member|24471|4|Described|p27, p29 Fig.2, p37-39|Late Permian|Late Permian|Tuff. Geochemical correlation with Warners Bay Tuff. Within Wongawilli Coal. Of Illawarra Coal Measures. Thickness: 0.49-1.3 m. Geological Province: Sydney Basin.||||||07-FEB-11
21778|Fermoy Volcanics|22831|4|Described|p 47|Lochkovian|Pridolian|||||||
21778|Fermoy Volcanics|22857|5|Briefly described|p448 App.1, Tb.A1.6|Pridolian|Pridolian|Of the Derriwong Group. Feldspar porphyry lava or shallow intrusion. Max. thickness: 200m. Geological Province: Bogan Gate Terrace.||||||
21778|Fermoy Volcanics|43441|5|Briefly described|27|Early Devonian|Late Silurian|||||||08-JAN-10
21778|Fermoy Volcanics|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
21794|Five Hundred Acre Granodiorite|22815|4|Described|p62|||||||||
21794|Five Hundred Acre Granodiorite|23866|5|Briefly described|p122 Fig. 2|||Also in text as 500 Acre Granodiorite.  Geological Province: Murrumbidgee Batholith.||||||
21794|Five Hundred Acre Granodiorite|43233|5|Briefly described|Map Legend||Late Silurian|Possible Silurian age. Of Shannons Flat Suite.||||||
21799|Flint Hill Chert Member|22638|4|Described|p19|Early Devonian|Late Silurian|Bribbaree Formation. New name.||||||
21799|Flint Hill Chert Member|22857|4|Described|p418 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Bribbaree Formation. Dark grey-blue to black, generally thinly bedded chert.||||||
21799|Flint Hill Chert Member|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
21799|Flint Hill Chert Member|67322|5|Briefly described|p20|Darriwilian|Darriwilian|Darriwilian conodonts have been found in this Formation. Occurs in the Parkes-Forbes-Junee area.||Of the Bribbaree Formation|||Isolated chert unit.|21-FEB-18
21799|Flint Hill Chert Member|72082|5|Briefly described|p22|Darriwilian|Darriwilian|Age from conodonts. The chert may pre-date the sedimentary rocks of the "parent".||Bribbaree Formation.||||08-JAN-20
21800|Flixton Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Maules Creek Sub-basin, Gunnedah Basin.||Maules Creek Formation.||||
21817|Frogs Hollow Granodiorite|22815|4|Described|p77|||||||||
21817|Frogs Hollow Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Glenbog Suite.||||||
21817|Frogs Hollow Granodiorite|68592|6|Mentioned|p1675|Early Devonian|Early Devonian|||Unit in Glenbog Suite.||||
21833|Garland Granodiorite|22679|3|Fully described|p 45||Silurian|||||||
21833|Garland Granodiorite|23214|3|Fully described|p164|Late Silurian|Late Silurian|Intrudes the Adaminaby Group and Weemalla Formation. Typically moderately foliated, leucocratic, biotite-hornblende granodiorite. Reduced I-type granodiorite. Geological Province: Wyangala Batholith.||||||17-JUL-08
21833|Garland Granodiorite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of leucocratic, foliated, porphyritic to granophyritic, hornblende biotite granodiorite.||||||15-JUL-08
21833|Garland Granodiorite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Leucocratic, foliated, porphyritic to granophyritic, hornblende biotite granodiorite.||||||17-JUL-08
21833|Garland Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Of Wyangala Batholith.||||||15-JUL-08
21833|Garland Granodiorite|63285|6|Mentioned|p291 App. 1|Silurian|Silurian|||||||
21833|Garland Granodiorite|68592|6|Mentioned|p1305|Late Silurian|Late Silurian|In the Bathurst 1:250 000 map sheet area.||||Is intruded by Wyangala Granite.||
21833|Garland Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
21844|Gidginbung Volcanics|22434|6|Mentioned|11|||Host to Temora gold deposit. Geol province Lachlan Fold Belt||||||
21844|Gidginbung Volcanics|22638|4|Described|p23|Llandovery|Ashgillian|435 Ma zircon.||||||
21844|Gidginbung Volcanics|22857|4|Described|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Intermediate volcanic and volcaniclastic rocks. Age: 435+/-5Ma (U/Pb zircon).||||||24-FEB-06
21844|Gidginbung Volcanics|24007|5|Briefly described|p326|Ordovician|Ordovician|||||||
21844|Gidginbung Volcanics|24101|6|Mentioned|p109 Fig.2|||Geological Province: Lachlan Fold Belt||||||
21844|Gidginbung Volcanics|24417|6|Mentioned|p37|||||||||
21844|Gidginbung Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
21844|Gidginbung Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
21844|Gidginbung Volcanics|50191|6|Mentioned|p5, 16 Fig. 4|Early Silurian|Late Ordovician|||||||
21844|Gidginbung Volcanics|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Intermediate-mafic volcanics, intrusives and sediments.||||||
21844|Gidginbung Volcanics|63278|5|Briefly described|p145 Fig. 1, p149|Early Silurian|Early Silurian|Various ages, Early Ordovician age from a conodont species, 439-438Ma. Geol Prov: Junee-Narromine Volcanic Belt, LFB. Consists of strongly altered intermediate volcanic + volcaniclastic rocks, intruded by granodiorites to monzodiorites.||||||07-FEB-11
21844|Gidginbung Volcanics|64963|5|Briefly described|p182 Fig. 2|||Age: 439-436Ma (U-Pb unpublished/quote from Percival and Glen 2007).||||||22-APR-09
21844|Gidginbung Volcanics|67107|5|Briefly described|p689|||Located 16km WNW of Temora.|435 +/- 2.5 Ma (MDA, from andesite flow).||||A suite of volcanic (including an andesite flow) and volcanic-derived sedimentary rocks with coeval diorite, monzodiorite and quartz monzonite intrusions.|
21844|Gidginbung Volcanics|67322|6|Mentioned|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Overlain by early Llandovery limestone: most likely, part of the Ordovician arc sequence.|||||High K calc-alkaline to shoshonitic affinities.|
21844|Gidginbung Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||||||
21844|Gidginbung Volcanics|72082|6|Mentioned|p4|Silurian|Silurian|||||||
21844|Gidginbung Volcanics|72084|5|Briefly described|p12, p39, p40 Fig.42|Early Silurian|Late Ordovician|High magnetic response.||||Correlated with Junawarra Volcanics.||
21844|Gidginbung Volcanics|72495|5|Briefly described|p218, 227, p234, p236|||Described by Warren et al, 1995. Aeromagnetic data suggests this units is <7km wide and up to 66km long.||||Faulted against the Wagga Group.|Intermediate volcanic and volcaniclastic rocks, dominated by altered andesite, associated with volcaniclastic sediments, intruded by a range of bodies from granodiorite to monzodiorite.|
21844|Gidginbung Volcanics|72528|5|Briefly described|p1, p31-32, p108-9.|Telychian|Telychian|Mineralised. Part of the Macquarie Igneous Province.|Age range c. 439 Ma to  c.434 Ma.|||||
21844|Gidginbung Volcanics|73154|5|Briefly described|p77 Fig.3|Llandovery|Bolindian|Macquarie Arc, Phase 4. Junee-Narromine Belt|||||Intermediate-mafic lava.|
21854|Glen Ayr Syenite|22679|4|Described|p 39|Late Ordovician|Late Ordovician|||||||
21854|Glen Ayr Syenite|23100|5|Briefly described|p575 (Fig 1)||Ordovician|||||||
21854|Glen Ayr Syenite|23202|6|Mentioned|Fig.1||Ordovician|||||||
21854|Glen Ayr Syenite|23214|2|Defined|p91|Late Ordovician|Late Ordovician|Intrudes the Weemalla Formation and Forest Reefs Volcanics. Medium to coarse grained pale biotite-ferrohastingsite-ferrosilite syenite.||||||
21854|Glen Ayr Syenite|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Biotite syenite, biotite clinopyroxene monzonite.||||||17-JUL-08
21854|Glen Ayr Syenite|43782|6|Mentioned|Map Legend|Bolindian|Bolindian|||||||
21854|Glen Ayr Syenite|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
21904|Greenbah Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
21911|Gresham Granite|22679|5|Briefly described|p 28|Carboniferous|Carboniferous|||||||
21911|Gresham Granite|23214|3|Fully described|p250|Carboniferous|Carboniferous|Of Bathurst Batholith. Intrudes the Crudine Group and the Cunningham Formation.||||||
21911|Gresham Granite|43127|5|Briefly described|p4,Fig.2,Fig.3|||Middle Carboniferous||||||
21911|Gresham Granite|43653|5|Briefly described|Map Legend||Carboniferous|||||||
21911|Gresham Granite|43654|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Of Bathurst Batholith. Graphic biotite granite, porphyritic granite, doritic enclaves, aplite.||||||17-JUL-08
21911|Gresham Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of Bathurst Batholith.||||||17-JUL-08
21911|Gresham Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
21915|Grogan Volcanics|22638|4|Described|p27|Early Silurian|Late Ordovician|New name. Does not outcrop. Age questionable||||||
21915|Grogan Volcanics|22857|5|Briefly described|p418 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|||||||
21915|Grogan Volcanics|44192|5|Briefly described|Map Legend||Bolindian|||||||
21915|Grogan Volcanics|44936|5|Briefly described|Map Legend||Ordovician|||||||
21915|Grogan Volcanics|50191|6|Mentioned|p5 Fig. 4|Silurian|Ordovician|||||||
21915|Grogan Volcanics|63278|6|Mentioned|p145 Fig. 1|||Geological Province: Junee-Narromine Volcanic Belt, LFB.||||||07-FEB-11
21915|Grogan Volcanics|67322|6|Mentioned|p23|Ordovician|Ordovician|Defined and Ordovician age assigned by Warren et al. (1995). Age is speculative. Only recognised from (subsurface) borehole intersections.||||||22-FEB-18
21915|Grogan Volcanics|70684|6|Mentioned|p3|||Junee-Narromine Volcanic Belt.||||||
21923|Gunningrah Tonalite|22815|4|Described|p84|||||||||
21923|Gunningrah Tonalite|23329|5|Briefly described|1042|Silurian|Ordovician|||||||
21923|Gunningrah Tonalite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Kelvin Suite.||||||
21940|Hangmans Creek Granodiorite|22815|4|Described|p87|||||||||
21940|Hangmans Creek Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
21981|Hughies Bore beds|22893|2|Defined|p19,20||Late Devonian|Thickness unknown because of limited outcropping.||||||
21981|Hughies Bore beds|44188|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of Mulga Dowsn Group. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Fine- to medium-grained quartz arenite, low angle cross-beds and trough crossbeds; sporadsic interbeds with silicified siltstone or mudstone intra-clasts.||||||15-MAY-08
21983|Huntley Claystone Member|24471|4|Described|p27, 37-39 p29 Fig.2|Late Permian|Late Permian|Tuff. Within Bargo Claystone. Thickness: 1.14 m. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
21983|Huntley Claystone Member|73304|6|Mentioned|p65-66|||Sample PCW266 dated. From core hole Tower DDH 20, 600.37 m depth, 6 km southeast of
Appin, S34.185243 E150.884432. [Superseded by Huntley Claystone?].||Illawarra Coal Measures||||
21987|Hyde Creek Granodiorite|22815|5|Briefly described|p74-5|||||||||
21987|Hyde Creek Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Hyde Creek Suite.||||||
21988|Hyndmans Creek Formation|22736|2|Defined|p619,29|Namurian|Visean|Southern Hastings Block unit, author recommends use as replacement for lower section of Cooperabung Formation.||||||12-OCT-15
21988|Hyndmans Creek Formation|22857|4|Described|p500 App.1 Tb.A1.7|Visean|Visean|Age is inferred. Dark siltstone, interbedded fine lithic sandstone. Unconformably overlain by Mingaletta Formation. Max. thickness: 2000m. Geological Province: Tamworth Forearc Basin.||||||24-FEB-06
21988|Hyndmans Creek Formation|44093|5|Briefly described|p67 Fig. 6.6|Carboniferous|Carboniferous|In the Southern Hastings Block. Geological Province: New England Fold Belt.||||||
21988|Hyndmans Creek Formation|66090|6|Mentioned|p4, p8, pp18-19 map.|Early Carboniferous|Early Carboniferous|Southern Hastings Block. Part of the floor of the Lorne Basin.||||||
21988|Hyndmans Creek Formation|70939|6|Mentioned|p826, p828|Carboniferous|Carboniferous|Southern Hastings Block.||||||
21988|Hyndmans Creek Formation|71628|5|Briefly described|p17: 55, 78|||Hastings Block.||Quintoc Group.||Is intruded by Cairncross Monzogranite and Lorne Forest Granodiorite.||
21992|Illabo Formation|22638|4|Described|p21||Late Ordovician|New name.||||||
21992|Illabo Formation|22685|5|Briefly described|Fig1p729|Late Ordovician|Late Ordovician|Siltstone, chert, sandstone.||||||17-JAN-06
21992|Illabo Formation|22857|4|Described|p418 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Interbedded siltstone, chert and siliceous siltstone with minor sandstone intervals.||||||
21992|Illabo Formation|23309|6|Mentioned|p390|||||||||
21992|Illabo Formation|44192|5|Briefly described|Map Legend|Llandoverian|Eastonian|||||||
21992|Illabo Formation|72082|5|Briefly described|p22|Late Ordovician|Late Ordovician|Warren et al. (1995). Has similar age, lithology, metamorphic facies, bedding strike/dip, folding and interpreted turbiditic depositional environment, as the Trigalong, Bribbaree and Bronxhome Formations. Contains poorly-preserved graptolites which are the basis for the age interpretation.||||||08-JAN-20
21992|Illabo Formation|72084|5|Briefly described|p9|Late Ordovician|Late Ordovician|Warren et al. (1995), for exposures in Gerelgembeth Pit on the S side of Olympic Highway. Age from poorly-preserved graptolites. Deposition was contemporaneous with Bendoc Group.|||||Deformed sequence of siltstone, chert, siliceous siltstone and minor sandstone.|
21998|Ingalara Ashstone Member|49690|4|Described|Tb.2, p5, p8, p10,|Late Silurian|Late Silurian|Distinctive marker bed. Type section is along Ingalara Creek from GR 921350 to GR 928353.||Of the Colinton Volcanics||Is overlain by Rothlyn Formation.|Pale buff to white, siliceous, fine-grained tuff or ashstone. Consists of white to very pale grey, fine-grained, massive to faintly banded rhyolitic tuff or ashstone. Maximum thickness is 250m.|14-FEB-14
10001|Lady Don Quartzite|22631|6|Mentioned|p177|||||||||
10001|Lady Don Quartzite|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
10001|Lady Don Quartzite|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Pintapah Subgroup (Poolamacca Group). White silicified quartzite. Max. thickness: 150m. Geological Province: Adeliade Fold Belt. See also p402 App. 1 Tb.A1.3.||||||25-JAN-08
10001|Lady Don Quartzite|30261|4|Described|Table 1|||Willouran age||||||
10001|Lady Don Quartzite|33004|6|Mentioned|p134|||||||||
10001|Lady Don Quartzite|34812|3|Fully described|p54|||||||||
10001|Lady Don Quartzite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
10001|Lady Don Quartzite|35692|6|Mentioned|p23|||||||||
10001|Lady Don Quartzite|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
10001|Lady Don Quartzite|36733|6|Mentioned|Table 5|||||||||
10001|Lady Don Quartzite|37461|6|Mentioned|p335|||||||||
10001|Lady Don Quartzite|37854|6|Mentioned|Table 1|||||||||
10001|Lady Don Quartzite|37931|4|Described|p533|||||||||
10001|Lady Don Quartzite|38157|6|Mentioned|Table II|||||||||
10001|Lady Don Quartzite|39214|6|Mentioned|p5|||||||||
10001|Lady Don Quartzite|40294|6|Mentioned|Table 2|||||||||
10001|Lady Don Quartzite|40595|6|Mentioned|p91|||||||||
10001|Lady Don Quartzite|41403|4|Described|p48|||||||||
10001|Lady Don Quartzite|42222|6|Mentioned|p11|||||||||
10001|Lady Don Quartzite|42223|6|Mentioned|Fig.2 P36|||||||||
10001|Lady Don Quartzite|42531|5|Briefly described|Map legend|Adelaidean||||||||
10001|Lady Don Quartzite|42813|6|Mentioned|p14|||||||||
10001|Lady Don Quartzite|43265|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
10001|Lady Don Quartzite|43268|5|Briefly described|Map Legend||Neoproterozoic|of Pintapah Subgroup.||||||
10001|Lady Don Quartzite|62724|5|Briefly described|p16|||Of Callanna Group in NSW. Mature quartz sandstone.||||||07-FEB-11
10001|Lady Don Quartzite|69023|6|Mentioned|p63|||||||||
10001|Lady Don Quartzite|69999|5|Briefly described|p21|||Appears as Lady Done Quartzite. On the Torrowangee and Fowlers Gap 1:100 000 sheet areas.|||||Metamorphic mineralogy includes chlorite and muscovite.|
10001|Lady Don Quartzite|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|||Unit in Pintapah Subgroup.|||Fluviatile to shallow marine, mature sandstone.|
10001|Lady Don Quartzite|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Pintapah Subgroup.||Is overlain by Christine Judith Conglomerate.|Medium-grained, white, silicified quartzite.|
10001|Lady Don Quartzite|72461|6|Mentioned|p13, p16, p19|||||Pintapah Subgroup||||
10024|Laidlaw Volcanics|13996|6|Mentioned|p148|Ludlow|Ludlow|Tharwa area. Interfingers with a shale hosting acanthodian spines and associated scales.||||||
10024|Laidlaw Volcanics|22590|6|Mentioned|P761||Wenlock|Age of unit is 421+/-2 Ma||||||
10024|Laidlaw Volcanics|22768|6|Mentioned|p176|||||||||
10024|Laidlaw Volcanics|22857|4|Described|p176, p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Overlies the Yass Formation in the Canberra area. Age: 420+/-2.2Ma (K/Ar and Rb/Sr on biotite) in Canberra-Yass Shelf region. Max. thickness: 1km. Geol. Prov: Canberra-Yass Shelf. See also p462 App.1 Tb.A1.6.||||||11-NOV-14
10024|Laidlaw Volcanics|24248|5|Briefly described|p51, p50, Fig.1|Pridoli|Pridoli|Overlying Unit: Silverdale Formation. Underlying unit: Yass Formation. Thick sequence of ignimbritic quartz-feldpar-biotite volcanics. Age: 421.1 +/- 3 Ma (Rb/Sr) and 419.6 +/- 5 Ma (SHRIMP U-Pb).||||||11-NOV-14
10024|Laidlaw Volcanics|24417|6|Mentioned|p164|||||||||
10024|Laidlaw Volcanics|32106|6|Mentioned|p305|||Palaeomagnetic data||||||
10024|Laidlaw Volcanics|35325|4|Described|p483|||Chemical analysis p484.||||||02-JUN-08
10024|Laidlaw Volcanics|35326|6|Mentioned|p485|||||||||
10024|Laidlaw Volcanics|35412|6|Mentioned|p84|||||||||
10024|Laidlaw Volcanics|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Extrusive. ?I-type. Extrusive. Dark to light grey porphyritic rhyodacite ignimbrite. Overlies Yass Formation; unconformably overlies Glen Bower Formation; unconformably underlies Mountain Creek Volcanics. BMR map code: Svl.||||||
10024|Laidlaw Volcanics|36633|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
10024|Laidlaw Volcanics|37013|6|Mentioned|p13|||||||||
10024|Laidlaw Volcanics|37728|4|Described|Table 2|||||||||
10024|Laidlaw Volcanics|37752|6|Mentioned|p105|||||||||
10024|Laidlaw Volcanics|38035|4|Described|p90|||||||||
10024|Laidlaw Volcanics|38626|6|Mentioned|p297|||||||||
10024|Laidlaw Volcanics|39507|6|Mentioned|p171|||||||||
10024|Laidlaw Volcanics|39975|6|Mentioned|Fig.1|||||||||
10024|Laidlaw Volcanics|40689|6|Mentioned|p5|||||||||
10024|Laidlaw Volcanics|41356|5|Briefly described|p42|||||||||
10024|Laidlaw Volcanics|42497|5|Briefly described|Map legend|Ludlovian|Wenlockian|||||||
10024|Laidlaw Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
10024|Laidlaw Volcanics|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Laidlaw Volcanic Suite. Rhyodacitic ignimbrite, minor volcaniclastic and argillaceous sediments. Overlies Deakin Volcanics; faulted against Adaminaby beds and Shannons Flat Adamellite. BMR map symbol: Sul. Geol. Prov: Canberra Block.||||||
10024|Laidlaw Volcanics|42820|2|Defined|p36|early Ludlow||Of Laidlaw Volcanic Suite. Age earliest Ludlow.||||||15-DEC-08
10024|Laidlaw Volcanics|43158|4|Described|4,13||Late Silurian|K-Ar & Rb-Sr biotite ages 420+-2.2Ma (early Ludlovian). Up to 500m thick.||||||
10024|Laidlaw Volcanics|43159|4|Described|Fig.2 p4,P6,P8,p10.||Ludlovian|K-Ar and Rb-Sr dated at 420.7 +/-2.2 My. Of Laidlaw Suite.||||||15-DEC-08
10024|Laidlaw Volcanics|43481|6|Mentioned|3|||||||||
10024|Laidlaw Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv4||||||
10024|Laidlaw Volcanics|45147|2|Defined|M151|early Ludlovian|early Ludlovian|||||||
10024|Laidlaw Volcanics|49690|5|Briefly described|p1-2, p14-16, Figs.1-3, p22,p27, Tb.12|Ludlow|Ludlow|Of Owen and Wyborn (1979). 421 Ma age pooled from a number of Rb/Sr and K/Ar determinations Wyborn et al. (1982)|421 Ma pooled from  Rb/Sr and K/ Ar ages|||Conformably overlies the Deakin Volcanics|Similar to the Deakin and Colinton Volcanics. Grey, crystal-rich dacitic ash-flow tuff with fresh biotite in some parts.|14-FEB-14
10024|Laidlaw Volcanics|50230|5|Briefly described|Map legend|Late Silurian|Early Silurian|Of the Douro Group.  Overlies the Yass Formation; overlain by the Yanawe Formation.  Porphyritic rhyodacitic ignimbrite.||||||
10024|Laidlaw Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
10024|Laidlaw Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Group. Dark to light grey, very coarse-grained, porphyritic, rhyodacitic ignimbrite. Sporadically grades to a coarse-grained equigranular ignimbrite. Rare columnar structure.||||||02-JUN-08
10024|Laidlaw Volcanics|64571|5|Briefly described|p828|Ludlow|Ludlow|Age: 420.7+/-2.2Ma (K/Ar and Rb/Sr). ACT.||||||15-DEC-08
10024|Laidlaw Volcanics|64994|5|Briefly described|p1, p4, p6|||Age of this unit is in dispute. Originally given as 420.7+/-2.2Ma (Wyborn et al (1982).||||||07-FEB-11
10024|Laidlaw Volcanics|66197|5|Briefly described|p631, p631 Fig.3b|||Canberra-Yass Basin. Underlies the Silverdale Formation. Overlies the Yass Formation.||||||13-MAR-12
10024|Laidlaw Volcanics|68592|1|Redefined|p433-9, p441, p443, p489, p498, p514-23|Wenlock|Wenlock|See also p269, p428, p430 Fig.89, p431, p452, p473 Fig.97, p1869. Redefined in this study. Originally Laidlaw Porphyry of Mann (1921); later Laidlaw Series of Brown (1940); later Laidlaw Formation of Link (1970, 1971); Link and Druce (1972). Redefined by Pogson and Baker (1974) to exclude almost all volcanic material; again redefined by Owen and Wyborn (1979) as Laidlaw Volcanics. Here redefined to exclude the upper volcaniclastics and limestones (now the Yanawe Formation). Type and representative sections described. From 0-1200m thick. Explosive volcanism in subaerial to shallow marine environments. Peraluminous; S-type although no cordierite or garnet. Some geochemical similarities with Bullenbalong Supersuite plutons. The superseded term Laidlaw Formation is occasionally used (see p.434, 441). Unfossiliferous; age from surrounding units: discussed. Various isotope ages discussed. Contains three hydrothermal vein Cu occurrences in the Kangiara Extended group of prospects.|432.9 /- 3/1 Ma SHRIMP U-Pb zircon.|Unit in Douro Group.||Overlies Hawkins Volcanics and parts of Yass Formation gradationally, and Boambolo and Glen Bower Formations unconformably. Is overlain disconformably by Yanawe Formation.|Grey, medium-grained, massive, welded, rhyodacitic, orthopyroxene-biotite ignimbrite; lesser volcaniclastic sandstone, volcanic breccia, and minor airfall tuff. S-type.|
10024|Laidlaw Volcanics|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sdl. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group||Is unconformably overlain by Yanawe Formation. Overlies Boambolo Formation. Overlies Yass Formation and its constituents, Cliftonwood Limestone Member and O'Briens Creek Sandstone Member.|Medium grained, massive, strongly jointed, welded rhyodacite ignimbrite with well preserved cooling columns; lesser grey, medium-v. thick bedded, medium-v. coarse grained, massive, crystal rich volcaniclastic sandstone, volcanic breccia; minor tuff.|
10024|Laidlaw Volcanics|70210|5|Briefly described|p2, p33-34, p37, p39-41|Llandovery|Llandovery|Yass-Goulburn district. A similar, weighted mean age of 432.3 +/- 3.3 Ma is also given. Age contrasts with Rb-Sr and K-Ar geochronology date of 421 +/- 2 Ma obtained by Wyborn et al. 1982.  Field relationships show this unit is younger than the Canowindra Volcanics, despite their age determinations in this Report.|431.2 +/- 3.0 Ma.|||||11-APR-18
10024|Laidlaw Volcanics|70296|5|Briefly described|p1, p11-12, p18, p19, p24|Llandovery|Llandovery|Goulburn-Yass district. Age was previously defined as Ludlow in age due to conodont fossil evidence.|432.9 +/- 3.1 Ma (SHRIMP U-Pb)|||||21-JAN-21
10024|Laidlaw Volcanics|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Medium grained, massive, strongly jointed, welded rhyodacite ignimbrite with well preserved cooling columns; lesser grey, medium-v. thick bedded, medium-v. coarse grained, massive, crystal rich volcaniclastic sandstone, volcanic breccia; minor tuff.|
10024|Laidlaw Volcanics|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Medium grained, massive and strongly jointed, welded rhyodacitic ignimbrite with well preserved cooling columns. Lesser medium-very thickly bedded, medium-very coarse grained massive crystal rich volcaniclastic sandstone, breccia and minor tuff.|
10024|Laidlaw Volcanics|71656|6|Mentioned|p12 Fig.2, p19|Homerian|Sheinwoodian|Most likely range in age from early to mid-Wenlockian (early Sheinwoodian to mid Homerian). Shown as early Ludlow series in Fig.2.||Douro Group||Overlies Boambolo and underlies Yanawe Formation.|Volcanics.|
10024|Laidlaw Volcanics|73215|4|Described|p992-994, 1002, 1004|Late Silurian|Late Silurian|Yass Syncline.|433 +/- 3 Ma (Black, 2005).|Douro Group|||Overlies Yass, Glen Bower, Boambolo Formations. Is overlain by Yanawe Formation.|
10050|Lake George Formation (NSW)|40664|6|Mentioned|p248|||[Invalid name. Lake George Beds, beds, Formation WA has priority. CEBMar95]||||||
10050|Lake George Formation (NSW)|61155|5|Briefly described|p19|Pleistocene|Late Pliocene|Overlies Gearys Gap Formation. Thickness: 54m. In the Lake George region of NSW.||||||11-APR-06
10073|Lake Victoria Sand|22799|5|Briefly described|p50|||||||||
10073|Lake Victoria Sand|30996|2|Defined|p50|Holocene|late Pleistocene|Contains 3 members. U.Pleistocene-Holocene||||||
10073|Lake Victoria Sand|32007|4|Described|p162|||Fossils discussed. Late Pleistocene - Holocene.||||||
10073|Lake Victoria Sand|40439|6|Mentioned|p380|||||||||
10073|Lake Victoria Sand|42966|6|Mentioned|p239|||||||||
10103|Lambie Group|22451|5|Briefly described|p23|||||||||
10103|Lambie Group|22472|4|Described|p40|Devonian|Devonian|||||||
10103|Lambie Group|22529|6|Mentioned|8|Late Devonian|Late Devonian|||||||
10103|Lambie Group|22678|6|Mentioned|p723||Late Silurian|||||||
10103|Lambie Group|22704|6|Mentioned|Fig7,p66||Late Devonian|||||||
10103|Lambie Group|22768|6|Mentioned|p188||Late Devonian|||||||
10103|Lambie Group|22857|5|Briefly described|p188, p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Molassic sedimentation. Max. thickness: >3km. Geological Province: Lambie Basin. See also pages 213, p216 and 494 App.1 Tb.A1.7.||||||
10103|Lambie Group|22859|5|Briefly described|p207,213,216|||||||||
10103|Lambie Group|22863|6|Mentioned|p238|||||||||
10103|Lambie Group|23043|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
10103|Lambie Group|23163|6|Mentioned|p5||Late Devonian|||||||
10103|Lambie Group|23170|2|Defined|p236|Early Carboniferous|Late Devonian|Of Lachlan Fold Belt.||||||25-FEB-08
10103|Lambie Group|23214|3|Fully described|p239|Late Devonian|Late Devonian|Geological Province: Lambie Basin. Max. thickness 2200m.||||||
10103|Lambie Group|23218|5|Briefly described|Map. p17||Devonian|||||||
10103|Lambie Group|23219|5|Briefly described|Map Legend|Late Devonian||||||||
10103|Lambie Group|23309|6|Mentioned|p390|||||||||
10103|Lambie Group|23335|6|Mentioned|p17|||||||||27-OCT-04
10103|Lambie Group|24005|5|Briefly described|p293|Late Devonian|Middle Devonian|||||||
10103|Lambie Group|24123|5|Briefly described|p3|Devonian|Devonian|||||||26-NOV-10
10103|Lambie Group|24126|6|Mentioned|p188|||||||||
10103|Lambie Group|24233|5|Briefly described|p256, p258 Fig.6|Devonian|Devonian|Geological Province: Lachlan Orogen.||||||
10103|Lambie Group|24247|6|Mentioned|p37|Famennian|Frasnian|||||||
10103|Lambie Group|24317|5|Briefly described|p14, p15 Fig.1|Late Devonian|Late Devonian|Fluvial (to shallow marine) sedimentary rocks.||||||
10103|Lambie Group|24334|6|Mentioned|p45|Early Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
10103|Lambie Group|24580|6|Mentioned|p828 Fig. 1|||Group is Gp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
10103|Lambie Group|29989|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
10103|Lambie Group|30100|6|Mentioned|p205|||||||||
10103|Lambie Group|30109|6|Mentioned|Fig.1|||Devonian age.||||||
10103|Lambie Group|30329|6|Mentioned|p30|||On table P30||||||
10103|Lambie Group|30708|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|30709|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|30731|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|31161|5|Briefly described|PA5|||See also PA7||||||
10103|Lambie Group|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
10103|Lambie Group|32483|4|Described|p35|||U.Dev. Strat. table 1||||||
10103|Lambie Group|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|32619|6|Mentioned|p460|||Late Dev.||||||
10103|Lambie Group|32621|6|Mentioned|p1|||||||||
10103|Lambie Group|32622|6|Mentioned|p97|||||||||
10103|Lambie Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
10103|Lambie Group|32672|6|Mentioned|p674|||||||||
10103|Lambie Group|32708|5|Briefly described|p407|||PP407-416||||||
10103|Lambie Group|32865|4|Described|p483|||||||||
10103|Lambie Group|32999|3|Fully described|p38|||Dev. Refers Browne (1929). Facies diag.P10||||||
10103|Lambie Group|33002|6|Mentioned|p406|||U.Dev. Refers Doutch(1972)||||||
10103|Lambie Group|33006|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|33282|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|33285|5|Briefly described|p23|||Late Dev.||||||
10103|Lambie Group|33325|5|Briefly described|Table 5|||||||||
10103|Lambie Group|33732|4|Described|p120|||Table II||||||
10103|Lambie Group|34059|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|34109|3|Fully described|p151|||||||||
10103|Lambie Group|34334|6|Mentioned|p359|||?U.Dev.||||||
10103|Lambie Group|34403|6|Mentioned|p132|||||||||
10103|Lambie Group|34404|6|Mentioned|Fig.3.5b|||||||||
10103|Lambie Group|34405|6|Mentioned|Fig.3.9|||||||||
10103|Lambie Group|34406|6|Mentioned|p224|||||||||
10103|Lambie Group|34449|6|Mentioned|p25|||||||||
10103|Lambie Group|34481|6|Mentioned|Map legend|Early Carboniferous|Late Devonian|Late Devonian - Early Carboniferous||||||
10103|Lambie Group|34834|6|Mentioned|p228|||||||||
10103|Lambie Group|35128|6|Mentioned|p361|||Appears on figure||||||
10103|Lambie Group|35166|6|Mentioned|p121|||||||||
10103|Lambie Group|35185|6|Mentioned|p246|||||||||
10103|Lambie Group|35246|6|Mentioned|p165|||||||||
10103|Lambie Group|35316|6|Mentioned|p429|||||||||
10103|Lambie Group|35655|6|Mentioned|p209|||Stratigraphy||||||
10103|Lambie Group|35759|5|Briefly described|p37|||Geological setting.||||||
10103|Lambie Group|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|36516|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|36534|6|Mentioned|p225|||See also P229.||||||
10103|Lambie Group|37490|6|Mentioned|p274|||||||||
10103|Lambie Group|37727|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|37748|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10103|Lambie Group|39214|4|Described|p29|||||||||
10103|Lambie Group|39331|6|Mentioned|p71|||See also Fig.0-3||||||
10103|Lambie Group|40130|6|Mentioned|p195|||||||||
10103|Lambie Group|40132|6|Mentioned|p243|||||||||
10103|Lambie Group|40328|6|Mentioned|p166|||||||||
10103|Lambie Group|40762|6|Mentioned|p288|||||||||
10103|Lambie Group|40774|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|40886|6|Mentioned|Fig.1|||||||||
10103|Lambie Group|41611|6|Mentioned|p139|||||||||
10103|Lambie Group|41863|6|Mentioned|p8|||||||||
10103|Lambie Group|42142|5|Briefly described|p578|||See also Fig.3||||||
10103|Lambie Group|42414|5|Briefly described|Fig.3 P70|||||||||
10103|Lambie Group|42712|4|Described|8,16; Table1p13; p9.|Late Devonian|Late Devonian|Unconformable on Winburn Tuff and older units.||||||25-FEB-08
10103|Lambie Group|42849|5|Briefly described|p541|Late Devonian|Late Devonian|Geological Province: Lachlan Fold belt.||||||09-MAY-05
10103|Lambie Group|43188|5|Briefly described|p219||Late Devonian|||||||
10103|Lambie Group|43263|6|Mentioned|Map Legend|Early Carboniferous|Middle Devonian|||||||
10103|Lambie Group|43319|14|Not recorded|Map Legend|||||||||
10103|Lambie Group|43320|14|Not recorded|p6,7|||||||||
10103|Lambie Group|43344|14|Not recorded|p54,139-141,143,150||Late Devonian|p155||||||
10103|Lambie Group|43363|14|Not recorded|Map Legend||Late Devonian|(Provisional first edition)||||||
10103|Lambie Group|43383|14|Not recorded|p16||Late Devonian|||||||
10103|Lambie Group|43384|14|Not recorded|Map Legend||Late Devonian|||||||
10103|Lambie Group|43461|14|Not recorded|p625|Early Carboniferous|Late Devonian|||||||
10103|Lambie Group|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
10103|Lambie Group|43479|14|Not recorded|p132,151||Late Devonian|||||||
10103|Lambie Group|43491|14|Not recorded|pV/15||Late Devonian|||||||
10103|Lambie Group|43507|14|Not recorded|p124,126|||||||||
10103|Lambie Group|43508|14|Not recorded|p117|||||||||
10103|Lambie Group|43509|14|Not recorded|p112|||||||||
10103|Lambie Group|43510|14|Not recorded|p37-8,46|||||||||
10103|Lambie Group|43511|14|Not recorded|p129||Late Devonian|||||||
10103|Lambie Group|43515|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
10103|Lambie Group|43516|14|Not recorded|Map Legend||Late Devonian|||||||
10103|Lambie Group|43517|14|Not recorded|p161||Late Devonian|||||||
10103|Lambie Group|43519|14|Not recorded|Table p119|Famennian|Frasnian|||||||
10103|Lambie Group|43782|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
10103|Lambie Group|43834|6|Mentioned|p26||Late Devonian|||||||
10103|Lambie Group|44093|5|Briefly described|p211 App. 1|Early Carboniferous|Late Devonian|Underlies Sydney Basin unit, Snapper Point Formation unconformably. See also p64 Photo 1. See also p213 Appendix 1.||||||26-NOV-10
10103|Lambie Group|48926|6|Mentioned|p13|||P13 et seq.||||||
10103|Lambie Group|50234|5|Briefly described|Map Legend|Late Devonian|Early Devonian|Includes: Tarlo Formation, Cookbundoon Formation, Wiarborough Formation, Strathaird Formation.||||||
10103|Lambie Group|60423|5|Briefly described|p371|Lower Carboniferous|Upper Devonian|Geological Province: Lachlan Fold Belt. Conglomeratic sediments.||||||
10103|Lambie Group|61311|5|Briefly described|p44|Carboniferous|Late Devonian|Geological Province: Darling Basin. Age is Late Devonian to Middle Carboniferous.||||||16-JUN-06
10103|Lambie Group|61762|6|Mentioned|p19 Fig. 2(a)|Late Devonian|Late Devonian|||||||
10103|Lambie Group|61892|6|Mentioned|p201 Fig.1|Early Carboniferous|Late Devonian|||||||
10103|Lambie Group|62368|5|Briefly described|p378 Fig.1, p401, p403|Late Devonian|Late Devonian|||||||
10103|Lambie Group|63151|5|Briefly described|p3 Fig. 2|Late Devonian|Late Devonian|Overlies Bindook Volcanic Complex unconformably. Includes quartzites and shales.||||||31-JAN-08
10103|Lambie Group|63633|5|Briefly described|Map Legend|Early Carboniferous|Late Devonian|Includes Tarlo, Wiraborough and Strathaird Formations and Cookbundoon Sandstone.||||||
10103|Lambie Group|64238|5|Briefly described|Map legend|Devonian|Devonian|Includes the Cowpers Creek Conglomerate and Tarlo, Strataird and Cookbundoon Formations.||||||
10103|Lambie Group|64826|5|Briefly described|p1039 Fig. 2|Late Devonian|Late Devonian|||||||
10103|Lambie Group|66623|6|Mentioned|p438.|||Marine incursions in this unit were contemporaneous with deposition of the Wana Karnu Group.||||||
10103|Lambie Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle.||||||
10103|Lambie Group|68298|5|Briefly described|p216|||With Catombal Group forms eastern province of Connolly (1965), in which basal equivalents of Beargamil Subgroup are marine.||||||
10103|Lambie Group|68592|1|Redefined|p74 Tb.5, p232, p235, p278, p1722-1753|Late Devonian|Late Devonian|See also p326, p726, p734, p760, p787, p820, p829, p832-3, p835, p852, p873, p885, p890, p988, p1197. Redefined. Of MacKay (1961). The terms "Lambie Stage" and "Lambie Series" (Browne, 1929) had been commonly applied to Late Devonian sequences in NSW, including also the current Catombal and Hervey Groups. The Group was divided into three Formations by Brunker et al. (1970) and Offenberg (1974); Scheibner added a fourth (the Wiarborough Formation) which is discontinued here and replaced by the (new) Cowpers Creek Conglomerate. Type area is Mount Lambie (Brown and Joplin, 1938) but MacKay (1961) nominated a representative section along the Bowenfels-Rydal-Mount Lambie road. 1450-c.4300m thick. Is folded into a major structure, the Cookbundoon Syncline, 10km wide and 90 km long. Basal unconformity of Tabberabberan age.  Is intruded by plutons of the Bathurst Batholith. Has been quarried for "slate", road surfacing materials and drystone and wetstone walls. Goulburn and Bungonia structural zones: deformation described.|||Includes Cookbundoon, Tarlo and Strathaird Formations, Turon [River} Grits and Cowpers Creek Conglomerate.|Unconformably overlies Argyle, Kowmung and Rhyanna Formations (Mount Fairy Group), Torwood Granodiorite and Banshea and Lumley Granites nonconformably. Intruded by Kanangra Granite.|Dominated by fine-grained to conglomeratic sandstone with some extensive reddish purple mudstone sequences. Interbedded polymictic conglomerate, lithic-quartz sandstone and muddy siltstone.|
10103|Lambie Group|70192|5|Briefly described|Map Legend|Carboniferous|Frasnian|On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.|||Includes Cookbundoon Formation, Strathaird Formation, Tarlo Formation, Cowpers Creek Conglomerate.|||
10103|Lambie Group|70297|4|Described|map legend, on side 2 of map sheet|Famennian|Frasnian|Erosional base.|||Gibbons Creek Sandstone, Morgans Gully Siltstone, Slowmans Creek Conglomerate, Turon River Grits|With Catombal and Hervey Groups, overlies Dulladerry Volcanics.|Terrigenous to shallow marine, quartz sandstone, quartzite, siltstone, mudstone, conglomerate.|
10103|Lambie Group|70542|5|Briefly described|Map Legend|Late Devonian|Late Devonian||||Includes Cookbundoon Formation, Strathaird Formation, Tarlo Formation, Cowpers Creek Conglomerate.|||
10103|Lambie Group|70543|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Cookbundoon Formation, Strathaird Formation, Tarlo Formation, Cowpers Creek Conglomerate|||
10103|Lambie Group|71040|5|Briefly described|p13, p19-20, p30|Late Devonian|Late Devonian|Cookbundoon Syncline, Goulburn region. Deposition followed the Tabberabberan Orogeny. Deformation described and illustrated.||||Unconformably overlies Quialigo Volcanics.||
10103|Lambie Group|71069|6|Mentioned|p135, p141, p147, p172|Late Devonian|Late Devonian|||||Unconformably overlies the Mount Fairy Group, De Drack Formation.||
10103|Lambie Group|71656|5|Briefly described|p10, p13 Fig.2, p41|Famennian|Frasnian|Largely fluvio-lacustrine with a marine incusion (Strathaird Formation) at the base. Includes a variety of conodont species. Age by correlation with Merimbula Group's more abundant fossils.|||Tarlo Formation, Cookbundoon Formation, Cowpers Creek Conglomerate and Strathaird Formation.|Unconformably overlies Bindook Group. Correlated with Merimbula Group.|Includes congomerates overlaid with fossiliferous limestone.|
10103|Lambie Group|71700|5|Briefly described|p58, p63, p66|Late Devonian|Late Devonian|Deposited after the Mount Fairy and Bindook groups, though the relationship is not||||||
10103|Lambie Group|72528|5|Briefly described|p25.|Late Devonian|Late Devonian|||||Overlies Banshea Granite.||
10103|Lambie Group|73299|6|Mentioned|p1107 Fig.12|Late Devonian|Late Devonian|Capertree High.||||||
10103|Lambie Group|73457|6|Mentioned|p2|Late Devonian|Late Devonian|||||||
10103|Lambie Group|73582|5|Briefly described|p99, 105-106, 111-112, 118-120|Late Devonian|Late Devonian|Eastern Lachlan Fold Belt.||||Unconformably overlies/is faulted against Inspiration Point Formation.|Medium- to fine-grained, white-buff, well-bedded quartzites, quartz-rich sandstones and siltstones (phyllites). Local brachiopod fossils.|
10115|Lambton Subgroup|22969|4|Described|Fig 4.1a||Late Permian|||||||
10115|Lambton Subgroup|24121|5|Briefly described|p4, p61, 132|||Of Newcastle Coal Measures.||||||25-AUG-22
10115|Lambton Subgroup|24157|4|Described|p204|Permian|Permian|Basal unit of Newcastle Coal Measures. Geological Province: Sydney Basin||||||09-DEC-08
10115|Lambton Subgroup|39609|6|Mentioned|Table 1|||||||||
10115|Lambton Subgroup|42214|6|Mentioned|Table 1 P462|||||||||
10115|Lambton Subgroup|43344|14|Not recorded|p85||Permian|||||||
10115|Lambton Subgroup|43448|14|Not recorded|p224,226,230||Permian|Inc.Warratah Sandstone,Tighe's Hill,Bogey Hole,Bar Beach,Shepherd's Hill Formations(Newcastle C.M.)||||||
10115|Lambton Subgroup|43450|14|Not recorded|p10|||||||||
10115|Lambton Subgroup|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Newcastle Coal Measures.||Overlies Tomago Coal Measures. Is overlain by Adamstown Subgroup.||
10115|Lambton Subgroup|68711|5|Briefly described|p119, p116 Tbl 2|||Of McKenzie and Britten (1969). Replaced by Lambton Formation||Formerly of Newcastle Coal Measures|Included West Borehole, Borehole, Yard Coal, Tighes Hill, Bogey Hole Formation, Young Wallsend, Dudley Coal, Bar Beach Formation, Nobbys Coal, Shepherds Hill Formation, Victoria Tunnel Coal.|||
10115|Lambton Subgroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Newcastle Coal Measures|||Sandstone, siltstone, claystone, coal and tuffaceous sandstone.|
10117|Lamington Group|23811|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Includes Lismore Basalt.||||||19-NOV-08
10117|Lamington Group|23812|5|Briefly described|p37 Tb.5|Tertiary|Tertiary|||||||
10117|Lamington Group|30687|5|Briefly described|p65|||Tertiary age||||||
10117|Lamington Group|31130|6|Mentioned|p932|||Tertiary||||||
10117|Lamington Group|31273|6|Mentioned|p24|||||||||
10117|Lamington Group|33290|6|Mentioned|p37|||||||||
10117|Lamington Group|33381|6|Mentioned|p108|||Tertiary.||||||
10117|Lamington Group|34755|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|35045|6|Mentioned|p110|||||||||
10117|Lamington Group|35050|6|Mentioned|p130|||||||||
10117|Lamington Group|35126|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|35156|4|Described|p7|||See also Table.2||||||
10117|Lamington Group|35296|6|Mentioned|p12|||Statigraphy.||||||
10117|Lamington Group|35866|6|Mentioned|p407|||||||||
10117|Lamington Group|36779|5|Briefly described|p8|||||||||
10117|Lamington Group|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|38080|6|Mentioned|p55|||||||||
10117|Lamington Group|38441|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10117|Lamington Group|39445|6|Mentioned|Table 14|||||||||
10117|Lamington Group|39998|6|Mentioned|p190|||||||||
10117|Lamington Group|40623|5|Briefly described|p109|||||||||
10117|Lamington Group|40896|6|Mentioned|p49|||||||||
10117|Lamington Group|41906|3|Fully described|Table 4 P32|||||||||
10117|Lamington Group|43008|5|Briefly described|map legend|||||||||
10117|Lamington Group|44782|14|Not recorded|p44|||||||||
10117|Lamington Group|44783|14|Not recorded|p12,19|||||||||
10117|Lamington Group|44784|4|Described|p11,12||Tertiary|Includes: Hobwee Basalt, Binna Burra Rhyolite, Mount Lindsay Rhyolite, Chinghee Conglomerate, Hillview Rhyolite, Albert Basalt, Numinbah Valley Formation.||||||
10117|Lamington Group|44786|14|Not recorded|p193-202||Miocene|Early Miocene||||||
10117|Lamington Group|44813|14|Not recorded|p80-85,88||Tertiary|Apparent age: 22-20 Ma||||||
10117|Lamington Group|44818|6|Mentioned|p275|||||||||
10117|Lamington Group|61155|5|Briefly described|p19|Early Miocene|Early Miocene|Of the Main Range Volcanics. Associated with the Tweed Volcano. Overlies Numinbah Valley Formation. Age: 22-17Ma. In the Brisbane region.||||||
10117|Lamington Group|63779|6|Mentioned|p1140|Cenozoic|Cenozoic|Age: between 25 - 20Ma. Volcanics.||||||
10117|Lamington Group|68327|5|Briefly described|Map legend.|Tertiary|Tertiary|Three facies, labelled Ts, Tl and Tv, are mapped separately.|||||Ts = mudstone, siltstone, shale, sandstone, lenses of basalt; Tl = basalt flows, minor rhyolite and pyroclastics; Tv = mainly basalt flows.|
10117|Lamington Group|68553|6|Mentioned|Map legend|Paleogene|Paleogene|||||||
10120|Lamington Volcanics|22582|5|Briefly described|p69||Early Miocene|||||||
10120|Lamington Volcanics|23888|5|Briefly described|p262|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|24299|5|Briefly described|p4|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|30131|6|Mentioned|p8|||See also P11. Lithology||||||
10120|Lamington Volcanics|30604|6|Mentioned|p65|||||||||
10120|Lamington Volcanics|32491|6|Mentioned|p22|||||||||
10120|Lamington Volcanics|32492|6|Mentioned|Map legend|Miocene|Miocene|||||||
10120|Lamington Volcanics|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|33476|4|Described|p106|||||||||
10120|Lamington Volcanics|33766|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|35042|5|Briefly described|p129|||||||||
10120|Lamington Volcanics|35045|6|Mentioned|p110|||||||||
10120|Lamington Volcanics|35050|6|Mentioned|p130|||||||||
10120|Lamington Volcanics|35296|6|Mentioned|p12|||Statigraphy.||||||
10120|Lamington Volcanics|36806|6|Mentioned|p131|||||||||
10120|Lamington Volcanics|40328|6|Mentioned|p195|||||||||
10120|Lamington Volcanics|40896|6|Mentioned|p5|||||||||
10120|Lamington Volcanics|43150|5|Briefly described|Map Legend||Tertiary|||||||
10120|Lamington Volcanics|43881|14|Not recorded|p53||Tertiary|Equivalent to MacPherson Volcanics. Probably Eocene-Oligocene||||||
10120|Lamington Volcanics|44781|14|Not recorded|p355|||||||||
10120|Lamington Volcanics|44783|14|Not recorded|p2|||||||||
10120|Lamington Volcanics|48917|4|Described|p38|||See also P33. Stratigraphic table||||||
10120|Lamington Volcanics|60079|5|Briefly described|Map Legend|Tertiary|Tertiary|Includes: Lismore Basalt.||||||
10120|Lamington Volcanics|61310|6|Mentioned|p22|Tertiary|Tertiary|||||||
10120|Lamington Volcanics|65003|5|Briefly described|p7||Tertiary|Of Clarence-Moreton Basin.||||||30-MAR-12
10120|Lamington Volcanics|69594|6|Mentioned|p545|Cenozoic|Cenozoic|Clarence-Moreton Basin.||||||
10120|Lamington Volcanics|69599|5|Briefly described|p595|Miocene|Miocene|Gold Coast hinterland.|||Chinghee Conglomerate.|Overlies Numinbah Valley Formation.||
10120|Lamington Volcanics|72297|6|Mentioned|p732|Cenozoic|Cenozoic|Perlite is mined at the Numinbah deposit, in the McPherson Ranges SE of Beechmont. The deposit is a zone of volcanic glass within the unit.||||||
10120|Lamington Volcanics|73581|5|Briefly described|p6-7|||Extrusive products of the Tweed Volcano. Intercalated with components of the Main Range and Focal Peak volcanoes.|||Beechmont Basalt, Lismore Basalt, Hobwee Basalt, Blue Knob Basalt|Overlies Albert Basalt, Kyogle Basalt|Sequence of distinct basalt and rhyolite flows and tuff horizons.|
10139|Landers Creek Formation|22857|5|Briefly described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Boraig Group. Andesitic tuff, sandstone. Max. thickness: 420m. Geological Province: Bogan Gate Terrace.||||||
10139|Landers Creek Formation|29648|6|Mentioned|p25|||||||||
10139|Landers Creek Formation|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
10139|Landers Creek Formation|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
10139|Landers Creek Formation|33732|5|Briefly described|p111|||Boraig Gp.||||||
10139|Landers Creek Formation|34403|4|Described|p144|||||||||
10139|Landers Creek Formation|34405|6|Mentioned|Fig.3.15|||||||||
10139|Landers Creek Formation|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
10139|Landers Creek Formation|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Boraig Group.||||||
10194|Lark Hill Formation|721|5|Briefly described|Map legend|Stephanian|Westphalian|Feldsarenite, litharenite, subordinate orthoconglomerate and paraconglomerate, siltstone, rhyodacitic and dacitic ashflow and airfall tuff.  Geological Province: Tamworth Belt.||||||05-DEC-05
10194|Lark Hill Formation|22857|4|Described|p506 App.1 Tb.A1.8|Late Carboniferous|Late Carboniferous|Feldsarenite, litharenite; subordinate orthoconglomerate and paraconglomerate, siltstone, rhyodacitic and dacitic airfall and ashflow tuff. Max. thickness: >1500m.||||||
10194|Lark Hill Formation|23050|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
10194|Lark Hill Formation|23051|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
10194|Lark Hill Formation|23861|5|Briefly described|p4 Fig. 2, p3|Westphalian|Westphalian|Geological Province: New England Orogen.||||||
10194|Lark Hill Formation|24010|6|Mentioned|p381|||||||||
10194|Lark Hill Formation|24334|5|Briefly described|p49 Tb.1|Westphalian|Westphalian|Age: 305 - 311 Ma||||||
10194|Lark Hill Formation|24348|5|Briefly described|p131|Carboniferous|Carboniferous|||||||
10194|Lark Hill Formation|24603|5|Briefly described|p866|Stephanian|Westphalian|See also p895 Fig. 16.  Geological Province: Tamworth Belt.||||||
10194|Lark Hill Formation|24605|5|Briefly described|p931|Westphalian|Visean|Geological Province: New England Orogen.||||||
10194|Lark Hill Formation|30133|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
10194|Lark Hill Formation|30135|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
10194|Lark Hill Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
10194|Lark Hill Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
10194|Lark Hill Formation|32672|6|Mentioned|p674|||||||||
10194|Lark Hill Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
10194|Lark Hill Formation|34085|6|Mentioned|Cor.chart|||Stephanian||||||
10194|Lark Hill Formation|34349|5|Briefly described|p247|||||||||
10194|Lark Hill Formation|35390|6|Mentioned|p98|||"Predictive profiling" applied to a simple anomaly on the Dunrobin road||||||
10194|Lark Hill Formation|36528|6|Mentioned|p182|||||||||
10194|Lark Hill Formation|36961|6|Mentioned|Fig.3|||||||||
10194|Lark Hill Formation|37919|5|Briefly described|p477|||||||||
10194|Lark Hill Formation|39331|6|Mentioned|Table 10-1|||||||||
10194|Lark Hill Formation|41009|6|Mentioned|p5|||||||||
10194|Lark Hill Formation|42547|4|Described|p20|||Rocky Creek Syncline.||||||
10194|Lark Hill Formation|43017|5|Briefly described|Fig.2,p374|||||||||
10194|Lark Hill Formation|43091|5|Briefly described|Map legend|||||||||
10194|Lark Hill Formation|43383|14|Not recorded|p18|||||||||
10194|Lark Hill Formation|43409|14|Not recorded|Map Legend|||Equiv. of Currabubula Formation||||||
10194|Lark Hill Formation|43429|14|Not recorded|Map Legend|||To 2400 ft thick||||||
10194|Lark Hill Formation|43434|14|Not recorded|Map Legend||Carboniferous|||||||
10194|Lark Hill Formation|43435|2|Defined|Map Legend||Carboniferous|||||||
10194|Lark Hill Formation|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
10194|Lark Hill Formation|43446|14|Not recorded|p6029|||no data||||||
10194|Lark Hill Formation|43479|14|Not recorded|p177|Stephanian|Westphalian|||||||
10194|Lark Hill Formation|43582|6|Mentioned|p17|||||||||
10194|Lark Hill Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
10194|Lark Hill Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
10194|Lark Hill Formation|47056|6|Mentioned|Fig.2 P523|||||||||
10194|Lark Hill Formation|50613|5|Briefly described|p207|Namurian|Namurian|Of the Currangandi Group.||||||22-FEB-05
10194|Lark Hill Formation|50629|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Geological Province: New England Orogen.||||||
10194|Lark Hill Formation|60299|5|Briefly described|p209|Carboniferous|Carboniferous|Geological Province: Rocky Creek Block||||||
10194|Lark Hill Formation|61214|5|Briefly described|p171 Fig. 1, p172 Fig. 2.|Westphalian|Westphalian|Geological Province: Boomi Block.||||||
10194|Lark Hill Formation|61767|4|Described|p71|Westphalian|Westphalian|Consists mainly of coarse pebbly, cross-bedded lithic sandstone, tuffaceous sandstone, pebble conglomerate and siltstone in fining-upward cycles, disrupted by rhyolitic pyroclastic and  fall deposits. Max. thickness: 730m. Geol. Province: Tamworth Belt.||||||27-JAN-06
10194|Lark Hill Formation|62095|6|Mentioned|p267|||Geological Province: Rocky Creek block/Tamworth Belt.||||||
10194|Lark Hill Formation|63832|5|Briefly described|p131 fig 2|Moscovian|Bashkirian|Rocky Creek Syncline, Southern New England Fold Belt. The fourth glaciation (C4) occurred during deposition.|||||An interval of proglacial lake deposits with rhythmic grain-size alternation between clay, silt and sand laminae, and dispersed gravel.|13-DEC-17
10194|Lark Hill Formation|64631|5|Briefly described|p44 Fig.2.|Moscovian|Bashkirian|Southern New England Fold Belt, Rocky Creek Syncline. Some biostratigraphic and radiometric age control within unit.||||Overlies Rocky Creek Conglomerate.||
10194|Lark Hill Formation|65107|6|Mentioned|Fig 4 p279, Fig 9 p283|Late Palezoic|Late Palezoic|Rocky Creek Block. This unit helped constrain the Late Palezoic pole path for the New England orogen.||||||
10194|Lark Hill Formation|68003|5|Briefly described|p32 Fig.3-h, p136. |Westphalian|Westphalian|Tamworth Belt (North), New England Fold Belt.||||Overlies Rocky Creek Conglomerate.|Coarse lithic and feldspathic arenite, subordinate orthoconglomerate and paraconglomerate, siltstone, and rhyodacitic and dacitic ashflow tuff.|
10194|Lark Hill Formation|68004|6|Mentioned|p134.|||Potential for zeolite resources and levels of certainty are discussed.||||||
10194|Lark Hill Formation|68005|5|Briefly described|p49 Fig.3-M, p57, p142, p170.|Stephanian|Westphalian|Rocky Creek Block, Tamworth Belt. With Rocky Creek Conglomerate, represents a period of glacial retreat.|||Includes Hell Hole Pyroclastic Member.|Overlies Rocky Creek Conglomerate.|Coarse lithic and feldspathic arenite, subordinate orthoconglomerate and paraconglomerate, siltstone and rhyodacitic and dacitic ashflow tuff.|
10194|Lark Hill Formation|69793|6|Mentioned|p1121 Fig.12, p1122|Bashkirian|Bashkirian|Rocky Creek Block, Tamworth Belt.||||||
10194|Lark Hill Formation|70728|5|Briefly described|p265,271-273|Bashkarian|Bashkarian|Geological province: North Tamworth terrane, New England Orogen. Contains SHRIMP zircon age of 315.3+\-3.4 Ma (Roberts et al., 2003; Roberts et al., 2006; Roberts and James, 2010).Also contains  LA-ICP-MS zircon age of 316.6+\-3.3 Ma (this study).||||Underlain by Rocky Creek Conglomerate.||
10233|Laura Creek molybdenite|41603|6|Mentioned|p18|||||||||
10240|Laurieton Conglomerate|22616|6|Mentioned|Fig.1 p670|Triassic|Triassic|||||||
10240|Laurieton Conglomerate|22736|6|Mentioned|p611 Fig2||Triassic|||||||
10240|Laurieton Conglomerate|22857|5|Briefly described|p538 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Camden Haven Group. Red, pebble and cobble conglomerate with minor granule conglomerate, sandstone, red-brown claystone. Max. thickness: 210m. Geological Province: Lorne Basin.||||||
10240|Laurieton Conglomerate|32719|4|Described|p208|||See also p209, 212. map p207.||||||19-OCT-15
10240|Laurieton Conglomerate|35647|5|Briefly described|p50|||||||||
10240|Laurieton Conglomerate|36826|5|Briefly described|p89|||||||||
10240|Laurieton Conglomerate|40134|6|Mentioned|p283|||||||||
10240|Laurieton Conglomerate|41348|5|Briefly described|Map legend|Triassic|Triassic|Of the Camden Haven Group.  In the Hastings Block.||||||16-DEC-04
10240|Laurieton Conglomerate|44093|5|Briefly described|p67 Fig 6.6|Triassic|Triassic|Geological Province: Lorne Basin.||||||
10240|Laurieton Conglomerate|60281|5|Briefly described|p18, Fig. 8 App. 1|Triassic|Triassic|Of the Camden Haven Group.  Red, pebble to cobble conglomerate with minor granule conglomerate, sandstone and red-brown claystone beds.  Overlies Camden Head Claystone.  Max. thickness: 210m.   Geological Province: Lorne Basin.||||||03-FEB-09
10240|Laurieton Conglomerate|62058|5|Briefly described|map sheet|Early Triassic|Early Triassic|||Unit in Camden Haven Group.|||Quartz conglomerate.|
10240|Laurieton Conglomerate|63763|5|Briefly described|p4-5 Fig. 1|Early Triassic|Eary Triassic|Of Camden Haven Group. Chert conglomerate.||||||03-FEB-09
10240|Laurieton Conglomerate|66090|1|Redefined|pp1-2, p4, pp8-9, pp22-24. |Early Triassic|Early Triassic|Redefined in this study. Limited distribution in northeast Lorne Basin. Laterally equivalent to Coorabakh Conglomerate. Resistant, cliff-forming unit, well-exposed along the coast. Type section at Grants Head. Identified by >20% jasper clasts, and >3 cobbles in 0.25 m2 area. Clasts derived from outside the Basin; typical of New England Orogen provenance, and similar to the Digby Conglomerate (Gunnedah Basin) and Munmorah Conglomerate (Sydney Basin).||Unit in Camden Haven Group.||Overlies Camden Head Claystone and, locally, Jolly Nose Conglomerate. Is overlain conformably by Grants Head Formation.|Very thickly bedded, poorly sorted unit of chert, quartz and jasper, cobble and pebble conglomerates; uncommon pebble and minor granule conglomerate and sandstone interbeds; clast-supported fabric; poorly sorted sandstone and claystone matrix.|12-OCT-15
10263|Lawrence Sandstone Member|24471|4|Described|p39|Late Permian|Late Permian|See also Lawrence Sandstone. Erosively overlies Burragorang Claystone Member. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
10263|Lawrence Sandstone Member|29900|6|Mentioned|Table 2|||||||||
10263|Lawrence Sandstone Member|29901|4|Described|Table 1|||||||||
10263|Lawrence Sandstone Member|30006|5|Briefly described|p37|||||||||
10263|Lawrence Sandstone Member|31128|6|Mentioned|Table 1|||||||||
10263|Lawrence Sandstone Member|32849|6|Mentioned|Table 1|||Permian||||||
10263|Lawrence Sandstone Member|36220|6|Mentioned|p50|||See also Table 1 & P50.||||||
10263|Lawrence Sandstone Member|36593|6|Mentioned|Table 2|||||||||
10263|Lawrence Sandstone Member|37089|6|Mentioned|p208|||||||||
10263|Lawrence Sandstone Member|39661|6|Mentioned|Fig.1|||||||||
10263|Lawrence Sandstone Member|42787|6|Mentioned|Table 1 P126|||||||||
10263|Lawrence Sandstone Member|42896|4|Described|p24|||of Eckersley Formation||||||
10267|Lawsons Creek Shale|22529|5|Briefly described|4 fig 2, 8|Late Devonian|Late Devonian|Parent Mount Knowles Group. Overlying unit Derale Sandstone||||||
10267|Lawsons Creek Shale|22857|5|Briefly described|p492 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Mount Knowles Group. Mudstone, shale with thin quartz arenite interbeds. Max. thickness: 400m. Geological Province: Lambie Shelf.||||||
10267|Lawsons Creek Shale|23043|5|Briefly described|Map Legend|Famennian|Famennian|of Mount Knowles Group.||||||
10267|Lawsons Creek Shale|23170|2|Defined|p243|Late Devonian|Frasnian|of Mount Knowles Group.||||||
10267|Lawsons Creek Shale|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
10267|Lawsons Creek Shale|32485|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10267|Lawsons Creek Shale|39214|6|Mentioned|p29|||||||||
10267|Lawsons Creek Shale|43043|3|Fully described|p100|||late Devonian age.||||||
10267|Lawsons Creek Shale|43188|4|Described|p219||Late Devonian|Of Lambie Group. Late Devonian (Famennian) age.||||||
10267|Lawsons Creek Shale|43476|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
10267|Lawsons Creek Shale|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4, p1099|Late Devonian|Late Devonian|Capertree High. Locations in text include p1100 Fig.5.||Mount Knowles Group||Overlies the Bumberra Formation, Buckaroo Conglomerate, underlies the Derale Sandstone.||
10268|Lawsons Gully Porphyry|29907|2|Defined|Appendix 1|Early Devonian|Early Devonian|||||||
10268|Lawsons Gully Porphyry|29910|6|Mentioned|Map legend|Devonian|Devonian|||||||
10268|Lawsons Gully Porphyry|36411|6|Mentioned|p269|||Refers Bowman 1977.||||||
10268|Lawsons Gully Porphyry|40328|4|Described|p208|||||||||
10280|Leard Formation|22579|5|Briefly described|p219 Fig.2|Early Permian|Early Permian|||||||
10280|Leard Formation|22610|6|Mentioned|p 123|||||||||
10280|Leard Formation|22857|4|Described|p520 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Bellata Group. Pelletoidal clay sandstone and conglomerate, poorly bedded and carbonaceous; minor dull coal. Max. thickness: 32m. Geological Province: Gunnedah Basin.||||||
10280|Leard Formation|23050|5|Briefly described|p 82 Fig.17|Early Permian|Early Permian|of Gunnedah Basin||||||
10280|Leard Formation|23350|5|Briefly described|264|||||||||
10280|Leard Formation|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Of Bellata Group. Geological Province: Gunnedah Basin||||||
10280|Leard Formation|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
10280|Leard Formation|24603|5|Briefly described|p869 Fig. 4c|Permian|Permian|Geological Province: Tamworth Belt.||||||
10280|Leard Formation|36940|2|Defined|p156|Early Permian|Early Permian|||||||
10280|Leard Formation|37856|6|Mentioned|Table I|||||||||
10280|Leard Formation|38089|4|Described|p6|||||||||
10280|Leard Formation|38614|4|Described|p5|||||||||
10280|Leard Formation|39063|5|Briefly described|p10|||||||||
10280|Leard Formation|39572|6|Mentioned|p134|||||||||
10280|Leard Formation|39693|6|Mentioned|p14|||||||||
10280|Leard Formation|39913|5|Briefly described|p4|||||||||
10280|Leard Formation|40176|6|Mentioned|Fig.2|||||||||
10280|Leard Formation|40200|4|Described|p9|||||||||
10280|Leard Formation|40331|6|Mentioned|p5|||||||||
10280|Leard Formation|40332|6|Mentioned|Fig.3|||||||||
10280|Leard Formation|40680|6|Mentioned|Fig.1|||||||||
10280|Leard Formation|40767|6|Mentioned|Fig.10|||||||||
10280|Leard Formation|40952|4|Described|p5|||||||||
10280|Leard Formation|41130|4|Described|p47|||||||||
10280|Leard Formation|41264|5|Briefly described|p251|||Fmly Koogah, Willow Tree, Werris Creek, Wean and Condadilly Formations||||||
10280|Leard Formation|41290|4|Described|p225|||||||||
10280|Leard Formation|41451|6|Mentioned|p14|||||||||
10280|Leard Formation|41689|6|Mentioned|Table 1|||||||||
10280|Leard Formation|41990|6|Mentioned|p8|||||||||
10280|Leard Formation|42284|5|Briefly described|Fig.11 P104|||||||||
10280|Leard Formation|42463|6|Mentioned|Fig.6 P173|||Table just says 'Leard'.||||||
10280|Leard Formation|42679|5|Briefly described|Fig.3 P3|||||||||
10280|Leard Formation|43194|1|Redefined|p98 Tb. 8.2, p99-103, p133 App. 1|Early Permian|Early Permian|See also references on p95, p128, p129 Tb.8.3. Now of Bellata Group. Unconformably overlies Boggabri Volcanics and possibly Werrie Basalt; underlies Maules Creek Formation. Assigned Lower Stage 4 palynological age. Correlative of Skeletar Formation (Sydney Basin).||||||
10280|Leard Formation|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
10280|Leard Formation|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin.  Of the Bellata Group.  Underlies: Goonbri & Maules Creek Formations.  Overlies: Werrie Basalt & Boggabri Volcanics.||||||05-JUL-04
10280|Leard Formation|61313|5|Briefly described|p91, p94 Fig.G7|Early Permian|Early Permian|Marks the onset of sedimentation in the Gunnedah Basin. Distinctive peletoidal clayrock sequence. Conformably overlain by Goonbri Formation. Max. thickness: 32m. Geological Province: Gunnedah Basin. See also p95 Fig. G8,p98 Fig. G10.||||||
10280|Leard Formation|61377|5|Briefly described|p154 Fig. SU9|Early Permian|Early Permian|Lacustrine deposits. Geological Province: Gunnedah Basin. Presented as Leard only in figure.||||||07-FEB-11
10280|Leard Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
10280|Leard Formation|61776|5|Briefly described|p194 Fig. 3|Early Permian|Early Permian|Of Bellata Group. Geological Province: Gunnedah Basin. Clay pellet conglomerate, sandstone, siltstone and coal.||||||
10280|Leard Formation|63832|6|Mentioned|p131 fig 2|Kungurian|Sakmarian|Of Gunnedah Basin. Sixth (P2) glaciation.||||||
10280|Leard Formation|64631|5|Briefly described|p44 Fig.2.|Kungurian|Sakmarian|Gunnedah Basin. Some biostratigraphic age control.||||Overlies Werrie Basalt.Is overlain by Maules Creek Formation.||
10280|Leard Formation|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Gunnedah Basin. Overlies the Werrie Basalt, underlies the Goonbri Formation.||||||22-MAR-12
10280|Leard Formation|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Gunnedah Basin. Overlies Werrie Basalt.||||||
10280|Leard Formation|65114|5|Briefly described|p385 Fig.3|Early Permian||||||||
10280|Leard Formation|65116|5|Briefly described|Fig 2 p436, Fig 6 p441, p449 Fig 14|Early Permian|Early Permian|Underlies the Goonbri Formation, overlies the Werrie Basalt in the Gunnedah Basin. Flint clay, sandstone and conglomerate.||||||
10280|Leard Formation|66191|5|Briefly described|p485 Fig.2, p485|Early Permian|Early Permian|Gunnedah Basin. Underlies the Maules Creek Formation, overlies both the Boggabri Volcanics and the Werrie Basalt. Lacustrine sediments inundated by the Maules Creek Formation.||||||
10280|Leard Formation|68003|5|Briefly described|p38 Fig.3-j, p40.|Early Permian|Early Permian|Gunnedah Basin, Brigalow Belt South Bioregion. Part-equivalent to Greta Coal Measures in the Sydney Basin.||Unit in Bellata Group.||||
10280|Leard Formation|68004|5|Briefly described|p23 Table 1, p31, p137, p210.|Early Permian|Early Permian|Gunnedah Basin. A thin veneeer, a few metres thick, on the basal volcanics in the Maules Creek Sub-basin. Flint clay (kaolin) has been mined from this unit near Gunnedah; has moderate prospectivity.||Unit in Bellata Group.|||Pelletoidal claystone, conglomerate, sandstone and siltstone commonly interbedded with coal.|
10280|Leard Formation|70791|5|Briefly described|p275, p277-278, p281, p286-287, p292-294|Cisuralian|Cisuralian|Previously the Baan Baa Formation (after Thomson, 1986). Gunnedah Basin. Formed from erosion of kaolinised Werrie Basalt and Boggabri Volcanics. Up to 30m thick. Has low gamma ray response. Diachronous.||Bellata Group.||Nonconformably overlies Werrie Basalt and Boggabri Volcanics. Is overlain by Porcupine Formation.|Dark grey and light grey, barren pelletoidal claystones.|
10280|Leard Formation|70878|5|Briefly described|p718 Fig.13|Permian|Permian|Gunnedah Basin.||Bellata Group.||Is overlain by Goonbri Formation.||
10285|Lease Tuff Member|22857|5|Briefly described|p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Meryula Formation (Kopyje Group, Cobar Supergroup). Max. thickness: <250m. Geological Province: Kopyje Shelf (Darling Basin).||||||
10285|Lease Tuff Member|23171|6|Mentioned|p31|||||||||
10285|Lease Tuff Member|23173|6|Mentioned|Map Legend|||||||||
10285|Lease Tuff Member|35287|6|Mentioned|p7|||||||||
10285|Lease Tuff Member|39618|2|Defined|p78|Early Devonian|Early Devonian|||||||
10285|Lease Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
10285|Lease Tuff Member|72958|6|Mentioned|p52|||Of Felton (1981). Said to be interbedded with the Meryula Formation. In close proximity to a 'strongly chloritised and silicified rhyolite' (Leeson, 1975) which is consistent with the description of the dated, unnamed dacite (GASampleNo 2756756), with age 410.8+/-1.9 Ma, implying that this unit must have intruded Meryula Formation, rather than being interbedded.||Said to be Meryula Formation, Kopyje Group.|||Strongly chloritised and silicified rhyolite.|
10332|Lemington Seams|29942|4|Described|Fig.2|||||||||
10362|Levy Greywacke Member|31999|6|Mentioned|Table 1|||||||||
10362|Levy Greywacke Member|34554|6|Mentioned|p233|||||||||
10362|Levy Greywacke Member|41796|6|Mentioned|p307|||||||||
10362|Levy Greywacke Member|43400|2|Defined|p178||Givetian|not equal to Crawney Limestone Member||||||
10362|Levy Greywacke Member|43406|14|Not recorded|p42||Middle Devonian|Member of Yarrimie Formation (Tamworth Group)||||||
10362|Levy Greywacke Member|43428|14|Not recorded|p140|||||||||
10376|Lick Hole Formation|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
10376|Lick Hole Formation|32583|3|Fully described|p371|||L.Dev. See also P372-374||||||
10376|Lick Hole Formation|42032|6|Mentioned|p497|||||||||
10376|Lick Hole Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Ravine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
10378|Licking Hole Creek Diorite|32590|6|Mentioned|Fig.2|||||||||
10379|Licount Mudstone|37987|6|Mentioned|p223|||||||||
10383|Lidsdale Coal|22578|6|Mentioned|p398|||||||||
10383|Lidsdale Coal|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cullen Bullen Subgroup (Illawarra Coal Measures). Max. thickness: 2m. Geological Province: Sydney Basin.||||||
10383|Lidsdale Coal|39232|4|Described|p108|||||||||
10383|Lidsdale Coal|40256|6|Mentioned|Fig.3|||||||||
10383|Lidsdale Coal|40332|6|Mentioned|Fig.4|||||||||
10383|Lidsdale Coal|40806|2|Defined|p153|Permian|Permian|Prob. Permian||||||
10383|Lidsdale Coal|42657|5|Briefly described|p77|||||||||
10383|Lidsdale Coal|43146|6|Mentioned|p39|||||||||
10383|Lidsdale Coal|68003|6|Mentioned|p41.|Late Permian|Late Permian|Western Coalfield, Sydney Basin.||||||
10383|Lidsdale Coal|68004|5|Briefly described|p59.|Late Permian|Late Permian|Western Coalfield. Thickness varies betwewen 0.5 and 5 m. Unit is divided into upper and lower sections by a persistent thin tuffaceous claystone layer. Economic coal seam in lower section.||Unit in Cullen Bullen Subgroup.||Overlies Blackmans Flat Formation.|Predominantly dull coal, thin claystone, carbonaceous and tuffaceous claystone and siltstone.|
10430|Lincount Mudstone|23185|6|Mentioned|p160|||?Equivalent of Goonoo Goonoo Mudstone of Mory (1981).||||||
10430|Lincount Mudstone|32865|6|Mentioned|p481|||||||||
10430|Lincount Mudstone|43417|4|Described|Map Legend||Late Devonian|||||||
10430|Lincount Mudstone|45088|6|Mentioned|p11|||Refers Manser (1967,1968). Crook's terminology preferred.||||||
10438|Lingula beds|32918|6|Mentioned|p12|||Refers Rade (1963 unpubl)||||||
10438|Lingula beds|41639|6|Mentioned|p10|||||||||
10454|Liscombe Pools Limestone|13996|6|Mentioned|p132|Silurian|Silurian|Canowindra area. Contains one of two known endemic Silurian tabulates, Liscombea.||||||
10454|Liscombe Pools Limestone|22857|5|Briefly described|p458 App.1, Tb.A1.6|Llandovery|Llandovery|Of the Cudal Group. Max. thickness: 10m. Geological Province: Cowra Trough.||||||
10454|Liscombe Pools Limestone|23214|2|Defined|p115|Wenlock|Llandovery|Of Cudal Group. Originally included as part of the Millambri Formation. Max thickness 10m.  Overlying unit: Gospel Oak Shale, underlying unit: Millambri Formation.||||||
10454|Liscombe Pools Limestone|32590|6|Mentioned|Fig.1|||||||||
10454|Liscombe Pools Limestone|35244|6|Mentioned|p35|||||||||
10454|Liscombe Pools Limestone|36283|6|Mentioned|p109|||||||||
10454|Liscombe Pools Limestone|40328|4|Described|p83|||||||||
10454|Liscombe Pools Limestone|41296|6|Mentioned|p130|||||||||
10454|Liscombe Pools Limestone|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Cudal Group. Consists of grey, fine grained, commonly silicified bioclastic limestone.||||||15-JUL-08
10454|Liscombe Pools Limestone|43782|6|Mentioned|Map diagram|Llandovery|Llandovery|Of Cudal Group.||||||15-JUL-08
10454|Liscombe Pools Limestone|63287|5|Briefly described|p317 Fig. 2|Llandovery|Llandovery|Of the Cudal Group. Overlain by Gospal Oak Shale. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
10454|Liscombe Pools Limestone|68592|5|Briefly described|p413, p416, p1866-7|Llandovery|Llandovery|Cowra Trough. 15-20 km E of Canowindra. Contains the conodont Astropentagnathus irregularis.||Basal unit in Cudal Group.||||
10455|Lismore Basalt|22582|5|Briefly described|Fig2,p70|||Overlain by Nimbin Rhyolite||||||
10455|Lismore Basalt|22773|5|Briefly described|p345|||||||||
10455|Lismore Basalt|22857|6|Mentioned|p345|Cenozoic|Cenozoic|Predominantly tholeiitic with occasional alkaline types of formations. Included in the central-volcano provinces of NSW.||||||19-NOV-08
10455|Lismore Basalt|23811|5|Briefly described|Map Legend|Cenozoic|Cenozoic|Of Lamington Group.||||||19-NOV-08
10455|Lismore Basalt|23812|5|Briefly described|p37 Tb.5|Tertiary|Tertiary|||||||
10455|Lismore Basalt|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
10455|Lismore Basalt|30604|1|Redefined|p69|Cenozoic|Cenozoic|||||||19-NOV-08
10455|Lismore Basalt|30605|4|Described|p268|||||||||
10455|Lismore Basalt|30687|6|Mentioned|p65|||Tertiary age||||||
10455|Lismore Basalt|30785|6|Mentioned|p400|||||||||
10455|Lismore Basalt|31130|6|Mentioned|Fig. 2|||Correlation||||||
10455|Lismore Basalt|34092|5|Briefly described|p11|||||||||
10455|Lismore Basalt|34340|6|Mentioned|Table 6.1|||||||||
10455|Lismore Basalt|34593|6|Mentioned|p539|||||||||
10455|Lismore Basalt|35045|6|Mentioned|p110|||||||||
10455|Lismore Basalt|35050|6|Mentioned|p130|||||||||
10455|Lismore Basalt|35296|4|Described|p12|||||||||
10455|Lismore Basalt|36056|6|Mentioned|p29|||||||||
10455|Lismore Basalt|36411|6|Mentioned|p269|||Refs.Duggan & Mason 1978 for redefinition.||||||
10455|Lismore Basalt|36806|6|Mentioned|p131|||||||||
10455|Lismore Basalt|37391|6|Mentioned|p26|||||||||
10455|Lismore Basalt|40896|4|Described|p6|||||||||
10455|Lismore Basalt|43161|4|Described|12|||||||||
10455|Lismore Basalt|43344|14|Not recorded|p101|||Overlain by Dorroughby Tuff||||||
10455|Lismore Basalt|43881|2|Defined|p6-7,49,54-55,64,154||Tertiary|Basal unit of Macpherson Volcanics.||||||
10455|Lismore Basalt|44818|6|Mentioned|p275|||||||||
10455|Lismore Basalt|48917|6|Mentioned|p7|||Refers McDougal & Wilkinson (1967), McElroy (1962)||||||
10455|Lismore Basalt|60079|5|Briefly described|Map Legend|Tertiary|Tertiary|Of the Lamington Volcanics.||||||21-JUL-04
10455|Lismore Basalt|66855|6|Mentioned|p955.|||Tertiary.||||||
10455|Lismore Basalt|69599|5|Briefly described|p640|||Tweed volcano, centred on Mount Warning.|c.24 Ma.|||Approximate equivalent of Beechmont Basalt in QLD.||
10455|Lismore Basalt|73581|5|Briefly described|p6, p14|Oligocene|Oligocene|Tweed Volcano. Underlies Binna Burra Rhyolite/Nimbin Rhyolite.|23.9+/-0.2 Ma K-Ar (plagioclase)|Lamington Volcanics, basal part|||Basalt lavas.|
10470|Lithgow Coal|22857|5|Briefly described|p528App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cullen Bullen Subgroup (Illawarra Coal Measures). Max. thickness: 5m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
10470|Lithgow Coal|38603|6|Mentioned|p83|||||||||
10470|Lithgow Coal|38614|6|Mentioned|p9|||||||||
10470|Lithgow Coal|39232|4|Described|p108|||||||||
10470|Lithgow Coal|40256|6|Mentioned|p305|||||||||
10470|Lithgow Coal|40275|6|Mentioned|p62|||||||||
10470|Lithgow Coal|40321|6|Mentioned|p19|||||||||
10470|Lithgow Coal|40332|6|Mentioned|p23|||||||||
10470|Lithgow Coal|40806|2|Defined|p152|Permian|Permian|Prob. Permian||||||
10470|Lithgow Coal|40824|6|Mentioned|Table 1|||||||||
10470|Lithgow Coal|41226|6|Mentioned|Fig.13|||||||||
10470|Lithgow Coal|42657|4|Described|p75|||||||||
10470|Lithgow Coal|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
10470|Lithgow Coal|68003|6|Mentioned|p41.|Late Permian|Late Permian|Western Coalfield, Sydney Basin.||||||
10470|Lithgow Coal|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield. Crops out persistently throughout the region.||Unit in Cullen Bullen Subgroup.||Overlies Marrangaroo Formation. Is overlain by Blackmans Flat Formation.|Dull coal with minor bright layers; a few thin carbonaceous or tuffaceous claystone layers in the upper half.|
10511|Livingstone Porphyry|22768|6|Mentioned|p178|||||||||
10511|Livingstone Porphyry|22857|6|Mentioned|p178|Early Devonian|Early Devonian|||||||
10511|Livingstone Porphyry|32820|6|Mentioned|p6|||||||||
10511|Livingstone Porphyry|36413|2|Defined|p85|Early Devonian|Early Devonian|Also mention p45.||||||24-SEP-20
10511|Livingstone Porphyry|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Dacitic porphyry, minor xenoliths. GSNSW map code: S-Dl.||||||
10511|Livingstone Porphyry|39626|6|Mentioned|p276|||||||||
10511|Livingstone Porphyry|40328|4|Described|p208|||||||||
10511|Livingstone Porphyry|42820|6|Mentioned|p71|||||||||
10511|Livingstone Porphyry|49690|5|Briefly described|Tb.7, p15-16|||West of Michelago. Intrudes Colinton Volcanics, and Rothlyn Formation, near base.|||||Sill-like body. Mainly very coarse, massive, grey rhyolitic porphyry; phenocrysts include a few, small, pink K-feldspar; local fine-grained very k-feldspar-rich bodies|14-FEB-14
10511|Livingstone Porphyry|61895|6|Mentioned|p134 Fig.1,|||||||||
10520|Llanillo Silcrete|23053|6|Mentioned|Fig10p17|Early Eocene|Late Paleocene|||||||
10520|Llanillo Silcrete|35187|6|Mentioned|p55|||||||||
10520|Llanillo Silcrete|61155|5|Briefly described|p19|Early Oligocene|Early Oligocene|In the Walgett area.||||||
10520|Llanillo Silcrete|68593|5|Briefly described|p3, p6, p31|Eocene|Eocene|Taylor (1976, 1978). Silicified Cretaceous rocks usually extend down no more than 10m, with kaolinisation to 100m depth and local ferruginisation.||||||
10527|Lobbs Hole Limestone|32583|6|Mentioned|p371|||Refers Andrews (1901)||||||
10529|Lobelia Limestone Member|24551|6|Mentioned|p614||Late Llandovery|Of the Towanga Formation||||||
10529|Lobelia Limestone Member|37727|5|Briefly described|p49|||See also P19.||||||
10529|Lobelia Limestone Member|39447|6|Mentioned|p9|||||||||
10529|Lobelia Limestone Member|40328|6|Mentioned|p71|||||||||
10550|Lochinvar Formation|22591|6|Mentioned|p 66|||||||||
10550|Lochinvar Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 850m||||||
10550|Lochinvar Formation|22612|6|Mentioned|423|Early Permian|Early Permian|Geol province Sydney Basin||||||
10550|Lochinvar Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Basalt, siltstone, sandstone. Max. thickness: 835m. Geological Province: Sydney Basin.||||||
10550|Lochinvar Formation|22969|3|Fully described|p 16, Fig 2.2||Permian|Dated Sakmarian ~295-289 Ma. Of Dalwood Group, Sydney Basin. Overlying unit Allandale Formation. Max. thickness:  835 m.||||||12-NOV-08
10550|Lochinvar Formation|22970|5|Briefly described|Plate 6|Permian||||||||
10550|Lochinvar Formation|23540|5|Briefly described|Fig 3 p 420|||||||||
10550|Lochinvar Formation|24079|5|Briefly described|p430|Early Permian|Late Carboniferous|Of Dalwood Group.  Gewological Province: Sydney Basin.||||||
10550|Lochinvar Formation|24121|5|Briefly described|p4, p139|||Of Dalwood Group.||||||25-AUG-22
10550|Lochinvar Formation|29437|6|Mentioned|p136|||Permian||||||
10550|Lochinvar Formation|29915|6|Mentioned|p68|||||||||
10550|Lochinvar Formation|30341|6|Mentioned|p136|||Permian age||||||
10550|Lochinvar Formation|30450|6|Mentioned|Table 1|||Permian age||||||
10550|Lochinvar Formation|30545|6|Mentioned|Fig.2|||Sakmarian||||||
10550|Lochinvar Formation|31081|6|Mentioned|Fig. 2|||Listed in Table.||||||
10550|Lochinvar Formation|31298|6|Mentioned|p16|||||||||
10550|Lochinvar Formation|31883|6|Mentioned|Table 1|||||||||
10550|Lochinvar Formation|32094|6|Mentioned|p383|||||||||
10550|Lochinvar Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis elongata||||||
10550|Lochinvar Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
10550|Lochinvar Formation|32672|6|Mentioned|p676|||||||||
10550|Lochinvar Formation|32840|6|Mentioned|Table 5|||||||||
10550|Lochinvar Formation|32943|6|Mentioned|p94|||See also p105.||||||20-SEP-18
10550|Lochinvar Formation|32945|6|Mentioned|p74|||See also P83 & Fig.1||||||
10550|Lochinvar Formation|33701|6|Mentioned|Fig.1|||Sakmarian.||||||
10550|Lochinvar Formation|33711|6|Mentioned|p382|||See also Table 2.||||||
10550|Lochinvar Formation|33867|5|Briefly described|p3|||||||||
10550|Lochinvar Formation|34072|6|Mentioned|Fig.4.5|||||||||
10550|Lochinvar Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
10550|Lochinvar Formation|34170|6|Mentioned|p45|||Lower Permian.||||||
10550|Lochinvar Formation|34292|6|Mentioned|Table 1|||Permian||||||
10550|Lochinvar Formation|34444|6|Mentioned|Map legend|Permian|Permian|||||||
10550|Lochinvar Formation|34445|3|Fully described|p320|||||||||
10550|Lochinvar Formation|34447|5|Briefly described|p318|||Fossils. See also Fig.5.2||||||
10550|Lochinvar Formation|34448|4|Described|p431|||Permian||||||
10550|Lochinvar Formation|34512|6|Mentioned|p52|||Lower Permian||||||
10550|Lochinvar Formation|35284|6|Mentioned|Fig.1|||||||||
10550|Lochinvar Formation|35380|5|Briefly described|p190|||Glacial features||||||
10550|Lochinvar Formation|35862|6|Mentioned|Fig.7|||||||||
10550|Lochinvar Formation|36042|6|Mentioned|Table 1|||||||||
10550|Lochinvar Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
10550|Lochinvar Formation|36794|6|Mentioned|p386|||||||||
10550|Lochinvar Formation|37082|6|Mentioned|p160|||||||||
10550|Lochinvar Formation|37086|6|Mentioned|p183|||||||||
10550|Lochinvar Formation|37087|6|Mentioned|p192|||||||||
10550|Lochinvar Formation|37092|6|Mentioned|p229|||||||||
10550|Lochinvar Formation|37922|5|Briefly described|p481|||||||||
10550|Lochinvar Formation|38204|6|Mentioned|p79|||||||||
10550|Lochinvar Formation|38217|6|Mentioned|p272|||||||||
10550|Lochinvar Formation|38801|6|Mentioned|Fig.3|||||||||
10550|Lochinvar Formation|38837|6|Mentioned|p232|||||||||
10550|Lochinvar Formation|39262|6|Mentioned|p122|||||||||
10550|Lochinvar Formation|39287|6|Mentioned|p20|||See also Fig.2.5||||||
10550|Lochinvar Formation|39288|4|Described|p57|||||||||
10550|Lochinvar Formation|39304|6|Mentioned|Fig. 19.2|||||||||
10550|Lochinvar Formation|39306|6|Mentioned|p387|||||||||
10550|Lochinvar Formation|39307|6|Mentioned|p438|||||||||
10550|Lochinvar Formation|39833|6|Mentioned|p297|||||||||
10550|Lochinvar Formation|40093|6|Mentioned|p35|||[probably mistakenly entered as QLD unit.CEBNov97]||||||
10550|Lochinvar Formation|40166|6|Mentioned|Fig.2|||||||||
10550|Lochinvar Formation|40883|6|Mentioned|p14|||||||||
10550|Lochinvar Formation|41580|6|Mentioned|Table 1|||||||||
10550|Lochinvar Formation|41902|5|Briefly described|p5 Table 1|||||||||
10550|Lochinvar Formation|42000|6|Mentioned|p55|||||||||
10550|Lochinvar Formation|42547|5|Briefly described|p33|Permian||||||||
10550|Lochinvar Formation|43017|5|Briefly described|Fig.1,p372|||||||||
10550|Lochinvar Formation|43018|5|Briefly described|Table 1,p386|||||||||
10550|Lochinvar Formation|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Early Permian|Of Gyarran Volcanics (Hunter region) and Dalwood Group (Newcastle region), Sydney Basin. Thick basaltic and rhyolitic sequences deposited at the same time as the Boggabri Volcanics and Werrie Basalt (Gunnedah Basin).||||||
10550|Lochinvar Formation|43257|5|Briefly described|Map Legend||Early Permian|Of Dalwood Group.||||||
10550|Lochinvar Formation|43344|14|Not recorded|p84,88|Early Permian||Unit of Dalwood Group||||||
10550|Lochinvar Formation|43385|14|Not recorded|p179,180||Sakmarian|Early Permian||||||
10550|Lochinvar Formation|43440|14|Not recorded|p36,64,67,91|||||||||
10550|Lochinvar Formation|43447|4|Described|Table 1,p16||Permian|Part of Dalwood Group.||||||12-NOV-08
10550|Lochinvar Formation|43474|14|Not recorded|p7,25||Sakmarian|||||||
10550|Lochinvar Formation|43479|14|Not recorded|p186,218||Sakmarian|||||||
10550|Lochinvar Formation|44040|14|Not recorded|p27|||||||||
10550|Lochinvar Formation|44219|14|Not recorded|p29,31-32,35,43||Sakmarian|||||||
10550|Lochinvar Formation|44348|14|Not recorded|p56|||||||||
10550|Lochinvar Formation|44372|6|Mentioned|p40|||||||||
10550|Lochinvar Formation|44855|14|Not recorded|p18|Permian|Carboniferous|||||||
10550|Lochinvar Formation|45006|14|Not recorded|Tb.1,opp.p3|||||||||
10550|Lochinvar Formation|45016|14|Not recorded|p.18|||Glaciation.||||||
10550|Lochinvar Formation|45090|6|Mentioned|p7|||Time correlation chart||||||
10550|Lochinvar Formation|47041|6|Mentioned|p167|||See also Fig.2.||||||
10550|Lochinvar Formation|47056|6|Mentioned|Fig.2 P523|||||||||
10550|Lochinvar Formation|48926|6|Mentioned|p54|||p54 et seq.||||||20-SEP-18
10550|Lochinvar Formation|49644|5|Briefly described|Table|||||||||
10550|Lochinvar Formation|60281|5|Briefly described|p54|Early Permian|Early Permian|Of the Dalwood Group (lower part).  Poorly fossiliferous siltstone, claystone, sandstone - interbedded basalt flows, pyroclastics and tuff; crinoidal limestone at base.  Overlain by Allandale Fm.  Age: 295-290Ma and 293-285Ma.  Max. thick: 835m.||||||27-APR-05
10550|Lochinvar Formation|60289|6|Mentioned|p2|Early Permian||||||||22-FEB-05
10550|Lochinvar Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Asselian|Correlated with Beckers Formation, Wasp Head Formation, Woody Island Formation and Quamby Formation. Geological Province: Sydney Basin.||||||
10550|Lochinvar Formation|60386|6|Mentioned|p296|Cisuralian||Bowen/Sydney Basin. Non-marine. Age shown ~Asselian.||||||
10550|Lochinvar Formation|61315|5|Briefly described|p172, Table SY1|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: base of Sydney Basin/ Newcastle area.||||||
10550|Lochinvar Formation|61529|5|Briefly described|p871|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin.||||||
10550|Lochinvar Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||17-MAR-09
10550|Lochinvar Formation|61791|6|Mentioned|p325|||||||||
10550|Lochinvar Formation|63832|5|Briefly described|p131 fig 2, p135|Sakmarian|Sakmarian|Sussmilch and David (1919); Booker (1961). Hunter Valley, Sydney Basin. Fifth (P1) glaciation.||Unit in Dalwood Group.||||13-DEC-17
10550|Lochinvar Formation|64631|5|Briefly described|p44 Fig.2, p49.|Sakmarian|Sakmarian|NE Sydney Basin. Shows evidence of glaciation. Some biostratigraphic age control within unit.||Unit in lower Dalwood Group.||Is overlain by Allandale Formation.||
10550|Lochinvar Formation|67663|6|Mentioned|p518|Permian|Permian|Early Permian. Mis-spelt as Lochinar in Fig.1.||Of the Dalwood Group||||
10550|Lochinvar Formation|68003|5|Briefly described|p38 Fig.3-j, p40.|Early Permian|Early Permian|Hunter Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Mis-spelt as Lochinvale Formation in Fig.3-j. Thick volcanic sequence.||Unit in Dalwood Group.||Overlies Seaham Formation. Is overlain by Allandale Formation.||
10550|Lochinvar Formation|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||Basal unit in Dalwood Group.||Overlies Seaham Formation. Is overlain by Allandale Formation.||
10550|Lochinvar Formation|68493|5|Briefly described|p3 Fig.1, p5 Fig.2, p10 Fig.4|Sakmarian|Sakmarian|Sydney Basin. Approximately 835m thick in the Lochinvar area. Poorly exposed with limited fossil content.||Basal unit of the Dalwood Group.||Overlain by the Allandale Formation. Correlates with Beckers Formation in Cranky Corner Basin.|Dominated by a coarsening-upward sequence of mudstone and sandstone, with interbedded basalt flows.|
10550|Lochinvar Formation|69297|6|Mentioned|p501, p502 fig 5.43|Artinskian|Sakmarian|Sydney Basin.||Dalwood Group||Unconformably overlies the Seaham Formation. Overlain by the Allandale Formation.||
10550|Lochinvar Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|||Unit in Gyarran Volcanics.||||
10550|Lochinvar Formation|70096|6|Mentioned|p221|||Of northern Sydney Basin.||||||
10550|Lochinvar Formation|73304|6|Mentioned|p75|||||Gyarran Volcanics||||
10578|Lockyersleigh Granite|24317|5|Briefly described|p15 Fig.1|Carboniferous|Carboniferous|||||||
10578|Lockyersleigh Granite|42726|5|Briefly described|map legend|Carboniferous||52. Variation on Lockyersleigh Adamellite.||||||
10578|Lockyersleigh Granite|50234|5|Briefly described|Map Legend|Carboniferous|Carboniferous|||||||
10578|Lockyersleigh Granite|64238|5|Briefly described|Map legend|Carboniferous|Carboniferous|Of Lockyersleigh Suite. Pink, med.-gr. granite with K-feldspar and lesser zoned plag. phenocrysts in qtz-feldspar-biotite groundmass + hornblende; +accessory titanite and magnetite; marginal phase of grey, equigran.granodiorite; monzodiorite+aplite dykes.||||||09-SEP-08
10578|Lockyersleigh Granite|68592|2|Defined|p326, p812, p821, p843, p849, p1754-1766|Early Carboniferous|Early Carboniferous|See also p229, p230, p261. First mapped, described and named, as Lockyersleigh Adamellite, by O'Reilly (1966) [who actually used Lockyersleigh adamellite] and later workers. Lithology changed to Granite to comply with standard nomenclature. Redefined here, to incorporate Towrang Granodiorite and Chapmans Creek Granodiorite which were previously used to delineate the marginal phases. Assigned to Oberon Supersuite by Blevin (2011). Sole pluton (and thus type pluton) in Lockyersleigh Suite. Type area and representative locality described. Geochemistry and geophysical properties detailed. Intrudes and contact metamorphoses the Barrallier Ignimbrite. Is correlated with Tuglow, Oberon and Redfern Suites. Quarried for dimension stone at 3 locations W of Marulan. Aeolian sand derived from this unit has been quarried. Rb-Sr whole rock isotope age.|326 +/- 6 Ma (Carr and Jones, 1986).|Unit in Lockyersleigh Suite.||Intrudes Bendoc Group, Longreach Volcanics, Joaramin and Barrallier Ignimbrites, Covan Creek Formation and Kerrawary Siltstone. Is intruded by Billyrambija Dolerite.|An unfractionated, I-type, mafic, medium-grained granite comprising two phases: a central pink, porphyritic granitic phase surrounded by a grey, equigranular more granodioritic phase. Has miarolitic cavities, and monzodiorite and aplite dykes.|
10578|Lockyersleigh Granite|70192|5|Briefly described|Map Legend|Carboniferous|Carbononiferous|Cll. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Lockyersleigh Suite|||Medium-coarse grained, porphyritic, hornblende-biotite granite with equigranular, hornblende-biotite granodiorite marginal phase; monzodiorite and aplite dykes.|
10578|Lockyersleigh Granite|70542|5|Briefly described|Map Legend|Carboniferous|Carbononiferous|||Lockyersleigh Suite|||Medium-coarse grained, porphyritic, hornblende-biotite granite with equigranular, hornblende-biotite granodiorite marginal phase; monzodiorite and aplite dykes.|
10578|Lockyersleigh Granite|71069|6|Mentioned|p135, p170|Carboniferous|Carboniferous|||||Intrudes the Covan Creek Formation.||
10603|London Bridge Formation|12185|5|Briefly described|map legend|Middle Silurian|Middle Silurian|Grouped with Fairbairn Group, Mount Pleasant Porphyry, Saint Johns Beds in legend. Calcareous shale, limestone, sandstone, tuff, porphyry, altered acid lavas. BMR map symbol: Smf.||||||
10603|London Bridge Formation|33325|5|Briefly described|Table 2|||Early Ludlovian. ?Same as Cappanana Beds P14.||||||
10603|London Bridge Formation|37727|5|Briefly described|p68|||||||||
10603|London Bridge Formation|37728|6|Mentioned|Table 4|||||||||
10608|Londonderry Clay|31056|4|Described|p5|||||||||
10608|Londonderry Clay|33671|6|Mentioned|Fig.2|||||||||
10608|Londonderry Clay|35098|4|Described|p4|||||||||
10608|Londonderry Clay|35312|6|Mentioned|Fig.2|||||||||
10608|Londonderry Clay|39308|6|Mentioned|p494|||||||||
10608|Londonderry Clay|40656|6|Mentioned|p35|||||||||
10608|Londonderry Clay|41391|6|Mentioned|p46|||||||||
10608|Londonderry Clay|42442|6|Mentioned|p23|||||||||
10608|Londonderry Clay|42925|2|Defined|p35|early Miocene|late Oligocene|||||||
10608|Londonderry Clay|42926|4|Described|map legend||Miocene|||||||
10608|Londonderry Clay|65195|6|Mentioned|p4 Fig.2|Tertiary|Tertiary|Overlies Rickaby's Creek Gravels||||||
10608|Londonderry Clay|70587|5|Briefly described|Map Legend|Miocene|Oligocene||||||Clay with patches of ferruginised consolidated sand.|17-JUN-16
10608|Londonderry Clay|73248|4|Described|p304, p306-310, App. p6|||Cumberland Basin, northwest. [Gradational] upwards-finning contact with the underlying Rickabys Creek Gravel. Thickest along the down-warped southern margin of the Hawkesbury Plateau. Depositional environment is difficult to establish based on lithology alone. Probably lacustrine although may represent overbank sediments. A lake leading to the deposition of this unit may have developed due to pooling of water behind the rising Hornsby Plateau until such time that the river through the plateau was entrenched. Top surface of the unit dips towards the depocentre of the Penrith Basin, which indicates syn-depositional Cenozoic subsidence. Deposition probably predated the major phase of movement along the Lapstone Structural Complex.||||[Conformably?] underlain by Rickabys Creek Gravel.|Highly weathered, composed mainly of secondary clay, such as kaolinite and illite, and sandy lenses.|
10608|Londonderry Clay|75059|6|Mentioned|p8|Cenozoic|Cenozoic|NW Cumberland Basin, Sydney area.||||||
10619|Long Flat Volcanics|12185|5|Briefly described|map legend|Silurian|Silurian|Quartz felsite, rhyolite, toscanite, porphyry, tuff. BMR map symbol: Svl.||||||
10619|Long Flat Volcanics|22768|6|Mentioned|p176|||||||||
10619|Long Flat Volcanics|22857|4|Described|p176, p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Crystal-lithic and welded tuffs, rhyolite, minor sediments, arenite, siltstone and shale. Max. thickness: >1.5km. See also p480 App.1 Tb.A1.6.||||||
10619|Long Flat Volcanics|23048|6|Mentioned|p2|||||||||
10619|Long Flat Volcanics|23309|6|Mentioned|p390|||||||||
10619|Long Flat Volcanics|24266|5|Briefly described|p1485|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
10619|Long Flat Volcanics|24272|5|Briefly described|p1646, 1651|Late Silurian|Late Silurian|Age: 424-409 Ma.||||||09-MAR-05
10619|Long Flat Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
10619|Long Flat Volcanics|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
10619|Long Flat Volcanics|30735|2|Defined|p33|Silurian|Silurian|||||||
10619|Long Flat Volcanics|30736|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
10619|Long Flat Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
10619|Long Flat Volcanics|31161|5|Briefly described|PA7|||||||||
10619|Long Flat Volcanics|31411|5|Briefly described|p16|||||||||
10619|Long Flat Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
10619|Long Flat Volcanics|32672|6|Mentioned|p672|||||||||
10619|Long Flat Volcanics|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
10619|Long Flat Volcanics|33325|6|Mentioned|p14|||Sil.||||||
10619|Long Flat Volcanics|34059|6|Mentioned|Map legend|Silurian|Silurian|||||||
10619|Long Flat Volcanics|34692|6|Mentioned|p183|||||||||
10619|Long Flat Volcanics|36413|6|Mentioned|Table 3|||||||||
10619|Long Flat Volcanics|37727|5|Briefly described|p68|||See also P18 and P21.||||||
10619|Long Flat Volcanics|39028|6|Mentioned|Map legend|Pridolian|Ludlovian|Pridolian to Ludlovian||||||
10619|Long Flat Volcanics|40276|2|Defined|p6|Late Silurian|Late Silurian|||||||
10619|Long Flat Volcanics|40328|4|Described|p185|||||||||
10619|Long Flat Volcanics|42497|5|Briefly described|Map legend|Pridolian|Ludlovian|||||||
10619|Long Flat Volcanics|42726|5|Briefly described|map legend|Early Devonian|Silurian|||||||
10619|Long Flat Volcanics|44093|5|Briefly described|p221 App. 1|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
10619|Long Flat Volcanics|62070|5|Briefly described|p38|Late Silurian|Late Silurian|||Mount Fairy Group [?]||Overlies the De Drack Formation. Overlain by Palerang Formation.|Felsic volcanics.|
10619|Long Flat Volcanics|66300|5|Briefly described|p35, pp41-51. |Early Devonian|Early Devonian|The ages of all dated units in the LFV are indistinguishable from each other and the "northern phase" of the Braidwood Granodiorite.||Unit in Bindook Group.|Said in this study to include locally the Kadoona Dacite, Manar Ignimbrite, Toggannoggra Rhyolite, Croppies Gunyah Rhyolite and Kain Porphyry Members.|Intruded by Braidwood Granodiorite and Boro Granite.||
10619|Long Flat Volcanics|68592|6|Mentioned|p725-6|||Felton and Huleatt (1977) and Wyborn and Owen (1986) included additional formations in Mount Fairy Group in Braidwood and Araluen 1:100 000 map sheet areas. These included Long Flat Volcanics and Bombay Volcanics. However, recent mapping (Fitzherbert et al. 2011) and age dating (Bodorkos and Simpson 2008) has combined Long Flat and Bombay Volcanics and placed them in Bindook Group.||||||
10619|Long Flat Volcanics|69159|5|Briefly described|Map legend|Pragian|Lochkovian|||Unit in Bindook Group.|Includes Tooggannoggra Rhyolite, Ralpin Valley Sandstone, Kain Porphyry, Manar Ignimbrite, Kadoona Dacite, and Croppies Gunyah Ignimbrite, Members.|Overlies Jinglemoney Conglomerate.|Dacitic to rhyolitic, mainly crystal-rich welded ignimbrite; minor conglomerate, volcanic sandstone and rare siltstone; medium- to coarse-grained, crystal-rich, plagioclase-quartz-ferromagnesian-phyric dacite.|02-SEP-15
10619|Long Flat Volcanics|69270|6|Mentioned|p16, p23-4, p30|Early Devonian|Early Devonian|||||||
10619|Long Flat Volcanics|69564|5|Briefly described|p2, p5-6, p10, p14|Devonian|Devonian|Hosts minor gold mineralisation in the Dargues Reef-Majors Creek area.|411.5 +/- 3.1 Ma (Bodorkos et al., 2008).|||Is intruded by Braidwood Granodiorite.||
10619|Long Flat Volcanics|69635|6|Mentioned|p18||||||Includes Kadoona Dacite Member, Tally Ho Ignimbrite Member|||16-JUL-15
10619|Long Flat Volcanics|71069|6|Mentioned|p134, p143, p147, p154|Lochkovian|Lochkovian|Ages are SHRIMP U-Pb from Bodorkos et al 2008/2010.|414.1 +/- 2.8 Ma to 412.3 +/- 2.3 Ma|Bindook Group||Conformably overlies the De Drack Formation.|Pyroclastic felsic volcanics with abundant welded ignimbrite and dactic compositions.|
10619|Long Flat Volcanics|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Bindook Group.|Kadoona Dacite Member; Tally Ho, Croppies Gunyah, Manar, Ignimbrite Members; Toggannoggra Rhyolite Member; Kain Porphyry Member; Ralpine Valley Sandstone Member.|Overlies Jinglemoney Conglomerate.|Dacitic to rhyolitic, predominantly crystal-rich welded ignimbrite; medium- to coarse-grained, crystal-rich, plagioclase-quartz-ferromagnesian-phyric dacite, minor conglomerate, volcaniclastic sandstone and rare siltstone.|
10619|Long Flat Volcanics|71700|3|Fully described|vi, viii, p10, p15, p23-p26, CD|Early Devonian|Early Devonian|Named for the Long Flat property GR 744093 6060493 and the Long Flat Trigonometrical Station.No representative type section was nomiated by previous authors, the authors of this volume propose two representative sections between GR 743628 6095895 to GR 746755 6089855 and the other from GR 742033 6077844 to GR 739163 6079678. Anderson (1893) described the sequence of volcanics in Braidwood as the Long Flat Porphyries. Joplin (1953) used Manar Porphyry for the same rocks before Kennedy (1961) subdivided Manar Porphyry into four subunits. Best et al (1964) formally defined the Long Flat Volcanics in 1964. Wyborn and Owen (1986) thereafter discarded the Bombay Volcanics and included rocks previously assigned to that unit within the Long Flat Volcanics.  Ages are SHRIMP U-Pb dates, additional SHRIMP dates include 413.4 +/- 2.6 Ma and 413.0 +/- 2.3 Ma. All SHRIMP dates are derived from Bodorkos and Simpson 2008 and Bodorkos et al, 2010. Hosts small barite deposits and prospects. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. This unit had an estimated thickness of approximately 2000m however it is noted that this estimate by Felton and Huleatt (1977) did not include rocks belonging to the Bombay Volcanics which is now included in the Long Flat Volcanics; thus the total thickness is now estimated at 3745m. Also includes the Toggannoggra Rhyolite Member, Kain Porphyry Member, Ralpine Valley Sandstone Member and the Wongabel Rhyodacite Member.Faulted against the Abercrombie Formation, Cardinal View Formation and Boro Granite. See also p41-p44, p58, p62-p63, p65-p67, p71, p75, p79-p80, p82, p85-p86, p100, p103, p110, p114.|414.1 +/- 2.8 Ma to 412.3 +/- 2.3 Ma|Bindook Group|Includes the Kadoona Dacite Member, Tally Ho Ignimbrite Member, Manar Ignimbrite Member, Croppies Gunyah Ignimbrite Member.|Unconformably overlies the Adaminaby Group. Overlies the Mount Fairy Group. Conformably overlies the Jinglemoney Conglomerate. Intruded by the Braidwood Granodiorite.|Densely-welded, dacitic to rhyolitic ignimbrite, dacite, immature volcaniclastic conglomerate, sandstone and siltstone/mudstone.|
10624|Long Panel Tuff Member|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Majuba Volcanics (Kopyje Group).||||||
10624|Long Panel Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
10624|Long Panel Tuff Member|42566|3|Fully described|p85|||Reserved as Long Panel.||||||
10624|Long Panel Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|Reserved as Long Panel.||||||
10646|Lookdown Limestone|5253|5|Briefly described|p97, p99|Early Ludlow|Wenlock|Overlain by Cardinal View Shale. Equivalent to Lower Limestone of Carr et al. 1990. Includes tetracorals.||||||
10646|Lookdown Limestone|13996|6|Mentioned|p141-143|Ludlow|Wenlock|Bungonia district. Hosts Schismadon bungoniensis, a new genus and species of megalodont bivalve. Bivalve taxa distribution Table. Hosts a new species of septate murchisoniid.||||||
10646|Lookdown Limestone|22842|4|Described|p25,28|Devonian|Silurian|||||||
10646|Lookdown Limestone|40698|6|Mentioned|p53|||||||||
10646|Lookdown Limestone|70661|3|Fully described|vii, p6, p36-p39|Ludlow|Wenlock|Reinstated as separate to the Cardinal View Formation. Synonymous with Eastern and Lower Limestones of earlier workers. Originally included in  Bungonia Limestone. 100-270m thick.  Forms scattered clumps of boulders in the southern highlands plateau, elsewhere makes up the Bungonia Caves. Age constrained by fossils. Fossil assemblage, structure, geochemistry and metamorphism discussed.||Bungonia Group||Unconformably overlain by Cardinal View Formation, intruded by Glenrock Granodiorite, correlated with lower Campbells Group and Mount Fairy Group, time equivalent of Tugalong Limestone Member|Fossiliferous, biostromal limestone consisting dominantly of biomicrudite and biomicrite with small lenses of primary dolomite, spiculite and quartz rich anhydrite. Wollastonite skarn occurs near the contact with the Glenrock Granodiorite.|
10646|Lookdown Limestone|71303|5|Briefly described|map legend|Wenlock|Wenlock|||Of Bungonia Group.|||Fossiliferous, biostromal limestone; dominantly biomicrudite and biomicrite, with small lenses of primary dolomite. Secondary dolomitisation to 50% locally. Skarn formation locally at contact with intrusions.|
10646|Lookdown Limestone|71700|5|Briefly described|p16, CD|Late Silurian|Late Silurian|Bungonia Shelf. Interpreted to have been deposited in a carbonate shelf system in varied environments including tidal flats, reefs and marine barriers.||Bungonia Group||Overlain by or interfingers with the Cardinal View Formation.|Fossiliferous, biostromal limestone.|
10653|Loomberah Limestone Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Emsian|Emsian|Of the Yarrimie Formation (Tamworth Group). Limestone rudite grading into bioclastic limestone. Max. thickness: 45m. Geological Province: Tamworth Forearc Basin.||||||
10653|Loomberah Limestone Member|30650|4|Described|p315|||||||||
10653|Loomberah Limestone Member|30814|6|Mentioned|p71|||||||||
10653|Loomberah Limestone Member|31999|6|Mentioned|p150|||Table 1||||||
10653|Loomberah Limestone Member|32619|6|Mentioned|p460|||See also P461. L.-M. Dev. Fauna||||||
10653|Loomberah Limestone Member|34554|6|Mentioned|p234|||||||||
10653|Loomberah Limestone Member|39331|6|Mentioned|Table 10-1|||||||||
10653|Loomberah Limestone Member|43344|14|Not recorded|p93||Devonian|Unit of Tamworth Group||||||
10653|Loomberah Limestone Member|43400|2|Defined|p178,179,182,map||Couvinian|(Devonian)||||||
10653|Loomberah Limestone Member|43428|14|Not recorded|p138||Eifelian|Part of Silver Gully Formation (L.Eifelian)||||||
10653|Loomberah Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|||Unit in Tamworth Group.||||
10687|Lovetts Formation|29903|4|Described|p169|||||||||
10687|Lovetts Formation|33285|5|Briefly described|p65|||||||||
10693|Lowana Formation|721|5|Briefly described|Map legend|Famennian|Frasnian|Of the Parry Group.  Green-black siltstone and mudstone with thin, white tuffaceous beds.||||||
10693|Lowana Formation|22639|5|Briefly described|p276|Late Devonian|Late Devonian|||||||
10693|Lowana Formation|22857|5|Briefly described|p498 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Parry Group. Green-black Siltstone and mudstone with thin white tuffaceous beds. Max. thickness: 800m. Geological Province: Tamworth Forearc Basin.||||||
10693|Lowana Formation|23051|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|of Parry Group.||||||
10693|Lowana Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt||||||
10693|Lowana Formation|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
10693|Lowana Formation|24605|5|Briefly described|p934 Fig.3|Devonian|Devonian|Geological Province: New England Orogen.||||||
10693|Lowana Formation|30133|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10693|Lowana Formation|30135|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
10693|Lowana Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
10693|Lowana Formation|31999|6|Mentioned|p151|||||||||
10693|Lowana Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
10693|Lowana Formation|32865|6|Mentioned|p481|||Corr. with Baldwin Fm.||||||
10693|Lowana Formation|34555|4|Described|p238|||See also P240||||||
10693|Lowana Formation|35761|5|Briefly described|p64|||Stratigraphy discussed. See also Table 1.||||||
10693|Lowana Formation|36961|6|Mentioned|p208|||||||||
10693|Lowana Formation|37987|6|Mentioned|p221|||||||||
10693|Lowana Formation|38222|6|Mentioned|Fig.2|||||||||
10693|Lowana Formation|39331|6|Mentioned|Table 10-1|||||||||
10693|Lowana Formation|41009|6|Mentioned|Fig.2|||||||||
10693|Lowana Formation|42631|5|Briefly described|Fig.1 P265|||||||||
10693|Lowana Formation|43091|5|Briefly described|Map legend|||of Parry Group||||||
10693|Lowana Formation|43428|14|Not recorded|p140|||||||||
10693|Lowana Formation|43429|14|Not recorded|Map Legend|||Turbidites||||||
10693|Lowana Formation|43434|4|Described|Map Legend||Late Devonian|||||||
10693|Lowana Formation|43435|2|Defined|Map Legend||Late Devonian|||||||
10693|Lowana Formation|43436|14|Not recorded|Map Legend||Devonian|(Provisional Edition)||||||
10693|Lowana Formation|43575|6|Mentioned|p276||Late Devonian|||||||
10693|Lowana Formation|47056|6|Mentioned|Fig.2 P523|||||||||
10693|Lowana Formation|68003|5|Briefly described|p32 Fig.3-h, p139. |Famennian|Late Devonian|Tamworth Belt (North), New England Fold Belt. Coeval with Mostyn Vale Formation and Noumea beds. Mis-spelt as Lowanna Formation on p32.||Unit in Parry Group.||Is overlain by Keepit Conglomerate.|Green-black, thinly-bedded siltstone and mudstone with thin white tuffaceous beds.|
10693|Lowana Formation|68005|5|Briefly described|p49 Fig.3-M, p54, p170.|Late Devonian|Late Devonian|Tamworth Belt. Mis-spelt as Lowanna Formation on p.54 and p149.||Basal unit in Parry Group.||Overlies Yarrimie Formation. Is overlain by Eungai Mudstone.|Green-black, thinly-bedded siltstone and mudstone with thin white tuffaceous beds.|
10819|Lowlands Formation|35098|4|Described|p5|||||||||
10819|Lowlands Formation|41391|6|Mentioned|p49|||||||||
10819|Lowlands Formation|42925|2|Defined|p49||Pleistocene|||||||
10819|Lowlands Formation|42926|4|Described|map legend|Holocene|Pleistocene|||||||
10819|Lowlands Formation|65195|6|Mentioned|p4, p7, p9, p11, p22, p24, p26|Quarternary|Quarternary|Overlies Cranebrook Formation||||||
10819|Lowlands Formation|73248|6|Mentioned|App. p3|Pleistocene|Pliocene?||||||Fluvial deposit.|
10824|Lowther Creek Granite|42726|5|Briefly described|map legend|Carboniferous||25.||||||
10825|Loxton Sand|2967|6|Mentioned|p35, 44|||See also references to Loxton Sands (p43, 45, 49). South Australia.|||||Marine.|
10825|Loxton Sand|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Early Pliocene|Misspelt - see Loxton Sands. Geological Province: Murray Basin.||||||13-AUG-07
10825|Loxton Sand|22773|5|Briefly described|Fig24.8p352,354||Pliocene|||||||
10825|Loxton Sand|22857|5|Briefly described|p339, p352 Fig. 24.8, p354|Late Pliocene|Late Pliocene|Marine sands. Heavy mineral sands containing rutile, zircon and ilmenite. Geological Province: Murray Basin.||||||
10825|Loxton Sand|23226|6|Mentioned|p901|||May overlap Pata Formation depending upon geographic location.  Of Murray Basin.||||||
10825|Loxton Sand|23482|5|Briefly described|p9|Tertiary|Tertiary|||||||
10825|Loxton Sand|23731|6|Mentioned|p29|Tertiary|Tertiary|||||||
10825|Loxton Sand|30928|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
10825|Loxton Sand|32862|5|Briefly described|Table 3|||Lower Pliocene||||||
10825|Loxton Sand|33725|6|Mentioned|p9|||Small sinkholes.||||||
10825|Loxton Sand|33826|6|Mentioned|p42|||Strat. table||||||
10825|Loxton Sand|34418|6|Mentioned|p506|||Missing in Canopus Bore.||||||
10825|Loxton Sand|34757|6|Mentioned|p49|||||||||
10825|Loxton Sand|35071|6|Mentioned|Table 1|||||||||
10825|Loxton Sand|35174|6|Mentioned|p167|||||||||
10825|Loxton Sand|39322|6|Mentioned|Fig.3|||||||||
10825|Loxton Sand|40230|6|Mentioned|p6|||||||||
10825|Loxton Sand|41511|5|Briefly described|p19|||See also p20.||||||
10825|Loxton Sand|41537|6|Mentioned|Fig.2|||||||||
10825|Loxton Sand|41599|6|Mentioned|p192|||||||||
10825|Loxton Sand|42115|6|Mentioned|p7|||||||||
10825|Loxton Sand|42125|5|Briefly described|p137|||See also Fig.5||||||
10825|Loxton Sand|42126|6|Mentioned|p150|||||||||
10825|Loxton Sand|42127|5|Briefly described|p222|||||||||
10825|Loxton Sand|42130|6|Mentioned|Fig.3 P265|||||||||
10825|Loxton Sand|42132|6|Mentioned|Fig.5 P298|||||||||
10825|Loxton Sand|42134|4|Described|p339|||||||||
10825|Loxton Sand|42137|6|Mentioned|p370|||||||||
10825|Loxton Sand|42138|6|Mentioned|p392|||||||||
10825|Loxton Sand|43053|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal, siliceous and clayey sand.||||||25-MAY-05
10825|Loxton Sand|43073|4|Described|p12,Table 3|||||||||
10825|Loxton Sand|43195|5|Briefly described|Map Legend||Early Pliocene|see also commentary on back of map.||||||
10825|Loxton Sand|43258|5|Briefly described|Map Legend||Pliocene|||||||
10825|Loxton Sand|43298|6|Mentioned|Map Legend||Pliocene|||||||
10825|Loxton Sand|43655|5|Briefly described|p40-846|||||||||
10825|Loxton Sand|44133|5|Briefly described|p161|Late Pliocene|Early Pliocene|Geological Province: Murray Basin. Overlies: Bookpurnong Formation conformably. See also Loxton Sands.||||||27-OCT-08
10825|Loxton Sand|49040|6|Mentioned|p12|||||||||
10825|Loxton Sand|60452|6|Mentioned|p37|Cenozoic|Cenozoic|Of Ludbrook (1957, 1961). Upper part then named Parilla Sand (Firman, 1965). Also called Diapur Sand in SA (Lawrence, 1966). Now refered to as Loxton-Parilla Sand to describe the unit across Victoria and South Australia.||||||19-NOV-08
10825|Loxton Sand|60540|5|Briefly described|p999,p1000 Fig.2,p1001, p1002 Fig.4, |Early Pliocene|Early Pliocene|Rogers et al. (1995). Shown as Loxton Sands in Firman (1972).||||Conformably overlies the Bookpurnong Formation. Partly correlative with Norwest Bend Formation in W Murray Basin.|Fluvial channel sands and contemporaneous shingled, regressive shoreline deposits and marine sediments.|06-FEB-18
10825|Loxton Sand|60785|5|Briefly described|p184 Fig.1, p196.  |Zanclean|Zanclean|South Australia. Has yielded fossil cetacean elements.|||||Poorly-sorted coarse sand containing pebbles.|
10825|Loxton Sand|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Marine to marginal marine.||||||
10825|Loxton Sand|61108|5|Briefly described|map legend|Pliocene|Pliocene|Arcuate ridges, partly inherited from coastal ridges in underlying marine to marginal marine Loxton Sand (not exposed).||||||
10825|Loxton Sand|61964|6|Mentioned|p139|||Regional correlative is Calivil Sand (Renmark Group). Geological Province: Murray Basin.||||||
10825|Loxton Sand|63124|6|Mentioned|p94||Pliocene|Geological Province: Gambier Basin.||||||
10825|Loxton Sand|64237|5|Briefly described|p18 Fig. 2, p19 Fig. 2b|Late Pliocene|Late Miocene|Included in the original stratigraphic scheme for the Murray Group and over- and underlying units of Lawrence (1961) and over/under-lying units of Lawrence (1961).||||||13-AUG-15
10825|Loxton Sand|64961|5|Briefly described|p269 Fig. 9|||Of Ludbrook (1961), Firman (1973)Pufahl et al (2004). Superseded by Loxton-Parilla Sand.||||||
10825|Loxton Sand|65715|5|Briefly described|p12, p15 Tb.8|Neogene|Neogene|Of Wunghnu Group. Senior synonym of Diapur Sandstone, Loxton-Parilla Sands and Parilla Sand in Victoria.||||||
10825|Loxton Sand|66002|5|Briefly described|p13 Tb.9, p18|Neogene|Neogene|Of Wunghnu Group. Defined by Ludbrook 1957. Marine. Difficult to distinguish from overlying aeolian Parilla Sand. Senior synonym of Diapur Sandstone and Dorodong Sands.||||||
10825|Loxton Sand|67179|4|Described|p579-85, p580 Fig.1b, p583 Fig.3, Fig.4|Early Pliocene|Late Miocene|Proposes to redefine Loxton Sand to incorporate all of the Loxton-Parilla Sands and the Parilla Sand(s). Diachronous ~10-7.2 Ma. Regressive arcuate strandplain sequence, 350km across, 600 strand-line ridges; due to marine regression in the Murray Basin. Previously the Loxton-Parilla Sands and Parilla Sands in VIC. Loxton Sand previously used for marine strata, but often not possible to separate from dune sands, so unit revised herein. Contains mineral sand deposits. Gamma spikes in downhole logs (due to monazite) show offsets (faulting) indicating Neogene tectonism. Depositional lithofacies: backshore dune, shoaling, breaker, surf and swash zones.|7.2 Ma (Sr isotope age of underlying sediments)||Divided into Kerang Sand Member, Tragowel Member, Wandella Sandstone Member in Kerang region.|Underlies the Shepparton Formation in east and Blanchetown Clay in NW, overlies the Bookpurnong Beds and the Renmark Group, interfingers with the Calivil Formation.|Incorporates shallow marine, beach dune, estuarine and fluvial sediments.|10-MAY-16
10825|Loxton Sand|67462|5|Briefly described|Map legend.|||Murray Basin.||||||
10825|Loxton Sand|68116|5|Briefly described|Maps 1-11, 14-17, 21-24, 29-30, 38-39.|Zanclean|Messinian|Also occurs in the Appendix.|||||Quartz sandstone: well sorted, fine to medium grained; well bedded; abundant lag horizons containing shelly fossils, pebble beds, rounded ironstone fragments; some heavy mineral concentrations; dissected or remobilised strand lines.|
10825|Loxton Sand|68194|6|Mentioned|p23|||SA name for Parilla Sand.||||||
10825|Loxton Sand|68548|5|Briefly described|p13|Pliocene|Pliocene|Early Pliocene age.||||Overlies Bookpurnong Formation. Grades into the Norwest Bend Formation to the west.|Comprises fluvial channel deposits and contemporaneous shallow marine sediments.|
10825|Loxton Sand|68715|6|Mentioned|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||||||
10825|Loxton Sand|68716|5|Briefly described|p39-45|||Regionally extensive, unconfined or semi-confined aquifer. A source of lateral flow, saline groundwater discharges to the Murray River: c.one-half of the salt load entering in the Loxton reach.||||Overlain by the Blanchetown Clay. Underlain by the Bookpurnong Formation.||07-APR-17
10825|Loxton Sand|70718|4|Described|p24, p25, p28, p90-91, p104, p129|Pliocene|Late Miocene|Murray Basin. Formed in a marine to coastal environment and features aeolian, fluvial and lagoonal elements. Hosts economic heavy minerals in placer deposits that formed as a barrier system. Economic minerals include rutile, zircon, monazite, ilmenite and leucoxene. Deposition is linked to reactivated faults. Formerly the Loxton-Parilla Sands. From stratigraphic drill holes a thickness of 20-60m is interpreted a maximum thickness of 150m is interpreted from geophysics.||Wunghnu Group||Conformably overlies Bookpurnong beds. Disconformably overlies Renmark Group. Disconformably overlain by Blanchetown Clay. Overlain by Norwest Bend Formation. Interbedded with Calivil Formation.|High carbonate, yellow-brown, fine- to coarse-grained well-sorted sand; usually contains less than 15% clay with some pyrite.|02-JUN-19
10825|Loxton Sand|71593|4|Described|p53-p56, p60|Pliocene|Miocene|This unit is generally between 10-30m thick. Deposited in a high energy beach environment. Hosts heavy minerals. See also  p138-p139, p197-p198.||||Overlies the Bookpurnong Formation. Overlain by the Shepparton Formation. Equivalent to the Brighton Group.|Pebbly quartz sand that has been locally ferruginised.|
10825|Loxton Sand|72445|5|Briefly described|App.1, App.2; App 7 p7 Fig.4.|Pliocene|Pliocene|Shown as Loxton Sands in App.7. App.2 is a .csv format file. Identified in Stavely 01, 04, 05, 06, 08, 09, 10, 11, 14, 16. Variations to description in each hole. Locally gravelly Stavely 08, 09. Micaceous sand in Stavely 14.||Wunghnu Group.||Underlies Newer Volcanic Group, unconform.; Woorinen, Shepparton Fms, sharply. Overlies Olney Fm, gradational; Port Campbell Lst, Bookpurnong Fm, Geera Clay, sharply; Calivil Fm, sharply/gradational.|Silty sand to silty mud. Dominantly fine sand in Stavely01. Fine sand, locally muddy in Stavely02. Includes whitish yellow fine to coarse sand and mud. Some ferruginous concretions and organic staining in Stavely05. Includes silty and muddy sand.|
10825|Loxton Sand|73188|6|Mentioned|p320|Pliocene|Pliocene|Murray Basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
10825|Loxton Sand|73228|4|Described|p50-53, p55-60, p62|Early Pliocene|Late Miocene|Murray Basin. Shallow marine, beach dune, estuarine and fluvial sediments. Identified in Cooltong 1, Berri North 1, Nadda 1, and Loxton 1 drillholes. Interpreted as prograding beach strandplains and barrier islands. The beach sand contains [economic deposits of] heavy minerals, including ilmenite, zircon, rutile and tourmaline.||||Conformably underlain by and possible equivalent to Bookpurnong Formation. Underlain by Parilla Sand. Overlain by Blanchetown Clay and Molineaux Sand.|Glauconitic, micaceous and shelly fine sand, overlain by planar and cross-bedded fine to coarse-grained sand and fine gravel, and planar bedded, calcareous, micaceous, medium- to coarse-grained sandstone with abundant shell debris.|
10825|Loxton Sand|73229|5|Briefly described|p66-67, p70, p72, p74|Early Pliocene|Late Miocene|Murray Basin. [Analysed using pXRF; see article]. Shallow marine, beach, aeolian, lacustrine and fluvial.|||||Includes sand, glauconitic, micaceous, and shelly gravel; coarse-grained sand and fine gravel, and calcareous micaceous, medium- to coarse-grained sandstone.|
10825|Loxton Sand|73253|6|Mentioned|p13-14, p16|Late Miocene|Late Miocene|Murray Basin. Includes heavy mineral deposits. Preserved as paleostrandlines. Samples collected for heavy mineral provenance; interpreted to represent fluvial inputs from as far as Queensland but dominantly from the southeast via the ancestral Murray River (dominantly) and Darling River.||||||
10831|Loyola Limestone|23309|5|Briefly described|p154|||||||||
10831|Loyola Limestone|30245|6|Mentioned|p77|||Refers Talent(1965),Bell(1955)||||||
10831|Loyola Limestone|31331|6|Mentioned|p182|||See also P189||||||
10831|Loyola Limestone|31502|6|Mentioned|p95|||Devonian||||||
10831|Loyola Limestone|32074|5|Briefly described|p180|||||||||
10831|Loyola Limestone|32984|6|Mentioned|p344|||Fossil content||||||
10831|Loyola Limestone|33326|6|Mentioned|p435|||Fauna.||||||
10831|Loyola Limestone|33408|6|Mentioned|p231|||||||||
10831|Loyola Limestone|34251|6|Mentioned|p539|||See also PP540, 543||||||
10831|Loyola Limestone|38787|6|Mentioned|p143|||||||||
10831|Loyola Limestone|41555|6|Mentioned|p412|||||||||
10831|Loyola Limestone|42033|6|Mentioned|p649|||||||||
10831|Loyola Limestone|42383|6|Mentioned|p5|||Superseded by Walhalla Group? Used 1983.||||||
10831|Loyola Limestone|42827|6|Mentioned|p121|||||||||
10831|Loyola Limestone|43461|14|Not recorded|p627|Emsian|Siegenian|U.Siegenian-L.Emsian||||||
10831|Loyola Limestone|43525|14|Not recorded|p130,Table p131|||Equivalent to Coopers Creek Formation||||||
10831|Loyola Limestone|43529|14|Not recorded|p233||Siegenian|Early Siegenian||||||
10831|Loyola Limestone|43531|14|Not recorded|p796|||Ref.to Ripper 1937||||||
10831|Loyola Limestone|43533|14|Not recorded|p109,125,130|||Near Mansfield. L.Devonian fossils.||||||
10831|Loyola Limestone|43537|14|Not recorded|p7,22,24,29|||Devonian fossils from Loyola. Late Gedinnian or Siegenian||||||
10831|Loyola Limestone|48926|6|Mentioned|p32|||P41 et seq.||||||
10831|Loyola Limestone|63118|6|Mentioned|p203, p205|Early Devonian|Early Devonian|||||||
10831|Loyola Limestone|64616|5|Briefly described|p280|Devonian|Devonian|Near Howes Inlet, six olistoliths of pale crystalline crinoidal limestone cropped out. Most was quarried and burned for high-quality lime.||||||
10831|Loyola Limestone|70933|6|Mentioned|p94|||||||||
10831|Loyola Limestone|71924|6|Mentioned|p2|Pragian||Dated by conodonts. Includes Nadiastrophia.||||||
10831|Loyola Limestone|73143|6|Mentioned|p17|Pragian|Pragian|Contains ""Cystiphyllum"" sp. rugose coral (Hill, 1939).||||||
10842|Lucernia Coal|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Horseshoe Creek Subgroup.  Geological Province: Sydney Basin||||||17-OCT-12
10842|Lucernia Coal|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Horseshoe Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
10842|Lucernia Coal|29942|3|Fully described|p11|||||||||
10842|Lucernia Coal|37094|6|Mentioned|p243|||||||||
10842|Lucernia Coal|68004|5|Briefly described|p51 Table 5, p53.|Late Permian|Late Permian|Upper Hunter Coalfield.||Uppermost unit in Horseshoe Creek Sub-group.|Includes Carramere, Rombo and Eyriebower Coal Members; Hillsdale Claystone and Longford Creek Siltstone.|Overlies Strathmore Formation. Is overlain by Pinegrove Formation.|A rich coal-bearing sequence comprising distinctive phases of coal and tuffaceous sandstone.|
10849|Lucyvale Granite|22508|5|Briefly described|p2||Silurian|Koetong Supersuite, Lachlan Fold Belt||||||10-JUN-14
10849|Lucyvale Granite|23309|5|Briefly described|p344|||G575 - A-Type||||||
10849|Lucyvale Granite|24133|3|Fully described|p80||Ordovician|Geological Province: Lachlan Fold Belt.||||||
10849|Lucyvale Granite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
10849|Lucyvale Granite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
10849|Lucyvale Granite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
10849|Lucyvale Granite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
10849|Lucyvale Granite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
10849|Lucyvale Granite|42726|5|Briefly described|map legend|Silurian||Wagga Batholith. 552. Marked on map as two separate bodies (One in Vic. and the other in NSW)||||||
10849|Lucyvale Granite|68116|5|Briefly described|Appendix, Map 20.|Early Devonian|Early Devonian||||||Biotite leucogranite: deep pink, variably fine to coarse grained; contains greenish brown biotite pervasively altered; highly magnetic.|
10866|Lumley Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Lumley Adamellite.||||||
10866|Lumley Granite|50234|5|Briefly described|Map Legend|Pragian|Emsian|Part of the Marulan Batholith.||||||17-OCT-12
10866|Lumley Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Grey, medium- to coarse-grained, equigranular to weakly porphyritic, biotite granite with rare hornblende.||||||
10866|Lumley Granite|68592|2|Defined|p241, p261, p1611, p1630-3|Early Devonian|Early Devonian|Carr et al. (1979). The margins of the unit are slightly revised here; its distribution, including an apophysis within the Springponds Tonalite, is described. Type locality described. Forms low relief landscape with outcrops of small tors and low boulders, but mainly covered by alluvium. Geochemistry and geophysical properties briefly described. Post-dates Bogungra Dacite Member, and Barrallier Ignimbrite with which it is regarded as being broadly comagmatic. Is in contact with Torwood Granodiorite and Springponds Tonalite, but their relative age relationships are unknown.|393 +/- 7 Ma (K-Ar; Carr, Jones and Wright,1980).|Unit in Arthursleigh Suite.||Intrudes Bindook Group. Is overlain unconformably by Lambie Group.|Uniform internal composition. Medium-grained, massive, equigranular to weakly porphyritic, leucocratic granite. I-type.|
10866|Lumley Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dal. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Grey, medium - coarse-grained, equigranular to weakly porphyritic biotite granite with rare hornblende. Low to high K, low to medium Th and U response. High magnetic susceptibility.|
10866|Lumley Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Grey, medium - coarse-grained, equigranular to weakly porphyritic biotite granite with rare hornblende. Low to high K, low to medium Th and U response. High magnetic susceptibility.|
10907|Ma Ma Creek Member|13516|5|Briefly described|p159 fig 8|Early Jurassic|Early Jurassic|From Clarence-Moreton Basin.||Koukandowie Formation||||
10907|Ma Ma Creek Member|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Interbedded sandstone, mudstone. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|22865|6|Mentioned|Fig.22.10ap318|||||||||
10907|Ma Ma Creek Member|23799|5|Briefly described|p48 Fig. 3|Toarcian|Pliensbachian|Probably supersedes Ma Ma Creek Sandstone Member. Of the Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||27-AUG-08
10907|Ma Ma Creek Member|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Koukandowie Formation.  Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Early Jurassic|Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|41591|5|Briefly described|p21|||||||||
10907|Ma Ma Creek Member|41631|4|Described|p19|||See also Fig.2||||||
10907|Ma Ma Creek Member|42248|2|Defined|App.1 P411|Early Jurassic||Definition card approved by NSW. Distribution includes NSW.||||||
10907|Ma Ma Creek Member|42463|6|Mentioned|Fig.3 P170|||||||||
10907|Ma Ma Creek Member|42869|5|Briefly described|p32|||Of Koukandowie Formation.||||||27-AUG-08
10907|Ma Ma Creek Member|42951|5|Briefly described|Fig.11|||of Koukandowie Formation||||||
10907|Ma Ma Creek Member|43736|6|Mentioned|p29|||||||||
10907|Ma Ma Creek Member|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
10907|Ma Ma Creek Member|60281|5|Briefly described|p30, Fig.18 App.1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation.  Interbedded sandstone, mudstone.  Max. thickness: 50m.  Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60993|5|Briefly described|p6 Fig. 2, p27|||Supersedes Ma Ma Creek Sandstone Member. Of the Koukandowie Formation. Predominantly siltstone and shale; contains an isochronous ferruginous oolite marker bed. Geol. Prov: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60995|4|Described|p67, p51 Fig. 3|Early Jurassic|Early Jurassic|Base of the Koukandowie Formation. Thinly interbedded sandstone, claystone and mudstone. Overlain by Heifer Creek Sandstone Member.  Max. thickness: 50m. Geol. Prov: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60996|5|Briefly described|p72|||Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60997|5|Briefly described|p139 Fig. 1|Toarcian|Toarcian|Of the Koukandowie Formation. Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
10907|Ma Ma Creek Member|60998|5|Briefly described|p146 Fig. 2|||Of the Koukandowie Formation. Consists of upward-coarsening sequences and contains two ferruginous oolite marker beds. Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|60999|5|Briefly described|p174|Early Jurassic|Early Jurassic|Basal oolitic unit of Koukandowie Formation. See also Ma-Ma Creek Member.||||||
10907|Ma Ma Creek Member|61004|5|Briefly described|p232 Fig. 2|Jurassic|Jurassic|Of the Koukandowie Formation (Marburg Subgroup). Geological Province: Clarence-Moreton Basin.||||||
10907|Ma Ma Creek Member|61006|5|Briefly described|p286|Jurassic|Jurassic|Of the Koukandowie Formation. Potential hydrocarbon seal.||||||
10907|Ma Ma Creek Member|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Early Jurassic|Of the Koukandowie Sandstone. Silty quartz lithic sandstone, claystone, siltstone, chamositic oolite (Qld.). Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. See also p24.||||||
10907|Ma Ma Creek Member|64289|5|Briefly described|p6 Fig. 2|Early Jurassic|Early Jurassic|Of the Koukandowie Formation (Marburg Subgroup, Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
10907|Ma Ma Creek Member|64665|5|Briefly described|p53 Fig.2.|Early Jurassic|Early Jurassic|Clarence-Moreton Basin. Correlates with Evergreen Formation (Surat Basin) and Brighton beds (Southern Nambour Basin).||Lower unit in Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|67402|5|Briefly described|p187, p188, p190, p190 fig CLM6, p193|Pliensbachian|Sinemurian|Clarence-Moreton Basin. Represents a change in depositional environment from sandy braided streams to a floodplain environment includingextensive lake and swamp deposits.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|69297|5|Briefly described|p487 fig 5.38, p490|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 10-50m thick. Deposited as overbank or flood plain facies as part of a mixed fluvial or lacustrine system. Potential hydrocarbon seal unit.||Koukandowie Formation||Overlies the Towallum Basalt. Overlain by the Heifer Creek Sandstone Member.|Interbedded sandstones and mudstones.|
10907|Ma Ma Creek Member|69594|5|Briefly described|p519, p536 Fig.7.17, p544-546, p572|Toarcian|Toarcian|Northern Clarence-Moreton Basin. Has poor outcrop. The ferruginous oolite marker bed is equivalent to the Westgrove Ironstone Member of the Evergreen Formation, and ironstone marker beds in the Brighton beds and Tiaro Coal Measures.||Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member. Age-equivalent of Brighton beds, Tiaro Coal Measures and Westgrove Ironstone Member.|Includes a ferruginous oolite marker bed.|
10907|Ma Ma Creek Member|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Koukandowie Formation.||||
10907|Ma Ma Creek Member|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Koukandowie Formation.||Overlies Gatton Sandstone. Is overlain by Heifer Creek Sandstone Member.||
10907|Ma Ma Creek Member|71805|5|Briefly described|p76|Toarcian|Pleinsbachian|Clarence-Moreton Basin.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Heifer Creek Sandstone Member.||
10928|MacPherson Volcanics|35045|6|Mentioned|p110|||||||||
10928|MacPherson Volcanics|35050|6|Mentioned|p130|||||||||
10928|MacPherson Volcanics|43881|2|Defined|p6-7,49,53-66,154,||Tertiary|Includes Blue Knob Basalt,Nimbin Rhyolite,basal Lismore Basalt.Probably Eocene-Oligocene. Map 9.||||||
10952|Mackunda Formation|12597|5|Briefly described|p492 Tb.1, p500|Cenomanian|Cenomanian|Eromanga Basin. 60m thick.|||||Marginal marine sequence; labile sandstone, siltstone and mudstone, calcareous in part, containing bivalves, ammonites, belemnites, polyzoans and sharks' teeth.|
10952|Mackunda Formation|13497|5|Briefly described|p115 fig 6.33, p146, p149-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin. Mis-spelt as the Macunda Formation on p146.||Marree Subgroup||Overlies the Allaru Mudstone and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
10952|Mackunda Formation|22857|5|Briefly described|p296-7 Tb.22.1|Cenomanian|Albian|Of the Rolling Downs Group. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|22865|5|Briefly described|Table22.1p296-7|Cenomanian|Albian|||||||
10952|Mackunda Formation|22883|5|Briefly described|Fig2 P30||Late Cretaceous|Overlying unit is Winton Formation, underlying unit is Allura Mudstone||||||
10952|Mackunda Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
10952|Mackunda Formation|23056|6|Mentioned|12 table 2|||||||||
10952|Mackunda Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||20-FEB-07
10952|Mackunda Formation|23155|4|Described|p33|Early Cretaceous|Early Cretaceous|Determination of the spore-pollen assemblage indicate an Early Cretaceous (Albian) age. The unit conformably overlies both the Allaru Mudstone and Oodnadatta Formation on STRZELECKI.||||||11-NOV-13
10952|Mackunda Formation|23183|6|Mentioned|p223||Albian|||||||
10952|Mackunda Formation|23188|6|Mentioned|p283,287||Albian|||||||
10952|Mackunda Formation|23375|4|Described|Fig2 p265|Cenomanian|Albian|In the Eromanga Basin.||||||31-OCT-06
10952|Mackunda Formation|23425|5|Briefly described|Plate 10.2|||In the Eromanga Basin Province.||||||20-FEB-07
10952|Mackunda Formation|23430|4|Described|p524 Table 14.7|||Eromanga Basin Province. Maximum thickness <275 m.||||||
10952|Mackunda Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Manuka Sub-Group.||||||
10952|Mackunda Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Australian Superbasin.||||||
10952|Mackunda Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
10952|Mackunda Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
10952|Mackunda Formation|24175|3|Fully described|p28, p17 Fig. 3|Cenomanian|Albian|Overlain by Winton Formation; overlies Allaru Mudstone. Max. thickness: 57m. Geological Province: Eromanga Basin.||||||11-NOV-13
10952|Mackunda Formation|24204|5|Briefly described|p263 Fig.4, p267|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Underlain by Allaru Formation. Geological Province: Eromanga Basin||||||20-FEB-07
10952|Mackunda Formation|24321|5|Briefly described|Map legend|Cenomanian|Albian|Of the Neales River Group.||||||31-OCT-06
10952|Mackunda Formation|29591|6|Mentioned|p71|||||||||
10952|Mackunda Formation|30019|6|Mentioned|p2|||Upper Albian||||||
10952|Mackunda Formation|30020|6|Mentioned|p35|||||||||
10952|Mackunda Formation|30103|5|Briefly described|p9|||Unit of Rolling Downs Group. Table 3 on p9.||||||31-OCT-06
10952|Mackunda Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|30691|4|Described|p17|||See also p22,Table 4,6. Lower-Upper Cretaceous.||||||31-OCT-06
10952|Mackunda Formation|30804|6|Mentioned|p10|||||||||
10952|Mackunda Formation|30853|5|Briefly described|Table 3|||Albian age||||||
10952|Mackunda Formation|30854|4|Described|Table 4|||Albian||||||
10952|Mackunda Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Rolling Downs Group||||||
10952|Mackunda Formation|30856|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31098|6|Mentioned|p10|||||||||
10952|Mackunda Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31145|5|Briefly described|Table 1|||Lower Cretaceous||||||
10952|Mackunda Formation|31208|6|Mentioned|Fig. 7|||||||||
10952|Mackunda Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31431|5|Briefly described|Table 3|||Lower Cretaceous.||||||
10952|Mackunda Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
10952|Mackunda Formation|31434|6|Mentioned|p8|||||||||
10952|Mackunda Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|31572|4|Described|Fig. 1|||L.Cretaceous||||||
10952|Mackunda Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
10952|Mackunda Formation|32314|6|Mentioned|Fig. 4|||||||||
10952|Mackunda Formation|32395|6|Mentioned|p7|||Correlation||||||
10952|Mackunda Formation|32396|6|Mentioned|p9|||Correlated with Normanton Fm.||||||
10952|Mackunda Formation|32553|4|Described|p38|||||||||
10952|Mackunda Formation|32796|6|Mentioned|p303|||||||||
10952|Mackunda Formation|33016|6|Mentioned|p1|||Table on P1||||||
10952|Mackunda Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
10952|Mackunda Formation|33069|4|Described|p7|||L.-U.Cret.||||||
10952|Mackunda Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33075|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
10952|Mackunda Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||20-FEB-07
10952|Mackunda Formation|33089|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
10952|Mackunda Formation|33176|6|Mentioned|p171|||||||||
10952|Mackunda Formation|33182|6|Mentioned|p200|||L.Cret. See also Table 1||||||
10952|Mackunda Formation|33368|6|Mentioned|p25|||Strat.table.||||||
10952|Mackunda Formation|33372|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|33414|6|Mentioned|p211|||||||||
10952|Mackunda Formation|33561|6|Mentioned|p102|||||||||
10952|Mackunda Formation|33638|5|Briefly described|Table 1|||||||||
10952|Mackunda Formation|33639|5|Briefly described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33640|4|Described|Table 2|||L.Cret.||||||
10952|Mackunda Formation|33642|6|Mentioned|p144-5,147-8,Tb.1,|||Refers Vine & Day (1965). Figs. 1 & 2.||||||
10952|Mackunda Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
10952|Mackunda Formation|33825|6|Mentioned|p10|||Correlation table||||||
10952|Mackunda Formation|33832|5|Briefly described|p11|||Stratigraphy and correlation.||||||31-OCT-06
10952|Mackunda Formation|33964|4|Described|p6|||||||||
10952|Mackunda Formation|34065|4|Described|p6|||L.Cret.||||||
10952|Mackunda Formation|34091|5|Briefly described|Table 1|||L.Cret||||||
10952|Mackunda Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34218|4|Described|Table 1|||Lower Cretaceous. See also Table 2.||||||
10952|Mackunda Formation|34356|6|Mentioned|p21|||Albian.||||||
10952|Mackunda Formation|34485|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34486|4|Described|Table 1|||Lower - Upper Cretaceous||||||
10952|Mackunda Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|34611|6|Mentioned|Fig.65|||Correlation chart||||||
10952|Mackunda Formation|34619|3|Fully described|p.160. Pl.22||Adelaidean|||||||
10952|Mackunda Formation|35139|4|Described|Table.2|||||||||
10952|Mackunda Formation|35239|6|Mentioned|Fig.4|||||||||
10952|Mackunda Formation|35560|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35793|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|35811|5|Briefly described|Table 3|||||||||
10952|Mackunda Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
10952|Mackunda Formation|36229|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
10952|Mackunda Formation|36243|6|Mentioned|Table 6A|||||||||
10952|Mackunda Formation|36552|6|Mentioned|Fig.25|||||||||
10952|Mackunda Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
10952|Mackunda Formation|37263|6|Mentioned|p319|||||||||
10952|Mackunda Formation|37451|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|37608|3|Fully described|Table 1|||||||||
10952|Mackunda Formation|38226|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|38373|6|Mentioned|p621|||||||||
10952|Mackunda Formation|38779|6|Mentioned|p4|||||||||
10952|Mackunda Formation|38814|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39070|4|Described|p366|||||||||
10952|Mackunda Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,11,13 etc. Correlation||||||
10952|Mackunda Formation|39445|5|Briefly described|Table 11|||||||||
10952|Mackunda Formation|39478|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|39846|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|39847|5|Briefly described|p40|||||||||
10952|Mackunda Formation|39943|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40121|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|40199|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40220|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40249|6|Mentioned|p41|||||||||
10952|Mackunda Formation|40675|6|Mentioned|Table 8A|||||||||
10952|Mackunda Formation|40681|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|40687|3|Fully described|p419|||||||||
10952|Mackunda Formation|40801|6|Mentioned|p42|||||||||
10952|Mackunda Formation|40910|6|Mentioned|p17|||||||||
10952|Mackunda Formation|40926|6|Mentioned|p19|||||||||
10952|Mackunda Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
10952|Mackunda Formation|41062|6|Mentioned|Fig.5|||||||||
10952|Mackunda Formation|41063|6|Mentioned|p40|||||||||
10952|Mackunda Formation|41064|6|Mentioned|p62|||||||||
10952|Mackunda Formation|41084|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41085|6|Mentioned|p89|||||||||
10952|Mackunda Formation|41086|3|Fully described|p98, Fig.3|||||||||
10952|Mackunda Formation|41088|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41097|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41099|6|Mentioned|Fig.9|||||||||
10952|Mackunda Formation|41165|5|Briefly described|p363|||Mention Fig.15||||||
10952|Mackunda Formation|41176|6|Mentioned|Table 2|||||||||
10952|Mackunda Formation|41177|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41182|5|Briefly described|Fig.2|||||||||
10952|Mackunda Formation|41183|6|Mentioned|Fig.3 p308|||||||||
10952|Mackunda Formation|41187|6|Mentioned|Fig.2|||||||||
10952|Mackunda Formation|41198|6|Mentioned|Table 1|||||||||
10952|Mackunda Formation|41214|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41216|6|Mentioned|Fig.18|||||||||
10952|Mackunda Formation|41266|6|Mentioned|Fig.3|||||||||
10952|Mackunda Formation|41523|3|Fully described|p282|||See also p277.||||||31-OCT-06
10952|Mackunda Formation|41707|6|Mentioned|Fig.8|||||||||
10952|Mackunda Formation|41724|6|Mentioned|p383|||||||||
10952|Mackunda Formation|41950|5|Briefly described|Fig.2 P3|||||||||
10952|Mackunda Formation|42061|4|Described|Fig,11 P159|||||||||
10952|Mackunda Formation|42067|4|Described|Appendix 2|||See also Fig.2 p309.||||||31-OCT-06
10952|Mackunda Formation|42071|6|Mentioned|p117|||||||||
10952|Mackunda Formation|42084|6|Mentioned|Fig.3 P356|||||||||
10952|Mackunda Formation|42085|6|Mentioned|Fig.2 P374|||||||||
10952|Mackunda Formation|42395|5|Briefly described|Fig.13 P83|||||||||
10952|Mackunda Formation|42397|6|Mentioned|Fig.2 P3|||||||||
10952|Mackunda Formation|42429|6|Mentioned|Figs.6 & 9 P156|||||||||
10952|Mackunda Formation|42446|4|Described|p14|||||||||
10952|Mackunda Formation|42447|6|Mentioned|Fig. 1|||||||||
10952|Mackunda Formation|42477|5|Briefly described|p166|||||||||
10952|Mackunda Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
10952|Mackunda Formation|42520|5|Briefly described|p6|||||||||
10952|Mackunda Formation|42673|5|Briefly described|Fig.2, P184|||||||||
10952|Mackunda Formation|42746|5|Briefly described|p12|||See also Fig.6||||||
10952|Mackunda Formation|42749|6|Mentioned|Fig.2 P27|||||||||
10952|Mackunda Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
10952|Mackunda Formation|43002|5|Briefly described|Fig.2,p135|||||||||
10952|Mackunda Formation|43004|5|Briefly described|Table 1,p179|||||||||
10952|Mackunda Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone. Includes Mount Howie Sandstone.||||||25-MAY-05
10952|Mackunda Formation|43105|6|Mentioned|p15|||||||||
10952|Mackunda Formation|43114|5|Briefly described|p16|||||||||
10952|Mackunda Formation|43122|5|Briefly described|Fig.2.|||||||||
10952|Mackunda Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
10952|Mackunda Formation|43591|6|Mentioned|p40|||||||||
10952|Mackunda Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
10952|Mackunda Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44017|14|Not recorded|Map Legend|||||||||
10952|Mackunda Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44020|14|Not recorded|p10,Tb.1,2||Early Cretaceous|Of roling Dwons Grouop.||||||
10952|Mackunda Formation|44031|14|Not recorded|p3,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44033|14|Not recorded|map,p4,5,8,9||Cretaceous|||||||
10952|Mackunda Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
10952|Mackunda Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44067|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44082|6|Mentioned|p6,12,26,28,Tb.p34||Albian|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
10952|Mackunda Formation|44089|4|Described|Tb.1,p3,4,8,9,map||Early Cretaceous|||||||
10952|Mackunda Formation|44091|14|Not recorded|p60|||||||||
10952|Mackunda Formation|44133|4|Described|p122-123, 104 Fig. 9.11|Early Cenomanian|Late Albian|Geological Province: Eromanga Basin. Conformably overlies Oodnadatta Formation and Allaru Mudstone. Contains sediments from the now superseded Mount Alexander Sandstone Member and Blanchewater Formation.||||||
10952|Mackunda Formation|44361|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44362|4|Described|p12,Tb.1||Early Cretaceous|||||||
10952|Mackunda Formation|44374|14|Not recorded|p12||Cretaceous|early Late Albian sandstone,siltstone indicating shoaling of seas throughout Eromanga Basin.||||||
10952|Mackunda Formation|44376|14|Not recorded|p6|||||||||
10952|Mackunda Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44414|14|Not recorded|p110-112|||Sandstone, mudstone characterised by marine fossils overlain by Winton Formation.||||||
10952|Mackunda Formation|44417|2|Defined|p416,419-420|||Formerly called Mackunda Beds. Overlies Wilgunya Formation. Albian fossils. Unit of Rolling Downs Group.||||||31-OCT-06
10952|Mackunda Formation|44418|14|Not recorded|Map Legend||Early Cretaceous|||||||
10952|Mackunda Formation|44573|14|Not recorded|p98||Cretaceous|||||||
10952|Mackunda Formation|44807|14|Not recorded|unknown (p1-16)|||Allaru Mudstone, correlated with Normanton Formation.||||||
10952|Mackunda Formation|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965. Comparable to lower part of Blanchewater Formation in South Australia.||||||
10952|Mackunda Formation|44920|14|Not recorded|Map Legend,Sheet 4||Cretaceous|||||||
10952|Mackunda Formation|45052|5|Briefly described|p134|||Mesozoic||||||
10952|Mackunda Formation|45103|6|Mentioned|p8|||||||||
10952|Mackunda Formation|45110|6|Mentioned|p147|||See also Table 18.||||||
10952|Mackunda Formation|45168|6|Mentioned|p6|||||||||
10952|Mackunda Formation|46791|5|Briefly described|p48|||||||||
10952|Mackunda Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
10952|Mackunda Formation|48920|3|Fully described|p62|||||||||
10952|Mackunda Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
10952|Mackunda Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
10952|Mackunda Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Allaru Mudstone. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||
10952|Mackunda Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Allaru Mudstone and Oodnadatta Formation, with which it also interfingers laterally. Overlain by Winton Formation. Geological Province: Eromanga Basin.||||||31-JAN-08
10952|Mackunda Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marginal marine sandstone and siltstone.||||||
10952|Mackunda Formation|61312|5|Briefly described|p64, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Siltstone, sandstone, minor shale. Geological Province: Eromanga Basin (absent in NSW).||||||
10952|Mackunda Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
10952|Mackunda Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
10952|Mackunda Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
10952|Mackunda Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
10952|Mackunda Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
10952|Mackunda Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
10952|Mackunda Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta and Allaru Formations. Is overlain by Winton Formation.||
10952|Mackunda Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
10952|Mackunda Formation|63979|2|Defined|p53, Fig. 44|Cenomanian|Albian|Previously Mackunda Beds (Vine 1964). Of Manuka Subgroup (Rolling Downs Gp). Conformable on Allaru Mudstone. Conformable below Winton Fm. Max. thick: 150m. Interbedded sandstone, siltstone and mudstone and lesser mudclast intraformational conglomerate.||||||07-FEB-11
10952|Mackunda Formation|64048|6|Mentioned|p64 Tb. 2, p72|||Geological Province: Eromanga Basin.||||||07-FEB-11
10952|Mackunda Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Allaru Mudstone (Marree Subgroup); is overlain by Winton Formation.||10-DEC-15
10952|Mackunda Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
10952|Mackunda Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
10952|Mackunda Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Allaru Mudstone and Oodnadatta Formation. Overlain by Winton Formation.||||||08-MAR-12
10952|Mackunda Formation|65489|5|Briefly described|p49, p55, p58, p61, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 200m thick. Regional seal.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|65925|5|Briefly described|Appendix 2.||||||||Calcareous sandstone; siltstone; shale.|
10952|Mackunda Formation|66518|6|Mentioned|p19 Fig.4.|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||06-FEB-14
10952|Mackunda Formation|66529|6|Mentioned|p12 Fig.5, p16  |||||Unit in Rolling Downs Group.||Overlies Oodnadatta Formation and Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|66623|6|Mentioned|pp264-265.|||Partly equivalent to Allaru Mudstone in Koonenberry Belt, NSW.||||Overlies Allaru Mudstone.||
10952|Mackunda Formation|67323|5|Briefly described|p87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.|Feldspathic sandstone, siltstone.|
10952|Mackunda Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Albian|Eromanga Basin. Deposited in shallow marine or paralic environments. Maximum thickness of 100m. Estimated porosity of 10-25% with unknown permeability. See also p108, p109, p115 tbl ERO2.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.|Very fine to fine-grained sandstone, with laminations of siltstone and mudstone and lesser mud-clast intraformational conglomerate.|
10952|Mackunda Formation|67784|5|Briefly described|p25-26, p28-32|Albian|Albian|Northern Eromanga Basin. 90-275m thick.||||Overlies Allaru Formation, overlain by Winton Formation|Contains labeceratid ammonites.|08-FEB-18
10952|Mackunda Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Marginal marine to paralic; a marine regression. Fossiliferous: molluscs, forams, wood, diverse microflora, fish and vertebrates.||Unit in Neales River Group.||Conformably overlies Oodnadatta Formation. Is overlain conformably by Winton Formation.|Bimodal cross-bedded, yellow-brown fine to medium sand interbedded with greenish to grey silt and silty clay; then pale grey-green, interbedded, cross-bedded, glauconitic, sand-silt-shale and calcareous shales, mud and clay intraclasts common.|
10952|Mackunda Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Mackunda Formation as one unit.|||||Mudstone and siltstone.|
10952|Mackunda Formation|68206|6|Mentioned|p31-33|Albian|Albian|NE Eromanga Basin.||||Overlies Allaru Formation.||
10952|Mackunda Formation|68279|6|Mentioned|p18|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
10952|Mackunda Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.||
10952|Mackunda Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
10952|Mackunda Formation|68715|6|Mentioned|p30 Fig.7|Cenomanian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|68731|6|Mentioned|pp209-211|||||||||
10952|Mackunda Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Marine to coastal paralic. Mis-spelt as Mackundra Formation in Fig.2.||Of the Rolling Downs Group.||||16-JAN-17
10952|Mackunda Formation|68821|5|Briefly described|p292 Fig.1, p296|Cretaceous|Cretaceous|Lower Cretaceous age. Parallic to marine sediments.||Of the Rolling Downs Group.||||
10952|Mackunda Formation|69019|4|Described|p83 Fig.20, p85, p99-101.|Cenomanian|Albian|Of Vine and Day (1965). Eromanga Basin; final Cretaceous marine deposition. Thickness from 0-192 m. Has developed a porcellanite horizon.||Unit in Neales River Group.||Overlies Oodnadatta Formation conformably; overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt; shale and calcareous shale, often as intraclasts in upper sand beds. Contains ovoidal limestone concretions to tabular limestone bodies.|
10952|Mackunda Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93|Cenomanian|Albian|See also p105-106, p119, p122-123, p151, p191-192. Defined by Vine and Day (1965) in Queensland as the youngest marine to marginal marine unit within the Eromanga Basin. Thickness varies from <49 to ~82m. Marginal marine and paralic to deltaic. Diverse fauna listed. Weathering has formed porcellanite. Stratigraphic wells intersection data.||||Conformably overlies Oodnadatta Formation and Allaru Mudstone. Is overlain conformably by Winton Formation.|Pale grey-green, interbedded, glauconitic cross-bedded sand, silt, shale and calcareous shale. Local ferricrete capping.|
10952|Mackunda Formation|69457|4|Described|p41:2-3, 6-7, 10-12|Early Cretaceous|Early Cretaceous|Vine and Day (1965). Central and southern Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Thickness is variable, from 74m to >150m. Marine; distinguished by its lack of coal. Contains a diverse fossil assemblage, from a dinosaur to microfossils.||Manuka Subgroup.||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Thinly interbedded labile very fine- to fine-grained lithic sandstone, laminated siltstone and mudstone with numerous plant remains, and lesser mud-clast intraformational conglomerate.|12-JUL-16
10952|Mackunda Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|||Said to be a unit in Marree Subgroup.||||06-APR-22
10952|Mackunda Formation|69582|6|Mentioned|p65|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overrlain by the Winton Formation.||
10952|Mackunda Formation|69594|5|Briefly described|p519, p526, p530-531, p574|Cenomanian|Albian|Vine (1964); Vine and Day (1965). Eromanga Basin. Mostly 75-100+ metres thick. Boundaries in drill holes are distinguished by various geophysical properties (described). Shallow-marine and paralic deposits with abundant volcanilithic sediments from the E. Contains a distinct marine fauna (listed) including the "iconic" Muttaburrasaurus.||||Conformably overlies Allaru Mudstone. Is overlain conformably by Winton Formation.|Labile volcanic lithic-feldspathic interbedded sandstone, siltstone, mudstone and minor impure coquinitic and cone-in-cone limestone and intraformational conglomerate.|
10952|Mackunda Formation|69599|6|Mentioned|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by Moses Sandstone.||
10952|Mackunda Formation|69673|5|Briefly described|p155 fig 127|Cretaceous|Cretaceous|||Manuka Subgroup||Overlies Oodnadatta Formation, Allaru Mudstone, overlain by Winton Formation|Carbonaceous, pyritic shale with lesser interbedded sandstone.|
10952|Mackunda Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
10952|Mackunda Formation|69946|4|Described|p23, p26-28, p57, p94, p123|Late Cretaceous|Early Cretaceous|Vine and Day (1965). Type section is at the headwaters of Mackunda Creek on Gnalta Station. 60 - 120m thick. Wireline log correlations.||||Conformably overlies Allaru Mudstone and Oodnadatta Formation. Is overlain conformably by Winton Formation.|Interbedded, partly calcareous very fine-grained sandstone, siltstone and shale. Locally, transgressive mudstone units are interbedded with shoreface sandstones.|
10952|Mackunda Formation|69947|6|Mentioned|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marginal marine deposits.||||||
10952|Mackunda Formation|70821|5|Briefly described|p21, p33, p79-80|Late Cretaceous|Late Cretaceous|Eromanga Basin. Absent in the southern Thomson region. 30.5m thick in Mirintu 1 petroleum well. Hydrochemistry mentioned.||Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain by Winton Formation.||
10952|Mackunda Formation|70823|5|Briefly described|p25-p27, p41, p43-p44,p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Age is minimum depositional age. Up to 200m thick.|c. 101 Ma|||Overlies the Allaru Formation and the Oodnadatta Formation. Overlain by the Winton Formation.||
10952|Mackunda Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|70836|6|Mentioned|p474|Albian|Albian|Eromanga Basin.||||||
10952|Mackunda Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
10952|Mackunda Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlain by Winton Formation. Underlain by Mount Alexander Sandstone Member or Allaru Mudstone.||
10952|Mackunda Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch4 p25,|Cenomanian|Albian|Eromanga Basin. Defined by Vine and Day (1965) who nominated the type section at the headwaters of Mackunda Creek on Gnalta Station. Hosts a major confined aquifer. Up to 120m thick. Dated on the basis of palynology and rare macrofossils.Sedimentology and palaeoenvironment are discussed. Spore-pollen zone is given in Ch5 p57.  See also Ch5 p23, Ch5 p26-p28, Ch5 p33, Ch5 p57, Ch5 p125, Ch6 p8, Ch6 p10, Ch7 p13.||||Conformably overlies the Allaru Mudstone and the Oodnadatta Formation. Conformably overlain by the Winton Formation.|Interbedded, partly calcareous, very fine-grained sandstone, siltstone and shale.|
10952|Mackunda Formation|71855|5|Briefly described|p27|||||||Overlies the Toolebuc Formation.||
10952|Mackunda Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone. Overlain by the Winton Formation.||
10952|Mackunda Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW). Note that it also appears as a unit in the Neales River Group. Upper part: confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Oodnadatta FZ. Is overlain by Winton FZ.||
10952|Mackunda Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Sandstone, calcareous; siltstone and shale.|
10952|Mackunda Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
10952|Mackunda Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Allaru Mudstone, underlies the Winton Formation.||
10952|Mackunda Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity. Marginal marine.||||Underlain by Allura Mudstone. Underlain by and equivalent to Oodnadatta Formation.||
10952|Mackunda Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Allaru Mudstone. Equivalent to Winton Formation.||
10952|Mackunda Formation|73479|5|Briefly described|p156 Fig.2, p159-160, p166, p175|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97 Ma|||Overlies Allaru Mudstone, unconformably underlies Eyre Formation||
10956|Maclean Sandstone Member|22857|4|Described|p318-9, p548 App. 1 Tb.A1.12|Middle Jurassic|Middle Jurassic|Top unit of the Walloon Coal Measures. Sandy channel-fill feldspathic sandstone. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin.||||||
10956|Maclean Sandstone Member|22865|6|Mentioned|p318,Fig22.10ap318|||||||||
10956|Maclean Sandstone Member|23811|5|Briefly described|Map Legend description|Callovian|Bajocian|Of Walloon Coal Measures.  Consists of thick-bedded, crossbedded, feldspathic to lithic arenite, minor coal.  Geological province: Clarence-Moreton Basin.||||||20-DEC-04
10956|Maclean Sandstone Member|23812|5|Briefly described|p34 Tb.4|Middle Jurassic|Middle Jurassic|Of the Walloon Coal measures.  44m thick at type section. Geological Province: Clarence-Moreton Basin.||||||
10956|Maclean Sandstone Member|30785|2|Defined|p399|Late Jurassic|Late Jurassic|||||||
10956|Maclean Sandstone Member|41631|5|Briefly described|p20|||||||||
10956|Maclean Sandstone Member|60079|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|Of the Walloon Coal Measures.||||||20-JUL-04
10956|Maclean Sandstone Member|60993|5|Briefly described|p32|||Of Walloon Coal Measures. Sandstone with thin pebbly conglomeratic lenses and minor siltstone lenses. Name may be out of use now or valid only in the Maclean area where it is overlain by the Kangaroo Creek Sst?||||||28-AUG-12
10956|Maclean Sandstone Member|60995|4|Described|p68, p51 Fig. 3|Middle Jurassic|Middle Jurassic|Of Walloon Coal Measures. An upper feldspathic sandstone facies. Max. thickness: 50m. Geol. Prov: Clarence-Moreton Basin. Author believes this member warrants formation status for its consistency through the coal measures.||||||
10956|Maclean Sandstone Member|60997|5|Briefly described|p139 Fig. 1|Kimmeridgian|Kimmeridgian|Geological Province: Clarence-Moreton Basin.||||||
10956|Maclean Sandstone Member|60999|5|Briefly described|p172 Fig. 6|||||||||
10956|Maclean Sandstone Member|61000|5|Briefly described|p181, p182|Middle Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin.||||||
10956|Maclean Sandstone Member|61310|5|Briefly described|p21|Late Jurassic|Late Jurassic|Of the Walloon Coal Measures occurring in parts of the Clarence-Moreton Basin. Massive feldspathic sandstone at the top of the sequence. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin||||||
10956|Maclean Sandstone Member|69297|5|Briefly described|p487 fig 5.38|Middle Jurassic|Middle Jurassic|Clarence-Moreton Basin. Between 10-50m thick.||Walloon Coal Measures||Overlain by the Kangaroo Creek Sandstone.|Feldspathic sandstone.|
10956|Maclean Sandstone Member|70374|6|Mentioned|p808, p809 figure 1,|Oxfordian|Oxfordian|Only in NSW.||Of Walloon Coal Measures ?||||
10958|Macleay Group|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Lithic sandstone, mudstone, calcareous mudstone, crinoidal limestone, silicified limestone, felsic volcanics, minor diamictite. Max. thickness: >1500m. Geological Province: Barnard Basin (Nambucca Basin).||||||03-MAR-06
10958|Macleay Group|23720|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|Includes the Yessabah Limestone and Warbro Formation.||||||15-DEC-04
10958|Macleay Group|24120|5|Briefly described|p6|Permian|Permian|||||||
10958|Macleay Group|34556|5|Briefly described|p265|||Permian||||||
10958|Macleay Group|34590|6|Mentioned|p300|||Permian||||||
10958|Macleay Group|34713|6|Mentioned|p119|||||||||
10958|Macleay Group|39287|6|Mentioned|p13|||||||||
10958|Macleay Group|41347|4|Described|Table 5|||||||||
10958|Macleay Group|41348|5|Briefly described|Map legend|Permian|Permian|Includes: Yessabah Limestone, Warbro Formation, and Beechwood beds.  Lithic sandstone, mudstone, calcareous mudstone, crinoidal limestone, silicified limestone, felsic volcanics, and minor diamictite.||||||16-DEC-04
10958|Macleay Group|43384|14|Not recorded|Map Legend||Permian|||||||
10958|Macleay Group|43385|14|Not recorded|p167,179,180||Early Permian|SH56-10,SH56-14||||||
10958|Macleay Group|44450|3|Fully described|p24 Table 5|Early Permian|Early Permian|Geological Province: Hastings Block. Max. thickness: >1500 m.||||||
10958|Macleay Group|61805|5|Briefly described|p436|Permian|Carboniferous|Geological Province: New England Orogen. Volcanic and metasedimentary rocks.||||||17-NOV-08
10958|Macleay Group|71628|5|Briefly described|p17: 75, 86|||Hastings Block.|||Beechwood beds.|||
11025|Main Camp Syenite|33476|2|Defined|p96|Triassic|Triassic|Type area for trachytic phase in Main Camp Creek at  GR273232. Relationship with adjacent Cullens Creek Granite is not known.||||Intrudes Emu Creek Formation and Drake Andesite.|Complex consisting of trachyte, syentie, diorite, dolerate and gabbro.|06-MAR-19
11025|Main Camp Syenite|33766|6|Mentioned|Map legend|Triassic|Triassic|||||||
11025|Main Camp Syenite|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
11025|Main Camp Syenite|42378|6|Mentioned|Table 1 P11|||||||||
11025|Main Camp Syenite|43008|5|Briefly described|map legend|||||||||
11031|Main Range Volcanics|22601|6|Mentioned|405|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|23799|3|Fully described|p54, p9 Tb. 1|Early Miocene|Late Oligocene|Age: 25-19.4Ma (K/Ar, Webb et al, 1967).  Unconformably overlie Sugarloaf Mets., Cressbrook Gp., Tarong beds and Woogaroo Subgroup.  Max. thickness: ~1000m.  Geological Province: Main Range-Lamington Volcanic Province.||||||
11031|Main Range Volcanics|23800|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
11031|Main Range Volcanics|24560|5|Briefly described|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|29720|6|Mentioned|p80|||||||||
11031|Main Range Volcanics|30303|6|Mentioned|p322|||Overlies Cressbrook Group||||||
11031|Main Range Volcanics|31132|6|Mentioned|p148|||Refers Webb et al. (1967)||||||
11031|Main Range Volcanics|31273|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|32103|6|Mentioned|p406|||||||||
11031|Main Range Volcanics|32491|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|32492|6|Mentioned|Map legend|Miocene|Miocene|||||||
11031|Main Range Volcanics|32797|6|Mentioned|p17|||||||||
11031|Main Range Volcanics|32912|5|Briefly described|p157|||See also Table 1||||||
11031|Main Range Volcanics|32924|6|Mentioned|p111|||Refers Stevens (1965)||||||
11031|Main Range Volcanics|33091|5|Briefly described|p7|||Stratigraphy||||||
11031|Main Range Volcanics|33290|4|Described|p38|||||||||
11031|Main Range Volcanics|33381|4|Described|p121|||Tertiary. See also p123.||||||24-SEP-22
11031|Main Range Volcanics|33476|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|33705|6|Mentioned|p45|||||||||
11031|Main Range Volcanics|33751|6|Mentioned|p149|||||||||
11031|Main Range Volcanics|33766|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|34507|6|Mentioned|p87|||||||||
11031|Main Range Volcanics|35101|3|Fully described|p58|||||||||
11031|Main Range Volcanics|36579|6|Mentioned|p447|||||||||
11031|Main Range Volcanics|36779|6|Mentioned|p8|||||||||
11031|Main Range Volcanics|36926|6|Mentioned|p165|||||||||
11031|Main Range Volcanics|37252|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|37376|6|Mentioned|p491|||||||||
11031|Main Range Volcanics|37389|6|Mentioned|p54|||||||||
11031|Main Range Volcanics|37391|6|Mentioned|p26|||||||||
11031|Main Range Volcanics|37435|6|Mentioned|Fig.2|||||||||
11031|Main Range Volcanics|38205|2|Defined|p89|early Miocene|late Oligocene|Late Oligocene to Early Miocene||||||
11031|Main Range Volcanics|39071|6|Mentioned|p344|||||||||
11031|Main Range Volcanics|39445|5|Briefly described|Table 14|||||||||
11031|Main Range Volcanics|39998|6|Mentioned|p192|||||||||
11031|Main Range Volcanics|40475|5|Briefly described|p9|||Also Mention on P5.||||||
11031|Main Range Volcanics|40485|6|Mentioned|Fig.1|||||||||
11031|Main Range Volcanics|40486|6|Mentioned|p84|||||||||
11031|Main Range Volcanics|40488|6|Mentioned|p92|||||||||
11031|Main Range Volcanics|40513|6|Mentioned|p22|||||||||
11031|Main Range Volcanics|40623|5|Briefly described|p72|||||||||
11031|Main Range Volcanics|40734|6|Mentioned|p65|||||||||
11031|Main Range Volcanics|41906|6|Mentioned|p40|||||||||
11031|Main Range Volcanics|42041|6|Mentioned|p221|||||||||
11031|Main Range Volcanics|42485|4|Described|p264|||||||||
11031|Main Range Volcanics|42525|5|Briefly described|Map legend|Miocene|Oligocene|||||||
11031|Main Range Volcanics|43003|5|Briefly described|p169|||||||||
11031|Main Range Volcanics|43007|5|Briefly described|p258|||||||||
11031|Main Range Volcanics|43100|5|Briefly described|p49|||||||||
11031|Main Range Volcanics|43150|5|Briefly described|Map Legend||Tertiary|||||||
11031|Main Range Volcanics|44782|2|Defined|p39-42,44-46,49,51,||Tertiary|Pl.1.||||||
11031|Main Range Volcanics|44783|14|Not recorded|p2|||||||||
11031|Main Range Volcanics|44784|4|Described|p11,map 3||Tertiary|||||||
11031|Main Range Volcanics|44786|14|Not recorded|p193-202||Miocene|Early Miocene||||||
11031|Main Range Volcanics|44813|14|Not recorded|p80,82,83,85,89||Tertiary|Contains early Miocene flows. 22-24 Ma.||||||
11031|Main Range Volcanics|44818|6|Mentioned|p276|||||||||
11031|Main Range Volcanics|44923|5|Briefly described|Map Legend||Tertiary|||||||
11031|Main Range Volcanics|45087|5|Briefly described|p114|||Chemical analyses||||||
11031|Main Range Volcanics|45110|6|Mentioned|Table 21|||||||||
11031|Main Range Volcanics|48917|4|Described|p37|||See also p7. Refers Stevens (1966)||||||24-SEP-22
11031|Main Range Volcanics|50320|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|50322|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies: Walloon Coal Measures, Koukandowie Formation.||||||
11031|Main Range Volcanics|50384|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|50631|5|Briefly described|Map Legend|Tertiary|Tertiary|Basalt, minor trachyte.||||||
11031|Main Range Volcanics|60077|5|Briefly described|Map legend|Tertiary|Tertiary|Basalt, dolerite, minor shale, siltstone, diatomite.||||||
11031|Main Range Volcanics|60370|5|Briefly described|Map Legend|Tertiary|Tertiary|Olivine basalt; sandstone, shale, siltstone, conglomerate, diatomite.||||||
11031|Main Range Volcanics|60371|5|Briefly described|Map Legend|Tertiary|Tertiary|Olivine basalt; sandstone, shale, siltstone, conglomerate, diatomite, locally intercalated with basalt flows.||||||
11031|Main Range Volcanics|61007|5|Briefly described|p300|Early Miocene|Early Miocene|Extensive extruded basalts.||||||
11031|Main Range Volcanics|61310|6|Mentioned|p22|Tertiary|Tertiary|||||||
11031|Main Range Volcanics|63731|5|Briefly described|Map legend||Tertiary|Rhyolite (intrusive plug). Olivine basalt lava; minor mudstone and sandstone.||||||12-DEC-07
11031|Main Range Volcanics|63748|5|Briefly described|p22, p23-24|Early Miocene|Late Oligocene|Unconformably overlie Marburg Subgroup in the Warwick area; also overlies Walloon C.M. Geological province: Lamington-Main Range Volcanics Province. Massive, fine-grained olivine basalt, occurring mainly as flows. Also mentioned on p50.||||||07-FEB-11
11031|Main Range Volcanics|65003|4|Described|p7,p9, p22||Miocene|Of Clarence-Moreton Basin.|||||Olivine basalt, tuff, agglomerate, dolerite; minor shale, siltstone, and diatomite.|30-MAR-12
11031|Main Range Volcanics|67402|6|Mentioned|p258|||Tarong Basin.||||||
11031|Main Range Volcanics|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as Dundowran, Gin Gin and Mount Runsome Basalts; Minerva Hills, Peak Range and Waddy Point Volcanics; unnamed basalt and subordinate rhyolite (lavas and some plugs), are all mapped under the symbol, Tv.||||||
11031|Main Range Volcanics|68679|5|Briefly described|p322-323, p396, p455|Neogene|Paleogene|Tertiary.||||Unconformably overlies Maronghi Creek beds, Sugarloaf Metamorphics and Chahpingah Meta-Igneous Complex.||
11031|Main Range Volcanics|68901|6|Mentioned|p8 Fig. iii|Paleogene|Paleogene|||||||27-SEP-18
11031|Main Range Volcanics|69594|6|Mentioned|p545|Cenozoic|Cenozoic|Clarence-Moreton Basin.||||||
11031|Main Range Volcanics|69599|5|Briefly described|p584, p598|||Near Maidenwell, diatomite is commercially mined. An extensive duricrust developed on this (and other) units.|||||Contains a sedimentary assemblage of sandstone, shale, siltstone, conglomerate, tuffaceous sediments and diatomite interbedded with basalt.|
11031|Main Range Volcanics|69793|6|Mentioned|p1113 Fig.3|Cenozoic|Cenozoic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
11031|Main Range Volcanics|72297|5|Briefly described|p726|Miocene|Oligocene|Basalt lavas dammed local drainages, producing lakes in which diatomite deposits accumulated (eg Mount Sylvia, Maidenwell).|||||Basalt.|
11031|Main Range Volcanics|72298|6|Mentioned|p797|Cenozoic|Cenozoic|Underlies unconsolidated Quaternary alluvium which supplies most of the groundwater in the Lockyer Valley.||||||
11031|Main Range Volcanics|73113|5|Briefly described|p. 7, 22-23, 26, 41, 44-45, 48, 88...|||Surat Basin. Partial aquifer. More locations: p. 98, 116, 118-122, 140, 146, 151-152, 158, 160-161, 171-172.||||||
11031|Main Range Volcanics|73200|5|Briefly described|p532-p533, p539 Fig.11, p541, p543|Early Miocene|Late Oligocene|Abbreviated to MRV on p533 Fig.4 [and MRB on p542 Fig.14?].||||Overlies the Walloon Coal Measures.|Olivine basalt with pyroclastic rocks.|
11031|Main Range Volcanics|73450|4|Described|p90-95|Chattian|Chattian|Grouped into northern and southern subunits. In the southwest, there is a thick (up to 900 m) sequence of lavas, pyroclastic rocks and minor conglomerate that thins westward. In the southeast, erosion has exposed a related group of mafic and felsic shallow-level intrusive bodies in the Fassifern Valley. Mafic and felsic divisions are not in use on the current geological coverage. Felsic flows are locally glassy/devitrified, porphyritic or vesicular. Yielded various K-Ar and Ar-Ar ages averaging ca 26 Ma (or younger).|ca 26 Ma||Cooby Trachyte Member, Nutgrove Rhyolite Member||Includes metaluminous and peralkaline trachyte to rhyolite flows, breccia, tuffs and ignimbrites.|
11039|Maitland Group|22607|6|Mentioned|p 57|||||||||
11039|Maitland Group|22610|5|Briefly described|p 123, Fig 1|||||||||
11039|Maitland Group|22663|5|Briefly described|NSW97 - 1 p2|Late Permian|Early Permian|||||||01-MAR-10
11039|Maitland Group|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Includes the Mulbring Siltstone, Muree Sandstone and Branxton Formation. Max. thickness: 2000m. Geological Province: Sydney Basin. See also p536 App.1 Tb.A1.9.||||||
11039|Maitland Group|22969|5|Briefly described|p 6||Early Permian|||||||
11039|Maitland Group|23540|5|Briefly described|Fig 2 p 419|||Includes Branxton Formation. Also see p 417||||||20-FEB-07
11039|Maitland Group|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Geological Province: Sydney Basin.||||||
11039|Maitland Group|24121|5|Briefly described|p108|||||||||
11039|Maitland Group|24423|5|Briefly described|p230 Fig.3|Late Permian|Early Permian|Geological Province: Sydney Basin.||||||
11039|Maitland Group|29889|6|Mentioned|p130|||||||||
11039|Maitland Group|29922|6|Mentioned|Appendix 1|||||||||
11039|Maitland Group|29926|6|Mentioned|p5|||||||||
11039|Maitland Group|29942|6|Mentioned|p11|||||||||
11039|Maitland Group|29943|6|Mentioned|p37|||||||||
11039|Maitland Group|29944|6|Mentioned|FIg.18|||||||||
11039|Maitland Group|30005|6|Mentioned|p81|||||||||
11039|Maitland Group|30442|6|Mentioned|p24|||||||||
11039|Maitland Group|30555|6|Mentioned|p296|||||||||
11039|Maitland Group|31124|5|Briefly described|Table 1|||See also Fig. 1 & 2, P17. Petrology||||||
11039|Maitland Group|31125|6|Mentioned|p16|||Refers geology||||||
11039|Maitland Group|31251|6|Mentioned|p73|||Refers Ludbrook (1956)||||||
11039|Maitland Group|31375|6|Mentioned|p4|||Stratigraphy||||||
11039|Maitland Group|31706|6|Mentioned|p671|||Correlation chart for Gondwana System||||||
11039|Maitland Group|31855|6|Mentioned|p14|||Stratigraphic table||||||
11039|Maitland Group|31881|6|Mentioned|p331|||Correlated with Bickham Fm.||||||
11039|Maitland Group|31882|6|Mentioned|p244|||||||||
11039|Maitland Group|31883|6|Mentioned|p594|||See also Table 1||||||
11039|Maitland Group|31885|4|Described|p1438|||See also P1439. Table 1||||||
11039|Maitland Group|32266|6|Mentioned|p24|||||||||
11039|Maitland Group|32833|6|Mentioned|p108|||||||||
11039|Maitland Group|32945|6|Mentioned|p38|||Permian||||||
11039|Maitland Group|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
11039|Maitland Group|33132|6|Mentioned|Table 1|||||||||
11039|Maitland Group|33334|6|Mentioned|Fig.3|||||||||
11039|Maitland Group|33685|6|Mentioned|Table 1|||Permian.||||||
11039|Maitland Group|33711|6|Mentioned|p383|||Table 2||||||
11039|Maitland Group|33867|4|Described|p6|||||||||
11039|Maitland Group|34015|6|Mentioned|p323|||Permian||||||
11039|Maitland Group|34036|6|Mentioned|p434|||||||||
11039|Maitland Group|34037|6|Mentioned|Table 5.27|||||||||
11039|Maitland Group|34039|6|Mentioned|p355|||Permian||||||
11039|Maitland Group|34043|6|Mentioned|Fig.5.32|||Correlation.  Perm.||||||
11039|Maitland Group|34059|6|Mentioned|Map legend|Permian|Permian|||||||
11039|Maitland Group|34084|6|Mentioned|p368|||Perm.||||||
11039|Maitland Group|34138|6|Mentioned|Cor.Chart|||Artinskian - Kazanian||||||
11039|Maitland Group|34171|6|Mentioned|p16|||||||||
11039|Maitland Group|34204|6|Mentioned|p65|||||||||
11039|Maitland Group|34292|6|Mentioned|p32|||Permian. See also Tables 1 & 3||||||
11039|Maitland Group|34335|6|Mentioned|p369|||Permian||||||
11039|Maitland Group|34345|3|Fully described|p329|||Permian||||||
11039|Maitland Group|34350|6|Mentioned|p16|||Permian. See also P18.||||||
11039|Maitland Group|34399|6|Mentioned|p312|||||||||
11039|Maitland Group|34400|6|Mentioned|p9|||||||||
11039|Maitland Group|34444|6|Mentioned|Map legend|Permian|Permian|||||||
11039|Maitland Group|34445|6|Mentioned|Fig.5.3|||||||||
11039|Maitland Group|34446|6|Mentioned|p21|||||||||
11039|Maitland Group|34447|6|Mentioned|Table 5.2|||||||||
11039|Maitland Group|34448|5|Briefly described|p432|||||||||
11039|Maitland Group|34465|6|Mentioned|p334|||||||||
11039|Maitland Group|34466|6|Mentioned|p350|||||||||
11039|Maitland Group|34569|6|Mentioned|p10|||Permian||||||
11039|Maitland Group|34614|6|Mentioned|p29|||||||||
11039|Maitland Group|34845|6|Mentioned|p119|||||||||
11039|Maitland Group|35284|6|Mentioned|Fig.12|||||||||
11039|Maitland Group|35823|6|Mentioned|p31|||||||||
11039|Maitland Group|36042|6|Mentioned|Table 1|||||||||
11039|Maitland Group|36069|6|Mentioned|p23|||||||||
11039|Maitland Group|36940|6|Mentioned|p145|||||||||
11039|Maitland Group|37083|6|Mentioned|p165|||||||||
11039|Maitland Group|37084|6|Mentioned|p176|||||||||
11039|Maitland Group|37086|6|Mentioned|p182|||||||||
11039|Maitland Group|37087|6|Mentioned|p192|||||||||
11039|Maitland Group|37092|6|Mentioned|p229|||||||||
11039|Maitland Group|37094|4|Described|p240|||||||||
11039|Maitland Group|37100|6|Mentioned|p260|||||||||
11039|Maitland Group|37773|6|Mentioned|p22|||||||||
11039|Maitland Group|37922|5|Briefly described|p481|||||||||
11039|Maitland Group|37924|6|Mentioned|p488|||||||||
11039|Maitland Group|38064|6|Mentioned|p41|||||||||
11039|Maitland Group|38603|6|Mentioned|p79|||||||||
11039|Maitland Group|38614|6|Mentioned|p1|||See also P14||||||
11039|Maitland Group|38656|5|Briefly described|Table1.5.5|||P220||||||
11039|Maitland Group|38917|6|Mentioned|p168|||||||||
11039|Maitland Group|39267|6|Mentioned|p251|||||||||
11039|Maitland Group|39287|6|Mentioned|p13|||See also P42 & Fig.2.5||||||
11039|Maitland Group|39288|4|Described|p61|||||||||
11039|Maitland Group|39292|6|Mentioned|p104|||||||||
11039|Maitland Group|39294|6|Mentioned|p163|||||||||
11039|Maitland Group|39307|6|Mentioned|p437|||Permian foraminifera||||||
11039|Maitland Group|39308|6|Mentioned|p491|||See also Fig.23.4||||||
11039|Maitland Group|39346|6|Mentioned|Map legend|Late Permian|Middle Permian|Middle to Late Permian||||||
11039|Maitland Group|39811|6|Mentioned|Map legend|Permian|Permian|||||||
11039|Maitland Group|39812|6|Mentioned|Map legend|Permian|Permian|||||||
11039|Maitland Group|39830|6|Mentioned|Map legend|Late Permian|Middle Permian|Middle to Late Permian||||||
11039|Maitland Group|40166|5|Briefly described|p346|||See also Table 1 and Fig.2||||||
11039|Maitland Group|40222|6|Mentioned|Figure|||||||||
11039|Maitland Group|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
11039|Maitland Group|40245|6|Mentioned|p183|||||||||
11039|Maitland Group|40256|6|Mentioned|Fig.3|||||||||
11039|Maitland Group|40321|6|Mentioned|p21|||||||||
11039|Maitland Group|40330|6|Mentioned|Fig.4|||||||||
11039|Maitland Group|40331|6|Mentioned|p3|||||||||
11039|Maitland Group|40636|6|Mentioned|p43|||||||||
11039|Maitland Group|41010|6|Mentioned|p11|||||||||
11039|Maitland Group|41054|6|Mentioned|p155|||||||||
11039|Maitland Group|41290|6|Mentioned|Fig.8|||||||||
11039|Maitland Group|41514|6|Mentioned|p80|||||||||
11039|Maitland Group|41604|6|Mentioned|p2|||||||||
11039|Maitland Group|41637|6|Mentioned|p200|||||||||
11039|Maitland Group|41666|6|Mentioned|p11|||||||||
11039|Maitland Group|41689|6|Mentioned|Table 1|||||||||
11039|Maitland Group|41834|6|Mentioned|p590|||||||||
11039|Maitland Group|41902|5|Briefly described|p5 Table 1|||||||||
11039|Maitland Group|41903|6|Mentioned|Map legend|Late Permian||||||||
11039|Maitland Group|41904|6|Mentioned|Map legend|||Age not stated on map||||||
11039|Maitland Group|42182|6|Mentioned|Table 1|||||||||
11039|Maitland Group|42214|6|Mentioned|p460|||||||||
11039|Maitland Group|42547|6|Mentioned|p85|||||||||
11039|Maitland Group|42648|5|Briefly described|p33, p35|||||||||
11039|Maitland Group|42780|5|Briefly described|Fig.2 P412|||||||||
11039|Maitland Group|42916|5|Briefly described|Table 1|Late Permian|Middle Permian|||||||
11039|Maitland Group|42922|5|Briefly described|p38|||||||||
11039|Maitland Group|42925|5|Briefly described|Table 1|Late Permian|Early Permian|||||||
11039|Maitland Group|43050|5|Briefly described|p16|||||||||
11039|Maitland Group|43194|5|Briefly described|p128, p129 Tb. 8.3, p130|Middle Permian|Middle Permian|Hunter and Newcastle regions, Sydney Basin. Contains Branxton Formation, Muree Sandstone, Mulbring Siltstone. Overlain by Munmorah Conglomerate. Equivalent to the Porcupine and Watermark Formations in the Gunnedah Basin.||||||
11039|Maitland Group|43257|5|Briefly described|Map Legend||Permian|Age Middle to Late Permian.||||||
11039|Maitland Group|43317|6|Mentioned|Table 1 p7|||||||||
11039|Maitland Group|43318|14|Not recorded|opp  p6|||||||||
11039|Maitland Group|43319|14|Not recorded|Map Legend|||||||||
11039|Maitland Group|43320|14|Not recorded|Table 1 p9||Triassic|||||||
11039|Maitland Group|43344|14|Not recorded|p11,18-20,78,84,88||Permian|Equivalent to Shoalhaven Group. p169||||||
11039|Maitland Group|43383|14|Not recorded|Fig.5||Permian|||||||
11039|Maitland Group|43384|14|Not recorded|Map Legend||Late Permian|||||||
11039|Maitland Group|43385|14|Not recorded|p178,179||Late Permian|||||||
11039|Maitland Group|43425|14|Not recorded|p1||Permian|||||||
11039|Maitland Group|43440|14|Not recorded|p32,35,44,62,63,73,|||p76,77,82-84,90||||||
11039|Maitland Group|43447|14|Not recorded|p17,18,20,diag.p22||Permian|inc Mulbring Slts,Glendon Ls.Mb,Dochra Slts.Mb,Branxton Fm,Muree Ss.Mb,Cessnock Ss.Mb.p28,31,32,48-9||||||
11039|Maitland Group|43448|4|Described|p222-225,227-229,||Permian|Includes Mulbring and Branxton Subgroups. Pl.1,232,235,236||||||
11039|Maitland Group|43450|14|Not recorded|p9,11,16,17,24|||||||||
11039|Maitland Group|43451|14|Not recorded|Map Legend|||||||||
11039|Maitland Group|43474|14|Not recorded|p51|||||||||
11039|Maitland Group|43477|2|Defined|p12,14-5,17-19,22,28||Permian|p29,32-34,41,44-46,59,Pl.1,5||||||
11039|Maitland Group|43479|14|Not recorded|p188,190,193,218-9|Kazanian|Artinskian|||||||
11039|Maitland Group|43543|14|Not recorded|p576||Permian|||||||
11039|Maitland Group|43984|14|Not recorded|p135|||||||||
11039|Maitland Group|44040|14|Not recorded|p23,27|||||||||
11039|Maitland Group|44219|14|Not recorded|p39|||||||||
11039|Maitland Group|44244|4|Described|p232|Late Permian|Early Permian|Comprises Branxton Formation, Muree Sandstone and Mulbring Siltstone.  Conformably overlies the Greta Coal Measures.  Geological Province: Sydney Basin.||||||
11039|Maitland Group|44256|14|Not recorded|p183|||||||||
11039|Maitland Group|44311|14|Not recorded|p201|||||||||
11039|Maitland Group|44347|14|Not recorded|p77|||||||||
11039|Maitland Group|44348|14|Not recorded|p55,56|||||||||
11039|Maitland Group|44450|5|Briefly described|p147 Fig 43|Permian|Permian|Geological Province: Sydney Basin.||||||
11039|Maitland Group|44489|14|Not recorded|p70|||||||||
11039|Maitland Group|44859|14|Not recorded|p68,71|||Gastropod.||||||
11039|Maitland Group|44861|14|Not recorded|p228,232|||||||||
11039|Maitland Group|44998|14|Not recorded|p.104|Kungurian|Artinskian|Kungurian-U.Artinskian.||||||
11039|Maitland Group|45031|14|Not recorded|p28,48-56,60,62,67-8|||||||||
11039|Maitland Group|45090|6|Mentioned|p28|||Relationship of rock units||||||
11039|Maitland Group|48831|14|Not recorded|p.8,24,30,34,37-42|||||||||
11039|Maitland Group|48841|14|Not recorded|p27|||Fauna closely related to Middle Bowen Beds.||||||
11039|Maitland Group|48843|14|Not recorded|p.21|||(See Qld authors cards).||||||
11039|Maitland Group|48926|6|Mentioned|p41|||P41 et seq.||||||
11039|Maitland Group|48971|6|Mentioned|p9|||See also P11, P14, P20, P21.||||||
11039|Maitland Group|50268|5|Briefly described|Map Legend|Tatarian|Artinskian|Includes: Muree Sandstone, Branxton Formation, Mulbring Siltstone.  Geological Province: Sydney Basin.||||||
11039|Maitland Group|60281|4|Described|p58|Late Permian|Early Permian|Geological Province: Sydney Basin. Lower fine-grained marine section (Wandrawandian Silltstone in south, Branxton Formation in north); and, upper fine-grained marine section (Berry Siltstone in south, Mulbring Siltstone in north).||||||27-APR-05
11039|Maitland Group|60290|5|Briefly described|p15|Permian|Permian|Overlies Greta Coal Measures. Geological Province: Cranky Corner Basin.||||||07-FEB-11
11039|Maitland Group|60297|5|Briefly described|p168 Fig.1, p177|Permian|Permian|Marine. Overlies Greta Coal Measures.||||||18-MAY-05
11039|Maitland Group|61315|5|Briefly described|Table SY1|Late Permian|Early Permian|Oncludes the Branxton Formation, Muree Sandstone and Mulbring Siltstone. Geological Province: Sydney Basin||||||
11039|Maitland Group|61529|5|Briefly described|p853, p854 Fig.1b|Late Permian|Late Permian|Includes Branxton Formation, Muree Sandstone and Mulbring Siltstone. Fine-grained sandstone and siltstone. Overlain by Wittingham, Newcastle and Tomago Coal Measures. Geological Province: Sydney Basin.||||||17-FEB-06
11039|Maitland Group|63832|5|Briefly described|p131 fig 2|Roadian|Kungurian|Cranky Corner/Gresford Block, Southern New England Fold Belt; also NE Sydney Basin. Seventh (P3) glaciation.|||Includes Branxton Formation and Mulbring Siltstone.|||13-DEC-17
11039|Maitland Group|64631|5|Briefly described|p44 Fig.2.|Roadian|Kungurian|Southern New England Fold Belt, Cranky Corner/Gresford Block; and Sydney Basin. Biostratigraphic age control for base and top and radiometric control within unit.|||Includes Branxton Formation, Mulbring Siltstone in Sydney Basin.|Overlies Greta Coal Measures.||
11039|Maitland Group|65118|6|Mentioned|p496|||Formerly the 'Upper Marine epoch'(Carey and Browne 1938).||||||
11039|Maitland Group|67663|5|Briefly described|p518, p520 Tb.1|Permian|Permian|Late Permian.|||Includes Branxton Formation.|Overlies Greta Coal Measures. Overlain by the Tomago Coal Measures and Singleton Supergroup.|Comprises thick sequence of sand and silt.|
11039|Maitland Group|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.|||Branxton Formation, Muree Sandstone, Mulbring Siltstone.|Overlies Greta Coal Measures. Is overlain by Tomago Coal Measures.||
11039|Maitland Group|68003|5|Briefly described|p38 Fig.3-j, p40, p42, p130.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion. Correlative of Millie Group (Gunnedah Basin); Shoalhaven Group (Western Coalfield); and Bickham, Borambil Creek and Toll Bar Formations (Werrie Basin). Deposition during cold climate.|||Includes Branxton Formation, Muree Sandstone and Mulbring Siltstone.|Overlies Greta Coal Measures. Is overlain by Singleton Supergroup. Is unconformably overlain by Munmorah Conglomerate.||
11039|Maitland Group|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields. Equivalent to Millie Group (Gunnedah Basin) and upper part of Shoalhaven Group.|||Includes Branxton Formation, Muree Sandstone and Mulbring Siltstone.|Overlies Greta Coal Measures. Is overlain by Singleton and Tomago Coal Measures.||
11039|Maitland Group|68202|6|Mentioned|p176|Triassic|Triassic|Sydney Basin.||||||
11039|Maitland Group|68493|5|Briefly described|p1, p3 Fig.1, p5, p5 Fig.2, p6, p14|Permian|Permian|Sydney Basin. 1200 m thick. McKellar (1969) designated a composite type section, consisting of 790 m in the Greta-Branxton area overlain by an additional 510 m around Mulbring, separated by a highly fossiliferous siltstone 30-60 m thick (Fenestella Shale). The Group demonstrates the cyclicity of Permian sedimentation in the northern Sydney Basin.|||Includes Branxton Formation, Muree Sandstone, and Mulbring Siltstone.|Conformably overlies the Greta Coal Measures; is overlain by Tomago/Newcastle Coal Measures.|Dominated by thick successions of highly fossiliferous siltstone, sandstone, and conglomerate.|
11039|Maitland Group|68592|6|Mentioned|p1782|Permian|Permian|Hunter Valley.||||Broadly equivalent to Shoalhaven Group.||
11039|Maitland Group|69297|6|Mentioned|p501, p504|Capitanian|Kungurian|Sydney Basin. Sandstones of this group are good potential hydrocarbon reservoirs. Siltstones may also form regional sealing units.|||Includes the Branxton Formation, Muree Sandstone and the Mulbring Siltstone.|Overlies the Greta Coal Measures. Overlain by the Singleton Group.||
11039|Maitland Group|69683|5|Briefly described|p410 Fig.1, p411 Fig.2, p416 Fig.3|Late Permian|Middle Permian|See also p419 Fig.4, p420 Fig.5.|||Includes Branxton Formation; Cessnock and Muree Sandstones; Mulbring Siltstone.||Siltstone, claystone, fine- to coarse-grained sandstone, conglomerate.|
11039|Maitland Group|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
11039|Maitland Group|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin. Undifferentiated in this sheet area.|||||Quartz-lithic sandstone with sporadic marine fossils, conglomerate, grey siltstone, fossiliferous siltstone, minor claystone and chert.|
11039|Maitland Group|70661|6|Mentioned|p165|||Hunter Valley (North Sydney Basin).|||Branxton Formation, Mulbring Siltstone|||
11039|Maitland Group|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
11039|Maitland Group|70791|5|Briefly described|p277, p293 Fig.17|Guadalupian|Guadalupian|Hunter Coalfield and north Werrie Basin.|||Branxton Formation, Muree Sandstone, Mulbring Siltstone, Borambil Creek Formation.|||
11039|Maitland Group|70878|6|Mentioned|p715|Permian|Permian||||Branxton Formation.|Overlies Greta Coal Measures.||
11039|Maitland Group|73197|6|Mentioned|p478|Guadalupian|Guadalupian|Sydney Basin. Tuff layers sourced from the Currarong Orogen.|272-266 Ma||||Includes tuff layers.|
11039|Maitland Group|73304|6|Mentioned|p75||||||Mulbring Siltstone, Muree Sandstone, Branxton Formation|||
11044|Majurgong Formation|22639|5|Briefly described|p280|Early Devonian|Early Devonian|||||||
11044|Majurgong Formation|22857|5|Briefly described|p462 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Murrumbidgee Group. Quartzite, sandstone, siltstone. Max. thickness: 120m. Geological Province: Canberra-Yass Shelf. See also p464 App.1 Tb.A1.6.||||||
11044|Majurgong Formation|23522|5|Briefly described|p248 Fig 4|Emsian|Pragian|||||||
11044|Majurgong Formation|23898|5|Briefly described|p271 Fig.2, p272 Fig.3|||||||||
11044|Majurgong Formation|24005|5|Briefly described|p293|Early Devonian|Early Devonian|Of Murrumbidgee Group. Geological Province: Lachlan Fold Belt||||||
11044|Majurgong Formation|24250|5|Briefly described|p109 Fig.5|Early Devonian|Early Devonian|Parent: Murrumbidgee Group. Overlying Unit: Spirifer yassensis Limestone Member (conformable). Underlying Unit: Cavan Bluff Limestone||||||
11044|Majurgong Formation|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11044|Majurgong Formation|30069|6|Mentioned|p12|||Map on P12||||||
11044|Majurgong Formation|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11044|Majurgong Formation|31019|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11044|Majurgong Formation|32483|4|Described|p32|||Loer Devonian. Strat. table 1.||||||18-JUN-08
11044|Majurgong Formation|32583|6|Mentioned|p373|||L.Dev.||||||
11044|Majurgong Formation|32585|4|Described|p210|||||||||
11044|Majurgong Formation|32984|6|Mentioned|p342|||Correlation chart||||||
11044|Majurgong Formation|33327|5|Briefly described|p173|||See also Fig.2. Murrumbidgee Gp.||||||
11044|Majurgong Formation|33732|5|Briefly described|p112|||||||||
11044|Majurgong Formation|34692|5|Briefly described|p186|||||||||
11044|Majurgong Formation|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11044|Majurgong Formation|35386|3|Fully described|p49|||||||||
11044|Majurgong Formation|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
11044|Majurgong Formation|36441|5|Briefly described|map legend|Pragian|Pragian|Of Murrumbidgee Group. Brown to red siltstone and shale. Underlies Taemas Limestone; overlies Cavan Limestone. BMR map code: Dlj.||||||
11044|Majurgong Formation|40124|6|Mentioned|Fig.1|||||||||
11044|Majurgong Formation|42497|5|Briefly described|Map Legend|Pragian|Pragian|||||||
11044|Majurgong Formation|42577|6|Mentioned|p25|||||||||
11044|Majurgong Formation|43430|14|Not recorded|p144|||Part of Murrumbidgee Group||||||
11044|Majurgong Formation|43431|14|Not recorded|p1262|||Wee Jasper area||||||
11044|Majurgong Formation|43461|14|Not recorded|p622|||Part of Murrumbidgee Group||||||
11044|Majurgong Formation|43529|14|Not recorded|text-fig.1||Siegenian|||||||
11044|Majurgong Formation|43530|14|Not recorded|p1028|||||||||
11044|Majurgong Formation|43575|6|Mentioned|p280||Late Devonian|||||||
11044|Majurgong Formation|45078|6|Mentioned|Fig.1|||See also P7.||||||
11044|Majurgong Formation|47038|6|Mentioned|Fig.1|||||||||
11044|Majurgong Formation|50230|4|Described|Map legend|Emsian|Emsian|Of the Murrumbidgee Group.  Overlies the Cavan Bluff Limestone; underlies the Spirifer Yassensis Limestone Member (Taemas Limestone).  Purple to grey shale, quartz sandstone, siltstone.||||||
11044|Majurgong Formation|63025|5|Briefly described|p1052 Fig. 1, p1053|Pragian|Pragian|Replaces the now obsolete name Murrumbidgee Series of Green (1961).||||||
11044|Majurgong Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Murrumbidgee Group. Purple to grey shale, quartz sandstone, siltstone.||||||
11044|Majurgong Formation|64992|5|Briefly described|p60 Fig. 1, p61|Devonian|Devonian|Part of the Taemas-Wee Jasper succession. Conformably overlain by Splinella yassensis Member (Taemas Formation). Red beds - primarily reddish deposits and deposited under subaerial conditions.||||||26-MAR-09
11044|Majurgong Formation|65214|6|Mentioned|p272, p274|Devonian|Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
11044|Majurgong Formation|68592|2|Defined|p982,p984 Fig.162,p986,p999-1002,p1895-6|Emsian|Emsian|Named after Majurgong Trigonometrical Station. Originally Majurgong Stage of Browne (1959); subsequently Majurgong Formation by various authors including Pedder et al. (1970). Type section described. Thickness varies: 32-123m. Largely unfossiliferous except towards the top: fauna listed. Early Emsian age constrained by surrounding units. Easily recognised clastic marker unit.||Unit in Murrumbidgee Group.||Conformably overlies Cavan Bluff Limestone. Is overlain conformably by Spirifer yassensis Limestone Member.|Red-brown-maroon thinly-bedded to massive shale; fine- to very fine-grained quartz-rich sandstone; less common calcareous siltstone; near base a few beds of limestone with algal laminae occur; thin beds of calcareous siltstone common towards the top.|
11044|Majurgong Formation|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmj. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Murrumbidgee Group||Overlies Cavan Bluff Limestone. Is overlain by Spirifer yassensis Limestone Member (Taemas Limestone).|Red-brown-maroon, thinly bedded-massive shale,fine-very fine grained quartz rich sandstone and less common calcareous siltstone.|
11044|Majurgong Formation|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Red-brown-maroon, thinly bedded-massive shale,fine-very fine grained quartz rich sandstone and less common calcareous siltstone.|
11044|Majurgong Formation|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|||Red-brown-maroon, thinly bedded-massive shale,fine-very fine grained quartz rich sandstone and less common calcareous siltstone.|
11044|Majurgong Formation|71656|5|Briefly described|p12 Fig.2, p33|Emsian|Emsian|Located on Bloomfield Station in the Taemas district. Includes brachiopods.||Murrumbidgee Group||Overlies Cavan Bluff Limestone, underlies Spirifer yassensis Limestone Member.|Includes maroon siltstones and fossiliferous limestone.|
11044|Majurgong Formation|73215|5|Briefly described|p994|||Talmo-Taemas area.||Murrumbidgee Group.||Overlies Cavan Bluff Limestone. Is overlain by Taemas Limestone.||25-JAN-23
11055|Malabar Formation|22969|4|Described|Fig 4.1a||Late Permian|Jerrys Plain Subgroup||||||
11055|Malabar Formation|29942|4|Described|Fig.1|||Permian||||||
11055|Malabar Formation|35767|6|Mentioned|p8|||||||||
11055|Malabar Formation|37087|6|Mentioned|p197|||||||||
11055|Malabar Formation|38603|6|Mentioned|p81|||||||||
11055|Malabar Formation|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
11055|Malabar Formation|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
11055|Malabar Formation|40166|6|Mentioned|Fig.22|||See also Table 1||||||
11055|Malabar Formation|40256|6|Mentioned|p304|||||||||
11055|Malabar Formation|40805|2|Defined|p140|Permian|Permian|||||||
11055|Malabar Formation|41010|6|Mentioned|p13|||See also Fig.2||||||
11055|Malabar Formation|41123|6|Mentioned|p178|||||||||
11055|Malabar Formation|42078|6|Mentioned|Table 1 P5|||||||||
11055|Malabar Formation|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Jerrys Plains Subgroup (Wittingham Coal Measures).  Includes the Redbank Creek, Wambo, Whynot and Blakefield seams.||||||
11055|Malabar Formation|45090|4|Described|p56|||Relationship, correlation & age||||||
11055|Malabar Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Jerrys Plain Subgroup (Wittingham Coal Measures). Geological Province: Sydney Basin/Hunter Valley area.||||||
11055|Malabar Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield. About 160 m thick. Includes the Blakefield, Whynot, Wambo and, at the top, Redbank Creek seams.||Unit in Jerrys Plains Subgroup.||Overlies Mount Ogilvie Formation. Is overlain by Althorpe Formation.|Sandstone, siltstone, conglomerate, four named coal seams; minor claystone.|
11055|Malabar Formation|69683|6|Mentioned|p411 Fig.2, p415-419 Figs.3-4|Late Permian|Late Permian|||Unit in Jerrys Plains Subgroup.||||
11059|Malachis Hill Formation|23214|6|Mentioned|p68|||Now part of the Cheesemans Creek Formation.||||||
11059|Malachis Hill Formation|24398|5|Briefly described|p265|Late Ordovician|Late Ordovician|Now regarded as part of Cheesemans Creek Formation.  Geological Province: Lachlan Fold Belt.||||||19-MAY-16
11059|Malachis Hill Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11059|Malachis Hill Formation|32088|6|Mentioned|p5|||Refers Packham (1969)||||||
11059|Malachis Hill Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11059|Malachis Hill Formation|33006|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
11059|Malachis Hill Formation|33061|6|Mentioned|p15|||Refers Stevens (1956)||||||
11059|Malachis Hill Formation|33116|6|Mentioned|Fig.6|||Ord. Correlation||||||
11059|Malachis Hill Formation|33282|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
11059|Malachis Hill Formation|33285|6|Mentioned|p32|||Late Ord.||||||
11059|Malachis Hill Formation|34404|3|Fully described|p82|||||||||
11059|Malachis Hill Formation|34405|6|Mentioned|p123|||||||||
11059|Malachis Hill Formation|34576|6|Mentioned|p357|||Fauna||||||
11059|Malachis Hill Formation|37727|6|Mentioned|p28|||See also Fig.1.||||||
11059|Malachis Hill Formation|39331|6|Mentioned|p57|||||||||
11059|Malachis Hill Formation|39663|6|Mentioned|Table 1|||||||||
11059|Malachis Hill Formation|40328|6|Mentioned|Plate 4|||||||||
11059|Malachis Hill Formation|43516|14|Not recorded|Map Legend||Late Ordovician|||||||
11059|Malachis Hill Formation|44093|5|Briefly described|p194 App. 1|Early Silurian|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
11059|Malachis Hill Formation|60989|6|Mentioned|p111, p112 Fig.1|Late Ordovician|Late Ordovician|||||||
11059|Malachis Hill Formation|63278|5|Briefly described|p147 Fig. 2b, p153|Late Eastonian|Late Ordovician|Geol Prov: Molong Volcanic Belt, LFB. Contains graptolites that define an age of late Eastonian. Upper part consists of a mixture of volcaniclastic detritus and subordinate andesitic primary lavas (Stevens 1957; Semeniuk 1970; Simpson et al. 2007).||||||07-FEB-11
11059|Malachis Hill Formation|63283|5|Briefly described|p195 Fig. 2, p198, p210|Late Ordovician|Late Ordovician|Underlain by Bowan Park Limestone Subgroup. Geological Province: Molong Volcanic Belt. Consists of well-bedded planar-laminated turbidic black siltstone. See p198-199.||||||07-FEB-11
11059|Malachis Hill Formation|63287|4|Described|p316 Fig. 1, p317 Fig. 2, p333, p335|Bolindian|Eastonian|Of Cabonne Group. Overlain conformably by Bowan Park Limestone Subgroup, underlain by Cargo Volcanics. Thickness: 550m.  Geological Province: Molong Volcanic Belt. Consists of turbiditic siltstone and qtz-rich sandstone.||||||07-FEB-11
11059|Malachis Hill Formation|63290|5|Briefly described|p396 Fig. 3|Bolindian|Eastonian|Underlain by Bowen Park Limestone Subgroup. Geological Province: Molong Volcanic Belt.||||||
11059|Malachis Hill Formation|63293|6|Mentioned|p469 Fig. 2|Bolindian|Eastonian|Underlain by Bowan Park Limestone Subgroup. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
11059|Malachis Hill Formation|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
11059|Malachis Hill Formation|67322|5|Briefly described|p23-24; Fig.5|Hirnantian||Macquarie Arc. Stevens (1957). Higher in the Malachis Hill Formation (about 300m above siltstones with an undescribed early Bolindian graptolite fauna), probably allochthonous limestone pods contain diverse coral assemblages of a mid-late Bolindian age. Occurs in the Bowan Park region.||Of the Cabonne Group.||Overlies Ballingoole Limestone (Bowan Park Limestone Subgroup). Lower part is equivalent to the Rockdale Formation.||22-FEB-18
11059|Malachis Hill Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
11059|Malachis Hill Formation|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3). Molong Volcanic Belt. Shown as Malachis Hill Fm.|c. 449-443 Ma|Cabonne Group||||
11059|Malachis Hill Formation|70684|5|Briefly described|p34-35, p39 Fig.17, p40-42, p75|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Bolindian.||||Overlies Bowan Park Limestone Subgroup.|Volcaniclastic conglomerate, basaltic andesite, siltstone; basal laminated lithic calcilutites.|
11059|Malachis Hill Formation|70754|5|Briefly described|p450 Fig.2, p455-456|Late Ordovician|Late Ordovician|Also appears as Malachi's Hill Formation. Some fossil species named.||||Conformably overlies Ballingoole Limestone (Bowan Park Subgroup).|Basal limestone breccias, overlain by graptolitic siltstones and more limestone breccias.|
11059|Malachis Hill Formation|71091|5|Briefly described|p141, p143, p147|Late Ordovician|Late Ordovician|Bowan Park area. Has late Eastonian conodonts in lower parts, and mid-late Bolindian corals (probably allochthonous) higher up.||||Conformably overlies the Downderry Limestone Member. Correlated with Angullong Formation.||
11059|Malachis Hill Formation|73154|5|Briefly described|p77 Fig.3|Bolindian|Eastonian|Macquarie Arc, Phase 4. Molong Volcanic Belt.||||Overlies Bowan Park Limestone Subgroup.|Intermediate-mafic lava, conglomerate, siltstone.|
11059|Malachis Hill Formation|73299|6|Mentioned|p1104 Fig.10|Late Ordovician|Late Ordovician|Molong High.||||Overlies the Bowan Park Subgroup.||
11059|Malachis Hill Formation|73492|5|Briefly described|p696||Katian|||||Overlies Bowan Park Limestone Subgroup||
11085|Maldon Shale|35690|6|Mentioned|p121|||||||||
11126|Malongulli Formation|5250|5|Briefly described|p43, p59||Late Ordovician|Overlies Cliefden Caves Limestone Group. Contains the youngest Ordovician trimerellid brachiopod known in NSW.||||||16-JAN-12
11126|Malongulli Formation|13139|5|Briefly described|p7, p9 Fig. 4|Late Ordovician|Late Ordovician|Contains basal limestone breccias with Ozarkodina fossils.  Overlain by the Angullong Formation; conformably overlies the Cliefden Caves Limestone Subgroup.  Geological Province: Western Molong Volcanic Belt.||||||
11126|Malongulli Formation|13995|5|Briefly described|p68-69, p90|Late Ordovician|Late Ordovician|Central NSW. Off-platform island radiolarian assemblage; also highly endemic demosponge and hexactinellid sponges. Late Eastonian. Contains highly diverse conodonts in breccias.||||||
11126|Malongulli Formation|22503|6|Mentioned|Fig.4 p646|||||||||
11126|Malongulli Formation|22679|6|Mentioned|p 9|||||||||
11126|Malongulli Formation|22857|4|Described|p424 App.1 Tb.A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Calcareous and feldspathic siltstone, limestone, arenite, conglomerate, mudstone. Max. thickness: 462m.||||||
11126|Malongulli Formation|23181|5|Briefly described|p1-3,5,6, Fig.2||Eastonian|Molong Volcanic Belt.||||||
11126|Malongulli Formation|23213|6|Mentioned|p21||Eastonian|Contains shelly fauna with strong resemblance to that in the Oakdale Formation.||||||
11126|Malongulli Formation|23214|2|Defined|p53|Bolindian|Eastonian|Of Cabonne Group.  Geological Province: Lachlan Fold Belt. Max. thickness 462m.||||||
11126|Malongulli Formation|23334|5|Briefly described|9 Fig.4|Late Ordovician|Late Ordovician|||||||
11126|Malongulli Formation|23736|6|Mentioned|p16|||||||||
11126|Malongulli Formation|24265|5|Briefly described|p1445|Llanvirn|Arenig|Geological Province: Lachlan Fold Belt||||||
11126|Malongulli Formation|24266|5|Briefly described|p1471|Ordovician|Ordovician|Age: ~470-480 Ma. Geological Province: Lachlan Fold Belt.||||||
11126|Malongulli Formation|24268|6|Mentioned|p1536 Fig.2|||Geological Province: Lachlan Fold Belt||||||
11126|Malongulli Formation|24398|5|Briefly described|p259 Fig. 2|Bolindian|Eastonian|Overlies Cliefden Caves Limestone.  Geological Province: Lachlan Fold Belt.||||||
11126|Malongulli Formation|24417|6|Mentioned|p25|||||||||
11126|Malongulli Formation|29905|5|Briefly described|p6|||||||||
11126|Malongulli Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11126|Malongulli Formation|30072|6|Mentioned|p573|||||||||
11126|Malongulli Formation|32151|3|Fully described|p206|||See also p196. U.Eastonian. Refers Stevens (1952).||||||09-MAY-12
11126|Malongulli Formation|32590|3|Fully described|p15|||||||||
11126|Malongulli Formation|32591|6|Mentioned|p118|||||||||
11126|Malongulli Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
11126|Malongulli Formation|32672|6|Mentioned|p671|||||||||
11126|Malongulli Formation|33006|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle and Upper Ordovician.||||||07-SEP-18
11126|Malongulli Formation|33121|6|Mentioned|p85|||Correlation table. Late Ord.||||||
11126|Malongulli Formation|33125|6|Mentioned|p15|||Correlation chart||||||
11126|Malongulli Formation|33282|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle - Upper Ordovician.||||||07-SEP-18
11126|Malongulli Formation|33285|5|Briefly described|p43|||Middle Ord.||||||
11126|Malongulli Formation|33731|6|Mentioned|p612|||Trilobites - asaphids.||||||07-SEP-18
11126|Malongulli Formation|33733|6|Mentioned|p445|||||||||
11126|Malongulli Formation|33735|6|Mentioned|Fig.2|||||||||
11126|Malongulli Formation|33737|6|Mentioned|p168|||||||||
11126|Malongulli Formation|33740|6|Mentioned|p125|||||||||
11126|Malongulli Formation|33741|6|Mentioned|p246|||||||||
11126|Malongulli Formation|33764|4|Described|p712|||||||||
11126|Malongulli Formation|33875|6|Mentioned|p29|||Geological map, uranium prospects.||||||
11126|Malongulli Formation|34404|3|Fully described|p80|||||||||
11126|Malongulli Formation|34498|6|Mentioned|p150|||See also p155. Lower - Middle Ordovician||||||07-SEP-18
11126|Malongulli Formation|34575|6|Mentioned|p641|||See also pp642,644.||||||07-SEP-18
11126|Malongulli Formation|34576|6|Mentioned|p357|||Fauna||||||
11126|Malongulli Formation|35118|6|Mentioned|p426|||||||||
11126|Malongulli Formation|35258|6|Mentioned|p110|||||||||
11126|Malongulli Formation|35489|6|Mentioned|p91|||||||||
11126|Malongulli Formation|36534|6|Mentioned|p223|||||||||
11126|Malongulli Formation|37013|6|Mentioned|p11|||||||||
11126|Malongulli Formation|38219|6|Mentioned|p298|||See also Table 2.||||||
11126|Malongulli Formation|39214|5|Briefly described|p19|||||||||
11126|Malongulli Formation|39325|6|Mentioned|p431|||||||||
11126|Malongulli Formation|39331|6|Mentioned|p61|||See also p64.||||||07-SEP-18
11126|Malongulli Formation|39655|6|Mentioned|M1|||||||||
11126|Malongulli Formation|39657|6|Mentioned|Fig.1|||||||||
11126|Malongulli Formation|39663|6|Mentioned|Table 1|||||||||
11126|Malongulli Formation|40026|5|Briefly described|p245|||||||||
11126|Malongulli Formation|40127|6|Mentioned|p9|||||||||
11126|Malongulli Formation|40136|5|Briefly described|p30|||See also p15.||||||13-MAR-07
11126|Malongulli Formation|40328|6|Mentioned|p159|||||||||
11126|Malongulli Formation|40575|5|Briefly described|p3|||||||||
11126|Malongulli Formation|41046|6|Mentioned|p144|||||||||
11126|Malongulli Formation|41105|5|Briefly described|p230|||||||||
11126|Malongulli Formation|41108|5|Briefly described|p211|||||||||
11126|Malongulli Formation|42479|6|Mentioned|Fig. 2 P110|||||||||
11126|Malongulli Formation|42603|5|Briefly described|p56|||||||||
11126|Malongulli Formation|42612|5|Briefly described|p29, Figs 1&2, p30|||||||||
11126|Malongulli Formation|42802|5|Briefly described|p100|||||||||
11126|Malongulli Formation|43127|4|Described|p3,Fig.2,Fig.3||Ordovician|||||||
11126|Malongulli Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
11126|Malongulli Formation|43515|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(Provisional Edition) (M.-U.Ord)||||||
11126|Malongulli Formation|43516|14|Not recorded|Map Legend||Late Ordovician|(M.U.Ord)||||||
11126|Malongulli Formation|43548|2|Defined|p239-44,250-2,255,|Eastonian|Darriwilian|p260||||||
11126|Malongulli Formation|43569|6|Mentioned|p475||Late Ordovician|||||||
11126|Malongulli Formation|43571|6|Mentioned|p822||Eastonian|(Late Eastonian)||||||
11126|Malongulli Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
11126|Malongulli Formation|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Consists of calcareous and feldspathic siltstone, limestone, sandstone, conglomerate, mudstone.||||||15-JUL-08
11126|Malongulli Formation|43782|5|Briefly described|Map Legend|Bolindian|Eastonian|Of the Cabonne Group.||||||13-MAR-07
11126|Malongulli Formation|44086|14|Not recorded|p97-99,102,106||Early Ordovician|See also Lexicon. (Middle Ordovician)||||||
11126|Malongulli Formation|49794|6|Mentioned|p7|||||||||
11126|Malongulli Formation|60417|5|Briefly described|p155|Gisbornian|Darriwilian|Overlies Mount Pleasant Andesite. Overlain by Angullong Tuff.||||||
11126|Malongulli Formation|61893|6|Mentioned|p247-250|||Cliefden Caves. Faunal association described; compared with that of Jingerangle Formation.||||||
11126|Malongulli Formation|63121|5|Briefly described|p226|Late Ordovician|Late Ordovician|Of Percival (1978). Contains abundant spicules indicating presence of sponges.||||||13-MAR-07
11126|Malongulli Formation|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p152|Late Ordovician|Late Ordovician|Conformably overlian by Angullong Formation. Geological Province: Molong Volcanic Belt, LFB. Contains an early Bolindian graptolite assemblage in the uppermost beds.||||||07-FEB-11
11126|Malongulli Formation|63283|5|Briefly described|p195 Fig. 2, p199|Late Ordovician|Late Ordovician|Overlain by Angullong Formation, underlain by Cliefden Caves Limestone Subgroup. Geological Province: Molong Volcanic Belt. Consists of shale and siltstone.||||||07-FEB-11
11126|Malongulli Formation|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Bolindian|Bolindian|Underlain unconformably by Canomodine Limestone and Cliefden Caves Limestone Sub-group. Consists of calcareous and feldspathic sandstone, conglomerate and mudstone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
11126|Malongulli Formation|63287|4|Described|p317 Fig. 2, p322 Fig. 5, p334|Bolindian|Eastonian|Of Cabonne Gp. Confomably overlain by Millambri Fm and Angullong Fm, underlain by Regans Creek and Canomodine Lst, Cliefden Caves Lst.  Geol Prov: Molong volcanic Belt. Consists of grey-black laminated calcareous siltstones and fine-grained sandstones.||||||07-FEB-11
11126|Malongulli Formation|63290|5|Briefly described|p400 Fig. 5¿, p396 Fig. 3|Bolindian|Eastonian|Overlain by Angullong Formation, underlain by Cliefden Caves Limestone. Geological Province: Molong Volcanic Belt.||||||
11126|Malongulli Formation|63293|6|Mentioned|p469 Fig. 2|Bolindian|Eastonian|Overlain by Angullong Formation, underlain by Cliefden Caves Limestone Subgroup. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
11126|Malongulli Formation|64295|5|Briefly described|p200 Fig. 2, p204|||Overlies Cliefden Caves Limestone Subgroup. Contains allochthonous limestones.||||||01-SEP-08
11126|Malongulli Formation|67322|4|Described|Fig.5; p24|Hirnantian|Katian|Macquarie Arc. Stevens (1952). Contains diagnostic graptolite faunas close to its base (Eastonian) and top (Bolindian). Occurs in the Cliefden Caves region.||Of the Cabonne Group.||Overlies Vandon Limestone (Cliefden Caves Limestone Subgroup). Overlain by the Angullong Formation.|Siltstones and spiculites.|22-FEB-18
11126|Malongulli Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
11126|Malongulli Formation|70297|5|Briefly described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Post-phase 2 volcanic hiatus. Age: deposited from early to late Eastonian.||Cabonne Group||||
11126|Malongulli Formation|70684|5|Briefly described|p3, p18, p33-35, p41, p50, p75|Late Ordovician|Late Ordovician|Molong Volcanic Belt. Contains a prolific early Bolindian graptolite assemblage in its uppermost beds.||||Is overlain conformably by Angullong Formation.|Siltstone.|
11126|Malongulli Formation|70754|5|Briefly described|p447, p449-451, p455-461, p463-464|Late Ordovician|Late Ordovician|See also p466-475, p478-480. Numerous fossil species named, and age ranges shown. Systematic palaeontological descriptions.||||Overlies Cliefden Caves Limestone Subgroup. Is overlain by Angullong Formation.|Includes spiculites, graptolitic siltstones, and allochthonous limestone breccias containing high diversity lingulate faunas.|
11126|Malongulli Formation|71091|5|Briefly described|p141-143, p145-147, p153|Katian|Katian|Cliefden Caves district. Contains a diverse early Bolindian graptolite assemblage in its uppermost beds: species listed.||||Overlies Cliefden Caves Limestone Subgroup. Is overlain conformably by Angullong Formation. Correlated with Gunningbland Formation.||07-SEP-18
11126|Malongulli Formation|73208|5|Briefly described|p869, 872, 874-875|Late Ordovician|Late Ordovician|Contains fossils of nautiloids and graptolites, but is famous for its trilobite fauna in deep-water spiculites as well as deep-water sponge fauna in allochthonous limestones.||||Overlies Cliefden Caves Limestone Subgroup..||
11126|Malongulli Formation|73209|5|Briefly described|p879-885, 888|Late Ordovician|Late Ordovician|Contains a variety of important fossils (described).||||Overlies Vandon Limestone (Cliefden Caves Limestone Subgroup).|Deep-water, thinly-bedded, graptolitic laminites and allochthonous limestones. Includes calcareous and feldspathic siltstone, limestone, arenite, limestone breccia, and mudstone.|
11126|Malongulli Formation|73210|6|Mentioned|p893 Fig.2|||||||||
11126|Malongulli Formation|73492|5|Briefly described|p697, p704||||||||Contains allochthonous limestones, a lower limestone unit, and lower and upper limestone-breccia units.|
11159|Mandari Granodiorite|37986|2|Defined|p314|Early Devonian|Early Devonian|||||||
11183|Manilla Group|34555|4|Described|p238|||Formations described. See also PP239-241||||||
11183|Manilla Group|34590|6|Mentioned|p300|||||||||
11183|Manilla Group|37987|6|Mentioned|p214|||||||||
11183|Manilla Group|43344|14|Not recorded|p91||Devonian|||||||
11183|Manilla Group|43384|14|Not recorded|Map Legend||Late Devonian|||||||
11183|Manilla Group|43385|14|Not recorded|p174,175||Late Devonian|||||||
11183|Manilla Group|43397|14|Not recorded|p209,212||Late Devonian|||||||
11183|Manilla Group|43399|4|Described|p186,189,190,192||Late Devonian|||||||
11183|Manilla Group|43440|14|Not recorded|p38,fig4-3|||||||||
11183|Manilla Group|48600|14|Not recorded|Plate 3|||||||||
11186|Manning Group|22612|2|Defined|423,425,426,427,429|Early Permian|Early Permian|Geol province New England Orogen.||||||12-NOV-08
11186|Manning Group|22616|6|Mentioned|Fig.1 p670||Early Permian|||||||
11186|Manning Group|22736|6|Mentioned|p611 Fig2||Permian|||||||
11186|Manning Group|22857|4|Described|p512 App.1 Tb.A1.8|Early Permian|Early Permian|Diamictite, pebbly mudstone, conglomerate, mudstone, felsic and intermediate volcanics; biogenic limestone. Max. thickness: >5km. Geological Province: Barnard Basin.||||||
11186|Manning Group|23540|6|Mentioned|p 425|||||||||
11186|Manning Group|24008|6|Mentioned|p351 fig. 2|||||||||
11186|Manning Group|24040|5|Briefly described|p475, p482|Early Permian|Early Permian|Geological Province: Barnard Basin. Deposited in high energy, deep-marine sedimentary conditions (flysch sedimentation).||||||21-AUG-08
11186|Manning Group|31694|6|Mentioned|p345|||||||||
11186|Manning Group|34059|6|Mentioned|Map legend|Permian|Permian|||||||
11186|Manning Group|34556|4|Described|p266|||Permian||||||
11186|Manning Group|35129|6|Mentioned|p49|||||||||
11186|Manning Group|36961|6|Mentioned|Fig.5|||||||||
11186|Manning Group|38837|6|Mentioned|p233|||||||||
11186|Manning Group|39287|6|Mentioned|p13|||||||||
11186|Manning Group|41347|4|Described|Table 4|||||||||
11186|Manning Group|41348|5|Briefly described|Map legend|Permian|Permian|Includes: Cedar Party Limestone, Colraine Mudstone, Giro beds, Kimbriki Formation, Anderson Flat beds.  Diamictite, conglomerate, sandstone, mudstone, felsic and intermediate volcanics, and limestone.||||||16-DEC-04
11186|Manning Group|43017|5|Briefly described|Fig.1,p372|||||||||
11186|Manning Group|43385|14|Not recorded|p179,180||Sakmarian|Permian||||||
11186|Manning Group|43451|14|Not recorded|Map Legend|||||||||
11186|Manning Group|43755|6|Mentioned|Fig.1,p548||Permian|||||||
11186|Manning Group|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|In the Manning Basin. See also p 232 Appendix 1. Geological Province: New England Fold Belt.||||||15-MAR-05
11186|Manning Group|44447|5|Briefly described|p132, p133 Fig.2|Early Permian||Shale, siltstone, impure bioclastic limestone, diamictitic conglomerate and sandstone. Age: Early Permian (Tastubian)||||||
11186|Manning Group|44450|6|Mentioned|p20|||Geological Province: New England Fold Belt.||||||
11186|Manning Group|50014|5|Briefly described|p247|Permian|Permian|Geological Province: New England Fold Belt.||||||12-NOV-08
11186|Manning Group|50168|6|Mentioned|p156 Fig.1|Early Permian|Early Permian|Gamilaroi Terrane.|||||Diamictites.|
11186|Manning Group|61774|4|Described|p143-144|Early Permian|Early Permian|Sedimentary rocks occurring near Cooplacurripa; include breccias, conglomerates and diamictites.||||||
11186|Manning Group|61791|6|Mentioned|p326 Fig. 2|Permian|Carboniferous|In fig. 2 Group is Gp.||||||
11186|Manning Group|65114|5|Briefly described|p383 Tb.1|Cisuralian||Listed as Early Permian; 294-291 Ma; Tectonic unit: Southern New England Orogen, Barnard Basin, slivers in Texas Block||||||
11186|Manning Group|68005|5|Briefly described|p18, p22, p35, p57, p154, p170.|Early Permian|Early Permian|Southern New England Fold Belt. A deformed extensional marine sedimentary basin sequence.|||Includes Echo Hills Formation and Andersons Flat beds.||Diamictite, conglomerate, sandstone, mudstone, felsic and intermediate volcanics and limestone.|
11186|Manning Group|68006|6|Mentioned|p26.|Permian|Permian|Marine sediments.||||||
11186|Manning Group|68822|6|Mentioned|p327 Fig.7|Permian|Permian|||||||
11186|Manning Group|70217|5|Briefly described|p22|Early Permian|Early Permian|New England Orogen.||||Is intruded by the Barrington Tops Granodiorite.||
11186|Manning Group|70939|6|Mentioned|p826, p828|Permian|Permian|Northern Hastings Block.||||||
11186|Manning Group|71628|6|Mentioned|p6:18|||||||Is intruded by Gummi Plain Granodiorite.||
11186|Manning Group|73202|5|Briefly described|p625, p628-629, p637, p640|Early Permian|Late Carboniferous|New England Orogen, southern. Early Permian diamictites and mass-flow deposits regionally grouped together as the Manning Group (Mayer, 1972) or Barnard Beds (Allan and Leitch, 9990). Contains upper Carboniferous to lower Permian fossils (Price, 1973). Ca 288 Ma detrital zircon age is a maximum age of deposition in one of the larger southern basins (White et al., 2016). Serpentinite clasts described at the base of the Manning Group (Cross, 1983).|ca 288 Ma detrital zircon||Echo Hills Formation||Diamictites and mass-flow deposits filling strike-slip basins|
11186|Manning Group|73264|6|Mentioned|p1384 Fig.7|Early Permian|Early Permian|New England Orogen, southern.||||||
11186|Manning Group|73440|6|Mentioned|p126, p128-130, p132|Early Permian|Early Permian||||||Includes breccias and diamictites.|
11196|Manoora Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
11215|Manuka Subgroup|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Cretaceous|Late Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
11215|Manuka Subgroup|29591|6|Mentioned|p69|||||||||
11215|Manuka Subgroup|39445|6|Mentioned|Table 11|||||||||
11215|Manuka Subgroup|63979|5|Briefly described|p53|||Of Rolling Downs Group. Includes Mackunda and Winton Formations.||||||07-FEB-11
11215|Manuka Subgroup|69457|5|Briefly described|p41:6, 11-13|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga Basin.||Rolling Downs Group.|Mackunda and Winton Formations.|Overlies Wilgunya and Marree Subgroups.||12-JUL-16
11215|Manuka Subgroup|69673|6|Mentioned|p156||||||Includes Mackunda Formation, Winton Formation|Overlies Wilgunya Subgroup||
11229|Maradana Shale|5252|6|Mentioned|p66.||Lochkovian|Includes Lochkovian/early Gedinnian brachiopod fauna.||||||
11229|Maradana Shale|22768|6|Mentioned|p180|||||||||
11229|Maradana Shale|22857|5|Briefly described|p180, p454 App.1. Tb.A1.6|Silurian|Silurian|Of the Gregra Group. Tuffaceous muddy siltstone, shale, fine-grained feldspathic arenite. Overlain by Berkley Formation; overlies Goonigal Group. Equivalent to Cuga Burga Volcanics. Max. thickness: 300m.||||||
11229|Maradana Shale|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
11229|Maradana Shale|23170|2|Defined|p192|Lochkovian|Lochkovian|of Gregra Group.||||||
11229|Maradana Shale|23214|3|Fully described|p180|Lochkovian|Lochkovian|Of Gregra Group. Previously formed the upper part of Manilda Beds. Olive green to dark greyish brown coloured, laminated, calcareous shale. Max. thickness 300m.||||||
11229|Maradana Shale|23522|5|Briefly described|p248 Fig 4|Lochkovian|Lochkovian|||||||
11229|Maradana Shale|24248|6|Mentioned|p66|Lochkovian|Lochkovian|||||||
11229|Maradana Shale|24551|6|Mentioned|p619|||||||||
11229|Maradana Shale|31852|6|Mentioned|p718|||||||||
11229|Maradana Shale|32982|5|Briefly described|p657|||See also Fig.2||||||
11229|Maradana Shale|32983|6|Mentioned|p388|||||||||
11229|Maradana Shale|32984|6|Mentioned|p342|||Correlation chart||||||
11229|Maradana Shale|32985|6|Mentioned|Fig.2|||Correlation chart||||||
11229|Maradana Shale|32986|4|Described|p7|||See also PP1-51. Brachiopods.||||||
11229|Maradana Shale|33326|6|Mentioned|p430|||Fauna.||||||
11229|Maradana Shale|33732|5|Briefly described|p114|||||||||
11229|Maradana Shale|34478|6|Mentioned|p472|||Late Gedinnian||||||
11229|Maradana Shale|35283|6|Mentioned|p53|||||||||
11229|Maradana Shale|37727|6|Mentioned|Fig.1|||||||||
11229|Maradana Shale|38378|6|Mentioned|p133|||||||||
11229|Maradana Shale|40328|6|Mentioned|p82|||||||||
11229|Maradana Shale|42032|6|Mentioned|p494|||||||||
11229|Maradana Shale|42033|6|Mentioned|p651|||||||||
11229|Maradana Shale|43461|14|Not recorded|p620,table p621|Gedinnian|Ludlovian|||||||
11229|Maradana Shale|43494|4|Described|p22|Devonian|Devonian|Of the Gregra Group.  Mapped as "Murrabah Shale" by Maggs (1963). Renamed by Pickett (1982) to correlate with Maradana Shale of Savage (1969). Conformable over Wansey Fm. Est. thickness at wansey Creek: 450m.||||||16-MAR-06
11229|Maradana Shale|43640|5|Briefly described|Map Legend||Devonian|||||||
11229|Maradana Shale|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Gregra Group.||||||
11229|Maradana Shale|61859|5|Briefly described|p2-3, p5 Fig.2, p6-7, p10, p12-16,p21-22|||Manildra district. Coral fauna described. Deep-water sediments.||||Conformably and transitionally overlies the Goonigal Group. Conformably and gradationally underlies the Garra Limestone.|Richly fossiliferous shales and intercalations of thin, nodular limestones increasing up-section.|
11229|Maradana Shale|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Manildra. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
11229|Maradana Shale|66197|5|Briefly described|p633 Fig.4c|Lochkovian|Lochkovian|Cowra Trough-Molong High. Deep marine shale. Overlies the Wansey Formation.||||||13-MAR-12
11229|Maradana Shale|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Gregra Group||||19-MAY-16
11232|Maramingo Granite|23309|6|Mentioned|p436 App 1|||G31.||||||
11232|Maramingo Granite|30574|5|Briefly described|p10|||||||||
11232|Maramingo Granite|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11232|Maramingo Granite|35277|6|Mentioned|Fig.5.13|||||||||
11232|Maramingo Granite|35278|6|Mentioned|p359|||||||||
11232|Maramingo Granite|41641|6|Mentioned|Fig.5.13|||||||||
11232|Maramingo Granite|42726|5|Briefly described|map legend|Early Devonian||Variation on Maramingo Granite, Vic.||||||
11232|Maramingo Granite|42827|5|Briefly described|Fig 5.13|||||||||
11255|Marburg Subgroup|12597|5|Briefly described|p491, p492 Tb.1, p494, p501|Bathonian|Pliensbachian|Clarence-Moreton Basin. Appears as Marburg Formation on p496. Contains thin coal seams of no apparent commercial value in its lower parts.||Unit in Bundamba Group.|Includes Gatton Sandstone and Koukandowie Formation.|||
11255|Marburg Subgroup|13516|5|Briefly described|p159 fig 8|Jurassic|Jurassic|From Clarence-Moreton Basin.||Of Bundamba Group|Includes Gatton Sandstone, Koukandowie Formation|||
11255|Marburg Subgroup|22857|5|Briefly described|p318-9, p548 App. 1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Bundamba Group. Max. thickness: 1200m. Geological Province: Clarence-Moreton Basin. See also p548 App.1 Tb.A1.12.||||||
11255|Marburg Subgroup|22865|4|Described|p318,Fig22.9p317|||||||||
11255|Marburg Subgroup|23799|3|Fully described|p47|Early Jurassic|Early Jurassic|See also p10 Tb. 1.  Formerly Marburg Formation.  Currently defined to include Gatton Sandstone and Koukandowie Formation forming upper part of the Bundamba Group.  Overlies Woogaroo Group.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group.||||||11-DEC-07
11255|Marburg Subgroup|23811|5|Briefly described|Map Legend|||Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|23812|5|Briefly described|p33 Fig.6|||Of Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||27-AUG-08
11255|Marburg Subgroup|24237|5|Briefly described|p6 Fig.2|Early Jurassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Bundamba Group.||||||
11255|Marburg Subgroup|41631|4|Described|p14|||See also Fig.2 and Fig.4.||||||
11255|Marburg Subgroup|42248|1|Redefined|App.1 p409|Early Jurassic||Redefined from Marburg Formation.||||||27-SEP-18
11255|Marburg Subgroup|42463|6|Mentioned|Fig.3 P170|||||||||
11255|Marburg Subgroup|42869|5|Briefly described|Fig.2 P32|||||||||
11255|Marburg Subgroup|42894|5|Briefly described|Fig.1 P20|||||||||
11255|Marburg Subgroup|42951|5|Briefly described|Fig.11|||Of Bundamba Group.||||||11-DEC-07
11255|Marburg Subgroup|43150|5|Briefly described|Map Legend||Jurassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
11255|Marburg Subgroup|43736|6|Mentioned|p3|||||||||
11255|Marburg Subgroup|44450|5|Briefly described|p27|||Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Bundamba Group.  Includes: Gatton Sandstone, Koukandowie Formation.||||||
11255|Marburg Subgroup|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group. Geological Province: Moreton Basin||||||
11255|Marburg Subgroup|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Sandstone, conglomerate, siltstone, claystone, minor coal and basalt.||||||
11255|Marburg Subgroup|60281|5|Briefly described|p22, p27, Fig.18 App 1|Early Jurassic|Early Jurassic|Of the Bundamba Group. Includes the Gatton Sandstone and Koukandowie Formation.  Equivalent to the Evergreen Formation and Hutton Sandstone of the Surat Basin.  Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60993|3|Fully described|p17, p6 Fig. 2|||Of the Bundamba Group. Redefinition of constituent units within the group. Conformably overlain by Walloon Coal Measures. Conformably overlies the Woogaroo Subgroup. Geol. Prov: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60995|4|Described|p62-63, p51 Fig. 3|Early Jurassic|Early Jurassic|Of Bundamba Gp. Formerly referred to as the Marburg sequence ('formation', 'sandstone'). Geological Province: Clarence-Moreton Basin. Parts of the subgroup have been referred to as the Marburg sequence.||||||
11255|Marburg Subgroup|60996|5|Briefly described|p113 Fig. 64|||Includes the Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60997|5|Briefly described|p138, p142 Fig. 4|Bathonian|Sinemurian|Contains quartzo-feldspathic to quartz-lithic sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2.||||||
11255|Marburg Subgroup|60998|5|Briefly described|p144, p146 Fig. 2|||Includes the Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|60999|5|Briefly described|p164|Early Jurassic||Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|61004|5|Briefly described|p230|||Of the Bundamba Group. Includes the Gatton Sandstone and Koukandowie Formation. Contains high vitrinite and relatively low liptinite contents. Geological Province: Clarence-Moreton Basin.||||||08-MAY-13
11255|Marburg Subgroup|61006|5|Briefly described|p277, p278 Fig. 2|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.||||||
11255|Marburg Subgroup|61310|5|Briefly described|p14 Fig. C5|||Part of Bundamba Group (as Marburg Subgroup)? Or overlies the Bundamba Group? Overlain by Walloon Coal Measures. Geological Province: Clarence-Moreton Basin||||||
11255|Marburg Subgroup|63729|5|Briefly described|Map legend|Jurassic|Jurassic|Underlies Walloon Coal Measures; upper section interfingers with Kumbarilla beds. Medium- to coarse-grained quartzose and quartzofeldspathic sandstone and conglomerate.||||||11-DEC-07
11255|Marburg Subgroup|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Includes the Gatton Sandstone and Walloon Coal Measures.||||||12-DEC-07
11255|Marburg Subgroup|63732|5|Briefly described|Map legend||Jurassic|Fine- to medium-grained, highly porphyritic (titanite-biotite-) hornblende diorite; with numerous phenocrysts of plagioclase to ~1.5cm and brown hornblende to ~5mm.||||||
11255|Marburg Subgroup|63733|5|Briefly described|Map legend|Jurassic|Jurassic|Medium to coarse-grained quartzose and quartzofeldspathic sandstone and conglomerate.||||||
11255|Marburg Subgroup|63748|6|Mentioned|p19, p21-22|Jurassic|Jurassic|Upper part of Bundamba Group. Includes Gatton Sandstone. Overlies the Woogaroo Subgroup. In Warwick area, unconformably overlain by Main Range Volcanics, conformably overlain by Walloon Coal Measures.  See also p7 Fig. 3.||||||07-FEB-11
11255|Marburg Subgroup|64289|5|Briefly described|p6 Fig. 2, p17. p18|Middle Jurassic|Early Jurassic|Of the Woogaroo Subgroup (Bundamba Group). Includes Gatton Sandstone and Koukandowie Formation (and its two members). Geological province: Clarence-Moreton Basin. Hosts Plensbachian-Toarcian flora; fragmentary vertebrate remains occur also.||||||07-FEB-11
11255|Marburg Subgroup|64665|5|Briefly described|p53 Fig.2, p59.|Middle Jurassic|Early Jurassic|Clarence-Moreton and Southern Nambour Basins. Includes thin, uneconomic coals.||Upper unit in Bundamba Group.|Includes Gatton Sandstone, Koukandowie Formation, the upper part of Landsborough Sandstone, and Brighton beds.|Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|64856|5|Briefly described|p86|||Moreton Basin unit. Hutton Sandstone is laterally continuous into the upper part of this Subgroup. Shown as Marburg Sub-Group.|| ||||31-JAN-13
11255|Marburg Subgroup|65388|6|Mentioned|p213|||Moreton Basin.  Lower part laterally continuous with Evergreen Formation, Surat Basin.||||||
11255|Marburg Subgroup|67402|6|Mentioned|p187|||Clarence-Moreton Basin.||Bundamba Group|Includes the Gatton Sandstone and the Koukandowie Formation.|||
11255|Marburg Subgroup|68135|6|Mentioned|p64|||Lowood area, Clarence-Moreton Basin. Contains the late Early to early Middle Jurassic labyrinthodont amphibian, Austropelor, Longman, 1941.||||||
11255|Marburg Subgroup|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Bundamba Group, the Woogaroo Subgroup, and Landsborough Sandstone, are all mapped under the symbol, RJb.||Unit in Bundamba Group.||||
11255|Marburg Subgroup|68679|5|Briefly described|p452-453, p455|Jurassic|Jurassic|||||Unconformably overlies the Eight Mile Creek, Condamine and Rhyolite Range beds.||
11255|Marburg Subgroup|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
11255|Marburg Subgroup|69594|5|Briefly described|p519, p535-536, p543-545, p547|||Clarence-Moreton Basin and southern Nambour Basin. Meandering stream deposits.||Bundamba Group.|Koukandowie Formation, Gatton Sandstone, Brighton beds.|Overlies Woogaroo Subgroup. Is overlain transitionally by Walloon Coal Measures. Part-equivalent to the Evergreen Formation and Hutton Sandstone.||
11255|Marburg Subgroup|69639|6|Mentioned|p192, p222|Jurassic|Jurassic|||||Overlies the Cullendore Granite.||
11255|Marburg Subgroup|69790|5|Briefly described|p1063 Fig.2, p1076|Middle Jurassic|Early Jurassic|Northern Clarence-Moreton Basin area.||Unit in Bundamba Group.|Includes Gatton Sandstone and Koukandowie Formation.|||
11255|Marburg Subgroup|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Bundamba Group.|Gatton Sandstone, Koukandowie Formation.|Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|71628|5|Briefly described|p15: 34, 70; p16-4|Jurassic|Jurassic|Clarence-Moreton Basin. Appears as Marburg Supergroup on p15-34.|||Koreelah Conglomerate Member.|Locally overlies Cullendore Syenogranite and units of the Stanthorpe Complex.||
11255|Marburg Subgroup|71805|5|Briefly described|p76|Early Jurassic|Early Jurassic|Clarence-Moreton Basin.||Bundamba Group|Includes the Gatton Sandstone and the Koukandowie Formation.|||15-MAY-19
11255|Marburg Subgroup|72297|5|Briefly described|p726, p746|||Clarence-Moreton Basin. Quarried near Warwick and Yangan: coarse sandstone for landscaping; fine for tiles, sculpture and building stone. Carbonaceous shales may form hydrocarbon source rocks.|||Heifer Creek Sandstone Member.||Fine to coarse sandstones.|
11255|Marburg Subgroup|72298|6|Mentioned|p798|||Permeable sandstone beds in this unit are groundwater aquifers in the Ma Ma Creek catchment (Lockyer Valley).||||||
11255|Marburg Subgroup|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||Underlies the Walloon Coal Measures.||
11255|Marburg Subgroup|73306|5|Briefly described|p566-567, 569-570|Jurassic|Jurassic|Clarence-Moreton Basin. It is displaced by several minor normal faults.||Bundamba Group.||Overlies Woogaroo Subgroup. Is overlain by Walloon Coal Measures.||
11255|Marburg Subgroup|73570|5|Briefly described|p914|Early Jurassic|Early Jurassic|Clarence-Morton Basin. See also Marburg Group p915 Fig.4.|||Gatton Sandstone|||
11328|Marks Point Conglomerate|23055|6|Mentioned|Fig9p17|||||||||
11328|Marks Point Conglomerate|41463|6|Mentioned|Fig.1|||||||||
11329|Markwell Coal Measures|22857|4|Described|p536 App.1 Tb.A1.9|Early Permian|Early Permian|Pebble to boulder conglomerate with clasts of felsic volcanics; lenses of crossbedded sandstone and lenses of coal. Max. thickness: 18m. Geological Province: Sydney Basin.||||||
11329|Markwell Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
11329|Markwell Coal Measures|32836|5|Briefly described|p7|||Low in Permian||||||
11329|Markwell Coal Measures|32868|6|Mentioned|p210|||||||||
11329|Markwell Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
11329|Markwell Coal Measures|34556|4|Described|p267|||Permian||||||
11329|Markwell Coal Measures|36057|6|Mentioned|p350|||Refers Engel 1962. See also Fig.2.||||||
11329|Markwell Coal Measures|39266|6|Mentioned|p225|||||||||
11329|Markwell Coal Measures|39306|6|Mentioned|p396|||||||||
11329|Markwell Coal Measures|41054|6|Mentioned|p156|||||||||
11329|Markwell Coal Measures|42182|6|Mentioned|p303|||||||||
11329|Markwell Coal Measures|42833|5|Briefly described|p227|||Time equivalents of Alum Mountain Volcanics||||||
11329|Markwell Coal Measures|43447|14|Not recorded|Table 1,p14,28,39||Permian|||||||
11329|Markwell Coal Measures|43451|14|Not recorded|Map Legend|||||||||
11329|Markwell Coal Measures|44093|5|Briefly described|p231 App. 1|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||15-MAR-05
11329|Markwell Coal Measures|44244|2|Defined|p228|Early Permian|Early Permian|Disconformably overlies the Alum Mountain Volcanics; disconformably underlies the Bulahdelah Formation.  Max. thickness: 18m.  Type section in text.  Geological Province: Myall Block.||||||16-SEP-04
11329|Markwell Coal Measures|47056|6|Mentioned|Fig.2 P523|||||||||
11329|Markwell Coal Measures|50263|5|Briefly described|Map Legend|Artinskian|Sakmarian|Geological Province: Eastern Myall Block.  Overlies: Lakes Road Rhyolite Member (u).||||||
11364|Marrangaroo Conglomerate|22578|4|Described|Fig.3 p393, p398|||||||||
11364|Marrangaroo Conglomerate|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Cullen Bullen Subgroup (Illawarra Coal Measures). Quartz sandstone, pebbly coarse-grained. Max. thickness: 4m. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
11364|Marrangaroo Conglomerate|22969|5|Briefly described|p 24|||||||||
11364|Marrangaroo Conglomerate|23214|4|Described|p268|Late Permian|Late Permian|Of Illawarra Coal Measures.  Consists of medium to coarse grained pebbly, quartz-lithic sandstone with minor mudstone beds.  Maximum thickness: 20m.  Geological Province: Sydney Basin.||||||
11364|Marrangaroo Conglomerate|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
11364|Marrangaroo Conglomerate|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: upper Erins Vale Formation. Underlies: Woonona Coal Member.||||||
11364|Marrangaroo Conglomerate|24471|5|Briefly described|p31 Fig.3|Late Permian|Late Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
11364|Marrangaroo Conglomerate|29751|6|Mentioned|Fig.3|||||||||
11364|Marrangaroo Conglomerate|31855|6|Mentioned|p14|||Stratigraphic table||||||
11364|Marrangaroo Conglomerate|34040|4|Described|p384|||Perm. Base of coal measures.||||||13-AUG-15
11364|Marrangaroo Conglomerate|34156|6|Mentioned|p387|||Permian||||||
11364|Marrangaroo Conglomerate|34204|6|Mentioned|p65|||||||||
11364|Marrangaroo Conglomerate|34205|4|Described|p13|||Charbon Sub-group||||||
11364|Marrangaroo Conglomerate|34569|6|Mentioned|p9|||See also P10. Permian.||||||
11364|Marrangaroo Conglomerate|37093|6|Mentioned|p233|||||||||
11364|Marrangaroo Conglomerate|39232|4|Described|p108|||||||||
11364|Marrangaroo Conglomerate|39293|6|Mentioned|p139|||See also Fig.8.2||||||
11364|Marrangaroo Conglomerate|39308|6|Mentioned|p503|||||||||
11364|Marrangaroo Conglomerate|40256|6|Mentioned|Fig.3|||||||||
11364|Marrangaroo Conglomerate|40321|6|Mentioned|p19|||||||||
11364|Marrangaroo Conglomerate|40330|6|Mentioned|p66|||||||||
11364|Marrangaroo Conglomerate|40332|6|Mentioned|Fig.4|||||||||
11364|Marrangaroo Conglomerate|40806|2|Defined|p152|Permian|Permian|Prob. Permian||||||
11364|Marrangaroo Conglomerate|41123|6|Mentioned|p178|||||||||
11364|Marrangaroo Conglomerate|42182|6|Mentioned|p299|||||||||
11364|Marrangaroo Conglomerate|42284|6|Mentioned|p106|||||||||
11364|Marrangaroo Conglomerate|42310|5|Briefly described|p210|||||||||
11364|Marrangaroo Conglomerate|42379|5|Briefly described|p210|||||||||
11364|Marrangaroo Conglomerate|42657|4|Described|p75|||||||||
11364|Marrangaroo Conglomerate|42787|5|Briefly described|p129|||see also Table 1 P126||||||
11364|Marrangaroo Conglomerate|42896|6|Mentioned|p20|||||||||
11364|Marrangaroo Conglomerate|42947|5|Briefly described|p47|||||||||
11364|Marrangaroo Conglomerate|42948|6|Mentioned|p50|||||||||
11364|Marrangaroo Conglomerate|43146|6|Mentioned|Fig.2 p41|||of Illawarra Coal Measures.||||||
11364|Marrangaroo Conglomerate|43194|5|Briefly described|p111, p129 Tb. 8.3|Late Permian|Late Permian|Western Coalfield, Sydney Basin. Of Illawarra Coal Measures. A lithological correlative of a lower quartz-rich sandstone unit (now formally named as Brigalow Formation) within the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
11364|Marrangaroo Conglomerate|43317|4|Described|Table 1 p10|||||||||
11364|Marrangaroo Conglomerate|43318|14|Not recorded|opp p6||Permian|||||||
11364|Marrangaroo Conglomerate|43320|14|Not recorded|Table 1 p10||Triassic|Part of Illawarra Coal Measures, Occurs at base of Sydney Sub Group||||||
11364|Marrangaroo Conglomerate|43344|14|Not recorded|p21,173||Permian|Western Coalfield||||||
11364|Marrangaroo Conglomerate|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Charbon Sub-Group of Illawarra Coal Measures||||||
11364|Marrangaroo Conglomerate|43362|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Charbon Sub-Group of Illawarra Coal Measures||||||
11364|Marrangaroo Conglomerate|43477|14|Not recorded|p25,26,57,58|||See also Lexicon. (Lithgow Coal Measures)||||||
11364|Marrangaroo Conglomerate|43641|5|Briefly described|Map Legend||Permian|||||||
11364|Marrangaroo Conglomerate|43782|6|Mentioned|Map diagram|Late Permian|Late Permian|of Illawarra Coal Measures.||||||
11364|Marrangaroo Conglomerate|45090|6|Mentioned|p221|||Kazanian||||||
11364|Marrangaroo Conglomerate|60281|5|Briefly described|p61-62|Late Permian|Late Permian|Fluvial, pebbly sandstone to cobble conglomerate.  Overlaps the Wallis Creek Formation in the west where it thins out.  Numerous hydrocarbon shows recorded.  Geological Province: Sydney Basin.||||||
11364|Marrangaroo Conglomerate|61315|5|Briefly described|p180|Late Permian|Late Permian|Of the lower part of Illarawarra Coal Measures. Good reservoir potential. Geological Province: Sydney Basin||||||
11364|Marrangaroo Conglomerate|61529|6|Mentioned|p868|||Geological Province: Sydney Basin.||||||
11364|Marrangaroo Conglomerate|65116|6|Mentioned|p447|||In the Sydney Basin. Sequence boundary at base.||||||
11364|Marrangaroo Conglomerate|67663|6|Mentioned|p520 Tb.1|Permian|Permian|Late Permian.||Of the Illawarra Coal Measures.||||
11364|Marrangaroo Conglomerate|68003|5|Briefly described|p38 Fig.3-j, p41.|Late Permian|Late Permian|Western Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Referred to on p41 as "Marrangaroo and Blackmans Flat Formations" (sic). Alluvial deposits sourced from Lachlan Fold Belt.||Unit in Cullen Bullen Subgroup.||Overlies Nile Subgroup.||
11364|Marrangaroo Conglomerate|70661|6|Mentioned|p189|||||Illawarra Coal Measures||||
11364|Marrangaroo Conglomerate|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
11375|Marriangaah Siltstone|32672|6|Mentioned|p672|||||||||
11376|Marsden Park breccia|40263|6|Mentioned|Table 2|||||||||
11376|Marsden Park breccia|60299|6|Mentioned|p228 Tb.5|||Informal. Palaeopole position given.||||||
11385|Martins Creek Ignimbrite Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of Isismurra Formation; continues into Gresford Block as andesitic ignimbrite member at base of Newtown Formation. Age: 326+/-9Ma, 330+/-10Ma and 335Ma (K/Ar). Max. thickness: 35m. Geological Province: Tamworth Forearc Basin.||||||03-MAR-06
11385|Martins Creek Ignimbrite Member|24121|5|Briefly described|p4, p83, p151, 159|||Of Newtown Formation.||||||25-AUG-22
11385|Martins Creek Ignimbrite Member|31228|3|Fully described|p81|||||||||
11385|Martins Creek Ignimbrite Member|36528|6|Mentioned|p169|||||||||
11385|Martins Creek Ignimbrite Member|43576|6|Mentioned|p351|||||||||
11385|Martins Creek Ignimbrite Member|44093|5|Briefly described|p228 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
11385|Martins Creek Ignimbrite Member|44244|4|Described|p37-38, p90|Visean|Visean|Of the Isismurra Formation.  Overlies the Wallaringa Formation. Age: ~331Ma. Max. thickness: 45m. Type section in text. Geological Province: Gresford and Rouchel Blocks.||||||27-MAY-08
11385|Martins Creek Ignimbrite Member|50099|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Ashflow tuff. Age: 331 Ma. Geological Province: Tamworth Belt/New England Orogen.||||||
11385|Martins Creek Ignimbrite Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Newtown Formation (Gilmore Volcanic Group).  Blue-grey, red-mottled  welded andesitic ignimbrite with minor interbeds of beige to grey dacitic ignimbrite.  Geological Province: Gresford Block||||||
11385|Martins Creek Ignimbrite Member|50268|5|Briefly described|Map Legend|Visean|Visean|Overlies: Isismurra Formation, Wallaringa Formation, Flagstaff Formation. Of the Newtown Formation. Underlies: Isismurra Formation.||||||27-MAY-08
11385|Martins Creek Ignimbrite Member|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Of Isismurra Formation. Age: 332 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Gresford Block||||||
11385|Martins Creek Ignimbrite Member|61768|6|Mentioned|p82, p83 Fig. 2|||Of Newtown Fromation. Age: 332.3+/-2.2Ma (Roberts et al. 1995).||||||13-MAY-08
11385|Martins Creek Ignimbrite Member|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|Of the Isismurra Formation. Geological Province: Rouchel Block/Tamworth Belt.||||||
11385|Martins Creek Ignimbrite Member|65107|5|Briefly described|p275, 276, 282, Fig 4 p279, Fig 9 p283|Visean|Visean|AGE: 332.2+/-2.2Ma from SHRIMP U-Pb zircons, are not included as points in this study, Paleopole positions are much further east than other constraining units, this may be due to the rotation of Gresford block or magnetisations in the ignimbrite.||||||
11385|Martins Creek Ignimbrite Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Isismurra Formation||||
11385|Martins Creek Ignimbrite Member|73487|6|Mentioned|p566-567, p577|Visean|Visean|Rouchel and Gresford blocks. Rhipidomella fortimuscula zone.|ca 332 Ma|||||
11390|Marulan Granite|22857|6|Mentioned|p179|Middle Devonian|Early Devonian|||||||21-JAN-21
11390|Marulan Granite|29989|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
11390|Marulan Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
11390|Marulan Granite|30329|6|Mentioned|p30|||On table p30.||||||19-JUN-08
11390|Marulan Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
11390|Marulan Granite|30734|6|Mentioned|p54|||||||||
11390|Marulan Granite|32483|4|Described|p34|||Middle Devonian? Strat. table 1.||||||19-JUN-08
11390|Marulan Granite|32708|6|Mentioned|Fig.1|||||||||
11390|Marulan Granite|32999|6|Mentioned|p38|||Structural relationships||||||
11390|Marulan Granite|33004|6|Mentioned|p193|||||||||
11390|Marulan Granite|36390|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11390|Marulan Granite|36600|6|Mentioned|Table 1|||||||||
11390|Marulan Granite|38335|6|Mentioned|p1730|||||||||
11390|Marulan Granite|39331|6|Mentioned|Fig.0-3|||See also Fig.7-3||||||
11390|Marulan Granite|39568|5|Briefly described|p78|||||||||
11390|Marulan Granite|40328|4|Described|p208|||||||||
11390|Marulan Granite|41563|6|Mentioned|p511|||||||||
11390|Marulan Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
11390|Marulan Granite|50234|5|Briefly described|Map Legend|Pragian|Pragian|Part of the Marulan Batholith.||||||
11390|Marulan Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Arthursleigh Suite. Pinkish-grey, medium-grained, equigranular to strongly porphyritic, hornblende-biotite granite. High magnetic response.||||||
11390|Marulan Granite|66300|5|Briefly described|p76, 81, 85.|||This age is indistinguishable from that of the Barrallier Ignimbrite and the Newacres Ignimbrite Member.|416.7 +/- 3.1 Ma.|Unit in Arthursleigh Suite.||||29-OCT-13
11390|Marulan Granite|68592|2|Defined|p241, p261, p269, p271, p1634-8|Early Devonian|Early Devonian|Initially mapped as a distinct pluton by Carr (unpublished data); subsequently shown as such on the Lachlan Fold Belt granite map (Chappell et al. (1991) as a unit in the Arthursleigh Suite (Chappell, 1992). No previous type area: one is defined herein. Crops out as boulders and small tors in a subdued landscape. Geochemistry and geophysical properties briefly described. A SHRIMP U-Pb zircon age of 416.7 +/- 3.1 Ma (Black, 2005) does not accord with established palaeontologic constraints.||Unit in Arthursleigh Suite.||Intrudes Kerrawarra Dacite Member, Joaramin and Barrallier Ignimbrites (Bindook Group).|Uniform internal composition. Pinkish/grey coarsely equigranular granite, with a strongly porphyritic phase in the southern end. I-type.|
11390|Marulan Granite|70125|5|Briefly described|p392-p393, p396 Fig.9|||Lachlan Orogen. Sediment is transported to the coast by the Shoalhaven River.|417 Ma Bodorkos et al., 2010).|||||14-MAY-20
11390|Marulan Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dam. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.||Arthursleigh Suite|||Pinkish grey, coarse-grained, equigranular to strongly porphyritic, hornblende biotite and biotite granite. High magnetic susceptibility.|
11390|Marulan Granite|70296|5|Briefly described|p1, p11, p13, p24|||Goulburn-Yass district.|416.7 +/- 3.1 Ma (SHRIMP U-Pb)|||||21-JAN-21
11390|Marulan Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Arthursleigh Suite|||Pinkish grey, coarse-grained, equigranular to strongly porphyritic, hornblende biotite and biotite granite. High magnetic susceptibility.|
11390|Marulan Granite|70661|3|Fully described|p76, p79 fig 6, p83-p85|Lochkovian|Pridoli|Named after the township of Marulan. Originally included as part of the undifferentiated Marulan Batholith. Distribution, structure, metamorphism, geochemistry and geophysical characteristics discussed. Correlated with other plutons of the Arthursleigh Suite. Quarried for dimension stone in Moss Vale. Is distinguished from Glenrock Granodiorite by its more felsic characteristics.|416 +/- 7 Ma (SHRIMP)|Arthursleigh Suite||Intrudes Kerrawarra Dacite Member, Joaramin Ignimbrite, Barralier Ignimbrite|Contains pinkish grey/coarsely equigranular and strongly porphyritic granite phases. Composed of 35-40% anhedral quartz crystals, 30% stumpy plagioclase, 20-25% microperthitic orthoclase, 4-5% hornblende, biotite and accessory opaques.|
11390|Marulan Granite|71303|5|Briefly described|map legend|Pragian|Pragian|||Of Arthursleigh Suite.|||Pinkish-grey granite, mostly coarsely equigranular but with strongly porphyritic phases locally.|
11417|Maryland Granite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
11417|Maryland Granite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
11417|Maryland Granite|32492|6|Mentioned|Map legend|Triassic|Late Permian|Upper Permian or Triassic||||||
11417|Maryland Granite|32876|6|Mentioned|Map legend|Early Triassic|Late Permian|Upper Permian to Lower Triassic.||||||27-OCT-08
11417|Maryland Granite|32880|4|Described|p3|||See also p11. Upper Permian or Lower Triassic.||||||12-DEC-07
11417|Maryland Granite|33476|2|Defined|p70|Permian|Permian|Mention p50. Permian - Triassic||||||19-NOV-07
11417|Maryland Granite|33766|6|Mentioned|Map legend|Early Triassic|Permian|Permian - Early Triassic||||||
11417|Maryland Granite|35257|6|Mentioned|Fig.5|||||||||
11417|Maryland Granite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
11417|Maryland Granite|43008|5|Briefly described|map legend|||||||||
11417|Maryland Granite|44625|14|Not recorded|p383|||||||||
11417|Maryland Granite|48940|5|Briefly described|p70|||Refers Saint-Smith (1911).||||||27-OCT-08
11417|Maryland Granite|61789|5|Briefly described|p306|||Mineralogically separate to Maryland River Quartz Monzogranite. Has abundant mafic enclaves.||||||
11417|Maryland Granite|63732|5|Briefly described|Map legend|Early Triassic|Late Permian|Medium grey, medium-grained, uneven-grained to slightly porphyritic (allanite-titanite-) hornblende-biotite monzogranite; mafic inclusions common; high magnetic response.||||||11-DEC-07
11417|Maryland Granite|63748|3|Fully described|p35, p42|Late Permian|Permian|The only granite in the Maryland Suite. Intrudes Silverwood Group, faulted against Stanthorpe Granite; unconformably overlain by Marburg Formation. Medium grey, medium-grained, uneven grained to slightly porphyritic monzogranite. See also p29 Fig. 33, p86||||||07-FEB-11
11417|Maryland Granite|69639|4|Described|p1, p6, p8, p74, p151-p156|Lopingian|Lopingian|New England Orogen. SHRIMP age is interpreted as a magmatic crystallisation age. Sample locality, petrography, and geochronology is described. See also p217, p220, p222, p238.|252.4 +/- 1.5 Ma|Maryland Suite||Intrudes the Silverwood Group. Faulted against and intruded by the Stanthorpe Granite. Intruded by the Cullendore Granite.|Grey, medium-grained, equigranluar granodiorite.|
11417|Maryland Granite|70876|5|Briefly described|p81|||Provided age is a SHRIMP U-Pb zircon date; an additional Rb-Sr biotite age of c. 242 Ma is provided from Shaw and Flood (1993).|252.4 +/- 1.5 Ma (Chisholm et al, 2014b)|||||
11417|Maryland Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|252+/-1.5 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granodiorite.|
11417|Maryland Granite|71628|6|Mentioned|p19:97|||Flood (1970). After several variations, is now Maryland Granodiorite.||||||
11419|Marylebone Dolerite|33061|3|Fully described|p26|||Post U.Sil.||||||
11472|Maules Creek Formation|721|5|Briefly described|Map legend|Artinskian|Artinskian|Basal carbonaceous claystone, pelletoidal clay sandstone, minor coal, passing upward into upward-fining cycles of sandstone, thinly bedded siltstone/sandstone and coal; conglomerate dominant toward top.   Geological Province: Gunnedah Basin.||||||
11472|Maules Creek Formation|22500|5|Briefly described|p 7||Early Permian|Gunnedah Basin||||||
11472|Maules Creek Formation|22579|5|Briefly described|p217|Early Permian|Early Permian|||||||
11472|Maules Creek Formation|22609|5|Briefly described|Table 1||Early Permian|||||||
11472|Maules Creek Formation|22610|6|Mentioned|p 123|||||||||
11472|Maules Creek Formation|22857|4|Described|p520 App.1 Tb.A1.9, p315 Fig.22.8|Early Permian|Early Permian|Of the Bellata Group. Basal carbonaceous claystone, pelletoidal clay sandstone, minor coal (Brown seam), passing up into sandstone, thinly bedded siltstone/sandstone and coal. Max. thickness: >800m. Geological Province: Gunnedah Basin.||||||
11472|Maules Creek Formation|22865|6|Mentioned|Fig22.8p315|||||||||
11472|Maules Creek Formation|23050|5|Briefly described|p9 Fig.2|Late Permian|Late Permian|||||||
11472|Maules Creek Formation|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Parent: Bellata Group. Geological Province: Gunnedah Basin||||||
11472|Maules Creek Formation|23740|5|Briefly described|p1221|Permian|Permian|Geological Province: Gunnedah Basin.||||||17-SEP-08
11472|Maules Creek Formation|24159|5|Briefly described|p150 Fig.3, p149|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Overlying Unit: Porcupine Formation. Underlying Unit: Goonbri Formation.||||||
11472|Maules Creek Formation|24241|5|Briefly described|p19 Fig.4|Early Permian|Early Permian|||||||
11472|Maules Creek Formation|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
11472|Maules Creek Formation|24603|5|Briefly described|p869 Fig. 4c|Permian|Permian|Geological Province: Tamworth Belt.||||||
11472|Maules Creek Formation|36940|2|Defined|p156|Early Permian|Early Permian|||||||
11472|Maules Creek Formation|37856|6|Mentioned|p2|||||||||
11472|Maules Creek Formation|38089|4|Described|p8|||||||||
11472|Maules Creek Formation|38614|4|Described|p5|||||||||
11472|Maules Creek Formation|38958|5|Briefly described|p490|||||||||
11472|Maules Creek Formation|39063|4|Described|p11|||See also Fig.3.||||||
11472|Maules Creek Formation|39572|6|Mentioned|p134|||||||||
11472|Maules Creek Formation|39693|6|Mentioned|p14|||||||||
11472|Maules Creek Formation|39913|4|Described|p4|||||||||
11472|Maules Creek Formation|40176|6|Mentioned|Fig.2|||||||||
11472|Maules Creek Formation|40200|4|Described|p5|||||||||
11472|Maules Creek Formation|40332|6|Mentioned|Fig.3|||||||||
11472|Maules Creek Formation|40680|6|Mentioned|Fig.1|||||||||
11472|Maules Creek Formation|40767|4|Described|p4|||||||||
11472|Maules Creek Formation|40952|4|Described|p5|||||||||
11472|Maules Creek Formation|41130|6|Mentioned|p44|||||||||
11472|Maules Creek Formation|41226|6|Mentioned|p22|||||||||
11472|Maules Creek Formation|41229|6|Mentioned|p1|||||||||
11472|Maules Creek Formation|41264|6|Mentioned|p252|||||||||
11472|Maules Creek Formation|41290|4|Described|p225|||||||||
11472|Maules Creek Formation|41451|6|Mentioned|p5|||||||||
11472|Maules Creek Formation|41689|6|Mentioned|Table 1|||||||||
11472|Maules Creek Formation|41990|5|Briefly described|p8|||||||||
11472|Maules Creek Formation|42182|5|Briefly described|p300|||||||||
11472|Maules Creek Formation|42284|5|Briefly described|Fig.11 P104|||||||||
11472|Maules Creek Formation|42463|6|Mentioned|Fig.6 P173|||||||||
11472|Maules Creek Formation|42526|6|Mentioned|Map legend|||||||||
11472|Maules Creek Formation|42648|6|Mentioned|p38|||||||||
11472|Maules Creek Formation|42679|5|Briefly described|Fig.3 P3|||||||||
11472|Maules Creek Formation|42680|6|Mentioned|p19|||||||||
11472|Maules Creek Formation|43017|5|Briefly described|Fig.2,p374|||||||||
11472|Maules Creek Formation|43091|5|Briefly described|Map legend|||Of Gunnedah Basin.||||||17-SEP-08
11472|Maules Creek Formation|43194|1|Redefined|p98 Tb. 8.2, p99-103, p133 App. 1|Early Permian|Early Permian|See also references on p95, p97, p128, p129 Tb.8.3. Now of Bellata Group. Overlies and onlaps Leard and Goonbri Formations.  Underlies Porcupine Formation and Digby Formation. Equivalent to Rowan Formation (Sydney Basin). Assigned Upper to Lower Stage 4 palynological age.||||||
11472|Maules Creek Formation|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
11472|Maules Creek Formation|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin.  Of the Bellata Group. Underlies: Porcupine Formation.  Overlies: Leard Formation.||||||05-JUL-04
11472|Maules Creek Formation|60294|5|Briefly described|p123|||Includes carbonaceous shales. Geological Province: Maules Creek Sub-basin, Gunnedah Basin.||||||
11472|Maules Creek Formation|61313|5|Briefly described|p85, p94 Fig. G7|Early Permian|Early Permian|A major alluvial system characterised by an abundance of cobble and granule conglomerate with subordinate sandstone, siltstone, claystone and coal. Overlies Goonbri Formation. Max.thickness: 100m in Maules Creek Sub-basin. Geol. Prov: Gunnedah Basin.||||||
11472|Maules Creek Formation|61377|5|Briefly described|p149 Fig. SU8|Early Permian|Early Permian|Geological Province: Gunnedah Basin. See also p154 Fig. SU9.||||||07-FEB-11
11472|Maules Creek Formation|61612|6|Mentioned|p270, p272, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
11472|Maules Creek Formation|61772|6|Mentioned|p128 Fig. 2, p130||Early Permian|In New England Orogen.||||||17-SEP-08
11472|Maules Creek Formation|61776|5|Briefly described|p198, p199, p201, p194 Fig. 3|Permian|Early Permian|Of Bellata Group. Geological Province: Gunnedah Basin. Lithic sandstone, conglomerate, siltstone and coal.||||||
11472|Maules Creek Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Early Permian|Geological Province: Gunnedah Basin.||||||
11472|Maules Creek Formation|63832|6|Mentioned|p131 fig 2|Kungurian|Artinskian|Of Gunnedah Basin.||||||
11472|Maules Creek Formation|64631|5|Briefly described|p44 Fig.2.|Kungurian|Artinskian|Gunnedah Basin. Biostratigraphic age control for base and top.||||Overlies Leard Formation. Overlain by Porcupine Formation.||
11472|Maules Creek Formation|64856|6|Mentioned|p49|||Correlated with Buffel Formation.|| ||||31-JAN-13
11472|Maules Creek Formation|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Unit in the Gunnedah Basin. Overlies the Goonbri Formation.||||||22-MAR-12
11472|Maules Creek Formation|65113|5|Briefly described|p343, p345, Fig 4 p 340|Early Permian|Early Permian|From the Gunnedah Basin. Overlies the Goonbri Formation.||||||
11472|Maules Creek Formation|65114|5|Briefly described|p385 Fig.3|Early Permian||||||||
11472|Maules Creek Formation|65115|5|Briefly described|p411, Fig 2 p403|Permian|Permian|Gunnedah Basin. Overlies the Goonbri Formation.||||||
11472|Maules Creek Formation|65116|4|Described|p436, 441, p442-444, Fig 2 p436, p449|Early Permian|Early Permian|Overlies the Goonbri Formation in the Gunnedah Basin. Lithic conglomerate and coarse sandstone with coal, siltstone and claystone.||||||
11472|Maules Creek Formation|65118|5|Briefly described|p480, Fig 2 p479|Permian|Permian|Overlies the Goonbri Formation in the Gunnedah Basin.||||||
11472|Maules Creek Formation|66191|5|Briefly described|p485 Fig.2, p485|Early Permian|Early Permian|Gunnedah Basin. Underlies the Porcupine Formation, overlies both the Leard Formation and Goonbri Formation. Coal-bearing alluvial fan deposits.||||||
11472|Maules Creek Formation|67365|5|Briefly described|p88.|Early Permian|Early Permian|Gunnedah Basin. Coals have moderate gas contents (7-9 m3 per tonne), reasonable permeabilities and more than 96% methane.||||||
11472|Maules Creek Formation|68003|4|Described|p38 Fig.3-j, pp39-40, p57 Fig.3-n, p129.|Early Permian|Early Permian|Maules Creek Sub-basin, Gunnedah Basin, Brigalow Belt South Bioregion. Up to 1000 m of sediment deposited to the east of the Boggabri Ridge, which divided the Gunnedah Basin into two sub-basins (the other being the Mullaley Sub-basin). Contains coal seams of economic significance. Correlative of Willow Tree Formation (Werrie Basin). Part-equivalent to Greta Coal Measures in the Sydney Basin.||Unit in Bellata Group.||Overlies Leard and Goonbri Formations. Is overlain by Porcupine Formation.|Basal carbonaceous claystone, pelletoidal clay sandstone, minor coal; passing upwards into upward-fining cycles of sandstone, thinly-bedded siltstone/sandstone and coal. Conglomerate dominant towards top.|
11472|Maules Creek Formation|68004|4|Described|p23 Table 1, p84, p142, pp166-167.|||Maules Creek Sub-basin, Gunnedah Basin. Huge potential for coal seam methane. In the Bohena Sub-basin, the coals are thick, very gassy, highly fractured with little or no mineralisation, highly permeable and over-pressured. A potential oil source rock.||Unit in Bellata Group.||Overlies Mirrie Formation. Is overlain by Porcupine Formation.|Basal carbonaceous claystone, pelletoidal clay sandstone, passing into fining-up cycles of sandstone, siltstone and coal; conglomerate dominant towards top.|
11472|Maules Creek Formation|68006|5|Briefly described|p99, p100, p104.|Early Permian|Early Permian|Maules Creek Sub-basin. Onlaps the Boggabri Ridge in the west; progressively thickens to the ENE under the Mooki Fault. Maximum thickness 1200 m. Deposited in a braided stream environment, from the west. Excellent coal quality: vitrinite-rich, very low ash.|||||Regularly rhythmical series of conglomerate, sandstone, mudstone and coal.|
11472|Maules Creek Formation|70791|4|Described|p275-278, p280-294|Cisuralian|Cisuralian|Gunnedah Basin. Newly-named constituents in this article are Bibblewindi, Bohena, Collygra, Coxs, Mooki, Tullamullen, Coal Members. Provenances briefly described. Isopachs. Up to 110m thick. These 6 constituent coal seams thicken and coalesce into a continuous 35m section of coal immediately S of Narrabri in hole Yallambee 1. Contains no tuffs, hence no geochronology. Has microflora of APP22 to APP33 age. Coal properties described.||Bellata Group.|Also includes Cranleigh, Templemore, Tarrawonga, Flixton, Therebri, Northam, Nagero, Velyama, Merriown, Jeralong, Braymont, Thornfield, Teston, Onavale, Herndale, Coal Members.|Disconformably overlies Goonbri Formation.|An upward-coarsening sequence: siltstones and sandstones overlain by pebble conglomerate and massive sandstones. Includes coal seams. Sulfur and bioturbation common in upper parts.|
11472|Maules Creek Formation|70878|5|Briefly described|p718 Fig.13|Permian|Permian|Gunnedah Basin.||Bellata Group.||Overlies Goonbri Formation. Is overlain by Porcupine Formation (Millie Group).||
11472|Maules Creek Formation|71701|5|Briefly described|p170|||Gunnedah Basin.||||Overlies the Goonbri Formation.||
11472|Maules Creek Formation|73495|6|Mentioned|p506|Kungurian|Artinskian|Gunnedah Basin.||||||
11488|May Farm Mudstone Member|41542|6|Mentioned|p234|||||||||
11538|McDougalls Well Conglomerate|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
11538|McDougalls Well Conglomerate|22857|5|Briefly described|Tb 13.1 (insert p70-71), p398 Tb A1.3|Sturtian|Sturtian|Of Yancowinna Subgroup (Torrowangee Group). In the edge of Eurowie Block it represents the whole of Yancowinna Subgroup. Polymictic paraconglomerate. Age: ~700Ma. Max. thickness: 30m. Geological Province: Adelaide Fold Belt. See also p400 App.1 Tb.A1.3.||||||
11538|McDougalls Well Conglomerate|30261|4|Described|Table 1|||Sturtian age||||||
11538|McDougalls Well Conglomerate|33004|6|Mentioned|p136|||||||||
11538|McDougalls Well Conglomerate|34812|3|Fully described|p76|||||||||
11538|McDougalls Well Conglomerate|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
11538|McDougalls Well Conglomerate|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
11538|McDougalls Well Conglomerate|36733|6|Mentioned|Table 5|||||||||
11538|McDougalls Well Conglomerate|37931|4|Described|p532|||||||||
11538|McDougalls Well Conglomerate|38157|6|Mentioned|p261|||||||||
11538|McDougalls Well Conglomerate|39214|6|Mentioned|Table 1|||||||||
11538|McDougalls Well Conglomerate|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Yancowinna Subgroup.||||
11538|McDougalls Well Conglomerate|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Yancowinna Subgroup.||Is overlain by Corona Dolomite.|Polymictic paraconglomerate; clasts derived mainly from Willyama Supergroup and Poolamacca Group.|
11542|McInnes Formation|22601|6|Mentioned|407|Early Permian|Early Permian|||||||
11542|McInnes Formation|22736|6|Mentioned|p629||Namurian|||||||
11542|McInnes Formation|22857|4|Described|p510 App.1 Tb.A1.8|Late Carboniferous|Westphalian|Lithic arenite with minor interbeds of conglomerate, breccia and mudstone. Max. thickness: >1.5km towards east.||||||
11542|McInnes Formation|24118|5|Briefly described|p3|||||||||
11542|McInnes Formation|24121|5|Briefly described|p4, p229|||||||||25-AUG-22
11542|McInnes Formation|30074|3|Fully described|p17|||See also P19.||||||
11542|McInnes Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
11542|McInnes Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
11542|McInnes Formation|32868|6|Mentioned|p209|||||||||
11542|McInnes Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
11542|McInnes Formation|34085|6|Mentioned|Cor.chart|||Westphal. - Stephan.||||||
11542|McInnes Formation|34168|5|Briefly described|p254|||Carboniferous||||||
11542|McInnes Formation|36057|6|Mentioned|Fig.1|||||||||
11542|McInnes Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
11542|McInnes Formation|36528|6|Mentioned|p182|||||||||
11542|McInnes Formation|37068|6|Mentioned|p60|||||||||
11542|McInnes Formation|38801|6|Mentioned|Fig.3|||||||||
11542|McInnes Formation|39302|5|Briefly described|p346|||See also PP347 & 349||||||
11542|McInnes Formation|39303|6|Mentioned|p353|||Flora||||||
11542|McInnes Formation|39308|4|Described|p487|||See also P488 for Rhacopteris flora.||||||
11542|McInnes Formation|40872|6|Mentioned|p33|||||||||
11542|McInnes Formation|40883|6|Mentioned|p8|||||||||
11542|McInnes Formation|41348|5|Briefly described|Map legend|Carboniferous||In the Tamworth Belt.||||||16-DEC-04
11542|McInnes Formation|42547|4|Described|p36|||||||||
11542|McInnes Formation|43017|5|Briefly described|Fig.1,p372|||||||||
11542|McInnes Formation|43447|14|Not recorded|p12|||||||||
11542|McInnes Formation|44093|5|Briefly described|p230 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
11542|McInnes Formation|44244|2|Defined|p155-160|Westphalian|Westphalian|Conformably overlies Buckets Gap Formation; transitional beneath Johnsons Creek Conglomerate in Stroud-Gloucester Syncline area; also disconformably underlies Alum Mountain Volcanics.  Max. thickness: 1500m.   Geological Province: Myall Block.||||||25-AUG-04
11542|McInnes Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
11542|McInnes Formation|46849|6|Mentioned|p185|||||||||
11542|McInnes Formation|50099|5|Briefly described|p16|Late Carboniferous|Late Carboniferous|Intruded by the Cabbage Tree dolerite sill.||||||
11542|McInnes Formation|50147|5|Briefly described|Map legend|Late Carboniferous|Late Carboniferous|Geological Province: Western Myall Block.||||||
11542|McInnes Formation|50263|5|Briefly described|Map Legend|Westphalian|Westphalian|Overlies: Booral Formation.  Geological Province: Western Myall Block.||||||
11542|McInnes Formation|63832|5|Briefly described|p131 fig 2|Serpukhovian|Serpukhovian|Western Myall Block, Southern New England Fold Belt.||||||13-DEC-17
11542|McInnes Formation|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Serpukhovian|Southern New England Fold Belt, western Myall Block. Biostratigraphic age control at base and top and radiometric age control within unit.||||Overlain by Johnsons Creek Conglomerate.||
11542|McInnes Formation|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Serpukhovian|Myall Block, Tamworth Belt.||||||
11542|McInnes Formation|71628|6|Mentioned|p19:156|||||||Is intruded by Stroud Mountain Microgranite.||
11542|McInnes Formation|73487|6|Mentioned|p567|||||||||
11564|McLaughlins Flat Granodiorite|22815|4|Described|p45|Silurian|Silurian|||||||
11564|McLaughlins Flat Granodiorite|35109|2|Defined|p81|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
11564|McLaughlins Flat Granodiorite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
11564|McLaughlins Flat Granodiorite|36443|5|Briefly described|map legend|Early Silurian|Early Silurian|Of Gingera Batholith. Intrusive. Granodiorite. S-type. BMR map code: Sgm.||||||
11564|McLaughlins Flat Granodiorite|40328|4|Described|p208|||Also mentioned P16. Probably not misspelling of McLaughlin.||||||
11564|McLaughlins Flat Granodiorite|41133|6|Mentioned|p1134|||||||||
11564|McLaughlins Flat Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Bullenbalong Suite.||||||
11564|McLaughlins Flat Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb23.||||||
11564|McLaughlins Flat Granodiorite|45147|2|Defined|M212|Late Silurian|Late Silurian|Probably Late Silurian||||||
11564|McLaughlins Flat Granodiorite|60078|6|Mentioned|Map Legend||Silurian|||||||
11568|McLeod Hill Gabbro|22815|4|Described|p87,88|||||||||
11568|McLeod Hill Gabbro|42726|5|Briefly described|map legend|||Reserved as McLeods Hill. Reservation lapsed 1988.||||||
11568|McLeod Hill Gabbro|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|||||||
11577|McPherson Volcanics|34092|6|Mentioned|p11|||||||||
11577|McPherson Volcanics|34340|6|Mentioned|Table 6.1|||Tertiary||||||
11577|McPherson Volcanics|34593|6|Mentioned|p539|||||||||
11577|McPherson Volcanics|35296|6|Mentioned|p12|||Re stratigraphy.||||||
11577|McPherson Volcanics|44818|6|Mentioned|p275-289|||||||||
11583|Mcleods Trail Granogabbro|39409|6|Mentioned|Table XVII|||||||||
11589|Meadows Tank Formation|22518|5|Briefly described|Table 1, p6, 10,|Middle Devonian|Early Devonian|Mulga Downs Group, Darling Basin||||||
11589|Meadows Tank Formation|22857|4|Described|p211, p488 App.1 Tb.A1.7|Eifelian|Emsian|Basal unit of Mulga Downs Group. Overlain by Merrimerriwa Formation; overlies the Winduck Group. Max. thickness: 200m. Geological Province: Barka Basin.||||||
11589|Meadows Tank Formation|22859|4|Described|p211|||||||||
11589|Meadows Tank Formation|22887|3|Fully described|p27, Fig.4 p11||Early Devonian|possibly to Middle Devonian||||||
11589|Meadows Tank Formation|23173|6|Mentioned|Map Legend|||||||||
11589|Meadows Tank Formation|23252|5|Briefly described|Map Legend||Middle Devonian|Of the Mulga Downs Group.||||||11-JAN-10
11589|Meadows Tank Formation|24588|5|Briefly described|p31 Fig.15|Emsian|Emsian|Geological Province: Lachlan Fold Belt.||||||
11589|Meadows Tank Formation|37798|4|Described|p128|||See also Table 1.||||||
11589|Meadows Tank Formation|38292|6|Mentioned|Fig.1|||||||||
11589|Meadows Tank Formation|40913|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
11589|Meadows Tank Formation|41126|2|Defined|p108|Eifelian|Emsian|Emsian to Eifelian||||||
11589|Meadows Tank Formation|41138|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
11589|Meadows Tank Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
11589|Meadows Tank Formation|41821|2|Defined|p55|Early Devonian||||||||
11589|Meadows Tank Formation|42521|5|Briefly described|Fig.6 P20|||||||||
11589|Meadows Tank Formation|42983|6|Mentioned|Fig.3,p345|||||||||
11589|Meadows Tank Formation|43032|3|Fully described|p151|||Of Mulga Downs Group.||||||08-APR-09
11589|Meadows Tank Formation|61311|5|Briefly described|p44|Early Carboniferous|Middle Devonian|Of the Mulga Downs Group. Upward fining cycles of deposits. Geological Province: Darling Basin.||||||
11589|Meadows Tank Formation|64964|5|Briefly described|p163|||Of Mulga Downs Group. Presented as Meadows Tank only in list of formations.||||||08-APR-09
11589|Meadows Tank Formation|64967|5|Briefly described|p115 Fig. 3|||Probably misspelt - see Meadow Tank Formation.||||||08-APR-09
11589|Meadows Tank Formation|65759|5|Briefly described|p114 Fig.2|Eifelian|Esmian|Underlies the Merrimerriwa Formation. 200-1300m thick, part of the Mulga Downs Group. Also written as Meadow Tank Formation on the same diagram.||||||04-JUL-13
11589|Meadows Tank Formation|67870|6|Mentioned|p62|Devonian|Devonian|Darling Basin. Appears only as Meadows Tank (braided).||||||
11589|Meadows Tank Formation|70751|6|Mentioned|p12-p13|Emsian|Emsian|||Mulga Downs Group||||
11589|Meadows Tank Formation|72958|6|Mentioned|p11|Emsian|Emsian|Cobar Basin. Nymagee area.||Mulga Downs Group||Underlain by Gundaroo Sandstone (Winduck Group). Overlain by Merrimerriwa Formation.||
11589|Meadows Tank Formation|73264|6|Mentioned|p1395 Fig.17, p1402 Fig.23|Late Devonian|Middle Devonian|Lachlan Orogen.||Mulga Downs Group||||
11633|Melvilles Coal Member|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Pamboola Formation (Brothers Subgroup, Black Jack Group). Coal; minor fine-grained sandstone, carbonaceous siltstone and claystone, tuff. Max. thickness: 5m. Geological Province: Gunnedah Basin.||||||
11633|Melvilles Coal Member|37094|4|Described|p243|||||||||
11633|Melvilles Coal Member|38614|6|Mentioned|p9|||||||||
11633|Melvilles Coal Member|39693|6|Mentioned|p17|||||||||
11633|Melvilles Coal Member|39913|5|Briefly described|p6|||||||||
11633|Melvilles Coal Member|40060|6|Mentioned|p57|||||||||
11633|Melvilles Coal Member|40680|6|Mentioned|Fig.1|||||||||
11633|Melvilles Coal Member|40767|6|Mentioned|Fig.10|||||||||
11633|Melvilles Coal Member|40952|4|Described|p9|||||||||
11633|Melvilles Coal Member|41990|5|Briefly described|p8|||||||||
11633|Melvilles Coal Member|42679|6|Mentioned|Fig.3 P3|||||||||
11633|Melvilles Coal Member|43194|1|Redefined|p98 Tb. 8.2, p108-109, p133 App. 1|Late Permian|Late Permian|See also references on p105-106, p128. Of Black Jack Formation in this article. Now of Pamboola Formation of Brothers Subgroup, Black Jack Group. Occurs within basal lithic unit of Black Jack Formation. Thickness up to 5.03m. Age Lower Stage 5c.||||||
11633|Melvilles Coal Member|68004|5|Briefly described|pp143-145, p150.|||Mullaley Sub-basin, Gunnedah-Bowen Basin. Occurs widely, but has limited potential due to seam splits with beds of tuff and carbonaceous claystone. Potential improves in a small area SW of Boggabri. See also reference to Melvilles Seam p142.|||||Medium to high ash, high volatile thermal coal.|
11640|Menai Claystone Member|22745|6|Mentioned|Fig3,p128||Scythian|Sydney Basin.||||||
11640|Menai Claystone Member|33683|4|Described|p79|||Bulgo Ss. See also Table 1||||||
11640|Menai Claystone Member|33685|6|Mentioned|Table 2|||||||||
11640|Menai Claystone Member|39293|6|Mentioned|Fig.8.11|||||||||
11640|Menai Claystone Member|45090|6|Mentioned|p71|||Narrabeen Gp.||||||
11673|Merewether Conglomerate Member|23055|6|Mentioned|p18,Fig13p25|||||||||
11673|Merewether Conglomerate Member|29922|6|Mentioned|p49|||||||||
11673|Merewether Conglomerate Member|29926|6|Mentioned|p2|||||||||
11673|Merewether Conglomerate Member|34351|6|Mentioned|p344|||Fig.5.13||||||
11673|Merewether Conglomerate Member|37083|6|Mentioned|p164|||||||||
11673|Merewether Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
11673|Merewether Conglomerate Member|39308|6|Mentioned|p467|||||||||
11673|Merewether Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
11673|Merewether Conglomerate Member|43447|14|Not recorded|diag p26,diag p34|||Part of Cardiff Sub-Group||||||
11673|Merewether Conglomerate Member|43448|14|Not recorded|p228||Permian|Unit of Kotara Formation (Cardiff Subgroup)||||||
11673|Merewether Conglomerate Member|45090|6|Mentioned|p186|||Stratigraphic table||||||
11673|Merewether Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Kotara Formation.||||
11675|Mereworth alkali olivine basalt|36557|6|Mentioned|p657|||||||||
11678|Merigan Black Shale|30735|4|Described|p13|||||||||
11678|Merigan Black Shale|30736|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
11678|Merigan Black Shale|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
11678|Merigan Black Shale|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
11678|Merigan Black Shale|36413|6|Mentioned|Table 3|||||||||
11678|Merigan Black Shale|40136|5|Briefly described|p31|||[Originally entered for NT. CEBMar95]||||||
11678|Merigan Black Shale|42820|5|Briefly described|p11|||||||||
11678|Merigan Black Shale|43128|5|Briefly described|Fig.6,p476|||||||||
11678|Merigan Black Shale|71069|6|Mentioned|p58, p71|Late Ordovician|Late Ordovician|Obsolete name, equivalent to the Warbisco Shale.||||||
11682|Meringo Creek Formation|22477|6|Mentioned|p175|||||||||
11682|Meringo Creek Formation|22815|5|Briefly described|p116|Tertiary|Tertiary|||||||
11682|Meringo Creek Formation|29746|6|Mentioned|p2|||||||||
11682|Meringo Creek Formation|32126|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11682|Meringo Creek Formation|32129|5|Briefly described|p7|||||||||
11682|Meringo Creek Formation|32673|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
11682|Meringo Creek Formation|34341|6|Mentioned|p553|||||||||
11682|Meringo Creek Formation|35289|3|Fully described|p45|||||||||
11682|Meringo Creek Formation|42786|6|Mentioned|p364|||see also Fig.1 p358.||||||26-NOV-15
11682|Meringo Creek Formation|43465|14|Not recorded|Map Legend||Tertiary|||||||
11682|Meringo Creek Formation|61155|5|Briefly described|p19|Late Oligocene|Late Oligocene|Overlies the Moruya Province Volcanics.||||||
11705|Merriangaah Siltstone|22815|2|Defined|p35|Wenlock|Llandovery|||||||
11705|Merriangaah Siltstone|22857|4|Described|p134, p420 App. 1 Tb. A1.5|Early Silurian|Early Silurian|Of the Yalmy Group. Shale interbedded with very fine quartz arenite and coarse quartz siltstone. Unconformably overlies Tombong Formation. Max. thickness: 80m. Geological Province: Yalmy Basin.||||||
11705|Merriangaah Siltstone|23245|5|Briefly described|p134||Early Silurian|||||||
11705|Merriangaah Siltstone|23329|5|Briefly described|1042|Silurian|Silurian|||||||
11705|Merriangaah Siltstone|29994|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
11705|Merriangaah Siltstone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
11705|Merriangaah Siltstone|36413|6|Mentioned|Table 3|||||||||
11705|Merriangaah Siltstone|37727|5|Briefly described|p73|||See also P17, P19 and P29.||||||
11705|Merriangaah Siltstone|38151|6|Mentioned|Table 1|||||||||
11705|Merriangaah Siltstone|40328|3|Fully described|p113|||||||||
11705|Merriangaah Siltstone|41905|4|Described|p30|||||||||
11705|Merriangaah Siltstone|41933|5|Briefly described|Map legend|Middle Silurian|Early Silurian|||||||
11705|Merriangaah Siltstone|42647|6|Mentioned|p27|||||||||
11705|Merriangaah Siltstone|43233|5|Briefly described|Map Legend||Llandovery|of Yalmy Group||||||
11705|Merriangaah Siltstone|46574|5|Briefly described|Map Legend|Early Silurian|Early Silurian|Of the Canberra Rise. Geological Province: Lachlan Pre-Cratonic Province. Shale, siltstone.||||||09-NOV-04
11705|Merriangaah Siltstone|60988|5|Briefly described|p143-146   |Early Silurian|Early Silurian|Tombong Block. At least 80m thick. Contains late Llandovery graptolites (described).||||Conformably overlies the Tombong Formation. Unconformably underlies the Quidong Limestone.|Laminated beds of fine to very fine quartz sand intercalated with coarse quartz siltstone.|
11705|Merriangaah Siltstone|63290|5|Briefly described|p395, p403, p396 Fig. 3|Wenlock|Llandovery|Of Yalmy Group. Underlain by Tombong beds. Sandstones are matrix-poor and contain well-sorted and rounded vein and plutonic quartz grains.||||||
11708|Merricumbene Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11708|Merricumbene Granodiorite|40276|2|Defined|p14|Early Devonian|Early Devonian|||||||
11713|Merrimbula Group|22530|6|Mentioned|p699||Late Devonian|||||||
11713|Merrimbula Group|22605|5|Briefly described|p 12||Devonian|||||||
11713|Merrimbula Group|22815|4|Described|p96,124, fig31,32|Late Devonian|Late Devonian|Thickness undifferentiated.||||||
11713|Merrimbula Group|22857|5|Briefly described|p213, |Late Devonian|Late Devonian|Underlain by Comerong and Yalwal Volcanics. Max. thickness: 3.2km. Geological Province: Lambie Basin. See also p203.||||||
11713|Merrimbula Group|22859|4|Described|p203,213,216||Late Devonian|||||||
11713|Merrimbula Group|22878|5|Briefly described|p39|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
11713|Merrimbula Group|23309|5|Briefly described|p5 Fig. 1.3, p186-187|Carboniferous|Late Devonian|||||||
11713|Merrimbula Group|23327|5|Briefly described|1013|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|23329|5|Briefly described|1046|Famennian|Frasnian|||||||
11713|Merrimbula Group|23541|5|Briefly described|p398|||In the Lachlan Fold Belt||||||
11713|Merrimbula Group|24133|5|Briefly described|p20 Fig. 8|Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||
11713|Merrimbula Group|24551|6|Mentioned|p189|||Of the Boyd Volcanic Complex.||||||10-JUN-14
11713|Merrimbula Group|24580|5|Briefly described|p829|Late Devonian|Late Devonian|Overlies the Comerong Volcanics and Boyd Volcanic Complex. Geological Province: Eastern Lachlan Fold Belt.||||||
11713|Merrimbula Group|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
11713|Merrimbula Group|30329|6|Mentioned|p30|||On table p30.||||||05-FEB-08
11713|Merrimbula Group|30735|4|Described|p49|||||||||
11713|Merrimbula Group|30736|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|30938|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|31019|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|31161|5|Briefly described|PA8|||||||||
11713|Merrimbula Group|31918|6|Mentioned|p40|||||||||
11713|Merrimbula Group|32126|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|32127|4|Described|p262|||Stratigraphy||||||
11713|Merrimbula Group|32129|3|Fully described|p5|||||||||
11713|Merrimbula Group|32617|6|Mentioned|p31|||||||||
11713|Merrimbula Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
11713|Merrimbula Group|32672|6|Mentioned|p674|||||||||
11713|Merrimbula Group|33238|5|Briefly described|p644|||||||||
11713|Merrimbula Group|33268|6|Mentioned|Table 1|||||||||
11713|Merrimbula Group|33269|4|Described|p41|||Lithology||||||
11713|Merrimbula Group|33480|6|Mentioned|p244|||Refers age dating||||||
11713|Merrimbula Group|33875|6|Mentioned|p32|||Uraninite deposits.||||||
11713|Merrimbula Group|34519|6|Mentioned|p43|||||||||
11713|Merrimbula Group|35257|6|Mentioned|p120|||||||||
11713|Merrimbula Group|35526|4|Described|p95|||Relationship to Boyd Volcanic Complex discussed.||||||
11713|Merrimbula Group|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|37501|6|Mentioned|p414|||||||||
11713|Merrimbula Group|38367|6|Mentioned|p104|||||||||
11713|Merrimbula Group|39028|6|Mentioned|Map legend|Famennian|Frasnian|Famennian to Frasnian||||||
11713|Merrimbula Group|39313|5|Briefly described|p278|||||||||
11713|Merrimbula Group|39331|6|Mentioned|Fig.0-3|||||||||
11713|Merrimbula Group|39410|6|Mentioned|p573|||||||||
11713|Merrimbula Group|39713|6|Mentioned|p546|||||||||
11713|Merrimbula Group|40276|2|Defined|p27|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|40328|6|Mentioned|p202|||||||||
11713|Merrimbula Group|40387|6|Mentioned|p137|||||||||
11713|Merrimbula Group|40646|6|Mentioned|p11|||||||||
11713|Merrimbula Group|40776|6|Mentioned|p504|||||||||
11713|Merrimbula Group|40995|6|Mentioned|p396|||||||||
11713|Merrimbula Group|41430|6|Mentioned|p17|||||||||
11713|Merrimbula Group|41919|6|Mentioned|p160|||||||||
11713|Merrimbula Group|42158|6|Mentioned|p1|||||||||
11713|Merrimbula Group|42497|5|Briefly described|Map legend|Famennian|Frasnian|||||||
11713|Merrimbula Group|42786|5|Briefly described|p357|||||||||
11713|Merrimbula Group|42820|5|Briefly described|p95|||||||||
11713|Merrimbula Group|42848|5|Briefly described|Fig.2 p530|Late Devonian|Late Devonian|Includes Bellbird Creek Formation and Twofold Bay Formation and an unnamed basal conglomerate. See also Fig.1 P530.||||||09-MAY-05
11713|Merrimbula Group|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
11713|Merrimbula Group|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
11713|Merrimbula Group|43547|14|Not recorded|p155||Frasnian|||||||
11713|Merrimbula Group|44093|5|Briefly described|p56|Early Carboniferous|Late Devonian|See also p222 Appendix 1. Geological Province: Lachlan Fold Belt.||||||18-MAR-05
11713|Merrimbula Group|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Includes: Worange Point Formation, Bellbird Creek Formation, Twofold Bay Formation. Of the Lambie Shelf. Geological Province: Lambian Transitional Province.||||||
11713|Merrimbula Group|62070|5|Briefly described|p34 Fig.1,|Late Devonian|Frasnian|Grouped with Minuma Range Group and described as fluvial and marine. Frasnian date based on conodonts (Pickett, 1972)||||Nonconformably overlies the Nelligen Granodiorite (of the Moruya Suite)||
11713|Merrimbula Group|63605|5|Briefly described|p992 Fig. 1, p994|Famennian|Frasnian|Includes Twofold Bay, Bellbird Creek and Worange Point Formations. Shallow marine beds.||||||07-FEB-11
11713|Merrimbula Group|66499|6|Mentioned|p62 Fig.6||||||Includes from base, Twofold Bay Formation, Bellbird Creek Formation, Worange Point Formation|||
11713|Merrimbula Group|66768|5|Briefly described|p211 Fig.2, p211|Late Devonian|Late Devonian|Fluvial, quartzose sedimentary rocks. Conformably overlies Comerong Volcanics.||||||
11713|Merrimbula Group|67823|6|Mentioned|p365|||Mis-spelt in text as Merimbula Group.||||||
11713|Merrimbula Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle.||||||
11713|Merrimbula Group|67849|6|Mentioned|p22 Fig.1.|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|68116|5|Briefly described|Appendix, Maps 37, 46.|Late Devonian|Late Devonian||||||Sandstone, conglomerate, siltstone, quartzite, shale.|
11713|Merrimbula Group|68255|4|Described|p1050 Fig.1, p1051 Fig.2, p1053, p1054|Late Devonian|Late Devonian|Budawang Synclinorium. Age based on latest Upper Devonian age (International CommisSion on Stratigraphy, 2010). thrust under Ordovician Adaminaby Group along Buckenbowra Thrust, west of Nelligen Granodiorite.|ca. 359 Ma|||Underlain by the Nelligen Granodiorite. contact with Ordovician Adaminaby Group is variable.|Conglomerates, cream-purple sandstone, and red to brown sandstone.|17-JUL-20
11713|Merrimbula Group|68297|5|Briefly described|p194||Frasnian|Includes Frasnian limestone||||||
11713|Merrimbula Group|68298|5|Briefly described|p214, 215, p233|Famennian|Frasnian|Includes basal Twofold Bay Formation, with fish assemblage. Invertebrates in its lower parts. Marine Transgression. Misspelt as Merribula Group on p234.|||Includes Twofold Bay, Bellbird Creek and Worange Point Formations.|Overlies Boyd Volcanic Complex with local angular unconformities. Conformably overlies Comerong Volcanics.||
11713|Merrimbula Group|68309|6|Mentioned|p225|Late Devonian|Late Devonian|||||||
11713|Merrimbula Group|68592|5|Briefly described|p34|Frasnian|Frasnian|Steiner (1975); Lewis et al. (1994). Bega-Mallacoota 1:250 000 map area. See also references to [mis-spelt] Merimbula Group (p1737, p1908).|||Includes Bellbird Creek Formation.|||
11713|Merrimbula Group|69159|5|Briefly described|Map legend|Famennian|Frasnian||||Includes Worange Point Formation.|||07-SEP-15
11713|Merrimbula Group|70601|5|Briefly described|p25,27,30|Late Devonian|Late Devonian|Onshore geology. Conglomerate clasts derived from underlying Adaminaby Group. Intense cleavage in Budawang Synclinorium mudstones.|||Worange Point Formation.|Overlies Boyd Volcanic Complex and Comerong Volcanics.|Shallow marine, fluvial clastic deposits; mature quartzose and kaolin-rich sediments, weakly cleaved; basal conglomerates, overlying shallow marine succession, upper fluvial unit; red mustone beds in upper and lower units.|
11713|Merrimbula Group|70661|3|Fully described|vii, p101, p106-p110, p113, p114|Frasnian|Frasnian|Budawang Syncline, name derived from town of Merrimbula. Originally the Merrimbula Formation before being raised to group status by Steiner (1966). Distribution, geomorphology, structure, metamorphism and fossil assemblage discussed. 183-1740m thick.  Deposited in continetal, paralic and shallow marine environments.|||Twofold Bay Formation, Bellbird Creek Formation, Worange Point Formation, Ben Boyd Formation|Is faulted against Adaminaby Group. Overlies Yalwal Volcanics either unconformably or disconformably and gradationally.|Basal conglomerate, red beds, red mudstone, sandstone and rare conglomerate. Cross bedded quartzose sandstone, minor shale, siltstone, conglomerate, fossiliferous limestone and rare amygdaloidal basalt.|
11713|Merrimbula Group|71040|6|Mentioned|p32|Devonian|Devonian|Early folds in the Ordovician turbidites underlying the basal unconformity have been refolded to a recumbent orientation.||||||
11713|Merrimbula Group|71303|5|Briefly described|map legend|Frasnian|Frasnian||||Includes Twofold Bay Formation, Bellbird Creek Formation.|||
11713|Merrimbula Group|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Worange Point Formation.|||
11713|Merrimbula Group|71700|2|Defined|vi, p7, p29-p31, p36-p38|Late Devonian|Late Devonian|Named for the town of Merrimbula on the south coast of NSW. The type area for all constituent formations includes the coastal exposures from Jews Head to Red Point. The Merrimbula Group in BRAIDWOOD100, now thought to wholly comprise the Worange Point Formation, was mapped as undifferentiated Merrimbula Group by Felton and Huleatt (1975). Lewis et al. (1994) provide a comprehensive summary of previous work and synonymy for the unit in its type area near Eden. Seperated from the Abercrombie Formation and Willigam Sandstone Member by the Mongarlowe Fault. This unit is at least 3km thick in Braidwood100. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism,  geophysical characteristics, fossils, distinguishing features and economic geology are discussed. Lithology of the constituent Worange Point Formation is provided, see CD. See also p40, p44-p45, p54-p55, p61, p78, p81, CD.|||Includes the Worange Point Formation, Twofold Bay Formation, Bellbird Creek Formation and the Ben Boyd Formation.|Conformably overlies the Comerong Volcanics. Equivalent (broadly) to the Minuma Range Group.||
11713|Merrimbula Group|72528|5|Briefly described|p18.|Late Devonian|Late Devonian|||||Overlies Whipstick Monzogranite.||
11713|Merrimbula Group|73181|6|Mentioned|p62-67|Late Devonian|Late Devonian|Type area is in the Eden-Pambula area (Steiner, 1975).|||Worange Point Formation, Twofold Bay Formation, 'Ben Boyd' Formation, Bellbird Creek Formation|||
11713|Merrimbula Group|73457|6|Mentioned|p2|Late Devonian|Late Devonian|||||||
11724|Merrimerriwa Formation|22518|4|Described|Table 1, p 4, 6, 7|Middle Devonian|Early Devonian|Mulga Downs Group, Darling Basin||||||
11724|Merrimerriwa Formation|22857|4|Described|p211, p488 App.1 Tb.A1.7|Eifelian|Emsian|Of the Mulga Downs Group. Overlies the Meadows Tank Formation. Max. thickness: 380m.||||||
11724|Merrimerriwa Formation|22859|4|Described|p211-12|||||||||
11724|Merrimerriwa Formation|23171|6|Mentioned|p16|||||||||
11724|Merrimerriwa Formation|23173|6|Mentioned|Map Legend|||||||||
11724|Merrimerriwa Formation|29987|5|Briefly described|p23|||||||||
11724|Merrimerriwa Formation|34057|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11724|Merrimerriwa Formation|34469|6|Mentioned|p107|||Table. Upper Devonian||||||
11724|Merrimerriwa Formation|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
11724|Merrimerriwa Formation|35925|4|Described|p5|||||||||
11724|Merrimerriwa Formation|37798|4|Described|p128|||See also Table 1.||||||
11724|Merrimerriwa Formation|38292|6|Mentioned|Fig.1|||||||||
11724|Merrimerriwa Formation|40913|6|Mentioned|Map legend|Eifelian|Zlichovian|Eifelian-Zlichovian||||||
11724|Merrimerriwa Formation|41126|2|Defined|p117|Eifelian|Emsian|Emsian to Eifelian||||||
11724|Merrimerriwa Formation|41138|6|Mentioned|Map legend|Devonian|Devonian|||||||
11724|Merrimerriwa Formation|41276|6|Mentioned|p73|||||||||
11724|Merrimerriwa Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
11724|Merrimerriwa Formation|41821|2|Defined|p57|Eifelian|Emsian|||||||
11724|Merrimerriwa Formation|42467|5|Briefly described|Map Legend|||||||||
11724|Merrimerriwa Formation|42983|6|Mentioned|Fig.3,p345|||||||||
11724|Merrimerriwa Formation|43032|2|Defined|p168|Middle Devonian|Early Devonian|Of Mulga Downs Group.||||||08-APR-09
11724|Merrimerriwa Formation|43380|14|Not recorded|Map Legend||Late Devonian|Unit of Mulga Downs Group||||||
11724|Merrimerriwa Formation|43381|14|Not recorded|Map Legend||Late Devonian|Mulga Downs Group||||||
11724|Merrimerriwa Formation|43389|14|Not recorded|Map Legend||Late Devonian|||||||
11724|Merrimerriwa Formation|43398|14|Not recorded|Map Legend||Late Devonian|Part of Mulga Downs Group||||||
11724|Merrimerriwa Formation|47050|6|Mentioned|p239|||||||||
11724|Merrimerriwa Formation|61311|5|Briefly described|p44|Early Carboniferous|Middle Devonian|Of the Mulga Downs Group. Upward fining cycles of deposits. Geological Province: Darling Basin.||||||
11724|Merrimerriwa Formation|61964|6|Mentioned|p126|Late Devonian|Late Devonian|Contains rare fish plates.||||||
11724|Merrimerriwa Formation|64964|5|Briefly described|p163|||Of Mulga Downs Group. Presented as Merrimerriwa only in list of formations.||||||08-APR-09
11724|Merrimerriwa Formation|64967|5|Briefly described|p114 Fig. 2|Eifelian||Geological province: Darling Basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). See also p115 Fig. 3.||||||
11724|Merrimerriwa Formation|65759|5|Briefly described|p114 Fig.2||Eifelian|Underlies the Bulgoo Formation, overlies the Meadows Tank Formation. 200-300m thick, part of the Mulga Downs Group. Fluvial.||||||04-JUL-13
11724|Merrimerriwa Formation|70751|6|Mentioned|p12|Emsian|Emsian|||Mulga Downs Group||||
11724|Merrimerriwa Formation|72958|6|Mentioned|p11|Emsian|Emsian|Cobar Basin. Nymagee area.||Mulga Downs Group||Underlain by Meadows Tank Formation. Overlain by Bulgoo Formation.||
11741|Meryula Formation|730|6|Mentioned|p24.|||Unit of Kopyje Group. Includes White Tank Limestone Member.||||||11-NOV-14
11741|Meryula Formation|22857|4|Described|p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Kopyje Group (Cobar Supergroup). Quartz-lithic arenite or conglomerate, thinly laminated siltstone. Max. thickness: 1500m. Geological Province: Kopyje Shelf (Darling Basin).||||||
11741|Meryula Formation|23171|5|Briefly described|p12,15,31,55|||||||||
11741|Meryula Formation|23173|4|Described|Map Legend|||||||||
11741|Meryula Formation|23522|5|Briefly described|p253|Devonian|Devonian|||||||
11741|Meryula Formation|35287|6|Mentioned|p7|||||||||
11741|Meryula Formation|36118|6|Mentioned|p67|||||||||
11741|Meryula Formation|38292|6|Mentioned|p3|||||||||
11741|Meryula Formation|39083|4|Described|p27|||||||||
11741|Meryula Formation|39618|3|Fully described|p69|||||||||
11741|Meryula Formation|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
11741|Meryula Formation|41138|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
11741|Meryula Formation|41394|6|Mentioned|p60|||||||||
11741|Meryula Formation|41452|6|Mentioned|p22|||||||||
11741|Meryula Formation|41528|6|Mentioned|p17|||||||||
11741|Meryula Formation|42521|5|Briefly described|Fig.7 P21|||||||||
11741|Meryula Formation|42983|6|Mentioned|Fig.3,p345|||||||||
11741|Meryula Formation|43032|2|Defined|p28|Early Devonian|Early Devonian|of Kopyje Group. Age early Early to late Early Devonion.||||||
11741|Meryula Formation|43153|5|Briefly described|Map Legend||Lochkovian|of Kopyje Group||||||
11741|Meryula Formation|43774|1|Redefined|p19-24|Pragian|Lochkovian|||||||
11741|Meryula Formation|61905|5|Briefly described|p135 Fig. 1|||Geological Province: Cobar Basin.||||||
11741|Meryula Formation|65469|6|Mentioned|p14, p15, p17|||Lachlan Orogen.||Kopyje Group|Includes the White Tank Limestone Member and the Rookery Limestone Member.|||
11741|Meryula Formation|68823|6|Mentioned|p377, p378 Fig.4|Lochkovian|Ludlow|Kopyje Shelf, Lachlan Orogen.||Unit in Kopyje Group.|Includes the White Tank Limestone Member.|||
11741|Meryula Formation|69094|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Kopyje Group.|Includes Drouin Conglomerate Member and Dederang Siltstone Member.||Undifferentiated quartzose conglomerate, sandstone and siltstone.|
11741|Meryula Formation|69095|5|Briefly described|Map legend|Early Devonian|Late Silurian|||Unit in Kopyje Group.|Includes Drouin Conglomerate Member and Dederang Siltstone Member.|Overlies ?conformably Coronga Peak Quartzite.|Undifferentiated: quartzose conglomerate, sandstone and siltstone.|
11741|Meryula Formation|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
11741|Meryula Formation|69635|6|Mentioned|p105|Early Devonian|Late Silurian||||Includes Drouin Conglomerate Member.|||16-JUL-15
11741|Meryula Formation|70941|2|Defined|pviii, p4, p7 fig 3, p8 fig 4|Early Devonian|Late Ludlow|Named for the Meryula property. Broadly equivalent to Mallee Tank beds or Meryula Siltstone of previous workers. Distribution, geomorphology, structure, metamorphism, geophysical characteristics, fossil assemblage, distinguishing characteristics and economic geology discussed. Deposited as a shallow marine transgression sequence. Type area proposed. Age constrained on the basis of SHRIMP dating of the Florida Volcanics and fossil assemblage of its constituents. Time equivalent of the Coronga Peak Quartzite. Estimated to be 1100m thick in the map area.  Siltstones are difficult to distinguish from Girilambone Group. Hosts the Four Ms propsect at the faulted contact with the Girilambone Group. Interfingers with and conformably overlies the Coronga Peak Quartzite. See also p11 fig 6, p21, p76,  p77 fig 31, p78, p78 fig 32, p79, p80, p80 fig 33,p83-p89, p94, p97, p98, p110, p122, p127, p136, p137, p140, p147.||Kopyje Group|Drouin Conglomerate, Dederang Siltstone Member|Correlative of the Baledmund Formation. Unconformably overlies (or is faulted against)  the Girilambone Group. Unconformably overlies the Narrama and Ballast Formations.|Fining upwards sequence of pebble and cobble conglomerate, quartz arenite, tuffaceous arenite and siltstone.|
11741|Meryula Formation|71039|5|Briefly described|p12-p13, p27|||Anchizone, sub-greenschist regional metamorphic grade.||Kopyje Group|Includes the Rookery Limestone Member and the White Tank Limestone Member.|Overlies the Wild Wave Granodiorite.||
11741|Meryula Formation|71285|5|Briefly described|p538, p552 Fig.9|Early Devonian|Late Silurian|Cobar region.||Kopyje Group.||||
11741|Meryula Formation|71360|5|Briefly described|Map legend|Early Devonian|Late Silurian|Geophysical signature: typically non-magnetic sedimentary units; narrow trends of moderate magnetic intensity may relate to underlying rocks. Boundaries are mainly based on existing geological mapping. The unit as mapped includes Merrere Conglomerate Member, "Little Mountain Formation", and conglomerates of Brookong Formation and Drysdale Conglomerate Member extending from the Cobar 1:100 000 map sheet area.||Kopyje Group.|Dederang Siltstone, and Drouin Conglomerate, Members.||Cobble conglomerate, matrix-supported pebble conglomerate, sandstone and siltstone, locally foliated and cleaved.|
11741|Meryula Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Siltstone and minor fine-grained quartzose sandstone, interbedded with uncommon biohermal and biostromal limestone and felsic tuff; coarse quartz-lithic sandstone and conglomerate at base.|
11741|Meryula Formation|72958|6|Mentioned|p6-7, p52-58, p61|||Hosts an unnamed hornblende-phyric dacite sill that returned a SHRIMP U-Pb magmatic crystallisation age of 410.8 +/- 1.9 Ma; too young to be a stratigraphic member of the formation. Description of this sill is consistent with that of the Lease Tuff Member.|ca. 420 Ma|Kopyje Group|May include Lease Tuff Member of Felton, 1981.||Siltstone-rich.|
11741|Meryula Formation|73143|6|Mentioned|p2, p8-9|Lochkavian|Pridoli|||Kopyje Group|White Tank Limestone Member|||
11741|Meryula Formation|73174|6|Mentioned|p1036-1039|Lochkovian|Lochkovian|Kopyje Shelf. Contains age-diagnostic conodont.||Kopyje Group, Cobar Supergroup|White Tank Limestone Member, Rookery Limestone Member|Equivalent to Brookong Formation and Baledmund Formation.||23-NOV-22
11760|Micalong Creek beds|39660|6|Mentioned|p450|||||||||
11760|Micalong Creek beds|45147|3|Fully described|M124|||||||||
11773|Michelago Igneous Complex|22576|6|Mentioned|p201|Early Devonian|Late Silurian|||||||
11773|Michelago Igneous Complex|23559|5|Briefly described|p213|||I-type granitoids.||||||
11773|Michelago Igneous Complex|32820|6|Mentioned|p3|||Cullarin Anticlinorium||||||
11773|Michelago Igneous Complex|36413|2|Defined|p89|Devonian|Devonian|||||||
11773|Michelago Igneous Complex|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Onslow Granodiorite, Monkellan Granodiorite, Micaligo Adamellite and Koolambah Adamellite. GSNSW map code: gc.||||||
11773|Michelago Igneous Complex|39626|6|Mentioned|p276|||||||||
11773|Michelago Igneous Complex|39627|6|Mentioned|p268|||||||||
11773|Michelago Igneous Complex|40328|4|Described|p209|||||||||
11801|Middle River Coal Member|40806|6|Mentioned|p158|||||||||
11801|Middle River Coal Member|42657|5|Briefly described|p84|||of Farmers Creek Formation.||||||
11801|Middle River Coal Member|68004|5|Briefly described|p60 Table 6, p62.|Late Permian|Late Permian|Western Coalfield.||Unit in Farmers Creek Formation.||Overlies State Mine Creek Formation and Gap Sandstone.|A sequence of coal and argillaceous sedimentary rocks and oil shale; coal is basically dull with bright layers; sedimentary bands are thicker in upper parts of the unit.|
11838|Millah Murrah Granite|23214|3|Fully described|p256|Carboniferous|Carboniferous|Intrudes the Crudine Group.  I-type granite.  Prodominantly a medium grained, biotite granite with minor biotite-poor phase.||||||
11838|Millah Murrah Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
11838|Millah Murrah Granite|33006|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
11838|Millah Murrah Granite|33282|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
11838|Millah Murrah Granite|33285|6|Mentioned|p14|||||||||
11838|Millah Murrah Granite|34404|6|Mentioned|Fig.3.5b|||||||||
11838|Millah Murrah Granite|39331|6|Mentioned|Fig.7-1|||||||||
11838|Millah Murrah Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
11838|Millah Murrah Granite|43127|6|Mentioned|p14|||||||||
11838|Millah Murrah Granite|43515|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(Provisional Editon)(L.-M.Carb)||||||
11838|Millah Murrah Granite|43516|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(L.-M.Carb)||||||
11838|Millah Murrah Granite|43517|14|Not recorded|p156,map plate XII|||Probably part of or related to Bathurst Granite||||||
11838|Millah Murrah Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
11838|Millah Murrah Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|||||||
11838|Millah Murrah Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
11838|Millah Murrah Granite|71069|6|Mentioned|p10|Carboniferous|Carboniferous|||Bathurst Supersuite||||
11848|Millfield Farm Formation|39288|6|Mentioned|Fig.3.3|||||||||
11848|Millfield Farm Formation|68493|6|Mentioned|p11|||Contains Eurydesma cordatum shells.||||Correlative of the Allandale Formation.||
11875|Milton Monzonite|24424|5|Briefly described|p539 Tb.4|Triassic|Triassic|Age: ?220 Ma. Palaeomagnetic poles given.||||||
11875|Milton Monzonite|24552|6|Mentioned|p10 Fig.4|||||||||07-FEB-11
11875|Milton Monzonite|29360|6|Mentioned|p43|||Important resource.||||||
11875|Milton Monzonite|29992|6|Mentioned|Map legend|Permian|Permian|||||||
11875|Milton Monzonite|29994|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
11875|Milton Monzonite|30112|6|Mentioned|p111|||||||||
11875|Milton Monzonite|30661|6|Mentioned|Table 1|||||||||
11875|Milton Monzonite|30662|6|Mentioned|p188|||Palaeomagnetism||||||
11875|Milton Monzonite|32106|6|Mentioned|p305|||Palaeomagnetic data||||||
11875|Milton Monzonite|32126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
11875|Milton Monzonite|32129|6|Mentioned|p7|||Refers Brown (1933), Rose (1966)||||||
11875|Milton Monzonite|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
11875|Milton Monzonite|35524|6|Mentioned|p75|||||||||
11875|Milton Monzonite|36042|6|Mentioned|p41|||||||||
11875|Milton Monzonite|36954|6|Mentioned|p114|||||||||
11875|Milton Monzonite|37253|6|Mentioned|Table 1|||||||||
11875|Milton Monzonite|37818|6|Mentioned|Table 3|||||||||
11875|Milton Monzonite|39285|6|Mentioned|p8|||||||||
11875|Milton Monzonite|40365|6|Mentioned|p244|||||||||
11875|Milton Monzonite|42850|5|Briefly described|p546|Late Cretaceous|Late Cretaceous|||||||09-MAY-05
11875|Milton Monzonite|43446|14|Not recorded|p6044|||Ref.to Robertson 1964||||||
11875|Milton Monzonite|46524|6|Mentioned|p123|||||||||
11875|Milton Monzonite|60281|6|Mentioned|p61|||||||||
11875|Milton Monzonite|60299|6|Mentioned|p207|||||||||
11875|Milton Monzonite|61610|6|Mentioned|p256|Permian|Permian|||||||07-FEB-11
11875|Milton Monzonite|65490|6|Mentioned|p883|||Records heating event ~100 Ma ?prior to Tasman Sea rifting||||||
11875|Milton Monzonite|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Triassic|Permian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|245-260 Ma magnetic age range|||||24-APR-12
11875|Milton Monzonite|67029|6|Mentioned|p383 Fig. 5|||Embleton & McElhinny, 1982. Used for comparison of poles of magnetic overprint in the Cretaceous.||||||24-APR-12
11875|Milton Monzonite|67663|6|Mentioned|p518, p524 Fig.4, p535|||Southern Sydney Basin.||||||
11875|Milton Monzonite|68822|6|Mentioned|p339|Ladinian|Olenekian|Southern Sydney Basin.|245 +/- 6 Ma, K-Ar whole rock|||||27-JUL-15
11875|Milton Monzonite|71115|6|Mentioned|p182, 187|||Southern Sydney Basin.|245 +/- 6 Ma (K/Ar: Facer and Carr, 1979).||||One of several shoshonitic intrusions.|
11875|Milton Monzonite|73146|6|Mentioned|p15|||Sydney Basin. Has a normal magnetic overprint apparently carried by authigenic magnetite.||||||
11894|Mineral Hill Volcanics|9548|5|Briefly described|Map Legend|Early Devonian|Silurian|Rhyolite to dacite, tuff, agglomerate, lava, limestone and siltstone.||||||
11894|Mineral Hill Volcanics|22768|5|Briefly described|p170-71|Pridoli|Ludlow|||||||
11894|Mineral Hill Volcanics|22831|3|Fully described|p 39||Pridolian|Kopyje Group||||||
11894|Mineral Hill Volcanics|22857|4|Described|p170-171, p446 App.1, Tb.A1.6|Early Devonian|Late Silurian|Originally mapped within the "Ootha Group" (Rose and Brunker, 1969) and combined with Talingaboolba Formation by McClatchie (1971). Contains brachiopods, corals, lamellibranchs, conodonts. Max. thickness: >300m. Geological Province: Darling Basin.||||||
11894|Mineral Hill Volcanics|23171|6|Mentioned|p15|||||||||
11894|Mineral Hill Volcanics|23309|6|Mentioned|p390|||||||||
11894|Mineral Hill Volcanics|23454|5|Briefly described|p27 Fig.1|Silurian|Silurian|||||||
11894|Mineral Hill Volcanics|23522|5|Briefly described|p253|Devonian|Devonian|||||||
11894|Mineral Hill Volcanics|24477|6|Mentioned|p20|||Pyroclastics; siltstone-limestone-chert sediments; and rhyolites.||||||
11894|Mineral Hill Volcanics|29987|4|Described|p18|||||||||
11894|Mineral Hill Volcanics|30769|6|Mentioned|p34|||||||||
11894|Mineral Hill Volcanics|31161|5|Briefly described|PA4|||||||||
11894|Mineral Hill Volcanics|32087|4|Described|p12|||||||||
11894|Mineral Hill Volcanics|32088|6|Mentioned|p2|||||||||
11894|Mineral Hill Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
11894|Mineral Hill Volcanics|32674|5|Briefly described|p31|||||||||
11894|Mineral Hill Volcanics|33004|6|Mentioned|p173|||||||||
11894|Mineral Hill Volcanics|33480|6|Mentioned|p243|||Refers age dating||||||
11894|Mineral Hill Volcanics|34405|6|Mentioned|p127|||||||||
11894|Mineral Hill Volcanics|34449|6|Mentioned|Table 2-1|||||||||
11894|Mineral Hill Volcanics|34469|6|Mentioned|p108|||Silurian||||||
11894|Mineral Hill Volcanics|35163|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
11894|Mineral Hill Volcanics|35287|5|Briefly described|p10|||||||||
11894|Mineral Hill Volcanics|36066|5|Briefly described|p4|||||||||
11894|Mineral Hill Volcanics|37727|4|Described|p73|||||||||
11894|Mineral Hill Volcanics|39214|6|Mentioned|Table 11|||||||||
11894|Mineral Hill Volcanics|39627|6|Mentioned|Appendix|||||||||
11894|Mineral Hill Volcanics|40328|3|Fully described|p35|||||||||
11894|Mineral Hill Volcanics|40365|6|Mentioned|p240|||||||||
11894|Mineral Hill Volcanics|41528|6|Mentioned|p129|||||||||
11894|Mineral Hill Volcanics|41869|6|Mentioned|p2|||||||||
11894|Mineral Hill Volcanics|42449|6|Mentioned|p13|||||||||
11894|Mineral Hill Volcanics|42566|6|Mentioned|Fig.3 P6|||||||||
11894|Mineral Hill Volcanics|43089|5|Briefly described|Map Legend|||||||||
11894|Mineral Hill Volcanics|43263|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
11894|Mineral Hill Volcanics|43441|4|Described|25|Early Devonian|Late Silurian|||||||08-JAN-10
11894|Mineral Hill Volcanics|44093|5|Briefly described|p172 App. 1|Early Devonian|Late Silurian|In the Mineral Hill Zone. Geological Province: Lachlan Fold Belt.||||||
11894|Mineral Hill Volcanics|44160|5|Briefly described|Map Legend||Pridolian|||||||08-JAN-10
11894|Mineral Hill Volcanics|62367|6|Mentioned|p8|Silurian|Silurian|Of the "Majuba Supersuite".  Felsic I-type rocks. Age: 428-418Ma (Morrison et al 2004).||||||01-JUN-06
11894|Mineral Hill Volcanics|65469|6|Mentioned|p43, p52, p55 fig 3-19|||Lachlan Orogen. See also p62, p67, p367, App A-VI 3.||||||
11894|Mineral Hill Volcanics|67416|5|Briefly described|p83-85, p86-89, p91|||Canbelego-Mineral Hill Volcanic Belt. Considered to be genetically related to volcanic exhalative deposits of the Ag-Pb-Zn and Cu-Au Mineral Hill Mine. Age from microgranite clast in a crosscutting breccia dyke.|428 +/- 4 Ma.|||Is overlain unconformably by Talingaboolba Formation. Equivalent to Kopyje Group.|Rhyolitic to dacitic lapilli, crystal-lithic and vitric tuffs, minor agglomerate, lava and intercalated limestone, siltstone and sandstone. Local rhyolite lava. Sulfide-mineralised, locally oxidised but not leached. I-type.|
11894|Mineral Hill Volcanics|67806|6|Mentioned|p110|||Cut by tuffisite or diatreme structures at the Mineral Hill mine.||||||
11894|Mineral Hill Volcanics|68297|5|Briefly described|p181|Pridoli|Pridoli|NSW. Limestones include small vertebrate fossil fauna.||||||
11894|Mineral Hill Volcanics|69801|6|Mentioned|p1, p135|Silurian|Silurian|Cobar Basin.|421.1 +/- 3.4 (Spandler, 1998)|||||
11894|Mineral Hill Volcanics|70751|4|Described|p5, p8, p11, p13, p17, p21-p22, p27, p38|Pridoli|Ludlow|Canbelego-Mineral Hill Volcanic Belt. Additional dates derived via SHRIMP include 428.2 +/- 3.9 Ma (Spandler, 1998) and a date of 422.2 +/- 3.7 Ma (Spandler, 1998).  Intruded by a quartz-feldspar porphyry dated at 422 Ma. Late Silurian fossil assemblages are present but generally poorly preserved.|417.6 +/- 3.2 Ma (SHRIMP, this study).|Kopyje Group||Unconformably overlies the Forbes Group.||
11894|Mineral Hill Volcanics|70876|5|Briefly described|p9, p76|||Lachlan Orogen.||Kopyje Group|||Felsic, I-type volcanics.|
11894|Mineral Hill Volcanics|70950|6|Mentioned|p1030,1033,1042|||Geological province: Central Lachlan Orogen. Forms part of the Canbelego-Mineral Hill Volcanic Belt.||Unit of Kopyje Group.|||Felsic volcanic and volcaniclastic rocks, minor dolomites and dolomitic siltstones|
11894|Mineral Hill Volcanics|71039|6|Mentioned|p12-p13, p26|||Preserves a sub to lowest greenschist facies secondary hydrothermal mineral assemblages. This unit is mineralised in sections.||||Overlain by the Talingaboolba Formation. Intruded by the Wilmatha Granite.||
11894|Mineral Hill Volcanics|71040|5|Briefly described|p8 Fig.5|||Murda Syncline, southern Girilambone Zone. U-Pb zircon age range by Downes et al. (2016).|428 +/- 4 Ma to 418 +/- 3 Ma.|||||
11894|Mineral Hill Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Kopyje Group.|||Aphyric to crystal-poor dacite to moderately coarse-grained crystal-rich rhyolite, crystal-lithic and vitric volcaniclastic sandstone, lesser mudstone, siltstone, jasper/chert and limestone.|
11894|Mineral Hill Volcanics|72083|5|Briefly described|p36|Early Devonian|Early Devonian|Fossils indicate a stratigraphic break in the Lochkovian, consistent with the age of the Bindian Orogeny.||Cobar Supergroup.||Is overlain by Yarra Yarra Group probably unconformably.||
11894|Mineral Hill Volcanics|72908|5|Briefly described|p5, p7, p21, p25, p30|Pridolian|Pridolian|Hosts the Mineral Hill deposit.||Kopyje Group|||Felsic-dominated volcanic unit, includes limestones and siltstones.|
11894|Mineral Hill Volcanics|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Underlain by Mount Susannah Conglomerate. Overlain by and equivalent to Talingaboolba Formation. Equivalent to Majuba Volcanics.||
11894|Mineral Hill Volcanics|73174|6|Mentioned|p1038, p1046-1047|Lochkovian[?]|Ludlow[?]|Kopyje Shelf.|ca 425-415 Ma||||Rhyolite and rhyodacite ashflow and airfall tuffs.|23-NOV-22
11894|Mineral Hill Volcanics|73578|6|Mentioned|p7, p14, p21, p32, p35|Lochkovian|Gorstian|Shallow-level I-type rocks. Ages of 422.2 +/- 3.7 Ma reported by Spandler (1998) and 417.6 +/- 3.2 Ma by Downes et al. (2016).|422.2 +/- 3.7 Ma, 417.6 +/- 3.2 Ma|||||
11921|Minjary Volcanics|22768|6|Mentioned|p178|||||||||
11921|Minjary Volcanics|22857|4|Described|p178, p450 App.1, Tb.A1.6|Early Devonian|Early Devonian|Rhyolitic lavas and ignimbrites, minor polymictic conglomerates and sandstone; contains brachiopods, corals. Max. thickness: 350m. Geological Province: Bogan Gate Terrace.||||||
11921|Minjary Volcanics|29648|3|Fully described|p17|||||||||
11921|Minjary Volcanics|37270|6|Mentioned|p202|||||||||
11921|Minjary Volcanics|37529|5|Briefly described|p11|||||||||
11921|Minjary Volcanics|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
11921|Minjary Volcanics|40882|6|Mentioned|p25|||See also Fig.1||||||
11921|Minjary Volcanics|42313|3|Fully described|p142|Early Devonian||||||||
11921|Minjary Volcanics|42314|5|Briefly described|Map legend|Early Devonian||||||||
11921|Minjary Volcanics|42726|5|Briefly described|map legend|Early Devonian||137.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
11921|Minjary Volcanics|42828|5|Briefly described|Fig.2 P128|||||||||
11921|Minjary Volcanics|44093|5|Briefly described|p183 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
11921|Minjary Volcanics|63290|6|Mentioned|p403 Fig. 6(c)|Early Devonian|Early Devonian|Geological Province: Tumut Block.||||||
11921|Minjary Volcanics|66197|5|Briefly described|p631 Fig.3a||Devonian|Silicic volcanics. Tumut Trough. Younger than the ~411 Ma Gocup Granite.||||||13-MAR-12
11921|Minjary Volcanics|71040|6|Mentioned|p9|Early Devonian|Early Devonian|Tumut Trough. Post-dates deformation associated with Bindian (= Bowning) Orogeny; has a basal unconformity.||||||
11921|Minjary Volcanics|73215|6|Mentioned|p994|||Tumut Trough.||||||
11923|Minmi Member|23982|5|Briefly described|p58 Fig.18|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|24092|5|Briefly described|p8 Fig.3|||Of Bungil Formation. Geological Province: Surat Basin.||||||
11923|Minmi Member|30020|6|Mentioned|p30|||||||||
11923|Minmi Member|30021|6|Mentioned|p87|||||||||
11923|Minmi Member|30022|6|Mentioned|p28|||||||||
11923|Minmi Member|30024|6|Mentioned|p336|||||||||
11923|Minmi Member|30446|6|Mentioned|p39|||||||||
11923|Minmi Member|30691|5|Briefly described|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|30695|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30696|4|Described|Table 4|||Lower Cretaceous age||||||
11923|Minmi Member|30702|6|Mentioned|p21|||Of Blythesdale Formation||||||
11923|Minmi Member|30771|6|Mentioned|p4|||Cretaceous.Member of Hackdown Formation||||||
11923|Minmi Member|31116|4|Described|p41|||See also p42.||||||08-MAR-19
11923|Minmi Member|31208|6|Mentioned|Table 1|||||||||
11923|Minmi Member|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
11923|Minmi Member|32314|6|Mentioned|Fig. 4|||||||||
11923|Minmi Member|32796|6|Mentioned|p302|||||||||
11923|Minmi Member|34543|6|Mentioned|p98|||||||||
11923|Minmi Member|34613|6|Mentioned|p15|||||||||
11923|Minmi Member|34619|6|Mentioned|p.160, Pl.22||Adelaidean|||||||
11923|Minmi Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
11923|Minmi Member|36357|5|Briefly described|p77|||||||||
11923|Minmi Member|36552|6|Mentioned|p59|||||||||
11923|Minmi Member|36571|6|Mentioned|Table 4|||||||||
11923|Minmi Member|36574|6|Mentioned|p602|||||||||
11923|Minmi Member|37995|6|Mentioned|p66|||||||||
11923|Minmi Member|38373|6|Mentioned|p621|||||||||
11923|Minmi Member|38374|6|Mentioned|p605|||||||||
11923|Minmi Member|39211|5|Briefly described|p31|||||||||
11923|Minmi Member|39212|4|Described|p40|||Excursion site. See also p18.||||||08-MAR-19
11923|Minmi Member|39216|6|Mentioned|p55|||Fauna||||||
11923|Minmi Member|40541|4|Described|p111|||||||||
11923|Minmi Member|40666|4|Described|p358|||||||||
11923|Minmi Member|41057|6|Mentioned|p61|||||||||
11923|Minmi Member|41064|6|Mentioned|p60|||||||||
11923|Minmi Member|41266|6|Mentioned|Fig.3|||||||||
11923|Minmi Member|41427|6|Mentioned|p84|||||||||
11923|Minmi Member|42494|5|Briefly described|Table 1 P24|||||||||
11923|Minmi Member|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
11923|Minmi Member|44021|14|Not recorded|p232(Fig.1)|||||||||
11923|Minmi Member|44031|14|Not recorded|p11||Early Cretaceous|||||||
11923|Minmi Member|44082|6|Mentioned|p8,10,Tb.p34|||Part of Blythesdale Group. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
11923|Minmi Member|44376|4|Described|p1-9,11-8,20-3,25,29|||Fossils.||||||
11923|Minmi Member|44377|2|Defined|p1,2,10,13,map||Aptian|Top-most member of Blythesdale Formation. marine Aptian, mainly "calcareous and glauconitic protoquartzites", probably "near-shore facies equivalents of sediments in the lower part of the Roma Formation."||||||
11923|Minmi Member|44915|14|Not recorded|p18|||Ref. to Vine and Day 1965.||||||
11923|Minmi Member|45110|3|Fully described|p112|||See also p10. Of Bungil Formation.||||||08-MAR-19
11923|Minmi Member|45132|6|Mentioned|Table 2|||||||||
11923|Minmi Member|46791|6|Mentioned|Table 1|||||||||
11923|Minmi Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
11923|Minmi Member|46984|6|Mentioned|Table 1|||||||||
11923|Minmi Member|48919|4|Described|Table 5|||||||||
11923|Minmi Member|48920|6|Mentioned|p59|||See also P73. Member of Blythesdale Formation.||||||
11923|Minmi Member|49010|6|Mentioned|Fig.4|||Surat Basin||||||
11923|Minmi Member|49011|6|Mentioned|Fig.3|||Surat Basin||||||
11923|Minmi Member|64856|4|Described|p98,99|early Aptian|early Aptian|Of Day (1964). Originally included in Blythesdale Formation, now in Bungil Formation. Contains early Aptian dinoflagellate assemblages.|| ||||31-JAN-13
11923|Minmi Member|65384|5|Briefly described|S116, S117, S118|||Probably Aptian.Of Bungil Formation, Surat Basin.||||||
11923|Minmi Member|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Bungil Formation.||Overlies Nullawurt Sandstone Member.||
11923|Minmi Member|66623|6|Mentioned|p449.|Early Cretaceous|Early Cretaceous|Contains various bivalve species which occur also in the Milparinka-Tibooburra district (Rolling Downs Group).||||||
11923|Minmi Member|69594|5|Briefly described|p538|Aptian|Aptian|Northern Surat Basin. Previously included by Day (1964) in his Blythesdale Formation. The type area is near Bungil Creek at Minmi Crossing. Contains a sproradic but diverse marine fauna dominated by molluscs, and the dinosaur Minmi paravertebra. Marine and brackish water environment.||Bungil Formation.|||Calcareous and glauconitic sandstones, silty shales and siltstones and minor intraformational conglomerates.|
11923|Minmi Member|70821|5|Briefly described|p80|||Surat Basin.||Bungil Formation.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla Formation).||
11923|Minmi Member|71601|6|Mentioned|p121|Aptian|Aptian|||Bungil Formation||||
11923|Minmi Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||Bungil FZ.||Overlies Nullawurt Sandstone Member. Is overlain by Doncaster Member (Wallumbilla FZ).||
11927|Minnamurra Latite Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Pheasants Nest Formation (Cumberland Subgroup, Illawarra Coal Measures). Geological Province: Sydney Basin.||||||
11927|Minnamurra Latite Member|23544|5|Briefly described|Fig 2 p358|||In the Gerringong Volcanics||||||
11927|Minnamurra Latite Member|29900|6|Mentioned|Table 2|||||||||
11927|Minnamurra Latite Member|29901|6|Mentioned|Table 1|||||||||
11927|Minnamurra Latite Member|31128|6|Mentioned|Table 1|||||||||
11927|Minnamurra Latite Member|36220|3|Fully described|p45|||See also Table 10 & P38.||||||
11927|Minnamurra Latite Member|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
11927|Minnamurra Latite Member|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
11927|Minnamurra Latite Member|39309|6|Mentioned|p123|||||||||
11927|Minnamurra Latite Member|40519|6|Mentioned|Fig.3|||||||||
11927|Minnamurra Latite Member|42737|5|Briefly described|map legend|Permian||||||||
11927|Minnamurra Latite Member|71115|5|Briefly described|p179-180, 182, 188|Permian|Permian|Southern Sydney Basin.||Gerringong Volcanics (Pheasants Nest Formation).||Overlies Calderwood Latite Member. Is overlain by Berkeley Latite Member.|Basaltic.|
11927|Minnamurra Latite Member|73494|5|Briefly described|p542-543|Permian|Permian|Southern Sydney Basin. Late Permian.||Gerringong Volcanics.|||Shoshonitic basalt. Porphyritic (usually plagioclase); locally vesicular or amygdaloidal.|
11947|Minuma Range Group|22815|5|Briefly described|p102|||||||||
11947|Minuma Range Group|22857|5|Briefly described|p213, p494 App. 1 Tb.A1.7|Late Devonian|Late Devonian|Geological Province: Lambie Basin. See also p217.||||||
11947|Minuma Range Group|22859|6|Mentioned|p213,216-17|||||||||
11947|Minuma Range Group|24580|6|Mentioned|p828 Fig.1|||Group is Gp in text. Geological Province: Eastern Lachlan Fold Belt.||||||
11947|Minuma Range Group|39028|6|Mentioned|Map legend|Famennian|Frasnian|Famennian to Frasnian||||||
11947|Minuma Range Group|40276|2|Defined|p22|Late Devonian|Late Devonian|||||||
11947|Minuma Range Group|42820|5|Briefly described|p95|||||||||
11947|Minuma Range Group|43233|5|Briefly described|Map Legend||Late Devonian|||||||
11947|Minuma Range Group|44093|5|Briefly described|p222 App. 1|Early Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt.||||||18-MAR-05
11947|Minuma Range Group|61818|5|Briefly described|p85|Late Devonian|Late Devonian|Includes the Gundillion Conglomerate. Predominanlty "red bed" coarse sandstones and conglomerates. Geological Province: Lachlan Fold Belt.||||||
11947|Minuma Range Group|62070|5|Briefly described|p34 Fig.1,|Late Devonian|Late Devonian|Grouped with Merrimbula Group and described as fluvial and marine.||||||
11947|Minuma Range Group|64827|5|Briefly described|p1051|Late Devonian|Late Devonian|Terretrial conglomerates and coarse sandstones.||||||
11947|Minuma Range Group|67847|5|Briefly described|p60 fig 3.3.4|||Lambie Basin. Of the authors' proposed Kanimblan cycle.||||||
11947|Minuma Range Group|69159|5|Briefly described|Map legend|Late Devonian|Late Devonian||||Includes Gundillion Conglomerate.|||07-SEP-15
11947|Minuma Range Group|70601|5|Briefly described|p25,27|Devonian|Devonian|Onshore geology. Minuma Range. Conglomerate clasts derived from underlying Adaminaby Group. Also abbreviated to Minuma Group on p25.|||||Shallow marine, fluvial clastic deposits; mature quartzose and kaolin-rich sediments, weakly cleaved; basal conglomerates, overlying shallow marine succession, upper fluvial unit; red mustone beds in upper and lower units.|
11947|Minuma Range Group|71069|6|Mentioned|p147|Devonian|Devonian|||||Overlies the De Drack Formation.||
11947|Minuma Range Group|71699|5|Briefly described|Map legend.|Devonian|Devonian||||Gundillion Conglomerate.|||
11947|Minuma Range Group|71700|3|Fully described|vi, p7, p29, p36-p38|Late Devonian|Late Devonian|Named for the Minuma Range within the Deua National Park South in Araluen100. No type section has been nominated for this group. Synonymy is discussed in great detail, see CD. Distribution, geomorphic expression, outcrop, depositional environment, structure, fossils, metamorphism, geochemistry, geophysical characteristics, distinguishing features and economic geology are discussed. Maximum thickness is estimated at 1.2km. Late Devonian age is derived from fossil fauna in constituent units. See also p41, p45, p62, p66, p78, p81, p119, CD.|||Includes the Gundillion Conglomerate, Long Swamp Creek Formation, Big Hole Formation, Curmulee Conglomerate, Deua Formation and the Khan Yunis Formation.|Overlies the Comerong Volcanics. Equivalent (broadly) to the Merrimbula Group.|Alluvial fan conglomerate overlain by shallow marine shale and sandstone-rich deposits.|
11947|Minuma Range Group|73181|6|Mentioned|p65-67|Late Devonian|Late Devonian|Of Wyborn and Owen (1986). Name misspelt as Minima Range Group in figure caption p65, and also Minima Group p67.|||Gundillion Conglomerate, Big Hole Formation, Long Swamp Creek Formation, Curmulee Conglomerate, Deua Formation, Khan Yunis Formation|||
11956|Mirannie Volcanic Member|22857|5|Briefly described|p506 App.1 Tb.A1.8|Westphalian|Namurian|Of the Seaham Formation. Ignimbrite, pitchstone, agglomerate, tuff. Max. thickness: 230m. Geological Province: Tamworth Forearc Basin.||||||
11956|Mirannie Volcanic Member|32378|6|Mentioned|p113|||||||||
11956|Mirannie Volcanic Member|32379|6|Mentioned|Fig.7|||||||||
11956|Mirannie Volcanic Member|44244|4|Described|p109|||Of the Seaham Formation.  Max. thickness: >230m.  Geological Province: Gresford Block.  See also p107.||||||25-AUG-04
11956|Mirannie Volcanic Member|50268|5|Briefly described|Map Legend|Stephanian|Stephanian|Of the Seaham Formation.  Geological Province: Rouchel and Gresford Blocks.||||||
11956|Mirannie Volcanic Member|65107|5|Briefly described|P276, Fig 4 p279, Fig 11 p286-7|Serpukhovian|Serpukhovian|Helps to define the age of the Gresford Block, 321.3+/-4.4Ma. Provides segments that agree with east to west pole path (for the Gresford Block) for the New England Orogen.||||||16-JAN-12
11956|Mirannie Volcanic Member|73487|6|Mentioned|p566|Serpukhovian|Serpukhovian|Rouchel and Gresford blocks. Levipustula levis zone.||||||
11982|Mitchells Creek Group|39364|6|Mentioned|p51|||||||||
11992|Mittagang Gneiss|31386|5|Briefly described|Table 4|||||||||
11992|Mittagang Gneiss|34404|6|Mentioned|Fig.3.7|||Map legend||||||
12015|Mogongong Conglomerate Member|22857|5|Briefly described|p213, p490 App.1 Tb.A1.7|Devonian|Devonian|Of the Hervey Group. Contains fish plates. Geological Province: Hervey Basin.||||||
12015|Mogongong Conglomerate Member|22859|6|Mentioned|p213|||||||||
12015|Mogongong Conglomerate Member|23392|3|Fully described|p7|Frasnian|Givetian|of Conolly ;(1965). Fossil assemblage includes Cordaites and Protolepidoolendron. Of the Peaks Formation. Max Thickness: 120m||||||
12015|Mogongong Conglomerate Member|24417|3|Fully described|p126|Middle Devonian|Middle Devonian|Of Peaks Formation.  Previously divided by Jones (1984) into two units: lower "Debris Flow and upper "Fluviatile Conglomerate".||||||
12015|Mogongong Conglomerate Member|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
12015|Mogongong Conglomerate Member|43499|14|Not recorded|Map Legend|||(Provisional Edition) Part of Beargamil Sub-Group. Gooloogong-Grenfell Region||||||
12015|Mogongong Conglomerate Member|43507|2|Defined|p126,128,135,138,145||Late Devonian|Member of Peaks Sandstone (Beargamil Subgroup, Hervey Group)||||||
12015|Mogongong Conglomerate Member|43510|2|Defined|p41-2,58,60-1|||||||||
12015|Mogongong Conglomerate Member|50628|5|Briefly described|Map Legend|Devonian|Devonian|Of the Peak Formation (Hervey  Group). Polymictic conglomerate.||||||05-JUL-04
12015|Mogongong Conglomerate Member|60009|5|Briefly described|Map Legend|Frasnian|Frasnian|Of the Peaks Formation (Hervey Group).||||||13-JUL-04
12037|Mole Leucogranite|38842|6|Mentioned|p286|||||||||
12037|Mole Leucogranite|71628|4|Described|p1:6; p4:19; p19: 28, 31, 48, 108-127;|||See also p8: 82-86, 88-91; p10: 3, 8, 10; p15: 11, 86, 88; p19: 148-149, 170. Flinter (1982). Previously Mole Granite (Shaw, 1969); various informal/unpublished names were used prior to that. Origin of the name (Mole) is unknown. Occurs 15 km NW of Deepwater where it forms the Mole Tableland. Outcrop is 40 x 20-25 km. Appears to form a ~4 km-thick sill-like mass, only a little unroofed: incorporates several roof pendants. Extensively fractured. Many age determinations given, including metamorphism and vein mineralisation. Lithologies, mineralogy, geochemistry and mineralisation all described in very great detail. Most extensively mineralised intrusion in the southern New England Orogen; over 1,200 mineral occurrences.|249.8 +/- 1.5 Ma (SHRIMP: Chisholm et al., 2014).|Mole Suite.||Intrudes Texas beds, Bondonga beds and Wandsworth Volcanic group. Encloses a pendant of Terimbone Monzogranite.|Coarse- to very coarse-grained, seriate biotite leucomonzogranite to leucosyenogranites, with a marginal porphyritic phase, and minor microgranite; locally greisenous and silexite phases. Highly fractionated I-type.|
12050|Molong Limestone|6969|5|Briefly described|p13 Fig. 1, p15|Ludlow|Wenlock|Geological Province: Lachlan Fold Belt.||||||
12050|Molong Limestone|13996|5|Briefly described|p139-141, p143-145|||Contains mid-Wenlock brachiopods. Also the only rostroconch mollusc of Silurian age definitely known in Australia (Conocardium davidis). Contains a diverse Wenlock-aged trilobite fauna. Biogeographic implications.||||Equivalent to Mirrabooka Formation and Borenore Limestone.||
12050|Molong Limestone|22486|6|Mentioned|p 6|||||||||
12050|Molong Limestone|22857|5|Briefly described|p468 App.1 Tb.A1.6|Silurian|Silurian|Of the Mumbil Group. Massive or thickly bedded limestone. Max. thickness: 1220m.||||||
12050|Molong Limestone|23214|3|Fully described|p126|Late Silurian|Late Silurian|Of Mumbil Group. Previously included in Molong Beds, Gamboola Formation and Nanima Formation. Adrian (1977) formally seperated the unit from Reedy Creek Limestone. 1200m thick at type section.||||||
12050|Molong Limestone|23225|5|Briefly described|Fig.1 p18|Ludlow|Wenlock|||||||
12050|Molong Limestone|29362|2|Defined|p193|Silurian|Silurian|||||||
12050|Molong Limestone|29791|6|Mentioned|Fig.4|||||||||
12050|Molong Limestone|30044|6|Mentioned|Fig.7|||||||||
12050|Molong Limestone|30139|5|Briefly described|Table 1|||||||||
12050|Molong Limestone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
12050|Molong Limestone|32672|6|Mentioned|p672|||||||||
12050|Molong Limestone|33116|4|Described|p215|||See also PP216-219||||||
12050|Molong Limestone|33611|6|Mentioned|p130|||||||||
12050|Molong Limestone|34406|6|Mentioned|p220|||||||||
12050|Molong Limestone|34692|6|Mentioned|p184|||||||||
12050|Molong Limestone|34713|6|Mentioned|p118|||||||||
12050|Molong Limestone|34895|6|Mentioned|Fig. 1|||||||||
12050|Molong Limestone|35062|6|Mentioned|p278|||||||||
12050|Molong Limestone|35137|6|Mentioned|p88|||||||||
12050|Molong Limestone|35291|6|Mentioned|Fig.7|||||||||
12050|Molong Limestone|35412|6|Mentioned|Fig.9|||||||||
12050|Molong Limestone|37727|4|Described|p80|||||||||
12050|Molong Limestone|39214|5|Briefly described|p19|||||||||
12050|Molong Limestone|39331|6|Mentioned|Fig.6-3|||Biostratigraphy||||||
12050|Molong Limestone|40328|4|Described|p148|||||||||
12050|Molong Limestone|43039|5|Briefly described|Text-Fig.2,p5|||||||||
12050|Molong Limestone|43344|14|Not recorded|p139,161||Silurian|||||||
12050|Molong Limestone|43640|5|Briefly described|Map Legend||Silurian|||||||
12050|Molong Limestone|43782|5|Briefly described|Map Legend|Pridoli|Wenlock|Of Mumbil Group.||||||14-APR-08
12050|Molong Limestone|48971|6|Mentioned|p40|||See also P42.||||||
12050|Molong Limestone|50095|5|Briefly described|p108 Fig.1|Silurian|Silurian|||||||
12050|Molong Limestone|50096|6|Mentioned|p78|||Occurrence of Ozarkodina martinssoni auriformis (conodont).||||||29-NOV-04
12050|Molong Limestone|63083|6|Mentioned|p218|||Together with Borenore Limestone - forms lateral equivalent of Mirrabooka Formation.||||||07-FEB-11
12050|Molong Limestone|63287|5|Briefly described|p317 Fig. 2|Pridoli|Wenlock|Of Mumbil Group. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
12050|Molong Limestone|67651|5|Briefly described|p413-416,426,428|Ludlow|Wenlock|Broadly contemporaneous to Mirrabooka Formation and Borenore Limestone.||||Overlain by Wallace Shale. Laterally grades into Mirrabooka Formation.||
12050|Molong Limestone|68592|6|Mentioned|p1890|Ludlow|Wenlock|In the northern Molong High. Contains Thamnopora species, similar to those in Rhyanna Formation.||||||
12050|Molong Limestone|69635|5|Briefly described|p53-67|Ludlow|Wenlock|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation ages on 2 volcanic tuff samples. Index fossil (conodont) Polygnathoides siluricus from near-adjacent beds to one sample. Dating gives age control on large bivalves underlying tuff bed too. Shown as Molong limestone p7.|424.3+/-1.8 Ma; 428.2+/-1.8 Ma|||||15-JUL-15
12050|Molong Limestone|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: late early Silurian to earliest Devonian.||Mumbil Group|||Thick carbonate unit.|
12050|Molong Limestone|70684|6|Mentioned|p27 Fig.11|Silurian|Silurian|||||||
12050|Molong Limestone|71656|6|Mentioned|p30|Ludlow|Wenlock|Molong High.||||||
12050|Molong Limestone|73582|6|Mentioned|p113|||1050m thick. Conodont fauna compared with those of Kildrummie Formation and Jenolan Caves Limestone, to determine the latter's age.||||||
12067|Monaro Volcanics|22815|4|Described|p107,108 fig35|Tertiary|Tertiary|||||||
12067|Monaro Volcanics|23329|6|Mentioned|1042|||||||||
12067|Monaro Volcanics|36557|6|Mentioned|p651|||||||||
12067|Monaro Volcanics|43126|3|Fully described|p1-16||Eocene|||||||
12067|Monaro Volcanics|43233|5|Briefly described|Map Legend|Oligocene|Eocene|||||||
12067|Monaro Volcanics|50126|5|Briefly described|p69, p78, p83 App.2|Oligocene|Eocene|Age: ~50Ma||||||
12067|Monaro Volcanics|64837|5|Briefly described|p558, p561|Early Eocene|Late Paleocene|Age: 56-35Ma (K-Ar: Wellman and McDougall 1974; Roach 1996). Dominantly alkali olivine basalts.||||||02-FEB-09
12067|Monaro Volcanics|68592|5|Briefly described|p1803|||||||Is correlated with the Reevesdale Basalt.|Lava-field basalts.|
12098|Monga Granite|12185|5|Briefly described|map legend|Devonian|Silurian|Hornblende-biotite granite. BMR map symbol: ghq.||||||
12098|Monga Granite|22857|6|Mentioned|p215|||Geological Province: Lambie Basin.||||||
12098|Monga Granite|22859|6|Mentioned|p215|||||||||
12098|Monga Granite|23549|6|Mentioned|p528|||Mentioned only as stratigraphical nomenclature example.||||||05-APR-05
12098|Monga Granite|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
12098|Monga Granite|29994|6|Mentioned|Map legend|Devonian|Devonian|||||||
12098|Monga Granite|31019|6|Mentioned|Map legend|Devonian|Devonian|||||||
12098|Monga Granite|33325|6|Mentioned|p19|||||||||
12098|Monga Granite|39028|6|Mentioned|Map legend|Frasnian|Givetian|Frasnian to Givetian||||||
12098|Monga Granite|40276|2|Defined|p21|Late Devonian|Middle Devonian|Middle to Late Devonian||||||
12098|Monga Granite|40328|4|Described|p209|||||||||
12098|Monga Granite|40387|6|Mentioned|p137|||||||||
12098|Monga Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
12098|Monga Granite|60423|5|Briefly described|p381|Late Devonian|Late Devonian|Age: 371 +/- 6Ma (Wyborn & Owen 1986).||||||
12098|Monga Granite|66768|5|Briefly described|p211 Fig.2||Famennian|A-type. Rb/Sr age 371 +/- 6 Ma (Wyborn and Owen, 1986).||||||
12098|Monga Granite|71206|6|Mentioned|p373, 377, 384|||Lachlan Fold Belt. Contains both abundant brick-red K-feldspar and cream-white K-feldspar. Geochemistry graphs.||Monga Suite.|||Aluminous A-type granite.|
12103|Monkey Place Creek Tuff Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Charlton Formation.   Equivalent to Nobbys Tuff (Newcastle Coal Measures).   Geological Province: Sydney Basin||||||
12103|Monkey Place Creek Tuff Member|29942|3|Fully described|p11|||||||||
12103|Monkey Place Creek Tuff Member|39666|6|Mentioned|p66|||||||||
12103|Monkey Place Creek Tuff Member|45090|6|Mentioned|p188|||||||||
12140|Montrose Coal|23055|6|Mentioned|Fig4p11|||||||||
12140|Montrose Coal|23717|5|Briefly described|p118 Fig.2|Permian|Permian|Of the Adamstown Formation.   Geological Province: Sydney Basin||||||
12140|Montrose Coal|36042|6|Mentioned|p28|||||||||
12140|Montrose Coal|39287|6|Mentioned|Fig. 2.15|||||||||
12140|Montrose Coal|39308|6|Mentioned|Fig. 23.4|||||||||
12140|Montrose Coal|40516|6|Mentioned|p395|||||||||
12140|Montrose Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Montrose coal seam instead. See also p113.||Of Adamstown Subgroup||||
12140|Montrose Coal|73304|6|Mentioned|p75|||||Adamstown Formation, Newcastle Coal Measures||||
12170|Mooga Sandstone|730|6|Mentioned|p24.|||Fluviatile.||||||11-NOV-14
12170|Mooga Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497|Early Cretaceous|Early Cretaceous|N Surat Basin. 50-100m thick. Basal section is permeable and acts as a major aquifer.||||Grades laterally into upper part of Hooray Sandstone.|Quartzose, sub-labile, upward-fining fluvial sandstone, with interbeds of siltstone and mudstone at the top.|
12170|Mooga Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
12170|Mooga Sandstone|22757|5|Briefly described|Table6,p11||Early Cretaceous|60 m. Surat Basin.||||||
12170|Mooga Sandstone|22857|4|Described|p295, p296-7 Tb.22.1, p546 Tb.A1.12|Hauterivian|Berriasian|Of the Blythesdale Group. Fine-grained sublabile to quartzose arenite with interbedded siltstone and shale. Equivalent of Hooray Sandstone (Eromanga Basin). Max. thickness: 56m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
12170|Mooga Sandstone|22865|4|Described|p295,Table22.1p296-7|Valanginian|Berriasian|||||||
12170|Mooga Sandstone|23053|6|Mentioned|Fig10p17,26|Valanginian|Tithonian|||||||
12170|Mooga Sandstone|23056|6|Mentioned|9|||Geol province Eromanga Basin||||||
12170|Mooga Sandstone|23818|6|Mentioned|140|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
12170|Mooga Sandstone|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 140m.||||||
12170|Mooga Sandstone|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
12170|Mooga Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
12170|Mooga Sandstone|29379|6|Mentioned|Fig.11|||Showing oil company usage compared with Freytag(1966)&Forbes(1966).||||||
12170|Mooga Sandstone|29387|6|Mentioned|Table 5|||||||||
12170|Mooga Sandstone|29393|6|Mentioned|Table 4|||||||||
12170|Mooga Sandstone|29591|6|Mentioned|p77|||||||||
12170|Mooga Sandstone|29721|6|Mentioned|Table 246|||||||||
12170|Mooga Sandstone|30021|6|Mentioned|p87|||||||||
12170|Mooga Sandstone|30022|6|Mentioned|p28|||||||||
12170|Mooga Sandstone|30024|6|Mentioned|p332|||||||||
12170|Mooga Sandstone|30540|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
12170|Mooga Sandstone|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30695|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30696|4|Described|Table 4|||Lower Cretaceous age||||||
12170|Mooga Sandstone|30697|6|Mentioned|p34|||Major aquifer present||||||
12170|Mooga Sandstone|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30699|6|Mentioned|p53|||Middle Jurassic - Early Cretaceous. Stratigraphy||||||
12170|Mooga Sandstone|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|30702|4|Described|p48|||See also p49-51, Table 1, Fig.1,2.||||||13-JUN-22
12170|Mooga Sandstone|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
12170|Mooga Sandstone|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|31098|5|Briefly described|Table 1|||Lower Cretaceous||||||
12170|Mooga Sandstone|31116|4|Described|p40|||Cretaceous. See also Table 2||||||
12170|Mooga Sandstone|31369|6|Mentioned|Table 4|||Cretaceous||||||
12170|Mooga Sandstone|31376|6|Mentioned|p4|||||||||
12170|Mooga Sandstone|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|32797|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33070|4|Described|Table 2|||L.Cret.||||||
12170|Mooga Sandstone|33071|6|Mentioned|p6|||L.Cret.||||||
12170|Mooga Sandstone|33075|6|Mentioned|p451|||||||||
12170|Mooga Sandstone|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33090|4|Described|Table 4|||L.Cret.||||||
12170|Mooga Sandstone|33091|5|Briefly described|p7|||Stratigraphy||||||
12170|Mooga Sandstone|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33165|6|Mentioned|Chart|||Correlation chart only||||||
12170|Mooga Sandstone|33367|6|Mentioned|p17|||||||||
12170|Mooga Sandstone|33414|6|Mentioned|p214|||||||||
12170|Mooga Sandstone|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12170|Mooga Sandstone|33523|6|Mentioned|p27|||||||||
12170|Mooga Sandstone|33672|6|Mentioned|p44|||||||||
12170|Mooga Sandstone|33828|6|Mentioned|Table 3|||||||||
12170|Mooga Sandstone|33939|6|Mentioned|p412|||Blythesdale Group.||||||
12170|Mooga Sandstone|33971|6|Mentioned|Fig.29|||Strat. table.||||||
12170|Mooga Sandstone|34254|6|Mentioned|p491|||||||||
12170|Mooga Sandstone|34543|6|Mentioned|p98|||||||||
12170|Mooga Sandstone|34611|6|Mentioned|p140|||Jurassic. Correlation chart. Fig.65.||||||
12170|Mooga Sandstone|34613|4|Described|Table 4|||||||||
12170|Mooga Sandstone|35793|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|35937|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|36243|6|Mentioned|Table 7A|||||||||
12170|Mooga Sandstone|36570|4|Described|p49|||See also p45, Fig.9, p60.||||||13-JUN-22
12170|Mooga Sandstone|36751|6|Mentioned|p488|||||||||
12170|Mooga Sandstone|36827|6|Mentioned|p83|||||||||
12170|Mooga Sandstone|37117|5|Briefly described|p313|||||||||
12170|Mooga Sandstone|37995|4|Described|p65|||||||||
12170|Mooga Sandstone|38068|6|Mentioned|p71|||||||||
12170|Mooga Sandstone|39211|5|Briefly described|p31|||See also Fig.3||||||
12170|Mooga Sandstone|39212|5|Briefly described|p17|||Early Neocomian. See also p15.||||||13-JUN-22
12170|Mooga Sandstone|39215|6|Mentioned|p51|||Spore/pollen record||||||
12170|Mooga Sandstone|39218|6|Mentioned|p48|||Flora||||||
12170|Mooga Sandstone|39315|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39445|5|Briefly described|Table 10|||||||||
12170|Mooga Sandstone|39494|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|39914|6|Mentioned|p2|||||||||
12170|Mooga Sandstone|39943|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|39998|6|Mentioned|p192|||||||||
12170|Mooga Sandstone|40030|6|Mentioned|Fig.5|||||||||
12170|Mooga Sandstone|40245|6|Mentioned|Table 2|||||||||
12170|Mooga Sandstone|40249|6|Mentioned|p38|||Mention P41||||||
12170|Mooga Sandstone|40250|6|Mentioned|Fig.1|||||||||
12170|Mooga Sandstone|40541|3|Fully described|p110|||||||||
12170|Mooga Sandstone|40544|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|40666|4|Described|p358|||||||||
12170|Mooga Sandstone|40675|6|Mentioned|Table 9A|||||||||
12170|Mooga Sandstone|40687|6|Mentioned|p417|||||||||
12170|Mooga Sandstone|40926|6|Mentioned|p13|||||||||
12170|Mooga Sandstone|41057|6|Mentioned|p61|||||||||
12170|Mooga Sandstone|41060|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41061|6|Mentioned|Fig.6|||||||||
12170|Mooga Sandstone|41064|6|Mentioned|p60|||||||||
12170|Mooga Sandstone|41187|6|Mentioned|Fig.2|||||||||
12170|Mooga Sandstone|41188|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41210|5|Briefly described|Fig.3|||||||||
12170|Mooga Sandstone|41216|6|Mentioned|Fig.18|||||||||
12170|Mooga Sandstone|41246|6|Mentioned|Map legend|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|41247|6|Mentioned|Fig.7|||||||||
12170|Mooga Sandstone|41266|6|Mentioned|Fig.3|||||||||
12170|Mooga Sandstone|41681|6|Mentioned|p16|||||||||
12170|Mooga Sandstone|41712|6|Mentioned|p282|||||||||
12170|Mooga Sandstone|41992|4|Described|Fig.2 P183|||||||||
12170|Mooga Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
12170|Mooga Sandstone|42135|6|Mentioned|Fig.6 P357|||||||||
12170|Mooga Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
12170|Mooga Sandstone|42494|5|Briefly described|Table 1 P24|||||||||
12170|Mooga Sandstone|42634|6|Mentioned|Table 8 P34|||||||||
12170|Mooga Sandstone|43000|5|Briefly described|Fig.5,p112|||Of Blythesdale Group.||||||16-SEP-08
12170|Mooga Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
12170|Mooga Sandstone|43404|14|Not recorded|Table p11|Cretaceous|Jurassic|||||||
12170|Mooga Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group.  Misspelling of Mooga Formation?||||||
12170|Mooga Sandstone|43883|14|Not recorded|p18 Fig.4-3|||||||||
12170|Mooga Sandstone|43991|5|Briefly described|p50|Cretaceous|Jurassic|Part of the "Blythesdale Group".||||||
12170|Mooga Sandstone|43995|14|Not recorded|p13,57,58,Fig.5|||Part of Blythesdale Group.||||||
12170|Mooga Sandstone|44021|14|Not recorded|p233,238|||Equivalent to "Hooray Sandstone" in Eromanga Basin.||||||
12170|Mooga Sandstone|44087|14|Not recorded|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44088|4|Described|p6|||Equivalent to part of Blythesdale Group on Betoota sheet.||||||
12170|Mooga Sandstone|44091|14|Not recorded|p60||Cretaceous|||||||
12170|Mooga Sandstone|44171|14|Not recorded|p194|||||||||
12170|Mooga Sandstone|44375|14|Not recorded|p310,311|||Aquifer.||||||
12170|Mooga Sandstone|44377|1|Redefined|p2,7-11,15|||Redefined as Mooga Sandstone Member. Of Blythesdale Formation.||||||
12170|Mooga Sandstone|44915|14|Not recorded|p18|||Ref. to Day 1964, Whitehouse 1955, Vine and Day 1965. Equivalent to Village Well Formation in South Australia. No age given.||||||
12170|Mooga Sandstone|45103|6|Mentioned|p6|||||||||
12170|Mooga Sandstone|45110|2|Defined|p105|Early Cretaceous|Early Cretaceous|See also p9 and p24.||||||13-JUN-22
12170|Mooga Sandstone|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
12170|Mooga Sandstone|46791|5|Briefly described|p42|||||||||
12170|Mooga Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
12170|Mooga Sandstone|46984|6|Mentioned|Table 1|||||||||
12170|Mooga Sandstone|48634|14|Not recorded|p6,20||Late Jurassic|See also Fig.2,6, Pl.1,2 p5,19. Upper Jurassic. (G54-14).||||||
12170|Mooga Sandstone|48919|4|Described|p70|||See also Table 5||||||
12170|Mooga Sandstone|48920|6|Mentioned|Table 7|||Refers Exon & Vine (1970)||||||
12170|Mooga Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
12170|Mooga Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
12170|Mooga Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
12170|Mooga Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|63979|5|Briefly described|p40, p44|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
12170|Mooga Sandstone|64197|6|Mentioned|p630 Fig.7|Early Cretaceous|Early Cretaceous|||||Underlies Bungil Formation; overlies Orallo Formation.||
12170|Mooga Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|64856|3|Fully described|p79, p95-98|Valanginian|Berriasian|Surat Basin. Of Reeves (1947). Renamed Mooga Sandstone Member (of Blythesdale Formation) by Day (1964), with a type area along Blyth Creek, 24-34km ENE of Roma. Renamed back to Mooga Sandstone by Exon and Vine (1970) with a new type area near the junction of Bungil and Mooga-Mooga Creeks, 16km N of Roma. Overlies Orallo Formation conformably, locally disconformably. Grades into upper Hooray Sandstone to the west. Is overlain conformably by Bungil Formation. Age from palynofloral units APK1, 21. <168m. Sublabile to quartzose sandstone, minor siltstone.|| ||||29-NOV-17
12170|Mooga Sandstone|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|64858|6|Mentioned|p187-188|||See also Mooga Formation.||||||16-MAR-12
12170|Mooga Sandstone|65003|4|Described|p1,p13, p14, p25|Cretaceous|Cretaceous|||||Overlies the Orallo Formation and the Boondooma Igneous Complex|Fine to medium-grained fawn sandstone that weathers yellow and brown.|
12170|Mooga Sandstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin. Underlies the Bungil Formation, overlies the Orallo Formation.||||||22-MAR-12
12170|Mooga Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Orallo Formation, underlies the Bungil Formation.||||||
12170|Mooga Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
12170|Mooga Sandstone|65116|5|Briefly described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Bungil Formation, Overlies the Orallo Formation, Surat Basin.||||||
12170|Mooga Sandstone|65119|5|Briefly described|Fig 2 p503, Fig 7- 8, 14, 16-19|Early Cretaceous |Early Cretaceous|Surat Basin. Quartzose to lithic sandstone, some mud and siltstone, up to 300m thick.||||||
12170|Mooga Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|66915|5|Briefly described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Surat Basin.||||||12-JAN-17
12170|Mooga Sandstone|67133|5|Briefly described|p17, p21|Cretaceous|Cretaceous|Not included in this study. Part of the final cycle of deposition under fluvial conditions in the Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|67402|4|Described|p146 fig SRT3, p148, p156|Barremian|Tithonian|Surat Basin. Deposited in a braided or meandering fluvial environment. Approximately 178m thick.||Blythesdale Group||Overlies the Orallo Formation. Overlain by the Bungil Formation.|Sandstone, minor clay, siltstone and mudstone.|
12170|Mooga Sandstone|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Bungil Formation. Underlain by Orallo Formation.||
12170|Mooga Sandstone|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68004|6|Mentioned|p174, p175.|||Major aquifer for water production; excellent quality reservoir. Sealed by Wallumbilla Formation shales. A major hydrocarbon exploration target. See also reference to Mooga Formation p87.||||||
12170|Mooga Sandstone|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluvial environment.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone; minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Early Cretaceous|Surat Basin (NSW and QLD): contains plant macrofossils in the latter.||||Overlies Orallo Formation|Silty sandstone.|14-SEP-17
12170|Mooga Sandstone|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil, Orallo and Southlands Formations; Gubberamunda, Hooray and Longsight Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
12170|Mooga Sandstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Early Cretaceous|Fluvial deposits. One of the main artesian aquifers in the map area.||||Overlies Orallo Formation. Is overlain by Bungil Formation.|Quartzose, sub-labile sandstone, minor siltstone, shale, mudstone and coal.|
12170|Mooga Sandstone|68734|6|Mentioned|p218 Fig.2, p221 Fig.3|||Surat Basin. Fluvial. Pre-Barremian age.||||||16-JAN-17
12170|Mooga Sandstone|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Orallo Formation. Overlain by the Bungil Formation.||
12170|Mooga Sandstone|69594|5|Briefly described|p519, p527, p537-538, p573|Hauterivian|Valanginian|Reeves (1947); Exon and Vine (1970). Northern Surat Basin. Braided to meandering stream deposits. Up to 168m thick. An important local aquifer in the Roma district.||||Conformably overlies Orallo Formation, locally disconformably. Is overlain conformably by Bungil Formation. Equivalent to/laterally grades into Hooray Sandstone and Kumbarilla beds.|Three subunits: a lower sublabile to quartzose sandstone that is commonly conglomeratic; a middle mudstone; and an upper subunit of interbedded fine sublabile sandstone and siltstone.|
12170|Mooga Sandstone|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
12170|Mooga Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
12170|Mooga Sandstone|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal.||||||
12170|Mooga Sandstone|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p33, p80|Early Cretaceous|Jurassic|Surat Basin.  Aquifer: generally artesian. Appears as Mooga Sandstone Member in Fig.2.6.||||Overlies Walloon Coal Measures and Orallo Formation. Is overlain by Bungil Formation or Cadna-owie Formation.||
12170|Mooga Sandstone|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Berriasian-Valanginian.||||Overlies Orallo Formation. Is overlain by Bungil Formation.||
12170|Mooga Sandstone|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
12170|Mooga Sandstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Orallo FZ. Is overlain by Kingull Member (Bungil FZ).||
12170|Mooga Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Cretaceous|Shown as located in the Surat Basin, both Qld and NSW.||||Overlies Orallo Formation||
12170|Mooga Sandstone|73113|5|Briefly described|p. 22-24, 36-37, 41, 43, 69, 80, 88...|||Surat Basin. Regional aquifer. More locations: p. 116-117, 119, 146, 151-152, 160, 169-173, 177-178, 191.||||||
12170|Mooga Sandstone|73193|6|Mentioned|p369|Hauterivian|Valanginian|Surat Basin.||||Underlain by Orallo Formation. Overlain by Bungil Formation.||
12187|Moolayember Formation|13516|5|Briefly described|p159 fig 8, p160-164, p169, p170, p138|Middle Triassic|Middle Triassic|From Bowen Basin, Galilee Basin. Age: APT3|||Includes Snake Creek Mudstone Member, ?Showgrounds Sandstone Member|Diachronous contact with underlying Showgrounds Sandstone.||
12187|Moolayember Formation|22464|6|Mentioned|p9||Middle Triassic|Overlies Clematis Sandstone||||||
12187|Moolayember Formation|22757|4|Described|Table4,p9|Late Triassic|Middle Triassic|130 m thick. Conformable on Clematis Sandstone.||||||27-OCT-08
12187|Moolayember Formation|22857|6|Mentioned|p315 Fig. 22.8|||||||||
12187|Moolayember Formation|22865|6|Mentioned|Fig22.8p315|||||||||
12187|Moolayember Formation|22973|5|Briefly described|p13 Fig.2 (i)|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
12187|Moolayember Formation|22976|5|Briefly described|p42 Fig.4|Triassic|Triassic|||||||
12187|Moolayember Formation|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
12187|Moolayember Formation|23052|5|Briefly described|Map Legend|Triassic|Triassic|||||||
12187|Moolayember Formation|23161|4|Described|p33 table4 fig11||Triassic|||||||
12187|Moolayember Formation|23425|6|Mentioned|p391.|||||||||
12187|Moolayember Formation|23430|5|Briefly described|p514|||Underlying Unit Clematis Group. Bowen Basin Province.||||||
12187|Moolayember Formation|23740|6|Mentioned|p1221|||Geological Province: Bowen Basin||||||
12187|Moolayember Formation|23883|5|Briefly described|p129 Fig. 11.2|Triassic|Triassic|Age: 251-205Ma.  Geological Province: Great Australian Superbasin.||||||
12187|Moolayember Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Triassic|Geological Province: Great Artesian Basin.||||||
12187|Moolayember Formation|24069|5|Briefly described|p284|Middle Triassic|Middle Triassic|Geological Province: Surat Basin.||||||
12187|Moolayember Formation|24071|5|Briefly described|p319|Triassic|Triassic|Geological Province: Galilee Basin.||||||
12187|Moolayember Formation|24077|5|Briefly described|p411 Tb. 2|Middle Triassic|Early Triassic|Of Mimosa Group.  Max. thickness: 315m.  Geological Province: Bowen Basin.||||||
12187|Moolayember Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
12187|Moolayember Formation|24093|5|Briefly described|p176 Fig. 2|Triassic|Triassic|Age: <235Ma. Overlies the Clematis Group. Geological Province: Bowen Basin.||||||29-JAN-08
12187|Moolayember Formation|24159|5|Briefly described|p148, Fig.2, p149|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin. Overlying Unit: Unconformity with Precipice Sandstone.||||||
12187|Moolayember Formation|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|28288|14|Not recorded|?|||||||||
12187|Moolayember Formation|29385|6|Mentioned|p80|||See also P81,82||||||
12187|Moolayember Formation|29387|6|Mentioned|Table 3|||Also Table 4. Triassic.||||||
12187|Moolayember Formation|29388|6|Mentioned|p62|||Stratigraphy.||||||
12187|Moolayember Formation|29389|6|Mentioned|p17|||||||||
12187|Moolayember Formation|29391|6|Mentioned|Table 4|||See P19.||||||
12187|Moolayember Formation|29393|6|Mentioned|Table 2|||Triassic.||||||
12187|Moolayember Formation|29410|6|Mentioned|p274|||Geological map. Triassic.||||||
12187|Moolayember Formation|29411|6|Mentioned|p202|||||||||
12187|Moolayember Formation|29591|6|Mentioned|Table 15|||||||||
12187|Moolayember Formation|29721|6|Mentioned|p65|||||||||
12187|Moolayember Formation|29869|6|Mentioned|p37|||||||||
12187|Moolayember Formation|30102|4|Described|p14|||See also P10,12,15. May occur as a shale interval under the Hutton Sandstone in P.S. Glenaras 1.||||conformably overlies Clematis Sandstone. Unconformably overlain by Hutton Sandstone||08-FEB-13
12187|Moolayember Formation|30103|6|Mentioned|p8|||||||||
12187|Moolayember Formation|30455|5|Briefly described|p1|||See also P2-3. Triassic age||||||
12187|Moolayember Formation|30456|6|Mentioned|p95|||||||||
12187|Moolayember Formation|30457|6|Mentioned|p96|||||||||
12187|Moolayember Formation|30458|6|Mentioned|p3|||Middle Triassic age||||||
12187|Moolayember Formation|30459|6|Mentioned|p309|||||||||
12187|Moolayember Formation|30460|6|Mentioned|p1|||See also P3-7,9-16,19,20,22,26, Fig.1. Triassic age||||||
12187|Moolayember Formation|30465|6|Mentioned|p4|||||||||
12187|Moolayember Formation|30466|6|Mentioned|p4|||Triassic age||||||
12187|Moolayember Formation|30468|6|Mentioned|p383|||||||||
12187|Moolayember Formation|30472|6|Mentioned|p134|||Correlation||||||
12187|Moolayember Formation|30473|6|Mentioned|p377|||Similar miospore assemblage to that in Esk Formation.||||||
12187|Moolayember Formation|30475|6|Mentioned|p164|||||||||
12187|Moolayember Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
12187|Moolayember Formation|30546|14|Not recorded|p107|Late Triassic|Middle Triassic|Correlation.||||||
12187|Moolayember Formation|30565|6|Mentioned|p134|||||||||
12187|Moolayember Formation|30691|4|Described|p14|||See also Table 4,6. Middle-Upper Triassic age||||||
12187|Moolayember Formation|30692|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
12187|Moolayember Formation|30696|4|Described|Table 3|||Middle-Upper Triassic||||||
12187|Moolayember Formation|30699|6|Mentioned|p53|||Stratigraphic relationships||||||
12187|Moolayember Formation|30701|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
12187|Moolayember Formation|30853|6|Mentioned|p9|||Penetrated in Bury No.1||||||
12187|Moolayember Formation|30854|4|Described|Table 3|||Middle-Upper Triassic age||||||
12187|Moolayember Formation|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|30915|6|Mentioned|Table|||Shown on table for stratigraphic drilling||||||
12187|Moolayember Formation|31079|6|Mentioned|Fig. 6|||||||||
12187|Moolayember Formation|31115|4|Described|p32|||See also P33-34. Triassic||||||
12187|Moolayember Formation|31116|4|Described|p20|||See also P1. Middle Triassic||||||
12187|Moolayember Formation|31117|6|Mentioned|p378|||Mid Triassic||||||
12187|Moolayember Formation|31120|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|31121|6|Mentioned|p388|||||||||
12187|Moolayember Formation|31145|6|Mentioned|p7|||||||||
12187|Moolayember Formation|31305|6|Mentioned|Fig. 1|||||||||
12187|Moolayember Formation|31369|4|Described|p31|||See also P32-40. Triassic.||||||
12187|Moolayember Formation|31425|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|31553|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|31979|6|Mentioned|p22|||||||||
12187|Moolayember Formation|32136|6|Mentioned|p2|||Geol. map near Mundubbera No.1. Triassic||||||
12187|Moolayember Formation|32138|6|Mentioned|p393|||||||||
12187|Moolayember Formation|32193|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|32276|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper Triassic.M - U||||||
12187|Moolayember Formation|32490|4|Described|Table 1|||U.-M.Triassic||||||
12187|Moolayember Formation|32493|6|Mentioned|Map legend|Triassic|Triassic|||||||
12187|Moolayember Formation|32553|4|Described|p40|||||||||
12187|Moolayember Formation|32577|6|Mentioned|p25|||Mid. or Late Triassic||||||
12187|Moolayember Formation|32944|6|Mentioned|p703|||Triassic||||||
12187|Moolayember Formation|33059|4|Described|Table 1|||See also Fig.4. Middle Triassic||||||
12187|Moolayember Formation|33078|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33079|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33086|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33091|5|Briefly described|p8|||Stratigraphy||||||
12187|Moolayember Formation|33092|5|Briefly described|p6|||Strat. table||||||
12187|Moolayember Formation|33096|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33366|6|Mentioned|Fig.3|||Triassic.||||||
12187|Moolayember Formation|33372|4|Described|p21|||From wells. Mention P16.||||||
12187|Moolayember Formation|33381|6|Mentioned|p115|||Triassic.||||||
12187|Moolayember Formation|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic||||||08-FEB-13
12187|Moolayember Formation|33530|5|Briefly described|Table 1|||Middle Triassic||||||
12187|Moolayember Formation|33638|6|Mentioned|p8|||||||||
12187|Moolayember Formation|33639|5|Briefly described|p10|||M.-U.Triass.||||||
12187|Moolayember Formation|33640|4|Described|Table 3|||Triassic.||||||
12187|Moolayember Formation|33644|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33645|6|Mentioned|Map legend|Triassic|Triassic|Mimosa Gp.||||||
12187|Moolayember Formation|33646|5|Briefly described|p11|||||||||
12187|Moolayember Formation|33647|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|33648|5|Briefly described|p18|||||||||
12187|Moolayember Formation|33672|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|33673|4|Described|p287|||||||||
12187|Moolayember Formation|33675|4|Described|p412|||Lithology.||||||
12187|Moolayember Formation|33774|6|Mentioned|p42|||Correlation||||||
12187|Moolayember Formation|34009|6|Mentioned|p109|||||||||
12187|Moolayember Formation|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
12187|Moolayember Formation|34061|6|Mentioned|p53|||||||||
12187|Moolayember Formation|34065|6|Mentioned|p9|||Triassic||||||
12187|Moolayember Formation|34091|6|Mentioned|p4|||Triassic||||||
12187|Moolayember Formation|34133|6|Mentioned|p1|||Triassic. See also PP2-5,28||||||
12187|Moolayember Formation|34172|6|Mentioned|p53|||Triassic.||||||
12187|Moolayember Formation|34174|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper Triassic||||||08-FEB-13
12187|Moolayember Formation|34212|6|Mentioned|p1|||See also PP2,3,4 etc. Upper Triassic.||||||
12187|Moolayember Formation|34218|6|Mentioned|p9|||Triassic||||||
12187|Moolayember Formation|34254|6|Mentioned|p484|||||||||
12187|Moolayember Formation|34314|5|Briefly described|Table 3|||Triassic||||||
12187|Moolayember Formation|34391|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle - Upper TriassicM - U||||||
12187|Moolayember Formation|34408|6|Mentioned|p185|||On table||||||
12187|Moolayember Formation|34452|6|Mentioned|p1|||M.Triassic. See also P5||||||
12187|Moolayember Formation|34543|6|Mentioned|p98|||||||||
12187|Moolayember Formation|34613|4|Described|Table 3|||||||||
12187|Moolayember Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
12187|Moolayember Formation|35095|6|Mentioned|p115|||||||||
12187|Moolayember Formation|35141|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|35148|6|Mentioned|p415|||||||||
12187|Moolayember Formation|35426|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|35428|6|Mentioned|p124|||Miospore assemblages||||||
12187|Moolayember Formation|35457|6|Mentioned|p633|||Also Fig.4 biostratigraphic relationships||||||
12187|Moolayember Formation|35467|6|Mentioned|Fig.1|||Solid geology map.||||||
12187|Moolayember Formation|35560|4|Described|p288|||||||||
12187|Moolayember Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
12187|Moolayember Formation|35873|6|Mentioned|p16|||||||||
12187|Moolayember Formation|35901|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|36103|6|Mentioned|Table 4|||||||||
12187|Moolayember Formation|36233|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|36243|6|Mentioned|p74|||See also Table 3A.||||||
12187|Moolayember Formation|36570|6|Mentioned|p22|||||||||
12187|Moolayember Formation|36899|6|Mentioned|p1085|||||||||
12187|Moolayember Formation|36914|6|Mentioned|p87|||||||||
12187|Moolayember Formation|36921|6|Mentioned|p175|||See also Table 1.||||||
12187|Moolayember Formation|37065|5|Briefly described|p36|||||||||
12187|Moolayember Formation|37070|5|Briefly described|p70|||||||||
12187|Moolayember Formation|37075|5|Briefly described|Table 1|||||||||
12187|Moolayember Formation|37078|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|37108|6|Mentioned|p282|||||||||
12187|Moolayember Formation|37288|6|Mentioned|p41|||||||||
12187|Moolayember Formation|37451|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|37610|6|Mentioned|p302|||See also Fig.3.||||||
12187|Moolayember Formation|37612|6|Mentioned|Fig.1|||See also Fig.3.||||||
12187|Moolayember Formation|37705|6|Mentioned|Fig.1|||||||||
12187|Moolayember Formation|37749|6|Mentioned|p186|||||||||
12187|Moolayember Formation|37755|6|Mentioned|p79|||||||||
12187|Moolayember Formation|37757|6|Mentioned|p29|||||||||
12187|Moolayember Formation|37996|6|Mentioned|p77|||||||||
12187|Moolayember Formation|38306|6|Mentioned|p509|||||||||
12187|Moolayember Formation|38358|4|Described|p1|||||||||
12187|Moolayember Formation|38518|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|39212|4|Described|p15|||||||||
12187|Moolayember Formation|39217|6|Mentioned|p50|||Refers Evans(1966). Miospores P51||||||
12187|Moolayember Formation|39252|6|Mentioned|p26|||||||||
12187|Moolayember Formation|39261|6|Mentioned|Fig. 9|||||||||
12187|Moolayember Formation|39275|6|Mentioned|p332|||||||||
12187|Moolayember Formation|39298|6|Mentioned|p255|||||||||
12187|Moolayember Formation|39445|5|Briefly described|Table 9|||||||||
12187|Moolayember Formation|39478|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|39491|4|Described|p23|||||||||
12187|Moolayember Formation|39494|6|Mentioned|p129|||||||||
12187|Moolayember Formation|39757|6|Mentioned|p1601|||||||||
12187|Moolayember Formation|39815|6|Mentioned|p445|||||||||
12187|Moolayember Formation|39943|6|Mentioned|Table 5A|||||||||
12187|Moolayember Formation|40030|6|Mentioned|p135|||||||||
12187|Moolayember Formation|40095|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|40120|4|Described|p428|||||||||
12187|Moolayember Formation|40123|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|40245|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|40249|6|Mentioned|p38|||||||||
12187|Moolayember Formation|40250|4|Described|p30|||||||||
12187|Moolayember Formation|40375|6|Mentioned|p133|||||||||
12187|Moolayember Formation|40539|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|40541|3|Fully described|p108|||||||||
12187|Moolayember Formation|40544|6|Mentioned|p157|||||||||
12187|Moolayember Formation|40574|6|Mentioned|p5|||||||||
12187|Moolayember Formation|40623|5|Briefly described|p80|||||||||
12187|Moolayember Formation|40634|6|Mentioned|p32|||||||||
12187|Moolayember Formation|40675|6|Mentioned|p306|||Mention Table 5A||||||
12187|Moolayember Formation|40687|6|Mentioned|Table 3|||||||||
12187|Moolayember Formation|40767|4|Described|p14|||||||||
12187|Moolayember Formation|40789|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|40832|3|Fully described|p450|||||||||
12187|Moolayember Formation|40999|6|Mentioned|p303|||||||||
12187|Moolayember Formation|41059|6|Mentioned|p168|||||||||
12187|Moolayember Formation|41097|6|Mentioned|p165|||||||||
12187|Moolayember Formation|41116|4|Described|p433|||||||||
12187|Moolayember Formation|41188|6|Mentioned|p231|||||||||
12187|Moolayember Formation|41191|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|41198|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|41210|3|Fully described|p157|||||||||
12187|Moolayember Formation|41211|6|Mentioned|p176|||||||||
12187|Moolayember Formation|41246|6|Mentioned|Map legend|Triassic||||||||
12187|Moolayember Formation|41247|6|Mentioned|p127|||See also Fig.7||||||
12187|Moolayember Formation|41266|6|Mentioned|Fig.3|||||||||
12187|Moolayember Formation|41330|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|41535|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41605|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41707|6|Mentioned|p166|||||||||
12187|Moolayember Formation|41710|6|Mentioned|Fig.2|||||||||
12187|Moolayember Formation|41712|6|Mentioned|Fig.6|||||||||
12187|Moolayember Formation|41725|6|Mentioned|p403|||||||||
12187|Moolayember Formation|42061|6|Mentioned|p150|||||||||
12187|Moolayember Formation|42067|4|Described|Appendix 2|||See also Fig.2 P309||||||
12187|Moolayember Formation|42249|6|Mentioned|p23|||||||||
12187|Moolayember Formation|42447|6|Mentioned|p7|||||||||
12187|Moolayember Formation|42463|5|Briefly described|p176|||Bowen Basin||||||
12187|Moolayember Formation|42492|5|Briefly described|Table 2 P14|||||||||
12187|Moolayember Formation|42634|5|Briefly described|Table 2 P10|||||||||
12187|Moolayember Formation|42648|6|Mentioned|p41|||||||||
12187|Moolayember Formation|42701|5|Briefly described|p74|||||||||
12187|Moolayember Formation|42865|6|Mentioned|p18|||||||||
12187|Moolayember Formation|42911|5|Briefly described|p11|||||||||
12187|Moolayember Formation|42932|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|42999|5|Briefly described|Table 1,p90||Middle Triassic|||||||
12187|Moolayember Formation|43000|5|Briefly described|p108|||see also Fig.5,p112||||||
12187|Moolayember Formation|43072|5|Briefly described|p55|||||||||
12187|Moolayember Formation|43084|6|Mentioned|p16|||||||||
12187|Moolayember Formation|43105|5|Briefly described|p13|||||||||
12187|Moolayember Formation|43185|5|Briefly described|6||Triassic|||||||
12187|Moolayember Formation|43483|6|Mentioned|14||Triassic|||||||
12187|Moolayember Formation|43546|14|Not recorded|p123,p125|||||||||
12187|Moolayember Formation|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
12187|Moolayember Formation|43851|14|Not recorded|Tb p106,110,113|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
12187|Moolayember Formation|43920|14|Not recorded|p74|||||||||
12187|Moolayember Formation|43922|14|Not recorded|p326|||"The available evidence...suggests a late Lower Triassic or Middle Triassic age."||||||
12187|Moolayember Formation|43923|4|Described|p1-2||Triassic|||||||
12187|Moolayember Formation|43977|14|Not recorded|p576|||||||||
12187|Moolayember Formation|43982|14|Not recorded|Map Legend|||||||||
12187|Moolayember Formation|43987|14|Not recorded|p270,271,275,278|||||||||
12187|Moolayember Formation|43988|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|43989|14|Not recorded|Map Legend|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|43990|14|Not recorded|Map Legend||Triassic|Part of Mimosa Group||||||
12187|Moolayember Formation|43994|14|Not recorded|Map Legend|||||||||
12187|Moolayember Formation|43996|14|Not recorded|p88|||||||||
12187|Moolayember Formation|43997|14|Not recorded|p113|||||||||
12187|Moolayember Formation|43998|4|Described|p13,17,map||Triassic|||||||
12187|Moolayember Formation|44007|14|Not recorded|p49,51|||||||||
12187|Moolayember Formation|44022|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|44023|4|Described|Tb.3,p10||Triassic|||||||
12187|Moolayember Formation|44068|14|Not recorded|p17|||||||||
12187|Moolayember Formation|44091|14|Not recorded|p53,54||Triassic|||||||
12187|Moolayember Formation|44095|14|Not recorded|p283-286|||||||||
12187|Moolayember Formation|44103|14|Not recorded|p215|||||||||
12187|Moolayember Formation|44115|14|Not recorded|p17-20|||||||||
12187|Moolayember Formation|44116|14|Not recorded|p24,28|||||||||
12187|Moolayember Formation|44118|14|Not recorded|Map Legend||Triassic|||||||
12187|Moolayember Formation|44124|14|Not recorded|p4|||||||||
12187|Moolayember Formation|44129|14|Not recorded|p95-96||Triassic|||||||
12187|Moolayember Formation|44130|14|Not recorded|p280-283|||||||||
12187|Moolayember Formation|44133|6|Mentioned|p86|||Of the Galilee and Bowan Basins.||||||
12187|Moolayember Formation|44166|14|Not recorded|p8|||||||||
12187|Moolayember Formation|44169|2|Defined|Tb.1,6,8,9,12,map|||||||||
12187|Moolayember Formation|44170|2|Defined|p1,17,19-22,25,31,||Triassic|24-40,57,Pl.1,Tb.1,map||||||
12187|Moolayember Formation|44172|14|Not recorded|p1339|||||||||
12187|Moolayember Formation|44207|14|Not recorded|p115|||||||||
12187|Moolayember Formation|44243|14|Not recorded|p649,map||Triassic|||||||
12187|Moolayember Formation|44245|5|Briefly described|Map Legend||Triassic|||||||
12187|Moolayember Formation|44337|5|Briefly described|Map Legend||Triassic|Lithology.||||||
12187|Moolayember Formation|44381|14|Not recorded|p7|||||||||
12187|Moolayember Formation|44390|14|Not recorded|p6,8,14,Tb.1|Late Triassic|Middle Triassic|Of Mimosa Group.||||||
12187|Moolayember Formation|44391|14|Not recorded|Map Legend|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|44414|14|Not recorded|p114,-115|Late Triassic|Middle Triassic|||||||
12187|Moolayember Formation|44419|14|Not recorded|p274||Triassic|||||||
12187|Moolayember Formation|44420|14|Not recorded|p2,3,6,7,9,12-19,21,|||p22,24,Figs.14,15.||||||
12187|Moolayember Formation|44421|14|Not recorded|p6,9,10,13,15,18,19||Triassic|||||||
12187|Moolayember Formation|44422|14|Not recorded|p150,152,153|||(Middle-Late Triassic or Early Jurassic)||||||
12187|Moolayember Formation|44423|14|Not recorded|p21-22|||||||||
12187|Moolayember Formation|44426|14|Not recorded|p12||Triassic|Triassic, from macro and microfaunas.||||||
12187|Moolayember Formation|44573|14|Not recorded|p97||Triassic|||||||
12187|Moolayember Formation|44607|14|Not recorded|p35,36|||||||||
12187|Moolayember Formation|44608|14|Not recorded|p19||Jurassic|||||||
12187|Moolayember Formation|44610|14|Not recorded|p49,Tb.1|||||||||
12187|Moolayember Formation|44636|14|Not recorded|p164||Triassic|||||||
12187|Moolayember Formation|44640|14|Not recorded|p31|||||||||
12187|Moolayember Formation|44652|14|Not recorded|p70,73,74|||||||||
12187|Moolayember Formation|44668|14|Not recorded|p59,60|||||||||
12187|Moolayember Formation|44787|14|Not recorded|Tb.p12,124,diag.p126||Late Triassic|||||||
12187|Moolayember Formation|44892|14|Not recorded|p30|||||||||
12187|Moolayember Formation|45071|3|Fully described|p75|||On Table 14||||||
12187|Moolayember Formation|45073|6|Mentioned|p59|||Strat. table||||||
12187|Moolayember Formation|45095|6|Mentioned|p18|||Refers Malone et al. (1969)||||||
12187|Moolayember Formation|45110|3|Fully described|Table 17|||See also Fig.5.||||||
12187|Moolayember Formation|46881|6|Mentioned|Table 2|||||||||
12187|Moolayember Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
12187|Moolayember Formation|46989|5|Briefly described|Table 1|||||||||
12187|Moolayember Formation|48585|4|Described|p1,7,8,10,14,15,Pl.1|||||||||
12187|Moolayember Formation|48600|14|Not recorded|p13,20|||Springsure area.||||||
12187|Moolayember Formation|48606|14|Not recorded|p5,6,14,22|||(H/55-8 ; G55-12). Pl.1 sh.2.||||||
12187|Moolayember Formation|48611|4|Described|p7-9,12,16|||||||||
12187|Moolayember Formation|48626|14|Not recorded|Fig.1||Triassic|||||||
12187|Moolayember Formation|48898|6|Mentioned|p54|||Triassic||||||
12187|Moolayember Formation|48900|3|Fully described|p45|||Triassic.||||||
12187|Moolayember Formation|48919|2|Defined|p33|Late Triassic|Middle Triassic|See also P34-35. Middle - Upper Triassic.M - U||||||
12187|Moolayember Formation|48920|3|Fully described|p35|||Triassic||||||
12187|Moolayember Formation|48951|6|Mentioned|Table 1|||||||||
12187|Moolayember Formation|48995|6|Mentioned|p24|||||||||
12187|Moolayember Formation|61076|5|Briefly described|p188 Fig. 2|Triassic|Triassic|Age: <240Ma. Geological Province: Bowen Basin, Taroom Trough.||||||
12187|Moolayember Formation|61313|6|Mentioned|p104 Table G1|||||||||
12187|Moolayember Formation|61377|5|Briefly described|p151|Middle Triassic|Middle Triassic|Consists of marine + non-marine interbedded sandstone, siltstone, shale and coal. A major hydrocarbon reservoir on western side of Surat Basin. Conformably overlies the Snake Creek Mudstone Member. Geol.Prov: Surat Basin. See also p139, p149 Fig. SU8.||||||07-FEB-11
12187|Moolayember Formation|61612|6|Mentioned|p276, p277, p270 Fig. 1|Middle Triassic|Middle Triassic|Includes Snake Creek Mudstone Member. Geological Province: Bowen Basin.  QLD.||||||17-MAR-09
12187|Moolayember Formation|61782|5|Briefly described|p281, p282|Middle Triassic|Middle Triassic|Geological Province: Taroom Trough. Alluvial and lacustrine sediments.||||||
12187|Moolayember Formation|62357|5|Briefly described|p524 Fig. 7, p528|Middle Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
12187|Moolayember Formation|63172|6|Mentioned|p329|||Includes microfloras in both upper and lower sequences. In the Mimosa Syncline.||||||07-FEB-11
12187|Moolayember Formation|63713|5|Briefly described|p1507 Fig.2|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Clematis Group and Warang Sandstone.||
12187|Moolayember Formation|64665|5|Briefly described|p53 Fig.2.|Middle Triassic|Middle Triassic|Galilee and Bowen Basins.||||Overlies Clematis Group.||
12187|Moolayember Formation|64856|3|Fully described|p41-42, p46, p51, p70, p72-79, p102|Middle Triassic|Middle Triassic|Originally the Moolayember Shale of Reeves (1947). Renamed as Moolayember Formation by Phillips (1960) and defined by Mollan et al. (1972). Bowen Basin, Galilee Basin. Datum for the top of the Triassic. Interbedded mudstones and sandstones. Contains Snake Creek Mudstone Member. Overlies Showgrounds Sandstone conformably and Arbroath beds unconformably. Unconformably overlain by Precipice Sandstone. Age from palynoflora (units APT31-34). Thickness <736m.|| ||||29-NOV-17
12187|Moolayember Formation|64857|4|Described|p126-127, 128-129, p113 Fig.3|Triassic|Triassic|Bowen Basin. Overlies Clematis Group. Contains the Snake Creek Mudstone Member at its base, which grades up into the upper part of the formation. Upper part divided into two informal subunits which are distinguishable in seismic reflection data.||||||
12187|Moolayember Formation|64858|6|Mentioned|p180 Fig.2, p181 Tb. 1, p182 Fig.3, p183|Middle Triassic|Middle Triassic|Bowen Basin.||||||30-NOV-09
12187|Moolayember Formation|64859|5|Briefly described|p222-4, 225, 226, 193, 195, 196, 199|Triassic|Triassic|Includes Snake Creek Mudstone Member. Potential oil, condensate and gas source rock, but mostly immature.||||||
12187|Moolayember Formation|65003|5|Briefly described|p6|||Of Bowen Basin.||||Overlies the Rewan Formation. (Overlies the Clematis Group?).|Sandstone.|30-MAR-12
12187|Moolayember Formation|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Middle Triassic|Overlies Clematis Group. Unit in the Bowen Basin.||||||14-SEP-09
12187|Moolayember Formation|65113|5|Briefly described|p347, Fig 4 p340|Middle Triassic|Middle Triassic|lithic sandstones, overlies the Clematis Group. Depositonal environment was a meandering river system.||||||
12187|Moolayember Formation|65114|5|Briefly described|p385 Fig.3, p383|Middle Triassic||Shown as Middle Triassic in the Fig.3 correlation chart but referred to as Early Triassic in the text; youngest unit in the Bowen Basin; upper part of Supersequence I||||||06-APR-10
12187|Moolayember Formation|65115|5|Briefly described|p425-426, 427, Fig 2 p403, Fig 14 p421|Late Triassic|Late Triassic|Overlies the Clematis Group and Showgrounds Sandstone in the Bowen Basin. Part of Supersequence I.||||||
12187|Moolayember Formation|65116|5|Briefly described|p451, Fig 2 p436|Middle Triassic|Middle Triassic|Overlies the Clematis Group and Showgrounds Sandstone in the Bowen Basin.||||||
12187|Moolayember Formation|65118|6|Mentioned|p493, Fig 2 p479|Middle Triassic|Middle Triassic|Overlies the Clematis Group in the Denison Trough and the Showgrounds Sandstone in the Taroom Trough, Bowen Basin.Youngest unit of the Bowen Basin.||||||06-MAR-12
12187|Moolayember Formation|65119|5|Briefly described|Table 1, Figs 6-8, 11-12 ,14, 16-19|Middle Triassic|Middle Triassic|Bowen Basin.  Mudstone, lithic sandstone, carbonaceous shale, conglomerate. Alluvial and lacustrine deposition up to 1650 m thick. Age: 231-240 Ma. Fission Track age: 105-183 Ma. See also misspelling Moolyember Formation p503.||||||07-MAR-12
12187|Moolayember Formation|65489|5|Briefly described|p144 Fig.53|Middle Triassic|Middle Triassic|Galilee Basin.||||Overlies Warang Sandstone and Clematis Formation.||
12187|Moolayember Formation|66188|6|Mentioned|441, 450, Fig 3, TB1, Fig 16-17|Middle Triassic|Late Permian|Of the Eromanga Basin, providing an upper age on the Galilee Basin deformation.||||||
12187|Moolayember Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Clematis Sandstone. Is unconformably overlain by Hutton, Blantyre and Precipice Sandstones.||
12187|Moolayember Formation|66615|6|Mentioned|p2 Fig.1, p2-4, p4 Fig.2, p5 Fig.3, p6-8|Triassic|Triassic|Green (1997). Age determined from palynological evidence. Denison and Southern Taroom Trough, Bowen Basin. Makes up most of subcrop beneath the Surat Basin. Known in company nomenclature as Wandoan Formation.|||Includes Snake Creek Mudstone Member.|Overlies Clematis Group.||
12187|Moolayember Formation|67133|5|Briefly described|p2, p5, p9, p19-21|Middle Triassic|Middle Triassic|Two samples of this unit were analysed by XRD and optical microscopy for this study. Both contained illite-rich mixed-layers. Fluvial deposits in an internally drained basin.||||Overlies Clematis Group. Is overlain by Precipice Sandstone.|Interbedded mudstones and coarse-grained lithic sandstones.|
12187|Moolayember Formation|67323|5|Briefly described|p81, p84, p92, p93 Fig.12.3|Triassic|Triassic|Galilee Basin.||||Conformably overlies Warang Sandstone. Is overlain by Hutton Sandstone.|Includes siltstone and carbonaceous coaly material.|
12187|Moolayember Formation|67402|4|Described|p18 fig WSD2|Ladinian|Anisian|Bowen Basin. Regional hydrocarbon (gas) or carbon dioxide storage seal. Deposited in a fluvial to lacustrine environment. Generally more than 100m thick. See also p19 fig WSD3, WSD4, p129 fig GLL9, p131 fig GLL12, p132, p133, p134, p147 fig SRT5, p21, p30, p30 fig PSA7, p31 fig PSA8, PSA9, p45, p48, p50 fig BWS4, p52, p53, p55-p57, p59, p62, p72, p80, p82 fig BWN4, p85 tbl BWN2, p124 fig GLL1, p125 tbl GLL1, p127 fig GLL5, p128 fig GLL8, p129, p135-138, p165 tbl LPB1, p300.||||Overlain by the Precipice Sandstone. Overlies the Snake Creek Mudstone, Warang Sandstone and Clematis Sandstone.|Coarsening upwards succession of mudstone, siltstone and volcanolithic sandstones.|
12187|Moolayember Formation|67669|5|Briefly described|p11|Middle Triassic|Middle Triassic|Of Bowen Basin.||Unit of Mimosa Group.||Overlain by Precipice Sandstone. Underlain by Clematis Formation. Laterally grades into Wandoan Sandstone.||
12187|Moolayember Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||||Overlies Clematis Group. Is unconformably overlain by Precipice Sandstone.||
12187|Moolayember Formation|68004|5|Briefly described|p172.|Middle Triassic|Middle Triassic|Petroleum-producing. Low reservoir potential because of extensive silicification and alteration of clays. Acts as a regional seal.||||||
12187|Moolayember Formation|68279|5|Briefly described|p1-4, p5 Tb.2, p7, p13-19|Ladinian|Anisian|Galilee Basin. A potential seal to the Clematis Group, a carbon geostorage target reservoir. Mineralogy of 104 samples was grouped into five major types which are described in some detail. Deposited by low-energy westerly-flowing fluvial systems. Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||Conformably overlies Clematis Group.||
12187|Moolayember Formation|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably underlain by the Clematis Group.|Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|68413|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably underlain by the Warang Sandstone.|Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin.||||Conformably overlies Clematis Group.||
12187|Moolayember Formation|68576|4|Described|Q_4: p1,p3,p7,p12, p14-15, p17, p21, p24|Middle Triassic|Middle Triassic|Youngest unit in the Bowen Basin. The overlying unconformity represents a 40 m.y. hiatus and separates the Bowen Basin from the Surat Basin. Sediments sourced from a volcanic province to the E. Mainly fine-grained sediments which weather to a flat terrain with no outcrops. Deposition in a dominantly fluvial-lacustrine environment; locally abundant acritarchs in the upper part indicate at least brackish conditions occasionally.|||Snake Creek Mudstone Member.|Overlies Clematis Group. Is unconformably overlain by the Precipice Sandstone.|Dominantly interbedded olive, green-brown and green-grey mudstones and lithic to sub-labile, medium- to coarse-grained sandstones. Lesser grey to black carbonaceous shale, siltstone, mudstone, coal, conglomerate; minor tuff and limestone.|
12187|Moolayember Formation|68679|5|Briefly described|p353, p364, p376-377, p381, p383-384|Triassic|Triassic|See also p391, p397, p469-470. Mollan et al. (1972); Dickins and Malone (1973). Connors-Auburn Province. Youngest unit in the Bowen Basin. Sediment was sourced from the east. 736m thick. Enclosed fluvial deposits with marginal alluvial fans, meandering streams and lakes. Minor gas producer.|||Snake Creek Mudstone Member.|Overlies the Clematis Group and the Showgrounds Sandstone.|Interbedded olive and greenish mudstone and lithic to sublabile, medium- to coarse-grained sandstone; grey to black carbonaceous shale, siltstone, mudstone, conglomerate.|
12187|Moolayember Formation|68731|5|Briefly described|p198, p201, pp200-201 Fig 3.110|Middle Triassic|Middle Triassic|Bowen Basin. Largely equivalent to the upper Warang Sandstone, but, in the Lovelle Depression this uppermost unit overlies the Warang Sandstone.||||Underlain by the Warang Sandstone.||
12187|Moolayember Formation|68901|6|Mentioned|p2 Fig. i|Triassic|Triassic|||||||27-SEP-18
12187|Moolayember Formation|69582|5|Briefly described|p35, p38, p65|||Surat Basin.||||Overlies the Showgrounds Sandstone and the Clematis Sandstone.|Sandstone.|
12187|Moolayember Formation|69591|6|Mentioned|p100|Middle Triassic|Middle Triassic|Bowen Basin. Mentioned as being age-equivalent to redbeds from boreholes drilled into the Canobie Depression, ~40km N of Cloncurry.||||||
12187|Moolayember Formation|69594|6|Mentioned|p534, p535 Fig.7.16|||||||Is overlain unconformably by Eddystone beds and Precipice Sandstone.||
12187|Moolayember Formation|69681|6|Mentioned|p82|||Mineralogy and likely chemical changes from CO2 injection discussed.||||||
12187|Moolayember Formation|69952|6|Mentioned|p85|Triassic|Triassic|||||||
12187|Moolayember Formation|70821|5|Briefly described|p80|||Basement to Eromanga, Surat Basins.||||Is overlain unconformably by Precipice Sandstone.||14-DEC-16
12187|Moolayember Formation|71264|6|Mentioned|p581 Fig.4|Triassic|Triassic|Bowen Basin.||||||
12187|Moolayember Formation|71265|6|Mentioned|p590|Triassic|Triassic|S Galilee Basin.||||||
12187|Moolayember Formation|71710|5|Briefly described|p370, p383, p384, p385 Fig 21, p387|Middle Triassic|Middle Triassic|Geological province: Galilee Basin. Overfill basin phase associated with thrust loading.||sequence 10.||Underlain, gradationally in places, by Clematis Group; locally underlain by Warang Sandstone?|Predominantly multicoloured lutites with labile sandstone and subordinate quartzose sandstone.|
12187|Moolayember Formation|71805|5|Briefly described|p80|Triassic|Triassic|Cored in Woleebee Creek GW4. Wireline logs exist for the core and for this unit.||||Overlain by the Precipice Sandstone.||
12187|Moolayember Formation|72088|4|Described|p6, p8, p15, p17, p21, p23, p91|Ladinian|Anisian|Galilee and Bowen basins. The thickest and most widespread unit across the entire basin. Deposited in a fluvio-lacustrine environment. Partly laterally equivalent to the Warang Sandstone. Compositionally very similar to the Clematis Group, although it is generally much finer grained, moderately to poorly sorted and with numerous sub-angular grains. Hosts calcite and siderite veins,||||Conformably overlies the Clematis Group and the Warang Sandstone.|Green, grey, brown, purple and red mudstone with minor siltstone and some pebbly sandstone.|
12187|Moolayember Formation|72297|5|Briefly described|p697, p744-745|Middle Triassic|Middle Triassic|Bowen Basin. A potential regional seal.|||Snake Creek Mudstone Member.||Includes minor coal.|
12187|Moolayember Formation|72298|5|Briefly described|p801|Jurassic|Triassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||||Overlies Clematis Sandstone. Is overlain unconformably by Hutton or Precipice Sandstones.||
12187|Moolayember Formation|73037|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|73038|5|Briefly described|Map legend|Middle Triassic|Middle Triassic||||||Micaceous lithic sandstone, micaceous siltstone.|
12187|Moolayember Formation|73113|5|Briefly described|p. 22-24, 31, 37, 41, 46, 49, 88, 98...|||Bowen Basin. Tight aquitard. More locations: p. 115-116, 119, 146, 151-153, 169-172, 177, 179, 191.||||Underlain by Clematis Sandstone. Unconformably overlain by Precipice Sandstone.||
12187|Moolayember Formation|73246|6|Mentioned|p190|Middle Triassic|Middle Triassic|Bowen Basin, northeast and northwest. Misspelt as Moolyamber Formation p190 Fig.2.||||Underlain by Clematis Group.||30-MAR-23
12187|Moolayember Formation|73304|6|Mentioned|p76|||||||||
12187|Moolayember Formation|73306|5|Briefly described|p565|||Bowen Basin.||||Correlated with Toogoolawah Group.||
12187|Moolayember Formation|73472|4|Described|p115-116, p120, p123, p125, p130-131|Carnian|Ladinian|Galilee Basin and Bowen Basin. Maximum thickness of ca 150 m. Fluvio-lacustrine depositional setting. [See article for palynology]. An age range of 240-231 Ma was suggested based on apatite fission-track dating.|240-231 Ma|||Underlain by and interfingers with the Warang Sandstone. Underlain by Clematis Sandstone and Clematis Group. Equivalent to Warang Sandstone.|Predominantly reddish-brown claystone and light greyish siltstone with less abundant light greyish medium- to coarse-grained cross-bedded sandstones in fining-upwards intervals.|
12187|Moolayember Formation|73600|5|Briefly described|p192, p198-200, p203-204|Middle Triassic|Middle Triassic|Bowen Basin, topmost unit. Deposited in a fast-subsiding foreland setting. Believed to be derived entirely from the New England Orogen, despite no published detrital geochronology. May be recycled into the Eddystone Beds of the overlying Surat Basin, meaning that the two may be difficult to distinguish from one another.||||Unconformably overlain by the Precipice Sandstone.||
12215|Moon Island Beach Subgroup|24121|5|Briefly described|p4, p115, 132, 227, 231|||||||||25-AUG-22
12215|Moon Island Beach Subgroup|31551|6|Mentioned|p92|||See also Table 1||||||
12215|Moon Island Beach Subgroup|36593|6|Mentioned|p187|||||||||
12215|Moon Island Beach Subgroup|39609|6|Mentioned|Table 1|||||||||
12215|Moon Island Beach Subgroup|39666|6|Mentioned|Table 20|||||||||
12215|Moon Island Beach Subgroup|41463|5|Briefly described|p38|||||||||
12215|Moon Island Beach Subgroup|42214|6|Mentioned|Table 1 P462|||||||||
12215|Moon Island Beach Subgroup|43344|14|Not recorded|p85||Permian|||||||
12215|Moon Island Beach Subgroup|43448|14|Not recorded|p224,226,230||Permian|Unit of Newcastle Coal Measures. Inc. Catherine Hill Bay and Eleebana Formations||||||
12215|Moon Island Beach Subgroup|67786|5|Briefly described|p94, 96|Permian|Permian|Sydney Basin. Late Permian. Alluvial fan and braided river systems; sediments sourced from New England Fold Belt immediately to the N.||Newcastle Coal Measures.|Wallarah, Great Northern, Fassifern seams; Mannering Park, Booragul, Awaba Tuffs; Teralba, Bolton Point Conglomerates.|Overlies Boolaroo Subgroup. Is overlain by Narrabeen Group.|Includes a number of coarse pebble conglomerates, with associated sandstones and shales; several tuffaceous units (ash fall and ash flow).|
12215|Moon Island Beach Subgroup|68711|5|Briefly described|p118, p116 Tbl 2|||Of McKenzie and Britten (1969). Replaced in part by Moon Island Beach Formation. See also p113.||Formerly of Newcastle Coal Measures|Included Fassifern Coal, Eleebana Formation, Great Northern Coal, Catherine Hill Bay Formation, Wallarah Coal.|||
12215|Moon Island Beach Subgroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Newcastle Coal Measures|||Conglomerate, tuff, siltstone, claystone, black coal.|
12226|Moonbah Tonalite|22815|4|Described|p49|Early Devonian|Late Silurian|||||||
12226|Moonbah Tonalite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
12226|Moonbah Tonalite|35109|2|Defined|p77|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
12226|Moonbah Tonalite|35263|6|Mentioned|Table 3|||||||||
12226|Moonbah Tonalite|36411|6|Mentioned|p269|||Refers White et al 1977 for definition.||||||
12226|Moonbah Tonalite|40328|4|Described|p209|||||||||
12226|Moonbah Tonalite|41898|6|Mentioned|p1184|||||||||
12226|Moonbah Tonalite|41905|2|Defined|p93|Silurian||||||||
12226|Moonbah Tonalite|41933|5|Briefly described|Map legend|Late Silurian||||||||
12226|Moonbah Tonalite|43233|5|Briefly described|Map Legend|Late Silurian||Age Middle - Late Silurian. Of Jindabyne Suite.||||||
12226|Moonbah Tonalite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh15||||||
12226|Moonbah Tonalite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
12278|Moorara Granite|42726|5|Briefly described|map legend|Carboniferous||42.||||||
12281|Moore Creek Limestone Member|721|5|Briefly described|Map legend|Frasnian|Givetian|Of the Yarrimie Formation (Tamworth Group).  Olistostromal limestone lenses.||||||11-MAR-11
12281|Moore Creek Limestone Member|5254|5|Briefly described|p124 Table 1, p126, 124, 123, 121|Givetian|Eifelian|Member of Yarrimie Formation, Tamworth Group. Age mid-Eifelian to earliest Givetian. See also Moore Creek Limestone p121, p122 Fig.1.||||||
12281|Moore Creek Limestone Member|22520|6|Mentioned|p17|Middle Devonian|Middle Devonian|||||||
12281|Moore Creek Limestone Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Givetian|Givetian|Of the Yarrimie Formation (Tamworth Group). Coralline biohermal limestone. Max. thickness: 60m. Geological Province: Tamworth Forearc Basin.||||||
12281|Moore Creek Limestone Member|23185|6|Mentioned|p157,Fig5p161|Givetian|Eifelian|||||||
12281|Moore Creek Limestone Member|23522|5|Briefly described|p249 Fig 5|Givetian|Eifelian|||||||
12281|Moore Creek Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
12281|Moore Creek Limestone Member|31999|6|Mentioned|Table 1|||||||||
12281|Moore Creek Limestone Member|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|M.-L.Dev.||||||
12281|Moore Creek Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
12281|Moore Creek Limestone Member|34403|6|Mentioned|p150|||||||||
12281|Moore Creek Limestone Member|34554|6|Mentioned|p234|||Fauna||||||
12281|Moore Creek Limestone Member|39331|6|Mentioned|Table 10-1|||||||||
12281|Moore Creek Limestone Member|43400|14|Not recorded|p178,179table2,180-1|||Ref.to Benson 1913||||||
12281|Moore Creek Limestone Member|43407|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition) Part of Yarrimie Formation of Tamworth Group||||||
12281|Moore Creek Limestone Member|43418|14|Not recorded|Map Legend|||||||||
12281|Moore Creek Limestone Member|43428|14|Not recorded|p140||Eifelian|List of fauna (U.Eifelian)||||||
12281|Moore Creek Limestone Member|61765|4|Described|p58 Fig. 1, p61, p62, p62 Fig. 4|Givetian|Eifelian|Of Yarrimie Formation. Max thickness: 150m. Geological Province: Tamworth Belt. See p62 for more information.||||||07-FEB-11
12281|Moore Creek Limestone Member|63118|5|Briefly described|p201, p202 Fig. 1|Middle Devonian|Middle Devonian|Of the Yarrimie Formation. Contains coral fauna.||||||
12281|Moore Creek Limestone Member|65214|6|Mentioned|p278|Devonian|Devonian|NSW, Tamworth. Appears in text as Moore Ck Limestone Member. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
12281|Moore Creek Limestone Member|65940|6|Mentioned|p200|Eifelian|Eifelian|Contains stromatoporoid bioherms.||Unit of Yarrimie Formation.||||
12281|Moore Creek Limestone Member|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian|||Unit in Yarrimie Formation.|||Massive biohermal coralline limestone, crinoidal, calcareous sedimentary rocks.|
12281|Moore Creek Limestone Member|68005|5|Briefly described|p52, p150.|Middle Devonian|Middle Devonian|This name is used in the Attunga region for a unit which, in the Loombrah and Timor region, is called the Timor Limestone. The rank 'Member' is omitted on p52.||Unit in Yarrimie Formation.|||Olistostromal limestone lenses in Yarrimie Formation.|
12281|Moore Creek Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|||Unit in Tamworth Group.||||
12281|Moore Creek Limestone Member|71628|6|Mentioned|p7:19|||||||Is intruded by Inlet Monzogranite.||
12289|Moorlands Lignite Member|10010|5|Briefly described|p12 Fig. 3|Middle Eocene|Middle Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||13-AUG-07
12289|Moorlands Lignite Member|22773|5|Briefly described|Fig24.8p352|Middle Eocene|Middle Eocene|||||||
12289|Moorlands Lignite Member|22799|5|Briefly described|p24 Fig.10|Late Eocene|Late Eocene|||||||
12289|Moorlands Lignite Member|22857|5|Briefly described|p325 Fig.24.8|Middle Eocene|Middle Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|22887|5|Briefly described|Fig.6 p13|Late Eocene|Late Eocene|||||||
12289|Moorlands Lignite Member|22893|5|Briefly described|fig4 p9|Oligocene|Oligocene|||||||
12289|Moorlands Lignite Member|23671|6|Mentioned|p3|||Supersedes the Moorlands Coal Measures of Ludbrook (1961).  Of the Renmark Beds.||||||
12289|Moorlands Lignite Member|23818|5|Briefly described|p174 Fig.84, p179|Late Eocene|Late Eocene|Geological Province: Murray Basin. Of the Renmark Beds (Knight Group). Also referred to as "Moorlands Coal Measures".||||||21-JAN-05
12289|Moorlands Lignite Member|23884|5|Briefly described|p155 Fig. 13.2|Late Eocene|Late Eocene|Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|30754|6|Mentioned|p13|||Distribution||||||
12289|Moorlands Lignite Member|30758|6|Mentioned|p166|||Middle-Upper Eocene age||||||
12289|Moorlands Lignite Member|31625|6|Mentioned|Fig. 5.2|||Eocene||||||
12289|Moorlands Lignite Member|34308|6|Mentioned|p179|||U.Eocene. Formerly "Moorlands C.M."||||||
12289|Moorlands Lignite Member|37132|5|Briefly described|p367|||||||||
12289|Moorlands Lignite Member|39329|6|Mentioned|Fig.1|||||||||
12289|Moorlands Lignite Member|42125|6|Mentioned|Fig.5 p132|||||||||01-NOV-22
12289|Moorlands Lignite Member|42130|6|Mentioned|Fig.3 p265|||||||||01-NOV-22
12289|Moorlands Lignite Member|42134|6|Mentioned|Fig.3 p335|||||||||01-NOV-22
12289|Moorlands Lignite Member|42137|6|Mentioned|Fig.2 p368|||||||||01-NOV-22
12289|Moorlands Lignite Member|42138|6|Mentioned|Fig.2 p390|||||||||01-NOV-22
12289|Moorlands Lignite Member|42717|6|Mentioned|map legend|Eocene|Paleocene|||||||
12289|Moorlands Lignite Member|42881|4|Described|Fig.3, P84|||||||||
12289|Moorlands Lignite Member|42966|2|Defined|Table 12|Late Eocene||of Olney Formation. Also of Renmark beds||||||
12289|Moorlands Lignite Member|43073|5|Briefly described|Table 3|||of Renmark Beds||||||
12289|Moorlands Lignite Member|43791|6|Mentioned|p372, Fig1|||||||||
12289|Moorlands Lignite Member|43804|6|Mentioned|Fig.2,p49|||||||||
12289|Moorlands Lignite Member|44133|5|Briefly described|p158|||Of the Olney Formation (Renmark Group). Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|49038|5|Briefly described|p37|||||||||
12289|Moorlands Lignite Member|49040|6|Mentioned|Fig.6|||||||||
12289|Moorlands Lignite Member|61155|5|Briefly described|p18|Early Oligocene|Late Eocene|Of the Olney Formation. Geological Province: Murray Basin.||||||
12289|Moorlands Lignite Member|65552|6|Mentioned|p5 Fig. 3|Late Eocene|Late Eocene|Spelt Moorlands Lignite Mbr in figure. Western Murray Basin. Of Olney Formation.||||||
12289|Moorlands Lignite Member|72445|6|Mentioned|App.7 p7.|Late Eocene|Late Eocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' as Moorlands Lignite Member (from Brown & Stephenson 1991). Shown as Moorland Lignite Member in the text.|||||Includes lignite.|
12289|Moorlands Lignite Member|73228|6|Mentioned|p54|||||Olney Formation, Renmark Group|||Lignite.|
12292|Moorna Formation|24551|6|Mentioned|p340|||||||||
12292|Moorna Formation|30994|6|Mentioned|Fig. 1|||||||||
12292|Moorna Formation|30996|2|Defined|p40|Pliocene|Pliocene|Below Blanchetown Clay||||||
12292|Moorna Formation|31385|6|Mentioned|Table 4|||||||||
12292|Moorna Formation|32007|4|Described|p154|||Late Pliocene or Early Peistocene. Palaeontology.||||||
12292|Moorna Formation|34906|6|Mentioned|p16|||||||||
12292|Moorna Formation|35272|5|Briefly described|p283|||||||||
12292|Moorna Formation|41537|6|Mentioned|p350|||||||||
12292|Moorna Formation|41848|5|Briefly described|p358|||Possibly equivalent to Irymple Member of Blanchetown Clay||||||
12292|Moorna Formation|42125|5|Briefly described|p138|||||||||
12292|Moorna Formation|42827|5|Briefly described|p358|||||||||
12292|Moorna Formation|42966|1|Redefined|Table 28, p173|Early Pleistocene|Late Pliocene|||||||
12292|Moorna Formation|50079|6|Mentioned|p45|Early Pleistocene|Early Pleistocene|||||||
12292|Moorna Formation|60540|5|Briefly described|p999,p1000 Fig.2,|Pliocene|Pliocene|In central-west Murray Basin. Magnetostratigraphic data on age.||||Grades laterally into Parilla Sand. Incised into underlying Loxton Sand.|River sands incised into Loxton Sand.|06-FEB-18
12292|Moorna Formation|68548|6|Mentioned|p13 Fig.2|Pliocene|Pliocene|Late Pliocene age.||||Laterally equivalent to the Parilla Sand and the upper Norwest Bend Formation.||
12332|Morgans Gully Siltstone|22472|6|Mentioned|p38 Fig.3(a)|Late Devonian|Devonian|of the Lambie Group||||||
12332|Morgans Gully Siltstone|22857|5|Briefly described|p492 App.1 Tb.A1.7||Late Devonian|Of the Lambie Group. Massive purple siltstone and mudstone, minor thin arenite. Max. thickness: >460m. Geological Province: Lambie Basin.||||||
12332|Morgans Gully Siltstone|23214|3|Fully described|p243|Late Devonian|Late Devonian|Of Lambie Group, Lambie Basin. Overlying unit: Shoalhaven Group, Underlying unit: Turon River Grits. Max. thickness: 460m.||||||
12332|Morgans Gully Siltstone|32708|6|Mentioned|Fig.2|||||||||
12332|Morgans Gully Siltstone|35166|6|Mentioned|Fig.3|||||||||
12332|Morgans Gully Siltstone|43641|5|Briefly described|Map Legend||Devonian|||||||
12332|Morgans Gully Siltstone|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Lambie Group.||||||
12332|Morgans Gully Siltstone|68592|5|Briefly described|p1753|||Watkins, in Pogson and Watkins, (1998). In the Bathurst 1:250 000 map area.||Topmost unit in Lambie Group.||Is correlated with Tarlo Formation.||
12332|Morgans Gully Siltstone|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|Shown as Morgan Gully Slts.||Lambie Group||||
12337|Morkalla Formation|22773|5|Briefly described|Fig24.5p350|Early Cretaceous|Early Cretaceous|||||||
12337|Morkalla Formation|22799|5|Briefly described|p19|||Millewa Group||||||
12337|Morkalla Formation|22857|5|Briefly described|p548 App.1 Tb.A1.12|Albian|Aptian|Of the Millewa Group. Interbedded siltstone, mudstone and minor sandstone. Max. thickness: >120m. Geological Province: Berri Basin. See also p350 Fig.24.5.||||||
12337|Morkalla Formation|22887|3|Fully described|Fig.5 p12, p31|Early Cretaceous|Early Cretaceous|Proposed equivalent to sedimentary units in Booligal. See also Table 5 p31. of Renmark Trough.||||||
12337|Morkalla Formation|22893|6|Mentioned|table 5||Early Cretaceous|||||||
12337|Morkalla Formation|24551|5|Briefly described|p270|||Of the Millewa Group.  Overlies: Taparoo Sandstone.||||||
12337|Morkalla Formation|30905|5|Briefly described|p146|||||||||
12337|Morkalla Formation|31745|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
12337|Morkalla Formation|37873|6|Mentioned|p1|||||||||
12337|Morkalla Formation|39211|6|Mentioned|p38|||See Fig.23||||||
12337|Morkalla Formation|41642|5|Briefly described|p216|||||||||
12337|Morkalla Formation|42318|6|Mentioned|Fig.5 P12|||Murray Basin||||||
12337|Morkalla Formation|42827|5|Briefly described|p216|||see also Table 7.3||||||
12337|Morkalla Formation|42966|2|Defined|Table 9|Albian|Aptian|of Millewa Group||||||
12337|Morkalla Formation|43218|4|Described|Fig.3 p22, p27|Albian|Aptian|Of Millewa Group.||||||
12337|Morkalla Formation|49038|5|Briefly described|p23|||||||||
12337|Morkalla Formation|49040|6|Mentioned|p8|||||||||
12337|Morkalla Formation|61314|5|Briefly described|p129|Cretaceous|Cretaceous|Lacustrine sequence of interbedded siltstone, mudstone and minor sandstone. Overlies the Taparoo Sandstone. Geological Province: Murray Basin.||||||
12350|Moroka Glen Formation|22436|6|Mentioned|p2|Late Devonian|Late Devonian|||||||
12350|Moroka Glen Formation|23307|5|Briefly described|Map Legend|Devonian|Devonian|Of Avon River Group||||||
12350|Moroka Glen Formation|23309|5|Briefly described|p171, 173-184. Tb 2.65|||O the Delatite Group.||||||
12350|Moroka Glen Formation|23710|14|Not recorded|p84|||Excursion details.||||||
12350|Moroka Glen Formation|24551|5|Briefly described|p88 Fig. 3.15, 172|Late Devonian|Late Devonian|Of Delatite Group.  Maximum Thickness: 300m.||||||
12350|Moroka Glen Formation|31706|6|Mentioned|p645|||Devonian correlation chart||||||
12350|Moroka Glen Formation|32399|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
12350|Moroka Glen Formation|32865|4|Described|p485|||||||||
12350|Moroka Glen Formation|33393|6|Mentioned|p173|||||||||
12350|Moroka Glen Formation|33602|6|Mentioned|p21|||||||||
12350|Moroka Glen Formation|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
12350|Moroka Glen Formation|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
12350|Moroka Glen Formation|35073|6|Mentioned|p24|||See also Table 5.||||||
12350|Moroka Glen Formation|35112|6|Mentioned|p280|||||||||
12350|Moroka Glen Formation|35277|3|Fully described|p99|||||||||
12350|Moroka Glen Formation|35281|6|Mentioned|p23|||||||||
12350|Moroka Glen Formation|37330|5|Briefly described|p19|||||||||
12350|Moroka Glen Formation|38367|6|Mentioned|p108|||||||||
12350|Moroka Glen Formation|40761|5|Briefly described|p237|||||||||
12350|Moroka Glen Formation|40995|6|Mentioned|Fig.31|||||||||
12350|Moroka Glen Formation|41571|5|Briefly described|Fig.2.6|||||||||
12350|Moroka Glen Formation|41641|4|Described|p169|||||||||
12350|Moroka Glen Formation|42089|5|Briefly described|p26|||||||||
12350|Moroka Glen Formation|42797|5|Briefly described|p49, Fig.3 p40|||||||||
12350|Moroka Glen Formation|42827|4|Described|p169|||see also Table 5.3||||||
12350|Moroka Glen Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
12350|Moroka Glen Formation|43547|14|Not recorded|Table p153||Frasnian|Part of Avon River Group||||||
12350|Moroka Glen Formation|44185|5|Briefly described|Map legend.|Late Devonian|Late Devonian|||Unit in Avon River Group.|||Fluvial: sandstone, conglomerate.|
12350|Moroka Glen Formation|44187|5|Briefly described|Map Legend||Late Devonian|||||||
12350|Moroka Glen Formation|61161|5|Briefly described|p125-126, p76-77 Fig 6.1|||Of Delatite Group. Overlies Moornapa Sandstone with strong angular unconformity. Concordantly underlies Wellington Volcanic Group. Non-magnetic, massive to thick-bedded deep red siltstone. GSV map code: Dadm.||||||
12350|Moroka Glen Formation|61169|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Delatite Group and Avon Supergroup. Alluvial flood plain and channel deposits: massive to thick-bedded red mudstone, well sorted minor sandstone and conglomerate; GSV map code: Dadm.||||||
12350|Moroka Glen Formation|61170|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Delatite Group and Avon Supergroup. Alluvial flood plain and channel deposits: massive to thick-bedded red mudstone, well sorted minor sandstone and conglomerate; GSV map code: Dadm.||||||07-FEB-11
12350|Moroka Glen Formation|61171|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Delatite Group and Avon Supergroup. Alluvial flood plain and channel deposits: massive to thick-bedded red mudstone, well sorted minor sandstone and conglomerate; GSV map code: Dadm.||||||
12350|Moroka Glen Formation|61172|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Delatite Group and Avon Supergroup. Alluvial flood plain and channel deposits: massive to thick-bedded red mudstone, well sorted minor sandstone and conglomerate; GSV map code: Dadm.||||||
12350|Moroka Glen Formation|61173|5|Briefly described|map legend|Late Devonian|Late Devonian|Of Delatite Group and Avon Supergroup. Mudstone, minor sandstone, conglomerate: no mappable gravity response; nonmagnetic; area of outcrop too small to determine radiometric response; GSV map code: Dadm.||||||
12350|Moroka Glen Formation|66252|6|Mentioned|p212.|||Relatively quartz-rich sandstone, pebbly conglomerate. Licola area.||||||
12350|Moroka Glen Formation|68116|5|Briefly described|Appendix, Maps 34-35, 43-44.|Late Devonian|Late Devonian||||||Conglomerate, pebbly sandstone, sandstone, and red and grey mudstone: upward fining sequence; clasts are well-rounded and consist of quartzite, sandstone, vein quartz, chert and minor mudstone in a quartzose or clayey matrix; sparse basalt flows.|
12364|Morundury Porphyries|36390|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
12371|Moruya Suite|22606|6|Mentioned|P827|||||||||
12371|Moruya Suite|22719|6|Mentioned|p486|||||||||
12371|Moruya Suite|22778|4|Described|p 164|||||||||
12371|Moruya Suite|22779|4|Described|p 172|||||||||
12371|Moruya Suite|22815|4|Described|p88,89||Middle Devonian|Age: 379Ma.||||||
12371|Moruya Suite|22857|6|Mentioned|p13, p14 Fig. 11.9|||Geological Province: Lachlan Fold Belt.||||||
12371|Moruya Suite|22933|6|Mentioned|p13,Fig11.9p14|||||||||
12371|Moruya Suite|23439|5|Briefly described|p124 fig.1|||||||||
12371|Moruya Suite|23549|5|Briefly described|Fig 4 p518.|||Comprises 6 north-south trending elongate plutons on eastern side of Bega Batholith.  Includes Tuross Head Tonalite (quartz diorites), Moruya Tonalite (predominantly toanlites and granodiorites) and Bodalla Monzogranite (felsic granites.||||||05-APR-05
12371|Moruya Suite|24222|5|Briefly described|p9|||Chemistry of samples reported. I-type granite.  Geological Province: Moruya Batholith, Lachlan Fold Belt.||||||
12371|Moruya Suite|24517|6|Mentioned|p47|||Of the Bega Batholith. Includes Tuross Head pluton.||||||
12371|Moruya Suite|38822|6|Mentioned|p198|||||||||
12371|Moruya Suite|41563|6|Mentioned|p506|||||||||
12371|Moruya Suite|42726|5|Briefly described|map legend||Silurian|||||||
12371|Moruya Suite|42855|6|Mentioned|p624|||||||||
12371|Moruya Suite|43233|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|||||||
12371|Moruya Suite|44093|5|Briefly described|p225 App. 1|Middle Devonian|Early Devonian|Orogenic granite. Geological Province: Lachlan Fold Belt.||||||
12371|Moruya Suite|60423|6|Mentioned|p374|||Geological Province: Lachlan Fold Belt. Of the Bega Batholith||||||
12371|Moruya Suite|62070|5|Briefly described|p33, p34 Fig.1, p39, p40|Middle Devonian|Middle Devonian|Chemically similar rocks dredged from offshore and dated. 381.0+/-9.6 Ma K/Ar hornblende, 372.4+/-7.6 Ma K/Ar biotite and 337.5+/-6.8 Ma K/Ar alkali feldspar. These dates indicate slow cooling at depth.|||Includes Nelligen Granodiorite.|||
12371|Moruya Suite|68255|5|Briefly described|p1049-p1052, p1054, p1062, p1063|Emsian|Emsian|Bega Batholith. High-level, low temperature suite in which the Tuross pluton is dated at 396.2 +/- 1.4 Ma (U-Pb zircon; Healy 2009).|396.2 +/- 1.4 Ma||Includes Comerong Volcanics and Buckenbowra Granodiorite.||I-type.|20-JUL-15
12371|Moruya Suite|70601|5|Briefly described|p23, p25, p30-31, p34, p43, p46, p55|Middle Devonian|Silurian|See also p57-58. Offshore extension of Lachlan Orogen. Other ages given. Melt sourced only from asthenosphere and Cambrian greenstones.|381 +/- 10 Ma: K/Ar hornblende.||||Granodiorite, I-type granite.|
12371|Moruya Suite|73264|6|Mentioned|p1405|||||||||
12372|Moruya Supersuite|42726|5|Briefly described|map legend|||||||||
12372|Moruya Supersuite|42827|6|Mentioned|p429|||||||||
12406|Mosmans Swamp Andesite|39666|6|Mentioned|p103|||||||||
12406|Mosmans Swamp Andesite|44244|5|Briefly described|p87|||Of the Gilmore Volcanic Group.  Formerly assigned to the "Volcanic Stage" of the "Kuttung Series" (Osborne, 1922) and then to the  "Gilmore Volcanics" (Roberts, 1961).||||||25-AUG-04
12438|Mount Ainslie Volcanics|22768|5|Briefly described|p176|||||||||
12438|Mount Ainslie Volcanics|22857|4|Described|p176, p462 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Hawkins Suite. At base banded dacitic tuff, agglomerate and thin shale beds; at top medium-grained massive dacitic tuff; contains trilobites, brachiopods. Max. thickness: 700m.||||||
12438|Mount Ainslie Volcanics|39975|6|Mentioned|Fig.1|||||||||
12438|Mount Ainslie Volcanics|41356|5|Briefly described|p46|||See also P78||||||
12438|Mount Ainslie Volcanics|42497|5|Briefly described|Map legend|Wenlockian|Wenlockian|Actually spelt Mt Ainslie Volcanics.||||||
12438|Mount Ainslie Volcanics|42727|5|Briefly described|map legend|Wenlock|Wenlock|Of Hawkins Volcanic Suite. Dacitic ingnimbrite, minor ashstone, agglomerate and shale. Overlies Canberra Formation; disconformably underlies Mount Painter Volcanics. BMR map symbol: Sma. Geol. Prov: Canberra Block.||||||
12438|Mount Ainslie Volcanics|42820|2|Defined|p22|Early Silurian||of Hawkins Volcanic Suite||||||
12438|Mount Ainslie Volcanics|43159|4|Described|Fig.2p4,p3,p8,p9.||Silurian|||||||
12438|Mount Ainslie Volcanics|68592|6|Mentioned|p428, p443, p457|||Abell (1991) after Opik (1958). Equivalent to, but not yet formally included in, the Douro Group.||||||
12451|Mount Alfred Granite|23309|6|Mentioned|p437 App 1|||G567 S-Type.||||||
12451|Mount Alfred Granite|24133|3|Fully described|p61|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
12451|Mount Alfred Granite|24142|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
12451|Mount Alfred Granite|24143|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
12451|Mount Alfred Granite|24144|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
12451|Mount Alfred Granite|24145|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Two-mica cordierite granite: grey, fine grained and equigranular; abundant small metasedimentary enclaves; S-type; nonmagnetic; weathered.||||||09-SEP-04
12451|Mount Alfred Granite|24146|5|Briefly described|Map Legend|Silurian|Silurian|Geological Province: Lachlan Fold Belt. Biotite-muscovite-cordierite granite: S-type; nonmagnetic; high K, variable low Th, Variable U.||||||09-SEP-04
12451|Mount Alfred Granite|33779|6|Mentioned|p163|||Geol. map||||||
12451|Mount Alfred Granite|39860|6|Mentioned|p17|||||||||
12451|Mount Alfred Granite|42726|5|Briefly described|map legend|||||||||
12451|Mount Alfred Granite|68116|5|Briefly described|Appendix, Map 20.|Pridoli|Wenlock||||||Two-mica cordierite granite: pale brownish grey, fine grained and equigranular; abundant small metasedimentary enclaves; S-type; nonmagnetic; weathered.|
12454|Mount Allen Granite|29987|5|Briefly described|p14|||||||||
12454|Mount Allen Granite|34449|4|Described|Table 2-1|||U.Silurian - L.Devonian||||||
12454|Mount Allen Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
12454|Mount Allen Granite|37772|5|Briefly described|p8|||||||||
12454|Mount Allen Granite|39627|6|Mentioned|Table 3|||||||||
12454|Mount Allen Granite|40269|4|Described|p141|||||||||
12454|Mount Allen Granite|40328|4|Described|p209|||||||||
12454|Mount Allen Granite|40913|6|Mentioned|Map legend|Lochkovian|Lochkovian|||||||
12454|Mount Allen Granite|41126|2|Defined|p79|Early Devonian|Early Devonian|||||||
12454|Mount Allen Granite|41528|6|Mentioned|p98|||||||||
12454|Mount Allen Granite|41821|6|Mentioned|p24|||In Mount Allen sheet area||||||
12454|Mount Allen Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
12454|Mount Allen Granite|43089|5|Briefly described|Map Legend|||[?] of Girilambone Group||||||
12454|Mount Allen Granite|43202|5|Briefly described|Table 2,p20.|||||||||
12454|Mount Allen Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
12454|Mount Allen Granite|63891|6|Mentioned|p240, p243 Fig.3|||Mount is Mt in text. Crops out adjacent to non-volcanic sedimentary rocks.||||||
12454|Mount Allen Granite|70751|6|Mentioned|p8, p10, p12, p24, p28, p38|Silurian|Silurian||422.8 +/- 2.7 Ma (SHRIMP, this study)|||Intrudes and gradational contact with Double Peak Volcanics.|Medium-grained, S-type granite.|23-SEP-19
12454|Mount Allen Granite|71039|6|Mentioned|p21, 25, 26|Silurian|Silurian|S-type.|422.8 +/- 2.7 Ma (Downes et al. 2016)|||||
12454|Mount Allen Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Micrographic, microporphyritic muscovite microgranite and subporphyritic biotite monzogranite with sparse metasedimentary xenoliths.|
12454|Mount Allen Granite|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Intrudes[?] Mount Hope Group. Equivalent to Gilgunnia Granite.||
12454|Mount Allen Granite|73578|6|Mentioned|p7, p14, p21|Pridoli|Ludfordian|Age of 422.8 +/- 2.7 Ma reported by Downes et al. (2016).|422.8 +/- 2.7 Ma|||||
12467|Mount Arrowsmith Volcanics|22671|3|Fully described|p838-39,841-42,847||Neoproterozoic III|These volcanics occur within the Kara beds. Previously mapped as part of Mount Wright Volcanics.  Max Age: 586 (+/-) 7 Ma. Mt Arrowsmith Volcanics in text.||||||17-JAN-06
12467|Mount Arrowsmith Volcanics|22772|5|Briefly described|p62,69,Table13.1|Neoproterozoic III|Neoproterozoic III|Max Age: 586 (+/-) 7 Ma.||||||
12467|Mount Arrowsmith Volcanics|22857|5|Briefly described|p62, Tb. 13.1 (insert p70-71)|Neoproterozoic III|Neoproterozoic III|Of the Kara beds. Age: 586+/-7Ma (U/Pb SHRIMP zircon). Geological Province: Kanmantoo Fold Belt. See also p402 App. 1 Tb.A1.3 and p94.||||||24-MAR-06
12467|Mount Arrowsmith Volcanics|22858|5|Briefly described|p94||Neoproterozoic|||||||
12467|Mount Arrowsmith Volcanics|23562|5|Briefly described|p295 Fig 2|Neoproterozoic III|Neoproterozoic III|Mount is Mt. in text.||||||
12467|Mount Arrowsmith Volcanics|23932|6|Mentioned|p667|||||||||
12467|Mount Arrowsmith Volcanics|24509|5|Briefly described|p42, p44 Tb. 2|Neoproterozoic|Neoproterozoic|Mount is Mt in text. Alkaline volcanics. Contains abundant pillow lavas, and breccias, hyaloclastites, volcanoclastic sediments, minor carbonate sediment; trachybasalt. Age: 586+/-7Ma (SHRIMP U-Pb zircon; Crawford et al 1997). Geol Prov: Koonenberry Belt.||||||04-MAY-05
12467|Mount Arrowsmith Volcanics|24551|6|Mentioned|p74|||||||||
12467|Mount Arrowsmith Volcanics|24599|5|Briefly described|p495 Fig. 2, p496|Neoproterozoic|Neoproterozoic|Transitional alkaline to tholeiitic basaltic metamorphosed lavas.  Age: 586+/-7Ma (Crawford et al, 1997).  Mount is Mt in text. Geological Province: Bancannia trough.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|36534|6|Mentioned|p226|||||||||
12467|Mount Arrowsmith Volcanics|42966|5|Briefly described|p299|||Proterozoic - Cambrian.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|43560|6|Mentioned|fig.1,p227|||||||||
12467|Mount Arrowsmith Volcanics|44093|5|Briefly described|p108, p110|Neoproterozoic|Neoproterozoic|Max Age: Late Neoproterozoic. Min Age: Late Neoproterozoic. Age: 586+/-7Ma (U/Pb SHRIMP zircon). Geological Province: Tasman Fold Belt.||||||18-MAR-05
12467|Mount Arrowsmith Volcanics|50129|6|Mentioned|p21 Fig.7|||Mount is Mt. in text.||||||
12467|Mount Arrowsmith Volcanics|50154|5|Briefly described|p59|Neoproterozoic|Neoproterozoic|Age: 586 +/- 7 Ma (Crawford et al., 1997).||||||
12467|Mount Arrowsmith Volcanics|60650|6|Mentioned|p189|||In NSW. Mount is Mt in text.||||||01-SEP-08
12467|Mount Arrowsmith Volcanics|62787|5|Briefly described|p75|||Of Crook (1980). Age: 586+/-7Ma (SHRIMP, Crawford et al. (1997)). Alkaline rocks.||||||07-FEB-11
12467|Mount Arrowsmith Volcanics|63489|5|Briefly described|Map legend|||Age: ?Neoproterozoic. Alkali basalt, trachybasalt, trachyte and related intrusives.||||||10-SEP-07
12467|Mount Arrowsmith Volcanics|63789|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|Of Kara beds. Alkali basalt, trachybasalt, trachyte submarine and subaerial lava flows and sills, pyroclastics and related intrusives (gabbro, dolerite, diorite, syenite).||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|63790|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds. Alkali basaltic, trachybasaltic, trachytic submarine and subaerial lava flows and sills, pyroclastics and related intrusives (gabbro, dolerite, diorite, syenite).||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|63793|5|Briefly described|p19 Table 1, p30, 32.|||Separates the Kara beds into upper and lower parts.|586 +/- 7 Ma (Crawford et al. 1997).||||A transitional alkaline series of basaltic pillow lavas and pyroclastic tuffs; locally sub-aerial deposits; trachytic tuffs and lavas; melanocratic gabbro sills and small syenitic and dioritic intrusions.|19-JAN-15
12467|Mount Arrowsmith Volcanics|63848|5|Briefly described|p532, p538.|Ediacaran|Ediacaran|High-Nb suite, geochemically similar to volcanics from Red Creek, near Truro (SA).|586 +/- 7 Ma (SHRIMP zircon:Crawford et al. 1997).|||||
12467|Mount Arrowsmith Volcanics|64168|5|Briefly described|p31|Neoproterozoic|Neoproterozoic|Age: 586Ma. An alkali basaltic suite of rocks with associated intrusions.||||||14-MAY-08
12467|Mount Arrowsmith Volcanics|64671|5|Briefly described|Map legend|||Faulted into Kara beds. Intruded by a dacitic/rhyolitc dyke of the Cymbric Vale Formation. Rocks of the Gnalta Group are fault bounded against the Mount Arrowsmith Volcanics. Mount is Mt in text.||||||26-NOV-08
12467|Mount Arrowsmith Volcanics|64679|5|Briefly described|Map legend|Neoproterozoic III|Neoproterozoic III|Alkali basalt; trachybasalt, trachyte; rhyolite flows, sills; pyroclastic rocks.||||||27-NOV-08
12467|Mount Arrowsmith Volcanics|64680|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds? Part of Kara beds or faulted into Kara beds? Alkali basalt, trachybasalt, trachyte and related intrusives.||||||01-DEC-08
12467|Mount Arrowsmith Volcanics|64684|5|Briefly described|Map Legend|Proterozoic|Proterozoic|Of Kara beds. Part of Kara beds or faulted into Kara beds? Alkali basalt, trachybasalt, trachyte and related intrusives.||||||
12467|Mount Arrowsmith Volcanics|64687|5|Briefly described|Map Legend|Early Cambrian|Proterozoic|Of Kara beds (part of Kara beds or faulted into Kara beds?). Oldest rocks in the Koonenberry region. Alkali basalt, trachybasalt, trachyte and related intrusives.||||||
12467|Mount Arrowsmith Volcanics|65381|5|Briefly described|p688, Fig. 2|Neoproterozoic|Neoproterozoic|Of the Wertago zone, Broken Hill; subalkaline volcanics. Part of the Kara beds.||||||26-MAR-13
12467|Mount Arrowsmith Volcanics|66623|1|Redefined|pp26-29, p v, p14. |Neoproterozoic|Neoproterozoic|Formerly part of Torrowangee Series (Mawson 1912), Wonominta Beds (Warris 1967), Kara beds (Mills 1992). First named Mount Arrowsmith Volcanics by Crook (1980). Separated from Mount Wright Volcanics (Crawford et al.1997) on basis of geochemistry.|585.5 +/- 3.2 Ma.|Unit in Grey Range Group.||Interfingers with sedimentary units (Kara Formation) of Grey Range Group.|Basalt-ferrobasalt-trachybasalt-trachyandesite-alkali rhyolite suite, subject to low grade regional metamorphism. Large, scoriaceous pillow lavas, pyroclastic rocks, sub-volcanic sills; rare subaerial flows and pyroclastic deposits; nundorite.|
12467|Mount Arrowsmith Volcanics|66917|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.||Is overlain by Kara Formation.|Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|66918|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Four un-named units are mapped separately.||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|66927|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Narrow trends of high magnetic intensity, continuous over many kilometres, parallel to sub-parallel and dislocated by fractures.||||Is overlain by Kara Formation.|Alkali basalt, trachybasalt, trachyte; submarine and subaerial flows, sills and related intrusions.|
12467|Mount Arrowsmith Volcanics|66929|5|Briefly described|Map legend|Early Cambrian|Late Proterozoic|||||Intruded by a Cymbric Vale Formation felsic dyke.|Alkali basalt, trachybasalt, trachyte and related intrusives; limestone and shale; nundorite; scoria horizons, pyroclastics, hyaloclastites and pillow breccias.|
12467|Mount Arrowsmith Volcanics|66933|5|Briefly described|Map legend|Early Cambrian|Late Proterozoic|Includes, or is faulted into, Kara beds.|||||Alkali basalt, trachybasalt, trachyte and related intrusives; volcanic sediments including scoria horizons, pyroclastics, hyaloclastites and pillow breccias; trachytic tuffs, locally subaerial with accretionary lapilli and compaction welding.|
12467|Mount Arrowsmith Volcanics|67105|5|Briefly described|p651, 653-655, 659, 661, 663, 666|Ediacaran|Ediacaran|Crawford et al. (1997) distinguished these rocks from the Mount Wright Volcanics. Wonnaminta Zone, Koonenberry Belt. Clearly related to intra-plate rifting. Shares close geochemical affinities with the Farnell Group.|585.5 +/- 2.6 Ma (SHRIMP II U-Pb: Black, 2007).|Grey Range Group.||Equivalent to the Farnell Group.|Intercalated alkaline dominantly basaltic submarine lavas and related intrusives; rift-related. Rare rhyodacite.|
12467|Mount Arrowsmith Volcanics|67207|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|67208|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Eleven un-named sub-units with differing lithologies are mapped separately.||Upper unit in Grey Range Group.|||Mafic igneous rocks: alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; gabbro plugs; mafic pyroclastics, hyaloclastites and pillow breccias; pillow basalt; microgabbro.|
12467|Mount Arrowsmith Volcanics|68241|5|Briefly described|p21, p24 Fig.3, p32, p33 Fig.3|Ediacaran|Ediacaran|Spelt as Mt Arrowsmith Volcanics in the text. > 4000 m thick.|586+/-7Ma SHRIMP U-Pb zircon Crawford et al. 1997|||Intertongued by the Sturts Meadows Siltstone.||
12467|Mount Arrowsmith Volcanics|69841|5|Briefly described|p19|Ediacaran|Ediacaran|Western NSW. Possible correlate of mid-Ediacaran mafic volcanic rocks of Tasmania.|c.586 Ma.|||||
12467|Mount Arrowsmith Volcanics|69873|6|Mentioned|p85|Ediacaran|Ediacaran|Koonenberry Belt. An example of ~580 Ma rift tholeiites found along much of the 'Tasman Line' and through King Island to Tasmania.||||||
12467|Mount Arrowsmith Volcanics|69961|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|No outcrop in map area.||Unit in Grey Range Group.|||Undifferentiated mafic igneous rocks: alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70125|6|Mentioned|p400||||586 Ma (crystallisation age).|||||
12467|Mount Arrowsmith Volcanics|70648|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|9 un-named units: Microperthitic intrusion, commonly altered. Foliated albite-aegirine-nepheline-natrolite rock (nundorite); an altered alkaline tuff or intrusion. Undifferentiated mafic intrusions. Plugs and plutons of mafic (alkaline) gabbro, hornfelsed contacts and some alteration. Plagioclase-pyroxene plug or dyke, commonly altered. Mafic volcaniclastic rocks including pyroclastics, hyaloclastites, pillow breccias. Trachyte including trachytic tuffs. Latite or trachy-basalt with large skeletal feldspar phenocrysts. Coarse-grained, serpentinite-chlorite ultramafic rock,originally picrite.||Grey Range Group|Includes 9 un-named units.||Undifferentiated mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70650|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|4 unnamed units: Plugs and plutons of mafic (alkaline) gabbro, hornfelsed contacts, some internal metamorphic epidote-albite-chlorite-quartz alteration. Fine- to medium-grained plagioclase-pyroxene plug or dyke, commonly altered. Mafic volcaniclastic rocks including pyroclastics (eg. scoria beds), hyaloclastites and pillow breccias. Grey, feldspar-rich trachyte including trachytic tuffs, some subaerial with compaction welding and accretionary lapilli.||Grey Range Group|Includes 4 un-named units.||Mafic igneous rocks; alkali basalt, trachybasalt, trachyte; submarine and subaerial lava flows, sills and related intrusions; regionally metamorphosed to greenschist facies.|
12467|Mount Arrowsmith Volcanics|70744|6|Mentioned|p940|||Has an alkaline intraplate character considered characteristic of modern rifts.||||||
12467|Mount Arrowsmith Volcanics|70749|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Southern Thomson and Koonenberry area.|~596 Ma.|||||
12467|Mount Arrowsmith Volcanics|70838|5|Briefly described|p268-270, p274, p278, p281|Ediacaran|Ediacaran|Coeval with Kara Formation. Geochemistry suggests a continental rift setting during emplacement.|585 +/- 3.2 Ma (Black, 2007).|Grey Range Group.|||Mafic rocks.|
12467|Mount Arrowsmith Volcanics|71262|5|Briefly described|p3-4, p5 Fig 2, p8 Fig 5, p9, p12|Neoproterozoic|Neoproterozoic||||||Alkali basalts with minor ultramafic rocks|
12467|Mount Arrowsmith Volcanics|71415|5|Briefly described|p10,15|||Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin.||Unit of Grey Range Group.||Overlain by the Teltawongee Group and Ponto Group.||19-AUG-19
12467|Mount Arrowsmith Volcanics|71593|5|Briefly described|p121-p122, p188-p189|||Koonenberry Belt. Associated with Ni-Cu prospects.|c. 586 Ma||||Ultramafic volcanics.|
12467|Mount Arrowsmith Volcanics|71966|6|Mentioned|p989|Ediacaran|Ediacaran|Geological province: Delamerian Orogen. Of the Koonenbery Belt.|c. 586 Ma|||Correlable to Bathampton Metamorphics.||
12467|Mount Arrowsmith Volcanics|73059|6|Mentioned|p1061|||||||||
12467|Mount Arrowsmith Volcanics|73177|5|Briefly described|p1098, 1114-1115 Figs.16-17|Neoproterozoic|Neoproterozoic|Delamerian Orogen.||Grey Range Group.|||Alkaline volcanics.|
12467|Mount Arrowsmith Volcanics|74367|5|Briefly described|p18-19|Ediacaran|Ediacaran|Koonenberry Belt. Tentatively correlated to the Aruhna Subgroup.|585.5+/-3.2 Ma SHRIMP U-Pb zircon||||Silicic igneous formation, includes rhyolite.|
12468|Mount Arthur Coal Member|29942|4|Described|Fig.1|||Permian||||||
12468|Mount Arthur Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
12468|Mount Arthur Coal Member|39666|6|Mentioned|p81|||||||||
12468|Mount Arthur Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
12468|Mount Arthur Coal Member|40805|6|Mentioned|p133|||See also Table 1||||||
12468|Mount Arthur Coal Member|45090|6|Mentioned|p222|||Middle Tatarian||||||
12468|Mount Arthur Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Burnamwood Formation.||||
12470|Mount Arthur Granite|42726|5|Briefly described|map legend|Silurian||NOT variation on Mount Arthur Coal Member. Technically invalid name.||||||
12470|Mount Arthur Granite|71206|6|Mentioned|p373, 377|||Lachlan Fold Belt. This unit is apparently known also as Milmiland Granite.||Mount Arthur Suite.|||Aluminous A-type granite.|
12484|Mount Barney Central Complex|31694|6|Mentioned|p347|||||||||
12484|Mount Barney Central Complex|32924|6|Mentioned|p111|||Refers Stephenson (1956, 1959)||||||
12484|Mount Barney Central Complex|39445|5|Briefly described|Table 14|||||||||
12484|Mount Barney Central Complex|40780|4|Described|p11|||||||||
12484|Mount Barney Central Complex|40896|4|Described|p51|||||||||
12484|Mount Barney Central Complex|44091|14|Not recorded|p66||Tertiary|||||||
12484|Mount Barney Central Complex|44778|2|Defined|p135|||(Post Triassic - pre Eocene-Oligocene)||||||
12484|Mount Barney Central Complex|44781|2|Defined|p362|||Emplaced in Middle Carboniferous sediments.||||||
12484|Mount Barney Central Complex|44784|14|Not recorded|p12||Tertiary|||||||
12484|Mount Barney Central Complex|44813|14|Not recorded|p81||Tertiary|Intruded into Middle Carboniferous 23.4 Ma.||||||
12484|Mount Barney Central Complex|45014|14|Not recorded|p20|||SE Qld||||||
12484|Mount Barney Central Complex|48917|5|Briefly described|p36|||Refers Stephenson (1959,1960)||||||
12484|Mount Barney Central Complex|48928|6|Mentioned|p15|||||||||
12484|Mount Barney Central Complex|68553|6|Mentioned|Map legend|Paleogene|Paleogene|This unit, as well as the Silver Plains Nephelinite, Tabor Gabbro, Mount Jukes Intrusive Complex, and unnamed basaltic to rhyolitic plugs, are all mapped under the symbol, Ti.||||||
12484|Mount Barney Central Complex|73450|4|Described|p96-98|||Comprises the core and defining feature of the Focal Peak volcano. Associated intrusive structures include ring dykes, cone sheets, a broad dome and a closed ring fault.|||||A suite of dominantly felsic, high-level, intrusive and less common extrusive igneous rocks including diorites, dolerites, microsyenites, granophyres, rhyolites and trachytes as well as mafic to felsic pyroclastic rocks.|
12490|Mount Barney beds|23799|6|Mentioned|p126 Fig. 24|||Geological Province: Yarrol Province.||||||
12490|Mount Barney beds|30772|6|Mentioned|p1|||Fauna||||||
12490|Mount Barney beds|40623|5|Briefly described|p40|||||||||
12490|Mount Barney beds|40780|4|Described|p4|||||||||
12490|Mount Barney beds|40896|6|Mentioned|p47|||||||||
12490|Mount Barney beds|43008|5|Briefly described|map legend|||||||||
12490|Mount Barney beds|44372|6|Mentioned|p41|||||||||
12490|Mount Barney beds|61007|6|Mentioned|p293|Carboniferous|Carboniferous|||||||
12490|Mount Barney beds|68553|6|Mentioned|Map legend|Carboniferous|Carboniferous|This unit is mapped with Alice Creek beds under the symbol, Cy.||||||
12490|Mount Barney beds|68679|5|Briefly described|p306, p321, p350-351|Pennsylvanian|Pennsylvanian|Stephenson (1959); Olgers et al. (1974). Occurs in two down-faulted belts E and W of Mount Barney near the NSW border. Yarrol Province forearc rocks. Similar clasts noticed in rocks in Beenleigh Subprovince and in NSW: significance for possible extent of the Subprovince mentioned.||||Is intruded by Mount Barney Igneous Complex.|Basal calc-silicate rocks, overlain by lithic and feldspathic sandstone with interbedded rhyolitic and trachytic lava flows and tuffs, and dark fine-grained siltstone with spiriferoid brachiopods; then sandstone, conglomerate and crinoidal mudstone.|
12490|Mount Barney beds|69599|6|Mentioned|p640|Paleozoic|Paleozoic|Exposed around the Focal Peak volcano at Mount Barney.||||||
12582|Mount Charlotte Silcrete|23053|6|Mentioned|Fig10p17,38|Pliocene|Pliocene|||||||
12582|Mount Charlotte Silcrete|35187|6|Mentioned|p55|||||||||
12582|Mount Charlotte Silcrete|61155|6|Mentioned|p19|Late Miocene|Late Miocene|In the Walgett area.||||||
12582|Mount Charlotte Silcrete|68003|5|Briefly described|p92 Fig.3-v.|Pliocene|Pliocene|Coonamble Embayment.||||Is overlain by Trangie Formation.||
12582|Mount Charlotte Silcrete|68593|6|Mentioned|p1, p3, p31|Pliocene|Pliocene|Taylor (1976, 1978).||||||
12623|Mount Daubeny Formation|22518|4|Described|Table 1, p 3, 4, 10|Early Devonian|Late Silurian|Darling Basin||||||
12623|Mount Daubeny Formation|22580|5|Briefly described|p87|Early Devonian|Silurian|||||||
12623|Mount Daubeny Formation|22671|5|Briefly described|p832, Fig1p835|||Non-marine fluvial and lacustrine sediments and minor calc-alkaline volcanics.  Max. thickness: 6km.  Geological Province: Kanmantoo Fold Belt. Mount is Mt in text.||||||17-JAN-06
12623|Mount Daubeny Formation|22683|6|Mentioned|95|||||||||
12623|Mount Daubeny Formation|22730|5|Briefly described|p559,66|Early Devonian|Late Silurian|||||||
12623|Mount Daubeny Formation|22768|6|Mentioned|p141,166|||||||||
12623|Mount Daubeny Formation|22857|5|Briefly described|p141, p166, p200|Early Devonian|Late Silurian|Previously known as "Cootawundy beds" (Packham 1969a, Webby 1972). Also supersedes "Wertago-Cootawundy Series". See misspelt "Mount Daubney Formation". Clastic sediments with minor andesitic flows. Max. thickness: 6km. Geol. Prov: Mount Daubeny Basin.||||||
12623|Mount Daubeny Formation|22859|5|Briefly described|p200,211|Early Devonian|Late Silurian|||||||
12623|Mount Daubeny Formation|23336|3|Fully described|p11|Early Devonian|Late Silurian|Unconformably overlain by Ravendale Formation; overlies Ponto beds in south and Teltawongee beds in north. Max. thickness: >6km. Mount is Mt in text.||||||11-SEP-07
12623|Mount Daubeny Formation|23380|5|Briefly described|p107-110|Early Devonian|Late Silurian|of Wonaminta Block.||||||
12623|Mount Daubeny Formation|23469|5|Briefly described|Fig 2 p 319|||Spelt "Mt" in text.||||||11-SEP-07
12623|Mount Daubeny Formation|24345|5|Briefly described|p83, p84-85 Fig. 2|Early Devonian|Late Silurian|Mount is Mt in text.||||||
12623|Mount Daubeny Formation|42121|4|Described|p97|||See also Fig.2 a and b.||||||11-SEP-07
12623|Mount Daubeny Formation|42298|2|Defined|p29 (p101a)|Early Devonian|Late Silurian|Age from p105, Roy. Soc. NSW J & Proc 122(3 and 4): latest Silurian to Early Devonian||||||11-SEP-07
12623|Mount Daubeny Formation|42364|4|Described|p195, 197-205, 206-8|||Age: latest Silurian to Early Devonian.||||||11-SEP-07
12623|Mount Daubeny Formation|42460|4|Described|p205|||Mount is Mt in text. Variation of Mount Daubney Beds?||||||11-SEP-07
12623|Mount Daubeny Formation|43192|4|Described|p64,Table1 p61|Early Devonian|Late Silurian|Formerly Cootawundy beds.||||||11-SEP-07
12623|Mount Daubeny Formation|44093|5|Briefly described|p143 App. 1|Early Devonian|Late Silurian|Mount is Mt in text of Table. Geological Province: Kanmantoo Fold Belt.||||||18-MAR-05
12623|Mount Daubeny Formation|50129|6|Mentioned|p16 Fig.1|Early Devonian|Late Silurian|||||||
12623|Mount Daubeny Formation|50618|5|Briefly described|p248 Fig. 1|Middle Devonian|Ordovician|Mount is Mt in text. Geological Province: Wonominta Block.||||||
12623|Mount Daubeny Formation|60648|5|Briefly described|p40-41|Early Devonian|Late Silurian|Geological Province: Darling Basin.  Mount is Mt in text.||||||26-APR-05
12623|Mount Daubeny Formation|61213|5|Briefly described|p319 Fig. 3|Emsian|Late Silurian|Includes the Koonburra Creek Quartzite Member. Max. thickness: 6km (Deduced from field work: Neef et al 1989). Geological Province: Darling Basin. Mount is Mt in text.||||||
12623|Mount Daubeny Formation|63025|5|Briefly described|p1052 Fig. 1, p1053|Lochkovian|Lochkovian|Geological Province: Central Lachlan Orogen. Mount is Mt in text.||||||
12623|Mount Daubeny Formation|63489|5|Briefly described|Map legend|Early Devonian|Early Devonian|Fluviatile labile sandstone, conglomerate, quartzite, dacite-andesite.||||||
12623|Mount Daubeny Formation|63632|5|Briefly described|649|||Terminal fan deposits coeval with Maccullochs Range beds.  Mount is Mt in text.||||||
12623|Mount Daubeny Formation|63790|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Polymictic basal conglomerate with a variety of local and foreign clasts.||||||14-NOV-13
12623|Mount Daubeny Formation|63793|6|Mentioned|p19 Table 1, p24, 36, 43 .|Devonian|Silurian|||||Intruded by quartzofeldspathic dykes.||19-JAN-15
12623|Mount Daubeny Formation|64169|5|Briefly described|p20 Fig. 9|Devonian|Silurian|Overlies Snake Cave Sandstone. Rhyolitic and dacitic dykes, and dacitic and andesitic plugs occur.||||||15-MAY-08
12623|Mount Daubeny Formation|64671|5|Briefly described|Map legend|Early Devonian|Late Silurian|Contains the Koonburra Creek Quartzite Member. Unconformable on Ponto+Teltawongee beds. Intramontane seq. of lithic sandstones and siltstones mostly of red-bed character - further lithological detail included. Mount is Mt in text.||||||14-NOV-13
12623|Mount Daubeny Formation|64679|5|Briefly described|Map legend|Early Devonian|Late Silurian|Red, maroon, brown and green lithic sandstone, conglomerate and siltstone; pebble marker horizons; plant+trace fossils. Rhyolitic and dacitic dykes , sills and domes.||||||
12623|Mount Daubeny Formation|64680|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unconformably overlies Ponto beds and Teltawongee beds. An intramontane sequence consisting of lithic sandstones and siltstones mostly of red-bed character but with some grey-green bedded units, and some intermediate to felsic volcanic extrusives.||||||
12623|Mount Daubeny Formation|64682|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Includes Koonburra Creek Quartzite Member. Sequence containing conglomerates, sandstones and siltstones mostly of red-bed character but with some grey-green bedded units. Some intermediate to felsic volcanic extrusives and intrusives.||||||
12623|Mount Daubeny Formation|64683|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Red, maroon, brown and green lithic arenites, polymictic rudites and siltstones. Minor dacite pebble marker horizons. Late Silurian to Early Devonian plant fossils and trace fossils.||||||
12623|Mount Daubeny Formation|64684|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unconformably overlies Ponto beds and Teltawongee beds. An intramontane sequence consisting of lithic sandstones and siltstones mostly of red-bed character but with some grey-green bedded units.||||||
12623|Mount Daubeny Formation|64685|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Red, maroon, brown and green lithic arenites, polymictic rudites and siltstones, with andesitic, dacitic and rhyolitic flows, sills, dykes and plugs.||||||01-DEC-08
12623|Mount Daubeny Formation|64686|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Unconformably overlies Ponto beds and Teltawongee beds. An intramontane sequence consisting of lithic sandstones and siltstones mostly of red-bed character but with some grey-green bedded units, and some intermediate to felsic volcanic extrusives.||||||
12623|Mount Daubeny Formation|64967|5|Briefly described|p113, p114 Fig. 2|Emsian|Late Silurian|Alluvial/fluvial deposits. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113). Mount is Mt in text.||||||
12623|Mount Daubeny Formation|65381|5|Briefly described|p687-701,706, fig 2,4,6-7,9-10,12-15|Early Devonian|Late Silurian|Fill to the Mt Daubeny Basin, consists of non-marine lithic to siliciclastic sandstone with andesitic to dacitic extrusive and pyroclastic units low in the formation dated at 425 +/-7 Ma SHRIMP zircon (Black 2007). Dated by plant fossils. Cut by dykes, dated Silurian to Devonian.||||||14-NOV-13
12623|Mount Daubeny Formation|66623|3|Fully described|p78, p161, pp178-187. |Early Devonian|Late Silurian|Mount Daubeny Basin. Formerly part of Wertago-Cootawundy Series (Kenny 1934), Mount Daubeny beds (Warris 1967), Cootawundy beds (Scheibner 1978); defined as Mount Daubeny Formation by Neef et al. (1989). Rapid red-bed deposition, at least 6 km thick, in a suggested  dextral transpression pull-apart basin. Rare worm tubes, plants and non-marine arthropod traces occur. Hosts Wertago Volcanics epithermal copper mineralisation. .|Between 425.0 +/- 7 Ma and 414.2 +/- 2.7 Ma.||Includes Koonburra Creek Quartzite Member and Gnaltaknoko Member, and an un-named unit mapped separately.|Unconformably overlies Ponto and Teltawongee Groups and the Kara Formation. Is faulted against the Wana Karnu Group and Ravendale Formation. Is intruded by dykes and plugs of Wertago Volcanics.|Pale red, maroon, grey and greenish-grey feldspathic sandstone with subordinate siltstone and conglomerate; a 6m thick sequence of orthoquartzite interbedded with grey arenite and siltstone; matrix-supported conglomerate with mainly dacitic clasts.|
12623|Mount Daubeny Formation|66929|5|Briefly described|Map legend|Early Devonian|Late Silurian|Contains plant and trace fossils.|||Includes Koonburra Creek Quartzite Member.||An intramontane red-bed sequence of lithic sandstones and siltstones, with some grey-green bedded units; conglomerates, intermediate to felsic volcanic extrusives and intrusives; locally-derived volcanogenic sediments.|
12623|Mount Daubeny Formation|66933|5|Briefly described|Map legend|Early Devonian|Late Silurian|Koonenberry Zone, Delamerian Fold Belt.|||||Polymictic red-bed conglomerate with a range of local and foreign clasts.|
12623|Mount Daubeny Formation|67562|5|Briefly described|p91-92, p95-100 Fig.6, p105, p107|Ludfordian|Ludfordian|See also p110-111, p115. Darling Basin. Mount is spelt as Mt in text. 6 km thick. Deposited in a narrow basin adjacent to W side of Koonenberry Fault. Poly-deformed. Andesites of the older part of the Formation are ca. 430 Ma in age (Black, 2005). Intruded by feldspar porphyry and basalt c.417-414 Ma. Contains Baragwanathia Flora. Coeval with MacCullochs Range Beds.|ca. 425-400 Ma||Koonaburra Creek Quartzite Member.|Is overlain unconformably by Ravendale Formation or Muckabunnya Beds.||23-JAN-17
12623|Mount Daubeny Formation|67870|5|Briefly described|p62|Devonian|Devonian|Darling Basin. Appears only as Mount Daubeny (braided).||Winduck Group.||||
12623|Mount Daubeny Formation|70013|5|Briefly described|Map legend|Early Devonian|Silurian|Koonenberry Belt. Dykes and sills. Maximum age shown as ?Silurian.||||||
12623|Mount Daubeny Formation|70037|4|Described|p309 Fig.2, p310-311|Early Devonian|Late Silurian|Extensive area W of the Koonenberry Fault, Western Darling Basin. Mapped by Neef et al. (1989) and Neef and Bottrill (1991). Age range from fossils; geochronology from an andesitic lava flow "close to the base of the sequence".|423 +/- 7 Ma (Black, 2007).||Gnaltaknoko Member, Koonburra Creek Quartzite Member.||Medium- and coarse-grained immature arenite and minor conglomerate.|
12623|Mount Daubeny Formation|70210|5|Briefly described|p1, p17, p20, p38, p40-41|||Koonenberry-Tibooburra district. Is intruded by felsic dyke(s) aged c.421 Ma and c.418 Ma, and an unspecified dyke aged 414 M (Black, 2005).||||||
12623|Mount Daubeny Formation|70296|6|Mentioned|p1,p21,  p22, p24|Lochkovian||Age of this unit is older than provided SHRIMP age which is for a sill within this formation.|>413.8 +/- 2.7 Ma (SHRIMP U-Pb)|Ponto Group [?]||||22-JAN-21
12623|Mount Daubeny Formation|70651|5|Briefly described|Map Legend|Devonian|Silurian||||Includes Gnaltaknoka Member, Koonburra Creek Quartzite Member.||Largely immature clastic sedimentary rocks of pale red arenite with subordinate siltstone and conglomerate.
|
12623|Mount Daubeny Formation|71040|5|Briefly described|p4 Fig.2, p5, p7, p9, p31|Early Devonian|Late Silurian|A thick succession; relatively strongly deformed (post-414 Ma) but lacks cleavage. Deformation associated with Bindian (= Bowning) Orogeny described. U-Pb zircon ages by Greenfield et al. (2010).|425 +/- 7 Ma to 414 +/- 3 Ma.|||Is overlain unconformably by Ravendale Formation.||
12623|Mount Daubeny Formation|72522|5|Briefly described|p131.|||Of Mount Daubeny Basin.|||Includes Gnaltaknoko Member.|Intruded by Wertago Volcanics.|Includes basal conglomerate.|
12644|Mount Dromedary Igneous Complex|22580|6|Mentioned|p95||Cretaceous|||||||
12644|Mount Dromedary Igneous Complex|22815|3|Fully described|p106|Late Cretaceous|Early Cretaceous|K/Ar Age: 97+/-2 Ma.||||||
12644|Mount Dromedary Igneous Complex|22862|6|Mentioned|Map29p322-3||Late Cretaceous|||||||
12644|Mount Dromedary Igneous Complex|35289|4|Described|p21|||||||||
12644|Mount Dromedary Igneous Complex|36411|6|Mentioned|p269|||Refers Chalker & Bembrick 1977 for definition.||||||
12644|Mount Dromedary Igneous Complex|37818|6|Mentioned|Table 3|||||||||
12644|Mount Dromedary Igneous Complex|40178|5|Briefly described|p6|||||||||
12644|Mount Dromedary Igneous Complex|43233|5|Briefly described|Map Legend|Late Cretaceous|Early Cretaceous|||||||
12644|Mount Dromedary Igneous Complex|44093|5|Briefly described|p225 App. 1|Mesozoic|Mesozoic|Geological Province: Lachlan Fold Belt.||||||
12644|Mount Dromedary Igneous Complex|46524|6|Mentioned|p123|||||||||
12644|Mount Dromedary Igneous Complex|46574|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Monzonite, banatite, peridotite, ijolite, shonkinite, garnet pyroxenite, basic and internediate volcanics.  Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
12644|Mount Dromedary Igneous Complex|60299|5|Briefly described|p224|Cretaceous|Cretaceous|Age: 97 Ma. Palaeopole position given.||||||
12644|Mount Dromedary Igneous Complex|65490|5|Briefly described|p883|Albian|Albian|Mount is spelt Mt in text. Consists of felsic rocks and occurs on the NSW south coast. Age of 108 +/-3.9 Ma (after Hirata et al. 2005) given.||||||
12644|Mount Dromedary Igneous Complex|66889|5|Briefly described|p696, p698-701|Albian|Albian|Age analysis of averaged 206Pb/238U age for LA-ICPMS data is 108.8 +/- 3.9 Ma (2SD, n=8) on zircon, showing it to be significantly older than widely accepted value (98.8 +/ -0.6 Ma) on p700. Posible explanations for difference provided in text.|Age 108.8+/-3.9 Ma, LA-ICPMS zircon|||||11-MAY-11
12644|Mount Dromedary Igneous Complex|67785|5|Briefly described|p79, 85|||Tilba area, south coast of NSW.|98.5 +/- 1.6 Ma.||||Comprises two granitoid phases: a banatite/syenite core and a monzonite rim.|
12644|Mount Dromedary Igneous Complex|69541|6|Mentioned|p648|Cretaceous|Cretaceous|||||||
12644|Mount Dromedary Igneous Complex|70601|5|Briefly described|p27|Cretaceous|Cretaceous|Appears to be used interchangeably with informal Mount Dromedary Intrusive Suite and intrusion.|100 +/- 6 Ma (K/Ar on alkali feldspar).||||Monzonite, monzodiorite.|
12695|Mount Ephraim Granodiorite|42376|6|Mentioned|p45|||Variation of Mount Ephraim Granite?||||||
12695|Mount Ephraim Granodiorite|68005|5|Briefly described|p135.|Permian|Permian|||Unit in Nundle Suite.|||Trondhjemite, granodiorite.|
12695|Mount Ephraim Granodiorite|70217|4|Described|v, p1 tbl 1.1, p11, p17|Wuchiapingian|Wuchiapingian|New England Orogen. Primitive I-type geochemistry. SHRIMP ages derived from this volume and given age is interpreted as the magmatic crystallisation age. Additional ages of c. 265 Ma (Sm-Nd, Hensel et al 1985) and c. 273 Ma (ID-TIMS Pb-Pb, Kimbrough et al, 1993). Petrography, zircon morphology and SHRIMP results discussed in detail. See also p27-p31, p72, p73 tbl 14.1, p89.|255.3 +/- 1.3 Ma (SHRIMP U-Pb)|Mount Ephraim Suite||Overlain by the Liverpool Range Volcanics. Intrudes the Hawks Nest beds.|Moderately porphyritic granodiorite with 50 percent plagioclase, 30 percent amphibole, 10 percent quartz and 10 percent alkali feldspar.|
12695|Mount Ephraim Granodiorite|70876|5|Briefly described|p78|Permian|Permian|New England Orogen. Additional provided ages are as follows: c. 265 Ma (Sm-Nd whole rock, Hensel et al, 1985) and c. 273 Ma (ID-TIMS Pb-Pb zircon, Kimbrough et al, 1993). [Either part of the Clarence River Supersuite or a correlative-not made clear in the text].|255.3 +/- 1.3 Ma (Waltenberg et al, 2015)|||||
12695|Mount Ephraim Granodiorite|71628|4|Described|p9:2; p18: 1, 7, 16, 20-22|||Ashley (1990). Originally Mount Ephraim Granite (Crook, 1961), with a variety of subsequent variations. Crops out poorly as low rubble, in an area of 2 x 0.6 km, about 8 km SSE of Nundle. Geochemistry described. Is spatially, but probably not genetically, associated with placer Au deep lead deposits.|255.3 +/- 1.3 Ma (SHRIMP: Waltenberg et al., 2015)|Duncans Creek Suite.||Intrudes Parry Group.|Porphyritic to seriate, biotite-hornblende granodiorite to tonalite. I-type.|
12700|Mount Euriowie pegmatite|39652|6|Mentioned|p63|||||||||
12721|Mount Frome Limestone|22451|5|Briefly described|p24|||Mount  is written Mt in text||||||
12721|Mount Frome Limestone|22529|5|Briefly described|t|Eifelian|Emsian|||||||
12721|Mount Frome Limestone|22590|6|Mentioned|Fig3 P754||Emsian|Acturally spelt Mt Frome Lst.||||||
12721|Mount Frome Limestone|22768|6|Mentioned|p179||Middle Devonian|||||||
12721|Mount Frome Limestone|22857|4|Described|p179, p474 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Of the Kandos Group. Limestone, calcarenite. Max. thickness: 200m. Geological Province: Capertee Rise.||||||
12721|Mount Frome Limestone|23043|5|Briefly described|Map Legend|Eifelian|Emsian|Of Kandos Group.||||||28-AUG-08
12721|Mount Frome Limestone|23170|2|Defined|p139|Givetian|Eifelian|Of Kandos Group.||||||28-AUG-08
12721|Mount Frome Limestone|23522|5|Briefly described|p248 Fig 4|Early Devonian|Early Devonian|||||||
12721|Mount Frome Limestone|24580|5|Briefly described|p828|||Overlain conformably by the Boolgledie Formation. Mount is Mt. in text. Geological Province: Eastern Lachlan Fold Belt.||||||
12721|Mount Frome Limestone|24588|5|Briefly described|p31 Fig.15|Eifelian|Emsian|Mount is Mt in text. Geological Province: Lachlan Fold Belt.||||||13-DEC-04
12721|Mount Frome Limestone|24611|6|Mentioned|p194, p225|Eifelian|Emsian|See also p196 Fig. 2.||||||
12721|Mount Frome Limestone|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
12721|Mount Frome Limestone|30814|6|Mentioned|p71|||||||||
12721|Mount Frome Limestone|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
12721|Mount Frome Limestone|32413|6|Mentioned|p107|||||||||
12721|Mount Frome Limestone|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
12721|Mount Frome Limestone|32619|6|Mentioned|p458|||Early - Mid. Eifelian. Fauna||||||
12721|Mount Frome Limestone|32622|6|Mentioned|p7|||||||||
12721|Mount Frome Limestone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
12721|Mount Frome Limestone|32672|6|Mentioned|p673|||||||||
12721|Mount Frome Limestone|33326|6|Mentioned|p445|||Fauna.||||||
12721|Mount Frome Limestone|33732|4|Described|p118|||||||||
12721|Mount Frome Limestone|34250|6|Mentioned|p2|||Givetian. See also P10||||||
12721|Mount Frome Limestone|35246|6|Mentioned|p172|||||||||
12721|Mount Frome Limestone|36534|6|Mentioned|p225|||||||||
12721|Mount Frome Limestone|39214|5|Briefly described|p25|||||||||
12721|Mount Frome Limestone|40131|6|Mentioned|p211|||||||||
12721|Mount Frome Limestone|42032|6|Mentioned|p500|||||||||
12721|Mount Frome Limestone|42033|6|Mentioned|p656|||||||||
12721|Mount Frome Limestone|43188|4|Described|p216, Table 5 p213|Eifelian|Emsian|late early Emsian to earliest Eifelian. Fmn or member of Boogledie Fm by various authors.||||||
12721|Mount Frome Limestone|43461|14|Not recorded|Table p621|||||||||
12721|Mount Frome Limestone|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
12721|Mount Frome Limestone|43519|14|Not recorded|p117-8,Tb p119,120||Devonian|||||||
12721|Mount Frome Limestone|43530|14|Not recorded|p1028,1034||Givetian|L.Givetian||||||
12721|Mount Frome Limestone|43541|14|Not recorded|p264,267|||Fossils||||||
12721|Mount Frome Limestone|64296|6|Mentioned|p84, p85|||Upper part is probably Middle Devonian.||||||28-AUG-08
12721|Mount Frome Limestone|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Mudgee. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
12721|Mount Frome Limestone|68297|5|Briefly described|p186, 192, 193|Eifelian|Emsian|Includes Emsian vertebrate fossil fauna.||||||
12721|Mount Frome Limestone|73299|6|Mentioned|p1106|||||||Underlies the Boogledie Formation.||
12795|Mount Hercules Sandstone Member|22745|5|Briefly described|p139|||Bringelly Shale, Sydney Basin. 44 m.||||||
12795|Mount Hercules Sandstone Member|35690|6|Mentioned|p39|||||||||
12795|Mount Hercules Sandstone Member|39298|6|Mentioned|p257|||See also Figs 13.2, 13.3||||||
12795|Mount Hercules Sandstone Member|39626|2|Defined|p277|Middle Triassic|Middle Triassic|||||||
12795|Mount Hercules Sandstone Member|42896|3|Fully described|p47, Fig.7|||of Bringelly Shale; redefinition intended||||||
12809|Mount Hutton Formation|22578|5|Briefly described|Fig.9 p399, p402|||of Newcastle Coal Measures||||||
12809|Mount Hutton Formation|23055|6|Mentioned|Fig11p23|||||||||
12809|Mount Hutton Formation|24471|4|Described|p33|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Kembla Sandstone. Geological Province: Sydney Basin.||||||07-FEB-11
12809|Mount Hutton Formation|29922|6|Mentioned|Appendix 4|||||||||
12809|Mount Hutton Formation|29926|6|Mentioned|Fig.3|||||||||
12809|Mount Hutton Formation|29942|4|Described|Fig.2|||||||||
12809|Mount Hutton Formation|34351|5|Briefly described|p344|||Fig.5.13||||||
12809|Mount Hutton Formation|35319|6|Mentioned|Table 1|||||||||
12809|Mount Hutton Formation|37083|6|Mentioned|p164|||||||||
12809|Mount Hutton Formation|39292|6|Mentioned|Fig. 6.2|||||||||
12809|Mount Hutton Formation|39308|6|Mentioned|Fig. 23.4|||||||||
12809|Mount Hutton Formation|39609|6|Mentioned|Table 1|||||||||
12809|Mount Hutton Formation|41479|6|Mentioned|Fig.2|||||||||
12809|Mount Hutton Formation|43344|14|Not recorded|p85||Permian|||||||
12809|Mount Hutton Formation|43447|14|Not recorded|diag.p26|||Boolaroo Sub-Group||||||
12809|Mount Hutton Formation|43448|14|Not recorded|p224,Pl.2||Permian|On table only. Unit of Boolaroo Subgroup (Newcastle Coal Measures)||||||
12809|Mount Hutton Formation|45090|6|Mentioned|p186|||Stratigraphic table||||||
12809|Mount Hutton Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113. Change of boundary between Adamstown and Boolaroo Formations means that these rocks are probably now included in the Adamstown Formation.||Of Boolaroo Subgroup||||17-APR-14
12836|Mount Jellore Complex|32187|6|Mentioned|p9|||||||||
12849|Mount Johnstone Formation|22857|4|Described|p506 App.1 Tb.A1.8|Namurian|visean|Disconformably overlies Mowbray and Chichester Formations. Age: 321.9+/-4Ma and 323.2+/-3.2Ma (U/Pb SHRIMP). Basal conglomerate, passes into yellow-browm lithic arenite, pebble conglomerate, siltstone, tuff and ignimbrite.||||||
12849|Mount Johnstone Formation|24121|5|Briefly described|p4, p96, p119, 159|||||||||25-AUG-22
12849|Mount Johnstone Formation|24603|6|Mentioned|p898|||Geological Province: Tamworth Belt.||||||
12849|Mount Johnstone Formation|30074|6|Mentioned|p27|||See also P28.||||||
12849|Mount Johnstone Formation|31706|6|Mentioned|p653|||Upper Carb. correlation chart||||||
12849|Mount Johnstone Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12849|Mount Johnstone Formation|32672|6|Mentioned|p674|||||||||
12849|Mount Johnstone Formation|32868|6|Mentioned|p210|||||||||
12849|Mount Johnstone Formation|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12849|Mount Johnstone Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
12849|Mount Johnstone Formation|34085|6|Mentioned|Cor.chart|||Westphalian||||||
12849|Mount Johnstone Formation|34169|4|Described|Fig.4.6|||Stratigraphic column.||||||
12849|Mount Johnstone Formation|34238|6|Mentioned|p5|||See also P8||||||
12849|Mount Johnstone Formation|34239|6|Mentioned|p264|||Grandispora microflora||||||
12849|Mount Johnstone Formation|34444|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
12849|Mount Johnstone Formation|36042|6|Mentioned|Table 1|||||||||
12849|Mount Johnstone Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
12849|Mount Johnstone Formation|36528|6|Mentioned|p179|||||||||
12849|Mount Johnstone Formation|37922|5|Briefly described|p481|||||||||
12849|Mount Johnstone Formation|38801|6|Mentioned|Fig.3|||||||||
12849|Mount Johnstone Formation|39287|6|Mentioned|Fig. 2.5|||||||||
12849|Mount Johnstone Formation|39299|5|Briefly described|p279|||||||||
12849|Mount Johnstone Formation|39302|5|Briefly described|p343|||||||||
12849|Mount Johnstone Formation|39306|6|Mentioned|p387|||Pteridosperms. See also P390-391||||||
12849|Mount Johnstone Formation|42547|4|Described|p31|||Actually spelt Mt Johnstone Formation.||||||
12849|Mount Johnstone Formation|43383|14|Not recorded|p18|||||||||
12849|Mount Johnstone Formation|43432|14|Not recorded|p206|||Kuttung facies||||||
12849|Mount Johnstone Formation|43440|14|Not recorded|p37,66,68,76|||||||||
12849|Mount Johnstone Formation|43447|14|Not recorded|Table 1&2,p9-11||Carboniferous|||||||
12849|Mount Johnstone Formation|43451|14|Not recorded|Map Legend|||||||||
12849|Mount Johnstone Formation|43479|14|Not recorded|p159,177||Westphalian|||||||
12849|Mount Johnstone Formation|43576|6|Mentioned|Fig.1,p348||Late Carboniferous|||||||
12849|Mount Johnstone Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
12849|Mount Johnstone Formation|44093|5|Briefly described|p228 App. 1|Late Carboniferous|Early Carboniferous|Mount is Mt in text of Table. See alao p 229 Appendix 1. Geological Province: New England Fold Belt.||||||
12849|Mount Johnstone Formation|44244|2|Defined|p94|Westphalian|Namurian|Disconformably overlies the Mowbray Formation; underlies the Paterson Volcanics.  Max.. thickness: 650m.  Geological Province: Gresford Block.||||||16-SEP-04
12849|Mount Johnstone Formation|44254|14|Not recorded|p76,77,81||Stephanian|Partly corresponds with Italia Road Formation.||||||
12849|Mount Johnstone Formation|44833|14|Not recorded|p108|||Early Carboniferous faunal units. See also Lexicon.||||||
12849|Mount Johnstone Formation|45090|4|Described|p25|||Stratigraphic table||||||
12849|Mount Johnstone Formation|45097|4|Described|p18|||Distinct floral assemblages. See also P24, 25.||||||
12849|Mount Johnstone Formation|46849|6|Mentioned|Fig. 2|||||||||
12849|Mount Johnstone Formation|47056|6|Mentioned|Fig.2 P523|||||||||
12849|Mount Johnstone Formation|50099|5|Briefly described|p10|Late Carboniferous|Late Carboniferous|Overlies the Isismurra Formation. Geological Province: Tamwoth Belt/New England Orogen.||||||
12849|Mount Johnstone Formation|50268|5|Briefly described|Map Legend|Stephanian|Namurian|Underlies: Paterson Volcanics, Seaham Formation.  Geological Province: Rouchel and Gresford Blocks.||||||
12849|Mount Johnstone Formation|61768|6|Mentioned|p82, p83 Fig. 2|||Overlain by Paterson Volcanics.||||||13-MAY-08
12849|Mount Johnstone Formation|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|Geological Province: Rouchel Block/Tamworth Belt. Mount is Mt in text of Plate 1.||||||
12849|Mount Johnstone Formation|63832|6|Mentioned|p131 fig 2|Visean|Visean|Rouchel block and Cranky Corner/Gresford block, Southern New England Fold Belt.||||||
12849|Mount Johnstone Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, Rouchel Block and Cranky Corner/Gresford Block. Biostratigraphic age control for base and top.||||Is overlain by Paterson Volcanics.||
12849|Mount Johnstone Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.||||||
12849|Mount Johnstone Formation|70777|6|Mentioned|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||||||
12849|Mount Johnstone Formation|71233|5|Briefly described|p116|Carboniferous|Carboniferous|N of Seaham, Hunter Valley. Contains Grandispora Microflora. See Rattigan (1967).||||||
12849|Mount Johnstone Formation|73117|6|Mentioned|p10|||[Includes/supersedes Italia Road Formation].||||||
12872|Mount Knobby Formation|9548|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Includes: Mount Alma Conglomerate Member.||||||
12872|Mount Knobby Formation|22508|6|Mentioned|p5||Early Devonian|Lachlan Fold Belt||||||
12872|Mount Knobby Formation|22768|5|Briefly described|p170|||||||||
12872|Mount Knobby Formation|22857|4|Described|p170, p446 App.1, Tb.A1.6|Middle Devonian|Early Devonian|Of the Cobar Supergroup. Max. thickness: 3km. Geological Province: Melrose Trough (Darling Basin).||||||
12872|Mount Knobby Formation|41821|6|Mentioned|p11 Fig.5|||Occurs in Gindoono sheet area||||||
12872|Mount Knobby Formation|43089|5|Briefly described|Map Legend|||of Cobar Supergroup||||||
12872|Mount Knobby Formation|43263|6|Mentioned|Map Legend||Early Devonian|||||||
12872|Mount Knobby Formation|43757|6|Mentioned|p510|||||||||
12872|Mount Knobby Formation|70751|6|Mentioned|p12|Lochkovian|Pridoli|||Of Kopyje Group? or equivalent to?|May include Kooranjie Conglomerate [Member]?|||16-MAR-19
12872|Mount Knobby Formation|71039|6|Mentioned|p12|||Very little petrographic information and very few historic thin sections exist for this unit.|||||Chloritic-phyllite and deformed sandstone.|
12872|Mount Knobby Formation|71693|5|Briefly described|Map legend.|Lochkovian|Pridoli|||Of Kopyje Group.|||Parallel-laminated and ripple cross-bedded, partly graded, medium- to fine-grained, lithic-quartz and lithic sandstone, siltstone and massive polymictic pebble conglomerate; very minor crystal tuff.|16-MAR-19
12872|Mount Knobby Formation|72958|6|Mentioned|p11|Lochkovian|Pridoli|Cobar Basin. Nymagee area.||||Partly underlain by and equivalent to Kooranjie Conglomerate[?]. Equivalent to Babinda Volcanics.||
12887|Mount Lewin Limestone Member|23214|3|Fully described|p40|Eastonian|Eastonian|Of Vandon Limestone. Previously "grey unit" of Percival (1976). Max. thickness 30m.||||||
12887|Mount Lewin Limestone Member|38219|2|Defined|p311|Late Ordovician|Late Ordovician|See also Fig.2 and P301.||||||
12887|Mount Lewin Limestone Member|41046|6|Mentioned|Fig.2|||||||||
12887|Mount Lewin Limestone Member|42479|6|Mentioned|p109|||Actually spelt Mt. Lewin ...||||||
12893|Mount Lidgbird Basalt|22773|6|Mentioned|p348||Miocene|Max Age: 6.4 Ma||||||
12893|Mount Lidgbird Basalt|22857|5|Briefly described|p348|Miocene|Miocene|Tholeiitic basalts filling the caldera of the large seamount that became Lord Howe Island. These basalts concluded the volcanic activity on the island.||||||
12893|Mount Lidgbird Basalt|36958|3|Fully described|p162|Pliocene|Miocene|Porphyritic to aphyric basalts. Olivine, plagioclase and clinopyroxene phenocrysts. Flow textures. Mildly alkaline, trending towards hawaiite. Age: 4.40-6.42 +/- 0.14Ma.||||||14-NOV-13
12893|Mount Lidgbird Basalt|61943|5|Briefly described|Map Legend|||Lava flows, commonly contains plagioclase, clinopyroxene and olivine. Lord Howe Island.||||||14-NOV-13
12893|Mount Lidgbird Basalt|61946|5|Briefly described|p108|Pleistocene|Tertiary|Also uses previous name of Mount Lidgbird Volcanics. Alkali olivine basalt. Coarse grained, zeolites. Phenocrysts of olivine, plagioclase and clinopyroxene.||||||14-NOV-13
12893|Mount Lidgbird Basalt|73136|5|Briefly described|p188, p190, p194|Messinian|Messinian|Lord Howe Island. Comprises Mount Lidgbird and Mount Gower. Characterised by towering plunging cliffs due to relative resistance. [Geochron is eruption age?]. Lava flows are generally near horizontal. [Written as Mount Lidgbird Breccia on p191; probably unintentional].|6.4 Ma [K-Ar?]||||Alkaline olivine basalts and hawaiites which form horizontally bedded caldera fill. Includes massive basalt sections of flow lavas.|
12893|Mount Lidgbird Basalt|73554|4|Described|Map legend, back of map|Neogene|Neogene|Lord Howe Island. Part of the Lord Howe Volcanic Complex. Youngest volcanic rocks on the island at ca 6.6 Ma. Consists of many individual lava flows up to 30 m thick and shows columnar jointing. Possibly formed [in whole or part?] as caldera fill lava flows.|ca 6.6 Ma|Lord Howe Volcanic Complex|||Porphyritic basalt (mainly olivine with plagioclase and pyroxene crystals) basalt and aphyric basalt tabular, lava flow deposits up to 30 m thick. Sporadic columnar jointing, some basalt flows and very sparse tuffs.|
12893|Mount Lidgbird Basalt|73581|6|Mentioned|p28 Fig.8|||||||||
12914|Mount Marsden Claystone|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Nile Subgroup (Illawarra Coal Measures). Thin massive limestones, dolomite, claystone, siltstone; few pebble horizons. Max. thickness: 19m. Geological Province: Sydney Basin.||||||
12914|Mount Marsden Claystone|29751|5|Briefly described|p5|||||||||
12914|Mount Marsden Claystone|31621|6|Mentioned|p151|||||||||
12914|Mount Marsden Claystone|34204|6|Mentioned|Table|||||||||
12914|Mount Marsden Claystone|34205|2|Defined|p10|Permian|Permian|||||||
12914|Mount Marsden Claystone|34569|6|Mentioned|p9|||Permian. Fig.3||||||
12914|Mount Marsden Claystone|39232|6|Mentioned|Table 1|||||||||
12914|Mount Marsden Claystone|39293|6|Mentioned|Fig. 8.2|||||||||
12914|Mount Marsden Claystone|40256|6|Mentioned|Fig.3|||||||||
12914|Mount Marsden Claystone|40806|2|Defined|p150|Permian|Permian|Prob. Permian||||||
12914|Mount Marsden Claystone|42657|6|Mentioned|Table 1 P74|||||||||
12914|Mount Marsden Claystone|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Nile Sub-Group of Illawarra Coal Measures||||||
12914|Mount Marsden Claystone|43362|14|Not recorded|Map Legend||Permian|(Provisional first edition)Part of Nile Sub-Group of Illawarra Coal Measures||||||
12914|Mount Marsden Claystone|43363|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
12914|Mount Marsden Claystone|45090|6|Mentioned|p56|||Source of calcarenite in Coorongooba Ck. Sst.||||||
12914|Mount Marsden Claystone|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Nile Subgroup.||Is overlain by Coorongooba Creek Sandstone.||
12933|Mount Misery Granite|22679|4|Described|p 41|Silurian|Silurian|Formerly Mount Misery Adamellite.||||||15-JUL-08
12933|Mount Misery Granite|23214|2|Defined|p163|Late Silurian|Late Silurian|Originally named Mount Misery Adamellite. Intrudes the Adaminaby Group. Weakly deformed felsic granite to aplitic granite. Geological Province: Wyangala Batholith.||||||15-JUL-08
12933|Mount Misery Granite|42726|5|Briefly described|map legend|Silurian||252. Wyangala Batholith. Reserved as Mount Misery, NSW. NOT related to Mount Misery Granite, Vic.||||||
12933|Mount Misery Granite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of boitite granite, contaminated tonalite, microdiorite.||||||15-JUL-08
12933|Mount Misery Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Biotite granite, contaminated tonalite, microdiorite.||||||17-JUL-08
12933|Mount Misery Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|Of Wyangala Batholith.||||||15-JUL-08
12933|Mount Misery Granite|69592|5|Briefly described|p282|Silurian|Silurian|||White Springs Supersuite.|||I-type.|
12933|Mount Misery Granite|70297|5|Briefly described|map legend|Silurian|Silurian|Unassigned Silurian I-type intrusion.||||||
12955|Mount Murray Branch Formation|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Of Cooleman Group. Fossiliferous thin-bedded limestone, chert, siltstone, calcareous siltstone, shale. BMR map symbol: Sut.||||||
12955|Mount Murray Branch Formation|33325|6|Mentioned|Table 2|||||||||
12955|Mount Murray Branch Formation|37727|6|Mentioned|p74|||Synonymous with Pocket Beds.||||||
12955|Mount Murray Branch Formation|43479|14|Not recorded|p116|Ludlow|Wenlock|||||||
12955|Mount Murray Branch Formation|45147|6|Mentioned|M77|||||||||
12964|Mount Nebo Monchiquite|36220|4|Described|p96|||||||||
12964|Mount Nebo Monchiquite|37253|6|Mentioned|Table 1|||||||||
12964|Mount Nebo Monchiquite|42896|5|Briefly described|p55|||||||||
12987|Mount Olive Formation|45090|5|Briefly described|p56|||Relationships, correlation & age.||||||
13039|Mount Pleasant Limestone Member|22736|6|Mentioned|p611 Fig2||Permian|Mount spelled Mt in text||||||
13039|Mount Pleasant Limestone Member|22857|5|Briefly described|p514 App.1 Tb.A1.8|Early Permian|Early Permian|Of the Yessabah Limestone (Macleay Group). Geological Province: Barnard Basin (Nambucca Basin).||||||
13039|Mount Pleasant Limestone Member|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|Geological Province: New England Fold Belt.||||||
13039|Mount Pleasant Limestone Member|44450|5|Briefly described|p134|||Geological Province: New England Fold Belt.||||||
13039|Mount Pleasant Limestone Member|47059|4|Described|p147|||of Yessabah Limestone. INVALID NAME. Mount Pleasant already used in NSW, Vic, ACT, WA for ...||||||
13104|Mount Solitary formation|34449|6|Mentioned|p128|||||||||
13115|Mount Stromlo Granite|23214|4|Described|p258|Carboniferous|Carboniferous|First described as part of the Davies Creek Granite.  Intrudes the Rockley Volcanics.||||||
13115|Mount Stromlo Granite|42712|4|Described|Table 1 p13|Carboniferous|Early Carboniferous|||||||
13115|Mount Stromlo Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
13115|Mount Stromlo Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
13115|Mount Stromlo Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
13145|Mount Tomah basalt|37468|6|Mentioned|Table II|||||||||
13145|Mount Tomah basalt|43344|14|Not recorded|p55|||||||||
13171|Mount View Range Granodiorite|29915|2|Defined|p61|Early Carboniferous|Early Carboniferous|||||||
13171|Mount View Range Granodiorite|36413|6|Mentioned|p98|||||||||
13171|Mount View Range Granodiorite|36528|6|Mentioned|p182|||||||||
13171|Mount View Range Granodiorite|36961|6|Mentioned|Table 1|||||||||
13171|Mount View Range Granodiorite|40246|6|Mentioned|p170|||||||||
13171|Mount View Range Granodiorite|42547|4|Described|p31|||Actually spelt Mt View Range Granodiorite. Age 343my.||||||
13171|Mount View Range Granodiorite|44244|6|Mentioned|p259 Fig. 51|||Mount is Mt. in text.||||||
13171|Mount View Range Granodiorite|68822|6|Mentioned|p338|Carboniferous|Carboniferous|||||||
13171|Mount View Range Granodiorite|71628|3|Fully described|p19: 134-135, 173|||Originally Mt. View Range Granodiorite (Brakel, 1972). Named after Mount View Range, Pokolbin. Occurs ~7 km W of Cessnock as a ~3 x 0.3 km sliver. The type outcrop occurs in the SW corner of Mount Pleasant Vineyard property (Brakel, 1972). Is associated with minor Cu (Au, Ag) mineralisation.|349.3 +/- 2.1 Ma (SHRIMP: Jeon, 2012).|Mount View Suite.||Is nonconformably overlain by the Mount Bright Rhyolitic Ignimbrite Member (Pokolbin Hills Volcanics).|Biotite-hornblende-clinopyroxene granodiorite.|
13172|Mount View Sandstone|42214|6|Mentioned|Table 1 P462|||||||||
13173|Mount Vincent Formation|22969|4|Described|Fig 4.1a||Late Permian|||||||
13173|Mount Vincent Formation|32267|6|Mentioned|p430|||||||||
13173|Mount Vincent Formation|33867|6|Mentioned|Table 1|||||||||
13173|Mount Vincent Formation|39292|6|Mentioned|Fig. 6.3|||||||||
13173|Mount Vincent Formation|39308|5|Briefly described|p476|||See also Fig.23.4||||||
13177|Mount Wagra gneiss|34221|6|Mentioned|p11|||Refers Tattam (1929)||||||
13178|Mount Wallop Quartzite Member|22857|5|Briefly described|p398 App. 1 Tb.A1.3.|Neoproterozoic|Neoproterozoic|Of the Waukeroo Formation? Quartzite horizon with pebbles and cobbles.||||||
13178|Mount Wallop Quartzite Member|30261|5|Briefly described|p13|||||||||
13178|Mount Wallop Quartzite Member|34812|6|Mentioned|p66|||||||||
13178|Mount Wallop Quartzite Member|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13178|Mount Wallop Quartzite Member|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
13184|Mount Warning Central Complex|22773|6|Mentioned|p343|||||||||
13184|Mount Warning Central Complex|22857|5|Briefly described|p345|||At the centre of the Tweed volcano in the central-volcano provinces of NSW.||||||
13184|Mount Warning Central Complex|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|30131|4|Described|p10|||See also P8||||||
13184|Mount Warning Central Complex|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|34340|6|Mentioned|p476|||||||||
13184|Mount Warning Central Complex|34755|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
13184|Mount Warning Central Complex|40896|4|Described|p10|||||||||
13184|Mount Warning Central Complex|43161|4|Described|12-18|||K-Ar Dates: 22.9, 23.7 Ma. Aged: 23.4 Ma||||||
13184|Mount Warning Central Complex|43881|14|Not recorded|p53,72,170|Tertiary|Early Triassic|||||||
13244|Mount Woolooma lamprophyre|39623|6|Mentioned|p33|||||||||
13245|Mount Woowoolahra Granite|46889|6|Mentioned|p277|||Variation of Woowoolahra Granite?||||||
13247|Mount Wright Volcanics|14019|5|Briefly described|p20|Early Cambrian|Early Cambrian|Geological Province: Gnalta Shelf. Correlative of the Antrim Plateau Volcanics.||||||
13247|Mount Wright Volcanics|22671|3|Fully described|p835,838-39,845-47||Early Cambrian|In the Wonaminta Block.  Mount is Mt in text.||||||11-SEP-07
13247|Mount Wright Volcanics|22857|5|Briefly described|p75, p90 Fig. 14.7B|Early Cambrian|Early Cambrian|Of the Gnalta Group. Basalts and andesites with archaeocyathid limestone lenses. Overlain by Cymbric Vale Formation. Geological Province: Mount Wright Block. See also p94 and p404 App. 1 Tb. A1.4.||||||
13247|Mount Wright Volcanics|22858|5|Briefly described|p75,81,94||Neoproterozoic III|Part of the 'Kara beds' in N.S.W. Max Age: 586 (+/-) 7 Ma.||||||
13247|Mount Wright Volcanics|22859|6|Mentioned|p211|||||||||
13247|Mount Wright Volcanics|23932|5|Briefly described|p665 Table 1|Middle Cambrian|Early Cambrian|||||||
13247|Mount Wright Volcanics|24241|5|Briefly described|p15 Fig.2|Cambrian|Cambrian|Geological Province: Darling Basin.||||||
13247|Mount Wright Volcanics|24263|6|Mentioned|p1385|||Geological Province: Wonominta Block||||||
13247|Mount Wright Volcanics|24509|5|Briefly described|p42|Early Cambrian|Early Cambrian|Mount is Mt in text. Age: ~530-520Ma.||||||
13247|Mount Wright Volcanics|29991|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
13247|Mount Wright Volcanics|30683|6|Mentioned|p45|||||||||
13247|Mount Wright Volcanics|30908|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|Part of Gnalta Group||||||
13247|Mount Wright Volcanics|31705|6|Mentioned|p27|||||||||
13247|Mount Wright Volcanics|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
13247|Mount Wright Volcanics|33000|5|Briefly described|p3|||||||||
13247|Mount Wright Volcanics|33004|6|Mentioned|Fig.8|||||||||
13247|Mount Wright Volcanics|35235|6|Mentioned|p209|||||||||
13247|Mount Wright Volcanics|35320|6|Mentioned|p459|||Structural relationships mentioned||||||
13247|Mount Wright Volcanics|36534|6|Mentioned|p226|||||||||
13247|Mount Wright Volcanics|37461|6|Mentioned|p348|||||||||
13247|Mount Wright Volcanics|38661|6|Mentioned|p7|||||||||
13247|Mount Wright Volcanics|38692|6|Mentioned|Fig.9|||||||||
13247|Mount Wright Volcanics|39214|4|Described|p9|||||||||
13247|Mount Wright Volcanics|39885|6|Mentioned|p431|||See also P433||||||
13247|Mount Wright Volcanics|40455|6|Mentioned|Fig.2|||||||||
13247|Mount Wright Volcanics|40642|6|Mentioned|p163|||||||||
13247|Mount Wright Volcanics|41457|6|Mentioned|p10|||||||||
13247|Mount Wright Volcanics|41810|6|Mentioned|Fig.3|||||||||
13247|Mount Wright Volcanics|42266|6|Mentioned|p299|||||||||
13247|Mount Wright Volcanics|42274|6|Mentioned|p458|||||||||
13247|Mount Wright Volcanics|42910|6|Mentioned|p53|||||||||
13247|Mount Wright Volcanics|42966|5|Briefly described|p299|Cambrian||||||||11-SEP-07
13247|Mount Wright Volcanics|42982|5|Briefly described|p331|||Mount is Mt in text.||||||11-SEP-07
13247|Mount Wright Volcanics|43192|4|Described|p63|Early Cambrian|Early Cambrian|Of Gnalta Group.||||||11-SEP-07
13247|Mount Wright Volcanics|43263|6|Mentioned|Map Legend||Early Cambrian|of Gnaita Group. Spelt Mt.Wright Volcanics.||||||
13247|Mount Wright Volcanics|43502|14|Not recorded|Map Legend||Early Cambrian|(Provisional Edition) Part of Gnalta Group||||||
13247|Mount Wright Volcanics|43560|6|Mentioned|Table 1,p231|||Age: approx. 525 Ma||||||
13247|Mount Wright Volcanics|43704|6|Mentioned|p67|||||||||
13247|Mount Wright Volcanics|44093|5|Briefly described|p108|Cambrian|Cambrian|Underlies Cymbric Vale Volcanics. Medium-K to calc-alkaline volcanics.||||||18-MAR-05
13247|Mount Wright Volcanics|44133|5|Briefly described|p18, 31|Early Cambrian||Geological Province: Wonominta Block. Correlates with Mooracoochie Volcanics.||||||
13247|Mount Wright Volcanics|45102|6|Mentioned|Fig.2|||See also P47||||||
13247|Mount Wright Volcanics|46889|6|Mentioned|p267|||||||||
13247|Mount Wright Volcanics|50327|5|Briefly described|p308|Neoproterozoic|Neoproterozoic|Age: 586Ma (lower section of alkaline rift volcanics). Geological province: Curnamona Craton.  Mount is Mt in text.||||||07-FEB-11
13247|Mount Wright Volcanics|50618|5|Briefly described|p253|Early Cambrian|Early Cambrian|Mount is Mt in text. Geological Province: Wonominta Block.||||||
13247|Mount Wright Volcanics|60567|5|Briefly described|p39, p40|Early Cambrian|Early Cambrian|Calc-alkaline rocks, varying from calc-alkaline andesite to dacite with intrusions of calc-alkaline microdolerite to microdiorite.  Age: 525+/-8Ma (Zhou and Whitford, 1994). Geological Province: Koonenberry Belt.||||||
13247|Mount Wright Volcanics|60990|5|Briefly described|p81-82, p83 Fig.2|Early Cambrian|Early Cambrian|The upper part of this unit contains the same archaeocyath fauna as the overlying Cymbric Vale Formation.||Basal Gnalta Group. ||Underlies the Cymbric Vale Formation conformably.||
13247|Mount Wright Volcanics|62787|5|Briefly described|p77, p81|||Of Gnalta Group. Conformably overlain by Cymbric Vale Formation.||||||14-DEC-15
13247|Mount Wright Volcanics|63489|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Andesite, basalt, dacite, shale. Mount is Mt in text.||||||
13247|Mount Wright Volcanics|63789|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Mount = Mt in text. Calc-alkaline volcanics: andesite, basalt, dacite, lesser shale and chert, minor limestone with Archaeocyathid fauna.||||||27-NOV-08
13247|Mount Wright Volcanics|63793|5|Briefly described|p22, p34, p62.|Early Cambrian|Early Cambrian|At least 2438 m thick.||Basal unit in Gnalta Group.||Is overlain by Cymbric Vale Formation.|Calc-alkaline basalts and andesites, cherts, limestones and shales.|19-JAN-15
13247|Mount Wright Volcanics|64671|5|Briefly described|Map legend|Early Cambrian|Early Cambrian|Includes calc-alkaline volcanics - andesite, basalt, dacite; shale, minor chert. Mount is Mt in text.||||||26-NOV-08
13247|Mount Wright Volcanics|64679|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Of the Gnalta Group. Andesite, basalt and dacite; lesser shale and chert; minor limestone with archaeocyathid fossils.||||||27-NOV-08
13247|Mount Wright Volcanics|64680|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group. Calc-alkaline volcanics - andesites, basalt, dacite as well as shale and minor chert.||||||01-DEC-08
13247|Mount Wright Volcanics|64684|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of Gnalta Group.||||||
13247|Mount Wright Volcanics|65337|5|Briefly described|p95.|Early Cambrian|Early Cambrian|Gnalta Shelf. Correlative with Kalkarindji Volcanic Group.||Unit in Gnalta Group.||||
13247|Mount Wright Volcanics|65489|6|Mentioned|p119|||||||Correlated with Mooracoochie Volcanics (Warburton Basin).||
13247|Mount Wright Volcanics|66623|3|Fully described|pp57-61, p v, p14. |Early Cambrian|Early Cambrian|Formerly included in lower 'Gnalta Stage' of Mootwingee Series (Kenny 1934); defined as Mount Wright Volcanics by Warris (1967) but published as Mount Wright Formation (Rose and Brunker 1969). Redefined by Crawford et al. (1997) who separated the unit from Mount Arrowsmith Volcanics on basis of geochemistry. Has same calc-alkaline chemistry as felsic tuff in Ponto Group. Abundant archaeocyathids, with algae and sponge spicules, in limestone lenses. 1375 - c.4000m thick. Age-equivalent to Teltawongee and Ponto Groups.||Unit in Gnalta Group.||Faulted against underlying Mount Arrowsmith Volcanics and overlying Cymbric Vale Formation. Faulted on the east against Ravendale Formation.|Calc-alkaline andesite, dacite and minor basaltic andesite intruded by minor calc-alkaline microdolerite to microdiorite dykes; less commonly shale, chert, rare dolomitic limestone lenses.|
13247|Mount Wright Volcanics|66918|5|Briefly described|Map legend|Cambrian|Cambrian|||Unit in Gnalta Group.||Is overlain by Cymbric Vale Formation.|Calc-alkaline volcanics: basalt, andesite and dacite; shaly mudstone, some partly silicified; minor chert beds, limestone with Archaeocyathids, metamorphosed to prehnite-pumpellyite facies; plagioclase-pyroxene dyke or plug weathered to saprolite.|
13247|Mount Wright Volcanics|66927|5|Briefly described|Map legend|Cambrian|Cambrian|Broad areas of long wavelength magnetic features relating to deep sources beneath the Bancannia Trough.|||||Includes andesitic lavas and associated intrusives, minor siltstone, chert and limestone.|
13247|Mount Wright Volcanics|66929|5|Briefly described|Map legend|Early Cambrian|Early Cambrian||||||Calc-alkaline volcanics: andesite, basalt, dacite; shale, minor chert.|
13247|Mount Wright Volcanics|67105|5|Briefly described|p650-653, 655-658, 661, 663, 665|Cambrian|Cambrian|Mount Wright Arc, Koonenberry Belt. Shallow-marine shelf setting; a marginal volcanic arc. Geochemistry discussed in detail.|~511 Ma.|Gnalta Group.||Is overlain by Cymbric Vale Formation. Correlated with the Mooracoochie Volcanics.|A calc-alkaline basalt-andesite-dacite-rhyolite suite, intercalated with a package of mudstone, siltstone and limestone.|
13247|Mount Wright Volcanics|67208|5|Briefly described|Map legend.|Cambrian|Cambrian|||Unit in Gnalta Group.|||Andesitic lavas and associated intrusives, minor siltstone, chert and limestone with archaeocyathid fauna; regionally metamorphosed to prehnite-pumpellyite facies.|
13247|Mount Wright Volcanics|67322|4|Described|p5; Fig.5|Series 2|Series 2|Of Warris (1967); redefined by Crawford et al. (1997). At least 1375m thick: base not exposed. Age determined from fossils, esp. archeocyathans. Occurs in the Mount Wright-Mutawintji region.||Basal unit of the Gnalta Group.||Overlain by the Cymbric Vale Formation: faulted contact.|Calc-alkaline andesite and dacite with minor basaltic andesite, intruded by microdolerite to microdiorite dykes, overlying a lower section of massive dark cherts interbedded with altered basalts, siltstones, and dolomitised limestones.|22-FEB-18
13247|Mount Wright Volcanics|68822|5|Briefly described|p330|Guzhangian|Stage 2|Mount is spelt as Mt in text. Contains a spread of U-Pb SHRIMP ages from 505 +/- 5 Ma, 519 +/- 5 Ma to 521 +/- 5 Ma.||||||
13247|Mount Wright Volcanics|69043|5|Briefly described|p4, p100-101, p104|Early Cambrian|Early Cambrian|Delamerian Orogen. Mount Wright area, eastern side of the Bancannia Trough. Subduction arc related. Source of major magnetic anomalies at depth. Contains archaeocyathid faunas.||||Is overlain by Cymbric Vale Formation.||
13247|Mount Wright Volcanics|69445|5|Briefly described|p30:17|Early Cambrian|Early Cambrian|Gnalta Shelf, western NSW.||Gnalta Group.||Correlated with Kalkarindji Suite.||12-JUL-16
13247|Mount Wright Volcanics|69874|6|Mentioned|p96 Fig .4.1|||Shown as Mt Wright Volcanics in 520 Ma Fig ure.||||||
13247|Mount Wright Volcanics|70013|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Koonenberry Belt.||Unit in Gnalta Group.||||
13247|Mount Wright Volcanics|70648|5|Briefly described|Map Legend|Cambrian|Cambrian|Appears to be shown as either partially equivalent to, or including Cymbric Vale Formation.||Gnalta Group|||Andesitic lavas and associated intrusions, minor siltstone, chert and limestone with archaeocyathid fauna.|
13247|Mount Wright Volcanics|70650|5|Briefly described|Map Legend|Cambrian|Cambrian|3 un-named subunits: Mostly shaly mudstone, some partially silicified and minor chert beds: Fine- to medium-grained plagioclase-pyroxene dyke or plug, commonly weathered to a chloritic or montmorillonitic saprolite;  Calc-alkaline volcanics - basalt, andesite and dacite.||Gnalta Group|Includes 3 un-named units.||Andesitic lavas and associated intrusives, minor siltstone, chert and limestone with archaeocyathid fauna.|
13247|Mount Wright Volcanics|70744|5|Briefly described|p945|Middle Cambrian|Early Cambrian|Koonenberry Belt.|||||Quartzose turbidites.|
13247|Mount Wright Volcanics|70838|4|Described|p266-267, p269, p271, p276-278, p280-281|Cambrian|Cambrian|Koonenberry Belt. Deposition by repeated turbidity currents on an E-facing continental slope. Possible tectonic settings discussed. Botomian Stage from fossils.|c.517 Ma.|Gnalta Group.||Is overlain by Cymbric Vale Formation. Is faulted against Grey Range and Mutawintji Groups.|Calc-alkaline volcanics; limestone containing Archaeocyathids in upper part.|
13247|Mount Wright Volcanics|71262|5|Briefly described|p5 Fig 2, p8 Fig 5, p9, p10, 12|Cambrian|Cambrian|May have correlatives under the Bancannia Trough.||Unit of Gnalta Group||||
13247|Mount Wright Volcanics|71593|5|Briefly described|p188-p189|Early Cambrian|Early Cambrian|Koonenberry Province. Interpreted to have been deposited in a continental margin arc. Hosts minor fault related Cu prospects and a barite occurrence.|c. 511-506 Ma|||Overlies the Teltawongee Group.||
13247|Mount Wright Volcanics|72951|6|Mentioned|p1012|Cambrian|Cambrian|Delamarian Orogen. Koonenberry Belt. Described as lower-middle Cambrian.|||||Calc-alkaline volcanics.|
13247|Mount Wright Volcanics|73059|5|Briefly described|p1061|Cambrian|Cambrian|Northwest NSW. Formed in a convergent margin setting: arc to forearc environment. The equivalent deep-marine turbidites are represented by the Teltawongee Group to the NE.|525-505 Ma.|||||
13247|Mount Wright Volcanics|73093|5|Briefly described|map legend|Cambrian|Cambrian||||||Andesite (emplaced as lava), minor meta-siltstone, chert and meta-limestone with Archaeocyathids; mostly shaly mudstone, partly silicified chert beds; Fine- to medium-grained plagioclase-pyroxene saprolitic dyke rock; basalt, andesite and dacite.|09-DEC-21
13247|Mount Wright Volcanics|73177|5|Briefly described|p1098, 1100, 1115 Fig.17|Early Cambrian|Early Cambrian|SHRIMP U-Pb ages by Glen (2013).|521 +/- 5 Ma to 505 +/- 5 Ma.|Gnalta Group.|||Calc-alkaline.|
13247|Mount Wright Volcanics|73430|6|Mentioned|p494, p512|Cambrian|Cambrian|Classified as a volcanic arc suite. [Written as Mt Wright Volcanics.]|508+/-3 Ma, 510-500 Ma||||Calc-alkaline volcanics.|
13264|Mountain Creek Volcanics|12185|5|Briefly described|map legend|Lower Devonian|Lower Devonian|Of Black Range Group. Mainly rhyolite, andesite, dacite, agglomerate, tuff. BMR map symbol: Dlm.||||||
13264|Mountain Creek Volcanics|22590|5|Briefly described|P760||Early Devonian|||||||
13264|Mountain Creek Volcanics|22638|1|Redefined|p67|Pragian|Lochkovian|Part of the Boggy Plain Supersuite. Thickness: 5000 m.||||||22-APR-09
13264|Mountain Creek Volcanics|22691|6|Mentioned|Fig7 P319||Devonian|||||||
13264|Mountain Creek Volcanics|22768|6|Mentioned|p178|||||||||
13264|Mountain Creek Volcanics|22778|6|Mentioned|p 163|||||||||
13264|Mountain Creek Volcanics|22857|4|Described|p178, p462 App.1 Tb.A1.6|Lochkovian|Lochkovian|Basal subaerial volcanics of the Black Range Group; overlain by Kirawin Formation, Sugarloaf Creek Formation. Age: 406+/-1Ma (Rb/Sr). Max. thickness: 5km. Geological Province: Canberra-Yass Shelf. See also p464 App.1 Tb.A1.6.||||||
13264|Mountain Creek Volcanics|23309|6|Mentioned|p390|||||||||
13264|Mountain Creek Volcanics|24005|6|Mentioned|p293|||Of Black Range Group. Geological Province: Lachlan Fold Belt||||||
13264|Mountain Creek Volcanics|24266|5|Briefly described|p1486|||Geological Province: Lachlan Fold Belt. Of the Boggy Plain Supersuite.||||||
13264|Mountain Creek Volcanics|24317|5|Briefly described|p14|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|24417|5|Briefly described|p77|||Of Black Range Group.||||||
13264|Mountain Creek Volcanics|24514|5|Briefly described|p31|||Of the Boggy Plain Supersuite. Rhyolitic lavas. Geological Province: Lachlan Fold Belt.||||||
13264|Mountain Creek Volcanics|24580|6|Mentioned|p832|||Geological Province: Eastern Lachlan Fold Belt.||||||
13264|Mountain Creek Volcanics|29456|5|Briefly described|p423|||||||||
13264|Mountain Creek Volcanics|29648|6|Mentioned|p20|||||||||
13264|Mountain Creek Volcanics|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
13264|Mountain Creek Volcanics|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
13264|Mountain Creek Volcanics|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|30069|5|Briefly described|p7|||||||||
13264|Mountain Creek Volcanics|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|30734|6|Mentioned|p18|||||||||
13264|Mountain Creek Volcanics|31013|6|Mentioned|p3|||Lower Devonian||||||
13264|Mountain Creek Volcanics|31019|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|31111|6|Mentioned|p204|||Also mention P206, 210, 212||||||
13264|Mountain Creek Volcanics|32088|6|Mentioned|p10|||U.Sil.-L.Dev.||||||
13264|Mountain Creek Volcanics|32483|4|Described|p29|||Lower Devonian. Strat. table 1||||||17-JUN-08
13264|Mountain Creek Volcanics|32675|6|Mentioned|p8|||Refers Brunker & Offenberg (1970). Strat. Nomenclature||||||
13264|Mountain Creek Volcanics|33325|5|Briefly described|Table 4|||||||||
13264|Mountain Creek Volcanics|33326|6|Mentioned|p441|||Fauna.||||||
13264|Mountain Creek Volcanics|33959|6|Mentioned|p233|||||||||
13264|Mountain Creek Volcanics|34403|6|Mentioned|p141|||||||||
13264|Mountain Creek Volcanics|34405|6|Mentioned|p120|||||||||
13264|Mountain Creek Volcanics|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|35386|3|Fully described|p42|||||||||
13264|Mountain Creek Volcanics|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
13264|Mountain Creek Volcanics|36441|5|Briefly described|map legend|Lochkovian|Lochkovian|Extrusives. I-type. Rhyolite lava and ignimbrite, agglomerate, flow breccia, tuff, shale, sandstone and siltstone. Underlies Kirawin Formation; overlies Blue Waterhole Formation; unconformably overlies Uriarra Volcanics. BMR map code: Dlm1 to Dlm9.||||||
13264|Mountain Creek Volcanics|36443|5|Briefly described|map legend|Pragian|Lochkovian|Of Boggy Plain I-type Suite. Extrusive. Rhyolite, minor tuff. BMR map code: Dlm7.||||||
13264|Mountain Creek Volcanics|37727|6|Mentioned|Fig.1.|||||||||
13264|Mountain Creek Volcanics|38035|6|Mentioned|p93|||||||||
13264|Mountain Creek Volcanics|39409|6|Mentioned|Table XVII|||||||||
13264|Mountain Creek Volcanics|39800|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13264|Mountain Creek Volcanics|40328|6|Mentioned|p17|||See also P62||||||
13264|Mountain Creek Volcanics|40738|4|Described|p624|||||||||
13264|Mountain Creek Volcanics|40882|6|Mentioned|p22|||||||||
13264|Mountain Creek Volcanics|41133|6|Mentioned|p1115|||||||||
13264|Mountain Creek Volcanics|42313|6|Mentioned|p122|||||||||
13264|Mountain Creek Volcanics|42497|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
13264|Mountain Creek Volcanics|42726|5|Briefly described|map legend|Early Devonian||Is refered to as V32 and V42.  Of the Boggy Plain Suite (Boggy Plain Supersuite).||||||08-FEB-05
13264|Mountain Creek Volcanics|43158|4|Described|4,13||Early Devonian|||||||
13264|Mountain Creek Volcanics|43159|4|Described|Fig.2p4,p7,p10.||Early Devonian|Of Mountain Creek Suite.||||||20-MAY-08
13264|Mountain Creek Volcanics|43479|14|Not recorded|p125,151||Early Devonian|||||||
13264|Mountain Creek Volcanics|44092|5|Briefly described|map legend|Early Devonian|Early Devonian|Dlv3||||||
13264|Mountain Creek Volcanics|44093|5|Briefly described|p189 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||18-MAR-05
13264|Mountain Creek Volcanics|44192|5|Briefly described|Map Legend||Lochkovian|||||||
13264|Mountain Creek Volcanics|44936|5|Briefly described|Map Legend||Early Devonian|||||||
13264|Mountain Creek Volcanics|45147|2|Defined|M179|early Pragian|Lochkovian|Lochkovian, possibly to Early Pragian.||||||17-JUN-08
13264|Mountain Creek Volcanics|50230|5|Briefly described|Map legend|Pragian|Lochkovian|Of the Black Range Group.||||||
13264|Mountain Creek Volcanics|50231|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Black Range Group.||||||
13264|Mountain Creek Volcanics|60078|6|Mentioned|Map Legend|Devonian|Devonian|||||||
13264|Mountain Creek Volcanics|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Group. Contains 5 unnamed subunits. Dark purplish to dark grey, massive, occasionally flow banded porphyritic rhyodacitic to dacitic welded crystal-vitric ignimbrite and lava, minor volcaniclastic sandstone.||||||17-JUN-08
13264|Mountain Creek Volcanics|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
13264|Mountain Creek Volcanics|66197|5|Briefly described|p631 Fig.3b, p632|Early Devonian||Canberra-Yass Basin. Silicic volcanics. Underlies the Sugarloaf Creek Formation, the Kirawin Formation and, in places, the Murrumbidgee Group.||||||13-MAR-12
13264|Mountain Creek Volcanics|67823|6|Mentioned|p363 Fig.7|Lochkovian|Lochkovian|Ages from Fig.7(a).|418-412 Ma.|||Is overlain by Kirawin Formation.||
13264|Mountain Creek Volcanics|68592|2|Defined|p429, p446-7, p926-33, p935-6, p948-58|Lochkovian|Lochkovian|See also xxiv, p212-5, p226-8, p269. Name proposed by Walpole (1949) and published by Joplin et al. (1953) for the basal rhyolitic unit of the Black Range Series. Browne (1959) used instead the name Narrangullen Rhyolite, and further complicated matters by naming the upper unit of the Black Range Series the Mountain Creek Tuff. Although this was followed by Packham et al. (1969) and Pedder et al. (1970), most workers have returned to the nomenclature of Joplin et al. (1953); eg in Brunker and Offenberg (1970); Offenberg (1974), it overlay their Derringullen Formation. Type section and "good outcrops" are described. From 500 up to 4,000m thick, thinning to the S. Is correlated with the sequence in the Yass Syncline consisting of Sharpeningstone Conglomerate, Pilleuil Andesite and Waynes Knob Rhyolite, as well as Warrangong Volcanics. Forms undulating, hilly, to mountainous terrain. Associated with low-sulfidation epithermal-type mineralisation, eg Sugarbag Hill prospect. Quarried for aggregate at Bogo, near Bookham. Contact metamorphosed to hornblende-hornfels facies by Burrinjuck Granite. Geochemistry, lithology detailed; geophysical properties described. Unfossiliferous. A SHRIMP U-Pb zircon age of 420.2 +/- 3 Ma (Black, 2006) is considered too old and due to inherited zircons.||Unit in Black Range Group.||Unconformably overlies Goobarragandra Volcanics. Is overlain conformably by Kirawin Formation. Is intruded by Burrinjuck and Willawong Creek Granites. Is faulted against Bendick Formation.|Dark grey or black, rhyolitic to dacitic, welded ignimbrite and lava; minor basal polymictic, pebble to cobble conglomerate and pebbly sandstone, interbedded lenses of volcaniclastic sandstone and siltstone, and volcanic breccia. I -type.|
13264|Mountain Creek Volcanics|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dbm. Includes five unnamed members: volcanic breccia to conglomerate; conglomerate to pebbly sandstone; unfossiliferous limestone; volcaniclastic sandstone, tuffaceous siltstone, breccia; rhyolite to dacite. On Yass and Boorowa 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group||Unconformable base. Is overlain by Kirawin Formation.|Fine grained, feldspar phyric, rhyolitic-dacitic welded ignimbrite and flow banded lava. Lenses of volcaniclastic sandstone, siltstone and breccia; minor basal, polymictic, pebble-cobble conglomerate and pebbly sandstone; high mag susceptibility.|
13264|Mountain Creek Volcanics|70210|5|Briefly described|p2, p33, p36-37, p39-41|Silurian|Silurian|Yass-Goulburn district. A similar, weighted mean age of 420.9 +/- 3.3 Ma is also given.|420.3 +/- 3.0 Ma.|||||
13264|Mountain Creek Volcanics|70540|5|Briefly described|Map Legend|Devonian|Devonian|Includes five unnamed members: volcanic breccia to conglomerate;Coglomerate to pebbly sandstone; unfossiliferous limestone;volcaniclastic sst, tuffaceous siltst, breccia; rhyolite to dacite.||Black Range Group|Includes five unnamed members.||Fine grained, feldspar-phyric rhyolitic-dacitic welded ignimbrite and flow banded lava; lenses of volcaniclastic sandstone, siltstone and volcanic breccia; minor basal, polymictic conglomerate and pebbly sandstone. High magnetic susceptibility.|
13264|Mountain Creek Volcanics|70545|5|Briefly described|Map Legend |Devonian|Devonian|||Black Range Group|||Fine grained, feldspar phyric, rhyolitic-dacitic welded ignimbrite and flow banded lava. Lenses of volcaniclastic sandstone, siltstone and breccia; minor basal, polymictic, pebble-cobble conglomerate and pebbly sandstone; high mag susceptibility.|
13264|Mountain Creek Volcanics|70546|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of fine to coarse grained, thin to thick bedded volcaniclastic sandstone and tuffaceous siltstone; high-very high magnetic susceptibility||Black Range Group|||Fine grained, feldspar phyric, rhyolitic to dacitic welded ignimbrite and flow banded lava; lenses of volcaniclastic sandstone and siltstone and volcanic breccia. Minor basal, polymictic, pebble-conglomerate and pebbly sandstone.|
13264|Mountain Creek Volcanics|71040|5|Briefly described|p9, p11|Early Devonian|Early Devonian|Canberra Zone. Flat-lying to gently dipping.||||Unconformably overlies Cooleman Plains Group.||
13264|Mountain Creek Volcanics|71656|6|Mentioned|p12 Fig.2|Lochkovian|Lochkovian|Shown only in correlation chart (Fig.2).||Black Range Group||Overlies Sharpeningstone Conglomerate and underlies Kirawin Formation.|Volcanics.|
13264|Mountain Creek Volcanics|73215|4|Described|p991, 993-1004|Early Devonian|Early Devonian|Divided into two distinctive domains by a NW-trending fault. Photographs, map, cross-section.|420 +/- 3 Ma (Black, 2006).|Basal Black Range Group.|A major phase of silicic volcanism.|Is overlain by Sugarloaf Creek and Kirawin Formations. Overlies and is partly faulted against Talmo Formation.|Discontinuous basal massive boulder conglomerate. The eastern domain is dominantly dark dacitic rock; the western domain is more varied and mostly rhyodacitic and rhyolitic rocks. Local rheomorphic welded ignimbrites.|
13267|Mountain Dam Limestone|34449|6|Mentioned|Table 2-1|||||||||
13267|Mountain Dam Limestone|36118|6|Mentioned|p67|||||||||
13267|Mountain Dam Limestone|41394|2|Defined|p39|Early Devonian||||||||
13267|Mountain Dam Limestone|41395|6|Mentioned|Map legend|Pragian|Lochkovian|||||||
13267|Mountain Dam Limestone|41528|6|Mentioned|p105|||||||||
13267|Mountain Dam Limestone|41821|6|Mentioned|p11 Fig.5|||Occurs in Kilparney sheet area||||||
13267|Mountain Dam Limestone|43089|5|Briefly described|Map Legend|||of Cobar Supergroup||||||
13267|Mountain Dam Limestone|43757|6|Mentioned|p510|||||||||
13267|Mountain Dam Limestone|68297|5|Briefly described|p191|Lochkovian|Lochkovian|Includes Lochkovian vertebrate fossil fauna.||||||
13267|Mountain Dam Limestone|71039|6|Mentioned|p13|||||||||
13291|Moyne Farm Gabbro|42726|5|Briefly described|map legend|Carboniferous||31.||||||
13328|Mufflers Creek Granite|45147|6|Mentioned|M249|||||||||
13338|Mugincoble Chert|13139|5|Briefly described|p9 Fig. 4, p11|Gisbornian|Darriwilian|Geological Province: Cowra Trough.||||||
13338|Mugincoble Chert|22831|4|Described|p 33||Ordovician|||||||
13338|Mugincoble Chert|22857|4|Described|p416 App. 1 Tb. A1.5|Early Silurian|Late Ordovician|Black to grey massive to thick beds of chert with phyllite interbeds. Max. thickness: ?2km.||||||
13338|Mugincoble Chert|23334|5|Briefly described|9 Fig.4|Silurian|Ordovician|||||||
13338|Mugincoble Chert|24125|5|Briefly described|p3|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
13338|Mugincoble Chert|24215|5|Briefly described|p801|Ordovician|Ordovician|Geological Province:  Lachlan Fold Belt||||||
13338|Mugincoble Chert|24417|3|Fully described|p36|Late Ordovician|Middle Ordovician|Formerly "Mugincoble Beds".||||||
13338|Mugincoble Chert|24600|5|Briefly described|p481|Gisbornian|Darriwilian|Geological Province: Lachlan Fold Belt.||||||
13338|Mugincoble Chert|40365|2|Defined|p327|Middle Ordovician|Middle Ordovician|||||||
13338|Mugincoble Chert|40791|6|Mentioned|p181|||||||||
13338|Mugincoble Chert|40891|3|Fully described|p11|||||||||
13338|Mugincoble Chert|42262|6|Mentioned|Fig. 2 P1810|||||||||
13338|Mugincoble Chert|42489|5|Briefly described|Map legend|Llandovery|Bolindian|||||||
13338|Mugincoble Chert|43441|5|Briefly described|16,17,24|||||||||08-JAN-10
13338|Mugincoble Chert|44093|5|Briefly described|p180 App. 1|Early Silurian|Ordovician|Geological Province: Lachlan Fold Belt.||||||
13338|Mugincoble Chert|44160|5|Briefly described|Map Legend|Llandoverian|Bolindian|||||||08-JAN-10
13338|Mugincoble Chert|46522|2|Defined|p50|Late Ordovician||||||||
13338|Mugincoble Chert|46525|5|Briefly described|p152|||||||||
13338|Mugincoble Chert|46528|5|Briefly described|Map legend|Silurian||||||||
13338|Mugincoble Chert|60008|5|Briefly described|Map Legend|Ordovician|Ordovician|Metasediments.||||||
13338|Mugincoble Chert|60009|5|Briefly described|Map Legend|Gisbornian|Darriwilian|||||||13-JUL-04
13338|Mugincoble Chert|63289|6|Mentioned|p372, p373 Fig. 7|Gisbornian|Darriwilian|Age Da3-Gil.||||||07-FEB-11
13338|Mugincoble Chert|63290|6|Mentioned|p405|Gisbornian|Darriwilian|Age constraints by presence of conodonts.||||||
13338|Mugincoble Chert|63291|6|Mentioned|p419 Fig. 2|||||||||
13338|Mugincoble Chert|67107|6|Mentioned|p696|||Peak Hill, c.45km N of Parkes.||||||
13338|Mugincoble Chert|67322|6|Mentioned|p20|Darriwilian|Darriwilian|Bowman et al. (1982) after Brunker (1972); Krynen et al. (1990). Contains late Darriwilian conodonts. Occurs in the Parkes-Forbes-Junee area.||||||
13338|Mugincoble Chert|67821|6|Mentioned|p170, p177|||Peak Hill district.||||||
13338|Mugincoble Chert|67847|5|Briefly described|p21-p23, p25|Gisbornian|Darriwillian|Age derived from conodont fossil assemblage.||||Equivalent to the Numeralla Chert.||
13338|Mugincoble Chert|68466|6|Mentioned|p64, 66|||Parkes-Forbes-Junee area. Late Darriwilian conodonts.||||Correlates with Whinfell Chert Member (Ballast Formation).||
13338|Mugincoble Chert|70278|6|Mentioned|p1612|||Goonumbla district, Junee-Narromine volcanic belt, Central-west NSW.||||||
13338|Mugincoble Chert|70684|6|Mentioned|p14|Middle Ordovician|Middle Ordovician|Darriwilian age.||||Overlies (inferred) the Kirribilli Formation.||
13338|Mugincoble Chert|72082|5|Briefly described|p22|Late Ordovician|Middle Ordovician|Forbes 1:250K sheet area. Age from (Darriwilian to Gisbornian) conodonts.||||Correlated with Kirribilli Formation.||
13338|Mugincoble Chert|72495|5|Briefly described|p227, p233|Late Ordovician|Late Ordovician|Age is derived from conodont fossils. Structurally duplicated in the western part of the Kirribilli Formation. Appears lithologically similar to the Hoskins Chert Member.||Kirribilli Formation.|||Radiolarian bearing chert.|
13340|Muirs Creek Conglomerate|22736|6|Mentioned|p629||Namurian|||||||
13340|Muirs Creek Conglomerate|22857|4|Described|p512 App.1 Tb.A1.8|Late Carboniferous|Late Carboniferous|Rhyolitic pebble to cobble conglomerate. Max. thickness: 200m. Geological Province: Tamworth Forearc Basin.||||||
13340|Muirs Creek Conglomerate|23157|5|Briefly described|p110 fig2|||||||||
13340|Muirs Creek Conglomerate|24118|5|Briefly described|p3|Carboniferous|Carboniferous|||||||
13340|Muirs Creek Conglomerate|32868|6|Mentioned|p208,Fig.7|||||||||
13340|Muirs Creek Conglomerate|36057|2|Defined|p349|Late Carboniferous|Late Carboniferous|Prob.Upper Carboniferous||||||
13340|Muirs Creek Conglomerate|36528|6|Mentioned|p182|||||||||
13340|Muirs Creek Conglomerate|38801|6|Mentioned|Fig.3|||||||||
13340|Muirs Creek Conglomerate|39660|6|Mentioned|p450|||||||||
13340|Muirs Creek Conglomerate|40883|6|Mentioned|p8|||||||||
13340|Muirs Creek Conglomerate|42547|4|Described|p38|||||||||
13340|Muirs Creek Conglomerate|42833|4|Described|p225|||||||||
13340|Muirs Creek Conglomerate|43017|5|Briefly described|Fig.1,p372|||||||||
13340|Muirs Creek Conglomerate|44093|5|Briefly described|p231 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
13340|Muirs Creek Conglomerate|44244|2|Defined|p219|||Overlies the Koolanock Sandstone; underlies the Alum Mountain Volcanics.  Max thickness: >200m.  Type section in text.  Geological Province: Myall Block.  Synonymous with "Crawford Formation" (Engel 1962) in part.||||||25-AUG-04
13340|Muirs Creek Conglomerate|47056|6|Mentioned|Fig.2 P523|||||||||
13340|Muirs Creek Conglomerate|50263|5|Briefly described|Map Legend|Stephanian|Westphalian|Overlies: Koolanock Sandstone.  Geological Province: Eastern Myall Block.||||||
13340|Muirs Creek Conglomerate|63832|6|Mentioned|p131 Fig.2|Serpukhovian|Serpukhovian|Eastern Myall block, Southern New England Fold Belt. Second (C2) glaciation.||||||
13340|Muirs Creek Conglomerate|64631|6|Mentioned|p44 Fig.2.|Serpukhovian|Serpukhovian|Southern New England Fold Belt, eastern Myall Block. Biostratigraphic age control for base and top.||||||
13340|Muirs Creek Conglomerate|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Serpukhovian|Myall Block, Tamworth Belt.||||||
13354|Mulga Spring Complex|41594|6|Mentioned|p51|||||||||
13364|Mulgoa Laminite Member|35690|2|Defined|p180|Middle Triassic|Middle Triassic|||||||
13364|Mulgoa Laminite Member|39298|5|Briefly described|p262|||See also P263||||||
13364|Mulgoa Laminite Member|39626|6|Mentioned|p276|||||||||
13364|Mulgoa Laminite Member|40602|4|Described|p24|||||||||
13364|Mulgoa Laminite Member|42896|4|Described|p44, Fig.7|||of Ashfield Shale||||||
13364|Mulgoa Laminite Member|42925|4|Described|p22|||of Ashfield Shale||||||
13364|Mulgoa Laminite Member|70661|6|Mentioned|p211|Middle Triassic|Middle Triassic|Age derived from parent unit. Not present in the map sheet area (Moss Vale)||Ashfield Shale||||
13372|Mulla Creek Volcanics|35911|6|Mentioned|Fig.3|||||||||
13385|Mullamuddy Formation|13996|6|Mentioned|p149|Pragian|Pragian|Mudgee area. Contains Baragwanatha flora.||||||
13385|Mullamuddy Formation|22529|5|Briefly described|4 fig 2|Pragian|Lochkovian|Parent Parent Queens Pinch Group. Overlying unit Taylors Hill Formation||||||
13385|Mullamuddy Formation|22590|6|Mentioned|Fig3 P754|Pragian|Lochkovian|||||||
13385|Mullamuddy Formation|22857|4|Described|p476 App.1 Tb.A1.6|Pragian|Lochkovian|Of the Queens Pinch Group. Volcanic arenite and conglomerate, shale. Max. thickness: 750m. Geological Province: Capertee Rise.||||||
13385|Mullamuddy Formation|23043|5|Briefly described|Map Legend|Pragian|Lochkovian|of Queens Pinch Group.||||||
13385|Mullamuddy Formation|23170|2|Defined|p143|Lochkovian|Silurian|of Queens Pinch Group.||||||
13385|Mullamuddy Formation|23522|5|Briefly described|p248 Fig 4|Emsian|Lochkovian|||||||
13385|Mullamuddy Formation|24126|6|Mentioned|p138|||||||||
13385|Mullamuddy Formation|24612|5|Briefly described|p12|Lochkovian|Lochkovian|Contains Carlinastraea fauna.||||||
13385|Mullamuddy Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
13385|Mullamuddy Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
13385|Mullamuddy Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
13385|Mullamuddy Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
13385|Mullamuddy Formation|33326|6|Mentioned|p431|||Fauna.||||||
13385|Mullamuddy Formation|33732|4|Described|p117|||||||||
13385|Mullamuddy Formation|42033|6|Mentioned|p652|||||||||
13385|Mullamuddy Formation|43188|4|Described|p215,Table 4 p213|Pragian|Lochkovian|Queens Pinch Belt.||||||
13385|Mullamuddy Formation|43461|14|Not recorded|Table p621||Siegenian|||||||
13385|Mullamuddy Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
13385|Mullamuddy Formation|43519|14|Not recorded|Tb p119,120|Emsian|Siegenian|||||||
13385|Mullamuddy Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Mudgee. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
13385|Mullamuddy Formation|71924|5|Briefly described|p1, 2, 3|Pragian|Lochkovian|Queens Pinch, near Mudgee. Includes Boucotia loyolensis-Nadiastrophia Assemblage Zone.  Also includes conodonts. Fauna compared to Cunningham Formation fauna. Fauna younger than Crudine [Group], Waterbeach Formation fauna. Basal part unlikely to correlate with Cookman Formation. May correlate with Merrions Tuff.||||Correlated with basal Cunningham Formation, Taylors Hill Formation.||
13385|Mullamuddy Formation|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4|Early Devonian|Early Devonian|||Queens Pinch Group||Underlies the Taylors Hill Formation.||
13397|Mullions Range Volcanics|22679|6|Mentioned|p 28|||||||||
13397|Mullions Range Volcanics|22704|6|Mentioned|p65|||||||||
13397|Mullions Range Volcanics|22768|5|Briefly described|p180|||||||||
13397|Mullions Range Volcanics|22857|4|Described|p180, p470 App.1 Tb.A1.6|Middle Silurian|Middle Silurian|Of the Mumbil Group. Max. thickness: 1.7km. Geological Province: Hill End Trough.||||||
13397|Mullions Range Volcanics|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Mumbil Group.||||||
13397|Mullions Range Volcanics|23048|5|Briefly described|p11 table2||Ludlow|U/Pb Age: 417+/-4 Ma.||||||
13397|Mullions Range Volcanics|23091|6|Mentioned|p637|||||||||
13397|Mullions Range Volcanics|23170|2|Defined|p79|Late Silurian|Ludlow|of Mumbil Group.||||||
13397|Mullions Range Volcanics|23214|3|Fully described|p136-138|Ludlow|Ludlow|Originally included much of the Anson Formation. Mainly submarine deposition. Age 417 +/- 4Ma (SHRIMP U-Pb). Max. thickness: 2000m.||||||10-SEP-18
13397|Mullions Range Volcanics|23335|5|Briefly described|p14, p15 Tb. 1|Late Silurian|Late Silurian|||||||27-OCT-04
13397|Mullions Range Volcanics|24126|6|Mentioned|p2|||||||||
13397|Mullions Range Volcanics|24266|5|Briefly described|p1479|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||09-MAR-05
13397|Mullions Range Volcanics|29906|6|Mentioned|p12|||||||||
13397|Mullions Range Volcanics|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
13397|Mullions Range Volcanics|30099|6|Mentioned|Fig.2|||||||||
13397|Mullions Range Volcanics|31161|5|Briefly described|PA3|||||||||
13397|Mullions Range Volcanics|31411|6|Mentioned|p16|||||||||
13397|Mullions Range Volcanics|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
13397|Mullions Range Volcanics|32047|6|Mentioned|p2|||Acid volcanism along Molong Rise||||||
13397|Mullions Range Volcanics|32088|6|Mentioned|p10|||||||||
13397|Mullions Range Volcanics|32485|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
13397|Mullions Range Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
13397|Mullions Range Volcanics|32672|6|Mentioned|p672|||||||||
13397|Mullions Range Volcanics|33004|6|Mentioned|p181|||||||||
13397|Mullions Range Volcanics|33006|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
13397|Mullions Range Volcanics|33007|6|Mentioned|p11|||Distribution||||||
13397|Mullions Range Volcanics|33282|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
13397|Mullions Range Volcanics|33285|5|Briefly described|p22|||Middle Sil.||||||
13397|Mullions Range Volcanics|33742|6|Mentioned|p116|||Equiv. "Vale Cr. Volc."||||||
13397|Mullions Range Volcanics|34405|5|Briefly described|p111|||||||||
13397|Mullions Range Volcanics|34406|6|Mentioned|p220|||||||||
13397|Mullions Range Volcanics|35185|6|Mentioned|p245|||||||||
13397|Mullions Range Volcanics|35412|6|Mentioned|p10|||Location of Lewis Ponds-Mount Lindsay Cu-Pb-Zn sulphide mineralization.||||||
13397|Mullions Range Volcanics|36285|6|Mentioned|p59|||||||||
13397|Mullions Range Volcanics|37488|3|Fully described|p251|||Depositional environment, palaeogeography & tectonics setting.||||||
13397|Mullions Range Volcanics|37727|4|Described|p75|||||||||
13397|Mullions Range Volcanics|37806|6|Mentioned|p47|||||||||
13397|Mullions Range Volcanics|39214|5|Briefly described|p21|||Mid.- Late Silurian||||||
13397|Mullions Range Volcanics|39325|6|Mentioned|Fig.1|||||||||
13397|Mullions Range Volcanics|39331|6|Mentioned|Fig.8-2|||||||||
13397|Mullions Range Volcanics|39664|6|Mentioned|p121|||||||||
13397|Mullions Range Volcanics|39683|6|Mentioned|p314|||||||||
13397|Mullions Range Volcanics|40328|4|Described|p144|||||||||
13397|Mullions Range Volcanics|42413|4|Described|p54|||||||||
13397|Mullions Range Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
13397|Mullions Range Volcanics|43127|5|Briefly described|p4,Fig.2,Fig.3||Late Silurian|||||||
13397|Mullions Range Volcanics|43263|6|Mentioned|Map Legend||Silurian|Age Middle Silurian.||||||
13397|Mullions Range Volcanics|43476|14|Not recorded|Map Legend|Early Silurian|Early Silurian|(Provisional Edition) L-M. Silurian||||||
13397|Mullions Range Volcanics|43515|14|Not recorded|Map Legend||Early Silurian|(Provisional Edition) (M.Sil)||||||
13397|Mullions Range Volcanics|43516|14|Not recorded|Map Legend|Early Silurian|Early Silurian|(L.-M.Sil)||||||
13397|Mullions Range Volcanics|43517|14|Not recorded|p151,153-159,Pl.XII||Wenlockian|||||||
13397|Mullions Range Volcanics|43640|5|Briefly described|Map Legend||Silurian|||||||
13397|Mullions Range Volcanics|43653|5|Briefly described|Map Legend||Silurian|||||||
13397|Mullions Range Volcanics|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|of Mumbil Group.||||||
13397|Mullions Range Volcanics|43834|6|Mentioned|p32|||Molong High||||||
13397|Mullions Range Volcanics|44093|5|Briefly described|p207 App. 1|Early Devonian|Early Silurian|Of the Mumbil Group. Geological Province: Lachlan Fold Belt.||||||
13397|Mullions Range Volcanics|50124|5|Briefly described|p126|||Of the Mumbil Group. Overlies the Anson Formation. Geological Province: eastern Lachlan Fold Belt.||||||
13397|Mullions Range Volcanics|60424|5|Briefly described|p350 Fig. 1, p351 Fig. 2|Silurian|Silurian|Of the Mumbil Group. Geological Province: Hill End Trough. Porphyritic dacite.||||||
13397|Mullions Range Volcanics|66197|5|Briefly described|p632, p633 Fig.4b|Pridoli|Pridoli|Molong High-Hill End Trough. Quiet deep-water environment of deposition.|417 +/- 4 Ma.|||Overlies the Anson Formation. Underlies the Barnby Hills Shale.|Locally thick pile of silicic volcanics and volcaniclastics.|13-MAR-12
13397|Mullions Range Volcanics|67847|5|Briefly described|p30, p33|||Considered S-type by Pogson and Watkins (1998), however re-analysis in this volume has found that it is likely to be fractionated I-type or A-type.||||Overlies the Anson Formation. Equivalent to the Kangaloolah Volcanics.||
13397|Mullions Range Volcanics|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: late early Silurian to earliest Devonian.||Mumbil Group|||Submarine to subaerial felsic volcanic units of rhyolitic to dacitic lavas and volcaniclastics.|19-MAY-16
13397|Mullions Range Volcanics|73299|6|Mentioned|p1100, p1102 Fig.8|Early Devonian|Late Silurian|Hill End Trough, western. [Map symbol suggests Silurian age]||||Underlies the Barnby Hills Shale.||
13397|Mullions Range Volcanics|73431|6|Mentioned|p363 Fig.1, p366, p367 Tb.1, p368, p372|Silurian|Silurian|Lachlan Orogen. Previous zircon U/Pb SHRIMP weighted mean igneous age of 433.5+/-4.7 Ma, evidence of recrystallisation at 421.6+/-6.7 Ma, and inherited zircon cores of 542-614 Ma (Atton, 2013). Misspelt as Mullings Range Volcanics p365 and p368?|433.5+/-4.7 Ma zircon U/Pb SHRIMP igneous age||||Volcanic unit.|
13407|Mumbedah Granite|42726|5|Briefly described|map legend|Carboniferous||44. Not a variation on Mumbedah Beds.||||||
13407|Mumbedah Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
13408|Mumbidgle Formation|22831|3|Fully described|p 35||Silurian|Previously "Trewilga Beds"||||||
13408|Mumbidgle Formation|22857|4|Described|p450 App.1, Tb.A1.6|Late Silurian|Middle Silurian|Of the Forbes Group. Siltstone, shale, minor sandstone; contains brachiopods, trilobites, graptolites, gastropods, lamellibranchs. Max. thickness: 1000m. Geological Province: Bogan Gate Terrace.||||||
13408|Mumbidgle Formation|24125|5|Briefly described|p3|Silurian|Silurian|Geological Province: Lachlan Fold Belt.||||||
13408|Mumbidgle Formation|24417|3|Fully described|p42|Wenlock|Ludlow|Of Forbes Group.  Overlain by Calarie Sandstone; underlain by Bocobidgle Conglomerate.  Thickness: ~280m at type section.  May be up to 1000m thick.||||||
13408|Mumbidgle Formation|29907|6|Mentioned|Fig.8|||||||||
13408|Mumbidgle Formation|31722|6|Mentioned|p137|||See also Fig. 2||||||
13408|Mumbidgle Formation|33118|5|Briefly described|p1|||M.-U. Sil. Forbes Gp.||||||
13408|Mumbidgle Formation|33121|3|Fully described|p65|||Middle to Late Sil. Forbes Gp.||||||
13408|Mumbidgle Formation|33124|6|Mentioned|p227|||Mid.-Late Sil. graptolites||||||
13408|Mumbidgle Formation|33611|6|Mentioned|p132|||||||||
13408|Mumbidgle Formation|37727|4|Described|p59|||See also P26.||||||
13408|Mumbidgle Formation|39214|5|Briefly described|p18|||||||||
13408|Mumbidgle Formation|39618|6|Mentioned|Fig.7|||||||||
13408|Mumbidgle Formation|40328|6|Mentioned|Fig.12(C2)|||See also Fig.12(C2)||||||
13408|Mumbidgle Formation|40891|3|Fully described|p16|||||||||
13408|Mumbidgle Formation|42489|5|Briefly described|Map legend|Ludlow|Wenlock|||||||
13408|Mumbidgle Formation|43441|6|Mentioned|24|Late Silurian||Middle-late Silurian||||||08-JAN-10
13408|Mumbidgle Formation|46522|2|Defined|p59|Middle Silurian|Late Silurian|||||||
13408|Mumbidgle Formation|46525|6|Mentioned|Fig.1 P143|||||||||
13408|Mumbidgle Formation|46528|5|Briefly described|Map legend|Silurian||||||||
13408|Mumbidgle Formation|50299|5|Briefly described|Map Legend|Silurian|Silurian|Of the Forbes Group.||||||
13408|Mumbidgle Formation|60009|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Forbes Group. Overlies: Bocobidgle Conglomerate.||||||13-JUL-04
13408|Mumbidgle Formation|67847|5|Briefly described|p24|Late Wenlock|Late Wenlock|Age constrained on the basis of graptolite fossils.||Forbes Group||Unconformably overlain by the Calarie Sandstone. Equivalent to the Kirribilli Formation.|Fining-upwards sequence of sandstones and siltstones.|
13408|Mumbidgle Formation|73492|6|Mentioned|p691, p693|Silurian|Silurian|||||||
13411|Mumbil Group|6969|5|Briefly described|p12|Middle Silurian|Middle Silurian|Geological Province: Lachlan Fold Belt.||||||
13411|Mumbil Group|22472|5|Briefly described|p36|||||||||
13411|Mumbil Group|22529|6|Mentioned|1|||||||||
13411|Mumbil Group|22590|6|Mentioned|Fig3 P754||Wenlock|||||||
13411|Mumbil Group|22679|5|Briefly described|p 11||Silurian|||||||
13411|Mumbil Group|22768|5|Briefly described|p175,178,180||Late Silurian|||||||
13411|Mumbil Group|22798|6|Mentioned|p851 Fig.2||Silurian|||||||
13411|Mumbil Group|22857|5|Briefly described|p175, p178, p466 App.1 Tb.A1.6|Late Silurian|Silurian|Shelfal sequence of shale and limestone. Overlain by rocks of the Gregra Group; also overlain by Cuga Burga Volcanics. Geological Province: Hill End Trough and Capertee Rise. See also p454 and p478 App.1, Tb.A1.6.||||||
13411|Mumbil Group|23043|5|Briefly described|Map Legend|Lochkovian|Wenlock|||||||
13411|Mumbil Group|23091|5|Briefly described|p636||Late Silurian|||||||
13411|Mumbil Group|23100|5|Briefly described|p575 (Fig 1)||Silurian|||||||
13411|Mumbil Group|23170|2|Defined|p77|Devonian|Early Silurian|Supersedes 'Mumbil Formation'.||||||
13411|Mumbil Group|23202|6|Mentioned|Fig.1||Silurian|||||||
13411|Mumbil Group|23213|5|Briefly described|p20|Late Silurian|Early Silurian|Age: late Early Silurian to Late Silurian.||||||
13411|Mumbil Group|23214|2|Defined|p123|Early Devonian|Early Silurian|Characterised by widespread shale, fine sandstone/siltstone and carbonate deposition, in many areas in conjunction with felsic volcanic eruptive centres of rhyolitic to dacitic composition. Max. thickness 3000m.||||||
13411|Mumbil Group|23225|6|Mentioned|p12|||Of Lachlan Fold Belt.||||||04-MAR-09
13411|Mumbil Group|23309|6|Mentioned|p390|||||||||
13411|Mumbil Group|23334|6|Mentioned|7|||||||||
13411|Mumbil Group|24007|6|Mentioned|p342|||||||||
13411|Mumbil Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
13411|Mumbil Group|24398|5|Briefly described|p259 Fig. 2|Ludlow|Wenlock|Geological Province: Lachlan Fold Belt.||||||
13411|Mumbil Group|32154|6|Mentioned|p181|||Refers Vandyke (1970 unpubl.)||||||
13411|Mumbil Group|33611|5|Briefly described|p129|||||||||
13411|Mumbil Group|40328|4|Described|p144|||||||||
13411|Mumbil Group|43127|4|Described|p3,Fig.2,Fig.3||Late Silurian|||||||
13411|Mumbil Group|43494|6|Mentioned|p24|Silurian|Silurian|Includes Bells Creek Volcanics and Chesleigh Formation.||||||16-MAR-06
13411|Mumbil Group|43640|5|Briefly described|Map Legend||Silurian|||||||
13411|Mumbil Group|43642|5|Briefly described|Map Legend|Silurian|Silurian|Includes Wallace Shale and Ulah Formation.||||||15-JUL-08
13411|Mumbil Group|43654|5|Briefly described|Map Legend|Silurian|Silurian|Includes; Anson Formation, Wombiana Formation, Campbells Formation, Kangaloolah Volcanics, Bells Creek Volcanics, Alton Limestone Member, Fosters Creek Conglomerate, Box Ridge Volcanics.||||||
13411|Mumbil Group|43782|5|Briefly described|Map Legend|Lochkovian|Wenlock|Informally divided into Mumbil Group (Northwest) and Mumbil Group (East).||||||
13411|Mumbil Group|44093|5|Briefly described|p201 App. 1|Early Devonian|Silurian|See also pp202, 206-208, 213, 215. Includes Kangaloolah Volcanics, Kildrummie Member, Box Ridge Volcanics, Mullions Range Volcanics, Bells Creek Volcanics, Chesleigh Formation, and Tanwarra Shale.||||||
13411|Mumbil Group|50124|6|Mentioned|p125 Fig.2|Early Devonian|Late Silurian|Geological Province: eastern Lachlan Fold Belt.||||||
13411|Mumbil Group|50233|6|Mentioned|Map strat. chart|||Underlies Campbells Group.||||||13-MAY-04
13411|Mumbil Group|50590|5|Briefly described|Map Legend|Silurian|Silurian|Includes: Barnby Hills Shale, Gleneski Formation, Narragal Limestone.||||||
13411|Mumbil Group|60424|5|Briefly described|p350 Fig. 1, p351 Fig. 2|Silurian|Silurian|Includes: Anson Formation, Mullions Range Volcanics, Barnby Hills Shale. Geological Province: Hill End Trough.||||||
13411|Mumbil Group|60987|5|Briefly described|p153|Earliest Devonian|Early Silurian|Pickett (1982). Mumbil Shelf.|||Barnby Hills Shale.||Carbonate-volcanic-fine-grained clastic sequence.|11-MAY-17
13411|Mumbil Group|63287|5|Briefly described|p317 Fig. 2|Pridoli|Wenlock|Includes: Mirrabrooka Formation, Molong Limestone, Borenore Limestone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
13411|Mumbil Group|63290|6|Mentioned|p401 Fig. 5(d)|||Includes; Wallace Shale.||||||
13411|Mumbil Group|64826|5|Briefly described|p1040 Tb. 1|Ludlow|Wenlock|Appears as the corrupted MuMembil Group in Table 1. Contains Mirrabooka and Nandillyan Formations.||||||04-MAR-09
13411|Mumbil Group|68003|5|Briefly described|p24 Fig.3-e, pp145-146. |Pridoli|Llandovery|Lachlan Fold Belt, Brigalow Belt South Bioregion.|||Includes Dripstone and Gleneski Formations, Narragal Limestone, Wylinga Member and Barnby Hills Shale.||Mainly limestone.|
13411|Mumbil Group|68592|5|Briefly described|p426, p650|Late Silurian|Late Silurian||||Includes Anson and Karawina Formations, Bells Creek Volcanics.|Disconformably overlies Pipers Flat Formation.||
13411|Mumbil Group|70036|5|Briefly described|Map legend|||Lachlan Fold Belt. Included in a mapped unit of Silurian and Devonian sedimentary and volcanic rocks including strongly to moderately deformed felsic to andesitic metasedimentary rocks, conglomerate, sandstone, siltstone, mudstone, shale, tuff, basalt, andesite and rhyolite.||||||
13411|Mumbil Group|70297|4|Described|map legend, on side 2 of map sheet|Lochkovian|Wenlock|Age: late early Silurian to earliest Devonian. Erosional base. Interpreted as a shelf and slope sequence that outcrops in two north-trending belts on either side of the Hill End Trough. Includes thick carbonate units, submarine to subaerial felsic volcanic rocks and fine-grained clastic rocks.|||Formation: Anson, Hollanders, Karawina, Mirrabooka, Ulah, Wombiana. Shale: Barnby Hills, Tanwarra, Wallace. Volcanics: Bells Creek, Mullions Range. Limestone: Nandillyan, Molong, Borenore.|Underlies Chesleigh Group; adjacent to Campbells Group (relationship?).|Pyritic and calcareous siltstone/shale, mudstone, fine quartz- to lithic-rich sandstone/siltstone, and limestone. Contains two felsic units of rhyolitic to dacitic lavas and volcaniclastics.|
13411|Mumbil Group|70684|6|Mentioned|p50 Fig.24|Late Silurian|Late Silurian||||Wallace Shale.|||
13411|Mumbil Group|71069|6|Mentioned|p125, p154||||||Includes the Bells Creek Volcanics|||
13411|Mumbil Group|71600|6|Mentioned|p23 Fig 1|Silurian|Silurian|Geological province: Lachlan Fold Belt.|||Includes Barnby Hills Shale, Camelford Limestone, Warderie Volcanic Member.|||
13428|Munderoo Granodiorite|40328|4|Described|p209|||||||||
13428|Munderoo Granodiorite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
13428|Munderoo Granodiorite|45087|5|Briefly described|p34|||Chemical analyses||||||
13428|Munderoo Granodiorite|69801|5|Briefly described|p2, p4-p5, p104-109, p137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Obsolete name, incorporated into the Bogandyera Granite of the Bogandyera Suite by Chappell et al (1999). Occurs within the Maragle Batholith southwest of Adelong. Previously considered to be Devonian in age (Chappell et al., 1991). Sample locality, sample description, petrography, SHRIMP analyses and interpretation are detailed.|429.2 +/- 2.0 Ma (SHRIMP)|Mannus Creek Suite|||I-type, pale-grey, medium- to coarse-grained biotite granodioritic rocks.|
13430|Mundi Mundi Granite|22771|6|Mentioned|p42,49||Mesoproterozoic|||||||
13430|Mundi Mundi Granite|22857|6|Mentioned|p49|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|23818|5|Briefly described|p35|Calymmian|Calymmian|Of the Willyama Complex. Age: 1520 Ma. Geological Province: Willyama Block.||||||
13430|Mundi Mundi Granite|29863|6|Mentioned|p350|||||||||
13430|Mundi Mundi Granite|29864|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|29865|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|29991|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|30177|6|Mentioned|p195|||1560 Ma||||||26-FEB-13
13430|Mundi Mundi Granite|30260|6|Mentioned|Fig.2|||||||||
13430|Mundi Mundi Granite|30908|6|Mentioned|Map legend|Mesoproterozoic|Mesoproterozoic|||||||
13430|Mundi Mundi Granite|31012|6|Mentioned|p8|||Lithology. Carpentarian||||||
13430|Mundi Mundi Granite|31435|6|Mentioned|p38|||||||||
13430|Mundi Mundi Granite|31595|6|Mentioned|Table 1|||||||||
13430|Mundi Mundi Granite|31596|6|Mentioned|p282|||||||||
13430|Mundi Mundi Granite|32671|6|Mentioned|Map legend|Carpentarian|Carpentarian|||||||
13430|Mundi Mundi Granite|33004|6|Mentioned|p126|||||||||
13430|Mundi Mundi Granite|33287|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|33472|6|Mentioned|p475|||||||||
13430|Mundi Mundi Granite|33875|6|Mentioned|p17|||Uranium mineralisation.||||||
13430|Mundi Mundi Granite|34469|6|Mentioned|p109|||Upper Proterozoic. See also pp110,111||||||26-FEB-13
13430|Mundi Mundi Granite|34534|6|Mentioned|Fig.2.12|||||||||
13430|Mundi Mundi Granite|34537|6|Mentioned|p35|||1520my||||||
13430|Mundi Mundi Granite|34550|6|Mentioned|p23|||||||||
13430|Mundi Mundi Granite|34604|6|Mentioned|p251|||K/Ar age||||||
13430|Mundi Mundi Granite|34812|6|Mentioned|p12|||||||||
13430|Mundi Mundi Granite|34834|6|Mentioned|p219|||||||||
13430|Mundi Mundi Granite|34896|6|Mentioned|p296|||||||||
13430|Mundi Mundi Granite|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
13430|Mundi Mundi Granite|36584|6|Mentioned|Fig.19-42|||||||||
13430|Mundi Mundi Granite|37581|6|Mentioned|p76|||||||||
13430|Mundi Mundi Granite|37931|6|Mentioned|p534|||||||||
13430|Mundi Mundi Granite|38068|6|Mentioned|p67|||||||||
13430|Mundi Mundi Granite|38411|6|Mentioned|Fig.2|||||||||
13430|Mundi Mundi Granite|39214|6|Mentioned|p5|||||||||
13430|Mundi Mundi Granite|39638|6|Mentioned|Table 1|||||||||
13430|Mundi Mundi Granite|39640|6|Mentioned|p208|||||||||
13430|Mundi Mundi Granite|39652|6|Mentioned|p4|||||||||
13430|Mundi Mundi Granite|39885|6|Mentioned|Fig.1|||||||||
13430|Mundi Mundi Granite|40291|6|Mentioned|Fig.3|||||||||
13430|Mundi Mundi Granite|40582|5|Briefly described|p467|||||||||
13430|Mundi Mundi Granite|41402|6|Mentioned|p37|||||||||
13430|Mundi Mundi Granite|41405|5|Briefly described|p204|||||||||
13430|Mundi Mundi Granite|42090|6|Mentioned|p18|||||||||
13430|Mundi Mundi Granite|42813|6|Mentioned|p13|||||||||
13430|Mundi Mundi Granite|43052|6|Mentioned|p92|||||||||
13430|Mundi Mundi Granite|43269|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
13430|Mundi Mundi Granite|43344|14|Not recorded|p2|||Intrudes Willyama Complex||||||
13430|Mundi Mundi Granite|43491|14|Not recorded|pI/37|||||||||
13430|Mundi Mundi Granite|43501|14|Not recorded|Map Legend|Neoproterozoic|Mesoproterozoic|(Provisional Edition)||||||
13430|Mundi Mundi Granite|43502|14|Not recorded|Map Legend||Mesoproterozoic|(Provisional Edition)  1307-1466 my. Radiometric age||||||
13430|Mundi Mundi Granite|45003|14|Not recorded|p30|||||||||
13430|Mundi Mundi Granite|46595|14|Not recorded|p.283-287,301-307|||On many pages. p.310,311,313,319.  Age determinations. 1820 +/- 100 m.y. (H54-15,I54-3).||||||
13430|Mundi Mundi Granite|46597|14|Not recorded|p186|||||||||
13430|Mundi Mundi Granite|46889|6|Mentioned|p276|||||||||
13430|Mundi Mundi Granite|48894|6|Mentioned|p9|||Age. See also pp10,11.||||||26-FEB-13
13430|Mundi Mundi Granite|50081|5|Briefly described|p43|Calymmian|Calymmian|Age: ~1590 Ma. Geological Province: Curnamona Province.||||||24-FEB-05
13430|Mundi Mundi Granite|50606|5|Briefly described|p5.15|||Geological Province: Broken Hill Block.||||||
13430|Mundi Mundi Granite|50619|5|Briefly described|p175|Mesoproterozoic|Mesoproterozoic|Age: ca 1.59Ga.  Geological Province: Broken Hill Block.||||||12-AUG-04
13430|Mundi Mundi Granite|60485|5|Briefly described|p28 Fig. 2|||Age: 1600-1580Ma.  Geological Province: Broken Hill Domain.||||||03-MAR-05
13430|Mundi Mundi Granite|60657|5|Briefly described|p13 Fig. 2|Mesoproterozoic|Mesoproterozoic|Age: ~1500Ma. Geological Province: Curnamona Craton.||||||10-MAY-05
13430|Mundi Mundi Granite|62592|5|Briefly described|p16 Fig.2.2. |Calymmian|Statherian|Broken Hill Domain, Curnamona Province.|c.1600 - 1580 Ma.|||||
13430|Mundi Mundi Granite|63020|5|Briefly described|p987 Fig. 8|Mesoproterozoic|Mesoproterozoic|Age: 1590Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||10-AUG-07
13430|Mundi Mundi Granite|63102|5|Briefly described|p13,51|||Geological province: Broken Hill Domain, Curnamona Province.|~1600-1580 Ma|||||
13430|Mundi Mundi Granite|63489|5|Briefly described|Map legend|Mesoproterozoic|Mesoproterozoic|Geological Province: Mount Babbage Inlier.||||||10-SEP-07
13430|Mundi Mundi Granite|63866|6|Mentioned|p37-p38, p49||||1591 +/- 5 Ma (Page et al., 2005a)|||||
13430|Mundi Mundi Granite|64743|6|Mentioned|p344 Fig.5. |||Intruded the Broken Hill Block during the Olarian Orogeny. Age is U/Pb SHRIMP age from Page et al. 2005.|1591 +/- 5 Ma.|||||04-JUN-15
13430|Mundi Mundi Granite|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1591 +/- 5 Ma.|||||
13430|Mundi Mundi Granite|68126|5|Briefly described|p5-6|||Broken Hill Domain, Curnanoma Province. Occurs in Cusin Creek pluton and Brewery Creek pluton. Appears as Mundi Mundi granite on p6. Three age determinations (Page, 2006; Page et al., 2000) are in the age range c.1580 - c.1596 Ma.|||||Non-foliated, leucocratic 2-mica granite.|
13430|Mundi Mundi Granite|70657|5|Briefly described|p13 Fig.6, p48, p56|Calymmian|Statherian|Curnamona Province, Broken Hill Domain. Associated with Willyama Supergroup. Syn- to post-tectonic granites. Appears as Mundi Mundi Granites in Fig.6.|~1600-1580 Ma.|Ninnerie Supersuite.|||Granites.|
13430|Mundi Mundi Granite|71968|6|Mentioned|p5|||Geological province: Curnamona province.||||||
13430|Mundi Mundi Granite|72461|6|Mentioned|p6|||Gawler Craton. Broken Hill Domain.|1591 +/- 5 Ma|||||
13430|Mundi Mundi Granite|72949|6|Mentioned|p36|Calymmian|Calymmian|Curnamona Province. Broken Hill / Olary Blocks. See also Mundi Granite p35.|1591 +/- 5 Ma|||||24-DEC-21
13443|Mundoonen Sandstone|22857|5|Briefly described|p134, p424 App. 1 Tb. A1.5|Early Silurian|Early Silurian|Massive sandstone, siltstone, quartzite, argillite; contains lamellibranch fossils. Max. thickness: 2.8km (est.). Geological Province: Yass-Canberra Shelf.||||||
13443|Mundoonen Sandstone|23245|5|Briefly described|p134||Early Silurian|||||||
13443|Mundoonen Sandstone|23454|6|Mentioned|p33|||||||||
13443|Mundoonen Sandstone|24317|5|Briefly described|p14, p15 Fig.1|Early Silurian|Ordovician|Overlies Bendoc Group.||||||
13443|Mundoonen Sandstone|30069|5|Briefly described|p3|||||||||
13443|Mundoonen Sandstone|30332|3|Fully described|p124|||||||||
13443|Mundoonen Sandstone|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
13443|Mundoonen Sandstone|30734|6|Mentioned|p17|||||||||
13443|Mundoonen Sandstone|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
13443|Mundoonen Sandstone|32820|6|Mentioned|Table 1|||Refers Crook et al (1973)||||||
13443|Mundoonen Sandstone|33125|6|Mentioned|p15|||Correlation chart||||||
13443|Mundoonen Sandstone|34405|6|Mentioned|Fig.3.9|||||||||
13443|Mundoonen Sandstone|35384|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
13443|Mundoonen Sandstone|35386|3|Fully described|p9|||||||||
13443|Mundoonen Sandstone|36411|6|Mentioned|p269|||Refers Cramsie et al 1978 for definition||||||
13443|Mundoonen Sandstone|36413|6|Mentioned|p31|||See also Table 3||||||
13443|Mundoonen Sandstone|37752|6|Mentioned|p106|||||||||
13443|Mundoonen Sandstone|38151|6|Mentioned|Table 1|||||||||
13443|Mundoonen Sandstone|38202|6|Mentioned|Fig.1|||||||||
13443|Mundoonen Sandstone|39331|3|Fully described|p49|||||||||
13443|Mundoonen Sandstone|40328|3|Fully described|p159|||||||||
13443|Mundoonen Sandstone|50230|5|Briefly described|Map legend|Early Silurian|Early Silurian|Quartzose to lithic-quartz sandstone.  Overlies the Bendoc Group.  The nature of the contact with Bango Limestone Member above is unknown.||||||
13443|Mundoonen Sandstone|50231|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||
13443|Mundoonen Sandstone|50232|4|Described|Map legend|Llandoverian|Llandoverian|Thickly bedded massive to graded medium-grained to granule quartzose to lithic-quartz sandstone.||||||
13443|Mundoonen Sandstone|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of Margules Group. Thick-bedded massive to graded med-gr. granule quartzose to lithic-quartz sst.; thinly bedded, massive-fine- to med.gr.quartzose-lithic-qtz sst.interbedded with x-lam.sst; with 2 quartzose to lithic-quartz subunits...||||||09-SEP-08
13443|Mundoonen Sandstone|66197|5|Briefly described|p629, p631 Fig.3b|Llandovery|Eastonian|Canberra-Yass Basin. Deep marine shale and sandstone. Eastonian.||||||13-MAR-12
13443|Mundoonen Sandstone|67322|5|Briefly described|p17|Early Silurian|Late Ordovician|Modified by Sherwin, in Thomas et al.(in press), after Mundoonen Series of Sherrard (1939). Forms characteristic red, brown, and orange sandstone exposures. At least 1200 m thick. Occurs in the Goulburn region.||||May correlate with the Poidevins Sandstone, and Cobbannah or Yalmy Groups.|Turbiditic sandstone.|22-FEB-18
13443|Mundoonen Sandstone|68592|3|Fully described|p255, p269, p298, p325-7, p343-67, p420|Late Ordovician|Late Ordovician|See also p442-3, p1679, p1866-7. Forms the prominent Mundoonen Range. Over 1300m thick. Representative section described. Sediments sourced partly from Abercrombie Formation. Previously regarded as Silurian (Crook et al., 1973). Geophysical properties detailed. Problems with fossils and age determination discussed.||Unit in Margules Group.||Overlies Warbisco Shale gradationally. Is intruded/overlain by Hawkins Volcanics. Contact metamorphosed by Bundong Granite.|Brown to yellowish-brown, weathering to deep red, fine-grained to granule, thin- to thick-bedded, muddy lithic-quartz to quartzose sandstone, with minor interbedded siltstone. Small-scale cross-lamination and slump structures.|
13443|Mundoonen Sandstone|69159|5|Briefly described|Map legend|Bolindian|Bolindian|||Unit in Margules Group.||Overlies Warbisco Shale.|Medium- to very thickly-bedded, fine- to coarse-grained quartzose sandstone, and interbedded grey, buff and khaki siltstone.|07-SEP-15
13443|Mundoonen Sandstone|70192|4|Described|Map Legend|Bolindian|Bolindian|[Theta]mm. Includes two unnamed mapped members; one massive-graded, medium-coarse lithic-quartz sandstone with bimodal sorting and one massive-laminated, fine-medium grained, lithic-quartz sandstone interbedded with cross laminated siltstone. On Boorowa, Crookwell, Yass and Gunning 1:100 000 mapsheet portions of Time-Space Plot.||Margules Group|Includes two unnamed units.||Brown to yellowish brown, weathered to red, fine-grained to granule quartz-lithic quartz sandstone with interbedded ripple cross laminated siltstone, bedding is thin- very thick, massive to graded.|
13443|Mundoonen Sandstone|70540|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes an unnamed member of thinly bedded, massive and laminated, fine-medium grained lithic quartz-quartzose sandstone.||Margules Group|||Fine grained-granule, quartzose-lithic quartz sandstone with interbedded ripple cross-laminated siltstone; bedding varies from thin-very thick and massive-graded.|
13443|Mundoonen Sandstone|70541|4|Described|Map Legend|Ordovician|Ordovician|Includes two unnamed mapped members; one massive-graded, medium-coarse lithic-quartz sandstone with bimodal sorting and one massive-laminated, fine-medium grained, lithic-quartz sandstone interbedded with cross laminated siltstone.||Margules Group|Includes two unnamed members.||Brown to yellowish brown, weathered to red, fine-grained to granule quartz-lithic quartz sandstone with interbedded ripple cross laminated siltstone, bedding is thin- very thick, massive to graded.|
13443|Mundoonen Sandstone|70545|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes two unnamed subunits including a thickly bedded, massive to graded, medium-coarse grained lithic-quartz to quartzose sandstone and a thinly bedded, massive and laminated, fine-medium grained lithic quartz to quartzose sandstone.||Margules Group|||Brown to yellowish-brown, weathered to red, fine grained-granule quartzose-lithic quartz sandstone with interbedded ripple cross-laminated siltstone; bedding varies from thin to very thick and massive to graded.|
13443|Mundoonen Sandstone|70546|5|Briefly described|Map Legend|Ordovician|Ordovician|||Margules Group|||Fine grained to granule, quartzose to lithic quartz (muddy)sandstone with interbedded ripple cross laminated siltstone. Bedding varies from thin to very thick and massive to graded.|
13443|Mundoonen Sandstone|71069|3|Fully described|p22, p40 fig 17, p59, p73 fig 26, p82|Llandovery|Bolindian|Name derived from the Mundoonen Range. Previously termed the Mundoonen Series or Jerrawa Series. Subdivided into two unnamed facies: siltstone rich or sandstone rich packages. Forms prominent ridges of the Mundoonen Range or in the Primrose Valley.  Age derived from unit relationships. No type section given, although a representative section has been nominated. Estimated thickness ranging from 850m to 2400m. Interpreted to have been deposited in a deep marine, but proximal depositional environment on the basis of turbidite sequences. Distribution, primary structures/textures, tectonic structure and geophysical characteristics discussed. See also  p84, p87-98, p120, p169, p170,||Margules Group||Overlain by the Covan Creek Formation. Conformably overlies the Warbisco Shale. Equivalent to the Poidevins Sandstone.|Thickly bedded, massive to graded, medium to coarse grained lithic quartz to quartzose sandstone. Tinly bedded, massive and laminated, fine to medium grained lithic quartz to quartzose sandstone interbedded with ripple cross laminated siltstone.|
13443|Mundoonen Sandstone|71656|6|Mentioned|p12 Fig.2|Bolindian|Bolindian|Shown only in correlation chart (Fig.2).||Margules Group||||
13443|Mundoonen Sandstone|71691|5|Briefly described|Map legend.|Ordovician|Ordovician|The two facies are locally mapped separately.||Margules Group.||Overlies Warbisco Shale (Bendoc Group).|Medium- to very thick-bedded, fine- to coarse-grained quartzose sandstone with interbedded grey, buff and khaki siltstone.|
13443|Mundoonen Sandstone|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|The two facies are mapped separately.||Margules Group.||Overlies Warbisco Shale.|Medium- to very thick-bedded, fine- to coarse-grained quartzose sandstone and interbedded grey, buff and khaki siltstone.|
13443|Mundoonen Sandstone|71700|3|Fully described|vi, viii, p7, p9, p48-p50, |Llandovery|Early Bolindian|Named for the Mundoonen Range between Yass and Gunning in Goulburn250. The initial usage of this unit (Sherrard 1939) included parts of what is now mapped as Bendoc and Adaminaby Group. This unit now incorporates rocks previously regarded as Birkenburn Beds and De Drack by Felton and Huleatt (1975, 1977). This unit contains two unnamed packages; a sandstone-rich and siltstone-rich package. A type area is implied in the Mundoonen Range and a representative section south of the Mundoonen Trigonometrical Station was nominated in Thomas and Pogson 2012. This unit is estimated to be almost 1300m thick near the Mundoonen Trigonometrical Station. Lithology of the informal sub-units is described. Distribution, structure, geomorphic expression, outcrop, metamorphism, geophysical characteristics, depositional environment and distinguishing features are discussed. Faulted against the Abercrombie Formation. Equivalent to the Poidevins Sandstone, Dignams Siltstone, New Country Sandstone and the Willandra Sandstone. The age of this formation is poorly constrained but may extend into the Silurian. This unit is interpreted as the resumption of terrigenous sedimentation related to glacio-eustatic lowering of sea level in the early to mid Bolindian. Overlain by the Bango Limestone Member of the Hawkins Volcanics. Intruded by the Bundong Granite. See also p52, p64, p83, CD.||Margules Group||Conformably overlies the Warbisco Shale. Unconformably overlain by the Woodlawn Volcanics of the Mount Fairy Group.|Medium- to very thick-bedded, fine- to coarse-grained quartzose sandstone, and interbedded grey, buff and khaki siltstone which is ferruginised in places. The sandstone is rounded to sub-rounded and generally moderately-sorted.|
13443|Mundoonen Sandstone|73140|5|Briefly described|p495 Fig.1, Fig.7|Bolindian|Bolindian|Uncertainty indicated for minimum age.||Margules Group||Overlies Warbisco Shale||
13443|Mundoonen Sandstone|73264|6|Mentioned|p1392 Fig.14|||Shown as Mundoonen Ss. See also Mundoonen Formation.||||||
13470|Mungo Unit|29643|5|Briefly described|p47|||||||||
13477|Munmorah Conglomerate|22745|5|Briefly described|p127||Scythian|Narrabeen Group, Sydney Basin. Overlies Dooralong Shale. Overlain by Tuggerah Formation.||||||
13477|Munmorah Conglomerate|22857|4|Described|p520 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Narrabeen Group. Medium to coarse-grained sandstone and conglomerate; minor siltstone and claystone. Max. thickness: 140m. Geological Province: Sydney Basin.||||||
13477|Munmorah Conglomerate|22969|4|Described|Fig 4.1a||Early Triassic|||||||
13477|Munmorah Conglomerate|24121|5|Briefly described|p103|Triassic|Triassic|Of Narrabeen Group.||||||21-JAN-05
13477|Munmorah Conglomerate|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
13477|Munmorah Conglomerate|29915|6|Mentioned|p68|||||||||
13477|Munmorah Conglomerate|29922|6|Mentioned|p49|||||||||
13477|Munmorah Conglomerate|29926|6|Mentioned|Fig.3|||||||||
13477|Munmorah Conglomerate|30286|6|Mentioned|p1099|||Stratigraphic table||||||
13477|Munmorah Conglomerate|31129|5|Briefly described|p125|||Pt. Narrabeen Gp. See also P127-131||||||
13477|Munmorah Conglomerate|31276|6|Mentioned|p147|||Microflora||||||
13477|Munmorah Conglomerate|31297|6|Mentioned|p6|||||||||
13477|Munmorah Conglomerate|31426|6|Mentioned|Fig.1|||||||||
13477|Munmorah Conglomerate|31549|6|Mentioned|p159|||Stratigraphic succession||||||
13477|Munmorah Conglomerate|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
13477|Munmorah Conglomerate|31884|6|Mentioned|Table 1|||Triassic||||||
13477|Munmorah Conglomerate|32937|6|Mentioned|p54|||Geology||||||
13477|Munmorah Conglomerate|33683|4|Described|Table 1|||Narrabeen Gp.||||||
13477|Munmorah Conglomerate|33685|6|Mentioned|Table 2|||||||||
13477|Munmorah Conglomerate|33867|6|Mentioned|Table 1|||||||||
13477|Munmorah Conglomerate|33986|6|Mentioned|p30|||Table||||||
13477|Munmorah Conglomerate|34009|6|Mentioned|Table III|||||||||
13477|Munmorah Conglomerate|34106|6|Mentioned|p401|||||||||
13477|Munmorah Conglomerate|34236|6|Mentioned|p17|||||||||
13477|Munmorah Conglomerate|34241|6|Mentioned|p404|||||||||
13477|Munmorah Conglomerate|34270|6|Mentioned|p255|||Table 1||||||
13477|Munmorah Conglomerate|34336|5|Briefly described|p391|||On Table 5.16.||||||
13477|Munmorah Conglomerate|34339|6|Mentioned|p442|||||||||
13477|Munmorah Conglomerate|34351|6|Mentioned|p350|||Fig.5.13||||||
13477|Munmorah Conglomerate|34437|6|Mentioned|p406|||||||||
13477|Munmorah Conglomerate|34448|5|Briefly described|p433|||Permian||||||
13477|Munmorah Conglomerate|35873|6|Mentioned|p51|||||||||
13477|Munmorah Conglomerate|35901|6|Mentioned|p7|||||||||
13477|Munmorah Conglomerate|36042|6|Mentioned|Fig.22|||||||||
13477|Munmorah Conglomerate|37083|6|Mentioned|p164|||||||||
13477|Munmorah Conglomerate|37086|6|Mentioned|p185|||||||||
13477|Munmorah Conglomerate|37087|6|Mentioned|p198|||||||||
13477|Munmorah Conglomerate|37804|6|Mentioned|Table 1|||||||||
13477|Munmorah Conglomerate|37966|6|Mentioned|p4|||||||||
13477|Munmorah Conglomerate|38656|6|Mentioned|Fig.1.3.11|||P150||||||
13477|Munmorah Conglomerate|39287|6|Mentioned|Fig. 2.18|||||||||
13477|Munmorah Conglomerate|39292|6|Mentioned|Fig. 6.2|||||||||
13477|Munmorah Conglomerate|39294|4|Described|p165|||||||||
13477|Munmorah Conglomerate|39306|6|Mentioned|p406|||||||||
13477|Munmorah Conglomerate|39308|6|Mentioned|p458|||See also P463||||||
13477|Munmorah Conglomerate|39609|6|Mentioned|Table 1|||||||||
13477|Munmorah Conglomerate|40625|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic||||||
13477|Munmorah Conglomerate|42214|5|Briefly described|p466|||||||||
13477|Munmorah Conglomerate|43194|5|Briefly described|p118-119, p130|Early Triassic|Early Triassic|Also spelt Munmora Conglomerate. Of Narrabeen Group, Hunter Valley region, Sydney Basin. Equivalent to the informal 'lower lithic conglomerate unit' of the Digby Formation, Gunnedah Basin.||||||
13477|Munmorah Conglomerate|43317|4|Described|Table 1 p10|||||||||
13477|Munmorah Conglomerate|43318|14|Not recorded|opp p6||Late Triassic|See also Lexicon||||||
13477|Munmorah Conglomerate|43320|14|Not recorded|Table 1 p11,12||Triassic|Part of Clifton Subgroup||||||
13477|Munmorah Conglomerate|43342|14|Not recorded|Table 1 p107|||||||||
13477|Munmorah Conglomerate|43344|14|Not recorded|p21,88,164|||||||||
13477|Munmorah Conglomerate|43370|4|Described|p1,3-7|||Type section from Wyong Bore. Correlated with Clifton Sub-Group.||||||12-OCT-15
13477|Munmorah Conglomerate|43383|14|Not recorded|p22|||||||||
13477|Munmorah Conglomerate|43385|14|Not recorded|p182 Table||Early Triassic|||||||
13477|Munmorah Conglomerate|43395|14|Not recorded|p74|||||||||
13477|Munmorah Conglomerate|43447|14|Not recorded|Tbl 1,p24,diag.p26,|||Part of Narrabeen Group. p27,29,37||||||
13477|Munmorah Conglomerate|43508|14|Not recorded|p122|||||||||
13477|Munmorah Conglomerate|44610|14|Not recorded|p47,49|||||||||
13477|Munmorah Conglomerate|46849|6|Mentioned|p195|||||||||
13477|Munmorah Conglomerate|61315|5|Briefly described|Table SY1|Eary Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
13477|Munmorah Conglomerate|66090|6|Mentioned|p23.|Triassic|Triassic|Sydney Basin. Its chert and jasper clasts are typical of New England Orogen provenance; similar to Laurieton Conglomerate (Lorne Basin) and Digby Conglomerate (Gunnedah Basin).||||||
13477|Munmorah Conglomerate|67788|6|Mentioned|p23|Permian|Permian|Photograph of large alluvial channel deposits.||||||
13477|Munmorah Conglomerate|68003|5|Briefly described|p42.|Early Triassic|Early Triassic|Hunter Valley. Thick conglomerate sequences formed by large alluvial fans, generated by erosion in the uplifted New England Fold Belt.||Unit in Narrabeen Group.||Unconformably overlies Maitland Group.||
13477|Munmorah Conglomerate|68711|5|Briefly described|p117, p116 Tbl 2|||Previously included Vales Point Coal Member. Unclear if other Member units are still in use or not.||Of Narrabeen Group|Included Cowper Tuff Member, Karignan Conglomerate Member, Vales Point Coal Member.|||
13477|Munmorah Conglomerate|70647|5|Briefly described|Map Legend|Early Triassic|Late Permian|Sydney Basin.||Clifton Subgroup|||Conglomerate, pebbly sandstone, grey to green shale.|
13509|Muree Sandstone|22610|5|Briefly described|Fig 1|||Maximum thickness 300m||||||
13509|Muree Sandstone|22663|5|Briefly described|NSW97 - 1 p2||Late Permian|||||||01-MAR-10
13509|Muree Sandstone|22857|4|Described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Maitland Group. Fine to coarse-grained sandstone, conglomerate. Correlates with Weismantels Formation (Dewrang Group). Max. thickness: 108m. Geological Province: Sydney Basin.||||||
13509|Muree Sandstone|22969|4|Described|p 21, Fig 2.2||Late Permian|264 - 265 Ma. Underlying unit Branxton Formation. Max. thickness: 180 m.||||||
13509|Muree Sandstone|22970|5|Briefly described|Plate 6|Early Permian||||||||
13509|Muree Sandstone|23540|5|Briefly described|Fig 3 p 420|||||||||
13509|Muree Sandstone|24079|5|Briefly described|p432|Permian|Permian|Of Maitland Group. Geological Province: Sydney Basin.||||||
13509|Muree Sandstone|24121|5|Briefly described|p4, p108, 136|||||||||25-AUG-22
13509|Muree Sandstone|29752|6|Mentioned|p36|||||||||
13509|Muree Sandstone|30340|6|Mentioned|p2529|||Lithology||||||
13509|Muree Sandstone|32073|6|Mentioned|p21|||||||||
13509|Muree Sandstone|32266|6|Mentioned|p24|||||||||
13509|Muree Sandstone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
13509|Muree Sandstone|33702|6|Mentioned|Fig.1|||||||||
13509|Muree Sandstone|33867|5|Briefly described|p6|||||||||
13509|Muree Sandstone|34444|6|Mentioned|Map legend|Permian|Permian|||||||
13509|Muree Sandstone|34845|6|Mentioned|p116|||Also Table 1.||||||
13509|Muree Sandstone|36042|6|Mentioned|Table 1|||||||||
13509|Muree Sandstone|36045|6|Mentioned|p332|||||||||
13509|Muree Sandstone|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
13509|Muree Sandstone|37082|6|Mentioned|p161|||||||||
13509|Muree Sandstone|37773|6|Mentioned|Fig.2|||||||||
13509|Muree Sandstone|38614|6|Mentioned|p14|||||||||
13509|Muree Sandstone|38656|5|Briefly described|Fig.1.5.13|||P280||||||
13509|Muree Sandstone|39287|6|Mentioned|p20|||See also Fig.2.5||||||
13509|Muree Sandstone|39288|4|Described|p63|||||||||
13509|Muree Sandstone|39289|6|Mentioned|p81|||Correlation||||||
13509|Muree Sandstone|39307|6|Mentioned|Table 22.1|||||||||
13509|Muree Sandstone|39308|6|Mentioned|p493|||||||||
13509|Muree Sandstone|39830|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
13509|Muree Sandstone|40166|6|Mentioned|p346|||See also Fig.2||||||
13509|Muree Sandstone|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
13509|Muree Sandstone|40256|6|Mentioned|p306|||||||||
13509|Muree Sandstone|40872|6|Mentioned|p37|||||||||
13509|Muree Sandstone|41054|6|Mentioned|Fig.3|||||||||
13509|Muree Sandstone|41474|6|Mentioned|p59|||||||||
13509|Muree Sandstone|41604|6|Mentioned|Fig.2|||||||||
13509|Muree Sandstone|41834|6|Mentioned|p590|||||||||
13509|Muree Sandstone|41902|5|Briefly described|p5 Table 1|||||||||
13509|Muree Sandstone|41903|6|Mentioned|Map legend|Late Permian||||||||
13509|Muree Sandstone|42609|6|Mentioned|P 73|||Glendon||||||
13509|Muree Sandstone|42780|6|Mentioned|Table 1 P417|||||||||
13509|Muree Sandstone|42916|5|Briefly described|Table 1||Middle Permian|||||||
13509|Muree Sandstone|42925|5|Briefly described|Table 1|Late Permian||||||||
13509|Muree Sandstone|43194|5|Briefly described|p104, p128, p129 Tb. 8.3|Middle Permian|Middle Permian|Of Maitland Group, Hunter and Newcastle Coalfields, Sydney Basin. Near-shore quartz-lithic sand sheets. Correlative of Porcupine Formation in the Gunnedah Basin.||||||13-NOV-13
13509|Muree Sandstone|43257|5|Briefly described|Map Legend||Permian|Age Middle Permian. Of Maitland Group.||||||
13509|Muree Sandstone|43344|14|Not recorded|p88|||||||||
13509|Muree Sandstone|43383|14|Not recorded|p20|||||||||
13509|Muree Sandstone|43440|14|Not recorded|p65,72,83,90,35|||See also Lexicon||||||
13509|Muree Sandstone|43491|14|Not recorded|pVII/44||Permian|||||||
13509|Muree Sandstone|43893|14|Not recorded|p197-201||Permian|||||||
13509|Muree Sandstone|44244|4|Described|p233|Early Permian|Early Permian|Of the Maitland Group.  Underlies the Mulbring Siltstone.  Max. thickness: .83m.  Type Section in text.  Geological Province: Sydney Basin.||||||
13509|Muree Sandstone|48971|6|Mentioned|p9|||See also P17 and P21.||||||
13509|Muree Sandstone|50268|5|Briefly described|Map Legend|Kazanian|Ufimian|Geological Province: Sydney Basin.  Of the Maitland Group.  Overlies: Branxton Formation.  Underlies: Mulbring Siltstone.||||||
13509|Muree Sandstone|60281|5|Briefly described|p9,14, 59|Late Permian|Late Permian|Of the Maitland Group. Sandstone and minor conglomerate and siltstone. Overlies the Branxston Formation. Age: 267-265 Ma. Max. thickness: 180m; 82m at type section. Geological Province: Sydney Basin. Underlies the Mulbring Siltstone.||||||
13509|Muree Sandstone|61201|6|Mentioned|p7|||||||||
13509|Muree Sandstone|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Maitland Group. Marine deposits of reworked clean quartzose sandstones with excellent reservoir potential. Geological Province: Sydney Basin.||||||17-MAR-09
13509|Muree Sandstone|61529|5|Briefly described|p853, p854 Fig. 1b|Late Permian|Late Permian|Of the Maitland Group. Geological Province: Sydney Basin.||||||
13509|Muree Sandstone|61609|6|Mentioned|p239|Permian|Permian|Geological Province: Sydney Basin. Correlate of Nowra Sandstone.||||||07-FEB-11
13509|Muree Sandstone|61612|6|Mentioned|p272, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. NSW.||||||17-MAR-09
13509|Muree Sandstone|61770|6|Mentioned|p110|||||||||
13509|Muree Sandstone|61772|6|Mentioned|p131, p133|||||||||
13509|Muree Sandstone|67786|5|Briefly described|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||Maitland Group.||Overlies Branxton Formation. Is overlain by Mulbring Siltstone.||
13509|Muree Sandstone|68003|5|Briefly described|p38 Fig.3-j, p41.|Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion. A near-shore sand-sheet.||Middle unit in Maitland Group.||Overlies Branxton Formation. Is overlain by Mulbring Siltstone.||
13509|Muree Sandstone|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||Unit in Maitland Group.||Overlies Branxton Formation. Is overlain by Mulbring Siltstone.||
13509|Muree Sandstone|68493|4|Described|p3 Fig.1, p5 Fig.2, p6|Guadalupian|Guadalupian|Sydney Basin. Previously a Member of the Branxton Formation until raised to Formation status by McKelvey, McClung and Runnegar (1971). Type section: Bow Wow Gorge near Mulbring (McKellar 1969). 82 m thick. Forms prominent exposures.||Of the Maitland Group.||Overlies the Branxton Formation. Overlain by the Mulbring Siltstone.|Thick conglomerate and sandstone, overlain by interbedded sandstone and siltstone.|
13509|Muree Sandstone|69297|6|Mentioned|p501, p502 fig 5.43|Capitanian|Capitanian|Sydney Basin.||Maitland Group||Overlies the Branxton Formation. Overlain by the Mulbring Siltstone.||
13509|Muree Sandstone|69683|6|Mentioned|p411 Fig.2|Middle Permian|Middle Permian|||Unit in Maitland Group.||||
13509|Muree Sandstone|70791|5|Briefly described|p277|Guadalupian|Guadalupian|Hunter Coalfield.||Maitland Group.||||
13509|Muree Sandstone|73304|6|Mentioned|p75|||||Maitland Group||||
13509|Muree Sandstone|73625|6|Mentioned|p2|Permian|Permian|Hunter and Newcastle coalfields, Sydney Basin.||||Is overlain by Mulbring Siltstone.||
13516|Muriarra Formation|33328|6|Mentioned|p9|||Refs Phillips 1956.||||||
13516|Muriarra Formation|34404|4|Described|p90|||||||||
13516|Muriarra Formation|40136|6|Mentioned|p37|||||||||
13516|Muriarra Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
13516|Muriarra Formation|43385|14|Not recorded|p169,170||Llandeilian|||||||
13532|Murrabah Shale|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
13532|Murrabah Shale|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
13532|Murrabah Shale|40328|6|Mentioned|p102|||||||||
13532|Murrabah Shale|43476|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
13544|Murray Group|2967|5|Briefly described|p15 Fig.2.2, p24|Miocene|Oligocene|Ludbrook (1957). His Ettrick Formation was added to the Group as Ettrick Marl by Lawrence (1966). Western Murray Basin. Late Oligocene to middle Miocene.|||Geera Clay, Ettrick Marl, Duddo Limestone, Winnambool Formation, Bookpurnong beds, Parilla Sand.|Overlies Renmark Group. Is interbedded with Wunghnu Group.|Marine sequence.|
13544|Murray Group|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Early Oligocene|Includes Ettrick Formation, Mannum, Duddo and Gambier Limestones, and Winnabool Formation. Geological Province: Murray Basin.||||||13-AUG-07
13544|Murray Group|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|22773|5|Briefly described|p351|Middle Miocene|Early Oligocene|||||||
13544|Murray Group|22799|3|Fully described|p29|||||||||
13544|Murray Group|22857|5|Briefly described|p351, p352 Fig.24.8|Middle Miocene|Early Oligocene|Marine to marginal marine deposits. Geological Province: Murray Basin.||||||
13544|Murray Group|22887|5|Briefly described|Fig.6 p13, p33|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|23226|5|Briefly described|p890|||Originally included Mannum Formation, Finniss Clay, Morgan Limestone (including Caddell Marl lens) and Pata Limestone (Ludbrook 1961). Superseded by Murray Supergroup.||||||10-SEP-19
13544|Murray Group|23230|4|Described|Table4-1p40, 42, 44|Miocene|Oligocene|||||||
13544|Murray Group|23768|5|Briefly described|p33-34|||Raised to supergroup status by Lukasik and James (1998). Geological Province: Murray Basin.||||||
13544|Murray Group|23884|5|Briefly described|p153, p155 Gif. 13.2|Middle Miocene|Late Oligocene|Geological Province: Murray Basin.||||||
13544|Murray Group|24096|6|Mentioned|p4|||Geological Province: Murray Basin.||||||
13544|Murray Group|24106|5|Briefly described|p184|Miocene|Miocene|Geological Province: Murray Basin.||||||
13544|Murray Group|24361|6|Mentioned|p50, Fig.1b|||||||||
13544|Murray Group|24551|6|Mentioned|p322 Fig. 10.29, 543|||||||||
13544|Murray Group|24563|5|Briefly described|p485|Middle Miocene|Late Oligocene|Proposed by Lukasik and James(1998) to be raised to supergroup status.  Now reinstated as Murray Group.  Geological Province: Murray Basin.||||||
13544|Murray Group|29355|6|Mentioned|p179|||||||||
13544|Murray Group|31170|6|Mentioned|p295|||Aquifer systems||||||
13544|Murray Group|31625|6|Mentioned|Fig. 5.2|||Oligocene-Miocene||||||
13544|Murray Group|31746|3|Fully described|p194|||||||||
13544|Murray Group|31848|6|Mentioned|p12|||Refers Ludbrook (1961)||||||
13544|Murray Group|31849|6|Mentioned|p7|||||||||
13544|Murray Group|34308|6|Mentioned|p182|||||||||
13544|Murray Group|34418|6|Mentioned|p506|||See also P507||||||
13544|Murray Group|34735|5|Briefly described|p32|||||||||
13544|Murray Group|35187|6|Mentioned|Table1|||||||||
13544|Murray Group|36305|6|Mentioned|p358|||||||||
13544|Murray Group|37873|6|Mentioned|p1|||||||||
13544|Murray Group|38601|6|Mentioned|p5|||||||||
13544|Murray Group|40003|6|Mentioned|p38|||||||||
13544|Murray Group|41511|5|Briefly described|p18|||||||||
13544|Murray Group|41868|6|Mentioned|p551|||||||||
13544|Murray Group|42125|5|Briefly described|p135|||See also Fig.5||||||
13544|Murray Group|42126|6|Mentioned|p159|||||||||
13544|Murray Group|42127|5|Briefly described|p218|||See also Fig.1||||||
13544|Murray Group|42128|5|Briefly described|p227|||See also Fig.2||||||
13544|Murray Group|42129|6|Mentioned|p254|||See also Fig.6||||||
13544|Murray Group|42130|6|Mentioned|p264|||See also Fig.2||||||
13544|Murray Group|42133|6|Mentioned|p307|||||||||
13544|Murray Group|42134|6|Mentioned|Fig.3 P335|||||||||
13544|Murray Group|42137|5|Briefly described|p367|||See also Fig.2||||||
13544|Murray Group|42138|6|Mentioned|p388|||||||||
13544|Murray Group|42184|6|Mentioned|Fig.2 P348|||||||||
13544|Murray Group|42623|5|Briefly described|p2|||limestone, aquifer||||||
13544|Murray Group|42720|5|Briefly described|map legend|Miocene|Oligocene|||||||
13544|Murray Group|42813|6|Mentioned|p24|||||||||
13544|Murray Group|42827|4|Described|p268|||||||||
13544|Murray Group|42881|4|Described|Fig.3, P84|||||||||
13544|Murray Group|42966|3|Fully described|p113, 124|||||||||
13544|Murray Group|43195|5|Briefly described|Map Legend|Miocene|Oligocene|See also commentary on back of map.||||||
13544|Murray Group|43218|4|Described|Fig.3,p22||Middle Miocene|||||||
13544|Murray Group|43780|6|Mentioned|p5|||||||||
13544|Murray Group|43791|6|Mentioned|p372, Fig1|||||||||
13544|Murray Group|43801|6|Mentioned|p114|||||||||
13544|Murray Group|43804|6|Mentioned|p47|||||||||
13544|Murray Group|44133|5|Briefly described|p158|Middle Miocene|Late Oligocene|||||||
13544|Murray Group|44191|5|Briefly described|Map Legend|Middle Miocene|Early Oligocene|||||||
13544|Murray Group|45168|6|Mentioned|Table 1|||||||||
13544|Murray Group|49038|5|Briefly described|p26|||||||||
13544|Murray Group|49040|6|Mentioned|p11|||||||||
13544|Murray Group|50154|2|Defined|p26, p133, p135|Miocene|Oligocene|Geological Province: Murray Basin. Overlies the Renmark Group.||||||15-SEP-04
13544|Murray Group|50155|5|Briefly described|Map Legend|Miocene|Oligocene|Includes Ettrick Marl and Duddo Limestone||||||
13544|Murray Group|50156|5|Briefly described|Map Legend|Miocene|Oligocene|Includes the Ettrick Marl and Duddo Limestone.||||||
13544|Murray Group|50157|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50158|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50159|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50160|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|50161|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||22-JUN-04
13544|Murray Group|50162|5|Briefly described|Map Legend|Miocene|Oligocene|Includes the Ettrick Marl and Duddo Limestone.||||||22-JUN-04
13544|Murray Group|50163|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||24-JUN-04
13544|Murray Group|50164|5|Briefly described|Map Legend|Miocene|Oligocene|Includes: Ettrick Marl, Duddo Limestone||||||
13544|Murray Group|60421|5|Briefly described|p409|Miocene|Oligocene|Includes: Duddo Limestone||||||
13544|Murray Group|60451|5|Briefly described|p95 Fig. 61|||||||||
13544|Murray Group|60452|5|Briefly described|p15|Tertiary|Tertiary|Geogical Province: Murray Basin.||||||
13544|Murray Group|60461|5|Briefly described|Map legend|Pliocene|Oligocene|Includes the Shepparton and Calivil Formations.||||||
13544|Murray Group|60491|5|Briefly described|p16|Pliocene|Late Oligocene|||||||
13544|Murray Group|60538|6|Mentioned|p473 Fig.12|||||||||
13544|Murray Group|60540|5|Briefly described|p1000 Fig.2|Miocene|Miocene|Of Firman (1972), Rogers et al. (1995). Replaced by Murray Supergroup in this paper.||||||06-FEB-18
13544|Murray Group|60599|6|Mentioned|p15|Middle Miocene||Geological Province: Murray Basin.||||||
13544|Murray Group|61155|5|Briefly described|p4, p18|Middle Miocene|Late Oligocene|Shallow-marine calcarenites consisting of skeletal debris and quartz sand. Geological Province: Murray Basin.||||||
13544|Murray Group|61185|5|Briefly described|p58, p15|||Marine sediments. Geological Province: Murray Basin.||||||07-FEB-11
13544|Murray Group|61314|5|Briefly described|p129|Miocene|Oligocene|Geological Province: Murray Basin.||||||
13544|Murray Group|61837|5|Briefly described|p217|||Includes the Compton Conglomerate. Geological Province: Murray Basin.||||||
13544|Murray Group|61841|5|Briefly described|p242, p244|Miocene|Oligocene|Carbonate-dominated sediments. Geological Province: Murray Basin.||||||
13544|Murray Group|62370|6|Mentioned|p453|||Geological Province: Murray Basin.||||||
13544|Murray Group|63066|5|Briefly described|p485-486|||Nomenclature (preferred by P.A. Rogers over Murray Supergroup) consistent with that used for sediment packages of similar magnitude in the Murray Basin: Renmark Group, Heytesbury Group and Eucla Group.||||||22-MAY-13
13544|Murray Group|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Early Oligocene|Includes; Geera Clay, Ettrick and Winnambool Formations and Mannum Limestone. Lagoonal and marginal marine muddy facies and in deeper waters, marl and limestone.||||||
13544|Murray Group|64237|4|Described|p17-20|Middle Miocene|Late Oligocene|Detailed nomenclatural history is presented in this paper, commencing with the Ludbrook stratigraphic scheme through to the controversial upgrade of the Murray Group to Murray Supergroup followed by the reinstatement of the Murray Group.||||||18-SEP-09
13544|Murray Group|64569|6|Mentioned|p893|||||||||
13544|Murray Group|64961|5|Briefly described|p259|Miocene|Miocene|Geological province: Murray Basin.||||||21-APR-09
13544|Murray Group|65552|4|Described|p5 Fig. 3, p6, p26 App.5|Middle Miocene|Late Oligocene|Western Murray Basin. Deposited during a marine incursion. Contemporaneous with Geera Clay and Winnambool, Ettrick and Olney Formations to the east. Contains Mannum Formation and Pata, Morgan, Duddo, and Gambier Limestones.||||||
13544|Murray Group|65687|6|Mentioned|p189|Late Miocene|Oligocene|Parent of Morgan Limestone.||||||
13544|Murray Group|65715|6|Mentioned|p11 Tb.7|||Paleogene? Miocene?||||||
13544|Murray Group|65969|5|Briefly described|p27 Tb.3.3|Miocene|Oligocene|Includes Calivil Formation.||||||
13544|Murray Group|66002|5|Briefly described|p10 Tb.7|Paleogene|Paleogene|Includes Duddo Limestone. Defined by Ludbrook 1957.||||||
13544|Murray Group|66286|5|Briefly described|p179.|Miocene|Oligocene|Southern Murray Basin.|||Includes Duddo Limestone.||Dominated by shallow-marine platform limestones deposited during a marine transgression-regression into the Basin.|
13544|Murray Group|66287|6|Mentioned|p33|Miocene|Miocene||||||Limestones.|20-APR-12
13544|Murray Group|67061|6|Mentioned|p554 Fig.10.|Miocene||Murray Basin.||||||
13544|Murray Group|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.|||Includes Mannum Limestone, Winnambool Formation and Geera Clay.|||
13544|Murray Group|68140|5|Briefly described|p1701-1704, p1707|||See also Murray Group Limestone. Up to 130m thick. Enveloped by the Ettrick Formation, Geera Clay, Bookpurnong Beds, and Winnambool Formation.||||Underlain by the Renmark Formation. Overlain by the Loxton-Parilla Sands.|Comprises marine and marginal marine limestone with calcareous sands, marls, and silts.|09-FEB-18
13544|Murray Group|68189|6|Mentioned|p27 Tb.3.2, p29||||||Includes the Winnambool Formation, Geera Clay, and Duddo Limestone.|||
13544|Murray Group|68194|5|Briefly described|p22|||Murray Basin.|||Includes Geera Clay and Calivil Formation.|Overlies Renmark Group.||
13544|Murray Group|68715|5|Briefly described|p31 Fig.5|Miocene|Miocene|Murray Basin. Early to Middle Miocene age.|||Includes Cadell, Finniss, Mannum, Ettrick and Winnambool Formations; Geera Clay.|||07-APR-17
13544|Murray Group|69562|6|Mentioned|p674|||||||||
13544|Murray Group|70718|6|Mentioned|p25, p103||||||Includes the Geera Clay, Winnambool Formation. .||Limestones.|30-MAY-19
13544|Murray Group|71593|5|Briefly described|p51, p54|||Murray Basin.|||Includes the Duddo Limestone, Winnambool Formation, Ettrick Formation and the Geera Clay.|Overlies the Renmark Group. Overlain by the Wunghu Group.||
13544|Murray Group|72445|5|Briefly described|App.1, App2; App.5; App.7 p4-5, p7, p20.|Miocene|Oligiocene|App.2 is a .csv format file. Identified in Stavely 05,07,08,11,12, 14,16. Said (App.7 p7) to include Gambier, Duddo, Morgan and Patta Limestone Members in the far west of the basin; Geera Clay in the centre of the basin.|||Includes Calivil Formation, Geera Clay, Bookpurnong Formation, Ettrick Formation, Gambier Limestone, Duddo Limestone, Morgan Limestone, Winnambool Formation and Pata Limestone|Overlies Renmark Group (sharp  or gradational contact) and underlies Wunghnu Group (sharp or gradational contact), Bookpurnong Formation (sharp contact).|Glauconitic marl and limestone and light to dark grey micaceous and pyritic muddy sand and sand. Muddy sand and lesser carbonate and marl at base.|
13544|Murray Group|73118|5|Briefly described|p12, 82-83|Miocene|Oligocene|Murray Basin. Has large reserves of groundwater. Mainly concealed, but forms cliffs of River Murray gorge. Shallow-marine platform deposits.|||Winnambool, Ettrick, Mannum Formations; Geera, Finniss Clays; Gambier, Morgan, Pata, Duddo Limestones; Cadell Marl; Compton Conglomerate.||Includes skeletal calcarenite, calcareous-cemented quartz sandstone, marl, and bioclastic and micritic limestones. Characterised by abundant fragmental skeletal debris of diverse fossil assemblages.|
13544|Murray Group|73228|4|Described|p50, p52-57, p59-60|Early Oligocene|Late Early Oligocene|Murray Basin. [An informal lower subdivision is mentioned but not explicitly as a distinct unit]. Deposited on a shallow marine platform and includes lagoonal, marginal marine to estuarine, and shallow marine carbonate platform depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes.|||Cadell Formation, Finniss Formation, Geera Clay, Ettrick Formation, Winnambool Formation, Mannum Formation.|Underlain by Gambier Limestone, Ettrick Formation, and Renmark Group. Overlain by Bookpurnong Formation.|Shallow marine fossiliferous limestone and sandstone with minor clay and silt.|02-NOV-22
13544|Murray Group|73229|5|Briefly described|p66-67, p70-72, p74-75|Middle Miocene|Mid Oligocene|Murray Basin. [Analysed using pXRF; see article]. [An informal lower subdivision is frequently mentioned but not explicetly as a distinct unit].|||Cadell Formation, Finniss Formation, Geera Clay, Winnambool Formation, Mannum Formation, Ettrick Formation||Includes limestone, echinoidal, bryzoal, crinoidal; sandstone, calcareous; minor carbonaceous clay and silt.|
13544|Murray Group|73505|5|Briefly described|p2, p11, p13, p36|Miocene|Oligocene|Murray Basin. Generally thickens to the west.|||Geera Clay, Calivil Group|Overlies Olney Formation, Mologa Surface|Varies from 40-160 m thick.|
13549|Murrays Flats beds|22857|4|Described|p482 App.1 Tb.A1.6|Early Devonian|Early Devonian|Andesitic to felsic volcanics, volcaniclastics and clastics. Max. thickness: ~2km. Geological Province: Bindook Rise.||||||17-FEB-06
13549|Murrays Flats beds|42142|5|Briefly described|p579|||||||||
13549|Murrays Flats beds|44093|5|Briefly described|p219 App. 1|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
13558|Murringo Granite|42726|5|Briefly described|map legend|Silurian||425.||||||
13558|Murringo Granite|68592|6|Mentioned|p1246|||Of Chappell et al. (1991), for a separated area of granitoid E of Murringo; now considered part of the Young Granodiorite. Probably obsolete.||||||
13560|Murrumbateman Creek Formation|12185|5|Briefly described|map legend|Lower Silurian|Lower Silurian|Slate, interbeds of quartz sandstone. BMR map symbol: Slm.||||||
13560|Murrumbateman Creek Formation|22857|5|Briefly described|p138, p424 App.1 Tb.A1.5|Early Silurian|Early Silurian|Max. thickness: 900m. Geological Province: Canberra Block.||||||
13560|Murrumbateman Creek Formation|23245|6|Mentioned|p138|||||||||
13560|Murrumbateman Creek Formation|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
13560|Murrumbateman Creek Formation|29994|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
13560|Murrumbateman Creek Formation|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
13560|Murrumbateman Creek Formation|31111|6|Mentioned|p66|||See also P68, 72, 76||||||
13560|Murrumbateman Creek Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
13560|Murrumbateman Creek Formation|33325|5|Briefly described|Table 2|||||||||
13560|Murrumbateman Creek Formation|37727|4|Described|p76|||||||||
13560|Murrumbateman Creek Formation|40328|3|Fully described|p115|||||||||
13560|Murrumbateman Creek Formation|42727|5|Briefly described|map legend|Wenlock|Llandovery|Interbedded sandstone, siltstone and shale (proximal quartz turbidites). Unconformably underlies Camp Hill Sandstone Member; unconformably overlies Pittman Formation. BMR map symbol: Slm. Geol. Prov: Canberra Block.||||||
13560|Murrumbateman Creek Formation|42820|2|Defined|p13|Early Silurian||||||||
13560|Murrumbateman Creek Formation|44093|5|Briefly described|p198 App. 1|Early Silurian|Ordovician|In the Canberra Block. Geological Province: Lachlan Fold Belt.||||||
13570|Murrumburrah Monchiquite|22638|3|Fully described|p81|Early Jurassic|Early Jurassic|198.5 +/- 3 Ma.||||||
13570|Murrumburrah Monchiquite|29682|4|Described|p16|||||||||
13570|Murrumburrah Monchiquite|35070|2|Defined|p138|Early Jurassic|Early Jurassic|||||||
13570|Murrumburrah Monchiquite|35206|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
13570|Murrumburrah Monchiquite|35608|6|Mentioned|Map legend|Early Cretaceous|Jurassic|Jurassic to Early Cretaceous||||||
13570|Murrumburrah Monchiquite|35609|4|Described|p21|||||||||
13570|Murrumburrah Monchiquite|36411|6|Mentioned|p269|||Refers Basden et al 1978 for definition.||||||
13570|Murrumburrah Monchiquite|42313|5|Briefly described|p166|||||||||
13570|Murrumburrah Monchiquite|43715|6|Mentioned|p28|||||||||
13570|Murrumburrah Monchiquite|44192|5|Briefly described|Map Legend||Jurassic|||||||
13577|Murta Formation|13497|5|Briefly described|p115, p115 fig 6.33, p130, p138|Early Cretaceous|Early Cretaceous|Eromanga Basin, Dullingari Field. Deposited in a high-sinuosity fluvial, overbank, lacustrine or proximal deltal environment. This formation is an oil source rock. Oil and gas reservoir. See also p138 fig 8.17, p141, p142, p146, p151 fig 9.23, p152 fig 9.26, p170, p171, p183, p188, p216.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstones, siltstone, shale and minor coal.|
13577|Murta Formation|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||||||
13577|Murta Formation|22839|6|Mentioned|P33|||||||||
13577|Murta Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlain by Cadna-owie Formation, underlain by Namur Sandstone.||||||17-JAN-08
13577|Murta Formation|22912|5|Briefly described|33|||Geological Province: Eromagna Basin.||||||17-JAN-08
13577|Murta Formation|23054|6|Mentioned|Fig5p22|Valanginian|Berriasian|||||||
13577|Murta Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Includes McKinlay Member.||||||
13577|Murta Formation|23155|3|Fully described|p28 & Fig 15 on p28|Early Cretaceous|Early Cretaceous|The Murta Formation is Early Cretaceous (Neocomian) in age, from spore pollen determination.  See p28 for details of type section etc.||||||
13577|Murta Formation|23356|5|Briefly described|26 Tab.2|Neocomian|Neocomian|||||||
13577|Murta Formation|23375|4|Described|Fig2 p265|Valanginian|Berriasian|Laterally equivalent to upper Hooray Sandstone. In the Eromanga Basin.||||||17-JAN-08
13577|Murta Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Includes the McKinlay Member.  Geological Province: Eromanga Basin.||||||
13577|Murta Formation|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13577|Murta Formation|24482|5|Briefly described|p44|Cretaceous|Jurassic|Contains the McKinlay Member. Geological Province: Eromanga Basin.||||||
13577|Murta Formation|37287|6|Mentioned|p36|||||||||
13577|Murta Formation|41705|6|Mentioned|p128|||||||||
13577|Murta Formation|42071|6|Mentioned|p117|||||||||
13577|Murta Formation|44133|4|Described|p111, 104 Fig. 9.11|Neocomian|Neocomian|Geological Province: Eromanga Basin. Formerly upper part of the Mooga Formation known as the Murta Member. Overlies and intertongues with McKinlay Member and Namur Sandstone. Overlain transitionally by Cadna-owie Formation.||||||08-MAY-13
13577|Murta Formation|60717|5|Briefly described|p40 Fig. 2, p42|Early Cretaceous|Late Jurassic|Contains the McKinlay member. Overlies Westbourne Formation; overlain by Cadna-owie Formation; interfingers partially with Algebuckina Sandstone. Geological Province: Eromanga  Basin.||||||31-JAN-08
13577|Murta Formation|61614|5|Briefly described|p289, p294, p295, p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin. Largely carbonaceous siltstones deposited in lacustrine and paralic environments.||||||17-MAR-09
13577|Murta Formation|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13577|Murta Formation|62028|6|Mentioned|p11|||May provide a regional seal.||||||26-FEB-08
13577|Murta Formation|62029|5|Briefly described|p15 Fig. 4|||See also Murta Member.||||||08-APR-08
13577|Murta Formation|62537|6|Mentioned|p191 Fig.2, p192.|Early Cretaceous|Early Cretaceous|Eromanga Basin. Significant hydrocarbon source potential.||||Overlies Birkhead Formation. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|63979|2|Defined|p44, Fig. 44|Valanginian|Berriasian|Supersedes "Murta Member" in SA; also now extended to Qld. Passes laterally into upper part of Hooray Sst. Prev. referred to as Murta Member of Mooga Formation by petroleum companies.Detailed desc./explans. lithology/nomenclature included||||Laterally equivalent to upper part of Hooray Sandstone.||09-APR-13
13577|Murta Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses relatively low hydrocarbon source potential.||||||07-FEB-11
13577|Murta Formation|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Namur Sandstone. Overlain by Cadna-owie Formation.||||||08-MAR-12
13577|Murta Formation|65489|5|Briefly described|p15, p47, p49, p55, p73, p96, p132, p152|Early Cretaceous|Early Cretaceous|See also p154-158, p160. Eromanga Basin. 60m thick. Hydrocarbon source rock. Oil reservoir accounting for 10% of the Basin's production. Intraformational shale regional seal.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.|Lacustrine turbidite sandstones.|
13577|Murta Formation|65925|5|Briefly described|Appendix 2.||||||||Dark grey, argillaceous and carbonaceous siltstone with interbedded fine- to very fine-grained sandstone.|
13577|Murta Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|66623|5|Briefly described|pp240-242.|||Not identified in outcrop for this study, although recognised in borehole sections. Largely non-marine.|||||Interbedded siltstone, shale, very fine-grained sandstone and minor medium- to coarse-grained sandstone.|
13577|Murta Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|67561|5|Briefly described|p52 Fig.2|Valanginian|Berriasian|Australian Spore-Pollen zonation: australiensis.||||||
13577|Murta Formation|68068|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Eromanga Basin. Subsurface only.|||Includes McKinlay Member at base.|Overlies Namur Sandstone. Is overlain conformably by Parabarana Sandstone and Cadna-owie Formation.|Dark grey laminated carbonaceous siltstone, graded beds, ripple marks with interbeds of fine-grained to locally coarse-grained sandstone, ripple laminated, bioturbated; carbonate cemented layers near top; diagenetic siderite common.|
13577|Murta Formation|68731|6|Mentioned|pp209-211|||||||||
13577|Murta Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
13577|Murta Formation|69019|5|Briefly described|p85 Fig.21.|Valanginian|Berriasian|Southern Eromanga Basin.|||Includes McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|69023|4|Described|p79, p86, p89 Fig.20, p92, p191-192|Valanginian|Berriasian|Defined by Nugent (1969) as Murta Member, part of the Mooga Formation; later elevated to Formation status (Callen et al.,1994; Gravestock et al., 1995) and the Mooga Formation was discarded. The McKinlay Member (Mount, 1982) became a Member of the Murta Formation. Eromanga Basin. Thickness from ~33 to >53m. Stratigraphic wells intersection data.|||Includes McKinlay Member.|Overlies Namur and Algebuckina Sandstones. Passes laterally into Algebuckina Sandstone. Is overlain gradationally by Cadna-owie Formation.|Dark grey argillaceous and carbonaceous siltstone interbedded with fine- to very fine-grained sandstone, diagenetic siderite and calcite nodules and layers; overlain by thinly interbedded siltstone and sandstone; passing up into dark grey siltstone.|
13577|Murta Formation|69454|6|Mentioned|p38:13|||The uppermost shale of previous usage (eg Ambrose and Heugh, 2010) was referred to basal Cadna-owie Formation by Gray et al. (2002). This Formation, with the underlying Namur Sandstone (in the Cooper Basin), are equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13577|Murta Formation|69457|5|Briefly described|p41:3-5, 7|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Namur Sandstone. Is overlain conformably by Cadna-owie Formation.||12-JUL-16
13577|Murta Formation|69594|5|Briefly described|p519, p526-528, p531-532, p573|Hauterivian|Berriasian|Eromanga Basin; mostly in SA. Generally 50-60m thick; possibly >100m locally. Brackish environment. A significant hydrocarbon reservoir; has hydrocarbon source potential.||||Overlies Namur Sandstone; conformably overlies upper Namur Sandstone. Is overlain conformably/transitionally by Cadna-owie Formation. Lateral equivalent of (upper) Hooray Sandstone.|Interbedded and interlaminated sublabile to quartzose sandstone, silty sandstone, siltstone and lesser mudstone, intraformational conglomerate and coal.|
13577|Murta Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Namur Sandstone, overlain by Cadna-owie Formation||
13577|Murta Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Eromanga Basin.||||||
13577|Murta Formation|69797|5|Briefly described|p17 incl Fig.2|Early Cretaceous|Early Cretaceous|The best petroleum source rocks in Jurassic-Cretaceous sequence of Eromanga Basin are organic-rich shales and siltstones of the Murta Formation, the coals and carbonaceous shales of Birkhead Formation, and highly carbonaceous shales of Poolowanna Formation. Geol. Prov: Eromanga Basin.||||||17-JAN-17
13577|Murta Formation|69946|2|Defined|p11, p17-19, p56-58, p86-92|Early Cretaceous|Early Cretaceous|Siltstone and shale in the upper part of the Mooga Formation were defined as Murta Member by Nugent (1969); raised to Formation status by Gravestock et al. (1995). Equivalent to the upper Hooray Sandstone in Qld. Type section is the interval 1469.14 - 1526.13m in Dullingari North 1. Up to >90m thick. Wireline log correlations. Sedimentary facies log.|||Includes McKinlay Member.|Overlies and intertongues with Namur Sandstone. Is overlain gradationally by Cadna-owie Formation. Intertongues with Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey very fine- to fine-grained sandstone; minor medium- and coarse-grained sandstone. Diagenetic siderite nodules and layers.|
13577|Murta Formation|69947|5|Briefly described|p3, p8, p13 Fig.7.2, p29-31 Figs.7.18-20|Early Cretaceous|Early Cretaceous|Eromanga Basin. Widespread meandering fluvial, floodplain and lacustrine facies. Represents two major transgressive-regressive cycles; illustrated by a well log from the Maxwell Field.|||McKinlay Member.|Conformably overlies Namur, Hooray Sandstones. Is overlain conformably by Cadna-owie Formation.|Sandstone, siltstone.|
13577|Murta Formation|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Namur Sandstone. Is overlain by Cadna-owie Formation.||
13577|Murta Formation|70821|5|Briefly described|p31|||Previously part of the [obsolete] "Lower Hooray Sandstone". 44 m thick interval, between 395 and 439 m in Weilmoringle 1 well. See also Murta Member p21||||Overlies Namur Sandstone.||02-DEC-16
13577|Murta Formation|70823|4|Described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a meandering-anastomosing fluvial or lacustrine or overbank environments.|||Includes the McKinlay Member.|Overlies the Namur Sandstone. Overlain by the Cadna-owie Formation.|Sandstone, siltstone, shale and coal.|
13577|Murta Formation|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13577|Murta Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Algebuckina Sandstone, Namur Sandstone and the McKinlay Member.||24-OCT-19
13577|Murta Formation|71342|6|Mentioned|Ch 1 p6, Ch 1 p19, Ch4 p9, Ch5 p12|Cenomanian|Berriasian|Originally defined by Nugent (1969) as siltstone and shale in the upper part of the Mooga Formation. Gravestock et al, (1995) elevated the name to Murta Formation. This unit is equivalent to the upper Hooray Sandstone in Queensland. The type section is in Dullingari North 1 (Mount, 1981). Diagenetic siderite nodules and layers produce distinctive spikes on sonic and density logs. This unit has a maximum thickness >90m in the Nappamerri Trough. Age based partly on palynology. Interpreted to have been deposited in open lacustrine, lacustrine fan delta, distributary channel and lacustrine shoreline environments. A brackish to marine environment is suggested for the upper parts of this formation. Spore-pollen zone is given in Ch5 p57. A complete sedimentary facies log is given in Ch5 p88. Source rock characteristics are described in detail in Ch8 (p6). Forms a seal over the Namur Sandstone. Oil is produced from a very thin by extensive, high-permeability shoreface sand. See also  Ch5 p17-p18, Ch5 p30, Ch5 p32, Ch5 p57-p58, Ch5 p85-p92, Ch6 p5, Ch6 p7, Ch7 p3, Ch7 p8, Ch7 p11, Ch7 p13, Ch7 p29-p31, Ch8 p2, Ch8 p5-p6, Ch8 p8, Ch8 p10, Ch8 p17, Ch8 p22, Ch10 p3, Ch10 tbl 10.1, Ch10 p8, Ch10 p14, Ch10 p17-p20, Ch11 p2-p5, Ch11 p7-p8, Ch11 p17, Ch12 p5, Ch13 p2-p3, Ch13 p7, Ch13 p9-p10, Ch13 p25-p28, Ch13 p31, Ch13 p33, Ch14 p5.|||Includes the McKinlay Member.|Intertongues with and overlies the McKinlay Member and the Namur Sandstone. Conformably overlain by the Cadna-owie Formation. Intertongues with and is equivalent to the Algebuckina Sandstone.|Thinly interbedded dark grey siltstone, shale, pale grey, very fine to fine-grained sandstone and minor medium and coarse-grained sandstone.|
13577|Murta Formation|71863|6|Mentioned|p5|Hauterivian|Berriasian|Eromanga Basin.||||Overlies Namur Sandstone, overlain by Cadna-owie Formation.||
13577|Murta Formation|72297|5|Briefly described|p739, p742-743|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential. Oil flows >2000 bpd in Dullingari North 1 (in SA).||||||
13577|Murta Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.|||McKinlay Member.|Overlies Namur Sandstone. Is overlain by Cadna-owie FZ.||
13577|Murta Formation|73251|6|Mentioned|p55-56, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin. Deposited in freshwater lacustrine conditions. Capable of generating hydrocarbons (marginally mature for liquid hydrocarbon generation); constitutes the most shallow-lying and demonstrably effective petroleum source within the stacked Warburton, Cooper, and Eromanga Basins. Partly self-sourcing and likely to have contributed to hydrocarbon accumulations within the overlying Namur Sandstone and Cadnaowie Formation. Depositional environments included lacustrine turbidites, deltas, and shoreface.||||Underlain by and equivalent to Namur Sandstone. Overlain by [and equivalent to?] Cadna-owie Formation.||
13577|Murta Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
13615|Muswellbrook Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
13615|Muswellbrook Coal Member|40331|6|Mentioned|p13|||||||||
13618|Muttama Creek Siltstone|22638|1|Redefined|p64|Emsian|Lochkovian|Cootamundra Group. 1750 m thick. Conformably overlies Cowcumbala Rhyolite. Unconformably overlain by Bendick Formation.||||||
13618|Muttama Creek Siltstone|22857|5|Briefly described|p450 App.1, Tb.A1.6|Emsian|Emsian|Of the Cootamundra Group. Shale, siltstone, sandstone, minor volcanics. Max. thickness: 1750m. Geological Province: Bogan Gate Terrace.||||||
13618|Muttama Creek Siltstone|35070|2|Defined|p118|Early Devonian|Early Devonian|||||||
13618|Muttama Creek Siltstone|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
13618|Muttama Creek Siltstone|35608|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13618|Muttama Creek Siltstone|35609|6|Mentioned|p11|||||||||
13618|Muttama Creek Siltstone|36411|6|Mentioned|p269|||Refers Basden et al 1978 for definition.||||||
13618|Muttama Creek Siltstone|42313|6|Mentioned|p144|||||||||
13618|Muttama Creek Siltstone|44192|5|Briefly described|Map Legend||Lochkovian|||||||
13623|Myall Mudstone|37083|5|Briefly described|p171|||||||||
13664|Myuna Conglomerate|41463|6|Mentioned|Fig.1|||||||||
13682|Nagha Granite|23309|6|Mentioned|p440, Appendix 1|||G3, A-Type. Supersedes Nagha Adamellite.||||||
13682|Nagha Granite|42726|5|Briefly described|map legend|Middle Devonian||Reserved as Nagha Adamellite.||||||
13682|Nagha Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Gabo Suite.|||Aluminous A-type granite.|
13683|Naghi Granite|42726|5|Briefly described|map legend|Middle Devonian||Reserved as Naghi Adamellite.||||||
13683|Naghi Granite|68115|6|Mentioned|p6.|||Extended into Victoria from NSW. Name has been changed to Naghi Granite to meet GSV standards.||||||
13683|Naghi Granite|68116|5|Briefly described|Appendix.|Late Devonian|Late Devonian||||||Granite: pink to red, medium to fine grained, equigranular; contains biotite and minor hastingsite with rare fluorite; A-type.|
13683|Naghi Granite|71206|6|Mentioned|p373|||Lachlan Fold Belt.||Gabo Suite.|||Aluminous A-type granite.|
13702|Nalleen Tuff Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Dights Creek Coal.  Equivalent to the Awaba Tuff (Newcastle Coal Measures).   Geological Province: Sydney Basin||||||
13702|Nalleen Tuff Member|39666|6|Mentioned|p79|||||||||
13702|Nalleen Tuff Member|73304|6|Mentioned|p67|||Superseded; see Awaba Tuff or Awaba Tuff Member.||||||
13707|Namba Formation|13497|5|Briefly described|p115, p115 fig 6.33, p150-p154, |Miocene|Oligocene|Lake Eyre Basin.||||Unconformably overlies the Eyre Formation. Unconformably overlain by the Yandruwantha Sand.||
13707|Namba Formation|22459|6|Mentioned|p 17|||||||||
13707|Namba Formation|22712|5|Briefly described|p132|Tertiary|Tertiary|||||||
13707|Namba Formation|22773|6|Mentioned|p355|||||||||
13707|Namba Formation|22821|6|Mentioned|P8||Tertiary|||||||
13707|Namba Formation|22857|5|Briefly described|p355|Early Pliocene|Early Miocene|Max. thickness: ~75m. Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|22912|4|Described|32|||Geol province Lake Eyre Basin||||||
13707|Namba Formation|22931|6|Mentioned|10|||||||||
13707|Namba Formation|23154|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province - Lake Eyre Basin - Callabonna Basin.||||||
13707|Namba Formation|23155|4|Described|p34|||Little palaeontological information avaliable hence unit is identified by lithological correlation and continuity with similar sediments to the south. On FROME, ages established from palynofloras - latest Oligocene-?Late Miocene to Pliocene.||||||
13707|Namba Formation|23189|6|Mentioned|Table1p290,290,295||Middle Miocene|||||||
13707|Namba Formation|23339|6|Mentioned|5|||||||||
13707|Namba Formation|23477|5|Briefly described|p49 Fig 3|Tertiary|Tertiary|Geological Province: Curnamona Province.||||||
13707|Namba Formation|23478|5|Briefly described|p28|Pliocene|Oligocene|||||||
13707|Namba Formation|24102|5|Briefly described|p132|Late Miocene|Middle Miocene|||||||
13707|Namba Formation|24252|6|Mentioned|p299|Miocene|Miocene|||||||
13707|Namba Formation|24566|5|Briefly described|p113|Late Miocene|Middle Miocene|Low energy lacustrine facies. Geological Province: Frome Embayment.||||||03-MAY-05
13707|Namba Formation|29660|6|Mentioned|p6|||||||||
13707|Namba Formation|30055|6|Mentioned|p151|||Minerology P159.||||||
13707|Namba Formation|30056|2|Defined|p129|middle Miocene|middle Miocene|||||||
13707|Namba Formation|30920|6|Mentioned|Map legend|Miocene|Miocene|||||||
13707|Namba Formation|32121|6|Mentioned|p422|||||||||
13707|Namba Formation|32816|6|Mentioned|p85|||||||||
13707|Namba Formation|34882|6|Mentioned|p81|||||||||
13707|Namba Formation|35080|6|Mentioned|p14|||||||||
13707|Namba Formation|35619|6|Mentioned|p309|||||||||
13707|Namba Formation|35857|6|Mentioned|p197|||||||||
13707|Namba Formation|36213|6|Mentioned|p85|||||||||
13707|Namba Formation|36618|6|Mentioned|p9|||||||||
13707|Namba Formation|36620|5|Briefly described|Fig.1|||See also P24.||||||
13707|Namba Formation|36966|6|Mentioned|p86|||||||||
13707|Namba Formation|37062|6|Mentioned|p199|||||||||
13707|Namba Formation|37678|6|Mentioned|p243|||||||||
13707|Namba Formation|38682|6|Mentioned|Fig.3|||||||||
13707|Namba Formation|38982|5|Briefly described|p64|||||||||
13707|Namba Formation|39085|6|Mentioned|p13|||||||||
13707|Namba Formation|39322|6|Mentioned|Fig.2|||||||||
13707|Namba Formation|39666|6|Mentioned|p114|||||||||
13707|Namba Formation|39804|5|Briefly described|p163|||||||||
13707|Namba Formation|40664|6|Mentioned|p246|||||||||
13707|Namba Formation|40754|6|Mentioned|p10|||||||||
13707|Namba Formation|40755|5|Briefly described|p43|||||||||
13707|Namba Formation|40756|5|Briefly described|p3|||||||||
13707|Namba Formation|40757|3|Fully described|p75|||||||||
13707|Namba Formation|40758|6|Mentioned|p88|||||||||
13707|Namba Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
13707|Namba Formation|40926|6|Mentioned|Table 3|||||||||
13707|Namba Formation|41125|6|Mentioned|p34|||||||||
13707|Namba Formation|41537|6|Mentioned|p348|||See also Fig.2||||||
13707|Namba Formation|42090|5|Briefly described|p25|||||||||
13707|Namba Formation|42205|5|Briefly described|p246|||See also Fig.1||||||
13707|Namba Formation|42375|5|Briefly described|p26|Neogene||Callabonna Basin, Oligocene?||||||
13707|Namba Formation|42469|5|Briefly described|p39, p43|||||||||
13707|Namba Formation|42543|5|Briefly described|p4|||||||||
13707|Namba Formation|42746|5|Briefly described|p17|||Callabonna Basin||||||
13707|Namba Formation|42784|6|Mentioned|p494|||||||||
13707|Namba Formation|42813|6|Mentioned|p24|||||||||
13707|Namba Formation|42883|6|Mentioned|p8|||||||||
13707|Namba Formation|42957|6|Mentioned|p40|||||||||
13707|Namba Formation|43053|5|Briefly described|Map Legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||25-MAY-05
13707|Namba Formation|43258|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
13707|Namba Formation|43298|6|Mentioned|Map Legend|Pliocene|Miocene|||||||
13707|Namba Formation|44133|5|Briefly described|p193, 190 Fig. 10.30|Miocene|Miocene|Geoloigcal Province: Lake Eyre Basin. Disconformably overlies: Eyre Formation. Average Thickness: 90m.||||||
13707|Namba Formation|45128|6|Mentioned|Fig.42|||Correlation table of sediments containing Dromornithidae in Australia.||||||
13707|Namba Formation|45155|6|Mentioned|p46|||||||||
13707|Namba Formation|46815|6|Mentioned|p249|||||||||
13707|Namba Formation|46833|5|Briefly described|p53|||||||||
13707|Namba Formation|60564|4|Described|p4|Tertiary|Tertiary|Overlain by Willawortina Formation.||||||
13707|Namba Formation|60703|5|Briefly described|p704, p725 Fig.18|Early Miocene|Late Oligocene|Contains abundant gastrapod fossils. Geological Province: Lake Eyre Basin (Callabonna Sub-basin).||||||12-APR-05
13707|Namba Formation|60785|5|Briefly described|p184 Fig.1, pp197-198.   |?Serravallian|?Chattian|South Australia. Palynofloras suggest Miocene-Pliocene age (Alley et al., 1995). Woodburne et al. (1993) have suggested an age of 24-28 Ma for the Etadunna Formation (a correlate of the Namba Formation), implying a Late-Oligocene age. Has yielded fossil cetacean elements.||||Correlated with the Etadunna Formation.|Illite and kaolinite clays.|
13707|Namba Formation|60953|5|Briefly described|Map Legend|Pliocene|Miocene|Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|61108|5|Briefly described|map legend|Pliocene|Miocene|Lacustrine dolomite, clay, sand and silt. Geological Province: Lake Eyre Basin.||||||
13707|Namba Formation|61119|6|Mentioned|p124, pp128-9, p134, p137, p144, p147||Cenozoic|River, lake and estuarine sediments. Detailed descriptions of Lungfish fossil assemblages included.||||||28-MAR-12
13707|Namba Formation|61155|5|Briefly described|p4, p17|Middle Miocene|Early Miocene|Age: 23.5-12.5Ma. Max. thickness:250m. Geological Province: Tarkarooloo Basin.||||||
13707|Namba Formation|61823|5|Briefly described|p118|Pliocene|Oligocene|Lacustrine and alluvial deposits. Overlies Eyre Formation.  Geological Province: Lake Eyre Basin.||||||05-JUN-06
13707|Namba Formation|62592|5|Briefly described|p18.|Tertiary|Tertiary|Thin sedimentary cover, hosting roll-front uranium deposits including Honeymoon, Goulds Dam and Beverley.||||||
13707|Namba Formation|62724|5|Briefly described|p16 Fig. 2|Tertiary|Tertiary|Clay, sand, dolomite. Geological Province: Curnamona Province.||||||07-FEB-11
13707|Namba Formation|63102|4|Described|p8,62,71,74|Miocene|Miocene|Geological province: Curnamona Province. Of Callabonna Sub-basin. Widespread and directly overlies highly weathered basement in the southern Benagerie Ridge. Deposited in a low energy environment over the Eyre Formation.||||Underlain by Eyre Formation.|Fine clastics, olive to grey coloured clay, sandy clay and silts.|
13707|Namba Formation|65194|5|Briefly described|p36-37, p44-45, p47, p171|Miocene|Miocene|Lake Eyre Basin. Overlies Eyre Formation; is overlain by Willawortina Formation. Shown as including Alpha Mudstone, Beverley sands and Beverley clay. Thick clays act as an aquaclude, sealing the underlying Eyre Formation sands. Fills palaeovalleys which host uranium orebodies.||||||
13707|Namba Formation|65484|6|Mentioned|p 28,30, p29 Fig 2|Tertiary|Tertiary|Coarse sandy and gravel facies, fluvial and lacustrine.||||||
13707|Namba Formation|65925|4|Described|p44, pp49-65, p79, Appendix 2.|Miocene|Oligocene|Callabonna Sub-basin. Hosts the Beverley uranium deposit. Average thickness 90m. Equivalent to Etadunna Formation. Deposited in a fluvial lacustrine environment with meandering streams and billabongs.|c.24 Ma to 4-6 Ma.||Comprises Alpha Mudstone, Beverley Sands, Beverley Clay.|Disconformably overlies Eyre Formation and unconformably overlies Bulldog Shale. Is overlain by Willawortina Formation.|Sand, fine to medium-grained, poorly sorted, angular; silt, thin dolomite, oolitic dolomite interbeds. Shallow, brackish to fresh water lakes.|
13707|Namba Formation|66131|4|Described|p240, p242 Fig.2, p244 Fig.4, p245|Miocene|Oligocene|See also p255, p259. Callabonna Sub-basin. Defined by Callen and Tedford (1976). ~90-170 m thick. Contains abundant fossils: invertebrates in carbonate, vertebrates in upper clayey parts. Latest Oligocene to Miocene in age.||||Disconformably overlies Eyre Formation.|Comprises alternating fine to medium, poorly sorted sand, silt and clay, thin dolomite and limy, often oolitic dolomite. Silcrete capping.|
13707|Namba Formation|66303|5|Briefly described|pp27-28, p31 Fig.5, p33.|Paleogene|Paleogene|Lake Eyre Basin. Middle to Late Miocene. Palynological samples were few due to poor preservation and/or absence.||||Disconformably overlies Eyre Formation. Is overlain by Willawortina Formation.|Dominantly olive-grey clay, silt and mudstone.|
13707|Namba Formation|66518|5|Briefly described|p19 Fig.4, p20.|Miocene|Miocene|Lake Eyre Basin. Movement along faults (including the Poontana Fault) allowed thickening of these widespread fluviolacustrine deposits. The Beverley uranium deposit developed in a meandering channel within this Formation.||||Unconformably overlies Eyre Formation. Is overlain by Millyera Formation and possibly unconformably by the Willawortina Formation.|Clay, silt, sand and carbonate units.|
13707|Namba Formation|66573|6|Mentioned|p873|||Correlative of the Etadunna Formation.||||||
13707|Namba Formation|66623|6|Mentioned|p282.|||Lateral equivalent of Etadunna Formation; tentatively correlated with Doonbara Formation in NSW (Wopfner, 1974).||||||21-MAY-13
13707|Namba Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
13707|Namba Formation|68068|5|Briefly described|Map legend|Pliocene|Late Oligocene|Callabonna Sub-basin, Lake Eyre Basin. Equivalent to Etadunna Formation to the west and northwest. Commonly silcreted.|||||White, very fine-grained dolomite interbedded with olive-grey clay (palygorskite) near base; swelling clay with gypsum nodules; interbedded indurated dark sandy claystone; greenish laminated silt and fine sand; bioturbated.|
13707|Namba Formation|68157|6|Mentioned|p1, p17-25|Miocene|Miocene|Hosts the Beverley sandstone-hosted uranium deposit. Includes detrital zircons aged 1576 +/- 5 Ma, ~425 Ma and ~285 Ma, as well as other smaller groupings. Also includes informal Beverley sands and Alpha mudstone.|||Includes Beverley Clay.||Includes coarse-grained sandstone, clay and mudstone.|
13707|Namba Formation|68715|6|Mentioned|p29, p29 Fig.6, p32 Fig.6|Neogene|Neogene|||||Unconformably overlies Eyre Formation.|Includes fluvial gravels.|07-APR-17
13707|Namba Formation|68821|4|Described|p296, p307|Serravallian|Chattian|Consists largely of immature fluvio-lacustrine sand, silt, and clay deposited in an alkaline and anoxic environment. Includes levels of pyritic laminated carbonaceous mud and fossils - gastropods, ostracods, algae, fish, reptiles, birds and mammals.|26 - 12 Ma|||Locally underlain by the Eyre Formation.|Consists of quartz (< 50%), kaolinte (< 40%), feldspar (< 15%), mica (< 15%), smectite(< 5%), illite (a few %), palygorskite and dolomite, gypsum and alunite.|
13707|Namba Formation|69001|5|Briefly described|p22, p23, p45, p66, p70|Pliocene|Oligocene|Late Oligocene to Early Pliocene.|||||Comprises lacustrine and fluvial sand, silt and clay.|
13707|Namba Formation|69019|5|Briefly described|p83 Fig.20, p94 Fig.24, p110-113.|Pliocene|Oligocene|Of Callen and Tedford (1976). Type section is in Yalkalpo 1 drillhole. Callabonna Sub-basin. Thickness to 109.5 m. Extensive fossil fauna listed.||||Unconformably overlies Eyre Formation. Contemporaneous with Etadunna Formation.|Interbedded indurated dark sandy claystone with sand, with thin interbeds of dolomite and palygorskite clay; overlain by swelling clay with ochre mottling and interbedded laminated silt with fine angular sand; silcrete-porcellanite upper surface.|
13707|Namba Formation|69023|4|Described|p79, p87, p101, p109, p112, p117-120|Miocene|Oligocene|See also p125-126, p133, p136, p140, p142, p153, p161, p193. Of Callen and Tedford (1976). Lake Eyre Basin. Average thickness c.90m; maximum >158m. Surface commonly silicified. Diverse and diagnostic vertebrate fossils listed. Similar vertebrate and pollen fossils to Etadunna Formation. Weathering has formed porcellanite. Local Holocene gypcrete and gypsum caps. Contains beds of palygorskite clay, usually associated with basal dolomite. Probable source (with Eyre Formation) of Yandruwantha Sand. Stratigraphic wells intersection data.||||Unconformably overlies Eyre Formation. Is overlain by Willawortina Formation, by Millyera Formation disconformably and by Yandruwantha Sand unconformably. Time-equivalent of Etadunna Formation.|Dark grey to olive clay, with ochre mottling and interbedded white to yellow silt to coarse sand; fine clayey and arenaceous clastics dominate; local white very fine-grained dolomite; local green-grey to black carboniferous to manganiferous clays.|
13707|Namba Formation|69458|5|Briefly described|p42:16, 22|Miocene|Oligocene|Lake Eyre Basin. Extensive shallow, alkaline lacustrine to fluvial deposits. Lower parts contain a vertebrate assemblage with affinities with the Pwerte Marnte Marnte fauna.||||Correlated with Ulta Limestone.|Interbedded sandstone, siltstone, shale and locally developed dolostone.|12-JUL-16
13707|Namba Formation|69562|5|Briefly described|p662 Tb.2, p663 Fig.2, p664 Tb.4|Miocene|Oligocene|See also p666 Fig.3, p667 Fig.4, p668-669, p674-676, p679-684. Lake Eyre Basin. Deposition in paleovalleys. Hosts the Beverley uranium deposit. Overall low permeability. Electrical conductivity value used in forward modelling: 300 mS/m.|c.28 Ma.||Includes Alpha Mudstone, Beverley Sands and Beverley Clay.|Overlies Eyre Formation. Is overlain unconformably by Willawortina Formation.|Clayey overbank sediments; also contains alkaline clays and sandy lenses.|06-APR-22
13707|Namba Formation|69568|5|Briefly described|p443-444|Miocene|Miocene|Lake Frome region, Lake Eyre Basin. Lacustrine, alluvial and other low-relief environments.||||Disconformably overlies Eyre Formation. Is overlain by Willawortina Formation.|Angular immature sands and silts with minor conglomerates, black carbonaceous clays and green-grey clays with some dolomites and lignite. Capped by silcrete in Lake Frome area.|
13707|Namba Formation|69572|6|Mentioned|p1190|Oligocene|Oligocene|Contains fossil koalas of the Madakoala Genus.||||||
13707|Namba Formation|69654|6|Mentioned|p4|||Curnamona Province.||||||
13707|Namba Formation|69946|5|Briefly described|p29, p129|Miocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin. Krieg et al. (1990). Up to 210m thick.|||||Carbonate and clastics from evaporation of magnesian lakes.|
13707|Namba Formation|69947|5|Briefly described|p13 Fig.7.2|Miocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin.||||||
13707|Namba Formation|70340|5|Briefly described|map legend|Pliocene|Oligocene||||||Sand, fine to medium-grained, poorly sorted, angular, silt, thin dolomite, oolitic dolomite interbeds. Shallow, brackish to fresh water lakes.|
13707|Namba Formation|70383|5|Briefly described|p45, p52|Miocene|Oligocene|Lake Eyre Basin. Mixed lacustrine, fluvial and basin margin colluvium. Detrital zircon maximum depositional age. A similar determination is an ICPMS age of c.256 +/- 10 Ma by Wulser (2009).|<256 +/- 3 Ma (SHRIMP; Cross et al., 2010).|||Overlies Eyre Formation.||
13707|Namba Formation|70384|5|Briefly described|Map legend.|Pliocene|Oligocene|Callabonna Sub-basin, Lake Eyre Basin. The lower unit only occurs subsurface: interbedded indurated dark sandy claystone with skew planes, and sand (fine to coarse, low sphericity, subrounded, polished); structures like upper unit, burrows less evident; rare vertebrate, invertebrate and plant fossils; white very fine-grained dolomite interbedded with olive-grey clay (palygorskite) near base.|||||Upper unit: olive-grey (weathers black) swelling clay, gypsum nodules near top; greenish laminated silt and fine angular well-sorted sand; white lacustrine oolitic and conglomeratic dolomite nodules and beds; bioturbated; rare invertebrate fossils.|
13707|Namba Formation|70657|5|Briefly described|p9 Fig.3, p68, p77-78, p80|Miocene|Miocene|Widespread unit. Directly overlies highly weathered basement. Relatively high Zn content makes surface geochemical prospecting difficult.||||Overlies Eyre Formation.|Olive to grey clay (mainly smectites), sandy clay, silt, dolomite.|
13707|Namba Formation|70658|6|Mentioned|p14|Tertiary|Tertiary||||||Clay, sand, dolomite.|
13707|Namba Formation|70821|5|Briefly described|p25, p82|Miocene|Oligocene|Callen et al. (1975). Lake Eyre Basin (NSW, QLD).||||Equivalent to Whitula Formation.||
13707|Namba Formation|70823|5|Briefly described|p47|Late Oligocene|Late Oligocene|Callabonna Sub-basin. Maximum thickness of 210m.|ca 28 Ma||||Clay, fine-grained sand, carbonate and minor conglomerate.|
13707|Namba Formation|71317|5|Briefly described|p144|||||||Equivalent to the Garford Formation.||
13707|Namba Formation|71342|5|Briefly described|Ch5 p29, Ch5 p130, Ch7 p13|Miocene|Oligocene|Lake Eyre Basin. Maximum thickness of 210m in the Cooper region.||||Unconformably overlies the Eyre Formation. Unconformably overlain by the Yandruwantha Sand.|Carbonates and clastic rocks.|
13707|Namba Formation|72456|5|Briefly described|Map Legend|Pliocene|Oligocene|Marree 1:250k map sheet.  Deposited in shallow, brackish to fresh water lakes.|||||Sand, fine to medium-grained, poorly sorted, angular, silt, thin dolomite, oolitic dolomite interbeds.|
13707|Namba Formation|72457|5|Briefly described|p91, 96, 101|Miocene|Miocene|Callabonna sub-basin.||||Overlies Eyre Formation.|Fluvial successions.|
13707|Namba Formation|72458|6|Mentioned|p4|Neogene|Neogene|Low-energy fluviatile and lacustrine sediments.||||Overlain by Willawortina Formation and Pooraka Formation.||
13707|Namba Formation|73251|4|Described|p36-46, p48-53, p55, p57-62|Miocene|Miocene|Lake Eyre Basin, Callabonna Sub-basin. [Many informal subdivisions are referred to including: 'lower member', 'upper member', 'Namba carbonate', 'Alpha mudstone', 'Alpha sequence', 'Beverley sand', 'Beverley sequence', and 'basal unit 1', as well as lower, middle, and main aquitards]. Potential detrital U reductant and potential shallow hydrocarbon source rock. Sandstone hosts Beverley U deposit. Thermally sub-mature. Includes oil-prone organic facies. Depositional environments included fluviolacustrine, shallow/brackish lacustrine, and paludal/swamp. Records suboxic/anoxic bottom-water conditions during deposition of basal strata and oxic for upper strata. Callen and Tedford (1976) nominated the Wooltana 1 drillhole as one of several type localities. Basal strata (lowermost bed of 'lower member') has a reliable palynological date of c. 23 Ma. Contains Namba [organic] facies 1 and 2. [See article for organic petrology descriptions].||||Unconformably underlain by Eyre Formation. Overlain by Willawortina Formation unconformably[?] and Millyera Formation.||
13707|Namba Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Welldata.xlsx.||||||
13721|Namoi Formation|721|5|Briefly described|Map legend|Visean|Tournaisian|Of the Parry Group.  Thinly bedded mudstone and siltstone with minor conglomerate, litharenite, calcareous sandstone and siltstone, bioclastic limestone.||||||21-DEC-04
13721|Namoi Formation|22572|6|Mentioned|p108||Carboniferous|||||||
13721|Namoi Formation|22639|5|Briefly described|p276|Early Carboniferous|Early Carboniferous|||||||
13721|Namoi Formation|22736|6|Mentioned|p630||Tournaisian|||||||
13721|Namoi Formation|22857|4|Described|p496 App.1 Tb.A1.7|Visean|Tournaisian|Of the Parry Group. Thinly bedded mudstone and siltstone with minor conglomerate, litharenite, calcareous sandstone and siltstone, bioclastic limestone. Max. thickness: 1200m. Geological Province: Tamworth Forearc Basin.||||||
13721|Namoi Formation|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|of Parry Group.||||||
13721|Namoi Formation|23185|6|Mentioned|Fig1p156|Carboniferous|Carboniferous|||||||
13721|Namoi Formation|23522|5|Briefly described|p249 Fig 5||Early Carboniferous|||||||
13721|Namoi Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt||||||
13721|Namoi Formation|24010|5|Briefly described|p379|Early Carboniferous|Early Carboniferous|||||||
13721|Namoi Formation|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt.||||||
13721|Namoi Formation|24603|5|Briefly described|p867|Early Carboniferous|Early Carboniferous|See also p869 Fig.4a and p886 Fig. 11.  Geological Province: Tamworth Belt.||||||
13721|Namoi Formation|24605|5|Briefly described|p932 Fig.1|Tournaisian|Tournaisian|Geological Province: New England Orogen.||||||
13721|Namoi Formation|30070|6|Mentioned|Fig.2|||Devonian age.||||||
13721|Namoi Formation|30133|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13721|Namoi Formation|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13721|Namoi Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
13721|Namoi Formation|31519|6|Mentioned|Fig. 1|||||||||
13721|Namoi Formation|31586|6|Mentioned|p6|||Approx. equiv. Riverleigh Lst.||||||
13721|Namoi Formation|31802|6|Mentioned|p136|||Refers Voisey & Williams (1964)||||||
13721|Namoi Formation|32140|6|Mentioned|p22|||Carboniferous||||||
13721|Namoi Formation|32286|6|Mentioned|p49|||See also P50||||||
13721|Namoi Formation|32482|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13721|Namoi Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
13721|Namoi Formation|32672|6|Mentioned|p674|||||||||
13721|Namoi Formation|32683|6|Mentioned|p202|||Refers Leslie (1963)||||||
13721|Namoi Formation|32866|6|Mentioned|p3|||Fossil content||||||
13721|Namoi Formation|32867|6|Mentioned|p26|||||||||
13721|Namoi Formation|34072|6|Mentioned|Fig.4.5|||Carb. Fossils||||||
13721|Namoi Formation|34077|6|Mentioned|p252|||||||||
13721|Namoi Formation|34080|6|Mentioned|p248|||||||||
13721|Namoi Formation|34083|3|Fully described|p247|||Previously Lower Burindi Series||||||
13721|Namoi Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
13721|Namoi Formation|34086|6|Mentioned|p262|||Assemblages||||||
13721|Namoi Formation|34169|6|Mentioned|p250|||||||||
13721|Namoi Formation|34275|6|Mentioned|p193|||Fauna. L.Carb.||||||
13721|Namoi Formation|34349|5|Briefly described|p246|||||||||
13721|Namoi Formation|34555|6|Mentioned|Table 4.2|||||||||
13721|Namoi Formation|36057|6|Mentioned|p352|||||||||
13721|Namoi Formation|36528|6|Mentioned|p176|||||||||
13721|Namoi Formation|36961|6|Mentioned|p210|||||||||
13721|Namoi Formation|37919|6|Mentioned|Fig.2|||||||||
13721|Namoi Formation|37987|2|Defined|p227|Carboniferous|Carboniferous|||||||
13721|Namoi Formation|38215|6|Mentioned|Fig.2|||||||||
13721|Namoi Formation|38222|5|Briefly described|p358|||||||||
13721|Namoi Formation|39214|6|Mentioned|p35|||||||||
13721|Namoi Formation|39331|6|Mentioned|Table 10-1|||||||||
13721|Namoi Formation|39979|6|Mentioned|p50|||||||||
13721|Namoi Formation|40328|6|Mentioned|p198|||||||||
13721|Namoi Formation|41009|6|Mentioned|Fig.2|||||||||
13721|Namoi Formation|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.  Within the Tamworth Belt.||||||16-DEC-04
13721|Namoi Formation|41542|6|Mentioned|p239|||||||||
13721|Namoi Formation|41826|6|Mentioned|p337|||||||||
13721|Namoi Formation|42002|5|Briefly described|p94|||||||||
13721|Namoi Formation|42547|4|Described|p18, p20|Visean|Tournaisian|Age: Carboniferous (late Tournaisian to Visean)||||||
13721|Namoi Formation|42631|5|Briefly described|Fig.1 P265|||||||||
13721|Namoi Formation|42728|4|Described|p7|||||||||
13721|Namoi Formation|43091|5|Briefly described|Map legend|||of Parry Group||||||
13721|Namoi Formation|43383|14|Not recorded|p17|||||||||
13721|Namoi Formation|43407|14|Not recorded|Map Legend||Early Carboniferous|(Provisional Edition)||||||
13721|Namoi Formation|43409|14|Not recorded|Map Legend||Visean|L.Visean age||||||
13721|Namoi Formation|43418|14|Not recorded|Map Legend|||||||||
13721|Namoi Formation|43421|4|Described|p677||Carboniferous|||||||
13721|Namoi Formation|43429|14|Not recorded|Map Legend|||Bioclastic limestone lenses||||||
13721|Namoi Formation|43432|14|Not recorded|p202,204-207,211||Early Carboniferous|||||||
13721|Namoi Formation|43434|4|Described|Map Legend||Carboniferous|||||||
13721|Namoi Formation|43435|14|Not recorded|Map Legend||Carboniferous|||||||
13721|Namoi Formation|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
13721|Namoi Formation|43455|14|Not recorded|p460(Tb.)||Carboniferous|||||||
13721|Namoi Formation|43479|14|Not recorded|p158,159,177|Visean|Tournaisian|||||||
13721|Namoi Formation|43538|14|Not recorded|p2|||Lower Carboniferous fauna.||||||
13721|Namoi Formation|43575|6|Mentioned|p276||Early Carboniferous|||||||
13721|Namoi Formation|43860|5|Briefly described|Fig1, p3; p7||Early Carboniferous|||||||
13721|Namoi Formation|43983|14|Not recorded|p7||Visean|at Babbinboan. Early Visean.||||||
13721|Namoi Formation|44360|14|Not recorded|p33|||Visean fauna.||||||
13721|Namoi Formation|44379|14|Not recorded|p15|||Ref. to Roberts 1965.||||||
13721|Namoi Formation|44833|14|Not recorded|p115-117,121||Early Carboniferous|Faunal units.||||||
13721|Namoi Formation|44835|14|Not recorded|p44,45||Carboniferous|||||||
13721|Namoi Formation|45088|5|Briefly described|p62|||Correlation. Faunal zones||||||
13721|Namoi Formation|45097|5|Briefly described|p14|||See also P24 & correlation chart. Spirifer zone.||||||
13721|Namoi Formation|46803|6|Mentioned|p143|||Refers Roberts (1975)||||||
13721|Namoi Formation|47056|6|Mentioned|Fig.2 P523|||||||||
13721|Namoi Formation|48924|6|Mentioned|p4|||See also P5,8-16,20||||||
13721|Namoi Formation|50132|6|Mentioned|p247 Fig. 5, p248 Fig.6|Carboniferous|Carboniferous|||||Underlain by Tulcumba Sandstone at Keepit Dam.||27-MAR-12
13721|Namoi Formation|50613|5|Briefly described|p208 Fig. 3|||||||||
13721|Namoi Formation|61769|6|Mentioned|p99 Fig. 4|||||||||
13721|Namoi Formation|62095|5|Briefly described|p250|Carboniferous|Carboniferous|Geological Province: Werrie block/Tamworth Belt. See also Plate 1.||||||31-JAN-08
13721|Namoi Formation|63774|6|Mentioned|p1077, p1083|Carboniferous|Carboniferous|Geological Province: Tamworth Belt.||||||
13721|Namoi Formation|63832|5|Briefly described|p131 fig 2|Visean|Tournaisian|Rocky Creek and Werrie Synclines, Southern New England Fold Belt.||||Overlies Luton Formation and Tulcumba Sandstone.|Lower part consists of 22 cycles (cyclothems) of diamictite and dark grey marine mudrock with a hiatal surface between each facies. Overlain by mudrocks and sandstones, then marine strata incised by estuarine channel fills.|13-DEC-17
13721|Namoi Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Tournaisian|Southern New England Fold Belt, Rocky Creek Syncline, Werrie Syncline. Biostratigraphic age control of base and top, and some radiometric age control within unit. Time transgressive base? Older in Werrie Syncline than Rocky Creek Syncline.||||In Rocky Creek Syncline, overlies Luton Formation and is overlain by Caroda Formation.  In Werrie Syncline, overlies Tulcumba Sandstone and is overlain by Merlewood Formation.||
13721|Namoi Formation|65902|4|Described|p195 Fig.2, p199, p200 Fig.5, p203 Fig.7|Tournaisian|Tournaisian|Overlain by Merlewood Formation. Gradational contact with underlying Tulcumba Sandstone. Typically olive-green to brown laminated marine mudstone, siltstone, fine-grained feldspathic sandstone and minor limestone.||||||09-MAR-12
13721|Namoi Formation|66498|6|Mentioned|p49|||Vertebrate fossils listed.||||||
13721|Namoi Formation|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Four facies are mapped separately: mudstone-rich, sandstone-rich; conglomerate-rich, and limestone.||Unit in Parry Group.|||Undifferentiated mudstone, siltstone, sandstone, conglomerate and limestone.|
13721|Namoi Formation|68003|5|Briefly described|p32 Fig.3-h, p33, p138.|Visean|Tournaisian|Tamworth Belt (North), New England Fold Belt.||Unit in Parry Group.|Includes Pallal Conglomerate Member.|Overlies Tulcumba Sandstone and Luton Formation. Is overlain by Caroda Formation.|Conglomerate, sandstone, limestone, siltstone, mudstone.|
13721|Namoi Formation|68005|5|Briefly described|p49 Fig.3-M, p56, p59, pp146-147, p170.|Visean|Visean|Tamworth Belt. Dominated by felsic volcaniclastics: moderate to high K, Th, U radiometric responses.||Unit in Parry Group.|Includes Pallal Conglomerate, and Tiilungra Limestone, Members.|Overlies Tulcumba Sandstone. Is overlain by Caroda Formation.|Olive-green to olive-brown siltstone, mudstone, sandstone, limestone and conglomerate.|
13721|Namoi Formation|68297|5|Briefly described|p187, 197|Tournasian|Tournasian|NSW.  Includes 'bradyodont' shark teeth||||||
13721|Namoi Formation|69793|6|Mentioned|p1121 Fig.12|Tournaisian|Tournaisian|Rocky Creek Block, Tamworth Belt.||||||
13721|Namoi Formation|70050|5|Briefly described|p331-333, p364-365|Visean|Tournaisian|Campbell (1957). Halls Creek area near Bingara. Contains Cionodendron coral fossils (illustrations and systematic palaeontology), including the holotype of C. hallense.||||||
13721|Namoi Formation|70728|5|Briefly described|p265|Tournaisian|Tournaisian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Merlewood Formation. Underlain by Tulcumba Sandstone or Luton Formation.||
13721|Namoi Formation|70777|6|Mentioned|p8|Carboniferous|Carboniferous|Werrie Block, New England Orogen.||||||
13721|Namoi Formation|70907|5|Briefly described|p771-780|Carboniferous|Carboniferous|Werrie Syncline. 640-914m thick. Analysed for shale gas prospectivity: detailed. Found to be a prospective gas source.||||Overlies Tulcumba Sandstone. Is overlain by Merlewood Formation.|Dominantly olive-green mudstones with lenses of sandstone and oolitic limestone.|
13721|Namoi Formation|71628|6|Mentioned|p18:20|||||Parry Group.||||
13738|Namur Sandstone|13497|3|Fully described|p26, p115, p115 fig 6.33|Jurassic|Jurassic|Eromanga Basin. Deposited in a low sinuosity fluvial environment. See also p138 fig 8.17, p139 fig 8.18, p141, p146, p151 fig 9.23, p152 fig 9.25,  p171, p173, p184, p216. Incorrectly referred to as the obsolete Namur Sandstone Member in the App, p216.||||Overlies the Adori Sandstone and the Westbourne Formation. Overlain by the McKinlay Member, Murta Formation and the Cadna-owie Formation.|Sandstone.|
13738|Namur Sandstone|13516|6|Mentioned|p167 fig 10, p171 fig 12|Early Cretaceous|Late Jurassic|In Eromanga Basin.||||||
13738|Namur Sandstone|22839|6|Mentioned|P33|||||||||
13738|Namur Sandstone|22883|5|Briefly described|P31, Fig2||Late Jurassic|Overlying unit is Murta Formation, underlying unit is Birkhead Formation.||||||16-SEP-08
13738|Namur Sandstone|22909|5|Briefly described|42|||||||||
13738|Namur Sandstone|23054|6|Mentioned|Fig5p22|||||||||
13738|Namur Sandstone|23155|2|Defined|p26-27 & Fig 15 p28|Early Cretaceous|Late Jurassic|For Max. Thickness of type section see Fig 15 on p28.  For location of type section and details of previous names see p27.||||||16-APR-08
13738|Namur Sandstone|23375|4|Described|Fig2 p265,268-271|Berriasian|Oxfordian|Laterally equivalent to lower-middle Hooray Sandstone, Westbourne Formation and Adori Sandstone. IN the Eromanga Basin.||||||17-JAN-08
13738|Namur Sandstone|23849|5|Briefly described|p781|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24204|5|Briefly described|p266|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|24372|6|Mentioned|p22|||Geological Province: Cooper Basin.||||||
13738|Namur Sandstone|24482|5|Briefly described|p44|Cretaceous|Jurassic|Geological Province: Eromanga Basin.||||||
13738|Namur Sandstone|37287|6|Mentioned|p33|||||||||
13738|Namur Sandstone|38108|6|Mentioned|Table 1|||||||||
13738|Namur Sandstone|38730|6|Mentioned|p29|||||||||
13738|Namur Sandstone|40030|6|Mentioned|p131|||||||||
13738|Namur Sandstone|40670|6|Mentioned|p213|||||||||
13738|Namur Sandstone|41061|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41099|6|Mentioned|Fig.6|||||||||
13738|Namur Sandstone|41123|6|Mentioned|p180|||||||||
13738|Namur Sandstone|41216|6|Mentioned|p300|||||||||
13738|Namur Sandstone|41705|6|Mentioned|p122|||||||||
13738|Namur Sandstone|41712|6|Mentioned|p282|||||||||
13738|Namur Sandstone|41724|6|Mentioned|p382|||||||||
13738|Namur Sandstone|42357|6|Mentioned|p11|||||||||
13738|Namur Sandstone|43711|6|Mentioned|p18|||||||||
13738|Namur Sandstone|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Birkhead Formation; overlain by Murta Formation; lateral to Adori Sandstone, and possibly to Algebuckina Sandstone also. Geological Province: Eromanga  Basin.||||||31-JAN-08
13738|Namur Sandstone|61613|6|Mentioned|p282, p284|Jurassic|Jurassic|||||||07-FEB-11
13738|Namur Sandstone|61614|6|Mentioned|p295, p290 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
13738|Namur Sandstone|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|62028|6|Mentioned|p10|||Abbreviation? of Namur Sandstone Member.||||||26-FEB-08
13738|Namur Sandstone|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
13738|Namur Sandstone|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Algebuckina Sandstone. Is overlain by Bulldog Shale and Cadna-owie Formation.||
13738|Namur Sandstone|63979|5|Briefly described|Fig. 44|Berriasian|Oxford|Supersedes "Namur Sandstone member". As a formally defined SA unit, this encompasses the Queensland interval Adori Sandstone-Westbourne Formation-Hooray Sandstone.||||||07-FEB-11
13738|Namur Sandstone|64048|6|Mentioned|p71|||Superseded "Namur Sandstone Member" of the Mooga Formation in South Australia. Mooga Formation now obsolete. Geological Province: Eromanga Basin.||||||07-FEB-11
13738|Namur Sandstone|64197|6|Mentioned|p630 Fig.6|Late Jurassic|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Member.||
13738|Namur Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Late Jurassic|Eromanga Basin.||||Is overlain by Murta Formation.||
13738|Namur Sandstone|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Sheet sandstone of fluvial origin.||||||
13738|Namur Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Late Jurassic|Of Eromanga Basin. Overlain by Murta Formation. Unit shown to include unconformity around Jurassic-Cretaceous boundary? Quartz-rich sediment. See also "upper Namur Sandstone".||||||08-MAR-12
13738|Namur Sandstone|65489|5|Briefly described|p11, p15, p17, p47, p49, p61, p73, p96|Early Cretaceous|Jurassic|See also p154-155, p158-160. Eromanga Basin. Fair to excellent reservoir quality. Predominantly anticlinal traps. Gas and oil reservoir accounting for 30% and 15% respectively of the Basin's production.||||Overlies Westbourne Formation. Is overlain by Murta Formation.|Braided fluvial sandstone.|
13738|Namur Sandstone|65925|5|Briefly described|Appendix 2.||||||||White to pale grey, fine- to medium-grained, crossbedded and quartzose sandstone; minor siltstone and mudstone.|
13738|Namur Sandstone|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||||Overlies Injune Creek Group. Is overlain by Murta Formation.||
13738|Namur Sandstone|66623|3|Fully described|p34, p102, pp238-249. |Cretaceous|Cretaceous|Name introduced by Mount (1981) as member of Mooga Formation; formation status by Gravestock et al. (1995). Partly equivalent to Gum Vale Beds (Rose and Brunker 1969) and Warratta Sandstone Member (Moreton 1982). Equivalent to lower part of Hooray Sandstone and Algebuckina Sandstone in Queensland. Overall, an upward-fining sequence. Variably ferruginised and cross-bedded. Thickness varies to 1200 m. Basal section hosts flaky alluvial gold and nuggets. Silicified wood locally abundant.||||Unconformably overlies Nundora and Depot Glen Formations, as well as Tibooburra Granodiorite. Is overlain by Cadna-owie Formation and, locally, by Eyre Formation and Cordillo Silcrete.|Basal quartz pebble conglomerate; non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone; minor thin claystone lenses.|
13738|Namur Sandstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga Basin. In Fig.3 also shows "upper Namur Sandstone".||||||
13738|Namur Sandstone|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous sandstone and conglomerate is mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate.|
13738|Namur Sandstone|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|The ferruginous and  weathered units are mapped separately.|||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses; ferruginous sandstone, conglomerate; deeply weathered, kaolinised sandstone and claystone.|
13738|Namur Sandstone|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|66922|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Easter Monday Formation of the Warratta Group. Is overlain by Wyandra Sandstone Member of Cadna-owie Formation.|Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|67402|6|Mentioned|p109 tbl ERO1|||||||Equivalent to the Hooray Sandstone and Murta Formation.||
13738|Namur Sandstone|68068|5|Briefly described|Map legend|Early Cretaceous|Late Jurassic|Eromanga Basin. Subsurface only. Is replaced by Algebuckina Sandstone as it pinches out at Eromanga Basin margin. Sandy lacustrine and braided river deposits.||||Overlies Birkhead Formation. Is overlain by Murta Formation.|White, fine- to coarse-grained sandstone, flat to cross-bedded, locally with calcareous cement, channel lag conglomerate; siltstone interbeds, especially in middle part; minor mudstone and coal stringers.|
13738|Namur Sandstone|68135|5|Briefly described|p52 Fig.2b|Early Cretaceous|Tithonian|Eromanga Basin.||||Unconformably overlies Westbourne Formation.|Predominantly sandstone.|
13738|Namur Sandstone|68731|6|Mentioned|pp209-211|||||||||
13738|Namur Sandstone|69001|6|Mentioned|p16|||See also Namur sandstone. Interpretations by the NSW DPI of the Namur Sandstone flanking many of the inliers are broadly grouped in this study within the Algebuckina Sandstone and equivalent units.||||||
13738|Namur Sandstone|69019|5|Briefly described|p85 Fig.21.|Early Cretaceous|Early Cretaceous|Southern Eromanga Basin.||||Overlies Westbourne Formation. Is overlain by Murta Formation.||
13738|Namur Sandstone|69023|4|Described|p79, p89 Fig.20, p91, p191-192|Hauterivian|Berriasian|Named after Delhi Petroleum exploration well Namur 1 (Mount, 1981) as Namur Sandstone Member of Mooga Formation (Nugent, 1969). This last name has been abandoned (Gravestock et al.,1995) as the Namur Sandstone Member was elevated to Formation status (Callen et al.,1994; Gravestock et al.,1995; after Martin (1983). Eromanga Basin. Thickness from ~120 to ~194m, thinning to W. Stratigraphic wells intersection data.||||Overlies Birkhead Formation. Intertongues with Westbourne Formation. Passes laterally into Algebuckina Sandstone. Is overlain by Murta Formation.|White to pale grey, flat and cross-bedded, fine- to coarse-grained, quartzose sandstone; minor siltstone and mudstone interbeds; channel lag conglomerates. Locally strongly cemented with calcite.|
13738|Namur Sandstone|69454|6|Mentioned|p38:13|||Cooper Basin. With the overlying Murta Formation, is equivalent to the upper Algebuckina Sandstone in the Poolowanna Trough.||||||12-JUL-16
13738|Namur Sandstone|69457|6|Mentioned|p41:3-4, 7|||Eromanga Basin.||||Is overlain by Murta Formation.||12-JUL-16
13738|Namur Sandstone|69594|5|Briefly described|p519, p525-527, p532, p573|Tithonian|Tithonian|Eromanga Basin. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated and the succession is called the Namur Sandstone. In QLD, where differentiation is possible, the Westbourne Formation is overlain by the Hooray Sandstone, equivalent to the topmost, Murta Formation overlying the rest of the upper part of the Namur Sandstone. This unit separating Westbourne and Murta Formations is referred to in QLD as the [informally named] upper Namur Sandstone, echoing the obsolete Namur Sandstone Member (Gray et al. 2002). A significant hydrocarbon reservoir.||||?Overlies Birkhead and Westbourne Formations unconformably. Passes laterally into Westbourne Formation locally. Is overlain by Murta Formation.||
13738|Namur Sandstone|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Cretaceous|||||Overlies Westbourne Formation, overlain by McKinlay Member, Murta Formation||
13738|Namur Sandstone|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Late Jurassic|Eromanga Basin.||||||
13738|Namur Sandstone|69797|5|Briefly described|p17 Fig.2|Early Cretaceous||Age: Late Jurassic - Early Cretaceous (approximated from figure). Geol. Prov: Eromanga Basin.||||||
13738|Namur Sandstone|69946|3|Fully described|p11, p15-17, p57-58, p61, p83-85|Early Cretaceous|Late Jurassic|Originally Mooga Formation (Nugent, 1969) or part of Hooray Sandstone; named Namur Sandstone Member by Mount (1981) after Namur 1; elevated to Formation status by Gravestock et al. (1995) with the name Mooga Formation discarded in SA. In Qld the lower part of Hooray Sandstone is an equivalent. Type section is the interval 1435.22 - 1643.48m in Strzelecki 4. Generally 40 - 240m thick. Wireline log correlations.||||Conformably overlies Birkhead and Westbourne Formations. Intertongues with overlying Murta Formation or McKinlay Member. Lateral equivalent of Algebuckina Sandstone.|White to pale grey, fine- to coarse-grained sandstone with minor interbedded siltstone and mudstone; conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts; locally strongly cemented by diagenetic calcite.|
13738|Namur Sandstone|69947|5|Briefly described|p3, p7-8, p13 Fig.7.2, p27 Fig.7.16|Early Cretaceous|Late Jurassic|See also p29 Fig.7.18. Eromanga Basin. Lowstand braided fluvial sandstones form significant hydrocarbon reservoirs. Generalised stratigraphic section.||||Conformably overlies Birkhead Formation. Intertongues with Westbourne Formation. Is overlain transitionally by McKinlay Member (Murta Formation). ?Correlates with Hooray Sandstone.|Fluvial sandstones, minor shale.|
13738|Namur Sandstone|69948|6|Mentioned|Fig.4.2|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Is overlain by Murta Formation.||
13738|Namur Sandstone|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group?|||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|16-SEP-15
13738|Namur Sandstone|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. 2 un-named units: Clast supported conglomerate variant. Strongly silicified variant.|
13738|Namur Sandstone|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Un-named units: Ferruginous sandstone, conglomerate. Deeply weathered, leached and kaolinised sandstone and claystone.|||Includes 2 un-named units.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes un-named unit.||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses. Un-named unit is a strongly silicified variant.|
13738|Namur Sandstone|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Non-marine, medium- to coarse-grained, pale grey and buff, cross-bedded quartzose and pebbly sandstone with conglomerate beds and minor thin claystone lenses.|
13738|Namur Sandstone|70821|5|Briefly described|p21 Fig.2.6, p31|Early Cretaceous|Jurassic|Eromanga Basin. Previously part of the [obsolete] "Lower Hooray Sandstone". 29 m thick interval, between 439-468 m in Weilmoringle 1 well.|||Appears to include the Murta Member.|Overlies Westbourne Formation. Is overlain by Cadna-owie Formation, Murta Formation..||02-DEC-16
13738|Namur Sandstone|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Late Jurassic|Eromanga Basin.  Up to 210m thick. Deposited in a braided fluvial with intertonguing lacustrine environment.||||Intertongues with the Hutton Sandstone. Overlies the Westbourne Formation. Overlain by the Murta Formation.||
13738|Namur Sandstone|70824|5|Briefly described|p9|Cretaceous|Jurassic|Eromanga Basin.||||Overlies the Westbourne Formation. Overlain by the Cadna-owie Formation.||
13738|Namur Sandstone|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
13738|Namur Sandstone|71342|3|Fully described|Ch 1 p3, Ch 1 p6|Berriasian|Late Jurassic|Eromanga Basin. Mount (1981) named the Namur Sandstone Member after Namur 1. The unit was previously referred to as the Mooga Formation or Hooray Sandstone. Martin (1983), Gravestock et al. (1995) elevated the Namur Sandstone Member of the Mooga Formation to formation status and discarded the Mooga Formation in South Australia. Source of the majority of gas production in the Eromanga Basin. Equivalent to the lower part of the Hooray Sandstone. In Queensland this unit may be subdivided into the Adori Sandstone, Westbourne Formation and Namur Sandstone. A type section in Strzelecki 4 is given (Gravestock et al., 1995). This unit is generally 40 to 240m thick in the Cooper region. Interpreted to have been deposited in a low-sinuosity fluvial environment similar to that of the Algebuckina and Hutton Sandstones. Spore-pollen zone is given in Ch5 p57. Seal and reservoir characteristics discussed in Ch11.  Laterally equivalent to the Algebuckina Sandstone. See also Ch 1 p19, Ch3 p17-p18, Ch4 p9, Ch5 p12, Ch5 p14-p17, Ch5 p32, Ch5 p57-p58, Ch5 p82-p84, Ch6 p5-p7, Ch7 p7-p8, Ch7 p10, Ch7 p13, Ch7 p29, Ch8 p3, Ch8 p10, Ch8 p17, Ch9 p5, Ch9 p10-p11, Ch10 tbl 10.1, Ch10 p6-p8, Ch10 p14, Ch10 p18-p20, Ch11 p3-p5, Ch11 p7-p8, Ch11 p16, Ch12 p2, Ch12 p5-p6, Ch12 p15, Ch13 p2-p7, Ch13 p9-p10, Ch13 p18, Ch13 p21-p22, Ch13 p26-p27, Ch13 p29, Ch13 p31, Ch14 p3, Ch14 p5-p7.||||Conformably overlies the Birkhead Formation. Overlain by the Cadna-owie Formation. Intertongues with or is overlain by the Westbourne Formation (lower) and the Murta Formation or McKinlay Member.|White to pale grey, fine to coarse-grained sandstone with minor interbedded siltstone and mudstone. Conglomeratic interbeds consist of lithic and quartz pebbles, carbonaceous mudstone intraclasts and carbonised plant fragments.|
13738|Namur Sandstone|71415|5|Briefly described|p11-14|Cretaceous|Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Probably Cretaceous in age (Exon and Senior 1976; Hill et al. 2008). LA-ICPMS zircon age populations show peaks at c. 575, c. 510, 480+\-12 and 430+\-6 Ma. Also includes small Proterozoic zircon populations at c. 2020-900 Ma, and minor Archean c. 3330 to 2555 Ma populations.||||Overlain by Cadna-owie Formation. Laterally equivalent to Algebuckina Sandstone.||19-AUG-19
13738|Namur Sandstone|71863|6|Mentioned|p5|Valanginian|Tithonian|Eromanga Basin.||||Overlain by the Murta Formation.||
13738|Namur Sandstone|72298|5|Briefly described|p801|Cretaceous|Jurassic|Eromanga Basin (SA,QLD). Main confined aquifers, generally producing flowing artesian water bores.||||Overlies Westbourne FZ (Injune Creek Group). Is overlain by Murta FZ.||
13738|Namur Sandstone|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown with Hooray Sandstone as located in the Eromanga Basin.||||Unconformably overlies Westbourne Formation.||
13738|Namur Sandstone|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
13738|Namur Sandstone|73251|6|Mentioned|p49, p55-56, p62|Cretaceous|Late Jurassic|Eromanga Basin. Contains hydrocarbon accumulations to which the Murta Formation contributed.||||Underlain by Birkhead and Westbourne formations. Equivalent to Westbourne Formation, Adori Sandstone and Algebuckina Sandstone. Overlain by and equivalent to McKinlay Member (Murta Formation).||
13738|Namur Sandstone|73343|6|Mentioned|p337|Cretaceous|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Mooga Formation. Overlain by Cadna-owie Formation. Equivalent to Murta Member, Hooray Sandstone, and Westbourne Formation.||
13738|Namur Sandstone|73479|5|Briefly described|p156 Fig.2, p159, p164, p179|Cretaceous|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 152-140 Ma|||Overlies Mooga Formation, underlies Cadna-owie Formation||
13773|Nandillyan Limestone|6969|5|Briefly described|p12|Wenlock|Wenlock|Of the Mumbil Group.  Geological Province: Lachlan Fold Belt.||||||
13773|Nandillyan Limestone|13996|6|Mentioned|p128|Silurian|Silurian|Has a chronologically varied basal lag deposit with a sparse fauna of Llandovery-aged conodonts.||||||
13773|Nandillyan Limestone|22486|6|Mentioned|p 3|||||||||
13773|Nandillyan Limestone|22857|4|Described|p466 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Mumbil Group. Bedded highly fossiliferous limestone. Max. thickness: ~300m.||||||
13773|Nandillyan Limestone|23043|5|Briefly described|Map Legend|Wenlock|Wenlock|of Mumbil Group.||||||
13773|Nandillyan Limestone|23170|2|Defined|p85|Wenlock||Of Mumbil Group.||||||04-MAR-09
13773|Nandillyan Limestone|23214|3|Fully described|p131|Ludlow|Ludlow|Of Mumbil Group. Originally named Nadillyan Limestone Member. Also previously included as part of Gamboola Formation. Previously thought to be a synonym of Narragal Limestone. Max. thickness 600m.||||||04-MAR-09
13773|Nandillyan Limestone|23225|4|Described|p12||Wenlock|Age: graptolite zone 26 - basal. Large fossil assemblage assisting in age determination. Temporal equivalent of Dripstone Formation. Of Mumbil Group.||||||04-MAR-09
13773|Nandillyan Limestone|33611|6|Mentioned|p130|||||||||
13773|Nandillyan Limestone|34406|6|Mentioned|p220|||||||||
13773|Nandillyan Limestone|37276|6|Mentioned|p313|||||||||
13773|Nandillyan Limestone|39975|6|Mentioned|p135|||||||||
13773|Nandillyan Limestone|43517|14|Not recorded|p147||Silurian|See also Lexicon||||||
13773|Nandillyan Limestone|43640|5|Briefly described|Map Legend||Silurian|||||||
13773|Nandillyan Limestone|43782|5|Briefly described|Map Legend|Wenlock|Wenlock|Of Mumbil Group.||||||04-MAR-09
13773|Nandillyan Limestone|50095|5|Briefly described|p108 Fig.1|Silurian|Silurian|||||||
13773|Nandillyan Limestone|64826|5|Briefly described|p1042, p1043|Silurian|Silurian|Of the Mumbil Group. See also the misspelt Nandilyan Formation. Unconformable on Oakdale Formation. Dark grey, quite fossiliferous and rich in organic matter.||||||
13773|Nandillyan Limestone|68592|6|Mentioned|p1890|Ludlow|Wenlock|In the northern Molong High. Contains Thamnopora species, similar to those in Rhyanna Formation.||||||
13773|Nandillyan Limestone|70297|5|Briefly described|map legend, on side 2 of map sheet|Silurian|Silurian|Parent age: late early Silurian to earliest Devonian.||Mumbil Group|||Thick carbonate unit.|
13773|Nandillyan Limestone|71656|6|Mentioned|p30|Ludlow|Wenlock|Molong High.||||||
13774|Nandooka Sandstone|40595|6|Mentioned|Fig.7|||||||||
13778|Nangar Subgroup|22638|4|Described|p71|||Of Hervey Group.||||||25-JUN-08
13778|Nangar Subgroup|22831|5|Briefly described|Table 24|||||||||
13778|Nangar Subgroup|22859|6|Mentioned|p213|||||||||
13778|Nangar Subgroup|23214|6|Mentioned|p226|||Of Hervey Group. Name discontinued. Geological Province: Hervey Basin||||||
13778|Nangar Subgroup|30071|6|Mentioned|p369|||||||||
13778|Nangar Subgroup|37751|6|Mentioned|p143|||||||||
13778|Nangar Subgroup|43441|5|Briefly described|31||Late Devonian|||||||08-JAN-10
13778|Nangar Subgroup|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
13778|Nangar Subgroup|43507|2|Defined|p123-130,144-162||Late Devonian|||||||
13778|Nangar Subgroup|43510|14|Not recorded|p37,41-2,45-7,49-50,|||Constituent formations defined. p52,58,60,63,65-67,69-71,74,77,82||||||
13778|Nangar Subgroup|43513|14|Not recorded|p72|||||||||
13778|Nangar Subgroup|44192|5|Briefly described|Map Legend|||||||||
13778|Nangar Subgroup|50231|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of the Hervey Group.  Includes: Mandagery Formation, Bumberry Formation.||||||13-MAY-04
13778|Nangar Subgroup|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Hervey Group. Contains Mandagery and Bumberry Formations.||||||
13778|Nangar Subgroup|68298|5|Briefly described|p216||Late Devonian|Of Connolly (1965), central and western NSW sediments. Placoderm plates from various localities and horizons occur mainly within sandstones of this unit referred to by Connolly (1965) as the 'bothriolepid fish assemblage'.||Hervey Group||Overlies Beargamil Subgroup. Is overlain by Cookamidgera Subgroup.||
13778|Nangar Subgroup|68592|6|Mentioned|p1698, p1748|||Conolly (1965). Obsolete due to problems in correlation.||Unit in Hervey Group.||Probable part-correlate of Cookbundoon Formation.||
13831|Napperby Formation|721|5|Briefly described|Map legend|Ladinian|Anisian|Finely laminated quartzose sandstone and siltstone interbedded with thick, massive or crossbedded sandstones; minor conglomerate.  Geological Province: Gunnedah Basin.||||||21-DEC-04
13831|Napperby Formation|22579|5|Briefly described|p219 Fig.2|Triassic|Triassic|||||||
13831|Napperby Formation|22857|4|Described|p265, p518 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Max. thickness: 250m. Geological Province: Gunnedah and Sydney Basins. See also p526 App.1 Tb.A1.9 and p315 Fig. 22.8.||||||
13831|Napperby Formation|22864|6|Mentioned|p265|||||||||
13831|Napperby Formation|22865|6|Mentioned|Fig22.8p315|||||||||
13831|Napperby Formation|23043|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|In the Gunnedah Basin.||||||20-NOV-06
13831|Napperby Formation|23050|5|Briefly described|p 82 Fig.17|Middle Triassic|Early Triassic|In the Gunnedah Basin.||||||20-NOV-06
13831|Napperby Formation|23170|2|Defined|p310|Middle Triassic|Early Triassic|In the Sydney Basin.||||||20-NOV-06
13831|Napperby Formation|23566|5|Briefly described|p116 Fig. 2|Triassic|Triassic|Geological Province: Gunnedah Basin||||||
13831|Napperby Formation|23740|5|Briefly described|p1221|Triassic|Triassic|Geological Province: Gunnedah Basin||||||
13831|Napperby Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
13831|Napperby Formation|24092|5|Briefly described|p8 Fig.3|||||||||
13831|Napperby Formation|24159|5|Briefly described|p150 Fig.3, p151|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin. Underlain by Digby Formation; overlain by (unconformably) Purlawaugh Formation.||||||20-NOV-06
13831|Napperby Formation|24243|5|Briefly described|p3 Fig.2|Triassic|Triassic|||||||
13831|Napperby Formation|37856|6|Mentioned|Table I|||||||||
13831|Napperby Formation|38614|4|Described|p12|||||||||
13831|Napperby Formation|39063|6|Mentioned|Fig.3|||||||||
13831|Napperby Formation|40200|4|Described|p6|||||||||
13831|Napperby Formation|40332|6|Mentioned|p21|||||||||
13831|Napperby Formation|40767|4|Described|p8|||||||||
13831|Napperby Formation|40952|6|Mentioned|p8|||||||||
13831|Napperby Formation|41264|6|Mentioned|p252|||||||||
13831|Napperby Formation|41290|4|Described|p226|||||||||
13831|Napperby Formation|41330|4|Described|p21|||||||||
13831|Napperby Formation|41451|6|Mentioned|p14|||||||||
13831|Napperby Formation|41472|4|Described|p56|||||||||
13831|Napperby Formation|42284|5|Briefly described|Fig.11 P104|||||||||
13831|Napperby Formation|42463|6|Mentioned|Fig.6 P173|||||||||
13831|Napperby Formation|42679|5|Briefly described|Fig.3 P3|||||||||
13831|Napperby Formation|42809|5|Briefly described|p436|||see also Fig.2 p438.||||||20-NOV-06
13831|Napperby Formation|42918|6|Mentioned|p45|||||||||
13831|Napperby Formation|43091|5|Briefly described|Map legend|||In the Gunnedah Basin.||||||20-NOV-06
13831|Napperby Formation|43194|1|Redefined|p98 Tb 8.2, p118-127, p133 App. 1|Middle Triassic|Early Triassic|See also references on p95-96, p129 Tb.8.3, p131. Supersedes Napperby Series/Beds. Disconformably overlies Digby Formation. Underlies Deriah Formation. Correlated with the Gosford Formation (lower Napperby Formation), Hawkesbury Sandstone and Ashbury Shale (middle) and the lower part of Bringelly Shale.||||||13-NOV-13
13831|Napperby Formation|43494|4|Described|p12-13|Middle Triassic|Middle Triassic|Referred to as "Ballimore Formation" by Offenberg et al (1971) and included the Boulderwood Conglomerate. Overlies Dunedoo Fm (Permian); underlies Pilliga Sandstone (Jurassic). Max. thick in area: 70m. Equiv. to Wallingarah Fm of Loughan and Evans (1978).||||||20-NOV-06
13831|Napperby Formation|43582|6|Mentioned|Fig.5,p16|Middle Triassic|Early Triassic|||||||
13831|Napperby Formation|44093|5|Briefly described|p192 App. 1|Triassic|Triassic|Geological Province: Lachlan Fold Belt.||||||
13831|Napperby Formation|50590|5|Briefly described|Map Legend|Triassic|Triassic|Geological Province: Gunnedah Basin.  Siltstone thinly interbedded with sandstone, minor conglomerate.||||||
13831|Napperby Formation|50629|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Geological Province: Gunnedah Basin. Underlies: Deriah Formation.  Overlies: Digby Formation.||||||05-JUL-04
13831|Napperby Formation|60266|5|Briefly described|p2, p3 Tb. 1|Middle Triassic|Middle Triassic|Lacustrine and prograding delta sequence of quartz-lithic sandstone, siltstone and shale.  Overlies the Digby Formation; overlain by the Deriah Formation.  Geological Province: Gunnedah Basin.||||||03-AUG-04
13831|Napperby Formation|60267|5|Briefly described|p15, p28 Fig. 8|Triassic|Triassic|||||||
13831|Napperby Formation|61201|6|Mentioned|p2|Middle Triassic|Middle Triassic|||||||
13831|Napperby Formation|61313|5|Briefly described|p97, p94 Fig.G7|Early Triassic|Early Triassic|Distinctive shale/siltstone/sandstone sequence; basal part is a regionally extensive shale unit up to 40m thick and acts as a seal for Digby Formation "Quartz Sand" reservoirs. Disconformable over Digby Fm. Max. thickness: 215m. Geol.Prov: Gunnedah Basin||||||20-NOV-06
13831|Napperby Formation|61377|5|Briefly described|p149 Fig. SU8, p152, p154 Fig. SU9|Middle Triassic|Middle Triassic|East of Coonamble Embayment - commonly referred to as the Wallingarah Fm, differentiated into Rivers Sst Mbr (lower) and Boothenba Sst Mbr (upper) with an undifferentiated middle section of sltst and sst. Geol.Prov: Gunnedah Basin.||||||07-FEB-11
13831|Napperby Formation|61612|6|Mentioned|p275, p276, p277, p270 Fig. 1|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||17-MAR-09
13831|Napperby Formation|61772|6|Mentioned|p129, 130||Middle Triassic|||||||
13831|Napperby Formation|61776|5|Briefly described|p194 Fig. 3|Middle Triassic|Triassic|Geological Province: Gunnedah Basin. Quartz-lithic sandstone, laminite and siltstone.||||||
13831|Napperby Formation|62357|5|Briefly described|p524 Fig. 7|Early Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||
13831|Napperby Formation|63117|6|Mentioned|p156|||Includes Benelong flora, near Dubbo.||||||13-MAR-07
13831|Napperby Formation|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Early Triassic|Unit in the Gunnedah Basin. Overlies Digby Formation, underlies the Deriah Formation.||||||22-MAR-12
13831|Napperby Formation|65113|5|Briefly described|Fig 4 p340|Middle Triassic|Early Triassic|Gunnedah Basin. Underlies the Deriah Formation.||||||
13831|Napperby Formation|65114|5|Briefly described|p385 Fig.3|Middle Triassic|Early Triassic|||||||
13831|Napperby Formation|65115|6|Mentioned|Fig 2 p403|Triassic|Triassic|Underlies the Deriah Formation, overlies the Digby Formation in the Gunnedah Basin.||||||
13831|Napperby Formation|65116|4|Described|p450, 451, 449, Fig 2 p436, Fig 6 p441|Middle Triassic|Early Triassic|Underlies the Deriah Formation, Gunnedah Basin. Maximum thickness ~130m. Lower part equivalent to pre-Showgrounds Sandstone part of Clematis Group. Fine grained sandstone with interbedded silt and claystone in the upper half, the lower half is upward coarsening laminated silt/sandstone with varying bioturbation and burrows.||||||
13831|Napperby Formation|65118|5|Briefly described|Fig 2 p479|Triassic|Triassic|Underlies the Deriah Formation in the Gunnedah Basin.||||||
13831|Napperby Formation|66191|5|Briefly described|p485 Fig.2, p485|Early Triassic|Early Triassic|Gunnedah Basin. Underlies the Deriah Formation, overlies the Digby Formation. Siltstone/claystone, interbedded sandstone/siltstone to sandstone, derived from New England Fold Belt.||||||
13831|Napperby Formation|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment.||||Overlies Digby Formation. Is overlain unconformably by Garrawilla Volcanics.||
13831|Napperby Formation|67127|5|Briefly described|p111|Triassic|Triassic|Cut by a pipe-like body that hosts the Toongi deposit.|||||Quartzofeldspathic sandstone and minor siltstone.|
13831|Napperby Formation|68003|5|Briefly described|p38 Fig.3-j, pp42-43, pp46-47, p128.|Middle Triassic|Middle Triassic|Gunnedah Basin, Brigalow Belt South Bioregion. Correlative of the Wianamatta Group (Hunter Coalfield). Deposited in a gross regressive cycle, from lacustrine to delta and ultimately to fluvial sedimentation; main source was the New England Fold Belt.||||Overlies Digby and Black Jack Formations unconformably, and Wollar Sandstone. Is overlain by Deriah Formation and, unconformably, by Garrawilla Volcanics.|Basal section of lacustrine laminated siltstone and mudstone; then upward coarsening sequence of siltstone/claystone to sandstone; then fluvial, irregularly interbedded sandstone and siltstone sequences.|
13831|Napperby Formation|68004|5|Briefly described|p23 Table 1, p62, p139, p176.|Triassic|Triassic|Gunnedah Basin. Kaolin prospectivity is discussed. Acts as regional seal over Digby Formation reservoirs. A potential oil source rock.||||Overlies Digby Formation. Is overlain by Deriah Formation.|Coarsening-up sequences of dark grey siltstone/sandstone laminite overlain by parallel-bedded or low-angle crossbedded quartzose sandstone.|
13831|Napperby Formation|70036|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Included in a mapped unit of fluvial and lacustrine sequences: conglomerate, quartzose and lithic sandstone, siltstone and mudstone.||||||
13831|Napperby Formation|70791|5|Briefly described|p276-277|Middle Triassic|Middle Triassic|Gunnedah Basin. Lacustrine deposits.||||||
13831|Napperby Formation|70821|5|Briefly described|p80|Triassic|Triassic|Coonamble Embayment.||||Is overlain unconformably by Garrawilla Volcanics.||
13831|Napperby Formation|71600|6|Mentioned|p23 Fig 1|Mesozoic|Mesozoic|||||||
13831|Napperby Formation|71890|5|Briefly described|p5-p7, p18, p30-p31, p52-p53|Middle Triassic|Early Triassic|Gunnedah Basin.||||Overlain by the Purlawaugh Formation. Unconformably overlain by the Garrawilla Volcanics.||
13831|Napperby Formation|72298|5|Briefly described|p801|Triassic||Coonamble Embayment (NSW).||||Overlies Digby FZ. Is overlain unconformably by Garrawilla Volcanics.||
13874|Narrabeen Group|22500|5|Briefly described|p 6||Early Triassic|Sydney Basin||||||
13874|Narrabeen Group|22529|6|Mentioned|4 fig 2|Mesozoic|Mesozoic|||||||
13874|Narrabeen Group|22549|5|Briefly described|p525-7 p533-6||Triassic|||||||
13874|Narrabeen Group|22578|5|Briefly described|Fig.10 p400, p403||Triassic|||||||
13874|Narrabeen Group|22598|6|Mentioned|P789|||||||||
13874|Narrabeen Group|22601|6|Mentioned|417|Triassic|Triassic|Geol province Sydney Basin||||||
13874|Narrabeen Group|22607|6|Mentioned|p 57|||||||||
13874|Narrabeen Group|22663|5|Briefly described|NSW97 - 1 p2||Triassic|||||||01-MAR-10
13874|Narrabeen Group|22745|5|Briefly described|p125|Anisian|Scythian|Sydney Basin. 800 m. Overlain by Hawkesbury Sandstone.||||||
13874|Narrabeen Group|22749|5|Briefly described|p185-86,189,194|||||||||
13874|Narrabeen Group|22833|6|Mentioned|p653|||of Sydney basin.||||||
13874|Narrabeen Group|22857|5|Briefly described|p520 App.1 Tb.A1.9|Middle Triassic|Late Permian|Includes the Gosford, Clifton and Grose Subgroups. Correlative of Camden Haven Group. Geological Province: Sydney Basin. See also p530 App.1 Tb.A1.9.||||||
13874|Narrabeen Group|22892|5|Briefly described|p6 fig6||Triassic|||||||
13874|Narrabeen Group|22969|4|Described|p1, 25, 46||Early Triassic|||||||
13874|Narrabeen Group|22970|5|Briefly described|Plate 6||Triassic|||||||
13874|Narrabeen Group|23043|5|Briefly described|Map Legend|Early Triassic|Early Triassic|of Sydney Basin.||||||
13874|Narrabeen Group|23055|6|Mentioned|Fig4p11|||||||||
13874|Narrabeen Group|23170|2|Defined|p305|Triassic||In the Sydney Basin.||||||13-MAR-07
13874|Narrabeen Group|23214|5|Briefly described|p269|Early Triassic|Late Permian|Max. thickness 150m||||||
13874|Narrabeen Group|23218|5|Briefly described|Diagram p4, Map. p17|Permian|Permian|||||||
13874|Narrabeen Group|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
13874|Narrabeen Group|23256|6|Mentioned|p50|||||||||
13874|Narrabeen Group|23450|6|Mentioned|p527 Fig.1|||||||||
13874|Narrabeen Group|23540|5|Briefly described|Fig 1 p 418|||||||||
13874|Narrabeen Group|23881|5|Briefly described|p69 Fig. 7.2|||Includes Newport Fm., Bald Hill Claystone, Bulgo Sandstone, Stanwell Park Claystone, Scarborough Sandstone, Wombarra Shale and Coal Cliff Sandstone. Geological Province: Sydney Basin.||||||01-JUL-08
13874|Narrabeen Group|24079|5|Briefly described|p433|Triassic|Permian|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24083|6|Mentioned|p457|||Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24117|5|Briefly described|p3|||Geological Basin: Sydney Basin.||||||
13874|Narrabeen Group|24121|5|Briefly described|p4, p103, p227, 231|Triassic|Triassic|||||||25-AUG-22
13874|Narrabeen Group|24123|5|Briefly described|p3|Triassic|Triassic|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24126|5|Briefly described|p81|||||||||
13874|Narrabeen Group|24158|5|Briefly described|p172 Fig.3, p173 Fig.4|Triassic|Triassic|Unconformably overlies Newcastle Coal Measures. Geological Province: Sydney Basin||||||
13874|Narrabeen Group|24240|5|Briefly described|p20|Early Triassic|Early Triassic|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24342|5|Briefly described|p51|Early Triassic|Early Triassic|Overlying unit: Hawkesbury Sandstone, underlying unit: Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24423|5|Briefly described|p230 Fig.3||Late Permian|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|24471|5|Briefly described|p29 Fig.2|Triassic|Late Permian|Overlies Lawrence Sandstone. Overlain by Hawkesbury Sandstone. Geological Province: Sydney Basin.||||||07-FEB-11
13874|Narrabeen Group|29361|5|Briefly described|p4|||||||||
13874|Narrabeen Group|29376|6|Mentioned|p435|||||||||
13874|Narrabeen Group|29591|5|Briefly described|p97|||||||||
13874|Narrabeen Group|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
13874|Narrabeen Group|29745|6|Mentioned|p7|||||||||
13874|Narrabeen Group|29749|4|Described|p15|||||||||
13874|Narrabeen Group|29826|6|Mentioned|p18|||||||||
13874|Narrabeen Group|29901|4|Described|Table 1|||||||||
13874|Narrabeen Group|29915|6|Mentioned|p68|||||||||
13874|Narrabeen Group|29922|6|Mentioned|p49|||||||||
13874|Narrabeen Group|29924|6|Mentioned|p13|||||||||
13874|Narrabeen Group|29926|6|Mentioned|p3|||||||||
13874|Narrabeen Group|29942|6|Mentioned|p11|||||||||
13874|Narrabeen Group|29943|6|Mentioned|p39|||||||||
13874|Narrabeen Group|29944|6|Mentioned|Fig.18|||||||||
13874|Narrabeen Group|29993|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|30006|4|Described|p51|||||||||
13874|Narrabeen Group|30007|6|Mentioned|p61|||||||||
13874|Narrabeen Group|30109|6|Mentioned|Fig.1|||Triassic age.||||||
13874|Narrabeen Group|30132|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|30135|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|30228|6|Mentioned|p17|||Triassic age. Lithology||||||
13874|Narrabeen Group|30229|4|Described|p2020|||||||||
13874|Narrabeen Group|30286|6|Mentioned|p1069|||Refers McElroy(1969)||||||
13874|Narrabeen Group|30427|6|Mentioned|p39|||||||||
13874|Narrabeen Group|30455|6|Mentioned|p4|||Triassic age||||||
13874|Narrabeen Group|30460|6|Mentioned|p4|||See also P7,23||||||
13874|Narrabeen Group|30465|6|Mentioned|p5|||||||||
13874|Narrabeen Group|30466|6|Mentioned|p5|||Triassic age||||||
13874|Narrabeen Group|30545|6|Mentioned|p22|||Triassic. Correlated with Rewan Formation||||||
13874|Narrabeen Group|30547|6|Mentioned|p426|||Correlation||||||
13874|Narrabeen Group|30549|6|Mentioned|p26|||||||||
13874|Narrabeen Group|30555|6|Mentioned|Fig.21.2|||||||||
13874|Narrabeen Group|30565|6|Mentioned|p120|||||||||
13874|Narrabeen Group|30610|6|Mentioned|p326|||Refers Hind & Helby (1969)||||||
13874|Narrabeen Group|30707|6|Mentioned|p2|||Refers also Table 1||||||
13874|Narrabeen Group|30910|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|31057|6|Mentioned|p2|||||||||
13874|Narrabeen Group|31062|6|Mentioned|p478|||On Table. Triassic||||||
13874|Narrabeen Group|31128|5|Briefly described|p7|||||||||
13874|Narrabeen Group|31129|6|Mentioned|p125|||Includes Munmorah Congl.||||||
13874|Narrabeen Group|31276|6|Mentioned|p141|||Palynology. Refers Balme (1960)||||||
13874|Narrabeen Group|31296|6|Mentioned|p40|||||||||
13874|Narrabeen Group|31297|4|Described|p3|||See also p4-8. L. Triassic||||||
13874|Narrabeen Group|31326|6|Mentioned|p35|||Triassic||||||
13874|Narrabeen Group|31373|6|Mentioned|p176|||||||||
13874|Narrabeen Group|31375|6|Mentioned|p4|||Stratigraphy||||||
13874|Narrabeen Group|31426|4|Described|p65|||Triassic||||||
13874|Narrabeen Group|31549|6|Mentioned|p169|||Thickness control by synclinal subsidence||||||
13874|Narrabeen Group|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
13874|Narrabeen Group|31706|6|Mentioned|p671|||Correlation chart of Gondwana System||||||
13874|Narrabeen Group|31725|6|Mentioned|p6|||||||||
13874|Narrabeen Group|31726|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|31740|6|Mentioned|p13|||||||||
13874|Narrabeen Group|31855|6|Mentioned|p14|||Stratigraphic table||||||
13874|Narrabeen Group|31878|5|Briefly described|Table 1|||||||||
13874|Narrabeen Group|31879|5|Briefly described|p294|||Triassic.||||||
13874|Narrabeen Group|31885|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|31886|6|Mentioned|p394|||||||||
13874|Narrabeen Group|31887|5|Briefly described|p7|||||||||
13874|Narrabeen Group|31890|6|Mentioned|p77|||Stratigraphy||||||
13874|Narrabeen Group|32045|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|32047|6|Mentioned|p4|||||||||
13874|Narrabeen Group|32101|6|Mentioned|p107|||||||||
13874|Narrabeen Group|32187|5|Briefly described|p4|||||||||
13874|Narrabeen Group|32266|6|Mentioned|p24|||||||||
13874|Narrabeen Group|32267|6|Mentioned|p429|||||||||
13874|Narrabeen Group|32482|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|32485|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|32672|6|Mentioned|p675|||||||||
13874|Narrabeen Group|32719|6|Mentioned|p209|||Section||||||
13874|Narrabeen Group|32799|6|Mentioned|p8|||||||||
13874|Narrabeen Group|32800|6|Mentioned|p384|||Re palaeosols||||||
13874|Narrabeen Group|32801|6|Mentioned|p251|||||||||
13874|Narrabeen Group|32802|6|Mentioned|p19|||||||||
13874|Narrabeen Group|32803|6|Mentioned|p84|||||||||
13874|Narrabeen Group|32840|6|Mentioned|p16|||||||||
13874|Narrabeen Group|32849|6|Mentioned|p7|||Triassic||||||
13874|Narrabeen Group|32937|6|Mentioned|p54|||Geology||||||
13874|Narrabeen Group|32938|6|Mentioned|p67|||Geology||||||
13874|Narrabeen Group|32945|6|Mentioned|p82|||Permian||||||
13874|Narrabeen Group|32998|5|Briefly described|p111|||L.Trias. Gas discovery. See also P113||||||
13874|Narrabeen Group|33006|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
13874|Narrabeen Group|33129|6|Mentioned|p328|||||||||
13874|Narrabeen Group|33131|6|Mentioned|Fig.9|||||||||
13874|Narrabeen Group|33282|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|33285|5|Briefly described|p24|||Perm.-Trias.||||||
13874|Narrabeen Group|33334|6|Mentioned|p6|||||||||
13874|Narrabeen Group|33583|6|Mentioned|p9|||||||||
13874|Narrabeen Group|33676|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|33682|6|Mentioned|p22|||||||||
13874|Narrabeen Group|33683|3|Fully described|p77|||Triassic. See also PP78-88||||||
13874|Narrabeen Group|33685|6|Mentioned|Table 1|||Triassic||||||
13874|Narrabeen Group|33709|6|Mentioned|p103|||||||||
13874|Narrabeen Group|33867|4|Described|p11|||||||||
13874|Narrabeen Group|33869|6|Mentioned|Fig.2|||||||||
13874|Narrabeen Group|33873|6|Mentioned|p5|||||||||
13874|Narrabeen Group|33930|6|Mentioned|p15|||||||||
13874|Narrabeen Group|33986|6|Mentioned|p30|||Table||||||
13874|Narrabeen Group|34009|6|Mentioned|p108|||||||||
13874|Narrabeen Group|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
13874|Narrabeen Group|34020|6|Mentioned|p43|||See also P44||||||
13874|Narrabeen Group|34034|6|Mentioned|p554|||||||||
13874|Narrabeen Group|34037|6|Mentioned|Table 5.27|||||||||
13874|Narrabeen Group|34040|6|Mentioned|Fig.5.30|||Triassic||||||
13874|Narrabeen Group|34042|6|Mentioned|p399|||||||||
13874|Narrabeen Group|34043|6|Mentioned|p455|||||||||
13874|Narrabeen Group|34058|6|Mentioned|p395|||Triassic||||||
13874|Narrabeen Group|34059|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|34060|6|Mentioned|p24|||Triassic||||||
13874|Narrabeen Group|34106|6|Mentioned|p401|||||||||
13874|Narrabeen Group|34107|3|Fully described|p212|||||||||
13874|Narrabeen Group|34113|6|Mentioned|p67|||||||||
13874|Narrabeen Group|34121|6|Mentioned|p397|||See also PP397-399||||||
13874|Narrabeen Group|34139|6|Mentioned|p23|||||||||
13874|Narrabeen Group|34141|6|Mentioned|p7|||Triassic||||||
13874|Narrabeen Group|34157|6|Mentioned|p1|||Triassic.||||||
13874|Narrabeen Group|34158|6|Mentioned|p400|||||||||
13874|Narrabeen Group|34166|6|Mentioned|p59|||||||||
13874|Narrabeen Group|34172|6|Mentioned|p52|||||||||
13874|Narrabeen Group|34205|3|Fully described|p16|||Crook's subdivisions now further divided.||||||
13874|Narrabeen Group|34209|6|Mentioned|p137|||Triassic. See also PP141,142 etc.||||||
13874|Narrabeen Group|34236|6|Mentioned|p17|||||||||
13874|Narrabeen Group|34240|6|Mentioned|p395|||Triassic||||||
13874|Narrabeen Group|34241|4|Described|p404|||See also P405||||||
13874|Narrabeen Group|34242|6|Mentioned|p417|||||||||
13874|Narrabeen Group|34254|6|Mentioned|p488|||Late Permian - Middle Triassic||||||
13874|Narrabeen Group|34270|6|Mentioned|p254|||||||||
13874|Narrabeen Group|34283|6|Mentioned|Plate 6a|||Geomorphology||||||
13874|Narrabeen Group|34287|6|Mentioned|p153|||Triassic. See also PP154, 162, 172||||||
13874|Narrabeen Group|34301|6|Mentioned|p403|||||||||
13874|Narrabeen Group|34303|6|Mentioned|p15|||||||||
13874|Narrabeen Group|34331|6|Mentioned|p457|||Triassic||||||
13874|Narrabeen Group|34332|6|Mentioned|p19|||||||||
13874|Narrabeen Group|34336|3|Fully described|p388|||See also PP389-393. Triassic||||||
13874|Narrabeen Group|34337|4|Described|p393|||||||||
13874|Narrabeen Group|34338|6|Mentioned|p400|||||||||
13874|Narrabeen Group|34339|4|Described|p439|||Sedimentation||||||
13874|Narrabeen Group|34345|6|Mentioned|p331|||||||||
13874|Narrabeen Group|34351|6|Mentioned|p350|||Fig.5.13||||||
13874|Narrabeen Group|34398|6|Mentioned|p270|||Triassic||||||
13874|Narrabeen Group|34399|6|Mentioned|p312|||||||||
13874|Narrabeen Group|34400|5|Briefly described|p13|||Triassic.||||||
13874|Narrabeen Group|34429|4|Described|p66|||Triassic. Sections described. See also PP67-78.||||||
13874|Narrabeen Group|34434|6|Mentioned|Fig.5.25|||||||||
13874|Narrabeen Group|34437|4|Described|p405|||Macroflora & fauna. See PP406,407||||||
13874|Narrabeen Group|34444|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|34447|6|Mentioned|p315|||||||||
13874|Narrabeen Group|34448|5|Briefly described|p433|||||||||
13874|Narrabeen Group|34466|6|Mentioned|p351|||Triassic||||||
13874|Narrabeen Group|34467|6|Mentioned|p26|||||||||
13874|Narrabeen Group|34506|6|Mentioned|p408|||||||||
13874|Narrabeen Group|34547|6|Mentioned|p518|||Igneous fragmental material.||||||
13874|Narrabeen Group|34560|6|Mentioned|p23|||||||||
13874|Narrabeen Group|34561|6|Mentioned|p41|||||||||
13874|Narrabeen Group|34562|6|Mentioned|p60|||||||||
13874|Narrabeen Group|34585|6|Mentioned|p380|||Triassic||||||
13874|Narrabeen Group|34605|6|Mentioned|p375|||Fig.5.29||||||
13874|Narrabeen Group|34845|6|Mentioned|Fig.4|||||||||
13874|Narrabeen Group|35062|6|Mentioned|p278|||||||||
13874|Narrabeen Group|35280|6|Mentioned|p147|||||||||
13874|Narrabeen Group|35319|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|35416|6|Mentioned|p4|||Stratigraphy and palynological framework on Fig.2||||||
13874|Narrabeen Group|35488|6|Mentioned|p73|||||||||
13874|Narrabeen Group|35502|6|Mentioned|Fig.1|||Also on Table 1||||||
13874|Narrabeen Group|35524|6|Mentioned|Fig.2|||Stratigraphic sequence in southeastern part of Sydney Basin.||||||
13874|Narrabeen Group|35587|6|Mentioned|p46|||||||||
13874|Narrabeen Group|35647|6|Mentioned|p53|||||||||
13874|Narrabeen Group|35690|6|Mentioned|Fig.1.1|||See also P61.||||||
13874|Narrabeen Group|35762|6|Mentioned|p71|||||||||
13874|Narrabeen Group|35833|6|Mentioned|p35|||||||||
13874|Narrabeen Group|35873|6|Mentioned|p45|||||||||
13874|Narrabeen Group|35874|6|Mentioned|p1|||||||||
13874|Narrabeen Group|35878|6|Mentioned|p115|||||||||
13874|Narrabeen Group|35901|6|Mentioned|p4|||||||||
13874|Narrabeen Group|35914|6|Mentioned|p16|||||||||
13874|Narrabeen Group|36042|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|36045|6|Mentioned|p328|||||||||
13874|Narrabeen Group|36058|5|Briefly described|p4|||||||||
13874|Narrabeen Group|36069|6|Mentioned|p23|||||||||
13874|Narrabeen Group|36121|6|Mentioned|p25|||||||||
13874|Narrabeen Group|36147|6|Mentioned|Fig.2|||||||||
13874|Narrabeen Group|36148|6|Mentioned|p266|||||||||
13874|Narrabeen Group|36151|6|Mentioned|Table 1B|||||||||
13874|Narrabeen Group|36220|4|Described|p64|||See also Table 20.||||||
13874|Narrabeen Group|36222|6|Mentioned|Map legend|Late Triassic|Late Permian|Late Permian to Late Triassic||||||
13874|Narrabeen Group|36223|6|Mentioned|Map legend|Late Triassic|Late Permian|Late Permian to Late Triassic||||||
13874|Narrabeen Group|36390|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|36391|6|Mentioned|p156|||||||||
13874|Narrabeen Group|36593|6|Mentioned|p188|||See also Fig.2.||||||
13874|Narrabeen Group|36594|6|Mentioned|Table 1|||See also Table II.||||||
13874|Narrabeen Group|36601|6|Mentioned|p73|||||||||
13874|Narrabeen Group|36612|6|Mentioned|Fig.2|||||||||
13874|Narrabeen Group|36616|6|Mentioned|p4|||||||||
13874|Narrabeen Group|36751|6|Mentioned|p312|||||||||
13874|Narrabeen Group|36825|6|Mentioned|p21|||||||||
13874|Narrabeen Group|36899|6|Mentioned|p1085|||See also P1092.||||||
13874|Narrabeen Group|36901|6|Mentioned|p16|||||||||
13874|Narrabeen Group|36940|6|Mentioned|p146|||||||||
13874|Narrabeen Group|36961|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|37082|6|Mentioned|p161|||||||||
13874|Narrabeen Group|37083|6|Mentioned|p164|||||||||
13874|Narrabeen Group|37084|6|Mentioned|Fig.1|||||||||
13874|Narrabeen Group|37086|6|Mentioned|p183|||||||||
13874|Narrabeen Group|37087|5|Briefly described|p198|||||||||
13874|Narrabeen Group|37089|5|Briefly described|p208|||||||||
13874|Narrabeen Group|37091|5|Briefly described|p226|||||||||
13874|Narrabeen Group|37093|5|Briefly described|p231|||||||||
13874|Narrabeen Group|37094|6|Mentioned|p243|||||||||
13874|Narrabeen Group|37168|6|Mentioned|Fig.2|||||||||
13874|Narrabeen Group|37319|6|Mentioned|p606|||||||||
13874|Narrabeen Group|37322|6|Mentioned|p723|||||||||
13874|Narrabeen Group|37346|6|Mentioned|p44|||||||||
13874|Narrabeen Group|37561|6|Mentioned|p101|||||||||
13874|Narrabeen Group|37722|6|Mentioned|p23|||||||||
13874|Narrabeen Group|37730|6|Mentioned|p18|||||||||
13874|Narrabeen Group|37804|6|Mentioned|p55|||||||||
13874|Narrabeen Group|37812|6|Mentioned|p656|||||||||
13874|Narrabeen Group|38064|5|Briefly described|p41|||||||||
13874|Narrabeen Group|38358|6|Mentioned|p6|||||||||
13874|Narrabeen Group|38375|6|Mentioned|p547|||||||||
13874|Narrabeen Group|38575|6|Mentioned|p107|||||||||
13874|Narrabeen Group|38603|6|Mentioned|p83|||||||||
13874|Narrabeen Group|38615|5|Briefly described|p18|||||||||
13874|Narrabeen Group|38656|6|Mentioned|Fig.1.5.12|||P279||||||
13874|Narrabeen Group|38784|6|Mentioned|p78|||||||||
13874|Narrabeen Group|38820|6|Mentioned|p182|||||||||
13874|Narrabeen Group|38951|6|Mentioned|p409|||||||||
13874|Narrabeen Group|39214|6|Mentioned|p29|||Triassic||||||
13874|Narrabeen Group|39232|6|Mentioned|p110|||See also P111||||||
13874|Narrabeen Group|39287|6|Mentioned|Fig.2.5|||||||||
13874|Narrabeen Group|39288|6|Mentioned|p64|||||||||
13874|Narrabeen Group|39292|6|Mentioned|Fig.6.1|||See also Fig.6.2||||||
13874|Narrabeen Group|39293|3|Fully described|p141|||Analysis of redbeds Table 8.1, 8.2. See also Figs 8.9, 8.10, 8.11||||||
13874|Narrabeen Group|39294|4|Described|p163|||Lower Narrabeen Gp. See also PP163-168||||||
13874|Narrabeen Group|39295|4|Described|p171|||Uppermost unit only||||||
13874|Narrabeen Group|39296|6|Mentioned|p179|||||||||
13874|Narrabeen Group|39300|6|Mentioned|p313|||||||||
13874|Narrabeen Group|39306|6|Mentioned|p387|||See also P405,408,411,414,417||||||
13874|Narrabeen Group|39307|6|Mentioned|Table 22.1|||See Table 22.1||||||
13874|Narrabeen Group|39308|5|Briefly described|p454|||See also PP493 & 501||||||
13874|Narrabeen Group|39309|6|Mentioned|p132|||||||||
13874|Narrabeen Group|39356|6|Mentioned|p226|||||||||
13874|Narrabeen Group|39450|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|39467|6|Mentioned|Fig.1|||||||||
13874|Narrabeen Group|39609|6|Mentioned|Table 1|||||||||
13874|Narrabeen Group|39661|6|Mentioned|p443|||||||||
13874|Narrabeen Group|39666|6|Mentioned|p57|||||||||
13874|Narrabeen Group|39757|6|Mentioned|p1601|||||||||
13874|Narrabeen Group|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
13874|Narrabeen Group|40224|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
13874|Narrabeen Group|40245|6|Mentioned|p187|||||||||
13874|Narrabeen Group|40256|6|Mentioned|p301|||||||||
13874|Narrabeen Group|40268|6|Mentioned|Fig.1a|||||||||
13874|Narrabeen Group|40516|6|Mentioned|p382|||||||||
13874|Narrabeen Group|40526|6|Mentioned|p150|||||||||
13874|Narrabeen Group|40602|4|Described|p9|||||||||
13874|Narrabeen Group|40603|6|Mentioned|p4|||||||||
13874|Narrabeen Group|40625|6|Mentioned|Map legend|Middle Triassic|Late Permian|Late Permian to Middle Triassic||||||
13874|Narrabeen Group|40629|4|Described|p185|||||||||
13874|Narrabeen Group|40630|6|Mentioned|p173|||||||||
13874|Narrabeen Group|40631|6|Mentioned|p160|||||||||
13874|Narrabeen Group|40636|6|Mentioned|p43|||||||||
13874|Narrabeen Group|40650|6|Mentioned|Table 7|||||||||
13874|Narrabeen Group|40651|6|Mentioned|Table 6|||||||||
13874|Narrabeen Group|40652|6|Mentioned|p127|||||||||
13874|Narrabeen Group|40653|6|Mentioned|p121|||||||||
13874|Narrabeen Group|40654|6|Mentioned|p117|||||||||
13874|Narrabeen Group|40655|6|Mentioned|p41|||||||||
13874|Narrabeen Group|40744|6|Mentioned|p326|||||||||
13874|Narrabeen Group|40806|6|Mentioned|p150|||||||||
13874|Narrabeen Group|40999|6|Mentioned|Fig.1|||||||||
13874|Narrabeen Group|41010|4|Described|p17|||||||||
13874|Narrabeen Group|41195|6|Mentioned|p325|||||||||
13874|Narrabeen Group|41290|6|Mentioned|Fig.8|||||||||
13874|Narrabeen Group|41299|6|Mentioned|p118|||||||||
13874|Narrabeen Group|41348|5|Briefly described|Map legend|Triassic|Permian|Polymictic conglomerate, lithic sandstone, silty sandstone, and mudstone.||||||16-DEC-04
13874|Narrabeen Group|41463|6|Mentioned|Fig.1|||||||||
13874|Narrabeen Group|41473|6|Mentioned|p47|||||||||
13874|Narrabeen Group|41476|6|Mentioned|p75|||||||||
13874|Narrabeen Group|41479|6|Mentioned|Fig.2|||||||||
13874|Narrabeen Group|41639|6|Mentioned|p9|||||||||
13874|Narrabeen Group|41658|6|Mentioned|p545|||||||||
13874|Narrabeen Group|41718|4|Described|p237|||||||||
13874|Narrabeen Group|41834|6|Mentioned|p590|||||||||
13874|Narrabeen Group|41902|5|Briefly described|p5 Table 1|||||||||
13874|Narrabeen Group|41903|6|Mentioned|Map legend|Early Triassic||||||||
13874|Narrabeen Group|42008|6|Mentioned|p270|||||||||
13874|Narrabeen Group|42078|6|Mentioned|p4|||||||||
13874|Narrabeen Group|42091|6|Mentioned|Text fig.2 P284|||||||||
13874|Narrabeen Group|42171|6|Mentioned|p141|||||||||
13874|Narrabeen Group|42214|6|Mentioned|p460|||||||||
13874|Narrabeen Group|42287|6|Mentioned|p14|||||||||
13874|Narrabeen Group|42349|5|Briefly described|p65|||||||||
13874|Narrabeen Group|42378|6|Mentioned|p19|||||||||
13874|Narrabeen Group|42648|6|Mentioned|p33|||||||||
13874|Narrabeen Group|42656|6|Mentioned|p67|||||||||
13874|Narrabeen Group|42657|5|Briefly described|p73|||||||||
13874|Narrabeen Group|42663|6|Mentioned|Table 2 P11|||||||||
13874|Narrabeen Group|42737|5|Briefly described|map legend|Triassic||||||||
13874|Narrabeen Group|42767|5|Briefly described|Fig.5|||||||||
13874|Narrabeen Group|42780|5|Briefly described|p411, Fig.2 p412|||||||||
13874|Narrabeen Group|42787|6|Mentioned|Table 1 P126|||||||||
13874|Narrabeen Group|42795|5|Briefly described|Fig.2 P23|||||||||
13874|Narrabeen Group|42821|5|Briefly described|p90|||||||||
13874|Narrabeen Group|42896|3|Fully described|p25, Table 2|||see also Fig.5||||||
13874|Narrabeen Group|42916|5|Briefly described|Table 1||Early Triassic|||||||
13874|Narrabeen Group|42925|4|Described|p7|||see also Table 1||||||
13874|Narrabeen Group|42926|4|Described|map legend|Middle Triassic|Late Permian|||||||
13874|Narrabeen Group|42947|5|Briefly described|p41|||||||||
13874|Narrabeen Group|42948|6|Mentioned|p50|||||||||
13874|Narrabeen Group|43016|5|Briefly described|p366|||||||||
13874|Narrabeen Group|43017|5|Briefly described|Fig.1,p372|||||||||
13874|Narrabeen Group|43028|6|Mentioned|p617|||||||||
13874|Narrabeen Group|43044|5|Briefly described|p123|||||||||
13874|Narrabeen Group|43072|6|Mentioned|p78|||||||||
13874|Narrabeen Group|43146|6|Mentioned|Fig.2 p41|||||||||
13874|Narrabeen Group|43194|5|Briefly described|p129 Tb. 8.3, p130, p131|Triassic|Triassic|Sydney Basin. Equivalent to the Digby, Napperby and Deriah Formations in the Gunnedah Basin.||||||
13874|Narrabeen Group|43257|5|Briefly described|Map Legend|Middle Triassic|Late Permian|||||||
13874|Narrabeen Group|43263|6|Mentioned|Map Legend||Triassic|||||||
13874|Narrabeen Group|43317|4|Described|Table 1 p10|||||||||
13874|Narrabeen Group|43318|14|Not recorded|p73|||Contains marine organisms, See also Lexicon||||||
13874|Narrabeen Group|43319|14|Not recorded|Map Legend|||||||||
13874|Narrabeen Group|43320|14|Not recorded|Table 1 p5,10||Triassic|p16,17,20,25-31||||||
13874|Narrabeen Group|43322|14|Not recorded|p7-9|||SI 56-5 Broken Bay||||||
13874|Narrabeen Group|43323|14|Not recorded|p61,63,66,71|||Microflora||||||
13874|Narrabeen Group|43324|14|Not recorded|p18,19||Triassic|||||||
13874|Narrabeen Group|43338|14|Not recorded|p117||Triassic|||||||
13874|Narrabeen Group|43339|14|Not recorded|p6-7||Triassic|||||||
13874|Narrabeen Group|43341|14|Not recorded|p119|||||||||
13874|Narrabeen Group|43342|14|Not recorded|Table 1 p107|||||||||
13874|Narrabeen Group|43343|14|Not recorded|p119|||||||||
13874|Narrabeen Group|43344|14|Not recorded|p13,18,20,21,33-36,|||47,51-55,63,66-73,77,85,175,186||||||
13874|Narrabeen Group|43345|14|Not recorded|p3,5,6|||||||||
13874|Narrabeen Group|43346|2|Defined|p2,4 Map|||||||||
13874|Narrabeen Group|43349|14|Not recorded|Map|||||||||
13874|Narrabeen Group|43350|14|Not recorded|p 389,399|||||||||
13874|Narrabeen Group|43352|14|Not recorded|p 209-223||Triassic|||||||
13874|Narrabeen Group|43354|14|Not recorded|p105-108,p106|||||||||
13874|Narrabeen Group|43355|14|Not recorded|Map Legend||Triassic|Provisional Edition||||||
13874|Narrabeen Group|43356|14|Not recorded|Map Legend||Triassic|||||||
13874|Narrabeen Group|43357|14|Not recorded|155-161|Early Ordovician||||||||
13874|Narrabeen Group|43359|14|Not recorded|Map Legend||Triassic|Provisional first edition||||||
13874|Narrabeen Group|43360|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
13874|Narrabeen Group|43361|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
13874|Narrabeen Group|43362|14|Not recorded|Map Legend||Triassic|(Provisional first edition)||||||
13874|Narrabeen Group|43363|14|Not recorded|Map Legend|||(Provisional first edition)||||||
13874|Narrabeen Group|43370|14|Not recorded|p1,4|||||||||
13874|Narrabeen Group|43376|14|Not recorded|p149|||||||||
13874|Narrabeen Group|43378|14|Not recorded|p141|||||||||
13874|Narrabeen Group|43383|14|Not recorded|Fig.5, p22-24||Triassic|||||||
13874|Narrabeen Group|43384|14|Not recorded|Map Legend||Triassic|||||||
13874|Narrabeen Group|43385|14|Not recorded|p181,182||Triassic|(L.Brunker)Ref.to Lovering 1954||||||
13874|Narrabeen Group|43395|14|Not recorded|p61-63,67,74,map,76||Early Triassic|||||||
13874|Narrabeen Group|43405|14|Not recorded|Map Legend||Triassic|(Provisional Edition)||||||
13874|Narrabeen Group|43407|14|Not recorded|Map Legend||Triassic|(Provisional Edition)||||||
13874|Narrabeen Group|43414|14|Not recorded|p15|||||||||
13874|Narrabeen Group|43420|14|Not recorded|p282|||||||||
13874|Narrabeen Group|43440|14|Not recorded|p34,86,71|||||||||
13874|Narrabeen Group|43447|14|Not recorded|Tbl 1,p15,diag,26,||Triassic|p28,29||||||
13874|Narrabeen Group|43448|14|Not recorded|p221,224|||||||||
13874|Narrabeen Group|43449|14|Not recorded|p11;opp 12;Pl 2|||||||||
13874|Narrabeen Group|43451|14|Not recorded|Map Legend|||||||||
13874|Narrabeen Group|43476|14|Not recorded|Map Legend||Triassic|(Provisional Edition)||||||
13874|Narrabeen Group|43477|14|Not recorded|p27|||||||||
13874|Narrabeen Group|43479|14|Not recorded|p225|Middle Triassic|Early Triassic|||||||
13874|Narrabeen Group|43491|14|Not recorded|pVIII/11a|||||||||
13874|Narrabeen Group|43494|5|Briefly described|p12|Triassic|Triassic|Forms low cliffs of quartz pebble conglomerate and coarse quartz sandstone. Overlies Illawarra C.M.||||||16-MAR-06
13874|Narrabeen Group|43515|14|Not recorded|Map Legend||Triassic|(Provisional Edition)||||||
13874|Narrabeen Group|43516|14|Not recorded|Map Legend||Triassic|||||||
13874|Narrabeen Group|43637|6|Mentioned|Fig.2,p18|||||||||
13874|Narrabeen Group|43641|5|Briefly described|Map Legend||Triassic|||||||
13874|Narrabeen Group|43731|6|Mentioned|p89||Early Triassic|||||||
13874|Narrabeen Group|43782|5|Briefly described|Map Legend||Triassic|||||||
13874|Narrabeen Group|43873|14|Not recorded|p53|||||||||
13874|Narrabeen Group|43875|14|Not recorded|p59|||||||||
13874|Narrabeen Group|43881|14|Not recorded|p73|||Contains marine organisms. See also Lexicon||||||
13874|Narrabeen Group|43885|14|Not recorded|p419|||||||||
13874|Narrabeen Group|43895|4|Described|p116,117|||||||||
13874|Narrabeen Group|43918|14|Not recorded|p65,76|||||||||
13874|Narrabeen Group|43919|14|Not recorded|p37,41|||||||||
13874|Narrabeen Group|43980|14|Not recorded|p3-4,opp.1,Pl.1|||Gas found in Mulgoa no.2 well.||||||
13874|Narrabeen Group|44004|2|Defined|p18|||||||||
13874|Narrabeen Group|44005|14|Not recorded|p26,opp.23,Pl.4|||||||||
13874|Narrabeen Group|44093|5|Briefly described|p22 (photo)|Triassic|Triassic|Narrabeen Group sandstones resting on Permian coal measures and marine sediments.||||||
13874|Narrabeen Group|44244|6|Mentioned|p290 Tb.5|Triassic|Permian|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
13874|Narrabeen Group|44426|14|Not recorded|p12|||"A correlation between the Rewan Formation and the Narrabeen Group...is indicated."||||||
13874|Narrabeen Group|44450|5|Briefly described|p147 Fig 43|Early Triassic|Late Permian|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|44507|14|Not recorded|p103,106|||||||||
13874|Narrabeen Group|44607|14|Not recorded|p38|||||||||
13874|Narrabeen Group|44608|14|Not recorded|p19|||Middle part equivalent to Pickanjinnie Formation.||||||
13874|Narrabeen Group|44610|14|Not recorded|p47,49|||||||||
13874|Narrabeen Group|44668|14|Not recorded|p60|||||||||
13874|Narrabeen Group|44834|14|Not recorded|p475|||||||||
13874|Narrabeen Group|44855|14|Not recorded|p18|Late Triassic|Middle Triassic|||||||
13874|Narrabeen Group|44861|14|Not recorded|p181,188,226,258|||||||||
13874|Narrabeen Group|44998|14|Not recorded|p104|||Correlated with Erskine Sandstone & Blina Shale, Canning Basin.||||||
13874|Narrabeen Group|45018|14|Not recorded|p186|||||||||
13874|Narrabeen Group|45071|6|Mentioned|p77|||||||||
13874|Narrabeen Group|45090|6|Mentioned|p27|||Relationship of rock units||||||
13874|Narrabeen Group|45095|6|Mentioned|p38|||Refers Lassak & Golding (1967) & Sagittarius Sst.||||||
13874|Narrabeen Group|45138|6|Mentioned|p3|||||||||
13874|Narrabeen Group|45150|6|Mentioned|p4|||||||||
13874|Narrabeen Group|46849|6|Mentioned|p195|||||||||
13874|Narrabeen Group|48926|6|Mentioned|p9|||P9 et seq.||||||
13874|Narrabeen Group|48995|6|Mentioned|p19|||||||||
13874|Narrabeen Group|49644|5|Briefly described|Table|||||||||
13874|Narrabeen Group|50116|5|Briefly described|p66 Fig.2|Triassic|Triassic|Overlies the Illawarra Coal Measures. Geological Province: Sydney-Gunnedah Basin.||||||
13874|Narrabeen Group|60281|6|Mentioned|p9, p59, Fig. 15 App. 1|Middle Triassic|Early Triassic|Lithic conglomerate, quartz-lithic sandstone, and red, green and grey shale. Four subgroups: Grose and Caley in west; Gosford and Clifton in south.  Overlain by Hawkesbury Sst. Geol.Prov: Sydney Basin.||||||27-APR-05
13874|Narrabeen Group|60297|6|Mentioned|p168 Fig.1, p177|Permian|Permian|||||||
13874|Narrabeen Group|60300|5|Briefly described|p241|Triassic|Triassic|Sedimentary.||||||
13874|Narrabeen Group|60386|6|Mentioned|p296||Early Triassic|Bowen/Sydney Basin. Non-marine.||||||
13874|Narrabeen Group|60991|6|Mentioned|p40 |Early Triassic|Early Triassic|Sydney Basin. Contains Lepidopteris leaves.||||||
13874|Narrabeen Group|61315|5|Briefly described|p167, Table SY1|Middle Triassic|Early Triassic|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|61529|5|Briefly described|p853, p854 Fig. 1b|Triassic|Triassic|Geological Province: Sydney Basin.||||||
13874|Narrabeen Group|61610|4|Described|p252, p252 Fig. 2, p254-255, p257-259|Early Triassic|Early Triassic|Thickness: 90-700m. Geological Province: Sydney Basin. Comprises conglomerates, sandstones and shales deposited in a fluviatile, fluviatile-deltaic and lacustrine environments.||||||07-FEB-11
13874|Narrabeen Group|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
13874|Narrabeen Group|61772|6|Mentioned|p131, p132, p133|||||||||
13874|Narrabeen Group|62033|5|Briefly described|p25 (Table)|||Geological Province: Sydney Basin.||||||14-MAR-07
13874|Narrabeen Group|62921|6|Mentioned|p877|Early Triassic|Early Triassic|Sydney Basin. Contains stereospondyls (Tetrapoda, Temnospondyli).||||||
13874|Narrabeen Group|63868|5|Briefly described|p26|||Includes the Collaroy Claystone. In NSW.||||||07-FEB-11
13874|Narrabeen Group|63978|5|Briefly described|p7|||Geological province: Sydney Basin.||||||07-FEB-11
13874|Narrabeen Group|65195|6|Mentioned|p3, p4 Fig.2, p15, p17, p21, p30|Triassic|Permian|Contains Banks Wall Sandstone and Burralow Formation. One of the most exposed units in the Lapstone Structural Complex.||||||
13874|Narrabeen Group|65490|5|Briefly described|p 874, Fig. 1 p875|Middle Triassic|Early Triassic|Sedimentary unit of the Sydney Basin. Cut by faults dating between ~163 and 120 Ma, and reactivated post 51 Ma. See p882-883 for age discussion.||||||
13874|Narrabeen Group|65492|5|Briefly described|p889, p890 Fig. 1, p892, 894, 896, 899|Triassic|Triassic|Sydney Basin, overlain by the Hawkesbury Sandstone. Includes litharenite.||||||06-MAY-11
13874|Narrabeen Group|65758|5|Briefly described|p98|Triassic|Triassic|Sydney Basin. Overlies Wittingham Coal Measures. Sandstone and shale||||||
13874|Narrabeen Group|66577|6|Mentioned|pp995-997.|Triassic|Triassic|Lower part of this unit is deltaic; the upper part is fluvial.|||Includes Wombarra, Stanwell Park, Bald Hill Claystones; Scarborough, Bulgo Sandstones; Garie, Newport Formations.|Overlies Illawarra Coal Measures. Is overlain by Hawkesbury Sandstone.||
13874|Narrabeen Group|66891|5|Briefly described|p179, p180, p183, p184, pp190-191.|Early Triassic|Early Triassic|This unit is the source of Quaternary alluvium further from the Wybong Creek channel and adjacent to the valley escarpments. Low to moderate salinity groundwater in the Wybong Creek catchment had been attributed to chemical weathering of this unit. The occurrence of saline water in specific bores in this unit is attributed to point source groundwater discharge via fractures and/or faults connected to the Wittingham Coal Measures.||||Overlies Newcastle Coal Measures.||
13874|Narrabeen Group|67560|5|Briefly described|p258-272|Triassic|Triassic|Hanlon et al. (1954). ~623m thick in Eveleigh No.1 DDH. Sydney Basin. Magnetic susceptibility, mass properties, relative paleosalinity, gamma, velocity and resistivity properties detailed. Misnamed as Narrabeen Sandstone Group on p264, immediately after a mention of Hawkesbury Sandstone.|||Includes Coalcliff Sandstone, Wombarra Shale, Scarborough Sandstone, Stanwell Park Claystone, Bulgo Sandstone, Bald Hill Claystone, Garie Formation, Newport Formation.|Overlain by the Hawkesbury Sandstone. Underlain by the Illawarra Coal Measures.||23-MAY-17
13874|Narrabeen Group|67663|5|Briefly described|p519 Fig.1, p520-522|Triassic|Triassic|Approximately 800m thick. Deposition in estuarine/alluvial, fluvial, and fluvial-deltaic environments.||||Unconformably overlain by the Hawkesbury Sandstone. Unconformably overlies Illawarra Coal Measures, Newcastle Coal Measures, Singleton Supergroup.|Lithic conglomerate, quartz-lithic sandstone, and shale (red, green and grey).|
13874|Narrabeen Group|67786|6|Mentioned|p96|Triassic|Triassic|Newcastle Coalfield, Sydney Basin.||||Overlies Newcastle Coal Measures. Is overlain by Hawkesbury Sandstone.||
13874|Narrabeen Group|68003|5|Briefly described|p38 Fig.3-j, p42, p43, p130.|Middle Triassic|Early Triassic|Hunter and Western Coalfields, Brigalow Belt South Bioregion. Correlative of Digby Formation (Gunnedah Basin).|||Includes Munmorah Conglomerate, Newport and Terrigal Formations, Bald Hill Claystone and Wentworth Falls Claystone Member.|Overlies Wollombi Coal Measures and Murulla beds. Is overlain by Wianamatta Group.|Pebbly lithic-quartz to quartz sandstone, red-brown to green mudstone, sporadic lenses of quartz paraconglomerate.|
13874|Narrabeen Group|68004|5|Briefly described|p23 Table 1. |Triassic|Triassic|Sydney Basin.|||Includes Terrigal and Newport Formations.|Overlies Singleton Supergroup; Wollombi, Newcastle and Illawarra Coal Measures; Wallerawang and Sydney Subgroups. Is overlain by Napperby Formation.|Poorly-sorted volcanic-lithic pebble conglomerate overlain by coarse- to fine-grained quartz-lithic and then quartzose sandstone.|
13874|Narrabeen Group|68202|5|Briefly described|p176|Early Triassic|Early Triassic|Sydney Basin. Lacustrine, fluvial and floodplain deposits from the New England Fold Belt. The authors conclude that the Permian-Triassic mass exinction event is recorded ~1m above the Bulli Coal, i.e. in the basal shales of the Narrabeen Group.|||Wombarra Claystone; Coal Cliff, Otford, Scarborough Sandstones.|||
13874|Narrabeen Group|68493|6|Mentioned|p3 Fig.1, p5 Fig.2|Early Triassic|Early Triassic|Sydney Basin. Alluvial fan, alluvial plain, and estuarine-shallow marine.
Numerical age given is the Permo-Triassic boundary age in 2011, from the Subcommission on Permian stratigraphy.|252.16 Ma at base.|||Overlies Newcastle Coal Measures.|Conglomerate, sandstone, siltstone, claystone.|
13874|Narrabeen Group|68711|5|Briefly described|p116 Tbl 2|||Boundary with Newcastle Coal Measures modified. Boundary now above the uppermost coal, usually the Vales Point seam.||||Overlies Moon Island Beach Formation, Newcastle Coal Measures.||
13874|Narrabeen Group|69297|6|Mentioned|p403, p418, p434, p435, p501, p504|Anisian|Induan|Sydney Basin. Sandstones of this group are good potential hydrocarbon reservoirs. Claystones within this group may form seals to the underlying Triassic sandstones.|||Includes the Caley Subgroup, Grose Subgroup, Burralow Formation, Clifton Subgroup and the Gosford Subgroup.|Unconformably overlies the Illawarra Coal Measures. Overlain by the Hawkesbury Sandstone.||
13874|Narrabeen Group|69683|6|Mentioned|p410 Fig.1, p411 Fig.2, p412|Triassic|Triassic|Maximum thickness of 800m used in modelling in this study.||||||
13874|Narrabeen Group|69877|6|Mentioned|p379|Early Triassic|Early Triassic|Similar flora to Ross Formation and correlates in Tasmania.||||||
13874|Narrabeen Group|70036|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Included in a mapped unit of fluvial and lacustrine sequences: conglomerate, quartzose and lithic sandstone, siltstone and mudstone.||||||
13874|Narrabeen Group|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Triassic|Early Triassic|Erosional base. Sydney Basin.||||Overlies Illawarra Coal Measures.|Quartz-lithic to quartzose sandstone, conglomerate, mudstone, siltstone. Fluvial origin.|
13874|Narrabeen Group|70587|5|Briefly described|Map Legend|Triassic|Triassic||||||Quartz lithic to quartzose sandstone, conglomerate, mudstone, siltstone; rare coal.|
13874|Narrabeen Group|70647|5|Briefly described|Map Legend|Middle Triassic|Late Permian|Sydney Basin.|||Includes Gosford Subgroup, Clifton Subgroup.|||
13874|Narrabeen Group|70661|3|Fully described|p193-p197|Early Triassic|Late Permian|Name derived from the suburb of Narrabeen. Previously referred to as Narrabeen beds or Narrabeen Shales. Contains many more constituent units, however only two are named in this study. Forms cliffs in the map area. Distribution, distinguishing characteristics, structure, metamorphism and fossil assemblage discussed. Estimated 50m thick in map area, may be up to 700m thick elsewhere. Type section mentioned. Deposited in a fluvial to lacustrine environment with some shallow marine horizons present. Age derived from palynomorphs, plant macrofossils and vertebrates. Has some potential as a reservoir rock.|||Kangaloon Sandstone, Bald Hill Claystone|Locally unconformably overlies the Illawarra Coal Measures, conformably (or disconformably) overlain by Hawkesbury Sandstone, equivalent to the Digby Formation|lithic quartz sandstone, claystone, shale and minor conglomerate. Massive to laminated, medium to fine grained, lithic quartz sandstone with intercalated thin bedded grey siltstone.|
13874|Narrabeen Group|70777|6|Mentioned|p8|Triassic|Triassic|New England Orogen.||||||
13874|Narrabeen Group|70791|5|Briefly described|p277|Middle Triassic|Early Triassic|Hunter Coalfield.||||||
13874|Narrabeen Group|70878|5|Briefly described|p710, p712, p726|Triassic|Triassic|Sydney Basin.|||Digby Formation.|Overlies Newcastle Coal Measures.||
13874|Narrabeen Group|71115|6|Mentioned|p178|||Sydney Basin.||||Overlies Illawarra Coal Measures.|Includes chocolate shales.|
13874|Narrabeen Group|71303|5|Briefly described|map legend|Early Triassic|Early Triassic|Of Sydney Basin.|||None recognised on this map.||Lithic quartz sandstone with intercalated thinly bedded grey siltstone. Sandstone massive to laminated, mostly medium to fine-grained. Basal pebbly conglomerate locally.|
13874|Narrabeen Group|73146|5|Briefly described|p15|||Sydney Basin. Has magnetic overprinting with a uniformly normal polarity and steep inclination.|||||Red claystones and less oxidised grey and green shales and sandstones.|
13874|Narrabeen Group|73248|6|Mentioned|p301, p309|Middle Triassic|Early Triassic|Exposed by entrenched rivers in the Woronora Plateau.||||Conformably underlain by Illawarra Coal Measures. Overlain by Hawkesbury Sandstone.|Sandstone and claystone.|14-FEB-23
13874|Narrabeen Group|73264|6|Mentioned|p1402 Fig.23, p1404|Triassic|Triassic|Sydney Basin. Derived from New England Orogen.||||||
13874|Narrabeen Group|73304|6|Mentioned|p61, p71, p73-75, p78-79|||Sydney Basin. [Basal?] boundary marks a major extinction of peat-producing plants. Also contains the Induan-Olenkian boundary.|||Newport Formation, Garie Formation, Bald Hill Claystone, Bulgo Sandstone, Stanwell Park Claystone, Scarborough Sandstone, Wombarra Claystone, Coal Cliff Sandstone|||
13874|Narrabeen Group|73421|6|Mentioned|p3, p16|Triassic|Triassic|Sydney Basin, southern. Misspelt as Narabeen p3.||||Overlies Illawarra Coal Measures, Eckersley Formation|Includes conglomerate with cross bedding.|
13874|Narrabeen Group|73570|6|Mentioned|p916|||Sydney Basin.|||Terrigal Formation|||
13874|Narrabeen Group|73625|6|Mentioned|p2|Early Triassic|Early Triassic|Sydney Basin.||||Overlies Illawarra Coal Measures.||
13874|Narrabeen Group|75059|6|Mentioned|p10|Middle Triassic|Early Triassic|Sydney Basin.||||||
13890|Narraburra Granite|22638|4|Described|p73||Late Devonian|New name.||||||
13890|Narraburra Granite|24101|6|Mentioned|p110 Fig.3|||Geological Province: Lachlan Fold Belt||||||
13890|Narraburra Granite|41320|4|Described|p211|||||||||
13890|Narraburra Granite|42726|5|Briefly described|map legend|Late Devonian||||||||
13890|Narraburra Granite|44192|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
13890|Narraburra Granite|44936|5|Briefly described|Map Legend||Late Devonian|||||||
13890|Narraburra Granite|60423|6|Mentioned|p372|||Geological Province: Lachlan Fold Belt.||||||
13890|Narraburra Granite|71206|6|Mentioned|p373, 384|||Lachlan Fold Belt. Geochemistry graphs.||Narraburra Suite.||||
13890|Narraburra Granite|72084|6|Mentioned|p55 Fig.57|||A-type geochemical discrimination diagrams.||||||
13896|Narragal Limestone|6969|5|Briefly described|p12|Ludlow|Ludlow|Of the Mumbil Group.  Geological Province: Lachlan Fold Belt.||||||
13896|Narragal Limestone|13996|6|Mentioned|p130|Silurian|Silurian|Contains Ludlow-aged conodonts (species listed). Also appears as Narragal Formation on the same page.||||||
13896|Narragal Limestone|22486|6|Mentioned|p 6|||||||||
13896|Narragal Limestone|22857|4|Described|p466 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Mumbil Group. Massive to well-bedded limestone and dolomitic limestone; minor shale, rare chert. Max. thickness: 300m.||||||
13896|Narragal Limestone|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Mumbil Group.||||||
13896|Narragal Limestone|23170|2|Defined|p86|Ludlow|Ludlow|of Mumbil Group. Supercedes 'Narragal Limestone Member'.||||||
13896|Narragal Limestone|23214|5|Briefly described|p131|||Originally  Narragal Limestone Member.  Previously thought to be a synonym of Nandillyan Limestone.||||||
13896|Narragal Limestone|23225|4|Described|p12|Ludlow|Ludlow|Age: Early to Middle Ludlow. Byrnes 1992 regarded limestone as synonym of Nandillyan Limestone Member. Correlates with the upper part of the Molong Limestone. Of Mumbil Group.||||||17-FEB-06
13896|Narragal Limestone|31543|6|Mentioned|p111|||||||||
13896|Narragal Limestone|32154|6|Mentioned|p181|||Refers Vandyke (1970 unpubl.)||||||
13896|Narragal Limestone|32413|6|Mentioned|p101|||||||||
13896|Narragal Limestone|33611|4|Described|p129|||||||||
13896|Narragal Limestone|34406|6|Mentioned|p220|||||||||
13896|Narragal Limestone|39975|6|Mentioned|p135|||||||||
13896|Narragal Limestone|40328|3|Fully described|p148|||||||||
13896|Narragal Limestone|41048|6|Mentioned|p25|||||||||
13896|Narragal Limestone|43517|14|Not recorded|p153,154,160||Wenlockian|Lower member of Mumbil Formation||||||
13896|Narragal Limestone|50095|5|Briefly described|p108 Fig.1|Silurian|Silurian|||||||
13896|Narragal Limestone|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Mumbil Group.  Massive to bedded highly fossiliferous limestone.||||||
13896|Narragal Limestone|60987|6|Mentioned|p154 Fig.1|Silurian|Silurian|||||||
13896|Narragal Limestone|61894|6|Mentioned|p182|Silurian|Silurian|Pseudoplasmopora sp.B has been reported, but not described, in this unit.||||||
13896|Narragal Limestone|66197|5|Briefly described|p632, p633 Fig.4c|Ludlow|Ludlow|Cowra Trough-Molong High. Shallow marine limestone. Underlies the Barnby Hills Shale, overlies the Dripstone Formation.||||||14-MAR-12
13896|Narragal Limestone|68003|5|Briefly described|p24 Fig.3-e, p146. |Pridoli|Wenlock|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Mumbil Group.||Overlies Dripstone Formation.|Massive to bedded highly fossiliferous limestone; siltstone.|
13896|Narragal Limestone|71600|6|Mentioned|p23 Fig 2|Silurian|Silurian|Geological province: Lachlan Fold Belt.||Unit of Mumbil Group.||||
13896|Narragal Limestone|73299|6|Mentioned|p1105|Early Devonian|Silurian|Molong High. [Map symbol suggests Silurian age]||||Overlies the Dripstone Formation, underlies the Barnby Hills Shale.||
13911|Narrow Plain Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Coorabin Coal Measures. Poorly consolidated clayey sandstone. Max. thickness: 30m. Geological Province: Ovens Graben.||||||
13911|Narrow Plain Formation|35498|2|Defined|p144|Late Permian|Late Permian|||||||
13911|Narrow Plain Formation|35503|6|Mentioned|p202|||Defined in Standing Committee Coalfield Geology NSW (1978)||||||
13911|Narrow Plain Formation|38293|5|Briefly described|p20|||||||||
13911|Narrow Plain Formation|69798|5|Briefly described|p4 Fig.2, p11-12, p17 Fig.14, p18-19|Permian|Permian|Oaklands Basin. Seismic profiles. Fluvial-point bar depositional environment.||Coorabin Coal Measures.|Lanes Shaft Coal Member.|||06-FEB-18
13935|Native Dog Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Carboniferous|Carboniferous|Intertongues with Late Visean Woolooma Formation. Thick ignimbrite, arenites. Max. thickness: >500m. Geological Province: Tamworth Forearc Basin.||||||
13935|Native Dog Member|32529|3|Fully described|p198|||||||||
13935|Native Dog Member|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
13935|Native Dog Member|32869|5|Briefly described|p168|||Isismurra Fm.||||||
13935|Native Dog Member|39214|5|Briefly described|p29|||||||||
13935|Native Dog Member|41279|6|Mentioned|Fig.2|||||||||
13935|Native Dog Member|44244|5|Briefly described|p35|||Overlies the Ayr Conglomerate Member.  Max. thickness: >500m.  Geological Province: Rouchel Block.||||||
13935|Native Dog Member|45088|2|Defined|p48|Early Carboniferous|Early Carboniferous|See also Plate 2||||||
13935|Native Dog Member|50099|5|Briefly described|p10|Early Carboniferous|Early Carboniferous|Of the Isismurra Formation. Max. thickness: 500m. Geological Province: Tamworth Belt/New England Orogen. Lower fine-grained ignimbrite and upper sequence of green fine-grained ignimbrites, vitric lithic tuff and interbedded lithic sandstone & conglomerate||||||
13935|Native Dog Member|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Of the Isismurra Formation.  Overlies: Ayr Conglomerate Member.||||||
13935|Native Dog Member|62095|5|Briefly described|Plate 1|Carboniferous|Carboniferous|Of Isismurra Formation. Geological Province: Rouchel Block/Tamworth Belt.||||||
13935|Native Dog Member|68003|5|Briefly described|p136.|||Tamworth Belt (South), New England Fold Belt.||Unit in Isismurra Formation.|||Purple and buff welded tuff, red welded tuff.|
13935|Native Dog Member|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||Isismurra Formation||||
13935|Native Dog Member|73487|6|Mentioned|p566|Visean|Visean|Rouchel Block. Orthotetes australia zone.||||||
13946|Neara Volcanics|13516|5|Briefly described|p159 fig 8|Triassic|Triassic|From Clarence-Moreton Basin.||Of Toogoolawah Group||||
13946|Neara Volcanics|22757|5|Briefly described|p14||Triassic|Overlain by Ipswich Coal Measures.||||||18-AUG-08
13946|Neara Volcanics|22845|6|Mentioned|p11,18,21,46,57,82||Triassic|||||||
13946|Neara Volcanics|22846|6|Mentioned|p9,14,36,56,67|Middle Triassic|Early Triassic|Overlie  Gallangowan Granodiorite.||||||
13946|Neara Volcanics|23440|4|Described|p140|Triassic|Triassic|Of Toogoolawah Group.||||||18-AUG-08
13946|Neara Volcanics|23608|5|Briefly described|p50 Fig 1, p53|Carboniferous|Devonian|Intruded by Woolooga Granodiorite.||||||
13946|Neara Volcanics|23799|3|Fully described|p40, p37 Tb. 3, p37 Tb. 3|Middle Triassic|Early Triassic|Formerly "Lower Esk Series" of Hill (91930) and "Neara Series" of Bryan & Jones (1946).  Overlie Marumba beds, Claddagh Granodiorite and Mount Clara beds in east Esk Trough. Intruded by Kingaham Creek Granodiorite.Geological Province: Esk Trough.||||||12-NOV-15
13946|Neara Volcanics|23800|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group.||||||
13946|Neara Volcanics|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Of Toogoolawah Group.  Geological Province: Esk Trough. Maximum thickness: 1000m.||||||
13946|Neara Volcanics|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Volcaniclastic conglomerate, andesite, sandstone.||||||
13946|Neara Volcanics|29420|6|Mentioned|p98|||||||||
13946|Neara Volcanics|29720|6|Mentioned|Fig.1|||||||||
13946|Neara Volcanics|29968|6|Mentioned|p11|||||||||
13946|Neara Volcanics|30089|6|Mentioned|p853|||||||||
13946|Neara Volcanics|30302|6|Mentioned|p414|||Lower to Middle Triassic age||||||
13946|Neara Volcanics|30451|6|Mentioned|p69|||||||||
13946|Neara Volcanics|30466|6|Mentioned|p1|||Triassic age||||||
13946|Neara Volcanics|30473|6|Mentioned|p377|||Refers Cranfield & Schwarzbock(1972). Part of Toogoolawah Group.||||||
13946|Neara Volcanics|31450|6|Mentioned|p46|||||||||
13946|Neara Volcanics|31451|6|Mentioned|p78|||||||||
13946|Neara Volcanics|31811|6|Mentioned|Fig. 1|||||||||
13946|Neara Volcanics|33381|4|Described|p109|||Triassic. See also PP113,117,122.||||||
13946|Neara Volcanics|34010|6|Mentioned|Cor. chart|||M.Triassic||||||
13946|Neara Volcanics|34261|6|Mentioned|p100|||P99 refers Zimmerman (1956)||||||
13946|Neara Volcanics|34974|6|Mentioned|p946|||||||||
13946|Neara Volcanics|35101|3|Fully described|p38|||||||||
13946|Neara Volcanics|35161|6|Mentioned|p591|||||||||
13946|Neara Volcanics|35427|6|Mentioned|p122|||||||||
13946|Neara Volcanics|36246|6|Mentioned|p15|||||||||
13946|Neara Volcanics|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
13946|Neara Volcanics|36926|6|Mentioned|p175|||||||||
13946|Neara Volcanics|36954|6|Mentioned|p114|||See Fig.1.||||||
13946|Neara Volcanics|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
13946|Neara Volcanics|37376|6|Mentioned|p491|||||||||
13946|Neara Volcanics|37755|6|Mentioned|p79|||||||||
13946|Neara Volcanics|38304|6|Mentioned|p83|||||||||
13946|Neara Volcanics|39079|5|Briefly described|p8|||||||||
13946|Neara Volcanics|39445|5|Briefly described|Table 9|||See also Fig.7||||||
13946|Neara Volcanics|39505|6|Mentioned|p191|||||||||
13946|Neara Volcanics|40051|4|Described|p8|||||||||
13946|Neara Volcanics|40245|6|Mentioned|p182|||Mention P187||||||
13946|Neara Volcanics|40475|5|Briefly described|p8|||||||||
13946|Neara Volcanics|40477|6|Mentioned|p16|||||||||
13946|Neara Volcanics|40478|5|Briefly described|p24|||||||||
13946|Neara Volcanics|40479|6|Mentioned|p33|||||||||
13946|Neara Volcanics|40480|6|Mentioned|p39|||||||||
13946|Neara Volcanics|40484|6|Mentioned|Fig.2|||||||||
13946|Neara Volcanics|40623|5|Briefly described|p65|||||||||
13946|Neara Volcanics|41161|6|Mentioned|Fig.1|||||||||
13946|Neara Volcanics|41272|5|Briefly described|M 1of1 G15|||||||||
13946|Neara Volcanics|41591|5|Briefly described|p17|||||||||
13946|Neara Volcanics|41738|6|Mentioned|p163|||||||||
13946|Neara Volcanics|41917|6|Mentioned|p522|||||||||
13946|Neara Volcanics|42041|6|Mentioned|p222|||||||||
13946|Neara Volcanics|42492|5|Briefly described|Table 2 P14|||||||||
13946|Neara Volcanics|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.||||||15-JUL-04
13946|Neara Volcanics|42619|5|Briefly described|p29|||||||||
13946|Neara Volcanics|42694|5|Briefly described|map legend|Triassic||||||||
13946|Neara Volcanics|42902|5|Briefly described|p416|||||||||
13946|Neara Volcanics|43003|6|Mentioned|Fig.16,p168|||||||||
13946|Neara Volcanics|43092|4|Described|p29|Middle Triassic|Early Triassic|see also map enclosure.||||||
13946|Neara Volcanics|43993|14|Not recorded|p102|||Ref. to Bryan and Jones 1946.||||||
13946|Neara Volcanics|44026|14|Not recorded|p122-125||Triassic|Conformably overlies Bryden Beds. Lithologically equivalent to Blackwall Breccia, Weir Basalt, Mount Crosby Formation.||||||
13946|Neara Volcanics|44076|14|Not recorded|Fig.38,p269,271-4|||||||||
13946|Neara Volcanics|44091|14|Not recorded|p52||Triassic|||||||
13946|Neara Volcanics|44360|14|Not recorded|p20||Triassic|Equivalent to Muncon Volcanics.||||||
13946|Neara Volcanics|44573|14|Not recorded|p95|||||||||
13946|Neara Volcanics|44671|2|Defined|p249||Early Triassic|See also Lexicon.||||||
13946|Neara Volcanics|44781|14|Not recorded|p365|||||||||
13946|Neara Volcanics|44783|14|Not recorded|p2,33-35|||||||||
13946|Neara Volcanics|44786|14|Not recorded|p193-202||Middle Triassic|||||||
13946|Neara Volcanics|44814|14|Not recorded|p483,485||Late Triassic|||||||
13946|Neara Volcanics|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
13946|Neara Volcanics|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group||||||30-NOV-05
13946|Neara Volcanics|45110|6|Mentioned|p80|||||||||
13946|Neara Volcanics|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of Toogoolawah Group. Geological Province: Esk Trough (Wandilla Province).||||||18-AUG-08
13946|Neara Volcanics|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group.  Volcanic conglomerate, agglomerate, andesitic tuff, lahar, shale, sandstone.||||||19-JUL-04
13946|Neara Volcanics|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Of the Toogoolawah Group. Volcaniclastic conglomerate; andesite, sandstone; mudstone, siltstone laminae; conglomerate.||||||
13946|Neara Volcanics|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Of the Toogoolawah Group. Geological Province: Esk Trough. Volcaniclastic conglomerate; andesite, sandstone.||||||12-NOV-15
13946|Neara Volcanics|60993|6|Mentioned|p8 Tb. 2|||Geological Province: Clarence-Moreton Basin.||||||
13946|Neara Volcanics|61003|6|Mentioned|p224|Middle Triassic|Middle Triassic|||||||
13946|Neara Volcanics|61612|6|Mentioned|p274, p270 Fig. 1|Early Triassic|Late Permian|Geological Province: Esk Trough.||||||17-MAR-09
13946|Neara Volcanics|61782|5|Briefly described|p275, p277, p277 Fig. 3, p282|||Geol Prov: Esk Trough. Volcaniclastic sedimentary rocks and minor intermediate voolcanics.||||||
13946|Neara Volcanics|63821|6|Mentioned|p20|||||||||07-FEB-11
13946|Neara Volcanics|65668|6|Mentioned|p20|Middle Triassic|Middle Triassic|Age: 240.9 Ma. Intruded by Elgin Vale Diorite.||||||10-JAN-17
13946|Neara Volcanics|67203|5|Briefly described|p3, p36-37|Late Triassic|Late Triassic|Further geochronological work is required to test the correlation with Mount Marcella Volcanics, and determine the southern extent of Late Triassic volcanism.||||Equivalent to Mount Marcella Volcanics.||12-NOV-15
13946|Neara Volcanics|67402|5|Briefly described|p204, p205 tbl ESK/ABR1|Ladinian|Ladinian|Esk Trough. Deposited in a fluvial environment. Approximately 500m thick. Contains a potential intraformational shale seal. See also p206 fig ESK/ABR6, p208-p210.||Toogoolawah Group||Overlies the Bryden Formation. Overlain by the Ipswich Coal Measures.|Agglomerate, conglomerate, andesitic flows, tuffs and fossiliferous shales.|
13946|Neara Volcanics|67874|5|Briefly described|p11, p19, p35|Middle Triassic|Early Triassic|Cranfield (1989). Age is based largely on poorly-constrained plant fossils and limited radiometric age data.|~240 Ma.|||Equivalent to Mount Marcella Volcanics.||
13946|Neara Volcanics|68679|4|Described|p322, p326, p328-329, p331-332, p387|Middle Triassic|Early Triassic|See also p389-391, p411, p427, p429, p433, p440, p471. Esk Basin, North D'Aguilar Subprovince, northern New England Orogen. Widespread unit. Nine subdivisions are tabulated and described in some detail, reflecting spatial variations more than stratigraphic units. Differing stratigraphic interpretations discussed. Rich in plant fossils (species listed). RELATED UNITS (continued): Is faulted against the Rocksberg Greenstone and Wongella Metamorphics. Is intruded by Elgin Vale Diorite, Avoca Creek and Boonara Granodiorites, and Somerset Dam Igneous Complex.|241.2 +/- 11 Ma; 239.2 +/- 5 Ma (Campbell, 2005).|Toogoolawah Group.||Unconformably overlies Amamoor, Maronghi Creek beds, Kandanga Creek Megabreccia, Kingaham Creek Granodiorite and Mount Mia Serpentinite. Underlies concordantly Aranbanga Volcanic Group. See COMMENTS.|Volcaniclastic conglomerate, andesitic volcanics, sandstone, andesite boulder beds, mudstone, conglomerate, dacitic volcanics, hornfels, felsic volcanics, volcaniclastic sandstone. All elaborated in detail on p390.|
13946|Neara Volcanics|69952|6|Mentioned|p4, p47, p49|Early Triassic|Early Triassic|||||||
13946|Neara Volcanics|72297|5|Briefly described|p712|||Kilkivan area.|||||Contains multiphase carbonate quartz veins hosting cinnabar veinlets and disseminations in NNW-trending fracture zones.|
13946|Neara Volcanics|73306|5|Briefly described|p565-566|Middle Triassic|Middle Triassic|Esk Trough.|c.242 Ma (Campbell, 2005).|Toogoolawah Group.|||Intermediate volcanic rocks.|
13946|Neara Volcanics|73450|6|Mentioned|p107|||||||||
13976|Nelligen Granodiorite|35248|6|Mentioned|Fig.1|||||||||
13976|Nelligen Granodiorite|36600|6|Mentioned|Table 1|||See also P102.||||||
13976|Nelligen Granodiorite|39028|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
13976|Nelligen Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
13976|Nelligen Granodiorite|40276|2|Defined|p14|Early Devonian|Early Devonian|||||||
13976|Nelligen Granodiorite|42497|5|Briefly described|Map Legend|Eifelian|Pragian|||||||
13976|Nelligen Granodiorite|62070|5|Briefly described|p40,|||Middle Devonian age proposed from inference from overlying Merrimbula Group.||Of Moruya Suite.||Overlain nonconformably by basal sediments of the Merrimbula Group.||
13976|Nelligen Granodiorite|68255|6|Mentioned|p1051-p1055, p1058, p1060-p1063|||||||Overlain by the Merrimbula Group.||
14021|Neranleigh-Fernvale beds|22845|6|Mentioned|p46|Early Carboniferous|Late Devonian|||||||
14021|Neranleigh-Fernvale beds|23799|6|Mentioned|p8, p122|||Of the South D'Aguilar and Beenleigh Subprovinces.||||||
14021|Neranleigh-Fernvale beds|23811|5|Briefly described|Map Legend|Visean|Tournaisian|Feldspathic and lithic meta-arenite, metasiltstone, chert, jasper, metabasic volcanic rock, conglomerate.||||||20-DEC-04
14021|Neranleigh-Fernvale beds|23812|5|Briefly described|p15, p137|Early Carboniferous|Early Carboniferous|Geological Province: Clarence-Moreton Basin.||||||
14021|Neranleigh-Fernvale beds|24418|6|Mentioned|p11|||Metasediments.||||||30-JUN-06
14021|Neranleigh-Fernvale beds|37509|6|Mentioned|p504|||||||||
14021|Neranleigh-Fernvale beds|38307|6|Mentioned|Fig.1|||||||||
14021|Neranleigh-Fernvale beds|38805|6|Mentioned|p87|||||||||
14021|Neranleigh-Fernvale beds|39079|5|Briefly described|p6|||||||||
14021|Neranleigh-Fernvale beds|39943|6|Mentioned|Table 10A|||||||||
14021|Neranleigh-Fernvale beds|39998|5|Briefly described|p189|||||||||
14021|Neranleigh-Fernvale beds|40475|6|Mentioned|p3|||||||||
14021|Neranleigh-Fernvale beds|40484|6|Mentioned|p63|||||||||
14021|Neranleigh-Fernvale beds|40623|5|Briefly described|p6|||||||||
14021|Neranleigh-Fernvale beds|40780|4|Described|p5|||||||||
14021|Neranleigh-Fernvale beds|40787|5|Briefly described|p346|||||||||
14021|Neranleigh-Fernvale beds|40896|6|Mentioned|p10|||||||||
14021|Neranleigh-Fernvale beds|40960|6|Mentioned|p215|||||||||
14021|Neranleigh-Fernvale beds|41822|6|Mentioned|p240|||||||||
14021|Neranleigh-Fernvale beds|41906|3|Fully described|Table 1 p11|||||||||23-NOV-15
14021|Neranleigh-Fernvale beds|41917|6|Mentioned|Fig.3 P528|||||||||
14021|Neranleigh-Fernvale beds|42316|6|Mentioned|p17|||||||||
14021|Neranleigh-Fernvale beds|42317|4|Described|p2|||||||||
14021|Neranleigh-Fernvale beds|42336|4|Described|p2|||||||||
14021|Neranleigh-Fernvale beds|42619|5|Briefly described|p29|||||||||
14021|Neranleigh-Fernvale beds|42669|5|Briefly described|p234|||||||||
14021|Neranleigh-Fernvale beds|42901|5|Briefly described|Fig.12 P412|||see also Fig.11 P411||||||
14021|Neranleigh-Fernvale beds|42970|6|Mentioned|p116|||||||||
14021|Neranleigh-Fernvale beds|43076|5|Briefly described|p4|||||||||
14021|Neranleigh-Fernvale beds|43092|5|Briefly described|p20|||||||||
14021|Neranleigh-Fernvale beds|43161|5|Briefly described|14||Carboniferous|||||||
14021|Neranleigh-Fernvale beds|44093|5|Briefly described|p242 App. 1|Carboniferous|Devonian|In the Beenleigh Block. Geological Province: New England Fold Belt.||||||
14021|Neranleigh-Fernvale beds|60079|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Meta-arenite, metasiltstone, chert, jasper, basic metavolcanics, conglomerate.||||||
14021|Neranleigh-Fernvale beds|60993|5|Briefly described|p17|Paleozoic|Paleozoic|Unconformably overlain by the Marburg Subgroup units.||||||07-NOV-08
14021|Neranleigh-Fernvale beds|61775|5|Briefly described|p181||Early Carboniferous|Comprise greywacke, argillite and chert that have undergone low grade regional metamorphism. Interpreted as the upper part of an accretionary prism.||||||06-MAY-13
14021|Neranleigh-Fernvale beds|63779|6|Mentioned|p1140|Carboniferous|Devonian|||||||
14021|Neranleigh-Fernvale beds|65380|5|Briefly described|p658, 660-663, 665-667, 671-672, 676-679|||Beenleigh Block, D'Aguilar Block. Detrital zircons from granitic sources in this unit may be considerably older than depositional age. Sample from Mt Nebo gives 351 +/-2 Ma detrital zircon age. Maximum depositional age from detrital zircon: 332 +/-3 Ma|||||Includes sandstones.|
14021|Neranleigh-Fernvale beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|Beenleigh and South D'Aguilar Subprovinces.||||||
14021|Neranleigh-Fernvale beds|68679|3|Fully described|p321-322, p331, p333-336, p386, p392|Tournaisian|Tournaisian|See also p393 Fig.5.74, p394, p427, p433, p451. Fleming et al. (1974) and Korsch and Harrington (1981). Previously the Neranleigh-Fernvale Group of Bryan and Jones (1950); they combined the upper two units of the Brisbane Schists (Denmead, 1928): the Neranleigh Series and the Fernvale Series. The name Neranleigh itself was first used by Rands (1889) combining Neranwood (village) with Beenleigh (town). South D'Aguilar Subprovince, northern New England Orogen. The type area is the valley of Moggill Creek, W of Brisbane. Includes rocks in the Beenleigh Subprovince, from SE Brisbane to near Byron Bay. Upper plate accretionary assemblage. Deformation described in some detail. Other ages given. RELATED UNITS (continued): Correlated with the Texas beds. Possibly equivalent to Amamoor beds. Is intruded by Enoggera Granite, Samford and Mount Samson Granodiorites.|351 +/- 2 Ma (Korsch et al., 2009).|||Adjoins and partly faulted against Bunya Phyllite. Is faulted against and unconformably underlies Northbrook beds. Is overlain unconformably by Brisbane Tuff and Ipswich Coal Measures. See COMMENTS.|A heterogeneous succession of sandstone (commonly volcanolithic and locally oolitic), siltstone, chert and minor mafic volcanics (including pillow basalt), conglomerate and jasper; low greenschist metamorphosed. Fossils are rare.|
14021|Neranleigh-Fernvale beds|69599|6|Mentioned|p594|||||||Is overlain unconformably by the Oxley Group.||
14021|Neranleigh-Fernvale beds|69952|5|Briefly described|p38, p42|Carboniferous|Devonian|||||Is overlain unconformably by Brisbane Tuff. Is intruded by Enoggera Granite and Samford and Mount Samson Granodiorites.||
14021|Neranleigh-Fernvale beds|70125|5|Briefly described|p398|Carboniferous|Devonian|Beenleigh Block. Zircon ages described in some detail.||||||
14025|Nerong Volcanics|22516|5|Briefly described|p17||Carboniferous|||||||
14025|Nerong Volcanics|22586|6|Mentioned|398, 399|Carboniferous|Carboniferous|||||||
14025|Nerong Volcanics|22736|6|Mentioned|p629||Visean|||||||
14025|Nerong Volcanics|22857|4|Described|p512 App.1 Tb A1.8, p510 App.1 Tb A1.8|Visean|Visean|Ignimbrite interbedded with tuffaceous sandstone and conglomerate; dominant rhyodacitic ignimbrite up to 300m thick. Disconformably underlies Karuah Fm; disconformably overlies Boolambayte Fm. Correlative of Gilmore Volcanic Gp. Max. thickness: 820m.||||||
14025|Nerong Volcanics|23157|5|Briefly described|p109,126|||||||||
14025|Nerong Volcanics|24118|6|Mentioned|p3|||||||||
14025|Nerong Volcanics|24121|5|Briefly described|p4, p235, p245|Carboniferous|Carboniferous|||||||25-AUG-22
14025|Nerong Volcanics|30074|6|Mentioned|p24|||||||||
14025|Nerong Volcanics|31802|6|Mentioned|p136|||||||||
14025|Nerong Volcanics|32379|6|Mentioned|p5|||||||||
14025|Nerong Volcanics|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
14025|Nerong Volcanics|32868|6|Mentioned|p200|||||||||
14025|Nerong Volcanics|32869|4|Described|p171|||See also Fig.3B. Refers Engel (1972)||||||
14025|Nerong Volcanics|33808|6|Mentioned|Table 1|||Anal.||||||
14025|Nerong Volcanics|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
14025|Nerong Volcanics|34072|6|Mentioned|Fig.4.5|||Carb.||||||
14025|Nerong Volcanics|34085|6|Mentioned|Cor.chart|||Visean||||||
14025|Nerong Volcanics|34168|5|Briefly described|p254|||Carboniferous||||||
14025|Nerong Volcanics|34238|6|Mentioned|Table 1|||||||||
14025|Nerong Volcanics|34374|6|Mentioned|p255|||||||||
14025|Nerong Volcanics|36057|3|Fully described|p346|||Visean?||||||
14025|Nerong Volcanics|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
14025|Nerong Volcanics|36528|6|Mentioned|p178|||||||||
14025|Nerong Volcanics|38801|6|Mentioned|p121|||||||||
14025|Nerong Volcanics|39302|5|Briefly described|p345|||See also p346.||||||20-NOV-06
14025|Nerong Volcanics|39308|6|Mentioned|p482|||See also p490.||||||20-NOV-06
14025|Nerong Volcanics|42547|4|Described|p35, p37|||||||||
14025|Nerong Volcanics|42780|5|Briefly described|Fig.2 P412|||||||||
14025|Nerong Volcanics|42798|5|Briefly described|p56|||||||||
14025|Nerong Volcanics|43432|14|Not recorded|p208|||Myall facies.||||||20-NOV-06
14025|Nerong Volcanics|43437|14|Not recorded|p169-175||Carboniferous|||||||
14025|Nerong Volcanics|43447|14|Not recorded|Table 1&2,p10,13||Carboniferous|||||||
14025|Nerong Volcanics|43451|14|Not recorded|Map Legend|||||||||
14025|Nerong Volcanics|43479|14|Not recorded|p161,177|Namurian|Visean|||||||
14025|Nerong Volcanics|44093|5|Briefly described|p230 App. 1|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
14025|Nerong Volcanics|44244|2|Defined|p136-137, p203-206|Visean|Visean|Conformably overlies the Conger and Boolanbayte Formations; disconformably underlie Karuah Formation and Booti Booti Sandstone.  Max. thickness: ~2000m.  Type section in text.  Geological Province: Myall Block.||||||25-AUG-04
14025|Nerong Volcanics|45097|6|Mentioned|Fig.|||Correlation chart||||||
14025|Nerong Volcanics|47056|6|Mentioned|Fig.2 P523|||||||||
14025|Nerong Volcanics|50132|5|Briefly described|p248  Fig.6|||Early Namurian age||||Overlies the Boolambayte Formation. Underlies the Booti Booti Sandstone.||
14025|Nerong Volcanics|50147|5|Briefly described|Map legend|Visean|Visean|Red to buff rhyodacitic ignimbrite, minor dacite and rhyolitic pitchstone and occasional interbeds of tuffaceous sandstone and conglomerate.||||||
14025|Nerong Volcanics|50263|5|Briefly described|Map Legend|Visean|Visean|Overlies: Conger Formation, Boolambayte Formation.  Geological Province: Myall Block.||||||
14025|Nerong Volcanics|63832|6|Mentioned|p131 fig 2|Carboniferous|Carboniferous|Myall block, Southern New England Fold Belt.||||||
14025|Nerong Volcanics|64631|6|Mentioned|p44 Fig.2.|Visean|Tournaisian|Southern New England Fold Belt, western Myall Block. Some biostratigraphic and radiometric age control.||||||
14025|Nerong Volcanics|65107|5|Briefly described|p289|Early Carboniferous|Early Carboniferous|age: 338.6+/-3.8Ma SHRIMP U-Pb zircon. Constrains Paleomag results from Myall Block and New England Orogen (NEO) paleopole path, with Alum Mountain Volcanics||||||
14025|Nerong Volcanics|69323|4|Described|p1,3,61-67,69, 76|Mississippian|Mississippian|Geological province: New England Orogen. Represents part of the southern-most exposures of the New England Orogen (Rose et al., 1966). Voids in the ignimbrite are suggestive of degassing; zones and veins of hematisation are also apparent. Interbedded with sedimentary rocks containing Carboniferous Rhacopteris flora at Soldiers Point (White 1994). Roberts et al., 1995 reported an age of 338.6+\-2.8 Ma from the type section (does not specify where the type section is).  SHRIMP U-Pb zircon geochronology of GA 2129547 (rhyodacitic ignimbrite from the lowermost Nerong Volcanics) yielded an interpreted (weighted mean 206Pb/238U) magmatic crystallisation age of 340.5+\-2.0 Ma, broadly consistent with the 338.6+\-2.8 Ma age of Roberts et al., 1995. Sampling details, zircon characteristics, SHRIMP results and analyses are provided.|340.5+\-2.0 Ma (SHRIMP U-Pb; this study)|||Overlain disconformably by Booti Booti Sandstone and Karuah Formation. Underlain conformably by Conger Formation.||03-DEC-19
14025|Nerong Volcanics|69639|6|Mentioned|p8|||New England Orogen.||||||
14025|Nerong Volcanics|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Myall Block, Tamworth Belt.||||||
14025|Nerong Volcanics|73197|5|Briefly described|p465 Fig.4, p466 Tb.1, p467|Visean|Visean|New England Orogen, southern. Proximal-source arc volcanics of the Currabubula-Connors Arc. One U-Pb zircon age from Chisholm et al., (2014a), Roberts et al., (1995b) corrected for use of the SL13 standard.|338.6 +/- 3.8 Ma and 340.5 +/- 2 Ma U-Pb zircon||||Volcanics including rhyodacitic ignimbrites.|
14025|Nerong Volcanics|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, Carboniferous arc.||||||
14025|Nerong Volcanics|73487|5|Briefly described|p562, p564, p567, p569-571, p577-578|Visean|Visean|Well developed in the western Myall block, less so in the eastern Myall block. Equated with the Buggs Creek Ignimbrite (Geeve et al., 2002; Roberts et al., 1991). Shown as Nerong p566. See also p568 Fig.3, p574, p581, p583.|ca 339 Ma||||Ignimbritic in parts.|
14026|Nest Hill Granite|42726|5|Briefly described|map legend|||546.||||||
14026|Nest Hill Granite|69801|5|Briefly described|p2, p4-p5, p65-69, p135-137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Informal name; occurs between Wagga Wagga and Holbrook. Same age as the nearby Mount Flakney Granite. Petrography, zircon characteristics, SHRIMP analyses and interpretation are detailed.|429.2 +/- 2 Ma (Ickert and Williams, 2011)|||Intrudes the Wagga Group.|Weakly foliated, medium- to coarse-grained, biotite-granodiorite containing microgranitic enclaves.|
14105|Newman Member|39279|4|Described|p370|Late Permian|Late Permian|||Of Drake Volcanics.||overlain by Gilgurry Mudstone.||13-NOV-15
14105|Newman Member|42378|6|Mentioned|Table 1 P10|||||||||
14148|Nimbin Rhyolite|22582|4|Described|p69||Tertiary|Lamington Volcanics. Overlies Lismore Basalt, overlain by Blue Knob Basalt||||||
14148|Nimbin Rhyolite|24299|6|Mentioned|p184|||||||||
14148|Nimbin Rhyolite|29995|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14148|Nimbin Rhyolite|30604|1|Redefined|p69|Cenozoic|Cenozoic|||||||19-NOV-08
14148|Nimbin Rhyolite|30605|6|Mentioned|p268|||early Miocene?||||||
14148|Nimbin Rhyolite|30687|6|Mentioned|p65|||Tertiary age. See also p64, Miocene age.||||||
14148|Nimbin Rhyolite|31130|6|Mentioned|Fig. 2|||Correlation. Early Miocene.||||||
14148|Nimbin Rhyolite|32924|6|Mentioned|p113|||Refers McTaggart (1961)||||||
14148|Nimbin Rhyolite|34092|5|Briefly described|p11|||||||||
14148|Nimbin Rhyolite|34340|6|Mentioned|Table 6.1|||||||||
14148|Nimbin Rhyolite|34593|6|Mentioned|p540|||||||||
14148|Nimbin Rhyolite|35050|6|Mentioned|p130|||||||||
14148|Nimbin Rhyolite|35296|4|Described|p13|||See also P12.||||||
14148|Nimbin Rhyolite|36056|6|Mentioned|p31|||||||||
14148|Nimbin Rhyolite|36411|6|Mentioned|p269|||Refs.Duggan & Mason 1978 for redefinition.||||||
14148|Nimbin Rhyolite|36806|6|Mentioned|p131|||||||||
14148|Nimbin Rhyolite|40623|5|Briefly described|p39|||||||||
14148|Nimbin Rhyolite|40896|4|Described|p8|||||||||
14148|Nimbin Rhyolite|43161|4|Described|13|||||||||
14148|Nimbin Rhyolite|43881|1|Redefined|p6-7,49,55-58,63,154||Tertiary|Inc.Minyon Falls Rhyolite Mbr,Boomerang Ck.Obsidian Mbr,Dorroughby Tuff Mbr:inc in MacPherson Volcs.||||||
14148|Nimbin Rhyolite|44818|6|Mentioned|p275|||||||||
14148|Nimbin Rhyolite|45018|14|Not recorded|p38|||(Urbenville)||||||
14148|Nimbin Rhyolite|48917|6|Mentioned|p38|||Stratigraphy||||||
14148|Nimbin Rhyolite|69599|5|Briefly described|p640|||Tweed volcano, centred on Mount Warning.||||Approximate equivalent of Binna Burra and Springbrook Rhyolites in QLD.|Peraluminous or high-silica rhyolite.|
14148|Nimbin Rhyolite|73581|5|Briefly described|p6|||Tweed Volcano. Overlies Beechmont Basalt/Lismore Basalt. Underlies Hobwee Basalt/Blue Knob Basalt.|||||Rhyolitic tuff and rhyolite lavas up to 100 m thick.|
14179|Nioka Porphyritic Dacite Member|22857|5|Briefly described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of Emmaville Volcanics (Wandsworth Group). Dacite ash flow, porphyritic dacite lava. Geological Province: New England Fold Belt.||||||
14179|Nioka Porphyritic Dacite Member|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Emmaville Volcanics (Wandsworth Volcanic Group).  Dacitic ashflow, rhyolitic ash flow, porphyritic dacite lava.||||||20-DEC-04
14179|Nioka Porphyritic Dacite Member|23812|5|Briefly described|p27 Tb.3|Late Permian|Early Permian|Maximum thickness: ~10m.||||||
14179|Nioka Porphyritic Dacite Member|42378|5|Briefly described|Table 1 P8|||||||||
14198|Nobbys Tuff|22578|6|Mentioned|p400|||||||||
14198|Nobbys Tuff|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Newcastle Coal Measures. Tuff, tuffaceous sandstone, tuffaceous siltstone, claystone, chert. Max. thickness: 25m. Geological Province: Sydney Basin.||||||
14198|Nobbys Tuff|22969|5|Briefly described|p 40|||||||||
14198|Nobbys Tuff|23055|6|Mentioned|p15,22,Fig29p41|||||||||
14198|Nobbys Tuff|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Newcastle Coal Measures.   Equivalent to the Monkey Place Creek Member (Wollambi Coal Measures).||||||
14198|Nobbys Tuff|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Newcastle Coal Measures. Geological Province: Sydney Basin||||||
14198|Nobbys Tuff|24471|4|Described|p32 Fig.4, p27|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Huntley Claystone Member. Geological Province: Sydney Basin.||||||07-FEB-11
14198|Nobbys Tuff|29922|6|Mentioned|Appendix 4|||||||||
14198|Nobbys Tuff|33867|6|Mentioned|Fig.4|||||||||
14198|Nobbys Tuff|45090|6|Mentioned|p83|||Table of Perm. igneous rocks||||||
14198|Nobbys Tuff|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Newcastle Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
14198|Nobbys Tuff|62033|5|Briefly described|p25 (Table)|||Of the Newcastle Coal Measures. Overlain by Adamstown Formation; overlies Lambton Formation. Geological Province: Sydney Basin.||||||14-MAR-07
14198|Nobbys Tuff|68493|6|Mentioned|p5 Fig.2|Lopingian|Lopingian|||Of the Newcastle Coal Measures.|||Felsic tuff, tuffaceous sedimentary rock.|
14198|Nobbys Tuff|68711|3|Fully described|p119, 113, 115, p116 Tb 2, p114 Fig. 2|||Formation status. Replaces Nobbys Tuff Member, Nobbys Chert. Named after Nobbys Headland. Thickness: 0.5-25m, 24.4m in type section at Nobbys Headland. Also 1.44m thick in the standard section in DM AWABA DDH 2 (details given).||Of Newcastle Coal Measures||Conformably overlies Lambton Formation. Overlain by Adamstown Formation.|Tuff, tuffaceous sandstone, tuffaceous siltstone, claystone, chert.|14-JAN-15
14198|Nobbys Tuff|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian|Appears as Nobby's Tuff in Fig.2.||Unit in Newcastle Coal Measures.||||
14198|Nobbys Tuff|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin. CA-TIMS ages of 255.02 and 255.26 Ma (Metcalfe etal., 2015). Corresponding to APP5 zone (Lopingian).||Unit of Clifford Formation.||||
14198|Nobbys Tuff|70878|5|Briefly described|p710-712, p715 Fig.9, p723|Permian|Permian|Hunter Valley. 2.22m thick in Amoco Wybong 1 well. Calibration of palynological ages. Other radiometric age given.|255.02 +/- 0.03 Ma (Metcalfe et al., 2015).|Newcastle Coal Measures.||Overlies Lambton Formation. Is overlain by Adamstown Formation.||
14198|Nobbys Tuff|71701|5|Briefly described|p159, p169-p171||||255.02 +/- 0.03 Ma and 255.26 +/- 0.07 Ma|Newcastle Coal Measures||||10-FEB-23
14198|Nobbys Tuff|73163|6|Mentioned|p467|||Sydney Basin. Correlated with ash layers in the 'Fair Hill Formation equivalent'.||||||
14198|Nobbys Tuff|73304|5|Briefly described|p65-67, p75|Wuchiapingian|Wuchiapingian|Dating by U-Pb CA-TIMS method. Constitutes a regional marker horizon. [Also listed as belonging to Clifford Formation, Wollombi Coal Measures].|255.26 +/- 0.31 Ma, 255.02 +/- 0.30 Ma|Newcastle Coal Measures||||
14198|Nobbys Tuff|73472|6|Mentioned|p129|Wuchiapingian|Wuchiapingian|Sydney Basin.|255.26-255.02 Ma|||||
14209|Nolan Dolerite|29901|4|Described|Table 1|||||||||
14209|Nolan Dolerite|36220|5|Briefly described|p95|||||||||
14209|Nolan Dolerite|36222|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic.||||||
14209|Nolan Dolerite|42896|5|Briefly described|p55|||||||||
14234|Nootumbulla Sandstone|13995|5|Briefly described|p81, p95|||Gnalta Shelf: platform deposits associated with Delamerian Orogeny. Has a trilobite fauna similar to that of the Pacoota Sandstone; assigned to the SE China Province.|||||Coarse siliciclastics.|
14234|Nootumbulla Sandstone|22671|5|Briefly described|Fig2p837|Early Ordovician|Late Cambrian|Of the Mootwingee Group. Sandstone, shale, siltstone.||||||17-JAN-06
14234|Nootumbulla Sandstone|22857|5|Briefly described|p120, p408 App. 1 Tb. A1.4.|Early Ordovician|Late Cambrian|Of the Mootwingee Group. Sandstone, shale, siltstone. Max. thickness: 153m. Geological Province: Kanmantoo Fold Belt.||||||
14234|Nootumbulla Sandstone|22858|6|Mentioned|Fig14.7bp90-1|||||||||
14234|Nootumbulla Sandstone|23245|4|Described|p120|Datsonian|Payntonian|||||||
14234|Nootumbulla Sandstone|23469|5|Briefly described|p 319|||Parent: Mootwingee Group.||||||27-NOV-08
14234|Nootumbulla Sandstone|29991|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|||||||
14234|Nootumbulla Sandstone|30908|6|Mentioned|Map legend|Late Cambrian|Late Cambrian|Part of Mootwingee Group||||||
14234|Nootumbulla Sandstone|31572|6|Mentioned|Fig.|||Correlation chart 1. U.Cambrian||||||
14234|Nootumbulla Sandstone|32671|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
14234|Nootumbulla Sandstone|32677|6|Mentioned|p4|||||||||
14234|Nootumbulla Sandstone|33004|6|Mentioned|Fig.8|||||||||
14234|Nootumbulla Sandstone|33738|6|Mentioned|p46|||||||||
14234|Nootumbulla Sandstone|34469|6|Mentioned|p108|||Ordovician||||||
14234|Nootumbulla Sandstone|35118|6|Mentioned|Fig.5|||||||||
14234|Nootumbulla Sandstone|38692|6|Mentioned|p139|||||||||
14234|Nootumbulla Sandstone|39214|6|Mentioned|p10|||||||||
14234|Nootumbulla Sandstone|39319|6|Mentioned|p353|||||||||
14234|Nootumbulla Sandstone|40136|5|Briefly described|p34|||||||||
14234|Nootumbulla Sandstone|40810|5|Briefly described|p14|||[Originally entered for NT. CEBMar95]||||||
14234|Nootumbulla Sandstone|41810|6|Mentioned|p111|||||||||
14234|Nootumbulla Sandstone|42206|5|Briefly described|p257|||See also Fig.1||||||
14234|Nootumbulla Sandstone|42354|6|Mentioned|p20|||||||||
14234|Nootumbulla Sandstone|43501|14|Not recorded|Map Legend||Late Cambrian|(Provisional Edition) Part of Mootwingee Group||||||
14234|Nootumbulla Sandstone|43502|14|Not recorded|Map Legend||Late Cambrian|(Provisional Edition) Part of Mootwingee Group (U.U.Camb)||||||
14234|Nootumbulla Sandstone|43704|5|Briefly described|Fig.1,p68|||||||||
14234|Nootumbulla Sandstone|50129|5|Briefly described|p16|Late Cambrian|Late Cambrian|Of the Mootwingee Group.||||||
14234|Nootumbulla Sandstone|62787|5|Briefly described|p81|Late Cambrian|Late Cambrian|Basal unit of Mutawintji Group. Underlain by Gnalta Group.||||||07-FEB-11
14234|Nootumbulla Sandstone|62793|4|Described|p269 Fig.2, p270, p271, p272|Late Cambrian|Late Cambrian|Near Mount Wright. Coarse siliciclastics with thin limestone interval containing Latest Cambrian (Payntonian) conodonts.||Lowest unit of Mutawintji (formerly Mootwingee) Group.||Underlies Bynguano Quartzite.||21-MAR-12
14234|Nootumbulla Sandstone|62795|5|Briefly described|p347, p349 Fig.2|Late Cambrian|Late Cambrian|Basal unit of Mutawintji Group. Unconformably overlies Gnalta Group and underlies Bynguano Quartzite. Payntonian-Datsonian Stage of Late Cambrian.||||||
14234|Nootumbulla Sandstone|63121|5|Briefly described|p225 Fig. 2|Late Cambrian|Late Cambrian|Max. age is Datsonian. In the Koonenberry Belt, western NSW.||||||13-MAR-07
14234|Nootumbulla Sandstone|63789|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Mootwingee Group. Feldspathic sandstone; includes some limestone and basal conglomerate resembling the polished quartz pebble conglomerate (Burkes Cave Conglomerate) of Scopes Ranges.||||||
14234|Nootumbulla Sandstone|64671|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|Of the Mootwingee Group. This includes some limestone and basal conglomerate near Comarto on this map.||||||
14234|Nootumbulla Sandstone|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Of the Mutawintji Group. Grey, yellow and green feldspathic sandstone with minor limestone; brachiopod, trilobite and conodont fossils; oolites and oncolites; Rusophycus, Skolithos and other trace fossils.||||||30-JAN-12
14234|Nootumbulla Sandstone|64680|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Of Mootwingee Group. Includes some limestones and basal conglomerate.||||||
14234|Nootumbulla Sandstone|64685|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Equivalents of Nootumbulla Formation. Quartz sandstone, dolomite, limestone and basal conglomerate.||||||
14234|Nootumbulla Sandstone|64686|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Of Mootwingee Group. Includes some limestone and basal conglomerate.||||||
14234|Nootumbulla Sandstone|66623|1|Redefined|p128, pp134-138, pp143-145.|Late Cambrian|Late Cambrian|Named by Warris (1967), described by Shergold (1971); redefined in this study. Correlated with Funeral Creek Limestone on basis of conodonts, and assumed to be contemporaneous with lower Scropes Range, Hummock and Morden Formations. Also contains trilobites and brachiopods. Is the oldest fossiliferous formation in the Mutawintji Group. Thickness varies laterally.||Unit in Mutawintji Group.||Overlies Nuchea Conglomerate. Is overlain by Bynguano Quartzite.|Interbedded red shales, conglomerate lenses, and fossiliferous grey, yellow and green sandstones, initially feldspathic but becoming more quartzose towards the top; basal polished quartz pebble conglomerate. Local thin limestone horizon.|25-SEP-13
14234|Nootumbulla Sandstone|66918|5|Briefly described|Map legend|||||Unit in Mutawintji Group.||Map key suggests: Overlies Scropes Range Formation, is overlain by Bynguano Quartzite.|Folded and weakly cleaved feldspathic sandstone, interbedded with minor limestone; includes a basal polished quartz pebble conglomerate; regionally metamorphosed to prehnite-pumpellyite facies.|25-SEP-13
14234|Nootumbulla Sandstone|66929|5|Briefly described|Map legend|Early Ordovician|Late Cambrian|||Unit in Mootwingee Group.|||Sandstone; local limestone, basal conglomerate.|
14234|Nootumbulla Sandstone|67322|4|Described|p8-9, p13; Fig.5|Stage 10||Redefined by Percival, in Greenfield et al. (2010). The type area is on the east limb of the Gnalta Syncline. Age determined from fossils common throughout. Prolific fauna; many trilobites remain undescribed. Approximately 150-200m thick. Occurs in the Mount Wright-Mutawintji region.||Of the Mutawintji Group.||Overlies Nuchea Conglomerate. Overlain conformably by the Bynguano Quartzite. Correlated with Scropes Range Formation.|Interbedded red shales, conglomerate lenses, and sandstones (initially feldspathic but becoming more quartzose towards the top).|22-FEB-18
14234|Nootumbulla Sandstone|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Folded and weakly cleaved feldspathic sandstone, interbedded with minor limestone, includes a basal polished quartz pebble conglomerate.|
14234|Nootumbulla Sandstone|70838|5|Briefly described|p269 Fig.3, p270|Cambrian|Cambrian|Koonenberry Belt. Contains Datsonian conodont and trilobite fossils.|488-485 Ma.|Mutawintji Group.||Overlies Bilpa Conglomerate.||
14280|North Ridge Basalt|22773|6|Mentioned|p348|||||||||
14280|North Ridge Basalt|22857|6|Mentioned|p348|Cenozoic|Cenozoic|On Lord Howe Island.||||||19-NOV-08
14280|North Ridge Basalt|36958|3|Fully described|p160|Miocene|Miocene|Overlies Roach Island Tuff. Lavas. Age: 6.62-7.20 +/- 0.22Ma.||||||15-MAR-06
14280|North Ridge Basalt|61943|5|Briefly described|Map Legend|||Overlies: Roach Island Tuff. Contains large crystals of plagioclase, clinopyroxene and rare olivine.||||||14-NOV-13
14280|North Ridge Basalt|61946|5|Briefly described|p108|Pleistocene|Tertiary|Also uses previous name of North Ridge Volcanics. Alkali olivine basalt. Scoria and ash beds. Phenocrysts of olivine, plagioclase and clinopyroxene.||||||14-NOV-13
14280|North Ridge Basalt|73136|6|Mentioned|p190-191|Messinian|Messinian|Lord Howe Island. Comprises the North Ridge. Geochron is K-Ar date from McDougall, Embleton, and Stone (1981) [eruption age?]. Lava beds are inclined at moderate angles.|6.9 Ma K-Ar|||||
14280|North Ridge Basalt|73554|4|Described|Map legend, back of map|Neogene|Neogene|Lord Howe Island. Part of the Lord Howe Volcanic Complex. Approximately 6.9 Ma. Commonly intruded by thin vertical dykes of various compositions and textures, most of which strike toward Mount Lidgbird. Underlies most of the island and is well exposed at the northern cliffs. Consists of many moderately-dipping lava flow deposits varying from 1-10 m thick. Lower portions were emplaced sub-aqueously.|ca 6.9 Ma|Lord Howe Volcanic Complex||Underlain by Roach Island Tuff.|Basalt with plagioclase and clinopyroxene phenocrysts, commonly vesicular and amygdaloidal; basalt pillow lava deposits and basaltic hyaloclastite (glassy) breccia.|
14280|North Ridge Basalt|73581|6|Mentioned|p28 Fig.8||||||||Includes volcaniclastics.|
14282|North Toukley Coal Lens|34270|6|Mentioned|p254|||||||||
14313|Noumea beds|721|5|Briefly described|Map legend|Frasnian|Frasnian|Of the Parry Group.  Green-black siltstone and mudstone with abundant thin to thick, grey and grey-green lithic wacke, pebbly wacke, pebbly lithic wacke and breccia.||||||
14313|Noumea beds|22857|5|Briefly described|p498 App.1 Tb.A1.7||Late Devonian|Of the Parry Group. Green-black siltstone and mudstone with abundant grey-green lithic wacke, pebbly lithic wacke and breccia. Max. thickness: >300m. Geological Province: Tamworth Forearc Basin.||||||
14313|Noumea beds|23051|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of Parry Group.||||||14-APR-08
14313|Noumea beds|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||14-APR-08
14313|Noumea beds|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
14313|Noumea beds|24605|6|Mentioned|p932 Fig.1|||Geological Province: New England Orogen.||||||
14313|Noumea beds|37987|6|Mentioned|p221|||||||||
14313|Noumea beds|38222|6|Mentioned|Fig.2|||||||||
14313|Noumea beds|41009|6|Mentioned|p4|||||||||
14313|Noumea beds|42728|4|Described|p5|||||||||
14313|Noumea beds|42866|5|Briefly described|Table 2, P12|||||||||
14313|Noumea beds|43091|5|Briefly described|Map legend|||Of Parry Group.||||||14-APR-08
14313|Noumea beds|43860|5|Briefly described|2||Late Devonian|= Baldwin Formation.||||||14-APR-08
14313|Noumea beds|61769|6|Mentioned|p96|||Chestnut et al, 1973.||||||
14313|Noumea beds|68003|5|Briefly described|p32 Fig.3-h, p139. |Famennian|Late Devonian|Tamworth Belt (North), New England Fold Belt. Coeval with Mostyn Vale and Lowana Formations.||Unit in Parry Group.||Is overlain by Keepit Conglomerate.|Interbedded massive and andesitic lithic wacke, pebbly wacke, laminated siltstone and mudstone.|
14313|Noumea beds|68005|5|Briefly described|p26 Fig.3-C, p54, p55 Photos.3-O,P, p59.|Late Devonian|Late Devonian|Central Block and Tamworth Belt, New England Fold Belt. Parts have moderate to strong magnetic response.||Basal unit in Parry Group.||Overlies Yarrimie Formation. Is overlain by Eungai Mudstone.|Interbedded massive and andesitic lithic wacke, pebbly wacke, laminated siltstone and mudstone.|
14315|Novice Sandstone Member|29900|6|Mentioned|p175|||||||||
14315|Novice Sandstone Member|29901|4|Described|Table 1|||||||||
14315|Novice Sandstone Member|29944|6|Mentioned|Fig.18|||||||||
14315|Novice Sandstone Member|30006|5|Briefly described|p36|||||||||
14315|Novice Sandstone Member|31128|6|Mentioned|Table 1|||||||||
14315|Novice Sandstone Member|32849|6|Mentioned|Table 1|||Permian||||||
14315|Novice Sandstone Member|34569|6|Mentioned|p8|||Permian||||||
14315|Novice Sandstone Member|36220|6|Mentioned|p50|||See also Table 1 & P50.||||||
14315|Novice Sandstone Member|36593|6|Mentioned|Table 2|||||||||
14315|Novice Sandstone Member|37089|6|Mentioned|p208|||||||||
14315|Novice Sandstone Member|39661|6|Mentioned|Fig.1|||||||||
14315|Novice Sandstone Member|42787|6|Mentioned|Table 1 P126|||||||||
14315|Novice Sandstone Member|42896|4|Described|p23|||of Eckersley Formation||||||
14320|Nowra Sandstone|22447|4|Described|p624, Fig.1 p624||Early Permian|Shallow marine||||||
14320|Nowra Sandstone|22578|6|Mentioned|p394|||||||||
14320|Nowra Sandstone|22591|5|Briefly described|Fig 1||Early Permian|||||||
14320|Nowra Sandstone|22601|6|Mentioned|413|Permian|Permian|Geol province Sydney Basin||||||
14320|Nowra Sandstone|22663|5|Briefly described|NSW97 - 1 p2||Late Permian|||||||01-MAR-10
14320|Nowra Sandstone|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Shoalhaven Group. Quartz arenite, some phyllitic clasts. Max. thickness: 90m. Geological Province: Sydney Basin.||||||
14320|Nowra Sandstone|22969|4|Described|p 21, Fig 2.2||Late Permian|||||||
14320|Nowra Sandstone|22970|5|Briefly described|Plate 6|Late Permian||||||||
14320|Nowra Sandstone|23015|6|Mentioned|p319||Permian|||||||
14320|Nowra Sandstone|23349|5|Briefly described|247|Permian|Permian|||||||
14320|Nowra Sandstone|23544|5|Briefly described|Fig 2 p358|||In the Shoalhaven Group||||||
14320|Nowra Sandstone|24079|5|Briefly described|p432|Permian|Permian|Of Maitland Group. Geological Province: Sydney Basin.||||||
14320|Nowra Sandstone|24552|5|Briefly described|p5 Fig.2|Wordian|Wordian|Overlies Wandrawandian Siltstone, overlain by Berry Formation. Geological Province: Southern Sydney Basin.||||||07-FEB-11
14320|Nowra Sandstone|29745|6|Mentioned|p7|||||||||
14320|Nowra Sandstone|29750|6|Mentioned|Fig.1|||||||||
14320|Nowra Sandstone|29752|3|Fully described|p29|||||||||
14320|Nowra Sandstone|29901|4|Described|Table 1|||||||||
14320|Nowra Sandstone|29992|6|Mentioned|Map legend|Permian|Permian|||||||
14320|Nowra Sandstone|29994|6|Mentioned|Map legend|Permian|Permian|||||||
14320|Nowra Sandstone|30449|6|Mentioned|p2|||Fauna||||||
14320|Nowra Sandstone|30450|6|Mentioned|Table 1|||Permian. Sydney Basin||||||
14320|Nowra Sandstone|31062|6|Mentioned|p478|||Permian. On Table||||||
14320|Nowra Sandstone|31081|6|Mentioned|p49|||See also P66, 69 & Fig. 2||||||
14320|Nowra Sandstone|31126|6|Mentioned|p19|||||||||
14320|Nowra Sandstone|31128|5|Briefly described|p5|||||||||
14320|Nowra Sandstone|31277|6|Mentioned|p3|||||||||
14320|Nowra Sandstone|32073|6|Mentioned|p21|||||||||
14320|Nowra Sandstone|32142|6|Mentioned|p22|||Mid-Permian||||||
14320|Nowra Sandstone|32266|6|Mentioned|p24|||||||||
14320|Nowra Sandstone|32769|6|Mentioned|p70|||||||||
14320|Nowra Sandstone|32945|6|Mentioned|p84|||Permian. See also PP85,90. Shoalhaven Gp.||||||
14320|Nowra Sandstone|32950|6|Mentioned|Table 31.1|||||||||
14320|Nowra Sandstone|33420|6|Mentioned|Fig.2|||||||||
14320|Nowra Sandstone|33974|6|Mentioned|p163|||||||||
14320|Nowra Sandstone|34039|6|Mentioned|p355|||||||||
14320|Nowra Sandstone|34059|6|Mentioned|Map legend|Permian|Permian|||||||
14320|Nowra Sandstone|34084|6|Mentioned|p368|||Perm.||||||
14320|Nowra Sandstone|34138|6|Mentioned|Cor.Chart|||Kazanian||||||
14320|Nowra Sandstone|34211|6|Mentioned|p32|||Permian||||||
14320|Nowra Sandstone|34334|3|Fully described|p363|||||||||
14320|Nowra Sandstone|34335|6|Mentioned|p369|||Permian||||||
14320|Nowra Sandstone|34434|6|Mentioned|Fig.5.25|||||||||
14320|Nowra Sandstone|34533|6|Mentioned|p1285|||||||||
14320|Nowra Sandstone|34566|6|Mentioned|p38|||||||||
14320|Nowra Sandstone|34568|6|Mentioned|p218|||Permian. Fauna||||||
14320|Nowra Sandstone|34845|6|Mentioned|p116|||Also Table 1.||||||
14320|Nowra Sandstone|35145|6|Mentioned|Fig.2|||||||||
14320|Nowra Sandstone|35160|6|Mentioned|p1|||||||||
14320|Nowra Sandstone|35284|6|Mentioned|Fig.1|||P37||||||
14320|Nowra Sandstone|35472|6|Mentioned|p8|||||||||
14320|Nowra Sandstone|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
14320|Nowra Sandstone|36042|6|Mentioned|Table 1|||||||||
14320|Nowra Sandstone|36147|6|Mentioned|Fig.2|||See also Plate 2.||||||
14320|Nowra Sandstone|36148|6|Mentioned|p266|||||||||
14320|Nowra Sandstone|36207|6|Mentioned|Text Fig.2|||||||||
14320|Nowra Sandstone|36220|3|Fully described|p18|||See also Table 1.||||||
14320|Nowra Sandstone|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
14320|Nowra Sandstone|36901|6|Mentioned|p18|||||||||
14320|Nowra Sandstone|36954|6|Mentioned|Table 3|||||||||
14320|Nowra Sandstone|37082|6|Mentioned|p161|||||||||
14320|Nowra Sandstone|37092|6|Mentioned|Table 2|||||||||
14320|Nowra Sandstone|37804|6|Mentioned|p55|||||||||
14320|Nowra Sandstone|38227|6|Mentioned|p426|||||||||
14320|Nowra Sandstone|38690|6|Mentioned|p287|||||||||
14320|Nowra Sandstone|38797|6|Mentioned|p248|||||||||
14320|Nowra Sandstone|39267|6|Mentioned|p237|||||||||
14320|Nowra Sandstone|39287|6|Mentioned|p20|||||||||
14320|Nowra Sandstone|39288|6|Mentioned|p63|||||||||
14320|Nowra Sandstone|39289|4|Described|p77|||See also P78||||||
14320|Nowra Sandstone|39290|6|Mentioned|p95|||Palaeogeography map Fig. 5.9||||||
14320|Nowra Sandstone|39304|6|Mentioned|Photo 19.1|||||||||
14320|Nowra Sandstone|39305|5|Briefly described|p379|||Fossil occurrences.||||||12-MAR-09
14320|Nowra Sandstone|39307|6|Mentioned|Table 22.1|||||||||
14320|Nowra Sandstone|39308|6|Mentioned|p524|||||||||
14320|Nowra Sandstone|40166|6|Mentioned|Table 1|||||||||
14320|Nowra Sandstone|40256|6|Mentioned|p306|||||||||
14320|Nowra Sandstone|40591|6|Mentioned|p323|||||||||
14320|Nowra Sandstone|40872|6|Mentioned|p33|||||||||
14320|Nowra Sandstone|41475|6|Mentioned|p69|||||||||
14320|Nowra Sandstone|41580|6|Mentioned|Table 1|||||||||
14320|Nowra Sandstone|41666|6|Mentioned|p18|||||||||
14320|Nowra Sandstone|41832|6|Mentioned|Fig.2|||||||||
14320|Nowra Sandstone|42821|6|Mentioned|p75|||||||||
14320|Nowra Sandstone|42848|5|Briefly described|Fig.2 p530|||Of the Conjola Subgroup (Shoalhaven Group). Caps the Snapper Point Formation (at Mt Edwards).||||||09-MAY-05
14320|Nowra Sandstone|42925|5|Briefly described|Table 18||Late Permian|||||||
14320|Nowra Sandstone|42974|5|Briefly described|p193|||Of Shoalhaven Group.||||||12-MAR-09
14320|Nowra Sandstone|42994|6|Mentioned|p264|||||||||
14320|Nowra Sandstone|43081|5|Briefly described|p172|||Of Shoalhaven Group.||||||12-MAR-09
14320|Nowra Sandstone|43194|5|Briefly described|p128, p129 Tb. 8.3|Middle Permian|Middle Permian|Quartzose sand. Of Shoalhaven Group, southern Sydney Basin.||||||
14320|Nowra Sandstone|43344|14|Not recorded|p187|||||||||
14320|Nowra Sandstone|43345|14|Not recorded|p3||Triassic|||||||
14320|Nowra Sandstone|43346|2|Defined|p2,5 Map|||||||||
14320|Nowra Sandstone|43349|14|Not recorded|Map|||||||||
14320|Nowra Sandstone|43383|14|Not recorded|Fig.5,Fig.3||Permian|||||||
14320|Nowra Sandstone|43385|14|Not recorded|p179||Late Permian|||||||
14320|Nowra Sandstone|43465|14|Not recorded|Map Legend||Permian|||||||
14320|Nowra Sandstone|43474|14|Not recorded|p57|||||||||
14320|Nowra Sandstone|43475|14|Not recorded|p553||Permian|||||||
14320|Nowra Sandstone|43479|14|Not recorded|p189,218||Kungurian|||||||
14320|Nowra Sandstone|43491|14|Not recorded|pVII/50||Permian|||||||
14320|Nowra Sandstone|43677|6|Mentioned|p319||Permian|||||||
14320|Nowra Sandstone|43893|14|Not recorded|p202||Permian|||||||
14320|Nowra Sandstone|43981|1|Redefined|p3,24||Permian|||||||
14320|Nowra Sandstone|44244|6|Mentioned|p174|||||||||
14320|Nowra Sandstone|44282|14|Not recorded|p.15,17-19;Pl.3|||Porous interbeds found in Stockyard Mt No.1 Well.||||||
14320|Nowra Sandstone|44861|14|Not recorded|226,229||Permian|||||||
14320|Nowra Sandstone|45006|14|Not recorded|Tb.1,p5,32-3,87,89,|||p94-5,101,103,118,18,142,144.||||||
14320|Nowra Sandstone|45090|6|Mentioned|p27|||Relationship of rock units||||||
14320|Nowra Sandstone|48940|6|Mentioned|p99|||||||||
14320|Nowra Sandstone|49644|5|Briefly described|Table|||||||||
14320|Nowra Sandstone|60281|4|Described|p9, p59|Late Permian|Late Permian|Of the Maitland Group.  Overlain by Berry Siltstone. Age: 267-265Ma.  Geological Province: Sydney Basin.||||||
14320|Nowra Sandstone|60285|4|Described|p182 Fig.2|Artinskian|Sakmarian|Of the Shoalhaven Group. Overlies Wandrawandian Siltstone. Overlain by Berry Siltstone. Nearshore marine and coastal. Geological Province: Sydney Basin.||||||
14320|Nowra Sandstone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Shoalhaven Group. Marine deposits of reworked clean quartzose sandstones with excellent reservoir potential. Geological Province: Sydney Basin||||||
14320|Nowra Sandstone|61609|4|Described|p239, p240, p240 Tb. 1, p241, p244, p247|Permian|Permian|Of Shoalhaven Group. Includes Purnoo Conglomerate Member. Overlies Wandrawandian Siltstone, overlian by Berry Siltstone. Thick: 40m. Geol Prov: Sydney Basin. Correlated with Muree Sandstone also. See p240 for more info.||||||07-FEB-11
14320|Nowra Sandstone|61612|6|Mentioned|p272, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. NSW.||||||12-MAR-09
14320|Nowra Sandstone|62043|6|Mentioned|p438 Fig.2. |Late Permian|Late Permian|Southern Sydney Basin.||Unit in Shoalhaven Group.||Overlies Wandrawandian Siltstone. Is overlain by Berry Siltstone.||
14320|Nowra Sandstone|63461|5|Briefly described|p863|||Overlies Wandrawandian Sandstone. Geological Province: Sydney Basin. see also Nowra sandstone.||||||10-DEC-07
14320|Nowra Sandstone|63773|6|Mentioned|p1059|||Geological Province: Sydney Basin.||||||07-APR-09
14320|Nowra Sandstone|64631|5|Briefly described|p48 Fig.4.|Roadian|Roadian|Sydney Basin.||||Overlies Wandrawandian Siltstone. Is overlain by Berry Siltstone.||
14320|Nowra Sandstone|64877|5|Briefly described|p296|Permian|Permian|Southern Sydney Basin.||Shoalhaven Group.||||
14320|Nowra Sandstone|66300|6|Mentioned|p64.|Permian|Permian|||Unit in Shoalhaven Group.||Unconformably overlies Tullyangela Granite.||
14320|Nowra Sandstone|66577|6|Mentioned|p997 Fig.2, pp1001-1002.|Permian|Permian|Isopachs of this unit and the Wandrawandian Siltstone show distinct thickening into the Camden Syncline. The authors cite this as support for an extensional graben system in the central Sydney Basin in early-mid Permian.||Unit in Shoalhaven Group.||Overlies Wandrawandian Siltstone. Is overlain by Berry Siltstone.||
14320|Nowra Sandstone|67500|6|Mentioned|p18 Fig.6|||||||Underlies Berry Formation.||01-MAY-12
14320|Nowra Sandstone|68003|5|Briefly described|p41.|||Southern Sydney Basin. A near-shore sand-sheet.||||Is overlain by Berry Siltstone.||
14320|Nowra Sandstone|68592|5|Briefly described|p1779|Permian|Permian|||Unit in Shoalhaven Group.||Overlies Wandrawandian Siltstone. Is overlain by Berry Siltstone.||
14320|Nowra Sandstone|69297|6|Mentioned|p501, p502 fig 5.43|Capitanian|Capitanian|Sydney Basin.||Shoalhaven Group||Overlies and interfingers with the Wandrawandian Siltstone. Overlain by the Berry Siltstone.||
14320|Nowra Sandstone|70661|3|Fully described|p4, p161, p165, p167 - p174|Kungurian|Kungurian|Mistakenly called Nowra Formation on p172. Named for Nowra Township. Previously referred to as the Nowra Grits and included in the Upper Marine series of Stonier (1891) or the Megalong Conglomerate of Rose (1966a). Previously unsuccessfully (due to lack of structural trap and poor reservoir quality) drilled for petroleum. A disconformity occurs inside this unit.  Distribution, geomorphology, depositional environment, distinguishing characteristics, structure, fossil assemblage discussed. Type section mentioned. 25m- 80m thick. lithology discussed in great detail. Deposited in a shallow marine nearshore environment. Age derived from biostratigraphy and unit relationships.   See also p181, p182, p243.|ca. 272 Ma (biostratigraphy)|Shoalhaven Group|Purnoo Conglomerate Member|Conformably overlain by Berry Siltstone, Illawarra Coal Measures, conformably overlies Wandrawandian Formation, Snapper Point Formation.|Quartzose, locally micaceous, fine to coarse grained sandstone (sublitharenite) that is commonly pebbly and contains pebble conglomerate beds and lenses.|
14320|Nowra Sandstone|71303|5|Briefly described|map legend|Guadalupian|Guadalupian|Of Sydney Basin.||Of Shoalhaven Group.|Includes Purnoo Conglomerate Member.||White to light grey, cross-bedded quartzose fine to medium-grained sandstone, pebbly sandstone, matrix- to clast-supported pebble conglomerate; micaceous locally. Rare bioturbation and rare marine macrofossils.|
14320|Nowra Sandstone|71408|5|Briefly described|p1029, p1031|Permian|Permian|Marine foreshore deposits.|||||Sub-horizontally stratified sandstone with pebble layers up to 10cm thick.|
14320|Nowra Sandstone|71538|6|Mentioned|p54 fig 2, p62|Roadian|Roadian|Sydney Basin. Upper shoreface depositional environment.||||Overlies the Wandrawandian Siltstone. Overlain by the Berry Formation.||
14320|Nowra Sandstone|71542|5|Briefly described|p25, 26|Permian|Permian|Of southern Sydney Basin.||Unit of Shoalhaven Group.||Overlain by Berry Formation gradationally. Underlain by Wandrawandian Siltstone.||20-OCT-21
14320|Nowra Sandstone|73304|6|Mentioned|p78|||||||||
14320|Nowra Sandstone|73421|4|Described|p1, p2 Fig.1, p3, p5, p16-20|Wordian|Wordian|Sydney Basin, southern. Early Wordian. Deposited in a range of shoreline settings, from offshore through foreshore to shoreface environments. Transition from Wandrawandian Siltstone to Nowra Sandstone is interpreted to be slightly diachronous across the Roadian-Wordian boundary, may extend into late Roadian. Previously with Murree Sandstone based on sedimentary facies and marine faunas. Misspelt as Nowra Sanstone p2 Fig.1.||Shoalhaven Group||Conformably overlies Wandrawandian Siltstone, underlies Berry Siltstone.|Fine to coarse grained, often pebbly quartzose sandstone, variably fossiliferous.|
14320|Nowra Sandstone|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Shoalhaven Group.||Overlies Wandrawandian Siltstone. Is overlain by Berry Formation.||
14320|Nowra Sandstone|73625|6|Mentioned|p2|Permian|Permian|Southern coalfield, Sydney Basin.||||Is overlain by Berry Siltstone.||
14339|Nulla Nulla Sand Member|29897|6|Mentioned|p296|||||||||
14339|Nulla Nulla Sand Member|30996|2|Defined|p50|early Holocene|late Pleistocene|Upper Pleistocene to Lower Holocene||||||
14339|Nulla Nulla Sand Member|40439|6|Mentioned|p380|||||||||
14339|Nulla Nulla Sand Member|42966|5|Briefly described|p408|||See also Nulla Sand Member p239||||||
14383|Numinbah Valley Formation|30687|4|Described|p65|||Tertiary age||||||
14383|Numinbah Valley Formation|33756|5|Briefly described|p263|||Refers McTaggart (1961)||||||
14383|Numinbah Valley Formation|39445|5|Briefly described|Table 14|||||||||
14383|Numinbah Valley Formation|44784|14|Not recorded|p12||Tertiary|Unit of Lamington Group.||||||
14383|Numinbah Valley Formation|44813|14|Not recorded|p80||Tertiary|||||||
14383|Numinbah Valley Formation|61155|5|Briefly described|p19|Early Miocene|Late Oligocene|Overlain by the Lamington Group; overlies the Allandale Granite. Age: Thickness: 30m. In the Brisbane region.||||||
14383|Numinbah Valley Formation|69599|5|Briefly described|p595|Miocene|Miocene|Gold Coast hinterland and MacPherson Ranges. Up to 30m thick. Contains dicotyledonous leaves.||||Is overlain by Lamington Volcanics.|Shale and mudstone.|
14394|Nungar beds|22815|6|Mentioned|p18|Ordovician|Ordovician|||||||
14394|Nungar beds|24005|5|Briefly described|p293|Ordovician|Ordovician|||||||
14394|Nungar beds|42294|6|Mentioned|p15|||See also P24||||||
14394|Nungar beds|44092|5|Briefly described|map legend|Ordovician|Ordovician|Of3||||||
14394|Nungar beds|45147|3|Fully described|M52|||Darriwilian? - Early Eastonian||||||
14394|Nungar beds|60078|6|Mentioned|Map Legend|Ordovician|Ordovician|||||||
14398|Nungatta Granodiorite|22815|4|Described|p82|||||||||
14398|Nungatta Granodiorite|22878|6|Mentioned|p40|||||||||
14398|Nungatta Granodiorite|22879|5|Briefly described|map|Early Devonian|Early Devonian|Of the Candelo Supersuite. Hornblende-biotite granodiorite: grey, medium grained, weakly foliated; prominent hornblende crystals, plagioclase-rich.||||||13-JUN-14
14398|Nungatta Granodiorite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Candleo Supersuite. Hornblende-biotite granodiorite: grey, medium grained, weakly foliated; prominent hornblende crystals, plagioclase-rich.||||||13-JUN-14
14398|Nungatta Granodiorite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Candelo Supersuite. Hornblende-biotite granodiorite: Very highly magnetic. Up to 450 nT over outcrop, less magnetic (up to 220 nT) where buried. High K, low Th and U.||||||06-OCT-04
14398|Nungatta Granodiorite|23309|6|Mentioned|p440, App1|||G19 I-Type.||||||
14398|Nungatta Granodiorite|41850|6|Mentioned|p430|||||||||
14398|Nungatta Granodiorite|42827|6|Mentioned|p430|||of Candelo Supersuite||||||
14398|Nungatta Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Nungatta Suite.||||||
14398|Nungatta Granodiorite|68116|5|Briefly described|Appendix, Map 37.|Devonian|Silurian||||||Hornblende-biotite granodiorite: grey, medium grained, weakly foliated; prominent hornblende crystals; plagioclase-rich; I-type.|
14417|Nurri Group|730|6|Mentioned|p9, 23, 24.|Devonian|Devonian|Cobar Sub-basin, Darling Basin. Deep-water turbidite facies.||||||11-NOV-14
14417|Nurri Group|22768|5|Briefly described|p170|||||||||
14417|Nurri Group|22857|5|Briefly described|p170, p436 App. 1. Tb.A1.6|Early Devonian|Early Devonian|Lower part of Cobar Supergroup. Coarse-grained clastics and thick beds of sandstone. Geological Province: Cobar Basin.||||||
14417|Nurri Group|23095|5|Briefly described|p610 (table 1)|Early Devonian|Early Devonian|||||||
14417|Nurri Group|23096|6|Mentioned|p601 (Fig 1)|||Cobar Supergroup||||||
14417|Nurri Group|23101|5|Briefly described|p567 (Fig 1)|Silurian|Silurian|||||||
14417|Nurri Group|23171|6|Mentioned|p15,22,40|||||||||
14417|Nurri Group|23173|4|Described|Map Legend|||||||||
14417|Nurri Group|23734|5|Briefly described|p12 Fig. 1|||Includes Great Cobar Slate, Chesney Formation and Mouramba Group.||||||
14417|Nurri Group|35219|6|Mentioned|Fig.2|||||||||
14417|Nurri Group|35287|6|Mentioned|p6|||||||||
14417|Nurri Group|37798|6|Mentioned|p128|||||||||
14417|Nurri Group|37937|6|Mentioned|p147|||||||||
14417|Nurri Group|38292|3|Fully described|p3|||||||||
14417|Nurri Group|39083|6|Mentioned|p30|||||||||
14417|Nurri Group|39618|3|Fully described|p81|||||||||
14417|Nurri Group|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
14417|Nurri Group|40676|6|Mentioned|p28|||||||||
14417|Nurri Group|41090|6|Mentioned|Fig.1|||||||||
14417|Nurri Group|41138|6|Mentioned|Map legend|Pragian|Lochkovian|Lochkovian-Pragian||||||
14417|Nurri Group|41394|6|Mentioned|p10|||See also P38||||||
14417|Nurri Group|41410|5|Briefly described|p295|||||||||18-JAN-10
14417|Nurri Group|41821|6|Mentioned|p11 Fig.5|||Occurs in Cobar, Wrightville and Canbelego sheet areas||||||
14417|Nurri Group|41872|6|Mentioned|p8|||||||||
14417|Nurri Group|42144|6|Mentioned|p603|||||||||
14417|Nurri Group|42172|5|Briefly described|Fig.5 P167|||||||||
14417|Nurri Group|42208|6|Mentioned|Fig.1 P305|||||||||
14417|Nurri Group|42521|5|Briefly described|p15|||||||||
14417|Nurri Group|42566|5|Briefly described|p40, Fig.5 p11|||Supersedes "Cobar Group".||||||
14417|Nurri Group|42907|6|Mentioned|Fig.8, P8|||||||||
14417|Nurri Group|42983|6|Mentioned|p343|||||||||
14417|Nurri Group|43032|3|Fully described|p29|||Of Cobar Supergroup.||||||08-APR-09
14417|Nurri Group|43153|5|Briefly described|Map Legend|Pragian|Lochkovian|||||||
14417|Nurri Group|43263|6|Mentioned|Map Legend||Early Devonian|||||||
14417|Nurri Group|43757|5|Briefly described|p510|||||||||
14417|Nurri Group|43774|1|Redefined|p35-36||Devonian|||||||
14417|Nurri Group|46900|5|Briefly described|p15|||||||||
14417|Nurri Group|61905|5|Briefly described|p135|||Lower part of Cobar Supergroup - syn-rift sediments. Of Cobar Supergroup.||||||
14417|Nurri Group|64962|6|Mentioned|p202|||Sedimentary rocks, mainly siliciclastic facies.||||||
14417|Nurri Group|65469|5|Briefly described|p14, p15|Early Devonian|Late Silurian|Lachlan Orogen.|||Includes the Great Cobar Slate and the Chesney Formation.|||
14417|Nurri Group|68823|6|Mentioned|p376 Fig.3, p377, p378 Fig.4|Early Devonian|Early Devonian|A narrow strip of sedimentary rocks in eastern Cobar Basin. Derived from erosion of the Girilambone Group and intruding granite.|||Includes Chesney Formation and Great Cobar Slate.|||
14417|Nurri Group|69002|6|Mentioned|p14, Legend|||||||||
14417|Nurri Group|69042|6|Mentioned|map legends|Early Devonian|Late Silurian|Dcn. Lachlan Orogen. Belt of linear trends of low to moderate intensity. Sediments and tuff.||||||
14417|Nurri Group|69043|6|Mentioned|p79|||Cobar Basin, Lachlan Orogen.|||Chesney Formation.|||
14417|Nurri Group|69541|6|Mentioned|p645 Fig.1(b)|Early Devonian|Early Devonian|Lachlan Orogen.||||||
14417|Nurri Group|70821|5|Briefly described|p11|Early Devonian|Late Silurian|Typically non-magnetic.|||||Sandstone-dominated.|
14417|Nurri Group|70941|6|Mentioned|p98|||Cobar Basin.||||||
14417|Nurri Group|71039|5|Briefly described|p6, p19-20, p24-25, p29|Devonian|Silurian|Low metamorphic grade.|||Includes the Chesney Formation and the Great Cobar Slate.|||10-MAR-23
14417|Nurri Group|71285|5|Briefly described|p538-539, p548-p549|Late Silurian|Late Silurian|Cobar region. Part of the Cobar Basin fill.||Cobar Supergroup.|Great Cobar Slate, Chesney Formation.|||07-DEC-18
14417|Nurri Group|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Cobar Supergroup.|Great Cobar Slate, Chesney Formation.|||
14417|Nurri Group|71860|6|Mentioned|p6|Early Devonian|Late Silurian|||||||
14417|Nurri Group|72958|6|Mentioned|p5, p8, p60|||Deep water strata. Northern stratigraphic equivalent of Amphitheatre Group, 'lower'. Hosts the Peak Rhyolite.|||Includes Peak Rhyolite.|||
14417|Nurri Group|73143|6|Mentioned|p2|Devonian|Silurian||||Chesney Formation, Great Cobar Slate|||
14417|Nurri Group|73174|6|Mentioned|p1037|Lochkovian|Lochkovian|Cobar Basin. Represents syn-rift phase of sedimentation during rapid subsidence. Derived from the east from erosion of the Girilambone Group and early Silurian granites.||Cobar Supergroup||Overlain by and equivalent to Lower Amphitheatre Group and CSA Siltstone.||
14417|Nurri Group|73578|6|Mentioned|p2, p25, p28|||Cobar Basin.||Cobar Supergroup|Chesney Formation||Sandstone-dominated.|
14438|Nymboida Coal Measures|12597|6|Mentioned|p493 Fig.2|||||||||
14438|Nymboida Coal Measures|22857|4|Described|p273, p277, p540 App.1 Tb.A1.10|Middle Triassic|Middle Triassic|Lithic sandstone, siltstone, polymictic conglomerate, coal, rhyolite tuff and basalt. Rocks are a continuation of the Toogoolawah Group in the Esk Trough (Queensland), with diminishing volcanism. Max. thickness: >1km. See also p318 Fig. 22.10A.||||||
14438|Nymboida Coal Measures|22860|4|Described|p273,277,Fig20.2p278|||||||||
14438|Nymboida Coal Measures|22865|6|Mentioned|Fig22.9p317|||||||||
14438|Nymboida Coal Measures|22892|5|Briefly described|p7 fig6|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|23720|5|Briefly described|Map Legend|Triassic|Triassic|Quartz lithic sandstone (wacke and minor arenite), siltstone, polymictic conglomerate, coal, rhyolitic tuff, basalt.||||||15-DEC-04
14438|Nymboida Coal Measures|23799|5|Briefly described|p46|Late Triassic|Late Triassic|Originally included in the first defintion of the Clarence Basin (Elroy, 1962, 1969).  Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|23811|5|Briefly described|Map Legend|Ladinian|Anisian|Of Woogaroo Subgroup.  Lithic sandstone, (wacke, minor arenite), siltstone, polymictic conglomerate, coal, rhyolitic tuff, basalt.  Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
14438|Nymboida Coal Measures|23812|5|Briefly described|p35 Tb.4, p31|Middle Triassic|Middle Triassic|Maximum thickness: 2000m.  Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|23843|5|Briefly described|p456 Table 1|Triassic|Triassic|Geological Province: Clarence - Moreton Basin.  Maximum thickness: 1000m.||||||
14438|Nymboida Coal Measures|24127|5|Briefly described|p5|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|29869|6|Mentioned|p37|||||||||
14438|Nymboida Coal Measures|29988|6|Mentioned|Map legend|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|30784|6|Mentioned|p70|||List Fossil megafloras found||||||
14438|Nymboida Coal Measures|30785|6|Mentioned|p398|||||||||
14438|Nymboida Coal Measures|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|31276|6|Mentioned|p146|||Refers de Jersey (1959), McElroy (1959,1962)||||||
14438|Nymboida Coal Measures|31649|6|Mentioned|p63|||||||||
14438|Nymboida Coal Measures|31806|6|Mentioned|Map legend|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
14438|Nymboida Coal Measures|32801|6|Mentioned|p258|||||||||
14438|Nymboida Coal Measures|32803|6|Mentioned|Fig. 1|||||||||
14438|Nymboida Coal Measures|32838|6|Mentioned|p320|||||||||
14438|Nymboida Coal Measures|33381|6|Mentioned|p107|||||||||
14438|Nymboida Coal Measures|33476|6|Mentioned|p99|||||||||
14438|Nymboida Coal Measures|34010|6|Mentioned|Cor. chart|||M.Triassic||||||
14438|Nymboida Coal Measures|34340|4|Described|p457|||See also p458.||||||
14438|Nymboida Coal Measures|34400|5|Briefly described|p13|||||||||
14438|Nymboida Coal Measures|35161|6|Mentioned|p592|||||||||
14438|Nymboida Coal Measures|35647|6|Mentioned|p64|||||||||
14438|Nymboida Coal Measures|36045|6|Mentioned|p335|||||||||
14438|Nymboida Coal Measures|36327|6|Mentioned|p10|||||||||
14438|Nymboida Coal Measures|36570|6|Mentioned|p22|||||||||
14438|Nymboida Coal Measures|36954|6|Mentioned|p114|||||||||
14438|Nymboida Coal Measures|37065|6|Mentioned|p36|||||||||
14438|Nymboida Coal Measures|37112|4|Described|p298|||||||||
14438|Nymboida Coal Measures|37122|6|Mentioned|Table 1|||||||||
14438|Nymboida Coal Measures|37135|6|Mentioned|p300|||||||||
14438|Nymboida Coal Measures|37755|6|Mentioned|p79|||||||||
14438|Nymboida Coal Measures|37757|6|Mentioned|p13|||||||||
14438|Nymboida Coal Measures|38064|5|Briefly described|p41|||||||||
14438|Nymboida Coal Measures|38304|6|Mentioned|p83|||||||||
14438|Nymboida Coal Measures|38837|6|Mentioned|p235|||||||||
14438|Nymboida Coal Measures|40177|6|Mentioned|p52|||||||||
14438|Nymboida Coal Measures|40245|6|Mentioned|p182|||Mention p187||||||
14438|Nymboida Coal Measures|41059|6|Mentioned|p170|||||||||
14438|Nymboida Coal Measures|41591|5|Briefly described|p20|||||||||
14438|Nymboida Coal Measures|42182|5|Briefly described|p302|||||||||
14438|Nymboida Coal Measures|42248|6|Mentioned|Fig2 P399|||||||||
14438|Nymboida Coal Measures|42463|6|Mentioned|Fig.3 P170|||||||||
14438|Nymboida Coal Measures|42719|6|Mentioned|p15|||||||||
14438|Nymboida Coal Measures|42725|6|Mentioned|p24|||||||||
14438|Nymboida Coal Measures|42869|5|Briefly described|p33|||see also Fig.2 p32||||||
14438|Nymboida Coal Measures|43001|5|Briefly described|Fig.1,p118|||||||||
14438|Nymboida Coal Measures|43150|5|Briefly described|Map Legend||Triassic|Quartz-lithic sandstone, shale, polymictic conglomerate, coal, siltstone, rhyolite, tuff and basalt.  Esk Formation equivalent?||||||12-APR-05
14438|Nymboida Coal Measures|43344|14|Not recorded|p13|||Unconf.Overlain by Bundamba Group||||||
14438|Nymboida Coal Measures|43383|14|Not recorded|p23,24||Triassic|||||||
14438|Nymboida Coal Measures|43384|14|Not recorded|Map Legend||Triassic|||||||
14438|Nymboida Coal Measures|43736|6|Mentioned|p11||Triassic|||||||
14438|Nymboida Coal Measures|43881|1|Redefined|p6-7,11-27,80-5,147||Triassic|Incs. Basin Creek Fm, Cope's Creek Tuff, Bardool Clm, basal Clougher's Creek Fm. See also Lexicon.||||||
14438|Nymboida Coal Measures|43984|14|Not recorded|p139|||Probably equivalent to Ipswich Coal Measures.||||||
14438|Nymboida Coal Measures|44093|5|Briefly described|p72|Middle Triassic|Early Triassic|See also p73 Figure 7.3. Geological Province: Esk Trough.||||||
14438|Nymboida Coal Measures|44450|4|Described|p28 Table 7|Middle Triassic|Middle Triassic|Geological Province: Clarence-Moreton Basin. Max. thickness: 1000 m.||||||
14438|Nymboida Coal Measures|45150|6|Mentioned|p2|||||||||
14438|Nymboida Coal Measures|48917|6|Mentioned|p9|||Correlation||||||
14438|Nymboida Coal Measures|60079|5|Briefly described|Map Legend|Middle Triassic|Middle Triassic|Sandstone, siltstone, conglomerate, coal, rhyolitic tuff, basalt.||||||
14438|Nymboida Coal Measures|60281|5|Briefly described|page vi, p21|Middle Triassic|Middle Triassic|Sandstone, conglomerate, siltstone, claystone, coal, volcanics. Overlain by the Ipswich Coal Measures.  Max. thickness: >1000m.  Geological Province: Nymboida Basin which is overlain by the Ipswich Basin.  See also Figs.18 and 20 Appendix 1.||||||17-MAR-05
14438|Nymboida Coal Measures|60991|5|Briefly described|p39, p43, p47-49  |Middle Triassic|Middle Triassic||||Basin Creek, Cloughers Creek Formation.|||
14438|Nymboida Coal Measures|60992|6|Mentioned|p1, p9|Middle Triassic|Middle Triassic||||Basin Creek Formation.|||
14438|Nymboida Coal Measures|60993|6|Mentioned|p6 Fig. 2|||Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|60995|5|Briefly described|p51 Fig. 3|Middle Triassic|Middle Triassic|Sandstone, conglomerate, siltstone, claystone, coal, volcanics. Max. thickness: >1000m. Geological Province: Clarence-Moreton Basin. Coal Measures is written as C.M in text.||||||
14438|Nymboida Coal Measures|60997|5|Briefly described|p140 Fig. 2|||Overlain by the Bundamba Group. . Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|61001|6|Mentioned|p190 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|61002|5|Briefly described|p196 Fig. 1|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin (Cecil Plains Sub-basin) and Surat Basin. See also p202.||||||
14438|Nymboida Coal Measures|61004|5|Briefly described|p232 Fig. 2|Triassic|Triassic|Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|61006|5|Briefly described|p278 Figs. 1 and 2|Triassic|Triassic|Contain coal and carbonaceous shale. Geological Province: Clarence-Moreton Basin.||||||
14438|Nymboida Coal Measures|61310|4|Described|p16, p11 Fig. C2|Middle Triassic|Early Triassic|Sandstone, shale, conglomerate, felsic tuff, basalt and coal. Overlain by Ipswich Coal Measures; unconformably overlie the "Coffs Harbour Association". Max. thickness: ~1000m. Geol. Prov: Clarence-Moreton Basin. Equivalents are Chillingham Volcanics.||||||12-AUG-08
14438|Nymboida Coal Measures|61772|6|Mentioned|p128, p129 Fig. 4, p129||Middle Triassic|In New England Orogen. Contains tuffaceous sediments.||||||24-SEP-08
14438|Nymboida Coal Measures|63117|5|Briefly described|p156, p157|Middle Triassic|Middle Triassic|||||||
14438|Nymboida Coal Measures|63748|5|Briefly described|p21|||Overlie Bundamba Group (Marburg Subgroup).||||||07-FEB-11
14438|Nymboida Coal Measures|64298|5|Briefly described|p113|Middle Triassic|Early Triassic|Geological Province: Nymboida Sub-basin. Contains megafossils (Cycads of the Order Cycadales and Bennittitites of the extinct Order bennettitales (=Cycadioidales).||||||24-JUL-08
14438|Nymboida Coal Measures|68111|5|Briefly described|p966 Fig.1, p967|Middle Triassic|Triassic|Lower Triassic maximum age. Esk Trough. Contains macrofloras coeval with Esk Trough sediments to the north.||||||
14438|Nymboida Coal Measures|68679|5|Briefly described|p387, p392|Middle Triassic|Early Triassic|Southen margin of the Clarence-Moreton Basin. Correlated with the Esk Basin deposits; previously thought equivalent to the Ipswich Coal Measures or Chillingham Volcanics.||||||
14438|Nymboida Coal Measures|69297|5|Briefly described|p370, p386, p487 fig 5.38, p488|Lower Jurassic|Middle Triassic|Clarence-Moreton Basin. Gas prone source rocks are present. More than 1000m thick.|||||Sandstone, conglomerate, siltstones, claystone, coal and volcanics.|
14438|Nymboida Coal Measures|73306|5|Briefly described|p563-569, 572-575, 577-578|Late Triassic|Middle Triassic|Maximum thickness ~1,000m. It is displaced by a number of synsedimentary normal faults. Exact timing of deposition cessation is not known.|||Cloughers Creek Formation, Copes Creek Tuff, Bardool Conglomerate, Basin Creek Formation, Dalmally Basalt.|||
14438|Nymboida Coal Measures|73570|5|Briefly described|p911, p912 Fig.2, p914-916, p918-919|Carnian|Early Triassic|Probable southern continuation of the Esk Trough.|236+/-1 Ma maximum depositional age||||Includes thin granule conglomerate and quartzose sandstone.|
14445|Nyora Granite|42726|5|Briefly described|map legend|||500.||||||
14445|Nyora Granite|61964|3|Fully described|p14 Fig. 4, p37, p53, p92|Lochkovian|Pridoli|Of Rast Gp [?]. Initially thought to belong to Koetong Suite but its transitional S- to A-type character and Late Silurian age suggest otherwise. Varies from coarse-gr.alkali granite to megacrystic porph. microgranite, mod'ly mafic-leucocratic. Age: ~419.1Ma.||||||21-JAN-21
14445|Nyora Granite|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Coarsely crystalline granite with feldspar megacrysts to 10cm and rare metasedimentary xenoliths.||||||13-OCT-08
14445|Nyora Granite|63019|5|Briefly described|p920, p921 Fig.2|Lochkovian|Ludlow|Of Rast Group (?). Geological Province: Lachlan Orogen. similar age to Gurragong Volcanics.||||||21-JAN-21
14445|Nyora Granite|65469|5|Briefly described|p18 |Late Silurian|Late Silurian|Lachlan Orogen. Misspelt as the Nygora Granite on p18.||||||
14445|Nyora Granite|69161|5|Briefly described|Map legend|Early Devonian|Early Devonian||||||Coarsely crystalline granite with feldspar megacrysts to 10 cm and rare metasedimentary xenoliths.|
14445|Nyora Granite|70296|5|Briefly described|p1, p5-6, p10, p24|Lochkovian|Pridoli|Cargelligo district. Age is SHRIMP U-Pb date. Similar in age to the Gurragong Volcanics. Potentially related to the Ural Volcanics on the basis of dating.|419.1 +/- 2.5 Ma|||||21-JAN-21
14445|Nyora Granite|70777|5|Briefly described|p80|Lochkovian|Pridoli|Lachlan Orogen. Age is also provided in Colquhoun et al., 2005.|419.1 +/- 2.5 Ma (Black, 2005)|||||
14445|Nyora Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Coarsely crystalline granite to porphyritic microgranite with feldspar megacrysts to 10cm and rare metasedimentary xenoliths.|
14446|Nyrang Sandstone Member|23214|5|Briefly described|p129|||Of Wallace Shale.||||||
14446|Nyrang Sandstone Member|24249|5|Briefly described|p87|Pridoli|Pridoli|Top unit of the Wallace Shale||||||
14446|Nyrang Sandstone Member|33116|5|Briefly described|p221|||||||||
14446|Nyrang Sandstone Member|37727|4|Described|p92|||||||||
14446|Nyrang Sandstone Member|39331|6|Mentioned|p68|||||||||
14446|Nyrang Sandstone Member|40328|3|Fully described|p155|||||||||
14461|Oakdale Formation|13139|5|Briefly described|p4, p10|Bolindian|Gisbornian|Overlies the Ballingoole Limestone.||||||
14461|Oakdale Formation|22466|6|Mentioned|P8||Ordovician|||||||
14461|Oakdale Formation|22679|6|Mentioned|p 21|||||||||
14461|Oakdale Formation|22857|4|Described|p422 App. 1, Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Contains graptolites, brachiopods, conodonts. Max. thickness: 770m.||||||
14461|Oakdale Formation|23043|5|Briefly described|Map Legend|Eastonian|Eastonian|Of Cabonne Group.||||||04-MAR-09
14461|Oakdale Formation|23048|5|Briefly described|p11 table2|Early Silurian|Ordovician|||||||
14461|Oakdale Formation|23170|2|Defined|p47|Bolindian|Gisbornian|Age: late Gisbornian - Early Bolindian. Cabonne Group.||||||
14461|Oakdale Formation|23213|3|Fully described|p20, Fig.10|Bolindian|Darriwilian|Includes Angullong Tuff. NW and SE of Orange. Formerly the Oakdale group of Vandylee and Byrnes (1976). Of Cabonne Group.||||||28-AUG-08
14461|Oakdale Formation|23214|2|Defined|p70|Early Silurian|Eastonian|Of Cabonne Group. Overlying unit Waugoola Group. Underlying unit Byng Volcanics.  Lack of a complete type section as a result of faulting. Max. thickness 2000m.||||||
14461|Oakdale Formation|23334|6|Mentioned|4|||||||||
14461|Oakdale Formation|23739|6|Mentioned|p211|||||||||
14461|Oakdale Formation|24126|5|Briefly described|p95|||||||||
14461|Oakdale Formation|24398|4|Described|p261|Ordovician|Ordovician|Defined by Strusz (1960) for volcanic and sedimentary rocks in Bakers Swamp area.  Name used interchangeably with "Oakdale Formation" in this study.  Geological Province: Lachlan Fold Belt.||||||
14461|Oakdale Formation|29362|6|Mentioned|Table 1|||Upper Ordovician.||||||
14461|Oakdale Formation|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14461|Oakdale Formation|30099|6|Mentioned|Fig.2|||||||||
14461|Oakdale Formation|31161|5|Briefly described|PA2|||||||||
14461|Oakdale Formation|31543|6|Mentioned|p111|||||||||
14461|Oakdale Formation|32045|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14461|Oakdale Formation|32046|6|Mentioned|p115|||See also P125,187-189.||||||
14461|Oakdale Formation|32047|6|Mentioned|p13|||Mineralization||||||
14461|Oakdale Formation|32088|6|Mentioned|p5|||Refers Packham (1969)||||||
14461|Oakdale Formation|32154|6|Mentioned|p181|||Refers Strusz (1960)||||||
14461|Oakdale Formation|32485|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14461|Oakdale Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14461|Oakdale Formation|32672|6|Mentioned|p671|||||||||
14461|Oakdale Formation|33098|4|Described|p94|||Ord.-Sil. See also P95||||||
14461|Oakdale Formation|33611|6|Mentioned|p123|||See also P125. Now Group status.||||||
14461|Oakdale Formation|33733|6|Mentioned|p446|||||||||
14461|Oakdale Formation|33735|6|Mentioned|Fig.2|||||||||
14461|Oakdale Formation|34403|6|Mentioned|p138|||||||||
14461|Oakdale Formation|34404|6|Mentioned|Fig.3.4b|||||||||
14461|Oakdale Formation|34405|6|Mentioned|p123|||Fig.3.9||||||
14461|Oakdale Formation|35118|6|Mentioned|p439|||||||||
14461|Oakdale Formation|37727|6|Mentioned|p28|||See also Fig.1.||||||
14461|Oakdale Formation|40136|6|Mentioned|p32|||||||||
14461|Oakdale Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
14461|Oakdale Formation|43476|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
14461|Oakdale Formation|43479|14|Not recorded|p79,95f||Ordovician|||||||
14461|Oakdale Formation|43517|14|Not recorded|p147-161,Map Pl XII|Early Silurian|Late Ordovician|Same age as Sofala Volcanics||||||
14461|Oakdale Formation|43528|2|Defined|p128,131,133,135||Ordovician|||||||
14461|Oakdale Formation|43640|5|Briefly described|Map Legend||Ordovician|||||||
14461|Oakdale Formation|43653|5|Briefly described|Map Legend||Ordovician|||||||
14461|Oakdale Formation|43782|5|Briefly described|Map Legend|Llandovery|Eastonian|Of Cabonne Group.||||||04-MAR-09
14461|Oakdale Formation|44093|5|Briefly described|p56|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt.||||||
14461|Oakdale Formation|50590|5|Briefly described|Map Legend|Ordovician|Ordovician|Of the Cabonne Group. Andesitic-latitic volcaniclastic siltstone, sandstone, conglomerate, breccia.||||||29-JUN-04
14461|Oakdale Formation|60332|5|Briefly described|p937|Ordovician|Ordovician|Volcaniclastics. Has faulted contact with Camelford Limestone.||||||
14461|Oakdale Formation|60417|5|Briefly described|p157||Ordovician|Contains allochthonous limestones.||||||
14461|Oakdale Formation|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p152|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt, LFB. Consists of distal turbidites with less common debris-flow deposit. Upper in the unit are Eastonian graptolites. Late Darriwilian is indicated by conodonts.||||||22-SEP-16
14461|Oakdale Formation|63283|6|Mentioned|p194 Fig. 2, p199, p200-202|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
14461|Oakdale Formation|63286|5|Briefly described|p294 Fig. 1, p308 Fig. 9|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt. Consists of mafic sandstone, siltstone, conglomerate and mudstone.||||||07-FEB-11
14461|Oakdale Formation|63288|6|Mentioned|p361|||Geological Province: Molong Volcanic Belt.||||||
14461|Oakdale Formation|63290|6|Mentioned|p393 Tb. 1, p395|||Unconformably overlain by Anson Formation.||||||
14461|Oakdale Formation|63293|6|Mentioned|p468 Fig. 2|Bolindian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
14461|Oakdale Formation|64015|6|Mentioned|p67|Darriwilian|Darriwilian|||||||
14461|Oakdale Formation|64826|5|Briefly described|p1040 Tb. 1, p1043-4|Bolindian|Eastonian|Of the Cabonne Group. Unconformably overlain by the Nandillyan Limestone. Turbidites.||||||04-MAR-09
14461|Oakdale Formation|64963|5|Briefly described|p182 Fig. 2, p183|||Deep marine deposits. See also p184.||||||22-APR-09
14461|Oakdale Formation|67322|5|Briefly described|Fig.5; p25|Katian|Darriwilian|Macquarie Arc. Strusz (1960). Type area between Neurea and Dripstone, SE of Wellington. Contains conodonts (Eastonian and Darriwilian) and trilobites (Gisbornian). Includes carbonate rocks at 'Barham Winchester' 10km northeast of Molong, and limestones in the Bakers Swamp area. Areas on the western outcrop have recently been reinterpreted.|||||Volcaniclastic conglomeratic facies deposited as mass flows, turbiditic sandstone, and siltstone; limestone.|22-FEB-18
14461|Oakdale Formation|67821|6|Mentioned|p150|Ordovician|Ordovician|Molong Volcanic Belt.||||||08-FEB-18
14461|Oakdale Formation|67847|6|Mentioned|p20, p33-p34|||Macquarie Arc, Lachlan Orogen.||||||
14461|Oakdale Formation|68003|5|Briefly described|p24 Fig.3-e, p147. |Eastonian|Darriwilian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Cabonne Group.|||Basalt, basaltic andesite, latite lava and intrusions; volcaniclastic breccia, conglomerate, sandstone and siltstone; minor allochthonous limestone.|
14461|Oakdale Formation|68004|6|Mentioned|p43, p115.|Late Ordovician|Late Ordovician|Mineral potential and level of certainty are discussed.||||||
14461|Oakdale Formation|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
14461|Oakdale Formation|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 4 volcanic unit. Age: ranges from late Eastonian to mid Bolindian (Bo3).|c. 449-443 Ma, in part|Cabonne Group||||
14461|Oakdale Formation|70684|6|Mentioned|p3, p18, p25, p74|Late Ordovician|Late Ordovician|||||Is faulted against Fairbridge Volcanics.||
14461|Oakdale Formation|70754|5|Briefly described|p450 Fig.2, p451, p462-464|Katian|Katian|East of Molong. Fossil species named.|||||Contains dark grey calcareous marls of late Eastonian age interbedded with siltstones.|
14461|Oakdale Formation|71600|6|Mentioned|p23 Fig 1|Ordovician|Ordovician|Geological province: Lachlan Fold Belt.||Unit of Cabone Group.||||
14461|Oakdale Formation|72263|5|Briefly described|p515-517|Late Ordovician|Late Ordovician|Geological province: Lachlan Orogen. Misspelt as Oakadale on p517.||||Fault contact with Mitchell Formation and Fairbridge Volcanics.||
14461|Oakdale Formation|72503|6|Mentioned|p31|||H. holodentata biozone[?] documented in the unit.|||||Includes allochthonous limestones.|
14461|Oakdale Formation|73299|6|Mentioned|p1103, p1104 Fig.10, p1105|Upper Ordovician|Ordovician|Macquarie Arc. Molong High.||||Underlies the Mirrabooka Formation, Camelford Limestone, Dripstone Formation.||
14466|Oaklands Coal Measures|32413|6|Mentioned|p89|||||||||
14466|Oaklands Coal Measures|43467|14|Not recorded|p13|||(Attrib.to BMR Bulletin 19)Name is invalid||||||
14466|Oaklands Coal Measures|43520|14|Not recorded|p13|||||||||
14480|Oberon Granite|22728|5|Briefly described|p599 table1||Carboniferous|||||||
14480|Oberon Granite|23214|3|Fully described|p259|Carboniferous|Carboniferous|Intrudes the Adaminaby Group and Rockley Voclanics. Can be divided into two unnamed units.||||||
14480|Oberon Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
14480|Oberon Granite|30734|6|Mentioned|p54|||||||||
14480|Oberon Granite|33006|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
14480|Oberon Granite|33282|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
14480|Oberon Granite|33285|6|Mentioned|p79|||Carb.||||||
14480|Oberon Granite|35257|6|Mentioned|Fig.31|||||||||
14480|Oberon Granite|42712|4|Described|12,16;Tab1p13;Fg3p10|Carboniferous|Early Carboniferous|||||||
14480|Oberon Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
14480|Oberon Granite|43515|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(Provisional Edition) (L.-M.Carb)||||||
14480|Oberon Granite|43516|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(L.-M.Carb)||||||
14480|Oberon Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
14480|Oberon Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Does not appear on map face.||||||
14480|Oberon Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
14481|Oberon Hill Chert|40622|6|Mentioned|p29|||||||||
14514|Old Hut Limestone Member|22968|5|Briefly described|P113|Silurian|Silurian|Parent is Cowombat Siltstone, overlying unit is Avonmore Subgroup (unconformable)||||||
14514|Old Hut Limestone Member|23309|5|Briefly described|p92 Tb 2.31|||||||||
14514|Old Hut Limestone Member|24551|5|Briefly described|p135|||Of Cowombat Siltstone.||||||
14514|Old Hut Limestone Member|37727|6|Mentioned|p49|||||||||
14514|Old Hut Limestone Member|39447|6|Mentioned|p8|||||||||
14514|Old Hut Limestone Member|41585|6|Mentioned|p128|||||||||
14514|Old Hut Limestone Member|42827|6|Mentioned|p128|||of Cowombat Siltstone||||||
14519|Old Red Sandstone|42050|5|Briefly described|p234|||||||||
14519|Old Red Sandstone|42268|5|Briefly described|p325|||||||||
14553|Olney Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p20|||Lawrence (1975). Murray Basin. Lacustrine and paludal sediments.||Renmark Group.||Overlies Warina Sand. Is overlain by Ettrick Marl, Geera Clay and Calivil Formation.|Carbonaceous silt, with additional clays, claystones, coals and sand.|
14553|Olney Formation|10010|5|Briefly described|p12 Fig. 3|Early Miocene|Early Eocene|Overlies Renmark Group. Geological Province: Murray Basin.||||||13-AUG-07
14553|Olney Formation|22587|6|Mentioned|p79 Fig.7|Early Miocene|Middle Eocene|||||||
14553|Olney Formation|22773|5|Briefly described|p340,351,Fig24.8p352|Oligocene|Eocene|||||||
14553|Olney Formation|22799|2|Defined|p28|Middle Miocene|Eocene|||||||
14553|Olney Formation|22857|5|Briefly described|p351, p352 Fig.24.8|Miocene|Early Eocene|Of the Renmark Group. Lithologically variable carbonaceous silts. Sands and clay; local coal and lignite. Overlies the basal Warina Sand. Age: <60Ma. Max. thickness: 300m. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
14553|Olney Formation|22887|2|Defined|p33, Fig.6 p13|Middle Miocene|Early Eocene|Probably equivalent to upper 'Renmark beds'.||||||03-FEB-09
14553|Olney Formation|22893|3|Fully described|p25-28|Middle Miocene|Middle Eocene|||||||
14553|Olney Formation|22971|4|Described|p 26|Miocene|Eocene|Of the Renmark Group.||||||25-MAR-08
14553|Olney Formation|23234|6|Mentioned|p88|||||||||
14553|Olney Formation|23252|5|Briefly described|Map Legend||Tertiary|Of Renmark Group. The main basal unit for the Bolligal sheet area. Informally divided into Upper, Middle and Lower Olney Formation.||||||25-MAR-08
14553|Olney Formation|23884|5|Briefly described|p155 Fig.13.2|Middle Miocene|Early Eocene|Geological Province: Murray Basin. Of the Renmark Group.||||||
14553|Olney Formation|23921|5|Briefly described|p1114|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.  See also upper Renmark Group beds.||||||
14553|Olney Formation|24105|5|Briefly described|p158|Miocene|Late Eocene|Geological Province: Murray Basin. Underlying Unit: Warina Sand.||||||
14553|Olney Formation|24177|5|Briefly described|p14, p69|Neogene|Paleogene|Of the Renmark Group. Overlies the Warina Sand. Age: ~45Ma. Geological Province: Murray Basin.||||||07-NOV-08
14553|Olney Formation|24551|5|Briefly described|p320, p731 Table 17.1|||Of the Renmark Group. Max thickness: 200m.||||||
14553|Olney Formation|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14553|Olney Formation|30934|6|Mentioned|Map legend|Eocene|Eocene|||||||
14553|Olney Formation|31741|6|Mentioned|p6|||||||||
14553|Olney Formation|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
14553|Olney Formation|31746|4|Described|p194|||||||||
14553|Olney Formation|32315|6|Mentioned|Fig. 2|||||||||
14553|Olney Formation|34757|6|Mentioned|p46|||||||||
14553|Olney Formation|34813|5|Briefly described|p63|||Mention on P62 also.||||||
14553|Olney Formation|35187|6|Mentioned|Table1|||||||||
14553|Olney Formation|37809|6|Mentioned|Fig.7|||||||||
14553|Olney Formation|37873|6|Mentioned|p1|||||||||
14553|Olney Formation|38293|4|Described|p22|||||||||
14553|Olney Formation|38601|6|Mentioned|p7|||||||||
14553|Olney Formation|39329|6|Mentioned|Fig.1|||||||||
14553|Olney Formation|39929|6|Mentioned|p269|||||||||
14553|Olney Formation|40520|6|Mentioned|Fig.5|||||||||
14553|Olney Formation|40820|6|Mentioned|Fig.4|||||||||
14553|Olney Formation|41136|5|Briefly described|p215|||||||||
14553|Olney Formation|41868|5|Briefly described|p551|||||||||
14553|Olney Formation|42125|5|Briefly described|p132|||||||||
14553|Olney Formation|42126|6|Mentioned|p149, p158|||||||||
14553|Olney Formation|42127|5|Briefly described|p219|||See also Fig.3||||||
14553|Olney Formation|42130|6|Mentioned|Fig.3 P265|||||||||
14553|Olney Formation|42133|6|Mentioned|p302|||||||||
14553|Olney Formation|42134|6|Mentioned|Fig.3 P335|||||||||
14553|Olney Formation|42137|6|Mentioned|p369|||||||||
14553|Olney Formation|42138|6|Mentioned|p388|||||||||
14553|Olney Formation|42184|6|Mentioned|p351|||||||||
14553|Olney Formation|42648|5|Briefly described|p45|||Renmark Group||||||
14553|Olney Formation|42813|6|Mentioned|p24|||||||||
14553|Olney Formation|42827|4|Described|p268|||see also Fig 8.3. Of Renmark Group.||||||25-MAR-08
14553|Olney Formation|42881|4|Described|Fig.3, P84|||||||||
14553|Olney Formation|42966|2|Defined|p100|Middle Miocene|Eocene|Of the Renmark Group.||||||13-OCT-08
14553|Olney Formation|43195|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|See also commentary on back of map. Of Renmark Group.||||||
14553|Olney Formation|43218|4|Described|Fig.3,p22||Tertiary|Of the Renmark Group.||||||25-MAR-08
14553|Olney Formation|43780|6|Mentioned|p6|||||||||
14553|Olney Formation|43791|6|Mentioned|p372, Fig1|||||||||
14553|Olney Formation|43804|6|Mentioned|Fig.2,p49|||||||||
14553|Olney Formation|43841|5|Briefly described|8||Tertiary|||||||
14553|Olney Formation|44133|5|Briefly described|p158, 152 Fig. 10.2|Middle Miocene|Middle Eocene|Of the Renmark Group. Geological Province: Murray Basin. Includes: Moorlands Lignite Member||||||
14553|Olney Formation|44188|5|Briefly described|Map Legend|Miocene|Eocene|Of the Renmark Group. Geological province: Murray Basin. Unconsolidated to poorly consolidated, thinly bedded, dark brown, grey, black, carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised.||||||15-MAY-08
14553|Olney Formation|44191|5|Briefly described|Map Legend||Middle Miocene|Informally subdivided into Lower, Middle and Upper Olney Formation.||||||
14553|Olney Formation|49038|4|Described|Table 2|||Briefly described p24.||||||25-MAR-08
14553|Olney Formation|49040|6|Mentioned|p10|||||||||
14553|Olney Formation|50154|5|Briefly described|p26, p132|||Of the Renmark Group. Overlies the Warina Sand. Geological Province: Murray Basin.||||||
14553|Olney Formation|60451|5|Briefly described|p95 Fig. 61.|||||||||
14553|Olney Formation|60452|4|Described|p33|Middle Eocene|Early Eocene|Formerly the 'upper' Renmark Beds (Harris, 1996). Now upgraded to formation status. Disconformably overlain by the Calivil Formation, unconformably overlain by Murray Group. Overlies: Warina Sand conformably. Age: 45Ma. Max. Thickness: 300m.||||||25-MAR-08
14553|Olney Formation|60461|5|Briefly described|Map legend|Eocene|Paleocene|Fluviolacustrine and paludal deposits: carbonaceous silt, clay, brown coal and ligneous sand; pyritic, unconsolidated to poorly consolidated.||||||
14553|Olney Formation|60491|4|Described|p15|Eocene|Eocene|Of the Renmark Group. Overlies the Warina Sand. Overlain by the Geera Clay. Geological Province: Murray Basin||||||
14553|Olney Formation|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
14553|Olney Formation|60599|5|Briefly described|p15, p84|Early Pliocene|Middle Eocene|In the upper part of Renmark Group. Fine-grained marginal marine deposits. Geological Province: Murray Basin.||||||
14553|Olney Formation|61155|5|Briefly described|p3, p18|Middle Miocene|Middle Eocene|Of the Renmark Group.  Unconsolidated carbonaceous clastics - sands, silts, clays and peaty coals. Overlies Warina Sand. Overlain by and interfingers with Geera Clay. Thickness: 350m. Geological Province: Murray Basin.||||||
14553|Olney Formation|61185|5|Briefly described|p57, p15|Middle Miocene|Middle Eocene|In upper part of Renmark Group. Fine grained and relatively well-sorted distal deposits. Geological Province: Murray Basin.||||||03-JUL-13
14553|Olney Formation|61314|5|Briefly described|p129|Middle Miocene||Geological Province: Murray Basin.||||||
14553|Olney Formation|61837|5|Briefly described|p216|Middle Eocene|Middle Eocene|Carbonaceous silt, siltstone, sand and kaolinitic clay interbedded with lignite brown coal. Geological Province: Murray Basin.||||||
14553|Olney Formation|61964|3|Fully described|p14 Fig. 4, p139-141|Middle Miocene|Late Eocene|Of Renmark Group. Detailed lithology given. Commonly micaceous, pyritic or ferruginised horizons present. Unconformable below Calivil Formation. Thickness: 128m in type-section Victoria. Geological Province: Murray Basin. See also age discussion p.143||||||
14553|Olney Formation|62405|5|Briefly described|Map legend|Tertiary|Tertiary|Unconsolidated to poorly consol'd, thinly bedded, dark brown, grey, black carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised. Includes intercalations of poorly sorted, fine- to med.gr. quartz sand +polymictic sand.||||||
14553|Olney Formation|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Of Renmark Group. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt.||||||
14553|Olney Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Eocene|Of Renmark Group. Predominantly fluvial and lacustrine unit deposited contemporaneously with the marine Murray Group, Winnambool and Ettrick formations and Geera Clay. Underlies Wunghnu Group units, unconformably overlies Warina Sand.||||||
14553|Olney Formation|65969|5|Briefly described|p27 Tb.3.3, p30-1|Early Oligocene|Eocene|Of Renmark Group. Fluvial to paralic carbonaceous silt and clay; minor lignite: four resources identified by CRA Exploration but had excess ash, sulfur and overburden. Unconformable on Paleozoic basement. Upper contact is erosional with Calivil Formation. Over 100 m thick in the north of the BENDIGO 1:250 000 sheet. No magnetic response.||||||
14553|Olney Formation|66012|5|Briefly described|p17|||In Murray Basin. Of Renmark Group. Probable correlative of Dilwyn Formation|| ||||13-JUN-13
14553|Olney Formation|66286|5|Briefly described|p179.|||||Unit in Renmark Group.||Overlies Warina Sand.|Interbedded fluvio-lacustrine sands, silts and clays.|
14553|Olney Formation|67462|5|Briefly described|Map legend.|Early Miocene|Late Eocene|Murray Basin.||||||
14553|Olney Formation|68189|5|Briefly described|p3, p26, p27 Tb.3.2, p33|Miocene|Eocene|The oldest unit recorded in ST ARNAUD.  Middle Eocene to Lower Miocene age. Time equivalent of the upstream White Hills Granite in ST ARNAUD. Fluvial to paludal depositional environment.||Of the Renmark Group.||Disconformably overlain by the Parilla Sand. Overlain by the Geera Clay. Overlain by the Winnambool Formation.|Comprises carbonaceous sand, silt and clay, lignite.|
14553|Olney Formation|68194|5|Briefly described|p23|||||Unit in Renmark Group.||Overlies Warina Sand.|Carbonaceous siltstone and claystone.|
14553|Olney Formation|68715|6|Mentioned|p31 Fig.5|Chattian|Bartonian|Murray Basin.||Renmark Group.||||07-APR-17
14553|Olney Formation|69163|5|Briefly described|Map legend|Tertiary|Tertiary|Murray Basin.|||||Unconsolidated to poorly consolidated, thinly-bedded, dark brown, grey, black, carbonaceous sand, silt, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised; intercalated poorly-sorted fine-medium quartz sand and polymictic sand.|
14553|Olney Formation|69798|5|Briefly described|p4 Fig.2, p11|Miocene|Eocene|Murray Basin. Appears as Onley Formation in Fig.2. Seismic profiles.||Renmark Group.||||
14553|Olney Formation|70718|5|Briefly described|p17, p24-p25, p103|Middle Miocene|Early Eocene|Murray Basin. Previously the Upper Renmark Beds. Is one of the primary aquifers in the Hay map sheet area. Informally subdivided into an upper, middle and lower units. Up to 300m thick. Hosts more lignitic coal than any other formation in the Murray Basin. Deposition was intermittent in the eastern part of the Murray Basin. A second lithology description is provided in the appendix, p103.||Renmark Group|||Terrigenous clastic sands and clays with common interbeds of lignitic brown coal and peat.|
14553|Olney Formation|71593|5|Briefly described|p52-p54|Miocene|Oligocene|||Renmark Group||||
14553|Olney Formation|72445|5|Briefly described|App1; App.2; App.7 p2, p4-5, p7-8, p10|Miocene|Eocene|See also p13-14, p16-21. Data indicates deposition over weathered Palaeozoic bedrock during the Late Eocene but the precise timing needs to be confirmed. Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 04, 05,11,14,16. Pollen/spores identified in samples from Stavely 04, 11, 14. Dominantly micaceous and lignitic sand. Locally silty, muddy and gravelly. Sparse <1m intervals of lignite. Said to be non-marine, alluvial fan, fluvial.||Renmark Group||Underlies Calivil Formation, sharp contact; Ettrick Formation, gradational/sharp contact; Buccleuch beds. Partially equivalent to Murray Group. Overlies Glenthompson Sandstone, gradational.|Shown as including lignites and thick fluvio-lacustrine sands, silts and clays and mud beds in a fine sand.|
14553|Olney Formation|73118|5|Briefly described|p12, 17-18, 21, 24, 30, 34, 45, 48, 53|Miocene|Eocene|See also p64, 80, 83. Murray Basin. Has potential as a source of groundwater. Drill core summary logs. 200m thick. Entirely concealed, yet forms a thin, virtually continuous blanket beneath almost the entire Basin. Includes 'Upper Renmark beds' in SA. Fluvio-lacustrine, meandering channel, flood-plain, and swamp environments; includes deltaic and paralic sediments towards top.||Renmark Group.||Overlies Warina Sand, Glenthompson Sandstone and Saint Arnaud Group. Is overlain by Ettrick Formation, Geera Clay, Winnambool Formation and Loxton-Parilla Sands.|Un- to poorly-consolidated, thinly bedded dark carbonaceous silt, sand, clay, brown coal, peat; commonly micaceous, pyritic, ferruginised. Sand, sandy dolomite intercalations. Contains large uneconomic deposits of brown coal.|
14553|Olney Formation|73188|6|Mentioned|p320|Oligocene|Oligocene|Murray Basin.|||||Limestone, marl, clay.|
14553|Olney Formation|73228|4|Described|p50, p53-57, p60|Middle Miocene|Late Paleocene|Murray Basin. Floodplain and swamp sediments also with fluvial, lacustrine, and marginal marine (upper portion) depositional settings. Inferred to be mainly deposited in the vicinity of a coastal swamp based also on fossil content. Identified in Nadda 1 drillhole. More widespread than the underlying Warina Sand. [Also consists of a younger phase assigned to the Murray Group? See p55].||Renmark Group|Moorlands Lignite Member|Underlain by Warina Sand. Overlain by Ettrick Formation.|Alternating multi-coloured sandy silt and silty clay, thinly bedded grey to green carbonaceous sand, silt, clay and lignite.|
14553|Olney Formation|73229|6|Mentioned|p67|Early Miocene|Late Early Oligocene|Murray Basin.||Renmark Group||||31-OCT-22
14553|Olney Formation|73505|4|Described|p2, p10-11, p13-14, p36|Oligocene|Eocene|Murray Basin. Contains abundant plant material. Unconformable on Paleozoic basement, upper erosional contact. Topped by the Mologa Surface, Norval Regolith. No detectable magnetic response.||Renmark Group||Overlies Warina Formation, underlies Murray Group and Norval Regolith, underlies Calivil Formation with erosional contacts|Carbonaceous fluvial to lacustrine and paralic siltstone to claystone, contains brown coal with high levels of sulphur and ash. Thickness of 100+/-25 m.|
14578|Omeo Metamorphic Complex|22487|5|Briefly described|p200||Silurian|||||||11-SEP-08
14578|Omeo Metamorphic Complex|22597|6|Mentioned|Fig 13|||||||||
14578|Omeo Metamorphic Complex|22719|6|Mentioned|p491|||||||||
14578|Omeo Metamorphic Complex|22857|6|Mentioned|p132|||||||||
14578|Omeo Metamorphic Complex|22968|6|Mentioned|P12, P163||Early Silurian|||||||
14578|Omeo Metamorphic Complex|22971|5|Briefly described|p17, p12 Tb. 1|Silurian|Silurian|Mainly schist and gneiss.||||||10-JAN-07
14578|Omeo Metamorphic Complex|23020|5|Briefly described|Map legend|Wenlock|Llandovery|||||||
14578|Omeo Metamorphic Complex|23021|5|Briefly described|Map legend|Wenlock|Llandovery|Underlain by Yalmy Group.||||||10-JAN-07
14578|Omeo Metamorphic Complex|23028|5|Briefly described|Map legend|Wenlock|Llandovery|||||||
14578|Omeo Metamorphic Complex|23029|5|Briefly described|Map legend|Wenlock|Llandovery|||||||
14578|Omeo Metamorphic Complex|23030|5|Briefly described|Map legend|Silurian|Silurian|||||||
14578|Omeo Metamorphic Complex|23231|6|Mentioned|Fig5-2p48|||||||||
14578|Omeo Metamorphic Complex|23245|5|Briefly described|p132||Ordovician|||||||
14578|Omeo Metamorphic Complex|23309|5|Briefly described|p65-67, 289, 294|||||||||
14578|Omeo Metamorphic Complex|23454|5|Briefly described|p28|||||||||
14578|Omeo Metamorphic Complex|23615|5|Briefly described|p17, p20 Fig.6, p161|Ordovician|Ordovician|Geological Province: Lachlan Fold Belt.||||||
14578|Omeo Metamorphic Complex|23866|5|Briefly described|p132|||See also Omeo Complex.||||||
14578|Omeo Metamorphic Complex|23938|5|Briefly described|p14, p83|Middle Ordovician|Early Ordovician|Overthrusts Blueys Creek Formation. See also p139 Tb. 1 Appendix.||||||25-SEP-08
14578|Omeo Metamorphic Complex|24004|5|Briefly described|p273|||||||||
14578|Omeo Metamorphic Complex|24133|5|Briefly described|p22|||Geological Province: Lachlan Fold Belt.||||||
14578|Omeo Metamorphic Complex|24142|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
14578|Omeo Metamorphic Complex|24143|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
14578|Omeo Metamorphic Complex|24144|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt.||||||
14578|Omeo Metamorphic Complex|24145|5|Briefly described|Map Legend|||Geological Province: Lachlan Fold Belt||||||
14578|Omeo Metamorphic Complex|24263|4|Described|p1386|Middle Devonian|Late Silurian|Geological Province: Lachlan Fold Belt. Represents the oldest part of the Lachlan Fold Belt.||||||10-JAN-07
14578|Omeo Metamorphic Complex|24275|5|Briefly described|p1695|Late Ordovician|Late Ordovician|||||||
14578|Omeo Metamorphic Complex|24551|6|Mentioned|p138|||||||||
14578|Omeo Metamorphic Complex|33602|4|Described|p29|||||||||
14578|Omeo Metamorphic Complex|33603|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
14578|Omeo Metamorphic Complex|35112|6|Mentioned|p281|||||||||
14578|Omeo Metamorphic Complex|36515|6|Mentioned|p69|||||||||
14578|Omeo Metamorphic Complex|37330|3|Fully described|p4|||||||||
14578|Omeo Metamorphic Complex|38145|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
14578|Omeo Metamorphic Complex|38151|6|Mentioned|p35|||||||||
14578|Omeo Metamorphic Complex|38367|6|Mentioned|Fig.9.|||||||||
14578|Omeo Metamorphic Complex|39221|6|Mentioned|p1|||||||||
14578|Omeo Metamorphic Complex|39447|6|Mentioned|p4|||||||||
14578|Omeo Metamorphic Complex|39860|4|Described|p5|||||||||
14578|Omeo Metamorphic Complex|40136|6|Mentioned|p27|||||||||
14578|Omeo Metamorphic Complex|40761|5|Briefly described|p223|||||||||
14578|Omeo Metamorphic Complex|41137|5|Briefly described|p292|||Mention p307.||||||10-JAN-07
14578|Omeo Metamorphic Complex|41321|5|Briefly described|p223|||||||||
14578|Omeo Metamorphic Complex|41541|6|Mentioned|p15|||||||||
14578|Omeo Metamorphic Complex|41570|3|Fully described|p91|||||||||
14578|Omeo Metamorphic Complex|41572|5|Briefly described|p13|||||||||
14578|Omeo Metamorphic Complex|41590|6|Mentioned|Fig.7|||||||||
14578|Omeo Metamorphic Complex|41868|6|Mentioned|Table 12.3|||||||||
14578|Omeo Metamorphic Complex|42089|4|Described|p10|||See also Fig.3 P11||||||
14578|Omeo Metamorphic Complex|42647|6|Mentioned|p7|||||||||
14578|Omeo Metamorphic Complex|42790|6|Mentioned|p198|||||||||
14578|Omeo Metamorphic Complex|42791|5|Briefly described|Fig.1 P204|||||||||
14578|Omeo Metamorphic Complex|42827|4|Described|p91|||||||||
14578|Omeo Metamorphic Complex|42835|6|Mentioned|p249|||mentioned only in title||||||
14578|Omeo Metamorphic Complex|42836|6|Mentioned|p251|||mentioned only in title||||||
14578|Omeo Metamorphic Complex|42985|6|Mentioned|Fig.2,p385|||||||||
14578|Omeo Metamorphic Complex|43220|6|Mentioned|p9||Ordovician|||||||
14578|Omeo Metamorphic Complex|43770|6|Mentioned|p826|||||||||
14578|Omeo Metamorphic Complex|44093|6|Mentioned|p93|||||||||
14578|Omeo Metamorphic Complex|44184|5|Briefly described|Map Legend||Early Ordovician|||||||
14578|Omeo Metamorphic Complex|44185|5|Briefly described|Map legend.|Middle Ordovician|Early Ordovician|But symbols are OSs and OSn, implying Ordivician - Silurian age.|||||Gneiss, schist, spotted schist, phyllite.|31-OCT-14
14578|Omeo Metamorphic Complex|60503|5|Briefly described|p153, p17|Early Silurian||See also Omeo Metamorphics.  Includes larger intrusions Mac Creek and Wattle Grove Granodiorites. Schists and gneisses. See also p28 Fig. 9.||||||06-SEP-05
14578|Omeo Metamorphic Complex|60504|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||
14578|Omeo Metamorphic Complex|60505|5|Briefly described|Map legend|Llandovery|Llandovery|||||||
14578|Omeo Metamorphic Complex|60506|5|Briefly described|Map legend|Llandovery|Llandovery|||||||
14578|Omeo Metamorphic Complex|60507|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||
14578|Omeo Metamorphic Complex|60904|5|Briefly described|p784 Fig. 10|||Of the Lachlan Orogen. See also p785, p794. G17||||||
14578|Omeo Metamorphic Complex|61160|3|Fully described|p49, p10, p12, p18, p33 Tb. 5.2.|Silurian|Silurian|Composed of the regionally metamorphosed Pinnak Sandstone. Schist, gneiss and migmatite.||||||10-JAN-07
14578|Omeo Metamorphic Complex|61161|5|Briefly described|p84-88, p6, p76-77 Fig 6.1, p143, p78|||Protolith: Pinnak Sandstone. Phyllite, schist, gneiss, migmatite and S-type granite. Regional low-pressure/high-temperature metamorphism and deformation of protolith created OMC. Grade increases from south to north.||||||
14578|Omeo Metamorphic Complex|61163|3|Fully described|p126-130, p10 Fig. 31|Early Silurian|Early Silurian|Comprises schist, gneiss, mylonite and migmatite rocks. Geological Province: Lachlan Fold Belt (Omeo Zone). See also p14 Fig. 3.2, p37 Tb. 6.2.||||||
14578|Omeo Metamorphic Complex|61164|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite, Omeo Metamorphic Complex pegmatite, Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61165|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite, Omeo Metamorphic Complex pegmatite, Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61166|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite, Omeo Metamorphic Complex pegmatite, Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61167|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite, Omeo Metamorphic Complex pegmatite, Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||07-FEB-11
14578|Omeo Metamorphic Complex|61168|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite and unnamed Omeo Metamorphic Complex units including pegmatite (GSV map code: Sogp), muscovite-biotite leucogranite (Sogl), biotite granodiorite (Sogr), schist (Sos), gneiss (Sog) and migmatite (Som).||||||
14578|Omeo Metamorphic Complex|61169|5|Briefly described|map legend|Silurian|Silurian|Includes Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Cobungra Granite, Omeo Metamorphic Complex migmatite, Omeo Metamorphic Complex gneiss, Omeo Metamorphic Complex schist and Omeo Metamorphic Complex Phyllite.||||||
14578|Omeo Metamorphic Complex|61170|5|Briefly described|map legend|Silurian|Silurian|Includes Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Cobungra Granite, Omeo Metamorphic Complex migmatite, Omeo Metamorphic Complex gneiss, Omeo Metamorphic Complex schist and Omeo Metamorphic Complex Phyllite.||||||07-FEB-11
14578|Omeo Metamorphic Complex|61171|5|Briefly described|map legend|Silurian|Silurian|Includes Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Cobungra Granite, Omeo Metamorphic Complex migmatite, Omeo Metamorphic Complex gneiss, Omeo Metamorphic Complex schist and Omeo Metamorphic Complex Phyllite.||||||
14578|Omeo Metamorphic Complex|61172|5|Briefly described|map legend|Silurian|Silurian|Includes Omeo Metamorphic Complex leucogranite, Omeo Metamorphic Complex granodiorite, Cobungra Granite, Omeo Metamorphic Complex migmatite, Omeo Metamorphic Complex gneiss, Omeo Metamorphic Complex schist and Omeo Metamorphic Complex Phyllite.||||||
14578|Omeo Metamorphic Complex|61173|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Cobungra Granite and Omeo Metamorphic Complex informal units: Omeo Metamorphic Complex leucogranite (GSV map code: Sogl), granodiorite (Sogr), migmatite (Som), gneiss (Sog), schist (Sos) and phyllite (Sop).||||||
14578|Omeo Metamorphic Complex|61174|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||07-FEB-11
14578|Omeo Metamorphic Complex|61175|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61176|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61177|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Omeo Metamorphic Complex schist, Omeo Metamorphic Complex gneiss and Omeo Metamorphic Complex migmatite.||||||
14578|Omeo Metamorphic Complex|61178|5|Briefly described|map legend|Early Silurian|Early Silurian|Includes Omeo Metamorphic Complex informal units: schist (GSV map code: Sos), gneiss (Sog) and migmatite (Som).||||||
14578|Omeo Metamorphic Complex|61180|5|Briefly described|p6-7|||Consists of schists, gneisses and phyllites derived from Ordovician sediments.||||||
14578|Omeo Metamorphic Complex|61181|5|Briefly described|p188|||Contains rocks ranging from lower greenschist to upper amphibolite facies.||||||
14578|Omeo Metamorphic Complex|61187|5|Briefly described|p4, p5 Fig.3, p26 Fig.2, p29 Fig.4.  |Early Silurian|Early Silurian|Omeo and Deddick Zones. Generated during second phase of Benambran Orogeny (the Bindian Orogeny). Name shortened to Omeo Metamorphics on p.5.||||||
14578|Omeo Metamorphic Complex|61752|5|Briefly described|p2|||||||||07-FEB-11
14578|Omeo Metamorphic Complex|61964|6|Mentioned|p212|||See also Omeo-Wagga Metamorphic Complex.||||||
14578|Omeo Metamorphic Complex|66856|5|Briefly described|pp963-969.|Silurian|Ordovician|Southern Wagga Metamorphic Belt, Lachlan Fold Belt. Oxygen-isotope study shows little evidence of widespread fluid-rock interaction, hence minimal hydrothermal mineralisation. Deformed during Silurian. Several S- and I-type granites intruded c.420-412 Ma.|||||Includes metamorphosed turbidites.|
14578|Omeo Metamorphic Complex|67847|6|Mentioned|p78|||Omeo and Deddick Zones, Lachlan Orogen.||||||
14578|Omeo Metamorphic Complex|68116|5|Briefly described|Appendix, Maps 19-20, 26-28, 35-36.|Wenlock|Llandovery||||||Mica schist, gneiss, migmatite and various S-type granites; low pressure series; medium to high-grade metamorphosed Pinnak Sandstone.|
14578|Omeo Metamorphic Complex|70718|5|Briefly described|p44, 45|Wenlock|Llandovery|Wagga-Omeo Zone, Murray Basin. Formed as a result of the Benambran Orogeny. Includes Orogenic gold deposits.|||||Granite, pegmatite, leucogranite, granodiorite, schist, phyllite gneiss and migmatite.|02-JUN-19
14578|Omeo Metamorphic Complex|71040|6|Mentioned|p8, p10|||Eastern Victoria. Associated with several major, NW-trending strike-slip faults. Metamorphosed in the Benambran Orogeny and further affected by the Bindian (=Bowning) Orogeny.||||||
14578|Omeo Metamorphic Complex|72296|6|Mentioned|p6|||Name for the Wagga Metamorphic Belt in VIC. Consists of the Pinnak Sandstone.||||||
14578|Omeo Metamorphic Complex|75072|6|Mentioned|p255|Wenlock|Wenlock|Produced by high-grade regional metamorphism.|433-427 Ma.|||||
14592|Oodnadatta Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|SW Eromanga Basin. Up to 300m thick.|||||Calcareous mudstone and siltstone with minor thin interbeds of fine-grained calcareous sandstone. Contains a rich marine fauna of bivalves, ammonites and gastropods.|
14592|Oodnadatta Formation|13497|5|Briefly described|p115 fig 6.33, p152-p154, |Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Coorikiana Sandstone. Overlain by the Mackunda Formation and the Winton Formation.||
14592|Oodnadatta Formation|13516|5|Briefly described|p167 fig 10, p171 fig 12|Albian|Albian|In Eromanga Basin.||Of Marree Subgroup||||
14592|Oodnadatta Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlying unit is Mackunda Formtion, underlying unit is Coorikiana Sandstone||||||
14592|Oodnadatta Formation|22912|5|Briefly described|33|||Geol province Eromanga Basin||||||
14592|Oodnadatta Formation|23054|5|Briefly described|p21,26-7|Albian|Albian|||||||
14592|Oodnadatta Formation|23056|6|Mentioned|12 table 2|||||||||
14592|Oodnadatta Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Parent - Marree Subgroup of the Neales River Group.||||||
14592|Oodnadatta Formation|23155|4|Described|p31|Early Cretaceous|Early Cretaceous|The Oodnadatta Formation is of Early Cretaceous (Albian) age, based on spore pollen assemblages.||||||
14592|Oodnadatta Formation|23375|4|Described|Fig2 p265||Albian|Laterally equivalent to Toolebuc Formation and Allaru Mudstone. Of Eromanga Basin.||||||16-SEP-08
14592|Oodnadatta Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66, p158|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. Of the Neales River Group. Max. thickness: ~2000 ft.||||||
14592|Oodnadatta Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||
14592|Oodnadatta Formation|23982|5|Briefly described|p58 Fig.18|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24092|5|Briefly described|p8 Fig.3|||Of Neales River Group. Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24175|3|Fully described|p27, p17 Fig. 3|Albian|Albian|Of Marree Subgroup.  Overlies Coorikiana Sandstone.  Max. thickness: 229m.  Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
14592|Oodnadatta Formation|24321|5|Briefly described|Map legend|Albian|Albian|Parent: Marree Subgroup||||||
14592|Oodnadatta Formation|29379|6|Mentioned|p25|||Tambo Formation equivalent.||||||
14592|Oodnadatta Formation|29651|6|Mentioned|p25|||||||||
14592|Oodnadatta Formation|29660|6|Mentioned|Fig.1|||||||||
14592|Oodnadatta Formation|30539|6|Mentioned|p6|||Angiosperms||||||
14592|Oodnadatta Formation|30540|6|Mentioned|Fig.6|||||||||
14592|Oodnadatta Formation|30803|6|Mentioned|p1|||Cretaceous||||||
14592|Oodnadatta Formation|30804|6|Mentioned|p7|||See also P10, Table 1||||||
14592|Oodnadatta Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
14592|Oodnadatta Formation|30919|6|Mentioned|Map legend|Albian|Albian|||||||
14592|Oodnadatta Formation|30921|6|Mentioned|Map legend|Turonian|Albian|Neocomian - Turonian ?||||||
14592|Oodnadatta Formation|30924|6|Mentioned|Map legend|Albian|Albian|||||||
14592|Oodnadatta Formation|31208|6|Mentioned|Fig. 7|||||||||
14592|Oodnadatta Formation|31249|6|Mentioned|p63|||||||||
14592|Oodnadatta Formation|31699|4|Described|p133|||L.Cretaceous||||||
14592|Oodnadatta Formation|31923|6|Mentioned|p14|||||||||
14592|Oodnadatta Formation|32314|6|Mentioned|Fig. 4|||||||||
14592|Oodnadatta Formation|33075|6|Mentioned|Table 1|||Refers Wopfner et al. (1970)||||||
14592|Oodnadatta Formation|33490|6|Mentioned|p30|||Cret. Correlation||||||
14592|Oodnadatta Formation|33491|4|Described|p56|||Mention Fig.2||||||
14592|Oodnadatta Formation|33521|6|Mentioned|p8|||L. Cret.||||||
14592|Oodnadatta Formation|33819|6|Mentioned|p3|||||||||
14592|Oodnadatta Formation|33820|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14592|Oodnadatta Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|33822|6|Mentioned|Map legend|Albian|Neocomian|Neocomian - Albian||||||
14592|Oodnadatta Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
14592|Oodnadatta Formation|33824|6|Mentioned|p12|||See also Table 2||||||
14592|Oodnadatta Formation|33825|5|Briefly described|p8|||Lithology||||||
14592|Oodnadatta Formation|33827|6|Mentioned|p13|||See also Table 2||||||
14592|Oodnadatta Formation|33828|6|Mentioned|p9|||See also Table 1||||||
14592|Oodnadatta Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
14592|Oodnadatta Formation|33832|6|Mentioned|p6|||Stratigraphy||||||
14592|Oodnadatta Formation|33936|6|Mentioned|Fig.3A|||Cretaceous.||||||
14592|Oodnadatta Formation|33938|6|Mentioned|p41|||O'lain by Eyre Fm.||||||
14592|Oodnadatta Formation|33939|5|Briefly described|p386|||See also P405. L.Cret.||||||
14592|Oodnadatta Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
14592|Oodnadatta Formation|34611|6|Mentioned|Fig.65|||Cretaceous. See also Fig.66||||||
14592|Oodnadatta Formation|34725|6|Mentioned|p379|||||||||
14592|Oodnadatta Formation|34984|6|Mentioned|p323|||||||||
14592|Oodnadatta Formation|36490|6|Mentioned|p173|||||||||
14592|Oodnadatta Formation|36494|6|Mentioned|p145|||||||||
14592|Oodnadatta Formation|36552|6|Mentioned|p62|||||||||
14592|Oodnadatta Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
14592|Oodnadatta Formation|36733|6|Mentioned|p14|||||||||
14592|Oodnadatta Formation|36922|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|37776|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|38007|6|Mentioned|p38|||||||||
14592|Oodnadatta Formation|38022|6|Mentioned|p29|||||||||
14592|Oodnadatta Formation|38068|5|Briefly described|p72|||||||||
14592|Oodnadatta Formation|38199|6|Mentioned|p426|||||||||
14592|Oodnadatta Formation|38814|6|Mentioned|Table 1|||||||||
14592|Oodnadatta Formation|39211|5|Briefly described|Fig.6|||See also Figs 9-16 etc||||||
14592|Oodnadatta Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
14592|Oodnadatta Formation|39914|6|Mentioned|p2|||||||||
14592|Oodnadatta Formation|40003|6|Mentioned|Fig.9|||See also Table 7.||||||
14592|Oodnadatta Formation|40058|6|Mentioned|p5|||||||||
14592|Oodnadatta Formation|40199|6|Mentioned|p16|||||||||
14592|Oodnadatta Formation|40220|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|40670|6|Mentioned|Fig.9|||||||||
14592|Oodnadatta Formation|40681|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|40801|6|Mentioned|p85|||||||||
14592|Oodnadatta Formation|40910|6|Mentioned|p15|||||||||
14592|Oodnadatta Formation|40911|6|Mentioned|Map legend|Cenomanian|Cenomanian|Prob. Cenomanian||||||
14592|Oodnadatta Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|40926|3|Fully described|p17|||||||||
14592|Oodnadatta Formation|41012|6|Mentioned|p143|||||||||
14592|Oodnadatta Formation|41060|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|41062|6|Mentioned|Fig.5|||||||||
14592|Oodnadatta Formation|41064|6|Mentioned|p62|||||||||
14592|Oodnadatta Formation|41084|5|Briefly described|Fig.2|||||||||
14592|Oodnadatta Formation|41085|3|Fully described|p88|||||||||
14592|Oodnadatta Formation|41086|3|Fully described|p98|||||||||
14592|Oodnadatta Formation|41087|3|Fully described|p123|||||||||
14592|Oodnadatta Formation|41088|6|Mentioned|p141|||||||||
14592|Oodnadatta Formation|41098|4|Described|p176|||||||||
14592|Oodnadatta Formation|41117|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41165|5|Briefly described|p362|||See also Fig.15||||||
14592|Oodnadatta Formation|41175|6|Mentioned|Fig.1|||||||||
14592|Oodnadatta Formation|41177|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41182|5|Briefly described|Fig.2|||||||||
14592|Oodnadatta Formation|41183|6|Mentioned|Fig.3 p308|||||||||
14592|Oodnadatta Formation|41187|6|Mentioned|Fig.2|||||||||
14592|Oodnadatta Formation|41216|6|Mentioned|Fig.18|||||||||
14592|Oodnadatta Formation|41266|6|Mentioned|Fig.3|||||||||
14592|Oodnadatta Formation|41523|3|Fully described|p276|||||||||
14592|Oodnadatta Formation|41533|6|Mentioned|p263|||||||||
14592|Oodnadatta Formation|41950|5|Briefly described|Fig.2 P3|||||||||
14592|Oodnadatta Formation|42003|6|Mentioned|p141|||||||||
14592|Oodnadatta Formation|42071|6|Mentioned|Fig.2A P116|||||||||
14592|Oodnadatta Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
14592|Oodnadatta Formation|42375|6|Mentioned|Fig.28 P125, Table 1|Late Cretaceous|Jurassic|Eromanga Basin||||||
14592|Oodnadatta Formation|42395|5|Briefly described|Fig.13 P83|||||||||
14592|Oodnadatta Formation|42520|6|Mentioned|p6|||Old/alternate name for the Cadna-owie Formation?||||||
14592|Oodnadatta Formation|42746|4|Described|p12|||||||||
14592|Oodnadatta Formation|42905|5|Briefly described|p20|||of Marree Subgroup||||||
14592|Oodnadatta Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||25-MAY-05
14592|Oodnadatta Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
14592|Oodnadatta Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
14592|Oodnadatta Formation|43591|6|Mentioned|p40,165|||||||||
14592|Oodnadatta Formation|43628|6|Mentioned|Fig.3|Early Cretaceous|Early Cretaceous|||||||
14592|Oodnadatta Formation|43681|5|Briefly described|p296|||||||||
14592|Oodnadatta Formation|44133|4|Described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin. Includes: Woolridge Limestone Member. Previously included Coorikiana Sandstone and Mount Alexander Sandstone, now separate formations. Thickness: ~300m. Conformably underlies Mackunda Formation.||||||
14592|Oodnadatta Formation|44289|5|Briefly described|Map Legend||Albian|||||||
14592|Oodnadatta Formation|44658|14|Not recorded|map legend|||Neocom-Ablian. (G53-15).||||||
14592|Oodnadatta Formation|45132|6|Mentioned|p15|||||||||
14592|Oodnadatta Formation|46791|6|Mentioned|Table 2|||||||||
14592|Oodnadatta Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
14592|Oodnadatta Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
14592|Oodnadatta Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
14592|Oodnadatta Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Coorikiana Sandstone; interfingers laterally with Mackunda Formation. Overlain by Winton Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
14592|Oodnadatta Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marine mudstone.||||||
14592|Oodnadatta Formation|61014|6|Mentioned|p533 Fig.2.|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Sandstone.||21-JAN-15
14592|Oodnadatta Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Marine mudstone.||||||01-JUN-05
14592|Oodnadatta Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
14592|Oodnadatta Formation|61615|6|Mentioned|p302 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
14592|Oodnadatta Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
14592|Oodnadatta Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Formation and Bulldog Shale. Is overlain by Mackunda Formation.||
14592|Oodnadatta Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
14592|Oodnadatta Formation|63979|5|Briefly described|Fig. 44|Cenomanian|Albian|Overlies Coorikiana Sandstone. Underlies Mackunda Formation.||||||07-FEB-11
14592|Oodnadatta Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.6|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Coorikiana Sandstone; underlies Winton or Mackunda Formations.||
14592|Oodnadatta Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Coorikiana Sandstone. Overlain by Mackunda Formation.||||||08-MAR-12
14592|Oodnadatta Formation|65489|5|Briefly described|p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 300m thick. Appears as Oodnadatta Sandstone on p96.||||Overlies Coorikiana Sandstone and Bulldog Shale.||
14592|Oodnadatta Formation|65925|5|Briefly described|Appendix 2.||||||||Interbedded claystone and siltstone, with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and baryte veins.|
14592|Oodnadatta Formation|66518|5|Briefly described|p19.|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Overlies Bulldog Shale and, locally, Coorikiana Sandstone. Is overlain by Mackunda Formation.||
14592|Oodnadatta Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Neales River Group.|Includes Wooldridge Limestone Member.|||
14592|Oodnadatta Formation|66623|6|Mentioned|p265.|||Equivalent in part to Allaru Mudstone, Koonenberry Belt.||||||
14592|Oodnadatta Formation|67120|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Claystone and siltstone, interbedded; with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins.|
14592|Oodnadatta Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Formation and Bulldog Shale. Is overlain by Winton Formation.||
14592|Oodnadatta Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
14592|Oodnadatta Formation|67784|6|Mentioned|p26, p28 table 1|||Southern Eromanga Basin. Correlations based on belemnites.||||Overlies Coorikiana Sandstone. Correlated with Allaru Formation, Toolebuc Formation.||08-FEB-18
14592|Oodnadatta Formation|68068|5|Briefly described|Map legend|Albian|Albian|Eromanga Basin. Recognised in subsurface; surface exposures often indistinguishable from Bulldog Shale if no Coorikiana Sandstone present. Shallow marine.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation.|Dark grey to grey mudstone with fossiliferous limestone concretions (molluscs, forams, wood, microflora, fish, vertebrates); bioturbated, interbedded with calcareous siltstone and fine-grained sandstone.|
14592|Oodnadatta Formation|68206|6|Mentioned|p31-33|Albian|Albian|S Eromanga Basin.||||A partial correlative of Allaru and Toolebuc Formations.||
14592|Oodnadatta Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Marree Subgroup.||||
14592|Oodnadatta Formation|68715|6|Mentioned|p30 Fig.5|Albian|Albian|Eromanga Basin.||||||
14592|Oodnadatta Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Eromanga Basin (SW). Shallow marine.||Of the Rolling Downs Group.||||18-NOV-14
14592|Oodnadatta Formation|69019|4|Described|p83 Fig.20, p85 Fig.21, p98-99.|Albian|Albian|SW Eromanga Basin. Defined by Freytag et al. (1967). Type section at Mt Arthur, ~55 km E of Oodnadatta. It is almost impossible to distinguish this unit in the field from Bulldog Shale where Coorikiana Sandstone is absent; the general term Marree Subgroup is used on the map where this is the case. Thickness from ~40 m to 344.6 m max.||Unit in Marree Subgroup.||Overlies Coorikiana Sandstone conformably. Is overlain conformably by Mackunda Formation.|Grey laminated siltstone or mudstone with grey calcareous concretions, under dark grey mudstone and siltstone with fine-grained glauconitic and feldspathic sandstone interbeds. Slightly carbonaceous and finely micaceous; conspicuous shell fragments.|
14592|Oodnadatta Formation|69023|5|Briefly described|p87, p89 Fig.20, p93, p99-100, p102-103|Albian|Albian|See also p105, p191-192. Defined by Freytag et al.(1967). Where Coorikiana Sandstone is absent, the in-field recognition of Oodnadatta Formation is difficult: the name Marree Subgroup is applied. Thickness from <20 to >180m. Lithologically similar to Allaru Mudstone. Trace fossil assemblages similar to those in Bulldog Shale. Stratigraphic wells intersection data.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Equivalent to Allaru Mudstone. Is overlain conformably by Mackunda Formation.|A lower unit of siltstone with calcareous concretions is overlain by dark grey mudstone and siltstone with fine-grained glauconitic and feldspathic sandstone interbeds; zones of bioturbation.|
14592|Oodnadatta Formation|69457|5|Briefly described|p41:3, 6-8, 11-12, 17|Early Cretaceous|Early Cretaceous|Freytag (1966). SW Eromanga Basin. The lower part of this unit, together with Bulldog Shale and Coorikiana Sandstone, is equivalent to the Wallumbilla Formation. The middle and upper part of this unit is equivalent to the combined Toolebuc Formation and Allaru Mudstone.||Marree Subgroup.||Overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation. Correlative of Allaru Mudstone.|Claystone and siltstone with interbeds of fine-grained sandstone, calcareous and ferruginous concretions, and cone-in-cone limestone. Contains a rich fossil assemblage.|12-JUL-16
14592|Oodnadatta Formation|69562|6|Mentioned|p681-682|Mesozoic|Mesozoic|A relatively conductive sandy unit.||Unit in Marree Subgroup.||||
14592|Oodnadatta Formation|69594|6|Mentioned|p530|||||||Is correlated with the Allaru Mudstone.||
14592|Oodnadatta Formation|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||||Overlies Coorikiana Sandstone, overlain by Mackunda Formation||
14592|Oodnadatta Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
14592|Oodnadatta Formation|69946|3|Fully described|p22-24, p57, p94, p120-122|Early Cretaceous|Early Cretaceous|Freytag (1966). Type section is Mount Arthur, E of Oodnadatta. Up to c.300m thick. Contains a varied marine fauna. Middle-late Albian. Wireline log correlations.||Unit in Marree Subgroup.||Conformably overlies Coorikiana Sandstone. Is overlain conformably by Mackunda Formation. Passes laterally into Wallumbilla and Toolebuc Formations, Allaru Mudstone and Marree Subgroup.|Laminated and thin-bedded claystone and siltstone with interbeds of fine-grained sandstone; calcareous and ferruginous concretions and a thin unit of calcareous siltstone and fossil-rich concretionary limestone in the lower part of the unit.|
14592|Oodnadatta Formation|69947|5|Briefly described|p13 Fig.7.2|Late Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
14592|Oodnadatta Formation|69948|6|Mentioned|Figs.4.1, 18|||Eromanga Basin.||||Overlies Bulldog Shale.||
14592|Oodnadatta Formation|70336|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Of Marree Subgroup.|||Interbedded claystone and siltstone, with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins.|12-JAN-16
14592|Oodnadatta Formation|70383|5|Briefly described|p45|Albian|Albian|Eromanga Basin. Marine deposits.||||||
14592|Oodnadatta Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
14592|Oodnadatta Formation|70821|5|Briefly described|p21 Fig.2.6, p23|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Coorikiana Sandstone. Is overlain by Toolebuc Formation.||
14592|Oodnadatta Formation|70823|5|Briefly described|p43-p44|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 300m thick. Deposited in a restricted, stratified and anoxic marine environment.||||Overlies the Coorikiana Sandstone. Overlain by the Mackunda and Winton Formations.||
14592|Oodnadatta Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
14592|Oodnadatta Formation|70938|5|Briefly described|p807-808|Early Cretaceous|Early Cretaceous|||Neales River Group.||||
14592|Oodnadatta Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; shallow marine-fine-graned siliciclastics.||||Overlies the Bulldog Shale.||24-OCT-19
14592|Oodnadatta Formation|71342|3|Fully described|Ch1 p19, Ch4 p8, Ch5 p23-p24|Albian|Albian|Defined by Freytag (1966) as the fossiliferous siltstone and shale overlying the Bulldog Shale. Freytag also assigned the type section at Mount Arthur east of Oodnadatta. A maximum thickness of up to 300m is recorded in the Moomba area. Age derived from palynology studies and from macrofossil assemblage. Interpreted to have been deposited in a low-energy, shallow marine environment. Spore-pollen zone is given in Ch5 p57. Forms a seal over the Coorikiana Sandstone.  Laterally equivalent to the Wallumbilla Formation, Toolebuc Formation and Allaru Mudstone. See also  Ch5 p27, Ch5 p33, Ch5 p57, Ch5 p122-p124, Ch6 p10, Ch7 p13, Ch9 p21, Ch11 p5.||Marree Subgroup||Conformably overlies the Coorikiana Sandstone. Overlies the Bulldog Shale. Conformably overlain by the Mackunda Formation. Overlain by the Winton Formation.|Laminated and thinly-bedded claystone and siltstone with interbeds of fine-grained sandstone, calcareous siltstone and fossil-rich concretionary limestone.|
14592|Oodnadatta Formation|71348|6|Mentioned|p202|||Geological province: Gawler Craton.||||||
14592|Oodnadatta Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA).||Neales River Group.|Wooldridge Limestone Member.|Overlies Coorikiana Sandstone. Is overlain by Mackunda FZ.||
14592|Oodnadatta Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Claystone and siltstone, interbedded with fine-grained sandstone, calcareous and ferruginous concretions; limestone with celestite and barite veins,|
14592|Oodnadatta Formation|72476|6|Mentioned|p36 Fig.9|||Eromanga Basin. Time-temperature thermal history diagram.||||||
14592|Oodnadatta Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
14592|Oodnadatta Formation|73249|4|Described|p316-319, p320 Fig.2, p321-338|Albian|Albian|Eromanga Basin. Maximum age of mid-Albian, minimum age of late Albian. Up to 300m thick. Lateral variations in mineralogy between drill holes, dominant clay mineral is montmorillonite. Deposited in a shallow marine environment, more arid and warmer environment than the Cadna-owie Formation. Sediment sources interpreted to be a mix of felsic to mafic igneous rocks from the west and south.||||Conformably overlies the Coorikiana Sandstone, lateral equivalent of the Allaru Mudstone.|Laminated and thin-bedded claystone and siltstone, up to 300m thick.|
14592|Oodnadatta Formation|73251|6|Mentioned|p36, p62|Early Cretaceous|Early Cretaceous|Eromanga Basin, Frome Embayment. Marginal thermal maturity.||||Underlain by Bulldog Shale and Coorikiana Sandstone. Overlain by and equivalent to Mackunda Formation. Equivalent to Allura Mudstone and Toolebuc Formation.||
14592|Oodnadatta Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
14592|Oodnadatta Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Coorikiana Sandstone. Overlain by Winton Formation. Equivalent to Allaru Mudstone and Toolebuc Formation.||
14592|Oodnadatta Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 104-98 Ma|||Overlies Coorikiana Sandstone, underlies Winton Formation||
14598|Oolong Granite|42726|5|Briefly described|map legend|Silurian||||||||
14598|Oolong Granite|50232|5|Briefly described|Map legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
14598|Oolong Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Gunning Suite. Grey to cream, med- to coarse-gr., equigran. to porphyritic hornblende-biotite granite+granodiorite with abundant ovoid microdiorite enclaves. Pluton is zoned with core of fine- to med.gr. leucocratic qtz.-feldspar-phyric granite...||||||09-SEP-08
14598|Oolong Granite|68592|2|Defined|p294, p1312-1313, p1316-1321, p1341-1345|Early Silurian|Early Silurian|See also p231, p235, p256, p269-270. Chappell et al. (1991), after the locality of Oolong, 8km W of Gunning. Forms undulating terrain. Type locality near Mount Dixon described. Geochemistry detailed; geophysical properties described. Has been quarried for decorative aggregate. Holds potential for quarrying for dimension stone. Not isotopically dated.||Unit in Gunning Suite.||Intrudes Cuddyong and Abercrombie Formations.|Hard, grey to cream (weathering to brown), medium- to coarse-grained, mostly massive, porphyritic to equigranular granite and granodiorite; abundant ovoid microdioritic enclaves up to a metre. The larger body has compositional zoning. I-type.|
14598|Oolong Granite|70192|4|Described|Map Legend|Ludlow|Wenlock|Sgo. Includes one unnamed mapped member of white to cream, fine-medium grained, equigranular to porphyritic, leucocratic, quartz-feldspar-phyric granite and aplite. On Gunning 1:100 000 mapsheet portion of Time-Space Plot.||Gunning Suite|Includes one unnamed subunit.||Medium to coarse-grained, porphyritic to equigranular, hornblende biotite granite and granodiorite; abundant ovoid microdioritic enclaves; minor fine-medium grained, leucocratic, quartz-feldspar-phyric granite at the core of the zoned pluton.|
14598|Oolong Granite|70541|4|Described|Map Legend|Devonian|Silurian|Includes one unnamed mapped member of white to cream, fine-medium grained, equigranular to porphyritic, leucocratic, quartz-feldspar-phyric granite and aplite.||Gunning Suite|Includes one unnamed subunit.||Medium to coarse-grained, porphyritic to equigranular, hornblende biotite granite and granodiorite; abundant ovoid microdioritic enclaves; minor fine-medium grained, leucocratic, quartz-feldspar-phyric granite at the core of the zoned pluton.|
14623|Ootha Group|23522|5|Briefly described|p249 Fig 5|Lochkovian|Ludlow|||||||
14623|Ootha Group|24233|5|Briefly described|p256|Devonian|Silurian|Geological Province: Lachlan Orogen.||||||
14623|Ootha Group|24417|3|Fully described|p61||Pridoli|Previously referred to as "Ootha Series" and "Ootha Formation" and included in the Derriwong Group.  Overlain by Darbys Ridge Conglomerate;  overlies Girilambone Group.||||||
14623|Ootha Group|29907|6|Mentioned|p64|||||||||
14623|Ootha Group|29910|6|Mentioned|Map legend|Silurian|Silurian|||||||
14623|Ootha Group|29987|5|Briefly described|p18|||||||||
14623|Ootha Group|29993|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
14623|Ootha Group|32087|4|Described|p10|||||||||
14623|Ootha Group|33326|6|Mentioned|p443|||Fauna.||||||
14623|Ootha Group|34469|6|Mentioned|p108|||Silurian. Inc. Mineral Hill Volcanics||||||
14623|Ootha Group|36316|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
14623|Ootha Group|36317|6|Mentioned|p126|||||||||
14623|Ootha Group|37258|4|Described|p2|||||||||
14623|Ootha Group|42033|6|Mentioned|p650|||||||||
14623|Ootha Group|48971|6|Mentioned|p9|||See also P13, P18, P22, P30.||||||
14623|Ootha Group|60009|5|Briefly described|Map Legend|Lochkovian|Ludlow|||||||13-JUL-04
14623|Ootha Group|61964|4|Described|p14 Fig. 4, p95|Lochkovian|Pridoli|Supersedes "Ootha Series"; reduced to formation status (Ootha Formation) by Sherwin (1996b).Later revived as a group by Lyons et al (2000).  Includes Manna Conglomerate. Lithic quartz + qtz sst, pebble conglom., siltst.+ minor mudst(v.fine- to coarse-gr.)||||||20-OCT-08
14623|Ootha Group|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Manna Conglomerate. Pebble conglomerate, quartz and lithic quartz sandstone, mudstone.||||||10-APR-08
14623|Ootha Group|64568|5|Briefly described|Map legend|Silurian|Silurian|Includes Manna Conglomerate. Polymictic conglomerate, quartz and lithic sandstone, mudstone, rhyolitic tuff and volcaniclastic sandstone.||||||24-SEP-08
14623|Ootha Group|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Narromine. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
14623|Ootha Group|65469|6|Mentioned|p18, p43, p52, p55 fig 3-19|Late Silurian|Late Silurian|Lachlan Orogen. See also p62, p67, p146, p363, App A-VI 3.||||||
14623|Ootha Group|67847|5|Briefly described|p22-p24|Pridoli|Ludlow|||||Unconformably overlies the Kirribilli Formation.||
14623|Ootha Group|70751|5|Briefly described|p4, p6, p15, p17, p21|Devonian|Late Silurian|Cobar Superbasin, Kopyje Shelf.|||Includes the Yarnel Volcanics.|||
14623|Ootha Group|71039|5|Briefly described|p6, p13|Devonian|Silurian|Kopyje Shelf. Very little petrographic information and very few historic thin sections exist for this unit.|||||Vitric-rich mudstone and siltstone that has been silicified with varying degrees of clay alteration.|
14623|Ootha Group|71040|5|Briefly described|p12 Fig.7, p16-17|Early Devonian|Late Silurian||||Manna Conglomerate, Yiddah Formation.|||
14623|Ootha Group|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||Siltstone, sandstone, mudstone, basal polymictic conglomerate, locally abundant vitric-rich volcanic siltstone/mudstone and volcaniclastic sandstone.|
14623|Ootha Group|72908|6|Mentioned|p4|Early Devonian|Silurian|Kopyje Shelf.||||||
14635|Orallo Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499, p501|Early Cretaceous|Tithonian|N Surat Basin. Originally named the Fossil Wood Stage (Reeves, 1947). Also known for a while as Orallo Coal Measures (Jensen, 1926), but the coal was uneconomic. 150-200m thick.|||||Cross-bedded labile to sub-labile sandstone with minor conglomerate, carbonaceous siltstone, mudstone, bentonite and thin banded seams of coal; fossil wood is ubiquitous.|
14635|Orallo Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||||||
14635|Orallo Formation|22757|5|Briefly described|Table6,p12|Late Jurassic|Late Jurassic|245 m. Surat Basin||||||
14635|Orallo Formation|22857|4|Described|p296-7 Tb.22.1, p546 App.1 Tb.A1.12|Berriasian|Tithonian|Of the Blythesdale Group. Fine to medium-grained clayey arenite interbedded with carbonaceous siltstone and shales. Max. thickness: 230m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5.||||||
14635|Orallo Formation|22865|4|Described|p314,Table22.1p296-7|Berriasian|Tithonian|||||||
14635|Orallo Formation|23050|4|Described|p23 Table 4|Late Jurassic|Late Jurassic|Of Surat Basin. Palynology indicates a J6 Jurassic age.||||||08-APR-13
14635|Orallo Formation|23051|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|Of Surat Basin.||||||13-MAR-09
14635|Orallo Formation|23053|6|Mentioned|Fig10p17,26|Tithonian|Kimmeridgian|||||||
14635|Orallo Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
14635|Orallo Formation|23740|5|Briefly described|p1221|Jurassic|Jurassic|Geological Province: Durat Basin||||||
14635|Orallo Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Late Jurassic|Geological Province: Surat Basin.  Maximum thickness: 230m.||||||
14635|Orallo Formation|24070|5|Briefly described|p303|Late Jurassic|Middle Jurassic|Geological Province: Coonamble Embayment.||||||
14635|Orallo Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|24160|6|Mentioned|p18|Cretaceous|Cretaceous|Miles district, 350 km W of Brisbane. Major source of bentonite.||||||
14635|Orallo Formation|29387|6|Mentioned|Table 5|||||||||
14635|Orallo Formation|29393|6|Mentioned|Table 4|||||||||
14635|Orallo Formation|29591|6|Mentioned|Table 15|||||||||
14635|Orallo Formation|29721|6|Mentioned|Table 246|||||||||
14635|Orallo Formation|29870|4|Described|p15|||||||||
14635|Orallo Formation|30021|6|Mentioned|p90|||||||||
14635|Orallo Formation|30022|6|Mentioned|p32|||||||||
14635|Orallo Formation|30024|6|Mentioned|p332|||||||||
14635|Orallo Formation|30102|6|Mentioned|p26|||||||||
14635|Orallo Formation|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30694|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30695|4|Described|Table 4|||Upper Jurassic age||||||
14635|Orallo Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic age||||||
14635|Orallo Formation|30697|6|Mentioned|p34|||Minor aquifer present||||||
14635|Orallo Formation|30698|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper JurassicM - U||||||
14635|Orallo Formation|30701|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|30702|4|Described|p49|||See also P51, Fig.1 & 2, Table 1.||||||
14635|Orallo Formation|30914|6|Mentioned|Map legend|Cretaceous|Jurassic|Jurassic - Cretaceous||||||
14635|Orallo Formation|31086|6|Mentioned|p37|||Faunas||||||
14635|Orallo Formation|31097|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|31098|5|Briefly described|Table 1|||||||||
14635|Orallo Formation|31116|4|Described|p38|||See also P39-40||||||
14635|Orallo Formation|31208|6|Mentioned|Fig. 5|||||||||
14635|Orallo Formation|31244|6|Mentioned|p8|||||||||
14635|Orallo Formation|31369|6|Mentioned|Table 4|||Jurassic||||||
14635|Orallo Formation|31376|6|Mentioned|p4|||||||||
14635|Orallo Formation|32136|6|Mentioned|p9|||Miospores||||||
14635|Orallo Formation|32138|6|Mentioned|p398|||||||||
14635|Orallo Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
14635|Orallo Formation|32276|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|32797|4|Described|Table 4|||||||||
14635|Orallo Formation|33070|4|Described|Table 2|||U.Jur.||||||
14635|Orallo Formation|33071|6|Mentioned|p6|||L.Cret.||||||
14635|Orallo Formation|33075|6|Mentioned|p451|||||||||
14635|Orallo Formation|33080|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33090|4|Described|Table 4|||U.Jur.||||||
14635|Orallo Formation|33091|5|Briefly described|p10|||Stratigraphy||||||
14635|Orallo Formation|33094|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33367|5|Briefly described|Table 1|||||||||
14635|Orallo Formation|33368|6|Mentioned|p21|||U.Jur.Oil shale.Refers Jensen (1926).||||||
14635|Orallo Formation|33451|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
14635|Orallo Formation|33672|6|Mentioned|p44|||||||||
14635|Orallo Formation|34134|6|Mentioned|Cor.Chart|||Upper Jurassic.||||||
14635|Orallo Formation|34212|6|Mentioned|p2|||Jurassic.||||||
14635|Orallo Formation|34254|6|Mentioned|p489|||L. Jurassic||||||
14635|Orallo Formation|34408|6|Mentioned|p185|||On Table||||||
14635|Orallo Formation|34543|6|Mentioned|p98|||||||||
14635|Orallo Formation|34613|4|Described|Table 4|||||||||
14635|Orallo Formation|35016|6|Mentioned|p41|||||||||
14635|Orallo Formation|35793|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|35937|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|36243|6|Mentioned|Table 7A|||||||||
14635|Orallo Formation|36570|2|Defined|p45|Jurassic|Jurassic|Also mentioned Fig.9, Table 1, P46, P60.||||||
14635|Orallo Formation|36939|6|Mentioned|p214|||||||||
14635|Orallo Formation|37117|5|Briefly described|p313|||||||||
14635|Orallo Formation|37856|6|Mentioned|Table I|||||||||
14635|Orallo Formation|37995|4|Described|p65|||||||||
14635|Orallo Formation|38199|6|Mentioned|p428|||||||||
14635|Orallo Formation|39212|5|Briefly described|p17|||See also P38||||||
14635|Orallo Formation|39315|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|39445|5|Briefly described|Table 10|||||||||
14635|Orallo Formation|39494|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|39666|6|Mentioned|p112, 111|||||||||
14635|Orallo Formation|39708|6|Mentioned|p477|||||||||
14635|Orallo Formation|39942|6|Mentioned|p465|||||||||
14635|Orallo Formation|39943|6|Mentioned|Table 9A|||||||||
14635|Orallo Formation|39998|5|Briefly described|p193|||||||||
14635|Orallo Formation|40030|6|Mentioned|Fig.5|||||||||
14635|Orallo Formation|40245|6|Mentioned|Table 2|||||||||
14635|Orallo Formation|40249|6|Mentioned|p38|||||||||
14635|Orallo Formation|40250|6|Mentioned|Fig.1|||||||||
14635|Orallo Formation|40540|6|Mentioned|p155|||||||||
14635|Orallo Formation|40541|3|Fully described|p110|||||||||
14635|Orallo Formation|40544|6|Mentioned|Fig.6|||||||||
14635|Orallo Formation|40666|4|Described|p357|||||||||
14635|Orallo Formation|40675|6|Mentioned|Table 9A|||||||||
14635|Orallo Formation|40687|6|Mentioned|p417|||Mention P421||||||
14635|Orallo Formation|40767|4|Described|p13|||||||||
14635|Orallo Formation|41060|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|41064|6|Mentioned|p60|||||||||
14635|Orallo Formation|41187|6|Mentioned|Fig.2|||||||||
14635|Orallo Formation|41210|5|Briefly described|Fig.3|||||||||
14635|Orallo Formation|41216|6|Mentioned|Fig.18|||||||||
14635|Orallo Formation|41246|6|Mentioned|Map legend|Jurassic||||||||
14635|Orallo Formation|41247|6|Mentioned|Fig.7|||||||||
14635|Orallo Formation|41266|6|Mentioned|Fig.3|||||||||
14635|Orallo Formation|41290|6|Mentioned|p227|||||||||
14635|Orallo Formation|41681|6|Mentioned|p7|||||||||
14635|Orallo Formation|41992|4|Described|Fig.2 P183|||||||||
14635|Orallo Formation|42007|5|Briefly described|Fig.2 P182|||||||||
14635|Orallo Formation|42463|6|Mentioned|Fig.5 P172|||See also Fig.6 P173||||||
14635|Orallo Formation|42493|5|Briefly described|p20, Fig. 1 p18|||||||||
14635|Orallo Formation|42494|5|Briefly described|Table 1 P24|||||||||
14635|Orallo Formation|42634|6|Mentioned|Table 8 P34|||||||||
14635|Orallo Formation|42679|6|Mentioned|Fig.3 P3|||||||||
14635|Orallo Formation|42950|6|Mentioned|p41|||||||||
14635|Orallo Formation|43000|5|Briefly described|Fig.5,p112|||Of Blythesdale Group.||||||13-MAR-09
14635|Orallo Formation|43002|5|Briefly described|Fig.2,p135|||||||||
14635|Orallo Formation|43404|14|Not recorded|Table p11||Late Jurassic|||||||
14635|Orallo Formation|43539|14|Not recorded|p398|||||||||
14635|Orallo Formation|43582|6|Mentioned|Fig.5,p16||Late Jurassic|||||||
14635|Orallo Formation|43602|6|Mentioned|Fig3 p194|||In Surat Basin, Blythesdale Group.||||||
14635|Orallo Formation|43982|14|Not recorded|Map Legend||Late Jurassic|||||||
14635|Orallo Formation|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
14635|Orallo Formation|43994|14|Not recorded|Map Legend|||||||||
14635|Orallo Formation|43998|4|Described|p16,map|Cretaceous|Jurassic|||||||
14635|Orallo Formation|44021|14|Not recorded|p232,233,238|||||||||
14635|Orallo Formation|44023|6|Mentioned|Tb.3,p12|||||||||
14635|Orallo Formation|44028|14|Not recorded|Fig.2||Jurassic|See Strat Table.||||||
14635|Orallo Formation|44031|14|Not recorded|p10,11||Late Jurassic|||||||
14635|Orallo Formation|44084|14|Not recorded|p32(Tb)|Late Jurassic|Middle Jurassic|Surat Basin.||||||
14635|Orallo Formation|44091|14|Not recorded|p57||Late Jurassic|||||||
14635|Orallo Formation|44171|14|Not recorded|p194,197|||||||||
14635|Orallo Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
14635|Orallo Formation|44371|14|Not recorded|Map Legend||Jurassic|||||||
14635|Orallo Formation|44377|14|Not recorded|p1-8,11-2,19,21-2map||Late Jurassic|Name supersedes Fossil Wood Beds and Orallo Coal Measures.||||||
14635|Orallo Formation|44414|14|Not recorded|p114|Cretaceous|Jurassic|||||||
14635|Orallo Formation|44415|14|Not recorded|Fig.2,p23|||||||||
14635|Orallo Formation|44636|14|Not recorded|p167(Tb)||Late Jurassic|||||||
14635|Orallo Formation|44637|14|Not recorded|p287-291||Jurassic|||||||
14635|Orallo Formation|44786|14|Not recorded|p193-202||Early Jurassic|||||||
14635|Orallo Formation|45071|3|Fully described|Table 15|||||||||
14635|Orallo Formation|45110|2|Defined|p102|Late Jurassic|Late Jurassic|Formerly Orallo C.M.(Jensen,26),Fossil Wood Beds(Whitehouse).See P24.||||||
14635|Orallo Formation|46791|6|Mentioned|Fig.2|||||||||
14635|Orallo Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
14635|Orallo Formation|46984|6|Mentioned|Table 1|||||||||
14635|Orallo Formation|48919|6|Mentioned|Table 5|||See also P70||||||
14635|Orallo Formation|48920|6|Mentioned|Table 7|||Refers Day (1964)||||||
14635|Orallo Formation|49010|6|Mentioned|Fig.4|||Surat Basin||||||
14635|Orallo Formation|49011|6|Mentioned|Fig.3|||Surat Basin||||||
14635|Orallo Formation|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
14635|Orallo Formation|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
14635|Orallo Formation|61000|5|Briefly described|p186 Fig. 4|Tithonian|Tithonian|Geological Province: Surat Basin.||||||
14635|Orallo Formation|61310|5|Briefly described|p34|Late Jurassic|Late Jurassic|Geological Province: in the Queensland part of Clarence-Moreton Basin. May be equivalent to the Grafton Formation.||||||
14635|Orallo Formation|61313|5|Briefly described|p99, p98 Fig. G10|Early Cretaceous|Late Jurassic|Flood plain, alluvial, meandering fluvial deposits. Together with Mooga Formation, conformably overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||
14635|Orallo Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Blythesdale Group. Labile sandstone, carbonaceous siltstone, mudstone. Overlies Pilliga Sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8, p154 Fig. SU9.||||||07-FEB-11
14635|Orallo Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
14635|Orallo Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|63979|6|Mentioned|p40|Late Jurassic|Late Jurassic|Geological province: Surat Basin.||||||07-FEB-11
14635|Orallo Formation|64197|6|Mentioned|p630 Fig.7|Early Cretaceous|Early Cretaceous|||||Underlies the Mooga Sandstone, overlies the Gubberamunda Sandstone.||
14635|Orallo Formation|64665|5|Briefly described|p53 Fig.2, p60, p62.|Early Cretaceous|Early Cretaceous|Surat Basin. Contains thin coals.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|64856|3|Fully described|p79, p94-97|Berriasian|Late Jurassic|Surat Basin. Of Day (1964). Previously the Orallo Coal Measures and Orallo Measures (Jensen, 1926), "Fossil Wood Stages or Series" (Reeves, 1947) and "Fossil Wood Beds" (Whitehouse, 1955). Type area near Bungeworgorai Creek, near the abandoned Orallo rail siding. Transitionally overlies the Gubberamunda Sandstone. Grades up into Southlands Formation. Age from palynofloral unit APK1. Max. thickness 306m. Friable medium to coarse-grained sandstone, lesser interbedded carbonaceous siltstone, silty mudstone, bentonite, coal.|| ||||29-NOV-17
14635|Orallo Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Gubberamunda Sandstone, Surat Basin.||||||
14635|Orallo Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
14635|Orallo Formation|65003|4|Described|p1, p6, p8, p13-15, p21, p25-26||Middle Jurassic|Of Surat Basin.  Fluvial sediments. Extensive clay deposits.||||Overlain by the Mooga Sandstone. ?Overlies the Injune Creek Group.|Variably-sorted, labile to sub-labile in part, calcareous and clayey sandstone, interbedded carbonaceous siltstone, mudstone, shale, minor coal, bentonite, conglomerate and fossil wood.|30-MAR-12
14635|Orallo Formation|65112|5|Briefly described|p323; p327; Fig 11 p324; Fig 15 p327|Jurassic|Jurassic|Non-marine, upward-fining clastic sedimentary rock. A package (Supersequence L) comprising a lower sand-rich part, followed by a shale-rich unit.||||Overlies Gubberamunda and Pilliga Sandstones; underlies Mooga Sandstone.||22-MAR-12
14635|Orallo Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies both the Gubberamunda Sandstone and the  Pilliga Sandstone, underlies the Mooga Sandstone.||||||
14635|Orallo Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
14635|Orallo Formation|65116|4|Described|p456, Fig 2 p437|Early Cretaceous|Early Cretaceous|Shows increase in interbedded silt and mud in the sandstone compared with Pilliga Sst. Underlies the Mooga Formation, Overlies both the Gubberamunda Sandstone and Pilliga Sandstone, Surat  Basin.||||||06-MAR-12
14635|Orallo Formation|65119|5|Briefly described|Fig 2, Table 1, Fig 7-8, 13-14, 16-19|Early Cretaceous|Late Jurassic|Surat Basin. Lithic sandstone, mudstone, siltstone conglomerate and coal. Formationup to 270 m thick. Age: 140-149 Ma. Fission Track age: 100-140 Ma.||||||07-MAR-12
14635|Orallo Formation|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Gubberamunda and Pilliga Sandstones. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|67133|5|Briefly described|p2, p5, p16-17, p19-21|Cretaceous|Cretaceous|26 samples of this unit were analysed by XRD and optical microscopy for this study. Mainly low energy overbank and swamp deposits. Consists of quartz (30-68%), K-feldspars (~7%) and plagioclase (up to 48%). Kaolinite (up to 22%) is the main clay mineral. The mixed-layer clays vary locally from smectite- to illite-rich.||||Conformably overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.|Friable, medium- to coarse-grained, partly calcareous sandstones with minor siltstone, mudstone and coal beds; bentonitic tuffs indicate contemporaneous volcanic activity.|
14635|Orallo Formation|67402|4|Described|p146 fig SRT3, p148|Barremian|Tithonian|Surat Basin. Deposited in a fluvial environment with local ponding. Approximately 226m thick. See also p154 fig SRT15/16, p156.||Blythesdale Group||Overlies the Gubberamunda Sandstone. Overlain by the Mooga Sandstone.|Sandstone with silty mudstone, bentonite and coal.|
14635|Orallo Formation|67669|5|Briefly described|p11|Late Jurassic|Late Jurassic|Of Bowen Basin.||Unit of Blythesdale Group.||Overlain by Mooga Sandstone. Underlain by Gubberamunda Sandstone.||
14635|Orallo Formation|68003|5|Briefly described|p52, p56, p57 Fig.3-n.|Early Cretaceous|Early Cretaceous|Surat Basin. Equivalent to part of Keelindi beds.||Unit in Blythesdale Group.||Overlies Gubberamunda Sandstone and Pilliga Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|68004|5|Briefly described|p87, p174.|||Organic-rich: high TOC. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows. Forms a poor-quality seal for the Pilliga Sandstone.||||||
14635|Orallo Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Late Jurassic|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Fluvial environment.||||Conformably overlies Pilliga Sandstone. Is overlain by Mooga Sandstone.|Medium-grained, sub-lithic sandstone and interbedded siltstone and mudstone; minor coal seams.|
14635|Orallo Formation|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
14635|Orallo Formation|68135|5|Briefly described|p52 fig 2b|Early Cretaceous|Early Cretaceous|Surat Basin (NSW and QLD). Contains plant macrofossils.||||Overlies Pilliga and Gubberamunda Sandstones. Is overlain by Mooga Sandstone|Interbedded sandstone and siltstone.|14-SEP-17
14635|Orallo Formation|68139|6|Mentioned|p23|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|68553|6|Mentioned|Map legend; schematic diagram.|Early Cretaceous|Jurassic|Surat Basin. This unit, as well as Bungil and Southlands Formations; Gubberamunda, Hooray, Longsight and Mooga Sandstones, and Kumbarilla beds, are all mapped under the symbol, JKb.||||||
14635|Orallo Formation|68576|5|Briefly described|Q_4: p3-4, p22, p24|Early Cretaceous|Late Jurassic|Surat Basin. Previously known as Fossil Wood beds because it contains petrified wood. Is mined for bentonite. Deposited in a lacustrine environment with periods of volcanic activity.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.|Friable, medium- to coarse-grained, sub-labile to labile sandstone, in part calcareous, and lesser interbedded carbonaceous siltstone, silty mudstone, bentonite and coal. Fossil wood and conglomerate beds are common in the sandstone.|
14635|Orallo Formation|68593|5|Briefly described|p3-4, p45, p47|Early Cretaceous|Late Jurassic|Fluvial deposits. A minor aquifer in the map area.||||Overlies Pilliga Sandstone. Is overlain by Mooga Sandstone.|Medium-grained, sub-lithic sandstone and interbedded siltstone and mudstone with minor coal.|
14635|Orallo Formation|69582|5|Briefly described|p36, p38|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Gubberamunda Sandstone. Overlain by the Mooga Sandstone.|Sandstone, mudstone.|
14635|Orallo Formation|69594|5|Briefly described|p519, p527, p537-539, p573|Valanginian|Berriasian|Day (1964); = Orallo Measures and Orallo Coal Measures of Jensen (1926); = Fossil Wood Stage or Series of Reeves (1947); = Fossil Wood beds of Whitehouse (1955) in his Blythesdale Group. Northern Surat Basin. 150-350m thick. Fluvial deposits with sporadic lacustrine and swamp conditions in the upper part; deposition punctuated by tuffs. The source of most of QLD's bentonite (derived from tuffs). RELATED UNITS (continued): Equivalent to Hooray Sandstone and upper Kumbarilla beds.||||Conformably and transitionally overlies Gubberamunda Sandstone. Is overlain conformably by Mooga Sandstone (locally disconformably). Grades into lower Southlands Formation. See COMMENTS for more.|Sublabile to labile sandstones, lesser interbedded carbonaceous siltstone, mudstone, bentonite and minor coal with some conglomerates interbedded with the sandstones.|
14635|Orallo Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous|Mineralogy and likely chemical changes from CO2 injection discussed.||||||
14635|Orallo Formation|69790|6|Mentioned|p1063 Fig.2|Cretaceous|Cretaceous|Northern Surat Basin.||||||
14635|Orallo Formation|70036|5|Briefly described|Map legend|||Surat Basin. Included in a mapped unit of a Late Jurassic to Early Cretaceous meandering stream sequence: quartzose sandstone and conglomerate with minor shale, mudstone and coal.||||||
14635|Orallo Formation|70821|5|Briefly described|p21 Fig.2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Berriasian.||||Overlies Gubberamunda Sandstone. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|71806|6|Mentioned|p484|Cretaceous|Cretaceous|Surat Basin.||||||
14635|Orallo Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||||Overlies Gubberamunda and Pilliga Sandstones. Is overlain by Mooga Sandstone.||
14635|Orallo Formation|72921|5|Briefly described|p15 Fig.2.|Cretaceous|Late Jurassic|Shown as located in the Surat Basin, both Qld and NSW.||||Overlies Pilliga Sandstone and Gubberamunda Sandstone and underlies Mooga Sandstone||
14635|Orallo Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: 119, 146, 151-152, 168-172, 177-178, 191.||||||
14635|Orallo Formation|73193|6|Mentioned|p369|Valanginian|Berriasian|Surat Basin.||||Underlain by Gubberamunda Sandstone. Overlain by Mooga Sandstone.||
14671|Otford Sandstone Member|22745|6|Mentioned|p127|||Sydney Basin.||||||
14671|Otford Sandstone Member|29901|4|Described|Table 1|||||||||
14671|Otford Sandstone Member|30007|6|Mentioned|p61|||||||||
14671|Otford Sandstone Member|31128|6|Mentioned|Table 1|||||||||
14671|Otford Sandstone Member|31887|6|Mentioned|p7|||||||||
14671|Otford Sandstone Member|33685|6|Mentioned|Table 2|||||||||
14671|Otford Sandstone Member|34336|6|Mentioned|Table 5.15|||||||||
14671|Otford Sandstone Member|34337|6|Mentioned|Table 5.18|||||||||
14671|Otford Sandstone Member|36220|4|Described|p67|||See also Table 20.||||||
14671|Otford Sandstone Member|39296|6|Mentioned|Fig. 11.1|||||||||
14671|Otford Sandstone Member|42787|6|Mentioned|Table 1 P126|||||||||
14671|Otford Sandstone Member|42896|4|Described|p27|||of Wombarra Claystone||||||
14671|Otford Sandstone Member|43383|14|Not recorded|p22|||Part of Clifton Sub-Group||||||
14671|Otford Sandstone Member|45090|6|Mentioned|p197|||Refers Hanlon et al. (1953)||||||
14671|Otford Sandstone Member|67560|5|Briefly described|p258|Triassic|Triassic|A well-known marker bed. 5 m thick. Constrained by the age of the Wombarra Shale.||Of the Wombarra Shale.||||
14671|Otford Sandstone Member|68202|6|Mentioned|p176|Triassic|Triassic|Sydney Basin.||Wombarra Claystone.||||
14761|Paddys Flat Formation|32086|6|Mentioned|p325|||Refers Olgers & Flood (1970)||||||
14761|Paddys Flat Formation|32492|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
14761|Paddys Flat Formation|32494|6|Mentioned|p84|||L.Permian||||||
14761|Paddys Flat Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
14761|Paddys Flat Formation|33476|6|Mentioned|Table 1|||||||||
14761|Paddys Flat Formation|36528|6|Mentioned|p182|||||||||
14761|Paddys Flat Formation|36936|4|Described|p208|||||||||
14761|Paddys Flat Formation|36961|6|Mentioned|p212|||||||||
14761|Paddys Flat Formation|42866|5|Briefly described|Table 2, P12|||||||||
14761|Paddys Flat Formation|48940|3|Fully described|p44|||||||||
14761|Paddys Flat Formation|69793|5|Briefly described|p1109, p1113 Fig.3, p1114-1121|Gzhelian|Late Carboniferous|New name. Comprises the eastern part of the former Emu Creek Formation. Type section, and proposed secondary type section, described. Deltaic succession. Deformed by open, steeply inclined folds. Maximum ICP-MS U-Pb depositional age from detrital zircons.|305.5 +/- 1.4 Ma (Hoy et al., 2014).||||Thickly-bedded, immature sandstone with feldspathic and lithic clasts commonly altered to clay, and polymictic pebble-cobble, clast-supported conglomerate; minor interlaminated sandstone and siltstone.|
14761|Paddys Flat Formation|70728|5|Briefly described|p265-268,272|Gzelian|Gzelian|Geological province: Emu Creek terrane, New England Orogen. Slightly deformed, immature, shallow-marine sedimentary rocks. LA-ICP-MS detrital zircon age of c. 306 Ma (Hoy et al., 2014) as a maximum depositional constrant. Broadly correlable to Currabubula Formation.|c. 306 Ma (detrital zircon; Hoy et al., 2014).|||Overlain by Razorback Creek Mudstone. Underlain unconformably by Emu Creek Formation.||
14788|Palerang Formation|24116|5|Briefly described|p88|||||||||
14788|Palerang Formation|30735|2|Defined|p35|Silurian|Silurian|||||||
14788|Palerang Formation|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
14788|Palerang Formation|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
14788|Palerang Formation|31161|5|Briefly described|PA7|||||||||
14788|Palerang Formation|31411|5|Briefly described|p16|||||||||
14788|Palerang Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
14788|Palerang Formation|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
14788|Palerang Formation|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
14788|Palerang Formation|36413|6|Mentioned|Table 3|||||||||
14788|Palerang Formation|37727|5|Briefly described|p77|||||||||
14788|Palerang Formation|40276|6|Mentioned|p3|||||||||
14788|Palerang Formation|40328|5|Briefly described|p186|||||||||
14788|Palerang Formation|42497|5|Briefly described|Map Legend|Pridolian|Pridolian|||||||
14788|Palerang Formation|62070|5|Briefly described|p38,|Late Silurian|Late Silurian|||Top of the Mount Fairy Group.||Overlies Long Flat Volcanics.|Nonfossiliferous graded bedded quartzose sandstone siltstone and shale.|
14788|Palerang Formation|68592|6|Mentioned|p725-7, p834|||Felton and Huleatt (1977) and Wyborn and Owen (1986) included this formation in Mount Fairy Group in Braidwood and Araluen 1:100 000 map sheet areas, along with other units. However, now rocks of Palerang Formation have been attributed to other units.||||||
14788|Palerang Formation|71069|6|Mentioned|p134, p169|||Discontinued and constituent rocks placed within the Abercrombie Formation.||||||
14792|Paling Yard Formation|22857|5|Briefly described|p217 (photo #1), p492 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Of the Black Rock Subgroup (Catombal Group). Interbedded sandstone and reddish siltstone.||||||
14792|Paling Yard Formation|22859|6|Mentioned|p217|||||||||
14792|Paling Yard Formation|23043|5|Briefly described|Map Legend|Frasnian|Frasnian|of Black Rock Subgroup, Catombal Group.||||||
14792|Paling Yard Formation|23170|2|Defined|p250|Famennian|Frasnian|of Black Rock Subgroup.||||||
14792|Paling Yard Formation|23214|3|Fully described|p234|Late Devonian|Late Devonian|Of Black Rock Subgroup. Geological Province: Lambie Basin. Overlying unit: Brymedura Sandstone. Maximum thickness: 85m.||||||
14792|Paling Yard Formation|24247|5|Briefly described|p37, p40|||Parent: Black Rock Subgroup. Overlying Unit: Columbine Sandstone||||||
14792|Paling Yard Formation|32151|6|Mentioned|p209|||Refers Conolly (1963)||||||
14792|Paling Yard Formation|33116|6|Mentioned|p229|||?U.Dev.||||||
14792|Paling Yard Formation|33732|4|Described|p119|||||||||
14792|Paling Yard Formation|34109|4|Described|Table 3.9|||See also P159||||||
14792|Paling Yard Formation|35246|6|Mentioned|p172|||||||||
14792|Paling Yard Formation|43512|2|Defined|p73,76-78,102-104||Late Devonian|Buff to green shales and siltstones with some pebbly or conglomerate layers||||||
14792|Paling Yard Formation|43513|14|Not recorded|p72|||||||||
14792|Paling Yard Formation|43640|5|Briefly described|Map Legend||Devonian|||||||
14792|Paling Yard Formation|43782|6|Mentioned|Map diagram|Frasnian|Frasnian|of Black Rock Subgroup, Catombal Group.||||||
14792|Paling Yard Formation|73299|5|Briefly described|p1104 Fig.10, p1105|Late Devonian|Late Devonian|Molong High. Overlies the Lambian unconformity in Fig.10 cross-section.||Catombal Group||Overlies the Bulls Camp Volcanics, underlies the Brymedura Sandstone.|Conglomerate in lower part, sandstone in upper part.|
14860|Paragon Group|6823|6|Mentioned|p203, 205|Palaeoproterozoic|Palaeoproterozoic|||Willyama Supergroup||||26-MAR-22
14860|Paragon Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent WIllyama Supergroup Geol. province Broken Hill - Olary Domain||||||
14860|Paragon Group|22500|6|Mentioned|p10, 13|||||||||
14860|Paragon Group|22553|5|Briefly described|fig2p77|Proterozoic|Proterozoic|||||||
14860|Paragon Group|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
14860|Paragon Group|22588|6|Mentioned|p85|||||||||
14860|Paragon Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
14860|Paragon Group|22641|6|Mentioned|p692|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|22771|5|Briefly described|p44,47-48|||||||||
14860|Paragon Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: ~1700m.||||||07-NOV-08
14860|Paragon Group|22884|5|Briefly described|p40 Fig. 1, p43 Fig. 3, p46|||Of the Willyama Supergroup. Contains Mount Howden Formation. Overlies Sundown Group. Geological province: Olary/Broken Hill Domains.||||||26-MAR-09
14860|Paragon Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|22962|5|Briefly described|p73,76||Statherian|||||||
14860|Paragon Group|22966|5|Briefly described|p2,4||Proterozoic|||||||
14860|Paragon Group|22967|5|Briefly described|p25,6,30,2,3,39,49||Statherian|||||||
14860|Paragon Group|23025|6|Mentioned|Fig1p75|||||||||
14860|Paragon Group|23160|6|Mentioned|fig1|||||||||
14860|Paragon Group|23223|5|Briefly described|p43|||Of the informal Upper Willyama Supergroup. In the Curnamona Province.||||||11-SEP-07
14860|Paragon Group|23248|5|Briefly described|Fig2p169|||||||||
14860|Paragon Group|23346|6|Mentioned|48|||||||||
14860|Paragon Group|23347|6|Mentioned|p51 Tb. 1, p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
14860|Paragon Group|23369|6|Mentioned|p26|||||||||
14860|Paragon Group|24197|5|Briefly described|p62|||Of the Willyama Supergroup. Organic-rich sediments intially progressing to fine-grained turbidites. Geological Province: Broken Hill Block.||||||07-FEB-11
14860|Paragon Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
14860|Paragon Group|38969|4|Described|p210|||||||||
14860|Paragon Group|39662|2|Defined|p433|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|39883|6|Mentioned|p380|||||||||
14860|Paragon Group|39885|6|Mentioned|Fig.2|||||||||
14860|Paragon Group|40290|6|Mentioned|p5|||||||||
14860|Paragon Group|40595|6|Mentioned|p85|||||||||
14860|Paragon Group|40822|6|Mentioned|Fig.2|||||||||
14860|Paragon Group|41093|4|Described|p253|||||||||
14860|Paragon Group|41145|6|Mentioned|Fig.4|||||||||
14860|Paragon Group|41402|6|Mentioned|p37|||||||||
14860|Paragon Group|41630|5|Briefly described|p3|||||||||
14860|Paragon Group|42261|6|Mentioned|Fig 1 P530|||||||||
14860|Paragon Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
14860|Paragon Group|42537|4|Described|p15|||||||||
14860|Paragon Group|42720|5|Briefly described|map legend|Paleoproterozoic||Variation on Paragon Group, NSW.||||||07-NOV-08
14860|Paragon Group|42813|6|Mentioned|p9|||||||||
14860|Paragon Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
14860|Paragon Group|42953|6|Mentioned|p59|||||||||
14860|Paragon Group|43052|6|Mentioned|Fig.4.22|||||||||
14860|Paragon Group|43086|6|Mentioned|Fig.3|||||||||
14860|Paragon Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
14860|Paragon Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
14860|Paragon Group|43572|6|Mentioned|Fig.3.2 p6|||||||||
14860|Paragon Group|43583|5|Briefly described|Table 1, p2138|||||||||
14860|Paragon Group|46598|4|Described|p305|||||||||
14860|Paragon Group|50045|4|Described|p115 Fig. 2, p116 Fig. 3|Statherian|Statherian|Includes Dalnit Bore Metasediments, Bijerkerno Metasediments and Cartwrights Creek Metasediments. Geological Province: Broken Hill Block. Of the Willyama Supergroup. Underlain by Sundown Group. Age: 1640 Ma.||||||26-FEB-13
14860|Paragon Group|50606|5|Briefly described|p1.1|||Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||
14860|Paragon Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Uppermost unit of the Willyama Supergroup.  Conformably overlies the Sundown Group.  Geological Province: Broken Hill Block.||||||07-NOV-08
14860|Paragon Group|60485|5|Briefly described|p29|||Of the Willyama Supergroup. Geological Province: Broken Hill Domain.||||||
14860|Paragon Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill.||||||07-NOV-08
14860|Paragon Group|61606|5|Briefly described|p4 Fig. 2|||Of the Willyama Supergroup. Includes Dalnit Bore Metasediments, Bijerkerno Metasediments, Cartwrights Creek Metasediments.||||||
14860|Paragon Group|61735|5|Briefly described|p635 Fig. 1, p650-51|Paleoproterozoic|Paleoproterozoic|In the Euriowie Block. See also p636 Fig. 2.||||||30-JUN-09
14860|Paragon Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Contains Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Geological province: Broken Hill Domain.||||||
14860|Paragon Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
14860|Paragon Group|62373|5|Briefly described|p503 Fig.2|||Geological Province: Curnamona Province/Broken Hill Domain.||||||
14860|Paragon Group|62473|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Geological province: Broken Hill Domain.||||||17-JUN-09
14860|Paragon Group|62535|5|Briefly described|p663, p665, p666 Fig.3, p668, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill district. Ages from the middle of the Group; closely comparable to ages of tuff units associated with the Mount Isa and Hilton Pb-Zn-Ag orebodies (Gun Supersequence). Hosts minor Zn-Pb mineralization.|1657 +/- 4 Ma (middle) - c.1640 Ma (upper).||Cartwrights Creek, Bijerkerno, Dalnit Bore, Metasediments.||Includes tuffaceous sedimentary rocks.|
14860|Paragon Group|62536|4|Described|p633, 635-636, 638, 641, 649-651, 656|||See also p659. Broken Hill area. Similar zircon provenance ages as Broken Hill and Sundown Groups. Contains very minor Pb-Zn mineralisation.|~1655 Ma.||Bijerkerno, Dalnit Bore Metasediments.|Is intruded by Cusin Creek pluton.|Metasedimentary rocks, including calc-silicate and psammitic lithotypes.|
14860|Paragon Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. Coeval with the northern Australian Pb-Zn basins; possibly prospective for Mount Isa and Century styles of mineralisation.|>1650 to <1640 Ma.|Unit in Willyama Supergroup.|Includes King Gunnia Calc-silicate Member; Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group.||
14860|Paragon Group|62993|6|Mentioned|p35, p37, p39|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Cartwrights Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Equivalent to Strathearn Group.||19-DEC-21
14860|Paragon Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Age: ~1657-1640Ma. Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
14860|Paragon Group|63102|5|Briefly described|p9,13,35-36,p38-39,59|Neoproterozoic|Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.|||Includes Dalnit Bore metasediments, Bijerkerno Metasediments, Cartwight Creek Metasediments and King Ginnia Calc-silicate Member.|||22-OCT-19
14860|Paragon Group|63186|5|Briefly described|p66, p67|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Includes Bijerkerno Metasediments. Max. age: ca 1645 Ma. Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
14860|Paragon Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Includes the Gunnia Calc-Silicate Member. Geological Province: Broken Hill Domain; unnamed equivalents in Olary Domain.||||||07-NOV-08
14860|Paragon Group|63519|5|Briefly described|p5, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Overlies Sundown Group with sharp contact.||||||07-NOV-08
14860|Paragon Group|63866|5|Briefly described|p36, p38|||Broken Hill Domain, Curnamona Province.||Willyama Supergroup|Includes the Cartwrights Creek Metasediments, Bijerkerno Metasediments and the Dalnit Bore Metasediments.|||
14860|Paragon Group|64097|5|Briefly described|p302, p303|Paleoproterozoic|Paleoproterozoic|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Overlies Sundown Group. Geological province: Broken Hill Domain/Curnamona Province. Mostly siliciclastic metasediments, tending to be graphitic.||||||07-FEB-11
14860|Paragon Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
14860|Paragon Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
14860|Paragon Group|64725|6|Mentioned|p58 Fig.2. |||||||||
14860|Paragon Group|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Includes Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments. Geological province: Broken Hill Domain, Curnamona province. Broadly equivalent to Strathearn Group in the Olary Domain.||||||07-FEB-11
14860|Paragon Group|64742|5|Briefly described|p320, p322, pp326-327, p330, pp332-333.|||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.||Unit in Willyama Supergroup.|Includes King Gunnia Calc-Silicate Member, Cartwrights Creek Metasediments, Bijerkerno Metasediments and Dalnit Bore Metasediments.|||
14860|Paragon Group|64743|5|Briefly described|pp339-340, pp342-344,  pp346-347. |Paleoproterozoic|Paleoproterozoic|Broken Hill Block.|1660-1600 Ma.|Unit in Willyama Supergroup.||Overlies Sundown Group. Equivalent to Mount Howden Subgroup, Olary Block; and to McNamara Group, Mount Isa Inlier.||
14860|Paragon Group|64744|5|Briefly described|p353 Fig.4, p356. |Statherian|Statherian|Broken Hill Domain. Psammopelitic sediments.||Unit in Willyama Supergroup.||||
14860|Paragon Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Geological province: Broken Hill Domain. Equivalent of Strahearn Group in Olary Domain.||||||07-FEB-11
14860|Paragon Group|65887|5|Briefly described|p51|||Primarily pelitic and psammo-pelitic metasediments. Thought to be deposited in a continental slope to deep water environment.||||||
14860|Paragon Group|66302|5|Briefly described|p35, p36 Fig.9, p38, p39, p40, p73|||Broken Hill Domain, Curnamona Province. Represents sag phase deposition post-dating the climax of rifting. Peak metamorphism interpreted to have occurred at 1675 Ma.||Willyama Supergroup|Includes the Cartwrights Creek Metasediments, Bijerkerno Metasediments and the Dalnit Bore Metasediments.|Equivalent to the Strathearn Group.||
14860|Paragon Group|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Sundown Group.||
14860|Paragon Group|67323|5|Briefly described|Eastern Australia Time-Space Plot, p35|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Post-rift sedimentation.|~1660-1650 Ma.||Dalnit Bore, Bijerkerno, Cartwright Creek Metasediments.|||
14860|Paragon Group|67621|6|Mentioned|p224|||||||||
14860|Paragon Group|68126|5|Briefly described|p6, p26, p30|||Broken Hill Domain, Curnamona Province.|~1670-1640 Ma (Page et al. in prep).|Willyama Supergroup.||Overlies Sundown Group. Equivalent to Strathearn Group.||
14860|Paragon Group|69999|5|Briefly described|p3, p8 Photos 5,7, p12-13, p15, p20|Paleoproterozoic|Paleoproterozoic|Euriowie Block, Curnamona Province. Upper, post-rift, deeper water, sag phase deposition followed by marine regression. Contains the only greenschist facies rocks from the Olarian Orogeny.|||||Fine-grained chlorite-biotite-chiastolite schist.|
14860|Paragon Group|70000|5|Briefly described|p31, p33-34, p37, p39|Statherian|Statherian|||Unit in Willyama Supergroup.|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore, Metasediments.|Conformably overlies the Sundown Group.|Graphitic siltstones and aluminous metapelitic rocks with minor calc-silicate; grading upwards into albitic, rippled psammitic and interbedded phyllitic rocks; then thinly bedded graphitic, pelitic to psammopelitic phyllite with lesser psammite.|
14860|Paragon Group|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.|Includes Cartwrightrs Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group.|Mainly graphitic metasediments, including spotted and non-spotted phyllites, chiastolite phyllites and schists, albitic psammites, and very minor calc-silicate rock.|
14860|Paragon Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Cartwrights Creek, Bijerkerno and Dalnit Bore, Metasediments.|Overlies Sundown Group.|Predominantly graphitic metasedimentary rocks including phyllite, schist, psammite and minor calc-silicate.|
14860|Paragon Group|70405|6|Mentioned|p15, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1640 Ma - 1655 Ma|Wilyama Supergroup||||
14860|Paragon Group|70657|4|Described|p5, p6 Fig.1, p10 Fig.4, p11 Fig.5|Statherian|Statherian|See also p13 Fig.6, p15, p17, p20, p33, p40, p42, p44, p65. Curnamona Province; Broken Hill, Mulyungarie Domains. Unconformity mid-Group ~1655-1651 Ma. Age range inferred from Fig.4.|<1672 +/- 7 Ma - 1642 +/-5 Ma|Upper Willyama Supergroup|Cartwrights Creek, Bijerkerno and Dalnit Bore Metasediments.|Overlies Sundown Group (in Mulyungarie and Broken Hill Domains). Equivalent to the Strathearn Group.||
14860|Paragon Group|70658|5|Briefly described|p2, 7, 15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|~1655 Ma - 1642 +/- 5 Ma.|Willyama Supergroup.|Cartwrights Creek, Bijerkerno, Dalnit Bore Metasediments.|Equivalent to Strathearn Group (Olary Domain).||
14860|Paragon Group|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
14860|Paragon Group|71968|5|Briefly described|p1,3-4,18,26,28,35-36,38,45-47|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Occurs at the top of exposed Willyama Supergroup. Depositional age range of c. 1670-1640 Ma (Page et al., 2000; Page et al., 2005a, b; Stevens et al., 2008). Change from sliciclastic-dominated Sundown Group to fine-grained carbonaeous Paragon Group reflect a significant decrease (starving) in siliciclastic sediment input to the Curnamona Rift Basin; also reflects a change from older detrital zircons (c. 1792 Ma) in Sundown Group to younger populations in Paragon Group (c. 1754 Ma), possibly indicating a change in sediment source and supply and possibly exposure of a new source region based on relative sea level change.||Unit of Willyama Supergroup.|Includes Dalnit Bore Metasediments, Bijerkerno Metasediments, Cartwrights Creek Metasediments.|Underlain conformably by Sundown Group.||
14860|Paragon Group|72435|6|Mentioned|p715|Statherian|Statherian|Basal boundary with Sundown Group is gradational in places. Thickness: ~1700 m.|ca 1670 - 1640 Ma|||Underlain by Sundown Group.||
14860|Paragon Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain. Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup||||
14860|Paragon Group|72461|5|Briefly described|p5-6, p13, p16, p19|||||Willyama Supergroup|Includes the Dalnit Bore Metasediments, Bijerkerno Metasediments and the Cartwrights Creek Metasediments.|Conformably overlies the Sundown Group.|Sedimentary rocks.|
14860|Paragon Group|73165|6|Mentioned|p637, Fig. 12|||Curnamona Province.||||||
14860|Paragon Group|73243|6|Mentioned|p52 Fig.1, p53 Fig.2 p59|Statherian|Statherian|Broken Hill block-Euriowie block.|up to ~1640 Ma|Willyama Supergroup||||
14860|Paragon Group|73308|6|Mentioned|p607, 610, 622||||< c.1640 Ma.|Willyama Supergroup.||||
14860|Paragon Group|73429|6|Mentioned|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Willyama Supergroup, upper||||
14860|Paragon Group|73482|5|Briefly described|p422 Fig.3, p423, p426-427, p434|||Known thickness of 1.7 km. Younger than 1670 Ma in age. See also p428 Fig.7, p429 Fig.8.||Willyama Supergroup|Cartwright Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Overlies Sundown Group|Metasediments. Biotite and andalusite metamorphic grades in parts.|
14860|Paragon Group|73512|5|Briefly described|p1-4, p7|Statherian|Statherian|Curnamona Province, Broken Hill Block. Represents deeper-water basin fill. [Also written as upper Paragon Group, p1].||Willyama Supergroup||Underlain by Sundown Group.||
14860|Paragon Group|73524|6|Mentioned|p2|||Sag-phase metasediments.||Willyama Supergroup, upper||||
14860|Paragon Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3||Statherian|||Willyama Supergroup|Cartwrights Creek Metasediments, Bijerkerno Metasediments, Dalnit Bore Metasediments|Overlies Sundown Group||
14873|Parilla Sand|2967|4|Described|p9, 12, p15 Fig.2.2, p18, 21-22, 24|Pliocene|Miocene|Murray Basin. Is shown as a unit in the Murray Group in Fig.2.2, but on p24 is said to have been excluded from that Group by Lawrence (1966). A 60-100m thick unconfined aquifer of marine origin; saline. Late Tertiary. Originally defined by Firman (1965) in South Australia; Lawrence (1975) included the Victorian equivalents of the marine Loxton Sand of South Australia. Is separated from the overlying Blanchetown Clay by the Karoonda Surface. Hydrochemistry (salinity) detailed. See also p26-29, 31-33, 35-37, 40-41, 43-52, 80, 84-85, 87-88, 96, 102, 118, 132, 142, 145, 148, 154-156, 158, 162, 169, 172-179, 181-185, 187, 191-193, 195, 197-198, 205, 208-209, 213, 216, 221, 224, 229, 231, 235, 247, 254, 257, 259, 278, 280, 283, 285-286, 290, 292, 295-297, 300, 304, 313, 315, 318-320, 322, 328, 331, 333-334, 336-338.||Murray Group.|Kerang Sand Member, Tragowel Member, Wandella Sandstone Member.|Overlies Bookpurnong beds and Calivil Formation. Is separated from the underlying Geera Clay by the Mologa Surface. Is overlain by Shepparton Formation. See COMMENTS for more.|Sparingly fossiliferous, fine-grained, transgressive marine sandstones. Weathering has produced a silicified and ferruginised capping (the Karoonda Surface). Local occurrences of heavy mineral sands (beach or shallow marine placers) up to 1m thick.|
14873|Parilla Sand|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Late Pliocene|Geological Province: Murray Basin.||||||13-AUG-07
14873|Parilla Sand|22531|6|Mentioned|p2|Pliocene|Pliocene|||||||
14873|Parilla Sand|22756|6|Mentioned|P31|||||||||
14873|Parilla Sand|22773|5|Briefly described|Fig24.8p352,354||Pliocene|||||||
14873|Parilla Sand|22782|5|Briefly described|p13|Pliocene|Pliocene|||||||
14873|Parilla Sand|22799|4|Described|p35|||||||||
14873|Parilla Sand|22857|5|Briefly described|p339, p352 Fig. 24.8, p354|Late Pliocene|Late Pliocene|Marginal marine to non-marine sands. Heavy mineral sands containing rutile, zircon and ilmenite. Geological Province: Murray Basin.||||||
14873|Parilla Sand|22887|5|Briefly described|Fig.6 p13|Late Pliocene||||||||
14873|Parilla Sand|22893|3|Fully described|p34,35,37 fig9,11|Pleistocene|Pliocene|||||||
14873|Parilla Sand|23164|4|Described|p16|Early Pliocene|Late Miocene|||||||
14873|Parilla Sand|23166|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23167|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23168|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23169|5|Briefly described|Map legend||Miocene|||||||
14873|Parilla Sand|23307|5|Briefly described|Map Legend|Neogene|Neogene|||||||
14873|Parilla Sand|23560|5|Briefly described|p152|Pliocene|Pliocene|||||||
14873|Parilla Sand|23603|5|Briefly described|p11|Early Pliocene|Late Miocene|||||||
14873|Parilla Sand|23604|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23605|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23606|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23607|5|Briefly described|Map Legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|23818|5|Briefly described|p174 Fig.84, p213|Pliocene|Pliocene|Geological Province: Murray Basin. Overlying unit: Coomandook Formation.||||||
14873|Parilla Sand|23884|5|Briefly described|p155 Fig.13.2|Late Pliocene|Late Pliocene|Geological Province: Murray Basin. See also Parilla Sands.||||||28-APR-05
14873|Parilla Sand|24104|5|Briefly described|p149|Neogene|Neogene|Geological Province: Murray Basin.||||||
14873|Parilla Sand|24177|3|Fully described|p72, p103|Early Pliocene|Late Miocene|Overlain by the Shepparton Formation. Interfingered with Calivil Formation. Indication that the Bagshot Formation of Bendigo region (Cherry & Wilkinson) belongs to Parilla Sand due to no lithological differences. Geological Province: Murray Basin.||||||
14873|Parilla Sand|24328|5|Briefly described|Map legend|Neogene|Neogene|||||||
14873|Parilla Sand|24329|5|Briefly described|Map legend|Neogene|Neogene|||||||
14873|Parilla Sand|24439|5|Briefly described|p8, p15|Pliocene|Pliocene|Siliceous marine deposits.  Of Brown and Wilkinson (1991).  See also p47 Fig. 22.  Geological Province: Murray Basin.||||||06-APR-05
14873|Parilla Sand|24440|5|Briefly described|Map legend|||||||||
14873|Parilla Sand|24468|6|Mentioned|p415|Pliocene|Pliocene|Geological Province: Gippsland Basin||||||
14873|Parilla Sand|24551|5|Briefly described|p322 Fig. 10.29, p324, 306|||Of the Wunghnu Group.  Geological Province: Murray Basin.  Max thickness: 150m.||||||
14873|Parilla Sand|24574|6|Mentioned|p705|||Geological Province: Murray Basin||||||
14873|Parilla Sand|29591|6|Mentioned|Table 20|||||||||
14873|Parilla Sand|29697|5|Briefly described|Table 1|||||||||
14873|Parilla Sand|29898|6|Mentioned|p138|||||||||
14873|Parilla Sand|30145|6|Mentioned|p183|||||||||
14873|Parilla Sand|30522|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|30750|6|Mentioned|p1|||Late Pliocene||||||
14873|Parilla Sand|30751|6|Mentioned|Map legend|late Pliocene|late Pliocene|||||||
14873|Parilla Sand|30752|6|Mentioned|p4|||||||||
14873|Parilla Sand|30753|4|Described|p16|||Upper Pliocene||||||
14873|Parilla Sand|30754|2|Defined|Appendix 1|late Pliocene|late Pliocene|See also p14,22-24,38,41.||||||10-NOV-10
14873|Parilla Sand|30758|6|Mentioned|p66|||Stratigraphy||||||
14873|Parilla Sand|30807|6|Mentioned|p101|||Suggested map symbol||||||
14873|Parilla Sand|30905|6|Mentioned|p146|||||||||
14873|Parilla Sand|30934|6|Mentioned|Map legend|Pliocene|Pliocene|Equivalence with Dorodong Sand||||||
14873|Parilla Sand|30935|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|30936|6|Mentioned|Map legend|Miocene|Miocene|||||||
14873|Parilla Sand|30994|6|Mentioned|Fig. 2|||||||||
14873|Parilla Sand|30996|3|Fully described|p31|||Refers Firman (1971).||||||27-OCT-08
14873|Parilla Sand|31554|6|Mentioned|p13|||||||||
14873|Parilla Sand|31624|6|Mentioned|p125|||||||||
14873|Parilla Sand|31743|5|Briefly described|p8|||||||||
14873|Parilla Sand|31744|6|Mentioned|p427|||||||||
14873|Parilla Sand|31745|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|31746|3|Fully described|p196|||||||||
14873|Parilla Sand|31747|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
14873|Parilla Sand|31920|4|Described|p59|||See also Fig 3-2||||||
14873|Parilla Sand|31952|6|Mentioned|p7|||||||||
14873|Parilla Sand|32225|6|Mentioned|p22|||||||||
14873|Parilla Sand|32426|5|Briefly described|p141|||||||||
14873|Parilla Sand|32432|5|Briefly described|Table 1|||||||||
14873|Parilla Sand|32439|6|Mentioned|p99|||||||||
14873|Parilla Sand|32859|4|Described|p68|||Upper Pliocene.||||||14-JAN-09
14873|Parilla Sand|32861|5|Briefly described|Table 1|||U.Pliocene||||||
14873|Parilla Sand|33048|6|Mentioned|p197|||||||||
14873|Parilla Sand|33725|6|Mentioned|p9|||Small sinkholes||||||
14873|Parilla Sand|33826|6|Mentioned|p42|||Strat. table||||||
14873|Parilla Sand|33834|5|Briefly described|p11|||||||||
14873|Parilla Sand|34114|4|Described|p50|||Upper Pliocene||||||
14873|Parilla Sand|34180|6|Mentioned|p212|||Late Pliocene. Equivalent Norwest Bend Formation.||||||
14873|Parilla Sand|34191|6|Mentioned|Map legend|late Pliocene|late Pliocene|||||||
14873|Parilla Sand|34308|6|Mentioned|Fig.84|||Yatalan. See P186||||||
14873|Parilla Sand|34313|6|Mentioned|p165|||See also P166. Tertiary||||||
14873|Parilla Sand|34459|4|Described|p11|||U.Pliocene||||||
14873|Parilla Sand|34460|4|Described|p164|||||||||
14873|Parilla Sand|34735|4|Described|p33|||Also mention p31.||||||14-JAN-09
14873|Parilla Sand|34757|6|Mentioned|Fig.3|||||||||
14873|Parilla Sand|34758|6|Mentioned|Fig.2|||||||||
14873|Parilla Sand|34813|6|Mentioned|p63|||||||||
14873|Parilla Sand|35066|6|Mentioned|p216|||||||||
14873|Parilla Sand|35071|6|Mentioned|Table 1|||||||||
14873|Parilla Sand|35091|6|Mentioned|p30|||||||||
14873|Parilla Sand|35097|6|Mentioned|Fig.4|||||||||
14873|Parilla Sand|35131|6|Mentioned|p8|||||||||
14873|Parilla Sand|35172|6|Mentioned|p131|||||||||
14873|Parilla Sand|35174|6|Mentioned|p167|||||||||
14873|Parilla Sand|35187|6|Mentioned|Table1|||||||||
14873|Parilla Sand|35200|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
14873|Parilla Sand|35232|5|Briefly described|Table.3|||||||||
14873|Parilla Sand|35272|6|Mentioned|p281|||||||||
14873|Parilla Sand|35274|6|Mentioned|p425|||||||||
14873|Parilla Sand|35285|5|Briefly described|p414|||||||||
14873|Parilla Sand|35541|6|Mentioned|Fig.2|||Geological section of Tertiary and Quaternary sediments||||||
14873|Parilla Sand|36492|6|Mentioned|Fig.1|||||||||
14873|Parilla Sand|37796|6|Mentioned|p161|||||||||
14873|Parilla Sand|37809|6|Mentioned|p5|||||||||
14873|Parilla Sand|37873|4|Described|p2|||||||||
14873|Parilla Sand|38068|6|Mentioned|Fig.7|||See also Fig.8.||||||
14873|Parilla Sand|38601|6|Mentioned|Fig.2|||||||||
14873|Parilla Sand|39322|6|Mentioned|Fig.3|||||||||
14873|Parilla Sand|39329|6|Mentioned|p483|||||||||
14873|Parilla Sand|39967|4|Described|p44|||||||||
14873|Parilla Sand|40003|5|Briefly described|p39|||See also Table 8.||||||
14873|Parilla Sand|40230|6|Mentioned|Fig.1|||||||||
14873|Parilla Sand|40380|6|Mentioned|p221|||||||||
14873|Parilla Sand|40643|6|Mentioned|p157|||||||||
14873|Parilla Sand|40795|5|Briefly described|p80|||||||||
14873|Parilla Sand|41511|5|Briefly described|p19, p21|||||||||
14873|Parilla Sand|41537|6|Mentioned|p350|||||||||
14873|Parilla Sand|41599|6|Mentioned|p192|||||||||
14873|Parilla Sand|41642|6|Mentioned|p216|||||||||
14873|Parilla Sand|41765|6|Mentioned|p42|||||||||
14873|Parilla Sand|41848|6|Mentioned|p357|||Underlies Coonambidgal Formation, Blanchetown Formation, Age Pliocene (P267, 358)||||||
14873|Parilla Sand|41868|5|Briefly described|p552|||See also P579||||||
14873|Parilla Sand|42115|6|Mentioned|p7|||||||||
14873|Parilla Sand|42125|5|Briefly described|p137|||||||||
14873|Parilla Sand|42126|6|Mentioned|p150|||||||||
14873|Parilla Sand|42129|6|Mentioned|Table 1 P253|||||||||
14873|Parilla Sand|42130|6|Mentioned|Fig.3 P265|||||||||
14873|Parilla Sand|42132|6|Mentioned|Fig.5 P298|||||||||
14873|Parilla Sand|42134|4|Described|p339|||||||||
14873|Parilla Sand|42137|6|Mentioned|p370|||||||||
14873|Parilla Sand|42138|6|Mentioned|p392|||||||||
14873|Parilla Sand|42184|6|Mentioned|Fig.2 P348|||||||||
14873|Parilla Sand|42443|6|Mentioned|p4|||||||||
14873|Parilla Sand|42454|5|Briefly described|p12||Pliocene|||||||
14873|Parilla Sand|42509|4|Described|p2|||||||||
14873|Parilla Sand|42510|5|Briefly described|p35|||||||||
14873|Parilla Sand|42512|5|Briefly described|p68|||||||||
14873|Parilla Sand|42513|6|Mentioned|p96|||||||||
14873|Parilla Sand|42514|5|Briefly described|p116|||||||||
14873|Parilla Sand|42515|5|Briefly described|p134|||||||||
14873|Parilla Sand|42516|6|Mentioned|p152|||||||||
14873|Parilla Sand|42517|5|Briefly described|p169|||||||||
14873|Parilla Sand|42518|5|Briefly described|p185|||||||||
14873|Parilla Sand|42519|5|Briefly described|p205|||||||||
14873|Parilla Sand|42594|5|Briefly described|p247|||Pliocene||||||
14873|Parilla Sand|42635|6|Mentioned|p94|||||||||
14873|Parilla Sand|42717|5|Briefly described|map legend|Pliocene||||||||
14873|Parilla Sand|42720|5|Briefly described|map legend|Pliocene||||||||
14873|Parilla Sand|42813|5|Briefly described|p24|||||||||
14873|Parilla Sand|42827|3|Fully described|p270|||see also Fig 8.4||||||
14873|Parilla Sand|42881|4|Described|Fig.3, P84|||||||||
14873|Parilla Sand|42966|1|Redefined|Table 26, p162|Late Pliocene||||||||
14873|Parilla Sand|43053|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal, siliceous and clayey sand.||||||25-MAY-05
14873|Parilla Sand|43073|4|Described|p12,Table 3|||||||||
14873|Parilla Sand|43195|5|Briefly described|Map Legend||Late Pleistocene|see also commentary on back of map.||||||
14873|Parilla Sand|43218|4|Described|Fig.3,p22||Tertiary|||||||
14873|Parilla Sand|43258|5|Briefly described|Map Legend||Pliocene|||||||
14873|Parilla Sand|43261|5|Briefly described|Map Legend|Miocene|Oligocene|||||||
14873|Parilla Sand|43298|6|Mentioned|Map Legend||Pliocene|||||||
14873|Parilla Sand|43493|6|Mentioned|32||Pliocene|||||||
14873|Parilla Sand|43578|6|Mentioned|p342|||||||||
14873|Parilla Sand|43627|6|Mentioned|p6||Pliocene|||||||
14873|Parilla Sand|43655|5|Briefly described|p40-846|||||||||
14873|Parilla Sand|43669|4|Described|p22-23|||||||||
14873|Parilla Sand|43846|5|Briefly described|14||Miocene|||||||
14873|Parilla Sand|44133|5|Briefly described|p161|Late Pliocene|Late Pliocene|Geological Province: Murray Basin. Overlies Loxton Sand.||||||
14873|Parilla Sand|44186|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
14873|Parilla Sand|44188|5|Briefly described|Map Legend|Pleistocene|Pliocene|Geological province: Murray Basin. Poorly consolidated to consolidated, poorly sorted, mediuym- to coarse-grained quartz and sandstone.||||||15-MAY-08
14873|Parilla Sand|44931|5|Briefly described|Map Legend|Tertiary|Tertiary|Littoral sand deposits.||||||14-JUN-06
14873|Parilla Sand|46839|6|Mentioned|p82|||||||||
14873|Parilla Sand|46909|6|Mentioned|p83|||See also Fig.1||||||
14873|Parilla Sand|49038|5|Briefly described|p26|||See also P40||||||
14873|Parilla Sand|49040|6|Mentioned|p12|||||||||
14873|Parilla Sand|50154|1|Redefined|p42, p133, p136-137|Early Pliocene|Late Miocene|Overlies the Renmark Group, Murray Group, Bookpurnong beds and the Grampians Group. Overlain by Lowan Sand. Synonymous with the Diapur Sandstone. Geological Province: Murray Basin. Thickness: 40-150m. In part correlative with the Bookpurnong beds.||||||10-NOV-10
14873|Parilla Sand|50155|5|Briefly described|Map Legend|Pliocene|Miocene|Sand, silt, commonly forms strand lines||||||
14873|Parilla Sand|50156|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50157|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies Duddo Limestone. Overlain by Lowan Sand. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50158|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50159|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50160|5|Briefly described|Map Legend|Pliocene|Miocene|||||||
14873|Parilla Sand|50161|5|Briefly described|Map Legend|Pliocene|Miocene|Marine: sand, silt; commonly forms strand lines||||||
14873|Parilla Sand|50162|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies Duddo Limestone, Marn Mering Granodiorite, Schofield Granite, Kout Norien Granodiorite, Tuloona Granodiorite and Glenelg Metamorphic Complex. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50163|5|Briefly described|Map Legend|Pliocene|Miocene|Overlain by Lowan Sand. Overlies Duddo Formation. Marine: sand, silt; commonly forms strand lines||||||25-JUN-04
14873|Parilla Sand|50164|5|Briefly described|Map Legend|Pliocene|Miocene|Sand, silt, commonly forms strand lines.||||||
14873|Parilla Sand|60451|5|Briefly described|p30, 95 Fig. 61, 99|Early Pliocene|Late Miocene|Type section in text. Maximum Thickness: 25m+. Overlies: White Hills Gravel, conformably overlies Calivil Formation.||||||
14873|Parilla Sand|60452|4|Described|p37|Early Pliocene|Late Miocene|First named Loxton Sand; upper part then named Parilla Sand (also Diapur Sand). Also termed Loxton-Parilla Sand (Vic-SA). Divided into Kerang Sand, Tragowel and Wandella Sand Members by Macumber (1983). Disconformably overlain by Shepparton Formation.||||||
14873|Parilla Sand|60454|5|Briefly described|Map Legend|Neogene|Neogene|Unit does not appear on this map.||||||
14873|Parilla Sand|60456|5|Briefly described|Map Legend|Neogene|Neogene|Unit does not appear on this map.||||||
14873|Parilla Sand|60457|5|Briefly described|Map Legend|Neogene|Neogene|Littoral deposits; well sorted, fine to medium grained quartz sandstone; well bedded; abundant lag horizons containing shelly fossils, pebble beds, rounded ironstone fragments.||||||
14873|Parilla Sand|60458|5|Briefly described|Map Legend|Neogene|Neogene|Littoral deposits: well sorted, fine to medium grained quartz sandstone; well bedded; abundant lag horizons.||||||
14873|Parilla Sand|60461|5|Briefly described|Map legend|Pliocene|Miocene|Littoral to near shore marine deposits. Clay, silt, fine to coarse-grained quartz sand, minor quartz gravel, minor heavy mineral sands with disseminated zircon, tourmaline, ilmenite & rutile; commonly ferruginised; sorting good to moderate, cross-bedded.||||||06-OCT-04
14873|Parilla Sand|60462|5|Briefly described|Map Legend|Neogene|Neogene|Marginal marine sand, lesser silt and gravel; swales rarely weakly magnetic (to 2 nT); thorium high where outcropping.||||||15-SEP-04
14873|Parilla Sand|60491|4|Described|p16, p21-22|Pliocene|Late Miocene|Interfingers with the Calivil Formation. Disconformably overlies the Renmark Group sediments. Disconformably overlain by the Shepparton Formation. Max. thickness: 100m. Geological Province: Murray Basin.||||||
14873|Parilla Sand|60492|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group. Overlain by the Shepparton Formation. Paralic to marginal marine: moderately sorted sandstone and unconsolidated sand; ferruginised in part; fossiliferous; dunes highlighted.||||||
14873|Parilla Sand|60493|5|Briefly described|Map Legend|Neogene|Paleogene|Marginal marine strand deposits: linear N-S magnetic features up to about 5 nT; interdunes have slightly higher K, Th, U responses.||||||07-NOV-08
14873|Parilla Sand|60540|5|Briefly described|p999,p1000 Fig.2, p1002|Pliocene|Pliocene|||||Lateral equivalent to Moorna Formation and upper Norwest Bend Formation.|Aeolian and terrestrial sediments.|06-FEB-18
14873|Parilla Sand|60543|5|Briefly described|Map legend|Tertiary|Tertiary|||||||23-DEC-09
14873|Parilla Sand|60591|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60592|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60593|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60595|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60596|5|Briefly described|Map Legend|Pliocene|Miocene|Overlies the Renmark Group and Calivil Formation. Quartz pebbles, quartz sandstone, minor clay and silt; poor- to moderate-sorting and rounding, open framework, weakly cemented; minor burrows.||||||20-JAN-05
14873|Parilla Sand|60597|5|Briefly described|Map Legend|Pliocene|Miocene|Paralic to fluvial deposits: nonmagnetic.||||||
14873|Parilla Sand|60599|5|Briefly described|p7, p15, p80||Early Pliocene|Shallow marine and littoral deposits that interfinger with Calivil Formation; unconformably overlies Wild Duck Formation. Geological Province: Murray Basin.||||||
14873|Parilla Sand|60953|5|Briefly described|Map Legend|Pliocene|Pliocene|Fluviolacustrine and coastal aeolian, siliceous and clayey sand.||||||
14873|Parilla Sand|61108|5|Briefly described|map legend|Pliocene|Pliocene|Fluviolacustrine and coastal aeolian, siliceous and clayey sand.||||||
14873|Parilla Sand|61155|5|Briefly described|p5, p6|Pliocene|Pliocene|Fluvial clastic deposits. Geological Province:Murray Basin.||||||
14873|Parilla Sand|61180|5|Briefly described|p7|Pliocene|Late Miocene|Consists of well-sorted silt and fine-to coarse-grained quartz sand, with rare gravel.||||||
14873|Parilla Sand|61181|6|Mentioned|p28, p137|Pliocene|Miocene|See also Parilla Sands. See also p153 Fig. 47.||||||
14873|Parilla Sand|61183|4|Described|p18 Fig. 9, p67|Tertiary|Tertiary|Widespread quartz and carbonate sand. Includes subsurface occurrences of fossiliferous marine sandstone. See also p19, p129.||||||
14873|Parilla Sand|61185|5|Briefly described|p58, p15, p63|Pliocene|Late Miocene|Interfingers with and conformably underlies Calivil Formation. Geological Province: Murray Basin. Shallow marine and littoral. Interpreted as lateral equivalent of Yando Clay.||||||07-FEB-11
14873|Parilla Sand|61314|5|Briefly described|p129|Late Pliocene|Late Pliocene|Includes the Loxton Sand. Geological Province: Murray Basin.||||||
14873|Parilla Sand|61964|6|Mentioned|p139|||Regional correlative is Calivil Sand (Renmark Group). Geological Province: Murray Basin.||||||
14873|Parilla Sand|63124|6|Mentioned|p94||Pliocene|Geological Province: Gambier Basin.||||||
14873|Parilla Sand|63446|5|Briefly described|Map legend|Pliocene|Miocene||||||Marine: sand, silt.|
14873|Parilla Sand|64096|5|Briefly described|p283||Early Pliocene|Unconformably overlies Lake Boga Granite as a 1-5 m-thick layer of sandy sediment.||||||
14873|Parilla Sand|64237|5|Briefly described|p17, p18 Fig. 2, p19 Fig. 2b|Late Pliocene|Pliocene|Part of original stratigraphic scheme (Ludbrook 1961) tog. with Norwest Bend Fm and Loxton Sand.............Original configuration for this trio - Norwest Bend Fm/Parilla Sand/Loxton Sand was retained in the stratigraphic revision by Rogers et al (1998).||||||29-JUL-08
14873|Parilla Sand|65194|6|Mentioned|p25-27|||Forms an aquifer at Lake Tyrrell.||||||
14873|Parilla Sand|65552|5|Briefly described|p5 Fig. 3|Late Pliocene|Late Pliocene|Only differentiated in western Murray Basin. Elsewhere part of 'Loxton-Parilla Sands'. Where differentiated overlies Loxton Sands, underlies Blanchetown Clay.||||||
14873|Parilla Sand|65715|5|Briefly described|p15 Tb.8|||Possibly junior synonym of Loxton Sand in Victoria [probably still current in SA].||||||
14873|Parilla Sand|65719|5|Briefly described|p7|Miocene|Miocene|In Murray Basin. Lateral equivalent of Mystic Park Formation. Marginal marine or paralic. Late Miocene.||||||10-MAY-12
14873|Parilla Sand|65969|5|Briefly described|p3, p27 Tb.3.3, p30-1|Pliocene|Pliocene|Murray Basin. Equivalent to Shepparton Formation. Marginal marine to paralic sand. Relics of sand sheets on the sides of valleys. No magnetic response; high Th radiometric response where subsequently lateritised, elsewhere low in all channels.||||||
14873|Parilla Sand|66002|5|Briefly described|p13 Tb.9, p18-19|||Of Firman 1965. Aeolian. Difficult to distinguish from underlying marine Loxton Sand. Forms ridges and swales with an east-west pattern||||||
14873|Parilla Sand|66286|6|Mentioned|p181.|Pliocene|Miocene|Deposited during regression of a marine incursion into western Murray Basin. Its aeolian and associated sediments are correlated with the oyster-rich, upper of two informal members of the Norwest Bend Formation.||||||
14873|Parilla Sand|66287|6|Mentioned|p26, 33|Neogene|Neogene|Of Firman 1966 and 1973. Previous name for (minor) non-marine part of the Loxton-Parilla Sands.||||||20-APR-12
14873|Parilla Sand|67127|6|Mentioned|p73|||||||Overlies the Geera Clay.||
14873|Parilla Sand|67347|6|Mentioned|p836, 843|Early Pliocene|Early Pliocene|Generally saline aquifer.||||Underlain by the Lake Boga Granite.||11-MAY-12
14873|Parilla Sand|67462|5|Briefly described|Map legend.|Pliocene|Pliocene|Murray Basin.||||||
14873|Parilla Sand|68189|5|Briefly described|p4, p6 Fig.1, p19 Fig.8, pp25-32|Miocene|Miocene|Littoral to near-shore marine sequence which regresses to the west. Dominant near-surface unit where the Murray Basin is present in ST ARNAUD.|< 6 Ma|||Disconformably underlain by the Olney Formation. Conformably overlain and interfingered by the Shepparton Formation. Overlain by the Geera Clay. Underlain by the Winnambool Formation.|Comprises sand (often cross bedded).|
14873|Parilla Sand|68194|5|Briefly described|p6, p9, p11, p17, p20-21, p23-31, p34-36|Pliocene|Pliocene|See also p40, p43 Fig.42, p44, p55-57, p73-74. Blackburn (1962). Strandlines form ridged marine plains. Also appears as Parilla Sand Formation on p9 and p11. Called Loxton Sand in SA. Regolith and remote sensing profiles described.||Unit in Wunghnu Group.||Disconformably overlies Geera Clay. Is overlain disconformably by Shepparton Formation. Lateral facies equivalent of Bookpurnong beds.|Variably-sorted, fine- to very coarse-grained, subangular to subrounded quartz sandstone.|
14873|Parilla Sand|68548|5|Briefly described|p13|Pliocene|Pliocene|Late Pliocene age.||||Laterally equivalent to the Norwest Bend Formation and the Moorna Formation.|Comprises aeolian and associated terrestrial sediments.|
14873|Parilla Sand|68715|5|Briefly described|p31 Fig.5|Pliocene|Miocene|Murray Basin. Late Miocene maximum age.||Of the Murray Group.||||
14873|Parilla Sand|70718|5|Briefly described|p23|||Parilla Sands used p104.||||Equivalent to Shepparton Fomation?||30-MAY-19
14873|Parilla Sand|70961|14|Not recorded|p138|||Refers to Firman (1966).||||||
14873|Parilla Sand|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Pliocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as overlying Loxton Sands and equivalent to Norwest Bend Formation and underlying Blanchetown Clay.|Shown as including sand.|
14873|Parilla Sand|73188|5|Briefly described|p314, p320|Pliocene|Pliocene|Murray Basin.|||||Shallow marine calcareous sand, fluvial and coastal barrier sands.|
14873|Parilla Sand|73228|4|Described|p51, p58|||Derived mainly from Loxton Sand by aeolian and fluvial reworking and may include large transgressive dune complexes, as well as lacustrine and fluvial deposits laid down in depressions between stranded coastal ridges.||||Underlain by Loxton Sand.|Unfossiliferous, nonmarine, fine- to medium-grained clayey quartz sand with thin beds of sandy clay.|
14873|Parilla Sand|73496|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Magnetic interdunes several km long parallel arcuate magnetic high (about 10 nT) trending north to corthwest and concave west; where not covered or eroded, interdune topographic lows are radiometric highs.|
14873|Parilla Sand|73497|5|Briefly described|Map legend|Pliocene|Miocene|||Wunghnu Group|||Gravel, sand and silt: no distinctive magnetic responses, low K, Th and variable U.|
14873|Parilla Sand|73505|4|Described|p1-2, p4, p11-14, p23, p36, p38|Pliocene|Late Miocene|Murray Basin. Host to heavy mineral sands. Topography of upper surface is broad convex-west arcuate ridges, eroded away in places. Minor magnetic highs correlate with topographic lows. Th high where lateratised or mineralised.||Wunghnu Group||Overlies Bookpurnong beds, Calivil Formation, 'Middle Renmark Group', underlies Blanchetown Clay, sequence/time equivalent of Shepparton Formation and Bookpurnong beds|Marginal marine sand dunes.|
14913|Parrabel beds|22736|6|Mentioned|p611 Fig2||Permian|||||||
14913|Parrabel beds|22857|5|Briefly described|p516 App.1 Tb.A1.8|Early Permian||Diamictite, paraconglomerate, lithic sandstone, limestone; minor vitric tuff. Max. thickness: >1220m.||||||
14913|Parrabel beds|23720|5|Briefly described|Map Legend|||Of Nambucca beds.   Diamictite, lithic sandstone, siltstone, minor limestone,  metabasalt.||||||15-DEC-04
14913|Parrabel beds|41347|4|Described|Table 7|||||||||
14913|Parrabel beds|41348|5|Briefly described|Map legend|Permian|Permian|Diamictite, paraconglomerate, conglomerate, lithic sandstoen, mudstone, limestone, and minor vitric tuff.||||||16-DEC-04
14913|Parrabel beds|43755|6|Mentioned|Fig.1,p548||Permian|||||||
14913|Parrabel beds|44093|5|Briefly described|p67 Fig 6.6|Permian|Permian|See also p232 Appendix 1. Geological Province: New England Fold Belt.||||||
14913|Parrabel beds|44450|3|Fully described|p22 Table 4|Early Permian|Early Permian|Of Nambucca beds. Geological Province: Nambucca Block.||||||
14913|Parrabel beds|61771|5|Briefly described|p116|||See also Parrabel Beds. Geological Province: Northern Hastings Terrane.||||||
14913|Parrabel beds|61772|6|Mentioned|p128 Fig. 2||Early Permian|In New England Orogen.||||||24-SEP-08
14913|Parrabel beds|65317|6|Mentioned|p635, p634 Fig.13|||||||||
14913|Parrabel beds|70939|6|Mentioned|p826, p828|Permian|Permian|Northern Hastings Block.||||||
14913|Parrabel beds|71628|5|Briefly described|p17: 20, 95|||Nambucca Block.||||Is intruded by Carrai Granodiorite and Fife Monzogranite.||
14916|Parry Group|721|5|Briefly described|Map legend|Early Carboniferous|Late Devonian|||||||
14916|Parry Group|22768|6|Mentioned|p182|||||||||
14916|Parry Group|22857|5|Briefly described|p219, p498 App.1 Tb.A1.7|Early Carboniferous|Late Devonian|Geological Province: Tamworth Forearc Basin.||||||
14916|Parry Group|22859|5|Briefly described|p219|Early Carboniferous|Late Devonian|||||||
14916|Parry Group|23050|5|Briefly described|p9 Fig.2, p31|Devonian|Devonian|||||||
14916|Parry Group|23051|5|Briefly described|Map Legend|||Of Tamworth Belt.||||||04-JUN-07
14916|Parry Group|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt||||||
14916|Parry Group|24366|5|Briefly described|p17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
14916|Parry Group|33020|6|Mentioned|p231|||Refers Crook (1964). Tournaisian. Statistical anal.||||||
14916|Parry Group|34555|6|Mentioned|Table 4.2|||||||||
14916|Parry Group|38686|5|Briefly described|p56|Carboniferous|Carboniferous|Geological Province: New England Fold Belt||||||
14916|Parry Group|39214|6|Mentioned|p33|||||||||
14916|Parry Group|39331|6|Mentioned|p101|||See also Fig.10-1||||||
14916|Parry Group|41009|6|Mentioned|Fig.2|||||||||
14916|Parry Group|41238|4|Described|p82|||||||||
14916|Parry Group|41347|4|Described|Table 3|||Mention p357.||||||04-JUN-07
14916|Parry Group|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Includes: Namoi Fm., Tulcumba Sst., Tangaratta Fm., Mandowa Mudstone, Keepit Conglomerate, Goonoo Goonoo Mdst. and Baldwin Fm.  Mudstone, minor lithic and feldspathic sandstone, conglomerate, oolitic and crinoidal limestone, with andesitic? sills near top||||||16-DEC-04
14916|Parry Group|41990|5|Briefly described|p5|||||||||
14916|Parry Group|42554|6|Mentioned|p38|||||||||
14916|Parry Group|43091|5|Briefly described|Map legend|||||||||
14916|Parry Group|43399|2|Defined|p190,196,197,204-6|Early Carboniferous|Late Devonian|= Manilla Group and Lower Burrindi Group.||||||04-JUN-07
14916|Parry Group|43400|14|Not recorded|p176,178,map|Early Carboniferous|Late Devonian|||||||
14916|Parry Group|43406|14|Not recorded|p41-43,45,49|Tournaisian|Late Devonian|(L.Carb)||||||
14916|Parry Group|43418|14|Not recorded|Map Legend|||||||||
14916|Parry Group|43446|14|Not recorded|p6041,6049|||||||||
14916|Parry Group|43582|5|Briefly described|fig.2,p7||Early Carboniferous|||||||
14916|Parry Group|43860|5|Briefly described|7||Late Devonian|||||||
14916|Parry Group|43874|14|Not recorded|p204|||(H/56-13) no age given||||||
14916|Parry Group|44093|5|Briefly described|p227 App. 1|Early Carboniferous|Late Devonian|Geological Province: New England Fold Belt.||||||
14916|Parry Group|48600|14|Not recorded|Plate 3|||||||||
14916|Parry Group|50629|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Includes: Mostyn Vale Formation.  Geological Province: New England Orogen.||||||
14916|Parry Group|61392|5|Briefly described|p165 Fig. 2|Carboniferous|Givetian|In the Gamilaroi terrane.||||||07-FEB-11
14916|Parry Group|61761|6|Mentioned|p6|||||||||07-FEB-11
14916|Parry Group|62095|5|Briefly described|Plate 1|Devonian|Devonian|Geological Province: Rouchel Block/Tamworth Belt.||||||29-MAY-06
14916|Parry Group|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Devonian|Unconformably overlain by Derra Derra and Bingara Volcanics. Geological Province: Tamworth Belt.||||||10-DEC-07
14916|Parry Group|65398|6|Mentioned|p4 Fig.2, p6 Fig.3|Early Carboniferous|Late Devonian|||||||
14916|Parry Group|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous||||Includes Baldwin, Mostyn Vale and Namoi Formations; Keepit Conglomerate; Mandowa Mudstone; Tulcumba Sandstone.|Overlies Tamworth Group.||
14916|Parry Group|68003|5|Briefly described|pp138-139.|Devonian|Carboniferous|Tamworth Belt (North), New England Fold Belt.|||Includes Namoi, Luton, Mostyn Vale, Tangaratta, Lowana Formations; Tulcumba Sandstone; Rangari, Kiah  Limestones; Mandowa Mudstone; Keepit Conglomerate; Noumea beds.|||
14916|Parry Group|68005|5|Briefly described|p20, p47, pp54-56, pp146-150, p169.|Early Carboniferous|Late Devonian|Tamworth Belt, New England Fold Belt. Marine; intermediate to felsic rocks.|||Includes Noumea beds; Mostyn Vale, Lowana, Tangaratta, Luton and Namoi Formations; Eungai and Mandowa Mudstones; Keepit Conglomerate and Tulcumba Sandstone.|Overlies Tamworth Group.||
14916|Parry Group|68006|6|Mentioned|p20 Fig.3-A, p27, p115.|Early Carboniferous|Late Devonian|Tamworth Belt, New England Fold Belt. Contains extensive but thin and impure beds of limestone.||||||
14916|Parry Group|70217|5|Briefly described|p11, p22|Carboniferous|Carboniferous|New England Orogen.||||Is intruded by the Barrington Tops Granodiorite.||
14916|Parry Group|70777|6|Mentioned|p8|Devonian|Devonian|Rouchel Block, New England Orogen.||||||
14916|Parry Group|71628|5|Briefly described|p6:18; p18-20||||||Namoi, Tangaratta, Baldwin Formations; Tulcumba Sandstone; Mandowa, Goonoo Goonoo Mudstones; Keepit Conglomerate.|Is intruded by Gummi Plain and Mount Ephraim Granodiorites.||
14945|Paterson Volcanics|22736|6|Mentioned|p629|Namurian|Visean|||||||
14945|Paterson Volcanics|22857|4|Described|p506 App.1 Tb.A1.8|Visean|Visean|Age: 328.5+/-1.4Ma (SHRIMP U/Pb (Claoue-Long, Compstone et al, 1995) and 329.3+/-3.8Ma (U/Pb SHRIMP). Max. thickness: 150m. Geological Province: Kullatine-Yagon-Booral Shelf. See also p231 and p241.||||||
14945|Paterson Volcanics|22863|6|Mentioned|p231,241||Visean|Max Age: 328 (+/-) 1.4 Ma.||||||
14945|Paterson Volcanics|24121|5|Briefly described|p4, p65, p90|Permian|Permian|||||||25-AUG-22
14945|Paterson Volcanics|24603|5|Briefly described|p897 Fig. 17|Carboniferous|Carboniferous|Age: 328.5+/-1.4Ma (Claoue-Long et al, 1995).  Geological Province: Tamworth Belt.  In the Gresford Block.||||||
14945|Paterson Volcanics|29915|6|Mentioned|p62|||||||||
14945|Paterson Volcanics|31228|3|Fully described|p84|||||||||
14945|Paterson Volcanics|32378|6|Mentioned|p113|||||||||
14945|Paterson Volcanics|32379|6|Mentioned|p5|||||||||
14945|Paterson Volcanics|32868|6|Mentioned|p209|||||||||
14945|Paterson Volcanics|34072|6|Mentioned|Fig.4.5|||Carb.||||||
14945|Paterson Volcanics|34085|6|Mentioned|Cor.chart|||Stephanian||||||
14945|Paterson Volcanics|34238|6|Mentioned|p11|||||||||
14945|Paterson Volcanics|34444|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
14945|Paterson Volcanics|36042|6|Mentioned|Table 1|||||||||
14945|Paterson Volcanics|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
14945|Paterson Volcanics|36528|6|Mentioned|p169|||See also P182.||||||
14945|Paterson Volcanics|37922|5|Briefly described|p481|||||||||
14945|Paterson Volcanics|37926|6|Mentioned|p499|||||||||
14945|Paterson Volcanics|38801|6|Mentioned|Fig.3|||||||||
14945|Paterson Volcanics|39287|6|Mentioned|Fig. 2.5|||||||||
14945|Paterson Volcanics|39292|6|Mentioned|Fig. 6.1|||||||||
14945|Paterson Volcanics|39299|6|Mentioned|p282|||||||||
14945|Paterson Volcanics|39306|6|Mentioned|p391|||||||||
14945|Paterson Volcanics|42214|4|Described|p466|||||||||
14945|Paterson Volcanics|42547|4|Described|p12, p31, p32|||305my||||||
14945|Paterson Volcanics|42780|5|Briefly described|Fig.2 P412|||||||||
14945|Paterson Volcanics|43079|5|Briefly described|p74|||||||||
14945|Paterson Volcanics|43383|14|Not recorded|p18|||||||||
14945|Paterson Volcanics|43437|14|Not recorded|p169-175||Carboniferous|||||||
14945|Paterson Volcanics|43440|14|Not recorded|p37,66,68,76|||||||||
14945|Paterson Volcanics|43451|14|Not recorded|Map Legend||Carboniferous|||||||
14945|Paterson Volcanics|43479|14|Not recorded|p177||Westphalian|||||||
14945|Paterson Volcanics|43576|6|Mentioned|Fig.1,p348||Late Carboniferous|||||||
14945|Paterson Volcanics|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
14945|Paterson Volcanics|44093|5|Briefly described|p228 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: New England Fold Belt.||||||
14945|Paterson Volcanics|44244|2|Defined|p99-102|Carboniferous|Carboniferous|Underlies Seaham Formation.  Age: 308Ma.  Type section in text.  Geological Province: Gresford Block.||||||25-AUG-04
14945|Paterson Volcanics|44254|14|Not recorded|p76,77,83||Late Carboniferous|Equivalent to Paterson Toscanite and in part to Italia Road Formation.||||||
14945|Paterson Volcanics|44833|14|Not recorded|p108|||||||||
14945|Paterson Volcanics|45097|6|Mentioned|Fig.|||Correlation chart. Refers Helby & Morris.||||||
14945|Paterson Volcanics|46849|6|Mentioned|Fig. 2|||||||||
14945|Paterson Volcanics|47056|6|Mentioned|Fig.2 P523|||||||||
14945|Paterson Volcanics|50268|5|Briefly described|Map Legend|Stephanian|Westphalian|Overlies: Mount Johnstone Formation.  Underlies: Seaham Formation.  Geological Province: Rouchel and Gresford Blocks.||||||21-MAY-04
14945|Paterson Volcanics|60281|6|Mentioned|p53 App. 1|||Geological Province: New England Fold Belt.||||||
14945|Paterson Volcanics|60290|5|Briefly described|p16 Fig.1|||Overlain by Seaham Formation. Geological Province: Cranky Corner Basin.||||||07-FEB-11
14945|Paterson Volcanics|60299|5|Briefly described|p212 Fig.2c|Carboniferous|Carboniferous|Age: 328 Ma (U-Pb zircon, Roberts et al., 1995). Geological Province: Gresford Block.||||||
14945|Paterson Volcanics|61768|5|Briefly described|p81, p82, p83 Fig. 2, p86||Visean|Underlain by Mount Johnstone Formation, unconformably overlain by Seaham Formation. Age: 308Ma (K-Ar) and refined SHRIMP zircon age +328.5+/-1.4Ma. Rhyodacitic in composition.||||||
14945|Paterson Volcanics|63832|5|Briefly described|p131 fig 2|Visean|Visean|Rouchel Block and Cranky Corner/Gresford Block, Southern New England Fold Belt.|||||Largely fluvial conglomerates (towards the base); includes an interval of outsize clast-bearing, rhythmically laminated mudrocks. Upper part (C4) has 30 m interval of rhythmically laminated mudrocks overlain by a similar interval of diamictites.|13-DEC-17
14945|Paterson Volcanics|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, Rouchel Block and Cranky Corner/Gresford Block. Includes radiometric age control within unit.||||Overlies Mount Johnstone Formation.||
14945|Paterson Volcanics|65107|5|Briefly described|p276,282, Fig 4 p279, Fig 11 p286-7|Serpukhovian|Visean|Defines the age of the Gresford Block, 328.5+/-1.4 Ma. Provides segments that agree with east to west pole path (for the Gresford block) for the New England Orogen.||||||24-NOV-09
14945|Paterson Volcanics|69297|6|Mentioned|p501|Serpukhovian|Serpukhovian|Sydney Basin.|328 Ma|||Unconformably overlies the Mount Johnson Formation. Unconformably overlain by the Seaham Formation.||
14945|Paterson Volcanics|69635|5|Briefly described|p189, 193|Late Carboniferous|Late Carboniferous||308+/-4 Ma, 307+/-4 Ma (K-Ar)|||Correlated with the Pokolbin Hills Volcanics.|Ignimbrite flows, dacite and associated sedimentary rocks.|
14945|Paterson Volcanics|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.||||||
14945|Paterson Volcanics|71233|5|Briefly described|p105|Carboniferous|Carboniferous|||||Correlated with the top of Italia Road Formation.||
14945|Paterson Volcanics|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen.||||||
14945|Paterson Volcanics|73487|6|Mentioned|p566, p578|Serpukhovian|Visean|Rouchel and Gresford blocks. Marginirugus barringtonensis|ca 328 Ma|||||
14958|Paxton Formation|22601|6|Mentioned|410|Permian|Permian|Geol province Sydney Basin. Overlying unit Branxton Formation||||||
14958|Paxton Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 42m||||||
14958|Paxton Formation|22969|4|Described|Fig 4.1a||Early Permian|||||||
14958|Paxton Formation|23540|5|Briefly described|p 419-420|||Of Greta Coal Measures.||||||20-FEB-07
14958|Paxton Formation|33867|6|Mentioned|p6|||||||||
14958|Paxton Formation|34015|4|Described|p327|||Permian||||||
14958|Paxton Formation|34345|6|Mentioned|p330|||In Cessnock area.||||||
14958|Paxton Formation|37086|6|Mentioned|p185|||||||||
14958|Paxton Formation|40396|6|Mentioned|p13|||||||||
14958|Paxton Formation|45090|5|Briefly described|p152|||||||||
14958|Paxton Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
14958|Paxton Formation|69683|6|Mentioned|p411 Fig.2|Middle Permian|Middle Permian|Hunter Coalfield; Lochinvar area.||Unit in Greta Coal Measures.|Includes Bellbird Lens.|||
14964|Peachvale Rhyolite|22857|5|Briefly described|p492 App.1 Tb.A1.7|Devonian|Devonian|Of the Hyandra Creek Group. Rhyolite breccia, rhyolite, minor spilite. Max. thickness: 600m.||||||
14964|Peachvale Rhyolite|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Hyandra Creek Group.||||||
14964|Peachvale Rhyolite|23170|2|Defined|p206|Early Devonian|Early Devonian|of Hyandra Creek Group.||||||
14964|Peachvale Rhyolite|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
14964|Peachvale Rhyolite|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
14964|Peachvale Rhyolite|68003|5|Briefly described|p24 Fig.3-e, p143. |Lochkovian|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Hyandra Group.|||Rhyolite breccia, rhyolite, minor trachylatite, minor lithic sandstone.|
14980|Peats Ridge basalt|35758|6|Mentioned|Fig.2|||Demagnetisation curves.||||||
14980|Peats Ridge basalt|40263|6|Mentioned|Table 2|||||||||
14998|Pebbley Beach Formation|22591|5|Briefly described|p 64||Early Permian|||||||
14998|Pebbley Beach Formation|22970|5|Briefly described|Plate 6|Early Permian||||||||
14998|Pebbley Beach Formation|24079|5|Briefly described|p432|Permian|Permian|Of Conjola Subgroup.  Geological Province: Sydney Basin.||||||
14998|Pebbley Beach Formation|24552|4|Described|p5 Fig.2|Artinskian|Sakmarian|Overlies Wasp Head Fm, conformably overlain by Snapper Point Fm. Laminated or thin bedded mudstone to fine sandstone, interbedded hummocky cross-stratified + bioturbated sandstone, + conglomerate. Glendonites and dropstones indicate cold climate.||||||07-FEB-11
14998|Pebbley Beach Formation|29750|6|Mentioned|p1|||||||||
14998|Pebbley Beach Formation|29752|3|Fully described|p25|||||||||
14998|Pebbley Beach Formation|31081|2|Defined|p59|early Artinskian|late Sakmarian|See also P60-62. ?Late Sakmarian to Early Artinskian.||||||
14998|Pebbley Beach Formation|31128|6|Mentioned|p5|||||||||
14998|Pebbley Beach Formation|31298|6|Mentioned|p16|||||||||
14998|Pebbley Beach Formation|32084|6|Mentioned|p467|||||||||
14998|Pebbley Beach Formation|32945|6|Mentioned|p84|||Permian. See also P88. Conjola Sub-Gp.||||||
14998|Pebbley Beach Formation|35862|6|Mentioned|p276|||||||||
14998|Pebbley Beach Formation|36042|6|Mentioned|Table 1|||||||||
14998|Pebbley Beach Formation|37082|6|Mentioned|p161|||||||||
14998|Pebbley Beach Formation|37092|6|Mentioned|Table 2|||||||||
14998|Pebbley Beach Formation|37924|6|Mentioned|Fig.2|||||||||
14998|Pebbley Beach Formation|39287|6|Mentioned|p20|||||||||
14998|Pebbley Beach Formation|39289|6|Mentioned|p77|||||||||
14998|Pebbley Beach Formation|39290|6|Mentioned|p88|||Isopach map Fig. 5.10||||||
14998|Pebbley Beach Formation|39305|5|Briefly described|p378|||Fossil occurrences||||||
14998|Pebbley Beach Formation|39306|6|Mentioned|p398|||||||||
14998|Pebbley Beach Formation|39307|6|Mentioned|Table 22.1|||||||||
14998|Pebbley Beach Formation|39308|4|Described|p534|||||||||
14998|Pebbley Beach Formation|40166|6|Mentioned|Table 1|||||||||
14998|Pebbley Beach Formation|42925|5|Briefly described|Table 18||Early Permian|||||||
14998|Pebbley Beach Formation|42974|6|Mentioned|Fig.2,p192|||of Shoalhaven Group||||||
14998|Pebbley Beach Formation|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Of Conjola Subgroup, Shoalhaven Group, Southern Sydney Basin. Deposited during a marine transgression during the Early Permian.||||||
14998|Pebbley Beach Formation|45090|5|Briefly described|p7|||Correlation chart. Isopach map P34.||||||17-MAR-09
14998|Pebbley Beach Formation|49644|5|Briefly described|Table|||||||||
14998|Pebbley Beach Formation|60281|5|Briefly described|p57|Early Permian|Early Permian|Of the Shoalhaven Group. Dominated by siltstone, with minor sandstone, conglomerate and coal; channelling and cross-bedding are evident.  Unconformably overlies the Wasp Head Formation near Batemans Bay.  Geological Province: Sydney Basin.||||||17-MAR-05
14998|Pebbley Beach Formation|60285|3|Fully described|p179-182|Sakmarian|Sakmarian|Basal unit of Shoalhaven Group. Overlies Wasp Head Formation. Overlain by Snapper Point Formation. Weakly to intensley bioturbated sandstone to siltstone, minor claystone. Marine and estuarine, with nine facies defined. Trace fossils descibed in detail.||||||
14998|Pebbley Beach Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Upper part correlated with Billy Brook Formation, Rutherford Formation, Faulkner Group and Liffey Group. Lower part correlated with Cranky Corner Sandstone, Allandale Formation, Bundella Formaiton, Callytharra Formation and Golden Valley Group.||||||
14998|Pebbley Beach Formation|61315|5|Briefly described|Table SY2|Early Permian|Early Permian|Of the Conjola Subgroup (Shoalhaven Group). Geological Province: Sydney Basin||||||
14998|Pebbley Beach Formation|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Conjola Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
14998|Pebbley Beach Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||12-MAR-09
14998|Pebbley Beach Formation|62043|5|Briefly described|pp435-461.|Artinskian|Sakmarian|Southern Sydney Basin. Preserves a shallow marine record of one glacial interval, and its immediate postglacial period, of the Late Permian Gondwanan Ice Age. Lateral equivalent of the Yadboro Conglomerate and Yarrunga Coal Measures. The article subdivides the upper part of this unit into nine discrete sequences and provides a detailed facies analysis of each.||Unit in Shoalhaven Group.||Is overlain by Snapper Point Formation.|Sandstone, siltstone; lesser mudstone.|
14998|Pebbley Beach Formation|63713|6|Mentioned|p1531|Permian|Permian|Sydney Basin. Early Permian. Near-shore marine strata from the Late Paleozoic Ice Age.||||||
14998|Pebbley Beach Formation|63773|5|Briefly described|p1058 Fig. 2, p1069|Early Permian|Early Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-APR-09
14998|Pebbley Beach Formation|63832|4|Described|p131 fig 2, p136-137|Kungurian|Sakmarian|Gostin and Herbert (1973). Southern Sydney Basin. Base of this unit marks the onset of the sixth (P2) glaciation. Indicates large-scale relative sea-level changes. Described and implications discussed in detail.||Unit in Shoalhaven Group.||Overlies Wasp Head Formation. Is overlain by Snapper Point Formation.|Lower part consists of 22 cycles (cyclothems) of diamictite and dark grey marine mudrock with a hiatal surface between each facies. Overlain by mudrocks and sandstones, then marine strata incised by estuarine channel fills.|13-DEC-17
14998|Pebbley Beach Formation|64631|4|Described|p44 Fig.2, pp48-50, pp52-55.|Artinskian|Sakmarian|SE Sydney Basin. Type section at Pebbley Beach. Predominantly glaciomarine facies in lower portion. c.75 m thick. Contains rich marine invertebrate fossil record providing biostratigraphic age control at base and top. Top shown as time transgressive.||Unit in Shoalhaven Group.||Overlies Wasp Head Formation. Is overlain by Snapper Point Formation.|Cycles of strata comprising diamictite with abundant tree trunks, overlain by laminated and bioturbated mudrocks and siltstones. Dropstones are common.|
14998|Pebbley Beach Formation|64877|5|Briefly described|p293, p295-296, p305, p315|Permian|Permian|Southern Sydney Basin. Shallow-marine and associated coastal-plain deposits under icehouse conditions. Trace fossils illustrated.||Shoalhaven Group.||||
14998|Pebbley Beach Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Overlain by Snapper Point Formation.||
14998|Pebbley Beach Formation|70096|5|Briefly described|p220-221;Supp4|||Of southern Sydney Basin. Includes a horizon of glendolites in the upper part of the section. See also supplementary files in appendix for additional stratigraphic and locality information.||||Underlain by Wasp Head Formation.||
14998|Pebbley Beach Formation|71542|5|Briefly described|p25|Permian|Permian|Of southern Sydney Basin.||Unit of Shoalhaven Group.||Basal unit of Shoalhaven Group. Overlain by Snapper Point Formation. Underlain by Talaterang Group.||
14998|Pebbley Beach Formation|73304|6|Mentioned|p78|||Sydney Basin. Includes evidence of the [Permian] greenhouse crisis.||||||
14998|Pebbley Beach Formation|73421|4|Described|p1, p2 Fig.1, p3, p5, p15-17, p19-20|Artinskian|Artinskian|Sydney Basin, southern. Abbreviated to PBF in text. Deposited in an unprotected, strongly oxic coastal marine to estuarine setting. Age for PBF is older than what is indicated from the uppermost part being equated with the Rowan Formation by Metcalfe et al., (2015) and Briggs (1998). Misspelt as Pebbly p2 Fig.1, p16.||Shoalhaven Group||Overlies Wasp Head Formation, conformably underlies Snapper Point Formation|Predominantly siltstone and fine sandstone intercalated with conglomerate including glacial diamictite.|
14998|Pebbley Beach Formation|73494|5|Briefly described|p541|Permian|Permian|Southern Sydney Basin. Early Permian.||Conjola Subgroup.||Overlies Wasp Head Formation. Is overlain by Snapper Point Formation.||
15007|Peel Serpentinite|39331|6|Mentioned|Fig.10-1|||||||||
15007|Peel Serpentinite|41328|6|Mentioned|p14|||||||||
15007|Peel Serpentinite|43400|14|Not recorded|map opp.p.188||Permian|(M.Permian)||||||
15007|Peel Serpentinite|43401|4|Described|p209,210||Permian|M.Permian||||||
15011|Peelwood Porphyry|32999|3|Fully described|p29|||||||||
15012|Peelwood Shale|37727|6|Mentioned|p80|||||||||
15012|Peelwood Shale|68592|6|Mentioned|p1690|Devonian|Silurian|Name apparently replaced by Cuddyong Formation. The Peelwood copper deposit developed adjacent to the contact between this unit and the Kangaloolah Volcanics.||||||
15041|Penshurst Sandstone Member|22857|5|Briefly described|p438 App.1, Tb.A1.6|Devonian|Devonian|Of the Boothumble Formation (Cobar Supergroup). Arenite. Max. thickness: 700m. Geological Province: Mouramba Shelf.||||||
15041|Penshurst Sandstone Member|41394|2|Defined|p79|Early Devonian||Reserved as Penshurst Member||||||
15041|Penshurst Sandstone Member|41395|6|Mentioned|Map legend|Lochkovian||||||||
15042|Pentamerus Limestone|32585|6|Mentioned|p210|||Refers Etheridge (1892)||||||
15053|Peppercorn Formation|22857|4|Described|p466 App.1 Tb.A1.6|Ludlovian|Llandovery|Of the Cooleman Plains Group. Max. thickness: <1km.||||||
15053|Peppercorn Formation|23454|5|Briefly described|p28|Llandovery|Llandovery|||||||
15053|Peppercorn Formation|36441|5|Briefly described|map legend|Ludlovian|Llandoverian|Of Cooleman Plains Group. Arenite, siltstone and cleaved shale. Underlies Blue Waterhole Formation. BMR map code: Sme.||||||
15053|Peppercorn Formation|36443|5|Briefly described|map legend|Ludlovian|Llandoverian|Of Cooleman Plains Group. Basal conglomerate, overlain by arenite, siltstone and shale, with minor limestone lenses. Underlies Blue Waterhole Formation. Interfingers with Cooleman Limestone and Pocket Formation. BMR map code: Sme.||||||
15053|Peppercorn Formation|45147|2|Defined|M77|early Ludlovian|late Llandoverian|Late Llandoverian to Early ? Ludlovian||||||
15053|Peppercorn Formation|63290|5|Briefly described|p388, p394 Tb. 1, p398|Ludlow|Llandovery|Underlain unconformably by Tantangara Formation. Geological Province: Kiandra Volcanic Belt.||||||
15053|Peppercorn Formation|68592|6|Mentioned|p28, p92|Silurian|Silurian|In Tantangara and Brindabella 1:100 000 map areas. Part of a mid to late Silurian quartzose clastic and carbonate succession, which the Long Plain Fault has juxtaposed against the partly coeval Goobarragandra Volcanics.||||||
15147|Piallaway Trig Ignimbrite Member|24603|5|Briefly described|p868|Late Carboniferous|Late Carboniferous|Of the Currabubula Formation.  Relatively coarse-grained, crystal-rich, lithic, variably welded ignimbrite.  Age: 306.0+/-4.2Ma.  Geological Province: Tamworth Belt.||||||
15147|Piallaway Trig Ignimbrite Member|41800|4|Described|p496|||Reserved as Piallaway Trig Ignimbrite||||||
15147|Piallaway Trig Ignimbrite Member|42339|5|Briefly described|p55|||||||||
15147|Piallaway Trig Ignimbrite Member|42399|6|Mentioned|Fig.2 PB11|||||||||
15147|Piallaway Trig Ignimbrite Member|43718|6|Mentioned|Table 8.2,p129|||||||||
15147|Piallaway Trig Ignimbrite Member|50613|5|Briefly described|p213|||of the Currabubula Formation.||||||
15147|Piallaway Trig Ignimbrite Member|62095|5|Briefly described|p251, Plate 1|Carboniferous|Carboniferous|Of the Currabubula Formation. Geological Province: Werrie Block/Tamworth Belt.||||||
15147|Piallaway Trig Ignimbrite Member|65382|5|Briefly described|p717 App. 2|Pennsylvanian|Pennsylvanian|Near top of Currabubula Formation. Radiometric age 306.0 +/- 4.2 (Opdyke et al 2000)||||||
15147|Piallaway Trig Ignimbrite Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Ignimbrite.|
15147|Piallaway Trig Ignimbrite Member|68005|6|Mentioned|p57, p140.|Late Carboniferous|Late Carboniferous|||Unit in Currabubula Formation.||||
15178|Piercefield Coal Member|29942|4|Described|Fig.1|||Permian||||||
15178|Piercefield Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
15178|Piercefield Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
15178|Piercefield Coal Member|40805|6|Mentioned|p133|||||||||
15178|Piercefield Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Burnamwood Formation.||||
15182|Pigeon House Creek Siltstone|22591|4|Described|p 62, Fig 4||Early Permian|||||||
15182|Pigeon House Creek Siltstone|22857|4|Described|p504 App.1 Tb.A1.8|Early Permian|Early Permian|Fine-grained sandstone and carbonaceous siltstone. Max. thickness: >45m. Geological Province: Kanimblan Highlands.||||||
15182|Pigeon House Creek Siltstone|22969|4|Described|p 17||Early Permian|Talaterang Group, Sydney Basin. Overlying unit: Yadboro Conglomerate. Max. thickness: 45 m.||||||
15182|Pigeon House Creek Siltstone|29752|6|Mentioned|p9|||||||||
15182|Pigeon House Creek Siltstone|29992|6|Mentioned|Map legend|Permian|Permian|||||||
15182|Pigeon House Creek Siltstone|29994|6|Mentioned|Map legend|Permian|Permian|||||||
15182|Pigeon House Creek Siltstone|31081|4|Described|p51|||See also p52-54.||||||13-AUG-15
15182|Pigeon House Creek Siltstone|31128|6|Mentioned|p5|||Also mention Table 1.||||||
15182|Pigeon House Creek Siltstone|31277|6|Mentioned|p3|||||||||
15182|Pigeon House Creek Siltstone|31298|3|Fully described|p11|||||||||
15182|Pigeon House Creek Siltstone|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
15182|Pigeon House Creek Siltstone|32769|6|Mentioned|Fig.1|||||||||
15182|Pigeon House Creek Siltstone|32945|6|Mentioned|p84|||Shoalhaven Gp.||||||
15182|Pigeon House Creek Siltstone|34039|6|Mentioned|p355|||||||||
15182|Pigeon House Creek Siltstone|34059|6|Mentioned|Map legend|Permian|Permian|||||||
15182|Pigeon House Creek Siltstone|34211|6|Mentioned|p32|||||||||
15182|Pigeon House Creek Siltstone|34334|3|Fully described|p360|||||||||
15182|Pigeon House Creek Siltstone|35145|6|Mentioned|Fig.2|||||||||
15182|Pigeon House Creek Siltstone|36207|6|Mentioned|Text Fig.2|||||||||
15182|Pigeon House Creek Siltstone|37924|6|Mentioned|Fig.2|||||||||
15182|Pigeon House Creek Siltstone|39290|5|Briefly described|p84|||||||||
15182|Pigeon House Creek Siltstone|43465|14|Not recorded|Map Legend||Permian|||||||
15182|Pigeon House Creek Siltstone|43981|2|Defined|p3,18,36||Permian|Type Locality.||||||
15182|Pigeon House Creek Siltstone|45006|14|Not recorded|Tb.1,opp.p3|||||||||
15182|Pigeon House Creek Siltstone|45090|5|Briefly described|p140|||||||||
15182|Pigeon House Creek Siltstone|45097|6|Mentioned|Fig.|||Correlation chart. Microflora compares Seaham Fm.||||||
15182|Pigeon House Creek Siltstone|46849|6|Mentioned|p197|||||||||
15182|Pigeon House Creek Siltstone|60281|5|Briefly described|p55|Early Permian|Early Permian|Of the redefined Talaterang Group.  Disconformably overlain by Yadboro Conglomerate.  Thickness at type section: 45m.   Geological Province: Sydney Basin.||||||
15182|Pigeon House Creek Siltstone|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||17-MAR-09
15182|Pigeon House Creek Siltstone|68003|5|Briefly described|p40.|Early Permian|Early Permian|This article cites Tye et al. (1996) for including it (and, similarly, the Wasp Head Formation) in the Talaterang Group.||Unit in Talaterang Group.||||
15182|Pigeon House Creek Siltstone|70601|6|Mentioned|p28|||One of the basal formations of the Sydney Basin.||||||
15185|Pikedale beds|42559|4|Described|p9|||Stated to be informal name. Permian?||||||
15185|Pikedale beds|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic (locally pebbly) arenite, conglomerate and mudstone; rare vitric tuff.||||||11-DEC-07
15185|Pikedale beds|63748|5|Briefly described|p16, p18|Early Permian|Early Permian|Unconformably overlie Texas beds basement. Comprise lithic arenite, siltstone and mudstone, interlayered with sporadic discontinuous pebbly, conglomeratic lenses. Also mentioned: p68.||||||07-FEB-11
15185|Pikedale beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Bondonga, Silver Spur and Terrica beds, are all mapped under the symbol, Par.||||||
15185|Pikedale beds|68679|5|Briefly described|p452, p455|Permian|Permian|Silver Spur Subprovince, Woolomin Province. Forms a narrow, NNW-trending, partly fault-bounded wedge of sediments 30km W of Stanthorpe. Has open, gently plunging folds and moderate to locally steep dips. Fossil wood and other plant remains. Age from similarity with other Permian outliers.||||Unconformably overlies or is faulted against Texas beds.|Lithic sandstone, siltstone and mudstone, interlayered with sporadic discontinuous pebbly conglomerate lenses and local vitric tuff.|
15185|Pikedale beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||27-SEP-18
15185|Pikedale beds|70373|4|Described|p789-p792, p795, p797 Tb 1, p798-p804|Early Permian|Early Permian|No fossils reported, so early Permian age inferred from lithological similarities to other Permian units. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. 280-320m thick.|289.7 +/-9.9 Ma (LA-ICP-MS on zircons)|||Assumed to overlie Texas beds, contact probably faulted. Correlated with Bondonga, Silver Spur, Terrica and Alum Rock beds.|Sandstone, pebbly sandstone, conglomerate, diamictite and mudstone with clasts of chert, sandstone and volcanics.|
15197|Piles Creek Sandstone|40499|6|Mentioned|p147|||||||||
15197|Piles Creek Sandstone|43358|14|Not recorded|p51-53,55,58-60||Triassic|(Hawkesbury Sandstone)||||||
15202|Pillar Valley Formation|41631|6|Mentioned|Fig.4|||||||||
15202|Pillar Valley Formation|43736|6|Mentioned|p5|||||||||
15202|Pillar Valley Formation|60995|5|Briefly described|p53 Fig. 4|||Of Ties et al (1985a). Together with Ripley Raod Sandstone was part of the former "Peak Formation" in the "Pillar Valley Subgroup".||||||
15202|Pillar Valley Formation|61006|6|Mentioned|p277|||Of Ties and others (1985b) - superseded by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin.||||||
15202|Pillar Valley Formation|61310|5|Briefly described|p21, Table C1 (p22-23)|Early Jurassic|Early Jurassic|Of the Woogaroo Subgroup. Geological Province: Clarence-Moreton Basin||||||
15212|Pilliga Sandstone|721|5|Briefly described|Map legend|Tithonian|Oxfordian|Geological Province: Surat Basin.||||||11-NOV-14
15212|Pilliga Sandstone|730|6|Mentioned|p24.|||Fluviatile.||||||11-NOV-14
15212|Pilliga Sandstone|12597|5|Briefly described|p492 Tb.1, p494, p497|Tithonian|Oxfordian|S Surat Basin. 100-300m thick.||||Interfingers with Kumbarilla beds.|Quartzose sandstone with minor interbeds of siltstone and mudstone; thin pebble conglomerate bands occur throughout.|
15212|Pilliga Sandstone|22831|4|Described|p 84|Jurassic|Jurassic|Overlain by Cainozoic sediments.||||||17-SEP-08
15212|Pilliga Sandstone|22857|4|Described|p295, p296-7 Tb 22.1, p546 Tb A1.12|Late Jurassic|Callovian|Of the Injune Creek Group. Fullers earth occurs in a thin horizon. Merges with Gubberamunda Sandstone from Qld. Max. thickness: 300m. Geological Province: Surat Basin. See also p312-3 Fig. 22.6, p314-5..||||||
15212|Pilliga Sandstone|22865|4|Described|p295,Table22.1p296-7|Tithonian|Callovian|||||||
15212|Pilliga Sandstone|23016|6|Mentioned|p316||Jurassic|||||||
15212|Pilliga Sandstone|23043|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|of Surat Basin.||||||
15212|Pilliga Sandstone|23050|4|Described|p23 Table 4|Late Jurassic|Late Jurassic|of Surat Basin. Palnology indicates a J5 Jurassic age.||||||
15212|Pilliga Sandstone|23051|5|Briefly described|Map Legend|Late Jurassic|Late Jurassic|of Surat Basin.||||||
15212|Pilliga Sandstone|23053|4|Described|p8,10,25-6,57|Late Jurassic|Middle Jurassic|||||||
15212|Pilliga Sandstone|23170|2|Defined|p332|Late Jurassic|Late Jurassic|Of Surat Basin. Age from microfloral assemblage.||||||23-SEP-18
15212|Pilliga Sandstone|23214|6|Mentioned|p271|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
15212|Pilliga Sandstone|23566|5|Briefly described|p116 Fig. 2|Jurassic|Jurassic|Geological Province: Gunnedah Basin||||||
15212|Pilliga Sandstone|23740|5|Briefly described|p1220|Jurassic|Jurassic|Geological Province: Gunnedah Basin||||||
15212|Pilliga Sandstone|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
15212|Pilliga Sandstone|23883|6|Mentioned|p134|||Geological Province: Great Australian Superbasin.||||||
15212|Pilliga Sandstone|23982|5|Briefly described|p2|Cretaceous|Jurassic|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
15212|Pilliga Sandstone|24042|5|Briefly described|p510|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
15212|Pilliga Sandstone|24092|5|Briefly described|p8 Fig.3|||||||||
15212|Pilliga Sandstone|24126|5|Briefly described|p5|Jurassic|Triassic|||||||
15212|Pilliga Sandstone|24159|5|Briefly described|p148 Fig.2|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin. Underlying Unit: Walloon Coal Measures.||||||
15212|Pilliga Sandstone|29591|6|Mentioned|p75|||||||||
15212|Pilliga Sandstone|29869|6|Mentioned|Fig.1|||||||||
15212|Pilliga Sandstone|29870|6|Mentioned|p15|||||||||
15212|Pilliga Sandstone|29909|6|Mentioned|p145|||||||||
15212|Pilliga Sandstone|29986|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|29993|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30135|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30608|5|Briefly described|p116|||Lithology||||||
15212|Pilliga Sandstone|30610|1|Redefined|p322|Late Jurassic|Late Jurassic|||||||
15212|Pilliga Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
15212|Pilliga Sandstone|30699|6|Mentioned|p56|||Map||||||
15212|Pilliga Sandstone|30910|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|31326|4|Described|p38|||Jurassic||||||
15212|Pilliga Sandstone|31376|6|Mentioned|p4|||||||||
15212|Pilliga Sandstone|31726|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32045|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32482|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|32944|6|Mentioned|Fig.2|||||||||
15212|Pilliga Sandstone|33169|6|Mentioned|p322|||||||||
15212|Pilliga Sandstone|33676|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|33709|6|Mentioned|p102|||||||||
15212|Pilliga Sandstone|33873|6|Mentioned|p5|||||||||
15212|Pilliga Sandstone|34059|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|34134|6|Mentioned|Cor.Chart|||Upper Jurassic.||||||
15212|Pilliga Sandstone|34244|6|Mentioned|p299|||Jur. Aquifer. See also P300||||||
15212|Pilliga Sandstone|34254|6|Mentioned|p491|||||||||
15212|Pilliga Sandstone|34394|6|Mentioned|Fig.43|||Refers Dulhunty (1967).||||||
15212|Pilliga Sandstone|34444|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15212|Pilliga Sandstone|34982|6|Mentioned|p49|||||||||
15212|Pilliga Sandstone|35065|6|Mentioned|p45|||||||||
15212|Pilliga Sandstone|35095|6|Mentioned|p108|||||||||
15212|Pilliga Sandstone|35587|6|Mentioned|p44|||||||||
15212|Pilliga Sandstone|36570|2|Defined|p39|Jurassic|Jurassic|See p25, Fig.9.||||||22-SEP-18
15212|Pilliga Sandstone|36751|6|Mentioned|p488|||||||||
15212|Pilliga Sandstone|36961|6|Mentioned|Table 1|||||||||
15212|Pilliga Sandstone|37437|5|Briefly described|p29|||||||||
15212|Pilliga Sandstone|37794|4|Described|p191|||||||||
15212|Pilliga Sandstone|37856|6|Mentioned|Table I|||||||||
15212|Pilliga Sandstone|37995|6|Mentioned|p62|||||||||
15212|Pilliga Sandstone|38689|6|Mentioned|p308|||||||||
15212|Pilliga Sandstone|38813|5|Briefly described|p251|||||||||
15212|Pilliga Sandstone|39063|6|Mentioned|Fig.6|||||||||
15212|Pilliga Sandstone|39212|6|Mentioned|p25|||Aquifer||||||
15212|Pilliga Sandstone|39315|6|Mentioned|Fig.5|||||||||
15212|Pilliga Sandstone|39445|5|Briefly described|Table 10|||||||||
15212|Pilliga Sandstone|39664|6|Mentioned|p120|||||||||
15212|Pilliga Sandstone|39666|6|Mentioned|p94|||See also P112||||||
15212|Pilliga Sandstone|39913|6|Mentioned|Fig.1|||||||||
15212|Pilliga Sandstone|40328|6|Mentioned|p213|||||||||
15212|Pilliga Sandstone|40365|6|Mentioned|p245|||See also P293||||||
15212|Pilliga Sandstone|40767|6|Mentioned|p2|||||||||
15212|Pilliga Sandstone|40869|6|Mentioned|p29|||||||||
15212|Pilliga Sandstone|40952|6|Mentioned|p3|||||||||
15212|Pilliga Sandstone|40953|6|Mentioned|p19|||||||||
15212|Pilliga Sandstone|41266|6|Mentioned|Fig.3|||||||||
15212|Pilliga Sandstone|41290|5|Briefly described|p227|||||||||
15212|Pilliga Sandstone|41330|6|Mentioned|p21|||||||||
15212|Pilliga Sandstone|41779|6|Mentioned|p183|||||||||
15212|Pilliga Sandstone|42135|6|Mentioned|Fig.6 P357|||||||||
15212|Pilliga Sandstone|42596|5|Briefly described|Fig. 1 P24|||||||||
15212|Pilliga Sandstone|42657|6|Mentioned|p73|||||||||
15212|Pilliga Sandstone|42679|6|Mentioned|Fig.4 P3|||||||||
15212|Pilliga Sandstone|42918|6|Mentioned|p45|||||||||
15212|Pilliga Sandstone|43044|6|Mentioned|p121|||||||||
15212|Pilliga Sandstone|43091|5|Briefly described|Map Legend|||of Surat Basin||||||
15212|Pilliga Sandstone|43161|6|Mentioned|21-26||Jurassic|||||||
15212|Pilliga Sandstone|43194|5|Briefly described|p122|Jurassic|Jurassic|Gunnedah Basin. Disconformably overlies Napperby Formation.||||||
15212|Pilliga Sandstone|43276|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|||||||
15212|Pilliga Sandstone|43277|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|of Great Australian Basin.||||||
15212|Pilliga Sandstone|43354|5|Briefly described|p105-108,p107||Jurassic|||||||
15212|Pilliga Sandstone|43355|14|Not recorded|Map Legend||Jurassic|Provisional Edition||||||
15212|Pilliga Sandstone|43356|14|Not recorded|Map Legend||Jurassic|||||||
15212|Pilliga Sandstone|43383|14|Not recorded|p25||Jurassic|||||||
15212|Pilliga Sandstone|43393|14|Not recorded|p179-182||Jurassic|||||||
15212|Pilliga Sandstone|43394|14|Not recorded|p105-108||Jurassic|||||||
15212|Pilliga Sandstone|43404|14|Not recorded|Table p11|Cretaceous|Jurassic|||||||
15212|Pilliga Sandstone|43405|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43407|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43410|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43476|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43494|4|Described|p14|Late Jurassic|Late Jurassic|Lower lithic sandstone and polymictic conglomerate; and upper more quartz-rich rock, particularly the basal bed which is a very coarse quartz sandstone containing rounded qtz pebbles and subangular qtz granules. Overlies Pulrawaugh Fm. Max. thick: 100m.||||||16-MAR-06
15212|Pilliga Sandstone|43500|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
15212|Pilliga Sandstone|43534|14|Not recorded|p393,394|||||||||
15212|Pilliga Sandstone|43535|14|Not recorded|p133-136||Jurassic|||||||
15212|Pilliga Sandstone|43582|6|Mentioned|Fig.5,p16||Late Jurassic|||||||
15212|Pilliga Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
15212|Pilliga Sandstone|43678|6|Mentioned|p316||Jurassic|||||||
15212|Pilliga Sandstone|44028|14|Not recorded|p514|||Equivalent of Gubberamunda Sandstone. See Strat Table.||||||
15212|Pilliga Sandstone|44160|6|Mentioned|Map Legend||Jurassic|||||||
15212|Pilliga Sandstone|44450|6|Mentioned|p27|||Geological Province: Great Australian Basin.||||||
15212|Pilliga Sandstone|45110|2|Defined|p98|Late Jurassic|Late Jurassic|Formerly Pilliga Series (Kenny,1928), Pilliga Beds (Dulhunty,1939).||||||11-NOV-14
15212|Pilliga Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
15212|Pilliga Sandstone|48958|6|Mentioned|Plate 1|||||||||
15212|Pilliga Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
15212|Pilliga Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
15212|Pilliga Sandstone|49781|6|Mentioned|p4|||||||||
15212|Pilliga Sandstone|50590|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Great Australian Basin (possibly misspelt) .  Massive to cross-bedded coarse pebbly lithic-quartz sandstone, minor lithic sandstone and siltstone.||||||
15212|Pilliga Sandstone|50616|5|Briefly described|p275, 286|Jurassic|Jurassic|Interbedded sandstone and thicker shale and mudstone units.||||||
15212|Pilliga Sandstone|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin. Overlies: Purlawaugh Formation.||||||05-JUL-04
15212|Pilliga Sandstone|60266|5|Briefly described|p2,  p3 Tb. 1|Late Jurassic|Middle Jurassic|Piedmont deposits of quartzose sandstone and conglomerate.  Overlies Purlawaugh Formation; underlies the Keelindi beds.  Geological Province: Surat Basin.||||||08-DEC-04
15212|Pilliga Sandstone|60267|4|Described|p15|Jurassic|Jurassic|Quartz-rich sandstone conglomerate with siliceous clasts of vein quartz, chert and jasper.  Overlies Garrawilla Volcs; conformably overlain by Keelindi beds; also overlain by Warrumbungle Volcs.  Max. thickness:>100m.  Geol.Prov: Surat Basin.||||||
15212|Pilliga Sandstone|61313|5|Briefly described|p91, p94 Fig.G7|Late Jurassic|Middle Jurassic|Stacked sequence of braided fluvial sandstones with reservoir qualities but lacks laterally continuous seals. Conformably overlies Purlawaugh Sandstone; conformably overlain by Orallo and Mooga Fms. Thickness: 213m. Geol. Prov: Gunnedah and Surat Basins.||||||
15212|Pilliga Sandstone|61377|5|Briefly described|p152, p154 Fig. SU9|Late Jurassic|Middle Jurassic|Massive quartzose sandstones; minor siltstone and mudstone. Conformably overlies the Walloon Coal Measures; conformably overlain by Orallo, Mooga, Bungil and Wallumbilla Formations. Geological Province: Surat Basin. See also p148 Tb. SU1, p149 Fig. SU8.||||||07-FEB-11
15212|Pilliga Sandstone|61776|5|Briefly described|p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Quartz-sandstone with minor lithic sandstone and siltstone.||||||17-SEP-08
15212|Pilliga Sandstone|62534|5|Briefly described|p10 (legend)|Late Jurassic|Late Jurassic|Geological Province: Surat Basin. Quartzose sandstone.||||||07-FEB-11
15212|Pilliga Sandstone|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
15212|Pilliga Sandstone|63733|5|Briefly described|Map legend|Jurassic|Jurassic|Quartzose sandstone, conglomerate.||||||
15212|Pilliga Sandstone|64856|6|Mentioned|p90, p93|||Interfingers with Springbok Sandstone.|| ||||29-NOV-17
15212|Pilliga Sandstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Late Jurassic|Unit in the Surat Basin. Underlies the Orallo Formation in NSW; overlies the Purlawaugh Formation.||||||22-MAR-12
15212|Pilliga Sandstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Late Jurassic|Overlies the Purlawaugh Formation, underlies the Orallo Formation.||||||
15212|Pilliga Sandstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous|Late Jurassic|||||||
15212|Pilliga Sandstone|65116|4|Described|p456, Fig 2 p437|Early Cretaceous|Late Jurassic|Underlies the Orallo Formation, overlies the Purlawaugh Formation, Surat Basin. Equivalent to Springbok Sst + Westbourne Formation + Gubberamunda Formation. Medium to coarse-grained quartzose sandstone.||||||
15212|Pilliga Sandstone|65119|6|Mentioned|p504 Table 1|Late Jurassic|Early Jurassic|Age: 177-150 Ma. Fission Track age: 187+/-13 Ma.||||||20-MAR-13
15212|Pilliga Sandstone|66529|6|Mentioned|p12 Fig.5 |||Coonamble Embayment and Surat Basin.||||Overlies Walloon Coal Measures and Purlawaugh Formation. Is overlain by Kumbarilla beds and Keelindi Beds.||
15212|Pilliga Sandstone|68003|5|Briefly described|p52, pp54-57 Figs, pp64-66, p98, p127.|Late Jurassic|Middle Jurassic|Crops out over much of the Brigalow Belt South Bioregion. Forms cliffs.||||Conformably overlies Walloon Coal Measures and Purlawaugh Formation. Is conformably overlain by Keelindi beds and Orallo Formation.|Coarse-grained, quartzose, braided-stream sandstone; basal pebble lenses common; minor interbeds of siltstone and mudstone; common carbonaceous fragments and iron staining.|
15212|Pilliga Sandstone|68004|5|Briefly described|p87, p174, p182.|Late Jurassic|Late Jurassic|Excellent reservoir potential; sealed by the Orallo Formation but this becomes more sandy towards its depositional limits. Targeted for oil/gas exploration; only minor fluorescence and low level gas shows.|||||Widespread, excellent quality quartz sandstone.|
15212|Pilliga Sandstone|68005|5|Briefly described|p131.|Jurassic|Jurassic|Surat Basin.|||||Medium to coarse, cross-bedded quartzose sandstone with basal pebble lenses common; minor interbeds of siltstone and mudstone.|
15212|Pilliga Sandstone|68006|5|Briefly described|p92.|||Bores targetting this unit for water have intersected coal in the underlying Walloon Coal Measures.||||Overlies Walloon Coal Measures.||
15212|Pilliga Sandstone|68069|5|Briefly described|Map legend.|Late Jurassic|Late Jurassic|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Braided to meandering river system with extensive flood plains.||||Conformably overlies Purlawaugh Formation. Is overlain conformably by Orallo Formation.|Medium- to coarse-grained, well-sorted quartzose sandstone with minor interbeds of mudstone, siltstone and fine-grained sandstone.|
15212|Pilliga Sandstone|68135|5|Briefly described|p52 fig 2b|Tithonian|Oxfordian|Surat Basin (NSW)||||Disconformably overlies Purlawaugh Formation, overlain by Orallo Formation|Cross-bedded sandstone.|14-SEP-17
15212|Pilliga Sandstone|68593|5|Briefly described|p3-4, p45, p47|Late Jurassic|Late Jurassic|Deposited by a braided to meandering river system with extensive flood plains. One of the main artesian aquifers in the map area.||||Overlies Purlawaugh Formation. Is overlain by Orallo Formation.|Medium- to coarse-grained, well-sorted quartzose sandstone with minor interbeds of mudstone, siltstone and fine-grained sandstone.|
15212|Pilliga Sandstone|68679|6|Mentioned|p455|Early Cretaceous|Early Jurassic|||||||
15212|Pilliga Sandstone|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
15212|Pilliga Sandstone|69594|5|Briefly described|p537|||Exon (1976).||||Interdigitates with and passes into Westbourne Formation.||
15212|Pilliga Sandstone|69790|6|Mentioned|p1070|Late Jurassic|Late Jurassic|||||Equivalent to Springbok Sandstone in Qld.||
15212|Pilliga Sandstone|70036|5|Briefly described|Map legend|Late Jurassic|Late Jurassic|Surat Basin. Included in a mapped unit of a braided stream sequence: quartzose sandstone with minor mudstone, siltstone and coal.||||||
15212|Pilliga Sandstone|70821|5|Briefly described|p22 Fig.2.7, p80|Jurassic|Jurassic|Surat Basin; Coonamble Embayment. Aquifer: generally artesian.||Injune Creek Group.||Overlies Walloon Coal Measures or Purlawaugh Formation. Is overlain by Westbourne or Orallo Formations, Kumbarilla or Keelindi beds.||
15212|Pilliga Sandstone|71628|5|Briefly described|p4: 33, 35|||Surat Basin.||||Overlies Graman and Linton Monzogranites.||
15212|Pilliga Sandstone|71890|4|Described|vi-vii, p5-p8, p18, p24, p26, p30|Kimmeridgian|Toarcian|Surat Basin. Interpreted to have been deposited in a braided stream system. Eroded prior to Miocene volcanism in the area. This unit is the most extensively exposed sedimentary unit in the present study's map area. This unit is typically an aquifer. See also  p33-p34, p39, p52.|177-150 Ma|||Disconformably overlies the Purlawaugh Formation. Conformably overlain by Keelindi beds. Overlies the Garrawilla Volcanics.|Medium- to very coarse grained, well sorted, quartzose sandstone and minor pebble conglomerate. Rare to minor thin interbeds of mudstone, siltstone and fine-grained sandstone.|13-JUN-22
15212|Pilliga Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW), Coonamble Embayment (NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||||Overlies Walloon Coal Measures and Purlawaugh FZ. Is overlain by Orallo FZ, Kumbarilla and Keelindi beds.||
15212|Pilliga Sandstone|72700|5|Briefly described|Mapsheet 1 and 2|Mesozoic|Palaeozoic||||||Commonly cross-bedded, medium to coarse-grained quartz sandstone and lesser conglomerate, minor mudstone, siltstone and coal.|
15212|Pilliga Sandstone|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in New South Wales.||||Overlies and partly laterally equivalent to Purlawaugh Formation and underlies Orallo Formation.|Includes fossiliferous sandstone.|
15212|Pilliga Sandstone|73492|6|Mentioned|p691|||||||||
15212|Pilliga Sandstone|73581|6|Mentioned|p12|||||||||
15220|Pilot Range Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
15220|Pilot Range Granite|31713|5|Briefly described|p12|||||||||
15220|Pilot Range Granite|31800|6|Mentioned|p204|||||||||
15220|Pilot Range Granite|33602|6|Mentioned|p28|||||||||
15220|Pilot Range Granite|35257|6|Mentioned|p157|||||||||
15220|Pilot Range Granite|37885|4|Described|p4|||||||||
15220|Pilot Range Granite|38879|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15220|Pilot Range Granite|40782|5|Briefly described|p104|||||||||
15220|Pilot Range Granite|42089|6|Mentioned|p19|||||||||
15220|Pilot Range Granite|70910|14|Not recorded|p44|||Cassiterite. Geological map on opposite page.||||||
15244|Pine Mountain Granite|23309|5|Briefly described|p344.||Silurian|G99 A-Type. Supersedes Pine Mountain Granodiorite and Leucogranite. Age: 413+/-12Ma.||||||
15244|Pine Mountain Granite|24133|3|Fully described|p79|Early Devonian|Late Silurian|Intrudes the Corryong Granite.  Age: 404+/-12 Ma.  Geological Province: Lachlan Fold Belt.||||||23-JUN-14
15244|Pine Mountain Granite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
15244|Pine Mountain Granite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
15244|Pine Mountain Granite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
15244|Pine Mountain Granite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
15244|Pine Mountain Granite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt. Age: 404 +/- 12 Ma (Rb/Sr)||||||13-SEP-04
15244|Pine Mountain Granite|24551|6|Mentioned|p233|||||||||
15244|Pine Mountain Granite|29953|5|Briefly described|p3|||||||||
15244|Pine Mountain Granite|30332|6|Mentioned|Table 2|||413 +/- 12 Ma||||||23-JUN-14
15244|Pine Mountain Granite|33602|6|Mentioned|p27|||||||||
15244|Pine Mountain Granite|35278|6|Mentioned|p362|||||||||
15244|Pine Mountain Granite|35283|6|Mentioned|p49|||||||||
15244|Pine Mountain Granite|39291|6|Mentioned|Fig.20|||||||||
15244|Pine Mountain Granite|39860|5|Briefly described|p21|||||||||
15244|Pine Mountain Granite|40328|6|Mentioned|p204|||||||||
15244|Pine Mountain Granite|40498|6|Mentioned|p367|||||||||
15244|Pine Mountain Granite|41433|5|Briefly described|p161|||||||||
15244|Pine Mountain Granite|41868|6|Mentioned|p569|||||||||
15244|Pine Mountain Granite|42089|6|Mentioned|p19|||||||||
15244|Pine Mountain Granite|42726|5|Briefly described|map legend|Silurian||No 476.||||||04-JUN-11
15244|Pine Mountain Granite|42827|5|Briefly described|p569|||||||||
15244|Pine Mountain Granite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Pine Mountain I-type.||||||
15244|Pine Mountain Granite|45087|5|Briefly described|p12|||Chemical analyses||||||
15244|Pine Mountain Granite|68116|5|Briefly described|Appendix, Map 20.|Early Devonian|Early Devonian||||||Biotite leucogranite: pale to deep pink, medium to coarse grained; minor fine grained granite pods; nonmagnetic.|
15255|Pinegrove Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Doyles Creek Subgroup.  Includes the Hambledon Hill Sand Member, Wylies Flat Coal Member and the Glengowan Shale Member.   Geological Province: Sydney Basin||||||
15255|Pinegrove Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Doyles Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
15255|Pinegrove Formation|29942|3|Fully described|p11|||||||||
15255|Pinegrove Formation|45090|6|Mentioned|p187|||Refers Britten (1972)||||||
15255|Pinegrove Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Lower unit in Doyles Creek Sub-group.|Includes Glengowan Shale, Wylies Flat Coal, and Hambledon Hill Sandstone, Members.|Overlies Lucernia Coal. Is overlain by Waterfall Gully Formation.|A sequence of shale and sandstone with minor tuffaceous claystone. Contains a vestigial coal member comprising inferior coal plies and bands.|
15258|Pingbilly Formation|22857|5|Briefly described|p122, p408 App. 1 Tb. A1.4.|Early Ordovician|Early Ordovician|Mudstone, shale. Age is Bendigonian to Castlemanian. Geological Province: Gnalta Shelf (Kanmantoo Fold Belt).||||||
15258|Pingbilly Formation|23245|5|Briefly described|p122|Ordovician|Cambrian|||||||
15258|Pingbilly Formation|35118|6|Mentioned|Fig.5|||||||||
15258|Pingbilly Formation|40136|5|Briefly described|p36|||||||||
15258|Pingbilly Formation|44093|5|Briefly described|p142 App. 1|Early Ordovician|Cambrian|Geological Province: Kanmantoo Fold Belt.||||||22-MAR-05
15258|Pingbilly Formation|62787|6|Mentioned|p77|||||||||07-FEB-11
15258|Pingbilly Formation|62794|6|Mentioned|p298, p299|Early Ordovician|Early Ordovician|Mount Arrowsmith area, western NSW. Correlates with lower Horn Valley Siltstone in Amadeus Basin, NT.||||||
15258|Pingbilly Formation|63489|5|Briefly described|Map legend|Devonian|Silurian|Mudstone, quartzite, minor limestone.||||||
15258|Pingbilly Formation|63793|6|Mentioned|p24. |||||||||
15258|Pingbilly Formation|64671|5|Briefly described|Map legend|Ordovician|Ordovician|West of Mount Arrowsmith this unit is faulted against Cambrian formations and western Kara beds. Micaceous blue, grey, green and brown mudstone.||||||01-DEC-08
15258|Pingbilly Formation|64687|5|Briefly described|Map Legend|Ordovician|Ordovician|Micaceous blue, grey, green and brown mudstone. Faulted and unconformable against Cambrian formations and western Kara beds.||||||27-NOV-08
15258|Pingbilly Formation|66623|3|Fully described|pp152-155, pp158-159.|Early Ordovician|Early Ordovician|Contemporaneous with lower Rowena Formation. Poorly exposed. Thickness about 64 m. Only fossil described is a brachiopod, Celsiorthis bulancis, which occurs also in the underlying Tabita Formation. Deposition probably below wave-base.||Unit in Pimbilla Tank Group.||Overlies Tabita Formation.  The top is unknown/nowhere exposed.|Micaceous blue-grey, olive-green and brown mudstones and siltstones with fine-grained subangular quartz grains; occasional subangular to rounded lithic clasts to 40 mm diameter occur in the mudstone.|
15258|Pingbilly Formation|66917|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|Fossiliferous.||Unit in Pimbilla Tank Group.||Overlies Tabita Formation.|Poorly-outcropping, cleaved, blue-grey, green and brown micaceous mudstone and shale.|
15258|Pingbilly Formation|66929|5|Briefly described|Map legend|Ordovician|Ordovician||||||Micaceous blue, grey, green and brown mudstone.|
15258|Pingbilly Formation|66933|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15258|Pingbilly Formation|67208|5|Briefly described|Map legend.|Ordovician|Ordovician|||Unit in Pimbilla Tank Group.|||Poorly outcropping, cleaved, blue-grey, green and brown micaceous mudstone and shale; fossiliferous.|
15258|Pingbilly Formation|67322|4|Described|p10; Fig.5|Floian|Floian|Warris (1967). Approximately 70m thick. Age is poorly constrained; likely to be similar to underlying Tabita Formation due to the brachiopod Celsiorthis bulancis found in both. Occurs in the Mount Arrowsmith region.||Of the Pimbilla Tank Group.||Conformably overlies Tabita Formation.|Poorly outcropping micaceous mudstone; occasional subangular to rounded lithic clasts.|22-FEB-18
15278|Pintapah Subgroup|22772|4|Described|p64,Table13.1|Cryogenian|Cryogenian|||||||
15278|Pintapah Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Adelaide Fold Belt. See also p400 and 402 App. 1 Tb.A1.3.||||||
15278|Pintapah Subgroup|36733|6|Mentioned|Table 5|||||||||
15278|Pintapah Subgroup|41403|6|Mentioned|p48|||||||||
15278|Pintapah Subgroup|42531|5|Briefly described|Map legend|Adelaidean||||||||
15278|Pintapah Subgroup|43265|5|Briefly described|Map Legend||Neoproterozoic|of Poolamacca Group.||||||
15278|Pintapah Subgroup|43268|5|Briefly described|Map Legend||Neoproterozoic|of Poolamacca Group.||||||
15278|Pintapah Subgroup|43269|5|Briefly described|Map Legend||Neoproterozoic|of Poolamacca Group.||||||
15278|Pintapah Subgroup|70000|5|Briefly described|p34, p39|Neoproterozoic|Neoproterozoic|||Unit in Poolamacca Group.|Includes Lady Don Quartzite and Christine Judith Conglomerate.||Fluviatile to shallow marine, mature sandstone and lesser conglomerate.|
15278|Pintapah Subgroup|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Poolamacca Group.|Includes Lady Don Quartzite and Christine Judith Conglomerate.|Is overlain by Wendalpa Subgroup.|White quartzite interbedded with conglomerate.|
15278|Pintapah Subgroup|72461|6|Mentioned|p16 fig 9|||||Poolmacca Group|Includes the Christine Judith Conglomerate and the Lady Don Quartzite.|||
15278|Pintapah Subgroup|74367|6|Mentioned|p20|||||||||
15285|Pipeclay Creek Formation|22571|6|Mentioned|p19|||Overlain by Tamworth Group.||||||25-FEB-08
15285|Pipeclay Creek Formation|22736|6|Mentioned|p628 Fig7||Cambrian|||||||
15285|Pipeclay Creek Formation|22750|5|Briefly described|p 228||Middle Cambrian|||||||
15285|Pipeclay Creek Formation|22857|4|Described|p434 App. 1 Tb. A1.5|Late Cambrian|Middle Cambrian|Cherty siltstone, lenses of granule conglomerate. Max. thickness: 1km. Geological Province: New England Fold Belt.||||||
15285|Pipeclay Creek Formation|23185|6|Mentioned|Fig1p156,160|||||||||
15285|Pipeclay Creek Formation|30650|5|Briefly described|p317|||||||||
15285|Pipeclay Creek Formation|30911|6|Mentioned|Map legend|Silurian|Silurian|||||||
15285|Pipeclay Creek Formation|31999|6|Mentioned|p150|||Table 1||||||
15285|Pipeclay Creek Formation|32482|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15285|Pipeclay Creek Formation|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
15285|Pipeclay Creek Formation|32672|6|Mentioned|p673|||||||||
15285|Pipeclay Creek Formation|33326|6|Mentioned|p446|||Fauna.||||||
15285|Pipeclay Creek Formation|34397|6|Mentioned|p230|||||||||
15285|Pipeclay Creek Formation|34554|5|Briefly described|p231|||||||||
15285|Pipeclay Creek Formation|36961|6|Mentioned|p208|||See also Fig.3.||||||
15285|Pipeclay Creek Formation|37727|4|Described|p81|||||||||
15285|Pipeclay Creek Formation|38686|5|Briefly described|p54|Early Paleozoic|Early Paleozoic|Geological Province: New England Fold Belt. Overlying Unit: Drik-Drik Formation.||||||07-NOV-08
15285|Pipeclay Creek Formation|39214|6|Mentioned|p33|||||||||
15285|Pipeclay Creek Formation|39331|6|Mentioned|Fig.10-1|||||||||
15285|Pipeclay Creek Formation|40136|5|Briefly described|p37|||||||||
15285|Pipeclay Creek Formation|40328|3|Fully described|p197|||||||||
15285|Pipeclay Creek Formation|41347|4|Described|Table 3|||||||||
15285|Pipeclay Creek Formation|41348|5|Briefly described|Map legend|Ordovician|Cambrian|In the Tamworth Belt.||||||16-DEC-04
15285|Pipeclay Creek Formation|41796|6|Mentioned|p304|||||||||
15285|Pipeclay Creek Formation|42554|5|Briefly described|p37|||||||||
15285|Pipeclay Creek Formation|43400|2|Defined|p178,179,183,184,map||Gedinnian|||||||
15285|Pipeclay Creek Formation|43406|14|Not recorded|p42,48|||Formation of L.Devn Tamworth Group.||||||25-FEB-08
15285|Pipeclay Creek Formation|43407|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
15285|Pipeclay Creek Formation|43525|14|Not recorded|Table p132|Siegenian|Gedinnian|||||||
15285|Pipeclay Creek Formation|44093|5|Briefly described|p227 App. 1|Ordovician|Cambrian|Geological Province: New England Fold Belt.||||||
15285|Pipeclay Creek Formation|47056|6|Mentioned|Fig.2 P523|||||||||
15285|Pipeclay Creek Formation|50094|5|Briefly described|p315, p316 Fig.1, p317 Fig.2|Late Cambrian|Middle Cambrian|Unconformably overlain by Haedon Formation. Geological Province: New England Fold Belt.||||||
15285|Pipeclay Creek Formation|50168|6|Mentioned|p157 Fig.2, p159|||Gamilaroi Terrane. Probably Devonian; possibly Cambrian.||||||06-FEB-18
15285|Pipeclay Creek Formation|61392|5|Briefly described|p165 Fig. 2|Late Cambrian|Middle Cambrian|In the Gamilaroi terrane.||||||07-FEB-11
15285|Pipeclay Creek Formation|61762|6|Mentioned|p14 Tab. 1|Ordovician|Cambrian|Consists of conglomerate, sandstone and volcanic-derived mudstone. Forearc Basin environment.||||||
15285|Pipeclay Creek Formation|61765|6|Mentioned|p58|Cambrian|Cambrian|Excluded from Tamworth Group due to Cambrian aged fossils.||||||07-FEB-11
15285|Pipeclay Creek Formation|63119|5|Briefly described|p214|Late Cambrian|Late Cambrian|Includes spiculitic chert which contains conodonts.||||||
15285|Pipeclay Creek Formation|67322|4|Described|p3 Fig.1;Fig.5; p27|Early Devonian|Middle Cambrian|New England Orogen. Named by Crook (1961), who assigned an Early Devonian age. Chert beds in the Formation are of Middle to early Late Cambrian age based on the presence of paraconodonts and absence of euconodonts. Over 900m thick. Occurs in the Tamworth-Neminha area.||||Conformably overlies the Murrawong Creek Formation. Unconformably overlain by the Haedon Formation.|Consists predominantly of siltstone and mudstone with subsidiary chert, tuff, sandstone and fine-grained conglomerate.|22-FEB-18
15285|Pipeclay Creek Formation|68005|5|Briefly described|p49 Fig.3-M, p50, p151, p170.|Middle Cambrian|Middle Cambrian|Tamworth Belt. Deep marine sedimentary rocks.||||Overlies Murrawong Creek Formation. Is unconformably overlain by Haedon Formation.|Thinly banded black and white argillite and chert, volcanic wackes.|
15285|Pipeclay Creek Formation|68822|5|Briefly described|p329|Guzhangian|Drumian|Has a faulted base and lies unconformably below Ordovician strata.|ca. 502 - 499 Ma|||Underlain by the Murrawong Creek Formation.|Dominated by shale and siltstone, and also contains chert, tuff, sandstone and fine-grained conglomerates.|
15285|Pipeclay Creek Formation|73440|6|Mentioned|p146|Silurian|Ordovician|Reflects deep marine settings.|||||Deep marine tuffs, turbidites and conglomerates.|
15299|Pittman Formation|12185|5|Briefly described|map legend|Middle Ordovician|Middle Ordovician|Shale, sandstone, mudstone, radiolarite. BMR map symbol: Omp.||||||
15299|Pittman Formation|22843|6|Mentioned|p23||Ordovician|||||||
15299|Pittman Formation|22857|4|Described|p134, p424 App.1 Tb.A1.5|Early Ordovician|Early Ordovician|Quartz-rich arenite, shale, siltstone, minor black shale, chert, impure calcareous arenite. Unconformably overlain by State Circle Shale. Max. thickness: 2km.||||||
15299|Pittman Formation|23048|6|Mentioned|p2 fig5||Ordovician|||||||
15299|Pittman Formation|23213|5|Briefly described|Fig.10 p24|||Contains Darriwilian fossils. Of Monaro Trough.||||||22-MAY-08
15299|Pittman Formation|23245|6|Mentioned|p134||Early Ordovician|||||||
15299|Pittman Formation|24128|5|Briefly described|p3|Ordovician|Ordovician|Known as Foxlow Beds on MICHELAGO.  Geological Province: Lachlan Fold Belt.||||||
15299|Pittman Formation|24215|5|Briefly described|p804|||Geological Province:  Lachlan Fold Belt||||||
15299|Pittman Formation|29992|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15299|Pittman Formation|29994|6|Mentioned|Map legend|Middle Ordovician|Middle Ordovician|||||||
15299|Pittman Formation|30329|6|Mentioned|p30|||Table P30||||||
15299|Pittman Formation|30332|4|Described|p122|||Ordovician age||||||
15299|Pittman Formation|31019|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15299|Pittman Formation|31111|6|Mentioned|Map legend|Ordovician|Ordovician|Shown on attached map.||||||
15299|Pittman Formation|31161|5|Briefly described|PA5|||||||||
15299|Pittman Formation|31284|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Upper OrdovicianM - U||||||
15299|Pittman Formation|32483|6|Mentioned|p9|||L.Ord.||||||
15299|Pittman Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
15299|Pittman Formation|32672|6|Mentioned|p672|||||||||
15299|Pittman Formation|32820|6|Mentioned|Table 1|||Refers Crook et al (1973)||||||
15299|Pittman Formation|33004|6|Mentioned|Plate 16|||Shown photo 16||||||
15299|Pittman Formation|33125|6|Mentioned|p15|||Correlation chart.||||||
15299|Pittman Formation|33325|5|Briefly described|Table 1|||See also P22. Darriwilian - Gisbornian||||||
15299|Pittman Formation|33328|4|Described|Table 1|||P8||||||
15299|Pittman Formation|34287|6|Mentioned|p72|||||||||
15299|Pittman Formation|34404|4|Described|p89|||Mention p97.||||||19-OCT-22
15299|Pittman Formation|34405|6|Mentioned|Fig.3.9|||||||||
15299|Pittman Formation|35110|6|Mentioned|p3|||||||||
15299|Pittman Formation|35118|6|Mentioned|Fig.5|||||||||
15299|Pittman Formation|35614|5|Briefly described|p6|||||||||
15299|Pittman Formation|36413|6|Mentioned|Table 3|||||||||
15299|Pittman Formation|36633|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Late Ordovician||||||
15299|Pittman Formation|37348|6|Mentioned|p97|||||||||
15299|Pittman Formation|37727|6|Mentioned|Fig.1|||||||||
15299|Pittman Formation|37728|4|Described|Table 2|||||||||
15299|Pittman Formation|38664|5|Briefly described|p5|||||||||
15299|Pittman Formation|39331|4|Described|p50|||See also P45, Fig.0-3||||||
15299|Pittman Formation|39947|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle to Late Ordovician||||||
15299|Pittman Formation|40136|5|Briefly described|p37|||||||||
15299|Pittman Formation|40328|6|Mentioned|p55|||||||||
15299|Pittman Formation|41356|5|Briefly described|p34|||||||||
15299|Pittman Formation|42497|5|Briefly described|Map Legend|Bolindian|Darriwilian|||||||
15299|Pittman Formation|42727|5|Briefly described|map legend, map schematic section|Late Ordovician|Middle Ordovician|Includes Acton Shale Member. Distal quartz turbidites. Under Copper Creek Shale, Rutledge Quartzite Mbr, and Murrumbateman Creek, Canberra and Cappanana Fms. Underlies Gearys Gap Fm. Intruded by Sutton Granodiorite. BMR symbol: Op. Geol.Prov: Monaro Basin||||||
15299|Pittman Formation|42820|2|Defined|p7-10||Middle Ordovician|Type section designated by Opik in 1958 now in very poor condition. New reference sections described in Molonglo Gorge.||||||19-OCT-22
15299|Pittman Formation|43344|14|Not recorded|p110,113||Late Ordovician|||||||
15299|Pittman Formation|43384|14|Not recorded|Map Legend||Ordovician|||||||
15299|Pittman Formation|43385|14|Not recorded|p169,170|Llandeilian|Llanvirnian|||||||
15299|Pittman Formation|43472|14|Not recorded|p420,431,fig.1|||||||||
15299|Pittman Formation|43473|14|Not recorded|fig.1,opp.p1080||Early Ordovician|(M.Ord)||||||
15299|Pittman Formation|43479|14|Not recorded|p95f|Llandeilian|Arenigian|||||||
15299|Pittman Formation|43481|5|Briefly described|3,4|||||||||
15299|Pittman Formation|43795|5|Briefly described|p279|||||||||
15299|Pittman Formation|44093|5|Briefly described|p50|Ordovician|Ordovician|Includes Acton Shale Member. In the Bruce Block. Geological Province: Lachlan Fold Belt.||||||08-APR-05
15299|Pittman Formation|44970|2|Defined|p7,11-18,22,23,31,|Late Ordovician|Early Ordovician|p42,69,70,75,78,80,85,87,88,91,map.(M.-U.-Ord). See also Lexicon||||||
15299|Pittman Formation|45147|6|Mentioned|M9|||||||||
15299|Pittman Formation|46952|6|Mentioned|p150|||||||||
15299|Pittman Formation|47033|6|Mentioned|p79|||||||||
15299|Pittman Formation|47060|5|Briefly described|Fig.5 P166|||||||||
15299|Pittman Formation|49043|6|Mentioned|p6|||||||||
15299|Pittman Formation|50098|6|Mentioned|p10|Ordovician|Ordovician|Contains conodont moulds in silty shale.||||||
15299|Pittman Formation|67125|5|Briefly described|Slides 26, 36.|Ordovician|Ordovician|Locally contains marine fossils. Mis-spelt as Pittmann Formation on Slide 26.|c.470 Ma.|||Is unconformably overlain by Gearys Gap Formation. Intruded by Ellenden Granite.|Turbidites: phyllite and quartzite.|
15299|Pittman Formation|67322|4|Described|p16, p20 Fig.5|Sandbian|Darriwilian|Albury-Bega Terrane. Named and defined by Opik (1954, 1958). Graptolite faunas of two different ages occur in the Pittman Formation - one of probable late Darriwilian age and the other (about 30m below the overlying Acton Shale) with Gisbornian affinities (Opik 1958). Occurs in the Canberra-Queanbeyan region.||Of the Adaminaby Group||Overlain by the Acton Shale (Bendoc Group). Correlates with top of Adaminaby Group.|Sandstone, shale, and minor radiolarian chert beds up to 6m thick.|22-FEB-18
15299|Pittman Formation|68592|4|Described|p298, p338|Ordovician|Ordovician|Opik (1958). Canberra region.|||Includes Acton Shale Member.|Equivalent to Abercrombie Formation.|Sandstone-rich.|
15299|Pittman Formation|70377|5|Briefly described|p855, p857, p858 Fig 4|Late Ordovician|Late Ordovician|Lake George Basin. Strongly folded Ordovician bedrock beneath Lake George.||||Overlain unconformably by Gearys Gap Formation.|Strongly folded quartz-rich turbidites; phyllite; metasediment|
15299|Pittman Formation|71069|5|Briefly described|p19, p59, p84|||||||Equivalent to the Abercrombie Formation.|Micaceous, mostly quartz rich, turbiditic sandstone, siltstone, mudstone and chert.|
15299|Pittman Formation|71700|6|Mentioned|CD|||Occurs in the Canberra 1:100k map sheet area.|||Includes the Acton Shale Member.|||
15299|Pittman Formation|73140|6|Mentioned|p495 Fig.3|||Proposed to be superseded and replaced by the Abercrombie Formation.||||||
15299|Pittman Formation|73211|6|Mentioned|p909|Sandbian|late Darriwilian|Canberra region.|464-458Ma|||Overlain by Acton Shale.||
15332|Plug Tank Formation|42144|6|Mentioned|Fig.11 P615|||||||||
15351|Pocket Formation|22857|4|Described|p466 App.1 Tb.A1.6|Ludlovian|Llandovery|Of the Cooleman Plains Group. Mudstone, siltstone, shale, limestone. Max. thickness: >1km.||||||
15351|Pocket Formation|36443|5|Briefly described|map legend|Ludlovian|Llandoverian|Of Cooleman Plains Group. Lithic arenite, siltstone and mudstone. Includes limestone lenses (Spl). Underlies Blue Waterhole Formation. Interfingers with Peppercorn Formation and Cooleman Limestone. BMR map code: Sps.||||||
15351|Pocket Formation|39409|6|Mentioned|Table XVII|||||||||
15351|Pocket Formation|45147|2|Defined|M85|early Ludlovian|Wenlockian|Late ? Llandoverian to Early ? Ludlovian||||||
15351|Pocket Formation|68592|5|Briefly described|p92|Silurian|Silurian|In Tantangara and Brindabella 1:100 000 map areas. Part of a mid to late Silurian quartzose clastic and carbonate succession, which the Long Plain Fault has juxtaposed against the partly coeval Goobarragandra Volcanics.||||||
15389|Pokolbin Limestone|39263|6|Mentioned|p152|||Usage pre-empted by Pokolbin Hills Volcanics||||||
15389|Pokolbin Limestone|39307|6|Mentioned|p438|||See also photo 22.1,22.2||||||
15389|Pokolbin Limestone|41275|6|Mentioned|p27|||||||||
15389|Pokolbin Limestone|41514|6|Mentioned|p80|||||||||
15389|Pokolbin Limestone|43050|5|Briefly described|p29|||||||||
15418|Pollwombra Granodiorite|35248|6|Mentioned|Fig.1|||||||||
15430|Poolamacca Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
15430|Poolamacca Group|22772|5|Briefly described|p53,Fig13.1p63|Cryogenian|Cryogenian|||||||
15430|Poolamacca Group|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Neoproterozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb. A1.3.||||||
15430|Poolamacca Group|29864|6|Mentioned|p263|||||||||
15430|Poolamacca Group|30261|4|Described|Table 1|||Willouran age||||||
15430|Poolamacca Group|31012|6|Mentioned|p8|||Adelaidean. Lithology.||||||
15430|Poolamacca Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15430|Poolamacca Group|33004|6|Mentioned|p134|||||||||
15430|Poolamacca Group|34812|6|Mentioned|p4|||||||||
15430|Poolamacca Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
15430|Poolamacca Group|36411|6|Mentioned|p269|||Refs Cooper et al. 1978 for definition.||||||
15430|Poolamacca Group|36733|6|Mentioned|Table 5|||||||||
15430|Poolamacca Group|37854|6|Mentioned|Table 1|||||||||
15430|Poolamacca Group|37931|6|Mentioned|p531|||||||||
15430|Poolamacca Group|38157|6|Mentioned|Table II|||||||||
15430|Poolamacca Group|38794|5|Briefly described|p234|||||||||
15430|Poolamacca Group|38969|6|Mentioned|p199|||||||||
15430|Poolamacca Group|39214|6|Mentioned|Table 1|||||||||
15430|Poolamacca Group|39652|6|Mentioned|p78|||||||||
15430|Poolamacca Group|39885|6|Mentioned|p427|||||||||
15430|Poolamacca Group|40294|6|Mentioned|Table 2|||||||||
15430|Poolamacca Group|40595|6|Mentioned|p77|||||||||
15430|Poolamacca Group|41403|5|Briefly described|p50|||||||||
15430|Poolamacca Group|41405|6|Mentioned|p203|||||||||
15430|Poolamacca Group|42223|6|Mentioned|Fig.2 P36|||||||||
15430|Poolamacca Group|42531|5|Briefly described|Map legend|Adelaidean||||||||
15430|Poolamacca Group|42982|5|Briefly described|Table 1,p333|||||||||
15430|Poolamacca Group|43263|6|Mentioned|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43265|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43268|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|43269|5|Briefly described|Map Legend||Neoproterozoic|||||||
15430|Poolamacca Group|44093|5|Briefly described|p139 App. 1|Early Paleozoic|Neoproterozoic|Geological Province: Adelaide Fold Belt.||||||07-NOV-08
15430|Poolamacca Group|62724|5|Briefly described|p17 Fig. 4, p21|Willouran|Willouran|Includes Wilangee Volcanics, Boco Formation, Christine Judith Conglomerate and Lady Don Quartzite. Geological Province: Broken Hill Domain/Curnamona Province (NSW).||||||07-FEB-11
15430|Poolamacca Group|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|New South Wales equivalent of Poolamacca Group of South Australia. Basal quartzite and conglomerate, carbonate and basalt.||||||10-SEP-07
15430|Poolamacca Group|70000|5|Briefly described|p33-34, p39|Tonian|Tonian|Represents initial sedimentation in the Adelaide Rift Complex. Uplifted and eroded during Sturtian tectonism.|||Includes Pintapah and Wendalpa Subgroups.|Unit in Adelaide Rift Complex.|Fluviatile to shallow marine, mature sandstone and lesser conglomerate; followed by stromatolitic limestone; then a cover of continental flood basalt.|
15430|Poolamacca Group|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.|||Includes Pintapah and Wendalpa Subgroups.||Quartzite to quartz-rich conglomerate overlain by sandstone, limestone and basalt.|
15430|Poolamacca Group|72461|5|Briefly described|p13, p16||||||Includes the Pintapah Subgroup and the Wendalpa Subgroup.|||
15448|Pooraka Formation|10010|6|Mentioned|p14 Fig. 5e|||Geological Province: Murray Basin. Reworked colluvial outwash fans material.||||||13-AUG-07
15448|Pooraka Formation|22887|3|Fully described|p50|Late Pleistocene|Late Pleistocene|||||||
15448|Pooraka Formation|23054|6|Mentioned|p30|||||||||
15448|Pooraka Formation|23252|5|Briefly described|Map Legend||Pleistocene|||||||
15448|Pooraka Formation|23489|5|Briefly described|p43 Table 1|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|23719|4|Described|p29|Late Pleistocene|Late Pleistocene|See also page 30 table 9. Overlying unit Wiabuna Formation. Underlying unit Gibbon Beds. Max. thickness 5 m.||||||14-NOV-13
15448|Pooraka Formation|23818|4|Described|p212 Fig.108, p224|Late Pleistocene|Late Pleistocene|Geological Province: St. Vincent Basin. Overlying unit: Saint Kilda Formation. Underlying units: Hindmarsh Clay and Ripon Calcrete. Max. thickness: 20 ft.||||||18-APR-05
15448|Pooraka Formation|23887|6|Mentioned|p205|||||||||
15448|Pooraka Formation|24176|5|Briefly described|p21, p22 Tb. 1|Late Pleistocene|Late Pleistocene|Reddish clay-sand with lime horizon (Loveday Soil) near top.  Geological Province: Mount Painter Province.||||||
15448|Pooraka Formation|24484|5|Briefly described|p805|Quaternary|Quaternary|Max. Thickness: 10m.||||||
15448|Pooraka Formation|24566|5|Briefly described|p111, p114 Fig. 8|||Includes the Wilkatana fanglomerates.  Boulder conglomerates. Overlies Port Willunga Formation. Age: ca130-120Ka.||||||
15448|Pooraka Formation|29697|5|Briefly described|Table 3|||||||||
15448|Pooraka Formation|30055|6|Mentioned|p152|||||||||
15448|Pooraka Formation|30056|6|Mentioned|p148|||||||||
15448|Pooraka Formation|30176|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|30750|6|Mentioned|p3|||Upper Pleistocene age.||||||
15448|Pooraka Formation|30753|6|Mentioned|p15|||||||||
15448|Pooraka Formation|30754|4|Described|p35|||Stratigraphic table p22.||||||09-SEP-22
15448|Pooraka Formation|30756|6|Mentioned|p4|||||||||
15448|Pooraka Formation|30757|6|Mentioned|p2|||||||||
15448|Pooraka Formation|30758|6|Mentioned|p67|||Important source of fine aggregate & clay, P69||||||
15448|Pooraka Formation|30802|6|Mentioned|p10|||Pleistocene age||||||
15448|Pooraka Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
15448|Pooraka Formation|30924|6|Mentioned|Map legend|Recent|Pleistocene|Pleistocene - Recent||||||
15448|Pooraka Formation|31895|4|Described|p411|||Radiocarbon age||||||
15448|Pooraka Formation|31921|6|Mentioned|p6|||See also Fig.3||||||
15448|Pooraka Formation|31966|6|Mentioned|p6|||Equivalent mentioned||||||
15448|Pooraka Formation|32432|6|Mentioned|Fig.2|||See also Table 1||||||
15448|Pooraka Formation|32547|4|Described|p60|||Quaternary||||||
15448|Pooraka Formation|33422|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
15448|Pooraka Formation|33423|6|Mentioned|p14|||Strat.||||||
15448|Pooraka Formation|33557|6|Mentioned|Fig.2|||Map of Gawler Range Volcanic Complex||||||
15448|Pooraka Formation|33834|6|Mentioned|p16|||||||||
15448|Pooraka Formation|34069|6|Mentioned|Fig.3|||||||||
15448|Pooraka Formation|34180|5|Briefly described|p224|||See also P212||||||
15448|Pooraka Formation|34181|4|Described|p46|||See also pp57,53. Pleistocene||||||22-DEC-21
15448|Pooraka Formation|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|34758|6|Mentioned|Table 1|||||||||
15448|Pooraka Formation|35097|6|Mentioned|Fig.4|||||||||
15448|Pooraka Formation|35159|5|Briefly described|p12|||See also Fig.2.||||||
15448|Pooraka Formation|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|35232|5|Briefly described|Table.4|||||||||
15448|Pooraka Formation|35673|6|Mentioned|Fig.1|||Location plan, Para Hills quartzite quarry.||||||
15448|Pooraka Formation|35772|6|Mentioned|p13|||||||||
15448|Pooraka Formation|35905|6|Mentioned|p2|||||||||
15448|Pooraka Formation|36621|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36626|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36834|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|36835|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|37853|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|38068|5|Briefly described|p76|||See also P77.||||||
15448|Pooraka Formation|38107|6|Mentioned|Fig.2|||||||||
15448|Pooraka Formation|38605|6|Mentioned|p40|||||||||
15448|Pooraka Formation|39349|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|39351|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
15448|Pooraka Formation|39352|6|Mentioned|Map legend|late Holocene|Pleistocene|Pleistocene to Holocene||||||
15448|Pooraka Formation|40003|5|Briefly described|Table 4|||||||||
15448|Pooraka Formation|40149|6|Mentioned|p122|||||||||
15448|Pooraka Formation|40219|6|Mentioned|p3|||||||||
15448|Pooraka Formation|40439|6|Mentioned|p382|||||||||
15448|Pooraka Formation|40442|6|Mentioned|p37|||See also Fig.23,||||||
15448|Pooraka Formation|40450|6|Mentioned|p67|||||||||
15448|Pooraka Formation|40502|5|Briefly described|p83|||||||||
15448|Pooraka Formation|40910|6|Mentioned|p19|||||||||
15448|Pooraka Formation|40911|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
15448|Pooraka Formation|40914|6|Mentioned|Map legend|Cenozoic|Cenozoic|||||||19-NOV-08
15448|Pooraka Formation|40926|6|Mentioned|Table 3|||||||||
15448|Pooraka Formation|41119|6|Mentioned|p8|||||||||
15448|Pooraka Formation|41151|6|Mentioned|p14|||||||||
15448|Pooraka Formation|41292|6|Mentioned|Fig.1|||||||||
15448|Pooraka Formation|41362|6|Mentioned|p7|||||||||
15448|Pooraka Formation|41506|5|Briefly described|Fig.2|||||||||
15448|Pooraka Formation|41520|5|Briefly described|Fig.5|||||||||
15448|Pooraka Formation|41619|6|Mentioned|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42457|5|Briefly described|p163|||of Firman (1969)||||||
15448|Pooraka Formation|42466|6|Mentioned|Map legend|||||||||
15448|Pooraka Formation|42469|6|Mentioned|p48|||||||||
15448|Pooraka Formation|42475|6|Mentioned|p24|||||||||
15448|Pooraka Formation|42498|5|Briefly described|Map legend|late Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|42499|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42506|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42716|5|Briefly described|Map legend|Pleistocene||||||||
15448|Pooraka Formation|42720|5|Briefly described|map legend|Pleistocene||||||||
15448|Pooraka Formation|42721|6|Mentioned|map legend|Holocene||||||||
15448|Pooraka Formation|42722|6|Mentioned|map legend|Pleistocene|Pleistocene|Presented as an equivalent of this formation.||||||07-APR-05
15448|Pooraka Formation|42733|5|Briefly described|map legend|Quaternary||||||||
15448|Pooraka Formation|42738|5|Briefly described|map legend|Quaternary||||||||
15448|Pooraka Formation|42813|6|Mentioned|p25|||||||||
15448|Pooraka Formation|42966|2|Defined|p211|Late Pleistocene||||||||
15448|Pooraka Formation|43049|5|Briefly described|p27|||||||||
15448|Pooraka Formation|43053|5|Briefly described|Map Legend|Pleistocene|Pleistocene|||||||25-MAY-05
15448|Pooraka Formation|43071|5|Briefly described|p17,Table 3|||||||||
15448|Pooraka Formation|43094|6|Mentioned|p40|||||||||
15448|Pooraka Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
15448|Pooraka Formation|43298|6|Mentioned|Map Legend|Holocene|Pleistocene|||||||
15448|Pooraka Formation|44133|4|Described|p220 Fig. 11.2, 242|Late Pleistocene|Late Pleistocene|Age: ~35,000 BP (Williams 1937b), 30,000-20,000 BP (Belperio and Bateman 1986). Thickness: 450m. Geological Province: Saint Vincent Basin?.||||||22-DEC-21
15448|Pooraka Formation|44188|5|Briefly described|Map Legend|Holocene|Pleistocene|Geological province: Murray Basin. Unconsolidated, red-brown, poorly sorted clayey sand, gravel, conglomerate, breccia; local calcrete intercalations and cappings; in places cemented by ferruginised silicified matrix.||||||15-MAY-08
15448|Pooraka Formation|44660|14|Not recorded|map legend||Pleistocene|Pleistocene, lithology.||||||
15448|Pooraka Formation|49038|4|Described|Table 2|||Briefly described P33||||||
15448|Pooraka Formation|60953|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Gravelly and sandy clay, commonly gypcreted or calcreted.||||||
15448|Pooraka Formation|61070|5|Briefly described|Map Legend|Late Pleistocene|Middle Pleistocene|Alluvial reddish brown and yellowish brown gravelly and sandy clay, silt and sand with soft earthy carbonate.||||||12-JAN-10
15448|Pooraka Formation|61108|5|Briefly described|map legend|Pleistocene|Pleistocene|Gravelly and sandy clay of piedmont slopes and alluvial plains, commonly gypcreted or calcreted.||||||
15448|Pooraka Formation|61964|6|Mentioned|p175, p190|||Geological Province: Murray Basin. See also p192.||||||
15448|Pooraka Formation|62096|5|Briefly described|p288|||Variously referred to as Pooraka Formation I, P.F. !! and P.F. III, as well as various versions of Pooraka Formation gravels - see Pooraka Formation gravels for variations.||||||09-MAY-06
15448|Pooraka Formation|62577|6|Mentioned|p566|Late Pleistocene|Late Pleistocene|Mentioned only in the context of 'Pooraka Formation equivalents' in relation to Germein Bay Formation.  Alluvial deposits||||||
15448|Pooraka Formation|62893|4|Described|Map Legend, p24|Holocene|Pleistocene|Colluvial and fluvial. Forms veneers over locally exposed calcrete. Best developed as an apron around the Cleve Uplands and around granitic inselnergs to the northwest.|||||Dark brown and mottled green gravelly clay, silt, clay and conglomerate.|
15448|Pooraka Formation|64705|5|Briefly described|p80 Fig. 7d (photo)|Quaternary|Quaternary|Age: <120,000a. Sediments.||||||04-DEC-08
15448|Pooraka Formation|65552|6|Mentioned|p6, p27 App.6|Late Pleistocene|Late Pleistocene|Murray Basin unit. Derived from eastern flanks of Mount Lofty Ranges and Flinders Ranges. Hosts some silica sands resources. Mixed aeolian and colluvial deposits or outwash fans comparable with deposits along the margins of the Riverine Plain in NSW.||||||
15448|Pooraka Formation|65901|4|Described|p175-81, p181 Fig.4, p183-6, p183 Fig.5|Pleistocene|Pleistocene|Also called Hookina Creek Formation by Williams (1982). Fluvial. Optically stimulated luminescence age. Younger alluvial sediments, ages ~ 71 - 29 ka (Quigley et al. 2007) are no longer considered part of Pooraka Formation.|132-118 ka (Chen 1991).|||Overlies Taringa Formation. Interfingers with Glanville Formation.|Red/brown sandy clay deposit with occasional gravel lenses.|08-MAR-12
15448|Pooraka Formation|65922|5|Briefly described|p25 Tb. 4, p27|Pleistocene|Pleistocene|Red-brown-yellowish brown gravelly to sandy clay, silt and sand; local soft carbonate. Fluvial surface unit developed around the flanks and within the Gawler Ranges. Small-scale quarrying for aggregate.||||||
15448|Pooraka Formation|68068|5|Briefly described|Map legend|Pleistocene|Pleistocene|Callabonna Sub-basin, Lake Eyre Basin. An equivalent unit is mapped and described. Forms remnant deposits on the upper parts of dissected surfaces and plateaus. Represents a piedmont slope distal deposit.|||||Clay, silt and gravel with minor cobbles; dark yellow to orange to red-brown; upper parts usually fine-grained (silty or clayey) and not gibber clad.|
15448|Pooraka Formation|68126|6|Mentioned|p31|Paleozoic|Paleozoic|||||||
15448|Pooraka Formation|68131|6|Mentioned|p57, p89|Pleistocene|Pleistocene|||||||
15448|Pooraka Formation|68203|5|Briefly described|p9 Fig.6|||Mount Lofty Ranges.|85 +/- 11 ka.|||Overlies and is faulted against Apilla Tillite. Is faulted against Emeroo Quartzite.|Talus breccia overlain by river gravels.|
15448|Pooraka Formation|69019|5|Briefly described|p106 Fig.26, p122.|Pliocene|Pliocene|Of Firman (1966). W of Lake Blanche. Represents a distal piedmont slope deposit. Thickness from <1 to >3 m. Widely varying ages listed.|||||Dark yellow to red-brown clay, silt and gravel with minor cobbles forming remnant deposits on the upper parts of dissected surfaces and plateaus; much lateral facies change.|
15448|Pooraka Formation|69023|5|Briefly described|p128|Holocene|Pleistocene|Defined by Firman (1966); named after the Adelaide suburb of Pooraka. Found to be widespread as sedimentary aprons around the Mount Lofty and Flinders Ranges. Forms remnant deposits on the upper parts of dissected surfaces and plateaus. Variable thickness: <1 to ~3m.||||Unconformably overlies Bulldog Shale.|Clay, silt and gravel with minor cobbles; dark yellow to red-brown; lower parts more clay-rich; well-developed calcareous soil horizons with earthy to pisolitic carbonate or gypsum segregations are common in basal parts.|
15448|Pooraka Formation|69649|5|Briefly described|p33|||Forms an apron of variable thickness over much of eastern CHILDARA.|||||Alluvial, reddish-brown, sandy clay.|
15448|Pooraka Formation|69666|6|Mentioned|p25|||||||||
15448|Pooraka Formation|70333|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|70334|6|Mentioned|p62,65-66|||Alluvial sediments which underlie the Adelaide Plains.||||||
15448|Pooraka Formation|70384|5|Briefly described|Map legend.|Pleistocene|Pleistocene|Piedmont slope distal deposit. Remnants on dissected surfaces and plateaus. Relict 1-5m thick sheets of the lower, gravelly part emerge from rangelands and some intertongue distally with the upper silty/clayey part.|||||Clay, silt, gravel, minor cobbles; dark yellow to orange to red-brown. Upper part mostly silty or clayey, not gibber-clad. High terrace gravels: fluvial, cobble to gravel, well-rounded polymict clasts, coarse sand matrix. Weakly-moderately cemented.|
15448|Pooraka Formation|70660|5|Briefly described|p30, p32|||An alternative name for the Christies Beach Formation.||||||
15448|Pooraka Formation|71129|6|Mentioned|p166|||Of Adelaide Geosyncline.||||||
15448|Pooraka Formation|71317|5|Briefly described|p144|||The sand plains over Pletabinna were previously mapped as Pooraka Formation, however due to the lack of temporal correlation with these sediments and the Pooraka Formation this was not repeated in this study.|||||Clay, sand and carbonate earth, silty with gravel lenses.|
15448|Pooraka Formation|72456|5|Briefly described|Map Legend|Pleistocene|Pleistocene|Marree 1:250k map sheet.|||||Clay, sand and carbonate earth, salty, with gravel lenses.|
15448|Pooraka Formation|72458|6|Mentioned|p4|Quaternary|Pliocene|||||Underlain by Namba Formation.|Gravels and fanglomerates.|
15448|Pooraka Formation|73103|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|73110|5|Briefly described|Map legend.|Pleistocene|Pleistocene||||||Clay, sand and carbonate earth, silty, with gravel lenses.|
15448|Pooraka Formation|73188|5|Briefly described|[See comments]|Late Pleistocene|Late Pleistocene|St Vincent Basin. Geochron is thermoluminescence dating; see Bourman et al. (1997). Interpreted as distal sediments sourced from erosion of the rising Mount Lofty Ranges. Records the last significant uplift on a number of Adelaide's faults. p: 319-320, 323-324, 329, 331, 334-335, 337-338, 345-346, 349, 351, 358-359.|ca 0.125 Ma|||Equivalent to Christies Beach Formation.|Alluvial fans, clay, sand, gravel, and wind-blown sand; lacking ferruginous and siliceous induration.|
15448|Pooraka Formation|73228|6|Mentioned|p51|||||||||
15448|Pooraka Formation|73236|4|Described|p36, p38 p43, p46, p48|Late Pleistocene|Late Pleistocene|Alluvial and slope sediments. Forms prominent alluvial fans along the Eden-Burnside and Para fault scarps. Represented at Hallett Cove only by local channel fills of sandy and pebbly clay with rubbly, nodular calcrete paleosols in the north of the map area.|c. 0.13-0.08 Ma|||Underlain by Keswick Clay. Overlain by Ngankipari Sand.|Red-brown clay, locally pebbly and/or sandy, with incipient calcrete nodules.|
15452|Porcupine Formation|721|5|Briefly described|Map legend|Kungurian|Kungurian|Basal conglomerate passing upward into bioturbated silty sandstone and minor siltstone with dropped pebbles. Geological Province: Gunnedah Basin.||||||07-APR-09
15452|Porcupine Formation|22579|5|Briefly described|p219 Fig.2|Late Permian|Late Permian|||||||
15452|Porcupine Formation|22601|6|Mentioned|413|||Geol province Gunnedah Basin||||||
15452|Porcupine Formation|22857|4|Described|p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of Millie Group. Basal conglomerate rich in felsic volcanic clasts. Max. thickness: >160m. Geological Province: Gunnedah Basin. See also p315 Fig.22.8.||||||
15452|Porcupine Formation|22865|6|Mentioned|Fig22.8p315|||||||||
15452|Porcupine Formation|23050|5|Briefly described|p9 Fig.2, 17|Late Permian|Late Permian|Of Gunnedah Basin.||||||17-SEP-08
15452|Porcupine Formation|23566|5|Briefly described|p116 Fig. 2|Late Permian|Late Permian|Parent: Millie Group. Geological Province: Gunnedah Basin.||||||17-SEP-08
15452|Porcupine Formation|23740|5|Briefly described|p1221|Permian|Permian|Geological Province: Gunnedah Basin||||||
15452|Porcupine Formation|24159|5|Briefly described|p150 Fig.3, p149|Late Permian|Early Permian|Geological Province: Gunnedah Basin. Overlying Unit: Watermark Formation. Underlying Unit: Maules Creek Formation.||||||
15452|Porcupine Formation|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
15452|Porcupine Formation|29870|4|Described|p11|||||||||
15452|Porcupine Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
15452|Porcupine Formation|31882|6|Mentioned|p245|||Fossiliferous. Marine.||||||
15452|Porcupine Formation|31883|6|Mentioned|p594|||See also Table 1||||||
15452|Porcupine Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
15452|Porcupine Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
15452|Porcupine Formation|32944|6|Mentioned|p700|||See also PP702,703,704,710 & Fig.3. U.Perm.||||||
15452|Porcupine Formation|32950|6|Mentioned|p435|||||||||
15452|Porcupine Formation|34043|4|Described|p451|||Fossiliferous, correlated with Maitland Group.||||||
15452|Porcupine Formation|35284|6|Mentioned|p37|||||||||
15452|Porcupine Formation|36940|6|Mentioned|Fig.1|||||||||
15452|Porcupine Formation|36961|6|Mentioned|p210|||See also Fig.3.||||||
15452|Porcupine Formation|37082|6|Mentioned|p161|||||||||
15452|Porcupine Formation|37094|5|Briefly described|p241|||||||||
15452|Porcupine Formation|37856|6|Mentioned|p2|||||||||
15452|Porcupine Formation|38089|4|Described|p9|||||||||
15452|Porcupine Formation|38614|4|Described|p6|||||||||
15452|Porcupine Formation|39063|6|Mentioned|p11|||||||||
15452|Porcupine Formation|39288|5|Briefly described|p64|||||||||
15452|Porcupine Formation|39308|6|Mentioned|Fig. 23.12|||||||||
15452|Porcupine Formation|39468|6|Mentioned|Fig.2|||||||||
15452|Porcupine Formation|39572|6|Mentioned|p143|||||||||
15452|Porcupine Formation|39693|6|Mentioned|p16|||||||||
15452|Porcupine Formation|39913|5|Briefly described|p4|||||||||
15452|Porcupine Formation|40166|6|Mentioned|Table 1|||||||||
15452|Porcupine Formation|40200|4|Described|p5|||||||||
15452|Porcupine Formation|40332|6|Mentioned|Fig.3|||||||||
15452|Porcupine Formation|40680|6|Mentioned|Fig.1|||||||||
15452|Porcupine Formation|40767|4|Described|p4|||Mention Fig.1 and Fig.10||||||
15452|Porcupine Formation|40952|4|Described|p5|||||||||
15452|Porcupine Formation|41264|6|Mentioned|p252|||||||||
15452|Porcupine Formation|41290|5|Briefly described|p225|||||||||
15452|Porcupine Formation|41451|6|Mentioned|p14|||||||||
15452|Porcupine Formation|41689|6|Mentioned|Table 1|||||||||
15452|Porcupine Formation|42182|6|Mentioned|Table 1|||||||||
15452|Porcupine Formation|42284|5|Briefly described|Fig.11 P104|||||||||
15452|Porcupine Formation|42463|6|Mentioned|Fig.6 P173|||||||||
15452|Porcupine Formation|42679|5|Briefly described|Fig.3 P3|||||||||
15452|Porcupine Formation|42767|5|Briefly described|Fig.5|||||||||
15452|Porcupine Formation|43017|5|Briefly described|Fig.2,p374|||||||||
15452|Porcupine Formation|43091|5|Briefly described|Map legend|||of Gunnedah Basin||||||
15452|Porcupine Formation|43194|1|Redefined|p98 Tb. 8.2, p103-105, p118, p133 App. 1|Late Permian|Late Permian|See also references on p95, p97, p100, p101 Fig.8.2, p128, p129 Tb.8.3. Now in Millie Group. Overlies Maules Creek Formation and basement. Underlies Watermark Formation (gradational contact) and Digby Formation. Diachronous: Assigned to Upper Stage 4 in southern Gunnedah Basin; Lower Stage 5b in north.||||||
15452|Porcupine Formation|43384|14|Not recorded|Map Legend||Late Permian|||||||
15452|Porcupine Formation|43385|14|Not recorded|p179||Late Permian|||||||
15452|Porcupine Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition)||||||
15452|Porcupine Formation|43408|14|Not recorded|Map Legend|||Sandstone and conglomerate, some shale and limestone||||||
15452|Porcupine Formation|43409|14|Not recorded|Map Legend|||Marine Permian, 600ft thick. Correlated with Muree Formation (Hunter Valley)||||||
15452|Porcupine Formation|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
15452|Porcupine Formation|45006|14|Not recorded|Tb.1,opp.p3,6,45|||||||||
15452|Porcupine Formation|48600|14|Not recorded|Plate 3|||||||||
15452|Porcupine Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Millie Group. Underlies: Watermark Formation.  Overlies: Maules Creek & Goonbri Formations.||||||05-JUL-04
15452|Porcupine Formation|61313|5|Briefly described|p91, p94 Fig.G7|Early Permian|Early Permian|Strongly bioturbidated silty lithic sandstone, conglomerate and minor siltstone. Conformably overlain by Watermark Formation. Max. thickness: 160m. Geological Province: Gunnedah Basin. See also p95 Fig. G8, p98 Fig. G10||||||
15452|Porcupine Formation|61377|5|Briefly described|p149 Fig. SU8|Early Permian|Early Permian|Geological Province: Gunnedah Basin. See also p154 Fig. SU9.||||||07-FEB-11
15452|Porcupine Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
15452|Porcupine Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Millie Group. Geological Province: Gunnedah Basin. Silty sandstone, conglomerate and siltstone, bioturbated and burrowed, with shell fossil fragments.||||||17-SEP-08
15452|Porcupine Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Gunnedah Basin.||||||
15452|Porcupine Formation|63773|6|Mentioned|p1059|||||||||
15452|Porcupine Formation|63832|5|Briefly described|p131 Fig.2, p136|Roadian|Kungurian|Of Gunnedah Basin. Seventh (P3) glaciation. Dominantly glaciomarine deposits.|||||Dominated by thick intervals of marine diamictites (striated/faceted clasts); interbedded sandstone, conglomerate, diamictite.|13-DEC-17
15452|Porcupine Formation|64631|6|Mentioned|p49.|Roadian|Kungurian|Gunnedah Basin. Distal glaciomarine deposits. See also p44. Biostratigraphic age control for base and top.||||||
15452|Porcupine Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Gunnedah Basin. Overlies the Maules Creek Formation, underlies Watermark Formation||||||22-MAR-12
15452|Porcupine Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Early Permian|Gunnedah Basin. Underlies Watermark Formation.||||||
15452|Porcupine Formation|65114|5|Briefly described|p385 Fig.3|Late Permian|Early Permian|||||||
15452|Porcupine Formation|65115|6|Mentioned|Fig 2 p403|Permian|Permian|Underlies the Watermark Formation, Gunnedah Basin.||||||
15452|Porcupine Formation|65116|4|Described|p444, fig 2 p 436, Fig 6 p441, p449|Late Permian|Early Permian|Underlies the Watermark Formation in the Gunnedah Basin. Bioturbated, poorly sorted silty lithic sandstone and conglomerate.||||||
15452|Porcupine Formation|65118|6|Mentioned|p479 Fig.2.|Permian|Permian|Gunnedah Basin. Is overlain by Watermark Formation. Coeval with Oxtrack Formation (Taroom Trough) and upper Aldebaran Sandstone (Denison Trough), both in the Bowen Basin.||||||
15452|Porcupine Formation|66191|5|Briefly described|p485 Fig.2, p485|Late Permian|Late Permian|Gunnedah Basin. Underlies the Watermark Formation, overlies the Maules Creek Formation. Marine shelf deposits.||||||
15452|Porcupine Formation|68003|5|Briefly described|p38 Fig.3-j, p40, p57 Fig.3-n, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion.||Lower unit in Millie Group.||Overlies Maules Creek Formation. Is overlain by Digby and Watermark Formations.|Basal conglomerate passing upward into bioturbated silty sandstone and minor siltstone with dropped pebbles.|
15452|Porcupine Formation|68004|5|Briefly described|p23 Table 1, p173, p179.|||Gunnedah Basin. Wilga Park-1 flowed gas at a rate of 1.0 MMCFD.||Lower unit in Millie Group.||Overlies Maules Creek Formation. Is overlain by Watermark Formation.||
15452|Porcupine Formation|70791|5|Briefly described|p275, p277-278, p283-288, p292-294|Guadalupian|Guadalupian|Gunnedah Basin. Represents a Basin-wide glacio-marine transgression. Isopachs. Has microflora of APP32 to APP42 age.||Millie Group.||Disconformably overlies Leard Formation, Boggabri Volcanics, Werrie Basalt.|Pebble to cobble paraconglomerate with a grey lithic sandstone and mudstone matrix; clasts mostly felsic volcanics; bioturbation, sulfur-staining and marine fossils abundant throughout.|
15452|Porcupine Formation|70878|5|Briefly described|p718 Fig.13|Permian|Permian|Gunnedah Basin.||Millie Group.||Overlies Maules Creek Formation (Bellata Group). Is overlain by Watermark Formation.||
15452|Porcupine Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Is overlain by Watermark Formation.||
15493|Postmans Creek Granodiorite|33476|2|Defined|p58|Triassic|Permian|Permian - Triassic||||||
15493|Postmans Creek Granodiorite|33766|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
15493|Postmans Creek Granodiorite|37252|6|Mentioned|Map legend|Triassic|Permian|Permian-Triassic||||||
15493|Postmans Creek Granodiorite|43008|5|Briefly described|map legend|||||||||
15493|Postmans Creek Granodiorite|71628|5|Briefly described|p11:11; p19:18|||Has been identified as a fragment of the Dundee Rhyodacite (Blevin, pers. comm., 2014).||||Is intruded by Blake Snake Creek Granite.||
15493|Postmans Creek Granodiorite|72528|6|Mentioned|p78.|Lopingian|Lopingian|Of Thomson 1976. This unit has been reclassified as a fragment of the Dundee Rhyodacite (Bryant, 2017).||||Intruded by Black Snake Creek Granite.||
15497|Potosi Gneiss|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
15497|Potosi Gneiss|22961|6|Mentioned|p80||Paleoproterozoic|||||||07-NOV-08
15497|Potosi Gneiss|23461|5|Briefly described|p202|||||||||
15497|Potosi Gneiss|32657|6|Mentioned|p117|||||||||
15497|Potosi Gneiss|33262|5|Briefly described|PB222|||||||||
15497|Potosi Gneiss|35170|6|Mentioned|Fig.2|||||||||
15497|Potosi Gneiss|37461|6|Mentioned|p321|||||||||
15497|Potosi Gneiss|37581|6|Mentioned|p74|||||||||
15497|Potosi Gneiss|39883|6|Mentioned|p381|||||||||
15497|Potosi Gneiss|40448|6|Mentioned|p30|||||||||
15497|Potosi Gneiss|40852|5|Briefly described|p23|||||||||
15497|Potosi Gneiss|41145|6|Mentioned|Fig.5|||||||||
15497|Potosi Gneiss|41633|6|Mentioned|Fig.2.7|||||||||
15497|Potosi Gneiss|41870|6|Mentioned|p120|||||||||
15497|Potosi Gneiss|43610|6|Mentioned|p19|||1690+/-5 Ma (Zircon U-Pb)||||||
15497|Potosi Gneiss|45003|14|Not recorded|p333|||||||||
15497|Potosi Gneiss|45166|5|Briefly described|p25|||||||||
15497|Potosi Gneiss|46597|14|Not recorded|p187|||||||||
15497|Potosi Gneiss|46601|14|Not recorded|p.320,323|||Fig.7.||||||
15497|Potosi Gneiss|64316|5|Briefly described|p533 Fig. 1|||Reference also made to 'Possi-type gneiss'.  Geological Province: Broken Hill Block. This is a garnet-rich variant of the Hores Gneiss.||||||07-FEB-11
15497|Potosi Gneiss|64896|6|Mentioned|p1392 Fig. 3|||Geological Province: Curnamona Province.||||||
15497|Potosi Gneiss|68126|6|Mentioned|p26|||Apparently related to a c.1690 Ma thermal event.||||||
15512|Potts Hill Sandstone Member|35690|6|Mentioned|Fig.1.3|||||||||
15512|Potts Hill Sandstone Member|40602|5|Briefly described|p26|||||||||
15512|Potts Hill Sandstone Member|42896|5|Briefly described|Fig.8|||of Bringelly Shale||||||
15540|Precipice Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p496, p498|Early Jurassic|Early Jurassic|N Surat and Mulgildie Basins. 40-150m thick in Surat Basin; 60-150m thick in Mulgildie Basin.|||||Mainly quartzose sandstone, becoming finer upwards with minor siltstone bands.|
15540|Precipice Sandstone|13516|5|Briefly described|p159 fig 8, p163, 166,167, 168, 169 p139|Early Jurassic|Early Jurassic|From Callide Basin, Surat Basin, Eromanga Basin. Age of base varies across Surat Basin.||||||
15540|Precipice Sandstone|22482|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|22757|5|Briefly described|Table6,p12|Early Jurassic|Early Jurassic|200 m.||||||
15540|Precipice Sandstone|22865|4|Described|p295,Table22.1p296-7|Sinemurian|Early Jurassic|||||||
15540|Precipice Sandstone|22975|5|Briefly described|p34 Fig.6|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22976|5|Briefly described|p42 Fig.4|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22977|5|Briefly described|p67 Fig.2|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22980|5|Briefly described|p249 Fig.2|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|22981|5|Briefly described|p259|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|23037|5|Briefly described|p34,117||Jurassic|Underlain by Torsdale Volcanics.||||||14-FEB-07
15540|Precipice Sandstone|23050|5|Briefly described|p9 Fig.2, 17|Jurassic|Jurassic|of Surat Basin.||||||
15540|Precipice Sandstone|23053|6|Mentioned|Fig10p17|Sinemurian||||||||
15540|Precipice Sandstone|23056|6|Mentioned|8 table 1A|||||||||
15540|Precipice Sandstone|23425|6|Mentioned|p391.|||||||||
15540|Precipice Sandstone|23799|3|Fully described|p50, p10 Tb. 1|Early Jurassic|Early Jurassic|Part of this group was previously mapped as Marburg Subgroup.  See also p48 Fig. 3.  Overlain by Evergreen Formation; unconformably overlies parts of Chahpingah Meta-Igneous and Boondooma Igneous Complexes.   Max. thickness: >50m.Geol. Prov: Surat Basin.||||||
15540|Precipice Sandstone|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
15540|Precipice Sandstone|23841|5|Briefly described|p448|Early Jurassic|Early Jurassic|Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|23883|5|Briefly described|p129 Fig. 11.2|Early Jurassic|Early Jurassic|Geological Province: Great Australian Superbasin.||||||
15540|Precipice Sandstone|23982|5|Briefly described|p35 Fig. 7|Jurassic|Jurassic|Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|24068|4|Described|p269|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.  Maximum thickness: 180m.||||||
15540|Precipice Sandstone|24069|5|Briefly described|p284|Early Jurassic|Early Jurassic|Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|24092|5|Briefly described|p7|||Geological Province: Great Artesian Basin.||||||
15540|Precipice Sandstone|24159|5|Briefly described|p148 Fig.2, p151|Early Jurassic|Early Jurassic|Geological Province: Surat Basin. Overlying Unit: Evergreen Formation. Underlying Unit: unconformity with Moolayember Formation.||||||
15540|Precipice Sandstone|24236|5|Briefly described|p364|Jurassic|Jurassic|Overlies Callide Coal Measures. Geological Province: Callide Basin.||||||
15540|Precipice Sandstone|24241|5|Briefly described|p19 Fig.4|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24488|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24489|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24491|5|Briefly described|p12|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|24615|5|Briefly described|CD|Jurassic|Jurassic|[Jp].  Thick-bedded, cross-bedded, fine- to coarse-grained pebbly quartzose sandstone, and minor lithic sublabile sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|29385|6|Mentioned|p80|||Other references on P81,82. Jurassic.||||||
15540|Precipice Sandstone|29387|6|Mentioned|p30|||See also Table 5.||||||
15540|Precipice Sandstone|29389|6|Mentioned|p19|||Early Jurassic.||||||
15540|Precipice Sandstone|29393|6|Mentioned|Table 4|||Jurassic.||||||
15540|Precipice Sandstone|29394|6|Mentioned|p145|||||||||
15540|Precipice Sandstone|29410|6|Mentioned|p274|||Geological map. Jurassic.||||||
15540|Precipice Sandstone|29411|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|29532|6|Mentioned|p15|||||||||
15540|Precipice Sandstone|29537|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|29539|6|Mentioned|p8|||Drilling.||||||
15540|Precipice Sandstone|29540|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|29541|6|Mentioned|p9|||Drilling.||||||
15540|Precipice Sandstone|29591|6|Mentioned|p69|||||||||
15540|Precipice Sandstone|29721|6|Mentioned|p76|||||||||
15540|Precipice Sandstone|29961|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|29964|6|Mentioned|p5|||Jurassic||||||
15540|Precipice Sandstone|29967|6|Mentioned|p118|||||||||
15540|Precipice Sandstone|30102|6|Mentioned|p17|||Correlation with basal Hutton Sandstone.||||||
15540|Precipice Sandstone|30103|6|Mentioned|p10|||||||||
15540|Precipice Sandstone|30232|4|Described|p667,668,672-679||Early Jurassic|||||||
15540|Precipice Sandstone|30451|3|Fully described|p70|||See alsp p71. Early Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30455|6|Mentioned|p5|||See also P13. Jurassic age||||||
15540|Precipice Sandstone|30456|6|Mentioned|p95|||||||||
15540|Precipice Sandstone|30457|6|Mentioned|p96|||||||||
15540|Precipice Sandstone|30458|6|Mentioned|p3|||Jurassic age||||||
15540|Precipice Sandstone|30460|6|Mentioned|p5|||See also P13. Jurassic age||||||
15540|Precipice Sandstone|30462|6|Mentioned|p356|||||||||
15540|Precipice Sandstone|30464|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|30465|6|Mentioned|p4|||||||||
15540|Precipice Sandstone|30466|6|Mentioned|p40|||See also P5. Jurassic age||||||
15540|Precipice Sandstone|30469|6|Mentioned|p273|||||||||
15540|Precipice Sandstone|30471|6|Mentioned|p131|||||||||
15540|Precipice Sandstone|30472|6|Mentioned|p132|||Pollen distribution||||||
15540|Precipice Sandstone|30474|6|Mentioned|p249|||Proposed to include upper sandstone sequence of Callide Coal Measures.||||||
15540|Precipice Sandstone|30475|6|Mentioned|p168|||||||||
15540|Precipice Sandstone|30508|6|Mentioned|p91|||Productive formation||||||
15540|Precipice Sandstone|30691|4|Described|p6|||See also p15,19,20,21,Table 4. Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30692|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30694|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30695|4|Described|Table 3|||Lower Jurassic age||||||
15540|Precipice Sandstone|30696|4|Described|Table 4|||Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|30699|6|Mentioned|p53|||Early Jurassic age||||||
15540|Precipice Sandstone|30700|6|Mentioned|p22|||Map. Lower Jurassic age||||||
15540|Precipice Sandstone|30701|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|30702|6|Mentioned|Fig.1|||See Stratigraphic Table||||||
15540|Precipice Sandstone|30854|4|Described|Table 4|||Lower Jurassic age||||||
15540|Precipice Sandstone|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|30915|6|Mentioned|p98|||||||||
15540|Precipice Sandstone|30916|6|Mentioned|p98|||On table||||||
15540|Precipice Sandstone|31115|6|Mentioned|p32|||||||||
15540|Precipice Sandstone|31116|4|Described|p20|||See also p10. Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|31117|5|Briefly described|p379|||Lithology. Jurassic||||||
15540|Precipice Sandstone|31118|6|Mentioned|p311|||Part of Bundamba Gp. by Whitehouse (1954)||||||
15540|Precipice Sandstone|31120|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|31304|5|Briefly described|p628|||Lithology in drill hole.||||||
15540|Precipice Sandstone|31305|6|Mentioned|Fig. 1|||||||||
15540|Precipice Sandstone|31369|4|Described|p40|||See also p41-44. L.Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|31398|6|Mentioned|p268|||L.Jurassic.||||||
15540|Precipice Sandstone|31438|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|31656|6|Mentioned|p8|||Unconformable on Clematis Sst.||||||
15540|Precipice Sandstone|31659|6|Mentioned|p74|||L.Jurassic||||||
15540|Precipice Sandstone|32038|4|Described|p428|||See also p429, 437. Early Jurassic.||||||14-FEB-07
15540|Precipice Sandstone|32039|6|Mentioned|p115|||L.Jurassic. See also P119,120.||||||
15540|Precipice Sandstone|32040|6|Mentioned|p885|||Stratigraphic sequence||||||
15540|Precipice Sandstone|32136|6|Mentioned|p1|||Refers Reiser & Williams (1969)||||||
15540|Precipice Sandstone|32137|6|Mentioned|p357|||||||||
15540|Precipice Sandstone|32182|4|Described|p1|||Jurassic||||||
15540|Precipice Sandstone|32193|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32276|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32493|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32496|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|32712|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|32715|6|Mentioned|p1186|||Oil||||||
15540|Precipice Sandstone|32797|4|Described|Table 4|||L.Jur.||||||
15540|Precipice Sandstone|33059|4|Described|p311|||L.Jur.||||||
15540|Precipice Sandstone|33071|4|Described|p6|||L.Jur.||||||
15540|Precipice Sandstone|33078|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33079|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33088|4|Described|Table 3|||L.Jur.||||||
15540|Precipice Sandstone|33090|4|Described|Table 4|||L.Jur.||||||
15540|Precipice Sandstone|33091|6|Mentioned|p10|||Stratigraphy||||||
15540|Precipice Sandstone|33094|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33192|6|Mentioned|p21|||||||||
15540|Precipice Sandstone|33367|5|Briefly described|Table 1|||||||||
15540|Precipice Sandstone|33381|6|Mentioned|Table 1|||L.Jur.||||||
15540|Precipice Sandstone|33449|6|Mentioned|p6|||L.Jur.||||||
15540|Precipice Sandstone|33451|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|33530|5|Briefly described|Table 1|||Lower Jur.||||||
15540|Precipice Sandstone|33639|6|Mentioned|p10|||||||||
15540|Precipice Sandstone|33672|6|Mentioned|p41|||||||||
15540|Precipice Sandstone|33673|4|Described|p291|||||||||
15540|Precipice Sandstone|33675|4|Described|p412|||Lithology.||||||
15540|Precipice Sandstone|33774|3|Fully described|p46|||See also p24||||||14-FEB-07
15540|Precipice Sandstone|33971|6|Mentioned|p41|||Petroleum. Surat Basin.||||||
15540|Precipice Sandstone|34061|6|Mentioned|p54|||||||||
15540|Precipice Sandstone|34133|6|Mentioned|p1|||See also PP3,4,28. Jurassic.||||||
15540|Precipice Sandstone|34134|6|Mentioned|Cor.Chart|||Lower Jurassic.||||||
15540|Precipice Sandstone|34172|6|Mentioned|p53|||Jurassic.||||||
15540|Precipice Sandstone|34174|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|34212|6|Mentioned|p1|||Jurassic. See also PP2,3,4,5,etc.||||||
15540|Precipice Sandstone|34254|6|Mentioned|p481, p489|||Early Jurassic||||||
15540|Precipice Sandstone|34287|6|Mentioned|p170|||Jurassic. See also P173||||||
15540|Precipice Sandstone|34452|6|Mentioned|p1|||L.Jurassic. Palynology. See also PP2,3,4 etc||||||
15540|Precipice Sandstone|34613|4|Described|Table 4|||||||||
15540|Precipice Sandstone|35079|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|35148|4|Described|p415|||See also Table 1 and Fig.1.||||||
15540|Precipice Sandstone|35157|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|35560|6|Mentioned|p288|||||||||
15540|Precipice Sandstone|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
15540|Precipice Sandstone|35574|4|Described|Table 1|||Stratigraphic table - Surat Basin after Exon 1976.||||||
15540|Precipice Sandstone|35811|5|Briefly described|Table 5|||||||||
15540|Precipice Sandstone|35901|6|Mentioned|p17|||||||||
15540|Precipice Sandstone|35937|6|Mentioned|Fig.5|||||||||
15540|Precipice Sandstone|36103|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|36111|6|Mentioned|p34|||||||||
15540|Precipice Sandstone|36233|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|36235|3|Fully described|p181|||See also Fig.1.||||||
15540|Precipice Sandstone|36236|6|Mentioned|p183|||||||||
15540|Precipice Sandstone|36243|6|Mentioned|p74|||See also Table 6A.||||||
15540|Precipice Sandstone|36331|6|Mentioned|p3|||See also P24, 31, 53||||||
15540|Precipice Sandstone|36333|6|Mentioned|Map legend|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|36570|6|Mentioned|p26, p55|||See also Table 1.||||||
15540|Precipice Sandstone|36739|6|Mentioned|p4|||||||||
15540|Precipice Sandstone|36751|6|Mentioned|p387|||||||||
15540|Precipice Sandstone|36825|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|36905|4|Described|p17|||||||||
15540|Precipice Sandstone|36917|6|Mentioned|p151|||||||||
15540|Precipice Sandstone|36926|6|Mentioned|p176|||||||||
15540|Precipice Sandstone|37117|5|Briefly described|p313|||||||||
15540|Precipice Sandstone|37119|5|Briefly described|p318|||||||||
15540|Precipice Sandstone|37288|6|Mentioned|p41|||||||||
15540|Precipice Sandstone|37463|6|Mentioned|p483|||||||||
15540|Precipice Sandstone|37705|6|Mentioned|Fig.1|||||||||
15540|Precipice Sandstone|37749|6|Mentioned|p194|||||||||
15540|Precipice Sandstone|37995|4|Described|p62|||||||||
15540|Precipice Sandstone|37996|4|Described|p71|||||||||
15540|Precipice Sandstone|38064|6|Mentioned|42|||||||||
15540|Precipice Sandstone|38067|6|Mentioned|p59|||||||||
15540|Precipice Sandstone|38226|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|38358|6|Mentioned|p1|||||||||
15540|Precipice Sandstone|38447|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|38801|6|Mentioned|p129|||||||||
15540|Precipice Sandstone|39070|4|Described|p362|||||||||
15540|Precipice Sandstone|39212|4|Described|p15|||p24 petroleum reservoir. p25 aquifer. See alsopP37.||||||14-FEB-07
15540|Precipice Sandstone|39315|6|Mentioned|Fig.5|||||||||
15540|Precipice Sandstone|39445|5|Briefly described|Table 10|||||||||
15540|Precipice Sandstone|39478|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|39494|6|Mentioned|p137|||||||||
15540|Precipice Sandstone|39632|6|Mentioned|p209|||||||||
15540|Precipice Sandstone|39815|6|Mentioned|p444|||||||||
15540|Precipice Sandstone|39907|6|Mentioned|p8|||||||||
15540|Precipice Sandstone|39943|6|Mentioned|Table 8A|||||||||
15540|Precipice Sandstone|40030|6|Mentioned|p135|||||||||
15540|Precipice Sandstone|40090|6|Mentioned|p83|||||||||
15540|Precipice Sandstone|40094|6|Mentioned|p23|||||||||
15540|Precipice Sandstone|40115|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|40120|6|Mentioned|p429|||||||||
15540|Precipice Sandstone|40121|6|Mentioned|p446|||||||||
15540|Precipice Sandstone|40245|6|Mentioned|Table 2|||||||||
15540|Precipice Sandstone|40249|6|Mentioned|p38|||||||||
15540|Precipice Sandstone|40250|4|Described|p29|||||||||
15540|Precipice Sandstone|40539|6|Mentioned|Fig.2|||||||||
15540|Precipice Sandstone|40540|6|Mentioned|p150|||||||||
15540|Precipice Sandstone|40541|3|Fully described|p108|||||||||
15540|Precipice Sandstone|40544|6|Mentioned|p161|||||||||
15540|Precipice Sandstone|40623|5|Briefly described|p72|||||||||
15540|Precipice Sandstone|40666|4|Described|p355|||||||||
15540|Precipice Sandstone|40675|6|Mentioned|Table 8A|||||||||
15540|Precipice Sandstone|40687|6|Mentioned|Table 3|||||||||
15540|Precipice Sandstone|40767|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|40832|3|Fully described|p254|||||||||
15540|Precipice Sandstone|41060|6|Mentioned|p2|||See also Fig.3||||||
15540|Precipice Sandstone|41061|6|Mentioned|p19|||||||||
15540|Precipice Sandstone|41064|6|Mentioned|p60|||||||||
15540|Precipice Sandstone|41097|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|41159|6|Mentioned|Fig.4|||||||||
15540|Precipice Sandstone|41177|6|Mentioned|Fig.2|||||||||
15540|Precipice Sandstone|41187|6|Mentioned|p217|||||||||
15540|Precipice Sandstone|41188|5|Briefly described|p232|||||||||
15540|Precipice Sandstone|41198|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|41210|6|Mentioned|p157|||||||||
15540|Precipice Sandstone|41211|6|Mentioned|p181|||||||||
15540|Precipice Sandstone|41216|6|Mentioned|p305|||||||||
15540|Precipice Sandstone|41246|6|Mentioned|Map legend|Jurassic||||||||
15540|Precipice Sandstone|41247|6|Mentioned|p127|||||||||
15540|Precipice Sandstone|41266|6|Mentioned|Fig.3|||||||||
15540|Precipice Sandstone|41725|6|Mentioned|p400|||||||||
15540|Precipice Sandstone|41893|6|Mentioned|p514|||||||||
15540|Precipice Sandstone|41992|4|Described|Fig.2 P183|||||||||
15540|Precipice Sandstone|42007|5|Briefly described|Fig.2 P182|||||||||
15540|Precipice Sandstone|42067|4|Described|Apendix 2|||See also p311||||||14-FEB-07
15540|Precipice Sandstone|42250|6|Mentioned|p28|||||||||
15540|Precipice Sandstone|42370|5|Briefly described|Fig.3 P317|||||||||
15540|Precipice Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
15540|Precipice Sandstone|42493|5|Briefly described|p17, Fig.1 p18|||||||||
15540|Precipice Sandstone|42547|5|Briefly described|p46|||Jurassic.||||||
15540|Precipice Sandstone|42618|6|Mentioned|p14|||||||||
15540|Precipice Sandstone|42634|6|Mentioned|p12|||Jurassic.||||||
15540|Precipice Sandstone|42865|6|Mentioned|p18|||||||||
15540|Precipice Sandstone|42911|5|Briefly described|p13|||||||||
15540|Precipice Sandstone|43000|5|Briefly described|p109|||see also Fig.5,p112||||||
15540|Precipice Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
15540|Precipice Sandstone|43004|5|Briefly described|Table 1,p179|||||||||
15540|Precipice Sandstone|43108|5|Briefly described|p34|||||||||
15540|Precipice Sandstone|43185|6|Mentioned|6||Jurassic|||||||
15540|Precipice Sandstone|43462|14|Not recorded|p15|||||||||
15540|Precipice Sandstone|43582|6|Mentioned|Fig.5,p16||Early Jurassic|||||||
15540|Precipice Sandstone|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
15540|Precipice Sandstone|43714|6|Mentioned|Fig.3,p5||Early Jurassic|||||||
15540|Precipice Sandstone|43851|14|Not recorded|Tb p106,111||Early Jurassic|||||||
15540|Precipice Sandstone|43878|14|Not recorded|p85,86|||||||||
15540|Precipice Sandstone|43883|14|Not recorded|p18,19,21|||||||||
15540|Precipice Sandstone|43910|14|Not recorded|p5,19,20|||Correlated with Bundamba Group.||||||
15540|Precipice Sandstone|43912|14|Not recorded|p2,4,5,7|||||||||
15540|Precipice Sandstone|43915|14|Not recorded|p179|||||||||
15540|Precipice Sandstone|43916|14|Not recorded|p2479,2481||Jurassic|||||||
15540|Precipice Sandstone|43923|6|Mentioned|p1||Early Jurassic|||||||
15540|Precipice Sandstone|43924|14|Not recorded|p1,2,15||Lias|(Liassic)||||||
15540|Precipice Sandstone|43925|14|Not recorded|p31,37,48-50,Figs3,4|||||||||
15540|Precipice Sandstone|43960|14|Not recorded|p9,12||Jurassic|||||||
15540|Precipice Sandstone|43977|14|Not recorded|p576|||||||||
15540|Precipice Sandstone|43982|14|Not recorded|Map Legend|||||||||
15540|Precipice Sandstone|43989|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|43990|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|43993|14|Not recorded|p94,95,102|||Ref. to Whitehouse 1955. Equivalent to Helidon Sandstone.||||||
15540|Precipice Sandstone|43994|14|Not recorded|Map Legend|||||||||
15540|Precipice Sandstone|43995|14|Not recorded|p57,58|||Part of Bundamba Group.||||||
15540|Precipice Sandstone|43997|14|Not recorded|p114|||||||||
15540|Precipice Sandstone|43998|4|Described|p14,17,map||Early Jurassic|||||||
15540|Precipice Sandstone|44022|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|44023|4|Described|Tb.3,p10||Early Jurassic|||||||
15540|Precipice Sandstone|44026|14|Not recorded|p122,123|||||||||
15540|Precipice Sandstone|44028|14|Not recorded|Fig.2,p512||Jurassic|||||||
15540|Precipice Sandstone|44031|14|Not recorded|p9-11|||Artesian water.||||||
15540|Precipice Sandstone|44032|14|Not recorded|p462,464|||||||||
15540|Precipice Sandstone|44034|6|Mentioned|Tb.1|||||||||
15540|Precipice Sandstone|44084|14|Not recorded|p20,22,24,26,32||Early Jurassic|||||||
15540|Precipice Sandstone|44091|14|Not recorded|p54||Jurassic|||||||
15540|Precipice Sandstone|44095|2|Defined|p284-5|||||||||
15540|Precipice Sandstone|44116|14|Not recorded|p24,28,33|||||||||
15540|Precipice Sandstone|44118|14|Not recorded|Map Legend||Jurassic|||||||
15540|Precipice Sandstone|44124|14|Not recorded|p2,5,10,15-16|||||||||
15540|Precipice Sandstone|44163|4|Described|p1,2,10-14,19,20,||Triassic|Pl.1.||||||
15540|Precipice Sandstone|44169|2|Defined|Tb.1,p6,8,9,12,map|||||||||
15540|Precipice Sandstone|44170|2|Defined|p1,17,20-23,25,27,31||Early Jurassic|p32,35,40,Tb.1,map||||||
15540|Precipice Sandstone|44172|14|Not recorded|p1326,1330,1339||Jurassic|Springsure area.||||||
15540|Precipice Sandstone|44174|14|Not recorded|p345,347,348||Early Jurassic|||||||
15540|Precipice Sandstone|44207|14|Not recorded|p115|||||||||
15540|Precipice Sandstone|44304|14|Not recorded|p1|||||||||
15540|Precipice Sandstone|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
15540|Precipice Sandstone|44360|14|Not recorded|p36||Early Jurassic|||||||
15540|Precipice Sandstone|44379|4|Described|p1,2,20,21,24,map.||Early Jurassic|||||||
15540|Precipice Sandstone|44381|14|Not recorded|p7|||||||||
15540|Precipice Sandstone|44390|14|Not recorded|p6,8,9,12-16,Tb.1||Early Jurassic|||||||
15540|Precipice Sandstone|44391|14|Not recorded|Map Legend||Early Jurassic|||||||
15540|Precipice Sandstone|44414|14|Not recorded|p114||Jurassic|||||||
15540|Precipice Sandstone|44415|14|Not recorded|Fig.2,p23,24|||||||||
15540|Precipice Sandstone|44420|14|Not recorded|p1,3,9,11,18,21,22,|||p25,28,Fig.14||||||
15540|Precipice Sandstone|44421|14|Not recorded|p5,8-11,14,15,17-20||Jurassic|||||||
15540|Precipice Sandstone|44422|14|Not recorded|p148,149,153,154||Early Jurassic|||||||
15540|Precipice Sandstone|44426|14|Not recorded|p12||Jurassic|||||||
15540|Precipice Sandstone|44524|14|Not recorded|p17|||||||||
15540|Precipice Sandstone|44566|14|Not recorded|p13,15-17,Pls.2,3|||||||||
15540|Precipice Sandstone|44567|14|Not recorded|p11,13,14,Pls.1,2|||||||||
15540|Precipice Sandstone|44568|14|Not recorded|p1,4,7,Pls.2,3|||||||||
15540|Precipice Sandstone|44573|14|Not recorded|p97|||||||||
15540|Precipice Sandstone|44585|14|Not recorded|p45-Fig.2|||||||||
15540|Precipice Sandstone|44610|14|Not recorded|49,Tb.1|||||||||
15540|Precipice Sandstone|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
15540|Precipice Sandstone|44627|14|Not recorded|p139,141-144|Jurassic|Triassic|||||||
15540|Precipice Sandstone|44637|14|Not recorded|Table||Jurassic|||||||
15540|Precipice Sandstone|44640|14|Not recorded|p30|||||||||
15540|Precipice Sandstone|44652|14|Not recorded|p73(Tb.),74|||||||||
15540|Precipice Sandstone|44673|14|Not recorded|p25|||||||||
15540|Precipice Sandstone|44742|14|Not recorded|p91|||Lower part correlated with Razorback Beds in Liassic on palynological evidence.||||||
15540|Precipice Sandstone|44787|14|Not recorded|p122-126,128-129,Tb||Jurassic|Basal Jurassic||||||
15540|Precipice Sandstone|44805|14|Not recorded|p388|||||||||
15540|Precipice Sandstone|44840|14|Not recorded|p32,40|||Roma Shelf.||||||
15540|Precipice Sandstone|44844|14|Not recorded|p154||Early Jurassic|Moonie.||||||
15540|Precipice Sandstone|44852|14|Not recorded|p78|Jurassic|Triassic|||||||
15540|Precipice Sandstone|45071|3|Fully described|Table 15|||||||||
15540|Precipice Sandstone|45073|6|Mentioned|p58|||Geological history||||||
15540|Precipice Sandstone|45095|6|Mentioned|p62|||||||||
15540|Precipice Sandstone|45110|2|Defined|p85|Early Jurassic|Early Jurassic|See also Fig.5 and P24.||||||
15540|Precipice Sandstone|45168|6|Mentioned|p6|||||||||
15540|Precipice Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
15540|Precipice Sandstone|46984|6|Mentioned|Table 1|||||||||
15540|Precipice Sandstone|46989|5|Briefly described|Table 1|||||||||
15540|Precipice Sandstone|47404|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47414|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47448|14|Not recorded|?|||||||||
15540|Precipice Sandstone|47624|14|Not recorded|?|||||||||
15540|Precipice Sandstone|48600|14|Not recorded|p15|||||||||
15540|Precipice Sandstone|48606|14|Not recorded|p5,6,11,13,14,19-22|||(H/55-8 ; G/55-12). Pl.2||||||
15540|Precipice Sandstone|48619|14|Not recorded|?|||||||||
15540|Precipice Sandstone|48898|5|Briefly described|p2|||L.Jurassic. See also PP60,61,83||||||
15540|Precipice Sandstone|48900|4|Described|p50|||||||||
15540|Precipice Sandstone|48919|2|Defined|p36|Early Jurassic|Early Jurassic|See also p37-45.||||||14-FEB-07
15540|Precipice Sandstone|48920|3|Fully described|p36|||Lower Jurassic age.||||||14-FEB-07
15540|Precipice Sandstone|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
15540|Precipice Sandstone|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
15540|Precipice Sandstone|50190|5|Briefly described|p17, 85|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
15540|Precipice Sandstone|50197|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50209|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50214|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50215|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick-bedded, cross-bedded, fine- to coarse-grained pebbly quartzose sandstone and minor lithic sublabile sandstone, siltstone and mudstone.||||||18-JUN-09
15540|Precipice Sandstone|50301|5|Briefly described|Map Legend|Jurassic|Jurassic|||||||
15540|Precipice Sandstone|50317|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick bedded, cross-bedded fine to coarse-grained, pebbly quartzose sandstone, and minor lithic sublabile sandstone, sitlstone and mudstone.||||||09-JUN-04
15540|Precipice Sandstone|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Geological Province: Surat Basin||||||
15540|Precipice Sandstone|50597|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick/cross bedded pebbly quartzose sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|60114|6|Mentioned|p16|||Oil-bearing deposits.  Geological Province:  Cooper - Eromanga Basins.||||||
15540|Precipice Sandstone|60281|5|Briefly described|p27||Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
15540|Precipice Sandstone|60282|5|Briefly described|p11, p30|Jurassic|Jurassic|Geological Province: Mulgildie Basin.||||||
15540|Precipice Sandstone|60557|5|Briefly described|p19 Fig. 5b, p28|Early Jurassic|early Jurassic|Fluviatile sandstones.||||||09-JUN-05
15540|Precipice Sandstone|60995|6|Mentioned|p62|||Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|60996|6|Mentioned|p87|||Geological Province: Surat Basin. Equivalent to the Ripley Road Sandstone in the Clarence-Moreton Basin.||||||
15540|Precipice Sandstone|60998|5|Briefly described|p145|||Overlain by Evergreen Formation.||||||
15540|Precipice Sandstone|61005|6|Mentioned|p254 Tb. 4|||Equivalent to Ripley Road Sandstone and Helidon Sandstone.||||||
15540|Precipice Sandstone|61087|5|Briefly described|Map Legend|Jurassic|Jurassic|Thick-bedded, cross-bedded, fine to coarse-grained, pebbly quartzose sandstone and minor lithic sublabile sandstone, siltstone and mudstone.||||||
15540|Precipice Sandstone|61310|6|Mentioned|p21, p22|||Geological Province: Surat Basin. Correlated with the "Middle Bundamba Unit".||||||
15540|Precipice Sandstone|61377|5|Briefly described|p151|Early Jurassic|Early Jurassic|Braided stream sandstones. Conformably overlain by Evergreen Formation. Geological Province: Surat Basin. See also p139, p149 Fig. SU8.||||||07-FEB-11
15540|Precipice Sandstone|61611|5|Briefly described|p264, p266, p265 Fig. 3|Early Jurassic|Late Triassic|Lateral equivalent of Myrtle Creek Sandstone. Geological Province: Surat Basin.||||||15-JUL-13
15540|Precipice Sandstone|61832|5|Briefly described|p187, p190|Jurassic|Early Jurassic|On the MUNDUBERRA sheet.  Overlain by Evergreen Formation. Geological Province: Surat Basin.||||||
15540|Precipice Sandstone|62357|5|Briefly described|p535|Early Jurassic|Early Jurassic|||||||
15540|Precipice Sandstone|63218|6|Mentioned|p211 Fig.2. |Early Jurassic|Early Jurassic|Surat Basin.||||Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|63979|6|Mentioned|p33, Fig. 44|Toarcian|Pleinsbachian|Overlain by Evergreen Formation. Geological province: Surat Basin. Time-equivalent of Poolowanna Formation.||||||07-FEB-11
15540|Precipice Sandstone|64197|6|Mentioned|p630 Fig.7|Early Jurassic|Early Jurassic|||||Underlies Evergreen Formation.||
15540|Precipice Sandstone|64399|5|Briefly described|Map legend|Jurassic|Jurassic|Overlies Cynthia beds; below Evergreen Formation. Poorly sorted, thick bedded, x-bedded, fine- to v. coarse-gr., pebbly quartzose sst; minor laminated siltstone (upper part), carbonaceous shale, lithic sublabile sandstone, granule conglomerate.||||||19-AUG-08
15540|Precipice Sandstone|64665|5|Briefly described|p53 Fig.2, p57, p60, p61.|Early Jurassic|Early Jurassic|Eromanga and Surat Basins. Lateral equivalent of uppermost Poolowanna Formation. With the Evergreen Formation, forms the first of six cyclothems in the Surat Basin.||||Disconformably overlies Callide Coal Measures. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|64856|3|Fully described|p46 Fig.4, p61-62, p69, p75-76, p78-83|Sinemurian|Late Hettangian|Whitehouse (1952), for lowermost formation of the Bundamba Series. Type area described. Surat Basin. Unconformably overlies Bowen Basin units. Is overlain by Evergreen Formation. Up to 106m thick. Age from palynoflora (units APJ1, 21, 22). Grades laterally into Helidon Sandstone. Cross bedded pebbly quartzose sandstone, minor lithic sandstone, siltstone, argillite.|| ||||29-NOV-17
15540|Precipice Sandstone|64857|4|Described|p130-132, p113 Fig.3|Early Jurassic|Late Triassic|Overlies Bowen Basin sequence. Surat Basin. Mainly fine to coarse-grained pebbly quartzose sandstone. Braided stream deposition.||||||17-NOV-15
15540|Precipice Sandstone|64858|5|Briefly described|p181 Tb.1, p183, 187-188|||Basal Surat Basin unit in the central and northeastern part of the basin.||||||30-NOV-09
15540|Precipice Sandstone|64859|6|Mentioned|p194|Early Jurassic|Early Jurassic|Hydrocarbon reservoir, Surat Basin.||||||
15540|Precipice Sandstone|65003|5|Briefly described|p8, p31||Early Jurassic|Of Surat Basin.||||Overlain by the Evergreen Formation.||
15540|Precipice Sandstone|65096|6|Mentioned|p373|||Surat Basin. Compared with the Jurassic sandstones east of the Kumbarilla Ridge [accidently capitalised as Jurassic Sandstone] and the Ripley Road Sandstone of the Clarence-Moreton Basin, east of the Toowoomba Strait.||||||
15540|Precipice Sandstone|65112|6|Mentioned|Fig 11 p324|Early Jurassic|Early Jurassic|Unit in the Surat Basin. Underlies the Evergreen Sandstone.||||||22-MAR-12
15540|Precipice Sandstone|65113|5|Briefly described|p349, Fig 4 P340|Early Jurassic|Early Jurassic|Underlies the Evergreen Formation.||||||
15540|Precipice Sandstone|65114|5|Briefly described|p385 Fig.3, p383|Early Jurassic||Basal section of Supersequence J; basal Surat Basin||||||
15540|Precipice Sandstone|65116|5|Briefly described|p454, Fig 2 p437|Early Jurassic|Early Jurassic|Underlies the Evergreen Formation, Surat Basin. Quartzose sandstone.||||||
15540|Precipice Sandstone|65117|4|Described|p461, 6, 7, 9, 473, 4, Fig 4 p 465|Sinemurian|Sinemurian|Surat Basin, is overlain by Evergreen Formation with gradational contact. Unconformable over Tamworth Belt or Bowen Basin successions. Potential reservoir. Up to 150m thick in north. Average 60-80m thick. Included in Supersequence J||||||
15540|Precipice Sandstone|65118|6|Mentioned|p483, p493|Early Jurassic|Early Jurassic|Of Surat Basin||||||
15540|Precipice Sandstone|65119|5|Briefly described|p513, Fig 2, Table 1, Fig 4-5,7-13,15-17|Early Jurassic|Early Jurassic|Surat Basin. Quartzose sandstone, pebbly sandstone. Alluvial deposition up to 150m thick. Age: 198-205 Ma. Fission Track age: 98-120 Ma. Present in The Cockatoo Creek Well.||||||
15540|Precipice Sandstone|65385|5|Briefly described|pS134 Fig.7|Early Jurassic|Early Jurassic|Of Eromanga Basin. Overlain by Evergreen Formation.||||||08-MAR-12
15540|Precipice Sandstone|65388|4|Described|p208-211; p 210 Fig. 74, p203, p19|Pliensbachian|Sinemurian|Surat and Mulgilie Basins. Originally lowermost formation of the "Bundamba Series" of Whitehouse (1953). 30m to almost 150m thick. Unconformably overlies Muncon Volcanics, Winterbourne Volcanics, Cynthia beds, Torsdale Volcanics or Devonian to Permian rocks. Overlain by Evergreen Formation. Grades laterally into Helidon Sandstone of Moreton Basin in SE. Age on palynology: APJ1, APJ21 (Sinemurian-early Pliensbachian). White, thick-bedded, cross-stratified, fine to coarse-grained, pebbly quartzose sandstone with only minor lithic sublabile sandstone, siltstone and argillite.||||||
15540|Precipice Sandstone|66529|5|Briefly described|p10, p12 Fig.5|||Eromanga Basin.||||Unconformably overlies Moolayember Formation. Is overlain by Evergreen Formation.|Medium grained sandstone, non-marine.|
15540|Precipice Sandstone|66915|5|Briefly described|p6 Fig.3, p12|Early Jurassic|Early Jurassic|Eromanga and Surat Basins.||||||
15540|Precipice Sandstone|67133|5|Briefly described|p1-3, p5, p8, p10, p19-21|Jurassic|Jurassic|Surat Basin. A carbon geostorage target reservoir, sealed by Evergreen Formation. Large braided-stream deposits. 44 samples of this unit were analysed by XRD and optical microscopy for this study. Quartz is the main component (40-98%) and kaolinite (2-47%) is the dominant clay mineral.||||Overlies Peawaddy Formation. Is overlain conformably by Evergreen Formation.|A lower unit of predominantly coarse-grained quartzose sandstone, with thin to thick beds and a white clay matrix, is overlain by an upper fine- to medium-grained, thinly-bedded and sublabile unit.|
15540|Precipice Sandstone|67402|4|Described|p18 fig WSD2, p43 tbl HPB1|Pliensbachian|Sinemurian|Bowen and Surat Basins. Major aquifer that is also a highly prospective reservoir for the storage of carbon dioxide. Maximum thickness of 150m. Estimated storage potential of 1289 megatonnes of carbon dioxide. Deposited in a braided river system. See also p48, p56, p72, p146 fig SRT3, p147, p147 fig SRT5, p148, p151, p154, p155 fig SRT17, p156, p158, p162, p236, p239, p242, p243, p252, p253, p306.||||Overlies the Moolayember Formation and the Callide Coal Measures. Overlain by the Evergreen Formation or the Biloela Formation. Equivalent to the Myrtle Creek Sandstone.|Quartzose sandstone with a clay matrix that is overlain by fine-grained sandstone and siltstone.|
15540|Precipice Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Bundamba Group.||Overlain by Evergreen Formation. Underlain by Molyamber Formation or Wandoan Sandstone.||
15540|Precipice Sandstone|67788|6|Mentioned|p24|Early Jurassic|Early Jurassic|Carnarvon Gorge, QLD. Photograph illustrating broad alluvial plains formed by braided rivers.||||||
15540|Precipice Sandstone|68003|5|Briefly described|p57 Fig.3-n, p58 Fig.3-o.|Early Jurassic|Early Jurassic|Bowen Basin.||||Unconformably overlies Moolayember, Wandoan, and locally Napperby Formations. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|68004|5|Briefly described|pp172-174.|Early Jurassic|Early Jurassic|Petroleum-producing. Excellent reservoir; exploration targetting limited to very northern part of the Basin in NSW. Sealed in Queensland by Evergreen Formation, but in NSW that unit is sandy.||||||
15540|Precipice Sandstone|68008|3|Fully described|p3, p192-194, p203, p208-210, p219-223|Early Jurassic|Early Jurassic|See also p225-238, p246, p251-252, p254, p261-265, p292, p359, p361, p363, p372, p492-493, p621. Whitehouse (1953, 1955). Applied to basal Jurassic sedimentary rocks on the Monto 250k sheet by Dear (1968) and Dear et al. (1971). Includes the Razorback beds of Staines (1953) and Kirkegaard et al. (1970). Occurs mainly in four areas (listed and mapped). Almost always occurs as a ridge-capping, cliff-forming unit. N-flowing braided stream deposits. 45-100m thick. Age from spore assemblage. 6km E of Westwood, vertical columnar jointing occurs; the result of heating by (now eroded) Dalma Basalt. Has long been quarried for building stone; gold was mined at Mount Victoria. Geophysics modelling. Unconformably overlies Muncon, Winterbourne Volcanics, Annie Creek beds, Bushley Dacite, Callide Coal Measures, Bundaleer Tonalite, Quarry Gabbro, Moonmera Porphyritic Granodiorite, possibly Native Cat Andesite, and Flaggy Quartz Monzodiorite.||||Is overlain conformably by Evergreen Formation and unconformably by Dalma Basalt, Biloela Formation and Stanwell Formation. Equivalent to Helidon Sandstone. See Comments.|Extensive but thin sand sheet. Cream, white to buff quartzose sandstone, pebbly quartzose sandstone, and some siltstone; some conglomerate beds. Local well-developed columnar jointing.|21-SEP-18
15540|Precipice Sandstone|68117|6|Mentioned|p346|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|68135|5|Briefly described|p52 fig 2b, p59, p63 fig 6,  p64|Pleinsbachian|Sinemurian|Surat Basin (QLD). Age confirmed by dinosaur footprints. Plant macrofossils and vertebrate body parts and footprints found throughout.||||Overlain by Evergreen Formation|Sandstone.|14-SEP-17
15540|Precipice Sandstone|68139|6|Mentioned|p23|Early Jurassic|Early Jurassic|Surat Basin.||||Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
15540|Precipice Sandstone|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Surat and Mulgildie Basins. This unit, as well as the Evergreen Formation and Hutton Sandstone, are all mapped under the symbol, Jb.||||||
15540|Precipice Sandstone|68576|5|Briefly described|Q_4: p1, p3-5, p12-15, p21-22, p24|Early Jurassic|Early Jurassic|The basal unit in the Surat Basin. The unconformity represents a 40 m.y. hiatus and separates the Bowen Basin from the Surat Basin. A major aquifer. Forms the majority of cliff faces in Carnarvon Gorge. Displays braided fluvial sedimentary structures.||||Unconformably overlies Taroom and Eddystone beds, and Moolayember Formation. Is overlain conformably by Evergreen Formation.|Fine- to coarse-grained, pebbly quartzose sandstone with minor lithic sub-labile sandstone, siltstone and argillite.|
15540|Precipice Sandstone|68679|5|Briefly described|p312-313, p338, p398, p443|Jurassic|Jurassic|Northern New England Orogen. Covers much of the Callide Basin fill. A scarp-forming unit. Previously (Dear et al. , 1971) included in the Callide Coal Measures, but excluded on palynological grounds by de Jersey (1974).||||Disconformably or unconformably overlies Callide Coal Measures. Overlies Winterbourne Volcanics.||
15540|Precipice Sandstone|69457|5|Briefly described|p41:2-3|||NE Eromanga Basin and Surat Basin.|||Is overlain by Evergreen Formation.|Lateral equivalent of (part) Poolowanna Formation.||12-JUL-16
15540|Precipice Sandstone|69582|6|Mentioned|p35-p36, p38|Lower Jurassic|Lower Jurassic|Surat Basin.||||Overlain by the Evergreen Formation.||
15540|Precipice Sandstone|69594|5|Briefly described|p519, p524, p533-535, p539, p543-545|Pliensbachian|Sinemurian|See also p551, p560, p563, p572. Whitehouse (1952, 1955) identified a lower coarse subunit and an upper finer unit; the lower subunit is regarded as the formation (Green et al., 1997). Eromanga, northern Surat Basins. ~45m thick, thinning rapidly to the NW (also said to be up to 106m thick). Braided stream deposits. In the Mount Morgan and Stanwell areas, the Razorback beds are recognised as outliers of the Precipice Sandstone. Has a diachronous base younging to the W. The main Surat Basin reservoir for oil condensate, gas and LPG. Groundwater aquifer. RELATED UNITS (continued): Passes laterally into Poolowanna Formation. Merges with Ripley Road Sandstone in the Surat Basin. Upper part correlated with Gatton Sandstone.||||Unconformably overlies Eddystone beds, Moolayember Formation and Chong beds. Is overlain by Stanwell Formation, Dalma Basalt and conformably by Evergreen Formation. See COMMENTS for more.|Thick-bedded, coarse, quartzose sandstone.|
15540|Precipice Sandstone|69633|4|Described|p1-15, p20, Appendix 6.|Early Jurassic|Early Jurassic|Surat Basin. Hydrocarbon reservoir, sealed by Evergreen Formation. Has a widespread unconformity at its base. Fresh-water, fluvial braided-channel sediments succeeded by fluvio-lacustrine deposits. GSQ Chinchilla 4 and Roma 8 core logs detailed (Appendix 4 & 5). The authors argue that at least part of the lowest c.58m of the Evergreen Formation, ie below the Boxvale Sandstone Member, should be assigned to this unit. Palynology detailed. Data from sections from well completion reports are included in Appendix 1 and 2.||||Unconformably overlies Chong beds and Eddystone beds. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|69681|5|Briefly described|p74-87|Early Jurassic|Early Jurassic|Primary target for oil and gas exploration: has good porosity and high permeability, although permeability decreases by an order of magnitude below ~1500m. Yields oil in the Moonie field. Most of the core samples used for this study are from this unit and the Evergreen Formation. Potential for CO2 geostorage, sealed by Evergreen Formation, discussed.||||Is overlain by Evergreen Formation.|Sandstone; shale and siltstone common in upper part of this unit.|
15540|Precipice Sandstone|69682|4|Described|p91-110|Early Jurassic|Early Jurassic|Basal Surat Basin. Potential CO2 reservoir. 70m thick. Mineralogy discussed in detail. Conclusion is that it is suitable for residual pore-space, hydrodynamic and dissolution sequestration of CO2.||||Is conformably overlain by Evergreen Formation.|Laterally extensive, predominantly quartzose, fine- to very coarse-grained sandstone with pebbly horizons and minor siltstone.|
15540|Precipice Sandstone|69790|6|Mentioned|p1062|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|70374|6|Mentioned|p809 figure 1|Pliensbachian|Sinemurian|||||Is overlain by Evergreen Formation.||28-SEP-16
15540|Precipice Sandstone|70628|6|Mentioned|p952,964|Sinemurian|Sinemurian|Along with Evergreen Formation, forms part of the J-sequence (Hoffman et al 2009) of the Surat Basin.||||Underlies Evergreen Formation.|Sandstone.
|
15540|Precipice Sandstone|70821|5|Briefly described|p79-80|||Eromanga, Surat Basins. A deep, high-quality aquifer in the Great Artesian Basin.||||Unconformably overlies Moolayember Formation. Is overlain by Evergreen Formation.||
15540|Precipice Sandstone|71282|6|Mentioned|p457 Fig.1, p460|||The lithology is omitted in Fig.1. Appears as Evergreen & Precipice Formation on p460.||||||
15540|Precipice Sandstone|71805|4|Described|p75-p78, p80-p89|Toarcian|Sinemurian|Surat Basin. The term Precipice Sandstone was first used by Whitehouse (1952) who defined the type section as "Sandstone cliffs in the gorge of precipice Creek, a tributary of the Dawson River" located on the Taroom Sheet of Mollan et al. 1972. Further nomenclature details are provided by Exon (1976). This unit youngs to the west. This unit is a regional aquifer and ranges from less than 10m to nearly 150m in thickness. Informally referred to as upper and lower components. An upper and lower facies are described. Wireline logs exist for the core and for this unit.||||Overlies the Moolayember Formation. Conformably overlain by the Evergreen Formation.  Placement of boundary with Evergreen Formation discussed.|Quartzose sandstones, siltstone and mudstones with rare thin coals.|16-MAY-19
15540|Precipice Sandstone|71806|4|Described|p483-p488, p500|Lower Jurassic|Lower Jurassic|Surat Basin. Traditionally interpreted as a braided fluvial deposit; however, this study also found evidence of tidal to marine influence. This unit is an important aquifer and petroleum reservoir. Unconformably to disconformably overlies Permo-Triassic strata. Varies from over 150m in the axis of the basin to less than 20m on the eastern and western margins. Exposed in Boolimba Bluff. Lithology is derived from the 'informal type section' at Boolimba Bluff. Facies are described in detail.||||Overlain by the Evergreen Formation.|Very coarse- to medium-grained quartz arenite, fine- to very fine-grained quartz arenite with kaolinite clay matrix, granule to medium-pebble conglomerate and siltstone to mudstone beds.|
15540|Precipice Sandstone|72297|5|Briefly described|p697, p724, p726, p739, p744-746, p748|Early Jurassic|Early Jurassic|At Grafton Range, NE of Roma, contains sodium bicarbonate in high-salinity brines 800-1000m below ground surface. The bicarbonate originates from the underlying Aldebaran Sandstone. An excellent regional reservoir; produced the first commercial oil discovery in Australia (UOD Moonie, 210km SE of Roma) in 1961. Sealed by Evergreen Formation.|||Razorback beds.|Disconformably overlies the Callide Coal Measures.|Fluvial sheet sandstone.|
15540|Precipice Sandstone|72298|5|Briefly described|p790, p796, p801-802|Jurassic|Jurassic|Eromanga Basin (QLD,NSW), Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores. An aquifer which locally exhibits double porosity (primary porosity/permeability, and secondary porosity resulting from faulting and/or dissolution of silica). A source of groundwater in the Monto area. Crops out in the Great Dividing Range but has no specific discharge point.||||Unconformably overlies Moolayember and Wandoan FZs. Is overlain by Evergreen FZ.||
15540|Precipice Sandstone|72921|4|Described|p8-10, p15 Fig.2, p16-17, p21 Fig.7.|Early Jurassic|Early Jurassic|Site of demonstration effort aiming to inject 180,000 tons of CO2 as part of Surat Carbon Capture and Storage (CCS) project. Shown as located in the Surat Basin in Queensland. Sediments demonstrate a marine influence. See also p23 Fig.9, p24-25, p27-28, p48-p52, p54, p55, p77 App.1, p82.||||Conformably underlies Evergreen Formation|Includes sandstone and conglomerate and fossils.|
15540|Precipice Sandstone|73113|5|Briefly described|p. 2-3, 22-24, 29-31, 35-37, 41, 46...|||Surat Basin. Regional aquifer. Treated water is re-injected into this unit (since 2015). Relatively high incidences of fracturing in the unit. More locations: p. 60, 66-67, 69, 79-80, 92, 98, 116-117, 119, 123, 126-127, 130, 148-149, 152-153, 159-160, 162, 164, 168-173, 177, 179, 182-183, 191-193, 199.||||Unconformably underlain by Rewan Group, Bandanna Formation, Cattle Creek Formation, and Moolayember Formation. Overlain by Evergreen Formation.||
15540|Precipice Sandstone|73147|5|Briefly described|p127|Early Jurassic|Early Jurassic|Surat Basin.|||||Marine influenced.|
15540|Precipice Sandstone|73393|6|Mentioned|p20-21|Toarcian|Pliensbachian|Surat and Eromanga Basins.||||||
15540|Precipice Sandstone|73450|6|Mentioned|p51|||||||Underlain by Bushley Dacite.||
15540|Precipice Sandstone|73570|6|Mentioned|p914, p915 Fig.4, p916, p917 Fig.5|Early Jurassic|Early Jurassic|Surat Basin.||||||
15540|Precipice Sandstone|73600|4|Described|p189-192, p195-199, p201-205|Pliensbachian|Sinemurian|Surat Basin. Economically important due to its aquifer capacity and prospectivity for CO2 sequestration. Variable thickness with a maximum of ca 175 m. Gradational upper boundary. Comprises two main parts, a 'lower' and 'upper'. Grade from quartzose to more labile and mineralogically heterogeneous up-section. Interpreted to represent braided through to meandering fluvial settings, fluvial-lacustrine systems, and marine depositional settings. Palynology was previously used for biostratigraphic age constraint. Contains no known tuff horizons. Various detrital zircon maximum depositional ages are presented. Detrital zircon age spectra demonstrate complex sediment sourcing dominated by the Thomson Orogen. Absent on the Kumbarilla and Nebine ridges. Relatively uniform provenance and sediment characteristics across the study area.||||Conformably overlain by Evergreen Formation. Underlain by Eddystone Beds. Unconformably underlain by the Moolayember Formation.|Coarse-grained, thick-bedded sandstone capped by an overall fining-upward, fine- to medium-grained sandstone.|
15569|Pretty View Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||24-MAR-06
15569|Pretty View Tuff Member|35287|6|Mentioned|p7|||||||||
15569|Pretty View Tuff Member|42566|3|Fully described|p78|||||||||
15569|Pretty View Tuff Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
15634|Prudoe Shale|30286|6|Mentioned|p1099|||Stratigraphic table||||||
15642|Puddledock Complex|23720|5|Briefly described|Map Legend|Late Permian||Pyroxene syenite and pyroxene alkali granite.||||||15-DEC-04
15642|Puddledock Complex|30911|6|Mentioned|Map legend|Permian|Permian|||||||
15642|Puddledock Complex|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
15642|Puddledock Complex|44450|6|Mentioned|p35|||Geological Province: New England Fold Belt.||||||
15642|Puddledock Complex|71628|6|Mentioned|p13: 1-3, 16|||Spry (1954), Neilson (1970, unpublished). Now included in Highlands Complex.||||||
15673|Purgatory Creek adamellite|34220|5|Briefly described|p297|||Invalid use.||||||
15673|Purgatory Creek adamellite|71628|6|Mentioned|p19:146|||Gutsche (1969). Now Purgatory Monzogranite.||||||
15676|Purlawaugh Formation|721|5|Briefly described|Map legend|Oxfordian|Bajocian|Thinly bedded lithic-labile sandstone interbedded with siltstone and mudstone.  Geological Province: Surat Basin.||||||
15676|Purlawaugh Formation|12597|5|Briefly described|p492 Tb.1, p496-497, p501|Middle Jurassic|Middle Jurassic|S Surat Basin. 9-84m thick. Commercially inferior coal deposits.||||Grades laterally into Digilah and Ukebung Formations.|Thickly bedded labile sandstone, siltstone, dark mudstone and minor thin coal seams.|
15676|Purlawaugh Formation|22831|4|Described|p 82|Jurassic|Jurassic|||||||
15676|Purlawaugh Formation|22857|4|Described|p309, p546 App.1 Tb.A1.12|Late Jurassic|Middle Jurassic|Lithic to labile arenite interbedded with siltstone and mudstone, minor coal. Appears coeval with Garrawilla Volcanics, also disconformably overlies them. Max. thickness: 84m. See also p314-5.||||||
15676|Purlawaugh Formation|22865|5|Briefly described|p309,314,Fig22.8p315||Late Jurassic|||||||
15676|Purlawaugh Formation|23043|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|of Surat basin.||||||
15676|Purlawaugh Formation|23050|6|Mentioned|p81|||of Surat Basin||||||
15676|Purlawaugh Formation|23053|4|Described|p11,Fig10p17,25,86|Middle Jurassic|Early Jurassic|||||||
15676|Purlawaugh Formation|23170|2|Defined|p330, Fig.61, p283|Late Jurassic|Triassic|Of Surat Basin.||||||17-SEP-08
15676|Purlawaugh Formation|23246|6|Mentioned|p12|||Photos 2 and 3 used as an example in the information system. These photos contain the Purlawaugh Formation.||||||
15676|Purlawaugh Formation|23566|5|Briefly described|p116 Fig. 2|Jurassic|Jurassic|Geological Province: Gunnedah Basin||||||
15676|Purlawaugh Formation|23740|6|Mentioned|p1220|||Geological Province: Gunnedah Basin||||||
15676|Purlawaugh Formation|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
15676|Purlawaugh Formation|24042|5|Briefly described|p510|Jurassic|Jurassic|||||||
15676|Purlawaugh Formation|24092|5|Briefly described|p8 Fig.3|||||||||
15676|Purlawaugh Formation|24159|5|Briefly described|p150 Fig.3, p152|Middle Jurassic|Early Jurassic|Geological Province: Surat Basin. Underlying Unit: unconformably with Napperby and Deriah Formations.||||||
15676|Purlawaugh Formation|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
15676|Purlawaugh Formation|29870|4|Described|p15|||||||||
15676|Purlawaugh Formation|30610|2|Defined|p322|Middle Jurassic|Early Jurassic|Lower to Middle Jurassic.||||||
15676|Purlawaugh Formation|34157|6|Mentioned|p1|||Jurassic.||||||
15676|Purlawaugh Formation|34254|6|Mentioned|p481|||||||||
15676|Purlawaugh Formation|35095|6|Mentioned|p111|||||||||
15676|Purlawaugh Formation|35416|6|Mentioned|p8|||Stratigraphy and palynological framework on Fig.2||||||
15676|Purlawaugh Formation|36570|6|Mentioned|p31|||Also mention P58.||||||
15676|Purlawaugh Formation|36961|6|Mentioned|Table 1|||||||||
15676|Purlawaugh Formation|37597|6|Mentioned|p77|||||||||
15676|Purlawaugh Formation|37794|6|Mentioned|Table 1|||||||||
15676|Purlawaugh Formation|37856|6|Mentioned|Table I|||||||||
15676|Purlawaugh Formation|38614|6|Mentioned|p12|||||||||
15676|Purlawaugh Formation|39063|6|Mentioned|Fig.6|||||||||
15676|Purlawaugh Formation|39666|6|Mentioned|p111|||||||||
15676|Purlawaugh Formation|40767|4|Described|p9|||||||||
15676|Purlawaugh Formation|40952|6|Mentioned|p8|||||||||
15676|Purlawaugh Formation|41266|6|Mentioned|Fig.3|||||||||
15676|Purlawaugh Formation|41290|4|Described|p226|||||||||
15676|Purlawaugh Formation|41330|6|Mentioned|p21|||||||||
15676|Purlawaugh Formation|42284|6|Mentioned|p111|||||||||
15676|Purlawaugh Formation|42463|6|Mentioned|Fig.6 P173|||||||||
15676|Purlawaugh Formation|42657|5|Briefly described|p73|||||||||
15676|Purlawaugh Formation|42679|6|Mentioned|Fig.3 P3|||||||||
15676|Purlawaugh Formation|42918|5|Briefly described|p45|||||||||
15676|Purlawaugh Formation|43091|5|Briefly described|Map legend|||of Surat Basin||||||
15676|Purlawaugh Formation|43194|5|Briefly described|p122, p127|Jurassic|Jurassic|Medium-grained pebbly sandstone beds and coal seams. Disconformably overlies Napperby Formation, Deriah Formation.||||||
15676|Purlawaugh Formation|43276|5|Briefly described|Map Legend|Middle Jurassic|Early Jurassic|||||||
15676|Purlawaugh Formation|43277|5|Briefly described|Map Legend|Middle Jurassic|Early Jurassic|of Great Australian Basin.||||||
15676|Purlawaugh Formation|43494|4|Described|p13-14|Jurassic|Jurassic|Characteristically pelitic and coal-bearing. Represents upper part of former  "Ballimore Formation". Interbedded white siltstone and black carbonaceous siltstone. Max. thick: 74m. Divided into Ukebung Fm.overlain by Digilah Fm (Loughan and Evans 1978).||||||16-MAR-06
15676|Purlawaugh Formation|43582|6|Mentioned|p28|||||||||
15676|Purlawaugh Formation|44160|6|Mentioned|Map Legend||Jurassic|||||||
15676|Purlawaugh Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
15676|Purlawaugh Formation|49010|6|Mentioned|Fig.4|||Coonamble Embayment||||||
15676|Purlawaugh Formation|49011|6|Mentioned|Fig.3|||Coonamble Embayment||||||
15676|Purlawaugh Formation|50590|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Great Australian Basin (possibly misspelt).  Ferrugenised red siltstone, carbonaceous mudstone, lithic sandstone, ironstone, minor coal.||||||29-JUN-04
15676|Purlawaugh Formation|50629|5|Briefly described|Map Legend|Jurassic|Jurassic|Geological Province: Surat Basin. Underlies: Pilliga Sandstone.  Overlies: Garrawilla Volcanics.||||||05-JUL-04
15676|Purlawaugh Formation|60266|5|Briefly described|p2, p3 Tb. 1|Middle Jurassic|Early Jurassic|Supersedes the Ukebung Formation.  Stream, backswamp and lacustrine deposits of lithic sandstone, conglomerate, siltstone, shale and coal.  Onlaps the Glenrowan Intrusives and overlain by Pilliga Sandstone.  Geological Province: Surat Basin.||||||03-AUG-04
15676|Purlawaugh Formation|60267|4|Described|p15, p23|Jurassic|Jurassic|Kaolinitic clayrock.  Overlies Garrawilla Volcanics.  Max. thickness: <20m.  Geological Province: Surat Basin.||||||12-AUG-04
15676|Purlawaugh Formation|60726|5|Briefly described|p2 Fig.1, p5.|Early Jurassic|Early Jurassic|Gulgong area.|||Talbragar Fish Bed.|||
15676|Purlawaugh Formation|61313|5|Briefly described|p94 Fig. G7|Jurassic|Jurassic|Flood plain deposits including fluvial sandstones. Thickness: 76m. Upper parts are time equivalents of Walloon Coal Measures. Geological Province: Gunnedah, Surat and Bowen Basins. See also p98 Fig. G10.||||||
15676|Purlawaugh Formation|61377|5|Briefly described|p152, p148 Tb. SU1|Middle Jurassic|Early Jurassic|In Coonamble Embayment, this unit is represented by Digilah Fm, Doona Sandstone Member and Ukebung Fm. Labile sst, sltst, coal and mudstone. Overlies Wallingarah Fm. Geol.Prov: Surat Basin. See also p149 Fig. SU8, p154 Fig. SU9||||||07-FEB-11
15676|Purlawaugh Formation|61776|5|Briefly described|p194 Fig. 3|Jurassic|Jurassic|Geological Province: Surat Basin. Lithic sandstone, siltstone and mudstone.||||||
15676|Purlawaugh Formation|62578|5|Briefly described|p43|Late Jurassic|Jurassic|Contains the Fossil Fish Bed, and assemblage which represents a mass kill site.  This bed also known as Talbragar Fossil Fish Bed in which the most common fish genus is Leptolepis.||||||26-JUL-06
15676|Purlawaugh Formation|65112|6|Mentioned|Fig 11 p324|Late Jurassic|Middle Jurassic|Unit in the Surat Basin. Underlies the Pilliga Sandstone.||||||22-MAR-12
15676|Purlawaugh Formation|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Middle Jurassic|Underlies the Pilliga Sandstone.||||||
15676|Purlawaugh Formation|65114|5|Briefly described|p385 Fig.3|Late Jurassic|Middle Jurassic|||||||
15676|Purlawaugh Formation|65116|5|Briefly described|p455, Fig 2 p437|Late Jurassic|Middle Jurassic|Underlies the Pilliga Sandstone. Maximum thickness ~360m. Equivalent to Hutton Sandstone + Walloon Coal Measures.||||||06-MAR-12
15676|Purlawaugh Formation|66529|5|Briefly described|p12 Fig.5 |||Coonamble Embayment.||||Is overlain by Pilliga Sandstone.||14-SEP-17
15676|Purlawaugh Formation|68003|5|Briefly described|p52, p54-57 Figs., pp59-61, p127.|Middle Jurassic|Early Jurassic|Eastern Surat Basin. Continental river and lake deposits. Typically outcrops poorly; underlies gently undulating topography.|||Includes Talbragar Fossil Fish bed.|Conformably overlies the Garrawilla Volcanics. Unconformably overlies Deriah Formation. Is overlain by Pilliga Sandstone.|Thinly bedded carbonaceous mudstone, silty sandstone, and subordinate coal; abundant carbonaceous fragments; thin beds of flint clay.|
15676|Purlawaugh Formation|68004|5|Briefly described|p137, pp163-164, p176.|Jurassic|Jurassic|Moderately prospective for kaolin. Mis-spelt as Purlewaugh Formation on p137. Coal, when present, is not commercially viable. Contains a gas-saturated sandstone layer near Bellata. A potential oil source rock.|||Includes Ukebung Member.||Interbedded claystones, mudstones and minor fine- to medium-grained sandstones; coal as thin bands within the claystone units.|
15676|Purlawaugh Formation|68069|5|Briefly described|Map legend.|Middle Jurassic|Middle Jurassic|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only. Low-energy fluvial to paludal, aggradational plain or valley infill.||||Is overlain conformably by Pilliga Sandstone.|Siltstone, mudstone and kaolinitic claystone interbedded with carbonaceous to coaly shale, thin coal seams and fine- to medium-grained lithic-labile sandstone.|
15676|Purlawaugh Formation|68135|6|Mentioned|p52 fig 2b, p62, p63|Tithonian|Toarcian|Surat Basin (NSW). Age derived from fossil fish assemblage. Vertebrate body parts, invertebrate and plant macrofossils.||||Disconformably overlain by Pilliga Sandstone.|Interbedded siltstone and sandstone.|
15676|Purlawaugh Formation|68593|5|Briefly described|p3-4, p47|Middle Jurassic|Middle Jurassic|Oldest unit of the Surat Basin in the map area. Deposition occurred in a low-energy fluvial to paludal, perhaps swampy, aggradational plain or valley infill.||Rolling Downs Group.||Is overlain by Pilliga Sandstone.|Siltstone, mudstone, kaolinitic claystone interbedded with carbonaceous to coaly shale, thin coal seams and fine- to medium-grained lithic-labile sandstone.|
15676|Purlawaugh Formation|70036|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Surat Basin. Included in a mapped unit of fluvial and lacustrine sequences: lithic to quartzose sandstone, siltstone, mudstone, claystone and coal.||||||
15676|Purlawaugh Formation|70821|5|Briefly described|p80|||Coonamble Embayment. Aquiclude.||||Unconformably overlies Garrawilla Volcanics. Is overlain by Pilliga Sandstone.||
15676|Purlawaugh Formation|71890|4|Described|p5-p7, p17-p18, p24, p26|Bathonian|Pleinsbachian|Surat Basin. Inferred to have formed in lake, swamp and floodplain environments. This unit is typically recessive, weathering to clayey soils and characterised by poor outcrop and low relief. See also p30-p31, p33-p34, p52-p53.|190.8 to 166.1 Ma|||Conformably overlies the Garrawilla Volcanics. Disconformably overlies the Napperby Formation. Disconformably overlain by the Pilliga Sandstone.|Fine- to medium-grained, lithic to labile sandstone thinly interbedded with siltstone, mudstone and thin coal seams.|
15676|Purlawaugh Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Coonamble Embayment (NSW).||||Unconformably overlies Garrawilla Volcanics. Is overlain by Pilliga Sandstone.||
15676|Purlawaugh Formation|72700|5|Briefly described|Mapsheet 1 and 2|Mesozoic|Palaeozoic||||||Fine- to medium-grained sandstone interbedded with siltstone, mudstone and thin coal seams|
15676|Purlawaugh Formation|72921|5|Briefly described|p15 Fig.2.|Late Jurassic|Early Jurassic|Shown as located in the Surat Basin in New South Wales. Shown with a depositional break at the start of the Late Jurassic and including TFB [probably = Talbragar Fossil Fish Bed] in the upper part.||||Shown as unconformably overlying Garrawilla Volcanics and is underlying and laterally equivalent to Pilliga Sandstone.|May include fossiliferous siltstone.|
15683|Purnamoota Subgroup|22771|6|Mentioned|Table12.2p45|||||||||
15683|Purnamoota Subgroup|22857|4|Described|p45 Tb. 12.2, p390 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group. Max. thickness: >1000m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
15683|Purnamoota Subgroup|22965|5|Briefly described|Fig 1||Statherian|Part of the Broken Hill Group, contains Silver King Formation, Freyers Metasediments and Parnell Formation.||||||
15683|Purnamoota Subgroup|22966|6|Mentioned|Fig 1||Proterozoic|Rift stage of geological development.||||||
15683|Purnamoota Subgroup|22967|5|Briefly described|p39||Statherian|Contains Hores Gneiss, Silver King Formatiion, Freyers Metasediments and Parnell Formation.||||||
15683|Purnamoota Subgroup|23025|6|Mentioned|Fig1p75|||||||||
15683|Purnamoota Subgroup|23223|6|Mentioned|p42|||of Broken Hill Group.||||||
15683|Purnamoota Subgroup|23248|5|Briefly described|Fig2p169|||||||||
15683|Purnamoota Subgroup|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|Of the Broken Hill Group.   Name abandoned by this study.||||||23-JUN-08
15683|Purnamoota Subgroup|38969|4|Described|p208|||||||||
15683|Purnamoota Subgroup|39662|2|Defined|p425|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15683|Purnamoota Subgroup|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15683|Purnamoota Subgroup|39849|6|Mentioned|Table 2|||||||||
15683|Purnamoota Subgroup|40290|6|Mentioned|Fig.2|||||||||
15683|Purnamoota Subgroup|40822|6|Mentioned|Fig.2|||||||||
15683|Purnamoota Subgroup|41630|6|Mentioned|p27|||||||||
15683|Purnamoota Subgroup|41633|6|Mentioned|Fig2.27|||||||||
15683|Purnamoota Subgroup|42261|6|Mentioned|Fig 1 P530|||||||||
15683|Purnamoota Subgroup|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15683|Purnamoota Subgroup|42537|4|Described|p13|||||||||
15683|Purnamoota Subgroup|42595|6|Mentioned|Fig. 2 P5|||||||||
15683|Purnamoota Subgroup|42897|5|Briefly described|Fig.3, P321|||||||||
15683|Purnamoota Subgroup|43052|6|Mentioned|Fig.4.22|||||||||
15683|Purnamoota Subgroup|43086|6|Mentioned|Fig.3|||||||||
15683|Purnamoota Subgroup|43264|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
15683|Purnamoota Subgroup|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Broken Hill Group.||||||07-NOV-08
15683|Purnamoota Subgroup|43572|6|Mentioned|Fig.3.2 p6|||||||||
15683|Purnamoota Subgroup|46598|6|Mentioned|Fig.3 P302|||||||||
15683|Purnamoota Subgroup|50045|5|Briefly described|p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Broken Hill Group (Willyama Supergroup). Overlain by Sundown Group; underlain by Allendale Metasediments.||||||31-MAY-07
15683|Purnamoota Subgroup|50619|5|Briefly described|p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Of the Broken Hill Group (Willyama Supergroup).  Includes Hores Gneiss, Silver King and Parnell Formations, and Freyers Metasediments.  Geological Province: Broken Hill Block.||||||07-NOV-08
15683|Purnamoota Subgroup|60485|5|Briefly described|p28 Fig. 2|||Of the Broken Hill Group. Includes the Silver King Formation and Fryers Metasediments. Geological Province: Broken Hill Domain.||||||
15683|Purnamoota Subgroup|61908|5|Briefly described|p146|||Of the Broken Hill Group. Includes metapsammites and matepelites. Geological Province: Broken HIll Group.||||||22-JAN-08
15683|Purnamoota Subgroup|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Broken Hill Group.||||
15683|Purnamoota Subgroup|62993|6|Mentioned|p13, p15, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Broken Hill Group|Includes Hores Gneiss, Freyers Metasediments, Parnell Gneiss|||17-DEC-21
15683|Purnamoota Subgroup|63102|5|Briefly described|p13|||Geological province: Broken Hill Domain, Curnamona Province.||Unit of Broken Hill Group.|Includes Silver King Formation, Fryers Metasediments.|||
15683|Purnamoota Subgroup|63519|5|Briefly described|p6 Fig. 2|||Geological Province: Broken Hill Block-Euriowie Block.||||||11-JUN-08
15683|Purnamoota Subgroup|63866|5|Briefly described|p36|||Broken Hill Domain, Curnamona Province.||Broken Hill Group|Includes the Hores Gneiss, Silver King Formation, Freyers Metasediments and the Parnell Formation.|||
15683|Purnamoota Subgroup|64097|6|Mentioned|p329 Appx.|||Of Broken Hill Group. Adjacent to Wondervale Well Granite Gneiss, which intruded at or just above the base of Broken Hill Group.  Age: 1685+/-5Ma (SHRIMP U-Pb, zircon; this paper)||||||07-FEB-11
15683|Purnamoota Subgroup|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group (Willyama Supergroup). Includes Parnell Fm, Freyers Metasediments and Hores Gneiss. Geological Province: Broken Hill Block.||||||07-FEB-11
15683|Purnamoota Subgroup|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Gp. Includes Parnell Gneiss, Freyers Metasediments + Hores Gneiss. Geological province: Broken Hill Domain. Comprises two "Potosi-type" gneiss units enclosing the Freyers Metasediments between Parnell Gneiss below and Hores Gneiss above.||||||07-FEB-11
15683|Purnamoota Subgroup|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Broken Hill Group. Geological province: Broken Hill Domain.||||||07-FEB-11
15683|Purnamoota Subgroup|66302|5|Briefly described|p36 Fig.9|Statherian|Statherian|Broken Hill Domain, Curnamona Province.||Broken Hill Group|Includes the Parnell Gneiss, Freyers Metasediments and the Hores Gneiss.|||
15683|Purnamoota Subgroup|70000|5|Briefly described|p34, p36|Statherian|Statherian|||Unit in Broken Hill Group.|Includes Silver King Metadolerites and Hores Gneiss.|Overlies Allendale Metasediments.|Consists of two horizons of garnet-bearing quartzofeldspathic Potosi-type gneiss, separated by pelitic rocks. Minor calc-silicate, garnet-rich BIF, quartz-gahnite and quartz-garnet rock. Basic gneiss sills generally present and locally abundant.|
15683|Purnamoota Subgroup|70014|5|Briefly described|Map legend|||||Unit in Broken Hill Group.|Includes Parnell and Silver King Formations, Freyers Metasediments and Hores Gneiss.|Overlies Allendale Metasediments. Is overlain by Sundown Group.|A metasediment sequence with intercalated basic gneisses and garnet-rich quartzo-feldspathic gneisses (interpreted as basic and acid metavolcanics respectively), and "lode horizon" rocks (quartz-gahnite, garnet-quartz rocks).|
15683|Purnamoota Subgroup|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Broken Hill Group.|Includes Silver King Metadolerites and Hores Gneiss.|Overlies Allendale Metasediments.|Two main units of quartzofeldspathic to garnetiferous quartzofeldspathic gneiss separated by pelitic to psammitic metasedimentary rocks. Basic gneiss locally abundant.|
15683|Purnamoota Subgroup|70405|6|Mentioned|p28, p36, p43 Table 3|Mesoproterozoic|Paleoproterozoic|||Broken Hill Group|Includes Hores Gneiss, Freyers Metasediments|Correlated with Raven Hill Subgroup||
15683|Purnamoota Subgroup|70657|5|Briefly described|p13 Fig.6, p14-15, p17, p40-41|Statherian|Statherian|Curnamona Province; Broken Hill Domain.|<1693 Ma, >1650 Ma|Broken Hill Group|Freyers Metasediments, Parnell and Hores Gneisses.|Underlies Sundown Group. Overlies Allendale Metasediments. Equivalent to Raven Hill Subgroup (Olary Domain).||
15683|Purnamoota Subgroup|70658|6|Mentioned|p15|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Broken Hill Group.||||
15683|Purnamoota Subgroup|73429|5|Briefly described|p106 Fig.2|Statherian|Statherian|Curnamona Province, Broken Hill Domain.||Broken Hill Group||Overlies Allendale Mestasediments, underlies Sundown Group||
15683|Purnamoota Subgroup|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian|||Broken Hill Group|Parnell Formation, Freyers Metasediments, Hores Gneiss|Overlies Allendale Metasediments, underlies Sundown Group||
15730|Quarry Creek Limestone|5253|5|Briefly described|p99, p100, p103.|Wenlock|Llandovery|Overlain by Panuara Formation which contains graptolites originally assigned to the late Llandovery but now believed to be lower Wenlock.||||||16-JAN-12
15730|Quarry Creek Limestone|13996|6|Mentioned|p136|Wenlock|Llandovery|Rugose coral species and affinities with China. See also reference to [probably mis-spelt] Quarry Formation (p129).||||||
15730|Quarry Creek Limestone|22486|6|Mentioned|p 6|||||||||
15730|Quarry Creek Limestone|22857|5|Briefly described|p127, p468 App.1 Tb.A1.6|Llandovery|Llandovery|Of the Waugoola Group. Well-bedded very fossiliferous limestone; basal pebbly lithic sandstone; contains corals, stromatoporoids. Max. thickness: 6m. Geological Province: Molong Rise.||||||
15730|Quarry Creek Limestone|23214|4|Described|p107|||Of Waugoola Group. Not described separately as is too small to depict on the 1:100 000 Molong geological map sheet.||||||
15730|Quarry Creek Limestone|23245|6|Mentioned|p127||Llandovery|||||||
15730|Quarry Creek Limestone|32149|6|Mentioned|p662|||U.Llandovery. Coral described||||||
15730|Quarry Creek Limestone|32150|6|Mentioned|p26|||Refers Stevens & Packham (1955)||||||
15730|Quarry Creek Limestone|32153|6|Mentioned|p54|||Refers McLean (1974)||||||
15730|Quarry Creek Limestone|33125|6|Mentioned|p15|||Correlation chart||||||
15730|Quarry Creek Limestone|33611|6|Mentioned|p130|||Silurian.||||||
15730|Quarry Creek Limestone|34405|4|Described|p110|||||||||
15730|Quarry Creek Limestone|35137|6|Mentioned|p87|||||||||
15730|Quarry Creek Limestone|37727|4|Described|p78|||See also P9.||||||
15730|Quarry Creek Limestone|39331|6|Mentioned|Fig.6-3|||||||||
15730|Quarry Creek Limestone|40328|3|Fully described|p160|||||||||
15730|Quarry Creek Limestone|41048|6|Mentioned|p24|||||||||
15730|Quarry Creek Limestone|41296|6|Mentioned|p130|||||||||
15730|Quarry Creek Limestone|43517|14|Not recorded|p154|||||||||
15730|Quarry Creek Limestone|50096|5|Briefly described|p78|Wenlock|Wenlock|Occurrence of Ozarkodina (new sp.) - one specimen.||||||
15730|Quarry Creek Limestone|60989|6|Mentioned|p112 Fig.1, p113|Early Wenlock|Late Llandovery|Appears as Quarry Creek limestone in Fig.1.||||Is overlain by Panuara Formation.||
15730|Quarry Creek Limestone|61892|6|Mentioned|p216|Wenlock|Llandovery|Contains Acrotretella brachiopods, contrasted with those around the world.||||||
15730|Quarry Creek Limestone|63287|5|Briefly described|p317 Fig. 2, p335|Wenlock|Llandovery|Of Waugoola Group. Geological Province: Molong Volcanic Belt. Consists of fossiliferous limestone.||||||07-FEB-11
15730|Quarry Creek Limestone|73299|6|Mentioned|p1104 Fig.10|Silurian|Early Silurian|Molong High. Lower to middle Silurian age.||||||
15747|Queen Bee Porphyry|29621|6|Mentioned|p5|||||||||
15747|Queen Bee Porphyry|29947|6|Mentioned|p693|||||||||21-JAN-21
15747|Queen Bee Porphyry|32087|6|Mentioned|p69|||||||||
15747|Queen Bee Porphyry|32088|6|Mentioned|p2|||||||||
15747|Queen Bee Porphyry|34449|5|Briefly described|Table 2-1|||U.Silurian - L.Devonian||||||
15747|Queen Bee Porphyry|35385|6|Mentioned|p39|||Refers Rayner(1961,1969)||||||
15747|Queen Bee Porphyry|45003|14|Not recorded|p107|||||||||
15747|Queen Bee Porphyry|69801|6|Mentioned|p1, p135|Silurian|Silurian|Cobar Basin.|417.6 +/- 3 Ma (Black, 2005)|||||21-JAN-21
15747|Queen Bee Porphyry|70210|5|Briefly described|p1, p38|||Cobar-Bourke district. Not significantly older than Byrock and Compton Downs Granites.|417 Ma.|||||
15747|Queen Bee Porphyry|70296|5|Briefly described|p1, p10-11, p19, p24|Pridoli|Pridoli|Cobar district. Has an inherited component ranging in age from 460 Ma-1000 Ma.|417.6 +/- 3 Ma (SHRIMP U-Pb)|||||21-JAN-21
15747|Queen Bee Porphyry|70941|6|Mentioned|p78, p78 fig 32, p152|Devonian|Silurian|Eruption age.|417.6 +/- 3 Ma (Black, 2005)|||Intrudes the Chesney Formation.||21-JAN-21
15747|Queen Bee Porphyry|73174|6|Mentioned|p1039|Lochkovian|Lochkovian|Geochron is magmatic age from Black (2005).|416.9 +/- 2.9 Ma SHRIMP|||Intrudes CSA Siltstone.||24-NOV-22
15747|Queen Bee Porphyry|73578|6|Mentioned|p1, p25, p28|Lochkovian|Pridoli|SHRIMP U-Pb zircon age of 417.6 +/- 3.0 Ma reported by Black (2005).|417.6 +/- 3.0 Ma SHRIMP|||||
15761|Quidong Limestone|22486|6|Mentioned|p 6|||||||||
15761|Quidong Limestone|22768|6|Mentioned|p177||Late Wenlockian|||||||
15761|Quidong Limestone|22815|3|Fully described|p37|Ludlow|Ludlow|Thickness estimated at 130m||||||
15761|Quidong Limestone|22857|4|Described|p177, p466 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Bredbo Group. Massive and bedded limestone grading into shales. Max. thickness: <140m. Geological Province: Quidong Basin.||||||04-AUG-21
15761|Quidong Limestone|23329|5|Briefly described|1042|Late Silurian|Silurian|||||||
15761|Quidong Limestone|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
15761|Quidong Limestone|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
15761|Quidong Limestone|31161|5|Briefly described|PA10|||||||||
15761|Quidong Limestone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
15761|Quidong Limestone|32672|6|Mentioned|p672|||||||||
15761|Quidong Limestone|33125|6|Mentioned|p15|||Correlation chart||||||
15761|Quidong Limestone|33611|6|Mentioned|p132|||||||||
15761|Quidong Limestone|34692|5|Briefly described|p187|||||||||
15761|Quidong Limestone|37727|4|Described|p82|||See also p19 and p29.||||||04-AUG-21
15761|Quidong Limestone|38151|6|Mentioned|Table 1|||||||||
15761|Quidong Limestone|40328|4|Described|p117|||||||||
15761|Quidong Limestone|41905|4|Described|p30|||||||||
15761|Quidong Limestone|41933|5|Briefly described|Map legend|Late Silurian||||||||
15761|Quidong Limestone|43233|5|Briefly described|Map Legend||Ludlow|of Bredbo Group.||||||
15761|Quidong Limestone|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Ss3||||||
15761|Quidong Limestone|46574|5|Briefly described|Map Legend|Late Silurian|Silurian|Of the Yass-Canberra Rise. Geological Province: Lachlan Pre-Cratonic Province.  Bioclastic limestone, mudstone, sandstone.||||||09-NOV-04
15761|Quidong Limestone|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
15761|Quidong Limestone|60988|5|Briefly described|p143-146   |early Ludlovian|Wenlock|Quidong Basin. Highly fossiliferous.||||Overlies the Merriangaah Siltstone unconformably and Tombong Formation disconformably. Is overlain conformably by the Delegate River Mudstone.||
15761|Quidong Limestone|61894|6|Mentioned|p180 |||Delegate area.||||||
15761|Quidong Limestone|63290|6|Mentioned|p396 Fig. 3|Ludlow|Wenlock|||||||
15784|Raceview Formation|12597|5|Briefly described|p491, p492 Tb.1, p494, p500, p501|Rhaetian|Rhaetian|Clarence-Moreton Basin. Contains the oldest coal seams identified in the Surat, Clarence-Moreton and Eromanga Basins.||Unit in Woogaroo Subgroup.|||Sub-labile to quartzose sandstone, siltstone and mudstone; minor thin coal seams.|
15784|Raceview Formation|13516|5|Briefly described|p159 fig 8|Late Triassic|Late Triassic|From Clarence-Moreton Basin.||Of Woogaroo Subgroup||||
15784|Raceview Formation|22757|5|Briefly described|Table5,p10|Late Triassic|Late Triassic|Ipswich-Moreton Basin. 30 m.||||||
15784|Raceview Formation|22857|5|Briefly described|p318-9 Figs. 22.10A, B; p548 Tb A1.12|Early Jurassic|Rhaetian|Of the Woogaroo Subgroup (Bundamba Group). Interbedded sandstone, siltstone, claystone. Max. thickness: 250m. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|22865|6|Mentioned|Fig.22.10ap318|||||||||
15784|Raceview Formation|23799|5|Briefly described|p46|Late Triassic|Late Triassic|Of Woogaroo Subgroup.  Overlain by Ripley Road Sandstone; overlies Aberdare Conglomerate.  Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|23811|5|Briefly described|Map Legend|Rhaetian|Rhaetian|Of Woogaroo Subgroup. Thinly interbedded, fine- to medium-grained, quartz-lithic and quartz sandstone, silty sandstone, grey to buff siltstone and claystone, carbonaceous siltstone, claystone, minor laminite, coaly bands.Geol:Prov: Clarence-Moreton Basin.||||||20-DEC-04
15784|Raceview Formation|23812|5|Briefly described|p35 Tb.4|Late Triassic|Late Triassic|Of Bundamba Group.  Maximum thickness: 250m.  Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|23843|5|Briefly described|p456 Table 1|Jurassic|Late Triassic|Of Woogaroo Sub-Group. Geological Province:Moreton Basin.  Maximum thickness: 140m.||||||
15784|Raceview Formation|24081|5|Briefly described|p451|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group.  Geological Province: Nambour Basin.||||||
15784|Raceview Formation|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|29385|6|Mentioned|p82|||Jurassic.||||||
15784|Raceview Formation|29386|6|Mentioned|p454|||Upper Triassic.||||||
15784|Raceview Formation|30086|5|Briefly described|p4|||Triassic age. Part of Bundamba Group.||||||
15784|Raceview Formation|30087|4|Described|p3|||Unit of Bundamba Group. See also p4.||||||17-SEP-18
15784|Raceview Formation|30302|6|Mentioned|p415|||Refers to Staines(1964)||||||
15784|Raceview Formation|30458|6|Mentioned|p1|||See also p40.||||||17-SEP-18
15784|Raceview Formation|30459|6|Mentioned|p309|||||||||
15784|Raceview Formation|30461|6|Mentioned|p100|||||||||
15784|Raceview Formation|30463|6|Mentioned|p466|||Palynology. See also p464,467,471.||||||17-SEP-18
15784|Raceview Formation|30464|6|Mentioned|p3|||||||||
15784|Raceview Formation|30465|6|Mentioned|p4|||||||||
15784|Raceview Formation|30466|6|Mentioned|p3|||||||||
15784|Raceview Formation|30470|6|Mentioned|p459|||||||||
15784|Raceview Formation|30471|6|Mentioned|p129|||Miospore assemblages listed in Appendix.||||||
15784|Raceview Formation|30472|6|Mentioned|p132|||Pollen distribution.||||||
15784|Raceview Formation|30474|6|Mentioned|p251|||Correlation chart on p251.||||||17-SEP-18
15784|Raceview Formation|30475|6|Mentioned|p160|||||||||
15784|Raceview Formation|30477|6|Mentioned|p461|||||||||
15784|Raceview Formation|30478|6|Mentioned|p461|||||||||
15784|Raceview Formation|30508|6|Mentioned|p87|||Mesozoic age. Redbank Plains form Station site||||||
15784|Raceview Formation|30517|6|Mentioned|p436|||||||||
15784|Raceview Formation|30565|6|Mentioned|p129|||||||||
15784|Raceview Formation|30701|6|Mentioned|Map legend|Triassic|Triassic|||||||
15784|Raceview Formation|30915|6|Mentioned|p100|||||||||
15784|Raceview Formation|30916|6|Mentioned|p99|||||||||
15784|Raceview Formation|31118|4|Described|p320|||||||||
15784|Raceview Formation|31259|6|Mentioned|p325|||Refers Staines (1964).||||||17-SEP-18
15784|Raceview Formation|32136|6|Mentioned|p5|||Miospores||||||
15784|Raceview Formation|32176|6|Mentioned|p2|||Bundamba Gp. See also p3, Figs. 2&3.||||||17-SEP-18
15784|Raceview Formation|32179|6|Mentioned|p3|||Trias.||||||
15784|Raceview Formation|32180|6|Mentioned|Table 1|||||||||
15784|Raceview Formation|32492|6|Mentioned|Map legend|Late Triassic|Late Triassic|||||||
15784|Raceview Formation|32801|6|Mentioned|p266|||||||||
15784|Raceview Formation|32803|6|Mentioned|p95|||||||||
15784|Raceview Formation|33381|4|Described|p110|||See also pp115,117,118,122,Late Triassic. Map.||||||17-SEP-18
15784|Raceview Formation|33476|6|Mentioned|p99|||||||||
15784|Raceview Formation|34010|6|Mentioned|Cor. chart|||U.Triassic||||||
15784|Raceview Formation|34354|6|Mentioned|p3|||Triassic. See also p12.||||||17-SEP-18
15784|Raceview Formation|34457|6|Mentioned|p484|||Cor. with Borallon Beds||||||
15784|Raceview Formation|34505|6|Mentioned|p3|||Bundamba Group. See Figs.8,9,10,11||||||
15784|Raceview Formation|35079|6|Mentioned|p424|||||||||
15784|Raceview Formation|35101|6|Mentioned|p51|||||||||
15784|Raceview Formation|35901|6|Mentioned|p11|||||||||
15784|Raceview Formation|36237|6|Mentioned|Map legend|Late Jurassic|Late Triassic|Late Triassic to Early Jurassic||||||
15784|Raceview Formation|36243|6|Mentioned|Table 8A|||||||||
15784|Raceview Formation|36351|6|Mentioned|p373|||||||||
15784|Raceview Formation|36354|4|Described|p371|||||||||
15784|Raceview Formation|36779|6|Mentioned|p7|||||||||
15784|Raceview Formation|36825|6|Mentioned|p7|||||||||
15784|Raceview Formation|36899|6|Mentioned|p1085|||See also p1095.||||||17-SEP-18
15784|Raceview Formation|37111|6|Mentioned|Table 1|||||||||
15784|Raceview Formation|37122|5|Briefly described|Table 1|||||||||
15784|Raceview Formation|37375|4|Described|p474|||||||||
15784|Raceview Formation|37456|6|Mentioned|p268|||||||||
15784|Raceview Formation|37463|6|Mentioned|p483|||||||||
15784|Raceview Formation|37616|6|Mentioned|p33|||||||||
15784|Raceview Formation|37812|6|Mentioned|p657|||||||||
15784|Raceview Formation|38074|5|Briefly described|Table 1|||||||||
15784|Raceview Formation|38076|6|Mentioned|Table 3|||||||||
15784|Raceview Formation|38306|6|Mentioned|p509|||||||||
15784|Raceview Formation|38307|4|Described|p521|||||||||
15784|Raceview Formation|38441|6|Mentioned|Map legend|Rhaetian|Rhaetian|||||||
15784|Raceview Formation|39445|5|Briefly described|Table 10|||||||||
15784|Raceview Formation|39907|4|Described|p10|||Sedimentology||||||
15784|Raceview Formation|39943|6|Mentioned|Table 10A|||||||||
15784|Raceview Formation|40623|5|Briefly described|p32|||||||||
15784|Raceview Formation|41591|5|Briefly described|p19|||||||||
15784|Raceview Formation|41631|4|Described|p9|||See also Fig.2.||||||17-SEP-18
15784|Raceview Formation|41906|3|Fully described|Table 2 p16|||||||||17-SEP-18
15784|Raceview Formation|42248|6|Mentioned|p397|||||||||
15784|Raceview Formation|42316|6|Mentioned|p5|||||||||
15784|Raceview Formation|42336|5|Briefly described|Table 1 P5|||||||||
15784|Raceview Formation|42405|6|Mentioned|Table 3 P.7|||||||||
15784|Raceview Formation|42463|6|Mentioned|Fig.3 P170|||||||||
15784|Raceview Formation|42525|5|Briefly described|Map legend|Early Jurassic|Late Triassic|Of the Woogaroo Sub-Group (Bundamba Group).||||||15-JUL-04
15784|Raceview Formation|42869|5|Briefly described|Table 1, p33|||of Woogaroo Subgroup||||||17-SEP-18
15784|Raceview Formation|42893|5|Briefly described|Fig.2 p7|||||||||17-SEP-18
15784|Raceview Formation|42894|5|Briefly described|Fig.1 p20|||||||||17-SEP-18
15784|Raceview Formation|43150|5|Briefly described|Map Legend||Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Ipswich Basin.||||||12-APR-05
15784|Raceview Formation|43736|5|Briefly described|Table 1,p4|||||||||
15784|Raceview Formation|43910|14|Not recorded|p1,3,14,17,18,Fig.2|||||||||
15784|Raceview Formation|44450|5|Briefly described|p27|||Overlying unit Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|44633|14|Not recorded|p2|||||||||
15784|Raceview Formation|44734|14|Not recorded|p5,12,13,19|||Pine Mountain area.||||||
15784|Raceview Formation|44774|2|Defined|p30-32||Late Triassic|Conformable with both the overlying Ripley Road Sandstone and the underlying Aberdare Conglomerate.||||||
15784|Raceview Formation|44775|4|Described|p9||Late Triassic|||||||
15784|Raceview Formation|44776|14|Not recorded|p4,fig.3||Late Triassic|||||||
15784|Raceview Formation|44884|4|Described|p2,3,Figs.1,7|||||||||
15784|Raceview Formation|44885|14|Not recorded|p2,3|||||||||
15784|Raceview Formation|45110|3|Fully described|p82|||See also Table 17.||||||
15784|Raceview Formation|48917|5|Briefly described|p13|||See Table 2. Upper Triassic||||||
15784|Raceview Formation|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Of the Woogaroo Subgroup.  Sandstone, siltstone, claystone, conglomerate and minor coal.||||||
15784|Raceview Formation|60281|5|Briefly described|p27, p30, Fig. 18 App. 1|Late Triassic|Late Triassic|Of Woogaroo Subgp (Bundamba Gp).  Shale, siltstone and sst., giving way to a quartz sandstone-dominated sequence, the overlying Ripley Road Sandstone; overlies Laytons Range Conglom., Ipswich C.M.  Max. thick: 250m.  Geol.Prov: Clarence-Moreton Basin.||||||27-APR-05
15784|Raceview Formation|60993|4|Described|p4, p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup. Mixed labile to quartsoze sst and shale sequence of interbedded sandstone, siltstone, shale; minor coal. Unconformably overlies Evans Head Coal Measures. Geol.Prov: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60995|4|Described|p59, p51 Fig. 3|Late Triassic|Late Triassic|Of Woogaroo Subgp. Was correlated with "Mill Creek Siltstone". Overlain by Ripley Road Sst; overlies Laytons Range Congom; Evans Head Coal. Mes. (which may be misidentified Raceview Fm).  Max. thick: 250m.  Geol. Prov: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60996|5|Briefly described|p72, p81|||Overlain by Ripley Road Sandstone. Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|60997|5|Briefly described|p139 Fig. 1|Rhaetian|Rhaetian|Geological Province: Clarence-Moreton Basin. See also p140 Fig. 2.||||||
15784|Raceview Formation|60999|5|Briefly described|p164, p176|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Overlies the Laytons Range Conglomerate in several boreholes in NSW. Geological Province: Clarence-Moreton Basin. See also p169, p172 Fig. 6..||||||
15784|Raceview Formation|61002|5|Briefly described|p202|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.  See also p199 Fig. 3.||||||
15784|Raceview Formation|61004|5|Briefly described|p232 Fig. 2|Triassic|Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological Province: Clarence-Moreton Basin.||||||
15784|Raceview Formation|61005|5|Briefly described|p239, p242|||Geological Province: Clarence-Moreton Basin. See also p255 Figs. 23, 24 and 25.||||||
15784|Raceview Formation|61006|5|Briefly described|p277, p289|Triassic|Triassic|Mudstone, sandstone, composition variable. Some good hydrocarbon shows. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p286.||||||
15784|Raceview Formation|61310|5|Briefly described|p21, Table C1 (p22-23)|||Of the Woogaroo Subgroup. Pebble/cobble conglomerate, minor sandstone. Geological Province: Clarence-Moreton Basin||||||
15784|Raceview Formation|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Woogaroo Subgroup (Bundamba Group). Geological province: Clarence-Moreton Basin.||||||07-FEB-11
15784|Raceview Formation|64665|5|Briefly described|p53 Fig.2, p59.|Late Triassic|Late Triassic|Clarence-Moreton Basin. Fluvio-lacustrine deposits.||Unit in Woogaroo Subgroup.||Overlies Aberdare and Laytons Range Conglomerates. Is overlain by Ripley Road Sandstone.|Includes thin coal seams.|
15784|Raceview Formation|64856|6|Mentioned|p80|Rhaetian|Norian|Moreton Basin. Base of Bundamba Group.|| ||||29-NOV-17
15784|Raceview Formation|67402|4|Described|p165 tbl LPB1, p187|Norian|Norian|Clarence-Moreton Basin. Deposited in a fluvial system with suspended load channels. Approximately 100m thick. Sandstones are often reservoirs and potential reservoirs for the storage of carbon dioxide. See also p188, p190 fig CLM6, p192, p193, p223, p225.||Woogaroo Subgroup||Overlies the Aberdare and Laytons Range Conglomerates. Overlain by the Ripley Road Sandstone.|Interbedded sandstone, siltstone and claystone with minor coal deposits.|
15784|Raceview Formation|69297|5|Briefly described|p487 fig 5.38, p488, p490|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. Between 1-250m thick. Potential reservoir rock.||Woogaroo Subgroup||Overlies the Laytons Range Conglomerate. Overlain by the Ripley Road Sandstone.||
15784|Raceview Formation|69594|5|Briefly described|p519, p524, p534, p543-544,p546-547,p572|Late Triassic|Late Triassic|Clarence-Moreton Basin. Generally poorly outcropping.||Woogaroo Subgroup.||Overlies Aberdare Conglomerate (=Laytons Range Conglomerate in NSW); both are equivalent to the Eddystone beds. Is overlain by Ripley Road Sandstone. Equivalent to Eddystone beds.|Mudstone and siltstone predominate over sandstones (mostly feldspathic lithic and lithic); few minor conglomerates; cross-bedding and ripple cross-laminations fairly common.|
15784|Raceview Formation|69790|6|Mentioned|p1063 Fig.2|Triassic|Triassic|Northern Clarence-Moreton Basin area.||||||
15784|Raceview Formation|70821|5|Briefly described|p80|||Clarence-Moreton Basin. Shown as including Aberdare Conglomerate member.||Woogaroo Subgroup.||Is overlain by Ripley Road Sandstone.||
15784|Raceview Formation|72297|5|Briefly described|p700|||Clarence-Moreton Basin.||||Equivalent to Tiaro Coal Measures.||
15784|Raceview Formation|73570|6|Mentioned|p912 Fig.2|||||||Overlies Laytons Range Conglomerate||
15797|Raggatt Volcanics|22831|3|Fully described|p 28||Late Ordovician|||||||
15797|Raggatt Volcanics|22857|5|Briefly described|p416 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Andesitic lavas and volcanogenic arenite, horizons of limestone.||||||
15797|Raggatt Volcanics|36066|5|Briefly described|p9|||||||||
15797|Raggatt Volcanics|39660|6|Mentioned|p450|||||||||
15797|Raggatt Volcanics|39663|6|Mentioned|p348|||||||||
15797|Raggatt Volcanics|40365|2|Defined|p329|Early Devonian|Late Silurian|Late Silurian - Early Devonian||||||
15797|Raggatt Volcanics|41869|4|Described|p4|||||||||
15797|Raggatt Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
15797|Raggatt Volcanics|43441|4|Described|16|||Correlated with Goonumbla Volcanics. Age: ?Late Ordovician - pre Late Silurian||||||08-JAN-10
15797|Raggatt Volcanics|44093|5|Briefly described|p178 App. 1|Ordovician|Ordovician|Of the Parkes Zone. Geological Province: Lachlan Fold Belt.||||||
15797|Raggatt Volcanics|44160|5|Briefly described|Map Legend|Llandoverian|Darriwilian|||||||08-JAN-10
15797|Raggatt Volcanics|63278|5|Briefly described|p145 Fig. 1, p150|Late Odrovician|Late Ordovician|Of Northparkes Group. Geol Prov: Junee-Narromine Volcanic Belt, LFB. Comprises andesitic to trachyandesitic lavas, tuffs, volcaniclastic breccias + possibly allochthonous fossiliferous limestones. Sherwin (1996) correlated unit Goonumbla Volcanics.||||||07-FEB-11
15797|Raggatt Volcanics|67322|4|Described|p22|Katian|Katian|Now included in the Northparkes Group. Named by Sherwin (1996). Contains Eastonian corals and conodonts. Age assumed to be similar to that of the Northparkes Group. Occurs in the Junee-Narromine region.||Of the Northparkes Group.||Correlative of the Goonumbla Volcanics.|Andesitic to trachyandesitic lavas, tuffs, volcaniclastic breccias and sparse fossiliferous limestones.|22-FEB-18
15797|Raggatt Volcanics|70684|6|Mentioned|p3, p54|||Junee-Narromine Volcanic Belt.||Northparkes Group.||||
15797|Raggatt Volcanics|72495|5|Briefly described|p218-219,222, p226, p233, 240|Late Ordovician|Late Ordovician|Outcrops as three small bodies west of the Tullamore Syncline. Structural characteristics are described.||Northparkes Group||In fault contact with the Hervey Group and the Gobondry Granite.|Andesitic and trachyandesitic volcanic rocks, volcaniclastic rocks and monzonitic intrusives. Associated limestone float contains a Late Ordovician fauna.|30-MAR-20
15810|Rainbow Hill Member|24248|5|Briefly described|p52, 54|||Formely "Phacops Bed" (Jenkins, 1879) and "Middle Trilobite Bed" (Mitchell, 1887). Strongly bioturbated calcareous siltstone.||||||
15810|Rainbow Hill Member|37727|4|Described|p59|||Variation of Rainbow Hill Marl Member.||||||
15810|Rainbow Hill Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Rosebank Shale (Hattons Corner Group).  Formerly known as the "Middle Trilobite bed".  Highly fossiliferous mudstone, shale, siltstone and impure limestone.||||||10-MAY-04
15810|Rainbow Hill Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Rosebank Shale (Hattons Corner Group). Highly fossiliferous mudstone, shale, siltstone and impure limestone. Formerly known as "Middle Trilobite bed".||||||09-SEP-08
15810|Rainbow Hill Member|68592|2|Defined|p430 Fig.89, p560, p562, p590, p594-7|Ludlow|Ludlow|See also p1883-4. Owen and Wyborn (1979); Strusz and Garratt (1999). Formerly 'Middle Trilobite Bed', later Rainbow Hill Marl Member (Link, 1970, 1971). Type locality and good exposures are described. Forms an excellent marker horizon, even though thickness is only 2.3-8m. Richly fossiliferous, particularly of trilobites: fauna listed. Late Ludlow.||Unit in Rosebank Shale.||Conformably overlies Black Bog Shale.|Thin, persistent, strongly bioturbated, highly fossiliferous horizon of siltstone, mudstone, shale, minor calcareous siltstone and limestone.|
15810|Rainbow Hill Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shrr. [Previously known as] "Middle Trilobite Bed". On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Rosebank Shale (basal unit?)||Overlies Black Bog Shale.|Strongly bioturbated, highly fossiliferous siltstone, mudstone and shale; minor calcareous siltstone and limestone.|
15810|Rainbow Hill Member|70540|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Middle Trilobite Bed".||Rosebank Shale|||Strongly bioturbated, highly fossiliferous siltstone, mudstone and shale; minor calcareous siltstone and limestone.|
15810|Rainbow Hill Member|70546|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Middle Trilobite Bed".||Rosebank Shale|||Strongly bioturbated, highly fossiliferous siltstone, mudstone and shale; minor calcareous siltstone and limestone ("middle trilobite bed").|
15810|Rainbow Hill Member|71656|6|Mentioned|p12 Fig.2, p26-27|Ludlow|Ludlow|Diverse fauna of this member include many trilobite varieties, rugose coral, bivalves and echinoderms. This fauna inhabited quiet deeper water environments. Previously the 'Middle Trilobite Bed' of Etheridge and Mitchell (1895,1897) and others.||Of Rosebank Shale, Hattons Corner Group||Overlies Black Bog Shale.|Fossiliferous.|
15819|Ramrod Creek Coal Member|29942|4|Described|Fig.1|||Permian||||||
15819|Ramrod Creek Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
15835|Rangari Limestone Member|721|5|Briefly described|Map legend|Tournaisian|Tournaisian|Of the Tulcumba Formation (Parry Group).  Fine-grained oolitic and minor bioclastic limestone.||||||21-DEC-04
15835|Rangari Limestone Member|22857|5|Briefly described|p496 App.1 Tb.A1.7|Tournaisian|Tournaisian|Of the Tulcumba Sandstone (Parry Group). Fine-grained oolitic and minor bioclastic limestone. Max. thickness: 5m. Geological Province: Tamworth Forearc Basin.||||||
15835|Rangari Limestone Member|31519|6|Mentioned|Text Fig.1|||||||||
15835|Rangari Limestone Member|32286|6|Mentioned|Fig. 3|||||||||
15835|Rangari Limestone Member|34262|6|Mentioned|p242|||||||||
15835|Rangari Limestone Member|36528|6|Mentioned|p175|||||||||
15835|Rangari Limestone Member|37987|6|Mentioned|p225|||||||||
15835|Rangari Limestone Member|38215|6|Mentioned|Fig.2|||||||||
15835|Rangari Limestone Member|41009|6|Mentioned|Fig.2|||||||||
15835|Rangari Limestone Member|42547|5|Briefly described|p20|||of Tulcumba Sandstone.||||||
15835|Rangari Limestone Member|43091|5|Briefly described|Map legend|||of Parry Group||||||
15835|Rangari Limestone Member|43409|14|Not recorded|Map Legend|||"5-8ft thick oolitic lstn inc.fossil debris,detrital feldspathic rock frags and calcic feldspars."||||||
15835|Rangari Limestone Member|43418|14|Not recorded|Map Legend|||||||||
15835|Rangari Limestone Member|43432|14|Not recorded|p202||Early Carboniferous|||||||
15835|Rangari Limestone Member|45097|6|Mentioned|Fig.|||Correlation chart.||||||
15835|Rangari Limestone Member|66720|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|||Unit in Tulcumba Sandstone.|||Fine-grained, oolitic crinoidal limestone; minor bioclastic limestone and limestone conglomerate.|
15835|Rangari Limestone Member|70050|6|Mentioned|p318, p360-361, p366|Tournaisian|Tournaisian|Rangari area. Contains Pickettodendron (new genus) coral fossils (illustrations and systematic palaeontology), including the holotype of P. williamsi. Referred to as the Rangari Limestone on p366.||||||16-APR-18
15840|Rankin Formation|22857|5|Briefly described|p213, p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Cocoparra Group. Sandstone-siltstone sequence with conglomerates, some polymictic. Max. thickness: 1580m. Geological Province: Barka Basin.||||||
15840|Rankin Formation|22859|6|Mentioned|p213|||||||||
15840|Rankin Formation|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15840|Rankin Formation|34109|4|Described|Table 3.11|||||||||
15840|Rankin Formation|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15840|Rankin Formation|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
15840|Rankin Formation|43507|14|Not recorded|p125|||||||||
15840|Rankin Formation|43509|14|Not recorded|p113,117|||Formation of Cocoparra Group||||||
15840|Rankin Formation|43511|14|Not recorded|p129,132,134,139-149||Late Devonian|||||||
15840|Rankin Formation|44534|5|Briefly described|map legend||Late Devonian|SI 55-6. Includes the Mailman Gap Conglomerate Member and undifferentiated material of Upper Devonian age. O/lies Jimberoo Member of the Womboyne Formation, U/lies Tertiary sediments.||||||
15840|Rankin Formation|61964|3|Fully described|p14 Fig. 4, p125-126, p114, p117 Fig. 35|Famennian|Famennian|Of Cocoparra Group. Includes: Mailman Gap, Byawatha Conglomerate and Essex Members. Remaining sandstones of unit conformably overlie basal Mailman Gap Member. Detailed lithology included. Max. thickness: >1km (est.). Palaeontology of unit (p261)||||||
15840|Rankin Formation|62405|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Cocoparra Group. Includes Mailman Gap, Byawatha Conglomerate and Essex embers. Purple-brown, medium-grained trough to tabular corss-bedded quartz sandstone, minor pebbly quartz sandstone, conglomerate (vein quartz and quartzite clasts), siltstone.||||||25-MAR-08
15840|Rankin Formation|69161|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|Includes Mailman Gap Member.|Overlies Jimberoo Formation.|Purple-brown, medium-grained trough to tabular cross-bedded quartz sandstone, minor pebbly quartz sandstone, conglomerate (vein quartz and quartzite clasts), siltstone.|
15840|Rankin Formation|69162|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|Includes Mailman Gap Member, Essex Member, and Byawatha Conglomerate Member.||Purple-brown, medium-grained trough to tabular cross-bedded quartz sandstone, minor pebbly quartz sandstone, conglomerate (vein quartz and quartzite clasts), siltstone.|03-NOV-15
15840|Rankin Formation|69163|5|Briefly described|Map legend|Late Devonian|Late Devonian|||Unit in Cocoparra Group.|Includes Mailman Gap Member and Essex Member.|Is faulted against Square Head Formation.|Purple-brown, medium-grained trough to tabular cross-bedded quartz sandstone, minor pebbly quartz sandstone, conglomerate (vein quartz and quartzite clasts), siltstone.|03-NOV-15
15840|Rankin Formation|71040|5|Briefly described|p28 Fig.15|Devonian|Devonian|Diagram of major faults and contractional deformation related to Tabberabberan Orogeny.||Cocoparra Group.|Mailman Gap Member.|||
15840|Rankin Formation|71889|5|Briefly described|p48, p56|||Rankin Springs area.||Cocoparra Group||Equivalent to the Cocoparra Group, Upper.|Cross bedded and cross-laminated sandstone, pebbly sandstone and siltstone.|
15841|Ranmoor Member|23430|4|Described|p524 Table 14.7|||Of Wallumbilla Formation. Eromanga Basin Province.||||||
15841|Ranmoor Member|23982|5|Briefly described|p58 Fig.18|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|24092|5|Briefly described|p8 Fig.3|||Of Wallumbilla Formation. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|30020|6|Mentioned|p33|||||||||
15841|Ranmoor Member|30024|6|Mentioned|p332|||||||||
15841|Ranmoor Member|30042|6|Mentioned|p5|||Tambo faunas correlation.||||||
15841|Ranmoor Member|30443|6|Mentioned|p14|||Albian age||||||
15841|Ranmoor Member|31208|6|Mentioned|p48|||||||||
15841|Ranmoor Member|32314|6|Mentioned|Fig. 4|||||||||
15841|Ranmoor Member|33016|6|Mentioned|p1|||On table||||||
15841|Ranmoor Member|33017|6|Mentioned|p6|||||||||
15841|Ranmoor Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33165|6|Mentioned|Chart|||Correlation chart only||||||
15841|Ranmoor Member|33175|5|Briefly described|p280|||||||||
15841|Ranmoor Member|33182|6|Mentioned|Table 1|||L.Cret.||||||
15841|Ranmoor Member|33368|6|Mentioned|p25|||Strat. table.||||||
15841|Ranmoor Member|33414|6|Mentioned|p212,Tb.||Cretaceous|Part of Wallumbilla Formation.||||||
15841|Ranmoor Member|33638|5|Briefly described|Table 1|||||||||
15841|Ranmoor Member|33640|6|Mentioned|p12|||||||||
15841|Ranmoor Member|33642|6|Mentioned|144,147-8,Tb.1,Fig.2|||Refers Vine & Day(1965). Lower part-Lower Albian fauna, upper part has possible Middle Albian fossils.||||||
15841|Ranmoor Member|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
15841|Ranmoor Member|33648|6|Mentioned|p21|||Strat.||||||
15841|Ranmoor Member|34091|5|Briefly described|Table 1|||L.Cret||||||
15841|Ranmoor Member|35239|6|Mentioned|p265|||||||||
15841|Ranmoor Member|35560|6|Mentioned|p291|||||||||
15841|Ranmoor Member|35793|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|35811|6|Mentioned|p556|||Exploration carried out.||||||
15841|Ranmoor Member|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
15841|Ranmoor Member|36552|6|Mentioned|p61|||||||||
15841|Ranmoor Member|36571|6|Mentioned|Table 4|||||||||
15841|Ranmoor Member|38199|6|Mentioned|p428|||See also P429.||||||
15841|Ranmoor Member|38814|6|Mentioned|Table 1|||||||||
15841|Ranmoor Member|39211|5|Briefly described|Fig.3|||See also Figs 9,11,12 etc.Correlation||||||
15841|Ranmoor Member|40801|6|Mentioned|p46|||||||||
15841|Ranmoor Member|40926|6|Mentioned|Table 2|||||||||
15841|Ranmoor Member|41086|3|Fully described|Fig.3|||||||||
15841|Ranmoor Member|41088|6|Mentioned|p141|||||||||
15841|Ranmoor Member|41266|6|Mentioned|Fig.3|||||||||
15841|Ranmoor Member|44082|6|Mentioned|p10,18-20,Tb.p34||Albian|(Early Albian) Part of Wallumbilla Formation. Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
15841|Ranmoor Member|44087|14|Not recorded|p4,opp.7|||||||||
15841|Ranmoor Member|44089|14|Not recorded|Tb.1,p4||Early Cretaceous|(Wilgunya Formation)||||||
15841|Ranmoor Member|44346|14|Not recorded|p4,opp.p5||Aptian|?Aptian||||||
15841|Ranmoor Member|44352|14|Not recorded|Map Legend||Early Cretaceous|||||||
15841|Ranmoor Member|44373|14|Not recorded|p20|||Map only.||||||
15841|Ranmoor Member|44374|14|Not recorded|p12|||Albian in lower part, highly mudstone sequence, with carbonaceous interval, equivalent to non-marine Coreena Member.||||||
15841|Ranmoor Member|44406|14|Not recorded|p4,opp.p6|||Member of Wilgunya Formation.||||||
15841|Ranmoor Member|44408|14|Not recorded|p4,opp.p6||Aptian|||||||
15841|Ranmoor Member|44414|14|Not recorded|p110-112,114||Cretaceous|Correlated with Coreena Member.||||||
15841|Ranmoor Member|44417|2|Defined|p416,418-420||Albian|(Early Albian)||||||
15841|Ranmoor Member|44915|14|Not recorded|p18||Early Cretaceous|Ref. to Vine and Day 1965.||||||
15841|Ranmoor Member|45132|6|Mentioned|p11|||||||||
15841|Ranmoor Member|45145|6|Mentioned|p61|||||||||
15841|Ranmoor Member|46791|6|Mentioned|p44|||||||||
15841|Ranmoor Member|46937|6|Mentioned|Fig.10|||||||||
15841|Ranmoor Member|48908|14|Not recorded|Tb.1||Early Cretaceous|||||||
15841|Ranmoor Member|48920|6|Mentioned|p60|||See also Table 8. Refers Vine & Day (1965)||||||
15841|Ranmoor Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
15841|Ranmoor Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
15841|Ranmoor Member|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Of Wallumbilla Formation. Overlies Jones Valley Member. Geological Province: Eromanga Basin.||||||
15841|Ranmoor Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Wallumbilla Formation.||||
15841|Ranmoor Member|66623|6|Mentioned|p262.|||Equivalent to Coreena Member in NSW.||Unit in Rolling Downs Group in Queensland.||||
15841|Ranmoor Member|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Cretaceous|Cretaceous|Eromanga/Carpentaria Basins.||Wallumbilla Formation.|||Mudstone, commonly carbonaceous, minor siltstone.|
15841|Ranmoor Member|67784|5|Briefly described|p25-26, p28 Tb.1, p29, p31-33|Albian|Aptian|60-95m thick. Northern Eromanga Basin.||Wallumbilla Formation||Paraconformably overlies Jones Valley Member. Is overlain by Toolebuc Formation.||08-FEB-18
15841|Ranmoor Member|68206|5|Briefly described|p32-33|Albian|Albian|NE Eromanga Basin.||Wallumbilla Formation.||Overlies Jones Valley Member. Is overlain by Toolebuc Formation.||
15841|Ranmoor Member|69457|6|Mentioned|p41:10|||Eromanga Basin. This and other Members of Wallumbilla Formation are not recognised in the NT.||Wallumbilla Formation.||||12-JUL-16
15841|Ranmoor Member|69594|4|Described|p522, p526, p528|Albian|Albian|Vine and Day (1965). Eromanga Basin. The type section is near Glendower Station, E of Hughenden. Crops out in a discontinuous band from Glendower to NW of Richmond. No equivalent units have been identified. Thickness generally 60-95m; may be up to 312m. Contains early Albian ammonite, bivalves and belemnites.||Wallumbilla Formation.||Conformably overlies Jones Valley Member.|Dominated by mudstone and siltstone, with minor labile sandstone.|
15841|Ranmoor Member|70860|6|Mentioned|p281|||Great Artesian Basin.||Wallumbilla Formation.||||
15841|Ranmoor Member|72297|5|Briefly described|p753|||Eromanga Basin.||Wallumbilla Formation.||Is overlain conformably by the Toolebuc Formation.|Blue shale.|
15841|Ranmoor Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD).||Wallumbilla FZ.||Overlies Jones Valley Member. Is overlain by Toolebuc FZ.||
15860|Ravendale Formation|9250|5|Briefly described|Map legend|Late Devonian|Late Devonian|Of the Mulga Downs Group.  White clayey quartz sandstone.||||||
15860|Ravendale Formation|22518|4|Described|Table 1, p 6||Late Devonian|Of the Mulga Downs Group.||||||11-SEP-07
15860|Ravendale Formation|22580|5|Briefly described|p87|Carboniferous|Middle Devonian|||||||
15860|Ravendale Formation|22671|5|Briefly described|p833-34,Fig2p837|Carboniferous|Late Devonian|Quartz sandstone. Unconformably overlies Snake Cave Sandstone.||||||17-JAN-06
15860|Ravendale Formation|22730|5|Briefly described|p557||Late Devonian|||||||
15860|Ravendale Formation|22857|4|Described|p210, p486 App.1 Tb.A1.7|Late Devonian|Late Devonian|Quartz arenite interbedded with red sandy shale. Unconformably overlies Snake Cave Sandstone. Max. thickness: >1500m. Geological Province: Ravendale Basin.||||||
15860|Ravendale Formation|22859|4|Described|p210||Late Devonian|||||||
15860|Ravendale Formation|23336|5|Briefly described|p4, p8 Fig. 5|Famennian|Famennian|Unconformable over Mount Daubeny Formation.||||||21-MAR-06
15860|Ravendale Formation|23380|5|Briefly described|p109,119|Late Devonian|Middle Devonian|Equivalent to Nundooka Sandstone and upper Mulga Downs Group. Age: Givetian - Famennian. of Wonaminta Block.||||||
15860|Ravendale Formation|23469|4|Described|p 322|||Of the Mulga Down Group.||||||11-SEP-07
15860|Ravendale Formation|23833|5|Briefly described|p256 Table 1|Carboniferous|Devonian|||||||
15860|Ravendale Formation|24345|4|Described|p86, p85 Fig. 2|Famennian|Givetian|Mapped as Snake Cave Sandstone in error by Buckley (2000) and Stevens et al (2002).  Thickness: >1000m.  Underlain by Ponto Group.  Geological Province: Wonominta Block.||||||11-SEP-07
15860|Ravendale Formation|29991|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
15860|Ravendale Formation|30683|6|Mentioned|Table 1|||||||||
15860|Ravendale Formation|30908|6|Mentioned|Map legend|Carboniferous|Late Devonian|Carboniferous ? Upper Devonian||||||
15860|Ravendale Formation|31705|6|Mentioned|Fig. 1|||||||||
15860|Ravendale Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
15860|Ravendale Formation|32672|6|Mentioned|p674|||||||||
15860|Ravendale Formation|32677|5|Briefly described|p10|||||||||
15860|Ravendale Formation|32865|4|Described|p485|||||||||
15860|Ravendale Formation|32918|4|Described|p16|||||||||11-JAN-10
15860|Ravendale Formation|33004|6|Mentioned|Fig.8|||||||||
15860|Ravendale Formation|33732|5|Briefly described|p103|||||||||
15860|Ravendale Formation|34400|6|Mentioned|p2|||?Upper Devonian||||||
15860|Ravendale Formation|34401|4|Described|p71|||||||||
15860|Ravendale Formation|34469|6|Mentioned|p107|||Table. See also P116. Devonian||||||
15860|Ravendale Formation|34550|5|Briefly described|Table 2.1|||?Late Devonian||||||
15860|Ravendale Formation|38277|6|Mentioned|p154|||||||||
15860|Ravendale Formation|41276|6|Mentioned|p74|||||||||
15860|Ravendale Formation|41492|6|Mentioned|Fig.10|||||||||
15860|Ravendale Formation|42121|5|Briefly described|p98|||See also Fig.2b||||||
15860|Ravendale Formation|42298|6|Mentioned|p29 (p101a)|||||||||
15860|Ravendale Formation|42364|5|Briefly described|p199|||Also Fig.1 Fig.2||||||
15860|Ravendale Formation|42460|5|Briefly described|Fig.1 P206|||||||||
15860|Ravendale Formation|43263|6|Mentioned|Map Legend|Early Carboniferous|Late Devonian|||||||
15860|Ravendale Formation|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
15860|Ravendale Formation|43368|14|Not recorded|Map Legend|||||||||
15860|Ravendale Formation|43371|14|Not recorded|Map Legend||Late Devonian|||||||11-JAN-10
15860|Ravendale Formation|43383|14|Not recorded|p14,15|||||||||
15860|Ravendale Formation|43390|14|Not recorded|p14|||||||||
15860|Ravendale Formation|43501|14|Not recorded|Map Legend|Carboniferous|Devonian|(Provisional Edition)||||||
15860|Ravendale Formation|43502|14|Not recorded|Map Legend|Carboniferous|Late Devonian|(Provisional Edition)||||||
15860|Ravendale Formation|43704|5|Briefly described|Fig.1,p68|Carboniferous|Late Devonian|||||||
15860|Ravendale Formation|44093|5|Briefly described|p140 App. 1|Early Carboniferous|Middle Devonian|Unconformably overlies Snake Cave Sandstone. Geological Province: Kanmantoo Fold Belt.||||||23-MAR-05
15860|Ravendale Formation|50129|4|Described|p15, p23, p24|Famennian|Givetian|Conformably overlies the Ramparts Creek Sandstone Member (Waverly Creek Formation) and is paraconformable on the Snake Cave Sandstone in the Wonominta and Bancannia Trough. Geological Province: Darling Basin.||||||
15860|Ravendale Formation|61213|5|Briefly described|p318, p319 Fig. 3|Famennian|Givetian|Geological Province: Darling Basin.||||||
15860|Ravendale Formation|63489|5|Briefly described|Map legend|Late Devonian|Late Devonian|Sandy fluvial sediments.||||||
15860|Ravendale Formation|63789|5|Briefly described|Map Legend|Carboniferous|Late Devonian|White to bluff plane-laminated and cross-bedded fluvial quartzose sandstone. Rare pebbly sandstone and siltstone horizons. Locally developed red-bed sequence of siltstone, sandstone and conglomerate at the base.||||||08-DEC-08
15860|Ravendale Formation|63790|5|Briefly described|Map Legend|Carboniferous|Late Devonian|White to bluff plane-laminated and cross-bedded fluvial quartzose sandstones. Rare pebbly sandstone and siltstone horizons.||||||
15860|Ravendale Formation|63793|5|Briefly described|p19 Table 1, p42-44, p81-85, p87-88, 26,|Carboniferous|Late Devonian|Flat to gently dipping. Character of basal units reflects the underlying material. Diagenetic spheres generally <1 cm diameter are diagnostic. Intruded by a phlogopite-bearing mafic rock along the Buick Fault.||||Unconformably overlies Ponto Group.|Clean, well-bedded and laminated quartz sandstone with very few pebbly units; locally a distinctive basal upward-fining red-bed section.|19-JAN-15
15860|Ravendale Formation|64168|5|Briefly described|p30 (photo)|Late Devonian|Late Devonian|Geological Province: Koonenberry Belt.||||||01-JUL-08
15860|Ravendale Formation|64169|5|Briefly described|p20 Fig. 9|Devonian|Devonian|||||||
15860|Ravendale Formation|64679|5|Briefly described|Map legend|Carboniferous|Late Devonian|White to buff, thick-thin bedded, planar and x-bedded quartzose sst; rare pebbly sst+siltst; local red bed sequences of siltst.+sst; very rare fossil fish fragments; basal conglomerate (rounded pebbles-cobbles some with Skolithos tubes); siltst/claystone||||||27-NOV-08
15860|Ravendale Formation|64967|5|Briefly described|p113, p114 Fig. 2|Late Devonian|Middle Devonian|Geological province: Darling Basin/Blantyre Sub-basin. Part of a stratigraphic sequence correlated with three informally named "intervals" Winduck, Snake Cave and Ravendale Intervals defined on the basis of seismic marker horizons (p113).||||||
15860|Ravendale Formation|65381|6|Mentioned|p689|Devonian|Late Silurian|||||||07-MAR-12
15860|Ravendale Formation|65759|6|Mentioned|p134|||Deposits in this unit, described by Neef (2004), are similar to channel-fill, crevasse splay and floodplain complex environments.||||||
15860|Ravendale Formation|66623|1|Redefined|p121, p196, pp215-223. |Late Devonian|Middle Devonian|Formerly in Mootwingee Stage (Kenny 1934), Ravendale Beds (Spence 1958), Ravendale Formation in Mulga Downs Group (Frenda 1965), Ravendale Sandstone (Branagan et al. 1967); redefined in this study. Post-Tabberabberan Orogeny fluvial deposition. Outcrops extensively and is a thick (to 1820 m) subsurface sequence widely recognised in seismic sections throughout Darling Basin. Contains Skolithos, fish and trace fossils. Correlated with Nundooka Sandstone.|c.392-385 Ma (Young 2006).||Includes 3 contemporaneous basal units: Gum Creek Member, Turkaro Range Conglomerate Member and Rocky Tank Conglomerate Member; and an un-named minor siltstone unit.|Unconformably or paraconformably overlies Wana Karnu Group; unconformably overlies Kayrunnera Group. Faulted against Mount Wright Volcanics.|Predominantly homogeneous quartzose sandstone; white to buff, plane-laminated and cross-bedded; rare pebbly sandstone and siltstone horizons. Locally developed red-bed sequence of conglomerate, sandstone and siltstone.|26-MAR-13
15860|Ravendale Formation|66917|5|Briefly described|Map legend|Devonian|Devonian|Does not crop out in the map area.|||||White to buff, plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizons; locally basal red-bed sequence of siltstone, sandstone and conglomerate.|
15860|Ravendale Formation|66918|5|Briefly described|Map legend|Devonian|Devonian||||Includes Rocky Tank Conglomerate Member.||White to buff, plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizons; locally basal red-bed sequence of siltstone, sandstone and conglomerate.|
15860|Ravendale Formation|66933|5|Briefly described|Map legend|Late Devonian|Late Devonian|Koonenberry Zone, Delamerian Fold Belt.||||Conformably to unconformably overlies Snake Cave Sandstone.|Upward-fining basal red-bed sequence of conglomerate, sandstones and siltstones; plane-laminated and cross-bedded fluvial quartzose sandstones; basal beds containing Skolithos tubes suggest marine transgression.|
15860|Ravendale Formation|67105|6|Mentioned|p661|Devonian|Devonian|||||||
15860|Ravendale Formation|67208|5|Briefly described|Map legend.|Devonian|Devonian||||||White to buff, plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizons; at the base, a locally developed red-bed sequence of siltstone, sandstone and conglomerate.|
15860|Ravendale Formation|67562|5|Briefly described|p96-97, p99, p102 Fig.8, p104-107|Fammenian||See also p109-111, p113-115. ~ 1900m thick. Sag basin deposit. Almost lacking in marker horizons. Comprises two coarse sandstone units in the western block, and six 6m to 30m thick erosion-resistant sandstone units in the eastern block. Deformations described.||||Overlies the Ramparts Creek Sandstone Member conformably and Mount Daubeny Formation unconformably. Is overlain unconformably by Eyre Formation.|Subarkose-rich arenite, almost lacking marker horizons. Several palaeochannels near the base. Also described as plane-bedded, fine-grained sandstones.|24-JAN-17
15860|Ravendale Formation|67870|5|Briefly described|p62|Devonian|Devonian|Darling Basin.||Mulga Downs Group.||Unconformably overlies Snake Cave Sandstone.||
15860|Ravendale Formation|70013|5|Briefly described|Map legend|Carboniferous|Devonian|Mapped, and description of lithologies combined, with [underlying] Wana Karnu Group.||||Overlies Wana Karnu Group.|Quartz sandstone, conglomerate and siltstone. Pebbles of vein quartz and quartzite. Cross-, trough- and planar-bedded. Rare horizons contain vertical worm-tubes (?Skolithos) indicating marine incursions.|
15860|Ravendale Formation|70648|5|Briefly described|Map Legend|Devonian|Devonian|2 un-named units: Soft, white-weathering siltstone and claystone unit; rare dessication structures and minor shale chip conglomerate and very rare quartz pebbles and the base of the overlying quartz sandstones. Conglomerate containing clasts of surrounding Teltawongee and Ponto Group rocks.|||Includes 2 un-named units and Turkaro Range Conglomerate Member.||White to buff, plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizons; at the base, a locally developed red-bed sequence of siltstones, sandstone and conglomerate.|
15860|Ravendale Formation|70650|5|Briefly described|Map Legend|Devonian|Devonian|Un-named unit is soft, white-weathering siltstone and claystone unit; rare dessication structures and minor shale chip conglomerate and very rare quartz pebbles at the base of the overlying quartz sandstones.|||Includes un-named unit and Rocky Tank Conglomerate Member.||White to buff, plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizons; at the base, a locally developed red-bed sequence of siltstone, sandstone and conglomerate.|
15860|Ravendale Formation|70651|5|Briefly described|Map Legend|Devonian|Devonian||||Includes Rocky Tank Conglomerate Member, Gum Creek Member.||White to buff plane-laminated and cross-bedded fluvial quartzose sandstone, rare pebbly sandstone and siltstone horizon; at the base, a locally developed red-bed sequence of siltstone, sandstone and conglomerate.|
15860|Ravendale Formation|71040|5|Briefly described|p7, p9, p14, p28|Late Devonian|Late Devonian|Darling basin. Weakly deformed by Kanimblan Orogeny. Appears as Ravendale on p7.||||Unconformably overlies Mount Daubeny Formation and Wana Karnu Group.||
15860|Ravendale Formation|71262|6|Mentioned|p9 Fig 7|Devonian|Devonian|||||||
15860|Ravendale Formation|73177|5|Briefly described|p1112|Late Devonian|Middle Devonian|Young (2006). Deformation of this unit gives a maximum age for the Alice Springs Orogeny.||||Is overlain unconformably by Rolling Downs Group.||
15860|Ravendale Formation|73457|6|Mentioned|p2|Late Devonian|Late Devonian|||||||
15864|Ravensfield Sandstone Member|23540|5|Briefly described|p 419|||Basal member of Farley Formation.||||||
15864|Ravensfield Sandstone Member|32943|6|Mentioned|p98|||See also p105. Bivalves||||||
15864|Ravensfield Sandstone Member|32945|6|Mentioned|p83|||||||||
15864|Ravensfield Sandstone Member|33867|6|Mentioned|p5|||||||||
15864|Ravensfield Sandstone Member|34445|5|Briefly described|p322|||||||||
15864|Ravensfield Sandstone Member|35284|6|Mentioned|p37|||||||||
15864|Ravensfield Sandstone Member|35862|6|Mentioned|p262|||||||||
15864|Ravensfield Sandstone Member|39267|6|Mentioned|p251|||||||||
15864|Ravensfield Sandstone Member|39288|6|Mentioned|p59|||||||||
15864|Ravensfield Sandstone Member|39304|6|Mentioned|Fig. 19.2|||||||||
15864|Ravensfield Sandstone Member|43440|14|Not recorded|p32|||Member of Farley Formation||||||
15864|Ravensfield Sandstone Member|43447|14|Not recorded|p16,17||Permian|||||||
15864|Ravensfield Sandstone Member|43471|14|Not recorded|p239,241||Artinskian|Megadesmus, Astartila present. Member of Farley Formation. See also Lexicon||||||
15864|Ravensfield Sandstone Member|43474|14|Not recorded|p53,70,71,102|||||||||
15864|Ravensfield Sandstone Member|45090|6|Mentioned|p222|||Artinskian||||||
15864|Ravensfield Sandstone Member|68493|5|Briefly described|p6|Cisuralian|Cisuralian|Basal member of the Farley Formation. ~ 4-6m thick. Produced high-quality building stone for Maitland.||Of the Farley Formation.||||
15888|Ravine beds|22768|6|Mentioned|p174-75|||||||||
15888|Ravine beds|22857|4|Described|p173, p175, p454 App.1, Tb.A1.6|Late Silurian|Late Silurian|Shale, slate, siltstone, conglomerate. Max. thickness: 2100m. Geological Province: Tumut Trough.||||||
15888|Ravine beds|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Ss2||||||
15888|Ravine beds|45147|6|Mentioned|M128|||||||||
15888|Ravine beds|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
15908|Razorback Creek Mudstone|30911|6|Mentioned|Map legend|Permian|Permian|||||||
15908|Razorback Creek Mudstone|32492|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
15908|Razorback Creek Mudstone|32671|6|Mentioned|Map legend|Permian|Permian|||||||
15908|Razorback Creek Mudstone|33476|6|Mentioned|Table 1|||||||||
15908|Razorback Creek Mudstone|36936|6|Mentioned|Fig.8|||||||||
15908|Razorback Creek Mudstone|43008|5|Briefly described|map legend|||||||||
15908|Razorback Creek Mudstone|48940|3|Fully described|p45|||||||||
15908|Razorback Creek Mudstone|69639|4|Described|p170, p176, p182, p192, p222|Early Permian|Early Permian|||||Intruded by the Koreelan Creek Granodiorite and faulted against the Morgans Creek Monzogranite.||
15908|Razorback Creek Mudstone|69793|6|Mentioned|p1111, p1113 Fig.3, p1114 Fig.5, p1121|Permian|Permian|Of Olgers et al., (1974). Originally part of the Pretty Gully Series (Andrews, 1908), then Plumbago Creek Series (Voisey, 1936). The rocks were incorporated into the Emu Creek Beds of McCarthy et al. (1974) and Emu Creek Formation of Thomson (1976), but reinstated by Flood et al. (1994). Early Permian. The Jump-up Fault juxtaposes this unit against the Emu Creek Block (of the Tamworth Belt) to the east.||||||
15908|Razorback Creek Mudstone|70728|5|Briefly described|p265|Artinskian|Sakmarian|Geological province: Emu Creek terrane, New England Orogen.||||Underlain by Paddys Flat Formation.||
15908|Razorback Creek Mudstone|71628|5|Briefly described|p9: 5; p11: 38; p16: 4, 26, 29|Permian|Permian|See also p19: 52, 90, 131, 173-174. RELATED UNITS (continued): Is intruded by, and faulted against, Undercliffe Falls Monzogranite. Is faulted against Morgans Creek Leucomonzogranite.||||Is intruded by Bruxner and Koreelah Creek Granodiorites, Cullendore and Rivertree Syenogranites, Yellow Gully Leucosyenogranite, Girard Creek Diorite. See COMMENTS for more.||
15911|Razorback Sandstone Member|31725|6|Mentioned|p12|||||||||
15911|Razorback Sandstone Member|35690|6|Mentioned|p18|||||||||
15911|Razorback Sandstone Member|36042|6|Mentioned|Fig.27|||||||||
15911|Razorback Sandstone Member|39287|6|Mentioned|p50|||||||||
15911|Razorback Sandstone Member|40592|5|Briefly described|p229|||||||||
15911|Razorback Sandstone Member|40653|6|Mentioned|Fig.22|||||||||
15911|Razorback Sandstone Member|42896|4|Described|p47, Fig.7|||of Bringelly Shale||||||
15911|Razorback Sandstone Member|43194|6|Mentioned|p131|Triassic|Triassic|Alluvial deposits in the Sydney Basin.||||||
15930|Red Cliff Coal Measures|22857|4|Described|p284, p542 A.1 Tb.A1.11|Jurassic|Early Triassic|Lithic conglomerate and breccia, sandstone, siltstone, coal. Max. thickness: >100m. Geological Province: Ipswich Basin (under Clarence-Moreton Basin). See also p318-9 Figs. 22.10A,B.||||||
15930|Red Cliff Coal Measures|22860|6|Mentioned|Fig20.2p278|||||||||
15930|Red Cliff Coal Measures|22861|5|Briefly described|p284-85|||||||||
15930|Red Cliff Coal Measures|23811|5|Briefly described|Map Legend|Norian|Norian|Thin-bedded, to laminated carbonaceous claystone and siltstone, interbedded with lenses and beds of pebble-granule conglom. and breccia; minor carbonaceous, fine-grained lithic sandstone. Geological Province: Clarence-Moreton Basin.||||||22-SEP-05
15930|Red Cliff Coal Measures|23812|5|Briefly described|P31, p35 Tb.4|Late Triassic|Late Triassic|Together with Evans Head Coal Measures considered to be equivalent to the Ipswich Coal Measures. Maximum thickness: 600m.  Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|30784|6|Mentioned|p71|||List fossil megalforas found||||||
15930|Red Cliff Coal Measures|30785|6|Mentioned|p397|||||||||
15930|Red Cliff Coal Measures|30911|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|32838|6|Mentioned|p320|||||||||
15930|Red Cliff Coal Measures|32916|6|Mentioned|Map legend|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|33476|6|Mentioned|p99|||||||||
15930|Red Cliff Coal Measures|34340|2|Defined|p463|Triassic|Triassic|||||||
15930|Red Cliff Coal Measures|36327|6|Mentioned|p10|||||||||
15930|Red Cliff Coal Measures|37112|5|Briefly described|Table 1|||||||||
15930|Red Cliff Coal Measures|40245|6|Mentioned|Fig.2|||||||||
15930|Red Cliff Coal Measures|41550|3|Fully described|p491|||||||||
15930|Red Cliff Coal Measures|41591|6|Mentioned|Fig.1|||||||||
15930|Red Cliff Coal Measures|41631|4|Described|p4|||See also Fig.2||||||
15930|Red Cliff Coal Measures|42248|6|Mentioned|Fig2 P399|||||||||
15930|Red Cliff Coal Measures|43001|5|Briefly described|Fig.1,p118|||||||||
15930|Red Cliff Coal Measures|43150|5|Briefly described|Map Legend||Late Triassic|Geological Province: Ipswich Basin.||||||12-APR-05
15930|Red Cliff Coal Measures|43383|14|Not recorded|p24|||||||||
15930|Red Cliff Coal Measures|43384|14|Not recorded|Map Legend||Triassic|||||||
15930|Red Cliff Coal Measures|43468|14|Not recorded|Map Legend||Triassic|Provisional Edition||||||
15930|Red Cliff Coal Measures|43881|2|Defined|p6-7,27-8,80-3,103,||Triassic|p105-6,142.||||||
15930|Red Cliff Coal Measures|44093|5|Briefly described|p72|Late Triassic|Late Triassic|See also p73 Fig. 7.3. Geological Province: Ipswich Basin.||||||
15930|Red Cliff Coal Measures|44450|5|Briefly described|p26|Late Triassic|Late Triassic|Overlain by Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||19-FEB-08
15930|Red Cliff Coal Measures|60281|5|Briefly described|p21-22, p25|||Geological Province: Ipswich Basin, Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|60993|5|Briefly described|p6 Fig. 2, p8|||Of McElroy (1963). Same unit as McTaggart's Esk beds (1963). Superseded by Ipswich Coal Measures.||||||
15930|Red Cliff Coal Measures|60997|5|Briefly described|p140 Fig. 2|||Of McElroy (1963).||||||
15930|Red Cliff Coal Measures|61001|6|Mentioned|p190 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61002|5|Briefly described|p196 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61006|6|Mentioned|p278 Fig. 1|||Geological Province: Clarence-Moreton Basin.||||||
15930|Red Cliff Coal Measures|61310|5|Briefly described|p16, Table C1 (p22-23)|Late Triassic|Late Triassic|Consist of conglomerate, lithic sandstone, siltstone, mudstone and coal. Max. thickness: ~600m. Geological Province: Clarence-Moreton Basin.  Along with Evans Head Coal Measures are equivalent to Ipswich Coal Measures. See also p15||||||23-JUN-06
15930|Red Cliff Coal Measures|61772|6|Mentioned|p130 Fig. 5||Late Triassic|Coal Measures is C.M. in text.||||||24-SEP-08
15930|Red Cliff Coal Measures|66855|6|Mentioned|p955.|Late Triassic|Late Triassic|||||||
15930|Red Cliff Coal Measures|68111|6|Mentioned|p966 Fig.1|||Ipswich Basin.||||||
15930|Red Cliff Coal Measures|68679|5|Briefly described|p388, p392|Late Triassic|Late Triassic|||||Equivalent to the Ipswich Coal Measures.||
15968|Redan Gneiss|6823|5|Briefly described|p205, 207-208|Palaeoproterozoic|Palaeoproterozoic|Features a metamorphic age of roughly <1590 Ma, , both of Love (1992).|1827 +/- 18 Ma (magmatic age, SHRIMP U-Pb)|||Underlies the Thackaringa Group.||26-MAR-22
15968|Redan Gneiss|22553|5|Briefly described|fig2p77|Orosirian|Orosirian|Part of Willyama Supergroup.||||||23-JUN-08
15968|Redan Gneiss|22575|6|Mentioned|p179 Fig.2|||in the Broken Hill Block||||||
15968|Redan Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
15968|Redan Gneiss|22857|5|Briefly described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Max. thickness: 1.5km. Geological Province: Willyama Fold Belt.||||||07-NOV-08
15968|Redan Gneiss|22884|5|Briefly described|p41, p43 Fig. 3|||Geological province: Broken Hill Domain. Correlates with similar George Mine Formation.||||||26-MAR-09
15968|Redan Gneiss|22962|6|Mentioned|p74||Statherian|||||||
15968|Redan Gneiss|22965|6|Mentioned|Fig 1||Statherian|||||||
15968|Redan Gneiss|22966|5|Briefly described|p2,Fig 1||Proterozoic|Early rift stage of development.||||||
15968|Redan Gneiss|23248|5|Briefly described|Fig2p169|||||||||
15968|Redan Gneiss|24197|5|Briefly described|p29|Paleoproterozoic|Paleoproterozoic|Rocks are leucocratic, high in silica and are usually albitic. Age: ~1710Ma. Geological Province: Broken Hill Domain.||||||07-FEB-11
15968|Redan Gneiss|24307|5|Briefly described|p968 Fig. 3|Proterozoic|Proterozoic|||||||
15968|Redan Gneiss|29864|6|Mentioned|p263|||||||||
15968|Redan Gneiss|33287|6|Mentioned|Fig.1|||||||||
15968|Redan Gneiss|33875|6|Mentioned|p24|||Radioactivity.||||||
15968|Redan Gneiss|34071|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Lower to Middle Proterozoic||||||07-NOV-08
15968|Redan Gneiss|34468|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Willyama Complex. Middle - Lower Proterozoic||||||07-NOV-08
15968|Redan Gneiss|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
15968|Redan Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
15968|Redan Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
15968|Redan Gneiss|42897|2|Defined|p332|Proterozoic||see also Fig.3, p321.||||||29-MAY-07
15968|Redan Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
15968|Redan Gneiss|43086|6|Mentioned|Fig.3|||||||||
15968|Redan Gneiss|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|43273|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
15968|Redan Gneiss|43464|14|Not recorded|Map Legend|Mesoproterozoic|Paleoproterozoic|(Provisional Edition)||||||07-NOV-08
15968|Redan Gneiss|43572|6|Mentioned|p5||Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|46598|5|Briefly described|p302|||||||||
15968|Redan Gneiss|50045|5|Briefly described|p116 Fig. 3|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Ednas Gneiss.||||||31-MAY-07
15968|Redan Gneiss|50606|5|Briefly described|p1.3, Table 1.1|Paleoproterozoic|Paleoproterozoic|Of the Redan Suite. Geological Province: Broken Hill Block. Age: 1570-1920Ma (U-Pb).||||||07-NOV-08
15968|Redan Gneiss|50619|5|Briefly described|p175|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Broken Hill Block.||||||07-NOV-08
15968|Redan Gneiss|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group? Geological Province: Broken Hill Domain.||||||28-APR-05
15968|Redan Gneiss|61606|5|Briefly described|p4 Fig.2|||||||||
15968|Redan Gneiss|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Part of the Redan Block.See also p636 Fig. 2.||||||04-JUN-15
15968|Redan Gneiss|62536|6|Mentioned|p635-636|||Redan Block, Broken Hill area.||||||
15968|Redan Gneiss|62592|5|Briefly described|p14, p16 Fig.2.2.|||Possibly a part-equivalent of Ethiudna Subgroup.||Basal unit in Thackaringa Group.||||
15968|Redan Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|1710+/-4 Ma|||||19-DEC-21
15968|Redan Gneiss|63102|5|Briefly described|p13|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||22-OCT-19
15968|Redan Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
15968|Redan Gneiss|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: 1682+/-3Ma. Geological Province: Redan Sub-block.||||||07-NOV-08
15968|Redan Gneiss|63866|5|Briefly described|p36, p40|||Redan Subdomain of the Broken Hill Domain, Curnamona Province.|c. 1710 Ma|Willyama Supergroup||Overlain by the Ednas Formation, Mulculca Formation and the Farmcote Gneiss.||
15968|Redan Gneiss|64097|5|Briefly described|p302, p309|Paleoproterozoic|Paleoproterozoic|Lower unit of Rantyga Gp in Redan geophysical zone in SE Broken Hill Domain. Underlies Farmcote Gneiss. Age:~1710+/-4Ma to 1704+/-13Ma (age evidence analysed). Laminated albite-qtz-hornblende-magnetite rock, and albite-qtz-magnetite rock.||||||07-FEB-11
15968|Redan Gneiss|64316|5|Briefly described|p532, p533 Fig. 1|||In lower Willyama Supergroup. Part of the amphibole-quartz-albite-magnetite Redan geophysical Zone forming a magnetic high regionally. Geological Province: Broken Hill Block. Also referred to as Redan Gneisses.||||||07-FEB-11
15968|Redan Gneiss|64741|5|Briefly described|p301 Fig. 4|Paleoproterozoic|Paleoproterozoic|Of the Rantyga Group. Age: 1710+/-4Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
15968|Redan Gneiss|64744|6|Mentioned|p353 Fig.4. |Statherian|Statherian|Broken Hill Domain.||Unit in Willyama Supergroup.||Is overlain by Clevedale Migmatite.||
15968|Redan Gneiss|64944|5|Briefly described|p27, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Age: 1710+/-4Ma. Geological province: Broken Hill Domain. Similar in age to the intrusive part (the Amaroo Subsuite) of Basso Suite in Olary Domain.||||||07-FEB-11
15968|Redan Gneiss|66302|5|Briefly described|p8, p36 Fig.9, p39, p76 Fig.20|Statherian|Statherian|Redan Domain, Curnamona Province.|1710 +/- 4 Ma (Stevens et al, 2008)|Rantyga Group||Overlain by the Ednas Gneiss.||
15968|Redan Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1710 +/- 4 Ma.|Rantyga Group.||||
15968|Redan Gneiss|67581|6|Mentioned|p45|||||Willyama Supergroup.||||
15968|Redan Gneiss|68126|6|Mentioned|p26, p30|||Oldest rocks in the Broken Hill Domain, Curnamona Province.|1710+/-4 Ma; 1704+/-13 Ma (Stevens et al., 2008).|||||
15968|Redan Gneiss|70000|5|Briefly described|p34-35|Statherian|Statherian|The basal gneiss may represent an altered metavolcanic rock.|1710 +/- 4 Ma (Stevens, Page and Crooks 2008).|Unit in Rantyga Group.||Correlated with uppermost Curnamona Group.|Includes basal quartz-albite-K-feldspar-magnetite gneiss.|
15968|Redan Gneiss|70014|5|Briefly described|Map legend|||||Unit in Willyama Supergroup.||Is overlain by Ednas Gneiss.|Albite-hornblende-quartz rock, sodic plagioclase-quartz-magnetite rock, minor quartz-albite-magnetite gneiss.|
15968|Redan Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Rantyga Group.|||Albite-quartz-hornblende-magnetite (+/- K feldspar +/- clinopyroxene) gneiss, with hornblende-rich laminations and thicker (up to 20mm) layers of quartz-feldspar.|
15968|Redan Gneiss|70405|6|Mentioned|p9 table 1, p40|Paleoproterozoic|Paleoproterozoic||1710 Ma||||Metavolcanic gneiss and calc-albitic metasediments; highly magnetic.|
15968|Redan Gneiss|70657|5|Briefly described|p10 Fig.4, p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Broken Hill Domain. Shown as Ethiudna Subgroup + Redan Gneiss in Fig.4.but separately in Fig. 6. Relationship with Ethiudna Subgroup is unclear. In Willyama Supergroup. Age also shown as ~1710 Ma in Fig.6 and as 1710 +/- 4 Ma on p15.|~1720-1715 Ma|Rantyga Group||Underlies Thackaringa Group and Ednas Gneiss.||
15968|Redan Gneiss|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|1710 +/- 4 Ma.|||||
15968|Redan Gneiss|72461|5|Briefly described|p16 fig 9|||Redan sub-block of the Broken Hill Block.|1710 +/- 4 Ma|Rantyga Group||Overlain by the Ednas Gneiss.||
15968|Redan Gneiss|73243|6|Mentioned|p53 Fig.2|||||||||
15968|Redan Gneiss|73482|5|Briefly described|p422 Fig.3|Statherian|Statherian|Redan sub-block.|1710+/-4 Ma|Rantyga Group||||
15968|Redan Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|Statherian|Statherian|Redan Geophysical Zone.|1710+/-4 Ma|Rantyga Group||||
15989|Redfern Granite|42726|5|Briefly described|map legend|Carboniferous||29.||||||
15993|Redmanvale Creek Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Glen Gallic Subgroup.   Geological Province: Sydney Basin||||||
15993|Redmanvale Creek Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Glen Gallic Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
15993|Redmanvale Creek Formation|45090|6|Mentioned|p187|||Refers Britten (1972)||||||
15993|Redmanvale Creek Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Middle unit in Glen Gallic Sub-group.||Overlies Dights Creek Coal. Is overlain by Greigs Creek Coal.|Predominantly a coarse conglomerate containing rounded boulders and pebbles.|
16005|Regentville Siltstone Member|35690|2|Defined|p179|Middle Triassic|Middle Triassic|||||||
16005|Regentville Siltstone Member|39298|5|Briefly described|p262|||See also P263||||||
16005|Regentville Siltstone Member|39626|6|Mentioned|p276|||||||||
16005|Regentville Siltstone Member|40602|4|Described|p23|||||||||
16005|Regentville Siltstone Member|42896|5|Briefly described|p44|||of Ashfield Shale||||||
16005|Regentville Siltstone Member|42925|4|Described|p22|||of Ashfield Shale||||||
16005|Regentville Siltstone Member|70661|6|Mentioned|p211|Middle Triassic|Middle Triassic|Age derived from parent unit. Not present in the map sheet area (Moss Vale)||Ashfield Shale||||
16014|Reids Flat Granite|42726|5|Briefly described|map legend|Silurian||Reserved as Reids Flat (1977). Reservation lapsed 1983.||||||12-JUN-08
16014|Reids Flat Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
16014|Reids Flat Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Massive to strongly foliated porphyritic biotite-ex-cordierite soda-granite, soda-syenite, granodiorite.||||||
16014|Reids Flat Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream to grey, medium- to coarse-grained, foliated, porphyritic, often megacrystic muscovite-cordierite-biotite granite. High K and Th with variable U radioelement response.||||||
16014|Reids Flat Granite|66185|5|Briefly described|p397, p398 Fig.2, p399|||In Wyangala Batholith. Massive to strongly foliated, porphyritic, biotite-after-cordierite granite, soda syenite and granodiorite. Intrudes Adaminaby Group (426-419.5Ma). Aplite dykes, pegmatite pipes, sedimentary xenoliths and microgranitoid enclaves.||||||
16014|Reids Flat Granite|66713|5|Briefly described|p3 Fig.2, p5, p13|Ludlow|Wenlock|Frogmore area. U-Pb SHRIMP zircon age of 425 +/- 4 Ma (Lennox and Zwingmann, 2007). Unit in Hovells Suite. Possible source of the Dryburgh greisen-type tungsten mineralisation.||||||
16014|Reids Flat Granite|68592|2|Defined|p1262-4, p1268-70, p1274, p1284, p1294-8|Late Silurian|Late Silurian|See also p97, p324, p1255 Fig.220, p1260. Named by Close (1978); formerly included in the undifferentiated Wyangala Batholith by Stevens (1955) and Brunker and Offenberg (1970). The parent Wyangala Suite has been superseded by Hovells Suite, which incorporates several new units on geochemical grounds. Type locality described. Geochemistry detailed: not fractionated; geophysical properties described. Has a broad protomylonitic zone (dated 387 +/- 2 Ma: Glen et al., 1999) on the E margin recording W-over-E thrust movement. Age by Lennox and Zwingmann, reported in Downes et al. (2011). Age is given as 420 +/- 4 Ma on p1310.|425 +/- 4 Ma (SHRIMP U-Pb zircon).|Unit in Hovells Suite.||Intrudes Adaminaby and Bendoc Groups. Is intruded by Wywurri and Ballyhooley Granites. Is faulted against Wyangala Granite.|Cream to grey, coarse-grained, porphyritic, foliated, cordierite-muscovite-biotite; minor cordierite?-biotite granodiorite near margins; rhyolite, aplite and microgranitic dykes, metasedimentary xenoliths, biotite-rich mafic enclaves common. S-type.|
16014|Reids Flat Granite|69539|5|Briefly described|p615|Devonian|Devonian|40Ar/39Ar biotite total fusion age; consistent with Tabberabberan event deformation.|387 +/- 2 Ma (Glen et al., 1999).|||||
16014|Reids Flat Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sor. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot. Includes one unnamed member of leucocratic, medium grained, porphyritic, foliated, vesicular commonly flow banded, rhyolitic dykes.||Hovells Suite|Includes one unnamed member.||Coarse grained, porphyritic, commonly megacrystic and xenolithic, foliated cordierite-muscovite-biotite granite. Minor aplite and micrgranite dykes; minor phase of granodiorite near margins; High K, Th and U response; low magnetic susceptibility.|
16014|Reids Flat Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|Includes one unnamed member of leucocratic, medium grained, porphyritic, foliated, vesicular commonly flow banded, rhyolitic dykes.||Hovells Suite|Includes one unnamed member||Coarse grained, porphyritic, commonly megacrystic and xenolithic, foliated cordierite-muscovite-biotite granite. Minor aplite and micrgranite dykes; minor phase of granodiorite near margins; High K, Th and U response; low magnetic susceptibility.|
16014|Reids Flat Granite|70545|5|Briefly described|Map Legend |Devonian|Silurian|||Hovells Suite|||Coarse grained, porphyritic, commonly megacrystic and xenolithic, foliated cordierite-muscovite-biotite granite. Minor aplite and microgranite dykes. Minor medium-coarse grained, porphyritic, foliated cordierite-biotite granodiorite at margins.|
16014|Reids Flat Granite|70727|5|Briefly described|p172|||Intruded by metamorphosed (epidite-amphibolite reiognal metamorphism; transitional greenschist-amphibolite facies) mafic dykes. Comprises S and C foliations. S foliations developed during E-W shortening, C foliation from E-directed reverse movement.||||||
16036|Renmark Group|2967|5|Briefly described|p14-15, 17-24, 27-31, 34-35, 39, 46-47|Miocene|Palaeocene|Lawrence (1975); previously the Renmark Beds of Harris (1971); see references p14, 33. Murray Basin. Locally the Calivil Formation sediments fill in valleys incised into this Group. Deep aquifers. See also p79, 96, 105, 110, 112, 128, 151, 155, 178, 336.|||Olney Formation, Warina Sand.|Is overlain by Ettrick Marl and Geera Clay (Murray Group). Elsewhere, is separated from the overlying Parilla Sand and Calivil Formation by the Mologa Surface.|A widespread, thick suite of fine-grained sands and carbonaceous sediments.|
16036|Renmark Group|10010|5|Briefly described|p12 Fig. 3|Miocene|Paleocene|Overlain by Olney Formation. Geological Province: Murray Basin.||||||13-AUG-07
16036|Renmark Group|22487|6|Mentioned|p212 Fig. 13|Tertiary|Tertiary|Geological province: eastern Murray Basin.||||||11-SEP-08
16036|Renmark Group|22531|6|Mentioned|p6|Eocene|Eocene|||||||
16036|Renmark Group|22587|6|Mentioned|p79 Fig.7|Late Eocene|Late Paleocene|||||||
16036|Renmark Group|22712|5|Briefly described|p132|||||||||
16036|Renmark Group|22756|6|Mentioned|P28|||||||||
16036|Renmark Group|22773|6|Mentioned|p351|||||||||
16036|Renmark Group|22782|6|Mentioned|p15|||||||||
16036|Renmark Group|22799|2|Defined|p25|Middle Miocene|Paleocene|||||||
16036|Renmark Group|22857|5|Briefly described|p351, p352 Fig.24.8|Miocene|Paleocene|Age: ~60Ma. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
16036|Renmark Group|22887|6|Mentioned|p32, p75|Oligocene|Eocene|Fluvial||||||
16036|Renmark Group|22893|5|Briefly described|p25 fig9|Tertiary|Tertiary|||||||
16036|Renmark Group|22971|4|Described|p 26||Tertiary|||||||
16036|Renmark Group|23179|6|Mentioned|Fig.2||Early Oligocene|Murray Basin.||||||
16036|Renmark Group|23226|6|Mentioned|p889||Oligocene|||||||
16036|Renmark Group|23230|4|Described|Table4-1p40, 41, 43-4|Oligocene|Paleocene|||||||
16036|Renmark Group|23234|6|Mentioned|p88|Oligocene|Paleocene|||||||
16036|Renmark Group|23252|5|Briefly described|Map Legend||Tertiary|||||||
16036|Renmark Group|23402|5|Briefly described|p31|Early Miocene|Paleocene|Geological Province: Murray Basin||||||
16036|Renmark Group|23884|5|Briefly described|p153, p155 Fig. 13.2|Middle Miocene|Late Paleocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|23921|5|Briefly described|p1109|Middle Miocene|Eocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|24105|5|Briefly described|p159|||Overlain by Wunghnu Group.||||||13-MAR-07
16036|Renmark Group|24106|5|Briefly described|p184|Miocene|Miocene|Geological Province: Murray Basin.||||||
16036|Renmark Group|24177|4|Described|p69|Early Miocene|Paleocene|Overlain by the Calivil Formation. Age: ~65 Ma. Comprised of Warina Sand and Olney Formation. Correlated with Pebble Point, Wiridgil and Eastern View formations of the Wangerrip Group in Otway Basin. Geological Province: Murray Basin.||||||06-FEB-15
16036|Renmark Group|24239|5|Briefly described|p11|Tertiary|Tertiary|Geological Province: Murray Basin.||||||
16036|Renmark Group|24328|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|24329|5|Briefly described|Map legend|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|24383|6|Mentioned|p58|||||||||
16036|Renmark Group|24439|6|Mentioned|p37|||Time equivalent of parts of lower Loddon River Group.  Geological Province: Murray Basin.||||||
16036|Renmark Group|24470|6|Mentioned|p473|||||||||
16036|Renmark Group|24551|5|Briefly described|p320, 417, 421, 543|Ealry Oligocene|Paleocene|Maximum Thickness: 300m.||||||
16036|Renmark Group|24563|5|Briefly described|p485, p486|||Geological Province: Murray Basin.||||||
16036|Renmark Group|24574|6|Mentioned|p705|||Geological Province: Murray Basin||||||
16036|Renmark Group|29355|6|Mentioned|p179|||||||||
16036|Renmark Group|29591|6|Mentioned|Table 20|||||||||
16036|Renmark Group|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16036|Renmark Group|30934|6|Mentioned|Map legend|Eocene|Eocene|Equivalence with Wangerrip Group||||||
16036|Renmark Group|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
16036|Renmark Group|30936|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31625|6|Mentioned|Fig. 5.2|||Palaeocene-Eocene||||||
16036|Renmark Group|31654|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31713|6|Mentioned|p16|||||||||
16036|Renmark Group|31741|6|Mentioned|p6|||||||||
16036|Renmark Group|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
16036|Renmark Group|31746|3|Fully described|p191|||||||||
16036|Renmark Group|31747|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
16036|Renmark Group|31922|6|Mentioned|Fig.2|||||||||
16036|Renmark Group|31951|6|Mentioned|p7|||||||||
16036|Renmark Group|31952|6|Mentioned|p7|||||||||
16036|Renmark Group|31953|6|Mentioned|p9|||||||||
16036|Renmark Group|32225|6|Mentioned|p22|||||||||
16036|Renmark Group|32315|6|Mentioned|p4|||||||||
16036|Renmark Group|32862|6|Mentioned|Fig. 3|||Section from boreholes||||||
16036|Renmark Group|34312|5|Briefly described|p46|||L.Tertiary||||||
16036|Renmark Group|34313|6|Mentioned|p165|||||||||
16036|Renmark Group|34735|4|Described|p31|||||||||
16036|Renmark Group|34757|6|Mentioned|p45|||||||||
16036|Renmark Group|35091|4|Described|p7|||||||||
16036|Renmark Group|35094|6|Mentioned|p9|||||||||
16036|Renmark Group|35172|6|Mentioned|p127|||||||||
16036|Renmark Group|35285|5|Briefly described|p413|||||||||
16036|Renmark Group|35498|6|Mentioned|Fig.1|||||||||
16036|Renmark Group|36305|6|Mentioned|p358|||||||||
16036|Renmark Group|37873|6|Mentioned|p1|||||||||
16036|Renmark Group|38293|4|Described|Table 1|||||||||
16036|Renmark Group|38601|5|Briefly described|p7|||||||||
16036|Renmark Group|39329|6|Mentioned|p483|||||||||
16036|Renmark Group|39929|6|Mentioned|p269|||||||||
16036|Renmark Group|40599|5|Briefly described|p19|||||||||
16036|Renmark Group|40795|5|Briefly described|p80|||Mention p82.||||||13-MAR-07
16036|Renmark Group|41068|5|Briefly described|p65|||.||||||13-MAR-07
16036|Renmark Group|41423|6|Mentioned|p284|||||||||
16036|Renmark Group|41517|6|Mentioned|p139|||||||||
16036|Renmark Group|41765|4|Described|p34|||||||||
16036|Renmark Group|41868|5|Briefly described|p550|||||||||
16036|Renmark Group|42125|5|Briefly described|p132|||||||||
16036|Renmark Group|42126|6|Mentioned|p149, p152|||||||||
16036|Renmark Group|42127|5|Briefly described|p218|||See also Fig.1||||||
16036|Renmark Group|42129|6|Mentioned|p254|||See also Fig.6||||||
16036|Renmark Group|42130|6|Mentioned|p264|||||||||
16036|Renmark Group|42133|6|Mentioned|p301|||||||||
16036|Renmark Group|42134|4|Described|p340|||||||||
16036|Renmark Group|42137|5|Briefly described|p367|||||||||
16036|Renmark Group|42138|6|Mentioned|p388|||||||||
16036|Renmark Group|42184|6|Mentioned|p351|||||||||
16036|Renmark Group|42454|4|Described|p11|early Miocene|middle Eocene|||||||
16036|Renmark Group|42455|5|Briefly described|Map legend|early Miocene|middle Eocene|||||||
16036|Renmark Group|42623|5|Briefly described|p2|||aquifer||||||
16036|Renmark Group|42648|6|Mentioned|p45|||||||||
16036|Renmark Group|42827|3|Fully described|p265|||see also Fig 8.4||||||
16036|Renmark Group|42881|4|Described|Fig.3, p84|||||||||01-NOV-22
16036|Renmark Group|42966|2|Defined|p91|Middle Miocene|Paleocene|||||||
16036|Renmark Group|43195|5|Briefly described|Map Legend|Early Oligocene|Middle Eocene|See also commentary on back of map.||||||
16036|Renmark Group|43218|4|Described|Fig.3,p22||Tertiary|||||||
16036|Renmark Group|43493|6|Mentioned|32|||||||||
16036|Renmark Group|43655|5|Briefly described|p40-846|||||||||
16036|Renmark Group|43669|6|Mentioned|p9|||||||||
16036|Renmark Group|43780|5|Briefly described|p6|||||||||
16036|Renmark Group|43791|6|Mentioned|p371|||||||||
16036|Renmark Group|43804|6|Mentioned|p47|||||||||
16036|Renmark Group|44093|6|Mentioned|p145 App. 1|||||||||
16036|Renmark Group|44133|5|Briefly described|p158|Early Oligocene|Late Paleocene|Geological Province: Murray Basin. Includes: Warina Sand, Olney Formation.||||||
16036|Renmark Group|44188|6|Mentioned|Map Legend|Miocene|Eocene|Includes the Olney Formation. Geological province: Murray Basin.||||||15-MAY-08
16036|Renmark Group|44191|5|Briefly described|Map Legend||Middle Miocene|||||||
16036|Renmark Group|45168|6|Mentioned|p6|||See also Table 1.||||||
16036|Renmark Group|49038|5|Briefly described|p24|||See also p40||||||13-MAR-07
16036|Renmark Group|49040|6|Mentioned|p10|||||||||
16036|Renmark Group|50154|2|Defined|p26, p132-135|Middle Miocene|Late Paleocene|Geological Province: Murray Basin. Max. thickness: over 300m. Overlain by the Murray Group, Calivil Formation and Parilla Sand. Overlies the Grampians Group and Rocklands Volcanic Group. Correlates with the Wangerrip & Nirranda groups.||||||15-SEP-04
16036|Renmark Group|50155|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Fluvio-lacustrine; gravel, quartz sand, silt and clay||||||
16036|Renmark Group|50156|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50157|5|Briefly described|Map Legend|Miocene|Paleocene|Overlies Eumeralla Formation. Overlain by Ettrick Marl. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||13-MAR-07
16036|Renmark Group|50158|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly consolidated.||||||24-AUG-04
16036|Renmark Group|50159|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50160|5|Briefly described|Map Legend|Miocene|Paleocene|||||||
16036|Renmark Group|50161|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50162|5|Briefly described|Map Legend|Miocene|Paleocene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|50163|5|Briefly described|Map Legend|Miocene|Paleogene|Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||07-NOV-08
16036|Renmark Group|50164|5|Briefly described|Map Legend|Miocene|Paleocene|Overlies Otway Group. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||25-JUN-04
16036|Renmark Group|60421|5|Briefly described|p409, 415|Oligocene|Paleocene|||||||07-NOV-08
16036|Renmark Group|60451|5|Briefly described|p95 Fig. 61|||||||||
16036|Renmark Group|60452|5|Briefly described|p14, 15|Cenozoic|Cenozoic|Includes Warina Sand at base. See also p68.||||||19-NOV-08
16036|Renmark Group|60461|5|Briefly described|Map legend|Eocene|Paleocene|Includes the Olney Formation.||||||06-OCT-04
16036|Renmark Group|60491|4|Described|p21|Oligocene|Late Eocene|Includes the Olney Formation and Warina Sand. Disconformably overlain by the Parilla Sand. Max. thickness: 100m. Palynological studies yield late Eocene to Oligocene ages.||||||
16036|Renmark Group|60492|5|Briefly described|Map Legend|Oligocene|Paleocene|Overlies the Glenloth Suite and Pyrenees Formation. Overlain by Parilla Sand. Fluviolacustrine to marginal marine: carbonaceous silt and fine sand with calcareous bands and marine fossils; some lignite rich bands.||||||30-SEP-04
16036|Renmark Group|60538|6|Mentioned|p473 Fig.12|||||||||
16036|Renmark Group|60591|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60592|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60593|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60595|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60596|5|Briefly described|Map Legend|Paleocene|Paleocene|Unconformably overlies the Urana Formation. Overlain by the Calivil Formation. Fluvio-lacustrine deposits: gravel, quartz sand, silt and clay; pyritic, ferruginised, unconsolidated to poorly unconsolidated.||||||
16036|Renmark Group|60597|5|Briefly described|Map Legend|Eocene|Paleocene|Fluvio-lacustrine deposits: no distinctive magnetic responses.||||||
16036|Renmark Group|60599|2|Defined|p15, p84-85|Early Miocene|Middle Eocene|Formerly part of Knight Group (Sprigg and Boutakoff 1953). Originally informally divided into 'lower' and 'upper' Renmark Beds. Lithological details included. Overlain by Murray Gp+ Calivil Fm.||||||27-OCT-08
16036|Renmark Group|61155|5|Briefly described|p3, p18|Middle Miocene|Late Paleocene|Comprises Warina Sand, Olney Formation Buccleuch beds. Includes fluvial-lacustrine unconsolidated carbonaceous clastics. Age: ~53-~14.5Ma. Extends into the Miocene in eastern Murray Basin (Olney Formation). Geological Province: Murray Basin.||||||
16036|Renmark Group|61180|6|Mentioned|p37|||Contains brown coal seams up to 40m thick in some places.||||||
16036|Renmark Group|61181|5|Briefly described|p153 Fig. 47|||Sandy carbonaceous clay over sand and minor clay.||||||
16036|Renmark Group|61183|6|Mentioned|p133|||Geological Province: Murray and Otway Basins.||||||
16036|Renmark Group|61185|5|Briefly described|p57, p58||Middle Paleocene|Includes Olney Formation and Warina Sand. Disconformably underlies Calivil Formation. Geological Province: Murray Basin.||||||07-FEB-11
16036|Renmark Group|61822|6|Mentioned|p107|Paleogene|Paleogene|||||||07-NOV-08
16036|Renmark Group|61825|6|Mentioned|p138|Cenozoic|Cenozoic|In Broken Hill region.||||||19-NOV-08
16036|Renmark Group|61841|5|Briefly described|p242|Early Oligocene|Paleocene|Gravels and clays. Geological Province: Murray Basin.||||||
16036|Renmark Group|61964|5|Briefly described|p17, p139|Miocene|Oligocene|Includes the Olney Formation. Geological Province: Murray Basin. Informally subdivided into lower, middle and upper parts.||||||
16036|Renmark Group|63066|5|Briefly described|p485|Tertiary|Tertiary|Geological Province: Murray Basin.||||||08-FEB-07
16036|Renmark Group|63460|5|Briefly described|p839 Fig. 2b|early Oligocene|Early Oligocene|Geological province: Murray Basin.||||||
16036|Renmark Group|63777|5|Briefly described|p1104 Fig. 1, p1105|Late Miocene|Paleocene|Overlain by Calival Formation. Geological Province: Murray Basin. Fluvial clays, sand silt and gravels.||||||
16036|Renmark Group|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Includes; Warina Sand, Olney Fm and Buccleuch Fm. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt. Minor marine incursion during Late Eocene marked by clay and marl.||||||
16036|Renmark Group|64237|5|Briefly described|p17, p18 Fig. 2|Middle Miocene|Late Oligocene|Underlies Murray Group.||||||
16036|Renmark Group|64612|5|Briefly described|p28|Cainozoic|Cainozoic|Down hill extension of White Hills Gravel. Unclear if White Hills Gravel intended to be included in Renamrk Group. Geological Province: Murray Basin.||||||06-FEB-15
16036|Renmark Group|64823|5|Briefly described|p1011|Cenozoic|Cenozoic|Overlain by Calivil Formation. Fluvial clays, silts, sands and gravels; paleochannel deposits. Geological province: Murray Basin.||||||
16036|Renmark Group|65552|5|Briefly described|p5 Fig. 3, p6, p11 Fig.6, p12, p13-14|Middle Miocene|Late Palaeocene|See also p23,25,26 App. 2,4,5. Contains Olney Formation and Warina Sand. Unconformably overlies basement, unconformably underlies Wunghnu Group and Loxton-Parilla Sands. Associated with moderate concentrations of heavy minerals.||||||
16036|Renmark Group|65969|5|Briefly described|p27 Tb.3.3, p30|Oligocene|Eocene|Overlain by Murray Group. Includes Olney Formation and White Hills Gravel.||||||
16036|Renmark Group|66002|5|Briefly described|p10 Tb.7, p12|Paleogene|Paleogene|Replaces Knight Group of Boutakoff and Sprigg (1953). Name based on Renmark Beds of Harris (1966). Correlated in part with (obsolete) Loddon River Group. Defined by Lawrence and Abele, 1976.||||||
16036|Renmark Group|66012|5|Briefly described|p17|Miocene|Paleocene|In Murray Basin. Includes Olney Formation. Paleocene to early Miocene|| ||||13-JUN-13
16036|Renmark Group|66286|5|Briefly described|p179.|Oligocene|Paleocene|Southern Murray Basin.|||Includes Warina Sand and Olney Formation.|||
16036|Renmark Group|67127|6|Mentioned|p73|||||||Overlies the Grampians Grou;p. Underlies the Geera Clay.||
16036|Renmark Group|67179|5|Briefly described|p579, p584|Miocene|Paleocene|Fluvio-lacustrine, overlying the Neoproterozoic and early Paleozoic sediments, metasediments and granitoids of the Murray Basin basement.||||Underlies the Loxton Sand, Duddo Limestone, Geera Clay and Bookpurnong Beds.||28-MAY-13
16036|Renmark Group|67462|5|Briefly described|Map legend.|Late Eocene||Murray Basin.|||Includes Warina Sand.|||
16036|Renmark Group|68116|5|Briefly described|Appendix, Map 29.|Miocene|Thanetian||||||Gravel, quartz sand, silt and clay: pyritic, ferruginised, unconsolidated to poorly consolidated.|
16036|Renmark Group|68140|6|Mentioned|p1699, p1700 Fig.1, p1704 Fig.5|Miocene|Paleocene|This name seems to be used interchangeably with Renmark Formation (see references p1698, p1699, p1701-1708).|||||Lower: fluvial silts, sands, gravels, and clay.|09-FEB-18
16036|Renmark Group|68189|6|Mentioned|p26, p29||||||Includes the Warina Sand (base) and the Olney Formation.|||
16036|Renmark Group|68194|5|Briefly described|p22|Oligocene|Eocene|Murray Basin. Lawrence (1975); Lawrence and Abele (1988). Thickness <50m.|||Includes Warina Sand, Olney Formation.|Is overlain by Murray Group.||
16036|Renmark Group|68715|5|Briefly described|p31 Fig.5|Eocene|Eocene|Murray Basin.|||Includes Warina Sand, Olney Formation.|||07-APR-17
16036|Renmark Group|69562|5|Briefly described|p674|||||||||09-FEB-18
16036|Renmark Group|69798|5|Briefly described|p4 Fig.2|Miocene|Eocene|Murray Basin.|||Olney Formation.|||06-FEB-18
16036|Renmark Group|70718|5|Briefly described|p17, p24, p103, 129|Middle Miocene|Middle Paleocene|Murray Basin. Is one of the primary aquifers in the Hay map sheet area. Deposited in a warm, moist climate with rates of swamp and flood plain alluvium being generally slow.|||Includes the Warina Sand, Olney Formation.||Lower sequences are dominated by light-brown or grey quartz sand whilst the upper sequences are increasingly dominated by argillaceous and carbonaceous sediments.|02-JUN-19
16036|Renmark Group|71593|5|Briefly described|p51-p52, p54|||Murray Basin.|||Includes the Olney Group and the Warina Sand.|Overlain by the Murray Group.||
16036|Renmark Group|72445|5|Briefly described|App.1, App.2 p1; App.6 p2 Fig.1; App.7|Miocene|Paleocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). An extensive group ranging from the Paleocene conglomerates of the Warina Sand to the Miocene Mologa Surface in the eastern Murray Basin. App.2 is a .csv format file.  Identified in Stavely 04, 05, 06,07,09,10,11,12,14, 16.|||Includes Olney Formation, Warina Sand.|Overlies Nargoon Group, sharply; Moornambool Metamorphic Complex, Williamsons Road Serpentinite. Underlies Bookpurnong Fm, gradational; Wunghnu, Murray Grps, gradational/sharp; Winnambool Fm, sharply|Organic-rich muddy sand and sand. Sparse <1 m intervals of lignite.|
16036|Renmark Group|73118|6|Mentioned|p83|Miocene|Paleocene||||Olney Formation, Warina Sand.|||
16036|Renmark Group|73188|6|Mentioned|p320|Late Eocene|Late Eocene|Murray Basin.||||||
16036|Renmark Group|73228|4|Described|p50, p52-57, p60, p62|Early Oligocene|Late Paleocene|Murray Basin. [upper and lower informal subdivisions are occasionally used and once capitalised; interpreted as general terms rather than specific distinctions]. Dominated by marginal marine, fluvial to lacustrine sediments also with shallow marine and swamp depositional environments. Identified in Cooltong 1, Berri North 1, Nadda 1, Loxton 1, and Overland Corner 1 drillholes. Maximum thickness  330 m. Misspelt as Remark Group p51.|||Olney Formation, Buccleuch Formation, Warina Sand|Underlain by Coombool Member (Monash Formation). Overlain by Ettrick Formation and Murray Group.|Includes fine to coarse grained quartzose sand interbedded with clay and lime clay; pyritic, calcareous, fossiliferous, and glauconitic, with minor coal and lignite.|
16036|Renmark Group|73229|5|Briefly described|p66-67, p70-72, p74-75|Early Oligocene|Late Paleocene|Murray Basin. [Analysed using pXRF; see article]. Fluvial, lacustrine and swamp environments. Show in Fig. 1 as extending into the Miocene.|||Buccleuch Formation, Olney Formation, Warina Sand||Includes sandstone, carbonaceous sand; silt; clay; lignite.|01-NOV-22
16036|Renmark Group|73253|6|Mentioned|p15|||Murray Basin.||||||
16036|Renmark Group|73496|6|Mentioned|Map legend|Oligocene|Eocene|||||||
16036|Renmark Group|73505|5|Briefly described|p2, p10, p13, p36|Oligocene|Eocene|Murray Basin.|||Olney Formation, Warina Formation||Carbonaceous fluvial to paralic silt, clay; minor lignite.|
16052|Rewan Formation|22464|5|Briefly described|p9|Middle Triassic|Early Triassic|Cooper Basin||||||
16052|Rewan Formation|22757|4|Described|Table4,p9||Early Triassic|840 m thick. Unconformable on Blackwater Group. Unconformably overlain by Clematis Sandstone||||||
16052|Rewan Formation|23003|5|Briefly described|p423 Table 1|Triassic|Triassic|||||||
16052|Rewan Formation|23004|5|Briefly described|p431 Table 1|Triassic|Triassic|||||||
16052|Rewan Formation|23037|6|Mentioned|Fig 3|Triassic|Late Permian|Overlying unit Back Creek Group.||||||
16052|Rewan Formation|23425|6|Mentioned|p391.|||||||||
16052|Rewan Formation|23769|4|Described|p862|Early Triassic|Early Triassic|Parent: Mimosa Group.  Geological Province: Bowen Basin.||||||
16052|Rewan Formation|23883|5|Briefly described|p129 Fig. 11.2|Triassic|Triassic|Geological Province: Great Australian Superbasin.||||||
16052|Rewan Formation|23982|5|Briefly described|p35 Fig.7|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
16052|Rewan Formation|24069|5|Briefly described|p284|Early Triassic|Early Triassic|Geological Province: Surat Basin.||||||
16052|Rewan Formation|24071|5|Briefly described|p319|Triassic|Triassic|Geological Province: Galilee Basin.||||||
16052|Rewan Formation|24077|5|Briefly described|p410 Tb. 2|Middle Triassic|Early Triassic|Of Mimosa Group.  Max. thickness: 615m.  Geological Province: Bowen Basin.See also p411 Tb.3.||||||
16052|Rewan Formation|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16052|Rewan Formation|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Early Triassic|Geological Province: Gunnedah Basin.||||||17-MAR-05
16052|Rewan Formation|24615|5|Briefly described|CD|Triassic|Triassic|[Rr].  Green lithic sandstone, green and red mudstone and sandstone.||||||
16052|Rewan Formation|29385|6|Mentioned|p81|||Lower Triassic.||||||
16052|Rewan Formation|29387|6|Mentioned|Table 3|||See also Table 4. Triassic.||||||
16052|Rewan Formation|29388|6|Mentioned|p62|||Stratigraphy.||||||
16052|Rewan Formation|29389|6|Mentioned|p18|||Early Triassic.||||||
16052|Rewan Formation|29390|6|Mentioned|p54|||Only oil discovery in Bowen Basin.||||||
16052|Rewan Formation|29391|6|Mentioned|Table 3|||Appears on P18, see also Table 4 on P19.||||||
16052|Rewan Formation|29393|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|29409|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|29410|6|Mentioned|p273|||Correlation diagram P275. Conformably overlies Bandanna Fm.||||||
16052|Rewan Formation|29411|5|Briefly described|p201|||||||||
16052|Rewan Formation|29412|4|Described|p208|||Appears throughout article.||||||
16052|Rewan Formation|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
16052|Rewan Formation|29721|6|Mentioned|Table 65|||||||||
16052|Rewan Formation|30102|4|Described|p9|||See also P10-13. Lower Triassic age.||||||
16052|Rewan Formation|30103|6|Mentioned|p8|||||||||
16052|Rewan Formation|30137|6|Mentioned|p2|||Triassic age||||||
16052|Rewan Formation|30140|6|Mentioned|p2|||Triassic age. Lithology||||||
16052|Rewan Formation|30141|6|Mentioned|p135|||||||||
16052|Rewan Formation|30351|6|Mentioned|Fig.4|||Fig.4 on P32||||||
16052|Rewan Formation|30451|4|Described|p66|||Lower Triassic age||||||
16052|Rewan Formation|30455|5|Briefly described|p1|||See also P2-3. Triassic age||||||
16052|Rewan Formation|30457|6|Mentioned|p96|||||||||
16052|Rewan Formation|30458|6|Mentioned|p3|||Triassic age||||||
16052|Rewan Formation|30459|6|Mentioned|p309|||||||||
16052|Rewan Formation|30460|6|Mentioned|p1|||Triassic age. See also P3-22,24-27, Fig.1,2||||||
16052|Rewan Formation|30461|6|Mentioned|p100|||||||||
16052|Rewan Formation|30465|6|Mentioned|p4|||||||||
16052|Rewan Formation|30466|6|Mentioned|p4|||Triassic age||||||
16052|Rewan Formation|30468|6|Mentioned|p385|||||||||
16052|Rewan Formation|30472|6|Mentioned|p134|||Pollen distribution||||||
16052|Rewan Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
16052|Rewan Formation|30545|6|Mentioned|p22|||Triassic||||||
16052|Rewan Formation|30546|6|Mentioned|p107|||Correlation.Lower Triassic age.||||||
16052|Rewan Formation|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
16052|Rewan Formation|30549|6|Mentioned|p26|||||||||
16052|Rewan Formation|30565|6|Mentioned|p120|||||||||
16052|Rewan Formation|30691|4|Described|p14|||See also Table 4,6. Lower Triassic age||||||
16052|Rewan Formation|30696|4|Described|Table 3|||Lower Triassic age||||||
16052|Rewan Formation|30698|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|30699|6|Mentioned|p53|||Stratigraphy||||||
16052|Rewan Formation|30701|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|30743|6|Mentioned|p24|||Geological map||||||
16052|Rewan Formation|30851|6|Mentioned|p366.|||||||||
16052|Rewan Formation|30852|4|Described|Fig.2|||||||||
16052|Rewan Formation|30853|6|Mentioned|p9|||||||||
16052|Rewan Formation|30915|6|Mentioned|p98|||||||||
16052|Rewan Formation|30916|6|Mentioned|p98|||On table||||||
16052|Rewan Formation|31084|6|Mentioned|p13|||L. Triassic||||||
16052|Rewan Formation|31115|5|Briefly described|p32|||See also P33-34. Triassic||||||
16052|Rewan Formation|31116|4|Described|p11|||See also P1. Triassic||||||
16052|Rewan Formation|31120|6|Mentioned|Fig. 2|||||||||
16052|Rewan Formation|31121|6|Mentioned|p388|||||||||
16052|Rewan Formation|31122|6|Mentioned|p344|||||||||
16052|Rewan Formation|31145|6|Mentioned|p7|||||||||
16052|Rewan Formation|31167|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|31260|6|Mentioned|p16|||Facies analysis||||||
16052|Rewan Formation|31303|4|Described|Table 1|||||||||
16052|Rewan Formation|31305|4|Described|p571|||Mention Table 1||||||
16052|Rewan Formation|31369|4|Described|p26|||See also P27. Triassic||||||
16052|Rewan Formation|31398|6|Mentioned|p268|||L.Triassic. Fauna||||||
16052|Rewan Formation|31401|6|Mentioned|p33|||On Table 3.||||||
16052|Rewan Formation|31531|6|Mentioned|p13|||||||||
16052|Rewan Formation|31553|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|31620|5|Briefly described|p87|||See also P88-89||||||
16052|Rewan Formation|31647|6|Mentioned|Fig. 9|||||||||
16052|Rewan Formation|31656|4|Described|Table 2|||Triassic (Mimosa Gp.)||||||
16052|Rewan Formation|31690|6|Mentioned|p35|||||||||
16052|Rewan Formation|31979|6|Mentioned|p10|||||||||
16052|Rewan Formation|31984|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32040|6|Mentioned|p885|||Stratigraphic sequence||||||
16052|Rewan Formation|32136|6|Mentioned|p2|||Triassic. Geol map near Munduberra No.1||||||
16052|Rewan Formation|32138|6|Mentioned|p396|||||||||
16052|Rewan Formation|32139|6|Mentioned|p579|||||||||
16052|Rewan Formation|32177|6|Mentioned|p145|||||||||
16052|Rewan Formation|32193|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|32490|4|Described|Table 1|||L.Triassic||||||
16052|Rewan Formation|32493|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32496|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|32553|4|Described|p40|||||||||
16052|Rewan Formation|32556|4|Described|Table 4|||Triassic||||||
16052|Rewan Formation|32577|4|Described|p25|||Perm.-L.Triass.||||||
16052|Rewan Formation|32578|6|Mentioned|p347|||Perm. Strat. table||||||
16052|Rewan Formation|32689|6|Mentioned|Fig.2|||Strat. correlation table||||||
16052|Rewan Formation|32797|6|Mentioned|p10|||||||||
16052|Rewan Formation|32840|6|Mentioned|p1|||See also P26||||||
16052|Rewan Formation|32944|6|Mentioned|p703|||L.Triassic||||||
16052|Rewan Formation|33059|4|Described|Table 1|||L.Trias.||||||
16052|Rewan Formation|33078|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33079|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33086|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33092|5|Briefly described|p6|||Strat. table||||||
16052|Rewan Formation|33096|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33128|5|Briefly described|p51|||Geochemistry||||||
16052|Rewan Formation|33250|6|Mentioned|p140|||||||||
16052|Rewan Formation|33251|6|Mentioned|p2|||||||||
16052|Rewan Formation|33363|5|Briefly described|p115|||Triassic.||||||
16052|Rewan Formation|33366|6|Mentioned|Fig.3|||Triassic.||||||
16052|Rewan Formation|33368|6|Mentioned|p12|||Consuelo N.S.3 log.||||||
16052|Rewan Formation|33369|6|Mentioned|p214|||Strat. succession in GSQ Jericho 1.||||||
16052|Rewan Formation|33372|4|Described|p21|||Mention P16. Q.D.M. Aramac 1 & Hexham 1.||||||
16052|Rewan Formation|33390|5|Briefly described|p6|||||||||
16052|Rewan Formation|33451|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33530|5|Briefly described|Table 1|||Triassic||||||
16052|Rewan Formation|33561|6|Mentioned|p102|||||||||
16052|Rewan Formation|33639|5|Briefly described|p10|||L.Triass.||||||
16052|Rewan Formation|33640|4|Described|Table 3|||Triassic.||||||
16052|Rewan Formation|33646|5|Briefly described|p11|||||||||
16052|Rewan Formation|33647|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|33648|6|Mentioned|p18|||Strat.||||||
16052|Rewan Formation|33674|4|Described|p412|||||||||
16052|Rewan Formation|33675|4|Described|p412|||||||||
16052|Rewan Formation|33774|3|Fully described|p39|||||||||
16052|Rewan Formation|34009|6|Mentioned|Table III|||||||||
16052|Rewan Formation|34010|6|Mentioned|Cor. chart|||L.Triassic||||||
16052|Rewan Formation|34061|6|Mentioned|p53|||||||||
16052|Rewan Formation|34094|6|Mentioned|p1-4,Figs.2,3,4||Triassic|||||||
16052|Rewan Formation|34095|6|Mentioned|p3,4,6,Figs.5,6||Triassic|||||||
16052|Rewan Formation|34133|6|Mentioned|p2|||See also PP28,29||||||
16052|Rewan Formation|34172|6|Mentioned|p52|||||||||
16052|Rewan Formation|34174|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|34212|6|Mentioned|p2|||See also PP6,14 etc. Jurassic.||||||
16052|Rewan Formation|34218|6|Mentioned|p9|||Triassic||||||
16052|Rewan Formation|34235|6|Mentioned|p92|||||||||
16052|Rewan Formation|34254|6|Mentioned|Table 7.1|||||||||
16052|Rewan Formation|34276|6|Mentioned|p42|||Triassic||||||
16052|Rewan Formation|34314|5|Briefly described|Table 3|||Triassic. Mimosa Group||||||
16052|Rewan Formation|34331|6|Mentioned|p458|||L.Triassic||||||
16052|Rewan Formation|34391|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|34543|6|Mentioned|p98|||||||||
16052|Rewan Formation|34574|6|Mentioned|p115|||||||||
16052|Rewan Formation|34613|4|Described|Table 3|||||||||
16052|Rewan Formation|34614|6|Mentioned|p29|||||||||
16052|Rewan Formation|34837|6|Mentioned|Fig.4|||Also stratigraphy on Table 1||||||
16052|Rewan Formation|35079|6|Mentioned|p424|||||||||
16052|Rewan Formation|35095|6|Mentioned|p115|||||||||
16052|Rewan Formation|35148|4|Described|p414|||See also Table 1.||||||
16052|Rewan Formation|35280|6|Mentioned|p143|||||||||
16052|Rewan Formation|35426|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|35428|6|Mentioned|p125|||Biostratigraphy||||||
16052|Rewan Formation|35435|6|Mentioned|p44|||Summarised stratigraphic table of the Artesian Basin.||||||
16052|Rewan Formation|35457|6|Mentioned|p633|||Also Fig.4 biostratigraphic relationships||||||
16052|Rewan Formation|35467|6|Mentioned|p178|||||||||
16052|Rewan Formation|35488|6|Mentioned|p87|||||||||
16052|Rewan Formation|35560|6|Mentioned|p292|||||||||
16052|Rewan Formation|35562|6|Mentioned|p295|||Stratigraphy||||||
16052|Rewan Formation|35621|6|Mentioned|p331|||||||||
16052|Rewan Formation|35822|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|35859|6|Mentioned|p225|||||||||
16052|Rewan Formation|35873|4|Described|p16|||||||||
16052|Rewan Formation|36121|6|Mentioned|p25|||||||||
16052|Rewan Formation|36241|6|Mentioned|p110|||||||||
16052|Rewan Formation|36243|6|Mentioned|p74|||See also Table 3A.||||||
16052|Rewan Formation|36333|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16052|Rewan Formation|36825|6|Mentioned|p21|||||||||
16052|Rewan Formation|36899|6|Mentioned|p1085|||See also P1092.||||||
16052|Rewan Formation|36914|6|Mentioned|p87|||||||||
16052|Rewan Formation|36921|6|Mentioned|p175|||See also Table 1.||||||
16052|Rewan Formation|36925|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|37070|5|Briefly described|p70|||||||||
16052|Rewan Formation|37072|5|Briefly described|p90|||||||||
16052|Rewan Formation|37074|3|Fully described|p105|||||||||
16052|Rewan Formation|37075|5|Briefly described|Table 1|||||||||
16052|Rewan Formation|37076|4|Described|p121|||||||||
16052|Rewan Formation|37077|6|Mentioned|p130|||||||||
16052|Rewan Formation|37078|5|Briefly described|p135|||||||||
16052|Rewan Formation|37079|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|37080|5|Briefly described|p150|||||||||
16052|Rewan Formation|37262|6|Mentioned|p285|||||||||
16052|Rewan Formation|37288|6|Mentioned|p41|||||||||
16052|Rewan Formation|37400|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|37451|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|37610|6|Mentioned|p302|||||||||
16052|Rewan Formation|37749|6|Mentioned|p186|||||||||
16052|Rewan Formation|37812|6|Mentioned|p656|||||||||
16052|Rewan Formation|37858|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|37859|6|Mentioned|Table 1|||See also Tables 2 & 3.||||||
16052|Rewan Formation|38153|6|Mentioned|p373|||||||||
16052|Rewan Formation|38358|6|Mentioned|p13|||||||||
16052|Rewan Formation|38375|6|Mentioned|p545|||||||||
16052|Rewan Formation|38447|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|38713|6|Mentioned|p330|||Now named Arcadia Formation.||||||
16052|Rewan Formation|39217|6|Mentioned|p49|||Refers Evans(1966)||||||
16052|Rewan Formation|39219|6|Mentioned|p46|||Microflora||||||
16052|Rewan Formation|39252|6|Mentioned|p26|||||||||
16052|Rewan Formation|39260|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|39261|6|Mentioned|Fig. 9|||||||||
16052|Rewan Formation|39264|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|39270|5|Briefly described|p282|||||||||
16052|Rewan Formation|39275|6|Mentioned|p332|||||||||
16052|Rewan Formation|39412|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|39445|5|Briefly described|Table 9|||||||||
16052|Rewan Formation|39478|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|39491|4|Described|p18|||||||||
16052|Rewan Formation|39813|6|Mentioned|Map legend|Triassic|Triassic|||||||
16052|Rewan Formation|40095|6|Mentioned|Fig.6|||||||||
16052|Rewan Formation|40123|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|40249|6|Mentioned|p41|||Mention Fig.2||||||
16052|Rewan Formation|40634|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|40767|6|Mentioned|p18|||||||||
16052|Rewan Formation|40999|6|Mentioned|p298|||||||||
16052|Rewan Formation|41034|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|41116|4|Described|p433|||||||||
16052|Rewan Formation|41159|4|Described|p341|||||||||
16052|Rewan Formation|41198|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|41210|6|Mentioned|p165|||||||||
16052|Rewan Formation|41216|6|Mentioned|p304|||||||||
16052|Rewan Formation|41266|6|Mentioned|Fig.3|||||||||
16052|Rewan Formation|41330|6|Mentioned|Table 1|||||||||
16052|Rewan Formation|41475|6|Mentioned|Fig.1|||||||||
16052|Rewan Formation|41535|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|41707|6|Mentioned|Fig.8|||||||||
16052|Rewan Formation|41710|6|Mentioned|Fig.2|||||||||
16052|Rewan Formation|41725|6|Mentioned|p399|||See also Fig.2||||||
16052|Rewan Formation|42249|6|Mentioned|p23|||||||||
16052|Rewan Formation|42250|6|Mentioned|Fig.3 P30|||||||||
16052|Rewan Formation|42446|4|Described|p10|||||||||
16052|Rewan Formation|42447|6|Mentioned|Fig. 2|||||||||
16052|Rewan Formation|42463|6|Mentioned|Fig.5 P172|||||||||
16052|Rewan Formation|42492|5|Briefly described|Table 2 P14|||||||||
16052|Rewan Formation|42713|5|Briefly described|Fig. P18|||||||||
16052|Rewan Formation|42932|5|Briefly described|Fig.21|||||||||
16052|Rewan Formation|43017|5|Briefly described|p379|||||||||
16052|Rewan Formation|43072|6|Mentioned|p31|||||||||
16052|Rewan Formation|43812|6|Mentioned|Fig.3,p145|||||||||
16052|Rewan Formation|43851|14|Not recorded|Tb p106,113||Early Triassic|||||||
16052|Rewan Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
16052|Rewan Formation|43912|14|Not recorded|p2|||(Sunnybank No.1)||||||
16052|Rewan Formation|43920|14|Not recorded|p74|||||||||
16052|Rewan Formation|43922|14|Not recorded|p326|||L.Triassic, Bowen Basin.||||||
16052|Rewan Formation|43923|6|Mentioned|p1||Triassic|||||||
16052|Rewan Formation|43977|14|Not recorded|p576|||||||||
16052|Rewan Formation|43982|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|43987|14|Not recorded|p265-6,269-271,275,|||p277-279||||||
16052|Rewan Formation|43988|14|Not recorded|Map Legend||Triassic|Of Mimosa Group||||||
16052|Rewan Formation|43989|14|Not recorded|Map Legend||Early Triassic|||||||
16052|Rewan Formation|43990|14|Not recorded|Map Legend||Triassic|Part of Mimosa Group.||||||
16052|Rewan Formation|43994|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|43995|14|Not recorded|Tb.p9,23,53,Fig.14|Permian|Carboniferous|||||||
16052|Rewan Formation|43996|14|Not recorded|p88|||||||||
16052|Rewan Formation|43997|14|Not recorded|p113|||||||||
16052|Rewan Formation|43998|4|Described|p12,13,17,map||Triassic|||||||
16052|Rewan Formation|44000|14|Not recorded|p40|||||||||
16052|Rewan Formation|44003|14|Not recorded|Map Legend|||||||||
16052|Rewan Formation|44020|14|Not recorded|p10|||||||||
16052|Rewan Formation|44022|14|Not recorded|Map Legend||Triassic|||||||
16052|Rewan Formation|44023|4|Described|Tb.3||Triassic|||||||
16052|Rewan Formation|44031|14|Not recorded|p6||Triassic|||||||
16052|Rewan Formation|44040|14|Not recorded|p14|||||||||
16052|Rewan Formation|44085|2|Defined|Opp.4,12,13,15|||||||||
16052|Rewan Formation|44091|14|Not recorded|p53,54||Triassic|||||||
16052|Rewan Formation|44095|14|Not recorded|p284|||||||||
16052|Rewan Formation|44096|2|Defined|Fig.26,p187-8,193|||Overlies Bandanna Formation.||||||
16052|Rewan Formation|44115|14|Not recorded|p18,19,21|||||||||
16052|Rewan Formation|44118|14|Not recorded|Map Legend||Triassic|||||||
16052|Rewan Formation|44124|14|Not recorded|p1,2,4,5,10,12|||||||||
16052|Rewan Formation|44129|14|Not recorded|p95-96||Triassic|||||||
16052|Rewan Formation|44130|14|Not recorded|p280|||Unconformably overlain by Clematis Sandstone.||||||
16052|Rewan Formation|44166|14|Not recorded|p1|||||||||
16052|Rewan Formation|44169|2|Defined|Tb.1,6,8,9,map|||||||||
16052|Rewan Formation|44170|2|Defined|p1,6,12-17,19,25,28,||Early Triassic|p30,31,35-38,53-56,Tb.1,Pl.1,map||||||
16052|Rewan Formation|44172|14|Not recorded|Tb.1,p1325,1339||Triassic|Ref. to Hill 1957.||||||
16052|Rewan Formation|44218|14|Not recorded|p18|||||||||
16052|Rewan Formation|44242|14|Not recorded|p14|||||||||
16052|Rewan Formation|44243|14|Not recorded|p649,map,650||Triassic|||||||
16052|Rewan Formation|44337|5|Briefly described|Map Legend||Triassic|Lithology.||||||
16052|Rewan Formation|44381|14|Not recorded|p7|||||||||
16052|Rewan Formation|44390|14|Not recorded|p6,8,13,14,Tb.1,||Early Triassic|Of Mimosa Group.||||||
16052|Rewan Formation|44391|14|Not recorded|Map Legend||Early Triassic|||||||
16052|Rewan Formation|44419|14|Not recorded|p274|||||||||
16052|Rewan Formation|44420|14|Not recorded|p1-3,6-11,15,22,28||Early Triassic|||||||
16052|Rewan Formation|44421|14|Not recorded|p6,8-11,18||Triassic|||||||
16052|Rewan Formation|44422|14|Not recorded|p150,152,153||Early Triassic|||||||
16052|Rewan Formation|44426|14|Not recorded|p11-12||Triassic|Dicroidium; Triassic from micro and macrofaunas. "A correlation between the Rewan Formation and Narrabeen Group of the Sydney Basin is indicated."||||||
16052|Rewan Formation|44577|14|Not recorded|p137|||||||||
16052|Rewan Formation|44607|14|Not recorded|p10|||||||||
16052|Rewan Formation|44609|14|Not recorded|p64|||||||||
16052|Rewan Formation|44610|14|Not recorded|p47-49|||||||||
16052|Rewan Formation|44618|14|Not recorded|p511-513||Triassic|||||||
16052|Rewan Formation|44640|14|Not recorded|p36,map|||||||||
16052|Rewan Formation|44651|14|Not recorded|p117|||||||||
16052|Rewan Formation|44652|14|Not recorded|p70,73,74||Triassic|||||||
16052|Rewan Formation|44668|14|Not recorded|p59|||||||||
16052|Rewan Formation|44697|14|Not recorded|p91|||||||||
16052|Rewan Formation|44721|14|Not recorded|p28-36||Triassic|||||||
16052|Rewan Formation|44746|14|Not recorded|p50|||||||||
16052|Rewan Formation|44787|14|Not recorded|p121,Tb.p123,124,127||Early Triassic|||||||
16052|Rewan Formation|44792|14|Not recorded|p15|||||||||
16052|Rewan Formation|44815|14|Not recorded|unknown (p313-346)|Triassic|Permian|||||||
16052|Rewan Formation|45031|14|Not recorded|Fig.3,||Triassic|||||||
16052|Rewan Formation|45071|3|Fully described|p70|||See also Table 14||||||
16052|Rewan Formation|45073|6|Mentioned|p59|||Correlation chart||||||
16052|Rewan Formation|45095|6|Mentioned|p18|||Refers Malone et al. (1969)||||||
16052|Rewan Formation|45151|6|Mentioned|p15|||||||||
16052|Rewan Formation|46849|6|Mentioned|p194|||||||||
16052|Rewan Formation|46881|6|Mentioned|Table 2|||||||||
16052|Rewan Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
16052|Rewan Formation|46949|6|Mentioned|p96|||||||||
16052|Rewan Formation|48600|14|Not recorded|p13,20|||Shelf sediments. Springsure area.||||||
16052|Rewan Formation|48606|14|Not recorded|p14|||(H/55-8).||||||
16052|Rewan Formation|48626|14|Not recorded|p1,3,23-26,51,55,||Triassic|Pl.1,Fig.1,2.||||||
16052|Rewan Formation|48898|4|Described|p56|||Triassic. See also PP55,58 etc||||||
16052|Rewan Formation|48900|2|Defined|p41|Triassic|Triassic|||||||
16052|Rewan Formation|48915|6|Mentioned|Table 1|||Triassic. See also P10||||||
16052|Rewan Formation|48919|4|Described|p29|||L.Triassic. See also P30-32||||||
16052|Rewan Formation|48920|3|Fully described|p30|||Triassic||||||
16052|Rewan Formation|48922|4|Described|p22|||||||||
16052|Rewan Formation|48947|6|Mentioned|p10|||||||||
16052|Rewan Formation|48951|6|Mentioned|Table|||||||||
16052|Rewan Formation|48995|6|Mentioned|p128|||See also Fig.3.||||||
16052|Rewan Formation|49010|6|Mentioned|Fig.4|||Galilee Basin||||||
16052|Rewan Formation|49011|6|Mentioned|Fig.3|||Galilee Basin||||||
16052|Rewan Formation|49644|5|Briefly described|Table|||||||||
16052|Rewan Formation|50215|5|Briefly described|Map Legend|Triassic|Triassic|Green and reddish brown mudstone, lithic sandstone and minor conglomerate.||||||18-JUN-09
16052|Rewan Formation|50273|5|Briefly described|Map legend|Triassic|Triassic|Lithic sandstone and green to reddish brown mudstone and minor conglomerate.||||||
16052|Rewan Formation|50602|5|Briefly described|Map Legend|Early Triassic|Early Triassic|Green lithic sandstone, mudstone.||||||
16052|Rewan Formation|60700|5|Briefly described|p37|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16052|Rewan Formation|61772|6|Mentioned|p131|||||||||
16052|Rewan Formation|61832|5|Briefly described|p187|Early Triassic|Early Triassic|Sandstone and fine-grained rocks. Geological Province: Bowen Basin.||||||05-OCT-06
16052|Rewan Formation|62921|5|Briefly described|p877-879, p881-883|Early Triassic|Changhsingian|Not subdivided in the Galilee Basin (Exon, 1970). In the Bowen Basin it was elevated to Group status by Jensen (1975) who divided it into two Formations (Arcadia Formation and Sagittarius Sandstone). Contains Late Permian and Early Triassic miospores. This article describes the first tetrapod (Lydekkerina huxleyi) from this Formation, the second lydekkerinid from Australia. This Formation is equivalent in age to the Lystrosaurus Assemblage Zone in South Africa.||||Unconformably overlies Bandanna Formation. Is overlain by Dunda Beds. Correlated with Rewan Group (Bowen Basin). Said to conformably overlie Betts Creek Beds (Blackwater Group).|Pale buff to yellow, fine-grained sandstones and mudstones.|
16052|Rewan Formation|63172|6|Mentioned|p21|||Geological Province: Bowen Basin. Mentioned in the context of the combined units - "Rewan Formation-Clematis Sandstone interval".||||||07-FEB-11
16052|Rewan Formation|64665|6|Mentioned|p54.|Triassic|Triassic|Red-bed deposits.||||||
16052|Rewan Formation|64856|5|Briefly described|p68, p72|||Name used 1950s to 1970s. Superseded by Rewan Group.|| ||||29-NOV-17
16052|Rewan Formation|65003|5|Briefly described|p6|||Of Bowen Basin. Unconformably overlies the coal measures [?Baralaba Coal Measures].||||Overlain by the Clematis Group and Moolayember Formation.||30-MAR-12
16052|Rewan Formation|65388|6|Mentioned|p159, 202|||Bowen Basin, Galilee Basin. Replaced by Rewan Group by Jensen in 1975.||||||
16052|Rewan Formation|65489|5|Briefly described|p144 Fig.53|Early Triassic|Early Triassic|Koburra Trough, Galilee Basin.||||Overlies Betts Creek Beds. Is overlain by Dunda Formation.||
16052|Rewan Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin. Also appears as Rewan Fm/Gp in Fig.5.||||||
16052|Rewan Formation|67133|5|Briefly described|p9|||Primarily fluvial and lacustrine environments. Two samples of this unit were analysed by XRD and optical microscopy for this study; one was smectite-rich while the other was illite-rich.||Rewan Group.|||Includes sandstones which are generally quartzose, partly lithic (volcanic fragments) and with a clayey matrix.|
16052|Rewan Formation|67323|5|Briefly described|p84|Triassic|Triassic|Eastern Galilee Basin.||||Tentatively correlated with Warang Sandstone.||
16052|Rewan Formation|67402|5|Briefly described|p43 tbl HPB1, p52, p65|Olenekian|Changhsingian|Galilee Basin. Prospective reservoir unit for the storage of carbon dioxide; together with the Clematis Sandstone may be able to store 982 Megatonnes of carbon dioxide. More than 100m thick. See also  p69, p124 fig GLL1, p125 tbl GLL1, p128 fig GLL8, p129 fig GLL9, p131 fig GLL12, p132-p137, p140, p142, p144, p265, p300, p305.||||Overlies the Betts Creek beds.|Interbedded mudstone, siltstone and sandstone.|
16052|Rewan Formation|67669|5|Briefly described|p11|Early Triassic|Early Triassic|Of Bowen Basin.||Unit of Rewan Group.||||
16052|Rewan Formation|68411|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Unconformably underlain by the Blackwater Group. Conformably overlain by the Clematis Group.|Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanolithic pebble conglomerate (at base).|
16052|Rewan Formation|68413|5|Briefly described|Map Legend|Triassic|Triassic|Galilee Basin||||Conformably overlain by the Warang Sandstone.|Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanolithic pebble conglomerate (at base).|
16052|Rewan Formation|68679|6|Mentioned|p469|Triassic|Triassic|Bowen Basin. Part of the foreland loading during the evolution of the northern New England Orogen.||||||
16052|Rewan Formation|68731|6|Mentioned|p200, p201, p201 Fig 3.110|Middle Triassic|Early Triassic|Galilee Basin. Subdivided in the Bowen Basin and so elevated to Group status (Jensen 1975). Possibly equivalent to the Rewan Group. Written as the Rewan 'Formation' on p201.||||Probably unconformably overlain by the Clematis Formation. Conformably overlain by the Dunda beds.||11-MAY-16
16052|Rewan Formation|69379|5|Briefly described|map legend|Triassic|Triassic|[Not a current name; possibly intended as Arcadia Formation?]||Of Rewan Group|||Lithic sandstone, pebbly lithic sandstone, green to reddish brown mudstone and minor volcanilithic pebble conglomerate (at base).|
16052|Rewan Formation|69594|6|Mentioned|p534|||||||Is overlain unconformably by Eddystone beds.||
16052|Rewan Formation|70821|5|Briefly described|p80|||Basement to Surat Basin.||||Is overlain unconformably by Precipice Sandstone.||14-DEC-16
16052|Rewan Formation|70878|5|Briefly described|p717, p720-721, p725-726|Triassic|Triassic|Bowen Basin. Calibration of palynological ages (D. parvithola Zone). Base of this unit marks the base of the Triassic.||||Unconformably overlies Bandanna Formation.||
16052|Rewan Formation|71265|5|Briefly described|p589-590, p587, p599-600, p602-605|Olenekian|Olenekian|Galilee Basin. Called Rewan Group in the Denison Trough (Bowen Basin). Sedimentary logs of GSQ Muttaburra 1, CRD Montani 1, OEC Glue Pot Creek 1 and GSQ Tambo 1-1A.||||Unconformably overlies Betts Creek Group.||
16052|Rewan Formation|71276|5|Briefly described|p291, p293, p295 Fig.8|Early Triassic|Early Triassic|Galilee Basin.||||Unconformably overlies Bandanna Formation. Is overlain locally by Dunda Beds.||
16052|Rewan Formation|71278|5|Briefly described|p322|Early Triassic|Early Triassic|Bowen Basin. Considered as the reservoir seal in the Fairview Field. 61m thick.|||||Lithic sandstone, mudstone and basal conglomerate.|
16052|Rewan Formation|71701|4|Described|p155, p157-p158, p165-p166, p168-p169|Olenekian|Olenekian|Central Western Area, Galilee Basin; Denison Trough and Northern Area, Bowen Basin. A sample from this unit has a diverse assemblage of palynorphs; palnyology is discussed in some detail. Deposited in a non-marine environment. Intersected in CRD Montani 1, OEC Glue Pot Creek 1, GSQ Tambo 1-1A and GSQ Muttaburra 1.||||Unconformably overlies the Betts Creek Group and Bandanna Formation.||
16052|Rewan Formation|72088|6|Mentioned|p22, p68-p69|Early Triassic|Early Triassic|See Rewan Group.||||||
16052|Rewan Formation|72298|5|Briefly described|p801|||Eromanga (SA,QLD,NSW), Surat Basins. Appears as Rewan Fm./Gp in the SURAT BASIN (QLD,NSW) column on p801.||||Is overlain by Dunda beds or Clematis Sandstone.||
16052|Rewan Formation|73163|6|Mentioned|p468, p472|Triassic|Early Triassic|Galilee Basin. Unclear if Rewan Formation conformably or unconformably overlies the Bandanna Formation, but mudstone bed seen in some places, at boundary.||||Overlies the Bandanna Formation.||
16052|Rewan Formation|73472|6|Mentioned|p115-116|Olenekian|Olenekian|Galilee Basin.||||Overlain by and equivalent to Dunda beds. Equivalent to Rewan Group and Warang Sandstone.||
16070|Rhyolite Range beds|22601|4|Described|415|Permian|Permian|Within Silverwood Block. Thickness >1200 m. Overlain by Marburg Sandstone; underlain by Rosenthal Creek Formation.||||||12-DEC-07
16070|Rhyolite Range beds|39252|6|Mentioned|p22|||||||||
16070|Rhyolite Range beds|42994|6|Mentioned|p43|||||||||
16070|Rhyolite Range beds|43008|5|Briefly described|map legend|||||||||
16070|Rhyolite Range beds|43017|6|Mentioned|p377|||||||||
16070|Rhyolite Range beds|61392|5|Briefly described|p164 Fig. 1|Late Permian|Late Permian|Of the Wildash Group.||||||07-FEB-11
16070|Rhyolite Range beds|63731|5|Briefly described|Map legend|Permian|Permian|Arenite+siltstone; some conglomerate. Locally spherulitic rhyolite sills and flows, agglomerate, crystal tuff, quartz-feldspar porphyry + minor dacitic to andesitic lava. Siliceous pebbly orthoconglom. Fossiliferous/bioturbated litharenite and siltstone.||||||
16070|Rhyolite Range beds|63748|4|Described|p7 Fig. 3, p20|Late Permian|Middle Permian|Of Olgers et al (1974) - redefined by Dennis (1974a). Unconformable on Silverwood Group rocks; unconformable below Marburg Subgroup. Max. thickness:1300m. Mainly felsic volcanics. Detailed lithology provided. Geological province: Wandsworth Province.||||||07-FEB-11
16070|Rhyolite Range beds|68679|5|Briefly described|p446, p453|Permian|Permian|Mapped by Olgers et al. (1974) but redefined by Dennis (1974); the extent of the unit was modified by Van Noord (1999). Silver Spur Subprovince, Woolomin Province. Forms a narrow elongate belt 10km S of Warwick. >1300m thick. Contains a middle Permian marine fauna.||Wildash Group.||Unconformably overlies or is faulted against the Silverwood Group. Is overlain unconformably by the Marburg Subgroup. May correlate with Fitz Creek beds.|Mainly felsic volcanics, including spherulitic rhyolite sills (and flows?), breccia, crystal tuff, quartz-feldspar porphyry, and minor dacitic to andesitic lava; ~120-300m of locally pebbly lithic sandstone and siltstone at the base.|
16070|Rhyolite Range beds|71628|6|Mentioned|p16:4|||||||Is intruded by Cullendore Syenogranite.||
16079|Rickabys Creek Gravel|31056|4|Described|p5|||||||||
16079|Rickabys Creek Gravel|33671|6|Mentioned|Fig.2|||||||||
16079|Rickabys Creek Gravel|35098|4|Described|p2|||||||||
16079|Rickabys Creek Gravel|35312|6|Mentioned|Fig.2|||||||||
16079|Rickabys Creek Gravel|39308|6|Mentioned|p494|||||||||
16079|Rickabys Creek Gravel|41391|6|Mentioned|p46|||||||||
16079|Rickabys Creek Gravel|42795|4|Described|p25|||||||||
16079|Rickabys Creek Gravel|42925|2|Defined|p32|early Miocene|late Oligocene|||||||
16079|Rickabys Creek Gravel|42926|4|Described|map legend||Miocene|||||||
16079|Rickabys Creek Gravel|67850|5|Briefly described|p49, pp52-58.|Neogene|Paleogene|Sydney Basin. A thin (<2-3 m thick), surficial deposit of semi-consolidated gravels. Scattered exposures occur along the Lapstone Monocline from Lapstone to Warragamba.||||||
16079|Rickabys Creek Gravel|70587|5|Briefly described|Map Legend|Miocene|Oligocene||||||matrix-suported conglomerate.|
16079|Rickabys Creek Gravel|73248|4|Described|p304-310, App. p1-4|||[Also written as Rickaby's Creek Gravel]. Represents the deposits of a major drainage line carrying water and sediment across the northern Cumberland Basin. This unit is critical to understanding the development of the Cumberland Basin margins. Discontinuously distributed along the top of the Lapstone Structural Complex and across the Cumberland Basin. Timing of deposition relative to uplift of the Lapstone Monocline is uncertain [see article for discussion; author indicates uplift postdates deposition]. Author refers to units distributed across the floor of the Cumberland Basin as the namesake exposures [sensu stricto]. Initially recognised by Clarke (1878). Subsurface extent is far more widespread than the surface outcrops would suggest. Contains occasional lenses of cross-bedded sand. Pebble fabrics in outcrop show northerly dips atop the escarpment. Upwards-finning contact with the overlying Londonderry Clay. Clasts may have been sourced from rocks of the Lachlan Orogen or possible Permian glaciofluvial gravels from the southwest. The most conservative age estimate is post-Early Jurassic and pre-Late Pleistocene. Further age refinement depends on correlation of similar units [see article].||||Unconformably underlain by Hawkesbury Sandstone, and Ashfield Shale and Bingelly Shale of the Wianamatta Group. [Conformably?] overlain by Londonderry Clay.|Coarse-grained, consolidated to unconsolidated, rounded to well-rounded, pebble- to boulder-sized clasts of granite, quartz porphyry, quartzite, slate, silcreate, chert, hornfels, mudstone, and sandstone in a sandy or sandy clay matrix.|
16079|Rickabys Creek Gravel|75059|6|Mentioned|p8|Cenozoic|Cenozoic|NW Cumberland Basin, Sydney area. A train of fluvial deposits, traceable from the Blue Mountains Plateau, down the face of the Lapstone Monocline, and NE across the Cumberland Basin. Also appears as Rickaby's Creek Gravel.||||||
16116|Risdon Stud Formation|31999|6|Mentioned|Table 1|||||||||
16116|Risdon Stud Formation|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian?  to Lower Devonian. Of Silverwood Group.||||||25-OCT-05
16116|Risdon Stud Formation|32672|6|Mentioned|p673|||||||||
16116|Risdon Stud Formation|33146|5|Briefly described|p2|||See also p3. ?Sil.-L.Dev.||||||07-SEP-18
16116|Risdon Stud Formation|33703|6|Mentioned|p207|||||||||
16116|Risdon Stud Formation|35311|6|Mentioned|p207|||||||||
16116|Risdon Stud Formation|35652|4|Described|p6|||||||||
16116|Risdon Stud Formation|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
16116|Risdon Stud Formation|39071|6|Mentioned|p345|||||||||
16116|Risdon Stud Formation|39445|5|Briefly described|Table 5,p77|||||||||25-OCT-05
16116|Risdon Stud Formation|42031|5|Briefly described|Fig.3 P759|||||||||
16116|Risdon Stud Formation|48940|3|Fully described|p24|||||||||
16116|Risdon Stud Formation|61392|4|Described|p163-165, p166|Pridoli|Middle Cambrian|Of the Silverwood Group (Keinjan Terrane). Represents a normal clastic or mixed mud and mud/sand-rich slope apron. Age: 512-414Ma. Max. thickness: ~2500m.||||||07-FEB-11
16116|Risdon Stud Formation|63731|5|Briefly described|Map legend|Devonian|Silurian|Of the Silverwood Group. Silicified, fine-gr., cherty, andesitic crystal-lithic tuff, interbedded with subordinate thin to medium bedded, fine-gr. silicified arenite and mudstone (turbidites).||||||12-DEC-07
16116|Risdon Stud Formation|63748|4|Described|p6, p7 Fig. 3|Middle Silurian|Early Cambrian|Of Silverwood Group. Conformable below Connolly Volcanics. Max.thickness: ~2500m. Geol.Prov:Silverwood Prov.Silicified, fine-gr.cherty pyroclastic andesitic crystal-lithic tuffs, interbedded + subordinate thin-medium bedded, fine-gr.silicified turbidites.||||||07-FEB-11
16116|Risdon Stud Formation|68679|5|Briefly described|p445-447|Silurian|Silurian|Olgers et al. (1974). Silverwood Province. ~2500m thick. Age discussed.||Basal Silverwood Group.||Is overlain by Connolly Volcanics.|Cherty andesitic crystal-lithic tuff, and subordinate thin- to medium-bedded turbidites.|
16116|Risdon Stud Formation|71628|5|Briefly described|p19: 59, 67|||||Silverwood Group.||Is intruded by Herries Monzogranite.|Silicified, fine-grained, cherty, andesitic crystal-lithic tuff, interbedded with subordinate thin- to medium-bedded, fine-grained, silicified arenite and mudstone (turbidites).|
16153|Rixons Pass Teschenite|36220|4|Described|p96|||||||||
16153|Rixons Pass Teschenite|37253|6|Mentioned|Table 1|||||||||
16153|Rixons Pass Teschenite|42896|5|Briefly described|p55|||||||||
16202|Rockhampton Group|22482|6|Mentioned|Fig.1|||||||||
16202|Rockhampton Group|22800|6|Mentioned|Fig.14 p592|||||||||
16202|Rockhampton Group|23468|4|Described|p 305|||also see Fig 2 p 295||||||
16202|Rockhampton Group|23799|3|Fully described|p27, p15 Tb. 1|Carboniferous|Devonian|Formerly mapped as Caswell Cr. Gp. and Derrangabungy beds in the MONTO/MUNDUBBERA areas (Murphy, 1976a) - redefined by Yarrol Project Team (1997).  Detailed history of naming of units included on p27.  Max. thickness: <1000m.  Geol. Prov: Yarrol Province.||||||14-DEC-05
16202|Rockhampton Group|23800|5|Briefly described|Map legend|Carboniferous|Devonian|||||||
16202|Rockhampton Group|24399|3|Fully described|p275, p272 Fig. 1|Early Carboniferous|Early Carboniferous|Characterised by thick lenses of oolitic limestone, although not dominant.  Part of the Bindawalla Stratigraphic Assemblage (Bryan et al, 2001).  Geological Province: New England Fold Belt.||||||
16202|Rockhampton Group|24420|4|Described|p7|Early Carboniferous|Early Carboniferous|Previously mapped as Caswell Creek Group.||||||
16202|Rockhampton Group|24467|5|Briefly described|p392|Early Carboniferous|Late Devonian|Geological Province: Yarrol Terrane||||||
16202|Rockhampton Group|24488|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|24489|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|24491|4|Described|p19|Early Carboniferous|Early Carboniferous|Now includes Neils Creek Clastics, Caswell Creek Group and Cania Formation. Formerly referred to as Rockhampton Series.||||||
16202|Rockhampton Group|24571|6|Mentioned|p4|||||||||
16202|Rockhampton Group|24615|5|Briefly described|CD|Early Carboniferous|Early Carboniferous|[Cr].  Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||
16202|Rockhampton Group|30451|6|Mentioned|p30|||||||||
16202|Rockhampton Group|30840|5|Briefly described|p780|||||||||
16202|Rockhampton Group|30914|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian - Carboniferous||||||
16202|Rockhampton Group|31519|6|Mentioned|p917|||||||||
16202|Rockhampton Group|31656|6|Mentioned|p6|||||||||
16202|Rockhampton Group|31657|4|Described|p94|||See also p95, 101. U.Tournaisian to U.Visean||||||12-NOV-15
16202|Rockhampton Group|31658|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|31659|4|Described|p51, p52-54|Visean|Tournaisian|max. thickness: 6500ft. Mudstone, siltstone, feldspathic and lithic sandstone, conglomerate, oolitic limestone. See also Table 1.||||||08-OCT-08
16202|Rockhampton Group|32141|6|Mentioned|p149|||Visean||||||
16202|Rockhampton Group|32358|4|Described|Table 2|||p15.||||||12-NOV-15
16202|Rockhampton Group|32959|6|Mentioned|p47|||||||||
16202|Rockhampton Group|33879|6|Mentioned|p284|||||||||
16202|Rockhampton Group|34155|6|Mentioned|p91|||Lower Carboniferous. See also p105.||||||12-NOV-15
16202|Rockhampton Group|34287|6|Mentioned|p110|||See also p111.||||||12-NOV-15
16202|Rockhampton Group|34346|6|Mentioned|p1|||||||||
16202|Rockhampton Group|35008|5|Briefly described|p178|||||||||
16202|Rockhampton Group|35266|6|Mentioned|p201|||||||||
16202|Rockhampton Group|35952|5|Briefly described|p500|||||||||
16202|Rockhampton Group|36210|6|Mentioned|Fig.1|||See also p263.||||||12-NOV-15
16202|Rockhampton Group|36528|6|Mentioned|p173|||||||||
16202|Rockhampton Group|37565|6|Mentioned|Fig.6|||See also Fig.8||||||
16202|Rockhampton Group|38081|5|Briefly described|Table 1|||||||||
16202|Rockhampton Group|38084|5|Briefly described|p54|||||||||
16202|Rockhampton Group|38406|5|Briefly described|p11|||||||||
16202|Rockhampton Group|39445|6|Mentioned|Table 6|||||||||
16202|Rockhampton Group|39973|6|Mentioned|p4|||||||||
16202|Rockhampton Group|39987|6|Mentioned|p65|||||||||
16202|Rockhampton Group|40623|5|Briefly described|p79|||||||||
16202|Rockhampton Group|40735|6|Mentioned|Fig.1|||||||||
16202|Rockhampton Group|41576|4|Described|p17|||See also Table 1.||||||12-NOV-15
16202|Rockhampton Group|41577|6|Mentioned|Map legend|Early Carboniferous||||||||
16202|Rockhampton Group|41826|6|Mentioned|p325|||||||||
16202|Rockhampton Group|41922|4|Described|Table 1, p10|||||||||12-NOV-15
16202|Rockhampton Group|41925|5|Briefly described|p44|||||||||
16202|Rockhampton Group|42486|5|Briefly described|p198|||||||||
16202|Rockhampton Group|42547|5|Briefly described|p49|||||||||
16202|Rockhampton Group|42583|5|Briefly described|p65|||||||||
16202|Rockhampton Group|42929|5|Briefly described|p458|||||||||
16202|Rockhampton Group|43771|5|Briefly described|p813||Early Carboniferous|||||||
16202|Rockhampton Group|44091|14|Not recorded|p36||Early Carboniferous|||||||
16202|Rockhampton Group|44360|14|Not recorded|p4,31||Early Carboniferous|Compared with Caswell Creek Group. See also Lexicon.||||||
16202|Rockhampton Group|44369|2|Defined|p174-175|||See also Lexicon.||||||
16202|Rockhampton Group|44370|14|Not recorded|p219,Tb.7|||See also Lexicon.||||||
16202|Rockhampton Group|44379|14|Not recorded|p15|||Ref. to Fleming 1967.||||||
16202|Rockhampton Group|44388|2|Defined|p113,116||Early Carboniferous|Includes Gudman Oolite, Malchi Formation, Lion Creek Limestone.||||||
16202|Rockhampton Group|44619|14|Not recorded|Fig.2,p189,190|Visean|Tournaisian|(Tournaisian-Early Visean)||||||
16202|Rockhampton Group|44852|14|Not recorded|p73||Early Carboniferous|||||||
16202|Rockhampton Group|45097|6|Mentioned|p23|||?Correlation with Cania Fm.||||||
16202|Rockhampton Group|48921|6|Mentioned|p10|||||||||
16202|Rockhampton Group|50197|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50207|5|Briefly described|Map Legend|Early Permian|Early Carboniferous|||||||
16202|Rockhampton Group|50208|5|Briefly described|Map Legend|Early Permian|Early Carboniferous|||||||14-MAY-04
16202|Rockhampton Group|50209|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Includes: Gudman Oolite, Malchi Formation, Lion Creek Limestone.||||||
16202|Rockhampton Group|50212|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50213|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Overlain by Lorray Formation.||||||17-MAY-04
16202|Rockhampton Group|50214|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Overlain by  Youlambie Conglomerate.||||||17-MAY-04
16202|Rockhampton Group|50317|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
16202|Rockhampton Group|50598|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate.||||||21-JUL-04
16202|Rockhampton Group|60282|5|Briefly described|p9|Early Carboniferous|Early Carboniferous|Geological Province: Yarrol Province.||||||
16202|Rockhampton Group|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Dark grey mudstone, siltstone, felsic volcaniclastic sandstone, polymictic conglomerate, ooid bearing sandstone and conglomerate with mudstone rip up clasts; limestone; rare rhyolitic ignimbrite.||||||
16202|Rockhampton Group|60557|4|Described|p18 Fig. 5a, p22|Carboniferous|Carboniferous|Conformably overlies the Mount Alma Formation; conformably to disconformably overlain by Lorray Formation.  See also p19-20 Figs. 5b,c and p39.||||||09-JUN-05
16202|Rockhampton Group|60705|5|Briefly described|p645, p655|Early Carboniferous|Early Carboniferous|Correlative of the Campwyn Volcanics in northern New England Fold Belt. Age: 385-321 Ma and 350.9+/-2.7 Ma as the crystalline age. Geological Province: Yarrol terrane.||||||12-APR-05
16202|Rockhampton Group|61035|5|Briefly described|p13|Carboniferous|Early Carboniferous|Includes; Tournaisian oolitic limestones, Campwyn Volcanics. Geological Province: Yarrol Province.||||||07-FEB-11
16202|Rockhampton Group|61557|5|Briefly described|p878.|||Yarrol Shelf. Crops out SW of Rockhampton. ~2000m thick sequence deposited on a tectonically and volcanically active marine shelf bordering a continental landmass to the west.|||Includes Gudman Formation.||Sequence of siliciclastic-volcaniclastic sedimentary rocks punctuated by minor, scattered, laterally discontinuous carbonate intervals.|
16202|Rockhampton Group|61730|5|Briefly described|p994 Fig.1|Early Carboniferous|Early Carboniferous|Geological Province: Yarrol Province. See also p1000 Fig.3, p1008.||||||
16202|Rockhampton Group|61777|5|Briefly described|p230|||Geological Province: Yarrol Province.||||||07-FEB-11
16202|Rockhampton Group|61778|5|Briefly described|p234 Fig. 1, p237|Early Carboniferous|Early Carboniferous|Geological Province: Berserker Subprovince.||||||07-FEB-11
16202|Rockhampton Group|63832|6|Mentioned|p131 fig 2|Carboniferous|Carboniferous|Of east Bowen Basin.||||||
16202|Rockhampton Group|64398|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Dark grey mudstone, siltstone, felsic volcanoclastic sandstone, polymictic conglomerate, ooid-bearing sandstone and conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||18-AUG-08
16202|Rockhampton Group|64399|5|Briefly described|Map legend|Early Carboniferous|Early Carboniferous|Overlain by Lorray Fm. Dk grey mudst, siltst., felsic volcaniclastic sandst., polymictic conglom., ooid-bearing sandstone + conglomerate with mudstone rip-up clasts; oolitic and pisolitic limestone and minor skeletal limestone; rare rhyolitic ignimbrite.||||||19-AUG-08
16202|Rockhampton Group|64429|6|Mentioned|p16 Fig.1|Early Carboniferous|Early Carboniferous|Part of the Yarrol Block.||||||
16202|Rockhampton Group|64631|5|Briefly described|p44 Fig.2.|Serpukhovian|Carboniferous|Northern New England Fold Belt. Shown with Campwyn Volcanics. Biostratigraphic age control for top and oolitic limestone intervals. Also some radiometric age control within Group.||||||
16202|Rockhampton Group|65003|5|Briefly described|p3, p19|Early Carboniferous|Early Carboniferous|Of Yarrol Province. Sedimentary and volcanic rocks.||||||30-MAR-12
16202|Rockhampton Group|65388|4|Described|p73-74; p70, 58, 69, p70, 208, 439|Tournaisian||Rockhampton Subprovince, Yarrol Province. Previously unnamed D-Ca unit of Malone, 1970; Studied on the western side of Long Island by Leitch and others (1994) and were assigned to the Campwyn Volcanics; overlain conformably (gradationally) by rocks assigned to the Lorray Formation.  Unconformably overlain by Muncon Volcanics. Age: 350.9+/- 2.7 Ma U-Pb LA-ICP-MS age (Bryan et al 2004). Volcaniclastics and oolitic limestone (towards top).||||||
16202|Rockhampton Group|67203|5|Briefly described|p7, p10-11, p30-31|Early Carboniferous|Early Carboniferous|Formed a topographically diverse basement to Bobby Volcanics.||||Is overlain unconformably by Bobby Volcanics.||
16202|Rockhampton Group|67874|5|Briefly described|p14-15|Carboniferous|Carboniferous|||||Is overlain unconformably by Bobby Volcanics.||06-NOV-15
16202|Rockhampton Group|68008|2|Defined|Throughout.|Visean|Tournaisian|See also. Fleming (1960, 1967). Originally the Rockhampton Series of Daintree (1870). Expanded by the Yarrol Project Team (1997) to include the former Caswell Creek Group, Neils Creek Clastics, Cannindah Limestone and Cania Formation. Thus it is the most widely distributed unit in Yarrol Province: a discontinuous belt of scattered outcrops 260km long and up to 55km wide. The type sections for each constituent are in the type area at Malchi Creek (Fleming, 1967); details given of changes to the upper boundary (Lion Creek Limestone). 1980m thick at type section; up to c.4000m elsewhere. In Glenmore and Yarwun areas, mapped areas of the Group have been reassigned to Mount Alma Formation and Berserker Group respectively. Eleven sedimentary facies and six facies associations are described in great detail. Oolitic limestone is identical in lithology and age to that in Balaclava Formation. Geochemistry described in some detail. Geophysics modelling. Extremely low magnetic response. Numerous zircon U-Pb ages from ignimbrites; also 356.8+/-3.8 Ma (Fanning, 2012). Princhester Serpentinite is thrust over this unit. Structure and its timing discussed. Micropaleontology detailed. Shelly fossils listed; locations. Measured section diagram.|361.1 +/- 5.2 Ma; 350.9 +/- 2.7 Ma.||Gudman Oolite, Malchi Formation, Lion Creek Limestone.|Overlies Balaclava Formation, Three Moon Conglomerate and Mount Alma Formation. Is overlain by Lorray Formation and many others. Numerous intrusions. Equivalent to Wandilla Formation.|Dominated by siltstone and mudstone. Also calcareous sandstones, feldspatholithic sandstones, polymictic conglomerate, and characteristic oolitic/pisolithic limestones and ooid-bearing sandstones. Local andesitic to rhyolitic lavas and pyroclastics.|
16202|Rockhampton Group|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Yarrol Province.||||||
16202|Rockhampton Group|68679|4|Described|p308, p312-314, p316-317, p321, p337-341|Mississippian|Mississippian|See also p345, p347, p349-350, p419, p425-426, p441, p443 Fig.5.103, p468. Fleming (1960, 1967) in the Neerkol area. Rockhampton Subprovince, Northern Yarrol Province. Mainly volcaniclastic sediments from an arc to the west, but is characterised by repeated development of oolitic carbonate banks along the W margin. Lithologies and fossil faunas described in some detail. A source of sediments for the Moah Creek beds. U-Pb zircon ages by Bryan et al. (2004). RELATED UNITS (continued):  Is intruded by May Queen, Gracemere Gabbros, Zig Zag Tonalite, Mannersley Quartz Microdiorite, Bajool Quartz Diorite, Kabra Quartz Monzodiorite, Pack Granite and Bocoolima, Rocky Point Granodiorites.|361.1 +/- 5.2 Ma; 350.9 +/- 2.7 Ma.||Gudman Ooloite, Malchi Formation, Lion Creek Limestone.|Is overlain by Lorray Formation and unconformably by Berserker Group and Bobby Volcanics. Is faulted against the Marble Waterhole beds. See COMMENTS for more.|Oolitic, bioclastic and pisolitic limestone; calcareous, ooid-rich, medium to coarse sandstone; calcareous, fossiliferous, fine-grained to very coarse-grained sandstone; ooid-bearing feldspatholithic sandstone; siltstone and mudstone; conglomerate.|
16202|Rockhampton Group|69594|6|Mentioned|p561|||||||Is intruded by Ridler Monzonite.||
16202|Rockhampton Group|69952|6|Mentioned|p75|Early Carboniferous|Early Carboniferous|||||||06-NOV-15
16202|Rockhampton Group|70050|5|Briefly described|p316|Early Carboniferous|Early Carboniferous|Yarrol Basin. The type area is in the Lion Creek, Ridgelands and Fitzroy blocks. Numerous (coral) fossiliferous locality investigations mentioned.||||||
16202|Rockhampton Group|73197|6|Mentioned|p467|Carboniferous|Early Carboniferous|New England Orogen, northern. Yarrol Province. Forearc basin shallow marine environment. Described as lower to mid Carboniferous in text.|||||Common oolitic limestones.|
16202|Rockhampton Group|73450|6|Mentioned|p36, p59, p67|Carboniferous|Carboniferous|||||Intruded by Toondahra Granite and Ridler Monzonite (Glassford Igneous Complex).||
16209|Rockisle Granodiorite|38822|5|Briefly described|p194|||||||||
16209|Rockisle Granodiorite|39874|6|Mentioned|p375|||||||||
16209|Rockisle Granodiorite|41348|5|Briefly described|Map legend|Early Paleozoic||Adamellite, granodiorite.||||||07-NOV-08
16209|Rockisle Granodiorite|68005|5|Briefly described|p135.|Permian|Permian|||Unit in Nundle Suite.|||Granodiorite and minor monzogranite bearing trace secondary sub-aluminous calcic amphibole; primary hornblende-bearing granitoids of mafic complexes; some are amphibole-bearing phases in Clarence River Supersuite members.|
16209|Rockisle Granodiorite|71628|4|Described|p1:6; p3: 3-4, 69, 77; p9:1; p18:1|||See also p19: 2, 4, 151-156. Binns et al. (1967). Included in Nundle Suite by Hensel et al. (1985); excluded (unassigned) by Bryant et al. (2003), after unpublished work by Chappell and Bryant (1994). Named after a local homestead. Forms a broadly triangular, ~4 x 3 km, intrusion ~3 km SE of Niangala in cleared, flat farmland. Southern New England Orogen. Is interspersed with S-type granites. Excluded from Hillgrove Supersuite. Lithology and mineralogy described in great detail. Geochemistry detailed.|294.9 +/- 2.9 Ma (SHRIMP: Rosenbaum et al., 2012).|Rockisle Suite.||Intrudes Sandon Association.|Somewhat reduced I-type granitoids: greenish-grey to light grey, texturally heterogeneous, fine- to medium-grained hornblende-biotite granodiorite to monzogranite; sheared eastern margin.|
16213|Rockley Volcanics|13139|6|Mentioned|p10|||||||||
16213|Rockley Volcanics|22503|6|Mentioned|p645||Late Ordovician|||||||
16213|Rockley Volcanics|22577|5|Briefly described|p119,122||Ordovician|||||||
16213|Rockley Volcanics|22679|5|Briefly described|p 7, 23|||||||||
16213|Rockley Volcanics|22704|6|Mentioned|p65||Ordovician|||||||
16213|Rockley Volcanics|22857|4|Described|p126, p428 App. 1 Tb. A1.5|Late Ordovician|Late Ordovician|Of the Cabonne Group. Volcanic arenite, minor breccia and conglomerate; chert, siltstone. Overlies the Adaminaby Group. Max. thickness: 5000m in Oberon area. See also p430 App. 1 Tb. A1.5.||||||
16213|Rockley Volcanics|23214|3|Fully described|p76|Late Ordovician|Late Ordovician|Of Cabonne Group. Intruded by Davies Creek Granite. Consists of three unnamed units. Max. thickness 5000m.||||||
16213|Rockley Volcanics|23245|6|Mentioned|p126|||||||||
16213|Rockley Volcanics|23309|6|Mentioned|p390|||||||||
16213|Rockley Volcanics|23334|6|Mentioned|10|||||||||
16213|Rockley Volcanics|24269|4|Described|p1553, p1554 Fig.1B|Late Ordovician|Middle Ordovician|Underlain by Triangle Formation. Geological Province: Lachlan Fold Belt||||||28-MAY-08
16213|Rockley Volcanics|29903|6|Mentioned|p168|||||||||
16213|Rockley Volcanics|29989|6|Mentioned|Map legend|Paleozoic|Paleozoic|Cambrian?||||||07-NOV-08
16213|Rockley Volcanics|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|30109|6|Mentioned|Fig.1|||Ordovician age.||||||
16213|Rockley Volcanics|30453|6|Mentioned|Fig.2|||||||||
16213|Rockley Volcanics|30731|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|30734|6|Mentioned|p3|||||||||
16213|Rockley Volcanics|32088|6|Mentioned|p6|||Ordovician||||||
16213|Rockley Volcanics|32347|6|Mentioned|p182|||||||||
16213|Rockley Volcanics|32483|4|Described|p12|||Ord. Strat. table 1. See also p25.||||||28-MAY-08
16213|Rockley Volcanics|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|32672|6|Mentioned|p668|||||||||
16213|Rockley Volcanics|32999|5|Briefly described|p9|||Strat. Refers Stanton(1956). Section P17||||||
16213|Rockley Volcanics|33002|6|Mentioned|p417|||Teconic history||||||
16213|Rockley Volcanics|33004|6|Mentioned|p181|||||||||
16213|Rockley Volcanics|33006|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|33282|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|33285|5|Briefly described|p19|||||||||
16213|Rockley Volcanics|33742|6|Mentioned|p116|||Strat. table.||||||
16213|Rockley Volcanics|34059|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16213|Rockley Volcanics|34404|3|Fully described|p83|||||||||
16213|Rockley Volcanics|34405|6|Mentioned|p108|||||||||
16213|Rockley Volcanics|34481|6|Mentioned|Map legend|Late Ordovician|Late Ordovician|||||||
16213|Rockley Volcanics|35118|6|Mentioned|Fig.5|||||||||
16213|Rockley Volcanics|35185|6|Mentioned|p245|||||||||
16213|Rockley Volcanics|35875|6|Mentioned|p14|||||||||
16213|Rockley Volcanics|36390|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
16213|Rockley Volcanics|36534|5|Briefly described|p21|||Also mention P223.||||||
16213|Rockley Volcanics|37727|6|Mentioned|p28|||See also P41,66 and Fig.1.||||||
16213|Rockley Volcanics|39663|6|Mentioned|Table 1|||||||||
16213|Rockley Volcanics|39718|5|Briefly described|p143|||||||||
16213|Rockley Volcanics|40136|5|Briefly described|p38|||||||||
16213|Rockley Volcanics|40328|6|Mentioned|p166|||See also P176||||||
16213|Rockley Volcanics|40762|6|Mentioned|p272|||||||||
16213|Rockley Volcanics|41746|5|Briefly described|p451|||||||||
16213|Rockley Volcanics|42712|4|Described|8,12,16,19;Table1p14|Late Ordovician|Early Ordovician|Now forms part of Cabonne Group||||||
16213|Rockley Volcanics|42941|5|Briefly described|p1|||||||||
16213|Rockley Volcanics|43357|14|Not recorded|155-161|Early Ordovician||||||||
16213|Rockley Volcanics|43385|14|Not recorded|p169,170|Ashgillian|Caradocian|||||||
16213|Rockley Volcanics|43469|2|Defined|p131-35,137,139,142,||Late Ordovician|p144||||||
16213|Rockley Volcanics|43479|14|Not recorded|p79,94,95f|Ashgillian|Llandeilian|||||||
16213|Rockley Volcanics|43515|14|Not recorded|Map Legend||Ordovician|(Provisional Edition) See also Lexicon||||||
16213|Rockley Volcanics|43516|14|Not recorded|Map Legend||Ordovician|||||||
16213|Rockley Volcanics|43633|4|Described|p17|Late Ordovician|Early Ordovician|(M.Ord-L.Ord)||||||
16213|Rockley Volcanics|43639|5|Briefly described|Map Legend||Ordovician|||||||
16213|Rockley Volcanics|43641|5|Briefly described|Map Legend||Ordovician|||||||
16213|Rockley Volcanics|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Cabonne Group. Volcanic sandstone, minor breccia and conglomerate.||||||17-JUL-08
16213|Rockley Volcanics|43782|5|Briefly described|Map Legend|Bolindian|Gisbornian|of Cabonne Group.||||||
16213|Rockley Volcanics|44093|5|Briefly described|p112|Ordovician|Ordovician|Of the Cabonne Group. Interdigitate with the Burra Burra Creek Formation. See also p207 Appendix 1. Geological Province: Lachlan Fold Belt.||||||24-MAR-05
16213|Rockley Volcanics|44852|14|Not recorded|p60||Ordovician|||||||
16213|Rockley Volcanics|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p156|Late Ordovician|Late Ordovician|Includes; Rockley Volcanic Member, Swatchfield Monzonite. Geological Province: Rockley-Gulgong Volcanic Belt, LFB.||||||07-FEB-11
16213|Rockley Volcanics|63283|6|Mentioned|p195 Fig. 2, p205, p209|Late Ordovician|Late Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt. Unit consists of volcaniclastic rocks. Part unit probably correlates to the Byng Volcanics of the Molong Volcanic Belt.||||||07-FEB-11
16213|Rockley Volcanics|63286|6|Mentioned|p308 Fig. 9|Bolindian|Darriwilian|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
16213|Rockley Volcanics|63289|5|Briefly described|p369, p371|Ordovician|Ordovician|Probably overlie Triangle Formation. Intruded by Swatchfield Monzonite. Geological Province: Rockley - Gulgong Volcanic Belt. Consists of schistose, greenschist-facies pyroxene-phyric basalt, basaltic breccia.||||||07-FEB-11
16213|Rockley Volcanics|63290|5|Briefly described|p389, p396 Fig. 3|Late Ordovician|Gisbornian|Underlain by Triangle Formation and Mozart Chert. Geological Province: Junee - Narromine Volcanic Belt.||||||
16213|Rockley Volcanics|63293|5|Briefly described|p471, p469 Fig. 2|Bolindian|Gisbornian|Underlain by Triangle Formation, Mozart Chert. Intruded by Swatchfield Monzonite. Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
16213|Rockley Volcanics|63633|5|Briefly described|Map Legend|Llandovery|Bolindian|Andesite flows, andesite tuffs, talc schists, pyritic schist, pyroclastics.||||||
16213|Rockley Volcanics|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Cabonne Group. Andesite and andesitic volcaniclastic sandstone.||||||
16213|Rockley Volcanics|67106|6|Mentioned|p673-677, 679, 681-683|||Rockley-Gulgong Volcanic Belt.|454.3 +/- 2.9 Ma.||||Includes mafic volcaniclastic sandstone.|
16213|Rockley Volcanics|67322|5|Briefly described|p18|||Occurs in the Oberon-Rockley region. Discussion of possible regional geology scenarios.||||Overlain by the Triangle Formation.|Quartz siltstones and volcaniclastic strata.|22-FEB-18
16213|Rockley Volcanics|67847|5|Briefly described|p4, p20, p25, p26 fig 4.2|Silurian|Ordovician|Lachlan Orogen (together with the Triangle Formation comprises the southern part of the Rockley-Gulgong belt of the Macquarie Arc). See also p27-p29, p31-p32.||||Conformably overlies the Triangle Formation. Intruded by the Swatchfield Monzonite and the Greenslopes Porphyry.|Mafic volcanics.|
16213|Rockley Volcanics|68592|3|Fully described|p370-7, p386-8, p390-9, p421, p423, p425|Late Ordovician|Late Ordovician|See also p607. Stanton (1956); has un-named sub-units. Two occurrences have been re-allocated during recent mapping: Isabella River outcrops to the Jeremy Formation, and Phils River (near Thalaba) outcrops to Kangaloolah Volcanics. c.1200m thick. Suggested representative section mentioned. Geochemistry and lithology described in some detail. Non-fossiliferous. Quartz veins host minor Cu and Au mineralisation.||Unit in Cabonne Group.||Overlies Mozart Chert. Is intruded by Swatchfield Monzonite. Is overlain unconformably by Fosters Creek Conglomerate and Shivering Conglomerate, and by Wheeo Basalt.|Grey to green, massive, coarsely to finely porphyritic andesite or basalt; subordinate andesitic volcanic sandstone and siltstone, mafic schist.|22-SEP-16
16213|Rockley Volcanics|70192|5|Briefly described|Map Legend|Bolindian|Gisbornian|[Theta]cr. On Taralga 1:100 000 mapsheet portion of Time-Space Plot.||Cabonne Group|||Massive to flow banded, coarsely to finely porphyritic, andesite to basalt with phenocrysts of plagioclase, pyroxene and hornblende; minor andesitic volcanic sandstone and siltstone.|
16213|Rockley Volcanics|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc ?Phase 4 volcanic unit. Age range poorly known. Rockley-Gulgong Volcanic Belt.|c. 449-443 Ma|Cabonne Group||||
16213|Rockley Volcanics|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Cabonne Group|||Massive to flow banded, coarsely to finely porphyritic, andesite to basalt with phenocrysts of plagioclase, pyroxene and hornblende; minor andesitic volcanic sandstone and siltstone.|
16213|Rockley Volcanics|70684|6|Mentioned|p3, p75|Late Ordovician|Late Ordovician|Rockley-Gulgong Volcanic Belt.||||||
16213|Rockley Volcanics|73154|5|Briefly described|p77 Fig.3|Late Ordovician|Late Ordovician|Macquarie Arc, Phase 4. Rockley-Gulgong Volcanic Belt. Shoshonitic.|||||Intermediate-mafic lava, conglomerate, siltstone.|
16213|Rockley Volcanics|73264|6|Mentioned|p1391 Fig.13, p1407|Silurian|Early Ordovician|Lachlan Orogen, Macquarie Volcanic Province, phase 4. Probably Silurian in age.||||||
16213|Rockley Volcanics|73431|5|Briefly described|p364-365|Ordovician|Ordovician|Lachlan Orogen, Macquarie Arc. Apears as Rockley Volcnics p365.||||Intruded by Davies Creek Granite.|Tightly folded greenschist-facies meta-volcaniclastic and volcanic rocks.|
16213|Rockley Volcanics|73582|6|Mentioned|p107|Silurian|Silurian|||||||
16216|Rocksberg Greenstone|22784|6|Mentioned|p3|||||||||
16216|Rocksberg Greenstone|22845|4|Described|p7,9-12,67,fig6|||After Bryan an Jones (1950) and Cranfield (1976).  Correlates with Peters Creek Greenstone.||||||
16216|Rocksberg Greenstone|22846|6|Mentioned|p44|Carboniferous|Devonian|Intruded by Neurum Complex.||||||
16216|Rocksberg Greenstone|23251|6|Mentioned|p3|||Was previously included in the Gympie Group by Day & others (1978). Gympie Group.||||||
16216|Rocksberg Greenstone|23542|5|Briefly described|Fig 1 p378|||||||||
16216|Rocksberg Greenstone|24418|5|Briefly described|p5, Map 1|Carboniferous|Carboniferous|Volcanic rocks of basaltic composition. Strongly deformed. Outcrop: pale green, strong foliation (layering), fine grained greenschist, some layers mica schist.||||||30-JUN-06
16216|Rocksberg Greenstone|29555|6|Mentioned|p12|||||||||
16216|Rocksberg Greenstone|30797|5|Briefly described|Table 1|||Palaeozoic, useful for concrete aggregate and road screenings.||||||
16216|Rocksberg Greenstone|30914|6|Mentioned|Map legend|Permian|Carboniferous|Carboniferous - Permian||||||
16216|Rocksberg Greenstone|30915|6|Mentioned|p101|||||||||
16216|Rocksberg Greenstone|31131|5|Briefly described|p153|||Contact with Neranleigh-Fernvale Gp. discussed.||||||
16216|Rocksberg Greenstone|31271|6|Mentioned|Fig. 2|||||||||
16216|Rocksberg Greenstone|31756|6|Mentioned|p16|||Early Palaeozoic||||||
16216|Rocksberg Greenstone|31757|6|Mentioned|p9|||||||||
16216|Rocksberg Greenstone|31811|6|Mentioned|Fig. 1|||||||||
16216|Rocksberg Greenstone|31999|6|Mentioned|p133|||||||||
16216|Rocksberg Greenstone|35007|6|Mentioned|p73|||||||||
16216|Rocksberg Greenstone|35101|3|Fully described|p11|||||||||
16216|Rocksberg Greenstone|35126|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16216|Rocksberg Greenstone|35156|5|Briefly described|p4|||See also Table.2||||||
16216|Rocksberg Greenstone|35410|6|Mentioned|p91|||||||||
16216|Rocksberg Greenstone|35430|6|Mentioned|Table 1|||Interpretation of stratigraphic successions||||||
16216|Rocksberg Greenstone|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
16216|Rocksberg Greenstone|35866|6|Mentioned|p400|||See also P402.||||||
16216|Rocksberg Greenstone|36238|6|Mentioned|Table 1|||||||||
16216|Rocksberg Greenstone|36440|6|Mentioned|Map legend|Late Carboniferous|Early Carboniferous|Early to Late Carboniferous||||||
16216|Rocksberg Greenstone|36528|6|Mentioned|p171|||Also mention P174.||||||
16216|Rocksberg Greenstone|36547|6|Mentioned|Table 2|||||||||
16216|Rocksberg Greenstone|37252|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16216|Rocksberg Greenstone|38074|5|Briefly described|Table 1|||||||||
16216|Rocksberg Greenstone|38077|5|Briefly described|p29|||||||||
16216|Rocksberg Greenstone|38391|6|Mentioned|p7|||||||||
16216|Rocksberg Greenstone|39079|5|Briefly described|p6|||||||||
16216|Rocksberg Greenstone|39445|5|Briefly described|Table 7|||See also P79, P83 & Fig.7||||||
16216|Rocksberg Greenstone|40051|4|Described|p5|||||||||
16216|Rocksberg Greenstone|40245|6|Mentioned|p182|||||||||
16216|Rocksberg Greenstone|40475|6|Mentioned|p3|||||||||
16216|Rocksberg Greenstone|40517|6|Mentioned|p358|||||||||
16216|Rocksberg Greenstone|40579|6|Mentioned|Map legend|Permian|Carboniferous|Permian to Carboniferous||||||
16216|Rocksberg Greenstone|40623|5|Briefly described|p53|||||||||
16216|Rocksberg Greenstone|41917|6|Mentioned|p521|||||||||
16216|Rocksberg Greenstone|42525|5|Briefly described|Map legend|Paleozoic|Paleozoic|Geological Province: D'Aguilar Block.||||||07-NOV-08
16216|Rocksberg Greenstone|42547|4|Described|p54, p55|||||||||
16216|Rocksberg Greenstone|42619|6|Mentioned|p29|||||||||
16216|Rocksberg Greenstone|42970|5|Briefly described|p117|||||||||
16216|Rocksberg Greenstone|43006|5|Briefly described|Table 1,p239|||||||||
16216|Rocksberg Greenstone|43017|5|Briefly described|p379|||||||||
16216|Rocksberg Greenstone|43076|5|Briefly described|p5|||||||||
16216|Rocksberg Greenstone|43092|5|Briefly described|Fig.2|||||||||
16216|Rocksberg Greenstone|43100|6|Mentioned|p6|||||||||
16216|Rocksberg Greenstone|44211|14|Not recorded|p89|||||||||
16216|Rocksberg Greenstone|44925|5|Briefly described|Map Legend|Carboniferous|Devonian|||||||
16216|Rocksberg Greenstone|45003|14|Not recorded|p256|||||||||
16216|Rocksberg Greenstone|48940|5|Briefly described|p7|||Refers Bryan & Jones (1950), Mathews (1954)||||||
16216|Rocksberg Greenstone|60077|5|Briefly described|Map legend|Paleozoic|Paleozoic|Basic metavolcanics.||||||07-NOV-08
16216|Rocksberg Greenstone|68327|5|Briefly described|Map legend.|Paleozoic|Paleozoic||||||Greenstone.|
16216|Rocksberg Greenstone|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Late Devonian|North D'Aguilar Subprovince. This unit, as well as Amamoor, Booloumba and Kurwongbah beds, the Gobongo, Manumbar, Widgee and Wongella Metamorphics, the Jimna Phyllite, Peters Creek Greenstone, Talamy Schist and Wide Bay Creek Gneiss, are all mapped under the symbol, DCdm.||||||
16216|Rocksberg Greenstone|68679|5|Briefly described|p321, p324, p326-329, p332, p369|||Northern New England Orogen. Forms a narrow NNW-trending belt east of Dayboro. Detachment zone and lower plate accretionary assemblages; may represent subducted seamount material exhumed during later extension. Typical of equivalent units such as Peters Creek Greenstone (a correlate) and parts of the Widgee and Wongella Metamorphics. Tectonically interleaved with Kurwongah beds. Thermochronology of phengite ages by Little, Holcombe abd McWilliams (1993).|~262-260 Ma : 40Ar/39Ar plateau ages.|||Is overlain unconformably by Mount Byron Volcanics. Is intruded by Neurum Complex. Is faulted against Jimna Phyllite, Northbrook beds and Neara Volcanics. Correlated with Mount Mia Serpentinite.|Strongly foliated, moderately to coarsely crystalline greenschist containing discrete layers millimetres to metres thick, with blue amphibole; highly deformed fragmental rocks common; blueschist-greenschist units with abundant pseudomorphs after cpx.|
16221|Rockton Granodiorite|22815|4|Described|p79|||||||||
16221|Rockton Granodiorite|22878|6|Mentioned|p74|||||||||
16221|Rockton Granodiorite|41850|6|Mentioned|p430|||||||||
16221|Rockton Granodiorite|42827|6|Mentioned|p430|||||||||
16221|Rockton Granodiorite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|of Tonghi Suite.||||||
16236|Rocky Creek Conglomerate|721|5|Briefly described|Map legend|Westphalian|Westphalian|Orthoconglomerate, minor feldsarenite and litharenite, siltstone and intermediate ashflow tuff.  Geological Province: Tamworth Belt.||||||21-DEC-04
16236|Rocky Creek Conglomerate|22857|4|Described|p241, p506 App.1 Tb.A1.8|Late Carboniferous|Late Carboniferous|Orthoconglomerate, minor feldsarenite and litharenite, siltstone, intermediate ashflow tuff. Max. thickness: 730m.||||||
16236|Rocky Creek Conglomerate|22863|6|Mentioned|p241|||||||||
16236|Rocky Creek Conglomerate|23050|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
16236|Rocky Creek Conglomerate|23051|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
16236|Rocky Creek Conglomerate|23861|5|Briefly described|p3, p4 Fig. 2|Westphalian|Westphalian|Underlain by Clifden Formation.  Geological Province: New England Orogen.||||||
16236|Rocky Creek Conglomerate|24010|5|Briefly described|p381|Westphalian|Westphalian|||||||
16236|Rocky Creek Conglomerate|24334|5|Briefly described|p49 Tb.1|Namurian|Namurian|Age: 311 -316 Ma.||||||
16236|Rocky Creek Conglomerate|24348|5|Briefly described|p131|Carboniferous|Carboniferous|||||||
16236|Rocky Creek Conglomerate|24424|5|Briefly described|p538, 539 Tb.4|Carboniferous|Carboniferous|Age: 300-315 Ma. Palaeomagnetic poles given.||||||
16236|Rocky Creek Conglomerate|24603|5|Briefly described|p866|Westphalian|Westphalian|See also p868 Fig. 3.  Geological Province: Tamworth Belt.||||||
16236|Rocky Creek Conglomerate|24605|2|Defined|p931, p935 Fig.4, p941|Namurian|Namurian|Overlain by the Lark Hill Formation. Overlies the Clifden Formation. Age: 319 Ma. Geological Province: New England Orogen||||||
16236|Rocky Creek Conglomerate|30133|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
16236|Rocky Creek Conglomerate|30135|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
16236|Rocky Creek Conglomerate|30340|6|Mentioned|p2530|||Lithology||||||
16236|Rocky Creek Conglomerate|30341|5|Briefly described|p139|||||||||
16236|Rocky Creek Conglomerate|30661|6|Mentioned|Table 1|||||||||
16236|Rocky Creek Conglomerate|30662|6|Mentioned|p188|||Palaeomagnetism||||||
16236|Rocky Creek Conglomerate|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16236|Rocky Creek Conglomerate|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16236|Rocky Creek Conglomerate|32672|6|Mentioned|p674|||||||||
16236|Rocky Creek Conglomerate|32683|6|Mentioned|p204|||Mid. Carb.||||||
16236|Rocky Creek Conglomerate|34072|6|Mentioned|Fig.4.5|||||||||
16236|Rocky Creek Conglomerate|34085|6|Mentioned|Cor.chart|||Stephanian||||||
16236|Rocky Creek Conglomerate|34330|6|Mentioned|p63|||||||||
16236|Rocky Creek Conglomerate|34349|4|Described|p246|||||||||
16236|Rocky Creek Conglomerate|35390|6|Mentioned|p98|||"Predictive profiling" applied to a simple anomaly on the Dunrobin road||||||
16236|Rocky Creek Conglomerate|36042|6|Mentioned|Fig.7|||||||||
16236|Rocky Creek Conglomerate|36045|6|Mentioned|p329|||||||||
16236|Rocky Creek Conglomerate|36528|6|Mentioned|p182|||||||||
16236|Rocky Creek Conglomerate|36961|6|Mentioned|Fig.3|||||||||
16236|Rocky Creek Conglomerate|37818|6|Mentioned|Table 2|||||||||
16236|Rocky Creek Conglomerate|37919|3|Fully described|p476|||||||||
16236|Rocky Creek Conglomerate|39287|6|Mentioned|p21|||See also Fig.2.2||||||
16236|Rocky Creek Conglomerate|39299|5|Briefly described|p279|||||||||
16236|Rocky Creek Conglomerate|39331|6|Mentioned|p103|||||||||
16236|Rocky Creek Conglomerate|41009|6|Mentioned|Fig.2|||||||||
16236|Rocky Creek Conglomerate|42141|6|Mentioned|Table 2 P571|||||||||
16236|Rocky Creek Conglomerate|42547|4|Described|p19|||Rocky Creek Syncline||||||
16236|Rocky Creek Conglomerate|43091|5|Briefly described|Map legend|||||||||
16236|Rocky Creek Conglomerate|43161|5|Briefly described|30|||||||||
16236|Rocky Creek Conglomerate|43383|14|Not recorded|p17|||||||||
16236|Rocky Creek Conglomerate|43385|14|Not recorded|p177||Late Carboniferous|||||||
16236|Rocky Creek Conglomerate|43409|14|Not recorded|Map Legend|||Currabubula Formation may be equivalent of Rocky Creek Conglomerate||||||
16236|Rocky Creek Conglomerate|43429|14|Not recorded|Map Legend|||Fluvioglacial in N of sheet;in S are "probably fluvial piedmont deposits."||||||
16236|Rocky Creek Conglomerate|43434|4|Described|Map Legend||Carboniferous|||||||
16236|Rocky Creek Conglomerate|43435|14|Not recorded|Map Legend||Carboniferous|||||||
16236|Rocky Creek Conglomerate|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
16236|Rocky Creek Conglomerate|43446|14|Not recorded|p6028,6029,6044,6049||Late Carboniferous|||||||
16236|Rocky Creek Conglomerate|43479|14|Not recorded|p159,177||Westphalian|||||||
16236|Rocky Creek Conglomerate|43582|6|Mentioned|p17|||||||||
16236|Rocky Creek Conglomerate|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
16236|Rocky Creek Conglomerate|45097|6|Mentioned|Fig.|||Correlation chart||||||
16236|Rocky Creek Conglomerate|47056|6|Mentioned|Fig.2 P523|||||||||
16236|Rocky Creek Conglomerate|48600|14|Not recorded|p3|||||||||
16236|Rocky Creek Conglomerate|50132|6|Mentioned|p246||Late Carboniferous|||||||
16236|Rocky Creek Conglomerate|50613|5|Briefly described|p206 Fig. 2|Namurian|Namurian|Of the Currangandi Group.  Geological Province: New England Orogen.  See also p226 Appendix 1.||||||24-FEB-05
16236|Rocky Creek Conglomerate|50629|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|Includes: Plagyan Rhyodacite Tuff Member.  Geological Province: New England Orogen.||||||
16236|Rocky Creek Conglomerate|60299|6|Mentioned|p212 Fig.2c|||Geological Province: Rocky Creek Block. See also "Rocky Creek Conglomerate" and "Rocky Creek conglomerate"||||||18-MAY-05
16236|Rocky Creek Conglomerate|61214|5|Briefly described|p170, p172 Fig. 2|Westphalian|Namurian|Contains several members. Geological Province: Boomi, Kathrose and Darthula Blocks.||||||
16236|Rocky Creek Conglomerate|61767|4|Described|p71|Westphalian|Westphalian|Mainly cobble conglomerate, minor sandstone, glacio-lacustrine varvoid rocks and tillite interrupted by dacitic to rhyolitic pyroclastic deposits. Geological Province: Tamworth Belt.||||||
16236|Rocky Creek Conglomerate|62095|6|Mentioned|p267|||In the Rocky Creek Block/Tamworth Belt.||||||29-MAY-06
16236|Rocky Creek Conglomerate|63832|5|Briefly described|p131 Fig.2, p134-135|Bashkirian|Bashkirian|Rocky Creek Syncline, Southern New England Fold Belt. Proximal proglacial strata of third (C3) glaciation.|||||Alluvial conglomerate with rare thin intervals of rhythmically laminated mudrocks, and an interval of interbedded conglomerate, diamictite and rhythmite with outsized (striated and faceted) gravel at top.|13-DEC-17
16236|Rocky Creek Conglomerate|64631|5|Briefly described|p48.|Bashkirian|Bashkirian|Rocky Creek Syncline, southern New England Fold Belt. Contains an interval of proximal proglacial strata. See also p44. Some biostratigraphic age control.||||Lark Hill Formation overlies, Clifden Formation underlies.||
16236|Rocky Creek Conglomerate|65107|6|Mentioned|Fig 4, p279|Late Palezoic|Late Palezoic|Rocky Creek Block. This unit helped constrain the Late Paleozoic pole path for the New England orogen.||||||
16236|Rocky Creek Conglomerate|67562|6|Mentioned|p102|||Apparently a misnaming of the Rocky Tank Conglomerate Member.||||Conformably overlain by the Ramparts Creek Sandstone Member.||23-JAN-17
16236|Rocky Creek Conglomerate|68003|5|Briefly described|p32 Fig.3-h, pp136-137. |Namurian|Namurian|Tamworth Belt (North), New England Fold Belt.|||Includes Plagyan Rhyodacitic Tuff Member.|Overlies Clifden Formation and, locally, Peri Tuff. Is overlain by Lark Hill Formation.|Coarse boulder, cobble and pebble fluvial orthoconglomerate and paraconglomerate; minor feldsarenite and litharenite and intermediate ash flow, and glaciolacustrine tillite; unwelded ignimbrites and agglomerates, welded rhyolitic ignimbrites.|
16236|Rocky Creek Conglomerate|68004|6|Mentioned|p134.|||Potential for zeolite resources and levels of certainty are discussed.||||||
16236|Rocky Creek Conglomerate|68005|5|Briefly described|p49, p57-p58 Photo.3-R, pp143-144, p170.|Westphalian|Westphalian|Rocky Creek Block, Tamworth Belt. With Lark Hill Formation, represents a period of glacial retreat. Shown [wrongly] on p.143 as including the Penryn Rhyolite.||||Overlies Clifden Formation and Peri Tuff. Is overlain by Lark Hill Formation.|Coarse boulder, cobble and pebble fluvial orthoconglomerate and paraconglomerate, minor feldsarenite and litharenite and intermediate ash flow, and glaciolacustrine tillite.|
16236|Rocky Creek Conglomerate|68295|6|Mentioned|p28-29 Fig. 2.2|||Upper Carboniferous, Irving (1966).||||||
16236|Rocky Creek Conglomerate|69793|6|Mentioned|p1121 Fig.12|Bashkirian|Bashkirian|Rocky Creek Block, Tamworth Belt.||||||
16236|Rocky Creek Conglomerate|70728|5|Briefly described|p265,271-273|Bashkarian|Serpukhovian|Geological province: North Tamworth terrane, New England Orogen. Contains SHRIMP zircon age of 319+\-2.7 Ma at the bottom of the unit (Roberts et al., 2003; Roberts et al., 2006; Roberts and James, 2010). Also contains LA-ICP-MS detrital zircon age of 319+\-2.9 Ma (this study).||||Overlain by Lark Hill Formation. Underlain by Clifden Formation.||
16236|Rocky Creek Conglomerate|71628|6|Mentioned|p10-8|||Southern New England Orogen.||||||
16243|Rocky Hill Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16243|Rocky Hill Granite|40498|6|Mentioned|p392|||||||||
16243|Rocky Hill Granite|42726|5|Briefly described|map legend|Silurian||||||||
16249|Roden Quartz Syenite|39214|5|Briefly described|p21|||||||||
16249|Roden Quartz Syenite|39331|6|Mentioned|Fig.8-2|||||||||
16267|Rolling Downs Group|730|6|Mentioned|p24, p25.|||Marine.||||||11-NOV-14
16267|Rolling Downs Group|9250|5|Briefly described|Map legend|Cretaceous|Cretaceous|Sandstone, siltstone and claystone., porcellaneous in part.||||||
16267|Rolling Downs Group|12575|5|Briefly described|p781. |Albian|Albian|Uppermost unit in Laura Basin. Vitrinite reflectance data are detailed.|124-97 Ma.||Includes Wollena Claystone.||Glauconitic open marine shale.|
16267|Rolling Downs Group|13516|5|Briefly described|p167 fig 10, p169 fig 11|Late Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.|||Includes Wilgunya Subgroup, Manuka Subgroup|||14-NOV-12
16267|Rolling Downs Group|22757|5|Briefly described|p7|||Also Table6, p11. Surat Basin.||||||28-NOV-06
16267|Rolling Downs Group|22780|5|Briefly described|map|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|22781|4|Described|p41|Early Cretaceous|Early Cretaceous|In the Carpentaria Basin.||||||02-APR-07
16267|Rolling Downs Group|22857|5|Briefly described|p294, p544 App.1 Tb.A1.12|Cenomanian|Aptian|Includes the Wallumbilla Formation, Surat Siltstone, Griman Creek Formation, and Winton Formation. Geological Province: Surat and Eromanga Basins. See also p296-7 Tb.22.1, p315 Fig. 22.8, p552 App.1 Tb.A1.13.||||||
16267|Rolling Downs Group|22865|4|Described|p294,Table22.1p296-7|Cenomanian|Aptian|||||||
16267|Rolling Downs Group|23053|4|Described|p8,11,28,30-1|Albian|Aptian|||||||
16267|Rolling Downs Group|23056|6|Mentioned|6|||Geological province: Eromanga Basin.||||||28-NOV-06
16267|Rolling Downs Group|23065|5|Briefly described|18|||Geological province: Carpentaria Basin.||||||28-NOV-06
16267|Rolling Downs Group|23183|6|Mentioned|p217||Aptian|||||||
16267|Rolling Downs Group|23220|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|23224|5|Briefly described|p3|||Of McMinn 1981. Hosts the Wallumbilla Formation. Great Australian Basin.||||||07-MAR-06
16267|Rolling Downs Group|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: Early Cretaceous. Conformably overlies Coffin Hill Member. Thickness: <10m. Geological Province: Georgetown Region.||||||26-NOV-08
16267|Rolling Downs Group|23336|5|Briefly described|p5|Cretaceous|Cretaceous|Overlies Mulga Downs Group.||||||28-NOV-06
16267|Rolling Downs Group|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23420|6|Mentioned|p 131|||||||||
16267|Rolling Downs Group|23423|5|Briefly described|p267||Cretaceous|||||||
16267|Rolling Downs Group|23425|3|Fully described|p394 Table 9.7.|||Also see p378. Geological Province Carpentaria Basin.||||||03-APR-12
16267|Rolling Downs Group|23426|3|Fully described|p403 + Table 10.4 p407|Albian|Aptian|Formerly Battle Camp Shale and Wolena Claystone. Conformably underlain by Gilbert River Formation. Geological province: Laura Basin Province.||||||26-APR-07
16267|Rolling Downs Group|23427|5|Briefly described|Table 11.2 p418.|||||||||
16267|Rolling Downs Group|23428|5|Briefly described|p422|||||||||
16267|Rolling Downs Group|23430|5|Briefly described|p522|||Formerly Battle Camp Shale and Wolena Claystone. Basal shale is marine, variably calcareous and galuconitic, with minor siltstone and conglom. beds; overlain by marine silty/sandy claystone with calc.concretions. Geol. Prov: Laura Basin.||||||30-NOV-06
16267|Rolling Downs Group|23431|5|Briefly described|p544|||||||||
16267|Rolling Downs Group|23496|6|Mentioned|p59|||||||||
16267|Rolling Downs Group|23510|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|23511|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23512|5|Briefly described|Map Legend|Cretaceous|Middle Jurassic|||||||
16267|Rolling Downs Group|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|23833|5|Briefly described|p256 Table 1|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|23879|6|Mentioned|p18|||||||||
16267|Rolling Downs Group|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Geological Province: Great Australian Superbasin.||||||
16267|Rolling Downs Group|23911|5|Briefly described|p97 Fig. 11|Albian|Aptian|Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|23982|5|Briefly described|p2|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin. See also page 35 Fig.7.||||||
16267|Rolling Downs Group|24047|5|Briefly described|p11-12|||Geological Province: Western Gulf Sub-basin.||||||
16267|Rolling Downs Group|24048|6|Mentioned|p76|||Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24070|5|Briefly described|p303|Cretaceous|Cretaceous|Geological Province: Coonamble Embayment.||||||
16267|Rolling Downs Group|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Carpentaria Basin.||||||
16267|Rolling Downs Group|24089|5|Briefly described|Student Activites|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|24393|5|Briefly described|p152 Tb. 1|Mesozoic|Mesozoic|Shallow marine deposits <50m. thick.||||||
16267|Rolling Downs Group|29591|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|29961|6|Mentioned|p12|||||||||
16267|Rolling Downs Group|29991|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30019|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|30021|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30102|5|Briefly described|p34|||Cretaceous age. See also p17.||||||28-NOV-06
16267|Rolling Downs Group|30103|5|Briefly described|p9|||Lower Cretaceous age. Table 3 on p9. See also Fig.2.||||||28-NOV-06
16267|Rolling Downs Group|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30133|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30510|6|Mentioned|p103|||||||||
16267|Rolling Downs Group|30582|6|Mentioned|p4|||||||||
16267|Rolling Downs Group|30584|4|Described|Table 1|||||||||
16267|Rolling Downs Group|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30691|4|Described|p6|||See also p15-17,20,Table 4,Fig.2. Lower Cretaceous age.||||||28-NOV-06
16267|Rolling Downs Group|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30696|6|Mentioned|p16|||||||||
16267|Rolling Downs Group|30697|6|Mentioned|p34|||Minor aquifer present.||||||28-NOV-06
16267|Rolling Downs Group|30699|6|Mentioned|p53|||Stratigraphy. Early Cretaceous||||||
16267|Rolling Downs Group|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30702|4|Described|p48|||See also p51,52,Fig.1. Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|30853|5|Briefly described|Table 3|||Cretaceous||||||
16267|Rolling Downs Group|30854|4|Described|Table 4|||Lower to Upper Cretaceous age||||||
16267|Rolling Downs Group|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30856|4|Described|Table 3|||Lower Cretaceous age||||||
16267|Rolling Downs Group|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|30905|6|Mentioned|p147|||||||||
16267|Rolling Downs Group|30910|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31098|5|Briefly described|Table 1|||||||||
16267|Rolling Downs Group|31109|6|Mentioned|p40|||See also P42, 44, 46, 50, 52, 54, 56, 58 & Map 62.||||||
16267|Rolling Downs Group|31110|5|Briefly described|p6|||See also p8-26. Terrain classification.||||||28-NOV-06
16267|Rolling Downs Group|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
16267|Rolling Downs Group|31164|6|Mentioned|p8|||Lower Cretaceous||||||
16267|Rolling Downs Group|31165|5|Briefly described|Table.1.|||||||||
16267|Rolling Downs Group|31166|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31376|5|Briefly described|p4|||Mention p2.||||||28-NOV-06
16267|Rolling Downs Group|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes the Wallumbilla Formation, Toolebuc Limestone and Allaru Mudstone.||||||02-DEC-04
16267|Rolling Downs Group|31425|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|31430|4|Described|Table 1|||||||||
16267|Rolling Downs Group|31431|5|Briefly described|Table 3|||L.U.Cretaceous||||||
16267|Rolling Downs Group|31432|4|Described|Table 1|||L.Cretaceous||||||
16267|Rolling Downs Group|31433|5|Briefly described|p7|||Lower Cretaceous||||||
16267|Rolling Downs Group|31434|4|Described|Table 1|||Lower Cretaceous. See also p8.||||||28-NOV-06
16267|Rolling Downs Group|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous||||||
16267|Rolling Downs Group|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32274|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32275|4|Described|p8|||||||||
16267|Rolling Downs Group|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32277|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16267|Rolling Downs Group|32314|6|Mentioned|Fig.4|||||||||
16267|Rolling Downs Group|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32395|6|Mentioned|p6|||Stratigraphic table.||||||28-NOV-06
16267|Rolling Downs Group|32396|6|Mentioned|p8|||L.Cretaceous||||||
16267|Rolling Downs Group|32413|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|32563|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|32705|6|Mentioned|p183|||See also Fig.2||||||
16267|Rolling Downs Group|32706|4|Described|Table 1|||Mention p8.||||||28-NOV-06
16267|Rolling Downs Group|32796|4|Described|p301|||See also p302-303||||||28-NOV-06
16267|Rolling Downs Group|32918|4|Described|p18|||||||||11-JAN-10
16267|Rolling Downs Group|33011|6|Mentioned|p214|||||||||
16267|Rolling Downs Group|33016|6|Mentioned|p1|||||||||
16267|Rolling Downs Group|33017|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Includes Winton, Mackunda and Wallumbilla Formations and Allaru Mudstone and Toolebuc Limestone.||||||07-JUL-04
16267|Rolling Downs Group|33068|6|Mentioned|p476|||Cret.||||||
16267|Rolling Downs Group|33069|4|Described|p7|||L.-U.Cret.||||||
16267|Rolling Downs Group|33070|4|Described|Table 2|||L.Cret.||||||
16267|Rolling Downs Group|33072|4|Described|Table 1|||L.Cret.||||||
16267|Rolling Downs Group|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33075|6|Mentioned|p452|||||||||
16267|Rolling Downs Group|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
16267|Rolling Downs Group|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33087|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33088|4|Described|Table 3|||L.Cret.||||||
16267|Rolling Downs Group|33089|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33090|4|Described|Table 4|||L.Cret.||||||
16267|Rolling Downs Group|33091|6|Mentioned|p9|||Strat.||||||
16267|Rolling Downs Group|33092|6|Mentioned|p8|||Strat. table||||||
16267|Rolling Downs Group|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33150|4|Described|p8|||L.Cret.||||||
16267|Rolling Downs Group|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33176|6|Mentioned|p175|||||||||
16267|Rolling Downs Group|33177|5|Briefly described|Table 1|||||||||15-JUL-04
16267|Rolling Downs Group|33178|5|Briefly described|p11|||||||||
16267|Rolling Downs Group|33181|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33182|6|Mentioned|p193|||||||||
16267|Rolling Downs Group|33184|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33185|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33226|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33372|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
16267|Rolling Downs Group|33449|4|Described|Table 1|||L.-U.Cret.||||||
16267|Rolling Downs Group|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33529|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33561|6|Mentioned|p102|||||||||
16267|Rolling Downs Group|33638|5|Briefly described|Table 1|||See also p10.||||||28-NOV-06
16267|Rolling Downs Group|33639|5|Briefly described|p11|||L.Cret.||||||
16267|Rolling Downs Group|33640|4|Described|Table 2|||L.-U.Cret.||||||
16267|Rolling Downs Group|33642|6|Mentioned|p144,147,148|||Refers Vine & Day.(1965). Ref. to Whitehouse 1954. Subgroups. Ref to Jack 1886.||||||
16267|Rolling Downs Group|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|33646|5|Briefly described|p8|||Strat. table.||||||
16267|Rolling Downs Group|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
16267|Rolling Downs Group|33648|6|Mentioned|p19|||||||||
16267|Rolling Downs Group|33676|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|33709|6|Mentioned|p110|||Cretaceous.||||||
16267|Rolling Downs Group|33772|4|Described|p13|||||||||
16267|Rolling Downs Group|33773|4|Described|Table 1|||||||||
16267|Rolling Downs Group|33825|6|Mentioned|p10|||Correlation table||||||
16267|Rolling Downs Group|33832|5|Briefly described|p11|||Strat. and correlation.||||||28-NOV-06
16267|Rolling Downs Group|33882|4|Described|Table 1|||Mention p7,8.||||||28-NOV-06
16267|Rolling Downs Group|33883|6|Mentioned|p17|||||||||
16267|Rolling Downs Group|33884|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34065|4|Described|p6|||L.Cret.||||||
16267|Rolling Downs Group|34091|5|Briefly described|Table 1|||Cret. See also pp4,8.||||||28-NOV-06
16267|Rolling Downs Group|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
16267|Rolling Downs Group|34218|5|Briefly described|Table 1|||Lower Cretaceous.||||||28-NOV-06
16267|Rolling Downs Group|34254|6|Mentioned|p481|||||||||
16267|Rolling Downs Group|34282|6|Mentioned|p96|||Cret.||||||
16267|Rolling Downs Group|34287|6|Mentioned|p186|||Cret.||||||
16267|Rolling Downs Group|34469|6|Mentioned|p107|||Cretaceous. See also pp117,118.||||||28-NOV-06
16267|Rolling Downs Group|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|34550|5|Briefly described|Table 2.1|||Cretaceous||||||
16267|Rolling Downs Group|34811|4|Described|Table 1|||||||||
16267|Rolling Downs Group|34931|5|Briefly described|p320|||||||||
16267|Rolling Downs Group|35187|6|Mentioned|p53|||||||||
16267|Rolling Downs Group|35204|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35220|4|Described|p16|||||||||
16267|Rolling Downs Group|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35559|4|Described|Table 1|||||||||
16267|Rolling Downs Group|35560|6|Mentioned|p289|||||||||
16267|Rolling Downs Group|35601|6|Mentioned|p144|||Geothermal gradients correlate with contours of base of R.D.Group||||||
16267|Rolling Downs Group|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|35663|6|Mentioned|Table 1|||Biostratigraphy.||||||
16267|Rolling Downs Group|35793|6|Mentioned|p241|||Weathered profiles.||||||
16267|Rolling Downs Group|35811|5|Briefly described|Table 3|||||||||
16267|Rolling Downs Group|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
16267|Rolling Downs Group|36012|3|Fully described|Table 5|||||||||
16267|Rolling Downs Group|36056|6|Mentioned|p11|||||||||
16267|Rolling Downs Group|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|36473|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|36570|6|Mentioned|p46|||||||||
16267|Rolling Downs Group|36571|6|Mentioned|Table 4|||||||||
16267|Rolling Downs Group|36751|6|Mentioned|p488|||||||||
16267|Rolling Downs Group|36910|6|Mentioned|p61|||||||||
16267|Rolling Downs Group|36914|6|Mentioned|p87|||||||||
16267|Rolling Downs Group|36961|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|37116|6|Mentioned|p310|||||||||
16267|Rolling Downs Group|37608|3|Fully described|Table 1|||See also Table 2||||||
16267|Rolling Downs Group|37995|4|Described|Table 1|||||||||
16267|Rolling Downs Group|38064|5|Briefly described|p42|||Contain opal deposits of White Cliffs and Lightning Ridge.||||||
16267|Rolling Downs Group|38226|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|38374|6|Mentioned|p602|||||||||
16267|Rolling Downs Group|39211|6|Mentioned|p5|||Fig. 3,7,9,22,26 etc. Correlation||||||
16267|Rolling Downs Group|39315|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39445|5|Briefly described|Table 11|||||||||
16267|Rolling Downs Group|39478|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|39494|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39627|6|Mentioned|p269|||||||||
16267|Rolling Downs Group|39666|6|Mentioned|p110|||||||||
16267|Rolling Downs Group|39708|6|Mentioned|p478|||||||||
16267|Rolling Downs Group|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|39942|6|Mentioned|p468|||||||||
16267|Rolling Downs Group|40030|6|Mentioned|Fig.5|||||||||
16267|Rolling Downs Group|40199|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|40544|6|Mentioned|Fig.6|||||||||
16267|Rolling Downs Group|40584|6|Mentioned|p434|||||||||
16267|Rolling Downs Group|40595|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|40623|5|Briefly described|p88|||||||||
16267|Rolling Downs Group|40648|3|Fully described|p12|||||||||
16267|Rolling Downs Group|40766|5|Briefly described|p25|||||||||
16267|Rolling Downs Group|40801|6|Mentioned|p79|||||||||
16267|Rolling Downs Group|40926|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|41012|6|Mentioned|p137|||||||||
16267|Rolling Downs Group|41022|6|Mentioned|p279|||||||||
16267|Rolling Downs Group|41061|6|Mentioned|p19|||See also Fig.6. Generalized stratigraphy.||||||28-NOV-06
16267|Rolling Downs Group|41064|6|Mentioned|p55|||||||||
16267|Rolling Downs Group|41086|3|Fully described|p98|||See also Fig.3||||||
16267|Rolling Downs Group|41087|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41088|6|Mentioned|p143|||||||||
16267|Rolling Downs Group|41097|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|41117|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41177|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41188|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41210|5|Briefly described|Fig.3|||||||||
16267|Rolling Downs Group|41247|6|Mentioned|Fig.7|||||||||
16267|Rolling Downs Group|41266|6|Mentioned|Fig.3|||||||||
16267|Rolling Downs Group|41307|4|Described|p17|||||||||
16267|Rolling Downs Group|41568|4|Described|p15|||||||||
16267|Rolling Downs Group|41642|6|Mentioned|p217|||||||||
16267|Rolling Downs Group|41681|6|Mentioned|p2|||||||||
16267|Rolling Downs Group|41725|6|Mentioned|Fig.2|||||||||
16267|Rolling Downs Group|41992|4|Described|Fig.2 P183|||See also p186.||||||28-NOV-06
16267|Rolling Downs Group|42007|6|Mentioned|Fig.2 P182|||||||||
16267|Rolling Downs Group|42061|5|Briefly described|Fig.4 P151|||||||||
16267|Rolling Downs Group|42121|6|Mentioned|Fig.1 P97|||||||||
16267|Rolling Downs Group|42346|4|Described|p81, Fig.4 p82|Early Cretaceous||||||||
16267|Rolling Downs Group|42364|5|Briefly described|Fig. 1 P196|||||||||
16267|Rolling Downs Group|42460|5|Briefly described|Fig.1 P206|||||||||
16267|Rolling Downs Group|42464|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|42467|5|Briefly described|Map Legend|||||||||
16267|Rolling Downs Group|42596|5|Briefly described|Fig. 1 P24|||||||||
16267|Rolling Downs Group|42637|5|Briefly described|p10, 23|||||||||
16267|Rolling Downs Group|42650|4|Described|p16|||Conformably overlies/overlaps the Gilbert River Formation.||||||28-NOV-06
16267|Rolling Downs Group|42653|5|Briefly described|p318|||Terrain pattern description||||||
16267|Rolling Downs Group|42673|6|Mentioned|p195|||||||||
16267|Rolling Downs Group|43000|5|Briefly described|Fig.5,p112|||||||||
16267|Rolling Downs Group|43085|6|Mentioned|p8|||||||||
16267|Rolling Downs Group|43090|5|Briefly described|Map legend||Cretaceous|||||||
16267|Rolling Downs Group|43276|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43277|5|Briefly described|Map Legend||Early Cretaceous|In the Great Australian Basin.||||||28-NOV-06
16267|Rolling Downs Group|43366|14|Not recorded|Map Legend|||||||||22-DEC-09
16267|Rolling Downs Group|43367|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43368|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43369|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43371|14|Not recorded|Map Legend|||||||||11-JAN-10
16267|Rolling Downs Group|43383|14|Not recorded|p26-28, diag||Cretaceous|||||||
16267|Rolling Downs Group|43384|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43386|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43390|14|Not recorded|p15,16,27-34|||Divided into Winton,Tambo,Roma Formations||||||
16267|Rolling Downs Group|43402|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43403|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43404|14|Not recorded|p11-15,20,23-33||Cretaceous|Table p9,Table p11||||||
16267|Rolling Downs Group|43405|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43410|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43411|14|Not recorded|Map Legend|||||||||
16267|Rolling Downs Group|43436|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition)||||||
16267|Rolling Downs Group|43452|5|Briefly described|Map Legend||Cretaceous|Includes: Roma Formation, Tambo Formation, Winton Formation.||||||14-FEB-05
16267|Rolling Downs Group|43454|14|Not recorded|Map Legend||Cretaceous|||||||
16267|Rolling Downs Group|43459|14|Not recorded|p315-6|||||||||
16267|Rolling Downs Group|43487|5|Briefly described|20|||||||||
16267|Rolling Downs Group|43501|14|Not recorded|Map Legend||Cretaceous|(Provisional Edition) Inc. Yalpunga Beds, Oornoo Beds, Wittabrenna Beds||||||
16267|Rolling Downs Group|43542|14|Not recorded|Map Legend||Cretaceous|lithology||||||
16267|Rolling Downs Group|43596|4|Described|p40, p39 Tb. 4|Albian|Aptian|Max. thickness: 600m. Largely comprises mudstone, with beds and lenses of glauconitic, labile, white to buff quartzose fine sandstone; fossiliferous and with  concretionary limestone at base; shallow marine deposits.||||||15-JAN-09
16267|Rolling Downs Group|43602|5|Briefly described|Fig3 p194|||In Surat Basin/Eromanga Basin||||||
16267|Rolling Downs Group|43625|6|Mentioned|p47|||||||||
16267|Rolling Downs Group|43630|6|Mentioned|p69|||||||||
16267|Rolling Downs Group|43714|6|Mentioned|p8||Early Cretaceous|||||||
16267|Rolling Downs Group|43730|5|Briefly described|p24,29|||||||||
16267|Rolling Downs Group|43738|6|Mentioned|p5|||||||||
16267|Rolling Downs Group|43810|6|Mentioned|Fig.4,p209,210||Cretaceous|||||||
16267|Rolling Downs Group|43820|5|Briefly described|Map Legend||Early Cretaceous|||||||
16267|Rolling Downs Group|43881|14|Not recorded|p79,80|Cretaceous|Late Jurassic|See also Lexicon.||||||
16267|Rolling Downs Group|43995|14|Not recorded|Tb.p9,20 Fig.9||Cretaceous|Inc. Roma Formation, Tambo Formation and Winton Formation in the Eromanga Sub-Basin.||||||
16267|Rolling Downs Group|44020|14|Not recorded|p10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44033|14|Not recorded|Tb.1,opp.p4|||||||||
16267|Rolling Downs Group|44034|6|Mentioned|Tb.1,p2|||||||||
16267|Rolling Downs Group|44041|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|44087|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44089|14|Not recorded|Tb.1||Early Cretaceous|||||||
16267|Rolling Downs Group|44091|14|Not recorded|p60||Cretaceous|||||||
16267|Rolling Downs Group|44093|6|Mentioned|p68 (photo)|||Associated with Gum Vale beds.||||||
16267|Rolling Downs Group|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
16267|Rolling Downs Group|44112|6|Mentioned|p82|||||||||
16267|Rolling Downs Group|44121|14|Not recorded|p8|||||||||
16267|Rolling Downs Group|44122|14|Not recorded|p322|||||||||
16267|Rolling Downs Group|44207|14|Not recorded|p116|||||||||
16267|Rolling Downs Group|44269|14|Not recorded|p16||Cretaceous|||||||
16267|Rolling Downs Group|44291|14|Not recorded|p5|||||||||
16267|Rolling Downs Group|44346|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44375|14|Not recorded|p313|||||||||
16267|Rolling Downs Group|44406|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44408|14|Not recorded|p4|||||||||
16267|Rolling Downs Group|44415|14|Not recorded|p22,Fig.2,p23|||||||||
16267|Rolling Downs Group|44417|2|Defined|p417-421|Albian|Aptian|Contains: Winton, Mackunda and Wilgunya Formations. Overlies Gilbert River Formation. Probably Cenomanian.||||||
16267|Rolling Downs Group|44739|14|Not recorded|p19|||||||||
16267|Rolling Downs Group|44740|14|Not recorded|p29,39-42,47,48,52,|||p55,56,77||||||
16267|Rolling Downs Group|44744|14|Not recorded|p106-113|||||||||
16267|Rolling Downs Group|44800|14|Not recorded|p16,22,map||Cretaceous|||||||
16267|Rolling Downs Group|44819|14|Not recorded|p89|Albian|Aptian|Shaley basal formation is Roma Formation.||||||
16267|Rolling Downs Group|44836|14|Not recorded|p5,11,Figs.1-5||Cretaceous|||||||
16267|Rolling Downs Group|44852|14|Not recorded|p78||Early Cretaceous|||||||
16267|Rolling Downs Group|44989|14|Not recorded|p.125,126|||(E54-14).||||||
16267|Rolling Downs Group|45004|14|Not recorded|p.8|||Tb.1.||||||
16267|Rolling Downs Group|45011|14|Not recorded|p18,20|||Whitehouse correlated sediments in Polland Shale with Rolling Downs Group.||||||
16267|Rolling Downs Group|45110|6|Mentioned|p6|||||||||
16267|Rolling Downs Group|45145|3|Fully described|Table 5|||See also p23.||||||31-OCT-06
16267|Rolling Downs Group|46791|4|Described|p44|||Refers Galloway (1967)||||||
16267|Rolling Downs Group|46802|6|Mentioned|p131|||||||||
16267|Rolling Downs Group|46812|5|Briefly described|p241|||||||||
16267|Rolling Downs Group|46854|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|46872|6|Mentioned|p108|||||||||
16267|Rolling Downs Group|46881|6|Mentioned|Table 2|||||||||
16267|Rolling Downs Group|46911|6|Mentioned|Fig.1|||Geological map and distribution of weathered profiles.||||||
16267|Rolling Downs Group|46937|6|Mentioned|Fig.10|||||||||
16267|Rolling Downs Group|46939|6|Mentioned|Fig.1|||||||||
16267|Rolling Downs Group|47042|6|Mentioned|p171|||||||||
16267|Rolling Downs Group|47083|5|Briefly described|p20||Mesozoic|Carpentaria Basin.||||||
16267|Rolling Downs Group|48908|14|Not recorded|Tb.1||Cretaceous|||||||
16267|Rolling Downs Group|48920|3|Fully described|p56|||Cretaceous||||||
16267|Rolling Downs Group|48951|6|Mentioned|Table 1|||||||||
16267|Rolling Downs Group|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Comprises Wallumbilla and Toolebuc Formations, Allaru Mudstone and Mackunda Formation.  Overlies the Gilbert River Formation.  Geological Province:  Eromanga Basin.||||||
16267|Rolling Downs Group|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Includes Allaru Mudstone, Toolebuc Limestone, and Wallumbilla Formation.||||||
16267|Rolling Downs Group|61312|5|Briefly described|p66, p73|Albian|Aptian|Supersedes "Rolling Downs Formation". Comprises Wallumbilla and Toolebuc Formations, and Allaru Mudstone and Winton Formation. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Includes the Griman Creek Formation, Surat Siltstone and Wallumbilla Formation. Green silty mudstone, minor sandstone. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
16267|Rolling Downs Group|61823|5|Briefly described|p118|||Part of a marine transgressive sequence; overlies Gum Vale and Cadna-Owie Formations. Geological Province: Eromanga Basin.||||||
16267|Rolling Downs Group|62837|5|Briefly described|Stratigraphic columns|Late Cretaceous|Early Cretaceous|Includes Wallumbilla Formation, Allaru Mudstone and Normanton Formation.  Age: ~114-91Ma. Geological Province: Northern Gulf of Carpentaria, Southern Cape York and Burketown Depression.||||||01-MAR-10
16267|Rolling Downs Group|63450|5|Briefly described|p83|Cretaceous|Jurassic|Overlies Hooray Sandstone/Cadna-owie Formation. Marine deposits.||||||07-FEB-11
16267|Rolling Downs Group|63789|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Subaerial scree and slope debris deopsits on fossil hill slopes and valley walls containing dislodged angular blocks of underlying bedrock. Commonly with pebbly sand infill and silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63790|5|Briefly described|Map Legend|Cretaceous|Late Jurassic|Includes Hooray Sandstone. Beach pebble, cobble and boulder deposits formed from white quartzose sandstone. Commonly with silcrete cement.||||||08-DEC-08
16267|Rolling Downs Group|63793|6|Mentioned|p10.|Cretaceous|Jurassic|Eromanga Basin.||||||
16267|Rolling Downs Group|63979|6|Mentioned|p51-52|||Includes the Wilgunyah Subgroup.||||||07-FEB-11
16267|Rolling Downs Group|64061|6|Mentioned|p66|Cretaceous|Cretaceous|Contains the Griman Creek Formation. Geological Province: Surat Basin.||||||24-APR-08
16267|Rolling Downs Group|64570|5|Briefly described|p858|Early Cretaceous|Early Cretaceous|Volcanogenic sedimentary rocks and are rich in volcanic lithics.||||||22-DEC-08
16267|Rolling Downs Group|64665|5|Briefly described|p53 Fig.2, p62.|Early Cretaceous|Early Cretaceous|Laura Basin.||||Overlies Gilbert River Formation.|Dominantly marine shales and siltstones.|
16267|Rolling Downs Group|64679|5|Briefly described|Map legend|Cretaceous|Cretaceous|Conglomerate (pebbles of rounded white vein quartz and quartzite), quartz sandstone, siltstone and claystone; commonly silicified or ferruginised.||||||27-NOV-08
16267|Rolling Downs Group|64681|5|Briefly described|p2, p3 Fig. 1|Cretaceous|Cretaceous|Geological province: Eromanga Basin. Sandstone, siltstone, claystone.||||||
16267|Rolling Downs Group|64682|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Feldspathic and lithic sandstone, siltstone and mudstone; strongly kaolinised, mottled and ferruginised, locally containes exotic ?drop? boulders.||||||
16267|Rolling Downs Group|64683|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes Hooray Sandstone. Rounded waterworn white vein quartz and quartzite conglomerate, quartzose sandstones, siltstones and claystones deposited on undulating topography in underlying bedrock.||||||
16267|Rolling Downs Group|64820|4|Described|pS9, pS6 Fig. 4|Late Cretaceous|Middle Jurassic|Contains Garroway Sandstone, Gilbert River, Wallumbilla and Toolbeuc Formations, Allaru Mudstone and Normanton Formation. Overlain by Bulimba Formation.||||||
16267|Rolling Downs Group|64821|5|Briefly described|pS18, pS20-21, pS40|Cretaceous|Cretaceous|Discussed in relation to its saprolite zone in the East Weipa and Andoom areas where lenses of weakly lithified sandstone, clay and siltstone dominate. Unconformably overlain by the Bulimba Formation.||||||02-FEB-09
16267|Rolling Downs Group|64822|5|Briefly described|pS88, pS99|||Together with the overlying Bulimba Fm, hosted the development of the Weipa bauxite deposit - composed of a transported blanket of bauxite overlying a lateritic weathering profile. Geol.prov: Weipa Sub-basin, Carpentaria Basin.||||||02-FEB-09
16267|Rolling Downs Group|66529|6|Mentioned|p12 Fig.5|||Eromanga, Carpentaria, Surat Basins and Coonamble Embayment.|||Includes Wallumbilla, Toolebuc, Mackunda, Winton, Griman Creek Formations; Surat Siltstone; and Allaru Mudstone.|||
16267|Rolling Downs Group|66623|3|Fully described|p108, pp238-245, pp256-267.|Late Cretaceous|Early Cretaceous|Widespread throughout Eromanga Basin. Thickness c.600 m. Generally poor outcrops. Has fair hydrocarbon reservoir (no source) potential, and good local seal potential. Porous sandstone units provide groundwater resources.|||Includes Wilgunya Subgroup (in Queensland), Wallumbilla Formation (at base), Allaru Mudstone and Winton Formation (at top).|Overlies Cadna-owie Formation. Is unconformably overlain by Eyre Formation. Unconformably overlies Yancannia Formation.|Alternation of sandstone-poor and sandstone-rich intervals deposited in a marine environment; ice-rafted dropstone boulders in lower units.|07-JUN-13
16267|Rolling Downs Group|66915|5|Briefly described|p4-5, p15-17|||In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||Wallumbilla Formation, Toolebuc Formation|||12-JAN-17
16267|Rolling Downs Group|66917|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66918|5|Briefly described|Map legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz and quartzite; conglomerate; quartzose sandstone; siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|66921|6|Mentioned|Map legend|Cretaceous|Cretaceous||||Includes Cadna-owie Formation.|||
16267|Rolling Downs Group|67105|6|Mentioned|p661|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67208|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Cadna-owie Formation. Is overlain by Cordillo Silcrete.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67210|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||||Overlies Yancannia Formation. Unconformably overlies Warratta Group. Is overlain by Eyre Formation.|Marine white claystones, siltstones and fine-grained quartzose sandstones with bioturbation.|
16267|Rolling Downs Group|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||Includes Wallumbilla Formation and Allaru Mudstone.|Overlies Bunker Creek Formation and Warratta Group.|Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; overall upward-fining sequence with sparse marine fossils and large, rounded, quartzite dropstones.|
16267|Rolling Downs Group|67402|4|Described|p179, p226-p230, p232, p309|Cenomanian|Aptian|Proven hydrocarbon seal in the Eromanga Basin with a combined thickness of up to 1500m; also present in the Laura Basin. Formerly the Battle Camp Shale and the Wolena Claystone.|||Includes the Allaru Mudstone, Toolebuc Formation and the Wallumbilla Formation|Overlies the Gilbert River Formation|Basal shale with minor silty and conglomeratic beds that is overlain by silty or sandy claystone with calcareous concretions.|
16267|Rolling Downs Group|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.|||Includes Wallumbilla Formation.|Underlain by Blythesdale Group.||
16267|Rolling Downs Group|68003|5|Briefly described|p52, p57 Fig.3-n, pp70-71, p127.|Early Cretaceous|Early Cretaceous|Surat Basin. Deposited in a major marine transgression-regression cycle.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|Overlies Bungil Formation and Drildool beds conformably.|Semiconsolidated clays and claystone with minor fine clayey quartz sandstone; coal and calcareous clay and calcarenite occur near the base; rare conglomerate and gravel.|
16267|Rolling Downs Group|68004|6|Mentioned|p131, p205.|Early Cretaceous|Early Cretaceous|Hosts the Lightning Ridge Opal Field. Mineral potential tracts and levels of certainty are discussed.||||||
16267|Rolling Downs Group|68069|5|Briefly described|Map legend, p2.|Cretaceous|Cretaceous|Surat Basin.|||Includes Wallumbilla Formation, Surat Siltstone and Griman Creek Formation.|||
16267|Rolling Downs Group|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Laura, Carpentaria and Eromanga Basins.|||Includes Wallumbilla, Griman Creek, Toolebuc, Normanton, Mackunda and Winton Formations, and Allaru Mudstone.|||
16267|Rolling Downs Group|68593|5|Briefly described|p3-4|Early Cretaceous|Early Cretaceous|See individual units.|||Purlawaugh, Griman Creek Formations; Surat Siltstone.|Overlies Bungil Formation.||
16267|Rolling Downs Group|68734|5|Briefly described|p218 Fig.2|Albian|Barremian|Eromanga Basin (SW and NE) and Surat Basin.|||Includes Winton, Mackunda, Oodnadatta, Toolebuc, Wallumbilla, and Griman Creek Formations; Coorikiana Sandstone; Bulldog Shale; Allaru Mudstone; and Surat Siltstone.|||16-JAN-17
16267|Rolling Downs Group|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Includes both marine and fluvial sedimentary rocks. Thick fluvial to coastal plain sequence.|||Includes Winton Formation, Mackunda Formation, Griman Creek Formation, Allaru Formation, Toolebuc Formation, Surat Siltstone, and Bulldog Shale.||Comprises carbonaceous and pyritic shale, siltstone, and coarse volcaniclastic sandstone with minor coal layers.|
16267|Rolling Downs Group|68901|6|Mentioned|p7 Fig. ii|||Eromanga Basin.|||Includes the Winton and Wallumbilla Formations.|||27-SEP-18
16267|Rolling Downs Group|69001|6|Mentioned|p2 Fig.1B, p30|Cretaceous|Cretaceous||||Includes the Doncaster Member.|||
16267|Rolling Downs Group|69297|6|Mentioned|p274 fig 4.3|Cenomanian|Early Cretaceous||||Includes the Wallumbilla Formation, Allaru Mudstone, Toolebuc Formation and the Normanton Formation.|||
16267|Rolling Downs Group|69455|6|Mentioned|p39:2, 39:4 Fig.39.3|Cretaceous|Cretaceous|Central Carpentaria Basin.||||||12-JUL-16
16267|Rolling Downs Group|69457|5|Briefly described|p41:2, 6, 8, 12|||Whitehouse (1955). Applies to the succession in SW Eromanga Basin, from the top of the (ungrouped) Cadna-owie Formation to the top of the Winton Formation. Up to c.1700m thick.|||Wilgunya, Manuka, Marree Subgroups.|Overlies Cadna-owie Formation.||12-JUL-16
16267|Rolling Downs Group|69555|6|Mentioned|p46||||||Includes Winton Formation|||
16267|Rolling Downs Group|69591|6|Mentioned|p29|Cretaceous|Jurassic|||||||
16267|Rolling Downs Group|69594|4|Described|p521-522, p540, p573-574|Late Cretaceous|Aptian|Carpentaria, Laura Basins. Source of lateritic bauxite (at Weipa) and kaolin, formed by deep weathering during the Late Cretaceous regression. The Group acts as the confining beds for the main aquifers in the Basin. Not subdivided in the Laura Basin, where it is up to 212m thick and is equivalent to the Wallumbilla Formation in the Eromanga Basin. Coeval with Allaru Mudstone. Youngest deposit in the Laura Basin.|||Wallumbilla, Toolebuc Formations; Allaru Mudstone; Normanton Formation.|Conformably overlies Gilbert River Formation. Is equivalent to upper Battle Camp Formation, Wolena Claystone.|Undivided: basal marine unit of calcareous and glauconitic shales with minor siltstone and conglomerate, overlain by silty and sandy marine claystones with carbonate concretions.|
16267|Rolling Downs Group|69599|5|Briefly described|p601-602|Cretaceous|Cretaceous|Lateritisation of this unit produced the world's largest bauxite deposit at Weipa.|||Normanton Formation.|||
16267|Rolling Downs Group|69673|6|Mentioned|p156||||||Includes Wilgunya Subgroup, Manuka Subgroup|||
16267|Rolling Downs Group|69682|5|Briefly described|p93 Fig.1|Cretaceous|Cretaceous|Eromanga and Surat Basins.||||||
16267|Rolling Downs Group|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.|||Includes Winton and Wallumbilla Formations.|||
16267|Rolling Downs Group|69961|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Includes Namur Sandstone?||Rounded, waterworn white vein quartz, quartzite, conglomerate, quartzose sandstones, siltstones and claystones; sparse marine fossils; large quartzite dropstones. Bioturbated marine white claystones, siltstones and fine-grained quartzose sandstones.|16-SEP-15
16267|Rolling Downs Group|70036|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Surat Basin. Included in a mapped unit of a marine sequence of semi-consolidated clay and claystone, minor fine quartz sandstone, coal and calcareous clay.||||||
16267|Rolling Downs Group|70207|6|Mentioned|p74|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous||||Wilgunya Subgroup.|||
16267|Rolling Downs Group|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous||||Wallumbilla, Toolebuc Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous||||Includes Wilgunya Subgroup.|||
16267|Rolling Downs Group|70648|5|Briefly described|Map Legend|Cretaceous|Cretaceous|2 un-named units: Marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation. Silicified variant.|||Includes 2 un-named units.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||Includes Winton Formation, Allaru Mudstone, Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70650|5|Briefly described|Map Legend|Cretaceous|Cretaceous||||||Rounded, waterworn, white vein quartz quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70651|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Includes unnamed sub-unit of marine white claystone, siltstone and fine-grained quartzose sandstone with bioturbation.|||Includes unnamed unit.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, siltstone and claystone; overall upward fining sequence with sparse marine fossils and large rounded quartzite dropstones.|
16267|Rolling Downs Group|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Rounded quartz-rich gravel sourced from Namur Sandstone. Residual lag regolith and unconsolidated sediments also described.|||Includes Wallumbilla Formation.||Rounded, waterworn, white vein quartz, quartzite, conglomerate, quartzose sandstone, calcareous sandstone, siltstone and claystone; overall upward-fining sequence with sparse marine fossils and large, rounded quartzite dropstones.|
16267|Rolling Downs Group|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|70821|5|Briefly described|p21, p30-31, p33, p80, p109, p113-114|Late Cretaceous|Early Cretaceous|Eromanga, Surat Basins; Coonamble Embayment. Formerly included Hooray Sandstone. Sediments locally occupy palaeovalleys (eg Gongolgon).|||Wallumbilla, Toolebuc, Mackunda, Griman Creek, Winton Formations; Surat Siltstone; Allaru Mudstone.|Overlies Bungil or Cadna-owie Formations and Drildool beds. Is overlain unconformably by Glendower Formation.||
16267|Rolling Downs Group|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin.|||Griman Creek Formation.|||
16267|Rolling Downs Group|70860|6|Mentioned|p280-281|Cretaceous|Cretaceous|The main confining layer in the Great Artesian Basin.|||||A thick argillaceous marine sequence; mostly shallow-marine mudstone and siltstone.|
16267|Rolling Downs Group|71262|6|Mentioned|p9 Fig 7|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71342|6|Mentioned|Ch6 p12|||Originally subdivided by Whitehouse in 1926 who also subdivided this groups constituents into three sets of bed based on ammonite fauna. This scheme however was called into question by Casey (1960) and Day (1969). The validity of the Roma and Tambo Series was demonstrated by later workers (Dickins, 1960; Ludbrook, 1966; Day; 1969 and Morgan, 1980).|||Includes the Morven Bed, Roma Series, Maryborough Beds and the Tambo Series.|||
16267|Rolling Downs Group|71409|5|Briefly described|p1058-1059, p1061|Cretaceous|Cretaceous|Carpentaria Basin. Likely proximal source rocks for heavy minerals in central Cape York Peninsula. Outcrops in the northern tip of the Cape York Peninsula.||||Is overlain locally by Bulimba Formation.|Siltstones and claystones; deeply weathered and bauxitised.|23-APR-18
16267|Rolling Downs Group|71415|5|Briefly described|p11-p12|Late Cretaceous|Early Cretaceous|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. Represents sedimentation from Early to Late Cretaceous before marine regression and closure of the Eromanga Basin (Exon and Senior 1976; Greenfield, Gilmore and Mills 2010).||||Uppermost unit of the Eromanga Basin. Underlain by Cadna-owie Formation.|Alternating sandstone, mudstone and calcareous units.|19-AUG-19
16267|Rolling Downs Group|71601|6|Mentioned|p121|||Geological province: Surat Basin.|||Includes Griman Creek Formation.|||
16267|Rolling Downs Group|71792|4|Described|p57-p58|Late Cretaceous|Early Cretaceous|Carpentaria Basin.|||||Grey mudstone, siltstone and fine sandstone, minor glauconitic sandstone.|
16267|Rolling Downs Group|71849|6|Mentioned|p8, p195|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|71853|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous|The two facies are mapped separately.|||||Siltstone and mudstone; minor glauconitic sandstone. Deeply weathered siltstone and mudstone; minor glauconitic sandstone.|
16267|Rolling Downs Group|71854|5|Briefly described|Map legend.|Late Cretaceous|Early Cretaceous||||||Siltstone and mudstone with minor glauconitic sandstone; Deeply weathered siltstone and mudstone with minor glauconitic sandstone.|08-MAY-19
16267|Rolling Downs Group|71855|6|Mentioned|p20, p30|||Structure is briefly discussed.|||Includes the Toolebuc Formation.|||
16267|Rolling Downs Group|71863|5|Briefly described|p4|Late Cretaceous|Middle Jurassic|Carpentaria Basin. Deposited during a marine incursion.|||Includes the Wallumbilla Formation, the Toolebuc Formation, Allaru Mudstone and Normanton Formation.|||01-MAY-19
16267|Rolling Downs Group|71864|6|Mentioned|p13|||First described by Isbell (1957).|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|71890|6|Mentioned|p7|||Surat Basin.|||Includes the Wallumbilla Formation.|||
16267|Rolling Downs Group|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).|||Wallumbilla, Toolebuc, Mackunda, Winton, Normanton, Griman Creek FZs; Surat Siltstone; Allaru Mudstone.|Overlies Cadna-owie, Gilbert River, or Bungil FZ.||
16267|Rolling Downs Group|72914|6|Mentioned|p12|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|72915|6|Mentioned|p12, p26|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group (map symbol suggests Cretaceous age), and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Represented in the Congararra 1 borehole by 41.15 m TVD thickness of interbedded claystone, siltstone, sandstone and arkose where the top portion is an indurated silcrete (to 23.53 m TVD), and is weathered to ~42 m TVD, before becoming fresh gravelly sand.|||||Interbedded claystone, siltstone, sandstone and arkose|
16267|Rolling Downs Group|72967|6|Mentioned|p5|||Carpenteria Basin.|||Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation, Gilbert River Formation|||
16267|Rolling Downs Group|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
16267|Rolling Downs Group|73083|6|Mentioned|p51, p60-61, p68-69, p73|Mesozoic|Mesozoic|[Misspelt as Rolling Downs group on p61].|||Normanton Formation|||
16267|Rolling Downs Group|73144|6|Mentioned|p8|Cretaceous|Cretaceous|Carpentaria Basin. Contains units that constitute aquifers, partial aquifers, leaky aquitards and aquitards as well as host potential shale gas/oil plays and tight gas/oil.|||Normanton Formation, Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|Underlain by Gilbert River Formation.||17-OCT-22
16267|Rolling Downs Group|73147|5|Briefly described|p128-129|Albian|Aptian|Marine.|||Wallumbilla, Toolebuc, Normanton Formations; Allaru Mudstone.|||
16267|Rolling Downs Group|73177|5|Briefly described|p1112|Late Jurassic|Late Jurassic|Relatively undeformed; gives a minimum age for the Alice Springs Orogeny.||||Unconformably overlies Ravendale Formation.||
16296|Rombo Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Geological Province: Sydney Basin||||||
16296|Rombo Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Lucernia Coal. Geological Province: Sydney Basin||||||
16296|Rombo Coal Member|29942|3|Fully described|p11|||||||||
16296|Rombo Coal Member|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Lucernia Coal.||Overlies Hillsdale Claystone. Is overlain by Longford Creek Siltstone.||
16331|Rosebank Shale|13996|6|Mentioned|p146|Ludlow|Ludlow||||Rainbow Hill Marl Member.|||
16331|Rosebank Shale|22857|5|Briefly described|p458 App.1, Tb.A1.6|Late Silurian|Late Silurian|Of the Booroo Ponds Group. Geological Province: Canberra-Yass Shelf.||||||
16331|Rosebank Shale|23522|5|Briefly described|p248 Fig 4|Ludlow|Ludlow|||||||
16331|Rosebank Shale|24248|5|Briefly described|p52, p50 Fig.1|Pridoli|Late Silurian|Conformably overlain by the Cowridge Siltstone. Overlies the Black Bog Shale. Geological Province: Yass Syncline.||||||
16331|Rosebank Shale|24249|5|Briefly described|p90 Fig.3, p91|Pridoli|Pridoli|Overlying Unit: Cowridge Siltstone||||||
16331|Rosebank Shale|30069|6|Mentioned|p5|||||||||
16331|Rosebank Shale|30252|6|Mentioned|p183|||||||||
16331|Rosebank Shale|31852|5|Briefly described|p711|||See also p714,719,720 & Figs. 1,2,4,5. Upper Silurian.||||||12-JUN-08
16331|Rosebank Shale|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature||||||
16331|Rosebank Shale|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
16331|Rosebank Shale|33116|6|Mentioned|Fig.11|||Correlation||||||
16331|Rosebank Shale|33325|5|Briefly described|Table 2|||See also Table 3.||||||
16331|Rosebank Shale|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
16331|Rosebank Shale|35386|4|Described|p36|||||||||
16331|Rosebank Shale|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
16331|Rosebank Shale|36413|6|Mentioned|Table 3|||||||||
16331|Rosebank Shale|37013|6|Mentioned|p34|||||||||
16331|Rosebank Shale|37727|4|Described|p83|||See also p6.||||||12-JUN-08
16331|Rosebank Shale|38151|6|Mentioned|Table 1|||||||||
16331|Rosebank Shale|38691|5|Briefly described|Fig.1|||||||||
16331|Rosebank Shale|39331|6|Mentioned|Fig.5-5|||||||||
16331|Rosebank Shale|40328|3|Fully described|p52|||||||||
16331|Rosebank Shale|42029|5|Briefly described|Fig.1 P96|||See also p96.||||||12-JUN-08
16331|Rosebank Shale|42033|6|Mentioned|p650|||||||||
16331|Rosebank Shale|45075|6|Mentioned|p7|||||||||
16331|Rosebank Shale|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Hattons Corner Group.  Overlies Black Bog Shale; underlies Cowridge Siltstone.  Light and dark-grey shale, mudstone siltstone.  Contains the Rainbow Hill Member.||||||10-MAY-04
16331|Rosebank Shale|63083|6|Mentioned|p219|Ludlow|Ludlow|In the Yass district. Fossil fauna includes phacopids and dalmanitids.||||||07-FEB-11
16331|Rosebank Shale|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hattons Corner Group. Contains the Rainbow Hill Member. Light and dark grey shale, mudstone siltstone. Formerly the "Upper Trilobite bed".||||||12-JUN-08
16331|Rosebank Shale|67820|6|Mentioned|p136 Fig.3|Silurian|Silurian|||Hattons Corner Group.||||
16331|Rosebank Shale|68592|2|Defined|p430 Fig.89, p560-2, p590-7, p1883|Pridoli|Ludlow|Named after Rosebank property. Link (1970, 1971); Link and Druce (1972); unit in their Booroo Ponds Group. They included in it the Rainbow Hill Marl Member. Shale here transferred to redefined Hattons Corner Group. Type section described. 82-128m thick. Slaty cleavage common. Contains a rich fauna of trilobites, brachiopods and corals in lower part.||Unit in Hattons Corner Group.|Includes Rainbow Hill Member.|Conformably overlies Black Bog Shale. Is overlain conformably by Cowridge Siltstone.|Basal thin, persistent, strongly bioturbated, highly fossiliferous horizon of siltstone, mudstone, shale, minor calcareous siltstone and limestone; overlain by grey, green-grey and black shale, silty mudstone and siltstone.|13-JAN-17
16331|Rosebank Shale|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Shr. [Shown to be previously known as] "Upper Trilobite Bed"[but the Goulburn Notes2012 suggest that this is a typo on the map]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hattons Corner Group|Includes Rainbow Hill Member.|Is overlain by Cowridge Siltstone. Overlies Black Bog Shale.|Massive-laminated shale and mudstone with thin-very thin beds of siltstone.|13-JAN-17
16331|Rosebank Shale|70540|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Upper Trilobite Bed".||Hattons Corner Group|Includes Rainbow Hill Member.||Massive-laminated shale and mudstone with thin-very thin beds of siltstone.|
16331|Rosebank Shale|70546|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Upper Trilobite Bed".||Hattons Corner Group|Includes Rainbow Hill Member||Massive to laminated shale and mudstone with thin to very thin beds of siltstone ("upper trilobite bed").|
16331|Rosebank Shale|71656|5|Briefly described|p12 Fig.2, p19, p26|Pridoli|Ludlow|Graptolites are the only fossils described.||Hattons Corner Group.|Includes Rainbow Hill Member at base?|Underlies Cowridge Siltstone.|Fossiliferous shale with graptolite fauna.|
16341|Rosebrook Limestone|42414|6|Mentioned|p59|||||||||19-FEB-09
16342|Rosebrook Member|40664|3|Fully described|p238|Miocene|Miocene|||||||13-JUN-13
16342|Rosebrook Member|42035|6|Mentioned|p128|||||||||
16344|Rosedale Member|30340|6|Mentioned|p2530|||Lithology||||||
16344|Rosedale Member|30341|6|Mentioned|p138|||Unit of Currabubula Formation||||||
16344|Rosedale Member|37919|6|Mentioned|p476|||||||||
16344|Rosedale Member|38818|6|Mentioned|p169|||Geological Province: New England Fold Belt. Of the Currabubula Formation||||||
16344|Rosedale Member|39572|6|Mentioned|Fig.2|||||||||
16344|Rosedale Member|42339|5|Briefly described|p52|||||||||
16344|Rosedale Member|42547|5|Briefly described|p22|||of Currabubula Formation.||||||
16344|Rosedale Member|43446|14|Not recorded|p6028,6029||Late Carboniferous|||||||
16344|Rosedale Member|44835|2|Defined|p43,46-7,49-50,52-4||Late Carboniferous|Member of Currabubula Formation. Pl.1.||||||
16344|Rosedale Member|62095|5|Briefly described|p251|||Of the Currabubula Formation. Geological Province: Werrie Block/Tamworth Belt.||||||
16344|Rosedale Member|63832|5|Briefly described|p134-135|Bashkirian|Bashkirian|Third (C3) glaciation.||Currabubula Formation|||An interval of proglacial lake deposits with rhythmic grain-size alternation between clay, silt and sand laminae, and dispersed gravel.|
16368|Rossmore Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16368|Rossmore Formation|32482|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
16368|Rossmore Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16368|Rossmore Formation|36045|6|Mentioned|p329|||||||||
16368|Rossmore Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
16368|Rossmore Formation|36528|6|Mentioned|p179|||||||||
16368|Rossmore Formation|40883|6|Mentioned|p8|||||||||
16368|Rossmore Formation|42547|4|Described|p31|||||||||
16368|Rossmore Formation|43407|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition) Middle Carboniferous||||||
16368|Rossmore Formation|43417|4|Described|Map Legend||Late Carboniferous|||||||
16368|Rossmore Formation|44244|6|Mentioned|p95|Carboniferous|Carboniferous|||||||
16368|Rossmore Formation|45088|6|Mentioned|p59|||Refers Manser (1968)||||||
16368|Rossmore Formation|45097|6|Mentioned|p25|||No palaeontological control of age||||||
16368|Rossmore Formation|62095|6|Mentioned|p264|Carboniferous|Carboniferous|Of Manser (1968). Synonymous with Currabubula Formation of Voisey and Williams (1964) and Upper Kuttung Series of Carey (1937).||||||
16395|Rowena Formation|13995|5|Briefly described|p74|||Koonenberry Belt. Marginal marine deposits. Contains Early Ordovician (Arenig) lingulate brachiopods, quite distinct from those in the Yarrimbah Formation, W of Parkes, which occur with late Lancefieldian-early Bendigonian graptolites.|||||Quartz arenites.|
16395|Rowena Formation|22671|5|Briefly described|p833,Fig2p837||Early Ordovician|Of the Mootwingee Group. Shale, siltstone, limestone. Unconformably overlies Ponto beds and rocks correlated with the Kara beds.||||||17-JAN-06
16395|Rowena Formation|22857|5|Briefly described|p120, p408 App. 1 Tb. A1.4.|Early Ordovician|Early Ordovician|Of the Mootwingee Group. Shale, siltstone, limestone. Max. thickness: 1700m. Geological Province: Kanmantoo Fold Belt.||||||
16395|Rowena Formation|23245|5|Briefly described|p120,122||Early Ordovician|||||||
16395|Rowena Formation|23469|4|Described|p 319|||also see Fig 13 p 327. Of Mootwingee Group.||||||
16395|Rowena Formation|29991|6|Mentioned|Map legend|Early Ordovician|Early Ordovician|||||||
16395|Rowena Formation|30908|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16395|Rowena Formation|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
16395|Rowena Formation|32672|6|Mentioned|p671|||||||||
16395|Rowena Formation|32918|6|Mentioned|p13|||||||||
16395|Rowena Formation|33004|6|Mentioned|Fig.8|||||||||
16395|Rowena Formation|33738|6|Mentioned|p46|||||||||
16395|Rowena Formation|34469|6|Mentioned|p108|||Ordovician||||||
16395|Rowena Formation|35118|6|Mentioned|Fig.5|||||||||
16395|Rowena Formation|36047|6|Mentioned|p369|||||||||
16395|Rowena Formation|39214|4|Described|p10|||||||||
16395|Rowena Formation|40136|5|Briefly described|p38|||||||||
16395|Rowena Formation|41810|6|Mentioned|Fig.3|||||||||
16395|Rowena Formation|43501|14|Not recorded|Map Legend|Early Ordovician|Early Ordovician|(Provisional Edition) Part of Mootwingee Group. (L.-M.Ord)||||||
16395|Rowena Formation|43502|14|Not recorded|Map Legend||Ordovician|(Provisional Edition) Part of Mootwingee Group||||||
16395|Rowena Formation|43704|6|Mentioned|Fig.1,p68|Early Ordovician|Early Ordovician|||||||
16395|Rowena Formation|50129|5|Briefly described|p16|||Of the Mootwingee Group.||||||
16395|Rowena Formation|62793|4|Described|p269 Fig.2, p270, p271|Early Ordovician|Early Ordovician|Uppermost unit of Mutawintji (formerly Mootwingee) Group.||||Overlies Bynguano Quartzite.|Quartzose sediments containing shelly fossil fauna, predominantly brachiopods, and thin carbonate horizons containing conodonts.|21-MAR-12
16395|Rowena Formation|62794|6|Mentioned|p299|Early Ordovician|Early Ordovician|Bynguano Range area, western NSW. The lower part of the Formation correlates with Horn Valley Siltstone, Amadeus Basin.||||||
16395|Rowena Formation|62795|4|Described|p347, p348, p349|Middle Ordovician|Early Ordovician|Top of Mutawintji Group, overlying Bynguano Quartzite, unconformably underlying Snake Cave Sandstone. Includes Gundara Quartzite Member.Max thickness 1685m. Age based on trilobites and conodonts. Interbedded sandstone, siltstone, shale, impure limestone, and conglomerate.||||||
16395|Rowena Formation|63121|5|Briefly described|p225 Fig. 2, p232|Early Ordovician|Early Ordovician|Equivalent to the upper part of the Gnalta stage of the former Mootwingee Series. In the Koonenberry Belt, western NSW.  Age is Bendigonian to Chewtonian.||||||13-MAR-07
16395|Rowena Formation|63789|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Of Mootwingee Group. Conglomeratic quartzite, sandstone, red, grey to green silty shale. Terrestrial to marine. Early to Middle(?) Ordovician fossils.||||||
16395|Rowena Formation|63790|5|Briefly described|Map Legend|Ordovician|Late Cambrian|Of Mootwingee Group. Well-bedded white quartzites and pebbly quartzites on Burkes Lookout (Mt. Handtherunga). Minor green-grey and maroon siltstones and fine sandstones. Some worm burrows.||||||
16395|Rowena Formation|64671|5|Briefly described|Map legend|Middle Ordovician|Early Ordovician|Of the Mootwingee Group.||||||
16395|Rowena Formation|64679|5|Briefly described|Map legend|Ordovician|Late Cambrian|Of the Mutwintji Group.  Contains the Gundara Quartzite Member. Red, grey, green siltstone, grey to white quartzite, green and yellow sandstone; brachiopod, trilobite and conodont fossils; Skolithos tubes and other trace fossils.||||||27-NOV-08
16395|Rowena Formation|64680|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Of Mootwingee Group.||||||01-DEC-08
16395|Rowena Formation|64685|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|Equivalents of Rowena Formation. Quartzite and quartz sandstone.||||||
16395|Rowena Formation|64686|5|Briefly described|Map Legend|Middle Ordovician|Early Ordovician|Of Mootwingee Group.||||||
16395|Rowena Formation|66623|3|Fully described|pp134-136, p138, pp146-148.|Middle Ordovician|Early Ordovician|Named by Warris (1967), described by Shergold (1971), elaborated by Pogson and Scheibner (1976). Quartzite-dominated lithologies are resistant and form prominent exposures. Thickness varies laterally, from c.1230 m to c.2260 m. Contains trilobites, lingulide brachiopods, conodonts and trace fossils. Correlates with Tabita Formation and is contemporaneous in part with Scropes Range Formation.||Unit in Mutawintji Group.|Includes Gundara Quartzite Member.|Overlies Bynguano Quartzite. Is overlain unconformably or paraconformably by New Tank Formation of Wana Karnu Group.|Interbedded quartzose sandstones, siltstones, shales, conglomerates and occasional calcareous beds; a thin micrite/limestone horizon occurs in the middle of the Formation, which also has a c.15 m thick basal pebbly grey quartzite unit.|
16395|Rowena Formation|66918|5|Briefly described|Map legend|||||Unit in Mutawintji Group.|Includes Gundara Quartzite.|Overlies Bynguano Quartzite.|Folded and weakly cleaved sequence of basal pebbly quartz sandstone and red sandstone overlain by grey to green siltstone with interbedded decimetre-scale marl lenses; regionally metamorphosed to prehnite-pumpellyite facies.|
16395|Rowena Formation|66929|6|Mentioned|Map legend|Middle Ordovician|Early Ordovician|||Unit in Mootwingee Group.||||
16395|Rowena Formation|67322|4|Described|p8-9, p13; Fig.5|Darriwilian|Tremadocian|Of Warris (1967). Approximately 1700m thick. Age from fossils; discussion of age discrepancies from different fossil species. Occurs in the Mount Wright-Mutawintji region.||Of the Mutawintji Group.|Gundara Quartzite Member|Conformably overlies Bynguano Quartzite. Correlated with Scropes Range Formation.|Basal resistant quartzite; interbedded quartzose sandstones, siltstones and shales with occasional calcareous beds in the middle.|22-FEB-18
16395|Rowena Formation|67562|6|Mentioned|p110 Fig.14, p112 Fig.15|Ordovician|Ordovician|||||||
16395|Rowena Formation|70648|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|||Folded and weakly cleaved sequence of basal pebbly quartz sandstone and red sandstone overlain by grey to green siltstone with interbedded decimetre-scale fossiliferous marl lenses.
|
16395|Rowena Formation|70650|5|Briefly described|Map Legend|Ordovician|Cambrian|||Mutawintji Group|Includes Gundara Quartzite [Member?].||Folded and weakly cleaved sequence of basal pebbly quartz sandstone and red sandstone overlain by grey to green siltstone with interbedded decimetre-scale fossiliferous marl lenses.
|
16395|Rowena Formation|73346|6|Mentioned|p18|Darriwilian|Tremadocian|Koonenberry Belt. Includes the arandaspid Arandaspis sp. Indet.||||||
16421|Rubyview Gneiss|37871|4|Described|p4|||||||||
16421|Rubyview Gneiss|38367|6|Mentioned|Fig.27|||||||||
16421|Rubyview Gneiss|39858|6|Mentioned|Map legend|Silurian|Ordovician|Silurian - Ordovician||||||
16430|Rufus Formation|30994|6|Mentioned|p247|||Soil development discussed||||||
16430|Rufus Formation|30996|2|Defined|p43|Pleistocene|Pleistocene|||||||
16430|Rufus Formation|31385|6|Mentioned|p74|||||||||
16430|Rufus Formation|32007|4|Described|p160|||late Pleistocene||||||
16430|Rufus Formation|35232|6|Mentioned|Table 4|||||||||
16430|Rufus Formation|41537|6|Mentioned|p350|||||||||
16430|Rufus Formation|42592|6|Mentioned|p281|||||||||
16430|Rufus Formation|42966|3|Fully described|Table 32 p207|Late Pleistocene||||||||
16430|Rufus Formation|43655|5|Briefly described|p40-846|||||||||
16430|Rufus Formation|44133|6|Mentioned|p253|||||||||
16463|Rutherford Formation|22610|5|Briefly described|Fig 1|||Maximum thickness 384m||||||
16463|Rutherford Formation|22663|5|Briefly described|NSW97 -1 Fig.2|Early Permian|Early Permian|||||||01-MAR-10
16463|Rutherford Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Dalwood Group. Siltstone, marl: minor sandstone. Max. thickness: 385m. Geological Province: Sydney Basin.||||||
16463|Rutherford Formation|22969|4|Described|p 18, Fig 2.2||Early Permian|Dalwood Group.||||||05-AUG-08
16463|Rutherford Formation|22970|5|Briefly described|Plate 6|||||||||
16463|Rutherford Formation|23350|5|Briefly described|262|Early Permian|Early Permian|||||||
16463|Rutherford Formation|23540|5|Briefly described|Fig2 p 419|||Of the Dalwood Group.||||||20-FEB-07
16463|Rutherford Formation|24079|5|Briefly described|p432|Permian|Permian|Of Dalwood Group.  Geological Province: Sydney Basin.||||||
16463|Rutherford Formation|24121|5|Briefly described|p4|||Of Dalwood Group.||||||
16463|Rutherford Formation|24547|6|Mentioned|p24|||Of the Dalwood Group. Fossils indicate a broad correlation with the Golden Valley Group.||||||
16463|Rutherford Formation|29437|6|Mentioned|p136|||||||||
16463|Rutherford Formation|29752|6|Mentioned|p34|||||||||
16463|Rutherford Formation|29915|6|Mentioned|p68|||||||||
16463|Rutherford Formation|30341|6|Mentioned|p136|||Permian age||||||
16463|Rutherford Formation|30450|6|Mentioned|Table 1|||Permian age. Sydney Basin||||||
16463|Rutherford Formation|30545|6|Mentioned|Fig.2|||Sakmarian||||||
16463|Rutherford Formation|31081|6|Mentioned|p56|||See also Fig. 2||||||
16463|Rutherford Formation|31298|6|Mentioned|p16|||||||||
16463|Rutherford Formation|31598|6|Mentioned|p46|||||||||
16463|Rutherford Formation|31883|6|Mentioned|Table 1|||||||||
16463|Rutherford Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis konincki||||||
16463|Rutherford Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
16463|Rutherford Formation|32672|6|Mentioned|p675|||||||||
16463|Rutherford Formation|32840|6|Mentioned|Table 1|||||||||
16463|Rutherford Formation|32943|6|Mentioned|p105|||||||||
16463|Rutherford Formation|32945|6|Mentioned|p83|||See also Fig.1. Permian||||||
16463|Rutherford Formation|33334|6|Mentioned|Fig.6|||||||||
16463|Rutherford Formation|33701|6|Mentioned|Fig.1|||Sakmarian||||||
16463|Rutherford Formation|33711|6|Mentioned|p382|||||||||
16463|Rutherford Formation|33867|5|Briefly described|p5|||||||||
16463|Rutherford Formation|34099|6|Mentioned|p17|||||||||
16463|Rutherford Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
16463|Rutherford Formation|34170|6|Mentioned|p47|||Lower Permian||||||
16463|Rutherford Formation|34292|6|Mentioned|Table 1|||Permian||||||
16463|Rutherford Formation|34444|6|Mentioned|Map legend|Permian|Permian|||||||
16463|Rutherford Formation|34445|3|Fully described|p322|||||||||
16463|Rutherford Formation|34447|6|Mentioned|Table 5.2|||||||||
16463|Rutherford Formation|34448|4|Described|p431|||Permian||||||
16463|Rutherford Formation|34512|6|Mentioned|p52|||||||||
16463|Rutherford Formation|35284|6|Mentioned|Fig.1|||||||||
16463|Rutherford Formation|36042|6|Mentioned|Table 1|||||||||
16463|Rutherford Formation|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16463|Rutherford Formation|37065|6|Mentioned|p32|||||||||
16463|Rutherford Formation|37082|6|Mentioned|p161|||||||||
16463|Rutherford Formation|37086|6|Mentioned|p183|||||||||
16463|Rutherford Formation|37087|6|Mentioned|p192|||||||||
16463|Rutherford Formation|37561|6|Mentioned|p105|||||||||
16463|Rutherford Formation|38656|5|Briefly described|Fig.1.5.13|||P280||||||
16463|Rutherford Formation|38820|6|Mentioned|p180|||||||||
16463|Rutherford Formation|39262|6|Mentioned|p122|||||||||
16463|Rutherford Formation|39287|6|Mentioned|p20|||See also Fig.2.5||||||
16463|Rutherford Formation|39288|4|Described|p59|||||||||
16463|Rutherford Formation|39290|6|Mentioned|p88|||||||||
16463|Rutherford Formation|39304|6|Mentioned|p364|||See also Fig. 19.2||||||
16463|Rutherford Formation|39307|6|Mentioned|p438|||Foraminifera||||||
16463|Rutherford Formation|39308|6|Mentioned|p477|||||||||
16463|Rutherford Formation|39833|6|Mentioned|Fig.2|||||||||
16463|Rutherford Formation|40166|6|Mentioned|p343|||See also Table 1 and Fig.2||||||
16463|Rutherford Formation|40636|6|Mentioned|p43|||||||||
16463|Rutherford Formation|40997|6|Mentioned|p413|||||||||
16463|Rutherford Formation|41275|6|Mentioned|p27|||||||||
16463|Rutherford Formation|41315|6|Mentioned|p149|||||||||
16463|Rutherford Formation|41514|6|Mentioned|p79|||||||||
16463|Rutherford Formation|41580|6|Mentioned|Table 1|||||||||
16463|Rutherford Formation|41902|5|Briefly described|p5 Table 1|||||||||
16463|Rutherford Formation|42000|6|Mentioned|p55|||||||||
16463|Rutherford Formation|42925|5|Briefly described|Table 1||Early Permian|||||||
16463|Rutherford Formation|43017|5|Briefly described|Fig.1,p372|||||||||
16463|Rutherford Formation|43018|5|Briefly described|Table 1,p386|||||||||
16463|Rutherford Formation|43050|6|Mentioned|p9|||One of the locations for the fossil Earlandia condoni Crespin 1958. Geological province: Sydney Basin.||||||21-MAY-07
16463|Rutherford Formation|43194|5|Briefly described|p129 Tb. 8.3|Early Permian|Early Permian|Of Gyarran Volcanics (Hunter region) and Dalwood Group (Newcastle region), Sydney Basin.||||||13-NOV-13
16463|Rutherford Formation|43257|5|Briefly described|Map Legend||Early Permian|Of Dalwood Group.||||||
16463|Rutherford Formation|43344|14|Not recorded|p84|||Formerly called Rutherford Stage||||||
16463|Rutherford Formation|43385|14|Not recorded|p179,180||Sakmarian|||||||
16463|Rutherford Formation|43440|14|Not recorded|p36,62,74,91|||||||||
16463|Rutherford Formation|43447|4|Described|Table 1,p16||Permian|Part of Dalwood Group.||||||05-AUG-08
16463|Rutherford Formation|43448|14|Not recorded|p224||Permian|On table only||||||
16463|Rutherford Formation|43474|14|Not recorded|p10|||||||||
16463|Rutherford Formation|43479|14|Not recorded|p218||Artinskian|||||||
16463|Rutherford Formation|44040|14|Not recorded|p27|||||||||
16463|Rutherford Formation|44135|6|Mentioned|p43|||Unit in NSW.||||||07-DEC-09
16463|Rutherford Formation|44219|14|Not recorded|p29,31,32,37,43||Sakmarian|||||||
16463|Rutherford Formation|44855|14|Not recorded|p18|Permian|Carboniferous|||||||
16463|Rutherford Formation|45006|14|Not recorded|Tb.1,opp.p3|||||||||
16463|Rutherford Formation|45031|14|Not recorded|p25,51,64,67||Permian|||||||
16463|Rutherford Formation|45090|5|Briefly described|p7|||Time correlation chart. Isopach map P34.||||||
16463|Rutherford Formation|47041|6|Mentioned|Fig.2|||||||||
16463|Rutherford Formation|49644|5|Briefly described|Table|||||||||
16463|Rutherford Formation|60281|5|Briefly described|p56|Early Permian|Early Permian|Included in the Upper Dalwood Group.  Siltstone and minor sandstone with thin limestone and marl horizons in the Pokolbin area of the Hunter Valley.  Geological Province: Sydney Basin.||||||20-JAN-05
16463|Rutherford Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Sakmarian|Correlated with Billy Brook Formation, upper Pebbley Beach Formation, Faulkner Group and Liffey Group. Geological Province: Sydney Basin.||||||18-MAY-05
16463|Rutherford Formation|60330|5|Briefly described|p264|||Overlies Allandale Formation with sharp contact. Contains foraminiferida. Geological Province: Sydney Basin.||||||
16463|Rutherford Formation|60386|6|Mentioned|p296|Artinskian|Artinskian|Bowen/Sydney Basin. Deltaic - nearshore - shelf.||||||
16463|Rutherford Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin/ Newcastle area.||||||
16463|Rutherford Formation|61529|5|Briefly described|p871|Early Permian|Early Permian|Of the Dalwood Group. Geological Province: Sydney Basin.||||||
16463|Rutherford Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||17-MAR-09
16463|Rutherford Formation|63172|6|Mentioned|p301|||Of the Dalwood Group in NSW.||||||07-FEB-11
16463|Rutherford Formation|63832|5|Briefly described|p131 fig 2|Artinskian|Artinskian|Of Sydney Basin. Sixth (P2) glaciation.||Unit in Dalwood Group.||||14-DEC-17
16463|Rutherford Formation|64631|5|Briefly described|p44 Fig.2.|Artinskian|Sakmarian|Sydney Basin. Biostratigraphic age control at base and top.||Unit in Dalwood Group.||Overlies Allandale Formation.||
16463|Rutherford Formation|68003|5|Briefly described|p38 Fig.3-j.|Early Permian|Early Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Unit in Dalwood Group.||Overlies Allandale Formation. Is overlain by Farley Formation.||
16463|Rutherford Formation|68004|5|Briefly described|p23 Table 1.|||Hunter and Newcastle Coalfields.||Unit in Dalwood Group.||Overlies Allandale Formation. Is overlain by Farley Formation.||
16463|Rutherford Formation|68493|5|Briefly described|p1; p3,5 Figs.1,2; p6, p10 Fig.4, p12|Artinskian|Artinskian|Contains a Permian bivalve-dominated faunal assemblage exposed at Tocal near Paterson. Type section has not been designated. Thickness estimated around 384 m by McClung (1980). Deposited during Fielding et al.'s (2008) glacial episode P2.||Of the Dalwood Group.||Overlies the Allandale Formation. Correlative of Billy Brook Formation of Cranky Corner Basin. Overlain by the Farley Formation.|Siltstone, mudstone; shale, marl, sandstone, minor conglomerate.|19-JAN-17
16463|Rutherford Formation|69297|6|Mentioned|p501, p502 fig 5.43|Artinskian|Artinskian|Sydney Basin.||Dalwood Group||Overlies the Allandale Formation. Overlain by the Farley Formation.||
16463|Rutherford Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|||Unit in Gyarran Volcanics.||||
16463|Rutherford Formation|70096|5|Briefly described|p221;Supp2-3|||Of northern Sydney Basin. See also supplementary files in appendix for additional stratigraphic and locality information.||Unit of Dalwood Group.||Underlain by Allandale Formation.||
16463|Rutherford Formation|73304|6|Mentioned|p75|||||Gyarran Volcanics||||
16485|Rye Park Granite|29989|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
16485|Rye Park Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
16485|Rye Park Granite|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
16485|Rye Park Granite|30734|6|Mentioned|p12|||See also P18,54||||||
16485|Rye Park Granite|32483|4|Described|p34|||M.Dev.? Strat. table 1.||||||
16485|Rye Park Granite|35257|6|Mentioned|p99|||||||||
16485|Rye Park Granite|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
16485|Rye Park Granite|35386|3|Fully described|p60|||||||||
16485|Rye Park Granite|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
16485|Rye Park Granite|40328|4|Described|p210|||||||||
16485|Rye Park Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
16485|Rye Park Granite|50230|5|Briefly described|Map legend|Ludlow|Ludlow|Part of the Wyangala Batholith.  Muscovite-biotite granite.||||||
16485|Rye Park Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
16485|Rye Park Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Cream, leucocratic, medium- to coarse-grained, cordierite?-muscovite-biotite granite.||||||
16485|Rye Park Granite|66300|5|Briefly described|pp92-97.|||This age establishes the temporal equivalence of the Hovells, Burrawinda and Gunning Suites in west-central GOULBURN area. Hosts tungsten mineralisation.|431.4 +/- 4.9 Ma.|Unit in Hovells Suite.||Intrudes Hawkins Volcanics.|Medium-grained, equigranular to weakly seriate, bone-coloured leucocratic monzogranite.|
16485|Rye Park Granite|66713|6|Mentioned|p13|||Is the source of W-Sn-Mo mineralisation in the Rye Park skarn. Intrudes Hawkins Volcanics.||||||
16485|Rye Park Granite|67820|6|Mentioned|p135|||Highly fractionated. It is the source for W skarn mineralisation at the Rye Park scheelite mine.||||||
16485|Rye Park Granite|68592|2|Defined|p1262-4, p1268-9, p1284, p1299-1301|Late Silurian|Early Silurian|See also xxiv, p199, p206-9, p433, p443, p467, p1255 Fig.220, p1274. Originally studied and mapped by Sullivan and Dallwitz (1952), followed by later workers. First published by Brunker and Offenberg (1970). Named after the town of Rye Park. Here assigned to the Hovells Suite on geochemical grounds. Type section described. Geochemistry detailed; geophysical properties described. Highly fractionated, heavily altered and poorly exposed. Associated with W-Bi-Sn-Cu skarn mineralisation within Hawkins Volcanics; mined at the Rye Park Mine (Tungsten Deposit: detailed). Also dated at 428 +/- 3.9 Ma (SHRIMP zircon: Bodorkos, 2009).|427 +/- 11 Ma (lead model age; Downes, 2009).|Unit in Hovells Suite.||Intrudes Hawkins Volcanics.|Cream, leucocratic, medium- to coarse-grained, muscovite-biotite granite. S-type.|
16485|Rye Park Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Soy. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Leucocratic, medium-coarse grained, cordierite?-muscovite-biotite granite; very low magnetic susceptibility.|
16485|Rye Park Granite|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Hovells Suite|||Leucocratic, medium-coarse grained, cordierite?-muscovite-biotite granite with very low magnetic susceptibility.|
16485|Rye Park Granite|70545|5|Briefly described|Map Legend|Devonian|Silurian|||Hovells Suite|||Leucocratic, medium-coarse grained, cordierite?-muscovite-biotite granite; very low magnetic susceptibility.|
16489|Rylstone Volcanics|22529|5|Briefly described|2|Early Permian|Early Permian|Overlying unit Shoalhaven Group.||||||12-NOV-08
16489|Rylstone Volcanics|22545|6|Mentioned|p504||Darriwilian|||||||
16489|Rylstone Volcanics|22580|6|Mentioned|p95|Early Permian|Late Carboniferous|||||||
16489|Rylstone Volcanics|22857|5|Briefly described|p230, p504 App.1 Tb.A1.8|Early Permian|Early Permian|Ignimbrites, ashfall tuff horizons, flow-banded rhyolite lava. Max. thickness: est. 300m. Geological Province: Lachlan Fold Belt. See also p256.||||||
16489|Rylstone Volcanics|22863|5|Briefly described|p230||Early Permian|||||||
16489|Rylstone Volcanics|22864|6|Mentioned|p256|||||||||
16489|Rylstone Volcanics|23043|5|Briefly described|Map Legend|Early Permian|Early Permian|Of Sydney Basin..||||||12-NOV-08
16489|Rylstone Volcanics|23092|5|Briefly described|p627-628|Early Permian|Late Carboniferous|292+/-10 M yr||||||
16489|Rylstone Volcanics|23170|2|Defined|p281, 283 Fig.61|Permian|Carboniferous|Age: Rb/Sr age 292 Ma. of Sydney Basin.||||||
16489|Rylstone Volcanics|24040|6|Mentioned|p468 Fig. 1|||Geological Province: Sydney Basin.||||||12-NOV-08
16489|Rylstone Volcanics|34037|6|Mentioned|p426|||||||||
16489|Rylstone Volcanics|34130|6|Mentioned|p178|||||||||
16489|Rylstone Volcanics|36042|6|Mentioned|p41|||||||||
16489|Rylstone Volcanics|38837|6|Mentioned|p230|||||||||
16489|Rylstone Volcanics|42547|5|Briefly described|p43|||||||||
16489|Rylstone Volcanics|43188|4|Described|p221,Table 7 p220||Permian|Rb/Sr date of 292 Ma, earliest Permian.||||||
16489|Rylstone Volcanics|44093|5|Briefly described|p212 App. 1|Early Permian|Early Permian|Felsic volcanics; calc-alkaline I-type; unmetamorphosed, but altered;subaerial, several volcanic centres and volcanic subsidence structures. Geological Province: Lachlan Fold Belt: Capertee Zone.||||||
16489|Rylstone Volcanics|60266|5|Briefly described|p2, p3 Tb. 1|Early Permian|Early Permian|Felsic volcanics - rhyolitic to dacitic pyroclastic deposits.  Unconformably overlain by Dunedoo Formation.  Geological Province: Gunnedah Basin.||||||03-AUG-04
16489|Rylstone Volcanics|61791|6|Mentioned|p325|||||||||
16489|Rylstone Volcanics|61900|5|Briefly described|p129, p130 Fig. 3|Early Permian|Early Permian|Mainly dacitic and rhyolitic pyroclastics and epiclastics. Unconformably overlie the phyllites of the Coomber Formation. Age: 292Ma (Rb-Sr, Shaw et al 1989).  Geological Province: Sydney Basin.||||||
16489|Rylstone Volcanics|65114|5|Briefly described|p383 Tb.1, p396|Early Permian||Listed as Early Permian; 292 Ma; Tectonic unit: Southern and western Sydney Basin; felsic; Rb/Sr age of 292 Ma||||||
16489|Rylstone Volcanics|67663|6|Mentioned|p519 Fig.1, p533|||||||||
16489|Rylstone Volcanics|68003|5|Briefly described|p38 Fig.3-j, p40, p129, p131.|Early Permian|Early Permian|Western Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Thick volcanic sequence.|||||Rhyolitic to dacitic pyroclastic rocks; tuffaceous sandstone, thin airfall tuff horizons, lavas.|
16489|Rylstone Volcanics|68004|5|Briefly described|p64, p117.|Early Permian|Early Permian|Western Coalfield. Non-conformably overlies Carboniferous basement granites. Hosts the Bowdens Gift Ag-Pb-Zn prospect with a resource of 59 Mt at 43.8 g/t Ag.|||||Widely variable composition of rhyolitic to dacitic pyroclastic and ignimbrite sheets, flow-layered lavas and epiclastic units, which may show ripples, cross-beds and parallel laminations.|
16489|Rylstone Volcanics|68822|6|Mentioned|p321, p338|Lower Permian|Lower Permian|Beneath the Sydney Basin. Shows some relic supra-subduction zone component in the melt.||||||
16489|Rylstone Volcanics|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian felsic volcanic rocks: rhyolite, dacite, tuff and shale.||||||
16489|Rylstone Volcanics|73197|6|Mentioned|p470-471|Cisuralian|Late Carboniferous|Western edge of the Sydney Basin.|300-290 Ma||||Volcanics.|
16489|Rylstone Volcanics|73299|6|Mentioned|p1095, p1100 Fig.5|Permian|Cisuralian|Sydney Basin. Gently dipping at the base of the Sydney Basin succession, lowest Permian age.||||||
16491|Ryrie Formation|22815|1|Redefined|p33, fig10,16|Llandovery|Llandovery|Equivalent of Tombong Formation. Now excludes 'Gungoandra Siltstone Member'.||||||17-JAN-07
16491|Ryrie Formation|22857|4|Described|p134, p420 App. 1 Tb. A1.5|Late Silurian|Early Silurian|Of the Yalmy Group. Massive bedded arenite with siltstone interbeds. Max. thickness: >1.6km. Geological Province: Yalmy Basin. See also p468 App.1 Tb.A1.6.||||||
16491|Ryrie Formation|22968|6|Mentioned|P108|||Parent is Yalmy Group.||||||20-MAY-08
16491|Ryrie Formation|23245|5|Briefly described|p134||Early Silurian|||||||
16491|Ryrie Formation|23454|5|Briefly described|p33|Llandovery|Llandovery|||||||
16491|Ryrie Formation|32820|5|Briefly described|p2|||||||||
16491|Ryrie Formation|32822|6|Mentioned|p17|||Graptolites.||||||20-MAY-08
16491|Ryrie Formation|36413|2|Defined|p30|Early Silurian|Early Silurian|||||||
16491|Ryrie Formation|36414|5|Briefly described|map legend|Llandoverian|Llandoverian|Includes Gungoandra Siltstone Member. Quartzite with minor interbedded siltstone and shale. GSNSW map code: Sr.||||||03-OCT-07
16491|Ryrie Formation|39626|6|Mentioned|p276|||||||||
16491|Ryrie Formation|40328|5|Briefly described|p140|||||||||
16491|Ryrie Formation|42820|5|Briefly described|p9|||||||||
16491|Ryrie Formation|43233|5|Briefly described|Map Legend||Llandovery|Of Yalmy Group.||||||20-MAY-08
16491|Ryrie Formation|44093|5|Briefly described|p192 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
16491|Ryrie Formation|61413|5|Briefly described|p82 Fig.103.|Early Silurian|Early Silurian|||||Overlies Gungoandra Siltstone. Is unconformably overlain by Bredbo Group.|Turbidites.|
16491|Ryrie Formation|61895|6|Mentioned|p134 Fig.1,|||||||||
16491|Ryrie Formation|71069|6|Mentioned|p77|Early Silurian|Early Silurian|||||Conformably overlies the Gungoandra Siltstone.||
16491|Ryrie Formation|73264|6|Mentioned|p1392 Fig.14|||||||||
16495|Saddle Tuff|22857|5|Briefly described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Boraig Group. Rhyolitic tuff, conglomerate. Max. thickness: 270m. Geological Province: Bogan Gate Terrace.||||||
16495|Saddle Tuff|29648|6|Mentioned|p25|||||||||
16495|Saddle Tuff|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
16495|Saddle Tuff|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
16495|Saddle Tuff|33732|5|Briefly described|p111|||Boraig Gp.||||||
16495|Saddle Tuff|34403|4|Described|p144|||||||||
16495|Saddle Tuff|34405|6|Mentioned|Fig.3.15|||||||||
16495|Saddle Tuff|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
16495|Saddle Tuff|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Boraig Group.||||||
16499|Saddleback Mountain Agglomerate|36220|5|Briefly described|p95|||||||||
16499|Saddleback Mountain Agglomerate|36223|6|Mentioned|Map legend|Late Triassic|Late Triassic|Post Late Triassic.||||||
16499|Saddleback Mountain Agglomerate|43346|2|Defined|p4 Map|||See also Lexicon||||||
16499|Saddleback Mountain Agglomerate|43349|14|Not recorded|Map|||||||||
16535|Saint Heliers Coal Member|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
16535|Saint Heliers Coal Member|40331|6|Mentioned|p13|||||||||
16535|Saint Heliers Coal Member|70791|5|Briefly described|p293 Fig.17|Permian|Permian|Muswellbrook area.||Rowan Formation. ||||
16576|Sams Road Rhyolite Member|22601|6|Mentioned|407|Visean|Visean|Overlying unit Burdekin Basalt Member||||||
16576|Sams Road Rhyolite Member|42833|2|Defined|p225, p227|Early Permian||of Alum Mountain Volcanics||||||
16593|Sandgate Seam Lower|42182|6|Mentioned|p297|||||||||
16597|Sandhills Creek Limestone Member|22768|6|Mentioned|p176|||||||||
16597|Sandhills Creek Limestone Member|22857|5|Briefly described|p176, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of the De Drack Formation (Mount Fairy Group). Contains corals. Max. thickness: 200m.||||||
16597|Sandhills Creek Limestone Member|30735|4|Described|p19|||||||||
16597|Sandhills Creek Limestone Member|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
16597|Sandhills Creek Limestone Member|31411|5|Briefly described|p16|||||||||
16597|Sandhills Creek Limestone Member|32820|6|Mentioned|Table 1|||Refers Felton and Huleatt (in press)||||||
16597|Sandhills Creek Limestone Member|34713|6|Mentioned|p118|||||||||
16597|Sandhills Creek Limestone Member|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
16597|Sandhills Creek Limestone Member|36413|6|Mentioned|Table 3|||||||||
16597|Sandhills Creek Limestone Member|37727|6|Mentioned|p54|||||||||
16597|Sandhills Creek Limestone Member|40328|6|Mentioned|p184|||||||||
16597|Sandhills Creek Limestone Member|68592|5|Briefly described|p725 Fig.130, p760-1, p778|||Defined on Braidwood 1:100 000; Felton and Huleatt 1976. See also abbreviated Sandhills Limestone Member (p778).||Unit in De Drack Formation.||Kingsdale Limestone Member is a correlative.|Limestone.|
16597|Sandhills Creek Limestone Member|69159|5|Briefly described|Map legend|Ludlow|Wenlock|||Unit in De Drack Formation.|||Bedded to massive fossiliferous limestone.|07-SEP-15
16597|Sandhills Creek Limestone Member|71069|6|Mentioned|p25, p40 fig 17, p143, p146, p149-p151|||Contains brachiopod fossils that are assigned to the Conchidium sp. also contains conodonts and coniform fossils. Quarried for limestone.||De Drack Formation||||
16597|Sandhills Creek Limestone Member|71699|5|Briefly described|Map legend.|Devonian|Silurian|||De Drack Formation.|||Bedded to massive, variably fossiliferous limestone.|
16597|Sandhills Creek Limestone Member|71700|2|Defined|vi, p14, CD|Pridoli|Wenlock|Named for the Sandhills Creek which traverses this limestone south of Mount Fairy Trigonometrical Station. The type section is located in Caves Creek and Sandhills Creek between 737813 6102184 and GR 737713 6102884. This unit was previously included in the "Fairy Meadow Limestones" of Carne and Jones (1919). Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features, economic geology and hazards are discussed. This united is estimated to be at maximum up to 250m thick.  Age derived from fossil conodont assemblage.||De Drack Formation||Overlies and interfingers with the De Drack Formation. Equivalent to the Kingsdale Limestone Member.|Grey to blue-grey, massive to bedded, micrite and biomicritic limestones that is variably dolomitized. Cross-bedded calc-arenite has also been identified.|
16599|Sandmount sand|39512|6|Mentioned|p2|||||||||
16624|Sara beds|22490|5|Briefly described|7 fig 2|||||||||
16624|Sara beds|22857|6|Mentioned|p516 App.1 Tb.A1.8|Permian||Siliceous mudstone, siltstone and lithic wacke; minor orthoconglomerate; rare metabasalt and felsic volcanics.||||||
16624|Sara beds|23720|5|Briefly described|Map Legend|||Siliceous mudstone, siltstone and lithic wacke, minor orthoconglomerate, rare metabasalt and felsic volcanics.||||||15-DEC-04
16624|Sara beds|23811|5|Briefly described|Map Legend|Sakmarian|Tournaisian|Undifferentiated metasediments: folaited metaclaystone, metasiltstone, and lithic wacke, minor orthoconglomerate, rare chert, metabasalt and felsic volcanic rocks.||||||20-DEC-04
16624|Sara beds|23812|4|Described|p14, p11 Tb.1|Early Permian|Early Permian|Possibly equivalent to the "Coffs Harbour Association".||||||
16624|Sara beds|42866|5|Briefly described|Table 2, P12|||variation of Sara Beds||||||
16624|Sara beds|43017|5|Briefly described|Fig.2,p374|||||||||
16624|Sara beds|44450|4|Described|p18 Table 3|Late Carboniferous|Late Carboniferous|Geological Province: Dyamberin Block.||||||
16624|Sara beds|60079|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Hillgrove Suite.||||||
16624|Sara beds|71628|5|Briefly described|p3: 5, 52, 71; p8-92; p11: 16, 21|Carboniferous|Carboniferous|See also p14: 7, 16; p19: 12, 138. RELATED UNITS (continued): Is faulted against Black Knob Monzogranite and Newton Boyd Granodiorite. Abuts Wards Mistake Monzogranite and Kingsgate Syenogranite.||||Intruded by Black Knob, Henry River, Kookabookra Monzogranites, Oban River Leucomonzogranite, and Bruisers Creek Granodiorite Phase (of Mount Mitchell Monzogranite). See COMMENTS for more.|Foliated and metamorphosed claystone, siltstone and lithic greywacke; minor orthoconglomerate; rare chert, metabasalt and felsic volcanic rocks.|
16630|Sarona Downs Tuff Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Ash flow unit. Max. thickness: 250m. Geological Province: Kopyje Shelf (Darling Basin).||||||
16630|Sarona Downs Tuff Member|23171|5|Briefly described|p31,36,Fig11p37|||||||||
16630|Sarona Downs Tuff Member|23173|6|Mentioned|Map Legend|||||||||
16630|Sarona Downs Tuff Member|35287|6|Mentioned|p7|||||||||
16630|Sarona Downs Tuff Member|39618|2|Defined|p53|Early Devonian|Early Devonian|||||||
16630|Sarona Downs Tuff Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
16649|Sawpitt Granite|42726|5|Briefly described|map legend|Carboniferous||26. Not a variation on Sawpit Granodiorite, Tonalite Qld.||||||
16653|Says Hill Quartz-Orthoclase Porphyry|38915|6|Mentioned|p338|||||||||
16663|Scarborough Sandstone|22549|6|Mentioned|p526||Late Permian|||||||
16663|Scarborough Sandstone|22745|6|Mentioned|p129|||Sydney Basin.||||||
16663|Scarborough Sandstone|22857|5|Briefly described|p530 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Quartz-lithic sandstone, pebbly in parts. Max. thickness: ~24m. Geological Province: Sydney Basin.||||||
16663|Scarborough Sandstone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
16663|Scarborough Sandstone|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
16663|Scarborough Sandstone|29901|4|Described|Table 1|||||||||
16663|Scarborough Sandstone|30006|4|Described|p57|||||||||
16663|Scarborough Sandstone|30007|6|Mentioned|p61|||||||||
16663|Scarborough Sandstone|30132|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|31061|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|31128|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|31276|6|Mentioned|p147|||Palynology||||||
16663|Scarborough Sandstone|31297|6|Mentioned|Fig. 3|||||||||
16663|Scarborough Sandstone|31426|6|Mentioned|Fig.1|||||||||
16663|Scarborough Sandstone|31725|6|Mentioned|p10|||On table||||||
16663|Scarborough Sandstone|31878|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|31884|6|Mentioned|Table 1|||Triassic||||||
16663|Scarborough Sandstone|31886|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|31887|5|Briefly described|p8|||||||||
16663|Scarborough Sandstone|32801|6|Mentioned|Fig.10|||||||||
16663|Scarborough Sandstone|32998|6|Mentioned|p113|||Zones of rich gas||||||
16663|Scarborough Sandstone|33683|4|Described|Table 1|||Grose sst. unit.||||||
16663|Scarborough Sandstone|33685|6|Mentioned|Table 2|||||||||
16663|Scarborough Sandstone|33867|6|Mentioned|Table 1|||||||||
16663|Scarborough Sandstone|34009|6|Mentioned|Table III|||||||||
16663|Scarborough Sandstone|34058|5|Briefly described|p395|||Triassic||||||
16663|Scarborough Sandstone|34139|6|Mentioned|p23|||||||||
16663|Scarborough Sandstone|34205|4|Described|Table 1|||See P169.||||||
16663|Scarborough Sandstone|34236|6|Mentioned|p17|||||||||
16663|Scarborough Sandstone|34241|6|Mentioned|p404|||||||||
16663|Scarborough Sandstone|34336|6|Mentioned|Table 5.15|||||||||
16663|Scarborough Sandstone|34337|5|Briefly described|Table 5.18|||||||||
16663|Scarborough Sandstone|36042|6|Mentioned|Fig.22|||||||||
16663|Scarborough Sandstone|36220|4|Described|p67|||See also P65.||||||
16663|Scarborough Sandstone|36222|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
16663|Scarborough Sandstone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
16663|Scarborough Sandstone|36594|6|Mentioned|Table 1|||See also Table II.||||||
16663|Scarborough Sandstone|37168|6|Mentioned|p231|||||||||
16663|Scarborough Sandstone|37722|6|Mentioned|p23|||||||||
16663|Scarborough Sandstone|39287|6|Mentioned|Fig. 2.18|||||||||
16663|Scarborough Sandstone|39293|6|Mentioned|p146|||||||||
16663|Scarborough Sandstone|39296|6|Mentioned|p179|||||||||
16663|Scarborough Sandstone|39306|6|Mentioned|p406|||See also P410||||||
16663|Scarborough Sandstone|39450|6|Mentioned|Fig.4|||||||||
16663|Scarborough Sandstone|40516|6|Mentioned|Fig.3|||||||||
16663|Scarborough Sandstone|40602|5|Briefly described|Table 1|||||||||
16663|Scarborough Sandstone|40625|6|Mentioned|Map legend|Early Triassic|Late Permian|Late Permian to Early Triassic||||||
16663|Scarborough Sandstone|40652|6|Mentioned|p128|||||||||
16663|Scarborough Sandstone|42737|5|Briefly described|map legend|Triassic||||||||
16663|Scarborough Sandstone|42787|5|Briefly described|p134|||||||||
16663|Scarborough Sandstone|42896|3|Fully described|p27, Table 2|||of Clifton Subgroup||||||
16663|Scarborough Sandstone|42925|5|Briefly described|Table 18||Early Triassic|||||||
16663|Scarborough Sandstone|42926|4|Described|map legend||Early Triassic|||||||
16663|Scarborough Sandstone|43028|6|Mentioned|Fig.7,p618|||actually spelt Scarbo'h SST||||||
16663|Scarborough Sandstone|43194|5|Briefly described|p130|Triassic|Triassic|Sandy alluvial outwash material deposited in the southern Sydney Basin.||||||
16663|Scarborough Sandstone|43344|14|Not recorded|p21,69|||||||||
16663|Scarborough Sandstone|43383|14|Not recorded|p22|||Part of Clifton Sub-Group||||||
16663|Scarborough Sandstone|43395|14|Not recorded|p76|||||||||
16663|Scarborough Sandstone|45090|6|Mentioned|p71|||Narrabeen Gp.||||||
16663|Scarborough Sandstone|61315|5|Briefly described|Table SY2|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
16663|Scarborough Sandstone|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Narrabeen Group.||Overlies Wombarra Claystone. Is overlain by Stanwell Park Claystone.||
16663|Scarborough Sandstone|67560|5|Briefly described|p258, p260-p272|Triassic|Triassic|Constrained by the age of the Narrabeen Group.||Of the Narrabeen Group.||Overlain by the Stanwell Park Claystone. Underlain by the Wombarra Shale.|Coarse to conglomeratic sandstones, dark grey(-green) shales.|23-MAY-17
16663|Scarborough Sandstone|68003|5|Briefly described|p42.|Triassic|Triassic|Southern Sydney Basin.|||||Fine-grained sandstone with interbedded shale units.|
16663|Scarborough Sandstone|68202|6|Mentioned|p176|Triassic|Triassic|Sydney Basin.||Narrabeen Group.||||
16663|Scarborough Sandstone|73304|6|Mentioned|p61, p72, p74, p76, p78|||Sydney Basin, southern. Correlates to the GSSP-defined P-T boundary based on bracketing tuff ages.||Narrabeen Group||||
16688|Scotts Head Leucoadamellite|38842|6|Mentioned|p286|||||||||
16692|Scrub Mountain Conglomerate Member|34080|6|Mentioned|p248|||||||||
16692|Scrub Mountain Conglomerate Member|34555|5|Briefly described|p241|||||||||
16692|Scrub Mountain Conglomerate Member|39331|6|Mentioned|Table 10-1|||||||||
16692|Scrub Mountain Conglomerate Member|43399|2|Defined|p195-197,201,205||Early Carboniferous|Member of Goonoo Goonoo Mudstone(Early Lower Carb.) (Parry Gp)||||||
16692|Scrub Mountain Conglomerate Member|43400|14|Not recorded|map opp.p.188||Early Carboniferous|||||||
16692|Scrub Mountain Conglomerate Member|43406|14|Not recorded|p42,44||Tournaisian|||||||
16708|Seaham Formation|22736|6|Mentioned|p629|||||||||
16708|Seaham Formation|22857|4|Described|p506 App.1 Tb.A1.8|Westphalian|Namurian|Equivalent to "Pokolbin Hills Vocanics" and tuffs at Lochinvar. Age: 309+/-3Ma, 310.6+/-4Ma (on "Pokolbin Volcanics"). Max. thickness: 600m. Geological Province: Tamworth Forearc Basin. See also p508 App.1 Tb.A1.8.||||||14-DEC-07
16708|Seaham Formation|22969|6|Mentioned|p 9|||||||||
16708|Seaham Formation|23540|5|Briefly described|Fig 3 p 420|||||||||
16708|Seaham Formation|24079|5|Briefly described|p430|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||
16708|Seaham Formation|24121|5|Briefly described|p4, p144|||||||||25-AUG-22
16708|Seaham Formation|24423|5|Briefly described|p230 Fig.3|Carboniferous|Carboniferous|Geological Province: Sydney Basin (??!!)||||||20-JUN-12
16708|Seaham Formation|24603|5|Briefly described|p898|Carboniferous|Carboniferous|Contains the Mirannie Ignimbrite Member the age of which is 321.3+/-4.4Ma (Roberts et al, 1995b).  Geological Province: Tamworth Belt.||||||
16708|Seaham Formation|29752|6|Mentioned|p36|||||||||
16708|Seaham Formation|29915|3|Fully described|p67|||||||||
16708|Seaham Formation|30340|6|Mentioned|Fig.13|||Lithology||||||
16708|Seaham Formation|30341|4|Described|p137|||Carboniferous age||||||
16708|Seaham Formation|31081|6|Mentioned|p54|||See also Fig. 2||||||
16708|Seaham Formation|31228|3|Fully described|p84|||||||||
16708|Seaham Formation|31277|6|Mentioned|p4|||||||||
16708|Seaham Formation|31298|6|Mentioned|p9|||See also P11, 14. U.Carboniferous||||||
16708|Seaham Formation|31706|6|Mentioned|p653|||U.Carb. correlation chart||||||
16708|Seaham Formation|31883|6|Mentioned|Table 1|||||||||
16708|Seaham Formation|32094|6|Mentioned|p382|||||||||
16708|Seaham Formation|32379|6|Mentioned|p5|||||||||
16708|Seaham Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16708|Seaham Formation|32672|6|Mentioned|p674|||||||||
16708|Seaham Formation|32836|6|Mentioned|p5|||See also P7 and Table 1||||||
16708|Seaham Formation|32868|6|Mentioned|p202|||||||||
16708|Seaham Formation|33584|6|Mentioned|p27|||Overlies Paterson Toscanite||||||
16708|Seaham Formation|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16708|Seaham Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
16708|Seaham Formation|34085|6|Mentioned|Cor.chart|||Stephanian||||||
16708|Seaham Formation|34169|4|Described|Fig.4.6|||Stratigraphic column.||||||
16708|Seaham Formation|34237|6|Mentioned|p69|||Late Carboniferous. See P70.||||||
16708|Seaham Formation|34238|6|Mentioned|p5|||See also P10||||||
16708|Seaham Formation|34239|6|Mentioned|p264|||Microflora||||||
16708|Seaham Formation|34330|6|Mentioned|p63|||Permian||||||
16708|Seaham Formation|34444|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
16708|Seaham Formation|34445|6|Mentioned|p319|||||||||
16708|Seaham Formation|35268|6|Mentioned|p21|||||||||
16708|Seaham Formation|35284|6|Mentioned|Fig.12|||||||||
16708|Seaham Formation|35380|5|Briefly described|p190|||Also P191, discussion of glacial features.||||||
16708|Seaham Formation|35862|6|Mentioned|p274|||||||||
16708|Seaham Formation|36042|6|Mentioned|Table 1|||||||||
16708|Seaham Formation|36045|6|Mentioned|p329|||||||||
16708|Seaham Formation|36253|6|Mentioned|p130|||||||||
16708|Seaham Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
16708|Seaham Formation|36528|6|Mentioned|p182|||||||||
16708|Seaham Formation|36596|6|Mentioned|Text Fig.2|||||||||
16708|Seaham Formation|36718|6|Mentioned|p460|||||||||
16708|Seaham Formation|37068|6|Mentioned|p58|||||||||
16708|Seaham Formation|37086|6|Mentioned|p185|||||||||
16708|Seaham Formation|37922|3|Fully described|p480|||||||||
16708|Seaham Formation|37926|6|Mentioned|p499|||See also P500.||||||
16708|Seaham Formation|38217|6|Mentioned|p272|||||||||
16708|Seaham Formation|38801|6|Mentioned|Fig.3|||||||||
16708|Seaham Formation|38837|6|Mentioned|p232|||||||||
16708|Seaham Formation|39287|6|Mentioned|Fig. 2.2|||See also Fig.2.5||||||
16708|Seaham Formation|39288|6|Mentioned|Fig. 3.3|||||||||
16708|Seaham Formation|39290|6|Mentioned|p84|||Correlation||||||
16708|Seaham Formation|39292|6|Mentioned|Fig. 6.1|||||||||
16708|Seaham Formation|39299|5|Briefly described|p281|||||||||
16708|Seaham Formation|39302|5|Briefly described|p343|||||||||
16708|Seaham Formation|39304|6|Mentioned|Fig. 19.2|||||||||
16708|Seaham Formation|39306|6|Mentioned|p387|||See also P397||||||
16708|Seaham Formation|39308|6|Mentioned|p482|||||||||
16708|Seaham Formation|40883|6|Mentioned|p14|||||||||
16708|Seaham Formation|41689|6|Mentioned|Table 1|||||||||
16708|Seaham Formation|41902|5|Briefly described|p5 Table 1|||||||||
16708|Seaham Formation|42214|5|Briefly described|p466|||||||||
16708|Seaham Formation|42547|4|Described|p33|||||||||
16708|Seaham Formation|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Late Carboniferous|Newcastle and Hunter regions, Sydney Basin. Fluvio-lacustrine sediments.||||||
16708|Seaham Formation|43383|14|Not recorded|p18|||||||||
16708|Seaham Formation|43447|4|Described|Table 1&2,p10,11,15||Carboniferous|||||||
16708|Seaham Formation|43479|14|Not recorded|p159,177|Stephanian|Westphalian|||||||
16708|Seaham Formation|43576|6|Mentioned|Fig.1,p348||Late Carboniferous|||||||
16708|Seaham Formation|43755|6|Mentioned|p557|||||||||
16708|Seaham Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
16708|Seaham Formation|44093|5|Briefly described|p228 App. 1|Late Carboniferous|Early Carboniferous|Geological Province: New England Fold Belt.||||||29-MAR-05
16708|Seaham Formation|44244|2|Defined|p102|Early Permian|Late Carboniferous|Includes the Mirannie Volcanic Member.  Overlies the Gilmore Volcanic Group and Paterson Volcanics.||||||
16708|Seaham Formation|44450|5|Briefly described|p147 Fig 43|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||
16708|Seaham Formation|44833|14|Not recorded|p108|||See also Lexicon (renaming of Seaham Glacial Beds) Early Carboniferous faunal units.||||||
16708|Seaham Formation|45090|4|Described|p25|||Stratigraphic table||||||
16708|Seaham Formation|45097|5|Briefly described|p18|||See also P24, 28 & Correlation chart. Microflora||||||
16708|Seaham Formation|46849|6|Mentioned|p195|||||||||
16708|Seaham Formation|47041|6|Mentioned|p163|||||||||
16708|Seaham Formation|47056|6|Mentioned|Fig.2 P523|||||||||
16708|Seaham Formation|48995|6|Mentioned|p12|||||||||
16708|Seaham Formation|50268|5|Briefly described|Map Legend|Stephanian|Stephanian|Overlies: Paterson Volcanics, Mount Johnstone Formation.  Includes: Mirannie Volcanic Member.  Geological Province: Rouchel and Gresford Blocks.||||||
16708|Seaham Formation|60281|6|Mentioned|p53 App. 1|||Geological Province: New England Fold Belt.||||||
16708|Seaham Formation|60289|5|Briefly described|p2 Fig. 2|Late Carboniferous|Late Carboniferous|Includes Mount Durham Tuff Member. Underlies Tamby Creek Formation. Geological Province: Cranky Corner Basin.||||||
16708|Seaham Formation|60290|3|Fully described|p16, 17, 37|Late Carboniferous|Late Carboniferous|Overlies Paterson Vols. Overlain; Tamby Creek Fm. Conglom, vol conglom, sst, siltst, clayst, tuff + ignimbrite. Interpreted as pyroclastic deposition + reworking on an alluvial plain + braided river system. Geol Prov: Cranky Corner Basin.||||||07-FEB-11
16708|Seaham Formation|60291|4|Described|p51, 53 Tb.1|Late Carboniferous|Late Carboniferous|Ignombrite, volcanics sandstone, siltstone, conglomerate, reworked tuff. Braided fluvial to alluvial plain blanket of welded tuff. Petrology descirbed.||||||
16708|Seaham Formation|60292|4|Described|p65, p90 Fig.6|Late Carboniferous|Late Carboniferous|Overlain by Tamby Creek Formation. Geological Province: Cranky Corner Basin. Petrography and geochemistry described.||||||
16708|Seaham Formation|60293|5|Briefly described|p107, p108 Fig.1|||Overlain by Tamby Creek Formation. Vitrinite reflectance of organic matter described.||||||
16708|Seaham Formation|60294|5|Briefly described|p115, p116 Fig.1|Late Carboniferous|Late Carboniferous|Overlain by Tamby Creek Formation. Contains hydrocarbon source rock potential. Geological Province: Cranky Corner Basin.||||||18-MAY-05
16708|Seaham Formation|60295|4|Described|p127, p133 Fig.9, p134|Stephanian||Of Dalwood Group. Overlain by Tamby Creek Formation. Plant microfossils indicate low-energy, open-water and non-marine brackish environment of deposition. Geological Province: Cranky Corner Basin.||||||
16708|Seaham Formation|60296|5|Briefly described|p155, p156 Fig.1|Carboniferous|Carboniferous|Geological Province: Cranky Corner Basin.||||||
16708|Seaham Formation|60297|5|Briefly described|p167|Carboniferous|Carboniferous|Geological Province: Cranky Corner Basin.||||||
16708|Seaham Formation|60298|5|Briefly described|p180|Late Carboniferous|Late Carboniferous|Silt to sand, and rarely conglomerate, sized sedimentary rocks with pervasive reworked volcanic detritus.||||||
16708|Seaham Formation|60299|5|Briefly described|p207, 218|||Palaeomagnetism measured.||||||
16708|Seaham Formation|60300|5|Briefly described|p241|Carboniferous|Carboniferous|Overlain by the Dalwood Group. Geological Province: Cranky Corner Basin.||||||
16708|Seaham Formation|61612|6|Mentioned|p270, p270 Fig. 1|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||17-MAR-09
16708|Seaham Formation|61768|6|Mentioned|p82, p83 Fig. 2|||Includes Mirannie Ignimbrite. Underlain by Paterson Volcanics.||||||13-MAY-08
16708|Seaham Formation|61770|6|Mentioned|p108|||||||||
16708|Seaham Formation|62095|1|Redefined|p281 Appdx.|Westphalian|Namurian|Includes Kewell Creek Volc.Mbr, Well Gully, Elmswood and Mirannie Ig. Mbrs.  Redef.of former Seaham Fm. of Sussmilch and David (1920) and Roberts et al (1991) which replaced Grahamstown lake Fm.  Disconformable over Isismurra Fm; overlies Pokolbin Hills V||||||20-JUN-12
16708|Seaham Formation|63832|4|Described|p131 fig 2, p134-135|Kasimovian|Serpukhovian|Rouchel Block and Cranky Corner/Gresford Block, southern New England Fold Belt. Type section is at Seaham village (Sussmilch and David, 1919; Roberts et al., 1991). Deposition spanned the second (C2) to fourth (C4) glaciations.||||Is overlain by Tamby Creek Formation.|Composed largely of fluvial conglomerates. Lower part contains an interval of outsize clast-bearing, rhythmically laminated mudrocks.|14-DEC-17
16708|Seaham Formation|64631|5|Briefly described|p44 Fig.2, p47, p49, p54.|Kazimovian|Serpukhovian|Southern New England Fold Belt, Rouchel Block and Cranky Corner/Gresford Block. Some biostratigraphic and radiometric age control within unit.||||Is overlain by Tamby Creek Formation.|Conglomerate, sandstone, siltstone; contains an interval of outsized clast-bearing, rhythmically-laminated mudrocks.|
16708|Seaham Formation|65107|6|Mentioned|p276|Upper Pennsylvanian|Upper Pennsylvanian|Gresford Block. Includes the Mount Durham Tuff Member.||||||
16708|Seaham Formation|67029|5|Briefly described|p377-87|Gzhelian|Serpukhovian|Recognised in Rouchel and Gresford Blocks of Tamworth Belt, New England Orogen. Thickness at type section: ~600m. Magnetic properties of varves at Abercrombie Quarry are presented. In part previously Grahamstown Lake Formation (Rattigan, 1967). Age in text is Late Carboniferous - Stephanian to Namurian (Roberts et al. 2006).|||||Fluvioglacial conglomerates, tillites and varved shales, interbedded with sandstones and horizons of tuffs and volcanic agglomerates. Dropstones, soft sediment folding in varved shales (Sussmilch & David, 1920). Varves inferred of annual periodicity.|24-APR-12
16708|Seaham Formation|67663|6|Mentioned|p518, p520 Tb.1|Late Carboniferous|Late Carboniferous|Northern Sydney Basin.||||Overlain by the Dalwood Group.|Includes conglomerates.|
16708|Seaham Formation|68003|5|Briefly described|p32 Fig.3-h, p38 Fig.3-j, p40, p136.|Early Permian|Namurian|Tamworth Belt (South), New England Fold Belt, and Hunter Coalfield; Brigalow Belt South Bioregion. Lower part is coeval with Currabubula Formation, and Willuri Formation to the north. Fluvio-lacustrine sediments.|||Includes Kewell Creek Volcanics.|Is overlain by Dalwood Group.|Tillite, varved siltstones, tuff, red and green zeolitic mudstone with dropstones interbedded within thick bedded lithic sandstone and conglomerate.|
16708|Seaham Formation|68004|5|Briefly described|p23 Table 1. |||Hunter and Newcastle Coalfields.||||Is overlain by Lochinvar Formation (of the Dalwood Group) and (in the Hunter Coalfield) Gyarran Volcanics.||
16708|Seaham Formation|68005|5|Briefly described|p49 Fig.3-M, p57, p170.|Stephanian|Namurian|Rouchel Block, Tamworth Belt.|||||Tuff, felsic-ignimbrite, conglomerate, sandstone, siltstone and mudstone.|
16708|Seaham Formation|68493|6|Mentioned|p5|Permian||Conformably underlies the Permian succession. Cranky Corner Basin.||||||
16708|Seaham Formation|69297|6|Mentioned|p501|Moscovian|Serpukhovian|Sydney Basin.|327-308 Ma|||Unconformably overlies the Paterson Volcanics. Unconformably overlain by the Dalwood Group.||
16708|Seaham Formation|69793|6|Mentioned|p1121 Fig.12|Gzhelian|Serpukhovian|Rouchel and Gresford Blocks, Tamworth Belt.||||||
16708|Seaham Formation|70777|5|Briefly described|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.|||Includes the Kewell Creek Volcanic Member, Well Gully Ignimbrite Member, Elmswood Ignimbrite Member and the Mirannie Ignimbrite Member.|||
16708|Seaham Formation|70791|6|Mentioned|p277|Cisuralian||Hunter Coalfield.||||||
16708|Seaham Formation|71233|5|Briefly described|p116|Carboniferous|Carboniferous|Basal portion contains the Potonieisporites Microflora (Helby).||||Lateral equivalent of the Grahamstown Lake Formation.||
16708|Seaham Formation|73146|5|Briefly described|p15|Carboniferous|Carboniferous|Southern New England Orogen. Has magnetic overprinting with a uniformly normal polarity and steep inclination.|||||Varved siltstones; chert.|
16708|Seaham Formation|73304|6|Mentioned|p75|||||||||
16751|Sentry Box Granite|42726|5|Briefly described|map legend|Silurian||||||||
16751|Sentry Box Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Massive to foliated? porphyritic hornblende-biotite soda-granite.||||||
16751|Sentry Box Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Burrawinda Suite. Massive to foliated? porphyritic hornblende-biotite granite.||||||
16751|Sentry Box Granite|68592|2|Defined|p1354-5, p1358, p1368-70|Late Silurian|Early Silurian|Originally named Sentry Box Adamellite by Yacopetti (1987) after a local name for a shepherds' shelter. Included in Chappell et al. (1991). Renamed to accord with standard nomenclature for plutonic rocks. A small pluton (4 km2); type locality described. Geochemistry and geophysical properties described. Not isotopically dated; age from stratigraphic relationships.||Unit in Burrawinda Suite.||Intrudes Adaminaby Group. Is intruded by Yewrangara Granite.|Grey, medium- to coarse-grained, generally massive, equigranular to sparsely porphyritic, biotite granite; contains a few minor aplite veins; mild meridional foliation dips W. Has undergone low to moderate greenschist facies metamorphism. S-type.|
16751|Sentry Box Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sws. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Burrawinda Suite|||Medium-coarse grained, generally massive,equigranular to sparsely porphyritic biotite granite with minor aplite veins. High K and medium-high Th response.|
16751|Sentry Box Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Medium-coarse grained, generally massive,equigranular to sparsely porphyritic biotite granite with minor aplite veins. High K and medium-high Th response.|
16753|Separovitch pegmatite|39652|6|Mentioned|p105|||||||||
16765|Serpentine Creek Sandstone|23229|5|Briefly described|Table3-3p27|Wenlock|Llandovery|||||||
16765|Serpentine Creek Sandstone|23309|5|Briefly described|p142-146, 155, 274-275, Table 2.54||Llandovery|||||||
16765|Serpentine Creek Sandstone|24177|5|Briefly described|p50 Fig.22|Early Silurian|Early Silurian|Geological Province: Mount Easton Province.||||||
16765|Serpentine Creek Sandstone|24214|6|Mentioned|p788 Fig. 2|||||||||
16765|Serpentine Creek Sandstone|24551|5|Briefly described|p33, 88 Fig. 3.15|Silurian|Early Silurian|Of Jordan River Group. See also page 123.||||||23-JUN-14
16765|Serpentine Creek Sandstone|29709|4|Described|p33|||||||||
16765|Serpentine Creek Sandstone|33601|6|Mentioned|p5|||||||||
16765|Serpentine Creek Sandstone|34843|6|Mentioned|p5|||||||||
16765|Serpentine Creek Sandstone|35112|6|Mentioned|p280|||||||||
16765|Serpentine Creek Sandstone|35281|6|Mentioned|p16|||||||||
16765|Serpentine Creek Sandstone|36534|6|Mentioned|p222|||||||||
16765|Serpentine Creek Sandstone|41571|6|Mentioned|Fig.2.6|||||||||
16765|Serpentine Creek Sandstone|41585|4|Described|p118|||||||||
16765|Serpentine Creek Sandstone|42827|4|Described|p118|||see also Table 4.1||||||
16765|Serpentine Creek Sandstone|44187|5|Briefly described|Map Legend||Early Silurian|||||||
16765|Serpentine Creek Sandstone|60599|5|Briefly described|p47 Fig. 19|Wenlock|Llandovery|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
16765|Serpentine Creek Sandstone|64535|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; contains Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||
16765|Serpentine Creek Sandstone|64536|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||07-FEB-11
16765|Serpentine Creek Sandstone|64537|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||07-FEB-11
16765|Serpentine Creek Sandstone|64538|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||07-FEB-11
16765|Serpentine Creek Sandstone|64539|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; contains Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||
16765|Serpentine Creek Sandstone|64540|5|Briefly described|Map legend|Silurian|Silurian|Of Jordan River Group. Thick to thin bedded, coarse- to fine-grained sandstone; contains Tabc, Tbc and Tc turbidites; siltstone is laminated and bioturbated; deep marine turbidite fan deposits.||||||
16765|Serpentine Creek Sandstone|64605|5|Briefly described|Map legend|Silurian|Silurian|Of the Jordan River Group. Sandstone, siltstone; deep-marine deposits. Speckled blue-pink to brown in RGB. Nonmagnetic.||||||17-NOV-08
16765|Serpentine Creek Sandstone|64606|5|Briefly described|Map Legend|Silurian|Silurian|Of Jordan River Group. Sandstone, siltstone: deep-marine deposits. Speckled blue-pink to brown in RGB. Nonmagnetic.||||||11-NOV-08
16765|Serpentine Creek Sandstone|64616|4|Described|p77, p184-185, p189, p306|Llandovery|Llandovery|Of Jordan River Group. In faulted contact with Donnellys Creek Siltstone and conformably overlain by Murderers Hill Siltstone. 610-1250m thick. Medium and thick-bedded quartz sandstone turbidites dominate; laminated and bioturbated siltstone. Age inferred, correlated with McAdam Sandstone. Geophysical characteristics given.||||||
16765|Serpentine Creek Sandstone|68116|5|Briefly described|Appendix, Maps 34, 43, 52.|Telychian|Aeronian||||||Sandstone, siltstone: sandstone thick to thin-bedded, coarse to fine-grained, turbidites; siltstone: laminated and bioturbated.|
16778|Seventeen Flat Granogabbro|39409|6|Mentioned|Table XVII|||||||||
16803|Shannons Flat Granodiorite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Foliated contaminated granodiorite. BMR map symbol: gmn.||||||
16803|Shannons Flat Granodiorite|23551|5|Briefly described|p491|||Of Wyangala Supersuite||||||
16803|Shannons Flat Granodiorite|23866|4|Described|p120|||Intrudes the Paddys River Volcanics.  Geological Province: Murrumbidgee Batholith.||||||
16803|Shannons Flat Granodiorite|29953|5|Briefly described|p3|||||||||
16803|Shannons Flat Granodiorite|30332|6|Mentioned|p131|||Rb/Sr age 413+-6m.y.||||||
16803|Shannons Flat Granodiorite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
16803|Shannons Flat Granodiorite|32332|5|Briefly described|p491|||Source of detrital material.||||||
16803|Shannons Flat Granodiorite|34544|4|Described|p185|||||||||
16803|Shannons Flat Granodiorite|36413|6|Mentioned|p82|||||||||
16803|Shannons Flat Granodiorite|37728|6|Mentioned|Table 4|||Now known as Shannons Flat Adamellite||||||
16803|Shannons Flat Granodiorite|45003|14|Not recorded|p45,46|||||||||
16803|Shannons Flat Granodiorite|48894|6|Mentioned|p5|||Age||||||
16813|Shaw beds|35118|6|Mentioned|p436|||||||||
16822|Shepherds Hill Formation|22578|6|Mentioned|p401|||||||||
16822|Shepherds Hill Formation|23055|6|Mentioned|Fig5p12|||||||||
16822|Shepherds Hill Formation|29922|6|Mentioned|Appendix 4|||||||||
16822|Shepherds Hill Formation|29926|6|Mentioned|Fig.3|||||||||
16822|Shepherds Hill Formation|29942|4|Described|Fig.2|||Permian||||||
16822|Shepherds Hill Formation|34351|5|Briefly described|p343|||Fig.5.13||||||
16822|Shepherds Hill Formation|37083|6|Mentioned|p164|||||||||
16822|Shepherds Hill Formation|39292|6|Mentioned|Fig.6.2|||||||||
16822|Shepherds Hill Formation|39308|6|Mentioned|Fig. 23.4|||||||||
16822|Shepherds Hill Formation|39609|5|Briefly described|p4|||||||||
16822|Shepherds Hill Formation|41479|6|Mentioned|Fig.2|||||||||
16822|Shepherds Hill Formation|42767|6|Mentioned|p5|||||||||
16822|Shepherds Hill Formation|43447|14|Not recorded|diag.p26,34|||Part of Lambton Sub-Group||||||
16822|Shepherds Hill Formation|43448|14|Not recorded|p224||Permian|On table only. Unit of Lambton Subgroup (Newcastle Coal Measures)||||||
16822|Shepherds Hill Formation|45090|6|Mentioned|p186|||Refers McKenzie (1962)||||||
16822|Shepherds Hill Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Lambton Subgroup|Included Nobbys Tuff Member|||
16844|Shoalhaven Group|22488|5|Briefly described|p839 p841||Permian|||||||
16844|Shoalhaven Group|22529|5|Briefly described|4 fig 2, 8|Permian|Permian|Overlain by Illawarra Coal Measures, underlying unit Rylstone Volcanics||||||25-JUN-08
16844|Shoalhaven Group|22545|6|Mentioned|p499, Fig.2||Permian|||||||
16844|Shoalhaven Group|22578|6|Mentioned|p394, Fig.6 p396|||||||||
16844|Shoalhaven Group|22591|5|Briefly described|p 57||Early Permian|Sydney Basin||||||
16844|Shoalhaven Group|22605|5|Briefly described|p 12||Permian|||||||
16844|Shoalhaven Group|22624|6|Mentioned|Fig.4 p679|Permian|Permian|||||||
16844|Shoalhaven Group|22663|5|Briefly described|NSW97 - 1 p2||Early Permian|||||||01-MAR-10
16844|Shoalhaven Group|22857|4|Described|p528 Tb A1.9, p504 Tb A1.8, p532 Tb A1.9|Late Permian|Early Permian|The interpretation of Tye, Fielding and Jones (1996) includes Yadboro, Burrawang and Tallong Conglomerates, and the Badgerys Breccia in this group rather than the Talaterang Group. Max. thickness: 1000m in southern Sydney Basin. Geol. Prov: Sydney Basin.||||||
16844|Shoalhaven Group|22864|6|Mentioned|p263|||||||||
16844|Shoalhaven Group|22969|4|Described|p 19. Fig 2.2|Permian|Permian|||||||
16844|Shoalhaven Group|23043|5|Briefly described|Map Legend|Late Permian|Early Permian|of Sydney Basin.||||||
16844|Shoalhaven Group|23092|5|Briefly described|p627|Permian|Permian|||||||
16844|Shoalhaven Group|23170|2|Defined|p292 Fig.61|Early Permian|Early Permian|geological province:  Sydney Basin.||||||25-JUN-08
16844|Shoalhaven Group|23214|3|Fully described|p265|Late Permian|Early Permian|Geological Province: Sydney Basin. Max. thickness 100m.||||||
16844|Shoalhaven Group|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
16844|Shoalhaven Group|23544|4|Described|Fig 2 p358|||also see p372 + p357.||||||
16844|Shoalhaven Group|23896|4|Described|p249|Permian|Permian|Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|24123|5|Briefly described|p3|||||||||
16844|Shoalhaven Group|24126|5|Briefly described|p201|Permian|Permian|Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|24342|5|Briefly described|p51|Permian|Permian|Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|24471|5|Briefly described|p29 Fig.2|Late Permian|Permian|Conformably overlain by Erins Vale Formation. Geological Province: Sydney Basin.||||||07-FEB-11
16844|Shoalhaven Group|24552|5|Briefly described|p9||Sakmarian|Discnoformably overlies Talaterang Group. Geological Province: Southern Sydney Basin.||||||07-FEB-11
16844|Shoalhaven Group|24581|6|Mentioned|p822|Permian|Permian|Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|29728|6|Mentioned|p394|||||||||
16844|Shoalhaven Group|29748|6|Mentioned|p8|||||||||
16844|Shoalhaven Group|29750|6|Mentioned|p1|||||||||
16844|Shoalhaven Group|29751|6|Mentioned|Fig.3|||||||||
16844|Shoalhaven Group|29752|6|Mentioned|p5|||||||||
16844|Shoalhaven Group|29900|4|Described|Fig.2|||||||||
16844|Shoalhaven Group|29901|6|Mentioned|p163|||||||||
16844|Shoalhaven Group|29922|6|Mentioned|Appendix 1|||||||||
16844|Shoalhaven Group|29989|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|29993|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
16844|Shoalhaven Group|29994|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|30006|4|Described|p6|||||||||
16844|Shoalhaven Group|30228|6|Mentioned|p17|||Lithology. Permian age.||||||
16844|Shoalhaven Group|30329|6|Mentioned|p30|||On table P30||||||
16844|Shoalhaven Group|30340|6|Mentioned|p2528|||Lithology;Palaeogeography||||||
16844|Shoalhaven Group|30341|6|Mentioned|p134|||Permian age||||||
16844|Shoalhaven Group|30707|6|Mentioned|p2|||See also Table 1||||||
16844|Shoalhaven Group|31057|6|Mentioned|p2|||||||||
16844|Shoalhaven Group|31062|4|Described|p477|||See also p478.||||||25-JUN-08
16844|Shoalhaven Group|31081|6|Mentioned|p49|||See also Fig. 2 & P51.||||||
16844|Shoalhaven Group|31128|5|Briefly described|p5|||See also P3.||||||
16844|Shoalhaven Group|31156|6|Mentioned|p29|||Refers silica deposits||||||
16844|Shoalhaven Group|31277|6|Mentioned|p3|||||||||
16844|Shoalhaven Group|31298|6|Mentioned|p12|||||||||
16844|Shoalhaven Group|31802|5|Briefly described|p142|||Stratigraphy & age||||||
16844|Shoalhaven Group|31855|6|Mentioned|p14|||Stratigraphic table||||||
16844|Shoalhaven Group|31879|5|Briefly described|p294|||Permian||||||
16844|Shoalhaven Group|31885|6|Mentioned|p1439|||Table 1||||||
16844|Shoalhaven Group|31887|6|Mentioned|p3|||||||||
16844|Shoalhaven Group|32045|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|32047|6|Mentioned|p4|||||||||
16844|Shoalhaven Group|32126|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|32187|6|Mentioned|p3|||||||||
16844|Shoalhaven Group|32483|6|Mentioned|p4|||Perm. Strat. table 1.||||||
16844|Shoalhaven Group|32485|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
16844|Shoalhaven Group|32671|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|32672|6|Mentioned|p675|||||||||
16844|Shoalhaven Group|32849|6|Mentioned|p7|||Permian||||||
16844|Shoalhaven Group|32945|6|Mentioned|p84|||Permian||||||
16844|Shoalhaven Group|33006|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
16844|Shoalhaven Group|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
16844|Shoalhaven Group|33132|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|33282|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|33325|5|Briefly described|Table 5|||Perm.||||||
16844|Shoalhaven Group|33685|6|Mentioned|Table 1|||Permian||||||
16844|Shoalhaven Group|33867|6|Mentioned|p6|||See also Table 1.||||||
16844|Shoalhaven Group|33869|6|Mentioned|Fig.2|||||||||
16844|Shoalhaven Group|34015|6|Mentioned|p323|||Permian||||||
16844|Shoalhaven Group|34036|6|Mentioned|p434|||||||||
16844|Shoalhaven Group|34038|6|Mentioned|p435|||||||||
16844|Shoalhaven Group|34039|6|Mentioned|p355|||||||||
16844|Shoalhaven Group|34040|6|Mentioned|Table 5.14|||Permian||||||
16844|Shoalhaven Group|34059|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|34084|6|Mentioned|p368|||Perm.||||||
16844|Shoalhaven Group|34130|6|Mentioned|p178|||Permian||||||
16844|Shoalhaven Group|34138|6|Mentioned|Cor.Chart|||Sakmarian - Kazanian||||||
16844|Shoalhaven Group|34156|6|Mentioned|p387|||||||||
16844|Shoalhaven Group|34204|6|Mentioned|p65|||||||||
16844|Shoalhaven Group|34205|3|Fully described|p8|||Previously Capertee Group.||||||25-JUN-08
16844|Shoalhaven Group|34211|6|Mentioned|p32|||||||||
16844|Shoalhaven Group|34292|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|34334|3|Fully described|p357|||See also pp358-366.||||||25-JUN-08
16844|Shoalhaven Group|34335|6|Mentioned|p369|||Permian||||||
16844|Shoalhaven Group|34345|6|Mentioned|p329|||||||||
16844|Shoalhaven Group|34399|6|Mentioned|p312|||||||||
16844|Shoalhaven Group|34404|6|Mentioned|Fig.3.5b|||||||||
16844|Shoalhaven Group|34426|6|Mentioned|p9|||||||||
16844|Shoalhaven Group|34444|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|34451|6|Mentioned|p197|||||||||
16844|Shoalhaven Group|34533|6|Mentioned|p1285|||||||||
16844|Shoalhaven Group|34569|6|Mentioned|p9|||See also Fig.3||||||
16844|Shoalhaven Group|34585|6|Mentioned|p380|||Permian||||||
16844|Shoalhaven Group|34605|6|Mentioned|Fig.5.27|||||||||
16844|Shoalhaven Group|34845|6|Mentioned|p119|||||||||
16844|Shoalhaven Group|35316|6|Mentioned|p429|||||||||
16844|Shoalhaven Group|35524|5|Briefly described|p73|||||||||
16844|Shoalhaven Group|36042|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|36045|6|Mentioned|p328|||||||||
16844|Shoalhaven Group|36058|6|Mentioned|p2|||||||||
16844|Shoalhaven Group|36220|4|Described|p16|||See also Table 1.||||||
16844|Shoalhaven Group|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
16844|Shoalhaven Group|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
16844|Shoalhaven Group|36223|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
16844|Shoalhaven Group|36285|6|Mentioned|Fig.2|||See also Fig.3.||||||
16844|Shoalhaven Group|36390|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
16844|Shoalhaven Group|36593|6|Mentioned|p188|||||||||
16844|Shoalhaven Group|36594|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|36954|6|Mentioned|Table 3|||See also P114.||||||
16844|Shoalhaven Group|37089|5|Briefly described|p208|||||||||
16844|Shoalhaven Group|37091|6|Mentioned|p224|||||||||
16844|Shoalhaven Group|37092|6|Mentioned|p227|||||||||
16844|Shoalhaven Group|37093|5|Briefly described|p231|||||||||
16844|Shoalhaven Group|37924|6|Mentioned|p488|||||||||
16844|Shoalhaven Group|37986|6|Mentioned|p314|||||||||
16844|Shoalhaven Group|38154|6|Mentioned|p368|||||||||
16844|Shoalhaven Group|38615|5|Briefly described|p19|||||||||
16844|Shoalhaven Group|38656|5|Briefly described|Table1.5.5|||P220||||||
16844|Shoalhaven Group|38690|6|Mentioned|p287|||See also P288||||||
16844|Shoalhaven Group|38951|6|Mentioned|p409|||||||||
16844|Shoalhaven Group|39232|4|Described|p111|||See also Fig.4||||||
16844|Shoalhaven Group|39285|6|Mentioned|p9|||||||||
16844|Shoalhaven Group|39287|6|Mentioned|p13|||See also Fig.2.5||||||
16844|Shoalhaven Group|39289|6|Mentioned|p79|||||||||
16844|Shoalhaven Group|39290|4|Described|p91|||Isopachs Fig. 5.8||||||
16844|Shoalhaven Group|39293|4|Described|p135|||||||||
16844|Shoalhaven Group|39306|6|Mentioned|Fig. 21.2|||||||||
16844|Shoalhaven Group|39307|6|Mentioned|Table 22.1|||||||||
16844|Shoalhaven Group|39308|6|Mentioned|p494|||Cored ddh||||||
16844|Shoalhaven Group|39309|4|Described|p117|||||||||
16844|Shoalhaven Group|39331|6|Mentioned|Fig.0-3|||See also Fig.7-1||||||
16844|Shoalhaven Group|39442|6|Mentioned|p188|||||||||
16844|Shoalhaven Group|39450|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|39578|6|Mentioned|p108|||||||||
16844|Shoalhaven Group|40166|4|Described|p347|||||||||
16844|Shoalhaven Group|40256|6|Mentioned|Fig.3|||||||||
16844|Shoalhaven Group|40270|6|Mentioned|p167|||||||||
16844|Shoalhaven Group|40321|6|Mentioned|Fig.3|||||||||
16844|Shoalhaven Group|40519|6|Mentioned|p328|||||||||
16844|Shoalhaven Group|40591|6|Mentioned|p323|||||||||
16844|Shoalhaven Group|40602|5|Briefly described|Table 1|||||||||
16844|Shoalhaven Group|40625|6|Mentioned|Map legend|Permian|Permian|||||||
16844|Shoalhaven Group|40636|6|Mentioned|p43|||||||||
16844|Shoalhaven Group|40744|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|40806|6|Mentioned|p148|||||||||
16844|Shoalhaven Group|41323|6|Mentioned|Fig.1|||||||||
16844|Shoalhaven Group|41689|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|41832|5|Briefly described|p569|||||||||
16844|Shoalhaven Group|41857|6|Mentioned|p392|||||||||
16844|Shoalhaven Group|42182|6|Mentioned|Table 1|||||||||
16844|Shoalhaven Group|42648|5|Briefly described|p31|||||||||
16844|Shoalhaven Group|42657|6|Mentioned|p73|||||||||
16844|Shoalhaven Group|42737|5|Briefly described|map legend|Permian||||||||
16844|Shoalhaven Group|42787|6|Mentioned|Table 1 P126|||||||||
16844|Shoalhaven Group|42848|5|Briefly described|p529|Permian|Permian|Includes the Conjola Subgroup. See also Fig.2 p530.||||||09-MAY-05
16844|Shoalhaven Group|42896|4|Described|p9, Table 2|||see also Fig.4||||||
16844|Shoalhaven Group|42925|5|Briefly described|Table 18|Late Permian|Early Permian|||||||
16844|Shoalhaven Group|42926|4|Described|map legend||Late Permian|||||||
16844|Shoalhaven Group|42974|5|Briefly described|p191|||||||||
16844|Shoalhaven Group|43017|5|Briefly described|Fig.1,p372|||||||||
16844|Shoalhaven Group|43028|6|Mentioned|p617,Fig.5.|||||||||
16844|Shoalhaven Group|43043|5|Briefly described|p103|||||||||
16844|Shoalhaven Group|43050|5|Briefly described|p19|||||||||
16844|Shoalhaven Group|43081|6|Mentioned|p172|||||||||
16844|Shoalhaven Group|43146|6|Mentioned|Fig.2 p41|||||||||
16844|Shoalhaven Group|43188|6|Mentioned|p221||Early Permian|||||||
16844|Shoalhaven Group|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Early Permian|Western and Southern Sydney Basin. Deposited during a widespread marine transgression in the Early Permian. Correlates with Porcupine and Watermark Formations, Gunnedah Basin.||||||
16844|Shoalhaven Group|43263|6|Mentioned|Map Legend||Permian|||||||
16844|Shoalhaven Group|43319|14|Not recorded|Map Legend|||||||||
16844|Shoalhaven Group|43320|14|Not recorded|Table 1 p5,7||Permian|p8,28,29,30||||||
16844|Shoalhaven Group|43344|14|Not recorded|p11-20,53,54,69,||Permian|71-73,76,140,141,187||||||
16844|Shoalhaven Group|43345|14|Not recorded|p3 Table 1||Permian|||||||
16844|Shoalhaven Group|43346|14|Not recorded|p1,2|||||||||
16844|Shoalhaven Group|43349|14|Not recorded|Map|||Now includes Capertee Group||||||
16844|Shoalhaven Group|43359|14|Not recorded|Map Legend||Permian|Provisional first edition||||||
16844|Shoalhaven Group|43360|14|Not recorded|Map Legend||Permian|(Provisional first edition) Includes Berry Formation and Megalong Formation||||||
16844|Shoalhaven Group|43362|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
16844|Shoalhaven Group|43363|14|Not recorded|Map Legend||Permian|(Provisional first edition)||||||
16844|Shoalhaven Group|43377|14|Not recorded|p144|||||||||
16844|Shoalhaven Group|43383|14|Not recorded|Fig.3,Fig.5||Permian|||||||
16844|Shoalhaven Group|43384|14|Not recorded|Map Legend||Late Permian|||||||
16844|Shoalhaven Group|43385|14|Not recorded|p179||Late Permian|||||||
16844|Shoalhaven Group|43465|14|Not recorded|Map Legend||Permian|||||||
16844|Shoalhaven Group|43471|14|Not recorded|p239|||Megadesmus, Astartila||||||
16844|Shoalhaven Group|43476|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
16844|Shoalhaven Group|43477|14|Not recorded|p19,28,41,45,60,Pl.1||Permian|||||||
16844|Shoalhaven Group|43479|14|Not recorded|p188,193,218|Kazanian|Artinskian|||||||
16844|Shoalhaven Group|43491|4|Described|pVII/50||Permian|||||||
16844|Shoalhaven Group|43494|5|Briefly described|p28|Permian|Permian|Basal conglomeratic sandstone is overlain by fine white sandstone, in turn overlain by white siltstone.  The basal sandstone has been mapped as Snapper Point Formation in the Cudgegong-Ilford area (Pemberton et al 1994).||||||16-MAR-06
16844|Shoalhaven Group|43515|14|Not recorded|Map Legend||Permian|(Provisional Edition)||||||
16844|Shoalhaven Group|43516|14|Not recorded|Map Legend||Late Carboniferous|||||||
16844|Shoalhaven Group|43639|5|Briefly described|Map Legend||Permian|||||||
16844|Shoalhaven Group|43782|5|Briefly described|Map Legend|Late Permian|Early Permian|||||||
16844|Shoalhaven Group|43981|14|Not recorded|p3||Permian|= Upper Marine Series.||||||
16844|Shoalhaven Group|44093|5|Briefly described|p64 Photo 2|Permian|Permian|Geological Province: Sydney Basin. Overlies Carwell Creek Formation, Lachlan Fold Belt, with angular unconformity.||||||26-NOV-10
16844|Shoalhaven Group|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
16844|Shoalhaven Group|44700|14|Not recorded|p108-109|||Cataract No.1 well.||||||
16844|Shoalhaven Group|44791|14|Not recorded|p18|||||||||
16844|Shoalhaven Group|44859|14|Not recorded|p68,71|||Gastropod.||||||
16844|Shoalhaven Group|44861|4|Described|Fig.159,228-9,232||Permian|||||||
16844|Shoalhaven Group|45006|14|Not recorded|p5,6|||||||||
16844|Shoalhaven Group|45031|14|Not recorded|p35,49,52,54,63-4,67|||||||||
16844|Shoalhaven Group|45090|6|Mentioned|p7|||Time correlation chart||||||
16844|Shoalhaven Group|45138|6|Mentioned|p2|||||||||
16844|Shoalhaven Group|46849|6|Mentioned|p197|||||||||
16844|Shoalhaven Group|48926|6|Mentioned|p46|||P29 et seq.||||||
16844|Shoalhaven Group|50116|5|Briefly described|p63|Permian|Permian|Overlain by the Illawarra Coal Measures. Geological Province: Sydney-Gunnedah Basin.||||||10-MAR-05
16844|Shoalhaven Group|50234|5|Briefly described|Map Legend|Permian|Permian|Includes: Tallong Conglomerate.||||||
16844|Shoalhaven Group|60281|5|Briefly described|p57|Early Permian|Early Permian|Comprises marine shelf to coastal plain sediments.  Contains the Yadboro and Tallong Conglomerates in the west.  Disconformably overlies the Talaterang Group.  Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|60285|5|Briefly described|p181|Early Permian|Early Permian|Overlies Talaterang Group. Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|60300|6|Mentioned|p249|Permian|Permian|||||||
16844|Shoalhaven Group|61209|5|Briefly described|p225 Fig. 7b|Paleozoic|Paleozoic|Mentioned in the context of Shoalhaven Group Sediments. Geological Province: Sydney Basin.||||||07-NOV-08
16844|Shoalhaven Group|61315|5|Briefly described|p167, Table SY2|Permian|Permian|Includes the Conjola Subgroup, Wandrawandian Siltstone, Nowra Sandstone, Berry Siltstone and Budgong Sandstone. Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|61609|5|Briefly described|p239, p240 Tb. 1, p246 Fig. 5, p247|Permian|Permian|Includes Conjola Subgroup and other units. Geological Province: Sydeny Basin.||||||07-FEB-11
16844|Shoalhaven Group|61610|6|Mentioned|p252, p252 Fig. 2|Permian|Permian|Geological Province: Sydney Basin.||||||07-FEB-11
16844|Shoalhaven Group|61900|5|Briefly described|p129, p130 Fig. 3|Triassic|Permian|Includes Snapper Point Formation. Sandstones, conglomerates and shales.  Geological Province: Sydney Basin.||||||05-JUN-06
16844|Shoalhaven Group|62043|6|Mentioned|p438 Fig.2. |Late Permian|Early Permian|Southern Sydney Basin.|||Includes Yadboro and Tallong Conglomerates; Yarrunga Coal Measures; Pebbley Beach, Snapper Point and Broughton Formations; Wandrawandian and Berry Siltstones, and Nowra Sandstone.|Overlies Talaterang Group.||
16844|Shoalhaven Group|63151|5|Briefly described|p3 Fig. 2|Permian|Permian|Unconformably overlies Bindook Volcanic Complex in vicinity of Yerranderie. Comprises flat-lying sequence of conglomerates, sandstones and siltstones.||||||05-APR-07
16844|Shoalhaven Group|63461|5|Briefly described|p862 Fig. 1c|Permian|Permian|Contains a siltstone-domiated unit in the middle section, the Wandrawandian Siltstone. Geological Province: Sydney Basin.||||||10-DEC-07
16844|Shoalhaven Group|63773|5|Briefly described|p1057, p1059, p1058 Fig. 2, p1069|Middle Permian|Early Permian|Includes Wandrawandian Siltstone, Snapper Point Formation, Pebbley Beach Formation, Yadboro  and Tallong Conglomerate, Yarrunga Cola Measures, Broughton Formation and Berry Siltstone. Geological Province: Sydney Basin.||||||
16844|Shoalhaven Group|63832|5|Briefly described|p131 fig 2|Guadalupian|Cisuralian|Of Sydney Basin. Deposition spans sixth (P2) and seventh (P3) glaciations.|||Includes Yadboro and Tallong Conglomerates; Yarrunga Coal Measures; Snapper Point, Pebbley Beach, Broughton Formations; Wandrawandian and Berry Siltstones.|||14-DEC-17
16844|Shoalhaven Group|64238|5|Briefly described|Map legend|Permian|Permian|Includes the Tallong Conglomerate.||||||
16844|Shoalhaven Group|64631|5|Briefly described|p44 Fig.2.|Roadian|Sakmarian|SW, SE, NW Sydney Basin. Biostratigraphic age control at base and top.|||Includes Yadboro and Tallong Conglomerates, Yarrunga Coal Measures, Snapper Point Formation, Berry and Wandrawandian Siltstones, Pebbley Beach Formation.|Overlies Clyde Coal Measures and Wasp Head Formation. Is overlain by Illawarra Coal Measures.||
16844|Shoalhaven Group|64877|5|Briefly described|p296|Permian|Permian|Southern Sydney Basin. Shallow-marine to alluvial deposits.|||Yadboro, Tallong Conglomerates; Pebbley Beach, Snapper Point, Broughton Formations; Yurrunga Coal Measures; Wandrawandian, Berry Siltstones; Nowra Sandstone.|||
16844|Shoalhaven Group|66300|6|Mentioned|p52, p58, 64.|Permian|Permian|Sydney Basin.|||Includes Snapper Point Formation, Nowra Sandstone and Berry Siltstone.|||29-OCT-13
16844|Shoalhaven Group|66577|5|Briefly described|pp995-999.|Permian|Permian|Lower levels represent a pervasive transgression with deposition of fluvial, shoreface and marine facies. Later units represent deepening due to foreland loading by the hypothesised Currawong Orogen.|||Yadboro and Tallong Conglomerates; Pebbley Beach, Snapper Point, Broughton Formations; Yarrunga Coal Measures; Wandrawandian and Berry Siltstones; Nowra and Budgong Sandstones; Gerringong Volcanics.|Overlies Talaterang Group. Is overlain by Illawarra Coal Measures.||
16844|Shoalhaven Group|67500|6|Mentioned|p12 Tb.1|||Shown as Upper Shoalhaven Group.||Of the Gerringong volcanic facies.|Includes Broughton Formation.|||01-MAY-12
16844|Shoalhaven Group|67663|5|Briefly described|p518, p520 Tb.1, p536|Permian|Permian|Western and Southern Coalfields, Sydney Basin.|||Includes Snapper Point Formation, Berry Siltstone, Broughton Formation.|Overlain by the Illawarra Coal Measures and Gerringong Volcanics. Unconformably overlies Clyde Coal Measures and Wasp Head Formation.||
16844|Shoalhaven Group|68003|5|Briefly described|p38 Fig.3-j, p40, p131.|Late Permian|Late Permian|Western Coalfield (Sydney Basin), Brigalow Belt South Bioregion. Correlative of Millie Group (Gunnedah Basin); Maitland Group (Hunter Coalfield); and Bickham, Borambil Creek and Toll Bar Formations (Werrie Basin).|||Includes Yadboro and Tallong Conglomerates, Pebbley Beach Formation, Snapper Point Formation, Berry Siltstone and Budgong Sandstone.|Is overlain by Illawarra Coal Measures.|Polymictic conglomerate, lithic sandstone, shale, siltstone, claystone, minor carbonate and evaporite.|
16844|Shoalhaven Group|68202|6|Mentioned|p176|Triassic|Triassic|Sydney Basin.||||||
16844|Shoalhaven Group|68592|3|Fully described|p36, p1779-86||Permian|Joplin et al. (1952), presumably after the Shoalhaven River. Includes the old Capertee Group. A number of units in the original definition are now included in a redefined Talaterang Group (Tye et al., 1996). 60-70m thick in Goulburn 250 map area.|||Tallong Conglomerate. Elsewhere Yagers, Burrawang, Yadboro Conglomerates; Badgerys Breccia; Yurrunga Coal Measures; Pebbly Beach, Snapper Point, Broughton Formations; Wandrawandian, Berry Siltstones.|Disconformably overlies Talaterang Group. Is overlain conformably by Illawarra Coal Measures.|A thick, mainly sandstone and siltstone shallow marine sequence with a few valley-fill conglomerate units, commonly overlain by minor coal,  occurring at the base of the sequence along the SW Sydney Basin margin.|
16844|Shoalhaven Group|69297|6|Mentioned|p499, p501, p503, p504|Early Permian|Early Permian|Sydney Basin. Sandstones of this group are good potential hydrocarbon reservoirs. Siltstones may also form regional sealing units.|||Includes the Pebbly Beach Formation, Yadboro Conglomerate, Tallong Conglomerate, Snapper Point Formation, the Wandrawandian Siltstone, Nowra Sandstone and the Berry Siltstone.|Overlies the Talaterang Group. Overlain by the Broughton Formation.|Sandstones and marine siltstones.|
16844|Shoalhaven Group|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
16844|Shoalhaven Group|70192|5|Briefly described|Map Legend|Permian|Permian|On Goulburn 1:100 000 mapsheet portion of Time-Space Plot.|||Includes Tallong Conglomerate.|||
16844|Shoalhaven Group|70297|4|Described|map legend, on side 2 of map sheet|Guadalupian|Cisuralian|Basal conglomerate and sandstone overlain by siltstone. Erosional base. Sydney Basin. Age: late Early to Late Permian.||||Is overlain by Illawarra Coal Measures.|Polymictic pebble paraconglomerate, fine-grained muddy lithic sandstone, sandy micaceous siltstone, minor shale and siltstone.|
16844|Shoalhaven Group|70542|5|Briefly described|Map Legend|Permian|Permian||||Includes Tallong Conglomerate.|||
16844|Shoalhaven Group|70661|3|Fully described|vii, ix, x, p15, p70, p135|Mid-Permian|Early Permian|Deposited during multiple marine transgressive-regressive episodes in shelfal, shallow marine and near shore depositional environments.Named for Shoalhaven river valley. Parts of this group were once mapped as the Upper Marine Series of David and Stonier (1891). Distribution, geomorphology, depositional environments, metamorphism, structure, geophysical characteristics and fossil assemblages discussed. Gas generative petroleum system identified - further assessment required. Thickness ranges from 45m to over 1000m. See also p137-p140, p171.|||Berry Siltstone, Tallong Conglomerate, Yarrunga Coal Measures, Snapper Point Formation, Wandrawandian Formation, Nowra Sandstone, Broughton Formation|Unconformably overlies Adaminaby Group|Alternating units of interbedded pebble and pebble-cobble conglomerate, pebbly sandstone, silty sandstone, sandy siltstone and siltstone.Rare sedimentary breccia and coal seams occur.|
16844|Shoalhaven Group|70837|5|Briefly described|p246|||Of Southern Sydney Basin.||||||
16844|Shoalhaven Group|71115|5|Briefly described|p179-180, 182|Permian|Permian|Southern Sydney Basin.|||Broughton Formation; lower part of Gerringong Volcanics.|Is overlain by Cumberland Subgroup (Illawarra Coal Measures).||
16844|Shoalhaven Group|71303|5|Briefly described|map legend|Guadalupian|Cisuralian|Of Sydney Basin.|||Includes Tallong Conglomerate, Yarrunga Coal Measures, Snapper Point Formation, Wandrawandian Formation, Nowra Sandstone, Berry Siltstone, Broughton Formation.|||
16844|Shoalhaven Group|71538|6|Mentioned|p54 fig 2|Kungurian|Artinskian|Sydney Basin.|||Includes the Yadboro Formation, Tallong Formation, Pebbley Beach Formation, Mount Agony Formation, Snapper Point Formation and the Wandrawandian Siltstone.|||
16844|Shoalhaven Group|71542|5|Briefly described|p23, 25|Permian|Permian|Of southern Sydney Basin. Comprises dominant sedimentary fill in the southern Sydney Basin. Deposited on an extensive open continental shelf.|||Includes Broughton Formation, Berry Formation, Nowra Sandstone, Wandrawandian Siltstone, Snapper Point Formation and Pebbley Beach Formation.|Overlain by Illawarra Coal Measures. Underlain by Talaterang Group.|Alternating sandstone and siltstone successions.|20-OCT-21
16844|Shoalhaven Group|73248|6|Mentioned|p301|Permian|Permian|Known in the Cumberland Basin only from borehole records.||||Overlain by Illawarra Coal Measures.||
16844|Shoalhaven Group|73304|6|Mentioned|p65, p74|||Sydney Basin, southern.||Illawarra Coal Measures|Broughton Formation|||
16844|Shoalhaven Group|73421|5|Briefly described|p3, p5|Capitanian|Artinskian|Sydney Basin, southern. Marine sediments.|||Pebbly Beach Formation, Snapper Point Formation, Wandrawandian Siltstone, Nowra Sandstone, Berry Siltstone, Broughton Formation|Overlies Talaterang Group, underlies Illawarra Coal Measures|Includes sandstone and siltstone with pebble layers, lesser diamictite, conglomerate and claystone/shale. Intercalated with pyroclastics and lavas in upper part.|
16844|Shoalhaven Group|73494|4|Described|p540, 542|Permian|Permian|Southern Sydney Basin. Thickness reduces westwards (from ~1000m to 45m). Early to Late Permian.|||Conjola Subgroup; Gerringong Volcanics (lower part); Broughton, Berry Formations; Nowra Sandstone; Wandrawandian Siltstone.|Intercalated with the Gerringong Volcanics. Overlies Talaterang Group. Is overlain by Illawarra Coal Measures.|Fossiliferous volcaniclastic shallow-marine sandstone and siltstone. Intruded by numerous mafic dykes.|
16844|Shoalhaven Group|73582|5|Briefly described|p105, 119, 122|Permian|Permian|The basal Permian unit of the Sydney Basin. Crops out sporadically in the Jenolan area, mainly on ridge tops on an old erosion surface that extends N beyond Mudgee.||||Locally, unconformably overlies Jenolan Caves Limestone.|Glacial or fluvioglacial conglomerates (with distinctive white quartz pebbles) and sandstones.|
16848|Shoalwater Formation|22740|5|Briefly described|155,156 fig 2, 157|Paleozoic|Paleozoic|Geol province New England Fold Belt. Also on pages 158, 163.||||||07-NOV-08
16848|Shoalwater Formation|23799|6|Mentioned|p25|||Of the Curtis Island Group.  Possible correlative of the Bjelke Petersen beds.||||||
16848|Shoalwater Formation|24382|5|Briefly described|Map legend|Carboniferous|Carboniferous|Parent: Curtis Island Group.||||||18-AUG-08
16848|Shoalwater Formation|24420|5|Briefly described|p7|Carboniferous|Late Devonian|Of Curtis Island Group.||||||
16848|Shoalwater Formation|24489|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Curtis Island Group.||||||
16848|Shoalwater Formation|24490|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of Curtis Island Group. Quartz arenite, mudstone, schist.||||||04-SEP-08
16848|Shoalwater Formation|24615|5|Briefly described|CD|Carboniferous|Carboniferous|[Ccs].  Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.||||||
16848|Shoalwater Formation|30451|5|Briefly described|p8|||||||||
16848|Shoalwater Formation|30777|5|Briefly described|p417|||Discussed||||||
16848|Shoalwater Formation|31657|4|Described|p91|||See also p92. Ordovician - Silurian.||||||30-SEP-08
16848|Shoalwater Formation|31658|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16848|Shoalwater Formation|31659|2|Defined|p17, p18-19|Early Paleozoic|Early Paleozoic|max. thickness: >30,000ft. Quartz greywacke, mudstone, grading in places into schist and gneiss. See also Table 1.||||||07-NOV-08
16848|Shoalwater Formation|32357|4|Described|Table 1|||||||||
16848|Shoalwater Formation|32358|4|Described|Table 1|||||||||
16848|Shoalwater Formation|32361|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
16848|Shoalwater Formation|33769|5|Briefly described|p150|||||||||
16848|Shoalwater Formation|33774|6|Mentioned|p6|||Curtis Is. Group. Not recognisable in Mundubbera area.||||||
16848|Shoalwater Formation|36211|6|Mentioned|p269|||||||||
16848|Shoalwater Formation|36488|6|Mentioned|p3|||||||||
16848|Shoalwater Formation|36528|6|Mentioned|p170|||See also Fig.4||||||
16848|Shoalwater Formation|38081|5|Briefly described|Table 1|||||||||
16848|Shoalwater Formation|38143|6|Mentioned|p12|||||||||
16848|Shoalwater Formation|38391|6|Mentioned|p6|||||||||
16848|Shoalwater Formation|38406|5|Briefly described|p9|||||||||
16848|Shoalwater Formation|38447|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian to Carboniferous.||||||18-AUG-08
16848|Shoalwater Formation|39445|5|Briefly described|Table 6|||Middle? - Late Carb. See also P83||||||
16848|Shoalwater Formation|40475|6|Mentioned|p2|||||||||
16848|Shoalwater Formation|40960|5|Briefly described|p221|||||||||
16848|Shoalwater Formation|41576|4|Described|p16|||See also Table 1.||||||18-AUG-08
16848|Shoalwater Formation|41577|6|Mentioned|Map legend|Late Carboniferous||||||||
16848|Shoalwater Formation|41738|6|Mentioned|p166|||||||||
16848|Shoalwater Formation|41778|6|Mentioned|Table 1|||||||||
16848|Shoalwater Formation|41922|4|Described|Table 1, P11|||||||||
16848|Shoalwater Formation|42547|4|Described|p54|||||||||
16848|Shoalwater Formation|42660|4|Described|p23 p168|||||||||
16848|Shoalwater Formation|42901|6|Mentioned|p403|||||||||
16848|Shoalwater Formation|42980|5|Briefly described|Fig.4,p304|||||||||
16848|Shoalwater Formation|42985|6|Mentioned|p386|||||||||
16848|Shoalwater Formation|43008|5|Briefly described|map legend|||||||||
16848|Shoalwater Formation|43754|3|Fully described|p572-573||Early Carboniferous|||||||
16848|Shoalwater Formation|45107|6|Mentioned|p6|||||||||
16848|Shoalwater Formation|50190|6|Mentioned|p47|||||||||
16848|Shoalwater Formation|50207|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of the Curtis Island Group.||||||
16848|Shoalwater Formation|50212|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|Of Curtis Island Group||||||
16848|Shoalwater Formation|60479|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Quartzose sandstone, mudstone.||||||
16848|Shoalwater Formation|60557|5|Briefly described|p23|Carboniferous|Devonian|Of the Curtis Island Group. Comprises massive, thick quartz sandstone beds (2-3m thick), with interbedded dark grey to black, thin-bedded to laminated, strongly cleaved phyllitic mudstone.||||||09-JUN-05
16848|Shoalwater Formation|61035|6|Mentioned|p13, p14|Late Carboniferous|Late Carboniferous|Unconformably overlain by Double Mountain Volcanics and Peninsula Range Volcanics. Geological Province: Wandilla Province. Sandstone dominated unit and is also turbiditic in character. Age based on similarities with another unit in Yarrol Province.||||||07-FEB-11
16848|Shoalwater Formation|63821|5|Briefly described|p15, p34, p38|Carboniferous|Carboniferous|Of Curtis Island Group. Max. depositional age: 328.9+/-2.3Ma. Sequence of tightly folded, coarse-grained, quartz-arenite, slate and schist. Geological Province: Wandilla Province - Coastal Block.||||||07-FEB-11
16848|Shoalwater Formation|64556|5|Briefly described|p18|||Of Curtis Island Group. Source of sample material for age analysis was from folded leucocratic biotite microgranite dyke intruding this unit of strongly foliated metasediments.||||||07-FEB-11
16848|Shoalwater Formation|65380|5|Briefly described|p657,658, 660,666-670, 672-674, 676-679|||Coastal Block, New England Orogen. Maximum depositional age from detrital zircon: 327 +/- 1 Ma.|||||Quartz-rich sandstone with only minor volcanics.|27-MAR-12
16848|Shoalwater Formation|65385|6|Mentioned|pS133|||In the New England Orogen. Detrital zircon age of 952+/-9 Ma (Korsch et al., 2009).||||||08-MAR-12
16848|Shoalwater Formation|65452|5|Briefly described|p5-6|Carboniferous|Carboniferous|||||Is overlain by, or faulted against, Agnes Water Volcanics.|Low-grade metasediments.|
16848|Shoalwater Formation|68008|3|Fully described|p110-111, p117-120, p326, p481-482|||Kirkegaard et al. (1970) regarded this as the oldest [sic] unit in the Group. Comprises the Shoalwater terrane. Forms subdued topography with closely spaced dendritic drainage. Structure described. Thickness unknown; the estimated 10,000m of Kirkegaard et al. (1970) ignores its imbricate fault structure as part of an accretionary wedge. The only fossils are unidentifiable flant fragments in black shale. Metamorphosed at 276.8 +/- 4.6 Ma, 274.9 +/- 3.2 Ma (zircon rims: Carson et al., 2006). Other ages discussed.||Topmost Curtis Island Group.||Overlies transitionally, and is faulted against, Wandilla Formation. Is intruded by Miriam Vale Granodiorite.|Fine-grained, poorly sorted, thick quartzose sandstone beds, locally metamorphosed to quartz-muscovite-biotite schists and gneiss; alternating with grey to black, very thin-bedded to laminated mudstone; rare beds of chert or fine felsic tuff.|
16848|Shoalwater Formation|68319|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Wandilla Province.||||Facies variant of Gaythorn Metamorphics.|Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.|
16848|Shoalwater Formation|68421|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province.||||Conformably underlain by the Wandilla Formation.|Quartzose sandstone, mudstone; local quartz-muscovite-biotite schist.|
16848|Shoalwater Formation|68679|5|Briefly described|p317-319, p324, p336, p338, p420, p469|Carboniferous|Carboniferous|Coastal Subprovince, Wandilla Province, New England Orogen. Forms a chain of islands in Keppel Bay, a thin strip along eastern Curtis island to Facing Island, and reaches the mainland S of Gladstone. Estimated thickness of 10,000m is a gross exaggeration due to fault repetition. Chert or tuff beds crop out as strike ridges. Deep marine deposits. Deformation described. Contains unidentifiable plant fragments in black shales.||Curtis Island Group.||Conformably (transitionally) overlies Wandilla Formation. Possible correlative of Bjelke-Petersen beds. Is intruded by Chowey and Mingo Granites.|Quartzose sandstone beds (to 3m thick), fine- to medium-grained, poorly sorted, locally graded, locally metamorphosed to schist and gneiss; alternating with very thin-bedded to laminated mudstone beds; rare beds of chert or fine felsic tuff.|
16848|Shoalwater Formation|69952|6|Mentioned|p72|||New England Orogen. Forms hilly country.||||||
16848|Shoalwater Formation|73197|6|Mentioned|p468|||New England Orogen, northern. Coastal Subprovince. Deposited in outboard environment, contains range of zircon ages that were not sourced primarily from the Currabubula-Connors Arc, suggested to be from streams draining the continental interior.|||||Quartz-rich turbidites.|
16848|Shoalwater Formation|73201|6|Mentioned|p619|||New England Orogen. Outboard of a subduction complex.|||||Quartzose sandstones.|
16848|Shoalwater Formation|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen, accretionary complex.|||||Includes quartz-rich, medium-grained sandstone.|
16848|Shoalwater Formation|73450|6|Mentioned|p21|Paleozoic|Paleozoic|||||Intruded by Molangul Granite.||
16860|Showgrounds Sandstone|13516|5|Briefly described|p138, p162-163, p166|Middle Triassic|Middle Triassic|From Bowen Basin. Shown in text as Showgrounds Sandstone, but in Figs p159, p169 as Showgrounds Sandstone Member. P163 suggests there are facies-relationship grounds for considering Showgrounds Sandstone to be a Member of Moolayember Formation rather than a Fm of Clematis Group.||Of Clematis Group||Diachronous contact with overlying Moolayember Formation||
16860|Showgrounds Sandstone|22857|6|Mentioned|p295, p315 Fig. 22.8|||Mentioned only in terms of equivalents of this unit.||||||
16860|Showgrounds Sandstone|22865|4|Described|p295,Fig22.8p315|Middle Triassic|Early Triassic|||||||
16860|Showgrounds Sandstone|22975|5|Briefly described|p34 Fig.6|Triassic|Triassic|||||||
16860|Showgrounds Sandstone|22980|5|Briefly described|p249 Fig.2|Triassic|Triassic|||||||
16860|Showgrounds Sandstone|23359|6|Mentioned|76|||||||||
16860|Showgrounds Sandstone|24069|5|Briefly described|p284|Middle Triassic|Middle Triassic|Geological Province: Surat Basin.||||||
16860|Showgrounds Sandstone|24077|5|Briefly described|p411 Tb.3|Middle Triassic|Early Triassic|Of the Mimosa Group.  White coarse quartzose sandstone.  Max. thickness: 13m.  Geological Province: Bowen Basin.||||||
16860|Showgrounds Sandstone|24159|5|Briefly described|p148, Fig. 2|Middle Triassic|Middle Triassic|Geological Province: Bowen Basin. Overlying Unit: Snake Creek Mudstone Member. Underlying Unit: unconformably with Kianga Formation.||||||
16860|Showgrounds Sandstone|24241|5|Briefly described|p19 Fig.4|Middle Triassic|Middle Triassic|||||||
16860|Showgrounds Sandstone|29385|6|Mentioned|p82|||||||||
16860|Showgrounds Sandstone|29387|6|Mentioned|p29|||||||||
16860|Showgrounds Sandstone|29389|6|Mentioned|p17|||Early Triassic.||||||
16860|Showgrounds Sandstone|29390|6|Mentioned|p54|||Triassic resevoir for Roma.||||||
16860|Showgrounds Sandstone|29391|6|Mentioned|Table 4|||Appears on P19.||||||
16860|Showgrounds Sandstone|29393|6|Mentioned|Table 2|||Triassic.||||||
16860|Showgrounds Sandstone|29721|6|Mentioned|Table 65|||||||||
16860|Showgrounds Sandstone|30696|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|31115|6|Mentioned|p34|||||||||
16860|Showgrounds Sandstone|31369|4|Described|p30|||||||||
16860|Showgrounds Sandstone|33059|4|Described|Table 1|||M.Trias.||||||
16860|Showgrounds Sandstone|33530|5|Briefly described|Table 1|||Middle Triassic||||||
16860|Showgrounds Sandstone|34212|6|Mentioned|p1|||Triassic. See also PP2,3,4 etc.||||||
16860|Showgrounds Sandstone|36111|6|Mentioned|p34|||||||||
16860|Showgrounds Sandstone|36613|6|Mentioned|Table 4|||||||||
16860|Showgrounds Sandstone|36643|6|Mentioned|p61|||||||||
16860|Showgrounds Sandstone|36914|6|Mentioned|p85|||||||||
16860|Showgrounds Sandstone|37288|6|Mentioned|p41|||||||||
16860|Showgrounds Sandstone|39445|5|Briefly described|Table 9|||||||||
16860|Showgrounds Sandstone|39491|4|Described|p18|||||||||
16860|Showgrounds Sandstone|39494|6|Mentioned|p137|||||||||
16860|Showgrounds Sandstone|39815|6|Mentioned|p445|||||||||
16860|Showgrounds Sandstone|40030|6|Mentioned|p135|||||||||
16860|Showgrounds Sandstone|40249|6|Mentioned|p41|||||||||
16860|Showgrounds Sandstone|40544|6|Mentioned|p161|||||||||
16860|Showgrounds Sandstone|40767|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|41188|6|Mentioned|p231|||||||||
16860|Showgrounds Sandstone|41210|6|Mentioned|p163|||||||||
16860|Showgrounds Sandstone|41247|6|Mentioned|p117|||||||||
16860|Showgrounds Sandstone|41712|6|Mentioned|p275|||See also Fig.5||||||
16860|Showgrounds Sandstone|41725|6|Mentioned|p400|||See also P403||||||
16860|Showgrounds Sandstone|42250|6|Mentioned|p28|||||||||
16860|Showgrounds Sandstone|42618|6|Mentioned|p14|||||||||
16860|Showgrounds Sandstone|42634|5|Briefly described|Table 2 P10|||||||||
16860|Showgrounds Sandstone|42911|6|Mentioned|p20|||||||||
16860|Showgrounds Sandstone|43000|6|Mentioned|p108|||||||||
16860|Showgrounds Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
16860|Showgrounds Sandstone|43185|6|Mentioned|6||Triassic|||||||
16860|Showgrounds Sandstone|43711|6|Mentioned|p17|||||||||
16860|Showgrounds Sandstone|43714|6|Mentioned|Fig.3,p5||Triassic|||||||
16860|Showgrounds Sandstone|43883|14|Not recorded|p18 Fig.4-3|||Misspelling of 'Showground Ss'?||||||
16860|Showgrounds Sandstone|43960|14|Not recorded|p9,12||Triassic|||||||
16860|Showgrounds Sandstone|44116|14|Not recorded|p24,28|||||||||
16860|Showgrounds Sandstone|44422|14|Not recorded|p150,155|Late Triassic|Middle Triassic|=Clematis Sandstone.||||||
16860|Showgrounds Sandstone|44787|14|Not recorded|Tb.p121-125,127-128||Late Triassic|Equivalent to upper part of Clematis Sandstone.||||||
16860|Showgrounds Sandstone|45110|6|Mentioned|p52|||||||||
16860|Showgrounds Sandstone|61313|6|Mentioned|p105|||Equivalent to Digby Formation and the shales of Napperby Formation. Geological Province: Surat Basin||||||
16860|Showgrounds Sandstone|62357|5|Briefly described|p524 Fig. 7, p535|Early Triassic|Early Triassic|Geological Province: Bowen Basin.||||||
16860|Showgrounds Sandstone|64048|5|Briefly described|p67|Middle Triassic|Middle Triassic|Commercial gas production in its fluvial quartzose sandstones.||||||07-FEB-11
16860|Showgrounds Sandstone|64197|6|Mentioned|p630 Fig.7|Triassic|Triassic|||||Underlies the Moolayember Formation. Overlies the Rewan Group.||
16860|Showgrounds Sandstone|64856|4|Described|p42, p69-76, p78|Anisian|Anisian|Named but not defined by Derrington and Mott (1955). Bowen Basin. Medium to very coarse grained sandstone equivalent to upper part of the Clematis Group (Expedition Sandstone). Unconformable on the Rewan Group on the Roma Shelf and southwest Taroom Trough. Is overlain by Snake Creek Mudstone Member (Moolayember Formation). Contains palynofloras APT31 age (237.5-240 Ma).|| ||||29-NOV-17
16860|Showgrounds Sandstone|64857|5|Briefly described|p126-128, p113 Fig. 3|Triassic|Triassic|Bowen Basin. Mainly medium to coarse grained quartzose sandstone and conglomerate. Correlative of the Expedition Sandstone. Appears to be a member of the Clematis Group. Conformably underlies Snake Creek Mudstone Member.||||||15-JUL-13
16860|Showgrounds Sandstone|64858|6|Mentioned|p180 Fig.2|Middle Triassic|Middle Triassic|||||||30-NOV-09
16860|Showgrounds Sandstone|64859|6|Mentioned|p194|Middle Triassic|Middle Triassic|Hydrocarbon reservoir, Bowen Basin.||||||
16860|Showgrounds Sandstone|65112|6|Mentioned|Fig 4 p314|Middle Triassic|Middle Triassic|Unit in the Bowen Basin. Top unit in the Clematis Group of the Taroom Trough.||||Overlain by Moolayember Formation.||22-MAR-12
16860|Showgrounds Sandstone|65113|5|Briefly described|Fig 4 p340|Early Triassic|Early Triassic|Sst, in text. Underlies the Moolayember Formation.||||||
16860|Showgrounds Sandstone|65114|5|Briefly described|p385 Fig.3|Middle Triassic||||||||
16860|Showgrounds Sandstone|65115|5|Briefly described|p425, 426, Fig 2 p403|Triassic|Triassic|Of Clematis Group, Taroom Trough? Underlies the Moolayember Formation in the Taroom Trough, Bowen Basin. Part of Supersequence I.||||||
16860|Showgrounds Sandstone|65116|5|Briefly described|p450, 451, Fig 2 p436|Middle Triassic|Early Triassic|Of Clematis Group. Underlies the Moolayember Formation in the Bowen Basin.||||||
16860|Showgrounds Sandstone|65118|5|Briefly described|p493, Fig 2 p479|Triassic|Triassic|Of Clematis Group? Underlies the Moolayember Formation in the Denison Trough, Bowen Basin. Unconformably overlies the Rewan Group||||||06-MAR-12
16860|Showgrounds Sandstone|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||||||
16860|Showgrounds Sandstone|67402|4|Described|p18 fig WSD2, p19 fig WSD3, WSD4|Anisian|Anisian|Bowen and Surat Basins. Proven hydrocarbon reservoir and potential carbon dioxide storage reservoir. Deposited in a fluvial-deltaic environment. See also p30, p43 tbl HPB1, p45-49, p52, p53, p55-p57, p59, p62, p144, p147 fig SRT5, p300.||||Conformably overlain by the Snake Creek Mudstone. Overlies the Rewan Group.|Quartzose sandstone and conglomerate with some interbedded siltstone and shale.|
16860|Showgrounds Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Clematis Group.||||
16860|Showgrounds Sandstone|68004|5|Briefly described|p87, p172, p173, p175.|Middle Triassic|Middle Triassic|Surat Basin. Hydrocarbon reservoir in Queensland; targeted for oil/gas exploration in New South Wales from the 1960s; only minor fluorescence and low level gas shows. Sealed by Moolayember Formation. Discussed in some detail.||||||
16860|Showgrounds Sandstone|68679|5|Briefly described|p377, p381, p383-384|Middle Triassic|Middle Triassic|Traves and Thralls (1960). Roma Shelf, Bowen Basin. <40m thick. Braided fluvial stream deposits. Produces oil, gas and condensate.||||Overlies the Rewan group. Is overlain by the Moolayember Formation. Equivalent to upper Clematis Group in Roma area. Laterally equivalent to Expedition Sandstone.|Medium-grained to very coarse-grained quartzose sandstone, minor granule to pebble conglomerate.|
16860|Showgrounds Sandstone|69582|6|Mentioned|p35|||Surat Basin.||||Overlain by the Moolayember Formation.||
16860|Showgrounds Sandstone|72297|5|Briefly described|p744-745|||Western side of the Taroom Trough, Bowen Basin. A significant regional hydrocarbon reservoir; channel sandstones. Traps are structural-stratigraphic formed by later deformation.||Clematis Group.||||
16860|Showgrounds Sandstone|73113|6|Mentioned|p46|||Bowen Basin. Written as equivalent to Clematis Group [now a constituent].||||||
16866|Shume Formation|22857|4|Described|p438 App.1, Tb.A1.6|Pragian|Lochkovian|Of the upper Amphitheatre Group (Cobar Supergroup). Alternation of pockets of 3-12m thick arenite with 1-10m thick siltstone; massive bedding, parallel lamination, formed as submarine fan. Max. thickness: 1.8km. Geological Province: Cobar Basin.||||||
16866|Shume Formation|23171|6|Mentioned|p15|||(MacRae 1987).||||||
16866|Shume Formation|23173|4|Described|Map Legend|Lochkovian|Lochkovian|||||||
16866|Shume Formation|23734|5|Briefly described|p12 Fig. 1|||Parent: Amphitheatre Group.  Conglomerate and sandstone.||||||
16866|Shume Formation|35287|6|Mentioned|p6|||||||||
16866|Shume Formation|38292|6|Mentioned|Fig.2|||||||||
16866|Shume Formation|39618|3|Fully described|p99|||||||||
16866|Shume Formation|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
16866|Shume Formation|41528|2|Defined|p80|Early Devonian||||||||
16866|Shume Formation|41529|6|Mentioned|Map legend|Early Devonian||||||||
16866|Shume Formation|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
16866|Shume Formation|41821|3|Fully described|p36|Devonian|Early Devonian|Age: mid Early Devonian||||||
16866|Shume Formation|41872|6|Mentioned|p8|||||||||
16866|Shume Formation|42144|6|Mentioned|Fig.5 P608|||||||||
16866|Shume Formation|42521|5|Briefly described|Fig.1 P14|||||||||
16866|Shume Formation|42566|5|Briefly described|Fig.5 P11|||||||||
16866|Shume Formation|42907|6|Mentioned|Fig.8, P8|||||||||
16866|Shume Formation|42983|6|Mentioned|Fig.3,p345|||||||||
16866|Shume Formation|43032|6|Mentioned|p108|||||||||
16866|Shume Formation|43089|5|Briefly described|Map Legend|||of Amphitheatre Group||||||
16866|Shume Formation|65469|5|Briefly described|p15, p17, p43, p52|||Lachlan Orogen. In contact with the Amphitheatre Group, Lower [although the author doesn't give the relationship]. See also p55 fig 3-19, p62, p67, p138, p139, p351, App A-VI 3.||Amphitheatre Group||||
16866|Shume Formation|70751|6|Mentioned|p5, 12||||||||Minor felsic volcanic and volcaniclastic rocks.|23-SEP-19
16866|Shume Formation|70950|5|Briefly described|p1029,1033,1034, 1038-1039|||Geological province: Central Lachlan Orogen. Includes minor felsic volcanic and volcaniclastic rocks. Detailed mineralisation analysis provided.||Of Amphitheatre Group.|Includes Shuttleton Rhyolite Member.|Subdivides Amphitheater group into upper and lower subdivisions, Locally underlain by Shuttleton Rhyolite Member.|Tuffaceous siltstone, sandstone, shale, rhyolite.|
16866|Shume Formation|71039|6|Mentioned|p18-p19|||||||||
16866|Shume Formation|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Amphitheatre Group.||Overlies CSA Siltstone.|Massive to parallel-laminated, lesser cross-laminated and minor graded, moderate to well-sorted, medium- to fine-grained, lithic-quartz to quartz-rich sandstone interbedded with siltstone. Minor rhyolitic, crystal to crystal-lithic rich pyroclastics.|
16866|Shume Formation|72908|5|Briefly described|p3, p7, p8 Tb.1, p18, p21, p29-30|Early Devonian|Early Devonian|Cobar Basin. Hosts the Mallee Bull, R7 prospect, Sandy Creek and Shuttleton deposits.||Amphitheatre Group|||Sequence of quartz-rich to quartz-lithic sandstones and siltstones including minor felsic volcanic and volcaniclastic rocks.|
16866|Shume Formation|72958|5|Briefly described|ps 5, 7-8, 11, 14, 21-23, 29-35, 60-61|Pragian|Pridoli|Cobar Basin. Nymagee area. Rhyolite WLRCDD043W1 boulder breccia sample (part of an olistostromal slump package) yielded a SHRIMP U-Pb age of 420.8 +/- 1.9 Ma, which constitutes a maximum depositional age for the formation. Previously (McRae, 1987) considered to be Lochkovian to Pragian, but dating of the Shuttleton Rhyolite Member at 421.9+/-2.1 Ma, suggests older Pridoli age, although this rhyolite may also be part of an allochthonous package. May correlate directly with the lower volcaniclastics of Edgecombe and Soininen (2019). Separates the lower and upper Amphitheatre Group.|420.8 +/- 1.9 Ma SHRIMP U-Pb|Amphitheatre Group|Shuttleton Rhyolite Member|Overlain by Amphitheatre Group, 'upper'. Correlates to Lerida Limestone Member (Biddabirra Formation).|Includes porphyritic rhyolite.|
16866|Shume Formation|73174|6|Mentioned|p1037|Lochkovian|Lochkovian|Cobar Basin.||Amphitheatre Group, Cobar Supergroup||||
16866|Shume Formation|73578|6|Mentioned|p2, p4, p11, p18|Early Devonian|Early Devonian|Cobar Basin. [Written as Biddabirra/Shume formation on p2]. Hosts intrusions related to mineralisation at Norma Vale prospect.||Amphitheatre Group, Cobar Supergroup|||Includes brecciated and sheared siltstones.|
16867|Shuttleton Rhyolite Member|22857|4|Described|p438 App.1, Tb.A1.6|Pragian|Lochkovian|Of the upper Amphitheatre Group (Cobar Supergroup). Felsic volcanics. Max. thickness: 400m. Geological Province: Cobar Basin.||||||
16867|Shuttleton Rhyolite Member|41528|2|Defined|p90|Early Devonian||||||||
16867|Shuttleton Rhyolite Member|41529|6|Mentioned|Map legend|Early Devonian||||||||
16867|Shuttleton Rhyolite Member|70876|4|Described|p1, p3, p16-p23, p76, p94|Devonian|Silurian|Cobar Basin. S-type geochemistry. Sampling details, petrography, zircon morphology, U-Pb isotopic results and geochronological interpretation are discussed.|421.9 +/- 2.7 Ma (SHRIMP U-Pb)|Shume Formation||Nonconformably overlies the Thule Granite.|Grey-green, moderately crystal-rich, porphyritic, coherent rhyolite.|
16867|Shuttleton Rhyolite Member|70950|6|Mentioned|p1034,1038|||Geological province: Central Lachlan Orogen.||Unit of Shume Formation, Amphitheatre Group.||Locally overlain by Shume Formation.||23-SEP-19
16867|Shuttleton Rhyolite Member|72958|5|Briefly described|p5, p14, p23, p29-30, p35, p60|Pridoli|Pridoli|Ca. 10-12 Ma age disparity from the host rock (Shume Formation) discussed.|421.9 +/- 2.7 Ma|Shume Formation, Amphitheatre Group||||
16867|Shuttleton Rhyolite Member|73578|6|Mentioned|p7, p14, p21|Pridoli|Ludfordian|Age of 421.9 +/- 2.7 Ma reported by Waltenberg et al. (2016).|421.9 +/- 2.7 Ma|||||
16876|Signal Hill Conglomerate Member|29922|6|Mentioned|p49|||||||||
16876|Signal Hill Conglomerate Member|29926|6|Mentioned|Fig.3|||||||||
16876|Signal Hill Conglomerate Member|33867|6|Mentioned|Fig.3|||||||||
16876|Signal Hill Conglomerate Member|34351|6|Mentioned|p343|||Fig.5.13||||||
16876|Signal Hill Conglomerate Member|37083|6|Mentioned|p164|||||||||
16876|Signal Hill Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
16876|Signal Hill Conglomerate Member|39308|6|Mentioned|Fig. 23.4|||||||||
16876|Signal Hill Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
16876|Signal Hill Conglomerate Member|43447|14|Not recorded|diag.p26,34|||Of Lambton Sub-Group||||||
16876|Signal Hill Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Bar Beach Formation. ||||
16884|Silver Gully Formation|721|5|Briefly described|Map legend|Givetian|Givetian|Of the Tamworth Group.  Coarse andesitic sandstone, diamictite, and pebble orthoconglomerate; subordinate andesitic tuff and andesitic to dacitic lava, ashflow tuff and agglomerate; minor limestone.||||||21-DEC-04
16884|Silver Gully Formation|22750|5|Briefly described|p 228||Early Devonian|Tamworth Group||||||
16884|Silver Gully Formation|22857|5|Briefly described|p482 App.1 Tb.A1.6|Emsian|Emsian|Of the Yarrimie Formation (Tamworth Group). Arenite, conglomerate, minor siltstone, limestone, mafic tuffs and lavas, spilite. Max. thickness: 850m. Geological Province: Tamworth Forearc Basin.||||||
16884|Silver Gully Formation|23185|6|Mentioned|Fig5p161,161-2|Eifelian|Emsian|||||||
16884|Silver Gully Formation|23522|5|Briefly described|p249 Fig 5|Eifelian|Emsian|||||||
16884|Silver Gully Formation|24009|5|Briefly described|p368 Fig.1||Emsian|||||||
16884|Silver Gully Formation|30650|3|Fully described|p315|||||||||
16884|Silver Gully Formation|30814|6|Mentioned|p71|||[Unit mistakenly indexed as being in SA. CEBApr97]||||||
16884|Silver Gully Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
16884|Silver Gully Formation|31999|5|Briefly described|p150|||Table 1||||||
16884|Silver Gully Formation|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
16884|Silver Gully Formation|32619|6|Mentioned|p461|||Early Dev.||||||
16884|Silver Gully Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
16884|Silver Gully Formation|33326|6|Mentioned|p446|||Fauna.||||||
16884|Silver Gully Formation|34553|6|Mentioned|p308|||Lower - Middle Devonian||||||
16884|Silver Gully Formation|34554|6|Mentioned|p232|||||||||
16884|Silver Gully Formation|35783|6|Mentioned|Fig.1|||Mineral deposits and geology of Nundle gold field.||||||
16884|Silver Gully Formation|36961|6|Mentioned|p208|||See also Fig.3||||||
16884|Silver Gully Formation|37803|5|Briefly described|p83|||||||||
16884|Silver Gully Formation|39331|6|Mentioned|Table 10-1|||||||||
16884|Silver Gully Formation|41009|6|Mentioned|Fig.2|||||||||
16884|Silver Gully Formation|41347|5|Briefly described|p385|||||||||
16884|Silver Gully Formation|41348|5|Briefly described|Map legend|Devonian|Devonian|Of the Tamworth Group.||||||16-DEC-04
16884|Silver Gully Formation|41796|6|Mentioned|p306|||||||||
16884|Silver Gully Formation|41941|6|Mentioned|p44|||||||||
16884|Silver Gully Formation|42376|4|Described|p35|||||||||
16884|Silver Gully Formation|42796|5|Briefly described|Fig.2 P31|||||||||
16884|Silver Gully Formation|42849|6|Mentioned|p542|||||||||
16884|Silver Gully Formation|42866|5|Briefly described|Table 2, P12|||||||||
16884|Silver Gully Formation|43091|5|Briefly described|Map legend|||of Tamworth Group||||||
16884|Silver Gully Formation|43400|2|Defined|p178-181,182,184||Couvinian|(M.Devn)||||||
16884|Silver Gully Formation|43406|14|Not recorded|p42,45,48||Middle Devonian|Formation of Tamworth Group||||||
16884|Silver Gully Formation|43407|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition) Part of Tamworth Group||||||
16884|Silver Gully Formation|43428|14|Not recorded|p138|||||||||
16884|Silver Gully Formation|43479|14|Not recorded|p151||Middle Devonian|||||||
16884|Silver Gully Formation|43525|14|Not recorded|Table p132||Eifelian|||||||
16884|Silver Gully Formation|43529|14|Not recorded|p236|||Ref. to Pedder 1967||||||
16884|Silver Gully Formation|47056|6|Mentioned|Fig.2 P523|||||||||
16884|Silver Gully Formation|50094|5|Briefly described|p316 Fig.1, p317 Fig.2|Emsian|Emsian|Overlies Wogarda Argillite.||||||
16884|Silver Gully Formation|50168|6|Mentioned|p157 Fig.2|||Gamilaroi Terrane.||||||
16884|Silver Gully Formation|61392|5|Briefly described|p165 Fig. 2|Eifelian|Eifelian|In the Gamilaroi terrane.||||||07-FEB-11
16884|Silver Gully Formation|61765|6|Mentioned|p59 Fig. 2, p60, p62|Devonian|Devonian|Includes Sulcor Limestone Member. Geological Province: Tamworth Belt.||||||07-FEB-11
16884|Silver Gully Formation|65214|6|Mentioned|p275, p278|Devonian|Devonian|NSW, Nundle. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
16884|Silver Gully Formation|68005|5|Briefly described|p49 Fig.3-M, p52, p150, p170.|Eifelian|Emsian|Tamworth Belt. The article states that Moore Creek and Timor Limestones are the same unit, having different names in the Attunga region (Moore Creek Limestone) and Loombrah and Timor region (Timor Limestone).||Unit in Tamworth Group.||Overlies Wogarda Argillite and Bog Hole Formation. Is intruded by, and interbedded with, Folly Volcanics. Is overlain by Yarrimie Formation.|Coarse andesitic sandstone, diamictite and pebble orthoconglomerate; subordinate andesitic tuff and andesitic to dacitic lava, ashflow tuff and agglomerate; minor limestone and calc-silicate hornfels.|
16884|Silver Gully Formation|69639|6|Mentioned|p211, p218|Devonian|Devonian|||||Intruded by the Attunga Creek Monzogranite.||
16884|Silver Gully Formation|71628|5|Briefly described|p7: 19, 23, 31|||Hosts two small Au vein deposits (likely sourced from Inlet Monzogranite).||||Is intruded by Inlet and Moonbi Monzogranites.||
16884|Silver Gully Formation|73440|6|Mentioned|p132|||||||||
16898|Silverdale Formation|13996|5|Briefly described|p143, p146|Silurian|Silurian|Hattons Corner.|||Barrandella Shale Member.|||
16898|Silverdale Formation|22486|5|Briefly described|p 5, 6|||||||||
16898|Silverdale Formation|22857|5|Briefly described|p460 App.1 Tb.A1.6|Ludlovian|Ludlovian|Of the Hattons Corner Group. Contains rich fauna: important corals and conodonts. Max. thickness: 170.5m. Geological Province: Canberra-Yass Shelf.||||||
16898|Silverdale Formation|24248|5|Briefly described|p52, p50 Fig.1|Gorstian|Gorstian|Overlain by Black Bog Shale. Underlain by Laidlaw Volcanics. Geological Province: Yass Syncline.||||||02-JUN-08
16898|Silverdale Formation|29791|6|Mentioned|p117|||||||||
16898|Silverdale Formation|30069|5|Briefly described|p5|||||||||
16898|Silverdale Formation|30332|6|Mentioned|p116|||See also Table 1.||||||02-JUN-08
16898|Silverdale Formation|30731|6|Mentioned|Map legend|Silurian|Silurian|||||||
16898|Silverdale Formation|30734|6|Mentioned|p18|||||||||
16898|Silverdale Formation|31852|6|Mentioned|p718|||See also p720 and Figs. 1,2,4,5. Upper Silurian.||||||02-JUN-08
16898|Silverdale Formation|32624|6|Mentioned|p715|||Refers Link (1970).||||||02-JUN-08
16898|Silverdale Formation|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Strat. Nomenclature.||||||02-JUN-08
16898|Silverdale Formation|32820|6|Mentioned|Table 1|||Refers Pogson & Baker (1974)||||||
16898|Silverdale Formation|33116|6|Mentioned|Fig.11|||Correlation.||||||02-JUN-08
16898|Silverdale Formation|33325|5|Briefly described|Table 2|||||||||
16898|Silverdale Formation|33328|6|Mentioned|p15|||||||||
16898|Silverdale Formation|33606|6|Mentioned|p67|||||||||
16898|Silverdale Formation|33611|6|Mentioned|p132|||||||||
16898|Silverdale Formation|34692|6|Mentioned|p186|||||||||
16898|Silverdale Formation|35244|6|Mentioned|p36|||||||||
16898|Silverdale Formation|35384|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
16898|Silverdale Formation|35386|3|Fully described|p27|||||||||
16898|Silverdale Formation|35501|6|Mentioned|p156|||||||||
16898|Silverdale Formation|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition.||||||02-JUN-08
16898|Silverdale Formation|36413|6|Mentioned|Table 3|||||||||
16898|Silverdale Formation|37727|4|Described|p84|||See also p8 and p31.||||||02-JUN-08
16898|Silverdale Formation|37752|6|Mentioned|p105|||||||||
16898|Silverdale Formation|38035|6|Mentioned|p91|||||||||
16898|Silverdale Formation|38151|6|Mentioned|Table 1|||||||||
16898|Silverdale Formation|38230|5|Briefly described|p474|||Palaeontology||||||
16898|Silverdale Formation|38691|5|Briefly described|Fig.1|||||||||
16898|Silverdale Formation|39331|6|Mentioned|Fig.5-5|||||||||
16898|Silverdale Formation|39975|6|Mentioned|Table 1|||||||||
16898|Silverdale Formation|40328|4|Described|p110|||||||||
16898|Silverdale Formation|41260|4|Described|p116|||||||||
16898|Silverdale Formation|42029|5|Briefly described|Fig.1 P96|||||||||
16898|Silverdale Formation|42820|6|Mentioned|p29|||||||||
16898|Silverdale Formation|42994|6|Mentioned|p61|||||||||
16898|Silverdale Formation|43575|6|Mentioned|Fig.14,p283|||||||||
16898|Silverdale Formation|45075|5|Briefly described|p6|||Fauna||||||
16898|Silverdale Formation|45147|6|Mentioned|M152|||See also M153||||||
16898|Silverdale Formation|47037|6|Mentioned|p107|||||||||
16898|Silverdale Formation|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Hattons Corner Group.  Comprises 3 members: Bowspring, Barrandella and Hume Limestone Members.  Overlies Yanawe Formation.||||||
16898|Silverdale Formation|60988|6|Mentioned|p143 |Ludlovian|Ludlovian|Contains Ludlow brachiopods.||||||
16898|Silverdale Formation|61894|5|Briefly described|p180 |Late Silurian|Late Silurian|Hattons Corner, Yass district.|||Bowspring, Hume, Limestone Members.|||
16898|Silverdale Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hattons Corner Group. Includes Barrandella Shale, Hume Limestone and Bowspring Limestone Members.||||||12-JUN-08
16898|Silverdale Formation|66197|5|Briefly described|p631, p631 Fig.3b|Ludlow||Canberra-Yass Basin. Shallow marine sedimentary rocks in the lower Ludlow and deeper marine in the upper Ludlow.||||Overlies the Laidlaw Volcanics. Underlies the Hattons Corner Group.||14-MAR-12
16898|Silverdale Formation|67820|6|Mentioned|p136 Fig.3|Silurian|Silurian|||Hattons Corner Group.||||
16898|Silverdale Formation|68592|1|Redefined|p430 Fig.89, p513, p542, p560-2, p566-82|Ludfordian|Gorstian|See also p1877-80. Redefined. Link (1970, 1971); Link and Druce (1972); unit in their Hattons Corner Group. They also included Gums Road Limestone Member and Tullerah Sandstone Member, which are here transferred to the Yanawe Formation. Revised type section described. Lacks volcanic-rich sediments: the essential distinguishing feature separating this unit from the underlying Douro Group. 55-164m thick. Richly fossiliferous: fauna described.||Unit in redefined Hattons Corner Group.|Includes Bowspring and Hume, Limestone Members; Barrandella Shale Member.|Conformably overlies Yanawe Formation. Is overlain conformably by Black Bog Shale.|Basal persistent, well-bedded, semi-nodular, fossiliferous limestone with shale interbeds; overlain by shaly mudstone with thin beds of turbiditic siltstone, calcareous siltstone and shale; topped by biomicrite interbedded with shaly mudstone.|
16898|Silverdale Formation|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shs[3 asterisks]. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Hattons Corner Group|Includes Bowspring Limestone Member, Hume Limestone Member, Barrandella Shale Member.|Is overlain by Black Bog Shale. Overlies Yanawe Formation (Douro Group).|Well bedded, semi-nodular, fossiliferous limestone with shale interbeds; shaly mudstone; minor siltstone and calcareous siltstone.|
16898|Silverdale Formation|70540|5|Briefly described|Map Legend|Devonian|Silurian|||Hattons Corner Group|Includes Bowspring Limestone Member, Hume Limestone Member, Barrandella Shale Member.||Well bedded, semi-nodular, fossiliferous limestone with shale interbeds; shaly mudstone; minor siltstone and calcareous siltstone.|
16898|Silverdale Formation|70546|5|Briefly described|Map Legend|Devonian|Silurian|||Hattons Corner Group|Includes Bowspring Limestone Member, Hume Limestone Member, Barrandella Shale Member||Well bedded, semi nodular fossiliferous limestone with shale interbeds, shaly mudstone; minor siltstone and calcareous siltstone.|
16898|Silverdale Formation|71656|4|Described|p12 Fig.2, p19, p23, p52|Ludlow|Ludlow|Fossils including brachipods, dendroid graptoloids and conodonts are found SSW of Wellington in central west NSW.||Hattons Corner Group|Includes Hume Limestone Member, Barrandella Shale Member, Bowspring Limestone Member.|Hattons Corner Group. Overlies Yanawe Formation and underlies Black Bog Shale.|Fossiliferous limestone.|
16898|Silverdale Formation|73582|6|Mentioned|p113|||Yass district. Mentioned as age-equivalent to Jenolan Caves Limestone.||Hattons Corner Group||||
16903|Silverwood Group|22601|6|Mentioned|405|Devonian|Devonian|||||||
16903|Silverwood Group|23423|5|Briefly described|p267|||||||||
16903|Silverwood Group|23811|5|Briefly described|Map Legend|Emsian|Pridoli|Tuffaceous mudstone, fine-grained, intermediate to basic igneous rocks with minor lithic wacke, foliated metaclaystone and metasiltstone, conglomerate, limestone breccia, chert and jasper.||||||20-DEC-04
16903|Silverwood Group|23812|4|Described|p9|Devonian|Silurian|Same as Willowie Creek beds of Fergusson, (1984), which are included in the group.||||||
16903|Silverwood Group|24612|5|Briefly described|p12|Devonian|Devonian|Contains Carlinastraea fauna.||||||06-APR-05
16903|Silverwood Group|30914|6|Mentioned|Map legend|Devonian|Devonian|||||||
16903|Silverwood Group|31694|6|Mentioned|p346|||||||||
16903|Silverwood Group|31802|6|Mentioned|p137|||||||||
16903|Silverwood Group|31999|4|Described|p150|||Fig. 2||||||
16903|Silverwood Group|32359|5|Briefly described|p736|||||||||
16903|Silverwood Group|32360|6|Mentioned|p748|||||||||
16903|Silverwood Group|32491|5|Briefly described|p7|Early Devonian|Silurian|||||||
16903|Silverwood Group|32492|6|Mentioned|Map legend|Early Devonian|Silurian|Silurian to Lower Devonian.||||||14-APR-08
16903|Silverwood Group|32494|6|Mentioned|p84|||||||||
16903|Silverwood Group|32880|6|Mentioned|p2|||Dev.||||||
16903|Silverwood Group|33091|6|Mentioned|p6|||Refers Olgers &  Flood (1970)||||||
16903|Silverwood Group|33146|5|Briefly described|p2|||See also P3. ?Sil.-L.Dev.||||||
16903|Silverwood Group|33436|6|Mentioned|p243|||Devonian. Refers Lucas (1959).||||||
16903|Silverwood Group|33437|6|Mentioned|p61|||L.Dev. Conodonts also on PP62-68||||||
16903|Silverwood Group|33476|6|Mentioned|p50|||||||||
16903|Silverwood Group|33561|6|Mentioned|p102|||||||||
16903|Silverwood Group|33703|6|Mentioned|p207|||||||||
16903|Silverwood Group|34479|6|Mentioned|p309|||See also P312. Devonian||||||
16903|Silverwood Group|35311|6|Mentioned|p207|||||||||
16903|Silverwood Group|35652|4|Described|p5|||||||||
16903|Silverwood Group|36045|6|Mentioned|p325|||||||||
16903|Silverwood Group|36716|6|Mentioned|p141|||||||||
16903|Silverwood Group|36961|6|Mentioned|p205|||||||||
16903|Silverwood Group|37252|6|Mentioned|Map legend|Devonian|Devonian|||||||
16903|Silverwood Group|37509|6|Mentioned|p504|||||||||
16903|Silverwood Group|38806|6|Mentioned|p71|||||||||
16903|Silverwood Group|39445|6|Mentioned|p67|||Early Devonian with Late Ord. limestone blocks. See also Fig.8 & Table 5||||||
16903|Silverwood Group|39673|6|Mentioned|Fig. 3a|||||||||
16903|Silverwood Group|40245|6|Mentioned|p198|||||||||
16903|Silverwood Group|40246|6|Mentioned|p164|||||||||
16903|Silverwood Group|40435|6|Mentioned|p49|||||||||
16903|Silverwood Group|40514|6|Mentioned|p4|||||||||
16903|Silverwood Group|40960|6|Mentioned|p216|||||||||
16903|Silverwood Group|42031|5|Briefly described|Fig.8 P766|||||||||
16903|Silverwood Group|42140|6|Mentioned|p560|||||||||
16903|Silverwood Group|42297|6|Mentioned|Fig. 5 P5|Devonian||||||||
16903|Silverwood Group|42559|5|Briefly described|p7|||||||||
16903|Silverwood Group|42997|6|Mentioned|p38|||||||||
16903|Silverwood Group|43008|5|Briefly described|map legend|||||||||
16903|Silverwood Group|43083|6|Mentioned|p39|||Includes Rosenthal Creek Formation.  In the Warwick-Stanthorpe area.||||||17-JUN-09
16903|Silverwood Group|43461|14|Not recorded|Table p618|Middle Devonian|Early Devonian|L.-L.M.Dev||||||
16903|Silverwood Group|43745|6|Mentioned|Fig.4,p13|||||||||
16903|Silverwood Group|44070|14|Not recorded|p141|||||||||
16903|Silverwood Group|44091|14|Not recorded|p34|Middle Devonian|Early Devonian|||||||
16903|Silverwood Group|44093|5|Briefly described|p119|Early Devonian|Early Devonian|||||||
16903|Silverwood Group|44269|14|Not recorded|p14||Devonian|Lower or Middle Devonian.||||||
16903|Silverwood Group|44429|14|Not recorded|p228-229|||See also Lexicon.||||||
16903|Silverwood Group|44512|14|Not recorded|p15,16||Devonian|Ref. to Lucas 1960. See also Lexicon.||||||
16903|Silverwood Group|44563|14|Not recorded|p142-143|||See also Lexicon.||||||
16903|Silverwood Group|44783|14|Not recorded|p2,43-45|||||||||
16903|Silverwood Group|44786|14|Not recorded|p193-202|Middle Devonian|Early Devonian|||||||
16903|Silverwood Group|48940|6|Mentioned|p12|||Refers Richards & Bryan (1923)||||||
16903|Silverwood Group|60937|5|Briefly described|p424 Fig. 2|||||||||
16903|Silverwood Group|61392|3|Fully described|p163-165, p166|Early Carboniferous|Middle Cambrian|Also referred to as the Keinjan Terrane. Incl: Risdon Stud Fm, Connolly Volcs, Bald Hill Fm, Ormoral Volcs and Bromley Hills Fm. Comprises various lithologies. Effectively the same sequence as Willowie Creek beds.||||||07-FEB-11
16903|Silverwood Group|63731|5|Briefly described|Map legend|Devonian|Silurian|Includes Risodon Stud and Bald Hill Formations, Connolly, Ormoral and Bromley Hills Volcanics.||||||
16903|Silverwood Group|63732|5|Briefly described|Map legend|Devonian|Silurian|Mafic-dominated volcaniclastic deposits, lavas and subvolcanic metabasite sills; massive to thin-bedded volcaniclastic and epiclastic sediments+some chert; local conglom.+debris-flow deposits. Fine-gr.metadolerite and metabasalt.||||||
16903|Silverwood Group|63748|4|Described|p6, p7 Fig. 3|Paleozoic|Paleozoic|Formerly incl: Risdon Stud Fm, Connolly Volcs + Rosenthal Fm. Revised by Van Noord (1999b) to retain Risdon Stud Fm + Connolly Volcs but remainder now divided into Bald Hill Fm overlain by Omoral Volcanics + Bromley Hills Fm. Geol.prov:Silverwood Province||||||07-FEB-11
16903|Silverwood Group|68553|6|Mentioned|Map legend; schematic diagram.|Early Devonian|Silurian|Silverwood Province.||||||
16903|Silverwood Group|68679|5|Briefly described|p321, p444-447, p452-453, p455-456|Devonian|Silurian|Silverwood Province, northern New England Orogen. An oceanic arc sequence. Exposed as a roughly triangular area ~100 km2 between Warwick and the NSW border. Previously included the Rosenthal Creek Formation (Olgers et al., 1974), but this unit was divided by Van Noord (1999) into the three upper units. RELATED UNITS (continued): Is intruded by Herries Granite.|||Risdon Stud Formation, Connolly Volcanics, Bald Hill Formation, Ormoral Volcanics and Bromley Hills Formation.|Is faulted against the Eurydesma, Condamine, Wallaby, Eight Mile Creek, Rhyolite Range, beds (or is overlain unconformably by these last two). Equivalent to Willowie Creek beds in NSW. See COMMENTS.|Marine volcaniclastic, clastic and volcanic rocks.|
16903|Silverwood Group|68822|6|Mentioned|p336|||||||||
16903|Silverwood Group|68901|5|Briefly described|p8 Fig. iii|Devonian|Silurian|Silverwood Province.||||||27-SEP-18
16903|Silverwood Group|69639|6|Mentioned|p151|||||||Intruded by the Maryland Granite.|Sediments.|
16903|Silverwood Group|71628|5|Briefly described|p9:11-13, 15, 19, 23, 25, 27, 35; p11-26|Devonian|Silurian|See also p15: 33, 57, 69; p16-4; p18-13; p19: 59, 67, 97, 128, 147-148, 163. Apparently equivalent to Willowie Creek beds [?Beds] of Fergusson (1984). RELATED UNITS (continued): Is also intruded by Cullendore Syenogranite and all units of Dumbudgery Creek Complex. Is faulted against The Ridge Monzogranite.|||Connolly Volcanics; Bald Hill, Risdon Stud Formations; Willowie Creek beds.|Is intruded by Towgon Grange and Kaloe Tonalites, Rocky River and Moonta Gully Monzogranites, Mount Lindesay Monzogranite (Stanthorpe Complex). See COMMENTS for more.|Mafic to intermediate tuffs, flows and shallow intrusives with intercalated conglomerates, sandstones, tuffaceous argillites and altered limestones.|
16903|Silverwood Group|73143|6|Mentioned|p14|Early Devonian|Ludlow|Contains Heliolites tabulate coral (Jones and Hill, 1940).||||||
16903|Silverwood Group|73197|5|Briefly described|p460 Fig.1, p463, p464 Fig.3|Late Devonian|Silurian|New England Orogen, southern. Fragments of the obducted Silurian-late Devonian Calliope-Gamilaroi Oceanic Arc. Lithologies described are in relation to various outcrops of the Silverwood Group, Calliope Province and Gamilaroi Terrane.|||||Mix of rock types including felsic volcanic rocks and tuff, volcaniclastic sandstone and conglomerate, limestone, mudstone and, in the upper sequences, pillow basalt and dolerite.|
16939|Singleton Supergroup|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Contains the Wollombi and Wittingham Coal Measures. Geological Province: Sydney Basin.||||||
16939|Singleton Supergroup|22969|5|Briefly described|Fig 2.2|Late Permian|Late Permian|||||||
16939|Singleton Supergroup|37773|5|Briefly described|Table 2|||||||||
16939|Singleton Supergroup|39232|6|Mentioned|p110|||||||||
16939|Singleton Supergroup|39653|6|Mentioned|p69|||||||||
16939|Singleton Supergroup|39666|6|Mentioned|p65|||||||||
16939|Singleton Supergroup|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
16939|Singleton Supergroup|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
16939|Singleton Supergroup|40268|6|Mentioned|Fig.1a|||[Originally entered for Antarctica. CEBMar95]||||||
16939|Singleton Supergroup|40321|6|Mentioned|p17|||||||||
16939|Singleton Supergroup|40602|6|Mentioned|p7|||||||||
16939|Singleton Supergroup|40805|5|Briefly described|p142|||||||||
16939|Singleton Supergroup|40807|6|Mentioned|p161|||||||||
16939|Singleton Supergroup|41348|5|Briefly described|Map legend|Permian|Permian|||||||16-DEC-04
16939|Singleton Supergroup|41834|6|Mentioned|p590|||||||||
16939|Singleton Supergroup|41902|5|Briefly described|p5 Table 1|||||||||
16939|Singleton Supergroup|42078|6|Mentioned|p4|||See also Table 1||||||
16939|Singleton Supergroup|42378|5|Briefly described|p19|||||||||
16939|Singleton Supergroup|42916|5|Briefly described|Table 1||Late Permian|||||||
16939|Singleton Supergroup|42925|5|Briefly described|Table 1||Late Permian|||||||
16939|Singleton Supergroup|42945|6|Mentioned|p27|||||||||
16939|Singleton Supergroup|43017|6|Mentioned|p379|||||||||
16939|Singleton Supergroup|43050|5|Briefly described|p12|||||||||
16939|Singleton Supergroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Hunter region, Sydney Basin. Contains Wittingham and Wollombi Coal Measures and Watts Sandstone.||||||
16939|Singleton Supergroup|43257|5|Briefly described|Map Legend||Permian|||||||
16939|Singleton Supergroup|44244|5|Briefly described|p234|Late Permian|Late Permian|Includes the Wittingham Coal Measures, and Wollombi Coal measures.  Max. thickness: 1500m.  Geological Province: Sydney Basin.  See also p235 Tb. 3.||||||26-AUG-04
16939|Singleton Supergroup|44450|5|Briefly described|p147 Fig 43|Permian|Permian|Geological Province: Sydney Basin.||||||
16939|Singleton Supergroup|50268|6|Mentioned|Map Legend|||||||||
16939|Singleton Supergroup|60281|5|Briefly described|Fig. 7 Appendix 1|Late Permian|Late Permian|Includes the Newcastle and Tomago Coal Measures.  Geological Province: Sydney Basin.||||||
16939|Singleton Supergroup|61772|6|Mentioned|p129, p131, p132, p133||Late Permian|Contains abundant tuffs and juvenile volcanogenic sediments.||||||24-SEP-08
16939|Singleton Supergroup|62033|5|Briefly described|p24|||The Coalfield Geology Council in 2004 ratified the resolution that this supergroup in the Hunter Valley should now comprise Newcastle C.M., Watts Sandstone and the Wittingham C.M.||||||14-MAR-07
16939|Singleton Supergroup|67663|5|Briefly described|p520 Tb.1|Permian|Permian|Late Permian. Also appears as Singleton Super Group on p520.|||Includes Denman Formation, Bulga Formation.|Unconformably overlain by the Narrabeen Group. Underlain by the Maitland Group.||
16939|Singleton Supergroup|68003|5|Briefly described|p38 Fig.3-j, p130. |Late Permian|Late Permian|Hunter Coalfield, Brigalow Belt South Bioregion. Correlative of Black Jack Group (Gunnedah Basin) and Illawarra Coal Measures (Western Coalfield).|||Includes Wittingham and Wollombi Coal Measures, and Murulla beds.|Overlies Maitland Group. Is overlain by Narrabeen Group.||
16939|Singleton Supergroup|68004|5|Briefly described|p23 Table 1, p51.|||Hunter Coalfield. Equivalent to Black Jack Group (Gunnedah Basin), Illawarra Coal Measures (Western and Southern Coalfields) and Tomago and Newcastle Coal Measures (Newcastle Coalfield). About 1500 m thick.|||Includes Wittingham and Wollombi Coal Measures.|Overlies Maitland Group. Is overlain by Narrabeen Group.||
16939|Singleton Supergroup|68005|5|Briefly described|p133.|Permian|Permian|Hunter Coalfield.|||Includes Murula beds.|||
16939|Singleton Supergroup|69683|6|Mentioned|p411 Fig.2|Late Permian|Late Permian||||Includes Wittingham and Newcastle, Coal Measures; Waratah and Watts, Sandstones.|||
16939|Singleton Supergroup|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian coal measures: conglomerate, quartzose and lithic sandstone, siltstone, carbonaceous and calcareous mudstone, tuff and coal.||||||
16939|Singleton Supergroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.|||Includes Newcastle Coal Measures, Tomago Coal Measures.|||
16939|Singleton Supergroup|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
16939|Singleton Supergroup|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield and north Werrie Basin.|||Wittingham, Newcastle, Coal Measures; Toll Bar Formation.|||
16939|Singleton Supergroup|73304|6|Mentioned|p75|||||||||
16963|Skeletar Formation|22601|6|Mentioned|409|Permian|Permian|Geol province Sydney Basin||||||
16963|Skeletar Formation|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Greta Coal Measures. Pellet claystone, siltstone, chert. Max. thickness:120m. Geological Province: Sydney Basin.||||||
16963|Skeletar Formation|22969|4|Described|Fig 4.1a||Early Permian|||||||
16963|Skeletar Formation|23350|4|Described|263|||Proposed that Skeletar Formation and Gyarran Volcanics are combined to form the Dalwood Group (1994).||||||15-JUL-04
16963|Skeletar Formation|31880|6|Mentioned|p18|||||||||
16963|Skeletar Formation|31881|4|Described|p340|||Refers Raggatt (1938) & Robinson (1963)||||||
16963|Skeletar Formation|31882|6|Mentioned|p244|||Gyarran Volcanics||||||
16963|Skeletar Formation|34015|4|Described|p328|||Permian||||||
16963|Skeletar Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
16963|Skeletar Formation|34292|6|Mentioned|Table 1|||Permian||||||
16963|Skeletar Formation|34345|6|Mentioned|Fig.5.7|||Permian||||||
16963|Skeletar Formation|34614|6|Mentioned|p29|||||||||
16963|Skeletar Formation|36042|6|Mentioned|Table 1|||||||||
16963|Skeletar Formation|36940|6|Mentioned|p141|||||||||
16963|Skeletar Formation|37773|5|Briefly described|p18|||||||||
16963|Skeletar Formation|38614|6|Mentioned|Fig.6|||||||||
16963|Skeletar Formation|39287|6|Mentioned|Fig. 2.5|||||||||
16963|Skeletar Formation|39288|6|Mentioned|Fig. 3.3|||||||||
16963|Skeletar Formation|39346|6|Mentioned|Map legend|Middle Permian|Middle Permian|||||||
16963|Skeletar Formation|39664|6|Mentioned|p117|||See also Table 8||||||
16963|Skeletar Formation|40166|5|Briefly described|p345|||||||||
16963|Skeletar Formation|40331|6|Mentioned|p3|||||||||
16963|Skeletar Formation|41054|6|Mentioned|p156|||See also Fig.3||||||
16963|Skeletar Formation|41264|6|Mentioned|p251|||||||||
16963|Skeletar Formation|41834|6|Mentioned|p590|||||||||
16963|Skeletar Formation|41902|5|Briefly described|p5 Table 1|||||||||
16963|Skeletar Formation|42182|6|Mentioned|p298|||||||||
16963|Skeletar Formation|42916|5|Briefly described|Table 1||Early Permian|||||||
16963|Skeletar Formation|42925|5|Briefly described|Table 1||Early Permian|||||||
16963|Skeletar Formation|43017|5|Briefly described|Fig.1,p372|||||||||
16963|Skeletar Formation|43194|5|Briefly described|p100, p129 Tb. 8.3|Early Permian|Early Permian|Basal unit of Greta Coal Measures (Sydney Basin). Correlative of Leard Formation, Gunnedah Basin.||||||
16963|Skeletar Formation|43257|5|Briefly described|Map Legend||Early Permian|Of Greta Coal Measures.||||||
16963|Skeletar Formation|43477|14|Not recorded|p15,35,38,39,61,PL.3|||See also Lexicon. Unit of Greta Coal Measures.||||||
16963|Skeletar Formation|44244|5|Briefly described|p232|Permian|Permian|Of the Greta Coal Measures.  Conformably overlies the Gyarran Volcanics.||||||
16963|Skeletar Formation|45090|6|Mentioned|p7|||Time correlation chart||||||
16963|Skeletar Formation|61315|5|Briefly described|Table SY1|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin/Hunter Valley area.||||||
16963|Skeletar Formation|61529|5|Briefly described|p854 Fig. 1b|Early Permian|Early Permian|Of the Greta Coal Measures. Geological Province: Sydney Basin.||||||
16963|Skeletar Formation|68003|5|Briefly described|p38 Fig.3-j.|Early Permian|Early Permian|Hunter Coalfield, Brigalow Belt South Bioregion.||Lower unit in Greta Coal Measures.||Overlies Farley Formation. Is overlain by Rowan Formation.||
16963|Skeletar Formation|68004|5|Briefly described|p23 Table 1, p51 Table 5.|||Hunter Coalfield.||Lower unit in Greta Coal Measures.||Overlies Farley Formation. Is overlain by Rowan Formation.|Pellet claystone, siltstone and chert.|
16963|Skeletar Formation|69683|6|Mentioned|p411 Fig.2|Early Permian.|Early Permian.|Hunter Coalfield; Muswellbrook area.||Unit in Greta Coal Measures.||||
16963|Skeletar Formation|70791|5|Briefly described|p277, p286-287, p293 Fig.17|Cisuralian|Cisuralian|Hunter Coalfield and north Werrie Basin.||Greta Coal Measures.|Glenara, Loder, Lewis, Balmoral, Coal Members.|||
16963|Skeletar Formation|73304|6|Mentioned|p75, p78|||||Greta Coal Measures||||
17001|Sloggets Granite|23214|4|Described|p259|Carboniferous|Carboniferous|Part of Oberon Granite complex.  Intrudes Rockley Volcanics.||||||
17001|Sloggets Granite|42712|4|Described|Table1p13; Fig3p9|Carboniferous|Early Carboniferous|||||||
17001|Sloggets Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
17001|Sloggets Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|||||||
17001|Sloggets Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Oberon Supersuite||||
17002|Slowmans Creek Conglomerate|22472|5|Briefly described|p40|||||||||
17002|Slowmans Creek Conglomerate|22857|5|Briefly described|p492 App.1 Tb.A1.7|Devonian|Devonian|Of the Lambie Group. Red, purple, clast-supported oligomictic conglomerate, mudstone, arenite. Max. thickness: 150m. Geological Province: Lambie Basin.||||||
17002|Slowmans Creek Conglomerate|23214|3|Fully described|p241|Late Devonian|Late Devonian|Of the Lambie Group, Lambie Basin. Now includes the Mount Horrible Conglomerate, Winburndale Member and Bald Hill Conglomerate.  Underlying unit: Gibbons Creek Sandstone. Max. thickness: 285m.||||||
17002|Slowmans Creek Conglomerate|32708|6|Mentioned|Fig.2|||||||||
17002|Slowmans Creek Conglomerate|35166|6|Mentioned|Fig.3|||||||||
17002|Slowmans Creek Conglomerate|35246|6|Mentioned|p172|||||||||
17002|Slowmans Creek Conglomerate|43641|5|Briefly described|Map Legend||Devonian|||||||
17002|Slowmans Creek Conglomerate|43782|5|Briefly described|Map Legend|Famennian|Famennian|of Lambie Group.||||||
17002|Slowmans Creek Conglomerate|68592|5|Briefly described|p1742|||In the Bathurst 1:250 000 map area, present on both limbs of the syncline in the type area. A possible correlate of Cowpers Creek Conglomerate.|||||A discontinuous conglomerate unit.|
17002|Slowmans Creek Conglomerate|70297|5|Briefly described|map legend|Late Devonian|Late Devonian|Shown as Slowmans Ck Cgl.||Lambie Group||||
17026|Snake Creek Mudstone Member|13516|5|Briefly described|p159, p162-163, p169, p138|Middle Triassic|Middle Triassic|From Bowen Basin||Of Moolayember Formation||Diachronous boundaries with rest of Moolayember Formation and underlying Showgrounds Sandstone.||
17026|Snake Creek Mudstone Member|23740|5|Briefly described|p1221|||Parent: Moolayenber Formation.  Geological Province: Bowen Basin||||||
17026|Snake Creek Mudstone Member|24159|5|Briefly described|p148 Fig.2, p149|Middle Triassic|Middle Triassic|Overlies the Showgrounds Sandstone. Geological Province: Bowen Basin.||||||
17026|Snake Creek Mudstone Member|29385|6|Mentioned|p82|||||||||
17026|Snake Creek Mudstone Member|29721|6|Mentioned|p70|||||||||
17026|Snake Creek Mudstone Member|31115|6|Mentioned|p35|||||||||
17026|Snake Creek Mudstone Member|31116|4|Described|p20|||||||||
17026|Snake Creek Mudstone Member|31369|2|Defined|p88|Middle Triassic|Middle Triassic|See also p33.||||||
17026|Snake Creek Mudstone Member|35295|6|Mentioned|p601|||||||||
17026|Snake Creek Mudstone Member|39491|6|Mentioned|p23|||||||||
17026|Snake Creek Mudstone Member|39494|6|Mentioned|Fig.5|||||||||
17026|Snake Creek Mudstone Member|40030|6|Mentioned|Fig.5|||||||||
17026|Snake Creek Mudstone Member|40120|6|Mentioned|p424|||||||||
17026|Snake Creek Mudstone Member|40249|6|Mentioned|p38|||||||||
17026|Snake Creek Mudstone Member|40544|6|Mentioned|p161|||||||||
17026|Snake Creek Mudstone Member|40767|6|Mentioned|p13|||||||||
17026|Snake Creek Mudstone Member|41188|6|Mentioned|p231|||||||||
17026|Snake Creek Mudstone Member|41247|6|Mentioned|Fig.7|||||||||
17026|Snake Creek Mudstone Member|42634|6|Mentioned|p11|||||||||
17026|Snake Creek Mudstone Member|61313|6|Mentioned|p105|||?Of the Showgrounds Sandstone? Equivalent to Digby Formation and the shales of Napperby Formation. Geological Province: Surat Basin.||||||
17026|Snake Creek Mudstone Member|61377|5|Briefly described|p151|Middle Triassic|Middle Triassic|A uniform dark grey-black shale. Conformably overlies Showgrounds Sandstone; conformably overlain by the Moolayember Formation. Provides a good regional seal for Showgrounds Sandstone reservoirs. Geological Province: Surat Basin.||||||15-JUL-13
17026|Snake Creek Mudstone Member|61612|6|Mentioned|p276, p277, p270 Fig. 1|Middle Triassic|Middle Triassic|Of Moolayember Formation. QLD. Lacustrine flooding event.||||||17-MAR-09
17026|Snake Creek Mudstone Member|64856|4|Described|p42, p70 Fig.17, p73-77, p102|Middle Triassic|Middle Triassic|Defined by Hogetoorn (1970). Predominantly dark grey to black mudstone with minor laminae and thin beds of very fine grained sandstone. Bottom unit of the Moolayember Formation, conformably overlies Clematis Group, Showgrounds Sandstone. Palynoflora age APT31-32 (235-240 Ma). 41m thick.|| ||||29-NOV-17
17026|Snake Creek Mudstone Member|64857|4|Described|p126-128, 129, 134, p113 Fig. 3|Triassic|Triassic|Bowen Basin. Member of the Moolayember Formation. Consists mainly of mudstone with minor very fine grained quartzose sandstone. Conformable on Showgrounds Sandstone. Genetically related to underlying Showgrounds Sandstone, rather than overlying Moolayember Formation.||||||
17026|Snake Creek Mudstone Member|64858|6|Mentioned|p180 Fig.2|Middle Triassic|Middle Triassic|Of Moolayember Formation?||||||16-MAR-12
17026|Snake Creek Mudstone Member|64859|5|Briefly described|p222-3, p225, 226, 193, 196, |Triassic|Triassic|Of Moolayember Formation.||||||
17026|Snake Creek Mudstone Member|65115|5|Briefly described|p426, 427|||of Moolayember Formation. Widespread lacustrine sediments.||||||
17026|Snake Creek Mudstone Member|65116|6|Mentioned|p451|Middle Triassic|Middle Triassic|||||||
17026|Snake Creek Mudstone Member|66615|6|Mentioned|p2 Fig.1|||Southern Taroom Trough, Bowen Basin.||Unit in Moolayember Formation.||Overlies Showgrounds Sandstone.||
17026|Snake Creek Mudstone Member|68576|5|Briefly described|Q_4: p3, p21|Middle Triassic|Middle Triassic|Roma Shelf, Bowen Basin.||Moolayember Formation.||Overlies Clematis Group.|Mainly dark grey to black mudstone with minor laminae and thin beds of very fine-grained quartzose sandstone.|
17026|Snake Creek Mudstone Member|68679|5|Briefly described|p377, p383|Middle Triassic|Middle Triassic|Lake deposits.||Basal Moolayember Formation.|||Mudstone with lesser siltstone and sandstone.|
17026|Snake Creek Mudstone Member|72297|5|Briefly described|p744-745|||Bowen Basin. Lacustrine deposits. Potential hydrocarbon source rock. Forms a significant regional seal throughout the Basin.||Moolayember Formation.||||
17035|Snapper Point Formation|22447|4|Described|p624, Fig.1 p624||Early Permian|Shallow marine||||||
17035|Snapper Point Formation|22529|6|Mentioned|9|Mesozoic|Permian|||||||
17035|Snapper Point Formation|22591|5|Briefly described|p 57, 65||Early Permian|||||||
17035|Snapper Point Formation|22663|5|Briefly described|NSW97 - 1 p2||Early Permian|||||||01-MAR-10
17035|Snapper Point Formation|22857|4|Described|p528 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Shoalhaven Group. Sandstone, siltstone and conglomerate. Disconformably overlain by Berry Siltstone. Max. thickness: 170m in southern Sydney Basin. Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|22969|4|Described|p 38, 20, Fig 2.2|Late Permian|Early Permian|Of Shoalhaven Group. Underlying unit Tallong + Yadboro Conglomerate.||||||
17035|Snapper Point Formation|22970|5|Briefly described|Plate 6|Early Permian||||||||
17035|Snapper Point Formation|23015|6|Mentioned|p319||Permian|||||||
17035|Snapper Point Formation|23214|4|Described|p265|Late Permian|Early Permian|Of Shoalhaven Group. Formerly named Megalong Conglomerate. Lithic sandstone conglomerate. Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
17035|Snapper Point Formation|23349|6|Mentioned|248|||||||||
17035|Snapper Point Formation|23544|5|Briefly described|Fig 2 p358|||In the Conjala Subgroup of the Shoalhaven Group||||||
17035|Snapper Point Formation|24079|5|Briefly described|p432|Permian|Permian|Of Conjola Subgroup.  Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|24240|5|Briefly described|p21|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|24552|4|Described|p5 Fig.2|Kungurian|Artinskian|Conformably overlies Pebbley Beach Formation, overlain by Wandrawandian Siltstone. Interbedded sandstone, with some siltstone + wave rippled conglomerate. Shallow marine. Abundant bivalves (Eurydesma, megadesma). Geological Prov: Southern Sydney Basin.||||||07-FEB-11
17035|Snapper Point Formation|24581|6|Mentioned|p817|Permian|Permian|Geological Province: Sydney Basin||||||
17035|Snapper Point Formation|29750|6|Mentioned|p1|||||||||
17035|Snapper Point Formation|29752|3|Fully described|p27|||||||||
17035|Snapper Point Formation|31081|2|Defined|p62|Artinskian|Artinskian|See also p63-65. Prob. Artinskian||||||13-AUG-15
17035|Snapper Point Formation|31128|6|Mentioned|p5|||||||||
17035|Snapper Point Formation|31298|6|Mentioned|p9|||See also Fig. 4||||||
17035|Snapper Point Formation|32073|6|Mentioned|p21|||||||||
17035|Snapper Point Formation|32097|6|Mentioned|p231|||Occurrence of Martiniopsis brevis||||||
17035|Snapper Point Formation|32266|6|Mentioned|p24|||||||||
17035|Snapper Point Formation|32769|6|Mentioned|p70|||||||||
17035|Snapper Point Formation|32945|6|Mentioned|p84|||Permian. See also PP85 & 88. Conjola Subgp.||||||
17035|Snapper Point Formation|34845|6|Mentioned|p116|||Also Table 1.||||||
17035|Snapper Point Formation|35160|6|Mentioned|p4|||||||||
17035|Snapper Point Formation|35284|6|Mentioned|Fig.1|||||||||
17035|Snapper Point Formation|35314|4|Described|p433|||Sedimentological aspects discussed||||||
17035|Snapper Point Formation|35862|6|Mentioned|p277|||||||||
17035|Snapper Point Formation|36042|6|Mentioned|Table 1|||||||||
17035|Snapper Point Formation|36045|6|Mentioned|p332|||||||||
17035|Snapper Point Formation|36147|6|Mentioned|Fig.2|||||||||
17035|Snapper Point Formation|36148|6|Mentioned|p266|||||||||
17035|Snapper Point Formation|37082|6|Mentioned|p161|||||||||
17035|Snapper Point Formation|37092|6|Mentioned|Table 2|||||||||
17035|Snapper Point Formation|37924|6|Mentioned|p488|||||||||
17035|Snapper Point Formation|38227|5|Briefly described|p426|||||||||
17035|Snapper Point Formation|38586|6|Mentioned|p28|||||||||
17035|Snapper Point Formation|38614|6|Mentioned|Fig.6|||||||||
17035|Snapper Point Formation|38690|6|Mentioned|Fig.2|||||||||
17035|Snapper Point Formation|38797|6|Mentioned|p248|||||||||
17035|Snapper Point Formation|39267|6|Mentioned|p246|||||||||
17035|Snapper Point Formation|39287|6|Mentioned|p20|||||||||
17035|Snapper Point Formation|39289|4|Described|p77|||||||||
17035|Snapper Point Formation|39290|6|Mentioned|p88|||Isopach map Fig. 5.9||||||
17035|Snapper Point Formation|39293|4|Described|p135|||||||||
17035|Snapper Point Formation|39299|6|Mentioned|p284|||||||||
17035|Snapper Point Formation|39305|5|Briefly described|p378|||Marine invertebrates.||||||
17035|Snapper Point Formation|39307|6|Mentioned|Table 22.1|||||||||
17035|Snapper Point Formation|39308|6|Mentioned|p519|||||||||
17035|Snapper Point Formation|40166|6|Mentioned|Table 1|||||||||
17035|Snapper Point Formation|40591|4|Described|Fig.2|||||||||
17035|Snapper Point Formation|40886|6|Mentioned|p107|||||||||
17035|Snapper Point Formation|41580|6|Mentioned|Table 1|||||||||
17035|Snapper Point Formation|41832|6|Mentioned|Fig.2|||||||||
17035|Snapper Point Formation|42821|6|Mentioned|Fig 3.9|||||||||
17035|Snapper Point Formation|42848|5|Briefly described|p532|||Of Conjola Subgroup (Shoalhaven Group). Sandstone. Overlies Tallong Formation; and is capped by overlying Nowra Sandstone. . Max. thickness: 300m.||||||09-MAY-05
17035|Snapper Point Formation|42925|5|Briefly described|Table 18||Early Permian|||||||
17035|Snapper Point Formation|42974|6|Mentioned|p192|||of Shoalhaven Group||||||
17035|Snapper Point Formation|43018|6|Mentioned|p389|||||||||
17035|Snapper Point Formation|43050|5|Briefly described|p9|||||||||
17035|Snapper Point Formation|43188|4|Described|p221, Table 7 p220||Early Permian|Of Shoalhaven Group.||||||12-MAR-09
17035|Snapper Point Formation|43194|5|Briefly described|p104, p128, p129 Tb. 8.3|Early Permian|Early Permian|Of Shoalhaven Group, Western and Southern Coalfields, Sydney Basin. Correlative of Porcupine Formation in the Gunnedah Basin.||||||
17035|Snapper Point Formation|43494|6|Mentioned|p28|Permian|Permian|The basal unit of the Shoalhaven Group has been mapped as Snapper Point Formation in the Cudgegong-Ilford area by Pemberton and others (1994).||||||16-MAR-06
17035|Snapper Point Formation|43677|6|Mentioned|p319||Permian|||||||
17035|Snapper Point Formation|43782|5|Briefly described|Map Legend|Late Permian|Late Permian|of Shoalhaven Group.||||||
17035|Snapper Point Formation|44093|5|Briefly described|p64 Photo 1|Permian|Permian|Sedimentary breccia (shoreline rubble). Overlies Lambie Group unconformably. Underlies Berry Siltstone. Geological Province: Sydney Basin.||||||26-NOV-10
17035|Snapper Point Formation|45090|5|Briefly described|p27|||Relationship of rock units. Isopach map P38||||||
17035|Snapper Point Formation|47041|6|Mentioned|p167|||||||||
17035|Snapper Point Formation|49644|5|Briefly described|Table|||||||||
17035|Snapper Point Formation|60281|4|Described|p8, p58|Early Permian|Early Permian|Of the Shoalhaven Group.  Interfingers with and overlies the Tallong and Yadboro Conglomerates; also overlies the Clyde Coal Measures in places.  Age: 274-273Ma (Nicholl et al, 1998). Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|60285|4|Described|p181|Sakmarian|Sakmarian|Of Shoalhaven Group. Overlies Pebbley Beach Formation. Overlain by Wandrwandian Silstone. Shallow marine. Geological Province: Sydney Basin.||||||
17035|Snapper Point Formation|61315|5|Briefly described|Table SY2|Early Permian|Early Permian|Of the Conjola Subgroup (Shoalhaven Group). Geological Province: Sydney Basin||||||
17035|Snapper Point Formation|61609|5|Briefly described|p239, p240 Tb. 1, p240, p243|Permian|Permian|Of Conjola Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
17035|Snapper Point Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin. NSW.||||||17-MAR-09
17035|Snapper Point Formation|61900|5|Briefly described|p129, p130 Fig. 3|Triassic|Permian|Of the Shoalhaven Group. Contains basal conglomerates overlain by lithic and quartzite sandstone. Unconformable over Rylstone Volcanics. Geological Province: Sydney Basin.||||||05-JUN-06
17035|Snapper Point Formation|62043|6|Mentioned|p438 Fig.2. |Early Permian|Early Permian|Southern Sydney Basin.||Unit in Shoalhaven Group.||Overlies Yarrunga Coal Measures and Pebbley Beach Formation. Is overlain by Wandrawandian Siltstone.||
17035|Snapper Point Formation|62368|5|Briefly described|p379, p391 Fig.10, p401|Triassic|Permian|Composed of diamictite and conglomerate. See also "Snapper Point Formation". Geological Province: Sydney Basin.||||||02-JUN-06
17035|Snapper Point Formation|63021|5|Briefly described|p991|Permian|Permian|Shallow marine deposits. Overlain by the Wandrawandian Siltstone. Geological Province: St. Georges Basin.||||||22-JAN-07
17035|Snapper Point Formation|63461|5|Briefly described|p862 Fig. 1c|||Geological Province: Sydney Basin.||||||10-DEC-07
17035|Snapper Point Formation|63773|5|Briefly described|p1059, p1058 Fig. 2, p1066 Fig. 6|Middle Permian|Early Permian|Geological Province: Sydney Basin. Near shore marine deposition.||||||07-APR-09
17035|Snapper Point Formation|63832|5|Briefly described|p131 fig 2, p136|Kungurian|Artinskian|Of Sydney Basin. Contains "one spectacular example of an iceberg keel turbate" indicating post-glacial iceberg activity.||Unit in Shoalhaven Group.||Overlies Pebbley Beach Formation.|Coastal to nearshore marine sandstone dominated, contains little outsized gravel debris.|
17035|Snapper Point Formation|64631|5|Briefly described|p44 Fig.2, p48 Fig.4, p54.|Kungurian|Artinskian|SW, SE Sydney Basin. Biostratigraphic age control at base and top.||Unit in Shoalhaven Group.||Overlies Pebbley Beach Formation, ?Yarrunga Coal Measures. Is overlain by Wandrawandian Siltstone.||
17035|Snapper Point Formation|64877|5|Briefly described|p293, p295-296, p301, p303-307,|Permian|Permian|Southern Sydney Basin. Transgressive unit, dominantly shallow-marine but increasingly braidplain to the W. Facies described and illustrated in great detail. See also p310, p312, p314-315.||Shoalhaven Group.||||
17035|Snapper Point Formation|66300|6|Mentioned|p52, p58.|Permian|Permian|||Unit in Shoalhaven Group.||Unconformably overlies Bundundah Granite.||29-OCT-13
17035|Snapper Point Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Overlies Yadboro and Tallong Conglomerates, Yarrunga Coal Measures and Pebbley Beach Formation. Is overlain by Wandrawandian Siltstone.||
17035|Snapper Point Formation|67663|6|Mentioned|p518|Permian|Permian|Sourced from eroding Devonian quartzite headlands.||Of the Shoalhaven Group.||||
17035|Snapper Point Formation|68003|5|Briefly described|p38 Fig.3-j, p40.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion. Also southern Sydney Basin. A thick transgressive shoreline and near-shore deposit, mainly derived from Late Devonian quartzite of the Lachlan Fold Belt.||Basal unit in Shoalhaven Group.||||
17035|Snapper Point Formation|68592|5|Briefly described|p1779, p1785-6|Permian|Permian|||Unit in Shoalhaven Group.||Conformably overlies Tallong Conglomerate, Yurrunga Coal Measures and Pebbly Beach Formation. Is overlain by Wandrawandian Siltstone.|Includes cross-bedded sandstone.|
17035|Snapper Point Formation|69297|6|Mentioned|p501, p502 fig 5.43|Kungurian|Artinskian|Sydney Basin.||Shoalhaven Group||Overlies and interfingers with the Pebbly Beach Formation and the Yadboro and Tallong Conglomerates. Overlain by and interfingers with the Wandrawandian Siltstone.||
17035|Snapper Point Formation|70096|6|Mentioned|p221|||Of southern Sydney Basin.||||||
17035|Snapper Point Formation|70661|2|Defined|ix, p132, p135,p137,  p139|Artinskian|Artinskian|Overlies basement rocks unconformably. Named for Snapper Point in Kioloa parish. Previously included as part of the Conjola Formation and the Megalong Conglomerate. Parts of the Ottawa Creek Formation have been recognised as Snapper Point Formation. The pebbly sandstone typically forms cliff faces that step out, down the steep slopes of gorges in the Southern half of Moss Vale. Type section described. 170m thick at type section, generally thinner in mapped area. Lithology described in great detail. Age derived from shelly fossil fauna and palynology. Fossil assemblage, distinguishing characteristics and structure described. Considered to have been deposited in a near shore or shallow marine environment. conformably overlain by Wandrawandian Formation, overlain (probably unconformably) by Nowra Sandstone. See also  p141, p154-p161, p177.||Shoalhaven Group||Disconformably overlies Tallong Conglomerate, disconformably overlain by Berry Siltstone, interfingers with Yadboro Conglomerate.|Dominated by quartz-rich sandstone, pebbly sandstone and minor pebbly layers and conglomeratic lenses. Thinly interbedded quartz sandstone, pebble conglomerate and siltstone are found at the top of this unit.|
17035|Snapper Point Formation|71303|5|Briefly described|map legend|Cisuralian|Cisuralian|Of Sydney Basin.||Of Shoalhaven Group.|||White to yellow quartzose, fine to very coarse-grained sandstone, siltstone, pebbly sandstone, conglomerate. Fossiliferous locally.|
17035|Snapper Point Formation|71538|6|Mentioned|p54 fig 2, p61-p62|Kungurian|Kungurian|Sydney Basin. Inner Shelf depositional environment. Referred to as the SPF throughout the text.||Shoalhaven Group||Overlies the Mount Agony Formation. Disconformably overlies the Tallong Formation and the Yadboror Formation. Overlain by the Wandrawandian Siltstone.||
17035|Snapper Point Formation|71542|5|Briefly described|p25|Permian|Permian|Of southern Sydney Basin.||Unit of Shoalhaven Group.||Overlain by Wandrawandian Siltstone. Underlain by Pebbley Beach Formation.||
17035|Snapper Point Formation|73304|6|Mentioned|p78|||||||||
17035|Snapper Point Formation|73421|4|Described|p1, p2 Fig.1, p3-6, p10, p15-17, p19-20|Kungurian|Kungurian|Sydney Basin, southern. Abbreviated to SPF in text. Widely distributed. Suboxic, nearshore shallow marine succession. Syndepositional intrusion by the monzo-diorite Snake Bay intrusion interpreted as part of the Termeil Complex with U-Pb zircon age of 278.9+/-3.7 Ma regarded as a proxy for the SPF, early Kungurian. Early Kungurian, Roadian, late Kungurian-Wordian ages estimated by prior studies.|278.9+/-3.7 Ma|Shoalhaven Group||Conformably overlies Pebbley Beach Formation, underlies Wandrawandian Siltstone, intruded by Termeil Complex, Milton Complex|Dominated by sandstone with minor conglomerate and siltstone interbeds, sparsely fossiliferous.|
17035|Snapper Point Formation|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Early Permian.||Conjola Subgroup.||Overlies Pebbley Beach Formation. Is overlain by Wandrawandian Siltstone.||
17038|Snobs Creek Volcanics|23309|5|Briefly described|p163, 166, Table 2.60||Devonian|Age: 367+/-22 Ma.||||||
17038|Snobs Creek Volcanics|24551|5|Briefly described|p164, p163 Fig. 6.4|Late Devonian|Late Devonian|Of Taggery Subgroup, Marysville Igneous Complex||||||
17038|Snobs Creek Volcanics|32074|5|Briefly described|p186|||||||||
17038|Snobs Creek Volcanics|33732|5|Briefly described|Table III|||Famennian||||||
17038|Snobs Creek Volcanics|35073|5|Briefly described|Table 2|||||||||
17038|Snobs Creek Volcanics|35186|4|Described|p3|||||||||
17038|Snobs Creek Volcanics|35277|4|Described|p87|||||||||
17038|Snobs Creek Volcanics|37270|6|Mentioned|Table 2|||||||||
17038|Snobs Creek Volcanics|38327|6|Mentioned|p558|||||||||
17038|Snobs Creek Volcanics|39291|6|Mentioned|p213|||See also Table 1||||||
17038|Snobs Creek Volcanics|40995|6|Mentioned|Fig.31|||||||||
17038|Snobs Creek Volcanics|41385|6|Mentioned|p363|||||||||
17038|Snobs Creek Volcanics|41641|4|Described|p153|||See also P162||||||
17038|Snobs Creek Volcanics|42827|5|Briefly described|p153|||||||||
17038|Snobs Creek Volcanics|43547|14|Not recorded|p155|||||||||
17038|Snobs Creek Volcanics|48894|6|Mentioned|p93|||Age||||||
17038|Snobs Creek Volcanics|68311|5|Briefly described|p273-274|Late Devonian|Late Devonian|Cerberean Cauldron, Central Victoria. The earliest volcanic formation in the pre-collapse phase. Up to 285m thick.|373.2 +/- 1.8 Ma (SIMS U-Pb; Compston, 2004).|Taggerty Subgroup.||Overlies Wightmans Hill Conglomerate. Is overlain by Blue Range Formation.|A welded, phenocryst-poor rhyolite ignimbrite that grades upwards into a more biotite-rich rhyodacite ignimbrite and tuffs.|
17038|Snobs Creek Volcanics|70933|14|Not recorded|p98|||Table of Upper Devonian cauldron sequences.||||||
17050|Snowy Mountains Volcanics|33221|5|Briefly described|p15|||[May be a misspelling of Snowy River Volcanics?]||||||27-APR-22
17050|Snowy Mountains Volcanics|71040|6|Mentioned|p9|||[May be a misspelling of Snowy River Volcanics?]||||||27-APR-22
17062|Snowy River Volcanics|22535|6|Mentioned|p489|||||||||
17062|Snowy River Volcanics|22628|6|Mentioned|p117,p118|||||||||
17062|Snowy River Volcanics|22714|6|Mentioned|p219|||||||||
17062|Snowy River Volcanics|22768|6|Mentioned|p178|||||||||
17062|Snowy River Volcanics|22857|6|Mentioned|p178|||||||||
17062|Snowy River Volcanics|22866|6|Mentioned|p492|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|22876|4|Described|p15|Early Devonian|Early Devonian|Age: 400-390Ma.||||||11-JAN-07
17062|Snowy River Volcanics|22877|5|Briefly described|map|Devonian|Devonian|||||||
17062|Snowy River Volcanics|22968|5|Briefly described|P12, P136||Early Devonian|Contains Avonmore Subgroup, conformably overlain by the Buchan Group||||||
17062|Snowy River Volcanics|23020|5|Briefly described|Map legend|Early Devonian|Early Devonian|Overlying unit is Buchan Group, underlying unit is Mount Elizabeth Caldera Complex||||||
17062|Snowy River Volcanics|23021|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
17062|Snowy River Volcanics|23028|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
17062|Snowy River Volcanics|23029|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
17062|Snowy River Volcanics|23030|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|23228|6|Mentioned|p10|||||||||
17062|Snowy River Volcanics|23229|6|Mentioned|p24|||||||||
17062|Snowy River Volcanics|23231|5|Briefly described|p50||Early Devonian|||||||
17062|Snowy River Volcanics|23235|5|Briefly described|Fig7-1p68, 68||Early Devonian|Geol. Province: Buchan Basin||||||
17062|Snowy River Volcanics|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
17062|Snowy River Volcanics|23309|4|Described|p105-121, 126, 129-132, 304, Table 2.40|||||||||
17062|Snowy River Volcanics|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|23615|3|Fully described|p84, p20 Fig.6|Early Devonian|Early Devonian|Formerly referred to as Snowy  River Porphyries, Snowy River Series. Name used interchangeably with Snowy River Volcanics Group in this publication.  Overlain by Buchan Group.  Age: shown as Lochkovian - Emsian. Younger than Bindian deformation (folded Ludlow sediments) and older than Late Pragian? or Emsian Buchan Caves Limestone||||Buchan Group overlies||15-JAN-13
17062|Snowy River Volcanics|23710|14|Not recorded|p69|||Occurrence.||||||
17062|Snowy River Volcanics|23938|6|Mentioned|p6, p96|Devonian|Devonian|Includes the Little River Subgroup. Overlain by Buchan Caves Limestone. See also p99.||||||25-SEP-08
17062|Snowy River Volcanics|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
17062|Snowy River Volcanics|24004|5|Briefly described|p275 Fig.2|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|24098|5|Briefly described|p27 Fig. 2|Early Devonian|Early Devonian|Overlain by Buchan Group. Geological Province: Lachlan Fold Belt.||||||19-APR-05
17062|Snowy River Volcanics|24164|6|Mentioned|p15 Fig.8|Devonian|Silurian||||||Acid|
17062|Snowy River Volcanics|24266|5|Briefly described|p1483|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt. Overlain by Buchan Group.||||||11-JAN-07
17062|Snowy River Volcanics|24275|6|Mentioned|p1696 Fig. 2|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||
17062|Snowy River Volcanics|24334|5|Briefly described|p45, p48 Tb.1|Early Devonian|Ludlow|Age: 391 - 417 Ma||||||
17062|Snowy River Volcanics|24424|5|Briefly described|p539 Tb.4|Early Devonian|Early Devonian|Age: 384-410 Ma. Palaeomagnetic poles given.||||||
17062|Snowy River Volcanics|24551|5|Briefly described|p38, Fig. 2.41, 120, p132 Fig.5.23, 234|Lower Devonian|Lower Devonian|Name used interchangably with Snowy River Volcanic Group.||||||
17062|Snowy River Volcanics|24598|5|Briefly described|p514|Early Devonian|Early Devonian|Rhyodacitic ignimbrites.  Geological Province: Lachlan Orogen.||||||
17062|Snowy River Volcanics|29648|6|Mentioned|p20|||||||||
17062|Snowy River Volcanics|29742|6|Mentioned|p403|||||||||
17062|Snowy River Volcanics|29860|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|29878|6|Mentioned|p71|||||||||
17062|Snowy River Volcanics|29953|6|Mentioned|Fig.1|||||||||
17062|Snowy River Volcanics|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
17062|Snowy River Volcanics|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|30574|6|Mentioned|p12|||Refers Thomas (1949)||||||
17062|Snowy River Volcanics|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17062|Snowy River Volcanics|31060|6|Mentioned|p33|||||||||
17062|Snowy River Volcanics|31161|5|Briefly described|PA11|||||||||
17062|Snowy River Volcanics|31334|5|Briefly described|p662|||||||||
17062|Snowy River Volcanics|31338|6|Mentioned|p451|||||||||
17062|Snowy River Volcanics|31800|6|Mentioned|p203|||||||||
17062|Snowy River Volcanics|31823|6|Mentioned|p44|||||||||
17062|Snowy River Volcanics|31999|6|Mentioned|p155|||||||||
17062|Snowy River Volcanics|32219|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian||||||
17062|Snowy River Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
17062|Snowy River Volcanics|32908|6|Mentioned|p14|||Mineralisation||||||
17062|Snowy River Volcanics|33154|5|Briefly described|p6|||||||||
17062|Snowy River Volcanics|33238|5|Briefly described|p644|||||||||
17062|Snowy River Volcanics|33316|6|Mentioned|p409|||||||||
17062|Snowy River Volcanics|33393|6|Mentioned|p158|||||||||
17062|Snowy River Volcanics|33481|6|Mentioned|Fig.1|||||||||
17062|Snowy River Volcanics|33602|6|Mentioned|p5|||||||||
17062|Snowy River Volcanics|33603|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17062|Snowy River Volcanics|33606|3|Fully described|p64|||||||||
17062|Snowy River Volcanics|33608|6|Mentioned|p45|||||||||
17062|Snowy River Volcanics|33732|5|Briefly described|Table III|||||||||
17062|Snowy River Volcanics|34031|6|Mentioned|p277|||L.Dev.  See also PP278,280-285.||||||
17062|Snowy River Volcanics|34403|5|Briefly described|p146|||||||||
17062|Snowy River Volcanics|34405|6|Mentioned|p119|||||||||
17062|Snowy River Volcanics|34406|6|Mentioned|p221|||See also P222||||||
17062|Snowy River Volcanics|34519|5|Briefly described|p44|||||||||
17062|Snowy River Volcanics|34652|6|Mentioned|p350|||||||||
17062|Snowy River Volcanics|34653|6|Mentioned|p26|||||||||
17062|Snowy River Volcanics|34954|6|Mentioned|Fig.34|||||||||
17062|Snowy River Volcanics|34964|6|Mentioned|p452|||||||||
17062|Snowy River Volcanics|35014|3|Fully described|p362|||||||||
17062|Snowy River Volcanics|35112|6|Mentioned|Table 1|||||||||
17062|Snowy River Volcanics|35274|6|Mentioned|p421|||||||||
17062|Snowy River Volcanics|35277|6|Mentioned|p119|||||||||
17062|Snowy River Volcanics|35278|6|Mentioned|p358|||||||||
17062|Snowy River Volcanics|35283|6|Mentioned|p49|||||||||
17062|Snowy River Volcanics|36201|4|Described|p4|||||||||
17062|Snowy River Volcanics|37330|3|Fully described|p11|||||||||
17062|Snowy River Volcanics|37501|6|Mentioned|p414|||||||||
17062|Snowy River Volcanics|37586|6|Mentioned|p12|||||||||
17062|Snowy River Volcanics|37727|6|Mentioned|p25|||See also p49 and Fig.1.||||||11-JAN-07
17062|Snowy River Volcanics|38063|6|Mentioned|p30|||||||||
17062|Snowy River Volcanics|38367|6|Mentioned|Fig.1|||||||||
17062|Snowy River Volcanics|38545|6|Mentioned|p114|||||||||
17062|Snowy River Volcanics|39221|6|Mentioned|p266|||||||||
17062|Snowy River Volcanics|39291|4|Described|p218|||||||||
17062|Snowy River Volcanics|39447|6|Mentioned|p2|||See also P23||||||
17062|Snowy River Volcanics|39860|6|Mentioned|p8|||||||||
17062|Snowy River Volcanics|40328|6|Mentioned|p71|||||||||
17062|Snowy River Volcanics|40761|5|Briefly described|p230|||||||||
17062|Snowy River Volcanics|40819|6|Mentioned|p23|||||||||
17062|Snowy River Volcanics|40882|6|Mentioned|p25|||||||||
17062|Snowy River Volcanics|41137|6|Mentioned|p292|||||||||
17062|Snowy River Volcanics|41563|6|Mentioned|p512|||||||||
17062|Snowy River Volcanics|41570|6|Mentioned|p91|||||||||
17062|Snowy River Volcanics|41572|6|Mentioned|p3|||See also P18||||||
17062|Snowy River Volcanics|41585|4|Described|p133|||Mention p125.||||||11-JAN-07
17062|Snowy River Volcanics|41590|6|Mentioned|Fig.7|||||||||
17062|Snowy River Volcanics|41641|6|Mentioned|p189|||||||||
17062|Snowy River Volcanics|41755|4|Described|p168|||||||||
17062|Snowy River Volcanics|41850|6|Mentioned|p427|||||||||
17062|Snowy River Volcanics|41868|6|Mentioned|p478|||See also p585.||||||11-JAN-07
17062|Snowy River Volcanics|42089|6|Mentioned|p10|||||||||
17062|Snowy River Volcanics|42110|6|Mentioned|p127|||||||||
17062|Snowy River Volcanics|42141|6|Mentioned|p569|||||||||
17062|Snowy River Volcanics|42220|5|Briefly described|p383|||||||||
17062|Snowy River Volcanics|42294|6|Mentioned|Fig. 1b P16|||||||||
17062|Snowy River Volcanics|42577|6|Mentioned|Fig.2 p26|||||||||
17062|Snowy River Volcanics|42627|5|Briefly described|Map legend|Pragian|Lochkovian|||||||
17062|Snowy River Volcanics|42635|6|Mentioned|p29|||||||||
17062|Snowy River Volcanics|42647|4|Described|p29|||||||||
17062|Snowy River Volcanics|42726|5|Briefly described|map legend|Early Devonian||||||||
17062|Snowy River Volcanics|42791|5|Briefly described|p205|||||||||
17062|Snowy River Volcanics|42827|5|Briefly described|p133|||see also Table 4.1||||||
17062|Snowy River Volcanics|42967|5|Briefly described|p75|||see also Fig.1 p76||||||
17062|Snowy River Volcanics|43206|5|Briefly described|map legend|Lochkovian|Ludlow|||||||
17062|Snowy River Volcanics|43220|5|Briefly described|p10||Devonian|||||||
17062|Snowy River Volcanics|43228|5|Briefly described|p9||Early Devonian|||||||
17062|Snowy River Volcanics|43284|5|Briefly described|Map Legend||Early Devonian|||||||
17062|Snowy River Volcanics|43312|5|Briefly described|Map Legend||Early Devonian|||||||
17062|Snowy River Volcanics|43313|5|Briefly described|Map Legend||Early Devonian|||||||
17062|Snowy River Volcanics|43314|5|Briefly described|Map Legend|Emsian|Lochkovian|||||||
17062|Snowy River Volcanics|43315|5|Briefly described|Map Legend|Emsian|Lochkovian|Includes the Brodribb River Volcanics and Yeerung River Volcanics as well as undifferentiated volcanics.||||||03-MAY-05
17062|Snowy River Volcanics|43344|14|Not recorded|p110|Early Devonian||||||||
17062|Snowy River Volcanics|43384|14|Not recorded|Map Legend||Devonian|||||||
17062|Snowy River Volcanics|43461|14|Not recorded|p628|||||||||
17062|Snowy River Volcanics|43525|14|Not recorded|Table p132||Siegenian|||||||
17062|Snowy River Volcanics|43547|14|Not recorded|p151,Tb p153,155|Emsian|Siegenian|||||||
17062|Snowy River Volcanics|43755|6|Mentioned|Fig.9,p556|||||||||
17062|Snowy River Volcanics|44092|5|Briefly described|map legend|Early Devonian|Early Devonian|Dlv4||||||
17062|Snowy River Volcanics|44184|5|Briefly described|Map Legend||Early Devonian|||||||
17062|Snowy River Volcanics|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Includes Timbarra, Wombargo, White Monkey, Marroo, Berrmarr, Mount Dawson, Little River, Ninnie, Tara Range Subgroups; Tulloch Ard Ignimbrite, Devils Den Conglomerate and Trendale Formation.|||
17062|Snowy River Volcanics|45147|6|Mentioned|M175|||||||||
17062|Snowy River Volcanics|46053|14|Not recorded|p.444,447|||||||||
17062|Snowy River Volcanics|46574|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Of the Volcanic Arch. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
17062|Snowy River Volcanics|48872|14|Not recorded|p.6,7,10|||(I55-7).||||||
17062|Snowy River Volcanics|48971|6|Mentioned|p40|||See also P42.||||||
17062|Snowy River Volcanics|60078|6|Mentioned|Map Legend|Devonian|Devonian|||||||
17062|Snowy River Volcanics|60503|5|Briefly described|p13, p28 Fig. 9|Early Devonian|Early Devonian|Subaerial volcanics. Geological Province: Limestone Creek Graben.||||||
17062|Snowy River Volcanics|60541|6|Mentioned|p13, p16|Early Devonian|Early Devonian|Mentioned also in terms of equivalents.  See also p17 Tb. 1.||||||
17062|Snowy River Volcanics|60542|3|Fully described|p49, p15|Middle Devonian|Middle Devonian|Supersedes Snowy River Group. Felsic volcanics, volcaniclastics and intrusives. Age: 385-380Ma. See also p76-77 (Srv Intrusives) for description of unnamed separate intrusive bodies. Overlain by Spring Creek Member.||||||26-MAR-13
17062|Snowy River Volcanics|60904|6|Mentioned|p806|||Of the Lachlan Orogen.||||||
17062|Snowy River Volcanics|61160|6|Mentioned|p138|||In MURRINDAL.||||||
17062|Snowy River Volcanics|61180|5|Briefly described|p7, p17, p25|Early Devonian|Early Devonian|Thick sequence of acid and intermediate volcanics; overlain by limestone (Buchan Group).  Base metal mineralisation is concentrated into the upper parts of this sequence.||||||
17062|Snowy River Volcanics|61181|5|Briefly described|p12, p171|Early Devonian|Early Devonian|Consist mainly of a complex of acid volcanics, with some andesites and basalts; non-volcanic and volcanic-derived sediments; and high level intrusives - quartz ignimbrite lithology dominates. Large barite deposits are associated with the SRV in Victoria.||||||
17062|Snowy River Volcanics|61187|5|Briefly described|p6, p16, p26 Fig.2, p29 Fig.4, pp137ff.|Early Devonian|Early Devonian|Buchan Zone, Benambra Terrane. A mixture of volcanics and minor non-volcanic sediments. Correlative of Errinundra Group in Mallacoota Zone, Benambra Terrane. Age interpreted from Fig.3. Immediately overlies rocks which host enigmatic magnetite-haematite-pyrite deposits with occurrences of gold and copper.|c.400 Ma.||Includes Tara Range Subgroup and Spring Creek Member.|Is overlain by Buchan Group.|Arc volcanics and chert.|
17062|Snowy River Volcanics|62095|6|Mentioned|p267|||||||||
17062|Snowy River Volcanics|63025|5|Briefly described|p1052|Pragian|Lochkovian|Geological Province: Eastern Lachlan Orogen. See also Figure 1.||||||
17062|Snowy River Volcanics|63594|5|Briefly described|p1032|Devonian|Devonian|Includes the Fairy Formation. Unconformably underlain by Cowombat Formation.||||||
17062|Snowy River Volcanics|64963|6|Mentioned|p180 Fig. 1|||||||||
17062|Snowy River Volcanics|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Buchan. Appears in text as Snowy R Volcanics. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17062|Snowy River Volcanics|65381|6|Mentioned|p688|||South Eastern Australia.||||||07-MAR-12
17062|Snowy River Volcanics|66181|6|Mentioned|p304|Devonian|Devonian|Ignimbrites, lavas and epiclastics.||||||
17062|Snowy River Volcanics|66197|5|Briefly described|p634|Early Devonian|Early Devonian|Buchan Basin/Rift. Complicated and widespread silicic volcanism, incorporating basement-derived clastic successions, in a rift setting.||||||10-AUG-15
17062|Snowy River Volcanics|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Devonian|Devonian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996)|398-416 Ma magnetic age range|||||24-APR-12
17062|Snowy River Volcanics|68295|6|Mentioned|p29, p28-29 Fig. 2.2|Devonian|Silurian|Of SE Australia (Schmidt et al. 1987).||||||
17062|Snowy River Volcanics|70901|14|Not recorded|p6|||Refers to Talent (1959).||||||
17062|Snowy River Volcanics|70910|14|Not recorded|p44|||Refers to Talent (1959).||||||
17062|Snowy River Volcanics|71040|5|Briefly described|p8, p9, p12, p26|Pragian|Lochkovian|Bindi Syncline, NE Victoria. West-dipping, but large parts have low to subhorizontal dips. U-Pb zircon age.|411 +/- 3 Ma (Morand and Fanning, 2009).|||Unconformably overlies Enano Group. Is overlain by Buchan Group.|Sedimentary and volcanic rocks.|27-APR-22
17062|Snowy River Volcanics|73186|6|Mentioned|p229, Fig.2|Lochkovian|Lochkovian|Bega and eastern Victoria.|||||Volcanic, volcanoclastic and epiclastic sequences.|
17075|Sofala Volcanics|13139|5|Briefly described|p9 Fig. 4, p10|Late Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt.||||||12-APR-05
17075|Sofala Volcanics|22472|3|Fully described|p36|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|22486|4|Described|p 1, 2, 3, 4|Wenlockian|Late Ordovician|Hill End Trough||||||
17075|Sofala Volcanics|22529|4|Described|1, 6|||Parent Cabbone Group||||||
17075|Sofala Volcanics|22545|6|Mentioned|p502|||||||||
17075|Sofala Volcanics|22577|6|Mentioned|p122||Eastonian|||||||
17075|Sofala Volcanics|22679|6|Mentioned|p 25|||||||||
17075|Sofala Volcanics|22768|6|Mentioned|p180|||||||||
17075|Sofala Volcanics|22857|4|Described|p127, p430 App. 1 Tb. A1.5.|Late Ordovician|Late Ordovician|Of the Cabonne Group. Contains graptolites (poorly preserved), corals, algae. Max. thickness: 2000m. See also p180.||||||
17075|Sofala Volcanics|23043|5|Briefly described|Map Legend|Eastonian|Gisbornian|of Cabonne Group.||||||
17075|Sofala Volcanics|23170|2|Defined|p39|Bolindian|Gisbornian|Age: Middle Gisbornian - Late Bolindian (Ordovician). K/Ar date 447+/- 5Ma. Cabonne Group.||||||
17075|Sofala Volcanics|23181|5|Briefly described|p1,3,6,7, Fig.1|Bolindian|Gisbornian|Age: at least as old as Gisbornian (early late Ordovician). Includes Eastonian conodonts in allochthonous limestone blocks. Underlying strata are late Darriwilian.||||||
17075|Sofala Volcanics|23213|5|Briefly described|Fig.10 p24|Bolindian|Ordovician|Age: Middle Ordovician to Bolindian. of Rockley-Gulgong Volcanic Belt.||||||
17075|Sofala Volcanics|23214|3|Fully described|p74|Late Ordovician|Late Ordovician|Of Cabonne Group. Undifferentiated sequence of volcanic sandstone, conglomerate, breccia, siltstone, minor basaltic andesite, chert and limestone. Max thickness 2100m.||||||
17075|Sofala Volcanics|23245|6|Mentioned|p127|||||||||
17075|Sofala Volcanics|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|24126|5|Briefly described|p3|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|24278|5|Briefly described|p1764|Silurian|Ordovician|Metavolcanics. Min. age is Middle Silurian.||||||24-JUL-06
17075|Sofala Volcanics|24463|4|Described|p319|Ordovician|Ordovician|Conformably overlies the Adaminaby Group. Geological Province: Lachlan Fold Belt.||||||22-APR-09
17075|Sofala Volcanics|29669|6|Mentioned|p604|||||||||
17075|Sofala Volcanics|29671|6|Mentioned|p637|||||||||
17075|Sofala Volcanics|29993|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|30099|6|Mentioned|Fig.2|||||||||
17075|Sofala Volcanics|30329|6|Mentioned|p30|||On table P30||||||
17075|Sofala Volcanics|30334|6|Mentioned|Table 111|||||||||
17075|Sofala Volcanics|31161|5|Briefly described|PA2|||||||||
17075|Sofala Volcanics|32045|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|32046|6|Mentioned|p164|||See also P167,271||||||
17075|Sofala Volcanics|32047|6|Mentioned|p6|||Mineralization||||||
17075|Sofala Volcanics|32088|6|Mentioned|p6|||Ordovician||||||
17075|Sofala Volcanics|32485|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|32621|6|Mentioned|p1|||||||||
17075|Sofala Volcanics|32671|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17075|Sofala Volcanics|32672|6|Mentioned|p668|||||||||
17075|Sofala Volcanics|32708|6|Mentioned|Fig.2|||||||||
17075|Sofala Volcanics|33002|6|Mentioned|p417|||Tectonic history||||||
17075|Sofala Volcanics|33004|6|Mentioned|p65|||See also P77||||||
17075|Sofala Volcanics|33006|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|Middle and Upper OrdovicianM - U||||||
17075|Sofala Volcanics|33007|5|Briefly described|p12|||History & genesis||||||
17075|Sofala Volcanics|33282|6|Mentioned|Map legend|Late Ordovician|Middle Ordovician|M. & U. Ord.M - U||||||
17075|Sofala Volcanics|33285|5|Briefly described|p19|||Middle to Late Ord.||||||
17075|Sofala Volcanics|34404|4|Described|p83|||||||||
17075|Sofala Volcanics|34405|6|Mentioned|p105|||||||||
17075|Sofala Volcanics|34406|6|Mentioned|p219|||Conglomerate derived from Sofala Volcanics.||||||
17075|Sofala Volcanics|34498|6|Mentioned|p148|||Ordovician||||||
17075|Sofala Volcanics|34572|6|Mentioned|p82|||Ordovician. See also Table 1 & PP86,87,93 etc.||||||
17075|Sofala Volcanics|35072|6|Mentioned|p363|||||||||
17075|Sofala Volcanics|35118|6|Mentioned|Fig.5|||||||||
17075|Sofala Volcanics|35166|6|Mentioned|p121|||||||||
17075|Sofala Volcanics|35257|6|Mentioned|Fig.32|||||||||
17075|Sofala Volcanics|35877|6|Mentioned|p125|||||||||
17075|Sofala Volcanics|36283|6|Mentioned|p109|||||||||
17075|Sofala Volcanics|36285|3|Fully described|p50|||See also Fig.2.& 3.||||||
17075|Sofala Volcanics|36512|5|Briefly described|p21|||||||||
17075|Sofala Volcanics|36534|6|Mentioned|p223|||See also P229.||||||
17075|Sofala Volcanics|37727|6|Mentioned|p28|||See also Fig.1.||||||
17075|Sofala Volcanics|37810|6|Mentioned|Notes|||||||||
17075|Sofala Volcanics|38230|6|Mentioned|p469|||||||||
17075|Sofala Volcanics|39214|5|Briefly described|p23|||||||||
17075|Sofala Volcanics|39331|6|Mentioned|p71|||See also Fig.0-3||||||
17075|Sofala Volcanics|39663|6|Mentioned|Table 1|||||||||
17075|Sofala Volcanics|40106|6|Mentioned|p593|||||||||
17075|Sofala Volcanics|40130|6|Mentioned|p195|||||||||
17075|Sofala Volcanics|40136|5|Briefly described|p39|||[Originally entered for Tas. CEBMar95]||||||
17075|Sofala Volcanics|40328|6|Mentioned|p3|||||||||
17075|Sofala Volcanics|43127|6|Mentioned|p14|||||||||
17075|Sofala Volcanics|43263|6|Mentioned|Map Legend||Ordovician|||||||
17075|Sofala Volcanics|43344|14|Not recorded|p139,150,152,153||Late Ordovician|||||||
17075|Sofala Volcanics|43384|14|Not recorded|Map Legend||Ordovician|||||||
17075|Sofala Volcanics|43476|14|Not recorded|Map Legend||Ordovician|(Provisional Edition)||||||
17075|Sofala Volcanics|43494|6|Mentioned|p7, p24|Ordovician|Ordovician|||||||16-MAR-06
17075|Sofala Volcanics|43515|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(Provisional Edition) (M-U Ord)||||||
17075|Sofala Volcanics|43516|14|Not recorded|Map Legend|Late Ordovician|Early Ordovician|(M.-U.Ord.)||||||
17075|Sofala Volcanics|43517|2|Defined|p112-122,147-163|Early Silurian|Ordovician|Type section along Turon River. Map Plate XII||||||
17075|Sofala Volcanics|43633|6|Mentioned|p17|||||||||
17075|Sofala Volcanics|43641|5|Briefly described|Map Legend||Ordovician|||||||
17075|Sofala Volcanics|43782|5|Briefly described|Map Legend|Bolindian|Gisbornian|of Cabonne Group.||||||
17075|Sofala Volcanics|44093|5|Briefly described|p56|Ordovician|Ordovician|See also p211 Appendix 1. Of the Cabonne Group. Geological Province: Lachlan Fold Belt.||||||
17075|Sofala Volcanics|46524|6|Mentioned|p123|||||||||
17075|Sofala Volcanics|63278|5|Briefly described|p145 Fig. 1, p146 Fig. 2a, p156-157|Bolinidian|Late Darriwilian|Geol Prov: Rockley-Gulgong Volcanic Belt, LFB. Consists mainly of deep-water turbiditic volcaniclastic rocks, cherts. Age from graptolites yeilds late Darriwilian - Bolindian. Intruded by Early Silurian monzonite and diorite.||||||07-FEB-11
17075|Sofala Volcanics|63283|5|Briefly described|p194 Fig. 2, p205, p10|Late Ordovician|Middle Ordovician|Geological Province: Rockley-Gulgong Volcanic Belt. Consists of a thick fining-upwards sequence of chert, sandstone and conglomerate with subordinate clinopyroxene-phyric basalts. See also p205.||||||07-FEB-11
17075|Sofala Volcanics|63289|6|Mentioned|p371|Ordovician|Ordovician|Geological Province: Rockley - Gulgong Volcanic Belt.||||||07-FEB-11
17075|Sofala Volcanics|63290|5|Briefly described|p392 Tb. 1, p397 Fig. 3(b)|Bolindian|Darriwilian|Age: ca 460-443Ma. Geological Province: Rockley-Gulgong Volcanic Belt. Intrudes by monzonites and diorites||||||
17075|Sofala Volcanics|63293|5|Briefly described|p471, p468 Fig. 2|Gisbornian|Darriwilian|Overlain by Tucklan and Burranah Formations. Geological Province: Rockley - Gulgong Volcanic Belt. Monzonites and dorites intrude.||||||07-FEB-11
17075|Sofala Volcanics|64963|5|Briefly described|p182 Fig. 2|||Age: 440-439Ma (Ar/Ar for intrusion within these rocks).||||||22-APR-09
17075|Sofala Volcanics|67322|4|Described|Fig.5; p26|Early Silurian|Late Ordovician|First described in detail by Packham (1968). Poorly preserved graptolites provide an age range from the late Darriwilian to Gisbornian. Ages from Ar-Ar dating of monzonite and diorite intrusives (Perkins et al.,1995). Occurs in the Sofala-Dunedoo-Mudgee region.|438.5 +/- 0.8 Ma; 439.9 +/- 0.8 Ma (minimum age)||||Volcaniclastic conglomerates, sandstones and siltstones, with pyroxene-rich andesites and basaltic andesites. Allochthonous limestone blocks also occur in this sequence, as do massive to thick-bedded bands of chert, particularly in the lower part.|22-FEB-18
17075|Sofala Volcanics|67663|6|Mentioned|p519 Fig.1|||||||||
17075|Sofala Volcanics|67847|6|Mentioned|p74|Ordovician|Ordovician|Rockley-Gulgon Volcanic Belt. Hosts structurally controlled gold.||||||
17075|Sofala Volcanics|68592|6|Mentioned|p397-8, p426|||The Rockley Volcanics had been [probably incorrectly] correlated with this unit by Stuart-Smith et al. (1998).||||||
17075|Sofala Volcanics|70297|4|Described|map legend|Ordovician|Ordovician|Macquarie Volcanic Arc ?Phase 4 volcanic unit. Age range poorly known. Hosts significant structurally controlled low sulfide 'orogenic' gold mineralisation near Wattle Flat. Rockley-Gulgong Volcanic Belt.|c. 449-443 Ma.|Cabonne Group||||
17075|Sofala Volcanics|70684|6|Mentioned|p3, p74|||||||||
17075|Sofala Volcanics|71040|6|Mentioned|p19|Ordovician|Ordovician|Bathurst region.||||||
17075|Sofala Volcanics|71924|6|Mentioned|p2|||Hill End Trough.||||||
17075|Sofala Volcanics|73299|6|Mentioned|p1095, p1096 Fig.3, p1101, p1102 Fig.8|Ordovician|Ordovician|Capertree High. Wiagdon Fault is a significant boundary between the Sofala Volcanics and Silurian units in the eastern Hill End Trough. East-west trending folds document deformation prior to the dominant deformation (Powell and Edgecombe, 1978). Interpreted to outcrop within an anticline in the northern Capertree High, underlying the Tanabutta Group. Locations in text include p1097-1098 Fig.4 and p1108.||||Faulted against Bells Creek Volcanics.||
17078|Soho Street Amphibolite|22815|4|Described|p32|Early Devonian||K/Ar dated at 410+/-12 Ma. Ar/Ar dated at 407+/-2 Ma. These considered minimum ages.||||||
17078|Soho Street Amphibolite|22857|4|Described|p422 App. 1, Tb. A1.5|Late Silurian|Late Silurian|Small amphibolite bodies: dykes, pods of the Cooma Metamorphic Complex. Age: 412+/-12Ma (K/Ar) and 407+/-2Ma (hornblende, Ar/Ar). Max. thickness: 50m.||||||
17078|Soho Street Amphibolite|43233|5|Briefly described|Map Legend|Early Ordovician|Late Cambrian|of Cooma Metamorphic Complex.||||||
17078|Soho Street Amphibolite|49705|5|Briefly described|p11|||This reference is not a publication. BMR Records became publications in July 1991.||||||
17078|Soho Street Amphibolite|61413|5|Briefly described|p78.||||c.410 -407 Ma (Tetley 1979).||||Pyroxene-bearing amphibolite; pervasively intruded by pegmatite.|
17107|Sounder Limestone|34692|6|Mentioned|p185|||||||||
17108|Sourges Shale|22857|4|Described|p422 App. 1, Tb. A1.5|Llandovery|Gisbornian|Of the Cabonne Group. Well-bedded buff to pale-grey shale, siltstone and fine-grained sandstone, minor tuffaceous sandstone.||||||
17108|Sourges Shale|23043|5|Briefly described|Map Legend|Llandovery|Eastonian|of Cabonne Group.||||||
17108|Sourges Shale|23170|2|Defined|p53|Llandovery|Late Ordovician|Cabonne Group.||||||
17108|Sourges Shale|23213|3|Fully described|p22, Fig.10|Bolindian|Eastonian|Unit redefined in Dubbo 1:250 000 explanatory notes in prep 1999. Faulted against Hanover Formation at type section.||||||
17108|Sourges Shale|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
17108|Sourges Shale|32485|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
17108|Sourges Shale|40328|2|Defined|p85|Silurian|Silurian|||||||
17108|Sourges Shale|63278|5|Briefly described|p146 Fig. 2a, p152, p153|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt. Consists of shales and limestone. Age idenified with Eastonian corals and conodonts. See also p153.||||||07-FEB-11
17108|Sourges Shale|63283|6|Mentioned|p194 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt. Consists of limestone and shale.||||||07-FEB-11
17108|Sourges Shale|63290|6|Mentioned|p397 Fig. 3(b)|Eastonian|Gisbornian|Geological Province: Molong Volcanic Belt.||||||
17108|Sourges Shale|63293|6|Mentioned|p468 Fig. 2|Late Ordovician|Late Ordovician|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
17108|Sourges Shale|67322|5|Briefly described|p25|Silurian|Silurian|Several limestone lenses (Late Ordovician) have been mapped as an unnamed member of the Sourges Shale in the vicinity of Cumnock.||Of the Cudal Group||||
17108|Sourges Shale|68592|6|Mentioned|p371|||Molong-Wellington Volcanic Belt.||Unit in Cabonne Group.||||
17108|Sourges Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Cudal Group||||
17108|Sourges Shale|70684|6|Mentioned|p74|||||||||
17108|Sourges Shale|73299|6|Mentioned|p1105|||Cowra Trough. [Map symbol suggests Silurian age]||||||
17114|South Fassifern Coal|31549|6|Mentioned|p159|||Stratigraphy||||||
17114|South Fassifern Coal|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
17114|South Fassifern Coal|34270|6|Mentioned|p254|||||||||
17167|Spion Kop Conglomerate|721|5|Briefly described|Map legend|Namurian|Namurian|Lenses of massive orthoconglomerate, minor paraconglomerate with thin sandstone lenses.  Geological Province: Tamworth Belt.||||||21-DEC-04
17167|Spion Kop Conglomerate|22857|5|Briefly described|p506 App.1 Tb.A1.8|Carboniferous|Carboniferous|Lenses of massive orthoconglomerate; minor paraconglomerate; thin sandstone lenses. Max. thickness: 550m.||||||
17167|Spion Kop Conglomerate|23050|5|Briefly described|p9 Fig.2|Late Carboniferous|Late Carboniferous|of Tamworth Belt.||||||
17167|Spion Kop Conglomerate|23051|5|Briefly described|Map Legend|Late Carboniferous|Late Carboniferous|of Tamworth Belt||||||
17167|Spion Kop Conglomerate|23861|5|Briefly described|p3, p4 Fig. 2|Namurian|Namurian|Overlain by Ermelo Pyroclastics.  Geological Province: New England Orogen.||||||
17167|Spion Kop Conglomerate|24010|5|Briefly described|p379|||||||||
17167|Spion Kop Conglomerate|24603|5|Briefly described|p868 Fig. 3|Namurian|Namurian|Age: >321Ma.  Geological Province: Tamworth Belt.||||||
17167|Spion Kop Conglomerate|24605|4|Described|p932 Fig.1, p937|Namurian|Namurian|Geological Province: New England Orogen. Disconformably overlies the Caroda Formation. Overlain by the Ermelo Pyroclastics and the Peri Rhyolite Member.||||||
17167|Spion Kop Conglomerate|30133|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
17167|Spion Kop Conglomerate|30135|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
17167|Spion Kop Conglomerate|30340|6|Mentioned|p2530|||Lithology||||||
17167|Spion Kop Conglomerate|30341|6|Mentioned|p138|||||||||
17167|Spion Kop Conglomerate|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17167|Spion Kop Conglomerate|31802|6|Mentioned|p142|||Unconformities. McKelvey (1966)||||||
17167|Spion Kop Conglomerate|32094|6|Mentioned|p384|||||||||
17167|Spion Kop Conglomerate|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
17167|Spion Kop Conglomerate|32672|6|Mentioned|p674|||||||||
17167|Spion Kop Conglomerate|34072|6|Mentioned|Fig.4.5|||||||||
17167|Spion Kop Conglomerate|34085|6|Mentioned|Cor.chart|||Westphalian||||||
17167|Spion Kop Conglomerate|34349|4|Described|p246|||||||||
17167|Spion Kop Conglomerate|36253|6|Mentioned|p130|||||||||
17167|Spion Kop Conglomerate|36528|6|Mentioned|p179|||||||||
17167|Spion Kop Conglomerate|36961|6|Mentioned|p210|||See also Fig.3.||||||
17167|Spion Kop Conglomerate|37803|5|Briefly described|p88|||||||||
17167|Spion Kop Conglomerate|37919|6|Mentioned|p476|||||||||
17167|Spion Kop Conglomerate|37987|6|Mentioned|p230|||||||||
17167|Spion Kop Conglomerate|38837|6|Mentioned|p232|||||||||
17167|Spion Kop Conglomerate|39299|5|Briefly described|p279|||||||||
17167|Spion Kop Conglomerate|39331|6|Mentioned|Table 10-1|||||||||
17167|Spion Kop Conglomerate|41009|6|Mentioned|Fig.2|||||||||
17167|Spion Kop Conglomerate|42547|4|Described|p19|||Rocky Creek Syncline.||||||
17167|Spion Kop Conglomerate|43091|5|Briefly described|Map legend|||||||||
17167|Spion Kop Conglomerate|43383|14|Not recorded|p17|||||||||
17167|Spion Kop Conglomerate|43417|4|Described|Map Legend|||||||||
17167|Spion Kop Conglomerate|43421|5|Briefly described|p676||Carboniferous|Middle Carboniferous||||||
17167|Spion Kop Conglomerate|43429|14|Not recorded|Map Legend|||Max thickness = 1500ft||||||
17167|Spion Kop Conglomerate|43434|14|Not recorded|Map Legend||Carboniferous|||||||
17167|Spion Kop Conglomerate|43435|2|Defined|Map Legend||Carboniferous|||||||
17167|Spion Kop Conglomerate|43436|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
17167|Spion Kop Conglomerate|43479|14|Not recorded|p159,172,177||Namurian|||||||
17167|Spion Kop Conglomerate|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
17167|Spion Kop Conglomerate|45097|6|Mentioned|p24|||Correlated with Coeypolly Congl. Chart.||||||
17167|Spion Kop Conglomerate|47056|6|Mentioned|Fig.2 P523|||||||||
17167|Spion Kop Conglomerate|61214|5|Briefly described|p171 Fig. 1|Namurian|Namurian|See also p172 Fig. 2.||||||
17167|Spion Kop Conglomerate|61767|4|Described|p71|Namurian|Namurian|A fluvial cobble-grade conglomerate with subordinate sst and slts lenses, and local glacial deposits. Overlain by Ermelo Pyroclastics (north) and Clifden Fm (south). Disconformably overlies the Caroda Fm. Max. thickness: 548m. Geol. Prov: Tamworth Belt||||||
17167|Spion Kop Conglomerate|63832|4|Described|p131 fig 2, p134|Serpukhovian|Serpukhovian|Rocky Creek Syncline, Southern New England Fold Belt. Earliest glaciation (C1) of Late Devonian-early Mississippian.||||Overlain by Clifden Formation (conformably).|Thick succession of glacial diamictite and poorly sorted conglomerate with striated and faceted clasts.|14-DEC-17
17167|Spion Kop Conglomerate|64631|5|Briefly described|p44 Fig.2, p47.|Serpukhovian|Serpukhovian|Southern New England Fold Belt. Rocky Creek Syncline. Earliest evidence for Permo-Carboniferous Ice Age in eastern Australia. Represents proximal pro-glacial environment.||||Is overlain by Clifden Formation.|Thick succession of diamictite and poorly-sorted conglomerate.|
17167|Spion Kop Conglomerate|65382|4|Described|p714|Serpukhovian|Visean|Age of 330 - 320 Ma given by relationships with over- and underlying units. Overlies Caroda Formation. Overlain by Clifden Formation. Said to indicate oldest [Carboniferous] glaciation.||||||
17167|Spion Kop Conglomerate|68003|5|Briefly described|p32 Fig.3-h, p137. |Namurian|Namurian|Tamworth Belt (North), New England Fold Belt.||||Overlies Caroda Formation. Is overlain by Ermelo Dacite Tuff.|Cobble sized fluvial orthoconglomerate; subordinate wacke and siltstone.|
17167|Spion Kop Conglomerate|68004|6|Mentioned|p134.|||Also called the Spion Kop Formation (on the same page). Potential for zeolite resources and levels of certainty are discussed.||||||
17167|Spion Kop Conglomerate|68005|5|Briefly described|p49 Fig.3-M, p57, p58 Photo.3-Q, p145.|Namurian|Namurian|Rocky Creek Block, Tamworth Belt. With the Clifden Formation, represents a period of glacial retreat.||||Is overlain by Ermelo Dacite Tuff.|Cobble sized fluvial orthoconglomerate; subordinate wacke and siltstone.|
17167|Spion Kop Conglomerate|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Rocky Creek Block, Tamworth Belt.||||||
17167|Spion Kop Conglomerate|70728|5|Briefly described|p265|Visean|Visean|Geological province: North Tamworth terrane, New England Orogen.||Unit of Clifden Formation.||Overlain by Clifden Formation. Underlain by Caroda Formation.||
17167|Spion Kop Conglomerate|73197|6|Mentioned|p466|Carboniferous|Carboniferous|New England Orogen, southern. Forearc basin, northwest of Tamworth.|||||Includes tillite.|
17173|Spirifer yassensis Limestone Member|22857|5|Briefly described|p462 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Taemas Limestone. Fossiliferous thinly bedded limestone, shaly limestone. Max. thickness: 85m. Geological Province: Canberra-Yass Shelf.||||||
17173|Spirifer yassensis Limestone Member|23898|5|Briefly described|p269, p271 Fig.2|||Of Taemas Limestone. Overlain by Currajong Limestone Member.||||||
17173|Spirifer yassensis Limestone Member|24250|5|Briefly described|p105, p109 Fig5|Early Devonian|Early Devonian|Of the Taemas Limestone (Murrumbidgee Group). Maximum Thickness: 120m. Overlain by Currajong Limestone Member (conformable). Underlain by Majurgong Formation (conformable)||||||18-JUN-08
17173|Spirifer yassensis Limestone Member|32483|6|Mentioned|p33|||Refers Hills (1933,1941,1943)||||||
17173|Spirifer yassensis Limestone Member|35386|4|Described|p52|||||||||
17173|Spirifer yassensis Limestone Member|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition.||||||18-JUN-08
17173|Spirifer yassensis Limestone Member|42994|6|Mentioned|p224|||Of the Taemas Formation.||||||18-JUN-08
17173|Spirifer yassensis Limestone Member|65214|6|Mentioned|p272|Devonian|Devonian|NSW, Taemas. Appears in text as S. yassensis Limestone Mb. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17173|Spirifer yassensis Limestone Member|68592|2|Defined|p982, p984 Fig.162, p985-7, p1008-11|Emsian|Emsian|See also p1896-7. Originally Spirifer yassensis Limestone of Browne (1959), at the base of the Taemas Stage. Offenberg (1974) raised the latter to Formation status, and hence this unit became Spirifer yassensis Limestone Member. This has continued despite the fossils (after which it was named) having been renamed Spinella yassensis. Type locality is the famous Shearsby's Wallpaper, location described. 85-122m thick. Rich and diverse fauna described. Earliest Emsian age from conodonts.||Unit in Taemas Limestone.||Conformably overlies Majurgong Formation. Is overlain conformably by Currajong Limestone Member.|Interbedded, grey, thinly-bedded limestone (2 to 50 cm thick beds) and light grey shale or mudstone (5 to 8 cm thick beds); densely packed with brachiopods.|
17173|Spirifer yassensis Limestone Member|70192|5|Briefly described|Map Legend|Emsian|Emsian|Dmts. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot. [Correct palaeontological nomenclature requires generic/species names in following format: Spirifer yassensis Limestone Member.]||Taemas Limestone||Overlies Majurgong Formation. Is overlain by Currajong Limestone Member.|Grey, generally thinly bedded, fossiliferous limestone interbedded with light grey shale or mudstone.|
17173|Spirifer yassensis Limestone Member|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Taemas Limestone|||Grey, generally thinly bedded, fossiliferous limestone interbedded with light grey shale or mudstone.|
17173|Spirifer yassensis Limestone Member|70546|5|Briefly described|Map Legend|Devonian|Devonian||||||Grey, generally thinly bedded, fossiliferous limestone interbedded with light grey shale or mudstone.|
17173|Spirifer yassensis Limestone Member|71656|4|Described|p12 Fig.2, p33-35|Emsian|Emsian|The famous palaeontological heritage site known as 'Shearsby's Wallpaper' contains rich beds of brachiopod fossils at a road cutting through this member as wells as lungfish skulls, ostracods, nautiloids and conodonts.||Of Taemas Limestone, Murrumbidgee Group||Overlies Majurgong Formation and underlies Currajong Limestone Member.|Fossiliferous limestone.|
17179|Splinter Creek Formation|30451|4|Described|p26|||||||||
17179|Splinter Creek Formation|31586|6|Mentioned|p4|||||||||
17179|Splinter Creek Formation|31587|6|Mentioned|p60|||Distribution of Lithostrotion||||||
17179|Splinter Creek Formation|31659|6|Mentioned|p54|||Part of Caswell Creek Gp.||||||
17179|Splinter Creek Formation|32866|6|Mentioned|p22|||Fossil content||||||
17179|Splinter Creek Formation|33728|6|Mentioned|p52|||||||||
17179|Splinter Creek Formation|33774|6|Mentioned|p19|||Strat.||||||
17179|Splinter Creek Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
17179|Splinter Creek Formation|34155|6|Mentioned|p94|||Lower Carboniferous. Caswell Creek Group.||||||
17179|Splinter Creek Formation|39445|5|Briefly described|Table 6|||||||||
17179|Splinter Creek Formation|42547|4|Described|p50|||See also [typo] Creek Formation.||||||
17179|Splinter Creek Formation|44360|2|Defined|p1-4,7,8,10,12,21,||Visean|p23-27,30,32,33,35,map. Unit of Caswell Creek Group.||||||
17179|Splinter Creek Formation|44379|14|Not recorded|p15|||Ref. to Tom McKellar 1967||||||
17179|Splinter Creek Formation|44487|14|Not recorded|p199|||Ref. to McKellar 1967.||||||
17179|Splinter Creek Formation|45097|6|Mentioned|p23|||Fossils. Correlation chart||||||
17179|Splinter Creek Formation|46803|6|Mentioned|p143|||See also Fig. 4||||||
17179|Splinter Creek Formation|70050|5|Briefly described|p327, p341, p366|Visean|Visean|Monto area. Contains Cionodendron coral fossils.|||Kolonga Creek Limestone Member.|||16-APR-18
17190|Spring Creek Granodiorite|41898|6|Mentioned|p1211|||||||||
17194|Spring Creek Pegmatite|40328|4|Described|p210|||||||||
17198|Spring Valley Granite|34544|6|Mentioned|p194|||Lake George area (Garretty 1936).||||||
17205|Springbok Sandstone|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499|Oxfordian|Oxfordian|N Surat Basin. 50-150m thick.||Unit in Injune Creek Group.||Equivalent to Adori and Pilliga Sandstones and basal Kumbarilla beds.|Mainly cross-bedded labile sandstone, with carbonaceous siltstone and mudstone, and rare thin coal and bentonite lenses.|
17205|Springbok Sandstone|13516|6|Mentioned|p167 fig 10, p169 fig 11|Late Jurassic|Late Jurassic|In Surat Basin, Eromanga Basin.||||||
17205|Springbok Sandstone|22757|5|Briefly described|Table6,p12|Late Jurassic|Middle Jurassic|275 m. Surat Basin||||||
17205|Springbok Sandstone|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig.22.8|Callovian|Bathonian|Of the Injune Creek Group. Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|22865|5|Briefly described|Table22.1p296-7|Callovian|Bathonian|||||||
17205|Springbok Sandstone|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
17205|Springbok Sandstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|24068|4|Described|p270 Table 2|Late Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 150m.||||||
17205|Springbok Sandstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|29591|6|Mentioned|Table 15|||||||||
17205|Springbok Sandstone|30692|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|30694|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
17205|Springbok Sandstone|30695|4|Described|Table 4|||Middle-Upper Jurassic||||||
17205|Springbok Sandstone|30696|4|Described|Table 4|||Middle-Upper Jurassic||||||
17205|Springbok Sandstone|30699|6|Mentioned|p53|||Stratigraphy. Middle Jurassic-Early Cretaceous age||||||
17205|Springbok Sandstone|30701|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle-Upper JurassicM - U||||||
17205|Springbok Sandstone|30702|4|Described|p48|||See also P50-52,Fig.1,2. Stratigraphic table||||||
17205|Springbok Sandstone|31121|6|Mentioned|p389|||||||||
17205|Springbok Sandstone|32138|6|Mentioned|p396|||||||||
17205|Springbok Sandstone|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|32276|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.M - U||||||
17205|Springbok Sandstone|32797|6|Mentioned|Table 4|||M.-U. Jur.||||||
17205|Springbok Sandstone|33070|4|Described|Table 2|||M.-U.Jur.||||||
17205|Springbok Sandstone|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33090|4|Described|Table 4|||Mid.-U.Jur.||||||
17205|Springbok Sandstone|33091|5|Briefly described|p10|||Strat.||||||
17205|Springbok Sandstone|33094|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33367|3|Fully described|p23|||||||||
17205|Springbok Sandstone|33371|4|Described|p58|||||||||
17205|Springbok Sandstone|33451|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
17205|Springbok Sandstone|33672|6|Mentioned|p44|||||||||
17205|Springbok Sandstone|34613|4|Described|Table 4|||||||||
17205|Springbok Sandstone|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
17205|Springbok Sandstone|35663|6|Mentioned|p129|||||||||
17205|Springbok Sandstone|35937|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|36243|6|Mentioned|Table 7A|||||||||
17205|Springbok Sandstone|36570|6|Mentioned|p55|||||||||
17205|Springbok Sandstone|37117|5|Briefly described|p313|||||||||
17205|Springbok Sandstone|37993|6|Mentioned|p159|||||||||
17205|Springbok Sandstone|37994|6|Mentioned|p146|||||||||
17205|Springbok Sandstone|37995|4|Described|p64|||||||||
17205|Springbok Sandstone|37997|6|Mentioned|p86|||||||||
17205|Springbok Sandstone|39212|5|Briefly described|p16|||||||||
17205|Springbok Sandstone|39445|5|Briefly described|Table 10|||||||||
17205|Springbok Sandstone|39494|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|39943|6|Mentioned|Table 9A|||||||||
17205|Springbok Sandstone|40030|6|Mentioned|Fig.5|||||||||
17205|Springbok Sandstone|40245|6|Mentioned|Table 2|||||||||
17205|Springbok Sandstone|40249|6|Mentioned|p38|||||||||
17205|Springbok Sandstone|40250|6|Mentioned|Fig.7|||||||||
17205|Springbok Sandstone|40540|6|Mentioned|Fig.2|||||||||
17205|Springbok Sandstone|40541|3|Fully described|p109|||||||||
17205|Springbok Sandstone|40544|6|Mentioned|Fig.6|||||||||
17205|Springbok Sandstone|40666|4|Described|p357|||||||||
17205|Springbok Sandstone|41060|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41064|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41187|6|Mentioned|Fig.2|||||||||
17205|Springbok Sandstone|41188|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41210|5|Briefly described|Fig.3|||||||||
17205|Springbok Sandstone|41216|6|Mentioned|Fig.18|||||||||
17205|Springbok Sandstone|41247|6|Mentioned|Fig.7|||||||||
17205|Springbok Sandstone|41266|6|Mentioned|Fig.3|||||||||
17205|Springbok Sandstone|41992|4|Described|Fig.2 P183|||||||||
17205|Springbok Sandstone|42007|5|Briefly described|Fig.2 P182|||Misspelling of Springbok?||||||
17205|Springbok Sandstone|42463|6|Mentioned|Fig.5 P172|||||||||
17205|Springbok Sandstone|42493|5|Briefly described|Fig. 1 P18|||||||||
17205|Springbok Sandstone|43000|5|Briefly described|Fig.5,p112|||Of Injune Creek Group.||||||16-SEP-08
17205|Springbok Sandstone|43002|5|Briefly described|Fig.2,p135|||||||||
17205|Springbok Sandstone|44171|4|Described|p194,195,197,198|||Upgraded from Springbok Sandstone Lens.||||||
17205|Springbok Sandstone|45110|2|Defined|p95|Middle Jurassic|Middle Jurassic|Formerly Springbok Sst. Lens (Exon,1966) & Springbok Sst. Mbr. See also p24.||||||11-DEC-15
17205|Springbok Sandstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
17205|Springbok Sandstone|46984|6|Mentioned|Table 1|||||||||
17205|Springbok Sandstone|48917|6|Mentioned|p30|||Stratigraphic relationships||||||
17205|Springbok Sandstone|48919|2|Defined|p61|Middle Jurassic|Middle Jurassic|||||||
17205|Springbok Sandstone|48920|6|Mentioned|Table 7|||See also P50. Refers Power & Devine (1968)||||||
17205|Springbok Sandstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
17205|Springbok Sandstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
17205|Springbok Sandstone|60993|5|Briefly described|p36|Late Jurassic|Middle Jurassic|Comparable in age with Kangaroo Creek Sandstone. May be the equivalent of the lower sandstone section of the Woodenbong beds. Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|61000|5|Briefly described|p186 Fig. 4|Callovian|Bathonian|Geological Province: Surat Basin.||||||
17205|Springbok Sandstone|61005|6|Mentioned|p253|||Contains apatites. Equivalent to Kangaroo Sandstone (intended as Kangaroo Creek Sandstone). See also p255 Figs. 23, 24 and 25.||||||
17205|Springbok Sandstone|61377|5|Briefly described|p148 Tb. SU1|Jurassic|Middle Jurassic|Quartz sandstone, minor siltstone and shale. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
17205|Springbok Sandstone|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Late Jurassic|Geological Province: Surat Basin.||||||13-MAR-09
17205|Springbok Sandstone|63218|6|Mentioned|p211, p212 Fig.3, p217, pp219-221. |Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.|Basal clean, medium- to coarse-grained, quartzose sandstone. Contains thin coal seams with high (46 vol%) inertinite.|
17205|Springbok Sandstone|63979|5|Briefly described|p38|||Underlies Walloon Coal Measures. Intertongues with Adori Sandstone in places. Geological province: Surat Basin.||||||07-FEB-11
17205|Springbok Sandstone|64197|6|Mentioned|p630 Fig.7|Jurassic|Jurassic|Surat Basin.||||Underlies Westbourne Formation; overlies Walloon Coal Measures.||
17205|Springbok Sandstone|64665|5|Briefly described|p53 Fig.2, p62.|Late Jurassic|Late Jurassic|Surat Basin. Equivalent to the Adori Sandstone (Eromanga Basin).||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|64856|3|Fully described|p79, p88-93|Oxfordian|Callovian|Originally the Springbok Sandstone Lens of Exon (1966) in uppermost Birkhead Formation. Superseded by Springbok Sandstone Member (Exon et al., 1967), then the Springbok Sandstone (Power and Devine, 1968). Surat Basin. Type section is the interval 38-50m in BMR Mitchell 3. Conformably overlies Walloon Coal Measures. Laterally equivalent to Adori Sandstone in the Eromanga Basin. Lower part equivalent to the Proud Sandstone. Interfingers with Pilliga Sandstone to the south. Up to 157m thick. Age from palynofloral unit APJ5.|| ||||29-NOV-17
17205|Springbok Sandstone|64857|5|Briefly described|p133, p113 Fig.3|||Surat Basin. Overlies Walloon Coal Measures. Wireline log suggests disconformity.||||||
17205|Springbok Sandstone|64858|6|Mentioned|p182 Fig.3|||||||||30-NOV-09
17205|Springbok Sandstone|65003|5|Briefly described|p8||Jurassic|Of Surat Basin.||||||
17205|Springbok Sandstone|65096|5|Briefly described|p368, p370 Fig.2|Middle Jurassic|Middle Jurassic|Surat Basin?||||Unconformably overlies the Walloon Coal Measures.||
17205|Springbok Sandstone|65112|5|Briefly described|p323; p328; Fig 11 p 324; fig 16 p328|Jurassic|Jurassic||158-157 Ma.|||Underlies the Westbourne Formation, overlies the Walloon Coal Measures.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
17205|Springbok Sandstone|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Late Jurassic|Overlies the Walloon CM, underlies the Westbourne Formation.||||||
17205|Springbok Sandstone|65114|5|Briefly described|p385 Fig.3|Late Jurassic||||||||
17205|Springbok Sandstone|65116|5|Briefly described|Fig 2 p437|Late Jurassic|Late Jurassic|Underlies the Westbourne Formation, Overlies the Walloon Coal Measures, Surat Basin.||||||
17205|Springbok Sandstone|65117|5|Briefly described|p461, 462, 470-472,Table 1 p466|Oxfordian|Oxfordian|Surat Basin, Potential reservoir unit. Some scouring observed at base, so at least disconformable on Walloon Coal Measures. Feldspathic to lithic sandstone, minor siltstone, mudstone and coal. Max thickness 250m.||||||
17205|Springbok Sandstone|65119|6|Mentioned|Fig 13 p520, Fig 14 p521|||Present in the Rockwood 1 and Flinton 1 wells.||||||07-MAR-12
17205|Springbok Sandstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Injune Creek Group.||Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|66915|5|Briefly described|p6 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||||
17205|Springbok Sandstone|67133|5|Briefly described|p2, p5, p14-15, p19-21|Jurassic|Jurassic|21 samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (17-71%) and plagioclase always the dominant feldspar. Kaolinite (5-25%) is the dominant clay mineral. Mixed-layer clays are smectite-dominant.||||Overlies Walloon Subgroup. Is overlain conformably by Westbourne Formation.|Feldspathic sublabile to lithic sandstone, sometimes porous, friable, pebbly or with calcareous cement; andesitic debris and bentonitic tuffs from contemporaneous volcanism.|
17205|Springbok Sandstone|67402|5|Briefly described|p43 tbl HPB1|Oxfordian|Oxfordian|Surat Basin. Highly prospective for the storage of carbon dioxide. Deposited primarily in streams. Approximately 116m thick. See also  p146 fig SRT3, p148, p151, p154 fig SRT15/16, p156.||||Unconformably overlies the Walloon Subgroup. Conformably overlain by the Westbourne Formation.|Feldspathic to lithic sandstone commonly with a calcareous cement that is commonly interbedded with siltstone and mudstone.|
17205|Springbok Sandstone|67669|5|Briefly described|p11|Jurassic|Jurassic|Of Bowen Basin.||Unit of Injune Creek Group.||Overlain by Westbourn Formation. Underlain by Wallon CM.||
17205|Springbok Sandstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|68117|5|Briefly described|p346-347, p349-350|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Juandah Coal Measures (Walloon Subgroup). Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|68135|5|Briefly described|p52 fig 2b, p54|Oxfordian|Oxfordian|Surat Basin (QLD)||||Unconformably overlies Walloon Coal Measures. Overlain by Westbourne Formation|Sandstone.|15-SEP-17
17205|Springbok Sandstone|68139|5|Briefly described|p23-25, p30 Fig.11, p32|Late Jurassic|Late Jurassic|Surat Basin. A major aquifer. In many places, this unit has completely removed the Upper Juandah Coal Measures.||Injune Creek Group.||Unconformably overlies Upper Juandah Coal Measures (Walloon Subgroup). Is overlain unconformably by Westbourne Formation.|Includes volcanic debris and widespread ash-fall tuffs.|
17205|Springbok Sandstone|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|69574|6|Mentioned|p23-24, 26-28, 31-32, 34|Late Jurassic|Late Jurassic|Surat Basin. A major regional aquifer. Thin coal seams have only low gas contents (<2 m3/t).||||Unconformably overlies Walloon Subgroup.||
17205|Springbok Sandstone|69582|5|Briefly described|p36, p38|Late Jurassic|Late Jurassic|Surat Basin.||||Unconformably overlies the Walloon Coal Measures. Overlain by the Westbourne Formation.|Mudstone, sandstone.|
17205|Springbok Sandstone|69594|4|Described|p519, p525, p537, p573|Kimmeridgian|Oxfordian|Exon (1966); Exon et al. (1967). Northern Surat Basin. 12m thick in the type section in BMR Mitchell 3. Maximum thickness of 157m. Fluvial deposits, with increasing overbank and swamp sediments up-section. Volcanic detritus indicates penecontemporaneous volcanism.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain conformably by Westbourne Formation. Laterally continuous with and interfingers with Adori Sandstone.|Dominated by volcanic feldspathic and lithic sandstone with minor pebbly quartzose sandstones near the base and minor interbedded siltstones, mudstones and thin coals in the upper part.|
17205|Springbok Sandstone|69681|6|Mentioned|p74 Fig.3, p82|Late Jurassic|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||Unit in Injune Creek Group.||||
17205|Springbok Sandstone|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Walloon Subgroup. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|69790|5|Briefly described|p1061,p1064-1068, p1070-1072, p1077-1078|||||Unit in Injune Creek Group.||Unconformably overlies Walloon Subgroup. Equivalent to Pilliga Sandstone in NSW.||
17205|Springbok Sandstone|70374|6|Mentioned|p808, p809 figure 1, p812, p813|Kimmeridgian|Oxfordian|Previously considered to be Late Jurassic/Oxfordian, based on biostratigraphy.||Injune Creek Group.||Unconformably overlies Walloon Coal Measures. Is overlain ?conformably by Westbourne Formation.||28-SEP-16
17205|Springbok Sandstone|70725|5|Briefly described|p11, 13-20, 22-25|Late Jurassic|Late Jurassic|Surat Basin. Maceral composition and vitrinite reflectance graphed and discussed. 13C isotope vs. depth tabulated.||Walloon Subgroup.||Unconformably overlies Upper Juandah Coal Measures (Walloon Subgroup).||
17205|Springbok Sandstone|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Surat Basin. Aquifer: generally artesian.||Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne Formation.||
17205|Springbok Sandstone|71282|6|Mentioned|p456, p457 Fig.1, p459-460, p462|||Appears as Springbok Formation on p462.||||Unconformably overlies Walloon Subgroup.||
17205|Springbok Sandstone|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
17205|Springbok Sandstone|72297|5|Briefly described|p699 Fig.10.11, p745, p751|Jurassic|Jurassic|Surat Basin. Minor petroleum reserves in fault-related traps.||||Unconformably overlies Walloon Coal Measures or Walloon Subgroup.||
17205|Springbok Sandstone|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW). Main confined aquifers and confining beds, generally producing flowing artesian water bores.||Injune Creek Group.||Overlies Walloon Coal Measures. Is overlain by Westbourne FZ.||
17205|Springbok Sandstone|72921|5|Briefly described|p15 Fig.2, p50-51|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland.||||Underlies Westbourne Formation and shown as unconformably overlying Walloon Coal Measures.|Includes sandstone and siltstone.|
17205|Springbok Sandstone|73113|5|Briefly described|p. 2, 10, 13, 19, 22-24, 26-27, 29...|||Surat Basin. Groundwater model divides unit into upper and lower layers. Lower portion contains only a small amount of coal. Tight aquifer. More locations: p. 31, 36-37, 41, 49, 51-52, 56-57, 61, 67, 69-70, 75, 78, 80, 88, 94, 98, 116-117, 119, 123, 126-127, 129, 148-149, 152, 158, 160, 162, 165-174, 177-178, 191-193, 199.||||Underlain by Walloon Coal Measures. Overlain by Westbourne Formation.|Lower portions tend to be dominated by coarse to very coarse-grained sandstones; upper portion is typically comprised of fine to coarse-grained, felspathic to lithic sandstone interbedded with siltstone and mudstone.|
17205|Springbok Sandstone|73193|6|Mentioned|p367, p369-370, p372, p375|Kimmeridgian|Kimmeridgian|Surat Basin. Separated from the Walloon Subgroup by the Springbok unconformity.||Injune Creek Group||Unconformably underlain by Walloon Subgroup. Overlain by Westbourne Formation.||
17205|Springbok Sandstone|73200|6|Mentioned|p532 Fig.1, p533, p540|Jurassic|Jurassic|Exposed along the western banks of the Condamine River valley.||||||
17205|Springbok Sandstone|73393|6|Mentioned|p20-21|Tithonian|Tithonian|Surat Basin.||Injune Creek Group||Underlain by Walloon Coal Measures. Overlain by and equivalent to Westbourne Formation.||
17206|Springbrook Rhyolite|39969|6|Mentioned|Fig.22|||||||||
17206|Springbrook Rhyolite|40623|5|Briefly described|p39|||||||||
17206|Springbrook Rhyolite|40896|6|Mentioned|p32|||||||||
17206|Springbrook Rhyolite|42317|5|Briefly described|p2|||||||||
17206|Springbrook Rhyolite|43161|6|Mentioned|13,14|||||||||
17206|Springbrook Rhyolite|69599|5|Briefly described|p631, p633 Fig.8.35, p640, p641 Fig.8.44|||Northern side of the Tweed volcano, centred on Mount Warning. Resistant; forms cliff lines and waterfalls. Table of chemical analyses; REE diagram and comment.||||Approximate equivalent of Nimbin Rhyolite in NSW.|Peraluminous or high-silica rhyolite.|
17206|Springbrook Rhyolite|73450|4|Described|p99-101|||Associated with the Tweed Volcano. Up to 500 m thick. Separated from the Springbrook Rhyolite by basalt (at least locally). Has a glassy base with obsidian and perlite, and a glassy top.|||||Coherent felsic lava and minor pyroclastic deposits including ash flow tuff and ash fall tuff.|
17206|Springbrook Rhyolite|73581|6|Mentioned|p6|||(Stevens 1984). Lies on the northern slope of the Tweed Volcano. Overlies an unnamed basalt within the Binna Burra Rhyolite. Underlies Hobwee Basalt/Blue Knob Basalt.||||||
17234|Stafford Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Charlton Formation.   Geological Province: Sydney Basin||||||
17234|Stafford Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Charlton Formation. Geological Province: Sydney Basin||||||
17234|Stafford Coal Member|29942|3|Fully described|p11|||||||||
17234|Stafford Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Charlton Formation.||||
17274|Stanthorpe Granite|33437|6|Mentioned|Fig.1|||U.Perm.||||||
17274|Stanthorpe Granite|34423|6|Mentioned|p293|||On Table.||||||
17274|Stanthorpe Granite|34479|6|Mentioned|p312|||Permian ?||||||
17274|Stanthorpe Granite|34589|6|Mentioned|p275|||225 my||||||
17274|Stanthorpe Granite|36045|6|Mentioned|Fig.7|||||||||
17274|Stanthorpe Granite|39838|5|Briefly described|p341|||||||||
17274|Stanthorpe Granite|42559|4|Described|p13|||||||||
17274|Stanthorpe Granite|44068|14|Not recorded|p13|||||||||
17274|Stanthorpe Granite|44512|14|Not recorded|p16,17,map|||Intrudes "Silverwood Group". (epi-Permian or early Triassic)||||||
17274|Stanthorpe Granite|44563|14|Not recorded|p142-143|||||||||
17274|Stanthorpe Granite|44564|14|Not recorded|p166|||||||||
17274|Stanthorpe Granite|44625|14|Not recorded|p383,384|||||||||
17274|Stanthorpe Granite|44671|4|Described|p245|||||||||
17274|Stanthorpe Granite|44832|14|Not recorded|p9,10,13|||||||||
17274|Stanthorpe Granite|45087|5|Briefly described|p16|||Chemical analyses||||||
17274|Stanthorpe Granite|61772|6|Mentioned|p131|Triassic|Permian|||||||
17274|Stanthorpe Granite|63731|5|Briefly described|Map legend|Early Triassic|Early Triassic|Detailed lithology presented.||||||
17274|Stanthorpe Granite|63732|5|Briefly described|Map legend|Early Triassic|Early Triassic|Monzogranite to syenogranite.||||||
17274|Stanthorpe Granite|63748|3|Fully described|p36-39, p86 Appdx. 1|Early Triassic|Permian|Two outcroppings are referred to informally as Mayland River complex (NE) and Stanthorpe complex (in SW Stanthorpe-Wallangarra region). Age: 246.9+/-2.0Ma (U-Pb zircon SHRIMP). Intrudes Texas beds. I-type. Detailed lithology.See also p16, p25, p27 Fig. 27||||||07-FEB-11
17274|Stanthorpe Granite|65668|6|Mentioned|p32|Permian|Permian|Intrudes the Wallangarra Volcanics. Age ~247 Ma.||||||
17274|Stanthorpe Granite|67818|5|Briefly described|p131, Fig. 2|Middle Triassic|Middle Triassic|Northern New England region. Rb/Sr biotite age (Shaw, 1994), U/Pb zircon SHRIMP age (Hughes, 1993).|240.2 Ma Rb/Sr, ~237 Ma U/Pb|||||03-OCT-14
17274|Stanthorpe Granite|68111|5|Briefly described|p969 Tb.1|Anisian|Olenekian|Mis-spelt as Stanthrope. Also 243 - 238 Ma, Rb-Sr (biotite) (Shaw 1994).|246.9 +/- 2.0 Ma; U-Pb SHRIMP(Donchak et al 2007)|Of the Stanthorpe Supersuite.||||
17274|Stanthorpe Granite|68553|6|Mentioned|Map legend|Triassic|Triassic|This unit, as well as the Bungulla Monzogranite, and Ruby Creek, Sailor Jack and Dormans Flat Granites, are all mapped under the symbol, Rgn.||||||
17274|Stanthorpe Granite|68576|6|Mentioned|QLD_D1: p17|||Used for building and/or monumental stone. Map location.||||||
17274|Stanthorpe Granite|68679|4|Described|p446, p453-458, p461-466|Middle Triassic|Middle Triassic|By far the most extensive unit in the New England Batholith. ~1840 km2. Geochemistry discussed in some detail; geochemical plots, photographs. I-type. Similarities with Ruby Creek Granite. Associated with minor Mo mineralisation. Has untapped potential for dimension stone.|246.9 +/- 2.0 Ma (SHRIMP U-Pb zircon: GA).|Stanthorpe Suite.||Intrudes the Wallangarra Volcanics, Bungulla Monzogranite, Palgrave, Ballandean Granites. Is intruded by Ruby Creek Granite.|Pink, white or brown, medium-grained, porphyritic, leucocratic biotite monzogranite to syenogranite; minor hornblende-biotite monzogranite, aplitic leucogranite; local rapakivi textures, granophyric, miarolitic, vuggy pegmatite/aplo-pegmatite lenses.|
17274|Stanthorpe Granite|68901|5|Briefly described|p8, p128,129, 132,134, 136, 137|Early Triassic|Early Triassic|Rb-Sr ages: 238.1 - 242.2 Ma (Shaw, 1994). Close genetic relationship with Ruby Creek granite supported.|246.9+/-2 Ma SHRIMP, Donchak et al., 2007.|||Intrudes the Ballandean Granite. Intruded by the Ruby Creek Granite.||27-SEP-18
17274|Stanthorpe Granite|69639|4|Described|p2, p6, p8, p80, p151, p157|Triassic|Lopingian|New England Orogen. Sample locality, petrography, and geochronology is described. See also  p163-p168, p192-p193, p222, p239.|248.7 +/- 1.2 Ma (SHRIMP U-Pb)|Stanthorpe Suite||Intrudes and is faulted against the Maryland Granite. Faulted against the Koreelan Creek Granodiorite. Intrudes the Bookookoorara Monzogranite.|Massive, coarse-grained, alkali  feldspar-rich leucocratic granite (syenogranite).|
17274|Stanthorpe Granite|69793|6|Mentioned|p1113 Fig.3|Triassic|Triassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
17274|Stanthorpe Granite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Olenekian|New England Orogen. A SHRIMP age derived from unpublished Geoscience Australia data of 246.9 +/- 2.0 Ma is also provided.|248.7 +/- 1.2 Ma (SHRIMP, Chisholm et al, 2014b)|Stanthorpe Supersuite||||
17274|Stanthorpe Granite|70373|6|Mentioned|p800|Triassic|Triassic|May show fault displacement.|~250 Ma|||||
17274|Stanthorpe Granite|70876|5|Briefly described|p80|||Mineralisation is mentioned but no details are provided.||Stanthorpe Supersuite||||
17274|Stanthorpe Granite|71592|5|Briefly described|Appendix A.|||New England Orogen.|249+/-1.2 Ma (crystallisation: U-Pb zircon SHRIMP)||||Granite.|
17274|Stanthorpe Granite|71628|6|Mentioned|p15: 32, 38, 40, 81|||Gradwell (1960), after the ""Stanthorpe"" granite of Saint-Smith (1913, 1914). Now Stanthorpe Complex.||||||
17274|Stanthorpe Granite|72078|6|Mentioned|p4|||Geological province: New England Orogen. Together with the Ruby Creek Leucogranite forms the Ruby Creek Sn-W district.||||||14-JAN-20
17274|Stanthorpe Granite|72297|6|Mentioned|p759|||Gem-quality colourless (rarely blue) topaz with rare garnet and zircon occur in alluvium and tailings from tin mining near Stanthorpe; derived from cassiterite-bearing veins and greisen zones in the granite.||||||
17277|Stanthorpe Suite|38839|6|Mentioned|p244|||Geological Province: New England Fold Belt.||||||12-AUG-08
17277|Stanthorpe Suite|42876|6|Mentioned|Fig.1, p142|||Variation on Stanthorpe Granite, Adamellite?||||||
17277|Stanthorpe Suite|42997|6|Mentioned|Fig.2,p37|||||||||
17277|Stanthorpe Suite|63748|5|Briefly described|p36-37|Early Triassic|Permian|Of the Stanthorpe Supersuite. Includes Stanthorpe and Ruby Creek Granites.||||||07-FEB-11
17277|Stanthorpe Suite|68679|5|Briefly described|p456, p458-464, p466|||Northern New England Batholith. Placed into the Moonbi Supersuite by Blevin and Chappell (1996) and Bryant and Chappell (2010). Geochemistry discussed. Historical reports of high Au values in the Pikedale lode.|~248-245 Ma.|Stanthorpe Supersuite.|Ruby Creek, Stanthorpe Granites.|||
17277|Stanthorpe Suite|69639|5|Briefly described|p9, p26, p163, p175, p181, p187|||New England Orogen.||Stanthorpe Supersuite|Includes the Stanthorpe Granite, Morgans Creek Monzogranite, Ruby Creek Granite and the Rivertree Granite.|||
17277|Stanthorpe Suite|71628|5|Briefly described|p11: 5, 35, 46-47, 53, 58, 73, 77, 98|||See also p16-26; p17: 15, 20, 25, 31, 33, 38, 43, 56, 58, 62, 66, 69, 88, 93, 95, 99; p19: 20, 131, 175. Korsch (1977).||Stanthorpe Supersuite.||||
17285|Stanwell Park Claystone|22549|6|Mentioned|p526||Triassic|||||||
17285|Stanwell Park Claystone|22745|6|Mentioned|p129|||Sydney Basin.||||||
17285|Stanwell Park Claystone|22749|6|Mentioned|p 195|||||||||
17285|Stanwell Park Claystone|22833|6|Mentioned|p653|||of Sydney Basin.||||||
17285|Stanwell Park Claystone|22857|5|Briefly described|p530 App.1 Tb.A1.9|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Red, green and grey shale and quartz-lithic sandstone. Max. thickness: ~50m. Geological Province: Sydney Basin.||||||
17285|Stanwell Park Claystone|22969|6|Mentioned|p 27|||||||||
17285|Stanwell Park Claystone|23881|5|Briefly described|p69 Fig. 7.2|||Of the Narrabeen Group.  Geological Province: Sydney Basin.||||||
17285|Stanwell Park Claystone|29633|6|Mentioned|p435|||Permian/Triassic boundary||||||
17285|Stanwell Park Claystone|29901|4|Described|Table 1|||||||||
17285|Stanwell Park Claystone|30006|4|Described|p57|||||||||
17285|Stanwell Park Claystone|30007|6|Mentioned|p61|||Triassic||||||
17285|Stanwell Park Claystone|30132|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|30427|6|Mentioned|p39|||||||||
17285|Stanwell Park Claystone|30707|6|Mentioned|p6|||See also Fig.2||||||
17285|Stanwell Park Claystone|31061|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|31128|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|31276|6|Mentioned|p147|||Palynology||||||
17285|Stanwell Park Claystone|31297|6|Mentioned|Fig. 3|||||||||
17285|Stanwell Park Claystone|31426|6|Mentioned|Fig.1|||||||||
17285|Stanwell Park Claystone|31725|6|Mentioned|p10|||On table||||||
17285|Stanwell Park Claystone|31878|4|Described|p823|||See Table 1||||||
17285|Stanwell Park Claystone|31884|6|Mentioned|Table 1|||Triassic||||||
17285|Stanwell Park Claystone|31886|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|31887|5|Briefly described|p8|||||||||
17285|Stanwell Park Claystone|32187|6|Mentioned|p4|||Refers Chesnut (1976)||||||
17285|Stanwell Park Claystone|32801|6|Mentioned|Fig.10|||||||||
17285|Stanwell Park Claystone|33683|4|Described|Table 1|||Grose Sst.||||||
17285|Stanwell Park Claystone|33685|5|Briefly described|p396|||||||||
17285|Stanwell Park Claystone|33867|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|34009|6|Mentioned|Table III|||||||||
17285|Stanwell Park Claystone|34058|5|Briefly described|p395|||Triassic||||||
17285|Stanwell Park Claystone|34107|6|Mentioned|Fig.6|||||||||
17285|Stanwell Park Claystone|34121|6|Mentioned|p397|||||||||
17285|Stanwell Park Claystone|34139|6|Mentioned|p23|||Table||||||
17285|Stanwell Park Claystone|34205|6|Mentioned|Table 6|||Correlation with Mount York Claystone Member.||||||
17285|Stanwell Park Claystone|34236|6|Mentioned|p17|||||||||
17285|Stanwell Park Claystone|34240|6|Mentioned|p395|||Triassic||||||
17285|Stanwell Park Claystone|34241|6|Mentioned|p404|||||||||
17285|Stanwell Park Claystone|34301|6|Mentioned|p403|||||||||
17285|Stanwell Park Claystone|34336|6|Mentioned|Table 5.15|||||||||
17285|Stanwell Park Claystone|34337|5|Briefly described|Table 5.18|||||||||
17285|Stanwell Park Claystone|34339|6|Mentioned|p442|||Clay minerals||||||
17285|Stanwell Park Claystone|36042|6|Mentioned|Fig.22|||||||||
17285|Stanwell Park Claystone|36220|4|Described|p67|||See also P65 & Table 20.||||||
17285|Stanwell Park Claystone|36222|6|Mentioned|Map legend|Early Triassic|Early Triassic|||||||
17285|Stanwell Park Claystone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
17285|Stanwell Park Claystone|36594|6|Mentioned|Table 1|||See also Table II.||||||
17285|Stanwell Park Claystone|39296|6|Mentioned|p179|||||||||
17285|Stanwell Park Claystone|39306|6|Mentioned|p413|||Flora||||||
17285|Stanwell Park Claystone|39450|6|Mentioned|Table 1|||||||||
17285|Stanwell Park Claystone|40516|6|Mentioned|Fig.3|||||||||
17285|Stanwell Park Claystone|40602|5|Briefly described|Table 1|||||||||
17285|Stanwell Park Claystone|40625|6|Mentioned|Map legend|Early Triassic|Early Triassic|Early to Middle Triassic||||||
17285|Stanwell Park Claystone|40652|6|Mentioned|p128|||||||||
17285|Stanwell Park Claystone|42737|5|Briefly described|map legend|Triassic||||||||
17285|Stanwell Park Claystone|42896|3|Fully described|p28, Table 2|||of Clifton Subgroup||||||
17285|Stanwell Park Claystone|42925|5|Briefly described|Table 18||Early Triassic|||||||
17285|Stanwell Park Claystone|42926|4|Described|map legend||Early Triassic|||||||
17285|Stanwell Park Claystone|43028|6|Mentioned|Fig.7,p618|||actually spelt Stanwell P CL||||||
17285|Stanwell Park Claystone|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained outwash and overbank sediments, southern Sydney Basin.||||||
17285|Stanwell Park Claystone|43317|6|Mentioned|Table 3 p12|||||||||
17285|Stanwell Park Claystone|43342|14|Not recorded|Table 1 p107|||||||||
17285|Stanwell Park Claystone|43344|14|Not recorded|p21,69,70|||||||||
17285|Stanwell Park Claystone|43383|14|Not recorded|p22|||Part of Clifton Sub-Group||||||
17285|Stanwell Park Claystone|43385|14|Not recorded|p182 Table||Early Triassic|||||||
17285|Stanwell Park Claystone|43395|14|Not recorded|p76|||See also Lexicon||||||
17285|Stanwell Park Claystone|45090|6|Mentioned|p71|||Narrabeen Gp.||||||
17285|Stanwell Park Claystone|60281|6|Mentioned|p64-65|||Extension of the Narrabeen Group under the Hawkesbury Sandstone.||||||
17285|Stanwell Park Claystone|61315|5|Briefly described|Table SY2|Early Triassic|Early Triassic|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
17285|Stanwell Park Claystone|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Narrabeen Group.||Overlies Scarborough Sandstone. Is overlain by Bulgo Sandstone.||
17285|Stanwell Park Claystone|67560|5|Briefly described|p258, p260-p272|Triassic|Triassic|Constrained by the age of the Narrabeen Group.||Of the Narrabeen Group.||Overlain by the Bulgo Sandstone. Underlain by the Scarborough Sandstone.|Chocolate shale.|
17285|Stanwell Park Claystone|68003|5|Briefly described|p42.|Triassic|Triassic|Southern Sydney Basin.|||||Red, green and grey claystone and siltstone, often intercalated with or overlain by conglomeratic sediments.|
17285|Stanwell Park Claystone|73304|6|Mentioned|p74, p76|||Sydney Basin, southern.||Narrabeen Group||||
17298|State Circle Shale|12185|5|Briefly described|map legend|Lower Silurian|Lower Silurian|Grouped with Canberra Group and Camp Hill Sandstone in legend. Calcareous shale, sandstone, mudstone, limestone lenses, tuffaceous sediments, rhyolite. BMR map symbol: Slc.||||||
17298|State Circle Shale|22857|4|Described|p134, p424 App.1 Tb.A1.5|Early Silurian|Early Silurian|Massive pale-grey siltstone; upper unit stringly laminated shale with silty bands up to 10mm. Unconformably overlies the Pittman Formation. Max. thickness: 113m.||||||
17298|State Circle Shale|23245|5|Briefly described|p134-5||Early Silurian|||||||
17298|State Circle Shale|23309|6|Mentioned|p390|||||||||
17298|State Circle Shale|29857|4|Described|p433|||||||||
17298|State Circle Shale|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
17298|State Circle Shale|29994|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
17298|State Circle Shale|30332|3|Fully described|p124|||||||||
17298|State Circle Shale|31111|6|Mentioned|p66|||See also P68, 72, 76||||||
17298|State Circle Shale|31161|5|Briefly described|PA6|||||||||
17298|State Circle Shale|31197|6|Mentioned|p432|||||||||
17298|State Circle Shale|31284|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
17298|State Circle Shale|32376|6|Mentioned|p1541|||||||||
17298|State Circle Shale|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
17298|State Circle Shale|32672|6|Mentioned|p672|||||||||
17298|State Circle Shale|32820|6|Mentioned|Table 1|||Refers Crook et al. (1973)||||||
17298|State Circle Shale|33125|6|Mentioned|p15|||Correlation chart||||||
17298|State Circle Shale|33325|5|Briefly described|Table 2|||See also Table 3 & PP 14,23.||||||
17298|State Circle Shale|33328|4|Described|Table 1|||P9||||||
17298|State Circle Shale|34405|5|Briefly described|p119|||Early Silurian. Table 3.5||||||
17298|State Circle Shale|35110|6|Mentioned|p3|||||||||
17298|State Circle Shale|35614|5|Briefly described|p6|||||||||
17298|State Circle Shale|36413|6|Mentioned|p31|||See also Table 3||||||
17298|State Circle Shale|36633|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
17298|State Circle Shale|37270|6|Mentioned|Table 2|||||||||
17298|State Circle Shale|37348|6|Mentioned|p97|||||||||
17298|State Circle Shale|37727|5|Briefly described|p86|||See also P26.||||||
17298|State Circle Shale|37728|4|Described|Table 2|||||||||
17298|State Circle Shale|37752|6|Mentioned|Fig.2|||||||||
17298|State Circle Shale|38664|5|Briefly described|p5|||||||||
17298|State Circle Shale|39331|4|Described|p50|||See also P52||||||
17298|State Circle Shale|39947|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
17298|State Circle Shale|40328|3|Fully described|p120|||||||||
17298|State Circle Shale|40646|6|Mentioned|p39|||||||||
17298|State Circle Shale|41356|5|Briefly described|p67|||||||||
17298|State Circle Shale|42497|5|Briefly described|Map Legend|Llandoverian|Llandoverian|||||||
17298|State Circle Shale|42727|5|Briefly described|map legend|Llandovery|Llandovery|Shale, mudstone, siltstone and minor sandstone (proximal quartz turbidites). Unconformably underlies Canberra Formation; unconformable over Pittman Formation; underlies Black Mountain Sandstone. BMR map symbol: Slc. Geol. Prov: Canberra Block.||||||
17298|State Circle Shale|42820|2|Defined|p11|Llandovery||late Llandovery (middle Early Silurian).||||||
17298|State Circle Shale|43344|14|Not recorded|p110,112,113,115|Early Silurian||||||||
17298|State Circle Shale|43385|14|Not recorded|p172||Llandovery|||||||
17298|State Circle Shale|43479|14|Not recorded|p116||Llandoverian|||||||
17298|State Circle Shale|43481|5|Briefly described|3,5||Early Silurian|||||||
17298|State Circle Shale|44093|5|Briefly described|p197 App. 1|Early Silurian|Early Silurian|In the Bruce Block. Geological Province: Lachlan Fold Belt.||||||
17298|State Circle Shale|44970|2|Defined|p4,11,23-4,31,74,77,||Silurian|p79,88,90,map. See also Lexicon. Overlies Camp Hill Sandstone. Contains Acton Limestone Member||||||
17298|State Circle Shale|45147|6|Mentioned|M118|||||||||
17298|State Circle Shale|47033|5|Briefly described|p78|||||||||
17298|State Circle Shale|48894|6|Mentioned|p5|||Age||||||
17298|State Circle Shale|49043|5|Briefly described|p6|||||||||
17298|State Circle Shale|63290|6|Mentioned|p385|Llandovery|Llandovery|Underlain unconformably by Acton Shale.||||||
17298|State Circle Shale|66197|6|Mentioned|p629|||Canberra-Yass Basin. Deep marine quartz and lithic turbidites.||||||14-MAR-12
17298|State Circle Shale|68592|5|Briefly described|p13, p16, p420|Early Silurian|Early Silurian|Canberra district. Comparable lithology and graptolite fauna as Jerrara Formation.||||Is overlain unconformably by Camp Hill Sandstone Member. Correlated with Jerrara Formation.||
17298|State Circle Shale|71069|6|Mentioned|p72|||||||May be equivalent to the Gungoandra Siltstone.||
17298|State Circle Shale|72951|6|Mentioned|p1028|Ordovician|Ordovician|Lachlan Orogen. eNd = -9.7 (McCulloch and Chappell, 1982).|||||Metasediments.|
17298|State Circle Shale|73211|6|Mentioned|p909|Llandovery|Llandovery||ca 435 Ma|||Unconformably overlain by Camp Hill Sandstone Member, Canberra Formation.||
17298|State Circle Shale|73215|6|Mentioned|p994|||Canberra area.||||||
17312|Steamers Trachyte Member|39969|6|Mentioned|p9|||||||||
17312|Steamers Trachyte Member|42485|6|Mentioned|p264|||||||||
17312|Steamers Trachyte Member|48917|6|Mentioned|p7|||Refers Stevens (1965)||||||
17312|Steamers Trachyte Member|73450|6|Mentioned|p92|||||Governors Chair Volcanics|||Felsic.|
17329|Stewartsfield Granodiorite|31580|6|Mentioned|p272|||See also analysis table 1-4.||||||
17329|Stewartsfield Granodiorite|31581|3|Fully described|Table 1|||Analysis||||||
17329|Stewartsfield Granodiorite|32906|6|Mentioned|p239|||||||||
17329|Stewartsfield Granodiorite|36413|6|Mentioned|p78|||||||||
17329|Stewartsfield Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
17329|Stewartsfield Granodiorite|45147|3|Fully described|M196|||||||||
17355|Stockyard latite|37253|6|Mentioned|Table 1|||||||||
17356|Stokefield Metagabbro|22679|4|Described|p 36|Ordovician|Early Ordovician|||||||
17356|Stokefield Metagabbro|23214|2|Defined|p28|Late Ordovician|Ordovician|Originally named Stokefield Diorite and included in the Carcoar Granite (now Carcoar Granodiorite).  Intrudes Coombing Formation of Kenilworth Group. Intruded by the Carcoar Granodiorite.||||||
17356|Stokefield Metagabbro|24268|6|Mentioned|p1536 Fig.2|||Geological Province: Lachlan Fold Belt||||||
17356|Stokefield Metagabbro|43654|5|Briefly described|Map Legend|Ordovician|Ordovician|Foliated plagioclase-phyric metagabbro.||||||17-JUL-08
17356|Stokefield Metagabbro|43782|6|Mentioned|Map Legend|Eastonian|Eastonian|||||||
17356|Stokefield Metagabbro|49794|6|Mentioned|p10|||Variation of Stokefield Diorite (84/24549) or Stoke Metagabbro (R 1974, NLR||||||
17356|Stokefield Metagabbro|70297|5|Briefly described|map legend|||Macquarie Volcanic Arc Phase 4 intrusion. Age: ranges from latest Ordovician to earliest Silurian.||||||
17356|Stokefield Metagabbro|73431|6|Mentioned|p364-365, p366 Fig.3|Ordovician|Ordovician|Lachlan Orogen.||||Intruded by Browns Creek Intrusive Complex||
17372|Stony Creek Coal Measures|40963|6|Mentioned|p265|||||||||
17401|Stratford Coal Member|37094|5|Briefly described|p240|||||||||
17403|Strathaird Formation|22857|4|Described|p216, p494 App. 1 Tb.A1.7|Late Devonian|Late Devonian|Of the Lambie Group. Arenite, shale, breccia, conglomerate, arkose; phyllitic slate near faults. Max. thickness: 240m. Geological Province: Lambie Shelf.||||||
17403|Strathaird Formation|22859|5|Briefly described|p216|||||||||
17403|Strathaird Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
17403|Strathaird Formation|30731|6|Mentioned|Map legend|Devonian|Devonian|||||||
17403|Strathaird Formation|32865|6|Mentioned|p483|||||||||
17403|Strathaird Formation|32999|3|Fully described|p41|||Refers Brunker et al. (1970)||||||
17403|Strathaird Formation|34481|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
17403|Strathaird Formation|35655|6|Mentioned|p209|||Stratigraphy||||||
17403|Strathaird Formation|50234|5|Briefly described|Map Legend|Frasnian|Emsian|Of the Lambie Group.  Underlies Cookbundoon Formation, Wiarborough Formation.||||||25-JUN-08
17403|Strathaird Formation|63633|5|Briefly described|Map Legend|Late Devonian|Late Devonian|Of Lambie Group. Sandstone, shale, breccia, conglomerate, arkose, phyllitic slate, marine fossils.||||||
17403|Strathaird Formation|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Lambie Group. Red and purple to buff and cream, med.-gr. to granule, poorly bedded, lithic-qtz + q'tzose sst, pebbly to conglom. in part, purplish, fine-gr. qtz sst+siltst.; polymictic basal cobble conglom. +clasts of quartzite, sst., chert+felsic.||||||09-SEP-08
17403|Strathaird Formation|68592|2|Defined|p787, p1722-3, p1726-8, p1732-8, p1908|Late Devonian|Late Devonian|See also p34-5, p232, p235, p326. Brunker et al. (1970); named after the Parish of Strathaird. Includes most of Scheibner's (discontinued) Wiarborough Formation. Redesignated type area, and previous "good exposures" (of Offenberg, 1974), are described. 150-300m thick. Shallow marine deposition: brachiopods and ripple marks. Depositional environment discussed. Geophysical properties described. Quarried near Towrang for plum-coloured slate in late 1800s and late 1900s, and at Mount Werong where extraction has ceased. Potential source of structural clay/shale and kaolin. Previous mapping of area of De Drack Formation containing the Wowagin Dacite Member included Strathaird Formation (Felton 1974). Is correlated with Gibbons Creek Sandstone. Locally shows elevated uranium radiometric responses.||Basal unit in Lambie Group.||Unconformably overlies Bendoc Group, Barrallier Ignimbrite and Forest Lodge Quartz Monzodiorite. Is overlain by Cookbundoon Formation and onlapped by Cowpers Creek Conglomerate.|Thin to thickly bedded quartzose and lithic-quartz sandstones and mostly basal, discontinuous, cobble to boulder conglomerates, with well-laminated reddish purple mudstone and shale a common component; local calcareous sandstones.|
17403|Strathaird Formation|70192|5|Briefly described|Map Legend|Frasnian|Frasnian|Dls. On Taralga and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Lambie Group||Erosional at base. Is overlain by Cowpers Creek Conglomerate and Cookbundoon Formation.|Fine-coarse grained, thin-thickly bedded, moderately-well sorted, quartzose and lithic-quartz sandstone, pebbly-conglomeratic with interbedded mudstone and siltstone. Basal, thickly bedded, poorly sorted, cobble-boulder, polymictic conglomerate.|
17403|Strathaird Formation|70542|5|Briefly described|Map Legend|Devonian|Devonian|||Lambie Group|||Fine-coarse grained, thin-thickly bedded, moderately- well sorted quartzose and lithic quartz sandstone. Pebbly to conglomeratic in part with interbedded mudstone and siltstone. Thickly bedded, poorly sorted, cobble-boulder, polymictic conglomerate.|
17403|Strathaird Formation|70543|5|Briefly described|Map Legend|Devonian|Devonian|||Lambie Group|||Fine-coarse grained, thin-thickly bedded, moderately-well sorted, quartzose and lithic-quartz sandstone, pebbly-conglomeratic with interbedded mudstone and siltstone. Basal, thickly bedded, poorly sorted, cobble-boulder, polymictic conglomerate.|
17403|Strathaird Formation|71656|5|Briefly described|p13 Fig.2, p41|Frasnian||No conodonts found but includes eroded and polished lingulide brachiopod fragments, indicating a near shoreline environment. No maximum age given.||Lambie Group||Partially underlies Cookbundoon Formation and Cowpers Creek Conglomerate.|Fossiliferous limestone.|
17408|Strathbogie Granite|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
17408|Strathbogie Granite|22779|5|Briefly described|p 172|||||||||
17408|Strathbogie Granite|22882|5|Briefly described|p 13|Devonian|Devonian|||||||
17408|Strathbogie Granite|22885|5|Briefly described|map|||||||||
17408|Strathbogie Granite|22886|4|Described|Table.1|||Age: K/Ar 362 +/- 4Ma. Rb/Sr 365Ma. Of Strathbogie Batholith.||||||22-DEC-08
17408|Strathbogie Granite|22971|5|Briefly described|p18, p23|Middle Devonian|Middle Devonian|||||||19-JAN-06
17408|Strathbogie Granite|23203|6|Mentioned|Fig.1|||||||||
17408|Strathbogie Granite|23810|5|Briefly described|Table 1, p894||Devonian|Felsic S-Type. Age: 374+/-2 Ma (SHRIMP U-Pb age). Lachlan Fold Belt.||||||
17408|Strathbogie Granite|23814|6|Mentioned|p742 Fig. 1|||||||||
17408|Strathbogie Granite|24002|6|Mentioned|p234 Fig. 7|||||||||
17408|Strathbogie Granite|24096|5|Briefly described|p6|Devonian|Devonian|||||||
17408|Strathbogie Granite|24109|6|Mentioned|p282|||||||||
17408|Strathbogie Granite|24177|3|Fully described|p64|Late Devonian|Late Devonian|Intrudes Wilson Creek Shale and Walhalla Group. Age: Rb/Sr 365.3 Ma and 365.6 Ma (Richards & Singleton, 1981).||||||22-DEC-08
17408|Strathbogie Granite|24328|5|Briefly described|Map legend|Late Devonian|Late Devonian|||||||
17408|Strathbogie Granite|24329|5|Briefly described|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
17408|Strathbogie Granite|24551|6|Mentioned|p408|Carboniferous|Late Devonian|Age: 360 +/- 12Ma, 370 +/- 2Ma.||||||
17408|Strathbogie Granite|30906|6|Mentioned|Map legend|Devonian|Devonian|||||||
17408|Strathbogie Granite|31713|5|Briefly described|p7|||||||||
17408|Strathbogie Granite|32074|6|Mentioned|p90|||Map legend. U.Dev.||||||
17408|Strathbogie Granite|33601|6|Mentioned|p22|||||||||
17408|Strathbogie Granite|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
17408|Strathbogie Granite|34989|6|Mentioned|p80|||||||||
17408|Strathbogie Granite|34990|6|Mentioned|p435|||||||||
17408|Strathbogie Granite|35111|6|Mentioned|p6|||||||||
17408|Strathbogie Granite|35277|6|Mentioned|Fig.5.8|||||||||
17408|Strathbogie Granite|35283|6|Mentioned|p48|||||||||
17408|Strathbogie Granite|36389|5|Briefly described|p39|||||||||
17408|Strathbogie Granite|37501|6|Mentioned|p405|||||||||
17408|Strathbogie Granite|39319|6|Mentioned|p361|||||||||
17408|Strathbogie Granite|39331|6|Mentioned|Fig.1-1|||||||||
17408|Strathbogie Granite|39861|6|Mentioned|Fig.2|||||||||
17408|Strathbogie Granite|41563|6|Mentioned|p506|||||||||
17408|Strathbogie Granite|41641|4|Described|p166|||||||||
17408|Strathbogie Granite|41868|6|Mentioned|p471|||||||||
17408|Strathbogie Granite|42383|5|Briefly described|Fig. 1 P3|||||||||
17408|Strathbogie Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
17408|Strathbogie Granite|42827|6|Mentioned|p150|||||||||
17408|Strathbogie Granite|43202|6|Mentioned|p22|||||||||
17408|Strathbogie Granite|44197|5|Briefly described|Map Legend||Late Devonian|G217 S-type.||||||
17408|Strathbogie Granite|45087|5|Briefly described|p26|||Chemical analyses||||||
17408|Strathbogie Granite|60452|5|Briefly described|p69|Late Devonian|Late Devonian|Age: 370-360Ma.||||||
17408|Strathbogie Granite|60529|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G217. Biotite cordierite granite: non-magnetic, S-Type; textural and lithological variations include fine grained, cordierite-rich granite, medium grained granite with minor cordierite, and coarse grained tourmaline rich granite.||||||14-JUN-06
17408|Strathbogie Granite|60599|6|Mentioned|p105|Late Devonian|Late Devonian|On the NAGAMBIE sheet. Similar to Mount Black Granite.||||||
17408|Strathbogie Granite|61185|4|Described|p47-52, p14, p24-25 Fig. 7|Late Devonian|Late Devonian|Part of Strathbogie Suite (previously of Strathbogie igneous complex). Intrudes and metamorphoses Wilson Creek Shale and Walhalla Gp (including Montys Hut Fm). Underlies Shepparton Fm sediments. S-type, fractionated granite. Age:365.3Ma, 365.6Ma Rb/Sr.||||||26-MAR-19
17408|Strathbogie Granite|61187|5|Briefly described|p5 Fig.3. |Late Devonian|Late Devonian|Melbourne Zone, Melbourne Terrane. Age interpreted from Fig.3.|c.370-c.365 Ma.|||||
17408|Strathbogie Granite|61210|5|Briefly described|p246 Fig. 2|Devonian|Devonian|Predominantly S-type granites of the Strathbogie batholith.||||||
17408|Strathbogie Granite|61701|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G217. Biotite cordierite granite: non-magnetic, S-Type; textural and lithological variations include fine grained, cordierite-rich granite, medium grained granite with minor cordierite, and coarse grained tourmaline rich granite.||||||25-JUL-06
17408|Strathbogie Granite|61702|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G217. Biotite cordierite granite: non-magnetic, S-Type; textural and lithological variations include fine grained, cordierite-rich granite, medium grained granite with minor cordierite, and coarse grained tourmaline rich granite.||||||25-JUL-06
17408|Strathbogie Granite|61703|5|Briefly described|Map Legend|Late Devonian|Late Devonian|G217. Biotite cordierite granite: non-magnetic, S-Type; textural and lithological variations include fine grained, cordierite-rich granite, medium grained granite with minor cordierite, and coarse grained tourmaline rich granite.||||||25-JUL-06
17408|Strathbogie Granite|61704|6|Mentioned|Map legend|Devonian|Devonian|Outcropping granite has high K, generally low (rarely high) Th.||||||
17408|Strathbogie Granite|64536|5|Briefly described|Map legend|Late Devonian|Late Devonian|Cordierite-biotite granite,: grey, coarse-grained; contains trace amounts of garnet; S-type intrusion.||||||07-FEB-11
17408|Strathbogie Granite|64537|5|Briefly described|Map legend|Late Devonian|Late Devonian|Cordierite-biotite granite,: grey, coarse-grained; contains trace amounts of garnet; S-type intrusion.||||||07-FEB-11
17408|Strathbogie Granite|64538|5|Briefly described|Map legend|Late Devonian|Late Devonian|Cordierite-biotite granite,: grey, coarse-grained; contains trace amounts of garnet; S-type intrusion.||||||07-FEB-11
17408|Strathbogie Granite|64606|5|Briefly described|Map Legend|Middle Devonian|Middle Devonian|Cordierite-biotite granite: S-type intrusive rock. Speckled blue and pink to white-yellow in RGB. Nonmagnetic.||||||
17408|Strathbogie Granite|64616|4|Described|p127, p177, p181 Fig.6.28, p185, p190|Late Devonian|Late Devonian|See also p199, p203-205, p207-210, p213, p246-248, p282, p302, p316, p332-333, p344. Of Strathbogie Suite (White and Chappell, 1988). Used here only for the coarse-grained granite of the eastern portion of the batholith, around Mount Strathbogie. Grey, coarse-grained, cordierite-biotite granite; contains trace amounts of garnet. Hosted a tourmaline pegmatite dyke. Historical nomenclature confused. Coeval with Violet Town Volcanics. Postdates deformation of surrounding sediments and gold mineralisation at Tallangalook. Zircon U-Pb date 374+/-2 Ma (Bierlein et al., 2001), K-Ar dates 360+/-3 Ma. Geophysical characteristics given.||||||
17408|Strathbogie Granite|65969|5|Briefly described|p6 Fig.2, p11, p19-20 Fig.9, p25 Tb.3.1|Tournaisian|Famennian|A deep magnetic response (c.200 nT) below this unit was called the Terip Terip Granite by Edwards (2001). Rb/Sr muscovite age of 365+/-6 Ma. U-Pb zircon age of 374+/-2 Ma (Bierlein et al., 2001). Non-magnetic.||||||
17408|Strathbogie Granite|66244|5|Briefly described|p3.|||Now includes the former Trawool Granite on the SW end of the Strathbogie Batholith.|||||Coarse-grained biotite granite with K-feldspar phenocrysts to 2 cm.|
17408|Strathbogie Granite|66575|6|Mentioned|p963.|||Melbourne Zone, Victoria. A non-extensional or post-kinematic Lachlan Orogen S-Type, formed after final closure of the western Lachlan backarc as the entire Lachlan Orogen amalgamated.||||||
17408|Strathbogie Granite|67804|5|Briefly described|p65|Late Devonian|Late Devonian|Intrusion post-dates gold mineralisation.|374 +/- 2 Ma (SHRIMP U-Pb).|||||
17408|Strathbogie Granite|67847|6|Mentioned|p12, p43|||||||||
17408|Strathbogie Granite|67978|5|Briefly described|p496 Fig.1, p500 Tb.1|Famennian|Famennian|Zircon dating by Kemp et al. (2008).|366 Ma, SIMS U-Pb||||S-type.|19-SEP-14
17408|Strathbogie Granite|68116|5|Briefly described|Appendix, Maps 25-26, 32.|Late Devonian|Late Devonian|Informally subdivided into an aplitic phase.|||||Coarse-grained porphyritic biotite-cordierite granite; K-feldspar phenocrysts, less common quartz phenocrysts, garnet and cordierite; tourmaline aggregates. Aplite: massive grey, quartz-feldspar-biotite with cordierite; black tourmaline-rich nodules.|
17408|Strathbogie Granite|69089|5|Briefly described|Map legend|Late Devonian|Late Devonian|S-type.||||||
17408|Strathbogie Granite|70629|5|Briefly described|p986, p1000|||Melbourne Zone. Has a similar major element composition as the nearby Mo- and W-bearing granitic intrusions at Monkey Gully; anomalously high Fe content, shown in Harker diagrams.|||||Includes local mafic and garnet-bearing parts.|
17408|Strathbogie Granite|70933|14|Not recorded|p91,103|||Geological map.||||||
17417|Strathmore Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Horshoe Creek (spelt Horshoe Creek) Subgroup.   Geological Province: Sydney Basin||||||
17417|Strathmore Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Horseshoe Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
17417|Strathmore Formation|29942|3|Fully described|p11|||||||||
17417|Strathmore Formation|45090|6|Mentioned|p187|||Refers Britten (1972)||||||
17417|Strathmore Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Horseshoe Creek Sub-group.||Overlies Alcheringa Coal. Is overlain by Lucernia Coal.|A dominantly shaly sequence, richly carbonaceous, with minor claystone and sandstone beds occurring between two thick and distinctive coal sequences.|
17417|Strathmore Formation|71864|6|Mentioned|p3|||||||||
17458|Stuckeys Creek Formation|31618|6|Mentioned|p102|||||||||
17458|Stuckeys Creek Formation|36534|6|Mentioned|p225|||||||||
17517|Summit Porphyritic Granodiorite|38915|6|Mentioned|p338|||||||||
17521|Sun Valley Member|22736|6|Mentioned|p619,22|Namurian|Visean|part of Cooperabung Formation.||||||
17521|Sun Valley Member|38803|5|Briefly described|p105|||||||||
17531|Sundown Group|6823|5|Briefly described|p203, 205, 208, 211, 218-221, 223,|Palaeoproterozoic|Palaeoproterozoic|Metamorophic ages of 1593 +/- 10 Ma and 1636 +/- 10 Ma are provided, along with a crystallisation age of 1636+/-10 Ma. All ages reported herein are derived from this study. See also p227, 230, 232-236.  See also Sundown Schist p235.|1636 +/- 10 Ma (SHRIMP U-Pb zircon)|Willyama Supergroup||||26-MAR-22
17531|Sundown Group|22463|6|Mentioned|22 fig 27|Statherian|Statherian|Parent Willyama Supergroup Geol province Broken Hill - Olary Domain||||||
17531|Sundown Group|22500|4|Described|p3, 4, 13  Fig 5||Statherian|Age 1690Ma. Of the Willyama Supergroup.||||||29-MAY-07
17531|Sundown Group|22553|5|Briefly described|fig2p77,p83|||||||||
17531|Sundown Group|22575|6|Mentioned|p179 Fig.2|||||||||
17531|Sundown Group|22588|6|Mentioned|p85|||||||||
17531|Sundown Group|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
17531|Sundown Group|22771|5|Briefly described|Table12.2p45,47-48|||||||||
17531|Sundown Group|22857|4|Described|p45 Tb. 12.2, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Predominantly non-graphitic metasediment. Max. thickness: 1500m (1400 in type section). Geological Province: Willyama Fold Belt.||||||07-NOV-08
17531|Sundown Group|22884|6|Mentioned|p40 Fig. 1, p46|||Geological province: Broken Hill Domain; but also contains the only constituent/formation in the Olary Domain, namely, Mustering Paddock Formation.||||||11-JUN-14
17531|Sundown Group|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|22962|6|Mentioned|p74||Statherian|||||||
17531|Sundown Group|22963|5|Briefly described|p69||Paleoproterozoic|Broad correlation with the Mt Isa Llewellyn Creek Formation and the Georgetown (Qld) Daniel Creek Formation.||||||07-NOV-08
17531|Sundown Group|22964|6|Mentioned|p55,56||Proterozoic|||||||
17531|Sundown Group|22965|6|Mentioned|Fig 1||Statherian|||||||
17531|Sundown Group|22966|5|Briefly described|p2,3,4||Proterozoic|||||||
17531|Sundown Group|22967|5|Briefly described|p25,6,30,Fig14||Statherian|||||||
17531|Sundown Group|23025|6|Mentioned|Fig1p75|||||||||
17531|Sundown Group|23039|6|Mentioned|p166||Statherian|||||||
17531|Sundown Group|23160|6|Mentioned|fig1|||||||||
17531|Sundown Group|23223|5|Briefly described|p43|||Of the informal Upper Willyama Supergroup. Curnamona Province.||||||16-JUN-09
17531|Sundown Group|23248|5|Briefly described|Fig2p169|||||||||
17531|Sundown Group|23346|6|Mentioned|48|||||||||
17531|Sundown Group|23347|6|Mentioned|p54|||Geological province: Broken Hill Domain. Equivalent to Olary Domain rocks of the Strathearn Group.||||||24-MAR-09
17531|Sundown Group|23390|6|Mentioned|p8|||||||||
17531|Sundown Group|23391|6|Mentioned|p6|||||||||
17531|Sundown Group|23461|5|Briefly described|p202|||||||||
17531|Sundown Group|23565|6|Mentioned|p195|||||||||
17531|Sundown Group|24197|5|Briefly described|p62|||Of the Willyama Supergroup. Shallow marine sediments. Geological province: Broken Hill Block.||||||07-FEB-11
17531|Sundown Group|24307|4|Described|p974|Proterozoic|Proterozoic|||||||
17531|Sundown Group|38969|4|Described|p209|||||||||
17531|Sundown Group|39662|2|Defined|p431|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39826|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|39849|6|Mentioned|p87|||||||||
17531|Sundown Group|39883|6|Mentioned|p380|||||||||
17531|Sundown Group|40290|6|Mentioned|Fig.2|||||||||
17531|Sundown Group|40595|6|Mentioned|p86|||||||||
17531|Sundown Group|40822|6|Mentioned|Fig.2|||||||||
17531|Sundown Group|41093|4|Described|p253|||||||||
17531|Sundown Group|41145|5|Briefly described|p827|||||||||
17531|Sundown Group|41402|6|Mentioned|p37|||||||||
17531|Sundown Group|41630|5|Briefly described|p3|||See also p27.||||||10-OCT-06
17531|Sundown Group|41633|6|Mentioned|Fig.2.2|||||||||
17531|Sundown Group|41651|6|Mentioned|p189|||||||||
17531|Sundown Group|42261|6|Mentioned|Fig 1 P530|||||||||
17531|Sundown Group|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
17531|Sundown Group|42537|4|Described|p14|||||||||
17531|Sundown Group|42595|6|Mentioned|Fig. 2 P5|||||||||
17531|Sundown Group|42720|5|Briefly described|map legend|Paleoproterozoic||Same as Sundown Group, NSW.||||||07-NOV-08
17531|Sundown Group|42813|6|Mentioned|p9|||||||||
17531|Sundown Group|42897|5|Briefly described|Fig.3, P321|||||||||
17531|Sundown Group|42942|6|Mentioned|p17|||of Willyama Supergroup||||||
17531|Sundown Group|43052|6|Mentioned|p98|||||||||
17531|Sundown Group|43086|6|Mentioned|Fig.3|||||||||
17531|Sundown Group|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|43265|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43266|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43269|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43271|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
17531|Sundown Group|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|43485|6|Mentioned|2||Proterozoic|of Willyama Complex||||||
17531|Sundown Group|43572|6|Mentioned|Fig.3.2 p6|||||||||
17531|Sundown Group|43583|5|Briefly described|Table 1, p2138|||||||||
17531|Sundown Group|46598|4|Described|p304|||See also p302.||||||18-JAN-07
17531|Sundown Group|50045|4|Described|p115 Fig. 2, p116 Fig. 3|Statherian|Statherian|Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Paragon Group; underlain by Broken Hill Group. Age: 1640 Ma.||||||31-MAY-07
17531|Sundown Group|50606|5|Briefly described|p1.1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup.||||||
17531|Sundown Group|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Psammite and pelite deposits. Conformably overlies the Broken Hill Group; conformably overlain by the Paragon Group. Geological Province: Broken Hill Block.||||||15-MAY-13
17531|Sundown Group|60485|5|Briefly described|p28 Fig. 2|Statherian|Statherian|Age: <1672+/-7Ma. Equivalent to Saltbush Subgroup (Olary Domain). Geological Province: Broken Hill Domain.||||||15-MAY-13
17531|Sundown Group|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Age: <1700Ma. Geological Province: Broken Hill.||||||07-NOV-08
17531|Sundown Group|61606|5|Briefly described|p4 Fig. 2|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
17531|Sundown Group|61735|5|Briefly described|p649, p635 Fig. 1, p638, 639|Paleoproterozoic|Paleoproterozoic|Overlies Broken Hill Group. Age: 1680-1670Ma.  In the Euriowie Block. Includes psammites. See also p636 Fig. 2, p649-50.||||||04-JUN-15
17531|Sundown Group|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Ages for rocks within the group: </-1672+/-7Ma and </-1690Ma. Geological province: Broken Hill Domain.||||||
17531|Sundown Group|61908|5|Briefly described|p146|||Geological Province: Broken Hill Block.||||||
17531|Sundown Group|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
17531|Sundown Group|62373|5|Briefly described|p503 Fig.2|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Geological Province: Curnamona Province/Olary Domain.||||||07-NOV-08
17531|Sundown Group|62473|5|Briefly described|p73-4|Paleoproterozoic|Paleoproterozoic|Max. age: 1670Ma. Geological province: Broken Hill Domain. Dominantly pelitic.||||||17-JUN-09
17531|Sundown Group|62535|5|Briefly described|p666 Fig.3, p671-674|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.|<1672 +/- 7 Ma.|||Equivalent to the Saltbush Subgroup.|Mainly pelitic and psammopelitic schist with variable thin, planar psammite beds and occasional calc-silicate-rich ellipsoidal structures.|
17531|Sundown Group|62536|4|Described|p633, 635-636, 638-641, 649-650, 654|||See also p658-659. Broken Hill area. A variety of age determinations presented; depositional age remains uncertain. Metamorphosed c.1608-1598 Ma. Similar zircon provenance ages as Broken Hill Group and upper Paragon Group. Contains little stratiform mineralisation.|1788 +/- 8 Ma (MDA).||Cartwrights Creek Metasediments.|Overlies Broken Hill Group.|Layered, migmatised metasedimentary rocks.|
17531|Sundown Group|62592|5|Briefly described|p14, p15, p16 Fig.2.2.|||Broken Hill Domain, Curnamona Province. Equivalent to the Saltbush Group in the Olary Domain. Coeval with the northern Australian Pb-Zn basins; possibly prospective for Mount Isa and Century styles of mineralisation.|<1672 +/- 7 Ma.|Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|62728|5|Briefly described|p25 Fig. 2|||Geological Province: Curnamona Province.||||||07-FEB-11
17531|Sundown Group|62993|6|Mentioned|p35, p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup||||19-DEC-21
17531|Sundown Group|63020|5|Briefly described|p987 Fig. 8|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province (Broken Hill Domain).||||||07-NOV-08
17531|Sundown Group|63102|5|Briefly described|p9,13-14,32-34,39|Neoproterozoic|Neoproterozoic|Geological province: Broken Hill Domain, Curnamona Province.|<1672+\-7 Ma|||Equivalent to Walparuta Formation; Saltbush Subgroup.||
17531|Sundown Group|63110|6|Mentioned|p1129 Fig. 8|||Comprises pelitic to psammitic metasedimentary rocks.||||||11-JUN-08
17531|Sundown Group|63186|5|Briefly described|p66, p67,p70|Paleoproterozoic|Paleoproterozoic|Age: 1612+/-18 Ma and 1601+/-18 Ma (monzaite mean) and 1645 Ma. Geological Province: Broken Hill Domain, Curnamona Province.||||||07-NOV-08
17531|Sundown Group|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Pelitic to psammitic metasediments. Geological Province: Broken Hill Domain; with unnamed equivalents in Olary Domain.||||||07-NOV-08
17531|Sundown Group|63519|5|Briefly described|p6 Fig. 2, p7|Paleoproterozoic|Paleoproterozoic|Overlain by Paragon Gp with sharp contact; overlies Broken Hill Gp. Age: <1690Ma. Metasediments, not strongly deformed and preserving sedimentary structures. Geol Prov: Broken Hill Block-Euriowie Block. See also p29 Fig. 11.||||||07-NOV-08
17531|Sundown Group|63866|4|Described|p36, p38, p40|||Broken Hill Domain, Curnamona Province. U-Pb zircon ages are derived from Page et al., 2005a and are interpreted as the maximum depositional ages for this group.|1688 +/- 6 Ma (U-Pb zircon) and 1672 +/- 7 Ma|Willyama Supergroup||Overlies the Hores Gneiss (Broken Hill Group). Equivalent to the Saltbush Group.|Thin-bedded, commonly graded pelite, psammopelite and psammite with calc-silicate nodules.|
17531|Sundown Group|64097|5|Briefly described|p302, p303|Paleoproterozoic|Paleoproterozoic|Of the Willyama Group. Underlies Paragon Group; overlies Broken Hill Group. Age: 1680-1670Ma. Mostly siliciclastic metasediments||||||07-FEB-11
17531|Sundown Group|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.||Unit in Willyama Supergroup.||||
17531|Sundown Group|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Overlain by Paragon Group. Lithology is progressively greater in pelitic-psammitic component upwards into this group.  Geological Province: Broken Hill Block||||||07-FEB-11
17531|Sundown Group|64722|5|Briefly described|Fig. 5 p.13|Statherian|Statherian|Broken Hill region, South Australian Craton.||Of Willyama Supergroup.||||11-APR-12
17531|Sundown Group|64725|6|Mentioned|p58 Fig.2. |||||||||
17531|Sundown Group|64741|5|Briefly described|p301 Fig. 4, p309, p310|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergp.Overlies Broken Hill Gp. Age in upper levels:<1672+/-7Ma. Max.thickness: 1500m.Geol.prov: Broken Hill Domain. Comprises schistose interlayered psammopelite and pelite - more lith.detail (p309). Equiv.in Olary Domain is Walparuta Fm.||||||07-FEB-11
17531|Sundown Group|64742|5|Briefly described|p320, p323, pp327-328, p330. |||Broken Hill Domain. Major and trace element analyses, and Sm-Nd isotope data, are detailed.|<1672 Ma.|Unit in Willyama Supergroup.|||Psammites, calc-silicate rock.|
17531|Sundown Group|64743|5|Briefly described|pp339-340, pp342-344,  p346 Fig.7. |Paleoproterozoic|Paleoproterozoic|Broken Hill Block. Type section is c.1.35 km thick.|1690-1670 Ma.|Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|64744|5|Briefly described|p353 Fig.4, p356, p358. |Statherian|Statherian|Broken Hill Domain. Psammopelitic sediments.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of Willyama Supergroup. Age at upper levels: <1672+/-7Ma. Geological province: Broken Hill Domain.||||||07-FEB-11
17531|Sundown Group|65681|6|Mentioned|p734 Fig.1.|||Broken Hill Block.||||||
17531|Sundown Group|65887|5|Briefly described|p51|||Primarily pelitic and psammo-pelitic metasediments. Thought to be deposited in a continental slope to deep water environment.||||||
17531|Sundown Group|66302|4|Described|p35, p36 Fig.9, p37, p39, p40, p73|Statherian|Statherian|Olary Domain, Curnamona Province. Ages are derived from Page et al. (2005).|1688 +/- 6 Ma to 1672 +/- 7 Ma|Willyama Supergroup||Equivalent to the Saltbush Group.|Thin-bedded, commonly graded mudstone, siltstone and sandstone with calcsilicate nodules.|
17531|Sundown Group|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.||
17531|Sundown Group|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|1672 +/- 7 Ma (maximum depositional age).|||Overlies Broken Hill Group.||
17531|Sundown Group|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
17531|Sundown Group|68126|5|Briefly described|p6, p26, p29-30|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|~1685-1670 Ma (Page et al. in prep).|Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group. Equivalent to Saltbush Group.||
17531|Sundown Group|68315|6|Mentioned|p766|||Broken Hill district, Curnamona Province. Cut by the Stephens Creek Shear Zone.|||||Upper amphibolite-facies metapelites and felsic gneisses.|
17531|Sundown Group|69999|5|Briefly described|p3,p7 Photo 4,p9 Photo 9,p12-15,p18,p20|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Middle, rift-deepening, marine transgressive sedimentation with increased magmatic input. Represents much of the amphibolite facies for the Olarian Orogeny.||||||
17531|Sundown Group|70000|5|Briefly described|p31, p33-34, p36|Statherian|Statherian|Lithologically identical to upper part of Broken Hill Group, but lacks any syn-depositional igneous units.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain conformably by Paragon Group.|Interbedded pelite, psammopelitic and psammitic metasedimentary rocks.|
17531|Sundown Group|70014|5|Briefly described|Map legend|||Bedding well-developed within the metasediments, generally planar and continuous to lenticular. Graded bedding, small-scale cross-bedding, flame structures, and symmetrical and asymmetrical (climbing) ripple marks also present. Intrusive concordant and discordant K-feldspar-rich leucocratic rocks and intermixed pegmatite in some areas. Vary rare basic gneiss and quartz-gahnite rocks near the base. Rare finely-bedded quartz-tourmaline rocks and tourmaline schists also occur near the base. Zoned calc-silicate nodules are widespread in the metasediments.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.|Predominantly non-graphitic metasediment. Pelite-psammopelite units most abundant and more common in the lower half; psammite-psammopelite units more common in the upper half. Minor metasedimentary composite gneiss.|
17531|Sundown Group|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.||Overlies Broken Hill Group. Is overlain by Paragon Group.|Metapelite-metapsammopelite (abundant at base), and metapsammite-metapsammopelite (abundant at top); common calc-silicate ellipsoids; small basic gneiss and quartz-gahnite bodies at base.|
17531|Sundown Group|70405|6|Mentioned|p15, p29, p43 Table 3|Mesoproterozoic|Paleoproterozoic||1665 Ma-1680 Ma|Wilyama Supergroup||Correlated with Walparuta Formation||
17531|Sundown Group|70657|4|Described|p5, p6 Fig.1, p10 Fig.4, p11 Fig.5|Statherian|Statherian|See also p13 Fig.6, p14-15, p17, p33, p40, p44. Curnamona Province; Broken Hill, Mulyungarie, Olary Domains. Age inferred from Fig.4, but p15 suggests a minimum age c.1670 Ma. Fig.6 seems to suggest it includes Raven Hill Subgroup. With Broken Hill Group, is stratigraphically equivalent to Saltbush Group.|~1685-1655 Ma|Upper Willyama Supergroup.||Overlies Broken Hill Group. Underlies Cartwrights Creek Metasediments (Paragon Group). Equivalent to Walparuta Formation.||
17531|Sundown Group|70658|5|Briefly described|p2, 7, 15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.|<1672 +/- 7 Ma.|Willyama Supergroup.||Equivalent to Walparuta Formation.||
17531|Sundown Group|70858|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province. Regarded by the authors as a good candidate for 1.75 Ga and younger detrital zircons in the Wernecke Supersuite, Yukon.||Willyama Supergroup.||||
17531|Sundown Group|71799|5|Briefly described|p150 fig 2|Statherian|Statherian|Curnamona Province.|ca 1650 Ma|||Overlain by the Cartwrights Creek Formation|Sandstone and greywacke.|
17531|Sundown Group|71968|4|Described|p1-13,18,28,41,45,47-48|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province. Widespread in the Broken Hill Block. Page et al. (2005) reported maximum depositional ages of 1688+\-6 Ma in the Euriowie Block and 1672+\-7 Ma in the Monuments area. Sample GA 2676607 (sillimanite-rich psammite) yielded weighted mean 207Pb/206Pb ages of 1790+\-6 Ma and 1556+\-33 Ma, interpreted to be maximum depositional age of the psammite and minimum age for metamorphic zircon growth respectively. Reflects the usual spectrum of clastic zircon ages of the Willyama Supergroup.  Change from sliciclastic-dominated Sundown Group to fine-grained carbonaeous Paragon Group reflect a significant decrease (starving) in siliciclastic sediment input to the Curnamona Rift Basin; also reflects a change from older detrital zircons (c. 1792 Ma) in Sundown Group to younger populations in Paragon Group (c. 1754 Ma), possibly indicating a change in sediment source and supply and possibly exposure of a new source region based on relative sea level change.||Unit of Willyama Supergroup.||Overlain conformably by Paragon Group.|Predominantly metasediments, dominantly pelitic to psammopelitic rock units, with scattered calcsilicate nodules.|
17531|Sundown Group|72435|6|Mentioned|p715|Statherian|Statherian|Upper boundary with Paragon Group is gradational in places.|Between 1685 Ma and 1670 Ma|||Overlain by Paragon Group.||
17531|Sundown Group|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain. Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup||||
17531|Sundown Group|72461|5|Briefly described|p5-6, p13, p16, p19|||||Willyama Supergroup||Overlies the Broken Hill Group. Overlain Conformably by the Paragon Group.|Sedimentary rocks.|
17531|Sundown Group|73243|6|Mentioned|p52-53, p58-59, p61, p67, p78-79|Statherian|Statherian|Broken Hill block-Euriowie block. Shown on p52 Fig.1 and p53 Fig.2.|~1670-1680 Ma|Willyama Supergroup|||Metasediments.|
17531|Sundown Group|73308|4|Described|p605-607, 611-618, 620, 622-623|||Broken Hill Block. Hydrothermal plumes are proposed as the source of much of these magnetite deposits.|c.1680-1670 Ma.|Willyama Supergroup.||Overlies Hores Gneiss (Broken Hill Group).|Metasediments (pelitic to psammitic schists) containing small amounts of bedding-controlled magnetite. Granulite facies metamorphism.|
17531|Sundown Group|73429|5|Briefly described|p106 Fig.2, p107|Statherian|Statherian|Curnamona Province. Broken Hill Domain, Mulyungarie Domain.||Willyama Supergroup, upper||Overlies Broken Hill Group||
17531|Sundown Group|73482|5|Briefly described|p419, p422 Fig.3, p423, p425-427, p430|Statherian|Statherian|Areas of stratigraphy are parallel to the andalusite-sillimanite isograd, in other areas the isograd crosses stratigraphy. See also p424 Fig.4, p428 Fig.7, p429 Fig.8, p432-434.|1670-1680 Ma|Willyama Supergroup||Overlies Broken Hill Group, underlies Paragon Group|Metasediments. Andalusite and silimanite metamorphic grades, partially melted in parts.|
17531|Sundown Group|73512|5|Briefly described|p2-3|Statherian|Statherian|Curnamona Province, Broken Hill Block. Represents deeper-water basin fill.||Willyama Supergroup||Underlain by Broken Hill Group. Overlain by Paragon Group.||
17531|Sundown Group|73524|6|Mentioned|p2, p5 Fig.3|||Rift-phase metasediments.||lower Willyama Supergroup||||
17531|Sundown Group|73575|5|Briefly described|p828 Fig.2, p829 Fig.3, p835-836, p841|Statherian|Statherian||1670-1680 Ma|Willyama Supergroup||Overlies Broken Hill Group, Purnamoota Subgroup, Hores Gneiss, underlies Paragon group, Cartwrights Creek Metasediments||
17546|Surat Siltstone|12597|5|Briefly described|p492 Tb.1, p493 Fig.2, p495 Fig.3, p498|Albian|Albian|N Surat Basin. 100-130m thick.||||Overlies Coreena Member (Wallumbilla Formation).|Interbedded siltstone (commonly micaceous) and mudstone (generally carbonaceous and pyritic) with lenses of fine-grained glauconitic sandstone; small pelecypods common.|
17546|Surat Siltstone|13516|5|Briefly described|p167 fig 10, p169 fig 11|Early Cretaceous|Early Cretaceous|In Surat Basin, Eromanga Basin.||?Of Rolling Downs Group||||
17546|Surat Siltstone|22757|5|Briefly described|Table6,p11||Early Cretaceous|150 m thick. Surat Basin.||||||21-APR-09
17546|Surat Siltstone|22857|5|Briefly described|p296-7 Tb.22.1, p315 Fig. 22.8|Albian|Albian|Of the Rolling Downs Group. Basal mudstone overlain by thinly bedded siltstone. Equivalent to Surat Siltstone (Wallumbilla Formation) in Eromanga Basin. Max. thickness: ~220m. Geol. Province: Surat Basin. See also p312-3 Fig.22.6, p544 App.1 Tb.A1.12.||||||
17546|Surat Siltstone|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Albian|||||||
17546|Surat Siltstone|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||13-MAR-09
17546|Surat Siltstone|23911|5|Briefly described|p96 Fig. 10, p97 Fig. 11|Cretaceous|Cretaceous|Geological Basin: Surat Basin.||||||
17546|Surat Siltstone|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
17546|Surat Siltstone|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 110m.||||||
17546|Surat Siltstone|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
17546|Surat Siltstone|29387|6|Mentioned|Table 5|||||||||
17546|Surat Siltstone|29721|6|Mentioned|Table 246|||||||||
17546|Surat Siltstone|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
17546|Surat Siltstone|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
17546|Surat Siltstone|31116|4|Described|p44|||See also Table 2. Cretaceous.||||||
17546|Surat Siltstone|31208|6|Mentioned|Table 1|||See also Fig. 3 & 567. Early Albian||||||
17546|Surat Siltstone|31376|6|Mentioned|p4|||||||||
17546|Surat Siltstone|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|32314|6|Mentioned|Fig. 4|||||||||
17546|Surat Siltstone|32796|2|Defined|p301|middle Albian|early Albian|Lower-Middle Albian||||||
17546|Surat Siltstone|33016|6|Mentioned|p25|||||||||
17546|Surat Siltstone|33070|4|Described|Table 2|||L.Cret.||||||
17546|Surat Siltstone|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|33090|4|Described|Table 4|||L.Cret.||||||
17546|Surat Siltstone|33091|5|Briefly described|p9|||Strat.||||||
17546|Surat Siltstone|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|33448|6|Mentioned|p7|||||||||
17546|Surat Siltstone|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|34613|4|Described|Table 4|||||||||
17546|Surat Siltstone|35793|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
17546|Surat Siltstone|35937|6|Mentioned|Fig.5|||||||||
17546|Surat Siltstone|36243|6|Mentioned|Table 7A|||||||||
17546|Surat Siltstone|36581|6|Mentioned|p464|||||||||
17546|Surat Siltstone|37117|5|Briefly described|p313|||||||||
17546|Surat Siltstone|37995|4|Described|p66|||||||||
17546|Surat Siltstone|39211|5|Briefly described|Fig.21|||||||||
17546|Surat Siltstone|39212|5|Briefly described|p18|||||||||
17546|Surat Siltstone|39445|5|Briefly described|Table 11|||||||||
17546|Surat Siltstone|39943|6|Mentioned|Table 9B|||||||||
17546|Surat Siltstone|40245|6|Mentioned|Table 2|||||||||
17546|Surat Siltstone|40249|6|Mentioned|p38|||||||||
17546|Surat Siltstone|40801|6|Mentioned|p65|||||||||
17546|Surat Siltstone|41060|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|41064|6|Mentioned|p62|||||||||
17546|Surat Siltstone|41187|6|Mentioned|Fig.2|||||||||
17546|Surat Siltstone|41216|6|Mentioned|Fig.18|||||||||
17546|Surat Siltstone|41266|6|Mentioned|Fig.3|||||||||
17546|Surat Siltstone|41992|4|Described|Fig.2 P183|||||||||
17546|Surat Siltstone|42007|5|Briefly described|Fig.2 P182|||||||||
17546|Surat Siltstone|42429|5|Briefly described|p155|||||||||
17546|Surat Siltstone|42494|5|Briefly described|Table 1 P24|||||||||
17546|Surat Siltstone|42673|5|Briefly described|Fig.2, P184|||||||||
17546|Surat Siltstone|43000|5|Briefly described|Fig.5,p112|||Of Rolling Downs Group.||||||13-MAR-09
17546|Surat Siltstone|43002|5|Briefly described|Fig.2,p135|||||||||
17546|Surat Siltstone|43602|5|Briefly described|Fig3 p194|||In Surat Basin, Rolling Downs Group.||||||21-APR-09
17546|Surat Siltstone|45110|2|Defined|p120|middle Albian|middle Albian|See also P24.||||||
17546|Surat Siltstone|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
17546|Surat Siltstone|46791|4|Described|p47|||||||||
17546|Surat Siltstone|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
17546|Surat Siltstone|46984|6|Mentioned|Table 1|||||||||
17546|Surat Siltstone|49010|6|Mentioned|Fig.4|||Surat Basin||||||
17546|Surat Siltstone|49011|6|Mentioned|Fig.3|||Surat Basin||||||
17546|Surat Siltstone|60524|5|Briefly described|p488|Albian|Albian|Marine unit.  Geological Province: Surat Basin.||||||
17546|Surat Siltstone|61221|6|Mentioned|p1||Cretaceous|Geological Province: Surat Basin.||||||
17546|Surat Siltstone|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Siltstone, mudstone. Geological Province: Surat Basin.||||||07-FEB-11
17546|Surat Siltstone|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.||||||13-MAR-09
17546|Surat Siltstone|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|64197|6|Mentioned|p630 Fig.7|Cretaceous|Cretaceous|Surat Basin||||Underlies Griman Creek Formation; overlies Wallumbilla Formation.||
17546|Surat Siltstone|64856|3|Fully described|p79, p100-102|Albian|Albian|Surat Basin only. Of Reiser (1970). Implied type section is the interval 15-140m in GSQ Surat 1. Fine-grained sediments and sandstone. Conformably overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation. 100-130m thick. Associated with palynofloral units APK4 and 51. Contains dinoflagellate assemblages conformable with units ADK19, 21.|| ||||29-NOV-17
17546|Surat Siltstone|64857|5|Briefly described|p113 Fig.3|||Overlies Wallumbilla Formation, Surat Basin.||||||
17546|Surat Siltstone|64858|6|Mentioned|p187-188|||See also Surat Formation.||||||30-NOV-09
17546|Surat Siltstone|65112|6|Mentioned|Fig 11 p324|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin. Underlies the Griman Creek Formation; overlies the Coreena Member of the Wallumbilla Formation.||||||22-MAR-12
17546|Surat Siltstone|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Coreena Member and Wallumbilla Formation, underlies the Griman Creek Formation.||||||
17546|Surat Siltstone|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
17546|Surat Siltstone|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Underlies the Griman Creek Formation, Overlies both the Coreena Member and Wallumbilla Formation, Surat Basin.||||||
17546|Surat Siltstone|65119|6|Mentioned|Fig 6 p512, Fig 14 p521|Early Cretaceous|Early Cretaceous|Includes siltstone, mudstone and sandstone. Present in the Cabawin 1 well. See also variation Surat Sandstone p503.||||||07-MAR-12
17546|Surat Siltstone|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|66623|6|Mentioned|p258, p262.|||Surat Basin. Partly equivalent to Coreena Member.||||||
17546|Surat Siltstone|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
17546|Surat Siltstone|67402|4|Described|p146 fig SRT3, p148, p156|Albian|Albian|Surat Basin. Deposited in shallow marine or coastal swamp environments. Approximately 125m thick.||||Overlies the Wallumbilla Formation. Overlain by the Griman Creek Formation.|Interbedded carbonaceous siltstone and mudstone.|
17546|Surat Siltstone|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shallow marine environment. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group||Conformably overlies Wallumbilla Formation. Is conformably overlain by Griman Creek Formation.|Interbedded siltstone and carbonaceous and pyritic mudstone.|22-NOV-13
17546|Surat Siltstone|68117|6|Mentioned|p346|Early Cretaceous|Early Cretaceous|Surat Basin.||||||
17546|Surat Siltstone|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|68593|5|Briefly described|p4, p6, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.||Rolling Downs Group.||Overlies Wallumbulla Formation. Is overlain conformably by Griman Creek Formation.|Interbedded siltstone and carbonaceous and pyritic mudstone.|
17546|Surat Siltstone|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Albian|Albian|Surat Basin. Shallow marine.||Of the Rolling Downs Group.||||
17546|Surat Siltstone|68821|5|Briefly described|p292 Fig.1, p295|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent in age to the Toolebuc Formation.||Of the Rolling Downs Group.||Overlain by the Griman Creek Siltstone.||
17546|Surat Siltstone|69582|6|Mentioned|p36|Early Cretaceous|Early Cretaceous|Surat Basin.||||Overlies the Wallumbilla Formation. Overlain by the Griman Creek Formation.||
17546|Surat Siltstone|69594|5|Briefly described|p519, p538-539, p574|Albian|Albian|Reiser (1970). Entirely restricted to the Surat Basin. Generally 100-130m thick. Shallow-marine, intertidal, protected bay deposits; coastal swamps in the east.||||Conformably overlies Coreena Member (Wallumbilla Formation). Is overlain conformably by Griman Creek Formation.|Dominated by interbedded carbonaceous siltstones and mudstones with labile sandstone lenses. Mudstone dominates the lowest one-fifth of the Formation but in the east, lithic sandstones dominate throughout.|
17546|Surat Siltstone|69681|6|Mentioned|p74 Fig.3|Early Cretaceous|Early Cretaceous|||||||
17546|Surat Siltstone|70821|5|Briefly described|p21 Fig 2.6, p22 Fig.2.7, p80|Early Cretaceous|Early Cretaceous|Surat Basin.||Rolling Downs Group.||Overlies Coreena Member (Wallumbilla Formation). Is overlain by Griman Creek Formation.||14-DEC-16
17546|Surat Siltstone|70836|6|Mentioned|p474|||Lightning Ridge area, Surat Basin. Albian.||||Overlies Wallumbilla Formation. Is overlain by Griman Creek Formation.||
17546|Surat Siltstone|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Surat Basin (QLD,NSW).||||Overlies Coreena Member (Wallumbilla FZ). Is overlain by Griman Creek FZ.||
17546|Surat Siltstone|73113|6|Mentioned|p22|Late Cretaceous|Late Cretaceous|Partial aquifer.||||||
17560|Sutton Forest Formation|31297|6|Mentioned|p8|||||||||
17560|Sutton Forest Formation|34139|6|Mentioned|p23|||Table||||||
17560|Sutton Forest Formation|36220|6|Mentioned|p69|||||||||
17568|Swains Gully Limestone|41279|6|Mentioned|Fig.3|||||||||
17568|Swains Gully Limestone|70050|6|Mentioned|p365|Tournaisian|Tournaisian|Contains Amygdalophyllum fossils.||||||
17571|Swamp Creek Member|40328|6|Mentioned|Fig.12(H3)|||||||||
17571|Swamp Creek Member|45147|6|Mentioned|M159|||||||||
17602|Sydney Subgroup|22857|4|Described|p532 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Contains Bulli, Balgownie, Wongawilli, American Creek, Tongarra and Woonona coal seams. Max. thickness: 165m. Geological Province: Sydney Basin.||||||
17602|Sydney Subgroup|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
17602|Sydney Subgroup|24471|5|Briefly described|p32 Fig.4|||Applies to eastern part of the Southern Coalfield of the Illawarra Coal Measures. Overlies Cumberland Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
17602|Sydney Subgroup|31649|6|Mentioned|p59|||||||||
17602|Sydney Subgroup|36593|6|Mentioned|Table 1|||||||||
17602|Sydney Subgroup|37065|6|Mentioned|p32|||||||||
17602|Sydney Subgroup|39661|6|Mentioned|p443|||||||||
17602|Sydney Subgroup|40631|6|Mentioned|p162|||||||||
17602|Sydney Subgroup|42737|5|Briefly described|map legend|Permian||||||||
17602|Sydney Subgroup|42896|3|Fully described|p19, Table 2|||Of Illawarra Coal Measures.||||||12-MAR-09
17602|Sydney Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
17602|Sydney Subgroup|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin.||||||13-NOV-13
17602|Sydney Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Includes at least 13 named units. Geological Province: Sydney Basin||||||
17602|Sydney Subgroup|61609|6|Mentioned|p240 Tb. 1, p246 Fig. 5|Permian|Permian|Of Illawarra Coal Measures. Includes nine units. Geological Province: Sydney Basin.||||||07-FEB-11
17602|Sydney Subgroup|61610|5|Briefly described|p252|||Of Illawarra Coal Measures. Includes Wilton Formation. Geological Province: Sydney Basin.||||||07-FEB-11
17602|Sydney Subgroup|68003|5|Briefly described|pp41-42.|Late Permian|Late Permian|Illawarra region, Sydney Basin. Formed by southward-prograding major fluvio-deltaic systems.||||||
17602|Sydney Subgroup|69297|6|Mentioned|p502 fig 5.43|||Sydney Basin.||||||
17602|Sydney Subgroup|70661|6|Mentioned|p187|||Only subgroup of the Illawarra Coal Measures known in the Moss Vale map area. Deposited in a fluvial or deltaic environment with some shallow marine or braided fluvial deposition also recognised.||Illawarra Coal Measures||||
17602|Sydney Subgroup|73421|6|Mentioned|p19|Changhsingian|Capitanian|Sydney Basin, southern. Also includes Loddon Sandstone, Bulli Coal.||Illawarra Coal Measures|Wilton Formation, Tongarra Coal, Bargo Claystone, Darkes Forest Sandstone, Allans Creek Formation, Kembla Sandstone, Wongawilli Coal, Eckersley Formation, Burragorang Claystone, Balgownie Coal|||
17620|Tabita Formation|12066|5|Briefly described|p13|||||||||
17620|Tabita Formation|13995|5|Briefly described|p82-83, p99, p101|Middle Ordovician|Early Ordovician|Gnalta Shelf. Contains similar trilobite taxa as Caroline Creek Sandstone in Tasmania.||||||
17620|Tabita Formation|22857|5|Briefly described|p122, p408 App. 1 Tb. A1.4.|Ordovician|Cambrian|Shale and carbonates. Geological Province: Mount Arrowsmith Block.||||||
17620|Tabita Formation|23245|5|Briefly described|p122|Ordovician|Cambrian|||||||
17620|Tabita Formation|33738|6|Mentioned|p52|||||||||
17620|Tabita Formation|35118|6|Mentioned|Fig.5|||||||||
17620|Tabita Formation|36047|6|Mentioned|p369|||||||||
17620|Tabita Formation|38692|6|Mentioned|p138|||||||||
17620|Tabita Formation|40136|5|Briefly described|p40|||See also p27.||||||11-SEP-07
17620|Tabita Formation|41810|6|Mentioned|p111|||||||||
17620|Tabita Formation|44093|5|Briefly described|p142 App. 1|Early Ordovician|Cambrian|Geological Province: Kanmantoo Fold Belt.||||||
17620|Tabita Formation|45118|6|Mentioned|p4|||||||||
17620|Tabita Formation|45148|6|Mentioned|p18|||||||||
17620|Tabita Formation|62787|5|Briefly described|p77, p76 Fig. 1|Early Ordovician|Early Ordovician|Of Mutawintji Group. Conformably underlain by Yandaminta Quartzite.||||||07-FEB-11
17620|Tabita Formation|62793|6|Mentioned|p270, p271|Early Ordovician|Early Ordovician|Near Mount Arrowsmith. Contains diverse assemblage of conodonts from the Oepikodus evae Zone.||||||21-MAR-12
17620|Tabita Formation|62794|6|Mentioned|p298, p299, p337|Early Ordovician|Early Ordovician|Mount Arrowsmith area, western NSW. Correlates with lower Horn Valley Siltstone in Amadeus Basin, NT.||||||
17620|Tabita Formation|62795|6|Mentioned|p348|Early Ordovician|Early Ordovician|Near Mount Arrowsmith, northwestern NSW. Contains similar trilobite fauna to part of Rowena Formation.||||||
17620|Tabita Formation|63489|5|Briefly described|Map legend|Devonian|Silurian|Mudstone, quartzite, minor limestone.||||||
17620|Tabita Formation|63793|6|Mentioned|p24.|||||||||19-JAN-15
17620|Tabita Formation|64015|6|Mentioned|p67|||In western NSW.||||||28-AUG-08
17620|Tabita Formation|64671|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|West of Mount Arrowsmith this unit is faulted against Cambrian formations and western Kara beds. Fossiliferous limestone, shale, red conglomerate.||||||26-NOV-08
17620|Tabita Formation|64687|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Fossiliferous limestone, shale, red conglomerate. Faulted and unconformable against Cambrian formations and western Kara beds.||||||27-NOV-08
17620|Tabita Formation|66623|3|Fully described|p112, pp152-158. |Early Ordovician|Early Ordovician|Correlated with Wheeney Creek Formation, lower part of Rowena Formation, and Horn Valley Siltstone of Amadeus Basin. 82-130 m thick. Carbonates contain nautiloids (mostly removed by collectors), gastropods, bivalves, brachiopods, trilobites and conodonts.||Unit in Pimbilla Tank Group.||Overlies Yandaminta Quartzite. Is overlain by Pingbilly Formation.|Poorly-bedded siliceous grey mudstones, overlain by highly fossiliferous limestones grading to dolostones interbedded with olive to grey-green shales and siltstones.|
17620|Tabita Formation|66917|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|||Unit in Pimbilla Tank Group.||Overlies Yandaminta Quartzite. Is overlain by Pingbilly Formation.|Cleaved silty shale, mudstone, fossiliferous limestone, and basal red pebbly conglomerate.|
17620|Tabita Formation|66929|5|Briefly described|Map legend|Ordovician|Ordovician||||||Fossiliferous limestone, shale, red conglomerate.|
17620|Tabita Formation|66933|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
17620|Tabita Formation|67208|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|||Unit in Pimbilla Tank Group.|||Cleaved silty shale, mudstone, fossiliferous limestone, and basal red pebbly conglomerate.|
17620|Tabita Formation|67322|4|Described|p10, p12; Fig.5|Floian|Floian|Warrris (1967). Estimates of the thickness vary between 82 to 190m. Richly fossiliferous with a varied macrofauna. Age determined from Conodonts (Zhen et al. 2001; Zhen, Percival and Webby 2003; Percival et al. 2003). Occurs in the Mount Arrowsmith region.||Of the Pimbilla Tank Group.||Overlies Yandaminta Quartzite. Overlain conformably by the Pingbilly Formation.|Characterised by interbedded limestone and dolomite.|22-FEB-18
17626|Tablelands Complex|22612|6|Mentioned|423, 425|Tournaisian|Wenlock|Geol province New England Orogen||||||
17626|Tablelands Complex|23859|5|Briefly described|p930|||||||||
17626|Tablelands Complex|24040|5|Briefly described|p469|||Complexly deformed structure consisting largely of Devonian and Carboniferous deep-marine sedimentary rocks, including metabasalt-chert-argillite associations interpreted as part of a Middle-Late Palaeozoic subduction-accretion complex.||||||21-AUG-08
17626|Tablelands Complex|31601|6|Mentioned|p9|||Refers Runnegar (1974)||||||
17626|Tablelands Complex|31694|4|Described|p342|||||||||
17626|Tablelands Complex|35173|6|Mentioned|p101|||||||||
17626|Tablelands Complex|35747|6|Mentioned|Fig.1|||||||||
17626|Tablelands Complex|36961|6|Mentioned|p205|||||||||
17626|Tablelands Complex|37489|6|Mentioned|p261|||||||||
17626|Tablelands Complex|38229|6|Mentioned|p443|||||||||
17626|Tablelands Complex|38687|6|Mentioned|p43|||||||||
17626|Tablelands Complex|39468|5|Briefly described|p193|||||||||
17626|Tablelands Complex|39648|6|Mentioned|p257|||||||||
17626|Tablelands Complex|39673|6|Mentioned|p217|||||||||
17626|Tablelands Complex|40108|6|Mentioned|p183|||||||||
17626|Tablelands Complex|40246|6|Mentioned|p168|||||||||
17626|Tablelands Complex|40883|6|Mentioned|p3|||||||||
17626|Tablelands Complex|42780|4|Described|p411, Fig.1 p410|||||||||
17626|Tablelands Complex|42997|6|Mentioned|p36|||||||||
17626|Tablelands Complex|60904|6|Mentioned|p787 Fig. 13a|||In Southern New England region.||||||
17626|Tablelands Complex|61003|5|Briefly described|p224|Carboniferous|Devonian|Of Korsch (1977). An accretionary wedge of deep-water turbidites. Korsch subdivided this wedge into three tectono-stratigraphic associations: Woolomin, Sandon and Coff Harbour Associations.||||||27-MAY-08
17626|Tablelands Complex|61767|6|Mentioned|p71|||Of Korsch (1977). Also known as Central Complex (Voisey 1959). Geological Province: Southern New England Orogen.||||||25-JAN-06
17626|Tablelands Complex|61768|6|Mentioned|p81|||Probably a structural term. Accretionary wedge and has rocks as old as 530Ma.||||||10-SEP-14
17626|Tablelands Complex|62095|5|Briefly described|p250, p268|||Subduction-accretion complex. Intruded by Hillgrove Suite granitoids at 302Ma. Part of the New England Orogen.||||||21-AUG-08
17626|Tablelands Complex|62357|6|Mentioned|p518, p523 Fig. 6b|||Structural term in this context. Geological Province: New England orogen.||||||
17626|Tablelands Complex|63119|5|Briefly described|p210 Fig.1, p211|||Term used more in the context of a geological province. Includes Woolomin Formation.||||||
17626|Tablelands Complex|63748|6|Mentioned|p4 Fig. 1|||In the Woolomin Province. Geological province: New England Orogen.||||||07-FEB-11
17626|Tablelands Complex|66183|5|Briefly described|p359|Carboniferous|Devonian|deep marine sedimentary rocks||||||
17626|Tablelands Complex|67908|6|Mentioned|p279-280|||Southern New England Orogen.|||||Accretionary wedge metasedimentary rocks.|
17626|Tablelands Complex|69601|6|Mentioned|p404, p406|||Southern New England Orogen. Comprises Woolomin, Sandon and Nambucca Associations.||||||
17626|Tablelands Complex|69793|6|Mentioned|p1110|Carboniferous|Late Devonian|An accretionary complex in the southern New England Orogen. Intruded by 298-288 Ma S-type granitoids.||||||
17626|Tablelands Complex|69930|6|Mentioned|p252|||Southern New England Fold Belt. Fault-bounded crustal blocks.||||Is intruded by Hillgrove Plutonic Suite.|Metasediments: prehnite-pumpellyite to upper amphibolite facies.|
17626|Tablelands Complex|70125|6|Mentioned|p397|||A major sediment source (with the New England granites) for the Terrigal Formation as well as the NSW North Coast.||||||
17626|Tablelands Complex|70939|5|Briefly described|p821, p823|||Runnegar (1974). Southern New England Orogen. A subduction-accretion complex.||||||
17626|Tablelands Complex|71280|5|Briefly described|p401-404, p413-414|||Southern New England Orogen. Accretionary (sedimentary and metasedimentary) rocks have a volcanic arc provenance and are variably metamorphosed.||||||
17626|Tablelands Complex|71628|5|Briefly described|p1: 1-2; p4-5; p7: 2, 31; p8-1; p9-3|||See also p14-1; p18: 1-2. An accretionary trench complex; dominates the southern New England Orogen. Stitched to the Tamworth Belt across the Peel Fault by the Moonbi Monzogranite. Appears as Tableland Complex on p14-1.||||Is intruded by Bundarra and Uralla Supersuites and Greymare Tonalite.|Vertically dipping sequences of basalt, ribbon-bedded tuffaceous chert, tuffaceous siltstone and volcaniclastic sandstone.|
17626|Tablelands Complex|73197|5|Briefly described|p460 Fig.1, p465 Fig.4, p468, p486|Carboniferous|Carboniferous|New England Orogen, accretionary complex. Lithological description is applied to the broader accretionary complex of the Currabubula-Connors Arc including the Tablelands Complex.|||||Accretionary complex of deep-sea trench-fill turbidites and minor limestone, juxtaposed against oceanic basalt, chert and mudstone.|
17626|Tablelands Complex|73202|5|Briefly described|p625-626, p639 Fig.10|Carboniferous|Carboniferous|New England Orogen, southern. Intruded by S-type granites. Accretionary wedge referred to as Anaiwan terrane (Flood and Aitchison, 1988) or Tablelands Complex (Roberts and Engel, 1987).|||||Accretionary complex. Includes abundant isoclinaly folded turbidites, as well as chert and oceanic basalt.|
17642|Taemas Limestone|22857|5|Briefly described|p460 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Murrumbidgee Group. Contains rich fauna: mainly brachiopods and corals. Max. thickness: 970m. Geological Province: Canberra-Yass Shelf. See also p464 App.1 Tb.A1.6.||||||
17642|Taemas Limestone|23208|6|Mentioned|p185||Early Devonian|Contains fossil assemblage of Osteichthyan braincase.||||||
17642|Taemas Limestone|23522|5|Briefly described|p248 Fig 4|Emsian|Emsian|||||||
17642|Taemas Limestone|23898|4|Described|p269|Emsian|Emsian|Of Murrumbidgee Group.||||||
17642|Taemas Limestone|24005|5|Briefly described|p293|Early Devonian|Early Devonian|Of Murrumbidgee Group. Geological Province: Lachlan Fold Belt||||||
17642|Taemas Limestone|24019|6|Mentioned|p362|Emsian|Emsian|||||||
17642|Taemas Limestone|24250|5|Briefly described|p104, p109 Fig.5|Early Devonian|Early Devonian|Parent: Murrumbidgee Group. Underlying Unit: Majurgong Formation||||||
17642|Taemas Limestone|24551|6|Mentioned|p620|||||||||
17642|Taemas Limestone|29989|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17642|Taemas Limestone|30069|6|Mentioned|p7|||||||||
17642|Taemas Limestone|30731|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17642|Taemas Limestone|30814|6|Mentioned|p71|||||||||
17642|Taemas Limestone|31502|5|Briefly described|p94|||See also p95. Devonian corals.||||||18-JUN-08
17642|Taemas Limestone|32483|4|Described|p32|||Lower Devonian. Strat. table 1||||||18-JUN-08
17642|Taemas Limestone|32583|6|Mentioned|p373|||||||||
17642|Taemas Limestone|32585|4|Described|p210|||||||||
17642|Taemas Limestone|32984|6|Mentioned|p344|||||||||
17642|Taemas Limestone|33326|6|Mentioned|p434|||Fauna Emsian B. early Eifelian.||||||
17642|Taemas Limestone|33434|6|Mentioned|p42|||||||||
17642|Taemas Limestone|33606|6|Mentioned|p69|||||||||
17642|Taemas Limestone|33817|6|Mentioned|p127|||Emsian||||||
17642|Taemas Limestone|34692|5|Briefly described|p186|||||||||
17642|Taemas Limestone|35193|6|Mentioned|p20|||||||||
17642|Taemas Limestone|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17642|Taemas Limestone|35386|3|Fully described|p51|||||||||
17642|Taemas Limestone|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
17642|Taemas Limestone|36441|5|Briefly described|map legend|Zlichovian|Pragian|Of Murrumbidgee Group. Massive to thin-bedded fossiliferous limestone and calcareous shale. Underlies Hatchery Creek Conglomerate; overlies Majurgong Formation. BMR map code: Dlt.||||||
17642|Taemas Limestone|37273|6|Mentioned|p245|||||||||
17642|Taemas Limestone|38593|5|Briefly described|p86|||||||||
17642|Taemas Limestone|39881|6|Mentioned|p361|||||||||
17642|Taemas Limestone|40124|6|Mentioned|Fig.1|||||||||
17642|Taemas Limestone|42015|6|Mentioned|p318|||||||||
17642|Taemas Limestone|42032|6|Mentioned|p498|||||||||
17642|Taemas Limestone|42033|6|Mentioned|p656|||||||||
17642|Taemas Limestone|42497|5|Briefly described|Map Legend|Zlichovian|Pragian|||||||
17642|Taemas Limestone|43344|14|Not recorded|p117|||||||||
17642|Taemas Limestone|43430|14|Not recorded|p145|||||||||
17642|Taemas Limestone|43431|14|Not recorded|p1264|||||||||
17642|Taemas Limestone|43525|14|Not recorded|p130,Table p131|||||||||
17642|Taemas Limestone|43529|14|Not recorded|p235|Emsian|Siegenian|||||||
17642|Taemas Limestone|43530|14|Not recorded|p1028,1032||Emsian|||||||
17642|Taemas Limestone|43537|14|Not recorded|p11-16,28|||Near Wee Jasper. Devonian tetracorals. No age given||||||
17642|Taemas Limestone|45147|3|Fully described|M312|||||||||
17642|Taemas Limestone|48971|6|Mentioned|p9|||||||||
17642|Taemas Limestone|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Murrumbidgee Group. Thick-bedded fossiliferous limestone which contains 8 named limestone members - Warroo, Spirifer Yassensis, Receptaculites, Patmore, Crinoidal, Cockatoo Point, Currajong and Bloomfield Limestone Members. .||||||09-SEP-08
17642|Taemas Limestone|64296|5|Briefly described|p85|||Geological province: Lachlan Fold Belt. Has a 'serotinus' conodont fauna.||||||28-AUG-08
17642|Taemas Limestone|65214|6|Mentioned|p272, p274|Devonian|Devonian|NSW, Taemas. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17642|Taemas Limestone|65940|6|Mentioned|p203,207|Emsian|Emsian|Wee Jasper and Good Hope, NSW. Contains Xystriphyllum insigne Hill, ascribed mid-Emsian age.||||||
17642|Taemas Limestone|67823|6|Mentioned|p361|||||Of the Murrumbidgee Group.||||
17642|Taemas Limestone|68298|5|Briefly described|p224|Emsian||Conodonts in upper part of limestone sequence provide age limit of late Emsian.||||Is overlain by Hatchery Creek Conglomerate.||
17642|Taemas Limestone|68592|2|Defined|p982, p984 Fig.162, p985-8, p1003-37|Emsian|Emsian|See also p239, p1197, p1202, p1896-1904. Originally Taemas Series of David (1950); the upper, limestone-dominated part was later named Taemas Stage by Browne (1959). This was subsequently changed to Taemas Limestone by Pedder et al. (1970) and its subunits formalised as Members. It has been referred to as Taemas Formation. Type section described. Thickness estimated from 730 to 970 m. Its abundant, diverse and rich macrofauna is described. Earliest to late Emsian age from conodonts. Potential source of industrial and agricultural lime.||Unit in Murrumbidgee Group.|Includes Crinoidal, Warroo, Patmore, Receptaculites, Cockatoo Point, Bloomfield, Currajong and Spirifer yassensis, Limestone Members.|Conformably overlies Majurgong Formation (diachronously). Is overlain conformably by Wee Jasper Formation. Correlated with Buchan Group.|Blue-grey, thick- to thin-bedded or occasionally massive, richly fossiliferous limestone; also includes minor impure flaggy limestone, calcareous mudstone or shale, and tuffaceous sandstone.|
17642|Taemas Limestone|70192|5|Briefly described|Map Legend|Emsian|Pragian|Dmt. Constituents continued: Receptaculites Limestone Member, Spirifer yassensis Limestone Member and Warroo Limestone Member. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Murrumbidgee Group|Includes Bloomfield Limestone Member, Currajong Limestone Member, Cockatoo Point Limestone Member, Crinoidal Limestone Member, Patmore Limestone Member, see comments for more consituents.|Overlies Majurgong Formation. Is overlain by Wee Jasper Formation (Hatchery Creek Group).|Blue-grey, thick to thin, well bedded or massive, commonly richly fossiliferous limestone; minor impure flaggy limestone, calcareous mudstone or shale and tuffaceous sandstone.|
17642|Taemas Limestone|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|Includes Bloomfield, Currajong, Cockatoo Point, Crinoidal, Patmore Limestone Members, Receptaculites Limestone Member, Spirifer Yassensis Limestone Member and Warroo Limestone Member.||Blue-grey, thick to thin, well bedded or massive, commonly richly fossiliferous limestone; minor impure flaggy limestone, calcareous mudstone or shale and tuffaceous sandstone.|
17642|Taemas Limestone|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Murrumbidgee Group|Includes Bloomfield, Currajong, Cockatoo Point, Crinoidal, Patmore Limestone Members, Receptaculites Limestone Member, Spirifer Yassensis Limestone Member and Warroo Limestone Member.||Blue-grey, thick to thin, well bedded or massive, commonly richly fossiliferous limestone; minor impure flaggy limestone, calcareous mudstone or shale and tuffaceous sandstone.|
17642|Taemas Limestone|71656|5|Briefly described|p12 Fig.2, p32, 33-38, p38, p40|Emsian|Emsian|Rugose corals were described from the undifferentiated Taemas Limestone in the Wee Jasper area. Diachronous base. Younger in Wee Jasper area than Taemas area.||Murrumbidgee Group|Includes Spirifer yassensis, Currajong, Bloomfield, Cockatoo Point, Receptaculites, Patmore, Warroo and Crinoidal Limestone Members|Underlies Wee Jasper Formation. Overlies Majurgong Formation.|Fossiliferous limestone.|
17642|Taemas Limestone|71700|5|Briefly described|CD|||May be partially equivalent to the Lake Bathurst Limestone Member.||Murrumbidgee Group||||
17642|Taemas Limestone|73215|5|Briefly described|p994|||Talmo-Taemas area.||Murrumbidgee Group.||Overlies Majurgong Formation.||
17648|Taggarts Mountain Ignimbrite Member|24603|5|Briefly described|p868|||Of the Currabubula Formation. A relatively coarse-grained, crystal-rich, lithic, variably welded ignimbrite.  Geological Province: Tamworth Belt.||||||
17648|Taggarts Mountain Ignimbrite Member|41800|4|Described|p496|||Reserved as Taggarts Mountain Ignimbrite. See also p493||||||16-MAY-11
17648|Taggarts Mountain Ignimbrite Member|42339|5|Briefly described|Fig.2 P53|||||||||
17648|Taggarts Mountain Ignimbrite Member|42399|5|Briefly described|Fig.2 PB11|||||||||
17648|Taggarts Mountain Ignimbrite Member|43718|6|Mentioned|Table 8.2,p129|||||||||
17648|Taggarts Mountain Ignimbrite Member|65902|4|Described|p197-8, p202-4, p203 Fig.7|Bashkirian|Serpukhovian|Of Currabubula Formation. Occurs also in Willuri Formation, and is thus useful for correlation between Werrie Syncline and Clifton-Carroll Block. Described as hard, red to beige rhyolitic ignimbrite. Dated at 319.3 +/- 2.8 Ma in the Werrie Syncline.||||||09-MAR-12
17648|Taggarts Mountain Ignimbrite Member|68003|5|Briefly described|p134.|Carboniferous|Carboniferous|New England Fold Belt.||Unit in Currabubula Formation.|||Ignimbrite.|
17648|Taggarts Mountain Ignimbrite Member|68005|6|Mentioned|p57, p141.|Late Carboniferous|Late Carboniferous|||Unit in Currabubula Formation.||||
17665|Talbingo Basalt|22857|5|Briefly described|p452 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Boraig Group. Andesitic basalt. Max. thickness: 450m. Geological Province: Bogan Gate Terrace.||||||
17665|Talbingo Basalt|29648|6|Mentioned|p25|||||||||
17665|Talbingo Basalt|29992|6|Mentioned|Map legend|Devonian|Devonian|||||||
17665|Talbingo Basalt|29994|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
17665|Talbingo Basalt|33732|6|Mentioned|p111|||Boraig Group.||||||
17665|Talbingo Basalt|34403|4|Described|p144|||||||||
17665|Talbingo Basalt|34405|6|Mentioned|Fig.3.15|||||||||
17665|Talbingo Basalt|37491|6|Mentioned|Fig.1|||||||||
17665|Talbingo Basalt|40497|6|Mentioned|Map legend|Devonian|Devonian|||||||
17665|Talbingo Basalt|60086|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Boraig Group. Andesitic basalt.||||||
17675|Talbragar Fossil Fish Bed|34157|4|Described|p1|||Fossil fish. See also pp2-4.||||||10-MAR-19
17675|Talbragar Fossil Fish Bed|62578|3|Fully described|p44|Late Jurassic|Jurassic|Of Dulhunty and Eadie (1969). Also ref.to as Fossil Fish Bed, Fish Bed and "Fish Bed Chert". Overlies qtz. sandstones of parent Purlawaugh Fm; can probably be regarded as upper section of unit. Thickness: <60m. Age:151+/-4.27Ma (SHRIMP zircon). unclear if age is 'maximum depositional' or eruption of tuffs.||||||10-MAR-19
17686|Talgarno Schist|37871|4|Described|p7|||||||||
17686|Talgarno Schist|38367|6|Mentioned|Fig.27|||||||||
17686|Talgarno Schist|39858|6|Mentioned|Map legend|Silurian|Ordovician|Silurian - Ordovician||||||
17708|Tallong Conglomerate|22591|4|Described|p 63, Fig 4||Late Carboniferous|Max. thickness 206m.||||||25-JUN-08
17708|Tallong Conglomerate|22857|5|Briefly described|p532 Tb.A1.9, p504 Tb.A1.8|Early Permian|Early Permian|Interpreted as part of Shoalhaven Group by Tye, Fielding and Jones (1996). Formerly placed in Talaterang Group. Cobble conglomerate, minor pebble conglomerate, pebbly sst; rare sltst. Max. thickness: 207m. Geol. Prov: Kanimblan Highlands.||||||
17708|Tallong Conglomerate|22864|6|Mentioned|p262|||||||||
17708|Tallong Conglomerate|22969|5|Briefly described|Fig 2.2||Early Permian|Shoalhaven Group||||||
17708|Tallong Conglomerate|23256|6|Mentioned|p50|||of Sydney Basin||||||
17708|Tallong Conglomerate|24079|5|Briefly described|p430|Late Carboniferous|Late Carboniferous|Geological Province: Sydney Basin.||||||
17708|Tallong Conglomerate|24317|5|Briefly described|p15 Fig.1|Permian|Permian|Geological Province: Sydney Basin.||||||
17708|Tallong Conglomerate|24552|5|Briefly described|p9|Sakmarian|Sakmarian|Of Shoalhaven Group. Geological Province: Southern Sydney Basin.||||||07-FEB-11
17708|Tallong Conglomerate|29750|6|Mentioned|p1|||||||||
17708|Tallong Conglomerate|29752|3|Fully described|p16|||||||||
17708|Tallong Conglomerate|31081|4|Described|p54|||||||||
17708|Tallong Conglomerate|31128|6|Mentioned|p13|||||||||
17708|Tallong Conglomerate|31298|3|Fully described|p7|||||||||
17708|Tallong Conglomerate|32769|6|Mentioned|Fig.1|||||||||
17708|Tallong Conglomerate|32999|6|Mentioned|p44|||||||||
17708|Tallong Conglomerate|34481|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
17708|Tallong Conglomerate|36042|6|Mentioned|Table 1|||||||||
17708|Tallong Conglomerate|37924|4|Described|p488|||||||||
17708|Tallong Conglomerate|39287|6|Mentioned|p20|||See also Fig.2.5||||||
17708|Tallong Conglomerate|39289|6|Mentioned|Fig. 4.1|||||||||
17708|Tallong Conglomerate|39290|4|Described|p83|||Origin p86.||||||25-JUN-08
17708|Tallong Conglomerate|39299|5|Briefly described|p283|||||||||
17708|Tallong Conglomerate|39308|6|Mentioned|p518|||||||||
17708|Tallong Conglomerate|40328|6|Mentioned|p206|||||||||
17708|Tallong Conglomerate|40698|6|Mentioned|p53|||||||||
17708|Tallong Conglomerate|41689|6|Mentioned|Table 1|||||||||
17708|Tallong Conglomerate|42848|5|Briefly described|p532|Early Permian|Early Permian|Basal unit of the Conjola Subgroup (Shoalhaven Group). Overlain by Snapper Point Formation.  Max. thickness: 170m. See also p530 Fig. 1 and p531 Fig. 3.||||||09-MAY-05
17708|Tallong Conglomerate|42974|6|Mentioned|p198|||of Talaterang Group||||||
17708|Tallong Conglomerate|45090|6|Mentioned|p224|||Earliest Sakmarian.||||||
17708|Tallong Conglomerate|50234|5|Briefly described|Map Legend|Permian|Permian|Of the Shoalhaven Group.||||||
17708|Tallong Conglomerate|60281|5|Briefly described|p57|Early Permian|Early Permian|Of Shoalhaven Group.  A thin unit above this conglomerate has been interpreted as a separate unit  (Tye et al 1995) and named Yarrunga Coal Measures. Geol.Prov: Sydney Basin.||||||22-MAR-05
17708|Tallong Conglomerate|60285|5|Briefly described|p182 Fig.2|Sakmarian|Sakmarian|Of the Shoalhaven Group. Basin margin alluvial apron. Geological Province: Sydney Basin.||||||
17708|Tallong Conglomerate|60386|6|Mentioned|p296|Artinskian|Artinskian|Bowen/Sydney Basin. Deltaic - nearshore - shelf.||||||
17708|Tallong Conglomerate|61315|6|Mentioned|p176|||Localised terrestrial sediments at base of basin. Geological Province: Sydney Basin||||||
17708|Tallong Conglomerate|61612|6|Mentioned|p270, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||17-MAR-09
17708|Tallong Conglomerate|62043|6|Mentioned|p438 Fig.2. |Early Permian|Early Permian|Southern Sydney Basin.||||||
17708|Tallong Conglomerate|63461|5|Briefly described|p862 Fig. 1c|||Geological Province: Sydney Basin.||||||10-DEC-07
17708|Tallong Conglomerate|63633|5|Briefly described|Map Legend|Early Permian|Early Permian|Conglomerate, sandstone.||||||
17708|Tallong Conglomerate|63773|5|Briefly described|p1058 Fig. 2|Early Permian|Early Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-APR-09
17708|Tallong Conglomerate|63832|5|Briefly described|p131 fig 2|Cisuralian|Cisuralian|Of Sydney Basin. Sixth (P2) glaciation.||Unit in Shoalhaven Group.||||14-DEC-17
17708|Tallong Conglomerate|64238|5|Briefly described|Map legend|Permian|Permian|Of the Shoalhaven Group. Cobble conglomerate and minor pebble conglomerate; clasts of quartzite, sandstone and black chert.||||||09-SEP-08
17708|Tallong Conglomerate|64631|6|Mentioned|p44 Fig.2.|Artinskian|Sakmarian|Sydney Basin.||Unit in lower Shoalhaven Group.||||
17708|Tallong Conglomerate|64877|5|Briefly described|p295-296|Permian|Permian|SW Sydney Basin. Alluvial deposits.||Shoalhaven Group.||||
17708|Tallong Conglomerate|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Overlain by Snapper Point Formation.||
17708|Tallong Conglomerate|68003|5|Briefly described|p40.|Early Permian|Early Permian|||Unit in Shoalhaven Group.||||
17708|Tallong Conglomerate|68592|2|Defined|p36, p1779-86, p1791|Permian|Permian|These rocks were originally equated with the Megalong Conglomerate (Rose, 1966 and later workers). Defined as a separate unit by Herbert (1972), and assigned to the Talaterang Group by Gostin and Herbert (1973). Remapping by Tye et al. (1996) shows this unit disconformably overlying the Talaterang Group in the Jervis Bay area, and it is reassigned to Shoalhaven Group. Forms a well-defined palaeovalley deposit, 3-4 km wide and c.100 km long. Type area described, where it is 232.6 m thick; only 60-70 m thickness preserved in Goulburn 250 map area. Geochemistry unknown; geophysical properties briefly described. Unfossiliferous. Late Early Permian age from fossils in surrounding units. Equated with Yadboro, Yagers, Burrawang Conglomerates and Badgerys Breccia: all related valley-fill sequences considered to be lateral equivalents of Pebbly Beach and Snapper Point Formations. Source of road materials.||Unit in Shoalhaven Group.||Overlies Talaterang Group disconformably, and Adaminaby, Bendoc, Bindook and Mount Fairy Groups unconformably. Is overlain conformably by Yurrunga Coal Measures or Snapper Point Formation.|A poorly stratified sequence of cream, poorly sorted, clast-supported, cobble to pebble conglomerate with minor medium- to coarse-grained, pebbly quartz-lithic sandstone.|
17708|Tallong Conglomerate|69297|6|Mentioned|p501, p502 fig 5.43|Kungurian|Artinskian|Sydney Basin.||Shoalhaven Group||Overlies and interfingers with the Wasp Head Formation, Yadboro Conglomerate and the Pebbly Beach Formation. Overlain by and interfingers with the Snapper Point Formation.||
17708|Tallong Conglomerate|70192|5|Briefly described|Map Legend|Permian|Permian|Pst. On Goulburn 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Shoalhaven Group||Erosional at base.|Poorly stratified, poorly sorted, clast supported, cobble to pebble conglomerate with minor medium-coarse grained quartz-lithic sandstone. Clasts are subrounded-well rounded and comprise quartzite, sandstone, vein quartz, chert, volcanics.|
17708|Tallong Conglomerate|70542|5|Briefly described|Map Legend|Permian|Permian|||Shoalhaven Group|||Poorly stratified, poorly sorted, clast supported, cobble to pebble conglomerate with minor medium-coarse grained quartz-lithic sandstone. Clasts are subrounded-well rounded and comprise quartzite, sandstone, vein quartz, chert, volcanics.|
17708|Tallong Conglomerate|70661|2|Defined|ix, x, p4, p70, p137, p139|Early Permian|Early Permian|Overlies basement rocks unconformably. Named for Tallong township. Previously mapped as Kamilaroi strata and previously included in Megalong Conglomerate.  Includes rocks of the former Yagers Conglomerate and Burrawang Conglomerate. Previously included in Talaterang Group. Distribution, geomorphology, depositional environment, structure, geophysical characteristics, distinguishing characteristics and fossils discussed.Up to 230m thick (estimated). Type area mentioned.  Lithology described in detail. Age constrained by Permian glossopteris fossils and overlying/underlying units. Used as a source of road materials. Possibly correlates with Wasp Head Formation, correlated with Yadboro Conglomerate. See also p141-p146, p243.||Shoalhaven Group|Badgerys Breccia Member|Disconformably overlain (or interfingers with)  Snapper Point Formation, overlain (probably conformably) by Yarrunga Coal Measures.|Thick, massive to stratified quartzite, sandstone or quartz pebble-cobble conglomerate that is commonly clast supported. Pebbly and cross stratified sandstone, siltstone, sedimentary breccia also present.|
17708|Tallong Conglomerate|71069|6|Mentioned|p135|Permian|Permian|||||Unconformably overlies the Mount Fairy Group.||
17708|Tallong Conglomerate|71303|5|Briefly described|map legend|Cisuralian|Cisuralian|Of Sydney Basin.||Of Shoalhaven Group.|Includes Badgerys Breccia Member.||Poorly sorted, clast to matrix-supported pebble to cobble conglomerate, mostly massive, to well stratified ; pebbly quartz sandstone and quartz sandstone. Clasts: quartzite, metasandstone, quartz, less black chert and igneous lithologies.|
17708|Tallong Conglomerate|71538|6|Mentioned|p54 fig 2|Artinskian|Artinskian|Sydney Basin. Alluvial-braidplain deposit.||Shoalhaven Group||Unconformably overlies the Wasp Head Formation. Disconformably overlain by the Pebbley Beach Formation, Mount Agony Formation and the Snapper Point Formation.||
17708|Tallong Conglomerate|73421|6|Mentioned|p2 Fig.1|||Sydney Basin, southern.||||||
17757|Tamworth Group|721|5|Briefly described|Map legend|Frasnian|Givetian|Includes the Yarrimie Formation.||||||
17757|Tamworth Group|5254|5|Briefly described|p121|Middle Devonian|Early Devonian|Contains three carbonate units; in ascending order, Nemingah Limestone, Sulcor Limestone and Moore Creek Limestone.||||||
17757|Tamworth Group|22520|6|Mentioned|p17|||||||||
17757|Tamworth Group|22571|6|Mentioned|p19|||Overlies Pipeclay Creek Formation||||||
17757|Tamworth Group|22572|6|Mentioned|p108||Devonian|||||||
17757|Tamworth Group|22736|6|Mentioned|p629,30|Frasnian|Emsian|||||||
17757|Tamworth Group|22750|5|Briefly described|Table 1, p 228|Late Devonian|Early Devonian|||||||
17757|Tamworth Group|22768|5|Briefly described|p181,183||Early Devonian|||||||
17757|Tamworth Group|22857|4|Described|p181, p482 App.1 Tb.A1.6|Early Devonian|Early Devonian|Unconformably on Haedon Formation. Volcanic arc clastics dominate. Geological Province: Tamworth Forearc Basin.||||||
17757|Tamworth Group|23050|5|Briefly described|p31|||||||||
17757|Tamworth Group|23185|6|Mentioned|Fig1p156,Fig2p158|Frasnian|Early Devonian|||||||
17757|Tamworth Group|23710|14|Not recorded|p83|||Fauna correlated.||||||
17757|Tamworth Group|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||25-FEB-08
17757|Tamworth Group|24009|5|Briefly described|p368 Fig.1|||||||||
17757|Tamworth Group|24366|5|Briefly described|p5, 17 Fig. 3|Early Carboniferous|Late Devonian|Geological Province: Tamworth Belt.||||||
17757|Tamworth Group|30133|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian age.||||||
17757|Tamworth Group|30135|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian age.||||||
17757|Tamworth Group|30269|6|Mentioned|p401|||||||||
17757|Tamworth Group|30650|4|Described|p311|||||||||
17757|Tamworth Group|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
17757|Tamworth Group|31216|6|Mentioned|Fig. 1|||Geological map||||||
17757|Tamworth Group|31694|6|Mentioned|p341|||||||||
17757|Tamworth Group|31802|6|Mentioned|p134|||Refers Crook (1961). See also unconformity P43.||||||
17757|Tamworth Group|31999|4|Described|p145|||See also P149, Table 1||||||
17757|Tamworth Group|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian'||||||
17757|Tamworth Group|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
17757|Tamworth Group|32672|6|Mentioned|p673|||||||||
17757|Tamworth Group|33002|6|Mentioned|p421|||Tectonic history||||||
17757|Tamworth Group|33101|6|Mentioned|Fig.1|||||||||
17757|Tamworth Group|33220|6|Mentioned|p5|||||||||
17757|Tamworth Group|33393|6|Mentioned|p172|||||||||
17757|Tamworth Group|33873|6|Mentioned|p5|||||||||
17757|Tamworth Group|34093|6|Mentioned|p278|||||||||
17757|Tamworth Group|34397|6|Mentioned|p230|||||||||
17757|Tamworth Group|34400|5|Briefly described|p9|||||||||
17757|Tamworth Group|34545|4|Described|p235|||See also PP236-237. Lower & Middle Devonian||||||
17757|Tamworth Group|34554|4|Described|p234|||Measured section||||||
17757|Tamworth Group|34555|6|Mentioned|p238|||Upper Devonian series above it||||||
17757|Tamworth Group|34589|6|Mentioned|p272|||Metasomatism of limestones||||||
17757|Tamworth Group|34590|6|Mentioned|p300|||||||||
17757|Tamworth Group|34692|6|Mentioned|p188|||||||||
17757|Tamworth Group|35137|6|Mentioned|p85|||||||||
17757|Tamworth Group|35192|6|Mentioned|Fig.1|||||||||
17757|Tamworth Group|35257|6|Mentioned|p70|||||||||
17757|Tamworth Group|35783|5|Briefly described|p3|||||||||
17757|Tamworth Group|35964|6|Mentioned|p497|||||||||
17757|Tamworth Group|36716|6|Mentioned|p143|||||||||
17757|Tamworth Group|36961|6|Mentioned|p208|||See also Fig.3||||||
17757|Tamworth Group|37727|6|Mentioned|p21|||See also P86.||||||
17757|Tamworth Group|38064|5|Briefly described|p40|||||||||
17757|Tamworth Group|38065|6|Mentioned|p45|||||||||
17757|Tamworth Group|38229|5|Briefly described|p445|||||||||
17757|Tamworth Group|38684|6|Mentioned|p17|||Geological Province: New England Fold Belt||||||
17757|Tamworth Group|38686|5|Briefly described|p54|Middle Devonian|Early Devonian|Geological Province: New England Fold Belt.||||||25-FEB-08
17757|Tamworth Group|38802|6|Mentioned|p113|||||||||
17757|Tamworth Group|39214|5|Briefly described|p33|||||||||
17757|Tamworth Group|39331|6|Mentioned|p101|||See also Fig.10-1||||||
17757|Tamworth Group|39468|6|Mentioned|Fig.2|||||||||
17757|Tamworth Group|39528|6|Mentioned|p47|||||||||
17757|Tamworth Group|39673|6|Mentioned|p226|||||||||
17757|Tamworth Group|40053|6|Mentioned|p171|||||||||
17757|Tamworth Group|40246|6|Mentioned|p165|||Mention P166||||||
17757|Tamworth Group|40328|6|Mentioned|p196|||||||||
17757|Tamworth Group|40514|6|Mentioned|p10|||||||||
17757|Tamworth Group|40762|6|Mentioned|p277|||||||||
17757|Tamworth Group|40867|6|Mentioned|p65|||||||||
17757|Tamworth Group|40960|6|Mentioned|p215|||||||||
17757|Tamworth Group|41009|6|Mentioned|Fig.2|||||||||
17757|Tamworth Group|41347|4|Described|Table 3|||Mention P357||||||
17757|Tamworth Group|41348|5|Briefly described|Map legend|Devonian|Devonian|Includes: Yarrimie Formation, Silver Grey Formation, Wogarda Argillite, Northcotte Formation, Drik-Drik Formation, Copes Creek Keratophyre.  Cherty argillite, sandstone, conglomerate, limestone, tuff, keratophyre, basalt, and dolerite.||||||16-DEC-04
17757|Tamworth Group|41990|5|Briefly described|p5|||||||||
17757|Tamworth Group|42229|5|Briefly described|p4|||||||||
17757|Tamworth Group|42376|5|Briefly described|p35|||||||||
17757|Tamworth Group|42554|4|Described|p35|||||||||
17757|Tamworth Group|42629|6|Mentioned|p357|||||||||
17757|Tamworth Group|42849|6|Mentioned|p539|||Overlain by the Baldwin Group.||||||09-MAY-05
17757|Tamworth Group|42866|5|Briefly described|Table 2, P12|||||||||
17757|Tamworth Group|42868|5|Briefly described|p15|||||||||
17757|Tamworth Group|42997|5|Briefly described|p36|||||||||
17757|Tamworth Group|43091|5|Briefly described|Map legend|||||||||
17757|Tamworth Group|43344|14|Not recorded|p10,91,93|Early Devonian|Middle Devonian|||||||
17757|Tamworth Group|43383|14|Not recorded|p14|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43384|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43385|14|Not recorded|p174-5|Early Devonian|Early Devonian|Manilla SH56-9 (311)||||||
17757|Tamworth Group|43397|14|Not recorded|p210,211|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43399|14|Not recorded|p189,190,195,203|||||||||
17757|Tamworth Group|43400|2|Defined|p173,176,177,180,185|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43401|14|Not recorded|p210|||||||||
17757|Tamworth Group|43406|14|Not recorded|p41,42,45,46,49|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43407|14|Not recorded|Map Legend|||(Provisional Edition)Inc.Yarrimie Fm,Silver Gully Fm, Wogarda Arg,Drik-Drik Fm,Copes Ck Kphe||||||
17757|Tamworth Group|43409|14|Not recorded|Map Legend|||||||||
17757|Tamworth Group|43417|4|Described|Map Legend|||||||||
17757|Tamworth Group|43418|14|Not recorded|Map Legend|||||||||
17757|Tamworth Group|43419|14|Not recorded|p112,113|||||||||
17757|Tamworth Group|43427|14|Not recorded|p151|||Includes Moore Creek Limestone||||||
17757|Tamworth Group|43436|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
17757|Tamworth Group|43440|14|Not recorded|p38, fig.4-3||Carboniferous|||||||
17757|Tamworth Group|43447|14|Not recorded|p4,5|||||||||
17757|Tamworth Group|43479|14|Not recorded|p128,151,216|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43491|14|Not recorded|pV/13,14|Middle Devonian|Early Devonian|||||||
17757|Tamworth Group|43530|14|Not recorded|p1025||Eifelian|||||||
17757|Tamworth Group|43537|14|Not recorded|p24|||Ref.to Hill 1940,1941||||||
17757|Tamworth Group|43785|6|Mentioned|p369|||||||||
17757|Tamworth Group|43860|5|Briefly described|1||Late Devonian|||||||
17757|Tamworth Group|43874|14|Not recorded|p204|||(H/56-13) no age given||||||
17757|Tamworth Group|44093|5|Briefly described|p227 App. 1|Middle Devonian|Middle Devonian|Geological Province: New England Fold Belt.||||||
17757|Tamworth Group|44852|14|Not recorded|p73,||Late Devonian|||||||
17757|Tamworth Group|46103|14|Not recorded|p.6||Devonian|Intruded by dolerite body containing Au.Devn.(H56-13).||||||
17757|Tamworth Group|48600|14|Not recorded|Plate 3|||||||||
17757|Tamworth Group|48940|5|Briefly described|p13|||||||||
17757|Tamworth Group|50088|5|Briefly described|p472|Middle Devonian|Middle Devonian|Contains Belodella resima fossils (conodonts) in Attunga area.||||||
17757|Tamworth Group|50094|5|Briefly described|p315, p316 Fig.1, p317 Fig.2|Devonian|Silurian|Geological Province: New England Fold Belt.||||||23-JUN-06
17757|Tamworth Group|50168|4|Described|pp158-160, p162, p165|Devonian|Devonian|Lowermost unit of the Gamilaroi Terrane. Metamorphosed to prehnite-pumpellyite facies. Interpreted as an intra-oceanic island arc sequence. < 5 km thick. Suggested that no evidence exists which requires separation (as in Cawood 1983; Leitch and Cawood 1987; Cawood and Flood 1989) of the lowermost Tamworth Group (as defined by Crook 1961) into a separate sequence. Contains basaltic and doleritic rocks in upper levels.|||Includes the Yarrimie Formation (upper unit).||Comprises a sequence of volcaniclastic sandstones, conglomerates and breccias interbedded with voluminous fine-grained felsic tuffs, extrusive and high-level intrusive meta-andesite, rhyolite and dacite intrusions, flows and breccias.|06-FEB-18
17757|Tamworth Group|61392|5|Briefly described|p176 Tb. 4|Late Devonian|Cambrian|Also known as the Gailaroi terrane.||||||07-FEB-11
17757|Tamworth Group|61762|6|Mentioned|p16, p14 Tab. 1|Early Devonian|Middle Devonian|Consists of volcanics rocks, conglomerate, sandstone, mudstone and limestone. Island arc, intra-oceanic arc rift zones.||||||
17757|Tamworth Group|61765|5|Briefly described|p57, p58, p63|Devonian|Devonian|Consists of volcanics, pyroclastics, epiclastics, subordinate carbonates and radiolarian-rich siltstones. Geol Prov: Tamworth Belt.||||||07-FEB-11
17757|Tamworth Group|62070|5|Briefly described|p37,|Middle Devonian|Middle Devonian||||||Includes limestones.|
17757|Tamworth Group|62095|5|Briefly described|Plate 1|Devonian|Devonian|Geological Province: Werrie Block/Tamworth Belt.||||||29-MAY-06
17757|Tamworth Group|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Devonian|Geological Province: Tamworth Belt.||||||10-DEC-07
17757|Tamworth Group|63774|6|Mentioned|p1077, p1083|Devonian|Devonian|||||||
17757|Tamworth Group|64963|5|Briefly described|p189|Devonian|Devonian|Geological province: southern New England Fold Belt.||||||22-APR-09
17757|Tamworth Group|65398|6|Mentioned|p4 Fig.2, p6 Fig.3, p9, Fig 2|Early Carboniferous|Late Devonian|||||||
17757|Tamworth Group|66197|5|Briefly described|p642|Late Devonian||New England Fold Belt. Island arc accreted.||||||14-MAR-12
17757|Tamworth Group|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian||||Includes Yarrimie and Glencairn Formations.|Is overlain by Parry Group.||
17757|Tamworth Group|68005|5|Briefly described|p20, p47, p50, pp52-53, p169 Plan 1|Middle Devonian|Early Devonian|Tamworth Belt, New England Fold Belt. Deposited in a submarine to emergent island arc setting. Geophysical cover is described as inadequate at time of publication.|||Includes Copes Creek Andesite; Bog Hole, Drik-Drik, Northcotte, Silver Gully and Yarrimie Formations; Wogarda Argillite and Folly Spillite.|Is overlain by Parry Group.|A series of intermediate volcanics and volcaniclastics, red breccias and limestones.|
17757|Tamworth Group|68006|5|Briefly described|p20 Fig.3-A, pp26-27, p114.|Middle Devonian|Early Devonian|Tamworth Belt, New England Fold Belt. Hosts the Attunga limestone deposits at Jacksons and Sulcor Quarries.|||Includes Crawney, Moore Creek, Neminga, Sulcor, Timor and Loomberah Limestone Members.|||
17757|Tamworth Group|70777|6|Mentioned|p8|Devonian|Devonian|Rouchel Block, New England Orogen.||||||
17757|Tamworth Group|70907|6|Mentioned|p774 Fig.2|||||||||
17757|Tamworth Group|71628|5|Briefly described|p6-18; p7-31|Devonian|Devonian|||||Is intruded by Gummi Plain Granodiorite and Moonbi Monzogranite.||
17776|Tangaratta Formation|721|5|Briefly described|Map legend|Tournaisian|Tournaisian|Of the Tulcumba Formation (Parry Group). Thinly bedded, fine-grained frldsarenite, siltstone, mudstone, rare limestone.||||||
17776|Tangaratta Formation|22857|5|Briefly described|p496 App.1 Tb.A1.7|Tournaisian|Tournaisian|Of the Parry Group. Thinly-bedded, fine-grained felsarenite, siltstone, mudstone, rare limestone. Max. thickness: 900m. Geological Province: Tamworth Forearc Basin.||||||24-MAR-06
17776|Tangaratta Formation|23185|6|Mentioned|Fig1p156|Carboniferous|Carboniferous|||||||
17776|Tangaratta Formation|23790|5|Briefly described|p11 Fig. 2|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt||||||
17776|Tangaratta Formation|24366|5|Briefly described|p5, 17 Fig. 3|Early Carboniferous|Early Carboniferous|Geological Province: Tamworth Belt.||||||
17776|Tangaratta Formation|30135|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17776|Tangaratta Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
17776|Tangaratta Formation|31802|6|Mentioned|p134|||Latest Dev. - Early Carb. Equiv. Leeton Fm.||||||
17776|Tangaratta Formation|31999|6|Mentioned|p151|||Table 1||||||
17776|Tangaratta Formation|32482|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
17776|Tangaratta Formation|32671|6|Mentioned|Map legend|Carboniferous|Devonian|Devonian-Carb.||||||
17776|Tangaratta Formation|32865|6|Mentioned|p481|||Dev.||||||
17776|Tangaratta Formation|34080|6|Mentioned|p248|||||||||
17776|Tangaratta Formation|34555|6|Mentioned|p240|||||||||
17776|Tangaratta Formation|36961|6|Mentioned|p208|||See also Fig.3.||||||
17776|Tangaratta Formation|37987|6|Mentioned|p223|||||||||
17776|Tangaratta Formation|38222|6|Mentioned|p358|||||||||
17776|Tangaratta Formation|39331|6|Mentioned|Table 10-1|||||||||
17776|Tangaratta Formation|39468|6|Mentioned|p196|||||||||
17776|Tangaratta Formation|40245|6|Mentioned|Table 2|||||||||
17776|Tangaratta Formation|40246|6|Mentioned|Table 1|||||||||
17776|Tangaratta Formation|41009|6|Mentioned|Fig.2|||||||||
17776|Tangaratta Formation|41238|6|Mentioned|p82|||||||||
17776|Tangaratta Formation|41348|5|Briefly described|Map legend|Carboniferous|Devonian|Of the Parry Group.||||||16-DEC-04
17776|Tangaratta Formation|42547|4|Described|p20|Carboniferous|Devonian|Werrie Syncline. Age: late Devonian to early Carboniferous||||||
17776|Tangaratta Formation|43091|5|Briefly described|Map legend|||of Parry Group||||||
17776|Tangaratta Formation|43407|14|Not recorded|Map Legend||Early Carboniferous|(Provisional Edition)||||||
17776|Tangaratta Formation|43409|14|Not recorded|Map Legend|||||||||
17776|Tangaratta Formation|43417|6|Mentioned|Map Legend|||Correlated with Glenlawn Formation.||||||
17776|Tangaratta Formation|43418|14|Not recorded|Map Legend|||||||||
17776|Tangaratta Formation|43434|14|Not recorded|Map Legend|||||||||
17776|Tangaratta Formation|43435|14|Not recorded|Map Legend|||||||||
17776|Tangaratta Formation|43479|14|Not recorded|p136,151m,157||Late Devonian|||||||
17776|Tangaratta Formation|47056|6|Mentioned|Fig.2 P523|||||||||
17776|Tangaratta Formation|68003|5|Briefly described|p32 Fig.3-h, p138. |Tournaisian|Tournaisian|Tamworth Belt (North), New England Fold Belt.||Unit in Parry Group.||Overlies Mandowa Mudstone. Is overlain by Tulcumba Sandstone.|Thinly bedded, fine-grained feldsarenite, siltstone, mudstone and rare limestone.|
17776|Tangaratta Formation|68005|4|Described|p49 Fig.3-M, p54, pp147-148, p170.|Tournaisian|Tournaisian|Tamworth Belt. Broadly equivalent to Luton Formation north of Barraba.||Unit in Parry Group.|Includes Scrub Mountain, Dancing Dicks, Sutcliff and Garoo Conglomerates; Glenlawn and Martindale Mudstones; Duxford Member; Pyramid Hill Arenite and Gowrie Sandstone.|Conformably overlies Mandowa Mudstone. Is overlain by Tulcumba Sandstone.|Mudstone and fine sandstone; minor thin, laterally continuous sandstone and conglomerate members; rare limestone.|
17776|Tangaratta Formation|70907|6|Mentioned|p774 Fig.2|||||||||
17776|Tangaratta Formation|71628|6|Mentioned|p18-20|||||Parry Group.||||
17781|Tangy Dangy Coal Member|31549|6|Mentioned|p159|||Stratigraphic succession||||||
17781|Tangy Dangy Coal Member|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
17781|Tangy Dangy Coal Member|34270|6|Mentioned|p254|||Small coal unit in Tuggerah Region||||||
17804|Tanyarto Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
17804|Tanyarto Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Eurowie Subgroup (Torrowangee Group). Green grey siltstone, occasional sandy limestone lenses. Age: ~700Ma. Max. thickness: 950m. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
17804|Tanyarto Formation|30261|4|Described|Table 1|||Marinoan age||||||
17804|Tanyarto Formation|34812|3|Fully described|p83|||||||||
17804|Tanyarto Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
17804|Tanyarto Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
17804|Tanyarto Formation|36733|6|Mentioned|Table 5|||||||||
17804|Tanyarto Formation|39214|6|Mentioned|Table 1|||||||||
17804|Tanyarto Formation|41405|5|Briefly described|p204|||||||||
17804|Tanyarto Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
17804|Tanyarto Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Overlies Wammerra Formation. Is overlain by Yowahro Formation.|Green-grey siltstone with minor limestone and minor ripples. A separately mapped un-named subunit also contains thin to massive, variably continuous, clean to gritty carbonate beds.|08-SEP-15
17828|Tappitallee Mountain Tuff Member|36220|5|Briefly described|p40|||See also P38 & Table 33.||||||
17828|Tappitallee Mountain Tuff Member|38690|6|Mentioned|p294|||||||||
17834|Tarana Granite|22503|5|Briefly described|Fig.7 p650, p651||Carboniferous|||||||
17834|Tarana Granite|23214|3|Fully described|p251|Late Carboniferous|Carboniferous|Intrudes Bells Creek Volcanics. Previously included as part of the Bathurst Granite.||||||
17834|Tarana Granite|42712|4|Described|8,16; Table 1 p 13.|Carboniferous|Early Carboniferous|||||||
17834|Tarana Granite|42726|5|Briefly described|map legend|Carboniferous|Carboniferous|21.  Of the Bathurst Suite (Bathurst Supersuite).||||||07-FEB-05
17834|Tarana Granite|43639|5|Briefly described|Map Legend||Carboniferous|||||||
17834|Tarana Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
17834|Tarana Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Of Bathurst Batholith. Does not appear on map face.||||||04-MAR-09
17834|Tarana Granite|64826|6|Mentioned|p1041|Carboniferous|Carboniferous|||||||
17834|Tarana Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
17862|Tarpaulin Creek Ashstone Member|34405|6|Mentioned|p119|||Marker bed||||||
17862|Tarpaulin Creek Ashstone Member|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Of Uriarra Volcanics. Extrusive. ?I-type. Fine-grained bedded ashstone. Overlies Walker Volcanics. BMR map code: Svt.||||||
17862|Tarpaulin Creek Ashstone Member|37727|6|Mentioned|p91|||||||||
17862|Tarpaulin Creek Ashstone Member|40328|5|Briefly described|p133|||||||||
17862|Tarpaulin Creek Ashstone Member|43159|5|Briefly described|Fig.2 p4,P6,P9.|||Of Uriarra Volcanics||||||
17862|Tarpaulin Creek Ashstone Member|45147|3|Fully described|M162|||Refers Malcolm(1954)||||||
17909|Taylors Hill Formation|22529|5|Briefly described|4 fig 2|Emsian|Pragian|Parent Queens Pinch Group. Overlying unit Warratra Mudstone, underlying unit Mullamuddy Formation||||||
17909|Taylors Hill Formation|22590|6|Mentioned|Fig3 P754|Emsian|Pragian|Actually spelt Taylors Hill Fm.||||||
17909|Taylors Hill Formation|22857|4|Described|p476 App.1 Tb.A1.6|Pragian|Pragian|Of the Queens Pinch Group. Mudstone, arenite, basaltic conglomerate, limestone. Max. thickness: 240m. Geological Province: Capertee Rise.||||||
17909|Taylors Hill Formation|23043|5|Briefly described|Map Legend|Emsian|Pragian|of Queens Pinch Group.||||||
17909|Taylors Hill Formation|23170|2|Defined|p147|Pragian|Pragian|of Queens Pinch Group.||||||
17909|Taylors Hill Formation|23522|5|Briefly described|p248 Fig 4|Emsian|Lochkovian|||||||
17909|Taylors Hill Formation|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
17909|Taylors Hill Formation|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
17909|Taylors Hill Formation|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
17909|Taylors Hill Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
17909|Taylors Hill Formation|33326|6|Mentioned|p433|||Fauna.||||||
17909|Taylors Hill Formation|42033|6|Mentioned|p654|||||||||
17909|Taylors Hill Formation|43188|4|Described|p215,Table 4 p212|Pragian|Pragian|Age middle to late Pragian.||||||
17909|Taylors Hill Formation|43476|14|Not recorded|Map Legend||Early Devonian|(Provisional Edition)||||||
17909|Taylors Hill Formation|65214|6|Mentioned|p274|Devonian|Devonian|NSW, Mudgee. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
17909|Taylors Hill Formation|68297|5|Briefly described|p191|Pragian|Pragian|Mudgee area. Includes Pragian vertebrate fossil fauna.||||||
17909|Taylors Hill Formation|71924|6|Mentioned|p1|||Queens Pinch, near Mudgee. Fauna compared to Cunningham Formation fauna.||||Correlated with basal Cunningham Formation, Mullamuddy Formation.||
17909|Taylors Hill Formation|73299|6|Mentioned|p1096 Fig.3, p1097 Fig.4|Early Devonian|Early Devonian|||Queens Pinch Group||Overlies the Mullamuddy Formation.||
17916|Teamsters Creek Subgroup|22772|4|Described|p66-67,Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
17916|Teamsters Creek Subgroup|22857|5|Briefly described|p66, Tb. 13.1 (insert p70-71)|Marinoan|Marinoan|Overlain by Torrowangee Group. Geological Province: Adelaide Fold Belt. See also p400 App. 1 Tb.A1.3.||||||11-SEP-07
17916|Teamsters Creek Subgroup|34814|6|Mentioned|Table 1|||||||||
17916|Teamsters Creek Subgroup|36733|6|Mentioned|Table 5|||||||||
17916|Teamsters Creek Subgroup|38157|6|Mentioned|p265|||||||||
17916|Teamsters Creek Subgroup|41405|5|Briefly described|p204|||||||||
17916|Teamsters Creek Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Glacigenic, pebbly siltstone and sandstone, local diamictite and conglomerate. South Australian equivalent is Yerelina Subgroup.||||||11-SEP-07
17916|Teamsters Creek Subgroup|66623|6|Mentioned|p13.|||||Unit in Torrowangee Group.||Is overlain by Farnell Group.||
17916|Teamsters Creek Subgroup|68277|6|Mentioned|p96|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
17916|Teamsters Creek Subgroup|70000|5|Briefly described|p34, p39.|Neoproterozoic|Neoproterozoic|Records the fluvial and shallow marine reworking and mass flow deposition of glacigenic detritus.||Unit in Torrowangee Group.|Includes Alberta and Nunduro Conglomerates; Gairdners Creek Quartzite; Dering Siltstone.|Unconformably overlies Euriowie Subgroup.|Diamictite (with dropstones), conglomerate and lesser quartzite and sandstone.|
17916|Teamsters Creek Subgroup|70015|5|Briefly described|Map legend|Ediacaran|Cryogenian|Mineral deposits (if any) are shown.||Unit in Torrowangee Group.|Includes Alberta and Nunduro Conglomerates; Gairdners Creek Quartzite; Dering Siltstone.|Overlies Euriowie Subgroup.|Conglomerate and laminated siltstone-sandstone sequences.|
17938|Temi Formation|22857|5|Briefly described|p506 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Polymictic conglomerate, lithic arenite, shale, coal. Max. thickness: 150m. Geological Province: Tamworth Forearc Basin.||||||
17938|Temi Formation|23102|5|Briefly described|p561|||||||||
17938|Temi Formation|24603|5|Briefly described|p869 Figs. 4a, 4b|Permian|Permian|Unconformably overlies the Currabubula Formation. See also p886 Fig. 11.  Geological Province: Tamworth Belt.||||||
17938|Temi Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
17938|Temi Formation|31855|6|Mentioned|p14|||Stratigraphic table||||||
17938|Temi Formation|31883|6|Mentioned|p593|||See also Table 1||||||
17938|Temi Formation|32482|6|Mentioned|Map legend|Permian|Carboniferous|Perm.-Carb.||||||
17938|Temi Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
17938|Temi Formation|32944|6|Mentioned|p700|||See also P710. L.Permian||||||
17938|Temi Formation|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
17938|Temi Formation|34292|6|Mentioned|Table 1|||Permian||||||
17938|Temi Formation|36961|6|Mentioned|p210|||See also Fig.3.||||||
17938|Temi Formation|38818|5|Briefly described|p167|Permian|Permian|Geological Province: New England Fold Belt. Overlying Unit: Werrie Basalt||||||
17938|Temi Formation|38820|6|Mentioned|p180|||Geological Province: New England Fold Belt||||||
17938|Temi Formation|38837|6|Mentioned|p233|||||||||
17938|Temi Formation|39214|4|Described|p35|||||||||
17938|Temi Formation|39288|6|Mentioned|Fig. 3.3|||||||||
17938|Temi Formation|39331|6|Mentioned|Table 10-1|||||||||
17938|Temi Formation|39468|6|Mentioned|Fig.2|||||||||
17938|Temi Formation|39572|6|Mentioned|p134|||See also P141||||||
17938|Temi Formation|40166|6|Mentioned|Table 1|||||||||
17938|Temi Formation|41264|6|Mentioned|p251|||||||||
17938|Temi Formation|41347|4|Described|Table 3|||Mention P357||||||
17938|Temi Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
17938|Temi Formation|41461|6|Mentioned|p13|||||||||
17938|Temi Formation|41800|6|Mentioned|Fig.4|||||||||
17938|Temi Formation|42339|5|Briefly described|Fig.2 P53|||||||||
17938|Temi Formation|42399|5|Briefly described|Fig.2 PB11|||||||||
17938|Temi Formation|43407|14|Not recorded|Map Legend|Permian|Carboniferous|(Provisional Edition)||||||
17938|Temi Formation|43417|4|Described|Map Legend||Permian|||||||
17938|Temi Formation|44093|5|Briefly described|p227 App. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
17938|Temi Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
17938|Temi Formation|47056|6|Mentioned|Fig.2 P523|||||||||
17938|Temi Formation|61201|4|Described|p2, 5 Table 1, 6-7|Early Permian|Early Permian|Overlies the Currabubula Formation. Max. Thickness: 220m. Polymictic conglomerate, lithic sandstone, oil shale, coal, mudstone. Overlain by Werrie Basalt. Geological Province: Werrie Basin.||||||14-JUL-05
17938|Temi Formation|61772|6|Mentioned|p129||Early Permian|Contains distal tuffs.||||||24-SEP-08
17938|Temi Formation|61776|5|Briefly described|p196|Early Permian|Early Permian|Geological Province: Werrie Basin. Lithic conglomerate, sandstone, siltstone and coal.||||||
17938|Temi Formation|61801|5|Briefly described|p403, p404|Carboniferous|Carboniferous|Dominantly epiclastic. Coal, conglomerate, sandstone. Overlain by the Werrie Basalt. Overlies the Currabubula Formation.||||||
17938|Temi Formation|62095|5|Briefly described|p250|Early Permian|Early Permian|Disconformably overlies top member of the Woodton Formation, namely the Willawarra Rhyodacite Member. Overlies Kewell Creek Volcanic member also.  Age is Sakmarian. See also Plate 1.||||||31-JAN-08
17938|Temi Formation|63832|6|Mentioned|p131 fig 2|Sakmarian|Sakmarian|Werrie Syncline, Southern New England Fold Belt. Sixth (P2) glaciation.||||||
17938|Temi Formation|64631|5|Briefly described|p44 Fig.2.|Sakmarian|Sakmarian|Southern New England Fold Belt, Werrie Syncline. Age control from underlying Woodton Formation.||||Overlies Woodton Formation. Is overlain by Werrie Basalt.||
17938|Temi Formation|65114|5|Briefly described|p395|||Stratigraphically above the Brogans Rhyodacite Member of the Woodton Formation||||||14-MAR-10
17938|Temi Formation|68003|5|Briefly described|p38 Fig.3-j, p39, p40, p130.|Early Permian|Early Permian|Werrie Basin, Brigalow Belt South Bioregion. Contains coal at a lower stratigraphic level than known in the Gunnedah Basin. Fluvial sediments.||||Is overlain by Werrie Basalt.|Tuffaceous lithic sandstone and conglomerate, shale, carbonaceous shale.|
17938|Temi Formation|68004|5|Briefly described|pp65-66, p153.|Early Permian|Early Permian|Basal rocks of the Werrie Basin. c.200 m thick. Conglomerates are very similar to underlying Upper Carboniferous conglomerates. No economic coal seams.||||Overlies Currabubula Formation. Is overlain by Werrie Basalt.|Bottom 150 m is of conglomerates comprising predominantly felsic volcanic clasts; overlain by 50 m of fluviatile sandstones and coaly horizons (NW of New England Highway) or torbanite (to the SE).|
17938|Temi Formation|68006|6|Mentioned|p92, p95.|||Basal unit in Werrie Basin.||||||
17938|Temi Formation|69793|6|Mentioned|p1121 Fig.12|Sakmarian|Sakmarian|Werrie Block, Tamworth Belt.||||||
17938|Temi Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Early Permian fluvial sequences: conglomerate, tuffaceous sandstone, shale, carbonaceous shale and coal.||||||
17938|Temi Formation|70728|5|Briefly described|p265|Sakmarian|Sakmarian|Geological province: North Tamworth terrane, New England Orogen.||||Overlain by Werrie Basalt. Underlain by Woodton Formation.||
17938|Temi Formation|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
17938|Temi Formation|70791|5|Briefly described|p277|Cisuralian||Werrie Basin (north).||||||
17955|Tenningerie sand|39512|6|Mentioned|p2|||||||||
17964|Tent Hill Volcanics|22490|6|Mentioned|4|Late Permian|Late Permian|Parent  Wandsworth Volcanic Group. Geol province New England Fold Belt||||||
17964|Tent Hill Volcanics|22857|5|Briefly described|p536 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Volcanic Group. Porphyritic volcanics including interbedded ignimbrite and rhyodacite to pyroxene andesite lavas. Max. thickness: ~400m. Geological Province: New England Fold Belt.||||||
17964|Tent Hill Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of Wandsworth Volcanic Group.  Dominanly porphyritic volcanic rocks, incl. interbedded ignimbrite and lava, commonly dark blue-green in colour.  Main phenocrysts are andesine, hornblende and biotite.  Volcaniclastic rocks range from rhyolitic to andesitic||||||20-DEC-04
17964|Tent Hill Volcanics|23812|4|Described|p25, p27 Tb.3|Late Permian|Early Permian|Of Wandsworth Group. Maximum thickness: 400m.||||||
17964|Tent Hill Volcanics|23859|5|Briefly described|p929|Late Permian|Late Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
17964|Tent Hill Volcanics|38824|5|Briefly described|p212|||||||||
17964|Tent Hill Volcanics|40507|6|Mentioned|p75|||||||||
17964|Tent Hill Volcanics|40509|6|Mentioned|p47|||||||||
17964|Tent Hill Volcanics|42180|6|Mentioned|p245|||||||||
17964|Tent Hill Volcanics|42378|4|Described|Table 1 P6, Fig.1 P5|||Supercedes "Tent Hill Porphyrite" and "Tent Hill Volcanic Formation".||||||
17964|Tent Hill Volcanics|43017|6|Mentioned|p378|||||||||
17964|Tent Hill Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
17964|Tent Hill Volcanics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
17964|Tent Hill Volcanics|62534|4|Described|p8, p11 (legend), p12|Early Triassic|Late Permian|Of the Wandsworth Volcanic Group. Comprised predominantly of interbedded porphyritic rhyolitic to andesitic ignimbrite and lava which occur as an envelope around Dundee Rhyodacite, and overlie Emmaville Volcanics. Magnetics/radiometrics discussed.||||||07-FEB-11
17964|Tent Hill Volcanics|71628|5|Briefly described|p19-110|||||Wandsworth Volcanic Group.||Is intruded by Mole Leucogranite.||
17969|Teralba Conglomerate Member|23055|6|Mentioned|p26|||||||||
17969|Teralba Conglomerate Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Moon Island Beach Formation (Newcastle Coal Measures). Geological Province: Sydney Basin||||||
17969|Teralba Conglomerate Member|29922|6|Mentioned|p49|||||||||
17969|Teralba Conglomerate Member|29926|6|Mentioned|Fig.3|||||||||
17969|Teralba Conglomerate Member|31549|6|Mentioned|p159|||Stratigraphic succession||||||
17969|Teralba Conglomerate Member|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
17969|Teralba Conglomerate Member|33867|6|Mentioned|p11|||||||||
17969|Teralba Conglomerate Member|34270|6|Mentioned|p254|||||||||
17969|Teralba Conglomerate Member|34351|6|Mentioned|p348|||Fig.5.13||||||
17969|Teralba Conglomerate Member|37083|6|Mentioned|p164|||||||||
17969|Teralba Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
17969|Teralba Conglomerate Member|39308|5|Briefly described|p459|||||||||
17969|Teralba Conglomerate Member|39609|6|Mentioned|Table 1|||||||||
17969|Teralba Conglomerate Member|39666|6|Mentioned|Table 20|||||||||
17969|Teralba Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
17969|Teralba Conglomerate Member|43447|14|Not recorded|diag.p26,36|||Moon Island Beach Sub-Group||||||
17969|Teralba Conglomerate Member|43448|14|Not recorded|p226||Permian|Unit of Cardiff Subgroup?(Newcastle Coal Measures)||||||
17969|Teralba Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Catherine Hill Bay Formation.||||
17973|Termeil Essexite|29992|6|Mentioned|Map legend|Permian|Permian|||||||
17973|Termeil Essexite|29994|6|Mentioned|Map legend|Permian|Permian|||||||
17973|Termeil Essexite|32126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
17973|Termeil Essexite|32129|6|Mentioned|p7|||Refers Rose (1966)||||||
17973|Termeil Essexite|32671|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
17973|Termeil Essexite|36954|6|Mentioned|p114|||||||||
17973|Termeil Essexite|43465|14|Not recorded|Map Legend||Mesozoic|||||||
17973|Termeil Essexite|43715|6|Mentioned|p28|||||||||
17973|Termeil Essexite|43981|14|Not recorded|None recorded|||||||||
17973|Termeil Essexite|67663|6|Mentioned|p518, p519 Fig.1|||Southern Sydney Basin.||||||
17982|Terni Granite|22857|6|Mentioned|p231|Late Carboniferous|Early Carboniferous|||||||
17982|Terni Granite|22863|6|Mentioned|p231|||||||||
17982|Terni Granite|36516|6|Mentioned|Fig.2|||||||||
17982|Terni Granite|42726|5|Briefly described|map legend|Carboniferous||||||||
17991|Terrace Creek Rhyolite|40622|6|Mentioned|p29|||||||||
17999|Terrica beds|42559|4|Described|p9|||Stated to be informal name. Variation on Terrica Beds.||||||
17999|Terrica beds|43008|5|Briefly described|map legend|||||||||
17999|Terrica beds|43745|6|Mentioned|p16||Permian|||||||
17999|Terrica beds|60937|5|Briefly described|p425 Fig. 3, p437|Early Permian|Early Permian|Geological Province: Terrica Inlier (Texas Block). See also p426 and p434.||||||14-APR-08
17999|Terrica beds|63732|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic arenite, mudstone, siltstone; rare vitric tuff and conglomerate; locally fossiliferous.||||||
17999|Terrica beds|63733|5|Briefly described|Map legend|Early Permian|Early Permian|Lithic arenite, mudstone, siltstone; rare vitric tuff and conglomerate; locally fossiliferous.||||||29-APR-13
17999|Terrica beds|63748|5|Briefly described|p16, p18, p68|Permian|Permian|Of Lucas (1959, 1960c).Unconformable on and faulted against Texas beds. Interbedded med. to thick-banded, poorly sorted lithic arenite, mudstone and siltstone, with some vitric tuff and conglomerate. Permian fossils contained. Detailed lithology provided.||||||02-MAY-13
17999|Terrica beds|65107|6|Mentioned|p287|Sakmarian|Asselian|Permian inlier in the Texas beds.||||||
17999|Terrica beds|67908|6|Mentioned|p283|Permian.|Permian.|Texas Orocline. Early Permian.|||||Interbedded conglomerate, arenite, mudstone and siltstone layers.|
17999|Terrica beds|68553|6|Mentioned|Map legend; schematic diagram.|Permian|Permian|Silver Spur Subprovince. This unit, with the Alum Rock Conglomerate, and the Bondonga, Pikedale and Silver Spur beds, are all mapped under the symbol, Par.||||||
17999|Terrica beds|68679|5|Briefly described|p452, p455|Permian|Permian|Lucas (1959, 1960); Olgers and Flood (1970). Silver Spur Subprovince, Woolomin Province. 45km WNW of Stanthorpe. Coarser material derived from Texas beds. Contains a fauna similar to, but slightly younger than, Alum Rock Conglomerate.|||||Interbedded, medium- to thick-bedded, poorly sorted lithic sandstone, mudstone and siltstone with rare vitric tuff and conglomerate; sandstone is locally pebbly. Finer-grained material contains abundant plant material.|
17999|Terrica beds|68901|6|Mentioned|p8 Fig. iii|Permian|Permian|||||||27-SEP-18
17999|Terrica beds|70373|4|Described|p789-p792,  p795, p797 Tb 1, p798-p804|Early Permian|Early Permian|Fossils correlated with those in Alum Rock beds, suggesting Cisuralian age. Dating of detrital zircons indicates provenance from Carboniferous materials, and deposition in the Early Permian. Contain clasts of chert, sandstone, volcanic rocks thought to be derived from Texas beds. Other date from this unit: 297.8+/-4.3Ma. All LA-ICP-MS on zircon.  280-320m thick.|283.1+/-5.2 Ma, (LA-ICP-MS on zircons)|||Unconformably overlies and/or faulted against Texas beds. Correlated with Bondonga, Silver Spur, Pikedale and Alum Rock beds.|Sandstone, pebbly sandstone, conglomerate, diamictite and mudstone with clasts of chert, sandstone and volcanics. Crinoids and small spiriferid impressions present.|28-SEP-16
17999|Terrica beds|73487|6|Mentioned|p563, p574 Fig.8, p586|Sakmarian|Sakmarian|Upper Sakmarian in age (Archbold, 2001).||||||
18012|Texas beds|22601|6|Mentioned|405|Carboniferous|Carboniferous|||||||
18012|Texas beds|22857|5|Briefly described|p220, p502 App.1 Tb.A1.7|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||
18012|Texas beds|22859|5|Briefly described|p220|||||||||
18012|Texas beds|23050|4|Described|p14 Table 1|Visean|Visean|Age: Early Carboniferous (Visean) age indicated by fossils.||||||
18012|Texas beds|23051|5|Briefly described|Map Legend|Early Carboniferous|Early Carboniferous|||||||
18012|Texas beds|23811|5|Briefly described|Map Legend|Westphalian|Tournaisian|Low grade regionally metamorphosed, variably deformed lithic wacke, conglomerate, siltstone, mudstone, chert, basalt and rare tuff.||||||20-DEC-04
18012|Texas beds|23812|5|Briefly described|p15|Early Carboniferous|Early Carboniferous|Intruded by Mole Granite.||||||
18012|Texas beds|24480|5|Briefly described|p6|Carboniferous|Carboniferous|||||||
18012|Texas beds|35020|6|Mentioned|p345|Early Carboniferous|Early Carboniferous|||||||
18012|Texas beds|36961|6|Mentioned|p216|||||||||
18012|Texas beds|38222|6|Mentioned|Fig.2|||||||||
18012|Texas beds|39071|6|Mentioned|p339|||||||||
18012|Texas beds|39413|6|Mentioned|p55|||||||||
18012|Texas beds|39943|6|Mentioned|Table 11A|||||||||
18012|Texas beds|39987|6|Mentioned|p65|||||||||
18012|Texas beds|40435|5|Briefly described|p47|||||||||
18012|Texas beds|40514|5|Briefly described|p3|||||||||
18012|Texas beds|40623|5|Briefly described|p107|||||||||
18012|Texas beds|40787|6|Mentioned|p346|||||||||
18012|Texas beds|40960|6|Mentioned|p216|||||||||
18012|Texas beds|42297|5|Briefly described|p3|Carboniferous||||||||
18012|Texas beds|42554|5|Briefly described|p47|||||||||
18012|Texas beds|42559|4|Described|p7|||||||||
18012|Texas beds|42729|5|Briefly described|p12|||||||||
18012|Texas beds|42748|6|Mentioned|Fig.3 P9|Carboniferous||||||||
18012|Texas beds|42901|5|Briefly described|Fig.12 P412|||||||||
18012|Texas beds|43008|5|Briefly described|map legend|||||||||
18012|Texas beds|43009|5|Briefly described|Map Legend|||||||||
18012|Texas beds|43582|6|Mentioned|p4|||||||||
18012|Texas beds|43745|6|Mentioned|Fig.4,p13|||||||||
18012|Texas beds|60079|5|Briefly described|Map Legend|Permian|Carboniferous|Of the Hillgrove Suite.||||||
18012|Texas beds|60937|6|Mentioned|p422, p437|||Folded into a large synclinal structure.||||||02-MAY-13
18012|Texas beds|60993|5|Briefly described|p17|Paleozoic|Paleozoic|Unconformably overlain by Marburg Subgroup units.||||||07-NOV-08
18012|Texas beds|61392|5|Briefly described|p164 Fig. 1|Early Carboniferous|Late Devonian|||||||07-FEB-11
18012|Texas beds|61763|5|Briefly described|p25|Visean|Visean|A volcanic/limestone association. In the Texas Stanthorpe area. Geological Province: New England Orogen.||||||
18012|Texas beds|61770|6|Mentioned|p108|||||||||
18012|Texas beds|61796|5|Briefly described|p386 Fig. 1|Carboniferous|Carboniferous|Geological Province: New England Fold Belt.||||||24-JAN-06
18012|Texas beds|62534|5|Briefly described|p6, p11 (legend)|Early Carboniferous|Early Carboniferous|Intruded by dykes of the "Willowrie diorite".||||||07-FEB-11
18012|Texas beds|63347|5|Briefly described|p5 Fig. 2|Late Carboniferous|Middle Cambrian|In Central Block and Woodsreef Melange.||||||04-JUN-07
18012|Texas beds|63729|5|Briefly described|Map legend|Carboniferous|Carboniferous|Volcaniclastic arenite, siltst., mudst., local phyllite, lenses of jasper, chert, limest.  Thin jasper interlayered with argillite, locally grading into chert. Recrystallised limest., local lst/basalt breccia. maif lava, minor chert. Polymictic pebble to||||||
18012|Texas beds|63731|5|Briefly described|Map legend|Carboniferous|Carboniferous|Volcaniclastic arenite, siltst., mudst.+slate; local phyllite. Altered chert, mafic volcs.+ volcaniclastic+slate sequences; massive greywacke; arenite+argillite; mafic lava; recrystallised limestone, local lst/basalt breccia; chert , argillite; jasper.||||||
18012|Texas beds|63732|5|Briefly described|Map legend|Carboniferous|Carboniferous|Arenite, siltst, mudst.,slate; local phyllite, lenses of jasper, chert, limstn.+mafic volcs. Altered chert, mafic volcs.+slate sequences. Recryst.chert+ interlayered mudst. Jasper+subordinate mudstone. Recrystallised limst.||||||02-MAY-13
18012|Texas beds|63733|5|Briefly described|Map legend|Carboniferous|Carboniferous|Arenite, siltst., mudst. and slate; lenses of jasper, chert, limestone+ mafic volcanics. Altered chert, mafic volcanics and slate sequences. Jasper with layered mudst. grading locally into chert. Recrystallised l'st., lst/basalt breccia. Mafic lava, ...||||||13-DEC-07
18012|Texas beds|63748|3|Fully described|p9-16|Early Carboniferous|Early Carboniferous|Unconformably overlain by Bondonga, Pikedale and Terrica beds. Intruded by Stanthorpe Granite, Greymare Granodiorite, Herries Granite. Geol.prov: Woolomin Province. Seq.of volcaniclastic turbidites (lithic arenite+mudstone). Detailed lithology provided.||||||07-FEB-11
18012|Texas beds|65107|5|Briefly described|p287|Carboniferous|Carboniferous|Contains inliers of Alum Rock Conglomerate and Terrica beds. Also infolded with Silver Spur inlier.||||||
18012|Texas beds|67669|6|Mentioned|p14,18|||Geological province: New England Fold Belt.||||||
18012|Texas beds|67908|5|Briefly described|p279-285|Carboniferous|Devonian|Olgers et al. (1974). New England Orogen. Bedding is steeply-dipping to sub-vertical. Primary structures examined; photographs.|||||A sequence of volcaniclastic turbidites with minor chert and jasper, altered mafic volcanic rocks and limestone. Shows slaty cleavage.|
18012|Texas beds|68003|5|Briefly described|p31, p140.|Early Carboniferous|Early Carboniferous|Central Block, New England Fold Belt. Coeval with Whitlow Formation.|||Includes Ashford Limestone [Member].||Low grade regionally metamorphosed, variably deformed lithic wacke, conglomerate, siltstone, mudstone, chert, basalt, basic and andesitic volcanics, fossiliferous limestone, marble, magnetite-rich rock and rare tuff.|
18012|Texas beds|68005|4|Described|p18, p22, pp33-35, p70, p155, p170.|Carboniferous|Carboniferous|Anaiwan terrane, Central Block, New England Fold Belt. Texas-Sandon association: a thick sequence of deep marine deposition; locally highly deformed; uppermost part of subduction complex. Contact metamorphosed up to 2 km around Mole Granite intrusion. Written as Texas Beds on p70.|||Includes Ashford Limestone.|Overlies Whitlow Formation. Is intruded by Mole Granite.|Dominantly turbidites; typically thin-bedded, coarse lithic wacke or conglomerate horizons, siltstone, mudstone with subordinate chert, jasper and spilite.|
18012|Texas beds|68006|5|Briefly described|p25, p85 Figs.7-Aa,Ab, p114, p115.|Early Carboniferous|Late Devonian|Deposited in a deep marine setting; forms part of a subduction complex. Limestone outcrops near Ashford are thought to represent a seamount within Texas beds sandstone. Written as Texas Beds on pp114-115.||||Overlies Whitlow Formation.|Sandstones.|
18012|Texas beds|68553|6|Mentioned|Map legend; schematic diagram.|Carboniferous|Carboniferous|Texas Subprovince.||||||
18012|Texas beds|68679|5|Briefly described|p321, p446-453, p455-457, p463|Visean|Visean|Olgers et al. (1974); subdivided by Fergusson and Flood (1984) and Donchak et al. (2007). Most extensive unit in the Texas Subprovince, Woolomin Province, northern New England Orogen. Forms an arcuate, convex-north fold closure ~75km across. Numerous photographs; REE plot. Structure, age and provenance detailed. RELATED UNITS (continued): Is intruded by Ruby Creek, Clare Hills, Herries, Sailor Jack, Bullaganang, Mount You You, Granites; Boxwell, Greymare Granodiorites.||||Is overlain unconformably by the Wallangarra Volcanics (Wandsworth Volcanic Group), Texas and Pikedale beds. Correlated with Neranleigh-Fernvale beds and Wandilla Formation. See COMMENTS for more.|A succession of volcaniclastic turbidites (lithic sandstone and mudstone) with minor chert, jasper, argillite, altered mafic volcanics (greenstone) mostly alkalic basalts, and limestone. Lithologies and local variations described in detail.|
18012|Texas beds|68901|5|Briefly described|p8 Fig. iii|Carboniferous|Carboniferous|Woolowin Province.[probably typo for Woolomin].||||||27-SEP-18
18012|Texas beds|69600|5|Briefly described|p656-657|||Texas region. Contains karst topography features including numerous caves which contain diverse Quaternary fossil vetebrate faunas (described).|||||Includes limestone lenses up to 400m wide and 1000m long.|
18012|Texas beds|70036|5|Briefly described|Map legend|||Central Block, New England Fold Belt. Included in a mapped unit of Silurian to Carboniferous strongly deformed, andesitic to rhyolitic metasedimentary rocks, lithic sandstone, argillite, chert and jasper.||||||
18012|Texas beds|70373|5|Briefly described|p789, p791, p793, p800|Carboniferous|Devonian salt|||||Unconformably overlain by and/or faulted against Silver Spur, Terrica and Alum Rock beds. Cut by rhyolitic dyke that also cuts Bondonga beds.|Chert, sandstone and volcanic rocks (rhyolite dyke).|28-SEP-16
18012|Texas beds|71628|5|Briefly described|p4:33, 35; p5:2-3, 5-6, 10; p10:5, 9-10|Carboniferous|Carboniferous|See also p12: 10, 13, 18; p15: 33, 41, 43, 45, 82, 85, 89-90, 97; p18-10; p19: 6, 22, 27, 33, 59, 63, 65, 67, 70-71, 110, 145, 150, 157, 166, 171. Hosts various mineralisations including the Warroo Cu-Au mine, numerous small Au deposits W of Palgrave Monzogranite, and Back Creek and Sundown tin deposits. RELATED UNITS (continued): Is also intruded by Palgrave and Linton Monzogranites; Jibbinbar, Mount Bullaganang, Dumboy-Gragin, Wandera Leucosyenogranites; Mole, Treverton, Ruby Creek Leucogranites; Stanthorpe Complex; Amiens and Elsmore Leucomonzogranites; Greymare Tonalite; Cheviot Hills Granite; Pike Creek Dolerite; Willowrie Diorite; Reedy Gabbro. Is faulted against Passchendaele Monzogranite.||||Is intruded by Boxwell, Dry Creek, Kings Plains Granodiorites; Graman, Sailor Jack, Severn River, Strathaven, Benalla, Balladean, Herries, Clare Hills, Fairleigh Monzogranites. See COMMENTS for more.|Includes volcaniclastic arenite, phyllitic mudstone chert layers, sporadic meta-basalt flow and tuff; locally melange.|
18012|Texas beds|72297|5|Briefly described|p721|||Associated with arsenopyrite, cassiterite and copper in quartz greisen and sheeted veins at Sundown and Jibbinbar, where it is hornfelsed by the Ruby Creek Granite.||||Is intruded by Ruby Creek Granite.||
18012|Texas beds|73487|6|Mentioned|p563, p574 Fig.8|||||||||
18032|Tharwa Adamellite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Adamellite. BMR map symbol: amt.||||||
18032|Tharwa Adamellite|29953|6|Mentioned|p3|||||||||
18032|Tharwa Adamellite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
18032|Tharwa Adamellite|31580|6|Mentioned|p272|||See also analysis table 1-4.||||||
18032|Tharwa Adamellite|31581|3|Fully described|p182|||See also Fig. 1 & analysis Table 1||||||
18032|Tharwa Adamellite|32820|6|Mentioned|p3|||Murrumbidgee Batholith||||||
18032|Tharwa Adamellite|32905|4|Described|p230|||||||||
18032|Tharwa Adamellite|32906|6|Mentioned|p239|||||||||
18032|Tharwa Adamellite|34544|5|Briefly described|p185|||See also p186.||||||18-JAN-16
18032|Tharwa Adamellite|36413|2|Defined|p82|Silurian|Silurian|||||||
18032|Tharwa Adamellite|36414|5|Briefly described|map legend|Ludlovian|Ludlovian|Biotite adamellite. GSNSW map code: gmr.||||||
18032|Tharwa Adamellite|36633|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
18032|Tharwa Adamellite|37501|6|Mentioned|p414|||||||||
18032|Tharwa Adamellite|37728|4|Described|Table 3|||Age quoted in as being from Roddick & Compston (1976). Similar age and geochem analyses as Shannons Flat Adamellite.|414 +/- 6 Ma Rb/Sr.|||||18-JAN-16
18032|Tharwa Adamellite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
18032|Tharwa Adamellite|40328|4|Described|p211|||||||||
18032|Tharwa Adamellite|41356|5|Briefly described|p72|||Mention Fig.58||||||
18032|Tharwa Adamellite|42820|5|Briefly described|p66|||Age from Roddick & Compston (1976).||||||18-JAN-16
18032|Tharwa Adamellite|45003|14|Not recorded|p45,46|||||||||
18061|Thologolong Granite|23309|5|Briefly described|p344-346||Early Devonian|G102 A-Type||||||
18061|Thologolong Granite|24133|3|Fully described|p80||Ordovician|||||||
18061|Thologolong Granite|24142|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
18061|Thologolong Granite|24143|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
18061|Thologolong Granite|24144|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
18061|Thologolong Granite|24145|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Geological Province: Lachlan Fold Belt||||||
18061|Thologolong Granite|24146|5|Briefly described|Map Legend|Devonian|Devonian|Geological Province: Lachlan Fold Belt.||||||
18061|Thologolong Granite|24551|5|Briefly described|p233, 449|||||||||
18061|Thologolong Granite|32684|6|Mentioned|Fig.2|||Petrology P252||||||
18061|Thologolong Granite|38580|6|Mentioned|Fig.2|||||||||
18061|Thologolong Granite|39860|5|Briefly described|p21|||||||||
18061|Thologolong Granite|41868|6|Mentioned|p586|||||||||
18061|Thologolong Granite|42726|5|Briefly described|map legend|Early Devonian||554.  Of the Thologolong Suite (Boggy Plain Supersuite).||||||08-FEB-05
18061|Thologolong Granite|42827|6|Mentioned|p586|||||||||
18061|Thologolong Granite|44184|5|Briefly described|Map Legend||Early Devonian|Shown as Thologolong I-type.||||||
18061|Thologolong Granite|68116|5|Briefly described|Appendix, Map 20.|Middle Devonian|Early Devonian|Magnetic.|||||Leucogranite: pink, coarse- with fine-grained marginal phase; consists of quartz, plagioclase, perthitic K-feldspar and dark brown biotite; accessory muscovite, ilmenite, tourmaline, magnetite, zircon and fluorite; common miarolitic cavities.|
18061|Thologolong Granite|69801|5|Briefly described|p2, p4-p5, p71, p91, p94|Devonian|Early Devonian|Central Lachlan Orogen. Occurs south-east of Holbrook. In hand specimen similar to the Holbrook Granite, despite being geochemically distinct. Sample locality, sample description, petrography, SHRIMP analyses and interpretation are detailed. See also p98-p104, p135-137.|415.7 +/- 2.6 Ma (SHRIMP)|Boggy Plain Supersuite||Intrudes the Adaminaby Group.|A-type, coarse-grained, inequigranular to weakly seriate leucogranite.|
18061|Thologolong Granite|70777|5|Briefly described|p2, p81|Lochkovian|Lochkovian|Lachlan Orogen. A-type geochemistry.|415.7 +/- 2.6 Ma (Bodorkos et al., 2015)|||||
18061|Thologolong Granite|73082|5|Briefly described|p30|Devonian|Devonian|SE of Holbrook. Source of alluvial tin in Basin Creek.|||||Contains cassiterite-bearing quartz veins.|
18061|Thologolong Granite|73457|6|Mentioned|ii, p13 Fig.8, p14|Early Devonian|Early Devonian||415+/-2.6 Ma (Bodorkos et al., 2015)|||Nonconformably underlies Mandaring Formation||
18080|Thorkidaan Volcanics|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
18080|Thorkidaan Volcanics|22708|6|Mentioned|p212|||||||||
18080|Thorkidaan Volcanics|22968|5|Briefly described|P12, P111|Late Silurian|Silurian|Formerly mapped as Snowy River Volcanics, oldest unit of Enano Group||||||
18080|Thorkidaan Volcanics|23021|5|Briefly described|Map legend|Pridoli|Ludlow|Parent is Enano Group, overlying unit is Cowombat Siltstone||||||
18080|Thorkidaan Volcanics|23030|5|Briefly described|Map legend|Late Silurian|Late Silurian|Parent is the Enano Group||||||
18080|Thorkidaan Volcanics|23235|5|Briefly described|Fig7-1p68, 68|Late Silurian|Silurian|||||||
18080|Thorkidaan Volcanics|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
18080|Thorkidaan Volcanics|23615|3|Fully described|p78, p20 Fig.6, p161|Ludlow|Wenlock|Of Enano Group. Name used interchangeably with Thorkidaan Volcanics Formation throughout text.  Intrudes the Blueys Creek Formation and small lavas intrude the Towanga Sandstone.||||||14-NOV-13
18080|Thorkidaan Volcanics|23938|5|Briefly described|p14 Tb. 1, p139 Tb.1 App.|Late Silurian|Early Silurian|Of the Enano Group. Rhyolitic lavas, pyroclastics and shallow intrusives, with ~10% volcaniclastic sediments. Overlain by Cowombat Siltstone. In the Limestone Creek Graben. See also p38-39 Tb. 2, p77.||||||
18080|Thorkidaan Volcanics|24004|5|Briefly described|p280|Late Silurian|Late Silurian|||||||
18080|Thorkidaan Volcanics|24133|5|Briefly described|p20 Fig. 8|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
18080|Thorkidaan Volcanics|24275|4|Described|p1695, p1697 Fig. 3, p1698 Tb. 1|Late Silurian|Silurian|Of the Enano Group. Massive porphyritic rhyolite; minor stratified rhyolite, volcaniclastic sandstone, siltstone, conglomerate and pumiceous breccia. In fault contact with Gibsons Folly Formation. Thickness: 2-3km. Geol.Prov: LFB.||||||26-JUN-14
18080|Thorkidaan Volcanics|24551|4|Described|p135|Silurian|Silurian|Of the Enano Group. Overlain by Cowombat Siltstone and Gibsons Folly Formation. Includes 15 units, only which four are true members.||||||
18080|Thorkidaan Volcanics|24598|5|Briefly described|p515 Fig. 1|Late Silurian|Silurian|Geological Province: Lachlan Orogen.||||||
18080|Thorkidaan Volcanics|37330|4|Described|p10|||||||||
18080|Thorkidaan Volcanics|38367|6|Mentioned|Fig.1|||||||||
18080|Thorkidaan Volcanics|39291|4|Described|p218|||||||||
18080|Thorkidaan Volcanics|39447|6|Mentioned|p6|||See also P23||||||
18080|Thorkidaan Volcanics|39860|5|Briefly described|p8|||||||||
18080|Thorkidaan Volcanics|40761|5|Briefly described|p226|||Mention Fig.6||||||
18080|Thorkidaan Volcanics|41570|6|Mentioned|p92|||||||||
18080|Thorkidaan Volcanics|41572|5|Briefly described|p21|||||||||
18080|Thorkidaan Volcanics|41585|4|Described|p127|||||||||
18080|Thorkidaan Volcanics|41755|6|Mentioned|Fig.1|||||||||
18080|Thorkidaan Volcanics|42089|5|Briefly described|p18|||See also Fig.62||||||
18080|Thorkidaan Volcanics|42726|5|Briefly described|map legend|Silurian||Variation on Thorkidaan Volcanic Group etc?||||||
18080|Thorkidaan Volcanics|42791|5|Briefly described|p216|||||||||
18080|Thorkidaan Volcanics|42827|3|Fully described|p127|||Of Enano Group.||||||25-SEP-08
18080|Thorkidaan Volcanics|43128|5|Briefly described|Fig.6,p476||Late Silurian|||||||
18080|Thorkidaan Volcanics|43206|5|Briefly described|map legend||Wenlock|Of Enano Group||||||
18080|Thorkidaan Volcanics|43220|5|Briefly described|p9||Silurian|||||||
18080|Thorkidaan Volcanics|43770|5|Briefly described|p831|||||||||
18080|Thorkidaan Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv8||||||
18080|Thorkidaan Volcanics|44184|5|Briefly described|Map Legend||Early Silurian|||||||
18080|Thorkidaan Volcanics|44185|5|Briefly described|Map legend.|Early Silurian|Early Silurian||||||Felsic ignimbrite, porphyry, minor sediments.|
18080|Thorkidaan Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
18080|Thorkidaan Volcanics|60503|4|Described|p108, p15, p28 Fig. 9|Ludlow|Wenlock|Of the Enano Group. Includes Native Cat Volcaniclastic, Copperhead Volcaniclastic and Sapper Nose Rhyolite Members. Thick sequence of mixed subaerial and shallow marine rhyolitic lavas and minor volcaniclastics. Overlain by Enano Group.||||||14-NOV-13
18080|Thorkidaan Volcanics|60504|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Enano Group. Includes: Copperhead Volcaniclastic Member, Native Cat Volcaniclastic Member, Sapper Nose Rhyolite Member.||||||20-OCT-04
18080|Thorkidaan Volcanics|60505|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Enano Group. Includes: Copperhead Volcaniclastic Member, Native Cat Volcaniclastic Member, Sapper Nose Rhyolite Member.||||||
18080|Thorkidaan Volcanics|60506|5|Briefly described|Map legend|Ludlow|Ludlow|Of the Enano Group. Includes: Copperhead Volcaniclastic Member, Native Cat Volcaniclastic Member, Sapper Nose Rhyolite Member.||||||20-OCT-04
18080|Thorkidaan Volcanics|60507|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Enano Group. Includes: Copperhead Volcaniclastic Member, Native Cat Volcaniclastic Member, Sapper Nose Rhyolite Member.||||||20-OCT-04
18080|Thorkidaan Volcanics|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Rhyolite, sandstone: nonmagnetic cut by west-northwest, north, northeast weakly magnetic (10-20 nT) trends; northeast trending bands of high K, low Th, and low K, high Th.||||||
18080|Thorkidaan Volcanics|60541|5|Briefly described|p11 Fig. 2|Silurian|Silurian|Age is Middle Silurian.||||||
18080|Thorkidaan Volcanics|60542|5|Briefly described|p11 Fig. 2|Middle Silurian|Middle Silurian|||||||
18080|Thorkidaan Volcanics|61181|5|Briefly described|p171|Silurian|Silurian|Of the Enano Group. Rhyolite dominates the lithology.||||||
18080|Thorkidaan Volcanics|61187|5|Briefly described|p5 Fig.3, p24, p26 Fig.2, p29 Fig.4. |Silurian|Silurian|Buchan Zone, Benambra Terrane. Age interpreted from Fig.3. 2 km to 3 km thick. Mixed subaerial and shallow marine deposits. Radiometrically, can be clearly divided into Th-rich and K-rich (presumably acid volcanics) units.|c.425-c.412 Ma.||Unit in Enano Group.|Conformably overlies, and interfingers with, Towamba Sandstone.|Rhyolitic lavas, pyroclastics and shallow intrusions; minor volcaniclastic sediments.|
18080|Thorkidaan Volcanics|66197|5|Briefly described|p635 Fig.5c|||Buchan Basin. Silicic volcanics and volcaniclastics. Underlies the Cowombat Siltstone or Gibsons Folly Formation.||||||14-MAR-12
18080|Thorkidaan Volcanics|68116|5|Briefly described|Appendix, Maps 27-28, 35-36.|Ludlow|Wenlock||||||Rhyolitic lava, minor volcaniclastics, pyroclastics and shallow intrusions; volcaniclastics are massive, porphyritic with phenocrysts of quartz, K-feldspar, plagioclase and biotite.|
18082|Thorndale Composite Gneiss|6823|6|Mentioned|p205|Palaeoproterozoic|Palaeoproterozoic|||||Underlies the Thackaringa Group.||26-MAR-22
18082|Thorndale Composite Gneiss|22553|5|Briefly described|fig2p77,p78|Proterozoic|Proterozoic|||||||
18082|Thorndale Composite Gneiss|22575|6|Mentioned|p179 Fig.2|||In the Broken Hill Block.||||||11-JUN-08
18082|Thorndale Composite Gneiss|22588|6|Mentioned|p85|||||||||
18082|Thorndale Composite Gneiss|22631|6|Mentioned|table1, p173|Statherian|Statherian|||||||
18082|Thorndale Composite Gneiss|22771|6|Mentioned|Table12.2p45|||||||||
18082|Thorndale Composite Gneiss|22857|4|Described|p45 Tb. 12.2, p392 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Formerly the Thorndale Gneiss of Mawson (1912). Of the Willyama Supergroup. Max. thickness: 2km; in type section: 1400m. Geological Province: Willyama Fold Belt.||||||07-NOV-08
18082|Thorndale Composite Gneiss|22884|5|Briefly described|p41|||Overlain by units of Thackeringa Group. Geological province: Broken Hill Domain.||||||26-MAR-09
18082|Thorndale Composite Gneiss|22959|6|Mentioned|p95||Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|22962|6|Mentioned|p74||Statherian|||||||
18082|Thorndale Composite Gneiss|22963|5|Briefly described|p69||Paleoproterozoic|Possible correlation with Gandry Dam Gneiss (Mt Isa Maronan Supergroup) and lower sequence of the Georgetown (Qld) Etheridge Group.||||||07-NOV-08
18082|Thorndale Composite Gneiss|22965|6|Mentioned|p13, Fig1||Statherian|||||||
18082|Thorndale Composite Gneiss|22966|6|Mentioned|Fig1||Proterozoic|Rift stage of development.||||||
18082|Thorndale Composite Gneiss|22967|5|Briefly described|p25,6,39,41||Statherian|||||||
18082|Thorndale Composite Gneiss|23025|6|Mentioned|Fig1p75|||||||||
18082|Thorndale Composite Gneiss|23160|6|Mentioned|fig1|||||||||
18082|Thorndale Composite Gneiss|23248|5|Briefly described|Fig2p169|||||||||
18082|Thorndale Composite Gneiss|23347|6|Mentioned|p52|||Geological province: Broken Hill Domain. Equivalent to parts of Wiperaminga Subgroup.||||||24-MAR-09
18082|Thorndale Composite Gneiss|24307|5|Briefly described|p967 Fig. 2|Proterozoic|Proterozoic|||||||
18082|Thorndale Composite Gneiss|38969|4|Described|p204|||||||||
18082|Thorndale Composite Gneiss|39662|2|Defined|p412|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|39828|6|Mentioned|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|39849|6|Mentioned|p86|||||||||
18082|Thorndale Composite Gneiss|39883|6|Mentioned|p380|||||||||
18082|Thorndale Composite Gneiss|40290|6|Mentioned|Fig.2|||||||||
18082|Thorndale Composite Gneiss|40595|6|Mentioned|p86|||||||||
18082|Thorndale Composite Gneiss|40822|6|Mentioned|Fig.2|||||||||
18082|Thorndale Composite Gneiss|41093|4|Described|p251|||||||||
18082|Thorndale Composite Gneiss|41145|6|Mentioned|Fig.4|||||||||
18082|Thorndale Composite Gneiss|41630|6|Mentioned|p27|||||||||
18082|Thorndale Composite Gneiss|41633|6|Mentioned|p141|||||||||
18082|Thorndale Composite Gneiss|42261|6|Mentioned|Fig 1 P530|||||||||
18082|Thorndale Composite Gneiss|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
18082|Thorndale Composite Gneiss|42537|6|Mentioned|Fig.2 P5|||||||||
18082|Thorndale Composite Gneiss|42595|6|Mentioned|Fig. 2 P5|||||||||
18082|Thorndale Composite Gneiss|42720|5|Briefly described|map legend|Paleoproterozoic||South Australia.||||||07-NOV-08
18082|Thorndale Composite Gneiss|42813|6|Mentioned|p9|||||||||
18082|Thorndale Composite Gneiss|42897|5|Briefly described|Fig.3, P321|||||||||
18082|Thorndale Composite Gneiss|42942|6|Mentioned|p17|||Of Willyama Supergroup.||||||11-JUN-08
18082|Thorndale Composite Gneiss|43052|6|Mentioned|Fig.4.22|||||||||
18082|Thorndale Composite Gneiss|43086|6|Mentioned|Fig.3|||||||||
18082|Thorndale Composite Gneiss|43263|6|Mentioned|Map Legend||Paleoproterozoic|||||||07-NOV-08
18082|Thorndale Composite Gneiss|43268|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43270|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43271|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43272|5|Briefly described|Map Legend||Paleoproterozoic|Of the Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43274|5|Briefly described|Map Legend||Paleoproterozoic|Of Willyama Supergroup.||||||07-NOV-08
18082|Thorndale Composite Gneiss|43572|6|Mentioned|Fig.3.2 p6|||||||||
18082|Thorndale Composite Gneiss|43583|5|Briefly described|Table 1, p2139|||||||||
18082|Thorndale Composite Gneiss|46598|5|Briefly described|p303|||||||||
18082|Thorndale Composite Gneiss|50045|5|Briefly described|p116 Fig. 3, p114 Fig. 1|||Geological Province: Broken Hill Block. Of the Willyama Supergroup. Overlain by Thackaringa Group. Underlain by Clevedale Migmatite.||||||31-MAY-07
18082|Thorndale Composite Gneiss|50619|5|Briefly described|p174 Fig. 1|Paleoproterozoic|Paleoproterozoic|Of the Willyama Supergroup. Metasedimentary pelitic to psammitic gneiss. Geological Province: Broken Hill Block.||||||07-SEP-15
18082|Thorndale Composite Gneiss|60485|5|Briefly described|p28 Fig. 2|||Of the Thackaringa Group? Geological Province: Broken Hill Domain.||||||
18082|Thorndale Composite Gneiss|61606|5|Briefly described|p4 Fig.2|||Of the Willyama Supergroup.||||||
18082|Thorndale Composite Gneiss|61735|5|Briefly described|p635 Fig. 1, p653, 639|Paleoproterozoic|Paleoproterozoic|Overlies Clevedale Migmatite. See also p636 Fig. 2. Max depositional age 1830-1850 Ma. Max metamorphic age 1617+/-3 Ma U/Pb SHRIMP.||||||04-JUN-15
18082|Thorndale Composite Gneiss|61736|5|Briefly described|p666 Fig. 3|Paleoproterozoic|Paleoproterozoic|Age: </-1830-1850Ma. Geological province: Olary Domain.||||||24-FEB-10
18082|Thorndale Composite Gneiss|62473|5|Briefly described|p74|Paleoproterozoic|Paleoproterozoic|Apparent ages: 1640 to 1610Ma and older (SHRIMP zircon).||||||17-JUN-09
18082|Thorndale Composite Gneiss|62535|5|Briefly described|p666-667, p672|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain. Hosts various types of oxide-, sulfide-, and silicate-facies iron formation with minor strata-bound Cu, Co and/or Au deposits.|1850-c.1830 Ma.|||||
18082|Thorndale Composite Gneiss|62536|5|Briefly described|p635-636, 639-641, 653-654|||13 km E of Broken Hill. Zircon dating discussed. An alternative dating based on 5 analyses gives an MDA of 1850-1830 Ma.|1617 +/- 3 Ma (metamorphosed; MDA).|||Overlies Clevedale Migmatite. Is overlain by the Thackaringa Group.|Includes metapsammites and pervasive migmatitic segregations. Granulite facies metamorphism.|
18082|Thorndale Composite Gneiss|62592|6|Mentioned|p16 Fig.2.2. |||Broken Hill Domain, Curnamona Province.||Unit in Thackaringa Group.||||
18082|Thorndale Composite Gneiss|62993|6|Mentioned|p37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Willyama Supergroup|Includes Clevedale Migmatite Member|||15-DEC-21
18082|Thorndale Composite Gneiss|63102|5|Briefly described|p13-15|Statherian|Statherian|Geological province: Broken Hill Domain, Curnamona Province.||Unit of Thackaringa Group.||||
18082|Thorndale Composite Gneiss|63186|5|Briefly described|p71 Fig. 5|Paleoproterozoic|Paleoproterozoic|Age: 1715 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Metasedimentary composite gneiss.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63519|5|Briefly described|p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
18082|Thorndale Composite Gneiss|63866|5|Briefly described|p36||||c. 1710 Ma (Max. deposition)|Willyama Supergroup||||
18082|Thorndale Composite Gneiss|64097|5|Briefly described|p303, p325|Paleoproterozoic|Paleoproterozoic|Conformably overlain by Thackaringa Group. Geological province: Broken Hill Domain/Curnamona province. Partially melted metasediments with or without albitic alteration.||||||07-FEB-11
18082|Thorndale Composite Gneiss|64316|5|Briefly described|p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-FEB-11
18082|Thorndale Composite Gneiss|64742|6|Mentioned|p321 Fig.3, p323.|||A sample of this unit used for Sm-Nd analysis is listed under Thackaringa Group in Table 1, despite a clear separation of these units in Fig.3.||Unit in Willyama Supergroup.||||29-MAR-12
18082|Thorndale Composite Gneiss|64743|6|Mentioned|p339 Fig.1. |Paleoproterozoic|Paleoproterozoic|||||||
18082|Thorndale Composite Gneiss|64744|5|Briefly described|p353 Fig.4, p354.|Statherian|Statherian|Broken Hill Domain. High-grade metasedimentary rocks.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Thackaringa Group.||
18082|Thorndale Composite Gneiss|64944|5|Briefly described|p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain.||||||07-FEB-11
18082|Thorndale Composite Gneiss|66302|5|Briefly described|p36 Fig.9, p39, p40|Statherian|Statherian|Broken Hill Domain, Curnamona Province.|ca. 1710 (U-Pb zircon)|Thackaringa Group||Overlies the Clevedale Migmatite. Overlain by the Lady Brassey Formation.||
18082|Thorndale Composite Gneiss|66857|6|Mentioned|p972 Fig.2.|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Thackaringa Group.||
18082|Thorndale Composite Gneiss|67323|5|Briefly described|Eastern Australia Time-Space Plot|||Broken Hill Domain.|~1850-1830 Ma (max depositional age).|Thackaringa Group.|Clevedale Migmatite Member.|||
18082|Thorndale Composite Gneiss|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
18082|Thorndale Composite Gneiss|68126|5|Briefly described|p6, p29|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||Willyama Supergroup.||||
18082|Thorndale Composite Gneiss|69999|6|Mentioned|p3|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Basal, early-rift fluviatile to shallow marine sedimentation.||||||
18082|Thorndale Composite Gneiss|70000|5|Briefly described|p31, p33-35|||Among the oldest outcropping units in the Broken Hill Domain.|||Includes Clevedale Migmatite.||Metasedimentary gneiss and migmatite +/- albitic horizons hosting ubiquitous sills and dykes of basic gneiss.|
18082|Thorndale Composite Gneiss|70014|5|Briefly described|Map legend|||Segregations commonly disrupt bedding. Bedding in the composite gneiss/metasediments is generally disrupted, lenticular and/or discontinuous, and highly variable in thickness. Rare graded bedding, crossbedding, and scour-and-fill structures are present in places. Other rocks present include psammitic, psammopelitic and pelitic metasediments, basic gneiss, minor plagioclase-quartz rock and K-feldspar-rich leucocratic rock, and rare quartz-magnetite and quartz-iron oxide/sulfide rocks.||Unit in Willyama Supergroup.||Overlies Clevedale Migmatite. Is overlain by Alma Gneiss (Thackaringa Group).|Mainly metasedimentary quartz-feldspar-biotite-sillimanite +/- garnet +/- cordierite composite gneiss consisting of interlayered psammite and psammopelite, generally with minor pelite; abundant pegmatitic to granitic quartzo-feldspathic segregations.|
18082|Thorndale Composite Gneiss|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.||Unit in Willyama Supergroup.|Includes Clevedale Migmatite.||Metasedimentary (psammite/psammopelite) quartz-feldspar-biotite-sillimanite(-garnet)(-cordierite) composite gneiss, abundant pegmatitic/granitic segregations.|
18082|Thorndale Composite Gneiss|70657|4|Described|p10 Fig.4, p13 Fig.6, p15|Statherian|Statherian|Curnamona Province; Mulyungarie, Broken Hill Domains. Shown as Thackaringa Group + Thorndale Composite Gneiss + Clevedale Migmatite in Fig.4.|~1705-1700 Ma|Thackaringa Group|Includes Clevedale Migmatite.|Overlies Redan Gneiss. Underlies Lady Brassey Formation, and Alma Gneiss of Silver City Suite.||
18082|Thorndale Composite Gneiss|70658|6|Mentioned|p15-16|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain, Curnamona Province.||||||
18082|Thorndale Composite Gneiss|71968|6|Mentioned|p4|||Geological province: Curnamona province.||||||
18082|Thorndale Composite Gneiss|72454|6|Mentioned|p2 Fig.2, p8 Fig.6|Mesoproterozoic|Mesoproterozoic|Part of the Broken Hill Domain. Shown only on p2 Fig.2 and p8 Fig.6.||Willyama Supergroup|||Includes gneiss.|
18082|Thorndale Composite Gneiss|72461|6|Mentioned|p16 fig 9|||||||||
18082|Thorndale Composite Gneiss|73243|6|Mentioned|p52 Fig.1, p53 Fig.2, p59|||Broken Hill block-Euriowie block. Some amphibolite bodies appear to transgress bedding, interpreted as dykes emplaced during or immediately after deposition of the Broken Hill Group. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites.||Willyama Supergroup|||Contains amphibolite dykes.|
18082|Thorndale Composite Gneiss|73308|6|Mentioned|p607 Fig.1|||||Willyama Supergroup.||||
18082|Thorndale Composite Gneiss|73482|5|Briefly described|p422 Fig.3, p423|||||Willyama Supergroup|Clevedale Migmatite|||
18082|Thorndale Composite Gneiss|73512|6|Mentioned|p2, p7|||||Willyama Supergroup||||
18082|Thorndale Composite Gneiss|73524|6|Mentioned|p5 Fig.3|||||Thackaringa Group||||
18082|Thorndale Composite Gneiss|73575|5|Briefly described|p828 Fig.2, p829 Fig.3|||||Willyama Supergroup|Clevedale Migmatite|Underlies Thackaringa Group, Lady Brassey Formation||
18106|Thule Granite|22857|6|Mentioned|p412 App.1 Tb.A1.5|Late Silurian|Late Silurian|||||||
18106|Thule Granite|22887|5|Briefly described|p29|Silurian|Silurian|No obvious magnetic signature. Isotope ages range from 408+/-6 Ma to 422+/-6 Ma.||||||
18106|Thule Granite|23101|5|Briefly described|p567 (Fig 1)|||||||||
18106|Thule Granite|23171|5|Briefly described|p12|Ludlow|Wenlock|Max age: 422 (+/-) 6 Ma; Min Age: 416 (+/-) 6 Ma (K-Ar).||||||
18106|Thule Granite|23173|4|Described|Map Legend|Ludlovian|Ludlovian|||||||
18106|Thule Granite|23252|5|Briefly described|Map Legend|||Actually refers to Thule Granite equivalent.||||||
18106|Thule Granite|29987|5|Briefly described|p15|||||||||
18106|Thule Granite|34449|6|Mentioned|Table 2-1|||||||||
18106|Thule Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
18106|Thule Granite|38292|6|Mentioned|Fig.1|||||||||
18106|Thule Granite|39083|6|Mentioned|p30|||||||||
18106|Thule Granite|39618|6|Mentioned|p12|||||||||
18106|Thule Granite|39627|4|Described|p265|||||||||
18106|Thule Granite|40328|4|Described|p211|||||||||
18106|Thule Granite|40913|6|Mentioned|Map legend|Wenlockian|Wenlockian|||||||
18106|Thule Granite|41126|2|Defined|p17|Middle Silurian|Middle Silurian|||||||
18106|Thule Granite|41138|6|Mentioned|Map legend|Silurian|Silurian|||||||
18106|Thule Granite|41394|6|Mentioned|p9|||||||||
18106|Thule Granite|41528|6|Mentioned|p15|||||||||
18106|Thule Granite|41700|6|Mentioned|Map legend|Paleozoic||||||||07-NOV-08
18106|Thule Granite|41821|2|Defined|p20|Middle Silurian||Name introduced by Lloyd 1938||||||
18106|Thule Granite|42408|6|Mentioned|p415|||||||||
18106|Thule Granite|42521|5|Briefly described|p15|||422 +/- Ma||||||
18106|Thule Granite|42566|6|Mentioned|p37|||||||||
18106|Thule Granite|42726|5|Briefly described|map legdn|||||||||
18106|Thule Granite|42983|6|Mentioned|Fig.3,p345|||||||||
18106|Thule Granite|43032|2|Defined|p24|Late Silurian||||||||
18106|Thule Granite|43089|5|Briefly described|Map Legend|||||||||
18106|Thule Granite|43389|14|Not recorded|Map Legend||Silurian|||||||
18106|Thule Granite|43757|6|Mentioned|p510|||||||||
18106|Thule Granite|63891|5|Briefly described|p237, p240|||Exposed. Contact with Mount Hope Group not exposed. Interpreted to underlie Mount Hope Volcanics (Mount Hope Group).||||||
18106|Thule Granite|65469|5|Briefly described|p15, p16|Early Silurian|Early Silurian|Lachlan Orogen.||Koetong Supersuite||||
18106|Thule Granite|68823|6|Mentioned|p376 Fig.3, p377|Silurian|Silurian|Local source of sediments for Amphitheatre Group.||||||
18106|Thule Granite|69002|6|Mentioned|p15|||||||||
18106|Thule Granite|69511|4|Described|p1-3, p5, p7, p14, p22-27, p44, p48|Late Silurian|Late Silurian|Previously the Wirlong Granite (Lloyd, 1936).  Central Lachlan Orogen. Occurs as a fault-bounded batholith forming a meridional strip up to 8.5 km wide and over 70 km long. Is texturally and compositionally similar to the Erimeran Granite. This age determination implies that previous ages (details given) were at least partially reset.|425.7 +/- 2.4 Ma.|||Is faulted against the Amphitheatre, Winduck and Mulga Downs Groups. Is overlain by Mount Halfway Volcanics (inferred).|Felsic, fractionated, peraluminous quartz, two feldspar, biotite-muscovite granite. S-type.|
18106|Thule Granite|70751|5|Briefly described|p5, p9-p10, p12, p25, p30, p38|Late Silurian|Late Silurian|An additional date from Chisholm et al, 2014 is recorded as 427.2 +/- 3.1 Ma whilst a SHRIMP date of 424.1 +/- 2.9 Ma is recorded from this study. Prospective for Sn-W mineralisation.|425.7 +/- 2.4 Ma (SHRIMP, Chisholm et al, 2014)|||||
18106|Thule Granite|70876|5|Briefly described|p16, p20, p76|Silurian|Silurian|Lachlan Orogen.|425.7 +/- 2.4 Ma (Chisholm et al, 2014a)|||Nonconformably overlain by the Shuttleton Rhyolite Member, Amphitheatre Group.||
18106|Thule Granite|70950|6|Mentioned|p1030,1033,1037|Late Silurian|Late Silurian|Geological province: Central Lachlan Orogen. Intruded Ordovician basement, and upper Silurian to lowermost Devonian volcano-sedimentary sequences that overlie basement. U-Pb SHRIMP zircon dating indicates late Silurian age.||||Overlain unconformably by Gundaroo Sandstone and Booth Limestone Member.||
18106|Thule Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Equigranular to porphyritic, coarse-grained, muscovite and biotite-muscovite granite, and lesser porphyritic tourmaline-biotite-muscovite microgranite and greisen.|
18106|Thule Granite|72908|6|Mentioned|p5, p14, p16|Late Silurian|Late Silurian||~427-419 Ma|||Unconformably underlies Buckambool Sandstone, Gundaroo Sandstone||
18106|Thule Granite|72951|5|Briefly described|p1013, 1015-1016, 1021|Ludlow|Wenlock|Lachlan Orogen. Albury-Bega Terrane. S-type granite. SHRIMP U-Pb zircon isotope analyses from Chisholm et al. (2014). eHf = -5.7 +/- 0.7, and d18O = 9.44 +/- 0.13.|425.7 +/- 2.4 Ma||||Felsic muscovite granite.|
18106|Thule Granite|72958|6|Mentioned|p5, p11, p46, p61|Pridoli|Wenlock|Part of a series of Silurian basement granites that underlie the Cobar Basin.|424.5 +/- 2.6 Ma|||||
18106|Thule Granite|73578|6|Mentioned|p50|Pridoli|Homerian|Ages include 425.7 +/- 2.4 Ma and 427.2 +/- 3.1 Ma (Chisholm et al., 2014), and 424.1 +/- 2.9 Ma (Downes et al., 2016).|ca 242 Ma to 427 Ma|||||
18114|Tia Granodiorite|22857|6|Mentioned|p240|Late Carboniferous|Late Carboniferous|Age: 300Ma (SHRIMP zircon, Hand, Offler and Dirk, in press).||||||
18114|Tia Granodiorite|22863|6|Mentioned|p240||Stephanian|Max Age: 300 Ma.||||||
18114|Tia Granodiorite|29990|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
18114|Tia Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
18114|Tia Granodiorite|38804|4|Described|p95|||||||||
18114|Tia Granodiorite|41347|6|Mentioned|p365|||||||||
18114|Tia Granodiorite|41348|5|Briefly described|Map legend|Early Paleozoic||Of the Hillgrove Plutonic Suite.||||||07-NOV-08
18114|Tia Granodiorite|42803|4|Described|p111|||Radiometric age of 264 +/- 2.6 and 262 +/- 2.6 Ma.||||||
18114|Tia Granodiorite|42872|5|Briefly described|p105|||Of Hillgrove Suite.||||||25-SEP-08
18114|Tia Granodiorite|42984|5|Briefly described|p370|||||||||
18114|Tia Granodiorite|44093|5|Briefly described|p122|Late Carboniferous|Late Carboniferous|See also p235 and 236 Appendix 1. Of the Hillgrove Suite. Geological Province: New England Fold Belt.||||||
18114|Tia Granodiorite|44244|6|Mentioned|p301|||On the YARROWICH 1:100K sheet.  Of the Hillgrove Plutonic Suite.||||||26-AUG-04
18114|Tia Granodiorite|61770|6|Mentioned|p108, p110|||Age: 302+/-4Ma (U-Pb).||||||25-SEP-08
18114|Tia Granodiorite|65114|5|Briefly described|p397|Gzhelian||S-type plutons dated using U-Pb SHRIMP at 302 +/- 4 Ma; part of the Hillgrove Plutonic Suite||||||30-MAR-10
18114|Tia Granodiorite|68822|6|Mentioned|p338|Asselian|Asselian||ca. 296 Ma|||||
18114|Tia Granodiorite|69930|6|Mentioned|255|||Southern New England Fold Belt. Emplaced at deeper depth; regional scale metamorphic aureole.||||||
18114|Tia Granodiorite|71628|4|Described|p3: 1, 4, 6, 8, 10, 53, 81, 86-91|||Binns et al. (1967), after the small village of that name. Crops out 19 km SSW of Walcha; excellent outcrop. Wilkinson (1969) referred to it as Tia Adamellite-Granodiorite. Appears as Tia Monzogranite on p3-53. Underwent several deformations, detailed. Geochemistry described. Several age determinations (302 - 296 Ma) are given.|302 +/- 4 Ma (U-Pb TIMS: Landenberger, 1996).|Tia Suite.||Intrudes Tia Complex.|Medium- to coarse-grained, even-grained to weakly porphyritic, foliated biotite (+/- garnet) granodiorite, and lesser monzogranite; moderately to strongly deformed. S-type.|
18114|Tia Granodiorite|71703|5|Briefly described|p203, 204,  p193 Fig. 1|Cisuralian|Cisuralian|~296 Ma; Cawood et al., 2011. [Probably 295.7+/-2.8 Ma]. Age this paper: 300.1+/-2 Ma.|Recalc. 299.7+/-2 Ma (McKibbin et al.2017)|Of Hillgrove Supersuite.||Spatially associated with Bakers Creek Suite.||
18114|Tia Granodiorite|72313|6|Mentioned|p459 Table 2|||New England Orogen. S-type.  Hf isotope data included.|302 Ma|||||
18114|Tia Granodiorite|73197|6|Mentioned|p473|Sakmarian|Gzhelian|Reprocessing of U-Pb zircon ages from 295.7 +/- 2.8 Ma to 300.1 +/- 2 Ma to include all dated zircons including those older than 300Ma.|300.1 +/- 2 Ma U-Pb zircon|||||
18117|Tiabundie beds|38222|6|Mentioned|p358|||||||||
18127|Tibooburra Granodiorite|22671|6|Mentioned|Fig1 p835||Pridoli|I-type. Max Age: 410 Ma. In the Thomson Fold Belt.||||||19-JAN-17
18127|Tibooburra Granodiorite|22700|3|Fully described|Fig.3 p778|Devonian|Silurian|Supersedes Tibooburra Granite. See also p779-781. of Thomson Fold Belt. Intruded Wonominta beds and Easter Monday beds.||||||02-JUL-08
18127|Tibooburra Granodiorite|22768|6|Mentioned|p159,166|||||||||
18127|Tibooburra Granodiorite|22857|6|Mentioned|p166|||||||||
18127|Tibooburra Granodiorite|23309|5|Briefly described|P366|||||||||
18127|Tibooburra Granodiorite|40291|6|Mentioned|p15|||||||||
18127|Tibooburra Granodiorite|44093|5|Briefly described|p190 App. 1|Early Devonian|Early Devonian|Age: 410Ma (isotopic data: S. Shaw pers. comm. 1982).||||||29-MAR-05
18127|Tibooburra Granodiorite|61823|5|Briefly described|p118|Early Devonian|Late Silurian|Geological Province: Tibooburra Inlier.||||||06-MAY-13
18127|Tibooburra Granodiorite|63489|5|Briefly described|Map legend|Devonian|Silurian|Age: 410Ma.||||||
18127|Tibooburra Granodiorite|63793|6|Mentioned|p25.||||410 Ma (Shaw 1982).|||||
18127|Tibooburra Granodiorite|66623|3|Fully described|p103, pp160-166, pp170-175. |Silurian|Silurian|Formerly the Tibooburra Granite (Kenny 1934); recognised as a granodiorite by Morton (1982) and first published as Tibooburra Granodiorite by Stevens (1985). Outcrops as prominent hills of stacked, rounded tors with intervening valleys. A contact aureole extends up to 1 km in Easter Monday Formation. Is crosscut by prominent NE-trending, SE-dipping joint set and fault set. Geochemistry is discussed in detail.|420.6 +/- 3.3 Ma.|Unit in Tibooburra Suite.||Intrudes Easter Monday Formation. Is unconformably overlain by Namur Sandstone.|Mesocratic, medium-grained, homogeneous intrusion of quartz-plagioclase-biotite-hornblende with/without orthoclase, zircon and apatite; abundant mafic enclaves; rare sedimentary enclaves; quartz-feldspar porphyry dykes; pegmatites; aplite dykes.|
18127|Tibooburra Granodiorite|66920|5|Briefly described|Map legend|Silurian|Silurian|The three minor units are un-named but mapped separately.|||||Massive, weakly porphyritic, strongly jointed medium-grained seriate granodiorite; minor units of dark grey, porphyritic granodiorite dykes, massive leucocratic granitoid, and massive equigranular diorite.|
18127|Tibooburra Granodiorite|66921|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Tibooburra Suite.|||Discontinuous dykes of dark grey, massive, fine- to coarse-grained porphyritic granodiorite with phenocrysts of quartz, plagioclase, biotite and minor hornblende.|
18127|Tibooburra Granodiorite|66922|5|Briefly described|Map legend|Silurian|Silurian|||Unit in Tibooburra Suite.|||Sills and dykes of fine- to medium-grained hornblende-phyric monzodiorite with bladed plagioclase, minor K-feldspar and quartz, and accessory apatite; subalkaline geochemical affinity.|
18127|Tibooburra Granodiorite|66927|5|Briefly described|Map legend|Silurian|Silurian|An area of low to moderate magnetic intensity which shows complex concentric trends, particularly at the northern end. A strong contrast with more highly magnetised hornfelsed host is evident at boundaries.|||Unit in Tibooburra Suite.||Medium-grained, I-type granodiorite.|
18127|Tibooburra Granodiorite|66933|6|Mentioned|Map legend||||412 +/- 10 Ma.|||||
18127|Tibooburra Granodiorite|67207|5|Briefly described|Map legend.|Silurian|Silurian|||Unit in Tibooburra Suite.|||I-type; undeformed, massive, medium-grained hornblende granodiorite with smaller bodies of diorite, dacite, pegmatite and aplite; porphyritic granodiorite dykes; sills and dykes of subalkaline hornblende-phyric monzodiorite.|
18127|Tibooburra Granodiorite|67209|5|Briefly described|Map legend.|Silurian|Silurian|||Unit in Tibooburra Suite.|||Massive, weakly porphyritic, strongly jointed medium-grained seriate granodiorite; lesser massive, very coarse-grained pegmatite comprising quartz and K-feldspar with subordinate plagioclase, muscovite and tourmaline.|
18127|Tibooburra Granodiorite|68823|6|Mentioned|p385||||c.428 Ma.|||Intrudes the Warratta Group.||
18127|Tibooburra Granodiorite|70649|5|Briefly described|Map Legend|Silurian|Silurian|||Tibooburra Suite|||Massive, weakly porphyritic, strongly jointed medium-grained seriate granodiorite.|
18127|Tibooburra Granodiorite|70652|5|Briefly described|Map Legend|Silurian|Silurian|||Tibooburra Suite|||Massive, weakly porphyritic, strongly jointed medium-grained seriate granodiorite.|
18127|Tibooburra Granodiorite|71262|6|Mentioned|p5 Fig 2|||See also Tibooburra Granite, Fig 6.||||||
18127|Tibooburra Granodiorite|71415|5|Briefly described|p11,16|Silurian|Silurian|Geological province: SW Thomson Orogen. Of the Kooneberry Belt; of Eromanga Basin. I-type granodiorite. Intruded into Warratta Group sediments  (Greenfield, Gilmore and Mills 2010).|420.6+\-3.3 Ma|Unit of Tibooburra Suite.||||
18127|Tibooburra Granodiorite|71965|4|Described|p897,909|Pridoli|Pridoli|Geological province: Thomson Orogen. Well-exposed I-type granite in the southern Thomson Orogen. Emplaced/intruded into Easter Monday Formation at 420.6+\-3.3 Ma (Black, 2007; Vickery, 2010).|420.6+\-3.3 Ma (emplacement)|Unit of Tibooburra Suite.||Inrudes into the Easter Monday Formation.|Mesocratic, medium-grained quartz-plagioclase-biotite-hornblende granodiorite.|
18127|Tibooburra Granodiorite|72522|4|Described|p3, p119, p125, p131.|Lochkovian|Late Silurian|Emplacement age (Black, 2007 and Vickery, 2010).|420.6 +/- 3.3 Ma|Tibooburra Suite||Intrudes Easter Monday Formation.|I-type quartz-feldspar-biotite-hornblende granodiorite.|24-FEB-21
18127|Tibooburra Granodiorite|72951|5|Briefly described|p1013, 1019, 1024|Lochkovian|Ludlow|Thomson Orogen, southwest. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -1.8 +/- 0.5, and d18O = 6.51 +/- 0.21.|420.5 +/- 3.2 Ma, 420.6 +/- 3.2 Ma|Tibooburra Suite|||Medium-grained granodiorite.|
18134|Tidbinbilla Quartzite|12185|5|Briefly described|map legend|Silurian|Silurian|Sandstone, quartzite, thin limestone and shale, sedimentary breccia. BMR map symbol: St.||||||
18134|Tidbinbilla Quartzite|22857|4|Described|p420 App. 1, Tb. A1.5|Wenlockian|Llandovery|Only locally developed. Quartz, minor shale, chert, conglomerate and quartzite pebbles. Max. thickness: 300m.||||||
18134|Tidbinbilla Quartzite|24551|5|Briefly described|p103|||Large lens of clean quartzite with in the late Eastonian portion of the Warbisco Shale.||||||
18134|Tidbinbilla Quartzite|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
18134|Tidbinbilla Quartzite|29994|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
18134|Tidbinbilla Quartzite|30332|6|Mentioned|p127|||||||||
18134|Tidbinbilla Quartzite|31019|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
18134|Tidbinbilla Quartzite|31581|6|Mentioned|Fig. 1|||||||||
18134|Tidbinbilla Quartzite|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
18134|Tidbinbilla Quartzite|32672|6|Mentioned|p672|||||||||
18134|Tidbinbilla Quartzite|33325|5|Briefly described|Table 2|||? late Wenlockian or ? early Ludlovian P13.||||||
18134|Tidbinbilla Quartzite|34405|4|Described|p114|||||||||
18134|Tidbinbilla Quartzite|36441|5|Briefly described|map legend|Wenlockian|Llandoverian|Massive to thin-bedded quartz arenite and quartzite; minor shale. Intruded by Cow Flat Granite Porphyry; unconformably overlies Adaminaby Beds. Basal coarse gritstone. BMR map code: St.||||||
18134|Tidbinbilla Quartzite|36443|5|Briefly described|map legend|Late Silurian|Early Silurian|Conglomerate, formed of chert and quartzite pebbles. BMR map code: St.||||||
18134|Tidbinbilla Quartzite|37727|4|Described|p88|||See also P17.||||||
18134|Tidbinbilla Quartzite|39800|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
18134|Tidbinbilla Quartzite|40328|4|Described|p123|||||||||
18134|Tidbinbilla Quartzite|42497|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
18134|Tidbinbilla Quartzite|42820|5|Briefly described|p7|||||||||
18134|Tidbinbilla Quartzite|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|St1||||||
18134|Tidbinbilla Quartzite|44093|5|Briefly described|p190 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
18134|Tidbinbilla Quartzite|44970|14|Not recorded|p22|||See also Lexicon||||||
18134|Tidbinbilla Quartzite|45147|2|Defined|M114|early Wenlockian|late Llandoverian|Late Llandoverian to Early Wenlockian||||||
18134|Tidbinbilla Quartzite|60078|6|Mentioned|Map Legend|Late Silurian|Early Silurian|||||||
18134|Tidbinbilla Quartzite|67322|5|Briefly described|p16|Silurian|Silurian|300m thick lenticular unit. A Silurian age has been suggested based on lithological similarity to sandstones of the Yalmy Group. Occurs in the Brindabella Ranges.||||Intercalated within the Warbisco Shale. Equivalent to the Black Mountain Sandstone.|Very clean sandstone.|22-FEB-18
18134|Tidbinbilla Quartzite|71700|6|Mentioned|CD|||This unit is more than 300m thick and believed to be analagous to the Warbisco Shale west of Rugby in Boorowa100.||||||
18146|Tiger Snake Igneous Complex|40246|6|Mentioned|p166|||||||||
18147|Tighes Hill Formation|22578|6|Mentioned|p401|||||||||
18147|Tighes Hill Formation|29922|6|Mentioned|Appendix 4|||||||||
18147|Tighes Hill Formation|29926|6|Mentioned|Fig.3|||||||||
18147|Tighes Hill Formation|34351|5|Briefly described|p343|||||||||
18147|Tighes Hill Formation|37083|6|Mentioned|p164|||||||||
18147|Tighes Hill Formation|39292|6|Mentioned|Fig. 6.2|||||||||
18147|Tighes Hill Formation|39308|6|Mentioned|Fig. 23.4|||||||||
18147|Tighes Hill Formation|39609|5|Briefly described|p2|||||||||
18147|Tighes Hill Formation|41479|6|Mentioned|Fig.2|||||||||
18147|Tighes Hill Formation|43447|14|Not recorded|diag.p26,34|||Part of Lambton Sub-Group||||||
18147|Tighes Hill Formation|45090|6|Mentioned|p187|||Refers McKenzie (1962)||||||
18147|Tighes Hill Formation|68711|6|Mentioned|p116 Tbl 2|||This name has been dropped. See also p113.||Of Lambton Subgroup|Included Ferndale Conglomerate Member.|||
18148|Tilbuster Granodiorite|23720|5|Briefly described|Map Legend|||Of Uralla Plutonic Suite.  Augite-bronzite-hornblende-biotite granodiorite.||||||15-DEC-04
18148|Tilbuster Granodiorite|24366|6|Mentioned|p13|||||||||
18148|Tilbuster Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
18148|Tilbuster Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
18148|Tilbuster Granodiorite|38288|6|Mentioned|Fig.4|||||||||
18148|Tilbuster Granodiorite|42866|5|Briefly described|Table 2, P12|||||||||
18148|Tilbuster Granodiorite|44450|5|Briefly described|p98|||Geological Province: New England Fold Belt||||||
18148|Tilbuster Granodiorite|71628|4|Described|p8: 33-34, 36, 39, 106-110|||Binns et al. (1967) after work by Neilson (1970; unpublished). Named after Tilbuster homestead. A small (20 km2) intrusion 6km N of Armidale. Poor outcrop; forms large rounded tors. Age from intruded Mount Duval Monzogranite (252.8 Ma). Limited geochemistry described. Spatially associated with historically significant Au-Sb-As vein mineralisation, but it is doubted the source is from this unit.|c.253 Ma (maximum emplacement age).|Tilbuster Suite.||Intrudes Mount Duval Monzogranite, Dummy Creek Conglomerate and Sandon beds.|Grey, medium-grained, equigranular, hornblende-biotite-(pyroxene) granodiorite; fine-grained porphyritic marginal variant; minor silexite. I-type.|
18177|Timbury Hills Formation|22768|6|Mentioned|p153,159||Early Devonian|||||||
18177|Timbury Hills Formation|22857|5|Briefly described|p153|Early Devonian|?Early Devonian|Possibly correlates with Cobar Supergroup. See also p165 Fig. 16.6.||||||
18177|Timbury Hills Formation|24069|5|Briefly described|p282|Late Devonian|Late Devonian|Geological Province: Surat Basin.||||||
18177|Timbury Hills Formation|24075|5|Briefly described|p393|||Geological Province: Drummond Basin.||||||
18177|Timbury Hills Formation|29413|6|Mentioned|p295|||||||||
18177|Timbury Hills Formation|29488|6|Mentioned|p7|||||||||
18177|Timbury Hills Formation|29721|6|Mentioned|p69|||||||||
18177|Timbury Hills Formation|30692|6|Mentioned|Map legend|Early Paleozoic|Early Paleozoic|||||||07-NOV-08
18177|Timbury Hills Formation|30699|6|Mentioned|p55|||Map||||||
18177|Timbury Hills Formation|31369|6|Mentioned|p11|||Devonian||||||
18177|Timbury Hills Formation|31999|5|Briefly described|p136|||Table 1||||||
18177|Timbury Hills Formation|32578|5|Briefly described|p347|||Dev. Stratigraphy Roma area||||||
18177|Timbury Hills Formation|32712|6|Mentioned|Table 1|||||||||
18177|Timbury Hills Formation|33059|4|Described|Table 1|||Dev.||||||
18177|Timbury Hills Formation|33530|5|Briefly described|Table 1|||||||||
18177|Timbury Hills Formation|33672|6|Mentioned|p41|||||||||
18177|Timbury Hills Formation|33745|6|Mentioned|p205|||Devonian.||||||
18177|Timbury Hills Formation|34133|6|Mentioned|p29|||||||||
18177|Timbury Hills Formation|34212|6|Mentioned|p2|||See also P3. Devonian.||||||
18177|Timbury Hills Formation|36104|6|Mentioned|p122|||||||||
18177|Timbury Hills Formation|36233|5|Briefly described|Table 1|||||||||
18177|Timbury Hills Formation|36739|6|Mentioned|p22|||||||||
18177|Timbury Hills Formation|37450|6|Mentioned|p366|||||||||
18177|Timbury Hills Formation|37724|6|Mentioned|Fig.5|||||||||
18177|Timbury Hills Formation|39273|6|Mentioned|Fig. 2|||||||||
18177|Timbury Hills Formation|40030|6|Mentioned|p139|||||||||
18177|Timbury Hills Formation|40541|3|Fully described|p104|||||||||
18177|Timbury Hills Formation|40666|4|Described|p353|||||||||
18177|Timbury Hills Formation|40787|4|Described|p341|||||||||
18177|Timbury Hills Formation|41210|6|Mentioned|Fig.16|||||||||
18177|Timbury Hills Formation|41725|6|Mentioned|p403|||||||||
18177|Timbury Hills Formation|42031|4|Described|p766|||||||||
18177|Timbury Hills Formation|42041|6|Mentioned|Fig.4 P223|||||||||
18177|Timbury Hills Formation|42634|6|Mentioned|Fig.7 P26|||||||||
18177|Timbury Hills Formation|42987|4|Described|p19|||says unit can't have Formation status under the Australian Code of Stratigraphic Nomenclature||||||
18177|Timbury Hills Formation|42996|5|Briefly described|p14|||||||||
18177|Timbury Hills Formation|43000|5|Briefly described|p106|||||||||
18177|Timbury Hills Formation|43003|5|Briefly described|p167|||||||||
18177|Timbury Hills Formation|43007|5|Briefly described|Fig.2,p255|||||||||
18177|Timbury Hills Formation|43008|5|Briefly described|map legend|||||||||
18177|Timbury Hills Formation|43213|6|Mentioned|p61-63|Devonian|Devonian|Finlayson et al.(1990). Near the W edge of this unit, the Foyleview Geosuture - a major W-dipping detachment - marks the E edge of the Thomson Fold Belt.||||||
18177|Timbury Hills Formation|43461|14|Not recorded|p616,617|||Equivalent to Telemon and Mount Rankin Formations||||||
18177|Timbury Hills Formation|44023|5|Briefly described|Tb.2,p6||Late Devonian|||||||
18177|Timbury Hills Formation|44091|14|Not recorded|p39||Carboniferous|||||||
18177|Timbury Hills Formation|44115|14|Not recorded|p17-19,24|||||||||
18177|Timbury Hills Formation|44116|14|Not recorded|p24,28|||||||||
18177|Timbury Hills Formation|44118|14|Not recorded|Map Legend||Late Devonian|||||||
18177|Timbury Hills Formation|44163|14|Not recorded|p11|||||||||
18177|Timbury Hills Formation|44169|2|Defined|Tb.1,6,7,map|||||||||
18177|Timbury Hills Formation|44170|4|Described|p5-7,30,Tb.1||Late Devonian|||||||
18177|Timbury Hills Formation|44172|14|Not recorded|p1326,1329,1331,Tb.1||Devonian|||||||
18177|Timbury Hills Formation|44173|14|Not recorded|p112|||||||||
18177|Timbury Hills Formation|44422|14|Not recorded|p148,151-153,155||Devonian|Basement.||||||
18177|Timbury Hills Formation|44423|14|Not recorded|p20-22|||(Dev?Early Carb?Perm?)||||||
18177|Timbury Hills Formation|44585|14|Not recorded|p45-Fig.2|||||||||
18177|Timbury Hills Formation|44610|14|Not recorded|Fig.7|||||||||
18177|Timbury Hills Formation|44627|14|Not recorded|p139|||||||||
18177|Timbury Hills Formation|44636|14|Not recorded|p162|Early Devonian|Late Silurian|||||||
18177|Timbury Hills Formation|44646|14|Not recorded|p1|||Tarrawanga No.2.||||||
18177|Timbury Hills Formation|44686|14|Not recorded|p1-6,16|||||||||
18177|Timbury Hills Formation|44701|14|Not recorded|Tb.VI|||Dirinda 1||||||
18177|Timbury Hills Formation|44787|14|Not recorded|Tb.p123,125-127,diag||Late Devonian|||||||
18177|Timbury Hills Formation|44842|14|Not recorded|p13|||||||||
18177|Timbury Hills Formation|44897|14|Not recorded|p8,16|||||||||
18177|Timbury Hills Formation|45071|6|Mentioned|p45|||||||||
18177|Timbury Hills Formation|45095|6|Mentioned|p4|||||||||
18177|Timbury Hills Formation|45110|4|Described|p25|||See also P66.||||||
18177|Timbury Hills Formation|46989|6|Mentioned|p215|||||||||
18177|Timbury Hills Formation|48585|4|Described|p1,7,12-15,Pl.1|||||||||
18177|Timbury Hills Formation|48600|14|Not recorded|Plate 3|||||||||
18177|Timbury Hills Formation|48606|14|Not recorded|p3,5,6,11,13,14,22|||(H/55-8 ; G/55-12). Pl.1 sh.2, Pl.2.||||||
18177|Timbury Hills Formation|48611|14|Not recorded|p8,16,Fig.2|||||||||
18177|Timbury Hills Formation|48920|6|Mentioned|p85|||||||||
18177|Timbury Hills Formation|64855|4|Described|p16 Fig.2, p18-22, 36|Early Carboniferous|Devonian|Fine grained, quartz rich metasedimentary rocks of the Thomson and Lachlan fold belts, forming part of the basement to the Bowen Basin. Min age based on the Upper Devonian/Lower Carboniferous Roma granites that intrude this formation.||||||22-FEB-10
18177|Timbury Hills Formation|64856|5|Briefly described|p43, p46, p63, p74|Devonian|Devonian|Unconformably underlies Combarngo Volcanics,  Arbroath beds, Muggleton Formation. Considered part of source for Showgrounds Sandstone.|| ||||29-NOV-17
18177|Timbury Hills Formation|65115|6|Mentioned|p407|Devonian|Devonian|Intercepted in  AAO Glentulloch 1.||||||
18177|Timbury Hills Formation|67669|5|Briefly described|p11-12,22-23|Late Carboniferous|Late Carboniferous|Of Bowen Basin. Part of the basement assemblage to the Bowen Basin. Low-grade metasedimentary rocks in the Roma region. Intersected in Myall Creek-1 borehole at 2.1 km depth, and represents basement as modelled on Line 270.||||Overlain by Reid Dome beds, Lizzie Creek, Cmbarngo and Bulgonunna volcanics. Underlain by, and laterally grades into Kuttung Formation. Intruded by Roma granites.||
18177|Timbury Hills Formation|68679|5|Briefly described|p371-372|Devonian|Devonian|Murray (1994). Basement to the Bowen Basin in the Roma area. Possibly turbidites.||||Is intruded by the Roma granites.|Includes quartzose sandstone, siltstone and cleaved argillite. Metamorphosed to lower greenschist grade.|
18177|Timbury Hills Formation|68731|5|Briefly described|p164, p168, p213 Fig 3.118|Devonian|Devonian|Generally steeply dipping with usually a single slaty cleavage and regional low-grade metamorphism.|||||Consists of turbiditic quartzose sandstone and mudstone deposited in a deep-marine environment.|
18177|Timbury Hills Formation|69582|5|Briefly described|p32, p34-p35, p38|Devonian|Devonian|Surat Basin. Forms basement in the Roma Shelf. Undergone folding producing upright, tight to isoclinal folds. Metamorphosed to greenschist facies. Deposited in a deep marine environment. Intruded by the Roma granites. Interpreted to extend to at least 5km depth.|||||Steeply dipping metasediments including turbiditic quartzose sandstone and mudstone.|
18177|Timbury Hills Formation|69592|6|Mentioned|p229|Devonian||Roma area. An extensive, subsurface, metasedimentary unit; intruded by the c.356 Ma Roma granites.||||||
18177|Timbury Hills Formation|70033|6|Mentioned|p1-2|||See informal Timbury Hills formation for Geochron age.||||||
18177|Timbury Hills Formation|70673|4|Described|p3, p10, p62, p64, p66-70|Devonian|Devonian|Roma Shelf. Metamorphosed, deep-marine sedimentary rocks. Devonian age from plant fossils. Metamorphosed at 360 +/- 8 Ma. Previous determination gives a MDA of 417.6 +/- 3.1 Ma (Kositcin et al., 2015).|401 +/- 7 Ma (maximum depositional age).|||Intruded by Roma Granites.|Interbedded sandstone, siltstone and argillite metamorphosed to lower greenschist facies. Includes garnet-muscovite-biotite paragneiss. Has volcanic horizon(s).|
18177|Timbury Hills Formation|71592|5|Briefly described|Appendix A.|||Roma Shelf, Surat Basin. Metamorphosed at 360 +/- 8 Ma (U-Pb zircon SHRIMP).|401+/-7 Ma (MDA: U-Pb zircon SHRIMP)||||Gneiss.|
18177|Timbury Hills Formation|71965|5|Briefly described|p912,914|Middle Devonian|Early Devonian|Of Roma Shelf. Proposed to be correlable to Glenroy Formation in the Thomson Orogen. Underwent folding and metamorphism.||||||
18177|Timbury Hills Formation|72522|5|Briefly described|p98-104, p105, 107.||Early Devonian|Eastern Lachlan Orogen. Maximum depositional age determined from AAO Glenroy 1, in Roma region. Previous U-Pb SHRIMP max. dep. age dating from  a metasandstone in AAO Timbury Hills 2: 420+/-4 Ma. Another sample dated herein (2172124) at 388+/-5 Ma from UOD Weribone 1 , and originally interpreted as Timbury Hills Formation, is now interpreted as a younger Thomson Orogen unit.|412+/-6 Ma U-Pb SHRIMP.(Max dep age)||||Dated sample is grey-green, medium-grained quartzite.|24-FEB-21
18177|Timbury Hills Formation|73600|6|Mentioned|p203|||Roma Shelf. Characterised by the Pacific-Gondwanan detrital zircon ages.||||||
18183|Timor Limestone Member|22768|6|Mentioned|p183||Givetian|||||||
18183|Timor Limestone Member|22857|5|Briefly described|p482 App.1 Tb.A1.6|Givetian|Givetian|Of the Yarrimie Formation (Tamworth Group). Max. thickness: 360m. Geological Province: Tamworth Forearc Basin. See also p183 (photo #3).||||||
18183|Timor Limestone Member|23185|6|Mentioned|Fig5p161|Givetian|Eifelian|||||||
18183|Timor Limestone Member|23522|5|Briefly described|p249 Fig 5|Givetian|Eifelian|||||||
18183|Timor Limestone Member|30650|6|Mentioned|p315|||Refers Ellenor (1975)||||||
18183|Timor Limestone Member|30814|6|Mentioned|p71|||||||||
18183|Timor Limestone Member|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
18183|Timor Limestone Member|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
18183|Timor Limestone Member|32619|6|Mentioned|p457|||See also P461. Fauna. M.Dev.||||||
18183|Timor Limestone Member|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
18183|Timor Limestone Member|34554|4|Described|p234|||||||||
18183|Timor Limestone Member|35193|6|Mentioned|p23|||||||||
18183|Timor Limestone Member|40867|6|Mentioned|p55|||||||||
18183|Timor Limestone Member|43407|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition) Part of Yarrimie Formation of Tamworth Group||||||
18183|Timor Limestone Member|43428|14|Not recorded|p139||Givetian|fauna listed||||||
18183|Timor Limestone Member|65214|6|Mentioned|p278|Devonian|Devonian|NSW, Timor. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
18183|Timor Limestone Member|68005|5|Briefly described|p52, p150.|Middle Devonian|Middle Devonian|This name is used in the Loombrah and Timor region for a unit which, in the Attunga region, is called the Moore Creek Limestone. The rank 'Member' is omitted on p52.||Unit in Yarrimie Formation.|||Grey fossiliferous bioclastic limestone with local basal conglomerate, three cherty intervals and jasperoid nodules.|
18183|Timor Limestone Member|68006|6|Mentioned|p114.|Early Devonian|Early Devonian|||Unit in Tamworth Group.||||
18200|Tinderra Granite|730|6|Mentioned|p16, p20, p36.|Early Devonian|Early Devonian|Cobar area. K-Ar age of 403 Ma. May coalesce at depth with Wilgaroon Granite. Within the Omeo - Doradilla "tin belt".||||||11-NOV-14
18200|Tinderra Granite|23171|5|Briefly described|p12,16,18||Pridoli|Max Age: 410 Ma (K-Ar).||||||
18200|Tinderra Granite|23173|4|Described|Map Legend|Ludlovian|Ludlovian|||||||
18200|Tinderra Granite|29621|4|Described|p4|||||||||
18200|Tinderra Granite|30683|6|Mentioned|Table 1|||||||||
18200|Tinderra Granite|33342|5|Briefly described|p176|||Refers Longman & Meares (1972).||||||
18200|Tinderra Granite|34057|6|Mentioned|Map legend|Silurian|Silurian|||||||
18200|Tinderra Granite|34449|6|Mentioned|Table 2-1|||||||||
18200|Tinderra Granite|35287|5|Briefly described|p3|||||||||
18200|Tinderra Granite|35383|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
18200|Tinderra Granite|35385|3|Fully described|p16|||||||||
18200|Tinderra Granite|36411|6|Mentioned|p270|||Refers Baker 1978 for definition.||||||
18200|Tinderra Granite|37936|6|Mentioned|Fig.2|||||||||
18200|Tinderra Granite|38292|6|Mentioned|p3|||||||||
18200|Tinderra Granite|39083|6|Mentioned|p30|||||||||
18200|Tinderra Granite|39084|6|Mentioned|p19|||||||||
18200|Tinderra Granite|39214|6|Mentioned|Table 11|||||||||
18200|Tinderra Granite|39627|5|Briefly described|p266|||||||||
18200|Tinderra Granite|39683|6|Mentioned|Fig.3|||||||||
18200|Tinderra Granite|40328|4|Described|p211|||||||||
18200|Tinderra Granite|41821|6|Mentioned|p5 Fig.3|||Occurs in Cobar sheet area||||||
18200|Tinderra Granite|42467|5|Briefly described|Map Legend|||||||||
18200|Tinderra Granite|42566|6|Mentioned|p25|||||||||
18200|Tinderra Granite|42726|5|Briefly described|map legend|Silurian||||||||
18200|Tinderra Granite|43032|5|Briefly described|Table 1.|||||||||
18200|Tinderra Granite|43153|5|Briefly described|Map Legend|Silurian|Ordovician|||||||
18200|Tinderra Granite|43398|14|Not recorded|Map Legend||Silurian|||||||
18200|Tinderra Granite|43757|6|Mentioned|p510|||||||||
18200|Tinderra Granite|43774|3|Fully described|12-13||Silurian|Age: 403+/-10 Ma, 410+/-10 Ma||||||
18200|Tinderra Granite|45003|14|Not recorded|p20|||See also Lexicon||||||
18200|Tinderra Granite|46900|6|Mentioned|Fig.2|||Stratigraphic table||||||
18200|Tinderra Granite|46967|6|Mentioned|Fig.4|||||||||
18200|Tinderra Granite|68823|5|Briefly described|p376 Fig.3, p377|Emsian|Pridoli||410 +/- 10 Ma, K-Ar (Pogson and Hilyard 1981)|||||
18200|Tinderra Granite|71345|6|Mentioned|p25|||Lloyd 1937 suggested the Wilgaroon Granite and Tinderra Granite are part of the same batholith.||||||
18200|Tinderra Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|Ungrouped S-type intrusion.|||||Massive to foliated medium-grained muscovite-biotite granite.|
18207|Tingaringy Granodiorite|22815|4|Described|p54|Early Devonian|Silurian|Rb/Sr Age: 412+/- 3.7 Ma.||||||
18207|Tingaringy Granodiorite|33852|6|Mentioned|Fig.2|||Date on Table 1||||||
18207|Tingaringy Granodiorite|40328|4|Described|p211|||||||||
18207|Tingaringy Granodiorite|41905|2|Defined|p42|Early Silurian||||||||
18207|Tingaringy Granodiorite|41933|5|Briefly described|Map legend|Late Silurian||||||||
18207|Tingaringy Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Tingaringy Suite.||||||
18207|Tingaringy Granodiorite|49705|6|Mentioned|p17|||||||||
18208|Tingaringy Suite|22815|5|Briefly described|p54|Early Devonian|Silurian|||||||
18208|Tingaringy Suite|41905|5|Briefly described|p42|||||||||
18208|Tingaringy Suite|41933|5|Briefly described|Map legend|Late Silurian||||||||
18208|Tingaringy Suite|43233|5|Briefly described|Map Legend|Late Silurian||of Berridale Batholith.||||||
18212|Tingira Conglomerate Member|23055|6|Mentioned|Fig13p25|||||||||
18212|Tingira Conglomerate Member|29922|6|Mentioned|p49|||||||||
18212|Tingira Conglomerate Member|29926|6|Mentioned|p2|||||||||
18212|Tingira Conglomerate Member|33867|6|Mentioned|Fig.3|||||||||
18212|Tingira Conglomerate Member|34351|6|Mentioned|Fig.5.13|||Proposed name change from Violet Town Conglomerate||||||
18212|Tingira Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
18212|Tingira Conglomerate Member|39308|6|Mentioned|Fig. 23.4|||||||||
18212|Tingira Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
18212|Tingira Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Glebe Formation||||
18216|Tinkers Creek Granodiorite|40328|4|Described|p211|||||||||
18216|Tinkers Creek Granodiorite|60007|5|Briefly described|Map legend|Middle Devonian|Early Devonian|Of the Berridale Batholith.  Medium-grained, grey granodiorite with numerous xenoliths.||||||
18219|Tinonee beds|41348|5|Briefly described|Map legend|Carboniferous|Devonian|In the Hastings Block.||||||16-DEC-04
18250|Toaks Creek Conglomerate|23309|5|Briefly described|p89-97 Table 2.32|||||||||
18250|Toaks Creek Conglomerate|24551|4|Described|p136, p137|||Of the Wombat Creek Group.||||||
18250|Toaks Creek Conglomerate|38151|2|Defined|p38|Pridolian|Ludlovian|Pridolian to Ludlovian||||||
18250|Toaks Creek Conglomerate|39221|4|Described|p263|||||||||
18250|Toaks Creek Conglomerate|41585|4|Described|p124|||||||||
18250|Toaks Creek Conglomerate|42827|5|Briefly described|p124|||of Wombat Creek Group||||||
18250|Toaks Creek Conglomerate|60503|3|Fully described|p99, p15, p30|Early Silurian|Early Silurian|Of the Wombat Creek Group. Conglomerate deposited as fanglomerates; abundant rhyolite pebbles. Conformably overlies Undowah Siltstone;conformably overlain by Gibbo River Siltstone.||||||16-NOV-09
18250|Toaks Creek Conglomerate|60504|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Wombat Creek Group. Conglomerate; massive to crudely bedded, with high portion of rhyolite and porphyry clasts in lower part; minor sandstone lenses.||||||20-OCT-04
18250|Toaks Creek Conglomerate|60505|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Wombat Creek Group. Conglomerate; massive to crudely bedded, with high portion of rhyolite and porphyry clasts in lower part; minor sandstone lenses.||||||
18250|Toaks Creek Conglomerate|60506|5|Briefly described|Map legend|Pridoli|Pridoli|Of the Wombat Creek Group. Conglomerate; massive to crudely bedded, with high portion of rhyolite and porphyry clasts in lower part; minor sandstone lenses.||||||20-OCT-04
18250|Toaks Creek Conglomerate|60507|5|Briefly described|Map Legend|Pridoli|Pridoli|Of the Wombat Creek Group. Conglomerate; massive to crudely bedded, with high portion of rhyolite and porphyry clasts in lower part; minor sandstone lenses.||||||20-OCT-04
18250|Toaks Creek Conglomerate|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Of the Wombat Creek Group. Conglomerate: nonmagnetic (0-5nT); low total count, K, Th, U||||||08-NOV-04
18250|Toaks Creek Conglomerate|61161|6|Mentioned|p148, p153|Late Silurian|Late Silurian|||||||
18250|Toaks Creek Conglomerate|68116|5|Briefly described|Appendix, Map 27.|Pridoli|Ludlow||||||Pebble conglomerate: massive to crudely bedded, clasts well rounded; with high proportion of rhyolite and porphyry clasts in lower part; minor sandstone lenses.|
18250|Toaks Creek Conglomerate|71040|6|Mentioned|p10 Fig.6|Silurian|Silurian|||||||
18255|Tocumwal Granite|22857|5|Briefly described|p213|Devonian|Devonian|S-type, unfractionated and porhyritic. Geological Province: Barka Province.||||||
18255|Tocumwal Granite|22859|5|Briefly described|p213|||||||||
18255|Tocumwal Granite|23275|6|Mentioned|Fig14-7.7p472||Silurian|||||||
18255|Tocumwal Granite|24328|5|Briefly described|Map legend|Middle Devonian|Middle Devonian|||||||
18255|Tocumwal Granite|30909|6|Mentioned|Map legend|Silurian|Silurian|Prob. Silurian||||||
18255|Tocumwal Granite|33553|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
18255|Tocumwal Granite|40328|4|Described|p211|||||||||
18255|Tocumwal Granite|42726|5|Briefly described|map legend|Late Devonian|Middle Devonian|||||||
18255|Tocumwal Granite|44340|14|Not recorded|p.5|||I/55-14.||||||
18255|Tocumwal Granite|44341|14|Not recorded|map legend|||Upper Silurian?||||||
18255|Tocumwal Granite|45087|5|Briefly described|p28|||Chemical analyses.||||||
18267|Toll Bar Formation|32482|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
18267|Toll Bar Formation|43407|14|Not recorded|Map Legend||Late Permian|(Provisional Edition)||||||
18267|Toll Bar Formation|61201|4|Described|p2, 5 Table 1, 6-7|Late Permian|Late Permian|Geological Province: Werrie Basin. Max. Thickness: 600m+. Claystone, lithic sandstone, conglomerate, limestone. Previously known as Toll Bar Group. Overlies: Borambil Creek Formation.||||||
18267|Toll Bar Formation|61776|5|Briefly described|p194 Fig. 3|Late Permian|Late Permian|Geological Province: Werrie Basin. Claystone, lithic sandstone, conglomerate and limestone.||||||
18267|Toll Bar Formation|68003|5|Briefly described|p38 Fig.3-j, p41, p42, p129.|Late Permian|Late Permian|Werrie Basin (North), Brigalow Belt South Bioregion. Coeval with upper part of Bickham Formation in the south of the Basin.||||Overlies Borambil Creek Formation. Is unconformably overlain by Digby Formation.|Claystone, lithic sandstone, conglomerate, limestone.|
18267|Toll Bar Formation|70036|5|Briefly described|Map legend|Permian|Permian|Included in a mapped unit of Late Permian marine sequences: conglomerate, quartzose sandstone, siltstone, calcareous mudstone and limestone.||||||
18267|Toll Bar Formation|70791|5|Briefly described|p277|Permian|Permian|Werrie Basin (north).||Singleton Supergroup.||||
18286|Tom Groggin Suite|22508|6|Mentioned|p13, map|||Lachlan Fold Belt||||||
18286|Tom Groggin Suite|23439|5|Briefly described|p124 fig.1|||||||||
18286|Tom Groggin Suite|24133|5|Briefly described|p65|||Geological Province: Lachlan Fold Belt.||||||
18286|Tom Groggin Suite|24551|6|Mentioned|p233|||||||||
18286|Tom Groggin Suite|41563|6|Mentioned|p515|||||||||
18286|Tom Groggin Suite|42726|5|Briefly described|Map Legend||Silurian|||||||
18286|Tom Groggin Suite|44093|5|Briefly described|p171 App. 1|Silurian|Silurian|In the Wagga-Omeo Zone. Geological Province: Lachlan Fold Belt.||||||29-MAR-05
18286|Tom Groggin Suite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|Includes: Ganmain Granite, Wantabadgery Granite.||||||14-FEB-05
18286|Tom Groggin Suite|69801|6|Mentioned|p39, p110, p135|||Central Lachlan Orogen.||Koetong Supersuite|Includes the Ganmain Granite and the Green Hills Granodiorite.|||
18286|Tom Groggin Suite|72571|5|Briefly described|p90, p93|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail.|||Includes the Wantabadgery Granite.||Biotite granite and muscovite granite.|
18289|Tomago Coal Measures|22516|6|Mentioned|p15||Late Permian|||||||
18289|Tomago Coal Measures|22578|5|Briefly described|p391, Fig.5 p395||Late Permian|||||||
18289|Tomago Coal Measures|22601|6|Mentioned|417, 419|Permian|Permian|||||||
18289|Tomago Coal Measures|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Contains the Dempsey, Four Mile Creek and Wallis Creek Formations. Geological Province: Sydney Basin.||||||
18289|Tomago Coal Measures|22969|4|Described|p4, 23||Late Permian|||||||
18289|Tomago Coal Measures|22970|5|Briefly described|Plate 6||Permian|||||||
18289|Tomago Coal Measures|23055|6|Mentioned|Fig4p11,Fig11p23,36|||||||||
18289|Tomago Coal Measures|23214|6|Mentioned|p267|||||||||
18289|Tomago Coal Measures|23438|6|Mentioned|p25|||||||||
18289|Tomago Coal Measures|23450|6|Mentioned|p527 Fig.1|||||||||
18289|Tomago Coal Measures|23540|5|Briefly described|p 417|||||||||
18289|Tomago Coal Measures|23544|5|Briefly described|p372|||In the Sydney Basin.||||||22-MAY-08
18289|Tomago Coal Measures|24040|5|Briefly described|p470 Fig.2, p484|Late Permian|Late Permian|Geological Province: Lachlan Fold Belt.||||||21-AUG-08
18289|Tomago Coal Measures|24079|5|Briefly described|p432|Permian|Permian|Geological Province: Sydney Basin.||||||
18289|Tomago Coal Measures|24121|5|Briefly described|p4, p30, 73, 148|Permian|Permian|||||||25-AUG-22
18289|Tomago Coal Measures|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Overlying Unit: Waratah Sandstone. Geological Province: Sydney Basin||||||
18289|Tomago Coal Measures|24158|5|Briefly described|p170|||Grades up into Newcastle Coal Measures. See also p173 Fig.4 (caption). Geological Province: Sydney Basin||||||
18289|Tomago Coal Measures|29748|6|Mentioned|Fig.3|||||||||
18289|Tomago Coal Measures|29826|6|Mentioned|p18|||||||||
18289|Tomago Coal Measures|29827|6|Mentioned|p20|||||||||
18289|Tomago Coal Measures|29922|6|Mentioned|Appendix 3|||||||||
18289|Tomago Coal Measures|29926|6|Mentioned|p2|||||||||
18289|Tomago Coal Measures|29941|6|Mentioned|p13|||||||||
18289|Tomago Coal Measures|29942|6|Mentioned|p11|||||||||
18289|Tomago Coal Measures|30005|6|Mentioned|p81|||||||||
18289|Tomago Coal Measures|30340|6|Mentioned|Table 3|||||||||
18289|Tomago Coal Measures|30341|6|Mentioned|p136|||Upper Permian age||||||
18289|Tomago Coal Measures|30450|6|Mentioned|Table 1|||Permian. Sydney Basin||||||
18289|Tomago Coal Measures|30545|6|Mentioned|Fig.2|||Tatarian||||||
18289|Tomago Coal Measures|30547|6|Mentioned|p426|||Correlation of Upper Permian and Lower Triassic||||||
18289|Tomago Coal Measures|30555|6|Mentioned|Fig.21.5|||||||||
18289|Tomago Coal Measures|30622|6|Mentioned|p12|||||||||
18289|Tomago Coal Measures|30743|6|Mentioned|p32|||Upper Permian age. Correlation||||||
18289|Tomago Coal Measures|31124|6|Mentioned|p17|||Equivalent in age to Singleton C.M.||||||
18289|Tomago Coal Measures|31125|6|Mentioned|p16|||Geology||||||
18289|Tomago Coal Measures|31559|4|Described|p153|||||||||
18289|Tomago Coal Measures|31621|6|Mentioned|p151|||||||||
18289|Tomago Coal Measures|31649|6|Mentioned|p59|||||||||
18289|Tomago Coal Measures|31706|6|Mentioned|p657|||Permian correlation chart||||||
18289|Tomago Coal Measures|31855|6|Mentioned|p14|||Stratigraphic table||||||
18289|Tomago Coal Measures|31883|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|31885|6|Mentioned|p1439|||Table 1. Refers Robinson (1969)||||||
18289|Tomago Coal Measures|31887|6|Mentioned|p3|||||||||
18289|Tomago Coal Measures|32266|6|Mentioned|p24|||||||||
18289|Tomago Coal Measures|32267|6|Mentioned|p430|||||||||
18289|Tomago Coal Measures|32671|6|Mentioned|Map legend|Permian|Permian|||||||
18289|Tomago Coal Measures|32672|6|Mentioned|p675|||||||||
18289|Tomago Coal Measures|32833|6|Mentioned|p108|||||||||
18289|Tomago Coal Measures|32834|6|Mentioned|Table 3|||||||||
18289|Tomago Coal Measures|32840|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|32920|6|Mentioned|p93|||||||||
18289|Tomago Coal Measures|32937|6|Mentioned|Fig.2|||||||||
18289|Tomago Coal Measures|32945|6|Mentioned|p83|||See also P85. Permian||||||
18289|Tomago Coal Measures|33129|6|Mentioned|Table 1|||Adapted from Packham (1969)||||||
18289|Tomago Coal Measures|33131|6|Mentioned|Fig. 9|||||||||
18289|Tomago Coal Measures|33132|6|Mentioned|p1465|||||||||
18289|Tomago Coal Measures|33334|6|Mentioned|p6|||Perm. See also P7.||||||
18289|Tomago Coal Measures|33685|6|Mentioned|Table 1|||Permian.||||||
18289|Tomago Coal Measures|33702|6|Mentioned|Fig.1|||||||||
18289|Tomago Coal Measures|33711|6|Mentioned|p383|||Table 2.||||||
18289|Tomago Coal Measures|33867|4|Described|p7|||||||||
18289|Tomago Coal Measures|33986|6|Mentioned|p30|||Table||||||
18289|Tomago Coal Measures|34015|6|Mentioned|p323|||Permian||||||
18289|Tomago Coal Measures|34020|6|Mentioned|p43|||||||||
18289|Tomago Coal Measures|34036|6|Mentioned|p434|||||||||
18289|Tomago Coal Measures|34037|6|Mentioned|Table 5.27|||||||||
18289|Tomago Coal Measures|34038|6|Mentioned|p435|||||||||
18289|Tomago Coal Measures|34039|6|Mentioned|p355|||||||||
18289|Tomago Coal Measures|34040|6|Mentioned|p384|||Permian||||||
18289|Tomago Coal Measures|34048|4|Described|p28|||||||||
18289|Tomago Coal Measures|34059|6|Mentioned|Map legend|Permian|Permian|||||||
18289|Tomago Coal Measures|34138|6|Mentioned|Cor.Chart|||Tatarian||||||
18289|Tomago Coal Measures|34171|6|Mentioned|p16|||||||||
18289|Tomago Coal Measures|34287|6|Mentioned|p130|||Permian||||||
18289|Tomago Coal Measures|34292|6|Mentioned|p27|||See also P33, Tables 1 & 3. Permian||||||
18289|Tomago Coal Measures|34345|6|Mentioned|p329|||||||||
18289|Tomago Coal Measures|34351|6|Mentioned|p339|||||||||
18289|Tomago Coal Measures|34399|6|Mentioned|p312|||||||||
18289|Tomago Coal Measures|34400|6|Mentioned|p9|||||||||
18289|Tomago Coal Measures|34444|6|Mentioned|Map legend|Permian|Permian|||||||
18289|Tomago Coal Measures|34445|6|Mentioned|Fig.5.3|||||||||
18289|Tomago Coal Measures|34447|6|Mentioned|Table 5.2|||||||||
18289|Tomago Coal Measures|34448|5|Briefly described|Table 5.31|||||||||
18289|Tomago Coal Measures|34465|6|Mentioned|p334|||||||||
18289|Tomago Coal Measures|34466|6|Mentioned|p350|||||||||
18289|Tomago Coal Measures|34511|6|Mentioned|p47|||||||||
18289|Tomago Coal Measures|34516|6|Mentioned|p16|||||||||
18289|Tomago Coal Measures|34517|6|Mentioned|p46|||||||||
18289|Tomago Coal Measures|34569|6|Mentioned|p9|||Permian||||||
18289|Tomago Coal Measures|34605|6|Mentioned|p376|||||||||
18289|Tomago Coal Measures|34845|6|Mentioned|Fig.4|||||||||
18289|Tomago Coal Measures|35065|6|Mentioned|p43|||||||||
18289|Tomago Coal Measures|35138|6|Mentioned|p17|||||||||
18289|Tomago Coal Measures|35284|6|Mentioned|Fig.12|||||||||
18289|Tomago Coal Measures|35288|6|Mentioned|p63|||||||||
18289|Tomago Coal Measures|35319|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|35416|6|Mentioned|Fig.2|||Stratigraphy and palynological framework shown||||||
18289|Tomago Coal Measures|35767|6|Mentioned|p6|||||||||
18289|Tomago Coal Measures|35873|6|Mentioned|p14|||||||||
18289|Tomago Coal Measures|35901|6|Mentioned|p8|||||||||
18289|Tomago Coal Measures|36009|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|36042|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|36390|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
18289|Tomago Coal Measures|37065|6|Mentioned|p32|||||||||
18289|Tomago Coal Measures|37081|6|Mentioned|p156|||||||||
18289|Tomago Coal Measures|37082|6|Mentioned|p161|||||||||
18289|Tomago Coal Measures|37083|6|Mentioned|p165|||||||||
18289|Tomago Coal Measures|37084|4|Described|p177|||||||||
18289|Tomago Coal Measures|37085|6|Mentioned|p180|||||||||
18289|Tomago Coal Measures|37086|5|Briefly described|p181,183,185,Fig.1,3||Permian|Now not regarded as part of Singleton Supergroup.||||||
18289|Tomago Coal Measures|37087|6|Mentioned|p195|||||||||
18289|Tomago Coal Measures|37088|6|Mentioned|p205|||||||||
18289|Tomago Coal Measures|37446|6|Mentioned|p187|||||||||
18289|Tomago Coal Measures|37924|6|Mentioned|p488|||||||||
18289|Tomago Coal Measures|38656|4|Described|Fig.1.3.17|||p156.||||||14-MAR-07
18289|Tomago Coal Measures|38958|5|Briefly described|p493|||||||||
18289|Tomago Coal Measures|39268|6|Mentioned|Fig. 5|||||||||
18289|Tomago Coal Measures|39287|6|Mentioned|p20|||See also Fig.2.5||||||
18289|Tomago Coal Measures|39288|6|Mentioned|p64|||||||||
18289|Tomago Coal Measures|39292|3|Fully described|p101|||||||||
18289|Tomago Coal Measures|39294|6|Mentioned|p163|||||||||
18289|Tomago Coal Measures|39299|6|Mentioned|p288|||||||||
18289|Tomago Coal Measures|39306|6|Mentioned|Fig. 21.2|||||||||
18289|Tomago Coal Measures|39307|6|Mentioned|Table 22.1|||||||||
18289|Tomago Coal Measures|39308|6|Mentioned|Fig. 23.4|||||||||
18289|Tomago Coal Measures|39609|6|Mentioned|p2|||||||||
18289|Tomago Coal Measures|39664|6|Mentioned|Table 8|||||||||
18289|Tomago Coal Measures|40166|4|Described|p346|||||||||
18289|Tomago Coal Measures|40256|6|Mentioned|p303|||||||||
18289|Tomago Coal Measures|40321|6|Mentioned|p17|||||||||
18289|Tomago Coal Measures|40396|5|Briefly described|p13|||||||||
18289|Tomago Coal Measures|40602|6|Mentioned|p7|||||||||
18289|Tomago Coal Measures|40625|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
18289|Tomago Coal Measures|40631|6|Mentioned|p161|||||||||
18289|Tomago Coal Measures|40636|6|Mentioned|p43|||||||||
18289|Tomago Coal Measures|40807|6|Mentioned|p161|||||||||
18289|Tomago Coal Measures|40883|6|Mentioned|p9|||See also P15||||||
18289|Tomago Coal Measures|41130|6|Mentioned|p46|||||||||
18289|Tomago Coal Measures|41226|6|Mentioned|Table 1|||||||||
18289|Tomago Coal Measures|41474|4|Described|p62|||||||||
18289|Tomago Coal Measures|41580|6|Mentioned|p9|||||||||
18289|Tomago Coal Measures|41902|6|Mentioned|Table 1 P5|||||||||
18289|Tomago Coal Measures|42091|6|Mentioned|Text fig.2 P284|||||||||
18289|Tomago Coal Measures|42182|4|Described|p297|Late Permian|Late Permian|See also Table 1||||||04-NOV-04
18289|Tomago Coal Measures|42214|6|Mentioned|p459|||||||||
18289|Tomago Coal Measures|42378|6|Mentioned|p19|||||||||
18289|Tomago Coal Measures|42526|6|Mentioned|Map legend|||||||||
18289|Tomago Coal Measures|42648|5|Briefly described|p33|||||||||
18289|Tomago Coal Measures|42767|5|Briefly described|Fig.5|||||||||
18289|Tomago Coal Measures|42780|5|Briefly described|Fig.2 P412|||||||||
18289|Tomago Coal Measures|42992|6|Mentioned|p36|||||||||
18289|Tomago Coal Measures|43017|6|Mentioned|p379|||||||||
18289|Tomago Coal Measures|43194|5|Briefly described|p108, p128, p129 Tb. 8.3.|Late Permian|Late Permian|Newcastle Coalfield, Sydney Basin. Contains Kulnura Marine Tongue, Dempsey Formation. Correlated with the basal (coal bearing) lithic unit in the Black Jack Formation (now named Pamboola Formation) in the Gunnedah Basin.||||||
18289|Tomago Coal Measures|43344|14|Not recorded|p11,18,20,84,85,169|||Formerly called Tomago Stage||||||
18289|Tomago Coal Measures|43383|14|Not recorded|p20, Fig.5||Permian|||||||
18289|Tomago Coal Measures|43384|14|Not recorded|Map Legend||Late Permian|||||||
18289|Tomago Coal Measures|43385|14|Not recorded|p179||Late Permian|||||||
18289|Tomago Coal Measures|43424|14|Not recorded|p11|||||||||
18289|Tomago Coal Measures|43425|14|Not recorded|p1||Permian|||||||
18289|Tomago Coal Measures|43440|14|Not recorded|p35,44,62,63,72,73,|||p82,90||||||
18289|Tomago Coal Measures|43447|14|Not recorded|Tbl 1,p15,18,20-1,||Permian|Inc.Dempsey Fm, Four Mile Creek Fm, Wallis Creek Fm. Diag.p22,23,diag.p26,31,37,43,45-49||||||
18289|Tomago Coal Measures|43448|4|Described|p221-227,Pl.1,2,3,|||Inc. Wallis Creek, Four Mile Creek, Hexham Formations. p231,233-236||||||
18289|Tomago Coal Measures|43449|14|Not recorded|p12;opp 12;Pl 2|||||||||
18289|Tomago Coal Measures|43450|14|Not recorded|p9-13,16,17,24|||||||||
18289|Tomago Coal Measures|43451|14|Not recorded|Map Legend|||||||||
18289|Tomago Coal Measures|43477|2|Defined|p10,12-3,16-7,19,20,||Permian|p22-24,39,44-49,57,59-62,Pl.1,5||||||
18289|Tomago Coal Measures|43479|14|Not recorded|p190,214,218,219||Kazanian|||||||
18289|Tomago Coal Measures|43491|14|Not recorded|pVII/52||Permian|||||||
18289|Tomago Coal Measures|43881|14|Not recorded|p87-88,99||Permian|p87-88 (prox.anals.)||||||
18289|Tomago Coal Measures|43980|14|Not recorded|p4,Pl.1|||||||||
18289|Tomago Coal Measures|43984|14|Not recorded|p135,136,138|||||||||
18289|Tomago Coal Measures|44005|14|Not recorded|p26,Pl.4|||||||||
18289|Tomago Coal Measures|44040|14|Not recorded|p23|||||||||
18289|Tomago Coal Measures|44219|14|Not recorded|p31||Tatarian|||||||
18289|Tomago Coal Measures|44244|6|Mentioned|p276|||Contains the Dempsey Formation.||||||
18289|Tomago Coal Measures|44855|14|Not recorded|p18||Permian|||||||
18289|Tomago Coal Measures|44998|14|Not recorded|p104||Kazanian|Kazanian. Correlated with Condren Member, WA.||||||
18289|Tomago Coal Measures|45006|14|Not recorded|Tb.1,opp.p3|||||||||
18289|Tomago Coal Measures|45071|6|Mentioned|p68|||||||||
18289|Tomago Coal Measures|45088|6|Mentioned|p59|||Permian succession||||||
18289|Tomago Coal Measures|45090|6|Mentioned|p7|||Time correlation chart||||||
18289|Tomago Coal Measures|48735|6|Mentioned|p88|||||||||
18289|Tomago Coal Measures|48744|6|Mentioned|p.88.|||||||||
18289|Tomago Coal Measures|48830|1|Redefined|p.12|||On many pages. p.5,7-12,14,15,19,Fig.8,Pls.1,3. Redefined. Formerly contained Bayswater Formation & Rix's Creek Formation. Now Rix's Creek Formation. synonym of Tomago Coal Measures.||||||
18289|Tomago Coal Measures|49644|5|Briefly described|Table|||||||||
18289|Tomago Coal Measures|60281|5|Briefly described|p61|Late Permian|Late Permian|Divided into Wallis Creek, Four Mile Creek and Dempsey Formations. Overlain by Newcastle Coal Measures.  Age: 262-252Ma. Max. thickness: ~1250m.  Equivalent of the Wittingham Coal Measures.  Geological Province: Sydney Basin.  See also p6, p8.||||||22-MAY-08
18289|Tomago Coal Measures|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Includes: Wallis Creek Four Mile Creek, Dempsey Formations and the Kulnura Marine Tongue. Geological Province: Sydney Basin/Newcastle area.||||||
18289|Tomago Coal Measures|61529|5|Briefly described|p857 Fig. 3a|||Overlain by Newcastle Coal Measures. Geological Province: Sydney Basin. See also p868.||||||
18289|Tomago Coal Measures|61612|6|Mentioned|p273, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
18289|Tomago Coal Measures|61770|6|Mentioned|p111|||||||||
18289|Tomago Coal Measures|62033|5|Briefly described|p25 (Table)|||Geological Province: Sydney Basin.||||||14-MAR-07
18289|Tomago Coal Measures|63832|5|Briefly described|p131 fig 2, p136, 137|Lopingian|Guadalupian|Of Sydney Basin. Final (P4) Paleozoic glaciation, but basal strata show no dispersed gravel or other glacial indicators, suggesting a brief interglacial interval in the mid-Permian.|||Includes Shortland Formation.|||14-DEC-17
18289|Tomago Coal Measures|64098|5|Briefly described|p337|Late Permian|Late Permian|Deposition 263-255 Ma.||||||
18289|Tomago Coal Measures|64631|5|Briefly described|p44 Fig.2, p49.|Wuchiapingian|Wordian|NE Sydney Basin. Radiometric age control near base.|||Includes Shortland Formation.|Overlies Mulbring Siltstone. Is overlain by Newcastle Coal Measures.||
18289|Tomago Coal Measures|67500|6|Mentioned|p19|Late Permian|Late Permian|||||||
18289|Tomago Coal Measures|67663|5|Briefly described|p520 Tb.1|Permian|Permian|Late Permian.|||Includes Dempsey Formation and Kulnura Marine Tongue.|Overlain by the Newcastle Coal Measures. Underlain by the Maitland Group.||
18289|Tomago Coal Measures|67786|6|Mentioned|p96|Permian|Permian|Newcastle Coalfield, Sydney Basin.||||Overlies Maitland Group. Is overlain by Newcastle Coal Measures.||
18289|Tomago Coal Measures|68003|5|Briefly described|p41.|Late Permian|Late Permian|Northern Sydney Basin. Prograding fluvio-deltaic system, fed from the New England region. Referred to as 'Newcastle-Tomago Coal Measures sequence'  (p42) where both units were eroded off the Lochinvar Anticline before the Munmorah Conglomerate was unconformably deposited.||||||
18289|Tomago Coal Measures|68004|5|Briefly described|p23 Table 1.|||Newcastle Coalfield.|||Includes Kulnura Marine Tongue, Dempsey Formation and Waratah Sandstone.|Overlies Maitland Group. Is overlain by Newcastle Coal Measures.||
18289|Tomago Coal Measures|68202|6|Mentioned|p176|Permian|Permian|Sydney Basin. Swampy-deltaic conditions followed uplift of the New England Orogen in Late Permian.|||||Extensive coal deposits.|
18289|Tomago Coal Measures|68493|5|Briefly described|p3 Fig.1, p5, p5 Fig.2, p6|Lopingian|Lopingian|Sydney Basin. Deposition occurred on a deltaic and coastal plain by a delta originating from the south. Contains dropstones.|||Includes Dempsey Formation, Four Mile Creek Formation, and Wallis Creek Formation.|Overlies the Mulbring Siltstone. Is overlain conformably by Newcastle Coal Measures.|Comprises mudstone and sandstone with some discontinuous, relatively thin coal seams, and is characterised by abrupt vertical and lateral facies changes.|
18289|Tomago Coal Measures|69297|6|Mentioned|p499, p501, p502 fig 5.43, p503|Late Permian|Middle Permian|Sydney Basin. Deposited in a fluvial-deltaic environment. Has some potential as a gas or petroleum source rock.||Singleton Group||Overlies the Mulbring Siltstone. Overlain by the Newcastle Coal Measures.|Sandstones, siltstones and coals.|
18289|Tomago Coal Measures|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Singleton Supergroup|Includes Wallis Creek Subgroup, where differentiated.||Sandstone, siltstone, laminated sandstone/siltstone, carbonaceous claystone, coal and minor tuffaceous sandstone.|
18289|Tomago Coal Measures|71538|6|Mentioned|p54|||Sydney Basin.|||Includes the Thornton Claystone.|||
18289|Tomago Coal Measures|73197|6|Mentioned|p478|Guadalupian|Guadalupian|Sydney Basin. Tuff layers sourced from the Currarong Orogen.|272-266 Ma||||Includes tuff layers.|
18317|Tomingley Siltstone|22831|6|Mentioned|p 31|||||||||
18317|Tomingley Siltstone|24417|6|Mentioned|p35|||||||||
18317|Tomingley Siltstone|40365|2|Defined|p329|Middle Ordovician|Early Ordovician|E - M||||||
18317|Tomingley Siltstone|40791|6|Mentioned|p181|||||||||
18317|Tomingley Siltstone|40891|4|Described|p14|||||||||
18317|Tomingley Siltstone|42262|6|Mentioned|Fig. 2 P1810|||||||||
18317|Tomingley Siltstone|46522|5|Briefly described|p41|||||||||
18336|Tonghi Suite|22778|6|Mentioned|p 161|||||||||
18336|Tonghi Suite|22815|6|Mentioned|p79|||||||||
18336|Tonghi Suite|22878|6|Mentioned|p74|||Tonghi Supersuite||||||
18336|Tonghi Suite|24551|6|Mentioned|p235|||||||||
18336|Tonghi Suite|42726|5|Briefly described|map legend||Early Devonian|||||||
18336|Tonghi Suite|42827|5|Briefly described|p430|||||||||
18336|Tonghi Suite|43233|5|Briefly described|Map Legend|Early Devonian|Late Silurian|Of Bega Batholith.||||||01-OCT-08
18336|Tonghi Suite|60541|6|Mentioned|p64|||Includes the Tonghi Granodiorite. Geological Province: Lachlan Fold Belt.||||||
18338|Tonghi Supersuite|22878|6|Mentioned|p57 Table 7|||||||||
18338|Tonghi Supersuite|22879|5|Briefly described|map|Early Devonian|Early Devonian|||||||
18338|Tonghi Supersuite|22880|5|Briefly described|Map Legend|Early Devonian|Early Devonian|Includes: Noorinbee Granodiorite, Tonghi Granodiorite.||||||01-OCT-04
18338|Tonghi Supersuite|22881|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||06-OCT-04
18338|Tonghi Supersuite|24551|5|Briefly described|p235|||Consists of the Nalbaugh Suite and the Tonghi Suite||||||
18338|Tonghi Supersuite|42726|5|Briefly described|map legend|||||||||
18338|Tonghi Supersuite|42827|6|Mentioned|p429|||||||||
18338|Tonghi Supersuite|68592|6|Mentioned|p24|Early Devonian|Early Devonian|||||||
18352|Toogoolawah Group|13516|5|Briefly described|p159 fig 8|Middle Triassic|Middle Triassic|From Clarence-Moreton Basin, Ipswich Basin.|||Includes Esk Formation, Neara Volcanics, Bryden Formation.|||
18352|Toogoolawah Group|22857|5|Briefly described|p277|Middle Triassic|Middle Triassic|Intermediate to felsic calc-alkaline volcanics and volcaniclastic sediments. Max. thickness: >5km. Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|22860|5|Briefly described|p277||Middle Triassic|||||||
18352|Toogoolawah Group|23440|4|Described|p140|Triassic|Triassic|||||||
18352|Toogoolawah Group|23800|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|23842|5|Briefly described|p422 Table 1|Middle Triassic|Early Triassic|Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|24279|5|Briefly described|p1800|Middle Triassic.|Early Triassic|Terrestrial sedimentary and volcanic rocks. Overlain by Aranbanga Volcanic Group.||||||
18352|Toogoolawah Group|24382|5|Briefly described|Map legend|Early Triassic|Early Triassic|Constituents include: Kinellan Basalt, Gayndah Formation and Mount Marcella Volcanics||||||
18352|Toogoolawah Group|24560|5|Briefly described|Map legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|29386|5|Briefly described|p454|||Lower - Middle Triassic.||||||
18352|Toogoolawah Group|30302|6|Mentioned|p414|||Lower - Middle Triassic age||||||
18352|Toogoolawah Group|30303|6|Mentioned|p322|||Lower(?)to Middle Triassic. Strat.relationships with Cressbrook Group.||||||
18352|Toogoolawah Group|30470|6|Mentioned|p458|||||||||
18352|Toogoolawah Group|30473|6|Mentioned|p377|||Refers Granfield & Schawarzbock (1972)||||||
18352|Toogoolawah Group|30508|6|Mentioned|p91|||Triassic age. Palynology||||||
18352|Toogoolawah Group|30914|6|Mentioned|Map legend|Triassic|Triassic|||||||
18352|Toogoolawah Group|31118|6|Mentioned|p323|||Possible oil source||||||
18352|Toogoolawah Group|31450|6|Mentioned|p47|||||||||
18352|Toogoolawah Group|31811|6|Mentioned|p27|||||||||
18352|Toogoolawah Group|33774|6|Mentioned|p42|||Lower Middle Triassic. Refers Cranfield & Schwarzbock (1972)||||||
18352|Toogoolawah Group|33881|5|Briefly described|p96|||||||||
18352|Toogoolawah Group|35101|3|Fully described|p35|||||||||
18352|Toogoolawah Group|35161|6|Mentioned|p591|||||||||
18352|Toogoolawah Group|35428|6|Mentioned|p125|||Biostratigraphy||||||
18352|Toogoolawah Group|35431|6|Mentioned|Fig.2|||Simplified geological map of part of the North D'Aguilar Block.||||||
18352|Toogoolawah Group|36045|6|Mentioned|p334|||||||||
18352|Toogoolawah Group|36243|6|Mentioned|p74|||See also Table 10A.||||||
18352|Toogoolawah Group|36440|6|Mentioned|Map legend|Middle Triassic|Early Triassic|Middle to Early TriassicE - M||||||
18352|Toogoolawah Group|36954|6|Mentioned|p114|||||||||
18352|Toogoolawah Group|36961|6|Mentioned|Table 1|||||||||
18352|Toogoolawah Group|37065|6|Mentioned|p36|||||||||
18352|Toogoolawah Group|37252|6|Mentioned|Map legend|Triassic|Triassic|||||||
18352|Toogoolawah Group|37755|6|Mentioned|p79|||||||||
18352|Toogoolawah Group|38304|6|Mentioned|p83|||||||||
18352|Toogoolawah Group|38391|6|Mentioned|p10|||||||||
18352|Toogoolawah Group|38441|6|Mentioned|Map legend|Middle Triassic|Middle Triassic|||||||
18352|Toogoolawah Group|39079|6|Mentioned|p10|||||||||
18352|Toogoolawah Group|39445|6|Mentioned|Table 9|||||||||
18352|Toogoolawah Group|39943|6|Mentioned|Table 12A|||||||||
18352|Toogoolawah Group|40051|6|Mentioned|p8|||||||||
18352|Toogoolawah Group|40245|6|Mentioned|p182|||See also Table 2.||||||
18352|Toogoolawah Group|40475|5|Briefly described|p7|||||||||
18352|Toogoolawah Group|40480|6|Mentioned|p40|||||||||
18352|Toogoolawah Group|40623|5|Briefly described|p66|||||||||
18352|Toogoolawah Group|41591|5|Briefly described|p17|||||||||
18352|Toogoolawah Group|41736|6|Mentioned|p115|||||||||
18352|Toogoolawah Group|41738|4|Described|p165|||||||||
18352|Toogoolawah Group|41778|6|Mentioned|Fig.1|||||||||
18352|Toogoolawah Group|41790|5|Briefly described|p471|||||||||
18352|Toogoolawah Group|41906|3|Fully described|Table 2 P19|||||||||
18352|Toogoolawah Group|41917|6|Mentioned|Fig.3 P528|||||||||
18352|Toogoolawah Group|42525|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Includes: Esk and Bryden Formations and the Neara Volcanics.||||||15-JUL-04
18352|Toogoolawah Group|42893|6|Mentioned|p6|||||||||
18352|Toogoolawah Group|43001|6|Mentioned|p120|||||||||
18352|Toogoolawah Group|43002|5|Briefly described|Fig.2,p135|||||||||
18352|Toogoolawah Group|44923|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|44925|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|50320|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|60077|5|Briefly described|Map legend|Middle Triassic|Early Triassic|Includes: Esk Formation, Neara Volcanics, Bryden Formation.||||||
18352|Toogoolawah Group|60281|5|Briefly described|p24|Middle Triassic|Early Triassic|Geological Province: Esk Trough.||||||20-JAN-05
18352|Toogoolawah Group|60370|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Geological Province: Esk Trough. Includes the Bryden Formation, Neara Volcanics and Esk Formation.||||||
18352|Toogoolawah Group|60371|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|Includes the Gayndah Formation, Esk Formation and Neara Volcanics. Geological Province: Esk Trough||||||02-SEP-04
18352|Toogoolawah Group|61002|5|Briefly described|p198 Fig 2|Middle Triassic|Middle Triassic|Nonmarine polymict and volcaniclastic conglomerate, sandstone and shale with interbedded andesitic lava and tuff. Max. thickness: 2350m. Geological Province: Esk Trough. See also p199, p202.||||||29-MAY-06
18352|Toogoolawah Group|61005|5|Briefly described|p248|Middle Triassic|Middle triassic|Geological Province: Esk Trough.||||||
18352|Toogoolawah Group|61310|6|Mentioned|p25|||||||||
18352|Toogoolawah Group|61781|6|Mentioned|p267|Middle Triassic|Early Triassic|||||||
18352|Toogoolawah Group|61782|4|Described|p275|Middle Triassic|Early Triassic|Includes; Gayndah Formation, Mount Marcella Volcanics and Kinellan Basalt. Unconfomably overlie Marumba Beds, nonconformity with Claddagh Granodiorite. Max thick: 6000m. Geol Prov: Esk Trough.||||||
18352|Toogoolawah Group|63821|4|Described|p12, p19-20|Middle Triassic|Early Triassic|Comprises Kinella Basalt (base), Gayndah Formation, Mount Marcella Volcanics (top). Unconformably overlain by Aranbanga Volcanic Group. Geological Province: Esk Trough. Series of volcanic flows, pyroclastics, volcaniclastic sediments and fluvial deposits.||||||07-FEB-11
18352|Toogoolawah Group|64197|6|Mentioned|p630 Fig.7|Triassic|Triassic|Moreton Basin/Esk Trough.||||||
18352|Toogoolawah Group|65452|5|Briefly described|p37|Middle Triassic|Early Triassic|Gayndah area. Thought to represent subduction-related magmatism.|||Mount Marcella Volcanics.|||
18352|Toogoolawah Group|67402|5|Briefly described|p204, p207, p208|Ladinian|Anisian|Esk Trough.|||Includes the Esk Formation, Bryden Formation and the Neara Volcanics||Conglomerates, sandstone, shale and volcanics.|
18352|Toogoolawah Group|67874|6|Mentioned|p11||||||Includes Mount Marcella Volcanics.|||06-NOV-15
18352|Toogoolawah Group|68008|5|Briefly described|p188|Triassic|Triassic|Fills the Esk Trough,||||Correlated with Cynthia beds.||
18352|Toogoolawah Group|68553|6|Mentioned|Map legend; schematic diagram.|Triassic|Triassic|Bowen Basin. This unit, as well as the Muncon Volcanics and Native Cat Andesite, are all mapped under the symbol, Rvm.||||||
18352|Toogoolawah Group|68679|5|Briefly described|p312-313, p371, p385, p387-392,p420,p439|Middle Triassic|Early Triassic|The surface exposure of this unit defines the extent of the Esk Basin, northern New England Orogen. Includes units previously part of the Esk Series. Differing interpretations of the Basin's stratigraphy are outlined, and different unit names are applied in the northern part of the Basin. The former Mount Marcella Volcanics are mostly regarded as a northern equivalent to the Neara Volcanics. Estimates of thickness range from 2350m to 5000-6000m. Entirely continental deposits. Contains Middle Triassic macrofloras similar to those in the Brooweena Formation (Gympie Province). Basin evolution discussed.|||Bryden, Esk Formations and Neara Volcanics (southern Esk Basin); Kinellan Basalt, Gayndah Formation (northern Esk Basin).|Is faulted against and unconformably overlies the Cressbrook Creek Group, Northbrook beds and Marumba beds. Overlies Chowey and Mingo Granites. Is overlain unconformably by Abernethy Basalt.||
18352|Toogoolawah Group|69594|5|Briefly described|p560-561|Triassic|Triassic|W and NW of Brisbane.||||Is intruded by the Brisbane Valley Porphyrites.||
18352|Toogoolawah Group|73306|5|Briefly described|p565-566, 573|Middle Triassic|Middle Triassic|Esk Trough.|||Bryden, Esk Formations; Neara Volcanics.|Correlated with Moolayember Formation.|Continental volcaniclastic conglomerate, sandstone, shale, and intermediate volcanic rocks.|
18352|Toogoolawah Group|73450|6|Mentioned|p107|Triassic|Triassic|||||||
18375|Toolebuc Formation|12597|5|Briefly described|p492 Tb.1, p500|Albian|Albian|Eromanga Basin. 3-75m thick. Characteristic high gamma response. Contains abundant bivalves, fish skeletons and teeth, radiolarians, globigerinids and dinoflagellates.|||||Carbonaceous and calcareous mudstone and limestone with minor thin interbeds of fine-grained calcareous labile sandstone and siltstone; local 10m thick oil-shale horizon in N.|
18375|Toolebuc Formation|13497|5|Briefly described|p115, p115 fig 6.33, p146|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Shale and siltstone with minor shoreface sandstone.|
18375|Toolebuc Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Albian|Albian|In Eromanga Basin.||||||
18375|Toolebuc Formation|22464|5|Briefly described|p9||Early Cretaceous|In the Eromanga Basin. Overlies Wallumbilla Formation.||||||12-DEC-06
18375|Toolebuc Formation|22857|5|Briefly described|p295, p296-7 Tb.22.1, p314|Albian|Albian|Oil shales occur. Together with Allaru Mudstone thickness is ~100m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|22865|4|Described|p295,Table22.1p296-7|Cenomanian|Albian|||||||
18375|Toolebuc Formation|22883|5|Briefly described|Fig2 P30||Early Cretaceous|Overlain by Allaru Mudstone, underlain by Wallumbilla Formation.||||||01-FEB-07
18375|Toolebuc Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23031|5|Briefly described|31|||||||||
18375|Toolebuc Formation|23056|6|Mentioned|12 table 2|||||||||
18375|Toolebuc Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group) - not clear in legend however.||||||14-DEC-06
18375|Toolebuc Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The formation is restricted to the northern and western STRZELECKI.||||||
18375|Toolebuc Formation|23356|5|Briefly described|26 Tab.2|Albian|Albian|||||||
18375|Toolebuc Formation|23375|4|Described|Fig2 p265, 266||Albian|Laterally equivalent to lower Oodnadatta Formation. In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|23425|4|Described|Table 9.7 p394||Albian|see also p378. Of Rolling Downs Group. Overlain by Allaru Mudstone; underlain by Wallumbilla Formation. Carpentaria Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23430|4|Described|p522 + p524 Table 14.7|||In the Eromanga Basin Province.||||||12-DEC-06
18375|Toolebuc Formation|23431|5|Briefly described|p543|||||||||
18375|Toolebuc Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
18375|Toolebuc Formation|23864|6|Mentioned|p128|Albian|Albian|||||||
18375|Toolebuc Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
18375|Toolebuc Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
18375|Toolebuc Formation|23982|5|Briefly described|p12|Cretaceous|Cretaceous|Of the Rolling Downs Group. Geological Province: Eromanga Basin. See also page 35 Fig.7.||||||
18375|Toolebuc Formation|23986|5|Briefly described|p71|||||||||
18375|Toolebuc Formation|24048|5|Briefly described|p76|||||||||
18375|Toolebuc Formation|24085|5|Briefly described|p33, p36, p38|Albian|Albian|Geological Province: Eromanga Basin.||||||16-SEP-08
18375|Toolebuc Formation|24092|5|Briefly described|p8 Fig.3|||Of Rolling Downs Group. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24201|5|Briefly described|p379|Albian|Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
18375|Toolebuc Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup.  Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|24226|5|Briefly described|p391|Albian|Albian|Age: Late Albian.||||||
18375|Toolebuc Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Allaru Formation. Underlying Unit: Wallumbilla Formation. Maximum Thickness: <35m. Geological Province: Eromanga Basin||||||
18375|Toolebuc Formation|29394|6|Mentioned|p145|||Cretaceous.||||||
18375|Toolebuc Formation|30584|4|Described|Table 1|||||||||
18375|Toolebuc Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|31121|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|31165|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|31168|6|Mentioned|p10|||||||||
18375|Toolebuc Formation|32314|6|Mentioned|Fig. 4|||||||||
18375|Toolebuc Formation|32705|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|33017|6|Mentioned|p1|||See also p8.||||||12-DEC-06
18375|Toolebuc Formation|33075|4|Described|p451|||Type section p455.||||||12-DEC-06
18375|Toolebuc Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
18375|Toolebuc Formation|33176|6|Mentioned|p175|||||||||
18375|Toolebuc Formation|33177|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|33178|6|Mentioned|p11|||||||||
18375|Toolebuc Formation|33179|4|Described|p11|||||||||
18375|Toolebuc Formation|33368|6|Mentioned|p27|||Refers Smart (1972).||||||
18375|Toolebuc Formation|33414|6|Mentioned|p212,213,Tb.|||Part of Wilgunya Sub-group.||||||
18375|Toolebuc Formation|33772|6|Mentioned|p13|||||||||
18375|Toolebuc Formation|33773|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|33900|6|Mentioned|p21|||||||||
18375|Toolebuc Formation|34811|4|Described|Table 1|||||||||
18375|Toolebuc Formation|35220|6|Mentioned|Table 2|||||||||
18375|Toolebuc Formation|35239|6|Mentioned|p258|||||||||
18375|Toolebuc Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35457|6|Mentioned|p623|||||||||
18375|Toolebuc Formation|35560|4|Described|p291|||||||||
18375|Toolebuc Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
18375|Toolebuc Formation|35793|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|35811|5|Briefly described|Table 3|||Uranium exploration discussed p556.||||||12-DEC-06
18375|Toolebuc Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
18375|Toolebuc Formation|35936|6|Mentioned|p615|||||||||
18375|Toolebuc Formation|36012|3|Fully described|Table 5|||See also p18.||||||12-DEC-06
18375|Toolebuc Formation|36110|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36228|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|36229|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|36243|6|Mentioned|Table 6A|||||||||
18375|Toolebuc Formation|36251|4|Described|p3|||||||||
18375|Toolebuc Formation|36331|6|Mentioned|p92|||||||||
18375|Toolebuc Formation|36552|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36571|6|Mentioned|p95|||||||||
18375|Toolebuc Formation|36690|6|Mentioned|p47|||||||||
18375|Toolebuc Formation|36713|5|Briefly described|p361|||||||||
18375|Toolebuc Formation|36910|6|Mentioned|p61|||||||||
18375|Toolebuc Formation|36912|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|36922|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|37287|6|Mentioned|p36|||||||||
18375|Toolebuc Formation|37608|3|Fully described|Table 1|||||||||
18375|Toolebuc Formation|37776|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|38011|6|Mentioned|p126|||||||||
18375|Toolebuc Formation|38199|5|Briefly described|p426|||Palynology||||||
18375|Toolebuc Formation|38218|4|Described|p285|||||||||
18375|Toolebuc Formation|38226|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|38325|4|Described|p265|||||||||
18375|Toolebuc Formation|38372|6|Mentioned|p647|||||||||
18375|Toolebuc Formation|38373|6|Mentioned|p618|||||||||
18375|Toolebuc Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
18375|Toolebuc Formation|38779|6|Mentioned|p7|||||||||
18375|Toolebuc Formation|38780|6|Mentioned|p17|||||||||
18375|Toolebuc Formation|38814|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlain by Allaru Mudstone.||||||25-AUG-04
18375|Toolebuc Formation|39070|4|Described|p365|||||||||
18375|Toolebuc Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,12-16 etc. Correlation.||||||12-DEC-06
18375|Toolebuc Formation|39445|5|Briefly described|Table 11|||||||||
18375|Toolebuc Formation|39478|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|39480|6|Mentioned|p188|||||||||
18375|Toolebuc Formation|39481|6|Mentioned|p180|||||||||
18375|Toolebuc Formation|39482|6|Mentioned|Fig.7|||||||||
18375|Toolebuc Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39575|6|Mentioned|p103|||||||||
18375|Toolebuc Formation|39708|4|Described|p477|||||||||
18375|Toolebuc Formation|39754|6|Mentioned|p1690|||||||||
18375|Toolebuc Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
18375|Toolebuc Formation|39846|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|39847|5|Briefly described|p39|||||||||
18375|Toolebuc Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|39914|6|Mentioned|p3|||||||||
18375|Toolebuc Formation|39942|6|Mentioned|p463|||||||||
18375|Toolebuc Formation|39943|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|39989|6|Mentioned|p426|||||||||
18375|Toolebuc Formation|40121|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|40167|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|40199|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|40249|6|Mentioned|p41|||||||||
18375|Toolebuc Formation|40322|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|40452|6|Mentioned|p2|||||||||
18375|Toolebuc Formation|40648|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|40670|6|Mentioned|Fig.9|||||||||
18375|Toolebuc Formation|40675|6|Mentioned|Table 8A|||||||||
18375|Toolebuc Formation|40687|6|Mentioned|Table 3|||||||||
18375|Toolebuc Formation|40719|5|Briefly described|p61|||||||||
18375|Toolebuc Formation|40771|5|Briefly described|p429|||||||||
18375|Toolebuc Formation|40801|6|Mentioned|p46|||||||||
18375|Toolebuc Formation|40926|6|Mentioned|p18|||||||||
18375|Toolebuc Formation|41012|3|Fully described|p137|||||||||
18375|Toolebuc Formation|41036|6|Mentioned|p220|||||||||
18375|Toolebuc Formation|41052|6|Mentioned|p87|||||||||
18375|Toolebuc Formation|41060|6|Mentioned|p2|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41061|6|Mentioned|p19|||Generalized stratigraphy||||||
18375|Toolebuc Formation|41062|6|Mentioned|Fig.5|||||||||
18375|Toolebuc Formation|41063|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|41064|6|Mentioned|p62|||||||||
18375|Toolebuc Formation|41084|5|Briefly described|Fig.2|||||||||
18375|Toolebuc Formation|41086|3|Fully described|p101|||See also Fig.3||||||
18375|Toolebuc Formation|41087|3|Fully described|p121|||||||||
18375|Toolebuc Formation|41088|4|Described|p141|||||||||
18375|Toolebuc Formation|41089|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|41097|6|Mentioned|p166|||||||||
18375|Toolebuc Formation|41117|4|Described|p434|||||||||
18375|Toolebuc Formation|41121|6|Mentioned|p179|||||||||
18375|Toolebuc Formation|41125|6|Mentioned|p12|||||||||
18375|Toolebuc Formation|41165|5|Briefly described|p362, p368|||Mention Fig.20||||||
18375|Toolebuc Formation|41174|4|Described|p117|||||||||
18375|Toolebuc Formation|41175|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41176|6|Mentioned|p206|||See also Table 2||||||
18375|Toolebuc Formation|41177|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41178|6|Mentioned|p241|||||||||
18375|Toolebuc Formation|41179|6|Mentioned|p255|||||||||
18375|Toolebuc Formation|41180|5|Briefly described|p267|||||||||
18375|Toolebuc Formation|41181|6|Mentioned|p273|||||||||
18375|Toolebuc Formation|41182|5|Briefly described|p300|||||||||
18375|Toolebuc Formation|41183|6|Mentioned|p310|||||||||
18375|Toolebuc Formation|41184|6|Mentioned|p328|||||||||
18375|Toolebuc Formation|41187|6|Mentioned|Fig.2|||||||||
18375|Toolebuc Formation|41196|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|41198|6|Mentioned|Table 1|||||||||
18375|Toolebuc Formation|41214|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41216|6|Mentioned|Fig.18|||||||||
18375|Toolebuc Formation|41219|6|Mentioned|p338|||||||||
18375|Toolebuc Formation|41266|6|Mentioned|Fig.3|||||||||
18375|Toolebuc Formation|41306|6|Mentioned|p4|||||||||
18375|Toolebuc Formation|41307|6|Mentioned|p5|||||||||
18375|Toolebuc Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41482|6|Mentioned|p37|||||||||
18375|Toolebuc Formation|41483|6|Mentioned|p49|||||||||
18375|Toolebuc Formation|41523|3|Fully described|p279|||||||||
18375|Toolebuc Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
18375|Toolebuc Formation|41568|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|41707|6|Mentioned|p164|||||||||
18375|Toolebuc Formation|41724|6|Mentioned|p383|||||||||
18375|Toolebuc Formation|42061|4|Described|p155|||||||||
18375|Toolebuc Formation|42067|4|Described|Appendix 2|||||||||
18375|Toolebuc Formation|42071|6|Mentioned|p117|||||||||
18375|Toolebuc Formation|42084|6|Mentioned|Fig.3 P356|||||||||
18375|Toolebuc Formation|42085|6|Mentioned|Fig.2 P374|||||||||
18375|Toolebuc Formation|42374|6|Mentioned|p435|Albian||||||||
18375|Toolebuc Formation|42397|6|Mentioned|Fig.2 P3|||||||||
18375|Toolebuc Formation|42402|5|Briefly described|p115, 116|||||||||
18375|Toolebuc Formation|42429|6|Mentioned|p156|||||||||
18375|Toolebuc Formation|42446|4|Described|p13|||||||||
18375|Toolebuc Formation|42447|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
18375|Toolebuc Formation|42520|5|Briefly described|p6|||||||||
18375|Toolebuc Formation|42538|5|Briefly described|Fig. 25.2 P325|||||||||
18375|Toolebuc Formation|42585|5|Briefly described|p79|||||||||
18375|Toolebuc Formation|42588|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42637|4|Described|p11|||||||||
18375|Toolebuc Formation|42673|5|Briefly described|Fig.2, P184|||||||||
18375|Toolebuc Formation|42746|6|Mentioned|Fig.6 P8|||||||||
18375|Toolebuc Formation|42749|6|Mentioned|Fig.2 P27|||||||||
18375|Toolebuc Formation|42804|5|Briefly described|p115|||||||||
18375|Toolebuc Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
18375|Toolebuc Formation|43002|5|Briefly described|Fig.2,p135|||||||||
18375|Toolebuc Formation|43004|5|Briefly described|Table 1,p179|||||||||
18375|Toolebuc Formation|43105|6|Mentioned|p15|||||||||
18375|Toolebuc Formation|43114|5|Briefly described|p15|||||||||
18375|Toolebuc Formation|43122|5|Briefly described|p29|||see also Fig. 2.||||||
18375|Toolebuc Formation|43591|6|Mentioned|p40|||||||||
18375|Toolebuc Formation|43602|6|Mentioned|191|||In Eromanga Basin. Of the Rolling Downs Group.||||||12-DEC-06
18375|Toolebuc Formation|43630|6|Mentioned|p70|||also Fig.4||||||
18375|Toolebuc Formation|44112|6|Mentioned|p82|||||||||
18375|Toolebuc Formation|44133|5|Briefly described|p122, 104 Fig. 9.11|Late Albian|Middle Albian|Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|44291|14|Not recorded|p14|||||||||
18375|Toolebuc Formation|45145|3|Fully described|Table 5|||||||||
18375|Toolebuc Formation|45161|6|Mentioned|p67|||||||||
18375|Toolebuc Formation|46791|4|Described|p47|||||||||
18375|Toolebuc Formation|46872|6|Mentioned|p105|||||||||
18375|Toolebuc Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
18375|Toolebuc Formation|47042|4|Described|p171|||||||||
18375|Toolebuc Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
18375|Toolebuc Formation|48770|6|Mentioned|Fig.1|||||||||
18375|Toolebuc Formation|49010|6|Mentioned|Fig.4|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||12-DEC-06
18375|Toolebuc Formation|49254|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49273|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49278|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49330|14|Not recorded|?|||||||||
18375|Toolebuc Formation|49338|14|Not recorded|?|||||||||
18375|Toolebuc Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Contains calcareous bituminous shale (oil shale).  Geological Province: Carpentaria and Eromanga Basins.||||||
18375|Toolebuc Formation|50332|5|Briefly described|p22, p93, p96|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone. Also contains calcareous bituminous shale (oil shale).||||||07-FEB-11
18375|Toolebuc Formation|60331|5|Briefly described|p34 Fig.3|Albian|Albian|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||
18375|Toolebuc Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Limestone, calcareous sandstone.||||||
18375|Toolebuc Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Wallumbilla Formation. Overlain by Allaru Mudstone. Lateral to Oodnadatta Formation. Geological Province: Eromanga  Basin.||||||31-JAN-08
18375|Toolebuc Formation|61312|5|Briefly described|p66, p73|Albian|Aptian|Of the Rolling Downs Group. In Queensland it consists of carbonaceous and bitumous shale and siltstone with limestone lenses. In Queensland, overlies Wallumbilla Formation and is overlain by Allaru Mudstone. Geological Province: Eromanga Basin.||||||16-JUN-06
18375|Toolebuc Formation|61544|5|Briefly described|p374.|Albian|Albian|Eromanga Basin. Contains marine oil shales which are geochemically similar to asphaltite strandings along the Bight coast.|||||Includes marine oil shales.|
18375|Toolebuc Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
18375|Toolebuc Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
18375|Toolebuc Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
18375|Toolebuc Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Bulldog Shale. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
18375|Toolebuc Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~101-~98Ma. Geological Province: Southern Cape York and Burketown Depression.||||||01-MAR-10
18375|Toolebuc Formation|63979|2|Defined|p50, Fig. 44|Albian|Albian|Previously Toolebuc Member (Wilgunya Fm). Conformable over Wallumbilla Fm; overlain by Allaru Mudstone. Max.thick: 65m. Predominantly mudstone with thin layers of siltstone, sandstone and conglomerate, towards top; also contains limestone (incl. coquinite)||||||09-APR-13
18375|Toolebuc Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - oil shale. Geological Province: Eromanga Basin.||||||07-FEB-11
18375|Toolebuc Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Marree Subgroup.||Underlies Allaru Mudstone; overlies Wallumbilla Formation.||11-DEC-15
18375|Toolebuc Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
18375|Toolebuc Formation|64820|5|Briefly described|pS6 Fig. 4|Late Albian|Late Albian|Of the Rolling Downs Group. Carbonaceous to calcareous silt-claystone with minor sandstones. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
18375|Toolebuc Formation|65238|5|Briefly described|p7 Fig. 8|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
18375|Toolebuc Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 52 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Bulldog Shale. Is overlain by Oodnadatta Shale.|Limestone, calcareous bituminous shale.|
18375|Toolebuc Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Wallumbilla Formation. Overlain by Allaru Mudstone.||||||08-MAR-12
18375|Toolebuc Formation|65489|5|Briefly described|p49, p55, p58, p96, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 60m thick. Oil shale potential.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66529|5|Briefly described|p10, p12, p16-17, p41, p92    |Mesozoic|Mesozoic|Eromanga Basin. Previously investigated for oil shale. An ideal in situ reductant for U systems.|c.107 Ma.|Unit in Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Significant organic content. Black shale.|
18375|Toolebuc Formation|66623|6|Mentioned|p264.|||||||Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|66915|5|Briefly described|p6 Fig.3, p16|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins. In later Rolling Downs Group units, the Toolebuc Formation is the only distinct and laterally persistent seismic reflection for correlation and is widespread in the Eromanga Basin.|||||Includes a thin competent unit of calcareous and bituminous shale, and limestone (a distinct and laterally persistent seismic reflection for correlation).|
18375|Toolebuc Formation|67323|5|Briefly described|p39, p81, p85-89, p93-94, p95 Fig.12.5|Early Cretaceous|Early Cretaceous|See also p96, GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Widespread shallow-marine deposits. Hydrocarbon exploration target in the Eromanga Basin; bituminous shale occurs throughout its extent. Considered prospective for U in the Carpentaria Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale, limestone.|
18375|Toolebuc Formation|67402|4|Described|p108, p109, p112|Albian|Albian|Eromanga Basin. Generally only between 20-45m thick but may be up to 65m thick. Deposited in a restricted marine environment. See also  p113 fig ERO12, p123, p176, p177, p179 fig CRP/KRM6, p180, p181.||Rolling Downs Group||Overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Mudstone dominated succession that also contains limestone that is subordinate to calcareous, bituminous siltstone, labile sandstone and shale.|
18375|Toolebuc Formation|67561|6|Mentioned|p53 Fig.3|||||||||
18375|Toolebuc Formation|67784|5|Briefly described|p25-26, p28-29, p31-32, p34|Albian|Albian|6-25m thick. Carpentaria, northern Eromanga Basins. Appears as Toolebuc Limestone in Tb.1 (p28). Euxinic facies.||Wilgunya Subgroup.||Overlain by Allaru Mudstone. Overlies Ranmoor Member/Coreena Member (Wallumbilla Formation). Is correlated with Oodnadatta Formation|Contains distinctive Inoceramus coquinites and oil shale.|08-FEB-18
18375|Toolebuc Formation|67870|5|Briefly described|p46-47, p50-52|Late Cretaceous|Late Cretaceous|Hydrocarbon seal.|||||Shaly limestone, marl, organic-rich (10% TOC) limestone, sandstone.|
18375|Toolebuc Formation|68206|5|Briefly described|p31, 33|Albian|Albian|NE Eromanga Basin. See also reference to Toolebuc Limestone (p32).||||Overlies Ranmoor Member (Wallumbilla Formation). Is overlain by Allaru Formation.|Limestone; distinctive Inoceramus coquinites and oil shale.|
18375|Toolebuc Formation|68279|6|Mentioned|p19|||Galilee Basin stratigraphic cross-section, and mineralogy table.||||||
18375|Toolebuc Formation|68307|5|Briefly described|p92|Early Cretaceous|Early Cretaceous|Eromanga-Carpentaria Basin. Organic-rich. Forms a strong reflective seismic horizon.||||||
18375|Toolebuc Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.||
18375|Toolebuc Formation|68731|6|Mentioned|pp209-211|||||||||
18375|Toolebuc Formation|68734|5|Briefly described|p218 Fig.2|Albian|Albian|Eromanga Basin (NE). Shallow marine.||Of the Rolling Downs Group.||||
18375|Toolebuc Formation|68821|5|Briefly described|p292 Fig.1, p295, p296, p298|Cenomanian|Cenomanian|Lower Cretaceous age. Parallic to marine sediments. Contains ubiquitous disseminated pyrite. Equivalent in age to the Surat Siltstone.|101 - 98 Ma|Of the Rolling Downs Group.|||Dominantly organic-rich black shale with thin (< 3 cm) beds of limestone.|
18375|Toolebuc Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Albian|Southern Eromanga Basin.||||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Albian|||||||
18375|Toolebuc Formation|69056|6|Mentioned|Reference images sheet.|||Shown on the simplified surface geology map of the Quamby Project area.||||||
18375|Toolebuc Formation|69206|6|Mentioned|p2|Cretaceous|Cretaceous||||||Immature oil shale.|
18375|Toolebuc Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Albian|Upper Albian|Carpentaria Basin. The carbonaceous mudstones are the best potential source rocks in the basin.||Rolling Downs Group||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Carbonaceous mudstone, siltstone and claystone.|
18375|Toolebuc Formation|69454|6|Mentioned|p38:3|||Eromanga Basin.||||||12-JUL-16
18375|Toolebuc Formation|69455|6|Mentioned|p39:4 Fig.39.3|Early Cretaceous|Early Cretaceous|||||||12-JUL-16
18375|Toolebuc Formation|69457|3|Fully described|p41:2-3;41:5 Fig.41.4;41:6-8,10-12,15-18|Albian|Albian|Casey (1959). Eromanga, Carpentaria Basins. Widespread occurrence in drillholes. Shallow-marine deposits. Up to 65m thick. This unit and the Allaru Mudstone are together equivalent to the middle and upper part of Oodnadatta Formation. Has a distinctive, strong gamma signature in wireline logs. Regarded as an oil shale in the NE part of the Basin in Qld. A rich oil-gas source rock, the mudstone typically has a high TOC, generally 9-20%, locally 35%, derived from planktonic algae and cyanobacterial mats; it is an attractive oil shale and unconventional petroleum exploration target. Contains diverse fossil assemblages.||Wilgunya Subgroup.||Conformably overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Dark grey to black mudstone which may be carbonaceous, calcareous or pyritic, with thin layers of siltstone; subordinate labile sandstone, limestone, marl and conglomerate.|12-JUL-16
18375|Toolebuc Formation|69582|5|Briefly described|p22, p25-p26, p29, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga Basin. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone.|
18375|Toolebuc Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Wallumbilla Formation. Is overlain by Allaru Formation.||
18375|Toolebuc Formation|69594|4|Described|p518-519, p521-522, p526, p529-530, p533|Albian|Albian|See also p574. Carpentaria, Eromanga Basins. A thin, isochronous unit up to 65m thick; generally 20-45m. Represents maximum marine conditions within an epeiric basin system. Early late Albian. Contains oil shales; may also be prospective for shale gas. Has a distinct and strong gamma signature. Contains spectacular vertebrate fossils (listed).||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain conformably by Allaru Mudstone.|Coquinitic limestone, nodular limestone, oil shale, kerigenous shale, with minor siltstone and labile sandstone.|
18375|Toolebuc Formation|69673|6|Mentioned|p12 t5, p159, p160, p164, p165|||Prospective for unconventional hydrocarbons. Potential oil/gas source rock.||Wilgunya Subgroup||Overlain by Allaru Mudstone, overlies Wallumbilla Formation|Mudstone with thin layers of siltstone and subordinate labile sandstone, limestone, marl and conglomerate.|
18375|Toolebuc Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Toolebuc Fm.||||||
18375|Toolebuc Formation|69946|3|Fully described|p23-26, p57, p94|Albian|Albian|Originally Toolebuc Member (Casey, 1959) of the Wilgunya Formation. Later upgraded to Toolebuc Limestone (Vine et al., 1967), then defined as Toolebuc Formation by Senior et al. (1975). Casey's type section, outcrop on the Boulia-Winton Road 7 miles (11.3km) E of the Hamilton Hotel, was replaced because of poor outcrop by Senior et al. (1975) by the interval 25.3 - 35.8 m in BMR Boulia 3A. A reference section was also assigned to Boulia 3 (25 - 36m). High gamma ray response: its role in identifying Wallumbilla Formation mis-correlations from Qld into SA is discussed. Up to 50m thick. Wireline log correlations.||||Conformably overlies Wallumbilla Formation. Passes laterally into Oodnadatta Formation. Is overlain conformably by Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains; dark grey fossiliferous mudstone with coquinite comprising large bivalve shells; dark grey mudstone. Bituminous shales in the type section; local oil shale origins.|
18375|Toolebuc Formation|69947|5|Briefly described|p13 Fig.7.2|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Marree Subgroup.||||
18375|Toolebuc Formation|69948|6|Mentioned|Fig.4.18|||Eromanga Basin.||||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.|Calcareous bituminous shale and limestone.|
18375|Toolebuc Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|20-JAN-22
18375|Toolebuc Formation|70574|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Calcareous bituminous shale and limestone.|18-JAN-22
18375|Toolebuc Formation|70821|5|Briefly described|p21, p33, p80|Early Cretaceous|Early Cretaceous|Eromanga Basin. Absent in the southern Thomson region.||Rolling Downs Group.||Overlies Oodnadatta and Wallumbilla Formations. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|70823|5|Briefly described|p25-p27, p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 60m thick. Deposited in a restricted, stratified and anoxic marine environment. Hosts an oil shale source rock.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Formation.||
18375|Toolebuc Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts oil shale source rocks.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||
18375|Toolebuc Formation|70836|6|Mentioned|p474|Albian|Albian|||||Coeval with Griman Creek Formation.||
18375|Toolebuc Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
18375|Toolebuc Formation|71059|6|Mentioned|p6 Fig.5|||Eromanga Basin.||||||
18375|Toolebuc Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.||24-OCT-19
18375|Toolebuc Formation|71342|3|Fully described|Ch4 p25, Ch5 p23-p25|Late Albian|Middle Albian|Eromanga Basin. Originally named by Casey (1959) the Toolebuc Member of the Wilgunya Formation. Vine et al (1967) subsequently upgraded the member to formation status as the Toolebuc Limestone. Senior et al (1975) redefined the Limestone as the Toolebuc Formation. The type section for this unit was originally assigned to outcrop on the Boulia-Winton Road by Casey (1959). The BMR defined a new type section in Boulia 3A due to poor outcropping of the original section. A reference section was also given. Distribution and wireline log characteristics are given. A maximum thickness of 50m is recorded in Haddon Downs 1 in the northern Cooper region. Age derived from fossil assemblage and palynological studies. Interpreted to have been deposited in a restricted marine environment. Spore-pollen zone is given in Ch5 p57. See also Ch5 p57, Ch6 p9, Ch7 p13, Ch12 p12, Ch12 p14.||||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone.|Black calcareous and carbonaceous mudstone with abundant fish remains, dark grey fossiliferous mudstone with coquinite containing abundant bivalves and bituminous shales.|
18375|Toolebuc Formation|71382|5|Briefly described|p4, p11, p13, p16-p17|||Eromanga Basin. Intersected in GSQ Julia 1 from 156.65m-199.87m for a total of 43.22m thickness. Deposited during widespread shallow marine conditions. Temp log and stratlog are provided. Lithology is described in detail on p21. See also p21, p23, p25, p27, App 3, 4.||||Overlies the Wallumbilla Formation. Overlain by the Allaru Mudstone.|Mudstone and calcareous mudstone.|
18375|Toolebuc Formation|71601|6|Mentioned|p120, p121|Albian|Albian|NW Qld. Includes dinosaur fossils provisionally assigned to Minmi.||||||
18375|Toolebuc Formation|71855|4|Described|p1-p2, p4-p6, p9-p11, p13, p15, p18, p20|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria basins. This unit has three distinct lithofacies which are described. In places the contact with the underlying Wallumbilla Formation is faulted or disconformable. This unit is highly organic rich and has good source rock charactersitcs. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure, geochemistry and source rock potential are discussed. Typically greater than 15m thick. See also p22-p35, p42-p44, p47-p50, p52-p53, p56-p57, p61-p64, p66-p68, p73-p75.||Rolling Downs Group||Conformably (gradationally) overlies the Wallumbilla Formation. Conformably (gradationally) overlain by the Allaru Mudstone. Overlain by the Mackunda Formation.|Calcareous mudstone, coquinitic mudstone and organic-rich, slightly calcareous mudstone without calcite laminae.|
18375|Toolebuc Formation|71863|4|Described|p1-p18|Albian|Albian|Eromanga and Carpentaria basins. Originally defined as the Toolebuc Limestone by Vine et al. (1967). Subsequently this unit was redefined by Senior et al (1975) as the Toolebuc Formation due to recognition of significant mudstone component. The type section is defined in BMR Boulia 3A (Burger, 1974; Senior et al., 1975). Deposited during a marine incursion. Mudstone may contain laminae of carbonate form from bivalve remains Inoceramus and Aucellina (Ozimic, 1986). Deposited in a restricted, oxygen depleted marine environment. Wireline log characteristics, geochemistry, sedimentary facies, fossil assemblage, petroleum resources and mineralisation are discussed. Equivalent to the Wooldrige Limestone Member and Urisino beds.||Rolling Downs Group||Conformably overlies the Wallumbilla Formation. Conformably overlain by the Allaru Mudstone. Equivalent to the Wooldridge Limestone Member and Urisino beds.|Laminated calcareous and kerogenous mudstone, minor coquinite and limestone, labile sandstone and oil shale.|01-MAY-19
18375|Toolebuc Formation|72297|5|Briefly described|p712, p721, p728, p746, p751-753, p755|Early Cretaceous|Early Cretaceous|Eromanga and Carpentaria Basins. Julia Creek area; occurs north as far as 16 degrees S. Oxidised oil shales in the upper part produce soft oxide coquina, with associated large molybdenum and vanadium resources. Hosts a large gypsum deposit at Hughenden; other localities mentioned. An excellent though immature hydrocarbon source rock. Very high potential shale oil resources (perhaps the most extensive in Australia) despite very low grade; eg Julia Creek oil shale deposit (described).||||Conformably overlies the Ranmoor Member (Wallumbilla Formation). Is overlain conformably by the Allaru Mudstone.|A flat-lying unit comprising an upper, coarse limestone-clay-oil shale unit and a lower, fine carbonate-clay-oil shale unit. Contains mudstones rich in organic kerogenous material.|
18375|Toolebuc Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin.||Rolling Downs Group.||Overlies Coreena and Ranmoor Members (Wallumbilla FZ). Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|72799|6|Mentioned|p27|||||||||
18375|Toolebuc Formation|72913|6|Mentioned|p8.|||Three wells intersected this cover unit.||||||
18375|Toolebuc Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
18375|Toolebuc Formation|73083|6|Mentioned|p58, p62-63|||||||Underlain by the Wallumbilla Formation.|Includes shale and subordinate limestone.|
18375|Toolebuc Formation|73137|6|Mentioned|p6|Cretaceous|Cretaceous|||||||
18375|Toolebuc Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Aquitard with potential shale gas/oil play.||Rolling Downs Group||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Wallumbilla Formation. Is overlain by Allaru Mudstone.||
18375|Toolebuc Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
18375|Toolebuc Formation|73249|5|Briefly described|p319, p321, p323|Albian|Albian|Eromanga Basin. Deposited in a marine environment.||||Overlies the Wallumbilla Formation, underlies the Allaru Mudstone, lateral equivalent of the Coorikiana Sandstone.|Mudstone.|
18375|Toolebuc Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
18375|Toolebuc Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wallumbilla Formation. Overlain by Allaru Mudstone. Equivalent to Oodnadatta Formation.||
18375|Toolebuc Formation|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Open shallow marine depositional environment.|ca 103 Ma|||Overlies Wallumbilla Formation, underlies Allaru Mudstone||
18375|Toolebuc Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
18409|Toongi Hall Tuff|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Fine and coarse-grained cherty tuff, rhyolite tuff. Max. thickness: 450m. Geological Province: Cowra Trough.||||||
18409|Toongi Hall Tuff|23043|5|Briefly described|Map Legend|Pridoli|Ludlow|of Toongi Group.||||||
18409|Toongi Hall Tuff|23170|2|Defined|p119|Late Silurian|Late Silurian|of Toongi Group.||||||
18409|Toongi Hall Tuff|32045|6|Mentioned|Map legend|Silurian|Silurian|||||||
18409|Toongi Hall Tuff|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
18409|Toongi Hall Tuff|40328|2|Defined|p129|Silurian|Silurian|||||||
18409|Toongi Hall Tuff|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
18409|Toongi Hall Tuff|68003|5|Briefly described|p24 Fig.3-e, p144. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Whylandra Formation. Is overlain by Wirrabilla Formation.|Fine and coarse cherty tuff, tuffaceous siltstone, rhyolitic tuff, lithic quartz sandstone.|
18460|Torrowangee Group|22553|5|Briefly described|p77,p83|||part of the Adelaidean sequence||||||
18460|Torrowangee Group|22646|6|Mentioned|Fig 4 on p 102|||Adelaide Geosyncline (East).||||||
18460|Torrowangee Group|22730|5|Briefly described|p558 Fig1||Neoproterozoic|||||||
18460|Torrowangee Group|22772|5|Briefly described|p63,66,Table13.1|Neoproterozoic III|Cryogenian|||||||
18460|Torrowangee Group|22857|5|Briefly described|p64, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Geological Province: Adelaide Fold Belt. See also p398 and 400 App. 1 Tb.A1.3.||||||
18460|Torrowangee Group|23833|6|Mentioned|p256 fig.2|||||||||
18460|Torrowangee Group|29864|6|Mentioned|p263|||||||||
18460|Torrowangee Group|29921|6|Mentioned|Fig.1|||||||||
18460|Torrowangee Group|29991|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18460|Torrowangee Group|30261|6|Mentioned|Table 1|||Willouran to Marinoan||||||
18460|Torrowangee Group|30683|6|Mentioned|Table 1|||||||||
18460|Torrowangee Group|30908|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Probable Adelaide System equivalent.||||||
18460|Torrowangee Group|31012|6|Mentioned|p8|||Adelaidean. Lithology.||||||
18460|Torrowangee Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18460|Torrowangee Group|33004|6|Mentioned|Fig.8|||||||||
18460|Torrowangee Group|33468|6|Mentioned|p210|||||||||
18460|Torrowangee Group|33729|4|Described|p82|||U.Prot.||||||
18460|Torrowangee Group|33730|6|Mentioned|p191|||Late Precambrian||||||
18460|Torrowangee Group|33734|6|Mentioned|p494|||||||||
18460|Torrowangee Group|33875|6|Mentioned|p22|||Uranium deposit||||||
18460|Torrowangee Group|34468|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|Equivalents||||||
18460|Torrowangee Group|34469|6|Mentioned|p105|||Table. See also PP109,110 etc. Upper Proterozoic||||||
18460|Torrowangee Group|34563|6|Mentioned|p58|||Structure||||||
18460|Torrowangee Group|34812|6|Mentioned|p4|||See also P53||||||
18460|Torrowangee Group|34814|6|Mentioned|Fig.2|||||||||
18460|Torrowangee Group|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18460|Torrowangee Group|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
18460|Torrowangee Group|36733|6|Mentioned|Table 5|||||||||
18460|Torrowangee Group|37627|6|Mentioned|p185|||||||||
18460|Torrowangee Group|37931|6|Mentioned|p531|||||||||
18460|Torrowangee Group|38969|6|Mentioned|p199|||||||||
18460|Torrowangee Group|39214|5|Briefly described|p7|||||||||
18460|Torrowangee Group|39574|6|Mentioned|p155|||||||||
18460|Torrowangee Group|39652|6|Mentioned|p5|||||||||
18460|Torrowangee Group|39885|6|Mentioned|p427|||||||||
18460|Torrowangee Group|40595|6|Mentioned|p91|||||||||
18460|Torrowangee Group|41403|6|Mentioned|Table 5|||||||||
18460|Torrowangee Group|41405|5|Briefly described|p203|||||||||
18460|Torrowangee Group|41801|6|Mentioned|Fig.4|||||||||
18460|Torrowangee Group|42531|5|Briefly described|Map legend|Adelaidean||||||||
18460|Torrowangee Group|42982|5|Briefly described|Table 1,p333|||||||||
18460|Torrowangee Group|43192|6|Mentioned|Table1 p61|||||||||
18460|Torrowangee Group|43263|6|Mentioned|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43265|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43268|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43269|5|Briefly described|Map Legend||Neoproterozoic|||||||
18460|Torrowangee Group|43357|14|Not recorded|155-161||Neoproterozoic|||||||
18460|Torrowangee Group|43383|14|Not recorded|p3-6|Permian|Carboniferous|||||||
18460|Torrowangee Group|43464|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|43501|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|43502|14|Not recorded|Map Legend||Neoproterozoic|(Provisional Edition)||||||
18460|Torrowangee Group|44093|5|Briefly described|p110|Neoproterozoic|Neoproterozoic|See also p139 Appendix 1. Geological Province: Adelaide Fold Belt.||||||29-MAR-05
18460|Torrowangee Group|46889|6|Mentioned|p277|||||||||
18460|Torrowangee Group|48926|6|Mentioned|p67|||P67 et seq.||||||
18460|Torrowangee Group|60648|5|Briefly described|p41 Fig. 1|Neoproterozoic|Neoproterozoic|Unconformably overlies the Willyama Series of rocks.  Geological Province: Darling Basin.||||||28-APR-05
18460|Torrowangee Group|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Includes the Yancowinna Subgroup. Geological Province: Broken Hill Domain.||||||07-FEB-11
18460|Torrowangee Group|66623|5|Briefly described|p13, p17.|||Name replaced Torrowangee Series of Mawson (1912).|||Includes Teamsters Creek Subgroup.|Overlain by Kara Formation of Grey Range Group.|Wide variety of meta-sandstone, green-grey meta-siltstone, brown calcareous sandstone, grey quartzite, conglomerates, diamictite, dolomite, flaggy limestone and pyritic shale.|
18460|Torrowangee Group|67562|6|Mentioned|p102 Fig.8|Precambrian|Precambrian|||||||
18460|Torrowangee Group|70000|5|Briefly described|p32-34, p39|Ediacaran|Cryogenian|Syn-rift deposition in the Broken Hill area resumed following Sturtian tectonism. Hosts two glacially-distributed glacial successions separated by carbonate-rich interglacial deposits. Mis-spelt as Tarrowangee on p32-33 and p41.|||Includes Yancowinna, Euriowie and Teamsters Creek, Subgroups.|||
18460|Torrowangee Group|70013|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Burta (geophysical basement) Zone. Three facies are mapped separately: dominantly quartzite and sandstone, dominantly siltstone and claystone, ironstone (magnetite/hematite-rich beds). Interpreted as continental and marine sediments that accumulated within intra-continental rift basins. Part of a sedimentary package that unconformably overlies the Broken Hill Block.|||||Quartzite, sandstone, siltstone, claystone, limestone, ironstone.|
18460|Torrowangee Group|70015|5|Briefly described|Map legend|Ediacaran|Cryogenian|Mineral deposits (if any) are shown. Also appears (mis-spelt) as Tarrowangee Group.|||Includes Yancowinna, Euriowie and Teamsters Creek Subgroups.|Is overlain by Farnell Group.|Sandstone, quartzite, siltstone, shale +/- pyrite, flaggy limestone, sandy limestone, dolomite, polymictic (para)conglomerate, diamictite, pebbly siltstone/mudstone.|
18467|Torrumbarry Clay|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Late Miocene|Of the Wunghnu Group. Geological Province: Murray Basin.||||||13-AUG-07
18467|Torrumbarry Clay|22773|5|Briefly described|Fig24.8p352|Early Pliocene||||||||
18467|Torrumbarry Clay|22799|5|Briefly described|p23 Fig.8|Pliocene|Pliocene|||||||
18467|Torrumbarry Clay|22857|5|Briefly described|p352 Fig.24.8|Early Pliocene|Late Miocene|Of the Wunghnu Group. Geological Province: Murray Basin.||||||
18467|Torrumbarry Clay|22887|5|Briefly described|Fig.6 p13|Early Pliocene|Early Pliocene|||||||
18467|Torrumbarry Clay|23884|5|Briefly described|p155 Fig. 13.2|Late Miocene|Late Miocene|Geological Province: Murray Basin. Of the Wunghnu Group.||||||
18467|Torrumbarry Clay|24439|5|Briefly described|p15, p37|||Mapped by Lawrence (1975) as Torrumbarry Clay and correlated with Calivil Fm. by Lawrence (1975) and Brown and Stephenson (1991); interpreted as White Hills Gravel by Cherry and Wilkinson (1994). Also known as Axedale clay (Edwards et al, 1998).||||||
18467|Torrumbarry Clay|24551|6|Mentioned|p521|||||||||
18467|Torrumbarry Clay|31746|5|Briefly described|p197|||||||||
18467|Torrumbarry Clay|35091|6|Mentioned|p12|||||||||
18467|Torrumbarry Clay|42125|5|Briefly described|p137|||||||||
18467|Torrumbarry Clay|42130|6|Mentioned|Fig.3 P265|||||||||
18467|Torrumbarry Clay|42134|6|Mentioned|Fig.3 P335|||||||||
18467|Torrumbarry Clay|42827|4|Described|p271|||see also Fig 8.4||||||
18467|Torrumbarry Clay|42966|2|Defined|Table 29 p183|Early Pliocene|Late Miocene|||||||
18467|Torrumbarry Clay|43804|6|Mentioned|Fig.2,p49|||||||||
18467|Torrumbarry Clay|60599|5|Briefly described|p85|Tertiary|Tertiary|Of the Wunghnu Group. Geological Province: Murray Basin.||||||
18467|Torrumbarry Clay|61185|5|Briefly described|p63|||One of 5 members of Tickell (1977) of Shepparton Formation, including four sand bodies which were later abandoned (Tickell 1991). See Turrumbarry (probably misspelt) Clay (p63) where also stated as of Wunghnu Group (Lawrence 1966).||||||07-FEB-11
18467|Torrumbarry Clay|65552|5|Briefly described|p5 Fig. 3|Early Pliocene|Late Miocene|Of Wunghnu Group, eastern Murray Basin. Underlies Shepparton and Coonambidgal Formations.||||||
18467|Torrumbarry Clay|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown only on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||Wunghnu Group||Shown as equivalent to the Calivil Formation and underlying the Shepparton Formation.|Shown as including clay.|
18477|Touga Granite|42726|5|Briefly described|map legend|Carboniferous||53.||||||
18477|Touga Granite|66300|5|Briefly described|pp52-57.|Middle Carboniferous|Middle Carboniferous|Eastern Lachlan Orogen. Magmatic crystallisation age is indistinguishable from that of Bundundah Granite to the east, establishing Middle Carboniferous plutonism in southern MOSS VALE area; but much younger than previously-linked Tullyangela Granite.|325.5 +/- 2.6 Ma.|||Intrudes Adaminaby Group.|Even- and medium-grained (2-3 mm) melanocratic and quartz-poor hornblende granodiorite, containing very pale green vitreous plagioclase, biotite, amphibole and very clear quartz.|
18477|Touga Granite|70661|3|Fully described|vii, viii, p6, p123, p125|Serpukhovian|Serpukhovian|Named for Touga Plateau. Previously known as Weirimunga Quartz Monzonite and also undifferentiated granitic rocks. May be assigned to the Oberon Supersuite, however Blevin et al (2010) suggest the Supersuite classifications here used are unclear.Distribution, structure, metamorphism and geochemistry discussed briefly.  Outcrops as loose boulders and platforms. Temporally equivalent to Bundundah Granite and Wandandian Granite. Other given ages include  324 +/- 3 Ma, 322 +/-3  Ma (Rb/Sr). See also ,p126, p127, p128, p130,  p131, p245|325.5 +/- 2.6 Ma (SHRIMP U-Pb)|Oberon Supersuite||Intrudes the Adaminaby Group|Primarily equigranular, fine to medium grained quartz monzonite and some quartz monzodiorites and granodiorites. Clinopyroxene, opaque minerals, zircon and apatite visible in thin section.|
18477|Touga Granite|71303|5|Briefly described|map legend|Carboniferous|Carboniferous||||||Equigranular, fine- to medium-grained quartz monzonite and granodiorite with plagioclase, biotite, pink K-feldspar and hornblende. Aplite dykes and dark, fine-grained enclaves locally.|
18477|Touga Granite|73197|6|Mentioned|p465 Fig.4|Carboniferous|Carboniferous||||||Intrusives.|
18482|Toukley Coal Member|37083|6|Mentioned|p167|||||||||
18482|Toukley Coal Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Catherine Hill Bay Formation.||||
18490|Tout Intrusive Complex|730|6|Mentioned|p22 Fig.5.|||||||||11-NOV-14
18490|Tout Intrusive Complex|22831|4|Described|p 21||Late Ordovician|||||||
18490|Tout Intrusive Complex|33004|6|Mentioned|p106|||||||||
18490|Tout Intrusive Complex|40365|2|Defined|p330|Middle Devonian|Early Devonian|||||||11-NOV-14
18490|Tout Intrusive Complex|40682|5|Briefly described|p2|||||||||
18490|Tout Intrusive Complex|41871|6|Mentioned|p1|||||||||
18490|Tout Intrusive Complex|42077|6|Mentioned|p21|||||||||
18490|Tout Intrusive Complex|42912|6|Mentioned|Fig.1|||||||||
18490|Tout Intrusive Complex|43441|5|Briefly described|12, 21|||397 +/- 16Ma (K-Ar) (Thompson, 1974), but ?Late Ordovician||||||08-JAN-10
18490|Tout Intrusive Complex|44160|5|Briefly described|Map Legend||Eastonian|||||||08-JAN-10
18492|Towallum Basalt|22857|5|Briefly described|p319 Fig.22.10B, p548 App.1 Tb.A1.12|Early Jurassic|Early Jurassic|Of the Marburg Subgroup (Bundamba Group). Vesicular tholeiitic basalt, volcaniclastics. Max. thickness: 50m. Geological Province: Clarence-Moreton Basin. See also p318-9.||||||
18492|Towallum Basalt|22865|5|Briefly described|p318,Table22.2p308||Early Jurassic|Max Age: 187 (+/-) 5 Ma.||||||
18492|Towallum Basalt|23720|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|of the Walloon Coal Measures.  Basalt, minor basalt breccia.||||||
18492|Towallum Basalt|23812|5|Briefly described|p34 Tb.4|Early Jurassic|Early Jurassic|Of Koukandowie Formation. Maximum thickness: 50m.  Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|23843|5|Briefly described|p456 Table 1|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 15m.||||||
18492|Towallum Basalt|24127|5|Briefly described|p5|Jurassic|Jurassic|Max. thickness: 60m.||||||
18492|Towallum Basalt|24129|6|Mentioned|p4|||||||||
18492|Towallum Basalt|30785|6|Mentioned|p397|||||||||
18492|Towallum Basalt|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
18492|Towallum Basalt|34340|3|Fully described|p469|||||||||
18492|Towallum Basalt|34593|6|Mentioned|p539|||||||||
18492|Towallum Basalt|36570|6|Mentioned|p39|||||||||
18492|Towallum Basalt|37122|6|Mentioned|Table 1|||||||||
18492|Towallum Basalt|40245|6|Mentioned|p187|||||||||
18492|Towallum Basalt|42248|6|Mentioned|p405|||||||||
18492|Towallum Basalt|42925|6|Mentioned|p86|||||||||
18492|Towallum Basalt|43150|5|Briefly described|Map Legend||Jurassic|Of the Koukandowie Formation. Tholeiitic basalt at base in the south. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
18492|Towallum Basalt|43383|14|Not recorded|p24|Jurassic|Triassic|||||||
18492|Towallum Basalt|43479|14|Not recorded|p249,262|Late Jurassic|Middle Jurassic|||||||
18492|Towallum Basalt|43881|14|Not recorded|p6-7,11,37-8,49,52-3|Jurassic|Triassic|p59(anal.),62-3,133.||||||
18492|Towallum Basalt|44028|14|Not recorded|Fig.2||Jurassic|See Strat Table.||||||
18492|Towallum Basalt|44450|4|Described|p28 Table 7|Middle Jurassic|Middle Jurassic|Geological Province: Clarence-Moreton Basin. Max. thickness: >60 m.||||||
18492|Towallum Basalt|45003|14|Not recorded|p238|||||||||
18492|Towallum Basalt|60079|5|Briefly described|Map Legend|Early Jurassic|Early Jurassic|Of the Marburg Subgroup.||||||
18492|Towallum Basalt|60281|5|Briefly described|Fig.18 Appendix 1|Early Jurassic|Early Jurassic|Of the Koukandowie Formation.  Vesicular basalt, volcaniclastics.  Max. thickness: 50m.||||||
18492|Towallum Basalt|60993|5|Briefly described|p8 Fig. 4|||Of the Marburg Subgroup. Overlain by Koukandowie Formation members, Ma Ma Creek Member and Heifer Creek Sandstone Member. Overlies Gatton Sandstone. Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60995|4|Described|p65, p51 Fig. 3|Early Jurassic|Early Jurassic|Originally designated as part of Marburg Fm overlying Koukandowie Sst Mbr; revised and now part of Marburg Subgrp, beneath Heifer Creek Sst Mbr (part of Koukandowie Fm?). Max. thickness: 50m. Geol. Prov: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60996|5|Briefly described|p113 Fig. 64|||Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|60997|4|Described|p138|Toarcian|Pleinsbachian|Previously mapped as lying between the Marburg "Fm" and Walloon C.M with age 175-163Ma; now revised to age 187+/-10Ma lying between Gatton Sst and Heifer Creek Sst Mbr.  Max. thick: 15m. Geol. Prov: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|61310|5|Briefly described|Table C1 (p22-23)|Early Jurassic|Early Jurassic|Tholeiitic basalt. Geological Province: Clarence-Moreton Basin.||||||
18492|Towallum Basalt|61794|6|Mentioned|p355|||Olivine tholeiite.||||||
18492|Towallum Basalt|69297|5|Briefly described|p487 fig 5.38|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin. Between 10-50m thick. Deposited in a terrestrial or lacustrine environment.||Koukandowie Formation||Overlies the Gatton Sandstone. Overlain by the Ma Ma Creek Member.|Vesicular basalt and volcaniclastics.|
18520|Towradgi dolerite|40044|6|Mentioned|Table 1|||||||||
18525|Tragowel Member|2967|5|Briefly described|p35, 46-47, 49|||Macumber (1978). Loddon Plain, Murray Basin. Slightly deeper water deposit. Type section is 33m to 47m in the Meran 10 bore near Kerang. Up to 25m thick. On p46 the author gives contradictory accounts of its stratigraphic position. Appears as Tragowel Clay Member on p176.||Parilla Sand.|s|Overlies Kerang Sand Member and (locally) Loxton Sands. Is overlain by Wandella Sandstone.|A sequence of white clay and silt.|
18525|Tragowel Member|10010|5|Briefly described|p12 Fig. 3|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
18525|Tragowel Member|22773|5|Briefly described|Fig24.8p352|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22782|6|Mentioned|p15|||||||||
18525|Tragowel Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22857|5|Briefly described|p352 Fig.24.8|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sand? (relationship not clear in figure). Geological Province: Murray Basin.||||||
18525|Tragowel Member|22887|5|Briefly described|Fig.6 p13|Early Pliocene|Early Pliocene|||||||
18525|Tragowel Member|22893|5|Briefly described|fig4 p9|||||||||
18525|Tragowel Member|23884|5|Briefly described|p155 Fig. 13.2|Early Pliocene|Late Miocene|Geological Province: Murray Basin.||||||
18525|Tragowel Member|34757|6|Mentioned|p50|||||||||
18525|Tragowel Member|39329|6|Mentioned|Fig.1|||||||||
18525|Tragowel Member|40820|6|Mentioned|Fig.1|||||||||
18525|Tragowel Member|42134|6|Mentioned|Fig.3 P335|||||||||
18525|Tragowel Member|42966|2|Defined|Table 27, p172|Early Pliocene||of Loxton-Parilla Sands||||||
18525|Tragowel Member|43791|6|Mentioned|p372, Fig1|||||||||
18525|Tragowel Member|43804|6|Mentioned|Fig.2,p49|||||||||
18525|Tragowel Member|49040|6|Mentioned|Fig.6|||||||||
18525|Tragowel Member|60452|5|Briefly described|p37|Cenozoic|Cenozoic|Of the Parilla Sand. White clay and silt sequence. Overlies the Kerang Sand Member; overlain by the Wandella Sand Member. Max. thickness: 25m.||||||19-NOV-08
18525|Tragowel Member|65552|5|Briefly described|p5 Fig. 3|Early Pliocene|Early Pliocene|Of Loxton-Parilla Sands. Overlies Kerang Sand Member and underlies Wandella Sandstone Member.||||||
18525|Tragowel Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Shoreface and shelf sediments.||Unit in Loxton-Parilla sands.||Overlies Kerang Sand Member. Is overlain by Wandella Sandstone Member.||
18525|Tragowel Member|67179|4|Described|p581|Pliocene|Miocene|Marine, regressive.||Of Loxton Sand||Overlies the Kerang Sand Member, underlies the Wandella Sandstone.|Silt-sized clear quartz grains in a white clay matrix; marine.|28-MAY-13
18525|Tragowel Member|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown only on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||||Shown as partially overlying the Kerang Sand Member and partially underlying the Loxton-Parilla Sands. Partially equivalent to Bookpurnong beds.|Shown as including silt.|
18564|Trealmont Quartzite|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Max. thickness: 60m. Geological Province: Cowra Trough.||||||
18564|Trealmont Quartzite|23043|5|Briefly described|Map Legend|Lochkovian|Pridoli|of Toongi Group.||||||
18564|Trealmont Quartzite|23170|2|Defined|p121|Late Silurian|Late Silurian|of Toongi Group.||||||
18564|Trealmont Quartzite|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
18564|Trealmont Quartzite|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
18564|Trealmont Quartzite|40328|2|Defined|p129|Silurian|Silurian|||||||
18564|Trealmont Quartzite|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
18564|Trealmont Quartzite|68003|5|Briefly described|p24 Fig.3-e, p144. |Pridoli|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Dowd Formation. Is overlain by Glengeera Formation.|Quartzose sandstone, lithic quartzose sandstone, quartzite.|
18599|Trinkey Formation|22857|5|Briefly described|p518 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Nea Subgroup (Black Jack Group). Claystone, siltstone, fine-grained sandstone, tuff, carbonaceous claystone and tuffaceous stony coal. Max. thickness: 258m. Geological Province: Gunnedah Basin.||||||
18599|Trinkey Formation|42767|6|Mentioned|p5|||Of Black Jack Group. Reserved as Trinkey.||||||17-SEP-08
18599|Trinkey Formation|43194|5|Briefly described|Appendix 8.1 p133|Late Permian|Late Permian|Nea Subgroup. New, formal name for the 'tuffaceous coaly unit' in Black Jack Formation (now Black Jack Group). Formal definition published in an article released immediately prior to this article, however a summary of new nomenclature is provided in Appendix 1.||||||13-NOV-13
18599|Trinkey Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Nea Subgroup.||||||
18599|Trinkey Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Nea Subgroup (Black Jack Group). Geological Province: Gunnedah Basin. Claystone, siltstone, sandstone, conglomerate, tuff and coal.||||||
18599|Trinkey Formation|65116|5|Briefly described|p447, 448, fig 6, p441|Late Permian|Late Permian|?Of Black Jack Group, Gunnedah Basin.  Equivalent age to Ingelara Formation, based on palynology.SHRIMP zircon age from top of fm: 256.8 +/-3.8 Ma is consistent with palynology. Sequence D3. Finely bedded claystone, siltstone, sandstone, coal and tuff. Low energy fluvial deposits.||||||
18599|Trinkey Formation|68003|5|Briefly described|p38 Fig.3-j, p44 Photo.3-h, p129.|Late Permian|Late Permian|Formerly the Dunedoo Formation. Gunnedah Basin, Brigalow Belt South Bioregion. Contains plant fossils.||Upper unit in Nea Subgroup.||Overlies Wallala Formation. Is overlain by Digby Formation.|Claystone, siltstone and fine-grained sandstone intercalated with tuff.|
18599|Trinkey Formation|68004|5|Briefly described|p23 Table 1, p176.|||Gunnedah Basin. Forms a good regional seal over the Clare Sandstone.||Upper unit in Nea Subgroup.||Overlies Wallala Formation. Is overlain by Digby Formation.|Includes coals and tuffs.|
18599|Trinkey Formation|70791|5|Briefly described|p277|Lopingian|Lopingian|Gunnedah Basin.||Nea Subgroup.||||
18599|Trinkey Formation|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Gunnedah Basin. CA-TIMS age of 257.46 Ma (Laurie etal., in prep). Corresponding to APP5 zone (Lopingian).||||||
18599|Trinkey Formation|70878|4|Described|p715-718, p724-726|Permian|Permian|Gunnedah Basin. Other similar age determinations given. Calibration of palynological ages (D. parvithola Zone).|254.57 +/- 0.06 Ma.|Black Jack Group.||Overlies Wallala Formation. Is overlain unconformably by Digby Formation.|Includes tuff layers.|
18599|Trinkey Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Wallala Formation.||
18600|Triple Chance pegmatite|34944|6|Mentioned|p361|||||||||
18606|Troffs Formation|22519|6|Mentioned|p7|||of the Trundle Group||||||
18606|Troffs Formation|22520|6|Mentioned|p18|||of the Trundle Group||||||
18606|Troffs Formation|22831|2|Defined|p 62|Emsian|Pragian|||||||
18606|Troffs Formation|22857|4|Described|p448 App.1, Tb.A1.6|Pragian|Lochkovian|Of the Trundle Group. Arenite and siltstone; limestone horizons and lenses; contains brachiopods, trilobites, lamellibranchs, conodonts, corals. Max. thickness: 700m. Geological Province: Bogan Gate Terrace.||||||
18606|Troffs Formation|23522|5|Briefly described|p254|Middle Devonian|Early Devonian|||||||
18606|Troffs Formation|24125|5|Briefly described|p44|||Of the Hervey Group.  Geological Province: Lachlan Fold Belt.||||||
18606|Troffs Formation|24417|6|Mentioned|p89|||||||||
18606|Troffs Formation|29907|6|Mentioned|p8|||||||||
18606|Troffs Formation|29910|6|Mentioned|Map legend|Devonian|Devonian|||||||
18606|Troffs Formation|29985|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
18606|Troffs Formation|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
18606|Troffs Formation|30071|6|Mentioned|Fig.3|||||||||
18606|Troffs Formation|32865|6|Mentioned|p484|||Fauna||||||
18606|Troffs Formation|33121|6|Mentioned|p78|||?Mid.-Late Dev. Refers Conolly (1965). See also P76.||||||
18606|Troffs Formation|33732|5|Briefly described|p114|||||||||
18606|Troffs Formation|36066|6|Mentioned|p10|||||||||
18606|Troffs Formation|43441|4|Described|29||Early Devonian|Formerly of Hervey Group||||||08-JAN-10
18606|Troffs Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
18606|Troffs Formation|43499|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Nangar Sub-Group. In Tullamore Syncline||||||
18606|Troffs Formation|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition) Part of Nangar Sub-Group. In Tullamore Syncline||||||
18606|Troffs Formation|43507|2|Defined|p126,128-29,144-45,||Late Devonian|Formation of Nangar Subgroup (Hervey Group) p150-154||||||
18606|Troffs Formation|43510|2|Defined|p41,45,66,68-72,78|||p80||||||
18606|Troffs Formation|44160|5|Briefly described|Map Legend|Emsian|Pragian|||||||08-JAN-10
18606|Troffs Formation|48958|6|Mentioned|Plate 1|||||||||
18606|Troffs Formation|50299|5|Briefly described|Map Legend|Devonian|Devonian|Of the Trundle Group.||||||
18606|Troffs Formation|61894|6|Mentioned|p179 Fig.3|||||||||
18606|Troffs Formation|62569|5|Briefly described|p606|Devonian|Devonian|Originally mapped as Hervey Formation by Conolly (1965). Now included in Early Devonian rocks of Trundle Group. Geological Province: Lachlan Fold Belt.||||||10-AUG-07
18606|Troffs Formation|66498|6|Mentioned|p45|||||||||
18705|Turi Greywacke Member|34080|6|Mentioned|p248|||||||||
18705|Turi Greywacke Member|43399|2|Defined|p196,198,201,203,205||Tournaisian|||||||
18705|Turi Greywacke Member|43406|14|Not recorded|p42,48||Tournaisian|Part of Parry Group (L.Carb)||||||
18720|Turondale Formation|22472|5|Briefly described|p37|Devonian|Devonian|of the Crudine Group||||||
18720|Turondale Formation|22529|4|Described|1,8|Lochkovian|Lochkovian|Geol province Hill End Trough. Overlying unit Waterbeach Formation, underlying unit Piambong Formation||||||
18720|Turondale Formation|22590|3|Fully described|P750, P753, Fig1|Lochkovian|Pridoli|Age of unit is 411.5+/-4.1 Ma||||||
18720|Turondale Formation|22857|4|Described|p470 App.1 Tb.A1.6|Early Devonian|Late Silurian|Of the Crudine Group. Contains corals, brachiopods in limestone clasts, plant fragments. Age: 411.3+/-3.4Ma (U/Pb SHRIMP). Max. thickness: 900m. Geological Province: Hill End Trough and Capertee Rise.||||||
18720|Turondale Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
18720|Turondale Formation|23170|2|Defined|p158|Lochkovian|Lochkovian|Of Crudine Group.||||||28-AUG-08
18720|Turondale Formation|23214|3|Fully described|p189|Lochkovian|Lochkovian|Of Crudine Group. Age: 410+/-4Ma and 411+/-3Ma (SHRIMP U/Pb zircon). Max. thickness 700m.||||||
18720|Turondale Formation|23738|4|Described|p254|Devonian|Devonian|||||||
18720|Turondale Formation|23851|5|Briefly described|p797|Early Devonian|Early Devonian|||||||
18720|Turondale Formation|24394|4|Described|p169, p170|Lochkovian|Lochkovian|Geological Province: Lachlan Fold Belt.||||||
18720|Turondale Formation|33732|4|Described|p116|||||||||
18720|Turondale Formation|34403|4|Described|p134|||Devonian. See also P136||||||
18720|Turondale Formation|34405|6|Mentioned|Fig.3.9|||||||||
18720|Turondale Formation|34572|6|Mentioned|p92|||See also Table 1. Crudine Group||||||
18720|Turondale Formation|38216|5|Briefly described|p253|||||||||
18720|Turondale Formation|39331|6|Mentioned|Fig.7.6|||||||||
18720|Turondale Formation|40328|3|Fully described|p175|||||||||
18720|Turondale Formation|43127|5|Briefly described|p4,Fig.2,Fig.3||Early Devonian|||||||
18720|Turondale Formation|43494|4|Described|p25, p26||Devonian|Supersedes Lana Fm. Overlies Cookman Formation and Chesleigh Formation where Cookman Fm is missing. See also Turondale formation.||||||16-MAR-06
18720|Turondale Formation|43517|2|Defined|p123-161,Map Pl XII||Early Devonian|Lower part of Crudine Group.||||||
18720|Turondale Formation|43639|5|Briefly described|Map Legend|Devonian|Devonian|||||||
18720|Turondale Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
18720|Turondale Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
18720|Turondale Formation|43654|6|Mentioned|Map Legend|Devonian|Devonian|||||||17-JUL-08
18720|Turondale Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
18720|Turondale Formation|44093|5|Briefly described|p207 App. 1|Early Devonian|Late Silurian|Of the Crudine Group. Geological Province: Lachlan Fold Belt.||||||
18720|Turondale Formation|64296|5|Briefly described|p84 Tb. 1|Early Devonian|Early Devonian|Contains brachiopod fauna.||||||28-AUG-08
18720|Turondale Formation|64994|5|Briefly described|p1, p9|Lochkovian|Lochkovian|Age: 413.4+/-6.6Ma (Jagodzinski and Black 1999). Geological province: Lachlan Orogen/Hill End Trough. Upper section hosts allochthonous limestones containing conodonts, as well as a brachiopod fauna.||||||07-FEB-11
18720|Turondale Formation|66197|5|Briefly described|p633 Fig.4a|Pragian|Lochkovian|Of Crudine Group. Capertee High-Hill End Trough. Deep marine volcaniclastics. Age: 410-413 Ma.||||||14-MAR-12
18720|Turondale Formation|68003|5|Briefly described|p24 Fig.3-e, p143. |Pridoli|Pridoli|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Basal unit in Crudine Group.||Is overlain by Waterbeach Formation.|Thickly-bedded, crystal-lithic, rhyolitic to rhyodacitic volcaniclastic sandstone interbedded with lesser thinly-bedded, pelagic and volcaniclastic sandstone, siltstone and phyllitic shale; minor rhyolitic tuff and conglomerate.|
18720|Turondale Formation|68592|5|Briefly described|p1038, p1043, p1049|Lochkovian|Lochkovian|Northern Hill End Trough. Shelly and conodont faunas at the top of this unit indicate a late Lochkovian  age.||Unit in Crudine Group.||Correlated with Dunchurch Formation.||
18720|Turondale Formation|70297|5|Briefly described|map legend, on side 2 of map sheet|Early Devonian|Early Devonian|Rare conodonts enabled accurate age-dates.||Crudine Group|||Conodonts in limestones.|
18720|Turondale Formation|73299|6|Mentioned|p1096 Fig.3, p1097-1098 Fig.4|Early Devonian|Late Silurian|Hill End Trough. Locations in text include p1102 Fig.8. [Map symbol suggests Devonian age]||||Overlies the Cookman Formation, Piambong Formation, underlies the Waterbeach Formation.||
18725|Turrallo Quartz Diorite|30731|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
18725|Turrallo Quartz Diorite|32999|3|Fully described|p46|||||||||
18725|Turrallo Quartz Diorite|34481|6|Mentioned|Map legend|Carboniferous|Carboniferous|Misspelling of Turallo||||||
18725|Turrallo Quartz Diorite|63633|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|Quartz diorite, quartz diorite porphyry, dacite porphyry.||||||
18725|Turrallo Quartz Diorite|68592|6|Mentioned|p851, p869, p1659|||Obsolete. Name applied by Scheibner (1973) in the Strathaird area, west of Taralga, to the Gundary beds. Now subsumed into the Forest Lodge Quartz Monzodiorite because of pronounced lithological similarity.||||||
18731|Turtle Rock Volcanics|22831|4|Described|p 86||Tertiary|||||||
18731|Turtle Rock Volcanics|29986|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
18731|Turtle Rock Volcanics|39663|6|Mentioned|Table 1|||||||||
18731|Turtle Rock Volcanics|40328|6|Mentioned|p124|||||||||
18731|Turtle Rock Volcanics|43441|5|Briefly described|20, Fig. 3, p23||Tertiary|Great Artesian Basin?||||||08-JAN-10
18731|Turtle Rock Volcanics|43500|14|Not recorded|Map Legend||Late Devonian|(Provisional Edition)||||||
18731|Turtle Rock Volcanics|44160|5|Briefly described|Map Legend||Cenozoic|||||||08-JAN-10
18731|Turtle Rock Volcanics|48958|6|Mentioned|Plate 1|||||||||
18746|Twofold Bay Formation|22815|4|Described|p100, fig31,32|||||||||
18746|Twofold Bay Formation|22857|5|Briefly described|p216, p494 App. 1 Tb.A1.7|Devonian|Middle Devonian|Basal part of the Merrimbula Group. A fan to fluvial sequence of red, poorly sorted arenite with conglomeratic horizons and mudstone. Max. thickness: 400m. Geological Province: Lambie Basin.||||||
18746|Twofold Bay Formation|22859|6|Mentioned|p216|||||||||
18746|Twofold Bay Formation|23309|5|Briefly described|p186|||||||||
18746|Twofold Bay Formation|30938|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
18746|Twofold Bay Formation|32127|3|Fully described|p263|||Refers Steiner (1966)||||||
18746|Twofold Bay Formation|32865|6|Mentioned|p484|||||||||
18746|Twofold Bay Formation|33268|6|Mentioned|Table 1|||||||||
18746|Twofold Bay Formation|33269|4|Described|p47|||Lithology||||||
18746|Twofold Bay Formation|33732|6|Mentioned|p113|||||||||
18746|Twofold Bay Formation|35277|5|Briefly described|p121|||||||||
18746|Twofold Bay Formation|35526|6|Mentioned|Table 2|||Fossil types and localities||||||
18746|Twofold Bay Formation|38327|6|Mentioned|p564|||||||||
18746|Twofold Bay Formation|38899|6|Mentioned|p71|||||||||
18746|Twofold Bay Formation|39313|6|Mentioned|p280|||||||||
18746|Twofold Bay Formation|40276|6|Mentioned|p27|||||||||
18746|Twofold Bay Formation|40646|6|Mentioned|p24|||||||||
18746|Twofold Bay Formation|41385|6|Mentioned|p373|||||||||
18746|Twofold Bay Formation|41641|5|Briefly described|p191|||||||||
18746|Twofold Bay Formation|42050|5|Briefly described|p228|||||||||
18746|Twofold Bay Formation|42158|6|Mentioned|p2|||||||||
18746|Twofold Bay Formation|42827|5|Briefly described|p191|||of Merimbula Group||||||
18746|Twofold Bay Formation|42848|5|Briefly described|p530|||Of Merrimbula Group. Consists of interbedded red mudstone and sandstone with conglomerate beds - of terrestrial origin.||||||09-MAY-05
18746|Twofold Bay Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
18746|Twofold Bay Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
18746|Twofold Bay Formation|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Merrimbula Group (Lambie Shelf). Geological Province: Lambian Transitional Province.||||||
18746|Twofold Bay Formation|63605|5|Briefly described|p993 Fig.2, p999|Frasnian|Frasnian|Lower unit of the Merrimbula Group. Formerly the basal part of "Merimbula Formation". Directly overlies sediments and volcanics of the Boyd Volcanic Complex; overlain by Bellbird Creek Formation.||||||07-FEB-11
18746|Twofold Bay Formation|66499|5|Briefly described|p61, p62 Fig.6|Frasnian|Frasnian|Stratigraphically below the marine Bellbird Creek Formation. Includes fish fossils||Of Merrimbula Group||?Underlies Bellbird Creek Formation||
18746|Twofold Bay Formation|68298|5|Briefly described|p214; p234||Frasnian|Base unit of Merrimbula Group. Contains fish fauna near top of the formation. Bothriolepis fauna. Phyllolepid and possible remigolepid remains are associated.||Merrimbula Group||Is overlain by Bellbird Creek Formation.||
18746|Twofold Bay Formation|70661|3|Fully described|p107 fig 8, p110-p112|Frasnian|Frasnian|Named for Twofold Bay. Contains an informal basal conglomerate unit. Distribution, geomorphology and fossils are discussed. Type section is mentioned but not described. Estimated to be more than 160m thick in Moss Vale. Deposited in a braided stream environment. Minimum age poorly constrained.||Merrimbula Group||Faulted against Adaminaby Group, conformably overlain by Bellbird Creek Formation|Interbedded red mudstone and litharenite with rare conglomerate beds. A basal conglomerate with rhyolite clasts in a quartz matrix also occurs.|
18746|Twofold Bay Formation|71303|5|Briefly described|map legend|Frasnian|Frasnian|||Of Merrimbula Group.|||Continental sandstone, red mudstone and rare conglomerate.|
18746|Twofold Bay Formation|71700|5|Briefly described|CD|||||Merrimbula Group||||
18746|Twofold Bay Formation|73181|6|Mentioned|p62, p64-66|Frasnian|Frasnian|||Merrimbula Group|Wolumla Conglomerate Member|Underlain by Boyd Volcanic Complex. Overlain by Worange Point Formation and Bellbird Creek Formation.||
18747|Tyagong Serpentinite|29907|2|Defined|Appendix 1|Early Silurian|Early Silurian|Prob.Early Silurian||||||
18747|Tyagong Serpentinite|29910|6|Mentioned|Map legend|Silurian|Silurian|||||||
18747|Tyagong Serpentinite|35608|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
18747|Tyagong Serpentinite|35609|6|Mentioned|p2|||||||||
18747|Tyagong Serpentinite|36411|6|Mentioned|p270|||Refers Bowman 1977.||||||
18770|Ugalong Dacite|22857|5|Briefly described|p446 App.1, Tb.A1.6|Early Devonian|Early Devonian|Part of the Derriwong Group? Dacites. Max. thickness: ~5km. Geological Province: Darling Basin.||||||
18770|Ugalong Dacite|24417|3|Fully described|p47|Early Silurian|Early Silurian|Of Ungarie Suite.||||||
18770|Ugalong Dacite|35503|2|Defined|p207|Early Devonian|Early Devonian|New name refs Kemezys (1976)||||||
18770|Ugalong Dacite|50385|5|Briefly described|Map Legend|Silurian|Silurian|Crystal-rich biotite dacite and rhyodacite lavas and pyroclastics.||||||26-MAR-08
18770|Ugalong Dacite|50554|5|Briefly described|Map legend|Silurian|Silurian|Crystal-rich biotite dacite and rhyodacite lavas and pyroclastics.||||||21-JUN-04
18770|Ugalong Dacite|60008|5|Briefly described|Map Legend|Silurian|Silurian|Felsic volcanics.||||||
18770|Ugalong Dacite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||13-JUL-04
18770|Ugalong Dacite|61964|3|Fully described|p14 Fig. 4, p58|Early Silurian|Early Silurian|Two distinct fault-bounded bodies of massive, porphyritic, mid- to dk. grey dacite; S-type.Formerly mapped as Ungarie Granite (Pogson et al 1967). Located closely with Koetong Suite granites.  Ages: ~428.2Ma, 433.4+/-3.1Ma, 432.9+/-1.8Ma (SHRIMP U-Pb)||||||
18770|Ugalong Dacite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Porphyritic biotite dacite and rare pyroclastic rocks.||||||10-APR-08
18770|Ugalong Dacite|64568|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Crystal-rich biotite dacite and rhyodacite lavas and pyroclastic rocks.||||||
18770|Ugalong Dacite|65469|5|Briefly described|p18|Early Silurian|Early Silurian|Lachlan Orogen.||Koetong Suite||||
18770|Ugalong Dacite|66197|5|Briefly described|p634|Early Silurian|Early Silurian|Wagga-Omeo Zone. Silicic volcanics associated with granite plutons.||||||14-MAR-12
18770|Ugalong Dacite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.|||Crystal-rich biotite dacite and rhyodacite lavas and pyroclastic rocks.
|
18770|Ugalong Dacite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Porphyritic crystal-rich biotite dacite and rhyodacite (emplaced as lavas), and sporadic pyroclastic rocks.|
18779|Ulah Formation|13996|6|Mentioned|p138|Ludlow|Ludlow|Orange area. Formerly the Panuara Formation. Putative conulariids discussed.||||||
18779|Ulah Formation|22857|4|Described|p468 App.1 Tb.A1.6|Ludlovian|Wenlockian|Of the Mumbil Group. Graptolite-bearing quartzofeldspathic shale, coarse micaceous horizons, local basal siltstone. Max. thickness: 500m.||||||
18779|Ulah Formation|23214|3|Fully described|p138|Ludlow|Wenlock|Of the Mumbil Group. Originally included in the Panuara Formation.||||||
18779|Ulah Formation|35258|4|Described|p127|||||||||
18779|Ulah Formation|43640|5|Briefly described|Map Legend||Silurian|||||||
18779|Ulah Formation|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group. Consists of graptolite-bearing, quartzofeldspathic shale with coarse micaceous horizons; local basal siltstone.||||||15-JUL-08
18779|Ulah Formation|43782|5|Briefly described|Map Legend|Ludlow|Wenlock|Of Mumbil Group.||||||15-JUL-08
18779|Ulah Formation|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
18784|Ulan Coal|38603|6|Mentioned|p83|||||||||
18784|Ulan Coal|41595|6|Mentioned|p37|||||||||
18784|Ulan Coal|68003|5|Briefly described|p41, p42.|Late Permian|Late Permian|Western Coalfield, Sydney Basin.||||Is locally overlain by Narrabeen Group.||
18784|Ulan Coal|68004|5|Briefly described|p60 Table 6, p61, p157.|Late Permian|Late Permian|Western Coalfield. Has two sections: 3 plies in the upper, and 5 in the lower. c.14 m thick at Ulan. Described in detail. See also reference to "Ulan seam" (p62) and Ulan Seam (pp217-220).||||Overlies Blackmans Flat Formation. Is overlain by Newnes Formation.||
18806|Umberatana Group|7931|5|Briefly described|p98|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
18806|Umberatana Group|9862|5|Briefly described|Map Legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|22510|4|Described|p36, table1p37|||Age: Sturtian to Marinoan||||||
18806|Umberatana Group|22553|6|Mentioned|p77|||part of the Adelaidean sequence||||||
18806|Umberatana Group|22631|6|Mentioned|p177, fig2 p170|Cryogenian|Cryogenian|||||||
18806|Umberatana Group|22643|6|Mentioned|p186|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|22646|6|Mentioned|Fig 4 on p 102|||Adelaide Geosyncline (West). .||||||
18806|Umberatana Group|22677|5|Briefly described|p734, Fig.2 p735|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|22725|6|Mentioned|p242 fig1|||||||||
18806|Umberatana Group|22772|4|Described|p63,66,Table13.1|Neoproterozoic III|Cryogenian|||||||
18806|Umberatana Group|22830|6|Mentioned|P25||Adelaidean|||||||
18806|Umberatana Group|22857|5|Briefly described|p63, Tb. 13.1 (insert p70-71)|Marinoan|Sturtian|Now included in the Heysen Supergroup and belongs to a new Pangean supercycle (Veevers, 1990). Age: 700-590Ma. See also p66.||||||
18806|Umberatana Group|22869|6|Mentioned|P37|||||||||
18806|Umberatana Group|22889|5|Briefly described|p30|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|22911|6|Mentioned|37|||Geol province Adelaide Geosyncline||||||
18806|Umberatana Group|22926|5|Briefly described|37|||Geol province Adelaide Geosyncline. Underlying unit Burra Group||||||
18806|Umberatana Group|22947|6|Mentioned|p16|||Mentioned under - Adelaide Geosyncline Geodevelopments.||||||
18806|Umberatana Group|22949|5|Briefly described|p27|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23054|5|Briefly described|p14,34|||||||||
18806|Umberatana Group|23176|6|Mentioned|p12||Neoproterozoic|Adelaide Geosyncline||||||
18806|Umberatana Group|23178|6|Mentioned|Fig.1||Neoproterozoic|||||||
18806|Umberatana Group|23180|6|Mentioned|p36, Fig.1|||||||||
18806|Umberatana Group|23211|6|Mentioned|p45 Fig.1|||||||||
18806|Umberatana Group|23250|5|Briefly described|p1125 Fig.3||Cryogenian|For correlates see members.||||||
18806|Umberatana Group|23282|6|Mentioned|p54|||||||||
18806|Umberatana Group|23288|6|Mentioned|Fig.5,18|||of Adelaide Geosyncline.||||||05-APR-13
18806|Umberatana Group|23315|5|Briefly described|p344|Neoproterozoic|Neoproterozoic|Subdivided into Upper, Middle and Lower Umberatana Group.||||||07-FEB-07
18806|Umberatana Group|23351|5|Briefly described|283|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23394|5|Briefly described|Map legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|23411|6|Mentioned|Map Legend|||||||||
18806|Umberatana Group|23412|5|Briefly described|Map Legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|23445|5|Briefly described|p437|||||||||
18806|Umberatana Group|23478|5|Briefly described|p27|||||||||
18806|Umberatana Group|23557|5|Briefly described|p95 Fig.1|Neoproterozoic III|Cryogenian|Geological Province: Adelaide Rift Complex.||||||
18806|Umberatana Group|23719|4|Described|p26|Neoproterozoic|Adelaidean|See also page 25 table 7. Overlying unit Wilpena Group. Underlying unit Burra Group. Geological Province: Gawler Craton.||||||
18806|Umberatana Group|23806|5|Briefly described|p1122 Fig. 1|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|23818|5|Briefly described|p38 Fig.10, p63|Adelaidean|Adelaidean|Max. thickness: > 20 000 ft (in the southeast).||||||
18806|Umberatana Group|23913|4|Described|p110 Fig. 2|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.  Overlying Unit: Wilpena Group.  Underlying Unit: Burra Group (unconformable).||||||
18806|Umberatana Group|24045|5|Briefly described|p533 Fig.2|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|24175|4|Described|p12|Neoproterozoic|Neoproterozoic|Lowermost part of Heysen Supergroup.||||||
18806|Umberatana Group|24176|3|Fully described|p11, p24 Tb. 1|Adelaidean|Adelaidean|Comprises the Yudnamutana, Farina, Willochra and Yerelina Sub-Groups. Overlies the Burra Group.  Age is Marinoan. Geological Province: Mount Painter Province.||||||13-FEB-08
18806|Umberatana Group|24195|5|Briefly described|p45 Fig.3|||Geological Province: Adelaide Geosyncline||||||
18806|Umberatana Group|24261|5|Briefly described|p1047 Fig.1|Neoproterozoic|Neoproterozoic|Geological Province: Gawler Craton||||||
18806|Umberatana Group|24321|5|Briefly described|Map legend|Adelaidean|Adelaidean|Includes the Yerelina, Willochra, Farina and Yudnamutana Subgroups.||||||05-APR-13
18806|Umberatana Group|24481|5|Briefly described|p829 Fig. 9|||Overlies the Burra Group. Overlain by the Wilpena Group.||||||
18806|Umberatana Group|24484|5|Briefly described|p798 Fig.1|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|24546|5|Briefly described|p2 - 3 Fig.2|Neoproterozoic|Neoproterozoic|Age: ~700-620 Ma. Geological Province: Adelaide Fold Belt.||||||16-JAN-08
18806|Umberatana Group|24586|5|Briefly described|p50 Fig. 1, p51 Fig. 2|Adelaidean|Adelaidean|Of the Heysen Supergroup. Geological Province: Adelaide Geosyncline.||||||
18806|Umberatana Group|24593|5|Briefly described|p612 Fig. 1a|||Geological Province: Mount Painter Inlier.||||||
18806|Umberatana Group|29656|4|Described|Fig.3|||||||||
18806|Umberatana Group|29697|6|Mentioned|p7|||||||||
18806|Umberatana Group|29763|6|Mentioned|p45|||||||||
18806|Umberatana Group|29778|6|Mentioned|p167|||||||||
18806|Umberatana Group|29780|4|Described|p30|||||||||
18806|Umberatana Group|29781|6|Mentioned|Fig.5|||||||||
18806|Umberatana Group|29831|5|Briefly described|p175|||||||||
18806|Umberatana Group|29834|6|Mentioned|p196|||||||||
18806|Umberatana Group|29837|4|Described|p75|||||||||
18806|Umberatana Group|29840|6|Mentioned|Fig.3|||||||||
18806|Umberatana Group|29929|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|30028|6|Mentioned|Fig.4|||||||||
18806|Umberatana Group|30051|6|Mentioned|Fig.1|||Proterozoic age.||||||
18806|Umberatana Group|30052|6|Mentioned|Fig.5|||See also Fig.6. Proterozoic age.||||||
18806|Umberatana Group|30053|6|Mentioned|Fig.1|||Proterozoic age.||||||
18806|Umberatana Group|30176|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian - Marinoan||||||
18806|Umberatana Group|30177|4|Described|p66|||Sturtian - Marinoan age.||||||
18806|Umberatana Group|30190|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|30261|6|Mentioned|Table 1|||Sturtian - Marinoan age||||||
18806|Umberatana Group|30511|6|Mentioned|p36|||||||||
18806|Umberatana Group|30516|6|Mentioned|p64|||||||||
18806|Umberatana Group|30621|5|Briefly described|p501|||Contains 2 glaciogenic units||||||
18806|Umberatana Group|30713|6|Mentioned|p106|||||||||
18806|Umberatana Group|30798|5|Briefly described|p114|||||||||
18806|Umberatana Group|30799|6|Mentioned|p2|||Stratigraphy and terminology.||||||
18806|Umberatana Group|30801|6|Mentioned|p5|||Adelaidean. Table P5-6.||||||
18806|Umberatana Group|30802|6|Mentioned|p1|||||||||
18806|Umberatana Group|30805|6|Mentioned|p1|||||||||
18806|Umberatana Group|30807|6|Mentioned|p102|||||||||
18806|Umberatana Group|30808|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|30810|6|Mentioned|p2|||Pualco Tillite is Basal formation.||||||
18806|Umberatana Group|30917|6|Mentioned|p36|||||||||
18806|Umberatana Group|30920|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18806|Umberatana Group|30982|6|Mentioned|p434|||||||||
18806|Umberatana Group|31022|6|Mentioned|Fig. 4|||||||||
18806|Umberatana Group|31109|6|Mentioned|p20|||See also P22, 24, 26, 28, 30.||||||
18806|Umberatana Group|31698|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|31923|6|Mentioned|p8|||||||||
18806|Umberatana Group|32144|6|Mentioned|p123|||Palaeotemperature||||||
18806|Umberatana Group|32146|6|Mentioned|p346|||||||||
18806|Umberatana Group|32319|6|Mentioned|p109|||Regional geology||||||
18806|Umberatana Group|32322|6|Mentioned|p109|||||||||
18806|Umberatana Group|32364|6|Mentioned|p18|||See also Fig.2||||||
18806|Umberatana Group|32505|6|Mentioned|Table 3|||||||||
18806|Umberatana Group|32510|6|Mentioned|p106|||||||||
18806|Umberatana Group|32511|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|32547|4|Described|p60|||Sturtian||||||
18806|Umberatana Group|32635|6|Mentioned|p5|||||||||
18806|Umberatana Group|32671|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|32720|6|Mentioned|p7|||Late Adelaidean||||||
18806|Umberatana Group|32721|6|Mentioned|p72|||L.Camb.||||||
18806|Umberatana Group|32722|6|Mentioned|Fig.3|||Adelaidean. Stromatolite||||||
18806|Umberatana Group|32723|6|Mentioned|p101|||See also P116||||||
18806|Umberatana Group|32724|4|Described|p509|||See also p510-532. Sturtian - Marinoan||||||22-JUN-09
18806|Umberatana Group|32726|6|Mentioned|p189|||Stromatolites||||||
18806|Umberatana Group|32954|6|Mentioned|p171|||||||||
18806|Umberatana Group|33004|6|Mentioned|PP136|||||||||
18806|Umberatana Group|33037|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|33404|5|Briefly described|p108|||Proterozoic.||||||
18806|Umberatana Group|33422|6|Mentioned|Map legend|Precambrian|Precambrian|||||||
18806|Umberatana Group|33423|4|Described|p13|||||||||
18806|Umberatana Group|33474|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|33490|6|Mentioned|p11|||Stratigraphy||||||
18806|Umberatana Group|33551|6|Mentioned|Fig.1|||Proterozoic||||||
18806|Umberatana Group|33655|6|Mentioned|p90|||||||||
18806|Umberatana Group|33691|6|Mentioned|p131|||||||||
18806|Umberatana Group|33692|6|Mentioned|Fig.2|||U.Prot.||||||
18806|Umberatana Group|33794|6|Mentioned|p7|||See also Fig.2||||||
18806|Umberatana Group|33954|6|Mentioned|p97|||See also Fig.4||||||
18806|Umberatana Group|33957|6|Mentioned|p36|||See also Fig.1||||||
18806|Umberatana Group|34175|5|Briefly described|p37|||||||||
18806|Umberatana Group|34176|6|Mentioned|p49|||Adelaidean. Units of the group described.||||||
18806|Umberatana Group|34185|6|Mentioned|p129|||||||||
18806|Umberatana Group|34202|6|Mentioned|p1056|||See also P1058. Precambrian||||||
18806|Umberatana Group|34285|6|Mentioned|p178|||||||||
18806|Umberatana Group|34287|6|Mentioned|p39|||"Sturtian"||||||
18806|Umberatana Group|34291|6|Mentioned|p11|||Adelaidean. See also PP13,17||||||
18806|Umberatana Group|34318|6|Mentioned|p86|||||||||
18806|Umberatana Group|34483|6|Mentioned|p113|||||||||
18806|Umberatana Group|34534|6|Mentioned|Fig.2.13|||||||||
18806|Umberatana Group|34535|3|Fully described|p63|||Marinoan - Sturtian. Fig.16||||||
18806|Umberatana Group|34536|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian-Marinoan||||||
18806|Umberatana Group|34537|6|Mentioned|Fig.10|||||||||
18806|Umberatana Group|34563|6|Mentioned|p67|||Correlation and stratigraphy||||||
18806|Umberatana Group|34587|6|Mentioned|p36|||Sturtian||||||
18806|Umberatana Group|34612|6|Mentioned|p98|||||||||
18806|Umberatana Group|34766|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34812|6|Mentioned|Table 8|||See also P4||||||
18806|Umberatana Group|34833|6|Mentioned|p76|||||||||
18806|Umberatana Group|34835|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34836|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34844|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|34957|6|Mentioned|p395|||||||||
18806|Umberatana Group|34985|6|Mentioned|p309|||||||||
18806|Umberatana Group|35075|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35143|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35158|6|Mentioned|p47|||||||||
18806|Umberatana Group|35195|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35200|6|Mentioned|Map legend|Proterozoic|Proterozoic|||||||
18806|Umberatana Group|35217|6|Mentioned|p172|||||||||
18806|Umberatana Group|35232|6|Mentioned|p5|||See also Table.1||||||
18806|Umberatana Group|35255|5|Briefly described|p9|||See also Fig.3 and P13.||||||
18806|Umberatana Group|35270|6|Mentioned|Fig.3|||||||||
18806|Umberatana Group|35327|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|35328|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|35353|6|Mentioned|Fig.2|||Regional geology||||||
18806|Umberatana Group|35543|6|Mentioned|Fig.1|||Regional bedrock geology.||||||
18806|Umberatana Group|35582|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|35586|6|Mentioned|p25|||||||||
18806|Umberatana Group|35628|6|Mentioned|p10|||||||||
18806|Umberatana Group|35675|6|Mentioned|p31|||||||||
18806|Umberatana Group|36003|5|Briefly described|p1030|||||||||
18806|Umberatana Group|36081|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36084|6|Mentioned|Fig.2|||See also P484.||||||
18806|Umberatana Group|36126|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36137|4|Described|p3|||||||||
18806|Umberatana Group|36212|5|Briefly described|p3|||||||||
18806|Umberatana Group|36514|6|Mentioned|p55|||||||||
18806|Umberatana Group|36623|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36731|4|Described|p124|||||||||
18806|Umberatana Group|36733|4|Described|p47|||||||||
18806|Umberatana Group|36833|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|36837|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|36839|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|36898|6|Mentioned|p182|||||||||
18806|Umberatana Group|37015|5|Briefly described|p68|||See also Fig.2.||||||
18806|Umberatana Group|37113|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|37238|6|Mentioned|p355|||||||||
18806|Umberatana Group|37461|6|Mentioned|p332|||||||||
18806|Umberatana Group|37501|6|Mentioned|p415|||||||||
18806|Umberatana Group|37627|6|Mentioned|p181|||||||||
18806|Umberatana Group|37932|6|Mentioned|p539|||||||||
18806|Umberatana Group|38004|6|Mentioned|p82|||||||||
18806|Umberatana Group|38068|4|Described|p68|||See also Fig.4.||||||
18806|Umberatana Group|38110|6|Mentioned|p2|||||||||
18806|Umberatana Group|38157|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|38243|6|Mentioned|Fig.6|||||||||
18806|Umberatana Group|38581|6|Mentioned|p252|||||||||
18806|Umberatana Group|38703|6|Mentioned|p131|||||||||
18806|Umberatana Group|38704|6|Mentioned|p133|||||||||
18806|Umberatana Group|39210|6|Mentioned|Table 3|||||||||
18806|Umberatana Group|39320|6|Mentioned|p380|||||||||
18806|Umberatana Group|39344|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39348|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39349|6|Mentioned|Map legend|Precambrian|Adelaidean|Marinoan to Sturtian||||||
18806|Umberatana Group|39350|6|Mentioned|Map legend|Precambrian|Precambrian|Sturtian||||||
18806|Umberatana Group|39351|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|39352|6|Mentioned|Map legend|Precambrian|Adelaidean|Sturtian to Marinoan||||||
18806|Umberatana Group|39635|6|Mentioned|Fig.2|||||||||
18806|Umberatana Group|39724|6|Mentioned|Fig.6|||||||||
18806|Umberatana Group|39762|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|39802|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|40003|5|Briefly described|Table 2|||||||||
18806|Umberatana Group|40105|6|Mentioned|p313|||||||||
18806|Umberatana Group|40228|5|Briefly described|Fig.1|||||||||
18806|Umberatana Group|40257|6|Mentioned|p287|||||||||
18806|Umberatana Group|40294|3|Fully described|p41|||||||||
18806|Umberatana Group|40442|4|Described|p8|||||||||
18806|Umberatana Group|40448|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|40456|6|Mentioned|p25|||||||||
18806|Umberatana Group|40490|6|Mentioned|Table II|||||||||
18806|Umberatana Group|40595|6|Mentioned|p92|||See also Fig.8||||||
18806|Umberatana Group|40763|6|Mentioned|p209|||||||||
18806|Umberatana Group|40852|5|Briefly described|p26|||||||||
18806|Umberatana Group|40856|5|Briefly described|p312|||||||||
18806|Umberatana Group|40906|6|Mentioned|Fig.9|||||||||
18806|Umberatana Group|40910|6|Mentioned|p11|||||||||
18806|Umberatana Group|40911|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
18806|Umberatana Group|40914|6|Mentioned|Map legend|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|41236|6|Mentioned|p65|||||||||
18806|Umberatana Group|41256|6|Mentioned|p7|||||||||
18806|Umberatana Group|41364|6|Mentioned|p151|||||||||
18806|Umberatana Group|41400|6|Mentioned|p27|||||||||
18806|Umberatana Group|41401|6|Mentioned|p29|||||||||
18806|Umberatana Group|41402|6|Mentioned|p42|||||||||
18806|Umberatana Group|41403|6|Mentioned|p54|||||||||
18806|Umberatana Group|41404|6|Mentioned|p73|||||||||
18806|Umberatana Group|41405|3|Fully described|p125|||||||||
18806|Umberatana Group|41429|6|Mentioned|p213|||||||||
18806|Umberatana Group|41493|6|Mentioned|Table 1|||||||||
18806|Umberatana Group|41496|5|Briefly described|Fig.1|||||||||
18806|Umberatana Group|41500|6|Mentioned|Fig.1|||||||||
18806|Umberatana Group|41526|6|Mentioned|p4|||||||||
18806|Umberatana Group|41647|6|Mentioned|p834|||||||||
18806|Umberatana Group|41703|6|Mentioned|Fig. 9|||||||||
18806|Umberatana Group|41770|6|Mentioned|p246|||||||||
18806|Umberatana Group|42028|6|Mentioned|p137|||||||||
18806|Umberatana Group|42087|5|Briefly described|p13|||||||||
18806|Umberatana Group|42088|5|Briefly described|p546|||||||||
18806|Umberatana Group|42096|6|Mentioned|p37|||||||||
18806|Umberatana Group|42098|4|Described|p53|||||||||
18806|Umberatana Group|42109|5|Briefly described|Fig.1 P19|||||||||
18806|Umberatana Group|42167|6|Mentioned|Fig.2 P115|||||||||
18806|Umberatana Group|42215|6|Mentioned|Fig.2 P448|||||||||
18806|Umberatana Group|42222|4|Described|p15|||||||||
18806|Umberatana Group|42223|6|Mentioned|Table 1 P38|||||||||
18806|Umberatana Group|42235|4|Described|p139|||See also Fig.3||||||
18806|Umberatana Group|42237|6|Mentioned|Fig.2 P86|||||||||
18806|Umberatana Group|42238|4|Described|p73|||||||||
18806|Umberatana Group|42239|6|Mentioned|p160|||||||||
18806|Umberatana Group|42240|6|Mentioned|Fig.2 P165|||||||||
18806|Umberatana Group|42243|4|Described|p211|||||||||
18806|Umberatana Group|42271|6|Mentioned|p372|||||||||
18806|Umberatana Group|42272|6|Mentioned|p402|||||||||
18806|Umberatana Group|42357|6|Mentioned|p9|||||||||
18806|Umberatana Group|42410|6|Mentioned|p3|||||||||
18806|Umberatana Group|42469|5|Briefly described|p22|||Stuart Shelf||||||
18806|Umberatana Group|42505|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
18806|Umberatana Group|42542|6|Mentioned|p11|||||||||
18806|Umberatana Group|42544|5|Briefly described|Fig.1 P17|||||||||
18806|Umberatana Group|42546|5|Briefly described|Map legend|Adelaidean (Marinoan)|Adelaidean (Sturtian)|||||||
18806|Umberatana Group|42600|6|Mentioned|p6|||||||||
18806|Umberatana Group|42643|6|Mentioned|Fig. 4 P19|||||||||
18806|Umberatana Group|42720|5|Briefly described|map legend|Marinoan|Sturtian|||||||
18806|Umberatana Group|42723|5|Briefly described|map legend|Sturtian||||||||
18806|Umberatana Group|42733|5|Briefly described|map legend|Adelaidean||||||||
18806|Umberatana Group|42736|5|Briefly described|map legend|Neoproterozoic||||||||
18806|Umberatana Group|42761|5|Briefly described|Fig.2 P8|||||||||
18806|Umberatana Group|42763|5|Briefly described|Fig.2 P21|||||||||
18806|Umberatana Group|42813|4|Described|p17|||||||||
18806|Umberatana Group|42871|5|Briefly described|p90|||||||||
18806|Umberatana Group|42882|5|Briefly described|p5, Table 1 p3|||Of Heysen Supergroup.||||||03-FEB-09
18806|Umberatana Group|43052|4|Described|p183,Table 6.1|||||||||
18806|Umberatana Group|43053|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone. Glaciomarine diamictite, sandstone and siltstone and aeolian sandstone (Stuart Shelf) at top.||||||26-MAY-05
18806|Umberatana Group|43086|6|Mentioned|Appendix, Stop 7|||||||||12-JUL-16
18806|Umberatana Group|43094|6|Mentioned|p35|||||||||
18806|Umberatana Group|43190|5|Briefly described|p29, Fig.2.|||||||||
18806|Umberatana Group|43258|5|Briefly described|Map Legend||Neoproterozoic|||||||
18806|Umberatana Group|43298|5|Briefly described|Map Legend||Adelaidean|||||||
18806|Umberatana Group|43390|14|Not recorded|p3,diag.p8|||||||||
18806|Umberatana Group|43595|5|Briefly described|p545||Neoproterozoic|||||||
18806|Umberatana Group|43742|6|Mentioned|p37||Neoproterozoic|||||||
18806|Umberatana Group|43845|5|Briefly described|Fig3 p43 etc||Neoproterozoic|||||||12-JUL-16
18806|Umberatana Group|44111|6|Mentioned|p.58 Fig. 2|||in Adelaide Geosyncline||||||
18806|Umberatana Group|44133|5|Briefly described|p46, 51 Fig. 7.18|Adelaidian|Adeladian|Diamictite, siltstone, sandstone, limestone.||||||
18806|Umberatana Group|44538|4|Described|map legend|||(H53-16). Geol.Atlas Series. Equivalents: Pernatty Grit. Woocalla Dolomite Member. Sturtian.||||||
18806|Umberatana Group|44659|5|Briefly described|map legend|||Sturtian-Marinoan, lithology.||||||
18806|Umberatana Group|44660|14|Not recorded|map legend|||Marinoan, lithology.||||||
18806|Umberatana Group|44689|14|Not recorded|map legend|||Andamooka. (H53-12).||||||
18806|Umberatana Group|44690|4|Described|map legend|||Geol. Atlas Series. (I/54-5). Includes, - Grampus Quartzite, Pepuarta Tillite, Tarcowie Siltstone, Pekina Fm., Tapley Hill Fm., Braemar Iron Fm., Appila Tillite, Kadlunga Slate, Gilbert Range Quartzite, Mintaro Shale,Leasingham Quartzite.Sturtian-Marinoan||||||
18806|Umberatana Group|44934|5|Briefly described|Map Legend||Adelaidean|||||||
18806|Umberatana Group|45149|6|Mentioned|Table 1|||Page 17.||||||
18806|Umberatana Group|45155|6|Mentioned|Fig.7|||Adelaide geosyncline||||||
18806|Umberatana Group|47009|6|Mentioned|p330|||||||||
18806|Umberatana Group|47012|6|Mentioned|p332|||||||||
18806|Umberatana Group|60712|5|Briefly described|p28 Fig. 1|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline.||||||31-MAY-05
18806|Umberatana Group|60718|4|Described|p48, p49 Fig. 1, p52, 55|Adelaidean|Adelaidean|Geological Province: Adelaide Geosyncline. See also p51 Fig. 3.|||Comprises Yudnamutana, Nepouie and Upalinna Subgroups.|Unconformably overlies Callanna or Burra Groups.||15-APR-11
18806|Umberatana Group|60953|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes Nepouie and Upalinna Subgroups.||||||
18806|Umberatana Group|60955|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Includes: Elatina Formation, Amberoona Formation, Tapley Hill Formation.||||||
18806|Umberatana Group|60959|5|Briefly described|Map Legend|Adelaidean|Adelaidean|Of the Heysen Supergroup.||||||
18806|Umberatana Group|61108|5|Briefly described|map legend|Adelaidean|Adelaidean|Mainly interglacial Nepouie Subgroup and Upalinna Subgroup. Marine and marginal marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone.||||||06-JUN-05
18806|Umberatana Group|61238|5|Briefly described|p44 Fig. 1|Neoproterozoic|Neoproterozoic|Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.||||||10-MAY-07
18806|Umberatana Group|61307|6|Mentioned|p5|||Geological Province: Adelaide Fold Belt.||||||
18806|Umberatana Group|61308|5|Briefly described|p6|Adelaidean|Adelaidean|Limestone, siltstone and glacial deposits.||||||30-JUN-06
18806|Umberatana Group|61732|5|Briefly described|p3 Fig. 2, p4 Fig. 3|Marinoan|Sturtian|Includes subgroups: Yudnamutana, Upalinna and Yerelina; and the 657+/-17Ma Marino Arkose Member. Geological Province: Adelaide Rift Complex/Stuart Shelf.||||||05-APR-13
18806|Umberatana Group|62085|4|Described|throughout|Cryogenian|Cryogenian||||Upalinna, Nepouie, Yudnamutana Subgroups; Enorama Shale; Holowilena Ironstone; Pualco, Wilyerpa, Tapley Hill, Sunderland, Etina, Trezona, Yaltipena, Elatina Formations.|||
18806|Umberatana Group|62453|5|Briefly described|p11 Fig. 7, 12 Fig. 8|Ediacaran|Cryogenian|Geological Province: Adeliade Rift Complex/Stuart Shelf.||||||
18806|Umberatana Group|62592|5|Briefly described|p50 Table 5.1.|Marinoan|Sturtian|Adelaide Geosyncline.||Unit in Heysen Supergroup.|Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.|Unconformably overlies Burra Group. Is disconformably overlain by Wilpena Group.||
18806|Umberatana Group|62664|5|Briefly described|p138 Fig.2.|Neoproterozoic|Neoproterozoic|||Unit in lower Heysen Supergroup.|Includes Yudnamutana and Willochra Subgroups and Tapley Hill Formation.|Unconformably overlies Burra Group. Is unconformably overlain by Wilpena Group.||
18806|Umberatana Group|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Includes the Yudnamutana Subgroup.||||||07-FEB-11
18806|Umberatana Group|62962|5|Briefly described|p2284 Fig. 2, p2296 Tab. 6|Adelaidean|Adelaidean|Age: 657+/-17Ma (Preiss, 2000). Geological Province: Mount Painter Province.||||||07-FEB-11
18806|Umberatana Group|63020|5|Briefly described|p973|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|63102|6|Mentioned|p7|Neoproterozoic|Neoproterozoic|Geological province: Curnamona Province. unconformably overlie, or are faulted against Palaeoproterozoic rocks in the Olary Domain to the west, south, and to a limited extent, the north.||||||
18806|Umberatana Group|63458|6|Mentioned|p897 Fig.19. |Cryogenian|Cryogenian|Adelaide Geosyncline.|||Includes Yudnamutana, Farina, Yerelina, Willochra Subgroups; Tapley Hill Formation; Brighton Limestone.|Is overlain by Wilpena Group.||
18806|Umberatana Group|64319|5|Briefly described|p354, p356 Fig.2, p357 Fig.3   |Neoproterozoic|Neoproterozoic|Mis-spelt as Umberatanna on p354.||||Overlies Burra Group. Is overlain by Wilpena Group.|Limestones, quartzites and shales.|
18806|Umberatana Group|64400|6|Mentioned|p4|||Contains the Nuccaleena Dolomite and Elatina Formation. In the Adelaide Rift Complex.||||||07-FEB-11
18806|Umberatana Group|64455|5|Briefly described|p138 Fig. 1|Cryogenian|Cryogenian|Includes Elatina Formation.||||||29-JAN-09
18806|Umberatana Group|64647|5|Briefly described|p38 Fig. 1, p40|Adelaidean|Adelaidean|Overlies Burra Group. Marine sediments.||||||
18806|Umberatana Group|64724|5|Briefly described|p49 Fig. 7|Ediacaran|Cryogenian|Deposited in the Adelaide Geosyncline during (and slightly after) the Centralian 2 event (~700-635 Ma)||||||
18806|Umberatana Group|64797|5|Briefly described|p151, p153 Fig.2, p160 Fig.8.|Ediacaran|Cryogenian|See also p162 Fig.9, p163 Tb.5, p165-166. Adelaide Rift Complex. S-isotope data.|||Includes Fortress Hill Formation.|||
18806|Umberatana Group|64801|6|Mentioned|p110-113, p119|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex. Interglacial shelf deposits.||Heysen Supergroup.|Yudnamutana, Yerelina Subgroups; Tapley Hill, Sunderland, Etina, Trezona, Yaltipena Formations; Enorama Shale.|Overlies Burra Group. Is overlain by Wilpena Group.||
18806|Umberatana Group|64829|5|Briefly described|p1084 Fig. 1|Neoproterozoic|Neoproterozoic|||||||07-FEB-11
18806|Umberatana Group|64846|6|Mentioned|p197 Fig.2, p198 Fig.3, p199  |Cryogenian|Cryogenian|See also p208 Fig.10, p212.|||Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.|||
18806|Umberatana Group|65313|6|Mentioned|p576 Fig. 5|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65365|5|Briefly described|p10 Fig. 4|Ediacaran|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Marino Arkose Member.||||||
18806|Umberatana Group|65366|5|Briefly described|p23 Fig. 3|Ediacaran|Cryogenian|Adelaide Rift Complex / Stuart Shelf. Includes Marino Arkose Member.||||||
18806|Umberatana Group|65376|6|Mentioned|p92 Fig. 2.82. |Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65379|6|Mentioned|p643|||Includes Tindelpina Shale Member, Tapley Hill Formation and Mount Curtis Tillite. Asbestos occurrence hosted in dolomite and/or limestones in this group.||||||07-MAR-12
18806|Umberatana Group|65483|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Underlies Tent Hill Formation (Wilpena Group).||||||28-JAN-11
18806|Umberatana Group|65493|4|Described|p907-10, 924, Fig 1,2|Cryogenian|Cryogenian|Thick interglacial succession, includes thick platform carbonate deposits. Age: U-Pb zircon 658 Ma (tuff). By correlation of the Ghaub (Nambia) and Nantuo (South China) Formations with the underlying Elatina Formation, an interval of >15 Ma is available for deposition of this sequence.||||||
18806|Umberatana Group|65892|6|Mentioned|p33 Fig.18.|Cryogenian|Cryogenian||||Includes Pualco, Wilyerpa, Tapley Hill, Sunderland, Etina, Trezona, Yaltipena and Elatina Formations; Holowilena Ironstone; Enorama Shale.|||
18806|Umberatana Group|65921|6|Mentioned|p2 (map legend)|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|65925|5|Briefly described|p124 Fig.3, Appendix 2.||||||Includes Merinjina Tillite, Tapley Hill and Balcanoona Formations.||Tillite; sandstone; siltstone; arkose; dolomite; quartzite; conglomerate; shale; greywacke.|
18806|Umberatana Group|66464|5|Briefly described|p167, p168 Fig.2|Cryogenian|Tonian|Adelaide Rift Complex. Glacimarine deposits containing diamictite, sandstone, siltstone, limestone, dolomite, conglomerate and shale. 659.7 Ma. Sturtian glaciation.||||||
18806|Umberatana Group|66518|5|Briefly described|p19 Fig.4, p23.|Neoproterozoic|Neoproterozoic|Coombalarnie Platform. c.550m of this unit overlies c.700m of Burra Group in an 11 x 14 km basin west of Kalkaroo in a potential geothermal project.|||Includes Yudnamutana Subgroup.|Unconformably overlies Burra Group. Is overlain unconformably by Wilpena Group.||
18806|Umberatana Group|66884|5|Briefly described|p36-37, p41 Fig.3|||Undifferentiated. Shown also as Lower Umberatana Group in Fig.3 and lower Umberatana Group in text. Thickness: >2200 m.||Heysen Supergroup|Tindelpina Shale Member||Diamictite: well-rounded, pebble to boulder conglomerate with clasts of granite, granite porphyry, quartzite and dolostone; polymict, basal pebble conglomerate interpreted as tillite deposits; dolomite-rich siltstone interpreted as loessite deposits.|14-DEC-16
18806|Umberatana Group|67180|5|Briefly described|p599-600, p608, p612, Figs. 1, 2|Cryogenian|Cryogenian|Established by Thomson et al (1964). Poor age constraints.|||Includes Nepouie Subgroup, Upalinna Subgroup, Yudnamutana Subgroup, Yerelina Subgroup|||
18806|Umberatana Group|67484|6|Mentioned|p294 Tb.1|Cryogenian|Cryogenian|Adelaide Rift Complex.|||Includes Nuccaleena, Elatina and Tapley Hill Formations; Sturtian Tillite.|||27-MAY-15
18806|Umberatana Group|67536|6|Mentioned|Map Legend||||||||Marine siltstone and sandstone; oolitic, sandy and stromatolitic limestone; overlain and underlain by glaciomarine successions of diamictite, sandstone and siltstone.|
18806|Umberatana Group|67620|6|Mentioned|p5|Cryogenian|Cryogenian|Adelaide Rift Complex.||||Is overlain by Wilpena Group.||
18806|Umberatana Group|67870|5|Briefly described|p5, p9-10, p13, p17-18, p20-21, p23-25|Neoproterozoic|Neoproterozoic|See also p29-33. Adelaide Rift System. Thickens towards the east. Produces indistinct sets of low amplitude, discontinuous seismic reflections. The base of this unit is a major erosional surface, making an obvious sequence boundary.|||Yudnamutana, Nepouie, Upalinna, Yerelina Subgroups.|Unconformably overlies Burra Group.||
18806|Umberatana Group|67979|4|Described|p527-p531, p536, p537, p542-543, p545|Marinoan|Sturtian|Of Northern and Central Flinders Ranges. In the Adelaide Geosyncline, the initial and terminal occurrences of the Sturtian (Yudnamutana Subgroup) and Marinoan (Yerelina Subgroup) glacials define the basal and upper-most contacts of this group respectively. A thick complex interglacial succession containing abundant carbonate units separates the two glacial deposits. Placement of Sturtian-Marinoan Series boundary, and the Nepouie-Upalinna Subgroup boundary outside the Northern Flinders Ranges is difficult. Type section located in far Northern Flinders Ranges in Tindelpina-Mt Saturday region (p536 Fig.7). Geol. Prov: Adelaide Geosyncline|||base to uppermost: Yudnamutana Subgroup, Nepouie Subgroup, Upalinna Subgroup and Yerelina Subgroup.|overlies Burra Group; is overlain by Wilpena Group|complex array of sedimentary successions|
18806|Umberatana Group|68030|6|Mentioned|p236,238|||Flinders Ranges. 4.5km thick and encompasses two main phases of glacial deposition.||Unit of Heysen Supergroup.|Includes Tapley Hill Formation.|||
18806|Umberatana Group|68067|6|Mentioned|Map legend.|||||||||27-AUG-13
18806|Umberatana Group|68068|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.|||Includes Yudnamutana, Nepouie and Upalinna Subgroups.|||
18806|Umberatana Group|68138|6|Mentioned|p156|Neoproterozoic|Neoproterozoic|Adelaide Rift Complex.|||Sturtian Tillite; Tapley Hill, Elatina, Nuccaleena Formations.|||
18806|Umberatana Group|68270|5|Briefly described|p683|Cryogenian|Cryogenian|Adelaide Rift Complex.|||Includes Elatina Formation, Tindelpina Shale Member, Marino Arkose Member and Sturt Tillite.|Overlain by Wilpena Group. Underlain by Burra Group.||
18806|Umberatana Group|68271|6|Mentioned|p694|||Adelaide Rift Complex.||||||
18806|Umberatana Group|68473|6|Mentioned|p531|||Adelaide Rift Complex.||||||
18806|Umberatana Group|68713|6|Mentioned|p19|||Deposited during the Sturt glaciation onto an unconformity surface.||||||
18806|Umberatana Group|69019|4|Described|p41-54, p144, p162.|Neoproterozoic|Neoproterozoic|Of Coats (1964); revised by Preiss et al. (1998). Includes tillites from Sturt and Elatina glaciations. Regional unconformity at the base.|||Includes Yudnamutana, Nepouie, Upalinna and Yerelina Subgroups.||Tillite, sandstone, siltstone, shale, arkose, dolomite, quartzite, greywacke and conglomerate.|
18806|Umberatana Group|69023|5|Briefly described|p63-72, p146-147|Neoproterozoic|Neoproterozoic|Defined by Coats (1964); revised by Preiss et al. (1998). Includes tillites from Sturtian and Marinoan glaciations.|||Includes Yudnamutana, Nepouie and Upalinna Subgroups.||Includes tillites.|
18806|Umberatana Group|69255|6|Mentioned|p771|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|69666|6|Mentioned|p27 Fig.3|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|69873|6|Mentioned|p82|||Adelaide Rift Complex. Included in diagram showing Cryogenian-Ediacaran stratigraphy and correlations with Tasmanian succession.||||||
18806|Umberatana Group|70013|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Interpreted as continental and marine sediments that accumulated within intra-continental rift basins.||||||
18806|Umberatana Group|70021|6|Mentioned|p97|Cryogenian|Cryogenian|Northern Flinders Ranges, Adelaide Geosyncline.||||||
18806|Umberatana Group|70031|5|Briefly described|p245|Cryogenian|Cryogenian|Adelaide Geosyncline.|||Incldues Yerelina, Upalinna, Nepouie and Yudnamutana subgroups.|Overlain disconformably to unconformably by Wilpena Group/Nuccaleena Formation.||
18806|Umberatana Group|70323|5|Briefly described|p213|Cryogenian|Cryogenian|Central Flinders Ranges, Adelaide Geosyncline.|||Includes Nepouie and Yudnamutana subgroups.|Underlain by Burra Group.||
18806|Umberatana Group|70334|5|Briefly described|p19-20,30,38,47,77,81-82,90|Neoproterozoic|Neoproterozoic|Geological province: Gawler Craton. Of Adelaide Geosyncline and Stuart Shelf. Represents the first major episode of sedimentation (basinal marine to coastal) on the Stuart Shelf during the Neoproterozoic, recording the major Sturtian and marinoan glaciation events. Underwent erosion over the Cultana Inlier during fault reactivation of the Cultana Fault.|||Includes Yerelina, Upalinna and Nepouie subgroups.|Overlain by Wilpena Group.||
18806|Umberatana Group|70384|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Adelaide Geosyncline.  Age shown more specifically as Sturtian to Marinoan [Cryogenian].||Of Heysen Supergroup.|Includes Yudnamutana, Nepouie, Upalinna, Yerelina Subgroups.|||23-JAN-19
18806|Umberatana Group|70405|6|Mentioned|p50|Neoproterozoic|Neoproterozoic|||||||
18806|Umberatana Group|70406|6|Mentioned|p121 Fig 5|||||||Overlain by Wilpena Group.||09-MAY-16
18806|Umberatana Group|70407|5|Briefly described|p102 Fig 1, p103 Fig 2, p111, 112|Neoproterozoic|Neoproterozoic|Age: Sturtian - Marinoan||Of Heysen Supergroup.|Includes Pualco Tillite,  Holowilena Ironstone, Warcowie Dolomite, Tarcowie Siltstone, Etina Formation, Enorama Shale, Trezona Formation.|||
18806|Umberatana Group|70657|5|Briefly described|p8, p54|Neoproterozoic|Neoproterozoic|Curnamona Province.||||Unconformably overlies Burra Group.|Low-grade metasedimentary rocks.|
18806|Umberatana Group|70660|6|Mentioned|p34 fig 19e|||||||||
18806|Umberatana Group|70790|6|Mentioned|p258, p260 Fig.2|Neoproterozoic|Neoproterozoic||~700-620 Ma.|||||
18806|Umberatana Group|70819|6|Mentioned|p11, 13, 29|Neoproterozoic|Neoproterozoic|Clare Valley.|||Yudnamutana, Nepouie Subgroups.|Unconformably overlies Belair Subgroup.||
18806|Umberatana Group|71037|5|Briefly described|p22-23 Fig.2, p27 Fig.6|Neoproterozoic|Neoproterozoic|Shown only on the Six Mile Hill 1:75,000 surface geology map and p27 Fig.6. Age shown as Sturtian to Marinoan.|||Includes Tapley Hill Formation, Whyalla Sandstone, Upalinna Subgroup and Yerelina Subgroup.||Sandstone, siltstone and conglomerate.|
18806|Umberatana Group|71129|4|Described|p17,21, 99, 101,107,109,111-117|Neoproterozoic|Neoproterozoic|Geological Province: Gawler Craton. Represented by basinal marine to coastal to fluvial sedimentation in SIX MILE HILL. Some outcrops and subcrops of flat-lying kaolinitic conglomerates, sandstones and shales in the Myall Creek Homestead and Myall Creek Opal Mine are tentatively assigned to the upper part of this group; these may be correlatives of the Whyalla Sandstone or the 'Yudnapinna Beds'-Wilmington Formation. Historically difficult to distinguish between Whyalla Sandstone and Yudnapinna Beds-Wilmington Formation/Upalinna Subgroup in the southwestern Stuart Shelf, and therefore sandstone successions intersected in drillholes between Tapley Hill and Tent Hill formations are variably interpreted as Whyalla sandstone or undifferentiated Umberatana Group. Maximum depositional age constrained by Re-Os age of 643+\-2.5 Ma age for the basal Tapley Hill Formation. Minimum age constrained by c. 635 Ma based on correlation of overlying Nuccaleena Formation with correlative Marinoan glacial deposits and associated cap carbonates. See also p126,134,138,184,208,225,227,.|||Includes Whyalla Sandstone, Upalinna Subgroup Yerelina Subgroup, and Nepouie Subgroup.|Overlain by Tent Hill Formation. Underlain unconformably by Broadview Schist.||13-NOV-19
18806|Umberatana Group|71130|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age range shown as Sturtian into Marinoan.|||Upalinna and Yerelina Subgroups; Tapley Hill Formation, Whyalla Sandstone.|||
18806|Umberatana Group|71131|5|Briefly described|Map legend.|Neoproterozoic|Neoproterozoic|Age range shown as Sturtian into Marinoan.|||Upalinna and Yerelina Subgroups; Tapley Hill Formation, Whyalla Sandstone.|||
18806|Umberatana Group|71236|6|Mentioned|p28|||||||||
18806|Umberatana Group|71237|4|Described|p7-12|||New name.||||||
18806|Umberatana Group|71238|14|Not recorded|p1,2, 10|||||||||
18806|Umberatana Group|71240|14|Not recorded|p7|||||||||
18806|Umberatana Group|71241|14|Not recorded|p13, 14, 15, p9-10|||||||||
18806|Umberatana Group|71317|6|Mentioned|p15|Neoproterozoic|Neoproterozoic|Gawler Craton.||||||
18806|Umberatana Group|71322|5|Briefly described|p52 Fig.1|Neoproterozoic|Neoproterozoic||||||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale, greywacke.|
18806|Umberatana Group|71712|6|Mentioned|p411||Neoproterozoic|||||||
18806|Umberatana Group|71895|5|Briefly described|p10, p11 fig 2, p150-p151, APP4. p4, |||Stuart Shelf.|||Includes the Tapley Hill Formation, Brighton Limestone and Whyalla Sandstone.|Unconformably overlies the Beda Basalt. Overlain by the Wilpena Group.||
18806|Umberatana Group|72247|5|Briefly described|p43|Neoproterozoic|Neoproterozoic|Of Adelaide Geosyncline.||||Overlain by Wilpena Group. Underlain unconformably by Pandurra Formation.||
18806|Umberatana Group|72429|5|Briefly described|p952, p958|Sturtian|Sturtian|Mount Chambers Gorge, eastern Flinders Ranges.|||Includes the Tapley Hill Formation and the Wockerawirra Dolomite.|Underlies the Wilpena Group.|Red-brown weathered, blue-grey to green, thinly-laminated, part-flaggy siltstone and shales. Dolomitic in part.|
18806|Umberatana Group|72450|5|Briefly described|Brochure, Brochure map||||c. 650 Ma||Includes the Sturt Tillite, Tapley Hill Formation, Brighton Limestone, Angepena Formation, Marino Arkose, Wilmington Formation, Elatina Formation.|||
18806|Umberatana Group|72456|5|Briefly described|Map Legend|Neoproterozoic|Neoproterozoic|Marree 1:250k map sheet.|||||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale and greywacke.|
18806|Umberatana Group|72461|6|Mentioned|p19|Neoproterozoic|Neoproterozoic|Adelaidean Geosyncline.||||||
18806|Umberatana Group|72473|6|Mentioned|p2, p4|||Flinders Ranges, central. Brackets the Sturtian and Marinoan glaciations. The complete group is exposed within a relatively small area within the Enorama Diapir.||||||
18806|Umberatana Group|72489|6|Mentioned|p4 Fig.3|Cryogenian|Cryogenian|Adelaide Rift Complex. Only shown on p4 Fig.3. Simplified geological maps.||||||
18806|Umberatana Group|72601|6|Mentioned|p1, p5, p11, p25|Cryogenian|Cryogenian|Adelaide Rift Complex. Probably partly correlates with the Aralka Formation.||Heysen Supergroup|Tapley Hill Formation, Balcanoona Formation, Wockerawirra Dolomite, Enorama Shale, Wundowie Limestone Member, Tindelpina Shale Member|||
18806|Umberatana Group|72613|6|Mentioned|p2 fig 1, p3|Cryogenian|Cryogenian|Northern Flinders Ranges. Incorporates strata deposited during the Sturtian glaciation,  a nonglacial period between and the younger Marinoan glaciation. A tuff horizon from the uppermost Sturtian diamictite (Merinjina Diamictite/Tillite)  is dated at 663.03 +/- 0.11 Ma (Cox et al, 2018).|ca. 650 Ma||Includes the Angepena Formation, Elatina Formation, Yankaninna Formation,  Amberoona Formation, Enorama Shale, and the Weetootla Dolomite, Yudnamutana Subgroup.|||
18806|Umberatana Group|73092|6|Mentioned|p2|Cambrian|Neoproterozoic|||||||
18806|Umberatana Group|73188|5|Briefly described|p: 305, 315-316, 330, ~339-342, 351-352|Neoproterozoic|Neoproterozoic|Mount Lofty Ranges. Deposited under mainly sag-phase conditions.|||Yerelina Subgroup, Upalinna Subgroup, Nepouie Subgroup, Yudnamutana Subgroup, and units therein|||
18806|Umberatana Group|73222|5|Briefly described|p5-6, p20, p23|Cryogenian|Tonian|Adelaide Rift Complex. Sturtian to Marinoan. Thickness: 6 to 10,000 m. Deposited in glacial, glaciomarine, interglacial and post-glacial marine shelf settings. Records the Keele Peak [positive carbon isotope] excursion and the Trezona [negative carbon isotope] excursion.||Heysen Supergroup|||Diamictite, conglomerate, sandstone, and laminated siltstone.|
18806|Umberatana Group|73227|6|Mentioned|p23-25|Neoproterozoic|Neoproterozoic||||Whyalla Sandstone, Tapley Hill Formation, Elatina Formation, Brighton Limestone, Beda Basalt, Backy Point, Yudnapinna beds|||
18806|Umberatana Group|73234|6|Mentioned|p5-6, p20-21||||||Tapley Hill Formation, Brighton Limestone, Whyalla Sandstone, Yerelina Subgroup, Marino Arkose Member, Wilyerpa Formation|||
18806|Umberatana Group|73236|6|Mentioned|p35-36, p38|Ediacaran|Ediacaran|Marine sedimentary rocks.||Heysen Supergroup|Yerelina Subgroup, Upalinna Subgroup, Nepouie Subgroup, Yudnamutana Subgroup, and units therein|[Unconformably] overlain by Seacliff Sandstone (Sandison Subgroup, Wilpena Group).||
18806|Umberatana Group|73251|6|Mentioned|p36|Neoproterozoic|Neoproterozoic|Coombalarnie Platform.|||Yudnamutana Subgroup|Unconformably underlain by Burra Group. Unconformably overlain by Wilpena Group.|Metasediments.|
18806|Umberatana Group|73253|6|Mentioned|p16|||Adelaide Fold Belt. [Reworking] would contribute a zircon population centred on c. 1140 Ma coupled with zircons from age groupings 1900-1550 Ma and 2700-2100 Ma.||||||
18806|Umberatana Group|73262|6|Mentioned|p583|[Ediacaran?]|[Ediacaran?]|Includes the intervals of the Sturtian and Marinoan Glaciations.||Heysen Super Group|||Tillite, sandstone, siltstone, arkose, dolomite, quartzite, conglomerate, shale, greywacke.|
18806|Umberatana Group|74367|5|Briefly described|p3, p5-7, p15, p19, p21-22|||Thick interglacial succession up to ~4.5 km thick. Age of 713+/-38 Ma is pooled from from the Angepena Formation and Tapley Hill Formation (Webb et al., 1983) however the Tapley Hill Formation age has been confirmed as inaccurate.|713+/-38 Ma (middle part)|Heysen Supergroup|Yudnamutana Subgroup, Nepouie Subgroup, Upalinna Subgroup, Yerelina Subgroup|||
18806|Umberatana Group|75063|6|Mentioned|p94 Fig.2|||Northern Flinders Ranges area.||||||
18839|Ungarie Granite|22434|6|Mentioned|11 fig 14|Silurian|Silurian|Geol province Lachlan Fold Belt||||||
18839|Ungarie Granite|22508|5|Briefly described|p2||Silurian|Of the Koetong Supersuite. In the Lachlan Fold Belt.||||||13-JUN-13
18839|Ungarie Granite|22638|4|Described|p54|Early Devonian|Ludlow|Age: 403 +/- 8 Ma on biotite, 410 +/- 8 Ma on hornblende, K/Ar dating. Previously "Wyalong Granite", "Wyalong Granodiorite"||||||24-SEP-19
18839|Ungarie Granite|23365|5|Briefly described|8|Silurian|Silurian|||||||
18839|Ungarie Granite|24007|6|Mentioned|p325|||||||||
18839|Ungarie Granite|24417|3|Fully described|p52|Early Silurian|Early Silurian|Includes the former "Wyalong Granite" and "Wyalong Granodiorite".||||||
18839|Ungarie Granite|29907|6|Mentioned|p38|||||||||
18839|Ungarie Granite|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
18839|Ungarie Granite|31995|6|Mentioned|p36|||||||||
18839|Ungarie Granite|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
18839|Ungarie Granite|36316|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
18839|Ungarie Granite|40328|4|Described|p211|||Also mentioned on p42.||||||26-MAR-08
18839|Ungarie Granite|40365|6|Mentioned|p290|||||||||
18839|Ungarie Granite|42726|5|Briefly described|map legend|Silurian||Wagga Batholith.||||||
18839|Ungarie Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
18839|Ungarie Granite|44534|5|Briefly described|map legend|Devonian|Silurian|SI 55-6. Siluro-Devonian.||||||25-JUN-17
18839|Ungarie Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
18839|Ungarie Granite|50385|5|Briefly described|Map Legend|Silurian|Silurian|Medium-grained biotite granodiorite and granite||||||
18839|Ungarie Granite|60009|5|Briefly described|Map Legend|Llandovery|Llandovery|Of the Ungarie Suite.||||||13-JUL-04
18839|Ungarie Granite|61964|5|Briefly described|p14 Fig. 4, p37-38, p41 Tb. 2|Early Silurian|Early Silurian|Of Koetong Suite (Koetong Supersuite). S-type. Includes a northern extension known as the Derrida Phase. Unconformably overlain by Tullibigeal Leucitite as well as Quaternary aeolian sandsheets. Age: ~428.2Ma and 433+/-2Ma (SHRIMP), Lith.details given.||||||
18839|Ungarie Granite|62034|5|Briefly described|p26|Silurian|Silurian|Geological Province: Lachlan Orogen.||||||10-APR-06
18839|Ungarie Granite|62367|5|Briefly described|p10|Early Silurian|Early Silurian|Fractionated S-type granite. Age: 433+/-2Ma (U-Pb SHRIMP zircon; LP Black pers.comm 1998).||||||31-MAY-06
18839|Ungarie Granite|62405|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Contains the Derrida Phase. Medium-grained  equigranular to sporadically porphyritic biotite granodiorite and granite with biotite-rich microgranular enclaves and metasedimentary xenoliths.||||||26-MAR-08
18839|Ungarie Granite|64568|5|Briefly described|Map legend|Silurian|Silurian|Of the Koetong Suite. Medium-grained biotite granodiorite and granite; and includes an unnamed subunit of equigranular, fine- to medium-grained cordierite biotite granite.||||||
18839|Ungarie Granite|65469|5|Briefly described|p18|Early Silurian|Early Silurian|Lachlan Orogen.||Koetong Suite||||
18839|Ungarie Granite|69160|5|Briefly described|Map legend|Early Silurian|Early Silurian|||Unit in Koetong Suite.|||Medium-grained biotite granodiorite and granite.
|
18839|Ungarie Granite|70751|5|Briefly described|p4-p5, p8, p10, p12, p38|Late Silurian|Late Silurian|Rocks belonging to the Derrida Granite have been reinterpreted to belong to the Ungarie Granite instead on the basis of geophysical and whole-rock geochemical data.|||||Medium-grained, S-type granite.|
18839|Ungarie Granite|70777|5|Briefly described|p1, p46, p52-p53, p60, p79-p80|Wenlock|Llandovery|Lachlan Orogen. An additional age of 433.4 +/- 2.5 from Lyons (2000) is also provided. Previously included the southern outcrop of the Wargin Granite.|434.4 +/- 2.3 Ma  (Lyons et al., 2000)|Koetong Supersuite||Coeval with the Buddigower and Yalgogrin Granites.|S-type, felsic, unfractionated granite.|
18839|Ungarie Granite|71213|5|Briefly described|p94|Silurian|Silurian|Of Griffin (1960). Regarded as co-magmatic with Kikoira Granite, Ardlethan Granite.|||||generally grey in colour, fine to coarse in grainsize, with both biotite and muscovite present singly or together in various specimens.|25-JUN-17
18839|Ungarie Granite|71693|5|Briefly described|Map legend.|Silurian|Silurian|||Koetong Supersuite.|||Medium-grained equigranular to sporadically porphyritic biotite granodiorite and granite, with biotite-rich microgranular enclaves and metasedimentary xenoliths.|
18839|Ungarie Granite|72958|6|Mentioned|p11|Wenlock|Wenlock|Basement to Cobar Basin.||||||
18839|Ungarie Granite|73578|6|Mentioned|p50|Ludfordian|Homerian|An age of 426.3 +/- 3.3 Ma was reported by Downes et al. (2016).|426.3 +/- 3.3 Ma|||||
18966|Upson Downs Sandstone|22831|6|Mentioned|p 74|||||||||
18966|Upson Downs Sandstone|29986|6|Mentioned|Map legend|Devonian|Silurian|Silurian-Devonian||||||
18966|Upson Downs Sandstone|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
18966|Upson Downs Sandstone|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
18966|Upson Downs Sandstone|40328|4|Described|p45|||||||||
18966|Upson Downs Sandstone|48958|6|Mentioned|Plate 1|||||||||
18968|Ural Volcanics|22857|4|Described|p438 App.1, Tb.A1.6|Pragian|Lochkovian|Of Rast Group (Cobar Supergroup). White to black vitric and crystal rhyolites, reworked volcanics; minor cherty sediments, conglomerate to shale. Contains crinoids. Correlates with Shepherds Hill Volcanics. Geol. Prov: Rast Trough (Darling Basin).||||||
18968|Ural Volcanics|29987|4|Described|p16|||||||||
18968|Ural Volcanics|31161|5|Briefly described|PA2|||||||||
18968|Ural Volcanics|32088|6|Mentioned|p2|||||||||
18968|Ural Volcanics|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
18968|Ural Volcanics|32672|6|Mentioned|p672|||||||||
18968|Ural Volcanics|34109|6|Mentioned|p170|||||||||
18968|Ural Volcanics|34405|5|Briefly described|p127|||||||||
18968|Ural Volcanics|34406|6|Mentioned|p220|||Probably Middle Silurian||||||
18968|Ural Volcanics|34449|6|Mentioned|Table 2-1|||||||||
18968|Ural Volcanics|35163|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
18968|Ural Volcanics|36316|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
18968|Ural Volcanics|36317|5|Briefly described|p144|||||||||
18968|Ural Volcanics|36318|6|Mentioned|p14|||||||||
18968|Ural Volcanics|41394|6|Mentioned|p83|||||||||
18968|Ural Volcanics|42726|5|Briefly described|map legend|||||||||
18968|Ural Volcanics|43389|14|Not recorded|Map Legend||Silurian|||||||
18968|Ural Volcanics|44534|5|Briefly described|map legend|||SI 55-6. Silurian?||||||
18968|Ural Volcanics|60303|5|Briefly described|p5, p6 Fig. 1|Early Devonian|Silurian|Age is Middle Silurian to Early Devonian.  Geological Province: Lachlan Fold Belt.||||||
18968|Ural Volcanics|61964|3|Fully described|p14 Fig. 4, p72|Emsian|Lochkovian|Detailed nomenclatural history provided. A-type. Conformably overlies the Preston Formation, and Crossleys Tank Formation where the former disappears. Thickness: ~1km (in Ural Range area). Geol.Prov: Rast Trough.  Geophysics (p226); Palaeontology(p260)|410+/-8 Ma to 424+/-6 Ma U/Pb SHRIMP 2001|||||10-MAR-16
18968|Ural Volcanics|62034|5|Briefly described|p27|Devonian|Silurian|Sequence of submarine to subaerial silicic lavas, shallow intrusions, volcanic-rich turbidites and resedimented debris. Conformably overlies the Preston Formation.  Geological Province: Lachlan Orogen.||||||10-APR-06
18968|Ural Volcanics|62367|5|Briefly described|p4 Fig. 2, p5|Early Devonian|Late Silurian|Of the Rast Group. Felsic rocks. Geological Province: Rast Trough.||||||02-JUN-06
18968|Ural Volcanics|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Rast Group. Includes the Bootoowa Fossil Member and the Karingal Rhyolite Member.||||||
18968|Ural Volcanics|63019|5|Briefly described|p919-920|Early Devonian|Early Devonian|First named by Griffin (1960) as part of Cargelligo Group. Mainly submarine, rhyolitic to dacitic lavas and sills.Conformably overlies Crossleys Tank Formation (Rast Group). Thickness: ~1000m. Geol.province: Lachlan Orogen. See also p925, p939, p943.||||||
18968|Ural Volcanics|63025|5|Briefly described|p1052 Fig. 1, p1053|Pragian|Lochkovian|Geological Province: Delamerian Orogen.||||||
18968|Ural Volcanics|63891|5|Briefly described|p235-237, p245|||Of Rast Group. A-type. Felsic, volcaniclastic, volcanic, non-volcanic sedimentary. Upper Ural Volcanics mapped as age-equivalent, may underlie Walters Range Group. Overlies Crossleys Tank Fm; Preston Fm. Age 421+/-2Ma LA-ICPMS U/Pb zircon. ~1000m thick.||||||03-JUN-08
18968|Ural Volcanics|65469|5|Briefly described|p18, p43, p52, p62|Early Devonian|Late Silurian|Lachlan Orogen.||||||
18968|Ural Volcanics|69161|5|Briefly described|Map legend|Early Devonian|Early Devonian|Four un-named facies are mapped separately: slate, phyllite, mudstone, with sparse quartz-lithic sandstone interbeds; crystal-rhyolite-pumice breccia with fiamme; porphyritic rhyolite; matrix-rich breccia.||Unit in Rast Group.||Overlies Crossleys Tank Formation.|Undifferentiated rhyolitic-dacitic coherent volcanic and volcaniclastic rocks.|
18968|Ural Volcanics|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|Also includes 15 un-named but separately-mapped sub-units, mainly rhyolites, breccias and sandstones.||Unit in Rast Group.|Includes Bootoowa Fossil Member and Karingal Rhyolite Member.||Undifferentiated rhyolitic-dacitic coherent volcanic and volcaniclastic rocks.|
18968|Ural Volcanics|70296|6|Mentioned|p1, p10|||Potentially related to the Gurragong Volcanics and the Nyora Granite based on dating in this report.||||||
18968|Ural Volcanics|70751|4|Described|p7, p11-p12, p27-p28, p38|Silurian|Silurian|Formerly the Shepherds Hill Volcanics. Submarine to subaerial depositional environment. A-type. Present study shows this unit is not contemporaneous or co-magmatic with the Mount Hope Group.|412.2 +/- 2.6 Ma (SHRIMP, this study)||||Felsic volcanic rocks.|
18968|Ural Volcanics|70950|6|Mentioned|p1046|||||Of Rast Group?||||
18968|Ural Volcanics|71039|6|Mentioned|p22, p25|||||||||
18968|Ural Volcanics|71693|5|Briefly described|Map legend.|Devonian|Devonian|||Rast Group.||Overlies Preston and Crossleys Tank Formations.|Silicic coherent facies with less voluminous volcaniclastic facies and minor sedimentary facies. Rhyolitic to dacitic lavas, breccias and intrusions; volcaniclastic sandstone and siltstone, minor slate, phyllite, mudstone.|
18968|Ural Volcanics|72958|6|Mentioned|p6, p11, p57, p61|Lochkovian|Pridoli|Cobar Basin. Nymagee area. Comparable ages to the unnamed hornblende-phyric dacite sill, hosted within the Meryula Formation.|412.2 +/- 2.5 Ma|Rast Group||Underlain by Crossleys Tank Formation.||
18968|Ural Volcanics|73175|5|Briefly described|p1062|Early Devonian|Early Devonian|Cobar Basin, southern part. Similar to Louth Volcanics with linear- to curvilinear trends of moderate-to-high magnetic intensity.|412-410 Ma|Rast Group|||Includes minor mafic to intermediate facies including andesite, and diorite to leucogabbro dykes and sills.|
18968|Ural Volcanics|73179|6|Mentioned|p1134 Fig.1, p1151, p1153-1155|Silurian|Siluran|Cobar Basin, Central Lachlan Orogen.||||||20-SEP-22
18971|Uralla Granodiorite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Equigranular hornblende-biotite granodiorite with mafic and/or porphyritic variants.||||||
18971|Uralla Granodiorite|23720|5|Briefly described|Map Legend|||Of Uralla Plutonic Suite.  Medium-grained hornblende-biotite granodiorite.||||||15-DEC-04
18971|Uralla Granodiorite|24366|5|Briefly described|p9 Fig. 7|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.||||||
18971|Uralla Granodiorite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
18971|Uralla Granodiorite|30787|6|Mentioned|p49|||Differentation index||||||
18971|Uralla Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology and geochemistry.||||||
18971|Uralla Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
18971|Uralla Granodiorite|31140|6|Mentioned|Fig. 1|||Refers Flood (1971, upubl.)||||||
18971|Uralla Granodiorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
18971|Uralla Granodiorite|38288|6|Mentioned|Fig.12|||||||||
18971|Uralla Granodiorite|41603|6|Mentioned|p21|||||||||
18971|Uralla Granodiorite|41990|6|Mentioned|p10|||||||||
18971|Uralla Granodiorite|42866|5|Briefly described|Table 2, P12|||||||||
18971|Uralla Granodiorite|43091|5|Briefly described|Map legend|||||||||
18971|Uralla Granodiorite|44450|5|Briefly described|p102|||Geological Province: New England Fold Belt. Age most likely to be late Middle Permian p35.||||||
18971|Uralla Granodiorite|68111|5|Briefly described|p968 Tb.1|Anisian|Olenekian||251 - 246 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
18971|Uralla Granodiorite|69323|5|Briefly described|p13-14,41,70|Late Permian|Late Permian|Geological province: New England Orogen. Shaw et al., 1994 reported Rb-Sr age of 351-246 Ma.||Unit of Uralla Supersuite.||Intrudes into "Uralla volcanics' and Khatoun Tonalite.||
18971|Uralla Granodiorite|71628|4|Described|p8:3, 8, 55-56, 58, 60, 62, 65-67|||See also p8: 70-77, 79, 110-111, 115-116. Binns et al. (1967) after unpublished work by Ransley and Flood. A large triangular pluton (c.23 x 12km) with flat to low relief. Crops out as large tors, locally stacked, and dome-like platforms. Other age determinations given. Geochemistry described. Associated with the historically significant Uralla goldfield. RELATED UNITS (continued): Intrudes Sandon beds, Wandsworth Volcanic Group, Terrible Vale Porphyritic Microgranodiorite, Yarrowyck Granodiorite, Glenburnie Leucomonzogranite and ?Blackfellows Gully Leucomonzogranite.|248.5 Ma (Rb-Sr biotite; Shaw, 1994).|Uralla Suite.||Abuts/intrudes Khatoun and Wilhelmshohe Tonalites (possibly gradationally). Is intruded by Tolleys Gully Leucomonzogranite and Uralla Granodiorite. See COMMENTS for more.|Grey, coarse-grained, approximately equigranular, biotite-hornblende-(pyroxene) granodiorite, with minor monzogranite; finer-grained, porphyritic marginal variant. I-type.|
18973|Uralla Suite|22580|6|Mentioned|p99|||||||||
18973|Uralla Suite|22857|6|Mentioned|p204 Fig. 17.2|||Plutonic suite in the New England Batholith. See also p243 Fig. 18.4.||||||
18973|Uralla Suite|22859|6|Mentioned|Fig17.2p204|||||||||
18973|Uralla Suite|22863|6|Mentioned|Fig18.4p243|||||||||
18973|Uralla Suite|23050|5|Briefly described|p9 Fig.2|Triassic|Triassic|Of Central Block.||||||17-NOV-08
18973|Uralla Suite|24366|6|Mentioned|p13|||||||||
18973|Uralla Suite|38822|6|Mentioned|p193|||Geological Province: New England Fold Belt||||||
18973|Uralla Suite|38839|6|Mentioned|p244|||Geological Province: New England Fold Belt.||||||17-NOV-08
18973|Uralla Suite|38905|6|Mentioned|p307|||Geological Province: New England Fold Belt.||||||17-NOV-08
18973|Uralla Suite|42876|6|Mentioned|p142|||||||||
18973|Uralla Suite|42984|5|Briefly described|p365|||||||||
18973|Uralla Suite|60079|5|Briefly described|Map Legend|Late Permian|Permian|Includes: Wards Mistake Adamellite, Wellingrove Granodiorite.||||||20-JUL-04
18973|Uralla Suite|60422|5|Briefly described|p386|||Of the New England Batholith. Also classified as Supersuites (Chappell and Bryant).||||||
18973|Uralla Suite|61793|6|Mentioned|p342 Fig. 1(b)|||Includes Wards Mistake Adamellite.||||||07-FEB-11
18973|Uralla Suite|61795|6|Mentioned|p368|Early Triassic|Late Permian|Geological Province: New England Fold Belt. I-type granites.||||||17-NOV-08
18973|Uralla Suite|69323|5|Briefly described|p41|||Geological province: New England Orogen.||Unit of Uralla Supersuite.|Includes Khatoun Tonalite.|||
18973|Uralla Suite|71280|5|Briefly described|p410|Early Triassic|Permian||||||I-type plutonic rocks.|
18973|Uralla Suite|71628|5|Briefly described|p7-18; p8: 2-3, 49-79, 109, 118; p11-17|||Southernmost Suite, with some of the most mafic intrusives, in the Supersuite.||Uralla Supersuite.|Uralla Granodiorite; Khatoun, Wilhelmshohe Tonalites; Terrible Vale, Manuka Farm, Porphyritic Microgranodiorites; Kentucky Quartz Diorite.||Granites.|
18975|Urambie Granodiorite|41394|2|Defined|p30|Early Silurian||Reserved as Urambie Granite||||||
18975|Urambie Granodiorite|41395|6|Mentioned|Map legend|Silurian||||||||
18975|Urambie Granodiorite|41528|5|Briefly described|p15|||||||||
18975|Urambie Granodiorite|41821|6|Mentioned|p11 Fig.5|||Occurs in Kilparney sheet area||||||
18975|Urambie Granodiorite|42566|6|Mentioned|p37|||||||||
18975|Urambie Granodiorite|42954|6|Mentioned|p68|||||||||
18975|Urambie Granodiorite|43089|5|Briefly described|Map Legend|||||||||
18975|Urambie Granodiorite|43757|6|Mentioned|p510|||||||||
18975|Urambie Granodiorite|69801|4|Described|p1, p4, p18-p20, p22-23, p135-136|Middle Silurian|Middle Silurian|Central Lachlan Orogen. This unit is the most northerly of the 10 mid silurian S-type granites. Age indistinguishable from that of nearby Erimeran Granite. Sample locality, petrography, SHRIMP analyses and interpretation are detailed. Previously included in the Koetong Supersuite.|428.0 +/- 1.7 Ma (Isaacs, 2000)|||Intrudes the Wagga Group.|S-type, gray-white, medium  to coarse-grained and porphyritic biotite granodiorite.|
18975|Urambie Granodiorite|70751|6|Mentioned|p9-p10, p12, p28, p38|Silurian|Silurian||428 +/- 1.7 Ma (Bodorkos et al, 2015 SHRIMP)||||Porphyritic granodiorite.|
18975|Urambie Granodiorite|72958|6|Mentioned|p11|Wenlock|Wenlock|Basement to Cobar Basin.||||||
18975|Urambie Granodiorite|73578|6|Mentioned|p50|Gorstian|Homerian|An age of 428.1 +/- 1.7 Ma was reported by Bodorkos et al. (2015).|428.1 +/-1.7 Ma|||||
18976|Urana Formation|22531|5|Briefly described|p20|Permian|Carboniferous|||||||
18976|Urana Formation|22532|5|Briefly described|map legend|Permian|Carboniferous|||||||
18976|Urana Formation|22773|5|Briefly described|Fig24.5p350|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22799|2|Defined|p17|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22857|4|Described|p238, p504 App.1 Tb.A1.8|Early Permian|Late Carboniferous|Max. thickness: 900m. Geological Province: Infrabasin sediments below the Murray Basin. Correlated with Cape Jervis Formation. Geological Province: Tasman Epicratonic Province. See also p350 Fig.24.5.||||||
18976|Urana Formation|22863|6|Mentioned|p238|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22864|5|Briefly described|p259||Early Permian|||||||
18976|Urana Formation|22887|3|Fully described|p29, Fig.5 p12|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|22893|2|Defined|p21 table3|Early Permian|Early Permian|Unit confined to infrabasins below Murray Basin. Fine-gr.quartzose sandstone, abundantly chloritic at top and pyritic throughout; sandstone, conglomerate, +diamictite + clasts of qtz., quartzite, black shale and pyrite traces.Cape Jervis Formation equivs.||||||22-FEB-12
18976|Urana Formation|22971|4|Described|p18, p26|Permian|Carboniferous|Entirely marine deposits - grey to black organic-rich mudstone and siltstone with marine fossils indicating Early Permian age. Max. thickness: 900m.  Present in Ovens Graben and Numurkah Trough.||||||19-JAN-06
18976|Urana Formation|23252|5|Briefly described|Map Legend||Permian|||||||
18976|Urana Formation|23309|6|Mentioned|p189||Early Permian|||||||
18976|Urana Formation|24177|4|Described|p66, p14|Permian|Late Carboniferous|Thickness may be up to 1000m. Considered the glaciomarine equivalent of Wild Duck Formation. Geological Province: Murray Basin||||||
18976|Urana Formation|24328|5|Briefly described|Map legend|Permian|Permian|||||||
18976|Urana Formation|24329|5|Briefly described|Map legend|Permian|Permian|||||||
18976|Urana Formation|24551|5|Briefly described|p212||Permian|Maximum Thickness: 887m.||||||
18976|Urana Formation|40324|2|Defined|p63|Early Permian|Late Carboniferous|Late Carboniferous to Early Permian||||||
18976|Urana Formation|41637|5|Briefly described|p208|||||||||
18976|Urana Formation|42454|5|Briefly described|p11|||Variation on Urana Formation, NSW. Late Carboniferous to Early Permian?||||||
18976|Urana Formation|42827|5|Briefly described|p209|||||||||
18976|Urana Formation|42966|3|Fully described|p58|||||||||
18976|Urana Formation|43052|5|Briefly described|Table 2.1|||||||||
18976|Urana Formation|43218|4|Described|Fig.3 p22, p26|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|43627|6|Mentioned|p16|||||||||
18976|Urana Formation|43841|4|Described|7||Early Permian|Overlain unconformably by Coorabin Coal Measures. 50m thickness drilled in Ovens Valley, may be 200m.||||||27-OCT-08
18976|Urana Formation|44093|5|Briefly described|p145 App. 1|Permian|Carboniferous|See also p245 Appendix 1. Geological Province: Kanmantoo Fold Belt.||||||
18976|Urana Formation|44133|5|Briefly described|p44, 65 Fig. 8.4, 70|Permian|Carboniferous|Geological Province: Nadda Basin. Thickness: 395m.||||||
18976|Urana Formation|44188|5|Briefly described|Map Legend|Late Permian|Early Permian|Of the Millewa group. Geological province: Kanmantoo Fold Belt/Lachlan Fold Belt. Fine-grained quartzose sandstone.||||||15-MAY-08
18976|Urana Formation|44191|5|Briefly described|Map Legend|Early Permian|Late Carboniferous|||||||
18976|Urana Formation|60529|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||14-JUN-06
18976|Urana Formation|60591|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60592|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60593|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60595|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated||||||
18976|Urana Formation|60596|5|Briefly described|Map Legend|Permian|Carboniferous|Unconformably overlies the Castlemaine Supergroup. Unconformably overlain by the Renmark Group and Calivil Formation. Marine deposits: clay, minor pebbles; semi-consolidated to unconsolidated.||||||27-OCT-08
18976|Urana Formation|60597|5|Briefly described|Map Legend|Carboniferous|Carboniferous|Marine deposits: no distinctive magnetic responses||||||
18976|Urana Formation|60599|2|Defined|p76, p14|Early Permian|Carboniferous|Prev'ly Cape Jervis Beds. Three main facies: massive to lam'd siltst.+mudst; massive to parallel lam'd sst with rare pebbles + mud clasts; fine- to med.gr.diamictite.Thickness:880m in type section. Unconformable below Renmark Gp, Calivil + Shepparton Fms.||||||27-OCT-08
18976|Urana Formation|61163|6|Mentioned|p28|||Geological Province: Lachlan Fold Belt.||||||
18976|Urana Formation|61185|5|Briefly described|p53|Permian|Late Carboniferous|Do not outcrop on NAGAMBIE. Intersected in bore hole. Consists of blue, blue-grey, grey-white and mottled brown clay. No fossils recorded.||||||07-FEB-11
18976|Urana Formation|61701|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|61702|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|61703|5|Briefly described|Map Legend|Permian|Carboniferous|Marine sediments: clay and fine- to coarse-grained sand; semi-consolidated.||||||
18976|Urana Formation|66623|5|Briefly described|p231.|Permian|Permian|Ivanhoe Trough. Broadly correlated with Yanna Tank Formation, and with Cape Jervis Formation in SA.|||||Grey and laminated claystones, interbeds of fine-grained quartz sandstone and siltstone, basal tilloids and basal conglomerate.|
18976|Urana Formation|69798|5|Briefly described|p4, p11-16, p17 Fig.14, p18-19|Permian|Permian|Oaklands Basin. Early Permian. Glaciogene marine deposits in the lower part are overlain by paralic then marine deposits. Seismic profiles.|||Cocketgedong Member.|Unconformably overlies Boorhaman Conglomerate. Is overlain by Coorabin Coal Measures.||06-FEB-18
18976|Urana Formation|70125|5|Briefly described|p396-397|Permian|Permian|Oaklands Basin. 887m of glacio-marine deposits. Early Permian. Origins and ages of sediments detailed.|~290 Ma.|||Is overlain by Coorabin Coal Measures.||
18976|Urana Formation|70718|5|Briefly described|p21|Permian|Late Carboniferous|Ovens Graben. Predominatly marine sediments.||||||
18976|Urana Formation|71593|4|Described|p44, p46, p48-p49|Permian|Permian|Glacial deposits. Maximum thickness up to 370m. Preserved in the Netherby Trough. Intersected in Gunamalary 2. See also p85, p203.|||||Fluvioglacial sedimentary outwash and till deposits.|
18976|Urana Formation|73228|5|Briefly described|p50-54|Permian|Permian|Nadda Basin. Renmark Trough, Canegrass Lobe, and Paringa Embayment. Glacigene. Unconformably underlain by a sequence of Devonian clastics of the Darling Basin. At least 395 m thick, although may be thicker in the Renmark Trough. Glaciomarine to glaciolacustrine; appears to represent a proglacial to post- or non-glacial sequence. Identified in Cooltong 1, Berri North 1, Nadda 1, and Overland Corner 1 drillholes.||||Unconformably underlain by Kanmantoo Group. Overlain[?] by Pyap Member (Monash Formation).|Shale, siltstone, sandstone and diamictite with occasional conglomeratic and carbonaceous intervals; dropstones are common in the finer clastics.|
18976|Urana Formation|73229|5|Briefly described|p66-68, p70, p74|Permian|Permian|Nadda Basin. [Analysed using pXRF; see article].|||||Shale, siltstone, sandstone, diamictite and conglomerate of the glacigene.|
18976|Urana Formation|73496|6|Mentioned|Map legend|Cisuralian|Pennsylvanian|||||||
18976|Urana Formation|73497|5|Briefly described|Map legend|Permian|Permian||||||Marine to fluvial deposits beneath Renmark Group: no distinctive magnetic or radiometric responses.|
18992|Uriarra Volcanics|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Includes Tarpaulin Creek Sandstone Member. Dacite lavas and tuff, shale lenses. BMR map symbol: Suu.||||||
18992|Uriarra Volcanics|22768|6|Mentioned|p176|||||||||
18992|Uriarra Volcanics|22857|4|Described|p176, p464 App. 1 Tb.A1.6|Late Silurian|Late Silurian|Unconformably overlies the Hawkins Suite.||||||
18992|Uriarra Volcanics|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
18992|Uriarra Volcanics|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
18992|Uriarra Volcanics|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
18992|Uriarra Volcanics|31111|6|Mentioned|p172|||See also P174, 176, 178, 182, 186, 188||||||
18992|Uriarra Volcanics|33325|5|Briefly described|Table 2|||Mention P13.||||||
18992|Uriarra Volcanics|34405|5|Briefly described|p119|||See also P120.||||||
18992|Uriarra Volcanics|35109|6|Mentioned|p16|||||||||
18992|Uriarra Volcanics|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Includes Tarpaulin Creek Ashstone Member at (or near?) base. Extrusive. ?I-type. Dark grey to pink rhyodacite ignimbrite and air-fall tuff. Unconformably underlies Mountain Creek Volcanics. BMR map code: Svu.||||||
18992|Uriarra Volcanics|37727|4|Described|p91|||See also P27.||||||
18992|Uriarra Volcanics|37728|6|Mentioned|Table 4|||||||||
18992|Uriarra Volcanics|38251|6|Mentioned|p59|||||||||
18992|Uriarra Volcanics|40328|4|Described|p132|||||||||
18992|Uriarra Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
18992|Uriarra Volcanics|42820|6|Mentioned|p26|||||||||
18992|Uriarra Volcanics|43159|4|Described|Fig.2 p4,P6,P8,p10.||Ludlovian|Of Laidlaw Suite.||||||20-MAY-08
18992|Uriarra Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv3||||||
18992|Uriarra Volcanics|45147|2|Defined|M159|early Ludlovian|early Ludlovian|Prob.Early Ludlovian||||||
18992|Uriarra Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
19031|Vale Beder Ignimbrite|30069|6|Mentioned|p7|||||||||
19031|Vale Beder Ignimbrite|31852|6|Mentioned|p111|||Gedinnian. See also Figs. 1 & 2||||||
19031|Vale Beder Ignimbrite|33325|5|Briefly described|Table 2|||See also Table 3.||||||
19031|Vale Beder Ignimbrite|35386|6|Mentioned|Fig.3|||Revision of nomenclature, refers to Link(1970,1971)||||||
19031|Vale Beder Ignimbrite|37727|6|Mentioned|p40|||||||||
19031|Vale Beder Ignimbrite|45075|6|Mentioned|Fig.1|||||||||
19043|Valley View Metabasic Igneous Complex|42313|2|Defined|p61|Late Silurian|Middle Silurian|Reserved as Valley View Serpentinite in 1984. Age: early Middle Silurian to Late Silurian||||||
19043|Valley View Metabasic Igneous Complex|42314|5|Briefly described|Map legend|Early Silurian|Middle Silurian|||||||
19043|Valley View Metabasic Igneous Complex|67322|6|Mentioned|p20|Pridoli|Ludlow|Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 sheet: (Basden, 1990).||Of the Jindalee Group||||
19057|Vanity Member|40328|6|Mentioned|Fig.12(H3)|||||||||
19057|Vanity Member|45147|6|Mentioned|M159|||||||||
19066|Vaux Coal Member|29942|4|Described|Fig.1|||Permian||||||
19066|Vaux Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19066|Vaux Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19066|Vaux Coal Member|40805|6|Mentioned|Table 1|||||||||
19066|Vaux Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Burnamwood Formation.||||
19069|Vauxhall Formation|24042|5|Briefly described|p511|||||||||
19069|Vauxhall Formation|35187|6|Mentioned|p57|||||||||
19069|Vauxhall Formation|35372|5|Briefly described|p106|||See also Table 1.||||||
19078|Verandah Creek Diorite|40328|4|Described|p211|||||||||
19078|Verandah Creek Diorite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
19083|Verulam Oolite Member|22857|5|Briefly described|p500 App.1 Tb.A1.7|Visean|Tournaisian|Of the Wootton beds (included as part of the Flagstaff Formation on p510 App.1 Tb.A1.8). Limestone, oolith-bearing sandstone. Max. thickness: 55m. Geological Province: Tamworth Forearc Basin.||||||
19083|Verulam Oolite Member|30074|6|Mentioned|p8|||See also P10||||||
19083|Verulam Oolite Member|36528|6|Mentioned|p178|||||||||
19083|Verulam Oolite Member|39302|5|Briefly described|p347|||||||||
19083|Verulam Oolite Member|42547|4|Described|p34|||||||||
19083|Verulam Oolite Member|43576|6|Mentioned|p351|||||||||
19083|Verulam Oolite Member|44244|4|Described|p73, p128|Tournaisian|Tournaisian|Widespread oolite in the Barrington district.  Accommodates the Verulam Oolite Lens within Lostock Sandstone Member of Flagstaff Formation - and is known as the Verulam Oolite Member of the Wootton beds.  Max. thick: 55m.||||||16-SEP-04
19083|Verulam Oolite Member|46803|6|Mentioned|p148|||||||||
19083|Verulam Oolite Member|50147|5|Briefly described|Map legend|Visean|Visean|Grey, cross-bedded oolitic limestone within grey mudstone interbeds in the Lostock Sandstone Member of the Flagstaff Formation (Gresford Block);  and within the Wootton Beds (Western Myall Block).||||||
19109|Victoria Tunnel Coal|22578|6|Mentioned|Fig.9 p399|||||||||
19109|Victoria Tunnel Coal|23055|6|Mentioned|Fig5p12,15,18|||||||||
19109|Victoria Tunnel Coal|39292|6|Mentioned|p108|||See also p110, Fig.6.6.||||||
19109|Victoria Tunnel Coal|39308|6|Mentioned|p467|||See also p472.||||||
19109|Victoria Tunnel Coal|39609|6|Mentioned|Table 1|||||||||
19109|Victoria Tunnel Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Victoria Tunnel coal seam instead and is now considered part of the Adamstown Formation. See also p113.||Of Lambton Subgroup||||
19109|Victoria Tunnel Coal|73304|6|Mentioned|p75|||||Adamstown Formation, Newcastle Coal Measures||||
19123|Violet Hill Volcanic Member|22857|4|Described|p512 App.1 Tb.A1.8|Late Carboniferous|Early Carboniferous|Of the Yagon Siltstone. Basal conglomerate with dacitic boulders; dacitic volcanics overlain by tuffaceous sandstone and siltstone. Max. thickness: >120m.||||||
19123|Violet Hill Volcanic Member|32868|6|Mentioned|p208,Fig.7|||||||||
19123|Violet Hill Volcanic Member|36057|2|Defined|p348|Westphalian|Namurian|Namurian - Westphalian. Of Yagon Siltstone.||||||
19123|Violet Hill Volcanic Member|38801|6|Mentioned|p124 Fig.4|||Of Yagon Siltstone||||||
19123|Violet Hill Volcanic Member|39660|6|Mentioned|p450|||||||||
19123|Violet Hill Volcanic Member|44244|4|Described|p212, p207 Fig. 41|Westphalian|Visean|Of the Yagon Siltstone.  Max. thickness: 120m.  Type section in text.  Geological Province: Myall Block.||||||26-AUG-04
19123|Violet Hill Volcanic Member|50263|5|Briefly described|Map Legend|Westphalian|Namurian|Of the Yagon Siltstone.  Geological Province: Eastern Myall Block.||||||
19123|Violet Hill Volcanic Member|65380|5|Briefly described|p670|Visean|Visean|of Yagon Siltstone. SHRIMP age 331 +/-5 Ma (Roberts et al 1995)|SHRIMP age 331 +/- 5 Ma (Roberts et al. 1995).|Of Yagon Siltstone.||||27-MAR-12
19123|Violet Hill Volcanic Member|73487|6|Mentioned|p568 Fig.3, p577|Serpukhovian|Serpukhovian|||||||
19196|Wagonga Group|22815|3|Fully described|fig9, p9,15,121|Early Silurian|Late Cambrian|||||||
19196|Wagonga Group|22857|5|Briefly described|p89 Fig. 14.7A, p117|Late Cambrian|Cambrian|See also p432 App. 1 Tb. A1.5.||||||
19196|Wagonga Group|22858|6|Mentioned|Fig14.7ap88-9|||||||||
19196|Wagonga Group|23213|5|Briefly described|Fig.10|Bolindian|Cambrian|Age: Cambrian to Early Bolindian. Of Narooma Terrane.||||||02-OCT-15
19196|Wagonga Group|23245|5|Briefly described|p103,117,123,135||Cambrian|||||||
19196|Wagonga Group|42448|6|Mentioned|p7|||Variation of Wagonga beds, Wagonga Formation etc.||||||
19196|Wagonga Group|43233|5|Briefly described|Map Legend|Late Ordovician|Middle Cambrian|||||||
19196|Wagonga Group|44093|5|Briefly described|p225 App. 1|Ordovician|Cambrian|See also pp94 and 117. Includes Kianga Basalt, Narooma Chert and Bogolo Formation. Geological Province: Lachlan Fold Belt.||||||25-JAN-06
19196|Wagonga Group|60902|5|Briefly described|p859, p861 Fig.2a|||Superseded the Wagonga Formation and comprises Narooma Chert overlain by Bogolo Formation. Adjacent to Adaminaby Group. Consists of volcanics overlain by chert. Geological Province: Narooma Terrane.||||||05-MAR-12
19196|Wagonga Group|61731|5|Briefly described|p1035-1040|||Conformably overlies Adaminaby Group. Geological Province: Lachlan Fold Belt/Narooma Terrane.||||||
19196|Wagonga Group|62070|5|Briefly described|p33 ,p34 Fig.1, p39,p40,|Late Ordovician|Cambrian|Middle Cambrian to Late Ordovician rocks. Crops out around Batemans Bay and Narooma. Strongly deformed.|||||Includes chert, black shale, mafic volcanics, and broken formation containing quartzose-turbidite and mafic volcanic blocks. Strongly deformed.|
19196|Wagonga Group|67322|5|Briefly described|p4 Fig.2, p26; Fig.5|Bolindian|Late Cambrian|Narooma Terrane. Modified from Wagonga Series of Browne (1949); first named and defined as the Wagonga Group by Glen (1994). The upper black shales within this unit contain graptolite fauna of Eastonian and Bolindian age. These black shales possibly correlate with the Narooma Chert. Type area around Narooma.|||Narooma Chert, Bogolo Formation|||22-FEB-18
19196|Wagonga Group|67849|4|Described|p21, p22, p23, p27, p29 Fig.9, p30. |Ordovician|Cambrian|Lachlan Orogen. Continental and oceanic rocks with thrust faults displacing rocks of disparate ages. Easternmost part of a westward-dipping accretionary complex in the Batemans Bay area. Kubler Index measurements show this unit experienced much the same metamorphic conditions as Adaminaby Group. Underplating and associated metamorphism occurred c.460-440 Ma.||Unit in Narooma Accretionary Complex.|Includes Narooma Chert and Bogolo Formation.|Is overlain conformably by, and interfingers with, Adaminaby Group.|Includes chert, basalt, para-autochthonous limestone units, turbidites.|
19196|Wagonga Group|68255|5|Briefly described|p1049-p1051, p1057, p1059, p1061-p1064|Ordovician||Sequences within this unit have reached lower greenschist metamorphic grade.|||Includes Narooma Chert and Bogolo Formation.|Interfingered by lenses of the Adaminaby Group.|Contains the Narooma Chert, Bogolo Formation, undifferentiated chert, basalt and parautochthonous limestone units, undifferentiated turbidites, and interfingering lenses of the Adaminaby Group.|20-JUL-15
19196|Wagonga Group|68309|5|Briefly described|p224-226, 230-232|Ordovician|Cambrian|Occurs at two locations: Batemans Bay and Narooma. At the former, thrust faulting causes units to interfinger, and slivers of Adaminaby Group and undifferentiated metasiltstone, metasandstone and slate also occur. At Narooma, is part of a stack of imbricate thrust slices. Basalt chemical analyses tabulated, discussed.|||Narooma Chert, Bogolo Formation.|Conformably overlies (locally thrust- faulted against) Adaminaby Group.|Chert, shale and siltstone (comparable to Narooma Chert); chaotic clast-in-matrix melange (Bogolo Formation); interbedded silt- and sandstone; and one unit of basaltic breccia and associated limestone clasts and beds (crops out at Burrewarra Point).|
19196|Wagonga Group|68466|6|Mentioned|p64-66|Late Ordovician|Late Cambrian|Narooma Terrane.|||Narooma Chert, Bogolo Formation.|||
19196|Wagonga Group|69541|6|Mentioned|p648|Ordovician|Cambrian|Rocks near the c.100 Ma Mount Dromedary Igneous Complex contain Cretaceous zircons: mentioned to demonstrate zircon crystallisation in older rocks from younger hydrothermal or magmatic fluids.||||||
19196|Wagonga Group|69668|6|Mentioned|p929 Fig.2, p932|Late Ordovician|Late Cambrian|Narooma terrane. Interpreted either as an exotic terrane or an accretionary complex.|||Includes Narooma Chert and Bogolo Formation.|||
19196|Wagonga Group|70026|4|Described|p37-40,49, p52|Ordovician|Middle Cambrian|Geological province: Lachlan Orogen. Well exposed along the coast between the basal Sydney Basin succession north of Batemans Bay and the Adaminaby Group at Tomakin. Locally contains altered OIB basalt at Melville Point and Barlings Beach, NSW. Highly deformed, with tight folds, foliations, quartz veining and fault breccia (Miller and Gray 1996, 1997; Fergusson and Frikken 2003; Glen et al. 2004; Prendergast 2007; Prendergast and Offler 2012).|||Includes Kianga Basalt, Narooma Chert and Bogolo Formation.|Overlain by (or interfingers with) the Adaminaby Group.|Numerous fault slices with middle Cambrian to Upper Ordovician units of chert and/or siliceous mudstone with an upper conformable and/or gradational boundary to a unit of mudstone and conglomerate, with altered OIB basalts.|17-JUL-19
19196|Wagonga Group|70601|4|Described|p23-28, p34, p36-42, p45-50, p53-55, p57|Late Ordovician|Middle Cambrian|Onshore geology: preserved as a series of thrust sheets. Mafic volcanic rocks have ocean island, tholeiitic and boninitic basalt affinities. Geochemistry detailed. "Broken formation". Eastonian and lower Bolindian graptolites and upper Darriwilian to lower Gisbornian conodonts. Allochthonous: derived from Narooma Terrane. Contains basalt clasts from "Seamount Basalt". Various models of formation discussed. Timing and duration of deformation/metamorphism discussed. Includes basalts at Batemans Bay formerly mapped as Kianga Basalt (now superseded).|||Bogolo Formation, Narooma Chert, Wagonga Chert.|In Narooma Accretionary Complex|Deformed, cleaved, metabasalts, schists (foliated calcite-chlorite-albite-epidote), slates, serpentinite, cherts and carbonates, metamorphosed to greenschist/lower amphibolite facies. Fine-grained stylolitic banded marble; limestone with OIB basalt.|
19196|Wagonga Group|70661|6|Mentioned|p14|||||||Either faulted against or conformably overlain by Adaminaby Group||
19196|Wagonga Group|70684|6|Mentioned|p7 Fig.1||||||||Ocean-floor cherts.|
19196|Wagonga Group|70752|6|Mentioned|p125|Middle Cambrian|Middle Cambrian|Organophosphatic brachiopod faunas have been described from limestone blocks/parautochthonous limestone beds of this unit.||||||
19196|Wagonga Group|73059|5|Briefly described|p1055|Ordovician|Cambrian|Exposed east of Melville Point, south coast NSW. Part of a subduction complex.||||Is overlain by Adaminaby Group.|Mafic volcanic rocks, limestone, quartz-rich turbidites, mudstone and melange; widespread altered basalts.|
19229|Walgett Formation|23053|6|Mentioned|Fig10p17|||||||||
19229|Walgett Formation|35187|6|Mentioned|Fig.2|||||||||
19229|Walgett Formation|35372|5|Briefly described|p105|||See also Table 1.||||||
19229|Walgett Formation|61155|5|Briefly described|p19|Pleistocene|Pleistocene|Overlies the Warrend Formation. Age: <1.0Ma. Thickness: 10m. In the Walgett area.||||||
19233|Walhalla Group|12100|5|Briefly described|p819|Early Devonian|Early Devonian|Upward fining succession with an upward decrease in lithic content; very rapidly deposited.||Upper Group of the Yarra Supergroup.||||08-MAY-12
19233|Walhalla Group|22530|6|Mentioned|p698|||||||||
19233|Walhalla Group|22570|4|Described|p189|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|22603|6|Mentioned|p99||Emsian|||||||
19233|Walhalla Group|22628|6|Mentioned|p115|||Emsian in age||||||
19233|Walhalla Group|22729|5|Briefly described|p584,91||Early Devonian|||||||
19233|Walhalla Group|22768|6|Mentioned|p188||Emsian|||||||
19233|Walhalla Group|22857|5|Briefly described|p188|Emsian|Emsian|Contains Emsian fossils in the Melbourne Zone. Overlain by Cathedral Group.||||||
19233|Walhalla Group|22882|5|Briefly described|p 12|Devonian|Devonian|||||||
19233|Walhalla Group|22885|5|Briefly described|map|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|22886|5|Briefly described|p14|||||||||
19233|Walhalla Group|22971|5|Briefly described|p 18|||Thick- to thin-bedded sandstone turbidites and mudstone, and minor conglomerate.  Overlies Jordan River Group.||||||19-JAN-06
19233|Walhalla Group|23229|5|Briefly described|p26, 31, 33, 35|Zlichovian||||||||
19233|Walhalla Group|23264|5|Briefly described|Fig13-3.1p324||Early Devonian|||||||
19233|Walhalla Group|23265|6|Mentioned|p339, 342|||||||||
19233|Walhalla Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
19233|Walhalla Group|23309|5|Briefly described|p146, 148, 154-155. Table 2.25||Devonian|||||||
19233|Walhalla Group|23522|5|Briefly described|p247 Fig 3|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|23710|14|Not recorded|p74|||Depositional characteristics.||||||
19233|Walhalla Group|23938|6|Mentioned|p118|Devonian|Devonian|Hornfelsed sediments. See also p124 Fig. 59.||||||25-SEP-08
19233|Walhalla Group|24002|5|Briefly described|p237|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|24004|5|Briefly described|p277|||||||||
19233|Walhalla Group|24098|6|Mentioned|p27 Fig. 2|Middle Devonian|Emsian|Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||19-APR-05
19233|Walhalla Group|24177|4|Described|p59, p50 Fig.22|Middle Devonian|Early Devonian|Overlain by the Cathedral Group. Overlies the Wilson Creek Group. Geological Province: Mount Easton Province. Comprises two formations - Norton Gully Sandstone and Montys Hut Formation.||||||15-JAN-09
19233|Walhalla Group|24328|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes the Norton Gully Sandstone and Montys Hut Formation.||||||
19233|Walhalla Group|24329|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Norton Gully Sandstone and Montys Hut Formation.||||||21-OCT-08
19233|Walhalla Group|24383|6|Mentioned|p88 Fig.57|||Geological Province: Lachlan Fold Belt||||||
19233|Walhalla Group|24551|5|Briefly described|p88 Fig. 3.15, p123, p170 Fig. 6.10|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|24576|5|Briefly described|p744|Early Devonian|Early Devonian|Geological Province: Lachlan Fold Belt.||||||21-OCT-08
19233|Walhalla Group|24588|5|Briefly described|p23, p12 Fig.3|Emsian|Lochkovian|Overlies Wilson Creek Shale of Jordan River Group. Underlies Cathedral Group conformably. Geological Province: Mount Easton Province. Ar/Ar deformation age (cleavage in slate) 372+/-2 Ma? But older ages obtained for cover successions eg Marysville Igneous Complex.||||||29-NOV-13
19233|Walhalla Group|30245|6|Mentioned|p77|||Refers Talent(1965), Bell(1955)||||||
19233|Walhalla Group|30246|6|Mentioned|p192|||||||||
19233|Walhalla Group|30905|6|Mentioned|p161|||||||||
19233|Walhalla Group|30906|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
19233|Walhalla Group|30930|6|Mentioned|Map legend|Early Devonian|Early Devonian|Includes Centennial Beds, Coopers Creek Formation.||||||
19233|Walhalla Group|31161|5|Briefly described|PA10|||||||||
19233|Walhalla Group|31339|6|Mentioned|p426|||||||||
19233|Walhalla Group|32074|5|Briefly described|p180|||||||||
19233|Walhalla Group|33156|6|Mentioned|p130|||||||||
19233|Walhalla Group|33159|6|Mentioned|p16|||Faunas||||||
19233|Walhalla Group|33238|4|Described|p642|||||||||
19233|Walhalla Group|33393|6|Mentioned|p130|||||||||
19233|Walhalla Group|33459|6|Mentioned|Table 1|||||||||
19233|Walhalla Group|33601|2|Defined|p21|Middle Devonian|Early Devonian|Early - Middle Devonian.||||||14-JAN-09
19233|Walhalla Group|33602|6|Mentioned|p4|||||||||
19233|Walhalla Group|33604|6|Mentioned|p17|||L.Dev. Correlation chart||||||
19233|Walhalla Group|33607|6|Mentioned|Map legend|Devonian|Devonian|||||||
19233|Walhalla Group|33732|5|Briefly described|Table III|||Dev. Correlation chart.||||||21-OCT-08
19233|Walhalla Group|34815|6|Mentioned|p18|||||||||
19233|Walhalla Group|34843|4|Described|p6|||||||||
19233|Walhalla Group|34954|6|Mentioned|Fig.34|||Analysis Fig.33.||||||
19233|Walhalla Group|34990|6|Mentioned|p446|||||||||
19233|Walhalla Group|35073|6|Mentioned|p3|||||||||
19233|Walhalla Group|35112|6|Mentioned|p276|||||||||
19233|Walhalla Group|35274|6|Mentioned|p420|||||||||
19233|Walhalla Group|35281|6|Mentioned|p16|||||||||
19233|Walhalla Group|35283|6|Mentioned|p55|||||||||
19233|Walhalla Group|36389|6|Mentioned|p41|||||||||
19233|Walhalla Group|37270|6|Mentioned|p203|||||||||
19233|Walhalla Group|37727|6|Mentioned|p65|||||||||
19233|Walhalla Group|38420|6|Mentioned|Fig.5|||||||||
19233|Walhalla Group|38787|6|Mentioned|p143|||||||||
19233|Walhalla Group|39331|6|Mentioned|Table 2-1|||||||||
19233|Walhalla Group|39551|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
19233|Walhalla Group|39555|6|Mentioned|Map legend|Zlichovian|Zlichovian|||||||
19233|Walhalla Group|40761|6|Mentioned|p226|||||||||
19233|Walhalla Group|41554|4|Described|p421|||||||||
19233|Walhalla Group|41555|4|Described|p405|||||||||
19233|Walhalla Group|41571|6|Mentioned|Fig.2.7|||||||||
19233|Walhalla Group|41585|4|Described|p115|||Mention p103. Briefly described p112.||||||14-JAN-09
19233|Walhalla Group|41642|6|Mentioned|p231|||||||||
19233|Walhalla Group|41868|6|Mentioned|p574|||See also p580.||||||14-JAN-09
19233|Walhalla Group|42089|5|Briefly described|p1|||||||||
19233|Walhalla Group|42383|4|Described|p5|||||||||
19233|Walhalla Group|42635|6|Mentioned|p27|||||||||
19233|Walhalla Group|42797|5|Briefly described|p39|||||||||
19233|Walhalla Group|42827|3|Fully described|p115|||See also Table 4.1.||||||14-JAN-09
19233|Walhalla Group|42938|4|Described|p578|||see also Fig.3 p576.||||||14-JAN-09
19233|Walhalla Group|43461|14|Not recorded|p627,628|||||||||
19233|Walhalla Group|43525|14|Not recorded|Table p132|Emsian|Siegenian|||||||
19233|Walhalla Group|43547|14|Not recorded|p148,150,Tb p152-54||Emsian|||||||
19233|Walhalla Group|44187|5|Briefly described|Map Legend||Early Devonian|||||||
19233|Walhalla Group|44197|5|Briefly described|Map Legend|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|60529|5|Briefly described|Map Legend|Givetian|Emsian|Includes: Montys Hut Formation, Norton Gully Sandstone.||||||
19233|Walhalla Group|60599|5|Briefly described|p14, p47 Fig. 19|Middle Devonian|Late Emsian|Comprises Wilson Creek Shale, Norton Gully Sandstone and Montys Hut Formation. Overlain by Cathedral Group. Geological Province: Melbourne Zone, Lachlan Fold Belt.||||||
19233|Walhalla Group|61160|6|Mentioned|p18|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|61181|5|Briefly described|p127|Early Devonian|Early Devonian|Bluish grey, crystalline, fossiliferous limestone, interbedded with conglomerate, grit, sandstone and shale. Two of the larger lenses have been worked for lime.||||||
19233|Walhalla Group|61185|4|Described|p41, p43, p21 Fig. 6, p39, p49, p24-25|Middle Devonian|Emsian|First called Walhalla Series (Baragwanath 1925; Whitelaw 1916). Includes Montys Hut Fm (upper), Norton Gully Sandstone (lower). Overlain by Cathedral Gp. Intruded and metmorphosed by Strathbogie Granite. Geol.Prov: Mount Easton Province, Melbourne Zone.||||||07-FEB-11
19233|Walhalla Group|61187|6|Mentioned|p5 Fig.3. |Early Devonian|Early Devonian|Melbourne Zone, Melbourne Terrane.||||||
19233|Walhalla Group|61329|5|Briefly described|p121|Middle Devonian|Ordovician|Geological Province: Gippsland Basin.||||||
19233|Walhalla Group|61701|5|Briefly described|Map Legend|Givetian|Emsian|Includes: Montys Hut Formation, Norton Gully Sandstone.||||||
19233|Walhalla Group|61702|5|Briefly described|Map Legend|Givetian|Emsian|Includes: Montys Hut Formation, Norton Gully Sandstone.||||||
19233|Walhalla Group|61703|5|Briefly described|Map Legend|Givetian|Emsian|Includes: Montys Hut Formation, Norton Gully Sandstone.||||||
19233|Walhalla Group|61704|6|Mentioned|Map legend|Devonian|Devonian|Undifferentiated. Highly magnetic.||||||
19233|Walhalla Group|63170|6|Mentioned|p236|Earl;y Devonian|Early Devonian|In eastern Victoria.||||||07-FEB-11
19233|Walhalla Group|64312|6|Mentioned|p442|||Lithic sediments in the Melbourne Tectonic Zone.||||||
19233|Walhalla Group|64535|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone, White Star Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||
19233|Walhalla Group|64536|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||07-FEB-11
19233|Walhalla Group|64537|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||07-FEB-11
19233|Walhalla Group|64538|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||07-FEB-11
19233|Walhalla Group|64539|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone, White Star Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||
19233|Walhalla Group|64540|5|Briefly described|Map legend|Late Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone, White Star Sandstone and Montys Hut Formation. Sandstones and siltstone units.||||||
19233|Walhalla Group|64605|5|Briefly described|Map legend|Early Devonian|Early Devonian|Includes Easts Lookout Siltstone, Norton Gully Sandstone, White Star Sandstone and Montys Hut Formation. Sandstones-siltstones and siltstone-sandstones; mudstone and minor shale.||||||17-NOV-08
19233|Walhalla Group|64606|5|Briefly described|Map Legend|Middle Devonian|Early Devonian|Includes Montys Hut Formation,  Norton Gully Sandstone and Easts Lookout Sandstone.||||||12-NOV-08
19233|Walhalla Group|64616|3|Fully described|p105, p144, p147, p152, p156 Fig.6.5|Early Devonian|Early Devonian|See also p158 Fig.6.6, p159, p160, p163, p166-167, p175, p179, p181 Fig.6.28, p183-184, p186-187 Fig.6.30, p188, p190-191, p200 Fig.7.1, p202-204, p207-260, p278-281, p289, p293, p302-303, p343 Fig.23. Of Murrindindi Supergroup. Comprises Norton Gully Sandstone, Montys Hut Formation, Easts Lookout Formation, White Star Sandstone. Hosts major gold deposits. Characterised by tabular platy bedding of siltstones, devoid of bioturbation. In faulted contact with Wahroonga Breccia. Overlies Jordan River Group. Is overlain by Cathedral Group. Geophysical characteristics given.||||||
19233|Walhalla Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Walhalla. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19233|Walhalla Group|65716|5|Briefly described|p33|||Includes Norton Gully Sandstone. Turbiditic||||||
19233|Walhalla Group|65900|5|Briefly described|p156 Fig. 2, p158, p161, p167|Early Devonian|Early Devonian|Melbourne Zone.||Of Murrindindi Supergroup.||||10-MAY-12
19233|Walhalla Group|66184|6|Mentioned|p382|Early Devonian|Early Devonian|||||||
19233|Walhalla Group|66244|5|Briefly described|p3.||||||Includes Woori Yallock Formation.|||
19233|Walhalla Group|66576|5|Briefly described|pp970-972, p975. |Devonian|Devonian|Walhalla Synclinorium. A folded, weakly metamorphosed sedimentary sequence; auriferous.||Unit in Murrindindi Supergroup.|Includes the basal Norton Gully Sandstone and Montys Hut Formation.|||
19233|Walhalla Group|67804|5|Briefly described|p64|Early Devonian|Early Devonian|||||Intruded by Woods Point dyke swarm. Is overlain conformably by Cathedral Group.|Folded marine siliciclastic sediments.|
19233|Walhalla Group|67847|6|Mentioned|p44 fig 3.2.2.||||||Includes the Norton Gully Sandstone and Montys Hut Formation.|||
19233|Walhalla Group|68116|5|Briefly described|Appendix, Maps 25-26, 33, 42-43.|Emsian|Emsian||||||Sandstone, mudstone, minor conglomerate; marine turbidites and mass-flow deposits.|
19233|Walhalla Group|69089|5|Briefly described|Map legend|Early Devonian|Early Devonian||||Includes Norton Gully Sandstone and Montys Hut Formation.|||
19233|Walhalla Group|70742|5|Briefly described|p161-163|Early Devonian|Early Devonian|Marine deposits; closely folded.||Murrindindi Supergroup.|Norton Gully Sandstone, Montys Hut Formation.|Overlies Jordan River Group. Is overlain by Cathedral Group and Marysville Igneous Complex.||
19233|Walhalla Group|70933|5|Briefly described|p94|Emsian|Siegenian|Upper Siegenian to Lower Emsian.||||||
19233|Walhalla Group|73497|5|Briefly described|Map legend|Devonian|Devonian||||Norton Gully Sandstone, Montys Hut Formation|||
19240|Walker Volcanics|13996|6|Mentioned|p141, p143-145|Silurian|Silurian|NW of Canberra. Late Wenlock. Hosts a new pteriomorph, Umburra cinefacta; has its own monotypic family. Bivalve taxa distribution Table. Hosts a diverse late Wenlock trilobite fauna. Biogeographic affinities.||||||
19240|Walker Volcanics|22768|5|Briefly described|p176|||||||||
19240|Walker Volcanics|22857|4|Described|p176, p462 App.1 Tb.A1.6|Wenlockian|Wenlockian|Of the Hawkins Suite. Massive and banded dacitic ignimbrite; minor interbedded lenses of fossiliferous limestone and shale. Max. thickness: 1.5km. See also p464 App.1,Tb.A1.6.||||||
19240|Walker Volcanics|24248|6|Mentioned|p67, p72 Tb. 4|||||||||
19240|Walker Volcanics|36441|5|Briefly described|map legend|Wenlockian|Wenlockian|Extrusive. Green to purple dacite ignimbrite and bedded tuff, minor andesite, volcaniclastic sediment and limestone. Underlies Tarpaulin Creek Ashstone Member (Uriarra Volcanics). BMR map code: Svw.||||||
19240|Walker Volcanics|36633|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
19240|Walker Volcanics|37013|6|Mentioned|p13|||||||||
19240|Walker Volcanics|37728|4|Described|Table 2|||||||||
19240|Walker Volcanics|37752|6|Mentioned|p105|||||||||
19240|Walker Volcanics|38035|6|Mentioned|p92|||||||||
19240|Walker Volcanics|39975|6|Mentioned|p123|||||||||
19240|Walker Volcanics|41356|3|Fully described|p18|||||||||
19240|Walker Volcanics|42421|4|Described|p294|Wenlockian late||||||||
19240|Walker Volcanics|42497|5|Briefly described|Map Legend|Wenlockian|Wenlockian|||||||
19240|Walker Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
19240|Walker Volcanics|42727|5|Briefly described|map legend|Wenlock|Wenlock|Of Hawkins Volcanic Suite. Purple and greenish-grey dacitic ignimbrite. Disconformably underlies Mount Painter Volcanics; intruded by Federal Golf Course Tonalite. BMR map symbol: Smw. Geol. Prov: Canberra Block.||||||
19240|Walker Volcanics|42820|2|Defined|p26|Early Silurian||Of Hawkins Volcanic Suite.||||||14-APR-08
19240|Walker Volcanics|42994|6|Mentioned|p5|||||||||
19240|Walker Volcanics|43159|4|Described|Fig.2p4,p9.|||||||||
19240|Walker Volcanics|43481|6|Mentioned|3|||||||||
19240|Walker Volcanics|44092|5|Briefly described|map legend|Late Silurian|Early Silurian|Sv2||||||
19240|Walker Volcanics|45147|2|Defined|M144|late Wenlockian|late Wenlockian|||||||
19240|Walker Volcanics|47032|6|Mentioned|Fig.1|||||||||
19240|Walker Volcanics|47037|6|Mentioned|p107|||||||||
19240|Walker Volcanics|49013|5|Briefly described|p1|||||||||
19240|Walker Volcanics|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
19240|Walker Volcanics|60989|6|Mentioned|p111|||Canberra area. Includes an uncommon Silurian trimerellide brachiopod.||||||
19240|Walker Volcanics|63083|6|Mentioned|p218|||In Canberra area. Includes a fossil fauna of scutellids, illaenids, harpetids, cheirurids and staurocephalids.||||||07-FEB-11
19240|Walker Volcanics|68592|6|Mentioned|p428, p443, p457|Silurian|Silurian|Owen and Wyborn (1979). Equivalent to, but not yet formally included in, the Douro Group.||||||
19240|Walker Volcanics|71657|6|Mentioned|p37-38, p47|Silurian|Silurian|Holotype materials of the brachiopods Morinorhynchus oepiki and Salopina mediocostata were recovered from this unit.||||||
19242|Walkers Hill Granite|34449|6|Mentioned|Table 2-1|||||||||
19254|Wallaby beds|32945|6|Mentioned|p88|||Permian||||||
19254|Wallaby beds|43475|14|Not recorded|p553||Permian|See also Lexicon||||||
19254|Wallaby beds|63731|5|Briefly described|Map legend|Early Permian|Early Permian|Conglomerate, lithic arenite, and locally ferruginous siltstone.||||||
19254|Wallaby beds|63748|4|Described|p7 Fig. 3, p19|Permian|Permian|Unconformably overlies the Eurydesma beds; unconformably overlain by Eight Mile Creek beds. Thickness: ~150m. Consists of a lower sequence of conglomerate, lithic arenite and siltstone overlain by an upper sequence of mainly ferruginous siltstone.||||||07-FEB-11
19254|Wallaby beds|68679|5|Briefly described|p446, p452|Permian|Permian|Silver Spur Subprovince, Woolomin Province. ~150m thick.||Wildash Group.||Unconformably overlies the Eurydesma beds. Is overlain unconformably by Eight Mile Creek beds. Is downfaulted against the Silverwood Group.|Conglomerate, lithic sandstone and siltstone overlain by mainly ferruginous siltstone. Contains abundant marine and plant fossils.|
19257|Wallace Shale|13996|6|Mentioned|p138, p143|Pridoli|Pridoli|Molong district. Conulariid species. A few Pridoli trilobites.||||||
19257|Wallace Shale|22768|6|Mentioned|p178|||||||||
19257|Wallace Shale|22857|5|Briefly described|p178, p468 App.1 Tb.A1.6|Silurian|Silurian|Of the Mumbil Group. Overlain by Bulls Camp Volcanics in Molong Rise area. Red and green shale, rare arenite; allochthonous megaclasts. Max. thickness: 450m.||||||10-MAR-06
19257|Wallace Shale|23214|3|Fully described|p129|Early Devonian|Pridoli|Of Mumbil Group. Previously part of the Gamboola Formation. Max. thickness 300m.||||||
19257|Wallace Shale|23217|6|Mentioned|p9|Silurian|Silurian|Contains the "Nyrang Sandstone Member".  In the Cheesemans Creek district.||||||08-MAR-06
19257|Wallace Shale|24126|6|Mentioned|p188|||||||||
19257|Wallace Shale|24249|4|Described|p87, p90 Fig.3|Pridoli|Pridoli|Contains graptolites. Overlying Unit: Nyrang Sandstone Member. Underlying Unit: Mirrabooka Formation.||||||
19257|Wallace Shale|24417|5|Briefly described|p135|Silurian|Silurian|Contains the "Nyrang Sandstone Member".||||||
19257|Wallace Shale|29362|6|Mentioned|p187|||||||||
19257|Wallace Shale|29791|6|Mentioned|Fig.4|||||||||
19257|Wallace Shale|29993|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
19257|Wallace Shale|30073|6|Mentioned|p5|||Silurian - ? Devonian age. On map P54.||||||
19257|Wallace Shale|31161|5|Briefly described|PA4|||||||||
19257|Wallace Shale|31852|6|Mentioned|p718|||U.Sil.-L.Dev. See also Fig.4||||||
19257|Wallace Shale|32150|6|Mentioned|p2|||Refers Stevens & Packham (1953)||||||
19257|Wallace Shale|32151|6|Mentioned|p210|||Refers Stevens & Packham (1953)||||||
19257|Wallace Shale|32671|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
19257|Wallace Shale|32672|6|Mentioned|p672|||||||||
19257|Wallace Shale|32999|6|Mentioned|p27|||Similar to Whipbird Ck. Fm.||||||
19257|Wallace Shale|33006|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
19257|Wallace Shale|33116|4|Described|p219|||See also P220. Graptolites Fig.9||||||
19257|Wallace Shale|33121|6|Mentioned|p85|||Sil.-Dev. Correlation||||||
19257|Wallace Shale|33282|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
19257|Wallace Shale|33285|6|Mentioned|p18|||Late Sil.-Early Dev.||||||
19257|Wallace Shale|33326|6|Mentioned|p444|||Fauna.||||||
19257|Wallace Shale|33732|5|Briefly described|p115|||||||||
19257|Wallace Shale|33735|6|Mentioned|p206|||||||||
19257|Wallace Shale|34403|3|Fully described|p137|||||||||
19257|Wallace Shale|34404|6|Mentioned|Fig.3.3b|||||||||
19257|Wallace Shale|34405|6|Mentioned|p109|||||||||
19257|Wallace Shale|34406|6|Mentioned|p221|||||||||
19257|Wallace Shale|34491|6|Mentioned|p36|||Conularids||||||
19257|Wallace Shale|35137|6|Mentioned|p89|||||||||
19257|Wallace Shale|35246|6|Mentioned|Fig.5|||||||||
19257|Wallace Shale|35258|6|Mentioned|Table 1|||||||||
19257|Wallace Shale|35501|6|Mentioned|Table 1|||||||||
19257|Wallace Shale|37727|4|Described|p92|||See also P6.||||||
19257|Wallace Shale|38378|6|Mentioned|p134|||||||||
19257|Wallace Shale|39214|5|Briefly described|p19|||||||||
19257|Wallace Shale|39331|6|Mentioned|p64|||||||||
19257|Wallace Shale|40328|3|Fully described|p153|||||||||
19257|Wallace Shale|43344|14|Not recorded|p139|Early Devonian|Late Silurian|||||||
19257|Wallace Shale|43385|14|Not recorded|p171-173|||Late Silurian or Early Devonian||||||
19257|Wallace Shale|43461|14|Not recorded|Table p621|Gedinnian|Ludlovian|||||||
19257|Wallace Shale|43479|14|Not recorded|p105,116||Ludlovian|||||||
19257|Wallace Shale|43515|14|Not recorded|Map Legend||Late Silurian|(Provisional Edition)||||||
19257|Wallace Shale|43516|14|Not recorded|Map Legend||Late Silurian|||||||
19257|Wallace Shale|43517|14|Not recorded|p153|Gedinnian|Ludlovian|||||||
19257|Wallace Shale|43525|14|Not recorded|Table p127|||||||||
19257|Wallace Shale|43640|5|Briefly described|Map Legend||Silurian|||||||
19257|Wallace Shale|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Mumbil Group. Consists of red and green shale; rare sandstone; allochtonous megaclasts.||||||15-JUL-08
19257|Wallace Shale|43782|5|Briefly described|Map Legend|Lochkovian|Pridoli|of Mumbil Group.||||||
19257|Wallace Shale|48926|6|Mentioned|p30|||P30 et seq.||||||
19257|Wallace Shale|50095|5|Briefly described|p108 Fig.1, p121|Silurian|Silurian|||||||
19257|Wallace Shale|60332|6|Mentioned|p952|||Contains Belodella anomalis (conodont).||||||
19257|Wallace Shale|60987|5|Briefly described|p154-155|||Stevens and Packham (1953). Orange district. Contains Pridoli graptolites.|||||Distinctive red, green,and yellow banding.|
19257|Wallace Shale|61138|6|Mentioned|p213|Late Silurian|Late Silurian|NSW. Contains the trilobite Denckmannites rutherfordi Sherwin, 1968.||||||
19257|Wallace Shale|63287|5|Briefly described|p317 Fig. 2, p321 Fig. 4|Lochkovian|Pridoli|Geological Province: Molong Volcanic Belt. Consists of shale.||||||07-FEB-11
19257|Wallace Shale|63290|6|Mentioned|p401 Fig. 5(d)|Late Silurian|Late Silurian|Of Mumbil Group.||||||
19257|Wallace Shale|63292|6|Mentioned|p447|Early Silurian|Early Silurian|||||||
19257|Wallace Shale|67651|5|Briefly described|p414-415|Lochkovian|Pridoli|Contains graptolites with a late Pridoli age (Monograptus perneri ? M. transgrediens biozones) in the lower part of the formation.||||Underlain by Molong Limestone or Mirrabooka Formation or Borenore Limestone.||
19257|Wallace Shale|70297|5|Briefly described|map legend|Silurian|Silurian|||Mumbil Group||||
19257|Wallace Shale|70684|6|Mentioned|p50 Fig.24|Late Silurian|Late Silurian|||Mumbil Group.||||
19257|Wallace Shale|73299|6|Mentioned|p1104 Fig.10|Late Silurian|Late Silurian|Molong High.||||Overlies the Mirrabooka Formation, underlies the Bulls Camp Volcanics.||
19259|Wallah Granite|42726|5|Briefly described|map legend|Silurian||239. Part of the Wyangala Batholith.||||||12-JUN-08
19259|Wallah Granite|50231|5|Briefly described|Map Legend|Ludlow|Ludlow|Part of the Wyangala Batholith.||||||
19259|Wallah Granite|50233|5|Briefly described|Map Legend|Ludlow|Ludlow|Of the Wyangala Batholith. Massive to foliated porphyritic ex-cordierite-biotite granite, granodiorite.||||||
19259|Wallah Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Burrawinda Suite. Massive to foliated porphyritic cordierite-muscovite-biotite granite, granodiorite.||||||12-JUN-08
19259|Wallah Granite|68592|2|Defined|p1354-7, p1371-4, p1664|Late Silurian|Early Silurian|Chappell et al. (1991), after Wallah property and Wallah Parish. Now includes the Rugby Granite of Chappell et al. (1991). A large, irregular-shaped body forming mostly undulating terrain. Type locality described. Geochemistry and geophysical properties described. Age from parent. Has been used as a local source of road construction materials.||Unit in Burrawinda Suite.||Intrudes Adaminaby Group. Is intruded by Narrawa Granite and Bishopthorpe Suite.|Grey to cream, medium- to coarse-grained, massive to mildly foliated, equigranular, cordierite-muscovite-biotite granite and granodiorite; contains some metasedimentary xenoliths. Moderate to high greenschist facies metamorphism. S-type.|
19259|Wallah Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sww. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Burrawinda Suite|||Medium to coarse grained, massive to mildly foliated, equigranular, cordierite-muscovite-biotite granite and granodiorite with metasedimentary xenoliths; high K and Th response.|
19259|Wallah Granite|70544|5|Briefly described|Map Legend|Devonian|Silurian|||Burrawinda Suite|||Medium to coarse grained, massive to mildly foliated, equigranular, cordierite-muscovite-biotite granite and granodiorite with metasedimentary xenoliths; high K and Th response.|
19259|Wallah Granite|70545|5|Briefly described|Map Legend |Silurian|Silurian|||Burrawinda Suite|||Medium-coarse grained, massive to mildly foliated, equigranular, cordierite-muscovite-biotite granite and granodiorite with metasedimentary xenoliths; high K and Th response.|
19265|Wallangarra Volcanics|22857|5|Briefly described|p538 App.1 Tb.A1.9|Late Permian|Early Permian|Of the Wandsworth Group. Rhyolitic and rhyodacitic flows and tuffs. Max. thickness: 450m. Geological Province: New England Fold Belt.||||||
19265|Wallangarra Volcanics|23811|5|Briefly described|Map Legend|Late Permian|Late Permian|Of the Wandsworth Volcanic Group.  Ignimbrite rhyolite and rhyodacite and lesser rhyolitic lavas, including bedded epiclastic tuffs.||||||27-SEP-18
19265|Wallangarra Volcanics|23812|5|Briefly described|p28 Tb.3, p25|Late Permian|Early Permian|Of Wandsworth Volcanic Group.  Maximum thickness: 450m.||||||12-AUG-08
19265|Wallangarra Volcanics|23859|5|Briefly described|p930|Late Permian|Permian|Of Wandsworth Volcanic Group. Geological Province: New England Fold Belt.||||||
19265|Wallangarra Volcanics|31694|6|Mentioned|p350|||||||||
19265|Wallangarra Volcanics|38824|6|Mentioned|p215|||||||||
19265|Wallangarra Volcanics|39252|6|Mentioned|p28|||See also Fig.15||||||
19265|Wallangarra Volcanics|39445|6|Mentioned|Fig.8|||||||||
19265|Wallangarra Volcanics|40509|6|Mentioned|p47|||||||||
19265|Wallangarra Volcanics|42378|5|Briefly described|Table 1 p8|||||||||27-SEP-18
19265|Wallangarra Volcanics|42559|4|Described|p10|||Stated to be informal name.||||||
19265|Wallangarra Volcanics|60079|5|Briefly described|Map Legend|Late Permian|Permian|Of the Wandsworth Volcanic Group.||||||
19265|Wallangarra Volcanics|61793|6|Mentioned|p341|||Geological Province: New England Fold Belt.||||||07-FEB-11
19265|Wallangarra Volcanics|63732|5|Briefly described|Map legend|Late Permian|Late Permian|Dacitic to rhyolitic ignimbrite, strongly welded and moderately to very crystal-rich - numerous fragments of andesine, biotite, orthoclase, quartz.  Welded ignimbrite with fragments of orthoclase, oligoclase, quartz and minor biotite.||||||11-DEC-07
19265|Wallangarra Volcanics|63748|4|Described|p19, p36, p69|Late Permian|Late Permian|Unconformable on Texas beds; intruded by Stanthorpe Granite and possibly by Undercliffe Falls Granite. Max.thickness: 450m. Geol.prov: Wandsworth Province. Rhyolitic and rhyodacitic tuffs and lavas with possible epiclastic interbeds. Detailed lithology.||||||27-SEP-18
19265|Wallangarra Volcanics|65668|5|Briefly described|p2 Tb.1, p31-34|Permian|Permian|Stanthorpe area. Considered to be closely related to Emmaville Volcanics; both units placed in Wandsworth Volcanic Group by Barnes et al. (1991). Age: 253 +/- 2.4 Ma (SHRIMP U-Pb zircon). A 300-450 m thick sequence of rhyolitic to rhyodacitic ignimbrites and lavas. Is intruded by Stanthorpe Granite; is overlain by Dundee Rhyodacite.||||||
19265|Wallangarra Volcanics|68005|5|Briefly described|pp151-152.|Permian|Permian|||Unit in Wandsworth Volcanic Group.|||Ignimbritic rhyolite and rhyodacite and lesser rhyolitic lavas. Includes bedded epiclastic tuffs.|
19265|Wallangarra Volcanics|68111|5|Briefly described|p968 Tb.1|Olenekian|Wuchiapingian||253 +/- 2.4 Ma, U-Pb SHRIMP (Cross et al. 2009).|Of the Wandsworth Volcanic Group.||||
19265|Wallangarra Volcanics|68679|4|Described|p453, p455-458|Permian|Permian|Simmonds (1958) and several others listed. Stroud et al. (1992) included the unit in the Wandsworth Volcanic Group and equated it with the Emmaville Volcanics. Wandsworth Province. Crops out in the NSW-QLD border area between Ballandean and Wallangarra. 300-450m thick. High-K calc-alkaline. Represents eruption of a large silicic magma system. Is equated with the Emmaville Volcanics.|253 +/- 2.4 Ma (SHRIMP U-Pb: Cross et al., 2009).|Wandsworth Volcanic Group.||Unconformably overlies Texas beds. Is overlain unconformably by Dundee Rhyolite. Is intruded by Stanthorpe, Dormans Flat, Sailor Jack Granites and possibly the Bungulla Monzogranite.|Rhyolitic and rhyodacitic tuff and lava with possible epiclastic interbeds. Later decribed as two thick intracaldera ignimbrite units separated by <50m package of thinly bedded ignimbrite, air fall deposits, surge deposits and epiclastic sediments.|
19265|Wallangarra Volcanics|68901|5|Briefly described|p6, p8, p129|Late Permian|Late Permian|Age from Cross et al., 2009.
|253+/-2.4 Ma SHRIMP,|||||27-SEP-18
19265|Wallangarra Volcanics|69639|5|Briefly described|p220|||See also Wallangara Volcanics p44, p62.|235.0 +/- 2.4 Ma|Wandsworth Volcanic Group||Unconformably overlies the Texas Beds.||
19265|Wallangarra Volcanics|70876|5|Briefly described|p82|Late Permian|Late Permian||253 +/- 2.4 Ma (Cross et al, 2009).|Wandsworth Volcanic Group||Overlies the Drake Volcanics. Overlain by the Emmaville Volcanics.||
19265|Wallangarra Volcanics|71592|5|Briefly described|Appendix A.|||New England Orogen.|253+/-2.4 Ma (crystallisation: U-Pb zircon SHRIMP)||||Ignimbrite.|
19265|Wallangarra Volcanics|71628|5|Briefly described|p11-11; p12: 3, 5-6, 13; p15: 33, 40|Permian|Permian|See also p15: 57, 65, 75, 82-83, 97; p19: 6, 8, 160. RELATED UNITS (continued): Is also intruded by Severn River Monzogranite; Mount Norman Leucomonzogranite; Ruby Creek Leucogranite; Tenterfield Creek Leucosyenogranite; Stanthorpe Complex.||Wandsworth Volcanic Group.||Unconformably overlies Ballandean Monzogranite. Is intruded by Bungulla, Accommodation Creek, Blacksmiths Creek, Dormans Flat, Sailor Jack, Mount Lindesay Monzogranites. See COMMENTS for more.||
19265|Wallangarra Volcanics|71701|5|Briefly described|p170|Lopingian|Lopingian||253.8 +/- 2.4 Ma  (SHRIMP, Cross et al, 2009)|||||
19267|Wallangulla Sandstone Member|22857|5|Briefly described|p544 App.1 Tb.A1.12|Albian|Albian|Of the Griman Creek Formation (Rolling Downs Group). Fine to medium-grained pale clayey sandstone. Contains Finch clay facies. Max. thickness: 19m. Geological Province: Surat Basin.||||||
19267|Wallangulla Sandstone Member|36356|6|Mentioned|p66|||||||||
19267|Wallangulla Sandstone Member|42346|5|Briefly described|p83|||||||||
19267|Wallangulla Sandstone Member|43196|5|Briefly described|p418||Early Cretaceous|Member of Griman Creek Formation. Age:Early Cretaceous (Middle Albian)||||||12-JUN-14
19267|Wallangulla Sandstone Member|68004|5|Briefly described|p205.|Early Cretaceous|Early Cretaceous||||Includes Finch Clay.|||
19267|Wallangulla Sandstone Member|68069|5|Briefly described|p2.|Early Cretaceous|Early Cretaceous|||Lower unit in Griman Creek Formation.|Includes Finch clay facies.|Is overlain by Coocoran Claystone Member.|Fine- to medium-grained, pale, kaolinitic sandstone; locally cross-bedded and iron-stained; includes Finch clay facies.|
19267|Wallangulla Sandstone Member|68593|5|Briefly described|p5, p84|Albian|Albian|Byrnes (1977). 4-19m thick. Source of diverse fossils, significant for dinosaurs and opalised plants and animals (listed in Appendix 6).||Griman Creek Formation.|Finch clay facies.||Fine- to medium-grained, pale, clayey sandstone; claystone pellets; some cross-bedding.|
19267|Wallangulla Sandstone Member|71601|5|Briefly described|p121|Albian|Albian|Geological province: Surat Basin. Regressive beach or nearshore marine to paralic/deltaic, and fluvial floodplain deposits in the upper part of Griman Creek Fm.||Unit of Griman Creek Formation.||Overlies Finch clay facies.||
19267|Wallangulla Sandstone Member|73218|6|Mentioned|p1028|Early Cretaceous|Early Cretaceous|Reflects shallow marine to fluvial settings. Thickness: 3-19 m.||||Underlain by Finch Claystone.||
19269|Wallarah Coal|23055|6|Mentioned|Fig4p11|||||||||
19269|Wallarah Coal|23438|6|Mentioned|p25|||of Newcastle Coal Measures.||||||
19269|Wallarah Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Of the Moon Island Beach Formation.||||||05-FEB-08
19269|Wallarah Coal|24158|5|Briefly described|p172 Fig.3|||Of the Newcastle Coal Measures. Geological Province: Sydney Basin||||||
19269|Wallarah Coal|31549|6|Mentioned|p159|||Stratigraphic succession||||||
19269|Wallarah Coal|31551|6|Mentioned|Table 1|||Stratigraphy of Moon Island Beach Subgroup||||||
19269|Wallarah Coal|34270|6|Mentioned|p254|||||||||
19269|Wallarah Coal|36327|6|Mentioned|p8|||||||||
19269|Wallarah Coal|39294|6|Mentioned|Fig. 9.2|||||||||
19269|Wallarah Coal|39308|6|Mentioned|p458|||||||||
19269|Wallarah Coal|39609|6|Mentioned|Table 1|||||||||
19269|Wallarah Coal|39666|6|Mentioned|p93|||||||||
19269|Wallarah Coal|41226|6|Mentioned|Fig.12|||||||||
19269|Wallarah Coal|41463|6|Mentioned|p38|||||||||
19269|Wallarah Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Wallarah coal seam instead. See also p113.||Of Moon Island Beach Subgroup||||
19269|Wallarah Coal|73304|6|Mentioned|p65-66, p69, p75|||||Moon Island Beach Formation, Newcastle Coal Measures||Overlies Mannering Park Tuff.||
19273|Wallaringa Formation|22857|4|Described|p510 App.1 Tb.A1.8|Visean|Visean|Sandstone, lithic arenite. Conformably overlain by Gilmore Volcanic Group. Max. thickness: ~500m. Geological Province: Tamworth Forearc Basin.||||||
19273|Wallaringa Formation|24121|5|Briefly described|p4, p69, p93, p112|||||||||25-AUG-22
19273|Wallaringa Formation|30074|6|Mentioned|p24|||See also P25||||||
19273|Wallaringa Formation|31228|4|Described|p79|||See also P77. Stratigraphic table.||||||
19273|Wallaringa Formation|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
19273|Wallaringa Formation|32379|6|Mentioned|p3|||||||||
19273|Wallaringa Formation|32527|6|Mentioned|p403|||Refers Roberts & Oversby (1973)||||||
19273|Wallaringa Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19273|Wallaringa Formation|32836|6|Mentioned|Table 1|||Palaeobotany||||||
19273|Wallaringa Formation|32869|5|Briefly described|p170|||See also Fig.2. Depositional environment||||||
19273|Wallaringa Formation|34059|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19273|Wallaringa Formation|34072|6|Mentioned|Fig.4.5|||Carb.||||||
19273|Wallaringa Formation|34077|5|Briefly described|p252|||||||||
19273|Wallaringa Formation|34081|6|Mentioned|p260|||||||||
19273|Wallaringa Formation|34085|6|Mentioned|Cor.chart|||Visean||||||
19273|Wallaringa Formation|34169|4|Described|Fig.4.6|||Stratigraphic column.||||||
19273|Wallaringa Formation|34238|6|Mentioned|Fig.2|||||||||
19273|Wallaringa Formation|34239|6|Mentioned|p264|||Microflora||||||
19273|Wallaringa Formation|34444|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19273|Wallaringa Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
19273|Wallaringa Formation|37068|6|Mentioned|p58|||||||||
19273|Wallaringa Formation|39302|6|Mentioned|p342|||See also PP343,345||||||
19273|Wallaringa Formation|39306|6|Mentioned|Fig. 21.2|||||||||
19273|Wallaringa Formation|39308|6|Mentioned|p490|||||||||
19273|Wallaringa Formation|40224|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
19273|Wallaringa Formation|40883|6|Mentioned|p7|||||||||
19273|Wallaringa Formation|41902|5|Briefly described|p5 Table 1|||||||||
19273|Wallaringa Formation|41903|6|Mentioned|Map legend|Carboniferous||||||||
19273|Wallaringa Formation|42547|4|Described|p29|||||||||
19273|Wallaringa Formation|43383|14|Not recorded|p18|||Conf. on Glen Williams Beds||||||
19273|Wallaringa Formation|43417|6|Mentioned|Map Legend|||Sth equivalent of Waverley Formation||||||
19273|Wallaringa Formation|43432|14|Not recorded|p205,207||Early Carboniferous|||||||
19273|Wallaringa Formation|43440|14|Not recorded|p37,66,68,76|||Contains Wallarobba Conglomerate Member||||||
19273|Wallaringa Formation|43447|4|Described|Table 1&2,p9-11||Carboniferous|||||||
19273|Wallaringa Formation|43451|14|Not recorded|Map Legend|||||||||
19273|Wallaringa Formation|43479|14|Not recorded|p158,159,177||Visean|||||||
19273|Wallaringa Formation|43576|6|Mentioned|p351|||||||||
19273|Wallaringa Formation|44093|5|Briefly described|p229 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
19273|Wallaringa Formation|44244|2|Defined|p82|Visean|Visean|Contains the Wallarobba Conglomerate Member.  Overlies Flagstaff Formation; underlies Martins Ignimbrite Member (Newtown Formation).  Type section in text.  Geological Province: Gresford Block.||||||
19273|Wallaringa Formation|44253|14|Not recorded|p6||Carboniferous|||||||
19273|Wallaringa Formation|44254|2|Defined|p76-79||Early Carboniferous|||||||
19273|Wallaringa Formation|44255|14|Not recorded|p119-121,127|||||||||
19273|Wallaringa Formation|44265|14|Not recorded|Fig.1,p114|||||||||
19273|Wallaringa Formation|44266|14|Not recorded|p82||Visean|(Early Visean)||||||
19273|Wallaringa Formation|44833|14|Not recorded|p116,117|||||||||
19273|Wallaringa Formation|45090|4|Described|p25|||Stratigraphic table||||||
19273|Wallaringa Formation|45097|6|Mentioned|Fig.|||Correlation chart||||||
19273|Wallaringa Formation|46849|6|Mentioned|p185|||||||||
19273|Wallaringa Formation|47056|6|Mentioned|Fig.2 P523|||||||||
19273|Wallaringa Formation|50132|6|Mentioned|p246 Fig. 4|Early Carboniferous|Early Carboniferous|New England Fold Belt, Raymond Terrace area||||||
19273|Wallaringa Formation|50147|5|Briefly described|Map legend|Visean|Visean|Pink to brown thickly bedded lithic sandstone, conglomerate and minor siltstone.||||||
19273|Wallaringa Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Overlies: Flagstaff Formation.  Geological Province: Gresford Block.  Underlies: Martins Creek Ignimbrite Member.||||||
19273|Wallaringa Formation|63832|5|Briefly described|p131 fig 2|Visean|Visean|Cranky Corner/Gresford Block, Southern New England Fold Belt.||||Is overlain by Gilmore Volcanics.||14-DEC-17
19273|Wallaringa Formation|64631|5|Briefly described|p44 Fig.2.|Visean|Visean|Southern New England Fold Belt, Cranky Corner/Gresford Block. Biostratigraphic age control for base and top.||||Is overlain by Gilmore Volcanics.||
19273|Wallaringa Formation|69793|6|Mentioned|p1121 Fig.12|Visean|Visean|Gresford Block, Tamworth Belt.||||||
19273|Wallaringa Formation|71233|5|Briefly described|p116|Carboniferous|Carboniferous|Contains Grandispora Microflora. See Rattigan (1967).||||||
19274|Wallarobba Conglomerate Member|22857|5|Briefly described|p510 App.1 Tb.A1.8|Visean|Visean|Basal conglomerate of Wallaringa Formation. Max. thickness: 130m. Geological Province: Tamworth Forearc Basin.||||||
19274|Wallarobba Conglomerate Member|24121|5|Briefly described|p4|||Of Wallaringa Formation.||||||
19274|Wallarobba Conglomerate Member|32869|6|Mentioned|p170|||Wallaringa Fm.||||||
19274|Wallarobba Conglomerate Member|34072|6|Mentioned|p244|||||||||
19274|Wallarobba Conglomerate Member|34169|4|Described|p250|||||||||
19274|Wallarobba Conglomerate Member|39308|6|Mentioned|p490|||||||||
19274|Wallarobba Conglomerate Member|43432|14|Not recorded|p205|||||||||
19274|Wallarobba Conglomerate Member|43440|14|Not recorded|p37,fig.4-3|||||||||
19274|Wallarobba Conglomerate Member|43451|14|Not recorded|Map Legend||Carboniferous|Included in Wallaringa Formation||||||
19274|Wallarobba Conglomerate Member|44244|5|Briefly described|p82|Visean|Visean|Of the Wallaringa Formation.  Max. thickness: >130m.  Type section in text.  Geological Province: Gresford Block.||||||
19274|Wallarobba Conglomerate Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Wallaringa Formation.  Thickly bedded cobble conglomerate with clasts of devitrified volcanics, sediments and granitoids set in pink zeolitic sandstone matrix.||||||
19280|Wallerawang Granite|42726|5|Briefly described|map legend|Carboniferous||20. Not a variation on Wallerawang Subgroup.  Of the Hartley Suite (Bathurst Supersuite).||||||07-FEB-05
19281|Wallerawang Subgroup|22857|5|Briefly described|p528 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin.||||||
19281|Wallerawang Subgroup|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|||||||
19281|Wallerawang Subgroup|23219|5|Briefly described|Map Legend|Permian|Permian|||||||
19281|Wallerawang Subgroup|39232|3|Fully described|p110|||See also p113||||||22-FEB-17
19281|Wallerawang Subgroup|40806|2|Defined|p150|Permian|Permian|Prob. Permian||||||
19281|Wallerawang Subgroup|42657|6|Mentioned|Table 1 P74|||||||||
19281|Wallerawang Subgroup|42925|5|Briefly described|Table 18||Late Permian|||||||
19281|Wallerawang Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
19281|Wallerawang Subgroup|43194|5|Briefly described|p115, p129 Tb. 8.3|Late Permian|Late Permian|Of Illawarra Coal Measures, western Sydney Basin. Contains Gap Sandstone and Farmers Creek Formation. Lithofacies equivalent of the unnamed 'upper lithic sequence' (now Nea Subgroup) of the Black Jack Formation (now Black Jack Group), Gunnedah Basin.||||||
19281|Wallerawang Subgroup|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Illawarra Coal Measures. Geological Province: Sydney Basin||||||
19281|Wallerawang Subgroup|63832|5|Briefly described|p131 fig 2|Lopingian|Lopingian|Of Sydney Basin.||Unit in Illawarra Coal Measures.||||14-DEC-17
19281|Wallerawang Subgroup|64631|6|Mentioned|p44 Fig.2.|Changhsingian|Wuchiapingian|NW, SW Sydney Basin.||Unit in Illawarra Coal Measures.||Time equivalent to Newcastle Coal Measures.||
19281|Wallerawang Subgroup|68003|5|Briefly described|p38 Fig.3-j, p41.|Late Permian|Late Permian|Western Coalfield, Brigalow Belt South Bioregion. Formed by southward-prograding major fluvio-deltaic systems.||Unit in Illawarra Coal Measures.||Overlies Charbon Subgroup. Is overlain by Narrabeen Group.||
19281|Wallerawang Subgroup|68004|5|Briefly described|p60 Table 6.|Late Permian|Late Permian|Western Coalfield.||Unit in Illawarra Coal Measures.||Overlies Charbon Subgroup. Is overlain by Narrabeen Group.||
19286|Walli Volcanics|13139|5|Briefly described|p8, p9 Fig. 4, p10|Late Ordovician|Middle Ordovician|Unconformably overlain by the Cliefden Caves Limestone Subgroup.  Geological Province: Western Molong Volcanic Belt.||||||
19286|Walli Volcanics|22503|6|Mentioned|Fig.4 p646|||||||||
19286|Walli Volcanics|22857|4|Described|p426 App. 1 Tb. A1.5|Early Ordovician|Early Ordovician|Of the Kenilworth Group. Plagioclase basalt, volcaniclastic sandstone, siltstone. Max. thickness: 1100m.||||||
19286|Walli Volcanics|23214|3|Fully described|p27|Ordovician|Ordovician|Of Kenilworth Group. Formerly Walli Andesite. Geological Province: Lachlan Fold Belt.||||||
19286|Walli Volcanics|23334|5|Briefly described|9 Fig.4|Ordovician|Ordovician|||||||
19286|Walli Volcanics|24398|5|Briefly described|p259 Fig.2|Gisbornian|Darriwilian|Geological Province: Lachlan Fold Belt.||||||
19286|Walli Volcanics|36534|6|Mentioned|p223|||||||||
19286|Walli Volcanics|43357|14|Not recorded|155-161|Early Ordovician||||||||
19286|Walli Volcanics|43642|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Kenilworth Group. Consists of plagioclase basalt, volcaniclastic sandstone, siltstone. matrix-supported conglomerate.||||||15-JUL-08
19286|Walli Volcanics|43782|5|Briefly described|Map Legend|Darriwilian|Yapeenian|Of Kenilworth Group.||||||15-JUL-08
19286|Walli Volcanics|63277|6|Mentioned|p139|||||||||
19286|Walli Volcanics|63278|5|Briefly described|p145 Fig. 1, p147 Fig. 2b, p154|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt, LFB. See p154 for more information.||||||07-FEB-11
19286|Walli Volcanics|63283|5|Briefly described|p184, p199, p191 Tb. 2, p195 Fig. 2|Late Ordovician|Early Ordovician|Age: 460Ma (basalt, andesite, dacite and dolorite dyke). Geological Province: Molong Volcanic Belt. Consists of lavas with high-K and shosonitic affinities. See p199.||||||07-FEB-11
19286|Walli Volcanics|63284|6|Mentioned|p249|||Geological Province: Molong Volcanic Belt. Rocks show affinities extending from high-K calc-alkaline to shoshonitic (Crawford et al. 2007; Simpson et al. 2005).||||||
19286|Walli Volcanics|63286|5|Briefly described|p294 Fig. 1, p306, p308 Fig. 9|Ordovician|Ordovician|Consists of basaltic lava, volcanic sandstone, mudstone and conglomerate, also has mudium-K and high-K calc-alkaline affinities (Crawford et al. 2007). Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19286|Walli Volcanics|63287|4|Described|p316, p317 Fig. 2, p319, p336-339|Eastonian|Darriwilian|Of the Kenilworth Group. Overlain by Cliefden Caves Limestone. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19286|Walli Volcanics|63289|5|Briefly described|p366|||Overlain by Cliefden Caves Limestone Subgroup. Geological Province: Molong Volcanic Belt. Consists of volcaniclastic sandstone and siltstone intruded by mafic clinopyroxene + plagioclase-phyric basalt sills.||||||07-FEB-11
19286|Walli Volcanics|63290|6|Mentioned|p400 Fig. 5¿, p396 Fig. 3|Late Ordovician|Middle Ordovician|Geological Province: Molong Volcanic Belt.||||||
19286|Walli Volcanics|63293|6|Mentioned|p473, p469 Fig. 2|Gisbornian|Darriwilian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19286|Walli Volcanics|64295|5|Briefly described|p198 Fig. 1, p201|||Disconformably overlain by Fossil Hill Limestone Subgroup. On the Molong Volcanic Belt. See also p204.||||||01-SEP-08
19286|Walli Volcanics|64963|5|Briefly described|p182 Fig. 2, p183|||||||||
19286|Walli Volcanics|67322|5|Briefly described|Fig.5; p22, p24|Late Ordovician|Middle Ordovician|Macquarie Arc. Modified by Krynen and Pogson, in Pogson and Watkins (1998), after Stevens (1952). Minimum age not well constrained. Occurs in the Cliefden Caves region.||Of the Cabonne Group.||Disconformably overlain by the Cliefden Caves Limestone Subgroup. Correlative of the Kenyu Formation.||22-FEB-18
19286|Walli Volcanics|68592|6|Mentioned|p13, p371, p378|||Molong-Wellington Volcanic Belt. Formerly part of Kenilworth Group which has been discontinued (Pogson et al., 2012) in favour of Cabonne Group. Is contiguous with the Kenyu Formation which is considered to be of similar age.||Unit in Cabonne Group.||||
19286|Walli Volcanics|69539|6|Mentioned|p607|||||||||
19286|Walli Volcanics|70297|4|Described|map legend, on side 2 of map sheet|Ordovician|Ordovician|Macquarie Volcanic Arc Phase 2 volcanic units. Age: ranges from early Darriwilian (Da2) to latest Gisbornian. Molong Volcanic Belt.|c. 470-455 Ma|Cabonne Group||||
19286|Walli Volcanics|70684|6|Mentioned|p3, p12, p33-34, p75|Late Ordovician|Middle Ordovician|Southern Molong Volcanic Belt.|c.465 Ma.|||||
19286|Walli Volcanics|70727|6|Mentioned|p172|Ordovician|Ordovician|Geological province: Hill End Zone, Eastern Lachlan Orogen.||||Passive intruded by Wyangala Granite.||
19286|Walli Volcanics|70754|6|Mentioned|p450 Fig.2|Late Ordovician||||||Is overlain ?unconformably by Bowan Park Subgroup.||
19286|Walli Volcanics|71091|6|Mentioned|p142|||||||||
19286|Walli Volcanics|72495|6|Mentioned|p235|||Occurs to the south of Orange.||||||
19286|Walli Volcanics|73208|5|Briefly described|p873 Fig.5, p874|Late Ordovician|Late Ordovician||||||Volcaniclastic conglomerates (shoreline) overlain by mudstones and shales (lagoonal bay fill).|13-DEC-22
19286|Walli Volcanics|73209|6|Mentioned|p883, 888|||||||Is overlain disconformably by Fossil Hill Limestone (Cliefden Caves Limestone Subgroup).|Andesitic rocks.|
19286|Walli Volcanics|73492|5|Briefly described|p707|||Macquarie Arc.||||Underlies Cliefden Caves Limestone Subgroup||
19292|Wallis Creek Formation|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Tomago Coal Measures. Laminated sandstone, claystone, siltstone, tuff; numerous coal seams. Max. thickness: >300m. Geological Province: Sydney Basin.||||||
19292|Wallis Creek Formation|22969|4|Described|p 23|||Max. thickness: >300 m.||||||
19292|Wallis Creek Formation|33867|5|Briefly described|p7|||[Originally entered for NT. CEBMar95]||||||
19292|Wallis Creek Formation|34448|5|Briefly described|p433|||Permian. Tomago C.M.||||||
19292|Wallis Creek Formation|34465|6|Mentioned|Fig.5.11|||See P337||||||
19292|Wallis Creek Formation|35065|6|Mentioned|p43|||||||||
19292|Wallis Creek Formation|37084|6|Mentioned|p177|||||||||
19292|Wallis Creek Formation|39292|6|Mentioned|Fig. 6.3|||||||||
19292|Wallis Creek Formation|39308|6|Mentioned|p474|||See also Fig.23.4||||||
19292|Wallis Creek Formation|39609|6|Mentioned|p2|||||||||
19292|Wallis Creek Formation|40166|6|Mentioned|Fig.2|||||||||
19292|Wallis Creek Formation|40256|6|Mentioned|p303|||||||||
19292|Wallis Creek Formation|42182|6|Mentioned|p298|||||||||
19292|Wallis Creek Formation|43447|4|Described|Tbl 1,p21,diag.p22|||Part of Tomago Coal Measures.||||||14-DEC-06
19292|Wallis Creek Formation|43448|14|Not recorded|p224,225||Permian|Unit of Tomago Coal Measures||||||
19292|Wallis Creek Formation|45090|6|Mentioned|p26|||Relationship of rock units||||||
19292|Wallis Creek Formation|60281|5|Briefly described|p61|Late Permian|Late Permian|Of the Tomago Coal Measures.  Sandstone, siltstone, claystone and thin coals.  Max. thickness: >300m.  Geological Province: Sydney Basin.||||||
19292|Wallis Creek Formation|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Of the Tomago Coal Measures. Geological Province: Sydney Basin/Newcastle area.||||||
19292|Wallis Creek Formation|68493|6|Mentioned|p5 Fig.2|Lopingian|Lopingian|||Basal unit of the Tomago Coal Measures.||Overlies Mulbring Siltstone; is overlain by Four Mile Creek Formation.|Laminated sandstone, claystone, siltstone, coal, tuff.|
19293|Wallis Creek Subgroup|24471|5|Briefly described|p32 Fig.4|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Erins Vale Formation and Pheasants Nest Formation. Geological Province: Sydney Basin.||||||07-FEB-11
19293|Wallis Creek Subgroup|42214|6|Mentioned|p467|||||||||
19293|Wallis Creek Subgroup|43017|5|Briefly described|Fig.1,p372|||||||||
19293|Wallis Creek Subgroup|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Tomago Coal Measures|Includes Kulnura Marine Tongue.|||
19303|Walloon Coal Measures|12597|3|Fully described|p489, p491, p493 Fig.2, p496, p501-508|Middle Jurassic|Middle Jurassic|Clarence-Moreton and Surat Basins. Upgraded to Subgroup status in NE part of Clarence-Moreton Basin (Jones and Patrick, 1981). Known as Walloon Subgroup in Surat Basin. Unique high-volatile and perhydrous coal, suitable for synthetic fuels. Thickness to 600m. Type section in the Rosewood area (Cameron, 1970). Coal described in detail.|||Includes Taroom Coal Measures, Tangalooma Sandstone and Juandah Coal Measures.|Overlies Bundamba Group.|Lithic and feldspathic sandstones interbedded with siltstone, mudstone, carbonaceous shale and coal.|
19303|Walloon Coal Measures|13497|6|Mentioned|p142 |||Surat Basin.||||||
19303|Walloon Coal Measures|13516|6|Mentioned|p166, p167 fig 10, p173|Jurassic|Jurassic|In Surat Basin, Eromanga Basin.||||||
19303|Walloon Coal Measures|22757|5|Briefly described|p7|||Also Table6,p11. Surat Basin. 635 m.||||||
19303|Walloon Coal Measures|22820|6|Mentioned|p31 Fig. 11|Cretaceous|Jurassic|||||||
19303|Walloon Coal Measures|22857|4|Described|p295, p314-5, p546 App.1 Tb.A1.12|Late Jurassic|Middle Jurassic|Of Injune Creek Gp. Interbedded sst, sltst, claystone, coal, ironstone nodules. Contains significant coal deposits in Qld. Overlies Bundamba Gp; unconformably underlies Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Surat Basin. See p312-3 Fig.22.6||||||
19303|Walloon Coal Measures|22865|3|Fully described|p295,314,318|Bathonian|Middle Jurassic|||||||
19303|Walloon Coal Measures|22892|5|Briefly described|p7 fig6|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|23036|4|Described|6|||Max thickness: 700 m.||||||11-DEC-07
19303|Walloon Coal Measures|23050|4|Described|p23 Table 4|Late Jurassic|Middle Jurassic|Of Surat Basin. Age: palynology data indicates a J4 Jurassic age.||||||11-DEC-07
19303|Walloon Coal Measures|23051|5|Briefly described|Map Legend|Late Jurassic|Middle Jurassic|of Surat Basin.||||||
19303|Walloon Coal Measures|23053|6|Mentioned|Fig10p17|Callovian|Aalenian|||||||
19303|Walloon Coal Measures|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19303|Walloon Coal Measures|23375|6|Mentioned|p278|||of Surat Basin.||||||
19303|Walloon Coal Measures|23720|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|Grey claystone, lithic sandstone (arenites and wackes), coal.  Includes Towallum Basalt (basalt, minor basalt breccia) at the base.||||||15-DEC-04
19303|Walloon Coal Measures|23790|5|Briefly described|p10 Fig. 2|Jurassic|Jurassic|Geological Province: Surat Basin||||||
19303|Walloon Coal Measures|23799|4|Described|p49, p10 Tb. 1, p48 Fig. 3|Callovian|Bathonian|Supersedes Walloon beds (Cameron, 1907).   Correlated w Injune Creek Group. Unconformably overlain by Main Range Volcanics.  Max. thickness: 600m.  Type Section: in drillhole N.S.84, Ebenezer district. Geol. Prov: Clarence-Moreton Basin (also Surat Basin)||||||28-SEP-05
19303|Walloon Coal Measures|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|||||||
19303|Walloon Coal Measures|23811|5|Briefly described|Map Legend|Callovian|Bajocian|Thin-bedded, claystone, lithic and sublithic to feldspathic arenites, coal seams and partings; ironstone nodules and thin beds.  Includes Maclean Sandstone Member at top.Geological Province: Clarence-Moreton Basin.||||||20-DEC-04
19303|Walloon Coal Measures|23812|4|Described|p36, p34 Tb.4|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone, underlain by Bundamba Group.  Geological Province: Clarence-Moreton Basin.  Maximum thickness: 400m.||||||11-DEC-07
19303|Walloon Coal Measures|23818|6|Mentioned|p140|Triassic|Triassic|Geological Province: Great Artesian Basin.||||||
19303|Walloon Coal Measures|23843|4|Described|p455|Jurassic|Jurassic|Geological Province: Clarence-Moreton Basin.  Maximum thickness: 600m.||||||
19303|Walloon Coal Measures|23888|6|Mentioned|p262|||||||||
19303|Walloon Coal Measures|23982|5|Briefly described|p58 Fig.18|||Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|24068|4|Described|p270 Table 2|Middle Jurassic|Middle Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 520m.||||||
19303|Walloon Coal Measures|24070|5|Briefly described|p303|Jurassic|Jurassic|Geological Province: Coonamble Embayment.||||||
19303|Walloon Coal Measures|24092|5|Briefly described|p8 Fig.3|||Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|24127|5|Briefly described|p5|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24129|5|Briefly described|p4|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24159|5|Briefly described|p148 Fig. 2, p152|Middle Jurassic|Middle Jurassic|Geological Province: Surat Basin. Overlying Unit: Pilliga Sandstone. Underlying Unit: Hutton Sandstone.||||||
19303|Walloon Coal Measures|24160|6|Mentioned|p18|||Upper coal sequence produces bentonite as a byproduct.||||||
19303|Walloon Coal Measures|24225|5|Briefly described|p381|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|24237|5|Briefly described|p5 Fig.1|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|24243|5|Briefly described|p3 Fig.2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
19303|Walloon Coal Measures|24299|5|Briefly described|p3|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|24616|6|Mentioned|p35, p36, p37|||Geological Province: Clarence-Moreton and Surat Basins.||||||
19303|Walloon Coal Measures|29385|6|Mentioned|p82|||Jurassic.||||||
19303|Walloon Coal Measures|29393|6|Mentioned|p10|||Triassic.||||||
19303|Walloon Coal Measures|29591|6|Mentioned|p83|||||||||
19303|Walloon Coal Measures|29720|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|29869|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|29870|6|Mentioned|p15|||||||||
19303|Walloon Coal Measures|30024|6|Mentioned|p332|||||||||
19303|Walloon Coal Measures|30058|4|Described|p5|||See also p6-9. Jurassic age. type section illustrated p8. Is  the interval from 24ft 6 inches to 772ft in diamond drillhole N.S. 84 situated in the Ebenezer district. hole was drilled by the Department of Mines. Further description of location given, and shown on Fig.24, Fig. 25.||||||20-FEB-19
19303|Walloon Coal Measures|30131|6|Mentioned|p10|||See also P8||||||
19303|Walloon Coal Measures|30133|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|30455|6|Mentioned|p17|||See also P21. Jurassic age||||||
19303|Walloon Coal Measures|30457|6|Mentioned|p96|||||||||
19303|Walloon Coal Measures|30458|6|Mentioned|p3|||Jurassic age||||||
19303|Walloon Coal Measures|30460|6|Mentioned|p15|||See also P22. Jurassic age||||||
19303|Walloon Coal Measures|30463|6|Mentioned|p464|||Jurassic age||||||
19303|Walloon Coal Measures|30464|6|Mentioned|Fig.1|||Jurassic||||||
19303|Walloon Coal Measures|30465|6|Mentioned|p4|||||||||
19303|Walloon Coal Measures|30466|6|Mentioned|Fig.1|||Jurassic age||||||
19303|Walloon Coal Measures|30471|6|Mentioned|p131|||||||||
19303|Walloon Coal Measures|30475|6|Mentioned|p159|||||||||
19303|Walloon Coal Measures|30610|6|Mentioned|p326|||Refers Chesnut (1968) Hind & Helby (1969),Wallis (1968)||||||
19303|Walloon Coal Measures|30687|5|Briefly described|p63|||Middle-Upper Jurassic age. See also P65||||||
19303|Walloon Coal Measures|30692|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|30695|6|Mentioned|p3|||||||||
19303|Walloon Coal Measures|30699|6|Mentioned|p52|||See also P53. Stratigraphy. Map||||||
19303|Walloon Coal Measures|30701|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19303|Walloon Coal Measures|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19303|Walloon Coal Measures|30785|6|Mentioned|p397|||||||||
19303|Walloon Coal Measures|30911|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|30914|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|31086|6|Mentioned|p38|||? Mid Jurassic to ? Upper Jurassic age.||||||
19303|Walloon Coal Measures|31117|6|Mentioned|p379|||||||||
19303|Walloon Coal Measures|31118|4|Described|p322|||||||||
19303|Walloon Coal Measures|31132|6|Mentioned|p148|||||||||
19303|Walloon Coal Measures|31560|6|Mentioned|p630|||||||||
19303|Walloon Coal Measures|31563|6|Mentioned|p144|||||||||
19303|Walloon Coal Measures|32136|6|Mentioned|p5|||Miospores||||||
19303|Walloon Coal Measures|32137|6|Mentioned|p355|||||||||
19303|Walloon Coal Measures|32276|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper Jurassic.M - U||||||
19303|Walloon Coal Measures|32413|6|Mentioned|p86|||||||||
19303|Walloon Coal Measures|32492|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19303|Walloon Coal Measures|32671|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|32913|6|Mentioned|p393|||Stratigraphy||||||
19303|Walloon Coal Measures|32916|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|32920|6|Mentioned|p89|||||||||
19303|Walloon Coal Measures|32924|6|Mentioned|p112|||||||||
19303|Walloon Coal Measures|32990|6|Mentioned|p81|||||||||
19303|Walloon Coal Measures|33075|6|Mentioned|Table 1|||Refers Whitehouse (1954)||||||
19303|Walloon Coal Measures|33091|5|Briefly described|p10|||Stratigraphy||||||
19303|Walloon Coal Measures|33128|6|Mentioned|Fig.11|||||||||
19303|Walloon Coal Measures|33367|3|Fully described|p17|||Equiv.Birkhead Fm.||||||
19303|Walloon Coal Measures|33368|6|Mentioned|p17|||Oil shale seams.||||||
19303|Walloon Coal Measures|33371|4|Described|p58|||Equiv. Birkhead Fm.||||||
19303|Walloon Coal Measures|33381|3|Fully described|p110|||Jur. Map. See also pp117,119,120 and 123.||||||11-DEC-07
19303|Walloon Coal Measures|33476|4|Described|p104|||Mention Fig.10||||||
19303|Walloon Coal Measures|33672|6|Mentioned|p44|||||||||
19303|Walloon Coal Measures|33709|6|Mentioned|p100|||Jurassic.||||||
19303|Walloon Coal Measures|33766|6|Mentioned|Map legend|Middle Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|33774|6|Mentioned|p54|||Correlation||||||
19303|Walloon Coal Measures|33828|6|Mentioned|Table 3|||||||||
19303|Walloon Coal Measures|33939|6|Mentioned|p393|||Jurassic.  Flora.||||||
19303|Walloon Coal Measures|33971|6|Mentioned|p36|||See also Fig.29.||||||
19303|Walloon Coal Measures|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
19303|Walloon Coal Measures|34254|6|Mentioned|p489|||Jurassic||||||
19303|Walloon Coal Measures|34287|6|Mentioned|p171|||Jurassic. See also PP173,175||||||
19303|Walloon Coal Measures|34340|3|Fully described|p469|||||||||
19303|Walloon Coal Measures|34400|5|Briefly described|p13|||||||||
19303|Walloon Coal Measures|34452|6|Mentioned|p7|||See also PP12,13||||||
19303|Walloon Coal Measures|34540|6|Mentioned|p65|||Middle Jurassic||||||
19303|Walloon Coal Measures|34593|6|Mentioned|p539|||Jurassic||||||
19303|Walloon Coal Measures|34611|6|Mentioned|p140|||Jurassic||||||
19303|Walloon Coal Measures|34755|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|34881|6|Mentioned|p526|||||||||
19303|Walloon Coal Measures|34905|6|Mentioned|p530|||||||||
19303|Walloon Coal Measures|34950|5|Briefly described|p40|||||||||
19303|Walloon Coal Measures|35016|6|Mentioned|p41|||||||||
19303|Walloon Coal Measures|35053|5|Briefly described|p36|||||||||
19303|Walloon Coal Measures|35065|6|Mentioned|p45|||||||||
19303|Walloon Coal Measures|35101|6|Mentioned|p56|||||||||
19303|Walloon Coal Measures|35126|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19303|Walloon Coal Measures|35156|4|Described|p7|||See also Table.2||||||
19303|Walloon Coal Measures|35157|6|Mentioned|p525|||||||||
19303|Walloon Coal Measures|35435|6|Mentioned|p43|||||||||
19303|Walloon Coal Measures|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
19303|Walloon Coal Measures|35648|6|Mentioned|p16|||||||||
19303|Walloon Coal Measures|35663|6|Mentioned|p129|||||||||
19303|Walloon Coal Measures|35811|5|Briefly described|Table 5|||||||||
19303|Walloon Coal Measures|35866|6|Mentioned|p403|||||||||
19303|Walloon Coal Measures|35937|6|Mentioned|p621|||||||||
19303|Walloon Coal Measures|36172|6|Mentioned|Appendix|||||||||
19303|Walloon Coal Measures|36243|6|Mentioned|Table 7A|||||||||
19303|Walloon Coal Measures|36327|6|Mentioned|p7|||||||||
19303|Walloon Coal Measures|36354|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|36570|2|Defined|p34|Jurassic|Jurassic|See also p25 and Fig.9, p55.||||||04-JUN-07
19303|Walloon Coal Measures|36574|6|Mentioned|p599|||||||||
19303|Walloon Coal Measures|36579|6|Mentioned|p447|||||||||
19303|Walloon Coal Measures|36779|4|Described|p7|||||||||
19303|Walloon Coal Measures|36939|6|Mentioned|p218|||||||||
19303|Walloon Coal Measures|36961|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|37065|5|Briefly described|p38|||||||||
19303|Walloon Coal Measures|37114|6|Mentioned|p308|||||||||
19303|Walloon Coal Measures|37116|6|Mentioned|p310|||||||||
19303|Walloon Coal Measures|37117|4|Described|p313|||||||||
19303|Walloon Coal Measures|37118|6|Mentioned|p318|||||||||
19303|Walloon Coal Measures|37122|4|Described|p328, p331|||||||||
19303|Walloon Coal Measures|37252|6|Mentioned|Map legend|Jurassic|Jurassic|||||||
19303|Walloon Coal Measures|37375|4|Described|p473|||||||||
19303|Walloon Coal Measures|37436|6|Mentioned|p540|||||||||
19303|Walloon Coal Measures|37463|6|Mentioned|p479|||||||||
19303|Walloon Coal Measures|37856|6|Mentioned|Table 3|||||||||
19303|Walloon Coal Measures|37988|6|Mentioned|p209|||||||||
19303|Walloon Coal Measures|37991|6|Mentioned|p179|||||||||
19303|Walloon Coal Measures|37992|4|Described|p165|||||||||
19303|Walloon Coal Measures|37993|6|Mentioned|p153|||||||||
19303|Walloon Coal Measures|37994|5|Briefly described|p143|||||||||
19303|Walloon Coal Measures|37995|4|Described|p64|||||||||
19303|Walloon Coal Measures|37997|6|Mentioned|p83|||||||||
19303|Walloon Coal Measures|38064|5|Briefly described|p41|||||||||
19303|Walloon Coal Measures|38068|6|Mentioned|p71|||||||||
19303|Walloon Coal Measures|38074|5|Briefly described|Table 1|||||||||
19303|Walloon Coal Measures|38079|6|Mentioned|p46|||||||||
19303|Walloon Coal Measures|38080|6|Mentioned|p54|||||||||
19303|Walloon Coal Measures|38205|2|Defined|p86|Jurassic|Jurassic|Previously "Walloon Beds".||||||04-JUN-07
19303|Walloon Coal Measures|38391|6|Mentioned|p11|||||||||
19303|Walloon Coal Measures|38441|6|Mentioned|Map legend|Middle Jurassic|Early Jurassic|Early to Middle JurassicE - M||||||
19303|Walloon Coal Measures|38741|5|Briefly described|p337|||||||||
19303|Walloon Coal Measures|39071|6|Mentioned|p339|||||||||
19303|Walloon Coal Measures|39212|5|Briefly described|p16|||See also P22||||||
19303|Walloon Coal Measures|39218|6|Mentioned|p48|||Flora||||||
19303|Walloon Coal Measures|39413|6|Mentioned|p53|||||||||
19303|Walloon Coal Measures|39445|5|Briefly described|Table 10|||See also Fig.8||||||
19303|Walloon Coal Measures|39494|6|Mentioned|Fig.5|||||||||
19303|Walloon Coal Measures|39642|6|Mentioned|Fig.1|||||||||
19303|Walloon Coal Measures|39666|6|Mentioned|p113|||||||||
19303|Walloon Coal Measures|39708|6|Mentioned|p477|||||||||
19303|Walloon Coal Measures|39757|6|Mentioned|p1601|||||||||
19303|Walloon Coal Measures|39907|4|Described|p16|||||||||
19303|Walloon Coal Measures|39941|6|Mentioned|p471|||||||||
19303|Walloon Coal Measures|39942|6|Mentioned|p465|||||||||
19303|Walloon Coal Measures|39943|6|Mentioned|Table 9A|||||||||
19303|Walloon Coal Measures|39969|6|Mentioned|p11|||||||||
19303|Walloon Coal Measures|39988|6|Mentioned|p288|||||||||
19303|Walloon Coal Measures|40030|6|Mentioned|Fig.5|||||||||
19303|Walloon Coal Measures|40245|6|Mentioned|Table 1|||See also Table 2||||||
19303|Walloon Coal Measures|40249|6|Mentioned|p38|||||||||
19303|Walloon Coal Measures|40250|6|Mentioned|p35|||||||||
19303|Walloon Coal Measures|40540|6|Mentioned|p150|||||||||
19303|Walloon Coal Measures|40544|6|Mentioned|Fig.6|||||||||
19303|Walloon Coal Measures|40623|5|Briefly described|p30|||||||||
19303|Walloon Coal Measures|40767|6|Mentioned|p14|||||||||
19303|Walloon Coal Measures|40780|4|Described|p6|||||||||
19303|Walloon Coal Measures|40896|6|Mentioned|p51|||||||||
19303|Walloon Coal Measures|40926|6|Mentioned|Table 2|||||||||
19303|Walloon Coal Measures|40953|4|Described|p19|||||||||
19303|Walloon Coal Measures|41060|5|Briefly described|p2|||Generalized stratigraphy||||||
19303|Walloon Coal Measures|41122|6|Mentioned|p201|||||||||
19303|Walloon Coal Measures|41175|6|Mentioned|p195|||||||||
19303|Walloon Coal Measures|41176|6|Mentioned|p206|||||||||
19303|Walloon Coal Measures|41187|6|Mentioned|p217|||||||||
19303|Walloon Coal Measures|41188|6|Mentioned|Fig.3|||||||||
19303|Walloon Coal Measures|41210|6|Mentioned|p164|||||||||
19303|Walloon Coal Measures|41216|6|Mentioned|p300|||See also Fig.18||||||
19303|Walloon Coal Measures|41247|6|Mentioned|Fig.7|||||||||
19303|Walloon Coal Measures|41266|6|Mentioned|Fig.3|||||||||
19303|Walloon Coal Measures|41290|6|Mentioned|p226|||||||||
19303|Walloon Coal Measures|41591|6|Mentioned|p17|||See also Fig.2||||||
19303|Walloon Coal Measures|41631|4|Described|p20|||See also Fig.2||||||
19303|Walloon Coal Measures|41906|5|Briefly described|Table 2 P15|||||||||
19303|Walloon Coal Measures|41992|4|Described|Fig.2 P183|||||||||
19303|Walloon Coal Measures|42007|5|Briefly described|Fig.2 P182|||||||||
19303|Walloon Coal Measures|42182|5|Briefly described|p302|||||||||
19303|Walloon Coal Measures|42187|5|Briefly described|p321|||||||||
19303|Walloon Coal Measures|42248|5|Briefly described|p397|||||||||
19303|Walloon Coal Measures|42256|6|Mentioned|Fig.2 P243|||||||||
19303|Walloon Coal Measures|42336|5|Briefly described|p4|||||||||
19303|Walloon Coal Measures|42463|6|Mentioned|Fig.3 P170|||||||||
19303|Walloon Coal Measures|42493|5|Briefly described|Fig. 1 P18|||||||||
19303|Walloon Coal Measures|42525|5|Briefly described|Map legend|Late Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|42634|6|Mentioned|p24|||||||||
19303|Walloon Coal Measures|42648|5|Briefly described|p42|||||||||
19303|Walloon Coal Measures|42719|5|Briefly described|p15|||||||||
19303|Walloon Coal Measures|42869|5|Briefly described|Table 1, P33|||||||||
19303|Walloon Coal Measures|42894|5|Briefly described|Fig.1 P20|||||||||
19303|Walloon Coal Measures|42911|5|Briefly described|p13|||||||||
19303|Walloon Coal Measures|42951|5|Briefly described|Fig.11|||||||||
19303|Walloon Coal Measures|42998|5|Briefly described|p58|||||||||
19303|Walloon Coal Measures|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
19303|Walloon Coal Measures|43001|6|Mentioned|Fig.3,p120|||||||||
19303|Walloon Coal Measures|43002|5|Briefly described|Fig.2,p135|||||||||
19303|Walloon Coal Measures|43076|5|Briefly described|p9|||||||||
19303|Walloon Coal Measures|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Surat Basin.||||||12-APR-05
19303|Walloon Coal Measures|43344|14|Not recorded|p13,14|Jurassic|Late Triassic|Part of Bundamba Group||||||
19303|Walloon Coal Measures|43383|14|Not recorded|p24,25,28|||||||||
19303|Walloon Coal Measures|43384|14|Not recorded|Map Legend||Jurassic|||||||
19303|Walloon Coal Measures|43404|14|Not recorded|Table p11||Jurassic|||||||
19303|Walloon Coal Measures|43423|4|Described|p221,222,224-5|||||||||
19303|Walloon Coal Measures|43436|14|Not recorded|Map Legend||Jurassic|(Provisional Edition)||||||
19303|Walloon Coal Measures|43453|14|Not recorded|Map Legend|Cretaceous|Triassic|(Provisional Edition)||||||
19303|Walloon Coal Measures|43454|14|Not recorded|Map Legend|Cretaceous|Triassic|||||||
19303|Walloon Coal Measures|43459|14|Not recorded|p316|||||||||
19303|Walloon Coal Measures|43463|14|Not recorded|p8,9;map|||Spicer's Peak area,SE Qld||||||
19303|Walloon Coal Measures|43468|14|Not recorded|Map Legend||Jurassic|Provisional Edition||||||
19303|Walloon Coal Measures|43582|6|Mentioned|Fig.5,p16,28||Middle Jurassic|||||||
19303|Walloon Coal Measures|43602|6|Mentioned|Fig3 p194|||In Surat Basin||||||
19303|Walloon Coal Measures|43736|6|Mentioned|p3|||||||||
19303|Walloon Coal Measures|43881|2|Defined|p6-7,11-14,37-44,55,||Jurassic|In QLD on p80,87,135. In NSW on p71-4,85-87,91-7,106-108,164.||||||
19303|Walloon Coal Measures|43883|14|Not recorded|p18 Fig.4-3|||||||||
19303|Walloon Coal Measures|43884|14|Not recorded|p2,4||Jurassic|||||||
19303|Walloon Coal Measures|43895|14|Not recorded|p116|||||||||
19303|Walloon Coal Measures|43907|14|Not recorded|p11-13||Early Jurassic|||||||
19303|Walloon Coal Measures|43908|14|Not recorded|p1,6,26|||||||||
19303|Walloon Coal Measures|43910|14|Not recorded|p4,5,7,11,19|||||||||
19303|Walloon Coal Measures|43911|14|Not recorded|p17,18|||||||||
19303|Walloon Coal Measures|43917|14|Not recorded|p28,32|||||||||
19303|Walloon Coal Measures|43918|14|Not recorded|p54,63,64|||||||||
19303|Walloon Coal Measures|43923|6|Mentioned|p18||Jurassic|||||||
19303|Walloon Coal Measures|43924|14|Not recorded|p2,15|||See Walloon Formation.||||||
19303|Walloon Coal Measures|43925|14|Not recorded|p42,45|||||||||
19303|Walloon Coal Measures|43984|14|Not recorded|p130,131,139,140|||||||||
19303|Walloon Coal Measures|43991|4|Described|p48||Jurassic|Upper Marburg Formation.||||||
19303|Walloon Coal Measures|43993|14|Not recorded|p93-95,97-100,102||Jurassic|Ref. to Dunstan 1915.||||||
19303|Walloon Coal Measures|43995|14|Not recorded|Tb.p9&10,11-61,Map,||Early Cretaceous|Figs.3,4,9,11,15||||||
19303|Walloon Coal Measures|44021|14|Not recorded|p233 Fig.1|||Equivalent to Birkhead Formation in Eromanga Basin.||||||
19303|Walloon Coal Measures|44026|14|Not recorded|p123,124||Jurassic|||||||
19303|Walloon Coal Measures|44028|14|Not recorded|Fi.2,5,7,p509,511-14||Jurassic|Correlates with Gowen Beds. See Strat Table.||||||
19303|Walloon Coal Measures|44029|14|Not recorded|p153-5,157-8,167-8|||||||||
19303|Walloon Coal Measures|44031|14|Not recorded|p2,11|Late Jurassic|Middle Jurassic|||||||
19303|Walloon Coal Measures|44033|14|Not recorded|Tb.1,p4|Early Cretaceous|Jurassic|A.A.O. Beryl No.1||||||
19303|Walloon Coal Measures|44068|14|Not recorded|p15,16|||||||||
19303|Walloon Coal Measures|44077|14|Not recorded|p298|||||||||
19303|Walloon Coal Measures|44084|14|Not recorded|p2,4,6,10,12,14,16,||Middle Jurassic|p18,22,26,30,32||||||
19303|Walloon Coal Measures|44088|14|Not recorded|p6,7|||||||||
19303|Walloon Coal Measures|44089|4|Described|p4|||||||||
19303|Walloon Coal Measures|44091|14|Not recorded|p57,58||Jurassic|||||||
19303|Walloon Coal Measures|44128|14|Not recorded|Tb.1,p426|||||||||
19303|Walloon Coal Measures|44164|14|Not recorded|p24|||||||||
19303|Walloon Coal Measures|44171|14|Not recorded|p194,197,198|||Replaces Birkhead Formation.||||||
19303|Walloon Coal Measures|44240|14|Not recorded|p336|||||||||
19303|Walloon Coal Measures|44241|14|Not recorded|p6||Middle Jurassic|||||||
19303|Walloon Coal Measures|44252|14|Not recorded|p397|||||||||
19303|Walloon Coal Measures|44269|4|Described|p15,map||Jurassic|||||||
19303|Walloon Coal Measures|44375|14|Not recorded|p310|||Overlain by Blythesdale Group.||||||
19303|Walloon Coal Measures|44377|14|Not recorded|p3,8|||||||||
19303|Walloon Coal Measures|44423|14|Not recorded|p20|||||||||
19303|Walloon Coal Measures|44432|14|Not recorded|p58||Middle Jurassic|Occurs within Rosewood Stage.||||||
19303|Walloon Coal Measures|44450|4|Described|p28 Table 7|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton Basin.||||||11-DEC-07
19303|Walloon Coal Measures|44510|14|Not recorded|p259,Figs.35,36|||||||||
19303|Walloon Coal Measures|44511|14|Not recorded|p713||Early Jurassic|||||||
19303|Walloon Coal Measures|44553|14|Not recorded|p301|||||||||
19303|Walloon Coal Measures|44554|2|Defined|p288-295|||Overlies Marburg Sandstone.||||||
19303|Walloon Coal Measures|44605|14|Not recorded|p40|||||||||
19303|Walloon Coal Measures|44607|14|Not recorded|p35,36|||||||||
19303|Walloon Coal Measures|44611|14|Not recorded|p20|||||||||
19303|Walloon Coal Measures|44614|14|Not recorded|unknown (p22-26)|||Not listed on white card.||||||
19303|Walloon Coal Measures|44615|14|Not recorded|p21|||Clay deposits.||||||
19303|Walloon Coal Measures|44667|14|Not recorded|p306|||||||||
19303|Walloon Coal Measures|44674|14|Not recorded|p460|||||||||
19303|Walloon Coal Measures|44698|14|Not recorded|p111|||||||||
19303|Walloon Coal Measures|44711|14|Not recorded|p26|||Soils||||||
19303|Walloon Coal Measures|44727|14|Not recorded|p303-304|||||||||
19303|Walloon Coal Measures|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
19303|Walloon Coal Measures|44734|14|Not recorded|p5,6,13,16,19|||Pine Mountain area.||||||
19303|Walloon Coal Measures|44737|14|Not recorded|p129|||Fine grained and often calcareous in Bremer Valley, south of Rosewood.||||||
19303|Walloon Coal Measures|44752|14|Not recorded|p297|||Equivalent ot Tiaro Coal Measures.||||||
19303|Walloon Coal Measures|44774|5|Briefly described|p30||Early Jurassic|Rosewood area.||||||
19303|Walloon Coal Measures|44775|14|Not recorded|Map 2||Jurassic|||||||
19303|Walloon Coal Measures|44777|14|Not recorded|p55|||Footprints of large bipedal theropod in root shale of Striped Bacon Seam.||||||
19303|Walloon Coal Measures|44780|14|Not recorded|p297|||Flora suggests correlation with Ballow Group.||||||
19303|Walloon Coal Measures|44781|14|Not recorded|p359,363|||||||||
19303|Walloon Coal Measures|44782|2|Defined|p38,40-42,Pl.1|||||||||
19303|Walloon Coal Measures|44783|14|Not recorded|p2,20,24,26-29,43,44|||||||||
19303|Walloon Coal Measures|44784|14|Not recorded|p13,map 3||Jurassic|||||||
19303|Walloon Coal Measures|44803|14|Not recorded|p164,167||Early Jurassic|Plant fossils||||||
19303|Walloon Coal Measures|44813|14|Not recorded|p77||Jurassic|||||||
19303|Walloon Coal Measures|44819|14|Not recorded|p89|||||||||
19303|Walloon Coal Measures|45110|2|Defined|p94|Middle Jurassic|Middle Jurassic|See also p10 and p24.||||||04-JUN-07
19303|Walloon Coal Measures|45150|6|Mentioned|p2|||||||||
19303|Walloon Coal Measures|46159|14|Not recorded|p.404|||||||||
19303|Walloon Coal Measures|46791|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19303|Walloon Coal Measures|46984|6|Mentioned|Table 1|||||||||
19303|Walloon Coal Measures|48585|4|Described|p7,9,14,Pl.1|||||||||
19303|Walloon Coal Measures|48606|14|Not recorded|p6,Pl.1,sh.1,2|||(G/55-12).||||||
19303|Walloon Coal Measures|48611|4|Described|p9,11,Fig.2|||||||||
19303|Walloon Coal Measures|48770|6|Mentioned|p109|||||||||
19303|Walloon Coal Measures|48906|14|Not recorded|Tb.2,fig.1||Middle Jurassic|||||||
19303|Walloon Coal Measures|48908|6|Mentioned|p46||Jurassic|||||||
19303|Walloon Coal Measures|48917|3|Fully described|p24|||See stratigraphic table p13. Coal and Water p47.||||||11-DEC-07
19303|Walloon Coal Measures|48919|6|Mentioned|p58|||Refers Whitehouse (1954)||||||
19303|Walloon Coal Measures|48920|6|Mentioned|Table 7|||||||||
19303|Walloon Coal Measures|48926|6|Mentioned|p15|||P15 et seq.||||||
19303|Walloon Coal Measures|48928|6|Mentioned|p13|||Jurassic||||||
19303|Walloon Coal Measures|49010|6|Mentioned|Fig.4|||Surat Basin||||||
19303|Walloon Coal Measures|49011|6|Mentioned|Fig.3|||Surat Basin||||||
19303|Walloon Coal Measures|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Overlies: Koukandowie Volcanics.  Underlies: Main Range Volcanics.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
19303|Walloon Coal Measures|50631|5|Briefly described|Map Legend|Jurassic|Jurassic|Sandstone, siltstone, shale, coalseams.||||||06-JUL-04
19303|Walloon Coal Measures|60079|5|Briefly described|Map Legend|Middle Jurassic|Middle Jurassic|Includes: Maclean Sandstone Member.  Claystone, sandstones, coal.||||||20-JUL-04
19303|Walloon Coal Measures|60281|5|Briefly described|p22, Fig. 18 App.1|Middle Jurassic|Middle Jurassic|Interbedded sandstone, siltstone, claystone, coal, ironstone nodules. Contains the Maclean Sandstone Member. Overlain by Kangaroo Creek Sst.; overlies the Koukandowie Fm. Max. thickness: 400m. Geological Province: Clarence-Moreton, Surat & Eromanga Basins||||||
19303|Walloon Coal Measures|60699|6|Mentioned|p30|||See also informal references to Walloon coals and Walloon coal.||||||
19303|Walloon Coal Measures|60700|5|Briefly described|p37, p39|Jurassic|Jurassic|Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|60993|3|Fully described|p31, p6 Fig. 2|Bathonian|Aalenian|Supersedes Walloon Beds. Conformably overlain by Kangaroo Creek Sst; conformably overlies the Marburg Subgp. Max. thickness: ~60m. Geol. Prov: Clarence-Moreton Basin-Surat Basin. Passes laterally into Birkhead Fm. Of the Injune Creek Gp.||||||
19303|Walloon Coal Measures|60995|4|Described|p67, p51 Fig. 3|Middle Jurassic|Middle Jurassic|Sandstone, siltstone, grey claystone, coal; ironstone nodules. Conformably overlies the Bundamba Gp; overlain by Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Clarence-Moreton and Surat Basins.||||||
19303|Walloon Coal Measures|60996|5|Briefly described|p125|||Characteristically contains volcaniclastic detritus. Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|60997|5|Briefly described|p138, p142 Fig. 4|Kimmeridgian|Bathonian|Characterised by sandstone rich in volcanic rock fragments and feldspar. Overlain by Kangaroo Creek Sst; conformably overlies Koukandowie Formation. Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|60998|6|Mentioned|p146 Fig. 2|||||||||
19303|Walloon Coal Measures|60999|5|Briefly described|p168, p175|Middle Jurassic||Overlain by Kangaroo Creek Sandstone and Grafton Formation. Geological Province: Clarence-Moreton and Surat Basins. See also p172 Fig. 6.||||||
19303|Walloon Coal Measures|61000|5|Briefly described|p181, p182|Middle Jurassic|Middle Jurassic|Overlain by Kangaroo Creek Sandstone. Geological Province: Clarence-Moreton and Surat Basins. See also p186.||||||
19303|Walloon Coal Measures|61001|6|Mentioned|p189|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61002|5|Briefly described|p198 Fig 2|||Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61004|5|Briefly described|p230|Jurassic|Jurassic|Oil mature unit in the western and central parts of NSW, containing high vitrinite and low liptinite contents.  Geological Province: Clarence-Moreton Basin.||||||
19303|Walloon Coal Measures|61005|5|Briefly described|p239|||Geological Province: Clarence-Moreton Basin.  See also p255 Figs. 23, 24 and 25.||||||
19303|Walloon Coal Measures|61006|5|Briefly described|p277, p289|Jurassic|Jurassic|Mudstone, labile sandstone, coal; have significant potential to generate oil. Geological Province: Clarence-Moreton Basin. See also p279 Tb. 1, p285.||||||
19303|Walloon Coal Measures|61310|4|Described|p21, p11 Fig. C2|Middle Jurassic|Middle Jurassic|Grey claystone, commonly carbonaceous or with banded coal horizons and fine- to medium-grained grey lithic sst. Overlie Marburg Subgroup units; overlain by Kangaroo Creek Sst. Max. thickness: 400m. Geol. Prov: Clarence-Moreton, Surat and Eromanga Basins.||||||
19303|Walloon Coal Measures|61313|6|Mentioned|p99|||Time equivalent of upper parts of Purlawaugh Formation.||||||
19303|Walloon Coal Measures|61377|5|Briefly described|p151, p142|Middle Jurassic|Middle Jurassic|Coal measure sequence of coal, tight sandstone, sltst+ shale with good oil source characteristics; excellent seal for underlying reservoirs in Hutton Fm. Conformable below Pilliga Sst. Geol.Prov: Surat Basin. See also p148 Tb. SU1, p149 Fig. SU8.||||||07-FEB-11
19303|Walloon Coal Measures|61611|5|Briefly described|p264, p265 Fig. 3|Early Jurassic|Late Triassic|Lateral equivalent to Tiaro Coal Measures. Geological Province: Surat Basin.||||||13-MAR-09
19303|Walloon Coal Measures|61617|6|Mentioned|p346 Tb. 3|||Net coal thickness: 10-25m. Geological Province: Surat Basin.||||||11-FEB-09
19303|Walloon Coal Measures|61775|6|Mentioned|p182 Fig. 1||Mesozoic|||||||
19303|Walloon Coal Measures|63218|6|Mentioned|p211.|||Reid's (1921) name for the Walloon Beds of Cameron (1907). Subsequently upgraded to Walloon Subgroup by Jones and Patrick (1981).||||||
19303|Walloon Coal Measures|63347|5|Briefly described|p5 Fig. 2|Early Cretaceous|Middle Jurassic|Geological Province: Surat Basin.||||||
19303|Walloon Coal Measures|63729|5|Briefly described|Map legend|Jurassic|Jurassic|Overlie the Marburg Subgroup; Interfinger with Kumbarilla beds. Fine- to medium-grained feldspathic sandstone and coarse-grained quartzose sandstone.||||||11-DEC-07
19303|Walloon Coal Measures|63731|5|Briefly described|Map legend|Jurassic|Jurassic|Shale, siltstone, lithic-labile sandstone, coal, minor quartz sandstone.||||||12-DEC-07
19303|Walloon Coal Measures|63748|4|Described|p21, p23|Middle Jurassic|Middle Jurassic|Conformable on Marburg Subgroup (Bundamba Group). Unconformable below main Range Volcanics. Geol.prov:Clarence-Moreton Basin. Flat-lying sequence of lithic and feldspathic labile sandstone interbedded with siltstone, mudstone, carbonaceous shale and coal.||||||07-FEB-11
19303|Walloon Coal Measures|63979|5|Briefly described|p36, p38|||Overlies Springbok Sandstone. Geological Province: Surat and Moreton Basins.||||||07-FEB-11
19303|Walloon Coal Measures|64197|6|Mentioned|p630 Fig.7|Jurassic|Jurassic|Surat Basin.||||Underlies Springbok Sandstone; overlies Eurombah Formation.||
19303|Walloon Coal Measures|64232|6|Mentioned|p12|||Geological Province: Polda Basin.||||||24-JUL-08
19303|Walloon Coal Measures|64289|5|Briefly described|p6 Fig. 2, p11, p14|Middle Jurassic|Middle Jurassic|Geological province: Clarence-Moreton and Surat Basins.||||||07-FEB-11
19303|Walloon Coal Measures|64665|5|Briefly described|p53 Fig.2, p60, p61.|Middle Jurassic|Middle Jurassic|Surat and Clarence-Moreton Basins. It appears that Walloon Subgroup is used as an alternative name in the Surat Basin. Abundant stone and dirt bands produce high ash raw coal (30 - 40 %);  perhydrous and very hard; high volatile bituminous rank; feedstock for mine-mouth power plants but can be washed down to 12 - 17% export product.||Basal unit in Injune Creek Group.||Overlies Hutton Sandstone (Surat Basin) and Bundamba Group (Clarence-Moreton Basin).||
19303|Walloon Coal Measures|64856|3|Fully described|p79, p85-92, p102|Callovian|Bathonian|Reid (1921); formerly Walloon beds of Cameron (1907). Type section was designated as the interval 7-235m in drillhole N.S.84 by Cameron (1970). Surat Basin. Raised to Subgroup rank by Jones and Patrick in 1979. Argillaceous sandstone, siltstone, mudstone and coal. Conformably overlies Hutton Sandstone and laterally continuous with the Birkhead Formation. Up to 507m thick. Age from palynofloral units APJ42, 43, 5.|| ||||29-NOV-17
19303|Walloon Coal Measures|64857|5|Briefly described|p132-133, p113 Fig.3|||Lithic labile sandstones and coals. Relationship with underlying unit not clear: Figures show it overlying the Hutton Sandstone while text states it overlies Eurombah Formation. Surat Basin.||||||
19303|Walloon Coal Measures|64858|6|Mentioned|p180, p181 Tb.1, p187, p187 Fig.14|||Surat Basin.||||||30-NOV-09
19303|Walloon Coal Measures|64859|6|Mentioned|p195|||||||||
19303|Walloon Coal Measures|65096|5|Briefly described|p367-368, 371-374, 378, 379 Fig.7, 380|Middle Jurassic|Middle Jurassic|Eastern Surat Basin. Jones and Patrick (1981) accorded the Walloon Coal Measures sub-group status, but this was rejected by Green et al (1997). This study follows Jones and Patrick's usage. ~ 420-440 m thick in the eastern Surat Basin. Possibly exceeding 800 m in NSW.  A series of meander and back swamp deposits.|||Includes (from base) Eurombah Formation, Taroom Coal Measures,Tangalooma Sandstone, Juandah Coal Measures.|Equivalent of the Mulgildie Coal Measures, and the lower beds of the Injune Creek Group and the Birkhead Formation. Overlain by the Springbok Sandstone.|Includes high volatile bituminous coals with a high proportion of vitrinite.|
19303|Walloon Coal Measures|65112|5|Briefly described|p323, 327, 328; Fig 11 p324, fig 15 p327|Jurassic|Jurassic||166-158 Ma.|||Underlies the Springbok Sandstone; overlies the Hutton Sandstone.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|15-JAN-15
19303|Walloon Coal Measures|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Middle Jurassic|Underlies the Springbok Sandstone, overlies the Hutton Sandstone. Shown as Walloon CM.||||||
19303|Walloon Coal Measures|65114|5|Briefly described|p385 Fig.3|Late Jurassic|Middle Jurassic|Written as Walloon CM||||||
19303|Walloon Coal Measures|65116|5|Briefly described|p455, Fig 2 p437|Late Jurassic|Middle Jurassic|Underlies the Springbok Sandstone, overlies the Hutton Sandstone, Surat Basin. Interbedded lithic sandstone, siltstone, mudstone and coal.||||||
19303|Walloon Coal Measures|65117|4|Described|p461, 462-3, 469-72, Fig 4 p465, 466|Callovian|Bathonian|Surat Basin. Overlies and interfingers with Eurombah Formation. Overlain by Springbok Sandstone. Sandstone, siltstone, mudstone and rare to abundant coal seams. Thickness up to 650m. Base of unit youngs to west. Coal seam gas source.||||||
19303|Walloon Coal Measures|65119|6|Mentioned|p526, Fig 6 p512, Fig 13-14|Late Jurassic|Middle Jurassic|Of Injune Creek Group. Coal.||||||
19303|Walloon Coal Measures|65388|5|Briefly described|p215, 216|Callovian|Bathonian|Of Injune Creek Group. Correlated with Mulgildie Coal Measures on stratigraphic and lithological grounds. Conformably (transitionally) overlies Hutton Sandstone. Age: late Middle Jurassic (Bathonian to Callovian), based on palynofloras attributed to units APJ42, APJ43 and APJ5 (Price, 1997).||||||
19303|Walloon Coal Measures|65489|6|Mentioned|p24|||Volcanic-arc-derived sediments.||||||
19303|Walloon Coal Measures|66529|6|Mentioned|p12 Fig.5 |||Surat Basin.||||Overlies Hutton Sandstone and Eurombah Formation. Is overlain by Injune Creek Group, Kumbarilla beds and Pilliga Sandstone.||
19303|Walloon Coal Measures|66915|5|Briefly described|p6 Fig.3, p9|Middle Jurassic|Middle Jurassic|Surat Basin.||Injune Creek Group.||||
19303|Walloon Coal Measures|67365|5|Briefly described|p81, p85, p86. |Middle Jurassic|Middle Jurassic|Surat Basin. Coal seam gas extraction was applied to this field from 2000. High volatile, perhydrous, sub-bituminous and non-coking coals with moderate gas contents (5-10 m3 per tonne) and generally high permeabilities.|||Includes Juandah and Taroom Coal Members.|||
19303|Walloon Coal Measures|67402|6|Mentioned|p161, p188|Bajocian|Aalenian|||Walloon Subgroup||||
19303|Walloon Coal Measures|68003|5|Briefly described|p55 Fig.3-m, p57 Fig.3-n, pp63-64, p127.|Middle Jurassic|Middle Jurassic|Northern Brigalow Belt South Bioregion. Stratigraphic equivalent of upper part of Purlawaugh Formation. Deposited in meandering streams and swamps. Outcrops very poorly. Coal seams are more abundant towards the top. Subsurface, thickens northward to 180 m.||||Conformably overlies Hutton Sandstone. Is overlain conformably by Pilliga Sandstone and Springbok Sandstone.|Grey, lithic, labile sandstone, calcareous in places; granular to pebble conglomerate; grey siltstone; medium to dark grey and chocolate-brown mudstone; dull brown to shiny black coal.|
19303|Walloon Coal Measures|68004|5|Briefly described|p139, p163-164.|Jurassic|Jurassic|Kaolin prospectivity is discussed. Contains minor coal intervals with limited prospects. However, this unit is largely unexplored and there are several coal mines within this unit in Queensland. Forms a seal for Hutton Sandstone.||||||
19303|Walloon Coal Measures|68006|5|Briefly described|pp91-92.|Jurassic|Jurassic|A 3 m coal interval was intersected in water bores NE of Warialda, suggesting limited potential. However, the area is largely unexplored, and there are several coal mines within this unit in Queensland.||||Is overlain by Pilliga Sandstone.||
19303|Walloon Coal Measures|68008|5|Briefly described|p241-243, p246|Middle Jurassic|Middle Jurassic|Moreton Basin. Coal seams typically are lenticular with marked thickness variations and seam splitting.||||Correlated with Mulgildie Coal Measures.||
19303|Walloon Coal Measures|68117|5|Briefly described|p345, p347|||Reid (1921); previously the Walloon Beds of Cameron (1907). A type area near Walloon township was specified by Whitehouse (1955). Upgraded to Walloon Subgroup by Jones and Patrick (1981).||||Overlay Eurombah Formation. Overlain by Springbok Sandstone.||
19303|Walloon Coal Measures|68135|5|Briefly described|p49-50, p52-55, p57-58, p61-64|Callovian|Bajocian|Clarence-Moreton and Surat Basins. Important source of thermal coal and (in the Surat Basin) coal seam gas. Includes plant macrofossils, vertebrate fossils and tracks (dinosaur footprints dated c.168-161 Ma). Plant fossils listed; fish fossils illustrated.||||Overlies Hutton Sandstone, Koukandowie Formation. Is unconformably overlain by Kangaroo Creek and Springbok Sandstones.|Interbedded coal, mudstone and sandstone; volcanic ash beds.|15-SEP-17
19303|Walloon Coal Measures|68139|5|Briefly described|p23|Middle Jurassic|Middle Jurassic|Continuous across the Surat and Clarence-Moreton Basin (QLD and northern NSW). A prolific, low-rank coal seam gas resource. Fluvio-lacustrine environment.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain by Springbok Sandstone.|Very fine- to medium-grained litharenite, shale, siltstone, mudstone, minor limestone, ironstone (siderite) and coal. Includes volcanic debris and widespread ash-fall tuffs.|
19303|Walloon Coal Measures|68327|5|Briefly described|Map legend.|Jurassic|Jurassic||||||Shale, siltstone, sandstone, coal seams.|
19303|Walloon Coal Measures|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Jurassic|Clarence-Moreton and Surat Basins. This unit, as well as the Injune Creek Group and the Mulgildie Coal Measures, are all mapped under the symbol, Ji.||||||
19303|Walloon Coal Measures|68576|5|Briefly described|Q_4: p3|Middle Jurassic|Middle Jurassic|Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone. Is overlain unconformably by Springbok Sandstone.||
19303|Walloon Coal Measures|68679|5|Briefly described|p312-313, p455, p472|Jurassic|Jurassic|Northern New England Orogen.||||||
19303|Walloon Coal Measures|68901|6|Mentioned|p8 Fig. iii|Early Cretaceous|Early Jurassic|||||||27-SEP-18
19303|Walloon Coal Measures|69297|4|Described|p370, p386, p486|Upper Jurassic|Middle Jurassic|Clarence-Moreton Basin. Oil prone source rocks are present. Maximum thickness of approximately 600m. Deposited as sandy channel fill or overbank/floodplain deposits as part of a meandering fluvial system. See also p487 fig 5.38, p488, p489.|||Includes the Maclean Sandstone Member.|Overlies the Bundamba Group. Overlain by the Kangaroo Creek Sandstone.|Interbedded sandstone, siltstone, claystone, coal and ironstone nodules.|
19303|Walloon Coal Measures|69582|5|Briefly described|p35, p38|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies the Hutton Sandstone. Unconformably overlain by the Springbok Sandstone.|Sandstones, siltstones, mudstones and coal seams.|
19303|Walloon Coal Measures|69594|4|Described|p517, p519, p524, p536-537, p539|Middle Jurassic|Middle Jurassic|See also p544-547, p549, p573. Surat, Clarence-Moreton and Nambour Basins. First defined in the Clarence-Moreton Basin (Cameron, 1907; others listed). Swarbrick (1973) divided the Walloon Coal Measures (WCM) into six units in the NE Surat Basin; Jones and Patrick (1981) raise WCM to Subgroup status to include the Taroom Coal Measures, Tangalooma Sandstone and Juandah Coal Measures. Green et al. (1997), unable to distinguish the Eurombah Formation, included it within the WCM. Scott et al. (2004) succeeded in the NE Surat Basin, and so they are here regarded as members of the WCM [without the Rank term Member attached]. The WCM is not regarded here as warranting Subgroup status. Tectonic significance of volcanic ash beds discussed. Highly sinuous fluvial deposits in the lower part; coal swamps in the upper. Bathonian-Callovian palynomorphs. An important thermal coal, CSG and LNG resource (described). Minor source of bentonite. RELATED UNITS (continued): Is laterally equivalent to the Birkhead Formation and Tiaro Coal Measures.||Injune Creek Group.||Overlies Hutton Sandstone (conformably/transitionally) and Koukandowie Formation. Is overlain unconformably by Springbok Sandstone and Kangaroo Creek Sandstone (locally disconformably/conformably).|Labile sandstones, siltstone, mudstone and coal in the upper half to two-thirds of the formation, with lesser calcareous sandstone, impure limestone and ironstone. Coal decreases markedly to the WE. Includes silicic tuffs.|
19303|Walloon Coal Measures|69599|6|Mentioned|p595|||||||Is overlain unconformably by the Beaudesert beds.||
19303|Walloon Coal Measures|69633|5|Briefly described|p3|Middle Jurassic|Middle Jurassic|Surat Basin.||||Overlies Hutton Sandstone.||
19303|Walloon Coal Measures|69681|6|Mentioned|p74 Fig.3|Middle Jurassic|Middle Jurassic|||Unit in Injune Creek Group.||||
19303|Walloon Coal Measures|69682|5|Briefly described|p95 Fig.3|Middle Jurassic|Middle Jurassic|Name replaced by Walloon Subgroup.||||||
19303|Walloon Coal Measures|69790|5|Briefly described|p1063 Fig.2, p1065-1066|||Cameron (1970). Jones and Patrick (1981) raised this unit to Walloon Subgroup, in the NE Surat Basin. Northern Clarence-Moreton Basin area.||||Overlies Eurombah Formation. Is overlain by Springbok Sandstone.||
19303|Walloon Coal Measures|69793|6|Mentioned|p1113 Fig.3|Jurassic|Jurassic|Emu Creek Block, Tamworth Belt, southern New England Orogen.||||||
19303|Walloon Coal Measures|69946|6|Mentioned|p13-14, p75|||W Surat Basin.||||||
19303|Walloon Coal Measures|69947|5|Briefly described|p23 Fig.7.12|||Surat Basin. Volcanic-arc-derived sediments.||||Overlies Hutton Sandstone.|Lithic arenites, coal.|
19303|Walloon Coal Measures|70036|5|Briefly described|Map legend|Middle Jurassic|Middle Jurassic|Surat Basin. Included in a mapped unit of fluvial and lacustrine sequences: lithic to quartzose sandstone, siltstone, mudstone, claystone and coal.||||||
19303|Walloon Coal Measures|70374|4|Described|p807-814|Oxfordian|Aalenian|Surat and Clarence-Moreton Basins. Type section in Clarence Moreton Basin is difficult to relate to the occurences in the Surat Basin. Originally used by Bryan (1944). 350-450 m thick. Age determined by biostratigraphy in past, as in the 174.1 - 163.5 Ma range (Aalenian to Callovian). Maximum age in Clarence Moreton Basin (Aalenian) may be older than in Surat Basin, where age is now constrained by dating of tuffs in the Taroom Coal Measures and the Juandah Coal Measures.|~162 - 158 Ma CA-TIMS.|Lower part of Injune Creek Group.|Includes Taroom Coal Measures, Tangalooma Sandstone, Maclean Sandstone Member, Juandah Coal Measures.|Conformably overlies Hutton Sandstone or Eurombah Formation. Underlies Springbok Sandstone unconformably. Shown as lateral equivalent of Birkhad Formation.|Include tuff layers.|
19303|Walloon Coal Measures|70628|6|Mentioned|p952|Jurassic|Jurassic|Informally renamed Walloon Subgroup.||||||
19303|Walloon Coal Measures|70725|5|Briefly described|p12-14, 18-19, 24, 26|Late Jurassic|Late Jurassic|Surat Basin. Up to c.450m thick. Oxfordian. Diverse contributing plant taxa listed and discussed.|162-158 Ma.|Walloon Subgroup.|Taroom, Lower Juandah, Upper Juandah, Coal Measures; Tangalooma, Wambo Sandstones||Sub-bituminous rank coals.|
19303|Walloon Coal Measures|70820|6|Mentioned|p36-37|||Contains considerable coal seam gas reserves and is a target for potential extraction in the Richmond River catchment.||||||
19303|Walloon Coal Measures|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Surat Basin.||Injune Creek Group.||Overlies Hutton Sandstone or Koukandowie Formation (Marburg Subgroup, Bundamba Group). Is overlain by Springbok, Pilliga or Mooga Sandstones, or Kumbarilla beds.||
19303|Walloon Coal Measures|71342|5|Briefly described|Ch5 p14, Ch5 p74|||Surat Basin. See also the Birkhead Formation. Power and Devine (1968) recommended that this unit supersede the Birkhead Formation.||||||
19303|Walloon Coal Measures|71601|6|Mentioned|p120 , p121|Bathonian|Bajocian|SE Qld. Includes a possible stegosaur track.||||||
19303|Walloon Coal Measures|71805|6|Mentioned|p77, p86|||Surat Basin.||||||15-MAY-19
19303|Walloon Coal Measures|71863|6|Mentioned|p2|Mesozoic|Mesozoic|||||||
19303|Walloon Coal Measures|72297|5|Briefly described|p698-700, p739, p745-746, p750-751|Middle Jurassic|Middle Jurassic|Clarence-Moreton, Surat and Mulgildie Basins. Perhydrous cannel coals; characteristics and use in thermal power stations described. Produces commercial CSG and is a target of further exploration. Potential hydrocarbon source rock, but unlikely to have reached thermal maturity.||||Overlies Eurombah Formation ?conformably. Is overlain unconformably by Springbok Sandstone. Correlative of Mulgildie Coal Measures.|Coal seams in thick, banded intervals, separated by lenticular beds of carbonaceous shale, mudstone, siltstone and sandstone of varying thickness.|
19303|Walloon Coal Measures|72298|5|Briefly described|p801|Jurassic|Jurassic|Surat Basin (QLD,NSW).||Injune Creek Group.||Overlies Eurombah FZ and Hutton Sandstone. Is overlain by Springbok and Pilliga Sandstones and Kumbarilla beds.||
19303|Walloon Coal Measures|72478|6|Mentioned|p62 (digital)|||Surat Basin. Mid-Jurassic. Contains significant gas reserves. Lithology compared to Boorthanna Formation.|||||Said to contain sub-bituminous coal deposits.|
19303|Walloon Coal Measures|72921|4|Described|p13, p15 Fig.2, p16-17, p24, p47.|Middle Jurassic|Middle Jurassic|Includes a marine influence. Mostly swampy, fresh water. Interpreted as correlative across the Clarence-Moreton, Surat and Eromanga Basins. Shown as located within the Clarence-Moreton Basin, and the Surat Basin in Queensland. See also Walloon Subgroup p8, 13. See also p49-51, p54.||||Overlies Durabilla and Eurombah Formations, Koukandowie Formation and is shown as unconformably underlying Springbok Sandstone, Kangaroo Creek Sandstone.|Includes crossbedded sandstone, shales and siltstone. Also includes polymictic conglomerate and crossbedded sandstones.|
19303|Walloon Coal Measures|73113|5|Briefly described|p. 2, 10, 13-14, 16, 19, 22-24, 27-29...|||Surat Basin. 300 m thick in some places. Percentage of coal varies from <1 to ~20% (mean 8.5%). Groundwater model divides unit into lower, 3 middle, upper, and non-productive zones (layers). Interbedded aquitard. Incised by up to 120 m. Top contact zone forms the ""Condamine Alluvium transition zone"" ca 1-15 m thick. Non-productive part is relatively thin; <10 m. More locations: p. 31, 36-38, 41, 45, 49, 51-52, 57-58, 60-62, 66-71, 78, 80-82, 86, 89, 91, 94, 96-108, 116-117, 119, 123-124, 126-130, 132, 134, 136-138, 143, 145-150, 152, 154, 158-164, 166-169, 172-175, 177, 179-180, 191-194, 196, 199-200, 208.||||Underlain by Durabilla Formation. Overlain by Springbok Sandstone and unconformably by Condamine Alluvium.|Discontinuous permeable coal seams interbedded with low-permeability material consisting of siltstones, mudstones and fine-grained sandstones. Includes a top weathered/clay interval.|
19303|Walloon Coal Measures|73147|5|Briefly described|p127, 135-136, 140, 144|Late Jurassic|Middle Jurassic|Surat Basin. Shallow fluvial-estuarine setting with marine incursions.||||Coeval with Loth Formation.|Structureless to horizontally laminated fine-grained sandstones, siltstones and mudstones. Silicic tuff is widespread.|
19303|Walloon Coal Measures|73200|4|Described|p531-p533, p535, p539-542|Jurassic|Jurassic|Abbreviated to WCM in text. ca 159 Ma age from Wainman et al., (2015). Deposited in a fluvio-lacustrine environment with peat-forming conditions and contemporaneous volcanism during the Middle Jurassic, lithification was prior to the mid-Cretaceous (Hamilton et al., 2014). Mineral composition in upper section is predominantly kaolin, quartz and feldspar, with gypsum prevalent in carbonaceous layers.|ca 159 Ma||Macalister Seam|Angularly underlies the Condamine Alluvium, underlies the Kumbarilla Beds, Main Range Volcanics. Overlies the Marburg Sandstone.|Discontinuous thin coal seams in mudstone and siltstone with minor calcareous sandstone, limestone and ironstone matrix. Carbonaceous mudstone, thin and mostly dull coal, thin tuffs, lapilli and minor siltstone with minor weathering in upper section.|
19303|Walloon Coal Measures|73306|5|Briefly described|p566|Jurassic|Jurassic|Clarence-Moreton Basin.||||Overlies Marburg Subgroup (Bundamba Group). Is overlain by Kangaroo Creek Sandstone.||
19303|Walloon Coal Measures|73393|6|Mentioned|p19-22|Tithonian|Callovian|Surat Basin. Previously called the Walloon Series. The only pre-Cretaceous sauropod known from Australia, Rhoetosaurus brownei, was recovered from this unit (collected from the banks of a gully feeding the Eurombah Creek on Taloona Station, SE QLD). Detrital zircons collected alongside the fossil specimen yielded a maximum depositional age of 162.6 +/- 1.1 Ma; consistent with the unit's age range of ca 165-151 Ma from Wainman et al. (2015, 2018a, 2018b). This indicates the fossil was probably from the lower portion of the unit.|ca 165-151 Ma|Injune Creek Group||Underlain by Eurombah Formation. Overlain by Springbok Sandstone. Equivalent to Birkhead Formation.||
19303|Walloon Coal Measures|73570|6|Mentioned|p912 Fig.2, p920|||||||||
19323|Wallumbilla Formation|9528|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Dark purplish grey to white, fine to medium lithic sandstone, feldspathic sandstone.||||||
19323|Wallumbilla Formation|12597|4|Described|p492 Tb.1, p497, p498, p499-500|Albian|Aptian|Eromanga Basin. Division into the two Members is not possible in the NW, where the sequence is more uniform.|||Includes Doncaster and Coreena Members.||Marine, largely argillaceous sequence with common mollusc, gastropod, scaphopod and belemnites fossils.|
19323|Wallumbilla Formation|13497|5|Briefly described|p115 fig 6.33, p138 fig 8.17|Early Cretaceous|Early Cretaceous|Eromanga Basin. See also p144 fig 9.2, p145, p146, p148-p151.||Marree Subgroup||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.|||Includes Doncaster and Coreena Members|||
19323|Wallumbilla Formation|22464|5|Briefly described|p9||Early Cretaceous|Eromanga Basin. Overlain by Toolebuc Formation.||||||18-DEC-06
19323|Wallumbilla Formation|22744|5|Briefly described|Fig1, P12, Table4||Cretaceous|||||||
19323|Wallumbilla Formation|22747|6|Mentioned|p15||Mesozoic|||||||
19323|Wallumbilla Formation|22757|6|Mentioned|Table6,p11||Early Cretaceous|In the Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|22857|4|Described|p296-7 Tb.22.1, p544 App.1 Tb.A1.12|Albian|Aptian|Of the Rolling Downs Group. Sequence of mudstone and siltstone. Contains the Coreena Member. Max. thickness: 600m. Geological Province: Surat and Eromanga Basins. See also p312-3 Fig. 22.6, p314-5, p544 App.1 Tb.A1.12.||||||
19323|Wallumbilla Formation|22865|4|Described|p314,Table22.1p296-7|Albian|Aptian|||||||
19323|Wallumbilla Formation|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Toolebuc Formation, underlying unit is Cadna-owie Formation||||||
19323|Wallumbilla Formation|22912|5|Briefly described|33|||Geological province: Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23031|5|Briefly described|31|||||||||
19323|Wallumbilla Formation|23050|5|Briefly described|p 82 Fig.17|Early Cretaceous|Early Cretaceous|Of Surat Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23056|6|Mentioned|9|||Geol Province Eromanga Basin||||||
19323|Wallumbilla Formation|23065|5|Briefly described|18|||Geological  province: Carpentaria Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23071|6|Mentioned|p761|||||||||
19323|Wallumbilla Formation|23154|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Geological Province - Eromanga Basin.  Of the Marree Subgroup (Neales River Group).||||||18-DEC-06
19323|Wallumbilla Formation|23155|4|Described|p32|Early Cretaceous|Early Cretaceous|The unit is laterally equivalent to the Bulldog Shale and it is limited to the northern part of STRZELECKI.  Age Aptian-Albian.||||||
19323|Wallumbilla Formation|23183|6|Mentioned|p222||Aptian|||||||
19323|Wallumbilla Formation|23220|5|Briefly described|p16||Mesozoic|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23224|5|Briefly described|p3|||Hosts the Doncaster Member which hosts the Opal Deposits. Of Rolling Downs Group. In the Great Australian Basin.||||||01-FEB-07
19323|Wallumbilla Formation|23291|4|Described|p80 Tb. 3.6|Early Cretaceous|Early Cretaceous|Age: early Cretaceous. Conformably overlies Coffin Hill Member. Geological Province: Georgetown Region.||||||08-JUL-15
19323|Wallumbilla Formation|23375|4|Described|Fig2 p265|Albian|Barremian|Laterally equivalent to Bulldog Shale. of Eromanga Basin.||||||
19323|Wallumbilla Formation|23393|5|Briefly described|p24|Early Cretaceous|Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|23425|4|Described|Table 9.7 p394|Aptian|Aptian|+ Plate 9.2 + p378. Of Rolling Downs Group. Conformably overlain by Toolebuc Formation; underlain by Gilbert River Formation. Geological Province Carpentaria Basin. Max. thickness 500 m.||||||18-DEC-06
19323|Wallumbilla Formation|23430|5|Briefly described|p455|||Eromanga Basin Province.||||||
19323|Wallumbilla Formation|23496|5|Briefly described|Table 4, p59|Albian|Aptian|of Rolling Downs Group. Previously Blackdown Formation (Laing and Power 1959), then Wilgunya Subgroup (Grimes & Whittaker 1977) then of Smart and Others 1972/1980.||||||01-FEB-07
19323|Wallumbilla Formation|23499|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous|In the Eromanga Basin.||||||18-DEC-06
19323|Wallumbilla Formation|23510|5|Briefly described|Map Legend||Early Cretaceous|Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|23518|5|Briefly described|p13|Mesozoic|Mesozoic|Of Rolling Downs Group.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|23713|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|23818|6|Mentioned|p141 Fig.65|||Geological Province: Great Artesian Basin. Of the Wilunga Sub-Group.||||||
19323|Wallumbilla Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Contains the Coreena and Doncaster Members.  Geological Province: Great Australian Superbasin.||||||
19323|Wallumbilla Formation|23911|5|Briefly described|p90 Fig. 4|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.  Of the Rolling Downs Group.||||||
19323|Wallumbilla Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Includes the Coreena and Doncaster Members. Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|23986|5|Briefly described|p71|||||||||
19323|Wallumbilla Formation|24048|5|Briefly described|p76|||||||||
19323|Wallumbilla Formation|24068|4|Described|p270 Table 2|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin.  Maximum thickness: 310m.||||||
19323|Wallumbilla Formation|24073|5|Briefly described|p378 Table 2|Early Cretaceous|Early Cretaceous|Supersedes Balckdown Formation.  Of Rolling Downs Group. Maximum thickness: 200m.  Geological Province: Carpentaria Basin.||||||
19323|Wallumbilla Formation|24085|5|Briefly described|Not recorded|Albian|Aptian|Contains Doncaster Member. Geological Province: Eromanga Basin||||||16-MAR-05
19323|Wallumbilla Formation|24092|5|Briefly described|p5|Cretaceous|Jurassic|Geological Province: Great Artesian Basin.||||||
19323|Wallumbilla Formation|24175|5|Briefly described|p17 Fig. 3|Albian|Aptian|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24204|5|Briefly described|p263 Fig.4, p267, p282 Fig.21|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Marree Subgroup?  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|24251|5|Briefly described|p234 Fig.1, p245|Albian|Albian|Overlying Unit: Toolebuc Formation. Geological Province: Eromanga Basin||||||
19323|Wallumbilla Formation|29387|6|Mentioned|Table 5|||||||||
19323|Wallumbilla Formation|29393|6|Mentioned|Table 4|||Cretaceous.||||||
19323|Wallumbilla Formation|29591|6|Mentioned|p71|||||||||
19323|Wallumbilla Formation|29651|6|Mentioned|p25|||||||||
19323|Wallumbilla Formation|29721|6|Mentioned|Table 246|||||||||
19323|Wallumbilla Formation|30019|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|30020|4|Described|p29|||||||||
19323|Wallumbilla Formation|30021|6|Mentioned|p89|||||||||
19323|Wallumbilla Formation|30022|6|Mentioned|p32|||||||||
19323|Wallumbilla Formation|30024|6|Mentioned|p331|||||||||
19323|Wallumbilla Formation|30042|4|Described|p4|||? glauconite.||||||
19323|Wallumbilla Formation|30095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30102|6|Mentioned|Table 4|Cretaceous|Jurassic|See also P17.||||||
19323|Wallumbilla Formation|30103|5|Briefly described|p9|||Table 3 on p9.||||||18-DEC-06
19323|Wallumbilla Formation|30104|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30443|6|Mentioned|p2|||See also P4. Aptian age||||||
19323|Wallumbilla Formation|30446|6|Mentioned|p39|||||||||
19323|Wallumbilla Formation|30458|6|Mentioned|p7|||Cretaceous age||||||
19323|Wallumbilla Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19323|Wallumbilla Formation|30584|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|30585|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30587|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30691|4|Described|Table 4|||Lower-Upper Cretaceous age. Of Rolling Downs Group||||||
19323|Wallumbilla Formation|30692|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30694|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Lower Cretaceous age||||||
19323|Wallumbilla Formation|30695|4|Described|Table 4|||Lower Cretaceous age.||||||17-SEP-08
19323|Wallumbilla Formation|30696|4|Described|Table 4|||Aptian-Albian age||||||
19323|Wallumbilla Formation|30698|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30700|6|Mentioned|p22|||Lower Cretaceous age. Map||||||
19323|Wallumbilla Formation|30701|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30702|6|Mentioned|Table 1|||Stratigraphic table||||||
19323|Wallumbilla Formation|30804|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|30853|5|Briefly described|Table 3|||Aptian to Lower Albian age||||||
19323|Wallumbilla Formation|30854|4|Described|Table 4|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|30855|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|Unit in Rolling Downs Group||||||
19323|Wallumbilla Formation|30856|4|Described|Table 3|||Lower Cretaceous age.||||||
19323|Wallumbilla Formation|30857|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|30915|6|Mentioned|Table|||Shown on stratigraphic table||||||
19323|Wallumbilla Formation|31097|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31098|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31116|4|Described|p43|||See also Table 2. Cretaceous||||||
19323|Wallumbilla Formation|31120|6|Mentioned|Table|||||||||
19323|Wallumbilla Formation|31121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|31144|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31145|5|Briefly described|Table 1|||L. Cretaceous||||||
19323|Wallumbilla Formation|31164|5|Briefly described|p8|||Aptian - Lower Albian, See also P10.||||||
19323|Wallumbilla Formation|31165|6|Mentioned|Table 11|||||||||
19323|Wallumbilla Formation|31168|6|Mentioned|p10|||||||||
19323|Wallumbilla Formation|31208|6|Mentioned|Fig 36|||See also Table 1||||||
19323|Wallumbilla Formation|31209|4|Described|p159|||||||||
19323|Wallumbilla Formation|31376|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|31422|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, minor limestone, glauconitic sandstone.||||||02-DEC-04
19323|Wallumbilla Formation|31425|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31430|5|Briefly described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
19323|Wallumbilla Formation|31432|4|Described|Table 1|||L.Cretaceous||||||
19323|Wallumbilla Formation|31433|5|Briefly described|p6|||L.Cretaceous||||||
19323|Wallumbilla Formation|31434|3|Fully described|Table 1|||See also p8. L.Cretaceous.||||||17-SEP-08
19323|Wallumbilla Formation|31436|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31437|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31438|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31440|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31441|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31553|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|31832|6|Mentioned|Table 6|||||||||
19323|Wallumbilla Formation|32136|6|Mentioned|p3|||Continuously cored composite section||||||
19323|Wallumbilla Formation|32193|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32274|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32275|4|Described|p8|||||||||
19323|Wallumbilla Formation|32276|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32313|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|32314|6|Mentioned|Fig. 4|||||||||
19323|Wallumbilla Formation|32392|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32393|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|32395|6|Mentioned|p6|||Stratigraphic table||||||
19323|Wallumbilla Formation|32396|6|Mentioned|p8|||Stratigraphic table||||||
19323|Wallumbilla Formation|32490|6|Mentioned|p9|||Crops out W of Buchanan sheet||||||
19323|Wallumbilla Formation|32553|4|Described|p38|||||||||
19323|Wallumbilla Formation|32705|6|Mentioned|p188|||||||||
19323|Wallumbilla Formation|32796|6|Mentioned|p302|||||||||
19323|Wallumbilla Formation|32797|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33016|6|Mentioned|p1|||On table||||||
19323|Wallumbilla Formation|33017|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|33067|4|Described|Table 1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group.  Mudstone, siltstone,minor sandstone.||||||07-JUL-04
19323|Wallumbilla Formation|33069|4|Described|p7|||L.Cret.||||||
19323|Wallumbilla Formation|33070|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33071|4|Described|p2|||L.Cret.||||||
19323|Wallumbilla Formation|33072|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33075|6|Mentioned|p445|||||||||
19323|Wallumbilla Formation|33078|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33079|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33080|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33082|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33083|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
19323|Wallumbilla Formation|33087|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33088|4|Described|Table 3|||||||||
19323|Wallumbilla Formation|33089|4|Described|Table 2|||L.Cret.||||||
19323|Wallumbilla Formation|33090|4|Described|Table 4|||L.Cret.||||||
19323|Wallumbilla Formation|33091|5|Briefly described|p9|||Stratigraphy||||||
19323|Wallumbilla Formation|33092|5|Briefly described|p6|||Strat. table||||||
19323|Wallumbilla Formation|33094|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33095|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33096|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33150|4|Described|p9|||L.Cret.||||||
19323|Wallumbilla Formation|33151|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33165|6|Mentioned|Chart|||Correlatin chart only||||||
19323|Wallumbilla Formation|33175|6|Mentioned|p280|||||||||
19323|Wallumbilla Formation|33176|5|Briefly described|p172|||||||||
19323|Wallumbilla Formation|33177|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|33178|6|Mentioned|p11|||||||||
19323|Wallumbilla Formation|33179|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33180|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33182|6|Mentioned|p190|||||||||
19323|Wallumbilla Formation|33183|6|Mentioned|p233|||||||||
19323|Wallumbilla Formation|33368|6|Mentioned|p24|||Geol.Map.||||||
19323|Wallumbilla Formation|33372|4|Described|p17|||See also p20. From QDM Aramac 1.||||||18-DEC-06
19323|Wallumbilla Formation|33414|6|Mentioned|p212-214,Tb.||Aptian|Part of Wilgunya Sub-Group..||||||
19323|Wallumbilla Formation|33448|4|Described|Table 1|||L.Cret.||||||11-JAN-10
19323|Wallumbilla Formation|33449|4|Described|Table 1|||L.Cret.||||||
19323|Wallumbilla Formation|33451|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33452|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33561|6|Mentioned|p102|||||||||
19323|Wallumbilla Formation|33638|5|Briefly described|Table 1|||||||||
19323|Wallumbilla Formation|33639|5|Briefly described|p11|||L.Cret.||||||
19323|Wallumbilla Formation|33640|4|Described|Table 2|||||||||
19323|Wallumbilla Formation|33642|1|Redefined|p148|Early Cretaceous|Early Cretaceous|Includes Doncaster, Jones Valley, Ranmoor and Coreena Members. Contains Roma and older part of Tambo fauna of Aptian and Albian (Lower Cret)||||||
19323|Wallumbilla Formation|33643|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33644|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33645|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33646|6|Mentioned|p8|||Strat. table.||||||
19323|Wallumbilla Formation|33647|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|33648|6|Mentioned|p20|||||||||
19323|Wallumbilla Formation|33672|5|Briefly described|p44|||Lithology.||||||
19323|Wallumbilla Formation|33673|4|Described|p292|||||||||
19323|Wallumbilla Formation|33772|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33773|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|33825|6|Mentioned|p10|||Correlation table||||||
19323|Wallumbilla Formation|33832|5|Briefly described|p11|||Strat. and correlation.||||||18-DEC-06
19323|Wallumbilla Formation|33900|6|Mentioned|p21|||||||||
19323|Wallumbilla Formation|33939|6|Mentioned|p412|||||||||
19323|Wallumbilla Formation|33964|4|Described|p6|||Refers Vine et al. (1967).||||||
19323|Wallumbilla Formation|34065|4|Described|p6|||L.Cret.||||||
19323|Wallumbilla Formation|34091|5|Briefly described|Table 1|||See also P4. L.Cret. Part of Rolling Downs Group.||||||
19323|Wallumbilla Formation|34174|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34212|6|Mentioned|p2|||Cretaceous||||||
19323|Wallumbilla Formation|34217|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34218|4|Described|Table 1|||See also Table 2. Lower Cretaceous||||||
19323|Wallumbilla Formation|34356|6|Mentioned|p13|||Lower Cretaceous.||||||
19323|Wallumbilla Formation|34485|5|Briefly described|Table 1,p10|||Lower Cretaceous||||||
19323|Wallumbilla Formation|34486|5|Briefly described|Table 1|||Lower Cretaceous. See also Table 2||||||
19323|Wallumbilla Formation|34487|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19323|Wallumbilla Formation|34613|4|Described|Table 4|||||||||
19323|Wallumbilla Formation|34811|4|Described|Table 1|||||||||
19323|Wallumbilla Formation|35121|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35139|4|Described|Table.2|||||||||
19323|Wallumbilla Formation|35239|6|Mentioned|p258|||||||||
19323|Wallumbilla Formation|35253|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35457|6|Mentioned|Fig.5|||Stratigraphic correlation||||||
19323|Wallumbilla Formation|35560|4|Described|p290|||||||||
19323|Wallumbilla Formation|35640|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
19323|Wallumbilla Formation|35793|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|35811|5|Briefly described|Table 3|||||||||
19323|Wallumbilla Formation|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
19323|Wallumbilla Formation|35936|6|Mentioned|p615|||||||||
19323|Wallumbilla Formation|35937|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|36012|3|Fully described|Table 5|||See also p18.||||||18-DEC-06
19323|Wallumbilla Formation|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|36243|6|Mentioned|Table 6A|||||||||
19323|Wallumbilla Formation|36251|4|Described|p3|||||||||
19323|Wallumbilla Formation|36570|5|Briefly described|p50|||See also p60.||||||18-DEC-06
19323|Wallumbilla Formation|36571|6|Mentioned|p101|||See also Table 4.||||||
19323|Wallumbilla Formation|36574|6|Mentioned|p602|||||||||
19323|Wallumbilla Formation|36580|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|36581|6|Mentioned|p464|||||||||
19323|Wallumbilla Formation|36910|6|Mentioned|p61|||||||||
19323|Wallumbilla Formation|37117|5|Briefly described|p313|||||||||
19323|Wallumbilla Formation|37451|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|37597|6|Mentioned|p77|||||||||
19323|Wallumbilla Formation|37608|3|Fully described|Table 1 p316-319|||||||||
19323|Wallumbilla Formation|37995|4|Described|p66|||||||||
19323|Wallumbilla Formation|38199|5|Briefly described|p423|||Palynology||||||
19323|Wallumbilla Formation|38218|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|38226|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|38372|6|Mentioned|p651|||||||||
19323|Wallumbilla Formation|38373|6|Mentioned|p619|||||||||
19323|Wallumbilla Formation|38608|6|Mentioned|Map legend|Mesozoic|Mesozoic|||||||
19323|Wallumbilla Formation|38779|6|Mentioned|p7|||||||||
19323|Wallumbilla Formation|38780|6|Mentioned|p17|||||||||
19323|Wallumbilla Formation|38814|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39029|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Overlies Gilbert River Formation.||||||25-AUG-04
19323|Wallumbilla Formation|39070|4|Described|p364|||||||||
19323|Wallumbilla Formation|39211|5|Briefly described|Fig.3|||See also Figs 4,7,9,11-15 etc. Correlation||||||
19323|Wallumbilla Formation|39212|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|39216|6|Mentioned|p55|||||||||
19323|Wallumbilla Formation|39445|5|Briefly described|Table 11|||||||||
19323|Wallumbilla Formation|39478|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39627|6|Mentioned|p269|||||||||
19323|Wallumbilla Formation|39708|6|Mentioned|p478|||||||||
19323|Wallumbilla Formation|39797|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39799|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39846|6|Mentioned|p44|||||||||
19323|Wallumbilla Formation|39847|5|Briefly described|p38|||||||||
19323|Wallumbilla Formation|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|39917|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|39942|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|39943|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|39988|6|Mentioned|p288|||||||||
19323|Wallumbilla Formation|39989|4|Described|p423|||||||||
19323|Wallumbilla Formation|40058|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40121|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|40150|6|Mentioned|p81|||||||||
19323|Wallumbilla Formation|40199|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40218|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|40245|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|40249|6|Mentioned|p38|||Mention P41||||||
19323|Wallumbilla Formation|40250|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|40452|6|Mentioned|p2|||||||||
19323|Wallumbilla Formation|40541|3|Fully described|p111|||||||||
19323|Wallumbilla Formation|40544|6|Mentioned|p159|||||||||
19323|Wallumbilla Formation|40623|5|Briefly described|p108|||||||||
19323|Wallumbilla Formation|40648|6|Mentioned|p12|||||||||
19323|Wallumbilla Formation|40659|6|Mentioned|p250|||||||||
19323|Wallumbilla Formation|40666|4|Described|p358|||||||||
19323|Wallumbilla Formation|40670|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|40675|6|Mentioned|Table 8A|||||||||
19323|Wallumbilla Formation|40687|3|Fully described|p418|||||||||
19323|Wallumbilla Formation|40771|6|Mentioned|p429|||||||||
19323|Wallumbilla Formation|40801|6|Mentioned|p29|||See also P39||||||
19323|Wallumbilla Formation|40832|3|Fully described|p457|||||||||
19323|Wallumbilla Formation|40833|6|Mentioned|p468|||||||||
19323|Wallumbilla Formation|40926|6|Mentioned|p18|||||||||
19323|Wallumbilla Formation|40962|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41012|5|Briefly described|p137|||||||||
19323|Wallumbilla Formation|41060|6|Mentioned|Fig.3|||Generalized stratigraphy||||||
19323|Wallumbilla Formation|41062|6|Mentioned|Fig.5|||||||||
19323|Wallumbilla Formation|41063|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|41064|6|Mentioned|p60|||||||||
19323|Wallumbilla Formation|41084|5|Briefly described|Fig.2|||||||||
19323|Wallumbilla Formation|41086|3|Fully described|p98, Fig.3|||Mentioned p101.||||||18-DEC-06
19323|Wallumbilla Formation|41087|6|Mentioned|p123|||||||||
19323|Wallumbilla Formation|41088|6|Mentioned|p141|||||||||
19323|Wallumbilla Formation|41097|6|Mentioned|p165|||||||||
19323|Wallumbilla Formation|41099|6|Mentioned|Fig.9|||||||||
19323|Wallumbilla Formation|41117|6|Mentioned|Fig.2|||||||||
19323|Wallumbilla Formation|41165|5|Briefly described|p362|||||||||
19323|Wallumbilla Formation|41175|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41176|6|Mentioned|Table 2|||||||||
19323|Wallumbilla Formation|41177|6|Mentioned|p225|||||||||
19323|Wallumbilla Formation|41178|6|Mentioned|p242|||||||||
19323|Wallumbilla Formation|41182|5|Briefly described|p289|||||||||
19323|Wallumbilla Formation|41183|6|Mentioned|p310|||||||||
19323|Wallumbilla Formation|41184|6|Mentioned|p347|||||||||
19323|Wallumbilla Formation|41186|6|Mentioned|p197|||||||||
19323|Wallumbilla Formation|41187|6|Mentioned|p227|||||||||
19323|Wallumbilla Formation|41196|6|Mentioned|Fig.1|||||||||
19323|Wallumbilla Formation|41198|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|41214|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41216|6|Mentioned|Fig.18|||||||||
19323|Wallumbilla Formation|41246|6|Mentioned|Map legend|Cretaceous||||||||
19323|Wallumbilla Formation|41266|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41286|6|Mentioned|p118|||||||||
19323|Wallumbilla Formation|41306|6|Mentioned|p4|||||||||
19323|Wallumbilla Formation|41307|6|Mentioned|p5|||||||||
19323|Wallumbilla Formation|41361|6|Mentioned|Fig.3|||||||||
19323|Wallumbilla Formation|41427|6|Mentioned|p84|||||||||
19323|Wallumbilla Formation|41464|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41523|3|Fully described|p278|||||||||
19323|Wallumbilla Formation|41556|6|Mentioned|Map legend|Early Cretaceous||||||||
19323|Wallumbilla Formation|41568|5|Briefly described|p15|||||||||
19323|Wallumbilla Formation|41681|6|Mentioned|p11,p22|||||||||
19323|Wallumbilla Formation|41707|6|Mentioned|p164|||||||||
19323|Wallumbilla Formation|41992|4|Described|Fig.2 p183|||||||||26-APR-18
19323|Wallumbilla Formation|42007|5|Briefly described|p182|||||||||
19323|Wallumbilla Formation|42061|4|Described|p157|||See also Fig.11||||||
19323|Wallumbilla Formation|42067|5|Briefly described|p309|||See also Appendix 2||||||
19323|Wallumbilla Formation|42071|6|Mentioned|p117|||||||||
19323|Wallumbilla Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19323|Wallumbilla Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19323|Wallumbilla Formation|42369|5|Briefly described|Fig.10, P61|||||||||
19323|Wallumbilla Formation|42397|6|Mentioned|Fig.2 P3|||||||||
19323|Wallumbilla Formation|42429|5|Briefly described|Fig.3 P155|||||||||
19323|Wallumbilla Formation|42446|4|Described|p13|||||||||
19323|Wallumbilla Formation|42447|6|Mentioned|p16|||||||||
19323|Wallumbilla Formation|42474|5|Briefly described|p25|||||||||
19323|Wallumbilla Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19323|Wallumbilla Formation|42520|5|Briefly described|p6|||||||||
19323|Wallumbilla Formation|42634|6|Mentioned|Table 8 P34|||||||||
19323|Wallumbilla Formation|42637|4|Described|p10, 23|||||||||
19323|Wallumbilla Formation|42673|5|Briefly described|Fig.2, P184|||||||||
19323|Wallumbilla Formation|42746|6|Mentioned|Fig.6 P8|||||||||
19323|Wallumbilla Formation|42749|5|Briefly described|p31|||see also Fig.2 p27.||||||18-DEC-06
19323|Wallumbilla Formation|42804|5|Briefly described|p115|||||||||
19323|Wallumbilla Formation|42940|5|Briefly described|Plate 2|Mesozoic|Mesozoic|Siltstone, porcellanite, sandstone; marine fossils.  Geological province: Amadeus Basin.||||||23-JAN-08
19323|Wallumbilla Formation|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
19323|Wallumbilla Formation|43000|5|Briefly described|p114|||see also Fig.5,p112||||||
19323|Wallumbilla Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19323|Wallumbilla Formation|43004|5|Briefly described|Table 1,p179|||||||||
19323|Wallumbilla Formation|43083|5|Briefly described|p185|Cretaceous|Cretaceous|Argillaceouis deposits.||||||17-JUN-09
19323|Wallumbilla Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19323|Wallumbilla Formation|43114|5|Briefly described|p14|||||||||
19323|Wallumbilla Formation|43122|5|Briefly described|p25|||see also Fig. 2.||||||
19323|Wallumbilla Formation|43254|5|Briefly described|map legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43285|5|Briefly described|Map Legend|Early Cretaceous|Late Jurassic|||||||
19323|Wallumbilla Formation|43287|5|Briefly described|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|43404|14|Not recorded|Table p11||Cretaceous|||||||
19323|Wallumbilla Formation|43564|6|Mentioned|p453||Aptian|(Late Aptian)||||||
19323|Wallumbilla Formation|43591|6|Mentioned|p40|||||||||
19323|Wallumbilla Formation|43602|4|Described|191|||In the Eromanga Basin. Of the Rolling Downs Group.||||||18-DEC-06
19323|Wallumbilla Formation|43625|6|Mentioned|p48,74|||||||||
19323|Wallumbilla Formation|43630|6|Mentioned|p69, fig.4|||||||||
19323|Wallumbilla Formation|43989|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44016|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44017|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44018|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44019|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44020|14|Not recorded|Tb.1,2||Early Cretaceous|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|44031|14|Not recorded|p3,8,9,11,12||Cretaceous|||||||
19323|Wallumbilla Formation|44034|4|Described|Tb.2,p2,5,7-10,Fig.1|||||||||
19323|Wallumbilla Formation|44042|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44082|6|Mentioned|p3,4,6,8,10-30,Tb.34||Early Cretaceous|Mentioned with respect to Qld Cretaceous fossils which are either of stratigraphic significance or are illustrative of the occurrence of a particular group.||||||
19323|Wallumbilla Formation|44091|14|Not recorded|p60,63||Cretaceous|||||||
19323|Wallumbilla Formation|44099|14|Not recorded|Map Legend||Early Cretaceous|(Rolling Downs Group)||||||
19323|Wallumbilla Formation|44112|6|Mentioned|p82|||||||||
19323|Wallumbilla Formation|44133|5|Briefly described|p104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|44308|14|Not recorded|p11,|||||||||
19323|Wallumbilla Formation|44376|14|Not recorded|p3|||||||||
19323|Wallumbilla Formation|44410|14|Not recorded|Map Legend||Early Cretaceous|||||||
19323|Wallumbilla Formation|44637|14|Not recorded|p287-291||Cretaceous|||||||
19323|Wallumbilla Formation|44807|14|Not recorded|p9|||Correlated with Blackdown Formation.||||||
19323|Wallumbilla Formation|45022|6|Mentioned|p111|Albian|Aptian|||||||
19323|Wallumbilla Formation|45071|6|Mentioned|p79|||||||||
19323|Wallumbilla Formation|45110|6|Mentioned|p24|||See also Table 18.||||||
19323|Wallumbilla Formation|45132|6|Mentioned|Table 2|||See also Fig.1.||||||
19323|Wallumbilla Formation|45145|3|Fully described|Table 5|||||||||
19323|Wallumbilla Formation|45161|6|Mentioned|p67|||||||||
19323|Wallumbilla Formation|46791|4|Described|p44|||||||||
19323|Wallumbilla Formation|46881|6|Mentioned|p198|||||||||
19323|Wallumbilla Formation|46902|6|Mentioned|p36|||||||||
19323|Wallumbilla Formation|46937|6|Mentioned|Fig.10|||||||||
19323|Wallumbilla Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19323|Wallumbilla Formation|46984|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|47042|6|Mentioned|p171|||||||||
19323|Wallumbilla Formation|47083|5|Briefly described|p20||Mesozoic|Of Rolling Downs Group.||||||
19323|Wallumbilla Formation|48919|6|Mentioned|p71|||Cretaceous. See also P72||||||
19323|Wallumbilla Formation|48920|3|Fully described|p58|||Lower Cretaceous age||||||
19323|Wallumbilla Formation|48951|6|Mentioned|Table 1|||||||||
19323|Wallumbilla Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19323|Wallumbilla Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19323|Wallumbilla Formation|50100|5|Briefly described|p23|Cretaceous|Cretaceous|Of the Rolling Downs Group.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|50199|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||||||
19323|Wallumbilla Formation|50332|5|Briefly described|p22, p78|Mesozoic|Mesozoic|Geological Province: Carpentaria Basin. Main lithologies are mudstone, calcareous shale, limestone, sandstone and siltstone.||||||07-FEB-11
19323|Wallumbilla Formation|50627|5|Briefly described|Map legend|Cretaceous|Cretaceous|Clay-rich mudstone, silty mudstone, sandy siltstone, and sandstone.||||||
19323|Wallumbilla Formation|60081|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Mudstone and quartz-poor sandstone, minor glauconitic sandstone.||||||
19323|Wallumbilla Formation|60087|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, minor labile and galuconitic sandstone, limestone.||||||
19323|Wallumbilla Formation|60281|5|Briefly described|p27|Early Cretaceous|Early Cretaceous|Geological Province: Clarence-Moreton Basin, Cecil Plains Sub-basin.||||||20-JAN-05
19323|Wallumbilla Formation|60331|5|Briefly described|p34 Fig.3|Albian|Aptian|Overlies Gilbert River Formation. Overlain by Toolebuc Formation. Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60357|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Overlies: Coffin Hill Member (Gilbert River Formation). Mudstone and siltstone, minor sandstone. Geological Province: Carpentaria Basin.||||||20-AUG-04
19323|Wallumbilla Formation|60358|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Silty and sandy claystone, mudstone and siltstone, calcareous concretions; minor glauconitic sandstone. Geological Province: Laura Basin.||||||18-AUG-04
19323|Wallumbilla Formation|60359|5|Briefly described|Map Legend|Mesozoic|Mesozoic|Mudstone, siltstone.||||||
19323|Wallumbilla Formation|60524|5|Briefly described|p486 Fig. 1, p488|Albian|Aptian|Marine deposits; contains Viviparidae fossils.  Geological Province: Eromanga Basin.||||||
19323|Wallumbilla Formation|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Overlies Cadna-owie Formation. Overlain by Toolebuc Formation. Lateral to Bulldog Shale. Geological Province: Eromanga Basin.||||||31-JAN-08
19323|Wallumbilla Formation|61014|6|Mentioned|p533 Fig.2, p539. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Wyandra Sandstone Member. Is overlain by Allaru Mudstone.||
19323|Wallumbilla Formation|61312|4|Described|p64, p67 Fig. E5, p73-74|Early Cretaceous|Early Cretaceous|Of Rolling Downs Gp. Marine sediment sequence of mudstone and siltstone, with limestone, minor lenticular sandstone, and intraformational conglomerate. Overlies Cadna-owie Fm.; overlain by Toolebuc Fm in Qld. Thickness: 300m. Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|61377|5|Briefly described|p148 Tb. SU1|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Mudstone, siltstone, minor sandstone, coal, conglomerate. Overlies Pilliga Sandstone. Geological Province: Surat Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19323|Wallumbilla Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Maree Subgroup. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|61614|6|Mentioned|p290 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
19323|Wallumbilla Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
19323|Wallumbilla Formation|62029|5|Briefly described|p15|Cretaceous|Cretaceous|Siltstone and shale - impermeable and acts as reservoir seal. See also Fig. 4.||||||14-APR-08
19323|Wallumbilla Formation|62376|5|Briefly described|p84|Early Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
19323|Wallumbilla Formation|62537|6|Mentioned|p191 Fig.2. |Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Coorikiana Formation.||
19323|Wallumbilla Formation|62730|5|Briefly described|p352 Fig. 1|Cretaceous|Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
19323|Wallumbilla Formation|62837|5|Briefly described|Stratigraphic columns|Early Cretaceous|Early Cretaceous|Of the Rolling Downs Group. Age: ~113-~98Ma. Geological Province: Northern Gulf of Carpentaria.||||||01-MAR-10
19323|Wallumbilla Formation|63218|6|Mentioned|p211 Fig.2. |Early Cretaceous|Early Cretaceous|Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|63979|1|Redefined|p48, Fig. 44|Albian|Barremian|Lower part of Wilgunya Subgp.Equates to Bulldog Shale, Coorikiana Sst.+lower part of Oodnadatta Fm in SA. Informally subdiv.into lower+upper Wallumbilla Fm.Contains Doncaster +Coreena Members.Conformable on Cadna-owie Fm. Thickness:350m.Detailed lith.||||||03-DEC-18
19323|Wallumbilla Formation|64048|5|Briefly described|p64 Tb. 2|Early Cretaceous|Early Cretaceous|Contains the Coreena Member. Geological Province: Eromanga Basin.||||||07-FEB-11
19323|Wallumbilla Formation|64197|6|Mentioned|p625 Fig.1c, p630 Figs.6,7|Cretaceous|Cretaceous|Eromanga and Surat Basins.||Unit in Marree Subgroup.||Eromanga Basin: underlies Toolebuc Formation; overlies Cadna-owie Formation. Surat Basin: underlies the Surat Siltstone, overlies the Bungil Formation.||11-DEC-15
19323|Wallumbilla Formation|64665|6|Mentioned|p62.|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|64820|5|Briefly described|pS6 Fig. 4|Barremian|Albian|Of the Rolling Downs Group. Geological province: Weipa Sub-basin, Carpentaria Basin.||||||
19323|Wallumbilla Formation|64856|3|Fully described|p79, p98-101|Albian|Aptian|Named and defined in the Surat Basin by Vine et al. (1967), with the type section in Wallumbilla Creek, near Roma. Also in Eromanga Basin. Contains Doncaster and Coreena Members. Conformably overlies Bungil Formation. Age from pollen assemblages (units APK3, 4). Mudstone, siltstone, concretionary limestone, minor lenticular sandstone, conglomerate. Up to 475m thick.|| ||||29-NOV-17
19323|Wallumbilla Formation|64857|5|Briefly described|p113 Fig.3|||Overlies Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19323|Wallumbilla Formation|65112|6|Mentioned|Fig 11 p324; Fig 16 p 328|Early Cretaceous|Early Cretaceous|Unit in the Surat Basin.|||Includes Doncaster and Coreena Members.|Overlies the Bungil Formation; underlies the Surat Siltstone.||22-MAR-12
19323|Wallumbilla Formation|65113|5|Briefly described|Fig 4 p340|Early Cretaceous|Early Cretaceous|Overlies the Bungil Formation, Surat Siltstone.||||||
19323|Wallumbilla Formation|65114|5|Briefly described|p385 Fig.3|Early Cretaceous||||||||
19323|Wallumbilla Formation|65116|5|Briefly described|Fig 2 p437|Early Cretaceous|Early Cretaceous|Includes Coreena Member, Doncaster Member. Underlies the Surat Siltstone, Overlies the Bungil Formation, Surat Basin.||||||
19323|Wallumbilla Formation|65119|5|Briefly described|p503, 504, fig 7-8 p514, Fig 16-19|Early Cretaceous|Early Cretaceous|Surat Basin. Marine shelf deposits of siltstone, mudstone and fine sandstone. Age: 111-117 Ma. Fission Track age: 87-109 Ma.||||||07-MAR-12
19323|Wallumbilla Formation|65238|5|Briefly described|p7 Fig. 8, p14 Fig. 17|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Transgressive marine deposits.||||||
19323|Wallumbilla Formation|65384|6|Mentioned|S116, S118|||In Surat Basin? Includes Doncaster Member.||||||
19323|Wallumbilla Formation|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Cadna-owie Formation. Overlain by Toolebuc Formation.||||||08-MAR-12
19323|Wallumbilla Formation|65489|5|Briefly described|p49, p55-56, p58, p61, p155|Early Cretaceous|Early Cretaceous|Eromanga Basin. 450m thick. Regional seal.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|66529|6|Mentioned|p12 Fig.5|||||Unit in Rolling Downs Group.|Includes Doncaster, Coreena, Jones V and Ranmoor Members.|||
19323|Wallumbilla Formation|66623|3|Fully described|p239, pp242-245, pp256-259. |Albian|Aptian|Previously known as the Blackdown Formation in Queensland. c.360 m thick. Contains a wide range of fossils. Shoreline to deeper marine environment. Outcrops as low rolling hills. Hosts opals at White Cliffs; possible heavy mineral (magnetite and zircon) strandlines locally.||Unit in Rolling Downs Group.|Includes Coreena and Doncaster Members.|Conformably, but sharply overlies Wyandra Sandstone Member. Coreena Member is gradationally overlain by Allaru Mudstone. Doncaster Member disconformably overlies Cadna-owie Formation.|Muddy sandstone and siltstone with local large spherical calcareous concretions; black shale and minor sandstone with abundant dropstone boulders; pyritic and bioturbated mudstone, claystone and shale; calcareous and glauconitic sandstones.|05-JUN-13
19323|Wallumbilla Formation|66915|4|Described|p1-2, 4-6, p9, p11 Fig.7, p12, p16, p18|Cretaceous|Cretaceous|Carpentaria, Eromanga and Surat Basins. Base of Wallumbilla Formation (the "C-Horizon") and correlatives is the major bounding surface of the Great Artesian Basin.||Basal Rolling Downs Group|Coreena Member, Doncaster Member|Overlies Wyandra Sandstone Member (Cadna-owie Formation), Gilbert River and Bungil Formations.|Marine muds.|12-JAN-17
19323|Wallumbilla Formation|66920|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67133|5|Briefly described|p2, p5, p17-19|Early Cretaceous|Early Cretaceous|Samples of this unit were analysed by XRD and optical microscopy for this study. Consists of quartz (27-52%), feldspars (20-30%) with plagioclase dominant, minor (<8%) kaolinite and significant (13-26%) mixed-layer clays, mainly illite.|||Doncaster and Coreena Members.||Siltstones and mudstones with minor sandstones.|
19323|Wallumbilla Formation|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Cadna-owie Formation. Is overlain by Allaru Mudstone.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Rolling Downs Group.|Includes Doncaster and Coreena Members.|Overlies Easter Monday Formation.|Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice-rafted erratics.|
19323|Wallumbilla Formation|67323|5|Briefly described|p86-87, p92 Fig.12.2, p93, p94 Fig.12.4|Early Cretaceous|Early Cretaceous|See also GIS attrib tbl, Solid Geology Map, p95 Fig.12.5, p96. Eromanga/Carpentaria Basins. Marine sediments.|||Includes Ranmoor Member.|Overlies Cadna-owie and Gilbert River Formations and Longsight Sandstone. Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|67402|4|Described|p26, p26 tbl RRM4, p29|Albian|Aptian|Eromanga Basin. Deposited in a transgressive marine environment which was followed by paralic and fluvial deposition. Ranges from 200 to over 350m thick in the Eromanga Basin and up to 600m thick in the Carpentaria Basin. Proven regional seal for hydrocarbons. Misspelt as Wullumbilla on p265. See also p29 fig PSA4, PSA5, p108-p112, p113 fig ERO12, p115 tbl ERO2, p120, P123, p146 fig SRT3, p148, p156, p176, p177, p179 fig CRP/KRM6, p181, p265.||Rolling Downs Group||Overlies the Cadna-owie Formation and Gilbert River Formation. Overlain by the Allaru Mudstone and Toolebuc Formation.|Consists primarily of marine mudstone interbedded with sandy mudstone, siltstone, shale and limestone.|
19323|Wallumbilla Formation|67561|5|Briefly described|p51-60, p62 Fig.11, p67, p68|Aptian|Aptian|Eromanga Basin. Australian Spore-Pollen zonation: C.hughesi. Deposited on a shallow marine shelf during a cold climate transgression. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||||Correlative of the Bulldog Shale.|Contains glendonites, petrified wood, and ice-rafted boulders of exotic lithology.|20-JAN-17
19323|Wallumbilla Formation|67669|5|Briefly described|p11|Early Cretaceous|Early Cretaceous|Of Bowen Basin.||Unit of Rolling Downs Group.||Underlain by Bungil Formation.||
19323|Wallumbilla Formation|67784|6|Mentioned|p25, p26, p28-29, p31, p32|||185-253m thick. Northern Eromanga Basin.||Wilgunya Subgroup.|Includes Doncaster Member, Jones Valley Member, Ranmoor Member, Coreena Member|Overlies Gilbert River Formation, overlain by Toolebuc Formation||08-FEB-18
19323|Wallumbilla Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Rolling Downs Group.||Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68004|6|Mentioned|p175.|||A seal for reservoirs in the Hooray and Mooga Sandstones.||||||
19323|Wallumbilla Formation|68069|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Surat Basin. Shown on cross-sections and time-space plot and basement interpretation only.||Rolling Downs Group|Includes Coreena and Doncaster Members.|Overlies Bungil Formation. Is overlain conformably by Surat Siltstone.|Sandstone, claystone, siltstone and mudstone.|22-NOV-13
19323|Wallumbilla Formation|68117|5|Briefly described|p346|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|||
19323|Wallumbilla Formation|68206|5|Briefly described|p31-33|Aptian|Aptian|Carpentaria, Eromanga Basins.|||Doncaster, Jones Valley, Ranmoor Members.|Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19323|Wallumbilla Formation|68345|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68349|5|Briefly described|Map legend.|Early Cretaceous|Early Cretaceous|Carpentaria Basin.||||Conformably overlies Coffin Hill Member (Gilbert River Formation).|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68417|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|Carpentaria Basin. No outcrop in map area: shown only in subsurface and rock relationship diagram.||||Conformably underlain by the Coffin Hill Member, Gilbert River Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Surat, Eromanga, Laura and Carpentaria Basins.||Unit in Rolling Downs Group.||Is overlain conformably by Griman Creek Formation and Toolebuc Formation.||
19323|Wallumbilla Formation|68576|5|Briefly described|Q_4: p3|Early Cretaceous|Early Cretaceous|Surat Basin.|||Doncaster, Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|68593|5|Briefly described|p4, p47|Early Cretaceous|Early Cretaceous|Mainly marine deposits.|||Doncaster and Coreena Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.|Siltstone, mudstone, minor conglomerate, rare coal.|
19323|Wallumbilla Formation|68731|6|Mentioned|pp209-211|||||||||
19323|Wallumbilla Formation|68734|5|Briefly described|p218 Fig.2, p221 Fig.3|Aptian|Barremian|Eromanga Basin (NE). Marine to coastal paralic and shallow marine.||Of the Rolling Downs Group.|Includes Coreena Member and Doncaster Member.|||16-JAN-17
19323|Wallumbilla Formation|68821|5|Briefly described|p292 Fig.1, p292, p295, p296, p298|Cretaceous|Cretaceous|Lower Cretaceous age. Equivalent to the Bulldog Shale Formation. Parallic to marine sediments. Contains ubiquitous disseminated pyrite.||Of the Rolling Downs Group.|||Consist of pyrite and carbonaceous-rich marine mudstones and siltstones interbedded with fine sandstones.|
19323|Wallumbilla Formation|68901|5|Briefly described|p7 Fig. ii|Upper Cretaceous|Lower Cretaceous|Eromanga Basin.||Rolling Downs Group|||Mudstone, siltstone, sandstone; calcareous in part.|27-SEP-18
19323|Wallumbilla Formation|69019|5|Briefly described|p85 Fig.21.|Albian|Aptian|Southern Eromanga Basin.||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69023|6|Mentioned|p89 Fig.20, p99|Albian|Aptian|||||||
19323|Wallumbilla Formation|69297|5|Briefly described|p273, p274 fig 4. 3, p275|Upper Cretaceous|Upper Jurassic|Carpentaria Basin. Contains good TOC for hydrocarbon generation.||Rolling Downs Group||Overlies the Gilbert River Formation. Overlain by the Toolebuc Formation.|Lithic glauconitic sandstones, siltstone, claystone and limestone.|
19323|Wallumbilla Formation|69377|5|Briefly described|map legend|Early Cretaceous|Early Cretaceous||||||Mudstone and siltstone with calcareous concretions|
19323|Wallumbilla Formation|69379|5|Briefly described|map legend|Cretaceous|Cretaceous||||Doncaster Member|||
19323|Wallumbilla Formation|69454|6|Mentioned|p38:3, 13|||Eromanga Basin. Potential seal for Cadna-owie Formation sandstone reservoirs.||||||12-JUL-16
19323|Wallumbilla Formation|69455|5|Briefly described|p39:4 Fig.39.3; 39:14-15|Early Cretaceous|Early Cretaceous|Provides a seal to Gilbert River Formation sandstone reservoirs in the offshore Western Gulf Sub-basin. Organic-rich shale is a possible source rock.||||||12-JUL-16
19323|Wallumbilla Formation|69457|3|Fully described|p41:2-3; 41:5 Fig.41.4; 41:6-10, 14-16|Early Cretaceous|Early Cretaceous|Vine et al. (1967). Eromanga, Carpentaria and Surat Basins. Mostly subsurface; outcrops form mesas, buttes or low rounded duricrusted hills. Shallow-marine, nearshore to marginal marine, minor non-marine deposits. 143m to over 350m thick. Equivalent to the succession comprising Bulldog Shale, Coorikiana Sandstone and lower part of Oodnadatta Formation. The name Bulldog Shale has previously (and inappropriately) been used to describe this Formation in the NT (eg Questa, 1990; Ambrose and Heugh, 2010). Has fair to occasionally excellent petroleum source intervals. May seal Cadna-owie Formation reservoirs.||Wilgunya Subgroup.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Cadna-owie Formation conformably, and Algebuckina Sandstone disconformably/unconformably. Is overlain conformably by Toolebuc Formation.|Mudstone and siltstone; minor thin intervals of fine sandstone and limestone. Locally calcareous, and may contain glauconite; shell fragments common in places. Locally silicified to porcellanite. Contains diverse fossil assemblages.|12-JUL-16
19323|Wallumbilla Formation|69582|5|Briefly described|p22, p25-p26, p29, p36, p65-p66|Lower Cretaceous|Lower Cretaceous|Eromanga and Surat basins. Deposited in a marine depositional environment. Intersected in GSQ Longreach 2 drillhole.||||Overlain by the Toolebuc Formation and the Surat Siltstone. Overlies the Bungil Formation and the Cadna-owie Formation.|Sandstone.|
19323|Wallumbilla Formation|69591|6|Mentioned|p101 Fig.2.96|||||||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|69594|4|Described|p518-519, p521-522, p526, p528-530, p534|Aptian|Barremian|See also p538, p540, p550, p573. Vine et al. (1967). Carpentaria, Eromanga, Laura and northern Surat Basins. Much of the upper part was previously known as Blackdown Formation (Laing and Power, 1959; Woods, 1961). Up to 475m thick. Contains a rich marine fauna (listed). Members not always discernible. RELATED UNITS (continued): Equivalent to Rolling Downs Group in the Laura Basin, the Roma Formation and lower part of overlying Tambo Formation.||Wilgunya Subgroup.|Coreena, Doncaster, Jones Valley, Ranmoor, Trimble Members.|Conformably overlies Gilbert River, Cadna-owie, Bungil Formations, Longsight Sandstone, Ronlow and Helby beds. Is overlain by Toolebuc Formation, Surat Siltstone and Allaru Mudstone. See COMMENTS.|Volcanogenic. Dominated by thick successions of sporadically nodular siltstone with lesser glauconitic sandstone, volcanic crystal-lithic sandstone and silty limestone.|
19323|Wallumbilla Formation|69673|5|Briefly described|p155 fig 127, p156, p159, p161|Cretaceous|Cretaceous|||Wilgunya Subgroup|Includes Doncaster Member, Coreena Member|Overlies Mount Anna Sandstone Member, Cadna-owie Formation overlain by Toolebuc Formation, correlated with Bulldog Shale|Mudstone, shale and siltstone with minor thin interbeds of fine sandstone and limestone.|
19323|Wallumbilla Formation|69681|6|Mentioned|p74 Fig.3, p82|Early Cretaceous|Early Cretaceous||||Includes Doncaster and Coreena Members.|||
19323|Wallumbilla Formation|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin.||||||
19323|Wallumbilla Formation|69946|3|Fully described|p19, p21-25, p56-57, p94|Early Cretaceous|Early Cretaceous|Vine et al. (1967); formerly Roma Formation, used by the petroleum industry. Type section is 'Wallumbilla Creek, from Wallumbilla Township south for 12 miles [19.3km]'. Distribution is by definition controlled by Toolebuc Formation: where absent, Bulldog Shale is used. Lithology is identical to Bulldog Shale. Up to 596m thick. Early Aptian-Albian. Wireline log correlations.||||Conformably overlies Cadna-owie Formation. Is overlain conformably by Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone. Local pebbly and muddy diamictite containing metamorphic and sedimentary clasts.|
19323|Wallumbilla Formation|69947|5|Briefly described|p9, p13 Fig.7.2, p29 Fig.7.18|Early Cretaceous|Early Cretaceous|See also p31 Fig.7.20. Eromanga Basin.||Marree Subgroup.||Overlies Wyandra Sandstone Member (Cadna-owie Formation).|Thick, fossiliferous mudstones and siltstones.|
19323|Wallumbilla Formation|69948|6|Mentioned|p4; Figs.4.2, 18|||Eromanga Basin (an intracratonic basin). Sediment thickness, sonic log, gamma ray log all shown in contrast with Otway Basin (a rift basin).||||Overlies Cadna-owie Formation. Is overlain by Toolebuc Formation.|Marine shales.|
19323|Wallumbilla Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Mudstone, siltstone, sandstone; calcareous in part.|
19323|Wallumbilla Formation|70207|6|Mentioned|p14, p74|Early Cretaceous|Early Cretaceous|Georgetown region.||||||
19323|Wallumbilla Formation|70345|6|Mentioned|p3|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup.|||Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70354|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Rolling Downs Group.||Is overlain by Toolebuc Formation.|Mudstone and siltstone with calcareous concretions.|
19323|Wallumbilla Formation|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Wilgunya Subgroup|||Mudstone and siltstone with calcareous concretions.|20-JAN-22
19323|Wallumbilla Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|Includes Coreena Member, Doncaster Member.||Marine grey mudstone and siltstone with minor interbeds of fine-grained glauconitic and calcareous sandstone, local thin micritic limestone beds and heavy mineral strandline accumulations; down-sequence glacial ice rafted erratics.|
19323|Wallumbilla Formation|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Unconsolidated sediments also described.||Rolling Downs Group|Includes Coreena Member, Doncaster Member.|||
19323|Wallumbilla Formation|70673|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|70720|6|Mentioned|p24-25|Early Cretaceous|Early Cretaceous||||Doncaster Member.|||
19323|Wallumbilla Formation|70821|4|Described|p21 Fig.2.6, p22 Fig.2.7, p23, p28|Early Cretaceous|Early Cretaceous|See also p30-31, p33, p79-80, p82, p85-88, p111-112, p117. Vine et al. (1967). The most widely distributed marine unit within the Great Australian Superbasin: Eromanga, Carpentaria, Laura and parts of Surat Basins. Varying thicknesses given from wells. Aptian to Albian age. Hydrochemistry mentioned; hydrostratigraphic properties. Equivalent to Bulldog Shale and Oodnadatta Formation.||Rolling Downs Group.|Doncaster, Coreena Members.|Overlies Cadna-owie and Bungil Formations, Hooray Sandstone and Drildool beds. Is overlain by Toolebuc Formation or Surat Siltstone; locally by Winton Formation (conformably).||
19323|Wallumbilla Formation|70823|5|Briefly described|p43-p44, p78|Early Cretaceous|Early Cretaceous|Eromanga Basin. Up to 450m thick. Deposited in open marine transgressive to regressive marine shoreface environments.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Cadna-owie Formation. Overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|70836|6|Mentioned|p474|Early Cretaceous|Early Cretaceous|Lightning Ridge area, Surat Basin. Barremian-Albian.|||Coreena, Doncaster Members.|Overlies Bungil Formation. Is overlain by Surat Siltstone.||
19323|Wallumbilla Formation|70860|6|Mentioned|p281|||Great Artesian Basin.|||Coreena, Doncaster, Ranmoor, Jones Valley, Members.|||
19323|Wallumbilla Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29|||First described by Isbell (1957). Eromanga Basin. 186m total thickness in Eulo 1 borehole; it was not possible to differentiate the two Members in this borehole. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||Rolling Downs Group.|Coreena and Doncaster Members.|Overlies Wyandra Sandstone Member (Cadna-owie Formation). Is overlain by Winton Formation.|Generally monotonous, glauconitic, marine, dark bluish-grey carbonaceous mudstone with some lignite plant fragments, some thin (estimated <1m) beds of siltstone and fine sandstone.|
19323|Wallumbilla Formation|71321|5|Briefly described|p15,27,65|Cenomanian|Cenomanian|Of Eromanga Basin. Previously known as Roma Formation. Regressivee depositional package following peak early Cretaceous marine transgression; marginal marine shoreface deposit.||||Equivalent to Bulldog Shale. Overlain by the Toolebuc Formation.||24-OCT-19
19323|Wallumbilla Formation|71342|3|Fully described|Ch4 p4, Ch4 p9, Ch4 p25|Albian|Aptian|Eromanga Basin. Formally defined by Vine et al (1967)  to replace the Roma Formation. Vine et al also defined the type section in "Wallumbilla Creek,from Wallumbilla Township south for 12 miles" in Queensland. This unit reaches a maximum thickness of 596m in Coonatie 1 in the Patchawarra Trough and 260m in the Poolowanna Trough. Age derived from palynology. Interpreted to have been deposited in a shallow epicontinental sea at cold high latitudes as debris flows. Spore-pollen zone is given in Ch5 p57. See also Ch5 p22, Ch5 p24-p25, Ch5 p30, Ch5 p57, Ch6 p8-p9, Ch7 p9, Ch7 p13, Ch10 p17, Ch11 p4-p5, Ch12 p12, Ch12 p14.||||Conformably overlies the Wyandra Sandstone Member (Cadna-owie Formation). Conformably overlain by the Toolebuc Formation.|Grey mudstone and siltstone with minor interbeds of fine-grained sandstone.|
19323|Wallumbilla Formation|71382|5|Briefly described|p4, p13, p16-p17, p19-p20|||Intersected in GSQ Julia 1 from 199.87m-310.49m for a total of 110.62m thickness. Temp log and stratlog are provided. Lithology is described in detail on p20. See also p23, p25, p27, App 3, 4.||||Overlies the Hooray Sandstone. Overlain by the Toolebuc Formation.|Interbedded mudstone and sandstone with minor calcareous mudstone.|
19323|Wallumbilla Formation|71855|4|Described|p2, p4-p6, p9-p10, p13|Jurassic|Jurassic|Eromanga and Carpentaria basins. In places the contact with the overlying Toolebuc Formation is disconformable or faulted. Wireline log responses were described for this unit including Gamma-ray, sonic transit time and resistivity. Structure is discussed. See also p15, p27, p33-p35, p50, p52-p53, p56-p57, p75.||||Conformably (gradationally) overlain by the Toolebuc Formation.|Glauconitic, smectite-rich mudstone, siltstone or fine-grained sandstone.|
19323|Wallumbilla Formation|71863|5|Briefly described|p4-p9|Albian|Aptian|Eromanga and Carpentaria basins. Deposited in a marine incursion.||Rolling Downs Group|Includes the Doncaster Member and the Coreena Member.|Overlies the Gilbert River Formation, Helby beds and the Cadna-owie Formation. Conformably overlain by the Toolebuc Formation.||
19323|Wallumbilla Formation|71864|4|Described|p8, p10, p13-p14, p16-p20|||Intersected in GSQ Eulo 2 borehole between 23-51m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as glauconitic marine siltstones and claystones. Gamma log characteristics and magnetic susceptibility is provided.||Rolling Downs Group|Includes the Coreena Member and the Doncaster Member.|Overlain by the Winton Formation. Overlies the Waihora Volcanics.|Dark blue to light grey siltstone with a distinctive layer producing carbonaceous flecks and a fine quartzose sandstone layer in addition to mudstone.|
19323|Wallumbilla Formation|71890|6|Mentioned|p7|||Surat Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72297|5|Briefly described|p742, p746, p753|||Eromanga Basin. Acts as a regional seal. Potential hydrocarbon source rocks.|||Ranmoor Member.|Is overlain conformably by the Toolebuc Formation.|Shales and mudstones.|
19323|Wallumbilla Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (SA,QLD,NSW), Carpentaria Basin, Surat Basin (QLD,NSW), Coonamble Embayment (NSW).||Rolling Downs Group.|Doncaster, Coreena, Jones Valley, Ranmoor Members.|Overlies Wyandra Sandstone Member (Cadna-owie FZ); Gilbert River and Bungil FZs; Ronlow, Helby, Albany Pass and Drildool beds. Is overlain by Toolebuc FZ or Surat Siltstone.||
19323|Wallumbilla Formation|72913|6|Mentioned|p8.|||Two wells intersected this cover unit.||||||
19323|Wallumbilla Formation|72914|5|Briefly described|p12, p14, p16, p18, p20-21, p29, App. I|Cretaceous|Cretaceous|In Tongo 1 [borehole], the unit is semi-monotonous consisting chiefly of marine siltstone and claystone, but can occasionally has washes of coarser-grained quartzose sediments derived from local basement highs. Natural gamma emissions are relatively subdued and monotonous.||||Underlain by the Wyandra Sandstone Member (Cadna-owie Formation).|Marine siltstone and claystone with occasional washes of coarser-grained quartzose material.|
19323|Wallumbilla Formation|72915|6|Mentioned|p16, p19, p27, p39 App E, App I|Mesozoic|Mesozoic|Sedimentary rocks in the Congararra 1 borehole are attributed to the Rolling Downs Group, and may represent source-proximal Wallumbilla Formation (after Hawke and Cramsie, 1984). Mineralogical changes from clay-rich to quartz-rich are reflected in natural gamma emissions [data]. Relatively non-magnetic in Congararra 1. No groundwater was made from this unit in Congararra 1.||||||
19323|Wallumbilla Formation|72967|6|Mentioned|p5|||Carpenteria Basin.||Rolling Downs Group||||
19323|Wallumbilla Formation|72983|6|Mentioned|p15|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73083|6|Mentioned|p62-63|Cretaceous|Cretaceous|||||Overlain by the Toolebuc Formation.|Mudstone and siltstone.|
19323|Wallumbilla Formation|73113|5|Briefly described|p. 22-24, 36-37, 41, 69, 80, 88, 116...|||Surat Basin. Tight aquitard. More locations: p. 119, 146, 151-152, 168-172, 177-178, 191.||||||
19323|Wallumbilla Formation|73137|6|Mentioned|p6, p81|Cretaceous|Cretaceous|Carpentaria Basin. Intersected in drill hole GIDPDS5.||||||08-OCT-22
19323|Wallumbilla Formation|73144|6|Mentioned|p8, p13|Cretaceous|Cretaceous|Carpentaria Basin. Leaky aquitard.||Rolling Downs Group||Underlain by Gilbert River Formation. Overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73147|5|Briefly described|p129|Aptian|Aptian|||Rolling Downs Group.||Overlies Gilbert River Formation. Is overlain by Toolebuc Formation.||
19323|Wallumbilla Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
19323|Wallumbilla Formation|73203|6|Mentioned|p653|Early Cretaceous|Early Cretaceous||||Doncaster Member||Includes interbedded sandy/silty claystone and interbedded fine sandstones.|
19323|Wallumbilla Formation|73249|5|Briefly described|p319, p321, p323|Albian|Aptian|North and east of the Eromanga Basin [shown as within the Eromanga Basin on p319 Fig.2]. Laterally equivalent to the Bulldog Shale.||||Lateral equivalent to the Bulldog Shale, overlies the Cadna-owie Formation, underlies the Toolebuc Formation.|Siltstone and mudstone dominated.|
19323|Wallumbilla Formation|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73281|6|Mentioned|p1, Appendix (DIP)|||Eromanga Basin. See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
19323|Wallumbilla Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Wyandra Sandstone Member (Cadna-owie Formation). Overlain by Toolebuc Formation. Equivalent to Coorikiana Sandstone and Bulldog Shale.||
19323|Wallumbilla Formation|73472|6|Mentioned|p114|Cretaceous|Cretaceous|||||||
19323|Wallumbilla Formation|73479|5|Briefly described|p156 Fig.2, p159, p163, p164 Fig.7, p175|Cretaceous|Cretaceous|Eromanga Basin. Restricted open marine and shoreface depositional environment.|ca 125-104 Ma|||Overlies Wyandra Sandstone Member, underlies Toolebuc Formation||
19323|Wallumbilla Formation|73553|6|Mentioned|p7|Cretaceous|Cretaceous|||||||
19340|Walwa Granite|23309|6|Mentioned|p448 App 1|||G104. Obsolete Name.||||||22-OCT-10
19340|Walwa Granite|33779|4|Described|p164|||||||||
19340|Walwa Granite|39860|5|Briefly described|p17|||See also p26.||||||14-NOV-07
19340|Walwa Granite|42726|5|Briefly described|map legend|||||||||
19343|Wambo Coal Member|29942|4|Described|Fig.1|||Permian||||||
19343|Wambo Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19343|Wambo Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19343|Wambo Coal Member|40805|6|Mentioned|Table 1|||||||||
19343|Wambo Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Malabar Formation.||||
19350|Wammerra Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
19350|Wammerra Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Eurowie Subgroup (Torrowangee Group). Lenticular flaggy limestone. Age: ~700Ma. Max. thickness: 750m. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
19350|Wammerra Formation|30261|4|Described|Table 1|||Sturtian - Marinoan age.||||||
19350|Wammerra Formation|34812|3|Fully described|p82|||||||||
19350|Wammerra Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
19350|Wammerra Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
19350|Wammerra Formation|36733|6|Mentioned|Table 5|||||||||
19350|Wammerra Formation|37931|4|Described|p532|||||||||
19350|Wammerra Formation|39574|6|Mentioned|p155|||||||||
19350|Wammerra Formation|41405|5|Briefly described|p204|||||||||
19350|Wammerra Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
19350|Wammerra Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Is overlain by Tanyarto Formation.|Buff, flaggy, silty to sandy limestone grading into laminated siltstone-dominated sequences with minor limestone; thin, calcareous sandy interbeds common.|08-SEP-15
19364|Wandandian Granite|42726|5|Briefly described|map legend|Carboniferous||55.||||||
19364|Wandandian Granite|70661|6|Mentioned|p130|||||||||
19366|Wandella Sandstone Member|2967|5|Briefly described|p46|||Referred to as Wandella Sandstone (see references p35, 46-47) except for this one mention as the current, formal Wandella Sandstone Member.||Parilla Sand.|||Contains heavy mineral bands.|
19366|Wandella Sandstone Member|10010|5|Briefly described|p12 Fig. 3|Late Pliocene|Early Pliocene|Of Loxton-Parilla Sand. Geological Province: Murray Basin.||||||13-AUG-07
19366|Wandella Sandstone Member|22773|5|Briefly described|Fig24.8p352|||||||||
19366|Wandella Sandstone Member|22799|5|Briefly described|p24 Fig.10|Early Pliocene|Early Pliocene|||||||
19366|Wandella Sandstone Member|22857|5|Briefly described|p352 Fig.24.8|Late Pliocene|Early Pliocene|Of the Parilla Sand? Geological Province: Murray Basin.||||||
19366|Wandella Sandstone Member|22887|5|Briefly described|Fig.6 p13|Late Pliocene|Early Pliocene|||||||
19366|Wandella Sandstone Member|22893|5|Briefly described|fig4 p9|||||||||
19366|Wandella Sandstone Member|23884|5|Briefly described|p155 Fig. 13.2|Pliocene|Pliocene|Geological Province: Murray Basin.||||||
19366|Wandella Sandstone Member|39329|6|Mentioned|p485|||See also Fig.1||||||
19366|Wandella Sandstone Member|40820|6|Mentioned|Fig.4|||||||||
19366|Wandella Sandstone Member|42130|6|Mentioned|Fig.3 P265|||||||||
19366|Wandella Sandstone Member|42134|6|Mentioned|Fig.3 P335|||||||||
19366|Wandella Sandstone Member|42966|2|Defined|Table 27, p172|Pliocene||of Loxton-Parilla Sands||||||
19366|Wandella Sandstone Member|43791|6|Mentioned|p372, Fig1|||||||||
19366|Wandella Sandstone Member|43804|6|Mentioned|Fig.2,p49|||||||||
19366|Wandella Sandstone Member|49040|6|Mentioned|Fig.6|||||||||
19366|Wandella Sandstone Member|65552|5|Briefly described|p5 Fig. 3|Late Pliocene|Early Pliocene|Of Loxton-Parilla Sands. Unconformably overlies Geera Clay and Olney Formation. Overlies Tragowel and Wandella Sandstone Members. Underlies Blanchetown Clay.||||||
19366|Wandella Sandstone Member|66286|6|Mentioned|p179, 188|||Southern Murray Basin. Regressive beach sequence.||Unit in Loxton-Parilla sands.||Overlies Tragowel Member.||
19366|Wandella Sandstone Member|72445|6|Mentioned|App.7 p7 Fig.4.|Pliocene|Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991).||Probably of Loxton-Parilla Sands||May be partially equivalent to the Shepparton Formation, Wunghnu Group.|Shown as including sandstone.|
19383|Wandrawandian Formation|22601|6|Mentioned|411, 417, 419|Permian|Permian|Geol province Sydney Basin||||||
19383|Wandrawandian Formation|43377|14|Not recorded|p143|||Formation of Shoalhaven Group||||||
19383|Wandrawandian Formation|47041|6|Mentioned|p167|||||||||
19383|Wandrawandian Formation|60281|5|Briefly described|p9, p59|||Same as Wandrawandian Siltstone?  Of the Maitland Group [??].  Geological Province: Sydney Basin.||||||24-AUG-12
19383|Wandrawandian Formation|70661|4|Described|p6, p137, p139, p161-p167, p169, p174|Roadian|Kungurian|Named after Wandrawandian Creek (now Wandandian Creek). Previously termed Wandrawandian Pebbly sandstones, Wandrawandian Sandstone or Wandrawandian Siltstone. These were all replaced byWandrawandian Formation so as to better reflect the lithology. Distribution, geomorphology,  fossil assemblage and structure discussed.  Potential as hydrocarbon seal and source. Up to 200m thick in some places. Deposited in a cold climate, near shore marine environment. Age based on fossil evidence and correlation with Branxton Formation.||||Conformably overlain by Nowra Sandstone, Purnoo Conglomerate Member, conformably (and probably gradationally) overlies Snapper Point Formation, equivalent to Branxton Formation|Very fine to fine grained, lithic quartzose sandstone that is commonly silty and bioturbated, micaceous, sandy siltstone. Claystone, medium grained sandstone and rare pebble and cobble, matrix supported conglomerate.|
19383|Wandrawandian Formation|71303|5|Briefly described|map legend|Cisuralian|Cisuralian|Of Sydney Basin.||Of Shoalhaven Group.|||Dark to light grey, lithic-quartz very fine to medium-grained sandstone, sandy siltstone, silty claystone, rare siltstone + matrix-supported conglomerate. Micaceous, bioturbated, ubiquitousdropstones, macrofossils locally.|
19401|Wangellic Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
19423|Wantabadgery Granite|22508|5|Briefly described|p2||Silurian|Keotong Supersuite, Lachlan Fold Belt||||||
19423|Wantabadgery Granite|22638|3|Fully described|p50|Early Devonian|Llandovery|Previously "Ardlethan Granite" in small part, "Wantabadgery Granodiorite". 415 +/- 13 Ma. Tom Groggin Suite||||||04-OCT-05
19423|Wantabadgery Granite|22685|5|Briefly described|p728,Fig1p729,732||Silurian|S-type.||||||17-JAN-06
19423|Wantabadgery Granite|24119|5|Briefly described|p3|Silurian|Silurian|||||||
19423|Wantabadgery Granite|24417|6|Mentioned|p9|||||||||
19423|Wantabadgery Granite|29953|6|Mentioned|p3|||||||||
19423|Wantabadgery Granite|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
19423|Wantabadgery Granite|29994|6|Mentioned|Map legend|Silurian|Silurian|||||||
19423|Wantabadgery Granite|31800|6|Mentioned|p202|||||||||
19423|Wantabadgery Granite|34544|5|Briefly described|p183|||||||||
19423|Wantabadgery Granite|35607|6|Mentioned|p38|||See also P126,127,128.||||||
19423|Wantabadgery Granite|35608|6|Mentioned|Map legend|Silurian|Silurian|||||||
19423|Wantabadgery Granite|35609|4|Described|p18|||||||||
19423|Wantabadgery Granite|39331|6|Mentioned|p29|||||||||
19423|Wantabadgery Granite|40328|4|Described|p211|||||||||
19423|Wantabadgery Granite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
19423|Wantabadgery Granite|40498|6|Mentioned|p366|||||||||
19423|Wantabadgery Granite|40678|5|Briefly described|p5|||||||||
19423|Wantabadgery Granite|41320|5|Briefly described|p210|||||||||
19423|Wantabadgery Granite|42497|5|Briefly described|Map legend|Wenlockian|Llandoverian|||||||
19423|Wantabadgery Granite|42726|5|Briefly described|map legend|Silurian||||||||
19423|Wantabadgery Granite|43344|14|Not recorded|p135|||||||||
19423|Wantabadgery Granite|44192|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
19423|Wantabadgery Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
19423|Wantabadgery Granite|50191|5|Briefly described|p6, 32|Early Silurian|Early Silurian|S Type.||||||
19423|Wantabadgery Granite|60086|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
19423|Wantabadgery Granite|69371|6|Mentioned|p9, p14|Silurian|Silurian|||||||
19423|Wantabadgery Granite|69801|6|Mentioned|p2, p136|||Central Lachlan Orogen. Yielded four ages in total ranging from 434.2 +/- 3.6 Ma to 430.6 +/- 5.9 Ma (Ickert and Williams, 2011). Defines the southeast-trending spine of the Wagga Batholith in western and southern COOTAMUNDRA.|||||S-type granite.|
19423|Wantabadgery Granite|70777|5|Briefly described|p1, p16, p22, p32, p37, p80|Wenlock|Llandovery|Lachlan Orogen. Ages derived from Ickert and Williams, 2011.|434.2 +/- 2.6 Ma-430.6 +/- 5.9 Ma|||||
19423|Wantabadgery Granite|70910|14|Not recorded|p43|||Refers to Vallance (1953).||||||
19423|Wantabadgery Granite|72082|5|Briefly described|p4, p33|Early Silurian|Early Silurian|Geochronology by Ickert and Williams (2011). Effectively identical to a Geoscience Australia age of 432.3 +/- 5.0 Ma.|432.2 +/- 4.3 Ma (SHRIMP U-Pb zircon).|||Intrudes the Wagga Group. Abuts the Junee Reefs Granite.|Grey, equigranular, porphyritic, quartz-feldspar-biotite-muscovite granite; tourmaline-bearing, locally pegmatitic, xenolith-rich.|
19423|Wantabadgery Granite|72084|4|Described|p2, p6 Fig.5a, p17-29, p32, p35, p57-59|Silurian|Silurian|Very extensive pluton (over 2550 km2); forms an elongate body c.105km long. Forms well-rounded boulder, tor and pavement outcrops. Petrography and geochemistry detailed. Numerous photographs, photomicrographs and element plots.An additional SHRIMP U-Pb date of 432,3 +/- 5 Ma is derived from Geoscience Australias OZCHRON database.|432.2 +/- 4.3 Ma (Ickert and Williams, 2011).|||Intrudes Wagga Group, Junawarra Volcanics and Eurongillie Serpentinite. Surrounds Roseleigh rhyolite.|Cordierite-biotite granite with rare occurrences of layered pegmatite and aplite dykes. S-type. Each lithology described in detail.|29-AUG-19
19423|Wantabadgery Granite|72571|6|Mentioned|p90, p96-98, p100|||Of the Tasmanides of eastern Australia. Petrography of sample and zircon description and analyses are discussed in detail. S-type.||Tom Groggin Suite||||
19428|Wapentake Formation|13996|5|Briefly described|p138-139, p142|Llandovery|Llandovery|A new species of conulariid mentioned. The "Ilaenus Band" at the base of this unit is now thought to be early Wenlock. Bivalve taxa distribution Table. Gastropod species listed.||||Is overlain by Dargile Formation.||
19428|Wapentake Formation|22511|6|Mentioned|p660|||||||||
19428|Wapentake Formation|22542|6|Mentioned|p664|||||||||
19428|Wapentake Formation|22684|4|Described|p751, Fig.2 p746|Wenlock|Wenlock|||||||
19428|Wapentake Formation|22886|4|Described|p13|Wenlock|Llandovery|||||||
19428|Wapentake Formation|23229|4|Described|Table3-3p26, 28|Llandovery|Llandovery|Also known as 'Springfield Sandstone'||||||
19428|Wapentake Formation|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
19428|Wapentake Formation|23309|5|Briefly described|p115, 137, 153, 268. Table 2.49|Devonian|Silurian|||||||
19428|Wapentake Formation|24177|3|Fully described|p51, p50 Fig. 22|Early Silurian|Early Silurian|Overlain by the Dargile Formation. Overlies the Costerfield Siltstone. Geological Province: Melbourne Trough. Maximum Thickness: 1750m.||||||
19428|Wapentake Formation|24328|5|Briefly described|Map legend|Early Silurian|Early Silurian|||||||
19428|Wapentake Formation|24329|5|Briefly described|Map legend|Early Silurian|Early Silurian|||||||
19428|Wapentake Formation|24588|5|Briefly described|p12 Fig.3, p18|Wenlock|Llandovery|Geological Province: Darraweit Guim Province.||||||29-NOV-13
19428|Wapentake Formation|31161|5|Briefly described|PA10|||||||||
19428|Wapentake Formation|31654|6|Mentioned|Map legend|Wenlockian|Wenlockian|||||||
19428|Wapentake Formation|32074|6|Mentioned|Table 1|||Section. See also P180||||||
19428|Wapentake Formation|33315|6|Mentioned|Fig.1|||U.Sil.||||||
19428|Wapentake Formation|33394|5|Briefly described|p74|||||||||
19428|Wapentake Formation|33604|6|Mentioned|p17|||Correlation chart. Silurian||||||
19428|Wapentake Formation|35283|3|Fully described|p47|||||||||
19428|Wapentake Formation|37727|4|Described|p92|||||||||
19428|Wapentake Formation|37752|6|Mentioned|p115|||||||||
19428|Wapentake Formation|38070|6|Mentioned|Fig.8|||P96||||||
19428|Wapentake Formation|38378|6|Mentioned|Fig.1|||||||||
19428|Wapentake Formation|38787|6|Mentioned|p125|||||||||
19428|Wapentake Formation|39331|6|Mentioned|Table 2-1|||||||||
19428|Wapentake Formation|41585|4|Described|p107|||Mention p120.||||||21-OCT-22
19428|Wapentake Formation|42994|6|Mentioned|p37|||||||||
19428|Wapentake Formation|43871|14|Not recorded|p10,11 Fig.1,12-55|||Fauna||||||
19428|Wapentake Formation|48971|6|Mentioned|p9|||See also p11, p12, p17, p23, p24, p28, p29, p36.||||||21-OCT-22
19428|Wapentake Formation|60591|5|Briefly described|Map Legend|Llandovery|Llandovery|Distal continental shelf deposit: Coarsening upward sequence of turbiditic sandstone and siltstone; thinly to thickly bedded, minor large channels, ripple drift and swaley cross-laminations, minor burrows.||||||
19428|Wapentake Formation|60592|5|Briefly described|Map Legend|Llandovery|Llandovery|Distal continental shelf deposit: Coarsening upward sequence of turbiditic sandstone and siltstone; thinly to thickly bedded, minor large channels, ripple drift and swaley cross-laminations, minor burrows.||||||
19428|Wapentake Formation|60593|5|Briefly described|Map Legend|Llandovery|Llandovery|Distal continental shelf deposit: Coarsening upward sequence of turbiditic sandstone and siltstone; thinly to thickly bedded, minor large channels, ripple drift and swaley cross-laminations, minor burrows.||||||
19428|Wapentake Formation|60595|5|Briefly described|Map Legend|Llandovery|Llandovery|Distal continental shelf deposit: Coarsening upward sequence of turbiditic sandstone and siltstone; thinly to thickly bedded, minor large channels, ripple drift and swaley cross-laminations, minor burrows.||||||
19428|Wapentake Formation|60596|5|Briefly described|Map Legend|Llandovery|Llandovery|Distal continental shelf deposit: Coarsening upward sequence of turbiditic sandstone and siltstone; thinly to thickly bedded, minor large channels, ripple drift and swaley cross-laminations, minor burrows.||||||
19428|Wapentake Formation|60597|5|Briefly described|Map Legend|Llandovery|Llandovery|Low magnetic response, with weak magnetic linear features; moderate to high K, moderate Th.||||||29-NOV-04
19428|Wapentake Formation|60599|3|Fully described|p13, p20, p24 Tb. 4, p50-51, P106|Llandovery|Llandovery|Coarsening-upwards turbiditic sst+interbedded siltst.- lower part invariably iron-stained and quartz-cemented. Conformable under Dargile Formation; overlies Illaenus Band (Costerfield Siltstone). Max. thickness:1750m (est.). Geol.Prov: Melbourne Zone/LFB.||||||01-DEC-15
19428|Wapentake Formation|61185|5|Briefly described|p22, p13, p21 Fig. 6|Llandovery|Llandovery|Turbidites. Conformably overlies Dargile Fm. Unit relationships with Dargile Formation in text p22 conflict with p21 Fig 6. Geological Province: Lachlan Fold Belt, Melbourne Zone.||||||07-FEB-11
19428|Wapentake Formation|62469|6|Mentioned|p5 Fig. 2, p54, p15|Wenlock|Wenlock|Geological Province: Darraweit Guim Province.  Includes informal 'Illaenus band'.||||||12-FEB-15
19428|Wapentake Formation|63083|5|Briefly described|p215, p216 Tb. 1, p222|Wenlock|Wenlock|Formerly said to include the "Illaenus band" at its base (Thomas 1937), but this has now been placed at top of Costerfield Siltstone (Edwards et al 1998). Overlies Costerfield Siltstone. Dominated by the illaenid, Thomastus thomastus. See also p227 p230.||||||07-FEB-11
19428|Wapentake Formation|64611|5|Briefly described|Map legend|Wenlock|Wenlock|Of Murrindindi Supergroup. Sandstone and siltstone: fine- to medium-grained quartz sandstone with weathered siltstone interbeds; minor large channels, ripple drift, swaley x-laminations and burrows. Distal continental shelf deposits.||||||26-JUN-14
19428|Wapentake Formation|64612|2|Defined|p27, p37, p38-39|Ludlow|Late Llandovery|Of Murrindindi Supergroup. Conformable between Costerfield Siltstone and Dargile Formation. Thickness: 1750m. Fine-grained quartz sandstone interbedded with siltstone. Submarine deposition.||||||26-JUN-14
19428|Wapentake Formation|68116|5|Briefly described|Appendix, Maps 24, 32.|Sheinwoodian|Sheinwoodian||||||Sandstone and siltstone: fine to medium-grained quartz sandstone with weathered siltstone interbeds; minor large channels, ripple drift, swaley cross-laminations and burrows; distal continental shelf deposits.|
19428|Wapentake Formation|70904|4|Described|p 34|||||||||
19428|Wapentake Formation|70933|14|Not recorded|opp. p94|Devonian|Silurian|Generalised east-west section. Refers to Talent (1965).||||||19-APR-17
19428|Wapentake Formation|73497|5|Briefly described|Map legend|Silurian|Silurian|Marine.||Murrindindi Supergroup|||Sandstone, siltstone, conglomerate: low magnetic response, with weak magnetic linear features of short strike length (2km); moderate-high K, moderate Th, arcuate radiometric trends follow strike.|
19437|Waratah Sandstone|22578|5|Briefly described|Fig.5 p395, p400|||Of the Newcastle Coal Measures.||||||14-MAR-07
19437|Waratah Sandstone|22857|5|Briefly described|p522 App.1 Tb.A1.9|Late Permian|Late Permian|Max. thickness: 20m.||||||
19437|Waratah Sandstone|22969|5|Briefly described| Fig 3.1|||Lachlan Fold Belt.||||||
19437|Waratah Sandstone|23055|6|Mentioned|p1,22|||||||||
19437|Waratah Sandstone|24121|5|Briefly described|p4|||||||||
19437|Waratah Sandstone|24157|5|Briefly described|p187, p188 Tb.1, p209 Fig.19|Permian|Permian|Overlain by Newcastle Coal Measures. Underlain by Tomago Coal Measures. Geological Province: Sydney Basin||||||14-MAR-07
19437|Waratah Sandstone|24158|5|Briefly described|p173 Fig.4|Late Permian|Late Permian|Of the Tomago Coal Measures. Geological Province: Sydney Basin||||||
19437|Waratah Sandstone|24471|4|Described|p32 Fig.4, p33|Late Permian|Late Permian|Of Newcastle Coal Measures. Possibly stratigraphically equivalent to Darkes Forest Sandstone. Overlies Demspey Formation. Geological Province: Sydney Basin.||||||07-FEB-11
19437|Waratah Sandstone|29922|6|Mentioned|Appendix 4|||||||||
19437|Waratah Sandstone|29926|6|Mentioned|Fig.3|||Permian||||||
19437|Waratah Sandstone|29942|4|Described|Fig.2|||Permian||||||
19437|Waratah Sandstone|31885|6|Mentioned|p1439|||||||||
19437|Waratah Sandstone|33334|5|Briefly described|p8|||Permain||||||
19437|Waratah Sandstone|33867|6|Mentioned|p11|||||||||
19437|Waratah Sandstone|34351|5|Briefly described|p341|||Fig.5.13||||||
19437|Waratah Sandstone|34448|5|Briefly described|p433|||Permian||||||
19437|Waratah Sandstone|34465|6|Mentioned|p337|||||||||
19437|Waratah Sandstone|35319|6|Mentioned|Table 1|||||||||
19437|Waratah Sandstone|36042|6|Mentioned|Fig.9|||See also Fig.19.||||||
19437|Waratah Sandstone|37083|6|Mentioned|p174|||||||||
19437|Waratah Sandstone|37087|6|Mentioned|p198|||||||||
19437|Waratah Sandstone|38656|5|Briefly described|Fig.1.5.13|||P280||||||
19437|Waratah Sandstone|39287|6|Mentioned|p20|||See also Fig.2.15||||||
19437|Waratah Sandstone|39292|6|Mentioned|p101|||||||||
19437|Waratah Sandstone|39308|6|Mentioned|p481|||See also Fig.23.4||||||
19437|Waratah Sandstone|39609|6|Mentioned|Table 1|||||||||
19437|Waratah Sandstone|40166|6|Mentioned|p347|||See also Table 1 and Fig.2||||||
19437|Waratah Sandstone|40256|6|Mentioned|Fig.3|||||||||
19437|Waratah Sandstone|40321|6|Mentioned|Fig.3|||||||||
19437|Waratah Sandstone|40330|6|Mentioned|p68|||||||||
19437|Waratah Sandstone|40971|6|Mentioned|p210|||||||||
19437|Waratah Sandstone|41479|6|Mentioned|Fig.2|||||||||
19437|Waratah Sandstone|42182|6|Mentioned|p299|||||||||
19437|Waratah Sandstone|42214|6|Mentioned|Table 1 P462|||||||||
19437|Waratah Sandstone|43017|5|Briefly described|Fig.1,p372|||||||||
19437|Waratah Sandstone|43194|5|Briefly described|p129 Tb. 8.3|Late Permian|Late Permian|Newcastle region, Sydney Basin.||||||
19437|Waratah Sandstone|43344|14|Not recorded|p21,79,85||Permian|||||||
19437|Waratah Sandstone|43440|14|Not recorded|p32,35,49,51|||Unit of Newcastle Coal Measures||||||
19437|Waratah Sandstone|43447|14|Not recorded|Tb 1,p23,24,diag.p26|||Part of Newcastle Coal Measure||||||
19437|Waratah Sandstone|43448|14|Not recorded|p224,226,229,230,231||Permian|Unit of Lambton Subgroup (Newcastle Coal Measures). p235,236,Pl.1.||||||
19437|Waratah Sandstone|43477|14|Not recorded|p21,22,52,Pl.3||Permian|||||||
19437|Waratah Sandstone|45090|5|Briefly described|p63|||Lithology, relationships, correlation, age||||||
19437|Waratah Sandstone|60281|5|Briefly described|p62, p65|||Basal unit of the Newcastle Coal Measures.  A medium-grained sandstone, well sorted in the middle.  Thickness at type section: 20m.  Geological Province: Sydney Basin.||||||
19437|Waratah Sandstone|61315|5|Briefly described|Table SY1|Late Permian|Late Permian|Geological Province: Sydney Basin/Newcastle area.||||||
19437|Waratah Sandstone|61612|6|Mentioned|p274, p277|Late Permian|Late Permian|||||||
19437|Waratah Sandstone|62033|5|Briefly described|p24, p25 (Table)|||Underlies Newcastle Coal Measures. Overlies Tomago Coal Measures. Equivalent to Watts Sandstone in the Hunter Valley Coalfield. Geological Province: Sydney Basin.||||||17-APR-14
19437|Waratah Sandstone|68003|6|Mentioned|p41.|Late Permian|Late Permian|Sydney Basin. A marine incursion interrupting coal formation.||||||
19437|Waratah Sandstone|68004|5|Briefly described|p23 Table 1.|||Newcastle Coalfield.||Unit in Tomago Coal Measures.||Overlies Dempsey Formation. Is overlain by Newcastle Coal Measures.||
19437|Waratah Sandstone|68493|6|Mentioned|p5 Fig.2|Lopingian|Lopingian|Barrier bar depositional environment.||Basal unit of the Newcastle Coal Measures.|||Sandstone.|
19437|Waratah Sandstone|68711|4|Described|p113, 117, 119, p116 Tbl 2, p114 Fig. 2|||Modified. Now considered to conformably underlie Newcastle Coal Measures. The change is because the top of the unit is much easier to recognise than its gradational base.||Previously part of Newcastle Coal Measures||Conformably underlies Lambton Formation, Newcastle Coal Measures. Has gradational base.||
19437|Waratah Sandstone|69683|6|Mentioned|p411 Fig.2, p415-416 Fig.3|Late Permian|Late Permian|||Unit in Singleton Supergroup.||||
19437|Waratah Sandstone|70647|5|Briefly described|Map Legend|Late Permian|Late Permian|Sydney Basin.||Newcastle Coal Measures|||Medium-grained lithic sandstone, mostly massive, well sorted; fine-grained in mid-section.|
19437|Waratah Sandstone|73304|6|Mentioned|p75|||Shown as underlying the Newcastle Coal Measures.||||||
19437|Waratah Sandstone|73625|6|Mentioned|p2|Permian|Permian|Newcastle coalfield, Sydney Basin.||||Overlies upper Tomago Coal Measures. Is overlain by Newcastle Coal Measures.||
19441|Warbisco Shale|22503|5|Briefly described|p645, Fig.3b|||?Late Ordovician||||||
19441|Warbisco Shale|22577|6|Mentioned|p120||Gisbornian|||||||
19441|Warbisco Shale|22624|5|Briefly described|p678, Fig.3 p679|Late Ordovician|Late Ordovician|See also p683||||||
19441|Warbisco Shale|22628|6|Mentioned|fig1p108|Ordovician|Ordovician|||||||
19441|Warbisco Shale|22679|6|Mentioned|p 7|||||||||
19441|Warbisco Shale|22691|6|Mentioned|P321|||||||||
19441|Warbisco Shale|22815|2|Defined|p18,24,123, fig10|Late Ordovician|Late Ordovician|||||||
19441|Warbisco Shale|22857|4|Described|p112, p422 App. 1, Tb. A1.5|Late Ordovician|Late Ordovician|Of the Bendoc Group. Well-laminated black to grey fissile shale with millimetre-scale bedding laminations. Max. thickness: 500m. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|22876|5|Briefly described|p16|Late Ordovician|Late Ordovician|Bendoc Group||||||
19441|Warbisco Shale|22878|5|Briefly described|p33|Ordovician|Ordovician|Bendoc Group||||||
19441|Warbisco Shale|22879|5|Briefly described|map|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black siliceous shale: rich in graptolites; minor white, quartz rich sandstone.||||||01-OCT-04
19441|Warbisco Shale|22880|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black siliceous shale: rich in graptolites; minor white, quartz rich sandstone.||||||01-OCT-04
19441|Warbisco Shale|22881|5|Briefly described|Map legend|Ordovician|Ordovician|||||||06-OCT-04
19441|Warbisco Shale|22968|5|Briefly described|P30||Ordovician|Parent is Bendoc Group||||||
19441|Warbisco Shale|22971|5|Briefly described|p 17|||||||||
19441|Warbisco Shale|23214|5|Briefly described|p170|Ordovician|Ordovician|||||||
19441|Warbisco Shale|23229|5|Briefly described|Table3-2p21|Bolindian|Gisbornian|||||||
19441|Warbisco Shale|23245|6|Mentioned|p112||Late Ordovician|||||||
19441|Warbisco Shale|23309|5|Briefly described|p58-60, 87, 97, Table 2.19||Late Ordovician|||||||
19441|Warbisco Shale|23454|5|Briefly described|p33|Ordovician|Ordovician|||||||
19441|Warbisco Shale|23615|3|Fully described|p68, p20 Fig.6|Bolindian|Gisbornian|Of Bendoc Group. Originally included rocks now known as Sunlight Creek Formation. Overlain by Akuna Mudstone, overlies Sunlight Creek Formation.||||||20-MAY-16
19441|Warbisco Shale|23860|5|Briefly described|p944|||Of Bendoc Group. Underlying unit Pinnak Sandstone.||||||
19441|Warbisco Shale|23938|6|Mentioned|p54 Tb. 4|Ordovician|Ordovician|See also p59-61 Figs. 21-22.||||||25-SEP-08
19441|Warbisco Shale|24004|5|Briefly described|p275 Fig.2|Ordovician|Ordovician|||||||
19441|Warbisco Shale|24037|4|Described|p427|Bolindian|Gisbornian|Of Bendoc Group. Geological Province: Lachlan Fold Belt||||||
19441|Warbisco Shale|24133|3|Fully described|p38|Ordovician|Ordovician|Of the Bendoc Group. Geological Province: Lachlan Fold Belt.||||||03-JUN-08
19441|Warbisco Shale|24142|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|24143|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|24144|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|24145|5|Briefly described|Map Legend|Ordovician|Ordovician|Of Bendoc Group. Geological Province: Lachlan Fold Belt||||||
19441|Warbisco Shale|24215|5|Briefly described|p804 Fig. 3|||Geological Province:  Lachlan Fold Belt||||||
19441|Warbisco Shale|24339|5|Briefly described|p50|Late Ordovician|Late Ordovician|Geological Province: Lachlan Fold Belt||||||
19441|Warbisco Shale|24551|4|Described|p106|Bolindian|Gisbornian|Of the Bendoc Group. Overlain by New Country Sandstone, overlies Sunlight Creek Formation.||||||
19441|Warbisco Shale|38151|6|Mentioned|Table 1|||||||||
19441|Warbisco Shale|40126|6|Mentioned|p14|||||||||
19441|Warbisco Shale|40127|6|Mentioned|p6|||||||||
19441|Warbisco Shale|40136|5|Briefly described|p43|||||||||
19441|Warbisco Shale|40761|6|Mentioned|p224|||||||||
19441|Warbisco Shale|41570|3|Fully described|p93|||||||||
19441|Warbisco Shale|41572|5|Briefly described|p21|||||||||
19441|Warbisco Shale|41585|6|Mentioned|p129|||||||||
19441|Warbisco Shale|41905|2|Defined|p20|Late Ordovician||||||||
19441|Warbisco Shale|41933|5|Briefly described|Map legend|Late Ordovician||||||||
19441|Warbisco Shale|42294|4|Described|p21|||||||||
19441|Warbisco Shale|42560|6|Mentioned|p54|||||||||
19441|Warbisco Shale|42627|5|Briefly described|Map legend|late Eastonian||||||||
19441|Warbisco Shale|42647|2|Defined|p19||Late Ordovician|||||||
19441|Warbisco Shale|42651|5|Briefly described|p266|||||||||
19441|Warbisco Shale|42827|4|Described|p92|||see also Table 4.1||||||
19441|Warbisco Shale|43206|5|Briefly described|map legend||Eastonian|of Bendoc Group||||||
19441|Warbisco Shale|43228|5|Briefly described|p9||Late Ordovician|of Bendoc Group||||||
19441|Warbisco Shale|43233|5|Briefly described|Map Legend|Bolindian|Gisbornian|of Bendoc Group.||||||
19441|Warbisco Shale|43312|5|Briefly described|Map Legend|Bolindian|Eastonian|of Bendoc Group.||||||
19441|Warbisco Shale|43313|5|Briefly described|Map Legend|Bolindian|Eastonian|||||||
19441|Warbisco Shale|43314|5|Briefly described|Map Legend|Bolindian|Gisbornian|of Bendoc Group.||||||
19441|Warbisco Shale|43315|5|Briefly described|Map Legend|Bolindian|Gisbornian|Of the Bendoc Group. Shale; black, siliceous, very rich in graptolites, minor quartzitic sandstone.||||||20-MAY-16
19441|Warbisco Shale|43782|6|Mentioned|Map Diagram|||||||||
19441|Warbisco Shale|44093|5|Briefly described|p56|Late Ordovician|Late Ordovician|See also p199 Tb. 1. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|50230|5|Briefly described|Map legend|Late Ordovician|Late Ordovician|Black, laminated carbonaceous shale, sometimes strongly foliated, minor quartzose sandstone.||||||
19441|Warbisco Shale|50231|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Of the Bendoc Group.||||||
19441|Warbisco Shale|50232|4|Described|Map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group.  Overlies the Adaminaby Group; overlies and interfingers with the Malay Creek Formation.  Strongly foliated black laminated carbonaceous shale.||||||
19441|Warbisco Shale|50233|5|Briefly described|Map Lagend|Bolindian|Gisbornian|Of the Bendoc Group.  Black, laminated carbonaceous shale, sometimes strongly foliated, minor quartzose sandstone.||||||13-MAY-04
19441|Warbisco Shale|50234|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|Of the Bendoc Group.  Strongly foliated black laminated carbonaceous shale.  Overlies: Bumballa Formation.  Underlies: Dignams Siltstone (Bendoc Group).||||||13-MAY-04
19441|Warbisco Shale|60417|6|Mentioned|p157|||||||||
19441|Warbisco Shale|60503|3|Fully described|p86-87, p29|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, siliceous black siltstone; minor interbedded quartzose sandstone; abundant graptolites. Conformably overlain by New Country Sandstone; conformably overlies Sunlight Creek Formation. Max. thickness: 500m.||||||16-NOV-09
19441|Warbisco Shale|60504|5|Briefly described|Map Legend|Bolindian|Gisbornian|Of the Bendoc Group. Black shale, minor quartzitic sandstone.||||||13-OCT-04
19441|Warbisco Shale|60505|5|Briefly described|Map legend|Bolindian|Gisbornian|Of the Bendoc Group. Black shale, minor quartzite sandstone.||||||
19441|Warbisco Shale|60506|5|Briefly described|Map legend|Bolindian|Gisbornian|Of the Bendoc Group. Black shale, minor quartzitic sandstone.||||||20-OCT-04
19441|Warbisco Shale|60507|5|Briefly described|Map Legend|Eastonian|Gisbornian|Of the Bendoc Group. Black shale, minor quartzite sandstone.||||||20-OCT-04
19441|Warbisco Shale|60541|3|Fully described|p53, p27|Late Ordovician|Late Ordovician|Of Bendoc Gp. Previously contained basal Sunlight Creek Mudst Mbr (upgraded to formation). Dominated by black shale, black siliceous shale and minor interbedded quartzose sst... Grades up out of Sunlight Cr Fm. Overlain by Akuna Mudstone. Max. thick:>400m||||||23-JUN-05
19441|Warbisco Shale|60542|3|Fully described|p47-48, p12|Bolindian|Gisbornian|Black shale, very siliceous siltstone, with very minor pale coloured quartzitic sandstone; shale has high silica content. Overlies Sunlight Creek Formation. Thickness: 200m in Hospital Creek Syncline.||||||
19441|Warbisco Shale|60902|5|Briefly described|p876|||Of the Bendoc Group. Geological Province: Girilambone-Wagga Terrane.||||||11-APR-06
19441|Warbisco Shale|60904|5|Briefly described|p782|Late Ordovician|Late Ordovician|Overlies Sunlight Creek Formation.||||||
19441|Warbisco Shale|60988|5|Briefly described|p144 Fig.1, |Late Ordovician|Late Ordovician|||||||
19441|Warbisco Shale|61160|5|Briefly described|p48|Late Ordovician|Late Ordovician|Of the Bendoc Group. Geological Province: Lachlan Fold Belt.||||||
19441|Warbisco Shale|61161|5|Briefly described|p82, p31, p76-77 Fig 6.1|Late Gisbornian|Late Gisbornian|Of Bendoc Group. Overlies Sunlight Creek Formation. Outcrops dominated by siliceous black shale, and interbedded quartzose sandstone and/or thin-bedded dark grey to black chert. Thickness: not known due to structural complexity. GSV map code: Obw.||||||
19441|Warbisco Shale|61163|4|Described|p81-82, p14 Fig. 3.2|Late Ordovician|Late Ordovician|Of the Bendoc Group. Overlies Sunlight Creek Formation; overlain by New Country Sandstone. Geological Province: Lachlan Fold Belt (Tabberabbera Zone). See also p38 Tb. 6.2.||||||
19441|Warbisco Shale|61169|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale: black, siliceous, very rich in graptolites; minor white quartzitic sandstone; deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61170|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale: black, siliceous, very rich in graptolites; minor white quartzitic sandstone; deep-marine hemipelagic deposits. GSV map code: Obw.||||||07-FEB-11
19441|Warbisco Shale|61171|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale: black, siliceous, very rich in graptolites; minor white quartzitic sandstone; deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61172|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Shale: black, siliceous, very rich in graptolites; minor white quartzitic sandstone; deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61173|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of Bendoc Group. Shale: insufficient gravity data to determine response; nonmagnetic (weakly to moderately magnetic background level, 70 nT); moderate K, Th and total radioelements, moderate to high U. GSV map code: Obw.||||||
19441|Warbisco Shale|61174|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, mudstone, minor siltstone, sandstone: abundant Eastonian graptolites. Deep-marine hemipelagic deposits. GSV map code: Obw.||||||07-FEB-11
19441|Warbisco Shale|61175|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, mudstone, minor siltstone, sandstone: abundant Eastonian graptolites. Deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61176|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, mudstone, minor siltstone, sandstone: abundant Eastonian graptolites. Deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61177|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of the Bendoc Group. Black shale, mudstone, minor siltstone, sandstone: abundant Eastonian graptolites. Deep-marine hemipelagic deposits. GSV map code: Obw.||||||
19441|Warbisco Shale|61178|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Of Bendoc Group. Black shale, mudstone, minor siltstone, sandstone (turbidite): nonmagnetic (5 nT; k up to 10 x10^-6 cgs); moderate gravity; very low radioelements except moderate U. GSV map code: Obw.||||||
19441|Warbisco Shale|61181|6|Mentioned|p16|||Has faulted contact with Amboyne Granodiorite.||||||
19441|Warbisco Shale|61187|5|Briefly described|p5 Fig.3. |Late Ordovician|Middle Ordovician|Benambra Terrane. Correlative of Bendoc Group, and Mount Easton Shale in the Melbourne Zone, Melbourne Terrane.||||||
19441|Warbisco Shale|61413|5|Briefly described|p7, p69, p82 Fig.103.|Late Ordovician|Late Ordovician||||||Graptolite-bearing black shale; imbricated along with Early Ordovician turbidites; locally silicified.|
19441|Warbisco Shale|61731|6|Mentioned|p1037|||||||||
19441|Warbisco Shale|61762|6|Mentioned|p18|||||||||
19441|Warbisco Shale|61964|5|Briefly described|p25 Fig. 8|Bolindian|Gisbornian|Of the Bendoc Group in Victoria - represented by Currawalla Shale in NSW.||||||
19441|Warbisco Shale|63290|5|Briefly described|p396 Fig. 3|Bolindian|Gisbornian|Of Bendoc Group. Underlain by Adaminaby Group and Sunlight Creek Formation, overlain by Akuna Formation and Gungoandra Siltstone.||||||
19441|Warbisco Shale|64238|5|Briefly described|Map legend|Ordovician|Ordovician|Of the Bendoc Group. Black, laminated to medium-bedded pyritic carbonaceous shale, commonly strongly foliated and folded; minor quartzose sandstone.||||||
19441|Warbisco Shale|66196|5|Briefly described|p618|||Thin-bedded sandstone and shales. Conformably overlies the Sunlight Creek Formation.||||||
19441|Warbisco Shale|67322|4|Described|p15-17, p19; Fig.5|Late Ordovician||VandenBerg et al. (1991). Age has been determined due to the presence of graptolites in the lower part of this Formation. Weathered black shales previously known informally as the Foxlow beds are now referred to as the Warbisco Shale (Glen, Dawson and Colquhoun 2007). Occurs in the Cooma-Mallacoota and Goulburn areas. Intercalated with Tidbinbilla Quartzite.||Of the Bendoc Group||Overlies the Sunlight Creek and Bumballa Formations. Overlain by the Akuna Mudstone, New Country Sandstone, and (conformably) the Dignams Siltstone. Gradationally overlies the Gungoandra Siltstone.|Dominantly black shales.|22-FEB-18
19441|Warbisco Shale|68116|5|Briefly described|Appendix, Maps 20, 27-28, 35-37, 45-46.|Hirnantian|Sandbian|Age written as Gisbornian to Bolindian in text.|||||Shale: black, siliceous, very rich in graptolites; minor white quartzitic sandstone which is up to ~2m thick.|
19441|Warbisco Shale|68466|6|Mentioned|p65-67|Late Ordovician|Late Ordovician|Albury-Bega Terrane.||||||
19441|Warbisco Shale|68592|2|Defined|p320-2, p324-6, p338-43, p349-50, p354|Late Ordovician|Late Ordovician|See also p116-8, p228, p230, p271-2, p275 Fig.57, p276-7, p288 Fig.60, p291-2, p298, p356, p358, p360, p363-4, p366-8, p419-20, p792, p802, p1676, p1864-5. Of Vandenberg et al.(1992) after Webby et al.(1981). Named after Warbisco Track, SW of Cabanandra. Mapped as Bubalahla Formation (Scheibner, 1973) and included in Abercrombie Beds (Packham, 1968) and Adaminaby Group (Stuart-Smith and Wallace, 1997; Raymond et al., 1998). A regional marker unit. Major ridge-forming lithology. Type section and representative sections detailed. Up to 500m thick. Abundant Gisbornian to earliest Bolindian graptolites described. Faulted against Joppa Siltstone Member and Kerrawary Siltstone. Is quarried in several places (eg Carrick Hill) as high quality road material. Elevated Ba possibly concentrated by accumulated plankton.||Unit in Bendoc Group.||Overlies Bumballa and Abercrombie Formations conformably; is conformably overlain by Mundoonen and Poidevins Sandstones  + Dignams Siltstone; is unconformably (angular) overlain by Woodlawn Volcanics.|Laminated to medium-bedded black siliceous shale, weathering to pale grey; commonly with well-developed bedding fissility and slaty cleavage; graptolites common; sporadic intercalations of fine- to medium-grained sandstone.|
19441|Warbisco Shale|68822|5|Briefly described|p324|Upper Ordovician|Upper Ordovician|Tabberabbera Zone.||||Underlain by the Pinnak Sandstone.||
19441|Warbisco Shale|69159|5|Briefly described|Map legend|Bolindian|Gisbornian|||Unit in Bendoc Group.||Overlies Bumballa Formation. Is overlain by Mundoonen Sandstone.|Black to grey, laminated to medium-bedded, pyritic, carbonaceous shale, commonly strongly foliated and folded; minor quartzose sandstone.|07-SEP-15
19441|Warbisco Shale|69668|6|Mentioned|p929 Fig.2|Late Ordovician|Late Ordovician|Cooma-Bega and Goulburn-Braidwood areas, Albury-Bega terrane.||||Overlies Chakola or Bumballa Formations. Is overlain by Akuna Mudstone or Dignams Siltstone.||
19441|Warbisco Shale|70192|5|Briefly described|Map Legend|Bolindian|Gisbornian|[Theta]bw. On Boorowa, Crookwell, Taralga, Yass, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Bendoc Group|Includes one unnamed unit.|Overlies Nattery Chert Member and Abercrombie Fm. Overlies (and interfingers with?) Bumballa Formation. Is overlain by Poidevins Sst, Mundoonen Sst, Dignams Siltst (Margules Group).|Black, laminated to medium bedded, siliceous, carbonaceous, graptolitic shale, commonly strongly cleaved and folded; minor quartzose sandstone.|06-SEP-16
19441|Warbisco Shale|70297|5|Briefly described|map legend|Ordovician|Ordovician|||Bendoc Group||||
19441|Warbisco Shale|70540|5|Briefly described|Map Legend|Ordovician|Ordovician|||Bendoc Group|||Laminated-medium bedded, siliceous, carbonaceous, graptolitic shale; commonly strongly cleaved and folded. Minor quartzose sandstone is present.|
19441|Warbisco Shale|70541|5|Briefly described|Map Legend|Ordovician|Ordovician|||Bendoc Group|||Black, laminated to medium-bedded, siliceous, carbonaceous, graptolitic shale, commonly strongly cleaved and folded with some minor quartzose sandstone.|
19441|Warbisco Shale|70542|5|Briefly described|Map Legend|Late Ordovician|Late Ordovician|||Bendoc Group|||Black,laminated to medium-bedded, siliceous, carbonaceous, graptolitic shale, commonly strongly cleaved and folded with some minor quartzose sandstone.|
19441|Warbisco Shale|70543|5|Briefly described|Map Legend|Ordovician|Ordovician|||Bendoc Group|||Black, laminated to medium bedded, siliceous, carbonaceous, graptolitic shale, commonly strongly cleaved and folded; minor quartzose sandstone.|
19441|Warbisco Shale|70544|5|Briefly described|Map Legend|Ordovician|Ordovician|||Bendoc Group|||Laminated-medium bedded, siliceous, carbonaceous, graptolitic shale; commonly strongly cleaved and folded with minor quartzose sandstone.|
19441|Warbisco Shale|70545|5|Briefly described|Map Legend|Ordovician|Ordovician|Includes one unnamed subunit of medium-thickly bedded, fine-medium grained quartzose sandstone with carbonaceous shale mud chips; interbedded with carbonaceous shale.||Bendoc Group|Includes one unnamed subunit.||Black, laminated to medium bedded, siliceous, carbonaceous, graptolitic shale; commonly strongly cleaved and folded; minor quartzose sandstone present.|
19441|Warbisco Shale|70601|4|Described|p27, p43, p45, p48, p50-51, p54|Bolindian|Gisbornian|Albury-Bega Basin: Inland Zone. Widespread: Howqua River to Bermagui. Could be laterally transitional to upper part of Wagonga Chert.|ca 453-447Ma|Bendoc Group.||Underlies Bogolo Formation and Akuna Mudstone. Overlies Chakola Formation (Adaminaby Group) transitionally.|Anoxic fine-grained clastic black shale (graptolites), cherts, minor very fine turbidites.|
19441|Warbisco Shale|70661|3|Fully described|p19, p20 fig 3, p25, p26|Late Ordovician (Bolindian)|Late Ordovician (Eastonian)|Name derived from Warbisco track, synonymous with parts of the Tallong beds and Triangle Group. Up to 500m thick. Graptolite fossils common. Low K, U and high Th signiature. Low to highly magnetic. Average density of 2.64 g/cm3. little geochemical data. Widespread distribution over NSW, best exposures in shoal haven river and tributary creeks. Type section in Eastern Victoria.||Bendoc Group||Conformably overlies Bumballa Formation|Micaceous, organic rich black siliceous shale with well developed bedding fissility and slaty cleavage, siliceous mudstone and some sandstone turbidites. Sandstones are compositionally mature but commonly poorly sorted fine-medium grained.|
19441|Warbisco Shale|71069|2|Defined|p21 fig 7, p22, p39 fig 16|Bolindian|Gisbornian|Named for the Warbisco Track in Victoria. Rocks belonging to this unit have variously been mapped as Railway Shale, Bollongong Shale Member, Bubalahla Formation, Abercrombie Beds, Merrigan Black Shale or Acton Shale Member.Type section given, located at GR 734463 5887004 to 734913 5887684; numerous reference sections also mentioned. Contains abundant Gisbornian to Bolindian graptolite fossils which are the basis for age determinations of this unit. Thickness estimated to range from 400-500m. Generally forms major ridges in the Lachlan Orogen. Deposited in a deep marine setting characterised by hemipelagic sedimentation with periodic influx of terrigenous material.   Is quarried for high quality road material. Distribution, primary structure/textures, tectonic structure, geochemistry, metamorphism and fossil assemblage discussed in detail. Conformably overlain by the Mundoonen Sandstone, Dignams Siltstone, New Country Sandstone or the Akuna Mudstone.  See also  p40 fig 17, p51, p53 fig 19, p55 fig 20, p59, p66, p71, p73 fig 26, p74, p75, p76 fig 27, p77, p79-p83 ph 16, p84-88, p95, p106, p170.||Bendoc Group||Conformably overlies the Nattery Chert Member, Glen Fergus Member and the Bumballa Formation. Overlies the Adaminaby Group and the Sunlight Creek Formation.|Black to grey, laminated to medium-bedded, pyritic, carbonaceous or siliceous shales with rare lenses of ,medium-thickly bedded, poorly sorted, fine to medium grained, quartzose sandstone.|
19441|Warbisco Shale|71303|5|Briefly described|map legend|Katian|Sandbian|||Of Bendoc Group.|||Black laminated siltstone and mudstone and minor chert; interbedded with grey to cream, cross-laminated fine- to coarse-grained quartzose sandstone.|
19441|Warbisco Shale|71656|4|Described|p12 Fig.2, p15-16|Bolindian|Gisbornian|Includes Late Ordovician graptolites, conodonts.||Bendoc Group||Bendoc Group. Overlies Bumballa Formation, Abercrombie Formation and underlies Mundoonen Sandstone.|Siliceous shales.|
19441|Warbisco Shale|71691|5|Briefly described|Map legend.|Ordovician|Ordovician|||Bendoc Group.||Overlies Bumballa Formation. Is overlain by Mundoonen Sandstone (Margules Group).|Black to grey, laminated to medium-bedded, pyritic, carbonaceous shale, commonly strongly foliated and folded; minor quartzose sandstone.|
19441|Warbisco Shale|71699|5|Briefly described|Map legend.|Ordovician|Ordovician|||Bendoc Group.||Overlies Bumballa Formation and Abercrombie Formation.|Black to grey, laminated to medium-bedded, pyritic, carbonaceous shale; commonly strongly foliated and folded; minor quartzose sandstone.|
19441|Warbisco Shale|71700|2|Defined|vi, viii, p7, p9-p10, CD|Bolindian|Gisbornian|Lachlan Orogen. Named for the Warbisco Track, southwest of Cabanandra. The type section is along Mountain Creek in eastern Victoria from GR 734463 5887004 to GR 734913 5887684. A representative section is also provided.This unit was first mapped as Bubalahla Formation by Scheibner 1973a, 1973b. In Bathurst250 this unit was included in the "Abercrombie Beds" by Packham (1968). In Goulburn100 this unit was included in undifferntiated Ordovician (Brunker and Offenberg, 1970). Contains two unnamed members. Thickness ranges from 120m to approximately 900m thick in different areas. Distribution, geomorphic expression, outcrop, metamorphism, geochemistry, geophysical characteristics, fossil assemblage, age evidence, distinguishing features, economic geology and depositional environment are discussed. Overlain by a newly recognised unnamed limestone member that may be Silurian. Age derived from graptolite fauna. Conformably overlain by the Mundoonen Sandstone of the Margules Group. Unconformably overlain by the Mount Fairy Group. Equivalent to the Acton Shale Member. See also p39, p48, p50, p64, p82.||Bendoc Group||Overlies the Bumballa Formation and the Adaminaby Group. Conformably overlies the Nattery Chert Member of the Abercrombie Formation.|Black shale with minor lenses of quartzose sandstone; marl and impure unfossiliferous limestone.|
19441|Warbisco Shale|72528|5|Briefly described|p11, p108.|Hirnantian|Sandbian|Age given as Bolindian and Gisbornian [equivalent to Sandbian to Hirnantian]. This unit hosts the Paupong gold prospect south of Jindabyne, the new date of 430.9+/-2.1 Ma for the porphyry dyke establishes a mid-Silurian age for the dyke-swarm associated with Cu-Au mineralisation.||||||
19441|Warbisco Shale|73140|5|Briefly described|p495 Fig.1, Fig.6|Bolindian|Gisbornian|Age based on graptolites.||Bendoc Group||Overlies Sunlight Creek, Bumballa and Abercrombie formations, underlies Mundoonen Sandstone, Dignams Siltstone, Poidevins Sandstone, Akuna Mudstone, New Country Sandstone, Gungoandra Siltstone||
19456|Wards River Conglomerate|22857|4|Described|p534 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures). Conglomerate, sandstone; minor siltstone interbeds, shale and rare carbonaceous shale and coal. Max. thickness: ~20m. Geological Province: Sydney Basin.||||||
19456|Wards River Conglomerate|23623|5|Briefly described|p33 Fig. 2|Late Permian|Late Permian|Parent: Craven Subgroup.    Geological Province: New England Fold Belt||||||
19456|Wards River Conglomerate|34556|5|Briefly described|p267|||Permian||||||
19456|Wards River Conglomerate|37099|5|Briefly described|p257|||||||||
19456|Wards River Conglomerate|40872|6|Mentioned|Fig.2|||||||||
19456|Wards River Conglomerate|40883|6|Mentioned|p9|||||||||
19456|Wards River Conglomerate|41054|6|Mentioned|Fig.2|||||||||
19456|Wards River Conglomerate|44244|4|Described|p183, p167|Late Permian|Late Permian|Originally of Louhgan (1955). Conformably underlies the Jilleon Formation.  Max. thickness: 67m.  Type section in text.  Geological Province: Myall Block.||||||16-SEP-04
19456|Wards River Conglomerate|50147|5|Briefly described|Map legend|Late Permian|Late Permian|Of the Craven Subgroup (Gloucester Coal Measures).  Geological Province: Western Myall Block.||||||
19462|Warina Sand|2967|5|Briefly described|p14, p15 Fig.2.2, p17, 20, 77, 336|||Lawrence (1975). This unit is the basal regional aquifer in the Murray Basin. Lower Tertiary.||Renmark Group.||Is overlain by Olney Formation.|Medium- to coarse-grained quartz sand, sparingly carbonaceous and pyritic. Lesser gravel, ligneous clays and silts, minor lignites.|
19462|Warina Sand|10010|5|Briefly described|p12 Fig. 3|Early Eocene|Late Paleocene|Of the Renmark Group. Geological Province: Murray Basin.||||||13-AUG-07
19462|Warina Sand|22495|6|Mentioned|P222|||||||||
19462|Warina Sand|22587|6|Mentioned|p79 Fig.7|Middle Eocene|Middle Eocene|||||||
19462|Warina Sand|22712|5|Briefly described|p132|Tertiary|Tertiary|Of the Renmark Group.||||||15-JAN-09
19462|Warina Sand|22773|5|Briefly described|p351,Fig24.8p352|Early Eocene|Late Paleocene|||||||
19462|Warina Sand|22799|3|Fully described|p27|Middle Eocene|Early Eocene|||||||
19462|Warina Sand|22857|5|Briefly described|p351, p352 Fig. 24.8|Eocene|Late Paleocene|Basal unit of the Renmark Group. Overlain by Olney Formation. Age: ~60Ma. Max. thickness: ~200m. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
19462|Warina Sand|22887|5|Briefly described|Fig.6|Early Eocene|Late Paleocene|||||||
19462|Warina Sand|22893|5|Briefly described|fig4 p9|||||||||
19462|Warina Sand|23884|5|Briefly described|p153, p155 Fig. 13.2|Early Eocene|Late Paleozoic|Geological Province: Murray Basin. Age: ~60 Ma. Of the Renmark Group.||||||07-NOV-08
19462|Warina Sand|24105|5|Briefly described|p155|Eocene|Paleocene|Geological Province: Murray Basin. Overlying Unit: Olney Formation.||||||
19462|Warina Sand|24177|5|Briefly described|p69, p70|Paleogene|Paleogene|Of the Renmark Group. Overlain by Olney Formation. Age: <65 Ma. Geological Province: Murray Basin.||||||07-NOV-08
19462|Warina Sand|24551|6|Mentioned|p320, 421, 731 Table 17.1|||Of the Renmark Group. Maximum Thickness: 200m.||||||
19462|Warina Sand|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19462|Warina Sand|30934|6|Mentioned|Map legend|Eocene|Eocene|||||||
19462|Warina Sand|31741|6|Mentioned|p6|||||||||
19462|Warina Sand|31745|6|Mentioned|Map legend|Eocene|Eocene|||||||
19462|Warina Sand|31746|4|Described|p193|||||||||
19462|Warina Sand|34757|6|Mentioned|p45|||||||||
19462|Warina Sand|34813|5|Briefly described|p63|||Mention on P62 also.||||||
19462|Warina Sand|37809|6|Mentioned|Fig.7|||||||||
19462|Warina Sand|37873|6|Mentioned|p1|||||||||
19462|Warina Sand|38601|5|Briefly described|p7|||||||||
19462|Warina Sand|39329|6|Mentioned|Fig.1|||||||||
19462|Warina Sand|39929|6|Mentioned|p269|||||||||
19462|Warina Sand|41136|5|Briefly described|p215|||||||||
19462|Warina Sand|41868|5|Briefly described|p551|||||||||
19462|Warina Sand|42125|5|Briefly described|p132|||See also p139.||||||15-JAN-09
19462|Warina Sand|42126|6|Mentioned|p156, p149|||||||||
19462|Warina Sand|42130|6|Mentioned|Fig.3 p265|||||||||03-DEC-13
19462|Warina Sand|42133|6|Mentioned|p302|||||||||
19462|Warina Sand|42137|6|Mentioned|Fig.2 P368|||||||||
19462|Warina Sand|42138|6|Mentioned|p389|||||||||
19462|Warina Sand|42184|6|Mentioned|Fig.2 P348|||||||||
19462|Warina Sand|42720|6|Mentioned|map legend|Oligocene|Paleocene|||||||
19462|Warina Sand|42813|6|Mentioned|p24|||||||||
19462|Warina Sand|42827|5|Briefly described|p267|||Of Renmark Group.||||||27-OCT-08
19462|Warina Sand|42881|4|Described|Fig.3, P84|||||||||
19462|Warina Sand|42966|2|Defined|p97|Eocene|Paleocene|Of Renmark Group.||||||13-AUG-07
19462|Warina Sand|43052|5|Briefly described|Table 2.1|||||||||
19462|Warina Sand|43218|4|Described|Fig.3,p22||Tertiary|Of the Renmark Group.||||||27-OCT-08
19462|Warina Sand|43780|5|Briefly described|p6|Eocene|Paleocene|||||||
19462|Warina Sand|43791|6|Mentioned|p372, Fig1|||||||||
19462|Warina Sand|43804|6|Mentioned|Fig.2,p49|||||||||
19462|Warina Sand|44093|5|Briefly described|p145 App. 1|Tertiary|Tertiary|Geological Province: Kanmantoo Fold Belt.||||||
19462|Warina Sand|44133|5|Briefly described|p158, 152 Fig. 10.2|Middle Eocene|Late Paleocene|Of the Renmark Group. Geological Province: Murray Basin.||||||
19462|Warina Sand|44191|5|Briefly described|Map Legend|Early Eocene|Paleocene|||||||
19462|Warina Sand|49038|4|Described|Table 2|||Briefly described P24.||||||27-OCT-08
19462|Warina Sand|49040|6|Mentioned|p10|||||||||
19462|Warina Sand|50154|5|Briefly described|p132|||Of the Renmark Group. Overlain by the Olney Formation. Geological Province: Murray Basin.||||||
19462|Warina Sand|60451|5|Briefly described|p95 Fig. 61|||||||||
19462|Warina Sand|60452|5|Briefly described|p14, 33|Eocene|Paleocene|Fluvial deposits at the base of the Renmark Group. Formerly referred to as the 'lower' Renmark Beds (Harris, 1966).||||||
19462|Warina Sand|60491|4|Described|p15|Oligocene|Paleocene|Of the Renmark Group. Overlain by the Olney Formation.||||||
19462|Warina Sand|60599|5|Briefly described|p84|Late Paleocene|Late paleocene|Same unit as Warina Formation - names used interchangeably, but probably supersedes Warina Formation? At base of Renmark Group. Fluvial sediments. Geological Province:Murray Basin.||||||07-NOV-08
19462|Warina Sand|61155|5|Briefly described|p2, p18|Early Eocene|Late Paleocene|Of the Renmark Group. Sediments spread in thin sheets over large areas of the Murray Basin. Overlaid by the Olney Formation. Max. thickness: 200m. Age: >62-52Ma. Geological Province: Murray Basin.||||||
19462|Warina Sand|61185|5|Briefly described|p57|Late Paleocene|Middle Paleocene|Base of Renmark Group. Equivalent to White Hills Gravel and Wangerrip Group. Fluvial sediments. Geological Province: Murray Basin. See Warina Formation.||||||07-FEB-11
19462|Warina Sand|61314|6|Mentioned|p129|||Correlates with Renmark beds.||||||
19462|Warina Sand|63887|5|Briefly described|p20, p21 Fig. 1|Early Oligocene|Paleocene|Of Renmark Group. Floodplain and swamp environments dominates, resulting in deposition of carbonaceous sand, clay and silt.||||||
19462|Warina Sand|65552|5|Briefly described|p5 Fig.3, p6|Early Eocene|Late Palaeocene|Of Renmark Group. Fluvial unit of the Murray Basin. Unconformably overlies basement, underlies Olney Formation. c.60 Ma.||||||
19462|Warina Sand|66286|5|Briefly described|p179.|||||Unit in Renmark Group.||Is overlain by Olney Formation.|Poorly consolidated fluvial sands.|
19462|Warina Sand|67462|5|Briefly described|Map legend.|Paleogene|Paleogene|Murray Basin.||Unit in Renmark Group.||||
19462|Warina Sand|68189|5|Briefly described|p25, p26, p27 Tb.3.2|Eocene|Eocene|Braided plain system.||Basal unit of the Renmark Group.||||
19462|Warina Sand|68194|5|Briefly described|p23|||||Unit in Renmark Group.||Is overlain by Olney Formation.|Quartzose sandstone.|
19462|Warina Sand|68715|5|Briefly described|p31 Fig.5|Bartonian|Ypresian|Murray Basin.||Of the Renmark Group.||||
19462|Warina Sand|70718|6|Mentioned|p24|||Oldest sedimentation in the Murray Basin. Fluvial.|~60 Ma|Renmark Group||||30-MAY-19
19462|Warina Sand|71593|5|Briefly described|p52, p54|||||Renmark Group|||Quite pale and clean quartzose pebbly sand.|
19462|Warina Sand|72445|5|Briefly described|App.1, App.7 p5, p7, p8, p16, p20-21.|Paleocene|Paleocene|Characterised by the organic-poor nature of the sands that are a major component of this formation. Said to be non-marine. Suggested (App7 p20) to be equivalent to old 'Lower Renmark Beds'.||Renmark Group||Shown as underlying Olney Formation (sharp contact).|Fine- to coarse grained sand with lignitic fragments , muddy silt with lignite, silty clay and white vein quartz pebbles.|15-OCT-20
19462|Warina Sand|73118|5|Briefly described|p45, 53, 83|Eocene|Paleocene|Glenelg Zone, Western Victoria. Drill core summary log. Entirely concealed. 200m thick. Fluvial deposits.||Renmark Group.||Is overlain by Olney Formation.|Loose to friable grey, brown, poorly to well sorted, medium to coarse sand with minor intercalated fine sand, silt, clay, carbonaceous clay.|
19462|Warina Sand|73228|4|Described|p50-51, p53-57, p60|Early Oligocene|Late Paleocene|Murray Basin. Poorly consolidated fluvial sand. Sandy facies interpreted as a fluvial, braided-channel deposit and the finer grained interbeds as lacustrine and floodplain deposits. Floodplain and swamp sediments also with fluvial and lacustrine depositional environments. Identified in Nadda 1 drillhole. Restricted to deeper parts of the basin.||Renmark Group||Underlain by Coombool Member (Monash Formation). Overlain by Olney Formation.|Pale grey to pale brown medium- to coarse-grained quartz sand with minor thin, lenticular interbeds of locally carbonaceous silt and clay.|
19462|Warina Sand|73229|6|Mentioned|p67|Early Oligocene|Late Paleocene|Murray Basin.||Renmark Group||||
19498|Warratra Mudstone|22529|6|Mentioned|4 fig 2|Emsian|Emsian|Parent Queens Pinch Group. Overlying unit Sutchers Creek Formation, underlying unit Taylors Hill Formation||||||
19498|Warratra Mudstone|22590|6|Mentioned|Fig3 P754||Emsian|Actually spelt Warratra Mdst.||||||
19498|Warratra Mudstone|22857|4|Described|p476 App.1 Tb.A1.6|Emsian|Pragian|Of the Queens Pinch Group. Grey mudstone. Max. thickness: 120m. Geological Province: Capertee Rise.||||||
19498|Warratra Mudstone|23043|5|Briefly described|Map Legend|Emsian|Emsian|of Queens Pinch Group.||||||
19498|Warratra Mudstone|23170|2|Defined|p148|Emsian|Pragian|of Queens Pinch Group.||||||
19498|Warratra Mudstone|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
19498|Warratra Mudstone|32045|6|Mentioned|Map legend|Devonian|Devonian|||||||
19498|Warratra Mudstone|32485|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower - Middle Devonian||||||
19498|Warratra Mudstone|33326|6|Mentioned|p434|||Fauna.||||||
19498|Warratra Mudstone|42033|6|Mentioned|p654|||||||||
19498|Warratra Mudstone|42051|5|Briefly described|p143|||||||||
19498|Warratra Mudstone|43188|4|Described|p216,Table 4 p212|Emsian|Pragian|Age latest Pragian to earliest Emsian. Reverts to Wright's definition, not McCracken (1990).||||||
19498|Warratra Mudstone|43476|14|Not recorded|Map Legend||Middle Devonian|(Provisional Edition)||||||
19501|Warrawong Rhyolite Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Majuba Volcanics (Kopyje Group, Cobar Supergroup). Geological Province: Kopyje Shelf (Darling Basin).||||||
19501|Warrawong Rhyolite Member|42566|3|Fully described|p84|||||||||
19501|Warrawong Rhyolite Member|42568|5|Briefly described|Map legend|Pragian|Pragian|Reserved as Warrawong.||||||
19525|Warri Granite|42726|5|Briefly described|map legend|Early Devonian||Of the Watch Box Suite (Candelo Supersuite).  Not intended as a formal name.||||||09-FEB-05
19527|Warrie Basalt|40166|6|Mentioned|p343|||||||||
19530|Warrigundi Igneous Complex|22580|6|Mentioned|p97|Early Permian|Late Carboniferous|||||||
19530|Warrigundi Igneous Complex|22857|6|Mentioned|p258|||||||||
19530|Warrigundi Igneous Complex|22864|6|Mentioned|p258|||||||||
19530|Warrigundi Igneous Complex|23102|5|Briefly described|p562||Early Permian|||||||
19530|Warrigundi Igneous Complex|42780|5|Briefly described|p413|||see also Fig.1 P410, P419||||||
19530|Warrigundi Igneous Complex|44093|5|Briefly described|p227 App. 1|Early Permian|Early Permian|Geological Province: Lachlan Fold Belt.||||||
19530|Warrigundi Igneous Complex|61201|4|Described|p2, 5 Table 1, 6-7|Early Permian|Early Permian|Geological Province: Werrie Basin. Max. Thickness: 1500m+. Quartz dolerite, keratophyre, andesites, dacites, rhyolites. Interbedded with Werrie Basalt.||||||17-SEP-08
19530|Warrigundi Igneous Complex|61776|5|Briefly described|p196|Early Permian|Early Permian|Geological Province: Werrie Basin. Andesite, dacite, rhyolite, quartz diorite and monzonite.||||||
19530|Warrigundi Igneous Complex|61801|5|Briefly described|p403 Fig.1, p404|Permian|Permian|Intrusives and extrusives.||||||
19530|Warrigundi Igneous Complex|65114|5|Briefly described|p395|Gzhelian||Considered to be the volcanic centres for the Werrie Basalt; zircons from weathered material considered equivalent to the Warrigundi Igneous Complex have Pb/U age of 300 +/- 8 Ma||||||
19530|Warrigundi Igneous Complex|68003|5|Briefly described|p38 Fig.3-j, p130.|Early Permian|Early Permian|Werrie Basin (North), Brigalow Belt South Bioregion. Name shortened to Warrigundi Complex on p38.||||Is overlain by Willow Tree Formation.|Diorite, pyroxene andesite, dacite, rhyolite flows and dykes.|
19530|Warrigundi Igneous Complex|68004|5|Briefly described|p117.|Late Permian|Late Permian|Hosts the Mount Terrible epithermal gold-silver deposit with inferred resource of 132,000 t at 7.8 ppm Au. See also reference to Warrigundi Volcanic Complex p212.||||||
19530|Warrigundi Igneous Complex|68006|6|Mentioned|pp137-138.|Permian|Permian|Hosts the Mount Terrible epithermal gold-silver deposit.||||||
19530|Warrigundi Igneous Complex|71115|6|Mentioned|p192|Permian|Permian|New England Orogen. Interpreted volcanic centre.|269.4 +/- 4.6 Ma (Rb/Sr; Flood et al., 1988).|||||
19554|Wasp Head Formation|22591|4|Described|p 62, Fig 4|||||||||
19554|Wasp Head Formation|22663|5|Briefly described|NSW97 -1 Fig.2|Early Permian|Early Permian|||||||01-MAR-10
19554|Wasp Head Formation|22857|5|Briefly described|p504 App.1 Tb.A1.8|Sakmarian|Sakmarian|Fine- to medium-grained sandstone, four megabreccia units (up to 4m); contains brachiopods, bivalves, spores. Max. thickness: >90m. Geological Province: Kanimblan Highlands.||||||
19554|Wasp Head Formation|22969|4|Described|p 17, Fig 2.2||Early Permian|||||||
19554|Wasp Head Formation|23544|5|Briefly described|Fig 2 p358|||Of the Talaterang Group in the Sydney Basin.||||||
19554|Wasp Head Formation|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Of Conjola Sub-Group. Geological Province: Sydney Basin.||||||
19554|Wasp Head Formation|24240|5|Briefly described|p21|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
19554|Wasp Head Formation|24552|4|Described|p5 Fig.2|Sakmarian|Sakmarian|Marine breccia fining up to fine sandstone. Contains abundant brachiopods. Overlain by Pebbley Beach Formation. Unconformably overlies Ordovician shale and chert. Thcikness: ~80 m. Of Talaterang Group. Geological Province: Southern Sydney Basin.||||||07-FEB-11
19554|Wasp Head Formation|29752|6|Mentioned|p5|||||||||
19554|Wasp Head Formation|31081|2|Defined|p56|Sakmarian|Sakmarian|See also p57-58.||||||23-AUG-07
19554|Wasp Head Formation|31128|6|Mentioned|Table 1|||||||||
19554|Wasp Head Formation|31298|6|Mentioned|p16|||||||||
19554|Wasp Head Formation|32084|6|Mentioned|p466|||||||||
19554|Wasp Head Formation|32094|6|Mentioned|p382|||||||||
19554|Wasp Head Formation|32769|6|Mentioned|Fig.1|||||||||
19554|Wasp Head Formation|32945|6|Mentioned|p84|||See also PP86,87. Conjola Subgp. Permian||||||
19554|Wasp Head Formation|34845|6|Mentioned|Fig.4|||||||||
19554|Wasp Head Formation|35284|6|Mentioned|Fig.1|||||||||
19554|Wasp Head Formation|35862|6|Mentioned|p276|||||||||
19554|Wasp Head Formation|36042|6|Mentioned|Table 1|||||||||
19554|Wasp Head Formation|36534|6|Mentioned|p223|||||||||
19554|Wasp Head Formation|37082|6|Mentioned|p161|||||||||
19554|Wasp Head Formation|37092|6|Mentioned|Table 2|||||||||
19554|Wasp Head Formation|38204|6|Mentioned|p79|||||||||
19554|Wasp Head Formation|38690|6|Mentioned|Fig.2|||||||||
19554|Wasp Head Formation|39262|6|Mentioned|p122|||||||||
19554|Wasp Head Formation|39287|6|Mentioned|p20|||||||||
19554|Wasp Head Formation|39289|6|Mentioned|Fig. 4.2|||Stratigraphic section mention P75||||||
19554|Wasp Head Formation|39290|6|Mentioned|p92|||||||||
19554|Wasp Head Formation|39299|6|Mentioned|p288|||||||||
19554|Wasp Head Formation|39304|6|Mentioned|Photo 19.1|||||||||
19554|Wasp Head Formation|39305|5|Briefly described|p377|||Marine invertebrates||||||
19554|Wasp Head Formation|39307|6|Mentioned|Table 22.1|||||||||
19554|Wasp Head Formation|39833|6|Mentioned|p298|||||||||
19554|Wasp Head Formation|40166|6|Mentioned|Table 1|||||||||
19554|Wasp Head Formation|41315|6|Mentioned|p148|||||||||
19554|Wasp Head Formation|41580|6|Mentioned|Table 1|||||||||
19554|Wasp Head Formation|41832|6|Mentioned|Fig.2|||||||||
19554|Wasp Head Formation|42925|5|Briefly described|Table 18||Early Permian|||||||
19554|Wasp Head Formation|42974|6|Mentioned|Fig.2,p192|||Of Shoalhaven Group.||||||12-MAR-09
19554|Wasp Head Formation|43194|5|Briefly described|p128, p129 Tb. 8.3|Early Permian|Early Permian|Marine formation at the base of the Conjola Subgroup, Shoalhaven Group, southern Sydney Basin.||||||
19554|Wasp Head Formation|45090|6|Mentioned|p7|||Time correlation chart||||||
19554|Wasp Head Formation|49644|5|Briefly described|Table|||||||||
19554|Wasp Head Formation|60281|5|Briefly described|p8, p55|Early Permian|Early Permian|Of Talaterang Group. Type section dominated by fine- to medium-grained sandstone and breccia units - poorly sorted, internally chaotic and surrounded by a silt-rich matrix. Unconformably overlies Wagonga Beds; overlain by Pebbley Beach Fm. Age: 290-286Ma.||||||27-APR-05
19554|Wasp Head Formation|60285|4|Described|p181|Sakmarian|Sakmarian|Of Talaterang Group. Overlain by Pebbley Beach Formation. Shallow marine. Geological Province: Sydney Basin.||||||31-JAN-17
19554|Wasp Head Formation|60292|5|Briefly described|p98|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||
19554|Wasp Head Formation|60296|5|Briefly described|p156 Fig.1|Sakmarian|Asselian|Correlated with Beckers Formation, Lochinvar Formation, Woody Island Formation and Quamby Formation. Geological Province: Sydney Basin.||||||31-JAN-17
19554|Wasp Head Formation|61315|5|Briefly described|Table SY2|Early Permian|Early Permian|Of the Conjola Subgroup (Shoalhaven Group). Geological Province: Sydney Basin||||||
19554|Wasp Head Formation|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Conjola Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
19554|Wasp Head Formation|61612|6|Mentioned|p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||12-MAR-09
19554|Wasp Head Formation|62043|6|Mentioned|p438 Fig.2. |Sakmarian|Sakmarian|Southern Sydney Basin.||Unit in Talaterang Group.||||
19554|Wasp Head Formation|63461|5|Briefly described|p862|Permian|Permian|Of the Talaterang Group. Geological Province: Sydney Basin.||||||31-JAN-17
19554|Wasp Head Formation|63773|5|Briefly described|p1058 Fig. 2, p1069|Early Permian|Early Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-APR-09
19554|Wasp Head Formation|63832|5|Briefly described|p131 fig 2, p135-136|Sakmarian|Sakmarian|Gostin and Herbert (1973); Rygel et al. (1978). Of southern Sydney Basin. Fifth (P1) glaciation. Facies juxtapositions record relative sea-level shifts of the P1 to P2 interglacial interval.||||Is overlain by Pebbley Beach Formation.||14-DEC-17
19554|Wasp Head Formation|64631|5|Briefly described|p44 Fig.2, pp48-50, p54.|Sakmarian|Asselian|SE Sydney Basin. Contains record of glaciation. Biostratigraphic age control at base and top.||||Is overlain by Pebbley Beach Formation of the Shoalhaven Group.||
19554|Wasp Head Formation|64877|5|Briefly described|p293, p295-296, p314|Permian|Permian|Southern Sydney Basin. Shallow-marine deposits. Trace fossils described and illustrated.||Talaterang Group.||Correlative of Clyde Coal Measures.||
19554|Wasp Head Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Talaterang Group.||Overlain by Shoalhaven Group.||
19554|Wasp Head Formation|67663|5|Briefly described|p518, p520 Tb.1|Permian|Permian|Early Permian. Southern Sydney Basin.||||Unconformably overlain by the Shoalhaven Group. Unconformably overlies Talaterang Group conglomerates..|Beach and near shore sands.|13-AUG-15
19554|Wasp Head Formation|68003|5|Briefly described|p40.|Early Permian|Early Permian|This article cites Tye et al. (1996) for including it (and, similarly, the Pigeon House Creek Siltstone) in the Talaterang Group.||Unit in Talaterang Group.||||
19554|Wasp Head Formation|68592|6|Mentioned|p1779|Permian|Permian|||Unit in Talaterang Group.||||
19554|Wasp Head Formation|69297|6|Mentioned|p501, p502 fig 5.43|Artinskian|Artinskian|Sydney Basin.||||Interfingers with the Clyde Coal Measures. Overlain by the Pebbly Beach Formation and the Yadboro or Tallong Conglomerates.||
19554|Wasp Head Formation|70096|5|Briefly described|p220-221;Supp4|||Of southern Sydney Basin. Deposited under interglacial conditions (Rygel et al., 2008; see supplementary information). See also supplementary files in appendix for additional stratigraphic and locality information.||||Overlain by Pebbley Beach Formation.||
19554|Wasp Head Formation|70601|6|Mentioned|p28|||One of the basal formations of the Sydney Basin.||||||
19554|Wasp Head Formation|70661|6|Mentioned|p145|Early Permian|Early Permian|||Talaterang Group||Possibly correlates with Tallong Conglomerate.||
19554|Wasp Head Formation|71538|6|Mentioned|p54, p62|Middle Sakmarian|Early Sakmarian|Sydney Basin. Fluvial depositional environment.||Tallaterang Group||Overlies disconformably the Wagonga Beds. Disconformably overlies the Clyde Coal Measures. Unconformably overlain by the Yadboro Formation, Tallong Formation and the Pebbley Beach Formation.||
19554|Wasp Head Formation|73421|4|Described|p1, p2 Fig.1, p3, p5, p15-17, p19-20|Sakmarian|Asselian|Sydney Basin, southern. Abbreviated to WHF in text. Shallow marine, deposited during a transition from glacial to non-glacial periods. Late Asselian to Sakamarian age has relied on low-diversity brachiopod fauna (Cisterna and Shi, 2014). Interpolated Sr/Sr age of 289.6+/-1.5 Ma given to the top of the WHF by Garbelli et al., (2019).|289.6+/-1.5 Ma interpolated Sr/Sr age|Talaterang Group||Underlies Shoalhaven Group, Pebbley Beach Formation|Sandstone-dominated unit. Cross-bedded in part and includes conglomerates, siltstone and pebble layers.|
19554|Wasp Head Formation|73494|5|Briefly described|p541|Permian|Permian|Southern Sydney Basin. Early Permian.||Talaterang Group.||Is overlain by Pebbley Beach Formation.||
19559|Watch Box Granite|32820|6|Mentioned|p3|||Cullarin Anticlinorium||||||
19559|Watch Box Granite|36413|2|Defined|p110|Devonian|Devonian|||||||
19559|Watch Box Granite|36414|5|Briefly described|map legend|Early Devonian|Early Devonian|Microcline granite, massive, homogenous, medium grained. GSNSW map code: gw.||||||
19559|Watch Box Granite|39626|6|Mentioned|p276|||||||||
19559|Watch Box Granite|40328|4|Described|p212|||||||||
19559|Watch Box Granite|42726|5|Briefly described|map legend|Early Devonian||Wrongly shown as part of Wheeo Suite.||||||
19559|Watch Box Granite|69270|6|Mentioned|p23|||Richardson (1976) suggested Tinderry Granite is a southern continuation of Watch Box Granite, which outcrops only 2 km along strike to the north.||||||
19559|Watch Box Granite|71069|6|Mentioned|p201|||May be compositionally equivalent to the Harrisons Peak Granite.||||||
19575|Waterbeach Formation|22472|5|Briefly described|p37|Devonian|Devonian|of the Crudine Group||||||
19575|Waterbeach Formation|22529|5|Briefly described|1,4 fig 2, 8|Lochkovian|Lochkovian|Geol province Hill End Trough. Overlying unit Guroba Formation, underlying unit Turondale Formation||||||
19575|Waterbeach Formation|22590|5|Briefly described|P750|||||||||
19575|Waterbeach Formation|22857|5|Briefly described|p470 App.1 Tb.A1.6|Early Devonian|Early Devonian|Of the Crudine Group. Quartz and lithic wackes, slate, shale, siltstone. Max. thickness: 600m. Geological Province: Hill End Trough and Capertee Rise.||||||
19575|Waterbeach Formation|23043|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
19575|Waterbeach Formation|23170|2|Defined|p164|Lochkovian|Lochkovian|Of Crudine Group.||||||17-JUL-08
19575|Waterbeach Formation|23214|3|Fully described|p190|Lochkovian|Lochkovian|Of Crudine Group. Thinly and rhythmically bedded, grey and green, fine grained sandstone and siltstone. Max. thickness 700m.||||||
19575|Waterbeach Formation|23738|5|Briefly described|p251|Devonian|Devonian|||||||
19575|Waterbeach Formation|24394|5|Briefly described|p170|Pragian|Lochkovian|Of Merrions Formation. Geological Province: Lachlan Fold Belt.||||||
19575|Waterbeach Formation|30099|6|Mentioned|p386|||||||||
19575|Waterbeach Formation|33326|6|Mentioned|p444|||Fauna.||||||
19575|Waterbeach Formation|33732|5|Briefly described|p116|||||||||
19575|Waterbeach Formation|34403|4|Described|p135|||||||||
19575|Waterbeach Formation|34405|6|Mentioned|Fig.3.9|||||||||
19575|Waterbeach Formation|34406|6|Mentioned|p222|||||||||
19575|Waterbeach Formation|34572|6|Mentioned|Table 1|||Crudine Group||||||
19575|Waterbeach Formation|38216|5|Briefly described|p253|||||||||
19575|Waterbeach Formation|39331|6|Mentioned|Fig.7.6|||||||||
19575|Waterbeach Formation|40328|6|Mentioned|p173|||See also P174||||||
19575|Waterbeach Formation|42033|6|Mentioned|p652|||||||||
19575|Waterbeach Formation|43127|5|Briefly described|p4,Fig.2,Fig.3||Early Devonian|||||||
19575|Waterbeach Formation|43494|4|Described|p26|Devonian|Devonian|Consists of slaty shale and siltstone, commonly laminated, plus minor thin beds of lithic, feldspathic sandstone. Conformable over Turondale Formation. Max. thickness: 1200m.||||||16-MAR-06
19575|Waterbeach Formation|43517|2|Defined|p123-163,Map Pl XII||Early Devonian|Upper part of Crudine Group.||||||17-JUL-08
19575|Waterbeach Formation|43639|5|Briefly described|Map Legend||Devonian|||||||
19575|Waterbeach Formation|43641|5|Briefly described|Map Legend||Devonian|||||||
19575|Waterbeach Formation|43653|5|Briefly described|Map Legend||Devonian|||||||
19575|Waterbeach Formation|43654|6|Mentioned|Map Legend|Devonian|Devonian|Of Crudine Group. Siltstone, shale, minor lithic sandstone.||||||17-JUL-08
19575|Waterbeach Formation|43782|5|Briefly described|Map Legend|Lochkovian|Lochkovian|of Crudine Group.||||||
19575|Waterbeach Formation|64296|5|Briefly described|p84 Tb. 1|Early Devonian|Early Devonian|||||||
19575|Waterbeach Formation|68003|5|Briefly described|p24 Fig.3-e, p143. |Lochkovian|Lochkovian|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Crudine Group.||Overlies Turondale Formation. Is overlain by Guroba Formation.|Well-bedded to laminated slate, siltstone and phyllitic shale, with lesser lithic, feldspathic sandstone.|
19575|Waterbeach Formation|68592|6|Mentioned|p1038|||Northern Hill End Trough.||Unit in Crudine Group.||||
19575|Waterbeach Formation|70297|5|Briefly described|map legend|Early Devonian|Early Devonian|||Crudine Group||||
19575|Waterbeach Formation|71924|5|Briefly described|p2|Lochkovian||Of Garratt & Wright 1988. Hill End Trough. Includes important faunas. Fauna older than lower Mullamuddy [Formation].||Of Crudine Group.||||
19575|Waterbeach Formation|73299|5|Briefly described|p1096 Fig.3, p1098 Fig.4, p1101, p1108|Early Devonian|Late Silurian|Hill End Trough. Locations in text include p1102 Fig.8. [Map symbol suggests Devonian age]||||Overlies the Turondale Formation, underlies the Guroba Formation, Merrions Formation.|Locally thick, shale dominated.|
19576|Waterfall Gully Formation|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Doyles Creek Subgroup.||||||
19576|Waterfall Gully Formation|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Doyles Creek Subgroup (Wollombi Coal Measures). Geological Province: Sydney Basin||||||
19576|Waterfall Gully Formation|29942|3|Fully described|p11|||||||||
19576|Waterfall Gully Formation|39666|6|Mentioned|p79|||||||||
19576|Waterfall Gully Formation|45090|6|Mentioned|p187|||Refers Britten (1972)||||||
19576|Waterfall Gully Formation|68004|5|Briefly described|p51 Table 5, p52.|Late Permian|Late Permian|Upper Hunter Coalfield.||Upper unit in Doyles Creek Sub-group.||Overlies Pinegrove Formation. Is overlain by Dights Creek Coal.|Tuffaceous cherty claystone.|
19589|Watermark Formation|721|5|Briefly described|Map legend|Ufimian|Ufimian|Siltstone, claystone, silty sandstone, thinly bedded siltstone and sandstone. Geological Province: Gunnedah Basin.||||||17-SEP-08
19589|Watermark Formation|22579|5|Briefly described|p217|Late Permian|Late Permian|||||||
19589|Watermark Formation|22857|4|Described|p263, p520 App.1 Tb.A1.9|Late Permian|Late Permian|Of Millie Group. Siltstone, claystone, silty sandstone. Max. thickness: 230m. Geological Province: Gunnedah Basin. See also p315 Fig. 22.8.||||||
19589|Watermark Formation|22864|6|Mentioned|p263|||||||||
19589|Watermark Formation|22865|6|Mentioned|Fig22.8p315|||||||||
19589|Watermark Formation|23050|5|Briefly described|p9 Fig.2|Early Permian|Early Permian|Of Gunnedah Basin.||||||17-SEP-08
19589|Watermark Formation|23566|5|Briefly described|p116 Fig. 2|Late Permian|Late Permian|Parent: Millie Group. Geological Province: Gunnedah Basin||||||
19589|Watermark Formation|23740|5|Briefly described|p1221|Permian|Permian|Geological Province: Gunnedah Basin.||||||17-SEP-08
19589|Watermark Formation|24159|5|Briefly described|p150 Fig.3, p149|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Overlying Unit: Black Jack Group. Underlying Unit: Porcupine Formation.||||||
19589|Watermark Formation|24243|5|Briefly described|p3 Fig.2|Permian|Permian|||||||
19589|Watermark Formation|31883|6|Mentioned|p594|||See also Table 1||||||
19589|Watermark Formation|32944|6|Mentioned|p700|||See also PP702,710. U.Permian||||||
19589|Watermark Formation|34043|5|Briefly described|p452|||Perm. See Table 5.32||||||
19589|Watermark Formation|37094|5|Briefly described|p241|||||||||
19589|Watermark Formation|37856|6|Mentioned|p2|||||||||
19589|Watermark Formation|38089|4|Described|p9|||||||||
19589|Watermark Formation|38614|4|Described|p6|||||||||
19589|Watermark Formation|39063|4|Described|p11|||||||||
19589|Watermark Formation|39308|6|Mentioned|Fig. 23.12|||||||||
19589|Watermark Formation|39693|6|Mentioned|p17|||||||||
19589|Watermark Formation|39913|4|Described|p4|||||||||
19589|Watermark Formation|40060|6|Mentioned|p36|||||||||
19589|Watermark Formation|40200|6|Mentioned|p14|||||||||
19589|Watermark Formation|40321|6|Mentioned|Fig.3|||||||||
19589|Watermark Formation|40332|6|Mentioned|Fig.3|||||||||
19589|Watermark Formation|40680|6|Mentioned|Fig.1|||||||||
19589|Watermark Formation|40767|5|Briefly described|p16|||Mention Fig.1||||||
19589|Watermark Formation|40952|4|Described|p5|||||||||
19589|Watermark Formation|41264|6|Mentioned|Fig.2|||||||||
19589|Watermark Formation|41290|5|Briefly described|p225|||||||||
19589|Watermark Formation|41330|6|Mentioned|p19|||||||||
19589|Watermark Formation|41451|6|Mentioned|p14|||||||||
19589|Watermark Formation|41689|6|Mentioned|Table 1|||||||||
19589|Watermark Formation|41990|5|Briefly described|p8|||||||||
19589|Watermark Formation|42182|6|Mentioned|Table 1|||||||||
19589|Watermark Formation|42284|5|Briefly described|Fig.11 P104|||||||||
19589|Watermark Formation|42378|5|Briefly described|p19|||||||||
19589|Watermark Formation|42463|6|Mentioned|Fig.6 P173|||||||||
19589|Watermark Formation|42679|5|Briefly described|Fig.3 P3|||||||||
19589|Watermark Formation|42680|6|Mentioned|p19|||||||||
19589|Watermark Formation|42767|5|Briefly described|Fig.5|||||||||
19589|Watermark Formation|42950|5|Briefly described|p40|||||||||
19589|Watermark Formation|43091|5|Briefly described|Map legend|||ofGunnedah Basin||||||
19589|Watermark Formation|43194|1|Redefined|p98 Tb. 8.2, p104-106, 118, p133 App. 1|Late Permian|Late Permian|See also references on p95, p97, p101 Fig.8.2, p128, p129 Tb.8.3, p130. Now of Millie Group. Overlies Porcupine Formation (gradational contact). Underlies Black Jack and Digby Formations. Age Lower Stage 5b to Lower Stage 5c. Mulbring Siltstone and Berry Siltstone (lower part) are correlatives.||||||
19589|Watermark Formation|43409|14|Not recorded|Map Legend|||Equivalent of Gladstone Formation. See also Lexicon||||||
19589|Watermark Formation|50629|5|Briefly described|Map Legend|Late Permian|Late Permian|Geological Province: Gunnedah Basin. Of the Millie Group. Underlies: Brothers Subgroup.  Overlies: Porcupine Formation.||||||05-JUL-04
19589|Watermark Formation|61313|5|Briefly described|p91, p94 Fig. G7, p98 Fig. G10|Permian|Permian|Upper part forms a prodelta and delta-front facies. Conformably overlies Porcupine Formation. Max. thickness: 220m for combined upper and lower parts in eastern part of basin, thinning westwards. Geological Province: Gunnedah Basin. See also p95 Fig. G8||||||
19589|Watermark Formation|61377|5|Briefly described|p149 Fig. SU8|Early Permian|Early Permian|Geological Province: Gunnedah Basin. See also p154 Fig. SU9.||||||07-FEB-11
19589|Watermark Formation|61612|6|Mentioned|p272, p276, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Gunnedah Basin.||||||17-MAR-09
19589|Watermark Formation|61776|5|Briefly described|p194 Fig. 3|Permian|Permian|Of Millie Group. Geological Province: Gunnedah Basin. Siltstone, claystone, silty sandstone and lithic sandstone, bioturbated and burrowed in part.||||||
19589|Watermark Formation|62357|5|Briefly described|p524 Fig. 7|Middle Permian|Middle Permian|Geological Province: Gunnedah Basin.||||||
19589|Watermark Formation|63832|5|Briefly described|p131 Fig.2, p136|Roadian||Of Gunnedah Basin. Seventh (P3) glaciation. Dominantly glaciomarine deposits.|||||Contains complexly interbedded diamictites and other characteristic glacial facies.|14-DEC-17
19589|Watermark Formation|64631|6|Mentioned|p49.|Roadian|Roadian|Gunnedah Basin. Distal glaciomarine deposits. See also p44. Biostratigraphic age control for base and top.||||||
19589|Watermark Formation|65112|6|Mentioned|Fig 4 p314|Late Permian|Late Permian|Unit in the Gunnedah Basin. Overlies the Porcupine Formation, underlies the Black Jack Group.||||||22-MAR-12
19589|Watermark Formation|65113|5|Briefly described|Fig 4 p340|Late Permian|Late Permian.|Gunnedah Basin. Overlies Porcupine Formation, underlies Black Jack Group.||||||
19589|Watermark Formation|65114|5|Briefly described|p385 Fig.3|Late Permian||||||||
19589|Watermark Formation|65115|6|Mentioned|Fig 2 p403|Permian|Permian|Overlies the Porcupine Formation, underlies the Black Jack Group in the Gunnedah Basin.||||||
19589|Watermark Formation|65116|4|Described|Fig 2 p436, fig 6 p441, p449 Fig 14|Late Permian|Late Permian|Underlies the Black Jack Group, ?overlies the Porcupine Formation in the Gunnedah Basin. Laminated siltstone,sandstone and claystone.||||||
19589|Watermark Formation|65118|5|Briefly described|p491, Fig 2 p479|Permian|Permian|Underlies the Black Jack Group, Overlies the Porcupine Formation in the Gunnedah Basin.||||||
19589|Watermark Formation|66191|5|Briefly described|p485 Fig.2, p485|Late Permian|Late Permian|Gunnedah Basin. Underlies the Black Jack Group, overlies the Porcupine Formation. Siltstone and claystone.||||||
19589|Watermark Formation|68003|5|Briefly described|p38 Fig.3-j, p57 Fig.3-n, p129.|Late Permian|Late Permian|Gunnedah Basin, Brigalow Belt South Bioregion.||Upper unit in Millie Group.||Overlies Porcupine Formation. Is overlain by Pamboola Formation.|Fining-up sequence of intensely bioturbated silty sandstone to siltstone/claystone laminite with marine fossils, overlain by finely laminated siltstone/claystone, then a coarsening-up sequence.|
19589|Watermark Formation|68004|5|Briefly described|p23 Table 1, p176.|||Gunnedah Basin. Has potential as hydrocarbon reservoir. A potential oil source rock.||Upper unit in Millie Group.||Overlies Porcupine Formation. Is overlain by Pamboola Formation.||
19589|Watermark Formation|70791|5|Briefly described|p277|Guadalupian|Guadalupian|Gunnedah Basin.||Millie Group.||||
19589|Watermark Formation|70878|5|Briefly described|p715-p718, p723|Permian|Permian|Other age determinations given. Calibration of palynological ages (D. ericianus Zone).|262.54 +/- 0.16 Ma.|Millie Group.||Overlies Porcupine Formation. Is overlain by Pamboola Formation (Black Jack Group).||25-SEP-18
19589|Watermark Formation|73625|6|Mentioned|p2|Permian|Permian|Gunnedah Basin.||||Overlies Porcupine Formation. Is overlain by Pamboola Formation.||
19623|Waugoola Group|13139|5|Briefly described|p3 Fig. 2, p9 Fig. 4|Wenlock|Llandovery|Geological Province: Western and Eastern Molong Volcanic Belts.||||||
19623|Waugoola Group|22486|6|Mentioned|p 7|||||||||
19623|Waugoola Group|22857|4|Described|p127, p426 App. 1 Tb. A1.5|Early Wenlockian|Llandovery|Shale, limestone, siltstone, calcareous and feldspathic arenite, conglomerate; corals, brachiopods. Geological Province: Molong Rise. See also p468 App.1 Tb.A1.6.||||||17-FEB-06
19623|Waugoola Group|23213|6|Mentioned|p20||Early Silurian|||||||
19623|Waugoola Group|23214|2|Defined|p107|Early Silurian|Early Silurian|Originally included in the Panuara Formation (subsequently Panuara Group).  Max. thickness 176m.||||||
19623|Waugoola Group|23245|6|Mentioned|p127|||||||||
19623|Waugoola Group|23309|6|Mentioned|p390|||||||||
19623|Waugoola Group|23334|5|Briefly described|9 Fig.4|Silurian|Early Silurian|||||||
19623|Waugoola Group|24398|5|Briefly described|p259 Fig.2|Llandovery|Llandovery|Geological Province: Lachlan Fold Belt.||||||
19623|Waugoola Group|35258|4|Described|p120|||||||||
19623|Waugoola Group|41296|6|Mentioned|p130|||||||||
19623|Waugoola Group|43127|5|Briefly described|p3,Fig.2,Fig.3||Early Silurian|||||||
19623|Waugoola Group|43640|5|Briefly described|Map Legend||Silurian|||||||
19623|Waugoola Group|43642|5|Briefly described|Map Legend|Silurian|Silurian|Includes Cobblers Creek Limestone and Glendalough Formation.||||||15-JUL-08
19623|Waugoola Group|43782|5|Briefly described|Map Legend|Wenlock|Llandovery|||||||
19623|Waugoola Group|44093|5|Briefly described|p201 App. 1|Silurian|Silurian|Age: Middle Silurian. Geological Province: Lachlan Fold Belt.||||||
19623|Waugoola Group|60989|5|Briefly described|p111, p113|||Anggulong district.|||Cobblers Creek Limestone.|Overlies Ashburnia Group.||
19623|Waugoola Group|63278|6|Mentioned|p147 Fig. 2b|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt, LFB.||||||07-FEB-11
19623|Waugoola Group|63283|6|Mentioned|p195 Fig. 2|Early Silurian|Early Silurian|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19623|Waugoola Group|63287|5|Briefly described|p317 Fig. 2, p336, p349|Wenlock|Llandovery|Includes; Boree Creek Formation, Cobblers Creek Limestone, Quarry Creek Limestone, Glendalough Formation. Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19623|Waugoola Group|63290|5|Briefly described|p392 Tb. 1, p400 Fig. 5(b), p396 Fig. 3|Silurian|Llandovery|Includes; Cobblers Creek Limestone, Boree Creek Formation. Geological Province: Molong Volcanic Belt. Contains conglomerates that have well-rounded cobble to grit-sized clasts of Forest Reefs Volcanics.||||||
19623|Waugoola Group|63293|6|Mentioned|p469 Fig. 2|Wenlock|Llandovery|Geological Province: Molong Volcanic Belt.||||||07-FEB-11
19623|Waugoola Group|67106|6|Mentioned|p673|||Molong Volcanic Belt.||||||
19623|Waugoola Group|68592|6|Mentioned|p416|||Jenkins (1978); Pogson and Watkins (1998).|||Includes Glendalough Formation.|||
19623|Waugoola Group|70297|4|Described|map legend, on side 2 of map sheet|Llandovery|Llandovery|Age: late Llandovery to early Wenlock. Represents a marginal shallow to deep water sequence.|||Boree Creek Formation, Cobblers Creek Limestone, Glendalough Formation|Disconformably overlies Ashburnia Group.|Shale, limestone, siltstone, calcareous and feldspathic arenite, conglomerate; corals, brachiopods.|
19623|Waugoola Group|70684|5|Briefly described|p34, p48-49, p50 Fig.24, p75|Early Silurian|Early Silurian|Molong Volcanic Belt. A rift-sag sequence.|||Cobblers Creek Limestone, Glendalough Formation.||Basal conglomerate, overlain by siltstone and fine-grained quartz sandstone.|
19623|Waugoola Group|73154|6|Mentioned|p77 Fig.3|Wenlock|Llandovery|||||||
19633|Wave Hill Coal|22578|6|Mentioned|Fig.9 p399|||||||||
19633|Wave Hill Coal|23055|6|Mentioned|Fig4p11|||||||||
19633|Wave Hill Coal|23717|5|Briefly described|p118 Fig. 2|Permian|Permian|Parent: Adamstown Formation.   Geological Province: Sydney Basin||||||
19633|Wave Hill Coal|39308|6|Mentioned|Fig.23.4|||||||||
19633|Wave Hill Coal|40516|6|Mentioned|p395|||||||||
19633|Wave Hill Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Wave Hill coal seam instead. See also p113.||Of Adamstown Subgroup||||
19633|Wave Hill Coal|73304|6|Mentioned|p75|||||Adamstown Formation, Newcastle Coal Measures||||
19642|Waynes Knob Rhyolite|22857|4|Described|p458 App.1, Tb.A1.6|Lochkovian|Lochkovian|Of the Black Range Group. Rhyolite lavas and dykes, plugs. Geological Province: Canberra-Yass Shelf.||||||
19642|Waynes Knob Rhyolite|32675|6|Mentioned|p8|||Refers Link (1970, 1971). Back Ra. Gp.||||||
19642|Waynes Knob Rhyolite|35384|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
19642|Waynes Knob Rhyolite|35386|4|Described|p47|||||||||
19642|Waynes Knob Rhyolite|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
19642|Waynes Knob Rhyolite|37727|6|Mentioned|p40|||||||||
19642|Waynes Knob Rhyolite|50230|5|Briefly described|Map legend|Pragian|Lochkovian|Of the Black Range Group.||||||
19642|Waynes Knob Rhyolite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Black Range Grp. Pink to grey, fine-gr., flow banded, locally vesicular rhyolite - of anhedral phenocrysts of K-feldspar + magnetite, subordinate plagioclase, augite, bioitie+quartz, set in groundmass of finely cryptocrystalline qtz, feldspar, chlorite||||||17-JUN-08
19642|Waynes Knob Rhyolite|68592|2|Defined|p430 Fig.89, p926-33, p965-8|Early Devonian|Lochkovian|Link (1971) suggested this name for rhyolites at Mount Bowning and nearby peaks, and included it in his Bowning Group. Formally described and published by Cramsie et al. (1978) in the Black Range Group. Named after an eponymous hill 1.7km S of Bowning; it is actually made of Pilleuil Andesite: Link and Cramsie et al. misidentified the hill. Forms four separate intrusive bodies, three of which form knolls. Type locality described. Geochemistry detailed; geophysical properties described.||Unit in Black Range Group.||Intrudes Sharpeningstone Conglomerate, Cowridge Siltstone and Pilleuil Andesite; also overlies the latter. Correlated with Mountain Creek Volcanics.|Pink to grey, fine-grained, feldspar and minor quartz-phyric rhyolite stocks; flow-banding and subvertical columnar jointing occur, as do thin rhyolite dykes. I-type.|
19642|Waynes Knob Rhyolite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dby. On Yass 1:100 000 mapsheet portion of Time-Space Plot. Related units inferred from Time-Space Plot.||Black Range Group||Overlies Pilleuil Andesite.|Fine grained, flow banded, locally vesicular, feldspar and minor quartz-phyric rhyolite.|
19642|Waynes Knob Rhyolite|70540|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine grained, flow banded, locally vesicular, feldspar and minor quartz-phyric rhyolite.|
19642|Waynes Knob Rhyolite|70546|5|Briefly described|Map Legend|Devonian|Devonian|||Black Range Group|||Fine grained, flow banded, locally vesicular, feldspar and minor quartz phyric rhyolite.|
19642|Waynes Knob Rhyolite|73215|6|Mentioned|p994|||Yass Syncline.||Black Range Group.||||
19648|Wean Formation|29870|4|Described|p11|||||||||
19648|Wean Formation|30135|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19648|Wean Formation|30911|6|Mentioned|Map legend|Permian|Permian|||||||
19648|Wean Formation|31882|5|Briefly described|p245|||||||||
19648|Wean Formation|32671|6|Mentioned|Map legend|Permian|Permian|||||||
19648|Wean Formation|32944|6|Mentioned|Fig.2.3|||See also PP700-704. Permian. Nandewar Gp.||||||
19648|Wean Formation|34043|5|Briefly described|p449|||L.Perm.||||||
19648|Wean Formation|36940|6|Mentioned|p129|||||||||
19648|Wean Formation|39288|5|Briefly described|p59|||Microflora||||||
19648|Wean Formation|41264|6|Mentioned|p251|||Recently Leard Formation||||||
19648|Wean Formation|43429|14|Not recorded|Map Legend|||Many plant fossils||||||
19657|Webbs Consols Leucogranite|23050|4|Described|p51 Table.2|Early Triassic|Early Triassic|Age: no dating. Probably early Triassic as it intrudes Wandsworth Volcanic Group.||||||
19657|Webbs Consols Leucogranite|23051|5|Briefly described|Map Legend|Middle Triassic|Early Triassic|||||||
19657|Webbs Consols Leucogranite|42729|4|Described|p14|||||||||
19657|Webbs Consols Leucogranite|42748|2|Defined|p13||Early Triassic|||||||
19657|Webbs Consols Leucogranite|62534|5|Briefly described|p10 (legend)|Early Triassic|Early Triassic|Intruded Emmaville Volcanics. Occurs as a fine- to coarse-grained, coarsely porphyritic to equigranular, leucocratic granite. Magnetics/radiometrics discussed.||||||07-FEB-11
19657|Webbs Consols Leucogranite|68005|5|Briefly described|p134.|Triassic|Triassic|This unit appears suddenly in Appendix 4, where it is given as a unit in the Uralla Supersuite. Perhaps see also references to Webbs Consols Granite (p45 Fig.3-J, p64, pp68-70).|||||Medium- to coarse-grained leucocratic and granophyric alkali feldspar granite with large quartz and K-feldspar megacrysts; a second phase consists of graphic and granophyric fine-grained granite.|
19657|Webbs Consols Leucogranite|70217|4|Described|v, p1 tbl 1.1, p38, p43-p48, p75, p87|Wuchiapingian|Wuchiapingian|New England Orogen. SHRIMP ages are derived from this volume. Petrography, zircon morphology and SHRIMP results discussed in detail. Age interpreted as the magmatic crystallisation age.|255.9 +/- 1.4 Ma (SHRIMP U-Pb)|Mount Duval Suite||Intruded by the Wandsworth Volcanic Group.|Fine to medium-grained, porphyritic alkali feldspar granite containing 40 percent quartz, 50 percent alkali feldspar and minor plagioclase and biotite.|
19657|Webbs Consols Leucogranite|71628|3|Fully described|p19: 28, 31, 35-36, 78, 161-162, 168-171|||Stroud (1990, 1992), after unpublished work by McAuley (1975) and Meldrum (1983). Named presumably after the Webbs Consols mine. Located 10 km SW of Emmaville. Comprises 2 or 3 small (largest is ~4.5 x 3 km) bodies. Type locality (Stroud, 1992) is E and NE of the main Webbs Consols shaft (GR 5240 3615, Ashford 1:100,000 sheet). Geochemistry detailed; highly fractionated. Is spatially associated with economically significant base metal mineralisation (Ag, Pb, Zn, As, Cu, Bi, Au).|255.9 +/- 1.4 Ma (SHRIMP: Waltenberg et al., 2015)|Webbs Consols Suite.|Dumboy-Gragin Leucosyenogranite.|Intrudes Bondonga beds and Emmaville Volcanics.|Medium- to coarse-grained, leucocratic and granophyric biotite alkali feldspar granite. I-type.|
19681|Weemalla Diorite|43548|3|Fully described|p254|||No age given. Intrudes Silurian||||||
19681|Weemalla Diorite|49794|5|Briefly described|p10|||||||||
19707|Wellington Caves Limestone|34426|6|Mentioned|p8|||Palaeontology||||||
19707|Wellington Caves Limestone|34692|5|Briefly described|p184|||||||||
19731|Wendalpa Subgroup|22772|5|Briefly described|Map4p56-57,Table13.1|Cryogenian|Cryogenian|||||||
19731|Wendalpa Subgroup|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Willouran|Willouran|Of the Poolamacca Group. Geological Province: Adelaid Fold Belt. See also p398, 400 and 402 App. 1 Tb.A1.3.||||||
19731|Wendalpa Subgroup|36733|6|Mentioned|Table 5|||||||||
19731|Wendalpa Subgroup|41403|6|Mentioned|p50|||||||||
19731|Wendalpa Subgroup|42531|5|Briefly described|Map legend|Adelaidean||||||||
19731|Wendalpa Subgroup|43265|5|Briefly described|Map Legend||Neoproterozoic|of Poolamacca Group||||||
19731|Wendalpa Subgroup|43269|5|Briefly described|Map Legend||Neoproterozoic|of Poolamacca Group.||||||
19731|Wendalpa Subgroup|70000|5|Briefly described|p34|Neoproterozoic|Neoproterozoic|||Unit in Poolamacca Group.|Includes Boco Formation and Wilangee Basalt.|||
19731|Wendalpa Subgroup|70015|5|Briefly described|Map legend|Neoproterozoic|Neoproterozoic|Mineral deposits (if any) are shown.||Unit in Poolamacca Group.|Includes Boco Formation and Wilangee Basalt.|Overlies Pintapah Subgroup.|Quartz sandstone with minor limestone overlain by amygdaloidal basalt.|
19731|Wendalpa Subgroup|72461|6|Mentioned|p16 fig 9|||||Poolmacca Group|Includes the Wilangee Basalt and the Boco Formation.|||
19731|Wendalpa Subgroup|74367|6|Mentioned|p20|||||||||
19736|Wentworth Falls Claystone Member|23219|5|Briefly described|Map Legend|Triassic|Triassic|||||||
19736|Wentworth Falls Claystone Member|29749|4|Described|p11|||||||||
19736|Wentworth Falls Claystone Member|31061|3|Fully described|p1319|||Marker across Sydney Basin.||||||
19736|Wentworth Falls Claystone Member|31373|4|Described|Table 2|||Unit of Banks Wall Sst.||||||
19736|Wentworth Falls Claystone Member|31725|6|Mentioned|p10|||On table||||||
19736|Wentworth Falls Claystone Member|31886|4|Described|p394|||||||||26-JUL-12
19736|Wentworth Falls Claystone Member|32801|6|Mentioned|p254|||||||||
19736|Wentworth Falls Claystone Member|32802|6|Mentioned|p22|||||||||
19736|Wentworth Falls Claystone Member|37346|6|Mentioned|p48|||||||||
19736|Wentworth Falls Claystone Member|39287|6|Mentioned|p46|||||||||
19736|Wentworth Falls Claystone Member|39293|4|Described|p152|||||||||
19736|Wentworth Falls Claystone Member|39308|6|Mentioned|p501|||||||||
19736|Wentworth Falls Claystone Member|40653|6|Mentioned|Fig.20|||||||||
19736|Wentworth Falls Claystone Member|42925|4|Described|p12|||of Banks Wall Sandstone||||||
19736|Wentworth Falls Claystone Member|42926|4|Described|map legend||Early Triassic|||||||
19736|Wentworth Falls Claystone Member|43047|6|Mentioned|p276|||||||||
19736|Wentworth Falls Claystone Member|43194|5|Briefly described|p131|Triassic|Triassic|Thick claystone - siltstone red beds deposited in the Sydney Basin during the Triassic.||||||
19736|Wentworth Falls Claystone Member|65195|5|Briefly described|p3, p4 Fig.2, p7-12 Fig.4, p22-27 Fig.9|Early Triassic|Early Triassic|Upper part of the Banks Wall Sandstone. Underlies Burralow Formation. Red-brown to green claystone. Outcrops along cliffs adjacent to the Grose River.||||||
19736|Wentworth Falls Claystone Member|68003|5|Briefly described|p43.|Triassic|Triassic|Sydney Basin. Possibly terrestrial piedmont deposits.||Unit in upper part of Narrabeen Group.|||Thick claystone-siltstone red beds.|
19739|Wentworth Group|22530|6|Mentioned|p697||Early Devonian|||||||
19739|Wentworth Group|22628|6|Mentioned|fig1p108|Devonian|Devonian|||||||
19739|Wentworth Group|22768|5|Briefly described|Fig16.4p163,172,188|Pragian|Lochkovian|||||||
19739|Wentworth Group|22832|6|Mentioned|Fig.1b p634|Early Devonian|Early Devonian|||||||
19739|Wentworth Group|22857|5|Briefly described|p163 Fig. 16.4, p188|Pragian|Pragian|Shallow water sediments. Unconformably overlies Jemba Rhyolite.||||||
19739|Wentworth Group|23307|5|Briefly described|Map Legend|Devonian|Devonian|||||||
19739|Wentworth Group|23309|5|Briefly described|p103-104. Table 2.38||Devonian|||||||
19739|Wentworth Group|23522|5|Briefly described|p247 Fig 3||Early Devonian|||||||
19739|Wentworth Group|23710|14|Not recorded|p74|||Strongly folded and intruded.||||||
19739|Wentworth Group|24002|5|Briefly described|p228 Fig.2|Devonian|Devonian|||||||
19739|Wentworth Group|24004|5|Briefly described|p278|Early Devonian|Early Devonian|||||||
19739|Wentworth Group|24098|6|Mentioned|p27 Fig. 2|Middle Devonian|Emsian|Geological Province: Lachlan Fold Belt.||||||
19739|Wentworth Group|24551|4|Described|p138, 616|Devonian|Devonian|Includes Wild Horse Formation and Tabberabbera Formation.||||||
19739|Wentworth Group|29682|6|Mentioned|p15|||||||||
19739|Wentworth Group|32399|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
19739|Wentworth Group|33238|5|Briefly described|p644|||||||||
19739|Wentworth Group|33393|6|Mentioned|p163|||||||||
19739|Wentworth Group|33602|6|Mentioned|Table 1|||||||||
19739|Wentworth Group|33603|6|Mentioned|Map legend|Devonian|Devonian|||||||
19739|Wentworth Group|33606|3|Fully described|p67|||||||||
19739|Wentworth Group|33732|4|Described|p111|||||||||
19739|Wentworth Group|34287|6|Mentioned|p97|||||||||
19739|Wentworth Group|34989|6|Mentioned|p80|||||||||
19739|Wentworth Group|35112|6|Mentioned|Table 1|||||||||
19739|Wentworth Group|35283|6|Mentioned|p49|||||||||
19739|Wentworth Group|37330|4|Described|p16|||||||||
19739|Wentworth Group|40761|4|Described|p233|||||||||
19739|Wentworth Group|41137|6|Mentioned|p294|||||||||
19739|Wentworth Group|41570|6|Mentioned|Fig.3 13|||||||||
19739|Wentworth Group|41572|6|Mentioned|p14|||||||||
19739|Wentworth Group|41585|4|Described|p132|||||||||
19739|Wentworth Group|41590|6|Mentioned|Fig.2|||||||||
19739|Wentworth Group|42089|4|Described|p7|||||||||
19739|Wentworth Group|42577|5|Briefly described|p31|||||||||
19739|Wentworth Group|42827|4|Described|p132|||||||||
19739|Wentworth Group|43530|14|Not recorded|p1030|||||||||
19739|Wentworth Group|43541|14|Not recorded|p263|||||||||
19739|Wentworth Group|43547|14|Not recorded|p150,Table p153|Eifelian|Emsian|||||||
19739|Wentworth Group|44185|5|Briefly described|Map legend.|Early Devonian|Early Devonian||||Includes Wild Horse and Tabberabbera Formations.|||
19739|Wentworth Group|60503|5|Briefly described|p28 Fig. 9|Early Devonian|Early Devonian|||||||
19739|Wentworth Group|61160|6|Mentioned|p138|||In DARGO.||||||
19739|Wentworth Group|61161|5|Briefly described|p114, p8, p76-77 Fig 6.1|Early Devonian|Early Devonian|Includes Wild Horse Formation and Tabberabbera Formation. Fluvial gravel and siltstone accumulated unconformably on deformed Pinnak Sandstone; marine shelly fauna. Intruded by dykes and sills before deformation. GSV map code: Dw.||||||
19739|Wentworth Group|61163|6|Mentioned|p9|Silurian|Silurian|Geological Province: Lachlan Fold Belt (Tabberabbera Zoe).||||||
19739|Wentworth Group|61169|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Tabberabbera Formation and Wild Horse Formation.||||||
19739|Wentworth Group|61170|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Tabberabbera Formation and Wild Horse Formation.||||||07-FEB-11
19739|Wentworth Group|61171|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Tabberabbera Formation and Wild Horse Formation.||||||
19739|Wentworth Group|61172|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Tabberabbera Formation and Wild Horse Formation.||||||
19739|Wentworth Group|61173|5|Briefly described|map legend|Early Devonian|Early Devonian|Includes Tabberabbera Formation and Wild Horse Formation.||||||
19739|Wentworth Group|61187|5|Briefly described|p5 Fig.3.|Early Devonian|Early Devonian|Tabberabbera Zone, Benambra Terrane. Correlative of Buchan Group (Buchan and Mallacoota Zones, Benambra Terrane), and Lilydale Limestone and Wilson Creek Shale (Melbourne Zone, Melbourne Terrane).||||||
19739|Wentworth Group|63170|5|Briefly described|p229|||Contains the Tabberabbera Formation with conodonts. In eastern Victoria.||||||07-FEB-11
19739|Wentworth Group|65214|6|Mentioned|p273|Devonian|Devonian|VIC, Tabberabbera. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
19739|Wentworth Group|66197|5|Briefly described|p634, p639|Early Devonian|Early Devonian|Mitchell Syncline. Marginal to shallow marine environment deposition from a single source to the north. Includes Wild Horse Formation.||||||14-MAR-12
19739|Wentworth Group|69875|6|Mentioned|p262||||||Tabberabbera Formation.|||
19739|Wentworth Group|70742|6|Mentioned|p180|Emsian|Emsian|Tabberabbera area.||||||
19739|Wentworth Group|71040|5|Briefly described|p4 Fig.2, p13|Emsian|Emsian|Mitchell Syncline, E Victoria.||||Is overlain unconformably by Avon Supergroup.||
19745|Wermatong Metabasalt|22638|6|Mentioned|p9|||Tumut 1: 100 000 map sheet.||||||
19745|Wermatong Metabasalt|22687|6|Mentioned|110|Early Silurian|Ordovician|Geol province Lachlan Fold Belt||||||
19745|Wermatong Metabasalt|22857|4|Described|p452 App.1, Tb.A1.6|Middle Silurian|Silurian|Basalts, basaltic hyaloclastics, cherts, polymictic conglomerate. Contain radiolaria. Basement of the Tumut Trough.||||||
19745|Wermatong Metabasalt|37529|5|Briefly described|p7|||||||||
19745|Wermatong Metabasalt|42045|6|Mentioned|Fig.2 P148|||||||||
19745|Wermatong Metabasalt|42313|3|Fully described|p68||Early Silurian|Probable correlative of Brungle Creek Metabasalt. Age late Early Silurian||||||
19745|Wermatong Metabasalt|42314|5|Briefly described|Map|Early Silurian||||||||
19745|Wermatong Metabasalt|42828|5|Briefly described|Table 1 P129|Middle Silurian|Early Silurian|||||||
19745|Wermatong Metabasalt|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Sb2||||||
19745|Wermatong Metabasalt|44093|5|Briefly described|p183 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
19745|Wermatong Metabasalt|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
19745|Wermatong Metabasalt|67322|5|Briefly described|p20|Pridoli|Ludlow|Age constrained by that of the parent Jindalee Group: an Ordovician fragmented ophiolite sequence within a Silurian sedimentary matrix. On Tumut 1:100 000 sheet: (Basden, 1990).||Of the Jindalee Group||||22-FEB-18
19751|Werrie Basalt|721|5|Briefly described|Map legend|Sakmarian|Asselian|Basaltic lavas with intervening palaeosols and local thin coals.  Geological Province: Gunnedah Basin.||||||12-NOV-08
19751|Werrie Basalt|22572|6|Mentioned|p108|||overlain by Permian Hunter Coalfield||||||
19751|Werrie Basalt|22580|6|Mentioned|p97|Early Permian|Late Carboniferous|||||||
19751|Werrie Basalt|22857|4|Described|p244, p504 App.1 Tb.A1.8|Early Permian|Early Permian|Basaltic to dacitic lavas, autoclastic breccias, rare pyroclastic layers, minor sediments, palaeosols and thin coals. Max. thickness: 1500m. Geological Province: Meandarra Rift. See also p220, p256, p312 Fig. 22.6 and p315 Fig. 22.8||||||
19751|Werrie Basalt|22859|6|Mentioned|p220||Early Permian|||||||
19751|Werrie Basalt|22863|6|Mentioned|p242,244|||||||||
19751|Werrie Basalt|22864|6|Mentioned|p256,267|||||||||
19751|Werrie Basalt|22865|6|Mentioned|Fig22.6p312|||||||||
19751|Werrie Basalt|23050|5|Briefly described|p 82 Fig.17|Early Permian|Early Permian|Of Gunnedah Basin.||||||12-NOV-08
19751|Werrie Basalt|23102|5|Briefly described|p561|||||||||
19751|Werrie Basalt|23350|6|Mentioned|264|||||||||
19751|Werrie Basalt|23459|5|Briefly described|p158|||Gunnedah Basin.||||||12-NOV-08
19751|Werrie Basalt|23566|5|Briefly described|p116 Fig. 2|Early Permian|Early Permian|Geological Province: Gunnedah Basin||||||
19751|Werrie Basalt|24040|6|Mentioned|p468 Fig. 1|||Geolocical province: Tamworth Belt and margin of Surat Basin.||||||21-AUG-08
19751|Werrie Basalt|24159|5|Briefly described|p150 Fig. 3, p149|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Overlying Unit: Goonbri Formation.||||||10-SEP-19
19751|Werrie Basalt|24334|5|Briefly described|p49 Tb.1|Late Permian|Early Permian|Age: 256 - 290 Ma||||||
19751|Werrie Basalt|24603|5|Briefly described|p866, p870|Early Permian|Early Permian|See also p869 Fig. 4a, p886 Fig. 11 and p874 Tb. 1.  Geological Province: Tamworth Belt.||||||
19751|Werrie Basalt|29870|5|Briefly described|p8|||||||||
19751|Werrie Basalt|30135|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19751|Werrie Basalt|30911|6|Mentioned|Map legend|Permian|Permian|||||||
19751|Werrie Basalt|31802|4|Described|p136|||||||||
19751|Werrie Basalt|31855|6|Mentioned|p55|||Geol. map of Murrundi Oil-shale deposit||||||
19751|Werrie Basalt|31881|6|Mentioned|p331|||See also Fig.1 Refers Manser (1967)||||||
19751|Werrie Basalt|31882|6|Mentioned|p243|||||||||
19751|Werrie Basalt|31883|4|Described|p594|||See also Table 1||||||
19751|Werrie Basalt|32482|6|Mentioned|Map legend|Early Permian|Early Permian|||||||
19751|Werrie Basalt|32671|6|Mentioned|Map legend|Permian|Permian|||||||
19751|Werrie Basalt|32672|6|Mentioned|p674|||||||||
19751|Werrie Basalt|32944|6|Mentioned|Fig.2.3|||See also PP700-704. Permian||||||
19751|Werrie Basalt|32945|6|Mentioned|p88|||Permian||||||
19751|Werrie Basalt|33686|6|Mentioned|p21|||||||||
19751|Werrie Basalt|34043|5|Briefly described|p446|||Perm.  Corr. with Dalwood Gp.||||||
19751|Werrie Basalt|34085|6|Mentioned|Cor.chart|||Sakmarian||||||
19751|Werrie Basalt|34138|6|Mentioned|Cor.Chart|||Sakmarian||||||
19751|Werrie Basalt|34445|6|Mentioned|p319|||||||||
19751|Werrie Basalt|34447|6|Mentioned|Table 5.2|||||||||
19751|Werrie Basalt|36042|6|Mentioned|Fig.7|||||||||
19751|Werrie Basalt|36045|6|Mentioned|p330|||||||||
19751|Werrie Basalt|36534|6|Mentioned|p225|||||||||
19751|Werrie Basalt|36940|6|Mentioned|p125|||||||||
19751|Werrie Basalt|36961|6|Mentioned|p210|||||||||
19751|Werrie Basalt|37082|6|Mentioned|p160|||||||||
19751|Werrie Basalt|37558|6|Mentioned|Fig.1|||||||||
19751|Werrie Basalt|37773|6|Mentioned|p18|||||||||
19751|Werrie Basalt|37856|6|Mentioned|p2|||||||||
19751|Werrie Basalt|38089|6|Mentioned|p4|||||||||
19751|Werrie Basalt|38614|6|Mentioned|p5|||||||||
19751|Werrie Basalt|38684|6|Mentioned|p17|||Geological Province: New England Fold Belt||||||
19751|Werrie Basalt|38685|6|Mentioned|p26|||Geological Province: New England Fold Belt||||||
19751|Werrie Basalt|38818|5|Briefly described|p169|||Geological Province: New England Fold Belt. Underlying Unit: Temi Formation.||||||12-NOV-08
19751|Werrie Basalt|38837|6|Mentioned|p232|||||||||
19751|Werrie Basalt|39214|4|Described|p35|||||||||
19751|Werrie Basalt|39287|6|Mentioned|Fig. 2.2|||||||||
19751|Werrie Basalt|39288|6|Mentioned|p57|||||||||
19751|Werrie Basalt|39308|6|Mentioned|p494|||Cored ddh||||||
19751|Werrie Basalt|39331|6|Mentioned|Table 10-1|||||||||
19751|Werrie Basalt|39468|6|Mentioned|Fig.2|||||||||
19751|Werrie Basalt|39569|6|Mentioned|p95|||||||||
19751|Werrie Basalt|39572|6|Mentioned|p134|||||||||
19751|Werrie Basalt|39693|6|Mentioned|p14|||||||||
19751|Werrie Basalt|39833|6|Mentioned|p298|||||||||
19751|Werrie Basalt|39913|6|Mentioned|p2|||||||||
19751|Werrie Basalt|40166|6|Mentioned|Table 1|||||||||
19751|Werrie Basalt|40200|4|Described|p5|||||||||
19751|Werrie Basalt|40245|6|Mentioned|p198|||||||||
19751|Werrie Basalt|40246|6|Mentioned|p173|||||||||
19751|Werrie Basalt|40331|6|Mentioned|p5|||||||||
19751|Werrie Basalt|40762|6|Mentioned|p292|||||||||
19751|Werrie Basalt|40767|5|Briefly described|p2|||Mention Fig.4||||||
19751|Werrie Basalt|40867|6|Mentioned|p55|||||||||
19751|Werrie Basalt|40883|6|Mentioned|p15|||||||||
19751|Werrie Basalt|40952|6|Mentioned|p5|||||||||
19751|Werrie Basalt|41264|6|Mentioned|p251|||||||||
19751|Werrie Basalt|41290|6|Mentioned|Fig.5|||||||||
19751|Werrie Basalt|41347|4|Described|Table 3|||||||||
19751|Werrie Basalt|41348|5|Briefly described|Map legend|Permian|Permian|Amygdaloidal basalt, basaltic tuff, and tuffaceous sandstone.||||||16-DEC-04
19751|Werrie Basalt|41461|6|Mentioned|p11|||||||||
19751|Werrie Basalt|41689|6|Mentioned|Table 1|||||||||
19751|Werrie Basalt|41800|6|Mentioned|Fig.4|||||||||
19751|Werrie Basalt|42182|6|Mentioned|Table 1|||||||||
19751|Werrie Basalt|42284|5|Briefly described|Fig.11 P104|||||||||
19751|Werrie Basalt|42339|5|Briefly described|Fig.2 P53|||||||||
19751|Werrie Basalt|42399|5|Briefly described|Fig.2 PB11|||||||||
19751|Werrie Basalt|42463|6|Mentioned|Fig.6 P173|||Table actually says Werrie Basalts.||||||
19751|Werrie Basalt|42679|6|Mentioned|Fig.3 P3|||||||||
19751|Werrie Basalt|42780|5|Briefly described|p413|||see also p419.||||||23-SEP-18
19751|Werrie Basalt|42987|5|Briefly described|p29|||||||||
19751|Werrie Basalt|42997|5|Briefly described|p45|||||||||
19751|Werrie Basalt|43091|5|Briefly described|Map legend|||Of Gunnedah Basin.||||||17-SEP-08
19751|Werrie Basalt|43194|5|Briefly described|p97, p98 Tb. 8.2, p133 App. 1|Early Permian|Early Permian|See also references on p95, p99, p128, p129 Tb.8.3. Together with Boggabri Volcanics, forms basement to the Gunnedah Basin. May underlie Leard Formation.||||||13-NOV-13
19751|Werrie Basalt|43582|6|Mentioned|Fig.5,p16||Early Permian|||||||
19751|Werrie Basalt|44093|5|Briefly described|p227 App. 1|Early Permian|Early Permian|Geological Province: New England Fold Belt.||||||
19751|Werrie Basalt|47056|6|Mentioned|Fig.2 P523|||||||||
19751|Werrie Basalt|50629|5|Briefly described|Map Legend|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Underlies: Leard Formation. Interfingers with: Boggabri Volcanics.||||||05-JUL-04
19751|Werrie Basalt|60298|5|Briefly described|p192|Early Permian|Late Carboniferous|Age: 300+/-8 Ma. Geological Province: Gunnedah Basin.||||||17-DEC-07
19751|Werrie Basalt|61201|4|Described|p2, 5 Table 1, 6-7|Early Permian|Early Permian|Geological Province; Werrie Basin. Overlies Currabubula Formation, Temi Formation. Of the Warrigundi Igneous Complex? Basaltic lavas with intervening palaeosols. Max. Thickness: 1500m.||||||
19751|Werrie Basalt|61313|5|Briefly described|p98 Fig.G10|Early Permian|Early Permian|Geological Province: Gunnedah Basin. See also p104 Table G1.||||||
19751|Werrie Basalt|61377|6|Mentioned|p149 Fig. SU8|Early Permian|Early Permian|Geological Province: Gunnedah Basin. See also p154 Fig. SU9.||||||07-FEB-11
19751|Werrie Basalt|61612|6|Mentioned|p270 Fig. 1|Early Permian|Late Carboniferous|Geological Province: Gunnedah Basin.||||||17-MAR-09
19751|Werrie Basalt|61772|6|Mentioned|p127||Early Permian|In New England Orogen.||||||17-SEP-08
19751|Werrie Basalt|61776|5|Briefly described|p196, p194 Fig. 3|Early Permian|Early Permian|Geological Province: Gunnedah Basin. Basaltic lava with minor lithic sediments and coal.||||||17-SEP-08
19751|Werrie Basalt|61791|6|Mentioned|p325|||||||||
19751|Werrie Basalt|61792|5|Briefly described|p335|Early Permian|Early Permian|Geological Province: northern Sydney Basin.||||||27-JAN-06
19751|Werrie Basalt|61801|5|Briefly described|p403, p404|Early Permian|Early Permian|Reversely magnetised rock. Overlies the Temi Formation.||||||
19751|Werrie Basalt|62095|6|Mentioned|p250|Early Permian|Early Permian|Disconformably overlies the top member of the Temi Formation, namely the Willawarra Rhyodacite Member.  Age is Sakmarian.||||||
19751|Werrie Basalt|63774|6|Mentioned|p1075|||Geological Province: Lachlan Fold Belt.||||||
19751|Werrie Basalt|63832|5|Briefly described|p131 fig 2|Sakmarian|Sakmarian|Of Gunnedah Basin; also Werrie Syncline, Southern New England Fold Belt, where eruption was coeval with the sixth (P2) glaciation.||||Overlies and interfingers with Boggabri Volcanics.||14-DEC-17
19751|Werrie Basalt|64631|5|Briefly described|p44 Fig.2.|Artinskian|Sakmarian|Gunnedah Basin and southern New England Fold Belt. Sakmarian biostratigraphic age control for base and top in Maules Creek area, Gunnedah Basin. Shown as younger (up to Artinskian) in Werrie Syncline.||||Overlies Boggabri Volcanics in Maules Ck, Gunnedah Basin and Temi Formation in Werrie Syncline. Is overlain by Leard Formation.||
19751|Werrie Basalt|64855|6|Mentioned|p34-35|Early Permian|Early Permian|Tamworth Belt||||||22-FEB-10
19751|Werrie Basalt|65112|6|Mentioned|Fig 4 p314|Early Permian|Early Permian|Unit in the Gunnedah Basin. Overlies the Boggabri Volcanics, underlies the Leard Formation.||||||22-MAR-12
19751|Werrie Basalt|65113|5|Briefly described|Fig 4 p340|Early Permian|Early Permian|Gunnedah Basin. Overlies Boggabri Volcanics, underlies Leard Formation.||||||
19751|Werrie Basalt|65114|5|Briefly described|p383 Tb.1, p385 Fig.3, p394|Early Permian|Early Permian|300-?269 Ma age given for Werrie Basalt, Boggabri Volcanics together; Tectonic unit: Gunnedah Basin; mafic volcanic rocks; considered possibly to extend down into the APP1 palynological zone; stratigraphically above the Brogans Rhyodactite Member of the Woodton Formation||||||23-SEP-18
19751|Werrie Basalt|65116|5|Briefly described|p436, Fig. 2, p441 Fig. 6|Early Permian|Early Permian|Underlies the Leard Formation in the Gunnedah Basin. Mafic volcanics.||||||
19751|Werrie Basalt|65118|6|Mentioned|p484|||||||||
19751|Werrie Basalt|66191|5|Briefly described|p484 Fig.1, p485|Early Permian|Late Carboniferous|Gunnedah Basin. Basaltic and rhyolitic rift volcanics.||||||
19751|Werrie Basalt|67663|6|Mentioned|p519 Fig.1, p529 Tb.2|||||||||
19751|Werrie Basalt|68003|5|Briefly described|p38 Fig.3-j, p40, p57 Fig.3-n, pp129-130|Early Permian|Early Permian|Gunnedah and Werrie Basins, Brigalow Belt South Bioregion. Correlative of Gyarran Volcanics in Hunter Coalfield.||||Overlies Temi Formation. Is overlain by Willow Tree Formation.|Extensive mafic basalt extrusions; rhyolite; sandstone; intervening palaeosols and local thin coals.|
19751|Werrie Basalt|68004|5|Briefly described|p23 Table 1, p65.|||Gunnedah and Werrie Basins. Over 1000 m thick. Extruded from Piallaway and Mount Terrible volcanic centres.||||Overlies Temi Formation and, unconformably, the Currabubula Formation. Is overlain by Willow Tree Formation.||
19751|Werrie Basalt|68006|5|Briefly described|p103, p127.|||Constitutes the north Boggabri Ridge, which separates the Maules Creek and Mullaley Sub-basins. Source of kaolinitic clays in the Koogah Formation.||||||
19751|Werrie Basalt|68822|6|Mentioned|p321|Lower Permian|Lower Permian|||||||
19751|Werrie Basalt|69793|6|Mentioned|p1121 Fig.12|Sakmarian|Sakmarian|Werrie Block, Tamworth Belt.||||||
19751|Werrie Basalt|70036|5|Briefly described|Map legend|Permian|Permian|Early Permian.|||||Basalt.|
19751|Werrie Basalt|70329|6|Mentioned|p3 Fig.3|Permian|Permian|New England Orogen.|266.4 +/- 3.0 Ma (Li et al., 2014).|||||
19751|Werrie Basalt|70728|5|Briefly described|p265|Sakmarian|Sakmarian|Geological province: North Tamworth terrane, New England Orogen.||||Underlain by Temi Formation.||
19751|Werrie Basalt|70777|6|Mentioned|p8|Permian|Permian|New England Orogen.||||||
19751|Werrie Basalt|70791|5|Briefly described|p275-279, p281, p286-287, p292-294|Cisuralian|Cisuralian|Is assigned in this article to the Dalwood Group, "consistent with Hunter and Newcastle coalfield stratigraphy based on palynological ages and conformity relationships". Gunnedah, north Werrie Basins. Usually mentioned in association with Boggabri Volcanics. Both units are the source of sediments for Leard and Goonbri Formations.||||Is overlain by Bellata Group and Porcupine Formation, and nonconformably by Goonbri and Leard Formations.|Amygdaloidal basalt with minor interflow volcaniclastics. Generally weathers to dark grey kandite-rich rocks with relict volcanic textures.|
19751|Werrie Basalt|71115|5|Briefly described|p191-194|Permian|Permian|Southern New England Orogen, NW Tamworth Terrane. Paleomagnetic reconnaissance work, paleomagnetic poles for c.265 Ma, and paleomagnetic reliability, discussed.|266.4 +/- 3.0 Ma (40Ar/39Ar; whole rock).||||Includes pyroclastic rocks and ignimbrites.|
19751|Werrie Basalt|73197|6|Mentioned|p470-471, p472 Tb.2|Cisuralian|Late Carboniferous|Eastern edge of the Sydney Basin. Overlies Lachlan Orogen metasedimentary rocks. Limited outcrop, described from borehole data alongside the Boggabri Volcanics as aerially extensive ignimbrites and flows (Leitch, 1993). 292 +/- 10 Ma Rb-Sr age from Shaw et al., 1989), 300.0 +/- 8 Ma age from a heavy mineral separated from the Mount Terrible Complex, thought to be source of the Werrie Basalt.|300.0 +/- 8 Ma, 292 +/- 10 Ma Rb-Sr age||||Volcanics.|
19751|Werrie Basalt|73202|5|Briefly described|p626, p627 Fig.1, p640|Early Permian|Late Carboniferous|Sydney-Gunnedah Basin, part of the basal sequences. Sourced from a depleted asthenosphere, eNd = +2.05 to +6.00 (Caprarelli and Leitch, 2001).|ca 300-269 Ma, 266.4 +/- 3.0 Ma SHRIMP||||Mafic volcanic rocks.|
19754|Werrigundi intrusives|32671|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
19763|Werris Creek Coal Member|42182|6|Mentioned|p300|||||||||
19777|West Borehole Coal|23055|6|Mentioned|p1,14|||Lambton Formation.||||||
19777|West Borehole Coal|40516|6|Mentioned|p395|||||||||
19777|West Borehole Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal West Borehole coal seam instead. The west Borehole Coal/seam is said to be the combination of Nobbys, Dudley, Yard and Borehole Coal/seams.[???]. See also p113.||Of Lambton Subgroup||||
19796|Westbourne Formation|12597|5|Briefly described|p492 Tb.1, p495 Fig.3, p497, p499, p501|Kimmeridgian|Oxfordian|Northern Surat and eastern Eromanga Basins. Thickness generally 80-100m, up to 200m.||Unit in Injune Creek Group.||Conformably overlies Adori Sandstone. Interfingers with Pilliga Sandstone and lower Kumbarilla beds.|Cross-bedded, quartzose to sub-labile sandstone, siltstone and mudstone with lenticular bentonite beds and thin coal seams.|
19796|Westbourne Formation|13497|6|Mentioned|p115 fig 6.33, p130|Late Jurassic|Late Jurassic|Eromanga Basin. See also p141, p144 fig 9.2, p146, p148-p154, p216.||||Overlies the Adori Sandstone. Interfingers with and is overlain by the Namur Sandstone.||
19796|Westbourne Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Jurassic|Late Jurassic|In Eromanga Basin.||||||
19796|Westbourne Formation|22464|6|Mentioned|p9||Late Jurassic|Eromanga Basin. Overlies Adori Sandstone||||||
19796|Westbourne Formation|22857|5|Briefly described|p296-7 Tb.22.1, p314-5|Tithonian|Callovian|Fine-grained sandstone interbedded with siltstone, claystone, minor coal. Max. thickness: 220m. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
19796|Westbourne Formation|22865|4|Described|p314,Table22.1p296-7|Neocomian|Callovian|||||||
19796|Westbourne Formation|22883|6|Mentioned|P31|||||||||
19796|Westbourne Formation|23054|6|Mentioned|Fig5p22|Berriasian|Tithonian|||||||
19796|Westbourne Formation|23056|4|Described|20|||Geol province Eromanga Basin. Of the Injune Creek Group. Underlain by Adori Sandstone.||||||17-JAN-08
19796|Westbourne Formation|23155|5|Briefly described|p26|||The Westbourne Formation has not been recognised on STRZELECKI.||||||
19796|Westbourne Formation|23375|4|Described|Fig2 p265, 291|Tithonian|Tithonian|Laterally equivalent to part of Namur Sandstone. In the Eromanga Basin.||||||17-JAN-08
19796|Westbourne Formation|23425|5|Briefly described|Plate 10.2|||Of Injune Creek Group. Eromanga Basin Province.||||||
19796|Westbourne Formation|23426|5|Briefly described|p403|||Eromanga Basin Province.||||||
19796|Westbourne Formation|23430|4|Described|p523 + p524 Table 14.7|||Of Injune Creek Group. Overlain by Hooray Sandstone - unconformable. Eromanga Basin Province.||||||17-JAN-08
19796|Westbourne Formation|23818|6|Mentioned|p141 Fig.65, p142|Jurassic|Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|23883|5|Briefly described|p129 Fig. 11.2|Late Jurassic|Late Jurassic|Of the Injune Creek Group.  Geological Province: Great Australian Superbasin.||||||
19796|Westbourne Formation|23982|5|Briefly described|p35 Fig.7|Jurassic|Jurassic|Of Injune Creek Group. Geological Province: Great Artesian Basin.||||||
19796|Westbourne Formation|24068|4|Described|p270 Table 2|Late Jurassic|Late Jurassic|Of Injune Creek Group. Geological Province: Surat Basin.  Maximum thickness: 130m.||||||
19796|Westbourne Formation|24092|5|Briefly described|p8 Fig.3|||Of Injune Creek Group. Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24204|5|Briefly described|p266||Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|24210|5|Briefly described|p133 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||
19796|Westbourne Formation|29591|6|Mentioned|Table 15|||||||||
19796|Westbourne Formation|30021|6|Mentioned|p90|||||||||
19796|Westbourne Formation|30024|6|Mentioned|p332|||||||||
19796|Westbourne Formation|30102|5|Briefly described|p24|||Unit of the Injune Creek Group. See also P21,25,31,34.||||||
19796|Westbourne Formation|30103|5|Briefly described|p9|||Table 3 on P9. Upper Jurassic age.||||||
19796|Westbourne Formation|30104|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper Jurassic.M - U||||||
19796|Westbourne Formation|30508|6|Mentioned|p92|||Stratigraphic drilling||||||
19796|Westbourne Formation|30691|4|Described|p15|||See also Table 4. Upper Jurassic age||||||
19796|Westbourne Formation|30692|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|30695|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30696|4|Described|Table 4|||Middle-Upper Jurassic||||||
19796|Westbourne Formation|30699|6|Mentioned|p56|||Map||||||
19796|Westbourne Formation|30700|6|Mentioned|p27|||||||||
19796|Westbourne Formation|30702|6|Mentioned|Fig.1|||See also Table 1. Stratigraphic table||||||
19796|Westbourne Formation|30804|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|30853|5|Briefly described|Table 3|||Upper Jurassic age||||||
19796|Westbourne Formation|30854|4|Described|Table 4|||Upper Jurassic age||||||
19796|Westbourne Formation|30855|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Unit in Injune Creek Group||||||
19796|Westbourne Formation|30856|4|Described|Table 3|||On p10. Upper Jurassic age.||||||17-JAN-08
19796|Westbourne Formation|30857|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|Part of Injune Creek Group||||||
19796|Westbourne Formation|31116|4|Described|p36|||See also p27.||||||17-JAN-08
19796|Westbourne Formation|31120|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|31145|5|Briefly described|Table 1|||U. Jurassic||||||
19796|Westbourne Formation|31425|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|31431|5|Briefly described|Table 3|||M.-U.Jurassic||||||
19796|Westbourne Formation|31553|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|32138|6|Mentioned|p396|||||||||
19796|Westbourne Formation|32193|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33067|4|Described|Table 1|Late Jurassic|Jurassic|Of the Injune Creek Group.  Siltstone, shale, quartz sandstone.||||||07-JUL-04
19796|Westbourne Formation|33069|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|33071|5|Briefly described|p6|||M.-U.Jur.||||||
19796|Westbourne Formation|33075|6|Mentioned|p445|||||||||
19796|Westbourne Formation|33078|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33079|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33080|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33082|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33086|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle to Upper JurassicM - U||||||
19796|Westbourne Formation|33087|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33088|4|Described|Table 3|||U.Jur.||||||
19796|Westbourne Formation|33089|5|Briefly described|Table 2|||M.-U.Jur.||||||
19796|Westbourne Formation|33092|5|Briefly described|p9|||Stratigraphy||||||
19796|Westbourne Formation|33176|6|Mentioned|p175|||Correlated with Loth Fm.||||||
19796|Westbourne Formation|33183|6|Mentioned|p233|||||||||
19796|Westbourne Formation|33367|3|Fully described|p26|||||||||
19796|Westbourne Formation|33371|2|Defined|p58|Jurassic|Jurassic|See also p59. Prob. Jurassic.||||||17-JAN-08
19796|Westbourne Formation|33449|4|Described|Table 1|||U.Jur.||||||
19796|Westbourne Formation|33638|5|Briefly described|Table 1|||||||||
19796|Westbourne Formation|33639|5|Briefly described|Table 2|||||||||
19796|Westbourne Formation|33640|4|Described|Table 3|||M.-U.Jur.||||||
19796|Westbourne Formation|33643|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
19796|Westbourne Formation|33672|5|Briefly described|p44|||Lithology.||||||
19796|Westbourne Formation|33673|4|Described|p291|||See also p287||||||17-JAN-08
19796|Westbourne Formation|33821|6|Mentioned|Map legend|Late Jurassic|Late Jurassic|||||||
19796|Westbourne Formation|33825|5|Briefly described|p9,10|||Equiv. correl. Lithology. Correlation table.||||||
19796|Westbourne Formation|33827|6|Mentioned|p13|||||||||
19796|Westbourne Formation|33939|6|Mentioned|p412|||||||||
19796|Westbourne Formation|33998|6|Mentioned|p31|||||||||
19796|Westbourne Formation|34065|4|Described|p7|||U.Jur.||||||
19796|Westbourne Formation|34091|5|Briefly described|Table 1|||Jur.||||||
19796|Westbourne Formation|34134|6|Mentioned|Cor.Chart|||Middle Jurassic||||||
19796|Westbourne Formation|34174|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34218|4|Described|Table 1|||Upper Jurassic. See also Table 2.||||||
19796|Westbourne Formation|34386|6|Mentioned|p97|||Jurassic. See also P98,99,100 etc.||||||
19796|Westbourne Formation|34486|4|Described|Table 1|||See also Table 2, p10. Upper Jurassic.||||||17-JAN-08
19796|Westbourne Formation|34487|6|Mentioned|Map legend|Late Jurassic|Middle Jurassic|Middle - Upper JurassicM - U||||||
19796|Westbourne Formation|34611|6|Mentioned|Fig.65|||Correlation chart.||||||
19796|Westbourne Formation|35239|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|35560|6|Mentioned|p289|||||||||
19796|Westbourne Formation|35562|6|Mentioned|Table 4|||Biostratigraphy||||||
19796|Westbourne Formation|35663|5|Briefly described|p126|||||||||
19796|Westbourne Formation|35811|5|Briefly described|Table 3|||||||||
19796|Westbourne Formation|35937|6|Mentioned|Fig.5|||||||||
19796|Westbourne Formation|36243|6|Mentioned|Table 6A|||||||||
19796|Westbourne Formation|36251|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|36570|6|Mentioned|p55|||||||||
19796|Westbourne Formation|36910|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|37117|5|Briefly described|p313|||||||||
19796|Westbourne Formation|37287|6|Mentioned|p36|||||||||
19796|Westbourne Formation|37608|3|Fully described|Table 1|||||||||
19796|Westbourne Formation|37995|4|Described|p64|||||||||
19796|Westbourne Formation|38199|6|Mentioned|p423|||||||||
19796|Westbourne Formation|38226|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|38779|6|Mentioned|p7|||||||||
19796|Westbourne Formation|39070|4|Described|p363|||||||||
19796|Westbourne Formation|39212|5|Briefly described|p16|||See also P38||||||
19796|Westbourne Formation|39276|6|Mentioned|Fig. 2|||||||||
19796|Westbourne Formation|39445|5|Briefly described|Table 10|||||||||
19796|Westbourne Formation|39478|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|39494|6|Mentioned|p129|||See also Figs 3,5||||||
19796|Westbourne Formation|39846|6|Mentioned|p45|||||||||
19796|Westbourne Formation|39847|5|Briefly described|p36|||||||||
19796|Westbourne Formation|39914|6|Mentioned|p2|||||||||
19796|Westbourne Formation|39943|6|Mentioned|Table 8A|||||||||
19796|Westbourne Formation|39988|6|Mentioned|p289|||||||||
19796|Westbourne Formation|39989|4|Described|p422|||||||||
19796|Westbourne Formation|40030|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|40121|6|Mentioned|p446|||||||||
19796|Westbourne Formation|40199|6|Mentioned|Fig.1|||||||||
19796|Westbourne Formation|40245|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40249|6|Mentioned|p38|||Mention P41||||||
19796|Westbourne Formation|40250|6|Mentioned|Fig.7|||||||||
19796|Westbourne Formation|40540|6|Mentioned|p155|||||||||
19796|Westbourne Formation|40541|3|Fully described|p110|||||||||
19796|Westbourne Formation|40544|6|Mentioned|p159|||See also Fig.6||||||
19796|Westbourne Formation|40666|4|Described|p357|||||||||
19796|Westbourne Formation|40670|6|Mentioned|Fig.9|||||||||
19796|Westbourne Formation|40675|6|Mentioned|Table 8A|||Mention Table 9A||||||
19796|Westbourne Formation|40687|3|Fully described|p416|||||||||
19796|Westbourne Formation|40832|3|Fully described|p456|||||||||
19796|Westbourne Formation|40833|6|Mentioned|p468|||||||||
19796|Westbourne Formation|40910|6|Mentioned|Table 3|||||||||
19796|Westbourne Formation|40926|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|40962|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41060|6|Mentioned|p7|||Generalized stratigraphy||||||
19796|Westbourne Formation|41061|6|Mentioned|p19|||||||||
19796|Westbourne Formation|41062|6|Mentioned|p27|||See also P34 and Fig.5||||||
19796|Westbourne Formation|41063|6|Mentioned|p40|||||||||
19796|Westbourne Formation|41064|6|Mentioned|p60|||||||||
19796|Westbourne Formation|41084|5|Briefly described|p80|||See also Fig.2||||||
19796|Westbourne Formation|41097|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41099|6|Mentioned|p192|||||||||
19796|Westbourne Formation|41123|6|Mentioned|p177|||||||||
19796|Westbourne Formation|41175|5|Briefly described|p195|||||||||
19796|Westbourne Formation|41176|6|Mentioned|Table 2|||||||||
19796|Westbourne Formation|41177|6|Mentioned|p222|||||||||
19796|Westbourne Formation|41182|5|Briefly described|Fig.2|||||||||
19796|Westbourne Formation|41183|6|Mentioned|p310|||||||||
19796|Westbourne Formation|41186|4|Described|p208|||||||||
19796|Westbourne Formation|41187|6|Mentioned|Fig.2|||||||||
19796|Westbourne Formation|41198|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|41210|5|Briefly described|Fig.3|||||||||
19796|Westbourne Formation|41214|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41216|6|Mentioned|p300|||See also Fig.18||||||
19796|Westbourne Formation|41219|4|Described|p346|||||||||
19796|Westbourne Formation|41247|6|Mentioned|p120|||||||||
19796|Westbourne Formation|41266|6|Mentioned|Fig.3|||||||||
19796|Westbourne Formation|41681|6|Mentioned|p10|||See also P13||||||
19796|Westbourne Formation|41707|5|Briefly described|p163|||||||||
19796|Westbourne Formation|41724|6|Mentioned|p382|||||||||
19796|Westbourne Formation|41992|4|Described|Fig.2 P183|||||||||
19796|Westbourne Formation|42007|5|Briefly described|Fig.2 P182|||||||||
19796|Westbourne Formation|42061|4|Described|Fig,11 P159|||||||||
19796|Westbourne Formation|42067|4|Described|p308|||See also appendix 2||||||
19796|Westbourne Formation|42071|6|Mentioned|p117|||||||||
19796|Westbourne Formation|42084|6|Mentioned|Fig.3 P356|||||||||
19796|Westbourne Formation|42085|6|Mentioned|Fig.2 P374|||||||||
19796|Westbourne Formation|42397|5|Briefly described|p10|||||||||
19796|Westbourne Formation|42446|4|Described|p12|||||||||
19796|Westbourne Formation|42447|5|Briefly described|p5 + Fig. 1|||||||||
19796|Westbourne Formation|42463|6|Mentioned|Fig.5 P172|||||||||
19796|Westbourne Formation|42474|6|Mentioned|p25|||||||||
19796|Westbourne Formation|42493|5|Briefly described|p20, Fig.1 p18|||||||||
19796|Westbourne Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
19796|Westbourne Formation|42520|5|Briefly described|p6|||||||||
19796|Westbourne Formation|42634|6|Mentioned|p12|||||||||
19796|Westbourne Formation|42746|5|Briefly described|p9, p10|||See also Fig.6 P8, Fig.7 P37||||||
19796|Westbourne Formation|42749|4|Described|p30, Fig.5 p29|||see also Fig.2 p27.||||||17-JAN-08
19796|Westbourne Formation|42999|5|Briefly described|Table 2,p90||Late Jurassic|||||||
19796|Westbourne Formation|43000|5|Briefly described|Fig.5,p112|||of Injune Creek Group||||||
19796|Westbourne Formation|43002|5|Briefly described|Fig.2,p135|||||||||
19796|Westbourne Formation|43004|5|Briefly described|Table 1,p179|||||||||
19796|Westbourne Formation|43105|5|Briefly described|Fig.9,p15.|||||||||
19796|Westbourne Formation|43114|5|Briefly described|p12|||||||||
19796|Westbourne Formation|43122|5|Briefly described|p11|||see also Fig. 2.||||||
19796|Westbourne Formation|43404|14|Not recorded|Table p11||Late Jurassic|||||||
19796|Westbourne Formation|43591|6|Mentioned|p40|||||||||
19796|Westbourne Formation|43628|6|Mentioned|Fig.13||Late Jurassic|||||||
19796|Westbourne Formation|43711|6|Mentioned|p18|||||||||
19796|Westbourne Formation|43989|14|Not recorded|Map Legend|Late Jurassic|Middle Jurassic|||||||
19796|Westbourne Formation|44016|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44019|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44020|14|Not recorded|Tb.1,2|Late Jurassic|Middle Jurassic|Of Injune Creek Group.||||||
19796|Westbourne Formation|44021|14|Not recorded|p232-234,236-238||Late Jurassic|="Upper Intermediate Series" of Woolley 1941. Is upper part of Injune Creek Group. Overlies Birkhead Formation. Overlain by "Hooray Sandstone". Overlies Adori Sandstone. Plants and spores.||||||
19796|Westbourne Formation|44022|14|Not recorded|Map Legend||Late Jurassic|||||||
19796|Westbourne Formation|44023|4|Described|Tb.3,p12||Late Jurassic|||||||
19796|Westbourne Formation|44027|14|Not recorded|p110||Late Jurassic|||||||
19796|Westbourne Formation|44028|14|Not recorded|Fig.2,7,p514||Jurassic|Of Injune Creek Group. See Strat Table.||||||
19796|Westbourne Formation|44031|14|Not recorded|p5,8,12,13||Jurassic|||||||
19796|Westbourne Formation|44084|14|Not recorded|p32(Tb)|||||||||
19796|Westbourne Formation|44133|5|Briefly described|p110, 104 Fig. 9.11|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin. Conformably overlies: Adori Sandstone. Overlain and intertongued by Namur Sandstone.||||||28-SEP-16
19796|Westbourne Formation|44171|14|Not recorded|p194,19,197,198|||||||||
19796|Westbourne Formation|44337|5|Briefly described|Map Legend||Jurassic|Lithology.||||||
19796|Westbourne Formation|44374|14|Not recorded|p11|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44414|14|Not recorded|p112-115|Cretaceous|Jurassic|||||||
19796|Westbourne Formation|44415|14|Not recorded|Fig.2,p23|||||||||
19796|Westbourne Formation|45071|3|Fully described|Table 15|||See also p82.||||||17-JAN-08
19796|Westbourne Formation|45110|2|Defined|p97|Late Jurassic|Late Jurassic|See also Fig.5 and p24.||||||17-JAN-08
19796|Westbourne Formation|46791|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
19796|Westbourne Formation|46939|6|Mentioned|Fig.2|||See also Fig.1.||||||
19796|Westbourne Formation|46984|6|Mentioned|Table 1|||||||||
19796|Westbourne Formation|48919|4|Described|p63|||U.Jurassic. See also p64-65.||||||17-JAN-08
19796|Westbourne Formation|48920|3|Fully described|p53|||Part of Injune Creek Group.||||||16-SEP-08
19796|Westbourne Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
19796|Westbourne Formation|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
19796|Westbourne Formation|60717|5|Briefly described|p40 Fig. 2|Late Jurassic|Late Jurassic|Overlies Adori Sandstone; overlain by Murta Formation; lateral to Adori Sandstone? Geological Province: Eromanga  Basin.||||||31-JAN-08
19796|Westbourne Formation|60993|5|Briefly described|p36|||Of the Injune Creek Group. May be the equivalent of the upper sandstone section of the Woodenbong beds. Geological Province: Surat Basin.||||||
19796|Westbourne Formation|60999|5|Briefly described|p178 Fig. 10|||Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61000|5|Briefly described|p186 Fig. 4|Tithonian|Callovian|Geological Province: Surat Basin.||||||
19796|Westbourne Formation|61312|5|Briefly described|p67 Fig. E5|Late Jurassic|Jurassic|Of the Injune Creek Group. Siltstone, shale and fine-grained quartzose sandstone; productive reservoir unit. Geological Province: Eromanga Basin. See also p79 Table E2.||||||
19796|Westbourne Formation|61377|5|Briefly described|p148 Tb. SU1|Late Jurassic|Jurassic|Shale, siltstone, quartz sandstone, minor coal. Geological Province: Surat Basin. See also p149 Fig. SU8.||||||07-FEB-11
19796|Westbourne Formation|61611|6|Mentioned|p265 Fig. 3|Late Jurassic|Early Cretaceous|Geological Province: Surat Basin and Eromanga Basin.||||||13-MAR-09
19796|Westbourne Formation|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61614|6|Mentioned|p290 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||17-MAR-09
19796|Westbourne Formation|61615|6|Mentioned|p302 Fig. 2|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|61823|5|Briefly described|p118|Cretaceous|Jurassic|Fluvial-lacustrine sediments. Geological Province:  Eromanga Basin.||||||
19796|Westbourne Formation|62730|5|Briefly described|p352 Fig. 1|Late Jurassic|Late Jurassic|Geological Province: Eromanga Basin.||||||21-APR-08
19796|Westbourne Formation|63218|6|Mentioned|p211 Fig.2. |Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.|Includes Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|63979|4|Described|p38-39, Fig. 44|Tithonian|Oxford|Conformable on Adori Sst; overlain by/intertongues with Hooray Sst. and "upper Namur Sst". Max.thickness:166m. Fine to v.fine, rarely med.- to coarse-gr. sst, moderately to poorly sorted, interlaminated/interbedded with siltst.+ shale. In Eromanga Basin.||||||07-FEB-11
19796|Westbourne Formation|64048|5|Briefly described|p64 Tb. 2, p70|||Geological Province: Eromanga Basin. Possesses some hydrocarbon source potential.||||||07-FEB-11
19796|Westbourne Formation|64197|6|Mentioned|p625 Fig.1c, p630 Fig.7|Late Jurassic|Late Jurassic|Eromanga and Surat/Bowen Basins.||||Eromanga Basin: overlies Adori Sandstone; underlies Hooray Sandstone. Surat/Bowen Basins: overlies Springbok Sandstone; underlies Gubberamunda Sandstone.||11-DEC-15
19796|Westbourne Formation|64665|5|Briefly described|p53 Fig.2, p60.|Late Jurassic|Late Jurassic|Eromanga and Surat Basins. Contains thin coals.||Upper unit in Injune Creek Group.||Overlies Adori and Springbok Sandstones.||
19796|Westbourne Formation|64856|3|Fully described|p79, p88-95|Tithonian|Oxfordian|Defined by American Overseas Petroleum Ltd (1964) with a type section 389-503m in AOP Westbourne 1 well. Eromanga and Surat Basins. Interbedded shales and siltstones and very fine-grained, quartzose sandstones. Includes Norwood Mudstone Member. Conformably overlies the Springbok Sandstone, intertongues and grades into the Pilliga Sandstone to south. Underlies Gubberamunda Sandstone. Up to 220m thick. Age from palynoflora (units APJ5, 6).||||||18-JAN-22
19796|Westbourne Formation|64857|5|Briefly described|p113 Fig.3, p115|||Overlies Springbok Sandstone, Surat Basin.||||||
19796|Westbourne Formation|64858|6|Mentioned|p181 Tb.1, p187-188|||Surat Basin.||||||30-NOV-09
19796|Westbourne Formation|65003|5|Briefly described|p8||Jurassic|Of Surat Basin.||||||
19796|Westbourne Formation|65112|5|Briefly described|p323; p328; Fig 11 p 324; fig 16 p328|Jurassic|Jurassic||156-142 Ma.|||Overlies Springbok Sandstone, underlies Gubberamunda Sandstone.|Non-marine, upward-fining clastic sedimentary rock. A package with a lower sand-rich part, followed by a shale-rich unit.|22-MAR-12
19796|Westbourne Formation|65113|5|Briefly described|Fig 4 p340|Late Jurassic|Late Jurassic|Overlies the Springbok Formation, underlies Gubberamunda Sandstone.||||||
19796|Westbourne Formation|65114|5|Briefly described|p385 Fig.3|Late Jurassic||||||||
19796|Westbourne Formation|65116|5|Briefly described|Fig 2 p437|Late Jurassic|Late Jurassic|Underlies the Gubberamunda Sandstone, overlies the Springbok Sandstone, Surat Basin.||||||06-MAR-12
19796|Westbourne Formation|65117|5|Briefly described|p463, 471-472,  474,  Fig 4 p465|Tithonian|Oxfordian|Surat Basin, up to 200m thick. Conformable on Springbok Sandstone. Diachronous base. Older in Surat than Eromanga Basins. Interbedded mudstone, siltstone, coal and very fine grained quartzose to lithic-feldspathic sandstone.||||||
19796|Westbourne Formation|65119|6|Mentioned|Fig 6 p512, Fig 13-14|||Present in the Cabawin 1 and Rockwood 1 wells.||||||07-MAR-12
19796|Westbourne Formation|65238|5|Briefly described|p10|||Geological province: Eromanga Basin. Overbank and lacustrine-swamp deposits.||||||
19796|Westbourne Formation|65385|5|Briefly described|pS134 Fig.7|Late Jurassic|Late Jurassic|Of Eromanga Basin. Overlies Adori Sandstone. Sediment with volcanic component. See also "uppermost Westbourne Formation".||||||08-MAR-12
19796|Westbourne Formation|65489|5|Briefly described|p15, p49, p96, p155|Late Jurassic|Late Jurassic|Eromanga Basin. 210m thick. Fair source rock. Potential for stratigraphic structural traps. Oil reservoir accounting for 4% of the Basin's production.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|66529|6|Mentioned|p12 Fig.5|||Eromanga Basin.||Unit in Injune Creek Group.||Overlies Adori or Springbok Sandstones. Is overlain by Namur, Hooray or Gubberamunda Sandstones.||
19796|Westbourne Formation|66623|6|Mentioned|p239.|Early Cretaceous|Late Jurassic|||||||
19796|Westbourne Formation|66915|5|Briefly described|p6 Fig.3|Early Cretaceous|Late Jurassic|Eromanga and Surat Basins. In Fig.3 also shows "uppermost Westbourne Formation" in Eromanga Basin.||Injune Creek Group||||
19796|Westbourne Formation|67133|5|Briefly described|p2, p5, p15-16, p18-21|Jurassic|Jurassic|32 samples of this unit were analysed by XRD and optical microscopy for this study. Deposited in a lacustrine delta environment. Quartz is the main component (18-80%) with feldspars (12-40%); plagioclase is always dominant. Kaolinite (up to 33%) is the dominant clay mineral. The mixed-layer clays are highly variable.||||Conformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.|Very fine- to medium-grained, fairly to poorly sorted, sublabile to quartzose, often massive sandstones with laminated to thinly-bedded siltstones and shales.|
19796|Westbourne Formation|67323|5|Briefly described|p87-88, p93, p95 Fig.12.5|Late Jurassic|Late Jurassic|Eromanga Basin. Hydrocarbon exploration target in the Basin.||||Overlies Adori Sandstone. Is overlain by Hooray Sandstone.||
19796|Westbourne Formation|67402|4|Described|p26, p26 tbl RRM4, p108|Berriasian|Oxfordian|Eromanga Basin. Potential conventional seal for the storage of carbon dioxide. Proven seal of the Springbok Formation. Deposited in fluvial to fluvio-lacustrine environments during a series of regressive-transgressive cycles. Maximum thickness of 160m. Demonstrated hydrocarbon seal. See also p109, p113, p115, p123, p146, p148, p151, p152, p154 fig SRT15/16, p156, p226, p265.||||Overlies the Adori Sandstone. Conformably overlies the Springbok Sandstone. Overlain by the Hooray Sandstone.|Fine to very fine-grained sandstone, interlaminated and interbedded with siltstone and shale.|
19796|Westbourne Formation|67561|5|Briefly described|p52 Fig.2, p58 Fig.7, p59 Fig.8|Valanginian|Berriasian|Australian Spore-Pollen zonation: C.watherooensis.||||||
19796|Westbourne Formation|68003|5|Briefly described|p57 Fig.3-n.|||Bowen Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68117|5|Briefly described|p345-346|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.|Norwood Mudstone Member.|Overlies Springbok Sandstone.||
19796|Westbourne Formation|68135|5|Briefly described|p52 fig 2b, p57 fig 4|Tithonian|Kimmeridgian|Surat Basin (QLD) and Eromanga Basin.||||Overlies Springbok and Adori Sandstones. Is unconformably overlain by Gubberamunda, Hooray and Namur Sandstones.|Interbedded sandstone and siltstone.|15-SEP-17
19796|Westbourne Formation|68139|6|Mentioned|p23|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Unconformably overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|68279|6|Mentioned|p18-19|||Galilee Basin stratigraphic cross-sections, and mineralogy tables.||||||
19796|Westbourne Formation|68576|5|Briefly described|Q_4: p3|Late Jurassic|Late Jurassic|Surat Basin.||Injune Creek Group.||Overlies Springbok Sandstone. Is overlain unconformably by Gubberamunda Sandstone.||
19796|Westbourne Formation|68731|6|Mentioned|pp209-211|||||||||
19796|Westbourne Formation|69001|6|Mentioned|p16|Early Cretaceous|Jurassic|Recent interpretations by the NSW DPI broadly group this unit within the Algebuckina Sandstone and equivalent units.||||||
19796|Westbourne Formation|69019|5|Briefly described|p85 Fig.21.|Berriasian|Tithonian|Southern Eromanga Basin.||||Overlies Adori Sandstone. Is overlain by Namur Sandstone.||
19796|Westbourne Formation|69023|6|Mentioned|p89 Fig.20, p91|Berriasian|Tithonian|||||Intertongues with lower part of Namur Sandstone.||
19796|Westbourne Formation|69457|6|Mentioned|p41:3-4|||Eromanga Basin.||||||12-JUL-16
19796|Westbourne Formation|69582|5|Briefly described|p36, p38, p65-p66|Late Jurassic|Late Jurassic|Eromanga Basin. Intersected in GSQ Longreach 2 drillhole.||||Overlies the Springbok Sandstone and the Adori Sandstone. Unconformably overlain by the Gubberamunda Sandstone. Overlain by the Hooray Sandstone.|Mudstone, sandstone, siltstone.|
19796|Westbourne Formation|69594|3|Fully described|p519, p525-527, p531, p537, p573|Tithonian|Kimmeridgian|Exon (1966). Swarbrick et al. (1973) defined the lower part as the Norwood Mudstone Member. Eromanga, northern Surat Basins. The type section is 390-503m in AOP Westbourne 1, near Tambo. Discrimination from Adori Sandstone described. Along the SA border, the Namur Sandstone, Westbourne Formation and Adori Sandstone cannot be delineated. Up to 250m thick. Basal fluviatile, later lacustrine deposits. Has hydrocarbon source potential; is a significant reservoir. RELATED UNITS (continued): Is overlain by and interfingers with both Namur and Hooray Sandstones; is overlain conformably to unconformably by the upper Namur Sandstone; and Gubberamunda Sandstone conformably (locally disconformably).||Injune Creek Group.|Norwood Mudstone Member.|Conformably overlies Adori and Springbok Sandstones. Interdigitates with and passes into Pilliga Sandstone. See COMMENTS for more.|Fine, very fine, rarely medium or coarse, labile micaceous sandstones with interbedded siltstone and shale.|
19796|Westbourne Formation|69673|6|Mentioned|p154, p155 fig 127|Cretaceous|Jurassic|||||Overlies Adori Sandstone, overlain by Namur Sandstone||
19796|Westbourne Formation|69681|6|Mentioned|p74 Fig.3, p82|Late Jurassic|Late Jurassic|Mineralogy and likely chemical changes from CO2 injection discussed.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69682|5|Briefly described|p95 Fig.3|Late Jurassic|Late Jurassic|Surat Basin.||Unit in Injune Creek Group.||Overlies Springbok Sandstone. Is overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|69790|6|Mentioned|p1063 Fig.2, p1068 Fig.7|Late Jurassic|Late Jurassic|Eromanga Basin.||Unit in Injune Creek Group.||||
19796|Westbourne Formation|69797|5|Briefly described|p17 Fig.2|Late Jurassic|Late Jurassic|Geol. Prov: Eromanga Basin. Presented in figure as Westbourne Fm.||||||
19796|Westbourne Formation|69946|3|Fully described|p11, p15-16, p24, p57-58|Early Cretaceous|Late Jurassic|Named by Gerrard (1964) in an unpublished well completion report; Exon (1966) published the definition and assigned the type section: the interval 389.8 - 503.0m in Westbourne 1. Restricted to N Cooper region and easternmost Pedirka region in SA. 30 - 140m thick. Eromanga Basin. Wireline log correlations.||||Conformably overlies Adori Sandstone. Intertongues with overlying Namur and Algebuckina Sandstones.|Interbedded dark grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|69947|5|Briefly described|p7-8, p13 Fig.7.2, p31 Fig.7.20|Early Cretaceous|Late Jurassic|Eromanga Basin. Forms a couplet with Adori Sandstone, restricted to northern Cooper region and eastern-most Perdika region.||||Gradationally overlies Adori Sandstone. Is overlain by Namur Sandstone.|Dark grey shale, siltstone and minor sandstone interbeds.|
19796|Westbourne Formation|70374|6|Mentioned|p809 figure 1, p814|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Overlies ?conformably Springbok Sandstone.||28-SEP-16
19796|Westbourne Formation|70628|6|Mentioned|p952, Fig 4|Kimmeridgian|Kimmeridgian|Shown only as 'Westbourne' in fig 4. Along with Gubberamunda [Sandstone], Springbok Formation,  forms part of the L-sequence (Hoffman et al 2009) of the Surat Basin.||||Underlies Gubberamunda Sandstone. Overlies Springbok Formation.||
19796|Westbourne Formation|70821|5|Briefly described|p21 Fig.2.6, p80|Jurassic|Jurassic|Eromanga and Surat Basins. Aquitard.||Injune Creek Group.||Overlies Adori Sandstone and Springbok Sandstone. Is overlain by Namur Sandstone, Hooray Sandstone and Gubberamunda Sandstone.||
19796|Westbourne Formation|70823|5|Briefly described|p25-p27, p43, p78|Late Jurassic|Middle Jurassic|Eromanga Basin. Deposited in low-energy meandering fluvial and overbank floodplain environments.||||Overlies the Adori Sandstone. Overlain by the Namur Sandstone.||
19796|Westbourne Formation|70824|5|Briefly described|p9|Jurassic|Jurassic|Eromanga Basin.||||Overlies the Adori Sandstone. Overlain by the Murta Formation and the Hooray and Namur Sandstones.||
19796|Westbourne Formation|70860|6|Mentioned|p281|||Great Artesian Basin.||||||
19796|Westbourne Formation|71282|6|Mentioned|p457 Fig.1|||Appears just as Westbourne in Fig.1.||||||
19796|Westbourne Formation|71321|6|Mentioned|p15|||Of Eromanga Basin.||||||
19796|Westbourne Formation|71342|4|Described|Ch1 p19, Ch5 p12, Ch5 p15-p17, Ch5 p24|Berriasian|Tithonian|Originally defined by Gerrard (1964) in the Boree 1 unpublished well completion report, however, it was first published by Exon (1966) who defined it and assigned the type section. The type section is in Westbourne 1 in Queensland (Exon, 1966). This unit is generally 30 to 140m thick in the Cooper region. Spore-pollen zone is given in Ch5 p57. Interpreted to have been deposited in a lacustrine environment. Sedimentary characteristics are briefly discussed. See also  Ch5 p57-p58, Ch7 p7-p8, Ch7 p13, Ch8 p5, Ch8 p10, Ch8 p17, Ch13 p4, Ch13 p9.||||Conformably overlies the Adori Sandstone. Conformably overlain by the Namur and Algebuckina Sandstones. This unit intertongues with, and is laterally equivalent to the Algebuckina Sandstone.|Interbedded darky grey shale and siltstone with minor sandstone interbeds.|
19796|Westbourne Formation|71806|6|Mentioned|p484|Jurassic|Jurassic|Surat Basin.||||||
19796|Westbourne Formation|71863|6|Mentioned|p5|Valanginian|Berriasian|NE Eromanga Basin. Shown as "uppermost Westbourne Formation".||||||
19796|Westbourne Formation|72297|6|Mentioned|p739, p742|||Eromanga Basin. Petroleum reservoir, with marginal source rock potential.||||||
19796|Westbourne Formation|72298|5|Briefly described|p801|Jurassic|Jurassic|Eromanga Basin (SA,QLD,NSW), Surat Basin (QLD,NSW).||Injune Creek Group.||Overlies Adori or Springbok Sandstone. Is overlain by Namur and Hooray Sandstones.||
19796|Westbourne Formation|72921|5|Briefly described|p15 Fig.2, p16.|Late Jurassic|Late Jurassic|Shown as located in the Surat Basin in Queensland and the Eromanga Basin.||||Overlies and is laterally equivalent to Adori Sandstone and underlies Namur Sandstone and Hooray Sandstone.|May include siltstone.|
19796|Westbourne Formation|73113|5|Briefly described|p. 22-24, 31, 36-37, 41, 49, 66-67...|||Surat Basin. Tight aquitard. More locations: p. 69, 71, 78, 80, 98, 115-116, 119, 128-129, 148-149, 152, 167, 169-172, 177-178, 191.||||Underlain by Springbok Sandstone. Overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Jurassic|Eromanga Basin. Contains oil.||||||
19796|Westbourne Formation|73193|6|Mentioned|p369|Tithonian|Kimmeridgian|Surat Basin.||Injune Creek Group||Underlain by Springbok Sandstone. Unconformably overlain by Gubberamunda Sandstone.||
19796|Westbourne Formation|73200|6|Mentioned|p533|Jurassic|Jurassic|||||||
19796|Westbourne Formation|73251|6|Mentioned|p62|Late Jurassic|Late Jurassic|Eromanga Basin. Deposited in a braided-meandering fluvial setting. Oil show.||||Underlain by Adori Sandstone. Overlain by and equivalent to Namur Sandstone. Equivalent to Algebuckina Sandstone.||
19796|Westbourne Formation|73343|6|Mentioned|p337|Jurassic|Jurassic|Eromanga Basin. Hosts oil.||||Underlain by Adori Sandstone. Overlain by Hooray Sandstone.||
19796|Westbourne Formation|73393|6|Mentioned|p20-21|Tithonian|Tithonian|Surat and Eromanga Basins.||Injune Creek Group||Underlain by Adori Sandstone. Underlain by and equivalent to Springbok Sandstone.||
19796|Westbourne Formation|73479|5|Briefly described|p156 Fig.2, p159|Jurassic|Jurassic|Eromanga Basin. Braided fluvial-lacustrine depositional environment.|ca 150 Ma|||Overlies Adori Sandstone, underlies Hooray Sandstone||
19817|Western Sands|41290|6|Mentioned|Fig.5|||||||||
19834|Westley Park Sandstone Member|22433|5|Briefly described|p12 Table 1|||in the Sydney Basin||||||
19834|Westley Park Sandstone Member|22488|5|Briefly described|p841|||||||||
19834|Westley Park Sandstone Member|22578|6|Mentioned|p394|||||||||
19834|Westley Park Sandstone Member|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Of the Broughton Formation (Shoalhaven Group). Geological Province: Sydney Basin.||||||
19834|Westley Park Sandstone Member|23544|4|Described|Table 1 p360.|||also see p358-59 + Fig 2 p358. Of the Broughton Formation.||||||
19834|Westley Park Sandstone Member|23896|3|Fully described|p249, p264 App.1|Late Permian|Late Permian|Of Broughton Formation. See also p250 Table 1.  Overlain by Blow Hole Latite Member. Geological Province: Sydney Basin.||||||
19834|Westley Park Sandstone Member|29900|6|Mentioned|Table 2|||||||||
19834|Westley Park Sandstone Member|29901|4|Described|Table 1|||||||||
19834|Westley Park Sandstone Member|31128|6|Mentioned|Table 1|||||||||
19834|Westley Park Sandstone Member|36220|6|Mentioned|p37|||See also Table 1.||||||
19834|Westley Park Sandstone Member|39308|4|Described|p517|||Fossils at Black Head||||||
19834|Westley Park Sandstone Member|40270|6|Mentioned|p177|||||||||
19834|Westley Park Sandstone Member|41580|5|Briefly described|p9|||||||||
19834|Westley Park Sandstone Member|41832|6|Mentioned|p569|||||||||
19834|Westley Park Sandstone Member|45090|6|Mentioned|p171|||Refers Hanlon et al. (1953). Gerringong Volcanics||||||
19834|Westley Park Sandstone Member|67500|5|Briefly described|p11, 12, p12 Tb.1|Late Permian|Late Permian|Includes marine faunas||Of the Broughton Formation and Gerringong volcanic facies.|||Green-grey volcaniclastic sandstone, with locally abundant marine fossils. Displays evidence of large dropstones and glendonites.|01-MAY-12
19834|Westley Park Sandstone Member|71115|5|Briefly described|p180, 188|Permian|Permian|Southern Sydney Basin.||Broughton Formation.||Is overlain by Blow Hole Latite Member.||
19834|Westley Park Sandstone Member|71542|4|Described|p23,25,29-33|Late Permian|Late Permian|Of southern Sydney Basin. Thickness: approximately 190m. Complete succession can be seen at Mount Coolangatta. Interpreted as a sedimentary apron surrounding a volcanic vent on the NW edge of the magmastic arc in the Currarong Orogen, possibly part of a larger volcaniclastic apron surrounding a larger volcano 40km to the SE (vicinity of, or SE of Jervis Bay). Includes abundant body fossils at a few locations. Porphyritic igneous units are intercalated, extrusively and contemporaneously with sandstone beds, likely shed of the volcano as lahars, debris flow and turbidites. Top of the unit is marked by a breccia immediately below the first latite unit of the Broughton Fomation.||Unit of Broughton Formation.||Conformably overlies the Berry Formation. Includes Koo-Lee Tuff Member, Back Forest Tuff Bed. Overlain by Coolangatta Latite Member.|Fine- to coarse-grained volcanic-derived litharenite and bioturbated fine-grained sandstone. Tuff bed. Conglomerate beds. Breccia unit marks top.|20-OCT-21
19834|Westley Park Sandstone Member|73421|6|Mentioned|p18|||||Broughton Formation||Underlies Blowhole Latite||
19834|Westley Park Sandstone Member|73494|5|Briefly described|p542|Permian|Permian|Southern Sydney Basin. Late Permian.||Broughton Formation.||||
19873|Whinstone Basalt|32820|6|Mentioned|p7|||||||||
19873|Whinstone Basalt|36413|3|Fully described|p124|||||||||
19873|Whinstone Basalt|36414|5|Briefly described|map legend|Tertiary|Tertiary|Olivine basalt. GSNSW map code: Tb.||||||
19873|Whinstone Basalt|39626|6|Mentioned|p276|||||||||
19880|Whistle Waa Granite|23214|3|Fully described|p158|Late Silurian|Late Silurian|Intrudes Walli Volcanics. Forms a large elongate body more than 25km long and up to 8km wide. Geological Province: Wyangala Batholith||||||
19880|Whistle Waa Granite|42726|5|Briefly described|map legend|Silurian||||||||
19880|Whistle Waa Granite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Coarse to medium grained bitotie granite; scattered xenoliths.||||||15-JUL-08
19880|Whistle Waa Granite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||12-JUN-08
19880|Whistle Waa Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of the Cowra Suite. Coarse- to medium-grained, equigranular, biotite granite with occasional xenoliths.||||||12-JUN-08
19880|Whistle Waa Granite|68592|2|Defined|p1225, p1227, p1229-31, p1234, p1236-8|Late Silurian|Late Silurian|See also p1260. Originally mapped by Stevens (1955). Named and mapped by Chappell et al. (1991); subsequent mapping by Raymond et al. (1998). Named after Big Whistle Waa and Little Whistle Waa hill tops. Type area described. Geochemistry detailed; geophysical properties described. Very low magnetic susceptibility. Cannot be distinguished from Wyangala Granite on radiometric or magnetic images, but contrasts strongly with Kenyu Formation. Southern portion has now been included in Wyangala Granite. Age from geochemical association with Cowra Granodiorite.||Unit in Cowra Suite.||Inferred fault contact with Kenyu Formation and intrudes Walli Volcanics.|Grey, coarse- to medium-grained, equigranular, biotite granite with sparse xenoliths. Peraluminous, S-type.|
19880|Whistle Waa Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Saw. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Cowra Suite|||Coarse-medium grained, equigranular, biotite granite with sparse xenoliths; low magnetic susceptibility.|
19880|Whistle Waa Granite|70297|5|Briefly described|map legend|Silurian|Silurian|||Wyangala Supersuite||||
19880|Whistle Waa Granite|70545|5|Briefly described|Map Legend|Silurian|Silurian|||Cowra Suite|||Coarse-medium grained, equigranular, biotite granite with sparse xenoliths; low magnetic susceptibility.|
19914|White Tank Limestone Member|730|6|Mentioned|p24.|||Unit of Meryula Formation of Kopyje Group. Contains conodonts. Compared wth limestone near Stoney Tank, Bourke map sheet area, and the Kerrigundi area on the Louth 1:250 k sheet.||||||11-NOV-14
19914|White Tank Limestone Member|22857|5|Briefly described|p442 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Meryula Formation (Kopyje Group, Cobar Supergroup). Max. thickness: <300m. Geological Province: Kopyje Shelf (Darling Basin).||||||
19914|White Tank Limestone Member|23171|6|Mentioned|p31|||||||||
19914|White Tank Limestone Member|23173|6|Mentioned|Map Legend|||||||||
19914|White Tank Limestone Member|23522|5|Briefly described|p253|Middle Devonian|Early Devonian|||||||
19914|White Tank Limestone Member|35287|6|Mentioned|p7|||||||||
19914|White Tank Limestone Member|36118|6|Mentioned|p67|||||||||
19914|White Tank Limestone Member|39618|2|Defined|p74|Early Devonian|Early Devonian|||||||
19914|White Tank Limestone Member|40624|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
19914|White Tank Limestone Member|43032|5|Briefly described|p80|||of Meryula Formation||||||
19914|White Tank Limestone Member|65469|6|Mentioned|p15, p17|||Lachlan Orogen.||Meryula Formation||||
19914|White Tank Limestone Member|68823|6|Mentioned|p377|Lochkovian|Lochkovian|||Of the Meryula Formation.|||Limestone.|
19914|White Tank Limestone Member|70941|6|Mentioned|p147|Lochkovian|Lochkovian|Age based on conodont faunas.||Meryula Formation||||
19914|White Tank Limestone Member|71039|6|Mentioned|p13|||||Meryula Formation||||
19914|White Tank Limestone Member|73143|6|Mentioned|p8-9|Devonian|Devonian|Contains Caudicriodus woschmidti conodonts (Pickett, 1980) and (Drygant, 2010), one specimen was reidentified as Cypricriodus hesperius suggesting earliest Devonian age (Murphy et al., 2016). Younger (Pragian) age proposed by Mathieson et al., (2016).||Meryula Formation||||
19914|White Tank Limestone Member|73174|6|Mentioned|p1039|Lochkovian|Lochkovian|Contains early Lochkovian age-diagnostic conodont.||Meryula Formation, Kopyje Group, Cobar Supergroup||||24-NOV-22
19917|Whitebridge Conglomerate Member|23055|6|Mentioned|Fig13p25|||||||||
19917|Whitebridge Conglomerate Member|29922|6|Mentioned|p49|||||||||
19917|Whitebridge Conglomerate Member|29926|6|Mentioned|Fig.3|||||||||
19917|Whitebridge Conglomerate Member|33867|6|Mentioned|Fig.3|||||||||
19917|Whitebridge Conglomerate Member|34351|6|Mentioned|p344|||Fig.5.13||||||
19917|Whitebridge Conglomerate Member|37083|6|Mentioned|p164|||||||||
19917|Whitebridge Conglomerate Member|39292|6|Mentioned|Fig. 6.2|||||||||
19917|Whitebridge Conglomerate Member|41479|6|Mentioned|Fig.2|||||||||
19917|Whitebridge Conglomerate Member|43447|14|Not recorded|diag.p26|||Cardiff Sub-Group||||||
19917|Whitebridge Conglomerate Member|68711|6|Mentioned|p116 Tbl 2|||This Member has been dropped. See also p113.||Formerly of Kahibah Formation.||||
19944|Whybrow Coal Member|29942|4|Described|Fig.1|||Permian||||||
19944|Whybrow Coal Member|29944|6|Mentioned|Fig.18|||||||||
19944|Whybrow Coal Member|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19944|Whybrow Coal Member|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
19944|Whybrow Coal Member|40805|6|Mentioned|Table 1|||||||||
19944|Whybrow Coal Member|45090|6|Mentioned|p225|||U. Tatarian||||||
19944|Whybrow Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Mount Leonard Formation.||||
19948|Whychetella Formation|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Mudstone. Max. thickness: 380m. Geological Province: Cowra Trough.||||||
19948|Whychetella Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Toongi Group.||||||
19948|Whychetella Formation|23170|2|Defined|p120|Late Silurian|Late Silurian|of Toongi Group.||||||
19948|Whychetella Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
19948|Whychetella Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
19948|Whychetella Formation|40328|4|Described|p130|||||||||
19948|Whychetella Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
19948|Whychetella Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group.  Mudstone.||||||
19948|Whychetella Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Pridoli|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion. Mis-spelt as Whychetalla Formation on p24.||Unit in Toongi Group.||Overlies Wirrabilla Formation. Is overlain by Dowd Formation.|Mudstone.|
19959|Wiagdon Granite|23214|3|Fully described|p256|Carboniferous|Carboniferous|Intrudes the Chesleigh Formation. Forms an oval shaped body 5 x 3km.  I-type granite.||||||
19959|Wiagdon Granite|29993|6|Mentioned|Map legend|Middle Carboniferous|Middle Carboniferous|||||||
19959|Wiagdon Granite|33006|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
19959|Wiagdon Granite|33282|6|Mentioned|Map legend|Middle Carboniferous|Early Carboniferous|Lower to Middle Carboniferous||||||
19959|Wiagdon Granite|33285|6|Mentioned|p72|||||||||
19959|Wiagdon Granite|34404|6|Mentioned|Fig.3.5b|||||||||
19959|Wiagdon Granite|39331|6|Mentioned|Fig.7-1|||||||||
19959|Wiagdon Granite|42726|5|Briefly described|map legend|Carboniferous||10.  Of the Gulgong Suite (Bathurst Supersuite).||||||07-FEB-05
19959|Wiagdon Granite|43127|6|Mentioned|p14|||Bathurst sheet 8831.||||||
19959|Wiagdon Granite|43515|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(Provisional Edition) (L.-M.Carb)||||||
19959|Wiagdon Granite|43516|14|Not recorded|Map Legend|Early Carboniferous|Early Carboniferous|(L.-M.Carb.)||||||
19959|Wiagdon Granite|43517|14|Not recorded|p156,Map Plate XII|||Probably part of or related to Bathurst Granite||||||
19959|Wiagdon Granite|43641|5|Briefly described|Map Legend||Carboniferous|||||||
19959|Wiagdon Granite|43782|5|Briefly described|Map Legend|Late Carboniferous|Early Carboniferous|||||||
19959|Wiagdon Granite|70297|5|Briefly described|map legend|Carboniferous|Carboniferous|||Bathurst Supersuite||||
19967|Wianamatta Group|22500|5|Briefly described|p 6||Triassic|Sydeny Basin||||||
19967|Wianamatta Group|22663|5|Briefly described|NSW97 - 1 p2||Middle Triassic|||||||01-MAR-10
19967|Wianamatta Group|22745|5|Briefly described|p125|Ladinian|Anisian|Sydney Basin. 300 m.||||||
19967|Wianamatta Group|22833|6|Mentioned|p653|||of Sydney Basin.||||||
19967|Wianamatta Group|22857|4|Described|p265, p530 App.1 Tb.A1.9|Middle Triassic|Middle Triassic|Includes Bringelly and Ashfield Shales and Minchinbury Sandstone. Geological Province: Sydney Basin. See also p526 App.1 Tb.A1.9.||||||
19967|Wianamatta Group|22864|6|Mentioned|p265|||||||||
19967|Wianamatta Group|22865|6|Mentioned|p309|||||||||
19967|Wianamatta Group|22892|5|Briefly described|p7 fig6|Triassic|Triassic|||||||
19967|Wianamatta Group|22969|4|Described|p 26, Fig 2.2|Middle Triassic|Middle Triassic|||||||
19967|Wianamatta Group|22970|5|Briefly described|Plate 6||Triassic|||||||
19967|Wianamatta Group|23218|5|Briefly described|Diagram p4, 9, Map. p17|Triassic|Triassic|||||||
19967|Wianamatta Group|23219|5|Briefly described|Map Legend||Triassic|||||||
19967|Wianamatta Group|23450|6|Mentioned|p527 Fig.1|||||||||
19967|Wianamatta Group|24079|5|Briefly described|p433|Triassic|Triassic|Geological Province: Sydney Basin. Maximum thickness: 230m.||||||
19967|Wianamatta Group|24117|6|Mentioned|p85|||Geological Basin: Sydney Basin.||||||
19967|Wianamatta Group|24123|5|Briefly described|p3|||Geological Province: Sydney Basin.||||||
19967|Wianamatta Group|24240|5|Briefly described|p21|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin.||||||
19967|Wianamatta Group|24478|5|Briefly described|p14-15|||Shale. Overlies Hawkesbury Sandstone.||||||
19967|Wianamatta Group|29361|5|Briefly described|p4|||||||||
19967|Wianamatta Group|29591|5|Briefly described|p97|||||||||
19967|Wianamatta Group|29901|4|Described|Table 1|||||||||
19967|Wianamatta Group|29922|6|Mentioned|Appendix 1|||||||||
19967|Wianamatta Group|29924|6|Mentioned|p13|||||||||
19967|Wianamatta Group|30006|4|Described|p73|||||||||
19967|Wianamatta Group|30132|6|Mentioned|p4|||||||||
19967|Wianamatta Group|30228|6|Mentioned|p17|||Lithology. Triassic age.||||||
19967|Wianamatta Group|30229|4|Described|p2020|||||||||
19967|Wianamatta Group|30285|6|Mentioned|p546|||||||||
19967|Wianamatta Group|30286|6|Mentioned|p1094|||||||||
19967|Wianamatta Group|30427|6|Mentioned|p40|||||||||
19967|Wianamatta Group|30465|6|Mentioned|p5|||||||||
19967|Wianamatta Group|30466|6|Mentioned|p5|||Triassic age||||||
19967|Wianamatta Group|30475|6|Mentioned|p171|||||||||
19967|Wianamatta Group|30610|6|Mentioned|p326|||Refers Hind & Helby (1969)||||||
19967|Wianamatta Group|31056|5|Briefly described|p3|||||||||
19967|Wianamatta Group|31057|6|Mentioned|p2|||See also P8 re potential use.||||||
19967|Wianamatta Group|31062|6|Mentioned|p478|||Triassic. Table||||||
19967|Wianamatta Group|31128|5|Briefly described|p7|||See also P3.||||||
19967|Wianamatta Group|31276|6|Mentioned|p144|||Microfloral correlation.||||||
19967|Wianamatta Group|31296|4|Described|p29|||||||||
19967|Wianamatta Group|31725|4|Described|p11|||||||||
19967|Wianamatta Group|31855|6|Mentioned|p14|||Stratigraphic table||||||
19967|Wianamatta Group|31878|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|31885|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|31887|6|Mentioned|p3|||||||||
19967|Wianamatta Group|31947|6|Mentioned|p30|||See also P91||||||
19967|Wianamatta Group|32101|6|Mentioned|p107|||||||||
19967|Wianamatta Group|32136|6|Mentioned|p7|||Miospores||||||
19967|Wianamatta Group|32187|6|Mentioned|p4|||||||||
19967|Wianamatta Group|32315|6|Mentioned|p5|||||||||
19967|Wianamatta Group|32412|6|Mentioned|p86|||||||||
19967|Wianamatta Group|32413|6|Mentioned|p88|||||||||
19967|Wianamatta Group|32589|6|Mentioned|p54|||||||||
19967|Wianamatta Group|32671|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|32672|6|Mentioned|p675|||||||||
19967|Wianamatta Group|32803|6|Mentioned|p94|||||||||
19967|Wianamatta Group|32849|6|Mentioned|p7|||Triassic||||||
19967|Wianamatta Group|32917|6|Mentioned|p128|||||||||
19967|Wianamatta Group|32938|6|Mentioned|Fig.2|||||||||
19967|Wianamatta Group|33009|6|Mentioned|p136|||||||||
19967|Wianamatta Group|33129|6|Mentioned|p339|||Refs. Bunny (1972) & Cook (1969)||||||
19967|Wianamatta Group|33334|6|Mentioned|p6|||Triassic||||||
19967|Wianamatta Group|33583|6|Mentioned|p3|||||||||
19967|Wianamatta Group|33671|6|Mentioned|p3|||||||||
19967|Wianamatta Group|33685|6|Mentioned|Table 1|||Triassic.||||||
19967|Wianamatta Group|33709|6|Mentioned|p103|||||||||
19967|Wianamatta Group|33867|4|Described|p12|||||||||
19967|Wianamatta Group|33872|6|Mentioned|Fig.1|||||||||
19967|Wianamatta Group|34010|6|Mentioned|Cor. chart|||||||||
19967|Wianamatta Group|34034|6|Mentioned|p555|||||||||
19967|Wianamatta Group|34037|6|Mentioned|Table 5.27|||||||||
19967|Wianamatta Group|34059|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|34106|6|Mentioned|p401|||||||||
19967|Wianamatta Group|34107|4|Described|p219|||Triassic||||||
19967|Wianamatta Group|34172|6|Mentioned|p53|||||||||
19967|Wianamatta Group|34205|4|Described|p34|||||||||
19967|Wianamatta Group|34209|6|Mentioned|p148|||Triassic||||||
19967|Wianamatta Group|34228|6|Mentioned|p171|||||||||
19967|Wianamatta Group|34236|6|Mentioned|p17|||||||||
19967|Wianamatta Group|34243|6|Mentioned|p423|||Microfossils||||||
19967|Wianamatta Group|34254|6|Mentioned|p488|||M.Triassic||||||
19967|Wianamatta Group|34274|6|Mentioned|p121|||Triassic||||||
19967|Wianamatta Group|34287|6|Mentioned|p155|||See also P156,162. Triassic.||||||
19967|Wianamatta Group|34301|6|Mentioned|p403|||||||||
19967|Wianamatta Group|34305|6|Mentioned|Table 5.26|||||||||
19967|Wianamatta Group|34399|6|Mentioned|p312|||||||||
19967|Wianamatta Group|34400|5|Briefly described|p13|||||||||
19967|Wianamatta Group|34434|6|Mentioned|Fig.5.25|||||||||
19967|Wianamatta Group|34506|6|Mentioned|p408|||||||||
19967|Wianamatta Group|34560|6|Mentioned|p23|||||||||
19967|Wianamatta Group|34605|6|Mentioned|p377|||||||||
19967|Wianamatta Group|34845|6|Mentioned|Fig.4|||||||||
19967|Wianamatta Group|35062|6|Mentioned|p279|||||||||
19967|Wianamatta Group|35065|5|Briefly described|p44|||||||||
19967|Wianamatta Group|35095|6|Mentioned|p115|||||||||
19967|Wianamatta Group|35098|6|Mentioned|p1|||Also P4.||||||
19967|Wianamatta Group|35312|6|Mentioned|p3|||||||||
19967|Wianamatta Group|35416|6|Mentioned|p4|||Stratigraphy and palynological framework on Fig.2||||||
19967|Wianamatta Group|35502|6|Mentioned|p170|||Also on Table 1||||||
19967|Wianamatta Group|35524|6|Mentioned|Fig.2|||Stratigraphic sequence in southeastern part of Sydney Basin.||||||
19967|Wianamatta Group|35690|1|Redefined|p173|Middle Triassic|Middle Triassic|||||||
19967|Wianamatta Group|35878|6|Mentioned|p115|||||||||
19967|Wianamatta Group|35901|6|Mentioned|p4|||||||||
19967|Wianamatta Group|35913|6|Mentioned|p37|||||||||
19967|Wianamatta Group|35914|6|Mentioned|p16|||||||||
19967|Wianamatta Group|36042|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|36148|6|Mentioned|p266|||||||||
19967|Wianamatta Group|36220|4|Described|p91|||||||||
19967|Wianamatta Group|36221|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
19967|Wianamatta Group|36222|6|Mentioned|Map legend|Late Triassic|Middle Triassic|Middle to Late Triassic||||||
19967|Wianamatta Group|36390|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|36570|6|Mentioned|p22|||||||||
19967|Wianamatta Group|36594|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|36899|6|Mentioned|p1085|||||||||
19967|Wianamatta Group|36961|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|37065|6|Mentioned|p36|||||||||
19967|Wianamatta Group|37082|6|Mentioned|p161|||||||||
19967|Wianamatta Group|37089|5|Briefly described|p208|||||||||
19967|Wianamatta Group|37091|6|Mentioned|p226|||||||||
19967|Wianamatta Group|37093|5|Briefly described|p231|||||||||
19967|Wianamatta Group|37319|6|Mentioned|p610|||||||||
19967|Wianamatta Group|37757|6|Mentioned|p30|||||||||
19967|Wianamatta Group|37775|6|Mentioned|p7|||||||||
19967|Wianamatta Group|37804|6|Mentioned|p62|||||||||
19967|Wianamatta Group|37812|6|Mentioned|p657|||||||||
19967|Wianamatta Group|38064|5|Briefly described|p41|||||||||
19967|Wianamatta Group|38206|6|Mentioned|p53|||Clay resources||||||
19967|Wianamatta Group|38220|5|Briefly described|p319|||Structure||||||
19967|Wianamatta Group|38615|6|Mentioned|p18|||||||||
19967|Wianamatta Group|38656|6|Mentioned|Fig.1.5.12|||P279||||||
19967|Wianamatta Group|38837|6|Mentioned|p235|||||||||
19967|Wianamatta Group|39287|5|Briefly described|p50|||See also Fig.2.5||||||
19967|Wianamatta Group|39293|5|Briefly described|p160|||||||||
19967|Wianamatta Group|39298|3|Fully described|p262|||See also p255.||||||14-APR-20
19967|Wianamatta Group|39300|6|Mentioned|p298|||||||||
19967|Wianamatta Group|39306|6|Mentioned|p425|||See also P428, P428,Fig. 21.13||||||
19967|Wianamatta Group|39308|6|Mentioned|p493|||||||||
19967|Wianamatta Group|39450|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|39467|6|Mentioned|Fig.1|||||||||
19967|Wianamatta Group|39626|6|Mentioned|p276|||||||||
19967|Wianamatta Group|39811|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|39812|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|40245|6|Mentioned|Table 2|||||||||
19967|Wianamatta Group|40518|6|Mentioned|p344|||||||||
19967|Wianamatta Group|40592|5|Briefly described|p229|||||||||
19967|Wianamatta Group|40601|6|Mentioned|p94|||||||||
19967|Wianamatta Group|40602|3|Fully described|p21|||||||||
19967|Wianamatta Group|40603|6|Mentioned|p4|||||||||
19967|Wianamatta Group|40625|6|Mentioned|Map legend|Triassic|Triassic|||||||
19967|Wianamatta Group|40629|6|Mentioned|p184|||||||||
19967|Wianamatta Group|40631|6|Mentioned|p156|||||||||
19967|Wianamatta Group|40650|6|Mentioned|Table 7|||||||||
19967|Wianamatta Group|40653|6|Mentioned|p121|||||||||
19967|Wianamatta Group|40654|6|Mentioned|p115|||||||||
19967|Wianamatta Group|40744|6|Mentioned|Table 1|||||||||
19967|Wianamatta Group|41056|6|Mentioned|p22|||||||||
19967|Wianamatta Group|41290|6|Mentioned|Fig.8|||||||||
19967|Wianamatta Group|41639|6|Mentioned|p9|||||||||
19967|Wianamatta Group|42182|6|Mentioned|p300|||||||||
19967|Wianamatta Group|42664|5|Briefly described|p21|||||||||
19967|Wianamatta Group|42737|5|Briefly described|map legend|Triassic||||||||
19967|Wianamatta Group|42795|5|Briefly described|Fig.2 P23|||||||||
19967|Wianamatta Group|42896|3|Fully described|p40, Table 2|||||||||
19967|Wianamatta Group|42909|5|Briefly described|p3|||||||||
19967|Wianamatta Group|42925|3|Fully described|p17|||see also Table 1||||||
19967|Wianamatta Group|42926|4|Described|map legend||Middle Triassic|||||||
19967|Wianamatta Group|43028|5|Briefly described|p613|||||||||
19967|Wianamatta Group|43072|6|Mentioned|p78|||||||||
19967|Wianamatta Group|43194|5|Briefly described|p122, p131|Triassic|Triassic|Deposited during the last phase of tectonic development in the Sydney Basin. Very similar to, but not a time correlative of, the Napperby and Deriah Formations of the Gunnedah Basin.||||||
19967|Wianamatta Group|43263|6|Mentioned|Map Legend||Triassic|||||||
19967|Wianamatta Group|43317|14|Not recorded|Table 1 p13|||||||||
19967|Wianamatta Group|43318|14|Not recorded|p73,80|||Sydney basin.  Contains marine organisms||||||
19967|Wianamatta Group|43319|14|Not recorded|Map Legend|||||||||
19967|Wianamatta Group|43320|14|Not recorded|p13,14,20,25,29-31||Late Triassic|Inc. Camden subgroup and Liverpool Subgroup, Table 1||||||
19967|Wianamatta Group|43324|14|Not recorded|p18,19||Triassic|||||||
19967|Wianamatta Group|43325|14|Not recorded|Map Legend||Triassic|||||||
19967|Wianamatta Group|43341|14|Not recorded|p229|||||||||
19967|Wianamatta Group|43342|14|Not recorded|Table 1 p107|||||||||
19967|Wianamatta Group|43343|14|Not recorded|p119|||||||||
19967|Wianamatta Group|43344|14|Not recorded|p13,18,22,46,50,56,|||58,63,73,181||||||
19967|Wianamatta Group|43346|2|Defined|p2,4 Map|||||||||
19967|Wianamatta Group|43349|14|Not recorded|Map|||||||||
19967|Wianamatta Group|43352|14|Not recorded|p 209-223||Triassic|||||||
19967|Wianamatta Group|43358|14|Not recorded|p48|||||||||
19967|Wianamatta Group|43359|14|Not recorded|Map Legend||Mesozoic|Provisional first edition  (Liverpool Sub-Group)||||||
19967|Wianamatta Group|43365|14|Not recorded|p169-210||Triassic|||||||
19967|Wianamatta Group|43372|14|Not recorded|p86|||||||||
19967|Wianamatta Group|43373|14|Not recorded|p163|||||||||
19967|Wianamatta Group|43383|14|Not recorded|p22,23,Fig.3,Fig.5||Triassic|||||||
19967|Wianamatta Group|43384|14|Not recorded|Map Legend||Triassic|||||||
19967|Wianamatta Group|43385|14|Not recorded|p181,182||Rhaetian|||||||
19967|Wianamatta Group|43395|14|Not recorded|map|||||||||
19967|Wianamatta Group|43440|14|Not recorded|p34,fig4-3|||||||||
19967|Wianamatta Group|43449|14|Not recorded|p11;opp 12;Pl 2|||||||||
19967|Wianamatta Group|43479|14|Not recorded|p228,243||Late Triassic|||||||
19967|Wianamatta Group|43491|14|Not recorded|pVIII/8,15||Triassic|||||||
19967|Wianamatta Group|43873|14|Not recorded|p53|||||||||
19967|Wianamatta Group|43881|14|Not recorded|p73,80|||Contains marine organisms. Sydney Basin.||||||
19967|Wianamatta Group|43885|14|Not recorded|p419|||Dickite found.||||||
19967|Wianamatta Group|43895|14|Not recorded|p116|||||||||
19967|Wianamatta Group|43980|14|Not recorded|p3,opp.1,Pl.1|||||||||
19967|Wianamatta Group|44004|2|Defined|p18,20|||||||||
19967|Wianamatta Group|44005|14|Not recorded|opp.p23|||||||||
19967|Wianamatta Group|44244|5|Briefly described|p290 Tb. 5|Triassic|Triassic|Geological Province: northern Sydney Basin.||||||
19967|Wianamatta Group|44282|14|Not recorded|opp.p.15|||(I56-9/Kiama).||||||
19967|Wianamatta Group|44450|5|Briefly described|p147 Fig 43|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin.||||||
19967|Wianamatta Group|44507|14|Not recorded|p103,106|||||||||
19967|Wianamatta Group|44610|14|Not recorded|p47,49|||||||||
19967|Wianamatta Group|44668|14|Not recorded|p60|||||||||
19967|Wianamatta Group|44998|14|Not recorded|p104|||Correlated with Erskine Sandstone; Blina Shale, Canning Basin.||||||
19967|Wianamatta Group|45090|6|Mentioned|p7|||Time correlation chart||||||
19967|Wianamatta Group|60281|5|Briefly described|p9, p63,  p64|Middle Triassic|Middle Triassic|Mainly shaly with sporadic thin lithic sandstones. The shaly facies provides a regional reservoir seal for the Hawkesbury Sandstone.  Max. thickness: 300m.Geological Province: Sydney Basin.||||||17-MAR-05
19967|Wianamatta Group|60726|6|Mentioned|p2 Fig.1, p3.|Anisian|Anisian||||Ashfield Shale.|||
19967|Wianamatta Group|61209|5|Briefly described|p225 Fig. 7b|Mesozoic|Mesozoic|Geological Province: Sydney Basin.||||||
19967|Wianamatta Group|61315|5|Briefly described|Table SY2|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin||||||
19967|Wianamatta Group|61612|6|Mentioned|p276, p277, p270 Fig. 1|Middle Triassic|Middle Triassic|Geological Province: Sydney Basin.||||||17-MAR-09
19967|Wianamatta Group|61772|6|Mentioned|p129, 130, p132||Middle Triassic|Contains distal tuffs.||||||24-SEP-08
19967|Wianamatta Group|65195|6|Mentioned|p3-4, p4 Fig.2|Triassic|Triassic|Contains Ashfield Shale, Bringelly Shale and Minchinbury Sandstone. Overlain by Rickaby's Creek Gravels east of the Lapstone Structural Complex. Reference to Wianamatta Group Shale on p4 is probably the same unit. Spelt Wiannamatta in Fig.2||||||
19967|Wianamatta Group|65490|5|Briefly described|p 874, Fig. 1 p875|Middle Triassic|Early Triassic|Sedimentary unit of the Sydney Basin Cut by faults dating between ~163 and 120 Ma, and reactivated post 51 Ma. See p882-883 for age discussion.||||||
19967|Wianamatta Group|65492|6|Mentioned|p889, p890 Fig. 1 |Triassic|Triassic|||||||
19967|Wianamatta Group|66300|6|Mentioned|p87.|Triassic|Triassic|Sydney Basin.||||Intruded by 'Mount Gibraltar microsyenite'.||
19967|Wianamatta Group|66577|6|Mentioned|pp995-998, p1001 Fig.6.|Triassic|Triassic|Deposited in a single regressive episode following subsidence of the Hawkesbury Sandstone alluvial plain.|||Includes Bringelly and Ashfield Shales; Minchinbury Sandstone.|Overlies Hawkesbury Sandstone.||
19967|Wianamatta Group|67663|4|Described|p519 Fig.1, p520-522|Triassic|Triassic|Up to 300m thick. Deposited during a single major regression: subaqueous to shoreline to alluvial.|||Includes Ashfield Shale, Minchinbury Sandstone, Bringelly Shale.|Overlies Hawkesbury Sandstone.|Dominantly shale with sporadic thin lithic sandstones.|
19967|Wianamatta Group|67850|5|Briefly described|p51 Table 1, pp52-57. |Triassic|Triassic|||||||
19967|Wianamatta Group|68003|5|Briefly described|p38 Fig.3-j, p43.|Middle Triassic|Middle Triassic|Hunter Coalfield, Brigalow Belt South Bioregion, and Sydney Basin. Correlative of Napperby Formation (Gunnedah Basin). Deposited in a single regressive cycle.||||Overlies Narrabeen Group.||
19967|Wianamatta Group|68592|6|Mentioned|p1792|Middle Triassic|Middle Triassic|Deposition in a shallow marine to alluvial environment on a coastal plain.||||||
19967|Wianamatta Group|68811|5|Briefly described|p57|Triassic|Triassic||||||Interbedded shales and sandstones.|
19967|Wianamatta Group|69297|5|Briefly described|p403, p435, p499, p501, p504|Middle Triassic|Middle Triassic|Sydney Basin. Deposited in fluvial to shallow marine environments. Claystones may form seals to the underlying Triassic sandstones.||||Overlies the Hawkesbury Sandstone.|Shales, siltstones and sandstones.|
19967|Wianamatta Group|69683|6|Mentioned|p410 Fig.1, p412|Triassic|Triassic|Maximum thickness of 300m used in modelling in this study.||||||
19967|Wianamatta Group|70587|5|Briefly described|Map Legend|Triassic|Triassic||||||Sandstone, siltstone and shale; common bioturbation.|
19967|Wianamatta Group|70661|4|Described|vii, ix, p207-p210, p240, p242, p243|Middle Triassic|Middle Triassic|Name derived from Wianamatta Creek.  Previously referred to as the Wianamatta Beds, Shale, formation or series before being finally defined as a group. Distribution, distinguishing characteristics, geomorphology, structure, fossil assemblage discussed. Representative section mentioned. Maximum thickness of 304.2m (based on drillhole). Deposited in shallow marine environment, passing into a coastal plain environment.|||Bringelly Shale, Minchinbury Sandstone, Ashfield Shale|probably disconformably overlies the Mittagong Formation, disconformably overlies Hawkesbury Sandstone|Intecalated shale and sandstone.|
19967|Wianamatta Group|70791|6|Mentioned|p277|Middle Triassic|Middle Triassic|Hunter Coalfield.||||||
19967|Wianamatta Group|71303|5|Briefly described|map legend|Middle Triassic|Middle Triassic|Of Sydney Basin.|||Includes Ashfield Shale, Minchinbury Sandstone, Bringelly Shale.|||
19967|Wianamatta Group|73248|5|Briefly described|p301, p305-309, App. p2|Middle Triassic|Middle Triassic|Deposition may have been constrained by basement adjustments during the Early Triassic.|||Ashfield Shale, Minchinbury Sandstone, Bringelly Shale|Underlain by Hawkesbury Sandstone. Unconformably overlain by Rickabys Creek Gravel and Robertson Basalt.|Includes shales.|
19967|Wianamatta Group|73304|6|Mentioned|p75|||||||||
19967|Wianamatta Group|75059|5|Briefly described|p4, 9, 13-14|Middle Triassic|Middle Triassic|Sydney Basin.|||Ashfield, Bringelly Shales; Minchinbury Sandstone.|Overlies Hawkesbury Sandstone.|Shales and sandstones.|
19982|Widgelands Serpentine|34449|4|Described|Table 2-1|||U.Ordovician||||||
19986|Widgelli Pedoderm|34735|5|Briefly described|p41|||||||||
19986|Widgelli Pedoderm|35187|6|Mentioned|Table1|||||||||
19986|Widgelli Pedoderm|35272|4|Described|p279|||||||||
19986|Widgelli Pedoderm|41848|4|Described|p355|||Equivalent to Widgelli parna, Widgelli Member. Top unit of Shepparton Formation.||||||17-JUN-09
19986|Widgelli Pedoderm|42827|4|Described|p355|||||||||
19986|Widgelli Pedoderm|42966|2|Defined|Table 30 p196|Late Pleistocene||Of Shepparton Formation.||||||13-JUN-06
19986|Widgelli Pedoderm|60452|5|Briefly described|p40|||Overlies the entire sequence of members within the Shepparton Formation.||||||
19986|Widgelli Pedoderm|61185|5|Briefly described|p63|Quaternary|Quaternary|Of Lawrence (1966,1975) and Jenkin (1988). Top of the Shepparton Formation.||||||07-FEB-11
19998|Wightmans Hill Conglomerate|23309|5|Briefly described|p160, 163||Givetian|||||||
19998|Wightmans Hill Conglomerate|24551|5|Briefly described|p164, p163 Fig. 6.4|Late Devonian|Late Devonian|Of the Taggarty Subgroup, Marysville Igneous Complex.||||||
19998|Wightmans Hill Conglomerate|35073|5|Briefly described|Table 2|||||||||
19998|Wightmans Hill Conglomerate|35186|4|Described|p3|||||||||
19998|Wightmans Hill Conglomerate|35277|4|Described|p83|||||||||
19998|Wightmans Hill Conglomerate|39291|6|Mentioned|Table 1|||||||||
19998|Wightmans Hill Conglomerate|40995|6|Mentioned|Fig.31|||||||||
19998|Wightmans Hill Conglomerate|41641|4|Described|p153|||||||||
19998|Wightmans Hill Conglomerate|42827|5|Briefly described|p153|||see also Fig 5.4||||||
19998|Wightmans Hill Conglomerate|68311|5|Briefly described|p273-274|Late Devonian|Late Devonian|The basal unit in the Cerberean Cauldron, Central Victoria. Up to 30m thick. Pre-collapse phase.||Taggerty Subgroup.||Is overlain by Snobs Creek Volcanics.|Fluvial/alluvial conglomerate to sandstone. Clasts derived from basement metasediments.|
20009|Wild Cattle Trachyte Member|39969|6|Mentioned|p9|||||||||
20009|Wild Cattle Trachyte Member|73450|6|Mentioned|p92|||Of Stevens, 1965; Grenfell, 1984; Ewart & Grenfell, 1985. Never described in detail.||Governors Chair Volcanics|||Felsic.|29-SEP-22
20031|Wilgunya Subgroup|13516|5|Briefly described|p167 fig 10,  p169 fig 11|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Of Rolling Downs Group||||
20031|Wilgunya Subgroup|23496|6|Mentioned|p59|||||||||
20031|Wilgunya Subgroup|29591|6|Mentioned|p69|||||||||
20031|Wilgunya Subgroup|31168|5|Briefly described|p11|||See also Table 2.||||||
20031|Wilgunya Subgroup|33528|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|35855|6|Mentioned|Fig.2|||Early Cretaceous lithostratigraphy.||||||
20031|Wilgunya Subgroup|36228|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20031|Wilgunya Subgroup|39445|6|Mentioned|Table 11|||||||||
20031|Wilgunya Subgroup|39556|5|Briefly described|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|39899|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20031|Wilgunya Subgroup|41307|6|Mentioned|p17|||||||||
20031|Wilgunya Subgroup|43110|5|Briefly described|p55|||||||||
20031|Wilgunya Subgroup|43630|6|Mentioned|p70|||||||||
20031|Wilgunya Subgroup|63979|6|Mentioned|p48|||Of the Rolling Downs Group. Superseded Wilgunya Formation. Lower part comprises Wallumbilla Formation.||||||07-FEB-11
20031|Wilgunya Subgroup|66623|6|Mentioned|p258.|||Laterally equivalent to Wallumbilla Formation in NSW.||Unit in Rolling Downs Group (QLD).||||06-JUN-13
20031|Wilgunya Subgroup|67323|5|Briefly described|GIS attrib tbl, Solid Geology Map.|Early Cretaceous|Early Cretaceous|Eromanga/Carpentaria Basins|||||Fossiliferous mudstone, minor labile, glauconitic and quartzose sandstone, calcareous concretions common|
20031|Wilgunya Subgroup|67784|5|Briefly described|p26|Aptian|Barremian|Carpentaria, Eromanga Basins.|||Gilbert River, Wallumbilla, Toolebuc, Allaru, Normanton FZs.|||
20031|Wilgunya Subgroup|69457|5|Briefly described|p41:2-4, 6-11, 14|Early Cretaceous|Early Cretaceous|Casey (1959); Australian Water Resources Council (1975). Eromanga Basin. This Subgroup's nomenclature is more appropriate (than the Marree Subgroup) in the NT, where the Coorikiana Sandstone has not been recognised.||Rolling Downs Group.|Wallumbilla, Toolebuc Formations; Allaru Mudstone.|Is overlain by Manuka Subgroup. Equivalent to Marree Subgroup.||12-JUL-16
20031|Wilgunya Subgroup|69458|6|Mentioned|p42:16|||Eromanga Basin. Some rocks of this unit are mapped as Rumbalara Shale in HALE RIVER, McDILLS map areas.||||Is overlain unconformably by Etingambra Formation.||12-JUL-16
20031|Wilgunya Subgroup|69594|5|Briefly described|p528|||Great Australian Superbasin.||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|69599|5|Briefly described|p599|Cretaceous|Cretaceous|||||Is overlain unconformably by the Noranside Limestone.||
20031|Wilgunya Subgroup|69673|6|Mentioned|p156|||||Rolling Downs Group|Includes Wallumbilla Formation, Toolebuc Formation, Allaru Mudstone|Overlain by Manuka Subgroup||
20031|Wilgunya Subgroup|70352|5|Briefly described|Map legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group.|Wallumbilla Formation.|||
20031|Wilgunya Subgroup|70572|5|Briefly described|Map Legend|Early Cretaceous|Early Cretaceous|||Rolling Downs Group|Includes Allaru Mudstone, Toolebuc Formation, Wallumbilla Formation.|||20-JAN-22
20031|Wilgunya Subgroup|73083|6|Mentioned|p62, p65, p77|||Term used where the Wallumbilla Mudstone and Allaru Mudstone are indistinguishable. [Written as Wilgunyah Subgroup on p65 and p77].||||||
20034|Wilhelmshohe Tonalite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Medium to coarse-grained hornblende-biotite tonalite.||||||21-DEC-04
20034|Wilhelmshohe Tonalite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
20034|Wilhelmshohe Tonalite|30787|6|Mentioned|p45|||Also mention p46.||||||
20034|Wilhelmshohe Tonalite|30789|6|Mentioned|Fig.1B|||Petrology & Geochemistry||||||
20034|Wilhelmshohe Tonalite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
20034|Wilhelmshohe Tonalite|31140|6|Mentioned|p55|||||||||
20034|Wilhelmshohe Tonalite|43091|5|Briefly described|Map legend|||||||||
20034|Wilhelmshohe Tonalite|69323|5|Briefly described|p13-14,70|Late Permian|Late Permian|Geological province: New England Orogen.||Unit of Uralla Supersuite.||Intrudes into "Uralla volcanics'.||
20034|Wilhelmshohe Tonalite|71628|5|Briefly described|p8: 3, 50, 67, 72, 76-79; p19: 54-55|||Binns et al. (1967), after the property of that name. Occurs 8km SW of Uralla. Crops out as tors. Limited geochemistry described; has similarities with Khatoun Tonalite and Uralla Granodiorite. RELATED UNITS (continued): Abuts Kentucky Quartz Diorite (nature of boundary uncertain) and Uralla Granodiorite (gradationally).||Uralla Suite.||Intrudes Terrible Vale Porphyritic Microgranodiorite, Glenburnie Leucomonzogranite and Wandsworth Volcanic Group. See COMMENTS for more.|Grey-green, medium- to coarse-grained, broadly equigranular, biotite-hornblende tonalite - granodiorite. I-type.|
20045|Wilkawillina Limestone|22650|6|Mentioned|p 159|Cambrian|Cambrian|Province - Adelaide Geosyncline.||||||
20045|Wilkawillina Limestone|22651|6|Mentioned|p 191|||Province - Flinders Ranges SA.||||||
20045|Wilkawillina Limestone|22652|6|Mentioned|p 196|||||||||
20045|Wilkawillina Limestone|22688|6|Mentioned|127,128|||||||||
20045|Wilkawillina Limestone|22766|5|Briefly described|Fig.2 p561|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|23211|6|Mentioned|Fig.2|||of Hawker Group.||||||
20045|Wilkawillina Limestone|23287|6|Mentioned|Fig.2,4||Cambrian|of Adelaide Geosyncline.||||||02-MAY-13
20045|Wilkawillina Limestone|23818|4|Described|p87 Fig.33, p90|Cambrian|Cambrian|Of the Hawker Group. Underlying unit: Parachilna Formation. Contains abundant Archaecyatha.||||||
20045|Wilkawillina Limestone|23825|5|Briefly described|p254|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|23826|6|Mentioned|p95|||Geological Province: Arrowie Bain.||||||
20045|Wilkawillina Limestone|23981|5|Briefly described|p8-9 Fig. 4|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||04-FEB-08
20045|Wilkawillina Limestone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
20045|Wilkawillina Limestone|24138|4|Described|p29|Cambrian|Cambrian|Frequently referred to as the Archaeocyatha Limestone. Sandy and shaly beds with fossil algae. Geological Province: Adelaide Geosyncline.||||||17-JUN-05
20045|Wilkawillina Limestone|24176|4|Described|p16-17, p23 Tb. 1|Cambrian|Cambrian|Massive grey limestone.  Intertongues with the Parara Limestone.  Geological Province: Mount Painter Province.||||||
20045|Wilkawillina Limestone|24281|5|Briefly described|p7|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|24465|5|Briefly described|p345 Fig.2|Early Cambrian|Early Cambrian|Of the Hawker Group.  Geological Province: Arrowie Basin.||||||19-JAN-05
20045|Wilkawillina Limestone|24481|5|Briefly described|p828|||Of the Ajax Limestone.||||||
20045|Wilkawillina Limestone|24484|4|Described|p798 Fig.1, p804|Cambrian|Cambrian|Divided into Lower and Upper units by a regional unconformity. Overlies the Woodendinna Dolomite. Overlain by the Billy Creek Formation.||||||
20045|Wilkawillina Limestone|29780|6|Mentioned|p47|||||||||
20045|Wilkawillina Limestone|29929|6|Mentioned|p223|||||||||
20045|Wilkawillina Limestone|30051|6|Mentioned|p20|||||||||
20045|Wilkawillina Limestone|30176|6|Mentioned|Map legend|Early Cambrian|Early Cambrian|||||||
20045|Wilkawillina Limestone|30198|4|Described|p97|||||||||
20045|Wilkawillina Limestone|30374|6|Mentioned|p29|||||||||
20045|Wilkawillina Limestone|30801|6|Mentioned|p5|||Lower Cambrian. Table P5-6||||||
20045|Wilkawillina Limestone|30802|5|Briefly described|p11|||Cambrian.||||||
20045|Wilkawillina Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20045|Wilkawillina Limestone|31022|4|Described|Fig. 4|||||||||
20045|Wilkawillina Limestone|31344|5|Briefly described|p2|||||||||
20045|Wilkawillina Limestone|31536|6|Mentioned|p10|||||||||
20045|Wilkawillina Limestone|31539|6|Mentioned|Fig. 8|||See also Fig. 9, 11, 17, 24, 22, 28.||||||
20045|Wilkawillina Limestone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
20045|Wilkawillina Limestone|31729|6|Mentioned|p111|||Geological map||||||
20045|Wilkawillina Limestone|31730|6|Mentioned|p99|||Geochem. Stream Sediment sampling.||||||
20045|Wilkawillina Limestone|31797|6|Mentioned|Fig. 2|||L.Camb. of Hawker Gp.||||||
20045|Wilkawillina Limestone|32504|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|32720|6|Mentioned|Table 1|||Hawker Group||||||
20045|Wilkawillina Limestone|32722|6|Mentioned|Fig.3|||L.Camb.||||||
20045|Wilkawillina Limestone|33474|6|Mentioned|Fig.3|||||||||
20045|Wilkawillina Limestone|33655|6|Mentioned|p87|||||||||
20045|Wilkawillina Limestone|33932|4|Described|p14|||||||||
20045|Wilkawillina Limestone|33934|4|Described|Fig.2|||L.Camb.||||||
20045|Wilkawillina Limestone|33954|6|Mentioned|p101|||||||||
20045|Wilkawillina Limestone|33973|6|Mentioned|p18|||||||||
20045|Wilkawillina Limestone|34122|6|Mentioned|p301|||Lower Cambrian||||||
20045|Wilkawillina Limestone|34202|6|Mentioned|p1058|||Hawker Group.||||||
20045|Wilkawillina Limestone|34267|6|Mentioned|Fig.|||The Oraparinna & Enorama diapiric structures.||||||
20045|Wilkawillina Limestone|34269|6|Mentioned|Table 1|||||||||
20045|Wilkawillina Limestone|34612|5|Briefly described|p90|||Lower Cambrian. See Fig.33||||||
20045|Wilkawillina Limestone|35075|6|Mentioned|p77|||||||||
20045|Wilkawillina Limestone|35255|6|Mentioned|Fig.8|||||||||
20045|Wilkawillina Limestone|35373|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|35395|5|Briefly described|p102|||Stratigraphy||||||
20045|Wilkawillina Limestone|35577|6|Mentioned|p3|||||||||
20045|Wilkawillina Limestone|35798|6|Mentioned|p311|||||||||
20045|Wilkawillina Limestone|35835|6|Mentioned|p201|||||||||
20045|Wilkawillina Limestone|36198|6|Mentioned|Fig.I.2|||||||||
20045|Wilkawillina Limestone|36495|6|Mentioned|p118|||||||||
20045|Wilkawillina Limestone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
20045|Wilkawillina Limestone|36731|6|Mentioned|p125|||||||||
20045|Wilkawillina Limestone|37802|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|38068|5|Briefly described|p69|||||||||
20045|Wilkawillina Limestone|39675|6|Mentioned|p180|||||||||
20045|Wilkawillina Limestone|39904|6|Mentioned|p11|||||||||
20045|Wilkawillina Limestone|40431|4|Described|p12|||||||||
20045|Wilkawillina Limestone|40455|6|Mentioned|Fig.2|||||||||
20045|Wilkawillina Limestone|40642|6|Mentioned|p163|||||||||
20045|Wilkawillina Limestone|40672|6|Mentioned|p2|||||||||
20045|Wilkawillina Limestone|40831|6|Mentioned|p2|||||||||
20045|Wilkawillina Limestone|40852|6|Mentioned|p32|||||||||
20045|Wilkawillina Limestone|40856|6|Mentioned|Fig.23.6|||||||||
20045|Wilkawillina Limestone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
20045|Wilkawillina Limestone|40994|6|Mentioned|p266|||||||||
20045|Wilkawillina Limestone|40998|6|Mentioned|p441|||||||||
20045|Wilkawillina Limestone|41457|6|Mentioned|p1|||||||||
20045|Wilkawillina Limestone|41496|4|Described|p52|||||||||
20045|Wilkawillina Limestone|41526|6|Mentioned|p11|||||||||
20045|Wilkawillina Limestone|41996|6|Mentioned|p3|||||||||
20045|Wilkawillina Limestone|42011|5|Briefly described|p457|||||||||
20045|Wilkawillina Limestone|42090|6|Mentioned|p26|||||||||
20045|Wilkawillina Limestone|42095|5|Briefly described|Fig.3 P31|||||||||
20045|Wilkawillina Limestone|42192|6|Mentioned|p6|||||||||
20045|Wilkawillina Limestone|42213|5|Briefly described|p471|||See also Fig.1||||||
20045|Wilkawillina Limestone|42222|5|Briefly described|p20|||||||||
20045|Wilkawillina Limestone|42225|6|Mentioned|Fig.4 P224|||||||||
20045|Wilkawillina Limestone|42226|5|Briefly described|Fig.7 P241|||||||||
20045|Wilkawillina Limestone|42233|3|Fully described|p249|||See also Fig.2||||||
20045|Wilkawillina Limestone|42266|6|Mentioned|p299|||||||||
20045|Wilkawillina Limestone|42267|6|Mentioned|p314|||||||||
20045|Wilkawillina Limestone|42440|6|Mentioned|p605|||||||||
20045|Wilkawillina Limestone|42444|5|Briefly described|Fig.2 P16|||||||||
20045|Wilkawillina Limestone|42469|6|Mentioned|p25|||||||||
20045|Wilkawillina Limestone|42573|5|Briefly described|Fig.2 P191|||||||||
20045|Wilkawillina Limestone|43052|5|Briefly described|Table 2.1|||||||||
20045|Wilkawillina Limestone|43650|6|Mentioned|Fig.2,p444|||||||||
20045|Wilkawillina Limestone|43781|6|Mentioned|p4||Early Cambrian|||||||
20045|Wilkawillina Limestone|43845|6|Mentioned|Fig4 p44|||||||||12-JUL-16
20045|Wilkawillina Limestone|44133|5|Briefly described|p3, 22|Botomian||Conformably overlies: Parachilna Formation.||||||
20045|Wilkawillina Limestone|44659|5|Briefly described|map legend||Early Cambrian|L.Cambrian, lithology.||||||
20045|Wilkawillina Limestone|45102|6|Mentioned|p46|||||||||
20045|Wilkawillina Limestone|46957|6|Mentioned|p165|||||||||
20045|Wilkawillina Limestone|60418|5|Briefly described|p135|Early Cambrian|Early Cambrian|Of the Hawker Group. Overlain by Mernnerna Formation. Geological Province: Arrowie Basin of Adelaide Geosyncline.||||||
20045|Wilkawillina Limestone|60565|5|Briefly described|p18|Early Cambrian|Early Cambrian|Carbonates. Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|60889|4|Described|p247, p249, p253-4|Early Cambrian|Early Cambrian|Biostratigraphy is discussed. Waxy paraffinic crude was found in carbonate cores in Wilkatana-1.||Hawker Group|||Karstic. Consists of archaeocyathan bioherms (in LD97-1).|
20045|Wilkawillina Limestone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Hawker Group. Light to dark grey, massive, bedded lime mudstone, wackestone, grainstone.||||||
20045|Wilkawillina Limestone|60990|5|Briefly described|p83 Fig.2, p83, p85|Botoman|Atdbanian|Wilkawillina Gorge, Arrowie Basin.  Biogeographic correlation with Cymbric Vale Formation. Faunal links with Antarctica.||Hawker Group.||||
20045|Wilkawillina Limestone|61308|5|Briefly described|p7|Cambrian|Cambrian|Sandy limestone.||||||
20045|Wilkawillina Limestone|61565|5|Briefly described|p609 Fig. 3|Cambrian|Cambrian|Geological Province: Adelaide Fold Belt.||||||26-MAY-06
20045|Wilkawillina Limestone|62570|6|Mentioned|p582|||Correlates with Ouldburra Formation in Offcier Basin.  Geological Province: Arrowie Basin.||||||
20045|Wilkawillina Limestone|62592|5|Briefly described|p50 Table 5.1|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Hawker Group.||Overlies Wirrapowie Limestone. Is overlain by Mern Merna Formation.|Archaeocyathan limestone.|
20045|Wilkawillina Limestone|62784|5|Briefly described|p8 Fig.1, p10 Fig. 3|Cambrian|Cambrian|Arrowie Basin. Unit in Hawker Group. Includes Second Plain Creek Member. Is unconformably overlain by Mernmerna Formation.||||||
20045|Wilkawillina Limestone|63447|5|Briefly described|p961, p962, p963, Fig.2|Early Cambrian|Early Cambrian|Upper part and lower part discussed seperately and shown as separate units in Fig. 2. Shallow water sediments.  Bioherm complexes form major part of unit.||Hawker Group||Upper part is laterally equivalent to the Moorowie Formation. Lower part laterally equivalent to Wirrapowie Limestone.|Generally consists of platform-derived archaeocyathan-calci-microbe limestone with a predominance of rubbly and argillaceous limestone.|
20045|Wilkawillina Limestone|63569|5|Briefly described|pp116-122, p138|Cambrian|Cambrian|Arrowie Basin, Adelaide Geosyncline. Contains trilobite taxa from the Abadiella huoi Zone.||Unit in Hawker Group.|Includes Second Plain Creek Member.|Is overlain unconformably by Mernmerna Formation; contact is the red microstromatolite horizon of the Flinders Unconformity.||
20045|Wilkawillina Limestone|64813|5|Briefly described|p272|Early Cambrian|Early Cambrian|Geological province: Arrowie Basin, S.A. Marine dolomitic limestones.||||||
20045|Wilkawillina Limestone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. Contains marine archaeocyathids and shows local red breccias and paleokarst features created during exposure and dissolution.||||||07-FEB-11
20045|Wilkawillina Limestone|65313|6|Mentioned|p576 Fig. 5, p578 Fig. 6|Early Cambrian|Early Cambrian|~200 degrees burial temperature.||Of Hawker Group.||||26-MAR-12
20045|Wilkawillina Limestone|65625|5|Briefly described|p103 Fig.2|Early Cambrian|Early Cambrian|Lake Frome area.||||Overlies Pound Sandstone. Underlies Parara Limestone.||18-FEB-11
20045|Wilkawillina Limestone|65686|5|Briefly described|p413, p409 Fig 2, p412|Early Cambrian|Early Cambrian|Arrowie Basin.||||Underlies the Bunkers Sandstone.||07-MAY-12
20045|Wilkawillina Limestone|65892|4|Described|p7 Fig.3, p8, p10, p12, p29 Fig.14. |Early Cambrian|Early Cambrian|See also p38-39, p44, p46-48. Arrowie Basin. Platformal carbonates, including archaeocyathid-rich biohermal complexes. Described in some detail.|c.530 Ma.|Unit in Hawker Group.||Overlies Woodendinna Dolomite. Is locally interbedded with Mernmerna Formation.|Reefal limestone.|
20045|Wilkawillina Limestone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Archaeocyath-calcimicrobe limestone.|
20045|Wilkawillina Limestone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.||Unit in Hawker Group.||Unconformably underlies Mernmerna Formation.||
20045|Wilkawillina Limestone|66623|6|Mentioned|p443.|||Arrowie Basin. Lower and upper parts separated by the Flinders unconformity. An unzoned interval between this and the Syringocnema favus beds is correlated with Mount Wright Volcanics of Koonenberry Belt.||||||
20045|Wilkawillina Limestone|67344|6|Mentioned|p264 Tb.3, p266 |Cambrian|Cambrian|Of the Arrowie Basin. Unmetamorphosed Cambrian series 2 formation. Shallow-water marine carbonate deposit. Bulk organic carbon isotopic composition almost identical with Emu Bay Shale.||||||
20045|Wilkawillina Limestone|67870|5|Briefly described|p9-10, p15, p21|Cambrian|Cambrian|Arrowie Basin. Appears on p9 as Wilawillina Formation. Source of bituminous hydrocarbons recovered from this unit.||Hawker Group.||Is overlain by Billy Creek Formation.||
20045|Wilkawillina Limestone|67907|6|Mentioned|p257, p259-260|||Flinders Ranges. Upper portion mentioned.||||||
20045|Wilkawillina Limestone|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges. Contains Ediacaran trilobites and archaeocyathids.||Unit of Hawker Group.||Overlain unconformably by, and channel infilled with Billy Creek Formation; laterally grades ino Mernmerna Formation. Underlain by Woodendinna Dolomite.||
20045|Wilkawillina Limestone|68735|5|Briefly described|p233, p234|Early Cambrian|Early Cambrian|See also mis-spelt Wilkawilina Limestone (p233 Fig.2). Arrowie Basin. The lower part of this formation has marked lateral facies changes.||Of the Hawker Group.||Underlain and intertongued by the Wirrapowie Limestone. Overlain by the Mernmerna Formation.|Lower: transgressive succession of lime mudstone, wackestone and isolated archeocyath-Renalcis bioherms. Middle: platform carbonates, many of which are biohermal.|10-APR-17
20045|Wilkawillina Limestone|69570|6|Mentioned|p420-p426, p428, p430, p432-p434|||Arrowie Syncline, Flinder Ranges. The upper part is interfingered with and partially overlain by the Wirrapowie Limestone. Fossil assemblage and sample localities are described.|||Includes the Hideaway Well Member, Woodendinna Dolostone, Winnitinny Creek Member and the Mount Mantell Member.|||
20045|Wilkawillina Limestone|70833|5|Briefly described|p176,178,180-188,190-201,203,205|Series 2|Terreneuvian|Of Arrowie Basin. Key sections: MORO and MOG (S of Moro Gorge, Arrowie Syncline); BALC (Balcoracana Gorge, Bunkers Range); MMT (Bunkers Range, central Flinders Ranges); WILK (Wilkawillina Type Section, Bunkers Graben); 10MS-W (Ten Mile South, SE Bunkers Graben).  Includes K. rostana and M. etheridgei zones in the lower and upper parts of the section respectively. Time-equivalent to uppermost Kulpara Limestone and lower half of Heatherdale Shale. Correlable to Ajz and Wirrapowie limestones.||Unit of Hawker Group.|Includes Second Plain Creek, Winnitinny Creek, Hideaway Well and Mount Mantell members.|Overlain by Mernmerna Formation. Underlain by Woodendinna Dolostone.||
20045|Wilkawillina Limestone|70835|5|Briefly described|p335-337, 351, 353|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges. Type section is in Wilkawillina Gorge in the Bunkers Graben.||Hawker Group.|Mount Mantell, Hideaway Well, Winnitinny Creek, Members.|Overlies Woodendinna Dolostone. Is overlain unconformably by Mernmerna Formation.||
20045|Wilkawillina Limestone|71102|4|Described|p242,244-246,249,252,267,275|Series 2|Terreneuvian|Of Arrowie Basin. Intersected sections: DBS (Donkey Bore Syncline), MMF (Bunkers Range, Central Flinders Ranges), 10MS (10 Mile South, Bunkers Graben),  LMNB (Lower Mernmerna, North Boundary Creek, Chambers Gorge, E Flinders Ranges).|||Includes Winnitinny Creek Member.|Overlain by, and interfingers with Mernmerna Formation.|Bioclastic to clean micritic limestones. Rare muddy drapes.|
20045|Wilkawillina Limestone|72429|3|Fully described|p949, p952, p956, p959-961, p967|Lower Cambrian|Lower Cambrian|Mount Chambers Gorge, eastern Flinders Ranges. Up to 79m thick in measured section in the core of NE-SW-trending anticline. Outcrop is massive with beds up to 2m thick of silty yellow to buff-weathered partly dolomitic limestone with peloidal and oolitic interbeds of 0.5mm average grain diameter. It is internally pink to white with light grey patches and occasional limonitic buff-brown patches after weathered siderite. Stylolites and rare chert nodules are present. Fossils include abundant archaeocyaths, hyoliths and calciate brachiopods as well as large number tommotiid Micrina etheridgei, a zone fossil from the early Cambrian. Inferred habitat for the Wilkawillina Limestone fauna is biostromal mats or archaeocyath-calcimcirobe meadows scattered in the shallower and calmer waters of a shallow-marine shelf, but in the mid-platform away from high-energy margins. Clear-water sedimentation prevailed with well-agitated and oxygenated waters within the photic zone. Oolitic-to-peloidal shoals record active currents on the shelf. The environment corresponds to Shaw's least restricted zone of autochthonous sedimentary patterns in epeiric seas.||Hawker Group||Conformably underlies the Mernmerna Formation (Bendieuta Member). Interfingers with the Oraparinna Shale at top.|Massive, buff to pale yellow, silty to part sandy and oolitic archaeocyathan limestones, part dolomitic with calciate brachiopods.|
20045|Wilkawillina Limestone|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Shown in image on p1, 'Archaeocyaths in the Wilkawillina Limestone, Brachina Gorge' (photo 038766). Reefal limestone later formed a karst terrain.||||Overlies Bonney Limestone, ?Parachilna Formation, Woodendinna Dolomite and underlies Mernmerna Formation.|Light to dark grey, massive, bedded archaeocyathan limestone. A major erosional surface defined by karsting and a red weathering crust occurs within the unit.|
20045|Wilkawillina Limestone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature. Potential hydrocarbon reservoir and fairway.||Hawker Group||Unconformably overlain by Mernmerna Formation.||
20045|Wilkawillina Limestone|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Eoredlichia shensiensis trilobite fossils.||||Overlies the Woodendinna Dolomite, underlies the Bunkers Sandstone.|Carbonate rocks.|
20054|Wilkinson Cliff Limestone|31013|6|Mentioned|p3|||Upper Silurian||||||
20054|Wilkinson Cliff Limestone|33325|5|Briefly described|Table 2|||||||||
20054|Wilkinson Cliff Limestone|34692|5|Briefly described|p186|||||||||
20054|Wilkinson Cliff Limestone|43479|14|Not recorded|p116||Ludlovian|||||||
20078|Willbriggie clay loam|39512|6|Mentioned|p2|||||||||
20079|Willi Willi Limestone Member|34293|3|Fully described|p49|||Permian. Geological map P43.||||||
20084|Williams River Member|22857|5|Briefly described|p508 App.1 Tb.A1.8|Visean|Visean|Of the Chichester Formation. Conglomerate with interbeds of volcanics at base. Max. thickness: 300m. Geological Province: Tamworth Forearc Basin.||||||
20084|Williams River Member|36528|6|Mentioned|p178|||||||||
20084|Williams River Member|44244|4|Described|p64, p113|Visean|Visean|Of the Chichester Formation.  Max. thickness: 300m.  Type section in text.  Geological Province: Gresford Block.||||||30-AUG-04
20084|Williams River Member|50147|5|Briefly described|Map legend|Visean|Visean|Of the Chichester Formation.  Conglomerate with clasts of ignimbrite and minor sediment and granitoids set in a mtarix of red lithic sandstone.  Geological Province: Gresford Block||||||
20085|Williamsdale Dacite Member|42820|6|Mentioned|p40|||||||||
20085|Williamsdale Dacite Member|49690|3|Fully described|p7, p17-21, Appendix|Early Devonian|Late Silurian|Essentially a redefinition of Richardson's (1979) Williamsdale Volcanics. 2000-4000 m thick. Variation in ages may be due to chloritisation of the biotite analysed, and/or post-Silurian regional deformation.|418 +/- 3 Ma (K/Ar) to 403 +/- 4 Ma (Rb/Sr).|Colinton Volcanics|||Generally massive, pale to dark grey, dacitic crystal tuff; biotite in lower part; conspicuous inclusions of recrystallised pumice fragments.|05-DEC-13
20085|Williamsdale Dacite Member|69635|4|Described|p25-31|Ludlow|Wenlock|Eastern Lachlan Orogen. U-Pb SHRIMP zircon magmatic crystallisation age. Sample overlies Colinton Volcanics sample CAPTLJD0008.01A|427.5+/-3.1 Ma|Of Colinton Volcanics||Temporal equivalent to Kohinoor Volcanics, Woodlawn Volcanics.|Crystal-rich, medium-grained ignimbrite.|
20119|Willow Glen Formation|22529|4|Described|6|Ludlow|Wenlock|Parent Tannabutta Group||||||
20119|Willow Glen Formation|22590|6|Mentioned|Fig3 P754||Ludlow|Actually spelt Willow Glen Fm.||||||
20119|Willow Glen Formation|22857|4|Described|p476 App.1 Tb.A1.6|Pridoli|Pridolian|Of the Tannabutta Group. Conglomerate, pebbly and lithic arenite, fossiliferous mudstone and limestone. Max. thickness: 1000m. Geological Province: Capertee Rise.||||||
20119|Willow Glen Formation|23043|5|Briefly described|Map Legend|Ludlow|Ludlow|of Tannabutta Group.||||||
20119|Willow Glen Formation|23170|2|Defined|p66|Ludlow|Wenlock|Tannabutta Group.||||||
20119|Willow Glen Formation|36285|2|Defined|p54|Silurian|Silurian|See also Fig.2.& 3. Variation of Willow Formation ?||||||
20119|Willow Glen Formation|39660|6|Mentioned|p450|||||||||
20119|Willow Glen Formation|40106|6|Mentioned|p593|||||||||
20119|Willow Glen Formation|43188|4|Described|p203,Table 2 p201|Ludlovian|Wenlockian|Type section location given in Table 2. See also Fig. 2 p197.||||||
20119|Willow Glen Formation|44093|5|Briefly described|p211 App. 1|Ludlovian|Wenlockian|Geological Province: Lachlan Fold Belt.||||||
20119|Willow Glen Formation|66197|6|Mentioned|p633 Fig.4a|Pridoli|Wenlock|Capertee High-Hill End Trough. Locally overlies Dungeree Volcanics; is overlain by Toolamanang and Millsville Formations.||||||14-MAR-12
20121|Willowie Creek beds|22857|5|Briefly described|p319 Fig. 22.10B|Late Devonian|Late Devonian|Geological Province: Clarence-Moreton Basin.||||||
20121|Willowie Creek beds|22865|6|Mentioned|Fig22.10bp319||Late Devonian|||||||
20121|Willowie Creek beds|23812|5|Briefly described|p9, 10|Devonian|Silurian|Included in the Silverwood Group.||||||
20121|Willowie Creek beds|38755|5|Briefly described|p65 Fig.1, p67|Devonian|Silurian|Geological Province: Coffs Harbour Block||||||
20121|Willowie Creek beds|39648|6|Mentioned|p258|||||||||
20121|Willowie Creek beds|39673|3|Fully described|p226|||||||||
20121|Willowie Creek beds|40514|6|Mentioned|p5|||||||||
20121|Willowie Creek beds|40960|6|Mentioned|p216|||||||||
20121|Willowie Creek beds|42378|6|Mentioned|Table 1 P11|||||||||
20121|Willowie Creek beds|42629|5|Briefly described|p358|||||||||
20121|Willowie Creek beds|42719|4|Described|p7|||||||||
20121|Willowie Creek beds|60079|5|Briefly described|Map Legend|Devonian|Silurian|Of the "Silverwood Association".||||||
20121|Willowie Creek beds|60937|5|Briefly described|p424 Fig. 2|||||||||
20121|Willowie Creek beds|60995|5|Briefly described|p51 Fig. 3|Late Devonian|Late Devonian|Geological Province: Clarence-Moreton Basin. See also p56 Fig. 7.||||||
20121|Willowie Creek beds|61392|5|Briefly described|p163, p174|Late Devonian|Cambrian|Stratigraphy and facies characteristics very similar to the Silverwood Group - effectively the same sequence. Subunits consist of: slate, greenstone, greywacke and tuffaceous blue-grey mudstones. See also "Willowie Creek beds".||||||07-FEB-11
20121|Willowie Creek beds|61761|6|Mentioned|p4|||||||||07-FEB-11
20121|Willowie Creek beds|61770|6|Mentioned|p108|||||||||
20121|Willowie Creek beds|68679|6|Mentioned|p445|||||||Equivalent to the Silverwood Group.||
20121|Willowie Creek beds|71628|5|Briefly described|p9: 13, 29, 35-36; p18-13; p19: 147-148|||Hosts the Paddy Doughty Cu (As, Zn, Au) mine.||Silverwood Group.||Is intruded by Towgon Grange Tonalite and Purgatory Monzogranite. Equivalent to Silverwood Group (Henley et al., 2001).|Metasediment, argillite, hornfels.|
20135|Willyama Supergroup|6823|5|Briefly described|p203-205, 206, 233, 234, 236|Paleoproterozoic|Paleoproterozoic|Interpreted by Gustafson et al (1950) as a sequence of montonously alternating beds of clays, sandy clays and sands, intruded by thick granitic sills, thinner sills of gabbros and finally by sheets of pegmatite varying from very thick to very thin, all predominantly along bedding planes. This was more recently reinterpreted by Johnson and Klinger (1976), Stanton (1976), Archibald (1978), and Stevens et al (1983, 1988) as an upwards-fining, conformable 'layer cake' sequence 7-11km thick which can be correlated throught the Broken Hill Block. This sequence was supposedly punctuated by intervals of bimodal volcanism and minor exhalative chemical sediments. This study argues that the sequence includes granitic intrusions.|||||Garnet-cordeirite-sillimanite gneisses, amphibolites and augen and platy quartzo-feldspathic gneiss.|26-MAR-22
20135|Willyama Supergroup|22456|5|Briefly described|p16,fig15|||on map||||||
20135|Willyama Supergroup|22500|5|Briefly described|p 1||Proterozoic|Broken Hill Block||||||
20135|Willyama Supergroup|22553|3|Fully described|p75,fig1p76,p77||Proterozoic|||||||
20135|Willyama Supergroup|22575|4|Described|p178|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22588|4|Described|p85|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22631|5|Briefly described|table1p171,fig2,p170|Statherian|Statherian|||||||
20135|Willyama Supergroup|22641|5|Briefly described|p687, Fig.2 p689|Paleoproterozoic|Paleoproterozoic|See also p693||||||07-NOV-08
20135|Willyama Supergroup|22671|5|Briefly described|p832,Fig1p835||Paleoproterozoic|Geological Province: Adelaide Fold Belt.||||||07-NOV-08
20135|Willyama Supergroup|22709|6|Mentioned|p201|||||||||
20135|Willyama Supergroup|22712|5|Briefly described|p131|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|22720|6|Mentioned|Table 4 (p166)||Paleoproterozoic|Broken Hill Block||||||07-NOV-08
20135|Willyama Supergroup|22752|5|Briefly described|p 275||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22771|4|Described|p44-45,Table12.2p45||Statherian|Max Age: 1720 Ma.||||||
20135|Willyama Supergroup|22772|6|Mentioned|p53,62,70||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22773|5|Briefly described|Fig24.5p350|Precambrian|Precambrian|||||||
20135|Willyama Supergroup|22789|6|Mentioned|p50|||||||||
20135|Willyama Supergroup|22811|5|Briefly described|p604||Statherian|||||||
20135|Willyama Supergroup|22857|3|Fully described|p31, p44-45, p388 App1 Tb.A1.1|Paleoproterozoic|Paleoproterozoic|Multiply deformed metasedimentary schists and gneisses with abundant quartzofeldspathic gneisses, lesser mafic gneisses and minor 'lode' rocks. Max. Age: 1720Ma. Max. thickness: 9km. Geol.Prov: Adelaide Fold Belt (Willyama F.B.). See also p350 Fig.24.5.||||||07-SEP-09
20135|Willyama Supergroup|22858|6|Mentioned|p92,Fig14.9p100||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22884|5|Briefly described|p40 Fig. 1, p39, p43 Fig3||Paleoproterozoic|Located across the Olary and Broken Hill Domains.||||||26-MAR-09
20135|Willyama Supergroup|22887|5|Briefly described|Fig.5 p12|Precambrian|Precambrian|||||||
20135|Willyama Supergroup|22933|6|Mentioned|Table11.1p5||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22939|5|Briefly described|p243||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22956|6|Mentioned|p146||Proterozoic|||||||
20135|Willyama Supergroup|22959|4|Described|p95,96,101||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22960|4|Described|p89,90||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22962|5|Briefly described|p73||Statherian|||||||
20135|Willyama Supergroup|22963|6|Mentioned|p67||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|22964|5|Briefly described|p53,54||Proterozoic|||||||
20135|Willyama Supergroup|22966|5|Briefly described|p2,4||Proterozoic|||||||
20135|Willyama Supergroup|22967|4|Described|p21,2,4-7,30,3,41,3,||Statherian|||||||
20135|Willyama Supergroup|23025|5|Briefly described|p74|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|23068|5|Briefly described|p783|||||||||
20135|Willyama Supergroup|23093|5|Briefly described|p619||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23094|5|Briefly described|p616|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|23154|6|Mentioned|Map Legend|Mesoproterozoic|Mesoproterozoic|||||||
20135|Willyama Supergroup|23155|6|Mentioned|Fig 5 on p12|||||||||
20135|Willyama Supergroup|23160|5|Briefly described|p870 fig1||Proterozoic|||||||
20135|Willyama Supergroup|23210|5|Briefly described|p26||Paleoproterozoic|Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|23223|5|Briefly described|p39, Fig.1|||Informally divided into upper (see p.40) and lower (see p.39) - Age: ~1720 - 1650 Ma. of Curnamona Province.||||||
20135|Willyama Supergroup|23248|5|Briefly described|p168||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23336|6|Mentioned|p10|||||||||21-MAR-06
20135|Willyama Supergroup|23345|6|Mentioned|43|||||||||
20135|Willyama Supergroup|23346|5|Briefly described|48|||||||||
20135|Willyama Supergroup|23347|5|Briefly described|p51 Tb. 1, p53 Fig. 3|Statherian|Statherian|Age: ~1.71-1.64Ga. Comprises Strathearn and Curnamona Groups, Lady Louise and Basso Suites.||||||24-MAR-09
20135|Willyama Supergroup|23351|5|Briefly described|283|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|23380|5|Briefly described|p105||Proterozoic|of Broken Hill Block. Age: Middle Proterozoic.||||||
20135|Willyama Supergroup|23391|6|Mentioned|p6|||||||||
20135|Willyama Supergroup|23476|5|Briefly described|p50|||||||||
20135|Willyama Supergroup|23477|5|Briefly described|p49 Fig 3|Mesoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|23478|5|Briefly described|p27|||Olary Province.||||||
20135|Willyama Supergroup|23565|5|Briefly described|p193|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-NOV-08
20135|Willyama Supergroup|23731|6|Mentioned|p15|||||||||
20135|Willyama Supergroup|23775|5|Briefly described|p721|||||||||22-SEP-09
20135|Willyama Supergroup|23801|6|Mentioned|p20|||||||||
20135|Willyama Supergroup|23912|5|Briefly described|p778|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|24197|5|Briefly described|p62|||Dominates the Broken Hill Block region. Comprises 5 main groups including Thackaringa, Broken Hill, Sundown and Paragon Groups.||||||07-FEB-11
20135|Willyama Supergroup|24286|5|Briefly described|p25 Fig.2|||||||||
20135|Willyama Supergroup|24289|5|Briefly described|p42 Fig.1, p44, p46|Paleoproterozoic|Paleoproterozoic|Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|24307|4|Described|p966|Proterozoic|Proterozoic|Thickness: 7000m.||||||21-OCT-08
20135|Willyama Supergroup|24431|5|Briefly described|p190|Statherian|Statherian|Age: ~1710 - 1650 Ma. Geological Province: Olary Domain.||||||
20135|Willyama Supergroup|24522|6|Mentioned|p80 Fig. 2|||Metasedimentary and bimodal meta-igneous rocks.  Age: 1.69Ga (Page and Laing 1992). Geological Province: Curnamona Province (SA).  See also p82.||||||
20135|Willyama Supergroup|24526|5|Briefly described|p99|Paleoproterozoic|Paleoproterozoic|Metasedimentary rocks.  Age: c.1710-1649Ma.  Geological Province: Curnamona Craton.||||||07-NOV-08
20135|Willyama Supergroup|24582|5|Briefly described|p4|Paleoproterozoic|Paleoproterozoic|Includes Wiperaminga Subgroup. In the Olary Block.  Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|24592|4|Described|p634|Paleoproterozoic|Paleoproterozoic|Age: ca. 1710 - 1640 Ma. Of the Willyama Supergroup. Geological Province: Curnamona Province. Divided into the basal Quartzo-feldspathic Suite, and overlying Calc-silicate and Pelite Suites based on magnetic susceptibility.||||||09-MAY-13
20135|Willyama Supergroup|38969|4|Described|p199|||||||||
20135|Willyama Supergroup|39662|2|Defined|p408|Paleoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|39849|6|Mentioned|p86|||See also P87||||||
20135|Willyama Supergroup|39883|6|Mentioned|p380|||||||||
20135|Willyama Supergroup|39885|6|Mentioned|p427|||||||||
20135|Willyama Supergroup|40290|6|Mentioned|p1|||||||||
20135|Willyama Supergroup|40291|6|Mentioned|p9|||See also Fig.3||||||
20135|Willyama Supergroup|40448|5|Briefly described|p30|||||||||
20135|Willyama Supergroup|40582|6|Mentioned|p467|||||||||
20135|Willyama Supergroup|40595|5|Briefly described|p73|||||||||
20135|Willyama Supergroup|40642|6|Mentioned|p163|||||||||
20135|Willyama Supergroup|40914|6|Mentioned|Map legend|Mesoproterozoic|Paleoproterozoic|Early to Middle Proterozoic||||||07-NOV-08
20135|Willyama Supergroup|41006|6|Mentioned|p292|||||||||
20135|Willyama Supergroup|41092|6|Mentioned|Table 1|||||||||
20135|Willyama Supergroup|41093|4|Described|p250|||||||||
20135|Willyama Supergroup|41145|3|Fully described|p827|||||||||
20135|Willyama Supergroup|41402|5|Briefly described|p37|||||||||
20135|Willyama Supergroup|41403|6|Mentioned|p48|||||||||
20135|Willyama Supergroup|41419|6|Mentioned|p379|||||||||
20135|Willyama Supergroup|41526|6|Mentioned|p14|||||||||
20135|Willyama Supergroup|41630|5|Briefly described|p3|||||||||
20135|Willyama Supergroup|41633|6|Mentioned|p154|||See also Fig.2.27||||||
20135|Willyama Supergroup|41651|6|Mentioned|p188|||||||||
20135|Willyama Supergroup|41652|5|Briefly described|p193|||||||||
20135|Willyama Supergroup|41791|5|Briefly described|p267|||||||||
20135|Willyama Supergroup|41859|6|Mentioned|p426|||||||||
20135|Willyama Supergroup|41870|6|Mentioned|p131|||||||||
20135|Willyama Supergroup|41978|6|Mentioned|p495|||||||||
20135|Willyama Supergroup|42090|3|Fully described|p14|||See also Table 2||||||
20135|Willyama Supergroup|42098|6|Mentioned|p57|||||||||
20135|Willyama Supergroup|42171|6|Mentioned|p142|||||||||
20135|Willyama Supergroup|42181|6|Mentioned|p252|||||||||
20135|Willyama Supergroup|42223|6|Mentioned|Fig.2 P36|||||||||
20135|Willyama Supergroup|42261|6|Mentioned|p529|||See also Fig.1 P530.||||||
20135|Willyama Supergroup|42263|6|Mentioned|p15|||With "quartz bands up to 1/2" thick are drag and reverse folded".||||||
20135|Willyama Supergroup|42286|6|Mentioned|p7|||||||||
20135|Willyama Supergroup|42323|5|Briefly described|p3|Mesoproterozoic|Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|42357|6|Mentioned|p8|||||||||
20135|Willyama Supergroup|42507|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42527|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42528|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42529|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42530|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42531|5|Briefly described|Map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42537|5|Briefly described|p3|||||||||
20135|Willyama Supergroup|42595|5|Briefly described|p3, p5|||||||||
20135|Willyama Supergroup|42672|5|Briefly described|p372|||||||||
20135|Willyama Supergroup|42720|5|Briefly described|map legend|Paleoproterozoic||||||||07-NOV-08
20135|Willyama Supergroup|42725|5|Briefly described|p5|||||||||
20135|Willyama Supergroup|42746|6|Mentioned|p3|||||||||
20135|Willyama Supergroup|42755|6|Mentioned|p4|||||||||
20135|Willyama Supergroup|42813|4|Described|p9|||||||||
20135|Willyama Supergroup|42819|5|Briefly described|p315|||||||||
20135|Willyama Supergroup|42871|5|Briefly described|p88|||||||||
20135|Willyama Supergroup|42897|5|Briefly described|p319|||see also Fig.3, P321||||||
20135|Willyama Supergroup|42942|6|Mentioned|p17|||||||||
20135|Willyama Supergroup|42966|5|Briefly described|Fig.25 p47|||||||||
20135|Willyama Supergroup|42982|5|Briefly described|Fig.1,p332|||||||||
20135|Willyama Supergroup|42991|6|Mentioned|Fig.3|||||||||
20135|Willyama Supergroup|43052|4|Described|p82|||||||||
20135|Willyama Supergroup|43086|5|Briefly described|p1|||||||||
20135|Willyama Supergroup|43141|6|Mentioned|p63,Fig.1|||||||||
20135|Willyama Supergroup|43192|6|Mentioned|p62|||Same as Willyama Complex,p58.||||||
20135|Willyama Supergroup|43213|6|Mentioned|p63|Mesoproterozoic|Mesoproterozoic|Broken Hill Block. Tentatively equated with Ponto beds of Wonominta Block.||||||
20135|Willyama Supergroup|43264|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43265|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43266|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43267|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43268|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43269|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43270|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43271|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43272|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43273|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43274|5|Briefly described|Map Legend||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43485|5|Briefly described|2-3|||||||||
20135|Willyama Supergroup|43561|5|Briefly described|Fig.3,1434,1438|||1690 Ma||||||
20135|Willyama Supergroup|43572|6|Mentioned|p5||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|43583|6|Mentioned|p2138|||||||||
20135|Willyama Supergroup|43591|6|Mentioned|p163|||||||||
20135|Willyama Supergroup|43595|4|Described|p75,354-5|||Max. age of deposition: approx. 1.82 Ga, high-grade metamorphism: 1.66 Ga, intruded at 1.49 Ga||||||
20135|Willyama Supergroup|43685|5|Briefly described|p243||Paleoproterozoic|||||||07-NOV-08
20135|Willyama Supergroup|44093|5|Briefly described|p28, p41|Mesoproterozoic|Paleoproterozoic|See also p139 Appendix 1. Supersedes the Willyama "Complex". Sequence of highly deformed metasedimentary and meta-igneous schists and gneisses, and minor 'lode' rocks. Forms the Australian Craton. Geological Province: Willyama Fold Belt.||||||09-JUL-13
20135|Willyama Supergroup|44195|6|Mentioned|p349|||Broken Hill. Compared to Soldiers Cap Group.||||||
20135|Willyama Supergroup|46598|3|Fully described|p298|||||||||
20135|Willyama Supergroup|50045|5|Briefly described|p116, p116 Fig. 3|||Geological Province: Broken Hill Block. Includes the Thackaringa Group, Broken Hill Group and Paragon Group.||||||31-MAY-07
20135|Willyama Supergroup|50081|5|Briefly described|p43|Statherian|Statherian|Age: ~1710-1640 Ma. Geological Province: Curnamona Province.||||||24-FEB-05
20135|Willyama Supergroup|50547|5|Briefly described|p1226|||||||||
20135|Willyama Supergroup|50605|6|Mentioned|p6.1, 9.1|Paleoproterozoic|Paleoproterozoic|Geological Province: Olary Block. Intruded by Olary 1590 Ma Supersuite.||||||07-NOV-08
20135|Willyama Supergroup|50606|6|Mentioned|p1.1|||Geological Province: Broken Hill Block.||||||
20135|Willyama Supergroup|50619|5|Briefly described|p174 Fig. 1, p178 Fig. 3|Paleoproterozoic|Paleoproterozoic|Comprises the Paragon, Sundown, Broken Hill and Thackaringa Groups, Thorndale Composite Gneiss and the Clevedale Migmatite.  Geological Province: Broken Hill Block.  See also p175.||||||07-NOV-08
20135|Willyama Supergroup|60485|5|Briefly described|p28 Fig. 2|||Geological Province: Olary and Broken Hill Domains.||||||
20135|Willyama Supergroup|60953|5|Briefly described|Map Legend|Paleoproterozoic|Paleoproterozoic|Age: ~1730-1650Ma. Greenschist to granulite facies metasediments and mafic and felsic metavolcanics and intrusives.||||||07-NOV-08
20135|Willyama Supergroup|60959|5|Briefly described|Map Legend|Mesoproterozoic|Paleoproterozoic|Undifferentiated metasediments.||||||07-NOV-08
20135|Willyama Supergroup|61032|5|Briefly described|p6|Paleoproterozoic|Paleoproterozoic|Includes Wiperaminga Subgroup.||||||07-NOV-08
20135|Willyama Supergroup|61108|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic|Metasediment and felsic metavolcanic rock, greenschist to granulite facies. Mafic and felsic metamorphosed volcanic and intrusive rock. Age: ~1730-1650 Ma.||||||07-NOV-08
20135|Willyama Supergroup|61235|5|Briefly described|p13 Fig. 1|||Geological Province: Curnamona Province.||||||11-AUG-05
20135|Willyama Supergroup|61239|5|Briefly described|p53 Fig. 1|||||||||
20135|Willyama Supergroup|61262|5|Briefly described|p455 Fig. 11|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill.||||||07-NOV-08
20135|Willyama Supergroup|61311|6|Mentioned|p42|||||||||
20135|Willyama Supergroup|61314|6|Mentioned|p120|||||||||
20135|Willyama Supergroup|61318|5|Briefly described|p580.|Proterozoic|Proterozoic|Hosts a major stratiform Zn-Pb-Ag ore deposit at Broken Hill. General north-to-south increase of metamorphic grade from greenschist to granulite facies. Rocks have been folded and sheared.|||||Metamorphosed sequence of pelitic to psammitic sediments, subordinate felsic and mafic volcanic rocks and minor intercalated intrusive rocks.|
20135|Willyama Supergroup|61605|5|Briefly described|p768, p769|Paleoproterozoic|Paleoproterozoic|Incl: Thackaringa and Broken Hill Gps. Aluminous metasedimentary gneisses+locally abundant albite-rich rocks, basic gneisses (amphibolites), lesser quartzo-feldspathic gneisses; substantial bodies of deformed pegmatite and leucocratic quartzo-feldspathics||||||07-NOV-08
20135|Willyama Supergroup|61734|5|Briefly described|p51, p52 Fig.2, p54, p56, p67-68|Mesoproterozoic|Paleoproterozoic|Deposition in intracontinental rift or continental back-arc basin.|1720-1640 Ma||Includes the Curnamona and Strathearn Groups.||Package of metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|61735|5|Briefly described|p634, p635 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Broken Hill Domain. Discussed from a geochronological aspect. See also p636 Fig. 2.||||||04-JUN-15
20135|Willyama Supergroup|61736|4|Described|p663|Paleoproterozoic|Paleoproterozoic|Subdivided into Lower and Upper Willyama Supergroups. Geological province: Broken Hill Domain. Chronostratigraphy discussed on p670-71.||||||24-FEB-10
20135|Willyama Supergroup|61822|5|Briefly described|p104|Paleoproterozoic|Paleoproterozoic|Part of the southern Broken Hill Domain and the southeastern Euriowie Domain.||||||07-NOV-08
20135|Willyama Supergroup|61825|5|Briefly described|p130|Paleoproterozoic|Paleoproterozoic|Metasediments and meta-igneous rocks. Intruded by Mundi Mundi Granites. Geological Province: Broken Hill Domain and Eurowie Domain.||||||07-NOV-08
20135|Willyama Supergroup|61908|5|Briefly described|p146|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block.||||||07-NOV-08
20135|Willyama Supergroup|61936|6|Mentioned|p203|||Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|62373|5|Briefly described|p502|Paleoproterozoic|Paleoproterozoic|Metasedimentary sequence. Age: 1715-1645 Ma (Page et al 1998, 2000, 2003). Geological Province: Curnamona Province - Olary and Broken Hill Domains.||||||09-JUL-13
20135|Willyama Supergroup|62473|5|Briefly described|p72-74|||Stratigraphic coherence of the rocks of this supergroup is debated.||||||17-JUN-09
20135|Willyama Supergroup|62514|5|Briefly described|p746|||Basso Suite included. Includes pelitic and psammitic metasediments. Geological Province: Olary Domain/Curnamona Province.||||||09-JUL-13
20135|Willyama Supergroup|62535|5|Briefly described|p663-665, p668, p670-674|Paleoproterozoic|Paleoproterozoic|Dominant unit in the Curnamona Province. Base and top are indeterminate; thickness estimated at c.7 km. Multiply deformed, metamorphosed and locally intensely metasomatically altered during the ~1600 Ma Olarian Orogeny. Hosts minor strata-bound gold mineralization. Correlations discussed.|~1720-1640 Ma.||Broken Hill Group.|||
20135|Willyama Supergroup|62536|5|Briefly described|p633-636, 638, 640, 642, 647, 649, 651|Paleoproterozoic|Paleoproterozoic|See also p653, 655, 657-659. Broken Hill area. Deposition spanned ~70 m.y.|||Thackaringa, Broken Hill Groups.||Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|62592|4|Described|pp12-15, p16 Fig.2.2, p43, pp73-76, p78.|Late Paleoproterozoic|Late Paleoproterozoic|Curnamona Province. About 20,000 km2 in area and >7 km thick; neither top nor base have been observed. A-type plutons aged c.1712 Ma intrude the earliest rocks of this unit. Youngest bimodal magmatism was c.1685 Ma; youngest preserved sedimentary rocks are c.1640 Ma, with a further 20 m.y. deposition equivalent to the upper McNamara Group of the Mount Isa Inlier.|c.1718 - <1640 Ma.||Includes Thackaringa, Broken Hill, Sundown, Paragon, Curnamona and Strathearn Groups.||Bimodal volcanics and shallow-water sedimentary deposits, with deeper-water deposition in upper parts.|
20135|Willyama Supergroup|62641|6|Mentioned|p275, p286, p288-289.|||Curnamona (Broken Hill) region. Provenance correlations drawn with Nawa Domain (South Australian Craton) and Maronan Supergroup (Mount Isa region) suggest contiguity during late Paleoproterozoic; the lower part  of the Supergroup received detritus from Arunta region. It contains syn-depositional intrusives aged c.1715 Ma.||||||
20135|Willyama Supergroup|62724|5|Briefly described|p17 Fig. 4|Mesoproterozoic|Paleoproterozoic|First called "Willyama Complex" (Mawson 1912). Geological Province: Broken Hill and Olary Domains / Curnamona Province. See also p16 Fig. 2.||||||07-FEB-11
20135|Willyama Supergroup|62727|5|Briefly described|p8|||Host to uranium by cavity fill (fractures, veins, apophyses - within sodic granitoids of the group).  Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|62728|5|Briefly described|p26, p28|||Conformably encloses gneisses of the Basso Suite. See also Willyama Supergroup metasediments.||||||07-FEB-11
20135|Willyama Supergroup|62993|5|Briefly described|p1-6, 12,14-16,18,20, 22,23,28-32,35, 37|Paleoproterozoic|Paleoproterozoic|Broken Hill Domain and Olary Domains. See also figs on pp40, 44.|||Includes Broken Hill Group, Curnamona Group, Strathearn Group, Thackaringa Group, Rantyga Group, Sundown Group, Paragon Group|Intruded by Basso Suite, Bimbowrie Suite|Psammopelitic, psammitic, calcareous and calc-albititc metasediments.Pelitic kyanite bearing metasediments,|19-DEC-21
20135|Willyama Supergroup|63020|6|Mentioned|p971|||||||||
20135|Willyama Supergroup|63056|5|Briefly described|p81 Fig. 2|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|63102|5|Briefly described|p7-8,10, 12-14,22,32,35-36,38-39,44,52|Mesoproterozoic|Paleoproterozoic|Geological province: Curnamona Province. Total thickness unknown as neither top nor base have been observed. Estimated to be approximate 5km in Olary Domain (Laing 1996b), but between 4.5-13km in the Broken Hill Domain (Willis et al 1983). Source material for the Willyama Supergroup that is older than Mount Howden and Paragon groups may be the Arunta terrane of central Australia. See also p47, p60-61,63,67.|||Includes Broken Hill and Curnamona groups.|||22-OCT-19
20135|Willyama Supergroup|63110|6|Mentioned|p1130|||||||||
20135|Willyama Supergroup|63186|4|Described|p66|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa Group, and Wiperaminga and Ethiudna Subgroups. Age: 1720-1645 Ma. Geological Province: Curnamona Province.||||||07-NOV-08
20135|Willyama Supergroup|63489|5|Briefly described|Map legend|Paleoproterozoic|Paleoproterozoic|Represented by unnamed and undifferentiated metsediments and units. Geological Province: Mount Painter Inlier and Mount Babbage Inlier.||||||07-NOV-08
20135|Willyama Supergroup|63519|5|Briefly described|p8, p10 Fig. 3|Paleoproterozoic|Paleoproterozoic|Geological Province: Broken Hill Block-Euriowie Block.||||||07-NOV-08
20135|Willyama Supergroup|63539|5|Briefly described|p33 Fig. 1a|||Geological Province: Curnamona Province.||||||07-FEB-08
20135|Willyama Supergroup|63793|6|Mentioned|pp10-11.|||Broken Hill Block.||||||
20135|Willyama Supergroup|63866|4|Described|p34-p42, p44, p48|Statherian|Statherian|Broken Hill and Olary Domains, Curnamona Province. Deposited in a shallow marine environment. Rocks are metamorphosed to granulite-facies in the south and greenschist facies to the north. Informally subdivided into an upper and lower part on p38. Appears as the Willyama SG on p37. Also includes the Clevedale Migmatite, Thorndale Composite Gneiss, Redan Gneiss, Ednas Gneiss, Mulculca Formation|1719-1640 Ma||Includes the Broken Hill Group and the Thackaringa Group, Sundown Group, Curnamona Group, Paragon Group and the Strathearn Group.||Psammites, pelites, calc-silicates and carbonates. The lower part consists of migmatites, metasedimentary rocks, psammitic to psammopelitic gneisses passing up into gneisses interpreted as metamorphosed rhyodacitic flows or tuffs.|
20135|Willyama Supergroup|64097|4|Described|p302|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa, Broken Hill and Paragon Gps, and new Rantyga Group. Geol Prov: Broken Hill Domain + Olary Domain/Curnamona Prov.Succession of metaseds.+ minor metavolcs., extensively intruded ??..Considerable age evidence for constituents discussed.||||||07-FEB-11
20135|Willyama Supergroup|64130|6|Mentioned|p1382 |||Curnamona Province. Hosts the giant Broken Hill Pb-Zn-Ag deposit.||||||
20135|Willyama Supergroup|64249|6|Mentioned|p102|||Geological Province: Eastern Fold Belt. Albites are abundant in this unit.||||||22-APR-09
20135|Willyama Supergroup|64250|6|Mentioned|p25 fig 10|||Broken Hill Province.|||Includes Thackaringa, Broken Hill, Sundown, Paragon Groups.|||
20135|Willyama Supergroup|64316|5|Briefly described|p532, p533 Fig. 1|Paleoproterozoic|Paleoproterozoic|Includes Thackaringa, Broken Hill, Sundown and Paragon Groups. Upper section is turbiditic metasedimentary package dominated by Sundown Group. Geological Province: Broken Hill Block.||||||07-FEB-11
20135|Willyama Supergroup|64576|6|Mentioned|p636|||||||||
20135|Willyama Supergroup|64722|5|Briefly described|Fig. 2 p3-6, p14-15, 22|Statherian|Statherian|Curnamona Province. Age from intercalated tuffs.|1720 - 1640 Ma.||Contains Weekaroo Amphibolite; Bumba Formation (Olary Block); Paragon, Sundown, Broken Hill, Thackaringa Groups; Thorndale Gneiss; Clevedale Migmatite (Broken Hill region).|||11-APR-12
20135|Willyama Supergroup|64724|5|Briefly described|p46|Proterozoic||||||||
20135|Willyama Supergroup|64725|5|Briefly described|p58 Fig.2, pp71-72.|||Olary-Willyama Block. Sedimentary and bimodal volcanic rocks; hosts the stratiform Broken Hill massive sulfide deposits.|c.1730-1700 Ma.|||||
20135|Willyama Supergroup|64726|6|Mentioned|p89.|||Deeper water sedimentation along the eastern margin of the Australian continent after c.1670 Ma.||||||
20135|Willyama Supergroup|64741|4|Described|p297-8, p312-313|Paleoproterozoic|Paleoproterozoic|Age: ~1720-1640Ma. Geological province: Broken Hill and Olary Domains, Curnamona Province.||||||07-FEB-11
20135|Willyama Supergroup|64742|4|Described|pp318-335.|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Metamorphosed to granulite facies during the c.1600 Ma Olarian Orogeny; later (c.500 Ma) by the Delamerian Orogeny. Contains the world's largest known Pb-Zn-Ag deposit at Broken Hill. c.7 km thick.|||Includes Curnamona and Strathearn Groups in the Olary Domain; and Thackaringa, Broken Hill, Sundown and Paragon Groups in the Broken Hill Domain.||Sequence of generally shallow water metamorphosed quartzofeldspathic and pelitic sedimentary rocks, calc-silicates, minor volcanic and subvolcanic rocks.|
20135|Willyama Supergroup|64743|5|Briefly described|pp339-343, p346 Fig.7.|Paleoproterozoic|Paleoproterozoic|Discusses timing and tectonism of deformation of this unit.|||Includes Thackaringa, Broken Hill, Sundown and Paragon Groups.|||
20135|Willyama Supergroup|64744|5|Briefly described|pp352-354, p356, pp359-360, pp362-367.|Statherian|Statherian|Includes rocks from Calvert and Isa superbasins. Deformed and metamorphosed up to granulite facies. Intruded by S- and A-type granites, and mafic dykes and sills, between 1710-1680 Ma.|||SA = Wiperaminga, Ethiudna, Saltbush and Mount Howden Subgroups. NSW = Redan, Thorndale Composite, Alma, Rasp Ridge Gneisses; Clevedale Migmatite; Thackaringa, Broken Hill, Sundown, Paragon Groups.|||
20135|Willyama Supergroup|64896|6|Mentioned|p1390|||Geological Province: Curnamona Province.||||||
20135|Willyama Supergroup|64944|6|Mentioned|p26, p28 Fig. 1|Paleoproterozoic|Paleoproterozoic|Geological province: Olary Domain.||||||07-FEB-11
20135|Willyama Supergroup|65194|6|Mentioned|p40, p42-43|||||||||
20135|Willyama Supergroup|65220|5|Briefly described|p20, p21 Fig. 3|Paleoproterozoic|Paleoproterozoic|of the Curnamona Province. Informal subdivisions and age: 1715-1600 Ma shown in Fig. 3||||||10-DEC-09
20135|Willyama Supergroup|65375|6|Mentioned|p13.|Paleoproterozoic|Paleoproterozoic||c.1720-1640 Ma.|||||
20135|Willyama Supergroup|65376|6|Mentioned|p9 Fig.1.2. |Paleoproterozoic|Paleoproterozoic||||||Metasediments and felsic volcanic rocks.|
20135|Willyama Supergroup|65390|6|Mentioned|p27 Fig. 6|Statherian|Statherian|Curnamoma Province. Age c.1720 - 1640 Ma.||||||
20135|Willyama Supergroup|65407|5|Briefly described|p238|Paleoproterozoic|Paleoproterozoic|Basement to Curnamona Province.|||||Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|65489|6|Mentioned|p18, p120|Proterozoic|Proterozoic|Part of basement to Warburton Basin.||||||
20135|Willyama Supergroup|65681|6|Mentioned|pp733-734,|Paleoproterozoic|Paleoproterozoic||c.1690 Ma.||Includes Feral gneiss, Alma and Rasp Ridge Gneisses.|||16-MAY-13
20135|Willyama Supergroup|65756|5|Briefly described|p27, 38|Mesoproterozoic|Paleoproterozoic|||||||
20135|Willyama Supergroup|65925|5|Briefly described|p61, p64, p79, Appendix 2.|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Metasedimentary and metaigneous rocks. Several granitoid suites have high uranium contents.|||||Composite gneiss suite; calc-silicate suite; amphibolite; quartzofeldspathic gneiss.|
20135|Willyama Supergroup|66302|4|Described|p7-p9, p35-p38, p40-41, p48-p52, p64|Statherian|Statherian|Broken Hill Domain, Olary Domain, Curnamona Province. Estimated to be between 7 and 13km thick. Age derived from Nutman and Gibson (1998) and Page et al. (2000). See also p72-73, p75-77, p80-81, p88-89.|ca. 1710 to 1600 Ma||Includes the Curnamona Group, Broken Hill Group, Thackaringa Group, Paragon Group, Rantyga Group, Strathearn Group, Portia Formation and the Sundown Group.|Unconformably overlain by the Benagerie Volcanics. Intruded by the Silver City Suite. Probably equivalent to the Barossa Complex.|Metasedimentary and metavolcanic rocks.|
20135|Willyama Supergroup|66518|6|Mentioned|p18, p19 Fig.4, p22.|Paleoproterozoic|Paleoproterozoic|Forms part of the basement of the Curnamona Province.||||||
20135|Willyama Supergroup|66522|6|Mentioned|p28.|Proterozoic|Proterozoic|Likely source of detrital zircons found in Kooringa Member.||||||
20135|Willyama Supergroup|66800|6|Mentioned|p933.|||Central part has been correlated (Laing & Beardsmore 1986) with older part of Etheridge Group. Also, Laing (1996b) calculated a sedimentation rate for the central part of this unit at 1 mm/yr.||||||
20135|Willyama Supergroup|66857|5|Briefly described|p971, p976.|Paleoproterozoic|Paleoproterozoic|Broken Hill and Olary Domains. Metamorphosed during Mesoproterozoic Olarian Orogeny. Relict fragmental and porphyritic textures are preserved in quartzo-feldspathic gneisses, originally rhyolitic volcaniclastics and co-magmatic A-type granitoids.|||||Pelitic, psammopelitic and psammitic schists and gneisses, albitic and calc-silicate rocks, banded iron-formation and garnet-quartz rocks.|
20135|Willyama Supergroup|67058|5|Briefly described|p494 Fig.14, p497.|||Curnamona Province. Shows detrital zircon probability plots with peaks at 1685, 1790, 2660 and 2980 Ma. The upper part of the Supergroup is aged 1655-1640 Ma.||||||
20135|Willyama Supergroup|67181|5|Briefly described|p632 Fig.14, p633 Fig.15, |Statherian|Statherian|Curnamona Province, metasediments. Age from Fig.14 Barovich and Hand (2008).|c.1710-1670 Ma|||||
20135|Willyama Supergroup|67323|5|Briefly described|p33 Fig.4.6, p34-35|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Intraplate magmatism. Underwent a depositional hiatus ~1680-1670 Ma, and partial melting ~1640 Ma.||||||
20135|Willyama Supergroup|67536|5|Briefly described|Map Legend|||Curnamona Province.|||Includes Strathearn, Broken Hill and Curnamona Groups.|Possible equivalent of the Radium Creek Metamorphics ?|Metasediments.|
20135|Willyama Supergroup|67540|5|Briefly described|p25, p26 Fig.1, p29,31 Tb.2, p37|||The intrusions (granites and minor alkaline and mafic rocks) and volcanics in central Curnamona Province are now called the Ninnerie Supersuite and they variously intrude and overlie the Willyama Supergroup.|||Includes Tommie Wattie Formation, Ameroo Subsuite, Ethiudna Subgroup.|Intruded by the Crocker Well Suite and Bimbowrie Suite. Overlain by the Benagerie Volcanic Suite.||04-FEB-16
20135|Willyama Supergroup|67581|6|Mentioned|p44 Fig.8, 45|||Curnamona Province. Intrusive and extrusive magmatic activity occurred synchronously with deposition of sediments in the lower part of this Supergroup.|||Basso, Silver City and Lady Louise Suites; Redan, Farmcote and Hores Gneisses.|||
20135|Willyama Supergroup|67653|5|Briefly described|p3-4|Late Paleoproterozoic|Late Paleoproterozoic|Geological province: Curnamona Province.|||Includes Stratheam, Broken Hill and Curnamona groups.|||
20135|Willyama Supergroup|67900|5|Briefly described|p18-19|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent polyphase deformation and metamorphism during the Olarian and Delamerian Orogenies.|1720-1640 Ma.|||Is intruded by Ninnerie Supersuite.|Metasedimentary and meta-igneous rocks.|
20135|Willyama Supergroup|68021|6|Mentioned|p131|Statherian|Statherian|Shown as lower Willyama Supergroup, Age 1730-1670 Ma.||||||
20135|Willyama Supergroup|68068|5|Briefly described|Map legend|||Curnamona Province.||||||
20135|Willyama Supergroup|68126|4|Described|p1-2, p6, p26, p30-31, p33, p48|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Geochronology data for constituent units listed. Metamorphism at 1602 +/- 4 Ma. Geochemical analyses detailed. Appears as Willyama Supersuite on p48.|<1796 +/- 10 Ma (maximum depositional age).||Strathearn, Curnamona, Paragon, Sundown, Broken Hill, Thackeringa Groups; Thorndale Composite Gneiss.||Metasediments, quartzofeldspathic gneiss, composite gneiss, quartz-albite rocks, basic gneiss, calc-silicate and calc-albitite rocks; and metavolcanics.|
20135|Willyama Supergroup|68131|5|Briefly described|p2 Fig.1|Paleoproterozoic|Paleoproterozoic||||||Metasediments and felsic volcanic rocks.|
20135|Willyama Supergroup|68158|6|Mentioned|p17|||Curnamona Province.|~1715 Ma -~1650 Ma.|||||
20135|Willyama Supergroup|68315|6|Mentioned|p764-766, 771-772|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Underwent LP-HT amphibolite- to granulite-grade metamorphism in the c.1610-1590 Ma Olarian Orogeny.||||||
20135|Willyama Supergroup|68731|6|Mentioned|p170 Fig 3.83|Proterozoic|Proterozoic|||||||
20135|Willyama Supergroup|69023|5|Briefly described|p13 Fig.4, p15, p72-73, p79-80, p145|Proterozoic|Proterozoic|Geochronology suggests there may be no rocks of this unit in Mount Painter Province. Equated with Radium Creek Metamorphics on stratigraphic, but not radiometric, grounds.||||||
20135|Willyama Supergroup|69213|5|Briefly described|p32-35|Paleoproterozoic|Paleoproterozoic||1720-1640 Ma||Includes Curnamona Group||Metasediments with lesser volcanic components. Migmatites range from stromatic migmatites to diatexite migmatite . Stromatic migmatite is intruded by foliated, syntectonic leucogranite sheets.|
20135|Willyama Supergroup|69255|6|Mentioned|p788|Paleoproterozoic|Paleoproterozoic||||||Metasedimentary rocks.|
20135|Willyama Supergroup|69562|6|Mentioned|p665, p674 Fig.6|||||||||
20135|Willyama Supergroup|69567|6|Mentioned|p277|||Broken Hill.|||||Includes tourmalinites (tourmaline metaquartzites).|
20135|Willyama Supergroup|69591|6|Mentioned|p107 Fig.2.102|||Appears in a diagram of the geodynamic setting of ~1725-1690 Ma eastern Australia.||||||
20135|Willyama Supergroup|69650|4|Described|p1, p2, p5-6, p15-16, p21-23, p27-29|Paleoproterozoic|Paleoproterozoic|See also p34-35, p38, p41, p45. Southern Curnamona Province. Probable crustal source of most of Ninnerie Supersuite. Appears as Upper and Lower Willyama Supergroup on p16,29,34,38,41,45.|1720-1640 Ma.||Includes Ethiudna Subgroup, Tommie Wattie Formation, Bimba and Peryhumuck Formations.|Intruded and overlain by Ninnerie Supersuite.||
20135|Willyama Supergroup|69654|6|Mentioned|p2, 6, 25|Paleoproterozoic|Paleoproterozoic|Southern Curnamona Province.||||||
20135|Willyama Supergroup|69982|5|Briefly described|p15, p17-19, p45, p69, p86, p220|Paleoproterozoic|Paleoproterozoic|Forms crystalline basement below the southern Cooper Basin. Brief thin section descriptions. Bedding dip angles in wells listed.|||||Includes schists and phyllite.|
20135|Willyama Supergroup|69999|5|Briefly described|p1, p4, p17, p21|Paleoproterozoic|Paleoproterozoic|Willis et al. (1983). Broken Hill and Euriowie Blocks. Preserves evidence of two major metamorphic events: a prograde field gradient at c.1600 Ma (Olarian Orogeny) and a retrograde field gradient at c.500 Ma (Delamerian Orogeny).|||||A metamorphosed sequence of pelitic to psammitic sedimentary rocks with intercalated mafic/felsic volcanic and plutonic rocks.|
20135|Willyama Supergroup|70000|5|Briefly described|p31, p33-34|Statherian|Statherian||||Includes Curnamona, Rantyga, Thackaringa, Broken Hill, Sundown and Paragon Groups.|||
20135|Willyama Supergroup|70014|5|Briefly described|Map legend||||||Includes Redan, Ednas, and Thorndale Composite, Gneisses; Clevedale Migmatite; Mulculca Formation; Thackaringa, Broken Hill, Sundown and Paragon Groups.||Undifferentiated: mostly metasediments and composite gneisses with lesser quartzo-feldspathic and amphibole/pyroxene rich (basic) gneisses.|
20135|Willyama Supergroup|70015|5|Briefly described|Map legend|Statherian|Statherian|Mineral deposits (if any) are shown.|||Includes Curnamona, Rantyga, Thackaringa, Broken Hill, Sundown and Paragon Groups; Thorndale Composite Gneiss; Silver City Suite.||Low to high grade metasedimentary rock, composite gneiss, quartzofeldspathic gneiss, calc-silicate, Zn-, Mn- and Fe-rich rock, foliated granite, pegmatite; amphibolite stratiform or discordant dykes containing plagioclase, amphibole and/or pyroxene.|
20135|Willyama Supergroup|70339|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||Mount Howden, Ethiudna Subgroups; Saltbush, Curnamona Groups; George Mine Formation.||Psammopelite; psammite; pelite; metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite- or haematite-bearing; local iron formation, sulphidic metasediments, carbonate rocks.|02-FEB-16
20135|Willyama Supergroup|70340|5|Briefly described|map legend|Paleoproterozoic|Paleoproterozoic||||||Psammopelite; psammite; pelite; metasediments characterised by calc-silicate minerals and alkali feldspar, magnetite- or haematite-bearing; local iron formation, sulphidic metasediments, carbonate rocks.|
20135|Willyama Supergroup|70383|6|Mentioned|p51|Statherian|Statherian|Mentioned as a possible source of zircons aged c.1670 +/- 24 Ma, extracted from the Sprigg Diamictite Member.||||||
20135|Willyama Supergroup|70405|4|Described|p1,p6,p7,p12 figure 4,p 15, p83, p 86|Mesoproterozoic|Paleoproterozoic|Previously termed Willyama Complex.|1700 Ma -1650 Ma||Includes Curnamona Group, Bimba Formation, Plumbago Formation, Raven Hill Subgroup, Mount Howden Subgroup, Paragon Group, Sundown Group, Broken Hill Group, Thackaringa Group|Intruded by Bimbowrie Suite|Amphibolite facies albitic, siliciclastic and minor calcareous metasediments; Gneisses and migmatites. Numerous mafic dykes.|
20135|Willyama Supergroup|70657|4|Described|p6-17, p21, p28, p32, p42-46, p50-51|Statherian|Statherian|See also p53-54, p58-59, p65, p67, p69, p72. Olary, Mulyungarie and Olary Domains, Curnamona Province. Total thickness unknown: neither top nor base observed; probably c.5km, multiplied by structural repetition. Associated igneous suites include Ninnerie Supersuite, Lady Louise Suite, Basso Suite (all in the Olary Domain); Mundi Mundi Granites, Cusin Creek Granite, Purnamoota Road leucogneiss, Hores Gneiss, Parnell Gneiss, Silver City Suite (all in the Broken Hill Domain). The Arunta terrane may be a source for some of the sediment. The bulk of the metasediments are enriched in HFSE, REE, U and Th up to the Cartwrights Creek Metasediments. Deformation, particularly Delamerian Orogeny, discussed in detail.|1719  - < 1642 +/- 5 Ma.||Includes Sundown, upper Saltbush, Paragon, Strathearn, Thackaringa, Rantyga, Curnamona, Broken Hill Groups.|||
20135|Willyama Supergroup|70658|5|Briefly described|p1-2, 5, 9, 11, 14-16, 32, 47|Paleoproterozoic|Paleoproterozoic|Curnamona Province.|1720-1640 Ma.||Rantyga, Thackaringa Groups.|||
20135|Willyama Supergroup|70659|6|Mentioned|p4|||||||||
20135|Willyama Supergroup|70829|6|Mentioned|p33|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Enhanced conductivity discussed.||||||
20135|Willyama Supergroup|70858|6|Mentioned|p14, 27 Fig.11H, p33-34|Paleoproterozoic|Paleoproterozoic|Curnamona Province. Similar Zr geochronology and Nd isotope ratios suggest a shared depositional system with Tarcoola Formation and Isa Supergroup, and the Wernecke Supergroup of Yukon.|||Sundown Group.|||
20135|Willyama Supergroup|70947|6|Mentioned|p960|Statherian|Statherian|Geological province: Curnamona Province.|ca. 1720-1650 Ma|||||
20135|Willyama Supergroup|71322|5|Briefly described|p38|||Hosts the Cu-Au Kalkaroo deposit.||||||
20135|Willyama Supergroup|71341|6|Mentioned|p179 fig 1|Palaeoproterozoic|Palaeoproterozoic||ca. 1720-1640 Ma|||||
20135|Willyama Supergroup|71799|5|Briefly described|p150 fig 2, p165|Statherian|Statherian|Curnamona Province.|ca 1700 Ma|||||
20135|Willyama Supergroup|71968|5|Briefly described|p1,3-4,6,13,18-19,28,41,45|Paleoproterozoic|Paleoproterozoic|Geological province: Curnamona province .Deformation-related metamorphic assemblages may have been developed during the high-grade Olarian Orogeny during 1620-1580 Ma (Binns, 1964; Hobbs et al., 1984; Clarke et al., 1987; Page and Laing, 1992); most of the assemblages are betwen 1600-1590 Ma (Page et al., 2005a) based on metamorphic zircon, rutile and monazite ages, and syn- to late-tectonic granites (see p7 for references). Barovich and Hand (2008) suggested the NAC was the likely sediment source for the lower Wiillyama Supergroup based on whole rock Sm-Nd data.|||Includes Paragon Group, Sundown Group.|||06-DEC-19
20135|Willyama Supergroup|72004|4|Described|p73,83-90|Statherian|Statherian|Geological province: Olary Block. Broken Hill region. Age from Page et al., 2005. Underwent high-grade metamorphism at c. 1600 Ma (Grew et al., 2012, Page et al., 2005). Contains sodic rocks of possibly evaportic origin and bimodal volcanism, indicative of continental rift deposition.|c. 1700-1685 Ma|||Lithologically similar to prismatine-bearing granulites in the Windmill Islands, Wilkes Land and granulite-facies paragneisses, Larsemann Hills. Underlain by Thackaringa Group.|Metaevaporites, tourmaline-quartz rocks, sodic gneisses and apatitic iron formation|
20135|Willyama Supergroup|72435|6|Mentioned|p715|Palaeoproterozoic|Palaeoproterozoic|Broken Hill.||||||
20135|Willyama Supergroup|72454|5|Briefly described|p1, p2 Fig.2, p7, p12, p20, p25|Mesoproterozoic|Mesoproterozoic|Olary Domain. See also p34, p39, p42 Fig.26, p44, p47, p48 Fig.33, p49, p54. Volcanics were extruded over the eroded surface of the Willyama Supergroup. Bimbowrie Suite granites were largely derived from melting of Willyama Supergroup sediments.|c. 1600 to 1570 Ma.||Includes Paragon Group, Sundown Group, Broken Hill Group, Thackaringa Group, Thorndale Composite Gneiss, Strathearn Group, Curnamona Group.||Includes pelitic and psammopelitic metasediments.|09-SEP-20
20135|Willyama Supergroup|72461|5|Briefly described|p4-5, p13|||Of the  Curnamona Craton. Oldest rocks in NSW.|1700 Ma||Includes the Thackaringa Group, Broken Hill Group, Sundown Group and the Paragon Group.|||
20135|Willyama Supergroup|73021|5|Briefly described|p224-225|||Broken Hill area, SE Curnamona Craton. ~7 km thick. Intracontinental rift setting. Large areas of stratigraphy were inverted by the Olarian Orogeny.|~1710-1704 Ma (middle) to ~1642 Ma (top).||Thackaringa, Broken Hill Groups; Basso Suite.||A wide range of metamorphosed deformed lithologies including pelite, psammopelite, psammite, quartzofeldspathic and mafic rocks and hydrothermal sediments.|
20135|Willyama Supergroup|73030|5|Briefly described|p2147-2153|Statherian|Statherian|Curnamona Province. Oldest exposed rocks in the province. Deposited in a rift basin. Extensively altered by sodic metasomatism, potentially indicative of an evaporitic sedimentary component.|ca. 1710 to 1640 Ma|||||
20135|Willyama Supergroup|73092|6|Mentioned|p5|||Curnamona Province. Deposition was synchronous with that of the metasedimentary protoliths to the Barossa Complex and onset of the Kimban Orogeny in the Gawler Craton.||||||
20135|Willyama Supergroup|73093|5|Briefly described|map legend|Palaeoproterozoic|Paleoproterozoic|Undifferentiated.|||||Schist, gneiss, quartzite, migmatite.|12-DEC-21
20135|Willyama Supergroup|73118|6|Mentioned|p31|||||||||
20135|Willyama Supergroup|73129|6|Mentioned|p43|late Palaeoproterozoic|late Palaeoproterozoic|Curnamona Province|||||metasediments|
20135|Willyama Supergroup|73155|6|Mentioned|P286|||Curnamona Province.||||||
20135|Willyama Supergroup|73162|6|Mentioned|p449, Fig.1|Statherian|Statherian||1720-1640 Ma|||||
20135|Willyama Supergroup|73188|6|Mentioned|p352|Statherian|Statherian|Curnamona Province. Coeval with sedimentary protoliths of the high-grade metamophic basement rocks of the Mount Lofty Ranges (Conor and Preiss, 2008).|1720-1640 Ma|||||
20135|Willyama Supergroup|73235|6|Mentioned|p52|Statherian|Statherian||c. 1720-1650 Ma|||||
20135|Willyama Supergroup|73243|4|Described|p51, p52 Fig.1 p54, p57, p59|Statherian|Statherian|Broken Hill Domain, Broken Hill block-Euriowie block. ~7km-thick sequence. Amphibolite sills and dykes typical of rift tholeiites were emplaced before folding and metamorphism, are confined to the Broken Hill Group and stratigraphically lower groups. Zircon U-Pb dates from amphibolites range from 1674 +/- 8 Ma to 1691 +/- 9 Ma (Gibson and Nutman, 2004), and metamorphic grades range from lower amphibolite to hornblende granulite, produced by the Olarian Orogeny ca 1600 Ma. Amphibolite is used in text to refer to all highly metamorphosed pre-1600 Ma mafic rocks including hornblende granulites and pyroxene granulites. Some amphibolites have very high iron oxide values. Post-metamorphic intrusions include mafic to ultramafic dykes and plugs, minor granite bodies.|1691 +/- 9 Ma, 1674 +/- 8 Ma zircon U-Pb||Clevedale Migmatite, Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group||Sequence of metasedimentary rocks with minor metavolcanic units, highly metamorphosed and deformed. Intruded during deposition by abundant amphibolite (meta-dolerite) sills and dykes as well as granite bodies, now granite gneisses.|17-AUG-22
20135|Willyama Supergroup|73244|6|Mentioned|p86||||||||Metasedimentary/igneous[?].|
20135|Willyama Supergroup|73251|6|Mentioned|p36|Statherian|Statherian|Curnamona Province.|c. 1730-1640 Ma|||||
20135|Willyama Supergroup|73308|5|Briefly described|p605-608, 623||||1710-1640 Ma.||Paragon, Broken Hill, Sundown, Rantyga, Thackaringa Groups; Thorndale Composite Gneiss, Clevedale Migmatite.||Metasediments and minor volcanics. Includes mainly metasediments, with granite gneiss and garnet-biotite-rich quartzo-feldspathic gneiss, and sills and dykes of amphibolite and basic granulite.|
20135|Willyama Supergroup|73429|5|Briefly described|p105, p106 Fig.2, p107-108, p114|Statherian|Statherian|Curnamona Province. Deposited in an epi-continental rift basin. Deformed between c. 1610 Ma and c. 1590 Ma. Informally the supergroup is commonly subdivided into lower and upper packages separated by a regionally extensive redox boundary associated with stratiform Cu-Au mineralisation.|c. 1702-1640 Ma||lower Willyama Supergroup, upper Willyama Supergroup||Includes metasediments.|
20135|Willyama Supergroup|73479|6|Mentioned|p155, p156 Fig.2|Precambrian|Precambrian|Basement to Warburton Basin.|||||Meta-sedimentary.|
20135|Willyama Supergroup|73482|5|Briefly described|p419-420, p422 Fig.3, p423, p431|Paleoproterozoic|Paleoproterozoic|Intruded by granites, tholeiitic dolerite/gabbro sills and dykes from 1710 to 1680 Ma. Peak metamorphic grade at about 1600 Ma (SHRIMP U-Pb metamoprhic zircons; Page et al., 2005; Stevens et al., 2008). Ranges from chlorite grade in Euriowie Block, to two-pyroxene granulite grade in the southern Broken Hill Block. In major fold structures the upper stratigraphic units are at lower metamorphic grades.|1720-1640 Ma||Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group||Sedimentary-volcanic sequence, metamorphosed.|
20135|Willyama Supergroup|73512|5|Briefly described|p1-3, p7-8|Statherian|Statherian|Curnamona Province, Broken Hill Block. Reflects granulite facies Olarian metamorphism at ca 1600 Ma. Deposited in an intracratonic rift setting. [Informal lower and upper subdivisions are used on p3 and p7].|||Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Clevedale Migmatite, Thorndale Composite Gneiss|||
20135|Willyama Supergroup|73516|5|Briefly described|p2, p6|Statherian|Statherian|Curnamona Province. Commonly subdivided into a lower and upper supergroup. Lower-Middle Willyama Supergroup shown p3 Fig.1.|~1720-1640 Ma|||Intruded by Ninnerie Supersuite|Meta-sedimentary and meta-igneous units.|
20135|Willyama Supergroup|73524|5|Briefly described|p1-4, p19 Fig.17, p20-21|Statherian|Statherian|Curnamona Province. Total thickness estimates range from 8-15 km. Paleo-Mesoproterozoic metamorphic field gradient from greenschist-facies in the NW to granulite-facies in the SE. Early (c.1630 Ma) metamorphism attributed to elevated levels of radiogenic heat production.|1720-1640 Ma||lower Willyama Supergroup|Intruded by Ninnerie Supersuite|Dominated by metasedimentary rocks, including metamorphosed clastic, volcaniclastic, volcanic and intrusive lithologies.|
20135|Willyama Supergroup|73575|5|Briefly described|p825, p828 Fig.2, p833, p835|Paleoproterozoic|Paleoproterozoic||||Thorndale Composite Gneiss, Thackaringa Group, Broken Hill Group, Sundown Group, Paragon Group, Rantyga Group|||
20135|Willyama Supergroup|73600|6|Mentioned|p192|||Broken Hill Provence.||||||
20135|Willyama Supergroup|74367|6|Mentioned|p23|||Curnamona Province.||||||
20146|Wilmatha Granite|22519|6|Mentioned|p6|||||||||
20146|Wilmatha Granite|22831|4|Described|p 48|Early Devonian|Late Silurian|||||||
20146|Wilmatha Granite|29986|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
20146|Wilmatha Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
20146|Wilmatha Granite|32087|4|Described|p15|||||||||
20146|Wilmatha Granite|33732|6|Mentioned|p114|||||||||
20146|Wilmatha Granite|40328|4|Described|p212|||||||||
20146|Wilmatha Granite|40365|6|Mentioned|p243|||||||||
20146|Wilmatha Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
20146|Wilmatha Granite|43441|5|Briefly described|28|Early Devonian|Early Devonian|Age assumed||||||08-JAN-10
20146|Wilmatha Granite|43500|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
20146|Wilmatha Granite|43510|14|Not recorded|p73,75||Late Silurian|NW of Murda Syncline||||||
20146|Wilmatha Granite|44160|5|Briefly described|Map Legend||Lochkovian|||||||08-JAN-10
20146|Wilmatha Granite|48958|6|Mentioned|Plate 1|||||||||
20146|Wilmatha Granite|67416|5|Briefly described|p84-87, p91|||Mineral Hill district. Temporally and chemically related to volcanics in the Canbelego-Mineral Hill Volcanic Belt. Associated with minor Cu-Au-Bi mineralisation. Age also shown as 421 Ma.|422 +/- 4 Ma (SHRIMP: Spandler, 1998).||||Fractionated to relatively evolved composition. Has interconnected miarolitic cavities.|
20146|Wilmatha Granite|67806|6|Mentioned|p110|||There is minor Cu-Au-Bi mineralisation around this unit.||||||
20146|Wilmatha Granite|70751|6|Mentioned|p8, p12, p28|Silurian|Silurian|Located immediately east of Mineral Hill.|421.1 +/- 3.4 Ma (SHRIMP, Spandler, 1998)|||||
20146|Wilmatha Granite|70876|5|Briefly described|p76|Devonian|Silurian|Lachlan Orogen.|421.1 +/- 3.4 Ma (Spandler, 1998)|||||
20146|Wilmatha Granite|71039|5|Briefly described|p26|Early Devonian|Early Devonian|I-type.||||Intrudes the Mineral Hill Volcanics.||
20146|Wilmatha Granite|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||I-type. Fine- to medium-grained weakly porphyritic pale pink leucogranite commonly with miarolitic cavities and micrographic groundmass.|
20146|Wilmatha Granite|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||May intrude Mineral Hill Volcanics, Majuba Volcanics?||
20184|Wilton Formation|22578|6|Mentioned|Fig.3 p393|||See also Fig.8 p399||||||
20184|Wilton Formation|22969|6|Mentioned|p 24|||||||||
20184|Wilton Formation|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
20184|Wilton Formation|24471|4|Described|p29 Fig.2|Late Permian|Late Permian|Overlies Woonona Coal. Overlain by Appin Formation. Thickness: ~250 m. Of Illawarra Coal Measures. Possibly Stratigraphically equivalent to part of Four Mile Creek Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
20184|Wilton Formation|29900|5|Briefly described|p169|||||||||
20184|Wilton Formation|29901|4|Described|Table 1|||||||||
20184|Wilton Formation|29944|6|Mentioned|FIg.18|||||||||
20184|Wilton Formation|30006|4|Described|p12|||||||||
20184|Wilton Formation|31128|6|Mentioned|Table 1|||||||||
20184|Wilton Formation|31887|6|Mentioned|p5|||||||||
20184|Wilton Formation|32849|6|Mentioned|Table 1|||Permian||||||
20184|Wilton Formation|34060|6|Mentioned|p24|||Table. Permian||||||
20184|Wilton Formation|34205|6|Mentioned|p15|||||||||
20184|Wilton Formation|34569|6|Mentioned|p9|||Permian||||||
20184|Wilton Formation|34605|4|Described|p374|||Fig.5.29||||||
20184|Wilton Formation|36042|6|Mentioned|Fig.19|||||||||
20184|Wilton Formation|36220|4|Described|p51|||See also Table 1.||||||
20184|Wilton Formation|37089|6|Mentioned|p208|||||||||
20184|Wilton Formation|37090|6|Mentioned|p219|||||||||
20184|Wilton Formation|39287|6|Mentioned|p33|||See also Fig.2.15||||||
20184|Wilton Formation|39308|5|Briefly described|p514|||||||||
20184|Wilton Formation|39309|5|Briefly described|p124|||||||||
20184|Wilton Formation|39661|6|Mentioned|Fig.1|||||||||
20184|Wilton Formation|40256|6|Mentioned|p306|||||||||
20184|Wilton Formation|40744|6|Mentioned|Table 1|||||||||
20184|Wilton Formation|42787|5|Briefly described|p131|||||||||
20184|Wilton Formation|42896|3|Fully described|p19|||Of Sydney Subgroup.||||||12-MAR-09
20184|Wilton Formation|42925|5|Briefly described|Table 18||Late Permian|||||||
20184|Wilton Formation|45090|5|Briefly described|p63|||Lithology, relationships, correlation & age||||||
20184|Wilton Formation|60281|5|Briefly described|p63|||Disconformably overlies the eroded Erins Vale Formation.  Geological Province: Sydney Basin.||||||17-MAR-05
20184|Wilton Formation|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
20184|Wilton Formation|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
20184|Wilton Formation|61610|4|Described|p252, p252 Fig. 2, p254-255, p257-259|Late Permian|Late Permian|Of Sydney Subgroup. Overlies Shoalhaven Group. Geological Province: Sydney Basin. Fining upward sequence from conglomerates and sandstones to siltstone, and finally coals.||||||07-FEB-11
20184|Wilton Formation|63832|6|Mentioned|p131 fig 2|||Of Sydney Basin.||Unit in Illawarra Coal Measures.||||
20184|Wilton Formation|64631|6|Mentioned|p44 Fig.2.|Capitanian|Wordian|SE Sydney Basin. Biostratigraphic age control at base and top.||Unit in Illawarra Coal Measures.||||
20184|Wilton Formation|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Woonona Coal. Is overlain by Tongarra Coal.||
20184|Wilton Formation|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
20184|Wilton Formation|73421|5|Briefly described|p3, p5, p16, p18-19|Wuchiapingian|Capitanian|Sydney Basin, southern. Contains in lower part the Woonona Tuff dated to 258.89+/-0.89 Ma by Hyusken (2014), same age is also shown with the Woonona Coal p16.|258.89+/-0.89 Ma CA-TIMS|Sydney Subgroup|Woonona Coal|Overlies Erins Vale Formation, underlies Bargo Claystone, Tongarra Coal|Contains siltstone, sandstone and claystone/shale in upper part with dropstones. Conglomerate in lower part.|
20184|Wilton Formation|73625|6|Mentioned|p2, 25|Permian|Permian|Southern coalfield, Sydney Basin.||Illawarra Coal Measures.||Overlies Marangaroo Conglomerate. Is overlain by Bargo Claystone. Time-equivalent to Black Alley Shale.||
20192|Winburn Tuff|22590|6|Mentioned|P753|||||||||
20192|Winburn Tuff|23214|6|Mentioned|p193|||Now included in Merrions Formation.||||||
20192|Winburn Tuff|30099|6|Mentioned|Fig.2|||||||||
20192|Winburn Tuff|31161|5|Briefly described|PA4|||||||||
20192|Winburn Tuff|32619|6|Mentioned|p460|||Fauna||||||
20192|Winburn Tuff|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
20192|Winburn Tuff|32672|6|Mentioned|p673|||||||||
20192|Winburn Tuff|33282|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
20192|Winburn Tuff|33285|5|Briefly described|p20|||||||||
20192|Winburn Tuff|33732|6|Mentioned|p117|||Table II||||||
20192|Winburn Tuff|34059|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
20192|Winburn Tuff|34403|5|Briefly described|p131|||||||||
20192|Winburn Tuff|34404|6|Mentioned|Fig.3.5b|||||||||
20192|Winburn Tuff|34405|6|Mentioned|Fig.3.9|||||||||
20192|Winburn Tuff|34406|6|Mentioned|p224|||||||||
20192|Winburn Tuff|35128|6|Mentioned|p361|||Appears on figure||||||
20192|Winburn Tuff|35246|6|Mentioned|Fig.7|||||||||
20192|Winburn Tuff|37806|6|Mentioned|p47|||||||||
20192|Winburn Tuff|39214|6|Mentioned|p23|||||||||
20192|Winburn Tuff|39331|6|Mentioned|Fig.7-1|||||||||
20192|Winburn Tuff|41207|5|Briefly described|Table 1|||||||||
20192|Winburn Tuff|42051|6|Mentioned|p137|||||||||
20192|Winburn Tuff|42712|4|Described|8; Table 1 p13.|Middle Devonian|Middle Devonian|Overlies Limekilns Group conformably. Unconformable beneath Lambie Group.||||||
20192|Winburn Tuff|42726|5|Briefly described|map legend|Early Devonian||||||||
20192|Winburn Tuff|43263|6|Mentioned|Map Legend|Middle Devonian|Early Devonian|||||||
20192|Winburn Tuff|43344|14|Not recorded|p139,150,155||Middle Devonian|||||||
20192|Winburn Tuff|43461|14|Not recorded|Table p621||Givetian|||||||
20192|Winburn Tuff|43515|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|(Provisional Edition)||||||
20192|Winburn Tuff|43516|14|Not recorded|Map Legend|Middle Devonian|Early Devonian|||||||
20192|Winburn Tuff|43517|2|Defined|p112,141-161,||Givetian|Section in Cheshire Creek. Map Plate XII||||||
20214|Windellama Limestone Member|22678|3|Fully described|p711-13,715,717,724|Pragian|Lochkovian|||||||
20214|Windellama Limestone Member|22857|5|Briefly described|ERRATA sheet for p482|Middle Devonian|Middle Devonian|Supersedes the Windellama Limestone? Of the Tangerang Formation.||||||16-JUN-08
20214|Windellama Limestone Member|23522|5|Briefly described|p251|||Of Tangerong Formation.||||||
20214|Windellama Limestone Member|39568|1|Redefined|p82|Early Devonian|Early Devonian|||||||
20214|Windellama Limestone Member|42210|6|Mentioned|Fig.1 p273|||||||||16-JUN-08
20214|Windellama Limestone Member|68592|2|Defined|p231, p742, p840, p1079, p1083, p1093-7|Lochkovian|Lochkovian|See also p1905-7. Originally Windellama Limestone (Pickett and Huleatt, 1971), after the village of Windellama; included in the Fernleigh Group. Redefined by Jones, Carr et al. (1984) as an interbedded Member of Tangerang Formation. Includes several isolated limestone pods, some of which may be allochthonous. Forms low rises or ridges. Type section described. 152 - over 283m thick. Geochemistry and geophysical properties briefly described. Quarried from several sites at Wombeyan from 1960s to 1990s. A mid Lochkovian delta Zone conodont age. Diverse fossil fauna listed and described. See [shortened?] Windellama Limestone.||Tangerang Formation.||Possible correlation with the Sawtooth Ridge Limestone.|Very fossiliferous, fragmentary stromatoporoids and algae with a matrix of dolomite rhombs; overlain by medium-bedded and less dolomitic limestone; highest beds are dark grey to black, massive, and comparatively poorly fossiliferous.|
20214|Windellama Limestone Member|69159|5|Briefly described|Map legend|Devonian|Devonian|||Unit in Tangerang Formation.|||Pale grey, well-bedded fossiliferous limestone; fossil-rich base passes up into relatively fossil-poor, dark grey, more massive limestone.|
20214|Windellama Limestone Member|70661|6|Mentioned|p55|||||||||
20214|Windellama Limestone Member|71069|6|Mentioned|p143|||||||||
20214|Windellama Limestone Member|71656|4|Described|p11, p38, p39|Lochkovian|Pridoli|See also p13 Fig. 2. Fossil evidence include conodonts, brachiopods, gastropods and other faunal fragments. Base likely to be markedly diachronus. Note: Shown in Fig.2 as Pragian.||Tangerang Formation, Bindook Group|||Fossiliferous limestone.|
20214|Windellama Limestone Member|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Tangerang Formation.|||Pale grey, well-bedded fossiliferous limestone; fossil-rich base passes up into relatively fossil-poor, dark grey, more massive limestone.|
20214|Windellama Limestone Member|71700|2|Defined|vi, p24, p57, p74, CD|Lochkovian|Pridoli|Named for the village of Windellama. Pickett and Huleatt (1971) designated a type section in Limestone Creek where it extends from GR 762767 6123015 to 762645 6123370. The Windellama Limestone was defined as a formation by Felton and Huleatt (1977).. Jones et al (1984) demoted the unit to a member of the Tangerang Formation. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geochemistry, geophysical characteristics, fossils, distinguishing features and economic geology are discussed. A total thickness of 152m is interpreted in the type section, however Jones et al (1984) estimated a total thickness of 283m. Age is derived from fossil assemblage.||Tangerang Formation||Faulted against the Abercrombie Formation and the Cardinal View Formation.|Fossiliferous limestone at the base changing to massive- or medium-bedded limestone at higher levels that is also less dolomitic.|
20217|Windermere Granite|34544|6|Mentioned|p197|||||||||
20235|Windy Creek Diorite|40328|4|Described|p212|||||||||
20235|Windy Creek Diorite|44092|5|Briefly described|map legend|Late Ordovician|Late Ordovician|Og4||||||
20235|Windy Creek Diorite|46574|5|Briefly described|Map Legend|Silurian|Silurian|Of the Kosciusko Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
20235|Windy Creek Diorite|60078|6|Mentioned|Map Legend|Ordovician|Ordovician|||||||
20235|Windy Creek Diorite|60085|5|Briefly described|Map legend|Early Devonian|Early Devonian|||||||
20250|Winnambool Formation|2967|5|Briefly described|p14, p15 Fig.2.2, p24, 42|Miocene|Miocene|Western Murray Basin.||Murray Group.||Overlies Geera Clay and Duddo Limestone (and grades into the latter). Is separated from the overlying Bookpurnong beds by the Mologa Surface.||
20250|Winnambool Formation|10010|5|Briefly described|p12 Fig. 3|Middle Miocene|Late Oligocene|Of the Murray Group. Geological Province: Murray Basin.||||||13-AUG-07
20250|Winnambool Formation|22587|6|Mentioned|p79 Fig.7|Middle Miocene|Late Oligocene|||||||
20250|Winnambool Formation|22773|5|Briefly described|p351,Fig24.8p352|Miocene||||||||
20250|Winnambool Formation|22799|2|Defined|p33|Early Miocene|Late Oligocene|||||||
20250|Winnambool Formation|22857|5|Briefly described|p351, p352 Fig. 24.8|Miocene|Oligocene|Of the Murray Group. Geological Province: Murray Basin. See also p353 Fig. 24.9.||||||
20250|Winnambool Formation|22887|5|Briefly described|Fig.6 p13|Middle Miocene||||||||
20250|Winnambool Formation|22893|5|Briefly described|fig4 p9|Miocene|Miocene|||||||
20250|Winnambool Formation|23179|6|Mentioned|Fig.2|Middle Miocene|Late Oligocene|Murray Supergroup||||||
20250|Winnambool Formation|23226|6|Mentioned|p889,890,891,897|||Of Murray Supergroup.||||||
20250|Winnambool Formation|23884|5|Briefly described|p153, p155 Fig. 13.2|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.||||||21-SEP-09
20250|Winnambool Formation|23909|6|Mentioned|p298|||||||||
20250|Winnambool Formation|23921|5|Briefly described|p1109|Middle Miocene|Middle Miocene|Geological Province: Murray Basin.||||||
20250|Winnambool Formation|24551|6|Mentioned|p322 Fig 10.29, p731 Table 17.1|||Of the Murray Group. Max. Thickness: 130m.||||||
20250|Winnambool Formation|24563|5|Briefly described|p485|||Included in the Murray Supergroup by Lukasik and James (1998).  However, Murray Supergroup now abandoned and Murray Group reinstated - Winnambool Formation not included.  Geological Province: Murray Basin.||||||
20250|Winnambool Formation|29591|6|Mentioned|Table 20|||||||||
20250|Winnambool Formation|29898|6|Mentioned|p216|||||||||
20250|Winnambool Formation|30581|6|Mentioned|Map legend|Tertiary|Tertiary|||||||
20250|Winnambool Formation|30934|6|Mentioned|Map legend|Miocene|Miocene|||||||
20250|Winnambool Formation|30935|6|Mentioned|Map legend|Tertiary|Tertiary|Subsurface||||||
20250|Winnambool Formation|30936|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20250|Winnambool Formation|31741|6|Mentioned|p6|||||||||
20250|Winnambool Formation|31743|6|Mentioned|p8|||||||||
20250|Winnambool Formation|31746|4|Described|p196|||||||||
20250|Winnambool Formation|31747|6|Mentioned|Map legend|Miocene|Oligocene|Oligocene - Miocene||||||
20250|Winnambool Formation|34735|4|Described|p33|||Also mentioned on P32.||||||
20250|Winnambool Formation|34813|6|Mentioned|p62|||||||||
20250|Winnambool Formation|35285|5|Briefly described|p413|||||||||
20250|Winnambool Formation|37809|6|Mentioned|p7|||See also P7.||||||
20250|Winnambool Formation|39329|6|Mentioned|Fig.1|||||||||
20250|Winnambool Formation|39929|6|Mentioned|p268|||||||||
20250|Winnambool Formation|40820|6|Mentioned|Fig.4|||||||||
20250|Winnambool Formation|41511|6|Mentioned|p20|||||||||
20250|Winnambool Formation|41868|5|Briefly described|p551|||||||||
20250|Winnambool Formation|42125|5|Briefly described|p136|||See also Fig.5||||||
20250|Winnambool Formation|42126|6|Mentioned|p151|||||||||
20250|Winnambool Formation|42130|6|Mentioned|Fig.3 P265|||||||||
20250|Winnambool Formation|42133|6|Mentioned|p301|||||||||
20250|Winnambool Formation|42134|6|Mentioned|Fig.3 P335|||||||||
20250|Winnambool Formation|42137|4|Described|p371|||See also Table 2||||||
20250|Winnambool Formation|42138|6|Mentioned|p388|||||||||
20250|Winnambool Formation|42827|4|Described|p270|||||||||
20250|Winnambool Formation|42881|4|Described|Fig.3, P84|||||||||
20250|Winnambool Formation|42966|2|Defined|p146|Middle Miocene|Late Oligocene|Of the  Murray Group.||||||29-JUL-08
20250|Winnambool Formation|43655|5|Briefly described|p40-846|||||||||
20250|Winnambool Formation|43780|6|Mentioned|p5|Middle Miocene|Late Oligocene|||||||
20250|Winnambool Formation|43790|5|Briefly described|p383|||||||||
20250|Winnambool Formation|43791|5|Briefly described|p371|||||||||
20250|Winnambool Formation|43804|6|Mentioned|Fig.2,p49|||||||||
20250|Winnambool Formation|44133|5|Briefly described|p159|Middle Miocene|Early Miocene|Of the Murray Group. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|44191|5|Briefly described|Map Legend|Middle Miocene|Early Oligocene|||||||
20250|Winnambool Formation|49038|4|Described|Table 2|||||||||
20250|Winnambool Formation|49040|6|Mentioned|p11|||||||||
20250|Winnambool Formation|50154|5|Briefly described|p135|||Of the Murray Group.||||||
20250|Winnambool Formation|60538|5|Briefly described|p480 Fig. 19|||Geological Province: Murray Basin.||||||
20250|Winnambool Formation|61155|5|Briefly described|p4, p18|Middle Miocene||Of the Murray Group. Platform/lagoonal deposits - calcareous clays. Interfingers with and grades into Geera Clay; interfingers with Duddo Limestone. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|61314|5|Briefly described|p129|||Shallow water equivalent of Duddo Limestone in the eastern part of the basin. Geological Province: Murray Basin.||||||
20250|Winnambool Formation|63066|5|Briefly described|p485|||Revised stratigraphy of Lukasik and James (1999) incorporates this unit, the Ettrick Formation and Geera Clay into their new Murray Supergroup.  These were not formerly included in the definition of the Murray Group.||||||08-FEB-07
20250|Winnambool Formation|63460|5|Briefly described|p838, p839 Fig. 2b|||Of Lawrence and Abele (1976). Geological Province: Murray Basin.||||||06-FEB-09
20250|Winnambool Formation|63777|6|Mentioned|p1104 Fig. 1, p1105|||Geological Province: Murray Basin.||||||18-MAR-09
20250|Winnambool Formation|63887|5|Briefly described|p20, p21 Fig. 1|Middle Miocene|Late Oligocene|Of Murray Group. Marl.||||||
20250|Winnambool Formation|64237|5|Briefly described|p17, p19|Middle Miocene|Early Miocene|Of Lawrence (1966). Retained as a formal unit through the Lawrence (1975) and Lawrence and Abele(1988) revisions where it overlay the Geera Clay.  Became constituent in Murray Supergroup (Lukasic and James 1998), then retained in reinstateed Murray Group.||||||03-FEB-09
20250|Winnambool Formation|64823|5|Briefly described|p1011|Cenozoic|Cenozoic|Overlies Renmark Group. Terrestrial sands and gravels  Geological province: Murray Basin.||||||
20250|Winnambool Formation|65552|5|Briefly described|p5 Fig. 3, p6|Middle Miocene|Early Oligocene|Also spelt Winambool Formation in text. Murray Basin unit. Deposited contemporaneously with other Murray Basin units including Murray Group to the west and Geera Clay and Olney Formation to the east. Unconformably underlies Bookpurnong beds.||||||
20250|Winnambool Formation|67462|5|Briefly described|Map legend.|Miocene|Miocene|Murray Basin.||Unit in Murray Group.||||
20250|Winnambool Formation|68140|6|Mentioned|p1700-1701|Neogene|Paleogene|Middle Tertiary age.||||||09-FEB-18
20250|Winnambool Formation|68189|5|Briefly described|p27 Tb.3.2, p29|Miocene|Miocene|Maximum flooding surface.||Of the Murray Group.||Underlain by the Olney Formation. Overlain by the Parilla Sand.||
20250|Winnambool Formation|68715|5|Briefly described|p31 Fig.5|Burdigalian|Burdigalian|Murray Basin.||Of the Murray Group.||||
20250|Winnambool Formation|68716|6|Mentioned|p39 Fig.3|||||||Overlain by the Pata Formation. Underlain by the Glenforslan Formation.||
20250|Winnambool Formation|70718|5|Briefly described|p24-p25, p103|Middle Miocene|Late Oligocene|Murray Basin. Deposited in a lagoonal environment.||Of Murray Group.|||Marly limestone with thin interbeds of grey skeletal calcsiltite and calcarenite.|30-MAY-19
20250|Winnambool Formation|70961|14|Not recorded|p136|||Geological section.||||||
20250|Winnambool Formation|71593|5|Briefly described|p52, p54|Miocene|Oligocene|Murray Basin.||Murray Group||Interfingered with the Geera Clay, Olney Formation and the Calivil Formation.|Muddy shallow marine marl.|
20250|Winnambool Formation|72445|5|Briefly described|App.1, App.2; App.6 p2; App.7 p7 Fig.4.|Miocene|Late Oligocene|Shown in App 7 Fig 4 (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 12,16.||Murray Group||Overlain gradationally by Geera Clay. Overlies Renmark Group (sharp contact). Shown as unconformably underlying Bookpurnong beds.|Includes glauconitic marl and mud; glauconitic marl with limestone nodules or beds. marl, mud and limestone.|
20250|Winnambool Formation|73118|5|Briefly described|p53, 64, 82|Miocene|Oligocene|Glenelg Zone, Western Victoria. Drill core summary log. Abundant well-preserved and diverse faunas. Restricted-marine and lagoonal environments. 110m thick; mainly <50m.||Murray Group.||Overlies Olney Formation. Is overlain by Loxton-Parilla Sands.|Poorly consolidated, grey to green, glauconitic, highly fossiliferous calcareous clay (marl); intercalated skeletal calc-siltite, calcarenite, and dense micritic limestone.|
20250|Winnambool Formation|73228|4|Described|p50-51, p55-57, p60|Middle Miocene|Late Early Oligocene|Murray Basin. Shallow-water restricted marine and lagoonal facies. Mostly deposited adjacent to an estuarine environment due to the abundance of marine dinoflagellate cysts and freshwater algae.||Murray Group|||Grey to light green fossiliferous marl, glauconitic marly limestone and marly clay.|
20250|Winnambool Formation|73229|5|Briefly described|p66-67, p70|Middle Miocene|Mid Oligocene|Murray Basin. [Analysed using pXRF; see article]. Shallow water, restricted marine and lagoonal.||Murray Group|||Includes marl, fossiliferous; glauconitic marly limestone; marly clay.|
20268|Winton Formation|12597|5|Briefly described|p492 Tb.1, p500, p501|Cenomanian|Cenomanian|Eromanga Basin. 400-700m, locally up to 1200m, thick.||||Overlies Mackunda Formation.|Basal paralic-nonmarine transition zone, overlain by non-marine sequence of fine- to medium-grained labile sandstone, siltstone, mudstone and lenticular coal seams.|
20268|Winton Formation|13497|5|Briefly described|p13, p115, p115 fig 6.33|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposited in a high-sinuosity fluvial environment. See also p144, p144 fig 9.2, p146, p148-p154, .||||Overlies the Mackunda Formation and the Oodnadatta Formation. Unconformably overlain by the Mount Howie Sandstone and the Eyre Formation.|Sandstone, siltstone, shale and coal.|
20268|Winton Formation|13516|6|Mentioned|p167 fig 10, p169 fig 11, p171 fig 12|Late Cretaceous|Late Cretaceous|In Eromanga Basin.||||||
20268|Winton Formation|22464|6|Mentioned|p9||Late Cretaceous|Also p8. In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22587|5|Briefly described|p71|Cenomanian|Albian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|22773|6|Mentioned|p338|||||||||
20268|Winton Formation|22839|6|Mentioned|P33|||||||||
20268|Winton Formation|22857|4|Described|p296-7 Tb 22.1, p326, p552 Tb A1.13|Cenomainian|Cenomainian|Of the Rolling Downs Group. Interbedded mudstone and lithic and feldspathic arenite. Max. thickness: 400m in NSW. Geological Province: Eromanga Basin. See also p312-3 Fig. 22.6.||||||
20268|Winton Formation|22862|6|Mentioned|p327||Cenomanian|||||||
20268|Winton Formation|22865|4|Described|p314,Table22.1p296-7|Cenomanian|Cenomanian|||||||
20268|Winton Formation|22883|5|Briefly described|P31, Fig2||Late Cretaceous|Underlying unit is Mackunda Formation.||||||19-DEC-06
20268|Winton Formation|22912|6|Mentioned|34|||Geological province: Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23054|6|Mentioned|Fig5p22|||||||||
20268|Winton Formation|23056|6|Mentioned|9|||Geol province Eromanga Basin. Parent Rolling Downs Group||||||
20268|Winton Formation|23154|5|Briefly described|Map Legend|Late Cretaceous|Late Cretaceous|Geological Province - Eromanga Basin. Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|23155|4|Described|p33|Late Cretaceous|Early Cretaceous|Uppermost Eromanga Basin unit known on STRZELECKI, and is disconformably overlain by Tertiary Eyre Formation.||||||19-DEC-06
20268|Winton Formation|23375|5|Briefly described|Fig2 p265||Cenomanian|In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|23425|5|Briefly described|Plate 10.2|||Eromanga Basin Province.||||||
20268|Winton Formation|23818|5|Briefly described|p141 Fig.65, p144 Fig.66|Cenomanian|Cenomanian|Geological Province: Cooper Basin. Of the Manuka Sub-Group. Max. thickness: >2000 ft.||||||18-APR-05
20268|Winton Formation|23830|5|Briefly described|Fig. 3a|Cretaceous|Cretaceous|Geological Province: Boorthanna Trough, eastern Arckaringa Basin.||||||24-JAN-06
20268|Winton Formation|23883|5|Briefly described|p129 Fig. 11.2|Cretaceous|Cretaceous|Of Rolling Downs Group.  Geological Province: Great Australian Superbasin.||||||
20268|Winton Formation|23911|5|Briefly described|p97 Fig. 11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Of the Rolling Downs Group.||||||
20268|Winton Formation|23916|5|Briefly described|p523|Cenomanian|Albian|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|23982|5|Briefly described|p35 Fig.7|Cretaceous|Cretaceous|Of Rolling Downs Group. Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24092|5|Briefly described|p5|Cretaceous|Cretaceous|Geological Province: Great Artesian Basin.||||||
20268|Winton Formation|24112|5|Briefly described|p270|Cenomanian|Albian|Age: 97-90Ma (Krieg et al, 1995). Geological Province: Eromanga Basin||||||
20268|Winton Formation|24175|3|Fully described|p30, p17 Fig. 3|Cenomanian|Albian|Overlain by Eyre Formation; conformably overlies Mackunda Formation.  Max. thickness: 88m.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24204|5|Briefly described|p263 Fig.4, p267|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||17-DEC-04
20268|Winton Formation|24210|5|Briefly described|p133 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||
20268|Winton Formation|24243|5|Briefly described|p3 Fig.2|Cretaceous|Cretaceous|Of Rolling Downs Group.||||||
20268|Winton Formation|24251|5|Briefly described|p234 Fig.1|Cenomanian|Cenomanian|Geological Province: Eromanga Basin||||||
20268|Winton Formation|24321|5|Briefly described|Map legend|Cenomanian|Cenomanian|Of the Neales River Group.||||||19-DEC-06
20268|Winton Formation|29591|6|Mentioned|p71|||||||||
20268|Winton Formation|29721|6|Mentioned|Table 137|||||||||
20268|Winton Formation|30019|6|Mentioned|p2|||||||||
20268|Winton Formation|30055|6|Mentioned|p159|||||||||
20268|Winton Formation|30102|6|Mentioned|Table 4|||See also p36,37.||||||19-DEC-06
20268|Winton Formation|30104|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper? Cretaceous||||||
20268|Winton Formation|30514|6|Mentioned|p102|||Middle Cretaceous age.||||||
20268|Winton Formation|30539|6|Mentioned|p7|||Late Albian - early Cenomanian age||||||
20268|Winton Formation|30540|6|Mentioned|Fig.6|||||||||
20268|Winton Formation|30691|4|Described|p17|||See also p21,Table 4. Lower - Upper Cretaceous||||||19-DEC-06
20268|Winton Formation|30700|6|Mentioned|p28|||||||||
20268|Winton Formation|30803|6|Mentioned|p2|||Cretaceous age||||||
20268|Winton Formation|30804|6|Mentioned|p7|||On Table 1. See also Table 2.||||||
20268|Winton Formation|30807|6|Mentioned|p102|||Suggested map symbol||||||
20268|Winton Formation|30853|5|Briefly described|Table 3|||Lower to Upper Cretaceous||||||
20268|Winton Formation|30854|4|Described|Table 4|||Lower to Upper Cretaceous age.||||||19-DEC-06
20268|Winton Formation|30855|6|Mentioned|Map legend|Cretaceous|Cretaceous|Unit in Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|30856|4|Described|Table 3|||On p10. Lower-Upper Cretaceous.||||||19-DEC-06
20268|Winton Formation|30857|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|30914|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|30918|6|Mentioned|p82|||||||||
20268|Winton Formation|30919|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|30921|6|Mentioned|Map legend|Oligocene|Oligocene|||||||
20268|Winton Formation|31144|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|L. - U. Cretaceous||||||
20268|Winton Formation|31145|5|Briefly described|Table 1|||L. - U. Cretaceous||||||
20268|Winton Formation|31425|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower-Upper? Cretaceous||||||
20268|Winton Formation|31430|5|Briefly described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31431|5|Briefly described|Table 3|||L.Cretaceous||||||
20268|Winton Formation|31432|4|Described|Table 1|||L.-U.Cretaceous||||||
20268|Winton Formation|31436|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31438|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|31441|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31443|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|31553|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|31649|6|Mentioned|p63|||||||||
20268|Winton Formation|31699|4|Described|p133|||Middle Cretaceous||||||
20268|Winton Formation|31706|6|Mentioned|p669|||Cretaceous correlation chart||||||
20268|Winton Formation|31923|6|Mentioned|p15|||||||||
20268|Winton Formation|32274|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|32275|6|Mentioned|p6|||||||||
20268|Winton Formation|32277|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower Cretaceous - Upper Cretaceous.||||||
20268|Winton Formation|32314|6|Mentioned|Fig. 4|||||||||
20268|Winton Formation|32396|6|Mentioned|p10|||Equivalents||||||
20268|Winton Formation|32413|6|Mentioned|p103|||||||||
20268|Winton Formation|32472|6|Mentioned|p17|||||||||
20268|Winton Formation|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
20268|Winton Formation|32696|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|32796|6|Mentioned|p303|||||||||
20268|Winton Formation|32918|6|Mentioned|p20|||||||||
20268|Winton Formation|33016|6|Mentioned|p1|||Table on P1||||||
20268|Winton Formation|33017|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33067|4|Described|Table 1|Late Cretaceous|Early Cretaceous|Of the Rolling Downs Group.||||||07-JUL-04
20268|Winton Formation|33069|4|Described|p7|||||||||
20268|Winton Formation|33072|4|Described|Table 1|||L.Cret.||||||
20268|Winton Formation|33073|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|33075|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33078|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Cretaceous||||||
20268|Winton Formation|33079|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33081|6|Mentioned|p26|||||||||
20268|Winton Formation|33082|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33083|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33086|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33087|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33088|4|Described|Table 3|||Of the Rolling Downs Group.||||||19-DEC-06
20268|Winton Formation|33089|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33095|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|33165|6|Mentioned|Chart|||Correlation chart only||||||
20268|Winton Formation|33368|6|Mentioned|p25|||Strat.Table.||||||
20268|Winton Formation|33372|6|Mentioned|Table 1|||||||||
20268|Winton Formation|33414|6|Mentioned|p212-214,Tb.||Cenomanian|Part of Manuka Sub-Group.||||||
20268|Winton Formation|33448|4|Described|Table 1|||L.-U.Cret.||||||11-JAN-10
20268|Winton Formation|33449|4|Described|Table 1|||L.-U.Cret.||||||
20268|Winton Formation|33452|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower to Upper Cretaceous||||||
20268|Winton Formation|33490|6|Mentioned|p30|||Cret. sediments. Correlation||||||
20268|Winton Formation|33521|6|Mentioned|p10|||Upper Cretaceous||||||
20268|Winton Formation|33561|6|Mentioned|p102|||||||||
20268|Winton Formation|33569|6|Mentioned|p63|||||||||
20268|Winton Formation|33639|5|Briefly described|p12|||L.-U.Cret.||||||
20268|Winton Formation|33640|4|Described|Table 2|||L.-U.Cret.||||||
20268|Winton Formation|33642|6|Mentioned|p144-45,147,148,Tb.1|||Refers Dunstan (1916) & Whitehouse (1954)||||||
20268|Winton Formation|33647|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper? Creataceous||||||
20268|Winton Formation|33648|6|Mentioned|p19|||Stratigraphy.||||||
20268|Winton Formation|33819|6|Mentioned|p1|||||||||
20268|Winton Formation|33820|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33821|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|33822|6|Mentioned|Map legend|Cenomanian|Albian|Albian - Cenomanian||||||
20268|Winton Formation|33823|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33824|6|Mentioned|p7|||P12, Tables 1 & 2||||||
20268|Winton Formation|33825|6|Mentioned|p8|||Strat. table. Lithology||||||
20268|Winton Formation|33827|6|Mentioned|p7|||See also p3 and Tables 1 and 3.||||||19-DEC-06
20268|Winton Formation|33828|6|Mentioned|p9|||See also Table 1||||||
20268|Winton Formation|33831|6|Mentioned|Map legend|Cenomanian|Neocomian|Neocomian - Cenomanian||||||
20268|Winton Formation|33832|6|Mentioned|p6|||Strat.||||||
20268|Winton Formation|33936|6|Mentioned|Fig.3A|||Cret.||||||
20268|Winton Formation|33937|6|Mentioned|p3|||||||||
20268|Winton Formation|33938|6|Mentioned|p19|||Refers Jack (1930).||||||
20268|Winton Formation|33964|4|Described|p6|||||||||
20268|Winton Formation|33971|5|Briefly described|p37|||See also Fig.15.||||||
20268|Winton Formation|34035|6|Mentioned|p544|||Cret.||||||
20268|Winton Formation|34061|6|Mentioned|p53|||||||||
20268|Winton Formation|34065|4|Described|p6|||L.-U. Cret.||||||
20268|Winton Formation|34174|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34217|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|34218|4|Described|Table 1|||Lower - Upper Cretaceous. See also pp8,10-12 etc.||||||19-DEC-06
20268|Winton Formation|34254|6|Mentioned|p492|||||||||
20268|Winton Formation|34259|6|Mentioned|p451|||||||||
20268|Winton Formation|34282|6|Mentioned|p88|||See also PP90, 93 etc.||||||
20268|Winton Formation|34287|6|Mentioned|p199|||Cret.||||||
20268|Winton Formation|34356|6|Mentioned|p32|||||||||
20268|Winton Formation|34400|6|Mentioned|p14|||Lower Cretaceous||||||
20268|Winton Formation|34454|5|Briefly described|Table 1|||Cretaceous. See also pp6,12,15.||||||19-DEC-06
20268|Winton Formation|34485|5|Briefly described|Table 1|||Lower - Upper? Cretaceous.||||||19-DEC-06
20268|Winton Formation|34486|5|Briefly described|Table 1|||Lower - Upper? Cretaceous. See also Table 2||||||
20268|Winton Formation|34487|6|Mentioned|Map legend|Late Cretaceous|Early Cretaceous|Lower - Upper Cretaceous||||||
20268|Winton Formation|34543|6|Mentioned|p98|||||||||
20268|Winton Formation|34611|4|Described|p158|||Cretaceous. See Fig.65,66||||||
20268|Winton Formation|34909|6|Mentioned|p992|||||||||
20268|Winton Formation|34948|6|Mentioned|Fig. 70|||||||||
20268|Winton Formation|35067|6|Mentioned|Fig.4|||||||||
20268|Winton Formation|35139|6|Mentioned|p17|||||||||
20268|Winton Formation|35151|6|Mentioned|p147|||||||||
20268|Winton Formation|35239|6|Mentioned|p258|||||||||
20268|Winton Formation|35560|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|35793|4|Described|p241|||Details of weathering and profiles.||||||
20268|Winton Formation|35811|5|Briefly described|Table 3|||||||||
20268|Winton Formation|35894|6|Mentioned|p275|||||||||
20268|Winton Formation|36172|6|Mentioned|Appendix|||||||||
20268|Winton Formation|36213|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|36229|6|Mentioned|Map legend|Eocene|Eocene|||||||
20268|Winton Formation|36243|6|Mentioned|Table 6A|||||||||
20268|Winton Formation|36327|6|Mentioned|p7|||||||||
20268|Winton Formation|36571|6|Mentioned|p98|||See also Table 4.||||||
20268|Winton Formation|36912|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|36922|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|37065|5|Briefly described|p41|||||||||
20268|Winton Formation|37114|6|Mentioned|p308|||||||||
20268|Winton Formation|37116|4|Described|p312|||||||||
20268|Winton Formation|37261|6|Mentioned|p351|||||||||
20268|Winton Formation|37263|6|Mentioned|p319|||||||||
20268|Winton Formation|37287|6|Mentioned|p36|||||||||
20268|Winton Formation|37451|6|Mentioned|Table 2|||||||||
20268|Winton Formation|37603|6|Mentioned|p444|||||||||
20268|Winton Formation|37607|6|Mentioned|p333|||||||||
20268|Winton Formation|37608|3|Fully described|Table 1|||||||||
20268|Winton Formation|37776|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|38068|5|Briefly described|p72|||||||||
20268|Winton Formation|38226|6|Mentioned|p414|||See also Fig.6.||||||
20268|Winton Formation|38373|6|Mentioned|p622|||||||||
20268|Winton Formation|38779|6|Mentioned|p3|||||||||
20268|Winton Formation|38814|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39070|4|Described|p366|||||||||
20268|Winton Formation|39085|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39211|5|Briefly described|Fig.3, Fig.6|||See also Figs 4,5,7,14,15 etc. Correlation||||||
20268|Winton Formation|39352|6|Mentioned|Map legend|Albian|Aptian|Aptian to Albian||||||
20268|Winton Formation|39445|5|Briefly described|Table 11|||||||||
20268|Winton Formation|39478|6|Mentioned|Table 1|||||||||
20268|Winton Formation|39482|6|Mentioned|Fig.7|||||||||
20268|Winton Formation|39846|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|39847|5|Briefly described|p40|||||||||
20268|Winton Formation|39914|6|Mentioned|p3|||||||||
20268|Winton Formation|39943|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40003|6|Mentioned|Fig.9   or|||||||||
20268|Winton Formation|40058|6|Mentioned|Fig.1|||||||||
20268|Winton Formation|40121|6|Mentioned|Table 1|||||||||
20268|Winton Formation|40150|6|Mentioned|p77|||||||||
20268|Winton Formation|40199|6|Mentioned|p16|||||||||
20268|Winton Formation|40220|6|Mentioned|p7|||||||||
20268|Winton Formation|40249|6|Mentioned|p41|||||||||
20268|Winton Formation|40322|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|40670|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|40675|6|Mentioned|Table 8A|||||||||
20268|Winton Formation|40681|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|40756|6|Mentioned|Fig.1.2|||||||||
20268|Winton Formation|40757|6|Mentioned|p78|||Now known to be Eyre Formation||||||
20268|Winton Formation|40801|6|Mentioned|p29|||Mention also Fig.21||||||
20268|Winton Formation|40910|6|Mentioned|p15|||See also P17||||||
20268|Winton Formation|40911|6|Mentioned|Map legend|Cenomanian|Albian|Albian-?Cenomanian||||||
20268|Winton Formation|40925|6|Mentioned|Map legend|Cretaceous|Cretaceous|||||||
20268|Winton Formation|40926|3|Fully described|p18|||||||||
20268|Winton Formation|41057|6|Mentioned|p82|||||||||
20268|Winton Formation|41060|6|Mentioned|p3|||Generalized stratigraphy||||||
20268|Winton Formation|41061|6|Mentioned|p19|||||||||
20268|Winton Formation|41062|6|Mentioned|p35|||||||||
20268|Winton Formation|41063|6|Mentioned|p40|||||||||
20268|Winton Formation|41064|6|Mentioned|p62|||||||||
20268|Winton Formation|41085|6|Mentioned|p90|||||||||
20268|Winton Formation|41086|3|Fully described|p98|||See also Fig.3||||||
20268|Winton Formation|41088|6|Mentioned|p144|||See also Fig.2||||||
20268|Winton Formation|41097|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41098|4|Described|p177|||||||||
20268|Winton Formation|41099|6|Mentioned|Fig.9|||||||||
20268|Winton Formation|41165|5|Briefly described|p363|||See also Fig.15.||||||19-DEC-06
20268|Winton Formation|41174|6|Mentioned|p117|||||||||
20268|Winton Formation|41176|6|Mentioned|p206|||See also P211||||||
20268|Winton Formation|41177|6|Mentioned|p233|||||||||
20268|Winton Formation|41182|5|Briefly described|Fig.2|||||||||
20268|Winton Formation|41183|4|Described|p307|||||||||
20268|Winton Formation|41184|6|Mentioned|p346|||||||||
20268|Winton Formation|41187|6|Mentioned|Fig.2|||||||||
20268|Winton Formation|41198|6|Mentioned|Table 1|||||||||
20268|Winton Formation|41214|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41216|6|Mentioned|p299|||||||||
20268|Winton Formation|41219|6|Mentioned|p338|||||||||
20268|Winton Formation|41266|6|Mentioned|Fig.3|||||||||
20268|Winton Formation|41523|3|Fully described|p282|||See also p283.||||||19-DEC-06
20268|Winton Formation|41535|6|Mentioned|p369|||||||||
20268|Winton Formation|41707|6|Mentioned|Fig.8|||||||||
20268|Winton Formation|41720|6|Mentioned|p372|||||||||
20268|Winton Formation|41724|5|Briefly described|p383|||||||||
20268|Winton Formation|41950|5|Briefly described|Fig.2 P3|||||||||
20268|Winton Formation|42061|4|Described|Fig,11 P159|||See also Fig.11||||||
20268|Winton Formation|42067|6|Mentioned|Fig.2 P309|||||||||
20268|Winton Formation|42071|6|Mentioned|p117|||||||||
20268|Winton Formation|42084|6|Mentioned|Fig.3 P256|||||||||
20268|Winton Formation|42085|6|Mentioned|Fig.2 P374|||||||||
20268|Winton Formation|42187|6|Mentioned|Fig.5 P322|||||||||
20268|Winton Formation|42293|6|Mentioned|Fig.2 P.18|||||||||
20268|Winton Formation|42346|5|Briefly described|p84|Cretaceous||||||||
20268|Winton Formation|42375|6|Mentioned|p30, p121, p125|Late Cretaceous|Jurassic|Eromanga Basin.||||||
20268|Winton Formation|42395|5|Briefly described|Fig.13 P83|||||||||
20268|Winton Formation|42397|6|Mentioned|Fig.2 P3|||||||||
20268|Winton Formation|42429|5|Briefly described|p155|Cenomanian||||||||
20268|Winton Formation|42447|6|Mentioned|Fig. 1|||||||||
20268|Winton Formation|42496|5|Briefly described|p136, Fig.3 p132|||||||||
20268|Winton Formation|42520|5|Briefly described|p6|||||||||
20268|Winton Formation|42543|5|Briefly described|Fig.4 P6|||||||||
20268|Winton Formation|42645|6|Mentioned|p195|||||||||
20268|Winton Formation|42648|5|Briefly described|Fig.7 P43|||||||||
20268|Winton Formation|42673|5|Briefly described|Fig.2, P184|||||||||
20268|Winton Formation|42746|4|Described|p12|||See also Fig.2, Fig.6||||||
20268|Winton Formation|42749|6|Mentioned|Fig.2 P27|||||||||
20268|Winton Formation|42784|6|Mentioned|p492|||||||||
20268|Winton Formation|42905|5|Briefly described|p20, Fig 5.3|||||||||
20268|Winton Formation|42999|5|Briefly described|Table 2,p90||Late Cretaceous|||||||
20268|Winton Formation|43002|5|Briefly described|Fig.2,p135|||||||||
20268|Winton Formation|43004|5|Briefly described|Table 1,p179|||||||||
20268|Winton Formation|43053|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolaustrine mudstone and siltstone.||||||25-MAY-05
20268|Winton Formation|43085|5|Briefly described|Fig.3|||||||||
20268|Winton Formation|43105|6|Mentioned|p15|||||||||
20268|Winton Formation|43114|6|Mentioned|Table 2|||||||||
20268|Winton Formation|43122|5|Briefly described|Fig.2.|||||||||
20268|Winton Formation|43252|5|Briefly described|p163|||||||||
20268|Winton Formation|43258|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43298|5|Briefly described|Map Legend||Cretaceous|||||||
20268|Winton Formation|43344|14|Not recorded|p14|||||||||
20268|Winton Formation|43383|14|Not recorded|p27|||||||||
20268|Winton Formation|43384|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|43390|14|Not recorded|p16|||Part of Rolling Downs Group||||||
20268|Winton Formation|43452|14|Not recorded|Map Legend||Cretaceous|Of the Rolling Downs Group.||||||14-FEB-05
20268|Winton Formation|43459|14|Not recorded|p315|||||||||
20268|Winton Formation|43591|6|Mentioned|p40|||||||||
20268|Winton Formation|43602|6|Mentioned|191|||In Eromanga Basin, Rolling Downs Group||||||
20268|Winton Formation|43628|6|Mentioned|Fig.3|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|43883|14|Not recorded|p18 Fig.4-3|||||||||
20268|Winton Formation|43985|14|Not recorded|7-10,12,Fig.3,Pl.1,2|||||||||
20268|Winton Formation|43995|14|Not recorded|Tb.p9,30,57-8,Fig.3||Late Cretaceous|Fig.15||||||
20268|Winton Formation|44016|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44017|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44018|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44019|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44020|14|Not recorded|p8,10-11,13-15,Tb.1,|Late Cretaceous|Early Cretaceous|Of Rolling Downs Group. Tb.2,3, Fig.3,||||||
20268|Winton Formation|44031|14|Not recorded|p5,6,8,9||Cretaceous|||||||
20268|Winton Formation|44033|4|Described|map,4,8,9,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44034|4|Described|Tb.1,p2,4-6,9,10|||||||||
20268|Winton Formation|44040|14|Not recorded|p35|||||||||
20268|Winton Formation|44041|6|Mentioned|p251|||||||||
20268|Winton Formation|44066|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44067|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44068|14|Not recorded|p17,18|||||||||
20268|Winton Formation|44082|14|Not recorded|p28,30,Tb.p34|||||||||
20268|Winton Formation|44087|14|Not recorded|p4,8-12|||Lacustrine.||||||
20268|Winton Formation|44088|14|Not recorded|Tb.1,opp.p6,7,8,map|||||||||
20268|Winton Formation|44089|4|Described|p3-6,8-10,Tb.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44090|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44091|14|Not recorded|p61||Cretaceous|||||||
20268|Winton Formation|44098|14|Not recorded|p98|||||||||
20268|Winton Formation|44099|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|(Rolling Downs Group)||||||
20268|Winton Formation|44115|14|Not recorded|p17,20|||||||||
20268|Winton Formation|44119|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44120|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44121|14|Not recorded|p5-8,10,12||Cretaceous|See also Lexicon.||||||
20268|Winton Formation|44122|2|Defined|p318-324|||||||||
20268|Winton Formation|44133|4|Described|p123, 104 Fig. 9.11|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Maximum Thickness: ~1200m. Includes part of the now superseded Blanchewater Formation.||||||
20268|Winton Formation|44168|14|Not recorded|Tb.1p5,7,8,10,map|||||||||
20268|Winton Formation|44269|14|Not recorded|p18||Cretaceous|||||||
20268|Winton Formation|44291|14|Not recorded|p5|||||||||
20268|Winton Formation|44310|14|Not recorded|Map Legend||Cretaceous|||||||
20268|Winton Formation|44346|14|Not recorded|p4|||||||||
20268|Winton Formation|44374|14|Not recorded|p12||Cretaceous|Freshwater-final withdrawal of sea from Eromanga Basin.||||||
20268|Winton Formation|44375|14|Not recorded|p313|||||||||
20268|Winton Formation|44405|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44406|14|Not recorded|p3-14|Cenomanian|Albian|||||||
20268|Winton Formation|44407|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44408|14|Not recorded|p4,8-13,opp.6|||||||||
20268|Winton Formation|44410|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44413|14|Not recorded|p470,474|||||||||
20268|Winton Formation|44414|14|Not recorded|p110-112||Cretaceous|Mudstone, siltstone and characteristic coal seams.||||||
20268|Winton Formation|44415|14|Not recorded|p22|||||||||
20268|Winton Formation|44417|14|Not recorded|p416,417,420|||||||||
20268|Winton Formation|44418|14|Not recorded|Map Legend|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|44509|14|Not recorded|p342-343|||||||||
20268|Winton Formation|44548|14|Not recorded|p456||Cretaceous|||||||
20268|Winton Formation|44573|14|Not recorded|p98|||||||||
20268|Winton Formation|44611|14|Not recorded|p22,24|||||||||
20268|Winton Formation|44634|14|Not recorded|p29|||||||||
20268|Winton Formation|44715|14|Not recorded|Map Legend|||||||||
20268|Winton Formation|44732|14|Not recorded|Pl.1|||Taken from GeolMap QLD 1953.||||||
20268|Winton Formation|44807|14|Not recorded|p10|||||||||
20268|Winton Formation|44819|14|Not recorded|p89,90|||Non-marine sandstone, carbonaceous grey shale and coal. No age given.||||||
20268|Winton Formation|44848|14|Not recorded|p99-101|||||||||
20268|Winton Formation|44852|14|Not recorded|p78||Late Cretaceous|||||||
20268|Winton Formation|44915|14|Not recorded|p18,24|||Correlated with upper part of Blanchewater Formation in South Australia. Age not given.||||||
20268|Winton Formation|44998|14|Not recorded|p.169|||||||||
20268|Winton Formation|45004|14|Not recorded|p.8,9|||||||||
20268|Winton Formation|45110|6|Mentioned|Table 18|||||||||
20268|Winton Formation|45168|6|Mentioned|p6|||See also Table 1||||||
20268|Winton Formation|46791|5|Briefly described|p48|||||||||
20268|Winton Formation|46854|6|Mentioned|p241|||||||||
20268|Winton Formation|46911|5|Briefly described|p112|||Analyses of weathered profiles and parent rocks.||||||
20268|Winton Formation|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20268|Winton Formation|46939|6|Mentioned|Fig.1|||See also Table 1.||||||
20268|Winton Formation|48627|14|Not recorded|p3|||||||||
20268|Winton Formation|48634|4|Described|p5,19,20|||See also Fig.2,6,Pl.1,2. Subsidy report. (G54-14).||||||
20268|Winton Formation|48751|6|Mentioned|p19|||||||||
20268|Winton Formation|48906|14|Not recorded|p5,9,Tb.2,Fig.1,Pl.1|Late Cretaceous|Early Cretaceous|||||||
20268|Winton Formation|48908|14|Not recorded|Tb.1||Late Cretaceous|||||||
20268|Winton Formation|48920|3|Fully described|p62|||Cretaceous age||||||
20268|Winton Formation|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20268|Winton Formation|49011|6|Mentioned|Fig.3|||In the Eromanga Basin.||||||19-DEC-06
20268|Winton Formation|60080|5|Briefly described|Map legend|Late Cretaceous|Early Cretaceous|Very labile sandstone, siltstone and mudstone; calcareous in part, minor mud clast conglomerate.  Overlain by Glendower Formation.||||||22-JUL-04
20268|Winton Formation|60281|6|Mentioned|p11|||||||||
20268|Winton Formation|60331|5|Briefly described|p34 Fig.3||Cenomanian|Overlies Mackunda Formation. Geological Province: Eromanga Basin||||||
20268|Winton Formation|60717|5|Briefly described|p40 Fig. 2|Late Cretaceous|Late Cretaceous|Overlies Oodnadatta Formation and Mackunda Formation. Geological Province: Eromanga Basin. Non-marine to marginal marine deposits.||||||31-JAN-08
20268|Winton Formation|60726|6|Mentioned|p2 Fig.1, p6.|Late Cretaceous|Late Cretaceous|Winton area, Great Artesian Basin.||||||
20268|Winton Formation|60953|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Fluviolacustrine mudstone and siltstone.||||||
20268|Winton Formation|61108|5|Briefly described|map legend|Cretaceous|Cretaceous|Fluviolacustraine mudstone and siltstone.||||||
20268|Winton Formation|61312|5|Briefly described|p75, p79 Table E2|Cretaceous|Cretaceous|Of the Rolling Downs Group. Consists of interbedded mudstone and lithic and feldspathic sandstone deposited in terrestrial environments. Geological Province: Eromanga Basin (absent in NSW). See also p64, p67 Fig. E5.||||||19-DEC-06
20268|Winton Formation|61611|6|Mentioned|p265 Fig. 3|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||13-MAR-09
20268|Winton Formation|61613|6|Mentioned|p282 Fig. 2|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|61614|6|Mentioned|p290 Fig. 2|Late Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||17-MAR-09
20268|Winton Formation|61823|5|Briefly described|p118|Cenomanian|Late Albian|Predominantly alluvial deposits.  Geological Province: Eromanga Basin.||||||
20268|Winton Formation|62028|5|Briefly described|p10 Fig. 1|||||||||
20268|Winton Formation|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20268|Winton Formation|62046|5|Briefly described|p125 Fig. 2|Cretaceous|Cretaceous|Geological Province: Cooper-Eromanga Basins.||||||14-APR-08
20268|Winton Formation|62376|5|Briefly described|p84|Late Cretaceous|Early Cretaceous|Geological Province: Pedirka Basin.||||||09-FEB-10
20268|Winton Formation|62537|6|Mentioned|p191 Fig.2. |Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Mackunda Formation.||
20268|Winton Formation|62730|5|Briefly described|p352 Fig. 1|Late Cretaceous|Late Cretaceous|Geological Province: Eromanga Basin.||||||21-APR-08
20268|Winton Formation|63979|2|Defined|p54-55, Fig. 44|Cenomanian|Albian|Formerly Winton Series (Dunstan 1916). Forms upper part of Rolling Downs Gp.Conformable on Mackunda Fm; unconformable below Glendower Fm. Max.thick:1000m. Interbedded sands., sandy siltst., siltst., mudst.+ coal with minor intraformational conglomerate.||||||07-FEB-11
20268|Winton Formation|64048|5|Briefly described|p64 Tb. 2|||Source of hydrocarbons - lignite. Geological Province: Eromanga Basin.||||||07-FEB-11
20268|Winton Formation|64197|6|Mentioned|p625 Fig.1c, p627, p630 Figs.6,7|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deeply weathered upper surface.||||Overlies Oodnadatta and Mackunda Formations. Is overlain unconformably by Eyre Formation.||11-DEC-15
20268|Winton Formation|64232|5|Briefly described|p12|Cretaceous|Cretaceous|Geological Province: Eromanga Basin. Coal measures are present in this unit and are a potential target for CSM exploration activities.||||||24-JUL-08
20268|Winton Formation|64665|5|Briefly described|p62.|Cretaceous|Cretaceous|Eromanga Basin. Hosts coal seams up to 7 m thick; low rank lignites of no current (i.e. c.2008) commercial interest.||||||
20268|Winton Formation|64778|6|Mentioned|p13|Cretaceous|Cretaceous|Pedirka and Simpson Desert Basins.||||||
20268|Winton Formation|64856|6|Mentioned|p101|||Eromanga Basin. Younger than lithologically similar Griman Creek Formation in the Surat Basin.|| ||||29-NOV-17
20268|Winton Formation|65238|5|Briefly described|p7 Fig. 8, p10|Early Cretaceous|Early Cretaceous|Geological province: Eromanga Basin. Fluvial deposits.||||||
20268|Winton Formation|65342|5|Briefly described|p9.|||Eromanga Basin. Max. thickness at least 613 m. Seen as having potential as an insulating layer for geothermal energy.||||Overlies Oodnadatta Shale. Is overlain by Eyre Formation.|Sandstone, siltstone, mudstone; minor conglomerate, coal; predominantly alluvial deposits.|
20268|Winton Formation|65376|5|Briefly described|p9 Fig.1.2. |Cretaceous|Cretaceous||||||Marginal marine to fluvial mudstone and siltstone.|
20268|Winton Formation|65385|5|Briefly described|pS134 Fig.7|Late Cretaceous|Early Cretaceous|Of Eromanga Basin. Overlies Mackunda Formation.||||||08-MAR-12
20268|Winton Formation|65489|5|Briefly described|p49, p53, p55, p57-61, p96, p155-156|Late Cretaceous|Late Cretaceous|Eromanga Basin. 1200m thick. Rapid non-marine deposition: c.1100m in c.8 m.y.||||Overlies Mackunda and Oodnadatta Formations. Is locally overlain unconformably by Mount Howie Sandstone.||
20268|Winton Formation|65925|5|Briefly described|p15, Appendix 2.|||Thousand-metre thick package deposited in low-energy fluvial to lacustrine environment.|||||Sandstone, shale, siltstone; coal seams.|
20268|Winton Formation|66131|6|Mentioned|p239|Cenomanian|Cenomanian|||||||
20268|Winton Formation|66529|5|Briefly described|p10, p12 Fig.5 |||Eromanga Basin.||Unit in Rolling Downs Group.||Overlies Mackunda and Normanton Formations.|~1000m thick package of non-marine sandstones, shales and siltstones.|
20268|Winton Formation|66623|3|Fully described|p242, p245, pp256-257, pp266-267.|Cenomanian|Albian|Marks the stratigraphic top of the Rolling Downs Group throughout the Eromanga Basin. Correlates with upper half of Yalpunga Beds. Very poor outcrop; extensive post-deposition erosion reduced thickness from 0 to 1100 m. Fossils include vertebrates, plants, wood and microfossils.||Unit in Rolling Downs Group.||Conformably overlies Allaru Mudstone. Is overlain unconformably by fluvial Paleogene sedimentary rocks of Lake Eyre Basin, and by Cordillo Silcrete capping.|Medium-grained, cross-bedded sandstone with rounded intraclasts of siltstone and mudstone; calcareous labile sandstone, siltstone, carbonaceous and pyritic shale with intraclast conglomerate and minor coal; fresh volcanic detritus in sandstones.|07-JUN-13
20268|Winton Formation|66915|5|Briefly described|p6 Fig.3|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|67119|5|Briefly described|Map legend.|Cretaceous|Cretaceous|Non-marine.|||||Shale, siltstone, sandstone; minor coal horizons.|
20268|Winton Formation|67323|5|Briefly described|p86-87, p92, p93 Fig.12.3, p95 Fig.12.5|Cretaceous|Cretaceous|See also GIS attrib tbl, Solid Geology Map. Eromanga/Carpentaria Basins. Oil shale was discovered in two wells (AAP Fermoy 1 and AAP Mayneside 1) in this unit by Australian Aquitaine Petroleum Pty Ltd in 1966. Attention shifted to outcrops in Julia Creek but activity ceased in 1969. Fluvial deposits. Underwent deep chemical weathering during Late Cretaceous to Palaeogene.||||Overlies Mackunda Formation.|Labile sandstone, siltstone, mudstone, minor coal.|
20268|Winton Formation|67402|4|Described|p26 tbl RRM4|Cenomanian|Cenomanian|Eromanga Basin. Maximum thickness of 1000m. Deposited in fluvial and lacustrine environments. Estimated porosity of 10-25% with likely favourable permeability for Carbon dioxide storage. See also p106, p108, p109, p111 fig ERO8, p115 tbl ERO2.||||Overlies the Mackunda Formation.|Interbedded sandstone, sandy siltstone, siltstone, mudstone and coal with minor intraformational conglomerate.|
20268|Winton Formation|67462|5|Briefly described|Map legend.|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies Oodnadatta Formation.||
20268|Winton Formation|67578|6|Mentioned|p335 Fig.2|Cretaceous|Cretaceous|Lake Eyre region.||||||
20268|Winton Formation|67784|5|Briefly described|p25, p31|Cenomanian|Albian|Northern Eromanga Basin. Up to 400m thick. Non-marine deposits.||||Overlies Mackunda Formation||08-FEB-18
20268|Winton Formation|68003|5|Briefly described|p63 Fig.3-p.|Cretaceous|Cretaceous|Surat Basin.||||Overlies Coreena Member.||
20268|Winton Formation|68004|6|Mentioned|p204.|||Hosts opal. Ferruginisation increases toward the basal one-third of the profile.||||||
20268|Winton Formation|68068|5|Briefly described|Map legend|Cenomanian|Cenomanian|Eromanga Basin. Subsurface only. Fluvial to paludal-lacustrine. Fossil wood and leaves, freshwater bivalves, fish and vertebrates.||Unit in Neales River Group.||Conformably and gradationally overlies Mackunda Formation.|Dark grey-brown sandy silt-clay, finely laminated and cross-bedded, weakly bioturbated; basal portions carbonaceous to lignitic: lowest coal often taken as base of unit.|
20268|Winton Formation|68131|5|Briefly described|p2 Fig.1|Cretaceous|Cretaceous|Marginal marine to fluvial sediments. Mapped with Winton Formation as one unit.|||||Mudstone and siltstone.|
20268|Winton Formation|68206|6|Mentioned|p28|Cenomanian|Cenomanian|Great Artesian Basin. Marks a return to non-marine conditions after Barremian-Albian inundation.||||||
20268|Winton Formation|68553|6|Mentioned|Map legend; schematic diagram.|Cretaceous|Cretaceous|Eromanga and Carpentaria Basins.||Unit in Rolling Downs Group.||Conformably overlies Mackunda Formation.||
20268|Winton Formation|68713|5|Briefly described|p22|Cretaceous|Cretaceous|||Of the Neales River Group.||||
20268|Winton Formation|68715|6|Mentioned|p30 Fig.5|Cenomanian|Albian|Eromanga Basin.||||||
20268|Winton Formation|68731|6|Mentioned|pp209-211|||||||||
20268|Winton Formation|68734|5|Briefly described|p218 Fig.2, p218, p221 Fig.3|Cenomanian|Albian|Eromanga Basin (SW and NE). Fluvial to lacustrine. Late Albian maximum age. Opal is typically found in the upper 1-2 m of a claystone layer underlying a sandstone layer.||Of the Rolling Downs Group.|||Volcaniclastic.|18-JAN-22
20268|Winton Formation|68821|4|Described|p292 Fig.1, pp294-302, p307, p308 Fig.10|Cenomanian|Albian|Late Albian Maximum age. Contains ubiquitous disseminated pyrite. Preserved thickness is approximately 1200 m in the centre of the Eyre Basin. Fluvial to fluvial-lacustrine depositional environment.|97 - 93 Ma|Of the Rolling Downs Group.||Unconformably overlain by the Eyre Formation.|Comprises fluvial sandstone and siltstone.|
20268|Winton Formation|68901|5|Briefly described|p7 Fig. ii|||Eromanga Basin.||Rolling Downs Group|||Sandstone, siltstone, mudstone, calcareous in part.|27-SEP-18
20268|Winton Formation|69001|6|Mentioned|p18|Late Cretaceous||||||||
20268|Winton Formation|69019|4|Described|p83 Fig.20,p85,p94 Fig.24,p100-103,p169|Turonian|Cenomanian|Of Whitehouse (1953); formerly Winton Series (Dunstan, 1916). Named after Winton, Qld. Terrestrial deposition. Thickness from 0-150 m. Contains fossils of plants, lungfish teeth and possible dinosaur bone fragments. Of interest to explorers for biogenic coal seam gas.||Unit in Neales River Group.||Overlies Mackunda Formation. Is overlain disconformably by Eyre Formation and locally by Mount Howie Sandstone.|Dark khaki-grey to dark grey-brown, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained calcareous sandstone, sometimes feldspathic; seams of coal or lignite at/near the base; abundant plant fossils.|
20268|Winton Formation|69023|5|Briefly described|p79, p86-87, p89 Fig.20, p93, p100|Turonian|Cenomanian|See also p105-106, p110, p112, p163, p191-192. Whitehouse (1955); formerly the Winton Series of Dunstan (1916) for freshwater sediments with coal seams in bores around Winton, Qld. Eromanga Basin. Resembles underlying Mackunda Formation. <40m thick. Contains plant, invertebrate and vertebrate fossils. Stratigraphic wells intersection data.||||Conformably overlies Mackunda Formation and Marree Subgroup. Is overlain disconformably by Eyre Formation.|Dark khaki-grey to grey, carbonaceous and pyritic mudstone interbedded with pale grey, fine-grained, calcareous sandstone and coal seams. Typically weathers to yellow or white kaolinitic sandstone.|
20268|Winton Formation|69454|5|Briefly described|p38:3, 13|Late Cretaceous|Late Cretaceous|Eromanga Basin. Deposition of this thick unit initiated hydrocarbon generation in underlying Permian and post-Permian source rocks.||||||12-JUL-16
20268|Winton Formation|69457|3|Fully described|p41:2-6, 9, 11-13, 17|Late Cretaceous|Early Cretaceous|Whitehouse (1955). Uppermost unit in the Eromanga Basin. Formerly part of the superseded Blanchewater Formation, used for the combined undifferentiated Mackunda-Winton Formations interval. Fluviatile to paludal to lacustrine deposits; paralic, estuarine, deltaic and fluviatile near base. Maximum 620m thick in NT; c.1200m in the Patchawarra Trough in SA. Poorly exposed as highly weathered outcrops around dry lakes. Contains abundant micro- and macroflora and macrofauna. Late Albian to early Cenomanian. The seams of brown to black coal are uneconomic. Sediment loading by this thick unit is believed to have triggered hydrocarbon generation.||Manuka Subgroup.||Conformably overlies Mackunda Formation.|Claystone, siltstone and mudstone with interbedded very fine- to medium-bedded sandstone, and minor coal seams usually interbedded with carbonaceous mudstone; local minor intraformational conglomerate. Contains plant fragments and fossil wood.|12-JUL-16
20268|Winton Formation|69555|5|Briefly described|p43-44, p46-48|Turonian|Albian|Comprises the youngest Cretaceous strata of the Eromanga Basin. Fossil flora (palynological and macro) listed and described.||Rolling Downs Group|||Fossiliferous fine- to medium-grained, feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones, with very minor coal seams.|13-FEB-18
20268|Winton Formation|69582|6|Mentioned|p65|Late Cretaceous|Late Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|69594|5|Briefly described|p519, p526, p530-532, p563, p574|Cenomanian|Albian|Whitehouse (1955); Gray et al. (2002). Youngest deposits in the Eromanga Basin. Up to 1000m thick. The Mackunda-Winton boundary is difficult to pick. Unweathered outcrop is mainly well-cemented nodular sandstone; weathered outcrop is kaolinitised and ferruginised sandstones, mudstones and siltstone. Paralic, estuarine, deltaic and fluvial deposits in lower part; fluvio-lacustrine higher up. Contains a rich and diverse fossil flora, fauna and ichnofauna (listed and photographs); supports an economically important tourism industry. Detrital zircon plot.|~95 Ma (detrital zircon MDA: Greentree 2011).|||Conformably overlies Mackunda Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Much of the detritus is volcanogenic.|
20268|Winton Formation|69599|5|Briefly described|p599-600|Cretaceous|Cretaceous|||||Is overlain unconformably by Old Cork beds, Moses Sandstone, Edkins and Glendower Formations.||
20268|Winton Formation|69673|4|Described|p155 fig 127|Cretaceous|Cretaceous|Up to 620m thick.||Manuka Subgroup||Overlies Mackunda Formation, overlain by Mount Howie Sandstone Member|Claystone, siltstone and mudstone with interbedded very fine to fine to occasionally medium grained sandstone and minor coal seams.|
20268|Winton Formation|69742|5|Briefly described|p787, 788, 790, 793|Cenomanian|Albian|Great Artesian Basin. Hosts opal. Fluvial volcaniclastics. Geochemistry discussed.|||||Red-brown ironstone dominated by goethite and kaolinite with minor quartz and illite.|
20268|Winton Formation|69751|6|Mentioned|p35-38, 41|Cretaceous|Cretaceous|Eromanga Basin. Freshwater, broad fluvial-lacustrine environment of deposition (at least the upper part). Contains rich fossil assemblages; also silicified wood. Cenomanian-Turonian climate was seasonal and variable, with potential flooding and/or drought.|||||Fine- to medium-grained feldspatholithic or lithofeldspathic arenites, siltstones, mudstones and claystones; very minor coal seams.|
20268|Winton Formation|69797|5|Briefly described|p17 Fig.2|Late Cretaceous|Late Cretaceous|Geol. Prov: Eromanga Basin.||||||
20268|Winton Formation|69946|2|Defined|p27-28, p56-57, p124-125, p129|Late Cretaceous|Late Cretaceous|Eromanga Basin. Originally Winton Series (Dunstan, 1916), without formal definition. Renamed Winton Formation by Whitehouse (1955). His type section is 'blue shales and sandstones with intercalated coal seams met within the bores in and around Winton'. Distinguishing from Mackunda Formation is difficult in SA due to lack of coals, but easier in Qld due to coal seams, intraformational conglomerates and absence of marine fossils. 400-1100m thick. Late Albian - Cenomanian. Freshwater fossils listed. The top has been deeply (>40m) weathered.||||Conformably overlies Mackunda Formation. Is overlain unconformably by Eyre Formation.|Interbedded fine- to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates. Sandstone beds contain abundant fresh volcanogenic debris, lithics and feldspar.|
20268|Winton Formation|69947|5|Briefly described|p3, p9, p13 Fig.7.2|Late Cretaceous|Late Cretaceous|The final deposits in the Eromanga Basin. Is overlain by Tertiary sediments of the Lake Eyre Basin. On p9 the authors state: "the fluviolacustrine Winton Formation of the upper Marree Subgroup", which contradicts what appears in Fig.7.2.||||||
20268|Winton Formation|69948|6|Mentioned|p6; Figs.4.1, 18|||Eromanga Basin. Surface exposures of this and older units define the Birdsville Track Ridge.||||Overlies Mackunda Formation.||
20268|Winton Formation|69952|5|Briefly described|p16|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Rolling Downs Group.|||Sandstone, siltstone, mudstone; calcareous in part.|
20268|Winton Formation|70383|5|Briefly described|p45|Cretaceous|Cretaceous|Eromanga Basin. Non-marine deposits.||||||
20268|Winton Formation|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Rolling Downs Group|||Non-marine mudstone and siltstone with subordinate interbedded coarse lithic and feldspathic labile sandstone.|18-JAN-22
20268|Winton Formation|70720|6|Mentioned|p6|||Eromanga Basin.||||Overlies Coreena Member. Is overlain by Glendower Formation.||
20268|Winton Formation|70789|5|Briefly described|p318, p320 Fig.4|Cenomanian|Cenomanian|Eromanga Basin.|c.93 Ma.||||Marine mudstones, siltstones and shales.|
20268|Winton Formation|70821|4|Described|p21-24, p30-31, p33, p79-80, p82|Late Cretaceous|Late Cretaceous|See also p85-87, p115-116. Youngest Formation in the Eromanga Basin. Much of this unit in the southern Thomson region has been removed by erosion. Crops out as low breakaways, intensely weathered (kaolinitised and ferruginised): the weathering profile can be up to 95m deep. One of the two main groundwater resources in the Great Artesian Basin. Paralic, estuarine, deltaic and fluvial deposits in the lower part; fluvio-lacustrine in the upper. Fossil biota is dominated by fish, crocodiles, dinosaurs and pterosaurs. Late Albian to Cenomanian. Hydrochemistry mentioned; hydrostratigraphic properties.||Rolling Downs Group.||Overlies Mackunda Formation and locally the Wallumbilla Formation (conformably). Is overlain unconformably by Glendower Formation.|Interbedded labile volcanic lithic-crystal sandstone, sandy siltstone, siltstone, mudstone, intraformational conglomerate and coal. Also pyritic black shale. Much of the clastic material is volcanogenic, presumably from volcanic arcs to the E.|
20268|Winton Formation|70823|5|Briefly described|p25-p27, p41, p43-p45, p78|Cenomanian|Cenomanian|Eromanga Basin. Up to 1200m thick. Deposited in a non-marine to marginal marine environment. Hosts lignite source rock. Age range derived from Bryan et al., 2012 and Tucker et al., 2013.|c. 99-93 Ma|||Overlies the Mackunda and Oodnadatta Formations. Overlain by the Mount Howe Sandstone.||
20268|Winton Formation|70824|5|Briefly described|p9|Cretaceous|Cretaceous|Eromanga Basin. Hosts lignite.||||Overlies the Mackunda Formation.||
20268|Winton Formation|70836|6|Mentioned|p474, 482|Turonian|Albian|Eromanga Basin. Preserves a rich and diverse vertebrate fauna including the only named Australian megaraptoran, Australovenator.|c.103-92 Ma (Tucker et al., 2013).|||||
20268|Winton Formation|70938|5|Briefly described|p816|Late Cretaceous|Late Cretaceous|Extensive, fluvial deposits. Paleocurrents and detrital zircons indicate a NE Queensland source.|||||Contains extensive labile volcanic detritus.|
20268|Winton Formation|71251|4|Described|p8, p11-13, p15, p17-20, p29, p49|||Senior (1971). Eromanga Basin. 47m total thickness in Eulo 1 borehole. Non-marine deposits. Natural gamma, magnetic susceptibility data tabulated. Conductivity data/diagram.||||Overlies Coreena Member (Wallumbilla Formation).|Dark grey siltstone, weathering to white, finely-bedded mudstone and claystone mottled by goethite and hematite, with gypsum prevalent throughout the top of the unit; capped by a 5m-thick duricrust of porcellanite (white silicified mudstone).|
20268|Winton Formation|71321|5|Briefly described|p15,65|Cenomanian|Cenomanian|Of Eromanga Basin. Regressivee depositional package following peak early Cretaceous marine transgression; fluvio-lacustrine siltstone and sandstones and locally coal-bearing.||||Overlain by Mount Howie Formation. Underlain by Mackunda Formation.|Fluvio-lacustrine siltstone and sandstones and locally coal-bearing.|
20268|Winton Formation|71342|3|Fully described|Ch 1 p6, Ch 1 p19, Ch3 p4, Ch4 p6|Cenomanian|Albian|Eromanga Basin. Originally termed the Winton Series by Dunstan (1916) without formal definition. The name was changed to Winton Formation and a type section was designated in Queensland by Whitehouse (1955). The type section is described as "blue shales and sandstones with intercalated coal seams met within the bores in and around Winton". Hosts a major confined aquifer. Lithology, sedimentology, distribution and outcrop characteristics are discussed. This unit is generally thicker than 400m in the Cooper region and has a maximum thickness of 1100m in the northern Patchawarra Trough. Age derived on the basis of palynology and macrofossil assemblage. Spore-pollen zone is given in Ch5 p57. See also Ch4 p8, Ch4 p25, Ch5 p27-p28, Ch5 p30, Ch5 p33, Ch5 p56-p57, Ch5 p126-p127, Ch5 p130, Ch6 p9-p10, Ch7 p3, Ch7 p9, Ch7 p13, Ch9 p4-p5, Ch9 p10-p11, Ch9 p18, Ch10 p3.||||Conformably overlies the Mackunda Formation. Overlies the Oodnadatta Formation. Unconformably overlain by the Eyre Formation.|Interbedded fine to coarse-grained sandstone, carbonaceous and pyritic shale, siltstone and coal seams with intraclast conglomerates.|
20268|Winton Formation|71601|6|Mentioned|p120, p121|Turonian|Albian|Central west Qld. Ankylosaurian remains have been identified.||||||
20268|Winton Formation|71855|6|Mentioned|p20, p27, p30|||||||||
20268|Winton Formation|71863|5|Briefly described|p5|Cenomanian|Albian|Eromanga Basin.||||Overlies the Allaru Mudstone and the Mackunda Formation.||
20268|Winton Formation|71864|4|Described|p8, p10, p13-p14, p16-p20, p26|||Intersected in GSQ Eulo 2 borehole between 2-23m depth. Originally mapped in the area by Senior (1971). Described in Senior, 1971 as non-marine fine sandstone and siltstone. Gamma log characteristics and magnetic susceptibility is provided.||||Overlies the Wallumbilla Formation.|Mottled, deeply weathered mudstone regolith with gypsum flakes throughout, blue siltstone and thin quartzose and lithic gravel bands.|
20268|Winton Formation|72297|5|Briefly described|p700, p724, p751, p758|Cretaceous|Cretaceous|Eromanga Basin. All coal seams are of uneconomic thickness and of poor quality. CSG exploration results not encouraging. Has a large kaolin deposit 35km W of Winton (70-80% kaolinite). Hosts QLD's opal fields within a 300km wide, NNW-trending belt from Hungerford to Kyuna.|||||White mudstone. Contains seams of subhydrous lignite - sub-bituminous black coal.|
20268|Winton Formation|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin. Confined aquifers, generally producing non-flowing artesian water bores.||Rolling Downs Group.||Overlies Rumbalara Shale, Mackunda FZ.||
20268|Winton Formation|72456|5|Briefly described|Map Legend|Cretaceous|Cretaceous|Marree 1:250k map sheet.|||||Shale, siltstone, sandstone that is non-marine with minor coal horizons.|
20268|Winton Formation|72915|6|Mentioned|p16|||Absent in the area of the Congararra 1 borehole (after Hawke and Cramsie, 1984).||||||
20268|Winton Formation|73106|5|Briefly described|Map legend.|Cretaceous|Cretaceous||||||Shale, siltstone, sandstone. Non-marine, minor coal horizons.|
20268|Winton Formation|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin.||||||
20268|Winton Formation|73249|6|Mentioned|p319|Cretaceous|Cretaceous|Eromanga Basin.||||Overlies the Mackunda Formation.||
20268|Winton Formation|73251|6|Mentioned|p62|Late Cretaceous|Late Cretaceous|Eromanga Basin. Non-marine to marginal marine.||||Underlain by Mackunda Formation and Oodnadatta Formation.||
20268|Winton Formation|73281|6|Mentioned|Appendix (DIP)|||See DIP034_Petroleumdata.xlsx and DIP034_Welldata.xlsx.||||||
20268|Winton Formation|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||||Underlain by Oodnadatta Formation. Equivalent to Mackunda Formation.||
20268|Winton Formation|73393|6|Mentioned|p20||||||||Includes volcaniclastic sedimentary deposits.|
20268|Winton Formation|73479|5|Briefly described|p155, p156 Fig.2, p159-160|Cretaceous|Cretaceous|Eromanga Basin. Fluvial-lacustrine depositional environment. Significantly eroded following exhumation (late Cretaceous).|ca 97-93 Ma|||Overlies Oodnadatta Formation, unconformably underlies Eyre Formation||
20272|Winton Limestone Member|37987|6|Mentioned|p224|||||||||
20282|Wiradjuri Volcanics|29648|6|Mentioned|p20|||||||||
20282|Wiradjuri Volcanics|40328|6|Mentioned|p45|||||||||
20284|Wiragulla beds|31706|6|Mentioned|p651|||L.Carb. correlation chart||||||
20289|Wire Gully Limestone Member|23214|3|Fully described|p105|Llandovery|Llandovery|Of Bagdad Formation. Consists mainly of thinly to massively bedded reddish limestone, passes westward to a thick bedded limestone conglomerate.  Maximum thickness: 35m.||||||
20289|Wire Gully Limestone Member|35258|4|Described|p113|||See also Table 1.||||||
20289|Wire Gully Limestone Member|63278|6|Mentioned|p155|||Shallow-water limestones.||||||07-FEB-11
20289|Wire Gully Limestone Member|63290|6|Mentioned|p401 Fig. 5(d)|Llandovery|Llandovery|Of Ashburnia Group.||||||
20289|Wire Gully Limestone Member|70684|5|Briefly described|p50 Fig.24, p51-52|Early Silurian|Early Silurian|Molong Volcanic Belt.  Early Llandovery conodonts.||Bagdad Formation.|||Shallow-water limestones.|
20289|Wire Gully Limestone Member|71091|5|Briefly described|p143|Early Silurian|Early Silurian|Contains early Llandovery conodonts.||Basal Ashburnia Group.||Overlies Angullong Formation.|Shallow-water limestones.|
20294|Wirrabilla Formation|22857|5|Briefly described|p456 App.1, Tb.A1.6|Devonian|Silurian|Of the Toongi Group. Sandstone and siltstone. Max. thickness: 900m. Geological Province: Cowra Trough.||||||
20294|Wirrabilla Formation|23043|5|Briefly described|Map Legend|Pridoli|Pridoli|of Toongi Group.||||||
20294|Wirrabilla Formation|23170|2|Defined|p120|Late Silurian|Late Silurian|of Toongi Group.||||||
20294|Wirrabilla Formation|32045|6|Mentioned|Map legend|Devonian|Silurian|Siluro-Devonian||||||
20294|Wirrabilla Formation|32485|6|Mentioned|Map legend|Devonian|Silurian|Sil.-Dev.||||||
20294|Wirrabilla Formation|40328|4|Described|p132|||||||||
20294|Wirrabilla Formation|43476|14|Not recorded|Map Legend|Devonian|Silurian|(Provisional Edition)||||||
20294|Wirrabilla Formation|50590|5|Briefly described|Map Legend|Silurian|Silurian|Of the Toongi Group. Sandstone and siltstone.||||||
20294|Wirrabilla Formation|68003|5|Briefly described|p24 Fig.3-e, p144. |Ludlow|Ludlow|Lachlan Fold Belt, Brigalow Belt South Bioregion.||Unit in Toongi Group.||Overlies Toongi Hall Tuff. Is overlain by Whychetella Formation.|Lithic sandstone, minor conglomerate, hornfels.|
20300|Wirrealpa Limestone|22631|6|Mentioned|p178|Cambrian|Cambrian|||||||
20300|Wirrealpa Limestone|22766|5|Briefly described|Fig.2 p561, p562|Early Cambrian|Early Cambrian|||||||
20300|Wirrealpa Limestone|22772|5|Briefly described|Table 13.1|Middle Cambrian|Early Cambrian|||||||
20300|Wirrealpa Limestone|22857|5|Briefly described|Tb 13.1 (insert p70-71), p90 Fig. 14.7B|Middle Cambrian|Early Cambrian|Of Lake Frome Group. Age: ~509Ma. Geological Province: Arrowie Basin.||||||
20300|Wirrealpa Limestone|22858|6|Mentioned|p92,Fig14.7bp90-1|||||||||
20300|Wirrealpa Limestone|23155|6|Mentioned|p9|||Equivalent to the Kalladeina Formation (eastern Warburton Basin).||||||
20300|Wirrealpa Limestone|23250|5|Briefly described|p1124 Fig.2||Early Cambrian|Age: Stage 4 of Early Cambrian. Correlate of Yarrawurta Shale.||||||
20300|Wirrealpa Limestone|23818|5|Briefly described|p51 Fig.16|Cambrian|Cambrian|||||||18-APR-05
20300|Wirrealpa Limestone|23981|6|Mentioned|p8-9 Fig. 4|Toyonian|Toyonian|Overlies Billy Creek Formation; underlies Lake Frome Group. Geological Province: Arrowie Basin.||||||04-FEB-08
20300|Wirrealpa Limestone|24072|5|Briefly described|p369 Fig.1|Cambrian|Cambrian|Geological Province: Great Artesian Basin.||||||
20300|Wirrealpa Limestone|24138|5|Briefly described|p32|Cambrian|Cambrian|Marine. Contains abundant trilobites, brachiopods, sponge spicules and algae. Geological Province: Adelaide Geosyncline.||||||
20300|Wirrealpa Limestone|24176|5|Briefly described| p17|Middle Cambrian|Middle Cambrian|Treated as undifferentiated from Aroona Creek Limestone (COPLEY) in these Notes (p23 Tb. 1) and referred to as Wirrealpa Limestone-Aroona Creek Limestone (undifferentiated).  Overlain by Moodlatana Fm.(Lake Frome Gp.)||||||
20300|Wirrealpa Limestone|24465|5|Briefly described|p345 Fig.2|Middle Cambrian|Early Cambrian|Geological Province: Arrowie Basin.||||||19-JAN-05
20300|Wirrealpa Limestone|29929|6|Mentioned|Fig.4|||||||||
20300|Wirrealpa Limestone|30051|6|Mentioned|Fig.12|||See also p28. Middle Cambrian age.||||||19-DEC-06
20300|Wirrealpa Limestone|30176|6|Mentioned|Map legend|Middle Cambrian|Middle Cambrian|||||||
20300|Wirrealpa Limestone|30511|6|Mentioned|p47|||||||||
20300|Wirrealpa Limestone|30544|6|Mentioned|p49|||||||||
20300|Wirrealpa Limestone|30801|6|Mentioned|p5|||Table p5-6.||||||19-DEC-06
20300|Wirrealpa Limestone|30802|5|Briefly described|p11|||Lower Middle Cambrian.||||||
20300|Wirrealpa Limestone|30807|6|Mentioned|p102|||Suggested map symbol||||||
20300|Wirrealpa Limestone|31539|6|Mentioned|Fig. 28|||||||||
20300|Wirrealpa Limestone|31706|6|Mentioned|p633|||Cambrian correlation chart||||||
20300|Wirrealpa Limestone|31797|6|Mentioned|Fig. 2|||M.Camb. of Lake Frome Group.||||||19-DEC-06
20300|Wirrealpa Limestone|32669|6|Mentioned|p523|||M.Camb.||||||
20300|Wirrealpa Limestone|33332|6|Mentioned|p15|||M.Cambrian.||||||
20300|Wirrealpa Limestone|33474|6|Mentioned|Fig.3|||||||||
20300|Wirrealpa Limestone|33932|6|Mentioned|p14|||||||||
20300|Wirrealpa Limestone|33934|6|Mentioned|Fig.2|||M - U Camb.||||||
20300|Wirrealpa Limestone|33972|4|Described|p14|||Mention p13.||||||19-DEC-06
20300|Wirrealpa Limestone|33973|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|34269|6|Mentioned|Table 1|||||||||
20300|Wirrealpa Limestone|34535|6|Mentioned|Fig.16|||Cambrian||||||
20300|Wirrealpa Limestone|34612|6|Mentioned|Fig.33|||Cambrian||||||
20300|Wirrealpa Limestone|34812|6|Mentioned|Table 9|||||||||
20300|Wirrealpa Limestone|35255|6|Mentioned|Fig.8|||||||||
20300|Wirrealpa Limestone|35798|6|Mentioned|Fig.4|||Correlation of lower units in Desert Syncline drill holes.||||||
20300|Wirrealpa Limestone|35835|6|Mentioned|p207|||||||||
20300|Wirrealpa Limestone|35954|6|Mentioned|p1230|||See also Fig.2.||||||
20300|Wirrealpa Limestone|36137|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|36198|6|Mentioned|p249|||See also Fig.I.2||||||
20300|Wirrealpa Limestone|36495|6|Mentioned|p127|||||||||
20300|Wirrealpa Limestone|36525|6|Mentioned|Fig.4|||See also Fig.5.||||||
20300|Wirrealpa Limestone|37802|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|38004|6|Mentioned|Table 1|||||||||
20300|Wirrealpa Limestone|38068|6|Mentioned|p69|||See also Fig.4.||||||
20300|Wirrealpa Limestone|39344|6|Mentioned|Map legend|Cambrian|Cambrian|||||||
20300|Wirrealpa Limestone|39352|6|Mentioned|Map legend|Late Cambrian|Middle Cambrian|Middle to Late Cambrian||||||
20300|Wirrealpa Limestone|40455|6|Mentioned|Fig.2|||||||||
20300|Wirrealpa Limestone|40852|6|Mentioned|p33|||||||||
20300|Wirrealpa Limestone|40856|6|Mentioned|Fig.23.6|||||||||
20300|Wirrealpa Limestone|40914|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
20300|Wirrealpa Limestone|41401|6|Mentioned|p32|||||||||
20300|Wirrealpa Limestone|41496|5|Briefly described|Fig.1|||||||||
20300|Wirrealpa Limestone|41526|6|Mentioned|p60|||||||||
20300|Wirrealpa Limestone|42090|6|Mentioned|p26|||||||||
20300|Wirrealpa Limestone|42141|6|Mentioned|Table 2 P571|||||||||
20300|Wirrealpa Limestone|42192|6|Mentioned|p14|||||||||
20300|Wirrealpa Limestone|42225|6|Mentioned|p223|||||||||
20300|Wirrealpa Limestone|42266|6|Mentioned|Fig.2 P292|||||||||
20300|Wirrealpa Limestone|42269|6|Mentioned|p337|||||||||
20300|Wirrealpa Limestone|42272|6|Mentioned|p414|||||||||
20300|Wirrealpa Limestone|42357|5|Briefly described|p10|||||||||
20300|Wirrealpa Limestone|42440|4|Described|p601, p611|||||||||
20300|Wirrealpa Limestone|42573|5|Briefly described|Fig.1 P190|||||||||
20300|Wirrealpa Limestone|43011|6|Mentioned|Table 2,p12|||||||||
20300|Wirrealpa Limestone|43053|5|Briefly described|Map Legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds, peritidal to marine limestone.||||||25-MAY-05
20300|Wirrealpa Limestone|43258|5|Briefly described|Map Legend||Cambrian|||||||
20300|Wirrealpa Limestone|43298|6|Mentioned|Map Legend||Cambrian|||||||
20300|Wirrealpa Limestone|43781|6|Mentioned|p4||Middle Cambrian|||||||
20300|Wirrealpa Limestone|43845|6|Mentioned|Fig 4 p44|||||||||12-JUL-16
20300|Wirrealpa Limestone|44040|14|Not recorded|p38|||||||||
20300|Wirrealpa Limestone|44093|5|Briefly described|p138 App. 1|Middle Cambrian|Early Cambrian|Geological Province: Adelaide Fold Belt.||||||
20300|Wirrealpa Limestone|44133|5|Briefly described|p4 Fig. 7.2, 5, 17, 27, 29 Fig. 7.13|Early Cambrian|Early Cambrian|Geological Province: Arrowie Basin. Maximum Thickness: 135m.||||||
20300|Wirrealpa Limestone|45055|6|Mentioned|p6|||Location||||||
20300|Wirrealpa Limestone|45102|6|Mentioned|p48|||||||||
20300|Wirrealpa Limestone|45155|6|Mentioned|Fig.8|||||||||
20300|Wirrealpa Limestone|60418|6|Mentioned|p134 Fig.1|||||||||
20300|Wirrealpa Limestone|60419|5|Briefly described|p18|Middle Cambrian|Middle Cambrian|Geological Province: Adelaide Rift.  Contains fauna of Ordian age.||||||
20300|Wirrealpa Limestone|60889|5|Briefly described|p245 Fig.2, p247-9, p251-4|Early Cambrian|Early Cambrian|Shallow marine carbonates. Thickness: 120 m. Arrowie Basin. Primary dilling target (Moorowie-1).|>512 Ma.|||Overlies Billy Creek Formation. Is overlain (unconformably?) by Moodlatana Formation (basal Lake Frome Group).|Carbonates. Widespread; a potential reservoir-seal couplet where oolitic reservoir is overlain by micrite seal.|
20300|Wirrealpa Limestone|60953|5|Briefly described|Map Legend|Cambrian|Cambrian|Geological Province: Arrowie Basin.||||||
20300|Wirrealpa Limestone|60959|5|Briefly described|Map Legend|Early Cambrian|Early Cambrian|Of the Lake Frome Group. Lime mudstone, nodular limestone in a calcareous silty matrix.||||||
20300|Wirrealpa Limestone|60990|5|Briefly described|p83 Fig.2, p85 |Toyonian|Toyonian|Flinders Ranges. Faunal links with Antarctica.||||||
20300|Wirrealpa Limestone|61108|5|Briefly described|map legend|Cambrian|Cambrian|Shallow marine to terrestrial redbeds; peritidal to marine limestone. Geological Province: Arrowie Basin.||||||03-JUN-05
20300|Wirrealpa Limestone|62592|5|Briefly described|p50 Table 5.1, p59.|Early Cambrian|Early Cambrian|Adelaide Geosyncline.||Unit in Moralana Supergroup.||Overlies Billy Creek Formation. Is overlain by Lake Frome Group.|Fossiliferous limestone.|
20300|Wirrealpa Limestone|62784|5|Briefly described|p8 Fig.1|Cambrian|Cambrian|Arrowie Basin. Overlies Billy Creek Formation and is overlain by Moodlatana Formation of the Lake Frome Group.||||||
20300|Wirrealpa Limestone|62787|5|Briefly described|p82, p82 Fig. 3|Early Cambrian|Neoproterozoic|Geological Province: Arrowie Basin (SA).||||||07-FEB-11
20300|Wirrealpa Limestone|63447|6|Mentioned|p963 Fig.2 |Early Cambrian|Early Cambrian|Arrowie Basin||||Overlies Billy Creek Formation. Aroona Creek Limestone shown as lateral equivalent.||
20300|Wirrealpa Limestone|63489|5|Briefly described|Map legend|Middle Cambrian|Early Cambrian|Marine limestone.||||||10-SEP-07
20300|Wirrealpa Limestone|63569|4|Described|pp116-120, pp122-123, p125 Fig. 6|Early Cambrian|Early Cambrian|Arrowie Basin, Adelaide Geosyncline. 105-140 m thick transgressive-regressive carbonate sequence with lagoonal and ooid bank megafacies. Abundantly fossiliferous.||||Conformably overlies Billy Creek Formation. Is conformably overlain by Moodlatana Formation.|Lime mudstone; nodular limestone with calcareous silty matrix; skeletal, peloidal and oolitic beds; stromatolite and thrombolite bioherms; micrite; siltstone.|
20300|Wirrealpa Limestone|64829|5|Briefly described|p1084-5 Figs.1,  2|Early Cambrian|Early Cambrian|Unit discussed in the context of soilscapes and palaeosols. Basal section contains the trilobite, Redlichia guizhouensis.||||||07-FEB-11
20300|Wirrealpa Limestone|65313|5|Briefly described|p577, p576 Fig. 5,  p578 Fig. 6|Middle Cambrian|Middle Cambrian|Trilobites in this unit at Ten Mile Creek section eastern Arrowie Basin, correlated with 511.5 Ma R. gulzhouensis trilobite zone. Shown as Arcadian age in Fig. 6||||Underlies Lake Frome Group.||26-MAR-12
20300|Wirrealpa Limestone|65375|5|Briefly described|p33.|Early Cambrian|Early Cambrian|||||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation.||
20300|Wirrealpa Limestone|65625|5|Briefly described|p103 Fig.2|Middle Cambrian|Middle Cambrian|Lake Frome area.||||Overlies Billy Creek Formation. Underlies Lake Frome Group.||18-FEB-11
20300|Wirrealpa Limestone|65686|5|Briefly described|p411, 413, 415, p409 Fig 2|Early Cambrian|Early Cambrian|Arrowie Basin. Contains the youngest archaeocyath in Australia. 120m thick.||||||07-MAY-12
20300|Wirrealpa Limestone|65892|4|Described|p9 Fig.4, p10,p12, p38-39, p41, p45-46  |Early Cambrian|Early Cambrian|Arrowie Basin. 120m thick. Shallow marine carbonates. Contains Redlichia guizhouensis and the youngest archaeocyath fauna in Australia.|c.520 Ma.|||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation. Equivalent to Aroona Creek Limestone.|Grey limestone; fossiliferous.|
20300|Wirrealpa Limestone|65925|5|Briefly described|p14 Fig.2.2, Appendix 2.|Early Cambrian|Early Cambrian||||||Medium grey micritic limestone; basal dolomite.|
20300|Wirrealpa Limestone|66518|6|Mentioned|p19 Fig.4.|Cambrian|Cambrian|Arrowie Basin.||||Overlies Billy Creek Formation. Is overlain by Moodlatana Formation.||
20300|Wirrealpa Limestone|67536|5|Briefly described|Map Legend|Stage 2|Stage 2||ca. 523 +/- 2 Ma||||Shallow marine to terrestrial redbeds, peritidal to marine limestone|
20300|Wirrealpa Limestone|67870|6|Mentioned|p5, p9, p23-25|Cambrian|Cambrian|Arrowie Basin. Appears as Wirrealpa Formation on p9; and as Wirrealpa-Lake Frome Group on p25.||||||
20300|Wirrealpa Limestone|68030|5|Briefly described|p239|Cambrian|Cambrian|Flinders Ranges.||||Overlain by Lake Frome Group. Underlain unconformably by Billy Creek Formation.||
20300|Wirrealpa Limestone|68735|4|Described|p231, pp233-239|Early Cambrian|Early Cambrian|Arrowie Basin. Described by Youngs (1977). ~ 120 m thick. Contains abundant trilobites, brachiopods, and small shelly fossils. Also described are cyanobacterial-archaeocyathan-radio-cyathan bioherms (Kruse 1991): youngest archaeocyaths in Australia.||||Overlies Billy Creek Formation. Overlain by the Lake Frome Group. Is equivalent to Aroona Creek Limestone.|Comprises shallow marine carbonates at the top and bottom with slightly deeper water shales in the middle.|10-APR-17
20300|Wirrealpa Limestone|68993|6|Mentioned|p544 Fig.1|Early Cambrian|Early Cambrian|Arrowie Basin.||||||
20300|Wirrealpa Limestone|69570|6|Mentioned|p421 fig 1|Cambrian|Cambrian|Arrowie Syncline, Flinder Ranges.||||||
20300|Wirrealpa Limestone|69982|5|Briefly described|p19|||Arrowie Basin. Older than Templetonian-Floran, and younger than Botomian: age from surrounding units.||||May correlate with Diamond Bog Dolomite (Warburton Basin).||
20300|Wirrealpa Limestone|70752|6|Mentioned|p133|||Brachiopod fossil briefly discussed.||||||
20300|Wirrealpa Limestone|70833|6|Mentioned|p200|||Of Arrowie Basin.||||Underlain by Billy Creek Formation.||
20300|Wirrealpa Limestone|70835|6|Mentioned|p335|Cambrian|Cambrian|Arrowie Basin, Flinders Ranges.||||||
20300|Wirrealpa Limestone|72449|5|Briefly described|p1, p2 Map Legend|Cambrian|Cambrian|Shown as part of diapir formation diagram, p1.||||Overlies Billy Creek Formation and underlies Moodlatana Formation|Wavy bedded to nodular limestone in a silty matrix. Algal mats and stromatolites are common; fossil trilobites and brachiopods occuring.|
20300|Wirrealpa Limestone|73251|6|Mentioned|p36|Cambrian|Cambrian|Arrowie Basin, Moorowie and Yalkalpo Sub-basins. Thermally late to post-mature.||||Underlain by Billy Creek Formation. Overlain by Moodlatana Formation (Lake Frome Group).||
20300|Wirrealpa Limestone|73255|6|Mentioned|p534 Fig.2|early Cambrian|early Cambrian|Contains Redlichia guizhouensis trilobite fossils.||||Overlies the Billy Creek Formation, underlies the Moodlatana Formation.|Carbonate rocks.|
20334|Wittingham Coal Measures|22601|6|Mentioned|412|Permian|Permian|Geol province Sydney Basin||||||
20334|Wittingham Coal Measures|22857|5|Briefly described|p524 App.1 Tb.A1.9|Late Permian|Late Permian|Of the Singleton Supergroup. Contains Denham Formation, Jerrys Plain Subgroup and Vane Subgroup. Equivalent to Gloucester Coal Measures. Geological Province: Sydney Basin.||||||
20334|Wittingham Coal Measures|22969|6|Mentioned|p 22|||||||||
20334|Wittingham Coal Measures|23540|5|Briefly described|p 417|||||||||
20334|Wittingham Coal Measures|24079|5|Briefly described|p433 Fig. 6|Permian|Permian|Of Singleton Super Group. Geological Province: Sydney Basin.||||||
20334|Wittingham Coal Measures|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Overlying Unit: Wollombi Coal Measures. Geological Province: Sydney Basin||||||
20334|Wittingham Coal Measures|24423|5|Briefly described|p230 Fig.3|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||
20334|Wittingham Coal Measures|29942|3|Fully described|p16|||||||||
20334|Wittingham Coal Measures|31375|6|Mentioned|p3|||Stratigraphy||||||
20334|Wittingham Coal Measures|31649|6|Mentioned|p59|||||||||
20334|Wittingham Coal Measures|33334|6|Mentioned|p8|||Permian||||||
20334|Wittingham Coal Measures|35767|6|Mentioned|p8|||||||||
20334|Wittingham Coal Measures|36042|6|Mentioned|Table 1|||||||||
20334|Wittingham Coal Measures|36283|6|Mentioned|p100|||||||||
20334|Wittingham Coal Measures|37082|6|Mentioned|p160|||See also P161.||||||
20334|Wittingham Coal Measures|37086|6|Mentioned|p181|||||||||
20334|Wittingham Coal Measures|37087|4|Described|p199|||||||||
20334|Wittingham Coal Measures|37337|6|Mentioned|p19|||||||||
20334|Wittingham Coal Measures|37773|6|Mentioned|Table 2|||||||||
20334|Wittingham Coal Measures|39287|6|Mentioned|Fig. 2.5|||||||||
20334|Wittingham Coal Measures|39288|6|Mentioned|p64|||||||||
20334|Wittingham Coal Measures|39292|6|Mentioned|p101|||||||||
20334|Wittingham Coal Measures|39307|6|Mentioned|Table 22.1|||||||||
20334|Wittingham Coal Measures|39346|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20334|Wittingham Coal Measures|39693|6|Mentioned|p18|||||||||
20334|Wittingham Coal Measures|39830|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20334|Wittingham Coal Measures|40087|6|Mentioned|p234|||||||||
20334|Wittingham Coal Measures|40166|6|Mentioned|p343|||||||||
20334|Wittingham Coal Measures|40222|6|Mentioned|Figure|||||||||
20334|Wittingham Coal Measures|40224|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20334|Wittingham Coal Measures|40256|6|Mentioned|p304|||||||||
20334|Wittingham Coal Measures|40321|6|Mentioned|Fig.3|||||||||
20334|Wittingham Coal Measures|40330|6|Mentioned|Fig.4|||||||||
20334|Wittingham Coal Measures|40805|6|Mentioned|Fig.2|||||||||
20334|Wittingham Coal Measures|40883|6|Mentioned|p15|||||||||
20334|Wittingham Coal Measures|41010|4|Described|p12|||||||||
20334|Wittingham Coal Measures|41054|6|Mentioned|p156|||||||||
20334|Wittingham Coal Measures|41226|6|Mentioned|Table 1|||||||||
20334|Wittingham Coal Measures|41290|6|Mentioned|Fig.8|||||||||
20334|Wittingham Coal Measures|41604|6|Mentioned|p1|||||||||
20334|Wittingham Coal Measures|41834|6|Mentioned|p590|||||||||
20334|Wittingham Coal Measures|41902|5|Briefly described|p5 Table 1|||||||||
20334|Wittingham Coal Measures|41903|6|Mentioned|Map legend|Late Permian||||||||
20334|Wittingham Coal Measures|42078|6|Mentioned|p4|||||||||
20334|Wittingham Coal Measures|42182|5|Briefly described|p299|||||||||
20334|Wittingham Coal Measures|42526|6|Mentioned|Map legend|||||||||
20334|Wittingham Coal Measures|42648|5|Briefly described|p36, p37|||||||||
20334|Wittingham Coal Measures|42680|6|Mentioned|p19|||||||||
20334|Wittingham Coal Measures|42767|5|Briefly described|Fig.5|||||||||
20334|Wittingham Coal Measures|42780|5|Briefly described|Fig.2 P412|||||||||
20334|Wittingham Coal Measures|42916|5|Briefly described|Table 1||Late Permian|||||||
20334|Wittingham Coal Measures|42944|6|Mentioned|p26|||||||||
20334|Wittingham Coal Measures|42945|6|Mentioned|p27|||||||||
20334|Wittingham Coal Measures|42965|6|Mentioned|p38|||||||||
20334|Wittingham Coal Measures|43194|5|Briefly described|p106, p128, p129 Tb. 8.3|Late Permian|Late Permian|Of Singleton Supergroup, Hunter Coalfield, Sydney Basin. Contains Jerrys Plains and Vane Subgroups, Denman Formation, and Archerfield Sandstone. Together with Wollombi Coal Measures, correlates with Black Jack Formation, Gunnedah Basin.||||||
20334|Wittingham Coal Measures|43257|5|Briefly described|Map Legend||Late Permian|Of Singleton Supergroup.||||||14-MAR-07
20334|Wittingham Coal Measures|43752|5|Briefly described|p617||Late Permian|||||||
20334|Wittingham Coal Measures|44093|6|Mentioned|p64 Photo 3|||Geological Province: Sydney Basin.||||||30-MAR-05
20334|Wittingham Coal Measures|44244|4|Described|p234|Late Permian|Late Permian|Of the Singleton Supergroup.  Overlies the Mulbring Sltst; underlies the Wollombi C.M.  Includes the Denman Fm., Jerrys Plains Subgp., Archerfield Sst., Vane Subgp., Saltwater Creek Fm.  Max. thick: 1200m.  Geological Province: Sydney Basin.||||||14-MAR-07
20334|Wittingham Coal Measures|45090|6|Mentioned|p7|||Time correlation chart||||||
20334|Wittingham Coal Measures|50268|5|Briefly described|Map Legend|Tatarian|Tatarian|Geological Province: Sydney Basin.  Includes: Jerrys Plains Subgroup, Archerfield Sandstone, Vane Subgroup, Saltwater Creek Formation.  Overlies: Maitland Group.||||||
20334|Wittingham Coal Measures|60281|5|Briefly described|p59, p62|Late Permian|Late Permian|Overlie Mulbring Formation in western part of basin.  Equivalent of Tomago Coal Measures.  Geological Province: Sydney Basin.||||||
20334|Wittingham Coal Measures|60299|6|Mentioned|p208|||Geological Province: Sydney Basin||||||
20334|Wittingham Coal Measures|61315|5|Briefly described|p167, Table SY1|Late Permian|Late Permian|Subdivided into: Vane and Jerrys Plain Subgroups. Geological Province: Sydney Basin/Hunter Valley area.||||||
20334|Wittingham Coal Measures|61529|5|Briefly described|p853, p854 Fig. 1b|Late Permian|Late Permian|Includes Jerrys Plains and Vane Subgroups and Saltwater Creek Formation. Overlies Maitland Group; overlain by Wollombi Coal Measures. Geological Province: Sydney Basin.||||||03-FEB-06
20334|Wittingham Coal Measures|61612|6|Mentioned|p273, p270 Fig. 1|Late Permian|Late Permian|Geological Province: Sydney Basin.||||||17-MAR-09
20334|Wittingham Coal Measures|61770|6|Mentioned|p111|||||||||
20334|Wittingham Coal Measures|62033|5|Briefly described|p24, p25 (Table)|||Now part of Singleton Supergroup, after ratification by the Coalfield Geology Council in 2004, of the resolution that it be included together with Newcastle C.M. and Watts Sandstone in the supergroup. Includes Denman Fm. Geol. Prov: Sydney Basin.||||||14-MAR-07
20334|Wittingham Coal Measures|65758|5|Briefly described|p98|Permian|Permian|Sydney Basin. Shale and conglomerate, overlain by the Narrabeen Group||||||
20334|Wittingham Coal Measures|66891|5|Briefly described|p179, p190, p191.|Middle Permian|Middle Permian|Lies 300-400 m below the surface of Wybong Creek catchment. Saline groundwater of Big Flat Creek, and through the Mount Ogilvie Fault and into the Hunter River, have been related to groundwater discharge from this unit. Has salt efflorescences.||||||
20334|Wittingham Coal Measures|68003|5|Briefly described|p38 Fig.3-j, p41.|Late Permian|Late Permian|Hunter Coalfield (northern Sydney Basin), Brigalow Belt South Bioregion. Prograding fluvio-deltaic system, fed from the New England region.||Lower unit of Singleton Supergroup.|Includes Vane Subgroup; Archerfield Sandstone; Jerrys Plains Subgroup; Denman Formation, Saltwater Creek Formation and Watts Sandstone.|Overlies Mulbring Siltstone. Is overlain by Wollombi Coal Measures.||
20334|Wittingham Coal Measures|68004|5|Briefly described|p23 Table 1, pp51-52, p156.|Late Permian|Late Permian|Hunter Coalfield. Equivalent to Tomago Coal Measures and much of Illawarra Coal Measures. Includes the major coal-producing units in New South Wales. About 1200 m thick.||Lower unit in Singleton Supergroup.|Includes Vane and Jerrys Plains Subgroups, Archerfield Sandstone and Denman Formation.|Overlies Maitland Group. Is overlain by Wollombi Coal Measures.||
20334|Wittingham Coal Measures|68006|5|Briefly described|p99, p101.|Late Permian|Late Permian|Murrurundi Trough. Equivalent to the Black Jack Formation. The Bayswater Seam is equivalent to the Hoskissons Seam of the Gunnedah Basin. Of interest for coal seam methane potential: exploration drilling and regional mapping in the 1990s.|||Includes Bayswater Seam.|||
20334|Wittingham Coal Measures|69297|6|Mentioned|p499, p503|Late Permian|Middle Permian|Sydney Basin. Deposited in a fluvial-deltaic environment. Has some potential as a gas or petroleum source rock.|||||Sandstones, siltstones and coals.|
20334|Wittingham Coal Measures|69683|5|Briefly described|p410 Fig.1, p411 Fig.2, p414-415|Late Permian|Late Permian|See also p420 Fig.5, p422 Tb.4. All rocks of this unit are predicted to have maturity for (coal seam) gas generation.||Unit in Singleton Supergroup.|Includes Vane and Jerrys Plains Subgroups; Saltwater Creek and Denman Formations; Archerfield Sandstone.||Coal seams, tuff, claystone, siltstone, sandstone, conglomerate.|
20334|Wittingham Coal Measures|70791|5|Briefly described|p277|Permian|Permian|Hunter Coalfield.||Singleton Supergroup.|Vane, Jerrys Plains Subgroups; Archerfield, Watts Sandstones; Denman Formation.|||
20334|Wittingham Coal Measures|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Northern Sydney Basin.|||Includes Fairford Formation.|||
20334|Wittingham Coal Measures|70878|5|Briefly described|p710, p712, p723|Permian|Permian|Hunter Valley. 455.71m thick in Amoco Wybong 1 well.|||Althorpe, Fairford Formations.|Is overlain by Newcastle Coal Measures.||
20334|Wittingham Coal Measures|71701|5|Briefly described|p169|||Sydney Basin.||||Overlies the Greta Coal Measures.||
20334|Wittingham Coal Measures|73304|6|Mentioned|p66-67, p75, p78-79|||||Singleton Supergroup||||
20334|Wittingham Coal Measures|73625|6|Mentioned|p2|Permian|Permian|Hunter coalfield, Sydney Basin.|||Archerfield, Bulga Sandstones; Foybrook Formation.|Overlies Mulbring Siltstone. Is overlain by Denman Formation.||
20347|Wogarda Argillite|22750|5|Briefly described|Table 1 p 229||Early Devonian|Tamworth Group||||||
20347|Wogarda Argillite|22857|5|Briefly described|p484 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Of the Tamworth Group. Siltstone, minor arenite. Max. thickness: 400m. Geological Province: Tamworth Forearc Basin.||||||
20347|Wogarda Argillite|23185|6|Mentioned|Fig5p161|Emsian|Emsian|||||||
20347|Wogarda Argillite|23522|5|Briefly described|p249 Fig 5|Emsian|Emsian|||||||
20347|Wogarda Argillite|30650|4|Described|p317|||||||||
20347|Wogarda Argillite|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
20347|Wogarda Argillite|31999|6|Mentioned|p150|||Table 1||||||
20347|Wogarda Argillite|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
20347|Wogarda Argillite|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
20347|Wogarda Argillite|33326|6|Mentioned|p446|||Fauna.||||||
20347|Wogarda Argillite|34554|5|Briefly described|p232|||||||||
20347|Wogarda Argillite|36961|6|Mentioned|p208|||See also Fig.3||||||
20347|Wogarda Argillite|39331|6|Mentioned|Table 10-1|||||||||
20347|Wogarda Argillite|40328|6|Mentioned|p196|||||||||
20347|Wogarda Argillite|41348|5|Briefly described|Map legend|Devonian|Devonian|Of the Tamworth Group.||||||16-DEC-04
20347|Wogarda Argillite|41796|6|Mentioned|Table 1|||||||||
20347|Wogarda Argillite|42554|5|Briefly described|p38|||||||||
20347|Wogarda Argillite|43400|2|Defined|p178,179,182-184,map||Early Devonian|(Coblenzian)(Late L.Devn)||||||
20347|Wogarda Argillite|43406|14|Not recorded|p42,48||Early Devonian|Formation of Tamworth Group||||||
20347|Wogarda Argillite|43407|14|Not recorded|Map Legend|||(Provisional Edition) Part of Tamworth Group||||||
20347|Wogarda Argillite|43428|14|Not recorded|p137|||||||||
20347|Wogarda Argillite|43525|14|Not recorded|Table p132||Emsian|||||||
20347|Wogarda Argillite|47056|6|Mentioned|Fig.2 P523|||||||||
20347|Wogarda Argillite|50094|5|Briefly described|p316 Fig.1, p317 Fig.2|Emsian|Emsian|Overlies Northcote Formation. Overlain by Silver Gully Formation.||||||
20347|Wogarda Argillite|50168|6|Mentioned|p157 Fig.2, p159||Middle Devonian|Gamilaroi Terrane. Contains well-preserved entactinid radiolarians with robust tri-bladed spines reportedly characteristic of Middle Devonian or younger faunas (Holdsworth and Jones 1980; Nazarov and Ormiston 1986).||||||06-FEB-18
20347|Wogarda Argillite|61392|5|Briefly described|p165 Fig. 2|Emsian|Emsian|In the Gamilaroi terrane.||||||07-FEB-11
20347|Wogarda Argillite|61765|6|Mentioned|p62|||||||||07-FEB-11
20347|Wogarda Argillite|65214|6|Mentioned|p275|Devonian|Devonian|NSW, Nundle. Appears as Wogarda Arg in text. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
20347|Wogarda Argillite|68005|4|Described|p49 Fig.3-M, p50, p53 Photo.3-M, p150.|Emsian|Emsian|Tamworth Belt. Defined by Crook (1961b). Equivalent to part of Bog Hole Formation.||Unit in Tamworth Group.|Includes Nemingha Limestone Member.|Overlies Northcotte Formation. Is overlain by Silver Gully Formation.|Cherty argillites, fine lithic arenites, interbedded sandstone and mudstone, fine-grained tuffaceous siltstones, rare massive sandstone, conglomerates and limestone.|
20347|Wogarda Argillite|73440|6|Mentioned|p132|||||||||
20375|Wologorong Granite|22503|5|Briefly described|p651, Fig.7 p650|Early Devonian|Silurian|||||||
20375|Wologorong Granite|23214|3|Fully described|p174|Late Silurian|Late Silurian|Includes units previously named Tamboramboro Granite complex, Tamboramboro Granodiorite and Tamboramboro Granite.  Intrudes the Adaminaby Group.||||||
20375|Wologorong Granite|23335|6|Mentioned|p17, p18 Fig. 3|||||||||27-OCT-04
20375|Wologorong Granite|24269|5|Briefly described|p1554 Fig.1B|Early Carboniferous|Late Devonian|Geological Province: Lachlan Fold Belt||||||
20375|Wologorong Granite|29989|6|Mentioned|Map legend|Devonian|Devonian|||||||
20375|Wologorong Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
20375|Wologorong Granite|32483|4|Described|p26|||Silurian-Devonian. Strat. table 1||||||19-JUN-08
20375|Wologorong Granite|32708|6|Mentioned|Fig.1|||||||||
20375|Wologorong Granite|32999|6|Mentioned|p31|||Refers Garretty (1936)||||||
20375|Wologorong Granite|39331|6|Mentioned|Fig.7-3|||||||||
20375|Wologorong Granite|42726|5|Briefly described|map legend|Early Devonian||||||||08-FEB-05
20375|Wologorong Granite|43639|5|Briefly described|Map Legend||Silurian|||||||
20375|Wologorong Granite|43782|5|Briefly described|Map Legend|Ludlow|Ludlow|||||||
20375|Wologorong Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of Parkesbourne Suite. Includes 4 unnamed subunits. Cream to grey plag-phyric biotite granite; subunits of : white to cream fine- to medium-grained leucocratic granite/aplite; cream foliated to massive muscovite-biotite leucogranite; rhyolite dykes...||||||09-SEP-08
20375|Wologorong Granite|66087|5|Briefly described|p3 Fig. 2|Devonian|Devonian|||Of Parkesbourne Suite.||||10-MAY-12
20375|Wologorong Granite|68592|2|Defined|p300, p302, p306, p800, p1542-8, p1561-8|Early Devonian|Late Silurian|See also p269-70, p294. Named "Wologorong mass" by Garretty (1937) referring to granite around Wollogorang [sic] Lagoon. Brunker and Offenberg (1970) extended the Wologorong Granite [their name?] over 80km to the N; later named the Wologorong-Tumboramboro Granite by Scheibner (1973). Here only the southern part of that body is called the Wologorong Granite; the northern part is now largely regarded as the Tumboramboro Granite. The type pluton for Parkesbourne Suite and Wologorong Supersuite. Poor exposure in the south; scattered tors and whalebacks in the north. Type area described. Lithologies detailed. Variable deformation intensities from foliation to mylonitic fabrics. Age ranges from 380 Ma to 339 Ma discussed. Geophysical properties described. Locally quarried for construction material and decorative aggregate.|425.5 +/- 2.4 Ma (SHRIMP U-Pb: Black, 2005).|Unit in Parkesbourne Suite.||Intrudes Abercrombie and Cuddyong Formations. Encloses Kialla Quartz Diorite. Crookwell Basalt overlies. Contact metamorphism in Woodlawn Volcanics and Abercrombie Formation near Wologorong Granite.|Cream, pale grey and pink, medium- to coarse-grained, equigranular to sparsely porphyritic granite; local xenoliths and microgranitic enclaves; fine-grained, granodiorites; porphyritic rhyolite and microgranite and aplite dykes and sills. S-type.|
20375|Wologorong Granite|70192|5|Briefly described|Map Legend|Pragian|Pragian|Dpw. Includes four unnamed units of: leucocratic granite and aplite dykes and sills; potassic, foliated muscovite-biotite granite, 45-50% fractured K-feldspar, high K response; porphyritic rhyolite and microgranite, dykes and sills; leucocratic, coarse grained, porphyritic, biotite granite and fine grained, massive and equigranular, cordierite-biotite granodiorite; has a medium K and high Th response. On Taralga, Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot.||Parkesbourne Suite|||Leucocratic, medium-coarse grained, equigranular-sparsely porphyritic granite; metasedimentary xenoliths in places; fine-medium grained leucocratic granite, aplite and rhyolite dykes; low-high K, low Th and low-medium U; low magnetic susceptibility.|
20375|Wologorong Granite|70296|5|Briefly described|p1, p15, p16-17, p24|Wenlock|Wenlock|Goulburn-Yass district.|425.5 +/- 2.4 Ma (SHRIMP U-Pb)|||||21-JAN-21
20375|Wologorong Granite|70541|4|Described|Map Legend|Devonian|Devonian|||Parkesbourne Suite|||Leucocratic, medium-coarse grained, equigranular-sparsely porphyritic granite; metasedimentary xenoliths present; fine-medium grained leucocratic granite, aplite and rhyolite dykes; low-high K, low Th and low-medium U; low magnetic susceptibility.|
20375|Wologorong Granite|70542|5|Briefly described|Map Legend|Devonian|Devonian|Includes four unnamed members consisting of porphyritic rhyolite/microgranite dykes and sills,  cordierite biotite granodiorite, muscovite biotite granite and leucocratic granite and aplite dykes and sills.||Parkesbourne Suite|||Leucocratic, medium-coarse grained, equigranular-sparsely porphyritic granite; metasedimentary xenoliths in places; leucocratic granite, aplite and rhyolite dykes; low to high K, Low Th; medium U response; low magnetic susceptibility.|
20375|Wologorong Granite|70543|5|Briefly described|Map Legend |Devonian|Devonian|Includes one unnamed unit of leucocratic, coarse grained, porphyritic, biotite granite and fine grained, massive and equigranular, cordierite-biotite granite; has a medium K and high Th response.||Parkesbourne Suite|||Leucocratic, medium-coarse grained, equigranular-sparsely porphyritic granite; metasedimentary xenoliths in places; fine-medium grained leucocratic granite, aplite and rhyolite dykes; low-high K, low Th and low-medium U; low magnetic susceptibility.|
20375|Wologorong Granite|71069|6|Mentioned|p158|||Contact metamorphoses the Woodlawn Volcanics.||||Intrudes the Woodlawn Volcanics.||
20375|Wologorong Granite|71700|6|Mentioned|CD|||||||||
20389|Wombarra Claystone|22549|6|Mentioned|p526||Late Permian|||||||
20389|Wombarra Claystone|22857|5|Briefly described|p530 App.1 Tb.A1.9|Early Triassic|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Grey shale, minor quartz-lithic sandstone. Max. thickness: 30m. Geological Province: Sydney Basin.||||||
20389|Wombarra Claystone|22969|4|Described|Fig 4.1b|Late Permian|Late Permian|Of Clifton Subgroup||||||
20389|Wombarra Claystone|29901|4|Described|Table 1|||||||||
20389|Wombarra Claystone|30132|6|Mentioned|Table 1|||||||||
20389|Wombarra Claystone|31887|5|Briefly described|p7|||||||||
20389|Wombarra Claystone|32187|6|Mentioned|p4|||||||||
20389|Wombarra Claystone|36042|6|Mentioned|Fig.22|||||||||
20389|Wombarra Claystone|36220|4|Described|p67|||See also Table 20.||||||
20389|Wombarra Claystone|36221|6|Mentioned|Map legend|Late Permian|Late Permian|Prob.Late Permian||||||
20389|Wombarra Claystone|36222|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20389|Wombarra Claystone|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
20389|Wombarra Claystone|38615|6|Mentioned|p18|||||||||
20389|Wombarra Claystone|39287|6|Mentioned|Fig. 2.18|||||||||
20389|Wombarra Claystone|39293|6|Mentioned|Fig. 8.11|||||||||
20389|Wombarra Claystone|39296|6|Mentioned|Fig. 11.1|||||||||
20389|Wombarra Claystone|39306|6|Mentioned|p413|||Flora||||||
20389|Wombarra Claystone|39307|6|Mentioned|Table 22.1|||||||||
20389|Wombarra Claystone|39308|5|Briefly described|p511|||||||||
20389|Wombarra Claystone|40602|5|Briefly described|Table 1|||||||||
20389|Wombarra Claystone|40625|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20389|Wombarra Claystone|42737|5|Briefly described|map legend|Permian||||||||
20389|Wombarra Claystone|42896|3|Fully described|p27, Table 2|||of Clifton Subgroup||||||
20389|Wombarra Claystone|42925|5|Briefly described|Table 18||Late Permian|||||||
20389|Wombarra Claystone|42926|4|Described|map legend|Early Triassic|Late Permian|||||||
20389|Wombarra Claystone|43194|5|Briefly described|p130|Triassic|Triassic|Fine grained outwash and overbank sediments, southern Sydney Basin.||||||
20389|Wombarra Claystone|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Clifton Subgroup (Narrabeen Group). Geological Province: Sydney Basin||||||
20389|Wombarra Claystone|66577|6|Mentioned|p997 Fig.2.|Triassic|Triassic|||Unit in Narrabeen Group.||Overlies Bulli Coal. Is overlain by Scarborough Sandstone.||
20389|Wombarra Claystone|68003|5|Briefly described|p42.|Triassic|Triassic|Southern Sydney Basin.|||||Red, green and grey claystone and siltstone, often intercalated with or overlain by conglomeratic sediments.|
20389|Wombarra Claystone|68202|5|Briefly described|p176-178, 180-185|Triassic|Triassic|Sydney Basin. Stratigraphic column; C, N, S, trace and rare earth elements, isotope data plots.||Narrabeen Group.|Otford Sandstone Member.|Gradationally overlies Bulli Coal.|Very dark grey to black, becoming paler upwards. Mainly clays, with quartz and organic matter. Massive to very finely laminated.|
20389|Wombarra Claystone|73304|6|Mentioned|p71-72, p74, p77|||Sydney Basin, southern.||Narrabeen Group||||
20398|Wombat Creek Group|13996|6|Mentioned|p132|Silurian|Silurian|Contains the Hattons Corner (coral) assemblage (described).||||||
20398|Wombat Creek Group|22628|6|Mentioned|fig1p108|||||||||
20398|Wombat Creek Group|22768|4|Described|p167|||||||||
20398|Wombat Creek Group|22857|5|Briefly described|p167|||Shallow-marine conglomerate with limestone lenses, siltstone and turbiditic sandstone. Unconformably overlain by Dartella Volcanic Group; overlies the Mitta Mitta Volcanics. Max. thickness: 4km.||||||
20398|Wombat Creek Group|22968|6|Mentioned|P108|||||||||
20398|Wombat Creek Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
20398|Wombat Creek Group|23309|5|Briefly described|p90-97, 290, 294. Table 2.32||Silurian|||||||
20398|Wombat Creek Group|23454|5|Briefly described|p27|||Of Omeo Complex.||||||25-SEP-08
20398|Wombat Creek Group|23710|14|Not recorded|p69|||Pebble-evidence for pre-Middle Silurian granitic intrusion.||||||
20398|Wombat Creek Group|23938|5|Briefly described|p31-32 Fig. 12|Late Silurian|Late Silurian|Marine: conglomerate, sandstone, siltstone, limestone. See also p83 and p139 Tb. 1 Appendix..||||||
20398|Wombat Creek Group|24002|5|Briefly described|p228 Fig.2|Silurian|Silurian|||||||
20398|Wombat Creek Group|24098|6|Mentioned|p27 Fig. 2|Pridolian|Ludlovian|Geological Province: Lachlan Fold Belt.||||||
20398|Wombat Creek Group|24551|5|Briefly described|p120|||||||||
20398|Wombat Creek Group|29711|6|Mentioned|p70|||||||||
20398|Wombat Creek Group|29860|6|Mentioned|Map legend|Early Silurian|Early Silurian|||||||
20398|Wombat Creek Group|30574|6|Mentioned|p9|||Refers Talent (1969)||||||
20398|Wombat Creek Group|30938|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
20398|Wombat Creek Group|31060|6|Mentioned|p33|||Geology||||||
20398|Wombat Creek Group|31161|5|Briefly described|PA10|||||||||
20398|Wombat Creek Group|31618|6|Mentioned|p102|||||||||
20398|Wombat Creek Group|31800|6|Mentioned|p203|||||||||
20398|Wombat Creek Group|33238|5|Briefly described|p644|||||||||
20398|Wombat Creek Group|33393|6|Mentioned|p158|||||||||
20398|Wombat Creek Group|33606|3|Fully described|p62|||P63||||||
20398|Wombat Creek Group|33959|6|Mentioned|p235|||||||||
20398|Wombat Creek Group|34406|6|Mentioned|p219|||Middle Silurian.||||||25-SEP-08
20398|Wombat Creek Group|34519|5|Briefly described|p42|||||||||
20398|Wombat Creek Group|34954|6|Mentioned|Fig.34|||Analysis Fig.33||||||
20398|Wombat Creek Group|35274|6|Mentioned|p418|||||||||
20398|Wombat Creek Group|35283|6|Mentioned|p49|||||||||
20398|Wombat Creek Group|37330|6|Mentioned|p6|||||||||
20398|Wombat Creek Group|37727|3|Fully described|p93|||See also P15.||||||
20398|Wombat Creek Group|38151|3|Fully described|p38|||||||||
20398|Wombat Creek Group|38367|6|Mentioned|Fig.1|||||||||
20398|Wombat Creek Group|39221|3|Fully described|p263|||||||||
20398|Wombat Creek Group|39447|6|Mentioned|p11|||See also Fig.2||||||
20398|Wombat Creek Group|39860|4|Described|p9|||See also P8||||||
20398|Wombat Creek Group|40328|6|Mentioned|p71|||||||||
20398|Wombat Creek Group|40761|5|Briefly described|p228|||||||||
20398|Wombat Creek Group|41572|6|Mentioned|p19|||||||||
20398|Wombat Creek Group|41585|4|Described|p124|||||||||
20398|Wombat Creek Group|41868|5|Briefly described|p572|||||||||
20398|Wombat Creek Group|42089|6|Mentioned|p16|||||||||
20398|Wombat Creek Group|42313|6|Mentioned|p14|||||||||
20398|Wombat Creek Group|42635|5|Briefly described|p22.|||Silurian||||||
20398|Wombat Creek Group|42827|5|Briefly described|p124|||see also Table 4.1||||||
20398|Wombat Creek Group|43220|6|Mentioned|p9||Silurian|||||||
20398|Wombat Creek Group|44184|5|Briefly described|Map Legend||Late Silurian|||||||
20398|Wombat Creek Group|60503|3|Fully described|p95, p15, p28 Fig. 9|Late Silurian|Late Silurian|Superseded Wombat Creek Formation. Subdivided into: Toaks Creek Conglomerate, Gibbo River Siltstone (and Tongaro Formation?). Conglomerate, mudstone, sandstone and limestone sequence. Max. thickness: >2.5km. Geological Province: Wombat Creek Graben.||||||16-NOV-09
20398|Wombat Creek Group|60504|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes: Mitta Mitta Rhyolite, Undowah Siltstone, Toaks Creek Conglomerate, Gibbo River Siltstone, Tongaro Formation.||||||25-SEP-08
20398|Wombat Creek Group|60505|5|Briefly described|Map legend|Pridoli|Ludlow|Includes: Mitta Mitta Rhyolite, Undowah Siltstone, Toaks Creek Conglomerate, Gibbo River Siltstone, Tongaro Formation.||||||25-SEP-08
20398|Wombat Creek Group|60506|5|Briefly described|Map legend|Pridoli|Ludlow|Includes: Mitta Mitta Rhyolite, Undowah Siltstone, Toaks Creek Conglomerate, Gibbo River Siltstone, Tongaro Formation.||||||25-SEP-08
20398|Wombat Creek Group|60507|5|Briefly described|Map Legend|Pridoli|Ludlow|Includes: Mitta Mitta Rhyolite, Undowah Siltstone, Toaks Creek Conglomerate, Gibbo River Siltstone, Tongaro Formation.||||||25-SEP-08
20398|Wombat Creek Group|60508|5|Briefly described|Map legend|Late Silurian|Late Silurian|Includes: Undowah Siltstone, Toaks Creek Conglomerate, Gibbo River Siltstone, Tongaro Formation.||||||21-OCT-04
20398|Wombat Creek Group|61163|6|Mentioned|p9|Late Silurian|Late Silurian|Geological Province: Lachlan Fold Belt.||||||
20398|Wombat Creek Group|61181|6|Mentioned|p124|Silurian|Silurian|Mentioned in the context of Wombat Creek Group limestone near the junctions of the Gibbo River and Wombat Creek, with the Mitta Mitta River.||||||
20398|Wombat Creek Group|61187|5|Briefly described|p5 Fig.3.|Late Silurian|Late Silurian|Buchan and Mallacoota Zones, Benambra Terrane. Correlative of Humevale, McIvor and Mount Ida Formations, Melbourne Zone, Melbourne Terrane.||||||
20398|Wombat Creek Group|70890|5|Briefly described|p337|Late Silurian|Late Silurian|Age estimate provided by Ludlow fossils (~417 Ma from timescales of Tucker and McKerrow 1995, and Young and Laurie 1996).||||Underlain by Mitta mitta volcanics.||
20398|Wombat Creek Group|70910|14|Not recorded|p44|||Granite intrusions.||||||
20398|Wombat Creek Group|71040|5|Briefly described|p9|Late Silurian|Late Silurian|Wagga-Omeo Zone.|411 +/- 3 Ma (Morand and Fanning, 2009).|||||
20405|Wombeyan Limestone|22678|6|Mentioned|p722,724|Late Silurian|Late Silurian|||||||17-JAN-06
20405|Wombeyan Limestone|22768|6|Mentioned|p177|||||||||
20405|Wombeyan Limestone|22857|5|Briefly described|p177, p480 App.1 Tb.A1.6|Early Devonian|Late Silurian|Of the Taralga Group. Massive biogenic limestone. Geological Province: Murruin Basin.||||||
20405|Wombeyan Limestone|29989|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20405|Wombeyan Limestone|29993|6|Mentioned|Map legend|Silurian|Silurian|||||||
20405|Wombeyan Limestone|30734|6|Mentioned|p36|||||||||
20405|Wombeyan Limestone|32483|4|Described|p21|||Silurian. Strat. table 1.||||||03-JUN-08
20405|Wombeyan Limestone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
20405|Wombeyan Limestone|32672|6|Mentioned|p672|||||||||
20405|Wombeyan Limestone|32999|3|Fully described|p24|||See also pp20,22||||||03-JUN-08
20405|Wombeyan Limestone|34481|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20405|Wombeyan Limestone|34692|5|Briefly described|p185|||||||||
20405|Wombeyan Limestone|37490|6|Mentioned|p283|||||||||
20405|Wombeyan Limestone|37727|6|Mentioned|p87|||||||||
20405|Wombeyan Limestone|40298|6|Mentioned|Table II|||||||||
20405|Wombeyan Limestone|40328|4|Described|p189|||||||||
20405|Wombeyan Limestone|40821|6|Mentioned|p45|||||||||
20405|Wombeyan Limestone|42414|6|Mentioned|p59|||||||||
20405|Wombeyan Limestone|61892|5|Briefly described|p199|Late Silurian|Late Silurian|A biohermal unit. Contains conodonts.||Taralga Group.||Equivalent to (basal) Cobra Formation.||
20405|Wombeyan Limestone|63633|5|Briefly described|Map Legend|Ludlovian|Ludlovian|Of Taralga Group. Massive (? Biohermal) limestone.||||||27-JAN-09
20405|Wombeyan Limestone|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Bungonia Group. White, massive, fine-grained marble with relict fossils.||||||09-SEP-08
20405|Wombeyan Limestone|68592|3|Fully described|p742, p892-3, p895-7, p898-901, p922-5|Silurian|Silurian|See also p238, p240, p732. Originally Wombeyan Caves Limestone (Carne and Jones, 1919). Wombeyan Limestone was used in map legends by Brunker and Offenberg (1970), Brunker et al. (1970) before a description by Offenberg (1974). Scheibner (1973) placed the unit in the Taralga Group (now the Mount Fairy Group). Here it is relocated within Bungonia Group, being almost entirely carbonate and Silurian. Occurs in a small area at Wombeyan Caves, also the type area. Has been extensively mined NE of Taralga for dimension stone; also for glass making and chemical processes. Weathered surfaces show tabulate corals and stromatoporoids. Over 100m thick. Developed a karst surface before deposition of overlying Mares Forest Volcanics.||Unit in Bungonia Group.||Is intruded and recrystallised by Columba Granite. Is unconformably overlain by and faulted against Mares Forest Volcanics. Is correlated broadly with Mount Fairy Group.|Massive, white to pale grey, fine- to medium-grained marble, with impure clay-rich streaks and calcite veins. Pervasively recrystallised.|
20405|Wombeyan Limestone|70192|5|Briefly described|Map Legend|Pridoli|Ludlow|Sby. On Taralga 1:100 000 mapsheet portion of Time-Space Plot. Age max and min boundaries on Time-Space plot are marked with ?-?-?.||Bungonia Group|||Massive, fine to medium grained marble with clay rich streaks, calcite veins and uncommon relict fossils.|
20405|Wombeyan Limestone|70543|5|Briefly described|Map Legend|Silurian|Silurian|||Bungonia Group|||Massive, fine to medium grained marble with clay rich streaks, calcite veins and uncommon relict fossils.|
20405|Wombeyan Limestone|71069|6|Mentioned|p135, p144|||||||Unconformably overlain by the Mares Forest Volcanics. Overlain by Bradfordville Volcaniclastic Member.|Limestone.|
20405|Wombeyan Limestone|71656|6|Mentioned|p13 Fig.2|Ludlow|Ludlow|||Bungonia Group||||
20411|Womboyne Formation|22857|5|Briefly described|p213, p488 App.1 Tb.A1.7|Late Devonian|Late Devonian|Of the Cocoparra Group. Sandstone interbedded with red siltstone. Contains the Confreys Shale, Melbergen Sandstone and Jimberoo Members. Max. thickness: 2930m. Geological Province: Barka Basin.||||||
20411|Womboyne Formation|22859|5|Briefly described|p213|||||||||
20411|Womboyne Formation|32676|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20411|Womboyne Formation|34109|4|Described|Table 3.11|||See also p174.||||||27-OCT-08
20411|Womboyne Formation|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20411|Womboyne Formation|36316|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20411|Womboyne Formation|36317|6|Mentioned|p147|||||||||
20411|Womboyne Formation|43507|14|Not recorded|p125|||||||||
20411|Womboyne Formation|43509|14|Not recorded|p113||Late Devonian|Formation of Cocoparra Group||||||
20411|Womboyne Formation|43511|14|Not recorded|p129,131,134,139-149||Late Devonian|Inc. Confreys Shale, Melbergen Sandstone and Stitts Member||||||
20411|Womboyne Formation|44534|5|Briefly described|map legend|||SI 55-6. Includes the Confreys Shale Member, Melbergen Sandstone Member and the Jimberoo Member. Part of the Cocoparra Group. O/lies the Naradhan Sandstone U/lies the Mailman Gap Conglomerate Member.||||||
20423|Wondalga Granodiorite|22768|6|Mentioned|p156||Silurian|||||||
20423|Wondalga Granodiorite|22857|6|Mentioned|p156|Silurian|Silurian|||||||
20423|Wondalga Granodiorite|24265|5|Briefly described|p1452|Early Devonian|Late Silurian|Geological Province: Lachlan Fold Belt||||||
20423|Wondalga Granodiorite|37529|5|Briefly described|p5|||||||||
20423|Wondalga Granodiorite|40678|5|Briefly described|p13|||Mention p3.||||||
20423|Wondalga Granodiorite|42313|3|Fully described|p128|Late Silurian||||||||
20423|Wondalga Granodiorite|42314|5|Briefly described|Map|Late Silurian||||||||
20423|Wondalga Granodiorite|42497|5|Briefly described|Map Legend|Ludlovian|Wenlockian|||||||
20423|Wondalga Granodiorite|42990|6|Mentioned|p2|||||||||
20423|Wondalga Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh1||||||
20423|Wondalga Granodiorite|60078|6|Mentioned|Map Legend|Early Devonian|Late Silurian|||||||
20423|Wondalga Granodiorite|63290|6|Mentioned|p399, p403 Fig. 6(c)|Early Silurian|Late Ordovician|Age: 446.6+/-3.4Ma (zircon U-Pb SHRIMP).||||||
20423|Wondalga Granodiorite|73082|6|Mentioned|p13|||Adelong Goldfield. Discontinuous quartz veins were the source of alluvial gold in Adelong Creek.||||||
20430|Wondoba Coal Member|37094|4|Described|p243|||||||||
20430|Wondoba Coal Member|38614|4|Described|p9|||||||||
20430|Wondoba Coal Member|39693|6|Mentioned|p17|||||||||
20430|Wondoba Coal Member|39913|5|Briefly described|p6|||||||||
20430|Wondoba Coal Member|40060|6|Mentioned|Fig.3|||||||||
20430|Wondoba Coal Member|40680|5|Briefly described|p23|||||||||
20430|Wondoba Coal Member|40952|6|Mentioned|p3|||||||||
20430|Wondoba Coal Member|43194|5|Briefly described|p115|Late Permian|Late Permian|Name is obsolete but describes tuffaceous stony coal facies within the 'lithic conglomeratic unit' (now Wallala Formation) of the Black Jack Formation (now Black Jack Group).||||||
20443|Wongawilli Coal|22578|6|Mentioned|Fig.10 p400, p402|||||||||
20443|Wongawilli Coal|23881|5|Briefly described|p69 Fig. 7.2|||Of the Illawarra Coal Measures.  Geological Province: Sydney Basin.||||||
20443|Wongawilli Coal|24313|5|Briefly described|p23|Early Permian|Early Permian|Geological Province: Sydney Basin. Overlies: Kembla Sandstone.||||||
20443|Wongawilli Coal|24342|5|Briefly described|p51 Fig. 2|Late Permian|Late Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||
20443|Wongawilli Coal|24471|4|Described|p29 Fig.2|Late Permian|Late Permian|Overlies American Creek Coal. Overlain by Lawrence Sandstone and Eckersley Formation. Contains Farmborough Claystone Member. Of Illawarra Coal Measures. Thickness: 10 m. Geological Province: Sydney Basin.||||||07-FEB-11
20443|Wongawilli Coal|29900|5|Briefly described|p179|||||||||
20443|Wongawilli Coal|29901|4|Described|Table 1|||||||||
20443|Wongawilli Coal|29944|6|Mentioned|Fig.18|||||||||
20443|Wongawilli Coal|30006|4|Described|p25|||Permian||||||
20443|Wongawilli Coal|31128|6|Mentioned|Table 1|||||||||
20443|Wongawilli Coal|31887|5|Briefly described|p5|||||||||
20443|Wongawilli Coal|32618|6|Mentioned|Table 1|||Perm. Strat. table.||||||
20443|Wongawilli Coal|33869|6|Mentioned|Fig.2|||||||||
20443|Wongawilli Coal|36042|6|Mentioned|p28|||||||||
20443|Wongawilli Coal|36220|4|Described|p52|||See also Table 1 & P50.||||||
20443|Wongawilli Coal|36222|6|Mentioned|Map legend|Late Permian|Late Permian|Early Late Permian.||||||
20443|Wongawilli Coal|36593|5|Briefly described|Table 2|||See also Fig.2.||||||
20443|Wongawilli Coal|36594|6|Mentioned|Table 1|||||||||
20443|Wongawilli Coal|37089|6|Mentioned|p208|||||||||
20443|Wongawilli Coal|37090|4|Described|p222|||||||||
20443|Wongawilli Coal|37091|6|Mentioned|p226|||||||||
20443|Wongawilli Coal|37730|6|Mentioned|p18|||||||||
20443|Wongawilli Coal|38603|6|Mentioned|p80|||||||||
20443|Wongawilli Coal|39287|6|Mentioned|p40|||||||||
20443|Wongawilli Coal|39309|6|Mentioned|p128|||See also P132||||||
20443|Wongawilli Coal|39661|6|Mentioned|Fig.1|||||||||
20443|Wongawilli Coal|40744|4|Described|p327|||||||||
20443|Wongawilli Coal|40824|6|Mentioned|Table 1|||||||||
20443|Wongawilli Coal|41226|6|Mentioned|Fig.6|||See also Fig.12||||||
20443|Wongawilli Coal|42737|5|Briefly described|map legend|Permian||||||||
20443|Wongawilli Coal|42787|5|Briefly described|p133|||||||||
20443|Wongawilli Coal|42896|4|Described|p22|||of Sydney Subgroup||||||
20443|Wongawilli Coal|42925|5|Briefly described|Table 18||Late Permian|||||||
20443|Wongawilli Coal|42947|6|Mentioned|Fig.16|||||||||
20443|Wongawilli Coal|43028|6|Mentioned|Fig.7,p618|||of Illawarra Coal Measures||||||
20443|Wongawilli Coal|61315|5|Briefly described|Table SY2|Late Permian|Late Permian|Of the Sydney Subgroup (Illawarra Coal Measures). Geological Province: Sydney Basin||||||
20443|Wongawilli Coal|61609|6|Mentioned|p240 Tb. 1|Permian|Permian|Of Sydney Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
20443|Wongawilli Coal|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Kembla Sandstone. Is overlain by Eckersley Formation.||
20443|Wongawilli Coal|70837|5|Briefly described|p245|Lopingian|Lopingian|Of Southern Sydney Basin. CA-TIMS age of 253.59 Ma (Metcalfe etal., 2015), corresponding to D. parvihola zone (Wuchiangpingian).||Unit of Illawarra Coal Measures.||||
20443|Wongawilli Coal|73304|5|Briefly described|p65-66, p72, p74|Changhsingian|Changhsingian|Sydney Basin, southern. Tuff dated.|253.59 +/- 0.30 Ma U-Pb CA-TIMS.|Illawarra Coal Measures||||
20443|Wongawilli Coal|73421|5|Briefly described|p3, p16, p19|Changhsingian|Wuchiapingian|Sydney Basin, southern. Wongawilli Tuff dated to 253.59+/-0.30 Ma (Metcalfe et al., 2015).|253.59+/-0.30 Ma|Sydney Subgroup||||
20443|Wongawilli Coal|73472|6|Mentioned|p129|Changhsingian|Changhsingian|Sydney Basin. Age of 254.10-253.59 Ma reported for an unnamed tuff.|254.10-253.59 Ma|||||
20443|Wongawilli Coal|73625|6|Mentioned|p25|Permian|Permian|Sydney Basin.||||Time-equivalent to Black Alley Shale.||
20454|Wongwibinda Metamorphic Complex|22857|6|Mentioned|p247 Fig.18.5G|Early Permian|Early Permian|See also Wongwibinda Complex. See also p247 Fig. 18.5G.||||||
20454|Wongwibinda Metamorphic Complex|23720|5|Briefly described|Map Legend|||Includes the Rampsbeck Schist.||||||15-DEC-04
20454|Wongwibinda Metamorphic Complex|34918|6|Mentioned|p1|||||||||
20454|Wongwibinda Metamorphic Complex|44093|5|Briefly described|p122|Late Carboniferous|Late Carboniferous|See also p239 Appendix 1.||||||
20454|Wongwibinda Metamorphic Complex|44450|6|Mentioned|p32|||Geological Province: New England Fold Belt.||||||
20454|Wongwibinda Metamorphic Complex|71280|5|Briefly described|p401-406, p410, p412, p414|||A high-T low-P metamorphic terrane within the central Tablelands Complex of the southern New England Orogen. Abbreviated in the article to WMC.|c.297 Ma (monazite: Craven et al., 2012).|||||
20454|Wongwibinda Metamorphic Complex|71703|4|Described|p191-192, 194, 203, 204, 205|Sakmarian|Gzhelian|Of Tablelands Complex. High temperature, low pressure suite. Protolith includes Girrakool beds deep marine turbidites. 2 pulses of plutonism at ~300Ma and ~292Ma||||||
20454|Wongwibinda Metamorphic Complex|73197|6|Mentioned|p474|||Shear zones interpreted as compressional features, suggests a short period of compression around 305-300 Ma.||||||
20492|Woodburn Diorite|23720|5|Briefly described|Map Legend|Early Permian|Early Permian|Gabbro, diorite, granite.||||||15-DEC-04
20492|Woodburn Diorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
20492|Woodburn Diorite|31806|6|Mentioned|Map legend|Late Permian|Late Permian|||||||
20496|Woodenbong beds|22865|6|Mentioned|Fig22.9 p317|||||||||28-SEP-05
20496|Woodenbong beds|23812|5|Briefly described|p33 Fig.6|||Geological Province: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|40250|6|Mentioned|Fig.7|||||||||
20496|Woodenbong beds|43008|5|Briefly described|map legend|||||||||
20496|Woodenbong beds|43150|5|Briefly described|Map Legend||Jurassic|Geological Province: Clarence-Moreton Basin.||||||12-APR-05
20496|Woodenbong beds|60281|6|Mentioned|p27|||Replaced Woodenbong Beds. Lithic clastics. Geological Province: Clarence-Moreton Basin.||||||01-NOV-05
20496|Woodenbong beds|60993|3|Fully described|p4, p36|Late Jurassic|Middle Jurassic|Sandstone, siltstone, carbonaceous mudstone and minor coal. Conformably overlie Walloon C.M. Grades laterally into Kanagroo Creek Sandstone and probably Grafton Formation. Max. thickness: ?>400m. Geol. Prov: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|60995|5|Briefly described|p55 Fig. 6|||Interpreted as part of or equivalent to Kangaroo Creek Sst. Massive to medium-bedded, cross-bedded, labile, feldspathic and lesser quartzose sandstone sequence overlying the Walloon Coal. Mes.||||||
20496|Woodenbong beds|60997|5|Briefly described|p139 Fig. 1|Berriasian|Kimmeridgian|Geological Province: Clarence-Moreton Basin.||||||
20496|Woodenbong beds|69594|5|Briefly described|p544|||Clarence-Moreton Basin (QLD only). In NSW the lower part is known as the Kangaroo Creek Sandstone and the upper part is known as the Grafton Formation. >400m thick. Fluvial deposits, sourced from granites of the New England Batholith.||||Conformably overlies Walloon Coal Measures.|Lower part: massive, grey, cross-bedded labile sandstone, ripple-marked siltstone common. Upper part not described: may be similar to Grafton Formation.|
20496|Woodenbong beds|73570|5|Briefly described|p911|||Grades laterally to the southeast into the Kangaroo Creek Sandstone.|||||Feldspathic to lithic sandstones.|
20499|Woodford Coal Member|39232|6|Mentioned|Table 2|||||||||
20499|Woodford Coal Member|42657|6|Mentioned|Table 1 P74|||||||||
20510|Woodlands Granite|42726|5|Briefly described|map legend|Silurian||529.  Of  Wangarabell Suite. Felsic I-type undifferentiated.||||||23-AUG-12
20510|Woodlands Granite|60423|5|Briefly described|p372 Fig. 3|Early Devonian|Early Devonian|Age: ~417 Ma (U/Pb). Geological Province: Lachlan Fold Belt.||||||23-AUG-12
20510|Woodlands Granite|70876|5|Briefly described|p77|Devonian|Devonian|Lachlan Orogen.|413.9 +/- 2.0 Ma (Iles, 2012)|||||
20512|Woodlands Hill seam|37087|4|Described|p202|||||||||
20512|Woodlands Hill seam|40805|5|Briefly described|p143|||||||||
20512|Woodlands Hill seam|41010|6|Mentioned|p13|||||||||
20512|Woodlands Hill seam|42078|6|Mentioned|Table 1 P5|||||||||
20512|Woodlands Hill seam|44244|5|Briefly described|p236 Tb. 4|Late Permian|Late Permian|Of the Mount Ogilvie Formation (Jerrys Plains Subgroup).||||||
20516|Woodlawn Volcanics|22768|5|Briefly described|p176|||||||||
20516|Woodlawn Volcanics|22857|4|Described|p176, p474 App.1 Tb.A1.6|Late Silurian|Late Silurian|Submarine felsic volcanics. Overlain by and interfingering with Currawang Basalt. Age: 413+/-6Ma (whole rock U/Pb). Max. thickness: <1km.||||||03-JUN-08
20516|Woodlawn Volcanics|23048|5|Briefly described|p7 fig9|Late Silurian|Silurian|||||||
20516|Woodlawn Volcanics|24116|5|Briefly described|p104|||||||||
20516|Woodlawn Volcanics|24128|6|Mentioned|p82|||Geological Province: Lachlan Fold Belt.||||||
20516|Woodlawn Volcanics|30730|4|Described|p8|||Silurian age||||||
20516|Woodlawn Volcanics|30735|3|Fully described|p22|||||||||
20516|Woodlawn Volcanics|30736|6|Mentioned|Map legend|Middle Silurian|Middle Silurian|||||||
20516|Woodlawn Volcanics|32820|6|Mentioned|Table 1|||Refers Felton & Huleatt (in press)||||||
20516|Woodlawn Volcanics|35325|6|Mentioned|p483|||||||||
20516|Woodlawn Volcanics|35503|6|Mentioned|p202|||Defined in Felton and Huleatt (1977)||||||
20516|Woodlawn Volcanics|35660|6|Mentioned|p155|||||||||
20516|Woodlawn Volcanics|35662|6|Mentioned|p139|||Geology of the Woodlawn district.||||||
20516|Woodlawn Volcanics|36413|6|Mentioned|Table 3|||||||||
20516|Woodlawn Volcanics|39174|6|Mentioned|p1959|||||||||
20516|Woodlawn Volcanics|39331|6|Mentioned|p57|||||||||
20516|Woodlawn Volcanics|40276|6|Mentioned|p3|||||||||
20516|Woodlawn Volcanics|40328|5|Briefly described|p186|||||||||
20516|Woodlawn Volcanics|41140|6|Mentioned|p143|||||||||
20516|Woodlawn Volcanics|42177|6|Mentioned|p213|||||||||
20516|Woodlawn Volcanics|42726|5|Briefly described|map legend|Silurian||||||||
20516|Woodlawn Volcanics|42727|5|Briefly described|map legend|Ludlow|Ludlow|Of Mount Fairy Group. Rhyodacitic ignimbrite, tuffaceous shale and minor ashstone. Underlies Currawang Basalt; unconformably overlies Birkenburn beds. BMR map symbol: Suw. Geol. Prov: Rocky Pic Block.||||||
20516|Woodlawn Volcanics|42820|3|Fully described|p54|||Of Mount Fairy Group.||||||03-JUN-08
20516|Woodlawn Volcanics|50124|6|Mentioned|p132|Late Silurian|Late Silurian|Geological Province: eastern Lachlan Fold Belt.||||||
20516|Woodlawn Volcanics|50232|4|Described|Map legend|Ludlow|Ludlow|Of the Mount Fairy Group. Overlies Campbells Group rocks; partly overlain by Covan Creek Formation;  underlies Currawang Basalt also.||||||22-MAY-08
20516|Woodlawn Volcanics|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Mount Fairy Group. Dark grey to cream flow-banded quartz-feldspar-phyric rhyolite, volcaniclastics; +3 subunits of volc.sst/tuff.silst., porph.rhyolite+volc.breccia, sst.siltst,+shale, and  sm.unit chalcedony-haematite.||||||11-JUN-08
20516|Woodlawn Volcanics|66087|4|Described|p5-6, 11, 13, 16, Figs 2-3|Ludlow|Ludlow|Probably interfingers with overlying Currawang Basalt. Intruded by ?Early Devonian monzodiorites and dolerites. Age also constrained by palaeontology and stratigraphy. Hosts Woodlawn VHMS deposit.|423 Ma +/- 2.5 Ma U/Pb SHRIMP zircon (Black 2005).|Of the Mount Fairy Group.||Overlies De Drack Formation. Underlies Currawang Basalt.|Includes rhyolites, volcaniclastic sedimentary rocks, tuffaceous siltstones, carbonaceous shales and minor quartzose sandstone.|10-MAY-12
20516|Woodlawn Volcanics|66300|5|Briefly described|p23, p27, pp29-34. |||Age is indistinguishable from Ellenden Granite and leucogranite phase of Lockhart Igneous Complex.|423.3 +/- 2.6 Ma to 419.2 +/- 3.2 Ma.|Unit in Mount Fairy Group.|||Lower part is predominantly volcaniclastic; includes porphyritic rhyolite.|
20516|Woodlawn Volcanics|67820|6|Mentioned|p136 Fig.3|Late Silurian|Late Silurian|||Mount Fairy Group.||||
20516|Woodlawn Volcanics|68592|2|Defined|p783-4, p786, p790-1, p794-804, p807-8|Ludlow|Early Silurian|See also p172-4, p266, p726, p728-9, p735, p737, p739-40, p762-3, p769-72, p821. Felton and Huleatt (1977) after Felton (1974).  Intruded by Turrallo, Bishopthorpe Suites. Correlated with Wowagin Dacite Member,  Joppa Siltstone Member, Sooley Volcanic Member. Part equivalent to Kangaloolah and Kohinoor Volcanics. Type section described; a more appropriate composite type section is proposed. Max thickness varies from <1000 - <1500 m. Thins markedly to the north where it interfingers with De Drack Formation. Unconformable over quartzose turbiditic rocks which have contributed clasts to basal conglomerate. Moderately deep marine setting is proposed for greater part of volcanism, as pyroclastic volcanism was (apparently) largely suppressed. Subgreenschist to lower greenschist facies regional metamorphism.  Contact metamorphism may be from proximity of Wologorong Granite. Geophysical properties described. Fossils not age-diagnostic; SHRIMP zircon age (423.4 +/- 2.5 Ma, Black 2005), whole-rock U-Pb ages (413 +/- 6 Ma, Gulson 1977b), palaeontology and regional stratigraphic relationships cannot be reconciled. Likely total age range of early Wenlock to mid Ludlow. Hosts Woodlawn Cu-Pb-Zn-Ag-Au mine (VHMS deposit).||Unit in Mount Fairy Group.||Overlies Abercrombie Formation, angular unconformity; De Drack Formation overlies + interfingers; Currawang Basalt overlies conformably; Covan Creek Formation overlies conformably to disconformably.|Mostly rhyolite lava facies; basal conglomerate (volcaniclastic matrix and rounded quartzose sandstone and vein quartz clasts), resedimented proximal volcaniclastic facies; and isolated outcrops of red siliceous ironstone. I-type.|
20516|Woodlawn Volcanics|69159|5|Briefly described|Map legend|Ludlow|Wenlock|||Unit in Mount Fairy Group.|||Dark grey to cream flow-banded quartz-feldspar-phyric rhyolite; volcanic breccia; volcanic sandstone; conglomerate; tuffaceous siltstone; and mudstone.|07-SEP-15
20516|Woodlawn Volcanics|69270|6|Mentioned|p1|Late Silurian|Late Silurian|Coeval mineralised felsic volcanic units: ~425 Ma Kohinoor Volcanics (Fraser et al., in prep) and ~423 Ma Woodlawn Volcanics (Black, 2006; Bodorkos and Simpson, 2008).|~423 Ma, zircon|||||
20516|Woodlawn Volcanics|69635|5|Briefly described|p11, 14, 19, 21, 35, 46|Lochkovian|Ludlow|Previous SHRIMP U-Pb ages of 423.4+/-2.5 Ma (Black, 2005),  423.3+/-2.6 Ma (Bodorkos et al., 2010), intrusive  rhyolite in the upper portions 419.2+/-3.2 Ma (Bodorkos and Simpson, 2008). Also hosts economic VHMS mineralisation.||||Correlated with Kohinoor Volcanics, Colinton Volcanics.||
20516|Woodlawn Volcanics|70192|5|Briefly described|Map Legend|Ludlow|Wenlock|Sfw[3 asterisks]. Contains three unnamed members consisting of ironstone, porphyritic rhyolite and rhyolitic volcaniclastic sandstone. On Gunning and Goulburn 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot. Related Units continued:  Interleaves with Joppa Siltstone Member (De Drack Formation) and overlies undifferentiated De Drack Formation.||Mount Fairy Group|Includes three unnamed units.|Erosional at base. Is overlain by, and interleaves with, Currawang Basalt and Covan Creek Formation. See comments.|Flow banded, commonly amygdaloidal, porphyritic rhyolite; rare matrix-supported polymictic conglomerate; fine to coarse-grained, poorly sorted rhyolitic volcanic sandstone, tuffaceous siltstone and grey shale, uncommon siliceous ironstone.|
20516|Woodlawn Volcanics|70210|6|Mentioned|p1, p38|Late Silurian|Late Silurian||c.422 Ma.|||||
20516|Woodlawn Volcanics|70296|5|Briefly described|p1, p15, p17-18, p19, p24|Silurian|Silurian|Goulburn-Yass district.|423.4 +/- 2.5 Ma (SHRIMP U-Pb)|||||21-JAN-21
20516|Woodlawn Volcanics|70541|4|Described|Map Legend|Devonian|Silurian|Includes two unnamed mapped members: flow banded amygdaloidal porphyritic rhyolite with minor volcanic sandstone, siltstone and shale with some rare basal conglomerate with clasts of rhyolite and quartz sandstone in a quartzofeldspathic matrix; fine grained, poorly sorted rhyolitic volcaniclastic sandstone, tuffaceous siltstone and grey shale.||Mount Fairy Group|Includes two unnamed members.||Flow banded, commonly amygdaloidal, porphyritic rhyolite; rare matrix-supported polymictic conglomerate; fine to coarse grained, poorly sorted rhyolitic volcanic sandstone, tuffaceous siltstone and grey shale, uncommon siliceous ironstone.|
20516|Woodlawn Volcanics|70542|5|Briefly described|Map Legend|Devonian|Silurian|Contains three unnamed members consisting of ironstone, porphyritic rhyolite and rhyolitic volcaniclastic sandstone.||Mount Fairy Group|||Flow banded, commonly amygdaloidal, porphyritic rhyolite; rare matrix-supported polymictic conglomerate; fine to coarse-grained, poorly sorted rhyolitic volcanic sandstone, tuffaceous siltstone and grey shale, uncommon siliceous ironstone.|
20516|Woodlawn Volcanics|71069|3|Fully described|p9, p21 fig 7, p26, p28, p29, p35, |Ludlow|Late Silurian|Named for Woodlawn property. Previously a part of undifferentiated Mount Fairy Group. Incorporates rocks from the Ellenden Granite and defunct Mount Fairy Beds. Composite type section mentioned at GR 731650 6117420. Maximum thickness estimated at 1500m.  Hosts the Woodlawn Pb-Zn-Cu-Ag-Au VAMS mineralisation. Metaluminous and in some cases Tholeiitic affinities. Volcanic equivalent of the Thurralilly Suite. In places this unit rests unconformably on basement rocks. Contains fossils of Bohemograptus sp. Age derived from fossil assemblage and SHRIMP dating including a second age of 423.3. +/- 2.6 Ma (Bodorkos et al. 2010). Erupted in a shallow to deep marine environment.  Distribution, distinguishing features, geomorphology, primary structures/textures, geochemistry, tectonic structure, metamorphism and geophysical characteristics discussed. Intruded by the Turrallo and Bishopthorpe Suites. Chemical equivalent to the intrusive Ellenden Granite and granites of the Lockhart Igneous Complex. Equivalent to the Sooley Volcanic Member, Wowagin Dacite Member, Kohinoor Volcanics, Kangaloolah Volcanics and Bells Creek Volcanics. See also p38 fig 15, p40 fig 17, p41, p45, p47, p93, p111, p125, p127, p130, p133, p135, p136 fig 44, p139 fig 45, p140 tbl 4, p142, p144, p147, p148, p153-161, p164, p165, p176, p178, p182, p184, p185.|423.4 +/- 2.5 Ma (SHRIMP U-Pb, Black 2005)|Mount Fairy Group||Interfingers with and conformably overlies the De Drack Formation and the Joppa Siltstone Member. Conformably overlain by the Currawang Basalt.|Flow-banded, quartz-feldspar-phyric rhyolite, voclanic breccia, rhyolitic volcanic sandstone, conglomerate, fine-grained tuffaceous siltstone, mudstone and ironstone.|
20516|Woodlawn Volcanics|71691|5|Briefly described|Map legend.|Silurian|Silurian|||Mount Fairy Group.||Is overlain by Currawang Basalt. Abuts/interfingers with De Drack Formation.|Dark grey to cream, flow-banded quartz-feldspar-phyric rhyolite, volcanic breccia, volcanic sandstone, conglomerate, tuffaceous siltstone and mudstone.|
20516|Woodlawn Volcanics|71699|5|Briefly described|Map legend.|Devonian|Silurian|||Mount Fairy Group.||Is overlain by Currawang Basalt.|Dark grey to cream, flow-banded quartz-feldspar-phyric rhyolite, volcanic breccia, volcanic sandstone, conglomerate, tuffaceous siltstone and mudstone.|
20516|Woodlawn Volcanics|71700|2|Defined|vi, viii, p7, p14, p17, p21, p30|Ludlow|Ludlow|This unit is named for the Woodlawn property which historically had a homestead near GR 733190 6117190. A composite type section is proposed from GR 731650 6117420 to GR 732713 6116984.The Woodlawn Volcanics is depicted as a combination of undifferentiated Mount Fairy Group and unnamed granite on the 1st edition Canberra 1:250 000 geological sheet (Joplin et al. 1953), and partly as Ellenden Granite and partly as"Mount Fairy Beds" on the Canberra 1:250 000 2nd edition geological sheet (Best et al. 1964). Rhyolites within the De Drack Formation were previously labelled Woodlawn Volcanics on Braidwood100. Other rocks previously assigned as Woodlawn Volcanics have been included in the Quialigo Volcanics. Contains two unnamed constituents. Distribution, geomorphic expression, outcrop, depositional environment, metamorphism, geophysical characteristics, fossils, geochemistry, structure, distinguishing features and economic geology are discussed. Lithology at various areas, including the type section is provided. Additional SHRIMP ages of 423.3 +/- 2.6 Ma are derived from Bodorkos et al, 2010 and 419.2 +/- 3.2 Ma from Bodorkos and Simpson, 2008. Unconformably overlies the Warbisco Shale and the Abercrombie Formation. This unit correlates with Kohinoor Volcanics, Kangaloolah Volcanics and the Bells Creek Volcanics.The lower volcaniclastic wedge is up to 900m thick and the upper volcanic pile is up to 820m thick. Hosts the Woodlawn Zn-Pb-Cu-Ag (Au) mine. See also  p45, p48-p52, p59-p60, p75-p76, p79-p80, p84-p85, p90, p95, p123, CD.|423.4 +/- 2.5 Ma (Black 2005)|Mount Fairy Group||Unconformably overlies the Margules, Bendoc and Adaminaby groups. Conformably overlain by the Currawang Basalt. Interfingers with De Drack Formation.|Rhyolitic, moderately crystal-rich to crystal-lithic volcaniclastic submarine debris flow deposits with thin intervals of interbedded siltstone and quartzofeldspathic sandstone.|
20530|Woodsreef Melange|23050|4|Described|p15 Table.1|Silurian|Cambrian|Oldest age of crystallisation 530Ma (Pb-U age on zircon); final emplacement age Late Carbonfierous.||||||
20530|Woodsreef Melange|41328|2|Defined|p14|Late Carboniferous||||||||
20530|Woodsreef Melange|41329|6|Mentioned|Fig.3|||||||||
20530|Woodsreef Melange|43091|5|Briefly described|Map Legend|||||||||
20530|Woodsreef Melange|43582|5|Briefly described|fig.2,p7|Early Silurian|Middle Cambrian|||||||
20530|Woodsreef Melange|61764|6|Mentioned|p45, p46|||Ophiolitic rocks - serpentinite. See also Woodsreef melange.||||||
20530|Woodsreef Melange|65398|4|Described|p3, p6 Fig.3, p9, p15 ,p18, p21|Early Cambrian |Early Cambrian|Disrupted and extensively altered ophiolites, variably metasomatised to serpentinite: abundant schistose serpentinite, often with blocks of ophiolitic rocks; local masses of altered gabbro, dolerite, basalt and plagiogranite. Thermally metamorphosed by Bundarra Supersuite. Age: c.530 Ma SHRIMP (Aitchison and Ireland, 1995). Associated with slivers of the Glen Bell Formation.||||||
20530|Woodsreef Melange|66720|5|Briefly described|Map legend|Cambrian|Early Cambrian||c.530 Ma.||||Schistose serpentinite with local phacoids of gabbro, dolerite, harzburgite, pyroxenite, plagiogranite, basalt and sedimentary rocks; minor meta-igneous rocks, and interlayered masses of schistose serpentinite and altered ophiolitic rocks.|
20530|Woodsreef Melange|67322|5|Briefly described|p3 Fig.1, p28|Early Cambrian|Early Cambrian|New England Orogen.|530 Ma (zircons: Aitchison and Ireland, 1995).|||Correlated with Port Macquarie Serpentinite.|Includes serpentinised ultramafic rocks and plagiogranite blocks.|22-FEB-18
20530|Woodsreef Melange|68003|5|Briefly described|p31, p140.|Cambrian|Cambrian|New England Fold Belt. Interpreted as a dismembered ophiolite sequence.|||||Schistose and massive serpentinite; locally hosts plagiogranite, harzburgite, basalt, gabbro, dolerite and sedimentary rock; lesser metamorphosed igneous intrusions.|
20530|Woodsreef Melange|68005|4|Described|p22, pp24-26, pp157-158.|Cambrian|Cambrian|Weraerai terrane, Central Block, New England Fold Belt. Formerly the Great Serpentinite Belt (Benson 1913); formally defined by Aitchison et al. (1988). Variably metamorphosed, from pristine to blueschist/eclogite facies. Zircon U-Pb age from plagiogranites. Low radiometric and very high magnetic signatures.|c.530 Ma (Aitchison and Ireland 1995).|||Is overlain by Dinoga Formation.|A highly dismembered ophiolite sequence; serpentinised ultramafic rocks, predominantly harzburgite; blocks of gabbro, dolerite, plagiogranite, basalt and minor sedimentary rocks (mudstone, limestone, sandstone).|
20530|Woodsreef Melange|68006|5|Briefly described|p149.|||Limited potential for small Besshi-Cyprus VHMS-type mineralisation.|||||Deep marine, mafic to intermediate volcanics and chert.|
20530|Woodsreef Melange|71628|5|Briefly described|p7: 5, 31|||Part of the Great Serpentine Belt. Dismembered portions of this unit were incorporated into the Attunga Creek Monzogranite.||||Is intruded by Moonbi Monzogranite.||
20540|Woogaroo Subgroup|12597|5|Briefly described|p491, |||Of Cranfield and Schwarzbock (1972). Initially for the Ipswich area; extended basin-wide by Wells et al. (1990). Includes also formations previously mapped as Moorooka Formation, Helidon Sandstone and Wivenhoe Sandstone. 150-1120 m thick.||Unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|13516|5|Briefly described|p159 fig 8|Early Jurassic|Late Triassic|From Clarence-Moreton Basin.||Of Bundamba Group||||
20540|Woogaroo Subgroup|22845|6|Mentioned|p76|Jurassic|Triassic|||||||
20540|Woogaroo Subgroup|22857|5|Briefly described|p314, p318 Fig. 22.10A,B|Early Jurassic|Rhaetian|Of the Bundamba Group. Max. thickness: 480m. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|22865|5|Briefly described|p314,Fig22.9p317|||||||||
20540|Woogaroo Subgroup|23435|5|Briefly described|p66|||||||||
20540|Woogaroo Subgroup|23799|3|Fully described|p46, p10 Tb.1|Early Jurassic|Late Triassic|See also p48 Fig. 3. Of the Bundamba Group. Conformably overlain by Marburg Subgroup; unconformably overlies Maronghi Creek beds, Woolshed Mountain Granodiorite and Taron beds. Max. thickness: ~250m. Geological Province: Clarence-Moreton Basin.||||||04-JAN-17
20540|Woogaroo Subgroup|23800|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group.||||||
20540|Woogaroo Subgroup|23811|5|Briefly described|Map Legend|Pliensbachian|Anisian|Of Bundamba Group.  Includes: Nymboida, Red Cliff and Evans Head Coal Measures, Chillingham Volcanics, Laytons Range Conglomerate, Raceview Formation and Ripley Road Sandstone.||||||21-SEP-05
20540|Woogaroo Subgroup|23812|5|Briefly described|p33 Fig.6|||Of Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|24237|5|Briefly described|p6 Fig.2|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|24560|5|Briefly described|Map legend|Jurassic|Late Triassic|Of the Bundamba Group.  Quartzose sandstone, siltstone, shale, conglomerate, minor coal (Clarence-Moreton Basin).||||||
20540|Woogaroo Subgroup|36351|6|Mentioned|p373|||||||||
20540|Woogaroo Subgroup|36354|6|Mentioned|p371|||||||||
20540|Woogaroo Subgroup|36579|6|Mentioned|p447|||||||||
20540|Woogaroo Subgroup|37252|6|Mentioned|Map legend|Jurassic|Triassic|Triassic-Jurassic||||||
20540|Woogaroo Subgroup|37375|6|Mentioned|p474|||||||||
20540|Woogaroo Subgroup|37463|6|Mentioned|p479|||||||||
20540|Woogaroo Subgroup|37616|6|Mentioned|p31|||||||||
20540|Woogaroo Subgroup|38307|6|Mentioned|p521|||||||||
20540|Woogaroo Subgroup|38441|6|Mentioned|Map legend|Early Jurassic|Rhaetian|Rhaetian - Early Jurassic||||||
20540|Woogaroo Subgroup|39079|6|Mentioned|p10|||||||||
20540|Woogaroo Subgroup|39445|6|Mentioned|Table 10|||||||||
20540|Woogaroo Subgroup|39907|6|Mentioned|p8|||||||||
20540|Woogaroo Subgroup|39943|6|Mentioned|Table 10A|||||||||
20540|Woogaroo Subgroup|40579|6|Mentioned|Map legend|Early Jurassic|late Rhaetian|||||||
20540|Woogaroo Subgroup|40623|5|Briefly described|p7|||||||||
20540|Woogaroo Subgroup|40780|4|Described|p6|||||||||
20540|Woogaroo Subgroup|41591|6|Mentioned|p17|||||||||
20540|Woogaroo Subgroup|41631|4|Described|p6|||||||||
20540|Woogaroo Subgroup|41906|3|Fully described|Table 2 p15|||||||||02-DEC-13
20540|Woogaroo Subgroup|42248|5|Briefly described|p397|||||||||
20540|Woogaroo Subgroup|42316|6|Mentioned|p7|||||||||
20540|Woogaroo Subgroup|42317|5|Briefly described|p2|||||||||
20540|Woogaroo Subgroup|42319|5|Briefly described|p3|||||||||
20540|Woogaroo Subgroup|42336|5|Briefly described|p4|||||||||
20540|Woogaroo Subgroup|42463|6|Mentioned|Fig.3 P170|||||||||
20540|Woogaroo Subgroup|42869|5|Briefly described|Fig.2 P32|||||||||
20540|Woogaroo Subgroup|42893|6|Mentioned|p8|||||||||
20540|Woogaroo Subgroup|42894|5|Briefly described|Fig.1 P20|||||||||
20540|Woogaroo Subgroup|42951|5|Briefly described|Fig.11|||of Bundamba Group||||||
20540|Woogaroo Subgroup|43008|5|Briefly described|map legend|||||||||
20540|Woogaroo Subgroup|43076|5|Briefly described|p9|||||||||
20540|Woogaroo Subgroup|43150|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||12-APR-05
20540|Woogaroo Subgroup|43736|6|Mentioned|p3|||||||||
20540|Woogaroo Subgroup|50322|5|Briefly described|Map Legend|Jurassic|Late Triassic|Underlies: Gatton Sandstone.  Of the Bundamba Group.  Geological Province: Clarence-Moreton Basin.||||||09-JUN-04
20540|Woogaroo Subgroup|50384|5|Briefly described|Map Legend|Jurassic|Late Triassic|Of Bundamba Group. Geological Province: Moreton Basin||||||
20540|Woogaroo Subgroup|60079|5|Briefly described|Map Legend|Late Triassic|Late Triassic|Includes: Ripley Road Sandstone, Raceview Formation.||||||
20540|Woogaroo Subgroup|60281|5|Briefly described|p24, p29, Fig.18 App 1|Late Triassic|Late Triassic|Of the Bundamba Group.  Includes the Ripley Road Sandstone, Raceview Formation and Laytons Range Conglomerate. Overlain by the Gatton Sandstone (Marburg Subgroup).||||||
20540|Woogaroo Subgroup|60993|3|Fully described|p4, p6 Fig. 2|||Oldest part of the Bundamba Group. Comprises: Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone. Replaces the original Bundamba Group division of Tabulum Group of McElroy (1963). Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|60995|4|Described|p51 Fig. 3|Late Triassic|Late Triassic|Basal part of the Bundamba Group. The classic sequence of deposits within this subgroup show considerable variation across the basin.  Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|60997|5|Briefly described|p138, p142 Fig. 4|Sinemurian|Rhaetian|Contains quartzose to quartzo-feldspathic sandstone. Geological Province: Clarence-Moreton Basin. See also p139 Fig. 1, p140 Fig. 2..||||||
20540|Woogaroo Subgroup|60999|5|Briefly described|p164||Late Triassic|Of the Bundamba Group. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61002|6|Mentioned|p197|||Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61004|5|Briefly described|p230, p232|Jurassic|Triassic|Of the Bundamba Group. Includes Laytons Range Conglomerate, Raceview Formation and Ripley Road Sandstone. Contains vitrinite-rich coals; minor component is inertinite. Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61006|5|Briefly described|p277, p278 Fig. 2|Jurassic|Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|61310|5|Briefly described|Table C1 (p22-23)|Late Triassic|Late Triassic|Geological Province: Clarence-Moreton Basin.||||||
20540|Woogaroo Subgroup|63748|5|Briefly described|p21|||Basal unit of Bundamba Group. Overlain by Marburg Subgroup. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
20540|Woogaroo Subgroup|64289|5|Briefly described|p6 Fig. 2|Late Triassic|Late Triassic|Of the Bundamba Group. Includes the Aberdare Conglomerate, Raceview Formation and Ripley Road Sandstone. Geological province: Clarence-Moreton Basin.||||||07-FEB-11
20540|Woogaroo Subgroup|64665|5|Briefly described|p53 Fig.2, p59.|Early Jurassic|Late Triassic|Clarence-Moreton and Southern Nambour Basins.||Lower unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation, Ripley Road Sandstone, Nambour Formation, and the lower part of the Landsborough Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|67402|6|Mentioned|p187|||Clarence-Moreton Basin.||Bundamba Group|Includes the Aberdare Conglomerate, Laytons Range Conglomerate, Raceview Formation and the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|68553|6|Mentioned|Map legend; schematic diagram.|Jurassic|Late Triassic|Clarence-Moreton Basin. This unit, as well as the Bundamba Group, the Marburg Subgroup, and Landsborough Sandstone, are all mapped under the symbol, RJb.||Unit in Bundamba Group.||||
20540|Woogaroo Subgroup|68576|5|Briefly described|Q_8B: p11|Jurassic|Triassic|Shorncliffe, western side of Moreton Bay. Fluviatile sediments.||||||
20540|Woogaroo Subgroup|68679|5|Briefly described|p395|||||Bundamba Group.|Aberdare Conglomerate.|Unconformably overlies Ipswich Coal Measures.||
20540|Woogaroo Subgroup|69297|5|Briefly described|p487 fig 5.38|Upper Triassic|Upper Triassic|Clarence-Moreton Basin. More than 480m thick.||Bundamba Group|Includes the Laytons Range Conglomerate, Raceview Formation and the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|69594|4|Described|p519, p543-547, p560-561, p572|Early Jurassic|Rhaetian|Defined by Cranfield and Schwarzbock (1972) after Staines (1964). Clarence-Moreton Basin and southern Nambour Basin. Fluvial to lacustrine deposits. This name replaced the Helidon Sandstone (obsolete; used now only for the building stone quarried at Helidon).||Bundamba Group.|Ripley Road Sandstone, Raceview Formation, Aberdare Conglomerate, Nambour Formation.|Overlies North Arm Volcanic Group. Unconformably overlies Ipswich Coal Measures. Is overlain by Marburg Subgroup. Is intruded by the Brisbane Valley Porphyrites.|A thick succession of mainly conglomerate and sandstone.|
20540|Woogaroo Subgroup|69790|5|Briefly described|p1063 Fig.2|Early Jurassic|Triassic|Northern Clarence-Moreton Basin area.||Unit in Bundamba Group.|Includes Aberdare Conglomerate, Raceview Formation, Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|70821|5|Briefly described|p80|||Clarence-Moreton Basin.||Bundamba Group.|Raceview Formation, Ripley Road Sandstone.|Is overlain by Marburg Subgroup.||
20540|Woogaroo Subgroup|71628|5|Briefly described|p19-147|||Clarence-Moreton Basin.|||Laytons Range Conglomerate.|||
20540|Woogaroo Subgroup|71805|5|Briefly described|p76|Lower Jurassic|Lower Jurassic|Clarence-Moreton Basin.||Bundamba Group|Includes the Ripley Road Sandstone.|||
20540|Woogaroo Subgroup|72297|5|Briefly described|p724, p726, p748|||Clarence-Moreton Basin. At Ravensbourne, 34km NE of Toowoomba, is associated with kaolin deposits.|||Helidon Sandstone.|Includes/partly equivalent to Landsborough Sandstone.||
20540|Woogaroo Subgroup|72298|6|Mentioned|p802|||Clarence-Moreton Basin. Has supplied small supplies of groundwater for irrigation.||||||
20540|Woogaroo Subgroup|73200|6|Mentioned|p532 Fig.1|Jurassic|Jurassic|||||||
20540|Woogaroo Subgroup|73306|5|Briefly described|p566-567, 569|Jurassic|Late Triassic|Clarence-Moreton Basin. It is displaced by steep SW-dipping reverse faults.||Bundamba Group||Is overlain by Marburg Subgroup.||
20573|Woolomol Limestone|43427|14|Not recorded|p151|||Ref.to Etheridge 1899||||||
20573|Woolomol Limestone|48926|6|Mentioned|p21|||P21 et seq.||||||
20573|Woolomol Limestone|65940|6|Mentioned|p205|||Parish of Woolomol, NW of Tamworth, NSW.||||||
20575|Woolooma Formation|22857|4|Described|p508 App.1 Tb.A1.8|Visean|Visean|Hard blue-grey siltstone to brown mudstone, lithic arenite and minor limestone; thin tuffaceous layers; highly fossiliferous. Max. thickness: 560m.||||||
20575|Woolooma Formation|30911|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
20575|Woolooma Formation|32529|4|Described|p199|||Type section location given||||||
20575|Woolooma Formation|32530|6|Mentioned|Map legend|Early Carboniferous|Early Carboniferous|||||||
20575|Woolooma Formation|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
20575|Woolooma Formation|32866|6|Mentioned|p15|||Fossil content||||||
20575|Woolooma Formation|32867|6|Mentioned|p19|||||||||
20575|Woolooma Formation|32869|5|Briefly described|p168|||See also P169 & Figs. 2, 3B. Depositional environment||||||
20575|Woolooma Formation|36390|6|Mentioned|Map legend|Late Carboniferous|Late Carboniferous|||||||
20575|Woolooma Formation|36528|6|Mentioned|p177|||||||||
20575|Woolooma Formation|40883|6|Mentioned|p7|||||||||
20575|Woolooma Formation|41347|6|Mentioned|p361|||||||||
20575|Woolooma Formation|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In Barrington Tops district.||||||16-DEC-04
20575|Woolooma Formation|42547|5|Briefly described|p29|||See also Wooloma Formation (a misspelling)||||||
20575|Woolooma Formation|43576|6|Mentioned|p347|||||||||
20575|Woolooma Formation|43792|6|Mentioned|p362, Fig1||Carboniferous|||||||
20575|Woolooma Formation|44093|5|Briefly described|p228 App. 1|Visean|Visean|Geological Province: New England Fold Belt.||||||
20575|Woolooma Formation|44244|2|Defined|p29-30|Visean|Visean|Overlies the Waverley Formation.  Intercalates with the Isismurra Formation.  Max. thickness: 560m.  Type section in text.  Geological Province: Rouchel Block.||||||30-AUG-04
20575|Woolooma Formation|45088|2|Defined|p36|Early Carboniferous|Early Carboniferous|See also Plate 2||||||
20575|Woolooma Formation|45097|6|Mentioned|p15|||Orthotetes australis zone. Correlation chart||||||
20575|Woolooma Formation|46803|6|Mentioned|Fig. 3|||||||||
20575|Woolooma Formation|50099|5|Briefly described|p9|Early Carboniferous|Early Carboniferous|Blue-grey siltstone, grey to brown mudstone, lithic sandstone and minor limestone; highly fossiliferous. Overlies the Waverley Formation. Max. thickness: >800m. geological Province: Tamworth Belt/New England Orogen.||||||
20575|Woolooma Formation|50268|5|Briefly described|Map Legend|Visean|Visean|Geological Province: Rouchel Block.  Interbedded with the Oakfields Tongue.  Overlies and Underlies: Isismurra Formation.||||||
20575|Woolooma Formation|62095|5|Briefly described|Plate 1, p264|Carboniferous|Carboniferous|Marine unit containing fossiliferous siltstone, mudstone, sandstone and bioclastic limestone. Geological Province: Rouchel Block/Tamworth Belt. See also p281 Appendix. Intertongues with the medial part of Isismurra Formation.||||||31-JAN-08
20575|Woolooma Formation|70777|6|Mentioned|p8|Carboniferous|Carboniferous|Rouchel Block, New England Orogen.||||||
20575|Woolooma Formation|71628|5|Briefly described|p6: 18, 22|||||||Is intruded by Omadale Brook Granodiorite.||
20607|Woonona Coal|22578|5|Briefly described|p398, Fig.3 p393|||||||||
20607|Woonona Coal|24471|4|Described|p29 Fig.2|Late Permian|Late Permian|Overlies Erins Vale Formation. Overlain by Wilton Formation. Of Illawarra Coal Measures. Possibly stratigraphically equivalent to part of Four Mile Creek Subgroup. Geological Province: Sydney Basin.||||||07-FEB-11
20607|Woonona Coal|36042|6|Mentioned|Fig.18|||||||||
20607|Woonona Coal|40256|6|Mentioned|p306|||||||||
20607|Woonona Coal|40275|6|Mentioned|p62|||||||||
20607|Woonona Coal|41226|6|Mentioned|Fig.12|||||||||
20607|Woonona Coal|42737|5|Briefly described|map legend|Permian||||||||
20607|Woonona Coal|42947|6|Mentioned|Fig.16|||||||||
20607|Woonona Coal|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Illawarra Coal Measures.||Overlies Erins Vale Formation. Is overlain by Wilton Formation.||
20607|Woonona Coal|73304|6|Mentioned|p74|||Sydney Basin, southern.||Illawarra Coal Measures||||
20607|Woonona Coal|73421|5|Briefly described|p16, p20|Wuchiapingian|Wuchiapingian|Sydney Basin, southern. Age of 258.89+/-0.89 Ma (Woonona Tuff) from Huyskens, (2014).|258.89+/-0.89 Ma CA-TIMS|Wilton Formation, lower part||||
20618|Woorinen Formation|2967|5|Briefly described|p54|||Lawrence (1966). Contains pelletal clay structures. Has an abnormally high carbonate content.||||Overlies Blanchetown Clay.|Aeolian. Has six palaeosols.|
20618|Woorinen Formation|10010|5|Briefly described|p11, p14 Fig. 5f|Late Pleistocene|Late Pleistocene|Geological Province: Murray Basin.Includes surficial deposits such as mobile sand sheets, source-bordering dunes and lunettes. See also p16.||||||13-AUG-07
20618|Woorinen Formation|22531|5|Briefly described|p22|Quaternary|Quaternary|||||||
20618|Woorinen Formation|22532|5|Briefly described|map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|22799|2|Defined|p44|Holocene|Late Pleistocene|||||||
20618|Woorinen Formation|22857|5|Briefly described|p354|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20618|Woorinen Formation|22887|3|Fully described|p40|Late Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|22893|3|Fully described|p45,46|Late Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|23089|6|Mentioned|p649|||||||||
20618|Woorinen Formation|23252|5|Briefly described|Map Legend||Pleistocene|||||||
20618|Woorinen Formation|23402|5|Briefly described|p35|Quaternary|Quaternary|Geological Province: Adelaide Fold Belt||||||
20618|Woorinen Formation|23560|5|Briefly described|p150|||See also page 163.||||||
20618|Woorinen Formation|23818|5|Briefly described|p212 Fig.108|Late Pleistocene|Late Pleistocene|Geological Province: Great Artesian Basin and Murray Basin.||||||
20618|Woorinen Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20618|Woorinen Formation|24439|6|Mentioned|p38|Quaternary|Quaternary|||||||
20618|Woorinen Formation|24551|5|Briefly described|p338 Fig. 11.2, 341|Holocene|Middle Pleistocene|Overlies Blanchetown Clay.||||||03-JUL-13
20618|Woorinen Formation|29898|6|Mentioned|p216|||||||||
20618|Woorinen Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|30750|6|Mentioned|p4|||Reworked to form Bunyip Sands & Molineaux Sand||||||
20618|Woorinen Formation|30751|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|30752|6|Mentioned|p2|||See also P4,5.||||||
20618|Woorinen Formation|30753|4|Described|p15|Late Pleistocene||Upper Pleistocene age||||||22-JUL-09
20618|Woorinen Formation|30754|2|Defined|Appendix 1|late Pleistocene|late Pleistocene|See also Table 22, P35,38,41||||||
20618|Woorinen Formation|30755|6|Mentioned|p169|||Tectonic map||||||
20618|Woorinen Formation|30756|6|Mentioned|p4|||||||||
20618|Woorinen Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
20618|Woorinen Formation|30934|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
20618|Woorinen Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
20618|Woorinen Formation|30936|6|Mentioned|Map legend|Pliocene|Pliocene|||||||
20618|Woorinen Formation|30994|6|Mentioned|p250|||Palacosals [?palaeosols] discussed.||||||03-JUL-13
20618|Woorinen Formation|30996|6|Mentioned|p42|||||||||
20618|Woorinen Formation|31345|6|Mentioned|p293|||||||||
20618|Woorinen Formation|31741|6|Mentioned|p6|||||||||
20618|Woorinen Formation|31745|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20618|Woorinen Formation|32426|6|Mentioned|p141|||Loose sand||||||
20618|Woorinen Formation|32861|5|Briefly described|Table 1|||||||||
20618|Woorinen Formation|33725|6|Mentioned|p9|||Small sinkholes||||||
20618|Woorinen Formation|33767|6|Mentioned|Fig.5|||||||||
20618|Woorinen Formation|33826|6|Mentioned|p42|||Strat. table||||||
20618|Woorinen Formation|34180|5|Briefly described|p217|Late Pleistocene||Upper Pleistocene||||||22-JUL-09
20618|Woorinen Formation|34459|5|Briefly described|p11|Recent||Recent||||||22-JUL-09
20618|Woorinen Formation|34536|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|34735|4|Described|p45|||Also mention P35.||||||
20618|Woorinen Formation|34758|6|Mentioned|Fig.2|||||||||
20618|Woorinen Formation|34954|5|Briefly described|p199|||||||||
20618|Woorinen Formation|35012|6|Mentioned|p430|||||||||
20618|Woorinen Formation|35071|6|Mentioned|Fig.4|||||||||
20618|Woorinen Formation|35097|6|Mentioned|Fig.4|||||||||
20618|Woorinen Formation|35131|6|Mentioned|p10|||||||||
20618|Woorinen Formation|35200|6|Mentioned|Map legend|Pleistocene|Pleistocene|||||||
20618|Woorinen Formation|35232|5|Briefly described|Table.4|||||||||
20618|Woorinen Formation|35272|3|Fully described|p285|||||||||
20618|Woorinen Formation|35274|6|Mentioned|p425|||||||||
20618|Woorinen Formation|37873|4|Described|p3|||||||||
20618|Woorinen Formation|38068|6|Mentioned|Fig.8|||Murray Basin||||||
20618|Woorinen Formation|38383|6|Mentioned|Table 1|||||||||
20618|Woorinen Formation|38601|6|Mentioned|p7|||||||||
20618|Woorinen Formation|40215|6|Mentioned|p56|||||||||
20618|Woorinen Formation|40380|6|Mentioned|p222|||||||||
20618|Woorinen Formation|41848|4|Described|p360|||||||||
20618|Woorinen Formation|41868|6|Mentioned|p579|||||||||
20618|Woorinen Formation|42125|6|Mentioned|p139|||||||||
20618|Woorinen Formation|42134|4|Described|p339|||||||||
20618|Woorinen Formation|42136|4|Described|Table 1 P364|||||||||
20618|Woorinen Formation|42264|6|Mentioned|p13|||||||||
20618|Woorinen Formation|42635|5|Briefly described|p94|||||||||
20618|Woorinen Formation|42717|5|Briefly described|map legend|Pleistocene||||||||
20618|Woorinen Formation|42720|5|Briefly described|map legend|Pleistocene||||||||
20618|Woorinen Formation|42827|3|Fully described|p360|||see also Table 9.1||||||
20618|Woorinen Formation|42966|1|Redefined|p229|Late Pleistocene||||||||
20618|Woorinen Formation|43053|5|Briefly described|Map Legend|Quaternary|Quaternary|||||||25-MAY-05
20618|Woorinen Formation|43073|4|Described|p18,Table 4|||||||||
20618|Woorinen Formation|43218|4|Described|Fig.3,p22||Quaternary|||||||
20618|Woorinen Formation|43258|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
20618|Woorinen Formation|43627|6|Mentioned|p6||Recent|Includes dune formations.||||||28-OCT-04
20618|Woorinen Formation|43655|5|Briefly described|p40-846|||||||||
20618|Woorinen Formation|43669|4|Described|p23||Pleistocene|||||||
20618|Woorinen Formation|44133|5|Briefly described|p253|Holocene|Middle Pleistocene|Geological Province: Murray Basin. Includes: Piangil Member, Kyalite Member, Speewa Member, Bymue Member, Miralie Member.||||||
20618|Woorinen Formation|44188|5|Briefly described|Map Legend||Pleistocene|Geological province: Murray Basin. Unconsolidated red-brown, siliceous, silty sand, red calcareous silty clay, sandy clay, clay pellet aggregates.||||||15-MAY-08
20618|Woorinen Formation|44191|5|Briefly described|Map Legend|Holocene|Early Pleistocene|||||||
20618|Woorinen Formation|46802|6|Mentioned|Table 1|||||||||
20618|Woorinen Formation|46909|6|Mentioned|Fig.2|||||||||
20618|Woorinen Formation|49038|5|Briefly described|p32|||||||||
20618|Woorinen Formation|60005|5|Briefly described|Map legend|Pleistocene|Pleistocene|Aeolian: dune sand, calcareous, clayey, palaesols.||||||03-JUL-13
20618|Woorinen Formation|60543|5|Briefly described|Map legend|Quaternary|Quaternary|Wind blown sand in east west dunes.||||||23-DEC-09
20618|Woorinen Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials in interdunal areas.||||||
20618|Woorinen Formation|61108|5|Briefly described|map legend|Quaternary|Quaternary|Aeolian sand of inland dune fields. Includes associated alluvial and regolith materials (including calcrete) in interdunal areas.||||||
20618|Woorinen Formation|61155|5|Briefly described|p18|Pleistocene|Pleistocene|Overlies Blanchetown Clay. Age: <2.0Ma. Geological Province: Murray Basin.||||||
20618|Woorinen Formation|61181|5|Briefly described|p137|Recent|Pleistocene|Aeolian deposits containing calcrete (also known as kunkar or caliche). The calcrete sheets consist of light coloured concretionary calcite and minor dolomite.||||||
20618|Woorinen Formation|61207|5|Briefly described|p280 Fig. 2|Quaternary|Quaternary|Longitudinal dune sediments. Geological Province: Murray Basin.||||||
20618|Woorinen Formation|61964|3|Fully described|p14 Fig. 4, p168-171|Quaternary|Quaternary|Preceded by "The Featureless Sandplain". Now overlies this. Aeolian deposits of red-brown to light brown humic, clayey to silty, unconsolid' fine- to med.-grained quartz-lithic sand + red clay cutans. Over Blanchetown Clay in SW. Deposited: 0.7Ma-0.4Ma||||||
20618|Woorinen Formation|62405|5|Briefly described|Map legend|Quaternary|Quaternary|Aeolian-derived. Fossil dunefields of openly spaced, E-W linear dunes; red-brown to light brown humic, clayey to silty, fine- to med.-grained sand with red clay cutans, silty clay at depth; abundant pedogenic carbonate; extensively modified by pedogenesis||||||
20618|Woorinen Formation|65552|5|Briefly described|p2, p5 Fig 3, p6-7, p17, p27 App. 6|Quaternary|Quaternary|Aeolian deposits formed mainly in the late Pleistocene with minor Holocene reworking. A source of silica sands.||||||
20618|Woorinen Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Lawrence 1966.||||||
20618|Woorinen Formation|66012|5|Briefly described|p23|Quaternary|Quaternary|Aeolian. Possible correlative of Windgelli Clay|| ||||13-JUN-13
20618|Woorinen Formation|66287|5|Briefly described|p42, Fig 4-5,8|Holocene|Pleistocene|Forms parabolic and blow-out dune systems.||||Overlies the Bakara Soil.||20-APR-12
20618|Woorinen Formation|68116|5|Briefly described|Appendix, Maps 1-11, 14, 15, 22.|Holocene|Pleistocene|Forms discontinuous chains of east-west longitudinal dunes.|||||Dune deposits, unconsolidated; mainly red-brown siliceous silty sand, red calcareous silty clay, and sandy clay; calcareous nodules and palaeosols common; uppermost unit is mainly sand without calcareous nodules and clay matrix.|
20618|Woorinen Formation|68189|6|Mentioned|p30|Quaternary|Quaternary|||||||
20618|Woorinen Formation|68194|5|Briefly described|p19, p21, p24, p28, p71|Quaternary|Quaternary|Lawrence (1966). Is derived from local vertical weathering of Parilla Sand. Forms low longitudinal NE-SW dunes.|||Includes Piangil Member.|Unconformably overlies Parilla Sand and Shepparton Formation.|Aeolian sands: subangular to subrounded, fine- to medium-grained, iron-stained quartz grains with or without a red clay matrix.|
20618|Woorinen Formation|68716|6|Mentioned|p39 Fig.3|||||||Underlain by the Blanchetown Clay.||
20618|Woorinen Formation|69161|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69162|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69163|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|69164|5|Briefly described|Map legend|Quaternary|Quaternary|Fossil dunefields of open-spaced, east-west linear (aeolian) dunes.|||||Red-brown to light-brown humic, clayey to silty, fine- to medium-grained sand with red clay cutans, silty clay at depth; abundant regolithic and pedogenic carbonate; extensively modified by pedogenesis.|
20618|Woorinen Formation|70961|14|Not recorded|p136|||Section through east-west dune.||||||
20618|Woorinen Formation|72445|5|Briefly described|App.1, App.2.||Pliocene|App.2 is a .csv format file. Fine to medium sand in Stavely 04, 05, 07. Medium sand in Stavely 08. Silty sand (soil profile) in Stavely 11. Subangular to subrounded sandy mud in Stavely 14. Max age from underlying units.||||Overlies Calivil Formation (gradational contact), Loxton Sand (sharp contact).|Includes sandstone, mud and siltstone.|
20618|Woorinen Formation|73112|5|Briefly described|Map legend.|Pleistocene|Pleistocene|This unit is called the Woorinen Formation Equivalent in the map legend.|||||Pale brown aeolian calcareous silt-sand sheet containing carbonate of Loveday Soil.|
20618|Woorinen Formation|73118|6|Mentioned|p20|||||||Overlies Loxton-Parilla Sands.||
20618|Woorinen Formation|73496|5|Briefly described|Map legend|Pleistocene|Pleistocene||||||Wind blown silty sand in east-west linear dunes; no detectable magnetic response; radiometric response low in all channels.|
20618|Woorinen Formation|73505|5|Briefly described|p2, p12-13, p37|Quaternary|Quaternary|Murray Basin. Conformably overlies other units. Topography of convex-west arcuate dunes. Patchy low radiometric response from K, Th. No detectable magnetic response.|||||Windblown sand and silt.|
20622|Wootton beds|22736|6|Mentioned|p629|Visean|Tournaisian|||||||
20622|Wootton beds|22857|4|Described|p500 App.1 Tb.A1.7|Visean|Tournaisian|Mudstone, siliceous siltstone, lithic sandstone; minor conglomerate, limestone. Overlain by the Copeland Road and Conger Formations. Max. thickness: >1400m. Geological Province: Tamworth Forearc Basin.||||||
20622|Wootton beds|36057|6|Mentioned|Fig.1|||||||||
20622|Wootton beds|39468|6|Mentioned|p204|||||||||
20622|Wootton beds|41348|5|Briefly described|Map legend|Carboniferous|Carboniferous|In the Tamworth Belt.||||||16-DEC-04
20622|Wootton beds|44093|5|Briefly described|p230 App. 1|Late Devonian|Late Devonian|Geological Province: New England Fold Belt.||||||
20622|Wootton beds|44244|4|Described|p73, p124|||Of the Flagstaff Formation.  Includes the Verulam Oolite Member.  Max. thickness: 1400m.  Geological Province: Gresford and Myall Blocks.  Type section in text.||||||
20622|Wootton beds|69793|6|Mentioned|p1121 Fig.12|Visean|Tournaisian|Myall Block, Tamworth Belt. [Mis-spelt as Wooton].||||||
20622|Wootton beds|71628|6|Mentioned|p6-22|||||Gilmore Volcanic Group.||||
20622|Wootton beds|73487|5|Briefly described|p566-567, p568 Fig.3, p574, p577, p585|Visean|Tournaisian|Western Myall Block. Shown as Wootton p566. Late Tournaisian-middle Visean age range.|||||Volcaniclastic rocks.|
20623|Worange Point Formation|22815|4|Described|p101, fig31,32|||||||||
20623|Worange Point Formation|22857|5|Briefly described|p217, p494 App.1 Tb.A1.7|Late Devonian|Late Devonian|Sheet sandstone sequence within the Merrimbula Group. Overlies the Bellbird Creek Formation. Max. thickness: 1100m. Geological Province: Lambie Basin.||||||
20623|Worange Point Formation|22859|5|Briefly described|p217|||||||||
20623|Worange Point Formation|23309|6|Mentioned|p186-187|||||||||
20623|Worange Point Formation|23329|6|Mentioned|1044|||||||||
20623|Worange Point Formation|24334|5|Briefly described|p48 Tb.1|Famennian|Famennian|Age: 363 - 367 Ma. Formation is Fmn in text.||||||
20623|Worange Point Formation|24424|5|Briefly described|p539 Tb.4|Late Devonian|Late Devonian|Age: 354-365 Ma. Palaeomagnetic poles given.||||||
20623|Worange Point Formation|30938|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20623|Worange Point Formation|32127|3|Fully described|p264|||Refers Steiner (1966)||||||
20623|Worange Point Formation|32865|6|Mentioned|p484|||||||||
20623|Worange Point Formation|33268|6|Mentioned|Table 1|||||||||
20623|Worange Point Formation|33269|4|Described|p48|||Lithology.||||||05-FEB-08
20623|Worange Point Formation|33732|5|Briefly described|p113|||||||||
20623|Worange Point Formation|35277|5|Briefly described|p121|||||||||
20623|Worange Point Formation|35526|6|Mentioned|Table 2|||Fossil types and localities||||||
20623|Worange Point Formation|38899|6|Mentioned|p71|||||||||
20623|Worange Point Formation|39313|6|Mentioned|p280|||||||||
20623|Worange Point Formation|40646|6|Mentioned|p29|||||||||
20623|Worange Point Formation|40866|6|Mentioned|p180|||||||||
20623|Worange Point Formation|41641|6|Mentioned|p191|||||||||
20623|Worange Point Formation|42050|4|Described|p227|||||||||
20623|Worange Point Formation|42073|6|Mentioned|p293|||||||||
20623|Worange Point Formation|42158|6|Mentioned|p2|||||||||
20623|Worange Point Formation|42827|5|Briefly described|p191|||Of the Merimbula Group.||||||05-FEB-08
20623|Worange Point Formation|42848|6|Mentioned|p532|||||||||
20623|Worange Point Formation|43233|5|Briefly described|Map Legend|Famennian|Frasnian|||||||
20623|Worange Point Formation|43461|14|Not recorded|Table p625|Early Carboniferous|Late Devonian|||||||
20623|Worange Point Formation|43575|6|Mentioned|p284||Late Devonian|||||||
20623|Worange Point Formation|46574|5|Briefly described|Map Legend|Late Devonian|Middle Devonian|Of the Merrimbula Group (Lambie Shelf). Geological Province: Lambian Transitional Province.||||||
20623|Worange Point Formation|63605|5|Briefly described|p993 Fig.2, p999-1001|Famennian|Famennian|Upper unit of the Merrimbula Group. Max. thickness: 850m. Contains fossil fish assemblage. High parts in the formation have a few acritarchs in common with the late Famennian Fairfield Group in the Canning Basin (WA).||||||07-FEB-11
20623|Worange Point Formation|66499|5|Briefly described|p62 Fig.6|Famennian||Includes fish fossils and marine horizon near top||Of Merrimbula Group||||
20623|Worange Point Formation|67028|6|Mentioned|p370 Fig.7, p371 Tb. 5|Devonian|Devonian|Magnetic information for unit concerning Mid-Paleozoic to Early Mesozoic pole positions for Australia is presented, sourced from the Global Palaeomagnetic Database (GPMDB; McElhinny & Lock 1993, 1996).|359-375 Ma magnetic age range|||||10-AUG-15
20623|Worange Point Formation|68295|6|Mentioned|p28-29 Fig. 2.2, p43|||Upper Devonian, Thrupp et al. (1991).||||||
20623|Worange Point Formation|68298|5|Briefly described|p214, p235, p236|Famennian|Frasnian|Contains fish fauna. Contains youngest fauna in Eden-Pambula region, with a Bothriolepis-Remigolepis-Groenlandaspis association. Large Remigolepis typical, Bothriolepis remains less common and often fragmentary.||Merrimbula Group||Overlies Bellbird Creek Formation. Lack of phyllolepids suggests younger than Hervey Group placoderm fauna.||
20623|Worange Point Formation|69159|5|Briefly described|Map legend|Famennian|Frasnian|||Unit in Merrimbula Group.||Overlies Comerong Volcanics.|Purple and red to grey, quartz-lithic sandstone, locally pebbly and conglomeratic. Sandstone occurs as thick sheets separated by siltstone intervals and contains variable porportions of felsic volcanic vs. quartzose metasedimentary lithic fragments.|07-SEP-15
20623|Worange Point Formation|70601|5|Briefly described|p28, 30|Famennian|Famennian|||Uppermost Merrimbula Group.|||Lithic sandstone.|
20623|Worange Point Formation|71699|5|Briefly described|Map legend.|Devonian|Devonian|||Merrimbula Group.||Overlies Comerong Volcanics.|Purple and red to grey, feldspar-quartz-lithic sandstone, pebbly and conglomeratic in places; occurs as thick sheets separated by siltstone intervals; contains variable proportions of felsic volcanic versus quartzose metasedimentary lithic fragments.|
20623|Worange Point Formation|71700|2|Defined|vi, p7, p29, p42, p45, p55, CD|Famennian|Frasnian|Named for Worange Point a variant of the Worang Point in the northeast headland of Twofold Bay on the NSW south coast. The type area is at Worange Point on the northern edge of Twofold Bay (Steiner 1975). A representative section is along the Mount Budawang Road from GR 769895 6072625 to GR 771825 6069595.  Originally mapped as undifferentiated Merrimbula Group by Felton and Huleatt (1975,1977). Wyborn and Owen mapped equivalent units also as undifferentiated Merrimbula Group. Steiner (1975) divided the Merrimbula Formation into three subunits of which the Worange Point Formation was one. Glen and Lewis subdivided the formation and defined the Ben Boyd Formation. Taylor and Mayer (1990) suggested that some sections were equivalent to the Worange Point Formation of Steiner however a lack of marker beds prevented correlation with the latter. Lewis et al (1994) considered these coastal exposures to be part of the Ben Boyd Formation. This unit includes two unnamed subunits. Interpreted as alluvial deposits laid down in the upper to middle part of a flood plain. This unit has an estimated thickness between 700m and 1100m. Distribution, geomorphic expression, outcrop, depositional environment, structure, metamorphism, geophysical characteristics, fossils and distinguishing features are discussed. Lithology is discussed in great detail (see CD). Age is derived from fossil assemblages of the underlying units. This unit is potentially equivalent to the entire rest of the Merrimbula Group.||Merrimbula Group||Conformably overlies the Comerong Volcanics. Overlies the Bellbird Creek Formation.|Thick to very thick sandstone beds seperated by thinner intervals of siltstone and fine-grained sandstone. The sandstone is mostly composed of quartz, lithic fragments and minor feldspar.|
20623|Worange Point Formation|73181|6|Mentioned|p62, p64-65, p67|Famennian|Famennian|Contains fish fossils.||Merrimbula Group||Underlain by Twofold Bay Formation. Overlain by 'Ben Boyd' Formation.||
20630|Woronora Coal Member|24471|5|Briefly described|p31 Fig.3|Late Permian|Late Permian|Within Eckersley Formation. Of Illawarra Coal Measures. Geological Province: Sydney Basin.||||||07-FEB-11
20630|Woronora Coal Member|29900|6|Mentioned|p181|||||||||
20630|Woronora Coal Member|29901|4|Described|Table 1|||||||||
20630|Woronora Coal Member|29944|6|Mentioned|FIg.18|||||||||
20630|Woronora Coal Member|30006|5|Briefly described|p36|||||||||
20630|Woronora Coal Member|31128|6|Mentioned|Table 1|||||||||
20630|Woronora Coal Member|32849|6|Mentioned|Table 1|||Permian||||||
20630|Woronora Coal Member|36220|6|Mentioned|p50|||See also Table 1 & P50.||||||
20630|Woronora Coal Member|36593|6|Mentioned|Table 2|||||||||
20630|Woronora Coal Member|37089|6|Mentioned|p208|||||||||
20630|Woronora Coal Member|39661|6|Mentioned|Fig.1|||||||||
20630|Woronora Coal Member|42787|6|Mentioned|p136|||||||||
20630|Woronora Coal Member|42896|5|Briefly described|p23|||of Eckersley Formation||||||
20642|Woy Woy south basalt|40263|6|Mentioned|Table 2|||||||||
20654|Wroxley Lithic Sandstone Member|22857|5|Briefly described|p498 App.1 Tb.A1.7|Visean|Tournaisian|Of the Dangarfield Formation. Unfossiliferous crossbedded green lithic sandstone. Max. thickness: 62m. Geological Province: Tamworth Forearc Basin.||||||
20654|Wroxley Lithic Sandstone Member|35245|2|Defined|p21|Early Carboniferous|Early Carboniferous|||||||
20654|Wroxley Lithic Sandstone Member|41542|6|Mentioned|p234|||||||||
20654|Wroxley Lithic Sandstone Member|44244|4|Described|p23|Visean|Tournaisian|Of the Dangarfield Formation.  Conformably overlies the Macqueen Member; underlies Brushy Hill Limestone Member.||||||
20663|Wullwye Granodiorite|22815|4|Described|p60|Silurian|Silurian|Average Rb/Sr Age: 415.5 Ma.||||||
20663|Wullwye Granodiorite|33780|6|Mentioned|Map legend|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
20663|Wullwye Granodiorite|33852|6|Mentioned|p499|||Date given||||||
20663|Wullwye Granodiorite|35109|2|Defined|p50|Early Devonian|Late Silurian|Late Silurian to Early Devonian||||||
20663|Wullwye Granodiorite|36411|6|Mentioned|p270|||Refers White et al 1977 for definition.||||||
20663|Wullwye Granodiorite|38320|6|Mentioned|p189|||||||||
20663|Wullwye Granodiorite|38327|6|Mentioned|Table 4|||||||||
20663|Wullwye Granodiorite|38500|6|Mentioned|p82|||||||||
20663|Wullwye Granodiorite|39721|6|Mentioned|Table 2|||Sr isotopes||||||
20663|Wullwye Granodiorite|40328|4|Described|p212|||||||||
20663|Wullwye Granodiorite|43233|5|Briefly described|Map Legend|Late Silurian||of Wullwye Suite.||||||
20663|Wullwye Granodiorite|44092|5|Briefly described|map legend|Early Devonian|Late Silurian|ggh9||||||
20663|Wullwye Granodiorite|49705|5|Briefly described|p43|||See also P37.||||||
20663|Wullwye Granodiorite|60078|6|Mentioned|Map Legend|Devonian|Silurian|||||||
20663|Wullwye Granodiorite|61819|5|Briefly described|p92|||Of the Berridale Batholith. Granitoid pluton on which tors are commonly formed.||||||02-JUN-06
20663|Wullwye Granodiorite|72571|6|Mentioned|p90, p96-100, p103|||Of the Tasmanides of eastern Australia. Petrography of sample is discussed in detail. I-type.||||||
20670|Wunghnu Group|2967|6|Mentioned|p15 Fig.2.2||||||Calivil, Shepparton Formations.|Overlies Renmark Group. Is interbedded with Murray Group.||
20670|Wunghnu Group|10010|5|Briefly described|p12 Fig. 3|Pleistocene|Late Miocene|Geological Province: Murray Basin.||||||13-AUG-07
20670|Wunghnu Group|22756|6|Mentioned|P31|||||||||
20670|Wunghnu Group|22773|6|Mentioned|Fig24.8p352,354|||||||||
20670|Wunghnu Group|22799|5|Briefly described|p24 Fig.10|Pliocene|Pliocene|||||||
20670|Wunghnu Group|22857|5|Briefly described|p352 Fig.24.8, p354|Quaternary|Late Miocene|Includes the Shepparton, Torrumbarry and Calivil Formations. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|23884|5|Briefly described|p155 Fig. 13.2|Pliocene|Late Miocene|Geological Province: Murray Basin.||||||21-SEP-09
20670|Wunghnu Group|24105|5|Briefly described|p158, 159|||Geological Province: Murray Basin. Underlain by Renmark Group.||||||09-OCT-08
20670|Wunghnu Group|24551|5|Briefly described|p320, p322 Fig. 10.29, p324|Pliocene|Late Miocene|Overlies Murray Group beds unconformably.||||||
20670|Wunghnu Group|29591|6|Mentioned|Table 20|||||||||
20670|Wunghnu Group|29898|6|Mentioned|p213|||||||||
20670|Wunghnu Group|31741|6|Mentioned|p6|||||||||
20670|Wunghnu Group|31746|5|Briefly described|p197|||||||||
20670|Wunghnu Group|32021|4|Described|p41|||||||||
20670|Wunghnu Group|32315|6|Mentioned|Fig. 2|||||||||
20670|Wunghnu Group|34735|4|Described|p36|||||||||
20670|Wunghnu Group|35091|6|Mentioned|p7|||Refers Lawrence (1966).||||||
20670|Wunghnu Group|35272|6|Mentioned|p276|||||||||
20670|Wunghnu Group|35285|5|Briefly described|p414|||||||||
20670|Wunghnu Group|35498|6|Mentioned|Fig.1|||||||||
20670|Wunghnu Group|37873|6|Mentioned|p3|||||||||
20670|Wunghnu Group|38293|4|Described|Table 1|||||||||
20670|Wunghnu Group|40795|5|Briefly described|p80|||||||||
20670|Wunghnu Group|41848|5|Briefly described|p352|Quaternary|Tertiary|The Shepparton Formation and Coonambidgal Formation constitute the upper part of this Group||||||
20670|Wunghnu Group|41868|6|Mentioned|p551|||||||||
20670|Wunghnu Group|42125|6|Mentioned|Fig.5 P132|||||||||
20670|Wunghnu Group|42130|6|Mentioned|Fig.3 P265|||||||||
20670|Wunghnu Group|42134|6|Mentioned|Fig.3 P335|||||||||
20670|Wunghnu Group|42137|6|Mentioned|Fig.2 P368|||||||||
20670|Wunghnu Group|42138|6|Mentioned|Fig.2 P390|||||||||
20670|Wunghnu Group|42827|5|Briefly described|p352|||see also Fig 9.1||||||
20670|Wunghnu Group|42881|4|Described|Fig.3, P84|||||||||
20670|Wunghnu Group|42966|2|Defined|p179|Quaternary|Late Miocene|||||||
20670|Wunghnu Group|43780|5|Briefly described|p6|||||||||
20670|Wunghnu Group|43791|6|Mentioned|p372, Fig1|||||||||
20670|Wunghnu Group|43804|6|Mentioned|Fig.2,p49|||||||||
20670|Wunghnu Group|44093|5|Briefly described|p145 App. 1|Tertiary|Tertiary|Geological Province: Kanmantoo Fold Belt.||||||
20670|Wunghnu Group|50156|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50157|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50158|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50159|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50160|5|Briefly described|Map Legend|Quaternary|Miocene|||||||16-JUN-04
20670|Wunghnu Group|50161|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50162|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||
20670|Wunghnu Group|50163|5|Briefly described|Map Legend|Pleistocene|Miocene|Includes Shepparton Formation||||||22-JUN-04
20670|Wunghnu Group|60451|6|Mentioned|p95|||||||||
20670|Wunghnu Group|60492|5|Briefly described|Map Legend|Pleistocene|Pliocene|Includes: Shepparton Formation.||||||
20670|Wunghnu Group|60599|4|Described|p85|Tertiary|Tertiary|Includes the Tertiary Calivil Formation and Torrumbarry Clay, and the Quaternary Shepparton and Coonambidgal Formations. Geological Province:Murray Basin.||||||14-JAN-09
20670|Wunghnu Group|61163|4|Described|p29, p101-102|Pleistocene|Pliocene|Comprises Calivil and Shepparton Formations. Geological Province: Lachlan Fold Belt.||||||
20670|Wunghnu Group|61174|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||07-FEB-11
20670|Wunghnu Group|61175|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61176|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61177|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation and Calivil Formation.||||||
20670|Wunghnu Group|61178|5|Briefly described|map legend|Quaternary |Quaternary|Includes Shepparton Formation.||||||
20670|Wunghnu Group|61185|5|Briefly described|p57|Quaternary|Tertiary|Of Lawrence (1966) including Calivil Sand, Turrumbarry Clay, Shepparton Formation and Coonambidgal Formation. Geological Province: Murray Basin.||||||07-FEB-11
20670|Wunghnu Group|61314|5|Briefly described|p129|Pleistocene|Pleistocene|Includes the Bungunnia Limestone. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|61964|5|Briefly described|p139|Pliocene|Pliocene|Includes Shepparton Formation. Geological Province: Murray Basin.||||||
20670|Wunghnu Group|65552|5|Briefly described|p5 Fig. 3|Quaternary|Late Miocene|Upper (eastern) Murray Basin unit. Contains Shepparton and Calivil Formations, and Torrumbarry Clay. Unconformably overlies Renmark Group.||||||
20670|Wunghnu Group|65715|5|Briefly described|p11 Tb.7, p15 Tb.8|Neogene|Neogene|Includes Loxton Sand and Shepparton Formation. No longer includes Calivil Formation, which is considered older.||||||06-FEB-15
20670|Wunghnu Group|66002|5|Briefly described|p10 Tb.7, p13 Tb.9, p18|Neogene|Neogene|Includes Loxton Sand, Shepparton Formation. Previously included Calivil Formation.||||||27-MAY-13
20670|Wunghnu Group|66934|6|Mentioned|Map legend|Pliocene|Pliocene||||Includes Loxton-Parilla Sands.|||
20670|Wunghnu Group|68194|5|Briefly described|p22-24||Miocene|Lawrence (1966); Lawrence and Abeles (1988). Murray Basin. Deposition occurred during a final marine transgression that started in Late Miocene or Early Pliocene.|||Includes Bookpurnong beds, Parilla Sand, Karoonda Surface, Blanchetown Clay, Shepparton Formation, Yando Clay.|||
20670|Wunghnu Group|69798|5|Briefly described|p4 Fig.2|Pliocene|Pliocene|Murray Basin.|||Shepparton, Calivil Formations.|||
20670|Wunghnu Group|70718|5|Briefly described|p104||||||Includes the Loxton Sand and the Shepparton Formation.|||
20670|Wunghnu Group|70961|14|Not recorded|p136|||Refers to Lawrence (1966).||||||
20670|Wunghnu Group|72445|5|Briefly described|App1, App2; App.5; App.7 p7 Fig.4.|Pliocene|Late Miocene|Shown on the 'Lithostratigraphy of Cenozoic sediments in the Murray Basin' (from Brown & Stephenson 1991). App.2 is a .csv format file. Identified in Stavely 01,05,06,08,09,10, 11,12,14,16.|||Includes Loxton Sand, Calivil Formation, Torrumbarry Clay and Shepparton Formation.|Overlies Renmark, Heytesbury, Murray Groups, gradational/sharp contacts. Unconformably underlies Newer Volcanic Group. Shown as partial equivalent to Loxton-Parilla Sands, Blanchetown Clay.|Includes Silty sand to silty mud. Dominantly fine sand in Stavely01.|
20670|Wunghnu Group|73118|6|Mentioned|p81||||||Shepparton, Calivil Formations.|||
20670|Wunghnu Group|73496|5|Briefly described|Map legend|Holocene|Miocene||||Coonambidgal Formation, Blanchetown Clay, Shepparton Formation, Parilla Sand|||
20670|Wunghnu Group|73497|5|Briefly described|Map legend|Pleistocene|Neogene||||Calivil Formation, Parilla Sand, Shepparton Formation|||
20670|Wunghnu Group|73505|5|Briefly described|p13, p36|Pliocene|Late Miocene|Misspelt as Whungnu Group p11.|||Bookpurnong beds, Parilla Sand, Shepparton Formation, Blanchetown Clay|||
20680|Wuuluman Granite|22857|6|Mentioned|p231|Late Carboniferous|Early Carboniferous|||||||
20680|Wuuluman Granite|22863|6|Mentioned|p231|||||||||
20680|Wuuluman Granite|23043|5|Briefly described|Map Legend|Namurian|Tournaisian|Informally divided into Northern (smaller) and Southern (larger) plutons.||||||
20680|Wuuluman Granite|23170|4|Described|p256|Carboniferous|Carboniferous|of Lachlan Fold Belt.||||||
20680|Wuuluman Granite|24126|5|Briefly described|p4|||||||||
20680|Wuuluman Granite|29993|6|Mentioned|Map legend|Devonian|Devonian|||||||
20680|Wuuluman Granite|32045|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
20680|Wuuluman Granite|32046|6|Mentioned|p127|||See also P128,131,137,139||||||
20680|Wuuluman Granite|32047|5|Briefly described|p24|||Mineralization discussed||||||
20680|Wuuluman Granite|32088|6|Mentioned|p10|||||||||
20680|Wuuluman Granite|32485|6|Mentioned|Map legend|Carboniferous|Carboniferous|Prob. Carboniferous||||||
20680|Wuuluman Granite|32708|6|Mentioned|Fig.1|||||||||
20680|Wuuluman Granite|33098|6|Mentioned|p93|||Mineralisation fluids||||||
20680|Wuuluman Granite|34544|4|Described|p193|||||||||
20680|Wuuluman Granite|35257|6|Mentioned|Fig.24|||||||||
20680|Wuuluman Granite|39331|6|Mentioned|Fig.7-3|||||||||
20680|Wuuluman Granite|40328|6|Mentioned|p143|||See also P176||||||
20680|Wuuluman Granite|40766|6|Mentioned|p27|||||||||
20680|Wuuluman Granite|41563|6|Mentioned|p507|||||||||
20680|Wuuluman Granite|43476|14|Not recorded|Map Legend||Carboniferous|(Provisional Edition)||||||
20680|Wuuluman Granite|46560|14|Not recorded|p.11,13|||No age given. Intrudes Silurian sediments. I55-4.||||||
20680|Wuuluman Granite|60267|5|Briefly described|p14|Carboniferous|Carboniferous|Geological Province: Lachlan Fold Belt.||||||
20680|Wuuluman Granite|68003|5|Briefly described|p24 Fig.3-e, p141. |Visean|Tournaisian|Lachlan Fold Belt, Brigalow Belt South Bioregion. Consists of a smaller northern pluton and a larger southern pluton. Eight un-named constituents are mapped separately.|||||Megacrystic quartz monzodiorite, locally granitic 3-5 mm. Increasing K, decreasing magnetite content; accessory biotite, sphene, muscovite, allanite; leucocratic aplite; greisen.|
20680|Wuuluman Granite|68004|5|Briefly described|p21, p117, p122.|Middle Carboniferous|Early Carboniferous|Near Wellington. Multi-phase intrusion; plutons are generally unfractionated and of intermediate type.||||||
20680|Wuuluman Granite|70036|5|Briefly described|Map legend|Carboniferous|Carboniferous|Lachlan Fold Belt. Included in a mapped unit of Carboniferous intrusive rocks: quartz monzonite and granodiorite.||||||
20680|Wuuluman Granite|73299|6|Mentioned|p1094 Fig.2, p1107 Fig.12|Carboniferous|Carboniferous|U-Pb zircon ages of 341 +/- 3 Ma, 325 +/- 6 Ma (Meakin and Morgan, 1999), additional U-Pb zircon age of 334 +/- 3 Ma (Jeon and Williams, 2018).|341 +/- 3 Ma, 325 +/- 6 Ma U-Pb zircon||||Granite.|
20693|Wyanbene Limestone Member|22857|5|Briefly described|p480 App.1 Tb.A1.6|Late Silurian|Late Silurian|Of De Drack Formation.||||||
20693|Wyanbene Limestone Member|39028|6|Mentioned|Map legend|Ludlovian|Ludlovian|||||||
20693|Wyanbene Limestone Member|40276|2|Defined|p5|Late Silurian|Late Silurian|||||||
20693|Wyanbene Limestone Member|68592|5|Briefly described|p760|||Defined on Araluen 1:100 000; Wyborn and Owen (1987).||Unit in De Drack Formation.|||Limestone.|
20693|Wyanbene Limestone Member|71069|6|Mentioned|p146|||||De Drack Formation||||
20695|Wyandra Sandstone Member|12597|5|Briefly described|p492 Tb.1, p499|Barremian|Early Cretaceous|E Eromanga Basin. Up to 60m thick. Forms the youngest pressurised aquifer in the Basin.||Unit in Cadna-owie Formation.|||Fine- to coarse-grained quartzose to sub-labile sandstone, pebbly in part, generally well sorted, porous and permeable; with minor siltstone interbeds towards the top.|
20695|Wyandra Sandstone Member|13516|5|Briefly described|p167 fig 10, p169 fig 11, p171 fig 12|Early Cretaceous|Early Cretaceous|In Eromanga Basin.||Of Cadna-owie Formation||||
20695|Wyandra Sandstone Member|22883|5|Briefly described|P31, Fig2||Early Cretaceous|Overlying unit is Bulldog Shale, underlying unit is Murta Formation, parent is Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|22912|5|Briefly described|33|||Geol province Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|23375|4|Described|Fig2 p265,267,269,271,277,279|Barremian|Hauterivian|Of the Cadna-owie Formation. In the Eromanga Basin.||||||17-JAN-08
20695|Wyandra Sandstone Member|23430|4|Described|p524 Table 14.7|||Of Cadna-owie Formation. Eromanga Basin Province.||||||
20695|Wyandra Sandstone Member|23982|5|Briefly described|p57|Cretaceous|Jurassic|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||18-JUL-14
20695|Wyandra Sandstone Member|24092|5|Briefly described|p8 Fig.3|||Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24210|5|Briefly described|p133 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation.  Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|24482|5|Briefly described|p44|Cretaceous|Jurassic|Of the Cadna-owie Formation. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|32314|6|Mentioned|Fig. 4|||||||||
20695|Wyandra Sandstone Member|33017|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|33075|2|Defined|p452|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|33086|6|Mentioned|Map legend|Early Cretaceous|Early Cretaceous|||||||
20695|Wyandra Sandstone Member|35239|6|Mentioned|p265|||||||||
20695|Wyandra Sandstone Member|35663|6|Mentioned|Fig.2|||Subsurface correlations of the central basin rock units.||||||
20695|Wyandra Sandstone Member|36251|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|36571|6|Mentioned|Table 4|||||||||
20695|Wyandra Sandstone Member|38226|6|Mentioned|Table 1|||See also Fig.6.||||||
20695|Wyandra Sandstone Member|39070|4|Described|p364|||||||||
20695|Wyandra Sandstone Member|39211|5|Briefly described|Fig.3|||See also Fig.4||||||
20695|Wyandra Sandstone Member|39478|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|39480|6|Mentioned|p196|||||||||
20695|Wyandra Sandstone Member|39481|6|Mentioned|p181|||||||||
20695|Wyandra Sandstone Member|39846|6|Mentioned|p48|||||||||
20695|Wyandra Sandstone Member|39847|5|Briefly described|p38|||||||||
20695|Wyandra Sandstone Member|39989|4|Described|p423|||||||||
20695|Wyandra Sandstone Member|40199|4|Described|p25|||||||||
20695|Wyandra Sandstone Member|40249|6|Mentioned|p41|||||||||
20695|Wyandra Sandstone Member|40681|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|40687|3|Fully described|p417|||||||||
20695|Wyandra Sandstone Member|40832|6|Mentioned|p457|||||||||
20695|Wyandra Sandstone Member|40910|6|Mentioned|Table 3|||||||||
20695|Wyandra Sandstone Member|40926|6|Mentioned|Table 2|||||||||
20695|Wyandra Sandstone Member|41064|6|Mentioned|p62|||||||||
20695|Wyandra Sandstone Member|41089|6|Mentioned|p156|||||||||
20695|Wyandra Sandstone Member|41097|6|Mentioned|p165|||||||||
20695|Wyandra Sandstone Member|41165|5|Briefly described|p360|||||||||
20695|Wyandra Sandstone Member|41177|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|41183|6|Mentioned|p310|||||||||
20695|Wyandra Sandstone Member|41186|5|Briefly described|p200|||||||||
20695|Wyandra Sandstone Member|41198|6|Mentioned|Table 1|||||||||
20695|Wyandra Sandstone Member|41219|6|Mentioned|p334|||||||||
20695|Wyandra Sandstone Member|41266|6|Mentioned|Fig.3|||||||||
20695|Wyandra Sandstone Member|41286|6|Mentioned|p117|||||||||
20695|Wyandra Sandstone Member|41523|5|Briefly described|p271|||||||||
20695|Wyandra Sandstone Member|41681|6|Mentioned|p23|||||||||
20695|Wyandra Sandstone Member|41724|6|Mentioned|p382|||||||||
20695|Wyandra Sandstone Member|42067|5|Briefly described|p313|||||||||
20695|Wyandra Sandstone Member|42084|6|Mentioned|Fig.3 P356|||||||||
20695|Wyandra Sandstone Member|42085|6|Mentioned|Fig.2 P374|||||||||
20695|Wyandra Sandstone Member|42999|5|Briefly described|Table 2,p90||Early Cretaceous|||||||
20695|Wyandra Sandstone Member|43105|5|Briefly described|Fig.9,p15.|||Of Cadna-owie Formation.||||||16-SEP-08
20695|Wyandra Sandstone Member|43122|5|Briefly described|p23|||of Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|43602|5|Briefly described|203|||In Cadna-owie Formation||||||
20695|Wyandra Sandstone Member|44133|6|Mentioned|p115|||||||||
20695|Wyandra Sandstone Member|46791|6|Mentioned|Table 1|||See also Fig.7||||||
20695|Wyandra Sandstone Member|46937|5|Briefly described|Fig.10|||See also Table 1.||||||
20695|Wyandra Sandstone Member|46939|6|Mentioned|Fig.2|||||||||
20695|Wyandra Sandstone Member|49010|6|Mentioned|Fig.4|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|49011|6|Mentioned|Fig.3|||Eromanga Basin||||||
20695|Wyandra Sandstone Member|60717|5|Briefly described|p40 Fig. 2|Early Cretaceous|Early Cretaceous|Of the Cadna-owie Formation. Overlain by Wallumbilla Formation and partly by Bulldog Shale. Geological Province: Eromanga Basin.||||||16-SEP-08
20695|Wyandra Sandstone Member|61014|5|Briefly described|pp532-554. |Lower Cretaceous|Lower Cretaceous|Eromanga Basin. The uppermost oil reservoir in the Eromanga Basin succession in south-west Queensland. Trace fossils (burrows) occur throughout. A regressive-transgressive sequence of fluvial, overbank crevasse-splay, mouth bar, estuarine and distal distributary channel deposits. Grain-size analysis and sequence-stratigraphic analogues are detailed.||Unit in Cadna-owie Formation.|||An amalgamation of fining-upward sandstone units to 2 m thick, with ripple cross-lamination, flaser bedding and multiple layers of carbonaceous detritus; commonly capped by thin mudstone units; interbedded mudstone and thin coal; bioturbated at top.|
20695|Wyandra Sandstone Member|61312|5|Briefly described|p64|Early Cretaceous|Early Cretaceous|Uppermost part of the Cadna-owie Formation. Dominantly sandstone; may contain reservoir quality sands. Geological Province: Eromanga Basin.||||||
20695|Wyandra Sandstone Member|61613|6|Mentioned|p282 Fig. 2|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|61615|6|Mentioned|p302 Fig. 2|Early Cretaceous|Early Cretaceous|Geological Province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|62029|5|Briefly described|p15 Fig. 4|Cretaceous|Cretaceous|||||||
20695|Wyandra Sandstone Member|62730|5|Briefly described|p352 Fig. 1|Early Cretaceous|Early Cretaceous|Of the Cada-owie Formation. Geological Province: Eromanga Basin.||||||21-APR-08
20695|Wyandra Sandstone Member|63979|5|Briefly described|p46, Fig. 44|Barremian|Hauterivian|Of (upper) Cadna-owie Formation occupying same stratigraphic position in Qld. as Mount Anna Sandstone in SA. A major aquifer in Great Artesian Basin. Geological province: Eromanga Basin.||||||07-FEB-11
20695|Wyandra Sandstone Member|64048|5|Briefly described|p71, p72|||Of the Cadna-owie Formation. Records high oil flow rates.||||||07-FEB-11
20695|Wyandra Sandstone Member|64197|6|Mentioned|p625 Fig.1c|Cretaceous|Cretaceous|Eromanga Basin.||Unit in Cadna-owie Formation.||Is overlain by Bulldog Shale or Wallumbilla Formation.||
20695|Wyandra Sandstone Member|65385|5|Briefly described|pS134 Fig.7|Early Cretaceous|Early Cretaceous|Of Cadna-owie Formation. Overlain by Wallumbilla Formation and Bulldog Shale.||||||08-MAR-12
20695|Wyandra Sandstone Member|66529|6|Mentioned|p12 Fig.5|||||Unit in Cadna-owie Formation.||||
20695|Wyandra Sandstone Member|66623|3|Fully described|p239, p243, pp254-255.|Early Cretaceous|Early Cretaceous|Equivalent to the informal Mokely Creek Sandstone member (Morton 1982), and topmost Gum Vale Beds. Glacial dropstones preserved towards the top. A widespread marker unit in Tibooburra-Milparinka area. Thickness to 20 m. Similar fossil assemblage as Cadna-owie Formation. Upper boundary is strongly diachronous, younging towards basin margins.||Unit in Cadna-owie Formation.||Is conformably, but sharply overlain by Wallumbilla Formation (or, in SA, by Bulldog Shale).|Calcareous quartzose sandstone, pebbly sandstone and quartz pebble conglomerate; exotic lonestone cobbles and boulders of quartz-veined quartzite and felsic volcanic lithologies common throughout.|05-JUN-13
20695|Wyandra Sandstone Member|66915|4|Described|p6 Fig.3, p9, p11 Fig.7|Early Cretaceous|Early Cretaceous|Eromanga Basin. Abbreviated as Wyandra Sandstone in some figures and text. See also parent Cadna-owie in this paper.||Uppermost unit of Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||12-JAN-17
20695|Wyandra Sandstone Member|66921|5|Briefly described|Map legend|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67207|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate; local ferruginous, coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67209|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.||Overlies Namur Sandstone.|Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67211|5|Briefly described|Map legend.|Cretaceous|Cretaceous|||Unit in Cadna-owie Formation.|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|67323|5|Briefly described|p87|Early Cretaceous|Early Cretaceous|Eromanga Basin.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|67402|4|Described|p26, p26 tbl RRM4|Aptian|Aptian|Eromanga Basin. Maximum thickness of <10m. Deposited as beach sands during a marine transgressive cycle. Minor hydrocarbon reservoir but may be a major carbon dioxide storage reservoir. See also p43 tbl HPB1, p108, p109, p115, p121, p303.||Cadna-owie Formation.||Overlies the Lower Cadna-owie Formation. Overlain by the Wallumbilla Formation.|Mainly fine to medium-grained, thickly bedded sandstone with minor siltstone at the top.|
20695|Wyandra Sandstone Member|67561|5|Briefly described|p51, p52 Fig.2, p53, p64, p65, p67|Barremian|Valanginian|Eromanga Basin. Australian Spore-Pollen zonation: C.wonthaggiensis. Occurs at the top of the Cadna-Owie Formation. Previously regarded as a lowstand section, but re-interpreted by Bron (2010) as a tsunami deposit generated by the (125 +/- 1 Ma) Tookoonooka impact.||Of the Cadna-Owie Formation.||Overlain by the Bulldog Shale.|Coarse-grained sandstone.|20-JAN-17
20695|Wyandra Sandstone Member|68731|6|Mentioned|pp209-211|||||||||
20695|Wyandra Sandstone Member|69457|5|Briefly described|p41:3, 7|Early Cretaceous|Early Cretaceous|Senior et al. (1975). Eromanga Basin. Transitional (?beach setting) deposits.||Cadna-owie Formation.||Stratigraphic equivalent to Wyandra Sandstone Member (in Qld).||12-JUL-16
20695|Wyandra Sandstone Member|69594|5|Briefly described|p519, p526-528|Aptian|Barremian|Eromanga Basin. 3-18m thick. An important regional aquifer. A prominent regional marker. Beach deposits.||Topmost Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation)..|Coarse, sporadically pebbly, quartzose to sublabile sandstone.|
20695|Wyandra Sandstone Member|69673|6|Mentioned|p155 fig 127|Cretaceous|Cretaceous|||Cadna-owie Formation||Overlain by Doncaster Member||
20695|Wyandra Sandstone Member|69797|5|Briefly described|p17 Fig.2|Early Cretaceous|Early Cretaceous|Geol. Prov: Eromanga Basin. Presented in figure as Wyandra Sandstone Mbr.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|69946|3|Fully described|p19-21, p57, p94|Early Cretaceous|Early Cretaceous|Eromanga Basin. Defined in the subsurface in Qld (Senior et al., 1975) as the upper sandy part of the Cadna-owie Formation. Type section is the interval 357 - 373m in Water Bore No. 2049 (Queensland Irrigation and Water Supply records), 15km SE of Wyandra. Proposal for a new type section discussed. Can be correlated on wireline logs into the Cooper region in SA. 3-18m thick in Qld (subsurface). Wireline log correlations.||Uppermost unit in Cadna-owie Formation.||Is overlain conformably by Bulldog Shale or Wallumbilla Formation.|Medium- to coarse-grained, quartzose to labile sandstone with scattered pebbles. Locally contains up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|69947|5|Briefly described|p9, p13 Fig.7.2, p31-32 Figs.7.20-21|Early Cretaceous|Early Cretaceous|Lang et al. (2001). Eromanga Basin. Basal regional sequence boundary, overlain by amalgamated fluvial distributary channel fill. Appears simply as Wyandra Sandstone in Fig.7.20. Generalised stratigraphic log showing key surfaces and systems tracts.||Cadna-owie Formation||Is overlain by Bulldog Shale and the Wallumbilla Formation.|Basal in-filled fluvial channel sediments overlain by tidally-influenced sediments followed by heterolithic marine strata.|07-FEB-18
20695|Wyandra Sandstone Member|70649|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70652|5|Briefly described|Map Legend|Cretaceous|Cretaceous|||Cadna-owie Formation|||Coarse-grained, calcareous, quartzose sandstone, pebbly sandstone and conglomerate.|
20695|Wyandra Sandstone Member|70821|4|Described|p21 Fig.2.6, p22, p33, p79-80,p82,p85-86|Early Cretaceous|Early Cretaceous|Eromanga Basin. Typically 3-18m thick; locally considerably thicker. Historically considered a beach deposit; more recent work suggests it may well be an impact tsunami deposit formed by the Tookoonooka impact event to the NE of the project area (Bron, 2009). Hydrochemistry mentioned, hydrostratigraphic properties. Aquifer: generally artesian.||Cadna-owie Formation.||Is overlain by Doncaster Member (Wallumbilla Formation).|Coarse, sporadically pebbly, quartzose to sub-labile sandstone. Locally with dark carbonaceous laminae.|
20695|Wyandra Sandstone Member|71251|4|Described|p8, p11, p13, p15, p17, p19-20, p29|||See also p48-49, p51. Eromanga Basin. 30m total thickness in Eulo 1 borehole. An aquifer. Natural gamma, magnetic susceptibility data tabulated. Abbreviated in text to Wyandra Sandstone or simply Wyandra. Conductivity diagram.||Cadna-owie Formation.||Is overlain by Wallumbilla Formation.|Fine- to medium-grained sandstone, subangular quartz, feldspar and lithic fragments.|
20695|Wyandra Sandstone Member|71342|4|Described|Ch5 p19-p21, Ch5 p57, Ch6 p7|Aptian|Barremian|This unit was first defined by Senior et al (1975) as the upper sandy part of the Cadna-owie Formation. An initial type section was nominated by Senior et al (1975) however, Green, Brain et al (1989) proposed that a new type section was necessary if the original concept of Senior et al was to continue. This unit ranges between 3 and 18m thick in Queensland. Spore-pollen zone is given in Ch5 p57. Hosts commercially producible oil in Aldinga 1. Seal and reservoir characteristics discussed in Ch11. See also  Ch7 p9, Ch7 p11, Ch7 p13, Ch7 p32, Ch11 p2, Ch11 p5, Ch12 p3.||Cadna-owie Formation||Conformably overlain by the Wallumbilla Formation or the Bulldog Shale.|Medium to coarse-grained, quartzose to labile sandstone with scattered pebbles. Sandstones may contain up to 40% feldspar and rock fragments.|
20695|Wyandra Sandstone Member|71863|6|Mentioned|p5|Aptian|Aptian|Eromanga Basin.||Cadna-owie Formation||Overlain by the Doncaster Member.||
20695|Wyandra Sandstone Member|71864|6|Mentioned|p13-p14, p17, p26|||Waterbores are reported to intersect this unit which is a moderately producing aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|72297|5|Briefly described|p743|||Eromanga Basin. High oil flows recorded at Talgeberry.||||||
20695|Wyandra Sandstone Member|72298|5|Briefly described|p801|Cretaceous|Cretaceous|Eromanga Basin (QLD,NSW). Main confined aquifers, generally producing flowing artesian water bores.||Cadna-owie FZ.||Is overlain by Doncaster Member (Wallumbilla FZ).||
20695|Wyandra Sandstone Member|72914|5|Briefly described|p14-16, p18, p20-21, p27, p29-30, App.I|Cretaceous|Cretaceous|Major groundwater source in the local region; supplies fresh to slightly brackish water. Natural gamma emissions are very subdued, indicating the quartz-rich nature of the unit. See also accidental misspelling Wyandra Sandstone member p20.||Cadna-owie Formation||Overlain by the Wallumbilla Formation.|Clean quartz sandstone; quartzose and labile lithic gravels.|
20695|Wyandra Sandstone Member|72915|6|Mentioned|p27|Mesozoic|Mesozoic|Constitutes a local aquifer.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73167|6|Mentioned|p664 Fig. 2|Cretaceous|Cretaceous|Eromanga Basin. Contains oil and gas.||Cadna-owie Formation||||
20695|Wyandra Sandstone Member|73251|6|Mentioned|p62|Early Cretaceous|Early Cretaceous|||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73343|6|Mentioned|p337|Cretaceous|Cretaceous|Eromanga Basin.||Cadna-owie Formation||Overlain by Wallumbilla Formation.||
20695|Wyandra Sandstone Member|73479|5|Briefly described|p156 Fig.2, p159|Cretaceous|Cretaceous|Eromanga Basin. Deltaic shoreface marine depositional environment.|ca 125 Ma|Cadna-owie Formation||Overlies Cadna-owie Formation||
20699|Wyangala Granite|22679|4|Described|p 42|Silurian|Silurian|Formerly Wyangala Adamellite.||||||12-JUN-08
20699|Wyangala Granite|23214|3|Fully described|p159|Silurian|Silurian|Originally mentioned as a substitute for the whole Wyangala Batholith. Also previously named Wyangala Adamellite. Intrudes Adaminaby Group, Swan Ponds Tonalite and Garland Granodiorite. Geological Province: Wyangala Batholith||||||
20699|Wyangala Granite|23335|6|Mentioned|p18 Fig. 3|||||||||
20699|Wyangala Granite|37544|6|Mentioned|Fig.10|||||||||
20699|Wyangala Granite|39331|6|Mentioned|p64|||||||||
20699|Wyangala Granite|40136|6|Mentioned|p15|||||||||
20699|Wyangala Granite|42384|6|Mentioned|p10|||||||||
20699|Wyangala Granite|42726|5|Briefly described|map legend|Silurian||||||||
20699|Wyangala Granite|43642|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Consists of foliated porphyritic biotite granite.||||||15-JUL-08
20699|Wyangala Granite|43654|5|Briefly described|Map Legend|Silurian|Silurian|Of Wyangala Batholith. Foliated porphyritic biotite granite.||||||17-JUL-08
20699|Wyangala Granite|43782|5|Briefly described|Map Legend||Silurian|Part of Wyangla Batholith.||||||12-JUN-08
20699|Wyangala Granite|50231|5|Briefly described|Map Legend|Pridoli|Ludlow|Part of the Wyangala Batholith.||||||
20699|Wyangala Granite|63289|5|Briefly described|p367, p368 Fig. 5a|Silurian|Silurian|White mica in shear zone records very late cooling ages of 384+/-4Ma. Silurian granite.||||||07-FEB-11
20699|Wyangala Granite|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Hovells Suite. Grey to cream or white, medium- to coarse-grained, generally foliated, equigranular to porphyritic, often megacrystic cordierite-muscovite-biotite granite. High K and Th with moderate to high U radioelement response.||||||
20699|Wyangala Granite|66185|5|Briefly described|p395, p398 Fig.2, p399|||Part of the Wyangala Batholith, Eastern Lachlan Fold Belt. Light grey, foliated, porphyritic, biotite granite with large K-feldspar phenocrysts. Intrudes Ordovician metasediments.||||||
20699|Wyangala Granite|68592|2|Defined|p1262-4, p1268-9, p1274, p1284, p1302-7|Late Silurian|Late Silurian|See also p82, p96, p133, p230-1, p324, p373, p376, p379, p384-5, p1237, p1255 Fig.220. This name was originally mentioned by Hobbs and Hopwood (in Packham, 1969) as a substitute term for the whole Wyangala Batholith. Close (1978) mapped a body which he called the Wyangala Adamellite; this unit was remapped and renamed to accord with standard nomenclature by Chappell et al. (1991) as Wyangala Granite. Now includes much of the Cucum Granite and the southern portion of Whistle Waa Granite (Chappell et al., 1991). Type area and typical exposures are described. Geochemistry detailed; geophysical properties and metamorphism described. Extensive development of shear (S-C) fabrics from Frogmore Fault Zone. Has a broad protomylonitic zone (dated 384 +/- 4 Ma; Foster et al., 1999) on the E margin recording W-over-E thrust movement. Quarried for road construction material and, N of Boorowa, for dimension stone; potential for renewed extraction. The metamorphic aureole has produced cordierite spotting in pelitic lithologies. Cannot be distinguished from Whistle Waa Granite on radiometric images. Not isotopically dated: age from intrusive relationships.||Unit in Hovells Suite.||Intrudes Adaminaby Group, Kenyu Formation, Swan Ponds Tonalite and Garland Granodiorite. Is intruded by Wyoming and Briarlee Granites.|Grey to cream or white, medium- to coarse-grained, equigranular to porphyritic, commonly megacrystic, generally foliated, cordierite-muscovite-biotite granite and granodiorite; sporadic biotite-rich metasedimentary enclaves. S-type.|
20699|Wyangala Granite|69539|5|Briefly described|607-618|Silurian|Silurian|Lies within the Hill End Trough. SHRIMP U-Pb zircon crystallisation age. 40Ar/39Ar dating of K-feldspar gives plateau ages in the range 375-365 Ma, consistent with resetting during mylonitisation from west-over-east thrusting during the Tabberabberan event.|425.2 +/- 3.5 Ma; Lennox et al. (2014).|||Intrudes Adaminaby Group, Walli Volcanics and Coombing Formation.|Foliated, porphyritic biotite granite with K-feldspar megacrysts up to 100 mm diameter; locally mylonitised. S-type.|03-MAY-16
20699|Wyangala Granite|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Sow. On Boorowa 1:100 000 mapsheet portion of Time-Space Plot.||Hovells Suite|||Medium-coarse grained, equigranular-porphyritic, commonly megacrystic, generally foliated cordierite-muscovite-biotite granite and granodiorite; high K, Th and U response.|
20699|Wyangala Granite|70297|5|Briefly described|map legend|Silurian|Silurian|||Wyangala Supersuite||||
20699|Wyangala Granite|70545|5|Briefly described|Map Legend |Devonian|Silurian|||Hovells Suite|||Medium-coarse grained, equigranular-porphyritic, commonly megacrystic, generally foliated cordierite-muscovite-biotite granite and granodiorite; high K, Th and U response.|
20699|Wyangala Granite|70727|4|Described|p170-174,176,182-184,186-187|Silurian|Silurian|Geological province: Hill End Zone, Eastern Lachlan Orogen. The type pluton of the Hovell Suite. Emplaced along pre-existing faults (Lennox et al., 2005) and foliation planes in country rock 425+\-3.5 Ma (Lennox and Zwingmann, 2007; Lennox et al., 2014). Eastern margin of the granite consists of high strain shear zones (Part of Wyangala Fault; Pogson and Watkins, 1998), separated by granite with lower strain (Czarnota, 2002; Lennox et al., 2010; White and Lennox, 2010). Comprises S and C foliations. C foliations likely due to Wyangala Fault movement (380 Ma, Tabberabberan Orogeny, 40Ar-39Ar dating; Glen et al., 1999, Foster et al., 1999). Underwent solid-state ductile deformation and dynamic recrystallisation under transitional greenschist-amphibolite facies to lower amphibolite facies conditions with little or no apparent contribution from prior magmatic or sub-magmatic strain of the rock forming minerals.||||Intrudes into Ordovician metasediments e.g. Adaminaby Group, Walli Volcanics, Coombing Formation.|Paramagnetic ilmenite-bearing, S/marginal I type two-mica- to mainly biotite-granite with different biotite contents and local chlorite alteration.|02-AUG-19
20699|Wyangala Granite|73299|6|Mentioned|p1107 Fig.12|||Wyangala Batholith mentioned on p1106, Ar-Ar ages of 380-360 Ma determined for deformation.||||||
20699|Wyangala Granite|73431|6|Mentioned|p365, p367 Tb.1, p372|Silurian|Silurian|Lachlan Orogen.|425.2+/-3.5 Ma zircon U/Pb SHRIMP|||||
20701|Wyangala Supersuite|23551|5|Briefly described|p491|||||||||
20701|Wyangala Supersuite|41563|6|Mentioned|p512|||||||||
20701|Wyangala Supersuite|66713|6|Mentioned|p5, p12|||Contains Hovells Suite.||||||
20701|Wyangala Supersuite|68592|2|Defined|p651, p1253-78, p1356-7, p1545-7, p1664|Early Devonian|Late Silurian|Of Chappell et al. (1988), who originally included the Dalgety and Wyangala Suites. Work by Blevin (2011) has led to the recognition that other plutons belong to this group, and so the old name Wyangala Suite is abandoned in favour of the new name, Hovells Suite. The Hovells Suite is the type Suite. Geochemistry detailed.  All plutons show thin-section evidence of pervasive strain; some granites have broad protomylonitic zones recording W-over-E thrust movement. Some plutons intrude Late Silurian rocks, rather than Ordovician as previously suggested. Some units host W mineralisation.|||Includes Dalgety, Shannons Flat and Hovells Suites.|Intrudes Adaminaby Group, Kenyu Formation. Is intruded by Bishopthorpe Suite.|Predominantly cream to grey, medium- to coarse-grained, massive to foliated, equigranular to porphyritic (often megacrystic) granite to granodiorite. S-type.|
20701|Wyangala Supersuite|70297|4|Described|map legend, on side 2 of map sheet|Ludlow|Ludlow|Age: mid to late Silurian (Wenlock to Pridoli) for Wyangala Supersuite and Bullenbalong Supersuite.|||Wyangala Granite, Whistle Waa Granite, Bigga Granite||Reduced, unfractionated, foliated S-type biotite granite, porphyritic granite, leucogranite; scattered xenoliths and mafic enclaves.|
20701|Wyangala Supersuite|70727|5|Briefly described|p171|||Geological province: Hill End Zone, Eastern Lachlan Orogen. Constitutes the majority of the Wyangala Batholith plutions and comprises 3 suites and 23 plutons (Thomas and Pogson, 2012).|||Includes Hovell Suite.|||
20711|Wylies Flat Coal Member|23717|5|Briefly described|p117 Tb.1|Permian|Permian|Parent: Pinegrove Formation.   Geological Province: Sydney Basin||||||
20711|Wylies Flat Coal Member|24157|5|Briefly described|p188 Tb.1|Permian|Permian|Parent: Pinegrove Formation. Geological Province: Sydney Basin||||||
20711|Wylies Flat Coal Member|29942|3|Fully described|p11|||||||||
20711|Wylies Flat Coal Member|68004|5|Briefly described|p51 Table 5.|Late Permian|Late Permian|Upper Hunter Coalfield.||Unit in Pinegrove Formation.||Overlies Glengowan Shale Member. Is overlain by Hambledon Hill Sandstone Member.||
20736|Yabba Granite|23309|5|Briefly described|p102, 294, 343, 350,447.||Late Silurian|(G172) S-Type. Age 418+/-4 Ma [probably Rb/Sr from Steele, 1993 PhD]. Supersedes Yabba Adamellite.||||||09-DEC-16
20736|Yabba Granite|24551|6|Mentioned|p233, 717 Table 2.4|Early Devonian|Silurian|Age: 411 +/- 3Ma. Of the Cooma Supersuite.||||||
20736|Yabba Granite|32684|6|Mentioned|p250|||See also Fig.2||||||
20736|Yabba Granite|35278|6|Mentioned|p358|||||||||
20736|Yabba Granite|38580|6|Mentioned|Fig.2|||||||||
20736|Yabba Granite|39860|6|Mentioned|p17|||Muscovite-biotite adamellite: quartz, perthitic K-feldspar, plagioclase, biotite and muscovite with accessory cordierite and sillimanite; contains abundant sedimentary xenoliths.||||||30-NOV-04
20736|Yabba Granite|42726|5|Briefly described|map legend|Silurian||Variation on Yabba Granite, Vic.||||||
20736|Yabba Granite|68115|5|Briefly described|p7.|||Omeo Zone. Now includes the Lockhart Granite. On previous maps, they had been separated by a fault which, when restored, produces one intrusion.||||||
20736|Yabba Granite|68116|5|Briefly described|Appendix, Map 20.|Wenlock|Llandovery||||||Biotite-muscovite granite: weakly to strongly foliated; consists of quartz, perthitic K-feldspar, plagioclase, red-brown biotite and muscovite, with accessory cordierite and sillimanite; abundant metasedimentary enclaves; S-type.|
20742|Yackandandah Granite|22971|5|Briefly described|p 22, 28|Early Devonian||Age: 380+/-15Ma.||||||
20742|Yackandandah Granite|23309|5|Briefly described|p343.|Devonian|Devonian|G177 I-Type. Age: 392+/-7Ma, 389+/-15Ma, 380+/- 15 Ma. Supersedes Yackandandah Porphyritic Granite and Yackandandah Basin Granite.||||||24-JAN-07
20742|Yackandandah Granite|24551|6|Mentioned|p229|||Of the Tabberabbera Province.||||||
20742|Yackandandah Granite|31713|6|Mentioned|p6|||||||||
20742|Yackandandah Granite|37029|6|Mentioned|p48|||||||||
20742|Yackandandah Granite|37871|4|Described|p9|||||||||
20742|Yackandandah Granite|38879|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Middle to Lower Devonian||||||
20742|Yackandandah Granite|39446|5|Briefly described|p22|||||||||
20742|Yackandandah Granite|39858|6|Mentioned|Map legend|Early Devonian|Early Devonian|||||||
20742|Yackandandah Granite|40761|6|Mentioned|p241|||||||||
20742|Yackandandah Granite|41321|4|Described|p223|||||||||
20742|Yackandandah Granite|41572|6|Mentioned|p19|||||||||
20742|Yackandandah Granite|42089|6|Mentioned|p19|||||||||
20742|Yackandandah Granite|42726|5|Briefly described|map legend|Early Devonian||||||||
20742|Yackandandah Granite|42791|5|Briefly described|p212|||see also Fig.1 p204.||||||24-JAN-07
20742|Yackandandah Granite|42827|6|Mentioned|p19|||||||||
20742|Yackandandah Granite|50086|5|Briefly described|p10 Fig. 5|Early Devonian|Early Devonian|Geological Province:  Lachlan Fold Belt.||||||
20742|Yackandandah Granite|61163|3|Fully described|p111-115, p37 Tb. 6.2, p130|Middle Devonian|Early Devonian|Classified variously as Yackandandah and Mudgeegonga Granites (King 1982) representing its two phases; and Yackandandah, Mudgeegonga and Bruarong adamellites (Lightbody 1984). Concentric layered, mafic I-type intrusive. Intruded Pinnak Sst. Age: 392+/-7Ma||||||19-FEB-13
20742|Yackandandah Granite|61174|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: porphyritic phase (biotite-hornblende granite) and equigranular phase (biotite granite), with a gradational boundary between these two phases; GSV map code: G177a and G177b respectively; I-type intrusion.||||||07-FEB-11
20742|Yackandandah Granite|61175|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: porphyritic phase (biotite-hornblende granite) and equigranular phase (biotite granite), with a gradational boundary between these two phases; GSV map code: G177a and G177b respectively; I-type intrusion.||||||
20742|Yackandandah Granite|61176|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: porphyritic phase (biotite-hornblende granite) and equigranular phase (biotite granite), with a gradational boundary between these two phases; GSV map code: G177a and G177b respectively; I-type intrusion.||||||
20742|Yackandandah Granite|61177|5|Briefly described|map legend|Early Devonian|Early Devonian|Subdivided into two informal phases: porphyritic phase (biotite-hornblende granite) and equigranular phase (biotite granite), with a gradational boundary between these two phases; GSV map code: G177a and G177b respectively; I-type intrusion.||||||
20742|Yackandandah Granite|61178|5|Briefly described|map legend|Early Devonian|Early Devonian|Two informal phases: porphyritic phase (biotite-hornblende granite, 392+/-7Ma [K-Ar]) and equigranular phase (biotite granite, 391+/-7Ma [K-Ar]); mostly gradational boundary between phases. I-type. GSV map code: G177a and G177b respectively.||||||
20742|Yackandandah Granite|61186|5|Briefly described|p45 Fig. 14|||Victorian dimension stone - two main types of granite include: a grey coarse-grained porphyritic granite with white feldspars up to 5cm and some xenoliths; and a medium-grained, even-textured, light grey granite in the Mudgeegonga area.||||||
20742|Yackandandah Granite|68115|5|Briefly described|p7.|||Omeo Zone. Now includes the Mudgeegonga Granite. Magnetic imagery show they are parts of the same concentrically zoned pluton. There are two phases: coarse-grained porphyritic and medium-grained equigranular.||||||
20742|Yackandandah Granite|68116|5|Briefly described|Appendix, Map 19, 26.|Early Devonian|Early Devonian|Informally subdivided into equigranular and porphyritic phases, separated by a gradational boundary.|||||Biotite granite: grey leucocratic; medium to fine-grained; equigranular. Biotite-hornblende granite (porphyritic): grey; coarse-grained; with phenocrysts of K-feldspar commonly aligned to form a flow fabric; rare ovoid microdiorite enclaves.|
20742|Yackandandah Granite|71040|6|Mentioned|p19|Early Devonian|Early Devonian|Displaced by the sinistral strike-slip Kancoona Fault, reactivated by the Tabberabberan Orogeny.||||||
20742|Yackandandah Granite|71206|6|Mentioned|p384|||Lachlan Fold Belt.||||||
20743|Yadboro Conglomerate|22591|4|Described|p 63, Fig 4||Late Carboniferous|Max. thickness 180m.||||||17-MAR-09
20743|Yadboro Conglomerate|22857|5|Briefly described|p532 App.1 Tb.A1.9|Early Permian|Early Permian|Interpreted as part of the Shoalhaven Group by Tye, Fielding and Jones (1996) - formerly placed in the Talaterang Group. See also p504 App.1 Tb.A1.8.||||||
20743|Yadboro Conglomerate|22969|5|Briefly described|Fig 2.2||Early Permian|Shoalhaven Group.||||||17-MAR-09
20743|Yadboro Conglomerate|24079|5|Briefly described|p430|Late Carboniferous|Late Carboniferous|Of Talaterang Group. Geological Province: Sydney Basin.||||||
20743|Yadboro Conglomerate|24552|5|Briefly described|p9|Sakmarian|Sakmarian|Of Shoalhaven Group. Geological Province: Southern Sydney Basin.||||||07-FEB-11
20743|Yadboro Conglomerate|29752|6|Mentioned|p16|||||||||
20743|Yadboro Conglomerate|29992|6|Mentioned|Map legend|Permian|Permian|||||||
20743|Yadboro Conglomerate|29994|6|Mentioned|Map legend|Permian|Permian|||||||
20743|Yadboro Conglomerate|31081|4|Described|p54|||||||||
20743|Yadboro Conglomerate|31128|6|Mentioned|p5|||Also mention on Table 1.||||||
20743|Yadboro Conglomerate|31277|6|Mentioned|p1|||||||||
20743|Yadboro Conglomerate|31298|3|Fully described|p9|||||||||
20743|Yadboro Conglomerate|32671|6|Mentioned|Map legend|Carboniferous|Carboniferous|||||||
20743|Yadboro Conglomerate|32769|6|Mentioned|Fig.1|||||||||
20743|Yadboro Conglomerate|32945|6|Mentioned|p84|||Permian||||||
20743|Yadboro Conglomerate|34039|6|Mentioned|p355|||||||||
20743|Yadboro Conglomerate|34059|6|Mentioned|Map legend|Permian|Permian|||||||
20743|Yadboro Conglomerate|34211|6|Mentioned|p32|||||||||
20743|Yadboro Conglomerate|34333|6|Mentioned|p356|||||||||
20743|Yadboro Conglomerate|34334|4|Described|p360|||||||||
20743|Yadboro Conglomerate|35145|6|Mentioned|Fig.2|||||||||
20743|Yadboro Conglomerate|35490|6|Mentioned|Fig.2|||Stratigraphic distribution of crinoids||||||
20743|Yadboro Conglomerate|36042|6|Mentioned|Table 1|||||||||
20743|Yadboro Conglomerate|36207|6|Mentioned|Text Fig.2|||||||||
20743|Yadboro Conglomerate|37924|5|Briefly described|p488|||||||||
20743|Yadboro Conglomerate|39287|6|Mentioned|p20|||See also Fig.2.5||||||
20743|Yadboro Conglomerate|39289|6|Mentioned|Fig. 4.1|||||||||
20743|Yadboro Conglomerate|39290|6|Mentioned|p83|||See also P88||||||
20743|Yadboro Conglomerate|42821|6|Mentioned|p46|||||||||
20743|Yadboro Conglomerate|43383|14|Not recorded|p20|||||||||
20743|Yadboro Conglomerate|43465|14|Not recorded|Map Legend||Permian|||||||
20743|Yadboro Conglomerate|43479|14|Not recorded|p189,218||Artinskian|||||||
20743|Yadboro Conglomerate|43981|2|Defined|p3,19||Permian|||||||
20743|Yadboro Conglomerate|45090|5|Briefly described|p140|||||||||
20743|Yadboro Conglomerate|46849|6|Mentioned|p197|||||||||
20743|Yadboro Conglomerate|60281|5|Briefly described|p57|Permian|Permian|Of Shoalhaven Gp. Thin fluvioglacial drainage deposits. Disconformably overlies Pigeon House Ck. Sltst.  Along with Tallong Conglom., these infilled channels are lateral equivs. of Pebbley Beach and Snapper Pt. Fms. Geol.Prov: Sydney Basin||||||22-MAR-05
20743|Yadboro Conglomerate|60285|4|Described|p181|Sakmarian|Sakmarian|Of the Shoalhaven Group. Can be lithostatigraphically correlated with Pebbley Beach Formation. Basin margin alluvial apron. Geological Province: Sydney Basin.||||||
20743|Yadboro Conglomerate|60386|6|Mentioned|p296|Artinskian|Artinskian|Bowen/Sydney Basin. Deltaic - nearshore - shelf.||||||
20743|Yadboro Conglomerate|61315|6|Mentioned|p176|||Localised terrestrial sediments at base of basin. Geological Province: Sydney Basin||||||
20743|Yadboro Conglomerate|61612|6|Mentioned|p270, p270 Fig. 1|Early Permian|Early Permian|Geological Province: Sydney Basin.||||||17-MAR-09
20743|Yadboro Conglomerate|62043|5|Briefly described|pp437-438.  |Early Permian|Early Permian|Southern Sydney Basin. Exhibits abrupt lateral facies and thickness variations.||Unit in Shoalhaven Group.||Is overlain by Yarrunga Coal Measures.|Stacked alluvial conglomerates and sandstones; local thick, areally restricted coal bodies.|
20743|Yadboro Conglomerate|63461|5|Briefly described|p862 Fig. 1c|||Geological Province: Sydney Basin.||||||10-DEC-07
20743|Yadboro Conglomerate|63773|5|Briefly described|p1058 Fig. 2|Early Permian|Early Permian|Of Shoalhaven Group. Geological Province: Sydney Basin.||||||07-APR-09
20743|Yadboro Conglomerate|63832|5|Briefly described|p131 fig 2|Cisuralian|Cisuralian|Of Sydney Basin. Sixth (P2) glaciation.||Unit in Shoalhaven Group.||||14-DEC-17
20743|Yadboro Conglomerate|64631|6|Mentioned|p44 Fig.2.|Artinskian|Sakmarian|Sydney Basin.||Unit in lower Shoalhaven Group.||||
20743|Yadboro Conglomerate|64877|5|Briefly described|p295-296|Permian|Permian|SW Sydney Basin. Alluvial deposits.||Shoalhaven Group.||||
20743|Yadboro Conglomerate|66577|6|Mentioned|p997 Fig.2.|Permian|Permian|||Unit in Shoalhaven Group.||Overlain by Snapper Point Formation.||
20743|Yadboro Conglomerate|68592|6|Mentioned|p1779, p1786|Permian|Permian|||Unit in Shoalhaven Group.||||
20743|Yadboro Conglomerate|69297|6|Mentioned|p501, p502 fig 5.43|Kungurian|Artinskian|Sydney Basin.||Shoalhaven Group||Overlies and interfingers with the Wasp Head Formation, Tallong Conglomerate and the Pebbly Beach Formation. Overlain by and interfingers with the Snapper Point Formation.||
20743|Yadboro Conglomerate|70661|6|Mentioned|p139, p143|||||||Interfingers with Snapper Point Formation, correlates with Tallong Conglomerate, overlies Clyde Coal Measures||
20743|Yadboro Conglomerate|71538|6|Mentioned|p54 fig 2|Artinskian|Artinskian|Sydney Basin. Alluvial-braidplain deposit.||Shoalhaven Group||Unconformably overlies the Wasp Head Formation. Disconformably overlain by the Pebbley Beach Formation, Mount Agony Formation and the Snapper Point Formation.||
20743|Yadboro Conglomerate|73421|6|Mentioned|p2 Fig.1|||Sydney Basin, southern.||||||
20747|Yagon Siltstone|22500|6|Mentioned|p 7|||||||||
20747|Yagon Siltstone|22736|6|Mentioned|p629|Namurian|Visean|||||||
20747|Yagon Siltstone|22857|4|Described|p241, p512 App.1 Tb.A1.8|Late Carboniferous|Early Carboniferous|Fossiliferous dark siltstone; minor interbeds of mudstone and fossiliferous sandstone; upper portion has mudstone and volcanic beds. Max. thickness: 1100m. Geological Province: Kullatine-Yagon-Booral Shelf.||||||23-SEP-18
20747|Yagon Siltstone|22863|6|Mentioned|p241|||||||||
20747|Yagon Siltstone|23157|5|Briefly described|p110 fig2,7,8|Carboniferous|Carboniferous|||||||
20747|Yagon Siltstone|24118|5|Briefly described|p3|||||||||
20747|Yagon Siltstone|32388|6|Mentioned|p127|||||||||
20747|Yagon Siltstone|32868|6|Mentioned|p212|||||||||
20747|Yagon Siltstone|36057|2|Defined|p347|Westphalian|Namurian|Namurian - Westphalian||||||
20747|Yagon Siltstone|36528|6|Mentioned|p179|||See also P180.||||||
20747|Yagon Siltstone|38801|6|Mentioned|Fig.3|||||||||
20747|Yagon Siltstone|39660|6|Mentioned|p450|||||||||
20747|Yagon Siltstone|40883|6|Mentioned|p2|||||||||
20747|Yagon Siltstone|42547|4|Described|p37|||||||||
20747|Yagon Siltstone|44093|5|Briefly described|p231 App. 1|Early Permian|Late Carboniferous|Geological Province: New England Fold Belt.||||||
20747|Yagon Siltstone|44244|2|Defined|p209-216|Westphalian|Visean|Synonymous with "Crawford Formation".  Includes the Violet Hill Volcanic Member.  Overlies the Booti Booti Sandstone.  Max. thickness: 1100m.  Type section in text.  Geological Province: Myall Block.||||||30-AUG-04
20747|Yagon Siltstone|47056|6|Mentioned|Fig.2 P523|||||||||
20747|Yagon Siltstone|50132|5|Briefly described|p248  Fig.6|Namurian|Namurian|Early Namurian age.||||Overlies the Booti Booti Sandstone. Underlies the Koolanock Sandstone.||27-MAR-12
20747|Yagon Siltstone|50263|5|Briefly described|Map Legend|Westphalian|Namurian|Overlies: Booti Booti Sandstone.  Underlies: Koolanock Sandstone.  Includes: Violet Hill Volcanic Member.  Geological Province: Eastern Myall Block.||||||
20747|Yagon Siltstone|63832|5|Briefly described|p131 Fig.2, p134|Serpukhovian|Serpukhovian|Eastern Myall Block, southern New England Fold Belt. Earliest glaciation (C1) of Late Devonian-early Mississippian. The middle-to-upper units mark the end of Glaciation C1.|||||Contains an interval of dispersed gravel and glendonites among strongly soft-sediment-deformed mudrocks; this is overlain by a thick unit of undeformed, bedded marine mudrocks and sandstones.|14-DEC-17
20747|Yagon Siltstone|64631|5|Briefly described|p44 Fig.2, p47.|Serpukhovian|Visean|Southern New England Fold Belt, eastern Myall Block. Earliest evidence for Permo-Carboniferous Ice Age in eastern Australia. Biostratigraphic age control for base and top.||||Overlies Booti Booti Sandstone.|Shelfal mudstones, strongly soft-sediment deformed, with an interval containing dispersed gravel and glendonites.|
20747|Yagon Siltstone|65380|4|Described|p660 Table 1, p670, p672 Table 3|Pennsylvanian|Visean|Tamworth Belt. Includes brachiopod faunas of late Visean to Westphalian age below the Violet Hill Volcanic Member (331 Ma). Maximum depositional age from detrital zircon sample high in the unit: 323 Ma.|||Violet Hill Volcanic Member|Also called Blueys Beach Formation by Skilbeck and Cawood (1994).|Volcaniclastic sandstone.|26-MAR-12
20747|Yagon Siltstone|65382|4|Described|p714|Serpukhovian|Visean|Age from the Violet Hills Member (330.6 +/- 4.6 Ma Roberts et al., 1995), and by brachiopods of the Visean/Namurian Marginirugus barringtonensis and Levipustula levis Zones, which the article states are equivalent to 327 Ma.||||||23-SEP-18
20747|Yagon Siltstone|69793|6|Mentioned|p1121 Fig.12|Serpukhovian|Visean|Myall Block, Tamworth Belt.||||||
20747|Yagon Siltstone|73264|6|Mentioned|p1396 Fig.18|Carboniferous|Carboniferous|New England Orogen.||||||
20747|Yagon Siltstone|73487|6|Mentioned|p567, p568 Fig.3, p577|Serpukhovian|Serpukhovian|Shown as Yagon p566.||||||
20763|Yalgo Rhyolite Member|22857|5|Briefly described|p444 App.1, Tb.A1.6|Early Devonian|Early Devonian|Of the Baledmund Formation (Kopyje Group, Cobar Supergroup). Rhyolite flows. Geological Province: Kopyje Shelf (Darling Basin).||||||
20763|Yalgo Rhyolite Member|35287|6|Mentioned|p7|||||||||
20763|Yalgo Rhyolite Member|39618|6|Mentioned|Table 9|||||||||
20763|Yalgo Rhyolite Member|41528|2|Defined|p44|Early Devonian||||||||
20763|Yalgo Rhyolite Member|41529|6|Mentioned|Map legend|Lochkovian||||||||
20763|Yalgo Rhyolite Member|42566|2|Defined|p65|Early Devonian|Early Devonian|Age: mid Early Devonian. Originally included in Babinda Volcanics.||Baledmund Formation.|||Discontinuous series of silicic lava flows - porphyritic, blue-grey, rhyolitic. Fine pyrite is prevalent.|24-SEP-19
20763|Yalgo Rhyolite Member|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
20777|Yalmy Group|22530|5|Briefly described|p695||Early Silurian|||||||
20777|Yalmy Group|22628|6|Mentioned|fig1p108|Silurian|Silurian|||||||
20777|Yalmy Group|22704|6|Mentioned|p49||Early Silurian|||||||
20777|Yalmy Group|22708|6|Mentioned|p210|||||||||
20777|Yalmy Group|22815|4|Described|p33,124 fig10|Llandovery|Llandovery|Age: Mid to late Llandovery.||||||
20777|Yalmy Group|22832|6|Mentioned|p637|Early Silurian|Early Silurian|||||||
20777|Yalmy Group|22857|4|Described|p113, p420 App. 1 Tb. A1.5|Early Silurian|Early Silurian|Coarse-grained arenite, siltstone with Llandovery graptolites, thin to thick bedded sandstone.||||||27-JUN-14
20777|Yalmy Group|22866|6|Mentioned|p494|Llandovery|Llandovery|Age: Late Llandovery.||||||
20777|Yalmy Group|22876|4|Described|p15|Early Silurian|Early Silurian|440-430Ma||||||
20777|Yalmy Group|22877|5|Briefly described|map|Silurian|Silurian|||||||
20777|Yalmy Group|22878|5|Briefly described|p29|Early Silurian|Early Silurian|||||||
20777|Yalmy Group|22933|6|Mentioned|p20|||||||||
20777|Yalmy Group|22968|4|Described|P19, P30, P106||Early Silurian|Age of unit is 440-430 Ma, lateral equivalent of Towanga Sandstone and Seldom Seen Formation, maximum thickness 2500m.||||||25-SEP-08
20777|Yalmy Group|23020|5|Briefly described|Map legend|Llandovery|Llandovery|||||||
20777|Yalmy Group|23021|5|Briefly described|Map legend|Llandovery|Llandovery|Overlying unit is the Omeo Metamorphic Complex||||||
20777|Yalmy Group|23028|5|Briefly described|Map legend|Llandovery|Llandovery|||||||
20777|Yalmy Group|23029|5|Briefly described|Map legend|Llandovery|Llandovery|Overlying unit is the Omeo Metamorphic Complex||||||
20777|Yalmy Group|23030|5|Briefly described|Map legend|Silurian|Silurian|||||||
20777|Yalmy Group|23229|5|Briefly described|Table3-2p21||Bolindian|||||||
20777|Yalmy Group|23245|6|Mentioned|p113,134||Early Silurian|||||||
20777|Yalmy Group|23307|5|Briefly described|Map Legend|Silurian|Silurian|||||||
20777|Yalmy Group|23309|5|Briefly described|Table 2.30. p63, 75, 83-88, 303-304.|Early Silurian|Early Silurian|||||||
20777|Yalmy Group|23454|5|Briefly described|p28|Llandoverian|Llandoverian|||||||
20777|Yalmy Group|23564|5|Briefly described|p1442|Llandovery|Llandovery|||||||
20777|Yalmy Group|23615|3|Fully described|p73, p20 Fig.6|Llandovery|Llandovery|Overlies Akuna Mudstone.  Age:440-430Ma.  Regarded as lateral equivalent to Seldom Seen Conglomerate and Towanga Sandstone.||||||
20777|Yalmy Group|23938|6|Mentioned|p11, p31-32 Fig. 12.|Silurian|Silurian|Marine deposits: sandstone, siltstone. See also p59-61 Figs.21-22, p96, p103 Fig. 43, p139 Tb. 1 Appendix.||||||
20777|Yalmy Group|24002|5|Briefly described|p228 Fig.2|Silurian|Silurian|||||||
20777|Yalmy Group|24004|5|Briefly described|p280|Early Silurian|Early Silurian|||||||
20777|Yalmy Group|24098|6|Mentioned|p27 Fig. 2|Wenlockian|Llandoverian|Geological Province: Lachlan Fold Belt.||||||
20777|Yalmy Group|24164|6|Mentioned|p15 Fig.8|Silurian|Silurian|Deep marine.|||||Sandstone, shale, conglomerate|
20777|Yalmy Group|24551|4|Described|p131|Early Silurian|Early Silurian|Sub-divided into 3 informal units; Sy1. Sy2 and Sy3.||||||
20777|Yalmy Group|24600|5|Briefly described|p481|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
20777|Yalmy Group|38151|6|Mentioned|Table 1|||||||||
20777|Yalmy Group|39447|6|Mentioned|Fig.2|||||||||
20777|Yalmy Group|40126|6|Mentioned|p14|||||||||
20777|Yalmy Group|40136|5|Briefly described|p43|||||||||
20777|Yalmy Group|40761|5|Briefly described|p226|||Mention P224||||||
20777|Yalmy Group|41570|6|Mentioned|p92|||||||||
20777|Yalmy Group|41572|5|Briefly described|p21|||||||||
20777|Yalmy Group|41585|5|Briefly described|p131|||||||||
20777|Yalmy Group|41905|2|Defined|p23|Early Silurian||||||||
20777|Yalmy Group|41933|5|Briefly described|Map legend|Llandovery||||||||
20777|Yalmy Group|42294|6|Mentioned|p24|||||||||
20777|Yalmy Group|42627|5|Briefly described|Map legend|Wenlock||||||||
20777|Yalmy Group|42647|2|Defined|p22||Llandovery|||||||
20777|Yalmy Group|42827|4|Described|p129|||see also Table 4.1||||||
20777|Yalmy Group|43206|5|Briefly described|map legend||Llandovery|||||||
20777|Yalmy Group|43228|5|Briefly described|p9||Early Silurian|||||||
20777|Yalmy Group|43233|5|Briefly described|Map Legend||Llandovery|||||||
20777|Yalmy Group|43312|5|Briefly described|Map Legend||Llandovery|||||||
20777|Yalmy Group|43313|5|Briefly described|Map Legend||Llandovery|||||||
20777|Yalmy Group|43314|5|Briefly described|Map Legend||Llandovery|||||||
20777|Yalmy Group|43315|5|Briefly described|Map Legend|Llandovery|Llandovery|||||||03-MAY-05
20777|Yalmy Group|44092|5|Briefly described|map legend|Early Silurian|Early Silurian|Slf2||||||
20777|Yalmy Group|44093|5|Briefly described|p190 App. 1|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt.||||||
20777|Yalmy Group|44184|5|Briefly described|Map Legend||Early Silurian|||||||
20777|Yalmy Group|44185|5|Briefly described|Map legend.|Early Silurian|Early Silurian||||||Marine: sandstone, thick- to thin-bedded, siltstone.|
20777|Yalmy Group|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
20777|Yalmy Group|60503|5|Briefly described|p27, p28 Fig. 9|Early Silurian|Early Silurian|Includes the Towanga Sandstone and Seldon Seen Formation.||||||
20777|Yalmy Group|60541|3|Fully described|p54-55|Early Silurian|Early Silurian|Thick sequence of sandstone and mudstone divided into 3 component units: Sy-1, Sy-2 and Sy-3 (detailed lithology for each included); poorly fossiliferous. Age within the `Early Silurian deep marine sedimentation¿ period: 440-430Ma. See also p19 Tb. 1, p30.||||||16-AUG-18
20777|Yalmy Group|60542|4|Described|p48, p11 Fig. 2|Early Silurian|Early Silurian|Divided into: basal coarse-grained sandstone, middle predominantly siltstone and upper dominant quartzitic sandstone. Age: 440-430Ma.||||||
20777|Yalmy Group|60988|6|Mentioned|p144 Fig.1||||||||Undifferentiated sandstone, siltstone, shale.|
20777|Yalmy Group|61160|6|Mentioned|p48|||Concordantly overlies the Bendoc Group (east and southeast).||||||
20777|Yalmy Group|61161|6|Mentioned|p34|Llandovery|Llandovery|Deposition at end of the Llandovery (Early Silurian).||||||
20777|Yalmy Group|61163|5|Briefly described|p13, p86|Early Silurian|Early Silurian|Geological Province: Lachlan Fold Belt (Omeo Zone).||||||
20777|Yalmy Group|61181|6|Mentioned|p195|Silurian|Silurian|Includes interbedded carbonates where wollastonite fills cavities and replaces limestone clasts in gritstone.||||||
20777|Yalmy Group|61187|5|Briefly described|p5 Fig.3, p26 Fig.2, p29 Fig.4. |Early Silurian|Late Ordovician|Mallacoota Zone, Benambra Terrane. Correlative of Springfield, Chintin and Anderson Creek Formations in the Melbourne Zone, Melbourne Terrane.||||||
20777|Yalmy Group|61762|6|Mentioned|p18|||||||||
20777|Yalmy Group|61964|5|Briefly described|p25 Fig. 8|Llandovery|Llandovery|Unit in Victoria overlying the Bendoc Group.||||||
20777|Yalmy Group|62070|5|Briefly described|p34 Fig.1,|Early Silurian|Early Silurian|Sedimentary rocks.||||||
20777|Yalmy Group|63277|6|Mentioned|p140|||||||||
20777|Yalmy Group|63290|4|Described|p388, p391, p395, p403|Llandovery|Llandovery|Includes Towanga Sandstone,Tantangara Formation, Tombong beds, Merriangaah Siltstone Tidbinbilla Formation and Ryrie Sandstone. Benambran unconformity lies above this unit. Consists of turbidites.||||||
20777|Yalmy Group|66181|6|Mentioned|p307|||Quartzites forming high peaks (Mt. Tower 1315m).||||||
20777|Yalmy Group|67322|6|Mentioned|p16|Early Silurian|Late Ordovician|New Country Sandstone is viewed as the local transition into the Yalmy or Cobbannah Group sandstones of the Early Silurian.||||||22-FEB-18
20777|Yalmy Group|67802|6|Mentioned|p29||Early Silurian|In Benambra Terrane.|||||Turbiditic quartz-rich sandstone and siltstone.|
20777|Yalmy Group|68116|5|Briefly described|Appendix, Maps 28, 36, 45.|Llandovery|Llandovery||||Includes Seldom Seen Formation and Towanga Sandstone.||Sandstone, siltstone: thick to thin bedded; sandstone mostly quartzarenite and quartzite with some litharenite; deep-marine turbidite deposits.|
20777|Yalmy Group|68592|5|Briefly described|p13, p16, p420|Llandovery|Llandovery|VandenBerg, Nott and Glen (1992). Derived from erosion of a deformed and uplifted backarc region.|||||Quartzose sediments.|
20777|Yalmy Group|70601|5|Briefly described|p25, p43|Llandovery|Llandovery|Albury-Bega Basin: Inland Zone.||||Unconformably overlies Akuna Mudstone, Bogolo Formation. Unconformably underlies Bredbo Group.|Sedimentary rocks.|
20777|Yalmy Group|70684|6|Mentioned|p9 Fig.4(g,h)|Early Silurian|Early Silurian|||||||
20777|Yalmy Group|70718|5|Briefly described|p44|Silurian|Silurian|Wagga-Omeo Zone, Murray Basin. Deposited as a deep marine turbidite sequence.|c. 440-430 Ma||||Sandstone, mudstone and conglomereate.|
20777|Yalmy Group|71069|6|Mentioned|p74|||||||Conformably overlies the Bendoc Group.||
20777|Yalmy Group|71700|5|Briefly described|p10|||Derived from sediments shed off the Wagga-Omeo Zone during the Benambran Orogeny.||||||
20777|Yalmy Group|73186|6|Mentioned|p229, Fig.2|Llandovery|Llandovery|Tabberabera Zone and Omeo Zone.|||||Turbidites.|
20777|Yalmy Group|73264|5|Briefly described|p1390, p1392 Fig.14|Llandovery|Llandovery|Lachlan Orogen, eastern. Likely derived from reworked Ordovician turbidites.|||||Quartz-rich turbidites.|
20784|Yalwal Volcanics|22857|5|Briefly described|p213-214|Late Devonian|Middle Devonian|Rhyolites and basalts. Overlain by the Merrimbula Group. Geological Province: Lambie Basin.||||||
20784|Yalwal Volcanics|22859|6|Mentioned|p213-14|||||||||
20784|Yalwal Volcanics|32126|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|Prob.Middle Devonian||||||
20784|Yalwal Volcanics|32127|4|Described|p250|||Refers Wall (1965 unpubl.)||||||
20784|Yalwal Volcanics|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
20784|Yalwal Volcanics|32672|6|Mentioned|p673|||||||||
20784|Yalwal Volcanics|36390|6|Mentioned|Map legend|Middle Devonian|Middle Devonian|||||||
20784|Yalwal Volcanics|36391|6|Mentioned|p144|||Also P145-149||||||
20784|Yalwal Volcanics|66300|6|Mentioned|p52, 58 pp70-75.|Late Devonian|Late Devonian||||Includes Grassy Gully Rhyolite Member.|Is intruded by Bundundah Granite.||29-OCT-13
20784|Yalwal Volcanics|70661|3|Fully described|vii, viii, p14, p95-p103|Late Devonian|Middle Devonian|Budawang Syncline, Major part of the Eden-Comerong-Yalwal Volcanic Zone. Rocks of this formation were previously included in the Eden Rhyolite, Lochiel Formation, Boyd Volcanic Complex. Also includes one unnamed informal basalt unit. Distribution, depositional environment, relationships, structure, metamorphism, geochemistry, geophysical characteristics and fossil assemblage described in detail.Exposed discontinuously in some valleys. Estimated to have a maximum thickness of 1060m-1220m. Lithology discussed further and in detail.  Historic gold mines present in the area. Intruded by Bundundah Granite, Sloping Rock Monzogranite. Unconformably overlain by Shoalhaven Group. See also p109, p114, p130, p134.|384.5 +/-4.4 Ma (U/Pb SHRIMP)||Grassy Gully Rhyolite Member|Correlated with Boyd Volcanic Complex, Comerong Volcanics, Unconformably (or disconformably) and gradationally overlain by Bellbird Creek Formation,  Merrimbula Group.|Clastic sedimentary rocks,Brecciated bimodal volcanic and volcaniclastic rocks (carbonaceous and tuffaceous sandstone, siltstone and conglomerate). Sandstone, siltstone, pebbly sandstone, polymictic pebble conglomerate and mudstone.|
20784|Yalwal Volcanics|71303|5|Briefly described|map legend|Givetian|Givetian|Ungrouped.|||Includes Grassy Gully Rhyolite Member.||Quartzose sandstone, siltstone, mudstone, conglomerate; rare current bedding, macroflora; strongly silicified locally. Includes volcaniclastic rocks and hornfels. Rare mafic + felsic dykes or sills. Intercalated with mafic + felsic volcanic rocks.|
20787|Yamba Formation|22531|6|Mentioned|p6|||||||||
20787|Yamba Formation|22773|5|Briefly described|p339|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|22782|4|Described|p17|||||||||
20787|Yamba Formation|22799|3|Fully described|p55|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|22857|5|Briefly described|p339|Holocene|Late Pleistocene|Lacustrine and lunette sediments with gypsum deposits. Geological Province: Murray Basin.||||||
20787|Yamba Formation|23818|5|Briefly described|p212 Fig.108|Recent|Recent|Geological Province: Great Artesian Basin and Murray Basin.||||||
20787|Yamba Formation|23908|6|Mentioned|p6|||Overlies Gawler Craton rocks.||||||04-NOV-10
20787|Yamba Formation|23921|5|Briefly described|p1109 Table 1|Quaternary|Quaternary|Geological Province: Murray Basin.||||||
20787|Yamba Formation|24358|5|Briefly described|p32 Fig.1|||||||||04-NOV-10
20787|Yamba Formation|24551|5|Briefly described|p388 Fig. 11.2, 340|Holocene|Middle Pleistocene|Overlies Blanchetown Clay.||||||02-JUL-13
20787|Yamba Formation|24574|6|Mentioned|p706|||||||||
20787|Yamba Formation|30581|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20787|Yamba Formation|30751|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|30753|4|Described|p15|||Recent age||||||
20787|Yamba Formation|30754|2|Defined|Appendix 1|Recent|Recent|||||||
20787|Yamba Formation|30755|6|Mentioned|p169|||Tectonic map||||||
20787|Yamba Formation|30756|6|Mentioned|p2|||||||||
20787|Yamba Formation|30807|6|Mentioned|p101|||Suggested map symbol||||||
20787|Yamba Formation|30922|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|30934|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|30935|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|31312|6|Mentioned|p70|||||||||
20787|Yamba Formation|31320|6|Mentioned|Fig.1|||Quaternary||||||
20787|Yamba Formation|31741|6|Mentioned|p6|||||||||
20787|Yamba Formation|31745|6|Mentioned|Map legend|Recent|Recent|||||||
20787|Yamba Formation|31747|6|Mentioned|Map legend|Quaternary|Quaternary|||||||
20787|Yamba Formation|31850|4|Described|p40|||||||||
20787|Yamba Formation|32426|6|Mentioned|p142|||Stratigraphic table. Renmark area.||||||
20787|Yamba Formation|32435|6|Mentioned|Fig.1|||||||||
20787|Yamba Formation|32437|6|Mentioned|Fig.2|||||||||
20787|Yamba Formation|32438|6|Mentioned|Fig.2|||||||||
20787|Yamba Formation|34180|6|Mentioned|p212|||Recent||||||
20787|Yamba Formation|34536|6|Mentioned|Map legend|Recent|Recent|Equivalent||||||
20787|Yamba Formation|34965|6|Mentioned|p417|||||||||
20787|Yamba Formation|35029|6|Mentioned|p166|||||||||
20787|Yamba Formation|35097|6|Mentioned|Fig.4|||||||||
20787|Yamba Formation|35200|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|35232|5|Briefly described|Table.4|||||||||
20787|Yamba Formation|35272|5|Briefly described|p284|||||||||
20787|Yamba Formation|35772|6|Mentioned|p13|||||||||
20787|Yamba Formation|37873|5|Briefly described|p4|||||||||
20787|Yamba Formation|38068|5|Briefly described|p79|||||||||
20787|Yamba Formation|40215|6|Mentioned|p56|||||||||
20787|Yamba Formation|40448|6|Mentioned|p43|||||||||
20787|Yamba Formation|40941|6|Mentioned|Map legend|Holocene|Holocene|||||||
20787|Yamba Formation|40942|4|Described|p23|||||||||
20787|Yamba Formation|41499|6|Mentioned|p70|||||||||
20787|Yamba Formation|41848|5|Briefly described|p359|Recent|late Quaternary|Overlies Blanchetown Clay||||||
20787|Yamba Formation|41868|6|Mentioned|p571|||||||||
20787|Yamba Formation|42125|6|Mentioned|p139|||||||||
20787|Yamba Formation|42126|6|Mentioned|Fig.8 P155|||||||||
20787|Yamba Formation|42134|4|Described|p339|||||||||
20787|Yamba Formation|42136|4|Described|Table 1 P364|||||||||
20787|Yamba Formation|42292|6|Mentioned|Fig.1 P9|||||||||
20787|Yamba Formation|42466|6|Mentioned|Map Legend|||||||||
20787|Yamba Formation|42475|6|Mentioned|p26|||||||||
20787|Yamba Formation|42716|5|Briefly described|Map legend|Holocene||||||||
20787|Yamba Formation|42717|5|Briefly described|map legend|Holocene||||||||
20787|Yamba Formation|42738|5|Briefly described|map legend|Quaternary||||||||
20787|Yamba Formation|42827|5|Briefly described|p359|||see also Table 9.1||||||
20787|Yamba Formation|42881|6|Mentioned|Fig.2, P83|||||||||
20787|Yamba Formation|42966|1|Redefined|p252|Holocene|Late Pleistocene|||||||
20787|Yamba Formation|43049|5|Briefly described|p27|||||||||
20787|Yamba Formation|43053|5|Briefly described|Map Legend|Holocene|Holocene|||||||25-MAY-05
20787|Yamba Formation|43073|5|Briefly described|Table 4|||||||||
20787|Yamba Formation|43258|5|Briefly described|Map Legend||Holocene|||||||
20787|Yamba Formation|43298|5|Briefly described|Map Legend||Holocene|||||||
20787|Yamba Formation|43655|5|Briefly described|p40-846|||||||||
20787|Yamba Formation|43669|4|Described|p23-24|||||||||
20787|Yamba Formation|44133|5|Briefly described|p252|Holocene|Middle Pleistocene|Parts equivalent to Tyrrell Beds. Geological Province: Murray Basin.||||||
20787|Yamba Formation|44191|5|Briefly described|Map Legend||Late Pleistocene|||||||
20787|Yamba Formation|44660|14|Not recorded|map legend|||Recent, lithology.||||||
20787|Yamba Formation|44864|6|Mentioned|Map Legend||Holocene|||||||
20787|Yamba Formation|49038|5|Briefly described|p32|||||||||
20787|Yamba Formation|60005|5|Briefly described|Map legend|Holocene|Pleistocene|Aeolianites and evaporites: fine-grained gypsum.||||||11-JAN-10
20787|Yamba Formation|60953|5|Briefly described|Map Legend|Holocene|Pleistocene|||||||
20787|Yamba Formation|61070|6|Mentioned|Map Legend|Quaternary|Quaternary|||||||12-JAN-10
20787|Yamba Formation|61108|5|Briefly described|map legend|Quaternary|Quaternary|Lacustrine gypsiferous, saline and organic clay, silt and sand of modern playas and lakes.||||||
20787|Yamba Formation|62893|4|Described|Map Legend, p24-25|Holocene|Holocene|Lacustrine and aeolian; represents inland lakes occupying depressions in the Bridgewater Formation.|||||Halite, gypsite, gypsarenite, selenite and minor carbonate and gypsiferous mud.|
20787|Yamba Formation|65552|6|Mentioned|p23 App.2|Quaternary|Quaternary|Murray Basin unit. Hosts gypsum resources.||||||
20787|Yamba Formation|65715|5|Briefly described|p15 Tb.8, p25|Neogene|Neogene|Defined by Firman (1966).||||||
20787|Yamba Formation|66002|5|Briefly described|p13 Tb.9|Neogene|Neogene|Defined by Firman 1966.||||||
20787|Yamba Formation|67179|4|Described|p581, p582|Holocene|Pleistocene|Late Pleistocene to Holocene, deposited on the beds of saline lakes. Up to 1.5 m thick in Lake Tuchewop.|||||Friable gypsiferous clay, pelletal clay, gypsum-quartz sand aggregates and gypsum (Brown and Stevenson 1991), halite.|
20787|Yamba Formation|68116|5|Briefly described|Appendix, Maps 1-11, 14-16, 21, 22, 29.|Holocene|Pleistocene|Late Pleistocene maximum age.  Lacustrine evaporite deposits.|||||Pale grey gypsite, gypsiferous clay and grey pelletal gypsum-quartz sand aggregates; locally includes grey clay with crystalline gypsum mush under black sulphide-rich mud with ephemeral crusts of gypsum, halite, bischofite, thenardite and mirabilite.|
20787|Yamba Formation|68131|5|Briefly described|p71, p84|Holocene|Pleistocene|Flinders Island, Nuyts Domain, Gawler Craton.||||||
20787|Yamba Formation|70334|5|Briefly described|p74|||Modern saline playa deposits, occurring behind the Saint Kilda Formation at the head of False Bay.|||||Gypsiferous clay and gypsum-quartz sand mixtures and gypsum associated with dunes of seed and flour gypsum.|
20787|Yamba Formation|70337|5|Briefly described|Map legend.|Holocene|Pleistocene||||||Clay, lacustrine, gypsiferous, gypsum-quartz sand. Dunes, playa lakes.|
20787|Yamba Formation|73188|6|Mentioned|p320|Pleistocene|Pleistocene|Murray Basin.|||||Alluvial fans, clay, sand, gravel, wind-blown sand.|
20787|Yamba Formation|73496|5|Briefly described|Map legend|Holocene|Holocene||||||Evaporitic and associated clay deposits in topographic lows; nonmagnetic; low to high K, Th, U depending on water content.|
20793|Yammatree Granite|22638|1|Redefined|p46|Early Silurian||||||||
20793|Yammatree Granite|42726|5|Briefly described|map legend|||||||||
20793|Yammatree Granite|44192|5|Briefly described|Map Legend|Wenlockian|Llandoverian|||||||
20793|Yammatree Granite|44936|5|Briefly described|Map Legend||Silurian|||||||
20793|Yammatree Granite|50191|6|Mentioned|p21 Fig. 1|Silurian|Silurian|||||||
20793|Yammatree Granite|69801|6|Mentioned|p2, p4-p5, p52-57, p138|Devonian|Devonian|Eastern Lachlan Orogen. Occurs east of Junee. Previously mapped as Ulandra Granite (Brunker et al., 1970; Warren et al., 1995). Previously regarded as S-type granite by Chappell et al, 1991. Sample locality, petrography, SHRIMP analyses and interpretation are detailed. This unit is the sole member of the Yammatree Suite.|417.9 +/- 1.8 Ma (SHRIMP)|Yammatree Suite||Intrudes the Frampton Volcanics.|weathered and altered, medium-grained, I-type granite.|
20793|Yammatree Granite|73215|5|Briefly described|p994|||Tumut Trough.|418 +/- 2 Ma (Bodorkos et al.,2015).|||||
20809|Yancowinna Subgroup|22772|4|Described|p66,Table13.1|Cryogenian|Cryogenian|||||||
20809|Yancowinna Subgroup|22857|5|Briefly described|p66, Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Torrowangee Group. Age: ~700Ma. Max. thickness: 200m. See also p398 App. 1 Tb.A1.3.||||||
20809|Yancowinna Subgroup|36733|6|Mentioned|Table 5|||||||||
20809|Yancowinna Subgroup|37238|6|Mentioned|p355|||||||||
20809|Yancowinna Subgroup|38157|6|Mentioned|p261|||||||||
20809|Yancowinna Subgroup|40294|6|Mentioned|p48|||||||||
20809|Yancowinna Subgroup|41405|5|Briefly described|p203|||||||||
20809|Yancowinna Subgroup|42531|5|Briefly described|Map legend|Adelaidean||||||||
20809|Yancowinna Subgroup|43265|5|Briefly described|Map Legend||Neoproterozoic|Of the Torrowangee Group.||||||11-SEP-07
20809|Yancowinna Subgroup|62724|5|Briefly described|p17 Fig. 4|Sturtian|Sturtian|Of the Torrowangee Group. Geological Province: Broken Hill Domain.||||||07-FEB-11
20809|Yancowinna Subgroup|63489|5|Briefly described|Map legend|Adelaidean|Adelaidean|Diamictite, siltstone, sandstone, minor carbonate. South Australia equivalent is Yudnamutana Subgroup.||||||10-SEP-07
20809|Yancowinna Subgroup|68277|6|Mentioned|p96|Neoproterozoic|Neoproterozoic|The rank is not given in the text.||||||
20809|Yancowinna Subgroup|70000|5|Briefly described|p34, p39|Neoproterozoic|Neoproterozoic|||Unit in Torrowangee Group.|Includes McDougalls Well Conglomerate; Mulcatcha, Yangalla and Waukeroo Formations.|Is overlain by Euriowie Subgroup.|Diamictite (tillite), conglomerate, quartz sandstone and well-bedded siltstone/sandstone successions with abundant glacial clasts.|
20809|Yancowinna Subgroup|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Torrowangee Group.|Includes McDougalls Well Conglomerate; Mulcatcha, Yangalla and Waukeroo Formations.|Is overlain by Euriowie Subgroup.|Poorly sorted grit, sandstone, diamictite and siltstone, minor carbonate.|
20812|Yandaminta Quartzite|12066|5|Briefly described|p13|||||||||
20812|Yandaminta Quartzite|22857|5|Briefly described|p122, p408 App. 1 Tb. A1.4.|Ordovician|Cambrian|Quartzite and silty shale. Geological Province: Mount Arrowsmith Block.||||||
20812|Yandaminta Quartzite|23245|5|Briefly described|p122|Ordovician|Cambrian|||||||
20812|Yandaminta Quartzite|23469|5|Briefly described|p 319|||||||||
20812|Yandaminta Quartzite|23735|5|Briefly described|p129|Early Ordovician|Early Ordovician|Age: Mid-Arenig (Late Bedigonian to Chewtonian) is indicated.||||||
20812|Yandaminta Quartzite|35118|6|Mentioned|Fig.5|||||||||
20812|Yandaminta Quartzite|38692|6|Mentioned|p138|||||||||
20812|Yandaminta Quartzite|40136|5|Briefly described|p43|||||||||
20812|Yandaminta Quartzite|40810|5|Briefly described|p14|||[Originally entered for NT. CEBMar95]||||||
20812|Yandaminta Quartzite|41810|6|Mentioned|p111|||||||||
20812|Yandaminta Quartzite|44093|5|Briefly described|p142 App. 1|Early Ordovician|Cambrian|Geological Province: Kanmantoo Fold Belt.||||||
20812|Yandaminta Quartzite|62787|5|Briefly described|p77|Early Ordovician|Early Ordovician|Of Mutawintji Group. Conformably overlian by Tabita Formation.||||||07-FEB-11
20812|Yandaminta Quartzite|62793|6|Mentioned|p271|Early Ordovician|Early Ordovician|Near Mount Arrowsmith. Contains diverse assemblage of conodonts.||||||
20812|Yandaminta Quartzite|63489|5|Briefly described|Map legend|Devonian|Silurian|Mudstone, quartzite, minor limestone.||||||
20812|Yandaminta Quartzite|63793|6|Mentioned|p24. |||||||||
20812|Yandaminta Quartzite|64671|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|West of Mount Arrowsmith this unit is faulted against Cambrian formations and western Kara beds.||||||26-NOV-08
20812|Yandaminta Quartzite|64687|5|Briefly described|Map Legend|Early Ordovician|Early Ordovician|Faulted and unconformable against Cambrian formations and western Kara beds.||||||
20812|Yandaminta Quartzite|66623|3|Fully described|p73, pp152-157.|Early Ordovician|Early Ordovician|Correlative with Wheeney Creek Formation; contemporaneous with lower Rowena Formation. Forms high, narrow wall-like ridges. Thickness varies from 65 m to c.200 m. Contains conodonts, the mollusc Janospira, and well-preserved Anthoceras sp. Deposited with fluctuating sea-levels and sediment input.||Unit in Pimbilla Tank Group.||Unconformably overlies or is faulted against Wyarra Shale and Wydjah Formation. A similar division of opinion relates to the boundary with the Kara Formation. Is overlain by Tabita Formation.|Quartzite, generally white, medium-grained and well-sorted, mostly massive; conglomerate; grey-green mudstones with carbonate concretions in the middle of the unit; fine-grained red sandstones grading into quartzite.|
20812|Yandaminta Quartzite|66917|5|Briefly described|Map legend|Early Ordovician|Early Ordovician|||Unit in Pimbilla Tank Group.||Is overlain by Tabita Formation.|Boldly outcropping interbedded cross-bedded quartzite; fossiliferous, cleaved, grey mudstone; and red fine-grained sandstone.|
20812|Yandaminta Quartzite|66929|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
20812|Yandaminta Quartzite|66933|6|Mentioned|Map legend|Ordovician|Ordovician|||||||
20812|Yandaminta Quartzite|67208|5|Briefly described|Map legend.|Early Ordovician|Early Ordovician|||Unit in Pimbilla Tank Group.|||Boldly outcropping interbedded cross-bedded quartzite; fossiliferous, cleaved, grey mudstone and red fine-grained sandstone.|
20812|Yandaminta Quartzite|67322|4|Described|p10, p12; Fig.5|Floian||Warris (1967). Thickness varies along strike from 200m to 65m, possibly due to faulting along the lower boundary with the Wyarra Shale. Shallow marine shelf deposits. Age from conodont fauna in carbonate nodules.||Basal unit of the Pimbilla Tank Group.||Unconformably overlies/ faulted over Wyarra Shale. Overlain by the Tabita Formation.|Predominantly quartzite, generally massive but locally cross-bedded, and grading to conglomerate at its northern limit of outcrop. Grey-green shales containing carbonate nodules are common in the middle to upper part of the unit.|22-FEB-18
20812|Yandaminta Quartzite|67562|6|Mentioned|p112|||||||||24-JAN-17
20820|Yangalla Formation|22772|5|Briefly described|Table13.1|Cryogenian|Cryogenian|||||||
20820|Yangalla Formation|22857|5|Briefly described|Tb. 13.1 (insert p70-71)|Sturtian|Sturtian|Of the Yanocowinna Subgroup (Torrowangee Group). Boulder beds, lenticular interbedded siltstone, sandstone. Age: ~700Ma. Geological Province: Adelaide Fold Belt. See also p398 App. 1 Tb.A1.3.||||||
20820|Yangalla Formation|30261|4|Described|Table 1|||Sturtian age||||||
20820|Yangalla Formation|34812|3|Fully described|p70|||||||||
20820|Yangalla Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
20820|Yangalla Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
20820|Yangalla Formation|36733|6|Mentioned|Table 5|||||||||
20820|Yangalla Formation|37931|4|Described|p532|||||||||
20820|Yangalla Formation|38157|6|Mentioned|p261|||||||||
20820|Yangalla Formation|39214|6|Mentioned|Table 1|||||||||
20820|Yangalla Formation|41405|5|Briefly described|p204|||||||||
20820|Yangalla Formation|43265|5|Briefly described|Map Legend||Neoproterozoic|of Yancowinna Subgroup.||||||
20820|Yangalla Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Yancowinna Subgroup.||||
20820|Yangalla Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Yancowinna Subgroup.||Overlies Mulcatcha Formation. Is overlain by Euriowie Subgroup.|Bedded siltstone and sandstone, coarsening-upwards; the unit is rich in glacial clasts and erosional contacts occur throughout.|07-SEP-15
20830|Yaouk Leucogranite|12185|5|Briefly described|map legend|Devonian|Silurian|Of Murrumbidgee Batholith. Leucogranite. BMR map symbol: gmy.||||||
20830|Yaouk Leucogranite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
20830|Yaouk Leucogranite|31580|6|Mentioned|p272|||See also Table 1-4 analysis||||||
20830|Yaouk Leucogranite|31581|3|Fully described|p182|||See also Fig. 1 & analysis Table 1||||||
20830|Yaouk Leucogranite|32905|6|Mentioned|p224|||||||||
20830|Yaouk Leucogranite|32906|6|Mentioned|Fig.1|||||||||
20830|Yaouk Leucogranite|34544|6|Mentioned|p186|||||||||
20830|Yaouk Leucogranite|35109|4|Described|p80|||||||||
20830|Yaouk Leucogranite|36413|6|Mentioned|p83|||||||||
20830|Yaouk Leucogranite|36443|5|Briefly described|map legend|Late Silurian|Late Silurian|Of Murrumbidgee Batholith. Intrusive. Porphyritic coarse leucogranite, aplite, fine leucogranite. S-type. BMR map code: Smy.||||||
20830|Yaouk Leucogranite|44092|5|Briefly described|map legend|Silurian|Silurian|gab2||||||
20830|Yaouk Leucogranite|45003|14|Not recorded|p13|||||||||
20830|Yaouk Leucogranite|45147|3|Fully described|M196|||||||||
20830|Yaouk Leucogranite|46574|5|Briefly described|Map Legend|Early Devonian|Silurian|Of the Murrumbidgee Batholith. Geological Province: Lachlan Pre-Cratonic Province.||||||09-NOV-04
20830|Yaouk Leucogranite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
20837|Yar Sandstone|22857|4|Described|p440 App.1, Tb.A1.6|Emsian|Pragian|Of the Walters Range Group (Cobar Supergroup). Planar laminated and cross-bedded, medium-grained quartz-rich arenite. Max. thickness: >400m. Geological Province: Darling Basin.||||||
20837|Yar Sandstone|41395|6|Mentioned|Map legend|Pragian||||||||
20837|Yar Sandstone|61964|3|Fully described|p14 Fig. 4, p106|Pragian|Pragian|Of Walters Range Group. Sandstone, pebbly sandstone + minor conglomerate sequence of 4 unnamed units. Conformable on Lumgi Siltstone (KILPARNEY sheet). Gradationally (conformable) overlain by Scotts Craig Conglomerate. Age: <411.2Ma. Thickness: >520m.||||||
20837|Yar Sandstone|62405|5|Briefly described|Map legend|Early Devonian|Early Devonian|Of the Walters Range Group. Thick bedded, fine- to coarse-grained quartz-rich sandstone, medium to large scale trough cross bedding.||||||13-OCT-08
20837|Yar Sandstone|69163|5|Briefly described|Map legend|Early Devonian|Early Devonian|||Unit in Walters Range Group.|||Thick-bedded, fine- to coarse-grained quartz-rich sandstone, medium- to large-scale trough cross-bedding.|
20837|Yar Sandstone|69164|5|Briefly described|Map legend|Early Devonian|Early Devonian|Four facies are mapped as separate but un-named sub-units.||Unit in Walters Range Group.||Is overlain by Scotts Craig Conglomerate.|Thick-bedded, fine- to coarse-grained quartz-rich sandstone, medium- to large-scale trough cross-bedding.|
20837|Yar Sandstone|70751|6|Mentioned|p12|Pragian|Pragian|||Walters Range Group||||
20837|Yar Sandstone|72958|6|Mentioned|p11|Emsian|Pridoli|Cobar Basin. Nymagee area.||Walters Range Group||Underlain by and equivalent to Lumga Siltstone. Equivalent to Whoey Tank Formation and Winduck Group. Overlain by Crowl Creek Formation (Mulga Downs Group).||
20839|Yard Coal|23055|6|Mentioned|Fig4p11|||||||||
20839|Yard Coal|23717|5|Briefly described|p118 Fig 2|Permian|Permian|Parent: Lambton Formation.   Geological Province: Sydney Basin||||||
20839|Yard Coal|39292|6|Mentioned|Fig.6.6|||||||||
20839|Yard Coal|39308|6|Mentioned|Fig.23.4|||||||||
20839|Yard Coal|39609|5|Briefly described|p3|||||||||
20839|Yard Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Yard coal seam instead. See also p113.||Of Lambton Subgroup||||
20839|Yard Coal|73304|6|Mentioned|p75|||||Lambton Formation, Newcastle Coal Measures||||
20859|Yarra Granite|42027|4|Described|p649|||See also p702.||||||24-JUN-08
20859|Yarra Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Grey to pink foliated to protomylonitic porphyritic biotite granite, minor dolerite.||||||
20859|Yarra Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Whick Whack Suite. Pinkish to grey, medium- to coarse-grained, foliated to protomylonitic, equigranular to weakly porphyritic biotite granite. Low K, Th and U radioelement response.||||||
20859|Yarra Granite|68592|2|Defined|p1466,p1471,p1482, p1508, p1523-6, p1664|Early Devonian|Early Devonian|First mapped and named (after Yarra property) by Gibson (1973) and first published by Tobisch and Paterson (1990). Assigned to the Whick Whack Suite by Blevin (2011). Type pluton of Whick Whack Suite. The southern pluton is here named Asylum Granite and assigned to the Crooked Corner Suite. Type locality described. Has strongly developed, partly protomylonitic, foliation dipping to W. Geochemistry and geophysical properties described.|415 +/- 8 Ma (SHRIMP U-Pb zircon: Bodorkos,2012).|Unit in Whick Whack Suite.||Intrudes Cuddyong Formation. Is intruded by Bishopthorpe Suite.|Pinkish to grey, medium- to coarse-grained, equigranular to weakly porphyritic biotite granite; minor phase of similar, fine-grained biotite-quartz syenite. A-type.|
20859|Yarra Granite|70192|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Dwy. Includes one unnamed member of fine grained, protomylonitic, porphyritic biotite-quartz syenite. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Whick Whack Suite|Includes one unnamed member.||Medium-coarse grained, foliated-protomylonitic, equigranular-weakly porphyritic biotite granite; low K, Th and U response. Low magnetic susceptibility.|
20859|Yarra Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed member of fine grained, protomylonitic, porphyritic biotite-quartz syenite.||Whick Whack Suite|Includes one unnamed member||Medium-coarse grained, foliated-protomylonitic, equigranular-weakly porphyritic biotite granite; low K, Th and U response. Low magnetic susceptibility.|
20864|Yarrabandai Formation|22831|3|Fully described|p 46|Lochkovian|Lochkovian|Previously refered to as Trundle Beds.||||||14-NOV-13
20864|Yarrabandai Formation|22857|4|Described|p448 App.1, Tb.A1.6|Lochkovian|Pridolian|Of the Derriwong Group. Fine to medium-grained, flaggy, planar-bedded arenite; contains brachiopods, trilobites, tentaculites. Max. thickness: 900m. Geological Province: Bogan Gate Terrace.||||||
20864|Yarrabandai Formation|23522|5|Briefly described|p253|Devonian|Devonian|||||||
20864|Yarrabandai Formation|24417|3|Fully described|p73|Lochkovian|Lochkovian|Of Derriwong Group.  Parts formerly mapped as unnamed members of the "Wallingalair beds".  Overlain by Coonardoo Sandstone; underlain by Cookeys Plains Formation.||||||
20864|Yarrabandai Formation|36066|5|Briefly described|p10|||||||||
20864|Yarrabandai Formation|39660|2|Defined|p453|Early Devonian|Early Devonian|||||||
20864|Yarrabandai Formation|42456|6|Mentioned|p8|||in Derriwong Group||||||
20864|Yarrabandai Formation|43441|5|Briefly described|27|Early Devonian|Late Silurian|||||||08-JAN-10
20864|Yarrabandai Formation|44160|5|Briefly described|Map Legend||Lochkovian|||||||08-JAN-10
20864|Yarrabandai Formation|50299|5|Briefly described|Map Legend|Devonian|Silurian|Of the Derriwong Group.||||||
20864|Yarrabandai Formation|50554|5|Briefly described|Map legend|Devonian|Silurian|Of the Derriwong Group.  Cross-bedded pebbly sandstone.||||||
20864|Yarrabandai Formation|60009|5|Briefly described|Map Legend|Lochkovian|Lochkovian|Of the Derriwong Group.||||||13-JUL-04
20864|Yarrabandai Formation|61894|6|Mentioned|p179 Fig.3|||||||||
20879|Yarralumla Formation|5252|6|Mentioned|p86||Ludlovian|||||||
20879|Yarralumla Formation|12185|5|Briefly described|map legend|Upper Silurian|Upper Silurian|Of Red Hill Group. Calcareous shale and sandstone, fossiliferous limestone. BMR map symbol: Suy.||||||
20879|Yarralumla Formation|13996|6|Mentioned|p143|Silurian|Silurian|Canberra area. A gastropod mentioned.||||||
20879|Yarralumla Formation|22768|6|Mentioned|p176|||||||||
20879|Yarralumla Formation|22857|4|Described|p176, p462 App.1 Tb.A1.6|Ludlovian|Ludlovian|Overlain by Deakin Volcanics. Calcareous tuffaceous mudstone and siltstone; minor beds of limestone, quartz arenite. Max. thickness: 300m.||||||
20879|Yarralumla Formation|24248|6|Mentioned|p67|||||||||
20879|Yarralumla Formation|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
20879|Yarralumla Formation|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20879|Yarralumla Formation|31019|6|Mentioned|Map legend|Silurian|Silurian|||||||
20879|Yarralumla Formation|31111|6|Mentioned|p138|||Also mention P140, 144, 146.||||||
20879|Yarralumla Formation|31284|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20879|Yarralumla Formation|31852|6|Mentioned|Fig. 5|||Ludlovian||||||
20879|Yarralumla Formation|33325|5|Briefly described|Table 2|||See also Table 3.||||||
20879|Yarralumla Formation|33328|4|Described|Table 1|||See also p5 & 14.||||||29-SEP-16
20879|Yarralumla Formation|34405|5|Briefly described|Table 3.5|||||||||
20879|Yarralumla Formation|35110|6|Mentioned|Fig.3|||||||||
20879|Yarralumla Formation|35614|5|Briefly described|p6|||||||||
20879|Yarralumla Formation|36413|6|Mentioned|Table 2|||||||||
20879|Yarralumla Formation|36633|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20879|Yarralumla Formation|37013|6|Mentioned|p27|||||||||
20879|Yarralumla Formation|37141|5|Briefly described|Plan 6|||||||||
20879|Yarralumla Formation|37348|6|Mentioned|p97|||||||||
20879|Yarralumla Formation|37728|4|Described|Table 2|||||||||
20879|Yarralumla Formation|37752|6|Mentioned|p105|||||||||
20879|Yarralumla Formation|38035|6|Mentioned|p91|||||||||
20879|Yarralumla Formation|38664|5|Briefly described|p6|||See also P12||||||
20879|Yarralumla Formation|39331|6|Mentioned|p50|||||||||
20879|Yarralumla Formation|39947|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20879|Yarralumla Formation|39975|4|Described|p123|||||||||
20879|Yarralumla Formation|40328|3|Fully described|p118|||||||||
20879|Yarralumla Formation|40689|6|Mentioned|p4|||||||||
20879|Yarralumla Formation|41356|5|Briefly described|p63|||See also P29 and P84||||||
20879|Yarralumla Formation|42497|5|Briefly described|Map Legend|Wenlockian|Wenlockian|||||||
20879|Yarralumla Formation|42727|5|Briefly described|map legend|Ludlow|Ludlow|Calcareous and tuffaceous mudstone and siltstone; minor limestone, calc-silicate hornfels and quartz sst. Over Mount Painter Volcanics; intruded by Federal Golf Course Tonalite. BMR map symbol: Suy. Geol. Prov: Canberra Block.||||||23-AUG-12
20879|Yarralumla Formation|42820|2|Defined|p30|early Ludlow||of Laidlaw Volcanic Suite. Age early Late Silurian (early Ludlow)||||||
20879|Yarralumla Formation|42994|6|Mentioned|p19|||||||||
20879|Yarralumla Formation|43158|6|Mentioned|3|||||||||
20879|Yarralumla Formation|43159|6|Mentioned|Fig.2p4,p6.||Late Silurian|||||||
20879|Yarralumla Formation|43344|14|Not recorded|p110,113,115,116||Late Silurian|||||||
20879|Yarralumla Formation|43385|14|Not recorded|p171,172|||L.Ludlow||||||
20879|Yarralumla Formation|43481|6|Mentioned|3,5,11|||||||||
20879|Yarralumla Formation|44970|14|Not recorded|p1,34,38-9,42-46,48,||Late Silurian|p79,80,89,95,map. Unit of Red Hill Group||||||
20879|Yarralumla Formation|45147|6|Mentioned|M164|||||||||
20879|Yarralumla Formation|47037|6|Mentioned|p107|||||||||
20879|Yarralumla Formation|48971|6|Mentioned|p9|||See also P17.||||||
20879|Yarralumla Formation|49043|5|Briefly described|p7|||||||||
20879|Yarralumla Formation|49690|6|Mentioned|p27 |||Canberra region.||||||
20879|Yarralumla Formation|68592|6|Mentioned|p428, p443, p477, p502|||Opik (1958). Canberra area. Equivalent to, but not yet formally included in, the Douro Group.||||||
20879|Yarralumla Formation|73215|5|Briefly described|p994, 1002|||Canberra area.||||Overlies Hawkins Volcanic Suite. Is overlain by Laidlaw Volcanic Suite. May be equivalent to the Talmo Formation.||25-JAN-23
20888|Yarrangobilly Limestone|13996|6|Mentioned|p130|Silurian|Silurian|One of several occurrences of the cosmopolitan conodont Ozarkodina crispa.||||||
20888|Yarrangobilly Limestone|22687|6|Mentioned|118|||Geol province Lachlan Fold Belt||||||
20888|Yarrangobilly Limestone|22857|5|Briefly described|p454 App.1, Tb.A1.6|Silurian|Silurian|Massive limestone. Max. thickness: 450m. Geological Province: Tumut Trough.||||||10-MAR-06
20888|Yarrangobilly Limestone|29456|6|Mentioned|p432|||||||||
20888|Yarrangobilly Limestone|29648|6|Mentioned|Fig.2|||||||||
20888|Yarrangobilly Limestone|29992|6|Mentioned|Map legend|Silurian|Silurian|||||||
20888|Yarrangobilly Limestone|29994|6|Mentioned|Map legend|Late Silurian|Late Silurian|||||||
20888|Yarrangobilly Limestone|30247|6|Mentioned|p1120|||Upper Silurian belodelliform conodonts elements.||||||
20888|Yarrangobilly Limestone|30252|6|Mentioned|p183|||20579||||||
20888|Yarrangobilly Limestone|30253|6|Mentioned|Fig.1|||||||||
20888|Yarrangobilly Limestone|31161|5|Briefly described|PA6|||||||||
20888|Yarrangobilly Limestone|32583|6|Mentioned|p371|||||||||
20888|Yarrangobilly Limestone|32671|6|Mentioned|Map legend|Silurian|Silurian|||||||
20888|Yarrangobilly Limestone|32672|6|Mentioned|p672|||||||||
20888|Yarrangobilly Limestone|33325|5|Briefly described|Table 2|||Mention P11.||||||
20888|Yarrangobilly Limestone|33611|6|Mentioned|p132|||||||||
20888|Yarrangobilly Limestone|34405|4|Described|p116|||||||||
20888|Yarrangobilly Limestone|34692|5|Briefly described|p187|||||||||
20888|Yarrangobilly Limestone|35244|6|Mentioned|p36|||||||||
20888|Yarrangobilly Limestone|37727|4|Described|p95|||See also P8.||||||
20888|Yarrangobilly Limestone|38230|5|Briefly described|p474|||Palaeontology||||||
20888|Yarrangobilly Limestone|40298|6|Mentioned|Table II|||||||||
20888|Yarrangobilly Limestone|40328|6|Mentioned|p21|||See also P43||||||
20888|Yarrangobilly Limestone|40497|6|Mentioned|Map legend|Silurian|Silurian|||||||
20888|Yarrangobilly Limestone|40498|6|Mentioned|p425|||||||||
20888|Yarrangobilly Limestone|41869|6|Mentioned|p9|||||||||
20888|Yarrangobilly Limestone|42033|6|Mentioned|p650|||||||||
20888|Yarrangobilly Limestone|42313|6|Mentioned|p126|Ludlovian||||||||
20888|Yarrangobilly Limestone|43383|14|Not recorded|p12|||||||||
20888|Yarrangobilly Limestone|44092|5|Briefly described|map legend|Late Silurian|Late Silurian|Ss1||||||
20888|Yarrangobilly Limestone|45147|6|Mentioned|M128|||See also M136||||||
20888|Yarrangobilly Limestone|50088|5|Briefly described|p472|Late Silurian|Late Silurian|Contains Belodella anomalis fossils (conodonts).||||||24-FEB-05
20888|Yarrangobilly Limestone|50095|5|Briefly described|p121|Ludlow|Ludlow|Contains type specimen of Belodella Anomalis (conodont). NSW.||||||11-FEB-08
20888|Yarrangobilly Limestone|60078|6|Mentioned|Map Legend|Late Silurian|Late Silurian|||||||
20888|Yarrangobilly Limestone|60086|5|Briefly described|Map legend|Late Silurian|Late Silurian|Massive limestone.||||||
20888|Yarrangobilly Limestone|60332|6|Mentioned|p952|||Contains original specimen of Belodella anomalis (conodont)||||||
20888|Yarrangobilly Limestone|68592|6|Mentioned|p454|||Considered to overlie 'Goobarragandra Porphyry' by Adamson (in Booker, Rayner, Hall et al., 1960); presence of numerous thrust faults makes this questionable.||||||29-SEP-16
20896|Yarrimie Formation|721|5|Briefly described|Map legend|Frasnian|Givetian|Of the Tamworth Group.  Green-grey to black, siliceous, radiolarian siltstone and mudstone, with local radiolarian and biohermal limestone lenses ans sparse lithic wacke beds.||||||
20896|Yarrimie Formation|5178|6|Mentioned|p113|||Misspelling of Yarramie Formation? [This is the correct spelling!]||||||16-APR-12
20896|Yarrimie Formation|5254|5|Briefly described|p121, p122 Fig.1, p124|Middle Devonian|Early Devonian|Member of Tamworth Group. Includes Moore Creek Limestone Member. Lithologies include tuff, argillite, limestone, rudite and siltstone. Overlain by Baldwin Formation?||||||
20896|Yarrimie Formation|22736|6|Mentioned|p630|||||||||
20896|Yarrimie Formation|22750|5|Briefly described|p 228||Middle Devonian|Tamworth Group||||||
20896|Yarrimie Formation|22768|6|Mentioned|p182-83|||||||||
20896|Yarrimie Formation|22857|4|Described|p182, p482 App.1 Tb.A1.6|Middle Devonian|Middle Devonian|Upper part of Tamworth Group. Max. thickness: 1500m. Geological Province: Tamworth Forearc Basin.||||||
20896|Yarrimie Formation|23185|6|Mentioned|Fig1p156|Frasnian|Givetian|||||||
20896|Yarrimie Formation|23522|5|Briefly described|p249 Fig 5|Late Devonian|Early Devonian|||||||
20896|Yarrimie Formation|24009|5|Briefly described|p368 Fig.1|Late Devonian|Middle Devonian|Maximum thickness: ~1200m||||||
20896|Yarrimie Formation|30649|5|Briefly described|p77|||||||||
20896|Yarrimie Formation|30650|3|Fully described|p313|||||||||
20896|Yarrimie Formation|30814|6|Mentioned|p71|||||||||
20896|Yarrimie Formation|30911|6|Mentioned|Map legend|Devonian|Devonian|||||||
20896|Yarrimie Formation|31999|5|Briefly described|p150|||||||||
20896|Yarrimie Formation|32482|6|Mentioned|Map legend|Middle Devonian|Early Devonian|Lower to Middle Devonian||||||
20896|Yarrimie Formation|32584|6|Mentioned|p242|||||||||
20896|Yarrimie Formation|32619|6|Mentioned|p461|||Middle Devonian||||||
20896|Yarrimie Formation|32671|6|Mentioned|Map legend|Devonian|Devonian|||||||
20896|Yarrimie Formation|32865|6|Mentioned|p481|||Mid. Dev.||||||
20896|Yarrimie Formation|33392|6|Mentioned|p94|||Fauna.||||||
20896|Yarrimie Formation|34554|4|Described|p234|||||||||
20896|Yarrimie Formation|35062|6|Mentioned|p278|||||||||
20896|Yarrimie Formation|35761|5|Briefly described|p64|||Stratigraphy discussed. See also Table 1.||||||
20896|Yarrimie Formation|35783|6|Mentioned|Fig.1|||Mineral deposits and geology of Nundle gold field.||||||
20896|Yarrimie Formation|38207|6|Mentioned|p161|||||||||
20896|Yarrimie Formation|38802|4|Described|p113|||||||||
20896|Yarrimie Formation|39331|6|Mentioned|Table 10-1|||||||||
20896|Yarrimie Formation|40867|6|Mentioned|p55|||||||||
20896|Yarrimie Formation|41009|6|Mentioned|Fig.2|||||||||
20896|Yarrimie Formation|41347|5|Briefly described|p385|||||||||
20896|Yarrimie Formation|41348|5|Briefly described|Map legend|Devonian|Devonian|Of the tamworth Group.||||||16-DEC-04
20896|Yarrimie Formation|41796|6|Mentioned|p301|||||||||
20896|Yarrimie Formation|42229|5|Briefly described|p4|||||||||
20896|Yarrimie Formation|42554|5|Briefly described|p37|||||||||
20896|Yarrimie Formation|42629|5|Briefly described|p357|||||||||
20896|Yarrimie Formation|42796|5|Briefly described|Fig.2 P31|||||||||
20896|Yarrimie Formation|42866|5|Briefly described|Table 2, P12|||||||||
20896|Yarrimie Formation|43091|5|Briefly described|Map legend|||of Tamworth Group||||||
20896|Yarrimie Formation|43399|14|Not recorded|p204||Middle Devonian|||||||
20896|Yarrimie Formation|43400|2|Defined|p178,179-181,186,188||Givetian|(M.Devn)||||||
20896|Yarrimie Formation|43406|14|Not recorded|p41,42,45,47-50||Middle Devonian|Includes Levy Greywacke Member;Formation of Tamworth Group||||||
20896|Yarrimie Formation|43417|6|Mentioned|Map Legend|||Correlated with Timor Limestone and Lilberne Beds.||||||
20896|Yarrimie Formation|43428|14|Not recorded|p135,138|||||||||
20896|Yarrimie Formation|43479|14|Not recorded|p151||Middle Devonian|||||||
20896|Yarrimie Formation|43530|14|Not recorded|p1034|||||||||
20896|Yarrimie Formation|43785|6|Mentioned|p369||Middle Devonian|||||||
20896|Yarrimie Formation|47056|6|Mentioned|Fig.2 P523|||||||||
20896|Yarrimie Formation|50168|6|Mentioned|p157 Fig.2, p159, p162|Late Devonian||Well-preserved Upper Devonian (Frasnian) radiolarians have been recovered from in situ rocks of this unit. Gamilaroi Terrane.||||||06-FEB-18
20896|Yarrimie Formation|61392|5|Briefly described|p165 Fig. 2|Givetian|Eifelian|In the Gamilaroi terrane.||||||07-FEB-11
20896|Yarrimie Formation|61765|5|Briefly described|p58 Fig. 1, p60, p61, p62|Devonian|Devonian|Geological Province: Tamworth Belt.||||||07-FEB-11
20896|Yarrimie Formation|63118|5|Briefly described|p201, p202 Fig. 1|Middle Devonian|Middle Devonian|Includes Moore Creek Limestone Member. Contains coral fauna.||||||07-FEB-08
20896|Yarrimie Formation|65214|6|Mentioned|p278, p282|Devonian|Devonian|NSW, Nundle, Timor, Tamworth. Shows any correlations across Australia, and with South Africa, South America and East Greenland.||||||
20896|Yarrimie Formation|65940|6|Mentioned|p200|Eifelian|Eifelian|Contains stromatoporoid bioherms.|||Includes Moore Creek Limestone Member.|||
20896|Yarrimie Formation|66720|5|Briefly described|Map legend|Late Devonian|Early Devonian|||Unit in Tamworth Group.|Includes Moore Creek and Sulcor Limestone Members, and two un-named units mapped separately: interbedded lithic wacke and siliceous siltstone and sandy mudstone; massive to biohermal coral limestone.||Green-grey to black, siliceous, radiolarian siltstone and mudstone with local limestone lenses; minor volcaniclastic sandstone, tuff, lithic wacke and conglomerate.|
20896|Yarrimie Formation|68005|4|Described|p49 Fig.3-M, p52, p150, p170.|Givetian|Eifelian|Tamworth Belt. The article states that Sulcor and Loombrah Limestones are the same unit, having different names in the Attunga region (Sulcor Limestone) and Loombrah and Timor region (Loombrah Limestone). Mis-spelt as Yarrime Formation on p150.||Unit in Tamworth Group.|Includes Sulcor, Moore Creek, Crawney, Timor and Loombrah Limestone Members.|Overlies Silver Gully Formation. Is intruded by, and interbedded with, Folly Volcanics. Is overlain locally by Mostyn Vale Formation, Lowana Formation and Noumea beds.|Green, grey, black and white cherty argillites and fine mudstone; autochthonous and allochthonous limestone blocks; sparse lithic wacke beds.|
20896|Yarrimie Formation|73440|6|Mentioned|p132|||||||||
20898|Yarrowyck Granodiorite|721|5|Briefly described|Map legend|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.  Equigranular, medium-grained hornblende-biotite granodiorite and granite.||||||
20898|Yarrowyck Granodiorite|24366|5|Briefly described|p9 Fig. 7|Early Triassic|Late Permian|Of the Uralla Plutonic Suite.||||||
20898|Yarrowyck Granodiorite|30135|6|Mentioned|Map legend|Permian|Permian|||||||
20898|Yarrowyck Granodiorite|30787|6|Mentioned|p49|||Differentiation index||||||
20898|Yarrowyck Granodiorite|30789|6|Mentioned|Fig.1B|||Petrology & Geochemistry||||||
20898|Yarrowyck Granodiorite|30911|6|Mentioned|Map legend|Permian|Permian|||||||
20898|Yarrowyck Granodiorite|35257|6|Mentioned|Fig.15|||||||||
20898|Yarrowyck Granodiorite|38288|6|Mentioned|Fig.12|||||||||
20898|Yarrowyck Granodiorite|43091|5|Briefly described|Map legend|||||||||
20898|Yarrowyck Granodiorite|45087|5|Briefly described|p46|||Chemical analyses.||||||10-DEC-07
20898|Yarrowyck Granodiorite|68111|5|Briefly described|p968 Tb.1|Anisian|Olenekian||250 - 246 Ma, Rb-Sr (biotite) (Shaw 1994).|Of the Uralla Supersuite.||||
20898|Yarrowyck Granodiorite|69323|4|Described|p1,3,6-12,34,46,69,71, 76|Lopingian|Lopingian|Geological province: New England Orogen. Minor aplites and rare small pegmatite segregations occur in outcrop and small sparsely distributed mafic microgranular enclaves are also present. Phillips et al. (2011) obtained a 206Pb/238U age of 249+\-3 Ma, which is inconsistent with ages of other dated plutons in the region and mapped geological relationships. SHRIMP U-Pb zircon geochronology of GA 2129545 (hornblende-bearing granodiorite) yielded an interpreted (weighted mean 206Pb/238U age) magmatic crystallisation age of 254.9+\-1.5 Ma.|254.9+\-1.5 Ma (SHRIMP U-Pb, magmatic)|Unit of the Yarrowyck Suite||Intrudes into Balala Granodiorite. Intruded by Gwydir River Adamellite.|Medium-grained granodiorite that is intermediate-felsic in hand specimen.|03-DEC-19
20898|Yarrowyck Granodiorite|69639|5|Briefly described|p8, p32, p95, p133, p219|Changhsingian|Wuchiapingian|New England Orogen.|254.9 +/- 1.5 Ma (SHRIMP U-Pb)|Uralla Supersuite||||
20898|Yarrowyck Granodiorite|70217|5|Briefly described|p74 tbl 14.1|Olenekian|Wuchiapingian|New England Orogen. An age of 254.9 +/- 1.5 Ma is given by SHRIMP U-Pb from Chisholm et al, 2014a.|249 +/- 3 Ma (LA-ICPMS, Phillips et al, 2011)|||||
20898|Yarrowyck Granodiorite|71628|4|Described|p8: 4, 8, 28-29, 72, 113-119; p19-1|||Binns et al. (1967) after unpublished work by Ransley (1970). Forms a large pluton extending almost 20km NNE from Balala to NE of Yarrowyck. Forms low undulating country, cropping out as small boulders and large rock platforms. Dykes in the unit form more prominent outcrops. Unassigned to a Suite. Is said (p8-28) to be intruded by Gwydir River Monzogranite. Previous age determinations give slightly younger ages. Lithology described in great detail. Geochemistry described.|254.9 +/- 1.6 Ma (SHRIMP: Chisholm et al., 2014).|Yarrowyck Suite.||Intrudes Blackfellows Gully Leucomonzogranite, Balala Granodiorite, Gwydir River Monzogranite(?) and Sandon beds. Is intruded by Uralla Granodiorite, Wongalee Leucogranite.|Weakly zoned, from medium-grained biotite-hornblende-(pyroxene) granodiorite to fine-grained, leucocratic monzogranite. I-type.|
20902|Yarwood Siltstone Member|22857|5|Briefly described|p458 App.1, Tb.A1.6|Late Silurian|Late Silurian|Of the Booroo Ponds Group. Calcareous siltstone, shaly mudstone. Max. thickness: 33.5m. Geological Province: Canberra-Yass Shelf.||||||
20902|Yarwood Siltstone Member|24019|6|Mentioned|p362|Ludlow|Ludlow|||||||
20902|Yarwood Siltstone Member|24248|5|Briefly described|p51, p67|Ludfordian|Ludfordian|Parent: Black Bog Shale. Geological Province: Yass Syncline.||||||
20902|Yarwood Siltstone Member|30069|6|Mentioned|p5|||Also Table 5||||||
20902|Yarwood Siltstone Member|31852|5|Briefly described|p711|||U.Sil. See also P714,715, Figs. 1,2,4,5.||||||
20902|Yarwood Siltstone Member|32155|6|Mentioned|p186|||See also Fig. 1||||||
20902|Yarwood Siltstone Member|33116|6|Mentioned|Fig.11|||Correlation. Mb. Bog Shale.||||||
20902|Yarwood Siltstone Member|35244|6|Mentioned|p36|||||||||
20902|Yarwood Siltstone Member|35386|3|Fully described|p35|||||||||
20902|Yarwood Siltstone Member|36411|6|Mentioned|p270|||Refers Cramsie et al 1978 for definition||||||
20902|Yarwood Siltstone Member|37013|6|Mentioned|p24|||||||||
20902|Yarwood Siltstone Member|37727|6|Mentioned|p8|||||||||
20902|Yarwood Siltstone Member|38378|6|Mentioned|p142|||||||||
20902|Yarwood Siltstone Member|39331|6|Mentioned|Fig.5-5|||||||||
20902|Yarwood Siltstone Member|39975|6|Mentioned|p128|||||||||
20902|Yarwood Siltstone Member|40328|4|Described|p52|||Also mentioned on P21||||||
20902|Yarwood Siltstone Member|42994|6|Mentioned|p72|||of Black Bog Shale||||||
20902|Yarwood Siltstone Member|45075|5|Briefly described|p7|||Fauna||||||
20902|Yarwood Siltstone Member|50230|4|Described|Map legend|Ludlow|Ludlow|Of the Black Bog Shale (Hattons Corner Group).  Lies between upper and lower unnamed shale members of the Black Bog Formation.  Formerly known as the "Lower Trilobite bed".  Fossiliferous mudstone, shale, siltstone.||||||
20902|Yarwood Siltstone Member|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Black Bog Shale (Hattons Corner Group). Formerly the "Lower Trilobite bed".  Fossiliferous mudstone, shale and siltstone.||||||12-JUN-08
20902|Yarwood Siltstone Member|67651|5|Briefly described|p422|||Of Yass Basin. Contains trolobite assemblages (see p10) ascribed to Wenlock to Ludlow age.||Unit of Black Bog Shale.||||
20902|Yarwood Siltstone Member|68592|2|Defined|p430 Fig.89, p560, p562, p584-9, p1881-3|Ludfordian|Ludfordian|Named after Yarwood property. Formerly called the Lower Trilobite Bed. Link (1970, 1971), included this unit as a Member in Black Bog Shale; further described by Cramsie et al. (1978). Type locality described. 5-33.5m thick. Distinctive lateral variation in lithology. Slaty cleavage common. Rich fossil fauna listed.||Unit in Black Bog Shale.|||Thin but persistent calcareous mudstone or siltstone horizon with rare lenses or pods of micritic limestone; a rich brachiopod-trilobite-coral fauna.|
20902|Yarwood Siltstone Member|70192|5|Briefly described|Map Legend|Ludlow|Ludlow|Shby. [Previously known as] "Lower Trilobite Bed". On Yass 1:100 000 mapsheet portion of Time-Space Plot.||Black Bog Shale|||Fossiliferous, calcareous mudstone or siltstone.|
20902|Yarwood Siltstone Member|70540|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Lower Trilobite Bed".||Black Bog Shale|||Fossiliferous, calcareous mudstone or siltstone.|
20902|Yarwood Siltstone Member|70546|5|Briefly described|Map Legend|Devonian|Silurian|[Previously known as] "Lower Trilobite Bed".||Black Bog Shale|||Fossiliferous calcareous mudstone or siltstone ("lower trilobite bed")|
20902|Yarwood Siltstone Member|71656|4|Described|p12 Fig.2, p19, p24-27, p31|Ludlow|Ludlow|Initally called the 'Lower Trilobite Bed'. Diverse record of brachiopods, corals and bryozoa.||Of Black Bog Shale.|||Fossiliferous siltstone.|
20902|Yarwood Siltstone Member|71657|6|Mentioned|p39-40|||Contains the brachiopod Apopentamerus clarkei.||Black Bog Shale||||
20908|Yass Formation|22486|5|Briefly described|p 5||Ludlovian|||||||
20908|Yass Formation|22768|6|Mentioned|p176|||||||||
20908|Yass Formation|22857|4|Described|p176, p460 App.1 Tb.A1.6|Late Silurian|Late Silurian|Sequence of shelfal sediments including limestone. Underlies Laidlaw and Deakin Volcanics. Overlies Hawkins Suite. Max. thickness: 320m. See also p462 App.1 Tb. A1.6.||||||26-FEB-10
20908|Yass Formation|24248|5|Briefly described|p51, p52, p50 Fig.1|Late Silurian|Late Silurian|Overlying Unit: Laidlaw Volcanics. Underlying Unit: Hawkins Volcanics. Geological Province: Yass Syncline.||||||
20908|Yass Formation|36441|5|Briefly described|map legend|Ludlovian|Ludlovian|Interbedded shale and siltstone. Underlies Laidlaw Volcanics. BMR map code: Suy.||||||
20908|Yass Formation|37728|6|Mentioned|Table 4|||||||||
20908|Yass Formation|37752|6|Mentioned|p105|||||||||
20908|Yass Formation|38035|6|Mentioned|p90|||||||||
20908|Yass Formation|39975|6|Mentioned|p124|||||||||
20908|Yass Formation|42727|5|Briefly described|map legend|Ludlow|Ludlow|Calcareous and tuffaceous shale, sandstone, ashstone and limestone. BMR map symbol: Sy. Geol. Prov: Canberra Block.||||||23-AUG-12
20908|Yass Formation|42820|2|Defined|p29|early Ludlow||Of Laidlaw Volcanic Suite. Age early Late Silurian (earliest Ludlow).||||||22-MAY-08
20908|Yass Formation|42994|6|Mentioned|p73|||Of Douro Group.||||||20-MAY-08
20908|Yass Formation|43479|14|Not recorded|p103|||||||||
20908|Yass Formation|44093|5|Briefly described|p196 App. 1|Devonian|Silurian|Geological Province: Lachlan Fold Belt.||||||
20908|Yass Formation|45147|3|Fully described|M123|||||||||
20908|Yass Formation|47037|6|Mentioned|p107|||||||||
20908|Yass Formation|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Of the Douro Group. Fine-grained tuffaceous sandstone and siltstone. Overlies the Hawkins Volcanics.||||||05-SEP-07
20908|Yass Formation|50231|5|Briefly described|Map Legend|Ludlow|Wenlock|Of the Douro Group.||||||
20908|Yass Formation|64238|5|Briefly described|Map legend|Silurian|Silurian|Of Douro Gp. Includes O'Briens Creek Sandstone and Cliftonwood Limestone Members. Grey to olive laminated mudstone, siltstone and shale interbedded with quartzose to quartzofeldspathic sandstone; rare limestone.||||||
20908|Yass Formation|66197|5|Briefly described|p631 Fig.3b|Wenlock||Canberra-Yass Basin. Shallow marine, subaerial clastics. Underlies the Laidlaw Volcanics, overlies the Hawkins Volcanics. Age: ?late Wenlock.||||||14-MAR-12
20908|Yass Formation|68592|2|Defined|p454, p497-502, p504, p515-516, p520|Wenlock|Wenlock|See also p269, p428, p430 Fig.89, p431, p433-435, p437, p440-441, p1875-1876. Owen and Wyborn (1979). Originally Yass Beds (Jenkins, 1879); later Yass Series (Brown, 1940), then Yass Member (of Douro Volcanics) by Brunker and Offenberg (1970). Next raised to Group [!] status by Link (1970, 1971), Link and Druce (1972); subsequently reduced to Sub-Group status by Pogson and Baker (1974), then to Formation status by Owen and Wyborn (1979). Composite type section described. Thickness to 400m. Contains a diverse fossil fauna. Mid-Wenlock.||Unit in Douro Group.|Includes O'Briens Creek Sandstone Member and Cliftonwood Limestone Member.|Conformably overlies Hawkins Volcanics. Is faulted over Mountain Creek Volcanics. Is overlain conformably by Laidlaw Volcanics. Correlates with Glen Bower and Boambolo Formations.|Quartzose and quartzo-feldspathic sandstone and mudstone, overlain by well-bedded fossiliferous limestone and calcareous mudstone.|
20908|Yass Formation|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Sdy. On Boorowa and Yass 1:100 000 mapsheet portions of Time-Space Plot. Related units inferred from Time-Space Plot.||Douro Group||Overlies Hawkins Volcanics. Is overlain by Laidlaw Volcanics.|Quartzose to quartzofeldspathic sandstone and laminated mudstone (some calcareous), siltstone and shale; rare fossiliferous limestone.|
20908|Yass Formation|70540|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|Includes Cliftonwood Limestone Member, O'Briens Creek Sandstone Member.||Quartzose-quartzofeldspathic sandstone and laminated mudstone (some which is calcareous), siltstone and shale. Rare fossiliferous limestone also present.|
20908|Yass Formation|70545|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|||Quartzose to quartzofeldspathic sandstone and laminated mudstone (some calcareous), siltstone and shale; rare fossiliferous limestone.|
20908|Yass Formation|70546|5|Briefly described|Map Legend|Silurian|Silurian|||Douro Group|Includes Cliftonwood Limestone Member, O'Briens Creek Sandstone Member||Quartzose to quartzofeldspathic sandstone and laminated mudstone (some calcareous), siltstone and shale; rare fossiliferous limestone.|
20908|Yass Formation|71656|5|Briefly described|p12 Fig.2, p19, p22|Wenlock|Wenlock|Most fossils described from the Yass Formation have come from the Cliftonwood Limestone Member.||Douro Group|Includes Cliftonwood Limestone Member at top.|Overlies and partially equivalent to Glen Bower Formation.|Undifferentiated unit partially containing fossils from the Cliftonwood Limestone Member.|
20908|Yass Formation|71657|6|Mentioned|p48|Silurian|Silurian|Contains the brachiopod Spirinella caecistriata.|||Cliftonwood Limestone Member|||
20908|Yass Formation|73215|5|Briefly described|p993-994, 1002-1003|||Yass Syncline.||Douro Group||Overlies Hawkins Volcanics. Is overlain by Laidlaw Volcanics. May be equivalent to Talmo Formation.||
20920|Yathong Formation|29987|5|Briefly described|p24|||||||||
20920|Yathong Formation|34057|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20920|Yathong Formation|34469|6|Mentioned|p107|||Upper Devonian. Table||||||
20920|Yathong Formation|35163|6|Mentioned|Map legend|Late Devonian|Late Devonian|||||||
20920|Yathong Formation|42467|5|Briefly described|Map Legend|||||||||
20920|Yathong Formation|43032|5|Briefly described|Table 1.|||of Mulga Downs Group||||||
20920|Yathong Formation|43380|14|Not recorded|Map Legend||Late Devonian|Unit of Mulga Downs Group||||||
20920|Yathong Formation|43381|14|Not recorded|Map Legend|||Mulga Downs Group||||||
20920|Yathong Formation|43389|14|Not recorded|Map Legend||Late Devonian|||||||
20920|Yathong Formation|43398|14|Not recorded|Map Legend||Late Devonian|Part of Mulga Downs Group||||||
20939|Yellow Mountain Granite|22508|6|Mentioned|p2||Early Devonian|Keotong Supersuite, Lachlan Fold Belt||||||
20939|Yellow Mountain Granite|32674|6|Mentioned|p31|||||||||
20939|Yellow Mountain Granite|33004|6|Mentioned|p173|||||||||
20939|Yellow Mountain Granite|34449|6|Mentioned|Table 2-1|||||||||
20939|Yellow Mountain Granite|35287|5|Briefly described|p3|||||||||
20939|Yellow Mountain Granite|40328|4|Described|p213|||||||||
20939|Yellow Mountain Granite|41821|6|Mentioned|p11 Fig.5|||Occurs in Bobadah sheet area||||||
20939|Yellow Mountain Granite|42566|3|Fully described|p91|||||||||
20939|Yellow Mountain Granite|42568|5|Briefly described|Map legend|Lochkovian|Lochkovian|||||||
20939|Yellow Mountain Granite|43089|5|Briefly described|Map Legend|||||||||
20939|Yellow Mountain Granite|43263|6|Mentioned|Map Legend||Early Devonian|||||||
20939|Yellow Mountain Granite|43757|6|Mentioned|p510|||||||||
20939|Yellow Mountain Granite|67416|6|Mentioned|p84-85|||Temporally and chemically related to volcanics in the Canbelego-Mineral Hill Volcanic Belt.||||||
20939|Yellow Mountain Granite|70751|6|Mentioned|p8, p12|Silurian|Silurian||420.6 +/- 2.8 Ma (SHRIMP, Black, 2007)|||||
20939|Yellow Mountain Granite|70876|5|Briefly described|p76|Devonian|Silurian|Lachlan Orogen.|420.6 +/- 2.8 Ma (Black, 2007)|||||
20939|Yellow Mountain Granite|70950|6|Mentioned|p1044|||||||In contact with Majuba Volcanics.||
20939|Yellow Mountain Granite|71039|5|Briefly described|p11-p12, p26|Devonian|Silurian|Contact metamorphoses the Majuba Volcanics of the Kopyje Group.||||Intrudes the Majuba Volcanics (Kopyje Group).||
20939|Yellow Mountain Granite|71693|5|Briefly described|Map legend.|Devonian|Devonian||||||I-type. Foliated, medium-grained, equigranular and porphyritic biotite granite; mylonite zones common. Associated scattered porphyritic biotite micromonzogranite dykes intrude the granite margins.|
20939|Yellow Mountain Granite|72908|6|Mentioned|p24|Ordovician|Ordovician|||||||
20939|Yellow Mountain Granite|72951|5|Briefly described|p1013, 1017, 1022|Lochkovian|Ludlow|Lachlan Orogen. Hermidale Terrane. I-type. SHRIMP U-Pb zircon isotope analyses from Black (2007). eHf = -3.4 +/- 1.4, and d18O = 7.08 +/- 0.69.|420.6 +/- 2.8 Ma||||Granite.|
20939|Yellow Mountain Granite|72958|6|Mentioned|p11|Pridoli|Pridoli|Cobar Basin. Nymagee area.||||Intrudes[?] Majuba Volcanics.||
20979|Yewrangara Granite|42726|5|Briefly described|map legend|Middle Devonian||||||||
20979|Yewrangara Granite|50233|5|Briefly described|Map Legend|Pridoli|Ludlow|Of the Wyangala Batholith. Leucogranitic massive equigranular hornblende-biotite granite.||||||
20979|Yewrangara Granite|64238|5|Briefly described|Map legend|Devonian|Devonian|Of the Yewrangara Suite. Cream to creamy-grey, medium- to occasionally coarse-grained, generally massive, equigranular to weakly porphyritic hornblende-biotite granite. Contains sub-unit of mottled black/cream medium-grained, equigran., biotite graniite||||||09-SEP-08
20979|Yewrangara Granite|68592|2|Defined|p84,p276,p292,p324,p1358, p1482, p1535-8|Early Devonian|Early Devonian|These rocks were included in the Wyangala Batholith by Stevens (1955) and in the Bigga Granite by Hasan (1957). First recognised separately and named (after Yewrangara property) by Yacopetti (1987); published by Chappell et al. (1991). Type pluton for the felsic component of Keverstone Supersuite. Type area described. Geochemistry and geophysical properties described. Hosts Reids Flat Tin Prospect; has provided sources of local road materials.||Unit in Yewrangara Suite.||Intrudes Adaminaby and Bendoc Groups; Bigga and Sentry Box Granites and Goonoonglah Monzodiorite.|Cream to creamy-grey, medium- to sporadically coarse-grained, generally massive, equigranular to weakly porphyritic hornblende-biotite granite with a core of biotite granite; metasedimentary xenoliths and large diorite blocks locally common. A-type.|
20979|Yewrangara Granite|70192|5|Briefly described|Map Legend|Emsian|Emsian|Duy. Includes one unnamed subunit of medium grained, equigranular, biotite granite, with high K, Th and U response, moderate magnetic susceptibility. On Crookwell 1:100 000 mapsheet portion of Time-Space Plot.||Yewrangara Suite|Includes one unnamed subunit.||Medium-coarse grained, generally massive, equigranular to weakly porphyritic hornblende-biotite granite. High K, low to moderate Th and U response; low magnetic susceptibility.|
20979|Yewrangara Granite|70544|5|Briefly described|Map Legend|Devonian|Devonian|Includes one unnamed subunit of medium grained, equigranular, biotite granite.||Yewrangara Suite|Includes one unnamed subunit||Medium-coarse grained, generally massive, equigranular to weakly porphyritic hornblende-biotite granite. High K, low to moderate Th and U response; low magnetic susceptibility.|
20979|Yewrangara Granite|71069|6|Mentioned|p74|||||||||
20979|Yewrangara Granite|71206|6|Mentioned|p373, 377, 379-381, 384|||Lachlan Fold Belt. Chemical data and Zr saturation temperatures tabulated. Geochemistry discussed; graphs.||Yewrangara Suite.|||Fractionated, aluminous A-type granite.|
21021|Young Granodiorite|22638|1|Redefined|p57|Pridolian|Wenlockian|417 +/- 6 Ma on biotite. Previously "Young Granite".||||||12-JUN-08
21021|Young Granodiorite|22687|6|Mentioned|109|||||||||
21021|Young Granodiorite|22691|6|Mentioned|Fig7 p319||Silurian|||||||
21021|Young Granodiorite|22768|6|Mentioned|p155|||||||||
21021|Young Granodiorite|22857|6|Mentioned|p155||Silurian|||||||
21021|Young Granodiorite|23087|5|Briefly described|p655 (Fig 1)||Late Silurian|||||||
21021|Young Granodiorite|23214|3|Fully described|p168|Late Silurian|Early Silurian|Formerly included in the Cowra Granodiorite. Parts of the unit formerly included in Burrinjuck Granite Complex. Intrudes Douro Group and Goobarragandra Volcanics. Probably intrudes the Canowindra Volcanics and may be intruded by Broula Granite.||||||27-JAN-23
21021|Young Granodiorite|23366|5|Briefly described|p12, p13 fig.8|Silurian|Silurian|||||||22-FEB-05
21021|Young Granodiorite|24215|5|Briefly described|p801|Early Silurian|Early Silurian|Geological Province:  Lachlan Fold Belt||||||
21021|Young Granodiorite|24417|3|Fully described|p56|Silurian|Silurian|Previously called "Young Granite" (Adamson, 1960).  Possibly intrudes Illunie Volcanics.||||||
21021|Young Granodiorite|29449|6|Mentioned|p219|||||||||
21021|Young Granodiorite|29452|6|Mentioned|p215|||||||||
21021|Young Granodiorite|29453|4|Described|p25|||||||||
21021|Young Granodiorite|29682|4|Described|p13|||||||||
21021|Young Granodiorite|29902|6|Mentioned|p4|||||||||
21021|Young Granodiorite|29907|6|Mentioned|p8|||||||||
21021|Young Granodiorite|29908|6|Mentioned|p269|||||||||
21021|Young Granodiorite|29910|6|Mentioned|Map legend|Silurian|Silurian|||||||
21021|Young Granodiorite|30172|6|Mentioned|p43|||||||||
21021|Young Granodiorite|30510|6|Mentioned|p117|||||||||
21021|Young Granodiorite|30734|6|Mentioned|p18|||||||||
21021|Young Granodiorite|31019|6|Mentioned|Map legend|Devonian|Silurian|Silurian - Devonian||||||
21021|Young Granodiorite|31448|6|Mentioned|p19|||||||||
21021|Young Granodiorite|33004|6|Mentioned|p175|||||||||
21021|Young Granodiorite|33285|6|Mentioned|p21|||||||||
21021|Young Granodiorite|33480|6|Mentioned|p243|||Refers age dating||||||
21021|Young Granodiorite|34907|6|Mentioned|p294|||||||||
21021|Young Granodiorite|35070|2|Defined|p84|Early Devonian|Late Silurian|Late Silurian to Early Devonian.||||||12-JUN-08
21021|Young Granodiorite|35185|6|Mentioned|p232|||||||||
21021|Young Granodiorite|35206|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
21021|Young Granodiorite|35257|6|Mentioned|p152|||||||||
21021|Young Granodiorite|35384|6|Mentioned|Map legend|Early Devonian|Late Silurian|||||||
21021|Young Granodiorite|35386|3|Fully described|p59|||||||||
21021|Young Granodiorite|35522|6|Mentioned|Fig.2|||Schematic geological sections through the Coolac ophiolite suite.||||||
21021|Young Granodiorite|35607|6|Mentioned|p65|||See also P70,71,72,73,74,76,77,78,79,114-120,122,123.||||||
21021|Young Granodiorite|35608|6|Mentioned|Map legend|Early Devonian|Middle Silurian|Middle Silurian to Early Devonian||||||
21021|Young Granodiorite|35609|4|Described|p16|||||||||
21021|Young Granodiorite|36051|6|Mentioned|p411|||||||||
21021|Young Granodiorite|36411|6|Mentioned|p270|||Refers Basden et al 1978 for definition.||||||
21021|Young Granodiorite|37150|6|Mentioned|Fig.8|||||||||
21021|Young Granodiorite|37529|5|Briefly described|p5|||||||||
21021|Young Granodiorite|37544|6|Mentioned|p493|||||||||
21021|Young Granodiorite|39331|6|Mentioned|Fig.4-3|||See P36||||||
21021|Young Granodiorite|39627|6|Mentioned|Appendix|||||||||
21021|Young Granodiorite|40328|4|Described|p213|||||||||
21021|Young Granodiorite|40497|6|Mentioned|Map legend|Paleozoic|Paleozoic|||||||07-NOV-08
21021|Young Granodiorite|40498|6|Mentioned|p180|||||||||
21021|Young Granodiorite|40762|6|Mentioned|Fig.18|||||||||
21021|Young Granodiorite|41594|6|Mentioned|p52|||||||||
21021|Young Granodiorite|41798|6|Mentioned|Fig.2|||||||||
21021|Young Granodiorite|42045|6|Mentioned|p147|||||||||
21021|Young Granodiorite|42145|4|Described|Table 1 P624|||||||||
21021|Young Granodiorite|42313|3|Fully described|p135|Late Silurian||||||||
21021|Young Granodiorite|42314|5|Briefly described|Map|Late Silurian||||||||
21021|Young Granodiorite|42828|5|Briefly described|Table 1 P129|Late Silurian||||||||
21021|Young Granodiorite|42837|6|Mentioned|p366|||||||||
21021|Young Granodiorite|43782|5|Briefly described|Map Legend|Pridoli|Ludlow|||||||
21021|Young Granodiorite|44092|5|Briefly described|map legend|Silurian|Silurian|ggb8.||||||
21021|Young Granodiorite|44093|5|Briefly described|p94 (photo), p117|Late Silurian|Late Silurian|Geological Province: Tasman Fold Belt.||||||
21021|Young Granodiorite|44936|5|Briefly described|Map Legend||Silurian|||||||
21021|Young Granodiorite|45147|6|Mentioned|M233|||||||||
21021|Young Granodiorite|50191|5|Briefly described|p6, 18|Silurian|Silurian|S type.  Intruded the Coolac Serpentinite and Goobarragandra Volcanics.  Geological Province: Tumut Trough.||||||02-AUG-04
21021|Young Granodiorite|50230|5|Briefly described|Map legend|Wenlock|Wenlock|Part of the Young Batholith.  Muscovite-cordierite-biotite granite and granodiorite.||||||
21021|Young Granodiorite|50231|5|Briefly described|Map Legend|Ludlow|Wenlock|Part of the Young Batholith.||||||
21021|Young Granodiorite|50628|5|Briefly described|Map Legend|Silurian|Silurian|Fine to medium grained, biotite granodiorite.||||||05-JUL-04
21021|Young Granodiorite|60009|5|Briefly described|Map Legend|Ludlow|Wenlock|||||||13-JUL-04
21021|Young Granodiorite|60078|6|Mentioned|Map Legend|Silurian|Silurian|||||||
21021|Young Granodiorite|63290|6|Mentioned|p406 Fig. 7|||||||||
21021|Young Granodiorite|64238|5|Briefly described|Map legend|Silurian|Silurian|Part of the Young Suite. Cream to grey, medium- to coarse-grained, generally massive, equigranular muscovite+/-cordierite?-biotite granite+granodiorite, occasionally with abundant biotite-rich microgranitic enclaves+quartz xenoliths; minor ...||||||09-SEP-08
21021|Young Granodiorite|66197|5|Briefly described|p632|Wenlock|Llandovery|Zircon U-Pb date of 428 +/- 2 Ma. Intrudes ophiolitic rocks.||||||14-MAR-12
21021|Young Granodiorite|67127|6|Mentioned|p173|Silurian|Silurian|Interpreted to have played a major role in the formation of mineralised laterites.||||||
21021|Young Granodiorite|68592|2|Defined|p1219, p1225-7, p1229-30, p1239-40,p1246|Sheinwoodian|Telychian|See also p73, p269, p271, p442-3, p446, p451, p454, p520, p988. Originally the Young Granite of Adamson (in Booker et al. 1960). Best et al. (1964) included some southern parts in their Burrinjuck Granite; Adamson and Loudon (1966) included the southern part in their Burrinjuck Granite Complex. Ashley and Basden (1973) and Basden et al. (1978) separated the widespread grey biotite granodiorite mass as their Young Granodiorite, including the Cowra Granodiorite (described by Stevens 1951, 1952); this latter pluton is now regarded as a separate body (Chappell et al., 1991; Pogson and Watkins, 1998). Includes the Murringo Granite of Chappell et al. (1991). A very large elongate intrusion: c.3640 km2. Type area and several good exposures are described. Five minor phases mapped separately. Contains numerous strongly foliated zones. Geochemistry and geophysical properties described. Associated with three Pb-Zn-Ag-Cu skarn occurrences within Goobarragandra Volcanics, 5km S of Mount Bobbara. SHRIMP zircon U-Pb isotopic age. Co-magmatic with Goobarragandra Volcanics. Gradational boundary between sheeted dykes and the Hawkins Volcanics. Contains numerous strongly foliated zones. Hosts Au-bearing quartz veins which have been mined at various localities in the past. Binalong structural zone: deformation described.|428.8 +/- 1.9 Ma (Black, in Lyons et al. 2000).|Unit in Young Suite.||Intrudes Goobarragandra Volcanics, Micalong Suite and Hawkins Volcanics. Is overlain nonconformably by Hervey Group. Faulted against Mountain Creek Volcanics. Is intruded by Karoopa Granite.|Cream to grey, medium- to coarse-grained, massive, muscovite +/- cordierite?-biotite granite and granodiorite; abundant biotite rich enclaves and xenoliths of vein quartz. Minor rhyolite dykes, porphyritic rhyolite, leucogranite and trachyte. S-type.|
21021|Young Granodiorite|69801|6|Mentioned|p2, p137|Middle Silurian|Middle Silurian|Central Lachlan Orogen. Dated sample has the SampleID of 98844508.|428.8 +/- 1.9 Ma (Geoscience Australia)||||S-type granodiorite.|
21021|Young Granodiorite|70192|5|Briefly described|Map Legend|Wenlock|Wenlock|Syy. Includes five unnamed subunits consisting of: haematite-magnetite rock; leucocratic granite; quartz feldspar biotite rhyolite stock; cordierite-biotite granodiorite; and, leucocratic quartz-K feldspar porphyritic trachyte. On Boorowa and Yass 1:100 000 mapsheet portions of Time-Space Plot.||Young Suite|Includes five unnamed subunits.||Medium-coarse grained, massive, equigranular, muscovite-cordierite-biotite granite and granodiorite; locally with abundant biotite-rich microgranitic enclaves and quartz xenoliths; minor porphyritic biotite microgranite.|
21021|Young Granodiorite|70297|5|Briefly described|map legend|Silurian|Silurian|||Bullenbalong Supersuite||||
21021|Young Granodiorite|70540|5|Briefly described|Map Legend|Silurian|Silurian|Includes one unnamed member of fine grained, equigranular leucocratic granite.||Young Suite|||Medium-coarse grained, massive, equigranular, muscovite-cordierite?-biotite granite and granodiorite; locally with abundant biotite-rich microgranitic enclaves and quartz xenoliths; minor porphyritic biotite microgranite.|26-AUG-16
21021|Young Granodiorite|70545|5|Briefly described|Map Legend|Silurian|Silurian|Includes four unnamed subunits consisting of: haematite-magnetite rock, quartz feldspar biotite rhyolite stock, cordierite-biotite granodiorite and leucocratic quartz-K feldspar porphyritic trachyte.||Young Suite|||Medium-coarse grained, massive, equigranular, muscovite-cordierite-biotite granite and granodiorite; locally with abundant biotite-rich microgranitic enclaves and quartz xenoliths; minor porphyritic biotite microgranite.|20-SEP-17
21021|Young Granodiorite|71708|5|Briefly described|p335, p337, p336 Fig 1, p348, 350|Wenlock|Wenlock|Said to either intrude (Stuart-Smith, 1990), or be faulted against  (Basden, 1978, 1990) Coolac Serpentinite. Possibly both.|428 +/- 3 Ma U-Pb SHRIMP intrusion|||Likely provenance of zircons within intrusions of the Coolac Serpentinite.||
21021|Young Granodiorite|72495|6|Mentioned|p228|Silurian|Silurian|||||Faulted against the Jindalee Group.||
21021|Young Granodiorite|73215|5|Briefly described|p994, 1002|||Talmo-Taemas area.|429 +/- 2 Ma (Lyons and Percival, 2002).|||Intrudes Goobarragandra Volcanics and Hawkins Volcanics.||
21021|Young Granodiorite|73483|5|Briefly described|p407-409, p413|Late Silurian|Late Silurian|S-type. Faulted against Wambidgee Serpentinite Belt in the Fontenoy area. Intrusive and locally mylonitic contacts with Coolac Serpentinite Belt. A 417+/-6 Ma biotite K-Ar age (Basden, 1990; Evernden and Richards, 1962) was superseded by a 428+/-1.9 Ma (U-Pb zircon SHRIMP) and 428+/-3 Ma (LA-ICPMS U-Pb) age.|428+/-1.9 Ma U-Pb SHRIMP, 428+/-3 Ma LA-ICPMS U-Pb|||Faulted against 'Fontenoy Serpentinite'|Mylonitised in part.|
21022|Young Wallsend Coal|39292|6|Mentioned|p108|||||||||
21022|Young Wallsend Coal|39308|6|Mentioned|p470|||Treestumps in roof||||||
21022|Young Wallsend Coal|39609|5|Briefly described|p4|||||||||
21022|Young Wallsend Coal|40516|6|Mentioned|p395|||||||||
21022|Young Wallsend Coal|68711|6|Mentioned|p116 Tbl 2|||This Formation has been downgraded to the informal Young Wallsend coal seam instead. The Young Wallsend Coal/seam is said to be the combination of Nobbys and Dudley Coal/seams.[???]. See also p113.||Of Lambton Subgroup||||
21033|Yowahro Formation|22772|5|Briefly described|Table13.1|Neoproterozoic III|Neoproterozoic III|||||||
21033|Yowahro Formation|22857|4|Described|p400 App. 1 Tb.A1.3.|Neoproterozoic|Neoproterozoic|Of the Eurowie Subgroup (Torrownagee Group). Calcareous sandstone, finely laminated; siltstone and sandstone. Age: <700Ma.||||||
21033|Yowahro Formation|30261|4|Described|Table 1|||Marinoan age.||||||
21033|Yowahro Formation|34812|3|Fully described|p86|||||||||
21033|Yowahro Formation|35199|6|Mentioned|Map legend|Adelaidean|Adelaidean|||||||
21033|Yowahro Formation|36411|6|Mentioned|p270|||Refs Cooper et al. 1978 for definition.||||||
21033|Yowahro Formation|36733|6|Mentioned|Table 5|||||||||
21033|Yowahro Formation|37931|4|Described|p532|||||||||
21033|Yowahro Formation|39214|6|Mentioned|Table 1|||||||||
21033|Yowahro Formation|41405|5|Briefly described|p204|||||||||
21033|Yowahro Formation|70000|6|Mentioned|p34|Neoproterozoic|Neoproterozoic|||Unit in Euriowie Subgroup.||||
21033|Yowahro Formation|70015|5|Briefly described|Map legend|Cryogenian|Cryogenian|Mineral deposits (if any) are shown.||Unit in Euriowie Subgroup.||Overlies Tanyarto Formation. Is overlain by Alberta Conglomerate.|Buff, flaggy, silty to sandy limestone grading into laminated siltstone with minor limestone; thin, calcareous sandy interbeds common.|08-SEP-15
21076|Zanci Unit|29643|5|Briefly described|p47|||||||||
